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
55|Abner Sandstone|22538|6|Mentioned|Fig3 P708|||||||||
55|Abner Sandstone|22853|6|Mentioned|27|Proterozoic|Proterozoic|Of the Roper Group. Overlain by Corcoran Formation.||||||08-FEB-07
55|Abner Sandstone|23216|5|Briefly described|Table1p8,34|||||||||
55|Abner Sandstone|23776|5|Briefly described|p711|||Of Roper Group.||||||
55|Abner Sandstone|23937|5|Briefly described|p38, p26 Fig. 12|Calymmian|Calymmian|Of Roper Group.  Name now restricted to undifferentiated succession of sandstone in the Abner Range.  Former units Arnold Sst. Mbr, Jalboi Mbr. and Hodgson Sst. Mbr. are assigned to Collara Subgroup; Munyi Member to Corcoran Fm. Geol.Prov: McArthur Basin.||||||20-OCT-04
55|Abner Sandstone|24047|6|Mentioned|p27|||||||||
55|Abner Sandstone|24050|5|Briefly described|p47|||Of the Roper Group.||||||08-FEB-07
55|Abner Sandstone|37568|6|Mentioned|Fig.6|||||||||
55|Abner Sandstone|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
55|Abner Sandstone|40691|4|Described|Fig.46|||Mention p64.||||||08-FEB-07
55|Abner Sandstone|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
55|Abner Sandstone|41268|6|Mentioned|p291|||||||||
55|Abner Sandstone|41406|6|Mentioned|Map legend|Mesoproterozoic||||||||
55|Abner Sandstone|41531|6|Mentioned|p167|||||||||
55|Abner Sandstone|42385|5|Briefly described|p27|||||||||
55|Abner Sandstone|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
55|Abner Sandstone|42597|5|Briefly described|Map Legend|Adelaidean||||||||
55|Abner Sandstone|42638|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Age: Middle Proterozoic.||Lower Roper Group (Roper Group).|Hodgson Sandstone Member, Jalboi Member and Arnold Sandstone Member.|In schematic section, underlies Corcoran Formation; overlies Crawford Formation.|Detailed lithology given for constituents.|07-NOV-11
55|Abner Sandstone|42639|5|Briefly described|p41, Table 7 p39|||||||||
55|Abner Sandstone|42700|5|Briefly described|map legend|Mesozoic|Early Cretaceous|||||||
55|Abner Sandstone|42739|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Of the Lower Roper Group. Includes Hodgson Sandstone Member, Jalboi Member, Arnold Sandstone Member.||||||19-OCT-05
55|Abner Sandstone|42812|4|Described|p52, Table 5|||Of Roper Group.||||||08-FEB-07
55|Abner Sandstone|42846|5|Briefly described|Fig.1 p502|||Of Roper Group. Geological Province: McArthur Basin.||||||08-FEB-07
55|Abner Sandstone|43010|4|Described|Table 30.|||Of Roper Group.||||||08-FEB-07
55|Abner Sandstone|43036|4|Described|p61|||Of the Roper Group.||||||08-FEB-07
55|Abner Sandstone|43149|5|Briefly described|Map Legend|||Of Roper Group.||||||08-FEB-07
55|Abner Sandstone|43645|5|Briefly described|p561|||||||||
55|Abner Sandstone|43652|6|Mentioned|p386|||||||||
55|Abner Sandstone|44287|14|Not recorded|p.12-18,19,opp.11|||Here includes only Hodgson Sandstone, Jalboi and Arnold Sandstone Members. (E53-3).||||||08-FEB-07
55|Abner Sandstone|44288|14|Not recorded|map legend|||Quartz sandstone, siltstone, ferruginous sandstone, fine conglomerate Upper (?) Proterozoic.||||||
55|Abner Sandstone|44299|4|Described|p.13|||SD/53-7,8. U (?) Proterozoic. Table 1.||||||
55|Abner Sandstone|44300|14|Not recorded|map legend||Neoproterozoic|SD/53-7,8. U.Proterozoic. Part of Roper Group.||||||08-FEB-07
55|Abner Sandstone|44332|14|Not recorded|p.8,12,opp.6,map|||(D53-14).||||||
55|Abner Sandstone|44333|14|Not recorded|map legend|||Upper(?) Proterozoic.||||||
55|Abner Sandstone|44400|2|Defined|p.9,12,Tb.1,opp.p.6|||(D53-6), map.||||||
55|Abner Sandstone|44401|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
55|Abner Sandstone|44434|14|Not recorded|p.8, opp. p.6, map|||(D53-11,12). Includes Hodgson Sandstone Member, Jalboi Member.||||||
55|Abner Sandstone|44435|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
55|Abner Sandstone|44436|5|Briefly described|p.11, opp. p.7, map|||(E53-4).||||||02-DEC-04
55|Abner Sandstone|44437|5|Briefly described|map legend|Precambrian|Precambrian|Of the Roper Group.  Massive medium grained quartz sandstone.  Conformably overlies the Crawford Formation.  Upper (?) Proterozoic.||||||08-DEC-04
55|Abner Sandstone|44459|14|Not recorded|p.8, opp.p.6, map|||(E53-2). Part of Roper Group. Includes Hodgson Sandstone Member, Jalboi Member, Arnold Sandstone Member.||||||08-FEB-07
55|Abner Sandstone|44460|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
55|Abner Sandstone|44471|14|Not recorded|p.9,10, opp.p.7, map|||(D53-10). Includes Munyi, Hodgson Sandstone, Jalboi and Arnold Sandstone Members.||||||08-FEB-07
55|Abner Sandstone|44472|5|Briefly described|map legend|||Of the Roper Group.  Upper (?) Proterozoic.||||||02-DEC-04
55|Abner Sandstone|44473|14|Not recorded|opp.p.7|||(E53-7).||||||
55|Abner Sandstone|44474|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
55|Abner Sandstone|44530|14|Not recorded|p.11, opp.12|||(D53-15).||||||
55|Abner Sandstone|44531|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
55|Abner Sandstone|45022|14|Not recorded|p80,81 tb.11.pl.28||Adelaidean|Of Roper Group.||||||08-FEB-07
55|Abner Sandstone|45162|6|Mentioned|p163|||||||||
55|Abner Sandstone|46861|6|Mentioned|Fig.2A|||||||||
55|Abner Sandstone|60483|5|Briefly described|p7 Fig. 5|||Of the Roper Group. Geological Province: McArthur Basin||||||
55|Abner Sandstone|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Roper Group. Includes Hodgson Sandstone, Jalboi and Arnold Sandstone Members. Overlain by Corcoran Formation, underlain by Crawford Formation.||||||
55|Abner Sandstone|60574|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Roper Group. Overlies the Crawford Formation. White medium- to coarse-grained quartzose sandstone with large trough cross-beds.||||||
55|Abner Sandstone|61566|5|Briefly described|p622|Proterozoic|Proterozoic|Of the Roper Group. Morphologically prominent mature quartzite and sandstone deposits. Geological Province: McArthur Basin.||||||
55|Abner Sandstone|62376|5|Briefly described|p38|Mesoproterozoic|Mesoproterozoic|Of the Roper Group. Geological Province: Beetaloo Sub-Basin.||||||11-FEB-10
55|Abner Sandstone|64784|5|Briefly described|p2 Fig.2 |Proterozoic|Proterozoic|Beetaloo Basin.||Unit in Roper Group.||Is overlain by Corcoran Formation.||
55|Abner Sandstone|64815|6|Mentioned|p5 Fig.3 |||||Of the Roper Group.||||
55|Abner Sandstone|64816|6|Mentioned|p2 Fig.1 |||||||||
55|Abner Sandstone|64817|6|Mentioned|p353 Fig.4 |||||Of the Roper Group.|Includes Arnold Sandstone, Jalboi, and Hodgson Sandstone, Members.|||
55|Abner Sandstone|65228|5|Briefly described|Fig.02.|||McArthur Basin.||Unit in Roper Group.|Includes Arnold Sandstone, Jaiboi, Hodgson Sandstone Members.|Overlies Crawford Formation. Is overlain by Corcoran Formation.||
55|Abner Sandstone|65236|5|Briefly described|p3 Fig. 3|Mesoproterozoic|Mesoproterozoic|Of the Roper Group. Intruded by a sill of age 1280-110Ma. Geological province: Beetaloo Sub-basin.||||||04-JUN-09
55|Abner Sandstone|65340|5|Briefly described|p62.|Mesoproterozoic|Mesoproterozoic|Deposited in an intertidal to shallow platform setting.||Unit in Roper Group.||Overlies Crawford Formation.|White, very thickly-bedded, quartzose medium sandstone, containing medium-scale trough crossbeds and minor ripples.|
55|Abner Sandstone|65342|6|Mentioned|p8.|||McArthur Basin. ||Unit in Roper Group.|Includes Hodgson and Jalboi Members.|||
55|Abner Sandstone|67144|5|Briefly described|Map legend.|Calymmian|Calymmian|Ridge-forming.||Unit in Roper Group.|Includes Arnold Sandstone and Hodgson Sandstone Members.|Overlies Crawford Formation.||
55|Abner Sandstone|67323|6|Mentioned|Mount Isa Block Time-Space Plot|||See also Eastern Australia Time-Space Plot. Camooweal-Murphy Domain, Mount Isa Inlier (QLD); McArthur region (NT).||||||
55|Abner Sandstone|67352|6|Mentioned|p13 Tb.2|Calymmian|Calymmian|McArthur Basin.||Roper Group|Arnold Sandstone Member|Conformably overlies Crawford Formation.||
55|Abner Sandstone|69018|6|Mentioned|p450 Fig.1b|Calymmian|Calymmian|Obsolete terminology.||Of Roper Group.||||
55|Abner Sandstone|69430|4|Described|p15:3, 26, 29-30, 34, 62|||An undifferentiated succession restricted to the Abner Range, southern McArthur Basin. In the Roper River region, this unit was divided into four mappable Members: Arnold Sandstone, Jalboi, Hodgson Sandstone, and Munyi, Members (Dunn, 1963). Haines et al. (1993) assigned the Munyi Member to the base of the Corcoran Formation; Abbott et al. (2001) raised the other three Members to Formation rank.||Collara Subgroup.||Overlies Crawford Formation. Is overlain by Corcoran Formation.||12-JUL-16
55|Abner Sandstone|69673|6|Mentioned|p16 fig 13|||Southern McArthur Basin.||||||
55|Abner Sandstone|70897|6|Mentioned|Fig.1.7.6,9|||McArthur Basin.||||||29-NOV-17
55|Abner Sandstone|70968|4|Described|p39-42, p44, p47, p50, p55, p131|Calymmian|Calymmian|First mentioned by Dunn (1963) who named four (Arnold Sandstone, Jalboi, Hodgson, Munyi) Members. The first three were defined as Formations by Abbott et al. (2001); the Munyi Member was reassigned to the Corcoran Formation by Haines et al. (1993). Named after the Abner Range, where the Jalboi Formation is absent and the surrounding Arnold and Hodgson Sandstones cannot be distinguished; the name Abner Sandstone is used for the undivided succession of sandstone, as mapped by Smith (1964) and Pietsch et al. (1991). Their type and reference sections are regarded as representative of Abner Sandstone as a whole. Forms spectacular parakarstic landforms, particularly "organ pipes". Up to 700m thick. Coastal tidal platform facies.||Collara Subgroup.||Conformably overlies Crawford Formation. Is overlain conformably by Corcoran Formation.|A thick monotonous succession of strongly jointed, well-bedded, fine- to medium- (less commonly coarse-)grained quartz sandstone.|
55|Abner Sandstone|71059|4|Described|p3|Mesoproterozoic|Mesoproterozoic|McArthur Basin. 35-220m thick. Coastal tidal platform deposits.||Collara Subgroup.||Conformably and/or disconformably overlies Crawford Formation. Equivalent to Arnold and Hodgson Sandstones.|Fine to medium, less commonly coarse, quartz sandstone.|
55|Abner Sandstone|71779|5|Briefly described|p2, Fig. 1|||Bauhinia Downs Region, McArthur Basin.||Collara Subgroup||||24-SEP-18
55|Abner Sandstone|71893|5|Briefly described|p17, p20, p24|||Abner Range in BAUHINIA DOWNS.||||Disconformably overlies the Crawford Formation. In part equivalent to the Arnold Sandstone and Hodgson Sandstone.||
55|Abner Sandstone|72526|5|Briefly described|p8 Fig.1.3.|Ectasian|Calymmian|Shown as located in the southern part of the Batten Fault zone and the Southeastern McArthur Basin.||Collara Subgroup||Overlies Crawford Formation.||
55|Abner Sandstone|72718|6|Mentioned|p7|||Southern McArthur Basin. Batten Fault Zone (partial) and southeastern McArthur Basin (partial).||Collara Subgroup, Roper Group||Underlain by Crawford Formation. Partly equivalent to Hodgson Sandstone, Jalboi Formation, and Arnold Sandstone.||
55|Abner Sandstone|72912|5|Briefly described|p5 Fig.3.|Mesoproterozoic|Mesoproterozoic|Located in the southern part of the Batten Fault Zone and the Southeastern McArthur Basin in the Southeastern McArthur Basin.||Collara Subgroup||Overlies Crawford Formation and is equivalent to Hodgson Sandstone, Jalboi Formation and Arnold Sandstone.||
55|Abner Sandstone|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|Southern McArthur Basin, Roper Superbasin.||Collara Subgroup, Roper Group||Underlain by Crawford Formation.||
55|Abner Sandstone|73412|5|Briefly described|p4, 8, 11|||Southern McArthur Basin.||Collara Subgroup.||Overlies Crawford Formation. Is overlain by Corcoran Formation.||
71|Acacia Gap Quartzite Member|22810|5|Briefly described|P13|||||||||
71|Acacia Gap Quartzite Member|22813|5|Briefly described|Map|Paleoproterozoic|Paleoproterozoic|Part of the Wildman Siltstone. Quartzite, commonly pyritic.||||||07-NOV-08
71|Acacia Gap Quartzite Member|23714|4|Described|p10|Proterozoic|Proterozoic|See also page 8 Table 1.  Of Wildman Siltstone. Max. thickness: 300 m.||||||
71|Acacia Gap Quartzite Member|23715|5|Briefly described|Map legend||Proterozoic|Of the Mount Partridge Group, in the Rum Jungle Region.||||||02-DEC-08
71|Acacia Gap Quartzite Member|23733|5|Briefly described|p32 Fig. 19|||Of Wildman Siltstone (Mount Partridge Group).||||||
71|Acacia Gap Quartzite Member|24001|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Fine to medium quartzite, pyritic interbedded phyllite.||||||
71|Acacia Gap Quartzite Member|39068|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Wildman Siltstone. Quartzite, commonly pyritic; sandstone with interbedded siltstone; metamorphosed to lower greenschist facies.||||||14-FEB-06
71|Acacia Gap Quartzite Member|39069|4|Described|p7|||See also Table 1.||||||
71|Acacia Gap Quartzite Member|39801|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Wildman Siltstone. Orthoquartzite, pyritic in places; sandstone, gritty sandstone, interbedded shale or argillite, commonly carbonaceous.||||||07-NOV-08
71|Acacia Gap Quartzite Member|40492|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
71|Acacia Gap Quartzite Member|40493|4|Described|p12|||||||||
71|Acacia Gap Quartzite Member|40808|3|Fully described|p12|||||||||
71|Acacia Gap Quartzite Member|41304|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
71|Acacia Gap Quartzite Member|41305|4|Described|p15|||||||||
71|Acacia Gap Quartzite Member|42012|6|Mentioned|p30|||||||||
71|Acacia Gap Quartzite Member|43187|5|Briefly described|p2|||||||||
71|Acacia Gap Quartzite Member|46675|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Wildman Siltstone (Mount Partridge Group). Orthoquartzite, pyritic in places; sandstone, gritty sandstone interbedded shale or argillite, commonly carbonaceous.||||||07-JAN-09
71|Acacia Gap Quartzite Member|47049|5|Briefly described|Table|||Minor name change; raised from base of Wildman Siltstone.||||||
71|Acacia Gap Quartzite Member|60575|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Wildman Siltstone (Mount Partridge Group).||||||
71|Acacia Gap Quartzite Member|60677|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Orthoquartzite, sandstone, gritty sandstone, interbedded shale or argillite, commonly carbonaceous. Of Wildman Siltstone.||||||
71|Acacia Gap Quartzite Member|61389|5|Briefly described|Map Legend|||Of the Wildman Siltstone. Orthoquartzite, sandstone, gritty sandstone, interbedded shale and argillite, commonly carbonaceous.||||||
71|Acacia Gap Quartzite Member|64662|5|Briefly described|p44|||Of the Wildman Siltstone. Geological Province: Pine Creek Orogen. Dominated by detrital zircon ~2.5Ga old, like Ferdies Member, Dead Bullock Formation, Tanami region. Could indicate widespread Neoarchean crust in northern Australia.||||||07-FEB-11
71|Acacia Gap Quartzite Member|64676|5|Briefly described|v, p1, p19, p22-23|||Has a Neoarchean provenance (2710-2495 Ma) comprising many age groups.|<2512 +/- 13 Ma (maximum deposition age).|Wildman Siltstone.|||Fine-grained, grey magnetic quartzite.|
71|Acacia Gap Quartzite Member|64698|4|Described|lithinterp table|Orosirian|Paleoproterozoic|Of Wildman Siltstone which has age 2026Ma SHRIMP U/Pb, so Member must be similar age. Max thickness 200m. Pyritic quartz sandstone, interbedded carbonaceous siltstone and mudstone.||||||10-FEB-10
71|Acacia Gap Quartzite Member|64730|5|Briefly described|p125 Fig. 3, p139|Paleoproterozoic|Paleoproterozoic|Age referred from ages of tuffaceous beds in the Wildman Siltstone, above Acacia Gap Quartzite Member. Includes detrital zircons of  Rum Jungle Complex age (Archean)|2019 +/- 4 Ma min. deposition age.|||||02-MAY-12
71|Acacia Gap Quartzite Member|65232|5|Briefly described|p51|||Of Wildman Siltstone. Orthoquartzite beds.||||||18-FEB-10
71|Acacia Gap Quartzite Member|65339|4|Described|p6 Table 1, p11, p16, p18.|||Formerly Acacia Gap Tongue Member (Malone 1962a, b), Acacia Gap Sandstone Member (Needham et al. 1980); revised to this name by Crick (1987). 50 - 300 m thick. Indurated ferricrete benches have formed on scree slopes near Townend Road. Stratiform pyrrhotite horizons produce curvilinear zones of high magnetic intensity. Is offset by NE-trending dextral strike-slip faults.|c.2025 Ma (Worden et al. 2004).|Unit in Wildman Siltstone.|||Pale grey, well sorted and rounded, fine- to medium-grained, evenly grained, dense quartzite with interbedded phyllite, sandstone; pyrite cubes common; quartz veining is abundant.|
71|Acacia Gap Quartzite Member|67186|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Unit in Wildman Siltstone.|||Pyritic quartz sandstone, interbedded carbonaceous siltstone and mudstone.|23-NOV-11
71|Acacia Gap Quartzite Member|67355|4|Described|p2, p7 Tb.2, p10-12|Orosirian|Neoarchean|Thickness of the Member varies greatly, a single quartzite ridge approximately 80 m thick occurs. Ages (2498 and 2512 Ma) are the maximum depositional age based on youngest and average of 6 youngest dated zircons.|2498 +/- 24 Ma, 2512 +/- 13 Ma (SHRIMP Zircon).|Wildman Siltstone |||Shallow-marine arenite; medium to coarse, well sorted, light grey quartz sandstone, interbedded with carbonaceous shale and siltstone. Coarse, disseminated euhedral pyrite grains/cubic casts. Rare crossbedding, commonly massive.|25-JAN-17
71|Acacia Gap Quartzite Member|67779|5|Briefly described|p6 Fig.5.|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen.|2019 +/- 4 Ma (Worden et al. 2008a).|Unit in Wildman Siltstone.||||
71|Acacia Gap Quartzite Member|69420|4|Described|p5:4, 8, 10-11, 16, 117-118|Paleoproterozoic|Paleoproterozoic|Rum Jungle region, Central Domain, Pine Creek Orogen. A typo error show it as Acacia Gap quartzite Member on 5:8. Up to 300m thick. Shallow marine deposits. SHRIMP U-Pb detrital zircon maximum deposition age. Similar Neoarchean detrital zircon population peaks as Beestons Formation: indicate a provenance in a Rum Jungle Complex-type Archean terrane. A source of fine sand deposits.|<2498 +/- 24 Ma (Cross et al., 2005).|Wildman Siltstone.|||Succession of pyritic sandstone, quartzite, shale.|12-JUL-16
71|Acacia Gap Quartzite Member|69917|5|Briefly described|p43-45, 52|Paleoproterozoic|Neoarchean|Pine Creek Orogen, Central Domain. U/Pb SHRIMP zircon dating, Hf analytical data. Youngest age used for maximum depositional age. Also shown as Acacia Gap Quartzite p45.|2498+/-24 Ma max dep|Of Wildman Siltstone|||Fine-grained, grey magnetic quartzite.|
71|Acacia Gap Quartzite Member|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||Wildman Siltstone.|||Pyritic quartz sandstone, interbedded with carbonaceous siltstone and mudstone.|
71|Acacia Gap Quartzite Member|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|2512+/-13 Ma (MDA: U-Pb zircon SHRIMP)||||Fine-grained, grey magnetic quartzite.|
92|Adam Shale|8217|5|Briefly described|Map Legend|Cambrian|Cambrian|Green and red shale and sandstone, bioturbated.||||||
92|Adam Shale|12951|5|Briefly described|p143, p145 Fig 6|Early Cambrian|Early Cambrian|Georgina Basin.||||Laterally equivalent to Mount Baldwin Formation. Unconformably overlies Elkera Formation.|Siliciclastics.|
92|Adam Shale|22954|6|Mentioned|Fig3p9|Early Cambrian||||||||
92|Adam Shale|24111|5|Briefly described|p215 Fig. 11|Cambrian|Cambrian|Name appears as Adam only in text.  Geological Province: Georgina Basin.||||||
92|Adam Shale|35798|2|Defined|p312|Early Cambrian|Early Cambrian|||||||
92|Adam Shale|37462|6|Mentioned|Fig.4.16|||||||||
92|Adam Shale|37928|6|Mentioned|Fig.4|||||||||
92|Adam Shale|37929|6|Mentioned|Fig.2|||||||||
92|Adam Shale|38157|6|Mentioned|p281, Table IX|||||||||
92|Adam Shale|39921|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
92|Adam Shale|40856|6|Mentioned|Fig.23.6|||||||||
92|Adam Shale|40906|6|Mentioned|Fig.9|||||||||
92|Adam Shale|41103|6|Mentioned|p261|||||||||
92|Adam Shale|41388|6|Mentioned|p552|||||||||
92|Adam Shale|41524|6|Mentioned|Fig.3|||||||||
92|Adam Shale|41801|6|Mentioned|Fig.4|||||||||
92|Adam Shale|42059|6|Mentioned|Fig.2 P131|||||||||
92|Adam Shale|42956|5|Briefly described|p27|||||||||
92|Adam Shale|43595|5|Briefly described|p548,Fig.5-33,549||Early Cambrian|||||||
92|Adam Shale|45155|6|Mentioned|Fig.8|||||||||
92|Adam Shale|47035|6|Mentioned|p85|||||||||
92|Adam Shale|49027|5|Briefly described|p6|||||||||
92|Adam Shale|60122|6|Mentioned|p9, p11 Tb. 1|||Within Supersequence 4.  Disconformably overlain by Red Heart Dolostone.  See also p14.||||||11-MAY-05
92|Adam Shale|61404|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Of the Shadow Group.  Shale; basal sandstone. Geological Province: southern Georgina Basin.||||||
92|Adam Shale|62983|6|Mentioned|p11|||Geological Province: Georgina Basin.||||||
92|Adam Shale|63450|4|Described|p78 Fig. 5, p80|Early Cambrian|Early Cambrian|Disconformably overlain by Red Heart Dolomite. Max. thickness: 16m. Geological province: Georgina Basin, West Toko Syncline. Comprises bioturbated red and green shale and sandstone; acritarchs.||||||07-FEB-11
92|Adam Shale|63562|6|Mentioned|p345|Early Cambrian|Ediacaran|Georgina Basin. ||||||
92|Adam Shale|64068|3|Fully described|p x, pp54-55, p57|Early Cambrian|Early Cambrian|Previously included in underlying Grant Bluff Formation. Potential host for epigenetic, stratiform, sediment-hosted Pb-Zn. Correlations: Mount Baldwin Formation, Octy Formation, Neutral Junction Formation, possibly Sylvester Sandstone.||Of Shadow Group.||Disconformably overlies Grant Bluff Formation and underlies Red Heart Dolostone.|Green and brown pyritic shale, black shale toward top; minor brown-grey sandstone.|04-APR-12
92|Adam Shale|64778|6|Mentioned|p13|Cambrian|Cambrian|Toko Syncline, Southern Georgina Basin.||||||
92|Adam Shale|64812|5|Briefly described|p237 Fig. 2|Early Cambrian|Early Cambrian|Geological Province: southern Georgina Basin.||||||07-FEB-11
92|Adam Shale|64813|5|Briefly described|p256 Fig. 3|Early Cambrian|Early Cambrian|Overlain by Red Heart Dolostone. Geological Province: southern Georgina Basin.||||||11-FEB-09
92|Adam Shale|65237|5|Briefly described|p3 Fig. 4|Early Cambrian|Early Cambrian|Interfingers with Mount Baldwin Formation. Geological province: southern Georgina Basin.||||||07-FEB-11
92|Adam Shale|65342|6|Mentioned|p7.|Early Cambrian|Early Cambrian|||||||
92|Adam Shale|67323|5|Briefly described|p83|Cambrian|Cambrian|West Toko Syncline, Georgina Basin.||||Is overlain unconformably by Red Heart Dolomite.||
92|Adam Shale|67402|6|Mentioned|p213 fig GRG3|Early Cambrian|Early Cambrian|Georgina Basin. ||||Unconformably overlain by the Red Heart Dolomite.||
92|Adam Shale|67870|6|Mentioned|p43|Early Cambrian|Early Cambrian|Georgina Basin.||||||
92|Adam Shale|69437|5|Briefly described|p22:10|Cambrian|Cambrian|Southern Georgina Basin.||||Is overlain by Red Heart Dolostone.||12-JUL-16
92|Adam Shale|69443|3|Fully described|p28:7, 14-15; 28:38 Fig.28.36|Early Cambrian|Early Cambrian|Walter in Walter et al. (1979). Southern Georgina Basin. Generally recessive unit. 16m thick in its type section in cored drillhole BMR Hay River-11B. Marine, presumably below wave-base, deposits.||Shadow Group.||Disconformably overlies Grant Bluff Formation. Is overlain disconformably by Red Heart Dolostone. Is correlated with Mount Baldwin, Octy and Neutral Junction Formations, and ?Sylvester Sandstone.|Laminated pyritic shale with sandy laminations; minor medium-coarse sandstone. Contains acritarchs and bioturbated beds.|12-JUL-16
92|Adam Shale|69561|6|Mentioned|p33 fig 2|Cambrian|Cambrian|||||Overlain by Red Heart Dolostone||
92|Adam Shale|69673|5|Briefly described|p114 fig 92, p116, p119 fig 94|||16m thick.||Shadow Group|||Laminated pyritic shale with sandy laminations and minor sandstone.|
92|Adam Shale|69917|6|Mentioned|p115|||Georgina Basin. Walter et al (1995) assigned this unit to Supersequence 4 of their Centralian Superbasin.||||||
92|Adam Shale|72516|6|Mentioned|p90|Cambrian|Cambrian|Georgina Basin.||||Equivalent to the Mount Baldwin Formation.||02-JUN-21
151|Age Creek Formation|22954|6|Mentioned|Fig3p9||Undillan|||||||
151|Age Creek Formation|23031|5|Briefly described|17|||||||||
151|Age Creek Formation|23408|5|Briefly described|p527|Middle Cambrian|Middle Cambrian|Contains platform and platform-edge carbonates.||||||15-JUN-09
151|Age Creek Formation|30479|6|Mentioned|Fig.7|||Stratigraphic relationships||||||
151|Age Creek Formation|30914|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
151|Age Creek Formation|31506|6|Mentioned|p119|||||||||
151|Age Creek Formation|33111|4|Described|p27,31|||||||||
151|Age Creek Formation|34395|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
151|Age Creek Formation|34659|6|Mentioned|p227|||||||||
151|Age Creek Formation|35054|6|Mentioned|Table 23|||||||||
151|Age Creek Formation|35121|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
151|Age Creek Formation|35139|4|Described|Table.2|||||||||
151|Age Creek Formation|35553|6|Mentioned|p77|||See also Appendix 2, description of Agnostid localities.||||||
151|Age Creek Formation|36234|6|Mentioned|p168|||||||||
151|Age Creek Formation|37572|4|Described|p157|||See also Fig.7||||||
151|Age Creek Formation|38446|6|Mentioned|Table 23|||||||||
151|Age Creek Formation|39445|5|Briefly described|Table 4|||See also p62||||||17-JUL-06
151|Age Creek Formation|39690|6|Mentioned|Table 1|||||||||
151|Age Creek Formation|40686|5|Briefly described|p407|||||||||
151|Age Creek Formation|40855|6|Mentioned|Fig.24.1|||||||||
151|Age Creek Formation|41129|6|Mentioned|Fig.8|||||||||
151|Age Creek Formation|41240|6|Mentioned|Fig.1|||||||||
151|Age Creek Formation|41298|6|Mentioned|Map legend|Middle Cambrian||||||||
151|Age Creek Formation|44210|4|Described|map, Tb.2|||out crop||||||
151|Age Creek Formation|44211|2|Defined|p92,96||Middle Cambrian|See also Lexicon. Confined to Undilla Basin.||||||
151|Age Creek Formation|44213|14|Not recorded|Map Legend||Middle Cambrian|||||||
151|Age Creek Formation|44274|14|Not recorded|p11|||||||||
151|Age Creek Formation|44275|14|Not recorded|Map Legend|||||||||
151|Age Creek Formation|44441|14|Not recorded|p.8|||Interfingers with Camooweal Dolomite.||||||
151|Age Creek Formation|44920|14|Not recorded|Map Legend, Sheet 2||Middle Cambrian|||||||
151|Age Creek Formation|45012|14|Not recorded|p338|||No data.||||||
151|Age Creek Formation|45052|3|Fully described|p95|||M. Camb.||||||
151|Age Creek Formation|45054|6|Mentioned|p6|||M.Cambrian. Fossil locality||||||
151|Age Creek Formation|45079|6|Mentioned|p18|||||||||
151|Age Creek Formation|45119|6|Mentioned|p4|||||||||
151|Age Creek Formation|47058|6|Mentioned|p134|||||||||
151|Age Creek Formation|48906|14|Not recorded|Tb.1|||||||||
151|Age Creek Formation|60122|6|Mentioned|p57 Appendix|||Correlated with parts of Arthur Creek Formation.  Geological Province: eastern Georgina Basin.||||||
151|Age Creek Formation|63450|5|Briefly described|p82|Middle Cambrian|Middle Cambrian|Geological Province: Undilla Sub-basin.||||||07-FEB-11
151|Age Creek Formation|64068|4|Described|p62, 63, 64, 139, 225|||Totts Creek, northeastern Georgina Basin. Hosts Pb and Zn in fractures and vugs. Correlated with to Arthur Creek Formation, Inca Formation, Quita Formation, Roaring Siltstone, Devoncourt Limestone.||Narpa Group.|||Flat-lying to gently-dipping vuggy chert after dolostone; almost entirely covered by black soil and 'ironstone' duricrust (up to 9.5% Pb).|21-MAR-16
151|Age Creek Formation|64443|6|Mentioned|p14, p41|Boomerangian|Floran|Correlative of Ranken Limestone; laterally interdigitates with Camooweal Dolostone.||||||
151|Age Creek Formation|65337|6|Mentioned|p68.|||Laterally interdigitates with Camooweal Dolostone.||||||
151|Age Creek Formation|67323|4|Described|GIS tbl, map; p72, p83|Middle Cambrian|Middle Cambrian|Undilla Sub-basin, Georgina Basin. Contains Pb, Zn and Pb-Zn anomalies 50-75km NE of Camooweal.||Narpa Group.||Unconformably overlies Beetle Creek Formation. Lateral equivalent of Camooweal Dolomite. Is overlain by Split Rock Sandstone.|Dolomite, pelletal dolomite, dolomitic limestone, limestone, calcarenite and dolarenite, chert nodules.|
151|Age Creek Formation|69443|5|Briefly described|p28:16, 20, 23|Middle Cambrian|Middle Cambrian|Georgina Basin. Appears as Age Creek Limestone in 18:20.||Narpa Group.||Is overlain by and partially interfingers with Currant Bush Limestone. Correlated with Ranken Limestone.||12-JUL-16
151|Age Creek Formation|69573|6|Mentioned|p659|||Contains Drumian Stage [Cambrian] fossil sites.||||||
151|Age Creek Formation|69591|4|Described|p87-90, p96, p98 Fig.2.91|Cambrian|Cambrian|Undilla Sub-basin, Georgina Basin. Up to 1200m thick. Carbonate ramp deposits. Contains rich faunas of phosphatic brachiopods and trilobites in limestone interbeds. Interdigitates with Camooweal Dolostone (to the W) and with parts of Thorntonia, Currant Bush, V Creek and Mail Change Limestones and Inca Formation (to the E and NE).||Narpa Group.||Unconformably overlies Beetle Creek Formation; disconformably overlies Thorntonia Limestone. Is overlain by Split Rock Sandstone. See COMMENTS for more.|Sandy clastic, pelletal and two-tone crystalline dolomite and limestone with interbeds of calcareous sandstone. Cross-bedding common, with foresets up to 15m thick.|
151|Age Creek Formation|70723|5|Briefly described|p24 Fig. 2|Cambrian|Cambrian|Georgina Basin.||Narpa Group||Overlies Currant Bush Limestone.|Dolomite.|
151|Age Creek Formation|72321|6|Mentioned|Fig 2|Drumian|Drumian|Undilla Sub-basin, Georgina Basin. Australian Stages: Floran to Undillan. ||of Narpa Group.||||
151|Age Creek Formation|72516|6|Mentioned|p92|Cambrian|Cambrian|Eastern Georgina Basin.||||Equivalent to the Arthur Creek Formation.||03-JUN-21
151|Age Creek Formation|73418|5|Briefly described|p4 Fig.3|Miaolingian|Miaolingian|Georgina Basin, Undilla Sub-basin.||Narpa Group||Overlies Currant Bush Limestone|Dolomite.|
168|Aileron Metamorphics|8222|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block.||||||
168|Aileron Metamorphics|23316|6|Mentioned|p357|||Contains granulite-facies pelites.||||||07-FEB-07
168|Aileron Metamorphics|41051|6|Mentioned|p410|||||||||
168|Aileron Metamorphics|42217|6|Mentioned|p411|||||||||
168|Aileron Metamorphics|44114|6|Mentioned|p324|||Anmatjira-Reynolds Range region, Arunta Inlier. Granulite-facies metamorphosed equivalents of the Lander assemblage.||||||
168|Aileron Metamorphics|64737|6|Mentioned|p231|||In Aileron Province. Metamorphosed to granulite grade.||Of Lander Package.||||01-MAY-12
168|Aileron Metamorphics|65341|6|Mentioned|p2 Fig.2. |Paleoproterozoic|Paleoproterozoic|||||||19-JUN-13
168|Aileron Metamorphics|68997|4|Described|vi-vii,p1,23-26|Orosirian|Orosirian|Granulite-facies pelitic and psammitic gneisses and lesser mafic granulite and amphibolite that outcrop at the SE end of the Reynolds Range on the western edge of ALCOOTA. Similar stratigraphic position to Lander Rock Formation. Sample: AC08CJE222: Grid Reference: MGA94 Zone 53: 353286mE 7490699mN. Zircon age spectra of 1861+\-5 Ma, interpreted as maximum depositional age. Metamorphic rims dated from zircons with age of 1809+\-10 Ma, interpreted to reflect Stafford-aged metamorphism. Metamorphic zircon rims dated at 1753+\-7 Ma are interpreted to reflect a marginally younger event than the 1780-1770 Ma Yambah Event.|1861+\-5 Ma (max dep age: U-Pb zircon)||||Garnet-biotite gneiss, cordierite gneiss, calc-silicate rock and marble, quartz-rich metasedimentary rock, mafic granulite and amphibolite.|
168|Aileron Metamorphics|69427|4|Described|p12:4, 6, 21, 26, 32|||SE Reynolds Range, Aileron Province. Crops out near the SE end of the Reynolds Range. This unit now includes rocks previously mapped as unassigned granulite-facies rocks in adjacent regions of ALCOOTA map area, which have this maximum depositional age.|<c.1864 Ma (Beyer et al., 2010).|||Is intruded by Mount Boothby Orthogneiss and Napperby Gneiss.|Mainly pelitic granulites with lesser mafic granulite, cordierite gneiss, garnet-biotite gneiss, calc-silicate rock and marble, quartz-rich metasedimentary rock, and amphibolite.|12-JUL-16
168|Aileron Metamorphics|69917|5|Briefly described|p57-61, 109||Paleoproterozoic|Central Arunta Region, Aileron Province. Migmatitic metapelite sampled. U/Pb SHRIMP zircon dating, Hf analytical data. Maximum depositional age of 1861+/-5 Ma. Metamorphism during both Stafford (1810-1790 Ma) and Yambah (1780-1770 Ma) high-grade events.|||||Dominant lithologies include garnet-biotite gneiss, cordierite gneiss, calc-silicate rock and marble, quartz-rich metasedimentary rock,with subordinate mafic granulite and amphibolite.|
168|Aileron Metamorphics|69932|6|Mentioned|p301, 303, 307|||Northern Province, Arunta Inlier.|||||Migmatite (probably metavolcanic).|
168|Aileron Metamorphics|70376|5|Briefly described|p833 fig 2, p835|Paleoproterozoic|Paleoproterozoic|Previously considered equivalents of the Lander Rock Formation. Cm scale gradational changes suggestive of presence of recrystallised graded beds.|||||Migmatites which generally contain cordierite-sillimanite-K-feldspar-quartz-biotite assemblages. Metasedimentary gneisses. Some primary lithological layering evident: variations from Si-rich psammitic layers to Mg-Al rich pelitic layers.|24-JAN-22
168|Aileron Metamorphics|71348|6|Mentioned|p209,215-216|||Geological province: Tanami Region, North Australian Craton. See p215 for summary of U-Pb geochronological data.||||||
168|Aileron Metamorphics|71592|5|Briefly described|Appendix A.|||Arunta Orogen. A range of monazite U-Pb LA-ICPMS ages of metamorphism.|1576+/-10 Ma to 1513+/-15 Ma.||||Metapelite, metapelitic gneiss, pegmatite, gneiss.|
168|Aileron Metamorphics|73399|6|Mentioned|App.E||||||||May include granulite, amphibolite, and gneiss.|
262|Algebuckina Sandstone|12597|6|Mentioned|p492 Tb.1, p498-499|Early Cretaceous|Pliensbachian|NW Eromanga Basin.||||||
262|Algebuckina Sandstone|13497|6|Mentioned|p115 fig 6.33|Late Jurassic|Middle Jurassic|Eromanga Basin. ||||||
262|Algebuckina Sandstone|13516|6|Mentioned|p167 fig 10, p171 fig 12|Early Cretaceous|Jurassic|In Eromanga Basin.||||||
262|Algebuckina Sandstone|22613|6|Mentioned|p17|||Eromanga Basin||||||
262|Algebuckina Sandstone|22874|6|Mentioned|P18|||||||||
262|Algebuckina Sandstone|22883|5|Briefly described|P31, Fig2|Early Cretaceous|Early Jurassic|Lateral equivalent of Hutton Sandstone, Birkhead Formation, Adori Sandstone, Westbourne Formation, Namur Sandstone and Murta Formation, underlying unit is Poolowanna Formation.||||||16-SEP-08
262|Algebuckina Sandstone|22922|6|Mentioned|33 fig 2|||||||||
262|Algebuckina Sandstone|23054|5|Briefly described|p21-3,36|Neocomian|Late Jurassic|||||||
262|Algebuckina Sandstone|23154|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Geological Province - Eromanga Basin.||||||
262|Algebuckina Sandstone|23155|4|Described|p30|Early Cretaceous|Early Jurassic|||||||
262|Algebuckina Sandstone|23282|6|Mentioned|p85 Fig 6.2|||of Eromanga Basin.||||||
262|Algebuckina Sandstone|23818|4|Described|p141 Fig.65, p144 Fig.66|Late Jurassic|Late Jurassic|Geological Province: Great Artesian Basin. Max. thickness: ~70 ft.||||||
262|Algebuckina Sandstone|23830|5|Briefly described|Fig. 3a|Jurassic|Jurassic|Geological Province: Boorthanna Trough, eastern Arckaringa Basin.||||||24-JAN-06
262|Algebuckina Sandstone|23849|5|Briefly described|p781|Late Jurassic|Late Jurassic|Geological Province: Eromanga Basin.||||||
262|Algebuckina Sandstone|23982|5|Briefly described|p2|Cretaceous|Jurassic|Geological Province: Great Artesian Basin. See also page 35 Fig.7.||||||
262|Algebuckina Sandstone|24067|5|Briefly described|p249 Fig.2|Mesozoic|Mesozoic|Geological Province: Officer Basin.||||||
262|Algebuckina Sandstone|24092|5|Briefly described|p8 Fig.3|||Geological Province: Eromanga Basin.||||||
262|Algebuckina Sandstone|24112|5|Briefly described|p254 Fig.2|Early Cretaceous|Late Jurassic|Geological Province: Eromanga Basin||||||
262|Algebuckina Sandstone|24176|5|Briefly described|p19, p22 Tb. 1|Late Jurassic|Late Jurassic|Equivalent to Village Well Formation.  Geological Province: Mount Painter Province.||||||
262|Algebuckina Sandstone|24210|5|Briefly described|p133 Fig. 2|Late Jurassic|Middle Jurassic|Geological Province: Eromanga Basin.||||||
262|Algebuckina Sandstone|24321|5|Briefly described|Map legend|Tithonian|Kimmeridgian|||||||11-JAN-10
262|Algebuckina Sandstone|24506|5|Briefly described|p17|Mesozoic|Mesozoic|Considered to prospective for gold and diamonds.||||||
262|Algebuckina Sandstone|29379|4|Described|p30|||Lithology. Upper Jurassic-Lower Cretaceous.||||||
262|Algebuckina Sandstone|29591|6|Mentioned|p79|||||||||
262|Algebuckina Sandstone|29660|6|Mentioned|p6|||||||||
262|Algebuckina Sandstone|30176|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
262|Algebuckina Sandstone|30177|6|Mentioned|p101|||||||||
262|Algebuckina Sandstone|30514|6|Mentioned|p102|||||||||
262|Algebuckina Sandstone|30804|6|Mentioned|p7|||On table 2||||||
262|Algebuckina Sandstone|30807|6|Mentioned|p102|||Suggested mapping symbol||||||
262|Algebuckina Sandstone|30917|6|Mentioned|p42|||||||||
262|Algebuckina Sandstone|30918|6|Mentioned|p81|||||||||
262|Algebuckina Sandstone|30919|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
262|Algebuckina Sandstone|30921|6|Mentioned|Map legend|Late Jurassic|Early Jurassic|Early to Late Jurassic||||||
262|Algebuckina Sandstone|30924|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
262|Algebuckina Sandstone|31244|5|Briefly described|p3|||Jurassic||||||
262|Algebuckina Sandstone|31248|6|Mentioned|p60|||Palynology correlation||||||
262|Algebuckina Sandstone|31532|6|Mentioned|Table 1|||||||||
262|Algebuckina Sandstone|31699|4|Described|p133|||Upper Jurassic.||||||17-JAN-08
262|Algebuckina Sandstone|31923|6|Mentioned|p14|||||||||
262|Algebuckina Sandstone|32033|6|Mentioned|p2|||||||||
262|Algebuckina Sandstone|32313|6|Mentioned|p164|||||||||
262|Algebuckina Sandstone|33075|6|Mentioned|p451|||||||||
262|Algebuckina Sandstone|33165|6|Mentioned|Chart|||Correlation chart only||||||
262|Algebuckina Sandstone|33224|6|Mentioned|p69|||Palynology||||||
262|Algebuckina Sandstone|33491|4|Described|p56|||Mention Fig.2.||||||17-JAN-08
262|Algebuckina Sandstone|33523|4|Described|p26|||See also p9.||||||17-JAN-08
262|Algebuckina Sandstone|33820|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
262|Algebuckina Sandstone|33821|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
262|Algebuckina Sandstone|33822|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
262|Algebuckina Sandstone|33823|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
262|Algebuckina Sandstone|33824|5|Briefly described|p7|||Table 2||||||
262|Algebuckina Sandstone|33825|4|Described|p8|||Lithology.||||||17-JAN-08
262|Algebuckina Sandstone|33827|6|Mentioned|p7|||Table 2||||||
262|Algebuckina Sandstone|33828|5|Briefly described|p5|||Table 1||||||
262|Algebuckina Sandstone|33829|6|Mentioned|p263|||||||||
262|Algebuckina Sandstone|33832|5|Briefly described|p7|||Stratigraphy||||||
262|Algebuckina Sandstone|33931|6|Mentioned|p9|||U.Jur.||||||
262|Algebuckina Sandstone|33936|6|Mentioned|Fig.3A|||Jurassic.||||||
262|Algebuckina Sandstone|33938|6|Mentioned|p20|||||||||
262|Algebuckina Sandstone|33939|2|Defined|p386|Early Cretaceous|Late Jurassic|Upper Jurassic - Lower Cretaceous||||||
262|Algebuckina Sandstone|33942|6|Mentioned|Fig.1|||||||||
262|Algebuckina Sandstone|33964|6|Mentioned|p6|||Correlation||||||
262|Algebuckina Sandstone|33970|6|Mentioned|Fig.1|||||||||
262|Algebuckina Sandstone|33971|5|Briefly described|p37|||Refers Wopfner et al. (1970)||||||
262|Algebuckina Sandstone|33976|6|Mentioned|Fig.2|||||||||
262|Algebuckina Sandstone|34611|4|Described|p146|||Jurassic. See Fig.65.||||||
262|Algebuckina Sandstone|34766|6|Mentioned|p58|||||||||
262|Algebuckina Sandstone|35080|6|Mentioned|Fig.3|||||||||
262|Algebuckina Sandstone|35149|5|Briefly described|Table 1|||See also mention on Fig.4.||||||
262|Algebuckina Sandstone|35548|5|Briefly described|p18|||||||||
262|Algebuckina Sandstone|35549|6|Mentioned|Map legend|Cretaceous|Jurassic|||||||
262|Algebuckina Sandstone|35628|6|Mentioned|Table 4|||||||||
262|Algebuckina Sandstone|36214|5|Briefly described|p58|||||||||
262|Algebuckina Sandstone|36733|6|Mentioned|p14|||See also P53.||||||
262|Algebuckina Sandstone|36895|6|Mentioned|p9|||||||||
262|Algebuckina Sandstone|36922|6|Mentioned|Fig.3|||||||||
262|Algebuckina Sandstone|38022|6|Mentioned|Fig.4|||||||||
262|Algebuckina Sandstone|38068|4|Described|p71|||||||||
262|Algebuckina Sandstone|38604|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
262|Algebuckina Sandstone|38605|4|Described|p20|||See also Table 4.||||||
262|Algebuckina Sandstone|38814|6|Mentioned|Table 1|||||||||
262|Algebuckina Sandstone|39211|5|Briefly described|Fig.6|||See also Figs 10,14,15, etc. Correlation||||||
262|Algebuckina Sandstone|39352|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
262|Algebuckina Sandstone|39629|6|Mentioned|Fig.1|||||||||
262|Algebuckina Sandstone|40003|5|Briefly described|p33|||See also Fig.8||||||
262|Algebuckina Sandstone|40220|6|Mentioned|Fig.2|||||||||
262|Algebuckina Sandstone|40670|6|Mentioned|Fig.9|||||||||
262|Algebuckina Sandstone|40910|6|Mentioned|p15|||See also P26||||||
262|Algebuckina Sandstone|40911|6|Mentioned|Map legend|Cretaceous|Jurassic|||||||
262|Algebuckina Sandstone|40912|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
262|Algebuckina Sandstone|40925|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
262|Algebuckina Sandstone|40926|3|Fully described|p13|||||||||
262|Algebuckina Sandstone|41060|6|Mentioned|p2|||||||||
262|Algebuckina Sandstone|41061|6|Mentioned|p20|||||||||
262|Algebuckina Sandstone|41063|2|Defined|p46|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
262|Algebuckina Sandstone|41084|5|Briefly described|p81|||||||||
262|Algebuckina Sandstone|41085|3|Fully described|p87|||||||||
262|Algebuckina Sandstone|41125|6|Mentioned|Table 10|||||||||
262|Algebuckina Sandstone|41165|5|Briefly described|p363, Fig.15|||||||||
262|Algebuckina Sandstone|41175|6|Mentioned|p196|||||||||
262|Algebuckina Sandstone|41183|6|Mentioned|Fig.3 p308|||||||||
262|Algebuckina Sandstone|41186|5|Briefly described|p212|||||||||
262|Algebuckina Sandstone|41187|6|Mentioned|Fig.2|||||||||
262|Algebuckina Sandstone|41216|6|Mentioned|p300|||||||||
262|Algebuckina Sandstone|41266|6|Mentioned|Fig.3|||||||||
262|Algebuckina Sandstone|41361|6|Mentioned|p5|||||||||
262|Algebuckina Sandstone|41523|6|Mentioned|p271|||||||||
262|Algebuckina Sandstone|41681|6|Mentioned|p22|||||||||
262|Algebuckina Sandstone|41724|6|Mentioned|p381|||||||||
262|Algebuckina Sandstone|41950|5|Briefly described|Fig.2 P3|||||||||
262|Algebuckina Sandstone|42071|6|Mentioned|Fig.2A P116|||||||||
262|Algebuckina Sandstone|42084|6|Mentioned|Fig.3 P356|||||||||
262|Algebuckina Sandstone|42085|6|Mentioned|Fig.2 P374|||||||||
262|Algebuckina Sandstone|42099|6|Mentioned|p62|||||||||
262|Algebuckina Sandstone|42283|6|Mentioned|p89|||||||||
262|Algebuckina Sandstone|42293|6|Mentioned|Fig.2 P.18|||||||||
262|Algebuckina Sandstone|42341|6|Mentioned|Fig.7 P57|||||||||
262|Algebuckina Sandstone|42346|5|Briefly described|p77, Fig.2 p79|Early Cretaceous|Late Jurassic|||||||
262|Algebuckina Sandstone|42357|6|Mentioned|p11|||||||||
262|Algebuckina Sandstone|42375|6|Mentioned|Fig. 28 P125|||||||||
262|Algebuckina Sandstone|42463|6|Mentioned|Fig.4 P171|||||||||
262|Algebuckina Sandstone|42465|5|Briefly described|Map Legend|||||||||
262|Algebuckina Sandstone|42469|4|Described|p27|||||||||
262|Algebuckina Sandstone|42504|5|Briefly described|p81|||||||||
262|Algebuckina Sandstone|42520|5|Briefly described|p6|||||||||
262|Algebuckina Sandstone|42546|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|||||||
262|Algebuckina Sandstone|42736|5|Briefly described|map legend|Early Cretaceous|Late Jurassic|||||||
262|Algebuckina Sandstone|42746|4|Described|p9|||See also Fig.2, Fig.6.||||||
262|Algebuckina Sandstone|42816|4|Described|p17|||||||||
262|Algebuckina Sandstone|42899|5|Briefly described|p347|||||||||
262|Algebuckina Sandstone|42905|5|Briefly described|p19|||see also Fig 5.3||||||
262|Algebuckina Sandstone|43035|6|Mentioned|p27|||||||||
262|Algebuckina Sandstone|43048|5|Briefly described|p21|||||||||
262|Algebuckina Sandstone|43053|5|Briefly described|Map Legend|Jurassic|Jurassic|Fluvial sandstone.||||||25-MAY-05
262|Algebuckina Sandstone|43085|5|Briefly described|Fig.5|||||||||
262|Algebuckina Sandstone|43094|5|Briefly described|p36|||||||||
262|Algebuckina Sandstone|43105|5|Briefly described|Fig.9,p15|||||||||
262|Algebuckina Sandstone|43258|5|Briefly described|Map Legend||Jurassic|||||||
262|Algebuckina Sandstone|43298|5|Briefly described|Map Legend||Jurassic|||||||
262|Algebuckina Sandstone|43591|5|Briefly described|p28,40||Jurassic|||||||
262|Algebuckina Sandstone|43743|6|Mentioned|Fig.2,p33|Early Cretaceous|Late Jurassic|||||||
262|Algebuckina Sandstone|43840|5|Briefly described|Fig3 p12|||Cretaceous-Jurassic age||||||12-JUL-16
262|Algebuckina Sandstone|44133|5|Briefly described|p75 Fig. 8.13, 106-108|Early Cretaceous|Early Jurassic|Geological Province: Eromanga Basin. Overlies: Poolowanna Formation. Thickness: 750m. ||||||
262|Algebuckina Sandstone|44289|5|Briefly described|Map Legend||Neocomian|||||||
262|Algebuckina Sandstone|44658|14|Not recorded|map legend|||? Jurassic (G53-15).||||||
262|Algebuckina Sandstone|44689|14|Not recorded|map legend|||Andamooka, (H53-12). Equivalent. Cretaceous. (lower??).||||||
262|Algebuckina Sandstone|44935|5|Briefly described|Map Legend||Late Jurassic|||||||
262|Algebuckina Sandstone|45041|6|Mentioned|p114|||||||||
262|Algebuckina Sandstone|46791|6|Mentioned|Table 2|||||||||
262|Algebuckina Sandstone|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
262|Algebuckina Sandstone|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
262|Algebuckina Sandstone|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
262|Algebuckina Sandstone|60717|5|Briefly described|p40 Fig. 2|Late Jurassic|Middle Jurassic|Overlies Poolowanna Formation; underlies Cadna-owie Formation. Lateral to Hutton Sandstone, Birkhead Formation and Namur Sandstone but relationship(s) unclear. Geological Province: Eromanga  Basin.||||||31-JAN-08
262|Algebuckina Sandstone|60953|5|Briefly described|Map Legend|Cretaceous|Jurassic|Fluvial sandstone.||||||
262|Algebuckina Sandstone|60955|5|Briefly described|Map Legend|Cretaceous|Jurassic|Coarse sands and grits, ferruginous sandstones.||||||13-APR-05
262|Algebuckina Sandstone|61108|5|Briefly described|map legend|Cretaceous|Jurassic|Fluvial sandstone.||||||
262|Algebuckina Sandstone|61615|6|Mentioned|p302 Fig. 2|Jurassic|Middle Jurassic|Geological Province: Eromanga Basin.||||||07-FEB-11
262|Algebuckina Sandstone|61823|6|Mentioned|p118|Cretaceous|Jurassic|Mentioned only in terms of equivalents. Geological Province: Eromanga Basin||||||09-JUN-06
262|Algebuckina Sandstone|61836|5|Briefly described|p211|Jurassic|Jurassic|Kaolin-rich, thick sedimentary unit. Geological Province: Eromanga Basin.||||||05-OCT-06
262|Algebuckina Sandstone|62537|6|Mentioned|p191 Fig.2. |Late Jurassic|Middle Jurassic|Eromanga Basin.||||Overlies Hutton Sandstone and Poolowanna Formation. Is overlain by Namur Sandstone.||
262|Algebuckina Sandstone|63894|5|Briefly described|p169|Early Cretaceous|Jurassic|Aquifer. Underlies Cadna-owie Formation. Overlies Proterozoic rocks.||||||
262|Algebuckina Sandstone|63979|5|Briefly described|p37 Fig. 44|Callovian|Toarcian|Overlain by Cadna-owie Formation.||||||07-FEB-11
262|Algebuckina Sandstone|64197|6|Mentioned|p630 Fig.6|Early Cretaceous|Late Jurassic|Eromanga Basin.||||Underlies the Cadna-owie Formation.||
262|Algebuckina Sandstone|64665|5|Briefly described|p53 Fig.2, pp61-62.|Early Cretaceous|Early Jurassic|Eromanga Basin. Equivalent to Hutton Sandstone further east.||||Is overlain by Cadna-owie Formation.||
262|Algebuckina Sandstone|65238|5|Briefly described|p3, p5 Fig. 6, p7 Fig. 8|Jurassic|Jurassic|Geological province: Eromanga Basin. Braided fluvial deposits. See also p10, p14 Fig. 17.||||||
262|Algebuckina Sandstone|65309|4|Described|pp14-15,  pp19-20.|Jurassic|Jurassic|Fairly weathered outcrops preserved on summit and scarps of mesas and buttes in southeast Musgrave Block. Also known as De Souza Sandstone and, in Queensland, as Hooray Sandstone. Commonly 7-15m thick. Deposited by braided streams in broad plains.||||Overlies basement granite and gneiss. Disconformably overlies Idracowra Sandstone. Overlies Cadna-owie Formation in much of the Eromanga Basin. Probably unconformably overlies Langra Formation.|Friable, white, poorly sorted, kaolinitic, medium quartz sandstone; lesser well-rounded vein quartz conglomerate and angular quartz grit sandstone. Strongly cross-bedded.|
262|Algebuckina Sandstone|65342|6|Mentioned|p9.|||Eromanga Basin. Max. thickness at least 620 m.||||Is overlain by Cadna-owie Formation.||
262|Algebuckina Sandstone|65374|5|Briefly described|p30||Cretaceous|||||||
262|Algebuckina Sandstone|65376|5|Briefly described|p9 Fig.1.2. |Cretaceous|Jurassic||||||Fluvial to marginal marine sandstone.|
262|Algebuckina Sandstone|65385|5|Briefly described|pS128 Fig.2, pS133, pS134 Fig.7|Early Cretaceous|Early Jurassic|Of Eromanga Basin. Overlain by Cadna-owie Formation. Unit shown to contain two unconformities: Late Jurassic and around Jurassic-Cretaceous boundary. Sandstone, fine to coarse-grained, with granulite and pebble layers, and shale intraclasts. ||||||
262|Algebuckina Sandstone|65489|5|Briefly described|p17, p55, p58-62, p88, p96, p137, p139|Late Jurassic|Early Jurassic|See also p151, p154-156, p158-160. Eromanga Basin. 800m thick. Fair to excellent source and reservoir potential. Contains a hot groundwater resource of 130 degrees C at 2km depth. A component of the main artesian aquifer. Appears as Algebuckina Formation on p55 and 96.||||Overlies Poolowanna Formation. Is overlain by Cadna-owie Formation.|Sandstones with intraformational shales and coals.|
262|Algebuckina Sandstone|65925|5|Briefly described|p139, Appendix 2.|Mesozoic|Mesozoic||||||Fine- to coarse-grained sandstone with granule and pebble layers and shale intraclasts.|
262|Algebuckina Sandstone|66529|5|Briefly described|p10, p12 Fig.5|||Eromanga Basin. |||||Sandstone.|
262|Algebuckina Sandstone|66623|6|Mentioned|p247, p252.|||Equivalent in part to the Namur Sandstone.||||||
262|Algebuckina Sandstone|67058|5|Briefly described|p499 Fig. 3|Mesozoic|Mesozoic|Fluvial white kaolinitic sand||||||
262|Algebuckina Sandstone|67120|5|Briefly described|Map legend|Cretaceous|Jurassic||||||Sandstone, fine to coarse-grained, with granule and pebble layers, and shale intraclasts.|
262|Algebuckina Sandstone|67462|5|Briefly described|Map legend.|Late Jurassic|Jurassic|Eromanga Basin.||||Is overlain by Cadna-owie Formation.||
262|Algebuckina Sandstone|67474|5|Briefly described|p56|||coarse-grained, unconsolidated sandstone with conglomerate bands. Aquifer unit in Great Artesian Basin.||||||21-DEC-11
262|Algebuckina Sandstone|68068|5|Briefly described|Map legend|Early Cretaceous|Early Jurassic|Eromanga Basin. Subsurface only. Replaces Namur and Hutton Sandstones as they lens out towards the margin of the Basin.||||Is overlain by Hutton Sandstone.|Undifferentiated alluvial and fluvial deposits, chiefly white, medium- to coarse-grained, quartzose and pebbly, kaolinitic.|
262|Algebuckina Sandstone|68128|5|Briefly described|p14, p27, p43, p53, p71, p77, p83|Mesozoic|Mesozoic|Gawler Craton.|||||Sandstone, fine to coarse-grained with granule and pebble layers and shale intraclasts.|
262|Algebuckina Sandstone|68131|5|Briefly described|p2 Fig.1, p77|Cretaceous|Jurassic|Fluvial to marginal marine deposits. Mapped with Cadna-owie Formation as one unit.|||||Sandstone.|
262|Algebuckina Sandstone|68713|6|Mentioned|p22|Cretaceous|Jurassic|Fluvial sedimentation - mostly derived from the Bopeechee Regolith.||||||
262|Algebuckina Sandstone|68715|6|Mentioned|p30 Fig.5|Berriasian|Bajocian|Eromanga Basin.||||||
262|Algebuckina Sandstone|68734|6|Mentioned|p218 Fig.2|||Eromanga Basin (SW). Fluvial to lacustrine. Pre-Barremian age.||||||16-JAN-17
262|Algebuckina Sandstone|69001|5|Briefly described|p11, pp15-17, p27, p33, p36, pp71-73|Early Cretaceous|Jurassic|Equivalent to locally defined units of McMinn (1981b) and/or Morton (1982) such as the Gum Vale Beds or Gum Vale Formation. Recent interpretations by the NSW DPI broadly group the Namur Sandstone, Poolowanna Formation, Hutton Sandstone, Birkhead Formation, Adori Sandstone, Westbourne Formation, and Murta Formation as equivalents to Algebuckina Sandstone also.||||Underlain by the Easter Monday Formation. Equivalent to the Cadna-Owie Formation and the Gum Vale Beds.|Terrestrial sediments: dominantly moderate- to high energy, cross-bedded fluvial sandstone and conglomerate.|08-NOV-13
262|Algebuckina Sandstone|69004|6|Mentioned|p12, p15|Cretaceous|Jurassic|Eromanga Basin.||||||
262|Algebuckina Sandstone|69019|3|Fully described|p83 Fig.20, p85-87, p168.|Early Cretaceous|Early Jurassic|SW Eromanga Basin. Of Wopfner et al. (1970) after Freytag et al. (1967). Type area is ~3 km S of Algebuckina Hill. Thickness varies from 5 to 114 m. A significant regional aquifer. Has been affected by silcrete processes.||||Overlies Poolowanna Formation. Is overlain gradationally to disconformably by Cadna-owie Formation or Parabarana Sandstone.|White or greyish, medium- to coarse-grained widespread non-marine quartzose and kaolinitic fluvial sandstone.|
262|Algebuckina Sandstone|69023|5|Briefly described|p79, p87, p89-91, p191-192|Early Cretaceous|Early Jurassic|Eromanga Basin. From ~167 to ~192m thick. In W Eromanga Basin, passes laterally into Namur Sandstone. Stratigraphic wells intersection data.||||Overlies Epsilon Formation. Lateral equivalent of Namur Sandstone. Is overlain by Murta Formation, and conformably by Parabarana Sandstone and Cadna-owie Formation.||
262|Algebuckina Sandstone|69203|6|Mentioned|p12|Jurassic|Jurassic|||||||
262|Algebuckina Sandstone|69372|6|Mentioned|p38|Jurassic|Jurassic|Eromanga Basin.|||||Kaolinite and sandstone.|
262|Algebuckina Sandstone|69454|5|Briefly described|p38:3, 7 Fig.38.6; 38:12-15|Early Cretaceous|Jurassic|Eromanga Basin. Has fair to good reservoir potential, sealed by Cadna-owie Formation basal shale.||||Overlies Poolowanna Formation.||12-JUL-16
262|Algebuckina Sandstone|69457|4|Described|p41:2-8, 14-16|Early Cretaceous|Early Jurassic|Wopfner et al. (1970). A thick (757m ) unit, widely distributed along western Eromanga Basin. Mapped as De Souza Sandstone in KULGERA, FINKE and RODINGA map areas, and as Hooray Sandstone in ILLOGWA CREEK map area. Fluviatile deposits. Mainly exposed as mesas and buttes. Laterally equivalent to a succession consisting of Hutton Sandstone, Birkhead Formation, Adori Sandstone, Westbourne Formation, Namur Sandstone and Murta Formation. Toarcian to Berriasian age. Contains a zone of manganese enrichment at Umbeara. Has significant petroleum source potential; contained a 15m residual oil column in Blamore-1. May form reservoirs sealed by "Murta Member"/Cadna-owie Formation; it has good to excellent porosity and permeability, and forms a major artesian aquifer.||||Conformably (locally disconformably/unconformably) overlies, and intertongues with, Poolowanna Formation. Is overlain conformably by Cadna-owie Formation.|A thick succession of fine- to coarse-grained, quartzic continental sandstone, with granule and pebble layers; minor shale and siltstone. Shale intraclasts are common in coarser beds. Contains a variety of plant macrofossils.|12-JUL-16
262|Algebuckina Sandstone|69554|6|Mentioned|p131|Jurassic|Jurassic|Northern Gawler Craton.||||||
262|Algebuckina Sandstone|69562|6|Mentioned|p667 Fig.4, p668|Cretaceous|Jurassic|||||||
262|Algebuckina Sandstone|69594|6|Mentioned|p524|||||||Conformably ovelries Poolowanna Formation.||
262|Algebuckina Sandstone|69648|5|Briefly described|p20, p28, p33, map legend|Early Cretaceous|Late Jurassic|Of Eromanga Basin. Interpreted equivalents, with latest Jurassic to Early Cretaceous palynofloras, have been intersected in Maralinga drillholes 3B, 6, and 7 (Alley, 1993). Reworking of Algebuckina Sandstone contributes to unnamed Quaternary donga and playa lake sediments on OOLDEA.|||||Interpreted equivalents: off-white, kaolinitic clay, in part sandy to gritty, and sandstone; faceted pebbles occur at base, and muscovite and pyrite are locally present; unit passes up into carbonaceous clay, silt and sand.|
262|Algebuckina Sandstone|69673|6|Mentioned|p160, p161|||Good reservoir rock. ||||Overlain by Cadna-owie Formation, overlies Poolowanna Formation||
262|Algebuckina Sandstone|69797|5|Briefly described|p17 Fig.2|||Age: Middle Jurassic - Early Cretaceous (approximated from figure). Geol. Prov: Eromanga Basin.||||||
262|Algebuckina Sandstone|69946|3|Fully described|p11-17,p19,p38,p44,p51,p56-57,p62-67|Early Cretaceous|Early Jurassic|Sprigg (1958). Type locality defined, and a reference section near Mount Anna given, by Wopfner et al. (1970). Eromanga Basin. Lateral equivalents include Hutton, Adori and Namur Sandstones and Birkhead, Westbourne and Murta Formations in the Cooper region. Up to 800m thick.||||Intertongues with and overlies Poolowanna Formation. Correlated with De Souza Sandstone (NT). Is overlain conformably by Cadna-owie Formation.|White, fine- to coarse-grained quartzose sandstone with granule and pebble layers and shale intraclasts common in coarser beds; minor lenses of siltstone and shale are locally developed.|
262|Algebuckina Sandstone|69947|5|Briefly described|p3, p13 Fig.7.2|Late Jurassic|Middle Jurassic|Eromanga Basin. Sand-rich lowstand deposits form significant hydrocarbon reservoirs.||||||
262|Algebuckina Sandstone|69948|6|Mentioned|Figs.4.1, 18|||Eromanga Basin.||||Overlies Purni Formation and (locally) Crown Point Formation unconformably, and Poolowanna Formation conformably. Is overlain by Cadna-owie Formation.||
262|Algebuckina Sandstone|70336|5|Briefly described|Map legend|Cretaceous|Jurassic||||||Fine- to coarse-grained sandstone with granule and pebble layers and shale intraclasts.|
262|Algebuckina Sandstone|70338|5|Briefly described|Map legend.|Cretaceous|Jurassic||||||Sandstone, fine- to coarse-grained, with granule and pebble layers and shale intraclasts.|
262|Algebuckina Sandstone|70383|5|Briefly described|p45|||Eromanga Basin. Fluvial sediments.||||Is overlain by Cadna-owie Formation and Bulldog Shale.||
262|Algebuckina Sandstone|70789|5|Briefly described|p320-321, p325|Late Jurassic|Late Jurassic|Gawler Craton. AFT results tabulated; central ages from 166 +/- 174 Ma to a more robust 255 +/- 25 Ma. This name is used interchangeably with Algebuckina Formation (see references p318, p324, p326, p328-329).||||||
262|Algebuckina Sandstone|70821|5|Briefly described|p21|Early Cretaceous|Jurassic|Eromanga Basin.||||Lateral equivalent to Hooray Sandstone.|Strongly cross-bedded fluvial sandstone.|
262|Algebuckina Sandstone|70823|5|Briefly described|p43|Early Cretaceous|Late Jurassic|Eromanga Basin. ||||Overlain by the Namur Sandstone.||
262|Algebuckina Sandstone|70938|5|Briefly described|p807-808, p814, p816|Late Jurassic|Late Jurassic||||||Medium- to coarse-grained sandstone, silicified at the top and containing plant fossils.|
262|Algebuckina Sandstone|71321|4|Described|p1,4,9,15,24-27,30, 65-66,68|Neocomian|Early Jurassic|Of Eromanga Basin. Deposited in a braided fluvial environment (Alexander et al., 2006). Forms a major artesian aquifer and a potential hydrocarbon reservoir rock (Cotton, et al., 2006); also a key target for sediment-hosted uranium mineralisation (Wilson et al., 2012). See p25 for detailed lithological descriptions from field observations. Spore-pollen microfossil assemblage indicate an Early Jurassic to Early Cretaceous (Neocomian) age range (Krieg et al., 1995). Traditionally difficult to differentiate Cadna-owie Formation from the underlying Algebuckina Formation in the TIEYON area, and included as part of Algebuckina Formation in the TIEYON area.||||Confomably overlain by Cadna-owie Formation or Bulldog Shale. Correlable with De Souza Sandstone. Overlies the Poolowanna Formation and basement unconformably.|Sandstone, fine- to coarse-grained, quartzose, with granule and pebbly layers, and shale intraclasts. Minor lenses of siltstone and shale are locally developed.|24-OCT-19
262|Algebuckina Sandstone|71342|3|Fully described|Ch 1 p6, Ch 1 p19, Ch4 p8, Ch4 p25|Valanginian|Toarcian|Eromanga Basin. Hosts a major confined aquifer. First introduced by Sprigg (1958b) for 'A gently dipping sequence of cross-bedded grits and sandstones'. In 1970 Wopfner et al defined the type section. In the Northern Territory the Algebuckina Sandstone is correlated with the lower De Souza Sandstone. A maximum thickness of 800m is recorded in the Poolowanna Trough. Spore-pollen zone is given in Ch5 p57. Equivalent to the Hutton Sandstone, Birkhead Formation, Adori Sandstone, Westbourne Formation, Namur Sandstone and Murta Formation. Seal and reservoir characteristics discussed in Ch11. See also Ch5 p11-p12, Ch5 p14, Ch5 p17, Ch5 p19, Ch5 p30-p31, Ch5 p38, Ch5 p44, Ch5 p51, Ch5 p56-p57, Ch5 p62-p67, Ch6 p5-p7, Ch6 p14, Ch6 p18, Ch7 p3, Ch7 p13, Ch8 p4, Ch8 p28, Ch9 p3-p4, Ch9 p9-p11, Ch9 p18, Ch9 p21, Ch11 p4, Ch12 tbl 12.1, Ch12 p12-p14, Ch14 p3, Ch14 p5-p7.||||Conformably overlies the Poolowanna Formation. Unconformably overlies the Purni Formation or the Mount Toondina Formation. Conformably overlain by the Cadna-owie Formation.|White, fine to coarse-grained quartzose sandstone with granule and pebble layers and shale intraclasts common in the coarser beds. Minor lenses of siltstone and shale also occur.|
262|Algebuckina Sandstone|71348|6|Mentioned|p202|||Geological province: Gawler Craton.||||||
262|Algebuckina Sandstone|71415|5|Briefly described|p12|Early Cretaceous|Early Cretaceous|Geological province: SW Thomson Orogen. Of the Kooneberry Belt; of Eromanga Basin.||||Laterally equivalent to Namur Sandstone.||
262|Algebuckina Sandstone|71416|5|Briefly described|Map legend.|Cretaceous|Jurassic||||||Sandstone, massive to low-angle trough cross-bedded, immature, poorly to moderately sorted, medium- to coarse-grained quartzose fluvial sandstones containing angular to subrounded granules and pebbles of milky vein quartz.|
262|Algebuckina Sandstone|72298|5|Briefly described|p801|Cretaceous|Jurassic|Eromanga Basin (SA). Main confined aquifers, generally producing flowing artesian water bores.||||Overlies Poolowanna FZ. Is overlain by Cadna-owie FZ.||
262|Algebuckina Sandstone|72461|6|Mentioned|p24|Mesozoic|Mesozoic|||||||
262|Algebuckina Sandstone|72476|6|Mentioned|p36 Fig.9|||Eromanga Basin. Time-temperature thermal history diagram.||||||
262|Algebuckina Sandstone|72478|5|Briefly described|p6, p25-26, p82-83[doc],|Early Cretaceous|Late Jurassic|See also p51, 61, p70, p74 [of the document]. Aquifer is discussed.|c. 152 Ma-130 Ma|||Unconformably overlies the Mt Toondina Formation. Unconformably underlies the Cadna-owie Formation.||29-MAR-21
262|Algebuckina Sandstone|73099|5|Briefly described|Map legend.|Early Cretaceous|Late Jurassic|Eromanga basin.||||Overlies Mount Toondina Formation unconformably. Is overlain conformably by Cadna-owie Formation (Neales River Group).|Grey, pebbly, medium to coarse quartz sandstone with white claystone interbeds; clayey sandstone.|
262|Algebuckina Sandstone|73251|6|Mentioned|p54, p62|Cretaceous|Jurassic|Eromanga Basin. Hosts an aquifer in the northern Lake Frome district[?]||||Equivalent to Murta Formation, Namur Sandstone, Westbourne Formation, Adori Sandstone, Birkhead Formation, and Hutton Sandstone.||
262|Algebuckina Sandstone|73281|6|Mentioned|Appendix (DIP)|Jurassic|Jurassic|See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
291|Allaru Mudstone|12597|5|Briefly described|p492 Tb.1, p500|Albian|Albian|Eromanga Basin. 150-400m thick. Mis-spelt as Allura Mudstone in Tb.1.|||||Calcareous mudstone with interbeds of calcareous siltstone and fine-grained, partly calcareous labile sandstone; contains a rich marine fauna of bivalves, ammonites, gastropods and belemnites.|
291|Allaru Mudstone|13497|5|Briefly described|p115 fig 6.33|Early Cretaceous|Early Cretaceous|Eromanga Basin. Mis-spelt as the  Alluru Mudstone on p146. See also p144 fig 9.2, p145, p146, p148-p154 .||Marree Subgroup||Overlies the Toolebuc Formation. Overlain by the Mackunda Formation.||
291|Allaru Mudstone|13516|6|Mentioned|p167 fig 10, p169 fig 11, p171 fig 12|Late Cretaceous|Albian|In Eromanga Basin.||||||
291|Allaru Mudstone|22747|6|Mentioned|p15|||||||||
291|Allaru Mudstone|22857|5|Briefly described|p296-7 Tb.22.1, p314|Albian|Albian|Of the Rolling Downs Group. Black and grey claystone. Max. thickness: ~100m. (inc. Toolebuc Mudstone). Geological Province: Eromanga Basin. See also p312-3 Fig. 22.6, p544 App.1 Tb.A1.12.||||||
291|Allaru Mudstone|22865|4|Described|p314,Table22.1p296-7|Cenomanian|Albian|||||||
291|Allaru Mudstone|22883|5|Briefly described|Fig2 P30||Early Cretaceous|Overlying unit is Mackunda Formation, underlying unit is Toolebuc Formation||||||
291|Allaru Mudstone|22912|5|Briefly described|33|||Geological province: Eromanga  Basin.||||||30-JAN-07
291|Allaru Mudstone|23054|6|Mentioned|Fig5p22|||||||||
291|Allaru Mudstone|23056|6|Mentioned|12 table 2|||||||||
291|Allaru Mudstone|23065|5|Briefly described|18|||Geological province: Carpentaria Basin. Of the Rolling Downs Group.||||||30-JAN-07
291|Allaru Mudstone|23154|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Geological Province - Eromanga Basin. Of the Marree Subgroup (Neales River Group).||||||30-JAN-07
291|Allaru Mudstone|23155|4|Described|p32|Albian|Albian|Allaru Mudstone is laterally equivalent to the middle and upper parts of the Oodnadatta Formation, and the name Allaru Mudstone is only used when Toolebuc Formation is present.  The unit is Albian in age based on spore-pollen assemblages.||||||29-APR-10
291|Allaru Mudstone|23375|4|Described|Fig2 p265||Albian|Laterally equivalent to upper Oodnadatta Formation. In the Eromanga Basin.||||||30-JAN-07
291|Allaru Mudstone|23393|5|Briefly described|p24|Early Cretaceous|Early Cretaceous|Of Rolling Downs Group.||||||
291|Allaru Mudstone|23425|4|Described|Table 9.7 p394||Albian|Also see p378. Of Rolling Downs Group. Overlain by Normanton Formation; underlain by Toolebuc Formation - conformable. Geological Province Carpentaria Basin. Max. thickness 700 m.||||||16-SEP-08
291|Allaru Mudstone|23518|5|Briefly described|p13|Mesozoic|Mesozoic|Of Rolling Downs Group.  Geological Province: Carpentaria Basin.||||||
291|Allaru Mudstone|23883|5|Briefly described|p129 Fig. 11.2|Cretaceous|Cretaceous|Of Rolling Downs Group.  Geological Province: Great Australian Superbasin.||||||
291|Allaru Mudstone|23911|5|Briefly described|p97 Fig. 11|Cretaceous|Cretaceous|Geological Province: Eromanga Basin.  Of the Rolling Downs Group.||||||
291|Allaru Mudstone|23916|6|Mentioned|p534|Albian|Albian|||||||
291|Allaru Mudstone|23982|5|Briefly described|p35 Fig.7|Cretaceous|Cretaceous|Of Rolling Downs Group. Geological Province: Great Artesian Basin.||||||
291|Allaru Mudstone|24048|5|Briefly described|p76|||||||||
291|Allaru Mudstone|24073|5|Briefly described|p378 Table 2|Early Cretaceous|Early Cretaceous|Of Rolling Downs Group. Geological Province: Carpentaria Basin.||||||
291|Allaru Mudstone|24085|5|Briefly described|p33, p36|Albian|Albian|||||||
291|Allaru Mudstone|24092|5|Briefly described|p8 Fig.3|||Of Rolling Downs Group. Geological Province: Eromanga Basin.||||||
291|Allaru Mudstone|24175|5|Briefly described|p28, p17 Fig. 3|Albian|Albian|Supersedes Allaru Member.  Transitionally overlain by Mackunda Formation.  Geological Province: Eromanga Basin.||||||
291|Allaru Mudstone|24204|5|Briefly described|p263 Fig.4, p267, p282 Fig.21|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||17-DEC-04
291|Allaru Mudstone|24210|5|Briefly described|p133 Fig. 2|Early Cretaceous|Early Cretaceous|Of the Marree Subgroup.  Geological Province: Cooper Basin.||||||
291|Allaru Mudstone|24243|5|Briefly described|p3 Fig.2|Cretaceous|Cretaceous|Of Rolling Downs Group.||||||
291|Allaru Mudstone|29591|6|Mentioned|Table 72|||||||||
291|Allaru Mudstone|30019|6|Mentioned|p2|||||||||
291|Allaru Mudstone|30020|5|Briefly described|p30|||||||||
291|Allaru Mudstone|30095|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|30103|6|Mentioned|p6|||||||||
291|Allaru Mudstone|30104|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|30446|6|Mentioned|p38|||||||||
291|Allaru Mudstone|30539|6|Mentioned|p28|||Late middle Albian age||||||
291|Allaru Mudstone|30584|4|Described|Table 1|||||||||
291|Allaru Mudstone|30585|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|30691|4|Described|p17|||See also Table4,6.Lower Cretaceous. Part of Wilgunya Sub-group.||||||30-JAN-07
291|Allaru Mudstone|30804|5|Briefly described|Table 2|||||||||
291|Allaru Mudstone|30853|5|Briefly described|Table 3|||Albian age.||||||
291|Allaru Mudstone|30854|4|Described|Table 4|||Upper Albian age||||||
291|Allaru Mudstone|30855|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|Unit of Rolling Downs Group||||||
291|Allaru Mudstone|30856|4|Described|Table 3|||Lower Cretaceous||||||
291|Allaru Mudstone|30857|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|30914|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
291|Allaru Mudstone|31098|6|Mentioned|p10|||||||||
291|Allaru Mudstone|31121|6|Mentioned|Table 2|||||||||
291|Allaru Mudstone|31144|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|31145|5|Briefly described|Table 1|||L. Cretaceous||||||
291|Allaru Mudstone|31164|14|Not recorded|p8||Albian|Blue grey mudstone minor calcareous labilie sandstone and cone-in-cone limestone,marine.||||||
291|Allaru Mudstone|31168|6|Mentioned|p10|||||||||
291|Allaru Mudstone|31208|6|Mentioned|Fig. 7|||||||||
291|Allaru Mudstone|31422|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Of the Rolling Downs Group.  Mudstone, minor limestone and labile sandstone.||||||02-DEC-04
291|Allaru Mudstone|31425|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|31430|5|Briefly described|Table 1|||L.Cretaceous||||||
291|Allaru Mudstone|31431|5|Briefly described|Table 3|||L.Cretaceous||||||
291|Allaru Mudstone|31432|4|Described|Table 1|||L.Cretaceous||||||
291|Allaru Mudstone|31433|5|Briefly described|p6|||L.Cretaceous||||||
291|Allaru Mudstone|31434|3|Fully described|Table 1|||See also p8. L.Cretaceous||||||17-JUL-06
291|Allaru Mudstone|31436|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|31437|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|31438|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|31440|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|31441|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|31443|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|31553|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|32274|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|32275|5|Briefly described|p9|||||||||
291|Allaru Mudstone|32277|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|32314|6|Mentioned|Fig. 4|||||||||
291|Allaru Mudstone|32392|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|32393|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|32395|4|Described|p6|||Stratigraphic table||||||
291|Allaru Mudstone|32396|6|Mentioned|p6,8||Early Cretaceous|Palynomorphs ? Cenomanian. Marine.||||||
291|Allaru Mudstone|32553|4|Described|p38|||||||||
291|Allaru Mudstone|32705|6|Mentioned|p188|||||||||
291|Allaru Mudstone|32796|6|Mentioned|p303|||||||||
291|Allaru Mudstone|33016|6|Mentioned|Table 1|||||||||
291|Allaru Mudstone|33017|6|Mentioned|p5|||||||||
291|Allaru Mudstone|33067|4|Described|Table 1|Early Cretaceous|Early Cretaceous|Of the Rolling Downs Group.||||||07-JUL-04
291|Allaru Mudstone|33069|4|Described|p7|||L.-U. Cret. Rolling Downs Gp.||||||22-DEC-09
291|Allaru Mudstone|33072|4|Described|Table 1|||L.Cret.||||||
291|Allaru Mudstone|33073|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|33075|6|Mentioned|Table 1|||||||||
291|Allaru Mudstone|33078|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|33079|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|33082|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|33083|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|33086|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower to Upper Cretaceous||||||
291|Allaru Mudstone|33087|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||22-DEC-09
291|Allaru Mudstone|33088|4|Described|Table 3|||L.Cret.||||||
291|Allaru Mudstone|33089|4|Described|Table 2|||L.Cret.||||||
291|Allaru Mudstone|33092|6|Mentioned|p6|||Strat. table.||||||
291|Allaru Mudstone|33095|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|33096|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|33150|4|Described|p8|||L.Cret.||||||
291|Allaru Mudstone|33151|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|33165|6|Mentioned|Chart|||Correlation chart only||||||
291|Allaru Mudstone|33175|6|Mentioned|p280|||||||||
291|Allaru Mudstone|33176|6|Mentioned|p171|||||||||
291|Allaru Mudstone|33177|6|Mentioned|p12|||||||||
291|Allaru Mudstone|33178|6|Mentioned|p11|||||||||
291|Allaru Mudstone|33179|6|Mentioned|Table 3|||||||||
291|Allaru Mudstone|33182|6|Mentioned|Fig.1|||L. Cretaceous||||||
291|Allaru Mudstone|33183|5|Briefly described|p227|||Underlies Normanton Formation.||||||30-JAN-07
291|Allaru Mudstone|33368|6|Mentioned|p24|||Geol.Map.||||||
291|Allaru Mudstone|33372|6|Mentioned|Table 1|||||||||
291|Allaru Mudstone|33414|6|Mentioned|p212,213,Tb.|||part of Wilgunya Sub-Group||||||
291|Allaru Mudstone|33448|6|Mentioned|p6|||||||||
291|Allaru Mudstone|33449|6|Mentioned|p7|||||||||
291|Allaru Mudstone|33561|6|Mentioned|p102|||||||||
291|Allaru Mudstone|33638|5|Briefly described|Table 1|||Lower Cret.||||||
291|Allaru Mudstone|33639|5|Briefly described|p11|||L.Cret. See also Table 4||||||
291|Allaru Mudstone|33640|4|Described|Table 2|||L.Cret.||||||
291|Allaru Mudstone|33642|5|Briefly described|p145,147,151,Table 1|||||||||
291|Allaru Mudstone|33643|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|33644|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|33647|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|33648|6|Mentioned|p21|||Strat.||||||
291|Allaru Mudstone|33772|6|Mentioned|p13|||||||||
291|Allaru Mudstone|33773|6|Mentioned|p17|||||||||
291|Allaru Mudstone|33825|6|Mentioned|Table 4|||||||||
291|Allaru Mudstone|33832|5|Briefly described|p11|||Strat. and correlation||||||17-JUL-06
291|Allaru Mudstone|33900|6|Mentioned|p21|||||||||
291|Allaru Mudstone|33964|4|Described|p6|||||||||
291|Allaru Mudstone|34065|4|Described|p6|||L.Cret.||||||
291|Allaru Mudstone|34091|4|Described|Table 1|||L.Cretaceous. Of the Rolling Downs Group.||||||30-JAN-07
291|Allaru Mudstone|34174|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|34217|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|34218|5|Briefly described|Table 2|||Lower Cretaceous.||||||
291|Allaru Mudstone|34356|6|Mentioned|p21|||Lower Cretaceous.||||||
291|Allaru Mudstone|34485|6|Mentioned|Table 1|||See also Table 2. Lower Cretaceous||||||
291|Allaru Mudstone|34486|4|Described|Table 1|||See also Table 2. Lower Cretaceous||||||
291|Allaru Mudstone|34487|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|34611|4|Described|Fig.65|||Wilgunya Sub-Group.||||||16-SEP-08
291|Allaru Mudstone|34619|6|Mentioned|p.160, Pl.22||Early Cretaceous|||||||
291|Allaru Mudstone|34811|4|Described|Table 1|||||||||
291|Allaru Mudstone|35121|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|35139|4|Described|Table.2|||||||||
291|Allaru Mudstone|35239|6|Mentioned|p258|||||||||
291|Allaru Mudstone|35253|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|35560|6|Mentioned|Fig.3|||||||||
291|Allaru Mudstone|35640|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|35663|6|Mentioned|Fig.2|||Subsurface correlations of the central basin rock units.||||||
291|Allaru Mudstone|35811|5|Briefly described|Table 3|||||||||
291|Allaru Mudstone|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
291|Allaru Mudstone|36012|3|Fully described|Table 5|||See also p20.||||||17-JUL-06
291|Allaru Mudstone|36228|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
291|Allaru Mudstone|36243|6|Mentioned|Table 6A|||||||||
291|Allaru Mudstone|36251|4|Described|p3|||||||||
291|Allaru Mudstone|36552|6|Mentioned|Fig.25|||||||||
291|Allaru Mudstone|36571|6|Mentioned|p98|||See also Table 4.||||||
291|Allaru Mudstone|37263|6|Mentioned|Fig.14|||||||||
291|Allaru Mudstone|37451|6|Mentioned|Table 2|||||||||
291|Allaru Mudstone|37608|3|Fully described|Table 1|||See also Table 2||||||
291|Allaru Mudstone|38226|6|Mentioned|Table 1|||||||||
291|Allaru Mudstone|38372|6|Mentioned|p651|||||||||
291|Allaru Mudstone|38373|6|Mentioned|p622|||||||||
291|Allaru Mudstone|38608|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
291|Allaru Mudstone|38780|6|Mentioned|p17|||||||||
291|Allaru Mudstone|38814|6|Mentioned|Table 1|||||||||
291|Allaru Mudstone|39029|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Overlies Toolebuc Formation.||||||25-AUG-04
291|Allaru Mudstone|39070|4|Described|p365|||||||||
291|Allaru Mudstone|39211|5|Briefly described|Fig.3|||See also Figs 9,11-16,19 etc. Correlation||||||
291|Allaru Mudstone|39445|5|Briefly described|Table 11|||||||||
291|Allaru Mudstone|39478|6|Mentioned|Table 1|||||||||
291|Allaru Mudstone|39556|5|Briefly described|Map legend|Cretaceous|Cretaceous|||||||
291|Allaru Mudstone|39575|6|Mentioned|p103|||||||||
291|Allaru Mudstone|39708|6|Mentioned|p478|||||||||
291|Allaru Mudstone|39797|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|39799|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|39846|6|Mentioned|Fig.2|||||||||
291|Allaru Mudstone|39847|5|Briefly described|p40|||||||||
291|Allaru Mudstone|39899|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
291|Allaru Mudstone|39943|6|Mentioned|Table 8A|||||||||
291|Allaru Mudstone|39989|4|Described|p424|||||||||
291|Allaru Mudstone|40121|6|Mentioned|Table 1|||||||||
291|Allaru Mudstone|40199|6|Mentioned|Fig.1|||||||||
291|Allaru Mudstone|40249|6|Mentioned|p41|||||||||
291|Allaru Mudstone|40452|6|Mentioned|p2|||||||||
291|Allaru Mudstone|40623|5|Briefly described|p111|||||||||
291|Allaru Mudstone|40648|6|Mentioned|p12|||||||||
291|Allaru Mudstone|40670|6|Mentioned|Fig.9|||||||||
291|Allaru Mudstone|40675|6|Mentioned|Table 8A|||||||||
291|Allaru Mudstone|40687|3|Fully described|p418|||||||||
291|Allaru Mudstone|40801|6|Mentioned|p42|||||||||
291|Allaru Mudstone|40833|6|Mentioned|p468|||||||||
291|Allaru Mudstone|40926|6|Mentioned|p18|||||||||
291|Allaru Mudstone|41012|5|Briefly described|p137|||||||||
291|Allaru Mudstone|41060|6|Mentioned|Fig.3|||Generalized stratigrapgy||||||
291|Allaru Mudstone|41062|6|Mentioned|Fig.5|||||||||
291|Allaru Mudstone|41063|6|Mentioned|p40|||||||||
291|Allaru Mudstone|41064|6|Mentioned|Fig.4|||||||||
291|Allaru Mudstone|41084|5|Briefly described|Fig.2|||||||||
291|Allaru Mudstone|41086|3|Fully described|p98, Fig.3|||||||||
291|Allaru Mudstone|41087|3|Fully described|p127|||||||||
291|Allaru Mudstone|41088|6|Mentioned|p141|||||||||
291|Allaru Mudstone|41097|6|Mentioned|Table 1|||||||||
291|Allaru Mudstone|41099|6|Mentioned|Fig.9|||||||||
291|Allaru Mudstone|41117|6|Mentioned|Fig.2|||||||||
291|Allaru Mudstone|41121|6|Mentioned|p179|||||||||
291|Allaru Mudstone|41165|5|Briefly described|p362|||See also Fig.15||||||
291|Allaru Mudstone|41175|6|Mentioned|Fig.1|||||||||
291|Allaru Mudstone|41176|6|Mentioned|Table 2|||||||||
291|Allaru Mudstone|41177|6|Mentioned|p225|||||||||
291|Allaru Mudstone|41178|6|Mentioned|p242|||||||||
291|Allaru Mudstone|41182|5|Briefly described|Fig.2|||||||||
291|Allaru Mudstone|41183|6|Mentioned|Fig.3 p308|||||||||
291|Allaru Mudstone|41187|6|Mentioned|Fig.2|||||||||
291|Allaru Mudstone|41214|6|Mentioned|Fig.3|||||||||
291|Allaru Mudstone|41216|6|Mentioned|Fig.18|||||||||
291|Allaru Mudstone|41266|6|Mentioned|Fig.3|||||||||
291|Allaru Mudstone|41306|6|Mentioned|p4|||||||||
291|Allaru Mudstone|41307|6|Mentioned|p5|||||||||
291|Allaru Mudstone|41464|6|Mentioned|Map legend|Early Cretaceous||||||||
291|Allaru Mudstone|41523|3|Fully described|p279|||See also p281.||||||
291|Allaru Mudstone|41556|6|Mentioned|Map legend|Early Cretaceous||||||||
291|Allaru Mudstone|41568|5|Briefly described|p15|||||||||
291|Allaru Mudstone|42003|6|Mentioned|p141|||||||||
291|Allaru Mudstone|42061|5|Briefly described|p157|||See also Fig.11||||||
291|Allaru Mudstone|42071|6|Mentioned|p117|||See also Fig.2A p116||||||
291|Allaru Mudstone|42084|6|Mentioned|Fig.3 P356|||||||||
291|Allaru Mudstone|42085|6|Mentioned|Fig.2 P374|||||||||
291|Allaru Mudstone|42397|6|Mentioned|Fig.2 P3|||||||||
291|Allaru Mudstone|42429|6|Mentioned|Fig.10 P156|||||||||
291|Allaru Mudstone|42446|4|Described|p14|||||||||
291|Allaru Mudstone|42447|6|Mentioned|Fig.1|||||||||
291|Allaru Mudstone|42496|5|Briefly described|p136, Fig.3 p132|||||||||
291|Allaru Mudstone|42520|5|Briefly described|p6|||||||||
291|Allaru Mudstone|42588|5|Briefly described|p115|||||||||
291|Allaru Mudstone|42637|5|Briefly described|p11|||||||||
291|Allaru Mudstone|42673|5|Briefly described|Fig.2, P184|||||||||
291|Allaru Mudstone|42746|6|Mentioned|Fig.6 P8|||||||||
291|Allaru Mudstone|42749|6|Mentioned|Fig.2 P27|||||||||
291|Allaru Mudstone|42804|5|Briefly described|p115|||||||||
291|Allaru Mudstone|43002|5|Briefly described|Fig.2,p135|||||||||
291|Allaru Mudstone|43004|5|Briefly described|Table 1,p179|||||||||
291|Allaru Mudstone|43105|6|Mentioned|p15|||||||||
291|Allaru Mudstone|43114|5|Briefly described|p16|||||||||
291|Allaru Mudstone|43122|5|Briefly described|Fig.2.|||||||||
291|Allaru Mudstone|43591|6|Mentioned|p40|||||||||
291|Allaru Mudstone|43602|6|Mentioned|191|||In Eromanga Basin, Rolling Downs Group||||||
291|Allaru Mudstone|43630|6|Mentioned|p70|||also Fig.4||||||
291|Allaru Mudstone|44016|14|Not recorded|Map Legend||Early Cretaceous|||||||
291|Allaru Mudstone|44017|14|Not recorded|Map Legend||Early Cretaceous|||||||
291|Allaru Mudstone|44018|14|Not recorded|Map Legend||Early Cretaceous|||||||
291|Allaru Mudstone|44019|14|Not recorded|Map Legend||Early Cretaceous|||||||
291|Allaru Mudstone|44020|14|Not recorded|Tb.1,2||Early Cretaceous|Of Rolling Downs Gruop.||||||
291|Allaru Mudstone|44031|14|Not recorded|p3,Tb.1,p8||Cretaceous|||||||
291|Allaru Mudstone|44034|4|Described|Tb.1,p2,4,5,9,10|||||||||
291|Allaru Mudstone|44042|14|Not recorded|Map Legend||Early Cretaceous|||||||
291|Allaru Mudstone|44082|6|Mentioned|p3,4,10,12,20,24,28||Albian|Mentioned with respect to Qld Cretaceous fossils which are either of stratigraphic significance or are illustrative of the occurrence of a particular group.||||||
291|Allaru Mudstone|44091|14|Not recorded|p60|||Part of Wilgunya Sub-Group.||||||
291|Allaru Mudstone|44098|14|Not recorded|p98||Cretaceous|||||||
291|Allaru Mudstone|44112|6|Mentioned|p82|||||||||
291|Allaru Mudstone|44133|5|Briefly described|p104 Fig. 9.11, 122|Cretaceous|Cretaceous|Geological Province: Eromanga Basin. Conformably underlies: Mackunda Formation.||||||
291|Allaru Mudstone|44308|14|Not recorded|p11|||||||||
291|Allaru Mudstone|44410|14|Not recorded|Map Legend||Early Cretaceous|||||||
291|Allaru Mudstone|44807|14|Not recorded|p3,Tb.1,p8||Cretaceous|||||||
291|Allaru Mudstone|45103|6|Mentioned|p8|||||||||
291|Allaru Mudstone|45110|6|Mentioned|Table 18|||||||||
291|Allaru Mudstone|45132|6|Mentioned|p17|||||||||
291|Allaru Mudstone|45145|3|Fully described|Table 5|||||||||
291|Allaru Mudstone|45161|6|Mentioned|p67|||||||||
291|Allaru Mudstone|46791|5|Briefly described|p48|||||||||
291|Allaru Mudstone|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
291|Allaru Mudstone|46939|6|Mentioned|Fig.1|||See also Table 1.||||||
291|Allaru Mudstone|47042|6|Mentioned|p171|||||||||
291|Allaru Mudstone|48920|3|Fully described|p61|||Cretaceous age||||||
291|Allaru Mudstone|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
291|Allaru Mudstone|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
291|Allaru Mudstone|50100|5|Briefly described|p23|Cretaceous|Cretaceous|Of the Rolling Downs Group.  Geological Province: Carpentaria Basin.||||||
291|Allaru Mudstone|50332|5|Briefly described|p22|Mesozoic|Mesozoic|Geological Province: Carpentaria Basin. Main lithologies are mudstone, calcareous shale, limestone, sandstone and siltstone.||||||07-FEB-11
291|Allaru Mudstone|60087|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Of the Rolling Downs Group.  Mudstone, minor limestone, labile sandstone.||||||19-JUL-04
291|Allaru Mudstone|60331|5|Briefly described|p34 Fig.3|Albian|Albian|Overlies Toolebuc Formation. Overlain by the Mackunda Formation. Geological Province: Eromanga Basin.||||||
291|Allaru Mudstone|60359|5|Briefly described|Map Legend|Mesozoic|Mesozoic|Mudstone, calcareous siltstone.||||||
291|Allaru Mudstone|60717|5|Briefly described|p40 Fig. 2|Early Cretaceous|Early Cretaceous|Overlies Toolebuc Formation. Overlain by Mackunda Formation. Interfingers laterally with Oodnadatta Formation. Geological Province: Eromanga Basin.||||||31-JAN-08
291|Allaru Mudstone|61014|6|Mentioned|p533 Fig.2.|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Wallumbilla Formation.||
291|Allaru Mudstone|61312|5|Briefly described|p75, p79 Table E2|Cretaceous|Cretaceous|Of Rolling Downs Group. In Queensland, consists of mainly blue-grey mudstone with interbeds of thin calcareous siltstone. Forms marine deposits in deeper parts of the Eromanga Basin. Absent in NSW. Overlies Toolebuc Formation. See also p64, p67 Fig. E5||||||
291|Allaru Mudstone|61611|6|Mentioned|p265 Fig. 3|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||13-MAR-09
291|Allaru Mudstone|61613|6|Mentioned|p282 Fig. 2|Late Cretaceous|Early Cretaceous|Of Maree Subgroup. Geological Province: Eromanga Basin.||||||07-FEB-11
291|Allaru Mudstone|61615|6|Mentioned|p302 Fig. 2|Early Cretaceous|Early Cretaceous|Of Marree Subgroup. Geological Province: Eromanga Basin.||||||07-FEB-11
291|Allaru Mudstone|62028|5|Briefly described|p10 Fig. 1|||||||||
291|Allaru Mudstone|62029|5|Briefly described|p15 Fig. 4|Cretaceous|Cretaceous|||||||
291|Allaru Mudstone|62376|5|Briefly described|p84|Early Cretaceous|Early Cretaceous|Geological Province: Pedirka Basin?||||||11-FEB-10
291|Allaru Mudstone|62837|5|Briefly described|Stratigraphic columns|Late Cretaceous|Early Cretaceous|Of the Rolling Downs Group.  Age: ~96-~94Ma. Geological Province: Northern Gulf of Carpentaria, Southern Cape York and Burketown Depression.||||||01-MAR-10
291|Allaru Mudstone|63113|6|Mentioned|p1219 Fig.8. |||||||Overlies Lawn Hill Formation.||
291|Allaru Mudstone|63979|2|Defined|p49, p51-52, Fig. 44|Albian|Albian|Top unit of Wilgunyah Subgroup (Rolling Downs Gp). Formerly Allaru Member (Wilgunyah Fm). Conformable on Toolebuc Formation or Wallumbilla Formation;conformable below Mackunda Fm. Max.thick: 400m. Detailed lithology provided. Geol.prov: Eromanga Basin|||||Primarily blue-grey mudstone (partly pyritic) and interbedded calcareous siltstone, cone-in-cone limestone and lesser sandstone.|29-APR-16
291|Allaru Mudstone|64048|6|Mentioned|p64 Tb. 2|||Geological Province: Eromanga Basin.||||||07-FEB-11
291|Allaru Mudstone|64197|6|Mentioned|p625 Fig.1c, p630 Figs.6,7|Cretaceous|Cretaceous|Eromanga Basin.||Unit in Marree Subgroup.||Overlies Toolebuc Formation; is overlain by Mackunda Formation.||10-DEC-15
291|Allaru Mudstone|64778|6|Mentioned|p13|Cretaceous|Cretaceous|Pedirka and Simpson Desert Basins.||||||
291|Allaru Mudstone|64820|5|Briefly described|pS6 Fig. 4|Albian|Albian|Of the Rolling Downs Group. Medium-grained galuconitic sandstone grading up into interbedded siltstone and sandstone. Geological province: Weipa Sub-basin, Carpentaria Basin.||||||
291|Allaru Mudstone|65238|5|Briefly described|p7 Fig. 8|Early Cretaceous|Early Cretaceous|Geological province: Eromanga Basin. Transgressive marine deposits.||||||17-FEB-10
291|Allaru Mudstone|65385|5|Briefly described|pS134 Fig.7|Late Cretaceous|Early Cretaceous|Of Eromanga Basin. Overlies Toolebuc Formation. Overlain by Mackunda Formation.||||||08-MAR-12
291|Allaru Mudstone|65489|5|Briefly described|p49, p55, p58-59, p61, p96, p155|Early Cretaceous|Early Cretaceous|Eromanga Basin. 300m thick. Appears as Allaru Formation on p155. Regional seal.||||Overlies Toolebuc Formation. Is overlain by Mackunda Formation.||
291|Allaru Mudstone|65925|5|Briefly described|Appendix 2.|||||||||
291|Allaru Mudstone|66529|5|Briefly described|p10, p12 Fig.5|||Eromanga Basin. ||Unit in Rolling Downs Group.|||Deeper marine shale and mudstone.|
291|Allaru Mudstone|66623|3|Fully described|p242, pp256-257, pp264-266.|Albian|Albian|Formerly a member of Wilgunya Formation (Casey 1959), Allaru Member (Vine and Day 1965), reinstated as a Formation (Vine et al. 1967). Very poorly exposed: mudstone-dominated and masked by silcrete gibbers. Thickness from 87 m to 270 m. Wide range of fossils. Partly equivalent to Griman Creek and Oodnadatta Formations,Yalpunga Formation, lower half of Yalpunga Beds, and to the diachronous base of Mackunda Formation.||Unit in Rolling Downs Group.||Is conformably overlain by Winton Formation. In QLD, overlies Toolebuc Formation and underlies Mackunda Formation. Gradationally overlies Coreena Member (Wallumbilla Formation).|Blue shale with interbedded buff to grey, calcareous, fossiliferous fine silty sandstone, siltstone and mudstone; local gypsiferous concretions of calcareous, chocolate-brown shale exhibit cone-in-cone structures.|07-JUN-13
291|Allaru Mudstone|66915|5|Briefly described|p6 Fig.3|Cretaceous|Cretaceous|Carpentaria and Eromanga Basins.||||||
291|Allaru Mudstone|67209|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||Unit in Rolling Downs Group.||Overlies Coreena Member of Wallumbilla Formation. Is overlain by Cordillo Silcrete.|Regressive marine and non-marine grey claystone with silty and sandy intervals up-sequence.|
291|Allaru Mudstone|67211|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||Unit in Rolling Downs Group.|||Regressive marine and non-marine grey claystone with silty and sandy intervals up-sequence.|
291|Allaru Mudstone|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map|Late Cretaceous|Late Cretaceous|See also p86-87, p92-93, p94 Fig.12.4, p95 Fig.12.5, p96. Eromanga/Carpentaria Basins. Widespread shallow-marine deposits.||||Overlies Toolebuc Formation. Is overlain by Mackunda, Normanton Formations.|Mudstone, calcareous siltstone.|
291|Allaru Mudstone|67402|4|Described|p26, p26 tbl RRM4, p29, p29 fig PSA4|Albian|Albian|Eromanga Basin. Maximum thickness of 400m in the Eromanga Basin but may be up to 700m thick in the Carpentaria Basin. Proven regional seal for hydrocarbons. See also PSA5, p108-p112, p113 fig ERO12, p115 tbl ERO2, p123, p176, p177, p179 fig CRP/KRM6, p181.||Rolling Downs Group||Overlies the Wallumbilla Formation. Overlain by the Mackunda Formation.|Consists primarily of marine mudstone interbedded with calcareous siltstone, very fine-grained, laminated sandstone, shale and limestone.|
291|Allaru Mudstone|67784|6|Mentioned|p28-29, p33|Albian|Albian|See also references to Allaru Formation (p25-26, p32).||||||08-FEB-18
291|Allaru Mudstone|67870|5|Briefly described|p46-47, p50-52|Late Cretaceous|Late Cretaceous|Hydrocarbon seal.|||||Shaly limestone, marl, organic-rich (10% TOC) limestone, sandstone.|
291|Allaru Mudstone|68206|6|Mentioned|p32|Albian|Albian|NE Eromanga Basin. See also references to Allaru Formation (p31, 33).||||||
291|Allaru Mudstone|68279|6|Mentioned|p18-19|||Galilee Basin stratigraphic cross-sections, and mineralogy tables.||||||
291|Allaru Mudstone|68553|6|Mentioned|Map legend; schematic diagram.|Cretaceous|Cretaceous|Eromanga and Carpentaria Basins.||Unit in Rolling Downs Group.||Conformably overlies Toolebuc Formation. Is overlain conformably by Mackunda Formation.||
291|Allaru Mudstone|68731|6|Mentioned|pp209-211|||||||||
291|Allaru Mudstone|68734|5|Briefly described|p218 Fig.2, p221 Fig.3|Albian|Albian|Eromanga Basin (NE). Shallow marine.||Of the Rolling Downs Group.||||
291|Allaru Mudstone|69019|5|Briefly described|p85 Fig.21.|Albian|Albian|Southern Eromanga Basin.||||Overlies Toolebuc Formation. Is overlain by Winton and Mackunda Formations.||
291|Allaru Mudstone|69023|6|Mentioned|p89 Fig.20, p102, p105|Albian|Albian|||||Lateral equivalent of Oodnadatta Formation.||
291|Allaru Mudstone|69056|6|Mentioned|Reference images sheet.|||Shown on the simplified surface geology map of the Quamby Project area.||||||
291|Allaru Mudstone|69297|5|Briefly described|p273, p274 fig 4. 3, p275|Upper Cretaceous|Upper Jurassic|Carpentaria Basin. This unit is a good potential seal. ||Rolling Downs Group||Overlies the Toolebuc Formation. Overlain by the Normanton Formation.|Mudstone, siltstone and claystone.|
291|Allaru Mudstone|69454|6|Mentioned|p38:3|||Eromanga Basin.||||||12-JUL-16
291|Allaru Mudstone|69455|6|Mentioned|p39:4 Fig.39.3|Early Cretaceous|Early Cretaceous|||||||12-JUL-16
291|Allaru Mudstone|69457|3|Fully described|p41:2-3;41:5 Fig.41.4;41:6-8,10-12,17-18|Early Cretaceous|Early Cretaceous|Vine and Day (1965); Vine et al. (1967). Widely distributed: Eromanga and Carpentaria Basins. Entirely subsurface in NT. Quiet water, shallow-marine deposits; generally 200-300m thick, up to 400m. Laterally equivalent to middle and upper parts of Oodnadatta Formation; this latter name was previously used to describe the Allaru Mudstone in the NT. Late Albian to ?early Cenomanian age range from palynoflora. The basal part of this unit contains a 40m thick gas-charged interval, and has untested unconventional petroleum potential.||Wilgunya Subgroup.||Conformably overlies Toolebuc or Wallumbilla Formations. Is overlain conformably by Mackunda Formation. Correlative of Oodnadatta Formation.|Mostly blue-grey, partly pyritic mudstone with calcareous siltstone interbeds, cone-in-cone limestone; minor sandstone and limestone. Contains a rich fossil assemblage.|12-JUL-16
291|Allaru Mudstone|69582|5|Briefly described|p22, p25-p26, p29, p65-p66|Upper Cretaceous|Lower Cretaceous|Eromanga Basin. Deposited in a marine depositional environment. Intersected in GSQ Longreach 2 drillhole.||||Overlies the Toolebuc Formation. Overlain by the Normation Formation and the Mackunda Formation.|Mudstone.|
291|Allaru Mudstone|69594|4|Described|p518-519, p521-522, p526, p529-530|Albian|Albian|See also p531 Fig.7.11, p574. Vine et al. (1967); Vine and Day (1965). Carpentaria, Eromanga Basins. Generally 200-300m thick; up to 350-400m. Generally poor surface expression. Contains rich shallow-marine late Albian macrofauna and microfauna (listed and photographs). Seismic interpretations suggest a significant intraformational unconformity. Appears as Allaru Formation in Fig.7.11.||Rolling Downs Group.||Conformably overlies Toolebuc Formation. Is overlain (conformably) by Normanton, Winton and Mackunda Formations. Is correlated with the Oodnadatta Formation.|Claystone, siltstone, cone-in-cone calcareous mudstone, minor limestone, labile volcanic-derived sandstone, glauconitic sandstone and sporadic coquinite.|
291|Allaru Mudstone|69673|5|Briefly described|ix, p155 fig 127, p156|||Prospective for unconventional hydrocarbons. 200-300m thick.||Wilgunya Subgroup||Overlies Toolebuc Formation, overlain by Mackunda Formation|Mudstone, in parts pyritic with thin interbeds of calcareous siltstone, cone in cone limestone and minor very fine grained sandstone and concretionary limestone.|
291|Allaru Mudstone|69797|5|Briefly described|p17 Fig.2|Early Cretaceous|Early Cretaceous|Geol. Prov: Eromanga Basin.||||||
291|Allaru Mudstone|69946|3|Fully described|p23, p26-27, p57, p94|Early Cretaceous|Early Cretaceous|Of Casey (1959), who assigned it as the uppermost Member of the Wilgunya Formation. Renamed Allaru Member by Vine and Day (1965); raised to Formation status as Allaru Mudstone by Vine et al. (1967). Type section is on the Richmond-Winton Road, from Richmond S to Twenty-Mile Creek. Its extent is limited by definition to the extent of the Toolebuc Formation. Generally 100-240m thick, to >600m. Late Albian. Wireline log correlations.||||Conformably overlies Toolebuc Formation. Is overlain conformably by Mackunda Formation. Passes laterally into Oodnadatta Formation.|Grey mudstone with thin calcareous siltstone and minor thin, very fine-grained sandstone interbeds identical to the Oodnadatta Formation.|
291|Allaru Mudstone|69947|5|Briefly described|p13 Fig.7.2|Early Cretaceous|Early Cretaceous|Eromanga Basin.||Marree Subgroup.||||
291|Allaru Mudstone|69948|6|Mentioned|Fig.4.18|||Eromanga Basin.||||Overlies Toolebuc Formation. Is overlain by Mackunda Formation.||
291|Allaru Mudstone|70354|5|Briefly described|Map legend|Cretaceous|Cretaceous|||Rolling Downs Group.||Overlies Toolebuc Formation.|Mudstone and calcareous siltstone.|
291|Allaru Mudstone|70572|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|||Wilgunya Subgroup|||Mudstone, calcareous siltstone.|20-JAN-22
291|Allaru Mudstone|70649|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||Rolling Downs Group|||Regressive marine and non-marine grey claystone with silty and sandy intervals up-sequence.|20-JAN-22
291|Allaru Mudstone|70821|4|Described|p21 Fig.2.6, p22 Fig.2.7, p23, p30, p33|Early Cretaceous|Early Cretaceous|See also p80, p82. Surat Basin. Not an equivalent of Oodnadatta Formation.  87m thick in Toompine 1 well; 212.5m thick in Mirintu 1 petroleum well. Low-energy marine deposits. Biotas include benthic and nektonic molluscs, turtles, fish, pliosaurs and a dinosaur. Hydrostratigraphic properties.||Rolling Downs Group.||Conformably overlies Toolebuc Formation or Wallumbilla Formation. Is overlain conformably by Mackunda Formation.|Includes minor calcareous labile (volcanic) sandstone. Includes coquinite beds and hummocky crossbeds.|
291|Allaru Mudstone|70824|5|Briefly described|p9|Cretaceous|Cretaceous|Eromanga Basin.||||Overlies the Toolebuc Formation. Overlain by the Mackunda Formation.||
291|Allaru Mudstone|70860|6|Mentioned|p281|||Great Artesian Basin.||||||
291|Allaru Mudstone|71321|6|Mentioned|p15|||Of Eromanga Basin.||||Overlies the Toolebuc Formation. Overlain by the Mackunda Formation.||24-OCT-19
291|Allaru Mudstone|71342|3|Fully described|Ch3 p4, Ch4 p25|Albian|Albian|Eromanga Basin. Originally named by Casey (1959) as the uppermost member of the Wilgunya Formation. Vine and Day (1965) assigned the name Allaru Member before Vine et al (1967) elevated the mudstone to formation status. Replaces the obsolete Tambo Formation. Casey (1959) assigned the type section on the Richmond-Winton road from Richmond south to Twenty-Mile Creek in Queensland. This unit is generally 100-240m thick in the Cooper region but reaches thicknesses in excess of 600m in the Patchawarra Trough. Deposited in a low energy, shallow marine environment. Spore-pollen zone is given in Ch5 p57. Forms a seal for the Coorikiana Sandstone. See also  Ch5 p23-p27, Ch5 p57, Ch7 p13, Ch11 p5.||||Conformably overlies the Toolebuc Formation. Conformably overlain by the Mackunda Formation.|Grey mudstone with thin calcareous siltstone and minor thin, very fine-grained sandstone interbeds identical to the Oodnadatta Formation.|
291|Allaru Mudstone|71382|5|Briefly described|p4, p9, p11, p13, p16-p17|||Eromanga Basin. Intersected in GSQ Julia 1 from 0-156.65m for a total of 156.65m thickness. Deposited during widespread shallow marine conditions. Temp log and stratlog are provided. Lithology is described in detail on p22. See also p21-p23, p25, p27, App 3, 4.||||Overlies the Toolebuc Formation.|Mudstone interbedded with sandstone.|07-OCT-22
291|Allaru Mudstone|71601|6|Mentioned|p120, p121|Albian|Albian|NW Qld. Includes dinosaur fossils provisionally assigned to Minmi.||||||
291|Allaru Mudstone|71855|4|Described|p2, p4-p5, p9-p10, p13, p15, p27|Cretaceous|Cretaceous|Eromanga and Carpentaria basins. Wireline log responses were described for this unit including Gamma-ray, sonic transit time and resistivity. Structure is discussed. See also p33-p35, p50, p52-p53, p56-p57, p61-p62, p75.||||Conformably (gradationally) overlies the Toolebuc Formation.|Light grey, predominantly non-calcareous mudstone, and calcareous in part mudstone.|
291|Allaru Mudstone|71863|5|Briefly described|p4-p5, p7-p9|Albian|Albian|Eromanga Basin and Carpentaria basins. Deposited in a marine incursion.||Rolling Downs Group||Conformably overlies the Toolebuc Formation. Overlain by the Normanton Formation, Mackunda Formation and the Winton Formation.||
291|Allaru Mudstone|72297|5|Briefly described|p753|||Eromanga Basin.||||Conformably overlies the Toolebuc Formation.||
291|Allaru Mudstone|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA,QLD,NSW), Carpentaria Basin.||Rolling Downs Group.||Overlies Toolebuc FZ. Is overlain by Mackunda or Normanhurst FZ.||
291|Allaru Mudstone|72913|6|Mentioned|p8.|||Two wells intersected this cover unit.|||||Includes mudstone.|
291|Allaru Mudstone|72967|6|Mentioned|p5|||Carpenteria Basin.||Rolling Downs Group||||
291|Allaru Mudstone|73083|6|Mentioned|p62, p77|Cretaceous|Cretaceous|||||||
291|Allaru Mudstone|73137|6|Mentioned|p6|Cretaceous|Cretaceous|||||||
291|Allaru Mudstone|73144|6|Mentioned|p8, p13|Cretaceous|Cretaceous|Carpentaria Basin. Leaky aquitard.||Rolling Downs Group||Underlain by Toolebuc Formation. Overlain by Normanton Formation.||
291|Allaru Mudstone|73147|5|Briefly described|p129|Aptian|Aptian|||Rolling Downs Group.||Overlies Toolebuc Formation. Is overlain by Normanton Formation.||
291|Allaru Mudstone|73167|6|Mentioned|p664 Fig. 2|Cretaceous|Cretaceous|Eromanga Basin.||||||
291|Allaru Mudstone|73249|5|Briefly described|p319, p321||Albian|Eromanga Basin.||||Lateral equivalent to the Oodnadatta Formation, overlies the Allaru Formation, underlies the Mackunda Formation.|Siltstone and mudstone dominated.|
291|Allaru Mudstone|73251|6|Mentioned|p62|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Underlain by Toolebuc Formation. Overlain by Mackunda Formation. Equivalent to Oodnadatta Formation.||
291|Allaru Mudstone|73281|6|Mentioned|Appendix (DIP)|||See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
291|Allaru Mudstone|73343|6|Mentioned|p337|Cretaceous|Cretaceous|Eromanga Basin.||||Underlain by Toolebuc Formation. Overlain by Mackunda Formation. Equivalent to Oodnadatta Formation.||
291|Allaru Mudstone|73479|5|Briefly described|p156 Fig.2, p159|Cretaceous|Cretaceous|Eromanga Basin. Open shallow marine depositional environment.|ca 100 Ma|||Overlies Toolebuc Formation, underlies Mackunda Formation||
303|Allia Creek Granite|22809|6|Mentioned|13|||||||||
303|Allia Creek Granite|24197|5|Briefly described|p18, p105 Tb. 15.1|Paleoproterozoic|Paleoproterozoic|Of the Allia Creek Suite. Age: ~1845Ma. Geological province: Litchfield Block/Pine Creek Inlier.||||||07-FEB-11
303|Allia Creek Granite|32170|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
303|Allia Creek Granite|33376|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
303|Allia Creek Granite|33377|6|Mentioned|Table 1|||Stratigraphy||||||
303|Allia Creek Granite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
303|Allia Creek Granite|39889|6|Mentioned|p486|||||||||
303|Allia Creek Granite|41660|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Biotite adamellite, often coarsely porphyritic with large phenocrysts of microcline; some xenoliths; associated muscovite-tourmaline quartz microcline pegmatites.||||||07-NOV-08
303|Allia Creek Granite|41661|3|Fully described|p17|||||||||
303|Allia Creek Granite|41980|5|Briefly described|Table 3 P575|||||||||
303|Allia Creek Granite|42012|6|Mentioned|p33|||||||||
303|Allia Creek Granite|45003|14|Not recorded|p77|||||||||
303|Allia Creek Granite|45022|14|Not recorded|p146,304||Carpentarian|Pet. Description on Tech.File D/52-12||||||02-MAR-18
303|Allia Creek Granite|45087|5|Briefly described|p19|||Chemical analyses.||||||
303|Allia Creek Granite|45112|5|Briefly described|Table 4|||||||||
303|Allia Creek Granite|48942|3|Fully described|p30|||||||||
303|Allia Creek Granite|50586|5|Briefly described|p1.1, 3.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Of the Allia Suite.||||||07-NOV-08
303|Allia Creek Granite|63866|5|Briefly described|p107|||Litchfield Province, Pine Creek Orogen.||||||
303|Allia Creek Granite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age 1820-1850Ma. I-type. Biotite adamellite, commonly coarsely porphyritic with large phenocrysts of microcline, some xenoliths, assoc. muscovite-tourmaline-quartz pegmatites. Intrudes Burrell Creek Formation, unconf. overlain by Depot Creek Sandstone.||||||10-FEB-10
303|Allia Creek Granite|64956|5|Briefly described|p2 Tb. 1, p47-49|Paleoproterozoic|Paleoproterozoic|Has hornfels contact with Burrell Creek Formation. Max. intrusion age: 1806+/-7Ma. Geological province: Pine Creek Orogen. Has distinctive K-feldspar megacrysts up to 60mm in length; also contains sedimentary/metasedimentary xenoliths.||||||07-FEB-11
303|Allia Creek Granite|65232|6|Mentioned|App. 2|||||||||09-FEB-10
303|Allia Creek Granite|67167|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Unit in Allia Creek Suite.|||Biotite quartz monzonite, commonly coarsely porphyritic with large phenocrysts of microcline, some xenoliths, associated muscovite-tourmaline-quartz pegmatites.|
303|Allia Creek Granite|67232|5|Briefly described|p5. |Paleoproterozoic|Paleoproterozoic|Litchfield Province, Pine Creek Orogen. An S-type granitoid, much younger than typical such intrusions which are aged 1863 - 1850 Ma.|1806 Ma (Worden et al. 2008a).|||||
303|Allia Creek Granite|69420|5|Briefly described|p5:18-19, 28, 85, 109|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Mineralogy and petrology/geochemistry summarised. SHRIMP U-Pb zircon age.|1806 +/- 7 Ma: Worden et al. (2008).|Allia Creek Suite.|||Coarse porphyritic biotite quartz monzonite/granodiorite: large microcline phenocrysts to 60mm.|12-JUL-16
303|Allia Creek Granite|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|1805+/-6.8 Ma crystallisation: U-Pb zircon SHRIMP||||K-feldspar-megacrystic biotite granite.|
332|Alsace Quartzite|22438|6|Mentioned|p549, Fig.12|||||||||
332|Alsace Quartzite|22585|6|Mentioned|Fig3 P738|||Actually written as Alsace Qtz. in text.||||||17-JUL-06
332|Alsace Quartzite|23031|5|Briefly described|24|||Geol. Province: Mount Isa Fold Belt. Of the Myally Subgroup.||||||09-SEP-14
332|Alsace Quartzite|23395|5|Briefly described|p386 Fig.3|||Of Myally Subgroup.||||||17-JUL-06
332|Alsace Quartzite|23396|5|Briefly described|p407 Fig.2|||Of Myally Subgroup (Haslingden Group).||||||17-JUL-06
332|Alsace Quartzite|23518|4|Described|p11|Proterozoic|Proterozoic|Of Myally Subgroup. Geological Province: Western Fold Belt.||||||01-OCT-08
332|Alsace Quartzite|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Myally Subgroup (Haslingden Group). Overlies Eastern Creek Volcanics;  underlies Bortala Formation.||||||01-OCT-08
332|Alsace Quartzite|30534|2|Defined|p304|Carpentarian|Carpentarian|||||||
332|Alsace Quartzite|33900|4|Described|p12|||||||||
332|Alsace Quartzite|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
332|Alsace Quartzite|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
332|Alsace Quartzite|38232|6|Mentioned|p84|||||||||
332|Alsace Quartzite|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
332|Alsace Quartzite|39445|5|Briefly described|Table 2|||See also p40||||||17-JUL-06
332|Alsace Quartzite|39556|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||
332|Alsace Quartzite|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Myally Subgroup (Haslingden Group). Fine to coarse feldspathic sandstone and orthoquartzite. Overlies the Eastern Creek Volcanics.||||||15-JUN-06
332|Alsace Quartzite|39622|6|Mentioned|Fig.2|||||||||
332|Alsace Quartzite|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
332|Alsace Quartzite|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
332|Alsace Quartzite|40221|3|Fully described|p8|||||||||
332|Alsace Quartzite|40623|5|Briefly described|p99|||||||||
332|Alsace Quartzite|41298|6|Mentioned|Map legend|Carpentarian||||||||
332|Alsace Quartzite|41307|4|Described|p10|||||||||
332|Alsace Quartzite|42523|5|Briefly described|Fig. 2 P373|||||||||
332|Alsace Quartzite|45136|5|Briefly described|p49|||||||||
332|Alsace Quartzite|45166|5|Briefly described|p14|||See also p71||||||17-JUL-06
332|Alsace Quartzite|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
332|Alsace Quartzite|47083|4|Described|p7|||Oldest member of Myally Subgroup (Haslingden Group). O'lying unit Bortala Fm - conformable. U'lying unit Pickwick Metabasalt Member - conformable.||||||17-JUL-06
332|Alsace Quartzite|50332|6|Mentioned|p17|Proterozoic|Proterozoic|Of the Myally Subgroup.||||||07-FEB-11
332|Alsace Quartzite|50550|6|Mentioned|p1144 Fig.7||Statherian|Geological Province: Western Fold Belt.||||||19-DEC-07
332|Alsace Quartzite|61929|5|Briefly described|p128 Fig. 2|||Of the Myally Subgroup. ||||||
332|Alsace Quartzite|62988|5|Briefly described|p34|||Geological Province: Mount Isa Inlier.||||||25-JAN-07
332|Alsace Quartzite|63023|5|Briefly described|p1025 Fig. 2, p1208|Paleoproterozoic|Paleoproterozoic|Basal unit of Myally Subgroup (Haslingden Group). Overlies eastern Creek Volcanics (Haslingden Group). Age: 1779+/-5Ma. Geological Province: Leichhardt Superbasin. See also p1027 Tb. 1.||||||09-SEP-14
332|Alsace Quartzite|63109|6|Mentioned|p1108 Fig. 3|||Underlain by Eastern Creek Volcanics, overlain by Bortala Formation. Geological Province: Leichhardt Superbasin. Consists of sandstone.||||||
332|Alsace Quartzite|63111|5|Briefly described|p1163 Fig. 3|Statherian|Statherian|Of Myally Subgroup. Overlain by Bortalla Formation, underlain by Eastern Creek Volcanics. Age: 1779+/-5Ma.  Geological Province: Leichhardt Superbasin. Consists mostly of conglomerate.||||||07-FEB-11
332|Alsace Quartzite|63113|5|Briefly described|p1214 Fig.2, p1225 Fig.13.|||Appears as Alsace Qtz in Fig.2.||Of the Haslingden Group||Overlies Eastern Creek Volcanics. Is overlain by Bortala Formation.||
332|Alsace Quartzite|63114|5|Briefly described|p1253 Fig.2. |||||Of the Myally Subgroup||Overlies Eastern Creek Volcanics. Is overlain by Bortala Formation.||
332|Alsace Quartzite|63115|6|Mentioned|p1279 Fig.4.|||Leichhardt superbasin.||||||
332|Alsace Quartzite|63116|6|Mentioned|p1297 Fig.2,p1299 Tb.1, |||Leichhardt superbasin. Material properties detailed.||||||
332|Alsace Quartzite|63866|5|Briefly described|p58|||Leichhardt Superbasin.||Myally Supersequence||||
332|Alsace Quartzite|64834|5|Briefly described|p13 Fig.2|||Leichhardt Superbasin. Western Succession of Mount Isa Basin.||Myally Subgroup|||Conglomerate.|
332|Alsace Quartzite|65505|6|Mentioned|979|Proterozoic|Proterozoic|Contains detrital zircons aged 1780 Ma.||||||
332|Alsace Quartzite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot. Mount Isa Inlier, Leichhardt Superbasin.|1779 +/- 5 Ma (maximum depositional age).|Myally Subgroup.|||Fine to coarse feldspathic sandstone and orthoquartzite, minor siltstone.|
332|Alsace Quartzite|68732|5|Briefly described|p160, p161, p165 Fig.3|Statherian|Statherian|Shoreline facies deposited above fair-weather wave base. Of the Myally Supersequence. Maximum sedimentary depositional age.|1779 +/- 5 Ma|Of the Haslingden Group.|||Fine- to coarse-grained quartzites and arenites, fining upwards into thinly bedded sandstones.|30-NOV-17
332|Alsace Quartzite|69222|6|Mentioned|p222 Fig.2|Statherian|Statherian|Leichhardt River Fault Trough.||Myally Subgroup||Overlies Pickwick Metabasalt||
332|Alsace Quartzite|69591|4|Described|p33, p57|||Mount Oxide and Leichhardt River Domains, Leichhardt Superbasin. Also appears as Alsace Formation. Part of Myally Supersequence. Tide-dominated shelf deposits.|1779 +/- 5 Ma (MDA: Neumann et al., 2006).|Myally Subgroup.||Is overlain by Lochness Formation.|Fine to coarse feldspathic sandstone and orthoquartzite, minor siltstone.|
332|Alsace Quartzite|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Myally Subgroup.||Is overlain by Bortala Formation.|Fine- to coarse-grained feldspathic sandstone and orthoquartzite; minor siltstone.|
332|Alsace Quartzite|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Myally Subgroup.||Is overlain by Bortala Formation.|Fine- to coarse-grained feldspathic sandstone and orthoquartzite; minor siltstone.|
332|Alsace Quartzite|71592|5|Briefly described|Appendix A.|||Leichhardt River Domain, Mount Isa Orogen.|1779+/-5 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
332|Alsace Quartzite|71799|4|Described|p150 fig 2, p152|Statherian|Statherian|Lawn Hill. Deposited under fluviatile to lacustrine conditions. Ages are derived from Neumann et al, 2006 and also includes a tuff horizon dated at 1773 +/- 2 Ma (Neumann et al, 2006.|1779 +/- 5 Ma (max. dep. Age)|Myally Supergroup||Overlies the Pickwick Metabasalt (Eastern Creek Volcanics)|Quartzite, sandstone and greywacke.|03-OCT-18
332|Alsace Quartzite|71980|5|Briefly described|map legend sheet 1|Proterozoic|Proterozoic|Rythmic coarsening up coastal offlap sequences transitional upward into regressive coastal to inshore (lagoonal)deltaic and fan fringe facies.||Of Myally Subgroup||Transitional to overlying Bortala Formation.|Arkose, feldspathic sandstone, quartz arenite; some basalt.|
332|Alsace Quartzite|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Lawn Hill Platform and Leichhardt River Fault Trough of the Mount Isa Province.||Myally Subgroup||Overlies Eastern Creek Volcanics and underlies Bortala Formation.||
332|Alsace Quartzite|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Lawn Hill Platform and Leichhardt River Fault Trough of the Mount Isa Province.||Myally Subgroup||Overlies Eastern Creek Volcanics and underlies Bortala Formation.||
332|Alsace Quartzite|72919|6|Mentioned|p63|||||Myally Subgroup, Myally Supersequence||||
332|Alsace Quartzite|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Mount Isa Province, Leichhardt Superbasin.||Myally Subgroup||Underlain by Eastern Creek Volcanics. Overlain by Bortala Formation.||
332|Alsace Quartzite|73525|6|Mentioned|p4-5 Fig.2, p19 Fig.13|||Leichhardt River Domain.|||||Clastics.|
393|Amulda Member|22566|6|Mentioned|Fig 2 on p77|||Of the Parke Siltstone.||||||17-JUL-06
393|Amulda Member|22646|6|Mentioned|p 107|||Of the Parke Siltstone||||||17-JUL-06
393|Amulda Member|22760|5|Briefly described|p335|Late Devonian|Late Devonian|Of the Parke Siltstone.||||||17-JUL-06
393|Amulda Member|22761|6|Mentioned|p350|||Of the Parke Siltstone.||||||17-JUL-06
393|Amulda Member|31566|2|Defined|p237|Devonian|Devonian|See also p238||||||17-JUL-06
393|Amulda Member|35102|6|Mentioned|p39|||||||||
393|Amulda Member|41385|6|Mentioned|Fig.12|||||||||
393|Amulda Member|43225|5|Briefly described|Map Legend||Devonian|Of Pertnjara Group.||||||22-DEC-09
393|Amulda Member|43503|6|Mentioned|42-45|Late Devonian|Middle Devonian|||||||
393|Amulda Member|47050|6|Mentioned|Fig.2|||||||||
393|Amulda Member|67565|5|Briefly described|p42.|Devonian|Devonian|||Topmost unit in Parke Siltstone.||Overlies Dare Siltstone Member.|White to brown sandstone and sandy micaceous siltstone.|
393|Amulda Member|69438|4|Described|p23:38-39|||Jones (1972). Amadeus Basin. Type section is to the E of Areyonga, where it is c.135m thick. Thins to the S. Contains mudcracks and rarer rain pits; halite pseudomorphs are absent.||Parke Siltstone.||Conformably/gradationally overlies Dare Siltstone Member. Is overlain conformably/gradationally by Hermannsburg Sandstone.|Interbedded fine- to coarse-grained sandstone and sandy, micaceous siltstone; siltstone is more abundant towards the base and is laminated or massive.|12-JUL-16
393|Amulda Member|69673|6|Mentioned|p67|||||Parke Siltstone||||
409|Anamarra Orthogneiss|39887|6|Mentioned|Fig.3 p449|||||||||
409|Anamarra Orthogneiss|39888|6|Mentioned|Fig.8 p467|||||||||
409|Anamarra Orthogneiss|60547|5|Briefly described|Map Legend|Precambrian|Precambrian|Granitic gneiss, amphibolite.||||||
410|Anburla Anorthosite|23844|3|Fully described|p23|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Province. Max Thickness: <1000m. See also Fig. 14, 16, 17||||||07-NOV-08
410|Anburla Anorthosite|43225|5|Briefly described|Map Legend||Paleoproterozoic|||||||22-DEC-09
410|Anburla Anorthosite|43503|2|Defined|6,19,76|||||||||
410|Anburla Anorthosite|49831|5|Briefly described|p7|||Reserved as Anburla Leuconorite.  Supersedes Mount Hay Anorthosite.||||||
410|Anburla Anorthosite|60668|5|Briefly described|p9, p2 Tb. 1|||Intrusive rock. See also Figs. 18a and 18b. ||||||
410|Anburla Anorthosite|69427|5|Briefly described|p12:17, 20, 23|||Warren and Shaw (1995). Forms three separate bodies along a 38-km belt, SE from Mount Hay to near the Redbank Thrust. Interpreted as a cumulate which separated from the magma that formed the mafic component of Mount Hay Granulite.||||Is faulted against the Mount Hay Granulite.|Monomineralic plagioclase rock (anorthosite); more mafic variants with up to 30% ferromagnesian minerals; plagioclase-bearing mafic granulite (metagabbro); leucogabbro. Variably deformed.|12-JUL-16
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.|
466|Anmatjira Orthogneiss|23270|5|Briefly described|Table 1, p5||Proterozoic|of Arunta Block.||||||
466|Anmatjira Orthogneiss|23271|5|Briefly described|Map legend||Proterozoic|of Arunta Block. Age: Middle Proterozoic.||||||23-DEC-09
466|Anmatjira Orthogneiss|23844|5|Briefly described|p36|Paleoproterozoic|Paleoproterozoic|Porphyritic granitic gneiss and rapakivi granite. Intrudes the Mount Stafford beds and dolerites||||||07-NOV-08
466|Anmatjira Orthogneiss|24197|5|Briefly described|p19, p59 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Of the Harverson Suite. Coarse-grained, grey, granitic augen gneiss. Age: ~1820Ma. Geological province: Arunta Inlier.||||||07-FEB-11
466|Anmatjira Orthogneiss|37058|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
466|Anmatjira Orthogneiss|39888|6|Mentioned|Fig.8|||||||||
466|Anmatjira Orthogneiss|41964|5|Briefly described|p179|||||||||
466|Anmatjira Orthogneiss|42326|5|Briefly described|Table 2 P11|||||||||
466|Anmatjira Orthogneiss|48992|2|Defined|p6|Mesoproterozoic|Mesoproterozoic|||||||
466|Anmatjira Orthogneiss|50369|5|Briefly described|p1.3, 4.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Haverson Suite. Age: 1818 +/- 15Ma (Shrimp).||||||07-NOV-08
466|Anmatjira Orthogneiss|62378|6|Mentioned|p17|||Macroscopic similarities to the Redhackle Granite.||||||
466|Anmatjira Orthogneiss|64956|5|Briefly described|p3 Tb. 1, p12, p15|Paleoproterozoic|Paleoproterozoic|Has also been referred to as Anmatjira Granite and Mount Stafford Granite as it cross-cuts metamorphic isograds in the Mount Stafford beds in the Yundurbulu Range. Cryst. ages: 1798+/-3Ma, 1795+/-4Ma. Geological province: Arunta region.||||||07-FEB-11
466|Anmatjira Orthogneiss|65232|6|Mentioned|App. 2|||||||||09-FEB-10
466|Anmatjira Orthogneiss|65338|3|Fully described|p16, 21, p32-33, p69, App 2|Statherian|Orosirian|Constitutes much of Yundurbulu and Bilba Hills and an area encompassing Mount Stafford. Mineralogy, geochemistry and microstructure are detailed. Granite phase thought to comprise sub-concordant, relatively thin sheet-like bodies.|1798 +/- 3 Ma. Granitic phase 1795 +/- 4 Ma.|||Intrudes Lander Rock Formation, Weldon Metamorphics.  Intruded by Aloolya Gneiss.|An augen gneiss; less intensely deformed rapakivi granite in the northwest of the map area. The orthogneiss and migmatite locally form a hybrid diatexite which apparently transitions into megacrystic granite.|
466|Anmatjira Orthogneiss|65343|6|Mentioned|p3 Fig.4|||||||||
466|Anmatjira Orthogneiss|67164|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region; Aileron Province.|||||Biotite granite, rapakivi texture, tourmaline-bearing; also equigranular/seriate porphyritic, and orbicular textural variants; microgranite; locally gneissic.|
466|Anmatjira Orthogneiss|67892|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Arunta Region; Aileron Province.|||||Biotite granite, mantled K-feldspar phenocrysts (rapakivi texture), tourmaline-bearing; also equigranular/seriate porphyritic, and orbicular textural variants, microgranite; predominantly granitic, locally gneissic.|
466|Anmatjira Orthogneiss|69226|5|Briefly described|p239, p243, p247, p255-256|||Reynolds-Anmatjira Ranges region. Associated with the c.1780-1770 Ma Strangways Orogeny. Crustal heat production discussed.|||||Voluminous sheet-like granites; metamorphosed.|
466|Anmatjira Orthogneiss|69417|5|Briefly described|p2:5|Statherian|Orosirian|Aileron Province.|1820-1790 Ma.|||||12-JUL-16
466|Anmatjira Orthogneiss|69427|5|Briefly described|p12:3, 6, 20-21, 26, 44|Statherian|Statherian|Aileron Province. Previously (Stewart, 1981) included rocks now called the Stafford Granite. SHRIMP U-Pb zircon age.|1798 +/- 3 Ma (Worden et al., 2008).|||Intrudes Weldon Metamorphics and Tyson Creek Granulite. Is intruded by Aloolya Gneiss.|Foliated to gneissic megacrystic granite.|12-JUL-16
466|Anmatjira Orthogneiss|70376|6|Mentioned|p833 fig 2|Paleoproterozoic|Paleoproterozoic|Also shown as Anmatjira Granulites.||||||
466|Anmatjira Orthogneiss|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen.|1798+/-2.5 Ma crystallisation: U-Pb zircon SHRIMP||||Granite.|
466|Anmatjira Orthogneiss|71858|5|Briefly described|p5, p44, p54, p70|||Aileron Province.|||||Foliated biotite orthogneiss, typically with ovoid microcline megacrysts.|
466|Anmatjira Orthogneiss|73399|6|Mentioned|p2, App.E|||||||||
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.||||||
496|Anuma Schist|9199|5|Briefly described|Map legend|Precambrian|Precambrian|Of the Strangways Metamorphic Complex.  Kyanite schist, staurolite schist.  Geological Province: Arunta Block.||||||03-NOV-04
496|Anuma Schist|23983|5|Briefly described|p27|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
496|Anuma Schist|23984|5|Briefly described|p3 Fig.2|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
496|Anuma Schist|39887|6|Mentioned|Fig.3|||||||||
496|Anuma Schist|39888|6|Mentioned|Appendix|||Published isotopic ages.||||||
496|Anuma Schist|60547|5|Briefly described|Map Legend|Precambrian|Precambrian|Of the Strangways Metamorphic Complex. Kyanite schist, staurolite schist. Geological Province: Arunta Block.||||||06-JUN-05
496|Anuma Schist|69929|6|Mentioned|p233, 244|||N of the Winecke Range, Arunta Block.|||||A belt of strongly sheared rocks.|
513|Aquarium Formation|22538|6|Mentioned|Fig3 P709|||||||||
513|Aquarium Formation|22670|6|Mentioned|55|||Geol province McArthur Basin||||||
513|Aquarium Formation|22853|3|Fully described|10|Proterozoic|Proterozoic|Geol. province: McArthur Basin. Of the Tawallah Group. Max thickness 200 m. Overlies Wununmantyala Sandstone.||||||18-JUL-06
513|Aquarium Formation|23065|6|Mentioned|15|||Geol province: McArthur Basin. Of theTawallah Group. Overlying unit: Settlement Creek Volcanics, underlying unit: Sly Creek Sandstone||||||18-JUL-06
513|Aquarium Formation|23395|5|Briefly described|p388 Fig.4|||||||||
513|Aquarium Formation|23733|5|Briefly described|p32 Fig. 19|||Of Tawallah Group.  Geological Province: MacArthur Basin.||||||
513|Aquarium Formation|23776|5|Briefly described|p705 Fig 2|||Of Tawallah Group.||||||
513|Aquarium Formation|23910|5|Briefly described|p292 Fig. 3|||Of Tawallah Group.  Geological Province: McArthur Basin.||||||
513|Aquarium Formation|23963|5|Briefly described|p1238, 1239 Fig.2|||Geological Province: McArthur Basin. Of the Tawallah Group||||||03-MAR-05
513|Aquarium Formation|23968|6|Mentioned|p1362|||Geological Province: McArthur Basin.||||||
513|Aquarium Formation|24179|5|Briefly described|p84 Fig. 2|||Overlies the Wunnunmantyala Formation.  Overlain by the Settlement Creek Volcanics.  Geological Province:  McArthur Basin.||||||
513|Aquarium Formation|32660|5|Briefly described|Table 4|||||||||
513|Aquarium Formation|32904|6|Mentioned|p89|||||||||
513|Aquarium Formation|35114|6|Mentioned|p203|||||||||
513|Aquarium Formation|35640|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
513|Aquarium Formation|36012|3|Fully described|Table 2|||||||||
513|Aquarium Formation|36439|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
513|Aquarium Formation|36442|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
513|Aquarium Formation|37568|5|Briefly described|p78|||||||||
513|Aquarium Formation|38042|6|Mentioned|p160|||||||||
513|Aquarium Formation|38584|6|Mentioned|p14|||||||||
513|Aquarium Formation|39445|5|Briefly described|Table 2|||||||||
513|Aquarium Formation|40489|6|Mentioned|p89|||||||||
513|Aquarium Formation|40691|5|Briefly described|p9|||||||||
513|Aquarium Formation|41721|3|Fully described|p21|Proterozoic|Proterozoic|Of the Tawallah Group. Conformably overlies Sly Creek Sandstone; conformably overlain by Settlement Creek Volcanics. Thickness: 70m. Medium to coarse, moderately sorted, subangular to subrounded, galuconitic sandstone. Geological province: McArthur Basin.||||||01-AUG-07
513|Aquarium Formation|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
513|Aquarium Formation|42385|3|Fully described|p10, p8 Fig. 5, p9 tb. 3|Mesoproterozoic|Mesoproterozoic|Of the Tawallah Group. Max. thickness: 200m. Red, purple and grey dolostones, in places recrystallised; thinly bedded dololutite, silty dololutite and fine- to medium-grained dolarenite.||||||18-SEP-07
513|Aquarium Formation|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
513|Aquarium Formation|42638|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Age: Middle Proterozoic.||Of Tawallah Group.||In schematic section, underlies Wununmantyala Sandstone; overlies Rosie Creek Sandstone Member (Sly Creek Sandstone).|Dolostones, dololutite, dolarenite, shale, sandstone. Detailed lithology given.|07-NOV-11
513|Aquarium Formation|42639|4|Described|p10 Table 4 p11|||||||||
513|Aquarium Formation|42700|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
513|Aquarium Formation|42739|5|Briefly described|map legend|Statherian|Statherian|Of the Tawallah Group. Dolostone, mudstone, sandstone, dololutite, dolarenite, pebble breccia.||||||19-OCT-05
513|Aquarium Formation|42812|3|Fully described|p17, Table 3|||Of Tawallah Group||||||18-JUL-06
513|Aquarium Formation|43010|5|Briefly described|Fig.6||Mesoproterozoic|Of Tawallah Group. Of "Mid Proterozoic" age.||||||18-JUL-06
513|Aquarium Formation|43036|3|Fully described|p21|||Of Tawallah Group.||||||18-JUL-06
513|Aquarium Formation|44287|14|Not recorded|opp.p.7|||Equiv.of Rosie Creek Sandstone.||||||
513|Aquarium Formation|44305|14|Not recorded|p.6,12,21; opp 6,18|||(E53-8).||||||
513|Aquarium Formation|44306|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
513|Aquarium Formation|44436|5|Briefly described|p.8, opp. p.7, map|||(E53-4).||||||02-DEC-04
513|Aquarium Formation|44437|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Of the Tawallah Group.  Micaceous galuconitic siltstone, fine-grained quartz sandstone, minor dolomite, dolomitic siltstone.  Conformably overlain by Settlement Creek Volcanics.||||||07-NOV-08
513|Aquarium Formation|44530|14|Not recorded|p.9|||(D53-15).||||||
513|Aquarium Formation|45162|2|Defined|p27|Proterozoic|Proterozoic|||||||
513|Aquarium Formation|45166|5|Briefly described|p28|||||||||
513|Aquarium Formation|46804|6|Mentioned|p154|||||||||
513|Aquarium Formation|48894|6|Mentioned|p21|||1473my - 1601my (dated on glauconite)||||||
513|Aquarium Formation|60483|5|Briefly described|p7 Fig. 5, p29|||Of the Tawallah Group. Geological Province: McArthur Basin||||||
513|Aquarium Formation|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Tawallah Group. Overlain by Wununmantyala Sandstone, underlain by Sly Creek Sandstone.||||||
513|Aquarium Formation|60574|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Tawallah Group. Overlain by Serrlement Creek Dolerite. Brown to green, dolomitic, glauconitic siltstone, shale and minor sandstone; locally hornfelsed.||||||07-NOV-08
513|Aquarium Formation|63112|6|Mentioned|p1192, p1206 ||||||||Lower fine-grained sandstone and upper dololutites and dolomitic mudstone with glauconite, halite and anhydrite pseudomorphs.|
513|Aquarium Formation|63866|5|Briefly described|p54|||||Prize Supersequence||||
513|Aquarium Formation|64815|6|Mentioned|p4 Fig.2, p5 Fig.3|||||Of the Tawallah Group.||||
513|Aquarium Formation|64817|6|Mentioned|p353 Fig.4,p355 Fig.5,p367 Tb.2,p369  |||||Of the Tawallah Group.|||Carbonate-mudstone +/- sandstone.|
513|Aquarium Formation|65228|5|Briefly described|p21, Figs.02, 05-08.|||Formerly incorrectly mapped as underlying the Wunnunmantyala Sandstone in the MOUNT YOUNG area. Written as "Aquarium Formation" in Figs. 05 and 07.||Unit in Tawallah Group.||Overlies Wununmantyala Sandstone. Is overlain by Settlement Creek Volcanics. Shown as equivalent to Wuraliwuntya Member.||
513|Aquarium Formation|65337|6|Mentioned|p49.|||Southern McArthur Basin. Has fine- to medium-grained sandstone with amalgamated low-angle trough and hummocky cross-stratification, similar to the Tobacco Member of Crow Formation.||||||
513|Aquarium Formation|65340|1|Redefined|pp12-17, pp92-93.|||Revised definition in this study. Upper 15 m has fine parallel-laminated red/brown (oxic) mudstone, massive to locally disrupted. Storm-dominated restricted marine shelf environment. Was in sedimentological continuum with the Wollogorang Formation prior to intrusion of Settlement Creek Dolerite. Hornfelsed and locally brecciated within 1 to 10 m of overlying Settlement Creek Dolerite. Correlated with Wuraliwuntya Member of Wununmantyala Sandstone; and tentatively with Bonanza Creek, lower McCaw, Dhunganda and Yuduyudu Formations in northern McArthur Basin.|c.1740 - 1730 Ma.|Unit in Tawallah Group.||Overlies Wununmantyala Sandstone. Is nonconformably overlain by a sill of Settlement Creek Dolerite.|Upward-fining unit of fine sandstone, maroon, thick-bedded, glauconite and gypsum pseudomorphs; and dolomitic mudstone, glauconitic, micaceous and ferruginous, with fine sandstone and  intervals of dololutite and dolarenite, halite pseudomorphs.|
513|Aquarium Formation|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map|Paleoproterozoic|Paleoproterozoic|See also Eastern Australia Time-Space Plot. McArthur region, Leichhardt Superbasin||Tawallah Group.|||Glauconitic sandstone, brown siltstone|
513|Aquarium Formation|67352|6|Mentioned|p15 tab 2|||||||Overlain by Settlement Creek Volcanics.||
513|Aquarium Formation|69430|4|Described|p15:3, 10-12|Statherian|Statherian|Outcrops in the Batten Fault Zone and SW McArthur Basin, previously included in this unit, are now assigned to the McDermott Formation (Rawlings, 1999). Over 200m thick. Shallow-marine storm-dominated shelf deposits, shallowing upward into marginal marine or lacustrine saline sediments.||Tawallah Group.||Conformably and gradationally overlies Sly Creek Sandstone. Gradational contact with Wununmantyala Sandstone. Is overlain by the intrusive Settlement Creek Dolerite.|Siltstone, shale and fine sandstone: dolomitic, galuconitic and ferruginous; local evaporites.|12-JUL-16
513|Aquarium Formation|69591|5|Briefly described|p39, p58|||Camooweal-Murphy Domain, Mount Isa Province. Part of the McArthur Basin succession. Shallow subaqueous deposits.||Tawallah Group.||Lateral equivalent of Peters Creek Volcanics.|Glauconitic sandstone, brown siltstone.|
513|Aquarium Formation|69673|6|Mentioned|p16 fig 13, p17 fig 14, p24|||||Tawallah Group||Overlain by Settlement Creek Dolerite, overlies Wununmantyala Sandstone, correlated with Wuraliwuntya Member||
513|Aquarium Formation|70849|5|Briefly described|Map legend.|Statherian|Statherian|McArthur Basin.||Tawallah Group.||Overlies Sly Creek Sandstone. Is overlain by Settlement Creek Volcanics.|Glauconitic sandstone, fine- to medium-grained; glauconite and dolomitic siltstone; dolomitic siltstone; dolomite.|
513|Aquarium Formation|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Southeastern McArthur Basin.||Tawallah Group||Overlies and is partially equivalent to Wununmantyala Sandstone and underlies Settlement Creek Dolorite.||
513|Aquarium Formation|72718|6|Mentioned|p7|||Southern McArthur Basin.||Tawallah Group||Underlain by and equivalent to Wununmantyala Sandstone. Overlain by Settlement Creek Dolerite. Equivalent to Wuraliwuntya Member.||
513|Aquarium Formation|72912|5|Briefly described|p5 Fig.3, p19.|Statherian|Statherian|Located in the Southeastern McArthur Basin.||Tawallah Group||Overlies and is equivalent to Wununmantyala Sandstone and underlies Settlement Creek Dolorite.||
513|Aquarium Formation|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin, Calvert Superbasin.||Tawallah Group||Underlain by and equivalent to Wununmantyala Sandstone. Overlain by Settlement Creek Dolorite.||
513|Aquarium Formation|73083|6|Mentioned|p78|||||||Underlain by Wunnunmantyala Sandstone.||
513|Aquarium Formation|73412|5|Briefly described|p4, 8|||Southern McArthur Basin.||Tawallah Group.||Overlies Wununmantyala Sandstone. Is overlain by Settlement Creek Dolerite.||
522|Arafura Group|23374|6|Mentioned|p20|||Of Arafura Basin.||||||18-JUL-06
522|Arafura Group|24047|5|Briefly described|p11|Devonian|Devonian|Siltstone, sandstone and shale.  Geological Province: Arafura Basin.||||||
522|Arafura Group|42056|4|Described|p96|||||||||
522|Arafura Group|42933|5|Briefly described|Fig.94 p258|||||||||
522|Arafura Group|62506|5|Briefly described|p1-2|Carboniferous|Devonian|||||||
522|Arafura Group|62508|5|Briefly described|p32|Devonian|Devonian|||||||
522|Arafura Group|62510|5|Briefly described|p3|Early Carboniferous|Late Devonian|Geological Province: Arafura Basin.||||||
522|Arafura Group|63062|4|Described|p9 Fig. 9, p16|Late Devonian|Late Devonian|Includes the Djabura, Yabooma and Darbilla Formations. Overlies the Goulburn Group. Geological Province: Arafura and Money Shoal Basins.||||||07-FEB-11
522|Arafura Group|69297|5|Briefly described|p283, p285, p289|Upper Devonian|Upper Devonian|Arafura Basin.  Maximum thickness of approximately 1500m. Deposited in shallow marine and non-marine environments. Sandstones and interbedded mudstones are potential hydrocarbon reservoirs. |||Includes the Djabura Formation, Yabooma Formation and the Darbilla Formation.||Interbedded mudstone, siltstone, sandstone and minor carbonate.|
522|Arafura Group|69451|4|Described|p35:2-4, 6, 8-11, 13-14|Late Devonian|Late Devonian|Petroconsultants (1989); Bradshaw et al. (1990). Arafura Basin (offshore). There is a hiatus of c.100 m.y. following the Goulburn Group, and another 45 m.y. before the Kulshill Group. Shallow-marine to non-marine deposits. Up to 1500m thick. Early mature to mature for oil generation. Generally poor petroleum source potential, but interbedded sandstone/shale units are potential reservoirs and host oil shows. Thick shale intervals could form intraformational seals and possibly a regional seal.|||Djabura, Yabooma, Darbilla Formations.|Unconformably overlies Goulburn Group. Is overlain unconformably by Kulshill Group.|Interbedded mudstone, siltstone, sandstone and minor carbonate rocks.|12-JUL-16
522|Arafura Group|69456|5|Briefly described|p40:2 Fig.40.3|Late Devonian|Late Devonian|Arafura Basin.||||Overlies Goulburn Group. Is overlain by Kulshill Group.||12-JUL-16
522|Arafura Group|69673|6|Mentioned|p197|||1500m thick.|||Includes Djabura Formation, Yabooma Formation, Darbilla Formation||Interbedded mudstone, siltstone, sandstone and minor carbonate rocks.|
522|Arafura Group|70098|4|Described|p5, p7-9, p18 Fig.4, p22 Fig.8|Late Devonian|Late Devonian|Arafura Basin and Goulburn Graben. Max thickness: ~1 500 m. Significant oil shows in Paleozoic reservoirs were intersected. Potential source and reservoir rocks occur.|||Djabura Formation (oldest constituent), Yabooma Formation, Darbilla Formation|Overlies Goulburn Group. Unconformably overlain by Carboniferous to early Permian (Cisuralian) succession, considered approximately equivalent to Kulshill Group.|Fluvio-deltaic sediments. Shallow marine to non-marine interbedded mudstone, siltstone, sandstone and minor carbonate.|
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|||||
556|Ardmore Chert Member|24419|5|Briefly described|p18|Late Cambrian|Middle Cambrian|Of Thorntonia Limestone. Regionally extensive layer of rubbly black to white banded and convoluted chert and chert breccia that is well developed in the Quita Creek area and crops out in ther Ardmore Outlier.  Geological Province:  Georgina Basin.||||||
556|Ardmore Chert Member|30479|6|Mentioned|Fig.6|||Stratigraphic relationships||||||
556|Ardmore Chert Member|39690|6|Mentioned|p90|||||||||
556|Ardmore Chert Member|40856|6|Mentioned|Fig.23.6|||||||||
556|Ardmore Chert Member|45079|6|Mentioned|p35|||Map legend p35. Middle Cambrian age||||||18-JUL-06
556|Ardmore Chert Member|47058|6|Mentioned|Table 1 P125|||||||||
556|Ardmore Chert Member|69591|5|Briefly described|p90|||A thin (3-5m) unit, interpreted as the remnant of a substantial evaporite succession.||Beetle Creek Formation.|||Rubble and breccia, chert having replaced the evaporite.|
566|Aremra Granodiorite|39888|6|Mentioned|Fig.8|||||||||
566|Aremra Granodiorite|39898|5|Briefly described|Map legend|Proterozoic|Proterozoic|Granodiorite, tonalite, diorite. Geological Province: Arunta Block.||||||21-JUN-13
566|Aremra Granodiorite|49036|2|Defined|p3|Mesoproterozoic|Mesoproterozoic|Mid-Proterozoic or older. Previously of the Arunta complex.||||||18-JUL-06
566|Aremra Granodiorite|50369|6|Mentioned|p26.1|||Timing & Relationships: The age of this unit is not known. No geochemical analyses of this unit are available, and so it has not been grouped with any other unit. However, Shaw et al. (1982), state that this unit is similar lithologically to the Atnarpa Igneous Complex, and also to the Atneequa Granitic Complex. Units of the Atnarpa Igneous Complex have been dated at ~1880 Ma, and others at ~1750 Ma. The Atneequa Granitic Complex has been dated at ~1760 Ma.|||||granodiorite and tonalite, with some diorite and quartz|28-SEP-12
566|Aremra Granodiorite|68517|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Arunta Block.|||||Granodiorite, tonalite, diorite.|
566|Aremra Granodiorite|69917|5|Briefly described|p158-160|Statherian|Statherian|Eastern Arunta Region, Aileron Province. U/Pb LA-ICPMS zircon dating, Hf analytical data.|1762+/-6 Ma emplacement|Of Ambulbinya Supersuite||Geochemically similar to ca 1770 Ma Huckita Suite and Inkamulla Granodiorite.|Although dominated by granodiorite, the suite also includes diorite. Hornblende granodiorite sampled.|
566|Aremra Granodiorite|71255|6|Mentioned|p2|||Overprinted by the Illogwa Shear Zone during the Palaeozoic Alice Springs Orogeny.|~1762 Ma (Beyer et al, 2012)|||Contact metaorphosed the Salthole Gneiss.||24-MAY-19
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.|
605|Arltunga Nappe Complex|22524|6|Mentioned|p37|||||||||
605|Arltunga Nappe Complex|22762|5|Briefly described|p376|||||||||
605|Arltunga Nappe Complex|22804|6|Mentioned|p454|||||||||
605|Arltunga Nappe Complex|23361|6|Mentioned|8 Fig.1b|||||||||
605|Arltunga Nappe Complex|23858|6|Mentioned|p923|||||||||
605|Arltunga Nappe Complex|23983|6|Mentioned|p27|||||||||
605|Arltunga Nappe Complex|23984|6|Mentioned|p5|||||||||
605|Arltunga Nappe Complex|33102|5|Briefly described|p441|||||||||
605|Arltunga Nappe Complex|33103|6|Mentioned|p25|||Refers Stewart (1971)||||||
605|Arltunga Nappe Complex|33306|4|Described|p205|Early Carboniferous|Early Carboniferous|See also pp206-211. K/Ar dates of formation of Nappe Complex.|358+/-7 Ma, 322+/-6 Ma,  K/Ar|||||27-MAR-14
605|Arltunga Nappe Complex|33699|6|Mentioned|p446|||||||||
605|Arltunga Nappe Complex|33921|6|Mentioned|p391|||||||||
605|Arltunga Nappe Complex|39210|5|Briefly described|p39|||||||||
605|Arltunga Nappe Complex|39565|6|Mentioned|p32|||||||||
605|Arltunga Nappe Complex|39610|4|Described|p9|||||||||
605|Arltunga Nappe Complex|39888|6|Mentioned|p463|||||||||
605|Arltunga Nappe Complex|40100|5|Briefly described|Fig.1|||||||||
605|Arltunga Nappe Complex|41083|6|Mentioned|p461|||||||||
605|Arltunga Nappe Complex|41270|6|Mentioned|p268|||||||||
605|Arltunga Nappe Complex|42843|5|Briefly described|p443, p442 Fig. 1|||See also p441.||||||09-MAY-05
605|Arltunga Nappe Complex|42845|6|Mentioned|p498|||||||||
605|Arltunga Nappe Complex|43697|6|Mentioned|p28|||||||||
605|Arltunga Nappe Complex|46730|4|Described|p13|Paleoproterozoic|Paleoproterozoic|Intrudes Cavenagh, Tommys Gap and Hillsoak Bore Metamorphics. Age: 1651+/-47Ma (Black, et al, 1983). Geological Province: Amadues Basin. Overlying Unit: Heavitree Quartzite.||||||07-MAR-14
605|Arltunga Nappe Complex|48880|4|Described|p23|||Discussed under Structure, Alice Springs Orogeny (mainly Devonian), as containing two large nappes: the Winnecke Nappe and the White Range Nappe|||Involves recumbent folding, faulting and metamorphism of Arunta Complex, Heavitree Quartzite and Bitter Springs Formation rocks.|||
605|Arltunga Nappe Complex|50228|5|Briefly described|p489|Paleoproterozoic|Paleoproterozoic|Granitoid rocks. Age: 1879+/-11Ma.||||||07-NOV-08
605|Arltunga Nappe Complex|50246|5|Briefly described|p9|Silurian|Silurian|Age: ~430-300Ma?||||||07-FEB-11
605|Arltunga Nappe Complex|61309|6|Mentioned|p8 Fig. 1b|Paleozoic|Paleozoic|See also p15.||||||07-NOV-08
605|Arltunga Nappe Complex|66767|6|Mentioned|p61|Carboniferous|Carboniferous|Developed by structural interleaving of SE Aileron Province and basal Amadeus Basin sedimentary rocks, within S-directed mid-crustal imbricate thrust stacks.||||||
605|Arltunga Nappe Complex|67621|6|Mentioned|p209-210|||Central Australia. An intraplate orogen. Cooled between 430-260 Ma.||||||
605|Arltunga Nappe Complex|67856|6|Mentioned|p349|||Of Northern margin of Amadeus Basin.||||||
605|Arltunga Nappe Complex|69227|6|Mentioned|p283 Fig.8|||Between the Amadeus Basin and Harts Range.||||||
605|Arltunga Nappe Complex|69427|5|Briefly described|p12:2, 16, 40, 48-49, 57|Carboniferous|Carboniferous|Aileron Province. It is likely that upper amphibolite-facies metamorphism occurred during the 1735-1690 Ma Strangways Event. Hosts the Arltunga goldfield, c.110 km NE of Alice Springs.||||||12-JUL-16
605|Arltunga Nappe Complex|69444|6|Mentioned|p29:7|||Development of this unit was synchronous (c.330 Ma) with high-grade metamorphism in the Entia Dome, and exhumation and cooling of the Harts Range area west of that Dome; amongst the last events to take place in the Alice Springs Orogeny.||||||12-JUL-16
605|Arltunga Nappe Complex|69925|6|Mentioned|p18, 20|||Arunta Inlier.||||||
605|Arltunga Nappe Complex|69928|6|Mentioned|p209|||||||||
605|Arltunga Nappe Complex|69929|6|Mentioned|p230, 233-234, 236-237|||Forman et al. (1967). Extends E-W for over 75km east of Alice Springs. Basement rocks of the Arunta Block were thrust southward over the Amadeus Basin (Heavitree Quartzite, Bitter Springs Formation) via several megashears (described).||||||
605|Arltunga Nappe Complex|70085|6|Mentioned|p243|||Central Australia. Details in a table listing cooling ages and rates.||||||
632|Arrinthrunga Formation|8217|5|Briefly described|Map Legend|Cambrian|Cambrian|Limestone, minor dolomite and sandstone-grainstone, algal boundstone, mudstone.||||||
632|Arrinthrunga Formation|9394|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Georgina Basin. Brown massive dolomite, yellow flaggy dolomite, blue-purple oolitic limestone, thin beds of siltstone and sandstone. Underlies: Tomahawk beds. Overlies: Arthur Creek beds.||||||01-NOV-04
632|Arrinthrunga Formation|9694|5|Briefly described|Map Legend|Late Cambrian|Middle Cambrian|Underlies Tomahawk beds. Overlies Arthur Creek Formation. Includes: Eurowie Sandstone Member. Grey dolomite and limestone, rare thin beds of siltstone and sandstone. Geological Province: Georgina Basin.||||||
632|Arrinthrunga Formation|12891|5|Briefly described|p733 Fig. 2|Middle Cambrian|Middle Cambrian|Geological province: SW Georgina Basin.||||||07-FEB-11
632|Arrinthrunga Formation|12951|5|Briefly described|p143,  p145 fig 6, p148, 149|Late Cambrian|Late Cambrian|Georgina Basin.||||Said to be lateral equivalent of Chabalowe Formation p148. Overlies Arthur Creek Formation.|Mixed carbonates and siliciclastics.|
632|Arrinthrunga Formation|22524|6|Mentioned|p41|Cambrian|Cambrian|||||||
632|Arrinthrunga Formation|22954|6|Mentioned|Fig3p9|Idamean|Mindyallan|||||||
632|Arrinthrunga Formation|24065|5|Briefly described|p234|Late Cambrian|Late Cambrian|Geological Province: Georgina Basin.||||||
632|Arrinthrunga Formation|24066|6|Mentioned|p237|||Geological Province: Georgina Basin.||||||
632|Arrinthrunga Formation|24442|5|Briefly described|p45|Late Cambrian|Late Cambrian|Unit includes calcimudstone, microbial laminite, peloid/intraclast and ooid grainstone, stromatolite boundstone and quartzic limestone and their dolomitised equivalents, together with minor quartz sandstone.||||||
632|Arrinthrunga Formation|31572|6|Mentioned|Fig.|||Correlation chart 1. U.Cambrian||||||
632|Arrinthrunga Formation|32469|6|Mentioned|p532|||||||||
632|Arrinthrunga Formation|33103|6|Mentioned|Table 4|||||||||
632|Arrinthrunga Formation|33111|6|Mentioned|p17|||||||||
632|Arrinthrunga Formation|33738|6|Mentioned|p480|||||||||
632|Arrinthrunga Formation|35005|5|Briefly described|p145|||||||||
632|Arrinthrunga Formation|35121|6|Mentioned|Map legend|Late Cambrian|Late Cambrian|||||||
632|Arrinthrunga Formation|35139|4|Described|Table.2|||||||||
632|Arrinthrunga Formation|36234|6|Mentioned|p175|||||||||
632|Arrinthrunga Formation|36473|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian to Ordovician||||||
632|Arrinthrunga Formation|37572|4|Described|p161|||See also Fig.8 and P165||||||
632|Arrinthrunga Formation|38532|4|Described|Fig.4|||||||||
632|Arrinthrunga Formation|39210|6|Mentioned|p54|||||||||
632|Arrinthrunga Formation|39921|6|Mentioned|Map legend|Late Cambrian|Late Cambrian|||||||
632|Arrinthrunga Formation|40102|6|Mentioned|p164|||||||||
632|Arrinthrunga Formation|40136|6|Mentioned|p40|||||||||
632|Arrinthrunga Formation|40538|5|Briefly described|Map legend|Late Cambrian|Middle Cambrian|Dolostone and limestone, micrite to grainstone, oolitic, stromatolitic, intraclastic: minor silt or quartz-arenite interbeds. Geological Province: Georgina Basin.||||||15-NOV-05
632|Arrinthrunga Formation|40810|5|Briefly described|p14|||||||||
632|Arrinthrunga Formation|40906|4|Described|p26|||||||||
632|Arrinthrunga Formation|41204|6|Mentioned|p13|||||||||
632|Arrinthrunga Formation|41385|6|Mentioned|Fig.4|||||||||
632|Arrinthrunga Formation|41388|6|Mentioned|p552|||||||||
632|Arrinthrunga Formation|41524|3|Fully described|p19|||||||||
632|Arrinthrunga Formation|41525|5|Briefly described|Map legend|Late Cambrian|Late Cambrian|Dolostone and and limestone, peloidal, oolitic, stromatolititc, micritic; thin siltstone, sandstone, shale interbeds.||||||26-OCT-05
632|Arrinthrunga Formation|42059|5|Briefly described|Fig.2 P131|||See also p134||||||18-JUL-06
632|Arrinthrunga Formation|42060|6|Mentioned|Fig.5 P140|||||||||
632|Arrinthrunga Formation|42477|5|Briefly described|p32|||||||||
632|Arrinthrunga Formation|42504|5|Briefly described|Table 54 P79|||||||||
632|Arrinthrunga Formation|42643|3|Fully described|p30|Late Cambrian|Middle Cambrian|||||||
632|Arrinthrunga Formation|42644|5|Briefly described|Map Legend|Late Cambrian|Middle Cambrian|Dolostone and minor limestone, peloidal, oolitic, stromatolitic, intraclastic, sandy, recessive; dolomitic sandstone. Geological Province: Georgina Basin.||||||15-NOV-05
632|Arrinthrunga Formation|42956|5|Briefly described|p31 Fig.4|||||||||
632|Arrinthrunga Formation|43105|5|Briefly described|Fig.4,p9.|||||||||
632|Arrinthrunga Formation|43807|6|Mentioned|p352|||||||||
632|Arrinthrunga Formation|44233|14|Not recorded|p.60||Early Cambrian|Fig.1. Upper Cambrian.||||||
632|Arrinthrunga Formation|44320|14|Not recorded|p.8,9,12,13,14||Late Cambrian|U.Camb. Table 1.||||||
632|Arrinthrunga Formation|44321|14|Not recorded|map legend||Late Cambrian|(F53-7). U.Camb.||||||
632|Arrinthrunga Formation|44327|14|Not recorded|p.10|||See also pages 11,13,14,16,17 for more details. Map. (F53-11).||||||
632|Arrinthrunga Formation|44328|14|Not recorded|map legend||Late Cambrian|Upper Cambrian.||||||
632|Arrinthrunga Formation|44334|14|Not recorded|map legend||Late Cambrian|Upper Cambrian.||||||
632|Arrinthrunga Formation|44358|4|Described|p9,Tb.1||Late Cambrian|||||||
632|Arrinthrunga Formation|44457|14|Not recorded|p.6||Late Cambrian|U.Cambrian. Outcrops on Elkedra sheet. (F53-7).||||||
632|Arrinthrunga Formation|44469|2|Defined|p.8, opp.p.6, Tb.I|||(F53-12). See also p.13,15,16, Tb.2. O/lies conf. Marqua Beds. Algae. Aquifers.||||||
632|Arrinthrunga Formation|44470|5|Briefly described|map legend||Late Cambrian|Upper Cambrian.||||||02-DEC-04
632|Arrinthrunga Formation|44852|14|Not recorded|p69||Early Cambrian|||||||
632|Arrinthrunga Formation|44920|14|Not recorded|Map Legend, Sheet 4||Late Cambrian|||||||
632|Arrinthrunga Formation|45052|2|Defined|p104|Late Cambrian|Late Cambrian|||||||
632|Arrinthrunga Formation|45148|6|Mentioned|Fig.4|||Georgina Basin||||||
632|Arrinthrunga Formation|45155|6|Mentioned|Fig.8|||||||||
632|Arrinthrunga Formation|46740|14|Not recorded|p.187||Middle Cambrian|U.Cambrian.||||||
632|Arrinthrunga Formation|46897|6|Mentioned|p352|||||||||
632|Arrinthrunga Formation|46958|6|Mentioned|Fig.2|||||||||
632|Arrinthrunga Formation|47024|6|Mentioned|Table 2|||||||||
632|Arrinthrunga Formation|47058|6|Mentioned|p134|||||||||
632|Arrinthrunga Formation|48844|2|Defined|p.35-6|||On many pages. p.2,16,17,21,25,35-6,38-9,46,47,49-50, F.26,58,62,63,66-69, Pl.4,8. New name. (F53-11).||||||
632|Arrinthrunga Formation|48901|14|Not recorded|Not recorded||Late Cambrian|F53-4,7,12. U.Cambrian.||||||
632|Arrinthrunga Formation|49027|4|Described|p11|||||||||
632|Arrinthrunga Formation|60122|3|Fully described|p19, p4-5|Late Cambrian|Late Cambrian|Includes Eurowie Sst Mbr. Dolostone, limestone, minor qtz sst., sltst, shale, marl, conglom. Conf.overlies Arthur Cr Fm/Steamboat Sst; underlies Ninmaroo/Tomahawk Fms.  Laterally interfingers with Georgina Lst. Max.thick:975m. Geol. Prov: Georgina Basin.||||||11-MAY-05
632|Arrinthrunga Formation|60123|4|Described|p5|Cambrian|Cambrian|Thickness: 975m. Disconformably underlies: Tomahawk Formation, Ninmaroo Formation. Conformably overlies: Chabalowe Formation, Steamboat Sandstone, Arthur Creek Formation. Dolostone, Limestone.||||||28-APR-05
632|Arrinthrunga Formation|60551|5|Briefly described|Map Legend|Late Cambrian|Cambrian|Includes: Eurowie Sandstone Member. Underlies: Tomahawk Beds. Overlies: Arthur Creek Formation. Geological province: Georgina Basin.  Grey dolomite and limestone, rare thin beds of siltstone and sandstone.||||||
632|Arrinthrunga Formation|60590|5|Briefly described|Map legend|Late Cambrian|Late Cambrian|Dolostone, limestone, minor quartz sandstone, siltstone, shale, marl and conglomerate.  Conformably overlies the Steamboat Sandstone; overlain by the Tomahawk Formation.||||||23-DEC-09
632|Arrinthrunga Formation|60675|5|Briefly described|Map legend|Late Cambrian|Late Cambrian|Overlies Chabalowe and Arthur Creek Formations. Dolostone, limestone, minor quartz sandstone, siltstone, shale, marl and conglomerate.||||||11-JAN-05
632|Arrinthrunga Formation|61022|5|Briefly described|p15 Fig. 2|Late Cambrian|Late Cambrian|Contains the Eurowie Sandstone Member and the Hagen Member. Geological Province: Georgina Basin. Named in abstract for: Carbonate ramp facies and oil plays in Late Cambrian-southern Georgina Basin (abstract) by Ambrose, G.J. and Putnam, P.E.||||||16-JUN-05
632|Arrinthrunga Formation|61404|5|Briefly described|Map legend|Late Cambrian|Late Cambrian|Of the Narpa Group. Includes the Eurowie Sandstone Member. Dolostone, limestone, minor quartz sandstone, siltstone, shale, marl and conglomerate. Geological Province: southern Georgina Basin.||||||
632|Arrinthrunga Formation|62376|5|Briefly described|p53|Late Cambrian|Late Cambrian|Geological Province: Georgina Basin||||||09-FEB-10
632|Arrinthrunga Formation|62595|6|Mentioned|p28 Fig.4.|Late Cambrian|Late Cambrian|Georgina Basin. Relative probability plots of detrital zircon data are shown.||||||
632|Arrinthrunga Formation|62658|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Narpa Group. Dolostone and limestone with siliceous nodules and concretions; minor quartz sandstone, siltstone and shale.||||||
632|Arrinthrunga Formation|62759|5|Briefly described|p1|Late Cambrian|Late Cambrian|Includes the Hagen Member.||||||01-FEB-07
632|Arrinthrunga Formation|62789|5|Briefly described|p128, p129 Fig. 2|Late Cambrian|Late Cambrian|Southern Georgina Basin. Pacific Oil & Gas spudded their Baldwin No. 1 exploration well in this unit and intersected its base at 470.4 m.|||Includes Eurowie Sandstone Member.||Limestone, dolomite.|28-MAR-12
632|Arrinthrunga Formation|62790|5|Briefly described|p209, 210|Late Cambrian|Late Cambrian|Southern Georgina Basin. 470.4 m thick in Pacific Oil & Gas Baldwin No. 1 well.||||Overlies Arthur Creek Formation.|Limestones and dolomites.|28-MAR-12
632|Arrinthrunga Formation|63450|5|Briefly described|p78 Fig. 5, p80|Late Cambrian|Middle Cambrian|Overlies the Marqua Formation. Thickness: 601m. Geological province: Georgina Basin, West Toko Syncline. Comprises a mixture of grainstones, algal boundstones, sandy conglomerate and intraclastic limestones. See also p81.||||||07-FEB-11
632|Arrinthrunga Formation|63562|5|Briefly described|p338 fig 3, p345 fig 7, p347 fig 9.|Late Cambrian|Middle Cambrian|See also p348-349, p351, p352 fig 10, p355. Of Georgina Basin. Deposited in a peritidal and restricted shallow subtidal marine environment. Detrital zircons peak at c.1.85 Ga suggesting a sediment source in Arunta Inlier.||||Overlies Arthur Creek Formation. Correlated with Shannon Formation. Is overlain disconformably by Tomahawk Formation.|A thick, well-bedded dolostone and limestone unit with rare siliciclastic beds including calcarenite.|06-DEC-17
632|Arrinthrunga Formation|64068|3|Fully described|p20, pp65-71, p81, p89|Late Cambrian|Late Cambrian|Mapped as Ninmaroo Formation by Noakes et al (1959).  Hosts base metal mineralisation. Interdigitates with Georgina Limestone and Chabalowe Formation at base. Basal part correlated with Chabalowe Formation, Hagen Member, Selwyn Range Limestone.||Of Narpa Group.|Includes Eurowie Sandstone Member in middle.|Conformably overlies Steamboat Sandstone, Chabalowe Formation, or Arthur Creek Formation. Disconformably overlain by Tomahawk and Ninmaroo Formations.|Locally silicified and evaporitic limestone and dolostone; minor quartz sandstone, siltstone, shale. Contains stromatolites.|04-APR-12
632|Arrinthrunga Formation|64443|4|Described|p2, p5 Fig.3, p6 Tb.1, p9, p17-18, p40|Late Cambrian|Middle Cambrian|Of Smith (1964); formerly Meeta beds (Nichols and Fehr 1964). Disconformably underlies Tomahawk Formation and Ninmaroo Formation; laterally interdigitates with Georgina Limestone. Max 975m thick. Forms prominent isolated hills.||Of the Narpa Group.||Conformably overlies Camooweal Dolostone, Arthur Creek Formation, Steamboat Sandstone, Chabalowe Formation and possibly Wonarah Formation. See Comments.|Dolostone and limestone with minor quartz sandstone, siltstone, shale. Features includes stromatolites, thrombolites, nodular evaporites, gypsum crystals, fenestrae.|14-MAY-14
632|Arrinthrunga Formation|64778|6|Mentioned|p13, 30, 33|Cambrian|Cambrian|Toko Syncline, Southern Georgina Basin.||||||
632|Arrinthrunga Formation|64812|5|Briefly described|p237 Fig. 2, p251|Late Cambrian|Late Cambrian|Geological Province: southern Georgina Basin.||||||07-FEB-11
632|Arrinthrunga Formation|64813|5|Briefly described|p256 Fig. 3|Late Cambrian|Late Cambrian|Overlies Chabalowe Formation. Geological Province: southern Georgina Basin. Carbonate and siliciclastic rocks.||||||11-FEB-09
632|Arrinthrunga Formation|65237|5|Briefly described|p3 Fig. 4, p9|Late Cambrian|Late Cambrian|Overlies Arthur Creek Formation. Max. thickness: 700m in the Dulcie Syncline. Geological province: southern Georgina Basin. Mixed carbonate and siliciclastic sediments.||||||07-FEB-11
632|Arrinthrunga Formation|65337|6|Mentioned|p68.|Late Cambrian|Late Cambrian|||||Overlies Camooweal Dolostone.||
632|Arrinthrunga Formation|65341|5|Briefly described|p2 Fig.2, p18.|Late Cambrian|Late Cambrian|||||Conformably overlies Chabalowe Formation. Is disconformably overlain by Tomahawk Formation.|Carbonate-dominated.|
632|Arrinthrunga Formation|65342|5|Briefly described|p7.|||Georgina Basin. Max. thickness at least 456 m.|||Includes Eurowie Sandstone Member.||Dolostone, limestone; minor quartz sandstone, siltstone, shale, marl and conglomerate.|
632|Arrinthrunga Formation|65489|6|Mentioned|p125-126|Ordovician|Cambrian|Georgina Basin.||||Is overlain unconformably by Ninmaroo Formation.||
632|Arrinthrunga Formation|66767|5|Briefly described|p59|Cambrian|Cambrian|Southern Georgina Basin.||Narpa Group.|Eurowie Sandstone Member.|Overlies Chabalowe Formation.|A thick succession of peritidal, evaporitic and stromatolitic limestone and dolostone, with minor quartz sandstone, siltstone and shale.|
632|Arrinthrunga Formation|67323|5|Briefly described|p83, p90, p92 Fig.12.2|Cambrian|Cambrian|West Toko Syncline, Georgina Basin. An aquifer; supplies water bores.||||Unconformably overlies Marqua Formation. Is overlain unconformably by Ninmaroo Formation.||
632|Arrinthrunga Formation|67402|4|Described|p25 tbl RRM3, p213 fig GRG3|Iverian|Undillian|Georgina Basin, West Toko Syncline. Maximum thickness of 622m. Deposited in a very shallow and intermittently emergent sea. See also p215, p217 tbl GRG2. ||||Overlies the Georgina Limestone. Unconformably overlies the Thorntonia Limestone or Hay River Formation. Unconformably overlain by the Ninmaroo Formation.|Carbonate and carbonate siliciclastic sequence.|
632|Arrinthrunga Formation|67870|6|Mentioned|p43|Late Cambrian|Middle Cambrian|Georgina Basin.||Narpa Group.||||
632|Arrinthrunga Formation|69437|5|Briefly described|p22:10, 15|Cambrian|Cambrian|Southern Georgina Basin. May have potential as a petroleum source rock.||||Overlies Chabalowe Formation and Steamboat Sandstone. Is overlain by Tomahawk, Ninmaroo Formations.||12-JUL-16
632|Arrinthrunga Formation|69443|4|Described|p28:7, 16, 18-19, 21, 24, 26, 31, 35-36|Late Cambrian|Late Cambrian|See also 28:38, 40, 45, 47. K.G. Smith (1964). Southern Georgina Basin. Very thick unit, forming low rubbly exposures to substantial ridges. Up to 975m thick; generally over 300m. Wide variety of sedimentary structures; fossiliferous. Shallow subtidal to peritidal deposits on a restricted carbonate platform, with intermittent local emergence. Laterally interdigitates with Georgina Limestone. Associated with the Box Hole-Turkey Creek Pb-Zn prospect and abandoned mine. Hosts the Trackrider Pb prospect. Basal black shale has high TOC: is a viable petroleum source rock. Has had hydrocarbon shows in drilled wells. Is being explored for oil shale and tight gas.||Narpa Group.|Eurowie Sandstone Member.|Overlies Chabalowe or Arthur Creek Formations and Steamboat Sandstone gradationally, and Camooweal Dolostone (Barkly Group) conformably. Is overlain disconformably by Tomahawk and Ninmaroo Formations.|Locally silicified and evaporitic limestone and dolostone, minor quartz sandstone, siltstone and shale.|12-JUL-16
632|Arrinthrunga Formation|69561|6|Mentioned|p33 fig 2|Iverian|Mindyallan|||||Overlies Chabalowe Formation, Steamboat Sandstone||
632|Arrinthrunga Formation|69591|6|Mentioned|p88|Cambrian|Cambrian|Undilla Sub-basin, Georgina Basin.||||Overlies ("apparently") the Camooweal Dolostone.||
632|Arrinthrunga Formation|69673|4|Described|p103, p117, p126, p127, p129, p135, p136|||975m thick. Includes fossils of stromatolites, brachiopods, hyoliths, molluscs, ichnofossils and rare trilobites.||||Correlated with Shannon Formation, Conformably overlies Chabalowe Formation, Steamboat Sandstone, disconformably overlain by Tomahawk Formation, Ninmaroo Formation|Locally silicified and evaporitic limestone and dolostone; minor sandstone, siltstone and shale. Microbial, peloid, ooid mudstones.|
632|Arrinthrunga Formation|70380|6|Mentioned|p745|Series 4|Series 3|Southern Georgina Basin.||||||
632|Arrinthrunga Formation|70723|5|Briefly described|p24 Fig. 2|Cambrian|Cambrian|Georgina Basin. Oil show.||Narpa Group|Includes Eurowie Sandstone Member|Overlies Steamboat Sandstone or Chabalowe Formation.||
632|Arrinthrunga Formation|70951|6|Mentioned|p1080|||Geological province: Georgina Basin. High reflectance measured.||||||
632|Arrinthrunga Formation|71800|5|Briefly described|p26-p27|Middle Cambrian|Middle Cambrian|Georgina Basin.||||Overlies the Arthur Creek Formation.|Calcarenite.|
632|Arrinthrunga Formation|72321|5|Briefly described|Fig 2, p6 fig 3|Jiangshanian|Guzhangian|Elkedra Shelf/Dulcie Syncline, Toko Syncline, Georgina Basin.  Base older in Toko Syncline than Dulcie Syncline. Australian stages: Mindyallan to Iverian.||of Narpa Group.||Overlies Arthur Creek Foramtion in Baldwin 1.||
632|Arrinthrunga Formation|72358|5|Briefly described|p117, p125|||Of Georgina Basin. Equivalent to Jay Creek Limestone in the Amadeus Basin. G. reticulatus Zone is recorded in petroleum well Netting Fence 1 (Green & Balfe, 1980).||||||10-JAN-20
632|Arrinthrunga Formation|72515|5|Briefly described|Map Legend|Cambrian|Cambrian|Jervois Range Special Map Sheet. Georgina Basin. Includes fossil stromatolites, trilobites, brachiopods, hyoliths, molluscs and ichnofossils.||Narpa Group|Eurowie Sandstone Member|Overlies the Steamboat Sandstone.|Evaporitic dolostone, limestone, medium-thick bedded; minor quartz sandstone, siltstone, shale.|05-JUL-22
632|Arrinthrunga Formation|72516|3|Fully described|p11-12, p92-94, p154|Furongian|Furongian|Georgina Basin. Occurs in eastern BARROW CREEK, ELKEDRA, HUCKITTA, TOBERMORY, SANDOVER RIVER, AVON DOWNS, HAY RIVER, MOUNT WHELAN, GLENORMISTON and URANDANGI map sheets. In the Jervois Range Special it outcrops on both sides of the Lucy Creek Fault Zone and forms low rubbly exposures to substantial ridges. Contains fossil stromatolites, trilobites, brachiopods, hyoliths, molluscs, ichnofossils which suggest a Furongian age. <100m thick in mapped area, 975m thick elsewhere. Deposited in a shallow subtidal to peritidal, restricted carbonate platform with intermittent local emergence. Age correlations are interpreted with the Chabalowe Formation, Georgina Limestone. Stratigraphically equivalent ot the Mungerebar Limestone, Selwyn Range Limestone, O'Hara Shale, Pomegranate Limestone of the Georgina Basin. Also equivalent to the Cleland Sandstone, Petermann Sandstone, Deception Siltstone, Jay Creek Limestone, Shannon Formation and Goyder Formation of the Amadeus Basin. Additionally correlated with the Brady Gneiss of the Irindina Province.|ca 825 Ma (U-Pb SHRIMP max dep age)|Narpa Group|Includes the Eurowie Sandstone Member.|Disconformably overlain by the Tomahawk Formation. Conformably and gradationally overlies the Steamboat Sandstone and Arthur Creek Formation.|Medium- to thick-bedded evaporitic dolostone and limestone; minor siliciclastic quartz sandstone, siltstone, shale.|14-APR-22
632|Arrinthrunga Formation|73083|6|Mentioned|p10, p42, p75|Cambrian|Cambrian|Previously the Meeta beds.||||Underlain by Camooweal Dolostone.|Includes dolostone, limestone, quartz sandstone, siltstone, and shale.|
632|Arrinthrunga Formation|73591|6|Mentioned|p40|||Georgina Basin.||||||
645|Arthur Creek Formation|9694|5|Briefly described|Map Legend|Late Cambrian|Middle Cambrian|Underlies: Arrinthrunga Formation. Overlies: Mount Baldwin Formation, Errarra Formation. Geological Province: Georgina Basin. Shale, limestone, sandstone.||||||
645|Arthur Creek Formation|12891|5|Briefly described|p733 Fig. 2|Middle Cambrian|Middle Cambrian|Geological province: SW Georgina Basin.||||||07-FEB-11
645|Arthur Creek Formation|12951|4|Described|p144-148 149-157|Middle Cambrian|Middle Cambrian|Georgina Basin. Some old informal terminology abandoned, but new informal subdivisions introduced, based on electric log response and lithology.||||Unconformably overlies Thorntonia Limestone.|Basal anoxic hot shale passing upwards into paler dolomitic beds with some conglomerate to east. Then a pale carbonate interval with dolomudstone dominant and some oolite and laminated silty dolostone at top.|
645|Arthur Creek Formation|22954|6|Mentioned|Fig3p9|||||||||
645|Arthur Creek Formation|24442|5|Briefly described|p45|Middle Cambrian|Middle Cambrian|Overlain by Steamboat Sandstone.  On SANDOVER RIVER sheet.  ||||||
645|Arthur Creek Formation|40538|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Calcareous siltstone, fossiliferous, poorly exposed, limestone interbeds and quartz arenaceous limestone at top. Geological Province: Georgina Basin.||||||15-NOV-05
645|Arthur Creek Formation|40906|2|Defined|p57|Middle Cambrian|Middle Cambrian|||||||
645|Arthur Creek Formation|41018|6|Mentioned|p239|||||||||
645|Arthur Creek Formation|41021|6|Mentioned|p261|||||||||
645|Arthur Creek Formation|41129|6|Mentioned|p16|||||||||
645|Arthur Creek Formation|41204|6|Mentioned|p13|||Formerly Sandover beds||||||
645|Arthur Creek Formation|41524|3|Fully described|p16|||||||||
645|Arthur Creek Formation|41525|5|Briefly described|Map legend|Middle Cambrian||Siltstone, fossiliferous, pale yellow, part silicified in outcrop; grey black, calcareous, carbonaceous, phosphatic and pyritic at depth.||||||07-MAY-13
645|Arthur Creek Formation|42059|5|Briefly described|Fig.2|||See also P134||||||
645|Arthur Creek Formation|42070|6|Mentioned|p4|||||||||
645|Arthur Creek Formation|42504|6|Mentioned|p21|||||||||
645|Arthur Creek Formation|42643|6|Mentioned|p26|||Supersedes Sandover Beds||||||
645|Arthur Creek Formation|42956|5|Briefly described|p31 Fig.4|||||||||
645|Arthur Creek Formation|42994|6|Mentioned|p7|||||||||
645|Arthur Creek Formation|44133|5|Briefly described|p42|||Overlies Errarra Formation.||||||
645|Arthur Creek Formation|47035|6|Mentioned|Fig.1|||||||||
645|Arthur Creek Formation|47058|6|Mentioned|p138|||Variation of Arthur Creek Formation, NT.||||||
645|Arthur Creek Formation|60122|1|Redefined|p17, p56 Appendix|Middle Cambrian|Middle Cambrian|Formerly Arthur Creek beds. Now incorporates part of Sandover beds of ELKEDRA, Marqua Fm. and "Upper Hay River Formation Member2" of TOBERMORY. Disconformably overliesThorntonia Lst or Red Heart Dolostone; conformably underlies Steamboat Sst, Chabalowe Fm||||||26-OCT-05
645|Arthur Creek Formation|60123|4|Described|p5|Cambrian|Cambrian|Thickness: 457m. Conformably underlies Arrinthrunga Formation, Chabalowe Formation, Hagen Member, Steamboat Sandstone. Disconformably overlies Thorntonia Limestone. Dolostone.||||||26-OCT-05
645|Arthur Creek Formation|60551|5|Briefly described|Map Legend|Cambrian|Cambrian|Underlies: Arrinthrunga Formation. Overlies: Errarra Formation, Mount Baldwin Formation. Geological province: Georgina Basin.  Buff shale, laminated limestone, sandstone, dolomite.||||||
645|Arthur Creek Formation|60590|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Dolostone, limestone (upper); foetid pyritic-carbonaceous black shale, laminated dolostone (lower part).  Overlies the Thorntonia Limestone; conformably overlain by Steamboat Sandstone.||||||25-NOV-04
645|Arthur Creek Formation|60675|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Underlies Chabalowe and Arrinthrunga Formations; overlies Thorntonia Limestone. Upper: dolostone, limestone. Lower: foetid pyritic- carbonaceous black shale, laminated dolostone.||||||12-JAN-05
645|Arthur Creek Formation|60684|6|Mentioned|p14|||||||||
645|Arthur Creek Formation|61022|5|Briefly described|p14, p15 Fig. 2|Middle Cambrian|Middle Cambrian|Geological Province: Georgina Basin. Named in abstract for: Carbonate ramp facies and oil plays in Late Cambrian-southern Georgina Basin (abstract) by Ambrose, G.J. and Putnam, P.E.||||||20-APR-05
645|Arthur Creek Formation|61250|5|Briefly described|p43|Middle Cambrian|Middle Cambrian|Contains petroleum systems. Geological Province: Georgina Basin.||||||
645|Arthur Creek Formation|61404|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Of the Narpa Group. Divided into: upper dolostone, limestone; lower foetid pyritic-carbonaceous black shale, laminated dolostone. Geological Province: southern Georgina Basin.||||||
645|Arthur Creek Formation|61732|5|Briefly described|p113|Middle Cambrian|Middle Cambrian|Overlies Elkera Formation Huckitta 7 drillhole.  Geological Province: Georgina Basin.||||||07-FEB-11
645|Arthur Creek Formation|62376|5|Briefly described|p53|Middle Cambrian|Middle Cambrian|Geological Province: Georgina Basin||||||09-FEB-10
645|Arthur Creek Formation|62759|5|Briefly described|p1|Middle Cambrian|Middle Cambrian|Overlain by Steamboat Sandstone. Geological Province: Georgina Basin. Includes shoals and sandy debris flows; contains extremely rich oil-prone microbial source rocks.||||||05-FEB-08
645|Arthur Creek Formation|62789|5|Briefly described|p128, p129 Fig. 2, p132|Middle Cambrian|Middle Cambrian|Fossiliferous mudstone, siltstone, limestone, minor sandstone. Contains diverse trilobite assemblage. In southern Georgina Basin, overlies early Middle Cambrian Thorntonia Limestone and underlies Upper Cambrian Chabalowe Formation.||||Overlies early Middle Cambrian Thorntonia Limestone and underlies Upper Cambrian Chabalowe Formation.|Fossiliferous mudstone, siltstone, limestone, minor sandstone.|28-MAR-12
645|Arthur Creek Formation|62790|4|Described|p206, 208, p210, p219, p220|Middle Cambrian|Middle Cambrian|Georgina Basin. Contains a small bradoriid and phosphatocopid fauna.||||Underlies Arrinthrunga Formation and overlies Thorntonia Limestone.|Fossiliferous mudstone, siltstone, limestone, minor sandstone.|28-MAR-12
645|Arthur Creek Formation|62983|5|Briefly described|p11|Cambrian|Cambrian|Referred to informally as the lower Arthur Creek Formation. Extensive anoxic carbonaceous shale. Geological Province: Georgina Basin.||||||07-MAY-13
645|Arthur Creek Formation|63450|4|Described|p78 Fig. 5, p80-81|Middle Cambrian|Middle Cambrian|Thickness: >800m. Geological province: Georgina Basin, West Toko Syncline. Equivalent to upper Hay River Formation and Marqua Formation. Comprises a lower pyritic black shale and laminated dolostone lower unit and dolostone and limestone upper unit. Richly fossiliferous.||||||22-FEB-16
645|Arthur Creek Formation|63562|5|Briefly described|p338 fig 3, p348|Middle Cambrian|Middle Cambrian|Of Georgina Basin.||||Correlated with Giles Creek Dolomite. Is overlain by Arrinthrunga Formation.|Carbonate-rich.|06-DEC-17
645|Arthur Creek Formation|64068|4|Described|p59-63, 65,  67, 83  p86-91, p44, p ix|Middle Cambrian|Middle Cambrian|Fossiliferous. Potential hydrocarbon source rock. Potential host for epigenetic, stratiform, sediment-hosted Pb-Zn. Contains turquoise.  A detailed petrography is provided.||Of Narpa Group.|Now includes rocks formerly assigned to Marqua Formation, 'upper Hay River Formation Member 2' and some Sandover beds|Disconformably overlies Thorntonia Limestone. Conformably overlain by Steamboat Sandstone in Sth and by Chabalowe Formation in SW.|Anoxic shale below dolostone, limestone and siliciclastic mudstone.|05-APR-12
645|Arthur Creek Formation|64443|4|Described|iii, p6 Tb.1, p9, p40, 41. |Floran||Correlative of Wonarah Formation, Ranken Limestone, Camooweal Dolostone. Max 457m thick.||||Conformably underlies Arrinthrunga Formation; disconformably overlies Thorntonia Limestone or unconformably overlies undivided South Nicholson Group.|Foetid pyritic-carbonaceous black shale and laminated dolostone, overlain by dolostone and limestone; their contact is identifiable in drillholes. Has nodular evaporite, brecciated texture, fossils, disseminated pyrite.|14-MAY-14
645|Arthur Creek Formation|64778|6|Mentioned|p13, 25-26|Cambrian|Cambrian|Dulcie Syncline, Southern Georgina Basin. Potential hydrocarbon source.||||||
645|Arthur Creek Formation|64812|5|Briefly described|p236, p241-9, p251|Middle Cambrian|Middle Cambrian|Overlies Thorntonia Limestone. Geol.Prov: Georgina Basin. Described as Lower A.C. Formation, outer ramp facies of marine anoxic dolomite shale; and, Upper A.C.Fm, middle ramp facies grading to increasingly oxygenated, mixed clastic/ carbonate sediments.||||||07-FEB-11
645|Arthur Creek Formation|64813|5|Briefly described|p254, p255, p256 Fig. 2|Middle Cambrian|Middle Cambrian|Geol.prov:Georgina Basin.Comprises marine anoxic shale (outer ramp facies) grading into middle- + inner-ramp carbonate + clastic rocks. 'Hot shale' at base, rich in algal/bacterial organic matter, provides petroleum source/seal rocks for Georgina Basin.||||||11-FEB-09
645|Arthur Creek Formation|65237|4|Described|p3 Fig. 4, p6|Middle Cambrian|Middle Cambrian|Informally subdivided into upper/lower Arthur Creek Formations; oil prone rocks in lower part. Max.thickness: 400m in basin/800m in Toko Syncline. Geol.prov:Georgina Basin. Depositional environment details included. Contains E-log marker "Hot Shale".||||||07-FEB-11
645|Arthur Creek Formation|65239|5|Briefly described|p2|Middle Cambrian|Middle Cambrian|Unconformably overlies Thorntonia Limestone. Geological province: Georgina Basin.||||||
645|Arthur Creek Formation|65342|5|Briefly described|p7.|Middle Cambrian|Middle Cambrian|Georgina Basin. Max. thickness at least 457 m. Seen as having potential as an insulating layer for geothermal energy.|||||Dolostone, limestone in upper part; black, foetid, pyritic-carbonaceous shale in lower part.|
645|Arthur Creek Formation|65345|5|Briefly described|p6 Fig.5, p7, p14.|Cambrian|Cambrian|Southern Georgina Basin. Waterbore RN013015 contains a 3 m interval containing 16.9% P2O5.||||Unconformably overlies Thorntonia Limestone. Is overlain by Steamboat Sandstone.||
645|Arthur Creek Formation|65489|5|Briefly described|p124, p126-127|||Georgina Basin. Over 80,000 km2. Rich in algal/bacterial organic matter: provides the principal source/seal rocks of the Basin. 20-100m thick.|||||Anoxic, pyritic and carbonaceous, partly dolomitic shale.|
645|Arthur Creek Formation|66767|5|Briefly described|p59|Middle Cambrian|Middle Cambrian|Southern Georgina Basin.||Narpa Group.|||Black shale and dolostone.|
645|Arthur Creek Formation|67126|5|Briefly described|p1-7, p10-16, p19, p22-25, p27-33|Middle Cambrian|Middle Cambrian|See also p36, p38. Georgina Basin. A source rock ("hot shale") worthy of serious consideration as a potential gas shale (reasons detailed). Rock Eval analysis, Rock Eval Temperature Programme: Pyrolysis, Thermovaporisation, Pyrolysis Gas Chromatography results presented in detail.||||||
645|Arthur Creek Formation|67352|6|Mentioned|p69|||||||||
645|Arthur Creek Formation|67402|6|Mentioned|p216|||Georgina Basin. Potential seal unit.|||||Dolomitic mudstone.|
645|Arthur Creek Formation|67870|5|Briefly described|p39, p43, p46-47, p50-53, p55|Middle Cambrian|Middle Cambrian|Western Georgina Basin. Includes an organic-rich, potential source-rock, unit. 4% TOC. Detailed modelling showing transformation ratios, expulsion mass (bulk) and expulsions mass for oil and gas.||Narpa Group.||Equivalent to the Devoncourt Limestone.|Organic-rich (8% TOC) shale, marl.|
645|Arthur Creek Formation|68518|6|Mentioned|p14|||In HUCKITTA (Freeman, 1986). Sandover beds will be shown mainly as this unit on 2nd ed of ELKEDRA (Stidolph and others, in. prep.)||||||30-JUN-14
645|Arthur Creek Formation|69206|6|Mentioned|p2-3|||Georgina Basin. Contains hydrocarbon source rocks.||||||
645|Arthur Creek Formation|69418|5|Briefly described|p3:31, 36|Middle Cambrian|Middle Cambrian|Georgina Basin. Hosts the Barrow Creek 1 and Arganara phosphate deposits (briefly described). The lower part of this unit has potentially prolific marine source rocks, particularly the basal "hot shale" facies, as well as considerable unconventional shale gas and oil potential. The upper part has shale gas potential.||||||12-JUL-16
645|Arthur Creek Formation|69437|5|Briefly described|p22:10-11, 15-16|Cambrian|Cambrian|Southern Georgina Basin, Centralian B Superbasin. Sequence 2. Deposition was in relatively deep, followed by relatively shallow restricted, marine conditions. An important potential petroleum source rock; also potential reservoir in the upper part. The lower part of this unit has considerable unconventional shale gas and oil potential, with shale gas potential in the upper part.||||Overlies Thorntonia Limestone. Is overlain by Steamboat Sandstone and Chabalowe Formation.|Pyritic-carbonaceous black shale, dolostone and minor siliciclastic rocks overlain by carbonate rocks and siliciclastic mudstone.|12-JUL-16
645|Arthur Creek Formation|69439|6|Mentioned|p24:10|||Georgina Basin.||||Lower part is correlated with the Bloodwood Formation (Ngalia Basin).||12-JUL-16
645|Arthur Creek Formation|69443|4|Described|p28:16-19, 22-25, 32, 41, 43, 45-47|Middle Cambrian|Middle Cambrian|Freeman (1986) after K.G. Smith (1964); modified by Kruse et al. (2002). Southern Georgina Basin. From <30m thick to over 483m (possibly 720m?). Richly fossiliferous: latest Ordian to Boomerangian. Dysoxic to anoxic deeper marine, shallowing upwards to restricted platform, deposits. Passes laterally into Wonarah Formation. Correlated with Anthony Lagoon Formation, Ranken Limestone and Camooweal Dolostone. Contains >1100 ppm Zn at depth in the Trackrider prospect area. Is associated with the phosphate deposits at Ammaroo and near Ooratippra. Forms a reservoir-seal couplet with underlying Thorntonia Limestone, as well as intraformational couplets in middle and upper parts of the Formation. Is a potentially world-class petroleum source rock. Also a potential petroleum reservoir, and its shales provide a regional seal. Has had hydrocarbon shows in drilled wells.||Narpa Group.||Disconformably overlies Thorntonia Limestone or Red Heart Dolostone. Is overlain conformably by Steamboat Sandstone and Chabalowe or Arrinthrunga Formations.|Foetid pyritic-carbonaceous black shale and laminated dolostone interval with minor dolomitic quartz sandstone and conglomerate; overlain by dolostone, limestone and minor quartzose dolostone and siliciclastic mudstone.|12-JUL-16
645|Arthur Creek Formation|69561|5|Briefly described|p33 fig 2, p34|Boomerangian|Templetonian|Trilobite fossil assemblage constrains age of underlying Thorntonita Limestone.||||Overlain by Steamboat Sandstone, Chabalowe Formation|Fossiliferous siltstone.|
645|Arthur Creek Formation|69573|6|Mentioned|p656, 659, 661|||Georgina Basin. Features Cambrian Stage 5 fossil sites.||||||
645|Arthur Creek Formation|69673|4|Described|p103,    p120, p123,   p128,  p131, p141|Cambrian|Cambrian |Georgina Basin. Petroleum source rock, potential as a conventional and unconventional reservoir rock also. Shale within this unit may form a hydrocarbon seal. More than 483m thick.||||Disconformably overlies Thorntonia Limestone, Red Heart Dolostone, conformably overlain by Steamboat Sandstone, Chabalowe Formation||
645|Arthur Creek Formation|70380|6|Mentioned|p745|Series 3|Series 3|Southern Georgina Basin.||||||
645|Arthur Creek Formation|70723|5|Briefly described|p22, p24 Fig. 2|Cambrian|Cambrian|Georgina Basin.||Narpa Group||Overlies Thorntonia Limestone, Overlain by Chabalowe Formation or Steamboat Sandstone.|Sandy limestone.|
645|Arthur Creek Formation|70752|6|Mentioned|p140-141|||Georgina Basin. Brachiopod species discussed.||||||
645|Arthur Creek Formation|70951|4|Described|p1069-1072,1074-1084||Wuliuan|Geological province: Georgina Basin. Base of Arthur Creek Formation interpreted as older in Dulcie Sycline (Templetonian/Stage 5) than in Toko Syncline (Floran/Drumian) and is characterised by regionally extensive organic-rich shales with high TOC across the southern basin depocenters from west to east (Dulcie Domain, older succession; Toko Domain, younger succession). Quartz and carbonate dominated in the Dulcie Domain, carbonate, white mica and quartz-dominated in Toko Domain.||Unit of Narpa Group.||Underlain by Thorntonia Limestone. Overlain by Steamboat Sandstone.|Characterised by regionally extensive basal organic-rich shales with high TOC. ?overlying units characterised by a mixture of quartz rich, calcite and dolomite mineralogy.|08-MAR-23
645|Arthur Creek Formation|71800|6|Mentioned|p26 fig 3|Middle Cambrian|Middle Cambrian|Georgina Basin.||||Overlain by the Arrinthrunga Formation.||
645|Arthur Creek Formation|72321|4|Described|Fig 2, p3-4, p5, 6, 7|Guzhangian|Wulian|Dulcie Syncline, Toko Syncline, Georgina Basin. Diachronous. Youngs to East. Age range in Dulcie Syncline is latest Ordian to Undillan or younger, but Boomerangian sediments absent or thin. Age more restricted  in Toko Syncline from Floran, but up to Boomerangian (from agnostid trilobites).||of Narpa Group.||Overlain by Steamboat Sandstone in Toko Syncline. Lower part in Dulcie Syncline unconformably overlies Hay River Formation and correlates with Thorntonia Limestone, Undilla Sub-Basin.||
645|Arthur Creek Formation|72515|5|Briefly described|Map Legend|Cambrian|Cambrian|Jervois Range Special Map Sheet. Georgina Basin. Contains fossil trilobites, brachiopods, echinoderms.||Narpa Group||Overlain by the Steamboat Sandstone. Disconformably overlies the Thorntonia Limestone.|Black shale; pyritic-carbonaceous, undulose laminated, flaser bedded; minor laminated dolostone; dolomitic sandstone, conglomerate; dolostone, limestone; minor mudstone; fossiliferous.|05-JUL-22
645|Arthur Creek Formation|72516|3|Fully described|p11-12, p91-93|Cambrian Series 3|Cambrian Series 3|Georgina Basin. Poorly to moderately exposed in ELKEDRA, HUCKITTA, TOBERMORY, HAY RIVER, SANDOVER RIVER and JERVOIS RANGE SPECIAL map sheets. Outcrops in the Jervois Range and north of the Johansen Range. Type section in cored drillhole NTGS99/1. Informally subdivided into an upper and lower interval. The lower interval was deposited in dysoxic to anoxic, deep marine environment whilst the upper interval was deposited in an aerobic, restricted, platformal marine environment above wave base. Contains fossil trilobites, brachiopods and echinoderms in the upper interval which indicate a Series 3 of the Cambrian depositional age. 250m thick in the map sheet area, 42-720m thick elsewhere. Interpreted to correlate wioth the Anthony Lagoon beds, Wonarah beds, Ranken Limestone, Camooweal Dolostone, Age Creek Formation, Currant Bush Limestone, V-Creek Limestone, Mail Change Limestone, Split Rock Sandstone, Inca Formation, Devoncourt Limestone, Roaring Siltstone, Beetle Creek Formtion, Blazan Shale, Quita Formation, Selwyn Range Limestone, Giles Creek Dolostone, Hugh River Shale, Tempe Formation.||Narpa Group||Conformably and gradationally overlain by the Arrinthrunga Formation. Conformably overlain  by Steamboat Sandstone. Disconformably overlies the Thorntonia Limestone and Red Heart Dolostone.|Black shale; pyritic, carbonaceous, undulose-laminated, flaser bedded; minor laminated dolostone; dolomitic sandstone, conglomerate. Dolostone, limestone and minor mudstone.|14-APR-22
645|Arthur Creek Formation|73288|5|Briefly described|p697-700, 702-707, 709 Fig.10, 710-713|Middle Cambrian|Middle Cambrian|Southern Georgina Basin. Non-economic oil and gas shows have been recorded. Downhole (Hylogger) logs; scratch test results tabulated.||Narpa Group.||Unconformably overlies Thorntonia Limestone. Is overlain by the Chabalowe Formation.|Upward-shallowing sequence with basal marine anoxic dolomitic organic-rich shales (TOC up to 16 wt%), grading up to mixed clastic/carbonate sediments and capped by near-shoreline carbonate and quartz-rich sandstone.|07-MAR-23
668|Arumbera Sandstone|9199|5|Briefly described|Map legend|Cambrian|Cambrian|Of the Pertaoorrta Group. Red-brown sandstone, siltstone, conglomerate sandstone; fossiliferous. Geological Province: Amadeus Basin.||||||16-JUN-09
668|Arumbera Sandstone|9814|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Pertaoorrta Group. Silty sandstone, siltstone.||||||
668|Arumbera Sandstone|12891|5|Briefly described|p733 Fig. 2|Early Cambrian|Early Cambrian|Geological province: Amadeus Basin.||||||07-FEB-11
668|Arumbera Sandstone|12951|6|Mentioned|p143|||Amadeus Basin.||||Lower part correlated with Elkera Formation, Georgina Basin.||
668|Arumbera Sandstone|22561|4|Described|p18|Neoproterozoic|Neoproterozoic|Age: 570-580 Ma (estimated base age p18).||||||18-JUL-06
668|Arumbera Sandstone|22563|6|Mentioned|p55|||||||||
668|Arumbera Sandstone|22564|5|Briefly described|p59|Early Cambrian|Neoproterozoic|||||||
668|Arumbera Sandstone|22565|4|Described|p71 & Table 1|||Approx. thickness measured from seismic data - 740 m thick||||||
668|Arumbera Sandstone|22566|4|Described|p82 &p74|Early Cambrian|Neoproterozoic|Stratigraphic relationships described p82.  Of the Pertaoorrta Group.||||||18-JUL-06
668|Arumbera Sandstone|22567|6|Mentioned|p91|||||||||
668|Arumbera Sandstone|22646|4|Described|p 100|Cambrian|Neoproterozoic|informal name - lower Arumbera Sandstone is mentioned (p 101).||||||18-JUL-06
668|Arumbera Sandstone|22649|6|Mentioned|Fig 1 on p 138|Cambrian|Neoproterozoic|||||||
668|Arumbera Sandstone|22650|6|Mentioned|p 159|Cambrian||Parent - Pertaoorrta Group.||||||
668|Arumbera Sandstone|22651|4|Described|p 176|Neoproterozoic|Neoproterozoic|Informally divided into upper and lower Arumbera Sandstone. Forms the base of the Pertaoorrta Group.||||||18-JUL-06
668|Arumbera Sandstone|22652|5|Briefly described|p 195|||||||||
668|Arumbera Sandstone|22653|6|Mentioned|p 228||Cambrian|||||||
668|Arumbera Sandstone|22654|6|Mentioned|p 245|||||||||
668|Arumbera Sandstone|22746|5|Briefly described|p519, p529|Neoproterozoic III|Neoproterozoic III|||||||
668|Arumbera Sandstone|22762|5|Briefly described|p369|Early Cambrian|Neoproterozoic|||||||
668|Arumbera Sandstone|22763|5|Briefly described|p398|Cambrian|Neoproterozoic|||||||
668|Arumbera Sandstone|22804|4|Described|p441-451|Cambrian|Neoproterozoic|Of Pertaoorrta Group.  Informally divided into upper and lower Arumbera Sandstone.||||||18-JUL-06
668|Arumbera Sandstone|22805|4|Described|p471-472|Neoproterozoic|Neoproterozoic|||||||
668|Arumbera Sandstone|22807|6|Mentioned|p500|Early Cambrian|Neoproterozoic|||||||
668|Arumbera Sandstone|22816|5|Briefly described|p10 Fig. 4|Cambrian|Neoproterozoic|Amadeus Basin||||||
668|Arumbera Sandstone|22824|5|Briefly described|p533|||Of the Pertaoorrta Group.||||||18-JUL-06
668|Arumbera Sandstone|22826|4|Described|p571|Early Cambrian|Neoproterozoic|||||||
668|Arumbera Sandstone|22828|6|Mentioned|p591|||||||||
668|Arumbera Sandstone|22901|6|Mentioned|76 fig 2|||Geol province Amadeus Basin||||||
668|Arumbera Sandstone|22907|6|Mentioned|42|||Geol province Amadeus Basin||||||
668|Arumbera Sandstone|23250|5|Briefly described|p1124 Fig.2|Early Cambrian|Neoproterozoic III|Subdivided informally into Unit 1,2,3 and 4. Correlate of Bonney Sandstone, Rawnsley Quartzite, Uratanna Formation and Hawker Group.||||||
668|Arumbera Sandstone|23282|6|Mentioned|p65|||Geol. Prov:  Amadeus Basin. May be equivalent to Narana Formation.||||||18-JUL-06
668|Arumbera Sandstone|23287|6|Mentioned|Fig.4|||Age: Upper Ediacaran. of Amadeus Basin.||||||07-MAY-13
668|Arumbera Sandstone|23314|5|Briefly described|333||Neoproterozoic III|||||||
668|Arumbera Sandstone|23361|5|Briefly described|16 Fig.4|Neoproterozoic III|Neoproterozoic|||||||
668|Arumbera Sandstone|23557|5|Briefly described|p95 Fig.1|Neoproterozoic III|Neoproterozoic III|Geological Province: Amadeus Basin.||||||
668|Arumbera Sandstone|23806|5|Briefly described|p1122 Fig. 1|Neoproterozoic|Neoproterozoic|||||||
668|Arumbera Sandstone|24064|5|Briefly described|p229 Fig.7|Cambrian|Cambrian|Of Pertaoorrta Group. Geological Province: Amadeus Basin.||||||
668|Arumbera Sandstone|24111|5|Briefly described|p214 Fig. 9|Cambrian|Neoproterozoic|Geological Province: Amadeus Basin.  See also p215 Fig. 11.||||||
668|Arumbera Sandstone|24301|5|Briefly described|p17|Neoproterozoic|Neoproterozoic|Geological Province: Amadeus Basin||||||
668|Arumbera Sandstone|24334|5|Briefly described|p48 Tb.1|Early Cambrian|Neoproterozoic|Age: 530 - 560 Ma.||||||18-JUL-06
668|Arumbera Sandstone|24442|6|Mentioned|p38|||Geological Province: Victoria Basin.||||||
668|Arumbera Sandstone|29721|6|Mentioned|Table 44|||||||||
668|Arumbera Sandstone|29972|6|Mentioned|Table 1|||Lower Cambrian.||||||05-SEP-18
668|Arumbera Sandstone|30220|6|Mentioned|Fig.13|||||||||
668|Arumbera Sandstone|30258|6|Mentioned|Fig.2|||Cambrian age. Part of Pertaoorrta Group.||||||05-SEP-18
668|Arumbera Sandstone|30313|6|Mentioned|p56|||||||||
668|Arumbera Sandstone|30374|6|Mentioned|Fig.5|||Correlation.||||||05-SEP-18
668|Arumbera Sandstone|30544|6|Mentioned|p48|||On map legend.||||||05-SEP-18
668|Arumbera Sandstone|30659|6|Mentioned|p87|||Proterozoic-Cambrian age||||||
668|Arumbera Sandstone|30660|6|Mentioned|Table 1|||Lower Cambrian age||||||
668|Arumbera Sandstone|30661|6|Mentioned|Table 1|||||||||
668|Arumbera Sandstone|30662|6|Mentioned|p188|||Palaeomagnetic dates||||||
668|Arumbera Sandstone|30727|6|Mentioned|p45|||Palaeomagnetic pole positions||||||
668|Arumbera Sandstone|31026|5|Briefly described|p61|||||||||
668|Arumbera Sandstone|31973|6|Mentioned|p3|||Correlation||||||
668|Arumbera Sandstone|32720|6|Mentioned|Table 1|||||||||
668|Arumbera Sandstone|32722|6|Mentioned|Fig.3|||Stromatolite. Adelaidean.||||||05-SEP-18
668|Arumbera Sandstone|33025|6|Mentioned|p928|||Precamb.-Camb.||||||
668|Arumbera Sandstone|33307|6|Mentioned|Fig.6|||||||||
668|Arumbera Sandstone|33625|6|Mentioned|p187|||||||||
668|Arumbera Sandstone|33655|5|Briefly described|p101|||L.Camb.||||||
668|Arumbera Sandstone|33734|5|Briefly described|p495|||Refers Daily (1972). Trace fossils.||||||
668|Arumbera Sandstone|33761|6|Mentioned|p146|||Adelaidean - Cambrian.||||||05-SEP-18
668|Arumbera Sandstone|34111|4|Described|Table 2|||See also Table 4. Cambrian||||||
668|Arumbera Sandstone|34287|6|Mentioned|p42|||||||||
668|Arumbera Sandstone|34433|6|Mentioned|p17|||||||||
668|Arumbera Sandstone|34442|5|Briefly described|Table 1|||Cambrian.||||||05-SEP-18
668|Arumbera Sandstone|34488|4|Described|Table 1|||See also pp10,16. Cambrian||||||18-JUL-06
668|Arumbera Sandstone|34557|6|Mentioned|p357|||||||||
668|Arumbera Sandstone|34579|6|Mentioned|p15|||Cambrian. See also pp16,17.||||||05-SEP-18
668|Arumbera Sandstone|35088|6|Mentioned|p91|||Also Fig.2.||||||
668|Arumbera Sandstone|35102|6|Mentioned|Fig.2|||||||||
668|Arumbera Sandstone|35136|6|Mentioned|Fig.2|||||||||
668|Arumbera Sandstone|35221|6|Mentioned|p14|||||||||
668|Arumbera Sandstone|35222|6|Mentioned|p10|||||||||
668|Arumbera Sandstone|35798|6|Mentioned|p310|||||||||
668|Arumbera Sandstone|35805|6|Mentioned|Fig.3|||||||||
668|Arumbera Sandstone|35863|6|Mentioned|Table 1|||||||||
668|Arumbera Sandstone|36014|6|Mentioned|p151|||||||||
668|Arumbera Sandstone|36198|6|Mentioned|p294|||See also Fig.III.2||||||
668|Arumbera Sandstone|36898|6|Mentioned|Fig.4|||||||||
668|Arumbera Sandstone|37015|6|Mentioned|p75|||||||||
668|Arumbera Sandstone|37371|6|Mentioned|p387|||||||||
668|Arumbera Sandstone|37462|4|Described|Table 4.IX|||||||||
668|Arumbera Sandstone|37627|6|Mentioned|p185|||||||||
668|Arumbera Sandstone|37818|6|Mentioned|p81|||||||||
668|Arumbera Sandstone|37928|6|Mentioned|Fig.4|||||||||
668|Arumbera Sandstone|37929|6|Mentioned|Fig.2|||||||||
668|Arumbera Sandstone|38445|6|Mentioned|p102|||||||||
668|Arumbera Sandstone|38606|6|Mentioned|Map legend|Early Cambrian|Neoproterozoic|Late Proterozoic to Early Cambrian.||||||05-SEP-18
668|Arumbera Sandstone|38885|6|Mentioned|Map legend|Early Cambrian|Neoproterozoic|Early Cambrian - Late Proterozoic.||||||05-SEP-18
668|Arumbera Sandstone|39210|5|Briefly described|p38|||See also p54.||||||05-SEP-18
668|Arumbera Sandstone|39583|6|Mentioned|Map legend|Early Cambrian|Neoproterozoic|Late Proterozoic to Early Cambrian.||||||05-SEP-18
668|Arumbera Sandstone|39757|6|Mentioned|p1607|||||||||
668|Arumbera Sandstone|39898|5|Briefly described|Map legend|Early Cambrian|Neoproterozoic|White, grey and purple-brown sandstone at base; siltstone in middle; purple-brown to pale brown sandstone at top. Geological Province: Amadeus Basin.||||||14-FEB-06
668|Arumbera Sandstone|39931|6|Mentioned|Map legend|Early Cambrian|Neoproterozoic|Late Proterozoic to Early Cambrian.||||||05-SEP-18
668|Arumbera Sandstone|40105|6|Mentioned|p311|||See also P319||||||
668|Arumbera Sandstone|40254|6|Mentioned|p284|||||||||
668|Arumbera Sandstone|40740|3|Fully described|p15|||See also P||||||
668|Arumbera Sandstone|40810|4|Described|p3|||||||||
668|Arumbera Sandstone|40852|6|Mentioned|p34|||||||||
668|Arumbera Sandstone|40906|6|Mentioned|Fig.9|||||||||
668|Arumbera Sandstone|40998|6|Mentioned|p431|||||||||
668|Arumbera Sandstone|41005|6|Mentioned|Fig.2|||||||||
668|Arumbera Sandstone|41018|6|Mentioned|Fig.2|||||||||
668|Arumbera Sandstone|41115|4|Described|p1388|||Formerly Eninta Formation.||||||18-JUL-06
668|Arumbera Sandstone|41190|6|Mentioned|Fig.4|||||||||
668|Arumbera Sandstone|41203|5|Briefly described|p25|||See also p47.||||||05-SEP-18
668|Arumbera Sandstone|41224|6|Mentioned|Fig.2|||||||||
668|Arumbera Sandstone|41233|3|Fully described|p15|||||||||
668|Arumbera Sandstone|41270|6|Mentioned|Table 1|||||||||
668|Arumbera Sandstone|41429|5|Briefly described|p246|||||||||
668|Arumbera Sandstone|41618|6|Mentioned|Fig.2|||||||||
668|Arumbera Sandstone|41711|6|Mentioned|p262|||||||||
668|Arumbera Sandstone|41717|5|Briefly described|p355|||||||||
668|Arumbera Sandstone|41801|4|Described|p210|||||||||
668|Arumbera Sandstone|42037|5|Briefly described|Table 3 P79|||||||||
668|Arumbera Sandstone|42059|5|Briefly described|p130|||||||||
668|Arumbera Sandstone|42082|6|Mentioned|Fig.3 P323|||||||||
668|Arumbera Sandstone|42504|5|Briefly described|p76|||||||||
668|Arumbera Sandstone|42643|6|Mentioned|p21|||Amadeus Basin||||||
668|Arumbera Sandstone|42661|6|Mentioned|p130|||||||||
668|Arumbera Sandstone|42886|4|Described|p223|||see also Fig.2 p219.||||||05-SEP-18
668|Arumbera Sandstone|42940|5|Briefly described|Plate 2|Cambrian|Cambrian|Sandstone, siltstone, shale; marine fossils.  Age: 590-500Ma. Geological province: Amadeus Basin.||||||23-JAN-08
668|Arumbera Sandstone|43011|6|Mentioned|Table 2,p12|||||||||
668|Arumbera Sandstone|43225|5|Briefly described|Map Legend|Cambrian|Neoproterozoic|Of Pertaoorrta Group.||||||22-DEC-09
668|Arumbera Sandstone|43230|6|Mentioned|p9||Cambrian|Reservoir target.||||||
668|Arumbera Sandstone|43503|6|Mentioned|11-50|Atdabanian||from Ediacaran to||||||
668|Arumbera Sandstone|43595|5|Briefly described|p548,Fig.5-33,549|Cambrian|Adelaidean|||||||
668|Arumbera Sandstone|43646|6|Mentioned|Fig.3,p554|Early Cambrian|Precambrian|||||||
668|Arumbera Sandstone|43648|6|Mentioned|Fig.27,p509|||||||||
668|Arumbera Sandstone|43649|6|Mentioned|p457|||||||||
668|Arumbera Sandstone|43756|6|Mentioned|p542|||||||||
668|Arumbera Sandstone|43781|6|Mentioned|p4||Cambrian|Interval of mixed magnetic polarity||||||
668|Arumbera Sandstone|44111|6|Mentioned|p.58 Fig. 2|||in Amadeus Basin. Presented as Arumbera 1 & 2 and Arunbera [sic] 3 & 4 in Fig. 2.||||||
668|Arumbera Sandstone|44133|6|Mentioned|p42|||Also listed as upper Arumbera Sandstone.||||||
668|Arumbera Sandstone|44335|4|Described|p.10||Cambrian|Table 2.||||||
668|Arumbera Sandstone|44336|14|Not recorded|map legend||Cambrian|Cambrian pt of Pertaoorrta Gp. SG/53-3.||||||
668|Arumbera Sandstone|44402|5|Briefly described|map legend||Cambrian|Of Pertaoorrta Group.||||||18-JUL-06
668|Arumbera Sandstone|44433|14|Not recorded|map legend||Cambrian|||||||
668|Arumbera Sandstone|44484|14|Not recorded|Tb.2|||||||||
668|Arumbera Sandstone|44497|4|Described|p.9, Table 1||Cambrian|SF/53-13.||||||
668|Arumbera Sandstone|44498|14|Not recorded|map legend||Cambrian|Part of Pertaoorrta Group.||||||
668|Arumbera Sandstone|45041|4|Described|p57|||Refers Wells et al. (1967). L.Camb.||||||
668|Arumbera Sandstone|45102|6|Mentioned|p43|||See also p49.||||||05-SEP-18
668|Arumbera Sandstone|45155|6|Mentioned|p34|||Amadeus Basin. See also Figs 7 & 8||||||
668|Arumbera Sandstone|46730|5|Briefly described|p17|||Of Pertaoorrta Group.||||||
668|Arumbera Sandstone|46865|6|Mentioned|Fig.2|||||||||
668|Arumbera Sandstone|46903|6|Mentioned|p53|||||||||
668|Arumbera Sandstone|46928|6|Mentioned|Table 1|||||||||
668|Arumbera Sandstone|46957|6|Mentioned|p165|||||||||
668|Arumbera Sandstone|47035|6|Mentioned|p83|||||||||
668|Arumbera Sandstone|48639|4|Described|p.6||Early Cambrian|Lower Cambrian. See page 1,4,16, Pl.1,Sh.3.||||||
668|Arumbera Sandstone|48865|14|Not recorded|Fig.4,opp.p.10|||Unit of Pertaoorrta Group (F53-13).||||||
668|Arumbera Sandstone|48890|4|Described|p.31||Cambrian|See also Tables, Figs, Plates. Of the Pertaoorrta Group.||||||18-JUL-06
668|Arumbera Sandstone|48963|6|Mentioned|Fig.3|||||||||
668|Arumbera Sandstone|50246|5|Briefly described|p8-9, p20 Fig. 2|Early Cambrian|Neoproterozoic|Conformably overlain by Todd River Dolomite. A cyclical red-brown mudstone and sandstone comprising four upward coarsening members spanning Neoproterozoic-Cambrian boundary.||||||07-FEB-11
668|Arumbera Sandstone|60287|5|Briefly described|p384|Early Cambrian|Early Cambrian|Thickness: 200 m.||||||
668|Arumbera Sandstone|60547|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Pertaoorrta Group. Red-brown sandstone, siltstone, conglomeratic sandstone; fossiliferous. Geological Province: Amadeus Basin.||||||
668|Arumbera Sandstone|60674|5|Briefly described|Map legend|Cambrian|Neoproterozoic|Brown, thinly-bedded, fine and medium micaceous feldspathic sandstone; minor pebble conglomerate and micaceous siltstone. Geological Province: Amadeus Basin.||||||23-DEC-09
668|Arumbera Sandstone|61309|5|Briefly described|p16 Fig. 4|||Geological Province: Amadeus Basin.||||||06-FEB-08
668|Arumbera Sandstone|61385|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Buff dolomitic limestone, silicified limestone, massive grey calcareous sandstone, chert.   Geological Province: Amadeus Basin.||||||20-OCT-05
668|Arumbera Sandstone|61518|5|Briefly described|Map Legend|Cambrian|Neoproterozoic|Brown, thin bedded fine-and medium grained micaceous feldspathic sandstone; minor pebble conglomerate and micaceous siltstone. Geological Province: Amadeus Basin.||||||23-DEC-09
668|Arumbera Sandstone|61732|3|Fully described|p4 Fig. 3, p99|Cambrian|Marinoan|Formerly "Arumbera Greywacke". Once part of Pertaoorta Formation (now Pertaoorrta Group). Conformably overlies the Julie Fm; overlain by Hugh River Shale, Todd River and Giles Creek Dolomites. Thick: 2km. Geol.Prov: See also p5 Tb. 1, p91.||||||17-APR-13
668|Arumbera Sandstone|62359|6|Mentioned|p554|||Geological Province: northern Amadeus Basin. ||||||
668|Arumbera Sandstone|62376|5|Briefly described|p18|Early Cambrian|Late Proterozoic|Of the Pertaoorrta Group. Geological Province: Amadeus Basin.||||||09-FEB-10
668|Arumbera Sandstone|62379|5|Briefly described|p7 Fig. 2, p24|Middle Cambrian|Late Proterozoic|Of the Pertaoorrta Group. Geological Province: Amadeus Basin.||||||
668|Arumbera Sandstone|62428|5|Briefly described|p351 Tb. 6|Early Cambrian|Neoproterozoic III|Unit close to the Neoproterozoic-Cambrian border with age of: ~540Ma. Palaeomagnetic data.||||||10-FEB-09
668|Arumbera Sandstone|62453|5|Briefly described|p12 Fig. 8|Cambrian|Ediacaran|Geological Province: Amadeus Basin.||||||
668|Arumbera Sandstone|62595|5|Briefly described|pp8-9, p29 Fig.6, p30 Fig.7.|Cambrian|Neoproterozoic|Contains a variety of non-skeletal metazoan fossils, contemporaneous with Ediacara fauna, and a wealth of trace fossils in upper parts. 1000-1200 Ma detrital zircons reflect uplift of the Musgrave Block during the Petermann Orogeny between 570-530 Ma.||||Is conformably overlain by Todd River Dolomite.|A cyclical red-brown mudstone and sandstone unit consisting of four upward-coarsening members; massive, fine- to medium-grained, dirty sandstone into laminated shales, siltstones and rare carbonates.|
668|Arumbera Sandstone|62903|6|Mentioned|p730 Fig.1|||Amadeus Basin. Presented in figure as Arumbera.||||overlies Julie Formation||
668|Arumbera Sandstone|62984|5|Briefly described|p14|||Correlated with Central Mount Stuart Formation. Geological Province: Amadeus Basin.||||||23-JAN-07
668|Arumbera Sandstone|63397|6|Mentioned|p15|||Geological Province: Amadeus Basin.||||||23-JUL-07
668|Arumbera Sandstone|63458|6|Mentioned|p897 Fig.19. |Cambrian|Ediacaran|Amadeus Basin. Appears only as Arumbera 1&2, 3&4.||||Overlies Julie Formation.||
668|Arumbera Sandstone|63562|4|Described|p338 fig 3, p341, p345-8, p351-352|Early Cambrian|Ediacaran|Of Amadeus Basin. Either distal facies of foreland basin sediments, or reworked "autocannibalised" foreland sediments. Most zircons in it are 1.2-1.0 Ga, suggesting a source in Musgrave Inlier.||||Overlies Julie Formation. Correlated with Mount Baldwin Formation. Overlain by Todd River Dolomite.|Cross-bedded, fine- to medium-grained, red-brown quartz sandstone. Contains trace fossils.|
668|Arumbera Sandstone|64068|6|Mentioned|p51, 56, 224|||Amadeus Basin. Correlated in part with Central Mount Stuart Formation, part 3-4 with Octy Formation, Neutral Junction Formation, southern Georgina Basin.||||||
668|Arumbera Sandstone|64103|6|Mentioned|p401|Early Cambrian|Ediacaran|Geological Province: Amadeus Basin.||||||07-FEB-11
668|Arumbera Sandstone|64625|5|Briefly described|p244-245, p250-251|Cambrian|Neoproterozoic|Amadeus Basin||||Disconformably overlies Julie Formation, overlain by Giles Creek Dolomite|Deep red sandstone.|
668|Arumbera Sandstone|64778|6|Mentioned|p13, 15-16, 18, 22|Neoproterozoic|Neoproterozoic|Amadeus Basin. Thermal history summarised. Max. palaeotemperature analysis summary.|590-560 Ma.|||||
668|Arumbera Sandstone|64794|6|Mentioned|p238 fig 2|Early Cambrian|Ediacaran|||||||
668|Arumbera Sandstone|64797|6|Mentioned|p153 Fig.2|Cambrian|Ediacaran|Amadeus Basin. Lithology not shown in diagram.||||||
668|Arumbera Sandstone|64809|4|Described|p1-2, p3 Fig.2, p6 Fig.4, p11 Fig.10   |Early Cambrian|Late Proterozoic|See also p12, p13 Fig.13, p15 Fig.15. Hydrocarbon reservoir; a principal exploration objective. Sourced from Musgrave Province to N and NE; deposited in predominantly deltaic environment.||Unit in Pertaoorrta Group.||Conformably (gradationally) overlies Julie Formation.|Molasse sediments: ridge-forming sandstone, recessive siltstone; contains trace fossils.|
668|Arumbera Sandstone|65233|3|Fully described|p3 Fig. 2, p7|Early Cambrian|Late Neoproterozoic|Basal unit of Pertaoorrta Group. Conformable on Julie Formation. Geological province: Amadeus Basin/Carmichael Sub-basin. Divided into 2 main depositional successions of 800m and 500m thicknesses; but max. thickness is 2000m in NE. Fluvio-deltaic.||||||07-FEB-11
668|Arumbera Sandstone|65237|6|Mentioned|p5|||Mentioned only as a correlative of the Elkera Formation in the southern Georgina Basin. Geological province: Amadeus Basin.||||||07-FEB-11
668|Arumbera Sandstone|65256|6|Mentioned|p19|Cambrian||Of the northern Amadeus Basin. Correlated with Mount Currie Conglomerate.||||||
668|Arumbera Sandstone|65272|5|Briefly described|p319, p320|Early Cambrian|Ediacaran|Amadeus Basin. Deposited during the Petermann Ranges Orogeny (570-530 Ma).||||||
668|Arumbera Sandstone|65341|5|Briefly described|pp17-18.|Ediacaran|Ediacaran|Amadeus Basin. Contains elements of the Mount Skinner fauna, similar to the Tops Member of Central Mount Stuart Formation. Upper parts also correlated with Octy Formation.||||||
668|Arumbera Sandstone|65342|6|Mentioned|p4.|||Amadeus Basin. Max. thickness at least 386 m.||||Overlies Julie Formation (equivalent). Is overlain by Todd River Dolostone.||
668|Arumbera Sandstone|65365|5|Briefly described|p10 Fig. 4|Cambrian|Ediacaran|Amadeus Basin. Shown to include an unconformity above the known Ediacara fauna.||||||
668|Arumbera Sandstone|65366|5|Briefly described|p23 Fig. 3|Cambrian|Ediacaran|Amadeus Basin. Shown to include an unconformity above the known Ediacara fauna.||||||
668|Arumbera Sandstone|65410|6|Mentioned|p74.|||Amadeus Basin. Makes up Supersequence 4.||||||
668|Arumbera Sandstone|66589|6|Mentioned|p178|Early Cambrian|Early Cambrian|Case studies cited; not visited in the field by the authors of this study.||||||
668|Arumbera Sandstone|67326|5|Briefly described|p2-6, p13, Appx.2|Neoproterozoic|Neoproterozoic|Amadeus Basin. Intersected by stratigraphic drillhole LA05DD01. Composite log.||Pertaoorrta Group.||Overlies Julie Formation. Is overlain by Todd River Dolostone and Chandler Formation.||
668|Arumbera Sandstone|67565|4|Described|p5 Fig.3, p39, p46.|Tommotian|Ediacaran|Amadeus Basin. Includes the unit previously mapped (Ranford, 1969) as Eninta Sandstone in the Gardiner Range. Thickness c.1200 m. Braided stream and prograding deltaic sediments probably sourced from highlands produced by the 570-530 Petermann Orogeny in the Musgrave Block. Sparse Ediacaran macrofauna towards the base; diverse Cambrian ichnofauna towards the top.||||Overlies the Pertatataka Formation and the Bitter Springs Formation unconformably.|Red-brown to purple-brown, thinly-bedded, fine- and medium-grained ferruginous, micaceous, feldspathic sandstone with minor pebble conglomerate and micaceous siltstone.|
668|Arumbera Sandstone|67620|6|Mentioned|p5, 22|Cambrian|Ediacaran|Amadeus Basin. In the correlation table on p5, is shown as two units: Arumbera 1 and 2, overlain by Arumbera 3 and 4. Mis-spelt as Arumberia Sandstone on p22; contains the microbial mat structure named Arumberia[sic].||||Overlies Julie Formation.||
668|Arumbera Sandstone|67856|5|Briefly described|p338 fig 4-30, p345, 346|Cambrian|Ediacaran|Shown in two parts. Includes unconformity. Contains a late Proterozoic metazoan fauna.||Of Pertaoorta Group.||Overlies Julie Formation.||
668|Arumbera Sandstone|68100|6|Mentioned|p27|||Amadeus Basin. Detrital zircon ages mentioned.||||||
668|Arumbera Sandstone|68271|5|Briefly described|p696|Ediacaran|Ediacaran|Adelaide Rift Complex. Similar lithology and taxa to Bonney Sandstone. Interpreted stratigraphic age of c. 600 Ma. Sediments like dervied from Musgrave Block.|c. 600 Ma|||||
668|Arumbera Sandstone|68323|5|Briefly described|p1-10, p12-13, p15|Early Cambrian|Neoproterozoic|Mineralogy detailed: dominated by carbonate, with lesser phengite and quatrz. Tray screem imagery.||Pertaoorrta Group.||Is overlain by Tempe Formation.|Carbonate-rich.|
668|Arumbera Sandstone|69437|5|Briefly described|p22:4-5, 8-10, 14|Early Cambrian|Ediacaran|Amadeus Basin, Centralian A Superbasin. Supersequence 4. The lower part is correlated with lower part of Yuendumu Sandstone. The upper part is included in the Centralian B Superbasin. Contains uneconomic sediment-hosted Cu occurrences.||||Overlies Inindia beds and Julie Formation. Is overlain by Namatjira, Tempe Formations and Todd River Dolostone. Equivalent to Central Mount Stuart Formation and (probably) to Carnegie Formation.|Sandstone, siltstone, shale and minor conglomerate.|12-JUL-16
668|Arumbera Sandstone|69438|3|Fully described|p23:2-8, 17-18, 20-21, 23-30, 43, 50, 53|Early Cambrian|Ediacaran|See also 23:59-60. Defined by Wells et al. (1967) as the basal Formation of the Pertaoorrta Group. Had several earlier names. Thins to the W. Comprises two fluvio-deltaic successions of upward-coarsening siltstone and sandstone, separated by a disconformity. Total thickness up to 1300m. Amadeus Basin. Forms prominent red-brown strike ridges. Includes the former Eninta Sandstone. Provenance briefly discussed; detrital zircons suggest mainly from the Musgrave Province to the S. Contains Ediacaran fauna, ichnospecies and shelly fossils. The position of the Neoproterozoic-Cambrian boundary within this unit is briefly discussed. Is overlain disconformably by Chandler Formation and Hugh River Shale, and unconformably by Tempe Formation. Contains dispersed, non-economic copper mineralisation in Namatjiras prospect (Areyonga Copper Deposit), and elsewhere eg (Ellery Creek). Has provided numerous gas shows. Reservoirs are sealed by Chandler Formation salt and possibly Tempe Formation or Giles Creek Dolostone shales.||Pertaoorrta Group.||Overlies Julie Formation conformably to disconformably. Correlative of Winnall beds and possibly Carnegie Formation. Is overlain by and interfingers with Todd River Dolostone and Namatjira Formation.|Red-brown to purple-brown, thinly-bedded, fine- and medium-grained, ferruginous, micaceous feldspathic sandstone, with minor pebble conglomerate, micaceous siltstone and dolostone.|12-JUL-16
668|Arumbera Sandstone|69439|6|Mentioned|p24:9|||Amadeus Basin. The uppermost parts of this unit contain the trace fossil Planolites ballandus Webby, which is also preserved in the Yuendumu Sandstone (Ngalia Basin).||||||12-JUL-16
668|Arumbera Sandstone|69443|6|Mentioned|p28:10|||Amadeus Basin. Correlates with part of the Mopunga Group (Georgina Basin).||||||12-JUL-16
668|Arumbera Sandstone|69444|6|Mentioned|p29:2 Fig.29.3|||Amadeus Basin. Detrital zircon probability distribution diagram.||||||12-JUL-16
668|Arumbera Sandstone|69449|6|Mentioned|p34:2 Fig.34.2|Cambrian|Neoproterozoic|Eastern Amadeus Basin.||||||12-JUL-16
668|Arumbera Sandstone|69606|5|Briefly described|p4 fig 2, p16, p19|Cambrian|Ediacaran|Deposited during the Petermann Orogeny. Reservoir of the Pertatataka petroleum system. Amadeus Basin.||||Overlies the Julie Formation, overlain by the Upper Pertaoorta Group. Lower part is correlated with the Carnegie Formation.|Black shales and sandstone.|
668|Arumbera Sandstone|69673|5|Briefly described|p65, p76, p82, p84, p86, p91, p98, p99, |Cambrian|Ediacaran |Hosts dingo and orange gas prospects.||Pertaoorrta Group||Overlain by Namatjira Formation, Todd River Dolostone, correlates with Carnegie Formation, disconformably overlain by Chandler Formation, overlies Julie Formation|Sub-arkosic to quartzic, very fine to coarse graine, locally pebbly sandstone, some siltstone and shale.|
668|Arumbera Sandstone|69937|6|Mentioned|p34|Early Cambrian|Neoproterozoic|||||Overlies Julie Formation.||
668|Arumbera Sandstone|70018|5|Briefly described|p234-235|Neoproterozoic|Neoproterozoic|Amadeus Basin. Entirely of Supersequence 4 in the northern Amadeus Basin. Correlable to Mount Currie Conglomerate/Ayers Rock Arkose, and Winnall Beds.||||Underlain unconformably by Julie Formation.||
668|Arumbera Sandstone|70094|6|Mentioned|p80|||Detrital zircons from this and other units were analysed to establish similar provenances for Harts Range Group, Amadeus and Georgina Basins.||||||
668|Arumbera Sandstone|70416|5|Briefly described|p65 Fig.2|Early Cambrian|Ediacaran|Arunta Province, Amadeus Basin.||||Lateral equivalent to Winnall Group.||
668|Arumbera Sandstone|70749|5|Briefly described|p52-53|Cambrian|Cambrian|Amadeus Basin. Deposited during the Petermann Orogeny. Contains abundant 1300-900 Ma aged detrital zircons.||||||
668|Arumbera Sandstone|70752|5|Briefly described|p126 Fig.1|Proterozoic|Proterozoic|||Pertaoorrta Group.|||Fossiliferous reddish-brown sandstone; siltstone with rare dolostone.|
668|Arumbera Sandstone|70790|6|Mentioned|p271|||||||Equivalent to Bonney Sandstone.||
668|Arumbera Sandstone|70839|5|Briefly described|p329-330,341-343,345|Cambrian|Ediacaran|Of Amadeus Basin. Part of Supersequence 4. Well-dated biostratigraphically and straddles the Ediacaran-Cambrian boundary. Interpreted as part of an immature deltaic succession.||Unit of Pertaoorrta Group.||Basal unit of Pertaoorrta Group.||12-AUG-19
668|Arumbera Sandstone|71001|6|Mentioned|p20 Fig.4, p23, 27|||Amadeus Basin. Carbon isotope correlation graph.||||Unconformably overlies Julie Formation.|Terrestrial sandstone.|
668|Arumbera Sandstone|71080|5|Briefly described|p20,  p29 fig 20, p30, 31|Ediacaran|Ediacaran|Amadeus Basin, NT. Arumberia locally common. Supersequence 4. Reservoir for Dingo Gas field in eastern Amadeus.||||Equivalent to the Carnegie Formation.|Dominantly sandstone. Some shale.|04-FEB-19
668|Arumbera Sandstone|71088|6|Mentioned|p1, p10, p12, p15, p17, p25|Cambrian|Ediacaran|Amadeus Basin. Coeval with the Petermann Orogeny. Displays late Paleoproterozoic peaks in geochronology analyses.||||Overlies the Julie Formation. Equivalent to the Maurice Formation.||01-MAY-23
668|Arumbera Sandstone|71114|5|Briefly described|p170-171, p172-175, p178-9|Terreneuvian|Ediacaran|Amadeus Basin. Age based on rare occurrences of small shelly fossils, and trace fossil Plagiogmus. Deposited in a fluvio-deltaic to basinal environment. 298m thick in Dingo 1 well.|~541-521 Ma|||Conformably overlain by Todd River Dolostone.||14-FEB-18
668|Arumbera Sandstone|71279|5|Briefly described|p353, p355 Fig.2, p358, p365-366|Early Cambrian|Ediacaran|See also p368-370, p372, p376-381, p382. Amadeus Basin. A relatively oxidised unit. Linear magnetic anomalies discussed in detail; magnetic modelling. Appears as Arumbera Shale in Tb.1 (p382).|ca 545-521 Ma (Schmid et al., 2016)|Pertaoorrta Group.|||Sandstone, siltstone, mudstone.|27-OCT-17
668|Arumbera Sandstone|71800|5|Briefly described|p26-p27|Early Cambrian|Ediacaran|Amadeus Basin.||||Overlies the Julie Formation. Overlain by the Todd River Dolostone. Correlative of Winnall beds.|Sandstone and quartz sandstone.|03-MAY-23
668|Arumbera Sandstone|71841|5|Briefly described|p1|Early Cambrian|Ediacaran|Of Amadeus Basin.||Unit of Pertaoorrta Group.||Equivalent to Winnall beds. Underlain by Inindia beds or Julie Formation.||
668|Arumbera Sandstone|71842|5|Briefly described|p2-3,9|Early Cambrian|Ediacaran|Of Amadeus Basin. Nomenclature after Edgoose 2013 (NE Amedeus, NT). Divided into four informal unnamed units.||||Underlain by Julie Formation. Correlable to Amadeus Basin Early Cambrian rocks and Carnegie Formation.||08-JAN-20
668|Arumbera Sandstone|72358|6|Mentioned|p118|Series 2|Ediacaran|Of Amadeus Basin.||||||
668|Arumbera Sandstone|72369|5|Briefly described|p20-21|||Of Amadeus Basin. SHRIMP U-Pb dating by Maidment (2005) and Buick et al (2005) indicate detrital provenance spectra sominated by c. 1200-1000 Ma zircons, indicating a Musgrave Province source. Possibly correlable to Puna Kura Kura Formation.||Unit of Pertaoorrta Group.||||
668|Arumbera Sandstone|72374|6|Mentioned|p12|||Of Amadeus Basin. Correlated with Eninta Sandstone, in part.||||||11-OCT-19
668|Arumbera Sandstone|72375|5|Briefly described|p31|Early Cambrian|Late Neoproterozoic|Of Amadeus Basin. Depositional age constrained to late Neoproterozoic to early Cambrian (Edgoose, 2013; Kositcin et al., 2015).||||Underlain by Julie Formation.||
668|Arumbera Sandstone|72489|6|Mentioned|p5 Fig.4|||Only shown on p5 Fig.4. Geological field images. Same as Arumbera Formation as indicated in the Fig.4. notes.||||Partially overlies Julie Formation.|Includes sandstone.|
668|Arumbera Sandstone|72516|6|Mentioned|p90|Cambrian|Cambrian|Amadeus Basin. Age correlative of the Mount Baldwin Formation.||||||02-JUN-21
668|Arumbera Sandstone|72601|5|Briefly described|p3, p7, p25|Cambrian|Ediacaran|Amadeus Basin. Unit records the Precambrian-Cambrian boundary in the eastern Amadeus Basin by the first appearance of a Cambrian trace fossil assemblage.||||Underlain, unconformably in part, by the Julie Formation. Equivalent to Carnegie Formation, Mu Formation and Winnall beds.||
668|Arumbera Sandstone|73085|4|Described|piii, p1, p3, p7, p11, p13, p27|early Cambrian|Ediacaran|Amadeus Basin. [Written as ?Arumbera Sandstone on p3]. Lithology is here described from a 81-metre-thick equivalent in drillhole LA05DD01. Sandstone below the silicified, altered sandstone breccia at the base of the Tempe Formation were revised to be Arumbera Sandstone equivalents. Partly overlain, equivalent to and underlain by Namatjira Formation.||Pertaoorrta Group [and equivalents?]||Partly underlain by Julie Formation and Inindia beds. Overlain by Tempe Formation[?], Giles Creek Dolostone, Chandler Formation. Partly overlain by and equivalent to Todd River Dolostone.|[Possibly] finely laminated, red, fine-grained sandstone and minor siltstone with buff to grey reduction spots and common intervals of grey-green, fine-grained sandstone without reduction spots and white to pink variably kaolinised sandstone.|
668|Arumbera Sandstone|73086|6|Mentioned|p3, p5, p133|Ediacaran|Ediacaran|Amadeus Basin. Partly included in Supersequence IV. Preserves the Precambrian/Cambrian boundary.||||Underlain by Julie Formation and Inindia beds. Equivalent to Winnall Group.||
668|Arumbera Sandstone|73088|6|Mentioned|p1|Ediacaran|Ediacaran|Amadeus Basin, northeast.||||Underlain by Julie Formation.||
668|Arumbera Sandstone|73180|6|Mentioned|p48 Fig.1|Early Cambrian|Neoproterozoic|Amadeus Basin.||||Conformably overlies the Julie Formation.||
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).||
780|Austral Downs Limestone|8187|5|Briefly described|Map legend|Tertiary|Tertiary|Chert, limestone.||||||24-JUN-04
780|Austral Downs Limestone|8217|5|Briefly described|Map Legend|Tertiary|Tertiary|Chert, Limestone.||||||
780|Austral Downs Limestone|10116|5|Briefly described|Map Legend|Tertiary|Tertiary|Chalcedony, shale, tufa.||||||
780|Austral Downs Limestone|22954|6|Mentioned|Fig3p9||Tertiary|||||||
780|Austral Downs Limestone|24419|5|Briefly described|p19|Miocene|Miocene|Lacustrine limestone deposit cropping out within the western third of URANDANGI 1:250 000 sheet.||||||08-MAR-05
780|Austral Downs Limestone|24442|5|Briefly described|p45|Cenozoic|Cenozoic|Lacustrine deposits.  On the SANDOVER RIVER sheet.||||||
780|Austral Downs Limestone|31532|4|Described|Table 1|||||||||
780|Austral Downs Limestone|32418|6|Mentioned|p2|||||||||
780|Austral Downs Limestone|34395|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
780|Austral Downs Limestone|34441|6|Mentioned|p15|||||||||
780|Austral Downs Limestone|35121|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
780|Austral Downs Limestone|35139|4|Described|Table 2|||||||||
780|Austral Downs Limestone|35798|6|Mentioned|Fig.1|||Geological map of Desert Syncline.||||||
780|Austral Downs Limestone|37607|5|Briefly described|p333|||See also Fig.4||||||
780|Austral Downs Limestone|38532|4|Described|Fig.1|||||||||
780|Austral Downs Limestone|38832|6|Mentioned|p157|||||||||
780|Austral Downs Limestone|39445|5|Briefly described|Table 14|||||||||
780|Austral Downs Limestone|39921|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
780|Austral Downs Limestone|41298|6|Mentioned|Map legend|Miocene||||||||
780|Austral Downs Limestone|43883|14|Not recorded|p18 Fig.4-3|||||||||
780|Austral Downs Limestone|44088|14|Not recorded|Tb.1,opp.p.6|||Similar to limestone on Betoota sheet.||||||
780|Austral Downs Limestone|44121|14|Not recorded|p6|||||||||
780|Austral Downs Limestone|44122|14|Not recorded|Fig.48,321|||||||||
780|Austral Downs Limestone|44133|5|Briefly described|p190 Fig. 10.30|Pliocene|Pliocene|||||||
780|Austral Downs Limestone|44168|14|Not recorded|Tb.1,p6,8|||Similar to Tertiary limestone on Birdsville sheet. Also on NT card.||||||
780|Austral Downs Limestone|44210|14|Not recorded|map, Tb.2|||||||||
780|Austral Downs Limestone|44212|14|Not recorded|p110|||Not on white card.||||||
780|Austral Downs Limestone|44221|14|Not recorded|p87,88,89,102|||||||||
780|Austral Downs Limestone|44222|14|Not recorded|p119,120|||||||||
780|Austral Downs Limestone|44273|14|Not recorded|Map Legend||Tertiary|||||||
780|Austral Downs Limestone|44275|14|Not recorded|Map Legend|||||||||
780|Austral Downs Limestone|44283|14|Not recorded|p.8|||Similar to Brunette Limestone.||||||
780|Austral Downs Limestone|44285|2|Defined|p.9,10||Tertiary|Tb.opp.p.6. Tertiary. Avon Downs. (F53-4). White nodular limestone and dolomite, some chert.||||||
780|Austral Downs Limestone|44291|2|Defined|Tb.1,opp.p6,10,map|||Equivalent to Horse Creek Formation. Overlies Wilgunya Formation.||||||
780|Austral Downs Limestone|44301|14|Not recorded|p.9|||(F53-4)||||||
780|Austral Downs Limestone|44308|14|Not recorded|p11,Tb.2||Tertiary|||||||
780|Austral Downs Limestone|44309|2|Defined|Tb.1,opp.p7,14,map||Tertiary|Fossils rare.||||||
780|Austral Downs Limestone|44312|14|Not recorded|Map Legend||Tertiary|||||||
780|Austral Downs Limestone|44313|14|Not recorded|Map Legend||Tertiary|||||||
780|Austral Downs Limestone|44326|14|Not recorded|Map Legend||Tertiary|||||||
780|Austral Downs Limestone|44334|14|Not recorded|map legend||Tertiary|Tertiary.||||||
780|Austral Downs Limestone|44351|2|Defined|p12-15,18-27,fig.13,||Tertiary|Pls.7-9,11. (Tertiary or Quaternary) Overlies Ninmaroo Formation. Possibly equivalent to Noranside Limestone.||||||
780|Austral Downs Limestone|44355|14|Not recorded|map legend||Tertiary|White nodular limestone and dolomite, some chert.||||||
780|Austral Downs Limestone|44358|4|Described|p12,Tb.1||Tertiary|Age assumed.||||||
780|Austral Downs Limestone|44361|14|Not recorded|Map Legend||Tertiary|||||||
780|Austral Downs Limestone|44362|4|Described|Tb.1,p13||Tertiary|||||||
780|Austral Downs Limestone|44457|2|Defined|p.9, Tb.1, map||Tertiary|Sandover River sheet. (F53-8).||||||
780|Austral Downs Limestone|44458|5|Briefly described|map legend|||Limestone; white, red, crystalline, layered algal(?), siliceous.  Tertiary (?).||||||16-NOV-04
780|Austral Downs Limestone|44469|2|Defined|opp.p.6, Tb.I|||(F53-12). Gastropods.||||||
780|Austral Downs Limestone|44470|5|Briefly described|map legend||Tertiary|||||||02-DEC-04
780|Austral Downs Limestone|44543|14|Not recorded|p35,36|||||||||
780|Austral Downs Limestone|45032|14|Not recorded|p8||Tertiary|Tb.1. Pl.1. Barkly Tableland.||||||
780|Austral Downs Limestone|45052|4|Described|p136|||Cainozoic||||||
780|Austral Downs Limestone|45145|6|Mentioned|Table 7|||||||||
780|Austral Downs Limestone|46902|6|Mentioned|Table 1|||Correlation chart for Cainozoic land-surfaces||||||
780|Austral Downs Limestone|46958|6|Mentioned|Fig.2|||||||||
780|Austral Downs Limestone|48844|14|Not recorded|p.57|||||||||
780|Austral Downs Limestone|49027|4|Described|p22|||||||||
780|Austral Downs Limestone|50100|6|Mentioned|p23|Cenozoic|Cenozoic|||||||
780|Austral Downs Limestone|60122|5|Briefly described|p35|Cenozoic|Cenozoic|Pale grey limestone, silicified to red-brown and white chert and chalcedony toward the top.  Unconformably overlies Kelly Creek and Ninmaroo Formations. Max. thickness: 8m. Geological Province: Georgina Basin.  See also p4-5, p10 Tb. 1.||||||19-NOV-08
780|Austral Downs Limestone|60123|4|Described|p5|Quaternary|Tertiary|Limestone, silicified to chert and chalcedony. Unconformably overlies Ninmaroo Formation. Thickness: 8m.||||||05-AUG-08
780|Austral Downs Limestone|60590|5|Briefly described|Map legend|Cenozoic|Cenozoic|Limestone; cherty and chalcedonic.||||||23-DEC-09
780|Austral Downs Limestone|60675|5|Briefly described|Map legend|Tertiary|Tertiary|Limestone: cherty and chalcedonic.||||||11-JAN-05
780|Austral Downs Limestone|60703|6|Mentioned|p714, p725 Fig. 18|Tertiary|Tertiary|||||||12-APR-05
780|Austral Downs Limestone|61155|5|Briefly described|p16|Middle Miocene|Middle Miocene|Together with Noranside Limestone thickness is 35m. Geological Province: Georgina Basin.||||||03-MAR-10
780|Austral Downs Limestone|61404|5|Briefly described|Map legend|Neogene|Paleogene|Limestone: cherty and chalcedonic. Geological Province: southern Georgina Basin.||||||07-NOV-08
780|Austral Downs Limestone|62082|5|Briefly described|p19|Miocene|Miocene|Lacustrine deposits with a chert capping and associated duricrust. Overlies Aroota Lateritic Profile. Geological Province: Georgina and Arunta terrains.||||||07-FEB-11
780|Austral Downs Limestone|62658|5|Briefly described|Map Legend|Cenozoic|Cenozoic|Limestone: cherty and chalcedonic.||||||
780|Austral Downs Limestone|63450|5|Briefly described|p78 Fig. 5, p83|Cenozoic|Cenozoic|Geological province: Georgina Basin, East Toko Syncline.||||||07-FEB-11
780|Austral Downs Limestone|64047|5|Briefly described|p60, p61|Tertiary|Tertiary|Overlies Marion Formation. Geological province: Eromanga Basin.||||||16-APR-08
780|Austral Downs Limestone|64068|4|Described|pp79-81, p19, p42,  p ix|Miocene|Miocene|Austral Downs Basin. Overlies Georgina Basin rocks. Coeval with Brunette Limestone. Radiometrics indicate a signal sourced almost purely from U. Lower part correlated with Poodyea Formation.|||||Limestone, calcrete, chalcedony, chert, limestone breccia; minor sandstone, siltstone.|05-APR-12
780|Austral Downs Limestone|64443|5|Briefly described|p5 Fig.3, p6 Tb.1, p18-23, p31, p41 |Neogene|Miocene|Max 14m thick. Covers contact between Camooweal Dolostone and Arrinthrunga Formation. Lithologically identical with Brunette Limestone; distinguished geographically: this unit is within Georgina River drainage.||||Unconformably overlies Camooweal Dolostone.|Limestone, silicified to chert and chalcedony; characteristic features include rhizoliths and circum- and intragranular cracks.|14-MAY-14
780|Austral Downs Limestone|65337|6|Mentioned|p69.|Cenozoic|Cenozoic|In AVON DOWNS area. May correlate with Cleanskin beds, Brunette Limestone and Golliger beds.||||||
780|Austral Downs Limestone|65344|5|Briefly described|p13, p43-44|Cenozoic|Cenozoic|Of the Georgina Basin. See thin section descriptions for detail.||||||03-MAY-12
780|Austral Downs Limestone|66131|6|Mentioned|p242 Fig.2, p245|Miocene|Miocene|Late Miocene. Closely resembles Cadelga Limestone.||||||
780|Austral Downs Limestone|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Neogene|Paleogene|Age:Tertiary.|||||Brackish lacustrine and spring limestone and chalcedony overlying limestone and ferruginous detritus.|
780|Austral Downs Limestone|67870|6|Mentioned|p43|Cenozoic|Cenozoic|Georgina Basin.||||||
780|Austral Downs Limestone|68553|6|Mentioned|Map legend|Neogene|Paleogene|This unit, as well as Elliott, Mueller and Poodyea Formations; Horse Creek and Noranside Limestones; Mount Coley Sinter, Pomona beds and unnamed sedimentary units, are all mapped under the symbol, Tm.||||||
780|Austral Downs Limestone|69458|5|Briefly described|p42:20|Miocene|Miocene|Georgina River catchment and adjacent areas in Qld. Up to 35m thick. Forms prominent extensive plateaux with 7m high cliffs. Palaeopedogenic features are common.||||Overlies Ninmaroo Formation. Is correlated with the Brunette Limestone.|Pale grey, terrestrial lacustrine limestone, silicified to resistant, red-brown and white chert and chalcedony.|14-SEP-18
780|Austral Downs Limestone|69599|5|Briefly described|p584, p599-601|Miocene|Miocene|Noakes and Traves (1954). Austral Downs Basin. Up to 35m thick. Forms low plateaus. Fossils listed, none of which is age-diagnostic. Has Pliocene silcrete.||||?Overlies unconformably the Marion Formation. Correlated with Doonbara, Whitula and Poodyea Formations; Noranside and Horse Creek Limestones; and Mount Coley Sinter.|Basal 3m of spring-fed lacustrine limestone, pasing up into typical lacustrine limestones.|
780|Austral Downs Limestone|72516|6|Mentioned|p98|Neogene|Neogene|Southern Georgina Basin. Interpreted to be an age equivalent of the Waite Formation of the Waite Basin.||||||09-JUN-21
780|Austral Downs Limestone|73083|6|Mentioned|p10|Cenozoic|Cenozoic|||||||
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|||||||
1130|Barney Creek Formation|7071|5|Briefly described|p1|||Host to the giant HYC deposit. Geological Province: McArthur Basin.||||||
1130|Barney Creek Formation|14019|5|Briefly described|p4|Statherian|Statherian|Of the McArthur Group.  Age: 1639Ma (U-Pb zircon, Southgate et al, 2000).  Geological Province: Barney Creek Basin.||||||28-NOV-06
1130|Barney Creek Formation|22538|5|Briefly described|P710, P717||Statherian|Age of unit is 1640+/-4 Ma.||||||28-NOV-06
1130|Barney Creek Formation|22662|2|Defined|21-23 fig 2,24,25,28|Proterozoic|Proterozoic|Geol. province: McArthur Basin. Also on pages 29,30||||||20-JUL-06
1130|Barney Creek Formation|22664|5|Briefly described|33-37,39 fig 4, 42|Paleoproterozoic|Paleoproterozoic|Umbolooga Subgroup (McArthur Group). Geological Province: McArthur Basin. Also on pages 45 and 47.||||||07-NOV-08
1130|Barney Creek Formation|22665|5|Briefly described|Table1, P229||Statherian|||||||
1130|Barney Creek Formation|22853|3|Fully described|21|Proterozoic|Proterozoic|Of the Umbolooga Subgroup. Max thickness 700 m. Underlain by Coxco Dolomite Member.||||||28-NOV-06
1130|Barney Creek Formation|22955|6|Mentioned|160||Paleoproterozoic|||||||07-NOV-08
1130|Barney Creek Formation|23195|6|Mentioned|p4|||Hosts the HYC deposit within dolomitic black shales.||||||
1130|Barney Creek Formation|23196|6|Mentioned|p829|||Referred to as HYC-Barney Creek Formation - ie. stating Barney Ck Fm is at HYC. In the McArthur Basin.||||||28-NOV-06
1130|Barney Creek Formation|23197|6|Mentioned|Fig.1, p850|||||||||
1130|Barney Creek Formation|23356|5|Briefly described|26 Tab.2|Statherian|Statherian|Age: 1700-1500Ma.||||||28-NOV-06
1130|Barney Creek Formation|23387|6|Mentioned|p18 fig.19|||Of Umbolooga Subgroup.||||||
1130|Barney Creek Formation|23396|5|Briefly described|p407 Fig.2|Statherian|Statherian|Of the McArthur Group.||||||28-NOV-06
1130|Barney Creek Formation|23397|5|Briefly described|p473|Statherian|Statherian|Age: 1640+/-3Ma.||||||28-NOV-06
1130|Barney Creek Formation|23398|5|Briefly described|p442|Statherian|Statherian|Age: 1639+/-3Ma.||||||28-NOV-06
1130|Barney Creek Formation|23408|6|Mentioned|p520|||Contains laminated dolomitic siltstones at the McArthur River deposit.||||||15-JUN-09
1130|Barney Creek Formation|23409|5|Briefly described|p556|||||||||
1130|Barney Creek Formation|23534|5|Briefly described|p2318|||Geological Province: McArthur Basin.||||||
1130|Barney Creek Formation|23776|5|Briefly described|p705 Fig 2|||Of Umbolooga Subgroup.||||||
1130|Barney Creek Formation|23809|5|Briefly described|p47 Fig. 42|Paleoproterozoic|Paleoproterozoic|Age: 1639+/-3Ma. Geological Province: McArthur Basin.  Correlates with Shillinglaw Formation (Ashburton Province), Campbell Springs Dolostone (Birrindudu basin) and Mount Parker Sandstone (Osmond Basin, W.A.).||||||07-NOV-08
1130|Barney Creek Formation|23902|4|Described|p1568 Fig.2|||Of the Umbolooga Subgroup. Overlies the Teena Dolomite. Overlain by the Reward Dolomite.||||||
1130|Barney Creek Formation|23910|5|Briefly described|p291|Paleoproterozoic|Paleoproterozoic|Of Umbolooga Subgroup.  Geological Province: McArthur Basin.||||||07-NOV-08
1130|Barney Creek Formation|23937|5|Briefly described|p25 Tb. 2|||Of the McArthur Group.  Geological Province: McArthur Basin.  See also p92 Appendix 1.||||||13-APR-05
1130|Barney Creek Formation|23961|6|Mentioned|p1191|||Geological Province: Mt Isa Inlier.||||||
1130|Barney Creek Formation|23963|5|Briefly described|p1239 Fig.2|||Geological Province: McArthur Basin. Of the Umbolooga Subgroup||||||
1130|Barney Creek Formation|23968|5|Briefly described|p1345, 1347|||Geological Province: McArthur Basin.  Maximum Thickness: >700m.||||||
1130|Barney Creek Formation|24048|5|Briefly described|p37|||Geological Province: McArthur Basin.||||||
1130|Barney Creek Formation|24179|5|Briefly described|p83, 84 Fig. 2|Paleoproterozoic|Paleoproterozoic|Age: 1640 +/- 3 Ma, 1639 +/- 3 Ma and 1638 +/- 7 Ma (U-Pb).  Overlain by the Reward Formation.  Overlies the Teena Formation.  Geological Province:  McArthur Basin.||||||07-NOV-08
1130|Barney Creek Formation|24308|5|Briefly described|p1006|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
1130|Barney Creek Formation|24432|4|Described|p560 Tb.1|Statherian|Statherian|Age: 1640+/-3 Ma. Of Umbolooga Subgroup. Dolomitic siltstone, coarse sedimentary breccias, tuffaceous horizons and organic rich pyritic shale. Finely laminated, deep water deposition.||||||
1130|Barney Creek Formation|30272|6|Mentioned|p5|||Stratigraphic table p5.||||||28-NOV-06
1130|Barney Creek Formation|30318|6|Mentioned|p327|||||||||
1130|Barney Creek Formation|30344|6|Mentioned|Fig.4|||Part of Umbolooga Subgroup||||||
1130|Barney Creek Formation|30345|6|Mentioned|Table 1|||Carpentarian age. Lithology||||||
1130|Barney Creek Formation|30354|5|Briefly described|p20|||||||||
1130|Barney Creek Formation|30363|6|Mentioned|p22|||||||||
1130|Barney Creek Formation|32144|6|Mentioned|p81|||Solvent extractable organic matter||||||
1130|Barney Creek Formation|32363|6|Mentioned|p330|||||||||
1130|Barney Creek Formation|32479|6|Mentioned|p1393|||||||||
1130|Barney Creek Formation|32658|3|Fully described|Table 2|||See also Fig. 3 and 4.||||||28-NOV-06
1130|Barney Creek Formation|32660|5|Briefly described|Table 4|||||||||
1130|Barney Creek Formation|32908|6|Mentioned|p20|||Mineralisation.||||||28-NOV-06
1130|Barney Creek Formation|33550|6|Mentioned|p272|||||||||
1130|Barney Creek Formation|33665|6|Mentioned|p368|||||||||
1130|Barney Creek Formation|33666|6|Mentioned|Table 1|||||||||
1130|Barney Creek Formation|35162|6|Mentioned|Table.1|||||||||
1130|Barney Creek Formation|35261|6|Mentioned|p316|||||||||
1130|Barney Creek Formation|36796|6|Mentioned|p2|||||||||
1130|Barney Creek Formation|37217|6|Mentioned|p649|||||||||
1130|Barney Creek Formation|37371|6|Mentioned|p368|||||||||
1130|Barney Creek Formation|37462|4|Described|Table4.IV|||Also briefly described p249.||||||28-NOV-06
1130|Barney Creek Formation|37568|6|Mentioned|p79|||||||||
1130|Barney Creek Formation|37569|6|Mentioned|p93|||||||||
1130|Barney Creek Formation|38042|6|Mentioned|p158|||||||||
1130|Barney Creek Formation|38582|6|Mentioned|p218|||||||||
1130|Barney Creek Formation|39122|6|Mentioned|p154|||||||||
1130|Barney Creek Formation|39561|6|Mentioned|Fig.5|||||||||
1130|Barney Creek Formation|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
1130|Barney Creek Formation|40088|6|Mentioned|p224|||||||||
1130|Barney Creek Formation|40105|6|Mentioned|p314|||||||||
1130|Barney Creek Formation|40109|6|Mentioned|p302|||||||||
1130|Barney Creek Formation|40259|6|Mentioned|Table 1|||||||||
1130|Barney Creek Formation|40691|5|Briefly described|p12|||||||||
1130|Barney Creek Formation|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
1130|Barney Creek Formation|41220|6|Mentioned|p366|||||||||
1130|Barney Creek Formation|41268|3|Fully described|p293|||||||||
1130|Barney Creek Formation|41277|6|Mentioned|Fig.2|||||||||
1130|Barney Creek Formation|41957|6|Mentioned|p68|||||||||
1130|Barney Creek Formation|42202|6|Mentioned|p519|||||||||
1130|Barney Creek Formation|42385|4|Described|p20|||See also Table 4 p16.||||||28-NOV-06
1130|Barney Creek Formation|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
1130|Barney Creek Formation|42570|5|Briefly described|p546|||||||||
1130|Barney Creek Formation|42638|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Age: Middle Proterozoic.|1690 +29/-25 Ma in tuff (Page, 1981)|Of Umbolooga Subgroup (McArthur Group).||In schematic section, underlies Reward Dolomite; overlies Coxco Dolomite Member (Teena Dolomite).|Dolomitic, carbonaceous and pyritic shale and siltstone. Dololutite, rare sandstone. Detailed lithology given.|07-NOV-11
1130|Barney Creek Formation|42639|3|Fully described|p28, Table 5 p20|||||||||
1130|Barney Creek Formation|42700|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
1130|Barney Creek Formation|42739|5|Briefly described|map legend|Statherian|Statherian|Of the Umbolooga Subgroup. Siltstone and mudstone, thin-bedded to laminated, variously dolomitic, carbonaceous and pyritic; dololutite, tuffaceous mudstone, rare breccia and sandstone.||||||19-OCT-05
1130|Barney Creek Formation|42753|6|Mentioned|p2|||||||||
1130|Barney Creek Formation|42812|3|Fully described|p38, Table 4|||Of Umbolooga Subgroup (McArthur Group).||||||20-JUL-06
1130|Barney Creek Formation|42846|5|Briefly described|Fig.1 p502|||Of McArthur Group. Geological Province: Glyde River Sub-basin, McArthur Basin.||||||09-MAY-05
1130|Barney Creek Formation|42935|5|Briefly described|p528|||||||||
1130|Barney Creek Formation|43010|5|Briefly described|p128|||||||||
1130|Barney Creek Formation|43036|4|Described|p50|||Of Umbolooga Subgroup.||||||20-JUL-06
1130|Barney Creek Formation|43610|6|Mentioned|p20|||||||||
1130|Barney Creek Formation|45162|2|Defined|p98|Proterozoic|Proterozoic|||||||
1130|Barney Creek Formation|46915|6|Mentioned|Fig.1|||Stratigraphic section through McArthur Group.||||||
1130|Barney Creek Formation|46968|6|Mentioned|Fig.2|||||||||
1130|Barney Creek Formation|60483|5|Briefly described|p7 Fig. 5, p8, p30|Paleoproterozoic|Paleoproterozoic|Of Umbolooga Subgroup (McArthur Group). Contains W-Fold and HYC Shale Members, and Cooley Dolomite Member. Age: 1640+/-3Ma, 1639+/-3Ma. Geological Province: McArthur Basin.||||||07-NOV-08
1130|Barney Creek Formation|60553|5|Briefly described|p625|||Overlies the McArthur Group. Geological Province: McArthur Basin.||||||
1130|Barney Creek Formation|60558|5|Briefly described|p8 Fig. 6, p10, p13|Proterozoic|Proterozoic|Of Umbolooga Subgroup. Includes Cooley Dolomite Member, HYC Pyritic Shale Member and W Fold Shale Member. Overlian by Reward Dolomite, underlian by Teena Dolomite.||||||
1130|Barney Creek Formation|62084|4|Described|p936 Fig.5, p939, p941-p942, p957 Fig.16|||Isa Superbasin. McArthur Basin. Hosts McArthur River (formerly HYC) deposit (Zn-Pb-Ag stratiform) at base of HYC Pyritic Shale Member. Shown as Barney Ck Fm or Barney Creek Fm in figures.|1640+/-3 Ma U-Pb SHRIMP Carr et al. 1996|McArthur Group|HYC Pyritic Shale Member||Variably dolomitic organic siltstones and shales; regional marine carbonates.|
1130|Barney Creek Formation|62285|5|Briefly described|p381, p382|||See also upper Barney Creek Formation.||||||
1130|Barney Creek Formation|63062|5|Briefly described|p38|||Of the McArthur Group. Geological Province: McArthur Basin. Lacustrine deposits with source rock potential for petroleum.||||||07-FEB-11
1130|Barney Creek Formation|63112|6|Mentioned|p1191 Fig.2|||Isa Superbasin; southern McArthur Basin. Age approximated from Fig.2.|c.1635 Ma.|Unit in River Supersequence.||||
1130|Barney Creek Formation|63866|5|Briefly described|p54|Statherian|Statherian|Isa Superbasin.|c. 1640-1638 Ma (Page et al., 2000)|||||
1130|Barney Creek Formation|64813|6|Mentioned|p269|Palaeoproterozoic|Paleoproterozoic|Geological province: McArthur Basin, N.T. ||||||
1130|Barney Creek Formation|64815|5|Briefly described|p4 Fig.2, p5 Fig.3, p6, p8 Tb.1|||See also p14 Tb.5, p17-19. HYC mineralisation occurs towards the top of this unit.||Of the Umbolooga Subgroup.|Includes Cooley Dolostone Member, W-Fold Shale Member and HYC Pyritic Shale Member.|||
1130|Barney Creek Formation|64816|5|Briefly described|p1, p2 Fig.1, p18-21|Statherian|Statherian|Possible source of a component of the oil in this study. Deposited in lacustrine or lagoon setting.|1640 +/- 3 Ma.|Unit in McArthur Group.||||
1130|Barney Creek Formation|64817|6|Mentioned|p353 Fig.4, p356 |Statherian|Statherian|Thickens into the Emu Fault and thins gradually to the west.|1640 +/- 3 Ma and 1639 +/- 3 Ma.|Of the Umbolooga Subgroup.|Includes Cooley Dolomite Member, W-Fold Shale Member, HYC Pyritic Shale Member.|||
1130|Barney Creek Formation|65228|4|Described|p7, p18, p32, p35, Table 1,Figs.02,04,22|Statherian|Statherian|McArthur Basin. Part of River Supersequence. Shows rapid lateral facies changes related to syn-sedimentary tectonism. 1640 Ma. Hosts McArthur River Ag-Pb-Zn mine. Measured section.|1640 +/- 3 to 1638 +/- 7 Ma.|Unit in Umbolooga Subgroup.|Includes W-Fold Shale, HYC Pyritic Shale, Cooley Dolomite Members.|||
1130|Barney Creek Formation|65337|6|Mentioned|p74.|||At the McArthur River deposit; stratiform base metal sulfide mineralisation from exhalation of metalliferous saline basinal fluids into a localised deep-water brine pool along a regional strike-slip fault system.||||||
1130|Barney Creek Formation|66843|5|Briefly described|p37 Tb.1, p38 Fig.10|||SHRIMP U-Pb zircon ages: Page and Sweet (1998).|1640+/-3 - 1638+/-7 Ma.|McArthur Group.||||
1130|Barney Creek Formation|67144|5|Briefly described|Map legend.|Statherian|Statherian|Recessive.||Unit in Umbolooga Subgroup.||Overlies Teena Dolostone. Is overlain by Reward Dolostone.|Thinly-bedded to laminated, dolomitic, carbonaceous and pyritic shale and siltstone; dololutite, rare breccia and sandstone; gypsum casts.|
1130|Barney Creek Formation|67352|4|Described|p13 Tb.2|Statherian|Statherian|McArthur Basin. Over 900 m thick.||Umbolooga Subgroup||Conformably overlies Coxco Dolostone Member or Teena Dolostone. Overlain by Reward Dolostone, conformably or disconformably.|Thinly bedded to laminated dolomitic, carbonaceous and pyritic shale and siltstone; dolomudstone, tuff; rare breccia and sandstone.|
1130|Barney Creek Formation|68733|6|Mentioned|p186-187|||||McArthur Group.||||04-DEC-17
1130|Barney Creek Formation|69018|5|Briefly described|p450 Fig.1b|Statherian|Statherian|Of McArthur Basin.|1639+/-3 Ma, 1638+/-7 Ma.|Of McArthur Group.||||
1130|Barney Creek Formation|69418|5|Briefly described|p3:11, 13, 36|||McArthur Basin. Hosts sediment-hosted stratiform Zn-Pb-Ag deposits (described). Good potential hydrocarbon source rocks.|||||Black shale, siltstone, sandstone, chert, dolostone, micritic limestone and turbiditic rocks.|12-JUL-16
1130|Barney Creek Formation|69430|4|Described|p15:3, 14, 16, 18-19, 22-23, 32, 34-35|Statherian|Statherian|See also 15:37-39, 61-63. Southern McArthur Basin. 10m to over 900m thick. Largely recessive unit. Basinal shale deposited in actively subsiding sub-basins. Economically important: hosts various base metal occurrences, notably the world-class HYC (later McArthur River) deposit. Potential hydrocarbon source rock (up to 8% TOC) for small structural and diagenetic traps in the Batten Fault Zone. Has palaeo-hydrocarbon reservoirs: intervals contain extensive bitumen and other hydrocarbons.|1640 +/- 3 Ma (Pietsch et al., 1994).|Umbolooga Subgroup.|W-Fold Shale, HYC Pyritic Shale, Cooley Dolostone, Members.|Conformably and gradationally overlies Coxco Dolostone Member (Teena Dolostone). Is overlain conformably by Reward Dolostone. Time-equivalent of Saint Vidgeon Formation.|Thinly bedded to laminated, dolomitic, carbonaceous and pyritic shale and siltstone, dololutite, rare breccia and sandstone; occasional gypsum casts; talus slope breccia adjacent to Emu Fault. Locally abundant tuffs and breccias.|12-JUL-16
1130|Barney Creek Formation|69431|6|Mentioned|p16:25|||An equivalent unit was recognised in a succcession in the northern Tomkinson Province, hosting low-grade base metal mineralisation.||||||12-JUL-16
1130|Barney Creek Formation|69451|6|Mentioned|p35:13|||Potential petroleum source rock: TOC up to 8%.||McArthur Group.||||12-JUL-16
1130|Barney Creek Formation|69545|5|Briefly described|p99|Paleoproterozoic|Paleoproterozoic|McArthur Basin. Host to the supergiant HYC Pb-Zn-Ag deposit. Black shales locally contain over 7% TOC.|1640 Ma|||Overlies Wollogorang Formation.|Unmetamorphosed carbonaceous, pyritic and tuffaceous shales and siltstones.|13-FEB-18
1130|Barney Creek Formation|69673|4|Described|p18, p24,p27, p33, p40, p43, p45, p47|||McArthur Basin, Batten Fault Zone. Significant unconventional shale gas and oil prospect. Late mature to overmature for oil generation in places. Potential as both conventional and unconventional reservoir and seal.|1640 +/- 3 Ma, 1639 +/- 3 Ma|Umbolooga Subgroup|Includes HYC Pyritic Shale Member, W-Fold Shale Member, Cooley Dolostone Member|Conformably overlies Coxco Dolostone Member, conformably overlain by Reward Dolostone, Correlated with Saint Vidgeon Formation|Finely laminated to thinly bedded dolomitic, carbonaceous and pyritic siltstone, shale and dolomudstone and locally abundant tuff beds and breccias.|
1130|Barney Creek Formation|71059|5|Briefly described|p7, p10|||Batten Trough, McArthur Basin. Estimated shale/tight gas/shale oil and condensate resources detailed.||McArthur Group.||||
1130|Barney Creek Formation|71592|5|Briefly described|Appendix A.|||McArthur Basin.|1638+/-7 Ma (crystallisation: U-Pb zircon SHRIMP)||HYC Pyritic Shale Member.||Ash tuff, non-tuffaceous shale. Upper stylolitic marker.|
1130|Barney Creek Formation|71606|5|Briefly described|p138|Statherian|Statherian|Batten Trough, McArthur Basin. Depositional age of 1640+\-7 Ma|1640+\-7 Ma|Unit of Umbolooga Subgroup.||||
1130|Barney Creek Formation|72248|4|Described|p145-149,153,155|||Of McArthur Basin. Hosts the giant HYC Zn-Pn-Ag deposit at McArthur River. Recessive stratigraphic unit deposited during a period of pronounced tectonically controlled basin subsidence (Brown et al., 1978; Neudert and McGeough, 1996; Bull, 1998).||Unit of Umbolooga Subgroup.|Includes HYC Pyritic Shale, W-Fold Shale Member and Cooley Dolomite Member.|Underlain by Teena Dolomite.|Finely laminated to thin-bedded, planar-laminated dolomitic, carbonaceous and locally pyritic siltstone.|
1130|Barney Creek Formation|72373|5|Briefly described|p17|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. Dated at 1639+\-3 Ma; partially overlaps in age with Baiguridji Formation (Ahmad et al 2013).||Unit of upper McArthur Group.||||01-OCT-19
1130|Barney Creek Formation|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Batten Fault Zone of the Southern McArthur Basin. Three U-Pb zircon sedimentary depositional ages given including 1639+/-3 Ma, 1640+/-3 Ma.|1638+/-7 Ma.|Batten Subgroup||Overlies Coxco Dolostone and underlies Reward Dolostone.||
1130|Barney Creek Formation|72718|6|Mentioned|p7|Statherian|Statherian|Southern McArthur Basin. Batten Fault Zone.|1640 +/- 3 Ma, 1639 +/- 3 Ma|Umbolooga Sub-group, McArthur Group|Cooley Dolostone Member, W-Fold Shale Member, HYC Pyritic Shale Member|Underlain by Coxco Dolostone Member. Overlain by Reward Dolostone.||
1130|Barney Creek Formation|72912|5|Briefly described|p5 Fig.3, p36, p37 Fig.14.|Statherian|Statherian|Located in the Batten Fault Zone of the Southern McArthur Basin. Three U-Pb zircon sedimentary depositional ages given including 1639+/-3 Ma, 1640+/-3 Ma.Described as one of the best source rocks in the McArthur Basin.|1638+/-7 Ma.|Batten Subgroup||Overlies Coxco Dolostone Member and underlies Reward Dolostone.||15-MAR-21
1130|Barney Creek Formation|73042|6|Mentioned|p4|Statherian|Statherian|Southern McArthur Basin, Isa Superbasin. Geochronology is a U-Pb zircon sedimentary depositional age (?maximum depositional age).|1638+/-7 Ma, 1639+/-3 Ma, 1640+/-3 Ma|Batten Subgroup, McArthur Group||Underlain by Coxco Dolostone Member. Overlain by Reward Dolostone.||
1130|Barney Creek Formation|73098|6|Mentioned|p4, p7, p15|||McArthur Basin. Organic petrolography performed on one sample from the Bing Bong 6 well. This sample was low in bitumen. [See report for bitumen/maceral description].|||||Includes black shale.|
1130|Barney Creek Formation|73280|6|Mentioned|p1, p4-5, App.1A, App.1B, App.1C|||McArthur Basin. Sampled for XRD mineralogy to investigate brittleness and Kubler indices [see report]. Informal reference to upper dolomitic shales. [Also alludes to original well logs reporting these rocks as Surprise Creek - Pyritic Shale].|||HYC Pyritic Shale Member|||
1130|Barney Creek Formation|73405|5|Briefly described|p228, 237-238, 239 Fig.7, p240-241|Paleoproterozoic|Paleoproterozoic|McArthur Basin. Current interpretations as a restricted, deep marine paleoenvironment are challenged by biomarker resemblances to saline lacustrine systems (esp. Green River Formation, USA). Effects of putative marine incursions, or of microbial mats, are discussed.|1.64 Ga.|McArthur Group.|||Includes ubiquitous feldspar-rich dolomitic marlstones.|
1130|Barney Creek Formation|73412|4|Described|p1-2, 4, 8-9, 13, 16-17, 19-21|||Southern McArthur Basin. The most important Zn-Pb-Ag host unit in the Basin. Thick deposits accumulated in restricted sub-basins between Hot Spring Fault and Emu Fault Zone.|1640 +/- 3 Ma (Page and Sweet, 1998).|Umbolooga Subgroup.||Overlies Emmerugga and Teena Dolostones. Is overlain by Reward Dolostone.|Contains organic-rich and pyritic mudrocks (trap for Zn-Pb-Ag mineralised fluid transport).|
1243|Bath Range Formation|22538|6|Mentioned|Fig3 P708||Calymmian|Age of unit is 1599+/-11 Ma||||||
1243|Bath Range Formation|22600|4|Described|Map legend||Statherian|||||||
1243|Bath Range Formation|23937|5|Briefly described|p13|Calymmian|Statherian|Overlain by the Nathan Group.  Age: 1600Ma.||||||20-OCT-04
1243|Bath Range Formation|24048|3|Fully described|p62|Mesoproterozoic|Paleoproterozoic|Of Balma Group.  Overlain by Balbirini Dolomite; underlain by Baiguridji Formation.  Max. thickness: 600m.  Geological Province: McArthur Basin.||||||07-NOV-08
1243|Bath Range Formation|24049|5|Briefly described|Map Legend|Statherian|Statherian|Of Balma Group. Sandstone: fine to coarse-grained, lithic (chert clasts), commonly dolomitic; chert (silicified carbonate): relict peloidal and stromatolitic textures; tuffaceous mudstone: thin to thick-bedded. Geol. Prov: McArthur Basin.||||||11-OCT-05
1243|Bath Range Formation|24050|5|Briefly described|p11 Tb. 3|Calymmian|Calymmian|Tuffaceous claystone.  Age: 1599+/-11m.y. (SHRIMP U-Pb zircon).||||||
1243|Bath Range Formation|24432|5|Briefly described|p562 Fig.2|Calymmian|Calymmian|Of Habgood Group.  Age: 1599+/-11Ma. Geological Province: Northern McArthur Basin.||||||16-NOV-06
1243|Bath Range Formation|32660|5|Briefly described|Table 4|||||||||
1243|Bath Range Formation|41406|6|Mentioned|Map legend|Mesoproterozoic||||||||
1243|Bath Range Formation|42597|5|Briefly described|Map Legend|Carpentarian||||||||
1243|Bath Range Formation|43010|2|Defined|p122||Paleoproterozoic|Of McArthur Group. Of Statherian age.||||||07-NOV-08
1243|Bath Range Formation|44112|3|Fully described|p53-54,57||Statherian|Max Age: ~1600 Ma||||||
1243|Bath Range Formation|44299|4|Described|p.12||Paleoproterozoic|SD/53-7,8. L.Proterozoic. Table 1.||||||07-NOV-08
1243|Bath Range Formation|44300|14|Not recorded|map legend|||SD/53-7,8. Lower (?) Proterozoic.||||||
1243|Bath Range Formation|45162|6|Mentioned|p45|||||||||
1243|Bath Range Formation|61403|5|Briefly described|Map Legend|Statherian|Statherian|Of Balma Group. Sandstone: fine to coarse-grained, lithic (chert clasts), commonly dolomitic; chert (silicified carbonate): relict peloidal and stroma tolitic textures; tuffaceous mudstone: thin to thick-bedded. Geol. Prov: McArthur Basin.||||||
1243|Bath Range Formation|63866|5|Briefly described|p114|Calymmian|Statherian|Isa Superbasin.|1599 +/- 11 Ma (Pietsch et al., 1994)|Balma Group||Unconformably overlain by the Nathan Group.||
1243|Bath Range Formation|64817|6|Mentioned|p353 Fig.4 |Calymmian|Statherian||1599 +/- 11 Ma.|Of the Balma Group.||||
1243|Bath Range Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||McArthur region.|1599 +/- 11 Ma.|||||
1243|Bath Range Formation|69430|4|Described|p15:3, 21-22|Statherian|Statherian|Walker Fault Zone, northern McArthur Basin. c.600m thick. Most widely outcropping unit of the Group. Shallow-water (?marine), varying from subtidal storm-dominated to very shallow-water high-energy, deposits. SHRIMP U-Pb zircon age. This date overlaps the age of the upper Balbirini Dolostone (1589 +/- 3 Ma).|1599 +/- 11 Ma (Pietsch et al., 1994).|Balma Group.||Conformably overlies Baiguridji Formation. Is overlain by Nathan Group (contact not exposed).|Fine- to coarse-grained, chert clast-lithic, commonly dolomitic sandstone; chert (silicified carbonate) with relict peloidal and stromatolitic textures; white, rarely greenish or pink, thinly to thickly bedded tuffaceous mudstone.|12-JUL-16
1243|Bath Range Formation|69673|6|Mentioned|p16 fig 13|Mesoproterozoic|Paleoproterozoic|Walker Fault Zone|1599 +/- 11 Ma|Balma Group||Overlies Baiguridgi Formation, unconformably? Overlain by Balbirini Dolostone||
1243|Bath Range Formation|71592|5|Briefly described|Appendix A.|||McArthur Basin.|1599+/-11 Ma (crystallisation: U-Pb zircon SHRIMP)||||Ash tuff.|
1243|Bath Range Formation|71606|5|Briefly described|p138|Calymmian|Calymmian|Central Walker Trough, McArthur Basin. Upper unit in the Walker Trough. Tuffaceous mudstone in the base of the unit has maximum zircon age of 1599+\-11 Ma.|Max zircon age 1599+\-11 Ma.|||||
1243|Bath Range Formation|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.||Upper Balma Group.||||
1243|Bath Range Formation|72373|4|Described|iii,p1,17,20-24|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. Reference section: 7km NE of junction of Vaughton Creek and Rose River in southcentral PARSONS. Outcrop large restricted to BLUE MUD BAY map sheet. Relatively thick tuffaceous beds (1599+\-11 Ma, SHRIMP U-Pb; Pietsch et al 1994) near the base of the formation might indicate contemporaneous volcanism. Sample 2709634 (BM16TJM027: Fine-grained silty quartz sandstone) yielded interpreted max depositional age of 1624+\-16 Ma. Similar detrital zircon spectra with Baiguridji Formation, suggesting derivation from similar source areas and potentially in part laterally equivalent.|1624+\-16 Ma (max dep age)|Unit of Balma Group.||Uppermost unit of Balma Group. Overlain by Balbirini Dolostone/Nathan Group. Underlain by Baiguridji Formation. Correlated with Gwakura Formation.|Thinly to thickly bedded, fine- to coarse grained, dolomitic to leached lithic sandstone, chert (silicified carbonate rocks) and probably tuffaceous shale.|01-OCT-19
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.||||||
1257|Batten Subgroup|22538|6|Mentioned|P717|||||||||
1257|Batten Subgroup|22662|6|Mentioned|22,23 fig 2|Proterozoic|Proterozoic|Geol. province: McArthur Basin||||||20-JUL-06
1257|Batten Subgroup|22664|6|Mentioned|34,47|Paleoproterozoic|Paleoproterozoic|Of the McArthur Group. Geological Province:  McArthur Basin||||||07-NOV-08
1257|Batten Subgroup|22853|5|Briefly described|22|Proterozoic|Proterozoic|Of McArthur Group. Max thickness 1000 m. Underlying unit: Umbolooga Subgroup||||||20-JUL-06
1257|Batten Subgroup|23387|6|Mentioned|p18 fig.19|||Of McArthur Group.||||||
1257|Batten Subgroup|23398|5|Briefly described|p443|||Of McArthur Group||||||
1257|Batten Subgroup|23776|5|Briefly described|p705 Fig 2|||Of McArthur Group. Underlying unit: Umbolooga Subgroup. Max thickness: 1000 m.||||||20-JUL-06
1257|Batten Subgroup|23902|4|Described|p1568 Fig.2|||Of the McArthur Group. Overlies the Umbolooga Subgroup. Geological Province: McArthur Basin||||||
1257|Batten Subgroup|23937|6|Mentioned|p9|||Of the McArthur Group.   See also p89 Appendix 1.||||||20-OCT-04
1257|Batten Subgroup|23963|5|Briefly described|p1239 Fig.2|||Geological Province: McArthur Basin. Of the McArthur Group||||||03-MAR-05
1257|Batten Subgroup|24048|6|Mentioned|p57|||||||||
1257|Batten Subgroup|24432|4|Described|p562 Fig.2|Calymmian|Statherian|Of McArthur Group. Age: <1640 Ma. Geological Province: Southern McArthur Basin.||||||20-JUL-06
1257|Batten Subgroup|30344|6|Mentioned|Fig.4|||Part of McArthur Group||||||
1257|Batten Subgroup|32479|6|Mentioned|p1397|||||||||
1257|Batten Subgroup|35261|6|Mentioned|Fig.2|||||||||
1257|Batten Subgroup|37462|4|Described|Table4.IV|||||||||
1257|Batten Subgroup|37568|4|Described|p79|||See also Fig.5||||||
1257|Batten Subgroup|38042|6|Mentioned|Fig.1|||||||||
1257|Batten Subgroup|38582|6|Mentioned|p218|||||||||
1257|Batten Subgroup|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
1257|Batten Subgroup|40691|6|Mentioned|p48|||||||||
1257|Batten Subgroup|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
1257|Batten Subgroup|41277|6|Mentioned|Fig.2|||||||||
1257|Batten Subgroup|41406|6|Mentioned|Map legend|Mesoproterozoic||||||||
1257|Batten Subgroup|42385|5|Briefly described|p22|||See also Table 4 p16||||||20-JUL-06
1257|Batten Subgroup|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
1257|Batten Subgroup|42638|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Age: Middle Proterozoic.||Of McArthur Group.|Includes: Amos Formation; Looking Glass Formation; Stretton Sandstone; Yalco Formation; Donnegan, Hot Spring and Caranbirini Members (Lynott Formation).|Overlies Umbolooga Subgroup.||24-OCT-11
1257|Batten Subgroup|42639|4|Described|p31, Table 5 p20|||||||||
1257|Batten Subgroup|42700|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
1257|Batten Subgroup|42739|5|Briefly described|map legend|Statherian|Statherian|Of the McArthur Group.||||||19-OCT-05
1257|Batten Subgroup|42812|4|Described|p40, Table 4|||Of McArthur Group.||||||20-JUL-06
1257|Batten Subgroup|42935|6|Mentioned|p528|||||||||
1257|Batten Subgroup|43010|5|Briefly described|p128|||||||||
1257|Batten Subgroup|43036|4|Described|p52|||Of McArthur Group.||||||20-JUL-06
1257|Batten Subgroup|43595|5|Briefly described|p438|||||||||
1257|Batten Subgroup|44112|6|Mentioned|p58|||||||||
1257|Batten Subgroup|44287|14|Not recorded|p.11, opp.9|||Includes Looking Glass Formation, Stretton Sandstone, Yalco Formation, Lynott Formation. (E53-3).||||||
1257|Batten Subgroup|44288|14|Not recorded|map legend|||Lower (?) Proterozoic.||||||
1257|Batten Subgroup|44473|14|Not recorded|p.8|||(E53-7). Forereef seds. in McArthur Group - not present in this area.||||||20-JUL-06
1257|Batten Subgroup|44530|14|Not recorded|p.9,10,11, opp.10|||(D53-15).||||||
1257|Batten Subgroup|45162|4|Described|p108|Proterozoic|Proterozoic|||||||
1257|Batten Subgroup|46915|6|Mentioned|Fig.1|||Stratigraphic section through McArthur Group.||||||
1257|Batten Subgroup|46968|6|Mentioned|Fig.2|||||||||
1257|Batten Subgroup|60483|5|Briefly described|p7 Fig. 5, p8|||Of the McArthur Group. Unconformably overlies Batten Subgroup [???Can't overlie itself]. Geological Province: McArthur Basin||||||03-FEB-11
1257|Batten Subgroup|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of McArthur Group. Includes five units.||||||03-JUN-09
1257|Batten Subgroup|60573|5|Briefly described|Regional Setting legend|Paleoproterozoic|Paleoproterozoic|Of the McArthur Group.||||||23-DEC-09
1257|Batten Subgroup|64815|5|Briefly described|p3, p4 Fig.2, p11, p15 Fig.9 |Statherian|Statherian|See also p16-18 Figs.10-12, p17. SHRIMP zircon ages of Stretton Sandstone and Amos Formation respectively.|1625 +/- 2 Ma to 1614 +/- 4 Ma (Page et al, 2000)|Unit in McArthur Group.|Includes Stretton Sandstone; Yalco, Lynott, Looking Glass and Amos Formations.||Dolomitic.|
1257|Batten Subgroup|64817|6|Mentioned|p353 Fig.4 |||||Of the McArthur Group.|Includes Looking Glass, Amos, Yalco, Lynott Formations; Stretton Sandstone.|||
1257|Batten Subgroup|65228|5|Briefly described|p32, Fig.02.|||Lower part constitutes upper part of River Supersequence.||Unit in McArthur Group.|Includes Lynott, Yalco, Looking Glass, Amos Formations; Stretton Sandstone.|Overlies Umbolooga Subgroup.||
1257|Batten Subgroup|67323|5|Briefly described|Eastern Australia Time-Space Plot; p35|Paleoproterozoic|Paleoproterozoic|McArthur Basin.|1640 +/- 10 Ma to ~1600 Ma.|||||
1257|Batten Subgroup|67352|6|Mentioned|p12, p51|||Not preserved in this study area||McArthur Group||Overlies Umbolooga Subgroup.||
1257|Batten Subgroup|69430|4|Described|p15:3, 14, 16, 19, 22, 24, 34|Statherian|Statherian|Plumb and Brown (1973), Jackson et al. (1987). Southern McArthur Basin.||McArthur Group.|Lynott, Yalco, Looking Glass, Amos Formations; Stretton Sandstone; Lower Balbirini Dolostone.|Unconformably overlies Reward Dolostone (Umbolooga Subgroup). Is overlain unconformably by Smythe Sandstone, Nathan Group.|Dolostone, dololutite, quartz sandstone, dolomitic siltstone and shale.|08-JUL-20
1257|Batten Subgroup|69673|6|Mentioned|p16 fig 13|||Batten Fault Zone|||Includes Caranbirini Member, Lynott Formation, Yalco Formation, Stretton Sandstone, Looking Glass Formation, Amos Formation|Unconformably overlies Umbolooga Subgroup||
1257|Batten Subgroup|70897|5|Briefly described|p43|Statherian|Statherian||c.1640 Ma.|||Is overlain by Roper Group.|Includes cherty carbonate units.|
1257|Batten Subgroup|71606|5|Briefly described|p137|Statherian|Statherian|Batten Trough, McArthur Basin.||Unit of McArthur Group.|Includes Lynott Formation.|Upper unit of McArthur Group. Overlain unconformably by Nathan Group. Underlain by Umbolooga Subgroup.||
1257|Batten Subgroup|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.||Upper McArthur Group.|||Chertified evaporitic-stromatolitic dolostone, dolomitic siltstone, sandstone, pyritic-carbonaceous shale; minor pink chert beds (tuff?).|04-MAR-20
1257|Batten Subgroup|72248|5|Briefly described|p147-148|||Of McArthur Basin.||Unit of McArthur Group.|Includes Looking Glass Formation, Amos Formation, Stretton Sandstone, Yalco Formation, Lynott Formation and Caranbirini Member.|Underlain conformably to unconformably by Unbolooga Subgroup.||
1257|Batten Subgroup|72373|5|Briefly described|iii,14,27|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin.||Unit of McArthur Group.|Includes Stretton Sandstone and Yalco Formation.|||
1257|Batten Subgroup|72523|5|Briefly described|piii, p1, p2 Fig.2.|Statherian|Statherian|||McArthur Group|Includes Amos Formation, Looking Glass Formation, Stretton Sandstone|Unconformably underlies the Nathan Group.|Includes tuffaceous rock and sandstone.|
1257|Batten Subgroup|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Batten Fault Zone of the Southern McArthur Basin.||McArthur Group|Looking Glass Formation, Stretton Sandstone, Yalco Formation, Lynott Formation, Reward Dolostone,  Barney Creek Formation, Coxco Dolostone Member, Teena Dolostone and Emmerugga Dolostone.|Shown as overlying Umbolooga Subgroup and unconformably underlies Nathan Group.||
1257|Batten Subgroup|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Batten Fault Zone of the Southern McArthur Basin.||McArthur Group|Looking Glass, Yalco, Barney Creek and Lynott Formation, Stretton Sandstone, Reward, Coxco, Teena and Emmerugga Dolostone.|Overlies Umboloogna Subgroup and shown as unconformably underlying Nathan Group. Shown as possibly equivalent with Vizard Group.|Includes dolostone and sandstone.|
1257|Batten Subgroup|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin, Isa Superbasin.||McArthur Group|Looking Glass, Yalco, Lynott, Barney Creek formations; Stretton Sandstone; Reward, Teena, Emmerugga dolostones; Hot Springs, Coxco Dolostone, Mitchell Yard, Mara Dolostone members.|Underlain by Tooganinie Formation and Myrtle Shale. Unconformably overlain(?) by Smythe Sandstone.||
1257|Batten Subgroup|73412|5|Briefly described|p4, 8, 13, 18-19|||Southern McArthur Basin.||McArthur Group.|Lynott, Yalco, Looking Glass, Amos Formations; Stretton Sandstone; lower Balbirini Dolostone.|Overlies Umbolooga Subgroup. Is overlain unconformably by Nathan Group.||
1264|Battle Creek Formation|14019|5|Briefly described|p4 Fig. 3|||Of the Bullita Group.  Geological Province: Victoria Basin.||||||
1264|Battle Creek Formation|24047|5|Briefly described|p62|Mesoproterozoic|Mesoproterozoic|Geological Province: Victoria-Birrindudu Basin.||||||
1264|Battle Creek Formation|24122|5|Briefly described|p4 Fig.3|||Of Bullita Group.  Geological Province: Victoria Basin.||||||
1264|Battle Creek Formation|24297|3|Fully described|p13|Proterozoic|Proterozoic|Of Bullita Group.  Conformably overlies Weaner Sandstone. Maximum thickness: 179m.  See also p5 Tb. 2.||||||
1264|Battle Creek Formation|24298|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Bullita Group. Dolostone, siltstone, shale, dolomitic sandstone, sandstone.||||||20-JUL-06
1264|Battle Creek Formation|24441|5|Briefly described|p1 Fig. 1, Appendix 2-1:3|Mesoproterozoic|Mesoproterozoic|Of the Bullita Group. Microbial dolostone, mudstone, siltstone and subordinate sandstone. Overlies Mount Gordon Sandstone and Weaner Sandstone; unconformably overlain by Wondoan Hill Formation. Max. thickness: 179m. Geological province: Victoria Basin.||||||25-JAN-06
1264|Battle Creek Formation|24442|5|Briefly described|p50 Fig. 1|||Of the Bullita Group. Geological Province: Victoria Basin.||||||
1264|Battle Creek Formation|28255|3|Fully described|p54, Tb. 11 (opp.p8)|Adelaidean|Adelaidean|Of the Bullita Group. Conformably overlies Weaner Sandstone, except in Jasper Creek area, where it overlies Bynoe Formation.  Unconformably overlain by Wondoan Hill Formation.  Max. thickness: 80m. See also p136-137 Appendix.||||||
1264|Battle Creek Formation|31832|6|Mentioned|Table 6|||||||||
1264|Battle Creek Formation|32175|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Bullita Group. Flaggy red and grey dolomite, green siltstone; minor shale; stromatolitic near base, blocky sandstone at top.||||||02-DEC-04
1264|Battle Creek Formation|32660|5|Briefly described|Table 6|||||||||
1264|Battle Creek Formation|33374|5|Briefly described|p7|||Strat.||||||
1264|Battle Creek Formation|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
1264|Battle Creek Formation|33377|6|Mentioned|p267|||||||||
1264|Battle Creek Formation|45112|5|Briefly described|Table 10|||||||||
1264|Battle Creek Formation|48943|2|Defined|p66|Adelaidean|Adelaidean|Strat. section p136.||||||20-JUL-06
1264|Battle Creek Formation|60685|3|Fully described|p4 Figure 3, p1|Mesoproterozoic|Mesoproterozoic|Of the Bullita Group. Stromatolitic dolostone, mudstone, siltstone and subordinate sandstone and chert. Conformable on Weaner Sandstone; unconformable beneath Tijunna Group units. Geological Province: Victoria Basin.||||||
1264|Battle Creek Formation|65342|6|Mentioned|p11 Fig.13. |||Victoria Basin.||Unit in Bullita Group.||Overlies Mount Gordon and Weaner Sandstones. Is unconformably overlain by Wondoan Hill Formation of the Tijunna Group.||
1264|Battle Creek Formation|68733|5|Briefly described|p177 Fig.2, p179 Tb.1, p182-183,p185-186|||Previously included in the Victoria Basin by Cutovinos et al. (2002). Now included in the Birrindudu Basin due to a recent subdivision by the NGTS (Dunster and Ahmad 2013). Sm-Nd isotope data tabulated.||Of the Bullita Group.||Conformably underlain by the Weaner Sandstone.||04-DEC-17
1264|Battle Creek Formation|69432|4|Described|p17:2, 10, 12, 14|||Birrindudu Basin. Typically c.80m thick; up to 179m. Restricted, locally evaporitic, shallow-marine to slightly deeper-marine deposits, subjected to minor, periodic higher-energy conditions. Visible galena, copper and manganese mineralisation occurs at several localities.||Bullita Group.||Overlies Mount Gordon Sandstone, and Weaner Sandstone conformably.|Interbedded biohermal and biostromal stromatolitic dolostone, mudstone, siltstone and subordinate sandstone and chert. Minor barite occurs in carbonate rocks.|12-JUL-16
1264|Battle Creek Formation|69673|6|Mentioned|p48 fig 35|||||Bullita Group||Overlies Mount Gordon Sandstone, Weaner Sandstone, unconformably overlain by Wondoan Hill Formation||
1264|Battle Creek Formation|70855|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Bullita Group.||Overlies Weaner Sandstone. Is overlain unconformably by Wondoan Hill Formation (Tijunna Group).|Dolostone, siltstone, shale, dolomitic sandstone, sandstone.|
1264|Battle Creek Formation|70968|5|Briefly described|p115|||||Bullita Group.||Is overlain unconformably by Wondoan Hill Formation.|Interbedded mudrock and dolomitic sandstone.|
1264|Battle Creek Formation|71302|5|Briefly described|p6,35||Paleoproterozoic|Of Birindudu Basin.||Unit of Bullita Group.||Underlain conformably by Weaner Sandstone.||
1264|Battle Creek Formation|72718|6|Mentioned|p7|||Birrindudu Basin.||Bullita Group||Underlain by Weaner Sandstone. Overlain[?] by Wondoan Hill Formation (Tijunna Group). Equivalent to Banyan Formation.||
1264|Battle Creek Formation|73083|6|Mentioned|p45|Mesoproterozoic|Mesoproterozoic|Victoria Basin.||||||
1322|Beasley Knob Member|39827|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
1322|Beasley Knob Member|40494|4|Described|p13|||||||||
1322|Beasley Knob Member|60006|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Wolfe Creek Basin. Of Ranford Formation, Duerdin Group. Overlies Bucket Spring Member. Overlain by Ernie Lagoon Member. Quartz sandstone, conglomerate.||||||
1322|Beasley Knob Member|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
1333|Beatrice Island Limestone|42812|6|Mentioned|p57|||||||||
1333|Beatrice Island Limestone|44530|14|Not recorded|p.13, opp.12||Quaternary|Quaternary. (D53-15).||||||
1333|Beatrice Island Limestone|44531|14|Not recorded|map legend||Cenozoic|Undifferentiated.||||||19-NOV-08
1333|Beatrice Island Limestone|69458|5|Briefly described|p42:21|Pleistocene|Neogene|Plumb and Paine (1964); named after the island to which it is restricted. 10m thick.||||Correlated with the Vanderlin Limestone.|Marine, buff-coloured ooid limestone, deposited as ooid shoals during marine highstands. Contains gastropods and pelecypods.|12-JUL-16
1389|Beetle Creek Formation|22954|6|Mentioned|Fig3p9|Ordian-Early Templetonia||||||||
1389|Beetle Creek Formation|23031|6|Mentioned|17|||Geol province Georgina Basin||||||
1389|Beetle Creek Formation|23374|6|Mentioned|p23|||Of Georgina Basin.||||||02-APR-07
1389|Beetle Creek Formation|23393|6|Mentioned|p22|||||||||
1389|Beetle Creek Formation|23517|5|Briefly described|p28|||Main phosphate horizon.||||||
1389|Beetle Creek Formation|24034|6|Mentioned|p9|Middle Cambrian|Middle Cambrian|Geological Province: Mount Isa Inlier.||||||
1389|Beetle Creek Formation|24419|5|Briefly described|p18|Late Cambrian|Middle Cambrian|Conformably overlies and interfingers with Thorntonia Limestone.  Variably phosphatic and comprises chert, silicified coquinite, chert breccia and conglomerate, siliceous and phosphatic siltstone and phosphorite. Geological Province: Georgina Basin.||||||12-APR-05
1389|Beetle Creek Formation|29940|6|Mentioned|p169|||||||||
1389|Beetle Creek Formation|30239|4|Described|p1193|||||||||
1389|Beetle Creek Formation|30242|5|Briefly described|p9|||Clay mineralogy||||||
1389|Beetle Creek Formation|30479|6|Mentioned|Fig.5|||See also Fig.6 and 7. Stratigraphic relationships||||||
1389|Beetle Creek Formation|30773|6|Mentioned|p266|||Middle Cambrian age||||||
1389|Beetle Creek Formation|30774|6|Mentioned|p1|||||||||
1389|Beetle Creek Formation|30775|6|Mentioned|p1|||||||||
1389|Beetle Creek Formation|30778|6|Mentioned|p1,12,Fig.5|||||||||
1389|Beetle Creek Formation|30914|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
1389|Beetle Creek Formation|31289|6|Mentioned|p704|||See also Fig. 1||||||
1389|Beetle Creek Formation|31342|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
1389|Beetle Creek Formation|31396|6|Mentioned|Fig.3|||||||||
1389|Beetle Creek Formation|31504|5|Briefly described|p303|||M. Cambrian||||||
1389|Beetle Creek Formation|32466|6|Mentioned|p316|||Contains phosphate.||||||
1389|Beetle Creek Formation|32576|5|Briefly described|p49|||||||||
1389|Beetle Creek Formation|32952|4|Described|p1188|||See also pp1189-1194,1203 etc. L.M-Camb.||||||24-JUL-06
1389|Beetle Creek Formation|33111|4|Described|p6,31|||Mentioned p6.||||||
1389|Beetle Creek Formation|33482|5|Briefly described|p1|||Early Middle Cambrian. Phosphate in.||||||
1389|Beetle Creek Formation|33900|6|Mentioned|p19|||||||||
1389|Beetle Creek Formation|34287|6|Mentioned|Fig.3|||||||||
1389|Beetle Creek Formation|34395|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
1389|Beetle Creek Formation|34543|6|Mentioned|p98|||Middle Cambrian||||||
1389|Beetle Creek Formation|34754|6|Mentioned|p27|||||||||
1389|Beetle Creek Formation|34935|6|Mentioned|p274|||||||||
1389|Beetle Creek Formation|35001|6|Mentioned|Fig.45|||||||||
1389|Beetle Creek Formation|35004|6|Mentioned|Fig.60|||||||||
1389|Beetle Creek Formation|35054|6|Mentioned|Table 23|||||||||
1389|Beetle Creek Formation|35121|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
1389|Beetle Creek Formation|35139|4|Described|Table.2|||||||||
1389|Beetle Creek Formation|35146|6|Mentioned|p470|||||||||
1389|Beetle Creek Formation|35538|6|Mentioned|Fig.2|||||||||
1389|Beetle Creek Formation|35553|6|Mentioned|p56|||See also Appendix 2, description of Agnostid localities.||||||
1389|Beetle Creek Formation|35936|6|Mentioned|p615|||||||||
1389|Beetle Creek Formation|36234|6|Mentioned|p167|||||||||
1389|Beetle Creek Formation|36448|6|Mentioned|p395|||||||||
1389|Beetle Creek Formation|36525|6|Mentioned|Fig.4|||||||||
1389|Beetle Creek Formation|36645|5|Briefly described|p314|||See Fig.2,3, p307.||||||30-JAN-07
1389|Beetle Creek Formation|36751|6|Mentioned|p485|||||||||
1389|Beetle Creek Formation|36818|6|Mentioned|p203|||||||||
1389|Beetle Creek Formation|37271|6|Mentioned|p210|||||||||
1389|Beetle Creek Formation|37413|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
1389|Beetle Creek Formation|37572|4|Described|p157|||See also p158,165 and Figs.7 and 8||||||24-JUL-06
1389|Beetle Creek Formation|37816|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
1389|Beetle Creek Formation|38209|5|Briefly described|p176|||||||||
1389|Beetle Creek Formation|38350|6|Mentioned|p22|||||||||
1389|Beetle Creek Formation|38442|5|Briefly described|Map legend|Cambrian|Cambrian|||||||25-AUG-04
1389|Beetle Creek Formation|38444|5|Briefly described|p105|||||||||
1389|Beetle Creek Formation|38445|5|Briefly described|p98|||||||||
1389|Beetle Creek Formation|38446|6|Mentioned|Table 23|||||||||
1389|Beetle Creek Formation|38608|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
1389|Beetle Creek Formation|39445|5|Briefly described|Table 4|||See also p62.||||||24-JUL-06
1389|Beetle Creek Formation|39690|6|Mentioned|Table 1|||||||||
1389|Beetle Creek Formation|40004|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
1389|Beetle Creek Formation|40038|6|Mentioned|p248|||||||||
1389|Beetle Creek Formation|40221|4|Described|p20|||||||||
1389|Beetle Creek Formation|40386|6|Mentioned|p429|||||||||
1389|Beetle Creek Formation|40623|5|Briefly described|p96|||||||||
1389|Beetle Creek Formation|40686|5|Briefly described|p407|||||||||
1389|Beetle Creek Formation|40852|6|Mentioned|p34|||||||||
1389|Beetle Creek Formation|40855|6|Mentioned|p329|||||||||
1389|Beetle Creek Formation|40856|5|Briefly described|p313|||||||||
1389|Beetle Creek Formation|40857|5|Briefly described|p268|||||||||
1389|Beetle Creek Formation|40858|5|Briefly described|p132|||||||||
1389|Beetle Creek Formation|41109|6|Mentioned|p184|||||||||
1389|Beetle Creek Formation|41129|6|Mentioned|p17|||See also Fig.8||||||
1389|Beetle Creek Formation|41298|6|Mentioned|Map legend|Middle Cambrian||||||||
1389|Beetle Creek Formation|41639|6|Mentioned|p3,p15|||||||||
1389|Beetle Creek Formation|42058|6|Mentioned|p122|||||||||
1389|Beetle Creek Formation|42070|6|Mentioned|p4|||||||||
1389|Beetle Creek Formation|42477|5|Briefly described|p65, 67|||||||||
1389|Beetle Creek Formation|42575|5|Briefly described|Fig.2 P335|||||||||
1389|Beetle Creek Formation|44091|14|Not recorded|p16,-18,Tb.1||Middle Cambrian|||||||
1389|Beetle Creek Formation|44112|6|Mentioned|p78|||||||||
1389|Beetle Creek Formation|44205|14|Not recorded|p33|||||||||
1389|Beetle Creek Formation|44209|14|Not recorded|p136||Cambrian|||||||
1389|Beetle Creek Formation|44210|2|Defined|Tb.2,p13,114|||||||||
1389|Beetle Creek Formation|44211|2|Defined|p96,98-99,101-103|||Lower part called "Yelvertoft Bed".||||||24-JUL-06
1389|Beetle Creek Formation|44213|14|Not recorded|Map Legend||Middle Cambrian|||||||
1389|Beetle Creek Formation|44273|14|Not recorded|Map Legend||Middle Cambrian|||||||
1389|Beetle Creek Formation|44274|14|Not recorded|p11|||Contemporaneous with Border Waterhole Formation.||||||
1389|Beetle Creek Formation|44275|14|Not recorded|Map Legend||Middle Cambrian|||||||
1389|Beetle Creek Formation|44276|2|Defined|Tb.2,p22|||||||||
1389|Beetle Creek Formation|44277|14|Not recorded|Map Legend||Middle Cambrian|||||||
1389|Beetle Creek Formation|44529|14|Not recorded|p45||Middle Cambrian|Contains phosphate deposits.||||||
1389|Beetle Creek Formation|44757|6|Mentioned|p153,155|||||||||
1389|Beetle Creek Formation|44788|14|Not recorded|p27|||||||||
1389|Beetle Creek Formation|44878|14|Not recorded|p14||Middle Cambrian|||||||
1389|Beetle Creek Formation|44920|14|Not recorded|Map Legend,Sheet 2,4||Middle Cambrian|||||||
1389|Beetle Creek Formation|44989|14|Not recorded|Not recorded|||||||||
1389|Beetle Creek Formation|45044|14|Not recorded|p5,22||Middle Cambrian|||||||
1389|Beetle Creek Formation|45045|6|Mentioned|p7|||Trilobites||||||
1389|Beetle Creek Formation|45052|3|Fully described|p90|||M.Camb. Contains Yelvertoft Bed.||||||30-JAN-07
1389|Beetle Creek Formation|45055|6|Mentioned|p9|||Templetonian. See also P18,29,30,32,36||||||
1389|Beetle Creek Formation|45062|6|Mentioned|p7|||||||||
1389|Beetle Creek Formation|45079|3|Fully described|p22|||Lower Middle Cambrian age. See also p49||||||24-JUL-06
1389|Beetle Creek Formation|45114|6|Mentioned|p189|||||||||
1389|Beetle Creek Formation|45119|6|Mentioned|p4|||||||||
1389|Beetle Creek Formation|45161|6|Mentioned|p67|||||||||
1389|Beetle Creek Formation|45166|5|Briefly described|Table 15|||||||||
1389|Beetle Creek Formation|46792|6|Mentioned|p51|||Trilobite fauna||||||
1389|Beetle Creek Formation|47058|6|Mentioned|119|||||||||
1389|Beetle Creek Formation|48971|6|Mentioned|p10,18,21,25,27,29,|||p30.||||||
1389|Beetle Creek Formation|50100|5|Briefly described|p22, p75|Middle Cambrian|Middle Cambrian|Includes Monastery Creek Phosphorite Mbr. Predominantly shallow-marine, clastic, calcareous, dolomitic, cherty and phosphatic sedimentary rocks; commonly contains abundant trilobite fossils.  Disconformably overlies Thorntonia Lst; overlain by Inca Fm.||||||20-JAN-05
1389|Beetle Creek Formation|60122|6|Mentioned|p57 Appendix|||Correlated with parts of Arthur Creek Formation. Geological Province: eastern Georgina Basin and Burke River Structural Belt.||||||11-MAY-05
1389|Beetle Creek Formation|60264|6|Mentioned|p575|||Superseded by/or previously Monastery Creek Formation?  Geological Province: Burke River Structural Belt.||||||02-APR-07
1389|Beetle Creek Formation|60359|5|Briefly described|Map Legend|Cambrian|Cambrian|Siltstone, chert, shale, phospharite, phosphatic siltstone.||||||
1389|Beetle Creek Formation|60419|5|Briefly described|p18|Middle Cambrian|Middle Cambrian|Geological Province: Georgina Basin. Contains fauna of Ordian age.||||||
1389|Beetle Creek Formation|61181|5|Briefly described|p163|Middle Cambrian|Early Cambrian|Contains large resources of phosphorites. In north-west Queensland. ||||||
1389|Beetle Creek Formation|62504|6|Mentioned|p4|Cambrian|Cambrian|Age: Templetonian.||||||
1389|Beetle Creek Formation|62788|6|Mentioned|p103, p105, p124|Middle Cambrian|Middle Cambrian|Western Queensland unit in which Xystridura templetonensis is the predominant fossil. This and other species support correlation of this unit with the Jigaimara Formation in NT.||||||
1389|Beetle Creek Formation|63450|5|Briefly described|p81, p87|||Contains Monastery Creek Phosphorite Member, also referred to as Monastery Creek Member.||||||07-FEB-11
1389|Beetle Creek Formation|64068|4|Described|p62, 54, 58, pp89-90|Middle Cambrian|Middle Cambrian|Diverse trilobite fauna. Correlated with (lower) Arthur Creek Formation.||Of Narpa Group.|Includes Monastery Creek Phosphorite Member at top.|Disconformably overlies Thorntonia Limestone. Conformably overlain by Inca Formation.|Calcareous and siliceous siltstone, chert, foetid dolomitic phosphatic limestone, calcareous phosphorite, siltstone.|05-APR-12
1389|Beetle Creek Formation|64443|6|Mentioned|p40.|||||||Correlative of Wonarah Formation.||14-MAY-14
1389|Beetle Creek Formation|65337|6|Mentioned|p60.|||Northeastern Georgina Basin. ||||||
1389|Beetle Creek Formation|65345|6|Mentioned|p1.|||Positive tests in 1965-1966 for phosphate identified this unit as a target.||||||
1389|Beetle Creek Formation|65489|5|Briefly described|p126-127|Cambrian|Cambrian|Georgina Basin. Hydrocarbon potential: TOC at 0.19-1.51%|||Includes Monastery Creek Member.||Phosphate-bearing unit.|
1389|Beetle Creek Formation|67127|6|Mentioned|p78|||Primary host for phosphorite REE deposits.||||||
1389|Beetle Creek Formation|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map; p83|Cambrian|Cambrian|Georgina Basin.||Narpa Group.||Overlies Thorntonia Limestone. Is overlain by Inca Formation and (unconformably) by Camooweal Dolomite, Age Creek Formation, Currant Bush Limestone and Inca Formation.|Chert, siliceous shale with trilobite fossils, basal conglomerate.|
1389|Beetle Creek Formation|67352|6|Mentioned|p69|||||||||
1389|Beetle Creek Formation|67499|6|Mentioned|p940|Cambrian|Cambrian|Overlies Proterozoic rocks with angular unconformity.||||||08-MAY-12
1389|Beetle Creek Formation|67870|5|Briefly described|p38, p44|Middle Cambrian|Middle Cambrian|Georgina Basin. An important source of phosphate.||||Unconformably overlies Thorntonia Limestone.|Siltstone, chert and shale.|
1389|Beetle Creek Formation|68020|6|Mentioned|p126|Cambrian|Cambrian|Includes phosphorite deposits.||||||
1389|Beetle Creek Formation|69443|6|Mentioned|p28:14, 16, 22-23|||||||Unconformably overlies Shadow Group. Correlated with Anthony Lagoon, Wonarah Formations.||12-JUL-16
1389|Beetle Creek Formation|69573|6|Mentioned|p656, 661|||Deeper-water sediments. Features Cambrian Stage 5 fossil sites.|||Monastery Creek Phosphorite Member.|||
1389|Beetle Creek Formation|69591|4|Described|p87-88, p90, p92-93, p96-97,p98 Fig.2.91|Cambrian|Cambrian|Georgina Basin. Beetle Creek, near May Downs homestead W of Mount Isa. Hosts phosphorite deposits. Contains a well-known trilobite fauna (species listed). Occurs as small erosional residuals up to 20m thick. Composed of three "members" [only one with a valid stratigraphic name].||Narpa Group.|Ardmore Chert Member, Yelvertoft Bed.|Conformably overlies or grades into Thorntonia Limestone. Is overlain by Inca Formation, and unconformably by Blazan Shale, Camooweal Dolomite, Swift Formation and Age Creek Formation.|Siliceous shale, chert, siltstone and fine sandstone with thin interbeds of limestone in places. Richly fossiliferous: has a well-known trilobite fauna.|
1389|Beetle Creek Formation|70723|5|Briefly described|p24 Fig. 2|Cambrian|Cambrian|Georgina Basin.||Narpa Group||Undilla Sub-basin, Georgina Basin. Overlies Thorntonia Limestone. Is overlain by Inca Formation and Currant Bush Limestone.||
1389|Beetle Creek Formation|70864|6|Mentioned|p74 Fig 2||Paleozoic|Shown as a combined unit with Inca Formation||||||
1389|Beetle Creek Formation|72297|5|Briefly described|p732, p747|Middle Cambrian|Middle Cambrian|Georgina Basin. One of the two major producers of phosphate in QLD. TOC value of 0.19 - 1.51% reported.|||||Marine sequences of phosphorite (phosphatic siltstone) and chert, overlying limestone, sandstone and conglomerate.|
1389|Beetle Creek Formation|72321|6|Mentioned|Fig 2|Wulian|Wulian|Burke River Structural Belt, Undilla Sub-basin, Georgina Basin. Age Cambrian Series 3, Stage 5. Australian stage: Templetonian||of Narpa Group.||||
1389|Beetle Creek Formation|72516|6|Mentioned|p92|Cambrian|Cambrian|Eastern Georgina Basin.||||Equivalent to the Arthur Creek Formation.||03-JUN-21
1389|Beetle Creek Formation|73418|4|Described|p3, p4 fig 3|Miaolingian|Miaolingian|Georgina Basin, Burke River Structural Belt and Undilla Sub-basin. Dominantly apatitic (non-pelletal) mudstones in central and northern parts (Undilla Sub-basin) contain high contributions of terrigenous material and low REE concentrations. Largely pelletal phosphorites in southern parts (Burke River Structural Belt) can contain up to 0.5 wt% REE, and high concentrations of other elements that substitute into carbonate fluorapatite.||Narpa Group|Lower Siltstone Member, Monastery Creek Phosphorite Member|Overlies Thorntonia Limestone, underlies Inca Formation, Currant Bush Limestone|Phosphorite and shale units.|12-FEB-23
1503|Berinka Volcanics|22809|6|Mentioned|11|||||||||
1503|Berinka Volcanics|24197|5|Briefly described|p105 Tb. 15.1|Paleoproterozoic|Paleoproterozoic|Of the Gerowie Suite. Age: ~1885Ma. Geological Province: Pine Creek Inlier.||||||07-FEB-11
1503|Berinka Volcanics|30831|6|Mentioned|p10|||||||||
1503|Berinka Volcanics|32170|6|Mentioned|Map legend|Adelaidean|Adelaidean|Adelaidean or Carpentarian.Prob. Adelaidean||||||
1503|Berinka Volcanics|32307|4|Described|Table 1|||L.Proterozoic||||||
1503|Berinka Volcanics|32310|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
1503|Berinka Volcanics|32660|5|Briefly described|Table 2|||||||||
1503|Berinka Volcanics|32700|5|Briefly described|Table 1|||Mention p12||||||24-JUL-06
1503|Berinka Volcanics|33376|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
1503|Berinka Volcanics|39069|5|Briefly described|Table 1|||||||||
1503|Berinka Volcanics|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
1503|Berinka Volcanics|39889|6|Mentioned|Table 2|||||||||
1503|Berinka Volcanics|40493|5|Briefly described|Table 1|||||||||
1503|Berinka Volcanics|41645|3|Fully described|p11|||||||||
1503|Berinka Volcanics|41646|6|Mentioned|Map legend|Paleoproterozoic||Of the Finniss River Group. Altered to metamorphosed lithic crystal tuff; rhyodacite; micro-spherulitic rhyodacite; andesite; agglomerate; minor interlayered mudstone.||||||07-NOV-08
1503|Berinka Volcanics|41660|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Metamorphosed to altered spherulitic dacite; sheared lithic tuff; agglomerate; silicified-sericitised feldspar-crystal tuff; porphyritic rhyodacite; interlayered siltstone and mudstone. Clasts included in quartz conglomerate of Burrell Creek Formation.||||||07-NOV-08
1503|Berinka Volcanics|41661|3|Fully described|p13|||||||||
1503|Berinka Volcanics|41980|5|Briefly described|Table 2 P568|||||||||
1503|Berinka Volcanics|43187|5|Briefly described|p2|||||||||
1503|Berinka Volcanics|45022|14|Not recorded|p.40,44, Fig7, Tb2||Paleoproterozoic|Pl. 28 of Finniss River Group.||||||07-NOV-08
1503|Berinka Volcanics|45112|5|Briefly described|Table 21|||||||||
1503|Berinka Volcanics|46163|14|Not recorded|p.170|||||||||
1503|Berinka Volcanics|47047|6|Mentioned|p220|||||||||
1503|Berinka Volcanics|48942|3|Fully described|p13|||||||||
1503|Berinka Volcanics|50586|5|Briefly described|p1.1, 6.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Of the Gerowie Suite.||||||07-NOV-08
1503|Berinka Volcanics|63866|5|Briefly described|p105, p109|Orosirian|Orosirian|Litchfield Province, Pine Creek Orogen. |1861 +/- 4 Ma (Worden et al, in press)|Finniss River Group||||
1503|Berinka Volcanics|64677|5|Briefly described|v, p1, p9-12, p44-45|||Pine Creek Orogen.|1861.4 +/- 3.2 Ma.|Finniss River Group.|||Felsic volcanic rocks: dark grey-green, fine-grained, spherulitic; or weathered, altered and sheared.|
1503|Berinka Volcanics|64698|4|Described|lithinterp table|Orosirian|Orosirian|Of Finniss River Group. Age 1850-1863Ma. Max thick 2000m. Altered and metamorphosed lithic crystal tuff, rhyodactite, micro-spherulitic rhyodacite, andesite, agglomerate, minor interlayered mudstone.||||||10-FEB-10
1503|Berinka Volcanics|64730|4|Described|p125 Fig. 3, p126-127, p135-136|Paleoproterozoic|Paleoproterozoic|Age is extrusion age. Correlated with Meeway Volcanics and with Mulluk Mulluk Volcanic Member, and Warrs Volcanic Member (1862+/-3 Ma) of Burrell Creek Formation.|1861 +/- 4 Ma (U/Pb SHRIMP zircon).|Near base of Finniss River Group.|||Porphyritic and spherulitic rhyolite and dacite, feldspathic and lithic tuffs and agglomerates, highly sheared in places.|03-MAY-12
1503|Berinka Volcanics|64956|6|Mentioned|p72|||Of the Finniss River Group.||||||07-FEB-11
1503|Berinka Volcanics|65339|6|Mentioned|p5 Fig.4. ||||||||Felsic volcanic rocks.|
1503|Berinka Volcanics|67167|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Unit in Finniss River Group.|||Metamorphosed to altered spherulitic dacite; sheared lithic tuff; silicified-sericitised feldspar crystal tuff; porphyritic rhyodacite; interlayered siltstone and mudstone.|
1503|Berinka Volcanics|67232|5|Briefly described|p4, p5. |Paleoproterozoic|Paleoproterozoic|Felsic volcanism.|1861 +/- 4 Ma (Worden et al. 2006a,b).|||Is intruded by Wangi Basics.||
1503|Berinka Volcanics|67355|6|Mentioned|p7 Tb.2|||Walpole et al. (1968)||Finniss River Group||||25-JAN-17
1503|Berinka Volcanics|67779|5|Briefly described|p6 Fig.5.|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen.|1861 +/- 4 Ma (Worden et al. 2008a).|shown as unit in Burrell Creek Formation.||||14-MAY-18
1503|Berinka Volcanics|69420|4|Described|p5:4, 6, 8, 13, 32|Paleoproterozoic|Paleoproterozoic|Western region, Central Domain, Pine Creek Orogen. Crops out immediately W of the Giants Reef Fault. Up to 75m thick. Interbedded with conglomeratic rocks previously known as the Noltenius Formation (a defunct term): now basal Burrell Creek Formation. Fluvial to subtidal deposits. Comagmatic with Mulluk Mulluk, Meeway Volcanics and Warrs Volcanic Member. SHRIMP U-Pb zircon age.|1861 +/- 4 Ma (Worden et al., 2008).|Finniss River Group.||Is interbedded with basal Burrell Creek Formation.|Rhyolite, tuff and agglomerate, spherulitic or porphyritic dacite, basic lavas, and interbedded sandstone; near Giants Reef Fault the rocks are strongly sheared, altered and weathered.|12-JUL-16
1503|Berinka Volcanics|69917|6|Mentioned|p52|||||Basal volcanics of Finniss River Group||||
1503|Berinka Volcanics|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||dacite|
1503|Berinka Volcanics|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|1861+/-4 Ma (MDA: U-Pb zircon SHRIMP)||||Altered and sheared quartz arenite (volcanic?).|
1503|Berinka Volcanics|73083|6|Mentioned|p49|||||||||
1514|Bernborough Formation|23410|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Flynn Subgroup, Churchills Head Group. Includes Whippet Sandstone Member. Felsic crystal-lithic tuff, ignimbrite, lapilli tuff, and lava (?); chert. Siltstone, shale and fine grained lithic arenite and wacke; thin bedded and laminated.||||||07-NOV-08
1514|Bernborough Formation|23733|5|Briefly described|p32 Fig. 19|||Of Flynn Group.  Age: 1840Ma.||||||
1514|Bernborough Formation|23809|5|Briefly described|p27 Fig. 25, p29|Paleoproterozoic|Paleoproterozoic|Of the Flynn Group.  Age: 1853+/-5Ma.  Correlates with the Lower Yungkulungu Formation.  Geological Province: Tennant Inlier.||||||07-NOV-08
1514|Bernborough Formation|24172|4|Described|p18, p8 Tb.1|Paleoproterozoic|Paleoproterozoic|Of the Flynn Subgroup. Overlying Unit: Brumbreu Formation. Underlying Unit: Warramunga Formation. Geological Province: Tennant Creek Inlier. Max. Thick.: ~900m in type area. Age: 1840+/-8Ma (Compston, 1994) & 1870+/-15Ma (Black, 1984).||||||14-APR-15
1514|Bernborough Formation|30320|5|Briefly described|p421|||||||||
1514|Bernborough Formation|31734|5|Briefly described|p1388|||See also p1389||||||24-JUL-06
1514|Bernborough Formation|32174|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
1514|Bernborough Formation|32959|5|Briefly described|p21|||||||||
1514|Bernborough Formation|33307|5|Briefly described|p18|||Mention Fig.8.||||||
1514|Bernborough Formation|35771|4|Described|Table 1|||||||||
1514|Bernborough Formation|39213|5|Briefly described|p18|||See also Fig.8||||||
1514|Bernborough Formation|39571|4|Described|p127|||||||||
1514|Bernborough Formation|41465|5|Briefly described|p9|||||||||
1514|Bernborough Formation|41961|6|Mentioned|Table 1 P39|||||||||
1514|Bernborough Formation|41970|6|Mentioned|p335|||||||||
1514|Bernborough Formation|42853|5|Briefly described|p593|||Of Warramunga Group||||||24-JUL-06
1514|Bernborough Formation|42936|5|Briefly described|p546|||Of Warramunga Group.||||||24-JUL-06
1514|Bernborough Formation|43223|5|Briefly described|Map Legend||Paleoproterozoic|Of Flynn Subgroup||||||07-NOV-08
1514|Bernborough Formation|43751|6|Mentioned|Fig.2,p610||Paleoproterozoic|||||||07-NOV-08
1514|Bernborough Formation|46842|4|Described|p116|||||||||
1514|Bernborough Formation|46992|4|Described|p253|||||||||
1514|Bernborough Formation|48891|4|Described|p.10||Paleoproterozoic|Table 1, p.1,8,9,11,12,13,17,19,41. Lower Proterozoic.||||||07-NOV-08
1514|Bernborough Formation|50588|5|Briefly described|p2.1|Paleoproterozoic|Paleoproterozoic|Of the Tennant Creek Supersuite.  Geological Province: Tennant Creek/Davenport Province. Age: 1845-1840 +/- 8Ma (Shrimp).||||||07-NOV-08
1514|Bernborough Formation|60684|4|Described|p11, p7 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Flynn Subgroup (Churchills Head Group). Overlies Whippet Sandstone Member. Age: 1840+/-8Ma, 1845+/-4Ma (Compston 1991). Max. thickness:~900m. Correlates with Warrego Volcanics, and parts of Wundirgi and Yungkulungu Fms.||||||07-NOV-08
1514|Bernborough Formation|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Ooradidgee Group. Includes the Whippet Sandstone Member. Felsic, crystal-like tuff, lapilli tuff, ignimbrite, probably lava, chert; siltstone, shale, fine-grained lithic arenite/greywacke.  In the Tennant Creek region.||||||30-SEP-11
1514|Bernborough Formation|65209|5|Briefly described|p35 Fig.1, p36|Paleoproterozoic|Paleoproterozoic|||Ooradidgee Group|Whippet Sandstone Member|||
1514|Bernborough Formation|65222|5|Briefly described|p111, Tb 1, p110,116 Tb 3, p121-123,125|||Previous data: 1733 +/- 40 Ma Rb-Sr on volcanics; 1870+/- 15 Ma U-Pb; 1875+/-33 Ma U-Pb. Previously included in Warramunga Formation. Reassigned to Flynn Subgroup in 1991 (Donnellan). Two zircon sample localities, tuff and rhyolite.|1840+/- 8Ma, 1845 +/- 4 Ma U/Pb SHRIMP.|Of Flynn Subgroup|||Includes crystal-rich foliated volcanic rock; altered porphyritic rhyolite.|24-JAN-22
1514|Bernborough Formation|65338|5|Briefly described|pp16-17, p19.|Orosirian|Orosirian|Contemporaneous with syn- to immediately post-tectonic granite emplacement asssociated with the Tennant Event.|1845 +/- 4 and 1840 +/- 8 Ma.||||Includes ignimbrites.|
1514|Bernborough Formation|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Ooradidgee Group.|Includes Whippet Sandstone Member.||Felsic crystal-lithic tuff, lapilli tuff, ignimbrite, probable lava, chert; siltstone, shale, fine-grained lithic arenite/wacke.|
1514|Bernborough Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Tennant Creek/Davenport area.|1845 +/- 4 Ma.|Ooradidgee Group.|Whippet Sandstone Member.|||
1514|Bernborough Formation|69187|5|Briefly described|p53 Fig.2, p54 Fig.3|||||Ooradidgee Group||||
1514|Bernborough Formation|69424|3|Fully described|p9:3-5, 7, 10, 15-17, 19-22, 39 Fig.9.24|Paleoproterozoic|Paleoproterozoic|Warramunga Province. Felsic extrusives of this unit are included in the Tennant Creek Supersuite. Subaerial and subaqueous; volcanic rocks are predominantly subaerial and include a phreatomagmatic tuff cone or ring succession overlain by ignimbrite. c.900m thick in type section. The top of the basal Whippet Sandstone Member is a 2-5m green chert containing rare, large accretionary lapilli. U-Pb zircon ages from Compston (1995).|1845 +/- 4 Ma to 1840 +/- 8 Ma.|Ooradidgee Group.|Whippet Sandstone Member.|Correlative of Yungkulungu Formation - sedimentary lithofacies, and with Wundirgi Formation (upper part). Apparently intruded by Tennant Creek Granite.|Dacitic to rhyolitic ignimbrite, tuff, lapilli-tuff and other minor probable volcanic rocks, interbedded with thinly bedded siltstone, shale and chert; thinly to medium bedded lithic to sublithic sandstone; minor pebble conglomerate.|12-JUL-16
1514|Bernborough Formation|71592|5|Briefly described|Appendix A.|||Tennant Creek Region. See also Bernborough Volcanics.|1844+/-5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Rhyolite, porphyritic rhyolite, crystal-rich foliated volcanic rock. See also Bernborough Volcanics.|
1514|Bernborough Formation|73124|6|Mentioned|p2 Fig.1|||||Ooradidgee Group||Underlain by Monument Formation. Overlain by Brumbreu Formation. Equivalent to Wundirgi Formation.||
1514|Bernborough Formation|73125|5|Briefly described|p2|Palaeoproterozoic|Palaeoproterozoic|Warramunga Province.||Ooradidgee Group.||||
1514|Bernborough Formation|73427|6|Mentioned|p12|||||Ooradidgee Group||||
1514|Bernborough Formation|73460|6|Mentioned|p2|||Warramunga Province.||Ooradidgee Group||Underlain by Monument Formation. Overlain by Brumbreu Formation. Equivalent to Wundirgi Formation.||
1514|Bernborough Formation|73550|6|Mentioned|p5|Orosirian|Orosirian||ca 1840 Ma|||||
1514|Bernborough Formation|73590|6|Mentioned|p1-2|Orosirian|Orosirian||ca 1840 Ma|Ooradidgee Group||Underlain by Monument Formation. Overlain by Brumbreu Formation. Equivalent to Wundirgi Formation.||
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.|
1621|Bigie Formation|22438|4|Described|p535, Fig.3 p537|||Basal unit of Isa Superbasin. See also Fig.10a p546.||||||
1621|Bigie Formation|22457|5|Briefly described|P31|||||||||
1621|Bigie Formation|22498|5|Briefly described|Fig2 P235, P236|||||||||
1621|Bigie Formation|22585|5|Briefly described|Fig1 P736, Fig3|||||||||
1621|Bigie Formation|22665|6|Mentioned|P219, Table1|||||||||
1621|Bigie Formation|22680|6|Mentioned|83|||||||||
1621|Bigie Formation|23031|5|Briefly described|21|Paleoproterozoic|Paleoproterozoic|Geol province: Mount Isa Fold Belt. Overlying units: McNamara Group, Suprise Creek Formation, Fiery Creek Volcanics; underlying unit: Quilalar Formation||||||07-NOV-08
1621|Bigie Formation|23393|4|Described|p19, p16 Fig. 4|Paleoproterozoic|Paleoproterozoic|Geological Province: Lawn Hill Sub-province.||||||07-NOV-08
1621|Bigie Formation|23395|6|Mentioned|p383|||||||||
1621|Bigie Formation|23396|5|Briefly described|p407 Fig.2|||||||||
1621|Bigie Formation|23397|5|Briefly described|p467 Fig.2|||||||||
1621|Bigie Formation|23399|6|Mentioned|p489|||||||||
1621|Bigie Formation|23406|5|Briefly described|p603, p607 Fig. 8|||Geological province: Lawn Hill Platform. See also Fig. 5.||||||16-JUN-09
1621|Bigie Formation|23408|5|Briefly described|p511, p513 Fig. 2, p523|||Of Hutton et al (1981) who formalised the subdivision of the McNamara Group and added this new formation together with Fiery Creek Volcanics at the base.||||||15-JUN-09
1621|Bigie Formation|23466|5|Briefly described|p267|||||||||
1621|Bigie Formation|23518|4|Described|p9 Fig. 3, p11|Proterozoic|Proterozoic|Geological Province: Western Fold Belt.||||||
1621|Bigie Formation|23767|5|Briefly described|p1954 Fig. 1a|||See also p1955.||||||
1621|Bigie Formation|23965|5|Briefly described|p1297|||Geological Province: Mount Isa Inlier.||||||
1621|Bigie Formation|24307|5|Briefly described|p978||Paleoproterozoic|Geological Province: Mount Isa Block||||||07-NOV-08
1621|Bigie Formation|24308|5|Briefly described|p992, p987 Fig. 2|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
1621|Bigie Formation|24419|5|Briefly described|p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Of Fiery Suite.  Geological Province: Western Fold Belt, Lawn Hill Subprovince and Leichardt River Subprovince  (Mount Isa Orogen).||||||07-NOV-08
1621|Bigie Formation|24432|6|Mentioned|p562 Fig.2|Statherian|Statherian|||||||
1621|Bigie Formation|37459|2|Defined|p423|Mesoproterozoic|Mesoproterozoic|Age is more specifically Carpentarian||||||
1621|Bigie Formation|38232|6|Mentioned|p85|||||||||
1621|Bigie Formation|38237|4|Described|p126|||||||||
1621|Bigie Formation|38310|6|Mentioned|p237|||||||||
1621|Bigie Formation|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
1621|Bigie Formation|38835|6|Mentioned|p164|||||||||
1621|Bigie Formation|39445|5|Briefly described|Table 2|||||||||
1621|Bigie Formation|39556|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||
1621|Bigie Formation|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Sandstones and conglomerates. Overlies the Quilalar Formation.||||||15-JUN-06
1621|Bigie Formation|39622|6|Mentioned|Fig.2|||||||||
1621|Bigie Formation|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
1621|Bigie Formation|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
1621|Bigie Formation|39925|6|Mentioned|p329|||||||||
1621|Bigie Formation|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
1621|Bigie Formation|40221|3|Fully described|p11|||||||||
1621|Bigie Formation|40840|6|Mentioned|Map legend|||||||||
1621|Bigie Formation|41298|6|Mentioned|Map legend|Carpentarian||||||||
1621|Bigie Formation|41307|4|Described|p12|||||||||
1621|Bigie Formation|41978|6|Mentioned|p502|||||||||
1621|Bigie Formation|41979|6|Mentioned|Fig.2 P512|||||||||
1621|Bigie Formation|42565|5|Briefly described|Table 1 P5, P4|||||||||
1621|Bigie Formation|42676|5|Briefly described|Fig.2 P41|||||||||
1621|Bigie Formation|42706|5|Briefly described|map legend|Proterozoic|Proterozoic|Sandstone, conglomerate.||||||09-FEB-09
1621|Bigie Formation|42818|5|Briefly described|Fig.2 P205|||||||||
1621|Bigie Formation|43608|6|Mentioned|Fig.11,p11|||||||||
1621|Bigie Formation|43616|6|Mentioned|p4|||||||||
1621|Bigie Formation|45166|4|Described|p28|||||||||
1621|Bigie Formation|47083|4|Described|p11||Proterozoic|Previously included in Fiery Creek Volcanics and 'Myally Beds'. Unconformably overlain by Surprise Creek Fm; overlies Quilalar Fm unconformably and Myally Subgp. Thickness: 800 m.||||||25-JUL-06
1621|Bigie Formation|50100|5|Briefly described|p13 Fig.4|Statherian|Statherian|Geological Province: Western Fold Belt Province.||||||
1621|Bigie Formation|50332|5|Briefly described|p16, p20|Paleoproterozoic|Paleoproterozoic|Unconformably overlies the Quilalar Formation, overlain by Bigie Formation. Outcrops at eastern margin of Leichhardt River Subprovince. Consists of redbed sandstone, pebbly sanddtone and conglomerate.||||||07-FEB-11
1621|Bigie Formation|50550|5|Briefly described|p1139 Fig.2||Statherian|Overlies Quilalar formation at an angular unconformity. Conformably overlain by Fiery Creek Volcanics. Geological Province: Western Fold Belt.||||||17-DEC-07
1621|Bigie Formation|50624|5|Briefly described|p234 Fig.2||Paleoproterozoic|||||||07-NOV-08
1621|Bigie Formation|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: >1700Ma. Geological Province: western Mount Isa Block.||||||07-NOV-08
1621|Bigie Formation|61929|5|Briefly described|p128 Fig. 2|||||||||
1621|Bigie Formation|61936|5|Briefly described|p194 Fig. 6|||Intercalated with Fiery Creek Volcanics. Geological Province: Calvert Superbasin, Western Fold Belt, Mount Isa Inlier. ||||||
1621|Bigie Formation|62084|5|Briefly described|p936 Fig.5|||Calvert Superbasin. Shown as Bigie Fm. Age: U-Pb SHRIMP (after Page et al. 2000)|overlying unnamed unit 1709+/-2 Ma|||||
1621|Bigie Formation|62535|5|Briefly described|p672|Statherian|Statherian|||||Is overlain unconformably by Surprise Creek Formation.||
1621|Bigie Formation|62988|5|Briefly described|p34|||Probably coeval with the ~1710Ma Fiery Event. Now grouped in the Big Supersequence. Geological Province: Calvert Superbasin (Mount Isa Inlier).||||||25-JAN-07
1621|Bigie Formation|63023|5|Briefly described|p1024 Fig. 1, p1025 Fig. 2|Paleoproterozoic|Paleoproterozoic|Ages: 1762+/-18Ma, 1764+/-13Ma, 1783+/-5Ma. Unconformable on Quilalar Fm. Geological Province: Calvert Superbasin.  Rift-related immature conglomerates and sandstones. See also p1027 Tb. 1, p1031.||||||07-NOV-08
1621|Bigie Formation|63109|6|Mentioned|p1112, p1108 Fig. 3|||Overlain by Fiery Creek Volcanics and upper Peters Creek Volcanics. Geological Province: Calvert Superbasin. Consists of sandstone.||||||30-SEP-08
1621|Bigie Formation|63111|5|Briefly described|p1162, p1163 Fig. 3, p1164 Tb. 1|Statherian|Statherian|Overlian by Fiery Creek Volcanics, underlian by Quilalar Formation. Thickness: ~500m.  Geological Province: Calvert Superbasin. Coarse- to medium-grained, poorly sorted pebble to cobblestone conglomerates and sandstone.||||||07-FEB-11
1621|Bigie Formation|63113|6|Mentioned|p1225 Fig.13. |||Calvert Superbasin. Part of Big supersequence.||Of the Myally Subgroup||Overlies ?unconformably Quilalar Formation. Is overlain by Fiery Creek Formation.||
1621|Bigie Formation|63114|5|Briefly described|p1253 Fig.2. |||Calvert superbasin.||Of the Big supersequence||Overlies Quilalar Formation. Is overlain by Fiery Creek Volcanics.||
1621|Bigie Formation|63115|6|Mentioned|1279 Fig.4, p1281-1283, p1290.|||Calvert superbasin. High-permeability aquifer.||||||
1621|Bigie Formation|63116|6|Mentioned|p1297 Fig.2, p1299-1303, p1305-1309 |||Calvert superbasin. Material properties detailed. Aquifer.||||||
1621|Bigie Formation|63593|5|Briefly described|p288 Fig.2, p291 Fig.3 and Tb.2.|||Western Fold Belt. |Between c.1700 and 1670 Ma.||||Sandstone, conglomerate.|
1621|Bigie Formation|63866|5|Briefly described|p57-p58|Statherian|Statherian|Calvert Superbasin.|1709 +/- 3 Ma (Page and Sweet, 1998)|||(Possibly) coeval with the Fiery Creek Volcanics. Overlain by the Surprise Creek Formation, Warrina Park Quartzite, Torpedo Creek Quartzite and the Gunpowder Creek Formation.||
1621|Bigie Formation|64250|6|Mentioned|p11 fig 3, p16 fig.6, p19|||Western Fold Belt, Mount Isa Inlier. <1762 +/- 18 Ma.|c.1710 Ma.||||Sandstone and conglomerate.|
1621|Bigie Formation|64725|6|Mentioned|p58 Fig.2. |||Mount Isa Inlier.||||||
1621|Bigie Formation|64726|6|Mentioned|p83 Fig.2.|||||||||
1621|Bigie Formation|64744|6|Mentioned|p353 Fig.4. |Statherian|Statherian|Mount Isa Basin.||||||
1621|Bigie Formation|64834|5|Briefly described|p13 Fig.2|||Calvert Superbasin. Western Succession of Mount Isa Basin.||||Uncomformable base.|Conglomerate, with cobble bed near base.|
1621|Bigie Formation|65228|5|Briefly described|p21, Figs.04, 10.|Statherian|Statherian|Part of the Big Supersequence.|c.1720 Ma.|||Is overlain unconformably by Surprise Creek Formation.||12-APR-18
1621|Bigie Formation|65337|6|Mentioned|p5. |||Calvert Superbasin.||||||
1621|Bigie Formation|65396|5|Briefly described|p82, p175, p187, p241|Statherian|Statherian|Calvert Superbasin. Cover Sequence 2. Lawn Hill Platform, Leichhardt River Fault Trough, Kalkadoon-Leichhardt Belt.|c.1710 Ma.|||Overlain by Fiery Creek Volcanics.|Quartzite/sandstone and conglomerate with some mafic volcanics.|
1621|Bigie Formation|66824|6|Mentioned|p148|||||||Is overlain by Fiery Creek Volcanics. With Fiery Creek Volcanics, equivalent to Carter's Bore Rhyolite.||
1621|Bigie Formation|67323|4|Described|p8, p11, p13, p25, p33, p39, p107|Paleoproterozoic|Paleoproterozoic|See also GIS attrib tbl, Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Calvert Superbasin. Leichhardt River Domain, Mount Oxide Domain, Mount Isa Inlier. Fluvial deposits. Maximum depositional age of 1762 +/- 18 Ma said to be clearly much older than depositional age. |~1720-1710 Ma.|Of Big Supersequence||Unconformably overlies Quilalar Formation. Underlies Fiery Creek Volcanics.|Purple - brown hematitic labile sandstone, pebbly sandstone, tuff, conglomerate, red - brown siltstone.|
1621|Bigie Formation|68021|5|Briefly described|p135 fig 4, p136|Statherian|Statherian|Part of Big Supersequence, Calvert Superbasin, Western Succession. Follows major regional unconformity. Deposition in fault-angle depressions and fluviatile environments.||||Unconformably overlies Quilalar Formation, overlain by Fiery Creek Volcanics, intruded by Weberra Granite.|Fanglomerates and coarse sandstones.|
1621|Bigie Formation|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province. This unit is mapped with the Fiery Creek Volcanics under the symbol, -Pf.||||||
1621|Bigie Formation|68732|5|Briefly described|p161, p165 Fig.3, p166|Statherian|Statherian|Of the Big Supersequence. Detritus sourced from nearby Gin Granite. Maximum sedimentary depositional age.|1762 +/- 18, 1764 +/- 13, 1783 +/- 5 Ma||||Alluvial fan conglomerates and fluvial sandstones.|30-NOV-17
1621|Bigie Formation|69056|6|Mentioned|p2|||Mapped as one unit with Fiery Creek Volcanics.||||||
1621|Bigie Formation|69222|5|Briefly described|p221, p222 Fig.2|Statherian|Statherian|Western Fold Belt. Associated with the c. 1708 Ma Mount Isa Rift Event.||||Overlies Quilalar Formation, overlain by Carters Bore Rhyolite||09-FEB-18
1621|Bigie Formation|69370|6|Mentioned|p307 Fig.2|Statherian|Statherian|Western Fold Belt, Mount Isa Block.||||Intertongues with Fiery Creek Volcanics. Is overlain by Surprise Creek Formation.||25-JAN-19
1621|Bigie Formation|69591|5|Briefly described|p29, p37-40, p56, p106|Paleoproterozoic|Paleoproterozoic|Mount Oxide, Leichhardt River Domains, Calvert Superbasin. Part of the Big Supersequence. Fluvial/delta fan deposits.|1762 +/- 18 Ma (MDA: Neumann et al., 2006).|||Overlies Peters Creek Volcanics.|Mostly cobble conglomerate and sandstone. Purple-brown hematitic labile sandstone, pebbly sandstone, tuff, conglomerate, red-brown siltstone.|
1621|Bigie Formation|70282|5|Briefly described|p544 Tb.1|||Cover sequence 3, Mount Isa.|1710-1709 Ma|||Overlain by Fiery Creek Volcanics|Conglomerate and sandstone.|13-FEB-18
1621|Bigie Formation|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Three facies are mapped separately.|||||Purple-brown hematitic labile sandstone, pebbly sandstone, tuff, conglomerate and red-brown siltstone.|
1621|Bigie Formation|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Three facies are mapped separately.|||||Purple-brown hematitic labile sandstone, pebbly sandstone, tuff, conglomerate and red-brown siltstone.|
1621|Bigie Formation|71592|5|Briefly described|Appendix A.|||Kalkadoon-Leichhardt Domain, Mount Isa Orogen.|1796+/-6 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
1621|Bigie Formation|71606|5|Briefly described|p137|Statherian|Statherian|Lawn Hill Platform and Leichardt River Fault Trough, Mount Isa Inlier.||||Overlain by Weberer Granite and Fiery Creek Volcanics.||
1621|Bigie Formation|71799|5|Briefly described|p150 fig 2|Statherian|Statherian|Lawn Hill.|ca. 1725 Ma|||Overlain by the Fiery Creek Volcanics.|Red beds.|
1621|Bigie Formation|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown, with Fiery Creek Volcanics, as located in the Leichhardt River Fault Trough and the Kalkadoon-Leichhardt Belt of the Mount Isa Province. Unclear whether this unit or Fiery Creek Volcanics was dated. Age given as U-Pb zircon igneous crystallisation age.|1709 +/-3 Ma|||Shown as overlying Carrara Range Group and shown as unconformably underlying Surprise Creek Formation.||
1621|Bigie Formation|72889|6|Mentioned|p6 Fig.i.|||||||||
1621|Bigie Formation|72912|5|Briefly described|p5 Fig.3, p13.|Statherian|Statherian|Of Calvert Superbasin. Shown with Fiery Creek Volcanics. Lateral equivalents? Located in the Leichhardt River Fault Trough, Kalkadoon-Leichhardt Belt and the Lawn Hill Platform of the Mount Isa Province, and the East part of the South Nicholson Basin. U-Pb zircon igneous crystallisation age (Ma) shown.|1709+/-3 Ma|Big Supersequence||Shown as unconformably underlying Surprise Creek Formation and overlying Carrara Range Group, Quilalar Formation.|High energy clastic sediments.|
1621|Bigie Formation|73042|6|Mentioned|p4|Statherian|Statherian|Written as Fiery Creek Vol/Bigie Fm on chronostratigraphic diagram (Fig.1.2). South Nicholson Basin region and Mount Isa Province, Calvert Superbasin. Geochronology is a U-Pb zircon igneous crystallisation age (although it is unclear whether this age is from the Fiery Creek Volcanics or Bigie Formation(?), or if these two units can be distinguished from one another).|1709 +/- 3 Ma (see comments and Fig.1.2)|||Unconformably overlain(?) by Surprise Creek Formation. Equivalent to Fiery Creek Volcanics(?).||
1621|Bigie Formation|73137|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|||||||
1621|Bigie Formation|73144|6|Mentioned|p9-10|||Calvert Superbasin. Part of the Big Supersequence.||||Partly interbedded with Fiery Creek Volcanics.||
1621|Bigie Formation|73525|5|Briefly described|p4, p19 Fig.13|Statherian|Statherian|Mount Oxide-(Ardmore-May Downs) and Leichhardt River Domain.|1762+/-18 Ma maximum depositional age||||Medium-fine sandstone clastics.|
1637|Billicumidji Rhyolite Member|23065|5|Briefly described|15|||||||||
1637|Billicumidji Rhyolite Member|23398|5|Briefly described|p433|Orosirian|Orosirian|Of Cliffdale Volcanics. Age: 1851+/-3Ma.||||||25-JUL-06
1637|Billicumidji Rhyolite Member|24197|5|Briefly described|p22|||Of the Cliffdale Volcanics (Nicholson Suite). Geological province: Murphy Inlier.||||||07-FEB-11
1637|Billicumidji Rhyolite Member|35640|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
1637|Billicumidji Rhyolite Member|36012|3|Fully described|Table 1|||See also p8.||||||25-JUL-06
1637|Billicumidji Rhyolite Member|36217|6|Mentioned|p206|||Published by Grimes & others 1979. Definition approved by Qld SNC.||||||
1637|Billicumidji Rhyolite Member|36439|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
1637|Billicumidji Rhyolite Member|36442|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
1637|Billicumidji Rhyolite Member|38584|4|Described|p9|||||||||
1637|Billicumidji Rhyolite Member|41721|5|Briefly described|p7|||Within the upper sequence of the Cliffdale Volcanics. Flow-banded alkali rhyolite and minor tuff. Geological Province: Muprhy Inlier.||||||06-AUG-08
1637|Billicumidji Rhyolite Member|45166|5|Briefly described|p71|||||||||
1637|Billicumidji Rhyolite Member|49001|2|Defined|p4|Carpentarian|Carpentarian|||||||
1637|Billicumidji Rhyolite Member|50536|5|Briefly described|p3.1|Paleoproterozoic|Paleoproterozoic|Of the Cliffdale Volcanics.||||||07-NOV-08
1637|Billicumidji Rhyolite Member|67323|5|Briefly described|GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|Post-Barramundi basement||Cliffdale Volcanics|||Flow-banded and massive rhyolite lava and minor tuff|
1637|Billicumidji Rhyolite Member|70849|5|Briefly described|Map legend.|Orosirian|Orosirian|Murphy Province.||Cliffdale Volcanics.||Is overlain unconformably by Westmoreland Conglomerate (Tawallah Group). Is intruded by Nicholson Granite Complex.|Alkali rhyolite lava, red, flow-banded, with numerous ashfall tuff horizons.|
1637|Billicumidji Rhyolite Member|72919|4|Described|p11|Orosirian|Orosirian|[Also written as Billicumidji Rhyolite]. Murphy Province. Approximately 2000 m thick. A SHRIMP U-Pb zircon age of 1851 +/- 3 Ma was reported by Page et al. (2000).|1851 +/- 3 Ma U-Pb SHRIMP|Cliffdale Volcanics|||Flow-banded porphyritic alkali rhyolite, tuff beds and several minor pyroclastic flow deposits.|
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.|
1722|Birdum Creek beds|36335|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
1722|Birdum Creek beds|45148|6|Mentioned|Fig.5|||Formerly part of Winnecke Creek Tableland formation.||||||
1722|Birdum Creek beds|61155|5|Briefly described|p16|Middle Miocene|Middle Miocene|Age: >9Ma. Max. thickness: 20m. Geological Province: overlies Ord and Wiso Basins.||||||14-SEP-18
1722|Birdum Creek beds|65239|5|Briefly described|p3 Fig. 4|Tertiary|Tertiary|Geological province: overlies Wiso Basin. Continental in origin.||||||14-SEP-18
1722|Birdum Creek beds|65345|6|Mentioned|p7 Fig.6. |Cenozoic|Cenozoic|||||Overlies Campfield beds.||
1722|Birdum Creek beds|69458|5|Briefly described|p42:21|Neogene|Paleogene|Randal (1969). North of the Wiso Basin. Over 15m thick. Crops out as low scattered boulders on grassy plains. Contains at least two genera of freshwater gastropods.||||Probable equivalent of Camfield beds.|Hard, white, nodular fossiliferous limestone, soft chalky limestone, with locally developed opaline nodules, intervals of chalcedony and layers with abundant quartz sand.|14-SEP-18
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|||||||||
1807|Black Point Sandstone Member|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Bullo River Sandstone.  Reddish brown feldspathic quartz sandstone, minor conglomerate.||||||02-DEC-04
1807|Black Point Sandstone Member|32701|4|Described|Table 1|||Adelaidean||||||
1807|Black Point Sandstone Member|45112|4|Described|p34|||||||||
1807|Black Point Sandstone Member|48938|2|Defined|p56|Proterozoic|Proterozoic|?Adelaidean.||||||
1807|Black Point Sandstone Member|60006|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Wolfe Creek Basin. Of Bullo River Sandstone, Duerdin Group. Unconformably overlies Shoal Reach Formation and Spencer Sandstone. Unconformably overlain by Bucket Spring Member and Moonlight Valley Tillite.||||||22-JUL-04
1807|Black Point Sandstone Member|60682|4|Described|p17, 18|Neoproterozoic|Neoproterozoic|At base of Bullo River Sandstone. Thickness: 45-60m. Feldspathic and quartz sandstone, minor conglomerate. Geological Province: Wolfe Creek Basin.||||||
1807|Black Point Sandstone Member|65331|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of Bullo River Sandstone, Duerdin Group, Wolfe Creek Basin. Feldspathic and quartzose sandstone, minor conglomerate||||||02-FEB-10
1807|Black Point Sandstone Member|68733|5|Briefly described|p177 Fig.2, p179-189, p191, p193|Cryogenian|Cryogenian|Sweet and Pontifex (1972). Victoria and Wolfe Basins. Appears as Black Point Member Sandstone in Tb.1. Sm-Nd isotope data tabulated. Detritus sourced from Musgrave Province discussed.|Maximum depositional age of ca. 1018 +/- 13 Ma.|Basal subunit of the Bullo River Sandstone.||Unconformably underlain by the Shoal Reach Formation.|Consists of feldspathic sandstone and minor conglomerate.|05-DEC-17
1807|Black Point Sandstone Member|69442|5|Briefly described|p27:2, 3 Tb.27.1|||Wolfe Basin. 45-70m thick. Distinctive photo-pattern. Depositional environment not determined; possibly fluvial. Maximum depositional age from detrital zircons.|<1018 +/- 13 Ma (Carson, 2010).|Basal Bullo River Sandstone.|||Feldspathic and quartz sandstone, minor conglomerate lenses of pebbles (rare cobbles).|12-JUL-16
1807|Black Point Sandstone Member|69673|5|Briefly described|p190|||||Bullo River Sandstone|||Feldspathic sandstone.|
1807|Black Point Sandstone Member|70206|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Wolfe Basin. ||Bullo River Sandstone|||Feldspathic and quartzose sandstone, minor conglomerate.|
1807|Black Point Sandstone Member|71080|6|Mentioned|p25|||Of Victoria Basin. Higher stratigraphic level than Jasper Gorge Formation. Contains a significant component of late Mesoproterozoic detrital zircons.||Of Bullo River Sandstone.||||
1807|Black Point Sandstone Member|71302|5|Briefly described|p6,73-74|Neoproterozoic|Neoproterozoic|Of Wolfe Basin. Maximum depositional age: 1018+\-13 Ma (Carson, 2013; Munson, 2016 and Munson, in prep).||Unit of Duerdin Group.||Underlain unconformably by Shoal Reach Formation.||
1807|Black Point Sandstone Member|71592|5|Briefly described|Appendix A.|||Victoria River Region.|1018+/-13 Ma (MDA: Pb/Pb zircon).||||Sandstone.|
1843|Black Stump Arkose|8187|5|Briefly described|Map legend|Adelaidean|Adelaidean|Arkose, pebbly arkose, siltstone, shale.  Overlies Yardida Tillite; underlies Thorntonia Limestone.||||||21-JUN-04
1843|Black Stump Arkose|8217|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Arkose, pebbly arkose, siltstone, shale. Overlies: Yardida Tillite. Underlies: Wonnadinna Dolomite.||||||28-OCT-04
1843|Black Stump Arkose|22646|6|Mentioned|Fig 4 on p 102|||Georgina Basin.||||||
1843|Black Stump Arkose|24442|5|Briefly described|p49|Marinoan|Marinoan|Geological Province: Georgina Basin.||||||
1843|Black Stump Arkose|35798|6|Mentioned|Fig.1|||Geological map of Desert Syncline.||||||
1843|Black Stump Arkose|35863|6|Mentioned|Table 1|||||||||
1843|Black Stump Arkose|37928|6|Mentioned|Fig.4|||||||||
1843|Black Stump Arkose|37929|5|Briefly described|p526|||||||||
1843|Black Stump Arkose|37930|6|Mentioned|p528|||||||||
1843|Black Stump Arkose|38157|6|Mentioned|Table IX|||||||||
1843|Black Stump Arkose|39921|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
1843|Black Stump Arkose|40906|6|Mentioned|Fig.9|||||||||
1843|Black Stump Arkose|41405|6|Mentioned|p205|||||||||
1843|Black Stump Arkose|41801|6|Mentioned|Fig.4|||||||||
1843|Black Stump Arkose|45155|6|Mentioned|p28|||Correlation||||||
1843|Black Stump Arkose|46903|6|Mentioned|Fig.5|||Correlation chart||||||
1843|Black Stump Arkose|46959|6|Mentioned|p207|||||||||
1843|Black Stump Arkose|48990|2|Defined|p8|Adelaidean|Adelaidean|Formerly part of Field River Beds (Smith,1963) which have now been superseded.||||||25-JUL-06
1843|Black Stump Arkose|49027|5|Briefly described|p2|||||||||
1843|Black Stump Arkose|60122|4|Described|p4-5, p11 Tb. 1|Neoproterozoic|Neoproterozoic|Of Keepera Group. Red-brown to purple brown micaceous, fine to very coarse (to pebbly) arkose, sst and laminated micaceous mudst. Disconformably overlies Yardida Tillite; conformably underlies Wonnadinna Dolostone. Max. thick: >700m in type section.||||||
1843|Black Stump Arkose|60590|5|Briefly described|Map legend|Cryogenian|Cryogenian|Of the Keepera Group.  Micaceous (to pebbly) arkose, sandstone, micaceous mudstone.||||||23-DEC-09
1843|Black Stump Arkose|61404|5|Briefly described|Map legend|Cryogenian|Cryogenian|Of the Keepera Group.  Micaceous (to pebbly) arkose, sandstone, micaceous mudstone.  Geological Province: southern Georgina Basin.||||||
1843|Black Stump Arkose|63450|5|Briefly described|p78 Fig. 5|Neoproterozoic|Neoproterozoic|Together with Wonnadinna Dolomite overlies Yardida Tillite disconformably; grades up into Wonnadinna Dolomite. Geol.prov: Georgina Basin, West Toko Syncline. Coarse-grained arkose, sandstone and micaceous mudstone interpreted as glacial outwash deposits.||||||07-FEB-11
1843|Black Stump Arkose|63562|6|Mentioned|p344|||Of Georgina Basin.||||||
1843|Black Stump Arkose|64068|3|Fully described| p46, p viii, p18-19, p36|Cryogenian||Basal glacial outwash. Fairly high radiometric values from feldspathic and clay-rich sediments. Correlated with Sun Hill Arkose, Oorabra Arkose, Boko Formation, Olympic Formation, Pioneer Sandstone, Mount Doreen Formation.||Of Keepera Group.||Disconformable over Yardida Tillite. Conformable and gradational under Wonnadinna Dolostone.|Red-brown to purple-brown micaceous, fine to very coarse arkose, sandstone, laminated micaceous mudstone and siltstone.|18-JAN-16
1843|Black Stump Arkose|64778|6|Mentioned|p13|Neoproterozoic|Neoproterozoic|Toko Syncline, Southern Georgina Basin.||||||
1843|Black Stump Arkose|65338|6|Mentioned|p60.|||||Unit in Keepera Group.||||
1843|Black Stump Arkose|67323|5|Briefly described|GIS attrib tbl|Neoproterozoic|Neoproterozoic|Centralian Superbasin.|||||Feldspathic sandstone (locally pebbly), siltstone and shale.|
1843|Black Stump Arkose|68270|4|Described|p681-683,688|Cryogenian|Cryogenian|Southern Georgina Basin. Composite section: N flank Field River Anticline N of drillhole Hay River 7 (lat. 23'6'15"N, long. 137'51'18"E). Less than 700m thick. Proximal glacial outwash deposit related to Elatina glaciation. Correlative to Elatina Formation. Laterally equivalent to Sun Hill Arkose and Oorabra Arkose.||||Overlain by Wonnadinna Dolostone (paraconformity). Underlain disconformably by Yardida Tillite.|Poorly sorted, medium- to coarse-grained and pebbly arkose, with interbedded sandstone, laminated micaceous siltstone and shale and conglomerate.|03-JUL-19
1843|Black Stump Arkose|68553|6|Mentioned|Map legend; schematic diagram.|Early Paleozoic|Neoproterozoic|Georgina Basin. This unit, as well as Gnallan-a-gea and Sun Hill Arkoses, Little Burke and Yardida Tillites, are all mapped under the symbol, -P-Cg.||||||
1843|Black Stump Arkose|69437|5|Briefly described|p22:4-5, 7|Cryogenian|Cryogenian|SE Georgina Basin, Centralian A Superbasin. Supersequence 3.||Keepera Group.||Is overlain by Wonnadinna Dolostone.||12-JUL-16
1843|Black Stump Arkose|69438|6|Mentioned|p23:17|||Georgina Basin.||||Correlated with the Olympic Formation (Amadeus Basin).||12-JUL-16
1843|Black Stump Arkose|69443|4|Described|p28:7-9, 33; 28:38 Fig.28.36|Cryogenian|Cryogenian|Walter (1980). Georgina Basin. Over 700m thick. Proximal glacial outwash deposit. Exposed by Tarlton and Toomba Faults.||Keepera Group.||Disconformably overlies Yardida Tillite. Is overlain conformably and gradationally by Wonnadinna Dolostone.|Micaceous, fine to very coarse (to pebbly) arkose, sandstone, laminated micaceous mudstone and siltstone.|12-JUL-16
1843|Black Stump Arkose|69591|5|Briefly described|p94|||Toko Syncline. Up to 700m thick.||||Disconformably overlies Yardida Tillite. Is overlain disconformably by Gnallan-A-Gea Arkose.||
1843|Black Stump Arkose|69673|5|Briefly described|p114 fig 92, p115|Cryogenian|Cryogenian|More than 700m thick.||Keepera Group|||Arkose, sandstone, laminated micaceous mudstone and siltstone.|
1843|Black Stump Arkose|72516|6|Mentioned|p87|Ediacaran|Ediacaran|Georgina Basin. Age from equivalence with Oorabra Arkose.||||Equivalent to the Oorabra Arkose.||02-JUN-21
1843|Black Stump Arkose|73086|6|Mentioned|p101, p167|||Georgina Basin.||||Correlates to Olympic Formation.||
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|
1896|Blanche Creek Member|23410|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Hayward Creek Formation (Tomkinson Creek Subgroup, Churchills Head Group). Polymictic orthoconglomerate, in local channels.||||||07-NOV-08
1896|Blanche Creek Member|23733|6|Mentioned|p9, 10|||||||||
1896|Blanche Creek Member|23809|6|Mentioned|p27 Fig. 25|||Geological Province: Tennant Inlier.||||||
1896|Blanche Creek Member|24172|5|Briefly described|p25|Paleoproterozoic|Paleoproterozoic|Of Hayward Creek Formation.||||||07-NOV-08
1896|Blanche Creek Member|32174|6|Mentioned|Map legend|Carpentarian|Paleoproterozoic|Early Proterozoic or Carpentarian||||||07-NOV-08
1896|Blanche Creek Member|33307|6|Mentioned|Fig.8|||||||||
1896|Blanche Creek Member|35771|2|Defined|p23|early Carpentarian|early Carpentarian|Appendix.||||||
1896|Blanche Creek Member|39213|6|Mentioned|Fig.8|||||||||
1896|Blanche Creek Member|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Hayward Creek Formation (Tomkinson Creek Group). Polymictic orthoconglomerate. Underlies the Manga Mauda Member. In the Tennant Creek region.||||||07-NOV-08
1896|Blanche Creek Member|65209|5|Briefly described|p35 Fig.1, p37, p38|Paleoproterozoic|Paleoproterozoic|Geol. Prov: Tomkinson Creek Province. Likely Warramunga Formation/Ooradidgee Group provenance of Blanche Creek Member clasts.||Hayward Creek Formation.||Correlated with Rising Sun Conglomerate.|Conglomeratic.|05-JAN-17
1896|Blanche Creek Member|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Hayward Creek Formation.|||Polymictic orthoconglomerate.|
1896|Blanche Creek Member|69424|6|Mentioned|p9:26-27|Paleoproterozoic|Paleoproterozoic|||Hayward Creek Formation.||||12-JUL-16
1896|Blanche Creek Member|69425|6|Mentioned|p10:13|||||Hayward Creek Formation.||Correlated in part with Unimbra Sandstone.||12-JUL-16
1896|Blanche Creek Member|69431|4|Described|p16:3, 4-5, 7|Paleoproterozoic|Paleoproterozoic|Dodson and Gardener (1978). Tomkinson Province. c.150m thick. Fluviatile deposits.||Basal Hayward Creek Formation.||Lateral facies relationship with Manga Mauda Member. Overlies Ooradidgee Group unconformably. Possible correlate of Rising Sun Conglomerate.|Widespread but localised, poorly sorted lithic sandstone and polymictic conglomerate.|12-JUL-16
1931|Blatherskite Quartzite Member|35102|6|Mentioned|p27|||||||||
1931|Blatherskite Quartzite Member|43503|6|Mentioned|29|||||||||
1931|Blatherskite Quartzite Member|48992|2|Defined|p26|Neoproterozoic|Neoproterozoic|||||||
1931|Blatherskite Quartzite Member|73086|3|Fully described|p7, p9, p144|||Amadeus Basin. Of Stewart et al (1980). Type area: Heavitree Gap (possibly 28 m thick[?]). Widespread, occurring along the entire northern margin of the basin. Lithologically most typical of the Heavitree Formation.||Heavitree Formation|||Silicified, very fine- to medium-grained, well sorted sandstone.|
1937|Blazan Shale|22954|6|Mentioned|Fig3p9|Undillan|Early Cambrian|||||||
1937|Blazan Shale|24419|5|Briefly described|p18|Late Cambrian|Middle Cambrian|Interfingers with Quita Formation.  Siltstone, shale, thin-bedded chert, fine-grained sandstone and rare beds of bituminous limestone.  Geological Province: Georgina Basin.||||||08-MAR-05
1937|Blazan Shale|30242|6|Mentioned|Fig.2|||||||||
1937|Blazan Shale|30479|6|Mentioned|p19|||See also Fig.3. Name should be dropped||||||
1937|Blazan Shale|30914|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
1937|Blazan Shale|33482|6|Mentioned|p6|||Equiv. Inca Formation||||||
1937|Blazan Shale|34287|6|Mentioned|Fig.3|||||||||
1937|Blazan Shale|35054|6|Mentioned|Table 23|||||||||
1937|Blazan Shale|35121|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
1937|Blazan Shale|35139|4|Described|Table.2|||||||||
1937|Blazan Shale|35553|6|Mentioned|p180|||Appendix containing description of Agnostid localities.||||||
1937|Blazan Shale|36234|6|Mentioned|p168|||||||||
1937|Blazan Shale|37572|4|Described|p158|||See also Fig.8||||||
1937|Blazan Shale|38442|5|Briefly described|Map legend|Cambrian|Cambrian|||||||25-AUG-04
1937|Blazan Shale|38446|6|Mentioned|Table 23|||||||||
1937|Blazan Shale|38608|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
1937|Blazan Shale|39445|5|Briefly described|Table 4|||See also p62||||||25-JUL-06
1937|Blazan Shale|39690|6|Mentioned|Table 1|||||||||
1937|Blazan Shale|40856|5|Briefly described|p315|||||||||
1937|Blazan Shale|43105|5|Briefly described|Fig.4,p9.|||||||||
1937|Blazan Shale|44211|4|Described|p100,102|||See also Lexicon.||||||
1937|Blazan Shale|44273|14|Not recorded|Map Legend||Middle Cambrian|||||||
1937|Blazan Shale|44275|14|Not recorded|Map Legend|||||||||
1937|Blazan Shale|44920|14|Not recorded|Map Legend, Sheet 4||Middle Cambrian|||||||
1937|Blazan Shale|45052|3|Fully described|p100|||M.Camb.||||||
1937|Blazan Shale|45079|5|Briefly described|p30|||Cambrian age||||||
1937|Blazan Shale|47058|6|Mentioned|p134|||||||||
1937|Blazan Shale|49027|5|Briefly described|p7|||||||||
1937|Blazan Shale|60122|6|Mentioned|p57 Appendix|||Correlated with parts of Arthur Creek Formation. Geological Province: eastern Georgina Basin||||||11-MAY-05
1937|Blazan Shale|60359|5|Briefly described|Map Legend|Cambrian|Cambrian|Shaly siltstone.||||||
1937|Blazan Shale|63450|5|Briefly described|p78 Fig. 5, p81|Middle Cambrian|Middle Cambrian|Overlain by Georgina Limestone. Geological province: Georgina Basin, East Toko Syncline.||||||07-FEB-11
1937|Blazan Shale|64068|4|Described|p63, 62, 64, 69|Middle Cambrian|Middle Cambrian|Contains agnostine trilobites, brachiopods. Correlated with Arthur Creek Formation, Inca Formation, Roaring Siltstone, Devoncourt Limestone.||Of Narpa Group.||Disconformably overlies Beetle Creek Formation or Thorntonia Limestone. Conformably overlain by, and interdigitates with, Quita Formation.|Interbedded siliceous shale and sandstone; basal conglomerate.|05-APR-12
1937|Blazan Shale|64443|6|Mentioned|p40.|||||||Correlative of Wonarah Formation.||14-MAY-14
1937|Blazan Shale|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Middle Cambrian|Middle Cambrian|Georgina Basin||Narpa Group|||Siliceous shale, chert, siltstone, fine arenite, conglomerate, dolomitic and bituminous limestone, phosphorite|
1937|Blazan Shale|67352|6|Mentioned|p69|||||||||
1937|Blazan Shale|67870|6|Mentioned|p43|Middle Cambrian|Middle Cambrian|Georgina Basin.||||||
1937|Blazan Shale|69443|5|Briefly described|p28:16, 22-23|Middle Cambrian|Middle Cambrian|Georgina Basin.||Narpa Group.||Correlated with Anthony Lagoon, Wonarah Formations.||12-JUL-16
1937|Blazan Shale|69591|5|Briefly described|p87, p90-91, p96, p98 Fig.2.91|Cambrian|Cambrian|Oban Sub-basin, Georgina Basin. 39-60m thick. Contains trilobite fossils. Is lithologically identical with the Inca Formation.||||Unconformably overlies Beetle Creek Formation; disconformably overlies Thorntonia Limestone. Is overlain disconformably by Quita Formation.|Siliceous shale with interbeds of sandstone and conglomerate near the base.|
1937|Blazan Shale|70723|5|Briefly described|p24 Fig. 2|Cambrian|Cambrian|Georgina Basin.||Narpa Group||Overlies Thorntonia Limestone. Overlain by Quita Formation.|Shale and siltstone.|
1937|Blazan Shale|72321|6|Mentioned|Fig 2|Drumian|Drumian|Toko Syncline, Georgina Basin. Australian stages: Floran to Undillan.||of Narpa Group.||||
1937|Blazan Shale|72516|6|Mentioned|p92|Cambrian|Cambrian|Eastern Georgina Basin.||||Equivalent to the Arthur Creek Formation.||03-JUN-21
1937|Blazan Shale|73418|6|Mentioned|p3|||||Narpa Group||Lateral equivalent of Inca Formation||
1963|Bloodwood Formation|24064|4|Described|p226|Cambrian|Cambrian|Geological Province: Ngalia Basin. Maximum thicknes: >200m.||||||
1963|Bloodwood Formation|30258|6|Mentioned|Fig.2|||Cambrian age||||||
1963|Bloodwood Formation|31454|6|Mentioned|Fig.2|||||||||
1963|Bloodwood Formation|33757|3|Fully described|p9|||See also Table 2||||||
1963|Bloodwood Formation|33760|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
1963|Bloodwood Formation|33761|6|Mentioned|p145|||Cambrian||||||
1963|Bloodwood Formation|36473|6|Mentioned|Map legend|Ordovician|Adelaidean|Adelaidean to Ordovician||||||
1963|Bloodwood Formation|37537|5|Briefly described|Map legend|Cambrian|Cambrian|Red-brown, micaceous siltstone; red sandstone. Marine macrofossils. Geological Province: Ngalia Basin.||||||14-FEB-06
1963|Bloodwood Formation|40906|6|Mentioned|Fig.11|||||||||
1963|Bloodwood Formation|41717|6|Mentioned|Fig.19|||||||||
1963|Bloodwood Formation|42059|5|Briefly described|Fig.2|||See also P133||||||
1963|Bloodwood Formation|42504|5|Briefly described|Table 54 P79|||||||||
1963|Bloodwood Formation|43275|5|Briefly described|Map Legend||Cambrian|||||||
1963|Bloodwood Formation|43749|6|Mentioned|Fig.1,p6||Cambrian|||||||
1963|Bloodwood Formation|44158|4|Described|p33 Table.2|Cambrian|Cambrian|of Ngalia Basin.||||||
1963|Bloodwood Formation|45155|2|Defined|p33|Middle Cambrian|Early Cambrian|Late Early or Early Middle Cambrian||||||
1963|Bloodwood Formation|61385|5|Briefly described|Map legend|Cambrian|Cambrian|Red-brown mudstone and minor sandstone; sparsely fossiliferous.   Geological Province: Ngalia Basin.||||||
1963|Bloodwood Formation|64068|6|Mentioned|p225|||Ngalia Basin. Correlated with Narpa Group.||||||
1963|Bloodwood Formation|65232|5|Briefly described|p70|||Overlies Walbiri Dolostone. Mudstone and shale. Geol. Prov: Ngalia Basin.||||||18-FEB-10
1963|Bloodwood Formation|65329|5|Briefly described|Map legend|Palaeozoic|Palaeozoic|Of Ngalia Basin. Shown as younger than Walbiri Dolomite, older than Djagamara Formation. Red-brown mudstone and minor sandstone; sparsely fossiliferous||||||02-FEB-10
1963|Bloodwood Formation|65330|5|Briefly described|Map legend|Palaeozoic|Palaeozoic|Of Ngalia Basin. Shown as younger than Walbiri Dolomite, older than Djagamara Formation. Red-brown mudstone and minor sandstone; sparsely fossiliferous||||||02-FEB-10
1963|Bloodwood Formation|67565|6|Mentioned|p5 Fig.3.|||||||||04-DEC-15
1963|Bloodwood Formation|67872|5|Briefly described|p13, p15, p39|Cambrian|Cambrian|Ngalia Basin. Part of the M4 mega-sequence of Lindsay (2002).||||||
1963|Bloodwood Formation|69437|5|Briefly described|p22:10-11|Series 3|Series 3|Ngalia Basin, Centralian B Superbasin. Sequence 2. Shallow-marine, peritidal and subaerial deposits.|||||Mudstone and minor sandstone.|12-JUL-16
1963|Bloodwood Formation|69439|3|Fully described|p24:2-4, 9-10, 13-14, 18, 20-21|Cambrian|Cambrian|Ngalia Basin. Recessive unit. Estimated maximum thickness of 270m at the type section in the northern Walbiri Ranges. Fossils include sea pens, molluscs and trace fossils (Protichnites and Rusophycus). Shallow-marine to intertidal deposits, subaerial at times. Correlated with upper Giles Creek Dolostone, lower Hugh River Shale and Tempe Formation (Amadeus Basin), lower Arthur Creek Formation (Georgina Basin), and Point Wakefield beds (Wiso Basin). Contains potential reservoirs. Has potential for likely seals for Yuendumu Sandstone reservoirs.||||Conformably overlies Walbiri Dolostone. Is overlain unconformably by Mount Eclipse Sandstone and Djagamara Formation; is faulted against Djagamara Formation.|Dark red-brown, sparsely fossiliferous mudstone and minor, red-brown, fine-grained, sometimes micaceous thinly bedded sandstone. Some intraformational breccia occurs in the basal part.|12-JUL-16
1963|Bloodwood Formation|69673|4|Described|p107, p107 fig 85, p108|Cambrian|Cambrian |Up to 270m thick. Age derived from fossil fauna which also indicate the depositional environment to be shallow marine.||||Overlies Walbiri Dolostone, overlain by Djagamara Formation|Sparsely fossiliferous mudstone and minor thinly bedded sandstone.|
1981|Bludells Dolerite|23216|5|Briefly described|Table1p10,17|||||||||
1981|Bludells Dolerite|42756|6|Mentioned|Fig.5 P6|||||||||
1981|Bludells Dolerite|43149|5|Briefly described|Map legend||Paleoproterozoic|Of Orosirian age.||||||07-NOV-08
1981|Bludells Dolerite|43832|4|Described|35-36,Table8 p42, 45||Paleoproterozoic|Probably coeval with Cullen Batholith. Distinct from former "Bludells Monzonite" shown on map p34.||||||07-NOV-08
1981|Bludells Dolerite|60680|5|Briefly described|Map legend|Orosirian|Orosirian|Quartz dolerite and pyroxene-bearing monzonite rafts and xenoliths.||||||23-DEC-09
1981|Bludells Dolerite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Of Cullen Supersuite. Age 1840-1860Ma.  I-type. Quartz dolerite and pyroxene-bearing monzonite rafts and xenoliths. Remnants of dolerite in Cullen Batholith granites.||||||10-FEB-10
1981|Bludells Dolerite|67564|4|Described|p6 Table 2, p34, p38.|Paleoproterozoic|Paleoproterozoic|Previously mapped as Bludells Monzonite. Large (up to 1.5 km across) xenolithic rafts in Frances Creek Leucogranite (Cullen Supersuite); may represent country rock remnants within the pluton's roof zone.||||Intrudes Allamber Springs and Minglo Granites.|Altered quartz dolerite and fine- to medium-grained diorite; pyroxene-bearing monzonite, monzodiorite and quartz syenite.|
1981|Bludells Dolerite|69420|4|Described|p5:13-14|Paleoproterozoic|Paleoproterozoic|Formerly the Bludells Monzonite. Occurs as irregularly-shaped bodies up to 5km across within McCarthys Granite, Frances Creek Leucogranite and Allamber Springs Granite. Distinguished by high Ni and Cr, and much lower Ba and Sr. Probably coeval with Cullen Supersuite granites.||Cullen Supersuite.||Usually enclosed by Frances Creek Leucogranite.|Comprises clinopyroxene, orthopyroxene, olivine, biotite, opaques, plagioclase and minor quartz and K-feldspar; pyroxenes typically altered to actinolite.|12-JUL-16
1981|Bludells Dolerite|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.|||||Light grey-green, fine- to medium-grained quartz monzonite, monzodiorite and olivine dolerite; quartz syenite rafts and xenoliths.|
1990|Blue Hole Formation|14019|3|Fully described|p9-10|Paleoproterozoic|Paleoproterozoic|Of the Limbunya Group. Dolomitic mudstone, stromatolitic mudstone, dolostone, mudstone, siltstone. Conformably on Farquharson Sandstone; conformably overlain by Campbell Springs Dolostone. Age: 1636 +/- 5Ma. Max. thick: 330m. Geol. Prov: Birrindudu Basin.||||||07-NOV-08
1990|Blue Hole Formation|23809|5|Briefly described|p47 Tb. 6|Proterozoic|Proterozoic|See also Bluehole Formation.  Age: 1636+/-5Ma. Geological Province: Victoria-Birrindudu Basins.||||||17-MAR-05
1990|Blue Hole Formation|24122|5|Briefly described|p4 Fig.3|||Of Limbunya Group.  Geological Province: Birrindudu Basin.||||||
1990|Blue Hole Formation|24297|5|Briefly described|p4 Fig.3|Proterozoic|Proterozoic|Of Limbunya Group.  Geological Province: Birrindudu Basin.||||||
1990|Blue Hole Formation|24441|5|Briefly described|p1 Fig. 1|||Of the Limbunya Group. Overlies Farquharson Sandstone; overlain by Campbell Springs Dolostone. Geological Province: Birrindudu Basin.||||||
1990|Blue Hole Formation|24442|5|Briefly described|p50 Fig. 1|||Of the Limbunya Group.  Geological Province: Birrindudu Basin.||||||
1990|Blue Hole Formation|28255|3|Fully described|p21-22, Tb. 11 (opp. p8)|||Of Limbunya Gp. Predominanlty siltstone, silty dolomite, dolomite and dolarenite.  Conformably overlain by Black Springs Dolomite and conformably overlies Farquharson Sst.  Age os Adelaidean or Carpentarian. Max. thickness: 320m.  See also p123, p126-127.||||||07-JUN-05
1990|Blue Hole Formation|30003|4|Described|p9|||Of the Limbunya Group. Age is Carpentarian or Adelaidean. Max. thickness: 229m.||||||25-JUL-06
1990|Blue Hole Formation|30004|6|Mentioned|Map legend|Proterozoic|Proterozoic|Carpentarian or Adelaidean||||||
1990|Blue Hole Formation|32172|4|Described|Table 1|||Carpentarian or Adelaidean||||||
1990|Blue Hole Formation|32173|5|Briefly described|Map legend|Adelaidean|Carpentarian|Of the Limbunya Group.  Adelaidean or Carpentarian (per legend).  Pink, grey and purple silty dolomite, siltstone and dolomite, stromatolitic in places.  Conformably overlies the Farquharson Formation; conformably under the Campbell Springs Dolomite.||||||17-NOV-04
1990|Blue Hole Formation|32660|5|Briefly described|Table 6|||||||||
1990|Blue Hole Formation|33375|6|Mentioned|p9|||Dolomitic siltstone. Conformably overlies Farquharson Sandstone. Age is Carpentarian or Adelaidean.  Max. thickness: >100m.||||||27-APR-05
1990|Blue Hole Formation|33376|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
1990|Blue Hole Formation|33378|5|Briefly described|Map legend|||Dolomitic siltstone. Age is Carpentarian or Adelaidean.||||||27-APR-05
1990|Blue Hole Formation|45112|5|Briefly described|Table 7|||||||||
1990|Blue Hole Formation|48943|2|Defined|p25|Proterozoic|Proterozoic|Strat. section p132.||||||25-JUL-06
1990|Blue Hole Formation|60006|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Birrindudu Basin. Of Limbunya Group. Siltstone, silty dolostone.||||||07-NOV-08
1990|Blue Hole Formation|60589|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Limbunya Group.  Purple dolomitic mudstone, dololutite, stromatolitic dolostone and dolarenite, minor orange tuffite.  Conformably overlies the Farquharson Sandstone; conformably overlain by Campbell Springs Dolostone. Geol. Prov: Birrindudu Basin.||||||07-NOV-08
1990|Blue Hole Formation|60672|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Siltstone, silty dolostone, dolarenite, dolrudite. Of Limbunya Group. Overlain by Campbell Springs Dolostone. Overlies Farquharson Sandstone. Geological Province: Birrindudu Basin.||||||07-NOV-08
1990|Blue Hole Formation|60682|5|Briefly described|p7|Statherian|Statherian|Of Limbunya Group. Siltstone, silty dolostone, doloutite and dolarenite. Deposited in a low energy shallow marine environment. Conformably overlain by Campbell Springs Dolostone. Geological Province: Birrindudu Basin.||||||
1990|Blue Hole Formation|60685|5|Briefly described|p4 Fig. 3|||Of the Limbunya Group. Geological Province: Birrindudu Basin.||||||
1990|Blue Hole Formation|65331|5|Briefly described|Map legend|Palaeoproterozoic|Palaeoproterozoic|Of Limbunya Group, Birrindudu Basin.  Siltstone, silty dolostone ||||||
1990|Blue Hole Formation|65342|6|Mentioned|p11 Fig.13. |||Birrindudu Basin.||Unit in Limbunya Group.||Overlies Farquharson Sandstone. Is overlain by Campbell Springs Dolostone.||
1990|Blue Hole Formation|67151|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Birindudu Basin.||Unit in Limbunya Group.||Overlies Farquharson Sandstone. Is overlain by Campbell Springs Dolostone.|Dolomitic siltstone, siltstone.|
1990|Blue Hole Formation|68733|5|Briefly described|p177 Fig.2, p179 Tb.1, p184-186|Statherian|Statherian|Birrindudu Basin. Geochronology based on Sm-Nd whole rock analysis. Sm-Nd isotope data tabulated.|ca. 1640 Ma, tuff (Cutovinos et al. 2002)|Of the Limbunya Group.||||05-DEC-17
1990|Blue Hole Formation|69429|6|Mentioned|p14:2 Fig.14.2|Paleoproterozoic|Paleoproterozoic|||Limbunya Group.||||12-JUL-16
1990|Blue Hole Formation|69432|4|Described|p17:2, 7, 13|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin. Over 300m thick. Contains radiating clusters of botttom-nucleated acicular crystal pseudomorphs which are identical to Coxco Needles from the Teena Dolostone (McArthur Basin). Mostly quiescent shallow-marine deposits. Exploration target for base metals.|1636 +/- 5 Ma.|Limbunya Group.||Is overlain by Campbell Springs Dolostone.|Dolomitic mudstone, dolomitic mudstone and siltstone, biohermal stromatolitic dolostone, and dolomitic sandstone. Distinctive maroon-purple bioherms of digitate stromatolites, some several metres across, at the top.|12-JUL-16
1990|Blue Hole Formation|69673|6|Mentioned|p48 fig 35|||||Limbunya Group||Overlies Farquharson Sandstone, overlain by Campbell Springs Dolostone||
1990|Blue Hole Formation|70206|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Birindudu Basin [misspelling of Birrindudu Basin]. [Note: unit shown as Mesoproterozoic, but radiometric age date is Paleoproterozoic, suggesting it may be a 'maximum age of deposition'].|1636+/-5 Ma SHRIMP zircon|Limbunya Group|||Dolomitic mudstone, dololutite, stromatolitic dolostone and dolarenite, minor orange tuffite.|18-JUL-16
1990|Blue Hole Formation|70655|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Birindudu Basin.||Limbunya Group||Overlies Farquharson Sandstone. Is overlain by Campbell Springs Dolostone, or unconformably by Wickham Formation, Wattie Group.|Dolomitic siltstone, siltstone.|
1990|Blue Hole Formation|70854|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin. Maximum depositional age.|<1636 +/- 5 Ma (SHRIMP zircon age).|Limbunya Group.||Overlies Farquharson Sandstone. Is overlain by Campbell Springs Dolostone.|Siltstone, silty dolostone, dolarenite, dolorudite.|
1990|Blue Hole Formation|71302|5|Briefly described|p6,73|Paleoproterozoic|Paleoproterozoic|Of Birindudu Basin. Contains 1639+\-7 Ma tuffs (Fanning, 1991; Smith, 2001), proposed to have been sourced from reworking of upper Limbunya Group rocks (Smith 2001).||Unit of Limbunya Group.||Overlain by Campbell Springs Dolostone. Underlain by Farquharson Sandstone.||
1990|Blue Hole Formation|71374|5|Briefly described|p36|Statherian|Statherian||1636 +/- 5 Ma (SHRIMP U-Pb)|||Conformably overlies the Farquharson Sandstone.||
1990|Blue Hole Formation|72718|6|Mentioned|p7|Statherian|Statherian|Birrindudu Basin.|1636 +/- 5 Ma|Limbunyah Group||Underlain by Farquharson Sandstone. Overlain by Campbell Springs Dolostone.||
1990|Blue Hole Formation|73083|6|Mentioned|p31|||||||||
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.|
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|
2321|Border Waterhole Formation|23031|6|Mentioned|17|||Geological Province: Georgina Basin.||||||26-JUL-06
2321|Border Waterhole Formation|23393|5|Briefly described|p22|Middle Cambrian|Middle Cambrian|||||||
2321|Border Waterhole Formation|23448|4|Described|p480|Cambrian|Cambrian|||||||
2321|Border Waterhole Formation|24419|6|Mentioned|p18|||Equivalent to Beetle Creek Formation on URANDANGI 1:250 000 sheet.||||||
2321|Border Waterhole Formation|29940|6|Mentioned|p169|||||||||
2321|Border Waterhole Formation|30479|6|Mentioned|p15|||See also fig.3. Author suggests name should be dropped.||||||26-JUL-06
2321|Border Waterhole Formation|30914|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
2321|Border Waterhole Formation|31396|6|Mentioned|Fig.3|||||||||
2321|Border Waterhole Formation|33111|6|Mentioned|p26|||||||||
2321|Border Waterhole Formation|33482|6|Mentioned|p3|||Equiv. Beetle Creek Formation||||||
2321|Border Waterhole Formation|35001|6|Mentioned|p251|||||||||
2321|Border Waterhole Formation|35054|6|Mentioned|Table 23|||||||||
2321|Border Waterhole Formation|36473|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian to Ordovician||||||
2321|Border Waterhole Formation|36645|6|Mentioned|p308|||||||||
2321|Border Waterhole Formation|37572|4|Described|p157|||||||||
2321|Border Waterhole Formation|38291|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
2321|Border Waterhole Formation|38348|6|Mentioned|p24|||||||||
2321|Border Waterhole Formation|38446|6|Mentioned|Table 23|||||||||
2321|Border Waterhole Formation|39422|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Chert, siltstone, chert breccia, phophorite. Conformably overlain by Currant Bush Limestone; unconformably over rocks of the McNamara Group Top Rocky Rhyolite (Carrara Range Group).||||||10-JAN-05
2321|Border Waterhole Formation|39445|5|Briefly described|Table 4|||See also p62||||||26-JUL-06
2321|Border Waterhole Formation|39497|6|Mentioned|p14|||See also 16||||||26-JUL-06
2321|Border Waterhole Formation|39797|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
2321|Border Waterhole Formation|40852|6|Mentioned|p37|||||||||
2321|Border Waterhole Formation|40856|5|Briefly described|p315|||||||||
2321|Border Waterhole Formation|41240|6|Mentioned|p112|||||||||
2321|Border Waterhole Formation|41639|5|Briefly described|p4|||||||||
2321|Border Waterhole Formation|43652|6|Mentioned|Fig.15,p393|||||||||
2321|Border Waterhole Formation|44211|14|Not recorded|p100|||||||||
2321|Border Waterhole Formation|44274|2|Defined|Tb.1,p7,11,13,map||Middle Cambrian|Overlies Camooweal Dolomite. On QLD and NT white cards. (Not according to Mt Drummond 250K map, 2006)||||||09-AUG-06
2321|Border Waterhole Formation|44275|14|Not recorded|Map Legend|||||||||
2321|Border Waterhole Formation|44281|14|Not recorded|Map Legend||Middle Cambrian|||||||
2321|Border Waterhole Formation|44482|14|Not recorded|p.11,15, opp.p.6;map|||(E53-12).||||||
2321|Border Waterhole Formation|44483|5|Briefly described|map legend||Middle Cambrian|Middle Cambrian.||||||
2321|Border Waterhole Formation|44920|14|Not recorded|Map Legend||Middle Cambrian|||||||
2321|Border Waterhole Formation|44922|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|||||||01-JUL-04
2321|Border Waterhole Formation|45032|14|Not recorded|p8,10||Middle Cambrian|Tb.1, Pl.1. (E53-12).||||||
2321|Border Waterhole Formation|45052|3|Fully described|p91|||M.Camb.||||||
2321|Border Waterhole Formation|45079|6|Mentioned|p22|||Lower Middle Cambrian age. Should be included in Beetle Creek Formation||||||
2321|Border Waterhole Formation|45166|5|Briefly described|Table 15|||||||||
2321|Border Waterhole Formation|46792|6|Mentioned|p51|||Trilobite fauna.||||||26-JUL-06
2321|Border Waterhole Formation|47058|6|Mentioned|Fig.8 P129|||||||||
2321|Border Waterhole Formation|50600|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Overlain by Thorntonia Limestone.  Chert, chert breccia, siltstone, phosporite.||||||28-JUN-04
2321|Border Waterhole Formation|61904|5|Briefly described|p132 Fig. 2|Cambrian|Cambrian|Carbonates. See also p134.||||||
2321|Border Waterhole Formation|62659|5|Briefly described|Map Legend|Cambrian|Cambrian|Bioclast and bioclast ooid rudstone, commonly chertified.||||||
2321|Border Waterhole Formation|64068|6|Mentioned|p185, p59, 225|||Of northeastern Georgina Basin. Correlated with Thorntonia Limestone. Broken Hill South identified small phosphate deposits in this unit straddling the NT-Queensland border.||||||21-MAR-16
2321|Border Waterhole Formation|64317|5|Briefly described|p589|||Of Stewart and Mitchell (1987); Lindsay and Brasier (2006). Consists of siliceous breccia bordering the interior edge of Thorntonia Limestone annulus structure.  Mainly chert clasts and clumps of semi-consolidated muddy sediments containing chert nodules.||||||23-SEP-08
2321|Border Waterhole Formation|65337|3|Fully described|p9 Fig.5, p64, p75.|Middle Cambrian|Middle Cambrian|Southeast MOUNT DRUMMOND area. Hosts the Highland Plains phosphate deposit; 84 Mt @ 13.4% P^20^5 (Cook and Shergold 1979). Reported fossils include Ordian-age trilobites, molluscs and hyoliths.||Unit in Narpa Group.||Unconformably overlies McNamara Group. Is overlain by Currant Bush Limestone.|Siliceous shale, siltstone, chertified limestone, bedded to nodular chert; basal quartz-lithic sandstone, granule to pebble conglomerate.|
2321|Border Waterhole Formation|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Middle Cambrian|Middle Cambrian|Georgina Basin.||Narpa Group|||Siltstone, chert, chert breccia, phosphorite|
2321|Border Waterhole Formation|68020|6|Mentioned|p126|Cambrian|Cambrian|Includes phosphorite deposits.||||||
2321|Border Waterhole Formation|69418|6|Mentioned|p3:31|||Georgina Basin. Hosts the Highland Plains phosphate deposit (briefly described).||||||12-JUL-16
2321|Border Waterhole Formation|69437|5|Briefly described|p22:9-10|Series 2|Series 2|Eastern Undilla Sub-basin, Georgina Basin, Centralian B Superbasin. Sequence 1.||||Correlated with Thorntonia Limestone.||12-JUL-16
2321|Border Waterhole Formation|69443|4|Described|p28:16, 19-20, 43|Middle Cambrian|Middle Cambrian|Opik (1960). Undilla Sub-basin, Georgina Basin. Outcrops are typically obscured by regolith of chert breccia and pebbles. 30-180m thick. Fossiliferous. Shallow-marine deposits. Hosts the Highland Plains phosphate deposit.||Narpa Group.||Unconformably overlies Lawn Hill Formation. Is overlain conformably or disconformably by the Currant Bush Limestone. Grades laterally into, and interfingers with, Thorntonia Limestone.|Siliceous shale, siltstone, grey and black chertified limestone (including bioclast floatstone and rudstone), irregularly bedded to nodular chert, chert breccia, chert conglomerate and a basal pebble conglomerate.|12-JUL-16
2321|Border Waterhole Formation|69446|6|Mentioned|p31:3|||Georgina Basin. Broadly age-equivalent to Daly River Group(Daly Basin).||||||12-JUL-16
2321|Border Waterhole Formation|69447|6|Mentioned|p32:2|||Georgina Basin.||||Age-equivalent to Montejinni Limestone, Hooker Creek Formation and Lothari Hill Sandstone (Wiso Basin).||12-JUL-16
2321|Border Waterhole Formation|69448|6|Mentioned|p33:3|||Georgina Basin.||||Correlated with Negri Subgroup (Ord Basin) in part.||12-JUL-16
2321|Border Waterhole Formation|69591|5|Briefly described|p88, p96|Cambrian|Cambrian|Undilla Sub-basin, Georgina Basin.||Narpa Group.||||
2321|Border Waterhole Formation|69673|5|Briefly described|p116, p117, p142|||180m thick.||Narpa Group|||Shale, siltstone, chertified limestone, chert and conglomerate.|
2321|Border Waterhole Formation|70380|6|Mentioned|p745|Stage 5|Stage 4|Undilla Sub-basin, Georgina Basin.||||||
2321|Border Waterhole Formation|72297|5|Briefly described|p732|Middle Cambrian|Middle Cambrian|Georgina Basin. One of the two major producers of phosphate in QLD.|||||Marine sequences of phosphorite (phosphatic siltstone) and chert, overlying limestone, sandstone and conglomerate.|
2321|Border Waterhole Formation|72414|4|Described|map sheet|Middle Cambrian|Middle Cambrian|Of Geogina Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.||Unit of Narpa Group.||Overlain by Camooweal Dolomite or Thorntonia Limestone. Underlain by Colless Volcanics.|Siltstone, chert, chert breccia, phosphorite|
2321|Border Waterhole Formation|72415|4|Described|mapsheet|Early Ordovician|Cambrian|Of Geogina Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.||Unit of Narpa Group.||Overlain by Camooweal Dolomite or Thorntonia Limestone. Underlain by Colless Volcanics.|Siltstone, chert, chert breccia, phosphorite|
2321|Border Waterhole Formation|72516|6|Mentioned|p91|Cambrian|Cambrian|Georgina Basin.||||Equivalent to the Thorntonia Limestone.||02-JUN-21
2347|Bortala Formation|22438|6|Mentioned|p549, Fig.12|||||||||
2347|Bortala Formation|22585|6|Mentioned|Fig3 P738|||Actually written as Bortala Fm.||||||26-JUL-06
2347|Bortala Formation|23031|5|Briefly described|p24|||Geol. province: Mount Isa Fold Belt. Of the Myally Subgroup. Overlying unit: Witworth Quartzite, underlying unit: Alsace Quartzite||||||26-JUL-06
2347|Bortala Formation|23395|5|Briefly described|p386 Fig.3|||Of Myally Subgroup.||||||26-JUL-06
2347|Bortala Formation|23518|4|Described|p11|Proterozoic|Proterozoic|Of Myally Subgroup.  Geological Province: Western Fold Belt.||||||
2347|Bortala Formation|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Myally Subgroup (Haslingden Group).  Overlies the Alsace Quartzite; Underlies the Whitworth Quartzite.||||||25-AUG-04
2347|Bortala Formation|30534|2|Defined|p304|Carpentarian|Carpentarian|||||||
2347|Bortala Formation|33900|4|Described|p12|||||||||
2347|Bortala Formation|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
2347|Bortala Formation|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
2347|Bortala Formation|38232|6|Mentioned|p84|||||||||
2347|Bortala Formation|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
2347|Bortala Formation|39445|5|Briefly described|Table 2|||See also p40||||||26-JUL-06
2347|Bortala Formation|39556|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||
2347|Bortala Formation|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Myally Subgroup (Haslingden Group).  Flaggy, fine feldspathic siltstone, micaceous siltstone, dolomitic sandstone, tuffaceous siltstone, grey-green chert.Overlies the Alsace Quartzite.||||||15-JUN-06
2347|Bortala Formation|39622|6|Mentioned|Fig.2|||||||||
2347|Bortala Formation|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
2347|Bortala Formation|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
2347|Bortala Formation|40221|3|Fully described|p8|||||||||
2347|Bortala Formation|40623|5|Briefly described|p99|||||||||
2347|Bortala Formation|41298|6|Mentioned|Map legend|Carpentarian||||||||
2347|Bortala Formation|41307|4|Described|p10|||||||||
2347|Bortala Formation|42503|6|Mentioned|p336|||||||||
2347|Bortala Formation|42523|5|Briefly described|Fig. 2 p373|||||||||26-JUL-06
2347|Bortala Formation|42676|5|Briefly described|Fig.2, P41|||||||||
2347|Bortala Formation|45136|3|Fully described|p24|||||||||
2347|Bortala Formation|45166|5|Briefly described|p14|||||||||
2347|Bortala Formation|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
2347|Bortala Formation|47083|4|Described|p7|||Of Myally Subgroup of Haslingden Gp. O'lying unit: Whitworth Quartzite - conformable. U'lying: unit Alsace Quartzite - conformable. Maximum thickness: 500 m.||||||26-JUL-06
2347|Bortala Formation|50332|6|Mentioned|p17|Proterozoic|Proterozoic|Of the Myally Subgroup.||||||07-FEB-11
2347|Bortala Formation|50550|6|Mentioned|p1144 Fig.7||Statherian|Geological Province: Western Fold Belt.||||||19-DEC-07
2347|Bortala Formation|61929|5|Briefly described|p128 Fig. 2|||Of the Myally Subgroup. ||||||
2347|Bortala Formation|62988|5|Briefly described|p34|||Geological Province: Mount Isa Inlier.||||||25-JAN-07
2347|Bortala Formation|63023|5|Briefly described|p1025 Fig. 2, p1029|Paleoproterozoic|Paleoproterozoic|Of Myally Subgroup (Haslingden Group). Age: 1773+/-2Ma. Overlies Alsace Quartzite; overlain by Whitworth Quartzite. Geological Province: Leichardt Superbasin. Comprises pink feldspathic sandstone, recessive siltstone and shale. See also p1027 Tb. 1.||||||07-NOV-08
2347|Bortala Formation|63109|6|Mentioned|p1108 Fig. 3|||Overlain by Whitworth Quartzite, underlain by Alsace Quartzite. Geological Province: Leichhardt Superbasin. Consists of siltsone.||||||
2347|Bortala Formation|63113|5|Briefly described|p1214 Fig.2, p1225 Fig.13.|||||Of the Haslingden Group||Overlies Alsace Quartzite. Is overlain by Whitworth Quartzite.||
2347|Bortala Formation|63115|6|Mentioned|p1279 Fig.4.|||Leichhardt superbasin.||||||
2347|Bortala Formation|63116|6|Mentioned|p1297 Fig.2, p1299-1301, p1305, p1308|||Leichhardt superbasin. Material properties detailed. A seal above the Eastern Creek Volcanics.||||||
2347|Bortala Formation|63866|5|Briefly described|p58|Statherian|Statherian|Leichhardt Superbasin. Numeric age is a maximum depositional date.|1773 +/- 3 Ma (Neumann et al., 2006)|Myally Supersequence||Overlain by the Quilalar Formation.||
2347|Bortala Formation|65505|6|Mentioned|979|Proterozoic|Proterozoic|Of the Leichhardt River Fault Trough. Age: 1773 +/-2 Ma.||||||
2347|Bortala Formation|67323|4|Described|GIS attrib tbl, Solid Geology Map, p13|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot. Leichhardt Superbasin. Leichhardt River Domain, Mount Isa Inlier.|1773 +/- 2 Ma.|Myally Subgroup.||Overlies Eastern Creek Volcanics?|Flaggy, fine feldspathic sandstone, siltstone, micaceous siltstone, dolomitic sandstone, tuffaceous siltstone, grey - green chert.|
2347|Bortala Formation|68732|6|Mentioned|p160, p161, p165|Statherian|Statherian|Sedimentary depositional age from a volcaniclastic unit. Of the Myally Supersequence.|1773 +/- 2 Ma||||Mainly very fine-grained arkosic sandstones.|30-NOV-17
2347|Bortala Formation|69222|5|Briefly described|p222 Fig.2|Statherian|Statherian|Leichhardt River Fault Trough.||Myally Subgroup||Overlies Pickwick Metabasalt||09-FEB-18
2347|Bortala Formation|69591|5|Briefly described|p33, p57|||Mount Oxide and Leichhardt River Domains, Leichhardt Superbasin. Part of Myally Supersequence. Storm-dominated shelf deposits.|1773 +/- 2 Ma (Neumann et al., 2006).|Myally Subgroup.|||Flaggy, fine feldspathic sandstone, siltstone, micaceous siltstone, dolomitic sandstone, tuffaceous siltstone, grey-green chert.|
2347|Bortala Formation|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Myally Subgroup.||Overlies Alsace Quartzite. Is overlain by Whitworth Quartzite.|Flaggy, fine-grained feldspathic sandstone, siltstone, micaceous siltstone, dolomitic sandstone, tuffaceous siltstone and grey-green chert.|
2347|Bortala Formation|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Myally Subgroup.||Overlies Alsace Quartzite. Is overlain by Whitworth Quartzite.|Flaggy, fine-grained feldspathic sandstone, siltstone, micaceous siltstone, dolomitic sandstone, tuffaceous siltstone and grey-green chert.|
2347|Bortala Formation|71592|5|Briefly described|Appendix A.|||Leichhardt River Domain, Mount Isa Orogen.|1780+/-4 Ma (MDA: U-Pb zircon SHRIMP)||||Mudstone.|
2347|Bortala Formation|71960|6|Mentioned|p105|||||||||
2347|Bortala Formation|71980|5|Briefly described|map legend sheets 1, 2|Proterozoic|Proterozoic|Stacked channel fills at base; generally heterolithic, inshore, transitional, tidal||Of Myally Subgroup|||Pebbly sandstone at base, overlain by siltstone-mudstone, siltstone-feldspathic sandstone, siltstone-mudstone; sandstone throughout.|
2347|Bortala Formation|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Lawn Hill Platform and Leichhardt River Fault Trough of the Mount Isa Province.||Myally Subgroup||Overlies Alsace Quartzite and underlies Lochness Formation.||
2347|Bortala Formation|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Lawn Hill Platform and Leichhardt River Fault Trough of the Mount Isa Province.||Myally Subgroup||Overlies Alsace Quartzite and underlies Lochness Formation.||
2347|Bortala Formation|72919|6|Mentioned|p63|||||Myally Subgroup, Myally Supersequence||||
2347|Bortala Formation|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Mount Isa Province, Leichhardt Superbasin.||Myally Subgroup||Underlain by Alsace Quartzite. Overlain by Lochness Formation.||
2347|Bortala Formation|73525|6|Mentioned|p4-5 Fig.2, p19 Fig.13|||Leichhardt River Domain.|||||Clastics.|
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.|
2472|Bradshaw Complex|22479|5|Briefly described|fig4, pg10|Orosirian|Orosirian|||||||
2472|Bradshaw Complex|22538|6|Mentioned|P715||Orosirian|||||||
2472|Bradshaw Complex|22600|4|Described|Map legend|Orosirian|Orosirian|||||||
2472|Bradshaw Complex|23363|5|Briefly described|351 Tab.1|Orosirian|Orosirian|Age: 1867+/-12Ma.||||||02-AUG-06
2472|Bradshaw Complex|23374|5|Briefly described|Fig3p5||Paleoproterozoic|Of Arnhem Inlier.||||||07-NOV-08
2472|Bradshaw Complex|24047|5|Briefly described|p75 Fig. 60, p76|Paleoproterozoic|Paleoproterozoic|Unconformably overlain by Yirrkala Formation.  Geological Province: Carpentaria Basin.||||||07-NOV-08
2472|Bradshaw Complex|24048|3|Fully described|p10|Paleoproterozoic|Paleoproterozoic|Formerly included in the "Grindall Metamorphics" and "Bikerton Volcanics".  Can also be divided into the Melville Bay Metamorphics and the Drimmie Head Granite in the Arnhem Bay - GROVE.  Age: 1867+/-12Ma (SHRIMP U-Pb). Geological Province: Arnhem Inlier.||||||07-NOV-08
2472|Bradshaw Complex|24049|5|Briefly described|Map Legend|Orosirian|Orosirian|Includes Melville Bay Metamorphics and Drimmie Head Granite. Undivided Bradshaw Complex. Granite: garnet-biotite and cordierite bearing; migmatite; gneiss; calc-silicate and psammite types; mafic enclaves. Geol. Prov: McArthur Basin, Arnhem Inlier.||||||13-OCT-05
2472|Bradshaw Complex|41406|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
2472|Bradshaw Complex|43010|2|Defined|p25||Paleoproterozoic|Supersedes Bradshaw Granite. Of Orosirian age.||||||07-NOV-08
2472|Bradshaw Complex|43292|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
2472|Bradshaw Complex|44112|1|Redefined|p1,5,7,21,63,104|Orosirian|Paleoproterozoic|Previously mapped as 'Bradshaw Granite' by Dunnet (1965). Redefined by Plum and Roberts (1992) as a result of rationalisation of component units||||||07-NOV-08
2472|Bradshaw Complex|50591|5|Briefly described|p2.1|Paleoproterozoic|Paleoproterozoic|Of the Bradshaw Suite. Geological Province: Arnhem Block/McArthur Basin. Age: 1867-1845 +/- 12Ma (U-Pb). Intruded by Giddy Suite.||||||07-NOV-08
2472|Bradshaw Complex|60573|6|Mentioned|Regional Setting legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
2472|Bradshaw Complex|61403|5|Briefly described|Map Legend|Orosirian|Orosirian|Includes Melville Bay Metamorphics and Drimmie Head Granite. Undivided Bradshaw Complex. Granite: garnet-biotite and cordierite bearing; migmatite; gn eiss; calc-silicate and psammite types; mafic enclaves. Geol. Prov: McArthur Basin, Arnhem Inlier.||||||
2472|Bradshaw Complex|63866|5|Briefly described|p115, p117, p124|||Arnhem Inlier, Northern Caledon Shelf.|1867 +/- 12 Ma (Page, OZCHRON)|||Intrudes the Grindall Formation.|Granitic rocks.|
2472|Bradshaw Complex|65228|6|Mentioned|p20.|||Far north of the McArthur Basin. Regarded, with ~1840 granites, as basement of the Arnhem Inlier by Rawlings et al. (1997).||||||
2472|Bradshaw Complex|69417|5|Briefly described|p2:5|Orosirian|Orosirian|Arnhem Orogen.||||Intrudes Grindall Formation.||12-JUL-16
2472|Bradshaw Complex|69421|4|Described|p6:1-5|||Eastern Arnhem Province. Plumb and Roberts (1992), and Madigan and Rawlings (1997) had several informal subdivisions. Rawlings et al. (1997) simplified these into two named units and undivided Bradshaw Complex. Granulite facies in the N; mainly amphibolite-grade in the S. The Grindall Formation is at least part of the protolith. Peak metamorphic age of 1867 +/- 12 Ma (= age of Drimmie Head Granite) corresponding to the Nimbuwah Event in the Pine Creek Orogen.|||Melville Bay Metamorphics, Drimmie Head Granite.|Intrudes Grindall Formation. Is intruded by Bukudal and Garrthalala Granites. Is overlain by Spencer Creek Group.|A continuum of amphibolite-facies gneiss, migmatite, granitic gneiss and granite; fine- to coarse-grained, foliated to massive.|12-JUL-16
2472|Bradshaw Complex|69430|6|Mentioned|p15:13|||||||Is overlain unconformably by Coast Range Sandstone.||12-JUL-16
2472|Bradshaw Complex|69455|6|Mentioned|p39:7 Fig.39.8; 39:9|Paleoproterozoic|Paleoproterozoic|Part of the basement in the Gove area (Arnhem Province).||||||12-JUL-16
2472|Bradshaw Complex|69673|6|Mentioned|p3|||||||||
2472|Bradshaw Complex|70719|6|Mentioned|iv, p10|||Pietsch et al. (1997).||||||
2472|Bradshaw Complex|71592|5|Briefly described|Appendix A.|||Arnhem Province.|1854+/-6 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite, pegmatite.|
2472|Bradshaw Complex|71605|5|Briefly described|iii, p6, p15|||Arnhem Province.|||Includes the Melville Bay Metamorphics.|||
2472|Bradshaw Complex|71606|5|Briefly described|p137|Orosirian|Orosirian|North and Central Caledon Shelf, McArthur Basin. Associated with 1885-1870 Ma Barramundi Orogeny.||||||
2472|Bradshaw Complex|71620|6|Mentioned|p26|||Arnhem Province.  ||||||
2472|Bradshaw Complex|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Basement to McArthur Basin.||||||05-MAR-20
2472|Bradshaw Complex|73083|6|Mentioned|p49|Paleoproterozoic|Paleoproterozoic|||||Underlain by Roper Group.|Metamorphic rocks.|
2476|Brady Gneiss|9199|5|Briefly described|Map legend|||Sillimanite-garnet-muscovite-biotite-plagioclase-quartz gneiss.  Geological Province: Arunta Block.||||||04-NOV-04
2476|Brady Gneiss|9394|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block (Division 2). Of the Harts Range Group. Biotite gneiss, calc-silicte rock, schistose garnet-muscovite-biotite gneiss, muscovite-biotite gneiss.||||||
2476|Brady Gneiss|22524|6|Mentioned|p42|||||||||
2476|Brady Gneiss|24540|6|Mentioned|p6|||Hosts a sodic pegmatite suite. Geological Province: Arunta region.||||||07-FEB-11
2476|Brady Gneiss|33103|6|Mentioned|Table 1|||||||||
2476|Brady Gneiss|34488|6|Mentioned|p8|||||||||
2476|Brady Gneiss|35046|6|Mentioned|p376|||||||||
2476|Brady Gneiss|38885|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
2476|Brady Gneiss|39583|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
2476|Brady Gneiss|39887|6|Mentioned|Fig.3|||||||||
2476|Brady Gneiss|39898|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Harts Range Group. Calc-silicate rock containing clinozoisite, epidote, hornblende, clinopyroxene, scapolite, quartz, and feldspar; garnet-muscovite-biotite schistose gneiss, biotite gneiss. Geological Province: Arunta Block.||||||07-NOV-08
2476|Brady Gneiss|39931|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic. Of the Harts Range Group.||||||07-NOV-08
2476|Brady Gneiss|40100|5|Briefly described|Table 1|||||||||
2476|Brady Gneiss|40538|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Block.||||||07-NOV-08
2476|Brady Gneiss|40906|4|Described|p8|||||||||
2476|Brady Gneiss|44327|14|Not recorded|Tb.I||Archean|(F53-11).||||||07-NOV-08
2476|Brady Gneiss|44328|14|Not recorded|map legend||Archean|Archaean.||||||07-NOV-08
2476|Brady Gneiss|44964|14|Not recorded|p.39|||||||||
2476|Brady Gneiss|46730|4|Described|p6|||Of the Harts Range Group. Geological Province: Arunta Block.||||||
2476|Brady Gneiss|48844|14|Not recorded|p.10,15,Pl.8|||(F53-11).||||||
2476|Brady Gneiss|48880|4|Described|p.12||Archean|p.10. Ref to Joklik 1955. Archaean.||||||07-NOV-08
2476|Brady Gneiss|49036|6|Mentioned|p13|||||||||
2476|Brady Gneiss|60547|5|Briefly described|Map Legend|Precambrian|Precambrian|Of the Harts Range Group. Sillimanite-garnet-muscovite-biotite-plagioclase-quartz gneiss.||||||
2476|Brady Gneiss|62595|5|Briefly described|p4 Table 2, p28 Fig.4.|||Relative probability plots of detrital zircon data are shown.||Unit in Harts Range Group.|||Lower unit of garnet-bearing muscovite-biotite +/- sillimanite schist and gneiss, minor amphibolite and psammite; upper unit of clinozoisite-hornblende-clinopyroxene-scapolite-bearing calc-silicate rock, minor metapelite and psammitic layers.|
2476|Brady Gneiss|64337|5|Briefly described|p374|||||Of Harts Range Complex.||Structurally overlies Irindina Gneiss.|Metapelites, metapsammites and subordinate calsilicate rocks.|
2476|Brady Gneiss|66767|5|Briefly described|p59|||Irindina Province.|||||Comprises a lower pelitic and upper calcareous unit.|
2476|Brady Gneiss|68316|5|Briefly described|pp777-785||Series 2|Contains detrital zircon spectra similar to Amadeus Basin rocks such as Pacoota Sst. Can be subdivided into structurally lower and upper sub-units of predominantly metapelite and calcsilicate rocks, respectively. Age constrained by the Harts Range Meta-Igneous Complex.||Of the Harts Range Meta-Igneous Complex.|||Metapelite-dominated.|10-APR-17
2476|Brady Gneiss|68517|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Arunta Block. Early Proterozoic ? age. Two facies associations mapped separately.||Of the Harts Range Group.|||Calc-silicate rock, garnet-muscovite-biotite schistose gneiss, and biotite gneiss; schistose garnet-bearing muscovite-biotite gneiss, biotite gneiss and calc-silicate rock.|
2476|Brady Gneiss|68697|6|Mentioned|p22, p24, p46|||||Harts Range Metamorphic Complex.||||
2476|Brady Gneiss|69444|4|Described|p29:1-6, 8, 10|Cambrian|Cambrian|Irindina Province. Crops out N and E of the Entia Dome. The metamorphic grade is significantly lower than that of the underlying succession, suggesting a major structural break. The top is not exposed. SHRIMP U-Pb detrital zircon maximum depositional age. Metamorphism of calc-silicate rock is dated at 479 +/- 7 Ma. NE of the Entia Dome, is cut by late-stage, gossanous, radioactive breccia veins with minor to very high REE-Th mineralisation.|499 +/- 6 Ma (Maidment, 2005).|Harts Range Metamorphic Complex.||Overlies Irindina Gneiss. Is intruded by Lloyd gabbro.|Lower unit mainly garnet-muscovite-biotite schist, with minor amphibolite and metapsammitic rock and late-stage pegmatites; upper unit mainly quartz-clinozoisite-hornblende-clinopyroxene-scapolite calc-silicate rock with minor metapelitic schist.|12-JUL-16
2476|Brady Gneiss|69917|4|Described|p183, 114|||Of Harts Range Metamorphic Complex, Eastern Arunta Region, Irindina Province. No zircon from this sample. Previous SHRIMP U-Pb zircon dating of the Brady Gneiss yielded a maximum deposition age of ca 510 Ma (Buick et al 2005, Maidment 2005).|510 Ma|Uppermost unit of the Harts Range Metamorphic Complex||Conformably overlies Spriggs Gneiss.|Dominantly calcareous metapsammopelitic and metapelitic schists and calc-silicate rock. Calc-silicate rock sampled.|
2476|Brady Gneiss|70094|5|Briefly described|p76-77, 79-81, 85-86|||Harts Range. Mineralogy detailed.||Harts Range Group.||Overlies Irindina Gneiss.|Comprises a lower metapelitic and an upper calc-silicate units. Mafic rocks are comparatively rare.|
2476|Brady Gneiss|70744|5|Briefly described|p944-945|||Detrital zircon age distribution graph.||Harts Range Group.|||Metasedimentary rocks.|
2476|Brady Gneiss|71592|5|Briefly described|Appendix A.|||Arunta Orogen.|464+/-8 Ma (SHRIMP U-Pb zircon).||||Metapelite.|
2476|Brady Gneiss|72516|6|Mentioned|p7, p93-94|||Irindina Province. Correlation of upper part  of Brady Gneiss with the Tomahawk Formation proposed by Maidment et al (2013).||Harts Range Metamorphic Complex||Overlies the Irindina Gneiss. Equivalent to the Arrinthrunga Formation.||09-JUN-21
2526|Brewer Conglomerate|9141|5|Briefly described|Map Legend|||Age: c.a. 0.3 B.Y.||||||
2526|Brewer Conglomerate|9199|5|Briefly described|Map legend|Devonian|Devonian|Of the Pertnjara Group. Conglomerate, rare sandstone. Geological Province: Amadeus Basin.||||||06-FEB-08
2526|Brewer Conglomerate|9814|5|Briefly described|Map Legend|Devonian|Devonian|Of the Pertnjara Group. Pebbly sandstone, minor siltstone, rare conglomerate with clasts of quartzite, sedimentary and crystalline rocks.||||||
2526|Brewer Conglomerate|12891|5|Briefly described|p733 Fig. 2|Early Carboniferous|Late Devonian|Geological province: Amadeus Basin.||||||07-FEB-11
2526|Brewer Conglomerate|22561|5|Briefly described|p23||Devonian|Of the Pertnjara Group.||||||02-AUG-06
2526|Brewer Conglomerate|22565|5|Briefly described|p71 & Table 1||Devonian|Approx thickness measured from seismic data - 1780 meters||||||
2526|Brewer Conglomerate|22566|4|Described|p86||Devonian|Stratigraphic relationships described p85. Of the Pertnjara Group.||||||31-MAR-09
2526|Brewer Conglomerate|22646|6|Mentioned|p 105|Devonian|Devonian|Parent  - Pertnjara Group||||||
2526|Brewer Conglomerate|22650|6|Mentioned|p 166|Devonian|Devonian|Parent - Pertnjara Group.||||||
2526|Brewer Conglomerate|22656|6|Mentioned|p 282||Devonian|||||||
2526|Brewer Conglomerate|22760|4|Described|p337-340 & p342|Late Devonian|Late Devonian|Of the Pertnjara Group.||||||02-AUG-06
2526|Brewer Conglomerate|22761|5|Briefly described|p351|Late Devonian|Late Devonian|Of the Pertnjara Group.||||||02-AUG-06
2526|Brewer Conglomerate|22762|6|Mentioned|p364|Late Devonian|Middle Devonian|Of the Pertnjara Group.  Age - Frasnian-Famennian (p373).||||||02-AUG-06
2526|Brewer Conglomerate|22763|5|Briefly described|p402||Late Devonian|Of the Pertnjara Group.||||||02-AUG-06
2526|Brewer Conglomerate|22804|5|Briefly described|p454||Devonian|Of Pertnjara Group.||||||02-AUG-06
2526|Brewer Conglomerate|22805|5|Briefly described|p465||Middle Devonian|Of Pertnjara Group.||||||02-AUG-06
2526|Brewer Conglomerate|22824|4|Described|p531-533|||The upper part of the Brewer Conglomerate has been dated as pre-latest Famennian, corresponding to an age of about 360 Ma. See p526.||||||31-MAR-09
2526|Brewer Conglomerate|22825|6|Mentioned|Fig 1 on p542|||Parent - Pertnjara Group.||||||
2526|Brewer Conglomerate|22826|4|Described|p575|Devonian|Devonian|||||||
2526|Brewer Conglomerate|23361|5|Briefly described|16 Fig.4|Devonian|Devonian|Age: 400-350Ma.||||||02-AUG-06
2526|Brewer Conglomerate|23621|5|Briefly described|p36|||Geological Province: Amadeus Basin.||||||
2526|Brewer Conglomerate|23858|5|Briefly described|p915|Devonian|Devonian|Of Pertnjara Group. Geological Province: Amadeus Basin.||||||
2526|Brewer Conglomerate|24334|5|Briefly described|p48 Tb.1, p51|Late Devonian|Late Devonian|Age: 363 - 367 Ma. Overlies the Hermannsburg Sandstone. Geological Province: Amadeus Basin.||||||
2526|Brewer Conglomerate|24424|5|Briefly described|p539 Tb.4|Late Devonian|Late Devonian|Age: 354-365 Ma. Palaeomagnetic poles given.||||||04-FEB-05
2526|Brewer Conglomerate|29972|6|Mentioned|Table 1|||||||||
2526|Brewer Conglomerate|31566|3|Fully described|p241|||See also p242-243. Devonian.||||||31-MAR-09
2526|Brewer Conglomerate|31567|6|Mentioned|Fig. 3|||Diagrammatic cross section||||||
2526|Brewer Conglomerate|31707|6|Mentioned|p50|||||||||
2526|Brewer Conglomerate|32209|6|Mentioned|Map legend|Devonian|Devonian|||||||
2526|Brewer Conglomerate|32640|6|Mentioned|p235|||||||||
2526|Brewer Conglomerate|34111|5|Briefly described|Table 2|||Devonian - Carboniferous||||||
2526|Brewer Conglomerate|34579|4|Described|Table 3|||Devonian - Carboniferous.||||||14-APR-08
2526|Brewer Conglomerate|35102|6|Mentioned|p4|||||||||
2526|Brewer Conglomerate|36821|6|Mentioned|p397|||||||||
2526|Brewer Conglomerate|38606|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
2526|Brewer Conglomerate|38885|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
2526|Brewer Conglomerate|39565|6|Mentioned|p35|||||||||
2526|Brewer Conglomerate|39583|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
2526|Brewer Conglomerate|40201|5|Briefly described|p691|||||||||
2526|Brewer Conglomerate|40740|3|Fully described|p60|||||||||
2526|Brewer Conglomerate|40810|5|Briefly described|p12|||||||||
2526|Brewer Conglomerate|40859|5|Briefly described|p101|||See Fig.2. Informal name||||||
2526|Brewer Conglomerate|41018|6|Mentioned|p236|||||||||
2526|Brewer Conglomerate|41039|4|Described|p7|||||||||
2526|Brewer Conglomerate|41125|6|Mentioned|p40|||||||||
2526|Brewer Conglomerate|41190|6|Mentioned|Fig.4|||||||||
2526|Brewer Conglomerate|41270|6|Mentioned|p268|||||||||
2526|Brewer Conglomerate|41385|6|Mentioned|Fig.12|||||||||
2526|Brewer Conglomerate|41492|6|Mentioned|p158|||||||||
2526|Brewer Conglomerate|41708|6|Mentioned|Fig.1|||||||||
2526|Brewer Conglomerate|41717|6|Mentioned|Fig.2|||||||||
2526|Brewer Conglomerate|42037|5|Briefly described|Table 3 P79|||||||||
2526|Brewer Conglomerate|42049|6|Mentioned|Table 1 P217|||||||||
2526|Brewer Conglomerate|42059|6|Mentioned|Fig.2 P131|||||||||
2526|Brewer Conglomerate|42082|6|Mentioned|Fig.3 P323|||||||||
2526|Brewer Conglomerate|42141|6|Mentioned|Fig.3 P570|||||||||
2526|Brewer Conglomerate|42504|5|Briefly described|p80|||||||||
2526|Brewer Conglomerate|42564|6|Mentioned|p12|||Amadeus Basin.||||||
2526|Brewer Conglomerate|42886|5|Briefly described|p219|||||||||
2526|Brewer Conglomerate|42940|5|Briefly described|Plate 12|||||||||
2526|Brewer Conglomerate|43035|5|Briefly described|p23|||Of Pertnjara Group.||||||14-APR-08
2526|Brewer Conglomerate|43225|5|Briefly described|Map Legend||Devonian|Of Pertnjara Group||||||02-AUG-06
2526|Brewer Conglomerate|43503|6|Mentioned|11-17|Famennian|Frasnian|||||||
2526|Brewer Conglomerate|43646|6|Mentioned|Fig.3,p554|||||||||
2526|Brewer Conglomerate|43647|6|Mentioned|p530||Late Devonian|||||||
2526|Brewer Conglomerate|43648|6|Mentioned|Fig.13,p500|||||||||
2526|Brewer Conglomerate|43649|5|Briefly described|p453,463||Ordovician|||||||
2526|Brewer Conglomerate|43666|6|Mentioned|p25|||||||||
2526|Brewer Conglomerate|43748|6|Mentioned|p36|||Devonian age?|||Includes Undandita Member|||19-DEC-11
2526|Brewer Conglomerate|44335|4|Described|p.11|Carboniferous|Devonian|Dev-Carb. Table 2. p.10.||||||
2526|Brewer Conglomerate|44336|14|Not recorded|map legend|Carboniferous|Devonian|Dev-Carbon, pt of Pertnjara Group. SG/53-3.||||||23-DEC-09
2526|Brewer Conglomerate|44342|14|Not recorded|p.7|||SG53-5, fm of Pertnjara Group.||||||
2526|Brewer Conglomerate|44393|6|Mentioned|Fig.1|Carboniferous|Devonian|Dev-Carb, part of Pertnjara Group.||||||
2526|Brewer Conglomerate|44395|14|Not recorded|p.9, Tb.2||Devonian|Of Pertnjara Group.||||||
2526|Brewer Conglomerate|44396|5|Briefly described|map legend|||(Dev-Carb). SF/52-15.  Of Pernjara Group.||||||02-AUG-06
2526|Brewer Conglomerate|44433|14|Not recorded|map legend|||Devonian to Carboniferous.||||||
2526|Brewer Conglomerate|44497|4|Described|p.12, Table 2|Carboniferous|Devonian|SF/53-13. Dev-Carb.||||||
2526|Brewer Conglomerate|44498|14|Not recorded|map legend|Carboniferous|Devonian|Part of Pertnjara Group. Dev-Carb.||||||22-DEC-09
2526|Brewer Conglomerate|45041|4|Described|p99|||See also pp100-102.||||||02-AUG-06
2526|Brewer Conglomerate|45097|5|Briefly described|p27|||No fossil evidence of age. ?Early Carboniferous||||||
2526|Brewer Conglomerate|46928|6|Mentioned|Table 1|||||||||
2526|Brewer Conglomerate|47050|5|Briefly described|Fig.1|||||||||
2526|Brewer Conglomerate|48963|6|Mentioned|p22|||||||||
2526|Brewer Conglomerate|60547|5|Briefly described|Map Legend|Devonian|Devonian|Conglomerate, rare sandstone. Of the Pertnjara Group. Geological Province: Amadeus Basin.||||||03-JUN-05
2526|Brewer Conglomerate|61309|5|Briefly described|p16 Fig. 4|||Geological Province: Amadeus Basin.||||||06-FEB-08
2526|Brewer Conglomerate|61385|5|Briefly described|Map legend|Devonian|Devonian|Pebble and cobble conglomerate.  Geological Province: Amadeus Basin.||||||20-OCT-05
2526|Brewer Conglomerate|62082|5|Briefly described|p18, p20|||Has a matrix rich in carbonate, and releases a regolith of loose, large quartzite clasts. Geological Province: Amadeus Basin. See also p27, p29, and Figs.11, 13.||||||07-FEB-11
2526|Brewer Conglomerate|62376|5|Briefly described|p18|Late Devonian|Late Devonian|Of the Pertnjara Group. Geological Province: Amadeus Basin.||||||09-FEB-10
2526|Brewer Conglomerate|62379|5|Briefly described|p7 Fig. 2|Devonian|Devonian|Of the Pertnjara Group. Geological Province: Amadeus Basin.||||||
2526|Brewer Conglomerate|64778|6|Mentioned|p13, 33|Devonian|Devonian|Amadeus Basin.||||||
2526|Brewer Conglomerate|64809|5|Briefly described|p3, p6 Fig.4, p11 Fig.10 |Late Devonian|Late Devonian|Formed a sedimentary wedge, thinning southward from 3000 m to 1500 m over just 17 km.||Of the Pertnjara Group||||
2526|Brewer Conglomerate|65232|5|Briefly described|p72, p10, App. 2|Late Devonian|Late Devonian|At top of Pertnjara Group. Includes Undandita Member. Source rocks include high-U granitic orthogneiss of Iwupataka Metamorphic Complex and Teapot Granite Complex. Polymictic conglomerate. Geol. Prov: Amadeus Basin.||||||18-FEB-10
2526|Brewer Conglomerate|65233|5|Briefly described|p3 Fig. 2, p13|Late Devonian|Late Devonian|Of the Pertnjara Group. Unconformable to conformable on Hermannsberg Sandstone. Geological province: Amadeus Basin. Syn-orogenic, coarse alluvial conglomerate.||||||07-FEB-11
2526|Brewer Conglomerate|65382|5|Briefly described|p713, p712 Fig. 1,  p717 App. 2|Tournasian|Late Devonian|Amadeus Basin. Age (380-355 Ma, also written as Late Devonian to earliest Carboniferous) from fish plates and palynomorphs.||||||
2526|Brewer Conglomerate|66767|5|Briefly described|p60|Devonian|Devonian|Amadeus Basin.||Pertnjara Group.||||
2526|Brewer Conglomerate|67028|6|Mentioned|p370 Fig.7, p371 Tb. 5|Carboniferous|Devonian|Age shown in Fig 7 is Carboniferous, but numeric age is Devonian-Carboniferous. Magnetic information for unit concerning Mid-Paleozoic to Early Mesozoic pole positions for Australia is presented, sourced from the Global Palaeomagnetic Database (GPMDB; McElhinny & Lock 1993, 1996)|300-375 Ma magnetic age range|||||24-APR-12
2526|Brewer Conglomerate|67326|5|Briefly described|p2|Late Devonian|Late Devonian|Amadeus Basin.||Pertnjara Group.||Overlies Hermannsburg Sandstone.||
2526|Brewer Conglomerate|67856|6|Mentioned|p338 fig 4-30|Late Devonian|Late Devonian|||Of Pertnjara Group.||||
2526|Brewer Conglomerate|68323|6|Mentioned|p4 Fig.2|Late Devonian|Late Devonian|Amadeus Basin.||Pertnjara Group.||||
2526|Brewer Conglomerate|69418|6|Mentioned|p3:17|||Amadeus Basin. Hosts the Angela and Pamela sandstone-type U deposits (described).||||||12-JUL-16
2526|Brewer Conglomerate|69438|3|Fully described|p23:2-3, 7, 38-40, 46-48, 50-52|Famennian|Famennian|Wells et al. (1970). Northern Amadeus Basin. Type area is south of Stokes Pass in the western MacDonnell Ranges; principal exposure is in the Missionary Syncline to the S. Crops out as mounds of clasts forming low rounded hills with a distinctive dendritic drainage pattern. Up to 3000m thick. Interpreted as a synorogenic molasse deposit, sourced partly from uranium-rich granites from the Arunta Region: hosts several U deposits in the Undandita Member (described in detail).||Pertnjara Group.|Undandita Member.|Overlies Hermannsburg Sandstone conformably and transitionally (locally unconformably), Jay Creek Limestone (probably unconformably), Mereenie Sandstone unconformably.|Polymictic conglomerate with unsorted clasts to 1m; minor pebbly sandstone and rare mudstone are present towards the top of the sucession.|12-JUL-16
2526|Brewer Conglomerate|69439|5|Briefly described|p24:12||Devonian|The upper part of this unit may be contemporaneous (Early Carboniferous) with the upper Mount Eclipse Sandstone (Ngalia Basin).||Pertnjara Group.||||12-JUL-16
2526|Brewer Conglomerate|69673|4|Described|p64 fig 53|||Up to 3km thick. ||Pertnjara Group|Includes Undandita Member|Overlies Hermannsburg Sandstone,|Polymictic, pebble, cobble and boulder conglomerates with subordinate interbedded sandstone and conglomeratic sandstone.|
2526|Brewer Conglomerate|71146|5|Briefly described|p6|Famennian|Famennian|Amadeus Basin.||||Overlies the Hermannsburg Sandstone.|Sandstone.|
2526|Brewer Conglomerate|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
2526|Brewer Conglomerate|71279|5|Briefly described|p355 Fig.2, p364-368, p370, p376 Fig.26|Late Devonian|Late Devonian|See also p377, p382. Amadeus Basin. Magnetisation described in detail. Modelled magnetic properties.||Pertnjara Group.|Undandita Member.|||
2526|Brewer Conglomerate|72360|5|Briefly described|Map legend|Devonian|Devonian|Of Amadeus Basin.||Unit of Pertnjara Group.|||Pebble and cobble conglomerate.|09-SEP-19
2526|Brewer Conglomerate|72369|5|Briefly described|p40|||Of Amadeus Basin.||||Underlain by Hermannsburg Sandstone.||
2526|Brewer Conglomerate|73085|6|Mentioned|p1|late Devonian|late Devonian|||Pertnjara Group||Underlain by Hermannsburg Sandstone. Equivalent to Horseshoe Bend Shale / Idracowra Sandstone (Finke Group).||
2718|Brunette Limestone|24303|4|Described|p42|Miocene|Miocene|Max. Thickness: 4.6m. Max. Thickness in BRUNETTE DOWNS: 18m (Randal, 1966)||||||
2718|Brunette Limestone|24304|5|Briefly described|Map legend|Miocene|Miocene|White chalcedonic limestone with chert nodules and chalcedony; minor sandstone.||||||
2718|Brunette Limestone|32418|6|Mentioned|p2|||||||||
2718|Brunette Limestone|34151|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
2718|Brunette Limestone|34441|4|Described|Table 1|||Tertiary. pp15,18||||||02-AUG-06
2718|Brunette Limestone|36213|6|Mentioned|p86|||||||||
2718|Brunette Limestone|36335|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
2718|Brunette Limestone|44221|14|Not recorded|p87,88,89,90,102|||||||||
2718|Brunette Limestone|44222|14|Not recorded|p119||Miocene|Miocene?||||||
2718|Brunette Limestone|44283|14|Not recorded|p.8,9.||Tertiary|Alroy Sheet. (E53-15).||||||
2718|Brunette Limestone|44284|14|Not recorded|map legend||Tertiary|||||||
2718|Brunette Limestone|44285|14|Not recorded|p.9|||May have been deposited in similar marine environment to Austral Downs Limestone.||||||
2718|Brunette Limestone|44301|2|Defined|map, p.9,10||Tertiary|Brunette Downs sheet. (E53-11).||||||
2718|Brunette Limestone|44302|14|Not recorded|map legend||Tertiary|Nodular white limestone, minor quartz sandstone and conglomerate fossiliferous Tertiary; laterite.||||||
2718|Brunette Limestone|44441|2|Defined|p.10||Cenozoic|opp.p.6,Tb.1,map. (E53-16).||||||19-NOV-08
2718|Brunette Limestone|44442|14|Not recorded|map legend||Tertiary|||||||
2718|Brunette Limestone|44473|14|Not recorded|p.12, opp. p.7|||(E53-7).||||||
2718|Brunette Limestone|44474|14|Not recorded|map legend||Tertiary|||||||
2718|Brunette Limestone|44482|14|Not recorded|opp.p.6|||(E53-12).||||||
2718|Brunette Limestone|44965|14|Not recorded|Not recorded|||||||||
2718|Brunette Limestone|45032|14|Not recorded|p8,12||Tertiary|Tb.1., Pl.1.||||||
2718|Brunette Limestone|45052|4|Described|p136|||Cainozoic||||||
2718|Brunette Limestone|45064|4|Described|Table 1|||||||||
2718|Brunette Limestone|45148|4|Described|p24|||||||||
2718|Brunette Limestone|48925|6|Mentioned|p13|||Fauna. Miocene ? age||||||
2718|Brunette Limestone|60637|5|Briefly described|Map legend|||White chalchedonic limestone with chert nodules, chachedony, some sandstone.||||||
2718|Brunette Limestone|60703|6|Mentioned|p714, p725 Fig. 18|Tertiary|Tertiary|||||||12-APR-05
2718|Brunette Limestone|61155|5|Briefly described|p16|Middle Miocene||Age: <11.5Ma. Thickness: 12m.  Geological region: Barkly Tableland.||||||03-MAR-10
2718|Brunette Limestone|62657|5|Briefly described|Map Legend|Cenozoic|Cenozoic|Limestone: cherty and chalcedonic||||||
2718|Brunette Limestone|64068|5|Briefly described|p79, p43|Cenozoic|Cenozoic|Central Georgina Basin. Coeval with Austral Downs Limestone, but occupies a distinct drainage system. Lower part correlated with Poodyea Formation.||||||
2718|Brunette Limestone|64443|5|Briefly described|iii, p5 Fig.3, p6 Tb.1, p18-24, p31|Neogene|Miocene|Max 18m thick. Lithologically identical with Austral Downs Limestone; distinguished geographically: this unit is within drainage areas centred on lakes in south-central BRUNETTE DOWNS.||||Unconformably overlies Camooweal Dolostone, Ranken Limestone and Wonarah Formation.|Limestone, silicified to chert and chalcedony. Characteristic features include rhizoliths, Cambrian pebbles, alveolar texture, circum- and intragranular cracks.|14-MAY-14
2718|Brunette Limestone|65336|5|Briefly described|Map Legend|Cenozoic|Cenozoic|Cherty and chalcedonic limestone. Unconformably overlies Camooweal Dolostone of Barkly Group.||||||
2718|Brunette Limestone|65337|6|Mentioned|p69.|Cenozoic|Cenozoic|In BRUNETTE DOWNS, ALROY and RANKEN areas. May correlate with Cleanskin beds, Austral Downs Limestone and Golliger beds.||||||
2718|Brunette Limestone|65344|5|Briefly described|p3 Fig. 2, p7 Tables 1, 2, p13, 45-47|Miocene|Miocene|Of the Barkly Sub-basin, Georgina Basin. Thickness: 6.5m in BN04DD01. See thin section descriptions for detail.||||Overlies the Anthony Lagoon beds.||03-MAY-12
2718|Brunette Limestone|67144|5|Briefly described|Map legend.|Neogene|Paleogene||||||Cherty and chalcedonic limestone.|
2718|Brunette Limestone|67149|5|Briefly described|Map legend.|Neogene|Paleogene||||||Cherty and chalcedonic limestone.|
2718|Brunette Limestone|67150|5|Briefly described|Map legend.|Neogene|Paleogene||||||Cherty and chalcedonic limestone.|
2718|Brunette Limestone|67352|4|Described|v,p23,p25,p34-35,p38-40,p47,p51,p69|Miocene|Miocene|Noakes and Traves (1954). From 5 to 18 m thick.||||Overlies Anthony Lagoon Formation unconformably.|Massive, nodular to brecciated or tuffaceous, pale grey terrestrial carbonate rocks: dolomicrosparstone or mixed calci/dolomicrosparstone; selectively silicified to chert, megaquartz and chalcedony.|
2718|Brunette Limestone|69443|6|Mentioned|p28:22|Miocene|Miocene|||||Unconformably overlies Anthony Lagoon Formation.||12-JUL-16
2718|Brunette Limestone|69458|5|Briefly described|p42:19-21|||Noakes and Traves (1954). Up to 18m thick. Scattered rubbly outcrops with local prominent outcrops of strongly silicified limestone. Contains rhizoliths, petrified plant roots, minor alveolar texture, clay cutans, and rare Microidium.||||Overlies Golliger beds and (unconformably) Anthony Lagoon Formation. Is correlated with the Austral Downs Limestone.|Massive, nodular to brecciated or tuffaceous, pale grey terrestrial carbonate rocks: calci/dolomicrosparstone, selectively silicified to white, purple-brown and/or red/brown nodular chert, megaquartz and chalcedony.|14-SEP-18
2718|Brunette Limestone|72516|6|Mentioned|p98|Neogene|Neogene|Western and central Georgina Basin. Interpreted to be an age equivalent of the Waite Formation of the Waite Basin.||||||09-JUN-21
2782|Bucket Spring Member|28255|5|Briefly described|p76|||Division of the Ranford Formation by Pontifex et al (1968). on theAUVERGNE sheet.  Cannot be correlated with members named in Western Australia (names probably obsolete now?). .||||||
2782|Bucket Spring Member|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Ranford Formation (Duerdin Group).  Siltstone, micaceous sandstone.||||||02-DEC-04
2782|Bucket Spring Member|32701|4|Described|Table 1|||Adelaidean. See also p15. Duerdin Group||||||02-AUG-06
2782|Bucket Spring Member|45112|5|Briefly described|Table 18|||||||||
2782|Bucket Spring Member|48938|2|Defined|p71|Adelaidean|Adelaidean|||||||
2782|Bucket Spring Member|60006|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Wolfe Creek Basin. Of Ranford Formation, Duerdin Group. Unconformably overlies Bullo River Sandstone and Black Point Sandstone Member. Overlain by Beasly Knob Member. Siltstone, sandstone.||||||
2782|Bucket Spring Member|60682|5|Briefly described|p17 Table 4, 19|Neoproterozoic|Neoproterozoic|Of Ranford Formation. Overlies: Bullo River Sandstone. Partially equivalent to Moonlight Valley Tillite. Conformably overlain by Beasly Knob Member. Max. Thickness: <55m. Geological Province: Wolfe Creek Basin.||||||
2782|Bucket Spring Member|65331|5|Briefly described|Map legend|Neoproterozoic |Neoproterozoic |Of Ranford Formation, Wolfe Creek Basin. Siltstone, sandstone||||||
2782|Bucket Spring Member|69442|5|Briefly described|p27:3-4|||Wolfe Basin. Fluvial or marine glacial deposits. 55m thick.||Ranford Formation.||Overlies Bullo River Sandstone conformably (presumably). Is overlain gradationally by Beasly Knob Member. Partial lateral equivalent of Moonlight Valley Tillite.|Interbedded siltstone and fine-grained micaceous sandstone. Abundant ripple forms occur at the top of the unit.|12-JUL-16
2782|Bucket Spring Member|69673|6|Mentioned|p190|||||Ranford Formation||||
2782|Bucket Spring Member|70206|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Wolfe Basin. [previously of Ranford Formation. Ranford Formation not shown in legend]||Duerdin Group|||Siltstone, sandstone.|18-JUL-16
2782|Bucket Spring Member|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, siltstone|
2790|Buckingham Bay Sandstone|9534|5|Briefly described|Map legend||Cambrian|Of the Wessel Group.  Massive to blocky white quartz sandstone, clayey sandstone.||||||07-JUL-04
2790|Buckingham Bay Sandstone|9691|5|Briefly described|Map Legend|||Of the Wessel Group. Massive to blocky white quartz sandstone, clayey sandstone.||||||
2790|Buckingham Bay Sandstone|9701|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Wessel Group. Massive to blocky white quartz sandstone, clayey sandstone.||||||02-JUN-05
2790|Buckingham Bay Sandstone|9733|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Wessel Group. Massive to blocky white quartz sandstone, clayey sandstone.||||||
2790|Buckingham Bay Sandstone|22600|4|Described|Map legend|Neoproterozoic|Neoproterozoic|||||||
2790|Buckingham Bay Sandstone|23374|3|Fully described|Tb3p22,20,21,23,24,27|Neoproterozoic|Neoproterozoic|Of Wessel Group. Geological Province:  Arafura Basin.||||||02-AUG-06
2790|Buckingham Bay Sandstone|24049|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Wessel Group. Sandstone: white to red, fine to coarse-grained, mostly medium to thick-bedded, commonly cross-bedded, rare mudstone interbeds; common basal breccia or conglomerate. Geol. Prov: Arafura Basin.||||||13-OCT-05
2790|Buckingham Bay Sandstone|32660|5|Briefly described|Table 7|||||||||
2790|Buckingham Bay Sandstone|36535|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
2790|Buckingham Bay Sandstone|36635|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
2790|Buckingham Bay Sandstone|37815|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
2790|Buckingham Bay Sandstone|40810|5|Briefly described|p13|||||||||
2790|Buckingham Bay Sandstone|42058|5|Briefly described|p113|||||||||
2790|Buckingham Bay Sandstone|42597|5|Briefly described|Map Legend|Adelaidean||||||||
2790|Buckingham Bay Sandstone|43010|2|Defined|p174|Middle Cambrian|Early Cambrian|Of Wessel Group.||||||02-AUG-06
2790|Buckingham Bay Sandstone|44112|3|Fully described|Table13p74,75||Cambrian|||||||
2790|Buckingham Bay Sandstone|44338|14|Not recorded|p.7,opp.6|||Basal fm of Wessel Group. (C53-14).||||||
2790|Buckingham Bay Sandstone|44339|14|Not recorded|map legend||Neoproterozoic|Upper Proterozoic.||||||
2790|Buckingham Bay Sandstone|44475|2|Defined|p.8,opp.p.6,Tb.1,map||Neoproterozoic|(C53-15,16). Upper Proterozoic. Overlain by Raiwalla Shale; unconformably overlies Astell Sandstone.||||||02-AUG-06
2790|Buckingham Bay Sandstone|44476|14|Not recorded|map legend||Neoproterozoic|Upper Proterozoic.||||||
2790|Buckingham Bay Sandstone|45162|6|Mentioned|p153|||||||||
2790|Buckingham Bay Sandstone|46639|5|Briefly described|Map legend|Cambrian|Cambrian|Of the Wessel Group. Massive to blocky white quartz sandstone. Overlain by Raiwalla Shale (of Wessel Group).||||||14-AUG-07
2790|Buckingham Bay Sandstone|46792|6|Mentioned|p53|||Correlation||||||
2790|Buckingham Bay Sandstone|46955|6|Mentioned|p159|||||||||
2790|Buckingham Bay Sandstone|50586|5|Briefly described|p2.1|Cambrian|Cambrian|Overlies: Nimbuwah Complex (unconformably).||||||
2790|Buckingham Bay Sandstone|60550|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Wessel Group. Massive to blocky whte quartz sandstone, clayey sandstone.||||||
2790|Buckingham Bay Sandstone|60571|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of the Wessel Group. Sandstone: white to orange/red, fine- to coarse-grained, medium- to thick-bedded, planar cross-bedded; rare mudstone interbeds. Geological Province: Arafura Basin.||||||30-NOV-04
2790|Buckingham Bay Sandstone|61403|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Wessel Group. Sandstone: white to red, fine to coarse-grained, mostly medium to thick-bedded, commonly cross-bedded, rare mudstone interbeds; commo n basal breccia or conglomerate. Geol. Prov: Arafura Basin.||||||
2790|Buckingham Bay Sandstone|61560|5|Briefly described|p490|Neoproterozoic|Neoproterozoic|Overlies McArthur Basin sediments.  Form basal sediments of the Arafura Basin succession. Probably a correlative of the "Yingundji formation" found within the Liverpool Breccia ring around the Liverpool impact crater.||||||02-AUG-06
2790|Buckingham Bay Sandstone|61561|5|Briefly described|p531, p533|Neoproterozoic|Neoproterozoic|Of the Wessel Group. Commonly cross-bedded, moderately well sorted, medium- to coarse-grained, medium- to thickly-bedded; bedding thins progressively upwards. Overlain by Raiwalla Shale.||||||
2790|Buckingham Bay Sandstone|62504|5|Briefly described|p1, 2|Neoproterozoic|Neoproterozoic|Of the Wessel Group. Underlies Raiwalla Shale.||||||
2790|Buckingham Bay Sandstone|62505|4|Described|p3|Neoproterozoic|Neoproterozoic|Of the Wessel Group. Underlies: Raiwalla Shale. ||||||
2790|Buckingham Bay Sandstone|62788|5|Briefly described|p103, p104|Neoproterozoic|Neoproterozoic|Arafura Basin. Dated as Cambrian because of presumed Skolithos trace fossils (Plumb 1963) but reassigned as Neoproterozoic when they were reinterpreted as dewatering structures (Rawlings et al. 1997).||Basal unit of Wessel Group.||Underlies Raiwalla Shale.||28-MAR-12
2790|Buckingham Bay Sandstone|63062|5|Briefly described|p11|Neoproterozoic|Neoproterozoic|Of the Wessel Group. Geological Province: Arafura and Money Shoal Basins.||||||07-FEB-11
2790|Buckingham Bay Sandstone|65337|6|Mentioned|p95.|Ediacaran|Ediacaran|||Unit in Wessel Group.||||
2790|Buckingham Bay Sandstone|65340|6|Mentioned|pp63-64.|||Arhem Bay - Gove area. Contains subvertical tube-like structures, not unlike Skolithos but ascribed an abiogenic origin ( ?water escape conduits) by Rawling et al. (1997). Similar structures occur in the Bukalara Sandstone. ||||||
2790|Buckingham Bay Sandstone|69437|6|Mentioned|p22:4-5|Ediacaran|Ediacaran|Arafura Basin.||||||12-JUL-16
2790|Buckingham Bay Sandstone|69443|5|Briefly described|p28:12|||Onshore Arafura Basin. Reports of the ichnofossil Skolithos were reinterpreted as dewatering structures.||Wessel Group.||Is correlated with Bukalara Sandstone.||12-JUL-16
2790|Buckingham Bay Sandstone|69445|6|Mentioned|p30:5|Neoproterozoic|Neoproterozoic|Arafura Basin. Initially considered Cambrian because of ?Skolithos trace fossils; these were re-interpreted as dewatering structures and the unit was assigned a Neoproterozoic age.||||||12-JUL-16
2790|Buckingham Bay Sandstone|69451|3|Fully described|p35:3-6|Neoproterozoic|Neoproterozoic|Plumb and Roberts (1992). Arafura Basin. Thought to contain the Middle Cambrian fossil Skolithos, but this was reinterpreted as abiogenic dewatering structures. No metazoan fossils found. No complete section through the unit; a reference section/type locality is on the NW side of Flinders Peninsula around the mouth of the Kurala River, where the unit is c.350m thick. Deposition in a high-energy, shallow-marine environment.||Wessel Group.||Is overlain conformably by Raiwalla Shale. Probably correlates with Bukalara Sandstone (Georgina Basin).|White, grey, pale pink, yellow and red, fine- to coarse-grained, mostly medium to thickly bedded sandstone, with common cross-beds and occasionally ripples; rare mudstone interbeds; local basal breccia and conglomerate.|12-JUL-16
2790|Buckingham Bay Sandstone|69673|5|Briefly described|p195|||350m thick.||Wessel Group|||Sandstone, breccia or conglomerate and mudstone.|
2790|Buckingham Bay Sandstone|70968|5|Briefly described|p18, p20|Neoproterozoic|Neoproterozoic|Arafura Basin.||||Unconformably overlies Mainoru Formation.||
2790|Buckingham Bay Sandstone|72377|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Of Arafura Basin.||Unit of Wessel Group.||||
2790|Buckingham Bay Sandstone|73083|6|Mentioned|p33|||||||||
2790|Buckingham Bay Sandstone|73086|6|Mentioned|p118, p122|||Arafura Basin.||||Possibly correlates to Gaylad Sandstone and Pertatataka Formation.||
2809|Buddawadda Basalt Member|23065|6|Mentioned|15|||Geol province Lawn Hill Subprovince. Parent Peters Creek Volcanics||||||
2809|Buddawadda Basalt Member|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
2809|Buddawadda Basalt Member|23406|5|Briefly described|p601 Fig.3|||||||||
2809|Buddawadda Basalt Member|24419|5|Briefly described|p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: Lawn Hill Subprovince (north).||||||07-NOV-08
2809|Buddawadda Basalt Member|35640|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
2809|Buddawadda Basalt Member|36012|3|Fully described|Table 3|||See also p16.||||||01-AUG-07
2809|Buddawadda Basalt Member|36217|6|Mentioned|p206|||Published by Grimes and others 1979. Definition approved by Qld SNC.||||||01-AUG-07
2809|Buddawadda Basalt Member|36439|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
2809|Buddawadda Basalt Member|36442|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
2809|Buddawadda Basalt Member|38237|6|Mentioned|Fig.3|||||||||
2809|Buddawadda Basalt Member|38584|4|Described|p15|||||||||
2809|Buddawadda Basalt Member|39925|6|Mentioned|Fig.9|||||||||
2809|Buddawadda Basalt Member|41721|6|Mentioned|p28|||Of Peters Creek Volcanics. Lower section has been named Buddawadda Basalt Member and is considered to be equivalent to Seigal Volcanics.  Contains vesicular and massive basaltic lavas with interbeds of fine and medium feldspathic and glauconitic sandstone||||||01-AUG-07
2809|Buddawadda Basalt Member|45166|5|Briefly described|p71|||||||||
2809|Buddawadda Basalt Member|49001|2|Defined|p7|Carpentarian|Carpentarian|Basal member of Peters Creek Volcanics.||||||
2809|Buddawadda Basalt Member|67323|5|Briefly described|Mount Isa Block Time-Space Plot.|Paleoproterozoic|Paleoproterozoic|See also GIS attrib tbl. Camooweal-Murphy Domain, Mount Isa Inlier. Leichhardt Superbasin. Abbreviated to Buddawadda Bslt in the Time-Space Plot. See also Buddawaddah Basalt Member (p9).||Peters Creek Volcanics|||Vesicular, amygdaloidal and massive basalt; minor siltstone and sandstone|
2809|Buddawadda Basalt Member|69591|5|Briefly described|p33-34, p38|||Camooweal-Murphy Domain, Leichhardt Superbasin. Correlation with Seigal Volcanics is speculative.||Basal Peters Creek Volcanics.||Equated with the Eastern Creek Volcanics.||
2840|Bukalara Sandstone|22538|6|Mentioned|App1 P722|||||||||
2840|Bukalara Sandstone|22662|6|Mentioned|22|Cambrian|Cambrian|McArthur Basin||||||
2840|Bukalara Sandstone|22853|5|Briefly described|29|Early Cambrian|Early Cambrian|||||||
2840|Bukalara Sandstone|23115|5|Briefly described|p461||Cambrian|||||||
2840|Bukalara Sandstone|23216|5|Briefly described|p36|||||||||
2840|Bukalara Sandstone|23328|5|Briefly described|1030, 1031|||||||||07-SEP-09
2840|Bukalara Sandstone|23374|6|Mentioned|p21|||Equivalent to Buckingham Bay Sandstone. In the Arafura basin.||||||02-AUG-06
2840|Bukalara Sandstone|24442|6|Mentioned|p38|||See also Bukulara Sandstone (misspelt?).  Geological Province: Arafura Basin.||||||
2840|Bukalara Sandstone|31396|6|Mentioned|p1190|||||||||
2840|Bukalara Sandstone|32658|6|Mentioned|Fig.1|||L.Camb.||||||
2840|Bukalara Sandstone|32659|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
2840|Bukalara Sandstone|32660|5|Briefly described|Table 7|||||||||
2840|Bukalara Sandstone|33665|6|Mentioned|Fig.1|||||||||
2840|Bukalara Sandstone|34287|6|Mentioned|p43|||||||||
2840|Bukalara Sandstone|36335|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
2840|Bukalara Sandstone|36439|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
2840|Bukalara Sandstone|36442|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
2840|Bukalara Sandstone|36473|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
2840|Bukalara Sandstone|37644|5|Briefly described|p5.10.1|||||||||
2840|Bukalara Sandstone|38444|6|Mentioned|p307|||||||||
2840|Bukalara Sandstone|38582|6|Mentioned|p218|||||||||
2840|Bukalara Sandstone|38584|4|Described|p21|||||||||
2840|Bukalara Sandstone|39791|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
2840|Bukalara Sandstone|40810|5|Briefly described|p13|||||||||
2840|Bukalara Sandstone|41013|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
2840|Bukalara Sandstone|41268|5|Briefly described|Fig.12|||||||||
2840|Bukalara Sandstone|41319|6|Mentioned|Fig.1|||||||||
2840|Bukalara Sandstone|41406|6|Mentioned|Map legend|Ordovician|Cambrian|||||||
2840|Bukalara Sandstone|41721|4|Described|p29|Cambrian|Cambrian|Thickness: ~100m.  Sequence of red, fine to very coarse feldspathic sandstone and pebble to cobble conglomerate.||||||02-AUG-07
2840|Bukalara Sandstone|41722|6|Mentioned|Map legend|Early Cambrian||||||||
2840|Bukalara Sandstone|42191|6|Mentioned|p448|||||||||
2840|Bukalara Sandstone|42385|4|Described|p29|Early Cambrian||||||||
2840|Bukalara Sandstone|42386|5|Briefly described|Map legend|Early Cambrian||||||||
2840|Bukalara Sandstone|42638|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|||||In schematic section, unconformably? overlies Bessie Creek Formation.|Sandstone, trace fossils. Detailed lithology given.|07-NOV-11
2840|Bukalara Sandstone|42639|2|Defined|p45, p75|||||||||
2840|Bukalara Sandstone|42739|5|Briefly described|map legend|Early Cambrian|Early Cambrian|Fine to very coarse grained friable sandstone; thin to very thick-bedded, low-angle cross stratification; trace fossils.||||||19-OCT-05
2840|Bukalara Sandstone|42812|3|Fully described|p55|||||||||
2840|Bukalara Sandstone|42935|5|Briefly described|p528|||||||||
2840|Bukalara Sandstone|43010|6|Mentioned|p183|||||||||
2840|Bukalara Sandstone|44112|6|Mentioned|p75|||||||||
2840|Bukalara Sandstone|44287|14|Not recorded|p.6,12-18, opp.11|||(E53-3).||||||
2840|Bukalara Sandstone|44288|14|Not recorded|map legend||Early Cambrian|Medium to coarse-grained sandstone, Lower Cambrian.||||||
2840|Bukalara Sandstone|44305|14|Not recorded|p.6,8,10,15-17|||(E53-8). opp.p.6.||||||
2840|Bukalara Sandstone|44306|14|Not recorded|map legend||Early Cambrian|Lower Cambrian.||||||
2840|Bukalara Sandstone|44332|14|Not recorded|p.9,12,opp.6,map|||(D53-14).||||||
2840|Bukalara Sandstone|44333|14|Not recorded|map legend|||Lower Cambrian?||||||
2840|Bukalara Sandstone|44436|5|Briefly described|p.6,7,opp. p.7, map|||(E53-4). See p.11,13, for more details.||||||02-DEC-04
2840|Bukalara Sandstone|44437|5|Briefly described|map legend|Early Cambrian|Early Cambrian|Massive jointed medium- to coarse-grained quartz and feldspathic sandstone, minor pebble and cobble conglomerate.  Unconformably overlies Mainoru Formation and Limmen Sandstone.||||||08-DEC-04
2840|Bukalara Sandstone|44459|14|Not recorded|p.9,13, opp.p.6, map|||(E53-2).||||||
2840|Bukalara Sandstone|44460|14|Not recorded|map legend|||Lower Cambrian ?||||||
2840|Bukalara Sandstone|44473|14|Not recorded|p.6,7,opp. p.7|||(E53-7). See also p.10-12,14,15, for more details.||||||
2840|Bukalara Sandstone|44474|14|Not recorded|map legend||Early Cambrian|Lower Cambrian.||||||
2840|Bukalara Sandstone|44475|14|Not recorded|p.8||Cambrian|(C53-15,16). No longer compared with Wessel Group (Proterozoic). L-M.Cam.||||||
2840|Bukalara Sandstone|44482|14|Not recorded|p.10, opp. p.6 ; map|||(E53-12).||||||
2840|Bukalara Sandstone|44483|5|Briefly described|map legend|||Lower Cambrian?||||||
2840|Bukalara Sandstone|44530|14|Not recorded|p.6,7,12, opp.12,16|||(D53-15).||||||
2840|Bukalara Sandstone|44531|14|Not recorded|map legend||Early Cambrian|Lower Cambrian.||||||
2840|Bukalara Sandstone|45032|14|Not recorded|p9||Early Cambrian|Tb.1,10, Pl.1. (E53-7,12).||||||
2840|Bukalara Sandstone|45064|4|Described|Table 1|||||||||
2840|Bukalara Sandstone|45148|6|Mentioned|p9|||||||||
2840|Bukalara Sandstone|45162|3|Fully described|p152|||Mention p45.||||||02-AUG-06
2840|Bukalara Sandstone|45166|5|Briefly described|Table 15|||||||||
2840|Bukalara Sandstone|45168|6|Mentioned|p17|||||||||
2840|Bukalara Sandstone|46792|6|Mentioned|p53|||Correlation||||||
2840|Bukalara Sandstone|46915|6|Mentioned|p161|||||||||
2840|Bukalara Sandstone|46955|5|Briefly described|p159|||||||||
2840|Bukalara Sandstone|46968|6|Mentioned|Fig.1|||||||||
2840|Bukalara Sandstone|60574|5|Briefly described|Map Legend||Mesoproterozoic|White medium-to coarse-grained lithic sandstone, pebbly sandstone and cobble conglomerate with large trough cross-beds; local water escape structures.||||||02-AUG-06
2840|Bukalara Sandstone|61560|5|Briefly described|p487|Neoproterozoic|Neoproterozoic|Flat-lying rocks which have buried the Foelsche impact crater in the McArthur Basin. Infilling sediments conglomeratic sandstone containing shocked clasts displaying petrographic indicators and planar fractures in quartz.||||||
2840|Bukalara Sandstone|62376|5|Briefly described|p38|Cambrian|Cambrian|Geological Province: Beetaloo Sub-Basin.||||||09-FEB-10
2840|Bukalara Sandstone|62659|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Pink or yellow, friable, medium to coarse grained lithic sandstone; minor fine grained sandstone; basal pebbly sandstone and pebble to cobble conglomerate.||||||
2840|Bukalara Sandstone|64784|5|Briefly described|p2 Fig.2, p6 Fig.4  |Proterozoic|Proterozoic|Beetaloo Basin.||||Overlies Hayfield Mudstone. Is overlain by Antrim Plateau Volcanics.||
2840|Bukalara Sandstone|64815|6|Mentioned|p5, p19  |Cambrian|Cambrian|Georgina Basin. Blankets parts of McArthur Basin.||||||
2840|Bukalara Sandstone|64816|6|Mentioned|p2, p3 Fig.2, p10 Tb.1|Cambrian|Cambrian|Traces of hydrocarbon staining were found in this unit.||||||
2840|Bukalara Sandstone|65232|6|Mentioned|p5 Fig. 4|||Geol. Prov: Pine Creek Orogen [Included in a figure titled "Geology of the Pine Creek Orogen', but this unit prob not part of the Orogen] .||||||09-FEB-10
2840|Bukalara Sandstone|65236|5|Briefly described|p3 Fig. 3|Cambrian|Cambrian|Geological province: Beetaloo Sub-basin.||||||04-JUN-09
2840|Bukalara Sandstone|65337|4|Described|p v, p8, pp 60-62.|Ediacaran|Ediacaran|Basal deposits of Georgina Basin in northwest MOUNT DRUMMOND area. Forms isolated mesas and incised plateaux with a characteristic strongly jointed photopattern. One of youngest units overlain by Antrim Plateau Volcanics.||Unit in Kiana Group.||Unconformably overlies South Nicholson Group. Is overlain by Cox Formation and Nutwood Downs Volcanics.|Mainly pseudokarstically weathered, pink or yellow, friable, medium- to coarse-grained lithic sandstone and lesser fine-grained sandstone; basal pebbly quartz sandstone and pebble to cobble conglomerate common.|
2840|Bukalara Sandstone|65340|4|Described|pp63-64, pp66-67.|Neoproterozoic|Neoproterozoic|Fills in palaeovalleys and palaeosinkholes in underlying units. Contains subvertical tube-like structures interpreted by Rawlings et al.(1997) as water-escape conduits. Fluviatile to shallow marine environments. The Calvert Fault is expressed as a sinuous network of strike-slip fault splays. Forms a 6 km diameter circular outcrop at the Foelsche impact structure.||||Overlies Tawallah Group and Karns Dolomite. Is overlain by Antrim Plateau Volcanics.|Basal thickly bedded, poorly sorted, pebbly to cobbly sandstone and clast- and matrix-supported conglomerate; overlying friable, very thickly bedded, medium to very coarse lithic to quartzose sandstone with a cherty provenance; fine sandy interbeds.|
2840|Bukalara Sandstone|67144|5|Briefly described|Map legend.|Ediacaran|Ediacaran|||Unit in Kiana Group.||Unconformably overlies Mittiebah Sandstone. Is unconformably overlain by Top Springs Limestone.|Thickly to very thickly bedded, fine- to very coarse-grained quartz, feldspathic and lithic sandstone; lesser pebble to cobble conglomerate.|
2840|Bukalara Sandstone|67352|4|Described|v, p4, p16-17, p19, p46, p47, p49-51|Ediacaran|Ediacaran|Forms a high dissected plateau with characteristic strongly jointed photopattern. Max. thickness 300 m.||Kiana Group||Overlain by Cox Formation (conformably), Helen Springs Volcanics (unconformably) or Top Springs Limestone (unconformably).|Fine to medium quartz sandstone and associated pebble conglomerate, fine to very coarse feldspathic sandstone, and friable, medium to coarse lithic sandstone and lesser fine sandstone and cobble conglomerate.|
2840|Bukalara Sandstone|69018|6|Mentioned|p450 Fig.1b|||||||||
2840|Bukalara Sandstone|69423|6|Mentioned|p8:4 Fig.8.7|Neoproterozoic|Neoproterozoic|Georgina Basin.||||||12-JUL-16
2840|Bukalara Sandstone|69430|5|Briefly described|p15:24, 34, 49, 56-58, 62|Neoproterozoic|Neoproterozoic|Is shown [incorrectly] as part of Roper Group on 15:34. Fair to good conventional hydrocarbon reservoirs occur.||Kiana Group.||Unconformably overlies Amelia Dolostone, and Karns Dolostone (Nathan Group). Is intruded by Merlin kimberlite.|Fine- to very coarse-grained friable sandstone; thin to very thickly bedded, low-angle cross-stratified; trace fossils.|12-JUL-16
2840|Bukalara Sandstone|69434|5|Briefly described|p19:4|Neoproterozoic|Neoproterozoic|Georgina Basin.||||Unconformably overlies South Nicholson Group.||12-JUL-16
2840|Bukalara Sandstone|69437|5|Briefly described|p22:4-5, 7|Ediacaran|Ediacaran|Northern Georgina Basin.||Kiana Group.||||12-JUL-16
2840|Bukalara Sandstone|69443|4|Described|p28:7, 12-14, 21, 32|Ediacaran|Ediacaran|Dunn (1963). Central-northern Georgina Basin. Widespread. Crops out as sandstone mesas and plateaux with a characteristic NW to W strongly jointed photopattern. High-energy braided fluviatile to shallow-marine deposits. Reports of the ichnofossil Skolithos were reinterpreted as dewatering structures. Up to c.300m thick. Is correlated with Buckingham Bay Sandstone.||Kiana Group.||Unconformably overlies Roper and South Nicholson Groups. Is overlain conformably by Cox Formation, and unconformably by Helen Springs Volcanics. Is overlain disconformably by Top Springs Limestone.|Fine- to medium-grained quartz sandstone and pebble conglomerate, fine- to very coarse-grained feldspathic sandstone, friable medium- to coarse-grained lithic sandstone, lesser fine-grained sandstone and cobble conglomerate; minor interbedded shale.|12-JUL-16
2840|Bukalara Sandstone|69445|5|Briefly described|p30:4-5, 17|Neoproterozoic|Neoproterozoic|Initially considered Cambrian because of ?Skolithos trace fossils; these were re-interpreted as dewatering structures and the unit was assigned a Neoproterozoic age.||||Is overlain unconformably by Antrim Plateau Volcanics. Correlated with Buckingham Bay Sandstone.||12-JUL-16
2840|Bukalara Sandstone|69451|6|Mentioned|p35:5-6|||Georgina Basin.||||Is overlain by Cox Formation. Probable correlate of Buckingham Bay Sandstone (Arafura Basin).||12-JUL-16
2840|Bukalara Sandstone|69591|6|Mentioned|p53|Neoproterozoic|Neoproterozoic|||||Unconformably overlies South Nicholson Group.||
2840|Bukalara Sandstone|69673|6|Mentioned|p32, p39, p40, p46, p116, p129|||Maximum thickness of 300m. Regarded as having very good reservoir properties.||Kiana Group||Unconformably overlain by Helen Springs Volcanics, conformably overlain by Cox Formation|Fine to very coarse grained, quartz, feldspathic and lithic sandstone, minor interbedded pebble conglomerate, cobble conglomerate and shale.|
2840|Bukalara Sandstone|70849|5|Briefly described|Map legend.|Cambrian|Cambrian|Georgina Basin.||||Unconformably overlies Mittiebah Sandstone (South Nicholson Group).|Fine- to very coarse-grained feldspathic sandstone, quartz sandstone, pebble to cobble conglomerate.|
2840|Bukalara Sandstone|70968|5|Briefly described|p75, p84, p124-125, p131|Neoproterozoic|Neoproterozoic|Base of Georgina Basin succession. Fence diagram of wells in Beetaloo Sub-basin.||Kiana Group.||Unconformably overlies Chambers River Formation. Is overlain unconformably by Antrim Plateau Volcanics.||
2840|Bukalara Sandstone|71059|6|Mentioned|p3|Neoproterozoic|Neoproterozoic|||||Unconformably overlies Chambers River Formation.||
2840|Bukalara Sandstone|71369|6|Mentioned|p1, p49-50|Ediacaran|Ediacaran|||||Unconformably overlies South Nicholson Group.||20-FEB-18
2840|Bukalara Sandstone|71374|5|Briefly described|p21|Neoproterozoic|Neoproterozoic|||||Unconformably overlies the Chambers River Formation.||
2840|Bukalara Sandstone|71632|5|Briefly described|Map legend.|||Georgina Basin. Mapped with Antrim Plateau Volcanics, Cox Formation, Nutwood Downs Volcanics and Top Springs Limestone as a single unit.||||||
2840|Bukalara Sandstone|72526|4|Described|p2, p4, p6, p7, p8, p76-84, p86-87|Neoproterozoic|Neoproterozoic|Basal succession of the Georgina Basin. Age of deposition poorly constrained, but most likely late Neoproterozoic. U-Pb SHRIMP maximum depositional age determined. Georgina Basin. Underlying Jamison sandstone has an MDA of 959+/-18 Ma, which supports Neoproterozoic deposition for Bukalara Sandstone. Shown as located in the Urapunga Fault Zone, Beetaloo Sub-basin and northern part of the Batten Fault Zone. Up to 300 m thick.|1170+/-15 Ma max.dep. age.|Kiana Group||Shown as overlying Karns Dolostone and underlying Barkly Group and Nutwood Downs Volcanics.|Includes medium-grained quartz sandstone and pebble conglomerate, fine to very coarse-grained feldspathic sandstone, friable, medium to coarse-grained lithic and fine-grained sandstone, sandstone and cobble conglomerate, and minor interbedded shale.|
2840|Bukalara Sandstone|72527|6|Mentioned|p5, p7 Fig.1.4.|Neoproterozoic|Neoproterozoic|Shown as underlying undifferentiated Cambrian Georgina Basin.||||Unconformably overlies Mullera Formation.||
2840|Bukalara Sandstone|72718|6|Mentioned|p7|||Southern McArthur Basin.||||Partly underlain by Hayfield mudstone. Partly overlain by Cox formation and[?] Antrim Plateau Volcanics||
2840|Bukalara Sandstone|72912|5|Briefly described|p5 Fig.3, p24,  p31 Fig.11.|Neoproterozoic|Neoproterozoic|Georgina Basin. Shown as Mesoproterozoic on p5.||Kiana Group||Overlies Hayfield Mudstone.||
2840|Bukalara Sandstone|72919|5|Briefly described|p1, p5, p96-97|Neoproterozoic|Neoproterozoic|Underlies Cambrian successions of the Georgina Basin. A maximum deposition age of 1170 +/- 15 Ma was reported by Anderson et al. (2019) although the true depositional age may be considerably younger (Rawlings et al., 2008; Piesch et al., 1991). New data herein finds that strata previously interpreted as possibly Mittiebah Sandstone in drillhole CRDD001 is more likely to represent this unit (Bukalara Sandstone) based on similar detrital zircon signatures (included a new U-Pb SHRIMP zircon maximum depositional age of 1316 +/- 27 Ma, which does not help constrain the true depositional age).|1170 +/- 15 Ma (MDA)|Kiana Group||Unconformably underlain by Mullera Formation (Accident Subgroup, South Nicholson Group).||
2840|Bukalara Sandstone|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|Southern McArthur Basin, Roper Superbasin.||||Underlain by Hayfield Mudstone.||
2840|Bukalara Sandstone|73043|6|Mentioned|p7 Fig.2|Neoproterozoic|Neoproterozoic|||||||
2840|Bukalara Sandstone|73083|6|Mentioned|p27, p43, p46-47|Neoproterozoic|Neoproterozoic|Georgina Basin.||Kiana Group||Unconformably overlain by Top Springs Limestone.|Includes quartzite and sandstone.|
2840|Bukalara Sandstone|73086|6|Mentioned|p118|||Georgina Basin, northern. [Also written as Bukalara Formation, p122].||||Possibly correlates to Gaylad Sandstone and Pertatataka Formation.||
2843|Bukalorkmi Sandstone|23937|1|Redefined|p74 App. 1, p44|Calymmian|Calymmian|Previously Bukalorkmi Sst. Mbr. (McMinn Fm).  Upgraded to formation in Maiwok Subgp (Roper Gp). Conformably under Chambers River Fm; disconformably over Kyalla Fm.  Age: <1429+/-31Ma. Max. thickness: 20m.  Geol.Prov: McArthur Basin.||||||23-DEC-09
2843|Bukalorkmi Sandstone|24047|6|Mentioned|p106 Appendix 1|||Geological Province: McArthur Basin.||||||
2843|Bukalorkmi Sandstone|41268|6|Mentioned|p292|||||||||
2843|Bukalorkmi Sandstone|60573|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Roper Group. Quartz sandstone, thin to medium bedded.  Does not outcrop in the Roper River mapsheet area.||||||23-DEC-09
2843|Bukalorkmi Sandstone|61390|5|Briefly described|Map Legend|Ectasian|Calymmian|Of the Maiwok Subgroup. Quartz sandstone: thin to medium bedded, trough cross stratified, fine grained, ripple markes.||||||29-SEP-05
2843|Bukalorkmi Sandstone|64784|6|Mentioned|p3 |||McArthur Basin.||||||
2843|Bukalorkmi Sandstone|68193|5|Briefly described|p5|Calymmian|Calymmian|Hosts the Roper Field kimberlitic dykes.|1492 +/- 31 Ma (Abbott and Sweet, 2000).|||||
2843|Bukalorkmi Sandstone|69430|4|Described|p15:3, 27, 29-30, 59|Calymmian|Calymmian|Abbott et al. (2001) who raised the unit to Formation status and defined it. Originally (Dunn, 1963) the Bukalorkmi Sandstone Member of the McMinn Formation. Roper River region, southern McArthur Basin. 10-20m thick. Coastal tidal platform sediments.||Maiwok Subgroup.||Overlies Kyalla Formation probably disconformably (sharp and probably erosional contact). Is overlain probably conformably by Chambers River Formation. Is intruded by the Blackjack kimberlite.|Thinly to medium bedded, trough cross-stratified, well-sorted, fine quartz sandstone.|12-JUL-16
2843|Bukalorkmi Sandstone|69673|6|Mentioned|p16 fig 13|||Southern McArthur Basin.||Maiwok Subgroup||||
2843|Bukalorkmi Sandstone|70897|6|Mentioned|Fig.1.7.6|||Appears simply as Bukalorkmi. McArthur Basin.||||||
2843|Bukalorkmi Sandstone|70968|3|Fully described|p51, p74, p78-84, p86, p88, p124-127|Ectasian|Ectasian|See also p129, p131, p133, p140, p143. Sweet and Abbott in Abbott et al. (2001) after Dunn (1963) who named it the Bukalorkmi Sandstone Member (of his McMinn Formation). Raised to Formation rank by Abbott et al. (2001). Named after Bukalorkmi Creek. The type section, 80km W of Mount McMinn, is at 368000mE 8351000mN in the URAPUNGA sheet. Forms low cuestas, scarps and dip slopes. 10-20m thick. High-energy tide-dominated shoreline to shallow shelf deposits. Detrital zircon diagram.||Maiwok Subgroup.||Disconformably overlies Kyalla Formation. Is overlain by Chambers River Formation conformably, possibly disconformably. Is intruded by Derim Derim Dolerite sills.|White, light grey to brown, thinly to medium bedded, fine- to coarse-grained and locally granule-rich quartz sandstone with lesser fine-grained micaceous sandstone. Numerous sedimentary structures listed.|
2843|Bukalorkmi Sandstone|71059|4|Described|p3|Mesoproterozoic|Mesoproterozoic|McArthur Basin. 5-40m thick. Coastal tidal platform deposits.||Maiwok Subgroup.||Disconformably overlies Kyalla Formation. Is overlain conformably by Chambers River Formation.|Thinly to medium-bedded, cross-bedded fine quartz sandstone.|
2843|Bukalorkmi Sandstone|71374|6|Mentioned|p21|||||||Overlain by the Chambers River Formation.||
2843|Bukalorkmi Sandstone|71488|5|Briefly described|p141-p143, p149, p151|||Beetaloo Sub-basin. Mistakenly referred to as the Bukalorkmi Formation on p141. ||Maiwok Subgroup||Overlies the Kyalla Formation. Overlain by the Chambers River Formation. Previously correlated with the Jamison sandstone.||
2843|Bukalorkmi Sandstone|71779|5|Briefly described|p2 Fig.1|||Urapunga Region, McArthur Basin.||Maiwok Subgroup||||24-SEP-18
2843|Bukalorkmi Sandstone|71893|3|Fully described|p2-p4, p8, p36-p39|Calymmian|Calymmian|McArthur Basin. The type section occurs as a road cutting on the Roper Highway about 300m east of the Strangways River bridge in southern MOROAK. Appears in Sweet and Abbott in Abbott et al, 2001 after Dunn 1963a. Deposited in a high-energy, tide-dominated shoreline to shallow marine shelf setting. A maximum age of 1417 +/- 29 Ma and 1361 +/- 21 Ma from the Kalala and Wyworrie members of the Maiwok Subgroup are constrained. A minimum age of 1312.9 +/- 0.7 Ma is derived from the Derim Derim Dolerite which intrudes this sandstone.  Zircon description, LAICPMS U-Pb and Hf analysis, results and interpretation are provided.|1563 +/- 19 Ma (Max dep. U-Pb-Hf)|Maiwok Subgroup||Disconformably overlies the Kyalla Formation. Overlain by the Chambers River Formation. Intruded by the Derim Derim Dolerite.|Thinly to medium-bedded, trough cross-stratified, well-sorted, fine-grained quartz sandstone.|
2843|Bukalorkmi Sandstone|72526|5|Briefly described|p8 Fig.1.3.|Ectasian|Calymmian|Shown as located in the Urapunga Fault Zone, Beetaloo Sub-basin and northern part of the Batten Fault Zone.||Maiwok Subgroup||Overlies Kyalla Formation and underlies Jamison sandstone.||
2843|Bukalorkmi Sandstone|72527|6|Mentioned|p10.|Ectasian||Intruded by Derim Derim Dolerite (1312.9+/-0.7 Ma) as dykes and sills||Maiwok Subgroup||||
2843|Bukalorkmi Sandstone|72718|6|Mentioned|p7, p9|||Southern McArthur Basin. Wilton package (uppermost units). Urapunga Fault Zone, southwestern McArthur Basin, and Batten Fault Zone (north). Absent from the Beetaloo Sub-basin.||Maiwok Subgroup, Roper Group||Underlain by Kyalla Formation. Overlain by Derim Derim Dolerite.||
2843|Bukalorkmi Sandstone|72912|5|Briefly described|p5 Fig.3, p20.|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.||Top of Maiwok Subgroup.||Overlies Kyalla Formation and underlies Jamison Sandstone.||
2843|Bukalorkmi Sandstone|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|Southern McArthur Basin, Roper Superbasin.||Maiwok Subgroup, Roper Group||Underlain by Kyalla Formation. Overlain by Jamison Sandstone.||
2843|Bukalorkmi Sandstone|73242|5|Briefly described|p39|||||Maiwok Subgroup, Roper Group||Underlain by Kyalla Formation. Overlain by Chambers River Formation. Intruded by Derim Derim Dolerite.|Includes tidal Sandstone.|
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).||
3012|Bungitina metamorphics|23733|5|Briefly described|p34 Fig.20|||Informal name.||||||
3012|Bungitina metamorphics|23983|6|Mentioned|p42|||||||||
3012|Bungitina metamorphics|38885|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
3012|Bungitina metamorphics|39583|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
3012|Bungitina metamorphics|39887|6|Mentioned|Fig.3|||||||||
3012|Bungitina metamorphics|39898|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Strangways Metamorphic Complex. Amphibolite, biotite gneiss, quartzofeldspathic gneiss, muscovite-biotite schist. Geological Province: Arunta Block.||||||07-NOV-08
3012|Bungitina metamorphics|39931|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
3012|Bungitina metamorphics|40100|5|Briefly described|Table 1|||See also p255.||||||02-AUG-06
3012|Bungitina metamorphics|43568|6|Mentioned|p502|||||||||
3012|Bungitina metamorphics|46730|5|Briefly described|p4, 11|||Of Strangways Metamorphic Complex. Geological Province: Arunta Block.||||||07-JUN-12
3012|Bungitina metamorphics|48992|3|Fully described|p10|Mesoproterozoic|Mesoproterozoic|Prob.Middle Proterozoic. Informal "Redefinition" of Bungitina Granodiorite?||||||
3012|Bungitina metamorphics|68517|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Arunta Block. Early Proterozoic? age.||Of the Strangways Metamorphic Complex.|||Amphibolite, biotite gneiss, quartzofeldspathic gneiss, muscovite-biotite schist.|
3012|Bungitina metamorphics|72378|5|Briefly described|iii,p1,13-15,17-18,20-21|Paleoproterozoic|Paleoproterozoic|Geological province: Aileron Province. Associated with Oonagalabi Cu-Zn-(Ag-Pb) deposit in the Strangways Range in far eastern ALICE SPRINGS 1:250 000 mapsheet. Interpreted to have a predominantly metasedimentary origin; Hussey et al., 2006 describe a succession of metasandstones and metagreywackes with possible minor volcaniclastic beds, intruded by concordant to discordant amphibolite interpreted as mafic sills and dykes. Hussey et al., 2006 reported a maximum depositional age of 1765+\-4 Ma (SHRIMP 207Pb/206Pb zircon). Kositcin et al., 2018 reported magmatic crystallisation ages of 1770+\-4 and 1770+\-5, and zircon rim growth at 1726+\-4 Ma and 1734+\-21 (207Pb/206Pb) from intrusive gneiss samples (see p15, this study), which constrain a minimum depositional age for sedimentary protolith. LA-ICP-MS insitu muscovite geochronology of NTGS AS16MVM020 (gt orthogneiss) yielded the following interpretive results: a) garnet growth at 1772+\-17 Ma (207Pb/206Pb); b) main assemblage growth, fabric development and garnet deformation prior to 1724+\-12 Ma (207Pb/206Pb); and c) fluid infiltration events at 1724+\-12 Ma (207Pb/206Pb), 1669+\-15 Ma (207Pb/206Pb), 1020+\-20 Ma (206Pb/238U) and 450+\-5 Ma (206Pb/238U).||||Underlain by Strangways Metamorphic Complex.||
3134|Burrell Creek Formation|9324|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Finniss River Group. Phyllite; lithic quartz arenite; quartz conglomerate.||||||07-NOV-08
3134|Burrell Creek Formation|22574|5|Briefly described|map|Proterozoic|Proterozoic|Of the Finniss River Group.||||||13-NOV-06
3134|Burrell Creek Formation|22632|5|Briefly described|p520,2,5|Neoproterozoic|Proterozoic|Part of the Finniss River Group.||||||13-NOV-06
3134|Burrell Creek Formation|22810|4|Described|Table2 P4, P13||Proterozoic|Maximum thickness 3000m. Underlain by Mount Bonnie Formation, and South Alligator Group.||||||13-NOV-06
3134|Burrell Creek Formation|23120|5|Briefly described|p428|||Overlain by Tollis Formation.||||||02-AUG-06
3134|Burrell Creek Formation|23121|5|Briefly described|p418|||||||||
3134|Burrell Creek Formation|23122|6|Mentioned|p409|||||||||
3134|Burrell Creek Formation|23216|4|Described|p6, Table1p10|Orosirian|Orosirian|Of the Finniss River Group. Fine- to coarse-grained feldspathic greywacke; mudstone; minor quartz sandstone, volcanolithic pebble conglomerate, banded ironstone. Age: 1885-1870 Ma.||||||14-APR-08
3134|Burrell Creek Formation|23337|5|Briefly described|906 Fig.9|||||||||
3134|Burrell Creek Formation|23437|5|Briefly described|p36|Proterozoic|Proterozoic|||||||
3134|Burrell Creek Formation|23714|4|Described|p10|Proterozoic|Proterozoic|See also page 7 Table 1, page 13. Of Finniss River Group. Max. thickness: 1500 m.||||||
3134|Burrell Creek Formation|23715|5|Briefly described|Map legend||Proterozoic|Of the Finniss River Group, in the Rum Jungle and Central Regions and Litchfield Province||||||
3134|Burrell Creek Formation|23733|6|Mentioned|p5|||||||||
3134|Burrell Creek Formation|23822|5|Briefly described|p299|Proterozoic|Proterozoic|Geological Province: Litchfield Province.||||||
3134|Burrell Creek Formation|23999|5|Briefly described|p7|Paleoproterozoic|Paleoproterozoic|Isoclinally folded; a preferred orientation of sericite imparts a pronounced foliation sub-parallel to bedding; cross-cutting quartz veins are common. See also p6 Fig. 3.||||||07-FEB-11
3134|Burrell Creek Formation|24001|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Siltstone, shaleand phyllite, quartz veins, coarse quartz sandstone, quartz arenite, arkose, quartz pebble conglomerate.||||||
3134|Burrell Creek Formation|24047|5|Briefly described|p5 Fig.4|Paleoproterozoic|Paleoproterozoic|Of the Finniss River Group. Metagreywacke and slate. Unconformably overlain by Petrel Formation. Geological Province: Pine Creek Orogen.  See also p6 Fig. 5.See also p40, p62.||||||07-NOV-08
3134|Burrell Creek Formation|24048|6|Mentioned|p10|||Geological Province: Pine Creek Inlier.||||||
3134|Burrell Creek Formation|24197|5|Briefly described|p105 Tb. 15.1|Paleoproterozoic|Paleoproterozoic|Of the Gerowie Suite. Age: ~1885Ma. Geological Province: Pine Creek Inlier.||||||07-FEB-11
3134|Burrell Creek Formation|24260|6|Mentioned|p1013 Fig.1|||Geological Province: Pine Creek Inlier||||||
3134|Burrell Creek Formation|24340|5|Briefly described|p147 Fig. 3|Paleoproterozoic|Paleoproterozoic|Conformably overlain by the Tollis Formation. Geological Province: Pine Creek Inlier.||||||07-NOV-08
3134|Burrell Creek Formation|24442|5|Briefly described|p30, p40|Paleoproterozoic|Paleoproterozoic|A suite of fine to medium quartz-lithic sandstone, siltstone and interbedded carbonaceous shale. Intruded by Two Sisters Granite.||||||07-NOV-08
3134|Burrell Creek Formation|30559|6|Mentioned|p284|||||||||
3134|Burrell Creek Formation|30831|6|Mentioned|p10|||||||||
3134|Burrell Creek Formation|31435|6|Mentioned|p61|||||||||
3134|Burrell Creek Formation|32170|6|Mentioned|Map legend|early Adelaidean|early Adelaidean|Prob.Lower Adelaidean||||||
3134|Burrell Creek Formation|32660|5|Briefly described|Table 2|||||||||
3134|Burrell Creek Formation|32700|4|Described|Table 1|||Refers Walpole et al. (1968).||||||14-APR-08
3134|Burrell Creek Formation|32873|5|Briefly described|p36|||Lithology. See also Fig.1||||||
3134|Burrell Creek Formation|33278|5|Briefly described|Fig.2|||||||||
3134|Burrell Creek Formation|33376|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
3134|Burrell Creek Formation|34257|6|Mentioned|p445|||L. Prot.||||||
3134|Burrell Creek Formation|35140|6|Mentioned|p322|||See also Fig.2.||||||
3134|Burrell Creek Formation|35465|6|Mentioned|Fig.2|||Summary of positions of magnetic units in the Lower Proterozoic||||||
3134|Burrell Creek Formation|37579|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Micaceous sandy siltstone.||||||07-NOV-08
3134|Burrell Creek Formation|38239|6|Mentioned|Fig.2|||||||||
3134|Burrell Creek Formation|38349|6|Mentioned|Table 4|||||||||
3134|Burrell Creek Formation|38351|6|Mentioned|Table 3|||||||||
3134|Burrell Creek Formation|38557|6|Mentioned|p287|||||||||
3134|Burrell Creek Formation|39068|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Finnis River Group. Siltstone; shale; sandstone (quartz arenite, sublitharenite); quartz-pebble conglomerate; metamorphosed to lower greenschist facies.||||||31-MAR-06
3134|Burrell Creek Formation|39069|4|Described|p13|||||||||
3134|Burrell Creek Formation|39357|4|Described|p12|||See also p3.||||||02-AUG-06
3134|Burrell Creek Formation|39518|3|Fully described|p9|||||||||
3134|Burrell Creek Formation|39563|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
3134|Burrell Creek Formation|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
3134|Burrell Creek Formation|39801|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Finnis River Group. Siltstone, shale, greywacke, quartz pebble conglomerate.||||||07-NOV-08
3134|Burrell Creek Formation|39889|4|Described|p491|||See also p492.||||||02-AUG-06
3134|Burrell Creek Formation|40168|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Finnis River Group. Fine to coarse feldspathic greywacke, shale, slate, phyllite and siltstone.||||||07-NOV-08
3134|Burrell Creek Formation|40223|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Finniss River Group. Brown, grey and red sandy siltstone, siltstone, phyllite, slate and quartz-andalusite-muscovite-biotite-cordierite hornfels.||||||07-NOV-08
3134|Burrell Creek Formation|40243|6|Mentioned|Fig.2|||||||||
3134|Burrell Creek Formation|40248|6|Mentioned|p221|||||||||
3134|Burrell Creek Formation|40493|5|Briefly described|Table 1|||||||||
3134|Burrell Creek Formation|40495|6|Mentioned|Fig.5|||||||||
3134|Burrell Creek Formation|40765|6|Mentioned|p8|||||||||
3134|Burrell Creek Formation|40808|3|Fully described|p13|||||||||
3134|Burrell Creek Formation|40809|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
3134|Burrell Creek Formation|40823|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
3134|Burrell Creek Formation|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
3134|Burrell Creek Formation|41125|5|Briefly described|p55|||Mention Fig.14||||||
3134|Burrell Creek Formation|41294|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
3134|Burrell Creek Formation|41295|4|Described|p9|||||||||
3134|Burrell Creek Formation|41304|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
3134|Burrell Creek Formation|41305|3|Fully described|p17|||||||||
3134|Burrell Creek Formation|41309|4|Described|p6|||||||||
3134|Burrell Creek Formation|41311|4|Described|p10|||||||||
3134|Burrell Creek Formation|41397|6|Mentioned|p11|||||||||
3134|Burrell Creek Formation|41407|6|Mentioned|Map Legend|Proterozoic||||||||
3134|Burrell Creek Formation|41586|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
3134|Burrell Creek Formation|41645|4|Described|p10|||||||||
3134|Burrell Creek Formation|41646|6|Mentioned|Map legend|Paleoproterozoic||Of the Finnis River Group. Phyllite;  quartzarenite, quartz grit; quartz conglomerate +/- clasts of phyllite.||||||07-NOV-08
3134|Burrell Creek Formation|41660|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Phyllite; andalusite phyllite; quartz-mica and andalusite-quartz-mica schists; submature, immature or gritty quartz arenite, or quartz grit; andalusite hornfels; quartz conglomerate +/- Berinka Volcanics clasts +/- phyllite and quartz arenite.||||||07-NOV-08
3134|Burrell Creek Formation|41661|3|Fully described|p10|||||||||
3134|Burrell Creek Formation|41721|6|Mentioned|p4|||L:ithologically resembles Murphy Metamorphics (Murphy Inlier) and Yaringa Metamorphics (Mt Isa Block). Geological province: Pine Creek Geosyncline.||||||01-AUG-07
3134|Burrell Creek Formation|41860|6|Mentioned|p442|||||||||
3134|Burrell Creek Formation|41873|6|Mentioned|Table 2|||||||||
3134|Burrell Creek Formation|41874|5|Briefly described|p11|||||||||
3134|Burrell Creek Formation|41878|6|Mentioned|Fig.25|||||||||
3134|Burrell Creek Formation|42012|3|Fully described|p10|||See also Table 1 p7.||||||02-AUG-06
3134|Burrell Creek Formation|42014|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
3134|Burrell Creek Formation|42163|5|Briefly described|p61|||||||||
3134|Burrell Creek Formation|43140|4|Described|p3||Paleoproterozoic|Of Finniss River Group.||||||07-NOV-08
3134|Burrell Creek Formation|43149|5|Briefly described|Map Legend||Paleoproterozoic|Of Finniss River Group. Of Orosirian age.||||||07-NOV-08
3134|Burrell Creek Formation|43187|5|Briefly described|p2|||||||||
3134|Burrell Creek Formation|43624|5|Briefly described|Table 1,p9,10||Paleoproterozoic|Of Finniss River Group.  Max. thickness: >4000m.||||||07-NOV-08
3134|Burrell Creek Formation|43718|5|Briefly described|p2|||||||||
3134|Burrell Creek Formation|43762|6|Mentioned|p409||Proterozoic|||||||
3134|Burrell Creek Formation|43832|3|Fully described|19-20, Table3 p12||Paleoproterozoic|Only component of Finniss River Group in region. Mt Bonnie Formation underlies. Cullen Batholith intrudes.||||||04-APR-11
3134|Burrell Creek Formation|44201|14|Not recorded|p.7|||||||||
3134|Burrell Creek Formation|44314|2|Defined|p.6-10,map|||(D52-4) DARWIN sheet.||||||13-NOV-06
3134|Burrell Creek Formation|44315|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
3134|Burrell Creek Formation|44399|5|Briefly described|map legend||Paleoproterozoic|Of the Finniss River Group. Greywacke, siltstone, greywacke-siltstone.||||||07-NOV-08
3134|Burrell Creek Formation|45022|3|Fully described|p.7-232.||Paleoproterozoic|Of Finniss River Group.  On many pages.  Fig. 7-13. Tb.2,3. Pl.10,28,30||||||07-NOV-08
3134|Burrell Creek Formation|45112|5|Briefly described|Table 21|||||||||
3134|Burrell Creek Formation|46163|14|Not recorded|p.168,170|||Equivalent to Noltenius Formation.||||||
3134|Burrell Creek Formation|46658|4|Described|p551|||||||||
3134|Burrell Creek Formation|46675|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Siltstone, shale, slate, greywacke, quartz pebble conglomerate. Conformably overlies Mount  Bonnie Formation.||||||07-NOV-08
3134|Burrell Creek Formation|46676|14|Not recorded|map legend.||Paleoproterozoic|See also card 1. Page 6.||||||07-NOV-08
3134|Burrell Creek Formation|46678|5|Briefly described|Table 1|Proterozoic|Proterozoic|Of Finniss River Group.  Greywacke, siltstone, greywacke-siltstone.  Overlies and interfingers with Golden Dyke Formation.  Max. thickness: 8,000 feet.  Density 2.68-2.72.||||||
3134|Burrell Creek Formation|46679|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
3134|Burrell Creek Formation|46848|5|Briefly described|p167|||||||||
3134|Burrell Creek Formation|46877|6|Mentioned|Fig.1|||||||||
3134|Burrell Creek Formation|47049|5|Briefly described|Table|||Extended to cover areas of Fisher Creek Siltstone. Fig.2.||||||
3134|Burrell Creek Formation|48867|14|Not recorded|map|||map. Formation of Finniss River Group.||||||
3134|Burrell Creek Formation|48916|6|Mentioned|p13||Paleoproterozoic|||||||07-NOV-08
3134|Burrell Creek Formation|48942|5|Briefly described|p9|||||||||
3134|Burrell Creek Formation|49744|5|Briefly described|Fig.3|||||||||
3134|Burrell Creek Formation|50586|5|Briefly described|p1.1, 3.1, 4.5, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Of the Gerowie Suite. Intruded by Allia Suite, Cullen Supersuite.||||||07-NOV-08
3134|Burrell Creek Formation|50623|5|Briefly described|p260 Fig.3, p261|Paleoproterozoic|Paleoproterozoic|Turbiditic greywacke. Of Finnis River Group.||||||07-NOV-08
3134|Burrell Creek Formation|60526|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Finniss River Group. Laminated shale, siltstone and phyllite; minor massive quartzose, feldspathic and calcareous greywacke. Overlies: Mount Bonnie Formation.||||||02-NOV-04
3134|Burrell Creek Formation|60575|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Finniss Creek Group.||||||
3134|Burrell Creek Formation|60677|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Siltstone, shale greywacke, quartz pebble conglomerate. Overlies Mount Bonnie Formation. Of Finniss River Group.||||||
3134|Burrell Creek Formation|60680|5|Briefly described|Map legend|Orosirian|Orosirian|Of the Finniss River Group.  Geological Province: Pine Creek Orogen. Thick bedded to massive, fine to coarse feldspathic metagreywacke with graded bedding in places.||||||14-JAN-05
3134|Burrell Creek Formation|60684|6|Mentioned|p19|||Geological Province: Pine Creek Geosyncline.||||||
3134|Burrell Creek Formation|61389|5|Briefly described|Map Legend|||Of the Finniss River Group. Siltstone, shale, greywacke, quartz pebble conglomerate.||||||30-SEP-05
3134|Burrell Creek Formation|62082|6|Mentioned|p127|||Includes saprolites of deeply weathered subround clasts of goethite-stained quartz mica schist set in matrix of quartz, kaolinite and interstratified mica. Geological Province: Pine Creek Terrain.||||||07-FEB-11
3134|Burrell Creek Formation|62375|5|Briefly described|p10 Fig. 3, 18|Paleoproterozoic|Paleoproterozoic|Of the Finniss River Group. Greywacke, siltstone, shale. Conformably overlies Mount Bonnie Formation. Geological Province: Pine Creek Orogen. Thickness: 1000m+.||||||11-FEB-10
3134|Burrell Creek Formation|63866|5|Briefly described|p105, p108-p109|||Litchfield Province, Pine Creek Orogen. ||||||
3134|Burrell Creek Formation|64677|5|Briefly described|p13|||Pine Creek Orogen.||||Is overlain conformably by Chilling Sandstone. Is intruded by Koolendong Granite.||
3134|Burrell Creek Formation|64698|4|Described|lithinterp table|Orosirian|Orosirian|Of Finniss River Group. Age 1862Ma. Max thick 2000m. Brown/grey-green, thickly bedded/massive, fine/coarse feldspathic metagreywacke w some graded beds and minor lenses of volcanilithic pebble conglom; brown/grey, laminated phyllite, slate and mudst.||||||07-JAN-09
3134|Burrell Creek Formation|64730|5|Briefly described|p125 Fig. 3, p126|Paleoproterozoic|Paleoproterozoic|Near maximum deposition age from extrusion ages of Warrs Volcanic Member (1862+/-3 Ma) and laterally equivalent Berinka Volcanics (1861+/-4 Ma).||Of Finniss River Group.||Underlies Chilling Sandstone and Tollis Formation.|Dominated by greywackes and siltstones.|02-MAY-12
3134|Burrell Creek Formation|64731|5|Briefly described|p147, p150|||Lateral equivalent to Welltree Metamorphics?[p150]||Of Finniss River Group.||||12-APR-12
3134|Burrell Creek Formation|64956|4|Described|p2 Tb. 18, p50, p78-79|Paleoproterozoic|Paleoproterozoic|Of the Finniss River Group. Intruded by Fish Billabong Adamellite, Jammine Granite + Two Sisters Granite. Max depositional ages:1868+/-4Ma, 1862+/-3Ma.Geol.prov: Pine Creek Orogen. Sample is immature coarse sandstone.||||||04-APR-11
3134|Burrell Creek Formation|65232|5|Briefly described|p45, p7, p6 Fig. 5, p58, App. 2|Palaeoproterozoic|Palaeoproterozoic|Of Finniss River Group. Conformable over Mount Bonnie Formation (South Alligator Group). Turbiditic greywacke, siltstone, shale, minor felsic volcanics, sandstone, conglomerate.||||||09-FEB-10
3134|Burrell Creek Formation|65339|4|Described|p6 Table 1, pp13-14, p24.|||Forms low rises between sediment-choked drainages. Deposited by mass-transport turbidity flows. Deformed during the Barramundi Orogeny. Low radiometric response. Hosts Bandicoot Prospect gold reefs.||Unit in Finniss River Group.||Overlies Mount Bonnie Formation.|Reddish-brown shale, siltstone and phyllite, colour-banded; fine to very coarse sandstone, greywacke, feldspar and arkose, quartz pebble conglomerate and quartz-mica schist. Crosscutting quartz veins are prolific; pegmatites are common.|
3134|Burrell Creek Formation|67167|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Unit in Finniss River Group.|||Brown to grey-geen feldspathic metagreywacke, thickly bedded to massive, fine to coarse, local graded bedding, minor lenses of volcanilithic pebble conglomerate; laminated phyllite, slate and mudstone; minor quartz-mica schist, quartz-mica hornfels.|
3134|Burrell Creek Formation|67186|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Unit in Finniss River Group.|Includes Warrs Volcanic Member|Is overlain by Chilling Sandstone.  Is partially equivalent to Mulluk Mulluk Volcanics.|Brown to grey-green feldspathic metagreywacke, thickly bedded to massive, fine to coarse, local graded bedding and minor lenses of volcanilithic pebble conglomerate; laminated phyllite, slate and mudstone; minor quartz-mica schist.|23-NOV-11
3134|Burrell Creek Formation|67232|5|Briefly described|p4, p5, p6.|Paleoproterozoic|Paleoproterozoic||Detrital zircons 1865 Ma (Worden et al. 2008a).|Unit in Finniss River Group.||Is intruded by Benning Gabbro.||
3134|Burrell Creek Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Pine Creek area.|1862 +/- 5 Ma.|||Is intruded by Wagait Suite and Jammine Granite.||
3134|Burrell Creek Formation|67355|5|Briefly described|p6-7, p10, p12-14, p21, p67||Orosirian|Disappearance of tuff, banded ironstone or chert beds, and increased arenaceous material marks the boundary between the Mount Bonnie and Burrell Creek Formations. Bouma sequences indicate turbidity flows in a submarine fan. Hosts the Mount Woods, Adelaide River and Virginia mines.||Finniss River Group||Conformably overlies the Mount Bonnie Formation (South Alligator Group). Unconformably underlies the Depot Creek Sandstone.|Arenaceous. Repeated fining-upward Bouma sequences have been observed.|25-JAN-17
3134|Burrell Creek Formation|67564|3|Fully described|p7 Table 2, p9 Fig.4, p22, p24.|Paleoproterozoic|Paleoproterozoic|2000 to 3600 m of proximal mid-submarine fan turbidite deposits. Rocks of this unit mapped by Walpole (1963) are now in the Mount Bonnie Formation; this unit contains rocks Walpole (1963) had mapped as Fisher Creek Siltstone. Detailed descriptions are given of Cu, Au, Pb-Ag deposits.|c.1860 Ma.|Unit in Finniss River Group.||Overlies Mount Bonnie Formation. Is intruded by David Suite, Cullen Supersuite, Zamu and Oenpelli Dolerites. Is overlain by Tollis Formation and unconformably by El Sherana and Katherine River Groups.|Interbedded thickly-bedded to massive, fine to coarse feldspathic metagreywacke and laminated phyllite, slate and mudstone; minor volcanilithic pebble conglomerate; quartz-mica schist.|
3134|Burrell Creek Formation|67779|5|Briefly described|p6 Fig.5.|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen. Age from dominant detrital zircon component.|Max. deposition 1868 Ma.|Unit in Finniss River Group.|Appears to include Meeway and Berinka Volcanics, Mulluk Mulluk and Warrs Volcanic Members.|||18-MAY-18
3134|Burrell Creek Formation|69383|4|Described|p28-41, 44, 49|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen, Central Domain. LA-ICPMS  U-Pb and Hf geochronology analyses. 5 samples. Max deposition ages range from 1874 +/- 10 Ma to 1851 +/-9 Ma. Age from lowest sample in the unit: 1860+/-4 Ma |1860 +/-4 Ma, 1851+/-9 Ma|Of Finniss River Group.||Intruded by Mount Bundy Syenite. Overlain by Tolmer Group. Overlies South Alligator Group|Red, pink or grey gritty sandstone, some with minor muscovite and limonitic alteration of feldspar;  silty sandstone ; sandy siltstone|
3134|Burrell Creek Formation|69418|5|Briefly described|p3:6-7, 11-12, 15, 17, 21|||Pine Creek Orogen. Hosts several gold deposits; also the Anomaly A (Cu-Zn-Pb), Daly River (Cu), and Mount Diamond (Cu-Bi-Au) deposits (described). Also hosts the Adelaide River and George Creek vein-type U deposits (described). Hosts many (named and described) pegmatite Sn-Ta-Nb deposits and three vein Sn deposits (briefly described).|||Warrs Volcanic Member.||Includes schist and phyllite.|12-JUL-16
3134|Burrell Creek Formation|69420|4|Described|p5:4-6, 8, 12-13, 26-27, 29, 31, 33-37|Paleoproterozoic|Paleoproterozoic|See also 39-45, 65, 75, 79, 83-84, 86-88, 93, 99-104, 106-109, 117-118. Central region, Central Domain, Pine Creek Orogen. c.3000m thick. Proximal mid-submarine fan (turbidite) deposits. Detrital zircon maximum deposition age. Deformation and metamorphism occurred after this time but before 1829 Ma. Correlated with Hermit Creek and Welltree Metamorphics. Is also overlain by and folded in with the Dorothy Volcanics; is intruded by the Koolendong, Shoobridge and ?McMinns Bluff Granites. Hosts gold deposits in various goldfields (eg the Batman deposit), described in detail. Hosts the Adelaide River and George Creek U deposits. Hosts numerous Cu, Pb, Zn, Sn +/- Ta deposits: the Sn-Ta-Nb deposits are listed and described in detail. A source of fine sand deposits.|<1851 +/- 9 Ma (Hollis et al., 2009).|Finniss River Group.|Warrs Volcanic Member.|Conformably overlies Mount Bonnie Formation (South Alligator Group). Is overlain conformably by Tollis Formation and Chilling Sandstone. Is interbedded with Berinka, Meeway, Mulluk Mulluk Volcanics.|Interbedded phyllite, slate, mudstone, feldspathic greywacke and minor pebble conglomerate.|12-JUL-16
3134|Burrell Creek Formation|69421|5|Briefly described|p6:3|||Pine Creek Orogen.||Finniss River Group.||Overlies Gerowie Tuff.||12-JUL-16
3134|Burrell Creek Formation|69456|5|Briefly described|p40:6|Proterozoic|Proterozoic|Pine Creek Orogen.||||Is overlain unconformably by Darwin Formation.||12-JUL-16
3134|Burrell Creek Formation|69917|4|Described|p51-53|||Pine Creek Orogen, Central Domain. U/Pb SHRIMP zircon dating, Hf analytical data. Immature coarse sandstone sampled. Conservative maximum depositional age reported. Is consistent with the age of crystallisation of the basal volcanics of the Finniss River Group.|1868+/-4 Ma|Of Finniss River Group|||Shale, phyllite, siltstone and sandstone.|
3134|Burrell Creek Formation|70719|6|Mentioned|p5, p7|||Pine Creek Orogen. Was previously tentatively correlated with Grindall Formation, but their detrital age spectra are markedly different.||||||
3134|Burrell Creek Formation|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Porphyroblastic quartz-mica hornfels, and andalusite schist near granite contact.||Finniss River Group.|Includes Mulluk Mulluk Volcanic Member, Warrs Volcanic Member.||Feldspathic metagreywacke, brown to grey-green, thickly bedded to massive, fine- to coarse-grained, local graded bedding and minor lenses of volcanolithic pebble conglomerate; laminated phyllite, slate and mudstone; minor quartz-mica schist.|01-MAR-18
3134|Burrell Creek Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||greywacke|
3134|Burrell Creek Formation|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|1852+/- 8 Ma (MDA: U-Pb zircon LA-ICPMS).||||Silty sandstone; coarse-grained sandstone; medium-grained quartz sandstone; sandy siltstone.|
3134|Burrell Creek Formation|72527|6|Mentioned|p184, p192.|Paleoproterozoic|Paleoproterozoic|Given as an example of correlated units across the northern Australia with the Murphy Metamorphics. Ref Hollis et al., 2010; Carson, 2013; Cross and Crispe, 2007; Bodorkos et al., 2013; Kositcin et al., 2012, 2013, 2014, 2015a). Part of the Pine Creek Orogen.|||||Includes metamorphosed basement metasedimentary rocks.|
3134|Burrell Creek Formation|73089|6|Mentioned|p32, p36|Orosirian|Orosirian|Pine Creek Orogen, Central Domain. Paleoflow indicators near Pine Creek indicate a locally northerly trending current direction.|1861-1862 Ma|||Underlain[?] by South Alligator Group.||
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|
3176|Burtawurta Formation|14019|4|Described|p15|||Of the Wattie Group. Dominant siltstone and interbedded minor fine sandstone, mudstone and rare dolostone near top. Conformably overlies the Wickham Sandstone. Max Thickness: 30m. Geological Province: Victoria Basin.||||||
3176|Burtawurta Formation|24122|5|Briefly described|p4 Fig. 3|||Of Wattie Group.  Geological Province: Victoria Basin.||||||
3176|Burtawurta Formation|24297|3|Fully described|p6|Proterozoic|Proterozoic|Of Wattie Group. Conformably overlain by Hughie Sandstone, conformably overlies Wickham Formation. Maximum thickness: 53m.  See also p5 Tb. 2.||||||
3176|Burtawurta Formation|24298|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Parent:  Wattie Group. Siltstone, sandstone, dolomitic siltstone, minor dolostone.||||||19-OCT-05
3176|Burtawurta Formation|24441|5|Briefly described|p1 Fig. 1|Mesoproterozoic|Mesoproterozoic|Of the Wattie Group. Overlies the Wickham Formation; overlain by Hughie Sandstone. Geological Province: Victoria Basin.||||||
3176|Burtawurta Formation|24442|5|Briefly described|p50 Fig. 1|||Of the Wattie Group. Geological Province: Victoria Basin.||||||
3176|Burtawurta Formation|28255|3|Fully described|p34, Tb. 11(opp.p8)|Adelaidean|Adelaidean|Of the Wattie Group. Siltstone and sandstone mainly. Conformably overlies Wickham Formation; conformably overlain by Hughie Sandstone. Max. thickness: 38m.||||||08-JUN-05
3176|Burtawurta Formation|30003|4|Described|p8, p12|||Of the Wattie Group. Multicoloured and light grey-green siltstone; colours cut across bedding; minor quartz sandstone, mudstone and dolomite. Carpentarian or Adelaidean.||||||19-APR-05
3176|Burtawurta Formation|30004|6|Mentioned|Map legend|Proterozoic|Proterozoic|Carpentarian or Adelaidean||||||
3176|Burtawurta Formation|32172|4|Described|Table 1|||Carpentarian or Adelaidean||||||
3176|Burtawurta Formation|32173|5|Briefly described|Map legend|Adelaidean|Carpentarian|Of the Wattie Group.  Micaceous siltstone and fine sandstone.  Carpentarian or Adelaidean (per legend).||||||16-NOV-04
3176|Burtawurta Formation|32175|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Wattie Group.  Flaggy siltstone, fine sandstone; minor dolomitic siltstone, dolomite.||||||02-DEC-04
3176|Burtawurta Formation|32660|5|Briefly described|Table 6|||||||||
3176|Burtawurta Formation|33374|5|Briefly described|p7|||See also p9. Strat. tables.||||||02-AUG-06
3176|Burtawurta Formation|33375|4|Described|p7, p9 Tb. 1|Adelaidean|Adelaidean|Of the Wattie Group. Overlies the Wickham Formation. Thin sequence of siltstone and sandstone.||||||26-APR-05
3176|Burtawurta Formation|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
3176|Burtawurta Formation|33378|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Wattie Group.  Chocolate and greyish green siltstone, interbedded fine sandstone.||||||27-APR-05
3176|Burtawurta Formation|45112|6|Mentioned|p19|||||||||
3176|Burtawurta Formation|48943|2|Defined|p43|Proterozoic|Proterozoic|?Adelaidean||||||
3176|Burtawurta Formation|60589|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Wattie Group.  Siltstone, sandstone, dolomitic siltstone, minor dolostone.  Geological Province: Victoria Basin.||||||
3176|Burtawurta Formation|60672|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Siltstone, minor fine sandstone, mudstone, dolostone. Overlies Wickham Formation. Overlain by Hughie Sandstone. Of Wattie Group. Geological Province: Victoria Basin.||||||11-JAN-05
3176|Burtawurta Formation|60685|4|Described|p4 Fig. 3, p6|Paleoproterozoic|Paleoproterozoic|Of the Wattie Group. Micaceous siltstone interbedded with light grey, very fine quartz sandstone and dolostone. Conformably overlies Wickham Formation; conformably underlies Hughie Sandstone. Max. Thickness: 25m. Geological Province: Victoria Basin.||||||07-NOV-08
3176|Burtawurta Formation|65342|6|Mentioned|p11 Fig.13. |||Victoria Basin.||Unit in Wattie Group.||Overlies Wickham Formation. Is overlain by Hughie Sandstone.||
3176|Burtawurta Formation|67151|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Birindudu Basin.||Unit in Wattie Group.||Overlies Wickham Formation. Is overlain by Hughie Sandstone.|Siltstone, interbedded fine sandstone, dolomitic siltstone.|
3176|Burtawurta Formation|68733|5|Briefly described|p177 Fig.2, p178|||A recessive unit. 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).||Wattie Group.||Unconformably underlain by the Wickham Formation.||05-DEC-17
3176|Burtawurta Formation|69432|4|Described|p17:2, 9|||Birrindudu Basin. Probably less than 60m thick. Low-energy shallow-marine deposits with some brine logging of sediments and occasional subaerial exposure.||Wattie Group.||Conformably overlies Wickham Formation. Is overlain conformably by Hughie Sandstone.|Siltstone interbedded with minor fine sandstone, mudstone and rare dolostone near the top. Contains ripple marks, mudcracks and halite casts.|12-JUL-16
3176|Burtawurta Formation|69673|6|Mentioned|p48 fig 35|||||Wattie Group||Overlies Wickham Formation, overlain by Hughie Sandstone||
3176|Burtawurta Formation|70655|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Birindudu Basin.||Wattie Group.||Overlies Wickham Formation. Is overlain by Hughie Sandstone.|Siltstone, interbedded fine sandstone, dolomitic siltstone.|
3176|Burtawurta Formation|70854|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Wattie Group.||Overlies Wickham Formation. Is overlain by Hughie Sandstone.|Siltstone, minor fine sandstone, mudstone, dolostone.|
3176|Burtawurta Formation|70855|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Wattie Group.||Overlies Wickham Formation. Is overlain by Hughie Sandstone.|Siltstone, sandstone, dolomitic siltstone, minor dolostone.|
3176|Burtawurta Formation|71302|5|Briefly described|p6,15||Paleoproterozoic|Of Birindudu Basin.||Unit of Wattie Group.||Overlain conformably by Hughie Sandstone. Underlain by Wickham Formation.||
3176|Burtawurta Formation|72718|6|Mentioned|p7|||Birrindudu Basin.||Wattie Group||Underlain by Wickam Formation. Overlain by Hughie Sandstone.||
3176|Burtawurta Formation|73083|6|Mentioned|p49|||||||||
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.||
3225|Bynoe Formation|14019|5|Briefly described|p4 Fig. 3|||Of the Bullita Group.  Geological Province: Victoria Basin.||||||
3225|Bynoe Formation|24122|3|Fully described|p7, p5 Tb.1|Proterozoic|Proterozoic|Of Bullita Group. Conformably overlies the Skull Creek Formation. Maximum thickness: 190m.  Geological Province: Victoria Basin.||||||
3225|Bynoe Formation|24297|3|Fully described|p12|Proterozoic|Proterozoic|Of Bullita Group.  Unconformably overlain by Weaner Sandstone, conformably overlies Skull Creek Formation. Maximum thickness: 243m.  See also p5 Tb. 2.||||||
3225|Bynoe Formation|24298|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Bullita Group. Dolomitic siltstone and sandstone, dolostone, minor chert.||||||02-AUG-06
3225|Bynoe Formation|24300|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Parent: Bullita Group.   Geological Province: Victoria Basin||||||
3225|Bynoe Formation|24441|4|Described|p1 Fig. 1, p7, App. 2-1:4|Mesoproterozoic|Mesoproterozoic|Of Bullita Gp. Calcareous dolostone, laminated dolomitic siltstone............. Conformably overlies Skull Creek Fm (gradational contact). Unconformably overlain by Mt Gordon Sandstone and Weaner Sst. Max. thickness: 243m. Geol.Prov: Victoria Basin.||||||08-AUG-05
3225|Bynoe Formation|24442|5|Briefly described|p50 Fig. 1|||Of the Bullita Group. Geological Province: Victoria Basin.||||||
3225|Bynoe Formation|28255|3|Fully described|p51, Tb. 11(opp.p8)|Adelaidean|Adelaidean|Supersedes "Coolibah Formation".  Of Bullita Group. Siltstone/dolomitic sandstone. Conformable on Weaner Sst, Jasper Gorge Sst; conformable over Skull Creek Fm in most areas, but may be unconformable, locally, on Bardia Chert Member.  Max. thickness: 38m.||||||08-JUN-05
3225|Bynoe Formation|32170|6|Mentioned|Map legend|Adelaidean|Carpentarian|Adelaidean or Carpentarian||||||
3225|Bynoe Formation|32175|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Bullita Group.  Interbedded reddish brown and greyish green dolomitic siltstone;  grey dolomitic sandstone and dolomite.||||||02-DEC-04
3225|Bynoe Formation|32660|5|Briefly described|Table 6|||||||||
3225|Bynoe Formation|32700|4|Described|Table 1|||See also p14.||||||02-AUG-06
3225|Bynoe Formation|32775|5|Briefly described|Map legend|Adelaidean|Carpentarian|Of the Bullita Group.  Adelaidean or Carpentarian||||||02-DEC-04
3225|Bynoe Formation|33373|3|Fully described|p9|||Table 2.||||||
3225|Bynoe Formation|33374|6|Mentioned|p8|||Strat. table||||||
3225|Bynoe Formation|33375|6|Mentioned|p8 Tb. 1, p11|Adelaidean|Adelaidean|Top unit of the Bullita Group. Greyish green and reddish brown massive siltstone, dolomitic sandstone, dolomite; ripple marks, mud cracks and halite casts. Max. thickness: >100m.||||||26-APR-05
3225|Bynoe Formation|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
3225|Bynoe Formation|33377|6|Mentioned|p266|||||||||
3225|Bynoe Formation|33378|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Bullita Group. Greyish green and reddish brown siltstone, dolomitic sandstone, dolomite.||||||27-APR-05
3225|Bynoe Formation|34983|6|Mentioned|p32|||||||||
3225|Bynoe Formation|45112|6|Mentioned|Table 10|||||||||
3225|Bynoe Formation|48938|6|Mentioned|p20|||Nomenclature table.||||||
3225|Bynoe Formation|48942|2|Defined|p52|Adelaidean|Adelaidean|Strat. section P112.||||||
3225|Bynoe Formation|48943|3|Fully described|p62|||Strat. section p136.||||||02-AUG-06
3225|Bynoe Formation|60682|6|Mentioned|p29|||||||||
3225|Bynoe Formation|60685|3|Fully described|p4 Fig. 3, p1|Mesoproterozoic|Mesoproterozoic|Of the Bullita Group. Fine dolomitic sandstone; minor laminated mudstone and dolomitic siltstone. Conformable on Skull Creek Formation; unconformably below Weaner Sandstone. Max. Thickness: 243m. Geological Province: Victoria Basin.||||||
3225|Bynoe Formation|61573|5|Briefly described|p676, p678 Fig. 3|Mesoproterozoic|Mesoproterozoic|Of the Bullita Group. Purple-grey to red-brown siltstone, dolomitic sandstone. Overlain by Wondoan Hill Formation. Geological Province: Victoria Basin. See also p681 Tb. 1. ||||||
3225|Bynoe Formation|65342|6|Mentioned|p11 Fig.13. |||Victoria Basin.||Unit in Bullita Group.||Overlies Skull Creek Formation.||
3225|Bynoe Formation|67151|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Birindudu Basin.||Unit in Bullita Group.||Overlies Skull Creek Formation. Is unconformably overlain by Wondoan Hill Formation.|Siltstone, dolomitic siltstone and sandstone, dolostone.|
3225|Bynoe Formation|68733|5|Briefly described|p177 Fig.2, p182-183|Statherian||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).||Of the Bullita Group.||Unconformably overlain by the Weaner Sandstone.|Comprises dolomitic siltstone and sandstone.|05-DEC-17
3225|Bynoe Formation|69432|4|Described|p17:2, 10-12, 14|||Birrindudu Basin. Normally recessive. 243m thick. Deepens and thickens to the S.||Bullita Group.||Is overlain by Weaner Sandstone conformably or locally unconformably, and by Mount Gordon Sandstone unconformably.|Homogeneous fine dolomitic sandstone, sandstone, and massive micaceous siltstone. Local minor laminated dolomitic siltstone and mudstone near the top. Pink barite crystals occur on joint surfaces of fine sandstone.|12-JUL-16
3225|Bynoe Formation|69673|6|Mentioned|p48 fig 35|||||Bullita Group||Overlies Skull Creek Formation, unconformably overlain by Mount Gordon Sandstone, Weaner Sandstone||
3225|Bynoe Formation|70655|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Birindudu Basin.||Bullita Group.||Overlies Skull Creek Formation. Is unconformably overlain by Wondoan Hill Formation.|Siltstone, dolomitic siltstone and sandstone, dolostone.|
3225|Bynoe Formation|70850|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Bullita Group.||Conformably overlies Skull Creek Formation. Is overlain unconformably by Wondoan Hill Formation (Tijunna Group).|Dolomitic siltstone and sandstone, dolostone, minor chert.|
3225|Bynoe Formation|70855|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Bullita Group.||Overlies Skull Creek Formation. Is overlain by Weaner Sandstone, ?unconformably, and unconformably by Jasper Gorge Sandstone.|Dolomitic siltstone and sandstone, dolostone, minor chert.|
3225|Bynoe Formation|70968|5|Briefly described|p115, p120|||Birrindudu Basin.||Bullita Group.||Is overlain unconformably by Wondoan Hill and Stubb Formations (Tijunna Group), and Jasper Gorge Sandstone (Auvergne Group) locally.||
3225|Bynoe Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||sandstone, siltstone|
3225|Bynoe Formation|71302|5|Briefly described|p6,35||Paleoproterozoic|Of Birindudu Basin.||Unit of Bullita Group.||Overlain unconformably by Weaner Sandstone.||
3225|Bynoe Formation|72718|6|Mentioned|p7|||Birrindudu Basin.||Bullita Group||Underlain by Skull Creek Formation. Unconformably[?] overlain by Weaner Sandstone. Equivalent to Nero Siltstone.||
3256|Cabbage Gum Granite|22645|6|Mentioned|Table3 P213||Orosirian|Age of unit is 1848+/-7 Ma.||||||03-AUG-06
3256|Cabbage Gum Granite|23410|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Granite: biotite-bearing; seriate porphyritc to equigranular, medium to coarse grained and massive. Rapakivi texture. In drill core, foliated to sheared in part, locally gneissic. Minor metasediment xenoliths.||||||07-NOV-08
3256|Cabbage Gum Granite|23733|5|Briefly described|p7 Fig.1|Paleoproterozoic|Paleoproterozoic|Of the Tennant Creek Supersuite. Age: 1848 (Compton, 1995).||||||07-NOV-08
3256|Cabbage Gum Granite|23809|5|Briefly described|p27 Fig. 25|||Of the Tennant Creek Supersuite. Geological Province: Tennant Inlier.||||||06-AUG-08
3256|Cabbage Gum Granite|24172|3|Fully described|p39|Paleoproterozoic|Paleoproterozoic|Previously informally referred to as "Cabbage Gum granite complex" and "Cabbage Gum granite". Age: 1846+/-8Ma (Black, 1984) & 1848+/-7Ma (Compston, 1991). May, in part, be unconformably overlain by rocks of Hatches Creek Group and Helen Springs Volcanics.||||||07-NOV-08
3256|Cabbage Gum Granite|24197|5|Briefly described|p22|Paleoproterozoic|Paleoproterozoic|Of Tennant Creek Supersuite. Geological province: Tennant Creek Inlier.||||||07-FEB-11
3256|Cabbage Gum Granite|29135|4|Described|p40|||Informal use of name. -Pgc on Tennant Creek 1:250k sheet.||||||
3256|Cabbage Gum Granite|39571|4|Described|p125|||Isotopic data.||||||
3256|Cabbage Gum Granite|41465|5|Briefly described|p9|||||||||
3256|Cabbage Gum Granite|41961|6|Mentioned|Table 1 P39|||||||||
3256|Cabbage Gum Granite|41970|6|Mentioned|p332|||||||||
3256|Cabbage Gum Granite|42504|6|Mentioned|p59|||||||||
3256|Cabbage Gum Granite|42853|5|Briefly described|p593|||see also Fig.1 P592||||||
3256|Cabbage Gum Granite|42936|5|Briefly described|p546 Fig.1|||||||||
3256|Cabbage Gum Granite|43224|5|Briefly described|Map legend||Paleoproterozoic|||||||07-NOV-08
3256|Cabbage Gum Granite|43568|6|Mentioned|p506|||Age : 1846+/-8 Ma||||||03-AUG-06
3256|Cabbage Gum Granite|43850|4|Described|p263|||Known mainly from drill core.||||||03-AUG-06
3256|Cabbage Gum Granite|45167|5|Briefly described|p48|||||||||
3256|Cabbage Gum Granite|46842|6|Mentioned|p114|||||||||
3256|Cabbage Gum Granite|46964|6|Mentioned|p269|||||||||
3256|Cabbage Gum Granite|46992|6|Mentioned|p253|||||||||
3256|Cabbage Gum Granite|50588|5|Briefly described|p2.1|Paleoproterozoic|Paleoproterozoic|Of the Tennant Creek Supersuite. Geological Province: Tennant Creek/Davenport Province. Age: 1848 +/- 7Ma (SHRIMP).||||||14-APR-15
3256|Cabbage Gum Granite|60684|2|Defined|p53 Appendix, p20|Paleoproterozoic|Paleoproterozoic|Two-feldspar, biotite- to biotite-bearing granite - predominantly alkali feldspar (microcline and orthoclase), sodic plagioclase (oligoclase), strained quartz, reddish-brown biotite. Overlain by Hatches Creek group in Kelly Basin area. Age: 1848+/-7Ma.||||||07-NOV-08
3256|Cabbage Gum Granite|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Tennant Creek Supersuite. Biotite granite, seriate porphyritic to equigranular; rapakivi texture; minor metasediment xenoliths; foliated, sheared in part, and locally gneissic. In the Tennant Creek region.||||||07-NOV-08
3256|Cabbage Gum Granite|64559|6|Mentioned|p973|||Age: 1848+/-7Ma (U-Pb).||||||23-DEC-08
3256|Cabbage Gum Granite|65209|6|Mentioned|p35 Fig.1|Paleoproterozoic|Paleoproterozoic|||Tennant Creek Supersuite||||
3256|Cabbage Gum Granite|65222|5|Briefly described|p118-119, Tb 1, 109-111, p116 Tb 3,p125|Orosirian|Orosirian|Shown as intruding Warramunga Formation rocks in Fig 9 p125. Previous data: 1450+/- 36 Ma Rb-Sr; 1846+/- 8Ma U-Pb, 1630 Ma K/Ar. Poor exposure. Zircon sample locality from drillcore.|1848 +/- 7 Ma U/Pb SHRIMP.||||I-type granite.|24-JAN-22
3256|Cabbage Gum Granite|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Tennant Creek Supersuite.|||Biotite-bearing granite, seriate porphyritic to equigranular, rapakivi texture, minor metasediment xenoliths; foliated, sheared in part, and locally gneissic.|
3256|Cabbage Gum Granite|67323|5|Briefly described|Eastern Australia Time-Space Plot; p30|||Tennant Creek/Davenport area. Emplacement age; synchronous with minor deformation associated with the ~1850 Ma Tennant Event.|1848 +/- 7 Ma.||||Granite, granodiorite.|
3256|Cabbage Gum Granite|69187|5|Briefly described|p52, p53 Fig.2, p54 Fig.3|||Warramunga Province. Large intrusive complex||Tennant Creek Supersuite||intrudes Warramunga Formation||
3256|Cabbage Gum Granite|69424|5|Briefly described|p9:3, 6, 10-14, 17|Paleoproterozoic|Paleoproterozoic|Warramunga Province. Restricted compositional range on the boundary of the syeno-/monzogranite fields. No contacts exposed: relationships from drill-core only. Age given as 1847 +/- 8 Ma on p9:6.|1848 +/- 7 Ma (Compston, 1995).|Tennant Creek Supersuite.||Intrudes Junalki Formation.|Medium- to coarse-grained, seriate to porphyritic to equigranular granite; moderately to strongly foliated: local textural variation eg gneissic granite, augen gneiss.|12-JUL-16
3256|Cabbage Gum Granite|71592|5|Briefly described|Appendix A.|||Tennant Creek Region.|1848+/-7 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
3256|Cabbage Gum Granite|73124|6|Mentioned|p2 Fig.1|||||Tennant Creek Supersuite||||
3256|Cabbage Gum Granite|73125|5|Briefly described|p2|Palaeoproterozoic|Palaeoproterozoic|Warramunga Province.||Tennant Creek Supersuite.||||
3256|Cabbage Gum Granite|73460|6|Mentioned|p2|||Warramunga Province.||Tennant Creek Supersuite||||
3256|Cabbage Gum Granite|73590|6|Mentioned|p2|||||Tennant Creek Supersuite||||
3284|Cadna-owie Formation|730|6|Mentioned|p24, p25.|||Paralic.||||||11-NOV-14
3284|Cadna-owie Formation|12597|4|Described|p492 Tb.1, p499|Barremian|Early Cretaceous|Eromanga Basin. Up to 110m thick. Contains marine bivalves, gastropods, dinoflagellates and arenaceous foraminifera.|||Includes Mount Anna Sandstone, and Wyandra Sandstone, Members.|Conformably overlies Hooray Sandstone, Murta Member and Algebuckina Sandstone.|Siltstone and silty mudstone with interbeds of fine-grained labile sandstone and minor glauconite grading upwards to quartzose sandstone; overlain by Wyandra Sandstone Member (q.v.).|
3284|Cadna-owie Formation|13497|5|Briefly described|p50, p66-p67, p216|Early Cretaceous|Early Cretaceous|Eromanga Basin. See also p115, p115 fig 6.33, p138 fig 8.17, p141, p146, p149-p152, p154 .||||Overlies the Murta Formation. Overlain by the Bulldog Shale and Wallumbilla Formation.||
3284|Cadna-owie Formation|13516|5|Briefly described|p167 fig 10,  p169 fig 11, p171 fig 12|Early Cretaceous|Early Cretaceous|In Eromanga Basin.|||Includes Mount Anna Sandstone Member, Wyandra Sandstone Member|||
3284|Cadna-owie Formation|22839|6|Mentioned|P33|||||||||
3284|Cadna-owie Formation|22857|5|Briefly described|p296-7 Tb.22.1, p544 App.1 Tb.A1.12|Barremian|Valanginian|Known as the Gum Vale beds in Tibooburra area. Max. thickness: 130m. Geological Province: Eromanga Basin. See also p312-3 Fig. 22.6, p314.||||||
3284|Cadna-owie Formation|22865|4|Described|p314,Table22.1p296-7|Neocomian|Late Jurassic|||||||
3284|Cadna-owie Formation|22874|6|Mentioned|P18|||||||||
3284|Cadna-owie Formation|22883|5|Briefly described|P31, Fig2||Early Cretaceous|Overlying unit is Wallumbilla Formation, underlying unit is Murta Formation||||||
3284|Cadna-owie Formation|22912|5|Briefly described|33|||Geol. province: Eromanga Basin.||||||03-AUG-06
3284|Cadna-owie Formation|22922|6|Mentioned|33 fig 2|||||||||
3284|Cadna-owie Formation|23054|5|Briefly described|p21,23-4|Aptian|Aptian|||||||
3284|Cadna-owie Formation|23056|6|Mentioned|93 table 5|||Geol province Eromanga Basin||||||
3284|Cadna-owie Formation|23154|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Geological Province - Eromanga Basin.  Parent - Neales River Group.||||||
3284|Cadna-owie Formation|23155|4|Described|p30|Early Cretaceous|Early Cretaceous|Age Neocomian-Aptian. Formerly named as `Transition Beds' the new name Cadna-owie Formation was first used by Wopfner et al (1970).  On STRZELECKI the unit is underlain by Murta Formation (conformity).||||||
3284|Cadna-owie Formation|23282|6|Mentioned|p85 Fig 6.2|||of Eromanga Basin.||||||
3284|Cadna-owie Formation|23375|4|Described|Fig2 p264,265,267,269,271,277|Barremian|Valanginian|Geol. Prov:  Eromanga Basin.||||||03-AUG-06
3284|Cadna-owie Formation|23425|6|Mentioned|p391.|||Variation of Cadna-Owie Formation.||||||
3284|Cadna-owie Formation|23430|4|Described|p523 + p524 Table 14.7|||Eromanga Basin Province.||||||16-SEP-08
3284|Cadna-owie Formation|23818|4|Described|p141 Fig.65, p144 Fig.66, p156|Aptian|Aptian|Geological Province: Great Artesian Basin. Of the Neales River Group. Max. thickness: 250 ft. Overlying unit: Bulldog Shale.||||||
3284|Cadna-owie Formation|23830|5|Briefly described|Fig. 3a|Cretaceous|Cretaceous|Geological Province: Boorthanna Trough, eastern Arckaringa Basin.||||||
3284|Cadna-owie Formation|23849|5|Briefly described|p781|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||
3284|Cadna-owie Formation|23883|5|Briefly described|p129 Fig. 11.2|Cretaceous|Cretaceous|Geological Province: Great Australian Superbasin.||||||
3284|Cadna-owie Formation|23982|5|Briefly described|p2|Cretaceous|Jurassic|Geological Province: Great Artesian Basin. See also page 35 Fig.7.||||||
3284|Cadna-owie Formation|24067|5|Briefly described|p249 Fig.2|Mesozoic|Mesozoic|Geological Province: Officer Basin.||||||
3284|Cadna-owie Formation|24092|6|Mentioned|p5|||Geological Province: Great Artesian Basin.||||||
3284|Cadna-owie Formation|24112|5|Briefly described|p254 Fig.2|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin||||||
3284|Cadna-owie Formation|24175|3|Fully described|p19, p17 Fig. 3|Aptian|Neocomian|Thin transgressive sequence of sandstone, siltstone and shale.  Lies transitionally between Bulldog Shale above and Algebuckina Sandstone below.  Max. thickness: 50m.||||||
3284|Cadna-owie Formation|24210|5|Briefly described|p133 Fig. 2|Early Cretaceous|Early Cretaceous|Includes the Wyandra Sandstone Member.  Geological Province: Cooper Basin.||||||
3284|Cadna-owie Formation|24243|5|Briefly described|p3 Fig.2|Early Cretaceous|Early Cretaceous|Of Blythesdale Group.||||||
3284|Cadna-owie Formation|24321|5|Briefly described|Map legend|Barremian|Neocomian|Of theNeales River Group.||||||03-AUG-06
3284|Cadna-owie Formation|24372|6|Mentioned|p22|||Geological Province: Cooper Basin.||||||
3284|Cadna-owie Formation|24392|5|Briefly described|p139, p144 Appendix 1|Valanginian|Berriasian|Locally known as Parabarana Sandstone. See also page 140 Fig.1. Geological Province: Eromanga Basin.||||||
3284|Cadna-owie Formation|24482|5|Briefly described|p44|Cretaceous|Jurassic|Geological Province: Eromanga Basin.||||||
3284|Cadna-owie Formation|24507|6|Mentioned|p27|||Oil production has commenced from this unit. Geological Province: Cooper Basin.||||||
3284|Cadna-owie Formation|24510|6|Mentioned|p48|||Includes Livingston Tillite Member.||||||
3284|Cadna-owie Formation|29379|4|Described|p30|||Lithology. Early-Lower Cretaceous.||||||
3284|Cadna-owie Formation|29591|6|Mentioned|Fig.22|||||||||
3284|Cadna-owie Formation|29659|6|Mentioned|p8|||||||||
3284|Cadna-owie Formation|29660|6|Mentioned|p6|||||||||
3284|Cadna-owie Formation|29838|6|Mentioned|p4|||||||||
3284|Cadna-owie Formation|30024|6|Mentioned|p335|||See also Fig.3.||||||
3284|Cadna-owie Formation|30075|6|Mentioned|p9|||||||||
3284|Cadna-owie Formation|30512|6|Mentioned|p41|||||||||
3284|Cadna-owie Formation|30692|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
3284|Cadna-owie Formation|30804|6|Mentioned|p7|||See also P10 and Table 1.||||||
3284|Cadna-owie Formation|30807|6|Mentioned|p102|||Suggested map symbol||||||
3284|Cadna-owie Formation|30917|6|Mentioned|p42|||||||||
3284|Cadna-owie Formation|30919|6|Mentioned|Map legend|Neocomian|Neocomian|||||||
3284|Cadna-owie Formation|30920|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
3284|Cadna-owie Formation|30924|6|Mentioned|Map legend|Aptian|Aptian|||||||
3284|Cadna-owie Formation|31208|6|Mentioned|p46|||See also Fig. 7||||||
3284|Cadna-owie Formation|31244|6|Mentioned|p3|||Lower Cretaceous||||||
3284|Cadna-owie Formation|31249|6|Mentioned|p63|||||||||
3284|Cadna-owie Formation|31251|6|Mentioned|p74|||Microfloral assemblage in type section||||||
3284|Cadna-owie Formation|31697|6|Mentioned|p5|||L.Cretaceous||||||
3284|Cadna-owie Formation|31699|4|Described|p133|||L.Cretaceous||||||
3284|Cadna-owie Formation|32033|6|Mentioned|p2|||||||||
3284|Cadna-owie Formation|32204|4|Described|p8|||Details of Refraction and p8.  L.Cret.||||||03-AUG-06
3284|Cadna-owie Formation|32205|6|Mentioned|p13|||||||||
3284|Cadna-owie Formation|32275|6|Mentioned|p8|||Refers Wopfner Freytag & Heath (1970)||||||
3284|Cadna-owie Formation|32277|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
3284|Cadna-owie Formation|32314|6|Mentioned|Fig. 4|||||||||
3284|Cadna-owie Formation|33017|6|Mentioned|Table 1|||||||||
3284|Cadna-owie Formation|33075|6|Mentioned|Table 1|||Refers Wopfner et al. (1970)||||||
3284|Cadna-owie Formation|33086|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
3284|Cadna-owie Formation|33490|6|Mentioned|p30|||Correlation||||||
3284|Cadna-owie Formation|33491|4|Described|p56|||Mention Fig.2||||||
3284|Cadna-owie Formation|33521|6|Mentioned|p8|||||||||
3284|Cadna-owie Formation|33523|4|Described|p27|||||||||
3284|Cadna-owie Formation|33820|6|Mentioned|Map legend|Albian|Neocomian|Neocomian - Albian||||||
3284|Cadna-owie Formation|33821|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
3284|Cadna-owie Formation|33822|6|Mentioned|Map legend|Albian|Neocomian|Neocomian - Albian||||||
3284|Cadna-owie Formation|33823|6|Mentioned|Map legend|Cenomanian|Neocomian|Neocomian - Cenomanian||||||
3284|Cadna-owie Formation|33824|6|Mentioned|p12|||Table 2||||||
3284|Cadna-owie Formation|33825|6|Mentioned|p8|||Lithology||||||
3284|Cadna-owie Formation|33827|5|Briefly described|p13|||Table 2||||||
3284|Cadna-owie Formation|33828|6|Mentioned|p5|||Table 1||||||
3284|Cadna-owie Formation|33831|6|Mentioned|Map legend|Cenomanian|Neocomian|Neocomian - Cenomanian||||||
3284|Cadna-owie Formation|33832|6|Mentioned|p6|||Stratigraphy||||||
3284|Cadna-owie Formation|33844|6|Mentioned|p35|||Refers Wopfner (1969)||||||
3284|Cadna-owie Formation|33933|6|Mentioned|Fig.4|||||||||
3284|Cadna-owie Formation|33936|6|Mentioned|Fig.3a|||Cretaceous.||||||
3284|Cadna-owie Formation|33938|6|Mentioned|p46|||||||||
3284|Cadna-owie Formation|33939|2|Defined|p394|Early Cretaceous|Early Cretaceous|||||||
3284|Cadna-owie Formation|33964|4|Described|p6|||Cretaceous||||||
3284|Cadna-owie Formation|33971|6|Mentioned|p24|||See also P25 & Fig.15.||||||
3284|Cadna-owie Formation|33976|6|Mentioned|Fig.2|||||||||
3284|Cadna-owie Formation|34611|3|Fully described|p156|||Fig.65. Correlation chart. Cretaceous.||||||16-SEP-08
3284|Cadna-owie Formation|35149|5|Briefly described|Table 1|||See also mention on Fig.4.||||||
3284|Cadna-owie Formation|35239|6|Mentioned|Fig.4|||||||||
3284|Cadna-owie Formation|35548|6|Mentioned|p18|||||||||
3284|Cadna-owie Formation|35549|6|Mentioned|Fig.8|||Now called Marree Formation||||||
3284|Cadna-owie Formation|35560|6|Mentioned|p292|||||||||
3284|Cadna-owie Formation|35628|4|Described|Table 4|||||||||
3284|Cadna-owie Formation|35663|6|Mentioned|p124|||||||||
3284|Cadna-owie Formation|35793|6|Mentioned|Fig.3|||||||||
3284|Cadna-owie Formation|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
3284|Cadna-owie Formation|36214|5|Briefly described|p58|||||||||
3284|Cadna-owie Formation|36243|6|Mentioned|Table 6A|||||||||
3284|Cadna-owie Formation|36251|6|Mentioned|Fig.2|||||||||
3284|Cadna-owie Formation|36494|6|Mentioned|Fig.1|||||||||
3284|Cadna-owie Formation|36552|6|Mentioned|p59|||||||||
3284|Cadna-owie Formation|36571|6|Mentioned|Table 4|||||||||
3284|Cadna-owie Formation|36733|6|Mentioned|p14|||See also P53.||||||
3284|Cadna-owie Formation|36895|6|Mentioned|p9|||||||||
3284|Cadna-owie Formation|36912|6|Mentioned|p75|||||||||
3284|Cadna-owie Formation|36920|6|Mentioned|Table 1|||||||||
3284|Cadna-owie Formation|36922|6|Mentioned|Fig.3|||||||||
3284|Cadna-owie Formation|36966|6|Mentioned|p83|||||||||
3284|Cadna-owie Formation|37776|6|Mentioned|Fig.2|||||||||
3284|Cadna-owie Formation|37995|6|Mentioned|p66|||||||||
3284|Cadna-owie Formation|38022|6|Mentioned|Fig.4|||||||||
3284|Cadna-owie Formation|38068|4|Described|p72|||||||||
3284|Cadna-owie Formation|38199|6|Mentioned|p428|||||||||
3284|Cadna-owie Formation|38604|6|Mentioned|Map legend|Neocomian|Neocomian|||||||
3284|Cadna-owie Formation|38605|6|Mentioned|p20|||See also Table 4.||||||
3284|Cadna-owie Formation|38814|6|Mentioned|Table 1|||||||||
3284|Cadna-owie Formation|39070|4|Described|p364|||||||||
3284|Cadna-owie Formation|39211|5|Briefly described|p23|||See also Figs 4,7,8,10,13-15 etc. Correlation||||||
3284|Cadna-owie Formation|39352|6|Mentioned|Map legend|Albian|Aptian|Aptian to Albian||||||
3284|Cadna-owie Formation|39445|5|Briefly described|Table 10|||||||||
3284|Cadna-owie Formation|39630|6|Mentioned|Fig.3|||||||||
3284|Cadna-owie Formation|39846|6|Mentioned|p44|||||||||
3284|Cadna-owie Formation|39847|5|Briefly described|p37|||||||||
3284|Cadna-owie Formation|39914|6|Mentioned|p2|||||||||
3284|Cadna-owie Formation|39943|6|Mentioned|Table 8A|||||||||
3284|Cadna-owie Formation|39988|6|Mentioned|p291|||||||||
3284|Cadna-owie Formation|39989|4|Described|p423|||||||||
3284|Cadna-owie Formation|40003|6|Mentioned|p33|||See also Fig.8||||||
3284|Cadna-owie Formation|40030|6|Mentioned|p132|||||||||
3284|Cadna-owie Formation|40121|6|Mentioned|p446|||||||||
3284|Cadna-owie Formation|40199|4|Described|p25|||||||||
3284|Cadna-owie Formation|40220|6|Mentioned|p9|||||||||
3284|Cadna-owie Formation|40249|6|Mentioned|p41|||||||||
3284|Cadna-owie Formation|40544|6|Mentioned|p157|||||||||
3284|Cadna-owie Formation|40670|6|Mentioned|Fig.9|||||||||
3284|Cadna-owie Formation|40675|6|Mentioned|Table 8A|||||||||
3284|Cadna-owie Formation|40681|6|Mentioned|p9|||||||||
3284|Cadna-owie Formation|40687|3|Fully described|p417|||||||||
3284|Cadna-owie Formation|40832|3|Fully described|p456|||||||||
3284|Cadna-owie Formation|40833|6|Mentioned|p468|||||||||
3284|Cadna-owie Formation|40910|6|Mentioned|p16|||||||||
3284|Cadna-owie Formation|40911|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
3284|Cadna-owie Formation|40926|3|Fully described|p16|||||||||
3284|Cadna-owie Formation|40962|6|Mentioned|Table 1|||||||||
3284|Cadna-owie Formation|41060|6|Mentioned|p2|||||||||
3284|Cadna-owie Formation|41061|6|Mentioned|Fig.6|||Generalized stratigraphy||||||
3284|Cadna-owie Formation|41063|5|Briefly described|p40|||||||||
3284|Cadna-owie Formation|41064|6|Mentioned|p60|||||||||
3284|Cadna-owie Formation|41084|5|Briefly described|p81|||||||||
3284|Cadna-owie Formation|41085|3|Fully described|p87|||||||||
3284|Cadna-owie Formation|41086|3|Fully described|p104; Fig.3|||||||||
3284|Cadna-owie Formation|41088|6|Mentioned|p140|||||||||
3284|Cadna-owie Formation|41089|6|Mentioned|p156|||||||||
3284|Cadna-owie Formation|41097|6|Mentioned|p165|||||||||
3284|Cadna-owie Formation|41098|4|Described|p175|||||||||
3284|Cadna-owie Formation|41165|5|Briefly described|p360|||||||||
3284|Cadna-owie Formation|41175|6|Mentioned|Fig.1|||||||||
3284|Cadna-owie Formation|41176|6|Mentioned|Table 2|||||||||
3284|Cadna-owie Formation|41177|6|Mentioned|Fig.2|||||||||
3284|Cadna-owie Formation|41179|6|Mentioned|p262|||||||||
3284|Cadna-owie Formation|41182|6|Mentioned|p287|||||||||
3284|Cadna-owie Formation|41183|6|Mentioned|p310|||||||||
3284|Cadna-owie Formation|41184|6|Mentioned|p328|||||||||
3284|Cadna-owie Formation|41186|4|Described|p212|||||||||
3284|Cadna-owie Formation|41214|6|Mentioned|p257|||||||||
3284|Cadna-owie Formation|41216|6|Mentioned|p305|||||||||
3284|Cadna-owie Formation|41219|4|Described|p347|||Mention p351.||||||03-AUG-06
3284|Cadna-owie Formation|41247|6|Mentioned|p126|||||||||
3284|Cadna-owie Formation|41266|6|Mentioned|Fig.3|||||||||
3284|Cadna-owie Formation|41361|6|Mentioned|p4|||||||||
3284|Cadna-owie Formation|41523|5|Briefly described|p271,p275|||||||||
3284|Cadna-owie Formation|41535|6|Mentioned|p368|||||||||
3284|Cadna-owie Formation|41681|6|Mentioned|p22,p3|||||||||
3284|Cadna-owie Formation|41705|6|Mentioned|p116|||||||||
3284|Cadna-owie Formation|41707|5|Briefly described|p163|||||||||
3284|Cadna-owie Formation|41712|6|Mentioned|p282|||||||||
3284|Cadna-owie Formation|41724|5|Briefly described|p382|||||||||
3284|Cadna-owie Formation|41950|5|Briefly described|Fig.2 P3|||||||||
3284|Cadna-owie Formation|42061|4|Described|Fig,11 P159|||||||||
3284|Cadna-owie Formation|42064|6|Mentioned|Fig.4 P.170|||||||||
3284|Cadna-owie Formation|42067|4|Described|Appendix 2|||||||||
3284|Cadna-owie Formation|42090|6|Mentioned|p28|||||||||
3284|Cadna-owie Formation|42283|6|Mentioned|p89|||||||||
3284|Cadna-owie Formation|42293|5|Briefly described|Fig.3 P.19|||||||||
3284|Cadna-owie Formation|42341|6|Mentioned|Fig.7 P57|||||||||
3284|Cadna-owie Formation|42346|5|Briefly described|Fig.3 P80|Jurassic||||||||
3284|Cadna-owie Formation|42375|6|Mentioned|Fig. 28 P125, Table1|Late Cretaceous|Jurassic|Eromanga Basin||||||
3284|Cadna-owie Formation|42395|5|Briefly described|Fig.13 P83|||||||||
3284|Cadna-owie Formation|42397|6|Mentioned|Fig.2 P3|||||||||
3284|Cadna-owie Formation|42429|5|Briefly described|Fig.3 P155|||||||||
3284|Cadna-owie Formation|42446|6|Mentioned|p13|||||||||
3284|Cadna-owie Formation|42447|6|Mentioned|Fig.1|||||||||
3284|Cadna-owie Formation|42465|5|Briefly described|Map Legend|||||||||
3284|Cadna-owie Formation|42469|4|Described|p31|||||||||
3284|Cadna-owie Formation|42474|6|Mentioned|p25|||||||||
3284|Cadna-owie Formation|42520|5|Briefly described|p6|||||||||
3284|Cadna-owie Formation|42602|6|Mentioned|Fig.2 p20|||||||||
3284|Cadna-owie Formation|42746|4|Described|p10|||See also Fig.6, Fig.2||||||
3284|Cadna-owie Formation|42749|5|Briefly described|p31, Fig.9 p31|||see also Fig.2 p27||||||03-AUG-06
3284|Cadna-owie Formation|42816|6|Mentioned|p18|||||||||
3284|Cadna-owie Formation|42905|5|Briefly described|p19|||see also Fig 5.3||||||
3284|Cadna-owie Formation|42999|5|Briefly described|Table 2,p90||Early Cretaceous|||||||
3284|Cadna-owie Formation|43002|5|Briefly described|Fig.2,p135|||||||||
3284|Cadna-owie Formation|43004|5|Briefly described|Table 1,p179|||||||||
3284|Cadna-owie Formation|43053|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Transitional, non-marine to marine sandstone and siltstone.||||||25-MAY-05
3284|Cadna-owie Formation|43071|6|Mentioned|p20|||||||||
3284|Cadna-owie Formation|43085|5|Briefly described|Fig.6|||||||||
3284|Cadna-owie Formation|43094|5|Briefly described|p36|||||||||
3284|Cadna-owie Formation|43105|5|Briefly described|Fig.9,p15.|||||||||
3284|Cadna-owie Formation|43114|6|Mentioned|Table 2|||||||||
3284|Cadna-owie Formation|43122|5|Briefly described|p23|||see also Fig. 2.||||||
3284|Cadna-owie Formation|43258|5|Briefly described|Map Legend||Cretaceous|||||||
3284|Cadna-owie Formation|43298|5|Briefly described|Map Legend||Cretaceous|||||||
3284|Cadna-owie Formation|43591|6|Mentioned|p40|||||||||
3284|Cadna-owie Formation|43602|4|Described|191|||Geological Province: Eromanga Basin.||||||16-SEP-08
3284|Cadna-owie Formation|43743|6|Mentioned|Fig.2,p33||Early Cretaceous|||||||
3284|Cadna-owie Formation|43840|5|Briefly described|Fig3 p12|||Cretaceous-Jurassic age||||||12-JUL-16
3284|Cadna-owie Formation|44133|4|Described|p112, 104 Fig. 9.11|Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin. Previously named 'Transition beds'. Thickness: up to 100m.  Overlies: Murta Formation. Onlaps Algebuckina Sandstone.||||||11-NOV-13
3284|Cadna-owie Formation|44289|5|Briefly described|Map Legend||Aptian|||||||
3284|Cadna-owie Formation|44658|14|Not recorded|map legend|||Neoc.-Albian (G53-15).||||||
3284|Cadna-owie Formation|45110|6|Mentioned|p107|||||||||
3284|Cadna-owie Formation|45149|6|Mentioned|Table 1|||Page 15.||||||
3284|Cadna-owie Formation|45168|6|Mentioned|p9|||||||||
3284|Cadna-owie Formation|46791|6|Mentioned|Fig.11|||||||||
3284|Cadna-owie Formation|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
3284|Cadna-owie Formation|46939|6|Mentioned|Fig.2|||||||||
3284|Cadna-owie Formation|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
3284|Cadna-owie Formation|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
3284|Cadna-owie Formation|60717|5|Briefly described|p40 Fig. 2|Early Cretaceous|Early Cretaceous|Contains Wyandra Sandstone Member. Overlies Murta Formation and part of Algebuckina Sandstone; overlain by Wallumbilla Formation and Bulldog Shale. Geological Province: Eromanga Basin.||||||31-JAN-08
3284|Cadna-owie Formation|60953|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||||||
3284|Cadna-owie Formation|60955|5|Briefly described|Map Legend|Cretaceous|Jurassic|Coarse sands and grits, ferruginous sandstones.||||||
3284|Cadna-owie Formation|61014|5|Briefly described|pp532-533, p545, p550.|Lower Cretaceous|Lower Cretaceous|Eromanga Basin. Fluvio-lacustrine conditions characterised by internal drainage and infill of large interior cratonic lakes.|||Includes Wyandra Sandstone Member.|Overlies Hooray Sandstone. Is overlain by Bulldog Shale.||
3284|Cadna-owie Formation|61108|5|Briefly described|map legend|Cretaceous|Cretaceous|Transitional, non-marine to marine sandstone, siltstone, calcareous sandstone and pebbly sandstone.||||||
3284|Cadna-owie Formation|61312|4|Described|p73, p64, p67 Fig.E5|Early Cretaceous|Early Cretaceous|Includes the Wyandra Sandstone and Warratta Sandstone Members. The top of the unit has been called "Main Datum". Shale, minor sandstone. Overlain by Wallumbilla Fm. Geol. Prov: Eromanga Basin. Equivalent in the Surat Basin is Bungil Fm.||||||
3284|Cadna-owie Formation|61560|6|Mentioned|p492||Cretaceous|During its deposition this unit was impacted by the Tookoonooka meterorite fragment(s) a large circular structure in the Mesozoic strata of the Eromanga Basin. ||||||
3284|Cadna-owie Formation|61613|6|Mentioned|p282 Fig. 2|Early Cretaceous|Early Cretaceous|Includes Wyrandra Sandstone Member. Geological Province: Eromanga Basin.||||||07-FEB-11
3284|Cadna-owie Formation|61614|6|Mentioned|p290 Fig. 2|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||17-MAR-09
3284|Cadna-owie Formation|61615|6|Mentioned|p302 Fig. 2|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||07-FEB-11
3284|Cadna-owie Formation|62029|5|Briefly described|p15 Fig. 4|Cretaceous|Cretaceous|Misspelling of Cadna-Owie Formation.||||||14-APR-08
3284|Cadna-owie Formation|62537|6|Mentioned|p191 Fig.2. |Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Murta Formation and Namur Sandstone. Is overlain by Wallumbilla Formation and Bulldog Shale.||
3284|Cadna-owie Formation|62730|5|Briefly described|p352 Fig. 1|Early Cretaceous|Early Cretaceous|Includes the Wyandra Sandstone Member. Geological Province: Eromanga Basin.||||||21-APR-08
3284|Cadna-owie Formation|63450|5|Briefly described|p83|Cretaceous|Jurassic |May be equivalent to the upper part of Longsight Sandstone, which was renamed Cadna-owie Formation by Mond and Harrison (1978). Overlain by Rolling Downs Group. Geological province: Georgina Basin.||||||07-FEB-11
3284|Cadna-owie Formation|63894|5|Briefly described|p169|Early Cretaceous|Jurassic|Aquifer. Overlies Algebuckina Sandstone. Underlies Bulldog Shale.||||||
3284|Cadna-owie Formation|63979|2|Defined|p46, Fig. 44|Barremian|Valanginian|Contains Mount Anna Sandstone Mbr at top (SA), Wyandra Sandstone Mbr (Qld). Informally subdivided into upper + lower Cadna-owie Fm. Overlies Algebuckina Sst.Thick: 90m.Geol.p: Eromanga Basin. Interbedded sandstone, siltstone, silty mudstone + mudstone.||||||07-FEB-11
3284|Cadna-owie Formation|64048|6|Mentioned|p64 Tb. 2|||Geological Province: Eromanga Basin.||||||07-FEB-11
3284|Cadna-owie Formation|64197|6|Mentioned|p625 Fig.1c, p630 Figs.6,7|Early Cretaceous|Early Cretaceous|Eromanga Basin.|||Includes the Wyandra Sandstone Member.|Overlain by Bulldog Shale and Wallumbilla Formation; overlies Hooray and Algebuckina Sandstones.||10-DEC-15
3284|Cadna-owie Formation|64665|5|Briefly described|p53 Fig.2, p62.|Early Cretaceous|Early Cretaceous|Eromanga Basin. Marks the transition from fluvio-lacustrine and deltaic, to paralic and marine, environments.||||Overlies Algebuckina Sandstone, Murta Formation and Hooray Sandstone.||
3284|Cadna-owie Formation|64696|5|Briefly described|p133 Fig.14|Cretaceous|Cretaceous|||||||
3284|Cadna-owie Formation|64778|6|Mentioned|p13|Jurassic|Jurassic|Pedirka and Simpson Desert Basins.||||||
3284|Cadna-owie Formation|64783|6|Mentioned|p85 Figs.3 and 4|||||||||15-NOV-17
3284|Cadna-owie Formation|64856|5|Briefly described|p98|||Eromanga Basin unit, laterally equivalent to the Bungil Formation.| | ||||31-JAN-13
3284|Cadna-owie Formation|65194|6|Mentioned|p46, p48|||Main aquifer in the Great Artesian Basin. Separated from Eyre Formation by clay-rich rocks of the Marree Subgroup.||||||
3284|Cadna-owie Formation|65238|5|Briefly described|p10|Early Cretaceous|Late Jurassic|See also variations on this name: Cadna Owie Formation and Cadnaowie Formation in the figures. Eromanga basin. Fine grained sandstone, siltstone and claystone with minor limestone||||||
3284|Cadna-owie Formation|65309|6|Mentioned|pp14-15. |||||||Is overlain by Algebuckina Sandstone in much of the Eromanga Basin.||
3284|Cadna-owie Formation|65342|5|Briefly described|pp9-10.|||Eromanga Basin. Max. thickness at least 59 m.||||Overlies Algebuckina Sandstone. Is overlain by Bulldog Shale.|Sandstone, siltstone.|
3284|Cadna-owie Formation|65374|5|Briefly described|p30||Cretaceous|||||||
3284|Cadna-owie Formation|65376|5|Briefly described|p9 Fig.1.2. |Cretaceous|Jurassic||||||Fluvial to marginal marine sandstone.|
3284|Cadna-owie Formation|65385|5|Briefly described|pS133, pS134 Fig.7|Early Cretaceous|Early Cretaceous|Of Eromanga Basin. Includes Trinity Well Sandstone Member and Wyandra Sandstone Member. Overlies Algebuckina Sandstone, Murta Formation and Hooray Sandstone. Overlain by Bulldog Shale and Wallumbilla Formation.||||||08-MAR-12
3284|Cadna-owie Formation|65489|5|Briefly described|p49, p55-58, p61, p96, p155-156, p160|Early Cretaceous|Early Cretaceous|Eromanga Basin. 80m thick. Oil and gas shows. Regional sand sheet with good to excellent reservoir quality. Intraformational siltstone  seal.||||Overlies Murta Formation. Is overlain by Bulldog Shale or Wallumbilla Formation.||
3284|Cadna-owie Formation|65925|5|Briefly described|p20, p57, Appendix 2.|Cretaceous|Cretaceous|Frome Embayment, Eromanga Basin. Equivalent to Mount Anna Sandstone and Parabarana Sandstone. Discharge area for GAB aquifer via diffuse upwards leakage and mound springs.||||Is overlain by Bulldog Shale.|Sandstone, siltstone and carbonaceous claystone; minor conglomerate.|
3284|Cadna-owie Formation|66303|5|Briefly described|pp27-28.|Early Cretaceous|Early Cretaceous|Stratigraphically equivalent to Parabarana Sandstone. A thin, fine-grained unit widely recognised in Eromanga Basin. Correlated with Foraminisporis wonthaggiensis spore-pollen zone.|||Includes Livingston Tillite Member.|Is overlain by Bulldog Shale.|Pale grey siltstone and fine-grained sandstone, with minor carbonaceous claystone intervals; local diamictites, pebbles and coarse breccia layers.|
3284|Cadna-owie Formation|66518|5|Briefly described|p19.|Cretaceous|Cretaceous|Eromanga Basin.||||Is overlain by Bulldog Shale. Age-equivalent to Parabarana Sandstone in the northern Eromanga Basin.|Sands and silts.|06-FEB-14
3284|Cadna-owie Formation|66520|5|Briefly described|p11-12. |Cretaceous|Cretaceous|Gawler Craton. 18 m thick.|||||Feldspathic sandstone.|
3284|Cadna-owie Formation|66529|5|Briefly described|p10, p12 Fig.5, p16 |||Eromanga Basin. Appears on p16 as (Cadna-owie and Hooray Sandstones).|||Includes Wyandra Sandstone Member.|Overlies Hooray, Algebuckina and Murta Sandstones. Is overlain by Neales River and Rolling Downs Groups.|Marine sandstone.|
3284|Cadna-owie Formation|66623|3|Fully described|p102, pp238-245, pp250-255. |Early Cretaceous|Early Cretaceous|Preferential weathering of the dominant calcareous and fine-grained lithologies results in largely sandstone outcrops. Thickness varies to 260 m but this may include Murta Formation. Contains a wide range of fossils. Deposited in a variety of environments. Hosts glacial dropstones. Equivalent to top of Gum Vale Beds and lower Wittabrenna Beds, and to Pelican Well and Bungil Formations.||In SA, unit in Neales River Group.|Includes Wyandra Sandstone Member.|Overlies Namur Sandstone and Murta Formation; locally incised into Algebuckina Sandstone. Is disconformably overlain by Doncaster Membr (Wallumbilla Formation). Is overlain by Marree Formation in SA.|Erosion-resistant calcareous sandstone and siltstone; subordinate weathered grey shale and siltstone; minor pebbly sandstone and conglomerate.|11-NOV-13
3284|Cadna-owie Formation|66915|5|Briefly described|p4-6, p9, p11 Fig.7|Cretaceous|Cretaceous|Eromanga Basin. The "C-Horizon" is often referred to as "top Cadna-owie Formation". A readjustment of terminology is required, therefore it is better to understand the "C-Horizon" to represent "Base Wallumbilla" rather than "top Cadna-owie", or "top Bungil" or "top Gilbert River" or top whatever other unit underlies the Wallumbilla Formation in that area. See also Wallumbilla Formation.|||Wyandra Sandstone Member at top|Is overlain by Wallumbilla Formation.||12-JAN-17
3284|Cadna-owie Formation|66920|5|Briefly described|Map legend|Cretaceous|Cretaceous|The ferruginous rocks are mapped separately.|||Includes Wyandra Sandstone.||Marine, calcareous sub-labile to quartzose sandstone and siltstone interbedded with grey shales and siltstones; ferruginous calcareous sandstone and mudstone.|
3284|Cadna-owie Formation|66921|5|Briefly described|Map legend|Cretaceous|Cretaceous|||Unit in Rolling Downs Group.|Includes Wyandra Sandstone Member.||Marine calcareous, sub-labile to quartzose sandstone and siltstone interbedded with grey shales and siltstones.|
3284|Cadna-owie Formation|66922|5|Briefly described|Map legend|Cretaceous|Cretaceous|Includes three un-named but separately mapped sub-units.|||Includes Wyandra Sandstone.||Marine, calcareous, sub-labile to quartzose sandstone and siltstone interbedded with grey shales and siltstones.|
3284|Cadna-owie Formation|67120|5|Briefly described|Map legend|Cretaceous|Cretaceous||||||Sandstone, fine-grained, with coarse-grained sandstone beds, and pale grey siltstone, minor conglomerate.|18-NOV-14
3284|Cadna-owie Formation|67207|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||Includes Wyandra Sandstone Member.||Marine calcareous, sub-labile to quartzose sandstone and siltstone interbedded with grey shales and siltstones; local pebbly sandstone and conglomerate interbeds and ferruginous, calcareous sandstone and mudstone.|
3284|Cadna-owie Formation|67209|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||Includes Wyandra Sandstone Member.|Overlies Namur Sandstone. Is overlain by Doncaster Member of Rolling Downs Group.|Marine calcareous, sub-labile to quartzose sandstone and siltstone interbedded with grey shales and siltstones.|
3284|Cadna-owie Formation|67211|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||Includes Wyandra Sandstone Member.||Marine calcareous, sub-labile to quartzose sandstone and siltstone interbedded with grey shales and siltstones.|
3284|Cadna-owie Formation|67323|5|Briefly described|p87, p93 Fig.12.3, p95|Early Cretaceous|Early Cretaceous|Eromanga Basin.|||Wyandra Sandstone Member.|Overlies Hooray Sandstone. Is overlain by Wallumbilla Formation.||
3284|Cadna-owie Formation|67402|4|Described|p26 tbl RRM4, p43 tbl HPB1, p106|Aptian|Valanginian|Eromanga Basin. Deposited in a paralic or shallow marine environment. Maximum thickness of 10m. See also  p108 fig ERO4, p108-p110, p111 fig ERO8, p113 fig ERO12, p114 fig ERO13, p115.|||Includes the Wyandra Sandstone Member.|Overlies the Lower Cadna-owie Formation and the Hooray Sandstone. Overlain by the Wallumbilla Formation.|Upwards coarsening sequence of interbedded sandstone, siltstone and mudstone.|
3284|Cadna-owie Formation|67462|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Algebuckina Sandstone. Is overlain by Bulldog Shale.||
3284|Cadna-owie Formation|67784|5|Briefly described|p25-26|Aptian|Neocomian|Northern Eromanga Basin.||||Is overlain by Doncaster Member (Wallumbilla Formation).|Sandstone|08-FEB-18
3284|Cadna-owie Formation|68068|6|Mentioned|Map legend|||Time equivalent to the Parabarana Sandstone to the south.||||||18-NOV-14
3284|Cadna-owie Formation|68131|5|Briefly described|p2 Fig.1|Cretaceous|Jurassic|Fluvial to marginal marine deposits. Mapped with Algebuckina Sandstone as one unit.|||||Sandstone.|
3284|Cadna-owie Formation|68713|5|Briefly described|p22|Cretaceous|Cretaceous|||Of the Neales River Group.|Includes the Trinity Well Sandstone Member.|||
3284|Cadna-owie Formation|68715|6|Mentioned|p30 Fig.5|Barremian|Valanginian|Eromanga Basin.||||||
3284|Cadna-owie Formation|68734|6|Mentioned|p218 Fig.2|||Eromanga Basin (SW and NE). Fluvial to shallow marine. Pre-Barremian age.||||||16-JAN-17
3284|Cadna-owie Formation|68821|5|Briefly described|p292 Fig.1, p295, p297 Fig.3|Cretaceous|Cretaceous|Eromanga Basin. Lower Cretaceous age. Fluvial-paralic. Equivalent to the Bungil Formation. Contains diamictite deposits at its base.|||||Comprises quartz rich sandstones and conglomerates.|
3284|Cadna-owie Formation|69001|5|Briefly described|p2 Fig.1B, p11, pp16-18, pp35-37, p63|Early Cretaceous|Early Cretaceous|Terrestrial to marine transition sediments. Of the Eromanga Basin. Calcite induration is common (but not diagnostic) in parts of weathered Cadna-owie Formation. Includes locally defined units by McMinn (1981b) and/or Morton (1982) such as the Gum Vale Beds or Gum Vale Formation.||||Equivalent to the Algebuckina Sandstone and the Gum Vale Beds.|Comprises sandstones, siltstones, and some conglomerate.|
3284|Cadna-owie Formation|69019|3|Fully described|p56-57 Pl.9, p85, p87-91, p168.|Aptian|Valanginian|Eromanga Basin. Of Freytag et al. (1967) and Wopfner et al. (1970); formerly 'Transition Beds' of Whitehouse (1955). Type section in ~3 km WSW of Algebuckina Hill. Often associated with ferricrete capping. A significant regional aquifer.||Unit in Neales River Group.|Includes Mount Anna Sandstone Member, Livingston Tillite Member and Trinity Well Sandstone Member.|Overlies Murta Formation and Algebuckina Sandstone; Bunyeroo Formation unconformably. Is equivalent to Parabarana Sandstone. Is overlain by Bulldog Shale gradationally and by Wallumbilla Formation.|Grey siltstone coarsening upwards into fine- to medium-grained sandstone; sandstone interbeds commonly calcitic; near basal siltstone commonly carbonaceous; locally a basal pebbly interval; contains exotic lonestones to 1 m.|
3284|Cadna-owie Formation|69023|5|Briefly described|p79, p86-87, p89 Fig.20, p90, p92-95|Aptian|Valanginian|See also p99, p101, p191-192. Freytag et al. (1967) and Wopfner et al. (1970); previously the Transition Beds of Whitehouse (1955). Contrasts with Parabarana Sandstone are discussed. Thickness to c.69m. Stratigraphic wells intersection data.||||Overlies Murta Formation. Is overlain conformably by Bulldog Shale (Marree Subgroup).|Contains fossil ice-wedges.|
3284|Cadna-owie Formation|69203|6|Mentioned|p12|Cretaceous|Cretaceous|||||||
3284|Cadna-owie Formation|69454|5|Briefly described|p38:3, 13, 14 Fig.38.9|Cretaceous|Cretaceous|Eromanga Basin. Potential hydrocarbon trap, either by sealing Algebuckina Sandstone reservoirs or by having its own sandstone reservoirs sealed by the Wallumbilla Formation shales.||||||12-JUL-16
3284|Cadna-owie Formation|69457|3|Fully described|p41:2-3, 5-9, 16|Early Cretaceous|Early Cretaceous|Wopfner et al. (1970). Equivalent to the Transition beds of Whitehouse (1955). Eromanga Basin. Lacustrine to restricted/marginal marine, minor fluviatile and subtidal shallow marine deposits. 81m thick (>100m in Cooper Basin). Possibly equivalent to the upper part of De Souza Sandstone. Late Valanginian to early Aptian age from dinocysts and acritarchs. Hydrocarbon source potential is briefly discussed. May form a seal for underlying Algebuckina Sandstone reservoirs, and its own shoreline sandstone reservoirs in the NT may be sealed by the Wallumbilla Formation.|||Includes Mount Anna, Trinity Well, Wyandra, Sandstone Members.|Conformably overlies Algebuckina and Hooray Sandstones and Murta Formation. Is overlain conformably by Bulldog Shale and Wallumbilla Formation. Lateral equivalent of Wallumbilla Formation.|Thinly to thickly interbedded sandstone, siltstone, silty mudstone and mudstone; minor claystone. Parallel bedding and coarsening-upwards intervals typical. Local pebble layers, diamictites and coarse breccia layers.|23-JAN-19
3284|Cadna-owie Formation|69554|6|Mentioned|p131|Cretaceous|Cretaceous|Northern Gawler Craton.||||||
3284|Cadna-owie Formation|69562|6|Mentioned|p666 Fig.3, p667 Fig.4, p668|Cretaceous|Cretaceous|||||||
3284|Cadna-owie Formation|69568|6|Mentioned|p443|Cretaceous|Cretaceous|Lake Frome region, Eromanga Basin. A transitional depositional environment from terrestrial to marine.|||||Fine-grained, pale grey siltstone and sandstone with minor carbonaceous claystone intervals.|
3284|Cadna-owie Formation|69582|6|Mentioned|p65|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies the Hooray Sandstone. Overlain by the Wallumbilla Formation.||
3284|Cadna-owie Formation|69594|4|Described|p519, p526-528, p532-533, p538, p573|Barremian|Valanginian|Wopfner et al. (1970). Eromanga Basin. Subsurface. 60-90m thick. Paralic to shallow-marine deposits. Is a minor hydrocarbon reservoir. An important, shallow aquifer.|||Wyandra Sandstone Member.|Overlies Murta Formation and Hooray Sandstone transitionally. Is overlain by Doncaster Member (Wallumbilla Formation). Lateral equivalent to Bungil Formation.|Lower part consists of silty mudstone, siltstone and lithic to quartzose and sublabile sandstone with the proportion of sandstone increasing upwards; the upper part is mainly sublabile to lithic sandstone with minor siltstone near the top.|
3284|Cadna-owie Formation|69654|6|Mentioned|p4|||Curnamona Province.||||||
3284|Cadna-owie Formation|69673|5|Briefly described|p154, p155 fig 127, p159, p161 fig 131|Cretaceous|Cretaceous|Age derived from Palynoflora. Some source potential for oil and gas.|||Includes Mount Anna Sandstone Member, Wyandra Sandstone Member, Murta Member|Overlies Murta Formation, Algebuckina Sandstone, overlain by Wallumbilla Formation|Thinly to thickly interbedded sandstone, siltstone, silty mudstone and mudstone, minor claystone typically with parallel bedding and upwards coarsening intervals.|
3284|Cadna-owie Formation|69790|6|Mentioned|p1063 Fig.2|Cretaceous|Cretaceous|Eromanga Basin.||||||
3284|Cadna-owie Formation|69797|5|Briefly described|p17 Fig.2|Early Cretaceous|Early Cretaceous|Geol. Prov: Eromanga Basin.|||Includes Wyandra Sandstone Member.|||23-JAN-19
3284|Cadna-owie Formation|69946|2|Defined|p17, p19-20, p44, p56-58, p94, p96-98|Early Cretaceous|Early Cretaceous|Wopfner et al. (1970), for the mappable interval between Algebuckina Sandstone and Bulldog Shale. Previously the Transition beds of Whitehouse (1955), for a unit that records the transition from terrestrial to marine conditions. Eromanga Basin. Type section is Big Cadna-owie Spring, 5.5km SSW of Mount Dutton. Upper boundary is strongly diachronous, younging towards the Basin margin. Typically 10-20m thick, to a maximum of >115m. Includes marine and non-marine fossils. Wireline log correlations. Lateral equivalent of Village Well and Pelican Well Formations and Parabarana Sandstone.|||Includes Wyandra, Mount Anna and Trinity Well, Sandstone Members.|Overlies Murta Formation gradationally and Algebuckina Sandstone. Is overlain conformably by Bulldog Shale or Wallumbilla Formation. See Comments.|Subsurface: pale grey siltstone with very fine- to fine-grained sandstone interbeds and minor carbonaceous claystone; pebbly layers, diamictites and coarse breccia layers around the Basin margin. Outcrop: minor calcareous sandstone beds with ooids.|
3284|Cadna-owie Formation|69947|5|Briefly described|p8-9, p13 Fig.7.2, p29 Fig.7.18|Early Cretaceous|Early Cretaceous|See also p31 Fig.7.20. Eromanga Basin. Marks transition from terrestrial to marine deposition.|||Wyandra Sandstone Member.|Conformably overlies Murta Formation. Is overlain by Bulldog Shale and Wallumbilla Formation.|Mudstone, siltstone, sandstone.|
3284|Cadna-owie Formation|69948|6|Mentioned|p4; Figs.4.1-2, 13-20|||Eromanga Basin (an intracratonic basin). Sediment thickness, sonic log, gamma ray log all shown in contrast with Otway Basin (a rift basin). Seismic sections across the Gidgealpa, Dullingari, Poolowanna and Big Lake Fields, and other structures.||||Overlies Murta Formation or Algebuckina Sandstone. Is overlain by Bulldog Shale or Wallumbilla Formation.||
3284|Cadna-owie Formation|70336|5|Briefly described|Map legend|Cretaceous|Cretaceous||||||Fine-grained sandstone with coarse-grained sandstone beds and pale grey siltstone; minor conglomerate.|
3284|Cadna-owie Formation|70383|5|Briefly described|p45, p52|Early Cretaceous|Berriasian|Transgressive, marginal marine deposits. Maximum age from age of Sprigg Diamictite Member.|||Includes Sprigg Diamictite Member, Livingston Tillite Member.|Overlies Algebuckina Sandstone. Equivalent to Parabarana Sandstone.||15-JAN-19
3284|Cadna-owie Formation|70384|5|Briefly described|Map legend.|Cretaceous|Cretaceous|Eromanga Basin. This unit is the distal Basin-wide equivalent to the rangelands-proximal Parabarana Sandstone. Age shown more specifically as Neocomian to Aptian.||Of Neales River Group.|Includes Livingston Tillite, Sprigg Diamictite, Trinity Well Sandstone, Members.|Equivalent to Parabarana Sandstone.|Mostly subsurface: yellow-brown, fine-grained, calcitic quartz sandstone; coarse-grained buff-yellow gritstone lenses; lower zone more silty, grey, carbonaceous. Sandy beds usually ferruginous, locally gravelly or bouldery.|23-JAN-19
3284|Cadna-owie Formation|70649|5|Briefly described|Map Legend|Cretaceous|Cretaceous||||Includes un-named unit, Wyandra Sandstone Member.||Marine calcareous, sub-labile to quartzose sandstone and siltstone interbedded with grey shale and siltstone. Un-named unit is ferruginous, calcareous sandstone and mudstone.|
3284|Cadna-owie Formation|70652|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Unconsolidated sediments also described.|||Includes Wyandra Sandstone Member.||Marine calcareous, sub-labile to quartzose sandstone and siltstone interbedded with grey shale and siltstone.|
3284|Cadna-owie Formation|70789|5|Briefly described|p318, p320 Fig.4, p328|Early Cretaceous|Early Cretaceous|Eromanga Basin. Transgressive, fluvial to marginal marine deposits. Consistent thickness of 50-80m. A major aquifer in the Basin.||||Is overlain by Bulldog Shale.|Sandstones and siltstones.|
3284|Cadna-owie Formation|70821|4|Described|p21-22, p32-33, p72, p80, p82, p86|Early Cretaceous|Early Cretaceous|Eromanga Basin. Poorly expressed or unrecognised in the southern Thomson region. Late Valanginian-Early Aptian acritarchs and dinoflagellates indicate fresh to brackish water, lacustrine to restricted, marginal marine environments. Borehole wireline electrical and natural gamma logging and AEM inversion soundings. Hydrostratigraphic properties.|||Includes Wyandra Sandstone Member.|Overlies Algebuckina, Namur, Hooray (unconformably), Mooga Sandstones and Crowl Creek Formation. Is overlain by Bulldog Shale and Wallumbilla Formation.|Fairly well-bedded siltstone, fine to medium lithic sandstone and intraformational conglomerate; thin coaly layers, dark mudstone and layers of kaolin-like material, possibly altered tuff are also present. Volcanogenic components increase up-section.|23-JAN-19
3284|Cadna-owie Formation|70823|5|Briefly described|p41, p43-p44, p78|Early Cretaceous|Early Cretaceous|Eromanga Basin. See also Cadnowie Formation [which is a mis-spelling of this formation]. Age is a minimum depositional age.|c. 126 Ma|||Overlies the Murta Formation. Overlain by the Wallumbilla Formation and the Bulldog Shale.||
3284|Cadna-owie Formation|70824|5|Briefly described|p9|Cretaceous|Cretaceous|Eromanga Basin.||||Overlies the Murta Formation and the Hooray and Namur Sandstones. Overlain by the Wallumbilla Formation.||
3284|Cadna-owie Formation|70938|5|Briefly described|p807-808|Early Cretaceous|Early Cretaceous|||Neales River Group.|Mount Anna Sandstone Member.|||
3284|Cadna-owie Formation|71043|5|Briefly described|p106|||Gawler Craton.|||||Shale, minor sandstone.|
3284|Cadna-owie Formation|71251|5|Briefly described|p7-8, p11, p15, p17, p19-20, p29, p49|||Eromanga Basin. 65m total thickness in Eulo 1 borehole. Natural gamma, magnetic susceptibility data tabulated. Conductivity diagrams.|||Wyandra Sandstone Member.|Overlies Hooray Sandstone or (where that unit is absent) Nebine Metamorphics. Is overlain by Wallumbilla Formation.|Fine quartzose sandstone, and dark grey mudstone with carbonaceous flecks; basal conglomerate composed of quartz and basement lithic fragments.|
3284|Cadna-owie Formation|71321|4|Described|p1,15,24-28,65|Early Aptian|Valanginian|Of Eromanga Basin. Deposited under shallow-water, marginal marine conditions. Marks the onset of Early Cretaceous marine transgression (Alexander, et al., 2006; Krieg, et al., 1995; Wopfner, et al., 1970) i.e. westward transgression of a marine epicontinental seaway (Keireg et al., 1995). Paleontological data indicate Valanginian to early Aptian age (Krieg, et al., 1995). Traditionally difficult to differentiate Cadna-owie Formation from the underlying Algebuckina Formation in the TIEYON area, and included as part of Algebuckina Formation in the TIEYON area.||||Conformably underlain by Algebuckina Sandstone. Underlain by the Murta Formation.|Outcrop: Fine- to medium-grained, quartzose sandstones, minor mica, feldspar, heavy minerals, pyrite; glauconite, calcareous beds with ooids. Subsurface: pale grey siltstone with fine-grained sandstone interbeds and minor carbonaceous claystones.|24-OCT-19
3284|Cadna-owie Formation|71342|3|Fully described|Ch 1 p6, Ch 1 p19, Ch4 p4, Ch4 p8-p9|Aptian|Valanginian|Eromanga Basin. This unit was first named the Transition beds by Whitehouse (1955) as it records the transition from terrestrial to marine conditions. This name was first assigned by Wopfner et al (1970) to the mappable interval between the Algebuckina Sandstone and the Bulldog Shale. This units type section is located at Big Cadna-owie Spring and was defined by Wopfner et al., 1970. Hosts a major confined aquifer. Petrography is discussed. This unit is typically 10-20m thick around the basin margin, increasing to 75-100m in the deeper parts of the basin and reaches a maximum thickness in excess of 115m in the Nappamerri Trough. Age based on palynology. This unit is interpreted to have been deposited in shoreface and beach environments and members have been interpreted to have been deposited in fluviodeltaic environments. Sedimentary characteristics are discussed. Spore-pollen zone is given in Ch5 p57. Thermal history briefly described in Ch9.. Laterally equivalent to the Pelican Well Formation and the Parabarana Sandstone.See also Ch4 p20-p27, Ch5 p12, Ch5 p19-p21, Ch5 p24, Ch5 p30, Ch5 p32, Ch5 p38, Ch5 p56-p58, Ch5 p97-p99, Ch6 p7-p8, Ch7 p8-p9, Ch7 p11, Ch7 p13, Ch8 p6, Ch8 p10, Ch8 p23-p24, Ch9 p7, Ch9 p12, Ch9 p18, Ch9 p21, Ch9 p23, Ch10 tbl 10.1, Ch10 p8, Ch10 p17-p20, Ch11 p2, Ch11 p4-p5, Ch12 p12-p14, Ch13 p2, Ch13 p4, Ch13 p8-p9, Ch14 p5.|||Includes the Wyandra Sandstone Member, Mount Anna Sandstone Member, Trinity Well Sandstone Member and the Livingston Tillite Member.|Conformably overlies the Murta Formation. Unconformably overlies the Mount Toondina Formation. Overlies the Algebuckina Sandstone. Overlain by the Bulldog Shale and the Wallumbilla Formation.|Pale grey siltstone with very fine to fine-grained sandstone interbeds and minor carbonaceous claystone. Pebbly layers, diamictites and coarse breccia also occurs.|
3284|Cadna-owie Formation|71348|6|Mentioned|p202|||Geological province: Gawler Craton.||||||
3284|Cadna-owie Formation|71415|5|Briefly described|p11-14|Valanginian|Valanginian|Geological province: SW Thomson Orogen. Of the Kooneberry Belt; of Eromanga Basin. Terrestrial to marine transition sediments (Exon and Senior 1976). LA-ICPMS zircon age populations dominated by Neoproterozoic to Cambrian c. 600 to 316 Ma, and subordiante Mesoproterozoic c. 1300-250 Ma.||||Overlain by Rolling Downs Group. Underlain by Namur Sandstone.||19-AUG-19
3284|Cadna-owie Formation|71863|5|Briefly described|p5|Aptian|Valanginian|Eromanga Basin.|||Includes the Wyandra Sandstone Member.|Overlies the Murta Formation and the Hooray Sandstone. Overlain by the Wallumbilla Formation.||
3284|Cadna-owie Formation|71864|6|Mentioned|p14, p17||||||Includes the Wyandra Sandstone Member.|||
3284|Cadna-owie Formation|72297|6|Mentioned|p742|||Eromanga Basin. Petroleum reservoir.||||||
3284|Cadna-owie Formation|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA,QLD,NSW). Upper part: main confined aquifers, generally producing flowing artesian water bores.||Neales River Group.|Wyandra Sandstone Member.|Overlies Algebuckina Sandstone. Is overlain by Bulldog Shale or Wallumbilla FZ.||
3284|Cadna-owie Formation|72456|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marree 1:250k map sheet.|||||Sandstone, fine-grained, with coarse-grained sandstone beds, and pale grey siltstone, minor conglomerate.|
3284|Cadna-owie Formation|72476|6|Mentioned|p36 Fig.9|||Eromanga Basin. Time-temperature thermal history diagram.||||||
3284|Cadna-owie Formation|72478|5|Briefly described|p6, p8-p10, p12, p25-26,|Early Cretaceous|Early Cretaceous|Eromanga Basin. Represents a marine transgressive phase. See also p51, Fig.7 p70, p72-74, p82-83 [of the document], where described as Cadnaowie sandstone, Cadnaowie sands, Cadnaowie Formation.|c. 130-114 Ma|||Underlies the Bulldog Shale. Unconformably overlies the Algebuckina Sandstone.|Grey sandstone, fine to very-fine sandstone with locally developed coarse sandstone interbeds and carbonaceous claystones.|29-MAR-21
3284|Cadna-owie Formation|72915|6|Mentioned|p27||||||Wyandra Sandstone Member|||
3284|Cadna-owie Formation|72921|6|Mentioned|p16.|||Interpreted as correlative with a variety of units across the Clarence-Moreton, Surat and Eromanga Basins. [All the other units named are Jurassic, and most don't correlate with each other so there is some confusion about the intended meaning here]||||||
3284|Cadna-owie Formation|73090|5|Briefly described|Appendix.|Cretaceous|Cretaceous||||||Sandstone, fine-grained, with coarse-grained sandstone beds and pale grey siltstone, minor conglomerate.|
3284|Cadna-owie Formation|73099|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Eromanga basin.||Marree Subgroup.||Overlies Algebuckina Sandstone conformably and Mount Toondina Formation unconformably.|Ferruginised or kaolinised gritty quartz sandstone; fossil wood.|
3284|Cadna-owie Formation|73167|6|Mentioned|p664 Fig. 2|Cretaceous|Cretaceous|Eromanga Basin.|||Wyandra Sandstone Member|||
3284|Cadna-owie Formation|73203|6|Mentioned|p651-652|Early Cretaceous|Early Cretaceous|[Also misspelt as Cadna-Owie Formation]. A major aquifer host across the Great Artesian Basin. Found in the Jundah 1 well, central Queensland.||||||
3284|Cadna-owie Formation|73249|4|Described|p316-319, p320 Fig.2, p321-338|Barremian|Valanginian|Eromanga Basin. Minimum age of early Barremian. Depositional environments transition from continental (fluvio-deltaic to tidal) to shallow marine, period of marine transgression. Typically 60m thick, can be 10m thick at basin margins and up to 115m thick in the Nappamerri Trough. Dominant mineral phases are kaolinite and quartz, montmorillonite is also present. Deposited in a cold continental, humid climate. Sediment sources interpreted to be a mix of felsic to mafic igneous rocks from the west and south. [Locations in text include p321 Tb.1 and p324 Fig.4.]|||Mount Anna Sandstone Member|Conformably underlies the Bulldog Shale.|Siltstone with interbedded sandstone and mudstone, sandstone dominated with lesser clay-rich horizons, typically 60m thick.|
3284|Cadna-owie Formation|73251|5|Briefly described|p:36-37, 40, 43, 48-50, 52-54, 56-57, 62|Early Cretaceous|Early Cretaceous|Eromanga Basin, Frome Embayment. Marginal thermal maturity. Potential hydrocarbon reservoir and fairway. Contains hydrocarbon accumulations to which the Murta Formation contributed. Non-marine to marginal marine depositional setting. Contains Bulldog [organic] facies 1 [see article].|||Wyandra Sandstone Member|Underlain by Murta Formation and Namur Sandstone. Overlain by Bulldog Shale and Wallumbilla Formation. Equivalent to Parabarana Sandstone.||
3284|Cadna-owie Formation|73281|6|Mentioned|Appendix (DIP)|||Cadna-owie Formation reinterpreted as Cadna-Owie Formation [to indicate capitalisation of both components is considered preferable in this work?]. See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
3284|Cadna-owie Formation|73343|6|Mentioned|p337|Cretaceous|Cretaceous|Eromanga Basin.|||Wyandra Sandstone Member|Underlain by Namur Sandstone and Murta Member. Overlain by Bulldog Shale and Wallumbilla Formation.||
3284|Cadna-owie Formation|73398|5|Briefly described|p1-5, 7-8, 10-11, 13, 16, 19, 21-30|Early Cretaceous|Early Cretaceous|Eromanga Basin. Overlying the Prominent Hill IOCG deposit, this unit contains up to c.5000 ppm Cu; the authors conclude this was due to transport/deposition of mineralised sediments from underlying mineralised rock. Continental fluvial environment. One of the largest confined aquifers in the Great Australian Basin. Geochemistry, weathering analysed in great detail.|140-125 Ma.|||Unconformably overlies Boorthanna Formation. Is overlain conformably by Bulldog Shale.|Interbedded sandstone, siltstone and mudstone.|
3284|Cadna-owie Formation|73479|5|Briefly described|p156 Fig.2, p159, p164 Fig.7, p165-166|Cretaceous|Cretaceous|Eromanga Basin. Fluvial-shallow marine depositional environment. See also p175.|ca 140-126 Ma||Wyandra Sandstone Member|Overlies Namur Sandstone, Murta Member, underlies Wyandra Sandstone Member, Bulldog Shale||
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
3620|Carl Creek Limestone|23031|5|Briefly described|31|||||||||
3620|Carl Creek Limestone|23393|5|Briefly described|p24|Oligocene|Oligocene|||||||
3620|Carl Creek Limestone|23425|4|Described|p383, Table 9.7 p393.|||Geological Province: Karumba Basin.||||||03-AUG-06
3620|Carl Creek Limestone|34061|6|Mentioned|p54|||||||||
3620|Carl Creek Limestone|35620|6|Mentioned|p299|||Location of middle to late Miocene kangaroo.||||||
3620|Carl Creek Limestone|36213|6|Mentioned|p86|||||||||
3620|Carl Creek Limestone|36228|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
3620|Carl Creek Limestone|37607|6|Mentioned|p330|||See also p334 and Fig.5.||||||03-AUG-06
3620|Carl Creek Limestone|38291|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
3620|Carl Creek Limestone|38348|5|Briefly described|p25|||See also p24.||||||03-AUG-06
3620|Carl Creek Limestone|38373|6|Mentioned|p624|||||||||
3620|Carl Creek Limestone|38374|6|Mentioned|p606|||||||||
3620|Carl Creek Limestone|38528|6|Mentioned|p287|||||||||
3620|Carl Creek Limestone|39445|5|Briefly described|Table 14|||||||||
3620|Carl Creek Limestone|39497|6|Mentioned|p16|||||||||
3620|Carl Creek Limestone|39562|5|Briefly described|Map legend|early Miocene|late Oligocene|Massive limestone.   Part of the Trans-Australian Platform Cover.||||||15-JUN-06
3620|Carl Creek Limestone|39797|6|Mentioned|Map legend|Miocene|Miocene|||||||
3620|Carl Creek Limestone|41537|6|Mentioned|Fig.2|||||||||
3620|Carl Creek Limestone|42590|6|Mentioned|p204|||||||||
3620|Carl Creek Limestone|42637|6|Mentioned|p29|||||||||
3620|Carl Creek Limestone|44213|14|Not recorded|Map Legend||Tertiary|||||||
3620|Carl Creek Limestone|44238|14|Not recorded|p219-227,232|Early Miocene|Late Oligocene|See also Fig. 1,3,4,5,6. (L.Olig-Early Miocene).||||||
3620|Carl Creek Limestone|44274|2|Defined|Tb.1,p6,7,12,map||Tertiary|Rests on basement rocks and Thorntonia Limestone. (Tertiary or Late Cretaceous)||||||
3620|Carl Creek Limestone|44281|14|Not recorded|Map Legend||Tertiary|||||||
3620|Carl Creek Limestone|44351|14|Not recorded|p15,16|||Lacustrine,fossils.||||||
3620|Carl Creek Limestone|44482|14|Not recorded|opp.p.6|||(E53-12).||||||
3620|Carl Creek Limestone|44989|4|Described|p.102,127|||Renamed Verdon Limestone by Traves & Noakes 1954, but old name now re-established.||||||03-AUG-06
3620|Carl Creek Limestone|45128|6|Mentioned|p54|||||||||
3620|Carl Creek Limestone|45145|5|Briefly described|p37|||||||||
3620|Carl Creek Limestone|46902|6|Mentioned|Table 1|||Correlation chart for Cainozoic land-surfaces||||||
3620|Carl Creek Limestone|47044|6|Mentioned|p191|||||||||
3620|Carl Creek Limestone|47083|5|Briefly described|p20|Early Miocene|Late Oligocene|||||||
3620|Carl Creek Limestone|50600|5|Briefly described|Map legend|Early Miocene|Late Oligocene|Basal calcite-cemented breccia overlain by a thick-bedded sandy calcirudite containing gastropod and vertebrate remains.||||||
3620|Carl Creek Limestone|60703|5|Briefly described|p704 Fig. 2|Miocene|Miocene|See also p725 Fig. 18 and p731 Fig.20||||||12-APR-05
3620|Carl Creek Limestone|61119|6|Mentioned|p124, p130, p132, p137, pp142-143, p146||Cenozoic|Spring-fed perennial stream and ephemeral pool deposits? Detailed descriptions of Lungfish fossil assemblages included.||||||28-MAR-12
3620|Carl Creek Limestone|61155|5|Briefly described|p16|Miocene|Miocene|Overlain by Wyaaba and Falloch beds. Age: <21.5Ma Together with Gregory Downs Limestone thickness is 12m. Geological Province: Western Cape York, Karumba Basin.||||||03-MAR-10
3620|Carl Creek Limestone|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Neogene|Paleogene|Age:Tertiary.|||||Massive limestone.|
3620|Carl Creek Limestone|67402|5|Briefly described|p177 tbl CRP/KRM1||Longfordian|Karumba Basin. Deposited in a lacustrine environment. Unsuitable reservoir for the storage of carbon dioxide. See also p181 tbl CRP/KRM2, p239. Age probably equivalent to Aquitanian - Burdigalian.||||Overlies the Bulimba Formation. Unconformably overlain by the Wyaaba beds.|Micritic arenaceous limestone, claystone, chert and conglomerate.|17-SEP-18
3620|Carl Creek Limestone|69599|5|Briefly described|p585, p603, p651|Miocene|Oligocene|Riversleigh area, Carpentaria region. Forms escarpments and mesas. Lacustrine sediments. Contains many unnamed karst and lacustrine carbonate deposits (Oligocene to Holocene) containing abundant internationally significant vertebrate fauna (detailed account pp603-605). Silcrete weathered surface.||||Correlated with Carl Creek Limestone.||
3620|Carl Creek Limestone|71502|5|Briefly described|p1|Miocene|Oligocene|Some outcrops display Fe enrichment.||||Unconformably underlain by Thorntonia Limestone.|Freshwater carbonates including a basal calcite-cemented breccia overlain by thickly-bedded sandy calcrudites with gastropod and vertebrate remains.|
3624|Carlo Sandstone|8187|5|Briefly described|Map legend|Ordovician|Ordovician|||||||
3624|Carlo Sandstone|8217|5|Briefly described|Map Legend|Ordovician|Ordovician|Sandstone.||||||
3624|Carlo Sandstone|10116|5|Briefly described|Map Legend|Middle Ordovician|Middle Ordovician|Of the Toko Group. Quartzose sandstone, siltstone and mudstone clasts, minor mudstone.||||||
3624|Carlo Sandstone|12891|5|Briefly described|p733 Fig. 2|Late Ordovician|Middle Ordovocian|Geological province: SW Georgina Basin.||||||07-FEB-11
3624|Carlo Sandstone|12951|5|Briefly described|p143 fig 4, p145 fig 6, p152|Middle Ordovician|Early Ordovician|Georgina Basin.||||||
3624|Carlo Sandstone|13995|6|Mentioned|p76, p101|||Georgina Basin. Contains Middle Ordovician pelecypods.||||||
3624|Carlo Sandstone|22646|6|Mentioned|Fig 5 on p 105|Early Ordovician|Early Ordovician|Georgina Basin.||||||
3624|Carlo Sandstone|22954|6|Mentioned|Fig3p9|Llanvirnian|Llanvirnian|||||||
3624|Carlo Sandstone|24065|4|Described|p235|Middle Ordovician|Early Ordovician|Of Toko Group. Geological Province: Georgina Basin. Maximum thickness: 150m.||||||
3624|Carlo Sandstone|24442|6|Mentioned|p49|||On TOBERMORY sheet.||||||
3624|Carlo Sandstone|33111|4|Described|p33|||||||||
3624|Carlo Sandstone|33657|6|Mentioned|p1|||||||||
3624|Carlo Sandstone|33738|6|Mentioned|p54|||||||||
3624|Carlo Sandstone|34252|6|Mentioned|Po.2|||Fossils||||||
3624|Carlo Sandstone|34454|5|Briefly described|Table 2|||M.Ordovician||||||
3624|Carlo Sandstone|34847|6|Mentioned|Table 1|||Stratigraphy & hydrocarbon prospects||||||
3624|Carlo Sandstone|35121|6|Mentioned|Map legend|Middle Ordovician|Middle Ordovician|||||||
3624|Carlo Sandstone|35139|4|Described|Table.2|||||||||
3624|Carlo Sandstone|36234|3|Fully described|p173|||See also Fig.1.||||||
3624|Carlo Sandstone|36243|6|Mentioned|Table 1A|||||||||
3624|Carlo Sandstone|36580|6|Mentioned|p469|||See also Fig.1||||||
3624|Carlo Sandstone|37572|4|Described|p163|||||||||
3624|Carlo Sandstone|38832|6|Mentioned|p157|||||||||
3624|Carlo Sandstone|39445|5|Briefly described|Table 4|||||||||
3624|Carlo Sandstone|39921|6|Mentioned|Map legend|Middle Ordovician|Middle Ordovician|||||||
3624|Carlo Sandstone|39943|6|Mentioned|Table 2B|||||||||
3624|Carlo Sandstone|40136|5|Briefly described|p20|||||||||
3624|Carlo Sandstone|40810|5|Briefly described|p15|||||||||
3624|Carlo Sandstone|41524|6|Mentioned|p23|||||||||
3624|Carlo Sandstone|42059|6|Mentioned|Fig.2 P131|||||||||
3624|Carlo Sandstone|42060|6|Mentioned|Fig.5 P140|||||||||
3624|Carlo Sandstone|43105|5|Briefly described|Fig.4,p9.|||||||||
3624|Carlo Sandstone|43236|6|Mentioned|p14||Ordovician|Georgina Basin||||||
3624|Carlo Sandstone|43803|6|Mentioned|Fig.5,p71|||||||||
3624|Carlo Sandstone|44308|14|Not recorded|p2,10||Ordovician|||||||
3624|Carlo Sandstone|44309|2|Defined|Tb.1,p5,12,17,map||Ordovician|Fossils. Conformably overlies Nora Formation. Overlain by Mithaka Formation to south. Unit of Toko Group.||||||
3624|Carlo Sandstone|44312|14|Not recorded|Map Legend||Early Ordovician|(Middle Ordovician)||||||
3624|Carlo Sandstone|44326|14|Not recorded|Map Legend||Early Ordovician|(Middle Ordovician)||||||
3624|Carlo Sandstone|44334|14|Not recorded|map legend||Ordovician|Middle Ordovician.||||||
3624|Carlo Sandstone|44358|2|Defined|App.p18|Early Ordovician|Early Ordovician|See also p10, Tb.1. (Middle-Middle Ordovician).||||||11-FEB-09
3624|Carlo Sandstone|44469|2|Defined|p.10, opp.p.6, Tb.I||Ordovician|(F53-12). See also p.15,16,Tb.2. Conf.on Nora Fm. Fossils.Mid.Ordovician. Unit of Toko Group.||||||
3624|Carlo Sandstone|44470|5|Briefly described|map legend||Ordovician|Middle Ordovician.||||||02-DEC-04
3624|Carlo Sandstone|44848|14|Not recorded|p111|||||||||
3624|Carlo Sandstone|44852|14|Not recorded|p71||Ordovician|Middle Ordovician||||||
3624|Carlo Sandstone|44920|14|Not recorded|Map Legend, Sheet 4||Ordovician|Middle Ordovician||||||
3624|Carlo Sandstone|45052|3|Fully described|p128|||Middle Ordovician||||||
3624|Carlo Sandstone|45118|6|Mentioned|p2,3|||||||||
3624|Carlo Sandstone|45148|6|Mentioned|Fig.4|||Georgina Basin||||||
3624|Carlo Sandstone|46841|4|Described|p97|||||||||
3624|Carlo Sandstone|46897|6|Mentioned|Fig.3.|||||||||
3624|Carlo Sandstone|46940|6|Mentioned|p57|||||||||
3624|Carlo Sandstone|46959|6|Mentioned|Table 1|||||||||
3624|Carlo Sandstone|46973|6|Mentioned|Fig.3|||||||||
3624|Carlo Sandstone|47024|6|Mentioned|p1|||||||||
3624|Carlo Sandstone|48901|14|Not recorded|Not recorded||Ordovician|M. Ordovician. pt. Toko Group.||||||
3624|Carlo Sandstone|49027|4|Described|p18|||||||||
3624|Carlo Sandstone|60122|3|Fully described|p32-33, p10 Tb. 1|Middle Ordovician|Middle Ordovician|Of Toko Gp. Resistant, red-brown, well-sorted, fine to medium qtz sst and minor feldspathic sst, with prominent clay-pellet bed at base. Conformably overlies Nora Fm; unconf.underlies Mithaka Fm. and Poodyea Fm. Max. thick: 190m. See also p4-5, p28 Fig 33||||||
3624|Carlo Sandstone|60590|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Of the Toko Group.  Quartzose and minor feldspathic sandstone.  Overlies the Nora Formation.||||||23-DEC-09
3624|Carlo Sandstone|61404|5|Briefly described|Map legend|Middle Ordovician|Middle Ordovician|Of the Toko Group. Quartzose and minor feldspathic sandstone. Geological Province: southern Georgina Basin.||||||12-OCT-05
3624|Carlo Sandstone|64068|3|Fully described|p77, p19|Late Ordovician|Late Ordovician|Forms resistant plateau capping. Conformably and gradationally overlies Nora Formation. Conformably and gradationally overlain by Mithaka Formation, or unconformably by Cravens Peak beds.||Of Toko Group.||Conformably and gradationally overlies Nora Formation. Conformably and gradationally overlain by Mithaka Formation, or unconformably by Cravens Peak beds.|Fine to medium quartz sandstone; minor feldspathic sandstone and siltstone; basal clay-pellet bed.|04-APR-12
3624|Carlo Sandstone|64778|6|Mentioned|p13|Ordovician|Ordovician|Toko Syncline, Southern Georgina Basin.||||||
3624|Carlo Sandstone|64812|5|Briefly described|p237 Fig. 2|Middle Ordovician|Middle Ordovician|Geological Province: southern Georgina Basin.||||||07-FEB-11
3624|Carlo Sandstone|65237|5|Briefly described|p4 Fig. 7, p10|Ordovician|Ordovician|Geological province: southern Georgina Basin.||||||07-FEB-11
3624|Carlo Sandstone|65489|5|Briefly described|p125|Ordovician|Ordovician|Georgina Basin.||||Overlies Nora Formation. Is overlain by Mithaka Formation.||
3624|Carlo Sandstone|67323|5|Briefly described|p83, p90, p92 Fig.12.2, p96|Early Ordovician|Early Ordovician|See also GIS attrib tbl, Solid Geology Map. West Toko Syncline, Georgina Basin. Appears as Carlo Formation on p90 where its aquifer propeties are described.||Toko Group.||Overlies Nora Formation. Is overlain by Mithaka Formation.|Quartzose arenite, siltstone.|
3624|Carlo Sandstone|67402|6|Mentioned|p25, p25 tbl RRM3|Darriwillian|Castlemanian|Georgina Basin, West Toko Syncline. Maximum thickness of 178m. Assessed to be a potential unconventional seal for carbon dioxide storage. Misspelt as the Carlo Formation on p214. Deposited in a high energy barrier beach environment. See also p165 tbl LPB1, p213-p217. ||||Overlies the Nora Formation. Conformably overlain by the Mithaka Formation.|Quartzose sandstone.|
3624|Carlo Sandstone|69437|5|Briefly described|p22:10|Ordovician|Ordovician|Southern Georgina Basin.||||Overlies Nora Formation. Is overlain by Mithaka Formation.||12-JUL-16
3624|Carlo Sandstone|69443|4|Described|p28:7, 27-29, 46|Late Ordovician|Middle Ordovician|Casey in Smith (1963). Southern Georgina Basin. Resistant, range-capping unit. 22-190m thick. Sparse body fossils are listed; ichnofossils are relatively common and diverse throughout. Darriwilian to Sandbian age. Potential petroleum reservoir, sealed by Mithaka Formation.||Toko Group.||Conformably and gradationally overlies Nora Formation. Is overlain conformably and gradationally by Mithaka Formation, or unconformably by Cravens Peak beds.|Medium to thick beds of fine to medium quartz sandstone, and minor feldspathic sandstone and siltstone; various current features. Has a prominent basal clay-pellet bed.|12-JUL-16
3624|Carlo Sandstone|69458|5|Briefly described|p42:20|||Georgina Basin. Clasts of this unit occur in the Poodyea Formation.||||Is overlain unconformably by Poodyea Formation.||14-SEP-18
3624|Carlo Sandstone|69591|4|Described|p87, p95|Ordovician|Ordovician|West Toko Syncline, Georgina Basin. Up to 90m thick. Contains a sparse fossil fauna. Shallow coastal conditions associated with shoaling or barrier island formation are inferred.||Toko Group.||Conformably and transitionally overlies Nora Formation. Is overlain conformably and transitionally by Mithaka Formation.|Fine to medium quartz sandstone. Shows cross-stratification, flute casts and gouge marks, ichnofossils and bioturbation.|
3624|Carlo Sandstone|69599|6|Mentioned|p600|||||||Is overlain unconformably by the Poodyea Formation.||
3624|Carlo Sandstone|69673|5|Briefly described|p114 fig 92, p118, p119 fig 94, p136|Ordovician|Ordovician|Up to 174m thick. Some reservoir potential.||Toko Group||Overlies Nora Formation, overlain by Mithaka Formation|Thickly to medium bedded, fine to medium grained quartz sandstone; minor siltstone.|
3624|Carlo Sandstone|70380|6|Mentioned|p745|Sandbian|Sandbian|Southern Georgina Basin.||||||
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.|
3635|Carmichael Sandstone|12891|5|Briefly described|p733 Fig. 2|Late Ordovician|Late Ordovician|Geological province: Amadeus Basin.||||||07-FEB-11
3635|Carmichael Sandstone|13995|5|Briefly described|p90, p101, p103|Late Ordovician|Late Ordovician|Amadeus Basin. At least in part fluvial deposits. Contains indeterminate remains of ?Arandaspis.||||Conformably overlies Stokes Siltstone.||
3635|Carmichael Sandstone|22561|4|Described|p22||Neoproterozoic|||||||
3635|Carmichael Sandstone|22565|6|Mentioned|p72 & Table 1||Ordovician|Thickness at Areyonga Creek measured from surface expression - 100m thick.  Approx. thickness measured from seismic data - 100m.||||||
3635|Carmichael Sandstone|22566|6|Mentioned|p76|Late Ordovician|Ordovician|Of Larapinta Group.||||||03-AUG-06
3635|Carmichael Sandstone|22646|6|Mentioned|p 105|Ordovician|Ordovician|||||||
3635|Carmichael Sandstone|22650|4|Described|p 162|Ordovician|Ordovician|Of the Larapinta Group.||||||03-AUG-06
3635|Carmichael Sandstone|22651|6|Mentioned|Fig 10 btw p182-183|||Approx age Ordovician - Siluro-Devonian?||||||
3635|Carmichael Sandstone|22656|5|Briefly described|p 280|Late Ordovician|Late Ordovician|Date provided by fish fragments p 280.||||||
3635|Carmichael Sandstone|22761|5|Briefly described|p354|Late Ordovician|Late Ordovician|Of the Larapinta Group.||||||03-AUG-06
3635|Carmichael Sandstone|22763|6|Mentioned|Table 1 on p386||Late Ordovician|Of Larapinta Group.||||||03-AUG-06
3635|Carmichael Sandstone|22804|4|Described|p452|Late Ordovician|Late Ordovician|Of the Larapinta Group.||||||03-AUG-06
3635|Carmichael Sandstone|22805|6|Mentioned|p465||Ordovician|||||||
3635|Carmichael Sandstone|22806|6|Mentioned|Fig 11 on p485|||||||||
3635|Carmichael Sandstone|22807|6|Mentioned|Fig 3 on p495||Late Ordovician|Min. Age - (?)Late Ordovician. Of Larapinta Group.||||||03-AUG-06
3635|Carmichael Sandstone|22826|4|Described|p575|Ordovician|Ordovician|Of the Larapinta Group.||||||03-AUG-06
3635|Carmichael Sandstone|23361|5|Briefly described|16 Fig.4|Early Devonian|Caradoc|Age: 450-400Ma||||||03-AUG-06
3635|Carmichael Sandstone|23858|5|Briefly described|p914|Late Ordovician|Late Ordovician|Of Larapinta Group. Overlain by Mereenie Sandstone; underlain by Stokes Siltstone. Geological Province: Amadeus Basin. Max. thickness: >150 m.||||||03-AUG-06
3635|Carmichael Sandstone|24064|5|Briefly described|p229 Fig.7|Devonian|Silurian|Of the Larapinta Group.  Geological Province: Amadeus Basin.||||||
3635|Carmichael Sandstone|24301|4|Described|p21, p7 Tb. 2|Ordovician|Ordovician|Of Larapinta Group. Previously combined with Stokes Siltstone in "Stokes Formation". Overlies Stokes Siltstone, underlies Mereenie Sandstone.  Maximum thicknes: >150m. Geological Province: Amadeus Basin.||||||
3635|Carmichael Sandstone|24334|5|Briefly described|p43|Late Ordovician|Late Ordovician|Overlain by the Mereenie Sandstone.||||||
3635|Carmichael Sandstone|29721|6|Mentioned|p44|||||||||
3635|Carmichael Sandstone|29972|6|Mentioned|Table 1|||||||||
3635|Carmichael Sandstone|30238|4|Described|p68|||Cambrian - Ordovician age.||||||
3635|Carmichael Sandstone|30258|6|Mentioned|Fig.2|||Ordovician. Part of Larapinta Group.||||||03-AUG-06
3635|Carmichael Sandstone|30544|6|Mentioned|p49|||||||||
3635|Carmichael Sandstone|30659|6|Mentioned|p88|||||||||
3635|Carmichael Sandstone|30662|6|Mentioned|p188|||Upper Ordovician age. Stratigraphy.||||||
3635|Carmichael Sandstone|31566|6|Mentioned|p231|||See also Fig. 2||||||
3635|Carmichael Sandstone|31707|4|Described|p53|||Lithology||||||
3635|Carmichael Sandstone|32208|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
3635|Carmichael Sandstone|32209|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
3635|Carmichael Sandstone|33307|6|Mentioned|Fig.6|||||||||
3635|Carmichael Sandstone|33738|6|Mentioned|p53|||||||||
3635|Carmichael Sandstone|33761|6|Mentioned|p145|||Sil? -Dev. Of the Larapinta Group.||||||03-AUG-06
3635|Carmichael Sandstone|33971|5|Briefly described|p40|||Petroleum potential.||||||03-AUG-06
3635|Carmichael Sandstone|34111|6|Mentioned|p16|||||||||
3635|Carmichael Sandstone|34442|5|Briefly described|Table 1|||Camb.- Ord.||||||
3635|Carmichael Sandstone|35102|6|Mentioned|Fig.2|||||||||
3635|Carmichael Sandstone|36821|6|Mentioned|p398|||||||||
3635|Carmichael Sandstone|37727|6|Mentioned|Fig.1|||||||||
3635|Carmichael Sandstone|39213|6|Mentioned|Fig.6|||Amadeus Basin Succession||||||
3635|Carmichael Sandstone|40136|5|Briefly described|p20|||||||||
3635|Carmichael Sandstone|40740|3|Fully described|p57|||Mention p6||||||03-AUG-06
3635|Carmichael Sandstone|40810|4|Described|p11|||||||||
3635|Carmichael Sandstone|41039|4|Described|p6|||||||||
3635|Carmichael Sandstone|41115|6|Mentioned|Fig.2|||||||||
3635|Carmichael Sandstone|41190|6|Mentioned|Fig.4|||||||||
3635|Carmichael Sandstone|41224|6|Mentioned|p430|||||||||
3635|Carmichael Sandstone|41385|6|Mentioned|p364|||||||||
3635|Carmichael Sandstone|41409|6|Mentioned|p290|||||||||
3635|Carmichael Sandstone|41621|5|Briefly described|Map legend|Late Ordovician||||||||
3635|Carmichael Sandstone|41717|6|Mentioned|Fig.2|||||||||
3635|Carmichael Sandstone|41723|6|Mentioned|Map legend|Ordovician||||||||
3635|Carmichael Sandstone|41819|6|Mentioned|Map legend|Late Ordovician||||||||
3635|Carmichael Sandstone|41820|4|Described|p13|||||||||
3635|Carmichael Sandstone|42037|5|Briefly described|Table 3 P79|||||||||
3635|Carmichael Sandstone|42049|5|Briefly described|p217|||||||||
3635|Carmichael Sandstone|42059|6|Mentioned|Fig.2 P131|||||||||
3635|Carmichael Sandstone|42060|6|Mentioned|Fig.5 P140|||||||||
3635|Carmichael Sandstone|42082|6|Mentioned|Fig.3 P323|||||||||
3635|Carmichael Sandstone|42141|6|Mentioned|Fig.3 P570|||||||||
3635|Carmichael Sandstone|42354|6|Mentioned|p6|||||||||
3635|Carmichael Sandstone|42504|5|Briefly described|p77|||||||||
3635|Carmichael Sandstone|42699|5|Briefly described|map legend|Ordovician||||||||
3635|Carmichael Sandstone|42940|5|Briefly described|Plate 2|Silurian|Silurian|Sandstone, siltstone, claystone; marine fossils. Age: 440-410Ma.  Geological province: Amadeus Basin.||||||23-JAN-08
3635|Carmichael Sandstone|43035|5|Briefly described|p23|||Of Larapinta Group.||||||03-AUG-06
3635|Carmichael Sandstone|43105|5|Briefly described|Fig.3,p8.|||||||||
3635|Carmichael Sandstone|43225|5|Briefly described|Map Legend||Ordovician|Of Larapinta Group.||||||31-MAR-09
3635|Carmichael Sandstone|43503|6|Mentioned|11-39|Bolindian|Eastonian|||||||
3635|Carmichael Sandstone|43646|6|Mentioned|Fig.3,p554||Silurian|||||||
3635|Carmichael Sandstone|43647|6|Mentioned|p530|||||||||
3635|Carmichael Sandstone|43648|6|Mentioned|Fig.1,p488|||||||||
3635|Carmichael Sandstone|43649|5|Briefly described|Fig.1,p454-55,458|||||||||
3635|Carmichael Sandstone|43666|6|Mentioned|p20|||||||||
3635|Carmichael Sandstone|43749|6|Mentioned|p37|||||||||
3635|Carmichael Sandstone|44158|6|Mentioned|p33|||In the Amadeus Basin.||||||03-AUG-06
3635|Carmichael Sandstone|44342|4|Described|p.6, Table 2||Ordovician|SG/53-5. U-M Ordovician.||||||
3635|Carmichael Sandstone|44343|14|Not recorded|map legend||Late Ordovician|U.Ordovician.||||||
3635|Carmichael Sandstone|44395|14|Not recorded|p.9,12, Tb.2||Ordovician|Of Larapinta Group.||||||
3635|Carmichael Sandstone|44396|5|Briefly described|map legend|||(Camb-Ord). SF/52-15. Of Larapinta Group.||||||03-AUG-06
3635|Carmichael Sandstone|44402|5|Briefly described|map legend|Ordovician|Cambrian|Part of Larapinta Group. Camb-Ord.||||||02-DEC-04
3635|Carmichael Sandstone|44484|14|Not recorded|p.11, Tb.1|||Cam-Ord.||||||
3635|Carmichael Sandstone|44485|14|Not recorded|map legend|Ordovician|Cambrian|Part of Larapinta Group. Camb.Ord.||||||
3635|Carmichael Sandstone|44496|5|Briefly described|map legend||Ordovician|Red-brown silty sandstone and white cross-bedded sandstone.||||||02-DEC-04
3635|Carmichael Sandstone|44497|4|Described|p.11, Table 2|Ordovician|Cambrian|SF/53-13. Camb-Ord.||||||
3635|Carmichael Sandstone|44498|14|Not recorded|map legend|Ordovician|Cambrian|Part of Larapinta Group. Camb-Ord.||||||
3635|Carmichael Sandstone|44505|14|Not recorded|p.4,8, Table 1|Ordovician|Cambrian|Of Larapinta Group. Camb-Ord.||||||
3635|Carmichael Sandstone|44506|14|Not recorded|map legend|||Cambrian to Ordovician.||||||
3635|Carmichael Sandstone|45036|6|Mentioned|p3|||Upper Ordovician age||||||
3635|Carmichael Sandstone|45041|2|Defined|p80|Late Ordovician|Late Ordovician|See also p81.||||||03-AUG-06
3635|Carmichael Sandstone|45118|6|Mentioned|p3|||||||||
3635|Carmichael Sandstone|45155|6|Mentioned|Fig.8|||||||||
3635|Carmichael Sandstone|45170|6|Mentioned|p8|||||||||
3635|Carmichael Sandstone|46928|6|Mentioned|Table 1|||||||||
3635|Carmichael Sandstone|47050|6|Mentioned|Fig.2|||||||||
3635|Carmichael Sandstone|47052|6|Mentioned|p261|||||||||
3635|Carmichael Sandstone|48963|6|Mentioned|Fig.3|||||||||
3635|Carmichael Sandstone|50098|6|Mentioned|p1, p3 Fig.2||Late Ordovician|Of the Larapinta Group. Geological Province: Amadeus Basin.||||||
3635|Carmichael Sandstone|60674|5|Briefly described|Map legend|Ordovician|Ordovician|Of the Larapinta Group. Interbedded pale brown to red-brown sandstone, siltstone and mudstone.  Geological Province: Amadeus Basin.||||||23-DEC-09
3635|Carmichael Sandstone|61309|5|Briefly described|p16 Fig. 4|||Geological Province: Amadeus Basin.||||||06-FEB-08
3635|Carmichael Sandstone|61385|5|Briefly described|Map legend|Ordovician|Ordovician|Red-brown silty sandstone, minor siltstone. Geological Province: Amadeus Basin.||||||
3635|Carmichael Sandstone|61387|5|Briefly described|Map legend|Ordovician|Ordovician|Of the Larapinta Group. Red-brown silty sandstone, minor siltstone. Geological Province: Amadeus Basin.||||||
3635|Carmichael Sandstone|61518|5|Briefly described|Map Legend|Ordovician|Ordovician|Of the Larapinta Group. Geological Province: Amadeus Basin.||||||23-DEC-09
3635|Carmichael Sandstone|61519|5|Briefly described|Map Legend|Ordovician|Ordovician|Of the Larapinta Group. Red-brown, silty sandstone, minor siltstone. Geological Province: Amadeus Basin.||||||
3635|Carmichael Sandstone|62376|5|Briefly described|p18|Silurian|Late Ordovician|Of the Larapinta Group. Geological Province: Amadeus Basin.||||||09-FEB-10
3635|Carmichael Sandstone|62379|5|Briefly described|p7 Fig. 2|Ordovician|Ordovician|Of the Larapinta Group. Geological Province: Amadeus Basin.||||||
3635|Carmichael Sandstone|62794|5|Briefly described|p288, p289 Fig.2.|Ordovician|Ordovician|Uppermost unit of Larapinta Group, overlying Stokes Siltstone.||||||
3635|Carmichael Sandstone|62982|5|Briefly described|p7|Ordovician|Ordovician|Of the Larapinta Group. Overlies Stokes Siltstone. Deltaic deposits - immature clastics. Geological Province: Amadeus Basin.||||||31-MAR-09
3635|Carmichael Sandstone|63562|5|Briefly described|p338 fig 3, p350, p352 fig 10|Late Ordovician|Late Ordovician|Of Amadeus Basin. Sedimentation thickens southwards.||||Overlain by Mereenie Sandstone conformably. Correlated with Ethabuka Sandstone.|Mixed fluviatile and marine clastic rocks.|
3635|Carmichael Sandstone|64068|6|Mentioned|p78, 226|||Amadeus Basin. Correlated with Ethabuka Sandstone, Georgina Basin.||||||
3635|Carmichael Sandstone|64334|5|Briefly described|p39-42|Ordovician|Ordovician|Amadeus Basin. Immature deltaic clastic sediments generated by the onset of the Alice Springs Orogeny.||Larapinta Group.||Unconformably overlies Stokes Siltstone. Is overlain unconformably by Mereenie Sandstone.||
3635|Carmichael Sandstone|64778|6|Mentioned|p13|Ordovician|Ordovician|Amadeus Basin.||||||
3635|Carmichael Sandstone|64809|6|Mentioned|p2, p3 Fig.2 |Silurian|Late Ordovician|Dominantly estuarine environment.||||||
3635|Carmichael Sandstone|65233|4|Described|p3 Fig. 2, p9, p10|Late Ordovician|Late Ordovician|Of upper Larapinta Group. Gradational with the overlying Mereenie Sandstone .Max. thickness: 150m. Geological province: Amadeus Basin. Comprises a reasonably continuous red/brown sandstone, siltstone and muidstone succession.||||||07-FEB-11
3635|Carmichael Sandstone|65449|5|Briefly described|p34-35|||Amadeus Basin. Deltaic deposits.||||Disconformably overlies Stokes Siltstone. Time-correlative with Carribuddy Group and Worral Formation.||
3635|Carmichael Sandstone|65489|5|Briefly described|p63, p125|Ordovician|Ordovician|Amadeus Basin. May extend into at least the N part of Pedirka Basin and could provide a potential Ordovician reservoir.||Unit in Larapinta Group.||Overlies Stokes Siltstone.||
3635|Carmichael Sandstone|67326|5|Briefly described|p2|||Amadeus Basin.||Larapinta Group.||Overlies Stokes Siltstone. Is overlain by Mereenie Sandstone.||
3635|Carmichael Sandstone|67565|5|Briefly described|pp41-42, p52.|Late Ordovician|Late Ordovician|Thickness to 150 m. Contains poorly preserved (marine) vertebrate fossils. An important aquifer.|||||Interbedded pale-brown to red-brown sandstone, siltstone and mudstone.|
3635|Carmichael Sandstone|67856|6|Mentioned|p338 fig 4-30|Late Ordovician|Late Ordovician|||Of Larapinta Group.||||
3635|Carmichael Sandstone|67872|5|Briefly described|p13|||Amadeus Basin. Associated with Alice Springs Orogeny.|c.450 Ma.|||||
3635|Carmichael Sandstone|68297|5|Briefly described|p177|Ordovician|Ordovician|Amadeus Basin. Includes disarticulated vertebrate fossils. ||||Younger than Stairway Sandstone||
3635|Carmichael Sandstone|68323|6|Mentioned|p4 Fig.2|Silurian|Late Ordovician|Amadeus Basin.||Larapinta Group.||||
3635|Carmichael Sandstone|69437|5|Briefly described|p22:10|Ordovician|Ordovician|Amadeus Basin.||||Overlies Stokes Siltstone.||12-JUL-16
3635|Carmichael Sandstone|69438|3|Fully described|p23:2-3, 20, 32, 36-37, 46, 48, 56-57|Late Ordovician|Late Ordovician|Wells et al. (1970). Previously mapped as part of upper Stokes Siltstone (eg Pritchard and Quinlan, 1962) or of lower Mereenie Sandstone (eg Ranford et al., 1965). Named after Carmichael Crag at the W end of George Gill Range, Amadeus Basin. The type section is on the N side of the Range, where it is c.100m thick. Maximum thickness is 150m in the S of the Basin. Poorly exposed in the W and absent in the E. Immature deltaic sediments following the Rodingan Event. Also appears as Carmichael Formation on 23:32. Rare ichnofossils and fragmentary fish plates.||Larapinta Group.||Unconformably overlies Stokes Siltstone and Winnall beds. Is overlain conformably, locally (in the E) unconformably, by Mereenie Sandstone.|Interbedded pale brown to red-brown sandstone, siltstone and mudstone. Sandstone is fine- to medium-grained, moderately to poorly sorted. Siltstone and mudstone sometimes have mudcracks and halite pseudomorphs.|12-JUL-16
3635|Carmichael Sandstone|69439|5|Briefly described|p24:10-11|Late Ordovician|Late Ordovician|Amadeus Basin. Possible correlative of Djagamara Formation and/or Kerridy Sandstone (Ngalia Basin).||||||12-JUL-16
3635|Carmichael Sandstone|69443|6|Mentioned|p28:27|||Amadeus Basin.||||Correlated with Toko Group.||12-JUL-16
3635|Carmichael Sandstone|69449|6|Mentioned|p34:2 Fig.34.2|Ordovician|Ordovician|Eastern Amadeus Basin.||||||12-JUL-16
3635|Carmichael Sandstone|69606|5|Briefly described|p4 fig 2|Silurian|Ordovician|Deposited during the Alice Springs Orogeny. Amadeus Basin. Potential reservoir rock.||||Overlies (locally unconformably) the Larrapinta Group. Unconformably overlain by the Mereenie Sandstone.|Sandstone.|
3635|Carmichael Sandstone|69673|5|Briefly described|p64 fig 53, p66, p149 fig 120|Ordovician|Cambrian |150m thick in the southern part of the Amadeus basin.||Larapinta Group||Overlies Stokes Siltstone, overlain by Mereenie Sandstone|Interbedded sandstone, siltstone and mudstone.|
3635|Carmichael Sandstone|71080|6|Mentioned|p30 fig 21|Ordovician|Ordovician|Conformably to unconformably overlies Larrapinta [sic] Group. Unconformably overlain by Mereenie Sandstone. |||||Dominantly sandstone.|
3635|Carmichael Sandstone|71146|5|Briefly described|p6|Wenlock|Llandovery|Amadeus Basin.||Larapinta Group||Overlain by the Mereenie Sandstone.|Sandstone.|
3635|Carmichael Sandstone|71171|6|Mentioned|p2|||Amadeus Basin.||||||
3635|Carmichael Sandstone|71279|5|Briefly described|p355 Fig.2|Late Ordovician|Late Ordovician|Amadeus Basin.||Larapinta Group.||||
3635|Carmichael Sandstone|71800|6|Mentioned|p26 fig 3|Late Ordovician|Late Ordovician|Amadeus Basin.||||Unconformably Overlies the Stokes Siltstone.||
3635|Carmichael Sandstone|72360|5|Briefly described|Map legend|Ordovician|Ordovician|Of Amadeus Basin.||Unit of Larapinta Group.|||Red brown, silty sandstone, minor siltstone.|09-SEP-19
3635|Carmichael Sandstone|72369|4|Described|iii,p3-4,31,34-37|||Of Amadeus Basin. Depositinal environment: shallow marine, hypersaline and fluvial conditions (Owen in Kennard et al 1986). Poorly exposed, and obscured by Mereenie Sandstone scree in western and central Amadeus Basin. Absent in the east Amadeus basin, either non-depositional or eroded prior to Mereenie Sandstone deposition. Forms a prominent scarp where exposed. LA-ICP-MS U-Pb detrital zircon dating of sample HB15ND534 (medium-grained quartz arenite) yielded an interpreted maximum depositional age of 525+\-21 Ma (youngest concordant zircon), does not further constrain the age of the formation as the stratigraphic relationships of the unit imply a significantly younger late Ordovician age. Contains Late Paleoproterozoic to Mesoproterozoic (c. 1855-1015 Ma) zircon age populations that may have been recycled from underlying stratigraphy, or sediment input from Aileron, Warumpi and Musgrave provinces. Archean to early Paleoproterozoic zircons (c. 3215-2005 Ma) may be derived from the North Australian Craton or distal input from greater Gondwana. Cambrian zircon populations (c. 580-490 Ma) may have been derived from distal greater Gondwanan input, as there are no known Cambrian sources proximal to Amadeus Basin. Sample locality, zircon description, SHRIMP results and analyses are discussed.||Unit of Larapinta Group.||Overlain by Mereenie Sandstone. Underlain unconformably by Stokes Siltstone.|Interbedded pale brown to red sandstone; typically fine- to medium-grained with tabular beds and cross-beds, siltstone and mudstone.|18-DEC-19
3635|Carmichael Sandstone|72374|5|Briefly described|iii,p3-4,17-20,24,26|||Of Amadeus Basin. Widely distributed in Amadeus Basin, but only sporadically outcropping to the northern part of the basin. Previous LA-ICP-MS U-Pb zircon analysis yielded a maximum depositional age of c. 525 Ma (Sample HB15VJN534; Normington et al 2018), but this age is older than Upper Ordovician age implied by stratigraphic relationships. Sample HB16ND366 (fine-grained quartz arenite) yielded an interpreted maximum depositional age of 497+\-5 Ma. Dominated by c. 1300-920 Ma zircon age spectrum, likely source from Musgrave Province, either directly, or reworked from the underlying Amadeus Basin succession. Also contains c. 800-490 Ma zircons but no known proximal source, and likely derived distally from greater Gondwana. Older components (c. 3355-1400 Ma) also likely sourced from east Gondwana.||Unit of Larapinta Group.|||Interbedded pale brown to red sandstone, siltstone and mudstone.|
3635|Carmichael Sandstone|73085|6|Mentioned|p1|Silurian|late Ordovician|||||Underlain by Stokes Siltstone. Overlain by Mereenie Sandstone.||
3635|Carmichael Sandstone|73279|5|Briefly described|p3, p12-13|Ordovician|Ordovician|Amadeus Basin. Uppermost part of Larapinta Group. Detrital zircons analysed for Hf isotopic composition [see article].||Larapinta Group||Underlain by Stokes Siltstone.|Includes sandstone.|
3635|Carmichael Sandstone|73346|6|Mentioned|p18-19|Late Ordovician|Late Ordovician|Amadeus Basin. Includes the arandaspid Sacabambaspis sp. Unit has poor age constraint.||||||
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.||
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|||||||
3679|Carrara Range Group|24442|5|Briefly described|p22 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: 1750-1700Ma.  Geological Province: McArthur Basin.  See also p23 Fig. 2.||||||07-NOV-08
3679|Carrara Range Group|38835|6|Mentioned|p164|||||||||
3679|Carrara Range Group|39338|6|Mentioned|p351|||||||||
3679|Carrara Range Group|39422|5|Briefly described|Map legend|Carpentarian|Carpentarian|Includes: Top Rocky Rhyolite, Mitchiebo Volcanics and Don Creek Sandstone.||||||03-AUG-06
3679|Carrara Range Group|39497|4|Described|p7|||||||||
3679|Carrara Range Group|39925|6|Mentioned|p331|||||||||
3679|Carrara Range Group|40840|6|Mentioned|Map legend|||||||||
3679|Carrara Range Group|45166|4|Described|p27|||Mention p8.||||||03-AUG-06
3679|Carrara Range Group|49018|2|Defined|p1|Carpentarian|Carpentarian|||||||
3679|Carrara Range Group|62659|5|Briefly described|Map Legend|Statherian|Statherian|||||||
3679|Carrara Range Group|65337|4|Described|p6 Fig.3,  p10 Table 3, pp11-12. |Paleoproterozoic|Paleoproterozoic|2500 m thick. Leichhardt Superbasin; Lawn Hill Platform. Correlative of Peters Creek Volcanics, Tawallah Group, Eastern Creek Volcanics and Fiery Creek Volcanics. Lower part has sediments and flood basalts; upper part, rhyolitic volcanics and epiclastics.|c.1790-1720 Ma.||Includes Don Creek Sandstone, Mitchiebo Volcanics, Gator Sandstone and Top Rocky Rhyolite.|Unconformably overlies Murphy Metamorphics and Connelly Volcanics. Is overlain unconformably by Surprise Creek Formation.|Basal fluvial quartzose sandstone and flood basalt succession, overlain unconformably by subaerial rhyolitic volcanic and proximal alluvial epiclastic rocks.|
3679|Carrara Range Group|69417|6|Mentioned|p2:5|Statherian|Statherian|South Nicholson/Lawn Hill Basin.||||||12-JUL-16
3679|Carrara Range Group|69433|5|Briefly described|p18:2-3, 5-7, 10|Statherian|Statherian|Southern succession, Lawn Hill Platform. Unconformably overlies the Murphy Province succession.|||Don Creek, Gator Sandstones; Mitchiebo Volcanics; Top Rocky Rhyolite.|Is overlain unconformably by Surprise Creek Formation and McNamara Group. Correlative of Peters Creek Volcanics. Equivalent to the Tawallah Group.||12-JUL-16
3679|Carrara Range Group|69673|6|Mentioned|p3 fig 2, p51|Statherian|Statherian||||Includes Top Rocky Rhyolite, Gator Sandstone, Mitchiebo Volcanics, Don Creek Sandstone|||
3679|Carrara Range Group|71606|5|Briefly described|p137|Statherian|Statherian|South Nicholson Basin, and Lawn Hill Platform, Mount Isa Inlier.||||Overlain unconformably by McNamara Group. Equivalent to Peters Creek Volcanics, correlable to Weberer Granite anf Fiery Creek Volcanics.||
3679|Carrara Range Group|72526|5|Briefly described|p5, p6 Fig.1.2, p8 Fig.1.3.|Statherian|Statherian||||Includes Top Rocky Rhyolite, Gator Sandstone, Mitchiebo Volcanics and Don Creek Sandstone.|||
3679|Carrara Range Group|72527|4|Described|p1, p3,p7, p87, p147-148,p169, p193-194|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin.|||Includes Top Rocky Rhyolite, Gator Sandstone, Mitchiebo Volcanics and Don Creek Sandstone.|Unconformably underlies Surprise Creek Formation and is laterally equivalent to Peters Creek Volcanics.|Includes Rhyolite clasts; the remaining clasts are dominated by sandstone, siltstone, mudstone, layered chert, milky vein quartz and possibly small fragments of mafic volcanics.|
3679|Carrara Range Group|72912|5|Briefly described|p5 Fig.3, p25-26.|Statherian|Statherian|Located in the Lawn Hill Platform of the Mount Isa Province, and the East part of the South Nicholson Basin. Min age from dating Top Rocky Rhyolite, at the top of the Group.|min age c.1725 Ma.||Top Rocky Rhyolite, Gator Sandstone, Mitchiebo Volcanics, Don Creek Sandstone.|Shown as partially overlying Myally Subgroup and partially and unconformably underlying Fiery Creek Volcanics and Bigie Formation.||
3679|Carrara Range Group|72919|6|Mentioned|p3, p5|Paleoproterozoic|Paleoproterozoic||||Top Rocky Rhyolite, Gator Sandstone, Mitchiebo Volcanics, Don Creek Sandstone|Unconformably overlain by Surprise Creek Formation.||
3679|Carrara Range Group|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin region, Calvert Superbasin. Age range indicated to be quite uncertain, with ? above and below.|||Drummond Formation, Surprise Creek Formation*, Top Rocky Rhyolite, Gator Sandstone, Mitchlebo Volcanics, Don Creek Sandstone.|||
3679|Carrara Range Group|73043|6|Mentioned|p15 Fig.8|Paleoproterozoic|Paleoproterozoic|||||||
3701|Carters Bore Rhyolite|22665|5|Briefly described|P221, Table1||Statherian|Age of unit is 1678+/2 Ma||||||
3701|Carters Bore Rhyolite|22680|6|Mentioned|83|||||||||
3701|Carters Bore Rhyolite|23363|5|Briefly described|351 Tab.1|Statherian|Statherian|Age: 1678+/-2Ma.||||||03-AUG-06
3701|Carters Bore Rhyolite|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Fold Belt.||||||07-NOV-08
3701|Carters Bore Rhyolite|23396|5|Briefly described|p419|Statherian|Statherian|Age. 1678+/-2Ma.||||||03-AUG-06
3701|Carters Bore Rhyolite|23397|5|Briefly described|p469|Statherian|Statherian|Age: 1678+/-2Ma.||||||03-AUG-06
3701|Carters Bore Rhyolite|23398|5|Briefly described|p449|Statherian|Statherian|Age: 1678+/-2Ma.||||||03-AUG-06
3701|Carters Bore Rhyolite|23408|5|Briefly described|p513 Fig.2, p514 Fig. 4|||Of McNamara Group.||||||02-APR-07
3701|Carters Bore Rhyolite|23466|5|Briefly described|p268 Fig.2|Statherian|Statherian|Age: 1678+/-2Ma.||||||03-AUG-06
3701|Carters Bore Rhyolite|23776|5|Briefly described|p707 Fig 4|Statherian|Statherian|Age: 1678+/-2 Ma||||||02-NOV-07
3701|Carters Bore Rhyolite|24197|5|Briefly described|p95 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Of the Sybella Suite. Age: 1670Ma. Geological Province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
3701|Carters Bore Rhyolite|24308|5|Briefly described|p987 Fig. 2|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
3701|Carters Bore Rhyolite|24419|5|Briefly described|p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Of the Sybella Suite.  Comagmatic and mainly intrusive.  Geological Province: Western Fold Belt, Lawn Hill Subprovince and Leichardt River Subprovince (Mount Isa Orogen).||||||07-NOV-08
3701|Carters Bore Rhyolite|30534|6|Mentioned|p300|||See also p305.||||||03-AUG-06
3701|Carters Bore Rhyolite|31342|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
3701|Carters Bore Rhyolite|32660|5|Briefly described|Table 5|||||||||
3701|Carters Bore Rhyolite|32959|6|Mentioned|Fig.21|||||||||
3701|Carters Bore Rhyolite|33900|5|Briefly described|p13|||||||||
3701|Carters Bore Rhyolite|35074|6|Mentioned|Fig.2|||||||||
3701|Carters Bore Rhyolite|35167|2|Defined|p155|Carpentarian|Carpentarian|||||||
3701|Carters Bore Rhyolite|35286|4|Described|p145|||||||||
3701|Carters Bore Rhyolite|35458|6|Mentioned|p239|||Listing of new or revised names of units published recently.||||||
3701|Carters Bore Rhyolite|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
3701|Carters Bore Rhyolite|36548|6|Mentioned|p513|||||||||
3701|Carters Bore Rhyolite|37217|6|Mentioned|p650|||||||||
3701|Carters Bore Rhyolite|37413|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
3701|Carters Bore Rhyolite|37459|6|Mentioned|p423|||||||||
3701|Carters Bore Rhyolite|37462|4|Described|Table4.VII|||See also p244.||||||03-AUG-06
3701|Carters Bore Rhyolite|37565|5|Briefly described|p11|||||||||
3701|Carters Bore Rhyolite|37816|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
3701|Carters Bore Rhyolite|38234|4|Described|p104|||||||||
3701|Carters Bore Rhyolite|38237|6|Mentioned|p125|||||||||
3701|Carters Bore Rhyolite|38276|6|Mentioned|Fig.1|||||||||
3701|Carters Bore Rhyolite|38348|6|Mentioned|p6|||||||||
3701|Carters Bore Rhyolite|38350|4|Described|p14|||||||||
3701|Carters Bore Rhyolite|38560|6|Mentioned|p115|||||||||
3701|Carters Bore Rhyolite|38584|6|Mentioned|p17|||||||||
3701|Carters Bore Rhyolite|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
3701|Carters Bore Rhyolite|38834|6|Mentioned|p162|||||||||
3701|Carters Bore Rhyolite|39202|6|Mentioned|p242|||||||||
3701|Carters Bore Rhyolite|39338|6|Mentioned|p352|||||||||
3701|Carters Bore Rhyolite|39445|5|Briefly described|Table 2|||Age: 1678 Ma. See also p36 and p41.||||||03-AUG-06
3701|Carters Bore Rhyolite|39497|6|Mentioned|p19|||||||||
3701|Carters Bore Rhyolite|39925|6|Mentioned|p335|||||||||
3701|Carters Bore Rhyolite|39934|6|Mentioned|Fig.3|||||||||
3701|Carters Bore Rhyolite|40105|6|Mentioned|p310|||||||||
3701|Carters Bore Rhyolite|40221|6|Mentioned|p6|||||||||
3701|Carters Bore Rhyolite|40811|6|Mentioned|p318|||||||||
3701|Carters Bore Rhyolite|40840|6|Mentioned|Map legend|||||||||
3701|Carters Bore Rhyolite|41277|6|Mentioned|Fig.5|||||||||
3701|Carters Bore Rhyolite|41298|6|Mentioned|Map legend|Carpentarian||||||||
3701|Carters Bore Rhyolite|41307|6|Mentioned|p13|||||||||
3701|Carters Bore Rhyolite|41381|6|Mentioned|p323|||||||||
3701|Carters Bore Rhyolite|41721|6|Mentioned|p28|||Correlated with Peters Creek Volcanics.||||||01-AUG-07
3701|Carters Bore Rhyolite|41791|6|Mentioned|p272|||||||||
3701|Carters Bore Rhyolite|41957|6|Mentioned|p68|||||||||
3701|Carters Bore Rhyolite|41978|6|Mentioned|p502|||||||||
3701|Carters Bore Rhyolite|41979|6|Mentioned|p514|||||||||
3701|Carters Bore Rhyolite|42367|5|Briefly described|p17|||Dated at 1678 Ma||||||
3701|Carters Bore Rhyolite|42565|5|Briefly described|Table 1 P5, P4|||||||||
3701|Carters Bore Rhyolite|42706|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Age: ~1880Ma. Porphyritic felsic volcanics.||||||09-FEB-09
3701|Carters Bore Rhyolite|43608|6|Mentioned|Fig.11,p11|||||||||
3701|Carters Bore Rhyolite|43615|6|Mentioned|p13|||Age. 1680+/-3 Ma. (SHRIMP).||||||03-AUG-06
3701|Carters Bore Rhyolite|44195|6|Mentioned|p350|||||||||
3701|Carters Bore Rhyolite|45161|6|Mentioned|p12|||||||||
3701|Carters Bore Rhyolite|45162|6|Mentioned|p11|||See also p45.||||||03-AUG-06
3701|Carters Bore Rhyolite|45166|4|Described|p27|||||||||
3701|Carters Bore Rhyolite|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
3701|Carters Bore Rhyolite|46919|6|Mentioned|p222|||||||||
3701|Carters Bore Rhyolite|46960|6|Mentioned|p216|||||||||
3701|Carters Bore Rhyolite|47083|5|Briefly described|p11|||Overlain by Surprise Crk Fm, Mount Isa Group and McNamara Group; underlain by Haslingden Gp, and Quilalar Fm - unconformable.||||||03-AUG-06
3701|Carters Bore Rhyolite|48997|6|Mentioned|Fig.3|||||||||
3701|Carters Bore Rhyolite|49041|5|Briefly described|Table 1|||||||||
3701|Carters Bore Rhyolite|50100|6|Mentioned|p13 Fig.4|Statherian|Statherian|Geological Province: Western Fold Belt Province.||||||
3701|Carters Bore Rhyolite|50536|5|Briefly described|p1.5, 7.1, 8.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Sybella Suite. Age: 1678 +/- 2Ma (U-Pb-Shrimp).||||||07-NOV-08
3701|Carters Bore Rhyolite|50624|5|Briefly described|p234 Fig.2||Paleoproterozoic|||||||07-NOV-08
3701|Carters Bore Rhyolite|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Porphyritic rhyolite.||||||
3701|Carters Bore Rhyolite|60558|5|Briefly described|p4 Fig. 3|Paleoproterozoic|Paleoproterozoic|Geological Province: Western Fold Belt.||||||03-JUN-09
3701|Carters Bore Rhyolite|61736|5|Briefly described|p672 Fig. 7, p673|Paleoproterozoic|Paleoproterozoic|Age: 1680-1670Ma. Felsic magmatism.||||||
3701|Carters Bore Rhyolite|61929|5|Briefly described|p128 Fig. 2|||||||||
3701|Carters Bore Rhyolite|61936|5|Briefly described|p194 Fig. 6|||Geological Province: Calvert Superbasin, Western Fold Belt, Mount Isa Inlier. See also p196.||||||
3701|Carters Bore Rhyolite|62535|6|Mentioned|p672-673|Statherian|Statherian||1678 +/- 2 Ma.|||||
3701|Carters Bore Rhyolite|62988|5|Briefly described|p34|Paleoproterozoic|Paleoproterozoic|Coeval with Sybella Granite. Age: ~1675-1670Ma. Geological Province: Mount Isa Inlier.||||||07-NOV-08
3701|Carters Bore Rhyolite|63023|5|Briefly described|p1035|Paleoproterozoic|Paleoproterozoic|Of the Sybella Suite. Age: ca 1700Ma. Geological Province: Western Fold Belt. ||||||07-NOV-08
3701|Carters Bore Rhyolite|63110|6|Mentioned|p1141 Fig. 17|Statherian|Statherian|||||||
3701|Carters Bore Rhyolite|63593|6|Mentioned|p288 Fig.2. |||Western Fold Belt. |Between c.1700 and 1670 Ma.|||Is intruded by Sybella Granite.||
3701|Carters Bore Rhyolite|63866|5|Briefly described|p58||||1678 +/- 2 Ma (Page and Sweet, 1998)|||||
3701|Carters Bore Rhyolite|64250|6|Mentioned|p16 fig 6, p11 fig 3, p21|||Western Fold Belt, Mount Isa Inlier. Shallow intrusion.|1678 +/- 2 Ma|||||
3701|Carters Bore Rhyolite|64744|6|Mentioned|p353 Fig.4, p358.|Statherian|Statherian|Mount Isa Basin.|1678 +/- 2 Ma.|||||
3701|Carters Bore Rhyolite|64834|5|Briefly described|p32|||Regionally occurring extrusion.|1678+/-2 Ma|||||
3701|Carters Bore Rhyolite|65228|6|Mentioned|pp20-21, Fig.04.|Statherian|Statherian|Mount Isa region.|1678 +/- 2 Ma.|||||
3701|Carters Bore Rhyolite|65396|5|Briefly described|p16, p82, p175, p190, p193, p241|Statherian|Statherian|Lawn Hill Platform, Western Fold Belt.|1678 +/- 2 Ma||||Rhyolite and mafic volcanics.|
3701|Carters Bore Rhyolite|66800|6|Mentioned|p933.|||Western Fold Belt, Mount Isa Inlier. Correlated with younger parts of Eastern Fold Belt on basis of SHRIMP data (Page and Sun 1998).||||||
3701|Carters Bore Rhyolite|66844|6|Mentioned|p245|Statherian|Statherian|Mount Isa region. Age from SHRIMP dating.|1678+\-2 Ma|||||
3701|Carters Bore Rhyolite|67323|5|Briefly described|GIS attrib tbl, p12, p34, p107|Paleoproterozoic|Paleoproterozoic|See also Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Isa Superbasin. Sybella/Leichhardt River Domain, Mount Isa Inlier. Shown as separating Lower and Upper parts of the Warrina Park Quartzite.|1678 +/- 2 Ma.|||Sybella Batholith rocks are same age.|Porphyritic rhyolite, minor basalt.|
3701|Carters Bore Rhyolite|68021|6|Mentioned|p135 fig 4, p136|Statherian|Statherian|Calvert Superbasin, Western Succession.|1678 Ma|||||
3701|Carters Bore Rhyolite|68146|6|Mentioned|p194||||c.1678 Ma (Page and Sweet, 1998).|||||
3701|Carters Bore Rhyolite|68732|5|Briefly described|p165 Fig.3, p167|Statherian|Statherian|Correlative with the Eastern Creek Volcanics. Igneous crystallisation ages.|1670 +/- 3, 1678 +/- 2 Ma|||||
3701|Carters Bore Rhyolite|69222|5|Briefly described|p222 Fig.2, p223|Statherian|Statherian|Leichhardt River Fault Trough.|1678 +/- 2 Ma (Page and Sweet, 1998).|||Overlies Bigie Formation, Fiery Creek Volcanics, overlain by Surprise Creek Formation||09-FEB-18
3701|Carters Bore Rhyolite|69591|5|Briefly described|p41, p43, p56, p107|||Mount Isa Province. Coeval with emplacement of the Sybella Granite at ~1678 Ma.|1678 +/- 3 Ma (Page and Sweet, 1998).||||Porphyritic rhyolite, minor basalt.|
3701|Carters Bore Rhyolite|70283|6|Mentioned|p25 |Statherian|Statherian|West of the Mount Isa fault zone.|~ 1680 Ma (Page, 1983).|||||14-FEB-18
3701|Carters Bore Rhyolite|70897|6|Mentioned|p41|||Source of 1680 Ma zircons in Mullera Formation.||||||
3701|Carters Bore Rhyolite|71369|6|Mentioned|p4|||||||||
3701|Carters Bore Rhyolite|71592|5|Briefly described|Appendix A.|||Leichhardt River Domain, Mount Isa Orogen.|1678+/-2 Ma (crystallisation: U-Pb zircon SHRIMP)||||Rhyolite.|
3701|Carters Bore Rhyolite|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Lawn Hill Platform of the Mount Isa Province and the east part of the South Nicholson Basin. Age given as U-Pb zircon igneous crystallisation age.|1678+/-2 Ma|||Shown as unconformably and conformably overlying lower Gunpowder Creek Formation.||
3701|Carters Bore Rhyolite|72889|5|Briefly described|p20, p23-25, p28.|Statherian|Statherian|Magmatic age from Page and Sweet (1998). Co-magmatic with Sybella Batholith granites, and dolerite reported herein as 1674+/-2.4 Ma.|1678 +/- 2 Ma.|||Co-magmatic with dolerite reported herein.||
3701|Carters Bore Rhyolite|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Lawn Hill Platform of the Mount Isa Province, and the East part of the South Nicholson Basin. U-Pb zircon igneous crystallisation age (Ma) shown.|1678 +/- 2 Ma|||Shown as unconformably overlying lower Gunpowder Creek Formation and older than Sybella Granite.||
3701|Carters Bore Rhyolite|73042|6|Mentioned|p4|Statherian|Statherian|South Nicholson Basin region and Mount Isa Province, Isa Superbasin. Geochronology is a U-Pb zircon igneous crystallisation age.|1678 +/- 2 Ma (see Fig.1.2)|||||
3701|Carters Bore Rhyolite|73413|6|Mentioned|p3|||Mount Isa Inlier, Western Fold Belt, Lawn Hill Platform.||||||
3701|Carters Bore Rhyolite|73525|5|Briefly described|p4-5 Fig.2|Statherian|Statherian|Mount Oxide-(Ardmore-May Downs) and Leichhardt River Domains.|1678+/-2 Ma crystallisation age||||Felsic extrusives.|
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
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.|
3784|Catfish Conglomerate|41268|5|Briefly described|Fig.10|||||||||
3784|Catfish Conglomerate|72718|6|Mentioned|p7|||Southern McArthur Basin. Batten Fault Zone (south).||Batten Sub-group, McArthur Group||Underlain by Yalco Formation. Overlain[?] by and equivalent to Stretton Sandstone.||
3844|Cavenagh Metamorphics|9199|5|Briefly described|Map legend|||Tonalitic schist, flaggy quartzite, marble.  Geological Province: Arunta Block.||||||04-NOV-04
3844|Cavenagh Metamorphics|22524|6|Mentioned|p39|||||||||
3844|Cavenagh Metamorphics|42770|6|Mentioned|Fig.14|||||||||
3844|Cavenagh Metamorphics|43568|6|Mentioned|Fig.4,p506|||||||||
3844|Cavenagh Metamorphics|50246|5|Briefly described|p9, p21 Fig. 3|Paleoproterozoic|Paleoproterozoic|Mainly metasediments, including calcareous units, and quartzofeldspathic gneiss with minor iron formation. Presented as informal Cavenagh metamorphics in Fig. 3.||||||07-FEB-11
3844|Cavenagh Metamorphics|60547|5|Briefly described|Map Legend|Precambrian|Precambrian|Tonalitic schist, flaggy quartzite, marble.||||||
3844|Cavenagh Metamorphics|62595|5|Briefly described|p9, p31 Fig.9.|||Part of the Alice Springs Arltunga Nappe Complex, a south-directed thrusting event c.430-300 Ma. With Heavitree Quartzite, hosts the Arltunga goldfield deposit. Written as Cavenagh metamorphics in Fig.9.|||||Predominantly metasediments, including calcareous units, and quartzofeldspathic gneiss with minor iron-formation.|13-APR-16
3844|Cavenagh Metamorphics|69427|5|Briefly described|p12:9, 16, 57-58|Paleoproterozoic|Paleoproterozoic|Strangways Range region, Aileron Province. Crops out in the NE part of the White Range Nappe, near the Arltunga goldfield: hosts gold deposits. Metamorphosed at lower amphibolite facies, then retrogressed during the Alice Springs Orogeny.||||Correlated with Tommys Gap Metamorphics.|Two unnamed units: foliated quartzofeldspathic rock, metasedimentary and meta-igneous amphibolites, schists, quartzite, biotite gneiss; and feldspathic schist, quartzite, foliated granite, hornblende amphibolite and quartz-rich metasedimentary rock.|12-JUL-16
3844|Cavenagh Metamorphics|69438|5|Briefly described|p23:49|||Aileron Province.|||||Chloritic schist; quartz-rich metasediment.|12-JUL-16
3844|Cavenagh Metamorphics|73088|6|Mentioned|p2|Palaeoproterozoic|Palaeoproterozoic|Aileron Province||||||
3865|Central Mount Stuart Formation|9380|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Ngalia Basin. Sandstone, siltstone, silty sandstone, pebbly sandstone.||||||
3865|Central Mount Stuart Formation|11884|5|Briefly described|Map Legend|Cambrian|Mesoproterozoic|Adelaidean to Cambrian|||||Pebbly feldspar - quartz sandstone, feldspathic quartzite.|
3865|Central Mount Stuart Formation|22646|6|Mentioned|p 101|Neoproterozoic|Neoproterozoic|Informal name - upper Central Mount Stuart Formation - used p 101||||||04-AUG-06
3865|Central Mount Stuart Formation|23270|5|Briefly described|Table 1, p4||Proterozoic|Of Georgina Basin. Age: Late Proterozoic.||||||19-APR-06
3865|Central Mount Stuart Formation|23271|5|Briefly described|Map legend||Proterozoic|Of Ngalia Basin.  Age: Late Proterozoic.||||||04-AUG-06
3865|Central Mount Stuart Formation|23733|6|Mentioned|p31|Proterozoic|Proterozoic|In BARROW CREEK.||||||
3865|Central Mount Stuart Formation|24111|5|Briefly described|p216|Neoproterozoic|Neoproterozoic|Geological Province: Georgina Basin.||||||24-MAR-05
3865|Central Mount Stuart Formation|32480|6|Mentioned|Map legend|Early Cambrian|Adelaidean|Adelaidean to Early Cambrian||||||
3865|Central Mount Stuart Formation|34810|4|Described|Table 1|||||||||
3865|Central Mount Stuart Formation|35136|6|Mentioned|p141|||||||||
3865|Central Mount Stuart Formation|35221|2|Defined|p13|Late Precambrian|Late Precambrian|||||||
3865|Central Mount Stuart Formation|35254|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
3865|Central Mount Stuart Formation|36335|6|Mentioned|Map legend|Early Cambrian|Adelaidean|Adelaidean to Early Cambrian||||||
3865|Central Mount Stuart Formation|37058|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
3865|Central Mount Stuart Formation|37537|5|Briefly described|Map legend|Adelaidean|Adelaidean|Redbed arenite sequence, local basal diamictite. Lower sandstone, thick bedded, medium grained. Upper sandstone; fine to coarse grained, silty, micaceous feldspathic with arkose, conglomerate, siltstone, shale. Geological Province: Georgina Basin.||||||31-MAR-06
3865|Central Mount Stuart Formation|37627|6|Mentioned|p185|||||||||
3865|Central Mount Stuart Formation|37928|3|Fully described|p522|||See also p515.||||||04-AUG-06
3865|Central Mount Stuart Formation|37929|4|Described|p525|||||||||
3865|Central Mount Stuart Formation|41005|6|Mentioned|p217|||||||||
3865|Central Mount Stuart Formation|41405|6|Mentioned|p205|||||||||
3865|Central Mount Stuart Formation|41801|6|Mentioned|p219|||See also Fig.16||||||
3865|Central Mount Stuart Formation|42504|5|Briefly described|p83|||||||||
3865|Central Mount Stuart Formation|42643|3|Fully described|p21|||||||||
3865|Central Mount Stuart Formation|42644|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Georgina Basin.||||||15-NOV-05
3865|Central Mount Stuart Formation|45148|6|Mentioned|p31|||||||||
3865|Central Mount Stuart Formation|45155|2|Defined|p43|Adelaidean|Adelaidean|See also p26.||||||04-AUG-06
3865|Central Mount Stuart Formation|46844|6|Mentioned|p135|||||||||
3865|Central Mount Stuart Formation|60122|6|Mentioned|p9|||||||||
3865|Central Mount Stuart Formation|60684|6|Mentioned|p1. p24|||On BARROW CREEK map sheet.||||||
3865|Central Mount Stuart Formation|61388|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of the Mopunga Group. Geological Province: Georgina Basin.||||||
3865|Central Mount Stuart Formation|61404|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Mopunga Group. Includes the Adnera and Tops Members and undifferentiated rocks.  Age: Ediacaran.  Geological Province: southern Georgina Basin.||||||
3865|Central Mount Stuart Formation|61560|5|Briefly described|p496|Neoproterozoic|Neoproterozoic|Contains the Spring Range impact structure. Geological Province: southwestern Georgina Basin. Mount is Mt in text. ||||||
3865|Central Mount Stuart Formation|61567|5|Briefly described|p632||Neoproterozoic|Contains body and trace fossils (Mt Skinner fauna) of Late Neoproterozoic age.  Mount is Mt in text.||||||
3865|Central Mount Stuart Formation|61732|3|Fully described|p5 Tb. 1, p110-112|Ediacaran|Ediacaran|Of Mopunga Gp.Consists mainly of red beds, terrestrial or deltaic in origin. Overlies Elkera Fm with an erosional contact. Age appears to range from lower Sturtian to Cambrian in some parts. Geological Prov: Georgina Basin. See also p31, p106.||||||10-APR-12
3865|Central Mount Stuart Formation|62082|5|Briefly described|p65|||Basal part is a saprock of coarse, polymictic grit to conglomerate. Geological Province: Georgina Terrane.  Mount is Mt in text.||||||10-APR-12
3865|Central Mount Stuart Formation|62636|6|Mentioned|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Georgina Basin.||||||
3865|Central Mount Stuart Formation|62642|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Mopunga Group. Geological Province: Georgina/Ngalia Basin. Arkose, subarkose, quartz arenite and siltstone; locally granular, trough cross-bedded.||||||16-AUG-06
3865|Central Mount Stuart Formation|62984|5|Briefly described|p13|Neoproterozoic III|Neoproterozoic III|Of the Mopunga Group. Deltaic clastics. Geological Province: Georgina Basin.||||||23-JAN-07
3865|Central Mount Stuart Formation|63562|6|Mentioned|p345|Early Cambrian||Georgina Basin. |||||Siliciclastic rocks.|06-DEC-17
3865|Central Mount Stuart Formation|64068|4|Described|p51, p44, 47, 53, 55,82 p viii,  p x|Ediacaran|Ediacaran|800 m thick. Modified after Offe (1978). Previously included Amesbury Quartzite Member,  Forster Member. Correlated with Andagera Formation, Elkera Formation, Julie Formation, Arumbera Sandstone, Yuendumu Sandstone. Contains Cu anomalies.||Of Mopunga Group.|Includes Tops and Adnera Members.|Overlies Elkera and Grant Bluff Formations. Is overlain (probably disconformably) by Octy Formation.|Basal polymict conglomerate and  varicoloured sandstone, arkose, siltstone; minor dolostone.|05-APR-12
3865|Central Mount Stuart Formation|64103|6|Mentioned|p401|Early Cambrian|Ediacaran|Geological Province: Georgina Basin.||||||07-FEB-11
3865|Central Mount Stuart Formation|65194|6|Mentioned|p72|||Georgina Basin.||||||
3865|Central Mount Stuart Formation|65237|5|Briefly described|p5|||Caps the Elkera Formation (Mopunga Group). Geological province: southern Georgina Basin. Siliciclastics: immature clastic sediments of fluvial-deltaic origin, increasingly marine to the east.||||||10-APR-12
3865|Central Mount Stuart Formation|65333|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Mopunga Group, Wiso Basin. Cross-section only. Arkose, subarkose, quartz arenite and siltstone.||||||
3865|Central Mount Stuart Formation|65334|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Mopunga Group, Wiso Basin. Subsurface only.  Arkose, subarkose, quartz arenite and siltstone.||||||
3865|Central Mount Stuart Formation|65335|5|Briefly described|Map Legend|||Of Georgina Basin. ?Neoproterozoic. Overlies Lander Rock Formation and granite; low gravity response.||||||
3865|Central Mount Stuart Formation|65338|4|Described|p iv, p60, pp65-67.|Ediacaran|Ediacaran|Georgina Basin. Deltaic clastic rocks.||Unit in Mopunga Group.|Includes Tops and Adnera Members.|Overlies Elkera and Grant Bluff Formations. Unconformably overlies Amesbury Quartzite and Boko Formation. Is dis- or un-conformably overlain by Octy Formation.|Lithic, arkosic and quartzitic arenite, siltstone, dolostone and minor conglomerate.|
3865|Central Mount Stuart Formation|65341|5|Briefly described|p2 Fig.2, p5, pp15-17, p24.|||Type section is at Central Mount Stuart. Younger parts of this Formation are probably lateral equivalents of Mount Baldwin Formation, at least in part. Uneconomic occurrences of Cu, Pb and Zn have been tested.||Unit in Mopunga Group.|Includes Adnera and Tops Members; formerly included Forster Member (now abandoned).|||
3865|Central Mount Stuart Formation|65342|5|Briefly described|p13. |Proterozoic|Proterozoic|Outcrops in Georgina Basin, and is sub-surface in Wiso Basin (Lander Trough). Part of Proterozoic basement; probably Ediacaran. 800 m thick.|||||Arkose, subarkose, quartz arenite and siltstone.|
3865|Central Mount Stuart Formation|65343|5|Briefly described|p3 Fig.4|Neoproterozoic|Neoproterozoic|Georgina Basin. Outlier.||||||
3865|Central Mount Stuart Formation|66767|6|Mentioned|p58-59|Ediacaran|Ediacaran|Terminal Neoproterozoic deposition in the Georgina Basin.||||||
3865|Central Mount Stuart Formation|67164|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Georgina/Ngalia Basins.||Unit in Mopunga Group.||Overlies Grant Bluff Formation.|Arkose, subarkose, quartz arenite and siltstone; locally granular, trough cross-bedded.|
3865|Central Mount Stuart Formation|67352|6|Mentioned|p18|||Lithologically similar to Andagera Formation.||||||
3865|Central Mount Stuart Formation|67565|6|Mentioned|p5 Fig.3.|||||||||04-DEC-15
3865|Central Mount Stuart Formation|67620|6|Mentioned|p22|||Contains the microbial mat structure named Arumberia.||||||
3865|Central Mount Stuart Formation|67892|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|||Unit in Mopunga Group.||Overlies Grant Bluff Formation.|Arkose, subarkose, quartz arenite and siltstone; locally granular, trough cross-bedded.|
3865|Central Mount Stuart Formation|69437|5|Briefly described|p22:4-5, 7-8|Ediacaran|Ediacaran|SW Georgina Basin, Centralian A Superbasin. Supersequences 3 & 4. Terrestrial to deltaic deposits.||||Equivalent to Andagera Formation. Correlated with (lower) Arumbera Sandstone and (upper) Elkera Formation.|Sandstone and siltstone.|12-JUL-16
3865|Central Mount Stuart Formation|69443|4|Described|p28:7-12, 14, 34-35|Ediacaran|Ediacaran|Offe (1978) after Smith and Milligan (1964) and modified by Walter (1980), Haines in Haines et al. (1991) and Haines et al. (2007). Southern Georgina Basin. Up to 780m thick. Fossils listed. Probable correlative of Andagera Formation. Associated with base metal mineralisation in Mount Skinner area.||Mopunga Group.|Tops and Adnera Members.|Conformably overlies Elkera and Grant Bluff Formations. Overlies Amesbury Quartzite unconformably and Boko Formation disconformably. Is overlain (?disconformably) by Octy Formation.|Basal polymict conglomerate and succeeding quartzic, feldspathic and lithic sandstone, arkose, siltstone, dolostone and minor conglomerate.|12-JUL-16
3865|Central Mount Stuart Formation|69673|5|Briefly described|p114 fig 92, p116|Ediacaran|Ediacaran |780m thick.||Mopunga Group||Overlies Grant Bluff Formation, overlain by Andagera Formation|Basal conglomerate overlain by sandstone, siltstone, dolostone and minor conglomerate.|
3865|Central Mount Stuart Formation|69917|4|Described|p115-117|Neoproterozoic|Neoproterozoic|Georgina Basin. 780m thick. Intensely sheared muscovite-bearing psammitic quartzite sampled. U/Pb LA-ICPMS zircon dating shows Musgrave Province events etc. Maximum depostional age: 747+/-9 Ma, but  likely age 550-530 Ma. Walter et al (1995) assigned this unit to Supersequence 4 of their Centralian Superbasin. |||||Terrestrial to deltaic sediments consisting of a basal polymict conglomerate and succeeding sandstone, siltstone and minor dolostone.|
3865|Central Mount Stuart Formation|70839|5|Briefly described|p344|||Of Georgina Basin. Part of Supersequence 4 equivalent to Amadeus Basin. Includes some late Mesoproterozoic age components that could be derived from the Musgrave region (c. 1.19, 1.16, 1.05 Ga; Beyer et al., 2013). Palaeoproterozoic components (major age peak at c. 1.8 Ga), suggest significant Arunta region contribution (Beyer et al., 2013), consistent with sediment transport from NW and evidence for coeval faulting of adjacent Arunta basement (Haines et al., 1991).||||||
3865|Central Mount Stuart Formation|71080|6|Mentioned|p20|Ediacaran|Ediacaran|Georgina Basin. Arumberia locally common.||||||
3865|Central Mount Stuart Formation|71592|5|Briefly described|Appendix A.|||Georgina Basin.|747+/-9 Ma (MDA: zircon U-Pb LA-ICPMS).||||Muscovite-bearing psammitic quartzite.|
3865|Central Mount Stuart Formation|71858|5|Briefly described|p5|||Georgina Basin||||Unconformably overlies the Wangala Granite.||
3865|Central Mount Stuart Formation|72516|6|Mentioned|p86, p90|Ediacaran|Cryogenian|Georgina Basin. Ages based on equivalent units.||||Equivalent to the Elkera Formation and basal diamictite may be equivalent to the Mount Cornish Formation.||02-JUN-21
3865|Central Mount Stuart Formation|73086|6|Mentioned|p133|||Georgina Basin.||||Correlates to Julie Formation.||
3865|Central Mount Stuart Formation|73592|6|Mentioned|p2|||Aileron Province.|||Tops Member.|||
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
3897|Chambers River Formation|22538|6|Mentioned|Fig3 P708|||||||||
3897|Chambers River Formation|23216|4|Described|Table1p7, p35, p51|||Of Roper River Group. Consists of mainly quartz-rich siltstone and sandstone, and rarely exposed quartz-poor mudstone. Conformably overlies Bukalorkmi Sandstone Member (McMinn Formation). Max. thickness: ~2000m.||||||19-JAN-06
3897|Chambers River Formation|23404|5|Briefly described|p639|||Of Roper Group.||||||
3897|Chambers River Formation|23937|2|Defined|p75 App. 1|Calymmian|Calymmian|Of the Maiwok Subgroup (Roper Group).  Unconformably overlain by Antrim Plateau Volcanics; conformably underlain by Bukalorkmi Sandstone.  Max. thickness: <300m.  Geological Province: McArthur Basin.||||||
3897|Chambers River Formation|32660|6|Mentioned|Fig.7|||||||||
3897|Chambers River Formation|40691|6|Mentioned|Fig.4|||||||||
3897|Chambers River Formation|41268|6|Mentioned|p293|||||||||
3897|Chambers River Formation|42395|6|Mentioned|Fig.26 P86|||||||||
3897|Chambers River Formation|42639|6|Mentioned|p44|||top of Maiwok Subgroup||||||
3897|Chambers River Formation|42812|6|Mentioned|p54|||||||||
3897|Chambers River Formation|42846|5|Briefly described|Fig.1 p502|||Of Roper Group. Geological Province: McArthur Basin.||||||09-MAY-05
3897|Chambers River Formation|43010|5|Briefly described|Fig.6||Mesoproterozoic|Of Maiwok Subgroup. Of "Mid Proterozoic"age.||||||04-AUG-06
3897|Chambers River Formation|43149|5|Briefly described|Map Legend||Mesoproterozoic|of Maiwok Subgroup. Of Calymmian age.||||||
3897|Chambers River Formation|44201|14|Not recorded|p.9|||||||||
3897|Chambers River Formation|44332|14|Not recorded|p.8,opp.6,map|||(D53-14).||||||
3897|Chambers River Formation|44333|14|Not recorded|map legend|||Upper(?) Proterozoic.||||||
3897|Chambers River Formation|44471|14|Not recorded|p.10, opp.p.7, map|||(D53-10). Top formation of Maiwok Subgroup, Roper Group.||||||
3897|Chambers River Formation|44472|5|Briefly described|map legend|||Of the Maiwok Sub-Group.  Blocky quartz sandstone, flaggy micaceous quartz sandstone, siltstone.  Upper (?) Proterozoic.||||||02-DEC-04
3897|Chambers River Formation|45022|4|Described|p.84||Adelaidean|Of Maiwok Subgroup.  Tb.11, Pl.28.||||||
3897|Chambers River Formation|45162|6|Mentioned|Fig.4|||||||||
3897|Chambers River Formation|46679|14|Not recorded|map legend||Neoproterozoic|Upper Proterozoic.||||||
3897|Chambers River Formation|46861|6|Mentioned|Fig.2a|||||||||
3897|Chambers River Formation|60573|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Roper Group.  Thin bedded siltstone, mudstone and very fine sandstone; micaceous.  Does not outcrop in the Roper River mapsheet area.||||||23-DEC-09
3897|Chambers River Formation|61390|5|Briefly described|Map Legend|Ectasian|Calymmian|Of the Maiwok Subgroup. Thin bedded siltstone, mudstone and very fine grained sandstone: micaceous.||||||23-DEC-09
3897|Chambers River Formation|64784|6|Mentioned|p3|||McArthur Basin.||||||
3897|Chambers River Formation|64816|6|Mentioned|p2 Fig.1|||||Unit in Roper Group.||||
3897|Chambers River Formation|64817|6|Mentioned|p353 Fig.4 |||||Of the Roper Group||||
3897|Chambers River Formation|69018|6|Mentioned|p450 Fig.1b|||||Of Roper Group.||||
3897|Chambers River Formation|69430|4|Described|p15:3, 27, 29-30|Calymmian|Calymmian|Roper River region, NW McArthur Basin. Up to 300m thick. Storm-dominated shelf sediments.||Maiwok Subgroup.||Overlies Bukalorkmi Sandstone probably conformably.|Thinly to medium bedded, laminated micaceous siltstone and mudstone; minor very fine sandstone.|12-JUL-16
3897|Chambers River Formation|69673|6|Mentioned|p16 fig 13, p38|||Northwestern and Southern McArthur Basin.||||Overlies McMinn Formation||
3897|Chambers River Formation|70734|6|Mentioned|p16 Fig. 2|||McArthur Basin. 2000 m thick? Storm-dominated shelf (mudstone-dominated, at base).||||Overlies the McMinn Formation.||10-JUL-18
3897|Chambers River Formation|70897|6|Mentioned|Fig.1.7.6,9|||McArthur Basin.||||||28-NOV-17
3897|Chambers River Formation|70968|2|Defined|p51, p82-86, p88-89, p124-126, p131-132 |Tonian|Mesoproterozoic|See also p140, p143. Sweet in Abbott et al. (2001) after Dunn (1963). First mapped by Walpole (1958) as the Chambers River Beds. Named after Chambers River. Generally poor exposure: forms low, rubble-strewn rounded hills. Age and stratigraphic affinities (especially with Hayfield mudstone) are unclear. Up to c.2000m thick, thinning to the E and SE to <300m. The complicated type section (described) starts from 306200mE 8386800mN (base) and ends at 304900mE 8390700mN in the KATHERINE sheet. The variable lithologies are briefly described. Coastal tidal platform sediments.||Maiwok Subgroup.||Overlies Bukalorkmi Sandstone conformably /possibly disconformably. Is overlain unconformably by Antrim Plateau Volcanics and Bukalara Sandstone.|Mudrocks, siltstone and subordinate sandstone in varying proportions: thinly interbedded siltstone, laminated siltstone to claystone and very fine-grained sandstone beds.|
3897|Chambers River Formation|71059|4|Described|p3|Mesoproterozoic|Mesoproterozoic|McArthur Basin. <300-2000m thick. Storm-dominated marine shelf deposits.||Maiwok Subgroup.||Conformably overlies Bukalorkmi Sandstone. Is overlain unconformably by Bukalara Sandstone.|Mudrock, siltstone and sandstone in varying proportions.|
3897|Chambers River Formation|71374|3|Fully described|iii, p1 tbl 1, p21-p23, p53-p54|Ectasian|Ectasian|McArthur Basin. Type area occurs near Katherine. The type section of Sweet in Abbott et al (2001) occurs from about 306200mE 8386800mN to 304900mE 8390700mN. SHRIMP age is interpreted as a maximum depositional age. Possible Musgrave zircon provenenance. Sampling site provided along with zircon description and SHRIMP analytical discussion.|1320 +/- 15 Ma (SHRIMP U-Pb)|Roper Group||Overlies the Bukalorkmi Sandstone. Unconformably overlain by the Antrim Plateau Volcanics and Bukalara Sandstone. Equivalent to the Hayfield mudstone.|Well exposed, quartz-rich, fine- to medium-grained sandstone and more rarely exposed siltstone and quartz-poor claystone.|02-MAY-18
3897|Chambers River Formation|71488|5|Briefly described|p141 fig 1b, p142|||Beetaloo Sub-basin. Possibly a correlative of ungrouped units at the top of the Beetaloo Sub-basin rather than a part of the Roper Group.||||Overlies the Bukalorkmi Sandstone.||02-MAY-18
3897|Chambers River Formation|71779|5|Briefly described|p2 Fig.1|||Urapunga Region, McArthur Basin.||Maiwok Subgroup||||24-SEP-18
3897|Chambers River Formation|71893|5|Briefly described|p8, p37|||McArthur Basin.||Maiwok Subgroup||Overlies the Bukalorkmi Sandstone.||
3897|Chambers River Formation|72718|6|Mentioned|p7, p9|||Southern McArthur Basin. Wilton package (uppermost units). Urapunga Fault Zone, southwestern McArthur Basin, and Batten Fault Zone (north). Absent from the Beetaloo Sub-basin.||||Underlain by Derim Derim Dolerite. Overlain by Jamison sandstone.||
3897|Chambers River Formation|73242|5|Briefly described|p39|||||Maiwok Subgroup, Roper Group||Underlain by Bukalorkmi Sandstone.|Includes interbedded mudstone and fine sandstone.|
3910|Channingum Granite|22645|6|Mentioned|Table3 P213||Orosirian|Age of unit is 1840+/-9 Ma.||||||04-AUG-06
3910|Channingum Granite|23410|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Granite: biotite-bearing; seriate porphyritic to equigranular, medium to coarse grained and massive. Minor rapakivi texture. Minor metasediment and dolerite xenoliths. Alteration including silicification, albitisation and tourmalisation.||||||07-NOV-08
3910|Channingum Granite|23733|5|Briefly described|p7 Fig.1|Paleoproterozoic|Paleoproterozoic|Of the Mount Tennant Supersuite.  Age: 1840Ma.  See also p34 Fig. 20.||||||07-NOV-08
3910|Channingum Granite|23809|5|Briefly described|p29, p27 Fig. 25|Paleoproterozoic|Paleoproterozoic|Of the Tennant Creek Supersuite.  Age: 1840Ma.  Geological Province: Tennant Inlier.||||||07-NOV-08
3910|Channingum Granite|24172|5|Briefly described|p38|Paleoproterozoic|Paleoproterozoic|Previously referred to informally as "New Hope granite" and "Channingum granite" (Mendum & Tonkin, 1976). Intrudes the Yungkulungu Formation (Flynn Subgroup) as six small plutons. Age: 1850+/-6Ma (Compston, 1994).||||||07-NOV-08
3910|Channingum Granite|24197|5|Briefly described|p68 Tb. 6.1|Paleoproterozoic|Paleoproterozoic|Of the Tennant Creek Supersuite. Age: ~1850Ma. Geological Province: Tennant Creek/Davenport Province. See also the misspelt Chaninggum Granite.||||||07-FEB-11
3910|Channingum Granite|29135|4|Described|p39|||Informal use of name. -Pga & -Pgb on Tennant Creek 1:250k sheet.||||||
3910|Channingum Granite|43224|5|Briefly described|Map legend||Paleoproterozoic|||||||07-NOV-08
3910|Channingum Granite|43850|4|Described|p263|||Previously New Hope Granite (Mendum + Tonkin 1976).||||||23-DEC-08
3910|Channingum Granite|46842|6|Mentioned|p117|||||||||
3910|Channingum Granite|50588|5|Briefly described|p1.4, 2.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Tennant Creek/Davenport Province. Of the Tennant Creek Supersuite. Age: 1840 +/- 9Ma (SHRIMP).||||||17-APR-15
3910|Channingum Granite|60684|5|Briefly described|p51-52 Appendix|Paleoproterozoic|Paleoproterozoic|Previously mapped as New Hope Granite. Two-feldspar, biotite- to biotite-bearing granite, predominantly alkali feldspar, sodic plagioclase, strained quartz and red-brown biotite. Intrudes Flynn Subgroup (Yungkulungu Fm).Age: 1833+/-4Ma (Compston 1991).||||||07-NOV-08
3910|Channingum Granite|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Tennant Creek Supersuite. Biotite granite, seriate porphyritic to equigranular; rapakivi texture; minor xenoliths and rare porphyritic enclaves. In the Tennant Creek region.||||||07-NOV-08
3910|Channingum Granite|64559|6|Mentioned|p973|||Age: 1840+/-9Ma (U-Pb).||||||23-DEC-08
3910|Channingum Granite|65209|6|Mentioned|p35 Fig.1|Paleoproterozoic|Paleoproterozoic|||Tennant Creek Supersuite||||
3910|Channingum Granite|65222|5|Briefly described|p110 Fig.2, p116 Tb 3, p118, 119, 125|Orosirian|Orosirian|Intruded post regional deformation. Zircon sample locality.|1840+/- 9 Ma U/Pb SHRIMP.|||Apparently intrudes the base of the Flynn Subgroup.|Undeformed even-grained massive granite. I-type.|24-JAN-22
3910|Channingum Granite|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Tennant Creek Supersuite.|||Biotite-bearing granite, seriate porphyritic to equigranular, rapakivi texture, minor xenoliths and rare porphyritic enclaves.|
3910|Channingum Granite|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Tennant Creek/Davenport area.|1840 +/- 9 Ma.|||Intrudes Ooradidgee Group.||
3910|Channingum Granite|69187|5|Briefly described|p52, p53 Fig.2, p54 Fig.3|||Warramunga Province. Large intrusive complex||Tennant Creek Supersuite||intrudes Warramunga Formation||
3910|Channingum Granite|69424|5|Briefly described|p9:3, 11-13, 17, 22|Paleoproterozoic|Paleoproterozoic|Warramunga Province. Has a narrow zone of quartz-muscovite schist at contact with Ooradidgee Group. U-Pb zircon age.|1840 +/- 9 Ma (Compston, 1995).|Tennant Creek Supersuite.||Intrudes Yungkulungu Formation (Ooradidgee Group).|Medium- to coarse-grained, equigranular to seriate porphyritic granite (syeno- to monzogranite); minor rapakivi texture; hiatal-textured porphyry forms marginal phase to granite; rare felsic porphyry autoliths and late-stage aplite dykes.|12-JUL-16
3910|Channingum Granite|71592|5|Briefly described|Appendix A.|||Tennant Creek Region.|1840+/-9 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
3910|Channingum Granite|73124|6|Mentioned|p2 Fig.1|||||Tennant Creek Supersuite||||
3910|Channingum Granite|73125|5|Briefly described|p2|Palaeoproterozoic|Palaeoproterozoic|Warramunga Province.||Tennant Creek Supersuite.||||
3910|Channingum Granite|73460|6|Mentioned|p2|||Warramunga Province.||Tennant Creek Supersuite||||
3910|Channingum Granite|73590|6|Mentioned|p2|||||Tennant Creek Supersuite||||
3934|Chatsworth Limestone|22646|6|Mentioned|Fig 5 on p 105||Cambrian|Of the Georgina Basin.||||||02-APR-07
3934|Chatsworth Limestone|22954|4|Described|p8,10-1,Fig5p16||Payntonian|||||||
3934|Chatsworth Limestone|23553|5|Briefly described|p2276|Ordovician|Cambrian|Geological Province: Georgina Basin.||||||
3934|Chatsworth Limestone|24065|5|Briefly described|p234|Late Cambrian|Late Cambrian|Geological Province: Georgina Basin. Maximum thickness: 460m.||||||11-JUN-08
3934|Chatsworth Limestone|30479|6|Mentioned|Fig.5|||Stratigraphic relations||||||
3934|Chatsworth Limestone|30598|6|Mentioned|p50|||||||||
3934|Chatsworth Limestone|30778|6|Mentioned|p5,Fig.5|||||||||
3934|Chatsworth Limestone|30914|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
3934|Chatsworth Limestone|31572|3|Fully described|Fig. 1|Late Cambrian|Late Cambrian|Refers Casey (1959).||||||11-JUN-08
3934|Chatsworth Limestone|32576|6|Mentioned|Fig.2|||||||||
3934|Chatsworth Limestone|32952|4|Described|p1188|||See also pp1190,1192,1193. M.-U. Cambrian||||||04-AUG-06
3934|Chatsworth Limestone|33111|4|Described|p33|||Mention p4.||||||04-AUG-06
3934|Chatsworth Limestone|33482|6|Mentioned|Fig.1|||Middle - Upper Cambrian||||||
3934|Chatsworth Limestone|33738|6|Mentioned|p49|||||||||
3934|Chatsworth Limestone|35121|6|Mentioned|Map legend|Late Cambrian|Late Cambrian|||||||
3934|Chatsworth Limestone|35139|4|Described|Table.2|||||||||
3934|Chatsworth Limestone|35936|6|Mentioned|p614|||||||||
3934|Chatsworth Limestone|37413|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
3934|Chatsworth Limestone|37572|4|Described|p160|||See also Fig.8||||||
3934|Chatsworth Limestone|38444|6|Mentioned|p106|||||||||
3934|Chatsworth Limestone|38446|5|Briefly described|p152|||||||||
3934|Chatsworth Limestone|38532|4|Described|Fig.1|||||||||
3934|Chatsworth Limestone|38608|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
3934|Chatsworth Limestone|39029|5|Briefly described|Map legend|Cambrian|Cambrian|||||||25-AUG-04
3934|Chatsworth Limestone|39445|5|Briefly described|Table 4|||See also p64.||||||02-APR-07
3934|Chatsworth Limestone|39690|6|Mentioned|Fig.2|||||||||
3934|Chatsworth Limestone|40136|5|Briefly described|p21|||||||||
3934|Chatsworth Limestone|40810|5|Briefly described|p14|||||||||
3934|Chatsworth Limestone|40852|6|Mentioned|Fig.3.7|||||||||
3934|Chatsworth Limestone|41109|6|Mentioned|p184|||||||||
3934|Chatsworth Limestone|41306|6|Mentioned|p4|||||||||
3934|Chatsworth Limestone|41587|6|Mentioned|p913|||||||||
3934|Chatsworth Limestone|42058|4|Described|p115|||||||||
3934|Chatsworth Limestone|42139|6|Mentioned|Fig.9 P72|||||||||
3934|Chatsworth Limestone|42354|6|Mentioned|p11|Payntonian||See also p20. Age: Late Cambrian (early Payntonian).||||||11-JUN-08
3934|Chatsworth Limestone|43579|6|Mentioned|p367||Late Cambrian|||||||
3934|Chatsworth Limestone|43781|6|Mentioned|p18|||||||||
3934|Chatsworth Limestone|43807|5|Briefly described|p345-6|||||||||
3934|Chatsworth Limestone|43883|14|Not recorded|p18 Fig.4-3|||||||||
3934|Chatsworth Limestone|43995|14|Not recorded|p62,7||Late Cambrian|||||||
3934|Chatsworth Limestone|44091|14|Not recorded|p17,Tb.1,p19||Late Cambrian|1d a mean.||||||
3934|Chatsworth Limestone|44211|2|Defined|p90,96,100,104,107||Late Cambrian|Rests above Pomegranate Limestone. Overlain by Ninmaroo Formation. (Franconian - Trempealeauan).||||||21-APR-09
3934|Chatsworth Limestone|44275|14|Not recorded|Map Legend|||||||||
3934|Chatsworth Limestone|44276|2|Defined|Tb.2,p20,22|||||||||
3934|Chatsworth Limestone|44277|14|Not recorded|Map Legend||Late Cambrian|||||||
3934|Chatsworth Limestone|44291|14|Not recorded|p7||Late Cambrian|||||||
3934|Chatsworth Limestone|44361|14|Not recorded|Map Legend||Late Cambrian|||||||
3934|Chatsworth Limestone|44362|4|Described|Tb.1,p9||Late Cambrian|||||||
3934|Chatsworth Limestone|44457|14|Not recorded|p.6||Late Cambrian|Upper Cambrian. (F53-10).||||||
3934|Chatsworth Limestone|44543|2|Defined|p32,33,36|Late Cambrian|Middle Cambrian|Overlies O'Hara Shale.||||||
3934|Chatsworth Limestone|44620|14|Not recorded|p88||Late Cambrian|Conodonts.||||||
3934|Chatsworth Limestone|44719|14|Not recorded|p143|||Upper two-thirds of the Upper Cambrian conodonts.||||||
3934|Chatsworth Limestone|44848|14|Not recorded|p110|||||||||
3934|Chatsworth Limestone|44920|14|Not recorded|Map Legend, Sheet4||Late Cambrian|||||||
3934|Chatsworth Limestone|45002|14|Not recorded|p18,20-22|||Late Cambrian fossils.||||||
3934|Chatsworth Limestone|45012|14|Not recorded|p6.31|||Upper Cambrian fauna.||||||
3934|Chatsworth Limestone|45044|14|Not recorded|p5||Late Cambrian|||||||
3934|Chatsworth Limestone|45051|5|Briefly described|Fig.3|||See also p1,4,5,9. Upper Cambrian age.||||||04-AUG-06
3934|Chatsworth Limestone|45052|2|Defined|p113|Late Cambrian|Late Cambrian|||||||
3934|Chatsworth Limestone|45053|6|Mentioned|p4|||Lithology equivalent Gola Beds||||||
3934|Chatsworth Limestone|45058|6|Mentioned|p8|||See also p23. Correlation with Clark Sandstone.||||||02-APR-07
3934|Chatsworth Limestone|45079|6|Mentioned|p34|||Cambrian age. Lithology||||||
3934|Chatsworth Limestone|45094|4|Described|p7|||||||||
3934|Chatsworth Limestone|45130|4|Described|p3|||||||||
3934|Chatsworth Limestone|45166|5|Briefly described|Table 15|||||||||
3934|Chatsworth Limestone|46887|6|Mentioned|p253|||||||||
3934|Chatsworth Limestone|46897|6|Mentioned|Fig.2|||||||||
3934|Chatsworth Limestone|46958|6|Mentioned|Fig.2|||||||||
3934|Chatsworth Limestone|48906|14|Not recorded|Tb.1,App.D|||||||||
3934|Chatsworth Limestone|50100|5|Briefly described|p22|Early Ordovician|Early Cambrian|Grey to dark grey and locally fossiliferous.  Overlies the O'Hara Shale.  ||||||
3934|Chatsworth Limestone|50244|5|Briefly described|p88, p89 Fig. 1, p92 Fig. 3, p95, p99|Cambrian|Cambrian|Includes Lily Creek Member. Geological Province: Georgina Basin. Carbonates, generally medium- to dark-grey or reddish grey limestones and marls with subhorizontal bedding. On p100 Fig. 7 also.||||||
3934|Chatsworth Limestone|60359|5|Briefly described|Map Legend|Ordovician|Cambrian|Limestone; minor breccia, marl.||||||
3934|Chatsworth Limestone|60419|5|Briefly described|p42|Late Cambrian|Late Cambrian|Contains echinoderms. Geological Province: Georgina Basin.||||||
3934|Chatsworth Limestone|62793|6|Mentioned|p272, p281, p282, p283|Late Cambrian|Late Cambrian|Contains conodont fossils including Prooneotodus terashimai, characteristic of the upper Iverian Stage of the Late Cambrian.||||Underlies Ninmaroo Formation.||21-MAR-12
3934|Chatsworth Limestone|63450|5|Briefly described|p78 Fig. 5, p82|Late Cambrian|Late Cambrian|Thickness: 500m. Geological province: Georgina Basin, Burke River Structural Belt. Contains calcareous siltstone, pelletal limestone, minor calcareous siltstone, calcareous sandstone, skeletal grainstones and intraformational breccia.||||||07-FEB-11
3934|Chatsworth Limestone|64068|3|Fully described|p70-71, p73, 74, p8, 225|Late Cambrian|Late Cambrian|Formerly Gola beds of Casey (1959). Thickness 158 m in type section. Max. 880 m. Paleopoles from this (and other) units define a major change in APWP.||Of Cockroach Group.|Includes Lily Creek Sandstone Member at top.|Conformably and gradationally overlies Pomegranate Limestone. Conformably and gradationally overlain by and may interdigitate with Ninmaroo Formation.|Limestone, calcareous siltstone, sandstone, quartzic dolostone, intraformational breccia and chert.|21-MAR-16
3934|Chatsworth Limestone|65489|5|Briefly described|p126-127|Late Cambrian|Late Cambrian|Burke River Structural Belt, Georgina Basin. Little hydrocarbon potential: TOC at 0.12%.||||Is overlain conformably by Ninmaroo Formation.||
3934|Chatsworth Limestone|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map; p83|Late Cambrian|Late Cambrian|Burke River Structural Belt, Georgina Basin.||Cockroach Group.||Overlies Pomegranate Limestone. Is overlain by Ninmaroo Formation.|Thin-bedded, light to medium grey limestone (peloid grainstone), sandy and intraclast limestone, calcareous siltstone.|
3934|Chatsworth Limestone|67402|6|Mentioned|p216|||Georgina Basin. Potential seal unit.|||||Fine-grained limestone.|
3934|Chatsworth Limestone|67870|5|Briefly described|p39, p43-46|Cambrian|Cambrian|Georgina Basin. Part of a ~600m thick package with high amplitude discontinuous seismic reflections.||Cockroach Group.||||
3934|Chatsworth Limestone|69377|5|Briefly described|map legend|Cambrian|Cambrian|||Cockroach Group|||Thin-bedded, limestone (peloid grainstone), sandy and intraclast limestone and calcareous siltstone|
3934|Chatsworth Limestone|69443|5|Briefly described|p28:7, 25-26|Late Cambrian|Late Cambrian|Southern Georgina Basin. Contains trilobites and conodonts which indicate Iverian and Payntonian stages (Late Cambrian/Furongian).||Cockroach Group.||Is overlain conformably by Ninmaroo Formation.||12-JUL-16
3934|Chatsworth Limestone|69591|4|Described|p87, p92-93, p96-97|Cambrian|Cambrian|Burke River Structural Belt, Georgina Basin. 300m thick at the type section, just south of Lily Creek, 2km S of Chatsworth Station (Shergold, 1980); cumulative thickness up to 610m. A noticeable feature is limonite pseudomorphs (after pyrite?) but the hopper crystal habit suggests halite. Rich and diverse fauna (listed). Now includes rocks assigned to the Gola beds in the Momedah Anticline.||||Overlies Pomegranate Limestone. Is overlain conformably by Ninmaroo Formation.|Grey, thin-bedded calcarenite and calcilutite, sandy and oolitic limestone, coarse biosparite and coquinite, marly interbeds and common intraformational breccias. Chert (silicified limestone) in thin layers and nodules; silicified fossils locally.|
3934|Chatsworth Limestone|72297|6|Mentioned|p747-748|||Georgina Basin. TOC values indicate this unit has one of the best source rock potentials in the Burke River Structural Belt. Lacks permeability, so would be a good cap rock.||||||
3934|Chatsworth Limestone|72321|6|Mentioned|Fig 2|Jiangshanian|Jiangshanian|Burke River Structural Belt, Georgina Basin.  Australian stage: Iverian.||Of Cockroach Group.||||
3934|Chatsworth Limestone|72358|6|Mentioned|p117|||||||||
3971|Chewings Range Quartzite|7837|6|Mentioned|p93-94|||Offe and Shae (1983). Southern Arunta Inlier.||||||
3971|Chewings Range Quartzite|9141|5|Briefly described|Map Legend|||Age: 2-1.5 B.Y.||||||
3971|Chewings Range Quartzite|9199|5|Briefly described|Map legend|Proterozoic|Proterozoic|Quartzite, muscovite-quartz schist, sericite-quartz phyllite.  Geological Province: Arunta Block.||||||03-NOV-04
3971|Chewings Range Quartzite|31991|5|Briefly described|p293|||Metamorphic events and migmatisation.||||||04-AUG-06
3971|Chewings Range Quartzite|37544|6|Mentioned|p477|||||||||
3971|Chewings Range Quartzite|38606|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
3971|Chewings Range Quartzite|38885|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
3971|Chewings Range Quartzite|39583|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
3971|Chewings Range Quartzite|39887|6|Mentioned|Fig.3|||||||||
3971|Chewings Range Quartzite|41816|4|Described|p12|||||||||
3971|Chewings Range Quartzite|41837|6|Mentioned|Map legend|Proterozoic||||||||
3971|Chewings Range Quartzite|41963|6|Mentioned|p158|||||||||
3971|Chewings Range Quartzite|42326|5|Briefly described|p11|||||||||
3971|Chewings Range Quartzite|42504|5|Briefly described|p65|||||||||
3971|Chewings Range Quartzite|43225|5|Briefly described|Map Legend||Paleoproterozoic|Of Iwupataka Metamorphic Complex.||||||07-NOV-08
3971|Chewings Range Quartzite|43503|4|Described|8,24|||Max. age: 1587+/-70Ma (Rb-Sr).||||||04-AUG-06
3971|Chewings Range Quartzite|43649|6|Mentioned|fig.1,p454-455|||||||||
3971|Chewings Range Quartzite|44114|5|Briefly described|p320-321|||Southern Arunta Inlier. Shallow-water marine sedimentary rocks.|1650-1610 Ma (Collins et al., 1995).||||Orthoquartzite.|
3971|Chewings Range Quartzite|48992|1|Redefined|p17|Mesoproterozoic|Mesoproterozoic|Prob.Middle Proterozoic||||||
3971|Chewings Range Quartzite|60547|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block. Quartzite, muscovite-quartz schist, sericite-quartz phyllite.||||||
3971|Chewings Range Quartzite|67565|5|Briefly described|p4, p7 Table 1, p12, p13, p36. |Paleoproterozoic|Paleoproterozoic|Correlated with upper part of Ikuntji Metamorphics.|Max. deposition 1669 +/- 13 Ma (Cross et al. 2004)|Unit in Iwupataka Metamorphic Complex.||||
3971|Chewings Range Quartzite|68832|5|Briefly described|p36-41, 35|||Warumpi Province, Arunta Region. SHRIMP U-Pb zircon geochronology. Maximum deposition age, but likely to be mixed with metamorphic zircon.|1669+/-13 Ma|Top of Iwupataka Metamorphic Complex.||Compared with Ikuntji Metamorphics.|Crystalline metasedimentary quartzite.|
3971|Chewings Range Quartzite|69428|4|Described|p6/07/2016 13:03|Paleoproterozoic|Paleoproterozoic|Stewart et al. (1980). Haasts Bluff Domain, Warumpi Province. Forms the prominent Chewings Range. Deposited between the Liebig Orogeny (1640-1630 Ma) and the Chewings Orogeny (1590-1570 Ma). Type locality in eastern HERMANNSBURG map area. SHRIMP U-Pb detrital zircon maximum depositional age.|1669 +/- 13 Ma (Cross et al., 2005).|Iwupataka Metamorphic Complex.|||Crystalline metamorphosed quartz sandstone, locally pebbly and interlayered with quartz-muscovite schist; kyanite occurs within the quartzite locally, and staurolite-bearing interbeds occur near Standley Chasm.|12-JUL-16
3971|Chewings Range Quartzite|69925|6|Mentioned|p21|||Southern Arunta Province, Arunta Inlier.||||Conformably overlies Rungutjirba Gneiss.||
3971|Chewings Range Quartzite|71592|5|Briefly described|Appendix A.|||Warumpi Province, Arunta Orogen.|1669+/-13 Ma (MDA: U-Pb zircon SHRIMP)||||Quartzite.|
3971|Chewings Range Quartzite|73086|6|Mentioned|p9|||Considered part of the Heavitree Formation[?]. Unconformably underlies the Heavitree Formation. [Also written as Chewings Quartzite]. Belongs to Iwupataka Metamorphic Complex[?]. Warumpi Province. Basement rock below the Amadeus Basin[?].||||Unconformably overlain by Heavitree Formation.||
3990|Chilling Sandstone|9324|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Finniss River Group. Siliceous quartz arenite, cross bedded.||||||07-NOV-08
3990|Chilling Sandstone|22809|4|Described|12|Proterozoic|Proterozoic|Of the Finniss River Group.||||||04-AUG-06
3990|Chilling Sandstone|22810|5|Briefly described|Table2 P4|||Conformable on Burrell Creek Formation||||||
3990|Chilling Sandstone|23714|5|Briefly described|p11|Proterozoic|Proterozoic|See also page 7 Table 1. Of Burrell Creek Formation.||||||
3990|Chilling Sandstone|23733|5|Briefly described|p32 Fig. 19|||||||||
3990|Chilling Sandstone|32170|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
3990|Chilling Sandstone|32307|4|Described|Table 1|||Lower Proterozoic||||||04-AUG-06
3990|Chilling Sandstone|32310|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
3990|Chilling Sandstone|32660|5|Briefly described|Table 2|||||||||
3990|Chilling Sandstone|32700|4|Described|Table 1|||L.Proterozoic. Refers Walpole et al. (1968) See p12.||||||04-AUG-06
3990|Chilling Sandstone|33376|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
3990|Chilling Sandstone|33377|6|Mentioned|Table 1|||Stratigraphy||||||
3990|Chilling Sandstone|35140|6|Mentioned|p322|||||||||
3990|Chilling Sandstone|36473|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
3990|Chilling Sandstone|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
3990|Chilling Sandstone|40493|5|Briefly described|Table 1|||||||||
3990|Chilling Sandstone|40808|5|Briefly described|Table 2|||||||||
3990|Chilling Sandstone|41645|4|Described|p12|||||||||
3990|Chilling Sandstone|41646|6|Mentioned|Map legend|Paleoproterozoic||Of the Finniss River Group. Quartzarenite, sometimes siliceous, micaceous, cross-bedded, ripple marked.||||||07-NOV-08
3990|Chilling Sandstone|41660|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Finniss River Group. Quartz arenite, sometimes siliceous, micaceous, ripple marked and cross-bedded.||||||07-NOV-08
3990|Chilling Sandstone|41661|4|Described|p14|||||||||
3990|Chilling Sandstone|41980|4|Described|p574|||||||||
3990|Chilling Sandstone|43187|5|Briefly described|p2|||||||||
3990|Chilling Sandstone|45022|3|Fully described|p.52||Paleoproterozoic|On many pages.  Fig.7,13, Tb.2, Pl.28.||||||07-NOV-08
3990|Chilling Sandstone|45112|5|Briefly described|Table 4|||||||||
3990|Chilling Sandstone|46163|14|Not recorded|p.168|||Unit of Finniss River Group.||||||
3990|Chilling Sandstone|46676|14|Not recorded|p.6||Paleoproterozoic|Table 1, opp. p.6 L. Proterozoic; group in Agicondian System.||||||07-NOV-08
3990|Chilling Sandstone|47047|6|Mentioned|p220|||||||||
3990|Chilling Sandstone|48942|3|Fully described|p17|||||||||
3990|Chilling Sandstone|63866|5|Briefly described|p105|Orosirian|Orosirian|Litchfield Province, Pine Creek Orogen. |1830 +/- 7 Ma (Worden et al., 2006b)|||||
3990|Chilling Sandstone|64677|5|Briefly described|v, p1, p14-17, p47-48|||Pine Creek Orogen. This is the age of a granite-granodiorite sill intruding the unit and giving a minimum depositional age (the text says maximum).|1830.0 +/- 6.8 Ma.||||Felsic volcanic rock.|
3990|Chilling Sandstone|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1850-1863Ma. Finniss River Group. Max thick 8000m. Quartz arenite, sometimes siliceous, micaceous cross-bedded and ripple-marked; Altered rhyodacite, rhyolite, banded tuff. Conform overlies Burrell Creek Formation, intruded by Ti Tree Granophyre.||||||07-JAN-09
3990|Chilling Sandstone|64730|5|Briefly described|p125 Fig. 3, p126|Paleoproterozoic|Paleoproterozoic|Maximum deposition age from dating of extrusion of underlying units: Warrs Volcanic Member (Burrell Creek Formation) 1862+/-3 Ma and Berinka Volcanics 1861+/-4 Ma.||Of Finniss River Group.||||02-MAY-12
3990|Chilling Sandstone|64956|4|Described|p2 Tb. 19, p81-82|Paleoproterozoic|Paleoproterozoic|Of the Finniss River Group. Conformable on Burrell Creek Formation. Max. depositional age: 1861+/-4Ma. Geological province: Pine Creek Orogen. Sample is a sandstone from a sequence of massive medium-grained quartz-arenite and quartzite.||||||07-FEB-11
3990|Chilling Sandstone|65339|6|Mentioned|p13.|||Litchfield Province, Pine Creek Orogen.||Unit in Finniss River Group.||||
3990|Chilling Sandstone|67167|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Unit in Finniss River Group.|||Quartz sandstone, sometimes siliceous, micaceous cross-bedded and ripple-marked.|
3990|Chilling Sandstone|67186|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Unit in Finniss River Group.||Overlies Burrell Creek Formation.|Quartz sandstone, sometimes siliceous, micaceous cross-bedded and ripple-marked.|23-NOV-11
3990|Chilling Sandstone|67232|5|Briefly described|p6, p35.|Paleoproterozoic|Paleoproterozoic||1861 +/- 4 Ma (Worden et al. 2008a).|||Is intruded by prominent sills of Benning Gabbro.||
3990|Chilling Sandstone|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Pine Creek area.|1862 +/- 2 Ma (maximum deposition age).|||||
3990|Chilling Sandstone|67779|5|Briefly described|p6 Fig.5.|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen.|<1861 +/- 4 Ma (Worden et al. 2008b).|Unit in Finniss River Group.||||
3990|Chilling Sandstone|69418|6|Mentioned|p3:21|||Pine Creek Orogen (Litchfield Domain). Hosts the Muldiva field Sn pegmatite deposit. ||||||12-JUL-16
3990|Chilling Sandstone|69420|4|Described|p5:4, 6-7|Paleoproterozoic|Paleoproterozoic|Crops out near the western margins of the Central Domain, Pine Creek Orogen. c.6500m thick. Shallow-marine to fluvial deposits. A conservative maximum depositional age from detrital zircons.|<1861 +/- 4 Ma (Worden et al., 2008).|Finniss River Group.||Overlies Burrell Creek Formation. Correlated with El Sherana Group and ?Tollis Formation.|Quartz sandstone; minor conglomerate, siltstone and tuff.|12-JUL-16
3990|Chilling Sandstone|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||Finniss River Group.||Overlies Burrell Creek Formation ?conformably.|White quartz sandstone, locally micaceous, ripple-marked and cross-bedded; minor conglomerate, siltstone and tuff.|
3990|Chilling Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
3990|Chilling Sandstone|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|1861+/-4 Ma (MDA: U-Pb zircon SHRIMP)||||Massive medium-grained quartz arenite.|
4123|Cleanskin beds|39422|5|Briefly described|Map legend|Tertiary|Tertiary|Light grey limestone.||||||10-JAN-05
4123|Cleanskin beds|39497|4|Described|p16|||||||||
4123|Cleanskin beds|62659|5|Briefly described|Map Legend|Cenozoic|Cenozoic|White porus unfossiliferous limestone and saprolitic limestone.||||||
4123|Cleanskin beds|65337|5|Briefly described|pp68-70.|Cenozoic|Cenozoic|May correlate with Brunette and Austral Downs Limestones, and even further-afield units like Golliger beds.|||||Loose scattered blocks of white, porous unfossiliferous limestone and saprolitic limestone along narrow blacksoil plains; pores and vughs commonly infilled by banded chalcedony.|
4123|Cleanskin beds|69458|5|Briefly described|p42:21-22|||Smith and Roberts (1963). Eastern NT. Widely mapped originally, but Rawlings et al. (2008) suggested it is more limited in extent. Loose scattered blocks along narrow vertosol ("blacksoil") plains. May be synonymous with very similar limestone in adjacent areas: the Brunette and Austral Downs Limestones.|||||White, porous, unfossiliferous limestone and saprolitic limestone. Pores and ?vugs are commonly infilled by banded chalcedony.|12-JUL-16
4151|Cliffdale Volcanics|22457|6|Mentioned|Fig29 P30|||||||||
4151|Cliffdale Volcanics|22479|5|Briefly described|fig4, pg10|Orosirian|Orosirian|||||||
4151|Cliffdale Volcanics|22644|5|Briefly described|5|||Geol province: Mount Isa Basin.||||||04-AUG-06
4151|Cliffdale Volcanics|22673|6|Mentioned|64|||Geol province: Mount Isa Basin.||||||04-AUG-06
4151|Cliffdale Volcanics|22747|6|Mentioned|Table1,p7|||Correlates with Ewan Granite||||||
4151|Cliffdale Volcanics|22853|5|Briefly described|33|||Geol province Murphy Inlier.||||||04-AUG-06
4151|Cliffdale Volcanics|23065|6|Mentioned|11, 15, 17|Proterozoic|Proterozoic|Geol province: Murphy Province.||||||04-AUG-06
4151|Cliffdale Volcanics|23066|5|Briefly described|p807, Fig.1|Proterozoic|Proterozoic|||||||
4151|Cliffdale Volcanics|23363|5|Briefly described|344 Fig.3|Orosirian|Orosirian|Age: ~1851Ma.||||||04-AUG-06
4151|Cliffdale Volcanics|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
4151|Cliffdale Volcanics|23395|5|Briefly described|p389|||||||||
4151|Cliffdale Volcanics|23398|4|Described|p433|Orosirian|Orosirian|||||||
4151|Cliffdale Volcanics|23405|6|Mentioned|p565|||||||||
4151|Cliffdale Volcanics|23406|5|Briefly described|p601 Fig.3|||||||||
4151|Cliffdale Volcanics|24197|5|Briefly described|p22, p94 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Of the Nicholson Suite. Includes the Billicumidji Rhyolite Member. Age: 1850Ma. Geological province: Murphy Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
4151|Cliffdale Volcanics|24419|5|Briefly described|p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Of the Nicholson Granite Complex. Geological Province: Murphy Province, Lawn Hill Subprovince (north).||||||07-NOV-08
4151|Cliffdale Volcanics|24442|5|Briefly described|p22 Fig. 1|||Geological Province: McArthur Basin.||||||
4151|Cliffdale Volcanics|26310|5|Briefly described|p7, Fig. 2, Table 1|Proterozoic|Proterozoic|Lavas, tuff, agglomerate.||||||
4151|Cliffdale Volcanics|30318|6|Mentioned|p328|||||||||
4151|Cliffdale Volcanics|30536|6|Mentioned|p102|||Correlation ? with Tewinga Group||||||
4151|Cliffdale Volcanics|30912|6|Mentioned|p136|||Proterozoic||||||
4151|Cliffdale Volcanics|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
4151|Cliffdale Volcanics|31348|6|Mentioned|p344|||||||||
4151|Cliffdale Volcanics|31421|6|Mentioned|p507|||||||||
4151|Cliffdale Volcanics|31824|6|Mentioned|p28|||||||||
4151|Cliffdale Volcanics|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
4151|Cliffdale Volcanics|32660|5|Briefly described|Table 2|||||||||
4151|Cliffdale Volcanics|35114|6|Mentioned|p200|||||||||
4151|Cliffdale Volcanics|35495|6|Mentioned|p344|||||||||
4151|Cliffdale Volcanics|35640|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
4151|Cliffdale Volcanics|35950|6|Mentioned|p304|||||||||
4151|Cliffdale Volcanics|36012|3|Fully described|Table 1|||See also p8.||||||04-AUG-06
4151|Cliffdale Volcanics|36439|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
4151|Cliffdale Volcanics|36442|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
4151|Cliffdale Volcanics|36473|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
4151|Cliffdale Volcanics|36873|5|Briefly described|p27|||||||||
4151|Cliffdale Volcanics|37217|6|Mentioned|p650|||||||||
4151|Cliffdale Volcanics|37371|6|Mentioned|p368|||||||||
4151|Cliffdale Volcanics|37372|6|Mentioned|p2|||||||||
4151|Cliffdale Volcanics|37565|6|Mentioned|p11|||See also Fig.5||||||
4151|Cliffdale Volcanics|37568|6|Mentioned|Fig.5|||||||||
4151|Cliffdale Volcanics|38042|6|Mentioned|p167|||||||||
4151|Cliffdale Volcanics|38557|6|Mentioned|p293|||||||||
4151|Cliffdale Volcanics|38584|4|Described|p8|||||||||
4151|Cliffdale Volcanics|38902|6|Mentioned|p28|||||||||
4151|Cliffdale Volcanics|39123|6|Mentioned|p157|||||||||
4151|Cliffdale Volcanics|39445|5|Briefly described|Table 2|||Base of Carpentarian. Age p39. See also p35 and p38.||||||04-AUG-06
4151|Cliffdale Volcanics|39559|6|Mentioned|Table 1|||||||||
4151|Cliffdale Volcanics|39685|6|Mentioned|Fig.1|||||||||
4151|Cliffdale Volcanics|39925|6|Mentioned|Fig.9|||||||||
4151|Cliffdale Volcanics|40489|6|Mentioned|p88|||||||||
4151|Cliffdale Volcanics|40491|6|Mentioned|p79|||||||||
4151|Cliffdale Volcanics|40675|6|Mentioned|p306|||||||||
4151|Cliffdale Volcanics|40840|6|Mentioned|Map legend|||||||||
4151|Cliffdale Volcanics|41125|6|Mentioned|p35|||See also fig.22.||||||
4151|Cliffdale Volcanics|41319|6|Mentioned|p195|||||||||
4151|Cliffdale Volcanics|41406|6|Mentioned|Map legend|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
4151|Cliffdale Volcanics|41465|6|Mentioned|p9|||||||||
4151|Cliffdale Volcanics|41594|6|Mentioned|p50|||||||||
4151|Cliffdale Volcanics|41721|4|Described|p6|||Contains Billicumidji Rhyolite Member. Thickness: 4000m+. Alkali rhyolite lava, rhyolitic and alkali rhyolitic ignimbrite. Geological province: Murphy Inlier.||||||01-AUG-07
4151|Cliffdale Volcanics|41722|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
4151|Cliffdale Volcanics|41757|5|Briefly described|p207|||||||||
4151|Cliffdale Volcanics|41961|6|Mentioned|Table 1 P39|||||||||
4151|Cliffdale Volcanics|42343|5|Briefly described|p28|||||||||
4151|Cliffdale Volcanics|42385|5|Briefly described|p3|||||||||
4151|Cliffdale Volcanics|42639|6|Mentioned|p6|||||||||
4151|Cliffdale Volcanics|42812|6|Mentioned|p60|||||||||
4151|Cliffdale Volcanics|43010|5|Briefly described|Fig.6||Paleoproterozoic|Of Early Proterozic age.||||||07-NOV-08
4151|Cliffdale Volcanics|43036|6|Mentioned|p26|||||||||
4151|Cliffdale Volcanics|43788|6|Mentioned|p13||Proterozoic|||||||
4151|Cliffdale Volcanics|43832|6|Mentioned|Table 17 p90||Paleoproterozoic|||||||07-NOV-08
4151|Cliffdale Volcanics|44271|14|Not recorded|p38|||||||||
4151|Cliffdale Volcanics|44272|14|Not recorded|Map Legend||Neoproterozoic|||||||
4151|Cliffdale Volcanics|44275|14|Not recorded|Map Legend|||||||||
4151|Cliffdale Volcanics|44280|14|Not recorded|Tb.1|||||||||
4151|Cliffdale Volcanics|44305|14|Not recorded|p.6,8,9,10,17||Paleoproterozoic|(E53-8). p18,19,20,opp.6,18. L.Prot.||||||07-NOV-08
4151|Cliffdale Volcanics|44306|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
4151|Cliffdale Volcanics|44482|14|Not recorded|p.6|||(E53-12).||||||
4151|Cliffdale Volcanics|44530|14|Not recorded|p.8|||Equiv.of Scrutton Volcanics. (D53-15).||||||
4151|Cliffdale Volcanics|44751|14|Not recorded|p302|||||||||
4151|Cliffdale Volcanics|44989|14|Not recorded|p.113|||Tb.II.||||||
4151|Cliffdale Volcanics|45086|5|Briefly described|p29|||Lithology and mineralization.||||||04-AUG-06
4151|Cliffdale Volcanics|45140|6|Mentioned|p12-13|||McArthur Basin region.|1770 +/- 20 Ma.|||||
4151|Cliffdale Volcanics|45162|6|Mentioned|p11|||||||||
4151|Cliffdale Volcanics|45166|4|Described|p13|||||||||
4151|Cliffdale Volcanics|45167|5|Briefly described|Fig.27|||||||||
4151|Cliffdale Volcanics|45287|14|Not recorded|p.226-7,229||Paleoproterozoic|Intruded by Nicholson Granite.  Mineralised U, Pb? Cu. Acid lavas. L. Proterozoic||||||07-NOV-08
4151|Cliffdale Volcanics|46804|6|Mentioned|p153|||Stratigraphy||||||
4151|Cliffdale Volcanics|46864|4|Described|p39|||||||||
4151|Cliffdale Volcanics|48901|14|Not recorded|Not recorded||Carpentarian|||||||
4151|Cliffdale Volcanics|49001|5|Briefly described|p1|||||||||
4151|Cliffdale Volcanics|49002|6|Mentioned|p1|||||||||
4151|Cliffdale Volcanics|50536|5|Briefly described|p1.4, 3.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Nicholson Suite. Age: ~1850Ma (SHRIMP), 1732 +/- 20Ma (Rb-Sr). Thckness: 4000m.||||||26-MAR-18
4151|Cliffdale Volcanics|60558|5|Briefly described|p9 Fig. 7|||Age: 1850Ma (SHRIMP). Geological Province: Murphy Basin.||||||03-JUN-09
4151|Cliffdale Volcanics|61936|5|Briefly described|p194 Fig. 6|||Geological Province: Lawn Hill Platform, Western Fold Belt, Mount Isa Inlier. ||||||
4151|Cliffdale Volcanics|63109|6|Mentioned|p1109|||Age: ~1850Ma. Repersentation of the 'Barramundi' basement. Geological Province: Murphy Inlier.||||||30-SEP-08
4151|Cliffdale Volcanics|63112|5|Briefly described|p1190|||Part of basement to southern McArthur Basin.|c. 1850 Ma.|||||
4151|Cliffdale Volcanics|63116|6|Mentioned|p1299 Tb.1,|||Material properties detailed.||||||
4151|Cliffdale Volcanics|64250|6|Mentioned|p23|||Discussed as possible sediment source for Quilalar Formation.|1851 +/- 3 Ma|||||20-MAR-18
4151|Cliffdale Volcanics|65228|5|Briefly described|p20.|||SE McArthur Basin. 4,000 m+ thick. Felsic; geochemically similar to Scrutton Volcanics. May correlate with Leichhardt Volcanics.||||Unconformably overlies Murphy Metamorphic complex.||
4151|Cliffdale Volcanics|65232|5|Briefly described|p9, p8 Fig. 7, p66-68|||Unconform. over Murphy Metamorphics; unconform. under Westmoreland Conglomerate. Contact with Nicholson Granite. Felsic to intermediate ignimbrite and rhyolite. Age: 1851 Ma. Uranium mineralisation. Geol Prov: Murphy Inlier.||||||09-FEB-10
4151|Cliffdale Volcanics|65337|5|Briefly described|p5, p6 Fig.3, p8.||Paleoproterozoic|Murphy Inlier. Felsic volcanics, comagmatic with Nicholson Granite. Probably correlates with Connelly Volcanics.|c.1860-1845 Ma.|||||
4151|Cliffdale Volcanics|65340|6|Mentioned|p7, p83.|||Felsic. Emplaced with comagmatic Nicholson Granite into Murphy Metamorphics to form the regional basement, which is not exposed in this map area.|c.1860 - 1845 Ma.|||||
4151|Cliffdale Volcanics|65396|6|Mentioned|p196|Orosirian|Orosirian|Murphy Inlier.|1851 +/- 3 Ma |||||
4151|Cliffdale Volcanics|66529|5|Briefly described|p20-21  |Paleoproterozoic|Paleoproterozoic|Age of upper units.|~1840 Ma (M. Ahmad, NTGS, pers.comm.)|||Unconformably overlies the Murphy Metamorphics.|Alkali rhyolite lava and rhyolitic and alkali rhyolitic ignimbrite.|
4151|Cliffdale Volcanics|67323|4|Described|GIS attrib tbl, p9, p29, p39, p107|||See also Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Camooweal-Murphy Domain, Mount Isa Inlier. Informally divided into 12 subunits.|~1845 Ma.|Tawallah Group.||Is intruded by Nicholson Granite Complex. Correlated with the Leichhardt Volcanics.|Rhyolitic to dacitic ignimbrite, rhyolitic lava, tuff, vent breccia; grey porphyritic andesite; pink medium, even granofels.|
4151|Cliffdale Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province.||||||
4151|Cliffdale Volcanics|69417|5|Briefly described|p2:5, 9|Orosirian|Orosirian|Murphy Orogen.|c.1851 Ma.|||Unconformably overlies the Murphy Metamorphics.||12-JUL-16
4151|Cliffdale Volcanics|69418|5|Briefly described|p3:17, 19|||Murphy Province. Hosts the Eva Mine unconformity-related U deposit (described).||||Is overlain unconformably by Westmoreland Conglomerate.||12-JUL-16
4151|Cliffdale Volcanics|69423|4|Described|p8:1-4|Orosirian|Orosirian|Murphy Inlier, Murphy Province. Coeval and comagmatic with Connellys Volcanics and Nicholson Granite Complex. Over 4km thick. Complicated, apparently mutually intrusive relationship with Nicholson Granite Complex. SHRIMP U-Pb zircon age. Hosts copper occurrences including the Norris Copper Mine, and a number of uranium occurrences including the Eva (Pandanus Creek) Mine which also contains gold.|1851 +/- 3 Ma (Page et al., 2000).|||Unconformably overlies Murphy Metamorphics. Is overlain unconformably by Westmoreland Conglomerate.|Rhyolite, alkali rhyolite and dacitic lavas, ignimbrites and intrusions; minor andesite and sedimentary intervals.|12-JUL-16
4151|Cliffdale Volcanics|69429|5|Briefly described|p14:3|Paleoproterozoic|Paleoproterozoic|Murphy Province.|c.1850 Ma.|||Age-equivalent to Scrutton Volcanics (Scrutton Inlier).||12-JUL-16
4151|Cliffdale Volcanics|69430|5|Briefly described|p15:10, 49-50|||Underlies southern McArthur Basin succession. Hosts small U-Au deposits (eg Eva, described in some detail).||||Is overlain unconformably by Westmoreland Conglomerate (Tawallah Group).|Includes rhyolitic and alkali rhyolitic ignimbrite, and alkali rhyolite lava.|12-JUL-16
4151|Cliffdale Volcanics|69433|5|Briefly described|p18:2-3|||A probable source of 1847 +/- 13 Ma sediment (zircons) for Wire Creek Sandstone, and conglomerate clasts in the Fish River Formation.||||Is overlain unconformably by Wire Creek Sandstone.||12-JUL-16
4151|Cliffdale Volcanics|69434|5|Briefly described|p19:1, 4|||Murphy Inlier. A source of siliciclastic sediments for the Caulfield beds, South Nicholson Basin.|c.1850 Ma (Page et al., 2000).|||||12-JUL-16
4151|Cliffdale Volcanics|69591|5|Briefly described|p29-31, p58|Paleoproterozoic|Paleoproterozoic|Camooweal-Murphy Domain. Co-magmatic with Nicholson Granite. Dated at 1851 +/- 3 Ma by Page, Jackson and Krassay (2000).|c.1865 - c.1845 Ma.|||Is intruded by Nicholson Granite Complex.|Rhyolitic to dacitic ignimbrite, rhyolitic lava, tuff.|
4151|Cliffdale Volcanics|69673|6|Mentioned|p3 fig 2|Orosirian|Orosirian|||||||
4151|Cliffdale Volcanics|69917|5|Briefly described|p199, 201|Orosirian|Orosirian|Co-magmatic with Nicholson Granite.||||Unconformably underlies Westmoreland Conglomerate.||
4151|Cliffdale Volcanics|70284|6|Mentioned|p1244, 1245|Orosirian|Orosirian||~1850 Ma|||||
4151|Cliffdale Volcanics|70849|5|Briefly described|Map legend.|Orosirian|Orosirian|Murphy Province.|||Billicumidji Rhyolite Member.|Is overlain unconformably by Westmoreland Conglomerate (Tawallah Group). Is intruded by Nicholson Granite Complex.|Rhyolitic and alkali rhyolitic ignimbrite; rhyolitic lava, ashfall tuff.|
4151|Cliffdale Volcanics|71369|6|Mentioned|p47|||Basement rocks of the South Nicholson Basin.||||||
4151|Cliffdale Volcanics|71592|5|Briefly described|Appendix A.|||Murphy Region.|1851+/-3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Rhyolite.|
4151|Cliffdale Volcanics|71606|5|Briefly described|p137|Orosirian|Orosirian|Murphy Tectonic Ridge.||||Correlable to Nicholson Granite. Underlain by Murphy Metamorphics.||
4151|Cliffdale Volcanics|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Part of the early Basin volcanism and plutonism in the McArthur Basin.|||||Rhyolitic to dacitic volcanics, tuff.|
4151|Cliffdale Volcanics|71799|5|Briefly described|p150 fig 2||||||||Silicic volcanics, porphyry.|
4151|Cliffdale Volcanics|72526|5|Briefly described|p6 Fig.1.2, p8 Fig.1.3.|Paleoproterozoic|Paleoproterozoic|Shown as located in the Southeastern McArthur Basin. U-Pb zircon igneous crystallisation age.|1851 +/-3 Ma|Tawallah Group||Shown as overlying Murphy Metamorphics and partially underlying Nicholson Granite Complex.||
4151|Cliffdale Volcanics|72527|5|Briefly described|p5, p161, p184-185,|Orosirian|Orosirian|Murphy Province. The siliclastic detritus generated by this unit is thought to contribute to the Caulfield beds. Ref Ahmad et al. (2013).|1851 +/-3 Ma|||Unconformably overlies Murphy Metamorphics.||
4151|Cliffdale Volcanics|72912|5|Briefly described|p5 Fig.3, p19.|Orosirian|Orosirian|Located in the Southeastern McArthur Basin. U-Pb zircon igneous crystallisation age (Ma) shown.|1851+/-3 Ma|||Shown as overlying Murphy Metamorphics and underlies Nicholson Granite Complex and partially equivalent to Scrutton Volcanics.||15-MAR-21
4151|Cliffdale Volcanics|72919|4|Described|p1, p4-6, p11-14, p93|Orosirian|Orosirian|Murphy Province, North Australian Craton. Over 4000 m thick. Five members have been mapped, although only the uppermost member has been named (the Billicumidji Rhyolite Member). New U-Pb SHRIMP zircon magmatic crystallisation age of 1857 +/- 7 Ma. Broadly coeval with Connellys Volcanics, Nicholson Granite Complex, and Scrutton Volcanics.|1857 +/- 7 Ma U-Pb SHRIMP||Billicumidji Rhyolite|Unconformably underlain by Murphy Metamorphics.|Rhyolite (locally flow-banded) and dacitic lavas, tuffs and 'calc-alkaline ignimbrites'.|
4151|Cliffdale Volcanics|73042|6|Mentioned|p4|Orosirian|Orosirian|Southern McArthur Basin and South Nicholson Basin region. Geochronology is a U-Pb zircon igneous crystallisation age.|1851 +/- 3 Ma (see Fig.1.2)|||||
4151|Cliffdale Volcanics|73427|5|Briefly described|p1, p5, p12-13, App.A|Orosirian|Orosirian|North Australian Craton, Murphy Inlier/Murphy Province. Flat-lying. Co-magmatic with Nicholson Granite.|1855-1845 Ma||||Predominantly felsic lava and ignimbrite.|
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.|
4338|Colless Volcanics|14019|6|Mentioned|p19|||Geochemically identical with Antrim Plateau Volcanics, Helen Springs Volcanics and Peaker Piker Volcanics in N.T.||||||
4338|Colless Volcanics|23328|5|Briefly described|1030|||||||||07-SEP-09
4338|Colless Volcanics|23393|5|Briefly described|p22|Early Cambrian|Early Cambrian|||||||
4338|Colless Volcanics|24303|6|Mentioned|p62 Appendix|||Geological Province: Georgina Basin. Possible correlative of Helen Springs Volcanics.||||||
4338|Colless Volcanics|26310|5|Briefly described|p4 Table 1|Cambrian|Proterozoic|Basalt. Maximum Thickness: 200 feet?||||||
4338|Colless Volcanics|30242|6|Mentioned|p10|||||||||
4338|Colless Volcanics|30914|6|Mentioned|Map legend|Early Cambrian|Proterozoic|Proterozoic - Early Cambrian||||||
4338|Colless Volcanics|31396|6|Mentioned|Fig.3|||||||||
4338|Colless Volcanics|32659|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
4338|Colless Volcanics|33482|6|Mentioned|p9|||||||||
4338|Colless Volcanics|34162|6|Mentioned|p117|||Early Cambrian.||||||
4338|Colless Volcanics|35054|6|Mentioned|p245|||||||||
4338|Colless Volcanics|36003|6|Mentioned|Fig.8|||||||||
4338|Colless Volcanics|36644|6|Mentioned|p213|||||||||
4338|Colless Volcanics|37572|5|Briefly described|p155|||See also p151.||||||07-AUG-06
4338|Colless Volcanics|38444|6|Mentioned|p139|||||||||
4338|Colless Volcanics|38446|6|Mentioned|p143|||||||||
4338|Colless Volcanics|39445|5|Briefly described|Table 4|||See also p62.||||||07-AUG-06
4338|Colless Volcanics|39797|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
4338|Colless Volcanics|40852|6|Mentioned|p36|||||||||
4338|Colless Volcanics|40856|5|Briefly described|p315|||||||||
4338|Colless Volcanics|41240|6|Mentioned|p112|||||||||
4338|Colless Volcanics|44271|2|Defined|p38,40,42,57||Neoproterozoic|Appears to underlie Camooweal Dolomite.||||||
4338|Colless Volcanics|44274|2|Defined|Tb.2,p9,10,16,map|||Unconformably overlies Mullera Formation and Constance Sandstone. Unconformably overlain by Thorntonia Limestone.||||||24-MAR-16
4338|Colless Volcanics|44275|14|Not recorded|Map Legend|||||||||
4338|Colless Volcanics|44281|14|Not recorded|Map Legend|||Early Cambrian or Neoproterozoic.||||||
4338|Colless Volcanics|44290|2|Defined|p439|||Neoproterozoic or Early Cambrian.||||||
4338|Colless Volcanics|44482|14|Not recorded|p.11,15-16|||(E53-12). U.Prot. or L.Cam.||||||
4338|Colless Volcanics|44806|14|Not recorded|p298|||Petrographic descriptions.||||||
4338|Colless Volcanics|44920|14|Not recorded|Map Legend, Sheet 2||Adelaidean|||||||
4338|Colless Volcanics|44922|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Vesicular basalt; sandstone lenses.||||||01-JUL-04
4338|Colless Volcanics|44989|2|Defined|p.124|||Overlies Mullera Formation; underlies Camooweal Dolomite. (E54-9).||||||
4338|Colless Volcanics|45052|4|Described|p72|||Adelaidean or Cambrian.||||||12-NOV-08
4338|Colless Volcanics|45079|6|Mentioned|p8|||Petrography. Lower Cambrian age||||||
4338|Colless Volcanics|45287|14|Not recorded|p.223||Cambrian|||||||
4338|Colless Volcanics|60122|5|Briefly described|p15|Early Cambrian|Early Cambrian|Conformably overlain by Thorntonia Limestone.||||||
4338|Colless Volcanics|62557|5|Briefly described|p461, 462|Cambrian|Cambrian|Of the Kalkarindji continental flood basalt province.||||||24-NOV-09
4338|Colless Volcanics|64068|5|Briefly described|p81, p58, 225|Early Cambrian|Early Cambrian|Kalkarindji Flood Basalt Province, central and northwest Georgina Basin.|c.513-c.504 Ma.|||[Said to be] conformably and gradationally overlain by Thorntonia Limestone[but neither of the references given support this statement].||24-MAR-16
4338|Colless Volcanics|64589|5|Briefly described|chemistry file|||Geochemical analyses.||||||12-NOV-08
4338|Colless Volcanics|65337|6|Mentioned|p94.|||Probable minimum thickness of 60 m.||Unit in Kalkarindji Volcanic Group.||||
4338|Colless Volcanics|66526|5|Briefly described|p27.|Early Cambrian|Early Cambrian|Kalkarindji Large Igneous Province.|c.510 Ma.|||||
4338|Colless Volcanics|67323|5|Briefly described|p83, p107; GIS attrib tbl|Early Cambrian|Neoproterozoic|See also Solid Geology Map. Undilla Sub-basin, Centralian Superbasin.||||Is overlain unconformably by Thorntonia Limestone.|Amygdaloidal basalt, trachyte, arenite|
4338|Colless Volcanics|67352|6|Mentioned|p31 |||Part of the Kalkarindji Continental Flood Basalt Province, covering a vast area of NT-QLD-WA with an average thickness of .5 km.||||||
4338|Colless Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Early Paleozoic|Neoproterozoic|Georgina Basin. ||||||
4338|Colless Volcanics|69443|6|Mentioned|p28:16|||Kalkarindji Province.||||Is overlain conformably and gradationally by Thorntonia Limestone (Narpa Group).||12-JUL-16
4338|Colless Volcanics|69445|3|Fully described|p30:1, 5, 16-17|Early Cambrian|Early Cambrian|Carter (1959), Carter and Opik (1961). Widespread small exposures of sub-aerial basaltic lavas on the margins of eastern Georgina Basin. Probable minimum thickness of 60m. Type section at about GDA94 54K 216029mE 7935918mN in western LAWN HILL map area.||Kalkarindji Suite.||Unconformably overlies Mullera Formation (South Nicholson Group). Is overlain by Thorntonia Limestone (unconformably) and Camooweal Dolostone.|Amygdaloidal basalt and other tholeiitic lavas.|12-JUL-16
4338|Colless Volcanics|69591|5|Briefly described|p29, p54, p87|Cambrian|Neoproterozoic|Camooweal-Murphy Domain. Georgina Basin.||Kalkarindji Volcanic Group.|||Amygdaloidal basalt, trachyte, arenite.|
4338|Colless Volcanics|71369|5|Briefly described|p45|Cambrian|Cambrian|Forms part of the southern margin of the South Nicholson Basin.|Middle Cambrian|Middle Cambrian||Correlative of Antrim Plateau Volcanics.||20-FEB-18
4338|Colless Volcanics|72408|4|Described|map sheet|Early Cambrian|Neoproterozoic|Of Geogina Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet.||Unit of Kalkarindji Volcanic Group.|||Amydaloidal basalt, trachyte, arenite.|
4338|Colless Volcanics|72414|4|Described|map sheet|Early Cambrian|Neoproterozoic|Of Geogina Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.||Unit of Kalkarindji Volcanic Group.|||Amydaloidal basalt, trachyte, arenite.|
4338|Colless Volcanics|72415|4|Described|mapsheet|Early Cambrian|Neoproterozoic|Of Geogina Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.||Unit of Kalkarindji Volcanic Group.|||Amydaloidal basalt, trachyte, arenite.|
4338|Colless Volcanics|72416|4|Described|map sheet|Early Cambrian|Neoproterozoic|Of Geogina Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet Geological Compilation Series.||Unit of Kalkarindji Volcanic Group.|||Amydaloidal basalt, trachyte, arenite.|
4338|Colless Volcanics|72526|5|Briefly described|p6 Fig.1.2.|Cambrian|Cambrian|Shown with Helen Springs Volcanics.||||||
4338|Colless Volcanics|72889|6|Mentioned|p6 Fig.i.|||||||||
4338|Colless Volcanics|73083|6|Mentioned|p3, p69|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.|
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.|
4462|Conway Formation|22538|6|Mentioned|Fig3 P708|||||||||
4462|Conway Formation|22600|4|Described|Map legend|Statherian|Statherian|||||||
4462|Conway Formation|24048|3|Fully described|p57|Mesoproterozoic|Paleoproterozoic|Of the Balma Group.  Overlain by Zamia Creek Siltstone; underlain by Vaughton Siltstone.  Max. thickness: 100m.  Geological Province: McArthur Basin.||||||07-NOV-08
4462|Conway Formation|24049|5|Briefly described|Map Legend|Statherian|Statherian|Of Balma Group. Upper: chert bands (silicified carbonate), massive to weakly stromotolitic. Lower: cherty to dolomitic siltstone, laminated; sandstone, dolomitic; interbedded mudstone. Geol. Prov: McArthur Basin.||||||13-OCT-05
4462|Conway Formation|32660|5|Briefly described|Table 4|||||||||
4462|Conway Formation|42597|5|Briefly described|Map Legend|Carpentarian||||||||
4462|Conway Formation|43010|2|Defined|p115||Paleoproterozoic|Of McArthur Group. Of Statherian age.||||||07-NOV-08
4462|Conway Formation|44112|6|Mentioned|p30,58|||||||||
4462|Conway Formation|44299|4|Described|p.12|||SD/53-7,8. Lower (?) Proterozoic. Table 1.||||||
4462|Conway Formation|44300|14|Not recorded|map legend|||SD/53-7,8. Lower (?) Proterozoic.||||||
4462|Conway Formation|45162|6|Mentioned|p45|||||||||
4462|Conway Formation|61403|5|Briefly described|Map Legend|Statherian|Statherian|Of Balma Group. Upper: chert bands (silicified carbonate), massive to weakly stromotolitic. Lower: cherty to dolomitic siltstone, laminated; sandstone , dolomitic; interbedded mudstone. Geol. Prov: McArthur Basin.||||||
4462|Conway Formation|64817|6|Mentioned|p353 Fig.4 |||||Of the Balma Group.||||
4462|Conway Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot; p35|Paleoproterozoic|Paleoproterozoic|McArthur Basin. Appears as Conway Siltstone on p35.|1645-1620 Ma.||||Siltstone.|
4462|Conway Formation|69430|4|Described|p15:3, 21-22|Statherian|Statherian|Walker Fault Zone, northern McArthur Basin. Resistant, ridge-forming unit. c.50-100m thick. Upward-shallowing, from subtidal to intertidal, deposits. Correlates with Hot Spring Member (Lynott Formation): many lithological similarities.||Balma Group.||Conformably and gradationally overlies Vaughton Siltstone.  Is overlain probably conformably by Zamia Creek Siltstone, locally unconformably by Ngilipitji Conglomerate Member (Yarrawirrie Formation).|Black to grey when fresh, laminated, thinly to medium bedded cherty to dolomitic siltstone, fine-grained dolomitic sandstone, interbedded khaki mudstone; overlain by grey to white chert bands (silicified carbonate), massive to weakly stromatolitic.|12-JUL-16
4462|Conway Formation|69673|6|Mentioned|p16 fig 13|Mesoproterozoic|Paleoproterozoic|Walker Fault Zone||Balma Group||Overlain by Zamia Creek Siltstone, overlies Vaughton Siltstone||
4462|Conway Formation|71374|5|Briefly described|p12|Statherian|Statherian|May correlate with the Yarawoi Formation (Habgood Group). ||Balma Group||||
4543|Coolibah Formation|8187|5|Briefly described|Map legend|Ordovician|Ordovician|Limestone (micrite, grainstone, cryptalgal boundstone), marl, chert.||||||
4543|Coolibah Formation|10116|5|Briefly described|Map Legend|Early Ordovician|Early Ordovician|Wackestones, grainstones, micrite, conglomerate.||||||
4543|Coolibah Formation|12891|5|Briefly described|p733 Fig. 2|Middle Ordovician|Early Ordovician|Geological province: SW Georgina Basin.||||||07-FEB-11
4543|Coolibah Formation|12951|6|Mentioned|p143 fig 4, p145 fig 6|Middle Ordovician|Early Ordovician|Georgina Basin.||||||
4543|Coolibah Formation|13995|5|Briefly described|p67, p75, p77, p79, p89, p99, p101|Middle Ordovician|Early Ordovician|Georgina Basin. Bendigonian-Castlemanian. Rostroconch species listed. Gastropod species and biogeographic links. Nautiloid fauna (includes the first actinoceratid in Australia) have contemporaries in Horn Valley Siltstone and Stairway Sandstone (Amadeus Basin). Conodonts in this unit have links to those in N China and elsewhere in Asia and the Americas.||||||
4543|Coolibah Formation|22646|6|Mentioned|Fig 5 on p 105|Early Ordovician|Early Ordovician|Georgina Basin.||||||
4543|Coolibah Formation|22954|6|Mentioned|Fig3p9|Early Ordovician|Early Ordovician|||||||
4543|Coolibah Formation|24065|4|Described|p235|Middle Ordovician|Early Ordovician|Of Toko Group. Geological Province: Georgina Basin. Maximum thickness: 110m.||||||
4543|Coolibah Formation|24442|5|Briefly described|p49|Cambrian|Early Cambrian|Overlies the Kelly Creek Formation.  On TOBERMORY sheet.||||||
4543|Coolibah Formation|30983|4|Described|p70|||Arenigian||||||
4543|Coolibah Formation|33111|4|Described|p34|||Mention Fig.9||||||
4543|Coolibah Formation|33657|6|Mentioned|p1|||||||||
4543|Coolibah Formation|33738|6|Mentioned|p54|||||||||
4543|Coolibah Formation|34252|6|Mentioned|Po.2|||Fossils||||||
4543|Coolibah Formation|34454|5|Briefly described|Table 2|||M.Ordovician||||||
4543|Coolibah Formation|34847|6|Mentioned|Table 1|||Stratigraphy and hydrocarbon prospects.||||||07-AUG-06
4543|Coolibah Formation|35121|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
4543|Coolibah Formation|35139|4|Described|Table.2|||||||||
4543|Coolibah Formation|35146|6|Mentioned|p468|||||||||
4543|Coolibah Formation|36234|3|Fully described|p172|||See also Fig.1.||||||
4543|Coolibah Formation|36243|6|Mentioned|Table 1A|||||||||
4543|Coolibah Formation|36580|6|Mentioned|p469|||See also Fig.1||||||
4543|Coolibah Formation|37572|4|Described|p163|||See also Fig.8||||||
4543|Coolibah Formation|39445|5|Briefly described|Table 4|||See also p61 and Fig.5.||||||07-AUG-06
4543|Coolibah Formation|39921|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
4543|Coolibah Formation|39943|6|Mentioned|Table 2B|||||||||
4543|Coolibah Formation|40136|5|Briefly described|p22|||||||||
4543|Coolibah Formation|41524|6|Mentioned|Fig.3|||||||||
4543|Coolibah Formation|42059|5|Briefly described|Fig.2 P131|||See also p134.||||||07-AUG-06
4543|Coolibah Formation|42060|6|Mentioned|Fig.5 P140|||||||||
4543|Coolibah Formation|43105|5|Briefly described|Fig.4,p9.|||||||||
4543|Coolibah Formation|43803|6|Mentioned|Fig.5,p71|||||||||
4543|Coolibah Formation|43808|5|Briefly described|p293||Early Ordovician|||||||
4543|Coolibah Formation|44308|14|Not recorded|p10,Tb.1||Early Ordovician|||||||
4543|Coolibah Formation|44309|2|Defined|Tb.1,p12,17|||Fauna closely related to Kelly Creek Formation.||||||
4543|Coolibah Formation|44312|14|Not recorded|Map Legend||Early Ordovician|||||||
4543|Coolibah Formation|44326|14|Not recorded|Map Legend||Early Ordovician|||||||
4543|Coolibah Formation|44358|6|Mentioned|p10,19|||||||||
4543|Coolibah Formation|44469|2|Defined|p.10,19,opp.p.6,Tb.I|||(F53-12). Unit of Toko Group. Overlies Kelly Creek Formation.; overlain by Nora Formation.||||||11-FEB-09
4543|Coolibah Formation|44470|5|Briefly described|map legend||Early Ordovician|Lower Ordovician.||||||02-DEC-04
4543|Coolibah Formation|44852|14|Not recorded|p71||Ordovician|Middle Ordovician||||||
4543|Coolibah Formation|44920|14|Not recorded|Map Legend, Sheet 4||Early Ordovician|Unit of Toko Group.||||||
4543|Coolibah Formation|45022|14|Not recorded|p.86|||Tb.12||||||
4543|Coolibah Formation|45052|2|Defined|p127|Early Ordovician|Early Ordovician|||||||
4543|Coolibah Formation|45115|6|Mentioned|p6|||||||||
4543|Coolibah Formation|45118|6|Mentioned|p3|||||||||
4543|Coolibah Formation|45148|6|Mentioned|Fig.4|||Georgina Basin||||||
4543|Coolibah Formation|45155|6|Mentioned|Fig.8|||||||||
4543|Coolibah Formation|46841|6|Mentioned|p97|||||||||
4543|Coolibah Formation|46897|6|Mentioned|Fig.3|||||||||
4543|Coolibah Formation|46959|6|Mentioned|Table 1|||||||||
4543|Coolibah Formation|47024|6|Mentioned|p1|||||||||
4543|Coolibah Formation|47052|6|Mentioned|p262|||||||||
4543|Coolibah Formation|48901|14|Not recorded|Not recorded||Ordovician|M.Ordovician, Toko Gp.||||||
4543|Coolibah Formation|48938|6|Mentioned|p20|||Nomenclature table.||||||
4543|Coolibah Formation|48942|6|Mentioned|p59|||Refers Laing and Allen (1956).||||||07-AUG-06
4543|Coolibah Formation|48943|6|Mentioned|p62|||Refers Laing and Allen (1956).||||||07-AUG-06
4543|Coolibah Formation|49027|4|Described|p17|||||||||
4543|Coolibah Formation|60122|3|Fully described|p29-30, p10 Tb. 1|Early Ordovician|Early Ordovician|Of the Toko Group. Grey and white limestone, quartzic limestone, dolostone marl, siltstone, basal conglomerate; local chert lenses. Conformably overlies Kelly Cr Fm; conformably underlies Nora Fm. Max. thick: 110m. Geol.Prov: Georgina Basin. See also p4-5||||||
4543|Coolibah Formation|60590|5|Briefly described|Map legend|Early Ordovician|Early Ordovician|Of the Toko Group.  Limestone, quartzic limestone, dolostone, marl, siltstone; basal limestone.  Overlies the Kelly Creek Formation; overlain by Nora Formation.||||||
4543|Coolibah Formation|61404|5|Briefly described|Map legend|Early Ordovician|Early Ordovician|Of the Toko Group. Limestone, quartzic limestone, dolostone, marl, siltstone; basal sandstone. Geological Province: southern Georgina Basin.||||||12-OCT-05
4543|Coolibah Formation|62794|5|Briefly described|p298|Early Ordovician|Early Ordovician|Georgina Basin. Underlies Nora Formation. Stait & Druce (1993) correlated uppermost Coolibah Formation with lower Horn Valley Siltstone in the  Amadeus Basin, on the basis of conodont faunas.||||||05-DEC-12
4543|Coolibah Formation|63450|4|Described|p78 Fig. 5, p82|Arenig|Arenig|Conformably overlies Kelly Creek Formation; overlain by Nora Formation.Max. thickness: 110m. Geological province: Georgina Basin, West Toko Syncline. Comprises limestones, quartzic limestone, dolostone and marl.||||||07-FEB-11
4543|Coolibah Formation|64068|3|Fully described|p76, 75, p19|Middle Ordovician|Middle Ordovician|Variable thickness. Very diverse fauna. Correlations: Upper part of Kelly Creek Formation, Horn Valley Siltstone, possibly Djagamara Formation.||Of Toko Group.||Conformably to disconformably overlies Kelly Creek Formation. Is conformably overlain by Nora Formation.|Grey and white limestone, quartzic limestone, dolostone, marl, lenticular chert; basal sandstone, conglomerate or silicified microbial boundstone.|04-APR-12
4543|Coolibah Formation|64812|5|Briefly described|p237 Fig. 2|Middle Ordovician|Middle Ordovician|Geological Province: southern Georgina Basin.||||||07-FEB-11
4543|Coolibah Formation|64813|5|Briefly described|p256 Fig. 3|Middle Ordovician|Middle Ordovician|Geological Province: southern Georgina Basin.||||||11-FEB-09
4543|Coolibah Formation|65237|5|Briefly described|p4 Fig. 7|Ordovician|Ordovician|Geological province: southern Georgina Basin.||||||07-FEB-11
4543|Coolibah Formation|65489|5|Briefly described|p123, p125-126|Ordovician|Ordovician|Georgina Basin. Contains bitumen. Gas show from Ethabuka 1 in the Toko Syncline.||||Overlies Kelly Creek Formation.||
4543|Coolibah Formation|67323|5|Briefly described|GIS attrib tbl, p83, p88, p92 Fig.12.2|Early Ordovician|Early Ordovician|See also Solid Geology Map. Georgina Basin. A gas flow of c.6000 m3/day was recorded from this unit in AOD Ethabuka 1.||Toko Group.||Overlies Kelly Creek Formation. Is overlain by Nora Formation.|Limestone, calcilutite, dolomite, marl, chert|
4543|Coolibah Formation|67402|5|Briefly described|p25 tbl RRM3, p213 fig GRG3|Castlemanian|Chewtonian|Georgina Basin, West Toko Syncline. Maximum thickness of 110m. Potentially a conventional seal for carbon dioxide storage. Not likely to be a reservoir for carbon dioxide as it is believed to have inadequate injectivity. See also p213 fig GRG5, p215, p216, p217.||||Overlies the Kelly Creek Formation. Is laterally equivalent to or is conformably overlain by the Nora Formation.|Limestone, quartzitic limestone, dolostone and marl.|
4543|Coolibah Formation|68553|6|Mentioned|Map legend; schematic diagram.|Ordovician|Ordovician|Georgina Basin. This unit, as well as Kelly Creek Formation and the Toko Group, are all mapped under the symbol, Ot.||||||
4543|Coolibah Formation|69437|5|Briefly described|p22:10|Ordovician|Ordovician|Southern Georgina Basin.||||Overlies Kelly Creek Formation. Is overlain by Nora Formation.||12-JUL-16
4543|Coolibah Formation|69443|3|Fully described|p28:7, 27-28|Early Ordovician|Early Ordovician|Casey in Smith (1965). Southern Georgina Basin. Poorly exposed. Upper and lower contacts are diachronous. Up to 110m thick; only 7.5m in the type area in southeast TOBERMOREY map area. Contains a varied fossil fauna (listed) indicating a mid- to late-Floian age. Intertidal to shallow-subtidal marine deposits with fluctuating energy conditions.||Toko Group.||Conformably to disconformably overlies Kelly Creek Formation. Is overlain by Nora Formation conformably.|Limestone, quartzose limestone, dolostone, marl and local lenticular chert; basal interval of sandstone, conglomerate or silicified microbial boundstone.|12-JUL-16
4543|Coolibah Formation|69591|5|Briefly described|p87, p94-95|Early Ordovician|Early Ordovician|West Toko Syncline, Georgina Basin. This unit is here removed from the otherwise clastic-dominated Toko Group and assigned to the carbonate-dominated Cockroach Group. Variable thickness up to 160m. Age from acritarchs and conodonts.||Cockroach Group.||Disconformably/conformably overlies Kelly Creek Formation. Is overlain by Nora Formation.|Includes limestone, sandy limestone, calcilutite, dolomite and marl with some lenses of chert.|
4543|Coolibah Formation|69673|4|Described|p118, p119 fig 94, p136, p140|Ordovician|Ordovician|up to 110m thick (in Queensland). Reasonable reservoir potential.||Toko Group||Conformably overlies Kelly Creek Formation, overlain by Nora Formation|Limestone, dolostone, marl and local lenticular chert with a basal interval of sandstone, conglomerate or silicified microbia boundstone.|
4543|Coolibah Formation|70380|6|Mentioned|p745|Dapingian|Floian|Southern Georgina Basin.||||||
4543|Coolibah Formation|70968|6|Mentioned|p115, p117|||Laing and Allen (1956), who included rocks subsequently named the Wondoan and Stubbs Formations.||||||
4543|Coolibah Formation|72500|6|Mentioned|p386, p393-394, p396-397, p399|Middle Ordovician|Early Ordovician|Georgina Basin. Said to be Arenig age.||||||28-AUG-20
4543|Coolibah Formation|72503|6|Mentioned|p33|||Georgina Basin. Contains typical shallow-water [conodont] forms (e.g., Aurilobodus leptosomatus and Tangshanodus sp.).||||||
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.||||
4714|Cordillo Silcrete|22912|6|Mentioned|34|||||||||
4714|Cordillo Silcrete|23155|6|Mentioned|p36|||From the Innamincka Dome on the eastern Innamincka map sheet.  Data from STRZELECKI suggest that this material could well be mainly late Tertiary, not Oligocene-Miocene as suggested by Wopfner (1974).||||||
4714|Cordillo Silcrete|24204|6|Mentioned|p270|Eocene|Eocene|Geological Province: Poolowanna Trough.||||||
4714|Cordillo Silcrete|38605|6|Mentioned|p35|||||||||
4714|Cordillo Silcrete|39322|6|Mentioned|p396|||||||||
4714|Cordillo Silcrete|40910|6|Mentioned|p17|||||||||
4714|Cordillo Silcrete|40911|6|Mentioned|Map legend|Oligocene|Eocene|||||||03-JUL-06
4714|Cordillo Silcrete|40925|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
4714|Cordillo Silcrete|40926|3|Fully described|p25|||||||||
4714|Cordillo Silcrete|41098|5|Briefly described|p177|||||||||
4714|Cordillo Silcrete|42375|6|Mentioned|p21|||? Lake Eyre Basin. ? Oligocene.||||||
4714|Cordillo Silcrete|42469|5|Briefly described|p46|||used by Wopfner, 1978.||||||
4714|Cordillo Silcrete|42746|5|Briefly described|p19|||||||||
4714|Cordillo Silcrete|42905|5|Briefly described|p23, Fig 5.3|||||||||
4714|Cordillo Silcrete|44133|6|Mentioned|p202|||||||||
4714|Cordillo Silcrete|61836|5|Briefly described|p211||Eocene|||||||03-JUL-06
4714|Cordillo Silcrete|64778|6|Mentioned|p13|Tertiary|Tertiary|Pedirka and Simpson Desert Basins.||||||
4714|Cordillo Silcrete|65238|6|Mentioned|p6|Eocene|Eocene|||||||
4714|Cordillo Silcrete|65925|6|Mentioned|p139.|||||||||
4714|Cordillo Silcrete|66131|5|Briefly described|p242 Fig.2, p245, p249, p259|Oligocene|Eocene|Occurs in upper Cordillo Surface. Called Cordillo Silcrete Surface on p245. Developed over the Eyre Formation.||Of the Cordillo Surface.||Overlain by the Doonbarra Formation.||
4714|Cordillo Silcrete|66623|1|Redefined|p239, pp266-283.|Oligocene|Oligocene|Redefined and discussed in detail. Followed deep weathering of Eyre Formation and exists over much of inland Australia. Forms a resistant cap on escarpments, producing flat crests and mesas. More weakly silicified sandstones are mapped as Eyre Formation.||||Grades downwards into Eyre Formation. Locally overlain unconformably by Doonbara Formation. Forms capping over Winton Formation.|Variably siliceous, sheet-like bodies of silica-indurated sandstone and some conglomerate, now mainly comprising chalcedonic and locally opaline rocks; light grey to pale orange-brown.|05-JUN-13
4714|Cordillo Silcrete|67207|5|Briefly described|Map legend.|Neogene|Paleogene||||||Silcrete, variably silicified sandstone and conglomerate; columnar and massive variants.|19-SEP-11
4714|Cordillo Silcrete|67208|5|Briefly described|Map legend.|||Shown in Paleogene - Neogene age grouping.|||||Silcrete, variable silicified sandstone and conglomerate; columnar and massive variants.|20-SEP-13
4714|Cordillo Silcrete|67209|5|Briefly described|Map legend.|Paleogene|Paleogene|Two un-named sub-units with differing lithologies are mapped separately.||||Overlies Allaru Mudstone.|Silcrete, variably silicified sandstone and conglomerate; columnar and massive variants; local light grey highly siliceous silcrete; local pale brown/grey moderately siliceous silcrete with common relict sedimentary features (bedding and pebbles).|
4714|Cordillo Silcrete|67210|5|Briefly described|Map legend.|||Age given as Paleogene-Neogene.|||||Silcrete, variably silicified sandstone and conglomerate; columnar and massive variants.|
4714|Cordillo Silcrete|67211|5|Briefly described|Map legend.|||Age stated as Paleogene-Neogene.|||||Silcrete, variably silicified sandstone and conglomerate; columnar and massive variants; local light grey highly siliceous silcrete; local pale brown/grey moderately siliceous silcrete with common relict sedimentary features (bedding and pebbles).|
4714|Cordillo Silcrete|69019|6|Mentioned|p118.|Miocene|Oligocene|Developed widely across northern and central SA.||||||
4714|Cordillo Silcrete|69023|6|Mentioned|p120|||See also Cordillo Surface (p108). Developed in the top of the Eyre Formation. Silcrete genesis and timing discussed in detail.||||||
4714|Cordillo Silcrete|69946|5|Briefly described|p29, p129|Oligocene|Oligocene|Caps Eyre Formation to produce prominent mesas. Gently folded and tilted during Early Oligocene. Reworked into the Mirackina Conglomerate.||||||
4714|Cordillo Silcrete|69961|5|Briefly described|Map legend|Neogene|Paleogene||||||Silcrete, variably silicified sandstone and conglomerate; columnar and massive variants.|
4714|Cordillo Silcrete|70648|5|Briefly described|Map Legend|Neogene|Paleogene||||||Silcrete, variable silicified sandstone and conglomerate; columnar and massive variants.|20-JAN-22
4714|Cordillo Silcrete|70649|5|Briefly described|Map Legend|Neogene|Paleogene|2 un-named units: Light grey highly siliceous silcrete, conglomeratic in places; commonly columnar and massive. Pale brown to grey moderately siliceous silcrete with common relict sedimentary features including bedding and pebbles.|||Includes 2 un-named units.||Silcrete, variable silicified sandstone and conglomerate; columnar and massive variants.|
4714|Cordillo Silcrete|71321|6|Mentioned|p65|Oligocene|Late Eocene|Of Eromanga Basin. Nomenclature after Wopfner (1974, 1978).||||||
4714|Cordillo Silcrete|71342|6|Mentioned|Ch5 p29, Ch5 p130|Oligocene|Eocene|Lake Eyre Basin. This unit was gently folded and tilted during the Oligocene.||||Overlies the Eyre Formation.||
4714|Cordillo Silcrete|73234|6|Mentioned|p13|Early Oligocene|Late Eocene|Correlated with the topographically high-lying silcrete surface named 'Tent Hill surface' by Twidale et al. (1970).||||||
4739|Coronation Sandstone|9534|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Pebbly coarse quartz sandstone, commonly tuffaceous.||||||07-NOV-08
4739|Coronation Sandstone|9691|5|Briefly described|Map Legend|||Of the Edith River Group. Pebbly coarse quartz sandstone, commonly tuffaceous.||||||
4739|Coronation Sandstone|9701|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Edith River Group. Pebbly coarse quartz sandstone, commonly tuffaceous.||||||02-JUN-05
4739|Coronation Sandstone|23384|6|Mentioned|Fig 27|||Of Needham and Stuart-Smith (1985).||||||
4739|Coronation Sandstone|23733|5|Briefly described|p32 Fig. 19|||Of the El Sherana Group.  Contains constituent Scintio Breccia.||||||
4739|Coronation Sandstone|23867|5|Briefly described|Fig. 3|||Of El Sherana Group.  Formerly Coronation Member (Edith River Volcanics).  Geological Province: McArthur Basin.||||||
4739|Coronation Sandstone|24197|5|Briefly described|p105 Tb. 15.1|Paleoproterozoic|Paleoproterozoic|Of El Sherana Suite. Age: ~1865Ma. Geological Province: Pine Creek Inlier.||||||07-FEB-11
4739|Coronation Sandstone|24340|5|Briefly described|p147 Fig.3|||Overlain by the Pul Pul Rhyolite. Geological Province: Pine Creek Inlier.||||||
4739|Coronation Sandstone|31723|6|Mentioned|p523|||Stratigraphy||||||
4739|Coronation Sandstone|39357|4|Described|p14|||||||||
4739|Coronation Sandstone|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
4739|Coronation Sandstone|40248|3|Fully described|p222|||||||||
4739|Coronation Sandstone|40823|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
4739|Coronation Sandstone|40861|5|Briefly described|p122|||||||||
4739|Coronation Sandstone|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
4739|Coronation Sandstone|41125|6|Mentioned|p28|||See also Fig.15||||||
4739|Coronation Sandstone|41311|4|Described|p12|||||||||
4739|Coronation Sandstone|41397|4|Described|p13|||||||||
4739|Coronation Sandstone|41407|6|Mentioned|Map legend|Proterozoic||||||||
4739|Coronation Sandstone|41594|6|Mentioned|p20|||||||||
4739|Coronation Sandstone|42324|5|Briefly described|p5|||||||||
4739|Coronation Sandstone|42344|5|Briefly described|p54|||||||||
4739|Coronation Sandstone|43187|5|Briefly described|p2|||||||||
4739|Coronation Sandstone|43718|5|Briefly described|p2|||||||||
4739|Coronation Sandstone|43720|5|Briefly described|p12|||||||||
4739|Coronation Sandstone|43749|6|Mentioned|p30|||||||||
4739|Coronation Sandstone|43832|4|Described|21-23,Table6 p22, 97||Paleoproterozoic|Age ~1870 Ma||||||07-NOV-08
4739|Coronation Sandstone|46658|6|Mentioned|p556|||||||||
4739|Coronation Sandstone|47049|5|Briefly described|Table|||Elevation to formation from member status; redefined; placed in El Sherana Group.||||||07-AUG-06
4739|Coronation Sandstone|49744|5|Briefly described|Fig.3|||||||||
4739|Coronation Sandstone|50586|5|Briefly described|p1.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Of the El Sherana Suite. Intruded by Jim Jim Suite.||||||07-NOV-08
4739|Coronation Sandstone|60680|5|Briefly described|Map legend|Orosirian|Orosirian|Of the El Sherana Group (Jim Jim Suite). Moderately sorted quartz to sublithic sandstone; polymictic pebble to cobble conglomerate with lenses of poorly sorted medium to coarse lithic sandstone at base.||||||23-DEC-09
4739|Coronation Sandstone|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1829-1845Ma. Of El Sherana Group. Max thick 600m. Trough cross-bedded, coarse/v coarse, mod sorted qtz to sublithic sandst; polymictic pebble to cobble conglom with lenses of poorly sorted med/coarse lithic sandst at base.||||||07-JAN-09
4739|Coronation Sandstone|64730|5|Briefly described|p125 Fig. 3, p126|Paleoproterozoic|Paleoproterozoic|Age referred from overlying Pul Pul Rhyolite.|Min. deposition age of 1829 +/- 5 Ma.|Of El Sherana Group.|||Immature clastic sedimentary rocks and minor felsic volcanics.|02-MAY-12
4739|Coronation Sandstone|65232|5|Briefly described|p45, p46, p44 Fig. 29, p49, App. 2|||Of El Sherana Group. Unconformable over Koolpin Formation, and both units are faulted against Pul Pul Rhyolite. Pebbly and coarse sandstone; felsic and mafic volcanics; sedimentary breccia. Minor U mineralisation.||||||09-FEB-10
4739|Coronation Sandstone|67564|3|Fully described|p7 Table 2, p22, pp26-27, p39 Fig.20.|Paleoproterozoic|Paleoproterozoic|Jawoyn Sub-basin. 600 m thick; valley-fill succession of juvenile braided fluviatile sediments and extrusive volcanic rocks. Outcrops as discontinuous resistant lenses. Contains rocks previously mapped by Walpole et al. (1960) as Coronation Member and Walpole (1963) as Edith River Volcanics. Au and U mineralisation is related to reverse faults at the contact with Koolpin Formation.|1827 +/- 4 Ma (SHRIMP U-Pb: Jagodzinski 1999).|Unit in El Sherana Group.||Unconformably overlies Namoona, Mount Partridge, South Alligator and Finniss River Groups. Is intruded by Malone Creek Granite.|Basal polymictic, well-rounded, pebble to cobble conglomerate; cross-bedded, coarse to very coarse, quartz to sublithic sandstone; lithic sandstone; amygdaloidal basaltic lava; minor intrusive rhyolitic porphyry.|
4739|Coronation Sandstone|67779|5|Briefly described|p6 Fig.5.|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen.||Basal unit in El Sherana Group.||Is overlain by Pul Pul Rhyolite.||
4739|Coronation Sandstone|69418|6|Mentioned|p3:6|||Pine Creek Orogen. Hosts gold deposits (described).||||||12-JUL-16
4739|Coronation Sandstone|69420|4|Described|p5:4, 7, 15, 37, 51-52, 64-65, 78-80|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen. South Alligator region. Up to 600m thick. Juvenile braided fluviatile (sedimentary rocks), subaerial (volcanic rocks) deposits. Hosts the Coronation Hill Au deposit (described in detail). Hosts small U deposits. SHRIMP U-Pb zircon age.|1827 +/- 4 Ma (Jagodzinski, 1999).|El Sherana Group.||Unconformably overlies Finniss River Group. Is overlain by Pul Pul Rhyolite. Is interbedded with Scinto Breccia.|A valley-fill succession of cross-bedded, coarse to very coarse, quartz to sublithic sandstone; polymictic, pebble to cobble conglomerate; lithic sandstone; amygdaloidal basaltic lava; minor intrusive rhyolite porphyry.|12-JUL-16
4739|Coronation Sandstone|70293|5|Briefly described|p597|Orosirian|Orosirian|See also references to Coronation Hill Sandstone (p597, p599, p601, p613). Jawoyn Sub-basin. On p597, this is described as the basal unit of the El Sherana Group, (unconformably) onlapping steep topography of South Alligator Group and Zamu Dolerite, yet overlying Pul Pul Rhyolite and Big Sunday Formation (also of El Sherana Group). This is contradicted by Fig.3 which [correctly] shows the latter two units overlying the Coronation Sandstone.||Basal El Sherana Group.|||Includes polymictic conglomerate, basalt.|
4749|Corrie Member|22954|4|Described|Fig1p6,17,23-4|Warendan|Warendan|||||||
4749|Corrie Member|37572|4|Described|p162|||||||||
4749|Corrie Member|40136|5|Briefly described|p22|||||||||
4749|Corrie Member|40810|5|Briefly described|p14|||||||||
4749|Corrie Member|40852|6|Mentioned|Fig.3.7|||||||||
4749|Corrie Member|42354|6|Mentioned|p11|||Of Ninmaroo Formation.||||||07-AUG-06
4749|Corrie Member|46897|6|Mentioned|Fig.2|||||||||
4749|Corrie Member|46958|6|Mentioned|p195|||||||||
4749|Corrie Member|50244|6|Mentioned|p89 Fig. 1, p100 Fig. 7|Ordovician|Cambrian|Of Ninmaroo Formation. Geological Province: Georgina Basin.||||||22-APR-09
4749|Corrie Member|64068|4|Described|p74, 75|Early Ordovician|Early Ordovician|110 m thick in type section. Correlated with Kelly Creek Formation. [Said on p74 to be overlain by Jiggamore Member, but this makes no sense - probably a typo?]||Of Ninmaroo Formation.||Conformably overlies Mort Member. Is conformably overlain by Datson Member.|Bioclast (echinoderm), ooid, peloid and peloid-bioclast-intraclast grainstone, dolomitic sandstone, chert.|21-MAR-16
4749|Corrie Member|67323|5|Briefly described|GIS attrib tbl|Early Ordovician|Late Cambrian|Georgina Basin||Cockroach Group|||Limestone (pelmatozoan, peloid, clast and ooid grainstone), dolomitic sandstone, calcareous siltstone.|
4859|Cravens Peak beds|8187|5|Briefly described|Map legend|Devonian|Devonian|Sandstone, conglomerate. Overlie Ethabuka Sandstone and Mithaka Formation.||||||05-SEP-14
4859|Cravens Peak beds|8217|5|Briefly described|Map Legend|Devonian|Devonian|Sandstone, conglomerate.||||||
4859|Cravens Peak beds|12951|5|Briefly described|p142, p143 fig 4, p145 fig 6, p152|Devonian|Devonian|Georgina Basin. Fan-delta sediments.||||Correlated with Dulcie Sandstone.||
4859|Cravens Peak beds|23858|5|Briefly described|p917|Middle Devonian|Middle Devonian|Geological Province: Georgina Basin.||||||
4859|Cravens Peak beds|24442|5|Briefly described|p49|Middle Devonian|Early Devonian|On TOBERMORY sheet||||||
4859|Cravens Peak beds|38593|6|Mentioned|p90|||Georgina Basin||||||
4859|Cravens Peak beds|38832|6|Mentioned|p157|||||||||
4859|Cravens Peak beds|42643|6|Mentioned|p32|||||||||
4859|Cravens Peak beds|45148|6|Mentioned|p20|||||||||
4859|Cravens Peak beds|45155|6|Mentioned|Fig.8|||||||||
4859|Cravens Peak beds|49027|4|Described|p20|||||||||
4859|Cravens Peak beds|60122|4|Described|p34|Devonian|Devonian|Originally included rocks now mapped as Ethabuka Sst, Cravens Peak beds proper and Poodyea Formation. Unconformably overlies Ethabuka Sandstone and Mithaka Formation. Max. thickness: 280m. Geological Province: Georgina Basin. See also p4-5, p10 Tb. 1||||||08-AUG-06
4859|Cravens Peak beds|60590|5|Briefly described|Map legend|Devonian|Devonian|Calcareous sandstone and siltstone, limestone, minor conglomerate; grades upward into quartz sandstone and conglomerate.||||||
4859|Cravens Peak beds|61404|5|Briefly described|Map legend|Devonian|Devonian|Calcareous sandstone and siltstone, limestone, minor conglomerate; grades upwards into quartz sandstone and conglomerate. Geological Province: southern Georgina Basin.||||||11-FEB-09
4859|Cravens Peak beds|62983|5|Briefly described|p11|Devonian|Devonian|Synorogenic sedimentation. Geological Province: Georgina Basin.||||||
4859|Cravens Peak beds|63450|5|Briefly described|p78 Fig. 5, p83|Middle Devonian|Early Devonian|Geological province: Georgina Basin, West Toko Syncline.||||||07-FEB-11
4859|Cravens Peak beds|64068|4|Described|p78-79, p77, p19, p ix|Eifelian|Pragian|Ungrouped. Formerly included in what are now Ethabuka Sandstone and Poodyea Formation (see Draper 1980). Diverse fauna, particularly fish. Thickness over 280 m. Correlations: Dulcie Sandstone, Mereenie Sandstone or Parke Siltstone.||||Unconformably overlies Ethabuka or Carlo Sandstones or Mithaka Formation.|Calcareous siltstone and sandstone, limestone; minor conglomerate; overlain by sandstone and conglomerate.|05-APR-12
4859|Cravens Peak beds|64778|6|Mentioned|p13|Devonian|Devonian|Toko Syncline, Southern Georgina Basin.||||||
4859|Cravens Peak beds|64812|5|Briefly described|p237 Fig. 2|Devonian|Devonian|Geological Province: southern Georgina Basin.||||||07-FEB-11
4859|Cravens Peak beds|64813|5|Briefly described|p256 Fig. 3|Devonian|Devonian|Geological Province: southern Georgina Basin.||||||11-FEB-09
4859|Cravens Peak beds|65237|5|Briefly described|p4 Fig. 7, p10|||Geological province: southern Georgina Basin. Also written as Craven Creek Beds.||||||07-FEB-11
4859|Cravens Peak beds|65489|5|Briefly described|p126|Middle Devonian|Early Devonian|See also Cravens Peak Beds (p125). Deposition of these sediments in the Toko Syncline to Dulcie Syncline was as a response to the Pertnjara-Brewer Movement. Thrusted and folded during Alice Springs Orogeny.|||||Fluvial and marginal marine siliciclastics.|
4859|Cravens Peak beds|66499|6|Mentioned|p61 Fig.5|||Georgina Basin. [Misspelt as Cravens Peak Beds in text]||||||
4859|Cravens Peak beds|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Middle Devonian|Early Devonian|Georgina Basin. Age: Ordovician?|||||Conglomerate, sandstone, minor shale; limestone and calcareous siltstone at base.|
4859|Cravens Peak beds|67870|6|Mentioned|p43|Middle Devonian|Early Devonian|Georgina Basin.||||||
4859|Cravens Peak beds|68553|6|Mentioned|Map legend; schematic diagram.|Devonian|Devonian|||||||
4859|Cravens Peak beds|69443|4|Described|p28:5, 7, 27, 29-30, 32-33|Middle Devonian|Early Devonian|Reynolds in Smith (1965). Toko Syncline, Southern Georgina Basin. Synorogenic (Pertnjara-Brewer events of the Alice Springs Orogeny) foreland deposition of clastic sediments. Well-exposed as strike ridges or steep cuestas along the Toomba Range; elsewhere generally poorly exposed as low rubble-covered rises or dip slopes. Over 280m thick. Fossil assemblage contains ostracodes, fish, a plant and stromatolites. Pragian to early Eifelian age. Appears alliteratively, albeit incorrectly, as Craven Creek Beds in Figs.28.3 and 28.4.||||Unconformably overlies Carlo Sandstone and Mithaka Formation (Toko Group) or Ethabuka Sandstone. Correlative of Dulcie Sandstone.|A lower interval of calcareous siltstone, calcareous sandstone, limestone and minor conglomerate; an upper interval of cross-bedded, fine- to medium-grained quartz sandstone with clay pellets, and conglomerate.|12-JUL-16
4859|Cravens Peak beds|69458|6|Mentioned|p42:20|||Georgina Basin.||||Is overlain unconformably by Poodyea Formation.||14-SEP-18
4859|Cravens Peak beds|69591|5|Briefly described|p94, p112|Devonian|Devonian|Toko Syncline. Occurs along the Toomba Range SW of Boulia. Deposition was initiated by the Alice Springs Orogeny. Originally included rocks now mapped as Ethabuka Sandstone and Poodyea Formation. Contains an extensively-studied, Emsian-Eifelian fossil fish assemblage.|||||Calcareous sandstone and siltstone, limestone, minor conglomerate grading upward into coarse sandstone and conglomerate.|
4859|Cravens Peak beds|69673|4|Described|p111, p118, p119 fig 94|Devonian|Devonian|Informal name. At least 280m thick. ||||Correlated with Dulcie Sandstone|Calcareous siltstone, calcareous sandstone, limestone and minor conglomerate, fine to medium grained quartz sandstone with clay pellets and conglomerate.|
5070|Currant Bush Limestone|22954|6|Mentioned|Fig3p9|Undillan|Middle Cambrian|||||||
5070|Currant Bush Limestone|23031|4|Described|28|||Geol province: Georgina Basin.||||||08-AUG-06
5070|Currant Bush Limestone|23393|5|Briefly described|p22|Paleozoic|Paleozoic|||||||07-NOV-08
5070|Currant Bush Limestone|23408|6|Mentioned|p527|||Includes two-toned deeper-water ramp carbonates.||||||15-JUN-09
5070|Currant Bush Limestone|26310|4|Described|Table 1|Middle Cambrian|Middle Cambrian|Maximum Thickness: 500 feet.  Limestone, some marl.||||||
5070|Currant Bush Limestone|30242|6|Mentioned|Fig.2|||||||||
5070|Currant Bush Limestone|30479|6|Mentioned|Fig.5|||See also Fig.6, Fig.7. Stratigraphic relationships||||||
5070|Currant Bush Limestone|30914|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
5070|Currant Bush Limestone|31396|6|Mentioned|Fig.3|||||||||
5070|Currant Bush Limestone|32948|4|Described|p111|||Re fossil locality.||||||08-AUG-06
5070|Currant Bush Limestone|33111|4|Described|p35|||By inference, the type locality is in the vicinity of Currant Bush Creek, 16 km SW of Thorntonia homestead. No type section has been specified.||||||24-NOV-22
5070|Currant Bush Limestone|33368|5|Briefly described|p5|||||||||
5070|Currant Bush Limestone|33482|6|Mentioned|Fig.2|||Middle Cambrian||||||
5070|Currant Bush Limestone|34287|6|Mentioned|Table.3?|||||||||
5070|Currant Bush Limestone|34395|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
5070|Currant Bush Limestone|34659|6|Mentioned|p228|||||||||
5070|Currant Bush Limestone|35004|6|Mentioned|Fig.60|||||||||
5070|Currant Bush Limestone|35054|6|Mentioned|Table 23|||||||||
5070|Currant Bush Limestone|35121|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
5070|Currant Bush Limestone|35139|4|Described|Table.2|||||||||
5070|Currant Bush Limestone|35553|6|Mentioned|p36|||See also Appendix 2, description of Agnostid localities.||||||
5070|Currant Bush Limestone|35843|6|Mentioned|p444|||Source of ostracods.||||||
5070|Currant Bush Limestone|36473|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian to Ordovician||||||
5070|Currant Bush Limestone|36818|6|Mentioned|p203|||||||||
5070|Currant Bush Limestone|37275|6|Mentioned|p287|||||||||
5070|Currant Bush Limestone|37572|4|Described|p157|||See also p165 and Fig.7||||||08-AUG-06
5070|Currant Bush Limestone|38444|5|Briefly described|p105|||||||||
5070|Currant Bush Limestone|38445|6|Mentioned|p105|||||||||
5070|Currant Bush Limestone|38446|6|Mentioned|Table 23|||||||||
5070|Currant Bush Limestone|39422|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Thin-bedded grey limestone and lenses and interbeds of marl and sandy dolomite. Conformably overlies Border Waterhole Formation; conformably overlain and interfingered with Camooweal Dolomite.||||||11-JUN-08
5070|Currant Bush Limestone|39445|5|Briefly described|Table 4|||See also p62||||||08-AUG-06
5070|Currant Bush Limestone|39497|6|Mentioned|p16|||||||||
5070|Currant Bush Limestone|39690|6|Mentioned|Table 1|||||||||
5070|Currant Bush Limestone|39708|5|Briefly described|p477|||||||||
5070|Currant Bush Limestone|39942|6|Mentioned|p465|||||||||
5070|Currant Bush Limestone|40038|6|Mentioned|p248|||||||||
5070|Currant Bush Limestone|40686|5|Briefly described|p407|||||||||
5070|Currant Bush Limestone|40856|5|Briefly described|p315|||Mention Fig.23.6||||||
5070|Currant Bush Limestone|41018|6|Mentioned|p239|||||||||
5070|Currant Bush Limestone|41129|6|Mentioned|Fig.8|||||||||
5070|Currant Bush Limestone|41240|6|Mentioned|Fig.1|||||||||
5070|Currant Bush Limestone|41388|6|Mentioned|Fig.2|||||||||
5070|Currant Bush Limestone|42139|6|Mentioned|Fig.13 P80|||||||||
5070|Currant Bush Limestone|42477|5|Briefly described|p68|||||||||
5070|Currant Bush Limestone|44091|14|Not recorded|p16,Tb.1,18||Cambrian|||||||
5070|Currant Bush Limestone|44205|14|Not recorded|p89,155|||See also Lexicon.||||||
5070|Currant Bush Limestone|44210|2|Defined|map, Tb.2|||Overlies Inca Formation.||||||23-NOV-22
5070|Currant Bush Limestone|44211|4|Described|p97,100-103|||Contemporaneous with most of Age Creek Formation, Inca Formation, Quita Formation.||||||23-NOV-22
5070|Currant Bush Limestone|44213|14|Not recorded|Map Legend|||Not on white card.||||||
5070|Currant Bush Limestone|44274|2|Defined|Tb.1,p10,11,13,map||Middle Cambrian|See also Lexicon. Conformably overlies Border Waterhole Formation.||||||
5070|Currant Bush Limestone|44275|14|Not recorded|Map Legend|||||||||
5070|Currant Bush Limestone|44281|14|Not recorded|Map Legend||Middle Cambrian|||||||
5070|Currant Bush Limestone|44441|14|Not recorded|p.8||Middle Cambrian|O/lain by Camooweal Dolomite to North. Middle Cambrian. (E53-16).||||||
5070|Currant Bush Limestone|44482|14|Not recorded|p.11-12, opp.p.6,map|||(E53-12). See also p.15, for more details||||||
5070|Currant Bush Limestone|44483|5|Briefly described|map legend||Middle Cambrian|Middle Cambrian.||||||
5070|Currant Bush Limestone|44922|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Overlies Border Waterhole Formation.||||||01-JUL-04
5070|Currant Bush Limestone|45032|14|Not recorded|p8,10||Middle Cambrian|Tb.1, Pl.1. (E53-12).||||||
5070|Currant Bush Limestone|45052|3|Fully described|p93|||M.Camb.||||||
5070|Currant Bush Limestone|45054|6|Mentioned|p6|||M.Cambrian. Fossil locality||||||
5070|Currant Bush Limestone|45079|5|Briefly described|p34|||Cambrian age||||||
5070|Currant Bush Limestone|45102|6|Mentioned|p43|||||||||
5070|Currant Bush Limestone|45119|6|Mentioned|p3,p5|||||||||
5070|Currant Bush Limestone|45166|5|Briefly described|Table 15|||||||||
5070|Currant Bush Limestone|47058|5|Briefly described|p132|||||||||
5070|Currant Bush Limestone|60122|6|Mentioned|p57 Appendix|||Correlated with parts of Arthur Creek Formation. Geological Province: eastern Georgina Basin||||||11-MAY-05
5070|Currant Bush Limestone|60418|5|Briefly described|p140|Middle Cambrian|Middle Cambrian|||||||
5070|Currant Bush Limestone|62659|5|Briefly described|Map Legend|Cambrian|Cambrian|Partially dolomitised foetid argillaceous, quartzic and bioclast limestone; interbeds of ooid grainstone, dolostone, shale, siltstone and marl.||||||
5070|Currant Bush Limestone|63450|5|Briefly described|p82|Middle Cambrian|Middle Cambrian|Geological Province: Undilla Sub-basin.||||||07-FEB-11
5070|Currant Bush Limestone|64068|5|Briefly described|p63, 62, 64, p137|||Correlative with Arthur Creek Formation in NT. Sparked interest in oil shale potential of the Georgina Basin. Correlated with Blazan Shale, Inca Formation, Quita Formation, Roaring Siltstone, Devoncourt Limestone.||||Overlies and interdigitates with Inca Formation.|Contains thin oil shale, bituminous limestone and bituminous shale.|05-APR-12
5070|Currant Bush Limestone|64443|6|Mentioned|pg6 Tb.1, p14, p40.|||Correlative of Wonarah Formation, Ranken Limestone; conformably underlies the Camooweal Dolostone.||||||
5070|Currant Bush Limestone|65337|3|Fully described|p9 Fig.5, pp64-65.|Middle Cambrian|Middle Cambrian|Southeast MOUNT DRUMMOND area. 50 - 116 m thick. Occasional ellipsoidal concretions are characteristic.||Unit in Narpa Group.||Overlies Border Waterhole Formation. Is overlain by Camooweal Dolostone.|Grey and tan, partially dolomitised foetid argillaceous, quartzic and bioclastic limestone; interbeds of ooid grainstone, sandstone, shale, siltstone and marl.|
5070|Currant Bush Limestone|67323|5|Briefly described|Solid Geology Map; p72, p83|Middle Cambrian|Middle Cambrian|See also GIS attrib tbl. Undilla Sub-basin, Georgina Basin. Contains Pb, Zn and Pb-Zn anomalies 50-75km NE of Camooweal.||Narpa Group.||Overlies Inca Formation and (unconformably) Beetle Creek Formation. Is overlain by V-Creek Limestone. Partial lateral equivalent of Age Creek Formation.|Limestone, bituminous limestone, sandy limestone, calcilutite, minor arenite, chert nodules.|
5070|Currant Bush Limestone|69437|5|Briefly described|p22:10|Series 3|Series 3|Eastern Undilla Sub-basin, Georgina Basin, Centralian B Superbasin. Sequence 2.||||Is overlain by Camooweal Dolostone.||12-JUL-16
5070|Currant Bush Limestone|69443|4|Described|p28:16, 20, 22-24|Middle Cambrian|Middle Cambrian|Opik (1956, 1960). Undilla Sub-basin, Georgina Basin. Unclear stratigraphic relationships. Is overlain transitionally, and is partly equivalent to, Camooweal Dolostone. Correlated with Anthony Lagoon, Wonarah Formations and Ranken Limestone. Shallow-marine, carbonate ramp deposits. Contains a very diverse fossil assemblage; age determinations are discussed.||Narpa Group.||Overlies Border Waterhole Formation conformably or disconformably; Thorntonia Limestone unconformably; Gowers Formation disconformably. Overlies and interfingers with Age Creek and Inca Formations.|Mainly bedded, partially dolomitised foetid argillaceous, quartzose and bioclast limestone and dolomitic limestone, with interbeds of ooid grainstone, shale, siltstone, marl and chert, which occurs as discrete layers or irregular patches.|12-JUL-16
5070|Currant Bush Limestone|69573|6|Mentioned|p659|||Contains Drumian Stage [Cambrian] fossil sites.||||||
5070|Currant Bush Limestone|69591|5|Briefly described|p87-90, p96-97, p98 Fig.2.91|Cambrian|Cambrian|Undilla Sub-basin, Georgina Basin. Contains an extremely diverse fauna (listed).||Narpa Group.||Overlies and in part equivalent to Inca Formation; disconformably overlies Thorntonia Limestone and Age Creek Formation. Is overlain conformably by V Creek Limestone.|A bituminous, flaggy limestone with oolitic, shaly and marly interbeds up to 120m thick. Local beds up to 2m thick of rip-up conglomerates, and numerous algal-bound unbedded build-ups up to 10m diameter piercing the otherwise thin bedding.|
5070|Currant Bush Limestone|69673|4|Described|p116, p117|||116m thick.||Narpa Group|||Bedded, partially dolomitized foetid, argillaceous, quartzic and bioclast limestone, dolomitic limestone interbedded with ooid grainstone, shale, siltstone, marl and chert.|
5070|Currant Bush Limestone|70380|6|Mentioned|p745|Series 3|Series 3|Undilla Sub-basin, Georgina Basin.||||||
5070|Currant Bush Limestone|70723|4|Described|p21-29, p31|Cambrian|Cambrian|Georgina Basin. Deposited under anoxic conditions on a carbonate ramp. Contains a highly divese fossil assemblage. Karst features occur in the lower part of the unit. Oil-prone source rock. Kerogen type and biomarker compositions discussed in detail. Mis-spelt as Current Bush Limestone on p25.||Narpa Group||Overlies Beetle Creek and Inca Formations. Is overlain by Age Creek Formation.|Partially dolomitized argillaceous, fossiliferous, quartzic and bioclastic limestone with fine layers of shale; siltstone, marl and chert.|
5070|Currant Bush Limestone|72297|6|Mentioned|p752|Cambrian|Cambrian|Georgina Basin.||||||
5070|Currant Bush Limestone|72321|6|Mentioned|Fig 2|Drumian|Wulian|Undilla Sub-basin, Georgina Basin. Australian Stages: Floran to Undillan. ||of Narpa Group.||||
5070|Currant Bush Limestone|72516|6|Mentioned|p92|Cambrian|Cambrian|Eastern Georgina Basin.||||Equivalent to the Arthur Creek Formation.||03-JUN-21
5070|Currant Bush Limestone|72967|6|Mentioned|p5|||Georgina Basin.||Napa Group||||
5070|Currant Bush Limestone|73418|5|Briefly described|p4 Fig.3|Miaolingian|Miaolingian|Georgina Basin, Undilla Sub-basin.||Narpa Group||Overlies Gowers Formation, Beetle Creek Formation, Inca Formation, underlies V-Creek Limestone, Age Creek Formation|Limestone.|
5163|Daly River Group|9324|5|Briefly described|Map Legend|Ordovician|Cambrian|Limestone, siltstone, sandstone, conglomerate.||||||
5163|Daly River Group|9579|5|Briefly described|Map Sheet|Cambrian||||||Shown as unconformably overlying the Fitzmaurice Group.||10-NOV-14
5163|Daly River Group|22600|6|Mentioned|Map legend|||||||||
5163|Daly River Group|22808|6|Mentioned|7 fig 4|||||||||
5163|Daly River Group|22809|5|Briefly described|1|Ordovician|Cambrian|||||||
5163|Daly River Group|22810|5|Briefly described|Table3 P7, P19|Ordovician|Cambrian|||||||
5163|Daly River Group|22813|5|Briefly described|Map|Ordovician|Cambrian|Limestone, siltstone, sandstone, conglomerate.||||||19-OCT-05
5163|Daly River Group|23119|5|Briefly described|p433|||||||||
5163|Daly River Group|23120|5|Briefly described|p428|||||||||
5163|Daly River Group|23216|4|Described|p3, p38|Early Ordovician|Middle Cambrian|(Noakes, 1949). Consists of: Oolloo Dolostone, Jinduckin Formation and Tindall Limestone.||||||19-JAN-06
5163|Daly River Group|23374|5|Briefly described|Fig3p5,18|Ordovician|Cambrian|Of Daly Basin.||||||08-AUG-06
5163|Daly River Group|23714|5|Briefly described|p36|Paleozoic|Paleozoic|See also page 7 Table 1. Max. thickness: 700 m.||||||07-NOV-08
5163|Daly River Group|23822|5|Briefly described|p302 Fig. 2|Ordovician|Cambrian|Geological Province: Litchfield Province.||||||
5163|Daly River Group|24049|5|Briefly described|Map Legend|Paleozoic|Paleozoic|In regional setting map legend.||||||07-NOV-08
5163|Daly River Group|24122|4|Described|p13|Early Ordovician|Middle Cambrian|Geological Province: Daly Basin.||||||
5163|Daly River Group|24300|5|Briefly described|Map Legend|Ordovician|Cambrian|Geological Province: Daly Basin.|||Includes Tindall Limestone, Jinduckin Formation, ? Montejinni Limestone.|||14-MAR-18
5163|Daly River Group|29591|6|Mentioned|p107|||||||||
5163|Daly River Group|32109|6|Mentioned|Table 1|||Mid.Camb.-L.Dev.||||||
5163|Daly River Group|32170|6|Mentioned|Map legend|Early Ordovician|Middle Cambrian|Middle Cambrian - Lower Ordovician||||||
5163|Daly River Group|32171|6|Mentioned|p8|||Middle Cambrian||||||
5163|Daly River Group|32700|4|Described|p16|||See also Table 2. Mid. Cam. - L. Ord.||||||
5163|Daly River Group|35055|6|Mentioned|p222|||||||||
5163|Daly River Group|35064|6|Mentioned|p208|||||||||
5163|Daly River Group|35465|6|Mentioned|Fig.1|||Geology of Pine Creek Geosyncline||||||
5163|Daly River Group|35495|6|Mentioned|p350|||||||||
5163|Daly River Group|36473|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian to Ordovician||||||
5163|Daly River Group|38267|6|Mentioned|p84|||||||||
5163|Daly River Group|39069|6|Mentioned|p23|||||||||
5163|Daly River Group|39210|6|Mentioned|p48|||||||||
5163|Daly River Group|39679|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
5163|Daly River Group|40136|5|Briefly described|p22|||||||||
5163|Daly River Group|40168|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian to Ordovician||||||
5163|Daly River Group|40957|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian to Ordovician||||||
5163|Daly River Group|41294|6|Mentioned|Map legend|Middle Cambrian|Early Cambrian|||||||
5163|Daly River Group|41295|6|Mentioned|p6|||||||||
5163|Daly River Group|41406|6|Mentioned|Map legend|Ordovician|Cambrian|||||||
5163|Daly River Group|41646|6|Mentioned|Map legend|Cambrian|Ordovician|Limestone, siltstone, sandstone, conglomerate.||||||17-OCT-05
5163|Daly River Group|41660|5|Briefly described|Map legend|Ordovician|Cambrian|Includes Tindall Limestone and ?Antrim Plateau Volcanics?. Limestone, siltstone, sandstone, conglomerate.||||||08-AUG-06
5163|Daly River Group|41661|6|Mentioned|Fig.5|||||||||
5163|Daly River Group|42012|2|Defined|p43|Early Ordovician|Middle Cambrian|See also p14.||||||08-AUG-06
5163|Daly River Group|42014|5|Briefly described|Map legend|Cambrian|Ordovician|||||||
5163|Daly River Group|42070|4|Described|p3|||||||||
5163|Daly River Group|43010|5|Briefly described|p139|||||||||
5163|Daly River Group|43140|5|Briefly described|p4|Ordovician|Cambrian|||||||
5163|Daly River Group|43149|5|Briefly described|Map Legend|Ordovician|Cambrian|||||||
5163|Daly River Group|43187|5|Briefly described|p7|||||||||
5163|Daly River Group|43292|5|Briefly described|Map Legend||Cambrian|||||||
5163|Daly River Group|43624|6|Mentioned|Table 1,p9|Ordovician|Cambrian|||||||
5163|Daly River Group|43832|4|Described|30-31, Table7 p26|||Within Daly River Basin. Underlain by Cambrian Jindare Formation.||||||
5163|Daly River Group|44112|6|Mentioned|p67||Middle Cambrian|||||||
5163|Daly River Group|44113|5|Briefly described|p240|Early Ordovician|Middle Cambrian|Geological Province: Daly River Basin||||||
5163|Daly River Group|44161|14|Not recorded|p.47|||||||||
5163|Daly River Group|44201|14|Not recorded|p.10|||||||||
5163|Daly River Group|44954|14|Not recorded|Not recorded|||||||||
5163|Daly River Group|44965|14|Not recorded|Not recorded|||||||||
5163|Daly River Group|45022|2|Defined|pp.100,101|Late Ordovician|Middle Cambrian|On many pages.||||||
5163|Daly River Group|45058|5|Briefly described|p18|||Mid Camb - L.Ord.||||||
5163|Daly River Group|46675|5|Briefly described|Map legend|Paleozoic|Paleozoic|Includes the Jinduckin Formation, Tindall Limestone and Jindare Formation.  Unconformably overlies the Tolmer Group.||||||07-NOV-08
5163|Daly River Group|46676|14|Not recorded|p.6||Middle Cambrian|M.Cambrian; contains Tindall Limestone, Jinduckin Formation & Oolloo Limestone.||||||
5163|Daly River Group|46679|14|Not recorded|map legend|||Map legend of Katherine, 1 mile (D53-9).||||||
5163|Daly River Group|48800|14|Not recorded|Not recorded|||||||||
5163|Daly River Group|48867|14|Not recorded|p.7|||map. Katherine-Darwin area.||||||
5163|Daly River Group|48942|4|Described|p82|||||||||
5163|Daly River Group|60573|6|Mentioned|Regional Setting legend|Paleozoic|Paleozoic|||||||07-NOV-08
5163|Daly River Group|61403|5|Briefly described|Map Legend|Paleozoic|Paleozoic|In regional setting map legend.||||||07-NOV-08
5163|Daly River Group|63866|5|Briefly described|p108, p111|Cambrian|Cambrian|Litchfield Province, Pine Creek Orogen. Overlies the Proterozoic stratigraphy in this province.||||||
5163|Daly River Group|64443|6|Mentioned|p40|||Of Daly Basin. Correlative of Barkly Group, Georgina Basin in part.||||||
5163|Daly River Group|64698|4|Described|lithinterp table|Cambrian|Cambrian|Age ~500-545Ma. Daly Basin. Vesicular and amygdaloidal basalt at base followed by sandstone, limestone, dolostone, oolitic and stromatolitic dolostone.||||||07-JAN-09
5163|Daly River Group|65339|6|Mentioned|p5 Fig.4. ||||||Includes Tindall Limestone, Jinduckin Formation and Oolloo Dolostone.|||
5163|Daly River Group|65345|6|Mentioned|p4.||||||Includes basal Tindall Limestone, Jinduckin Formation and Oolloo Dolostone.|||
5163|Daly River Group|67186|5|Briefly described|Map legend.|Cambrian|Cambrian||||Includes Tindall Limestone and Jinduckin Formation.|||23-NOV-11
5163|Daly River Group|69420|5|Briefly described|p5:105|Paleozoic|Paleozoic||||||Siltstone, dolomitic siltstone and limestone.|12-JUL-16
5163|Daly River Group|69443|6|Mentioned|p28:21|||Daly Basin.||||Correlated with Barkly Group.||12-JUL-16
5163|Daly River Group|69446|5|Briefly described|p31:1-6|Middle Cambrian|Middle Cambrian|Noakes (1949). Daly Basin. 709m thick in the stratotype section in cored drillhole NTGS 86/1 (Kruse et al., 1990). Base age from diverse fauna from basal Tindall Limestone. Sparse fossils in Jinduckin Formation, Olloo Dolostone are not diagnostic. Lithological correlation of Jinduckin Fm with Anthony Lagoon Fm suggests whole Group is Middle Cambrian.|||Tindall Limestone, Jinduckin Formation, Oolloo Dolostone.|Is overlain unconformably by Florina Formation.||13-SEP-18
5163|Daly River Group|69673|6|Mentioned|p191|||709m thick.|||Includes Tindall Limestone, Jinduckin Formation, Oolloo Dolostone|||
5163|Daly River Group|70380|3|Fully described|p743-759|Middle Cambrian|Middle Cambrian|Noakes (1949), who did not name constituent Formations. This was done by Malone (1962) and Randal (1962); the three units were formally defined by Kruse (in Kruse et al., 1990) who renamed the Oolloo Limestone as Oolloo Dolostone to reflect its dominant lithology. Maximum thickness of 709m in the stratotype section in cored drill hole NTGS86/1 in the centre of the Daly Basin in the Jinduckin 1:100 000 sheet area. This unit came to be regarded as extending into the Early Ordovician, because of the misassignment of strata (in the Claravale area) later recognised as the separate, Florina Formation.|||Tindall Limestone, Jinduckin Formation, Oolloo Dolostone.|Is overlain unconformably by Florina Formation.|Has a karstified surface.|
5163|Daly River Group|70850|5|Briefly described|Map legend.|Cambrian|Cambrian|Daly Basin.|||Tindall Limestone, Jinduckin Formation.|||
5163|Daly River Group|70866|5|Briefly described|Map legend.|Ordovician|Cambrian|Daly Basin.|||Includes Oolloo Dolostone, Jinduckin Formation, Tindall Limestone.|||01-MAR-18
5163|Daly River Group|71632|5|Briefly described|Map legend.|||Daly Basin. Mapped with Antrim Plateau Volcanics and Jindare Formation as a single unit.||||||
5202|Darbilla Formation|42058|5|Briefly described|p116|||||||||
5202|Darbilla Formation|62506|5|Briefly described|p1-3|Carboniferous|Devonian|Of the Arafura Group. Sandy siltstone. ||||||
5202|Darbilla Formation|62510|5|Briefly described|p3|Early Carboniferous|Late Devonian|||||||
5202|Darbilla Formation|62837|5|Briefly described|Stratigraphic columns|Tournaisian|Tournaisian|Age: 355-~354Ma. Geological Province: Money Shoals Basin.||||||01-MAR-10
5202|Darbilla Formation|63062|5|Briefly described|p9 Fig. 9, p48 Tb. 1|Late Devonian|Late Devonian|Of the Arafura Group. Overlies the Yabooma Formation. Age is Famennian. Geological Province: Arafura and Money Shoal Basins. Non-marine mudstone and siltstone deposits.||||||07-FEB-11
5202|Darbilla Formation|69297|5|Briefly described|p283, p285|Famennian|Famennian|Arafura Basin. Deposited largely in a non-marine environment. ||Arafura Group||Overlies the Yabooma Formation.|Mudstone and siltstone.|
5202|Darbilla Formation|69451|4|Described|p35:3-4, 8-9; 35:13 Fig.35.9|Late Devonian|Late Devonian|Bradshaw et al. (1990). Arafura Basin (offshore). Non-marine, possible sabkha or tidal-flat, and fluvial, deposits. 262-380m thick. Palynoflora indicate a latest Famennian age.||Arafura Group.||Overlies Yabooma Formation apparently conformably. Is overlain unconformably by Kulshill Group.|Mudstone, sandy siltstone and lesser interbedded sandstone; includes fining-upward intervals; palynoflora.|12-JUL-16
5202|Darbilla Formation|69673|6|Mentioned|p197|||||Arafura Group||||
5202|Darbilla Formation|70098|4|Described|p5, p8, p19 Fig.5|Famennian|Famennian|Depositional environment: largely non-marine environment.||Arafura Group||Overlies Yabooma Formation. Is overlain by Kulshill Group (and equivalent?)|Mudstone and siltstone dominated succession.|
5204|Dare Siltstone Member|22566|6|Mentioned|Fig 2 on p77|||Of Parke Siltstone.||||||08-AUG-06
5204|Dare Siltstone Member|22760|4|Described|p340|Late Devonian|Late Devonian|Of Parke Siltstone.  Contains a sparse fish fauna known from the Cleland Hills, Dare Plain and Ross River.  At Dare Plain the age of the Dare Siltstone is Frasnian but the age probably decreases toward the south east.||||||08-AUG-06
5204|Dare Siltstone Member|22761|6|Mentioned|p350|||Of the Parke Siltstone.  Stratigraphically equivalent to the N'Dhala Member.||||||08-AUG-06
5204|Dare Siltstone Member|31566|2|Defined|p236|Devonian|Devonian|See also p237.||||||08-AUG-06
5204|Dare Siltstone Member|32208|6|Mentioned|Map legend|Devonian|Devonian|||||||
5204|Dare Siltstone Member|32209|6|Mentioned|Map legend|Devonian|Devonian|||||||
5204|Dare Siltstone Member|35102|6|Mentioned|p39|||||||||
5204|Dare Siltstone Member|40740|6|Mentioned|p97|||||||||
5204|Dare Siltstone Member|41385|6|Mentioned|Fig.2|||See also Fig.12||||||
5204|Dare Siltstone Member|43225|5|Briefly described|Map Legend||Devonian|Of Pertnjara Group.||||||08-AUG-06
5204|Dare Siltstone Member|43503|6|Mentioned|42-45|Late Devonian|Middle Devonian|||||||
5204|Dare Siltstone Member|43647|6|Mentioned|Fig.7,p538|||||||||
5204|Dare Siltstone Member|43648|6|Mentioned|Fig.27,p509|||||||||
5204|Dare Siltstone Member|43649|5|Briefly described|p463|||||||||
5204|Dare Siltstone Member|47050|6|Mentioned|Fig.2|||||||||
5204|Dare Siltstone Member|67565|5|Briefly described|p42.|Devonian|Devonian|||Unit in Parke Siltstone.||Overlies Harajica Sandstone Member. Is overlain by Amulda Member.|A cyclic succession of siltstone units.|
5204|Dare Siltstone Member|69438|3|Fully described|p23:38-39|||Jones (1972). Amadeus Basin. A much broader distribution than the underlying Members. About 500m thick at the type locality in the LAKE AMADEUS map area. Has ripple marks, mudcracks and halite pseudomorphs.||Parke Siltstone.||Overlies Harajica Sandstone Member conformably and gradationally, Mereenie Sandstone and Larapinta Group disconformably. Is overlain conformably and gradationally by Amulda Member.|A cyclic succession of laminated and massive siltstone. Thin beds of very fine-grained calcareous sandstone occur near the base; thin beds of fine-grained silty sandstone occur towards the top.|12-JUL-16
5204|Dare Siltstone Member|69673|6|Mentioned|p67|||||Parke Siltstone||||
5252|Darwarunga Sandstone|22538|6|Mentioned|Fig3 P708|||||||||
5252|Darwarunga Sandstone|22600|4|Described|Map legend|Statherian|Statherian|||||||
5252|Darwarunga Sandstone|24048|6|Mentioned|p59|||Of Habgood Group.||||||08-AUG-06
5252|Darwarunga Sandstone|24049|5|Briefly described|Map Legend|Statherian|Statherian|Of Habgood Group. Lower part (ridge forming): sandstone; minor stromatolitic chert (silicified carbonate) and cauliflower chert nodules. Upper part (recessive): sandstone, dolomitic siltstone and silty dolostone. Geol. Prov: McArthur Basin.||||||13-OCT-05
5252|Darwarunga Sandstone|32660|5|Briefly described|Table 4|||||||||
5252|Darwarunga Sandstone|43010|2|Defined|p134||Paleoproterozoic|Of Habgood Group. Of Statherian age.||||||07-NOV-08
5252|Darwarunga Sandstone|44112|4|Described|p30,58-59|||||||||
5252|Darwarunga Sandstone|61403|5|Briefly described|Map Legend|Statherian|Statherian|Of Habgood Group. Lower part (ridge forming): sandstone; minor stromatolitic chert (silicified carbonate) and cauliflower chert nodules. Upper part (r ecessive): sandstone, dolomitic siltstone and silty dolostone. Geol. Prov: McArthur Basin.||||||
5252|Darwarunga Sandstone|64817|6|Mentioned|p353 Fig.4 |||||Of the Habgood Group.||||
5252|Darwarunga Sandstone|67323|6|Mentioned|Eastern Australia Time-Space Plot|||McArthur region.||||||
5252|Darwarunga Sandstone|69430|4|Described|p15:3, 20|||Walker Fault Zone, northern McArthur Basin. c.350m thick. Shallow water deposits with periodic evaporitic conditions and exposure. Lower contact not exposed.||Habgood Group.||Overlies Yarawoi Formation. Is overlain by Ulunourwi Formation possibly conformably.|A lower very resistant white, grey to pink sandstone, medium bedded, blocky; minor chert and relict stromatolitic layers, under an upper more recessive unit of interbedded sandstone, dolomitic mudstone and minor dolostone, sparse stromatolites.|12-JUL-16
5252|Darwarunga Sandstone|69673|6|Mentioned|p16 fig 13|||Walker Fault Zone||Habgood Group||Overlain by Ulunourwi Formation, overlies Yarawoi Formation||
5252|Darwarunga Sandstone|71374|4|Described|iii, p1 tbl 1, p12, p14-p17, p49-p50|Statherian|Statherian|Northern McArthur Basin. SHRIMP age is interpreted as the maximum depositional age for this formation. Sampling site provided along with zircon description and SHRIMP analytical discussion. The reference section of Pumb and Roberts (1992) was the sampling site for this unit; there is no type section for this unit. 350m thick, prominent ridge-forming unit. Informally subdivided into two units. |1661 +/- 19 Ma (SHRIMP U-Pb)|Habgood Group||Overlies the Yarawoi Formation. Overlain by the Ulunourwi Formation. Equivalent to the Yarrawirrie Formation.|Fine-grained quartz sandstone.|
5252|Darwarunga Sandstone|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.||Upper Habgood Group.||||
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|
5263|Datson Member|22954|4|Described|Fig1p6,17,23-5||Warendan|||||||
5263|Datson Member|36217|6|Mentioned|p206|||Published by Druce 1978. Definition approved by Qld SNC.||||||
5263|Datson Member|37572|4|Described|p162|||||||||
5263|Datson Member|38532|4|Described|p245|||||||||
5263|Datson Member|40127|6|Mentioned|p8|||||||||
5263|Datson Member|40136|6|Mentioned|p23|||||||||
5263|Datson Member|40852|6|Mentioned|Fig.3.7|||||||||
5263|Datson Member|46897|6|Mentioned|Fig.2|||||||||
5263|Datson Member|46958|6|Mentioned|p195|||||||||
5263|Datson Member|50244|6|Mentioned|p89 Fig. 1|Ordovician|Cambrian|Of Ninmaroo Formation. Geological Province: Georgina Basin.||||||21-APR-09
5263|Datson Member|64068|4|Described|p74-75|Early Ordovician|Early Ordovician|210 m thick in type section. Fossiliferous. Correlated with Kelly Creek Formation.Conodonts indicate early Early Ordovician (late Warendian Chosonodina herfurthi-Cordylodus angulatus Assemblage Zone; Shergold and Nicoll 1992).||Of Ninmaroo Formation||Conformably overlies Corrie Member. Laterally grades into, and is gradationally overlain by, Swift Formation.|Bioclast (dolo)grainstone, (dolo)boundstone and chert.|21-MAR-16
5263|Datson Member|67323|5|Briefly described|GIS attrib tbl|Early Ordovician|Late Cambrian|Georgina Basin||Cockroach Group|||Thin-bedded limestone or dolomite with interbedded chert|
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).||||||
5310|Deception Formation|22561|5|Briefly described|p21|Neoproterozoic|Neoproterozoic|||||||
5310|Deception Formation|22565|6|Mentioned|p71 in Table 1|||||||||
5310|Deception Formation|22650|6|Mentioned|p 159|Cambrian|Cambrian|||||||
5310|Deception Formation|22651|5|Briefly described|p 187|Late Cambrian|Middle Cambrian|Of the Pertaoorrta Group.||||||08-AUG-06
5310|Deception Formation|22763|6|Mentioned|Table 1 on p386|Cambrian|Cambrian|Of Pertaoorrta Group.||||||08-AUG-06
5310|Deception Formation|22804|6|Mentioned|Fig 2 on p432|Cambrian|Cambrian|Of Pertaoorrta Group.||||||08-AUG-06
5310|Deception Formation|22826|6|Mentioned|Fig 2 on p565|Cambrian|Cambrian|||||||
5310|Deception Formation|23250|5|Briefly described|p1124 Fig.2||Late Cambrian|Correlate of Lake Frome Group.||||||
5310|Deception Formation|23361|5|Briefly described|16 Fig.4|Cambrian|Neoproterozoic III|||||||
5310|Deception Formation|29721|6|Mentioned|p44|||||||||
5310|Deception Formation|33307|6|Mentioned|Fig.6|||||||||
5310|Deception Formation|34186|6|Mentioned|Fig.3|||See also Fig.4. Cambrian.||||||
5310|Deception Formation|34442|5|Briefly described|Table 1|||Cambrian||||||
5310|Deception Formation|35102|6|Mentioned|Fig.2|||||||||
5310|Deception Formation|36198|6|Mentioned|p294|||See also Fig.III.2||||||
5310|Deception Formation|39213|6|Mentioned|Fig.6|||Amadeus Basin Succession||||||
5310|Deception Formation|40254|6|Mentioned|Fig.7|||||||||
5310|Deception Formation|40740|3|Fully described|p43|||Mention p5.||||||08-AUG-06
5310|Deception Formation|40810|6|Mentioned|p3|||||||||
5310|Deception Formation|41039|6|Mentioned|Fig.2|||||||||
5310|Deception Formation|41190|6|Mentioned|Fig.4|||||||||
5310|Deception Formation|41224|6|Mentioned|Fig.2|||||||||
5310|Deception Formation|41270|6|Mentioned|Table 1|||||||||
5310|Deception Formation|41717|6|Mentioned|Fig.2|||||||||
5310|Deception Formation|41723|6|Mentioned|Map legend|Neoproterozoic||||||||
5310|Deception Formation|42082|6|Mentioned|Fig.3 P323|||||||||
5310|Deception Formation|42940|5|Briefly described|Plate 8|||See also Plate 12.||||||
5310|Deception Formation|43225|5|Briefly described|Map Legend||Cambrian|Of Pertaoorrta Group.||||||08-AUG-06
5310|Deception Formation|43503|6|Mentioned|12-50|Mindyallan|Undillan|||||||
5310|Deception Formation|43649|6|Mentioned|p457|||||||||
5310|Deception Formation|44395|14|Not recorded|p.8||Cambrian|Correlates with Cleland Sandstone.||||||
5310|Deception Formation|44402|5|Briefly described|map legend||Cambrian|Part of Pertaoorrta Group.||||||02-DEC-04
5310|Deception Formation|44484|14|Not recorded|p.10, Tb.1||Cambrian|Part of Pertaoorrta Group.||||||
5310|Deception Formation|44485|14|Not recorded|map legend||Cambrian|Part of Pertaoorrta Group.||||||
5310|Deception Formation|44497|5|Briefly described|p.10, Table 1||Cambrian|SF/53-13.||||||
5310|Deception Formation|44498|14|Not recorded|map legend||Cambrian|Part of Pertaoorrta Group.||||||
5310|Deception Formation|44505|14|Not recorded|p.7, Table 1||Cambrian|Of Pertaoorrta Group.||||||
5310|Deception Formation|44506|14|Not recorded|map legend||Cambrian|||||||
5310|Deception Formation|45041|4|Described|p53|||M.Camb.||||||
5310|Deception Formation|45170|6|Mentioned|Table 3|||||||||
5310|Deception Formation|48863|2|Defined|p22||Middle Cambrian|Tb.1. opp.p.7,9,20,24,Pl.10,15,16. Middle Cambrian. (G52-4,G53-1).||||||08-JUN-21
5310|Deception Formation|48865|14|Not recorded|Fig.4.opp.p.10|||(G52-4,F53-13).||||||
5310|Deception Formation|48963|6|Mentioned|Fig.3|||||||||
5310|Deception Formation|60674|5|Briefly described|Map legend|Cambrian|Cambrian|Of the Pertaoorrta Group. Red-brown micaceous siltstone; interbeds of sandstone, dolostone and limestone. Geological Province: Amadeus Basin.||||||23-DEC-09
5310|Deception Formation|61309|5|Briefly described|p16 Fig. 4|||Geological Province: Amadeus Basin.||||||06-FEB-08
5310|Deception Formation|61385|5|Briefly described|Map legend|Cambrian|Cambrian|White crystalline dolomite with chert nodules and bands, some dolomitic limestone. Geological Province: Amadeus Basin.||||||06-FEB-08
5310|Deception Formation|61518|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Pertaoorta Group. Red-brown micaceous siltstone, interbeds of sandstone, dolostone and limestone. Geological Province: Amadeus Basin.||||||23-DEC-09
5310|Deception Formation|61732|5|Briefly described|p99|Cambrian|Cambrian|Together with other Cambrian units overlies the Arumbera Sandstone.||||||07-FEB-11
5310|Deception Formation|67565|5|Briefly described|p40, p47.|||A recessive unit in the Gardiner Range. Thickness to 175 m. Lateral equivalent of Hugh River Shale.||||Conformably overlies Illara Sandstone. Is overlain conformably by Petermann Sandstone.|Red-brown micaceous siltstone, with minor interbeds of red-brown, fine-grained micaceous sandstone, dolostone and limestone; some lower beds are bioturbated.|
5310|Deception Formation|67856|6|Mentioned|p338 fig 4-30|Cambrian|Cambrian|||Of Pertaoorta Group.||||
5310|Deception Formation|69437|5|Briefly described|p22:10|Series 3|Series 3|Amadeus Basin.||||Overlies Illara Sandstone. Is overlain by Goyder Formation.||12-JUL-16
5310|Deception Formation|71114|5|Briefly described|p171, p170 fig 1b, p175-177, p180|Guzhangian||Amadeus Basin western succession. Deposited between ~511 and 490 Ma. Deposited under lacustrine, evaporitic conditions in the central basin, while it reflects deposition on a fluvial floodplain or delta in the western part||||Overlies Illara Sandstone. Is overlain by Petermann Sandstone.||14-FEB-18
5310|Deception Formation|71279|5|Briefly described|p355 Fig.2|Middle Cambrian|Middle Cambrian|Amadeus Basin.||Pertaoorrta Group.||||
5310|Deception Formation|71898|4|Described|iii, p1, p3, p11-p14, p16|Late Cambrian|Middle Cambrian|Amadeus Basin. Originally defined by Wells et al (1965). Outcrops in the AREYONGA (5439) map sheet in the Gardiner, Walker Creek Petermann Creek and Parana Hill anticlines. SHRIMP age is interpreted to be a maximum depositional age. Sample location, description at location, zircon morphology, SHRIMP analysis, results and methods are discussed. This unit has a maximum thickness of 180m in the Gardiner Range. Interpreted to represent part of a prograding fluvial-deltaic system.|516 +/- 11 Ma (SHRIMP U-Pb)|Pertaoorrta Group||Conformably overlies the Illara Sandstone. Conformably overlain by and interfingers with the Petermann Sandstone.|Red micaceous siltstone, shale, micaceous quartz sandstone, dolostone and limestone and fine-grained sandstone.|19-NOV-18
5310|Deception Formation|72358|6|Mentioned|p118|Series 3|Series 3|Of Amadeus Basin.||||||
5310|Deception Formation|72374|6|Mentioned|p15|||Of Amadeus Basin.||||Partially laterally equivalent to Illara Sandstone.||
5354|Delny Gneiss|33103|4|Described|Table 1|||Mention p14.||||||08-AUG-06
5354|Delny Gneiss|33104|6|Mentioned|Map legend|Precambrian|Precambrian|||||||
5354|Delny Gneiss|39887|6|Mentioned|Fig.5|||||||||
5354|Delny Gneiss|40906|6|Mentioned|p8|||||||||
5354|Delny Gneiss|46868|6|Mentioned|Fig.2|||||||||
5354|Delny Gneiss|48992|6|Mentioned|p10|||||||||
5354|Delny Gneiss|50369|6|Mentioned|p9.2|||Intruded by Copia Granite.||||||
5354|Delny Gneiss|61208|5|Briefly described|p208|||Unconformably overlain by Ledan Schist. ||||||
5354|Delny Gneiss|61388|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Meta-sedimentary gneiss, schist, amphibolite, minor quartzite, rare calcsilicate gneiss; abundant pegmatite intrusions. Geological Province: Arunta Region.||||||07-NOV-08
5354|Delny Gneiss|65341|5|Briefly described|p4. |||||||Intruded by Crooked Hole Granite and probably by Woodgreen Granite Complex.|Muscovite-biotite schist, felsic gneiss, amphibolite, minor quartzite; rare calc-silicate rock.|
5354|Delny Gneiss|69427|6|Mentioned|p12:12|||Shaw and Warren (1975); subsequently the Delny Metamorphics (Haines and Scrimgeour, 2007).||||||12-JUL-16
5379|Depot Creek Sandstone|9324|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Tolmer Group. Quartz arenite, thick bedded medium to coarse grained.||||||
5379|Depot Creek Sandstone|14019|5|Briefly described|p4 Fig. 3|||Base of the Tolmer Group. Unconformably overlies the Umbrawarra Leucogranite (Pine Creek Geosyncline).||||||19-AUG-09
5379|Depot Creek Sandstone|22809|4|Described|15|||Of the Tolmer Group.Overlying unit: Stray Creek Sandstone; underlying unit: Allia Creek Granite.||||||08-AUG-06
5379|Depot Creek Sandstone|22810|4|Described|Table3 P7, P18||Proterozoic|Unconformably overlies Waterhouse Complex.||||||07-JAN-09
5379|Depot Creek Sandstone|22813|5|Briefly described|Map|Mesoproterozoic|Mesoproterozoic|Overlain by the Stray Creek Sandstone. Part of the Tolmer Group. Pink orthoquartzite and quartz sandstone.||||||08-AUG-06
5379|Depot Creek Sandstone|23714|5|Briefly described|p36|Proterozoic|Proterozoic|Of Tolmer Group.||||||
5379|Depot Creek Sandstone|23715|5|Briefly described|Map legend||Proterozoic|In the Litchfield Province and Central Region||||||
5379|Depot Creek Sandstone|23822|5|Briefly described|p299|Proterozoic|Proterozoic|Geological Province: Litchfield Province.||||||
5379|Depot Creek Sandstone|24001|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Pink orthoquartzite and sandstone, commonly ripple marked.||||||
5379|Depot Creek Sandstone|24047|5|Briefly described|p40|Mesoproterozoic|Mesoproterozoic|Geological Province: Victoria-Birrindudu Basin.||||||
5379|Depot Creek Sandstone|24122|5|Briefly described|p4 Fig.3|||Of Tolmer Group. Geological Province: Birrindudu Basin.||||||19-AUG-09
5379|Depot Creek Sandstone|24297|5|Briefly described|p4 Fig.3|Proterozoic|Proterozoic|Of Tolmer Group. Geological Province: Birrindudu Basin.||||||19-AUG-09
5379|Depot Creek Sandstone|24441|5|Briefly described|p1 Fig. 1|||Of the Tolmer Group. Unconformably overlies Pine Creek Geosyncline. Overlain by Stray Creek Sandstone. Geological Province: Birrindudu Basin.||||||19-AUG-09
5379|Depot Creek Sandstone|24442|5|Briefly described|p50 Fig. 1|||Of the Tolmer Group. Geological Province: Birrindudu Basin.||||||19-AUG-09
5379|Depot Creek Sandstone|32700|6|Mentioned|p14|||Now Auvergne Gp.||||||
5379|Depot Creek Sandstone|39679|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
5379|Depot Creek Sandstone|40168|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Tolmer Group. Laminated to thickly bedded, pink to brown, medium to coarse quartz sandstone and minor pebbly quartz sandstone, quartzite.||||||18-OCT-05
5379|Depot Creek Sandstone|40495|6|Mentioned|Fig.5|||||||||
5379|Depot Creek Sandstone|40808|4|Described|p17|||||||||
5379|Depot Creek Sandstone|40809|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
5379|Depot Creek Sandstone|40856|6|Mentioned|p311|||||||||
5379|Depot Creek Sandstone|40957|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
5379|Depot Creek Sandstone|41304|6|Mentioned|Map legend|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
5379|Depot Creek Sandstone|41305|4|Described|p20|||||||||
5379|Depot Creek Sandstone|41586|6|Mentioned|Map legend|Mesoproterozoic||||||||
5379|Depot Creek Sandstone|41660|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of Tolmer Group. Quartz arenite, massive to thickly bedded; rare, thin, quartz pebble layers; thin basal conglomerate in places. Thickness: ~ 400m.||||||07-OCT-05
5379|Depot Creek Sandstone|41661|3|Fully described|p18|||||||||
5379|Depot Creek Sandstone|42012|4|Described|p13|||||||||
5379|Depot Creek Sandstone|42014|5|Briefly described|Map legend|Mesoproterozoic||||||||
5379|Depot Creek Sandstone|42070|6|Mentioned|Fig.3 P4|||||||||
5379|Depot Creek Sandstone|43140|4|Described|p4||Mesoproterozoic|Of Tolmer Group.||||||08-AUG-06
5379|Depot Creek Sandstone|43187|5|Briefly described|p2|||||||||
5379|Depot Creek Sandstone|43624|6|Mentioned|p37||Neoproterozoic|||||||
5379|Depot Creek Sandstone|43832|4|Described|29,Table7 p27, 97||Mesoproterozoic|||||||
5379|Depot Creek Sandstone|46658|6|Mentioned|p560|||||||||
5379|Depot Creek Sandstone|50623|5|Briefly described|p260 Fig.3, p261|Statherian|Statherian|Age: 1720-1700 Ma. Correlated with upper part of Katherine River Group. Shallow marine platform sandstone.||||||07-DEC-04
5379|Depot Creek Sandstone|60685|5|Briefly described|p4 Fig. 3|||Of the Tolmer Group. Geological Province: Birrindudu Basin.||||||
5379|Depot Creek Sandstone|61389|5|Briefly described|Map Legend|||Of the Tolmer Group. Pink orthoquartzite & quartz sandstone, quartz pebble conglomerate lenses.||||||
5379|Depot Creek Sandstone|64698|4|Described|lithinterp table|Statherian|Orosirian|Age ~1700-1825Ma. Of Tolmer Group. Max. thickness 1500m. Pink quartz sandstone, quartz pebble conglomerate lenses; Silica cemented quartz sandstone, minor siltstone and pebble conglomerate. Overlain by Stray Creek Sandstone.||||||
5379|Depot Creek Sandstone|65232|5|Briefly described|p51-52, p57, p63|Statherian|Statherian|Over Geolsec Formation. Mount Partridge Group rocks are overthrusted. Unconformable base. Correlated with upper part of Katherine River Group gives depositional age of 1720-1700 Ma. Fluvial platform-cover sandstone; conglomerate. Quartz breccia with hematitic matrix marks basal boundary with Geolsec Formation.||||||12-APR-12
5379|Depot Creek Sandstone|65339|6|Mentioned|p14.|||||Unit in Tolmer Group.||||
5379|Depot Creek Sandstone|65342|6|Mentioned|p11 Fig.13. |||Birrindudu Basin.||Unit in Tolmer Group.||Is overlain by Stray Creek Sandstone.||
5379|Depot Creek Sandstone|67167|5|Briefly described|Map legend.|||||Unit in Tolmer Group.|||Quartz sandstone, quartz pebble conglomerate lenses, commonly ripple marked.|
5379|Depot Creek Sandstone|67186|5|Briefly described|Map legend.|||||Unit in Tolmer Group.||Is overlain by Stray Creek Sandstone.|Quartz sandstone, quartz pebble conglomerate lenses, commonly ripple marked.|23-NOV-11
5379|Depot Creek Sandstone|67355|5|Briefly described|p7 Fig. 5, p14, p16, p60, p67, p69||late Paleoproterozoic|Gently dipping to horizontal. The absolute age is unknown. Shallow marine.|1700 - 1740 Ma?|Tolmer Group||Overlies the Burrell Creek Formation. Correlated with the upper Katherine River Group.|Consists of pink, fine to coarse, rippled quartz sandstone and thin conglomerate lenses and beds.|25-JAN-17
5379|Depot Creek Sandstone|67479|5|Briefly described|p2 Tb.1, p15-18, p58, p63 Tb.5, p64 Tb.5|Orosirian|Orosirian|Maximum depositional age.|1837 +/- 15 Ma|Of the Tolmer Group.||Conformably overlain by the Stray Creek Sandstone.|Foliated greenschist-facies psammite.|24-JAN-17
5379|Depot Creek Sandstone|67779|5|Briefly described|p6 Fig.5.|Paleoproterozoic|Paleoproterozoic|Litchfield Province, Pine Creek Orogen.||Unit in Tolmer Group.||||
5379|Depot Creek Sandstone|68575|6|Mentioned|p125|||Western Pine Creek Orogen. Age distribution is remarkably similar to other basal McArthur Basin clastics (eg Kombolgie Subgroup; Westmoreland Conglomerate).||Tolmer Group.||||
5379|Depot Creek Sandstone|68733|6|Mentioned|p186||Orosirian|Maximum depositional age of ca. 1830 Ma.|Maximum depositional age of ca. 1830 Ma.|Basal Tolmer Group.||||05-DEC-17
5379|Depot Creek Sandstone|69420|4|Described|p5:14, 76, 105, 116|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin. SHRIMP U-Pb zircon "conservative" maximum depositon age.|1837 +/- 15 Ma: Carson et al. (2010).|Tolmer Group.||Unconformably overlies Geolsec Formation.|Sandstone and conglomerate.|12-JUL-16
5379|Depot Creek Sandstone|69432|4|Described|p17:2, 5|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin. Formerly a Member of the Buldiva Sandstone (Walpole et al., 1968); raised to Formation status by Dundas et al. (1987). The name Buldiva Sandstone is now abandoned. Paralic becoming tidal shallow-marine deposits.||Tolmer Group.||Is overlain conformably by Stray Creek Sandstone.|Cross-bedded and ripple-marked, medium- to coarse-grained sandstone, conglomerate and orthoquartzite.|12-JUL-16
5379|Depot Creek Sandstone|69673|6|Mentioned|p48 fig 35|||||Tolmer Group||Overlain by Stray Creek Sandstone||
5379|Depot Creek Sandstone|70866|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Tolmer Group.||Is overlain conformably by Stray Creek Sandstone.|Massive cross-bedded quartz sandstone, commonly ripple-marked; quartzite, quartz-pebble conglomerate lenses.|
5379|Depot Creek Sandstone|71302|5|Briefly described|p6|Paleoproterozoic|Paleoproterozoic|Of Birindudu Basin.||Unit of Tolmer Group.||||
5379|Depot Creek Sandstone|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|1837+/-15 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
5434|Devils Marbles Granite|22446|6|Mentioned|p29|Statherian|Statherian|||||||
5434|Devils Marbles Granite|23733|5|Briefly described|p15|Paleoproterozoic|Paleoproterozoic|Of Devils Suite. See also p32 Fig.19, p34 Fig.20.  Geological Province: Davenport Province.||||||07-NOV-08
5434|Devils Marbles Granite|23809|5|Briefly described|p27 Fig. 25|||Geological Province: Davenport Province.||||||
5434|Devils Marbles Granite|24089|5|Briefly described|p27 Fig. 15|||||||||14-NOV-06
5434|Devils Marbles Granite|24197|5|Briefly described|p28, p68 Tb. 6.1|Paleoproterozoic|Paleoproterozoic|Of the Devils Suite. Age: ~1710Ma. Geological Province: Tennant Creek/Davenport Province.||||||07-FEB-11
5434|Devils Marbles Granite|40578|5|Briefly described|Map legend|Proterozoic|Proterozoic|Porphyritic muscovite-biotite and biotite granite.  Age: ~1640Ma?  Intrudes the Kurinelli Sandstone.||||||10-JAN-05
5434|Devils Marbles Granite|41204|4|Described|p12|||Mention p3.||||||08-AUG-06
5434|Devils Marbles Granite|41205|5|Briefly described|Map legend|Proterozoic|Proterozoic|Porphyritic muscovite-biotite granite.||||||16-NOV-05
5434|Devils Marbles Granite|41408|6|Mentioned|Map legend|Proterozoic||||||||
5434|Devils Marbles Granite|41970|6|Mentioned|p336|||||||||
5434|Devils Marbles Granite|42504|5|Briefly described|Table 3 P60|||||||||
5434|Devils Marbles Granite|42754|6|Mentioned|p3|||||||||
5434|Devils Marbles Granite|43751|6|Mentioned|p6131|||Biotite K-Ar ages: 1680+/-35 Ma||||||
5434|Devils Marbles Granite|43802|6|Mentioned|p78|||||||||
5434|Devils Marbles Granite|45167|5|Briefly described|p49, Table 2|||Probable age older than reported 1540 Ma.||||||08-AUG-06
5434|Devils Marbles Granite|49033|2|Defined|p30|Proterozoic|Proterozoic|||||||
5434|Devils Marbles Granite|50588|5|Briefly described|p1.4, 4.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Tennant Creek/Davenport Province. Of the Devils Suite. Age: 1711 +/- 11Ma (SHRIMP).||||||07-MAR-13
5434|Devils Marbles Granite|64735|6|Mentioned|p206|||||Of Devils Suite.||||30-APR-12
5434|Devils Marbles Granite|64738|5|Briefly described|p247 Fig.1, p249, p250 Table 1,p257-8|Statherian|Statherian||Crystallised 1711 +/- 11 Ma.|Unit in Devils Suite.||||
5434|Devils Marbles Granite|65209|6|Mentioned|p35 Fig.1, p37|Paleoproterozoic|Paleoproterozoic|Appears [incorrectly] as Devils Marble Granite in Fig.1.||Devils Suite.||||
5434|Devils Marbles Granite|67352|6|Mentioned|p8|Statherian|Statherian|||Devils Suite||||
5434|Devils Marbles Granite|68150|5|Briefly described|p11 Tb.3.2|||Age: SHRIMP, MSWD 1.7, 4 analyses, Page (1996).|1711 +/- 11 Ma, magmatic crystallisation|||||
5434|Devils Marbles Granite|69187|6|Mentioned|p52|Statherian|Statherian||1711 +/- 4 Ma|||||
5434|Devils Marbles Granite|69424|5|Briefly described|p9:28-29|Paleoproterozoic|Paleoproterozoic|Davenport Province.|1711 +/- 4 Ma (Page, 1995).|Devils Suite.||||12-JUL-16
5434|Devils Marbles Granite|69425|4|Described|p10:13, 20-22, 25|||Assigned to the Devils Suite by Wyborn et al. (1998). Davenport Province. Interpreted to post-date the Hatches Creek Group and Davenport Event folding. Associated with W-bearing quartz veins in the Wauchope mineral field. Is associated with greisenisation in Yeeradgi and Kurinelli Sandstones, and has hornfelsed Taragan Sandstone.|1711 +/- 4 Ma (Page, 1995).|Devils Suite.||Intrudes lowermost Unimbra Sandstone.|Pink, medium- to coarse-grained two-mica granite with phenocrystic microcline and subhedral andesine; accessory minerals are fluorite, titanite, apatite, zircon and opaque oxides.|12-JUL-16
5434|Devils Marbles Granite|71592|5|Briefly described|Appendix A.|||Tennant Creek Region.|1711+/-11.0 Ma crystallisation: U-Pb zircon SHRIMP||||Granite.|
5439|Devoncourt Limestone|9830|5|Briefly described|Map Legend|Cambrian|Cambrian|Limestone, calcilutite, marl. Underlies Selwyn Range Limestone, O'Hara Shale. Overlies Roaring Siltstone.||||||30-JAN-07
5439|Devoncourt Limestone|22954|6|Mentioned|Fig3p9|||||||||
5439|Devoncourt Limestone|23182|6|Mentioned|p232|||||||||
5439|Devoncourt Limestone|30479|6|Mentioned|Fig.5|||Stratigraphic relationships||||||
5439|Devoncourt Limestone|30773|6|Mentioned|p266|||Middle Cambrian age||||||
5439|Devoncourt Limestone|30775|6|Mentioned|p1|||||||||
5439|Devoncourt Limestone|30778|6|Mentioned|p14,Fig.5|||||||||
5439|Devoncourt Limestone|30914|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
5439|Devoncourt Limestone|31396|6|Mentioned|Fig.3|||||||||
5439|Devoncourt Limestone|32952|6|Mentioned|p1188|||See also p1189. M.-U. Cambrian||||||08-AUG-06
5439|Devoncourt Limestone|33111|4|Described|p35|||||||||
5439|Devoncourt Limestone|33113|6|Mentioned|Fig.1|||Middle Camb.||||||
5439|Devoncourt Limestone|33482|6|Mentioned|Fig.4|||Middle - Upper Cambrian||||||
5439|Devoncourt Limestone|34287|6|Mentioned|Fig.3|||||||||
5439|Devoncourt Limestone|34903|6|Mentioned|p582|||||||||
5439|Devoncourt Limestone|35054|6|Mentioned|Table 23|||||||||
5439|Devoncourt Limestone|35121|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
5439|Devoncourt Limestone|35139|4|Described|Table.2|||||||||
5439|Devoncourt Limestone|35553|6|Mentioned|p18|||||||||
5439|Devoncourt Limestone|35939|6|Mentioned|p633|||||||||
5439|Devoncourt Limestone|37275|6|Mentioned|p290|||||||||
5439|Devoncourt Limestone|37413|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
5439|Devoncourt Limestone|37572|4|Described|p159|||See also Fig.8||||||
5439|Devoncourt Limestone|37816|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
5439|Devoncourt Limestone|38444|6|Mentioned|p139|||||||||
5439|Devoncourt Limestone|38446|6|Mentioned|Table 23|||||||||
5439|Devoncourt Limestone|38608|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
5439|Devoncourt Limestone|39445|5|Briefly described|Table 4|||See also p62.||||||08-AUG-06
5439|Devoncourt Limestone|39690|6|Mentioned|Table 1|||See also Fig.2||||||
5439|Devoncourt Limestone|40856|5|Briefly described|p313|||||||||
5439|Devoncourt Limestone|41388|6|Mentioned|Fig.2|||||||||
5439|Devoncourt Limestone|41639|6|Mentioned|p3|||||||||
5439|Devoncourt Limestone|42139|6|Mentioned|Fig.18 P90|||||||||
5439|Devoncourt Limestone|42994|6|Mentioned|p3|||||||||
5439|Devoncourt Limestone|43807|6|Mentioned|Fig.2,p347|||||||||
5439|Devoncourt Limestone|43883|14|Not recorded|p18 Fig.4-3|||||||||
5439|Devoncourt Limestone|44091|14|Not recorded|Tb.1,p1||Middle Cambrian|||||||
5439|Devoncourt Limestone|44205|2|Defined|p5,9-17,21-59,65-95,||Middle Cambrian|p107,134,141,161,170-184.||||||
5439|Devoncourt Limestone|44211|2|Defined|p96,100-104|||Overlies sharp but conformable contact on Roaring Siltstone. Overlain by Selwyn Range Limestone.||||||
5439|Devoncourt Limestone|44275|14|Not recorded|Map Legend|||||||||
5439|Devoncourt Limestone|44276|2|Defined|p20,21,Tb.2|||||||||
5439|Devoncourt Limestone|44882|14|Not recorded|p201||Cambrian|Selwyn Range. In French.||||||
5439|Devoncourt Limestone|44920|14|Not recorded|Map Legend, Sheet 4||Middle Cambrian|||||||
5439|Devoncourt Limestone|45002|14|Not recorded|p16,21,24|||||||||
5439|Devoncourt Limestone|45012|14|Not recorded|p8,91,127||Middle Cambrian|||||||
5439|Devoncourt Limestone|45052|3|Fully described|p102|||M.Camb.||||||
5439|Devoncourt Limestone|45079|6|Mentioned|p34|||Cambrian age. Lithology||||||
5439|Devoncourt Limestone|45166|5|Briefly described|Table 15|||||||||
5439|Devoncourt Limestone|47058|6|Mentioned|p134|||||||||
5439|Devoncourt Limestone|48633|14|Not recorded|p96|||Ref. to Opik 1961.||||||
5439|Devoncourt Limestone|48906|14|Not recorded|Tb.1|||||||||
5439|Devoncourt Limestone|48971|6|Mentioned|p9|||See also P11, P30.||||||
5439|Devoncourt Limestone|50100|5|Briefly described|p22|Early Ordovician|Early Cambrian|Hard, flaggy, medium-bedded to laminated, and essentially detrital; trilobite fossils locally.  Conformably overlies the Roaring Siltstone; conformably overlain by Selwyn Range Limestone and O'Hara Shale. ||||||
5439|Devoncourt Limestone|50244|6|Mentioned|p88, p95, p99|Late Cambrian|Late Cambrian|Geological Province: Georgina Basin.||||||21-APR-09
5439|Devoncourt Limestone|60359|5|Briefly described|Map Legend|Cambrian|Cambrian|Limestone, marl, calcilutite.||||||
5439|Devoncourt Limestone|62790|6|Mentioned|p208, 216|Middle Cambrian|Middle Cambrian|Eastern Georgina Basin. Contains the comptalutid Aristaluta gutta Opik, 1961.||||||28-MAR-12
5439|Devoncourt Limestone|63450|5|Briefly described|p78 Fig. 5, p81|Middle Cambrian|Middle Cambrian|Overlies Inca Formation (with hiatus). Conformably overlain by Pomegranate Limestone. Geological province: Georgina Basin, Burke River Structural Belt. Max. thickness (est.): 210m. Bituminous, flaggy limestone.||||||07-FEB-11
5439|Devoncourt Limestone|64068|3|Fully described|p64, 62, 63, 67, 70|Middle Cambrian|Middle Cambrian|Diverse fossil fauna. Correlated with Georgina Limestone, upper Arthur Creek Formation, lower part with Blazan Shale, Quita Formation. Part correlated with Roaring Siltstone. Previously mapped as Thorntonia Limestone (Opik, 1963; Shergold and Druce, 1980).||Of Narpa Group.||Conformably overlies Inca Formation and Roaring Siltstone. Conformably and gradationally overlain by Selwyn Range Limestone and O'Hara Shale.|Interbedded  limestones: laminated, marly, foetid, and nodular; calcareous shale; minor intraformational breccia.|04-APR-12
5439|Devoncourt Limestone|64443|6|Mentioned|p41|||Correlative of Ranken Limestone, Camooweal Dolostone.||||||
5439|Devoncourt Limestone|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map; p83|Middle Cambrian|Middle Cambrian|Burke River Structural Belt, Georgina Basin. Appears as Devencourt Limestone on p83.||Narpa Group.||Overlies Roaring Siltstone conformably and Inca Formation unconformably. Is overlain by Pomegranate Limestone and Selwyn Range Limestone.|Impure limestone, calcilutite, bituminous limestone, marl.|
5439|Devoncourt Limestone|67870|5|Briefly described|p39, p43, p47, p50-53|||Burke River Structural Belt, Georgina Basin.||||Equivalent to the Arthur Creek Formation.||
5439|Devoncourt Limestone|69443|5|Briefly described|p28:16, 24-25|Middle Cambrian|Middle Cambrian|Georgina Basin.||Narpa Group.||Correlated with Ranken Limestone and Camooweal Dolostone.||12-JUL-16
5439|Devoncourt Limestone|69573|6|Mentioned|p659, 661, 666, 668|||Georgina Basin. Intertidal to subtidal environment.||||Passes laterally and vertically (downwards) into Roaring Siltstone.||
5439|Devoncourt Limestone|69591|5|Briefly described|p87, p92-93, p96-97, p98 Fig.2.91|Cambrian|Cambrian|Burke River Structural Belt, Georgina Basin. Up to 215m thick. A noticeable feature is limonite pseudomorphs (after pyrite?) but the hopper crystal habit suggests halite. Has a rich trilobite fauna of the Lejopyge laevigata Zone. Mis-spelt on p87 as Devencourt Limestone.||||Overlies Roaring Siltstone conformably (and passes laterally into it) and, unconformably, Inca Formation. Is overlain by Pomegranate Limestone and locally Selwyn Range Limestone.|Flaggy, thin-bedded limestones including sandy, bituminous and nodular types with the last leaving large thick ellipsoidal nodules up to 25cm in diameter upon weathering. Some fine cross-bedding and a few thin intraformational breccias occur.|
5439|Devoncourt Limestone|72321|6|Mentioned|Fig 2|Guzhangian|Drumian|Burke River Structural Belt, Georgina Basin.  Australian stages:  Undillan to Boomerangian.||of Narpa Group.||||
5439|Devoncourt Limestone|72516|6|Mentioned|p92|Cambrian|Cambrian|Eastern Georgina Basin.||||Equivalent to the Arthur Creek Formation and the Steamboat Sandstone.||03-JUN-21
5439|Devoncourt Limestone|72683|5|Briefly described|Map legend|Cambrian|Cambrian|Georgina Basin.||Narpa Group||Overlies Roaring Siltstone and underlies Selwyn Limestone.|Impure limestone, calcilutite, bituminous limestone and marl.|
5439|Devoncourt Limestone|72684|5|Briefly described|Map legend|Cambrian|Cambrian|Georgina Basin. Overlies the Mitakoodi Domain. Shown as younger than the Isan Orogeny (1590-1500 Ma).||Narpa Group||Overlies Roaring Siltstone and underlies  Selwyn Range Limestone.|Impure limestone, calcilutite, bituminous limestone and marl.|
5439|Devoncourt Limestone|73418|5|Briefly described|p4 Fig.3|Miaolingian|Miaolingian|Georgina Basin, Burke River Structural Belt.||Narpa Group||Overlies Inca Formation, Roaring Siltstone, underlies Selwyn Range Limestone|Limestone.|
5539|Djabura Formation|42058|4|Described|p116|||||||||
5539|Djabura Formation|62506|5|Briefly described|p1-2|Devonian|Devonian|Of the Arafura Group. Thickness: 466m. Sandstone, siltstone, calcareous in part. ||||||
5539|Djabura Formation|62510|5|Briefly described|p3|Late Devonian|Late Devonian|||||||
5539|Djabura Formation|63062|5|Briefly described|p9 Fig. 9, p48 Tb. 1|Late Devonian|Late Devonian|Basal unit of the Arafura Group. Unconformably overlain by Yabooma Formation. Geological Province: Arafura and Money Shoal Basins. Mainly shallow marine deposits - interbedded clastics and minor limestone.||||||07-FEB-11
5539|Djabura Formation|69297|5|Briefly described|p283, p285|Frasnian|Frasnian|Arafura Basin. Deposited in a shallow marine environment. ||Arafura Group||Overlain by the Yabooma Formation.|Interbedded clastics and minor limestone.|
5539|Djabura Formation|69451|4|Described|p35:3-4, 8; 35:13 Fig.35.9|Late Devonian|Late Devonian|Bradshaw et al. (1990). Arafura Basin (offshore). Nearshore shallow-marine deposits. 295-466m thick. Conodonts indicate an early Famennian age; palynological data indicate Frasnian.||Arafura Group.||Unconformably overlies Mooroongga Formation (Goulburn Group). Is overlain unconformably by Yabooma Formation or Kulshill Group.|Interbedded mudstone, siltstone, sandstone and minor carbonate rocks; diverse fossil fauna including conodonts, ostracods, phosphatic brachiopods, conulariids and fish fossils; palynoflora.|12-JUL-16
5539|Djabura Formation|69673|6|Mentioned|p197|||||Arafura Group||||
5539|Djabura Formation|70098|4|Described|p5, p8, p19 Fig.5|Late Devonian|Late Devonian|Conodont biostratigraphy indicates an early Famennian age for the Djabura Formation (Nicoll, 2006), but palynological dating suggests that it is older (Frasnian; Purcell, 2006). Depositional Environment: dominantly shallow marine.||Arafura Group||Is unconformably overlain by Yabooma Formation. ?Unconformably overlies Mooroongga Formation.|Succession of interbedded clastics and minor limestone.|
5548|Dneiper Granite|9394|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Strongly foliated biotite granite or orthogneiss, minor hornblende granite. Geological Province: Arunta Block.||||||05-NOV-04
5548|Dneiper Granite|23363|5|Briefly described|351 Tab.2|Statherian|Statherian|1771+/-15Ma U/Pb SHRIMP pooled age. Magmatic crystallisation or emplacemnet age.||||||03-FEB-20
5548|Dneiper Granite|23732|5|Briefly described|p3, p15, p32|Paleoproterozoic|Paleoproterozoic|Age: 1771 +/- 15Ma (SHRIMP U-Pb; Zhao and Bennett, 1995) and 1770Ma.||||||07-NOV-08
5548|Dneiper Granite|23733|5|Briefly described|p34 Fig.20|||||||||
5548|Dneiper Granite|23868|5|Briefly described|p741|Paleoproterozoic|Paleoproterozoic|Age: 1771+/-15Ma.  Geological Province: Arunta Inlier.||||||07-NOV-08
5548|Dneiper Granite|24197|5|Briefly described|p60 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Of the Jervois ?Suite (Jervois presented in Table 4.1 in isolation). Age: ~1771Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
5548|Dneiper Granite|39888|6|Mentioned|Fig.7|||||||||
5548|Dneiper Granite|40538|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
5548|Dneiper Granite|40906|4|Described|p12|||||||||
5548|Dneiper Granite|42326|5|Briefly described|Table 2 P11|||||||||
5548|Dneiper Granite|44327|14|Not recorded|Tb.I,p.7||Paleoproterozoic|(F53-11). Lower Proterozoic.||||||07-NOV-08
5548|Dneiper Granite|44328|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
5548|Dneiper Granite|46868|6|Mentioned|p76|||||||||
5548|Dneiper Granite|48844|14|Not recorded|p.14,Pl.8|||Intrudes Arunta Complex.||||||
5548|Dneiper Granite|49036|2|Defined|p8|Proterozoic|Proterozoic|E to Mid-Proterozoic. Previously mapped as Arunta Complex. Mention p7.||||||09-AUG-06
5548|Dneiper Granite|50369|5|Briefly described|p1.4, 9.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Jervois Suite. Age: 1771 +/- 15Ma (SHRIMP).||||||07-MAR-13
5548|Dneiper Granite|64738|5|Briefly described|p247 Fig.2, p249, p250 Table 1.|Paleoproterozoic|Paleoproterozoic|A sample contained two metamorphic zircons aged c.1670 Ma. Metamorphosed 1670 +/- 42 Ma.||||Intruded by Mount Swan Granite.||23-APR-12
5548|Dneiper Granite|67181|5|Briefly described|p631|Statherian|Statherian|Of the Main Group (geochemical grouping) of Arunta Region felsic magmatism.|1771 +/- 15 Ma|||||
5548|Dneiper Granite|68150|5|Briefly described|p4, p11 Tb.3.2, p19|||Studies by Zhao and Bennett (1995) indicated that Jervois Granite (and Dneiper Granite) were some 100 m.y. younger than Barramundi Association, but Dneiper Granite is intruded by an unnamed biotite granite SHRIMP dated at 1805 +/-4 Ma (p4).|1670 +/- 42 Ma, metamorph'm, Zhao and Bennett 1995|||||30-SEP-15
5548|Dneiper Granite|69427|5|Briefly described|p12:3, 29-30, 40, 55|Statherian|Statherian|Shaw et al. (1984); Freeman (1986). Mopunga Range region, Aileron Province. Hosts the Perenti Cu prospect. SHRIMP U-Pb zircon age.|1771 +/- 15 Ma (Zhao and Bennett, 1995).||||Grey, biotite-rich, strongly foliated granite containing ubiquitous small xenoliths of biotite-rich rock, quartzite and calc-silicate.|12-JUL-16
5548|Dneiper Granite|69925|5|Briefly described|p17-18, 21, 24-25, 33-39|||Northern Arunta Province, Arunta Inlier. Considered the oldest granite in the region. Ion probe U-Pb isotope analyses tabulated.|1771 +/- 15 Ma (crystallisation).|||Is intruded by Mount Swan Granite. Correlated with Copia and Crooked Creek Granites.|Grey, biotite-rich gneissic granite, locally hornblende-bearing; numerous small xenoliths. Deformed.|
5548|Dneiper Granite|69931|6|Mentioned|p269, 274, 280, 296|Paleoproterozoic|Paleoproterozoic|Arunta Inlier. REE analyses, Sm-Nd isotopic analyses, tabulated.||Dneiper suite.|||Foliated tonalite.|
5548|Dneiper Granite|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen.|1771+/-15 Ma (crystallisation: U-Pb zircon SHRIMP)||||Strongly-foliated biotite-rich tonalitic gneiss.|
5548|Dneiper Granite|71750|5|Briefly described|iii,p6|Statherian|Statherian|Geological province: Aileron Province. Surrounds and intrudes Perenti Metamorphics. SHRIMP 207Pb/206Pb zircon age of 1771+\-15 Ma (Zhao and Bennett 1995).|1771+/-15 Ma.|||Intrudes Perenti Metamorphics.||20-SEP-19
5548|Dneiper Granite|72516|6|Mentioned|p192|||Aileron Province.||||Intrudes the Perenti Metamorphics.||
5548|Dneiper Granite|73123|6|Mentioned|piii, p5, p8|Orosirian|Orosirian|A SHRIMP zircon magmatic crystallisation age of 1771 +/- 15 Ma for this unit is not considered robust. An unnamed granite 'Pgk' was interpreted to be from this unit and yielded an igneous crystallisation age of 1805 +/- 4 Ma. Also possibly represented by granites in the Macdonald Downs map area with magmatic crystallisation ages of 1810 +/- 4 Ma and 1802 +/- 8 Ma.|ca 1805 Ma|Black Label Suite||||
5548|Dneiper Granite|73591|5|Briefly described|piv, p2, p27-29, p31|Statherian|Orosirian|Aileron Province. Previous SHRIMP U-Pb zircon ages of 1802 +/- 8 Ma and 1810 +/- 4 Ma reported by Kositcin et al. (2011, 2014). Analysed for Lu-Hf isotopes.|1810 +/- 4 Ma, 1802 +/- 8 Ma U-Pb SHRIMP|Black Label Suite|||Includes biotite granite.|
5608|Donnegan Member|22538|6|Mentioned|Fig3 P709|||||||||
5608|Donnegan Member|22664|6|Mentioned|35,39 fig 4,|Paleoproterozoic|Paleoproterozoic|Lynott Formation, Batten Subgroup, McArthur Basin. Also on pages 40 fig 5, 41 & 46||||||07-NOV-08
5608|Donnegan Member|22853|4|Described|22|Proterozoic|Proterozoic|Of Lynott Formation. Max thickness 120 m.||||||09-AUG-06
5608|Donnegan Member|23396|5|Briefly described|p413|||Of Lynott Formation. Geological Province: McArthur Basin.||||||09-AUG-06
5608|Donnegan Member|23398|5|Briefly described|p443|||Of Lynott Formation.||||||
5608|Donnegan Member|23776|5|Briefly described|p705 Fig 2.|||Possibly of the Lynott Formation. Of Batten Subgroup.||||||
5608|Donnegan Member|23902|4|Described|p1568 Fig.2|||Of the Lynott Formation (Batten Subgroup). Overlies the Hot Spring Member. Overlain by the Yalco Formation. Geological Province: McArthur Basin||||||
5608|Donnegan Member|23963|5|Briefly described|p1239 Fig.2|||Geological Province: McArthur Basin. Of the Lynott Formation.||||||
5608|Donnegan Member|32658|3|Fully described|Table 2|||See also Fig. 3.||||||09-AUG-06
5608|Donnegan Member|33666|6|Mentioned|p528|||Table 1.||||||
5608|Donnegan Member|37568|5|Briefly described|p79|||||||||
5608|Donnegan Member|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
5608|Donnegan Member|40691|6|Mentioned|Fig.4|||||||||
5608|Donnegan Member|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
5608|Donnegan Member|41220|6|Mentioned|p367|||||||||
5608|Donnegan Member|41268|5|Briefly described|Fig.10|||||||||
5608|Donnegan Member|42385|4|Described|p22|||See also Table 4 p16.||||||09-AUG-06
5608|Donnegan Member|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
5608|Donnegan Member|42638|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Age: Middle Proterozoic.||Of Lynott Formation.||In schematic section, underlies Yalco Formation; overlies Hot Spring Member (Lynott Formation).|Siltsone, dolomitic sandstone and sandy dolarenite.|09-NOV-11
5608|Donnegan Member|42639|4|Described|p32, Table 5 p20|||||||||
5608|Donnegan Member|42700|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
5608|Donnegan Member|42739|5|Briefly described|map legend|Statherian|Statherian|Of the Lynott Formation. Dolomitic mudstone, fine to coarse grained dolomitic sandstone and lesser sandy dolarenite; thin bedded, cross bedded.||||||19-OCT-05
5608|Donnegan Member|42812|4|Described|p41, Table 4|||Of Lynott Formation.||||||09-AUG-06
5608|Donnegan Member|42935|6|Mentioned|p529 Fig.2|||Of Lynott Formation.||||||09-AUG-06
5608|Donnegan Member|43036|5|Briefly described|p54|||Of Lynott Formation.||||||09-AUG-06
5608|Donnegan Member|44287|2|Defined|p.11, opp.9||Mesoproterozoic|Of McArthur Group. Sandstone and dolomitic sandstone band at top of Lynott Formation. M.Prot. Defn. on Tech.File E/53-3.||||||09-AUG-06
5608|Donnegan Member|44288|14|Not recorded|map legend|||Quartz sandstone, dolomitic sandstone. Lower (?) Proterozoic.||||||
5608|Donnegan Member|45162|4|Described|p116|||||||||
5608|Donnegan Member|60483|5|Briefly described|p7 Fig. 5|||Of Lynott Formation (Batten Subgroup, McArthur Group). Age: 1636+/-4Ma. Geological Province: McArthur Basin.||||||05-OCT-07
5608|Donnegan Member|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Lynott Formation.||||||03-JUN-09
5608|Donnegan Member|64815|6|Mentioned|p4 Fig.2 |||||Unit in Lynott Formation.||||
5608|Donnegan Member|64817|6|Mentioned|p353 Fig.4 |||||Unit in Lynott Formation.||||
5608|Donnegan Member|65228|6|Mentioned|Figs.02, 22.|||||Top unit in Lynott Formation.||Overlies Hot Spring Member. Is overlain by Yalco Formation.||
5608|Donnegan Member|69430|4|Described|p15:3, 16, 19|||Jackson et al. (1987). Southern McArthur Basin. 0-134m thick. Peritidal, supratidal to sabkha deposits on a stable platform. Sampled near top of unit for geochronology.|1636 +/- 4 Ma (Page et al., 2000).|Lynott Formation.||Conformably and gradationally overlies Hot Spring Member. Is overlain conformably by Yalco Formation.|Red-brown to buff, dolomitic siltstone, fine- to coarse-grained dolomitic sandstone and dolarenite; thinly to medium bedded, commonly rippled and cross-bedded; small botryoidal quartz nodules (cauliflower chert and enterolithic chert).|14-DEC-17
5608|Donnegan Member|69673|6|Mentioned|p16 fig 13|||Batten Fault Zone||Lynott Formation||Overlies Hot Spring Member, conformably overlain by Yalco Formation||
5608|Donnegan Member|71374|6|Mentioned|p9|||McArthur Basin.||Lynott Formation||Conformably overlain by the Yalco Formation.||04-MAY-18
5608|Donnegan Member|72248|5|Briefly described|p147|||Of McArthur Basin.||Unit of Lynott Formation.||||
5608|Donnegan Member|72718|6|Mentioned|p7|||Southern McArthur Basin. Batten Fault Zone.||Lynott Formation, Batten Sub-group, McArthur Group||Underlain by Hot Spring Member. Overlain by Yalco Formation.||
5617|Dook Creek Formation|22538|6|Mentioned|Fig3 P708|||||||||
5617|Dook Creek Formation|22600|4|Described|Map legend|Calymmian|Calymmian|||||||
5617|Dook Creek Formation|23216|5|Briefly described|p30,32|||||||||
5617|Dook Creek Formation|23374|3|Fully described|Tb2p10,18,19,5,6,20,30,34,35|Calymmian||Of Mount Rigg Group, McArthur Basin.||||||09-AUG-06
5617|Dook Creek Formation|23396|5|Briefly described|p 407 fig.2|||Of Mount Rigg Group.||||||09-AUG-06
5617|Dook Creek Formation|23937|3|Fully described|p14. p24-25 Tb. 2|Calymmian|Statherian|Of the Mount Rigg Group.  Overlain unconformably by Limmen Sandstone; overlies conformably the Jamberline Sandstone Member.  Divided into Units 1 and 2, Jamberline Sst Member and Unit 4 for the purpose of description.  Geological Province: McArthur Basin.||||||27-OCT-04
5617|Dook Creek Formation|24048|4|Described|p68|Mesoproterozoic|Mesoproterozoic|Of Mount Rigg Group.  Geological Province: McArthur Basin.||||||09-AUG-06
5617|Dook Creek Formation|24049|5|Briefly described|Map Legend|Calymmian|Calymmian|Of Mount Rigg Group. Chert: blue-grey to brown, altered carbonate containing relict stromatolites, ooids and intraclast breccia. Geol. Prov: McArthur Basin.||||||13-OCT-05
5617|Dook Creek Formation|24050|3|Fully described|p34, p9 Tb. 2|Mesoproterozoic|Paleoproterozoic|Of Mount Rigg Group.  Siltstone, sandstone, dolostone.  Overlies Bone Creek Sandstone; underlies disconformably or with angular unconformity the Limmen Sandstone.  Max. thickness: 600m.||||||07-NOV-08
5617|Dook Creek Formation|24051|5|Briefly described|Map Legend|Calymmian|Statherian|Of Mount Rigg Group. Geological Province: McArthur Basin.||||||23-DEC-09
5617|Dook Creek Formation|30318|6|Mentioned|p327|||||||||
5617|Dook Creek Formation|32660|5|Briefly described|Table 4|||||||||
5617|Dook Creek Formation|32722|6|Mentioned|p58|||Adelaidean||||||
5617|Dook Creek Formation|32723|6|Mentioned|p99|||||||||
5617|Dook Creek Formation|35114|6|Mentioned|p204|||||||||
5617|Dook Creek Formation|37568|6|Mentioned|p79|||||||||
5617|Dook Creek Formation|37569|6|Mentioned|p90|||||||||
5617|Dook Creek Formation|38243|6|Mentioned|p354|||||||||
5617|Dook Creek Formation|39210|6|Mentioned|p50|||||||||
5617|Dook Creek Formation|42597|5|Briefly described|Map Legend|Carpentarian||||||||
5617|Dook Creek Formation|42812|6|Mentioned|p44|||||||||
5617|Dook Creek Formation|43010|2|Defined|p142|Mesoproterozoic|Paleoproterozoic|Of Mount Rigg Group. Of Statherian or Calymmian age.||||||07-NOV-08
5617|Dook Creek Formation|43149|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of Mount Rigg Group.||||||07-NOV-08
5617|Dook Creek Formation|44112|5|Briefly described|Table11p63,65,67|||||||||
5617|Dook Creek Formation|44201|14|Not recorded|p.9|||||||||
5617|Dook Creek Formation|44299|6|Mentioned|p.11|||SD/53-7,8.||||||
5617|Dook Creek Formation|44400|2|Defined|p.4,5,8,9,12,13,Tb.1|||Conformably overlies Bone Creek Formation. Mount Marumba Sheet. (D53-6),opp.p.6, map.||||||09-AUG-06
5617|Dook Creek Formation|44401|14|Not recorded|map legend|||Lower (?) Proterozoic.||||||
5617|Dook Creek Formation|44471|14|Not recorded|opp.p.7, map|||(D53-10). Carbonate beds + chert breccia band at top of Mt Rigg Group.||||||
5617|Dook Creek Formation|44472|5|Briefly described|map legend|||Of the Mount Rigg Group.  Quartz sandstone, siltstone, chert, dolomite containing stromatolites; chert breccia.Lower (?) Proterozoic.||||||02-DEC-04
5617|Dook Creek Formation|45022|4|Described|p.75,77,78,79||Carpentarian|Of Mount Rigg Group. Fig.16,17, Tb.3,8,10, Pl.28.||||||
5617|Dook Creek Formation|45162|6|Mentioned|p139|||See also Fig.152||||||
5617|Dook Creek Formation|46679|14|Not recorded|map legend||Neoproterozoic|Upper Proterozoic.||||||
5617|Dook Creek Formation|48894|6|Mentioned|p26|||1210my||||||
5617|Dook Creek Formation|60571|5|Briefly described|Map legend|Calymmian|Calymmian|Of the Mount Rigg Group. Mount is Mt in legend. Sandstone: medium-grained quartz arenite and silty sandstone; chert; blue/grey to brown, massive to banded; chert breccia. Geological Province: McArthur Basin.||||||30-NOV-04
5617|Dook Creek Formation|60573|5|Briefly described|Map legend|Calymmian|Statherian|Of the Mount Rigg Group.  Dolostone, chert, quartz sandstone,conglomerate, mudstone.  Does not outcrop in the Roper River mapsheet area.||||||23-DEC-09
5617|Dook Creek Formation|61390|5|Briefly described|Map Legend|Calymmian|Statherian|Of the Mount Rigg Group.||||||
5617|Dook Creek Formation|61403|5|Briefly described|Map Legend|Calymmian|Calymmian|Of Mount Rigg Group. Chert: blue-grey to brown, altered carbonate containing relict stromatolites, ooids and intraclast breccia. Geol. Prov: McArthur Basin.||||||
5617|Dook Creek Formation|61572|5|Briefly described|p667||Mesoproterozoic|Of the Mount Rigg Group. Geological Province: McArthur Basin.||||||09-AUG-06
5617|Dook Creek Formation|64817|6|Mentioned|p353 Fig.4 |||||Of the Mount Rigg Group.||||
5617|Dook Creek Formation|67564|6|Mentioned|p51.|Paleoproterozoic|Paleoproterozoic|Does not occur in this sheet area.||Unit in Mount Rigg Group.||Conformably overlies Bone Creek Sandstone.||
5617|Dook Creek Formation|69418|6|Mentioned|p3:11|||McArthur Basin. Hosts Pb-Zn deposits (described).||||||12-JUL-16
5617|Dook Creek Formation|69430|4|Described|p15:3, 24-26, 30, 43-44|||NW McArthur Basin. Up to 220m thick. Peritidal, from shallow-subtidal to supratidal deposits; storm-dominated marine shelf sediments in upper part. A paleoregolith is developed below the Roper Group unconformity. Hosts the Bulman base metal mineral field (described), associated with sills of Derim Derim Dolerite.||Mount Rigg Group.|Jamberline Sandstone Member.|Conformably and gradationally overlies Bone Creek Sandstone. Is overlain unconformably by the Limmen Sandstone (Roper Group). The lower part is correlated with Knuckey Formation.|Stromatolitic and intraclastic dolostone, mudstone and siltstone; laminated very fine sandstone and coarse siltstone.|12-JUL-16
5617|Dook Creek Formation|69673|6|Mentioned|p16 fig 13|Paleoproterozoic|Paleoproterozoic|Northwestern McArthur Basin.||Mount Rigg Group||Overlies Bone Creek Formation||
5617|Dook Creek Formation|70968|5|Briefly described|p13, p15, p17|||Source of clasts in conglomerate in overlying Limmen Sandstone.||Mount Rigg Group.||Is overlain unconformably by Limmen Sandstone (Roper Group).||
5619|Doomadgee Formation|22453|6|Mentioned|p 12|||In the McArthur Basin.||||||15-MAR-07
5619|Doomadgee Formation|22665|5|Briefly described|Table1, p229||Statherian|Age of unit is 1613+/-5 Ma U/Pb SHRIMP.||||||16-MAR-18
5619|Doomadgee Formation|22673|6|Mentioned|63,78|||Geol province: Mount Isa Basin.||||||09-AUG-06
5619|Doomadgee Formation|22680|6|Mentioned|84,85,87|||Geol province Mount Isa Basin. Of Fickling Group.||||||09-AUG-06
5619|Doomadgee Formation|23065|6|Mentioned|16|||Geol province: Lawn Hill Subprovince. Parent Fickling Group. Age: 1613 +/- 5 Ma.||||||09-AUG-06
5619|Doomadgee Formation|23393|5|Briefly described|p21|Paleoproterozoic|Paleoproterozoic|Of Fickling Group.||||||07-NOV-08
5619|Doomadgee Formation|23396|5|Briefly described|p407 Fig.2|||Of Fickling Group.||||||09-AUG-06
5619|Doomadgee Formation|23397|5|Briefly described|p466|Statherian|Statherian|Age: 1613+/-3Ma.||||||09-AUG-06
5619|Doomadgee Formation|23398|4|Described|p446|Statherian|Statherian|Age: 1619+/-5Ma U/Pb SHRIMP.||||||16-MAR-18
5619|Doomadgee Formation|23405|4|Described|p566|Statherian|Statherian|Of Fickling Group. Age: 1619+/-5Ma.||||||09-AUG-06
5619|Doomadgee Formation|23406|4|Described|p609 Fig. 9, p615|Statherian|Statherian|In Walford Creek area, consists mainly of dolarenite and and dolomitic sst grading up into laminated very fine-grained sandstone and siltstone; flaggy, micaceous, fine- to medium-gr. sst and pebble conglom. beds occasionally present. Age: 1619+/-5Ma.||||||16-JUN-09
5619|Doomadgee Formation|23407|5|Briefly described|p632|||||||||
5619|Doomadgee Formation|23409|5|Briefly described|p556|||Of Fickling Group.||||||09-AUG-06
5619|Doomadgee Formation|24308|5|Briefly described|p987 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of Fickling Group.   Geological Province:  Mount Isa Superbasin||||||07-NOV-08
5619|Doomadgee Formation|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Age: c.1613 Ma. Geological Province: Lawn Hill Platform.||||||
5619|Doomadgee Formation|24442|5|Briefly described|p22 Fig. 1|Mesoproterozoic|Mesoproterozoic|Of the Fickling Group (upper part).  Geological Province: McArthur Basin.||||||
5619|Doomadgee Formation|35640|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
5619|Doomadgee Formation|36012|3|Fully described|Table 3|||See also p16.||||||09-AUG-06
5619|Doomadgee Formation|36217|6|Mentioned|p206|||Published by Grimes and others 1979. Definition approved by Qld SNC.||||||09-AUG-06
5619|Doomadgee Formation|36439|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
5619|Doomadgee Formation|36442|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
5619|Doomadgee Formation|38237|6|Mentioned|p130|||||||||
5619|Doomadgee Formation|38348|6|Mentioned|p18|||||||||
5619|Doomadgee Formation|38584|4|Described|p17|||||||||
5619|Doomadgee Formation|39445|5|Briefly described|Table 2|||See also p39.||||||09-AUG-06
5619|Doomadgee Formation|39497|6|Mentioned|Fig.4|||||||||
5619|Doomadgee Formation|39685|6|Mentioned|p407|||||||||
5619|Doomadgee Formation|39925|6|Mentioned|p333|||||||||
5619|Doomadgee Formation|41721|4|Described|p28|||||||||
5619|Doomadgee Formation|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
5619|Doomadgee Formation|43010|5|Briefly described|Fig.6||Mesoproterozoic|of Fickling Group. Of "Mid Proterozoic" age.||||||
5619|Doomadgee Formation|45162|6|Mentioned|p146|||||||||
5619|Doomadgee Formation|45166|5|Briefly described|p30|||||||||
5619|Doomadgee Formation|49001|2|Defined|p11|Carpentarian|Carpentarian|||||||
5619|Doomadgee Formation|60558|5|Briefly described|p5 Fig. 4|||Of Fickling Group. Underlain by Mount Les Siltstone.||||||03-JUN-09
5619|Doomadgee Formation|61936|5|Briefly described|p194 Fig. 6|||Age: >1600Ma. Geological Province: Lawn Hill Platform, Western Fold Belt, Mount Isa Inlier, Isa Superbasin.||||||15-MAR-07
5619|Doomadgee Formation|62659|5|Briefly described|Map Legend|Calymmian|Statherian|Grey and green carbonaceous shale, flaggy reddish brown to maroon, dolomitic, micaceous, fine grained sandstone and siltstone; minor sandstone, dololutite, dolarenite, breccia.||||||
5619|Doomadgee Formation|63109|6|Mentioned|p1108 Fig. 3|||Geological Province: Isa Superbasin. Consists of shale.||||||30-SEP-08
5619|Doomadgee Formation|63113|6|Mentioned|p1225 Fig.13. |||Isa Superbasin. Seems to be part of Term, Lawn, Wide and Doom supersequences.||||Overlies Lawn Hill Formation. Is overlain by Widallion Sandstone.||
5619|Doomadgee Formation|63115|6|Mentioned|p1279 Fig.4.|||Isa superbasin.||||||
5619|Doomadgee Formation|63116|6|Mentioned|p1297 Fig.2, |||Isa superbasin.||||||
5619|Doomadgee Formation|65228|5|Briefly described|pp35-36|Statherian|Statherian|Lower part of this unit constitutes Term Supersequence in the northern Lawn Hill Platform. It extends through the Lawn Supersequence (where it is dated 1613 +/- 5 Ma) into the Wide Supesequence. Shore-face and inner ramp facies.|1619 +/- 5 Ma (Page et al. 2000).|||||
5619|Doomadgee Formation|65337|4|Described|p9 Fig.5, p22 Table 4, pp31-32.|Mesoproterozoic|Paleoproterozoic|Northeast MOUNT DRUMMOND area. 200 - 250 m of marine shelf deposits. Time-equivalent to Lawn Hill Formation.|>1613 +/- 5 Ma to 1595 +/- 6 Ma.|Unit in Fickling Group.||Overlies Mount Les Siltstone. Is disconformably, locally unconformably, overlain by South Nicholson Group.|Coarsening-up shale, through flaggy maroon, dolomitic, micaceous, fine-grained sandstone and siltstone, to pale sublithic fine to coarse sandstones; dolostones, minor dolomitic sandstone and intraclast breccia; carbonaceous shale and siltstone.|
5619|Doomadgee Formation|67323|5|Briefly described|GIS attrib tbl|Mesoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Camooweal-Murphy Domain, Mount Isa Inlier. Isa Superbasin. Informally subdivided into 3 units. Shown as Lower and Upper Doomadgee Formation in both Time-Space Plots.|1613 +/- 5 Ma (maximum depositional age).|Fickling Group.|||Reddish fine to coarse sandstone; conglomerate beds at base. Dark grey fissile shale and siltstone with flaggy claystone interbeds. Grey and brown, laminated fine sandstone; dolomite, dolomitic sandstone and conglomerate.|
5619|Doomadgee Formation|68146|4|Described|p2, p6, p41-50, p196, p198, p211|||South Nicholson Region. This age is within error of two previous determinations from tuffs (c.1613 Ma and c.1619 Ma). Whole-rock Sm-Nd isotopic data tabulated.|1632 +/- 14 Ma maximum deposition age.|Uppermost Fickling Group.||Is overlain unconformably by South Nicholson Group.|Includes a 75-100mm thick bed of green tuffaceous metasediment, very fine-grained to glassy with interbedded thin sandy layers.|
5619|Doomadgee Formation|68575|5|Briefly described|p11|||||Fickling Group.||Is overlain unconformably by Hedleys Sandstone.||
5619|Doomadgee Formation|69433|4|Described|p18:2, 4-5|Statherian|Statherian|Northern succession, Lawn Hill Platform. Is c.400m thick in the type section in WESTMORELAND map area. SHRIMP detrital zircon maximum deposition age.|<1619 +/- 5 Ma (Page et al., 2000).|Fickling Group.||Disconformably, locally conformably, overlies Mount Les Siltstone. Is overlain unconformably by the South Nicholson Group.|Conglomerate, sandstone, siltstone, shale and dolostone; arranged in upward-coarsening cycles from shale to sandstone, punctuated by dolostone intervals. A variety of sedimentary structures is listed.|12-JUL-16
5619|Doomadgee Formation|69591|5|Briefly described|p43 Fig.2.31, p47, p55|||Camooweal-Murphy Domain, Isa Superbasin. Part of Lawn and Wide Supersequences. Is presented on p43 (in Fig.2.31) as Lower and Upper Doomadgee Formations.|1619 +/- 5 Ma (Page et al., 2000).|Fickling Group.||The lower part is equated with the Lawn Supersequence; the upper part with Wide and Doom Supersequences.|Brown and green shale, thin-bedded siltstone, fine sandstone.|
5619|Doomadgee Formation|69673|4|Described|p52 fig 42, p53 |Statherian|Statherian||1619 +/- 5 Ma||||Conglomerate, sandstone, siltstone, shale and dolostone.|
5619|Doomadgee Formation|70849|5|Briefly described|Map legend.|Statherian|Statherian|Lawn Hill Platform.||Fickling Group.||Unconformably overlies Mount Les Siltstone. Is overlain unconformably by Constance Sandstone (South Nicholson Group).|Grey and brown or reddish, fine- to coarse-grained sandstone; dark grey fissile shale and siltstone with flaggy claystone interbeds; dolomite, dolomitic sandstone and conglomerate.|
5619|Doomadgee Formation|71369|5|Briefly described|p4, p9, p11|||Crops out as resistant benches (of sandstone).||Fickling Group.||Is overlain unconformably by Hedleys Sandstone.|Includes fine-grained sandstones, siltstone and shale.|20-FEB-18
5619|Doomadgee Formation|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1632+/-14 Ma (MDA: U-Pb zircon SHRIMP)||||Ash tuff.|
5619|Doomadgee Formation|72526|4|Described|p1-2, p4, p7, p8, p20-32, p85, 87.|Statherian|Statherian|Lawn Hill Platform, Mount Isa Province. Shown as being located in the central and west of the South Nicholson Basin. This unit is c. 200-400m thick (Grimes and Sweet, 1979; Sweet et al., 1981; Ahmad and Munson, 2013a).  2 ages determined are maximum depositional ages (MDAs). Previous dating of tuff from lower Doomagee Formation, at 1619 +/- 5 Ma and 1613 +/- 5 Ma, is interpreted as depositional age (Page and Sweet, 1998; Page et al., 2000; Carson et al., 2011b).|1612+/-11 Ma, 1630+/-14 Ma max dep age.|Fickling Group||Disconormably overlies Mount Les Siltstone and shown as underlying South Nicholson Group.|Includes shale, micaceous, dolomitic fine-grained sandstone and siltstone, medium-to coarse-grained sandstone and pebble conglomerate, tuff and claystone.|
5619|Doomadgee Formation|72527|6|Mentioned|p10|Paleoproterozoic|Paleoproterozoic|Tuff bands within the middle of this unit yielded an age of 1613 +/- 5 Ma (Page and Sweet, 1998).|Middle of unit 1613 +/- 5 Ma.|Uppermost Fickling Group|||Includes tuff bands.|
5619|Doomadgee Formation|72912|5|Briefly described|p5 Fig.3, p33 Fig.12, p45.|Statherian|Statherian|Located in the West and Central of the South Nicholson Basin. Three U-Pb zircon sedimentary depositional ages [?] given for this unit on p5, two of them also shown on p33, suggesting that the 1613 date is from the upper part of the unit and the 1632 date from around the middle.|1632 +/- 14 Ma to 1613 +/- 5 Ma|Fickling Group||Unconformably overlies Mount Les Siltstone and partially equivalent to Lawn Hill Formation.|Includes dolomitic siltstone.|
5619|Doomadgee Formation|72913|5|Briefly described|p4, p7, p8, p9 Tb.1, p18, p21, p26.|Paleoproterozoic|Paleoproterozoic|Shown as being in the central part of the Isa Superbasin. Identified in Amoco DDH 83-4 well in this study. Mineral composition boxplot shows majority quartz, microcline, muscovite and siderite.|1632 +/- 14, 1613 +/- 5 Ma|Fickling Group||Unconformably overlies Mount Les Siltstone.|Includes dolomitic siltstone.|
5619|Doomadgee Formation|72967|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|Lawn Hill Platform.||Fickling Group||||
5619|Doomadgee Formation|73042|5|Briefly described|p1, p4, p6, p14, p16-17||Statherian|Re-Os age overlaps with existing zircon depositional age constraints (generated from a number of sources) and is interpreted to record the timing of deposition for the unit. 4 other ages are given on p4 ranging from 1632+/-14Ma to 1613+/-5 Ma.  Mount Isa Province (Lawn Hill Platform) and South Nicholson Basin region, Isa Superbasin. Maximum thickness: 400m. Broadly equivalent in age to Lawn Hill Formation.|1609 +/- 61 Ma Re-Os|Fickling Group||Disconformably underlain by Mount Les Siltstone. Partly overlain by Wangalinji Member of Playford Sandstone, unconformably.|Shale, micaceous dolomitic fine-grained sandstone and siltstone, medium-to coarse-grained sandstone and pebble conglomerate.|
5639|Dorothy Volcanic Member|9538|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Tollis Formation (El Sherana Group). Basalt, pitchstone;  minor banded chert and dark grey tuff.||||||07-JAN-09
5639|Dorothy Volcanic Member|23119|5|Briefly described|p434|||||||||
5639|Dorothy Volcanic Member|23216|5|Briefly described|Table1p10,12||Orosirian|||||||
5639|Dorothy Volcanic Member|41586|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
5639|Dorothy Volcanic Member|43149|5|Briefly described|Map Legend||Paleoproterozoic|Of Tollis Formation.||||||07-NOV-08
5639|Dorothy Volcanic Member|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1850-1863Ma. Of Tollis Formation, Finniss River Group. Max. thickness 200m. Pitchstone, mafic tuff, minor banded chert.||||||07-JAN-09
5639|Dorothy Volcanic Member|69420|5|Briefly described|p5:40|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen.||Tollis Formation.|||Includes mafic tuffs.|12-JUL-16
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.||
5784|Dulcie Sandstone|9694|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Geological Province: Georgina Basin. Overlies: Nora Formation. Arenite, rare conglomerate.||||||
5784|Dulcie Sandstone|12891|5|Briefly described|p733 Fig. 2|Early Devonian|Early Devonian|Geological province: SW Georgina Basin.||||||07-FEB-11
5784|Dulcie Sandstone|12951|5|Briefly described|p142, 149, 152, p143 fig4, p145, 154|Devonian|Devonian|Georgina Basin. Fluvial deposits.||||Correlated with Cravens Peak beds.|Continental sandstone.|
5784|Dulcie Sandstone|22646|6|Mentioned|p 107|||informally divided into upper and lower Dulcie Sandstone p107.  Situated in the Georgina Basin.||||||28-FEB-13
5784|Dulcie Sandstone|22804|5|Briefly described|p454|||Geological Province: western Georgina Basin.||||||05-SEP-14
5784|Dulcie Sandstone|22954|6|Mentioned|Fig3p9|Emsian|Emsian|||||||
5784|Dulcie Sandstone|23732|5|Briefly described|p31|Late Devonian|Early Devonian|Geological Province: Georgina Basin.||||||
5784|Dulcie Sandstone|23818|5|Briefly described|p114|Late Devonian|Late Devonian|||||||
5784|Dulcie Sandstone|23858|5|Briefly described|p917|Early Devonian|Early Devonian|Geological Province: Georgina Basin.||||||
5784|Dulcie Sandstone|24065|4|Described|p235|Devonian|Silurian|Geological Province: Georgina Basin. Maximum thickness: ~646m.||||||
5784|Dulcie Sandstone|24066|5|Briefly described|p237|Devonian|Devonian|Geological Province: Georgina Basin.||||||
5784|Dulcie Sandstone|24613|6|Mentioned|p39|||Geological province: Georgina Basin.||||||07-FEB-11
5784|Dulcie Sandstone|30017|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
5784|Dulcie Sandstone|32865|4|Described|p482|||Frasnian||||||
5784|Dulcie Sandstone|33103|4|Described|Table 4|||||||||
5784|Dulcie Sandstone|33104|6|Mentioned|Map legend|Devonian|Devonian|||||||
5784|Dulcie Sandstone|33326|6|Mentioned|p449|||Fauna||||||
5784|Dulcie Sandstone|33625|6|Mentioned|p191|||||||||
5784|Dulcie Sandstone|34612|6|Mentioned|p114|||Upper Devonian||||||
5784|Dulcie Sandstone|34810|6|Mentioned|p9|||Re ages.||||||
5784|Dulcie Sandstone|36473|6|Mentioned|Map legend|Devonian|Devonian|||||||
5784|Dulcie Sandstone|37272|6|Mentioned|p237|||||||||
5784|Dulcie Sandstone|37727|4|Described|p56|||See also p23.||||||09-AUG-06
5784|Dulcie Sandstone|39978|6|Mentioned|p65|||||||||
5784|Dulcie Sandstone|40538|5|Briefly described|Map legend|Late Devonian|Late Devonian|Quartz arenite, thin to thick bedded, cross-bedded, scarp-forming, brown to pale yellow brown. Geological Province: Georgina Basin.||||||15-NOV-05
5784|Dulcie Sandstone|40836|6|Mentioned|Map legend|Devonian|Devonian|Prob. Devonian||||||
5784|Dulcie Sandstone|40906|4|Described|p29|||||||||
5784|Dulcie Sandstone|41018|6|Mentioned|p239|||||||||
5784|Dulcie Sandstone|41204|6|Mentioned|p14|||||||||
5784|Dulcie Sandstone|41276|6|Mentioned|p75|||||||||
5784|Dulcie Sandstone|41385|6|Mentioned|p363|||||||||
5784|Dulcie Sandstone|41524|3|Fully described|p21|||||||||
5784|Dulcie Sandstone|41525|5|Briefly described|Map legend|Devonian|Devonian|Quartz sandstone, whitish, crossbedded, medium to thick-bedded.||||||26-OCT-05
5784|Dulcie Sandstone|41820|6|Mentioned|p15|||||||||
5784|Dulcie Sandstone|41883|6|Mentioned|Fig.49|||||||||
5784|Dulcie Sandstone|42059|6|Mentioned|Fig.2 P131|||||||||
5784|Dulcie Sandstone|42504|6|Mentioned|p83|||Georgina Basin||||||
5784|Dulcie Sandstone|42643|3|Fully described|p32|Middle Devonian|Early Devonian|||||||
5784|Dulcie Sandstone|42644|5|Briefly described|Map Legend|Devonian|Devonian|Quartz arenite, medium-to-thick bedded, cross-bedded, white to brown. Geological Province: Georgina Basin.||||||15-NOV-05
5784|Dulcie Sandstone|44233|14|Not recorded|Fig.1||Late Devonian|||||||
5784|Dulcie Sandstone|44320|14|Not recorded|p.10||Late Devonian|U.Dev. Table 1.||||||
5784|Dulcie Sandstone|44321|14|Not recorded|map legend||Late Devonian|(F53-7). U.Dev.||||||
5784|Dulcie Sandstone|44322|5|Briefly described|map legend||Devonian|||||||22-DEC-09
5784|Dulcie Sandstone|44327|2|Defined|p.11,14,17||Late Devonian|(F53-11). Tb.I, map. Upper Devonian.||||||14-NOV-07
5784|Dulcie Sandstone|44328|14|Not recorded|map legend||Late Devonian|Upper Devonian.||||||
5784|Dulcie Sandstone|44964|14|Not recorded|p.350||Ordovician|Of Harts Range Group. Ordovician?||||||
5784|Dulcie Sandstone|44998|14|Not recorded|p56||Late Devonian|||||||
5784|Dulcie Sandstone|45041|6|Mentioned|p89|||||||||
5784|Dulcie Sandstone|45052|2|Defined|p132|Devonian|Devonian|See also p39.||||||09-AUG-06
5784|Dulcie Sandstone|45064|4|Described|Table 1|||||||||
5784|Dulcie Sandstone|45148|6|Mentioned|Fig.5|||Of Milligan and others 1966; Milligan 1976; renamed Lake Surprise Sandstone.||||||09-AUG-06
5784|Dulcie Sandstone|45155|6|Mentioned|Fig.8|||||||||
5784|Dulcie Sandstone|45167|5|Briefly described|p54|||||||||
5784|Dulcie Sandstone|45168|6|Mentioned|p6|||||||||
5784|Dulcie Sandstone|47050|5|Briefly described|Fig.1|||||||||
5784|Dulcie Sandstone|48844|1|Redefined|p.51||Late Devonian|On many pages. p.16,47,51,53-56, F.26,65,68, Pl.8, U.Devn.ss.which caps the Dulcie Range.O/lies Nora Fm. & Tomahawk Beds. (F53-11).||||||
5784|Dulcie Sandstone|48901|14|Not recorded|Not recorded||Late Devonian|U.Devonian. "Revision of usage" - on Tech File F/53-11.||||||28-FEB-13
5784|Dulcie Sandstone|60122|6|Mentioned|p32, p57 Appendix|||Lower part synonymous with Tomahawk Formation (Joklik 1955), together with the major portion of the former Tomahawk Beds (Smith 1964), excluding  the uppermost section which is now referred to Kelly Creek Formation.||||||
5784|Dulcie Sandstone|61022|5|Briefly described|p15 Fig. 2|Middle Devonian|Middle Devonian|Geological Province: Georgina Basin. Named in Abstract for: Carbonate ramp facies and oil plays in Late Cambrian-southern Georgina Basin (abstract) by Ambrose, G.J. and Putnam, P.E.||||||09-AUG-06
5784|Dulcie Sandstone|61404|5|Briefly described|Map legend|Devonian|Devonian|Quartz arenite: fine to medium; rare conglomerate. Geological Province: southern Georgina Basin.||||||12-OCT-05
5784|Dulcie Sandstone|62376|5|Briefly described|p53|Mesozoic|Mid Devonian|Geological Province: Georgina Basin||||||09-FEB-10
5784|Dulcie Sandstone|62522|5|Briefly described|p23|||Geological Province: Georgina Basin.||||||14-NOV-07
5784|Dulcie Sandstone|62983|5|Briefly described|p11|Devonian|Devonian|Synorogenic sedimentation. Geological Province: Georgina Basin.||||||23-JAN-07
5784|Dulcie Sandstone|63562|4|Described|p338 fig 3, p345 fig 7, p347 fig 9.|Devonian|Devonian|See also p350-351, p352 Fig.10, p355. Dulcie Syncline, Georgina Basin. Syn-orogenic clastic sedimentary unit sourced from uplifted Alice Springs Orogen to the S. Divided into lower clay-cemented (Early Devonian) and upper silica-cemented (Frasnian) units. The upper unit has mixed zircon ages similar to Stairway Sandstone, suggesting derivation from reworked Cambro-Ordovician sedimentary rocks.|c.365 Ma (Frasnian) upper part.|||Correlated with Pertnjara Group.|Well-sorted, medium- to thickly-bedded non-marine quartz sandstone.|18-SEP-18
5784|Dulcie Sandstone|64068|3|Fully described|p78, p40, p71, p75,77,  p ix|Eifelian|Pragian|Ungrouped. Formerly (Joklik 1955) included rocks now in Tomahawk Formation, Kelly Creek Formation, Nora Formation. Synorogenic, continental aeolian and freshwater sedimentation in a siliciclastic foreland, accompanied by high heat flow. No overlying units. Correlations: Cravens Peak beds, Mereenie Sandstone or Parke Siltstone.||||Unconformably overlies Nora Formation or Kelly Creek Formation.|Crossbedded quartz arenite, silty calcareous sandstone, pebble conglomerate.|04-APR-12
5784|Dulcie Sandstone|64778|6|Mentioned|p13, 33|Devonian|Devonian|Dulcie Syncline, Southern Georgina Basin.||||||
5784|Dulcie Sandstone|64812|5|Briefly described|p237 Fig. 2|Devonian|Devonian|Geological Province: southern Georgina Basin.||||||07-FEB-11
5784|Dulcie Sandstone|64813|5|Briefly described|p256 Fig. 3|Devonian|Devonian|Geological Province: southern Georgina Basin.||||||11-FEB-09
5784|Dulcie Sandstone|65237|5|Briefly described|p4 Fig. 7, p10|Devonian|Devonian|Geological province: southern Georgina Basin.||||||07-FEB-11
5784|Dulcie Sandstone|65338|5|Briefly described|p iv, p67.|Devonian|Devonian|Georgina Basin.|||||Medium- to thickly-bedded, cross-bedded quartz arenite.|
5784|Dulcie Sandstone|65341|6|Mentioned|p2 Fig.2. |Devonian|Devonian|||||||
5784|Dulcie Sandstone|65342|6|Mentioned|p6.|||Georgina Basin. Max. thickness at least 216 m.||||||
5784|Dulcie Sandstone|66499|6|Mentioned|p59, p65 Fig.8|||Includes fish fossils||||||
5784|Dulcie Sandstone|66767|5|Briefly described|p59|Devonian|Devonian|Southern Georgina Basin. Synorogenic (Alice Springs Orogeny) sedimentation: over 650m thickness preserved.||||||
5784|Dulcie Sandstone|67164|5|Briefly described|Map legend.|Paleozoic|Paleozoic|Georgina/Ngalia Basins.|||||Quartz arenite, medium- to thick-bedded, cross-bedded.|
5784|Dulcie Sandstone|67892|5|Briefly described|Map legend|Paleozoic|Paleozoic||||||Quartz arenite, medium- to thick-bedded, cross-bedded.|
5784|Dulcie Sandstone|68298|5|Briefly described|p234|||Georgina Basin. Placoderm association occurs in upper part of this unit (Young, 1988b).||||Includes similar fauna to Hervey Group, Khan Yunis Formation||
5784|Dulcie Sandstone|68518|5|Briefly described|p11, p14|Devonian|Devonian|Outcropping. A few small low mesas in the far west have been mapped as possible Dulcie Sandstone. Age: possible Devonian, however now regarded as Cambrian by NTGS (Stidolph, P.A., pers. comm., 1986).|||||Unfossiliferous fine-grained and medium-bedded sandstone with minor silty laminae.|30-MAY-16
5784|Dulcie Sandstone|69427|6|Mentioned|p12:48|Devonian|Devonian|Georgina Basin.||||||12-JUL-16
5784|Dulcie Sandstone|69443|4|Described|p28:3-5, 7, 28, 30, 32, 45|Middle Devonian|Early Devonian|K.G. Smith (1964) after Joklik (1955). Dulcie Syncline, Southern Georgina Basin. Synorogenic (Pertnjara-Brewer events of the Alice Springs Orogeny) foreland deposition of clastic sediments. Forms prominent cliff-forming caps and scarps. No overlying units. 450-650m thick. Contains Pragian to early Eifelian fish fauna. Continental aeolian and braided fluviatile deposits. Has been modelled for sediment-hosted uranium mineralisation.||||Unconformably overlies Nora or Kelly Creek Formations. Correlative of Cravens Peak beds.|Prominently cross-bedded, medium- to thickly-bedded quartz sandstone, with rare beds of silty calcareous sandstone and pebble conglomerate.|12-JUL-16
5784|Dulcie Sandstone|69447|6|Mentioned|p32:6|||Georgina Basin. Lithologically similar to Lake Surprise Sandstone (Wiso Basin).||||||12-JUL-16
5784|Dulcie Sandstone|69673|6|Mentioned|p111, p118, p119 fig 94|Devonian|Devonian|650m thick. Fossil assemblage of Devonian fish and rare ichnofossils.||||Correlated with Cravens Peak beds|Sandstone with rare beds of silty calcareous sandstone and pebble conglomerate.|
5784|Dulcie Sandstone|73591|6|Mentioned|p40, p42|||Georgina Basin.||||||
5843|Dungaminnie Formation|22538|6|Mentioned|Fig3 P709|||||||||
5843|Dungaminnie Formation|23216|6|Mentioned|p33|||||||||
5843|Dungaminnie Formation|23387|6|Mentioned|p18 fig.19|||Of Nathan Group.||||||
5843|Dungaminnie Formation|23396|5|Briefly described|p 407 fig.2|||Of Nathan Group. Formation spelt as Fm. Geological Province: McArthur Basin.||||||09-AUG-06
5843|Dungaminnie Formation|23405|5|Briefly described|p594|||Of Nathan Group.||||||
5843|Dungaminnie Formation|23407|5|Briefly described|p628 fig.4|||||||||
5843|Dungaminnie Formation|23776|5|Briefly described|p708|||Of Nathan Group.||||||
5843|Dungaminnie Formation|24048|5|Briefly described|p64|Calymmian|Calymmian|Of Nathan Group.  Geological Province: McArthur Basin.||||||09-AUG-06
5843|Dungaminnie Formation|32658|4|Described|Table 2|||See also Fig. 3||||||
5843|Dungaminnie Formation|32660|5|Briefly described|Table 4|||||||||
5843|Dungaminnie Formation|35261|6|Mentioned|Fig.2|||||||||
5843|Dungaminnie Formation|37462|4|Described|Table4.IV|||Of the McArthur Group.  Formation written as Fm.||||||09-AUG-06
5843|Dungaminnie Formation|37568|6|Mentioned|p79|||||||||
5843|Dungaminnie Formation|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
5843|Dungaminnie Formation|40259|6|Mentioned|Table 1|||||||||
5843|Dungaminnie Formation|40691|4|Described|Fig.43|||Mention p61.||||||09-AUG-06
5843|Dungaminnie Formation|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
5843|Dungaminnie Formation|41220|6|Mentioned|Fig.3|||||||||
5843|Dungaminnie Formation|41268|5|Briefly described|Fig.3|||||||||
5843|Dungaminnie Formation|41277|6|Mentioned|Fig.2|||Of the Nathan Group.||||||09-AUG-06
5843|Dungaminnie Formation|42385|5|Briefly described|Fig.5 P8|||Of Nathan Group.||||||09-AUG-06
5843|Dungaminnie Formation|42638|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Age: Middle Proterozoic.||Of Nathan Group||Not shown in schematic sections.|Sandy dolarenite and dololutite. Stromatolites. Detailed lithology given.|09-NOV-11
5843|Dungaminnie Formation|42812|5|Briefly described|p42, Fig.5|||||||||
5843|Dungaminnie Formation|42846|5|Briefly described|p503, Fig.1 p502|||Of Nathan Group. Geological Province: McArthur Basin.||||||09-MAY-05
5843|Dungaminnie Formation|43010|5|Briefly described|Fig.6||Mesoproterozoic|Of "Mid Proterozoic" age.||||||09-AUG-06
5843|Dungaminnie Formation|43036|6|Mentioned|Fig.5|||Of Nathan Group.||||||09-AUG-06
5843|Dungaminnie Formation|44112|6|Mentioned|p65|||||||||
5843|Dungaminnie Formation|45162|2|Defined|p143|Proterozoic|Proterozoic|||||||
5843|Dungaminnie Formation|46915|6|Mentioned|Fig.1|||Stratigraphic section through McArthur Group.||||||
5843|Dungaminnie Formation|46968|6|Mentioned|Fig.2|||||||||
5843|Dungaminnie Formation|60483|5|Briefly described|p7 Fig. 5|||Of the Nathan Group. Geological Province: McArthur Basin.||||||05-OCT-07
5843|Dungaminnie Formation|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Nathan Group. Underlain by Balbirini Dolomite.||||||03-JUN-09
5843|Dungaminnie Formation|63112|6|Mentioned|p1191 Fig.2|||Isa Superbasin; southern McArthur Basin. Age approximated from Fig.2.|c.1580 Ma.|Unit in Doom Supersequence.||||
5843|Dungaminnie Formation|63866|5|Briefly described|p54|||Isa Superbasin.||Doom Supersequence||||
5843|Dungaminnie Formation|64815|5|Briefly described|p3, p5 Fig.3  |||Up to 240 m thick.||Unit in Nathan Group.|||Dolostone; beds of fine sandstone and siltstone in lower portion.|
5843|Dungaminnie Formation|64816|6|Mentioned|p2 Fig.2 |||||Unit in Nathan Group.||||
5843|Dungaminnie Formation|64817|6|Mentioned|p353 Fig.4 |||||Of the Nathan Group.||||
5843|Dungaminnie Formation|65228|5|Briefly described|p39, Table 1, Figs.04, 24, 27.|||McArthur Basin. Base of this unit marks the boundary between Wide and Doom Supersequences. Feldspathic to arkose. Measured section.||Unit in Nathan Group.||Overlies Balbirini Dolomite. Is overlain by Limmen Sandstone.||
5843|Dungaminnie Formation|66843|4|Described|p24-26, p33-34, p38 Fig.10, p39|||Southern McArthur Basin. Composite stratigraphic column.||Nathan Group.||Overlies Balbirini Dolomite. Is overlain unconformably by Roper Group.|A lower unit of fine-grained dolomitic sandstone, locally pebbly, and an upper unit of sandy carbonates with conical, domal stromatolites, oolites, ripples, rare halite.|
5843|Dungaminnie Formation|67269|5|Briefly described|p20-21 Fig.19|Calymmian|Calymmian|McArthur Basin. Contains un-named stromatolites with an axial zone; photograph shown to demonstrate the continuity of such zones through geological time, and to support the biogenic origin of stromatolitic structures in Strelley Pool Formation (East Pilbara Terrane).|c.1575 Ma.|Nathan Group.||||
5843|Dungaminnie Formation|68280|6|Mentioned|p26 fig 24|||McArthur Basin.||Nathan Group||||
5843|Dungaminnie Formation|69018|5|Briefly described|p450 Fig.1b|Calymmian|Statherian|Of McArthur Basin.||Of Nathan Group||||
5843|Dungaminnie Formation|69430|4|Described|p15:3, 24|||Restricted to a syncline around the top of the Abner Range, southern McArthur Basin. Less than 240m thick. Shallow-water to emergent, and terrestrial (mainly fluvial), sediments.||Nathan Group.||Conformably overlies Balbirini Dolostone. Is overlain unconformably by Roper Group.|Lower: thinly bedded fine sandstone and siltstone with rare conglomerate lenses. Upper: laminated sandy dolarenite and dololutite; stromatolitic, intraclasts, ooids and ripples.|12-JUL-16
5843|Dungaminnie Formation|69673|6|Mentioned|p16 fig 13|Paleoproterozoic|Paleoproterozoic|||Nathan Group||Overlies Balbirini Dolostone||
5843|Dungaminnie Formation|70897|5|Briefly described|p43|Mesoproterozoic|Mesoproterozoic|||Nathan Group.||Is overlain unconformably by Limmen Sandstone.||
5843|Dungaminnie Formation|71494|6|Mentioned|p22|||Identified in the BMR log 1987-48 as Mantungula Formation; however, in the earlier Amoco log identified as Dungaminnie Formation.||||||
5843|Dungaminnie Formation|72523|5|Briefly described|p1, p2 Fig.2.|Early Mesoproterozoic|Early Mesoproterozoic|This unit is only known in the Abner Range area.||Top of Nathan Group in Abner Range region.||Overlies Balbirini Dolostone.||
5843|Dungaminnie Formation|72526|5|Briefly described|p8 Fig.1.3.|Calymmian|Calymmian|Shown as located in the Batten Fault Zone of the Southern McArthur Basin.||Nathan Group||Overlies Balbaririni Dolostone, Upper and unconformably underlies Collara Subgroup.||
5843|Dungaminnie Formation|72718|6|Mentioned|p7|||Southern McArthur Basin. Batten Fault Zone.||||Underlain by upper Balbirini Dolostone. Unconformably overlain by Limmen Sandstone (Collara Subgroup, Roper Group).||
5843|Dungaminnie Formation|72912|5|Briefly described|p5 Fig.3.|Calymmian|Calymmian|Located in the Batten Fault Zone of the Southern McArthur Basin.||Nathan Group||Overlies Balbirini Dolostone and equivalent to Karns Dolostone and unconformably underlies Nathan Group.||
5843|Dungaminnie Formation|73042|6|Mentioned|p4|Mesoproterozoic|Paleoproterozoic|Southern McArthur Basin, Isa Superbasin.||Nathan Group||Underlain by Upper Balbirini Dolostone. Unconformably overlain(?) by Limmen Sandstone.||
5843|Dungaminnie Formation|73412|6|Mentioned|p8|||Southern McArthur Basin.||Nathan Group.||||
5886|Dynamite Creek Member|23518|5|Briefly described|p11|Proterozoic|Proterozoic|Of Eastern Creek Volcanics.  Geological Province: Western Fold Belt.||||||
5886|Dynamite Creek Member|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
5886|Dynamite Creek Member|38560|2|Defined|p114|Jurassic|Jurassic|||||||
5886|Dynamite Creek Member|39495|6|Mentioned|p142|||||||||
5886|Dynamite Creek Member|39556|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||
5886|Dynamite Creek Member|39934|6|Mentioned|Fig.3|||||||||
5886|Dynamite Creek Member|41307|4|Described|p8|||||||||
5886|Dynamite Creek Member|45166|5|Briefly described|p15|||||||||
5886|Dynamite Creek Member|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Paleoproterozoic|Paleoproterozoic|Leichhardt Superbasin||Lower Haslingden Group|||Pink to buff, fine to coarse labile sandstone, conglomerate|
5886|Dynamite Creek Member|67539|5|Briefly described|p3, p4 Fig.3|||||Of the Eastern Creek Volcanics.|||Contains up to a 200m sequence of conglomerate and conglomerate lenses in sandstone with cobbles and boulders of granite and porphyry.|
5886|Dynamite Creek Member|69591|6|Mentioned|p33|||Mount Oxide and Leichhardt River Domains, Leichhardt Superbasin.||||||
5886|Dynamite Creek Member|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Eastern Creek Volcanics.||Is overlain by Cromwell Metabasalt Member.|Pink to buff, fine- to coarse-grained labile sandstone and conglomerate.|
5886|Dynamite Creek Member|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Eastern Creek Volcanics.||Is overlain by Cromwell Metabasalt Member.|Pink to buff, fine- to coarse-grained labile sandstone and conglomerate.|
5911|Eastern Creek Volcanics|22438|4|Described|p535, Fig.3 p537|||See also Fig.10a p546||||||
5911|Eastern Creek Volcanics|22457|4|Described|p31|||Of the Haslingden Group.||||||13-APR-18
5911|Eastern Creek Volcanics|22498|6|Mentioned|Fig1 P234|||||||||
5911|Eastern Creek Volcanics|22514|6|Mentioned|p393|||||||||
5911|Eastern Creek Volcanics|22585|6|Mentioned|P746, Fig1 P736|||||||||
5911|Eastern Creek Volcanics|22644|5|Briefly described|3,5,12|||Geological province: Mount Isa Basin. Of the Haslingden Group. Max thickness 7000 m.||||||30-JAN-07
5911|Eastern Creek Volcanics|22667|6|Mentioned|P238|||||||||
5911|Eastern Creek Volcanics|22747|5|Briefly described|p6||Precambrian|See also Table1,p7. Unconformably overlies Argylla Formation. Unconformably overlain by Corella Formation. Thickness: 6000+m. Part of Soldiers Cap Formation||||||15-AUG-06
5911|Eastern Creek Volcanics|22836|6|Mentioned|Fig.10 p402|||||||||
5911|Eastern Creek Volcanics|23031|6|Mentioned|18|||Geol province Mount Isa Fold Belt. Overlying unit Myally Subgroup. See p 21||||||
5911|Eastern Creek Volcanics|23073|5|Briefly described|p744 (fig 2)|||||||||
5911|Eastern Creek Volcanics|23205|5|Briefly described|p44|||Age: 1700Ma. Of Haslingden Group, Mount Isa Inlier.||||||15-AUG-06
5911|Eastern Creek Volcanics|23363|5|Briefly described|344 Fig.3|||||||||
5911|Eastern Creek Volcanics|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|Of Haslingden Group.  Geological Province: Mount Isa Fold Belt.||||||07-NOV-08
5911|Eastern Creek Volcanics|23395|6|Mentioned|p385|||||||||
5911|Eastern Creek Volcanics|23396|5|Briefly described|p407 Fig.2|||||||||
5911|Eastern Creek Volcanics|23399|5|Briefly described|p501|||||||||
5911|Eastern Creek Volcanics|23466|5|Briefly described|p265|||||||||
5911|Eastern Creek Volcanics|23518|4|Described|p9 Fig. 3, p11|Proterozoic|Proterozoic|Geological Province: Western Fold Belt.  Of the Haslingden Group.||||||
5911|Eastern Creek Volcanics|23554|6|Mentioned|pB35 Fig 1|||||||||
5911|Eastern Creek Volcanics|23767|5|Briefly described|p1954 Fig. 1a|||Geological Province: Leichhardt Superbasin. See also p1955.||||||
5911|Eastern Creek Volcanics|23961|6|Mentioned|p1191|||Geological Province: Mt Isa Inlier.||||||
5911|Eastern Creek Volcanics|23965|4|Described|p1296|Paleoproterozoic|Paleoproterozoic|Of Haslingden Group. Geological Province: Mount Isa Inlier.||||||07-NOV-08
5911|Eastern Creek Volcanics|23969|6|Mentioned|p1371 Fig.2|||Geological Province: Mount Isa Inlier. Of the Haslingden Group.||||||
5911|Eastern Creek Volcanics|24033|5|Briefly described|p1, p5, p28|||Includes Lena Quartzite Member and Cromwell Basalt Member.||||||
5911|Eastern Creek Volcanics|24034|6|Mentioned|p9|||Geological Province: Mount Isa Inlier. Flood basalts.||||||
5911|Eastern Creek Volcanics|24168|6|Mentioned|p637|||||||||
5911|Eastern Creek Volcanics|24197|5|Briefly described|p132|||Continental tholeiite. Age: <1870Ma. Geological province: Mount Isa Inlier.||||||07-FEB-11
5911|Eastern Creek Volcanics|24253|6|Mentioned|p4|||Geological Province: Mount Isa Block.||||||
5911|Eastern Creek Volcanics|24308|5|Briefly described|p991, p987 Fig.2|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
5911|Eastern Creek Volcanics|24419|5|Briefly described|p16, p12 Fig. 4, p13 Fig. 5|Proterozoic|Proterozoic|Of Haslingden Gp. Massive to strongly cleaved basalt lava flows, with interlayered quartz and feldspathic sandstone, conglomerate and other sedimentary rocks. Conformably underlies Myally Subgroup; conformably overlies Mount Guide Quartzite.||||||18-JAN-07
5911|Eastern Creek Volcanics|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Overlies Mount Guide Quartzite. Overlain by Myally Subgroup. Mafic.||||||
5911|Eastern Creek Volcanics|29961|6|Mentioned|p6|||||||||
5911|Eastern Creek Volcanics|29966|6|Mentioned|p396|||||||||
5911|Eastern Creek Volcanics|29969|6|Mentioned|p393|||||||||
5911|Eastern Creek Volcanics|30095|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
5911|Eastern Creek Volcanics|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Haslingden Group.  Underlies the Myally Subgroup.||||||25-AUG-04
5911|Eastern Creek Volcanics|30534|6|Mentioned|p300|||See also p305.||||||15-AUG-06
5911|Eastern Creek Volcanics|30535|6|Mentioned|p403|||||||||
5911|Eastern Creek Volcanics|30536|6|Mentioned|p100|||Stratigraphy||||||
5911|Eastern Creek Volcanics|30558|6|Mentioned|p43|||||||||
5911|Eastern Creek Volcanics|30721|6|Mentioned|p54|||Precambrian||||||
5911|Eastern Creek Volcanics|30723|5|Briefly described|p340|||See also p347,348. U-Th-Pb plot.||||||15-AUG-06
5911|Eastern Creek Volcanics|30725|5|Briefly described|p574|||Lower Proterozoic||||||
5911|Eastern Creek Volcanics|30912|6|Mentioned|p365|||||||||
5911|Eastern Creek Volcanics|31207|6|Mentioned|p1416|||||||||
5911|Eastern Creek Volcanics|31342|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
5911|Eastern Creek Volcanics|31821|6|Mentioned|p1024|||||||||
5911|Eastern Creek Volcanics|31824|6|Mentioned|p32|||L.Proterozoic||||||
5911|Eastern Creek Volcanics|32041|4|Described|p358|||||||||
5911|Eastern Creek Volcanics|32042|5|Briefly described|p35|||||||||
5911|Eastern Creek Volcanics|32211|6|Mentioned|p12|||Stratigraphy||||||
5911|Eastern Creek Volcanics|32264|5|Briefly described|p383|||||||||
5911|Eastern Creek Volcanics|32287|6|Mentioned|p18|||||||||
5911|Eastern Creek Volcanics|32660|5|Briefly described|Table 5|||||||||
5911|Eastern Creek Volcanics|32951|6|Mentioned|Table 1|||||||||
5911|Eastern Creek Volcanics|32952|6|Mentioned|p1188|||Precambrian||||||
5911|Eastern Creek Volcanics|32959|6|Mentioned|Fig.21|||See also p31.||||||15-AUG-06
5911|Eastern Creek Volcanics|33214|5|Briefly described|p1277|||Age discussed||||||
5911|Eastern Creek Volcanics|33482|6|Mentioned|Fig.4|||||||||
5911|Eastern Creek Volcanics|33893|5|Briefly described|p22|||See also pp30-31.||||||15-AUG-06
5911|Eastern Creek Volcanics|33894|6|Mentioned|Table 2|||||||||
5911|Eastern Creek Volcanics|33896|5|Briefly described|p457|||||||||
5911|Eastern Creek Volcanics|33897|6|Mentioned|p1280|||||||||
5911|Eastern Creek Volcanics|33900|4|Described|p11|||Mention p10.||||||15-AUG-06
5911|Eastern Creek Volcanics|34395|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
5911|Eastern Creek Volcanics|34499|6|Mentioned|Table 1|||||||||
5911|Eastern Creek Volcanics|34955|6|Mentioned|p227|||||||||
5911|Eastern Creek Volcanics|35074|6|Mentioned|Fig.2|||||||||
5911|Eastern Creek Volcanics|35115|6|Mentioned|Fig.1|||||||||
5911|Eastern Creek Volcanics|35116|6|Mentioned|p180|||||||||
5911|Eastern Creek Volcanics|35121|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
5911|Eastern Creek Volcanics|35139|4|Described|Table.2|||||||||
5911|Eastern Creek Volcanics|35146|6|Mentioned|p469|||||||||
5911|Eastern Creek Volcanics|35167|6|Mentioned|p151|||||||||
5911|Eastern Creek Volcanics|35286|6|Mentioned|Fig.17|||||||||
5911|Eastern Creek Volcanics|35295|6|Mentioned|p602|||||||||
5911|Eastern Creek Volcanics|35495|6|Mentioned|p341|||||||||
5911|Eastern Creek Volcanics|35892|6|Mentioned|p370|||||||||
5911|Eastern Creek Volcanics|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
5911|Eastern Creek Volcanics|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
5911|Eastern Creek Volcanics|36308|6|Mentioned|p209|||||||||
5911|Eastern Creek Volcanics|36548|6|Mentioned|p513|||||||||
5911|Eastern Creek Volcanics|36733|6|Mentioned|p12|||||||||
5911|Eastern Creek Volcanics|37413|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
5911|Eastern Creek Volcanics|37459|6|Mentioned|p423|||||||||
5911|Eastern Creek Volcanics|37568|5|Briefly described|p81|||See also p84.||||||15-AUG-06
5911|Eastern Creek Volcanics|37572|6|Mentioned|Fig.8|||||||||
5911|Eastern Creek Volcanics|37816|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
5911|Eastern Creek Volcanics|37862|6|Mentioned|p581|||See also P586.||||||
5911|Eastern Creek Volcanics|38232|6|Mentioned|p81|||||||||
5911|Eastern Creek Volcanics|38233|5|Briefly described|Table 1|||||||||
5911|Eastern Creek Volcanics|38234|4|Described|p103|||||||||
5911|Eastern Creek Volcanics|38236|6|Mentioned|p120|||||||||
5911|Eastern Creek Volcanics|38276|6|Mentioned|Fig.1|||||||||
5911|Eastern Creek Volcanics|38348|6|Mentioned|p6|||||||||
5911|Eastern Creek Volcanics|38350|4|Described|p9|||||||||
5911|Eastern Creek Volcanics|38442|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Haslingden Group.  Overlies Mount Guide Quartzite.||||||25-AUG-04
5911|Eastern Creek Volcanics|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
5911|Eastern Creek Volcanics|38544|6|Mentioned|p295|||||||||
5911|Eastern Creek Volcanics|38557|5|Briefly described|p289|||||||||
5911|Eastern Creek Volcanics|38560|6|Mentioned|p112|||||||||
5911|Eastern Creek Volcanics|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
5911|Eastern Creek Volcanics|38834|6|Mentioned|p162|||||||||
5911|Eastern Creek Volcanics|38900|6|Mentioned|p59|||||||||
5911|Eastern Creek Volcanics|38919|6|Mentioned|p493|||||||||
5911|Eastern Creek Volcanics|39125|6|Mentioned|p163|||||||||
5911|Eastern Creek Volcanics|39202|6|Mentioned|p242|||||||||
5911|Eastern Creek Volcanics|39362|6|Mentioned|p1468|||||||||
5911|Eastern Creek Volcanics|39445|5|Briefly described|p41|||See also p35 and Table 2.||||||15-AUG-06
5911|Eastern Creek Volcanics|39556|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||
5911|Eastern Creek Volcanics|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Includes the Pickwick Metabasalt and Lena Quartzite Members.  Underlies the Alsace Quartzite.||||||10-AUG-04
5911|Eastern Creek Volcanics|39602|6|Mentioned|p602|||||||||
5911|Eastern Creek Volcanics|39622|6|Mentioned|p19|||||||||
5911|Eastern Creek Volcanics|39798|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
5911|Eastern Creek Volcanics|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
5911|Eastern Creek Volcanics|39925|6|Mentioned|p334|||||||||
5911|Eastern Creek Volcanics|39934|4|Described|p317|||||||||
5911|Eastern Creek Volcanics|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
5911|Eastern Creek Volcanics|40202|6|Mentioned|p719|||||||||
5911|Eastern Creek Volcanics|40221|3|Fully described|p7|||||||||
5911|Eastern Creek Volcanics|40394|6|Mentioned|p284|||||||||
5911|Eastern Creek Volcanics|40598|6|Mentioned|p38|||||||||
5911|Eastern Creek Volcanics|40623|5|Briefly described|p95|||Briefly described p98.||||||15-AUG-06
5911|Eastern Creek Volcanics|40840|6|Mentioned|Map legend|||||||||
5911|Eastern Creek Volcanics|41125|6|Mentioned|p10|||See also P45||||||
5911|Eastern Creek Volcanics|41248|5|Briefly described|p74|||||||||
5911|Eastern Creek Volcanics|41277|6|Mentioned|Fig.5|||||||||
5911|Eastern Creek Volcanics|41298|6|Mentioned|Map legend|Carpentarian||||||||
5911|Eastern Creek Volcanics|41307|4|Described|p8|||||||||
5911|Eastern Creek Volcanics|41465|5|Briefly described|p11|||||||||
5911|Eastern Creek Volcanics|41802|5|Briefly described|p530|||||||||
5911|Eastern Creek Volcanics|41978|6|Mentioned|p494|||||||||
5911|Eastern Creek Volcanics|41979|6|Mentioned|p537|||||||||
5911|Eastern Creek Volcanics|42072|4|Described|p1618|||||||||
5911|Eastern Creek Volcanics|42110|5|Briefly described|p131|||||||||
5911|Eastern Creek Volcanics|42166|6|Mentioned|p110|||||||||
5911|Eastern Creek Volcanics|42197|6|Mentioned|p238|||||||||
5911|Eastern Creek Volcanics|42367|5|Briefly described|p27|||Of the Haslingdon Group.||||||30-JAN-07
5911|Eastern Creek Volcanics|42503|6|Mentioned|p336|||||||||
5911|Eastern Creek Volcanics|42523|5|Briefly described|Fig.2 P373|||||||||
5911|Eastern Creek Volcanics|42565|5|Briefly described|Table 1 P5, P2|||||||||
5911|Eastern Creek Volcanics|42661|6|Mentioned|p96|||McArthur Basin||||||
5911|Eastern Creek Volcanics|42676|5|Briefly described|Fig.2 P41|||||||||
5911|Eastern Creek Volcanics|42706|5|Briefly described|map legend|Proterozoic|Proterozoic|Of the Haslingden Group. Mafic lava: minor clastic sedimentary rocks.||||||09-FEB-09
5911|Eastern Creek Volcanics|42772|6|Mentioned|p17|||||||||
5911|Eastern Creek Volcanics|42782|5|Briefly described|p457|||see also Fig.1 p459.||||||30-JAN-07
5911|Eastern Creek Volcanics|42812|6|Mentioned|p65|||||||||
5911|Eastern Creek Volcanics|42818|4|Described|p206, Table 1 p207|||Of Haslingden Group.||||||15-AUG-06
5911|Eastern Creek Volcanics|43608|6|Mentioned|Fig.11,p11|||||||||
5911|Eastern Creek Volcanics|43616|6|Mentioned|p3|||||||||
5911|Eastern Creek Volcanics|43760|5|Briefly described|p431|||||||||
5911|Eastern Creek Volcanics|43788|6|Mentioned|p20|||||||||
5911|Eastern Creek Volcanics|43928|6|Mentioned|23|||||||||
5911|Eastern Creek Volcanics|43972|14|Not recorded|p7|||||||||
5911|Eastern Creek Volcanics|44162|14|Not recorded|p35,37||Paleoproterozoic|||||||07-NOV-08
5911|Eastern Creek Volcanics|44195|5|Briefly described|p358|||||||||
5911|Eastern Creek Volcanics|44210|2|Defined|map,Tb.1,p8-11,14-5|||||||||
5911|Eastern Creek Volcanics|44213|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
5911|Eastern Creek Volcanics|44270|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
5911|Eastern Creek Volcanics|44271|14|Not recorded|p33|||||||||
5911|Eastern Creek Volcanics|44273|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
5911|Eastern Creek Volcanics|44275|14|Not recorded|Map Legend|||||||||
5911|Eastern Creek Volcanics|44276|2|Defined|p10,17,Tb.1,map|||||||||
5911|Eastern Creek Volcanics|44277|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
5911|Eastern Creek Volcanics|44278|2|Defined|Tb.1,2,p4,5,9,map|||||||||
5911|Eastern Creek Volcanics|44279|2|Defined|p4,5,9,map,Tb.1,2|||||||||
5911|Eastern Creek Volcanics|44309|2|Defined|Tb.1,opp.p7,map|||Intruded by Sybella Granite.||||||
5911|Eastern Creek Volcanics|44326|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
5911|Eastern Creek Volcanics|44361|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
5911|Eastern Creek Volcanics|44362|4|Described|p5,Tb.1||Paleoproterozoic|||||||07-NOV-08
5911|Eastern Creek Volcanics|44517|14|Not recorded|p234-236|||Overlies Mount Guide Formation.||||||
5911|Eastern Creek Volcanics|44521|14|Not recorded|p1,4,6-14,21-26,32-3||Paleoproterozoic|||||||07-NOV-08
5911|Eastern Creek Volcanics|44522|14|Not recorded|p1,3,4||Paleoproterozoic|||||||07-NOV-08
5911|Eastern Creek Volcanics|44552|14|Not recorded|p24|||||||||
5911|Eastern Creek Volcanics|44749|14|Not recorded|p26|||||||||
5911|Eastern Creek Volcanics|44751|14|Not recorded|p301|||||||||
5911|Eastern Creek Volcanics|44755|2|Defined|p89-93,||Mesoproterozoic|Includes Pickwick Beds, Paroo Beds, Cromwell Beds and Lena Quartzite.||||||
5911|Eastern Creek Volcanics|44765|14|Not recorded|p14-16||Paleoproterozoic|||||||07-NOV-08
5911|Eastern Creek Volcanics|44766|14|Not recorded|p23,25|||Intruded by Kalkadoon Granite.||||||
5911|Eastern Creek Volcanics|44767|14|Not recorded|p763|||Has " a number of quartz veins of supposed hydrothermal origin that contain disseminated crystals of sulfide."||||||
5911|Eastern Creek Volcanics|44769|14|Not recorded|p1284|||||||||
5911|Eastern Creek Volcanics|44788|14|Not recorded|p26|||||||||
5911|Eastern Creek Volcanics|44806|14|Not recorded|p288|||Petrographic descriptions.||||||
5911|Eastern Creek Volcanics|44812|14|Not recorded|p6|||Soils.||||||
5911|Eastern Creek Volcanics|44843|14|Not recorded|p175|||||||||
5911|Eastern Creek Volcanics|44847|14|Not recorded|p652,653|||Uranium||||||
5911|Eastern Creek Volcanics|44854|14|Not recorded|p51|||Mineralisation.||||||
5911|Eastern Creek Volcanics|44919|14|Not recorded|p596,600,Tb.||Carpentarian|||||||
5911|Eastern Creek Volcanics|44920|14|Not recorded|Map Legend,Sheet 2,4||Carpentarian|||||||
5911|Eastern Creek Volcanics|44989|2|Defined|p.73-6|||Tb.II-IV. On many pages. Pls.4,13,14. Tb.VI. (E54-13,14,F54-1,2,5,6,9.).||||||01-SEP-08
5911|Eastern Creek Volcanics|45052|4|Described|p72|||Carpentarian.||||||13-APR-18
5911|Eastern Creek Volcanics|45072|6|Mentioned|p10|||||||||
5911|Eastern Creek Volcanics|45087|5|Briefly described|p105|||Chem. analyses.||||||
5911|Eastern Creek Volcanics|45136|3|Fully described|p47|||||||||
5911|Eastern Creek Volcanics|45161|4|Described|p23|||||||||
5911|Eastern Creek Volcanics|45166|6|Mentioned|p13|||||||||
5911|Eastern Creek Volcanics|45287|14|Not recorded|p.225-230|||Uranium.||||||
5911|Eastern Creek Volcanics|46801|6|Mentioned|p115|||See also Fig. 14||||||
5911|Eastern Creek Volcanics|46859|4|Described|p313|||||||||
5911|Eastern Creek Volcanics|46919|6|Mentioned|p219|||||||||
5911|Eastern Creek Volcanics|46960|6|Mentioned|p219|||||||||
5911|Eastern Creek Volcanics|46962|4|Described|Table 1|||See also Fig.3.||||||
5911|Eastern Creek Volcanics|46995|6|Mentioned|p271|||||||||
5911|Eastern Creek Volcanics|47011|6|Mentioned|p331|||||||||
5911|Eastern Creek Volcanics|47083|4|Described|p5-6||Proterozoic|Consists of three formal members. Of Haslingden Group. Overlain by Myally Subgroup.||||||30-JAN-07
5911|Eastern Creek Volcanics|48906|14|Not recorded|p28|||||||||
5911|Eastern Creek Volcanics|49009|6|Mentioned|p39|||||||||
5911|Eastern Creek Volcanics|49041|6|Mentioned|p8|||||||||
5911|Eastern Creek Volcanics|50100|5|Briefly described|p16-17|Proterozoic|Proterozoic|Of the lower Haslingden Group.  Includes Cromwell Metabasalt, Lena Quartzite and Pickwick Metabasalt Members.  Conformably overlie Mount Guide and Leander Quartzites.  Unconformably overlie Leichhardt Volcanics.  Geological Province: Western Fold Belt.||||||20-JAN-05
5911|Eastern Creek Volcanics|50332|5|Briefly described|p17, p50, p70, p84|Proterozoic|Proterozoic|Includes; Cromwell Metabasalt Member, Lena Quatrzite Member + Pickwick Meatbasalt Member. Conformably overlain by Myally Subgroup, comformably underlain by Mount Guide and Leander Quartzites. Geological Province: Leichhardt River Subprovince.||||||07-FEB-11
5911|Eastern Creek Volcanics|50536|6|Mentioned|p8.4|||Geological Province: Mount Isa Inlier.||||||
5911|Eastern Creek Volcanics|50550|4|Described|p1139 Fig.2, p1149||Statherian|Max. thickness: 6-8 km. Min. thickness: ~2 km. Includes continental tholeiitic basalts. Conformably overlain by Myally Subgroup. Geological Province: Western Fold Belt
.||||||20-JUN-22
5911|Eastern Creek Volcanics|50624|5|Briefly described|p234 Fig.2||Paleoproterozoic|Of the Haslingden Group.||||||07-NOV-08
5911|Eastern Creek Volcanics|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Haslingdon Group. Metabasalt, amphibolite, sedimentary lenses; minor gneiss, migmatite.||||||11-DEC-13
5911|Eastern Creek Volcanics|60513|6|Mentioned|p289, 290|||Basaltic.||||||
5911|Eastern Creek Volcanics|60558|5|Briefly described|p4 Fig. 3, p12|Paleoproterozoic|Paleoproterozoic|Geological Province: Western Fold Belt.||||||03-JUN-09
5911|Eastern Creek Volcanics|61204|4|Described|p538, p539, p540 Fig. 1|||Geological Province: Mount Isa Inlier. Of the Haslingden Group. Metabasalts and intercalated metasedimentary rocks.||||||31-MAY-07
5911|Eastern Creek Volcanics|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: >1750Ma. Geological Province: western Mount Isa Block.||||||07-NOV-08
5911|Eastern Creek Volcanics|61922|5|Briefly described|p8, p9 Fig. 3, p20 Fig.12.|||Comprises: lower and upper basaltic units separated by a sandstone layer. Discordantly underlie the Myally Subgroup rocks. Max. thickness: >4km. Geological Province: Mount Isa Inlier/Western Fold Belt.||||||15-AUG-06
5911|Eastern Creek Volcanics|61923|5|Briefly described|p27, p34 Fig.6|||Of the Haslingden Group. Comprises: Cromwell Metabasalt, Lena Quartzite and Pickwick Metabasalt. Overlain by Mount Isa Group. Geological Province: Mount Isa Inlier. See also p29 Fig.2, p30 Fig.3, p32 Fig.4.||||||
5911|Eastern Creek Volcanics|61924|5|Briefly described|p44|||||||||
5911|Eastern Creek Volcanics|61929|5|Briefly described|p128 Fig. 2|||Includes Lena Quartzite and Cromwell Metabasalt.||||||
5911|Eastern Creek Volcanics|61936|5|Briefly described|p193|||Iron-rich continental flood basalt. Overlain by Myally Subgroup. Geological Province: Leichhardt Superbasin, Eastern Fold Belt, Mount Isa Inlier. ||||||
5911|Eastern Creek Volcanics|62084|6|Mentioned|p936 Fig.5, p951 Fig.15|||Leichhardt Superbasin. Shown as Eastern Ck Volcs.||||||
5911|Eastern Creek Volcanics|62287|5|Briefly described|p130, p131|||Metamorphosed basalts and sediments. Overlain by Urquhart Shale.  Geological Province: Mount Isa Inlier.||||||30-JAN-07
5911|Eastern Creek Volcanics|62288|5|Briefly described|p120, p121 Fig. 1, p122 Fig. 2|Paleoproterozoic|Paleoproterozoic|Age: 1785-1710Ma. Geological Province: Western Fold Belt/ Mount Isa Inlier.||||||07-NOV-08
5911|Eastern Creek Volcanics|62373|6|Mentioned|p510, p516|||||||||
5911|Eastern Creek Volcanics|62873|4|Described|p691, p693, p707, p709|Paleoproterozoic|Paleoproterozoic|Of Haslingden Gp. Comprises 3 members. Series of copper-rich tholeiitic basalts adj. to giant sediment-hosted Mount Isa copper deposit; intercalated metabasalts and metasedimentary rocks. Age: 1710+/-25Ma and 1807+/-78Ma. Max. thickness: 7km.||||||07-NOV-08
5911|Eastern Creek Volcanics|63023|5|Briefly described|p1025 Fig. 2|||Of Haslingden Group. Overlain by Myally Subgroup (Haslingden Group); underlain by Mount Guide Quartzite (Haslingden Group). Geological Province: Leichardt Superbasin.||||||
5911|Eastern Creek Volcanics|63109|6|Mentioned|p1108, p1111|||Consists of mafic volcanics rocks. Geological Province: Leichhardt and Calvert Superbasin.||||||30-SEP-08
5911|Eastern Creek Volcanics|63111|5|Briefly described|p1163 Fig. 3, p1164 Tb. 1|Statherian|Statherian|Includes; Cromwell Metabasalt Member, Pickwick Metabasalt Member, Lena Quartzite Member. Overlain by Myally Subgroup, underlain by Mount Guide Quartzite.. Thickness: 7000m. Geological Province: Leichhardt Superbasin.||||||07-FEB-11
5911|Eastern Creek Volcanics|63113|5|Briefly described|p1214 Fig.2, p1225 Fig.13.|||||Of the Haslingden Group||Overlies Mount Guide Quartzite. Is overlain by Alsace Quartzite.||
5911|Eastern Creek Volcanics|63114|6|Mentioned|p1253 Fig.2, p1269-1270. |||||||Overlies Mount Guide Quartzite. Is overlain by Alsace Quartzite (Myally Subgroup).||
5911|Eastern Creek Volcanics|63115|6|Mentioned|1279 Fig.4, p1290. |||Leichhardt superbasin.||||||
5911|Eastern Creek Volcanics|63116|6|Mentioned|p1297 Fig.2, p1299-1305, p1310 |||Leichhardt superbasin. Material properties detailed. ||||||
5911|Eastern Creek Volcanics|63593|5|Briefly described|p284, p288 Fig.2, p291 Fig.3 and Tb.2 |||Western Fold Belt. The probable source of copper and associated metals ores in the Mount Isa mine. 7000 m thick.|||||Mafic lava, minor sandstone, siltstone and conglomerate.|
5911|Eastern Creek Volcanics|63866|5|Briefly described|p54, p56-p58|||Leichhardt Superbasin.||Myally Supersequence||Equivalent to the Seigal Volcanics and the Buddawadda Basalt. Overlies the Guide Supersequence.|Continental tholeiitic volcanics.|
5911|Eastern Creek Volcanics|63884|5|Briefly described|p14|||Metabasalts. Underlies Mt Isa Group.||||||
5911|Eastern Creek Volcanics|64250|5|Briefly described|p8, p16 fig 6, p19, p21-4|||Western Fold Belt, Mount Isa Inlier. Forms a single Supersequence with the Myally Subgroup.|<1779 +/- 4 Ma|Haslingden Group|Lena Quartzite|Overlies Mount Guide Quartzite. Is overlain by Myally Subgroup.|Mafic lavas.|12-MAY-14
5911|Eastern Creek Volcanics|64367|5|Briefly described|p553|Paleoproterozoic|Paleoproterozoic|Series of Cu-rich tholeiitic basalts,erupted into a continental rift .......Max.thickness: 7km - upper section is Pickwick Member, lower part is Cromwell Member, separated by Lena Quartzite. Age: 1.8Ga. Intruded by Sybella Batholith.||||||07-FEB-11
5911|Eastern Creek Volcanics|64575|6|Mentioned|p656|||||||||
5911|Eastern Creek Volcanics|64725|6|Mentioned|p58 Fig.2. |||Mount Isa Inlier.||||||
5911|Eastern Creek Volcanics|64726|6|Mentioned|p83 Fig.2.|||||||||
5911|Eastern Creek Volcanics|64744|6|Mentioned|p353 Fig.4, p354, p356, |Statherian|Statherian|Mount Isa Basin. Basaltic volcanics.|1790 Ma.|||Is overlain by Myally Subgroup.||
5911|Eastern Creek Volcanics|64817|6|Mentioned|p373 |Statherian|Statherian|>5 km thick. Mount Isa Basin.|1780 Ma||||Flood basalt sequence.|
5911|Eastern Creek Volcanics|64832|5|Briefly described|p1153, p1155 Figs. 2, 3|Paleoproterozoic|Paleoproterozoic|Of Haslingden Group.Comprises Cromwell Metabasalt Mb (lower) + Pickwick Metabasalt Mmb (upper). Age: 1785-1775Ma. Intruded by Sybella Granite. Geol.Prov: Mt Isa Inlier. Thick series of intercalated metabasalts + metasedimentary rocks.Detailed chemistry.||||||07-FEB-11
5911|Eastern Creek Volcanics|64834|5|Briefly described|p11-16, p31, p33, p35-36|||Leichhardt Superbasin. Western Succession of Mount Isa Basin. Hosts Valhalla U deposit. Thickness: >6 km. Detailed lithology and mineralogy given.|1779¿4 Ma Neumann et al. 2006||Lena Quartzite, (lower part) Cromwell Metabasalt Member, (upper part) Pickwick Formation|Is unconformably overlain by Surprise Creek Formation. Unconformable upper contact.|Volcanics and interbedded conglomerate (with cobble bed) and sandstone; thick sequence of metabasalts that comprise varying amounts of epidote, actinolite, albite, calcite, sphene, chlorite and magnetite.|
5911|Eastern Creek Volcanics|65228|5|Briefly described|p23, Fig.09.|Statherian|Statherian|Leichhardt River Fault Trough.|c.1780 Ma.|||Is overlain unconformably by Surprise Creek Formation.||13-APR-18
5911|Eastern Creek Volcanics|65337|6|Mentioned|p11. |||Correlated with Mitchiebo Volcanics. ||||||
5911|Eastern Creek Volcanics|65387|6|Mentioned|p1, p55-56|Statherian|Statherian||c.1780 Ma (Neumann and Fraser, 2007).|||Equated with Jayah Creek Metabasalt.||04-APR-18
5911|Eastern Creek Volcanics|65396|4|Described|p16, p82, p173, p175, p187, p190, p192|Statherian|Statherian|See also p193-194, p197, p241. Leichhardt Superbasin. Widespread unit in Cover Sequence 2. Lawn Hill Platform, Leichhardt River Fault Trough.|<1779 +/- 4 Ma|Haslingden Group|Includes Lena Quartzite|Overlies Mount Guide Quartzite; overlain by Myally Subgroup. Is correlated (possibly) with Kamarga Volcanics.|Mafic lavas.|03-APR-17
5911|Eastern Creek Volcanics|65505|5|Briefly described|979, 981, Fig 9|Proterozoic|Proterozoic.|Age equivalent with the Argylla Formation ~1780 Ma.||||||
5911|Eastern Creek Volcanics|65887|5|Briefly described|p52|Statherian|Statherian|Mount Isa Western Succession. Metatholeiites. ~1760 Ma.||||||
5911|Eastern Creek Volcanics|66302|6|Mentioned|p63|Statherian|Statherian|Has similar chemistry to the Tidnamurkuna and Myola Volcanics. |ca. 1790-1780 Ma (Wyborn et al, 1987)|||||
5911|Eastern Creek Volcanics|66529|5|Briefly described|p2, p32-37, p40, p41       |||Leichhardt Superbasin rift fill. Also appears as Eastern Creek Formation on p32, and Eastern Creek Basalt on p40. Has well-developed regional alteration assemblages; hosts most uranium deposits in the Mount Isa uranium field.|~1780 Ma|||Overlies Mount Guide Quartzite. Overlain by Myally Subgroup.|Continental tholeiite basalt; siliciclastic lenses.|
5911|Eastern Creek Volcanics|66824|6|Mentioned|p133, 135, 139|||||||Overlies Mount Guide Quartzite.||
5911|Eastern Creek Volcanics|67026|6|Mentioned|p336 Fig.3. |Proterozoic|Proterozoic|||Unit in Haslingden Group.||||
5911|Eastern Creek Volcanics|67057|5|Briefly described|p462.|Paleoproterozoic|Paleoproterozoic||1780 - 1760 Ma.|||||
5911|Eastern Creek Volcanics|67323|4|Described|p11-14, p16, p24-25, p39, p53|Paleoproterozoic|Paleoproterozoic|See also GIS attrib tbl, Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Leichhardt Superbasin. Of Leichhardt River Domain, basement to Mount Oxide Domain, Mount Isa Inlier. Rocks previously included in this unit have been renamed in this report as the Alpha Centauri Metamorphics. Previously equated with Marraba Volcanics, but the latter are too young. Up to 8km thick.|~1775-1765 Ma.|(Lower) Haslingden Group.|Includes Cromwell Metabasalt Member, Lena Quartzite Member, Pickwick Metabasalt Member.|Is overlain unconformably by Surprise Creek Formation locally. Geophysics suggests this unit may underlie the Myally Subgroup in the far north of Mt Oxide Domain.|Voluminous continental tholeiitic basalt, metabasalt, amygdaloidal basalt, quartzite, tuff, pelitic schist.|
5911|Eastern Creek Volcanics|67497|5|Briefly described|p909||||Age range ~1790-1730 Ma||||Mafic volcanics.|07-MAY-12
5911|Eastern Creek Volcanics|67499|4|Described|pp938-941, pp944-947, p940 Fig.3|Statherian|Statherian|Intruded by the Sybella batholith around 1657 +/- 7 Ma, using SHRIMP zircon dating from samples of the Elizabeth Creek felsic pluton.|1830 Ma|Of the Haslingden Group.|Cromwell Metabasalt Member, Pickwick Metabasalt Member, Lena Quartzite.|Overlain by the Myally Subgroup.|Tholeiitic flood metabasalt and intercalated metasediments.|08-MAY-12
5911|Eastern Creek Volcanics|67539|5|Briefly described|p2, p3, p4 Fig.3, p8, p9 Fig.7|Statherian|Statherian|Recent geochronology indicates that rocks intruded by the Sybella Granite in the southern Ardmore 1:100k Sheet area are not the Eastern Creek Volcanics as previously believed. |~ 1780 Ma||Includes Dynamite Creek Member|Parts intruded by Ewen Granite and Leichhardt Metamorphics, parts appear to unconformably overlie Ewen Granite.||
5911|Eastern Creek Volcanics|67788|6|Mentioned|p22|||Mentioned in a list of units containing braided and low-sinuosity river deposits. Age is given as Precambrian.||||||
5911|Eastern Creek Volcanics|68020|5|Briefly described|p126, p127|||||||In faulted contact with Mount Isa Group, at the mine.|Metamorphosed basic volcanics and pelitic and psammitic metasediments.|
5911|Eastern Creek Volcanics|68021|5|Briefly described|p134, p135 fig 4, p135, 136, p138|Statherian|Statherian|Part of Myally Supersequence, Leichhardt Superbasin, Western Succession. Subaerial or shallow water.|1780 - 1775 Ma|||Overlies Mount Guide Quartzite, overlain by Myally Subgroup, inferred correlation with Marraba Volcanics, Argylla Formation, intruded by Sybella Granite.|Continental flood basalts and interbedded siliciclastic sediment.|
5911|Eastern Creek Volcanics|68542|6|Mentioned|p10|||||Haslingden Group|Includes Cromwell Member|||
5911|Eastern Creek Volcanics|68575|5|Briefly described|p97, p112-113|||Previous equating of this unit with the Oroopoo Metabasalt is called into question by detrital zircon population ages.||||Overlies Mount Guide Quartzite.||
5911|Eastern Creek Volcanics|68576|5|Briefly described|Q_2: p10, p12|Proterozoic|Proterozoic|||Haslingden Group.|||Basalts; fluvial sedimentary interbeds.|
5911|Eastern Creek Volcanics|68732|5|Briefly described|p165|||Associated with the c.1780 Ma Argylla Magmatic Event.||||Correlated with Cone Creek Volcanic Member. Interbedded with the Myally Supersequence.|Basaltic rocks.|30-NOV-17
5911|Eastern Creek Volcanics|69056|6|Mentioned|p52-53|||Western Mount Isa Inlier. Previously equated with Marraba Volcanics in the Mitakoodi Domain, but this latter unit is much younger.||||||
5911|Eastern Creek Volcanics|69222|5|Briefly described|p221, p222 Fig.2, p224 Fig.3|||Leichhardt River Fault Trough.|||Includes Lena Quartzite, Cromwell Metabasalt|Overlies Mount Guide Quartzite, overlain by Myally Subgroup|Voluminous continental tholeiites.|
5911|Eastern Creek Volcanics|69433|6|Mentioned|p18:6|||Mount Isa Inlier.||||Correlated with Mitchiebo Volcanics.||12-JUL-16
5911|Eastern Creek Volcanics|69542|5|Briefly described|p132, p133 Fig.2, p135|Mesoproterozoic|Paleoproterozoic|Western Fold Belt. Abbreviated in the text to ECV.||Haslingden Group|||Tholeiitic basalt and metabasalts.|09-FEB-18
5911|Eastern Creek Volcanics|69591|4|Described|p33-35, p38, p41, p45, p49, p57|||Wilson, Derrick and Perkins (1984). Mount Oxide and Leichhardt River Domains, Leichhardt Superbasin. Part of Myally Supersequence. Up to 8km thick in basin depocentres. Eruption may have been synchronous with Argylla Formation. Correlation with Seigal Volcanics is speculative.|1779 +/- 4 Ma (MDA: Neumann et al., 2006).|Haslingden Group.||Is overlain by Myally Subgroup. Is equated with Buddawadda Basalt Member (Peters Creek Volcanics). Is faulted against Mount Isa Group.|Voluminous Fe-rich continental flood basalt: metabasalt, amygdaloidal basalt, quartzite, tuff, pelitic schist. Highly magnetic.|
5911|Eastern Creek Volcanics|70282|5|Briefly described|p544 Fig.1, p546, p551|||Cover sequence 2, Mount Isa. Up to 6km thick.|1790-1760 Ma (or 1720 Ma)|||Overlies Mount Guide Quartzite. Is overlain by Myally Subgroup. Overlain by Urquhart Shale|Basaltic; extensive.|13-FEB-18
5911|Eastern Creek Volcanics|70283|5|Briefly described|p24-26, p31-33|Paleoproterozoic|Paleoproterozoic|Biotite, muscovite ages discussed. Appears as Eastern Creek volcanics on p33.||Haslingden Group|||Metabasalt and interbedded sandstone.|14-FEB-18
5911|Eastern Creek Volcanics|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Haslingden Group.|Dynamite Creek, Cromwell Metabasalt, Lena Quartzite, Pickwick Metabasalt, Members.|Is overlain by Myally Subgroup.|Metabasalt (locally amygdaloidal), quartzite, tuff and pelitic schist.|
5911|Eastern Creek Volcanics|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Haslingden Group.|Dynamite Creek, Cromwell Metabasalt, Lena Quartzite, Pickwick Metabasalt, Members.|Is overlain by Myally Subgroup.|Metabasalt (locally amygdaloidal), quartzite, tuff and pelitic schist.|
5911|Eastern Creek Volcanics|70858|6|Mentioned|p31|Paleoproterozoic|Paleoproterozoic|Leichhardt Superbasin.|1780-1775 Ma.|||||
5911|Eastern Creek Volcanics|71348|6|Mentioned|p217|||Geological province: North Australian Craton. Formed in a back-arc setting consistent with mafic and bimodal magmatism.||||||
5911|Eastern Creek Volcanics|71606|5|Briefly described|p137|Statherian|Statherian|Lawn Hill Platform, Mount Isa Inlier.||||Overlain by Myally Subgroup. Underlain by Leichardt Volcanics and Kalkadoon Granite. Equivalent to Haslingden Group.||
5911|Eastern Creek Volcanics|71799|5|Briefly described|p150 fig 2, p151 fig 3|Statherian|Statherian|Lawn Hill. Ages are derived from underlying  Lena Quartzite and overlying Myally Supersequence. Geochemistry is discussed. See also p152, p153 tbl 1, p154, p156-p158, p162, p165.|ca 1775 Ma||Includes the Cromwell Metabasalt Member, Lena Quartzite Member and Pickwick Metabasalt Member.|Overlies the Mount Guide Formation.|Basalt, dolerite, gabbro or amphibolite.|
5911|Eastern Creek Volcanics|71960|5|Briefly described|p77, 78, 81, 82, 83, 85, 86, 95,103,105|Proterozoic|Proterozoic|~3km thick east of Hero Syncline.||Of Haslingden Group.|Includes Cromwell Metabasalt?|Unconformably overlain/truncated by lower Mount Isa Group in Hero Syncline.||
5911|Eastern Creek Volcanics|71980|5|Briefly described|map legend sheets 1, 2|Proterozoic|Proterozoic|Fluviolacustrine between basalt flows.||Of Haslingden Group|Includes Pickwick Metabasalt Member, Lena Quartzite Member, Cromwell Metabasalt Member, Native Bee Siltstone|Underlies Myally Subgroup.|metabasalt; fluviolacustrine sandstone between basalt flows.|
5911|Eastern Creek Volcanics|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Lawn Hill Platform and Leichhardt River Fault Trough of the Mount Isa Province.||||Overlies Mount Guide Quartzite and underlies Alsace Quartzite.||
5911|Eastern Creek Volcanics|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Leichhardt River Domain. Includes an epidotic quartzite and meta-arenite conglomerate marker bed and two other informal subdivisions.||Haslingden Group||Underlies Myally Subgroup.|Metabasalt (locally amygdaloidal), quartzite, tuff and pelitic schist. Epidotic quartzite, meta-arenite conglomerate. Quartz sandstone, feldspathic quartzite, conglomerate, epidote quartzite; minor dolomitc sst. Schist, quartzite, amphibolite.|
5911|Eastern Creek Volcanics|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Leichhardt River Domain. Includes an epidotic quartzite and meta-arenite conglomerate marker bed and two other informal subdivisions.||Haslingden Group||Underlies Myally Subgroup.|Metabasalt (locally amygdaloidal), quartzite, tuff and pelitic schist. Epidotic quartzite, meta-arenite conglomerate. Quartz sandstone, feldspathic quartzite, conglomerate, epidote quartzite; minor dolomitc sst. Schist, quartzite, amphibolite.|
5911|Eastern Creek Volcanics|72912|5|Briefly described|p5 Fig.3, p12.|Statherian|Statherian|Part of the Leichhradt Superbasin. Located in the Lawn Hill Platform and Leichhardt River Fault Trough of the Mount Isa Province.||Guide Supersequence||Overlies Mount Guide Quartzite and partially overlies Bottletree Formation.|Includes continental flood basalts.|
5911|Eastern Creek Volcanics|72919|6|Mentioned|p63|||||Myally Supersequence||||
5911|Eastern Creek Volcanics|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Mount Isa Province, Leichhardt Superbasin.||||Partly underlain by Mount Guide Quartzite. Overlain by Alsace Quartzite (Myally Subgroup).||
5911|Eastern Creek Volcanics|73083|6|Mentioned|p74|||||||||
5911|Eastern Creek Volcanics|73525|5|Briefly described|p2 Fig.1, p4-5 Fig.2, p19 Fig.13|Statherian|Statherian|Mount Oxide-(Ardmore-May Downs) and Leichhardt River Domains.|<1779+/-4 Ma maximum depositional age||||Mafic extrusives, includes clastics, siliciclastics.|
5911|Eastern Creek Volcanics|73553|5|Briefly described|p125-126, p231-232|||Western Succession.|||Cromwell Metabasalt Member||Tholeiitic continental flood basalts.|
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
5978|Edith River Group|9534|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Rhyolite, dacite, minor basic volcanics; lenses of ignimbrite and tuffaceous sandstone.||||||07-NOV-08
5978|Edith River Group|9538|5|Briefly described|Map legend|Proterozoic|Proterozoic|Contains the Plum Tree Volcanics, Hindrance Creek Sandstone.||||||01-NOV-04
5978|Edith River Group|9691|5|Briefly described|Map Legend|||Rhyolite, dacite, minor basic volcanics; lenses of ignimbrite and tuffaceous sandstone.||||||
5978|Edith River Group|9701|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Rhyolite, dacite, minor basic volcanics; lenses of ignimbrite and tuffaceous sandstone.||||||02-JUN-05
5978|Edith River Group|22479|5|Briefly described|fig1p2|Orosirian|Orosirian|McArthur Basin.||||||28-MAR-18
5978|Edith River Group|22538|3|Fully described|Fig4 P710, P714|||Part of the Redbank package.||||||15-AUG-06
5978|Edith River Group|22600|6|Mentioned|Map legend|||||||||
5978|Edith River Group|22748|5|Briefly described|p235 Fig.1|Orosirian|Orosirian|Age: ~1830 Ma.||||||15-AUG-06
5978|Edith River Group|22808|6|Mentioned|7 fig 4|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
5978|Edith River Group|23216|4|Described|Fig3p5,12-3,50-1||Orosirian|Age: 1830 Ma. Consists of: Plum Tree Creek Volcanics, Phillips Creek Sandstone and Hindrance Creek Sandstone.||||||
5978|Edith River Group|23363|5|Briefly described|344 Fig.3|||||||||
5978|Edith River Group|23374|5|Briefly described|Fig3p5||Paleoproterozoic|Of Pine Creek Inlier.||||||07-NOV-08
5978|Edith River Group|23714|5|Briefly described|p6 Fig 4|Proterozoic|Proterozoic|||||||
5978|Edith River Group|23733|5|Briefly described|p32 Fig. 19|||||||||
5978|Edith River Group|23867|5|Briefly described|p2|Paleoproterozoic|Paleoproterozoic|Geological Province: McArthur Basin.  See also Fig. 3.||||||07-NOV-08
5978|Edith River Group|23937|6|Mentioned|p88 App. 1|||Geological Province: McArthur Basin.||||||
5978|Edith River Group|24047|5|Briefly described|p5 Fig.4|Paleoproterozoic|Paleoproterozoic|Felsic volcanics, conglomerate, sandstone.  Age: 1822Ma.  Geological Province: Pine Creek Orogen.  See also p6 Fig. 5, p12 Fig. 10.||||||07-NOV-08
5978|Edith River Group|24048|6|Mentioned|p6|||||||||
5978|Edith River Group|24049|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|In regional setting map legend.||||||07-NOV-08
5978|Edith River Group|24197|5|Briefly described|p28|Paleoproterozoic|Paleoproterozoic|The volcanics of this group are included in the Jim Jim Suite.||||||07-FEB-11
5978|Edith River Group|24340|5|Briefly described|p147 Fig. 3|Paleoproterozoic|Paleoproterozoic|Age: 1830 Ma (U-Pb). Geological Province: Pine Creek Inlier.||||||07-NOV-08
5978|Edith River Group|39357|4|Described|p14|||||||||
5978|Edith River Group|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
5978|Edith River Group|39801|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Acid and minor basic volcanics, pyroclastics, sandstone.||||||07-NOV-08
5978|Edith River Group|40168|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Acid and minor basic volcanics, pyroclastics, sandstone. Microgranite, granite.||||||07-NOV-08
5978|Edith River Group|40223|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Acid and minor basic volcanics, pyroclastics, sandstone.||||||07-NOV-08
5978|Edith River Group|40243|6|Mentioned|p139|||||||||
5978|Edith River Group|40248|3|Fully described|p224|||||||||
5978|Edith River Group|40823|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
5978|Edith River Group|40861|6|Mentioned|Fig.1|||||||||
5978|Edith River Group|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
5978|Edith River Group|41125|6|Mentioned|p26|||See also fig.6.||||||
5978|Edith River Group|41146|6|Mentioned|p858|||||||||
5978|Edith River Group|41294|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
5978|Edith River Group|41295|4|Described|p12|||||||||
5978|Edith River Group|41304|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
5978|Edith River Group|41305|5|Briefly described|Fig.4|||||||||
5978|Edith River Group|41311|4|Described|p13|||||||||
5978|Edith River Group|41325|6|Mentioned|p18|||||||||
5978|Edith River Group|41397|4|Described|p16|||||||||
5978|Edith River Group|41406|6|Mentioned|Map legend|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
5978|Edith River Group|41407|6|Mentioned|Map legend|Proterozoic||||||||
5978|Edith River Group|41465|6|Mentioned|p6|||||||||
5978|Edith River Group|41466|6|Mentioned|p32|||||||||
5978|Edith River Group|41586|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
5978|Edith River Group|41594|6|Mentioned|p20|||||||||
5978|Edith River Group|41970|6|Mentioned|p336|||||||||
5978|Edith River Group|42012|6|Mentioned|Fig.3 P3|||||||||
5978|Edith River Group|42014|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
5978|Edith River Group|42812|6|Mentioned|p60|||||||||
5978|Edith River Group|42927|6|Mentioned|p428|||||||||
5978|Edith River Group|43010|6|Mentioned|p76|||||||||
5978|Edith River Group|43036|5|Briefly described|p68|||||||||
5978|Edith River Group|43140|5|Briefly described|p3||Paleoproterozoic|||||||07-NOV-08
5978|Edith River Group|43149|5|Briefly described|Map Legend||Paleoproterozoic|Of Orosirian age.||||||07-NOV-08
5978|Edith River Group|43187|5|Briefly described|p2|||||||||
5978|Edith River Group|43292|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
5978|Edith River Group|43624|6|Mentioned|Table 1, p9|Mesoproterozoic|Paleoproterozoic|Age: 1830 Ma||||||07-NOV-08
5978|Edith River Group|43718|6|Mentioned|p2,24|||||||||
5978|Edith River Group|43720|5|Briefly described|p4|Mesoproterozoic|Paleoproterozoic|Late Palaeoproterozoic - Mesoproterozoic||||||07-NOV-08
5978|Edith River Group|43726|6|Mentioned|p2|||||||||
5978|Edith River Group|43832|4|Described|23-25,Table6 p22, 97||Paleoproterozoic|Age 1870-1830 Ma (p21,24). In Pine Ck Geosyncline. El Sherana Group underlies, Katherine River Group overlies.||||||07-NOV-08
5978|Edith River Group|44112|6|Mentioned|p63|||||||||
5978|Edith River Group|46639|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Rhyolite, dacite, minor basic volcanics; lenses of ignimbrite and tuffaceous sandstone; minor chloritoid or silicified spherulitic metamorphosed equivalents.  Valley fill volcanics.||||||07-NOV-08
5978|Edith River Group|46658|4|Described|p557|||||||||
5978|Edith River Group|46675|5|Briefly described|Map legend for regional setting...|Paleoproterozoic|Paleoproterozoic|Acid and minor basic volcanics, pyroclastics, sandstone; microgranite, granite; granite, adamellite, granodiorite, minor syenite.  Geological Province: Pine Creek Geosyncline.||||||07-NOV-08
5978|Edith River Group|47049|5|Briefly described|Table|||New name.||||||
5978|Edith River Group|50586|6|Mentioned|p4.1|||||||||
5978|Edith River Group|60573|6|Mentioned|Regional Setting legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
5978|Edith River Group|60574|5|Briefly described|Map Legend|||Geological Province: McArthur Basin.||||||
5978|Edith River Group|60680|5|Briefly described|Map legend|Orosirian|Orosirian|Includes Plum Tree Creek Volcanics and Kurrundie Sandstone.||||||23-DEC-09
5978|Edith River Group|61403|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|In regional setting map legend.||||||07-NOV-08
5978|Edith River Group|61861|6|Mentioned|Fig.2.|||Pine Creek.||||Unconformably overlies El Sherana Group. Is unconformably overlain by Katherine River Group.||
5978|Edith River Group|62375|5|Briefly described|p8 Table 1, 9 table 2, 10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Ignimbrite, microgranite, rhyolite, minor basalt and cherty sediments. Age: 1820Ma. Thickness: 1200m. Geological Province: Pine Creek Orogen. Unconformably Underlies: Finniss River Group.||||||11-OCT-11
5978|Edith River Group|63866|5|Briefly described|p106, p110-p111, p123|||Litchfield Province, Pine Creek Orogen.||||Unconformably overlies the El Sherana Group. Overlain by the Plum Tree Creek Volcanics.||
5978|Edith River Group|64329|6|Mentioned|p20|||||||||
5978|Edith River Group|64677|6|Mentioned|v,|||||||||
5978|Edith River Group|64698|5|Briefly described|lithinterp table|Statherian|Orosirian|Includes Phillips Creek Sandstone, Hindrance Creek Sandstone,  Plum Tree Volcanics (1825 Ma), Kurrundie Sandstone.||||||07-JAN-09
5978|Edith River Group|64722|5|Briefly described|Fig. 2 p3-6, p10, 22|Orosirian|Orosirian|Volcanic and sedimentary rocks of Pine Creek Orogen. Age range for this and underlying El Sherana Group.|1830-1825 Ma.|||Unconformably overlies El Sherana Group. Is overlain by Katherine River Group.||11-APR-12
5978|Edith River Group|64725|6|Mentioned|p61.|||Deposited in graben or half-graben structures.|>1835 Ma. |||||
5978|Edith River Group|64730|5|Briefly described|p125 Fig. 3, p126, p141, Fig. 11|Paleoproterozoic|Paleoproterozoic|Age from Plum Tree Creek Volcanics (Page 1996).|Min. deposition age at 1825 +/- 4 Ma.||Includes Plum Tree Creek Volcanics, Phillips Creek Sandstone, Kurundie Sandstone, Hindrance Creek Sandstone.|||02-MAY-12
5978|Edith River Group|64817|6|Mentioned|p352-355 Figs.3,4,5; p367 Tb.2 |Orosirian|Orosirian|Arnhem Shelf, McArthur Basin.|1822 +/- 6 Ma.||Includes the Plumtree Creek Volcanics and the Kurrundie Sandstone.||Includes felsic volcanics, sandstone and conglomerate.|04-JUN-18
5978|Edith River Group|65232|5|Briefly described|p45, p6 Fig. 5, p7, p24, p5 Fig. 4|Orosirian|Orosirian|Includes Kurrundie Sandstone and Plum Tree Creek Volcanics. Unconformably overlies El Sherana Group; unconformable under Katherine River Group. Felsic volcanics, conglomerate, sandstone. Age: ~1822 Ma. Geol. Prov: Pine Creek Orogen.||||||09-FEB-10
5978|Edith River Group|65340|6|Mentioned|p9.|||Arnhem Shelf, McArthur Basin.||||||
5978|Edith River Group|65390|6|Mentioned|p27 Fig. 6|Paleoproterozoic|Paleoproterozoic|Pine Creek Inlier. Figure 6 infers age is between about 1850 and 1650 Ma.||||||
5978|Edith River Group|66683|6|Mentioned|p367.|||Deposition in a rift-related half-graben.|1825 Ma.|||||
5978|Edith River Group|67323|6|Mentioned|Eastern Australia Time-Space Plot|||Pine Creek area.||||||
5978|Edith River Group|67355|6|Mentioned|p5-6, p7 Tb.2||Orosirian|Previously part of the Katherine River Group. Rift fill dominated by volcanic intervals synchronous with felsic plutonic activity.|1826 Ma (SHRIMP)|||Coeval with Cullen Supersuite and David Suite. Underlies the Katherine River Group, overlies the El Sherana Group.||25-JAN-17
5978|Edith River Group|67479|5|Briefly described|p6 Fig.2, p58|Orosirian|Orosirian||1829-1825 Ma||||Felsic extrusive volcanic rocks.|24-JAN-17
5978|Edith River Group|67564|3|Fully described|p iv, p7 Table 2, p9 Fig.4, pp29-30.|Paleoproterozoic|Paleoproterozoic|Jawoyn Sub-basin. Formerly Edith River Volcanics. Bimodal volcanic and fluviatile volcaniclastic sedimentary rocks, up to 1000 m thick. Correlative of Allia Creek Suite and Cullen Supersuite to the west, and David Suite to the east. Mildly deformed. An ignimbrite in Plum Tree Creek Volcanics is aged 1825 +/- 4 Ma.|Between 1830 - 1723 Ma.||Includes Kurrundie, Hindrance Creek and Phillips Creek Sandstones and Plum Tree Creek Volcanics.|Unconformably overlies El Sherana Group and Masson Formation. Is unconformably overlain by Mamadawerre Sandstone.|Bimodal volcanic rocks, conglomerate, sandstone.|
5978|Edith River Group|67779|4|Described|p5 Fig.4(b), p6 Fig.5, p8 Table 1, p30.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Sub-aerial valley fill deposits. Their ages suggest that this unit, the Cullen Supersuite granites and the Nabarlek Granite formed as part of the same thermal event.|1825 +/- 4 Ma (Page, 1996a).||Includes Hindrance Creek, Kurrundie and Phillips Creek Sandstones, and Plum Tree Creek Volcanics.|Is overlain unconformably by Kombolgie Subgroup.|Rhyolite, quartz rhyolite, dacite, minor mafic volcanics; lenses of ignimbrite and tuffaceous sandstone; finely laminated tuffaceous siltstone.|
5978|Edith River Group|69417|5|Briefly described|p2:4-5|Orosirian|Orosirian|Pine Creek Orogen.|1825-1810 Ma.|||Is intruded by Cullen Supersuite.|Sandstone, felsic volcanic rocks.|12-JUL-16
5978|Edith River Group|69419|6|Mentioned|p4:2 Fig.4.2|||||||||12-JUL-16
5978|Edith River Group|69420|4|Described|p5:2, 4-7, 14-17, 23, 38-39, 62, 66, 79|Paleoproterozoic|Paleoproterozoic|See also 85, 100, 111, 115. Central Domain, Pine Creek Orogen. As in Needham and Stuart-Smith (1984). Formerly Edith River Volcanics (as in Walpole et al.,1968). Deposition in fault-bounded shallow grabens. Has no auriferous veins.|c.1825 Ma.||Hindrance Creek, Kurrundie, Phillips Creek Sandstones; Plum Tree Creek Volcanics.|Disconformably overlies El Sherana Group.||12-JUL-16
5978|Edith River Group|69424|6|Mentioned|p9:4|||Pine Creek Orogen.||||Time-correlative of Ooradidgee Group.||12-JUL-16
5978|Edith River Group|69430|5|Briefly described|p15:3-5, 7|||Pine Creek Orogen.|1822 +/- 6 Ma.|||Is overlain unconformably by Katherine River Group. A likely correlative of Bickerton Rhyolite.||12-JUL-16
5978|Edith River Group|69577|6|Mentioned|p117 Fig.6|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||||||
5978|Edith River Group|69673|6|Mentioned|p16 fig 13|Orosirian|Orosirian|Northwestern McArthur Basin.|1822 +/- 6 Ma|||||
5978|Edith River Group|70293|4|Described|p597-599, p613, p615, p619-620|Orosirian|Orosirian|Unmetamorphosed and only mildly folded sedimentary rocks. Deposition was terminated by the 1800-1780 Ma Shoobridge Event.|1835 - 1825 Ma||Plum Creek Volcanics, Kurrundie Sandstone.|Unconformably overlies El Sherana Group. Is overlain by Kombolgie Subgroup.|Basal lithic quartz sandstone and polymictic conglomerate, overlain by felsic and minor mafic volcanic rocks, and lenses of quartz sandstone.|
5978|Edith River Group|71256|6|Mentioned|p18 Fig 1|||||||||
5978|Edith River Group|71374|5|Briefly described|p2|||northern McArthur Basin.||||Broadly equivalent to the Tawalah Group.||
5978|Edith River Group|71606|5|Briefly described|p137|Paleoproterozoic|Paleoproterozoic|West Arnhem Shelf, McArthur Basin. ||||Overlain unconformably by Katherine River Group. Coeval with Pine Creek Granites.||
5978|Edith River Group|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Part of the early Basin volcanism and plutonism in the McArthur Basin. Mapped with El Sherana Group as a single unit.|||||Felsic volcanics, sandstone, mudstone, conglomerate; minor basalt.|
5978|Edith River Group|72373|5|Briefly described|p2|Paleoproterozoic|Paleoproterozoic|Broadly equivalent to Redbank package, Tawallah Group (central/southern McArthur Basin), Birrindudu and Tolmer groups (Birrindudu Basin) and Tomkinson Creek and Hatches Creek groups (Tomkinson Province).||||||
5978|Edith River Group|73089|6|Mentioned|p32, p38, p42|Orosirian|Orosirian|Pine Creek Orogen, Central Domain. Bimodal character may suggest an extensional setting for 1829-1822 Ma igneous rocks.|[c.]1840-1815 Ma|||Correlates[?] to Ware Group.|Includes felsic volcanic and lesser basaltic rocks.|
6073|Elkera Formation|9394|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Georgina Basin. Of the Mopunga Group. Interbedded siltstone, dolomite, sandstone and shale; stromatolitic dolomite at top. Underlies: Errarra beds. Overlies: Grant Bluff Formation.||||||01-NOV-04
6073|Elkera Formation|9694|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Mopunga Group. Geological Province: Georgina Basin. Underlies: Errarra Formation, Mount Baldwin Formation. Overlies: Grant Bluff Formation.||||||
6073|Elkera Formation|12951|5|Briefly described|p143,  fig 4|Neoproterozoic|Neoproterozoic|Georgina Basin.||Top of the Mopunga Group.||Correlates with lower Arumbera Sandstone of Amadeus Basin. Unconformably overlain by Mount Baldwin Formation, Adam Shale.|Silty turbidites.|
6073|Elkera Formation|22646|6|Mentioned|p 101|Neoproterozoic|Neoproterozoic|Informal name - lower Elkera Formation used p 101.  Situated in the Georgina Basin.||||||07-MAY-13
6073|Elkera Formation|23314|5|Briefly described|331 Fig.2|||||||||
6073|Elkera Formation|24111|5|Briefly described|p216|Neoproterozoic|Neoproterozoic|Geological Province: Georgina Basin.||||||24-MAR-05
6073|Elkera Formation|38157|6|Mentioned|Table IX|||||||||
6073|Elkera Formation|40538|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Mopunga Group. Siltstone to sandstone, micaceous, laminated to thin bedded, blue grey to dusky red; dolostone horizons. Geological Province: Georgina Basin.||||||15-NOV-05
6073|Elkera Formation|40906|4|Described|p56|||||||||
6073|Elkera Formation|41005|6|Mentioned|Fig.2|||||||||
6073|Elkera Formation|41801|5|Briefly described|p215|||See also p218.||||||15-AUG-06
6073|Elkera Formation|42059|6|Mentioned|Fig.2 P131|||||||||
6073|Elkera Formation|42504|5|Briefly described|Table 4 P73|||||||||
6073|Elkera Formation|42643|6|Mentioned|p21|||||||||
6073|Elkera Formation|42956|5|Briefly described|p29|||Of Mopunga Group.||||||15-AUG-06
6073|Elkera Formation|47035|6|Mentioned|p85|||||||||
6073|Elkera Formation|48990|2|Defined|p10|Adelaidean|Adelaidean|||||||19-APR-22
6073|Elkera Formation|60122|6|Mentioned|p9|||Formerly of the Grant Bluff Formation but excluded with revision of the unit (Walter 1980).  In the Supersequence 4.||||||15-AUG-06
6073|Elkera Formation|60551|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Mopunga Group. Geological province: Georgina Basin. Underlies: Mount Baldwin Formation, Errarra Formation. Overlies: Grant Bluff Formation. Interbedded siltstone, dolomite, sandstone and shale, stromatolitic dolomite.||||||17-NOV-04
6073|Elkera Formation|61022|5|Briefly described|p15 Fig. 2|Neoproterozoic|Neoproterozoic|Geological Province: Georgina Basin. Named in abstract for: Carbonate ramp facies and oil plays in Late Cambrian-southern Georgina Basin (abstract) by Ambrose, G.J. and Putnam, P.E.||||||20-APR-05
6073|Elkera Formation|61404|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Mopunga Group. Siltstone, sandstone: micaceous, laminated to thin-bedded; minor dolostone, some stromatolitic. Age: Ediacaran.  Geological Province: southern Georgina Basin.||||||
6073|Elkera Formation|61732|3|Fully described|p5 Tb. 1, p109-110|Ediacaran|Ediacaran|Of Mopunga Gp. Overlies Grant Bluff Fm; underlies Central Mount Stuart Fm ( according to Fig. 40 but stated to be unconformably beneath Mount Baldwin Fm. p109). Thick: 270m. Geol.Prov: Georgina Basin. See also p65,  p106.||||||07-FEB-11
6073|Elkera Formation|62376|5|Briefly described|p53|Early Cambrian|Neoproterozoic|Geological Province: Georgina Basin||||||09-FEB-10
6073|Elkera Formation|62984|5|Briefly described|p14|Neoproterozoic III|Neoproterozoic III|Of the Mopunga Group. Overlies Grant Bluff Formation; overlain by and intertongues with lower Central Mount Stuart Formation. Geological Province: Georgina Basin. Consists of carbonates, immature clastics and evaporites.||||||23-JAN-07
6073|Elkera Formation|63562|6|Mentioned|p338 fig 3, p345 fig 7, p352 Fig.10|Ediacaran|Ediacaran|Of Georgina Basin.||||Overlies Grant Bluff Formation.||
6073|Elkera Formation|64068|3|Fully described|p51, 52, 55,  viii|Ediacaran|Ediacaran|Of Mopunga Group. Formerly included in upper part of Grant Bluff Formation of Smith (1964). See also Tops Member of Central Mount Stuart Formation.||Of Mopunga Group.||Conformable on Grant Bluff Formation. Is disconformably overlain by Mount Baldwin Formation or Red Heart Dolostone.|Interbedded siltstone and dolostone, locally stromatolitic; quartz arenite to shale, locally evaporitic.|07-MAY-13
6073|Elkera Formation|64724|5|Briefly described|p49 Fig. 7|Ediacaran|Ediacaran|Deposited in the Georgina Basin during the Centralian 3 event (~600-544 Ma)||||||
6073|Elkera Formation|64812|5|Briefly described|p237 Fig. 2|Neoproterozoic|Neoproterozoic|Geological Province: southern Georgina Basin.||||||07-FEB-11
6073|Elkera Formation|64813|5|Briefly described|p256 Fig. 3|Neoproeterozoic|Neoproterozoic|Unconformably overlain by Mount Baldwin Formation. Geological Province: southern Georgina Basin.||||||11-FEB-09
6073|Elkera Formation|65237|5|Briefly described|p5|||Of Mopunga Gp. Overlies Grant Bluff Fm; unconformably overlain by Mount Baldwin Fm in the south. Geol.prov: southern Georgina Basin. Immature clastic rocks + evaporites; silty, turbiditic rocks. Correlates with lower Arumbera Sandstone in Amadeus Basin||||||07-FEB-11
6073|Elkera Formation|65338|5|Briefly described|p iv, pp63-64.|Ediacaran|Ediacaran|This unit has not been mapped separately from the Central Mount Stuart Formation in MOUNT PEAKE.||Unit in Mopunga Group.||Is overlain by Central Mount Stuart Formation.|Carbonate, clastic and evaporitic rocks.|
6073|Elkera Formation|65341|6|Mentioned|p2 Fig.2, p16. |||||Unit in Mopunga Group.||Is overlain by Mount Baldwin Formation.||
6073|Elkera Formation|69437|5|Briefly described|p22:4-5, 7-8|Ediacaran|Ediacaran|SE Georgina Basin, Centralian A Superbasin. Supersequences 3 & 4. Peritidal to shallow-marine deposits.||Mopunga Group.||Overlies Grant Bluff Formation. Upper part is correlated with Central Mount Stuart Formation.||12-JUL-16
6073|Elkera Formation|69438|6|Mentioned|p23:20|||Georgina Basin.||||Correlated with Julie Formation (Amadeus Basin).||12-JUL-16
6073|Elkera Formation|69443|4|Described|p28:7, 10-11, 15|Ediacaran|Ediacaran|Walter (1980); modified by Freeman (1986) who included the silty sandstone/granule orthoquartzite where the stromatolitic dolostone is absent. Southern Georgina Basin. Generally recessive. 70-270m thick. Partial lateral equivalent of Andagera and Central Mount Stuart Formations. Peritidal to shallow-marine deposits.||Mopunga Group.||Conformably and gradationally overlies Grant Bluff Formation. Is overlain conformably by Central Mount Stuart Formation, and disconformably by Mount Baldwin Formation or Red Heart Dolostone.|A succession of interbedded siltstone, quartz sandstone to sublithic sandstone, and shale; capped by dolostone (locally with columnar stromatolites) which is locally evaporitic. Locally includes a silty sandstone and a granule orthoquartzite bed.|12-JUL-16
6073|Elkera Formation|69673|5|Briefly described|p114 fig 92, p115|Ediacaran|Ediacaran |270m thick.||Mopunga Group||Overlies Grant Bluff Formation, overlain by Andagera Formation|Interbedded siltstone, sandstone and shale, capped by dolostone.|
6073|Elkera Formation|71621|5|Briefly described|p30|||Of Georgina Basin. Said to have an unconformable and in part faulted contact with the Xanten Granodioritie [although the exact nature of this contact isn't provided].||||||02-FEB-19
6073|Elkera Formation|71800|6|Mentioned|p26 fig 3|Ediacaran|Ediacaran|Georgina Basin.||||Overlies the Grant Bluff Formation.||
6073|Elkera Formation|72515|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Jervois Range Special Map Sheet. Georgina Basin. Contains rare halite pseudomorphs; ichnofossils, local columnar stromatolites, microbial mat fragments.||Mopunga Group||Overlies the Grant Bluff Formation.|Interbedded siltstone, dolostone; quartz-arenite, sublitharenite, mudstone; granule quartz sandstone; planar bedded, low-angle cross stratified; micaceous.|
6073|Elkera Formation|72516|3|Fully described|p12-13, p15-16, p61, p87-90|Ediacaran|Ediacaran|Georgina Basin, occurs in HUCKITTA, northeastern ALCOOTA and MOUNT PEAKE map sheets in addition to the JERVOIS RANGE SPECIAL. Outcrops along the Jervois and Johansen ranges. Type section is defined at Valley Bore in Jervois Range (Walter, 1980).  Based on new field work rocks previously assigned to the Grant Bluff Formation in the Charlotte Fault Zone are reassigned to this unit.  Contains ichnofossils, local columnar stromatolites and microbial mat fragments. 270m thick, 70m thick in Jinka. Deposited in a peritidal to shallow marine environment. Faulted against the Oorabra Arkose. Equivalent to the Central Mount Sutart Formation and the Julie Formation. See also  p95, p154-155, p173, p186, p218.||Mopunga Group||Conformably to gradationally overlies the Grant Bluff Formation. Unconformably overlies the Thring Granite. Disconformably overlain by the Mount Baldwin Formation or the Red Heart Dolostone.|Interbedded siltstone, dolostone; quartz-arenite, sublitharenite, mudstone; granule quartz sandstone; planar bedded, low-angle cross-stratified; micaceous; rare hailte pseudomorphs.|19-APR-22
6073|Elkera Formation|73086|6|Mentioned|p133|||Georgina Basin.||||Correlates to Julie Formation.||
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.||||||
6118|Elyuah Formation|9394|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Georgina Basin. Of the Mopunga Group. Brown and green shale, basal pebbly conglomerate. Underlies: Grant Bluff Formation. Overlies: Arunta Block units.||||||01-NOV-04
6118|Elyuah Formation|9694|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Mopunga Group. Geological Province: Georgina Basin. Underlies: Grant Bluff Formation. Overlies: Oorabra Arkose. Shale, pebbly sandstone.||||||
6118|Elyuah Formation|22646|6|Mentioned|Fig 4 on p 102|Neoproterozoic|Neoproterozoic|Georgina Basin.  Age - Ediacarian in text.||||||
6118|Elyuah Formation|22649|5|Briefly described|p 152|||Consists of mudrocks ressembling the Peratatataka Formation.  Province - Georgina Basin.||||||
6118|Elyuah Formation|22762|6|Mentioned|p362|||Geological Province - Georgina Basin.||||||
6118|Elyuah Formation|23844|5|Briefly described|p37|Neoproterozoic|Neoproterozoic|Geological Province: Georgina Basin.||||||30-SEP-08
6118|Elyuah Formation|24047|6|Mentioned|p105 Appendix 1|||Geological Province: Georgina Basin.||||||
6118|Elyuah Formation|24442|6|Mentioned|p49|||Geological Province: Georgina Basin.||||||
6118|Elyuah Formation|33111|6|Mentioned|p38|||||||||
6118|Elyuah Formation|35005|5|Briefly described|p145|||||||||
6118|Elyuah Formation|37572|5|Briefly described|p154|||See also Fig.8||||||
6118|Elyuah Formation|38157|6|Mentioned|Table IX|||||||||
6118|Elyuah Formation|39210|4|Described|p51|||||||||
6118|Elyuah Formation|40538|6|Mentioned|Map legend|Adelaidean|Adelaidean|Of the Mopunga Group. Shale with interbeds of silty sandstone and a basal pebble conglomerate. Geological Province: Georgina Basin.||||||15-NOV-05
6118|Elyuah Formation|40906|4|Described|p21|||||||||
6118|Elyuah Formation|41005|6|Mentioned|Fig.2|||||||||
6118|Elyuah Formation|41429|6|Mentioned|p247|||||||||
6118|Elyuah Formation|41801|6|Mentioned|p218|||||||||
6118|Elyuah Formation|42059|6|Mentioned|Fig.2 P131|||||||||
6118|Elyuah Formation|42504|5|Briefly described|Table 4 P73|||||||||
6118|Elyuah Formation|42643|6|Mentioned|Fig.4 P19|||||||||
6118|Elyuah Formation|44327|14|Not recorded|p.7,8,18|||(F53-11). Tb.I. part of Mopunga Gp. basal arkose, sh.slight disconf.on Mt.Cornish Fm.&unconf. on PreCamb.metamorphic & igneous rocks.||||||
6118|Elyuah Formation|44328|14|Not recorded|map legend|Early Cambrian|Neoproterozoic|||||||15-AUG-06
6118|Elyuah Formation|45052|4|Described|p68|Adelaidean|Adelaidean|Unit of Mopunga Group.||||||30-SEP-08
6118|Elyuah Formation|45102|6|Mentioned|p45|||See also p49.||||||15-AUG-06
6118|Elyuah Formation|45155|6|Mentioned|Fig.7|||Georgina Basin||||||
6118|Elyuah Formation|48844|2|Defined|p.20-30||Neoproterozoic|On many pages. p.1,16,17,20-30, F.14,26,58,67, Pl.8. (new name). U.Proterozoic. Contains Oorabra Arkose Mem.Overlain by Grant Bluff Fm. Correl.with Pertatataka Fm. (F53-11).||||||15-AUG-06
6118|Elyuah Formation|48901|14|Not recorded|Not recorded||Adelaidean|Pt. Mopunga Gp. Defn on Tech.File F/53-11.||||||
6118|Elyuah Formation|48990|1|Redefined|p11|Adelaidean|Adelaidean|||||||
6118|Elyuah Formation|49036|6|Mentioned|p6|||||||||
6118|Elyuah Formation|60122|4|Described|p12-13|Neoproterozoic|Neoproterozoic|Of the Mopunga Group. Redefined by Walter (1980) to exclude the then constituent Oorabra Arkose Member.  Disconformably overlies Wonnadinna Dolostone an||||||13-MAR-17
6118|Elyuah Formation|60551|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Mopunga Group. Geological province: Georgina Basin. Underlies: Grant Bluff Formation. Overlies: Oorabra Arkose. Basal pebbly sandstone, brown and green shale.||||||
6118|Elyuah Formation|60590|5|Briefly described|Map legend|Cryogenian|Cryogenian|Of the Mopunga Group.  Mudstone, siltstone; thin basal sandstone or pebbly arkose (Keepera Ridges only).||||||
6118|Elyuah Formation|60668|5|Briefly described|Fig. 23a|||Quartz arenite and quartz greywacke.  Geological Province: Georgina Basin. ||||||
6118|Elyuah Formation|61388|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of the Mopunga Group. Dark grey to black mudstone with thin fine-grained sandstone interbeds; basal conglomerate. Geological Province: Georgina Basin.||||||
6118|Elyuah Formation|61404|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Mopunga Group. Mudstone, siltstone; thin basal sandstone or pebbly arkose.  Age: Ediacaran.  Geological Province: southern Georgina Basin.||||||11-OCT-05
6118|Elyuah Formation|61732|3|Fully described|p5 Tb. 1, p108|Ediacaran|Ediacaran|Of Mopunga Gp. Formerly included Oorabra Arkose which is now excluded from this unit. Transitionally overlain by Grant Bluff Fm. Max. thickness: 90m (est.). Geol.Prov: Georgina Basin. See also p106, p108 Fig. 40.||||||13-MAR-17
6118|Elyuah Formation|62642|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Mopunga Group. Geological Province: Georgina/Ngalia Basin. Shale, interlaminated, fissile chocolate brown and green; interbedded carbonate rocks.||||||
6118|Elyuah Formation|62984|5|Briefly described|p14|Neoproterozoic III|Neoproterozoic III|Of the Mopunga Group. Overlain by Grant Bluff Formation. Geological Province: Georgina Basin. Includes black mudstones.||||||23-JAN-07
6118|Elyuah Formation|63562|6|Mentioned|p338 fig 3, p352 Fig.10|Ediacaran|Ediacaran|Of Georgina Basin. Mis-spelt as Eluyah in Fig.7.||||Overlies Oorabra Arkose. Is overlain by Grant Bluff Formation.||
6118|Elyuah Formation|64068|3|Fully described|p49, p162, p19, p viii,  p x|Ediacaran|Ediacaran|Hosts galena mineralisation. Shales give this unit a moderately high, K-dominant radiometric signature. Unconformable on Palaeoproterozoic units.||Of Mopunga Group.||Disconformable above Boko Formation, Oorabra Arkose. Conformable above Gnallan-a Gea Arkose. Comformably and gradationally overlain by Grant Bluff Formation.|Green, red and grey micaceous shale and siltstone; minor quartz sandstone in outcrop; thin basal sandstone or pebbly arkose.|04-APR-12
6118|Elyuah Formation|65237|5|Briefly described|p5|||Basal unit of the Mopunga Group. Gradational with Grant Bluff Formation above. Geological province: southern Georgina Basin. Black mudstone.||||||07-FEB-11
6118|Elyuah Formation|65338|4|Described|p iv, p62, p64.|Ediacaran|Ediacaran|Georgina Basin. Locally interdigitates with Gnallan-a-gea Arkose. Typically recessive or non-outcropping.||Unit in Mopunga Group.||Dis- or un-conformably overlies Boko Formation. Is overlain by Grant Bluff Formation.|Laminated, fissile, black, chocolate brown to green, predominantly micaceous shale; locally a basal arkosic pebble conglomerate; intervals of calcrete; interbedded, fine-grained, flaggy sandstone.|
6118|Elyuah Formation|65341|5|Briefly described|p5, pp14-15. |||Shallow marine, mostly below wave base, depositional environment. Very recessive and rarely exposed.||Unit in Mopunga Group.||Unconformably overlies Oorabra Arkose and Boko Formation. Is overlain conformably by Grant Bluff Formation.|Subsurface: dark grey to black micaceous mudstone with thin, fine-grained micaceous sandstone interbeds, basal conglomerate; surface: rare outcrop of red and white mudstone.|
6118|Elyuah Formation|67164|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Georgina/Ngalia Basins.||Unit in Mopunga Group.||Is overlain by Grant Bluff Formation.|Shale, interlaminated, fissile chocolate-brown and green; interbedded carbonate rocks.|
6118|Elyuah Formation|67892|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|||Unit in Mopunga Group.||Is overlain by Grant Bluff Formation.|Shale, interlaminated, fissile chocolate brown and green; interbedded carbonate rocks.|
6118|Elyuah Formation|69437|5|Briefly described|p22:4-5, 7|Ediacaran|Ediacaran|SE Georgina Basin, Centralian A Superbasin. Supersequence 3.||Mopunga Group.||Is overlain by Grant Bluff Formation.||12-JUL-16
6118|Elyuah Formation|69443|5|Briefly described|p28:7, 9-10, 34|Ediacaran|Ediacaran|Southern Georgina Basin. Associated with epigenetic base metal mineralisation in Mount Skinner area.||Mopunga Group.||Overlies Boko Formation unconformably, and Gnallan-a-Gea Arkose gradationally (also interdigitates with it). Is overlain by Grant Bluff Formation.||12-JUL-16
6118|Elyuah Formation|69673|5|Briefly described|p114 fig 92, p115|Ediacaran|Ediacaran |210m thick.||Mopunga Group||Overlain by Grant Bluff Formation|Shale and siltstone.|
6118|Elyuah Formation|71800|6|Mentioned|p26 fig 3|Ediacaran|Ediacaran|Georgina Basin.||||Overlain by the Grant Bluff Formation.||
6118|Elyuah Formation|72515|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Jervois Range Special Map Sheet. Georgina Basin. Contains intermediate spheroidal acritarchs, large organic amorphous fragments.||Mopunga Group||Overlain by the Grant Bluff Formation.|Basal sandstone, pebbly arkose, conglomerate, laminated micaceous shale, siltstone, interbedded black micaceous shale, micaceous sandstone, minor quartz sandstone.|
6118|Elyuah Formation|72516|3|Fully described|p13, 15-16, p63, p88|Ediacaran|Ediacaran|Georgina Basin. On the JERVOIS RANGE SPECIAL outcrops as a recessive unit. Type section is located near the eastern end of the Dulcie Range in northern JINKA. Contains intermediate spheroidal acritarchs; large organic amorphous fragments. 82-108m thick. Deposited in a low-energy, shallow to moderately deep-marine environment. Petrography and fossils are discussed.  Equivalent to the Gnallan-a-Gea Arkose of the southern Georgina Basin and the lower Pertatataka Formation of the Amadeus Basin. See also p186, p188, p218.||Mopunga Group||Disconformably overlies the Oorabra Arkose; unconformably overlies the Unca Granite. Conformably overlain by the Grant Bluff Formation.|Basal sandstone, pebbly arkose, conglomerate; laminated micaceous shale, siltstone; interbedded black micaceous shale, micaceous sandstone; minor quartz sandstone.|19-APR-22
6118|Elyuah Formation|73086|6|Mentioned|p118, p122|||Georgina Basin, south-eastern.||||Possibly correlates to Gaylad Sandstone and Pertatataka Formation.||
6134|Emily Gap Schist|9199|5|Briefly described|Map legend|Precambrian|Precambrian|Of the Hayes Complex.  Biotite-feldspar-quartz schist.  Geological Province: Arunta Block.||||||05-NOV-04
6134|Emily Gap Schist|41664|6|Mentioned|Map legend|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
6134|Emily Gap Schist|41816|6|Mentioned|p7|||||||||
6134|Emily Gap Schist|60547|5|Briefly described|Map Legend|Precambrian|Precambrian|Of the Hayes Complex. Geological Province: Arunta Block. Biotite-feldspar-quartz schist.||||||
6134|Emily Gap Schist|69427|5|Briefly described|p12:14-16|||Wigley Domain, Aileron Province.||Hayes Metamorphic Complex.|||Biotite-muscovite schist, schistose metasandstone and amphibolite.|12-JUL-16
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|
6192|Eninta Sandstone|22651|6|Mentioned|p 174|||equivalent to Arumbera Sandstone.||||||
6192|Eninta Sandstone|29721|6|Mentioned|p44|||||||||
6192|Eninta Sandstone|31973|6|Mentioned|p3|||Correlation||||||
6192|Eninta Sandstone|33307|6|Mentioned|Fig.6|||||||||
6192|Eninta Sandstone|34442|5|Briefly described|Table 1|||Camb.||||||
6192|Eninta Sandstone|35088|6|Mentioned|p96|||||||||
6192|Eninta Sandstone|35102|6|Mentioned|Fig.2|||||||||
6192|Eninta Sandstone|35136|6|Mentioned|p140|||||||||
6192|Eninta Sandstone|36198|6|Mentioned|p294|||See also Fig.III.2||||||
6192|Eninta Sandstone|39213|6|Mentioned|Fig.6|||Amadeus Basin Succession||||||
6192|Eninta Sandstone|40740|5|Briefly described|p12|||||||||
6192|Eninta Sandstone|40810|6|Mentioned|p3|||||||||
6192|Eninta Sandstone|40852|6|Mentioned|Fig.3.7|||||||||
6192|Eninta Sandstone|41224|6|Mentioned|Fig.2|||||||||
6192|Eninta Sandstone|41233|5|Briefly described|p16|||Is considered to belong to Arumbera Sandstone||||||
6192|Eninta Sandstone|42141|6|Mentioned|Table 2 P571|||||||||
6192|Eninta Sandstone|43011|6|Mentioned|Table 2,p12|||||||||
6192|Eninta Sandstone|43649|6|Mentioned|p457|||||||||
6192|Eninta Sandstone|43781|6|Mentioned|p4|||||||||
6192|Eninta Sandstone|44402|5|Briefly described|map legend||Cambrian|Part of Pertaoorrta Group.||||||02-DEC-04
6192|Eninta Sandstone|44484|14|Not recorded|p.10,14, Tb.1||Cambrian|Part of Pertaoorrta Group.||||||
6192|Eninta Sandstone|44485|14|Not recorded|map legend||Cambrian|Part of Pertaoorrta Group.||||||
6192|Eninta Sandstone|44497|4|Described|p.9, Table 1||Cambrian|SF/53-13.||||||
6192|Eninta Sandstone|44498|14|Not recorded|map legend||Cambrian|Part of Pertaoorrta Group.||||||
6192|Eninta Sandstone|45041|4|Described|p52|||||||||
6192|Eninta Sandstone|45155|6|Mentioned|p28|||See also P34||||||
6192|Eninta Sandstone|46903|6|Mentioned|Fig.3|||Magnetic polarity sequences||||||
6192|Eninta Sandstone|48863|14|Not recorded|Not recorded|||||||||
6192|Eninta Sandstone|48865|14|Not recorded|Not recorded|||||||||
6192|Eninta Sandstone|48963|6|Mentioned|Fig.3|||||||||
6192|Eninta Sandstone|61385|5|Briefly described|Map legend|Cambrian|Cambrian|Red brown sandstone, silty sandstone.  Geological Province: Amadeus Basin.||||||20-OCT-05
6192|Eninta Sandstone|64068|6|Mentioned|p224|||Amadeus Basin. Correlated with Shadow Group, Georgina Basin.||||||
6192|Eninta Sandstone|67565|6|Mentioned|p39.|Early Cambrian|Neoproterozoic|These strata, previously mapped (Ranford, 1969) in the Gardiner Range, are now included in the Arumbera Sandstone.||||||
6192|Eninta Sandstone|69437|6|Mentioned|p22:10|Cambrian|Cambrian|Amadeus Basin.||||||12-JUL-16
6192|Eninta Sandstone|69438|4|Described|p23:3, 24, 27, 53|Early Cambrian|Early Cambrian|Wells et al. (1965). Forms a prominent strike ridge in the Gardiner Range Anticline, Amadeus Basin. The type area was defined in MOUNT LIEBIG map, but the unit is subsumed into Arumbera Sandstone.||Pertaoorrta Group.|||Sandstone with minor siltstone and conglomerate. Generally thin-bedded, cross-bedded, micaceous, feldspathic and immature. Local beds of conglomerate, with clasts predominantly of chert and carbonate rocks.|12-JUL-16
6192|Eninta Sandstone|69443|6|Mentioned|p28:14|||Amadeus Basin.||||Correlated with (part of) the Shadow Group.||12-JUL-16
6192|Eninta Sandstone|72369|5|Briefly described|p20-21|||Of Amadeus Basin. Possibly correlable to Puna Kura Kura Formation.||Unit of Pertaoorrta Group.||||
6192|Eninta Sandstone|72374|5|Briefly described|iii,p3-4,12-14|Early Cambrian|Neoproterozoic|Of Amadeus Basin. Typically thinly-bedded, crossbedded, micaceous, feldspathic and immature (Edgoose 2013), with basal conglomerates. Originally mapped and interpreted to be laterally equivalent to Arumbera Sandstone and Quandong Conglomerate (Ranford and Cook, 1964). Sample HB16ND276 (sandstone) yielded an interpreted maximum depositional age of 1021+\-9 Ma. Dominant zircon population between c. 1205 to 1000 Ma (peak c. 1162 Ma) likely derived from Musgrave Province (either directly or reworking from underlying stratigraphy). Subordinate c. 1900-1380 Ma zircon age spectrum likely sourced from the Aileron and Warumpi provinces to the north, and Musgrave Province to the south. Archean c. 2756-2400 Ma zircons likely sourced from terranes from east Gondwana, or the North Australian Craton.||Unit of Pertaoorrta Group.|||Sandstone with minor siltstone and conglomerate.|11-OCT-19
6195|Ennugan Mountains Granite|23809|5|Briefly described|p46, p41 Tb. 5|Proterozoic|Proterozoic|Foliated granite.  Intrudes Lander Rock beds.  Age: 1622+/-7Ma.  Geological Province: Arunta Province.||||||
6195|Ennugan Mountains Granite|24197|5|Briefly described|p61 Tb. 4.1|Mesoproterozoic|Paleoproterozoic|Of the Ennugan Mountains Suite. Age: 1600Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
6195|Ennugan Mountains Granite|24540|6|Mentioned|p8|||See also Ennugan Granite. Age: 1622Ma (Smith 2000).||||||07-FEB-11
6195|Ennugan Mountains Granite|42326|5|Briefly described|Table 2 P11|||||||||
6195|Ennugan Mountains Granite|50369|5|Briefly described|p1.5, 23.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Ennugan Mountains Suite. Age: 1600 +/- 7Ma (Sm-Nd).||||||07-NOV-08
6195|Ennugan Mountains Granite|64329|5|Briefly described|p16|Proterozoic|Proterozoic|Allanite-bearing granite in the Arunta region. Seen as prospective for U-Th-REE.||||||29-JUL-08
6195|Ennugan Mountains Granite|65338|5|Briefly described|p5 Fig.3, p70, p73.|Paleoproterozoic|Paleoproterozoic|Penecontemporaneous with a final phase of granite and associated porphyry magmatism in MOUNT PEAKE and LANDER RIVER areas. Small concentrations of uranium associated with calcrete developed in the immediate subsurface.|c.1620 Ma.|||||
6195|Ennugan Mountains Granite|68998|4|Described|v, p1, p18-25, Appendix Tbs.5-8|||Beyer et al. (2012). Arunta Region; forms the Ennugan Mountains. Extensive unit. High heat-producing. Encloses several zones of strongly foliated biotite-muscovite-quartz rock that is U-Th-REE enriched; this was dated at 1615 +/- 3 Ma and represents altered and deformed Ennugan Mountains Granite. The cross-cutting granite dyke is dated at 1618 +/- 2 Ma. The Ennugan Mountains Granite was previously dated at 1622 +/- 7 Ma by Smith (2001).|1621 +/- 5 Ma.|||Intrudes the Lander Rock Formation. Is overlain by Vaughan Springs Quartzite.|Coarse-grained biotite porphyritic granite; cross-cut by fine-grained equigranular biotite granite dykes.|
6195|Ennugan Mountains Granite|69439|5|Briefly described|p24:5|Statherian|Statherian|Aileron Province. Mentioned as a possible source for sediments of the Vaughan Springs Quartzite. Zircon age.|1621 +/- 5 Ma (Beyer et al., 2012).|||||12-JUL-16
6195|Ennugan Mountains Granite|69794|6|Mentioned|iv, p7|Statherian|Statherian|Geological province: Aileron Province. Of Arunta region. Similar in age to Rapide Granite.||||||06-APR-20
6195|Ennugan Mountains Granite|69917|6|Mentioned|p117|||Exposed 50 km to the west of Central Mount Stuart Formation.||||||
6195|Ennugan Mountains Granite|69932|6|Mentioned|p303, 306-307, 311|||Northern Province, Arunta Inlier. Sm-Nd data tabulated. Only one Mountain on p307.|1600 Ma.||||Undeformed, coarse-grained, feldspar megacrystic, fluorite-bearing granite.|
6195|Ennugan Mountains Granite|70301|4|Described|v, p1, p26-30|Paleoproterozoic|Paleoproterozoic|Aileron Province, Arunta Region. Extensive unit. One of the highest heat-producing granites in the Province. Forms the Ennugan Mountains. First dated by Smith (2001) at 1622 +/- 7 Ma; confirmed by this result by Kositcin et al. (2013). The biotite schist was dated at 1615 +/- 3 Ma; probably represents altered and deformed Ennugan Mountains Granite.|1621 +/- 5 Ma (SHRIMP U-Pb zircon).|||Is overlain nonconformably by Vaughan Springs Quartzite. Intrudes Lander Rock Formation.|Metaluminous granite, co-magmatic microgranite dyke, and biotite schist (interpreted as metasomatically altered Ennugan Mountains Granite). I-type.|
6195|Ennugan Mountains Granite|71592|5|Briefly described|Appendix A.|||Arunta Orogen. Other ages given: 1622+/-7 Ma, 1618+/-2 Ma, 1615+/-3 Ma all U-Pb zircon SHRIMP igneous crystallisation.Also 1574+/-7 Ma U-Pb monazite SHRIMP igneous crystallisation. and  U-Pb monazite SHRIMP metamorphic age: 1606 +/- 2 Ma. Various sample lithologies.|1621+/-5 Ma (U-Pb zircon SHRIMP)||||Granite, quartz rock.|16-JUN-20
6195|Ennugan Mountains Granite|71858|2|Defined|iii, p2, p4, p44-p68, p70, p72|Statherian|Statherian|Aileron Province. Definition proposed by E.E. Beyer. Named for the Ennugan Mountains which it forms on the NAPPERBY 1:250k, Tea Tree and Reynolds Range 1:100k and MOUNT PEAKE 1:250k, Mount Peake 1:100k sheets. The type section locality is located at GDA94 53k 290342E 7554773N in the southern Ennugan Mountains which is also the site of sampling for SHRIMP geochronology in Kositcin et al, 2013; an additional two reference sections are provided. First investigated in 1968 as part of mapping of the first edition Napperby 1;250k sheet (Evans and Glikson 1969, Evans 1972). The unit was first named in Stewart et al, 1980a and fully defined in Stewart et al, 1980b. This units extent is interpreted from regional magnetics as an ellipsoid roughly 40km long and 15km wide. Contains numerous distinct phases. Age is an interpreted magmatic crystallisation age; An additional age of 1621 +/- 5 Ma is derived from this study. Considered prospective for REE mineralisation. Petrographic descriptions, geochemistry, identifying features, structure, metamorphism, alteration, mineralisation, geochronology analyses and results are discussed.|1622 +/- 7 Ma (Smith, 2011)|||Intrudes the Lander Rock Formation. Unconformably overlain by the Vaughan Springs Quartzite.|I-type biotite hornblende monzogranite including porphyritic biotite bearing granite.|
6195|Ennugan Mountains Granite|73399|6|Mentioned|p9|Statherian|Statherian|Intrudes greenschist to lower amphibolite-grade rocks.|ca. 1620 Ma|||||
6207|Entia Gneiss Complex|23205|6|Mentioned|p43|||||||||
6207|Entia Gneiss Complex|23732|5|Briefly described|p22, p29|Paleoproterozoic|Paleoproterozoic|Age: 1730+/-1Ma (U-Pb zircon; Cooper et al, 1998). See also p30 Fig.27 and p31 Fig.29.  Geological Province: Arunta Province.||||||07-NOV-08
6207|Entia Gneiss Complex|23868|6|Mentioned|p753|||Geological Province: Arunta Inlier.||||||
6207|Entia Gneiss Complex|41242|6|Mentioned|p237|||||||||
6207|Entia Gneiss Complex|41967|5|Briefly described|p236|||||||||
6207|Entia Gneiss Complex|61208|5|Briefly described|p214|Paleoproterozoic|Paleoproterozoic|Includes the Huckitta and Inkamulla Granodiorites. Age: 1775-1760Ma. ||||||07-NOV-08
6207|Entia Gneiss Complex|62595|4|Described|p4 Table 2, pp11-12, p34 Fig.15.|Statherian|Statherian|Crops out in the core of the Entia Dome. Is basement to Harts Range Group. Geochemistry is similar to calc-alkaline suites in modern continental arcs. SHRIMP ages from Maidment et al. (2005); conventional zircon dating gives ages between c.1765 and c.1730 Ma (Cooper et al. 1988; Foden et al. 1995).|1773 +/- 4 Ma and 1762 +/- 3 Ma.|||Is overlain by Bruna Gneiss.|Dominantly orthogneiss, ranging from ultramafic to granitic in composition, intruding a volumetrically minor supracrustal sequence of calc-silicate, quartzite, aluminous metapelite and amphibolite.|
6207|Entia Gneiss Complex|64337|4|Described|pp374-375|Proterozoic|Proterozoic|Proterozoic basement. Structurally underlies Harts Range Complex. Metamorphic fabric developed at c.700 degrees C and c.8 kbar. Recent geochronological results are discussed.|Metasediment protoliths > c.1750-1740.|||Structurally underlying Harts Range Complex, separated by the Harts Range Detachment Zone.|Supracrustal assemblage.|
6207|Entia Gneiss Complex|64574|4|Described|p705, p705 Fig. 2, p706, p709, p714|Paleoproterozoic|Paleoproterozoic|Age: >1767-1730. Composed of gabbroic to granitic orthogneiss with a minor sedimentary component.||||||08-JUL-13
6207|Entia Gneiss Complex|66767|5|Briefly described|p58|||Aileron Province. Exposed in the Entia Dome.||||Is structurally overlain by Bruna Gneiss.|Dominated by 1770-1760 Ma granites, with lesser Paleoproterozoic metasedimentary rocks. Pervasively reworked by amphibolite-facies high-strain fabric.|
6207|Entia Gneiss Complex|67181|4|Described|p631, p632|Statherian|Statherian|ca.1770 Ma from Maidment et al. (2005). Occurs in the Calcalkaline-trondhjemitic Group (geochemical grouping) of the Arunta Region and eastern Aileron Province, North Australian Craton. Granitoids (ca 1780 Ma) interpreted as I-type formed in a setting similar to continental margin magmatic arc (Foden et al. 1998).|c.1780-1760 Ma max depos. age (Wade et al. 2008) ||||Includes calc-silicates and metapelites, I-type granites.|
6207|Entia Gneiss Complex|67479|6|Mentioned|p46|Paleoproterozoic|Paleoproterozoic||||||Orthogneiss-dominated.|
6207|Entia Gneiss Complex|68316|5|Briefly described|p777, p778 Fig.1, p778|Paleoproterozoic|Paleoproterozoic|Cooper et al. (1988).|1.77-1.73 Ma|||Structurally overlain by the Harts Range Metamorphic Complex.|Comprises mainly felsic orthogneisses.|
6207|Entia Gneiss Complex|69227|5|Briefly described|p263, p282-283|Paleoproterozoic|Paleoproterozoic|Crops out in the Entia Dome, eastern Arunta Inlier. Separated from Harts Range Group by the Bruna Detachment Zone. Metamorphosed to granulite facies at c.1730 Ma, then strongly reworked at c.480-470 Ma.||Strangways Metamorphic Complex.||Structurally overlies Harts Range Complex.||
6207|Entia Gneiss Complex|69383|5|Briefly described|p4 Table 1, p60|||Arunta region, Aileron Province.  In part replaced by Bruna Gneiss? LA-ICPMS  U-Pb geochronology analyses. Crystallisation age. IC07JAW154 described as Bruna Gneiss p60-63 and age reported as 1745+/- 6 Ma. See also Entia Gniess p56, 61|1739+/-12 Ma??|||Overlain by Bruna Gneiss?||14-JUL-15
6207|Entia Gneiss Complex|69427|4|Described|p12:30-31, 33, 35-36|Statherian|Statherian|Formerly the Entia Gneiss (Joklik, 1955). Lithologies described in some detail. Separated from the structurally overlying Harts Range Metamorphic Complex by the Bruna Granitic Gneiss. LA-ICPMS detrital zircon maximum deposition age; other ages given. Complex metamorphic history: events at c.1773 Ma, c.1719 Ma and 340-320 Ma.|1766 +/- 7 Ma (Wade et al., 2008).||||Mainly meta-igneous rocks varying in composition from granite to granodiorite, diorite, tonalite and gabbro (highly strained, interleaved felsic orthogneiss and biotite orthogneiss with lesser mafic amphibolite), with subordinate supracrustal rocks.|12-JUL-16
6207|Entia Gneiss Complex|69917|6|Mentioned|p133, 140, 143, 145, 156, 167|||Shown as "Entia Gneiss Complex". Previous usage? Not clear whose. May have previously included rocks now divided into Entia Metamorphics, Valley Metamorphics and Ambulbinya Supersuite?||||Intruded by Oodnarta Diorite. Interpreted to be intruded by Huckitta Suite granodiorite.||28-JUL-15
6207|Entia Gneiss Complex|69925|6|Mentioned|p18, 39|||Central Arunta Province, Arunta Inlier. Presented as Entia Orthogneiss Complex. Associated with a 1770-1750 Ma intrusive episode (Strangways Event) involving granulite metamorphism and multiple ductile deformation.||||||
6207|Entia Gneiss Complex|69928|5|Briefly described|p210-214, 217-220, 222-225|||Central Tectonic Province, Arunta Inlier. Exposed as an inlier in the Entia Dome. Referred to as EGC after first appearance in text. Nd isotopic evolution diagram.|Between 1765 Ma and 1735 Ma.||Huckitta Granodiorite, Huckitta Tonalite.|Is intruded by Bruna granite gneiss.|Dominantly composed of intrusive orthogneisses ranging in composition from gabbro, diorite and tonalite, to granite. Amphibolite facies complex. Minor supracrustal units include quartzites and meta-pelites to metabasalt, marble and calc-silicate.|
6207|Entia Gneiss Complex|69931|6|Mentioned|p278|||Arunta Inlier.||||||
6207|Entia Gneiss Complex|69932|6|Mentioned|p310|||Provides geochemical evidence for 1780-1750 Ma cordillera-type igneous activity.||||||
6207|Entia Gneiss Complex|71348|6|Mentioned|p217|Statherian|Statherian|Geological province: Arunta region. |c 1770 Ma|||||
6207|Entia Gneiss Complex|72516|5|Briefly described|p121|||Part of the calc-alkaline-trondhjemitic group of Zhao and McCulloch (1995). Incorporated into the Ambulbinya Supersuite. Outcrops below the informal CAT-line in the eastern aileron province.|ca. 1770-1750 Ma|||||
6207|Entia Gneiss Complex|73184|6|Mentioned|p197|||Cross-cut by numerous pegmatites with SHRIMP U-Pb monazite and zircon ages of ca 450-300 Ma.||||||
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.|
6241|Erontonga Metamorphics|23844|6|Mentioned|p29|||||||||
6241|Erontonga Metamorphics|23983|5|Briefly described|p27|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
6241|Erontonga Metamorphics|23984|5|Briefly described|p3 Fig.2|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
6241|Erontonga Metamorphics|39470|6|Mentioned|p42|||||||||
6241|Erontonga Metamorphics|42830|6|Mentioned|Fig.3 p155|||||||||16-AUG-06
6241|Erontonga Metamorphics|66860|4|Described|p8, p11, p15-16, p18, p24, p35, p88-89|||Hosts Harry Creek base metal prospect; closely associated with marble lenses. 1800.6 +/- 3.3 Ma; 1809.8 +/- 4.0 Ma. Date for Pb isotopes. Other dates are younger. Not all outcrops are synchronous.  Metamorphism from 1735 - 1700 Ma from SHRIMP U-Pb dating of leucosomes and metamorphic rims.|1764.8 +/- 4 Ma.|Strangways Metamorphic Complex||Structurally overlies Utnalanama Granulite. Intruded by Johannsen Metagabbro. Is overlain by Cadney Metamorphics.|Contains marble lenses; cordierite-orthopyroxene quartzite.|
6241|Erontonga Metamorphics|69427|4|Described|p12:9-11, 24, 41, 52|Orosirian|Orosirian|Shaw et al. (1979). Strangways Range region, Aileron Province. Tightly folded unit of unknown thickness. Hosts the Utnalanama and Harry Creek base metal prospects. Previously thought to unconformably overlie Utnalanama Granulite. Hosts the Harry Ceek Zn(-Cu-Pb) deposit (detailed). SHRIMP U-Pb zircon dating of probable volcanic precursors.|1810 +/- 4 Ma.|Strangways Metamorphic Complex.||Is overlain by Cadney Metamorphics. Is intruded by Gumtree Granite, Utnalanama Granulite and Johannsen Metagabbro. Has faulted and gradational contacts with Ingula Migmatite.|Migmatitic quartzofeldspathic and cordierite-bearing pelitic gneiss, with rare calc-silicate, magnesian and manganiferous rocks and mafic granulite.|12-JUL-16
6241|Erontonga Metamorphics|71592|5|Briefly described|Appendix A.|||Arunta Orogen.|1801+/-3.3 Ma (U-Pb zircon SHRIMP)||||Quartzite, quartz-cordierite rock, quartz-cordierite gneiss.|
6241|Erontonga Metamorphics|71839|5|Briefly described|p10|||Outcrops in ALICE SPRINGS.||Strangways Metamorphic Complex||Intruded by the Gumtree Granite.||
6241|Erontonga Metamorphics|72711|6|Mentioned|p2, p4 Tb.1.|Statherian|Orosirian|In the Utnalanama Range. Maximum mineralisation age Marrakesh prospect of c. 1788 Ma based on a protolith age of 1788 +/- 6 Ma. for the host Erontonga Metamorphics (zircon 207Pb/206Pb age; Kositcin et al 2015). Maximum mineralisation age Utnalanama prospect of 1810 Ma based on a protolith age of 1810+/- 4 Ma for the host Erontonga Metamorphics (zircon 207Pb/206Pb age; Hussey et al 2006).|protolith ages: 1810 Ma, 1788 Ma.||||Includes metamorphics.|
6282|Esperanza Formation|22438|4|Described|p539, Fig.3 p537|||See also Fig.10a p546.||||||18-SEP-06
6282|Esperanza Formation|22453|5|Briefly described|p 11  Fig 10|||||||||
6282|Esperanza Formation|22585|6|Mentioned|P739, Fig1, Fig2|||||||||
6282|Esperanza Formation|22665|6|Mentioned|P221, Table1|||||||||
6282|Esperanza Formation|22680|6|Mentioned|84 fig 2,85|||Geol province Mount Isa Basin. Parent McNamara Group. Formation as 'Fm' in text||||||
6282|Esperanza Formation|22681|6|Mentioned|91|||Overlying unit Lady Loretta Formation||||||
6282|Esperanza Formation|23031|5|Briefly described|26|||Geol. province: Lawn Hill Subprovince. Of the McNamara Group. Overlain by Lady Lorretta Formation; underlain by Paradise Creek Formation||||||18-SEP-06
6282|Esperanza Formation|23072|5|Briefly described|p754|||||||||
6282|Esperanza Formation|23073|5|Briefly described|p744 (fig 2), p745|||||||||
6282|Esperanza Formation|23362|5|Briefly described|339|||||||||
6282|Esperanza Formation|23387|6|Mentioned|p18 fig.19|||Of McNamara Group.||||||
6282|Esperanza Formation|23393|4|Described|p19, p20|Paleoproterozoic|Paleoproterozoic|Of McNamara Group. Overlain by Lady Loretta Formation.||||||07-NOV-08
6282|Esperanza Formation|23396|4|Described|p421, 407|Statherian|Statherian|Of McNamara Group. Age: 1657+/-3Ma U/Pb zircon analyses, [presumably detrital zircon, on SHRIMP].||||||16-MAR-18
6282|Esperanza Formation|23397|5|Briefly described|p469|||||||||
6282|Esperanza Formation|23398|4|Described|p447|Statherian|Statherian|Of McNamara Group.||||||
6282|Esperanza Formation|23399|5|Briefly described|p493 Fig.3|||Of McNamara Group.||||||18-SEP-06
6282|Esperanza Formation|23408|4|Described|p512, p513 Fig. 2, p521|||Of McNamara Group. Upper section includes accretions of deeper water 'organ pipe' digitate stromatolite bioherms and biostromes.||||||15-JUN-09
6282|Esperanza Formation|23409|5|Briefly described|p535 Fig.2|||Of McNamara Group||||||18-SEP-06
6282|Esperanza Formation|23466|5|Briefly described|p269|||||||||
6282|Esperanza Formation|23767|5|Briefly described|p1956 Fig. 2|||Geological Province: Western Fold Belt. See also p1957 Fig.3||||||
6282|Esperanza Formation|23958|5|Briefly described|p1134 Fig.2|Mesoproterozoic|Paleoproterozoic|Of McNamara Group.||||||07-NOV-08
6282|Esperanza Formation|23964|5|Briefly described|p1265|Proterozoic|Proterozoic|Of McNamara Group.  Geological Province: Mount Isa Inlier.  Maximum thickness: 250m.||||||21-NOV-16
6282|Esperanza Formation|23965|5|Briefly described|p1297|Mesoproterozoic|Paleoproterozoic|Of McNamara Group. Geological Province: Mount Isa Inlier.||||||07-NOV-08
6282|Esperanza Formation|23986|5|Briefly described|p65|||Of McNamara Group.||||||
6282|Esperanza Formation|24033|6|Mentioned|p25, p26 Fig. 10|||||||||
6282|Esperanza Formation|24308|5|Briefly described|p995 Fig. 8|||||||||
6282|Esperanza Formation|24432|4|Described|p562 Fig.2|Statherian|Statherian|Of McNamara Group. Overlies Paradise Creek Formation. Age: c.1657 Ma. Carbonate. Geological Province: Lawn Hill Platform.||||||
6282|Esperanza Formation|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
6282|Esperanza Formation|36937|6|Mentioned|p229|||||||||
6282|Esperanza Formation|37459|1|Redefined|p429|Mesoproterozoic|Mesoproterozoic|Age is more specifically Carpentarian.||||||18-SEP-06
6282|Esperanza Formation|37568|6|Mentioned|p84|||||||||
6282|Esperanza Formation|38237|4|Described|p129|||||||||
6282|Esperanza Formation|38291|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
6282|Esperanza Formation|38348|4|Described|p11|||||||||
6282|Esperanza Formation|38584|6|Mentioned|p22|||||||||
6282|Esperanza Formation|39445|5|Briefly described|Table 2|||||||||
6282|Esperanza Formation|39497|6|Mentioned|Fig.4|||||||||
6282|Esperanza Formation|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the McNamara Group. Stromatolitic chert and dolomite, siliceous and dolomitic siltstone.||||||15-JUN-06
6282|Esperanza Formation|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
6282|Esperanza Formation|39925|6|Mentioned|Fig.9|||||||||
6282|Esperanza Formation|39944|6|Mentioned|Fig.1|||||||||
6282|Esperanza Formation|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
6282|Esperanza Formation|40221|3|Fully described|p17|||||||||
6282|Esperanza Formation|40394|6|Mentioned|p286|||||||||
6282|Esperanza Formation|41298|6|Mentioned|Map legend|Carpentarian||||||||
6282|Esperanza Formation|43235|5|Briefly described|p9,Fig.10.|||Of McNamara Group.||||||27-MAY-08
6282|Esperanza Formation|45166|5|Briefly described|p30|||||||||
6282|Esperanza Formation|47083|3|Fully described|p16-17||Proterozoic|Previously part of Paradise Crk Fm by Carter and others (1961). Of McNamara Gp. Overlain by Lady Loretta Fm; underlain by Paradise Crk Fm. Max. thickness: 350 m.||||||18-SEP-06
6282|Esperanza Formation|50550|5|Briefly described|p1139 Fig.2||Statherian|Age: >1647 Ma, <1657 Ma. Conformably overlies Paradise Creek Formation. Conformably overlain by Lady Loretta Formation. Geological Province: Western Fold Belt.||||||17-DEC-07
6282|Esperanza Formation|50600|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the McNamara Group.  Stromatolitic chert, dolomitic sandstone, siltstone, oolitic dolomite. Overlies Paradise Creek Formation; overlain by Lady Loretta Formation.||||||21-NOV-16
6282|Esperanza Formation|60558|5|Briefly described|p5 Fig. 4|||Of McNamara Group. Overlain by Lady Loretta Formation, underlain by Paradise Creek Formation.||||||
6282|Esperanza Formation|61732|5|Briefly described|p25|||Superseded Paradise Creek Formation. Well preserved microfossils in stromatolites. In the Mount Isa region.||||||07-FEB-11
6282|Esperanza Formation|61936|5|Briefly described|p194 Fig. 6|||Geological Province: Lawn Hill Platform, Western Fold Belt, Mount Isa Inlier. ||||||
6282|Esperanza Formation|62084|5|Briefly described|p936 Fig.5|||Isa Superbasin. Lawn Hill. Shown as Esperanza Fm.||McNamara Group|||Platform carbonates.|
6282|Esperanza Formation|62535|5|Briefly described|p672|Statherian|Statherian|Lawn Hill Platform.|1657 +/- 3 Ma.|McNamara Group.||||
6282|Esperanza Formation|63023|6|Mentioned|p1037|Paleoproterozoic|Paleoproterozoic|Age: ca 1660-1655Ma. Of the Gun Supersequence.||||||07-NOV-08
6282|Esperanza Formation|63109|6|Mentioned|p1108 Fig. 3|||Geological Province: Isa Superbasin.||||||30-SEP-08
6282|Esperanza Formation|63111|5|Briefly described|p1164 Tb. 1|Statherian|Statherian|Of Gun Supersequence. Ages: 1668 - 1653Ma. Geological Province: Isa Superbasin. Laminated fine-grained sandstone and siltstones, dolomudstones, laminated carbonates.||||||07-FEB-11
6282|Esperanza Formation|63113|6|Mentioned|p1214 Fig.2, p1225 Fig.13. |||Part of Gun supersequence. Appears in Fig.2 only as Esp.|c.1657 Ma.|Of the McNamara Group||||
6282|Esperanza Formation|63114|5|Briefly described|p1253 Fig.2. |||Isa Superbasin.||Of the Gun supersequence||||05-APR-17
6282|Esperanza Formation|63115|6|Mentioned|p1279 Fig.4.|||Isa superbasin.||||||
6282|Esperanza Formation|63116|6|Mentioned|p1297 Fig.2, p1299 Tb.1, p1300 |||Isa superbasin. Material properties detailed.||||||
6282|Esperanza Formation|63866|5|Briefly described|p58|||Isa Superbasin.||Gun Supersequence||||
6282|Esperanza Formation|63884|5|Briefly described|p14|||Dolomitic.||||||
6282|Esperanza Formation|64250|6|Mentioned|p11 fig 3|||||Unit in McNamara Group.||||
6282|Esperanza Formation|65228|6|Mentioned|p24, Fig.04.|||Southern Lawn Hill Platform. Part of Gun Supersequence.||Unit in McNamara Group.||||
6282|Esperanza Formation|65337|5|Briefly described|p30.|||Equivalent to lower Brumby Formation.||||Overlies Paradise Creek Formation. Is overlain by Lady Loretta Formation.|Includes carbonate-chert-conglomerate facies.|
6282|Esperanza Formation|65396|5|Briefly described|p82, p175, p241|Statherian|Statherian|Isa Superbasin. Cover Sequence 3. Lawn Hill Platform.|1657 +/- 3 Ma|McNamara Group||Overlies Paradise Creek Formation; overlain by Lady Loretta Formation.||03-APR-17
6282|Esperanza Formation|66844|4|Described|p243-244,251,253, 254,270-273|Statherian|Statherian|Lawn Hill Platform. Age from SHRIMP dating. Comprises Gun 2.1 to 2.5 sequences. Shale-dominated MFS in lower part associated with Gun 2.2. Stromatolites are dominantly digitate columnar, indicative of silicification by late-stage diagenetic processes. Upper part received locally sourced, nearshore siliciclastic accummulations in the Kamarga Dome and Gregory River regions associated with basinward shift in facies.|1657+\-3 Ma SHRIMP|Of lower McNamara Group; Gun Supersequence (2.1-2.5).|Informally subdivided into upper and lower parts p267, 268.|Overlain unconformably by Lady Loretta Formation.|Includes ooid grainstones; digitage stromatolite and dolomudstone.|
6282|Esperanza Formation|67323|5|Briefly described|GIS attrib tbl, p26, p34|Paleoproterozoic|Paleoproterozoic|See also Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Mount Isa Inlier, Isa Superbasin.|~1660-1650 Ma.|McNamara Group.|||Stromatolitic chert and dolomite, siliceous and dolomitic sandstone.|
6282|Esperanza Formation|68542|5|Briefly described|p6|||||Lower McNamara Group||Overlain by Lady Loretta Formation, overlies Paradise Creek Formation|Stromatolitic chert and dolomitic siltstone.|
6282|Esperanza Formation|68576|5|Briefly described|Q_2: p6-7|||Lawn Hill Platform, Mount Isa Inlier.||Lower McNamara Group.||Overlies Paradise Creek Formation. Is overlain by Lady Loretta Formation.|Stromatolitic chert and dolomitic siltstone.|
6282|Esperanza Formation|68732|5|Briefly described|p162, p163, p168 Fig.5, p169|Statherian|Statherian|Geochronology based on a "pinkite": tuffaceous rock or peperite in the lower part of this formation.|1657 +/- 3 Ma|Of the McNamara Group.|||Includes stromatolitic bioherms and biostromes.|30-NOV-17
6282|Esperanza Formation|69591|5|Briefly described|p42-43, p44 Fig.2.36, p54|||Isa Superbasin. Deposition on a carbonate platform: tempestites/peritidal deposits. Part of Gun Supersequence.||McNamara Group.||Overlies Paradise Creek Formation. Is overlain by Lady Loretta Formation. Equated with the Urquhart Shale.|Stromatolitic dolomite and chert, siliceous and dolomitic sandstone.|
6282|Esperanza Formation|70864|5|Briefly described|p75, 74 Fig 2, p78, p80, 81, 84, p100|Mesoproterozoic||Host to sulphide mineralization in siliceous and calcareous rocks.||McNamara Group|||Stromatolitic chert, dolomitic siltstone, calcareous and siliceous siltstone, carbonaceous black shale, dolostones and sandstones.|21-NOV-16
6282|Esperanza Formation|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Lawn Hill Platform of the Mount Isa Province and the east part of the South Nicholson Basin. Age given as U-Pb zircon sedimentary depositional age.|1657 +/-3 Ma|McNamara Group||Overlies Paradise Creek Formation and underlies Lady Loretta Formation.||
6282|Esperanza Formation|72912|5|Briefly described|p5 Fig.3, p33 Fig.12.|Statherian|Statherian|Shown as being located in the Queensland part of the McNamara Group. Located in the The Lawn Hill Platform of the Mount Isa Province, and the East part of the South Nicholson Basin. Four U-Pb zircon sedimentary depositional ages [?] given for this unit on p33 are shown for the underlying Paradise Creek Formation on p5. The date listed is common to both figures.|1657 +/- 3 Ma|McNamara Group||Overlies Paradise Creek Formation and underlies Lady Loretta Formation.|Includes dolostone.|
6282|Esperanza Formation|72913|5|Briefly described|p7 Fig.2.|Paleoproterozoic|Paleoproterozoic|Shown as being in the eastern and Lawn Hill Platform part of the Isa Superbasin.|1653 +/- 7 Ma to 1658 +/- 3 Ma|McNamara Group||Overlies Paradise Creek Formation and underlies Lady Loretta Formation.|Includes dolostone.|
6282|Esperanza Formation|73042|6|Mentioned|p4|Statherian|Statherian|South Nicholson Basin region and Mount Isa Province, Isa Superbasin. Geochronology is a U-Pb zircon sedimentary depositional age (?maximum depositional age).|1657 +/- 3 Ma (see Fig.1.2)|McNamara Group||Underlain by Paradise Creek Formation. Overlain by Lady Loretta Formation.||
6282|Esperanza Formation|73144|6|Mentioned|p8-9|Statherian|Statherian|Isa Superbasin. Part of the Gun Supersequence. Partial aquifer.||McNamara Group||Underlain by Paradise Creek Formation. Overlain by Lady Loretta Formation.||
6282|Esperanza Formation|73525|6|Mentioned|p4-5 Fig.2|||Mount Oxide-(Ardmore-May Downs) Domain.|||||Carbonates.|
6287|Etadunna Formation|9862|5|Briefly described|Map Legend|Tertiary|Tertiary|Flaggy dolomite, green clay, sandstone and siltstone.||||||
6287|Etadunna Formation|22587|6|Mentioned|p78|Early Miocene|Early Miocene|||||||
6287|Etadunna Formation|22912|4|Described|32|||||||||
6287|Etadunna Formation|23394|5|Briefly described|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
6287|Etadunna Formation|23818|5|Briefly described|p174 Fig.84|Early Miocene|Early Miocene|Geological Province: Great Artesian Basin.||||||
6287|Etadunna Formation|24175|3|Fully described|p38, p32 Fig. 6|Pliocene|Late Oligocene|Age range given as above but "most probably largely Early Miocene".  Type section in Lake Eyre Bore 4.  Max. thickness: 44.5m.  Geological Province: Lake Eyre Basin.||||||
6287|Etadunna Formation|24176|6|Mentioned|p22 Tb. 1|Cenozoic|Cenozoic|Geological Province: Mount Painter Province.||||||19-NOV-08
6287|Etadunna Formation|24321|5|Briefly described|Map legend|Miocene|Miocene|Equivalent to Millers Creek Dolomite Member (of Mirkata Formation).  Includes the Moolarina Member.||||||
6287|Etadunna Formation|29427|6|Mentioned|p53|||||||||
6287|Etadunna Formation|29431|6|Mentioned|p23|||||||||
6287|Etadunna Formation|29659|6|Mentioned|p8|||||||||
6287|Etadunna Formation|29660|6|Mentioned|p5|||||||||
6287|Etadunna Formation|29897|6|Mentioned|p282|||||||||
6287|Etadunna Formation|30054|6|Mentioned|p803|||||||||
6287|Etadunna Formation|30055|6|Mentioned|p153|||||||||
6287|Etadunna Formation|30056|6|Mentioned|p135|||||||||
6287|Etadunna Formation|30061|6|Mentioned|p6|||?Late Olegocene.||||||
6287|Etadunna Formation|30163|6|Mentioned|p658|||||||||
6287|Etadunna Formation|30177|4|Described|p106|||Tertiary age.||||||
6287|Etadunna Formation|30514|6|Mentioned|p102|||||||||
6287|Etadunna Formation|30518|6|Mentioned|p88|||Tertiary age||||||
6287|Etadunna Formation|30540|6|Mentioned|Fig.6|||||||||
6287|Etadunna Formation|30804|5|Briefly described|p13|||See also Table 1||||||
6287|Etadunna Formation|30807|6|Mentioned|p101|||Suggested map symbol||||||
6287|Etadunna Formation|30918|6|Mentioned|p82|||||||||
6287|Etadunna Formation|30919|6|Mentioned|Map legend|Miocene|Miocene|||||||
6287|Etadunna Formation|30920|6|Mentioned|Map legend|Miocene|Miocene|Equivalent of Namba Formation||||||
6287|Etadunna Formation|31532|4|Described|Table 1|||||||||
6287|Etadunna Formation|31699|4|Described|p132|||Mid Tertiary||||||
6287|Etadunna Formation|31968|6|Mentioned|p8|||Refers Stirton et al. (1961)||||||
6287|Etadunna Formation|32121|6|Mentioned|p422|||||||||
6287|Etadunna Formation|32275|6|Mentioned|p9|||||||||
6287|Etadunna Formation|32418|6|Mentioned|p2|||||||||
6287|Etadunna Formation|32652|6|Mentioned|p279|||||||||
6287|Etadunna Formation|33569|6|Mentioned|p63|||||||||
6287|Etadunna Formation|33819|6|Mentioned|p3|||||||||
6287|Etadunna Formation|33820|6|Mentioned|Map legend|Miocene|Miocene|||||||
6287|Etadunna Formation|33822|6|Mentioned|Map legend|Miocene|Miocene|||||||
6287|Etadunna Formation|33823|6|Mentioned|Map legend|Miocene|Miocene|||||||
6287|Etadunna Formation|33824|6|Mentioned|p13|||Table 1 & 2||||||
6287|Etadunna Formation|33827|6|Mentioned|p14|||See also Table 1||||||
6287|Etadunna Formation|33828|6|Mentioned|p4|||See also Table 1||||||
6287|Etadunna Formation|33937|5|Briefly described|p1|||||||||
6287|Etadunna Formation|33938|6|Mentioned|p20|||||||||
6287|Etadunna Formation|34180|6|Mentioned|Fig.108|||?Oligocene.||||||
6287|Etadunna Formation|34308|6|Mentioned|p200|||Correlation chart. Batesfordian - Balcombian||||||
6287|Etadunna Formation|34615|6|Mentioned|p10|||||||||
6287|Etadunna Formation|34754|6|Mentioned|p32|||||||||
6287|Etadunna Formation|34996|6|Mentioned|p145|||||||||
6287|Etadunna Formation|35003|6|Mentioned|p122|||Analysis||||||
6287|Etadunna Formation|35080|6|Mentioned|p12|||||||||
6287|Etadunna Formation|35187|6|Mentioned|Table1|||||||||
6287|Etadunna Formation|35772|6|Mentioned|p9|||||||||
6287|Etadunna Formation|35857|6|Mentioned|p197|||||||||
6287|Etadunna Formation|36213|6|Mentioned|p83|||||||||
6287|Etadunna Formation|36966|6|Mentioned|p81|||||||||
6287|Etadunna Formation|37062|6|Mentioned|p199|||||||||
6287|Etadunna Formation|37678|6|Mentioned|p237|||||||||
6287|Etadunna Formation|37754|6|Mentioned|p101|||||||||
6287|Etadunna Formation|38068|6|Mentioned|Fig.7|||||||||
6287|Etadunna Formation|38371|6|Mentioned|p666|||||||||
6287|Etadunna Formation|38605|6|Mentioned|p30|||||||||
6287|Etadunna Formation|38982|5|Briefly described|p64|||||||||
6287|Etadunna Formation|39085|6|Mentioned|p13|||||||||
6287|Etadunna Formation|39322|6|Mentioned|Fig.2|||||||||
6287|Etadunna Formation|39352|6|Mentioned|Map legend|early Pleistocene|middle Miocene|Middle Miocene to Early Pleistocene||||||
6287|Etadunna Formation|39521|6|Mentioned|p119|||||||||
6287|Etadunna Formation|40150|6|Mentioned|Fig.1|||||||||
6287|Etadunna Formation|40754|6|Mentioned|p10|||||||||
6287|Etadunna Formation|40755|5|Briefly described|App.3.1|||||||||
6287|Etadunna Formation|40756|5|Briefly described|p1|||||||||
6287|Etadunna Formation|40757|3|Fully described|p78|||||||||
6287|Etadunna Formation|40758|6|Mentioned|p87|||||||||
6287|Etadunna Formation|40910|6|Mentioned|p19|||||||||
6287|Etadunna Formation|40926|6|Mentioned|p28|||||||||
6287|Etadunna Formation|41098|6|Mentioned|p178|||||||||
6287|Etadunna Formation|41165|5|Briefly described|p365|||||||||
6287|Etadunna Formation|41537|6|Mentioned|p348|||||||||
6287|Etadunna Formation|41600|6|Mentioned|p827|||||||||
6287|Etadunna Formation|42340|6|Mentioned|p25|Miocene|Oligocene|||||||
6287|Etadunna Formation|42375|4|Described|p25-29|||Lake Eyre Basin Defined Stirton 1961.||||||
6287|Etadunna Formation|42390|5|Briefly described|Fig.2 P335|||||||||
6287|Etadunna Formation|42469|5|Briefly described|p39|||||||||
6287|Etadunna Formation|42477|5|Briefly described|p184, 192, 196|||||||||
6287|Etadunna Formation|42508|5|Briefly described|p74|||||||||
6287|Etadunna Formation|42592|5|Briefly described|Fig.4 P270|||Type locality indicated p272.||||||18-SEP-06
6287|Etadunna Formation|42746|5|Briefly described|p17|||Lake Eyre Basin. See also Fig.2 p4.||||||18-SEP-06
6287|Etadunna Formation|42784|6|Mentioned|p485|||||||||
6287|Etadunna Formation|42813|6|Mentioned|p24|||||||||
6287|Etadunna Formation|43035|6|Mentioned|p27|||||||||
6287|Etadunna Formation|43041|5|Briefly described|Fig.1,p590|||||||||
6287|Etadunna Formation|43048|5|Briefly described|p22|||||||||
6287|Etadunna Formation|43053|5|Briefly described|Map Legend|Pliocene|Miocene|Lacustrine dolomite, clay, sand and silt. Geological Province: Lake Eyre Basin.||||||25-MAY-05
6287|Etadunna Formation|43071|5|Briefly described|p17|||||||||
6287|Etadunna Formation|43094|5|Briefly described|p38|||||||||
6287|Etadunna Formation|43258|5|Briefly described|Map Legend|Pliocene|Miocene|||||||
6287|Etadunna Formation|43298|6|Mentioned|Map Legend|Pliocene|Miocene|||||||
6287|Etadunna Formation|43681|6|Mentioned|p297||Miocene|||||||
6287|Etadunna Formation|44133|4|Described|p193, 187, 190 Fig. 10.30|Late Miocene|Late Oligocene|Correlates with the Neuroodla Formation. Geoloigcal Province: Lake Eyre Basin. Overlies Eyre Formation. Includes: Mampuwordu Sand, Muloorina Member. Thickness: 80m. ||||||
6287|Etadunna Formation|44221|14|Not recorded|p.93||Miocene|Miocene?||||||
6287|Etadunna Formation|44223|14|Not recorded|p.151,158||Oligocene|Fig.2.||||||
6287|Etadunna Formation|44224|14|Not recorded|p.1,5,27|Early Miocene|Late Oligocene|late Oligocene or early Miocene (H/54-5).||||||
6287|Etadunna Formation|44225|14|Not recorded|p.45|||(H/54-5).||||||
6287|Etadunna Formation|44238|14|Not recorded|p.225,227,228|Early Miocene|Late Oligocene|Fig.3. U.Olig.- L.Miocene.||||||
6287|Etadunna Formation|44829|6|Mentioned|p40|||On SA card.||||||
6287|Etadunna Formation|44934|6|Mentioned|Map Legend|Miocene|Eocene|||||||
6287|Etadunna Formation|45128|6|Mentioned|p53|||||||||
6287|Etadunna Formation|45145|6|Mentioned|p37|||See also Table 7.||||||
6287|Etadunna Formation|45155|6|Mentioned|p46|||||||||
6287|Etadunna Formation|46802|6|Mentioned|Table 1|||||||||
6287|Etadunna Formation|46833|6|Mentioned|p56|||||||||
6287|Etadunna Formation|60703|5|Briefly described|p704 Fig. 2, p725 Fig.18|Late Oligocene|Late Oligocene|Contains abundant gastrapod fossils. Overlain by the Wipajiri Formation. Age: 25.7-24.2 Ma. Geological Province: Lake Eyre Basin (Tirari Sub-basin).||||||12-APR-05
6287|Etadunna Formation|60785|5|Briefly described|p197.|||A correlate of the Namba Formation.|24 - 28 Ma (Woodburne et al. 1993).|||Correlate of the Namba Formation.||
6287|Etadunna Formation|60953|5|Briefly described|Map Legend|Pliocene|Miocene|Geological Province: Lake Eyre Basin.||||||
6287|Etadunna Formation|61108|5|Briefly described|map legend|Pliocene|Miocene|Lacustrine dolomite, clay, sand and silt. Geological Province: Lake Eyre Basin.||||||
6287|Etadunna Formation|61119|5|Briefly described|p124, p129, pp132-135, pp143-4, p146||Cenozoic|Older than Wipajiri Formation [underlies]. Freshwater lake deposits. Detailed descriptions of Lungfish fossil assemblages included.||||||28-MAR-12
6287|Etadunna Formation|61155|5|Briefly described|p4, p17|Middle Miocene|Early Miocene|Age: 21-12.5Ma. Thickness: 50m. Geological Province: Lake Eyre Basin.||||||03-MAR-10
6287|Etadunna Formation|61517|5|Briefly described|p312|Miocene|Miocene|Dolomitic limestone.||||||
6287|Etadunna Formation|64197|6|Mentioned|p627, p630 Fig.6|Middle Miocene|Middle Miocene|Unconformably overlies the Eyre Formation.||||||
6287|Etadunna Formation|65194|5|Briefly described|p49, p171|Miocene|Oligocene|Lake Eyre Basin. Dolomitic lacustrine deposits - these sediments form sheet or blanket cover sequences and palaeovalley infill.||||||
6287|Etadunna Formation|65684|6|Mentioned|p807|Late Oligocene|Late Oligocene|Age confirmed as Oligocene by magnetostratigraphy (Woobdurne et al, 1994).||||||
6287|Etadunna Formation|65925|5|Briefly described|p17, Appendix 2.|||Tirari Sub-basin. Equivalent to Namba Formation.|||||White dolomite and limestone with green and grey Mg rich claystone and fine-grained sand.|
6287|Etadunna Formation|66131|4|Described|p240, p242-245, p249, p255, p259|Miocene|Oligocene|Tirari Sub-basin. Between 25-80 m thick. Contains abundant fossils. Type section at Lake Palankarina.|||Includes Mampuwordu Sand, Muloorina Member.|Overlies Eyre Formation. Disconformably overlain by the Katipiri Formation. Correlative of the Caldelga Limestone and Alberga Limestone Member. ?Overlain by the Waite Formation.|Comprises white dolomite and limestone overlain by Mg-rich green and grey claystone and fine sand. Intraformational conglomerate and bioturbation are widespread. Silcrete capping.|
6287|Etadunna Formation|66573|5|Briefly described|Throughout the article.|Miocene|Oligocene|Disconformably overlies the Eyre Formation; is overlain unconformably by Tirari Formation. Grey dolomitic marls and shales. 26.1 - 23.6 Ma.||||||
6287|Etadunna Formation|66623|6|Mentioned|p282.|||Wopfner (1974) tentatively correlated at least the base of this unit with the Doonbara Formation in NSW.||||||21-MAY-13
6287|Etadunna Formation|67462|5|Briefly described|Map legend.|Miocene|Miocene|Tirari Sub-basin, Lake Eyre Basin.|||Includes Muloorina Member and Mampuwordu Sand.|||
6287|Etadunna Formation|67578|5|Briefly described|p333, p335-339, p342-344.|Miocene|Oligocene|Lake Eyre Basin. Originally defined by Stirton et al. (1961). Lacustrine facies. Age range determined from a single Rb/Sr isotope analysis, as well as foraminiferal assemblages (latest Oligocene to Middle Miocene). Thickness exceeds 20m in drill core. Affected by widespread post-depositional silicification.||||Unconformably overlain by the Eyre Formation.|Consists of white-grey, fine-grained chemical and clastic sediments. Channel sands occur in the upper part of the Formation at several locations.|
6287|Etadunna Formation|68068|5|Briefly described|Map legend|||Callabonna Sub-basin, Lake Eyre Basin. Occurs W & NW of Callabonna sheet.Equivalent to the Namba Formation to the east and southeast.||||||25-NOV-14
6287|Etadunna Formation|68715|6|Mentioned|p30 Fig.5|Langhian|Burdigalian|Tirai and northern Callabonna sub basins, Lake Eyre Basin.|||Muloorina Member.|||07-APR-17
6287|Etadunna Formation|68821|4|Described|p296|Serravallian|Chattian|Consists largely of immature fluvio-lacustrine sand, silt, and clay deposited in an alkaline and anoxic environment. Includes levels of pyritic laminated carbonaceous mud and fossils - gastropods, ostracods, algae, fish, reptiles, birds and mammals.|26 - 12 Ma|||Locally underlain by the Eyre Formation.|Consists of quartz (< 50%), kaolinte (< 40%), feldspar (< 15%), mica (< 15%), smectite(< 5%), illite (a few %), palygorskite and dolomite, gypsum and alunite.|
6287|Etadunna Formation|69019|3|Fully described|p83 Fig.20, p105 Fig.25, p110-113.|Miocene|Oligocene|Tirari Sub-basin, Lake Eyre Basin. Of Stirton et al. (1961). Type section is on western shores of Lake Palankarinna. Thickness to 44 m. Age is from a specimen of palygorskite clay. Has developed a porcellanite horizon.|c.25 Ma (Rb-Sr, Norrish and Pickering 1983)||Includes Muloorina Member.|Overlies Mirackina Conglomerate; unconformably overlies Eyre Formation. Is overlain by Yardinna Claystone, Alberga Limestone and Wipajiri Formation. Contemporaneous with Namba Formation.|Sandy claystone and sand with silty and gypseous clay and flaggy dolomite below bedded sandstone; overlain by  sand, silt and clay, cross-bedding throughout, and local intercalated dolomite nodules and beds.|
6287|Etadunna Formation|69023|5|Briefly described|p87, p108, p117-118, p120, p125, p193|||Stratigraphic wells intersection data.|||Includes Muloorina Member.|Time-equivalent of Namba Formation.||
6287|Etadunna Formation|69458|5|Briefly described|p42:16, 19, 22|Miocene|Oligocene|Lake Eyre Basin. Extensive shallow, alkaline lacustrine to fluvial deposits. Lower parts contain a vertebrate assemblage with affinities with the Pwerte Marnte Marnte fauna.||||Correlated with Ulta Limestone.|Interbedded sandstone, siltstone, shale and locally developed dolostone.|12-JUL-16
6287|Etadunna Formation|69572|6|Mentioned|p1188, 1190|Miocene|Oligocene|Contains fossils of the oldest (24 m.y.) phascolarctid koalas. Other species and locations tabulated.||||||
6287|Etadunna Formation|69946|5|Briefly described|p29, p129|Miocene|Oligocene|Tirari Sub-basin, Lake Eyre Basin. Callen et al. (1995). On p129, shown in two parts: Etadunna Formation (Lower) and Etadunna Formation (Upper).|||||Carbonate and clastics from evaporation of magnesian lakes.|
6287|Etadunna Formation|70321|6|Mentioned|p153-154|Oligocene|Oligocene|Contains the only late Oligocene terrestrial-mammal fossil assemblage radiometrically dated.||||||
6287|Etadunna Formation|71317|5|Briefly described|p144|||||||Equivalent to the Garford Formation.||
6287|Etadunna Formation|71342|5|Briefly described|Ch5 p29, Ch5 p130|Miocene|Oligocene|Lake Eyre Basin. |||||Carbonates and clastic rocks.|
6287|Etadunna Formation|72456|5|Briefly described|Map Legend|Pliocene|Oligocene|Marree 1:250k map sheet.|||||White dolomite and limestone with green and grey Mg rich claystone and fine-grained sand.|
6287|Etadunna Formation|73234|6|Mentioned|p23|||Lake Eyre Basin.||||Equivalent to Neuroodla Formation.||
6287|Etadunna Formation|73479|6|Mentioned|p156 Fig.2|Neogene|Neogene|Lake Eyre Basin.||||Overlies Eyre Formation||
6312|Etingambra Formation|32275|6|Mentioned|p9|||||||||
6312|Etingambra Formation|34488|6|Mentioned|p11|||||||||
6312|Etingambra Formation|44335|4|Described|p.13||Tertiary|Table 3. p.14.||||||
6312|Etingambra Formation|44336|14|Not recorded|map legend||Tertiary|SG/53-3.||||||
6312|Etingambra Formation|44393|4|Described|p.7,8,Tb.1||Tertiary|||||||
6312|Etingambra Formation|44394|14|Not recorded|map legend||Tertiary|||||||
6312|Etingambra Formation|45041|5|Briefly described|p115|||||||||
6312|Etingambra Formation|48890|2|Defined|p.56,57,58||Tertiary|Tb.1, Fig.4. Defn. on Tech.File F/53-15.||||||
6312|Etingambra Formation|61155|5|Briefly described|p16|Middle Eocene|Middle Eocene|Age: 51-45Ma. Thickness: 12m. Location:overlying East Amadeus Basin.||||||06-SEP-10
6312|Etingambra Formation|62609|5|Briefly described|Map Legend|Tertiary|Tertiary|Sandstone, conglomeratic sandstone, conglomerate, some siltstone.||||||
6312|Etingambra Formation|62620|5|Briefly described|Map Legend|Tertiary|Tertiary|Sandstone, conglomeratic sandstone, conglomerate, some siltstone.||||||
6312|Etingambra Formation|69458|5|Briefly described|p42:16-17|||Wells et al. (1967). Lake Eyre Basin. Generally exposed as caps on small mesas. 5-12 m thick.||||Unconformably overlies Wilgunya Subgroup. Equivalent to the Eyre Formation.|Medium- to coarse-grained, poorly bedded, often friable sandstone, with subordinate siltstone and irregular beds and lenses of fine conglomerate containing poorly to moderately rounded clasts.|12-JUL-16
6356|Eulo Queen Group|9541|5|Briefly described|Map legend|Late Jurassic|Middle Jurassic|Includes Loth Formation and Hampstead Sandstone.||||||
6356|Eulo Queen Group|22744|5|Briefly described|P12, Table3 P10||Jurassic|||||||
6356|Eulo Queen Group|22747|5|Briefly described|p9||Mesozoic|Eromanga Basin||||||
6356|Eulo Queen Group|23032|5|Briefly described|p47|Late Jurassic|Middle Jurassic|||||||
6356|Eulo Queen Group|23291|4|Described|p81 Tb 3.6|Late Jurassic|Middle Jurassic|Geological Province: Georgetown Region.||||||08-JUL-15
6356|Eulo Queen Group|23425|4|Described|Plate 9.3 p379.|||Comprises the Hampstead Sandstone and Loth Formation. Also see Table 9.7 p395. Overlain by Gilbert River Formation. Carpentaria Basin Province.||||||08-DEC-08
6356|Eulo Queen Group|23426|5|Briefly described|p403|||Carpentaria Basin Province.||||||
6356|Eulo Queen Group|23430|5|Briefly described|p455.|||Eromanga Basin Province||||||
6356|Eulo Queen Group|23453|5|Briefly described|p20|Cretaceous|Cretaceous|||||||
6356|Eulo Queen Group|23846|5|Briefly described|p5|Jurassic|Jurassic|Includes Hampstead Sandstone and Loth Formation. Quartzose sandstone, conglomerate, silstone, and shale. Underlies Gilbert River Formation. Geological province: Eronmanga Basin.||||||18-SEP-06
6356|Eulo Queen Group|23982|5|Briefly described|p58 Fig.18|||Geological Province: Carpentaria Basin.||||||
6356|Eulo Queen Group|24073|5|Briefly described|p378 Table 2|||Geological Province: Carpentaria Basin.||||||
6356|Eulo Queen Group|24092|5|Briefly described|p8 Fig.3|||Geological Province: Carpentaria Basin.||||||
6356|Eulo Queen Group|30020|6|Mentioned|p29|||||||||
6356|Eulo Queen Group|30587|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
6356|Eulo Queen Group|30914|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
6356|Eulo Queen Group|31164|5|Briefly described|p9|||Water supplies||||||
6356|Eulo Queen Group|31422|5|Briefly described|Map legend|Jurassic|Jurassic|Quartzose sandstone and siltstone, shale, conglomerate.||||||02-DEC-04
6356|Eulo Queen Group|31433|5|Briefly described|p8|||Correlation. Jurassic||||||
6356|Eulo Queen Group|31434|6|Mentioned|p8|||Refer Smart et al.(1971)||||||
6356|Eulo Queen Group|32531|6|Mentioned|Fig.2|||On p474.||||||18-SEP-06
6356|Eulo Queen Group|32705|6|Mentioned|p179|||See also p183.||||||18-SEP-06
6356|Eulo Queen Group|32706|6|Mentioned|p10|||||||||
6356|Eulo Queen Group|33086|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
6356|Eulo Queen Group|33176|4|Described|p171|||||||||
6356|Eulo Queen Group|33177|6|Mentioned|p10|||||||||
6356|Eulo Queen Group|33178|6|Mentioned|p11|||||||||
6356|Eulo Queen Group|33182|6|Mentioned|p190|||||||||
6356|Eulo Queen Group|33183|2|Defined|p230|Jurassic|Jurassic|||||||
6356|Eulo Queen Group|33644|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
6356|Eulo Queen Group|33648|4|Described|p19|||||||||
6356|Eulo Queen Group|33882|6|Mentioned|p19|||||||||
6356|Eulo Queen Group|33907|6|Mentioned|p5|||||||||
6356|Eulo Queen Group|35220|6|Mentioned|p16|||||||||
6356|Eulo Queen Group|35811|5|Briefly described|Table 3|||||||||
6356|Eulo Queen Group|35814|6|Mentioned|p582|||||||||
6356|Eulo Queen Group|35920|6|Mentioned|p26|||||||||
6356|Eulo Queen Group|35921|6|Mentioned|p31|||||||||
6356|Eulo Queen Group|36228|6|Mentioned|Map legend|Middle Jurassic|Middle Jurassic|||||||
6356|Eulo Queen Group|36229|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
6356|Eulo Queen Group|37576|6|Mentioned|p34|||||||||
6356|Eulo Queen Group|37603|6|Mentioned|p444|||||||||
6356|Eulo Queen Group|37608|3|Fully described|Table 1|||See also Table 2.||||||
6356|Eulo Queen Group|38199|6|Mentioned|Fig.1|||||||||
6356|Eulo Queen Group|39211|6|Mentioned|p36|||Fig.26||||||
6356|Eulo Queen Group|39337|6|Mentioned|Fig.1|||||||||
6356|Eulo Queen Group|39445|5|Briefly described|p128|||Sedimentation cycles. See also Table 10||||||
6356|Eulo Queen Group|39797|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
6356|Eulo Queen Group|39917|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
6356|Eulo Queen Group|40218|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Late Jurassic||||||
6356|Eulo Queen Group|40659|6|Mentioned|p250|||||||||
6356|Eulo Queen Group|41064|6|Mentioned|p60|||||||||
6356|Eulo Queen Group|41125|6|Mentioned|p42|||||||||
6356|Eulo Queen Group|41266|6|Mentioned|Fig.3|||||||||
6356|Eulo Queen Group|42061|4|Described|p155|||See also Fig.11||||||
6356|Eulo Queen Group|42637|5|Briefly described|p9|||||||||
6356|Eulo Queen Group|43286|5|Briefly described|Map Legend||Jurassic|||||||
6356|Eulo Queen Group|43603|5|Briefly described|p9|Late Jurassic|Middle Jurassic|||||||
6356|Eulo Queen Group|43630|6|Mentioned|Fig.4,p7||Jurassic|||||||
6356|Eulo Queen Group|45145|3|Fully described|Table 5|||||||||
6356|Eulo Queen Group|46791|6|Mentioned|Table 2|||||||||
6356|Eulo Queen Group|46937|6|Mentioned|Fig.10|||||||||
6356|Eulo Queen Group|49010|6|Mentioned|Fig.4|||Carpentaria Basin||||||
6356|Eulo Queen Group|49011|6|Mentioned|Fig.3|||Carpentaria Basin||||||
6356|Eulo Queen Group|50199|5|Briefly described|Map Legend|Jurassic|Jurassic|Includes: Loth Formation, Hampstead Sandstone.||||||
6356|Eulo Queen Group|50200|5|Briefly described|Map Legend|Jurassic|Jurassic|Includes: Loth Formation, Hampstead Sandstone.||||||
6356|Eulo Queen Group|50201|5|Briefly described|Map legend|Jurassic|Jurassic|||||||
6356|Eulo Queen Group|50210|5|Briefly described|Map Legend|Jurassic|Jurassic|Includes: Hampstead Sandstone, Loth Formation.  Underlies: Gilbert River Formation.||||||
6356|Eulo Queen Group|50211|5|Briefly described|Map Legend|Jurassic|Jurassic|Includes the Loth Formation and Hampstead Sandstone.||||||17-MAY-04
6356|Eulo Queen Group|50595|5|Briefly described|Map Legend|Early Cretaceous|Middle Jurassic|Includes: Hampstead Sandstone, Loth Formation.||||||
6356|Eulo Queen Group|50627|5|Briefly described|Map legend|Late Jurassic|Middle Jurassic|Includes the Hampstead Sandstone, and Loth  and Gilbert River Formations.||||||06-JUL-04
6356|Eulo Queen Group|60081|5|Briefly described|Map legend|Late Jurassic|Jurassic|Includes the Loth and Hamspstead Sandstone.  Quartzose sandstone, siltstone, minor shale and conglomerate.||||||22-JUL-04
6356|Eulo Queen Group|62837|5|Briefly described|Stratigraphic columns|Middle Jurassic|Hettangian|Age: 205-180 Ma. Geological Province: Burketown Depression.||||||01-MAR-10
6356|Eulo Queen Group|64707|5|Briefly described|Map legend|Jurassic|Jurassic|Includes Loth Formation and Hampstead Sandstone.||||||
6356|Eulo Queen Group|66529|6|Mentioned|p12 Fig.5 |||Presented as Eulo Qn Gp in figure, and does not appear elsewhere in article. Carpentaria Basin.|||Includes Hampstead Sandstone and Loth Formation.|||
6356|Eulo Queen Group|67323|5|Briefly described|p86, p96, p106|Jurassic|Jurassic|Carpentaria Basin. Appears as Eulo Queen beds on p86. A regional aquifer.||||||
6356|Eulo Queen Group|67402|5|Briefly described|p165 tbl LPB1, p176|Kimmeridgian|Oxfordian|Carpentaria Basin, Staaten Sub-basin. Contains aquifers. Generally 100m thick. See also p177, p180, p181 tbl CRP/KRM2, p226, p231.|||Includes the Loth Formation and Hampstead Sandstone.|Unconformably overlain by the Garraway Sandstone.||
6356|Eulo Queen Group|68349|5|Briefly described|Map legend.|Late Jurassic|Middle Jurassic|Carpentaria Basin.|||Includes Hampstead Sandstone and Loth Formation.|Is overlain conformably by Gilbert River Formation.||
6356|Eulo Queen Group|68417|6|Mentioned|Map Legend|Late Jurassic|Middle Jurassic|Of the Carpentaria Basin.|||Includes Loth Formation, Hampstead Sandstone.|Conformably overlain by the Gilbert River Formation.|Sandstone, siltstone, mudstone, conglomerate.|
6356|Eulo Queen Group|68553|6|Mentioned|Map legend; schematic diagram.|Jurassic|Jurassic|Eromanga and Carpentaria Basins. This unit is mapped with the Blantyre Sandstone under the symbol, Ju.||||||
6356|Eulo Queen Group|69297|6|Mentioned|p274 fig 4.3|Late Jurassic|Middle Jurassic |||||||
6356|Eulo Queen Group|69455|5|Briefly described|p39:15|||Southern Carpentaria Basin. Areally restricted.||||Is overlain by the Gilbert River Formation.|Includes quartzic sandstone.|12-JUL-16
6356|Eulo Queen Group|69591|5|Briefly described|p100|Jurassic|Jurassic|Fill in the Burketown Depression, overlying probably Permian tilloids.|||||Quartzose sandstones.|
6356|Eulo Queen Group|69594|5|Briefly described|p518, p521, p527-528, p540, p573|Late Jurassic|Middle Jurassic|Southern Staaten Sub-basin, Carpentaria Basin; extends into the northern Eromanga Basin. Deposited in palaeotopographic depressions. The two constituents are not differentiated in the Eromanga Basin.|||Hampstead Sandstone, Loth Formation.|Is overlain disconformably/unconformably by the Gilbert River Formation. Part-equivalent to Dalrymple Sandstone (Laura Basin).||
6356|Eulo Queen Group|70207|6|Mentioned|p14|Jurassic|Jurassic|Georgetown region.||||||
6356|Eulo Queen Group|72297|5|Briefly described|p746|||Carpentaria Basin. Excellent hydrocarbon reservoir potential because it contains aquifers.|||Garraway Sandstone.|||
6356|Eulo Queen Group|72298|5|Briefly described|p801|Jurassic|Jurassic|Carpentaria Basin.|||Hampstead Sandstone, Loth FZ.|Is overlain by Gilbert River FZ.||
6356|Eulo Queen Group|73144|6|Mentioned|p8|Jurassic|Jurassic|Carpentaria Basin. Aquifer. Basal and upper unconformity.||||||
6356|Eulo Queen Group|73147|5|Briefly described|p126-130|Late Jurassic|Middle Jurassic|Gregory Range area.|||Hampstead Sandstone, Loth Formation.|Is overlain by Yappar Member (Gilbert River Formation).||
6401|Eva Valley Granite|9538|5|Briefly described|Map legend|Proterozoic|Proterozoic|Biotite leucogranite, biotite granite and latered biotite granite.||||||28-OCT-04
6401|Eva Valley Granite|23216|5|Briefly described|Table1p9,14,18-9|||||||||
6401|Eva Valley Granite|23733|5|Briefly described|p32 Fig. 19|||Of Edith River Group.||||||
6401|Eva Valley Granite|24197|5|Briefly described|p28, p106 Tb. 15.1|Paleoproterozoic|Paleoproterozoic|Of the Jim Jim Suite. Age: ~1825Ma. Geological Province: Pine Creek Inlier.||||||07-FEB-11
6401|Eva Valley Granite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
6401|Eva Valley Granite|41406|6|Mentioned|Map legend|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
6401|Eva Valley Granite|43149|5|Briefly described|Map Legend||Paleoproterozoic|Of Orosirian age.||||||07-NOV-08
6401|Eva Valley Granite|50586|5|Briefly described|p1.1, 5.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Of the Jim Jim Suite.||||||07-NOV-08
6401|Eva Valley Granite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1820-1850Ma. I-type. Fine biotite leucogranite, fine to coarse biotite granite. Intrudes Grace Creek Granite.||||||07-JAN-09
6401|Eva Valley Granite|67564|6|Mentioned|p85.|Orosirian|Orosirian|Eastern Pine Creek Orogen.||Unit in David Suite.||||
6401|Eva Valley Granite|69420|5|Briefly described|p5:18, 21, 23|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Mineralogy and petrology/geochemistry summarised.||Jim Jim Suite.|||Biotite leucogranite and porphyritic biotite leucogranite.|12-JUL-16
6432|Ewen Granite|22747|6|Mentioned|p8||Statherian|Age: 1770 Ma.||||||18-SEP-06
6432|Ewen Granite|23518|5|Briefly described|p9 Fig.3|Proterozoic|Proterozoic|Geological Province: Kalkadoon-Ewen Province.||||||
6432|Ewen Granite|24197|5|Briefly described|p21, p93|Paleoproterozoic|Paleoproterozoic|Of the Kalkadoon Supersuite. Geological province: Mount Isa Inlier. See also p94 Tb. 12.1 (Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
6432|Ewen Granite|29969|6|Mentioned|p394|||||||||
6432|Ewen Granite|30095|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
6432|Ewen Granite|30534|6|Mentioned|p302|||See also P305||||||
6432|Ewen Granite|30536|6|Mentioned|p102|||||||||
6432|Ewen Granite|30723|6|Mentioned|p341|||Geological map||||||
6432|Ewen Granite|30725|5|Briefly described|p574|||||||||
6432|Ewen Granite|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
6432|Ewen Granite|31821|6|Mentioned|p1024|||||||||
6432|Ewen Granite|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
6432|Ewen Granite|32660|5|Briefly described|Table 5|||||||||
6432|Ewen Granite|32951|5|Briefly described|p1276|||||||||
6432|Ewen Granite|32959|6|Mentioned|Fig.21|||||||||
6432|Ewen Granite|33214|5|Briefly described|p1279|||||||||
6432|Ewen Granite|33897|6|Mentioned|p1280|||||||||
6432|Ewen Granite|33900|4|Described|p8|||Mention p7.||||||18-SEP-06
6432|Ewen Granite|35074|6|Mentioned|Fig.2|||||||||
6432|Ewen Granite|35295|6|Mentioned|p603|||||||||
6432|Ewen Granite|37462|5|Briefly described|Table4.VII|||||||||
6432|Ewen Granite|37568|6|Mentioned|p85|||||||||
6432|Ewen Granite|38232|6|Mentioned|p82|||||||||
6432|Ewen Granite|38276|6|Mentioned|Fig.1|||||||||
6432|Ewen Granite|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
6432|Ewen Granite|38560|6|Mentioned|p113|||||||||
6432|Ewen Granite|38833|6|Mentioned|p161|||||||||
6432|Ewen Granite|39202|6|Mentioned|p234|||||||||
6432|Ewen Granite|39445|5|Briefly described|Table 2|||See also p35 and p39.||||||18-SEP-06
6432|Ewen Granite|39556|5|Briefly described|Map legend|Carpentarian|Paleoproterozoic|Early Proterozoic to Carpentarian||||||07-NOV-08
6432|Ewen Granite|39798|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
6432|Ewen Granite|39934|6|Mentioned|Fig.3|||||||||
6432|Ewen Granite|40648|6|Mentioned|p6|||||||||
6432|Ewen Granite|40840|6|Mentioned|Map legend|||||||||
6432|Ewen Granite|41307|4|Described|p20|||||||||
6432|Ewen Granite|41465|5|Briefly described|p7|||||||||
6432|Ewen Granite|41961|6|Mentioned|Table 1 P39|||||||||
6432|Ewen Granite|41979|6|Mentioned|Table 1 P510|||||||||
6432|Ewen Granite|42754|6|Mentioned|p3|||||||||
6432|Ewen Granite|44068|14|Not recorded|p4|||||||||
6432|Ewen Granite|44091|14|Not recorded|p10||Paleoproterozoic|||||||07-NOV-08
6432|Ewen Granite|44210|14|Not recorded|p8|||||||||
6432|Ewen Granite|44257|14|Not recorded|p19,21,22|||1760-1800 Ma. Rb-Sr.||||||
6432|Ewen Granite|44271|14|Not recorded|p37,38,45|||Intrudes Argylla Formation. Overlain by Eastern Creek Volcanics.||||||
6432|Ewen Granite|44275|14|Not recorded|Map Legend|||||||||
6432|Ewen Granite|44276|14|Not recorded|p17|||||||||
6432|Ewen Granite|44279|14|Not recorded|p5,map|||||||||
6432|Ewen Granite|44749|14|Not recorded|p25,26|||||||||
6432|Ewen Granite|44751|14|Not recorded|p300||Precambrian|||||||
6432|Ewen Granite|44765|14|Not recorded|p15||Paleoproterozoic|||||||07-NOV-08
6432|Ewen Granite|44766|14|Not recorded|p23,25|||Age: 1760Ma. Suggests equivalent to older phase of Kalkadoon Granite.||||||
6432|Ewen Granite|44849|14|Not recorded|p69,74-5,87|||1780 Ma = approx age of Sybella Granite.||||||18-JUL-13
6432|Ewen Granite|44918|14|Not recorded|p75,77,88|||Emplaced in Argylla Formation at 1780+/- 20 Ma. (see NT author card)||||||18-JUL-13
6432|Ewen Granite|44989|2|Defined|p145-7|||Tb.IV. On many pages. Intrudes Argylla Formation. Underlies Eastern Creek Volcanics. (E54-14).||||||18-SEP-06
6432|Ewen Granite|45052|6|Mentioned|p73|||Rb/Sr age.||||||
6432|Ewen Granite|45087|5|Briefly described|p21|||Chemical analyses.||||||
6432|Ewen Granite|45166|6|Mentioned|p13|||||||||
6432|Ewen Granite|45287|14|Not recorded|p.227,228|||Related to Argylla Formation?||||||
6432|Ewen Granite|46801|6|Mentioned|p117|||See also Fig. 14||||||
6432|Ewen Granite|46919|6|Mentioned|p221|||||||||
6432|Ewen Granite|46962|4|Described|Fig.3|||||||||
6432|Ewen Granite|48906|14|Not recorded|p4|||||||||
6432|Ewen Granite|49041|5|Briefly described|Table 2|||||||||
6432|Ewen Granite|50100|5|Briefly described|p13 Fig.4|Orosirian|Orosirian|Geological Province: Western Fold Belt Province.||||||
6432|Ewen Granite|50536|5|Briefly described|p1.4, 2.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Kalkadoon Suite. Age: ~1820Ma (U-Pb).||||||07-NOV-08
6432|Ewen Granite|63866|5|Briefly described|p60|Orosirian|Orosirian|Kalkadoon-Leichhardt Belt.|c. 1820 Ma (Wyborn and Page, 1983)|||||
6432|Ewen Granite|65505|6|Mentioned|969, 978, 981, Fig1,4|Proterozoic|Proterozoic|Kalkadoon-Leichhardt Block basement. Age: 1856 +/-3 Ma (zircon).||||||
6432|Ewen Granite|66529|6|Mentioned|p67, p94|Paleoproterozoic|Paleoproterozoic|High potential along its eastern margin for magmatic-hydrothermal U mineralisation.||Unit in Kalkadoon Supersuite.||||
6432|Ewen Granite|67323|4|Described|GIS attrib tbl, Solid Geology Map, p14|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Kalkadoon Igneous Event. Kalkadoon-Leichhardt Domain, central Mount Isa Block. Age:1840 +/-20 Ma (Wyborn & Page 1983), 1859+/-3.3 Ma (Magee et al, in prep) from close to boundary with Eastern Creek Volcanics. May be two plutons of distinctly different age.|1856 +/- 3.3 Ma.|Kalkadoon Suite or Supersuite||Intrudes Leichhardt Volcanics. Boundary with Eastern Creek Volcanics appears to be intrusive.|Medium pink leucogranite, pink to grey coarse porphyritic granite and granodiorite microgranite, pegmatite, schist, mylonite; some phases possibly coeval with Kalkadoon Granite.|
6432|Ewen Granite|67539|5|Briefly described|p2, p3, p3 Fig.2, p4 Fig.3|||Boundary relationships reviewed. May be two distinct phases and ages. Description of outcrops has been modified significantly to include more metabasalt enclaves and less dolerite dykes. Outcrop is commonly as much as  ~ 15% enclaves of metabasalt. ||||Intrudes Myally Subgroup, parts of the Eastern Creek Volcanics, but in other places unconformably overlain by Dynamite Creek Member, Eastern Creek Volcanics.||
6432|Ewen Granite|68146|6|Mentioned|p193|||Age determinations by several authors (listed) are similar to the age determined in this study for the Kalkadoon Granodiorite and Plum Mountain Gneiss.||||||
6432|Ewen Granite|68575|5|Briefly described|p1, p6-7, p112-117, p124, p134|||Kalkadoon-Leichhardt Domain, Mount Isa Province. Whole rock Sm-Nd isotopic data and age (1859 Ma).|1859 +/- 3 Ma.||||Altered, coarse-grained granite characterised by euhedral plagioclase (typically replaced by fine-grained sericite) and interstitial microcline.|
6432|Ewen Granite|69591|5|Briefly described|p31, p60|||Kalkadoon Batholith, Kalkadoon-Leichhardt Domain, Mount Isa Province. Also dated as 1840 +/- 20 Ma (Wyborn and Page, 1983).|1859 +/- 3.3 Ma (Magee et al. in press).|Kalkadoon Suite.|||Medium pink leucogranite, pink to grey coarse porphyritic granite and granodiorite, microgranite, pegmatite, schist, mylonite; some phases possibly coeval with Kalkadoon Granodiorite.|
6432|Ewen Granite|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic||||||Pink medium-grained leucogranite, pink to grey coarse-grained porphyritic granite and granodiorite, microgranite, pegmatite, schist and mylonite. Coarse-grained granodiorite and tonalite (mapped separately).|
6432|Ewen Granite|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic||||||Pink medium-grained leucogranite, pink to grey coarse-grained porphyritic granite and granodiorite, microgranite, pegmatite, schist and mylonite. Coarse-grained granodiorite and tonalite (mapped separately).|
6432|Ewen Granite|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1859+/-3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
6432|Ewen Granite|72889|5|Briefly described|p1, p3, p7, p9-12, p17-18.|Orosirian|Orosirian|Kalkadoon-Leichhardt Domain. Magmatic crystallisation age of main phase  well established by zircon U-Pb SHRIMP dating. This Record reports magmatic crystallisation age of a quartz-poor phase that might be a younger intrusion, but the age obtained,1853.5+/-3.6 Ma, is within uncertainty of the main phases. The coarse grained granodiorite has a U-Pb age of 1855.9 +/- 2.4 Ma (Neumann et al., 2009). Refer to 1:250 000 sheet DOBBYN (SE5414). Located in Mount Isa Orogen. Part of the Ewen Batholith, a 72km x 15km body of granite rocks. Age derived from Sensitive High Resolution Ion MicroProbe (SHRIMP) U-Pb zircon results.|1859 +/- 3 Ma. (Magee et al., 2012)|Kalkadoon Suite||Coeval with Kalkadoon Granodiorite.|Includes medium-grained, leucogranite, coarse porphyritic granite and granodiorite phases and smaller outcrops of coarse-grained granodiorite and tonalite phases.|25-NOV-20
6432|Ewen Granite|72919|6|Mentioned|p7|Orosirian|Orosirian|Mount Isa Province. Ages of 1856 +/- 3 Ma and 1859 +/- 3 Ma were reported by Neumann et al. (2009) and Magee et al. (2012), respectively.|1856 +/- 3 Ma, 1859 +/- 3 Ma|||||
6432|Ewen Granite|73525|5|Briefly described|p4-5 Fig.2, p17, p19 Fig.13|Orosirian|Orosirian|Leichhardt River and Kalkadoon-Leichhardt Domains.|1856+/-3 Ma crystallisation age||||Felsic intrusive.|
6432|Ewen Granite|73553|6|Mentioned|p6|||Kalkadoon-Leichhardt Domain.||Kalkadoon Suite||||
6451|Eyre Formation|13497|5|Briefly described|p115, p115 fig 6.33, p146, p151|Tertiary|Tertiary|Lake Eyre Basin.||||Unconformably overlies the Mount Howie Sandstone and the Winton Formation. Unconformably overlain by the Namba Formation.|Fluvial sandstone with a basal conglomerate.|
6451|Eyre Formation|22442|6|Mentioned|p54|Tertiary|Tertiary|||||||
6451|Eyre Formation|22495|6|Mentioned|P222|Eocene|Paleocene|||||||
6451|Eyre Formation|22587|4|Described|p71|Middle Eocene|Paleocene|||||||
6451|Eyre Formation|22671|6|Mentioned|Fig2p837|Tertiary|Tertiary|Sandstone sediments.||||||17-JAN-06
6451|Eyre Formation|22700|6|Mentioned|p775|Tertiary|Tertiary|Of Thomson Fold Belt.||||||18-SEP-06
6451|Eyre Formation|22712|5|Briefly described|p132|Tertiary|Tertiary|||||||
6451|Eyre Formation|22730|4|Described|p557,66,67|Eocene|Paleocene|After Wopfner 1974.||||||18-SEP-06
6451|Eyre Formation|22773|5|Briefly described|p355|||||||||
6451|Eyre Formation|22857|5|Briefly described|p355|Middle Eocene|Paleocene|Thickness: ~30m in SA borehole near border. Geological Province: Lake Eyre Basin.||||||
6451|Eyre Formation|22912|5|Briefly described|32|||Geol province Lake Eyre Basin.||||||26-NOV-08
6451|Eyre Formation|23154|5|Briefly described|Map Legend|Middle Eocene|Late Paleocene|Geological Province - Lake Eyre Basin - Callabonna Basin.||||||
6451|Eyre Formation|23155|4|Described|p33|Tertiary|Tertiary|Location of type section is advised p33. Unit does not crop out on STRZELECKI, but is present over all of the area. Overlying unit - Namba Formation (disconformity).  Underlain by Winton Formation (disconformity).||||||03-MAY-13
6451|Eyre Formation|23224|5|Briefly described|p3|Eocene|Paleocene|May correlate to Tertiary cover over White Cliffs Opal fields.||||||07-MAR-06
6451|Eyre Formation|23336|6|Mentioned|4|||||||||
6451|Eyre Formation|23339|5|Briefly described|4|Tertiary|Tertiary|||||||
6451|Eyre Formation|23380|5|Briefly described|p107-108|Eocene|Paleocene|||||||
6451|Eyre Formation|23477|5|Briefly described|p49 Fig 3|Tertiary|Tertiary|Geological Province: Curnamona Province.||||||
6451|Eyre Formation|23478|5|Briefly described|p28|Eocene|Paleocene|||||||
6451|Eyre Formation|23889|5|Briefly described|p18|Paleogene|Paleogene|||||||07-NOV-08
6451|Eyre Formation|23982|6|Mentioned|p96 Appendix 13|||Geological Province: Great Artesian Basin.||||||
6451|Eyre Formation|24175|3|Fully described|p32, p32 Fig. 6|Eocene|Paleocene|Unconformably overlain by Etadunna Formation. Max. thickness: ~100 m. Geological Province: Lake Eyre Basin.||||||03-MAY-13
6451|Eyre Formation|24176|5|Briefly described|p19, p22 Tb. 1|Tertiary|Tertiary|Freshwater sands and gravels - calcareous sandstone, quartzite; agate, quartz and chert pebbles. Corresponds to the Murnpeowie Formation defined by Forbes (1966).||||||26-NOV-08
6451|Eyre Formation|24204|5|Briefly described|p263 Fig.4|Tertiary|Tertiary|Geological Province: Eyre Basin.||||||
6451|Eyre Formation|24321|5|Briefly described|Map legend|Early Eocene|Late Paleocene|Geological Province: Lake  Eyre Basin.||||||26-NOV-08
6451|Eyre Formation|24345|5|Briefly described|p82, 84-85 Fig.2|Eocene|Paleocene|||||||
6451|Eyre Formation|29658|6|Mentioned|p5|||||||||
6451|Eyre Formation|29660|6|Mentioned|p4|||||||||
6451|Eyre Formation|30054|5|Briefly described|p803|||||||||
6451|Eyre Formation|30055|6|Mentioned|p160|||||||||
6451|Eyre Formation|30056|6|Mentioned|p125|||See also p129, p134.||||||18-SEP-06
6451|Eyre Formation|30176|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
6451|Eyre Formation|30540|6|Mentioned|Fig.6|||||||||
6451|Eyre Formation|30804|4|Described|p12|||Lithology. See also Table 1||||||
6451|Eyre Formation|30807|6|Mentioned|p102|||Suggested map symbol||||||
6451|Eyre Formation|30919|6|Mentioned|Map legend|Eocene|Paleocene|Palaeocene - Eocene||||||
6451|Eyre Formation|30920|6|Mentioned|Map legend|Eocene|Paleocene|Palaeocene - Eocene||||||
6451|Eyre Formation|30921|6|Mentioned|Map legend|Oligocene|Oligocene|||||||
6451|Eyre Formation|31850|6|Mentioned|p33|||||||||
6451|Eyre Formation|32121|6|Mentioned|p422|||||||||
6451|Eyre Formation|32275|6|Mentioned|p9|||||||||
6451|Eyre Formation|33568|6|Mentioned|p48|||||||||
6451|Eyre Formation|33820|6|Mentioned|Map legend|Eocene|Paleocene|Palaeocene - Eocene||||||
6451|Eyre Formation|33821|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
6451|Eyre Formation|33822|6|Mentioned|Map legend|Eocene|Paleocene|Palaeocene - Eocene||||||
6451|Eyre Formation|33823|6|Mentioned|Map legend|Eocene|Paleocene|Paleocene - Eocene||||||
6451|Eyre Formation|33824|6|Mentioned|p7|||See also p12, Tables 1 and 2.||||||18-SEP-06
6451|Eyre Formation|33825|5|Briefly described|p8|||Strat. table. Lithology||||||
6451|Eyre Formation|33827|5|Briefly described|p14|||See also Table 1||||||
6451|Eyre Formation|33828|6|Mentioned|p11|||Table 1||||||
6451|Eyre Formation|33831|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
6451|Eyre Formation|33832|6|Mentioned|p6|||Strat.||||||
6451|Eyre Formation|33937|6|Mentioned|p1|||||||||
6451|Eyre Formation|33938|2|Defined|p18|early Tertiary|early Tertiary|||||||
6451|Eyre Formation|33971|6|Mentioned|p37|||Strat. section Fig. 15.||||||
6451|Eyre Formation|34882|6|Mentioned|Fig. 1|||||||||
6451|Eyre Formation|35187|6|Mentioned|Table1|||||||||
6451|Eyre Formation|35793|6|Mentioned|p237|||||||||
6451|Eyre Formation|36554|6|Mentioned|p1647|||||||||
6451|Eyre Formation|36618|5|Briefly described|Table 1|||||||||
6451|Eyre Formation|36620|5|Briefly described|Fig.1|||See also p24.||||||18-SEP-06
6451|Eyre Formation|36922|6|Mentioned|Fig.3|||||||||
6451|Eyre Formation|36966|6|Mentioned|p81|||||||||
6451|Eyre Formation|37062|6|Mentioned|p182|||||||||
6451|Eyre Formation|37607|6|Mentioned|p333|||See also Fig.4.||||||
6451|Eyre Formation|37776|6|Mentioned|Fig.2|||||||||
6451|Eyre Formation|38022|6|Mentioned|p29|||||||||
6451|Eyre Formation|38226|6|Mentioned|Table 1|||||||||
6451|Eyre Formation|38557|5|Briefly described|p291|||||||||
6451|Eyre Formation|38605|6|Mentioned|p35|||||||||
6451|Eyre Formation|38740|5|Briefly described|p306|||||||||
6451|Eyre Formation|39084|6|Mentioned|p22|||||||||
6451|Eyre Formation|39085|6|Mentioned|p13|||||||||
6451|Eyre Formation|39087|6|Mentioned|p15|||||||||
6451|Eyre Formation|39322|6|Mentioned|Fig.2|||||||||
6451|Eyre Formation|39352|6|Mentioned|Map legend|Miocene|Paleocene|Miocene to Palaeocene||||||
6451|Eyre Formation|39445|5|Briefly described|Table 14|||See also Fig.11.2||||||
6451|Eyre Formation|39478|6|Mentioned|Table 1|||||||||
6451|Eyre Formation|39949|6|Mentioned|p274|||||||||
6451|Eyre Formation|40220|6|Mentioned|p7|||||||||
6451|Eyre Formation|40395|6|Mentioned|p313|||||||||
6451|Eyre Formation|40595|6|Mentioned|p93|||||||||
6451|Eyre Formation|40756|6|Mentioned|p1|||||||||
6451|Eyre Formation|40757|6|Mentioned|p75|||||||||
6451|Eyre Formation|40910|6|Mentioned|p17|||||||||
6451|Eyre Formation|40911|6|Mentioned|Map legend|Eocene|Paleocene|Palaeocene-Eocene||||||
6451|Eyre Formation|40914|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
6451|Eyre Formation|40925|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
6451|Eyre Formation|40926|3|Fully described|p22|||||||||
6451|Eyre Formation|40950|6|Mentioned|p250|||||||||
6451|Eyre Formation|40982|6|Mentioned|p363|||||||||
6451|Eyre Formation|41085|6|Mentioned|Fig.8|||||||||
6451|Eyre Formation|41098|4|Described|p177|||||||||
6451|Eyre Formation|41125|6|Mentioned|p34|||||||||
6451|Eyre Formation|41165|5|Briefly described|p364|||Mention  Fig.21||||||
6451|Eyre Formation|41184|6|Mentioned|p347|||||||||
6451|Eyre Formation|41198|6|Mentioned|Table 1|||||||||
6451|Eyre Formation|41517|6|Mentioned|p140|||||||||
6451|Eyre Formation|41535|6|Mentioned|p368|||||||||
6451|Eyre Formation|41600|6|Mentioned|p816|||||||||
6451|Eyre Formation|42084|6|Mentioned|Fig.3 P356|||||||||
6451|Eyre Formation|42090|3|Fully described|p14|||See also Table 2.||||||18-SEP-06
6451|Eyre Formation|42340|5|Briefly described|p25|Eocene|Late Paleocene|||||||07-NOV-08
6451|Eyre Formation|42375|3|Fully described|p21-25, p29|early Oligocene?|Paleocene|Geological province: Birdsville Basin.||||||18-SEP-06
6451|Eyre Formation|42469|5|Briefly described|p35, p43, p44|||||||||
6451|Eyre Formation|42475|6|Mentioned|p20|||Birdsville Basin||||||
6451|Eyre Formation|42496|5|Briefly described|Fig.3 P132|||||||||
6451|Eyre Formation|42508|5|Briefly described|p66, p74|||||||||
6451|Eyre Formation|42541|6|Mentioned|p220|||||||||
6451|Eyre Formation|42543|5|Briefly described|Fig.4 P6|||||||||
6451|Eyre Formation|42592|5|Briefly described|Fig. 4 P270|||||||||
6451|Eyre Formation|42746|4|Described|p13|||See also Fig.2, Fig.9||||||
6451|Eyre Formation|42905|5|Briefly described|p23|||see also Fig.5.3||||||
6451|Eyre Formation|42957|6|Mentioned|p40|||||||||
6451|Eyre Formation|42999|6|Mentioned|p98|||||||||
6451|Eyre Formation|43035|5|Briefly described|p27|||||||||
6451|Eyre Formation|43048|5|Briefly described|p22|||||||||
6451|Eyre Formation|43052|5|Briefly described|Table 2.1|||||||||
6451|Eyre Formation|43053|5|Briefly described|Map Legend|Eocene|Paleocene|Fluvial sand and conglomerate, usually silcreted. Geological Province: Lake Eyre Basin.||||||25-MAY-05
6451|Eyre Formation|43071|5|Briefly described|p17|||||||||
6451|Eyre Formation|43094|5|Briefly described|p38|||||||||
6451|Eyre Formation|43258|5|Briefly described|Map Legend|Eocene|Paleocene|||||||
6451|Eyre Formation|43298|5|Briefly described|Map Legend|Eocene|Paleocene|||||||
6451|Eyre Formation|44041|6|Mentioned|p242|||||||||
6451|Eyre Formation|44133|4|Described|p192, 124, 190 Fig. 10.30|Middle Eocene|Late Paleocene|Geological Province: Lake Eyre Basin. Includes the Macumba Sandstone, Murnpowie Formation. Overlain unconformably by the Etadunna and Namba Formations.||||||
6451|Eyre Formation|44934|5|Briefly described|Map Legend|Miocene|Eocene|||||||
6451|Eyre Formation|45145|6|Mentioned|Table 7|||||||||
6451|Eyre Formation|46800|4|Described|p112|||See also p114.||||||18-SEP-06
6451|Eyre Formation|46802|6|Mentioned|Table 1|||||||||
6451|Eyre Formation|46833|6|Mentioned|p53|||||||||
6451|Eyre Formation|46854|6|Mentioned|p242|||||||||
6451|Eyre Formation|46902|6|Mentioned|Table 1|||Correlation chart for Cainozoic land-surfaces||||||
6451|Eyre Formation|46911|5|Briefly described|p113|||Analyses of weathered profiles and parent rocks.||||||
6451|Eyre Formation|60648|6|Mentioned|p42|Cenozoic|Cenozoic|||||||19-NOV-08
6451|Eyre Formation|60953|5|Briefly described|Map Legend|Eocene|Paleocene|Fluvial sand and conglomerate, usually silcreted. Geological Province: Lake Eyre Basin.||||||
6451|Eyre Formation|60955|5|Briefly described|Map Legend|Miocene|Eocene|Carbonaceous sandstones, siltstones, mudstones.||||||
6451|Eyre Formation|61108|5|Briefly described|map legend|Eocene|Paleocene|Fluvial sand and conglomerate, usually silcreted. Geological Province: Lake Eyre Basin.||||||
6451|Eyre Formation|61155|5|Briefly described|p2, p17|Middle Eocene|Late Paleocene|Sediments spread in thin sheets over large areas of the Birdsville Basin. Age: ~62-~42Ma. Max. thickness: 120m (in Lake Eyre Basin). Geological province: Oodnadatta area, Lake Eyre Basin and Tarkarooloo Basin.||||||03-MAR-10
6451|Eyre Formation|61823|5|Briefly described|p118|Middle Eocene|Paleocene|Overlain by Namba Formation. Age is Palaeogene.  Geological Province: Lake Eyre Basin.||||||
6451|Eyre Formation|61824|5|Briefly described|p128|Paleogene|Paleogene|Age is uncertain - it is also suggested that the rocks may be Mesozoic.||||||07-NOV-08
6451|Eyre Formation|61825|5|Briefly described|p138|Late Cretaceous|Late Cretaceous|Quartz and kaolin-rich sediments.  Overprinted by the "Cordillo Silcrete".  Geological Province:  Eromanga Basin.||||||
6451|Eyre Formation|62376|5|Briefly described|p84|Tertiary|Tertiary |Geological Province: Pedirka Basin.||||||09-FEB-10
6451|Eyre Formation|62724|5|Briefly described|p16 Fig. 2|Tertiary|Tertiary|Sandstone. Geological Province: Curnamona Province.||||||07-FEB-11
6451|Eyre Formation|63102|4|Described|p8,62,67,71,73|Late Eocene|Late Paleocene|Geological province: Curnamona Province. Of Callabonna Sub-basin. Deposited in palaeochannels incised into weathered basement rocks in the area north of the Ranges but occurs as a more widespread sheet facies further to the north. Southern channelled facies sourced from erosion of weather basement rocks in the Olary Domain and is dominated by clay (kaolinite) mineralogy.||||Overlain by Namba Formation.|Carbonaceous sand; very fine to coarse, moderately sorted, subrounded to subangular, with minor clay lenses.|
6451|Eyre Formation|63789|5|Briefly described|Map Legend|Tertiary|Tertiary|Predominatly coarse-grained quartozse sandstone, derived in part fom decayed granites with lesser fine sandstone and fine conglomeratic lenses with highly polished pebbles including fossil wood.||||||
6451|Eyre Formation|63793|5|Briefly described|p30, p49.|Eocene|Paleocene|Earliest Tertiary; apparently locally derived.|||||Soft, white, friable, flat-lying, gritty sandstones.|
6451|Eyre Formation|64047|5|Briefly described|p60, p61|Middle Eocene|Late Paleocene|Broad correlation with Marion Formation is indicated.  Upper section is probably equivalent to Glendower Formation.||||||
6451|Eyre Formation|64197|6|Mentioned|p627, p630 Fig.6|Late Eocene|Late Palaeocene|||||Unconformably overlies the Winton Formation. Is overlain unconformably by Etadunna Formation.||
6451|Eyre Formation|64679|5|Briefly described|Map legend|Tertiary|Tertiary|Quartz sandstone, siltstone, claystone and conglomerate; commonly silicified.||||||11-AUG-09
6451|Eyre Formation|64682|5|Briefly described|Map Legend|Tertiary|Tertiary|Sandstone and silty or clay rich sandstone.||||||
6451|Eyre Formation|64778|6|Mentioned|p13|Tertiary|Tertiary|Pedirka and Simpson Desert Basins.||||||
6451|Eyre Formation|64964|5|Briefly described|p160|Eocene|Paleocene|Thickness: 80m. Comprises fine-grained brown sandstone and clay with some boulders of Devonian sandstone. No fossils apart from a few worm burrows.||||||08-APR-09
6451|Eyre Formation|65194|5|Briefly described|p44-50|Eocene|Eocene|Fluvial sands. Overlain by Namba Formation. Fining-upward, braided-river sequences of angular, quartz-rich, poorly sorted sands interbedded with kaolinitic clays.||||||
6451|Eyre Formation|65238|5|Briefly described|p7 Fig. 8|Tertiary|Tertiary |Geological province: Eyre Basin. Fluvial and aeolian deposits.||||||
6451|Eyre Formation|65342|5|Briefly described|p9.|||Eromanga Basin. Max. thickness at least 191 m. Seen as having potential as an insulating layer for geothermal energy.||||Overlies Winton Formation.|Carbonaceous sandstone, siltstone, mudstone.|
6451|Eyre Formation|65484|5|Briefly described|p 28, 30, Fig 2|Tertiary|Tertiary|Tectonically  tilted exposure, laterally equivalent to sediments hosting Four Mile mineralisation. Later stages include silcrete development.||||||01-MAY-15
6451|Eyre Formation|65489|6|Mentioned|p60|||||||Unconformably overlies Winton Formation.||
6451|Eyre Formation|65925|4|Described| pp16-21, p47-69,  p139, Appendix 2.|Eocene|Latest Paleocene|Callabonna Sub-basin. Organic-rich sands host uranium deposits. Basal unit of Lake Eyre Basin. Fills a network of paleochannels.|Two-stage deposition: c.55-49 Ma and c.45-37 Ma.||Includes Murnpeowie Formation.|Unconformably overlies Bulldog Shale. Is disconformably overlain by Namba Formation.|Pyritic, carbonaceous sand, grain-size ranges from silt to small cobble, with beds of lignite and clay. Clays are montmorillonite, kaolinite and illite. Has silcrete cap. Braided streams.|
6451|Eyre Formation|66131|4|Described|p240-245, p248-253, p255, p258-259|Eocene|Paleocene|Widespread throughout Lake Eyre Basin. Latest Paleocene to Middle Eocene age based on palynological dating. ~100m thick. Plant fossils widespread. Largely deposited by braided streams.||||Correlative of the Glendower and Marion Formations. Equivalent to Mount Sarah Sandstone. Overlain by the Etadunna and Doonbarra Formations. Disconformably overlain by the Namba Formation.|Sandstone, carbonaceous clays and conglomerates. Lignite and clay, sometimes with root horizons, leaf beds and cross-bedding, are common. Diagnostic basal polished gravel.|
6451|Eyre Formation|66303|6|Mentioned|pp27-28, p31 Fig.5.|Paleogene|Paleogene|Lake Eyre Basin. Early Late Paleocene (Lygistepollenites balmei Zone) to Early Oligocene (Upper Nothofagidites asperus Zone). Uplifted, eroded and redeposited from Late Paleocene to Late Eocene. ||||Overlies Bulldog Shale. Is disconformably overlain by Namba Formation.||
6451|Eyre Formation|66518|5|Briefly described|p19 Fig.4, p20.|Cenozoic|Cenozoic|Basal unit in the Callabonna Sub-basin within Lake Eyre Basin. Fluvial sediments and alluvium. ||||Unconformably underlies Namba Formation.||
6451|Eyre Formation|66573|5|Briefly described|p873, p874 Fig.5, p875 Tb.2|Eocene|Paleocene|Disconformably overlain by the Etadunna Formation. Red claystones and silcretized sandstones.||||||
6451|Eyre Formation|66623|3|Fully described|p239, p248, pp268-276.|Eocene|Late Paleocene|Formerly Eyrian Series (Woolnough and David 1926). Equivalent to Glendower and Marion Formations; partly to Mount Sarah and Willalinchina Sandstones. Contains small polished erratic pebbles from underlying Cretaceous sequence. More strongly silicified sandstones are mapped as Cordillo Silcrete. Forms regional angular unconformity over variety of Cretaceous basement rocks. Top of this formation is marked by a palaeosol (Cordillo Surface, Wopnfer 1974) with silcrete cap (Cordillo Silcrete, Wopnfer 1978). Erosion of silcrete cap and Eyre Formation formed the overlying Doonbara Formation.|||In South Australia, incorporates Murnpeowie Formation and Macumba Sandstone.|Locally unconformably overlies Namur Sandstone and Easter Monday Formation. Grades upwards into Cordillo Silcrete. Is overlain unconformably by Doonbara Formation.|Sequence of mature quartz sandstones with local beds and laminae of distinctive and diagnostic, highly glossy, well-rounded, low-sphericity discoidal quartz pebble conglomerate  with subordinate black chert, yellow agate and silicified wood.|30-MAY-13
6451|Eyre Formation|66917|5|Briefly described|Map legend|Paleogene|Paleogene||||||Variably silcrete-altered quartzose sandstone, minor pebbly sandstone and conglomerate; ubiquitous glossy quartz pebbles.|
6451|Eyre Formation|66920|5|Briefly described|Map legend|Paleogene|Paleogene||||||Variably silcrete-altered quartzose sandstone, minor pebbly sandstone and conglomerate; ubiquitous glossy quartz pebbles.|
6451|Eyre Formation|66921|5|Briefly described|Map legend|Paleogene|Paleogene||||||Variably silcrete-altered quartzose sandstone, minor pebbly sandstone and conglomerate; ubiquitous glossy quartz pebbles.|
6451|Eyre Formation|67119|5|Briefly described|Map legend.|Eocene|Paleocene|Braided stream deposits.|||||Pyritic, carbonaceous sand, silt- to small cobble-sized grains, with beds of lignite and clay (montmorillonite, kaolinite and illite).|
6451|Eyre Formation|67207|5|Briefly described|Map legend.|Neogene|Paleogene||||||Variably silcrete-altered quartzose sandstone, minor pebbly sandstone and conglomerate; ubiquitous glossy quartz pebbles.|19-SEP-11
6451|Eyre Formation|67208|5|Briefly described|Map legend.|||Shown in Paleogene - Neogene age grouping.|||||Variably silcrete-altered quartzose sandstone, minor pebbly sandstone and conglomerate; ubiquitous glossy quartz pebbles.|20-SEP-13
6451|Eyre Formation|67209|5|Briefly described|Map legend.|Paleogene|Paleogene||||||Variably silcrete-altered quartzose sandstone, minor pebbly sandstone and conglomerate; ubiquitous glossy quartz pebbles.|
6451|Eyre Formation|67210|5|Briefly described|Map legend.|||Age given as Paleogene-Neogene.||||Overlies Rolling Downs Group.|Variably silcrete-altered quartzose sandstone, minor pebbly sandstone and conglomerate; ubiquitous glossy quartz pebbles.|
6451|Eyre Formation|67211|5|Briefly described|Map legend.|||Age stated as Paleogene-Neogene.|||||Variably silcrete-altered quartzose sandstone, minor pebbly sandstone and conglomerate; ubiquitous glossy quartz pebbles.|
6451|Eyre Formation|67462|5|Briefly described|Map legend.|Paleogene|Paleogene|Lake Eyre Basin.||||||
6451|Eyre Formation|67562|6|Mentioned|p105 Fig.11|Eocene|Eocene||||||Kaolinitic fine-grained sandstone.|
6451|Eyre Formation|67578|5|Briefly described|p333-334, p336-337, p341-342, p344, p347|Eocene|Paleocene|Birdsville Basin. Multi-channel or braided stream deposits. Upper part widely affected by post-depositional silicification.||||Unconformably overlies Bulldog Shale.|Yellow and yellow-orange cross-bedded sands and thin grey-brown silty-clay.|
6451|Eyre Formation|68068|5|Briefly described|Map legend|Middle Eocene|Late Paleocene|Callabonna Sub-basin, Lake Eyre Basin. Gravel clasts include quartz, chalcedony, silicified wood, silcrete; occasional leaf impressions, often lignitic in drill sections. Commonly silcreted.||||Overlies Mulligan Dam Regolith.|Basal gravel of highly-polished well-rounded clasts, consolidated but not cemented; fluvial quartz sand, rounded to angular, fine- to coarse-grained, grit beds common, occasional laminated lacustrine silt and clay.|
6451|Eyre Formation|68157|6|Mentioned|p1, p13-16|Paleogene|Paleogene|Hosts Four Mile East, Honeymoon and Goulds Dam sandstone-hosted uranium deposits. Includes detrital zircons aged ~1.58 Ga, ~900 Ma and ~485 Ma.|||||Includes coarse-grained sandstone.|
6451|Eyre Formation|68203|6|Mentioned|p9 Fig.6|||Mount Lofty Ranges.||||Is faulted against Willawortina Formation.||
6451|Eyre Formation|68713|6|Mentioned|p23||||||||Fluvial-paludal sediment dominated by fine-grained quartz sand and silt, and has been overprinted by groundwater silcrete.|
6451|Eyre Formation|68715|6|Mentioned|p29, p31, p32 Fig.6|Paleogene|Paleogene|Lake Eyre Basin. Fluvial and aeolian deposits.||||Is overlain unconformably by Namba Formation.||07-APR-17
6451|Eyre Formation|68821|3|Fully described|p296, p297 Fig.3, p307, p310|Lutetian|Danian|< 120 m thick. Fluvial and locally lacustrine sedimentary rocks. Locally abundant wood fragments, and contains large trunks of fossil trees.|62 - 42 Ma|||Locally overlain by the Etadunna Formation and Namba Formation. Unconformably underlain by the Bulldog Shale Formation, Oodnadatta Formation, and Winton Formation.|Includes conglomerate, pyritic mature quartz sandstone with interbeds of clay lenses (44% kaolinite) and shale pebbles, carbonaceous and micaceous siltstone, dolomitic siltstone and lignite.|03-OCT-13
6451|Eyre Formation|69001|5|Briefly described|p2 Fig.1B, p16, p18 Fig.8, p22 p23|Eocene|Paleocene|Late Paleocene to Middle Eocene age. Fluvial sediments. Previously incorrectly correlated with the Gum Vale Beds and Gum Vale Formation.|||||Comprises dominantly fluvial sandstone, carbonaceous clastics and quartzose conglomerates.|
6451|Eyre Formation|69019|4|Described|p83, p94, p104-110 Figs.20,24-26.|Eocene|Paleocene|Of Wopfner et al. (1974) after the term 'Eyrian Series' of Woolnough and David (1926); also previously known as Murnpeowie Formation (Forbes, 1966). Extensive sandy flood plain deposits. Thickness from <10 to >170 m. Has developed silcrete-porcellanite horizons. Of interest to explorers for biogenic coal seam gas. See also Pl.20, p119.||||Disconformably overlies Winton Formation. Is overlain unconformably by Namba and Etadunna Formations. Faulted against Marree Subgroup.|Well-washed, mature, moderately sorted quartz sand; grit beds common; comnmonly carbonaceous and pyritic, with lignite interbeds towards the base.|
6451|Eyre Formation|69023|4|Described|p79, p87, p101, p105-106, p108-120|Eocene|Paleocene|See also p122-123, p125, p143-144, p153, p162-163, p193. Defined by Wopfner et al. (1974); previously Eyrian Series of Woolnough and David (1926), and Murnpeowie Formation of Forbes (1966). Seven reference areas are described in the definition; two are mentioned here. Lake Eyre Basin. c.62m thick. Plant matter is commonly preserved. A measured section is provided. Deposited as a widespread fluvial sand sheet. Weathering has formed porcellanite and a silcrete cap. Probable source (with Namba Formation) of Yandruwantha Sand. Potential supply of construction sand and road gravel. Stratigraphic wells intersection data.||||Conformably overlies Mulligan Dam Regolith. Disconformably overlies Winton Formation or Bulldog Shale. Is overlain unconformably by Namba Formation.|Black, grey and brown coloured. Well-washed, mature, fine- to medium-grained, moderately sorted sand with subrounded grains; commonly carbonaceous and pyritic; interbeds of lignite towards the base. Local silcrete and calcite cemented zones.|
6451|Eyre Formation|69458|5|Briefly described|p42:16|Eocene|Paleocene|Lake Eyre Basin. Extensive shallow, braided stream system deposits with local swamp and lake settings.|||||Basal conglomerate with highly polished, resistant pebble clasts overlain by cross-bedded, mature pyritic and carbonaceous coarse-grained sandstone; lignite and clay units, containing plant fossils, occur.|12-JUL-16
6451|Eyre Formation|69562|5|Briefly described|p662 Tb.2, p663 Fig.2, p664 Tb.4|Eocene|Paleocene|See also p666 Fig.3, p667 Fig.4, p668-669, p674-676, p679-684. Lake Eyre Basin. Deposition in paleovalleys. Hosts more than 90% of known (U) mineralisation in Lake Frome area; highly permeable sands: 5 sq.m/day measured. Rich in organic material (plants and pyrite) for reductants. Electrical conductivity value used in forward modelling: 200-500 mS/m.|c.55 Ma.|||Overlies Marree Subgroup. Is overlain by Namba Formation.|Mature, fine- to coarse-grained, unconsolidated, carbonaceous, pyritic sands; occasional lignitic sandy lenses near the base.|06-APR-22
6451|Eyre Formation|69568|5|Briefly described|p441, 443-444|Eocene|Paleocene|Lake Frome region; basal Lake Eyre Basin. Hosts the Beverley North uranium deposits. Occurs in S-N paleochannels, commonly incised into underlying strata. Two depositional stages: ~55-49 Ma and ~45-37 Ma. Drill-core logs.||||Unconformably overlies Bulldog Shale. Is overlain disconformably by Namba Formation.|Dominantly fluvial and lacustrine deposits, characterised by pyritic carbonaceous mature sands of very fine to pebble size; includes coal seams; regionally capped by silcrete lenses.|
6451|Eyre Formation|69599|5|Briefly described|p584, p599-600|Eocene|Paleocene|Senior (1979) and Senior and Mabbutt (1979) included under this name all Eyre Formation equivalents in the SW corner of QLD; Draper (2002) excepted the Marion Formation. Capped by silcrete and laterite of the Canaway profile.||||Correlated (at least partly) with Moonie, Glendower, Edkins, Springvale and Marion Formations; Werite and Old Cork beds; Mueller and Moses Sandstones.||
6451|Eyre Formation|69654|6|Mentioned|p4|||Curnamona Province.||||||
6451|Eyre Formation|69946|5|Briefly described|p29, p125, p129|Eocene|Paleocene|Lake Eyre Basin. Wopfner et al. (1974). Up to 140m thick. Weathering down to 60m. Local Cordillo Silcrete caps produce prominent mesas.|||||Fluvial, fine- to medium-grained quartz sandstone with lignite interbeds and a basal conglomerate which includes reworked Late Cretaceous sediment.|
6451|Eyre Formation|69947|5|Briefly described|p13 Fig.7.2|Eocene|Paleocene|Callabonna Sub-basin, Lake Eyre Basin.||||||
6451|Eyre Formation|69961|5|Briefly described|Map legend|Neogene|Paleogene||||||Variably silcrete-altered quartzose sandstone, minor pebbly sandstone and conglomerate; ubiquitous glossy quartz pebbles.|
6451|Eyre Formation|70383|5|Briefly described|p45, p62|Paleogene|Paleogene|Lake Eyre Basin. Fluvial sediments.||||Is overlain by Namba Formation.||
6451|Eyre Formation|70384|5|Briefly described|Map legend.|Eocene|Paleocene|Callabonna Sub-basin, Lake Eyre Basin. Dominantly a braided stream and floodplain deposit. Palynology age range: late Paleocene to middle Eocene. Rare leaf fossils in silt or clay layers; variably lignitic near base (+/- pyrite). Reddish horizons and silcrete mark paleosols.|||||Quartz sand, rounded to angular, fine- to coarse-grained; grit beds common, cross-bedded channel fill; occasional laminated lacustrine silt and clay; basal gravel with highly polished, well-rounded clasts. Consolidated, rarely cemented.|
6451|Eyre Formation|70649|5|Briefly described|Map Legend|Neogene|Paleogene||||||Variably silcrete-altered quartzose sandstone, minor pebbly sandstone and conglomerate; ubiquitous glossy quartz pebbles.|
6451|Eyre Formation|70651|5|Briefly described|Map Legend|Paleogene|Paleogene||||||Variably silcrete-altered quartzose sandstone, minor pebbly sandstone and conglomerate; ubiquitous glossy quartz pebbles.|
6451|Eyre Formation|70652|5|Briefly described|Map Legend|Paleogene|Paleogene|Fluvial sandstone. In-situ regolith and transported sediments also described.|||||Variably silcrete-altered quartzose sandstone, minor pebbly sandstone and conglomerate; ubiquitous glossy quartz pebbles.|
6451|Eyre Formation|70657|5|Briefly described|p9 Fig.3, p68, p72, p77-80|Neogene|Paleogene|Cover sequence in Olary Domain. Deposition in palaeochannels incised into weathered basement rocks, or as widespread sheet facies. Hosts roll-front U mineralisation (described) near the Benagerie Ridge. Late Eocene to late Paleocene.||||Is overlain by Namba Formation.|Sandstone; carbonaceous sand, fine to coarse, subrounded to subangular, and minor clay (mainly kaolinite) lenses.|
6451|Eyre Formation|70658|6|Mentioned|p14|Tertiary|Tertiary||||||Sandstone.|
6451|Eyre Formation|70821|5|Briefly described|p25|Eocene|Eocene|Previously the Eyre Gravel (eg Lovering et al., 1972) [misquoted as the Eyre gravel in this study]. Lake Eyre Basin (SA). Is equivalent to the dendritic ridges formed by the Glendower Formation in Queensland and NSW.|||||Silcrete and ferricrete.|
6451|Eyre Formation|70823|5|Briefly described|p46-p47|Middle Eocene|Paleocene|Interpreted to have been deposited in a braided stream fluvial setting.|||||Carbonaceous sand, silt and gravel with some lignite and clay beds.|
6451|Eyre Formation|71342|4|Described|Ch1 p6, Ch5 p29, Ch5 p130, Ch7 p13|Eocene|Paleocene|Lake Eyre Basin. Hosts a major confined aquifer. Deposited in a fluvial environment. Up to 140m thick in the Cooper region. ||||Overlain by the Cordillo Silcrete. Unconformably overlies the Winton Formation. Unconformably overlain by the Namba Formation.|Fine to medium-grained, quartz sandstone with lignite interbeds and a basal conglomerate.|
6451|Eyre Formation|71415|5|Briefly described|p11|Neogene|Paleogene|Geological province: SW Thomson Orogen. Of the Kooneberry Belt; of Eromanga Basin.||||||
6451|Eyre Formation|72456|5|Briefly described|Map Legend|Eocene|Paleocene|Marree 1:250k map sheet. Deposited in a braided stream environment.|||||Pyritic, carbonaceous sand, grain-size ranges from silt to small cobble, with bands of lignite and clay. Clays are montmorillite, kaolinite and illite.|
6451|Eyre Formation|72457|5|Briefly described|p91|Eocene|Palaeocene|Callabonna sub-basin.||||Is overlain by Namba Formation.|Fluvial sands and gravels.|
6451|Eyre Formation|72461|6|Mentioned|p24|Cenozoic|Cenozoic|||||||
6451|Eyre Formation|73090|6|Mentioned|p6|Eocene|Palaeocene|||||||
6451|Eyre Formation|73106|5|Briefly described|Map legend.|Eocene|Paleocene||||||Pyritic carbonaceous sand; grain size ranges from silt to small cobble, with beds of lignite and clay. Clays are montmorillonite, kaolinite and illite. Braided streams.|
6451|Eyre Formation|73188|6|Mentioned|p345|Eocene|Paleocene|Similar to North Maslin Sand.||||||
6451|Eyre Formation|73251|4|Described|p36-38, p40-48, p50-51, p53, p56-58, p62|Eocene|Eocene|Lake Eyre Basin (widespread), Callabonna Sub-basin (basal unit). Potential detrital U reductant and potential shallow hydrocarbon source rock. Sandstone hosts U mineralisation at Four Mile East, Goulds Dam, Honeymoon, Oban, and Pepegoona. Thermally sub-mature. Includes oil-prone organic facies. Depositional environments include non-marine, meandering fluvial, fluviolacustrine, peat swamp, and floodplains. Sediment recovery in drill holes was poor, especially where the sands are clean (clay-free). Thickness in drill holes ranges from ca 23 m to 45 m thickening eastwards. Contains Eyre [organic] facies 1, 2, and 3. [See article for organic petrology descriptions].||||Unconformably overlain by Namba Formation.|Amalgamated fine- to medium-grained quartz sandstone (both clean and carbonaceous), lignite and carbonaceous mudstone.|
6451|Eyre Formation|73281|6|Mentioned|Appendix (DIP)|||See DIP034_Welldata.xlsx.||||||
6451|Eyre Formation|73479|5|Briefly described|p156 Fig.2|Paleogene|Paleogene|Lake Eyre Basin.||||Unconformably overlies Winton Formation, underlies Etadunna Formation|Fresh water coarse sand.|
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
6582|Fengshan Formation|42058|6|Mentioned|p115|||||||||
6584|Fenn Gap Conglomerate Member|35102|6|Mentioned|p27|||||||||
6584|Fenn Gap Conglomerate Member|43503|6|Mentioned|29|||||||||
6584|Fenn Gap Conglomerate Member|48992|2|Defined|p26|Neoproterozoic|Neoproterozoic|||||||
6584|Fenn Gap Conglomerate Member|50246|5|Briefly described|p8|Neoproterozoic|Neoproterozoic|Of the Heavitree Quartzite.||||||07-FEB-11
6584|Fenn Gap Conglomerate Member|61309|5|Briefly described|p17|||Of the Heavitree Quartzite. Geological Province: Amadeus Basin.||||||06-FEB-08
6584|Fenn Gap Conglomerate Member|62595|6|Mentioned|p8. |||||Unit in Heavitree Quartzite.||||
6584|Fenn Gap Conglomerate Member|73086|3|Fully described|p7-9, p144|||Amadeus Basin. Of Stewart et al (1980). Type area: Heavitree Gap (34 m thick). Widespread, occurring along the entire northern margin of the basin. Contact with the underlying Temple Bar Sandstone Member is locally disconformable. [Also written as Fenn Gap Member on p7; see Wells, 1967].||Heavitree Formation||||
6631|Fickling Group|7071|5|Briefly described|p1|Mesoproterozoic|Paleoproterozoic|Geological Province: northern Mount Isa Inlier.||||||07-NOV-08
6631|Fickling Group|22457|6|Mentioned|Fig29 P30|||||||||
6631|Fickling Group|22479|5|Briefly described|fig4, pg10|Statherian|Statherian|||||||
6631|Fickling Group|22644|5|Briefly described|5|||Geological province: Mount Isa Basin. Underlain by Peters Creek Volcanics.||||||18-SEP-06
6631|Fickling Group|22665|6|Mentioned|P219, P229|||||||||
6631|Fickling Group|22673|6|Mentioned|63,64,65|||Geol province Mount Isa Basin. Overlying unit South Nicholson Group Volcanics, underlying unit Peters Creek Volcanics.||||||23-DEC-08
6631|Fickling Group|22680|5|Briefly described|83-87|Mesoproterozoic|Paleoproterozoic|Geological province: Mount Isa Basin.||||||07-NOV-08
6631|Fickling Group|23031|6|Mentioned|27|||||||||
6631|Fickling Group|23065|6|Mentioned|11|Proterozoic|Proterozoic|Geol province Lawn Hill Subprovince||||||
6631|Fickling Group|23066|5|Briefly described|p807, Fig.1|Proterozoic|Proterozoic|||||||
6631|Fickling Group|23362|6|Mentioned|337|||||||||
6631|Fickling Group|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
6631|Fickling Group|23395|6|Mentioned|p383|||||||||
6631|Fickling Group|23396|5|Briefly described|p407 Fig.2|||||||||
6631|Fickling Group|23397|5|Briefly described|p463|||||||||
6631|Fickling Group|23398|4|Described|p445|||||||||
6631|Fickling Group|23405|4|Described|p566|||||||||
6631|Fickling Group|23406|4|Described|p606, p609 Fig. 9|Paleoproterozoic|Paleoproterozoic|Includes Fish River Formation, Walford Dolomite, Mount Les Siltstone and Doomadgee Formation. Overlain by South Nicholson Group. Age: 1700-1585Ma. In the Murphy Inlier.||||||17-JUN-09
6631|Fickling Group|23409|5|Briefly described|p533|||||||||
6631|Fickling Group|23958|6|Mentioned|p1132|||||||||
6631|Fickling Group|24308|5|Briefly described|p987 Fig. 2|Mesoproterozoic|Paleoproterozoic|Geological Province:  Mount Isa Superbasin||||||07-NOV-08
6631|Fickling Group|24419|5|Briefly described|p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: Lawn Hill Subprovince (north).||||||07-NOV-08
6631|Fickling Group|24432|6|Mentioned|p566 Fig.5|Statherian|Statherian|||||||25-FEB-05
6631|Fickling Group|24442|6|Mentioned|p22|Mesoproterozoic|Mesoproterozoic|Revised as a new unit and probably belongs to the South Nicholson Group.  Formerly mapped in the Bauhinia Dome. Age: 1670-1600Ma.  Geological Province: McArthur Basin.  See also p23 Fig. 2.||||||
6631|Fickling Group|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
6631|Fickling Group|31421|6|Mentioned|p509|||||||||
6631|Fickling Group|35640|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
6631|Fickling Group|36012|3|Fully described|Table 3|||See also p16.||||||09-AUG-06
6631|Fickling Group|36439|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
6631|Fickling Group|36442|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
6631|Fickling Group|37462|4|Described|Table4.VII|||||||||
6631|Fickling Group|37565|6|Mentioned|Fig.5|||||||||
6631|Fickling Group|37568|6|Mentioned|Fig.5|||||||||
6631|Fickling Group|38584|4|Described|p17|||||||||
6631|Fickling Group|39445|6|Mentioned|p36|||See also p39 & Table 2. Correlated with McArthur, McNamara & Mt Isa Group.||||||02-FEB-22
6631|Fickling Group|39497|6|Mentioned|Fig.4|||||||||
6631|Fickling Group|39685|6|Mentioned|Fig.1|||||||||
6631|Fickling Group|39925|6|Mentioned|p333|||||||||
6631|Fickling Group|40840|6|Mentioned|Map legend|||||||||
6631|Fickling Group|41319|6|Mentioned|Fig.1|||||||||
6631|Fickling Group|41406|6|Mentioned|Map legend|Mesoproterozoic||||||||
6631|Fickling Group|41721|6|Mentioned|p28|||Includes detailed descriptions of components Fish River Formation, Walford Dolomite, Mount Les Siltstone and Doomadgee Formation.||||||01-AUG-07
6631|Fickling Group|41722|6|Mentioned|Map legend|||||||||
6631|Fickling Group|42385|5|Briefly described|Fig.4 p7|||||||||02-FEB-22
6631|Fickling Group|42386|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
6631|Fickling Group|42638|6|Mentioned|Map legend|||Appears on Regional Setting map.|||||Dolostone, dolomitic siltstone, sandstone, shale.|07-NOV-11
6631|Fickling Group|42639|5|Briefly described|Fig.4 P7|||||||||
6631|Fickling Group|43010|5|Briefly described|Fig.6||Mesoproterozoic|Of "Mid Proterozoic" age.||||||18-SEP-06
6631|Fickling Group|43235|6|Mentioned|p8|||Proterozoic||||||
6631|Fickling Group|43486|5|Briefly described|21|||||||||
6631|Fickling Group|43615|6|Mentioned|p13|||||||||
6631|Fickling Group|45162|6|Mentioned|p147|||||||||
6631|Fickling Group|45166|5|Briefly described|p27|||||||||
6631|Fickling Group|46804|6|Mentioned|p154|||||||||
6631|Fickling Group|49001|2|Defined|p13|Carpentarian|Carpentarian|||||||
6631|Fickling Group|50225|5|Briefly described|p406 Fig. 10, p407|Paleoproterozoic|Paleoproterozoic|Geological Province: Calvert Superbasin.||||||07-FEB-11
6631|Fickling Group|60558|5|Briefly described|p3, p5 Fig. 4|||Includes; Fish River and Doomadgee Formations, Mount Les Siltstone and Walford Dolomite.||||||29-JUN-09
6631|Fickling Group|61736|5|Briefly described|p674|Paleoproterozoic|Paleoproterozoic|Age: 1640+/-7Ma (the Walford deposit).||||||
6631|Fickling Group|62473|5|Briefly described|p75||Paleoproterozoic|Age: ca. 1640Ma. Contains the Walford deposit.||||||17-JUN-09
6631|Fickling Group|62535|5|Briefly described|p674|||Hosts the Walford Pb-Zn-Ag deposit.|1640 +/- 7 Ma.|||||
6631|Fickling Group|62659|5|Briefly described|Map Legend|Calymmian|Statherian|||||||
6631|Fickling Group|63115|6|Mentioned|p1280-1281. ||||||Includes Mount Les Siltstone.|||
6631|Fickling Group|64575|6|Mentioned|p657|||Geological Province: Murphy Inlier.||||||
6631|Fickling Group|64724|5|Briefly described|p45 Fig.5, p46|Proterozoic|Proterozoic|South Nicholson Basin unit deposited as part of sedimentation in the Isa Superbasin (1660-1590 Ma)||||||
6631|Fickling Group|64815|6|Mentioned|p3|||||||||
6631|Fickling Group|65228|6|Mentioned|p9|||||||||
6631|Fickling Group|65337|5|Briefly described|p6 Fig.3, p30, p36.|Mesoproterozoic|Paleoproterozoic|Carbonate sediments; probably contiguous with McNamara Group to the south in the Carrara Range.|c.1670-1590 Ma.||Includes Walford Dolomite.|||
6631|Fickling Group|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map; p107||||||Includes Doom Supersequence, Doomagee Formation, Fish River Formation, Mount Les Siltstone, Walford Dolomite|||
6631|Fickling Group|68146|5|Briefly described|p2, p196, p198||||||Doomadgee Formation.|Is overlain unconformably by South Nicholson Group.||
6631|Fickling Group|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province.||||||
6631|Fickling Group|68575|6|Mentioned|p11|||||`|Doomadgee Formation.|Overlies Peters Creek Volcanics.||
6631|Fickling Group|69417|6|Mentioned|p2:5-6|Statherian|Statherian|South Nicholson/Lawn Hill Basin.||||||12-JUL-16
6631|Fickling Group|69423|6|Mentioned|p8:4 Fig.8.7|Paleoproterozoic|Paleoproterozoic|Lawn Hill Platform.||||||12-JUL-16
6631|Fickling Group|69433|4|Described|p18:1-4, 10|Statherian|Statherian|Formerly the Fickling beds (Carter, 1959). Northern succession, Lawn Hill Platform. Hosts the large low-grade pyrite-rich Walford Creek and Bluebush stratiform Pb-Zn deposits in Qld.|||Fish River, Doomadgee Formations; Walford Dolostone; Mount Les Siltstone.|Unconformably overlies Peters Creek Volcanics. Correlated with McArthur and McNamara Groups.|A succession of sandstone, dolostone, siltstone and shale.|12-JUL-16
6631|Fickling Group|69434|5|Briefly described|p19:1, 6|||Lawn Hill Platform. Mapping by Smith and Roberts (1963) included rocks later distinguished as a separate unit (the Caulfield beds) by Rawlings et al. (2008).||||Is overlain disconformably or unconformably by Accident Subgroup (South Nicholson Group).||12-JUL-16
6631|Fickling Group|69591|5|Briefly described|p29, p55|Paleoproterozoic|Paleoproterozoic|Camooweal-Murphy Domain, Mount Isa Province.|||Doomadgee, Fish River Formations; Mount Les Siltstone; Walford Dolomite.|||
6631|Fickling Group|69673|5|Briefly described|p3 fig 2, p51, p52 fig 42|Mesoproterozoic|Paleoproterozoic||||Includes Fish River Formation|Unconformably overlies Wire Creek Sandstone, Peters Creek Volcanics, Correlated with McNamara Group, McArthur Group|Sandstone, dolostone, siltstone and shale.|
6631|Fickling Group|70849|5|Briefly described|Map legend.|Statherian|Statherian|Lawn Hill Platform.|||Fish River, Doomadgee Formations; Walford Dolostone; Mount Les Siltstone.|Unconformably overlies Peters Creek Volcanics (Tawallah Group equivalent). Is overlain unconformably by Constance Sandstone (South Nicholson Group).||
6631|Fickling Group|70897|5|Briefly described|p39, p45|||Mixed carbonate-clastic lithofacies.||||All units are overlain with an angular unconformity by South Nicholson Group.||
6631|Fickling Group|71369|5|Briefly described|p4, p10-11|||Underwent moderate folding but little metamorphism during the 1585-1500 Ma Mount Isa Orogeny. Basement for South Nicholson Group.|||Doomadgee Formation.|Is overlain unconformably by the Hedleys Sandstone and the South Nicholson Group.||20-FEB-18
6631|Fickling Group|71606|5|Briefly described|p137|Statherian|Statherian|South Nicholson Basin.||||Overlain unconformably by South Nicholson Group. Underlain unconformably by Peters Creek Volcanics. Equivalent to McNamara Group.||
6631|Fickling Group|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Lawn Hill Platform.|||||Dolostone, dolomitic siltstone, sandstone, shale (+/- carbonaceous).|
6631|Fickling Group|72526|5|Briefly described|p1, p4, p6, p8, p20, 27, 33, 40, 46, 85|Statherian|Statherian|Shown as being located in the central and west of the South Nicholson Basin, p8. Said to be of theLawn Hill Platform, Mount Isa Province, p20 etc. Depositional ages from Page and Sweet, 1998; Page et al., 2000; Carson et al., 2011b.|c. 1649 Ma to 1613 Ma||Includes Doomadgee Formation, Mount Les Siltstone, Walford Dolomite, Fish River Formation.|Shown as partially overlying Weberra Granite and Nicholson Granite Complex.||
6631|Fickling Group|72527|6|Mentioned|p5, p10, p161, p185.|Statherian|Statherian||1613 +/- 5 Ma||Includes Doomadgee Formation|||
6631|Fickling Group|72912|4|Described|p5 Fig.3, p13, p32, p33, p35, p45-46.|Statherian|Statherian|Northwestern Mount Isa Province. Known to be potential sources of hydrocarbons. See also p35 Fig.13.|||Doomadgee Formation, Mount Les Siltstone, Walford Dolomite and Fish River Formation.|Unconformably underlies South Nicholson Group. Laterally equivalent to McNamara Group.|Includes shallow marine carbonates, dolomitic siltstone, organic rich siltstone and shales, and dolostone.|15-MAR-21
6631|Fickling Group|72913|5|Briefly described|p7, p9 Tb.1.|Paleoproterozoic|Paleoproterozoic|Shown as being in the west of the Isa Superbasin.|||Includes Doomadgee Formation, Mount Les Siltstone, Walford Dolostone/Dolomite and Fish River Formation||Includes dolomitic siltstone and dolostone.|
6631|Fickling Group|72919|6|Mentioned|p3, p98|Paleoproterozoic|Paleoproterozoic|Isa Superbasin.||||||
6631|Fickling Group|72967|6|Mentioned|p2, p6|Paleoproterozoic|Paleoproterozoic|Lawn Hill Platform.|||Doomadgee Formation, Mount Les Siltstone, Walford Dolostone|||
6631|Fickling Group|73042|6|Mentioned|p1, p3-4, p6, p14, p16-17|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin region, Isa Superbasin.|||Doomadgee Formation, Fish River Formation, Mount Les Siltstone, Walford Dolomite.|||
6639|Fiery Creek Volcanics|22438|3|Fully described|p537, Fig.3 p537|Paleoproterozoic|Paleoproterozoic|Bimodal volcanics (intercalated with sedimentary rocks of Bigie Formation). See also Fig.10a p546.||||||23-DEC-08
6639|Fiery Creek Volcanics|22457|4|Described|P29, Fig29, Fig30|||Equivalent to part of Peters Creek Volcanics?||||||
6639|Fiery Creek Volcanics|22585|5|Briefly described|Fig1 P736, Fig3|||||||||
6639|Fiery Creek Volcanics|22644|5|Briefly described|5 fig 2|||Geol. province: Mount Isa Basin. Underlain by Quilalar Formation. Volcanics as 'V' in text.||||||18-JAN-07
6639|Fiery Creek Volcanics|22665|5|Briefly described|P219, Table1||Statherian|Age of unit is 1709+/-3 Ma.||||||18-JAN-07
6639|Fiery Creek Volcanics|22680|6|Mentioned|83|||||||||
6639|Fiery Creek Volcanics|23031|5|Briefly described|21|Paleoproterozoic|Paleoproterozoic|Geol. province: Mount Isa Fold Belt. Underlain by Bigie Formation, Myally Subgroup, Quilalar Formation.||||||07-NOV-08
6639|Fiery Creek Volcanics|23205|6|Mentioned|p44|||Of Mount Isa Inlier.||||||23-DEC-08
6639|Fiery Creek Volcanics|23363|5|Briefly described|352 Tab.3|Statherian|Statherian|Age: ~1709+/-3Ma.||||||18-JAN-07
6639|Fiery Creek Volcanics|23393|5|Briefly described|p19, p16 Fig. 4|Paleoproterozoic|Paleoproterozoic|Age: 1709+/-3Ma.  Geological Province: Lawn Hill Sub-province.  See also p17 Fig.5.||||||07-NOV-08
6639|Fiery Creek Volcanics|23395|6|Mentioned|p385|||||||||
6639|Fiery Creek Volcanics|23396|4|Described|p418|Statherian|Statherian|||||||
6639|Fiery Creek Volcanics|23397|5|Briefly described|p463|||||||||
6639|Fiery Creek Volcanics|23398|5|Briefly described|p433 Fig.2|Statherian|Statherian|Age: 1709+/-3Ma.||||||18-JAN-07
6639|Fiery Creek Volcanics|23399|6|Mentioned|p489|||||||||
6639|Fiery Creek Volcanics|23406|5|Briefly described|p603, p607 Fig. 8|||Stated to be of a basal "rift" package. Geological province: Lawn Hill Platform.||||||16-JUN-09
6639|Fiery Creek Volcanics|23408|5|Briefly described|p511, p513 Fig. 2|||Unconformable below the McNamara Group. This unit was added by Hutton et al (1981) to the McNamara and Mount Isa Groups.||||||15-JUN-09
6639|Fiery Creek Volcanics|23466|5|Briefly described|p267|Statherian|Statherian|Age:1708+/-2Ma.||||||18-JAN-07
6639|Fiery Creek Volcanics|23518|4|Described|p9 Fig. 3, p11|Proterozoic|Proterozoic|Geological Province: Western Fold Belt.||||||
6639|Fiery Creek Volcanics|23767|5|Briefly described|p1954 Fig. 1a|||Geological Province: Mount Isa Superbasin. See also p1955.||||||
6639|Fiery Creek Volcanics|23965|5|Briefly described|p1297|Paleoproterozoic|Paleoproterozoic|Age: 1709 +/- 3Ma. Geological Province: Mount Isa Inlier.||||||07-NOV-08
6639|Fiery Creek Volcanics|24197|5|Briefly described|p28, p95 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Of the Fiery Supersuite. Age: 1710Ma. Geological Province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
6639|Fiery Creek Volcanics|24307|5|Briefly described|p978|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Block||||||07-NOV-08
6639|Fiery Creek Volcanics|24308|5|Briefly described|p987 Fig. 2|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
6639|Fiery Creek Volcanics|24309|5|Briefly described|p1017|||||||||
6639|Fiery Creek Volcanics|24419|5|Briefly described|p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Of the Fiery Suite.  Geological Province: Western Fold Belt, Lawn Hill Subprovince and Leichardt River Subprovince (Mount Isa Orogen).||||||07-NOV-08
6639|Fiery Creek Volcanics|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Age: 1709 Ma.||||||
6639|Fiery Creek Volcanics|36548|6|Mentioned|p513|||||||||
6639|Fiery Creek Volcanics|37459|2|Defined|p426|Mesoproterozoic|Mesoproterozoic|Age is more specifically Carpentarian.||||||23-DEC-08
6639|Fiery Creek Volcanics|37462|4|Described|Table4.VII|||See also p244.||||||18-SEP-06
6639|Fiery Creek Volcanics|37565|6|Mentioned|p11|||||||||
6639|Fiery Creek Volcanics|37568|6|Mentioned|p85|||||||||
6639|Fiery Creek Volcanics|38232|6|Mentioned|p82|||||||||
6639|Fiery Creek Volcanics|38237|5|Briefly described|p126|||||||||
6639|Fiery Creek Volcanics|38276|6|Mentioned|Fig.1|||||||||
6639|Fiery Creek Volcanics|38310|6|Mentioned|p237|||||||||
6639|Fiery Creek Volcanics|38348|6|Mentioned|p6|||||||||
6639|Fiery Creek Volcanics|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
6639|Fiery Creek Volcanics|38560|6|Mentioned|p113|||||||||
6639|Fiery Creek Volcanics|38584|6|Mentioned|p22|||||||||
6639|Fiery Creek Volcanics|38833|6|Mentioned|p161|||||||||
6639|Fiery Creek Volcanics|38835|6|Mentioned|p164|||||||||
6639|Fiery Creek Volcanics|38919|6|Mentioned|p497|||||||||
6639|Fiery Creek Volcanics|39445|5|Briefly described|p40|||See also p36 and Table 2.||||||18-JAN-07
6639|Fiery Creek Volcanics|39497|6|Mentioned|p8|||||||||
6639|Fiery Creek Volcanics|39556|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||
6639|Fiery Creek Volcanics|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||15-JUN-06
6639|Fiery Creek Volcanics|39622|6|Mentioned|Fig.2|||||||||
6639|Fiery Creek Volcanics|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
6639|Fiery Creek Volcanics|39925|6|Mentioned|p329|||||||||
6639|Fiery Creek Volcanics|39934|6|Mentioned|Fig.3|||||||||
6639|Fiery Creek Volcanics|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
6639|Fiery Creek Volcanics|40105|6|Mentioned|p310|||||||||
6639|Fiery Creek Volcanics|40221|3|Fully described|p12|||||||||
6639|Fiery Creek Volcanics|40691|5|Briefly described|p11|||||||||
6639|Fiery Creek Volcanics|40811|6|Mentioned|p318|||||||||
6639|Fiery Creek Volcanics|40840|6|Mentioned|Map legend|||||||||
6639|Fiery Creek Volcanics|40984|6|Mentioned|p400|||||||||
6639|Fiery Creek Volcanics|41307|4|Described|p13|||||||||
6639|Fiery Creek Volcanics|41978|6|Mentioned|p502|||||||||
6639|Fiery Creek Volcanics|41979|6|Mentioned|p522|||||||||
6639|Fiery Creek Volcanics|42565|5|Briefly described|Table 1 P5, P4|||||||||
6639|Fiery Creek Volcanics|43595|5|Briefly described|p440-1|||U-Pb Zircon age: 1678+/-3 Ma||||||
6639|Fiery Creek Volcanics|43616|6|Mentioned|p4|||Age 1680 Ma.||||||23-DEC-08
6639|Fiery Creek Volcanics|45166|5|Briefly described|p26|||||||||
6639|Fiery Creek Volcanics|46960|6|Mentioned|p215|||||||||
6639|Fiery Creek Volcanics|47083|4|Described|p11||Proterozoic|Comagmatic with Weberra Volcanics. Unconformably overlain by Surprise Crk Fm, Mt Isa and McNamara Groups. Unconformably overlies Haslingden Gp and Quilalar Fm. Max thick: 250 m.||||||18-SEP-06
6639|Fiery Creek Volcanics|49041|5|Briefly described|Table 1|||||||||
6639|Fiery Creek Volcanics|50224|6|Mentioned|p380 Fig. 6|||||||||07-FEB-11
6639|Fiery Creek Volcanics|50536|5|Briefly described|p1.4, 7.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Fiery Suite. Age: 1709 +/-3Ma (Shrimp).||||||07-NOV-08
6639|Fiery Creek Volcanics|50550|5|Briefly described|p1139 Fig.2||Statherian|Age: 1708 Ma. Conformably overlies Bigie Formation. Overlain by Surprise Creek Formation at a syn-rift unconformity. Geological Province: Western Fold Belt.||||||24-JAN-22
6639|Fiery Creek Volcanics|50624|5|Briefly described|p234 Fig.2||Paleoproterozoic|||||||07-NOV-08
6639|Fiery Creek Volcanics|60558|5|Briefly described|p4 Fig. 3, p12|Paleoproterozoic|Paleoproterozoic|Geological Province: Western Fold Belt.||||||03-JUN-09
6639|Fiery Creek Volcanics|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: ~1700Ma. Geological Province: western Mount Isa Block.||||||07-NOV-08
6639|Fiery Creek Volcanics|61924|5|Briefly described|p44|||||||||
6639|Fiery Creek Volcanics|61929|5|Briefly described|p128 Fig. 2|Paleoproterozoic|Paleoproterozoic|Age: 1708+/-2Ma. ||||||07-NOV-08
6639|Fiery Creek Volcanics|61936|5|Briefly described|p194 Fig. 6|Paleoproterozoic|Paleoproterozoic|Intercalated with the Bigie Formation. Age: 1709+/-3Ma. Geological Province: Calvert Superbasin, Western Fold Belt, Mount Isa Inlier. ||||||07-NOV-08
6639|Fiery Creek Volcanics|62535|5|Briefly described|p672|Statherian|Statherian||1709 +/- 3 Ma.|||||
6639|Fiery Creek Volcanics|62988|5|Briefly described|p34|Paleoproterozoic|Paleoproterozoic|Age: 1709+/-3Ma. (Page and Sweet 1998). Geological Province: Calvert Superbasin (Mount Isa Inlier).||||||07-NOV-08
6639|Fiery Creek Volcanics|63023|5|Briefly described|p1024 Fig. 1, p1025 Fig. 2|Paleoproterozoic|Paleoproterozoic|Age: ca 1710Ma. Geological Province: Calvert Superbasin. See also p1034.||||||07-NOV-08
6639|Fiery Creek Volcanics|63109|6|Mentioned|p1108, p1108 Fig. 3, p1111|||Overlain by Surprise Creek Formation, underlain by Bigie Formation. Consists of mafic volcanics rocks. Geological Province: Leichhardt and Calvert Superbasin.||||||
6639|Fiery Creek Volcanics|63110|6|Mentioned|p1141, p1141 Fig. 17|Statherian|Statherian|Geological Province: Calvert Superbasin.||||||11-JUN-08
6639|Fiery Creek Volcanics|63111|5|Briefly described|p1163 Fig. 3, p1164 Tb. 1|Statherian|Statherian|Overlain by Surprise Creek Formation, underlain by Bigie Formation. Age: ~1709Ma (U/Pb zircon ages). Geological Province: Calvert Superbasin. Consists of volcanic rocks.||||||07-FEB-11
6639|Fiery Creek Volcanics|63114|5|Briefly described|p1253 Fig.2. |||Calvert superbasin.||Of the Big supersequence||Overlies Bigie Formation. Is overlain by Surprise Creek Formation.||
6639|Fiery Creek Volcanics|63115|6|Mentioned|1279 Fig.4, p1281, p1290, |||Calvert superbasin. High-permeability aquifer.||||||
6639|Fiery Creek Volcanics|63116|6|Mentioned|p1297 Fig.2,p1299 Tb.1, |||Calvert superbasin. Material properties detailed.||||||
6639|Fiery Creek Volcanics|63866|5|Briefly described|p57-p58, p61|Statherian|Statherian|Calvert Superbasin.|1709 +/- 3 Ma (Page and Sweet, 1998)|||(Possibly) coeval with the Bigie Formation. Possibly equivalent to the Deighton Quartzite.||
6639|Fiery Creek Volcanics|64250|6|Mentioned|p19, p25 fig 10, p11 fig 3, p21, p24|||Western Fold Belt, Mount Isa Inlier. Co-magmatic with Weberra Granite.|1709 +/- 3 Ma||||Bimodal volcanics.|
6639|Fiery Creek Volcanics|64575|6|Mentioned|p656, p664|||||||||
6639|Fiery Creek Volcanics|64725|6|Mentioned|p58 Fig.2. |||Mount Isa Inlier.||||||
6639|Fiery Creek Volcanics|64726|6|Mentioned|p83 Fig.2.|||||||||
6639|Fiery Creek Volcanics|64744|6|Mentioned|p353 Fig.4, p354. |Statherian|Statherian|Mount Isa Basin. Bimodal volcanics.|1709 +/- 3 Ma.|||||
6639|Fiery Creek Volcanics|64748|6|Mentioned|p276 Fig. 9|Paleoproterozoic|Paleoproterozoic|Palaeomag results shown on polar wander path||||||
6639|Fiery Creek Volcanics|64834|5|Briefly described|p13 Fig.2|||Calvert Superbasin. Western Succession of Mount Isa Basin. Shown as Fiery Ck. Volcs.|||||Volcanics.|
6639|Fiery Creek Volcanics|65228|5|Briefly described|Figs.04, 10.|Statherian|Statherian|Mount Isa area. Part of the Big Supersequence.|1709 +/- 3 Ma (Page et al. 2000).|||||
6639|Fiery Creek Volcanics|65337|6|Mentioned|p5. |||Calvert Superbasin. Correlative of Carrara Range Group.||||||
6639|Fiery Creek Volcanics|65396|5|Briefly described|p16, p82, p175, p187, p190, p193|Statherian|Statherian|See also p195-197, p241. Calvert Superbasin. Cover Sequence 2. Lawn Hill Platform, Leichhardt River Fault Trough, Kalkadoon-Leichhardt Belt. Co-magmatic with Weberra Granite. Formations with detrital zircons from this unit are listed.|1709 +/- 3 Ma|||Overlies Bigie Formation.|Felsic and mafic volcanics.|
6639|Fiery Creek Volcanics|65887|5|Briefly described|p52|Statherian|Statherian|Mount Isa Western Succession. Metatholeiites. ~1710 Ma.||||||09-JUN-15
6639|Fiery Creek Volcanics|66529|6|Mentioned|p3|||Calvert Superbasin.|~1709 Ma|||||
6639|Fiery Creek Volcanics|66824|6|Mentioned|p148|||||||Overlies Bigie Formation. Is overlain unconformably by Surprise Creek Formation. With Bigie Formation, equivalent to Carter's Bore Rhyolite.||
6639|Fiery Creek Volcanics|67026|6|Mentioned|p336 Fig.3.|Statherian|Statherian||1709 +/- 2 Ma (Page et al. 2000).|||||24-APR-12
6639|Fiery Creek Volcanics|67323|4|Described|p9-11, p13, p24-25, p33, p39, p107|Paleoproterozoic|Paleoproterozoic|See also GIS attrib tbl, Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Bimodal volcanism associated with extension of the Calvert Superbasin. Mount Oxide Domain, Mount Isa Inlier. Age significantly younger than Peters Creek Volcanics. Shown as two parts, mafic ~10 my older than felsic, on both Time-Space Plots.|1709 +/- 3 Ma (felsic: Page & Sweet 1998).|Of Big Supersequence.||Coeval with Weberra Granite. Unconformably overlain by Surprise Creek Formation. Overlies Bigie Formation.|Reddish brown, grey and black vesicular volcanics, grey porphyritic volcanics, purple to brown labile and micaceous sandstone, tuffaceous conglomerate; minor felsic flows and breccia.|
6639|Fiery Creek Volcanics|68021|5|Briefly described|p135 fig 4, p136, 138|Statherian|Statherian|Part of Big Supersequence, Calvert Superbasin, Western Succession.|1710 Ma|||Overlies Bigie Formation?, Quilalar Formation, overlain by Surprise Creek Formation.|?Bimodal volcanics.|
6639|Fiery Creek Volcanics|68146|5|Briefly described|p6, p188-193|||Informal name. Mount isa Region. Sample did not yield results; zircons are interpreted as either xenocrysts and/or geological sampling contamination.||||Is overlain by Surprise Creek Formation or Torpedo Creek Quartzite.|(Weathered) brick-red rhyolite or rhyodacite, containing a very fine-grained matrix with prominent glassy quartz "eyes"; local flow layering.|
6639|Fiery Creek Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province. This unit is mapped with the Bigie Formation under the symbol, -Pf.||||||
6639|Fiery Creek Volcanics|68575|6|Mentioned|p40|||||||Upper part may be equivalent to the Bularnu Formation.||
6639|Fiery Creek Volcanics|68732|5|Briefly described|p165 Fig.3|Statherian|Statherian|Of the Big Supersequence. Igneous crystallisation age.|1709 +/- 3 Ma|||||
6639|Fiery Creek Volcanics|69056|5|Briefly described|p2, p54|||Mount Isa Western Succession; Calvert Superbasin. Mapped as one unit with Bigie Formation Volcanics.|||||Local bimodal volcanism.|
6639|Fiery Creek Volcanics|69222|5|Briefly described|p221, p222 Fig.2|Statherian|Statherian|Western Fold Belt. Associated with the Mount Isa Rift Event.|1708 +/- 2 Ma (Page and Sweet, 1998).|||Overlies Quilalar Formation, overlain by Carters Bore Rhyolite|Felsic volcanic rocks.|
6639|Fiery Creek Volcanics|69370|6|Mentioned|p307 Fig.2|Statherian|Statherian|Western Fold Belt, Mount Isa Block.||||Intertongues with Bigie Formation.||25-JAN-19
6639|Fiery Creek Volcanics|69591|5|Briefly described|p29, p37-39, p56, p106|Paleoproterozoic|Paleoproterozoic|Jackson, Scott and Rawlings (2000). Mount Oxide, Leichhardt River Domains, Calvert Superbasin. Part of the Big Supersequence. Bimodal felsic and highly altered mafic volcanics. Coeval with the ~1710 Ma Weberra Granite. May be the source of ~1712 Ma detrital zircons in Roxmere Quartzite. Jackson et al. (2005) dated this unit at 1701 +/- 23 Ma.|1709 +/- 3 Ma (Page and Sweet, 1998).|||Correlated with basal Deighton Quartzite.|Reddish-brown, grey and black vesicular volcanics, grey porphyritic volcanics, purple to brown labile and micaceous sandstone, tuffaceous conglomerate; minor felsic flows and breccia.|
6639|Fiery Creek Volcanics|70282|5|Briefly described|p544 table 1|||Cover sequence 3, Mount Isa.|1710-1709 Ma|||Overlies Bigie Formation|Bimodal volcanics.|13-FEB-18
6639|Fiery Creek Volcanics|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic||||||Reddish-brown, grey and black vesicular metabasalt and trachybasalt, locally porphyritic; purple to brown labile and micaceous sandstone, tuffaceous conglomerate; minor felsic flows and breccia.|
6639|Fiery Creek Volcanics|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic||||||Reddish-brown, grey and black vesicular metabasalt and trachybasalt, locally porphyritic; purple to brown labile and micaceous sandstone, tuffaceous conglomerate; minor felsic flows and breccia.|
6639|Fiery Creek Volcanics|70858|6|Mentioned|p31|Paleoproterozoic|Paleoproterozoic|Calvert Superbasin.|1709 +/- 3 Ma.|||||
6639|Fiery Creek Volcanics|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1709+/-3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Rhyodacite.|
6639|Fiery Creek Volcanics|71799|5|Briefly described|p150 fig 2, p153 tbl 1|Statherian|Statherian|Lawn Hill. Age is derived from SHRIMP U-Pb magmatic ages (not provided) derived from Page et al, 2000 and from Page, 1983. Geochemistry is discussed. See also p154, p156, p157 fig 5, p158.|1710-1705 Ma|||Overlies the Bigie Formation. Overlain by the Prize Supersequence.|Basalt, dolerite, gabbro or amphibolite.|
6639|Fiery Creek Volcanics|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown with Bigie Formation, as located in the Lawn Hill Platform of the Mount Isa Province and the east part of the South Nicholson Basin. Unclear whether this unit or Bigie Fm was dated. Age given as U-Pb zircon igneous crystallisation age.|1709 +/-3 Ma|||Shown as overlying Carrara Range Group and shown as unconformably underlying Surprise Creek Formation.||
6639|Fiery Creek Volcanics|72889|6|Mentioned|p6 Fig.i.|||||||||
6639|Fiery Creek Volcanics|72912|5|Briefly described|p5 Fig.3, p13.|Statherian|Statherian|Of Calvert Superbasin. Shown with Bigie Formation. Lateral equivalents? Located in the  Leichhardt River Fault Trough, the Lawn Hill Platform of the Mount Isa Province, and the East part of the South Nicholson Basin. U-Pb zircon igneous crystallisation age (Ma) shown.|1709 +/- 3 Ma|||Shown as unconformably overlying Quilalar Formation, Carrara Range Group and unconformably underlies Surprise Creek Formation.|Bimodal volcanics.|
6639|Fiery Creek Volcanics|73042|6|Mentioned|p4|Statherian|Statherian|Written as Fiery Creek Vol/Bigie Fm on chronostratigraphic diagram (Fig.1.2). South Nicholson Basin region and Mount Isa Province, Calvert Superbasin. Geochronology is a U-Pb zircon igneous crystallisation age (although it is unclear whether this age is from the Fiery Creek Volcanics or Bigie Formation(?), or if these two units can be distinguished from one another).|1709 +/- 3 Ma (see comments and Fig.1.2)|||Unconformably overlain(?) by Surprise Creek Formation. Equivalent to Bigie Formation(?).||
6639|Fiery Creek Volcanics|73137|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|||||||
6639|Fiery Creek Volcanics|73144|6|Mentioned|p9-10|||Calvert Superbasin. Part of the Big Supersequence.||||Partly interbedded with Bigie Formation.|Includes banded rhyolite flows.|
6639|Fiery Creek Volcanics|73412|6|Mentioned|p20|||Western Succession of the Mount Isa Inlier. Contains potassic alteration assemblages, interpreted as regional fluid flow associated with Zn-Pb-Ag metallogenesis.||||||
6639|Fiery Creek Volcanics|73525|5|Briefly described|p4, p19 Fig.13|Statherian|Statherian|Mount Oxide-(Ardmore-May Downs) Domain.|1709+/-3 Ma crystallisation age||||Mafic extrusives with clastics, and felsic extrusives.|
6661|Finke Group|22566|6|Mentioned|p79|||Geological province - Warburton Basin||||||
6661|Finke Group|22760|5|Briefly described|p340|Late Devonian|Late Devonian|||||||
6661|Finke Group|22762|5|Briefly described|p376|||The distal equivalent of the Pertnjara Group.||||||
6661|Finke Group|22763|6|Mentioned|Fig 3 on p389|||||||||
6661|Finke Group|22824|6|Mentioned|p530|||||||||
6661|Finke Group|22825|6|Mentioned|Fig 1 on p542|||||||||
6661|Finke Group|22826|6|Mentioned|p576|||||||||
6661|Finke Group|23858|5|Briefly described|p916|||Geological Province: Amadeus Basin. Max. thickness: >1000 m.||||||
6661|Finke Group|24301|6|Mentioned|p22|||||||||
6661|Finke Group|24302|5|Briefly described|Map Legend|Devonian|Devonian|Includes the Horseshoe Bend shale. Geological Province: Amadeus Basin. Mistakenly shown as Ordovician, but map symbol and Explanatory Notes indicate Devonian age.||||||25-OCT-06
6661|Finke Group|29442|6|Mentioned|p103|||||||||
6661|Finke Group|30544|6|Mentioned|p46|||Devonian age||||||
6661|Finke Group|31566|6|Mentioned|p244|||Devonian||||||
6661|Finke Group|31567|4|Described|p273|||See also p274-293. Refers Wells et al. (1964, 1966, 1967, 1970).||||||18-SEP-06
6661|Finke Group|32640|6|Mentioned|p241|||||||||
6661|Finke Group|33832|6|Mentioned|p8|||Refers Wells et al. (1970) and Youngs (1973).||||||18-SEP-06
6661|Finke Group|33964|6|Mentioned|p5|||Correlation. Refers Wells et al.(1966).||||||
6661|Finke Group|33971|6|Mentioned|p46|||Strat. table.||||||
6661|Finke Group|34111|5|Briefly described|Table 2|||Devonian - Carboniferous. See also p16.||||||18-SEP-06
6661|Finke Group|34580|4|Described|Table 1|||Devonian - Carboniferous||||||
6661|Finke Group|35102|6|Mentioned|p4|||||||||
6661|Finke Group|36473|6|Mentioned|Map legend|Carboniferous|Devonian|Between Carboniferous and Devonian||||||
6661|Finke Group|36751|6|Mentioned|p490|||||||||
6661|Finke Group|39565|6|Mentioned|p32|||||||||
6661|Finke Group|40642|6|Mentioned|p163|||||||||
6661|Finke Group|40910|6|Mentioned|p13|||||||||
6661|Finke Group|40911|6|Mentioned|Map legend|Devonian|Devonian|Prob. Devonian||||||
6661|Finke Group|40926|6|Mentioned|p12|||||||||
6661|Finke Group|41018|6|Mentioned|Fig.1|||||||||
6661|Finke Group|41125|6|Mentioned|Fig.24|||||||||
6661|Finke Group|41708|6|Mentioned|Fig.1|||||||||
6661|Finke Group|42296|6|Mentioned|p44|||||||||
6661|Finke Group|42504|5|Briefly described|p80|||||||||
6661|Finke Group|42699|5|Briefly described|map legend|Devonian||||||||
6661|Finke Group|42940|5|Briefly described|Plate 2|Devonian|Devonian|Sandstone, shale, siltstone, conglomerate.  Age: 410-360Ma. Geological province: Amadeus Basin.||||||23-JAN-08
6661|Finke Group|43035|4|Described|p24|||||||||
6661|Finke Group|43052|5|Briefly described|Table 2.1|||||||||
6661|Finke Group|44133|4|Described|p43, 44|Carboniferous?|Late Devonian|Overlies: Mereenie Sandstone. Includes: Polly Conglomerate, Langra Formation, Horseshoe Bend Shale. Lateral equivalent to Pertnjara Group.||||||
6661|Finke Group|44323|14|Not recorded|map legend|Carboniferous|Devonian|SG/53-6. Devon-Carbon.||||||
6661|Finke Group|44335|4|Described|p.11|Carboniferous|Devonian|Table 2. p.10, Dev-Carb.||||||
6661|Finke Group|44336|14|Not recorded|map legend|Carboniferous|Devonian|SG/53-3. Dev-Carbon.||||||
6661|Finke Group|44342|4|Described|p.7, Table 2|Carboniferous|Devonian|SG/53-5. Dev-Carbon.||||||
6661|Finke Group|44343|14|Not recorded|map legend|Carboniferous|Devonian|Devonian-Carbon.||||||
6661|Finke Group|44393|4|Described|p.3,7,8,Tb.1|Carboniferous|Devonian|Correlated with Pertnjara Group. Dev-Carb.||||||
6661|Finke Group|44394|14|Not recorded|map legend|||Devonian to Carboniferous.||||||
6661|Finke Group|44433|14|Not recorded|map legend|||Devonian to Carboniferous.||||||
6661|Finke Group|45041|4|Described|p103|||See also p104-111. Devonian||||||18-SEP-06
6661|Finke Group|45097|6|Mentioned|p28|||Approx. same age as Pertnjara Group.||||||
6661|Finke Group|47050|5|Briefly described|p240|||||||||
6661|Finke Group|48865|2|Defined|p.28-29||Paleozoic|On many pages. p.3-5,21,27,34,35,36,40,45,Fig.14,47-51,53,Pl.10,11. Includes Idracowra Sandstone, Horseshoe Bend Shale, Langra Fm, Polly Cong. (G53-5,6).||||||07-NOV-08
6661|Finke Group|48880|14|Not recorded|p.20|Carboniferous|Devonian|(map). Devn-Carb.||||||
6661|Finke Group|48890|4|Described|p.50-52|Carboniferous|Devonian|See also Tb.1, Tb.3, Fig.4, Pl.16. Dev - Carb.||||||
6661|Finke Group|48963|6|Mentioned|Plate 5|||||||||
6661|Finke Group|50372|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Amadeus Basin. Includes: Polly Conglomerate, Langra Formation, Horseshoe Bend Shale, Idracowra Sandstone.||||||
6661|Finke Group|60678|5|Briefly described|Map legend|Devonian|Devonian|Fine to medium quartz sandstone, minor siltstone and shale, pebble and boulder conglomerate.  Geological Province: Amadeus Basin.||||||11-JAN-05
6661|Finke Group|61154|5|Briefly described|p34|||Sedimentary succession. Onlaps the Musgrave basement. Geological Province: Amadeus Basin.||||||18-SEP-06
6661|Finke Group|62609|5|Briefly described|Map Legend|Carboniferous|Devonian|Sandstone, shale, siltstone, conglomerate. Underlies De Souza Sandstone.||||||14-AUG-06
6661|Finke Group|62620|5|Briefly described|Map Legend|Carboniferous|Devonian|Sandstone, shale, siltstone, conglomerate.||||||
6661|Finke Group|64334|5|Briefly described|p42|Devonian|Devonian|Deposition was synchronous with the main phase of the Alice Springs Orogeny.|||||Thick wedges of generally coarsening-upward non-marine clastic sediments.|
6661|Finke Group|64778|6|Mentioned|p13, 15-17, 19-21, 23, 32|Devonian|Devonian|Pedirka Basin. Thermal history summarised. Max. palaeotemperature analysis summary.|390-354 Ma.|||||
6661|Finke Group|64809|6|Mentioned|p3 |||Southern Amadeus Basin.||||||
6661|Finke Group|65232|5|Briefly described|p10 Fig 9.|||Combined age for Finke Group and Pertnjara Group shown as Late Devonian to Late Carboniferous||||||09-FEB-10
6661|Finke Group|65233|5|Briefly described|p13|Devonian|Devonian|Overlain by Horsebend Shale. Max. thickness: 400m. Coarse alluvial facies.||||||07-FEB-11
6661|Finke Group|65309|4|Described|pp13-14, p16, pp18-20.|Frasnian|Givetian|Southeast Amadeus Basin. Interfingers with Pertnjara Group. A typical locally-sourced, upward-fining basin-fill sequence resulting from minor uplift from the Alice Springs Orogeny.|||Includes Polly Conglomerate, Langra Formation, Horseshoe Bend Shale and Idracowra Sandstone.|Unconformably overlies basement.||
6661|Finke Group|66589|6|Mentioned|p180|Late Devonian|Late Devonian|Case studies cited; not visited in the field by the authors of this study.||||||
6661|Finke Group|69436|6|Mentioned|p21:20|||Amadeus Basin. Deposited during a single pulse of exhumation early in the 450-300 Ma Alice Springs Orogeny.||||||12-JUL-16
6661|Finke Group|69438|5|Briefly described|p23:2-4, 20, 38, 40-42|Late Devonian|Late Devonian|This author claims that the name Finke River Sandstone was first used by Chewings (1914) [who in fact used the names Finke River sandstones and Finke River sandstones formation]. The current name, Finke Group, applies to the Devonian succession underlying the Pedirka and Eromanga Basins but overlying basement rocks of the Musgrave Province or older successions of the Amadeus Basin. Southeast and south-central Amadeus Basin. Sediment supply was from the S and SW (Musgrave province) for the lowest three Formations; the upper unit was supplied from the N (Arunta Region). Unfossiliferous; age not well constrained.|||Polly Conglomerate, Langra Formation, Horseshoe Bend Shale, Idracowra Sandstone.|Correlative of, and interdigitates with, Pertnjara Group.||12-JUL-16
6661|Finke Group|69449|5|Briefly described|p34:2 Fig.34.2; 34:5-7|Devonian|Devonian|Eastern Amadeus Basin, with equivalents in the western Warburton Basin that are just over 1000m thick. Synorogenic deposition in response to largely compressional deformation during the Alice Springs Orogeny.|||Polly Conglomerate, Langra Formation, Horseshoe Bend Shale, Idracowra Sandstone.|Overlies Mereenie Sandstone.||12-JUL-16
6661|Finke Group|69458|6|Mentioned|p42:8|Devonian|Devonian|Amadeus Basin.||||||12-JUL-16
6661|Finke Group|69606|6|Mentioned|p10|Devonian|Devonian|Amadeus Basin. ||||||
6661|Finke Group|69673|6|Mentioned|p67, p86, p149 fig 120||||||Includes Polly Conglomerate, Langra Formation, Horseshoe Bend Shale, Idracowra Sandstone|Correlated with Pertnjara Group||
6661|Finke Group|71279|5|Briefly described|p355 Fig.2|Late Devonian|Late Devonian|Amadeus Basin.|||Polly Conglomerate, Langra Formation, Idracowra Sandstone, Horseshoe Bend Shale.|||
6661|Finke Group|71342|6|Mentioned|Ch9 p3, Ch9 p9, Ch9 p11|Devonian|Devonian|Thermal history briefly described (Ch9 p3). See also Ch9 p16-p17, Ch9 p20.||||Unconformably overlies the Mereenie Sandstone. Unconformably overlain by the Crown Point and Purni Formations.||
6661|Finke Group|72476|6|Mentioned|p36 Fig.9|||Amadeus Basin. Time-temperature thermal history diagram.||||||
6661|Finke Group|73085|6|Mentioned|p1|late Devonian|late Devonian||||Horseshore Bend Shale / Idracowra Sandstone, Langra Formation, Polly Conglomerate|Equivalent to Pertnjara Group.||
6661|Finke Group|73281|6|Mentioned|Appendix (DIP)|Permian|Permian|[Also written as Finke Group?]. See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
6669|Finniss River Group|9324|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Shale, siltstone, sandstone, greywacke, schist and gneiss, acid extrusive rocks.||||||07-NOV-08
6669|Finniss River Group|9534|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes the Fisher Creek Siltstone.||||||07-NOV-08
6669|Finniss River Group|9538|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Siltstone, greywacke, sandstone, felsic to mafic lavas, pyroclastics.  Conformably overlies the South Alligator Group.||||||07-NOV-08
6669|Finniss River Group|9579|5|Briefly described|Map Sheet|Paleoproterozoic|Paleoproterozoic|Early Proterozoic age.||||||
6669|Finniss River Group|9691|5|Briefly described|Map Legend|||||||||01-JUN-05
6669|Finniss River Group|9701|5|Briefly described|Map Legend|Proterozoic|Proterozoic|||||||02-JUN-05
6669|Finniss River Group|22536|5|Briefly described|p7|Proterozoic|Proterozoic|||||||
6669|Finniss River Group|22574|5|Briefly described|map|Proterozoic|Proterozoic|||||||
6669|Finniss River Group|22632|5|Briefly described|p520|Neoproterozoic|Proterozoic|Contains Burrell Creek Formation||||||24-JUL-06
6669|Finniss River Group|22810|5|Briefly described|Table2 P4, P13|||||||||
6669|Finniss River Group|22813|5|Briefly described|Map|Paleoproterozoic|Paleoproterozoic|Shale, siltstone, sandstone, greywacke, schist and gneiss.||||||07-NOV-08
6669|Finniss River Group|23120|5|Briefly described|p428|||||||||
6669|Finniss River Group|23121|5|Briefly described|p418|||||||||
6669|Finniss River Group|23122|5|Briefly described|p411|||||||||
6669|Finniss River Group|23216|5|Briefly described|Fig3p5,6,13,49||Orosirian|Age: 1870 Ma. Consists of: Burrell Creek Formation and Tollis Formation.||||||
6669|Finniss River Group|23714|5|Briefly described|p10|Proterozoic|Proterozoic|See also page 13.||||||
6669|Finniss River Group|23715|5|Briefly described|Map legend||Proterozoic|In the Rum Jungle and Central Regions and Litchfield Province||||||
6669|Finniss River Group|23733|5|Briefly described|p32 Fig. 19|||||||||
6669|Finniss River Group|24047|5|Briefly described|p5 Fig.4|Paleoproterozoic|Paleoproterozoic|Greywacke, siltstone, shale, minor felsic volcanics.  Geological Province: Pine Creek Orogen.  See also p6 Fig. 5.||||||07-JAN-09
6669|Finniss River Group|24260|6|Mentioned|p1013 Fig.1|||Geological Province: Pine Creek Inlier||||||
6669|Finniss River Group|24442|6|Mentioned|p43|||Of the Pine Creek Orogen. Overlain by the Tolmer Group.   Intruded by the Zamu Dolerite.||||||
6669|Finniss River Group|31824|6|Mentioned|p25|||Lithology||||||
6669|Finniss River Group|32170|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
6669|Finniss River Group|32307|4|Described|Table 1|||L.Proterozoic||||||
6669|Finniss River Group|32310|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
6669|Finniss River Group|32659|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
6669|Finniss River Group|32660|4|Described|Table 2|||||||||
6669|Finniss River Group|32700|3|Fully described|Table 1|||L. Proterozoic. Mention p12. Re Walpole et al. (1968)||||||24-JUL-06
6669|Finniss River Group|33225|6|Mentioned|p20|||||||||
6669|Finniss River Group|33376|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
6669|Finniss River Group|33377|6|Mentioned|Table 1|||Stratigraphy||||||
6669|Finniss River Group|33677|6|Mentioned|p395|||||||||
6669|Finniss River Group|35140|6|Mentioned|Fig.2|||||||||
6669|Finniss River Group|36473|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
6669|Finniss River Group|36535|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
6669|Finniss River Group|36635|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
6669|Finniss River Group|37462|4|Described|Table 4.II|||||||||
6669|Finniss River Group|37579|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes the Burrell Creek Formation and Fisher Creek Siltstone.||||||07-NOV-08
6669|Finniss River Group|37815|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
6669|Finniss River Group|38239|6|Mentioned|Fig.2|||||||||
6669|Finniss River Group|38349|6|Mentioned|p27|||||||||
6669|Finniss River Group|38884|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
6669|Finniss River Group|39068|5|Briefly described|Map legend|Proterozoic|Proterozoic|Includes the Burrell Creek Formation.||||||14-FEB-06
6669|Finniss River Group|39069|4|Described|p13|||||||||
6669|Finniss River Group|39320|6|Mentioned|Fig.1|||||||||
6669|Finniss River Group|39357|6|Mentioned|p12|||||||||
6669|Finniss River Group|39518|6|Mentioned|p9|||||||||
6669|Finniss River Group|39563|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
6669|Finniss River Group|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
6669|Finniss River Group|39801|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Siltstone, greywacke, sandstone, acid to basic lavas, pyroclastics.||||||07-NOV-08
6669|Finniss River Group|39889|6|Mentioned|Table 2|||||||||
6669|Finniss River Group|40104|6|Mentioned|p349|||||||||
6669|Finniss River Group|40168|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Siltstone, greywacke, sandstone, acid to basic lavas, pyroclastics.||||||07-NOV-08
6669|Finniss River Group|40223|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Siltstone, greywacke, sandstone, acid to basic lavas, pyroclastics.||||||07-NOV-08
6669|Finniss River Group|40243|6|Mentioned|Fig.2|||||||||
6669|Finniss River Group|40492|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
6669|Finniss River Group|40495|6|Mentioned|Fig.3|||||||||
6669|Finniss River Group|40809|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
6669|Finniss River Group|40823|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
6669|Finniss River Group|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
6669|Finniss River Group|41125|6|Mentioned|Fig.6|||||||||
6669|Finniss River Group|41294|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
6669|Finniss River Group|41304|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
6669|Finniss River Group|41305|4|Described|p17|||||||||
6669|Finniss River Group|41309|4|Described|p6|||||||||
6669|Finniss River Group|41311|4|Described|p10|||||||||
6669|Finniss River Group|41397|6|Mentioned|p11|||||||||
6669|Finniss River Group|41406|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
6669|Finniss River Group|41407|6|Mentioned|Map legend|Proterozoic||||||||
6669|Finniss River Group|41586|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
6669|Finniss River Group|41645|4|Described|p10|||||||||
6669|Finniss River Group|41646|6|Mentioned|Map legend|Paleoproterozoic||Shale, siltstone, sandstone, greywacke, conglomerate, acid extrusive rocks.||||||07-NOV-08
6669|Finniss River Group|41660|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes Chilling Sandstone, Burrell Creek Formation and Berinka Volcanics. Shale, siltstone, sandstone, greywacke, conglomerate, acid extrusive rocks.||||||07-NOV-08
6669|Finniss River Group|41661|4|Described|p10|||||||||
6669|Finniss River Group|41874|6|Mentioned|p11|||||||||
6669|Finniss River Group|41876|6|Mentioned|p21|||||||||
6669|Finniss River Group|42927|5|Briefly described|p428|||see also Fig.1p429, Fig.2 p430||||||24-JUL-06
6669|Finniss River Group|43140|5|Briefly described|p3||Paleoproterozoic|Burrell Creek Formation is only member of group to crop out in this area.||||||07-NOV-08
6669|Finniss River Group|43149|5|Briefly described|Map Legend||Paleoproterozoic|Of Orosirian age.||||||07-NOV-08
6669|Finniss River Group|43187|5|Briefly described|p7|||||||||
6669|Finniss River Group|43595|5|Briefly described|p351|||||||||
6669|Finniss River Group|43624|6|Mentioned|Table 1,p9||Paleoproterozoic|||||||07-NOV-08
6669|Finniss River Group|43720|5|Briefly described|p4||Paleoproterozoic|||||||07-NOV-08
6669|Finniss River Group|43832|5|Briefly described|19-20,Table3 p12, 97||Paleoproterozoic|Only Burrell Ck Fm described. Within Pine Ck Geosyncline. Overlies the Mt Bonnie Formation; overlain by El Sherana Group.||||||07-NOV-08
6669|Finniss River Group|44113|5|Briefly described|p240|Proterozoic|Proterozoic|Geological Province: Daly River Basin.||||||13-NOV-06
6669|Finniss River Group|44314|2|Defined|p.6-7,9,11,map|||(D52-4). DARWIN Sheet.||||||13-NOV-06
6669|Finniss River Group|44315|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
6669|Finniss River Group|44399|5|Briefly described|map legend||Paleoproterozoic|Includes the Burrell Creek Formation.||||||07-NOV-08
6669|Finniss River Group|45022|4|Described|p.40||Paleoproterozoic|On many pages.||||||07-NOV-08
6669|Finniss River Group|45064|5|Briefly described|p14|||||||||
6669|Finniss River Group|45086|4|Described|p26|||Lithology. L.Prot.||||||
6669|Finniss River Group|45112|4|Described|p50|||||||||
6669|Finniss River Group|46163|14|Not recorded|p.168-172,174|||Includes Noltenius Formation.||||||
6669|Finniss River Group|46675|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes the Burrell Creek Formation.  Conformably overlies the South Alligator Group. Intruded by the Shoobridge, Margaret and Cullen Granites, and Zamu Dolerite. Geological Province: Pine Creek Geosyncline.||||||07-NOV-08
6669|Finniss River Group|46676|14|Not recorded|p.6||Paleoproterozoic|L.Proterozoic; includes Noltenius Formation & Burrell Creek Formation.||||||07-NOV-08
6669|Finniss River Group|46678|5|Briefly described|Table 1|Proterozoic|Proterozoic|Contains the Burrell Creek Formation.||||||18-SEP-06
6669|Finniss River Group|46679|14|Not recorded|map legend|||Map legend of Katherine, 1 mile, (D53-9).||||||
6669|Finniss River Group|46700|5|Briefly described|P14, Table1 P10||Proterozoic|||||||
6669|Finniss River Group|46848|6|Mentioned|p167|||||||||
6669|Finniss River Group|46877|6|Mentioned|Fig.4|||||||||
6669|Finniss River Group|47047|6|Mentioned|p219|||||||||
6669|Finniss River Group|47049|6|Mentioned|Fig.2|||||||||
6669|Finniss River Group|48867|14|Not recorded|p.4|||map. Includes Burrell Creek Formation, Dorothy Volcanics.||||||
6669|Finniss River Group|48942|3|Fully described|p9|||See also pp10-21.||||||24-JUL-06
6669|Finniss River Group|60526|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Includes: Burrell Creek Formation.||||||
6669|Finniss River Group|60575|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Includes the Burrell Creek Formation.||||||10-JAN-05
6669|Finniss River Group|60677|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Overlies South Alligator Group.||||||
6669|Finniss River Group|61389|5|Briefly described|Map Legend|||||||||30-SEP-05
6669|Finniss River Group|61861|5|Briefly described|p13, Fig.2.|Orosirian|Orosirian|Pine Creek Orogen. Has similar lithology to Killi Killi Formation of Tanami Region.|1880-1850 Ma (Needham et al. 1988).|||Overlies South Alligator Group.||
6669|Finniss River Group|62375|5|Briefly described|p8 Table 1, 9 table 2, 10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Siltstone, shale, greywacke, arkose, quartzite, schist, minor interbedded volcanics. Thickness: 1500-5000m.Geological Province: Pine Creek Orogen.||||||11-FEB-10
6669|Finniss River Group|63866|4|Described|p105, p108-p109, p112, p123|Orosirian|Orosirian|Litchfield Province, Pine Creek Orogen. The basal felsic volcanics have crystallisation ages of ca 1863 Ma (see Warrs Volcanic Member and Berinka Volcanics)|ca. 1876-1861 Ma (Maximum depositional ages)||Includes the Warrs Volcanic Member and the Berinka Volcanics.|Conformably overlies the South Alligator Group. Intruded by the Ti-Tree Granophyre.|Turbiditic metasedimentary rocks and minor basal felsic volcanics.|
6669|Finniss River Group|64677|6|Mentioned|v,|||Pine Creek Orogen.|||Berinka Volcanics.|||
6669|Finniss River Group|64698|5|Briefly described|lithinterp table|Orosirian|Orosirian|Includes Tollis Formation, Chilling Sandstone, Burrell Creek Volcanics, Berinka Volcanics.||||||07-JAN-09
6669|Finniss River Group|64722|5|Briefly described|Fig. 2 p3-6, p9|Orosirian|Orosirian|Part of a younger component (1870-1860 Ma) of Central Domain of Pine Creek Orogen. See also mis-spelt Finnis River Group p.10.||||Overlain by El Sherana and Edith River Groups.||11-APR-12
6669|Finniss River Group|64730|5|Briefly described|p125 Fig. 3, p126, 139-140, 142 Fig. 11|Paleoproterozoic|Paleoproterozoic|Ages from extrusion ages of Warrs Volcanic Member and Berinka Volcanics, both low in the Group.|Max deposition ages 1862+/-3 Ma, 1861+/-4 Ma.||Includes Chilling Sandstone; Tollis and Burrell Creek Formations; Berinka and Meeway Volcanics.|Conformably overlies South Alligator Group.||02-MAY-12
6669|Finniss River Group|64731|5|Briefly described|p147, p149|||Central Domain, Pine Creek Orogen. Has been suggested as lower grade equivalent to Hermit Creek Metamorphics, but Pietsch & Edgoose (1988) say it unconformably overlies that unit.||||Conformably overlies South Alligator Group.||12-APR-12
6669|Finniss River Group|64956|5|Briefly described|p72, p78|||Contains the Burrell Creek Formation and Berinka Volcanics; conformable on South Alligator Group. Geological province: Pine Creek Orogen.||||||07-FEB-11
6669|Finniss River Group|65232|5|Briefly described|p6 Fig. 5, p5 Fig. 4|Palaeoproterozoic|Palaeoproterozoic|Includes Burrell Creek Formation. Intruded by Zamu Dolerite. Geol. Prov: Pine Creek Orogen.||||||09-FEB-10
6669|Finniss River Group|65339|5|Briefly described|p5 Fig.4, p6 Table 1, pp13-14.|||Flyschoid sedimentary rocks, believed to have been derived from a source to the west. Formerly included the Noltenius Formation, which is no longer recognised as a separate unit.|||Includes Burrell Creek Formation, Chilling Sandstone, Warrs Volcanics and Mulluk Mulluk Volcanics.||Greywacke, shale, siltstone.|
6669|Finniss River Group|67127|6|Mentioned|p175|Palaeoproterozoic|Palaeoproterozoic|Prospective for U-REE mineralisation. Hosts known unconformity-related vein-type U-Au mineralisation.||||||
6669|Finniss River Group|67167|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Unit in Cosmo Supergroup.|Includes Meeway and Berinka Volcanics; Henschke breccia; Burrell Creek Formation and Chilling Sandstone.|||
6669|Finniss River Group|67186|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Unit in Cosmo Supergroup.|Includes Burrell Creek Formation and Chilling Sandstone and Mulluk Mulluk Volcanics.|||23-NOV-11
6669|Finniss River Group|67232|6|Mentioned|p4. ||||||Includes Burrell Creek Formation.|||
6669|Finniss River Group|67323|5|Briefly described|Eastern Australia Time-Space Plot; p29|||Pine Creek area. Deposition age.|~1860-1850 Ma.||Tollis, Burrell Creek Formations; Chilling Sandstone.||Siltstone, greywacke, sandstone, felsic to mafic volcanic successions.|
6669|Finniss River Group|67355|5|Briefly described|p5, p7, p13, p15, p46-47 Figs.37-38, p69||Orosirian|Extensively exposed on the Batchelor Shelf and Central Trough.||Cosmo Howley Supergroup|Burrell Creek Formation, Noltenius Formation (abandoned), Berinka Volcanics, Dorothy Volcanics.|Overlying the South Alligator Group conformably.|Represents a succession of flyschoid sedimentary and minor volcanic rocks. Greywacke-siltstone-shale.|25-JAN-17
6669|Finniss River Group|67479|6|Mentioned|p56|||||||||
6669|Finniss River Group|67564|4|Described|p iv, p7 Table 2, p9 Fig.4, pp23-25.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Characteristically high-energy, oxidised flysch sedimentation. Deformed and metamorphosed to greenschist facies during the 1860 - 1850 Ma Nimbuwah Event. |||Includes Burrell Creek and Tollis Formations.|Overlies South Alligator Group conformably. Is intruded by David Suite. Is overlain unconformably by El Sherana and Katherine River Groups and Petrel Formation.||
6669|Finniss River Group|67779|4|Described|p5 Fig.4(b), p6 Fig.5, p105.|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen. Siliciclastic rocks were derived largely from an 1865 Ma source, with minor contribution from Neoarchean sources. |1863 Ma.|Unit in Cosmo Supergroup.|Includes Burrell Creek Formation, Chilling Sandstone and Tollis Formation.|Overlies South Alligator Group.||
6669|Finniss River Group|67824|5|Briefly described|p384|||Pine Creek Orogen.||||Underlain by the South Alligator Group.|Comprises iron-poor turbidites consisting of poorly sorted sandstones.|
6669|Finniss River Group|68733|6|Mentioned|p184|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||||||05-DEC-17
6669|Finniss River Group|69383|6|Mentioned|p28|||||Of Cosmo Supergroup|Includes Burrell Creek Formation.|||
6669|Finniss River Group|69419|6|Mentioned|p4:3 Fig.4.3|||W. Pine Creek Orogen.||||||12-JUL-16
6669|Finniss River Group|69420|4|Described|p5:2, 4-8, 11-13, 15-17, 25, 33, 79, 93|Paleoproterozoic|Paleoproterozoic|See also 99, 105, 116. Central Domain, Pine Creek Orogen. Deeper-water, high-energy mass-flow deposits. Maximum depositional age.|<1860 Ma (Worden et al., 2008).|Cosmo Supergroup.|Burrell Creek, Tollis Formations; Berinka, Dorothy Volcanics; Chilling Sandstone; Henschke Breccia.|Conformably overlies Mount Bonnie Formation (South Alligator Group). Probable equivalent to Welltree and Hermit Creek Metamorphics.|A thick succession of sedimentary rocks of turbiditic origin: siltstone, shale, phyllite, arenite and schist.|12-JUL-16
6669|Finniss River Group|69421|6|Mentioned|p6:3||||||Burrell Creek Formation|||12-JUL-16
6669|Finniss River Group|69423|6|Mentioned|p8:1|||Pine Creek Orogen. Possible stratigraphic equivalent of the Murphy Metamorphics.||||||12-JUL-16
6669|Finniss River Group|69424|6|Mentioned|p9:4|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Mis-spelled as Finnis River Group in 9:4.||||Time-correlative of Warramunga Formation.||12-JUL-16
6669|Finniss River Group|69577|6|Mentioned|p117 Fig.6|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||||||
6669|Finniss River Group|69917|5|Briefly described|p51,52|||Pine Creek Orogen, Central Domain|||Includes Burrell Creek Formation.|Conformably overlies South Alligator Group.||
6669|Finniss River Group|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. The undivided unit (under cover) and its constituents are mapped separately.||Cosmo Supergroup.|Includes Chilling Sandstone, Burrell Creek Formation.|Overlies South Alligator Group.||01-MAR-18
6669|Finniss River Group|71302|5|Briefly described|p73|Paleoproterozoic|Paleoproterozoic|Geological province: Litchfield Province. Paleoproterozoic metasedimentary sequence exposed on the North Australian Craton, and possibly one of several sources of zircon provenance to the Inverway Metamorphics.||||||
6679|Fish Billabong Adamellite|9324|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Biotite adamellite; aplite.||||||07-NOV-08
6679|Fish Billabong Adamellite|22809|4|Described|14|||||||||
6679|Fish Billabong Adamellite|24197|5|Briefly described|p18, p105 Tb. 15.1|Paleoproterozoic|Paleoproterozoic|Of the Allia Creek Suite. Age: ~1845Ma. Geological province: Litchfield Block/Pine Creek Inlier.||||||07-FEB-11
6679|Fish Billabong Adamellite|41980|5|Briefly described|Table 3 P575|||||||||
6679|Fish Billabong Adamellite|50586|5|Briefly described|p1.1, 3.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Of the Allia Suite.||||||07-NOV-08
6679|Fish Billabong Adamellite|63866|5|Briefly described|p105|Orosirian|Orosirian|Litchfield Province, Pine Creek Orogen. Numeric age is interpreted as the emplacement age.|1850  +/- 4 Ma (Worden et al, in review)|||||
6679|Fish Billabong Adamellite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1820-1850Ma. I-type. Biotite adamellite, aplite. Intrudes Hermit Creek Metamorphics, Wangi Basics.||||||07-JAN-09
6679|Fish Billabong Adamellite|64956|5|Briefly described|p2 Tb. 2, p50|Paleoproterozoic|Paleoproterozoic|Interpreted to intrude Burrell Creek Formation. Cryst. intrusion age: 1850+/-4Ma. Geological province: Pine Creek Orogen. Sample is pink, fine-medium grained, comprising K-feldspar. Quartz, plagioclase and biotite.||||||07-FEB-11
6679|Fish Billabong Adamellite|67186|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Unit in Allia Creek Suite.|||Biotite-quartz monzonite, aplite.|23-NOV-11
6679|Fish Billabong Adamellite|69420|5|Briefly described|p5:18-19, 28|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Mineralogy and petrology/geochemistry summarised. SHRIMP U-Pb zircon age.|1850 +/- 3 Ma: Worden et al. (2008).|Allia Creek Suite.|||Predominantly medium-grained, equigranular (partly heterogranular), partly foliated quartz monzonite.|12-JUL-16
6679|Fish Billabong Adamellite|69933|6|Mentioned|p1|||||||||
6679|Fish Billabong Adamellite|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||Allia Creek Suite.|||Unfoliated to moderately foliated quartz monzonite and granodiorite; associated tourmaline-bearing pegmatite.|
6679|Fish Billabong Adamellite|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|1850+/-3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Fine- to medium-grained quartz-K-feldspar-plagioclase-biotite granite.|
6682|Fish River Formation|22673|6|Mentioned|66 fig 3|||||||||
6682|Fish River Formation|22680|5|Briefly described|84 fig 2, 85,86|||Geol province Mount Isa Basin. Of theFickling Group.||||||18-SEP-06
6682|Fish River Formation|23065|6|Mentioned|16|||Geol province Lawn Hill Subprovince. Parent Fickling Group. Overlying unit Walford Dolomite.||||||
6682|Fish River Formation|23396|5|Briefly described|p407 Fig.2|||Of Fickling Group.||||||18-SEP-06
6682|Fish River Formation|23397|5|Briefly described|p463|||Of Fickling Group.||||||18-SEP-06
6682|Fish River Formation|23398|4|Described|p445|Statherian|Statherian|Age: ~1770Ma||||||18-SEP-06
6682|Fish River Formation|23406|4|Described|p608, p609 Fig. 9|||Of Fickling Group. Parts in both Gun and Prize Supersequences. Lithological details included in Fig. 9.||||||16-JUN-09
6682|Fish River Formation|31421|6|Mentioned|p509|||||||||
6682|Fish River Formation|32660|5|Briefly described|Table 5|||||||||
6682|Fish River Formation|35114|6|Mentioned|p202|||||||||
6682|Fish River Formation|35640|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
6682|Fish River Formation|36012|3|Fully described|Table 3|||See also p16.||||||18-SEP-06
6682|Fish River Formation|36439|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
6682|Fish River Formation|36442|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
6682|Fish River Formation|37568|6|Mentioned|Fig.5|||||||||
6682|Fish River Formation|38237|6|Mentioned|p126|||||||||
6682|Fish River Formation|38584|4|Described|p17|||||||||
6682|Fish River Formation|39445|5|Briefly described|Table 2|||See also p36 and p39.||||||18-SEP-06
6682|Fish River Formation|39497|6|Mentioned|Fig.4|||||||||
6682|Fish River Formation|39685|6|Mentioned|p407|||||||||
6682|Fish River Formation|39944|6|Mentioned|Fig.5|||||||||
6682|Fish River Formation|41406|6|Mentioned|Map legend|Mesoproterozoic||||||||
6682|Fish River Formation|41721|4|Described|p28|||||||||
6682|Fish River Formation|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
6682|Fish River Formation|43010|5|Briefly described|Fig.6||Mesoproterozoic|Of Fickling Group. Of "Mid Proterozoic" age.||||||18-SEP-06
6682|Fish River Formation|44305|14|Not recorded|p.13|||(E53-8). opp.6,18.||||||
6682|Fish River Formation|44306|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
6682|Fish River Formation|44482|14|Not recorded|p.8|||(E53-12).||||||
6682|Fish River Formation|45162|6|Mentioned|p147|||||||||
6682|Fish River Formation|45166|5|Briefly described|p30|||||||||
6682|Fish River Formation|46804|6|Mentioned|p154|||||||||
6682|Fish River Formation|49001|2|Defined|p8|Carpentarian|Carpentarian|||||||
6682|Fish River Formation|60558|5|Briefly described|p5 Fig. 4|||Of Fickling Group. Overlian by Walford Dolomite, underlain by Peters Creek Volcanics.||||||
6682|Fish River Formation|63111|5|Briefly described|p1162, p1164 Tb. 1|Statherian|Statherian|Ages: 1668 - 1653Ma. Geological Province: Isa Superbasin. Laminated fine-grained sanstone and siltstones, dolomudstones, laminated carbonates.||||||07-FEB-11
6682|Fish River Formation|63866|5|Briefly described|p56|||Calvert and Isa Superbasins.||||Equivalent to the Prize Supersequence.||
6682|Fish River Formation|65337|6|Mentioned|p30.|||||Basal unit in Fickling Group.||||
6682|Fish River Formation|67323|5|Briefly described|GIS attrib tbl, p26, p34|Paleoproterozoic|Paleoproterozoic|See also Solid Geology Map,Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Isa Superbasin. Listed as unit within the McNamara Group on p26 and p34. Shown as Lower and Upper Fish River Formation on both Time-Space Plots. MDA of 1715 +/- 11 Ma.|~1660-1650 Ma.|Fickling Group.|||Medium orthoquartzite|
6682|Fish River Formation|69433|4|Described|p18:2-4|Statherian|Statherian|Northern succession, Lawn Hill Platform. 10m to over 200m thick; c.250m in the type section in WESTMORELAND map area. Fluvial to shallow-marine tidal flat deposits. Age from detrital zircons (Page et al., 2000).|<1770 Ma (maximum deposition age).|Basal Fickling Group.||Unconformably overlies Peters Creek Volcanics. Is overlain conformably by Walford Dolostone.|Mainly sandstone: medium-grained, quartz-rich, with ripple marks, mudcracks and herringbone cross-strata; siltstone; and conglomerate lenses, with clasts derived from Wire Creek Sandstone, Peters Creek Volcanics and (?)Cliffdfale Volcanics.|12-JUL-16
6682|Fish River Formation|69591|5|Briefly described|p40, p42-43, p55|||Camooweal-Murphy Domain. S of Murphy Tectonic Ridge. Lower part was deposited during late Calvert time, with the upper part during Isa Superbasin time. Part of Loretta Supersequence. Fluvial/coastal deposits.|||||Medium orthoquartzite.|
6682|Fish River Formation|69673|5|Briefly described|p52 fig 42, p53 |||Maximum thickness of 200m. Deposited in shallow marine to tidal flat environment.||Fickling Group|||Sandstone with conglomerate lenses.|
6682|Fish River Formation|70849|5|Briefly described|Map legend.|Statherian|Statherian|Lawn Hill Platform.||Fickling Group.||Unconformably overlies Peters Creek Volcanics (Tawallah Group equivalent). Is overlain by Walford Dolostone.|Sandstone, fine- to coarse-grained, flaggy to massive; minor conglomerate and siltstone.|
6682|Fish River Formation|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1771+/-24 Ma (MDA: U-Pb zircon SHRIMP)||||Tuffite.|
6682|Fish River Formation|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as being located in the central and west of the South Nicholson Basin.||Fickling Group||Shown as partially overlying Weberra Granite and Nicholson Granite Complex and underlies Walford Dolomite.||
6682|Fish River Formation|72912|5|Briefly described|p5 Fig.3, p33 Fig.12.|Statherian|Statherian|Located in the West and Central of the South Nicholson Basin.||Fickling Group||Underlies Walford Dolomite and is partially equivalent to Drummond Formation, Brumby Formation and Bullrush Conglomerate.|Includes dolostone.|
6682|Fish River Formation|72913|5|Briefly described|p7 Fig.2.|Paleoproterozoic|Paleoproterozoic|Shown as being in the central part of the Isa Superbasin.||Fickling Group||Underlies Walford Dolomite.|Includes dolostone.|
6682|Fish River Formation|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin region, Isa Superbasin.||Fickling Group||Overlain by Walford Dolomite.||
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.||
6743|Fleming Sandstone|22538|6|Mentioned|Fig3 P708|||||||||
6743|Fleming Sandstone|22600|4|Described|Map legend|Statherian|Statherian|||||||
6743|Fleming Sandstone|24048|4|Described|p50|Paleoproterozoic|Paleoproterozoic|Of Parsons Range Group.  Geological Province: McArthur Basin.||||||07-NOV-08
6743|Fleming Sandstone|24049|5|Briefly described|Map Legend|Statherian|Statherian|Of Parsons Range Group. Quartz sandstone: white to pink, thin to thick-bedded, fine to medium-grained; flat-bedded to trough cross-bedded; mudflakes, rare mudstone intraclast conglomerate; cauliflower chert nodules. Geol. Prov: McArthur Basin.||||||12-OCT-05
6743|Fleming Sandstone|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Of Parsons Range Group. Geological Province: Northern McArthur Basin.||||||
6743|Fleming Sandstone|32660|5|Briefly described|Table 4|||||||||
6743|Fleming Sandstone|37462|5|Briefly described|p244|||||||||
6743|Fleming Sandstone|41406|6|Mentioned|Map legend|Mesoproterozoic||||||||
6743|Fleming Sandstone|42597|5|Briefly described|Map Legend|Carpentarian||||||||
6743|Fleming Sandstone|43010|2|Defined|p90||Paleoproterozoic|Of Parsons Range Group. Of Statherian age.||||||07-NOV-08
6743|Fleming Sandstone|44112|4|Described|p49,52|||||||||
6743|Fleming Sandstone|44299|4|Described|p.11||Paleoproterozoic|SD/53-7,8. L.Proterozoic. Table 1.||||||07-NOV-08
6743|Fleming Sandstone|44300|14|Not recorded|map legend||Paleoproterozoic|SD/53-7,8. L.Proterozoic.||||||07-NOV-08
6743|Fleming Sandstone|45162|6|Mentioned|p45|||||||||
6743|Fleming Sandstone|61403|5|Briefly described|Map Legend|Statherian|Statherian|Of Parsons Range Group. Quartz sandstone: white to pink, thin to thick-bedded, fine to medium-grained; flat-bedded to trough cross-bedded; mudflakes, rare mudstone intraclast conglomerate; cauliflower chert nodules. Geol. Prov: McArthur Basin.||||||
6743|Fleming Sandstone|64817|6|Mentioned|p353 Fig.4 |||||Unit in Parsons Range Group.||||
6743|Fleming Sandstone|69430|4|Described|p15:3, 13-14, 21-22|Statherian|Statherian|Walker Fault Zone, northern McArthur Basin. 50-200m thick. Shallow-marine (shoreline and tidal flat) deposits.||Parsons Range Group.||Conformably overlies Marura Siltstone. Is overlain conformably and gradationally by Koolatong Siltstone (Balma Group). Suggested correlative of most of Umbolooga Subgroup.|White to pink, fine- to medium-grained, thinly to thickly bedded quartz sandstone; local intraclast conglomerate and cauliflower chert.|12-JUL-16
6743|Fleming Sandstone|69673|6|Mentioned|p16 fig 13|||||||Overlain by Koolatong Siltstone, overlies Marura Siltstone||
6767|Floraville Formation|22747|6|Mentioned|p6||Precambrian|||||||
6767|Floraville Formation|23065|5|Briefly described|18|||Geol province Karumba Basin||||||
6767|Floraville Formation|23393|5|Briefly described|p24|Eocene|Paleocene|||||||
6767|Floraville Formation|23982|6|Mentioned|p96 Appendix 13|||Geological Province: Great Artesian Basin.||||||
6767|Floraville Formation|24073|5|Briefly described|p378 Table 2|Cenozoic|Cenozoic|Formerly part of Lynd Formation?  Maximum thickness: 40m.  Geological Province: Carpentaria Basin.||||||19-NOV-08
6767|Floraville Formation|30095|6|Mentioned|Map legend|Tertiary|Late Cretaceous|Upper Cretaceous - Tertiary||||||
6767|Floraville Formation|30582|6|Mentioned|p7|||||||||
6767|Floraville Formation|31433|4|Described|p6|||Upper Cretaceous-Tertiary||||||
6767|Floraville Formation|31434|3|Fully described|Table 1|||See also p9. U.Cretaceous-Tertiary||||||18-SEP-06
6767|Floraville Formation|31437|6|Mentioned|Map legend|Tertiary|Late Cretaceous|U.Cretaceous-Tertiary||||||
6767|Floraville Formation|33150|5|Briefly described|p13|||Possible equiv. Bulimba and Glendower Fms.||||||18-SEP-06
6767|Floraville Formation|33182|6|Mentioned|Fig.1|||Upper Cretaceous or Tertiary||||||
6767|Floraville Formation|33183|2|Defined|p227|early Tertiary|early Tertiary|Prob.Early Tertiary||||||
6767|Floraville Formation|34811|6|Mentioned|p5|||||||||
6767|Floraville Formation|35253|6|Mentioned|Map legend|early Tertiary|early Tertiary|Prob.Early Tertiary||||||
6767|Floraville Formation|35640|6|Mentioned|Map legend|early Tertiary|early Tertiary|Prob.Early Tertiary||||||
6767|Floraville Formation|36012|3|Fully described|Table 6|||See also p20.||||||18-SEP-06
6767|Floraville Formation|36228|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
6767|Floraville Formation|36439|6|Mentioned|Map legend|early Tertiary|early Tertiary|Prob.Early Tertiary||||||
6767|Floraville Formation|36442|6|Mentioned|Map legend|early Tertiary|early Tertiary|||||||
6767|Floraville Formation|37607|5|Briefly described|p334|||See also Fig.5.||||||
6767|Floraville Formation|38584|4|Described|p21|||||||||
6767|Floraville Formation|39445|5|Briefly described|Table 14|||Early Tertiary. See also p150.||||||18-SEP-06
6767|Floraville Formation|39556|5|Briefly described|Map legend|Oligocene|Paleocene|Palaeocene to Oligocene||||||
6767|Floraville Formation|39797|6|Mentioned|Map legend|early Tertiary|early Tertiary|Prob.Early Tertiary||||||
6767|Floraville Formation|40648|6|Mentioned|p12|||||||||
6767|Floraville Formation|41307|4|Described|p18|||||||||
6767|Floraville Formation|42637|6|Mentioned|p29|||||||||
6767|Floraville Formation|45145|5|Briefly described|p33|||See also Table 7.||||||
6767|Floraville Formation|46802|6|Mentioned|p135|||||||||
6767|Floraville Formation|46902|6|Mentioned|Table 1|||Correlation chart for Cainozoic land-surfaces||||||
6767|Floraville Formation|61155|5|Briefly described|p16|Eocene||Together with Louisa and Bulimba Formations thickness is 140m. Geological Province: Western Cape York, Karumba Basin.||||||03-MAR-10
6767|Floraville Formation|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Paleogene|Paleogene|Age: Early Tertiary?|||||Clayey quartz sandstone, conglomerate; minor mudstone and siltstone.|
6767|Floraville Formation|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as Oxley and Booval Groups; Petrie, Biloela, Bulimba, Duaringa, Emerald, Exevale, Glendower, Louisa, Lowmead, Marion, Red Mountain, Southern Cross, Springvale and Suttor Formations; Beaudesert, Casuarina, Nagoorin, Old Cork, Rossmoya, Takura and Water Park Creek beds; Fairview Gravel; Moses and Oakdale Sandstones, and unnamed units, are all mapped under the symbol, Tl.||||||
6767|Floraville Formation|69599|5|Briefly described|p580, p585, p602|Eocene|Paleocene|Carpentaria region. Capped by laterite and silcrete of the Tennant Creek Surface.||||Correlated with Fairview Gravel, Louisa and Bulimba Formations.||
6767|Floraville Formation|72421|4|Described|mapsheet|Paleogene|Paleogene|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet. Subsurface unit, appears on schematic diagram only.|||||Clayey quartz sandstone, conglomerate; minor mudstone and siltstone|10-DEC-19
6767|Floraville Formation|72422|4|Described|mapsheet|Eocene|Paleocene|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.|||||Clayey quartz sandstone, conglomerate; minor mudstone and siltstone|
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.||
6892|Fraynes Formation|14019|3|Fully described|p11, 18, 26|Paleoproterozoic|Paleoproterozoic|Of the Limbunya Group. Laminated dolomitic siltstone and mudstone; minor silty dolostone, dolostone, tuffite, siltstone, sandstone. Thick: 165m. Conformable on Campbell Springs Dolostone; Conformably overlain by Killaloc Fm. Geol. Prov: Birrindudu Basin.||||||07-NOV-08
6892|Fraynes Formation|23809|6|Mentioned|p52 Fig. 45|||Geological Province: Victoria-Birrindudu Basins.||||||30-MAR-05
6892|Fraynes Formation|24122|5|Briefly described|p4 Fig.3|||Of Limbunya Group.  Geological Province: Birrindudu Basin.||||||
6892|Fraynes Formation|24297|6|Mentioned|p21|||Of Limunya Group.  Geological Province: Birrindudu Basin.  See also p4 Fig. 3.||||||
6892|Fraynes Formation|24441|5|Briefly described|p1 Fig. 1|||Of the Limbunya Group. Overlies Campbell Springs Dolostone; overlain by Killaloc Formation. Geological Province: Birrindudu Basin.||||||
6892|Fraynes Formation|24442|5|Briefly described|p50 Fig. 1|||Of the Limbunya Group.  Geological Province: Birrindudu Basin.||||||
6892|Fraynes Formation|28255|3|Fully described|p26, Tb.11 (opp.p8)|||Of the Limbunya Group. Predominantly of silty dolomite with interbedded dolomite and siltstone and a chert horizon at the top. Conformably overlies Black Springs Dolomite; overlain, probably conformably, by Killaloc Fm. Max. thickness: 130m. See also p122||||||08-JUN-05
6892|Fraynes Formation|30003|4|Described|p9|||Of the Limbunya Group.  Max. thiockness: >40m.||||||19-SEP-06
6892|Fraynes Formation|30004|6|Mentioned|Map legend|Proterozoic|Proterozoic|Carpentarian or Adelaidean||||||
6892|Fraynes Formation|32172|4|Described|Table 1|||Carpentarian or Adelaidean||||||
6892|Fraynes Formation|32173|5|Briefly described|Map legend|Adelaidean|Carpentarian|Of the Limbunya Group.  Chert and minor dolerite, brecciated in places; siltstone and silty dolomite, minor dolomite, chert lenses and nodules.  Carpentarian or Adelaidean (per legend).||||||16-NOV-04
6892|Fraynes Formation|32660|5|Briefly described|Table 6|||||||||
6892|Fraynes Formation|33376|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
6892|Fraynes Formation|45112|5|Briefly described|Table 7|||||||||
6892|Fraynes Formation|48943|2|Defined|p32|Proterozoic|Proterozoic|||||||
6892|Fraynes Formation|60006|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Birrindudu Basin. Of Limbunya Group. Chert, feldspathic sandstone, tuffite.||||||07-NOV-08
6892|Fraynes Formation|60589|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Limbunya Group.  Dolomitic siltstone, silty dolostone, dolostone, purple/green micaceous siltstone, minor orange water-laid tuffite. Conformably overlies Campbell Springs Dolostone; conformably overlain by Killaloc Formation.  Geol.Prov: Birindudu Basin.||||||31-OCT-11
6892|Fraynes Formation|60672|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Silty dolostone, minor dolostone. Of Limbunya Group. Overlain unconformably by Wickham Formation. Overlies Campbell Springs Dolostone. Geological Province: Birrindudu Basin.||||||07-NOV-08
6892|Fraynes Formation|60682|4|Described|p7|Statherian|Statherian|Of Limbunya Group. Conformably overlies Campbell Springs Dolostone. Chert, cross-bedded feldspathic sandstone, dolostone and tuffite. Thickness: 20m. Geological Province: Birrindudu Basin.||||||
6892|Fraynes Formation|60685|5|Briefly described|p4 Fig. 3, p2|||Of the Limbunya Group. Overlain by the former Bardia Chert Member (Skull Creek Formation) now remapped as Tertiary silcrete/duricrust. Geological province: Birrindudu Basin.||||||19-MAY-05
6892|Fraynes Formation|65331|5|Briefly described|Map legend|Palaeoproterozoic|Palaeoproterozoic|Of Limbunya Group, Birrindudu Basin. Chert, feldspathic sandstone, "tuffite"||||||
6892|Fraynes Formation|65342|6|Mentioned|p11 Fig.13. |||Birrindudu Basin.||Unit in Limbunya Group.||Overlies Campbell Springs Dolostone. Is overlain by Killaloc Formation.||
6892|Fraynes Formation|67151|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Birindudu Basin. Shown as 'Undifferentiated Fraynes/Killaloc formations'.||Unit in Limbunya Group.|||Dolomitic siltstone, silicified dolostone.|31-OCT-11
6892|Fraynes Formation|68733|6|Mentioned|p177 Fig.2|||Birrindudu Basin.||Of the Limbunya Group.||||
6892|Fraynes Formation|69432|4|Described|p17:2, 7-8, 13|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin. Typically less than 100m thick. Some dolostone has a hydrocarbon odour. Concretions are common throughout; some appear to be balls or turbinate shapes of radiating clusters of Coxco Needles. Exploration target for base metals.||Limbunya Group.||Is overlain conformably by Killaloc Formation.|Basal fissile micaceous siltstone, overlain by fine-grained dolomitic rocks and siltstone; is proportionally more carbonate up-section; commonly capped by siliceous chert duricrust in outcrop. Waterlain tuff beds to 30cm thick mostly in lower half.|12-JUL-16
6892|Fraynes Formation|69673|6|Mentioned|p48 fig 35|||||Limbunya Group||Overlies Campbell Springs Dolostone, overlain by Killaloc Formation||
6892|Fraynes Formation|70206|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Birindudu Basin [misspelling of Birrindudu Basin]. [Note: unit shown as Mesoproterozoic, but radiometric age date is Paleoproterozoic, suggesting it may be a 'maximum age of deposition'].|1638+/-9 Ma SHRIMP zircon|Limbunya Group|||Dolomitic siltstone, silty dolostone, dolostone, micaceous siltstone, minor water laid tuffite.|18-JUL-16
6892|Fraynes Formation|70655|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Birindudu Basin. Shown as 'Undifferentiated Fraynes/Killaloc formations', with a single combined description.||Limbunya Group||Shown as unconformably overlain by Wickham Formation.|Dolomitic siltstone, silicified dolostone.|
6892|Fraynes Formation|70854|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin. Maximum depositional age.|<1638 +/- 9 Ma (SHRIMP zircon age).|Limbunya Group.||Overlies Campbell Springs Dolostone. Is overlain unconformably by Wickham Formation (Wattie Group).|Silty dolostone, minor dolostone.|21-SEP-17
6892|Fraynes Formation|70855|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin. No outcrop in map area: shown in Section only as undifferentiated Limbunya Group.||Limbunya Group.||||
6892|Fraynes Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||dolostone, siltstone|
6892|Fraynes Formation|71302|5|Briefly described|p6|Paleoproterozoic|Paleoproterozoic|Of Birindudu Basin.||Unit of Limbunya Group.||Overlain by Killaloc Formation. Underlain by Campbell Springs Dolostone.||
6892|Fraynes Formation|72248|6|Mentioned|p146|||Of Victoria Basin.||||||
6892|Fraynes Formation|72718|6|Mentioned|p7|||Birrindudu Basin.||Limbunyah Group||Underlain by Campbell Springs Dolostone. Overlain by Killaloc Formation.||
6892|Fraynes Formation|73083|6|Mentioned|p31|||||||||
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.|
7137|Georgina Limestone|8187|5|Briefly described|Map legend|Cambrian|Cambrian|Sandy and laminated micrite, intraformational conglomerate, two-toned limestone, algal boundstones, minor oolitic grainstones and silicification.  Overlies Thorntonia Limestone; underlies Ninmaroo Formation.||||||21-JUN-04
7137|Georgina Limestone|10116|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Sandy and laminated micrite, conglomerate, limestone, grainstones.||||||
7137|Georgina Limestone|22954|6|Mentioned|Fig3p9|Idamean|Undillan|||||||
7137|Georgina Limestone|24065|5|Briefly described|p234|Late Cambrian|Late Cambrian|Geological Province: Georgina Basin.  Maximum thickness: 30m.||||||
7137|Georgina Limestone|30479|6|Mentioned|Fig.6|||Stratigraphic relations||||||
7137|Georgina Limestone|30914|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
7137|Georgina Limestone|31287|3|Fully described|p424|||See also p425-432. Lithostratigraphy.||||||19-SEP-06
7137|Georgina Limestone|31288|6|Mentioned|p325|||||||||
7137|Georgina Limestone|31572|6|Mentioned|p4|||Refers Opik (1963, 1967)||||||
7137|Georgina Limestone|33111|4|Described|p36|||Mention p17,18||||||19-SEP-06
7137|Georgina Limestone|34454|5|Briefly described|Table 2|||U.Cambrian||||||
7137|Georgina Limestone|34847|6|Mentioned|Table 1|||Stratigraphy and hydrocarbon prospects.||||||19-SEP-06
7137|Georgina Limestone|35121|6|Mentioned|Map legend|Late Cambrian|Late Cambrian|||||||
7137|Georgina Limestone|35139|4|Described|Table.2|||||||||
7137|Georgina Limestone|36234|3|Fully described|p168|||See also Fig.1.||||||
7137|Georgina Limestone|36243|6|Mentioned|Table 1A|||||||||
7137|Georgina Limestone|37155|6|Mentioned|p265|||||||||
7137|Georgina Limestone|37572|4|Described|p161|||See also p165 and Fig.8.||||||19-SEP-06
7137|Georgina Limestone|38532|4|Described|p243|||See also Fig.1.||||||
7137|Georgina Limestone|39445|5|Briefly described|Table 4|||Was Ninmaroo Formation on map. See also p61, p64 and Fig.5.||||||19-SEP-06
7137|Georgina Limestone|39690|6|Mentioned|p88|||||||||
7137|Georgina Limestone|39921|6|Mentioned|Map legend|Late Cambrian|Middle Cambrian|Middle to Late Cambrian||||||
7137|Georgina Limestone|39943|6|Mentioned|Table 2A|||||||||
7137|Georgina Limestone|40038|6|Mentioned|p248|||||||||
7137|Georgina Limestone|40136|6|Mentioned|p29|||||||||
7137|Georgina Limestone|41587|6|Mentioned|p923|||||||||
7137|Georgina Limestone|41810|6|Mentioned|p112|||||||||
7137|Georgina Limestone|42060|6|Mentioned|Fig.5 P140|||||||||
7137|Georgina Limestone|42139|6|Mentioned|Fig.10 P74|||||||||
7137|Georgina Limestone|42956|5|Briefly described|p31 Fig.4|||||||||
7137|Georgina Limestone|43105|5|Briefly described|Fig.4,p9.|||||||||
7137|Georgina Limestone|43807|6|Mentioned|p352|||||||||
7137|Georgina Limestone|44091|14|Not recorded|p17,Tb.1,p18|Idamean|Mindyallan|||||||
7137|Georgina Limestone|44205|14|Not recorded|p8|||||||||
7137|Georgina Limestone|44211|2|Defined|p91,95,96,100-104|||Overlain disconformably by Ninmaroo Formation, rests on Mungerebar Limestone.||||||
7137|Georgina Limestone|44212|2|Defined|p110|||||||||
7137|Georgina Limestone|44285|14|Not recorded|p.4|||Ref. to Whitehouse. Qld,N.T. border.||||||
7137|Georgina Limestone|44308|14|Not recorded|p3,5,14,Tb.1||Late Cambrian|||||||
7137|Georgina Limestone|44309|2|Defined|Tb.1,p7,9,10,map|||||||||
7137|Georgina Limestone|44310|14|Not recorded|Map Legend||Early Cambrian|||||||
7137|Georgina Limestone|44312|14|Not recorded|Map Legend||Late Cambrian|||||||
7137|Georgina Limestone|44326|14|Not recorded|Map Legend||Late Cambrian|||||||
7137|Georgina Limestone|44362|6|Mentioned|p11|||||||||
7137|Georgina Limestone|44441|14|Not recorded|p.4|||Ref.to Whitehouse, 1931,1936. (E53-16).||||||
7137|Georgina Limestone|44457|14|Not recorded|p.3|||||||||
7137|Georgina Limestone|44543|14|Not recorded|p32|||Similar lithology to Mungerebar Limestone.||||||
7137|Georgina Limestone|44920|14|Not recorded|Map Legend,Sheet 4||Late Cambrian|||||||
7137|Georgina Limestone|45002|14|Not recorded|p14-122|||Late Cambrian fossils described. See also lexicon.||||||
7137|Georgina Limestone|45012|14|Not recorded|p101-154,162-167,|||p202-288,320-3. Late Cambrian fauna.||||||
7137|Georgina Limestone|45051|6|Mentioned|p5|||Cambrian age||||||
7137|Georgina Limestone|45052|3|Fully described|p115|||U.Camb.||||||
7137|Georgina Limestone|45053|6|Mentioned|p12|||||||||
7137|Georgina Limestone|45115|6|Mentioned|p6|||||||||
7137|Georgina Limestone|45130|6|Mentioned|p23|||||||||
7137|Georgina Limestone|46956|6|Mentioned|p160|||||||||
7137|Georgina Limestone|46958|6|Mentioned|Fig.2|||||||||
7137|Georgina Limestone|46959|6|Mentioned|Table 1|||||||||
7137|Georgina Limestone|47024|6|Mentioned|p1|||||||||
7137|Georgina Limestone|47058|6|Mentioned|p136|||||||||
7137|Georgina Limestone|48906|14|Not recorded|Tb.1,App.D|||||||||
7137|Georgina Limestone|48971|6|Mentioned|p10|||See aslo P27.||||||
7137|Georgina Limestone|49027|5|Briefly described|p8|||||||||
7137|Georgina Limestone|60122|6|Mentioned|p19|||||||||
7137|Georgina Limestone|60990|6|Mentioned|p85, |||||||||
7137|Georgina Limestone|63450|4|Described|p78 Fig. 5, p81|Late Cambrian|Middle Cambrian|Overlies Blazan Shale. Thickness at Mt Whelan: 406m. Geological province: Georgina Basin, East Toko Syncline. Dominated by fine-grained limestone with lesser calcarenite and intraformational conglomerate. See also p81.||||||21-MAR-16
7137|Georgina Limestone|64068|3|Fully described|p67-69, p64, 65, 73, 75|Late Cambrian|Middle Cambrian|Diverse fossil fauna. Lower part correlated with Devoncourt Limestone, Steamboat Sandstone. Correlated with Chabalowe Formation, Arrinthrunga Formation, Mungerebar Limestone, Devoncourt Limestone, Selwyn Range Limestone, O'Hara Shale, Pomegranate Limestone.||Of Narpa Group.||Conformably overlies Blazan Shale. Is overlain disconformably by Ninmaroo Formation.|Limestone, sandstone, interbedded mudstone and grainstone; overlain by grainstone and quartzic and silty limestone with breccia interbeds.|04-APR-12
7137|Georgina Limestone|64443|6|Mentioned|p3|Ordovician|Middle Cambrian|Of Ogilvie (1931) for fossiliferous carbonate rocks near the Georgina River. Mapped by Whitehouse (1936). Now defunct term embracing Middle Cambrian to Cambro-Ordovician rocks that straddle the NT-QLD border. Included by Noakes and Traves (1954) in their Barkly Group. Appears as Georgina Limestones on p3.||||Interdigitates with Arrinthrunga Formation.|Fossiliferous carbonate rocks.|14-MAY-14
7137|Georgina Limestone|65489|5|Briefly described|p125|Cambrian|Cambrian|Georgina Basin.||||Is overlain unconformably by Ninmaroo Formation.||
7137|Georgina Limestone|67323|5|Briefly described|GIS attrib tbl, p83,p88,p90,p92 Fig.12.2|Late Cambrian|Late Cambrian|See also Solid Geology Map. East Toko Syncline, Georgina Basin. Petroleum exploration target.||Narpa Group.||Unconformably overlies Thorntonia Limestone. Is overlain unconformably by Ninmaroo Formation.|Flaggy calcilutite and sandy calcilutite with chert, sandstone.|
7137|Georgina Limestone|67402|4|Described|p25 tbl RRM3|Iverian|Undillian|Georgina Basin, East Toko Syncline. Maximum thickness of 406m. Gas has been observed in fractures from this unit. Deposited in an open marine shelf environment. See also  p213 fig GRG3, p213 fig GRG5, p214, p215, p217.   ||||Overlies the Marqua beds. Unconformably overlies the Thorntonia Limestone or Hay River Formation. Overlain by the Arrinthrunga Formation.|Massive carbonate, dolomite, dolomitic limestone with minor argillaceous and sandy interbeds.|
7137|Georgina Limestone|67870|6|Mentioned|p43|Late Cambrian|Middle Cambrian|Georgina Basin.||||||
7137|Georgina Limestone|69443|5|Briefly described|p28:7, 16, 19, 26-28|Late Cambrian|Middle Cambrian|Southern Georgina Basin.||Narpa Group.||Interdigitates with Arrinthrunga Formation. Is overlain disconformably by Ninmaroo Formation and unconformably by Kelly Creek Formation (Toko Group).||12-JUL-16
7137|Georgina Limestone|69573|6|Mentioned|p659, 661|||Georgina Basin.||||||
7137|Georgina Limestone|69591|4|Described|p87, p93-94|Cambrian|Cambrian|West Toko Syncline, Georgina Basin. 30m thick. Crops out S of Glenormiston homestead around Tysons Bore and Pollys Lookout. Disputed relationship with Sun Hill Arkose is described. Low-energy intertidal or shallow subtidal environment with periodic episodes of higher energy. Contact not exposed. Time-equivalent to Pomegranate, Selwyn Range Limestones and O'Hara Shale. Contains a rich trilobite fauna.||Narpa Group.||Is overlain disconformably by Ninmaroo Formation.|Flaggy, grey, sandy limestone and pale aphanitic limestone (lower); cross-stratified, ripple-marked and ooid limestones.|
7137|Georgina Limestone|69673|6|Mentioned|p127|||||||||
7137|Georgina Limestone|70723|5|Briefly described|p24 Fig. 2|Cambrian|Cambrian|Georgina Basin.||Narpa Group||Overlies Mungerebar Limestone|Limestone.|
7137|Georgina Limestone|71283|6|Mentioned|p479|Late Cambrian|Late Cambrian|Glenormiston, western Queensland. Contains the type species of Eugonocare tessellatum Whitehouse (1939).||||||
7137|Georgina Limestone|72321|6|Mentioned|Fig 2|Jiangshanian|Pabian|Toko Syncline, Georgina Basin. Australian stages: Idamean to Iverian.||of Narpa Group.||||
7137|Georgina Limestone|72358|5|Briefly described|p117. p125|||Of Georgina Basin. Equivalent to Goyder Formation in the Amadeus Basin. G. reticulatus Zone is recorded in petroleum well Netting Fence 1 (Green & Balfe, 1980) at the base of the Georgina Limestone (195 m), and extended to occur throughout the Georgina Limestone (Laurie 2012). Also includes G. stolidotus zone.||||Underlain by Mungerebar Limestone.||10-JAN-20
7137|Georgina Limestone|72516|6|Mentioned|p92 - p94|||Southeastern Georgina Basin.||||Lower part equivalent to the Steamboat Sandstone, also generally equivalent to the Arrinthrunga Formation and the Eurowie Sandstone Member.||07-JUN-21
7197|Gilbert River Formation|9528|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|Includes two members: Coffin Hill and Yappar Members.  Fine to coarse clayey quartzose and lithic quartz sandstone, siltstone and shale.||||||
7197|Gilbert River Formation|9531|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|Includes: Coffin Hill Member, Yappar Member.||||||02-JUL-04
7197|Gilbert River Formation|9541|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|Quartzose sandstone, minor conglomerate, siltstone and shale.||||||
7197|Gilbert River Formation|12575|5|Briefly described|p781, p784 Table 1.|Albian|Late Jurassic|Laura Basin. Apatite fission track analyses, vitrinite reflectance data are detailed.|157-131 Ma.|||Overlies Dalrymple Sandstone.|Predominantly marine glauconitic sandstone.|
7197|Gilbert River Formation|22744|5|Briefly described|Fig1, P12, Table4||Cretaceous|||||||
7197|Gilbert River Formation|22747|5|Briefly described|p9||Mesozoic|||||||
7197|Gilbert River Formation|22780|5|Briefly described|map|Early Cretaceous|Late Jurassic|||||||
7197|Gilbert River Formation|22781|4|Described|p41|Early Carboniferous|Late Jurassic|In the Laura Basin.||||||19-SEP-06
7197|Gilbert River Formation|23031|5|Briefly described|31|||Geol province Carpentaria Basin||||||
7197|Gilbert River Formation|23032|5|Briefly described|p47|Cretaceous|Late Jurassic|||||||
7197|Gilbert River Formation|23065|5|Briefly described|18|||Geol province Carpentaria Basin||||||
7197|Gilbert River Formation|23071|6|Mentioned|p761|||||||||
7197|Gilbert River Formation|23220|6|Mentioned|p16||Mesozoic|||||||
7197|Gilbert River Formation|23291|4|Described|p80 Tb. 3.6|Early Cretaceous|Early Cretaceous|Age: Early Cretaceous. Conformably overlies Eulo Queen Group. Thickness: 10-12m. in Gilberton Plateau. Geological Province: Georgetown Region.||||||08-JUL-15
7197|Gilbert River Formation|23393|4|Described|p22|Early Cretaceous|Late Jurassic|||||||
7197|Gilbert River Formation|23420|6|Mentioned|p 131|||||||||
7197|Gilbert River Formation|23423|5|Briefly described|p259|Early Cretaceous|Late Jurassic|Carpentaria Basin.||||||
7197|Gilbert River Formation|23424|4|Described|Table 8.1 Fig 8.3 p340|Early Cretaceous|Late Jurassic|Age: Late Jurassic to Early Cretaceous? Maximum thickness ~10 m.||||||
7197|Gilbert River Formation|23425|4|Described|Table 9.7 p395|||Also see p378. Overlain by Wallumbilla Formation, conformably. Underlain by Garraway Sandstone, conformably. Geological Province Carpentaria Basin and Laura Basin. Max thickness 100 m.||||||30-JAN-07
7197|Gilbert River Formation|23426|4|Described|p403, Table 10.4 p407||Jurassic|Previously Battle Camp Sandstone. Overlain by Rolling Downs Group - conformable contact. Underlain by Dalrymple Sandstone - conformable contact. Geological Province: Laura Basin. Max. thickness 280 m.||||||30-JAN-07
7197|Gilbert River Formation|23428|6|Mentioned|p422|||||||||
7197|Gilbert River Formation|23430|4|Described|p455 & p520.|||Also found in Laura Basin, and Carpentaria Basin. Previously Battle Camp Sandstone in the Laura Basin. Underlain by Dalrymple Sandstone - in the Laura Basin. Eromanga Basin Province.||||||30-JAN-07
7197|Gilbert River Formation|23453|5|Briefly described|p19|Early Cretaceous|Early Cretaceous|||||||
7197|Gilbert River Formation|23493|4|Described|p7|Early Cretaceous|Early Cretaceous|Sandstone, conglomerate and shale.  Unconformably overlain by Lynd Formation; unconformably underlain by Inoruni Sandstone.  Of the Carpentaria and Great Artesian Basins.||||||30-JAN-07
7197|Gilbert River Formation|23495|5|Briefly described|map legend|Early Cretaceous|Early Cretaceous|||||||
7197|Gilbert River Formation|23496|5|Briefly described|Table 4, p59|Early Cretaceous|Late Jurassic|Thickness: ~107m.||||||19-SEP-06
7197|Gilbert River Formation|23498|5|Briefly described|p20 table 1||Cretaceous|Correlates with Blythesdale Sandstone.||||||
7197|Gilbert River Formation|23499|5|Briefly described|map legend|Early Cretaceous|Jurassic|Eromanga Basin||||||
7197|Gilbert River Formation|23500|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|Carpentaria and Karumba Basins. Age shown as Late Jurassic? - Early Cretaceous.||||||
7197|Gilbert River Formation|23501|5|Briefly described|map legend|Early Cretaceous|Late Jurassic|Late Jurassic? - Early Cretaceous, Carpentaria Basin.||||||
7197|Gilbert River Formation|23510|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|||||||
7197|Gilbert River Formation|23511|5|Briefly described|Map Legend|Cretaceous|Middle Jurassic|||||||
7197|Gilbert River Formation|23512|5|Briefly described|Map Legend|Cretaceous|Middle Jurassic|||||||
7197|Gilbert River Formation|23518|5|Briefly described|p13|Mesozoic|Mesozoic|Geological Province: Carpentaria Basin.||||||
7197|Gilbert River Formation|23616|5|Briefly described|Table 1C p12 p39|Early Cretaceous|Late Jurassic|Overlies Proterozoic rocks of the Dargalong Inlier. Carpentaria Basin.||||||
7197|Gilbert River Formation|23713|5|Briefly described|p8 Table 1|Early Cretaceous|Late Jurassic|See also p6.||||||19-SEP-06
7197|Gilbert River Formation|23846|5|Briefly described|p5|Early Cretaceous|Early Cretaceous|Overlies the Eulo Queen Group. Quartzose sandstone and conglomerate with some thin marine sediment beds. Geological Province: Eromanga Basin.||||||
7197|Gilbert River Formation|23982|5|Briefly described|p58 Fig.18|||Geological Province: Carpentaria Basin.||||||
7197|Gilbert River Formation|24013|5|Briefly described|p17 Tb. 1|Early Cretaceous|Early Cretaceous|Conglomerate, sandstone, arkose, siltstone.  Unconformably overlies Croydon Felsite.  Max. thickness: 250ft.  Geological Province: Great Artesian Basin.||||||
7197|Gilbert River Formation|24032|5|Briefly described|p5, p12, p23 Fig. 10, p29, p31 Fig. 11|Early Cretaceous|Late Jurassic|Max thickness: 3-40m. Consists of basal conglomerate overlain by cross bedded quartzose sandstone, and mudstone.||||||
7197|Gilbert River Formation|24048|6|Mentioned|p76|Mesozoic|Mesozoic|Geological Province: Carpentaria Basin.||||||
7197|Gilbert River Formation|24073|5|Briefly described|p378 Table 2|||Geological Province: Carpentaria Basin.||||||
7197|Gilbert River Formation|24086|5|Briefly described|p312 Fig. 1|Cretaceous|Jurassic|||||||
7197|Gilbert River Formation|24089|5|Briefly described|Student Activites|Early Cretaceous|Late Jurassic|||||||
7197|Gilbert River Formation|24092|5|Briefly described|p8 Fig.3|||Geological Province: Carpentaria Basin.||||||
7197|Gilbert River Formation|24213|5|Briefly described|p776 Fig. 1|Cretaceous|Jurassic|||||||
7197|Gilbert River Formation|24393|5|Briefly described|p152 Tb. 1|Mesozoic|Mesozoic|Contains the Batavia, Glennie and Briscoe Members.||||||
7197|Gilbert River Formation|24419|5|Briefly described|p19|Early Cretaceous|Late Jurassic|Of the Carpentaria and Eromanga Basin Sequences.||||||08-MAR-05
7197|Gilbert River Formation|24485|3|Fully described|p2, p38 Tb.6|Early Cretaceous|Late Jurassic|Max Thickness: ~107m. Basal unit of the Carpentaria Basin. Geological Province: Carpentaria Basin.||||||29-OCT-15
7197|Gilbert River Formation|24486|5|Briefly described|Map legend|Cretaceous|Late Jurassic|Geological Province: Carpentaria Basin.||||||
7197|Gilbert River Formation|29591|6|Mentioned|Table 72|||||||||
7197|Gilbert River Formation|30020|4|Described|p29|||||||||
7197|Gilbert River Formation|30021|6|Mentioned|p87|||||||||
7197|Gilbert River Formation|30095|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Upper Jurassic - Lower Cretaceous||||||
7197|Gilbert River Formation|30102|4|Described|p27|||See also p31-34. Correlation with Jurassic-Cretaceous units.||||||19-SEP-06
7197|Gilbert River Formation|30582|6|Mentioned|p4|||||||||
7197|Gilbert River Formation|30584|4|Described|Table 1|||Also mention p6.||||||19-SEP-06
7197|Gilbert River Formation|30585|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
7197|Gilbert River Formation|30587|6|Mentioned|Map legend|Early Cretaceous|Jurassic|Jurassic to Lower Cretaceous||||||
7197|Gilbert River Formation|30914|6|Mentioned|Map legend|Cretaceous|Jurassic|Jurassic - Cretaceous||||||
7197|Gilbert River Formation|30916|6|Mentioned|p98|||Table on P98.||||||
7197|Gilbert River Formation|31121|4|Described|p390|||||||||
7197|Gilbert River Formation|31163|6|Mentioned|p247|||Jurassic - Cretaceous||||||
7197|Gilbert River Formation|31164|5|Briefly described|p9|||Neocomian ? - Abtian||||||
7197|Gilbert River Formation|31165|5|Briefly described|Table 1|||||||||
7197|Gilbert River Formation|31166|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
7197|Gilbert River Formation|31168|4|Described|p10|||||||||
7197|Gilbert River Formation|31422|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|Quartzose sandstone and conglomerate; siltstone.||||||02-DEC-04
7197|Gilbert River Formation|31433|4|Described|p7|||Jurassic-Cretaceous||||||
7197|Gilbert River Formation|31434|3|Fully described|Table 1|||U.Jurassic - L.Cretaceous. See also p8.||||||19-SEP-06
7197|Gilbert River Formation|31437|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|U.Jurassic-L.Cretaceous||||||
7197|Gilbert River Formation|31440|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Upper Jurassic to Lower Cretaceous||||||
7197|Gilbert River Formation|31832|6|Mentioned|Table 6|||||||||
7197|Gilbert River Formation|32314|6|Mentioned|Fig. 4|||||||||
7197|Gilbert River Formation|32392|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|U.Jur.-L.Cret.||||||
7197|Gilbert River Formation|32393|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|U.Jur.-L.Cret.||||||
7197|Gilbert River Formation|32395|6|Mentioned|p6|||Stratigraphic table||||||
7197|Gilbert River Formation|32396|6|Mentioned|p8|||Stratigraphic table||||||
7197|Gilbert River Formation|32518|5|Briefly described|p765|||||||||
7197|Gilbert River Formation|32531|6|Mentioned|Fig.2|||On P474||||||
7197|Gilbert River Formation|32553|4|Described|p38|||||||||
7197|Gilbert River Formation|32563|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
7197|Gilbert River Formation|32705|5|Briefly described|p179|||||||||
7197|Gilbert River Formation|32706|6|Mentioned|p10|||||||||
7197|Gilbert River Formation|33075|6|Mentioned|p451|||||||||
7197|Gilbert River Formation|33086|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Upper Jurassic to Lower Cretaceous||||||
7197|Gilbert River Formation|33150|4|Described|p9|||||||||
7197|Gilbert River Formation|33151|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|U.Jur.-L.Cret.||||||
7197|Gilbert River Formation|33165|6|Mentioned|Chart|||Correlation chart only||||||
7197|Gilbert River Formation|33176|5|Briefly described|p171|||||||||
7197|Gilbert River Formation|33177|5|Briefly described|Table 1|||||||||15-JUL-04
7197|Gilbert River Formation|33178|5|Briefly described|p11|||||||||
7197|Gilbert River Formation|33179|4|Described|Table 2|||||||||
7197|Gilbert River Formation|33180|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Upper Jurassic to Lower Cretaceous||||||
7197|Gilbert River Formation|33182|1|Redefined|p190|Early Cretaceous|Late Jurassic|Replaces Wrotham Park Sandstone. U.Jur.- L.Cret.||||||19-SEP-06
7197|Gilbert River Formation|33183|3|Fully described|p230|||Description includes history of nomenclature.||||||19-SEP-06
7197|Gilbert River Formation|33184|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic - Early Cretaceous||||||
7197|Gilbert River Formation|33185|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
7197|Gilbert River Formation|33226|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
7197|Gilbert River Formation|33368|6|Mentioned|p25|||Strat.table.||||||
7197|Gilbert River Formation|33528|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic - Early Cretaceous||||||
7197|Gilbert River Formation|33529|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic - Early Cretaceous||||||
7197|Gilbert River Formation|33561|6|Mentioned|p102|||||||||
7197|Gilbert River Formation|33638|5|Briefly described|Table 1|||||||||
7197|Gilbert River Formation|33643|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
7197|Gilbert River Formation|33644|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
7197|Gilbert River Formation|33648|5|Briefly described|p19|||||||||
7197|Gilbert River Formation|33772|4|Described|p13|||||||||
7197|Gilbert River Formation|33773|4|Described|Table 1|||||||||
7197|Gilbert River Formation|33882|4|Described|p14|||Mention p8.||||||19-SEP-06
7197|Gilbert River Formation|33900|6|Mentioned|p21|||||||||
7197|Gilbert River Formation|33907|6|Mentioned|p5|||||||||
7197|Gilbert River Formation|33908|6|Mentioned|p595|||||||||
7197|Gilbert River Formation|34356|6|Mentioned|p2|||Upper Jurassic - Lower Cretaceous. See also pp10,11,12 etc.||||||19-SEP-06
7197|Gilbert River Formation|34811|4|Described|Table 1|||||||||
7197|Gilbert River Formation|35204|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
7197|Gilbert River Formation|35214|6|Mentioned|p8|||||||||
7197|Gilbert River Formation|35220|4|Described|p16|||||||||
7197|Gilbert River Formation|35253|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|||||||
7197|Gilbert River Formation|35434|6|Mentioned|p37|||||||||
7197|Gilbert River Formation|35559|4|Described|Table 1|||||||||
7197|Gilbert River Formation|35560|4|Described|p290|||||||||
7197|Gilbert River Formation|35640|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|||||||
7197|Gilbert River Formation|35648|6|Mentioned|p18|||||||||
7197|Gilbert River Formation|35793|6|Mentioned|Fig.3|||||||||
7197|Gilbert River Formation|35811|5|Briefly described|Table 3|||||||||
7197|Gilbert River Formation|35814|6|Mentioned|p582|||||||||
7197|Gilbert River Formation|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
7197|Gilbert River Formation|35920|6|Mentioned|p26|||||||||
7197|Gilbert River Formation|35921|6|Mentioned|p31|||||||||
7197|Gilbert River Formation|36012|3|Fully described|Table 5|||See also p18.||||||19-SEP-06
7197|Gilbert River Formation|36216|6|Mentioned|p211|||||||||
7197|Gilbert River Formation|36228|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
7197|Gilbert River Formation|36229|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
7197|Gilbert River Formation|36243|6|Mentioned|Table 6A|||||||||
7197|Gilbert River Formation|36552|6|Mentioned|p59|||||||||
7197|Gilbert River Formation|36571|6|Mentioned|Table 4|||||||||
7197|Gilbert River Formation|37603|6|Mentioned|p444|||||||||
7197|Gilbert River Formation|37608|3|Fully described|Table 2|||||||||
7197|Gilbert River Formation|38199|5|Briefly described|p423|||Palynology||||||
7197|Gilbert River Formation|38291|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late and/or Early Cretaceous||||||
7197|Gilbert River Formation|38348|6|Mentioned|p25|||||||||
7197|Gilbert River Formation|38608|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
7197|Gilbert River Formation|39027|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
7197|Gilbert River Formation|39029|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||25-AUG-04
7197|Gilbert River Formation|39211|5|Briefly described|p34|||Fossils in strat. holes. See also Fig.11||||||
7197|Gilbert River Formation|39315|6|Mentioned|Fig.6|||||||||
7197|Gilbert River Formation|39425|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
7197|Gilbert River Formation|39445|5|Briefly described|Table 10|||||||||
7197|Gilbert River Formation|39496|6|Mentioned|p7|||See also p16.||||||19-SEP-06
7197|Gilbert River Formation|39556|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
7197|Gilbert River Formation|39562|5|Briefly described|Map legend|Cretaceous|Jurassic|Pebbly quartz sandstone. Part of the Trans-Australian Platform Cover.||||||15-JUN-06
7197|Gilbert River Formation|39687|6|Mentioned|Fig.5|||||||||
7197|Gilbert River Formation|39797|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
7197|Gilbert River Formation|39799|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
7197|Gilbert River Formation|39899|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
7197|Gilbert River Formation|39917|6|Mentioned|Map legend|Early Cretaceous|Jurassic|Jurassic-Early Cretaceous||||||
7197|Gilbert River Formation|39943|6|Mentioned|Table 8A|||||||||
7197|Gilbert River Formation|40218|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
7197|Gilbert River Formation|40221|6|Mentioned|p20|||||||||
7197|Gilbert River Formation|40648|3|Fully described|p12|||||||||
7197|Gilbert River Formation|40659|6|Mentioned|p250|||Mention p254.||||||19-SEP-06
7197|Gilbert River Formation|40924|6|Mentioned|p7|||||||||
7197|Gilbert River Formation|41125|6|Mentioned|p42|||||||||
7197|Gilbert River Formation|41204|6|Mentioned|p14|||||||||
7197|Gilbert River Formation|41266|6|Mentioned|Fig.3|||||||||
7197|Gilbert River Formation|41306|6|Mentioned|p4|||||||||
7197|Gilbert River Formation|41307|4|Described|p17|||||||||
7197|Gilbert River Formation|41310|5|Briefly described|p14|||||||||
7197|Gilbert River Formation|41361|6|Mentioned|Fig.3|||||||||
7197|Gilbert River Formation|41675|6|Mentioned|p71|||||||||
7197|Gilbert River Formation|42061|4|Described|p155|||See also Fig.11||||||
7197|Gilbert River Formation|42369|3|Fully described|p57|||Supersedes Battle Camp Formation.||||||19-SEP-06
7197|Gilbert River Formation|42464|6|Mentioned|p8|||||||||
7197|Gilbert River Formation|42474|6|Mentioned|p28|||formerly Battle Camp Formation||||||
7197|Gilbert River Formation|42490|4|Described|p17||Cretaceous|Equivalent to the Battle Camp Formation (used 1965)||||||
7197|Gilbert River Formation|42500|5|Briefly described|p12|||Jurassic?||||||
7197|Gilbert River Formation|42556|5|Briefly described|p13|||||||||
7197|Gilbert River Formation|42632|6|Mentioned|p11|||||||||
7197|Gilbert River Formation|42637|4|Described|p10, 22|||||||||
7197|Gilbert River Formation|42640|5|Briefly described|p11|||||||||
7197|Gilbert River Formation|42650|4|Described|p16|||||||||
7197|Gilbert River Formation|42691|5|Briefly described|map legend|Mesozoic||||||||
7197|Gilbert River Formation|42693|5|Briefly described|map legend|Cretaceous|Jurassic|||||||
7197|Gilbert River Formation|42804|5|Briefly described|p115|||||||||
7197|Gilbert River Formation|42933|4|Described|p236|||||||||
7197|Gilbert River Formation|43060|4|Described|p58,Table 1c|Early Cretaceous|Late Jurassic|||||||
7197|Gilbert River Formation|43083|5|Briefly described|p185|Cretaceous|Late Jurassic|Includes quartzose sand, gravel and minor clay desposits.||||||17-JUN-09
7197|Gilbert River Formation|43087|6|Mentioned|p12|||||||||
7197|Gilbert River Formation|43098|4|Described|p47|||||||||
7197|Gilbert River Formation|43105|5|Briefly described|p16|||||||||
7197|Gilbert River Formation|43110|4|Described|p53|||In the Laura Basin.||||||19-SEP-06
7197|Gilbert River Formation|43124|5|Briefly described|p31|||||||||
7197|Gilbert River Formation|43254|5|Briefly described|map legend|Early Cretaceous|Late Jurassic|||||||
7197|Gilbert River Formation|43285|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|||||||
7197|Gilbert River Formation|43286|5|Briefly described|Map Legend|Cretaceous|Jurassic|||||||
7197|Gilbert River Formation|43287|5|Briefly described|Map Legend||Mesozoic|Late Jurassic? to Early Cretaceous.||||||
7197|Gilbert River Formation|43487|5|Briefly described|20|||||||||
7197|Gilbert River Formation|43564|6|Mentioned|p463|||||||||
7197|Gilbert River Formation|43596|4|Described|p40, p39 Tb. 4|Early Cretaceous|Late Jurassic|Overlies Dalrymple Sandstone. Geological province: Laura and Carpentaria Basins. Max. thickness: 283m. Mostly clayey quartzose sandstone; some coarser rocks towards base, lenses of coarser material including quartz gravels, throughout; top locally silicified.||||||07-APR-15
7197|Gilbert River Formation|43603|5|Briefly described|p9|Early Cretaceous|Late Jurassic|||||||
7197|Gilbert River Formation|43625|6|Mentioned|p9|Early Cretaceous|Late Jurassic|||||||
7197|Gilbert River Formation|43630|6|Mentioned|p16,69|||||||||
7197|Gilbert River Formation|43665|6|Mentioned|p24|Early Cretaceous|Late Jurassic|||||||
7197|Gilbert River Formation|43730|5|Briefly described|p9,29||Mesozoic|||||||
7197|Gilbert River Formation|43738|5|Briefly described|p5|||||||||
7197|Gilbert River Formation|43740|5|Briefly described|Fig.2,p11|Early Cretaceous|Late Jurassic|||||||
7197|Gilbert River Formation|43820|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|||||||
7197|Gilbert River Formation|43883|14|Not recorded|p18 Fig.4-3|||||||||
7197|Gilbert River Formation|43995|14|Not recorded|Tb.p9||Cretaceous|||||||
7197|Gilbert River Formation|44031|14|Not recorded|p3,Tb.1,p4|Early Cretaceous|Late Jurassic|||||||
7197|Gilbert River Formation|44047|14|Not recorded|Map Legend|||||||||
7197|Gilbert River Formation|44049|14|Not recorded|Map Legend||Early Cretaceous|||||||
7197|Gilbert River Formation|44050|14|Not recorded|p154,163,Pl.8|||||||||
7197|Gilbert River Formation|44082|6|Mentioned|p6,Tb.p34|Aptian|Neocomian|Mentioned with respect to Qld Cretaceous fossils which are either of stratigraphic significance or are illustrative of the occurrence of a particular group.||||||
7197|Gilbert River Formation|44112|6|Mentioned|p82|||||||||
7197|Gilbert River Formation|44246|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|||||||
7197|Gilbert River Formation|44251|14|Not recorded|p2|||Correlated with Wrotham Park Sandstone.||||||
7197|Gilbert River Formation|44346|14|Not recorded|opp.p5|||||||||
7197|Gilbert River Formation|44373|14|Not recorded|p20|||Map only.||||||
7197|Gilbert River Formation|44376|14|Not recorded|p4,5|||||||||
7197|Gilbert River Formation|44414|14|Not recorded|p111,114||Cretaceous|||||||
7197|Gilbert River Formation|44417|14|Not recorded|p417|||Overlain by Rolling Downs Group.||||||
7197|Gilbert River Formation|44514|2|Defined|p35,36||Aptian|(Lower Aptian) Fossils.||||||
7197|Gilbert River Formation|44656|2|Defined|p325,327,Fig.49,T.10|||Unconformably overlies Croydon Felsite, Inoruni Sandstone and Croydon Granite.||||||19-SEP-06
7197|Gilbert River Formation|44727|14|Not recorded|p302-303|||Unconformably overlies Inoruni Sandstone. (Gulf of Carpentaria)||||||
7197|Gilbert River Formation|44926|5|Briefly described|Map Legend|||Late Jurassic? - Early Cretaceous||||||
7197|Gilbert River Formation|45004|2|Defined|p.8,14,15|||Tb.2||||||
7197|Gilbert River Formation|45009|2|Defined|p21,35,62-69,71,110,||Early Cretaceous|p134,Pls.5,10,13,14. Overlain by Lynd Formation. Name "Gilbert River Formation" preferred to "Blythesdale Group" as sediments equivalent only to upper beds of Blythesdale Group fossils.||||||30-JAN-07
7197|Gilbert River Formation|45014|14|Not recorded|p57,63,Pl.39,41,42||Cretaceous|||||||
7197|Gilbert River Formation|45025|6|Mentioned|p95|||Ref. to Laing and Power 1960.||||||19-SEP-06
7197|Gilbert River Formation|45145|3|Fully described|p18 Table 5|||||||||14-JUN-13
7197|Gilbert River Formation|45161|6|Mentioned|p67|||||||||
7197|Gilbert River Formation|45167|5|Briefly described|p54|||||||||
7197|Gilbert River Formation|45168|6|Mentioned|p6|||||||||
7197|Gilbert River Formation|46791|5|Briefly described|p42|||||||||
7197|Gilbert River Formation|46881|6|Mentioned|Table 2|||||||||
7197|Gilbert River Formation|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
7197|Gilbert River Formation|47083|4|Described|p19-20|Aptian|Neocomian|In the Carpentaria Basin.||||||22-FEB-07
7197|Gilbert River Formation|48908|14|Not recorded|Tb.1||Early Cretaceous|||||||
7197|Gilbert River Formation|48995|5|Briefly described|p72|||Age and thickness only described.||||||
7197|Gilbert River Formation|49010|6|Mentioned|Fig.4|||Carpentaria Basin||||||
7197|Gilbert River Formation|49011|6|Mentioned|p28|||See also Fig.3.||||||
7197|Gilbert River Formation|49769|6|Mentioned|p4|||||||||
7197|Gilbert River Formation|50100|5|Briefly described|p23|Early Cretaceous|Late Jurassic|Partly fluvial and partly shallow-marine clastic unit.  Overlain by Rolling Downs Group.  Geological Province: Carpentaria Basin / Eromanga Basin.||||||
7197|Gilbert River Formation|50198|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|Consists of: Coffin Hill Member, Yappar Member.||||||
7197|Gilbert River Formation|50199|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|Includes: Yappar Member, Coffin Hill Member.||||||
7197|Gilbert River Formation|50210|5|Briefly described|Map Legend|Cretaceous|Late Jurassic|Overlies: Eulo Queen Group.  Includes: Yappar Member, Coffin Hill Member.||||||
7197|Gilbert River Formation|50211|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|Conformably overlies Loth Formation||||||
7197|Gilbert River Formation|50332|6|Mentioned|p77|Mesozoic|Mesozoic|Sedimentary rocks host a minor uranium mineralisation of the roll-front type.||||||07-FEB-11
7197|Gilbert River Formation|50587|5|Briefly described|Map Legend|Early Cretaceous|Middle Jurassic|Geological Province: Quincan Province, Laura Basin. Fine to coarse-grained, clayey quartzose sandstone.||||||28-JUN-04
7197|Gilbert River Formation|50595|5|Briefly described|Map Legend|Early Cretaceous|Middle Jurassic|Includes: Coffin Hill Member, Yappar Member.||||||
7197|Gilbert River Formation|50596|5|Briefly described|Map Legend|Cretaceous|Middle Jurassic|Overlies: Dalrymple Sandstone.  Quartz sandstone, conglomerate, mudstone.||||||
7197|Gilbert River Formation|50627|5|Briefly described|Map legend|Late Jurassic|Middle Jurassic|Of the Eulo Queen Group. Fine to coarse clayey quartzose and lithic-quartz sandstone; siltstone and shale.  Overlies Loth Formation.||||||06-JUL-04
7197|Gilbert River Formation|50630|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|Quartzose sandstone, minor conglomerate, siltstone, shale.||||||
7197|Gilbert River Formation|60081|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|Includes the Yappar and Coffin Hll Members.  Quartzose sandstone, with minor conglomerate, siltstone, shale.||||||22-JUL-04
7197|Gilbert River Formation|60087|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|Includes the Coffin Hill and Yappar Members.  Quartzose sandstone, shale, siltstone, minor conglomerate.||||||
7197|Gilbert River Formation|60357|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|Includes: Coffin Hill Member, Yappar Member. Underlies: Wallumbilla Formation. Geological Province: Carpentaria Basin.||||||20-AUG-04
7197|Gilbert River Formation|60358|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|Clayey quartzose sandstone, conglomeritic sandstone, pebble and cobble conglomerate; muddy sandstone, glauconitic sandstone, mudstone and siltstone. Geological Province: Laura Basin.||||||18-AUG-04
7197|Gilbert River Formation|60359|5|Briefly described|Map Legend|Mesozoic|Mesozoic|Sandstone, grit, conglomerate, claystone.||||||
7197|Gilbert River Formation|60425|5|Briefly described|p70, p110|Early Cretaceous|Late Jurassic|Overlies Nychum Volcanics in the west. Geological province: Carpentaria Basin.||||||07-FEB-11
7197|Gilbert River Formation|62837|5|Briefly described|Stratigraphic columns|Barremian|Kimmeridgian|Includes Batavia, Glennie and Briscol Members, and Coffin Hill and Yappar Members.  Age: 140-~114Ma.  Geological Province: Northern Cape York, Southern Cape York and Burketown Depression.||||||01-MAR-10
7197|Gilbert River Formation|64665|5|Briefly described|p53 Fig.2, p62.|Early Cretaceous|Early Cretaceous|Laura Basin.||||Overlies Bathurst Range Coal Measures and Dalrymple Sandstone. Is overlain by Rolling Downs Group.||
7197|Gilbert River Formation|64707|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|Clayey quartz sandstone.||||||
7197|Gilbert River Formation|64820|5|Briefly described|pS6 Fig. 4|Neocomian|Neocomian|Of the Rolling Downs Group. Coarse-medium-grained quartz sandstone with minor siltstone and claystone. Geological province: Weipa Sub-basin, Carpentaria Basin.||||||
7197|Gilbert River Formation|64822|5|Briefly described|pS89|Early Cretaceous|Early Cretaceous|Geological province: Weipa Sub-basin, Carpentaria Basin.||||||02-FEB-09
7197|Gilbert River Formation|65755|5|Briefly described|p7 Fig.4||Jurassic|Conglomerate, sandstone, siltstone, claystone.||||||
7197|Gilbert River Formation|66529|6|Mentioned|p12 Fig.5 |||Carpentaria Basin.||||Is overlain by Rolling Downs Group.||
7197|Gilbert River Formation|66915|5|Briefly described|p6 Fig.3|Cretaceous|Cretaceous|Carpentaria Basin. See also misspelt Gilbert River Group in this paper.||||Is overlain by Wallumbilla Formation in Carpentaria and Laura Basins, at C-horizon boundary.||
7197|Gilbert River Formation|67323|5|Briefly described|p84-87, p94 Fig.12.4, p96, p106|Early Cretaceous|Late Jurassic|See also GIS attrib tbl, Solid Geology Map. Eromanga/Carpentaria Basins. Fluvial and lacustrine sediments. A regional aquifer.||||Is overlain by Wallumbilla Formation.|Clayey quartz sandstone, some sublabile and glauconitic sandstone; minor ferruginised shale; locally bioturbated.|
7197|Gilbert River Formation|67402|4|Described|p165 tbl LPB1, p176|Aptian|Tithonian|Carpentaria and Laura Basins. Deposited in a lagoonal to marginal marine setting. Forms an aquifer with generally good water quality across the Carpentaria Basin. Generally 300m thick. Formerly the Battle Camp Sandstone. See also p177, p179 fig CRP/KRM5, p180, p181, p226, p228-p233.|||Includes the Yappar Member and the Coffin Hill Member.|Unconformably overlies the Garraway Sandstone. Overlain by the Wallumbilla Formation and the Rolling Downs Group.|Very fine to coarse-grained quartz to sublabile sandstone with minor silstone and claystone.|
7197|Gilbert River Formation|67498|6|Mentioned|p925, p926 Fig.5, p929, 930, p932 Fig.10|Early Cretaceous|Late Jurassic|Also shown informally as 'Jurassic mesa'.|||||Includes sandstones.|08-MAY-12
7197|Gilbert River Formation|67784|5|Briefly described|p25, p26, p31, p33|Aptian|Neocomian|Northern Eromanga Basin. Littoral deposits.||Wilgunya Subgroup.||Overlain by Wallumbilla Formation|Sandstone|08-FEB-18
7197|Gilbert River Formation|67870|5|Briefly described|p46-47, p50-52|Late Cretaceous|Late Cretaceous|Potential hydrocarbon reservoir.|||||Sandstone (quartzite), conglomerate, organic-rich siltstone, shale.|
7197|Gilbert River Formation|68135|5|Briefly described|p52 fig 2b, p65|Early Cretaceous|Tithonian|Carpentaria and Laura Basins. Contains plant and invertebrate fossils. Lagoonal to marginal marine deposits.||||Overlies Dalrymple Sandstone, Garraway beds, Helby beds|Interbedded sandstone and siltstone.|14-SEP-17
7197|Gilbert River Formation|68337|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic?|Carpentaria Basin.|||||Reddish brown, medium- to coarse-grained, clayey, quartzose sandstone, pebbly sandstone; minor quartz pebble conglomerate, siltstone, fine-grained quartzose sandstone; ferruginised in places.|
7197|Gilbert River Formation|68341|5|Briefly described|Map legend.|Early Cretaceous|Middle Jurassic||||||Clayey quartz sandstone.|
7197|Gilbert River Formation|68345|5|Briefly described|Map legend.|Early Cretaceous|Late Jurassic|Carpentaria Basin.|||Includes Yappar and Coffin Hill Members.|Is overlain conformably by Wallumbilla Formation.|Clayey quartzose sandstone, some sublabile and glauconitic sandstone; minor ferruginised shale; locally bioturbated.|
7197|Gilbert River Formation|68349|5|Briefly described|Map legend.|Early Cretaceous|Late Jurassic|Carpentaria Basin.|||Includes Yappar and Coffin Hill Members.|Conformably overlies Eulo Queen Group. Is overlain conformably by Wallumbilla Formation.|Clayey quartzose sandstone, some sublabile and glauconitic sandstone; minor ferruginised shale; locally bioturbated.|
7197|Gilbert River Formation|68356|5|Briefly described|Map legend.|Early Cretaceous|Late Jurassic|Carpentaria Basin.|||Includes Yappar and Coffin Hill Members.||Clayey quartzose sandstone, some sublabile and glauconitic sandstone; minor feruginised shale; locally bioturbated.|
7197|Gilbert River Formation|68405|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|Carpentaria and Karumba Basins.|||Includes Coffin Hill and Yappar Members.|Unconformably overlain by Bulimba Formation.|Medium to coarse-grained, clayey quartzose sandstone and pebbly sandstone (commonly cross-bedded); minor quartz pebble conglomerate, siltstone, mudstone.|24-AUG-15
7197|Gilbert River Formation|68417|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|Carpentaria Basin. No outcrop in map area: shown only in subsurface and rock relationship diagram.  |||Includes Coffin Hill Member, Yappar Member.|Conformably overlain by the Wallumbilla Formation. Conformably underlain by the Loth Formation, Eulo Queen Group.|(Undifferentiated):clayey quartz sandstone, some sublabile and glauconitic sandstone; minor ferruginised shale; locally bioturbated.|
7197|Gilbert River Formation|68553|6|Mentioned|Map legend; schematic diagram.|Early Cretaceous|Jurassic|Eromanga, Carpentaria and Laura Basins. ||||||
7197|Gilbert River Formation|68821|6|Mentioned|p292 Fig.1|Cretaceous|Cretaceous|Lower Cretaceous age.||||||
7197|Gilbert River Formation|69056|5|Briefly described|p57, Reference images sheet.|Early Cretaceous|Late Jurassic|Carpentaria Basin. Shown on the simplified surface geology map of the Quamby Project area. Unconformably overlies the ~3km-thick Millungera Basin sequence.||||||
7197|Gilbert River Formation|69079|6|Mentioned|p16|||Mesozoic gold placer deposits in this unit have been reworked and concentrated in the Palmer River goldfield.||||||
7197|Gilbert River Formation|69297|5|Briefly described|p273, p274 fig 4. 3|Upper Cretaceous|Upper Jurassic|Carpentaria Basin. This unit is a good potential hydrocarbon reservoir. ||||Overlain by the Wallumbilla Formation. Overlies the Garraway Sandstone.|Quartzose sandstone and quartzose glauconitic sandstone.|
7197|Gilbert River Formation|69377|5|Briefly described|map legend|Early Cretaceous|Late Jurassic||||||Clayey quartz sandstone, some sublabile and glauconitic sandstone; minor ferruginised shale; locally bioturbated|
7197|Gilbert River Formation|69455|5|Briefly described|p39:2; 39:4 Fig.39.3; 39:14-15|||Offshore Western Gulf Sub-basin, Carpentaria Basin. Contains sandstones with good reservoir potential, sealed by Wallumbilla Formation equivalent shales. Also is a possible source rock.||||Overlies Eulo Queen Group.|Includes fluvial quartzic sandstones.|12-JUL-16
7197|Gilbert River Formation|69591|5|Briefly described|p99, p101|Early Cretaceous|Late Jurassic|Carpentaria Basin.||||Is overlain by Wallumbilla Formation.||
7197|Gilbert River Formation|69594|4|Described|p518, p520-522, p526-528, p540, p573|Barremian|Tithonian|Carpentaria, Laura and northern Eromanga Basins. Diachronous: deposition progressed southwards. 30-123m thick; 58-280m in the Laura Basin. Fluvial to marine deposition. One of the main aquifers in the Basin. RELATED UNITS (continued): Equivalent to Yappar and Coffin Hill Members; Helby beds (and interfingers with it); and (lower sandstone part of) Battle Camp Formation.|||Yappar and Coffin Hill Members.|Overlies Garraway and Dalrymple Sandstones conformably and Eulo Queen Group disconformably/unconformably. Is overlain conformably by Wallumbilla Formation (Rolling Downs Group). See COMMENTS.|Dominated by clayey quartzose sandstones, fining upwards into siltstone and glauconitic sandstone. In Laura Basin: fine to coarse, quartzose to sublabile sandstone, minor mudstone, siltstone and conglomerate.|
7197|Gilbert River Formation|69673|6|Mentioned|p202 fig 165|||||||Overlies Garraway Sandstone||
7197|Gilbert River Formation|70207|6|Mentioned|p14, p74|Early Cretaceous|Late Jurassic|Georgetown region.||||||
7197|Gilbert River Formation|70345|6|Mentioned|p3|Early Cretaceous|Late Jurassic|||||||
7197|Gilbert River Formation|70354|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic||||||Clayey quartz sandstone, some sublabile and glauconitic sandstone; minor ferruginised shale; locally bioturbated.|
7197|Gilbert River Formation|70356|5|Briefly described|Map legend.|Early Cretaceous|Late Jurassic||||||Clayey quartz sandstone, some sublabile and glauconitic sandstone; minor ferruginised shale; locally bioturbated.|
7197|Gilbert River Formation|70570|5|Briefly described|Map legend.|Early Cretaceous|Late Jurassic||||||Clayey quartz sandstone, some sublabile and glauconitic sandstone; minor ferruginised shale; locally bioturbated.|05-MAY-16
7197|Gilbert River Formation|70572|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic||||||Clayey quartz sandstone, some sublabile and glauconitic sandstone; minor ferruginised shale; locally bioturbated.|20-JAN-22
7197|Gilbert River Formation|70673|6|Mentioned|p7, p100|Early Cretaceous|Late Jurassic|Lakeland Downs-Maytown region.||||||
7197|Gilbert River Formation|71409|5|Briefly described|p1058-1059, p1061|Jurassic|Jurassic|Carpentaria Basin. Likely distal source rocks for heavy minerals in central-eastern Cape York Peninsula. Outcrops in the northern tip of the Cape York Peninsula.|||||Sandstones.|23-APR-18
7197|Gilbert River Formation|71792|4|Described|p57-p58|Early Cretaceous|Late Jurassic|Carpentaria Basin. |||||Clayey quartz sandstone, some sublabile and glauconitic sandstone; minor ferruginised shale; locally bioturbated.|
7197|Gilbert River Formation|71849|5|Briefly described|p8, p43, p49, p119, p133, p144, p195|Early Cretaceous|Late Jurassic|Forms the base of the Carpentaria Basin sequence.||||Nonconformably overlies Morris, Wolverton and Meldrum Granites and Rokeby Quartz Monzodiorite.|Sandstone.|
7197|Gilbert River Formation|71853|5|Briefly described|Map legend.|Early Cretaceous|Late Jurassic|The two facies are mapped separately.|||||Clayey quartz sandstone, some sublabile and glauconitic sandstone; minor ferruginised shale; locally bioturbated. Another facies has identical lithologies but deeply weathered.|
7197|Gilbert River Formation|71854|5|Briefly described|Map legend.|Early Cretaceous|Late Jurassic|The two facies are mapped separately.|||||Clayey quartz sandstone, some sublabile and glauconitic sandstone; minor ferruginised shale; locally bioturbated. Another facies has identical lithologies but is deeply weathered.|
7197|Gilbert River Formation|71863|5|Briefly described|p5|Aptian|Berriasian|Carpentaria Basin.||||Overlain by the Wallumbilla Formation.||
7197|Gilbert River Formation|72088|6|Mentioned|p25|||Forms part of The Pyramid rock formation.||||Overlies the Blantyre Sandstone.||
7197|Gilbert River Formation|72297|5|Briefly described|p746, p748, p761|||Carpentaria, Laura Basins. Potential source rocks: minor hydrocarbons reported in AAO Karumba 8 (oil staining and fluorescence). Excellent hydrocarbon reservoir potential because it contains aquifers. Temperatures in its aquifers highlight a broad heat anomaly through the Carpentaria and Eromanga Basins; potential for geothermal energy.||||Overlies Eulo Queen Group.|Includes interbedded fine carbonaceous sedimentary rocks (mudstones).|
7197|Gilbert River Formation|72298|5|Briefly described|p801|Cretaceous|Jurassic|Carpentaria Basin. Main confined aquifers, generally producing flowing artesian water bores.||||Overlies Loth FZ (Eulo Queen Group) and Garraway beds. Is overlain by Wallumbilla FZ (Rolling Downs Group).||
7197|Gilbert River Formation|72526|6|Mentioned|p6 Fig.1.2.|Jurassic|Jurassic|||||||
7197|Gilbert River Formation|72683|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|?Eromanga Basin or Carpentaria Basin?||||Unconformably overlies Wimberu Granite, Narpa Group, Mount Albert Group, Kuridala Group, Malbon Group.|Clayey quartz sandstone, some sublabile and glauconitic sand stone; minor ferruginised shale; locally bioturbated.|
7197|Gilbert River Formation|72889|6|Mentioned|p8.||||||||Includes calc-silicate dominated rocks.|
7197|Gilbert River Formation|72913|6|Mentioned|p8.|||Four wells intersected this cover unit.||||||
7197|Gilbert River Formation|72967|6|Mentioned|p5|||Carpenteria Basin.||Rolling Downs Group||||
7197|Gilbert River Formation|72983|6|Mentioned|p15|Early Cretaceous|Late Jurassic|||||||
7197|Gilbert River Formation|73083|6|Mentioned|p57, p60-62, p77|Cretaceous|Jurassic||||||Includes fossiliferous sandstone and conglomerate.|
7197|Gilbert River Formation|73137|6|Mentioned|p6|Early Cretaceous|Jurassic|||||||
7197|Gilbert River Formation|73144|6|Mentioned|p8, p13|Cretaceous|Cretaceous|Carpentaria Basin. Aquifer with potential tight gas/oil. Basal unconformity.||||Overlain by Wallumbilla Formation (Rolling Downs Group).||14-OCT-22
7197|Gilbert River Formation|73147|5|Briefly described|p126-127, 129-131, 138, 141, 143-144|Aptian|Aptian|Gregory Range area, SE Carpentaria Basin.|||Yappar Member|Overlies Eulo Queen Group.||
7197|Gilbert River Formation|73472|6|Mentioned|p114|Cretaceous|Cretaceous|||||||
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.|
7242|Gilruth Volcanic Member|9534|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Kombolgie Formation (Katherine River Group).  Amygdaloidal basalt, tuff, tuffaceous siltstone, banded jasper rubble.||||||
7242|Gilruth Volcanic Member|9691|5|Briefly described|Map Legend|||Of the Kombolgie Formation. Amygdaloidal basalt, tuff, tuffaceous siltstone, banded jasperite rubble.||||||
7242|Gilruth Volcanic Member|9701|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Kombolgie Formation. Amygdaloidal basalt, tuff, tuffaceous siltstone, banded jasperite rubble.||||||02-JUN-05
7242|Gilruth Volcanic Member|9733|5|Briefly described|Map Legend|Carpentarian|Carpentarian|Of the Kombolgie Formation. Amygdaloidal basalt, tuff, tuffaceous siltstone, banded jasperite rubble.||||||
7242|Gilruth Volcanic Member|22538|6|Mentioned|Fig3 P708|||||||||
7242|Gilruth Volcanic Member|22548|5|Briefly described|p139|||||||||
7242|Gilruth Volcanic Member|23216|5|Briefly described|Table1p9,20,22|||||||||
7242|Gilruth Volcanic Member|23374|3|Fully described|Tb2p10,14,15,16,42,26||Statherian|At top of Gumarrirnbang Sandstone. Probably equivalent to Henwood Creek Volcanic Member. Geological Province: McArthur Basin.||||||19-SEP-06
7242|Gilruth Volcanic Member|23384|6|Mentioned|Fig 27|||||||||
7242|Gilruth Volcanic Member|23733|5|Briefly described|p32 Fig. 19|||||||||
7242|Gilruth Volcanic Member|23867|3|Fully described|p6|Paleoproterozoic|Paleoproterozoic|Of Gumarrirnbang Sandstone.  Weathered and altered mafic lavas.  Max. thickness: 15m.  Geological Province: McArthur Basin.  See also Table 1 and Figs. 3 and 30.||||||07-NOV-08
7242|Gilruth Volcanic Member|24050|4|Described|p13, p10|||Of the Gumarrirnbang Sandstone.  Basalt or tuff.||||||19-SEP-06
7242|Gilruth Volcanic Member|24051|5|Briefly described|Map Legend|Statherian|Statherian|Of Gumarrirnbang Sandstone, Kombolgie Subgroup. Geological Province: McArthur Basin.||||||
7242|Gilruth Volcanic Member|32394|5|Briefly described|p287|||Mention p289.||||||19-SEP-06
7242|Gilruth Volcanic Member|33186|4|Described|p293|||||||||
7242|Gilruth Volcanic Member|36085|6|Mentioned|p495|||||||||
7242|Gilruth Volcanic Member|36535|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
7242|Gilruth Volcanic Member|36635|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
7242|Gilruth Volcanic Member|37815|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
7242|Gilruth Volcanic Member|38884|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
7242|Gilruth Volcanic Member|39679|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
7242|Gilruth Volcanic Member|40248|6|Mentioned|p226|||||||||
7242|Gilruth Volcanic Member|43149|5|Briefly described|Map Legend||Paleoproterozoic|Of Kombolgie Formation. Of Statherian age.||||||07-NOV-08
7242|Gilruth Volcanic Member|46639|5|Briefly described|Map legend||Paleoproterozoic|Of the Kombolgie Formation. Uderlain by Kombolgie Formation. Amydaloidal basalt tuff, tuffaceous siltstone, banded jasperite rubble.||||||07-NOV-08
7242|Gilruth Volcanic Member|46700|5|Briefly described|P29, Table1 P8||Carpentarian|||||||
7242|Gilruth Volcanic Member|47049|6|Mentioned|p237|||||||||
7242|Gilruth Volcanic Member|48962|6|Mentioned|Fig.15|||||||||
7242|Gilruth Volcanic Member|60550|5|Briefly described|Map Legend|Carpentarian|Carpentarian|Of the Kombolgie Formation. Amygdaloidal basalt, tuff, tuffaceous siltstone, banded jasperite rubble.||||||
7242|Gilruth Volcanic Member|60571|5|Briefly described|Map legend|Statherian|Statherian|Of the Gumarrirnbang Sandstone (Kombolgie Subgroup, Katherine River Group). Ferruginous laterite and saprolite (possibly after volcanic rocks) or corresponding level above surface with dune structures. Geological Province: McArthur Basin.||||||30-NOV-04
7242|Gilruth Volcanic Member|60680|5|Briefly described|Map legend|Statherian|Statherian|Of the Gumarriirnbang Sandstone (Kombolgie Subgroup, Katherine River Group).  Highly ferruginised and weathered basalt. Geol.Prov: McArthur Basin.||||||23-DEC-09
7242|Gilruth Volcanic Member|64698|4|Described|lithinterp table|Statherian|Statherian|Age ~1750-1800Ma. McArthur Basin. Of Gumarrirnbang Sandstone, Katherine River Group. Max thickness 14m. Highly ferruginised and weathered basalt.||||||07-JAN-09
7242|Gilruth Volcanic Member|64817|6|Mentioned|p353 Fig.4, |||||Of the Kombolgie Subgroup.||||
7242|Gilruth Volcanic Member|65232|5|Briefly described|p7 Fig. 6|||Of ? (Kombolgie Subgroup, Katherine River Group). Underlies Marlgowa Sandstone; overlies misspelt Gumarrinbang Sandstone - parent/constituent relationship is unclear in paper. See also Gilruth Volcanics.||||||09-FEB-10
7242|Gilruth Volcanic Member|67564|4|Described|p6 Table 2, p39 Fig.20, pp42-43.|Paleoproterozoic|Paleoproterozoic|Forms a low scarp that often caps a broad bench of underlying Gumarrirnbang Sandstone. 14 m thick. Subaerial flows over fluviatile sediments. Has a narrow, high-U radiometric signature.||Unit in Gumarrirnbang Sandstone.|||Highly ferruginised and weathered, porphyritic and vesicular basalt.|
7242|Gilruth Volcanic Member|67779|5|Briefly described|p6 Fig.5, p8 Table 1, p32, pp36-38.|Paleoproterozoic|Paleoproterozoic|McArthur Basin. A thin bench, 5-15 m thick. Intensely weathered, soil-covered. Equivalent to Henwood Creek Volcanic Member. Has distinct, narrow and high U and Th radiometric responses.||Unit in Gumarrirnbang Sandstone.||Conformably overlies Gumarrirnbang Sandstone. Is overlain by Marlgowa Sandstone disconformably.|Amygdaloidal basalt, tuff, tuffaceous siltstone, banded jasper rubble.|14-MAY-18
7242|Gilruth Volcanic Member|69430|5|Briefly described|p15:3, 7-8, 51|||NW McArthur Basin. 5m thick. Assumed to be subaerial. Corresponds to a distinct, narrow, high U and Th pattern on the radiometric image. Age range ~1820 - 1729 Ma from Edith RIver Group (underlying  the whole Kombolgie Subgroup) and the intrusive Oenpelli Dolerite.||Gumarrirnbang Sandstone.|||A thin band of tuffaceous siltstone, tuff, minor banded quartz-jasper, and amygdaloidal and vesicular basalt.|22-SEP-18
7242|Gilruth Volcanic Member|69673|6|Mentioned|p16 fig 13|||Northwestern McArthur Basin.||Kombolgie Subgroup||Overlain by Marlgowa Sandstone, overlies Gumarrirnbang Sandstone||
7387|Glendower Formation|23493|6|Mentioned|p16 Tb. 1|Pliocene|Pliocene|Of Whitehouse (1954).  Correlated with Lynd Formation.  On HUGHENDEN Sheet.||||||
7387|Glendower Formation|23982|6|Mentioned|p96 Appendix 13|||Geological Province: Great Artesian Basin.||||||
7387|Glendower Formation|24013|5|Briefly described|p17 Tb. 1|Tertiary|Tertiary|Correlated with the Lynd Formation.||||||
7387|Glendower Formation|29660|6|Mentioned|p7|||||||||
7387|Glendower Formation|30103|5|Briefly described|p9|||Table 3 on p9. Early Tertiary age.||||||31-AUG-20
7387|Glendower Formation|30104|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7387|Glendower Formation|30853|5|Briefly described|Table 3|||Tertiary||||||
7387|Glendower Formation|30855|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7387|Glendower Formation|30856|4|Described|Table 4|||See p12. Tertiary.||||||31-AUG-20
7387|Glendower Formation|30857|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7387|Glendower Formation|31144|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7387|Glendower Formation|31145|5|Briefly described|Table 1|||Tertiary.||||||
7387|Glendower Formation|31430|5|Briefly described|Table 1|||Tertiary||||||
7387|Glendower Formation|31431|5|Briefly described|Table 3|||L.Cretaceous||||||
7387|Glendower Formation|31432|4|Described|Table 1|||Tertiary||||||
7387|Glendower Formation|31436|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7387|Glendower Formation|31438|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7387|Glendower Formation|31441|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7387|Glendower Formation|31443|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7387|Glendower Formation|31553|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7387|Glendower Formation|32553|4|Described|p38|||||||||
7387|Glendower Formation|33067|4|Described|Table 1|Tertiary|Tertiary|Quartz sandstone, sandy conglomerate, minor siltstone, silcrete.||||||07-JUL-04
7387|Glendower Formation|33069|4|Described|p7|||Tertiary||||||
7387|Glendower Formation|33072|4|Described|Table 1|||Tertiary||||||
7387|Glendower Formation|33074|6|Mentioned|p262|||||||||
7387|Glendower Formation|33078|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7387|Glendower Formation|33079|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7387|Glendower Formation|33081|6|Mentioned|p26|||||||||
7387|Glendower Formation|33082|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7387|Glendower Formation|33083|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7387|Glendower Formation|33086|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7387|Glendower Formation|33087|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7387|Glendower Formation|33088|4|Described|Table 4|||Tertiary||||||
7387|Glendower Formation|33089|4|Described|Table 2|||Tertiary||||||
7387|Glendower Formation|33092|5|Briefly described|p9|||Stratigraphy||||||
7387|Glendower Formation|33095|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7387|Glendower Formation|33150|5|Briefly described|p13|||Possible equiv. Floraville & Bulimba Fms.||||||
7387|Glendower Formation|33182|6|Mentioned|p193|||||||||
7387|Glendower Formation|33449|4|Described|Table 1|||Tertiary||||||
7387|Glendower Formation|33639|5|Briefly described|Table 2|||Tertiary.||||||
7387|Glendower Formation|33640|4|Described|Table 2|||Tertiary||||||
7387|Glendower Formation|33644|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7387|Glendower Formation|33647|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7387|Glendower Formation|33648|6|Mentioned|p21|||Stratigraphy.||||||
7387|Glendower Formation|33938|6|Mentioned|p48|||Refers Whitehouse (1954).||||||
7387|Glendower Formation|34065|4|Described|p6|||||||||
7387|Glendower Formation|34091|5|Briefly described|Table 1|||Tertiary. See also P9||||||
7387|Glendower Formation|34217|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7387|Glendower Formation|34218|4|Described|p11|||See also pp12,14,17, Table 1. Tertiary.||||||31-AUG-20
7387|Glendower Formation|34485|4|Described|Table 1|||Tertiary||||||
7387|Glendower Formation|34486|4|Described|Table 1|||Tertiary||||||
7387|Glendower Formation|34487|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7387|Glendower Formation|34948|6|Mentioned|p317|||||||||
7387|Glendower Formation|35187|6|Mentioned|Table1|||||||||
7387|Glendower Formation|35322|6|Mentioned|p418|||||||||
7387|Glendower Formation|36966|6|Mentioned|p92|||||||||
7387|Glendower Formation|37607|4|Described|p333|||See also Fig.4.||||||
7387|Glendower Formation|39322|6|Mentioned|Fig.3|||||||||
7387|Glendower Formation|39445|5|Briefly described|Table 14|||||||||
7387|Glendower Formation|40584|6|Mentioned|p435|||||||||
7387|Glendower Formation|40675|6|Mentioned|Table 8A|||||||||
7387|Glendower Formation|41710|6|Mentioned|p222|||||||||
7387|Glendower Formation|42084|6|Mentioned|Fig.3 P356|||||||||
7387|Glendower Formation|42447|6|Mentioned|Fig.10|||||||||
7387|Glendower Formation|42999|6|Mentioned|p98|||||||||
7387|Glendower Formation|43008|5|Briefly described|map legend|||||||||
7387|Glendower Formation|43995|14|Not recorded|Tb.p9||Tertiary|||||||
7387|Glendower Formation|44016|14|Not recorded|Map Legend||Tertiary|||||||
7387|Glendower Formation|44017|14|Not recorded|Map Legend||Tertiary|||||||
7387|Glendower Formation|44018|14|Not recorded|Map Legend||Tertiary|||||||
7387|Glendower Formation|44019|14|Not recorded|Map Legend||Tertiary|||||||
7387|Glendower Formation|44020|14|Not recorded|p8,11,14-5,Tb.1,Fig2||Tertiary|||||||
7387|Glendower Formation|44042|14|Not recorded|Map Legend||Tertiary|||||||
7387|Glendower Formation|44067|14|Not recorded|Map Legend||Tertiary|||||||
7387|Glendower Formation|44089|4|Described|Tb.1,p6,8,map||Tertiary|||||||
7387|Glendower Formation|44091|14|Not recorded|p65||Tertiary|||||||
7387|Glendower Formation|44098|14|Not recorded|p98||Tertiary|||||||
7387|Glendower Formation|44099|14|Not recorded|Map Legend||Tertiary|||||||
7387|Glendower Formation|44123|14|Not recorded|p388-390|||||||||
7387|Glendower Formation|44133|5|Briefly described|p190 Fig. 10.30|Late Eocene|Late Paleocene|Geological Province: Waite Basin.||||||
7387|Glendower Formation|44251|14|Not recorded|p4||Pliocene|Correlated with Lynd Formation. Ref. to Laing and Power 1959.||||||
7387|Glendower Formation|44252|14|Not recorded|p397|||||||||
7387|Glendower Formation|44269|14|Not recorded|p17,18||Cenozoic|||||||19-NOV-08
7387|Glendower Formation|44295|14|Not recorded|p6||Pliocene|||||||
7387|Glendower Formation|44373|14|Not recorded|p20|||Map only.||||||
7387|Glendower Formation|44377|14|Not recorded|p19|||See also Lexicon.||||||
7387|Glendower Formation|44587|14|Not recorded|p376,,381|||Boulders of 'billy'.||||||
7387|Glendower Formation|44800|4|Described|p16,18,53,map||Tertiary|(Early Tertiary)||||||
7387|Glendower Formation|45009|14|Not recorded|p73||Pliocene|||||||
7387|Glendower Formation|45110|5|Briefly described|p129|||||||||
7387|Glendower Formation|45145|6|Mentioned|Table 7|||||||||
7387|Glendower Formation|46802|6|Mentioned|p136|||||||||
7387|Glendower Formation|46902|6|Mentioned|Table 1|||Correlation chart for Cainozoic land-surfaces||||||
7387|Glendower Formation|48908|14|Not recorded|Tb.1||Tertiary|||||||
7387|Glendower Formation|49011|6|Mentioned|p28|||||||||
7387|Glendower Formation|60080|5|Briefly described|Map legend|Oligocene|Paleocene|Quartzose sandstone, sandy conglomerate with quartz, agate and chert clasts, minor siltstone; silcrete. Overlies Winton Formation; underlies Whitula Formation.||||||16-SEP-08
7387|Glendower Formation|61155|5|Briefly described|p17|Middle Eocene|Late Paleocene|Sediments spread in thin sheets over large areas of the Birdsville Basin. Max. thickness: 70m. See also p2, p3.||||||03-MAR-10
7387|Glendower Formation|61312|5|Briefly described|p66|Tertiary|Tertiary|Quartzose, arenaceous and conglomeratic fluviatile deposits. Found particularly in the Milparinka-Tibooburra district. Geological Provnce: Eromanga Basin.||||||
7387|Glendower Formation|63979|5|Briefly described|p55|Tertiary|Tertiary|Overlies the Winton Formation. Geological province: Eromanga Basin.||||||07-FEB-11
7387|Glendower Formation|64047|2|Defined|p60-61||Middle Eocene|Unconformable on Winton Fm; overlain by Whitula Fm. Max. thickness: 145m. Geol.prov: Eromanga Basin. Contains quartzose sandstone, quartz pebble conglomerate, sandy conglomerate and minor siltstone ans mudstone;  reworked clasts of Winton Fm. at base..||||||16-APR-08
7387|Glendower Formation|66131|5|Briefly described|p240, p242 Fig.2|Eocene|Paleocene|Late Paleocene to Late Eocene in age (from p.242 Fig.2 - stratigraphic correlation chart).||||Correlative of the Eyre Formation.||
7387|Glendower Formation|66623|6|Mentioned|p273.|||Lateral equivalent of Eyre Formation.||||||
7387|Glendower Formation|67561|6|Mentioned|p54, p56||||||||Comprises quartzose sandstone, quartz pebble conglomerate, sandy conglomerate and minor siltstone and mudstone.|
7387|Glendower Formation|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as Oxley and Booval Groups; Petrie, Biloela, Bulimba, Duaringa, Emerald, Exevale, Floraville, Louisa, Lowmead, Marion, Red Mountain, Southern Cross, Springvale and Suttor Formations; Beaudesert, Casuarina, Nagoorin, Old Cork, Rossmoya, Takura and Water Park Creek beds; Fairview Gravel; Moses and Oakdale Sandstones, and unnamed units, are all mapped under the symbol, Tl.||||||
7387|Glendower Formation|68901|5|Briefly described|p7 Fig. ii|Quaternary|Paleogene||||||Quartzose sandstone, conglomerate; commonly silcretised.|26-SEP-18
7387|Glendower Formation|69599|5|Briefly described|p580, p584, p599-600, p650|Eocene|Paleocene|Lake Eyre Basin. Formerly the Glendower Series. Now applies to all similar sedimentary packages covering the Eromanga Basin. Semicontinuous belt from E of Hughenden to near Longreach. Up to 170m thick. Fluvial valley fill sediments. No known fossils. Capped by silcrete and laterite of the Featherby Surface. RELATED UNITS (continued): Also correlated (at least partly) with Eyre, Moonie, Edkins, Springvale and Marion Formations; Werite and Old Cork beds; Mueller and Moses Sandstones.||||Unconformably overlies Winton Formation. Is overlain by Whitula Formation and, locally, by Sturgeon Basalt. See COMMENTS for more.|Quartz sandstone, pebble conglomerate, sandy conglomerate and sudordinate siltstone and mudstone. Upper parts are heavily silcretised in most areas.|
7387|Glendower Formation|69952|5|Briefly described|p16|Paleogene|Paleogene||||||Quartzose sandstone, conglomerate; commonly silcretised.|
7387|Glendower Formation|70720|6|Mentioned|p6|||||||Overlies Winton Formation.||
7387|Glendower Formation|70821|5|Briefly described|p15, p25-26, p33, p80, p82, p86,p115-116|Eocene|Eocene|Originally the Glendower Series of Bryan and Jones (1946); [misquoted in this study as the Glendower series]. Lake Eyre Basin (NSW and QLD). Forms a series of dendritic silcrete ridges, equivalent to the Eyre Formation in SA. Highly resistive. Forms slope deposits of scree or colluvium of gravel to boulder-sized fragments. 52m thick in Mirintu 1 petroleum well. Hydrostratigraphic properties.||||Unconformably overlies Winton Formation. Equivalent to Eyre Formation.|Silcreted and inverted palaeochannels of sandstone and conglomerate.|
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|
7486|Gold Creek Volcanics|22432|5|Briefly described|p21,22, Fig.23|||McArthur Basin.||||||20-SEP-06
7486|Gold Creek Volcanics|22538|6|Mentioned|App1 P722|||||||||
7486|Gold Creek Volcanics|22644|5|Briefly described|5 fig 2|||Geol province McArthur Basin. Overlain by McArthur Group; underlain by Wollogorang Formation. Creek as 'Ck' in text||||||20-SEP-06
7486|Gold Creek Volcanics|22670|6|Mentioned|53|||Geol province McArthur Basin||||||
7486|Gold Creek Volcanics|22853|3|Fully described|13|Proterozoic|Proterozoic|Geol province: McArthur Basin. Of Tawallah Group. Underain by Wollogorang Formation.||||||20-SEP-06
7486|Gold Creek Volcanics|23216|6|Mentioned|p24|||||||||
7486|Gold Creek Volcanics|23363|5|Briefly described|344 Fig.3|||||||||
7486|Gold Creek Volcanics|23395|5|Briefly described|p389|||||||||
7486|Gold Creek Volcanics|23396|5|Briefly described|p407 Fig.2|||Of Tawallah Group.||||||20-SEP-06
7486|Gold Creek Volcanics|23397|6|Mentioned|p480|||||||||
7486|Gold Creek Volcanics|23398|6|Mentioned|p437|||||||||
7486|Gold Creek Volcanics|23733|5|Briefly described|p32 Fig. 19|||||||||
7486|Gold Creek Volcanics|23776|5|Briefly described|p705 Fig 2.|||Of Tawallah Group.||||||
7486|Gold Creek Volcanics|23867|5|Briefly described|Fig. 30|||Of Tawallah Group.  Correlates with Diamond Creek Volcanics (Katherine River Group).  Geological Province: McArthur Basin.||||||
7486|Gold Creek Volcanics|23961|6|Mentioned|p1193 Fig. 4|||Geological Province: Mt Isa Inlier.||||||
7486|Gold Creek Volcanics|23963|4|Described|p1237, 1240|||Geological Province: McArthur Basin. Overlies the Settlement Creek Volcanics. Max. Thickness: 180m.||||||22-FEB-08
7486|Gold Creek Volcanics|23968|6|Mentioned|p1362|||Geological Province: McArthur Basin.||||||
7486|Gold Creek Volcanics|24050|6|Mentioned|p27|||||||||
7486|Gold Creek Volcanics|24179|5|Briefly described|p84 Fig. 2|||Overlies the Wollogorang Formation.  Overlain by the Tanumbirini Rhyolite.  Geological Province:  McArthur Basin.||||||
7486|Gold Creek Volcanics|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Of Upper Tawallah Group. Geological Province: Southern McArthur Basin.||||||
7486|Gold Creek Volcanics|26310|4|Described|p8, Table 1|Proterozoic|Proterozoic|Porphyritic acidic to intermediate lavas, interbedded sediments. Maximum Thickness: 300 feet. Overlies: Constance Sandstone.||||||
7486|Gold Creek Volcanics|32519|4|Described|Table 1|||||||||
7486|Gold Creek Volcanics|32904|6|Mentioned|p89|||||||||
7486|Gold Creek Volcanics|36012|6|Mentioned|Table 2|||||||||
7486|Gold Creek Volcanics|37670|6|Mentioned|p71|||||||||
7486|Gold Creek Volcanics|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
7486|Gold Creek Volcanics|40109|6|Mentioned|Fig.2|||||||||
7486|Gold Creek Volcanics|40259|6|Mentioned|Table 1|||||||||
7486|Gold Creek Volcanics|40489|6|Mentioned|p89|||||||||
7486|Gold Creek Volcanics|40691|5|Briefly described|p11|||Briefly described p19.||||||20-SEP-06
7486|Gold Creek Volcanics|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
7486|Gold Creek Volcanics|41406|6|Mentioned|Map legend|Mesoproterozoic||||||||
7486|Gold Creek Volcanics|41721|3|Fully described|p24|||Of the Tawallah Group. Conformably overlain by Hobblechain Rhyolite. Thickness: 180m. Trachyte, latite, tuff and sandstone. Geological province: McArthur Basin.||||||01-AUG-07
7486|Gold Creek Volcanics|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
7486|Gold Creek Volcanics|42385|4|Described|p13, p8 Fig. 5, p9 Tb. 3|Mesoproterozoic|Mesoproterozoic|Of Tawallah Group. Conformable on Wollogorang Formation.Thickness: <180m. Amydaloidal vesicular basaltic lavas, basaltic-dolerite sills and dykes, very fine- to medium-grained. Parts now mapped in with Settlement Creek Volcanics.||||||18-SEP-07
7486|Gold Creek Volcanics|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
7486|Gold Creek Volcanics|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.||Of Tawallah Group.||Not shown in schematic sections.|Basaltic lavas; basaltic-doleritic sills and dykes; feldspathic-micaceous sandstone; hyaloclastic breccia (peperite); rhyolitic lavas. Detailed lithology given.|09-NOV-11
7486|Gold Creek Volcanics|42639|4|Described|p15|||||||||
7486|Gold Creek Volcanics|42739|5|Briefly described|map legend|Statherian|Statherian|Of the Tawallah Group. Amygdaloidal basalt lava; dolerite dykes and sills; minor intercalated medium grained sandstone; hyaloclastic breccia with basalt blocks in sandy matrix.||||||19-OCT-05
7486|Gold Creek Volcanics|42812|3|Fully described|p24, Table 3|||Of Tawallah Group.||||||20-SEP-06
7486|Gold Creek Volcanics|42873|4|Described|p109|||see also Fig.1, P110||||||
7486|Gold Creek Volcanics|43010|5|Briefly described|Fig.6||Mesoproterozoic|Of Tawallah Group. Of "Mid Proterozoic" age.||||||20-SEP-06
7486|Gold Creek Volcanics|43036|5|Briefly described|p33|||||||||
7486|Gold Creek Volcanics|43715|6|Mentioned|p27|||||||||
7486|Gold Creek Volcanics|43788|6|Mentioned|p14|||||||||
7486|Gold Creek Volcanics|44271|14|Not recorded|p44|||||||||
7486|Gold Creek Volcanics|44272|14|Not recorded|Map Legend||Neoproterozoic|||||||
7486|Gold Creek Volcanics|44275|14|Not recorded|Map Legend|||||||||
7486|Gold Creek Volcanics|44280|14|Not recorded|p6,7,Tb.1,map|||||||||
7486|Gold Creek Volcanics|44287|14|Not recorded|p.8|||(E53-3).||||||
7486|Gold Creek Volcanics|44436|5|Briefly described|p.12|||(E53-4).||||||02-DEC-04
7486|Gold Creek Volcanics|44989|14|Not recorded|Tb.II||Neoproterozoic|Tb.II. Overlies Mullera Formation. Upper Proterozoic.||||||
7486|Gold Creek Volcanics|45162|3|Fully described|p41|||||||||22-FEB-18
7486|Gold Creek Volcanics|45287|14|Not recorded|p.223,226||Neoproterozoic|||||||
7486|Gold Creek Volcanics|60483|5|Briefly described|p7 Fig. 5, p29|||Of the Tawallah Group. Geological Province: McArthur Basin.||||||05-OCT-07
7486|Gold Creek Volcanics|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Tawallah Group. Overlain by Warramana Sandstone and Masterton Sandstone, underlain by Wollogorang Formation.||||||
7486|Gold Creek Volcanics|60574|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Tawallah Group. Interbedded with and overlies the Wollogorang Formation. Overlain by the Pungalina Member. Intruded by the Packsaddle Microgranite. Grey to red, vesicular to massive basalt; dolomitic sandstone, mudstone and peperite||||||07-NOV-08
7486|Gold Creek Volcanics|63110|6|Mentioned|p1141, p1141 Fig. 17|Statherian|Statherian|Of Tawallah Group. Shows extensive orthoclase-hematite alteration and base metal depletion. Geological Province: Calvert Superbasin.||||||11-JUN-08
7486|Gold Creek Volcanics|63112|6|Mentioned|p1189, p1192-1198, p1201, p1203-1206|||Calvert Superbasin. Framework grain dissolution after burial produced secondary porosity, allowing movement of basinal brines similar to those reported from Pb-Zn and U deposits of southern McArthur Basin. Age approximated from Fig.2. 15-230 m thick. |c.1725 Ma.|Unit in Big Supersequence.||Overlies Wollogorang Formation.|Seven 10- to 35m-thick vesicular basalt and fine-grained dolerite sheets divided by sandstone interbeds (proximal fluvial facies: poorly sorted and immature, coarse- to fine-grained).|
7486|Gold Creek Volcanics|64250|6|Mentioned|p25 fig 10|||Southern McArthur Basin.||Unit in Tawallah Group.||||
7486|Gold Creek Volcanics|64815|6|Mentioned|p4 Fig.2, p5 Fig.3, p16  |||Appears as GCV in Fig.2. Often missing in stratigraphic successions.||Of the Tawallah Group.||||
7486|Gold Creek Volcanics|64817|6|Mentioned|p353 Fig.4, p355 Fig.5, p367 Tb.2, p370 |||||Of the Tawallah Group.|||Basalt flows.|
7486|Gold Creek Volcanics|65228|5|Briefly described|p22, p25, Figs.02, 05, 06, 07, 10, 12.|Statherian|Statherian|Southern McArthur Basin. Felsic.|1723 +/- 4 Ma (Page et al. 2000).|Unit in Tawallah Group.||Overlies Wollogorang Formation. Is overlain by Warramana Sandstone, Pungalina Member (Echo Sandstone) and Hobblechain Rhyolite.||
7486|Gold Creek Volcanics|65337|6|Mentioned|p13.|||Southern McArthur Basin.||||||
7486|Gold Creek Volcanics|65340|3|Fully described|p12 Fig.6, pp25-38, pp68-78, p93. |||Wearyan Shelf. The upper flow unit in this formation is an interpreted extrusive correlative of the Settlement Creek Dolerite. Lithologies, conditions of deposition/emplacement, correlation are discussed in detail. Intertidal to supratidal hypersaline lake or restricted marine depositional environment; sequential emplacement of shallow basalt-peperite sills and flows into wet sediments; local fluidisation. Correlated with Diamond Creek Volcanics to the north, and Peters Creek Volcanics on the Lawn Hill Platform, and temporally with Settlement Creek Dolerite. Produces a high-frequency magnetic response beneath Mesozoic and Cenozoic cover. Hosts a number of Cu(-Co-Ni) stratabound and breccia pipe deposits, eg at Running Creek.||Unit in Tawallah Group.||Overlies Wollogorang Formation. Is intruded by Packsaddle Microgranite. Is overlain by Lower Pungalina Member and Hobblechain Rhyolite.|Grey to red, vesicular to massive, aphyric and locally porphyritic basalt; dolomitic to quartzose sandstone; mudstone; peperite breccia; local auotobreccia and massive sand bodies; local chlorite-bitumen alteration and sulfides.|
7486|Gold Creek Volcanics|67144|5|Briefly described|Map legend.|Statherian|Statherian|Recessive. ||Unit in Tawallah Group.||Overlies Wollogorang Formation.|Amygdaloidal vesicular basaltic lavas; dolerite sills and dykes; hyaloclastic breccia with basalt blocks in fine sandy matrix; very fine- to medium-grained feldspathic-micaceous sandstone; autoclastic flow-banded rhyolitic lavas.|
7486|Gold Creek Volcanics|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map; p34|Paleoproterozoic|Paleoproterozoic|See also Eastern Australia Time-Space Plot. McArthur Basin, Calvert Superbasin.|Erupted ~1730-1720 Ma.|Of Tawallah Group.|||Trachyte and latite flows, basalt; tuff; tuffaceous and lithic siltstone; siltstone.|
7486|Gold Creek Volcanics|67352|4|Described|p14 Tb.2|Statherian|Statherian|McArthur Basin. 225 m thick. Subaerial extrusive (quiet to explosive), shallow sills; terrestrial sediments.||Tawallah Group||Overlies Wollogorang Formation conformably. Intruded by Packsaddle Microgranite. Is overlain unconformably by Masterton Sandstone.|Basic to intermediate lavas, volcanic interbeds: trachyte or trachyandesite lava: vesicular, amygdaloidal, saussuritic, uralitic; agglomerate, tuff, dolerite, microsyenite, rhyolite; tuffaceous and lithic sandstone and siltstone.|
7486|Gold Creek Volcanics|69418|5|Briefly described|p3:11, 15, 29|||McArthur Basin. Hosts breccia pipe Cu(-Co-Ni) deposits, eg Redbank field (described).||||Overlies Wollogorang Formation.||12-JUL-16
7486|Gold Creek Volcanics|69430|4|Described|p15:3, 10-12, 44-48|Paleoproterozoic|Paleoproterozoic|Batten Fault Zone and SE McArthur Basin. 15-230m thick. Intertidal to supratidal hypersaline lake, or restricted marine, deposits. Hosts numerous Cu-bearing breccia pipes in the Redbank area (described in detail). Is intruded by Packsaddle Microgranite.||Tawallah Group.||Conformably overlies Wollogorang Formation. Is overlain by Pungalina Member (Warramana Sandstone) conformably to disconformably, and by Hobblechain Rhyolite and Echo Sandstone disconformably.|Porphyritic basalt; dolomitic to quartzic sandstone, mudstone, peperite breccia, local autobreccia, local stratiform polymict breccia and massive sandstone bodies, local chlorite-bitumen alteration and sulfides.|12-JUL-16
7486|Gold Creek Volcanics|69591|5|Briefly described|p56|||Camooweal-Murphy Domain, Mount Isa Province. Part of Tawallah Supersequence. Subaerial, local fluvial deposits.||Tawallah Group.|||Trachyte and latite flows, basalt; tuff, tuffaceous and lithic siltstone; siltstone.|
7486|Gold Creek Volcanics|69673|6|Mentioned|p16 fig 13, p17 fig 14|||||Tawallah Group||Overlain by Warramana Sandstone, Pungalina Member, Hobblechain Rhyolite, conformably overlies Wollogorang Formation|Basalt.|
7486|Gold Creek Volcanics|70849|5|Briefly described|Map legend.|Statherian|Statherian|McArthur Basin.||Tawallah Group.||Overlies Wollogorang Formation. Is overlain by Hobblechain Rhyolite.|Trachyte and latite flows, tuff, tuffaceous and lithic sandstone, siltstone.|
7486|Gold Creek Volcanics|71374|6|Mentioned|p6|||McArthur Basin.||Tawallah Group||Unconformably overlain by the Masterton Sandstone.||
7486|Gold Creek Volcanics|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown to be located in the Batten Fault Zone and the Southeastern McArthur Basin of the Southern McArthur Basin.||Tawallah Group||Partially overlies Wollogorang Formation and underlies Warramana Sandstone, Pungalina Member and Hobblechain Rhyolite.||
7486|Gold Creek Volcanics|72718|6|Mentioned|p7|||Southern McArthur Basin.||Tawallah Group||Underlain by Wollogorang Foramtion. Partly overlain by and equivalent to Warramana Sandstone. Partly overlain by Pungalina Member, Hobblechain Rhyolite, Packsaddle Microgranite.||
7486|Gold Creek Volcanics|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Batten Fault Zone and the Southeastern McArthur Basin of the Southern McArthur Basin.||Tawallah Group||Overlies Wollogorang Formation and is partially equivalent to and underlies Warramana Sandstone. Underlies Pungalina Member and Hobblechain Rhyolite.||
7486|Gold Creek Volcanics|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin, Calvert Superbasin.||Tawallah Group||Underlain by Wollogorang Formation. Partly overlain by Warramana Sandstone, Pungalina Member and Hobblechain Rhyolite.||
7486|Gold Creek Volcanics|73083|6|Mentioned|p40|||Speckled magnetic appearance.|||||Mafic volcanics.|
7486|Gold Creek Volcanics|73412|5|Briefly described|p2, 4, 8-9, 12, 14-15, 20|||Southern McArthur Basin. Higher conductivity and magnetic responses than most of the Group.||Tawallah Group.||Overlies Wollogorang Formation. Is overlain by Warramana Sandstone. Eruptive equivalent to Settlement Creek Volcanics sills.||
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|
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|
7636|Goulburn Group|22600|4|Described|Map legend||Middle Cambrian|||||||
7636|Goulburn Group|23356|5|Briefly described|26 Tab.2|Cambrian|Cambrian|||||||
7636|Goulburn Group|23373|3|Fully described|p318|Early Ordovician|Middle Cambrian|Comprises Jigaimara, Naningbura, Milingimbi and Mooroongga Formations. Of Arafura Basin.||||||28-MAR-12
7636|Goulburn Group|23374|3|Fully described|Tb3p22,23,6,20,35|Early Ordovician|Middle Cambrian|Comprises Jigaimara, Naningbura, Milingimbi and Mooroongga Formations. Of Arafura Basin.||||||21-SEP-06
7636|Goulburn Group|24047|5|Briefly described|p11|Ordovician|Cambrian|Geological Province: Arafura Basin.||||||
7636|Goulburn Group|24048|6|Mentioned|p5 Fig. 3|||||||||
7636|Goulburn Group|24049|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Includes Jigaimara Formation. Geol. Prov: Arafura Basin.||||||13-OCT-05
7636|Goulburn Group|42056|4|Described|p95|||||||||
7636|Goulburn Group|42058|5|Briefly described|p115|||||||||
7636|Goulburn Group|42864|5|Briefly described|Fig.21|||||||||
7636|Goulburn Group|44112|3|Fully described|Table13p74,78|Early Ordovician|Middle Cambrian|||||||
7636|Goulburn Group|60571|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Includes the Jigaimara Formation. Geological Province: Arafura Basin.||||||30-NOV-04
7636|Goulburn Group|61403|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Includes Jigaimara Formation. Geol. Prov: Arafura Basin.||||||
7636|Goulburn Group|62504|5|Briefly described|p1, 2|Cambrian|Cambrian|Overlies: Wessel Group. ||||||
7636|Goulburn Group|62505|4|Described|p2, 4|Ordovician|Cambrian|Dolomite dominated. Overlain unconformably by Djabura Formation. Unconformably overlies Elcho Island Formation.||||||
7636|Goulburn Group|62508|5|Briefly described|p32|Ordovician|Cambrian|||||||
7636|Goulburn Group|62510|5|Briefly described|p3|Orodvician|Cambrian|Geological Province: Arafura Basin.||||||
7636|Goulburn Group|62788|6|Mentioned|p103, p104 Fig. 2|||Arafura basin, NT. Fossiliferous early Middle Cambrian units - the Jigaimara Formation -  were reassigned from the Neoproterozoic Wessel Group into the Goulburn Group (Rawlings et al. 1997).|||Jigaimara Formation.|||28-MAR-12
7636|Goulburn Group|63062|4|Described|p9 Fig. 9, p14, p49|Ordovician|Cambrian|Includes Jigaimara, Naningbura, Milingimbi and Mooroongga Formation. Overlain by Arafura Group. Max. thickness: 1500m. Geol.Prov: Arafura and Money Shoal Basins. Shallow marine-non/marine interbedded mudstone, siltstone, sandstone and minor carbonates.||||||07-FEB-11
7636|Goulburn Group|63866|5|Briefly described|p115|Cambrian|Neoproterozoic|Arafura Basin.||||||
7636|Goulburn Group|64443|6|Mentioned|p40|||Of Arafura Basin. Correlative of Barkly Group, Georgina Basin.||||||
7636|Goulburn Group|69297|5|Briefly described|p283, p285, p289, p290|Lower Ordovician|Early Cambrian|Arafura Basin. Maximum thickness of 2500m in the central platform of the basin. Deposited in a shallow marine shelf environment. Limestones and dolomites are potential reservoirs for hydrocarbons. Mudstones may form hydrocarbon seals. |||Includes the Jigaimara Formation, Naningbura Dolomite and the Milingimbi and Mooroongga Formations.|Disconformably overlies the Wessel Group. Overlain (generally conformably) by the Arafura Group.||
7636|Goulburn Group|69421|6|Mentioned|p6:6|||Arafura Basin.||||||12-JUL-16
7636|Goulburn Group|69443|6|Mentioned|p28:21|||Arafura Basin.||||Correlated with Barkly Group.||12-JUL-16
7636|Goulburn Group|69451|4|Described|p35:1-4, 6-8, 10-11, 13-14|Early Ordovician|Middle Cambrian|Petroconsultants (1989); McLennan et al. (1990) and others. Arafura Basin. Is structurally conformable with the upper, post-rift portion of the Wessel Group. Up to 2000m thick in the central part of the Basin offshore. Only the basal part of the Jigaimara Formation is exposed; the rest is only intersected in drillholes. Mature to overmature for oil generation. Samples with TOC values up to 8.6% represent migrated hydrocarbons, although the Jigaimara Formation has source potential. Limestone and dolostone units are potential reservoirs, and have been shown to host oil and gas shows. Shale interbeds could provide intraformational seals.|||Naningbura Dolomite; Milingimbi, Mooroongga, Jigaimara Formations.|Overlies the Wessel Group disconformably or unconformably. Is overlain unconformably by Djabura Formation (Arafura Group).||12-JUL-16
7636|Goulburn Group|69456|5|Briefly described|p40:2 Fig.40.3|Ordovician|Cambrian|Arafura Basin.||||Overlies Wessel Group. Is overlain by Arafura Group.||12-JUL-16
7636|Goulburn Group|69673|6|Mentioned|p196, p198, p199|Ordovician|Cambrian |Age derived from marine fauna in Jigaimara Formation and Milingimbi Formation.|||Includes Jigaimara Formation, Naningbura Dolomite, Milingimbi Formation, Mooroongga Formation|Disconformably (or unconformably) overlies Wessel Group||
7636|Goulburn Group|70098|4|Described|p5, p7-9, p18 Fig.4, p19 Fig.5|Early Ordovician|Series 3|Arafura Basin and Goulburn Graben. Max thickness: 2 500 m. Depositional environment: shallow marine shelf. Significant oil shows in Paleozoic reservoirs were intersected. Potential source, reservoir and seal rocks occur.|||Jigaimara Formation (at base), Naningbura Dolomite, Milingimbi Formation, Mooroongga Formation|Disconformably overlies Wessel Group. Is overlain by Arafura Group.|Shallow marine limestones and dolomites.|
7636|Goulburn Group|71632|5|Briefly described|Map legend.|||Arafura Basin. Mapped with Wessels Group as a single unit.||||||
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).||
7652|Grace Creek Granite|9538|5|Briefly described|Map legend|Proterozoic|Proterozoic| Microgranite, hornblende-biotite granite, biotite granite.||||||01-NOV-04
7652|Grace Creek Granite|22538|6|Mentioned|P714|||||||||
7652|Grace Creek Granite|22600|6|Mentioned|Map legend|||||||||
7652|Grace Creek Granite|22808|6|Mentioned|7 fig 4|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
7652|Grace Creek Granite|23216|5|Briefly described|p2,Table1p10,12,14-6|||||||||
7652|Grace Creek Granite|23374|5|Briefly described|Fig3p5||Paleoproterozoic|Of Pine Creek Inlier.||||||07-NOV-08
7652|Grace Creek Granite|23733|5|Briefly described|p32 Fig. 19|||||||||13-NOV-06
7652|Grace Creek Granite|24049|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|In regional setting map legend.||||||07-NOV-08
7652|Grace Creek Granite|24197|5|Briefly described|p28, p106 Tb. 15.1|Paleoproterozoic|Paleoproterozoic|Of the Jim Jim Suite. Age: ~1825Ma. Geological Province: Pine Creek Inlier.||||||07-FEB-11
7652|Grace Creek Granite|32660|5|Briefly described|Table 2|||||||||
7652|Grace Creek Granite|33278|6|Mentioned|Fig.7|||||||||
7652|Grace Creek Granite|35061|6|Mentioned|p143|||||||||
7652|Grace Creek Granite|35465|6|Mentioned|Fig.1|||Geology of Pine Creek Geosyncline.||||||21-SEP-06
7652|Grace Creek Granite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
7652|Grace Creek Granite|40248|4|Described|p225|||||||||
7652|Grace Creek Granite|41294|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
7652|Grace Creek Granite|41295|4|Described|p15|||Formerly Mount Harvey Porphyry and Grace Creek Porphyry.||||||21-SEP-06
7652|Grace Creek Granite|41397|4|Described|p17|||||||||
7652|Grace Creek Granite|41406|6|Mentioned|Map legend|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
7652|Grace Creek Granite|41407|6|Mentioned|Map legend|Proterozoic||||||||
7652|Grace Creek Granite|41465|6|Mentioned|p8|||||||||
7652|Grace Creek Granite|41586|6|Mentioned|Map legend|||||||||
7652|Grace Creek Granite|41980|6|Mentioned|Fig.2 P545|||||||||
7652|Grace Creek Granite|43010|6|Mentioned|p64|||||||||
7652|Grace Creek Granite|43149|5|Briefly described|Map Legend||Paleoproterozoic|Of Orosirian age.||||||07-NOV-08
7652|Grace Creek Granite|43187|5|Briefly described|p2|||||||||
7652|Grace Creek Granite|43292|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
7652|Grace Creek Granite|43624|6|Mentioned|p13|||Of Pine Creek Plutonic Complex.||||||21-SEP-06
7652|Grace Creek Granite|43718|4|Described|Fig 1.1,p1,92|||||||||
7652|Grace Creek Granite|44201|14|Not recorded|p.11|||||||||
7652|Grace Creek Granite|44399|5|Briefly described|map legend||Paleoproterozoic|Granite, granite porphyry.||||||07-NOV-08
7652|Grace Creek Granite|45022|3|Fully described|p.147,148||Carpentarian|On many pages.||||||
7652|Grace Creek Granite|46658|5|Briefly described|p558|||||||||
7652|Grace Creek Granite|46678|6|Mentioned|p.9|||Mount Evelyn, N.T., Sheet D/53-5. B.M.R. Aust. 1:250,000 geol.Ser.Explan.Notes||||||
7652|Grace Creek Granite|46679|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
7652|Grace Creek Granite|46848|6|Mentioned|p167|||||||||
7652|Grace Creek Granite|47049|5|Briefly described|Table|||Redefined; extent diminished.||||||
7652|Grace Creek Granite|48867|14|Not recorded|p.5,15,18-20||Neoproterozoic|map. U.L. Proterozoic; it is "probably genetically related to the Cullen Granite."||||||
7652|Grace Creek Granite|50586|5|Briefly described|p1.1, 5.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Of the Jim Jim Suite. Age: 1863 +/- 5Ma (U-Pb).||||||07-NOV-08
7652|Grace Creek Granite|60573|6|Mentioned|Regional Setting legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
7652|Grace Creek Granite|60680|5|Briefly described|Map legend|Orosirian|Orosirian|Of the Jim Jim Suite. Porphyritic microgranite, layered in places.||||||14-JAN-05
7652|Grace Creek Granite|60684|6|Mentioned|p51 Appendix, p13|||Felsic intrusive.||||||28-APR-05
7652|Grace Creek Granite|61403|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|In regional setting map legend.||||||07-NOV-08
7652|Grace Creek Granite|63866|5|Briefly described|p110|Orosirian|Orosirian|Central Domain, Pine Creek Orogen. Numeric age likely contains inherited analyses.|1863 +/- 5 Ma (Page, OZCHRON)|David Suite||||
7652|Grace Creek Granite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1820-1850Ma. Of Jim Jim Suite. I-type. Porphyritic, commonly xenocrystic red to pink-grey granite, microgranite; Porphyritic pink grey-green fine to medium hornblende biotite granite.||||||07-JAN-09
7652|Grace Creek Granite|64725|6|Mentioned|p60 Fig.5, p61.||||1835-1800 Ma.|||||
7652|Grace Creek Granite|67564|3|Fully described|p7 Table 2, p29, p30, p37, p62,  p85.|Orosirian|Orosirian|Eastern Pine Creek Orogen. A large (1000 km2) concentrically-zoned pluton, comagmatic with Plum Tree Creek Volcanics. Has contact metamorphosed the Hindrance Sandstone. Rocks of this unit mapped by Walpole (1963) are now in Plum Tree Creek Volcanics.|1825 Ma.|Unit in David Suite.||Intrudes Tollis Formation and Hindrance Creek Sandstone. Is overlain nonconformably by Mamadawerre Sandstone.|Red to pink-grey microgranite with corroded K-feldspar xenocrysts to 6 cm; pink-grey, fine-grained and medium-grained xenocrystic and porphyritic granites.|
7652|Grace Creek Granite|69420|5|Briefly described|p5:17-18, 21, 23|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Geographically related, and compositionally similar, to Plum Tree Creek Volcanics. Mineralogy and petrology/geochemistry summarised.|1863 +/- 5 Ma: conventional U-Pb zircon (TIMS).|Jim Jim Suite.|||Fine- to coarse-grained equigranular to porphyritic alkali feldspar granite and greisens; porphyritic microgranite, medium-grained granite and porphyritic granophyre.|12-JUL-16
7652|Grace Creek Granite|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|1863+/-5.0 Ma (crystallisation: U-Pb).||||Granite.|
7690|Grant Bluff Formation|8217|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Sandstone(thin bedded), siltstone, shale. Overlies: Gnallan-a-gea Arkose.||||||28-OCT-04
7690|Grant Bluff Formation|9394|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Georgina Basin. Of the Mopunga Group. Sandstone, shale. Underlies: Elkera Formation. Overlies: Elyuah Formation.||||||01-NOV-04
7690|Grant Bluff Formation|9694|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Mopunga Group. Geological Province: Georgina Basin. Underlies: Elkera Formation. Overlies: Elyuah Formation. Fine thin-bedded sandstone.||||||
7690|Grant Bluff Formation|22646|6|Mentioned|Fig 4 on p 102|Neoproterozoic|Neoproterozoic|Georgina Basin.  Age - Ediacarian in text.||||||
7690|Grant Bluff Formation|22762|6|Mentioned|p362|||Geological Province - Georgina Basin.||||||
7690|Grant Bluff Formation|23844|5|Briefly described|p37|Neoproterozoic|Neoproterozoic|Geological Province: Georgina Basin||||||
7690|Grant Bluff Formation|24442|6|Mentioned|p49|||Geological Province: Georgina Basin.||||||
7690|Grant Bluff Formation|33103|4|Described|Table 4|||||||||
7690|Grant Bluff Formation|33104|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
7690|Grant Bluff Formation|33111|6|Mentioned|p38|||||||||
7690|Grant Bluff Formation|34557|6|Mentioned|p351|||Cambrian||||||
7690|Grant Bluff Formation|34724|6|Mentioned|p343|||||||||
7690|Grant Bluff Formation|35005|5|Briefly described|p145|||||||||
7690|Grant Bluff Formation|35121|6|Mentioned|Map legend|Early Cambrian|Adelaidean|||||||
7690|Grant Bluff Formation|35139|4|Described|Table.2|||See also p10.||||||21-SEP-06
7690|Grant Bluff Formation|35221|6|Mentioned|p14|||||||||
7690|Grant Bluff Formation|35798|4|Described|p307|||Proterozoic rather than Cambrian.||||||
7690|Grant Bluff Formation|35863|6|Mentioned|Table 1|||||||||
7690|Grant Bluff Formation|37572|5|Briefly described|p154|||See also p164 and Fig.8.||||||21-SEP-06
7690|Grant Bluff Formation|37928|6|Mentioned|Fig.4|||||||||
7690|Grant Bluff Formation|38157|6|Mentioned|Table IX|||||||||
7690|Grant Bluff Formation|39210|4|Described|p51|||||||||
7690|Grant Bluff Formation|39921|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
7690|Grant Bluff Formation|40538|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Mopunga Group. Quartz arenite to quartz wacke, fine grained, fissile and undulose laminated. Geological Province: Georgina Basin.||||||15-NOV-05
7690|Grant Bluff Formation|40906|4|Described|p21|||||||||
7690|Grant Bluff Formation|41005|6|Mentioned|p217|||||||||
7690|Grant Bluff Formation|41388|6|Mentioned|p552|||||||||
7690|Grant Bluff Formation|41429|6|Mentioned|p247|||||||||
7690|Grant Bluff Formation|41801|5|Briefly described|p215|||||||||
7690|Grant Bluff Formation|42059|6|Mentioned|Fig.2 P131|||||||||
7690|Grant Bluff Formation|42225|6|Mentioned|p219|||||||||
7690|Grant Bluff Formation|42504|5|Briefly described|Table 4 P73|||||||||
7690|Grant Bluff Formation|42643|5|Briefly described|p29|||||||||
7690|Grant Bluff Formation|44327|2|Defined|Tb.I,p.8,9,11,18|||(F53-11). Underlies conformably Mount.Baldwin Formation. Of the Mopunga Group.||||||29-SEP-11
7690|Grant Bluff Formation|44328|14|Not recorded|map legend|Early Cambrian|Neoproterozoic|Lower Cambrian to Upper Proterozoic.||||||
7690|Grant Bluff Formation|44334|14|Not recorded|map legend||Neoproterozoic|Upper Proterozoic.||||||
7690|Grant Bluff Formation|44358|4|Described|p8,Tb.1|Early Cambrian|Neoproterozoic|||||||
7690|Grant Bluff Formation|44469|2|Defined|p.7,opp.p.6, Tb.I|||(F53-12). See also p.16.||||||
7690|Grant Bluff Formation|44470|5|Briefly described|map legend|||Upper Proterozoic to Lower Cambrian.||||||02-DEC-04
7690|Grant Bluff Formation|45052|4|Described|p64|||See also Fig.9 and Table 8||||||21-SEP-06
7690|Grant Bluff Formation|45102|6|Mentioned|p43|||See also p44,45.||||||21-SEP-06
7690|Grant Bluff Formation|45155|6|Mentioned|Fig.7|||Georgina Basin||||||
7690|Grant Bluff Formation|46865|5|Briefly described|p48|||||||||
7690|Grant Bluff Formation|46903|6|Mentioned|p53|||||||||
7690|Grant Bluff Formation|47035|6|Mentioned|Fig.1|||||||||
7690|Grant Bluff Formation|48844|2|Defined|p.20-31|||On many pages. p.1,16,17,20-31,33,34,36,39, F.26,58,59,67, Pl.8. (new name).Overlies Elyuah Formation. Good marker bed. (F53-11).||||||21-SEP-06
7690|Grant Bluff Formation|48901|14|Not recorded|Not recorded||Adelaidean|Part of Mopunga Group.||||||21-SEP-06
7690|Grant Bluff Formation|48990|1|Redefined|p12|Adelaidean|Adelaidean|See also p10.||||||21-SEP-06
7690|Grant Bluff Formation|49027|5|Briefly described|p5|||||||||
7690|Grant Bluff Formation|60122|4|Described|p4-5, p13-14|Neoproterozoic|Neoproterozoic|Of the Mopunga Group.  Revised by Walter (1980) to exclude the Elkera Formation.  Quartz sandstone/quartzite, glauconitic quartz sandstone, mudstone. Conformable on Gnallan-a-Gea Arkose and Elyuah Fm. Max. thickness: 1170m in HAY RIVER. See also p11Tb. 1||||||21-SEP-06
7690|Grant Bluff Formation|60551|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Mopunga Group. Geological province: Georgina Basin.  Underlies: Elkera Formation. Overlies: Elyuah Formation. Thin bedded fine sandstone, shale.||||||17-NOV-04
7690|Grant Bluff Formation|60590|5|Briefly described|Map legend|Cryogenian|Cryogenian|Of the Mopunga Group.  Quartz sandstone/quartzite, glauconitic quartz sandstone, mudstone.  Overlies the Elyuah Formation and the Gnallan-a-Gea Arkose.||||||
7690|Grant Bluff Formation|60668|5|Briefly described|Fig. 23a|||Shale, silty sandstone and pebble conglomerate.   Geological Province: Georgina Basin. ||||||
7690|Grant Bluff Formation|61022|5|Briefly described|p15 Fig. 2|Neoproterozoic|Neoproterozoic|Geological Province: Georgina Basin. Named in abstract for: Carbonate ramp facies and oil plays in Late Cambrian-southern Georgina Basin (abstract) by Ambrose, G.J. and Putnam, P.E.||||||20-APR-05
7690|Grant Bluff Formation|61208|5|Briefly described|p208|||Unconformably overlies the Utopia Quartzite. Geological Province: Georgina Basin.||||||12-JAN-06
7690|Grant Bluff Formation|61388|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of the Mopunga Group. Fine-grained, thin bedded, flaggy white, brown and reddish sandstone; local coarse to pebbly sandstone; interbedded mudstone. Geological Province: Georgina Basin.||||||
7690|Grant Bluff Formation|61404|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Mopunga Group. Quartz sandstone/quartzite, glauconitic quartz sandstone, mudstone.  Age: Ediacaran.  Geological Province: southern Georgina Basin.||||||
7690|Grant Bluff Formation|61732|3|Fully described|p5 Tb. 1, p109|Ediacaran|Ediacaran|Of Mopunga Group. Transitionally overlies Eluyah Fm; underlies (probably unconconformably) Elkera Fm. Geol. Prov: Georgina Basin. See also p106, p108 Fig. 40.||||||07-FEB-11
7690|Grant Bluff Formation|62376|5|Briefly described|p53|Neoproterozoic|Neoproterozoic|Geological Province: Georgina Basin||||||09-FEB-10
7690|Grant Bluff Formation|62595|6|Mentioned|p28 Fig.4.|Late Neoproterozoic|Late Neoproterozoic|Georgina Basin. Relative probability plots of detrital zircon data are shown.||||||
7690|Grant Bluff Formation|62642|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Mopunga Group. Geological Province: Georgina/Ngalia Basin. Sandstone, micaceous-quartzofeldspathic, with abundant ripple marks, low angle tabular cross-bedding; conglomerate with granite clasts, pebbly or granular arkose.||||||21-SEP-06
7690|Grant Bluff Formation|62984|5|Briefly described|p13|Neoproterozoic III|Neoproterozoic III|Of the Mopunga Group. Overlies the Eyuah Formation; overlain by Elkera Formation. Geological Province: Georgina Basin. Sandy deposits.||||||23-JAN-07
7690|Grant Bluff Formation|63450|5|Briefly described|p78 Fig. 5, p79|Neoproterozoic|Neoproterozoic|Overlies Gnallan-A-Gea Arkose. Geological province: Georgina Basin, West Toko Syncline. Contains quartzose sandstone and numerous sedimentary structures including trace fossils, glauconitic sandstone and mudstone; marine in origin.||||||07-FEB-11
7690|Grant Bluff Formation|63562|4|Described|p338 fig 3, p344-345, p347 fig 9|Ediacaran|Ediacaran|See also p351, p352 fig 10. Of Georgina Basin. Forms escarpments in the Elua Range. Zircons are similar to, but more concordant than, those in Cyclops Member; source probably Arunta Inlier.||Mopunga Group||Overlies Elyuah Formation. Has been correlated with Cyclops Member (Pertatataka Formation). Is overlain by Elkera Formation.|Coarse-grained sandstone, with interbeds of fine-grained, thinly-bedded, recessive sandstone units. Contains ichnofossils, syneresis cracks and fine disseminated pyrite.|
7690|Grant Bluff Formation|64068|3|Fully described|p50-51, p44, 49, 52, 54, 57, 162|Ediacaran|Ediacaran|Now includes rocks formerly assigned to the Forster Member of the Central Mount Stuart Formation.||Of Mopunga Group.||Conformably, gradationally, overlies Elyuah Formation, Gnallan-a-Gea Arkose. Conformably and gradationally overlain by Elkera Formation, Central Mount Stuart Formation.|Orange-brown, white and purple quartz sandstone, quartzite and quartz greywacke, arkose, siltstone, shale, minor dolostone.|04-APR-12
7690|Grant Bluff Formation|65237|5|Briefly described|p5|||Of the Mopunga Group. Overlain by Elkera Formation; conformable/gradation on Elyuah Formation. Geological province: southern Georgina Basin.||||||07-FEB-11
7690|Grant Bluff Formation|65338|4|Described|p iv, p60, pp64-65.|Ediacaran|Ediacaran|Georgina Basin. Deltaic clastic rocks. Now recognised to be more widespread than previously mapped. Correlated with middle to upper Pertatataka Formation of Amadeus Basin. Cross-bedding and ripples are common. Shallow marine.||Unit in Mopunga Group.||Faulted against Amesbury Quartzite. Overlies Elyuah Formation and Gnallan-a-gea Arkose. Is overlain by Elkera and Central Mount Stuart Formations.|Laminated to thinly bedded, fine-grained quartz arenite and sublitharenite with micaceous partings; bounded by a lowermost and uppermost interval of well-sorted and well-rounded, medium- to coarse-grained, thinly to thickly bedded quartz arenite.|
7690|Grant Bluff Formation|65341|5|Briefly described|p2 Fig.2, p5, p15. |||Includes some outcrops previously (Shaw and Warren 1975) mapped as 'Central Mount Stuart beds'. Outcrops over basement near the northern map area are continuous with the mapped Forster Member of the Central Mount Stuart Formation; thus this Member is here abandoned. ||Unit in Mopunga Group.||Conformably overlies Elyuah Formation.|White, brown and reddish, thinly bedded, tabular, fine sandstone; local coarse to pebbly sandstone; interbedded mudstone.|
7690|Grant Bluff Formation|67164|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Georgina/Ngalia Basins.||Unit in Mopunga Group.||Overlies Elyuah Formation. Is overlain by Central Mount Stuart Formation.|Micaceous quartzofeldspathic sandstone with abundant ripple marks, low-angle tabular cross-bedding; conglomerate with granite clasts, pebbly or granular arkose.|
7690|Grant Bluff Formation|67892|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|||Unit in Mopunga Group.||Overlies Elyuah Formation. Is overlain by Central Mount Stuart Formation.|Sandstone, micaceous, quartzofeldspathic, with abundant ripple marks, low-angle tabular cross-bedding; conglomerate with granite clasts, pebbly or granular arkose.|
7690|Grant Bluff Formation|69437|5|Briefly described|p22:4-5, 7|Ediacaran|Ediacaran|SE Georgina Basin, Centralian A Superbasin. Supersequence 3.||Mopunga Group.||Overlies Elyuah Formation and Gnallan-a-Gea Arkose. Is overlain by Elkera Formation.||12-JUL-16
7690|Grant Bluff Formation|69443|4|Described|p28:7, 10-11, 15-16, 35|Ediacaran|Ediacaran|K.G. Smith (1964); modified by Walter (1980). Southern Georgina Basin. Forms widespread prominent strike ridges. Thickness varies considerably, from 20m to 1170m. Deposited as a transgressive sand sheet in a shallow- to marginal-marine environment. Is also overlain disconformably by Thorntonia Limestone or Adam Shale, or unconformably by Red Heart Dolostone.||Mopunga Group.||Gradationally overlies Elyuah Formation and Gnallan-a-Gea Arkose. Is overlain conformably and gradationally by Elkera and Central Mount Stuart Formations, and Andagera Formation.|Mainly laminated to medium undulose-bedded, medium to coarse quartz sandstone and quartzite with micaceous partings; also quartz greywacke, arkose, siltstone, shale, minor dolostone and local basal polymict conglomerate have been reported.|12-JUL-16
7690|Grant Bluff Formation|69673|5|Briefly described|p114 fig 92, p115|Ediacaran|Ediacaran |||Mopunga Group||Overlies Elyuah Formation, Gnallan-a-gea Arkose, overlain by Elkera Formation, Central Mount Stuart Formation|Sandstone and quartzite.|
7690|Grant Bluff Formation|71621|5|Briefly described|p30|||Georgina Basin. Said to have an unconformable and in part faulted contact with the Xanten Granodioritie [although the exact nature of this contact isnt provided].||||||02-FEB-19
7690|Grant Bluff Formation|71800|5|Briefly described|p26-p27|Ediacaran|Ediacaran|Georgina Basin.||||Overlies the Elyuah Formation. Overlain by the Ellkera Formation.|Medium sandstone.|
7690|Grant Bluff Formation|72515|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Jervois Range Special Map Sheet. Georgina Basin. Contains ichnofossils, microbial mat fragments.||Mopunga Group||Overlain by the Elkera Formation. Overlies the Elyuah Formation.|Quartz sandstone, quartzwacke; laminated to medium undulose-bedded, trough cross-bedded; syneresis cracks; ripple marks; minor arkose, locally glauconitic; minor siltstone, shale, dolostone; local basal conglomerate.|
7690|Grant Bluff Formation|72516|2|Defined|p15-16, 21, 46, 47, 85, 86, 88-90|Ediacaran|Ediacaran|Georgina Basin.Widespread unit forming prominent strike ridges and hills. Type section is defined 15km southeast of Grant Bluff in Elua Range in JINKA. In JERVOIS RANGE SPECIAL it forms ridges nof the Jervois Range and Johansen Range. Rocks previously assigned to this unit in the Charlotte Fault Zone are now assigned to Elkera Formation. Contains Ediacaran ichnofossils, indeterminate filaments, mat fragments, vendotaeniid fragments, leiospheres, acritarchs and microbial mat fragments. Deposited in a shallow to marginal-marine trangressive sheet sand environment. 66-90m thick in the map sheet area, 20-1170m thick elsewhere. Equivalent to the Cyclops Member and the Badens Camp Quartzite. See also p12, 13, p186, p189,198, 201, 218. Also misspelt as Grand Bluff Formation p186, p189, 198, 201, 218.|ca 818 Ma (max dep age)|Mopunga Group||Conformably to gradationally overlain by the Elkera Formation. Conformably overlies the Elyuah Formation, Unconformably overlies the Bonya Metamorphics,Tarlton Granite and the Jericho Granite.|Quartz sandstone, quartzwacke; laminated to medium-undulose-bedded, trough cross bedded; syneresis cracks; ripple marks; minor arkose, locally glauconitic; minor siltstone, shale, dolostone; local basal conglomerate.|16-JUN-21
7690|Grant Bluff Formation|73086|6|Mentioned|p122|||Georgina Basin, south-eastern.||||Correlates to Pertatataka Formation.||
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
7866|Gum Ridge Formation|22954|6|Mentioned|Fig3p9|Ordian-Early Templetonia|Ordian-Early Templetonia|||||||
7866|Gum Ridge Formation|23328|5|Briefly described|1030|Middle Cambrian|Early Cambrian|||||||07-SEP-09
7866|Gum Ridge Formation|23410|5|Briefly described|Map Legend|Ordian-Early Templetonia|Ordian-Early Templetonia|Chertified bioclast, onkoid and cryptomicrobial limestone, marly calcimudstone, minor siliciclastic mudstone; carbonate and evaporite nodules; basal sandstone and siliciclastic mudstone; fossiliferous. Geol. Prov: Georgina Basin.||||||02-NOV-05
7866|Gum Ridge Formation|23981|6|Mentioned|p65|||Geological Province: western Georgina Basin in NT.||||||
7866|Gum Ridge Formation|24172|4|Described|p55|Cambrian|Cambrian|Unconformably overlies Helen Springs Volcanics . Max. Thickness: 14m.||||||21-SEP-06
7866|Gum Ridge Formation|24297|5|Briefly described|p19|Middle Cambrian|Middle Cambrian|Lateral equivalent of Montejinni Limestone. Geological Province: Georgina Basin.||||||
7866|Gum Ridge Formation|24303|2|Defined|p36, p63 Appendix|Ordian-Early Templetonian|Ordian-Early Templetonian|Overlain by the Anthony Lagoon beds. Overlies the Helen Springs Volcanics. Geological Province: Barkly Sub-basin, Georgina basin. Max. Thickness: 150.5m. Equivalent to Montejinni Limestone, Tindall Limestone, Linekar Limestone, Panton Fm. & Top Springs Ls||||||24-MAR-16
7866|Gum Ridge Formation|24304|5|Briefly described|Map legend|Cambrian|Cambrian|Limestone: fine-grained sandstone and siliciclastic mudstone; bioclast, oncoid, styololitic and cryptomicrobial limestone, marly limestone; fossiliferous, nodular chert; carbonate and evaporite pseudomorphs; silicified, recessive.||||||17-OCT-05
7866|Gum Ridge Formation|29940|6|Mentioned|p169|||||||||
7866|Gum Ridge Formation|30017|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
7866|Gum Ridge Formation|30320|6|Mentioned|p422|||||||||
7866|Gum Ridge Formation|30479|6|Mentioned|p19|||||||||
7866|Gum Ridge Formation|32174|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|Early Middle Cambrian||||||
7866|Gum Ridge Formation|32959|6|Mentioned|Fig.12|||||||||
7866|Gum Ridge Formation|33307|6|Mentioned|Fig.8|||||||||
7866|Gum Ridge Formation|33516|6|Mentioned|p99|||||||||
7866|Gum Ridge Formation|34053|6|Mentioned|p8|||M.Camb.  See also P11||||||
7866|Gum Ridge Formation|34149|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
7866|Gum Ridge Formation|34151|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
7866|Gum Ridge Formation|34439|6|Mentioned|p9|||See also P11. Middle Cambrian||||||
7866|Gum Ridge Formation|34440|5|Briefly described|Table 1|||M.Camb. PP8,10||||||
7866|Gum Ridge Formation|34441|4|Described|Table 1|Middle Cambrian||M.Camb. See also pp11,12,14 etc.||||||14-NOV-06
7866|Gum Ridge Formation|35224|6|Mentioned|p5|||||||||
7866|Gum Ridge Formation|35231|6|Mentioned|p8|||||||||
7866|Gum Ridge Formation|35771|4|Described|Table 1|||||||||
7866|Gum Ridge Formation|36335|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|Middle Cambrian(Ordian).||||||
7866|Gum Ridge Formation|36473|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian to Ordovician||||||
7866|Gum Ridge Formation|37572|4|Described|p156|||See also p165.||||||21-SEP-06
7866|Gum Ridge Formation|39213|6|Mentioned|Fig.8|||||||||
7866|Gum Ridge Formation|39624|4|Described|p43|||||||||
7866|Gum Ridge Formation|39900|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|Middle Cambrian||||||
7866|Gum Ridge Formation|40580|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
7866|Gum Ridge Formation|40852|6|Mentioned|p37|||See also Fig.3.9||||||
7866|Gum Ridge Formation|40856|5|Briefly described|p315|||||||||
7866|Gum Ridge Formation|41128|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|Chert, ferruginised, laminated and concentrically banded; siltstone, laminated and fossiliferous, coquinite, ferruginised and silicified; minor sandstone; rare dolostone. Geological Province: Georgina Basin.||||||16-NOV-05
7866|Gum Ridge Formation|41129|3|Fully described|p15|||||||||
7866|Gum Ridge Formation|41204|4|Described|p13|||Mention p4.||||||21-SEP-06
7866|Gum Ridge Formation|41205|5|Briefly described|Map legend|Cambrian|Cambrian|Siltstone, chert, sandstone. Geological Province: Georgina Basin.||||||16-NOV-05
7866|Gum Ridge Formation|41308|4|Described|p13|||||||||
7866|Gum Ridge Formation|41310|5|Briefly described|p14|||||||||
7866|Gum Ridge Formation|41524|6|Mentioned|p6|||||||||
7866|Gum Ridge Formation|42643|6|Mentioned|p26|||||||||
7866|Gum Ridge Formation|42956|5|Briefly described|p31 Fig.4|||||||||
7866|Gum Ridge Formation|43223|5|Briefly described|Map Legend||Paleozoic|||||||07-NOV-08
7866|Gum Ridge Formation|43224|5|Briefly described|Map legend|Paleozoic|Neoproterozoic|||||||07-NOV-08
7866|Gum Ridge Formation|43652|6|Mentioned|p386|||||||||
7866|Gum Ridge Formation|44201|6|Mentioned|p.10|||||||||
7866|Gum Ridge Formation|44205|14|Not recorded|p49|||||||||
7866|Gum Ridge Formation|44283|14|Not recorded|p.8|||Outcrops to west of Alroy sheet.||||||
7866|Gum Ridge Formation|44285|14|Not recorded|Tb.opp.p.6||Middle Cambrian|May be continuous with Wonarah Beds. M.Cambrian.||||||
7866|Gum Ridge Formation|44322|5|Briefly described|map legend||Cambrian|||||||22-DEC-09
7866|Gum Ridge Formation|44441|14|Not recorded|opp.p.6, Tb.1||Middle Cambrian|May be continuous with Wonarah Beds. Mid.Cambrian. (E53-16).||||||
7866|Gum Ridge Formation|44960|14|Not recorded|Not recorded|||||||||
7866|Gum Ridge Formation|44965|14|Not recorded|Not recorded|||||||||
7866|Gum Ridge Formation|45032|14|Not recorded|p8||Middle Cambrian|||||||
7866|Gum Ridge Formation|45045|6|Mentioned|p7|||||||||
7866|Gum Ridge Formation|45052|2|Defined|p75|Middle Cambrian|Middle Cambrian|||||||
7866|Gum Ridge Formation|45055|6|Mentioned|p7|||See also P8,10,11,22,23||||||
7866|Gum Ridge Formation|45062|6|Mentioned|p11|||||||||
7866|Gum Ridge Formation|45064|3|Fully described|Table 1|||See also p19.||||||21-SEP-06
7866|Gum Ridge Formation|45148|6|Mentioned|p11|||||||||
7866|Gum Ridge Formation|45167|5|Briefly described|p53|||||||||
7866|Gum Ridge Formation|45373|14|Not recorded|p.177,178|||||||||
7866|Gum Ridge Formation|47058|6|Mentioned|Fig.3 P123|||||||||
7866|Gum Ridge Formation|48831|14|Not recorded|Not recorded|||||||||
7866|Gum Ridge Formation|48835|14|Not recorded|p.16,Pl.1|||||||||
7866|Gum Ridge Formation|48860|4|Described|p.17||Cambrian|On many pages. p.1,4,7,17,70, Pl.6. Lower Middle Cambrian. (E53-14/Tennant Creek). See base card under Helen Springs Volcs.||||||
7866|Gum Ridge Formation|48891|14|Not recorded|p.22||Cambrian|Tb.1. L-M Cambrian.||||||
7866|Gum Ridge Formation|60419|5|Briefly described|p18|Middle Cambrian|Middle Cambrian|Geological Province: Georgina Basin.  Contains fauna of Ordian age.||||||
7866|Gum Ridge Formation|60637|5|Briefly described|Map legend|||Fossiliferous siltstone and chert; silicified limestone; some sandstone and leached calcareous sandstone; silicified limestone.||||||
7866|Gum Ridge Formation|60684|4|Described|p14||Ordian-Early Templetonia|Chert, chert breccia, limestone. Most common lithotype: red-brown to yellow-grey tabular chertified rocks, with occasional trilobites and lingulate brachiopods.  Overlies Helen Springs Volcanics. Max. thickness: 145m (clay, dolostone, chert on FREW RIVER)||||||14-DEC-05
7866|Gum Ridge Formation|60685|5|Briefly described|p19|Middle Cambrian|Middle Cambrian|Lateral correlative of Montejinni Limestone. Geological Province: Georgina Basin.||||||
7866|Gum Ridge Formation|60990|6|Mentioned|p85|Middle Cambrian|Middle Cambrian|Georgina Basin. Faunal links with Antarctica.||||||
7866|Gum Ridge Formation|61567|5|Briefly described|p632|Cambrian|Cambrian|In the Amelia impact structure this unit is composed of chert and cherty breccias up to 10m thick.  See also p633 Tb. 1.||||||27-APR-06
7866|Gum Ridge Formation|62787|6|Mentioned|p82 Fig. 3|Cambrian|Neoproterozoic|Geological Province: Georgina Basin (NT).||||||07-FEB-11
7866|Gum Ridge Formation|63569|6|Mentioned|p123|Cambrian|Cambrian|Georgina Basin. Contains lingulate brachiopods that correlate with Redlichia guizhouensis Zone of China.||||||
7866|Gum Ridge Formation|64068|6|Mentioned|p53, 59|Cambrian|Cambrian|Western Georgina Basin. Correlated with Thorntonia Limestone.||||Transitionally or disconformably overlies Andagera Formation.||05-APR-12
7866|Gum Ridge Formation|64443|6|Mentioned|p10, p31, p40|Middle Cambrian|Ordian-Early Templetonian|Fossiliferous. Barkly Sub-basin.||Of Barkly Group.||||14-MAY-14
7866|Gum Ridge Formation|64780|5|Briefly described|p62 Fig.3 |Cambrian|Cambrian|||||||
7866|Gum Ridge Formation|65337|5|Briefly described|p94.|Middle Cambrian|Middle Cambrian|Barkly Sub-basin, central Georgina Basin. Carbonates.||||Unconformably overlies Kalkarindji Volcanic Group.||
7866|Gum Ridge Formation|65344|4|Described|p3, 5, 6, 7, 8, 9, 12, 20-24, Figs.,Tbls|Middle Cambrian|Middle Cambrian|Of the Barkly Sub-basin, Georgina Basin. See well logs and thin section descriptions for detail. Thickness: up to 148.8m in NTGS02/1||||Overlies the South Nicholson Group and the Helen Springs Volcanics. Underlies the Anthony Lagoon beds and the Wonarah Formation.|Dolostone.|03-MAY-12
7866|Gum Ridge Formation|65345|5|Briefly described|pp3-4, p6 Fig.5, p11 Fig.11. |Cambrian|Cambrian|Western Georgina Basin.Contains two intervals with anomalous phosphate.  Equivalent to the Tindall Limestone of the Daly Basin, and to the Montejinni Limestone/Hooker Creek Formation/Lothari Hill Sandstone sequence in the Wiso Basin.||||Is unconformably overlain by Anthony Lagoon beds.|Cherty limestone, mudstone, siltstone and sandstone.|
7866|Gum Ridge Formation|67148|5|Briefly described|Map legend.|Middle Cambrian|Middle Cambrian|||Unit in Barkly Group.||Is unconformably overlain by Wonarah Formation.|Limestone: grey, massive, mottled lithoclast-bioclast wackestone, ribbon limestone, minor oncoid rudstone; minor maroon dolomitic-siliciclastic siltstone and grey mudstone; nodular evaporite; local basal conglomerate.|
7866|Gum Ridge Formation|67149|5|Briefly described|Map legend.|Middle Cambrian|Middle Cambrian|Georgina Basin.||Unit in Barkly Group.||Overlies Helen Springs Volcanics. Is overlain by Anthony Lagoon and Wonarah Formations.|Limestone: grey, massive, mottled lithoclast-bioclast wackestone, mudstone interbeds; minor oncoid rudstone, maroon dolomitic-siliciclastic siltstone and grey mudstone; nodular evaporite; local basal conglomerate.|
7866|Gum Ridge Formation|67150|5|Briefly described|Map legend.|Middle Cambrian|Middle Cambrian|Georgina Basin.||Unit in Barkly Group.||Unconformably overlies Helen Springs Volcanics and South Nicholson Group. Is unconformably overlain by Anthony Lagoon Formation.|Limestone: grey, massive, mottled lithoclast-bioclast wackestone, mudstone interbeds; minor oncoid rudstone, maroon dolomitic-siliciclastic siltstone and grey mudstone; nodular evaporite; local basal conglomerate (cross-section only).|
7866|Gum Ridge Formation|67352|6|Mentioned|v, pages17-21,23,40,44-45,47,49,50-52,69|Middle Cambrian|Middle Cambrian|Full description on pp 19-21. Simplified lithology quoted here. Contains a widespread (NT-SA-Antarctica) fossil fauna.||Barkly Group||Correlative of Top Springs Limestone. Is conformably overlain by Anthony Lagoon or Wonarah Formations. Overlies (disconformably) Helen Springs Volcanics or Renner Group or South Nicholson Group.|Two successive marine limestone units, each underlain by thin (8-10 m thick) peritidal siliciclastic intervals.|
7866|Gum Ridge Formation|68518|6|Mentioned|p14|||Sandover beds are probable correlatives in Hatches Creek Region (Blake and other, 1986)||||||30-JUN-14
7866|Gum Ridge Formation|69437|5|Briefly described|p22:9-10|Series 2|Series 2|Barkly Sub-basin, Georgina Basin, Centralian B Superbasin. Sequence 1. Restricted marine and peritidal deposits.||||Overlies Helen Springs Volcanics. Is overlain by Anthony Lagoon Formation. Is equivalent to Top Springs Limestone.|Limestone and minor siliciclastic mudstone.|12-JUL-16
7866|Gum Ridge Formation|69438|5|Briefly described|p23:29|Middle Cambrian|Middle Cambrian|Georgina Basin. Correlation based on a distinct positive excursion in stable carbon and oxygen isotopes.||||Time-equivalent to Giles Creek Dolostone (Amadeus Basin).||12-JUL-16
7866|Gum Ridge Formation|69443|4|Described|p28:12, 16, 21-22, 42|Middle Cambrian|Middle Cambrian|Opik in Ivanac (1954). Central and western Georgina Basin. Crops out discontinuously as low, rubble-covered plateaux and rises. Commonly pervasively ferruginised and/or silicified to chert. Is correlated with Narpa Group, Tindall and Montejinni Limestones. Is lateral equivalent of, and likely to be continuous under cover with, Top Springs Limestone. Numerous sedimentary structures listed. Thickness consistently 141-151m, thinning locally to 51m. Diverse fossil assemblage. Restricted marine shelf deposits, subject to episodic peritidal influence. Hosts an ore-grade (>15% P2O5) phosphorite horizon in the Wonarah area.||Barkly Group.||Disconformably overlies Helen Springs Volcanics, Renner or South Nicholson Groups, Andagera Formation (?transitionally). Conformably underlies Anthony Lagoon or (disconformably?) Wonarah Formations.|Commonly partially dolomitised, massive, ribbon, bioclast, lithoclast and minor oncoid limestone, and minor cryptomicrobial dololaminite and siliciclastic mudstone. Local thin basal siltstone or basal conglomerate.|12-JUL-16
7866|Gum Ridge Formation|69445|5|Briefly described|p30:5, 17|Middle Cambrian|Middle Cambrian|Central Georgina Basin.||||Unconformably overlies Helen Springs Volcanics (Kalkarindji Suite).||12-JUL-16
7866|Gum Ridge Formation|69446|5|Briefly described|p31:3-4|Middle Cambrian|Middle Cambrian|Georgina Basin. Broadly age-equivalent to Daly River Group (Daly Basin).||||Is overlain by Anthony Lagoon Formation.|Carbonate-dominated.|12-JUL-16
7866|Gum Ridge Formation|69447|6|Mentioned|p32:2|||Georgina Basin.||||Age-equivalent to Montejinni Limestone, Hooker Creek Formation and Lothari Hill Sandstone (Wiso Basin).||12-JUL-16
7866|Gum Ridge Formation|69448|6|Mentioned|p33:3|||Georgina Basin.||||Correlated with Negri Subgroup (Ord Basin) in part.||12-JUL-16
7866|Gum Ridge Formation|69591|5|Briefly described|p88|Cambrian|Cambrian|Undilla Sub-basin, Georgina Basin.||Barkly Group.||||
7866|Gum Ridge Formation|69673|5|Briefly described|p117, p142|||151m thick.||Barkly Group|||Dolomitised limestone, siliciclastic mudstone.|
7866|Gum Ridge Formation|70380|5|Briefly described|p745, p759|Stage 5|Stage 4|Barkly Sub-basin, Georgina Basin.||||Correlated with Tindall Limestone (Daly Basin).||
7866|Gum Ridge Formation|70752|5|Briefly described|p125, p127, p131, p137, p141|Middle Cambrian|Middle Cambrian|Georgina Basin. Contains at least two linguliform brachiopod species also found in Giles Creek Dolostone. Ordian age from the age-diagnostic trilobite Redlichia gumridgensis. Systematic palaeontological descriptions.||||||
7866|Gum Ridge Formation|70968|5|Briefly described|p112|Middle Cambrian|Middle Cambrian|Georgina Basin. The Lake Woods beds were originally mapped as part of this unit in HELEN SPRINGS (Randal et al., 1966) and BEETALOO (Brown and Randal, 1969) .||||||
7866|Gum Ridge Formation|72321|5|Briefly described|Fig 2|Stage 4|Stage 4|Western Georgina Basin.   Age Cambrian Series 2, Stage 4, Australian Stage: Ordian.||of Narpa Group.||Correlated with Hay River Formation,  Top Springs Limestone.||
7866|Gum Ridge Formation|72516|6|Mentioned|p91|Cambrian|Cambrian|Georgina Basin.||||Equivalent to the Thorntonia Limestone.||02-JUN-21
7866|Gum Ridge Formation|73083|6|Mentioned|p7, p22, p25|Cambrian|Cambrian|Contains macrofossils of trilobites and brachiopods.||||||
7869|Gum Tree Granite|24197|5|Briefly described|p60 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Age: 1728Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
7869|Gum Tree Granite|24540|6|Mentioned|p8|||Example of a rare earth element-bearing granite. Geological Province: Arunta region.||||||07-FEB-11
7869|Gum Tree Granite|38885|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
7869|Gum Tree Granite|39470|6|Mentioned|p43|||||||||
7869|Gum Tree Granite|39552|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
7869|Gum Tree Granite|39583|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
7869|Gum Tree Granite|39610|6|Mentioned|p6|||||||||
7869|Gum Tree Granite|39887|6|Mentioned|Fig.3|||||||||
7869|Gum Tree Granite|39888|6|Mentioned|p462|||See also Fig.10||||||
7869|Gum Tree Granite|42504|6|Mentioned|p65|||||||||
7869|Gum Tree Granite|42830|6|Mentioned|Fig.3 P155|||||||||
7869|Gum Tree Granite|48992|6|Mentioned|p22|||Variation of the acceptable name Gumtree.||||||
7869|Gum Tree Granite|50369|5|Briefly described|p1.4, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Wuluma Suite.||||||07-NOV-08
7869|Gum Tree Granite|60525|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block. Porphyritic biotite gneiss, equigranular granite in places, numerous acid dykes.||||||
7869|Gum Tree Granite|64329|5|Briefly described|p16|Proterozoic|Proterozoic|Allanite-bearing granite in the Arunta region.||||||29-JUL-08
7869|Gum Tree Granite|68994|6|Mentioned|p24|||||||||
7869|Gum Tree Granite|69931|6|Mentioned|p273, 275, 296|Paleoproterozoic|Paleoproterozoic|Arunta Inlier. REE analyses, Sm-Nd isotopic analyses, tabulated.|||||Granite.|
7881|Gunbatgari Complex|41406|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
7881|Gunbatgari Complex|43010|2|Defined|p55||Paleoproterozoic|Of Orosirian age.||||||07-NOV-08
7881|Gunbatgari Complex|67779|5|Briefly described|p26.|||Little-studied unit which outcrops poorly in a small inlier beneath the Kombolgie Subgroup, on Mann River. Correlated with the Nimbuwah Complex.|||||Migmatitic hornblende-biotite-bearing monzogranite with a granoblastic fabric.|
7935|Gwakura Formation|22538|6|Mentioned|Fig3 P708|||||||||
7935|Gwakura Formation|22600|4|Described|Map legend|Statherian|Statherian|||||||
7935|Gwakura Formation|24048|6|Mentioned|p62|||Of the Habgood Group.||||||25-SEP-06
7935|Gwakura Formation|24049|5|Briefly described|Map Legend|Statherian|Statherian|Of Habgood Group. Sandstone: mostly fine-grained, commonly dolomitic; siltstone: dolomitic; chert (silicified carbonate): microbially laminated; tuffaceous mudstone; basal conglomerate or pebbly lithic sandstone: polymict. Geol. Prov: McArthur Basin.||||||10-OCT-05
7935|Gwakura Formation|32660|5|Briefly described|Table 4|||||||||
7935|Gwakura Formation|42597|5|Briefly described|Map Legend|Carpentarian||||||||
7935|Gwakura Formation|43010|2|Defined|p137||Paleoproterozoic|Of Habgood Group. Of Statherian age.||||||07-NOV-08
7935|Gwakura Formation|44112|4|Described|p54,61-62|||||||||
7935|Gwakura Formation|61403|5|Briefly described|Map Legend|Statherian|Statherian|Of Habgood Group. Sandstone: mostly fine-grained, commonly dolomitic; siltstone: dolomitic; chert (silicified carbonate): microbially laminated; tuffa ceous mudstone; basal conglomerate or pebbly lithic sandstone: polymict. Geol. Prov: McArthur Basin.||||||
7935|Gwakura Formation|64817|6|Mentioned|p353 Fig.4 |||||Of the Habgood Group.||||
7935|Gwakura Formation|67323|6|Mentioned|Eastern Australia Time-Space Plot|||McArthur region. For reasons of space in the diagram, appears as Gwk Frm.||||||
7935|Gwakura Formation|69430|4|Described|p15:3, 20|||Walker Fault Zone, northern McArthur Basin. c.600m exposed thickness. Storm-dominated, marine shelf sediments. Top contact not exposed.||Habgood Group.||Disconformably overlies Ulunourwi Formation.|Basal polymict conglomerate or pebbly lithic sandstone; interbedded grey to red sandstone, mudstone, dolomitic mudstone, dolarenite, tuffaceous mudstone and stromatolitic chert after dolostone.|12-JUL-16
7935|Gwakura Formation|69673|6|Mentioned|p16 fig 13|||Walker Fault Zone||Habgood Group||Overlies Ulunourwi Formation||
7935|Gwakura Formation|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.||Upper Habgood Group.||||
7935|Gwakura Formation|72373|5|Briefly described|p22|Paleoproterozoic|Paleoproterozoic|Of northern McArthur Basin. Associated with northern Walker Fault Zone. Interpreted to be correlable with Bath Range Formation (Haines 1994; Haines et al 1999).||Unit of Habgood Group.||Uppermost unit of Habgood Group.||
7964|Habgood Group|22479|5|Briefly described|fig4, pg10|Statherian|Statherian|Figure shows Parsons Range Group underlies and Nathan Group overlies.||||||04-MAR-20
7964|Habgood Group|22538|4|Described|P710, P717|||Part of the Glyde package.||||||25-SEP-06
7964|Habgood Group|22600|4|Described|Map legend|Statherian|Statherian|||||||
7964|Habgood Group|22808|6|Mentioned|7 fig 4|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
7964|Habgood Group|23374|5|Briefly described|Fig3p5,6,34||Paleoproterozoic|Of McArthur Basin.||||||07-NOV-08
7964|Habgood Group|23937|5|Briefly described|p4 Fig. 4|||Part of the Glyde package (of Rawlings, 1999).  Parts correlate with Vizard Group.  Geological Province: McArthur Basin.  See also p95 Appendix 1.||||||27-OCT-04
7964|Habgood Group|24047|5|Briefly described|p12 Fig. 10, p11|Paleoproterozoic|Paleoproterozoic|Age: 1670-1600Ma.  Together with the Balma Group overlies the Parsons Range Group.  Geological Province: McArthur Basin.||||||07-NOV-08
7964|Habgood Group|24048|5|Briefly described|p98 App.1|||Geological Province: McArthur Basin||||||
7964|Habgood Group|24049|5|Briefly described|Map Legend|Statherian|Statherian|Includes Gwakura Formation, Ulunourwi Formation, Darwarunga Sandstone, Yarawoi Formation and Slippery Creek Siltstone. Geol. Prov: McArthur Basin.||||||13-OCT-05
7964|Habgood Group|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Overlies Parsons Range Group. Overlain by Balbarini Dolomite. Geological Province: Northern McArthur Basin.||||||
7964|Habgood Group|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
7964|Habgood Group|32660|4|Described|Table 4|||||||||
7964|Habgood Group|36473|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
7964|Habgood Group|37462|4|Described|Table4.IV|||||||||
7964|Habgood Group|37568|6|Mentioned|Fig.5|||||||||
7964|Habgood Group|41406|6|Mentioned|Map legend|Mesoproterozoic||||||||
7964|Habgood Group|42597|5|Briefly described|Map legend|Carpentarian||||||||
7964|Habgood Group|43010|2|Defined|p129-||Paleoproterozoic|Of Statherian age.||||||28-MAR-18
7964|Habgood Group|43292|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
7964|Habgood Group|44112|3|Fully described|p10,54-55,57||Statherian|Part of Supersequence 3. Redefined by Haines (1994)||||||
7964|Habgood Group|44299|6|Mentioned|p.11|||SD/53-7,8.||||||
7964|Habgood Group|60574|5|Briefly described|Map Legend|||Geological Province: McArthur Basin.||||||
7964|Habgood Group|61403|5|Briefly described|Map Legend|Statherian|Statherian|Includes Gwakura Formation, Ulunourwi Formation, Darwarunga Sandstone, Yarawoi Formation and Slippery Creek Siltstone. Geol. Prov: McArthur Basin.||||||
7964|Habgood Group|63866|5|Briefly described|p114, p116, p123|||Walker Fault Zone. Partially equivalent to the Vizard Group.||||Conformably overlies the Parsons Range Group.||
7964|Habgood Group|64724|5|Briefly described|p45 Fig.5, p46|Statherian|Statherian|McArthur Basin unit deposited as part of sedimentation in the Isa Superbasin (1660-1590 Ma)||||||
7964|Habgood Group|64817|6|Mentioned|p352 Fig.3, p353 Fig.4 ||||||Includes Gwakura Formation, Ulunourwi Formation, Darwarunga Sandstone, Yarawoi Formation, Slippery Creek Siltstone.|||
7964|Habgood Group|65228|6|Mentioned|p18|||1650 - 1630 Ma. Evidence of fault-controlled sedimentation.||||||
7964|Habgood Group|65340|6|Mentioned|p10 Fig.5.|||||||||
7964|Habgood Group|67323|5|Briefly described|p35|Paleoproterozoic|Paleoproterozoic|McArthur Basin.|||Slippery Creek Siltstone.|||
7964|Habgood Group|69417|6|Mentioned|p2:5|Statherian|Statherian|McArthur Basin.||||||12-JUL-16
7964|Habgood Group|69430|4|Described|p15:2-4, 14, 20-23|||Dunnet (1965); redefined by Plumb and Roberts (1992) and Haines (1994). Walker Fault Zone, northern McArthur Basin. Originally included the Kurala Sandstone which was later assigned (Haines, 1994) to the Parsons Range Group. No geochronological data: correlation with McArthur Group is tentative at best.|||Slippery Creek Siltstone; Yarawoi, Ulunourwi, Gwakura Formations; Darwarunga Sandstone.|Conformably overlies Kurala Sandstone (Parsons Range Group).|Fine-grained siliciclastic rocks and minor dolostone.|12-JUL-16
7964|Habgood Group|69673|6|Mentioned|p3 fig 2, p15, p16 fig 13, p46, p47|Statherian|Statherian|Walker Fault Zone|||Includes Gwakura Formation, Ulunourwi Formation, Darwarunga Sandstone, Yarawoi Formation, Slippery Creek Siltstone|Overlies Parsons Range Group||
7964|Habgood Group|70968|6|Mentioned|p2 Fig.3|||||||||
7964|Habgood Group|71059|6|Mentioned|p2|Paleoproterozoic|Paleoproterozoic|McArthur Basin.||||||
7964|Habgood Group|71374|4|Described|iii, p1 tbl 1, p2, p12|Mesoproterozoic|Palaeoproterozoic|Northern McArthur Basin. On the basis of SHRIMP ages is interpreted as broadly equivalent to the McArthur Group. Zircon provenance suggests derivation from a source region in the Arnhem Province. See also p14-p16, p26, p28, p30, p33.|||Includes the Yarawoi Formation, Darwarunga Sandstone and Ulunourwi Formation.|Overlain by the Nathan Group.||07-MAY-18
7964|Habgood Group|71606|5|Briefly described|p135,137-138|Statherian|Statherian|North Walker Trough, McArthur Basin. Evaporite-carbonate sequence.||||Underlain by Parsons Range Group. Correlatable to Balma Group and Vizard Formation.||04-MAR-20
7964|Habgood Group|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.||||||
7964|Habgood Group|72373|5|Briefly described|p2,6,9,11,15|Paleoproterozoic|Paleoproterozoic|Of northern McArthur Basin. Broadly equivalent to Glyde Package, McArthur and Vizard groups (McArthur Basin) and Limbunya group (Birrindude Basin).|||Includes Slippery Creek Siltstone, Ulunourwi Formation, Gwakura Formation.|||
7964|Habgood Group|72377|5|Briefly described|p15|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. Rawlings et al (1997) suggested that Mount Bonner Sandstone may be an attenuated lateral facies variant of the Habgood Group, deposited on the higher-relief flanks of the main depositional areas for this group.||||||
7964|Habgood Group|72718|6|Mentioned|p5 Tb.1|||McArthur Basin. Isa Superbasin of Jackson et al. (1999, 2000). Glyde package.||||||
8056|Hanson River beds|13995|5|Briefly described|p91, p101|||SE Wiso Basin. Contains possible vertebrate remains.||||Probable correlative of Stairway Sandstone.||
8056|Hanson River beds|23858|5|Briefly described|p917|||Overlain by Lake Surprise Sandstone. Geological Province: Wiso Basin.||||||25-SEP-06
8056|Hanson River beds|36335|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
8056|Hanson River beds|42059|5|Briefly described|Fig.2 P131|||||||||
8056|Hanson River beds|45148|2|Defined|p16|Ordovician|Ordovician|See also Fig.5.||||||
8056|Hanson River beds|45155|6|Mentioned|Fig.8|||||||||
8056|Hanson River beds|60684|6|Mentioned|p50 Appendix|||Possibly overlie part of the Point Wakefield beds?||||||
8056|Hanson River beds|64068|6|Mentioned|p226|||Wiso Basin. Correlated with Toko Group, Georgina Basin.||||||
8056|Hanson River beds|65333|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Wiso Basin. Cross-section only. Unconformably underlies Lake Surprise Sandstone. Fine-grained sandstone, claystone and silty claystone; glauconite and mica-bearing in part; dolostone and dolostone with siltstone laminae; marine.||||||
8056|Hanson River beds|65334|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Wiso Basin. Unconformably underlies Lake Surprise Sandstone. Fine-grained sandstone, claystone and silty claystone; glauconite and mica-bearing in part; dolostone and dolostone with siltstone laminae; marine.||||||
8056|Hanson River beds|65338|5|Briefly described|p5 Fig.3, p67, p71, 74|Arenig|Arenig|Wiso Basin.  May have potential as an aquifer.|||||Silcrete [??]|30-SEP-11
8056|Hanson River beds|65345|5|Briefly described|p7 Fig.6. |Ordovician|Late Cambrian|Wiso Basin. Over 500 m thick. Fluvial to shallow to restricted marine deposits.||||||
8056|Hanson River beds|69437|6|Mentioned|p22:10, 15|Ordovician||Wiso Basin. Has potential as a petroleum source rock.||||||12-JUL-16
8056|Hanson River beds|69443|6|Mentioned|p28:27|||Wiso Basin.||||Correlated with Toko Group.||12-JUL-16
8056|Hanson River beds|69447|4|Described|p32:2-3, 5-6, 9|Middle Ordovician|Early Ordovician|Milligan et al. (1966). Wiso Basin. Shallow marine to ?fluviatile deposits. 170m up to 800m thick. Poor exposures, mostly rubbly rises. Consists of four informal units, described in some detail. Contains fossils with affinities to Stairway Sandstone and Stokes Siltstone (Amadeus Basin). Correlated with the Pacoota Sandstone-Stokes Siltstone interval in the Georgina Basin. Has fair to good petroleum source rock potential. May have potential for reservoirs (sandstones) and seals (intraformational claystone).||||Unconformably overlies Point Wakefield beds. Is overlain unconformably by Lake Surprise Sandstone.|Fine to medium sandstone, siltstone, micaceous claystone, limestone, glauconitic dolostone, microbialite; fossiliferous (trilobites, brachiopods, molluscs, conodonts, ichnofossils); ooids.|12-JUL-16
8056|Hanson River beds|69673|5|Briefly described|ix, p143, p145|Ordovician|Ordovician|800m thick.||||Overlain by Lake Surprise Sandstone|Fossiliferous carbonates and sandstones, siltstone.|
8056|Hanson River beds|70380|6|Mentioned|p745|Ordovician|Ordovician|Wiso Basin.||||||
8056|Hanson River beds|73083|6|Mentioned|p14|Ordovician|Ordovician|||||||
8064|Harajica Sandstone Member|9814|5|Briefly described|Map Legend|Devonian|Devonian|Of the Parke Siltstone. Fine to coarse sandstone, rare pebbly sandstone, thin sandy siltstone.||||||
8064|Harajica Sandstone Member|22566|6|Mentioned|Fig 2 on p77|||Of the Parke Siltstone.  Also see Harajica Sandstone.||||||25-SEP-06
8064|Harajica Sandstone Member|22760|4|Described|p340|Devonian|Devonian|Of the Parke Siltstone.  Contains the greatest variety and abundance of fossil fish and hydrophyllic plants, indicating a Givetian to early Frasnian age.||||||25-SEP-06
8064|Harajica Sandstone Member|22761|6|Mentioned|p350|||Of  Parke Siltstone.||||||25-SEP-06
8064|Harajica Sandstone Member|22762|5|Briefly described|p377||Devonian|Of the Pertnjara Group.||||||25-SEP-06
8064|Harajica Sandstone Member|31566|2|Defined|p234|Devonian|Devonian|See also p235-236.||||||25-SEP-06
8064|Harajica Sandstone Member|32208|6|Mentioned|Map legend|Devonian|Devonian|||||||
8064|Harajica Sandstone Member|32209|6|Mentioned|Map legend|Devonian|Devonian|||||||
8064|Harajica Sandstone Member|32640|6|Mentioned|p236|||||||||
8064|Harajica Sandstone Member|35102|6|Mentioned|p39|||||||||
8064|Harajica Sandstone Member|41018|6|Mentioned|Fig.2|||||||||
8064|Harajica Sandstone Member|41270|6|Mentioned|p277|||||||||
8064|Harajica Sandstone Member|41385|6|Mentioned|p364|||||||||
8064|Harajica Sandstone Member|43225|5|Briefly described|Map Legend||Devonian|Of Pertnjara Group.||||||25-SEP-06
8064|Harajica Sandstone Member|43503|6|Mentioned|16-43|Late Devonian|Middle Devonian|||||||
8064|Harajica Sandstone Member|43647|6|Mentioned|Fig.7,p538|||||||||
8064|Harajica Sandstone Member|43648|6|Mentioned|Fig.27,p509|||||||||
8064|Harajica Sandstone Member|43649|5|Briefly described|Fig.6,p460,462|||||||||
8064|Harajica Sandstone Member|46928|6|Mentioned|Table 1|||||||||
8064|Harajica Sandstone Member|47050|5|Briefly described|p240|||||||||
8064|Harajica Sandstone Member|64809|6|Mentioned|p6 Fig.4 |Late Devonian|Late Devonian|||Of the Parke Siltstone.||||
8064|Harajica Sandstone Member|67565|5|Briefly described|p42.|Frasnian|Givetian|Contains a bothriolepid-phyllolepid placoderm asssemblage which was correlated by Young (1988) with Givetian-Frasnian strata previously mapped as Mereenie Sandstone.||Unit in Parke Siltstone.||Overlies Deering Siltstone Member. Is overlain by Dare Siltstone Member.|A uniform succession of cross-bedded and planar-bedded, fine to coarse sandstone in fining-upward cycles.|
8064|Harajica Sandstone Member|69438|3|Fully described|p23:7, 38-39|Famennian|Famennian|Jones (1972). Amadeus Basin. Type section is near Stokes Pass. Up to c.500m thick, thinning to the S and lensing out; is absent to the E of Ellery Creek. Age from placoderm plates which occur at several localities.||Parke Siltstone.||Conformably/gradationally overlies Deering Siltstone Member. Is conformably/gradationally overlain by Dare Siltstone Member.|A uniform succession of cross-bedded and planar-bedded, fine- to coarse-grained sandstone, with some mudclasts and rare subrounded clasts of quartzic sedimentary rocks derived from Mereenie Sandstone.|12-JUL-16
8064|Harajica Sandstone Member|69673|6|Mentioned|p67|||||Parke Siltstone||||
8085|Hardway Granite|24197|5|Briefly described|p21, p94 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Of the Kalkadoon Supersuite. Age: 1860Ma. Geological province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
8085|Hardway Granite|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||25-AUG-04
8085|Hardway Granite|30531|6|Mentioned|p20|||Also mention P22||||||
8085|Hardway Granite|33900|5|Briefly described|p23|||Mention P15||||||
8085|Hardway Granite|35074|6|Mentioned|Fig.2|||||||||
8085|Hardway Granite|35167|2|Defined|p153|Middle Precambrian|Middle Precambrian|||||||
8085|Hardway Granite|35458|6|Mentioned|p239|||Listing of new or revised names of units published recently.||||||
8085|Hardway Granite|36052|6|Mentioned|Fig.1|||||||||
8085|Hardway Granite|38235|6|Mentioned|p115|||||||||
8085|Hardway Granite|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
8085|Hardway Granite|40840|6|Mentioned|Map legend|||||||||
8085|Hardway Granite|45136|3|Fully described|p59|||Also mention P29.||||||
8085|Hardway Granite|45166|5|Briefly described|p19|||||||||
8085|Hardway Granite|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
8085|Hardway Granite|49041|5|Briefly described|Table 2|||||||||
8085|Hardway Granite|50536|5|Briefly described|p1.4 Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Kalkadoon Suite.||||||07-NOV-08
8085|Hardway Granite|67323|5|Briefly described|GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|Kalkadoon Igneous Event.||Kalkadoon Supersuite|||Coarse to medium-grained biotite granite, leucogranite, aplite, minor granodiorite.|
8085|Hardway Granite|69591|5|Briefly described|p60|||Kalkadoon Batholith.|||||Medium- to coarse-grained, biotite granite, leucogranite, aplite, minor granodiorite.|
8085|Hardway Granite|72596|5|Briefly described|p1-p3, p56-61|Orosirian|Orosirian|Mary Kathleen Domain. Geochronologic constraint is a magmatic crystallisation age . Forms 3 main bodies with a total area of ca. 19 km2. Outcrops of Hardway Granite had been included in the ca. 1860 Ma Kalkadoon Granodiorite by Carter et al. (1961; their Kalkadoon Granite), but were subsequently delineated as a discrete unit by Derrick et al. (1977) who vaguely alluded to an age of 1681+/- 68 Ma and the unit was described as intruding the Corella Formation. The new geochronology does not support this interpretation, but is consistent with that of Budd et al. (2001) who included the unit in the Kalkadoon-Leichhardt Suite.|1862 +/- 3 Ma SHRIMP U-Pb||||Includes monzogranite.|
8085|Hardway Granite|73413|6|Mentioned|App.1|Orosirian|Orosirian|U-Pb age of 1862 +/- 3 Ma reported by Kositcin et al. (2019).|1862 +/- 3 Ma|||||
8085|Hardway Granite|73553|5|Briefly described|p1, p6, p8 Fig.1.2.3, p10-13, p28|Orosirian|Orosirian|Included in Kalkadoon-Leichhardt Igneous Province based on geochronology. Crops out in three main bodies as a basement inlier in the Mary Kathleen Domain. Mapped by Carter et al., (1961) as Kalkadoon Granite (now Kalkadoon Granodiorite) and delineated by Derrick et al., (1977a) as Hardway Granite; these authors refer to an age of 1681+/-68 Ma and an Rb-Sr age of 1645+/-67 Ma, described unit as intruding the Corella Formation [at odds with more recent isotopic dating]. Included in Kalkadoon Supersuite (1860 Ma) by Budd et al., (2001) on the basis of geochemistry. Appears as distinct magnetic lows in airborne TMI images, parts are slightly magnetic. Yellowish to slightly greenish tones in radiometric images. Intruded by a mafic intrusive phase or phases which have irregular but sharp contacts with the granite.|1862+/-3 Ma zircon U-Pb SHRIMP||||Heterogeneous in composition and fabric; dominated by mildly deformed, medium- to coarse-grained, equigranular biotite-amphibolite monzogranite to syenogranite. Locally contains leucogranite, aplite, pegmatite.|03-FEB-23
8127|Harts Range pegmatite|9694|5|Briefly described|Map Legend|Paleozoic|Paleozoic|Zoned or partly zoned pegmatite with quartz core, microline zone, plagioclase-muscovite wall zone and fine grained quartz mica border zone. Spatially associated with Irindina Gneiss. Geological Province: Arunta Block.||||||29-AUG-14
8127|Harts Range pegmatite|39898|5|Briefly described|Map legend|Paleozoic|Paleozoic|Pegmatite. Geological Province: Arunta Block.||||||07-NOV-08
8127|Harts Range pegmatite|39931|6|Mentioned|Map legend|Paleozoic|Proterozoic|Proterozoic to Palaeozoic||||||07-NOV-08
8127|Harts Range pegmatite|40538|6|Mentioned|Map legend|Paleozoic|Paleozoic|Pegmatite, poorly to well zoned with quartz core. Informal name.||||||07-NOV-08
8127|Harts Range pegmatite|48880|14|Not recorded|p.29|Devonian|Silurian|Silurian-U.Devn. 420-367 m.y.||||||
8127|Harts Range pegmatite|68517|5|Briefly described|Map Legend|Palaeozoic|Palaeozoic|Arunta Block.|||||Pegmatite with minor granite.|
8127|Harts Range pegmatite|69925|6|Mentioned|p38-39, 41|||Arunta Inlier.|520 +5/-4 Ma (Mortimer et al., 1987).|||||
8130|Haslingden Group|22457|5|Briefly described|p31, Fig30 p31|||Shown as Upper and Lower Haslingden Group in Fig29 p30.||||||04-APR-18
8130|Haslingden Group|22483|6|Mentioned|Table 2 p416.|||||||||
8130|Haslingden Group|22644|5|Briefly described|3,4,12|||Geol. province: McArthur Basin. Max thickness 17,000 m.||||||18-JAN-07
8130|Haslingden Group|22665|6|Mentioned|P220||Statherian|||||||
8130|Haslingden Group|23031|6|Mentioned|18|Proterozoic|Proterozoic|||||||
8130|Haslingden Group|23073|6|Mentioned|p744|||||||||
8130|Haslingden Group|23393|5|Briefly described|p18, p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Fold Belt.||||||07-NOV-08
8130|Haslingden Group|23395|4|Described|p384 Fig.2|||||||||
8130|Haslingden Group|23396|5|Briefly described|p407 Fig.2|||||||||
8130|Haslingden Group|23408|6|Mentioned|p512|||Mentioned only in the context of "......geological evolution of post-Haslingden group sedimentary rocks on the Lawn Hill Platform" (Hutton and Sweet 1982)..||||||15-JUN-09
8130|Haslingden Group|23965|4|Described|p1296|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier.||||||07-NOV-08
8130|Haslingden Group|23969|6|Mentioned|p1371 Fig.2|||Geological Province: Mount Isa Inlier.||||||
8130|Haslingden Group|24034|5|Briefly described|p9|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier. Feldspar sandstones, tuff, siltstone, quartzite and meta-basalt.||||||
8130|Haslingden Group|24419|5|Briefly described|p16, p14, p15 Fig. 6|Paleoproterozoic|Paleoproterozoic|Includes Myally Subgroup, Eastern Creek Volcanics, Jayah Creek and Oroopa Metabasalts, Mount Guide and Leander Quartzites and May Downs Gneiss Member.  See also misspelt Hasllngden Group (p13 Fig.5). Geol.Prov: Leichardt Superbasin. See also p13 Fig. 5.||||||07-NOV-08
8130|Haslingden Group|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|Includes the Myally Subgroup, Eastern Creek Volcanics and Mount Guide Quartzite.||||||25-AUG-04
8130|Haslingden Group|30530|6|Mentioned|p516|||||||||
8130|Haslingden Group|30531|6|Mentioned|p15|||||||||
8130|Haslingden Group|30534|2|Defined|p305|Carpentarian|Carpentarian|||||||
8130|Haslingden Group|30535|6|Mentioned|p403|||||||||
8130|Haslingden Group|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
8130|Haslingden Group|31342|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
8130|Haslingden Group|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
8130|Haslingden Group|32660|4|Described|Table 5|||||||||
8130|Haslingden Group|33111|6|Mentioned|p5|||||||||
8130|Haslingden Group|33900|4|Described|p10|||Mention p4.||||||25-SEP-06
8130|Haslingden Group|35074|6|Mentioned|Fig.2|||||||||
8130|Haslingden Group|35286|6|Mentioned|p145|||||||||
8130|Haslingden Group|35295|6|Mentioned|p601|||Also mentioned p603.||||||15-MAR-18
8130|Haslingden Group|35369|6|Mentioned|PB5|||||||||
8130|Haslingden Group|35495|6|Mentioned|p341|||||||||
8130|Haslingden Group|35950|6|Mentioned|p305|||||||||
8130|Haslingden Group|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
8130|Haslingden Group|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
8130|Haslingden Group|36733|6|Mentioned|p21|||||||||
8130|Haslingden Group|37217|6|Mentioned|Fig.1|||||||||
8130|Haslingden Group|37413|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
8130|Haslingden Group|37459|6|Mentioned|p423|||||||||
8130|Haslingden Group|37462|4|Described|Table4.VII|||||||||
8130|Haslingden Group|37565|5|Briefly described|p2|||See also Fig.5||||||
8130|Haslingden Group|37568|4|Described|p81|||See also p85.||||||25-SEP-06
8130|Haslingden Group|37816|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
8130|Haslingden Group|37862|6|Mentioned|p581|||||||||
8130|Haslingden Group|38232|6|Mentioned|p81|||||||||
8130|Haslingden Group|38233|6|Mentioned|p93|||||||||
8130|Haslingden Group|38235|6|Mentioned|p113|||||||||
8130|Haslingden Group|38237|6|Mentioned|p125|||||||||
8130|Haslingden Group|38276|6|Mentioned|Fig.1|||||||||
8130|Haslingden Group|38278|6|Mentioned|Fig.1|||||||||
8130|Haslingden Group|38350|4|Described|p9|||||||||
8130|Haslingden Group|38442|5|Briefly described|Map legend|Proterozoic|Proterozoic|Includes the Eastern Creek Volcanics and Mount Guide Quartzite.||||||25-AUG-04
8130|Haslingden Group|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
8130|Haslingden Group|38560|6|Mentioned|p114|||||||||
8130|Haslingden Group|38598|6|Mentioned|p197|||||||||
8130|Haslingden Group|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
8130|Haslingden Group|38833|6|Mentioned|p161|||||||||
8130|Haslingden Group|38835|6|Mentioned|p163|||||||||
8130|Haslingden Group|38836|6|Mentioned|p165|||||||||
8130|Haslingden Group|38900|6|Mentioned|p55|||||||||
8130|Haslingden Group|38919|6|Mentioned|p493|||||||||
8130|Haslingden Group|39202|6|Mentioned|Fig.2|||||||||
8130|Haslingden Group|39362|6|Mentioned|Fig.1|||||||||
8130|Haslingden Group|39445|5|Briefly described|p40|||See also p39 and Table 2.||||||25-SEP-06
8130|Haslingden Group|39556|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||
8130|Haslingden Group|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||15-JUN-06
8130|Haslingden Group|39622|6|Mentioned|p19|||See also Fig.2||||||
8130|Haslingden Group|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
8130|Haslingden Group|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
8130|Haslingden Group|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
8130|Haslingden Group|40105|6|Mentioned|p310|||||||||
8130|Haslingden Group|40202|6|Mentioned|p719|||||||||
8130|Haslingden Group|40221|3|Fully described|p6|||||||||
8130|Haslingden Group|40598|6|Mentioned|p31|||||||||
8130|Haslingden Group|40840|6|Mentioned|Map legend|||||||||
8130|Haslingden Group|41248|5|Briefly described|p69|||||||||
8130|Haslingden Group|41277|6|Mentioned|p83|||||||||
8130|Haslingden Group|41298|6|Mentioned|Map legend|Carpentarian||||||||
8130|Haslingden Group|41307|4|Described|p8|||||||||
8130|Haslingden Group|41381|6|Mentioned|p323|||||||||
8130|Haslingden Group|41465|6|Mentioned|p11|||||||||
8130|Haslingden Group|41744|6|Mentioned|Fig.1|||||||||
8130|Haslingden Group|41791|6|Mentioned|p266|||||||||
8130|Haslingden Group|41978|6|Mentioned|p490|||||||||
8130|Haslingden Group|41979|6|Mentioned|p523|||||||||
8130|Haslingden Group|42234|5|Briefly described|p1055|||||||||
8130|Haslingden Group|42342|6|Mentioned|p23|||||||||
8130|Haslingden Group|42367|5|Briefly described|p17, p18||Proterozoic|||||||
8130|Haslingden Group|42503|5|Briefly described|p336|||||||||
8130|Haslingden Group|42523|5|Briefly described|p372|||||||||
8130|Haslingden Group|42565|4|Described|Table 1 P5, P2|||||||||
8130|Haslingden Group|42676|5|Briefly described|Fig.2 p41|||||||||04-APR-18
8130|Haslingden Group|42706|5|Briefly described|map legend|Proterozoic|Proterozoic|Includes May Downs Gneiss, Mount Guide Quartzite, Eastern Creek Volcanics and the Myally Subgroup.||||||09-FEB-09
8130|Haslingden Group|42782|6|Mentioned|p457|||||||||
8130|Haslingden Group|42812|6|Mentioned|p65|||||||||
8130|Haslingden Group|42818|4|Described|p206, Fig.2 p205|||||||||
8130|Haslingden Group|43561|6|Mentioned|p1438|||||||||
8130|Haslingden Group|43595|5|Briefly described|p439|||||||||
8130|Haslingden Group|43760|5|Briefly described|p431|||||||||
8130|Haslingden Group|43788|6|Mentioned|p20|||||||||
8130|Haslingden Group|44195|6|Mentioned|p356 Fig.9|||||||||
8130|Haslingden Group|45136|4|Described|Table 1|||Also mention p2.||||||25-SEP-06
8130|Haslingden Group|45161|4|Described|p22|||See also p11.||||||25-SEP-06
8130|Haslingden Group|45162|6|Mentioned|p11|||||||||
8130|Haslingden Group|45166|4|Described|p14|||||||||
8130|Haslingden Group|46801|6|Mentioned|p115|||See also Table 1 and Fig.14.||||||
8130|Haslingden Group|46859|6|Mentioned|p313|||||||||
8130|Haslingden Group|46919|6|Mentioned|p213|||||||||
8130|Haslingden Group|46960|6|Mentioned|p218|||||||||
8130|Haslingden Group|46962|4|Described|Table 1|||See also Fig.3.||||||
8130|Haslingden Group|46995|5|Briefly described|p267|||||||||
8130|Haslingden Group|46996|6|Mentioned|p273|||||||||
8130|Haslingden Group|47083|4|Described|p5-10||Proterozoic|Includes Myally Subgroup. Overain by Quilalar Formation.||||||25-SEP-06
8130|Haslingden Group|49041|5|Briefly described|Table 1|||||||||
8130|Haslingden Group|50100|5|Briefly described|p11, p13 Fig. 4|Statherian|Statherian|Contains the Myally Subgroup.  Unconformably overlies the Bottletree Formation. Geological Province: Western Fold Belt Province.||||||11-FEB-09
8130|Haslingden Group|50332|6|Mentioned|p16|Paleoproterozoic|Paleoproterozoic|Age: 1800-1755Ma.||||||07-FEB-11
8130|Haslingden Group|50624|4|Described|p234 Fig.2||Paleoproterozoic|Overlain by Mount Isa Group.||||||07-NOV-08
8130|Haslingden Group|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Includes: Eastern Creek Volcanics, Mount Guide Quartzite, Judenan Beds.||||||
8130|Haslingden Group|61204|5|Briefly described|p537-538|Statherian|Paleoproterozoic|Geological Province: Mount Isa Inlier. Age: 1710 +/- 25 Ma. Includes Mount Guide Quartzite and Eastern Creek Volcanics.||||||07-NOV-08
8130|Haslingden Group|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: <1800Ma. Geological Province: western Mount Isa Block.||||||07-NOV-08
8130|Haslingden Group|61735|5|Briefly described|p658|||Includes the Argylla Formation. Geological province: Mount Isa Inlier.||||||30-JUN-09
8130|Haslingden Group|61736|5|Briefly described|p673, p674|Paleoproterozoic|Paleoproterozoic|Age: </-1790Ma. Sediments.||||||
8130|Haslingden Group|61923|5|Briefly described|p28 Fig.1|||Includes the Eastern Creek Volcanics. Intruded by Sybella Granite. Geological Province: Mount Isa Inlier.||||||
8130|Haslingden Group|62535|5|Briefly described|p673-674||||c.1790 Ma.|||||
8130|Haslingden Group|62536|6|Mentioned|p658|||Mount Isa Inlier.|||Argylla Formation.|||
8130|Haslingden Group|62873|5|Briefly described|p692|Paleoproterozoic|Paleoproterozoic|Mafic igneous rocks. Comprises Mount Guide Quartzite and Eastern Creek Volcanics. Intruded by the Sybella Batholith. Geological Province: Mount Isa Inlier.||||||07-NOV-08
8130|Haslingden Group|63023|5|Briefly described|p1024 Fig. 1, p1025 Fig. 2|||Comprises Eastern Creek Volcanics, Mount Guide Quartzite and the Myally Subgroup. Geological Province: Leichhardt Superbasin.||||||30-APR-13
8130|Haslingden Group|63113|5|Briefly described|p1214 Fig.2.|||Leichhardt Superbasin.|||Includes the Bottle Tree Formation, Mount Guide Quartzite, Eastern Creek Volcanics, Alsace Quartzite and Bortala Formation.|||
8130|Haslingden Group|64250|5|Briefly described|p11 fig 3, p19, p22, p23|||Age 1773 +/- 2 Ma from Myally Subgroup in upper part of Group.|c.1790 - c.1770 Ma.||Mount Guide Quartzite, Eastern Creek Volcanics, Myally Subgroup|||15-MAR-18
8130|Haslingden Group|64367|5|Briefly described|p555  Fig. 1c|Paleoproterozoic|Paleoproterozoic|Comprises Mount Guide Quartzite, Eastern Creek Volcanics and Quilalar Formation at the top. Age range: ca.1785Ma to 1763+/-8Ma.||||||07-FEB-11
8130|Haslingden Group|64725|6|Mentioned|p58 Fig.2. |||Mount Isa Inlier.||||||
8130|Haslingden Group|64832|5|Briefly described|p1154, p1155 Figs. 2, 3|Paleoproterozoic|Paleoproterozoic|Comprises Eastern Creek Volcanics, Mount Guide Quartzite and Myally Subgroup. Age ranges from ca.1785Ma to ca.1775Ma. Geological Province: Mt Isa Inlier.||||||07-FEB-11
8130|Haslingden Group|65337|5|Briefly described|p5, p11. |||Leichhardt Superbasin; Leichhardt River Fault Trough.|||Includes Myally Subgroup.|Overlies Bottletree Formation.||
8130|Haslingden Group|65387|6|Mentioned|p60|||Deposition of this unit is suggested to represent the unconformity between Argylla suite and Ballara Quartzite to the east.||||||
8130|Haslingden Group|65396|5|Briefly described|p82, p173, p175, p187, p193, p196, p241|||Cover Sequence 2, Western Fold Belt, Mount Isa Inlier.|c.1790-1770 Ma.||Includes Eastern Creek Volcanics, Mount Guide Quartzite, Myally Subgroup|Overlain by Quilalar Formation.||03-APR-17
8130|Haslingden Group|66824|6|Mentioned|p133|Paleoproterozoic|Paleoproterozoic|||||Is intruded by Sybella Granite.|Metavolcanic and metasedimentary units.|
8130|Haslingden Group|67026|6|Mentioned|p336 Fig. 2 & 3.|Proterozoic|Proterozoic||||Includes Mount Guide Quartzite, Eastern Creek Volcanics and Myally Subgroup.|||
8130|Haslingden Group|67323|5|Briefly described|Solid Geology Map, p11, p39, p107|||See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Mount Oxide Domain, Mount Isa Inlier. Small positive magnetic anomalies may indicate lower Haslingden Group beneath cover. See also references to Lower Haslingden Group (GIS attrib tbl, sol geol.; p107).|||Myally Subgroup, Eastern Creek Volcanics, Jayah Creek Metabasalt, Leander Quartzite, Mount Guide Quartzite.||Quartz, sandstone, feldspathic sandstone, metabasalt.|
8130|Haslingden Group|67499|6|Mentioned|p937, p938|||Western Fold Belt|||Eastern Creek Volcanics, Myally Subgroup, Mount Guide Quartzite.|||
8130|Haslingden Group|68542|6|Mentioned|p10|Paleoproterozoic|Paleoproterozoic||||Includes Eastern Creek Volcanics|||
8130|Haslingden Group|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province.||||Conformably overlies Bottletree Formation.||
8130|Haslingden Group|68576|5|Briefly described|Q_2: p10, p13|Proterozoic|Proterozoic|Leichhardt River Fault Trough. Deposited over 25 to 30 m.y.|||Eastern Creek Volcanics.|||
8130|Haslingden Group|68732|6|Mentioned|p159, p160, p164||||||Mount Guide, Alsace, Whitworth Quartzites; Bortala, Bottletree, Lochness Formations.|||30-NOV-17
8130|Haslingden Group|69370|6|Mentioned|p307 Fig.2|Statherian|Statherian|Western Fold Belt, Mount Isa Block.|||Includes Mount Guide Quartzite and Myally Subgroup.|||25-JAN-19
8130|Haslingden Group|69430|6|Mentioned|p15:9|||Isa Superbasin.||||May be contiguous with Tawallah Group (McArthur Basin).||12-JUL-16
8130|Haslingden Group|69542|5|Briefly described|p132, p134-135, p142|Mesoproterozoic|Paleoproterozoic|Blake and Stewart (1988). Western Fold Belt.|||Includes Eastern Creek Volcanics.||Sandstone and tholeiitic basalt interbedded with pelitic, psammopelitic and psammitic rocks.|09-FEB-18
8130|Haslingden Group|69591|5|Briefly described|p29, p41, p57|Paleoproterozoic|Paleoproterozoic|Mount Isa Province. Part of Myally and Guide Supersequences.|||Myally Subgroup; Eastern Creek Volcanics, Jayah Creek Metabasalt, Leander Quartzite, Mount Guide Quartzite.|||
8130|Haslingden Group|70283|5|Briefly described|p24-25|Paleoproterozoic|Paleoproterozoic|Leichhardt River fault trough, Western fold belt, Mount Isa Inlier. Is intruded by the 1660-1655 Ma Sybella batholith.|||Includes Eastern Creek Volcanics|Overlies Bottletree Formation; overlain by Mount Isa Group.|Sandstones, amphibolite, metasediments and chlorite schist.|14-FEB-18
8130|Haslingden Group|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic||||Myally Subgroup, Eastern Creek Volcanics.|||
8130|Haslingden Group|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic||||Myally Subgroup, Eastern Creek Volcanics.|||
8130|Haslingden Group|70864|6|Mentioned|p74 Fig 2|||Shown as Lower Haslingden Group.|||?Includes Myall Subgroup?|||
8130|Haslingden Group|70897|6|Mentioned|p41|||Mount Isa Inlier. Matches the age of some 1780-1770 Ma zircons extracted from Mullera Formation.||||||
8130|Haslingden Group|71606|5|Briefly described|p137|Statherian|Statherian|Lawn Hill Platform and Leichardt River Fault Trough, Mount Isa Inlier. Age from Blake and Stewart, 1992.|1790-1760 Ma|||Overlain by Myally Subgroup. Underlain by Leichardt Volcanics and Kalkadoon Granite. Equivalent to Eastern Creek Volcanics.||
8130|Haslingden Group|71960|5|Briefly described|p77, 86, 87|Proterozoic|Proterozoic|Provenence of basal part shown to be from east.|||Includes Leander Quartzite, Eastern Creek Volcanics, Myally Subgroup.|Unconformably overlain/truncated by Mount Isa Group.||
8130|Haslingden Group|71980|5|Briefly described|map legend sheet 1|Proterozoic|Proterozoic||||Includes Leander Quartzite, Eastern Creek Volcanics, Myally Subgroup.|Unconformably underlies Mount Isa Group.|Quartzite, metabasalt, sandstone, basalt, arkose, sandstone, siltstone.|03-APR-19
8130|Haslingden Group|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Leichhardt River Domain.|||Includes Mount Guide Quartzite, Eastern Creek Volcanics and Myally Subgroup|Shown as older than Quilalar Formation.|Includes variably feldspathic and lithic sandstone, siltstone and minor conglomerate and metavolcanic rocks. Metabasalt (locally amygdaloidal), quartzite, tuff and pelitic schist epidotic quartzite, sericitic, feldspathic and quartzose rocks.|
8130|Haslingden Group|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Leichhardt River Domain.|||Includes Mount Guide Quartzite, Eastern Creek Volcanics and Myally Subgroup|Shown as older than Quilalar Formation.|Includes variably feldspathic and lithic sandstone, siltstone and minor conglomerate and metavolcanic rocks. Metabasalt (locally amygdaloidal), quartzite, tuff and pelitic schist epidotic quartzite, sericitic, feldspathic and quartzose rocks.|
8130|Haslingden Group|72889|6|Mentioned|p6 Fig.i.|||||||||
8130|Haslingden Group|73137|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|||||||
8130|Haslingden Group|73413|6|Mentioned|p3|||Mount Isa Inlier, Western Fold Belt.||||||
8130|Haslingden Group|73525|6|Mentioned|p4-5 Fig.2, p19 Fig.13, p20|||Mount Oxide-(Ardmore-May Downs) Domain.|||||Mafic extrusives.|
8130|Haslingden Group|73553|6|Mentioned|p177 Tb.5.9.1|||Contains mafic intrusive rocks.||||||
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|||||||||
8195|Hay River Formation|8217|5|Briefly described|Map Legend|Cambrian|Cambrian|Limestone and chert overlying black pyritic shale, shelly dolomite at base.||||||
8195|Hay River Formation|12951|6|Mentioned|p143|||Probably obsolete name for rocks now included in part in the Thorntonia Limestone (lower part) and Arthur Creek Formation (upper part), Georgina Basin.||||||
8195|Hay River Formation|35798|2|Defined|p312|Middle Cambrian|Middle Cambrian|||||||
8195|Hay River Formation|39921|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
8195|Hay River Formation|40810|6|Mentioned|p5|||||||||
8195|Hay River Formation|40856|5|Briefly described|p316|||||||||
8195|Hay River Formation|41388|6|Mentioned|p557|||||||||
8195|Hay River Formation|41524|6|Mentioned|p17|||||||||
8195|Hay River Formation|41532|6|Mentioned|p301|||||||||
8195|Hay River Formation|41594|6|Mentioned|p49|||||||||
8195|Hay River Formation|42956|5|Briefly described|p31 Fig.4|||||||||
8195|Hay River Formation|43105|5|Briefly described|Fig.4,p9.|||||||||
8195|Hay River Formation|45155|6|Mentioned|Fig.8|||||||||
8195|Hay River Formation|47035|6|Mentioned|p85|||||||||
8195|Hay River Formation|49027|4|Described|p7|||||||||
8195|Hay River Formation|60122|5|Briefly described|p15|Middle Cambrian|Middle Cambrian|Name abandoned. Formerly divided into 3 discrete packages - the "Lower H. R. Formation", the "Upper H. R. Formation Member 1" and the "Upper H. R. Formation Member 2". Now assigned to Thorntonia Limestone and Arthur Creek Formation.||||||17-MAY-05
8195|Hay River Formation|63450|4|Described|p78 Fig. 5, p80|Middle Cambrian|Middle Cambrian|Subdivided into lower, middle and upper Hay River Formation. Unconformably overlies Red Heart Dolomite; conformably overlain by Marqua Formation. Max. thickness: 100m. Geological province: Georgina Basin, West Toko Syncline.||||||07-FEB-11
8195|Hay River Formation|64068|5|Briefly described|p57, 59, p18, p44, p151-152, 225|||Lower Hay River Formation and Upper Hay River Formation, Member 1, of Shergold in Walter et al (1979), replaced by Thorntonia Limestone.  Upper Hay River Formation, Member 2 replaced  by Arthur Creek Formation. Ground SIROTEM surveys identified conductors in the basal part of this unit, but subsequent drilling did not support the interpretation.||||||
8195|Hay River Formation|65489|6|Mentioned|p124|Middle Cambrian|Middle Cambrian|Georgina Basin.||||||
8195|Hay River Formation|67402|6|Mentioned|p213 fig GRG3|Templetonian|Ordian|Georgina Basin. ||||Unconformably overlies the Red Heart Dolomite. Unconformably overlain by the Arrinthrunga Formation, Georgina Limestone or the Marqua beds.||
8195|Hay River Formation|69206|6|Mentioned|p1-2|||Georgina Basin. A hydrocarbon source and reservoir.||||||
8195|Hay River Formation|69673|6|Mentioned|p122|||Previously abandoned name, reinstated the name to refer to the calcareous deposits at the base of the Narpa group.||||||
8195|Hay River Formation|70723|6|Mentioned|p22, p29, p31|||Name superseded by Thorntonia Limestone.||||||
8195|Hay River Formation|70752|6|Mentioned|p129, p141|Middle Cambrian|Middle Cambrian|Georgina Basin. Ordian. Brachiopod systematic palaeontological descriptions.||||||
8195|Hay River Formation|72321|4|Described|Fig 2, p4, 6, 7|Stage 4|Stage 4|Of Walter et al., 1979. Name reinstated here. Elkedra Shelf/Dulcie Syncline, Toko Syncline, Burke River Structural Belt, Georgina Basin.  Previously included in Thorntonia Limestone, but separated here, across southern portion of the basin, due to older age. Age Cambrian Series 2, Stage 4, Australian Stage: Ordian.||of Narpa Group.||Unconformably overlain by Arthur Creek Formation. Correlated with Top Springs Limestone, Gum Ridge Formation.||
8195|Hay River Formation|73418|5|Briefly described|p4 Fig.3|Cambrian Series 2|Cambrian Series 2|Georgina Basin, Burke River Structural Belt and Undilla Sub-basin.||Narpa Group||Underlies Thorntonia Limestone|Limestone.|
8199|Hayward Creek Formation|23363|5|Briefly described|351 Tab.2|Statherian|Statherian|Age: 1784+/-7Ma.||||||25-SEP-06
8199|Hayward Creek Formation|23410|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Includes Blanche Creek Member. Of Tomkinson Creek Subgroup, Churchills Head Group. Undifferentiated lithic and sublithic arenite; feldspathic sublitharenite; pebbly arenite; shale; deeply weathered, acid to intermediate volcanic rocks.||||||07-NOV-08
8199|Hayward Creek Formation|23733|3|Fully described|p9|||Of Tomkinson Creek Group. Includes the Manga Mauda, Meerie and Coodna Members.||||||
8199|Hayward Creek Formation|24047|5|Briefly described|p7 Fig. 6, p60|Paleoproterozoic|Paleoproterozoic|Age: 1780Ma.  Geological Province: Ashburton Province (Tennant Inlier).||||||07-NOV-08
8199|Hayward Creek Formation|24172|3|Fully described|p26, p6-7 Tb.1, p65-66 Tb. 9|Paleoproterozoic|Paleoproterozoic|Of the Tomkinson Creek Subgroup. Conformably overlain by Morphett Creek Formation; conformably underlain by Brumbreu Formation. Geological Province: Tennant Creek Inlier. Max. Thickness ~3000m. Maximum Age: 1784+/-9Ma.||||||07-NOV-08
8199|Hayward Creek Formation|24197|5|Briefly described|p25|Paleoproterozoic|Paleoproterozoic|Of the Tomkinson Subgroup in the Treasure Suite. Felsic to intermediate volcanics. Geological province: Tennant Creek Province.||||||07-FEB-11
8199|Hayward Creek Formation|24303|3|Fully described|p3, p4 Tb.1|Proterozoic|Proterozoic|Of the Tomkinson Creek Group. Max. Thickness: ~3500m. Part of the Lower Tomkinson Creek Group. Overlies the Flynn Group disconformably (?). Subdivided into Manga Mauda, Meerie, Coodna and Whittington Range Members.||||||14-APR-15
8199|Hayward Creek Formation|24304|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Tomkinson Creek Group.  Includes the Coodna, Meerie and Manga Mauda  Members as well as a lower and upper sandstone facies and undifferentiated rock.||||||07-NOV-08
8199|Hayward Creek Formation|24442|5|Briefly described|p14|||Of the Tomkinson Creek Group.  Geological Province: Ashburton Province.||||||
8199|Hayward Creek Formation|31637|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
8199|Hayward Creek Formation|32174|6|Mentioned|Map legend|Carpentarian|Paleoproterozoic|Early Proterozoic to Carpentarian||||||07-NOV-08
8199|Hayward Creek Formation|35125|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
8199|Hayward Creek Formation|35229|4|Described|Table.1|||||||||
8199|Hayward Creek Formation|35771|2|Defined|p22|early Carpentarian|early Carpentarian|Appendix.||||||
8199|Hayward Creek Formation|39624|5|Briefly described|Table 2|||||||||
8199|Hayward Creek Formation|43223|5|Briefly described|Map Legend||Paleoproterozoic|Of Tomkinson Creek Subgroup.||||||07-NOV-08
8199|Hayward Creek Formation|43224|5|Briefly described|Map legend||Proterozoic|Of Tomkinson Creek Subgroup.||||||25-SEP-06
8199|Hayward Creek Formation|43751|6|Mentioned|p611|||U-Pb age: 1795+/-8 Ma.||||||25-SEP-06
8199|Hayward Creek Formation|50353|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Tomkinson Creek Group.||||||07-NOV-08
8199|Hayward Creek Formation|50588|5|Briefly described|p3.1|||Geological Province: Tennant Creek/Davenport Province. Includes: Treasure Suite (?).||||||25-SEP-06
8199|Hayward Creek Formation|60684|5|Briefly described|p5 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Tomkinson Creek Subgroup (Churchills Head Gp). Lithic and sublithic arenite; feldspathic sublitharenite, pebbly sandstone; siltstone; volcanics.Conformably underlies Morphett Creek Fm; transitional over Brumbreu Formation. Max. thickness: ~3000m.||||||07-NOV-08
8199|Hayward Creek Formation|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Tomkinson Creek Group.  Includes the Blanche Creek, Manga Mauda, Meerie, Coodna and Whittington Range Members. In the Tennant Creek region.||||||07-NOV-08
8199|Hayward Creek Formation|64780|6|Mentioned|p69|||||||||
8199|Hayward Creek Formation|64817|6|Mentioned|p367|||Tomkinson Creek Province.||||||
8199|Hayward Creek Formation|65209|5|Briefly described|p35 Fig.1, p37|Paleoproterozoic|Paleoproterozoic|Geol. Prov: Tomkinson Creek Province.||Tomkinson Creek Group|Whittington Range Member, Coodna Member, Meerie Member, Manga Mauda Member and Blanche Creek Member|||
8199|Hayward Creek Formation|65222|5|Briefly described|p116 Tb 3, p122, 123, 126|Statherian|Statherian|Maximum depositional age given. Detrital data also obtained, showing Warramunga Formation as likely source rock.|1784+/- 7 Ma U/Pb SHRIMP.|Of Tomkinson Creek Subgroup|||Includes quartzite.|24-JAN-22
8199|Hayward Creek Formation|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Tomkinson Creek Group.|Includes Blanche Creek, Manga Mauda, Meerie, Coodna and Whittington Range Members.|||
8199|Hayward Creek Formation|69187|6|Mentioned|p53 Fig.2, p54 Fig.3|||Tomkinson Province.||||||
8199|Hayward Creek Formation|69424|5|Briefly described|p9:2-5, 16, 19, 26-28, 39 Fig.9.24|Paleoproterozoic|Paleoproterozoic|Tomkinson Province. Maximum deposition age from detrital zircons, consistent with reworking of upper Ooradidgee Group material.|1823 Ma (Compston, 1995).|Tomkinson Creek Group.|Whittington Range, Blanche Creek, Manga Mauda Members.|Conformably (locally unconformably or faulted) overlies Brumbreu Formation (Ooradidgee Group).||12-JUL-16
8199|Hayward Creek Formation|69425|5|Briefly described|p10:2, 12-13, 21|||Tennant Region.|||Whittington Range, Coodna, Meerie, Manga Mauda, Blanche Creek Members.|Intruded by Treasure Suite.||12-JUL-16
8199|Hayward Creek Formation|69431|4|Described|p16:1-8, 13-14, 22|Paleoproterozoic|Paleoproterozoic|Tomkinson Province. c.3500m thick. Fluvial, intertidal and shallow-marine deposits. Strata form extensive upstanding ridges and ranges and are locally overturned. Contains mafic sills, dykes and volcanic rocks associated with the contemporaneous extensional Murchison Event of c.1815-1805 Ma.||Basal Tomkinson Creek Group.|Blanche Creek, Manga Mauda, Meerie, Coodna, Whittington Range Members.|Variably overlies Brumbreu Formation. Is overlain by Morphett Creek Formation.|Lithic, sublithic and feldspathic-sublithic sandstone, pebble to cobble conglomerate; minor thinly bedded fine to medium sandstone, siltstone (including possible tuff), mudstone and intraformational conglomerate; basaltic lava.|12-JUL-16
8199|Hayward Creek Formation|69673|6|Mentioned|p58|||||Tomkinson Creek Group|||Mafic sills, dykes and volcanic rocks.|
8199|Hayward Creek Formation|71592|5|Briefly described|Appendix A.|||Tennant Creek Region.|1784+/-7 Ma (MDA: U-Pb zircon).||||Quartzite.|
8199|Hayward Creek Formation|73124|6|Mentioned|p2 Fig.1|||||||||
8199|Hayward Creek Formation|73125|6|Mentioned|p2|Palaeoproterozoic|Palaeoproterozoic|Warramunga Province.||||||
8199|Hayward Creek Formation|73460|6|Mentioned|p2|||Warramunga Province.||||||
8199|Hayward Creek Formation|73590|6|Mentioned|p2|||||||||
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|||||
8256|Helen Springs Volcanics|12891|5|Briefly described|p731|||Equivalent of Antrim Plateau Volcanics.||||||07-FEB-11
8256|Helen Springs Volcanics|14019|6|Mentioned|p19|||Geochemically identical with Antrim Plateau Volcanics, Peaker Piker Volcanics in the N.T. and  Colless Volcanics in Qld.||||Geochemically identical with Antrim Plateau Volcanics, Peaker Piker Volcanics in the N.T. and  Colless Volcanics in Qld.||24-NOV-09
8256|Helen Springs Volcanics|22954|6|Mentioned|Fig3p9|Early Cambrian|Early Cambrian|||||||
8256|Helen Springs Volcanics|23328|5|Briefly described|1030 Fig.1|||K-Ar age 508+/-12 Ma||||||07-SEP-09
8256|Helen Springs Volcanics|23410|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Weathered vesicular basalt; minor felsic volcanic and volcaniclastic rocks; pebble conglomerate and lithic arenite.||||||02-NOV-05
8256|Helen Springs Volcanics|24172|4|Described|p29|Cambrian|Cambrian|Unconformably overlies Warramunga Fm (Tennant Creek) and Flynn Subgroup. Part of this unit may belong to Whittington Range Member as suggested by Mendum and Tonkin (1976); conversely, Whittington Range Member rocks are possibly Helen Springs Volcanics.||||||26-SEP-06
8256|Helen Springs Volcanics|24303|2|Defined|p34, p62 Appendix|Early Cambrian|Early Cambrian|Max. Thickness: 36 m excluding Muckaty Sandstone Member. Disconformably overlain by the Gum Ridge Formation and Montejinni Limestone. Correlates with the Antrim Plateau Volcanics, Nutwood Downs Volcanics and possibly Peaker Piker and Colless Volcanics.||||||
8256|Helen Springs Volcanics|24304|5|Briefly described|Map legend|Cambrian|Cambrian|Includes basalt (tholeiitic, massive, aphanitic to coarse-grained), calcite or smoky quartz amydales; sandstone, quartz arenite; and, undifferentiated basalt, sandstone, pebble to cobble bearing sandstone and breccia.||||||17-OCT-05
8256|Helen Springs Volcanics|30320|6|Mentioned|p422|||||||||
8256|Helen Springs Volcanics|31637|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
8256|Helen Springs Volcanics|32174|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
8256|Helen Springs Volcanics|32959|6|Mentioned|Fig.12|||||||||
8256|Helen Springs Volcanics|33307|6|Mentioned|Fig.8|||||||||
8256|Helen Springs Volcanics|33516|6|Mentioned|p99|||||||||
8256|Helen Springs Volcanics|34051|6|Mentioned|p6|||L.Camb.||||||
8256|Helen Springs Volcanics|34053|6|Mentioned|p7|||L.Camb.||||||
8256|Helen Springs Volcanics|34149|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
8256|Helen Springs Volcanics|34151|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
8256|Helen Springs Volcanics|34162|6|Mentioned|p117|||Early Cambrian.||||||
8256|Helen Springs Volcanics|34440|5|Briefly described|Table 1|||L.Camb.||||||
8256|Helen Springs Volcanics|34441|4|Described|Table 1|||L.Camb. See also pp11,12 etc.||||||26-SEP-06
8256|Helen Springs Volcanics|35054|6|Mentioned|p245|||||||||
8256|Helen Springs Volcanics|35229|4|Described|Table.1|||||||||
8256|Helen Springs Volcanics|35771|4|Described|Table 1|||||||||
8256|Helen Springs Volcanics|36335|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
8256|Helen Springs Volcanics|36473|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
8256|Helen Springs Volcanics|37572|5|Briefly described|p155|||See also p151,165.||||||26-SEP-06
8256|Helen Springs Volcanics|38446|6|Mentioned|p143|||||||||
8256|Helen Springs Volcanics|39213|6|Mentioned|Fig.8|||||||||
8256|Helen Springs Volcanics|40852|6|Mentioned|p36|||||||||
8256|Helen Springs Volcanics|41129|6|Mentioned|p15|||||||||
8256|Helen Springs Volcanics|41524|6|Mentioned|Fig.3|||||||||
8256|Helen Springs Volcanics|42504|5|Briefly described|Table 4 P73|||||||||
8256|Helen Springs Volcanics|42956|5|Briefly described|p31 Fig.4|||||||||
8256|Helen Springs Volcanics|43223|5|Briefly described|Map Legend||Paleozoic|||||||07-NOV-08
8256|Helen Springs Volcanics|43224|5|Briefly described|Map legend|Paleozoic|Neoproterozoic|||||||07-NOV-08
8256|Helen Springs Volcanics|44482|14|Not recorded|p.11|||(E53-12).||||||
8256|Helen Springs Volcanics|44960|14|Not recorded|Not recorded|||||||||
8256|Helen Springs Volcanics|45052|4|Described|p64|||See also p69.||||||26-SEP-06
8256|Helen Springs Volcanics|45064|3|Fully described|Table 1|||See also p18.||||||26-SEP-06
8256|Helen Springs Volcanics|45079|6|Mentioned|p8|||Lower Cambrian age||||||
8256|Helen Springs Volcanics|45087|6|Mentioned|p152|||Chemical analyses||||||
8256|Helen Springs Volcanics|45140|6|Mentioned|p13|||Tennant Creek region.||||||
8256|Helen Springs Volcanics|45148|5|Briefly described|p9|||||||||
8256|Helen Springs Volcanics|45373|14|Not recorded|p.177-179|||||||||
8256|Helen Springs Volcanics|46842|6|Mentioned|p115|||||||||
8256|Helen Springs Volcanics|47058|6|Mentioned|Fig.3 p123|||||||||08-JUL-20
8256|Helen Springs Volcanics|48835|14|Not recorded|p.9|||||||||
8256|Helen Springs Volcanics|48860|14|Not recorded|map legend|||may legend of Tennant Creek, 1 mile. (SE 53-14).||||||
8256|Helen Springs Volcanics|48891|14|Not recorded|p.22||Early Cambrian|Tb.1. Lower Cambrian.||||||
8256|Helen Springs Volcanics|60637|5|Briefly described|Map legend|||Basalt; basalt sandstone and breccia.||||||02-DEC-04
8256|Helen Springs Volcanics|60684|4|Described|p14|Early Cambrian|Early Cambrian|Basic to intermediate volcanic rocks - largely composed of amygdaloidal or vesicular tholeiitic basalt. Unconformably overlie folded Warramunga Formation; parts unconformably overlie Rising Sun Conglomerate. Also underlies Gum Ridge Formation.||||||
8256|Helen Springs Volcanics|62557|5|Briefly described|p461-463|Middle Cambrian|Middle Cambrian|Of the Kalkarindji continental flood basalt province. Ar/Ar age 508+/-2 Ma.||||||24-NOV-09
8256|Helen Springs Volcanics|64068|5|Briefly described|p81|Early Cambrian|Early Cambrian|Kalkarindji Flood Basalt Province, central and northwest Georgina Basin. c.513-c.504 Ma. ||||||
8256|Helen Springs Volcanics|64443|4|Described|iii, p4, p6-8, Tb.1, p40.|Early Cambrian|Early Cambrian|Combined with Peaker Piker Volcanics (of Smith & Roberts, 1963) by Kruse (2003). Max 34m thick. Dated at 508 +/- 2 Ma (Glass and Phillips 2002).||||Unconformably underlies Wonarah Formation (Barkly Group); unconformably overlies Mittiebah Sandstone, Mullera Formation or undivided South Nicholson Group.|Basalt, trachyte, microdolerite; minor dolerite; basal pebbly mudstone, sandstone and conglomerate. Shows alteration and amygdales.|01-MAY-15
8256|Helen Springs Volcanics|64589|4|Described|dated_samples, chemistry files||Cambrian|Coarse grained basaltic rock. K-Ar whole rock crystallization age of basalt 500+/-12 Ma. Geochemical analyses from Helen Springs NT.||||||12-NOV-08
8256|Helen Springs Volcanics|64780|5|Briefly described|p62 Fig.3 |Cambrian|Cambrian|||||||
8256|Helen Springs Volcanics|65209|6|Mentioned|p38|||||||Correlated with Rising Sun Conglomerate.||05-JAN-17
8256|Helen Springs Volcanics|65336|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Kalkarindji Volcanic Group. Unconformably overlies South Nicholson Group; unconformably underlies Thorntonia Limestone of Narpa Group and Wonorah Formation, Barkly Group. Consists of basalt, trachyte, microdolerite, minor dolerite, basal mudstone, pebbly sandstone, conglomerate.||||||29-SEP-11
8256|Helen Springs Volcanics|65337|3|Fully described|p v, p6 Fig.3, pp61-63.|Early Cambrian|Early Cambrian|Part of cratonic-scale flood basalt event in northern Australia; represents basal Georgina Basin deposits in southern and western MOUNT DRUMMOND area. Has a distinctive aeromagnetic signature. Outcrops as sporadic corestones in red-brown pisolitic soils.|508+/-2 Ma (Glass and Phillips 2002).|Unit in Kalkarindji Volcanic Group.|Includes Muckaty Sandstone Member.|Unconformably overlies South Nicholson Group. Is unconformably overlain by Wonarah Formation.|Basal pebbly sandstone and conglomerate; basalt, trachyte, dolerite, variably altered and amygdaloidal.|
8256|Helen Springs Volcanics|65344|4|Described|p3, 6, 7, 9, 12, 13, 17-20, Figs., Tbls|Early Cambrian|Early Cambrian|Of the Barkly Sub-basin and Alexandria-Wonarah Basement High, Georgina Basin. See well logs and thin section descriptions for detail. Thickness: up to 155.9m in AY06DD0||||Overlies the Renner Group and the South Nicholson Group. Underlies Gum Ridge Formation and Wonarah Formation.|Metavolcanics.|03-MAY-12
8256|Helen Springs Volcanics|65345|6|Mentioned|p11 Fig.11. |||||||||
8256|Helen Springs Volcanics|67149|5|Briefly described|Map legend.|Early Cambrian|Early Cambrian|||||Overlies South Nicholson Group. Is overlain by Gum Ridge Formation.|Variably altered, locally amygdaloidal basalt and microdolerite; thin basal pebbly sandstone and conglomerate (cross-section only).|
8256|Helen Springs Volcanics|67150|5|Briefly described|Map legend.|Early Cambrian|Early Cambrian|||||Unconformably overlies South Nicholson Group. Is unconformably overlain by Gum Ridge Formation.|Basalt, dolerite; basal and interbedded mudstone, pebbly sandstone, conglomerate, breccia (cross-section only).|
8256|Helen Springs Volcanics|67352|4|Described|v, p6,16-17,19-21,31-32,42,45-49,51,54|Early Cambrian|Early Cambrian|Part of the Kalkarindji Continental Flood Basalt Province, covering a vast area of NT-QLD-WA with an average thickness of .5 km. Widespread in subsurface of central Georgina Basin. Not exposed in these map areas.|505 +/- 2 Ma (40Ar/39Ar, Glass and Phillips 2006)||Muckety Sandstone Member.|Overlies South Nicholson, Hatches Creek, Renner and McArthur Groups. Overlain by Gum Ridge Formation, Top Springs Limestone. Synonymous with Peaker Piker Volcanics.|Variably altered and locally amygdaloidal tholeiitic basalt, trachyte, microdolerite and minor dolerite, together with subordinate basal and intraformational sandstone, mudstone and conglomerate.|
8256|Helen Springs Volcanics|69424|5|Briefly described|p9:26-27|Early Cambrian|Early Cambrian|Kalkarindji Province.|||Muckaty Sandstone Member.||Tuffaceous siltstone and sandstone.|12-JUL-16
8256|Helen Springs Volcanics|69431|6|Mentioned|p16:18-19|||Kalkarindji Province.|||Muckaty Sandstone Member.|||12-JUL-16
8256|Helen Springs Volcanics|69434|5|Briefly described|p19:4|Early Cambrian|Early Cambrian|Kalkarindji Province.||||Unconformably overlies South Nicholson Group.||12-JUL-16
8256|Helen Springs Volcanics|69437|5|Briefly described|p22:10|Series 2|Series 2|Kalkarindji Large Igneous Province.||||Is overlain by Gum Ridge Formation and Thorntonia Limestone.||12-JUL-16
8256|Helen Springs Volcanics|69443|5|Briefly described|p28:5, 12, 21-22, 42|Early Cambrian|Early Cambrian|Kalkarindji Province.||||Unconformably overlies Bukalara Sandstone. Is overlain dis/unconformably by Wonarah Formation (Barkly Group).|Volcanic and minor sedimentary rocks.|12-JUL-16
8256|Helen Springs Volcanics|69445|3|Fully described|p30:1-2, 5-6, 8-9, 16-17|Early Cambrian|Early Cambrian|Noakes and Traves (1954). Georgina Basin (subsurface) and east of the Tennant Region (exposed). Synonymous with the former Peaker Piker Volcanics. Up to 156m thick; 36m thick in the type section in HELEN SPRINGS map area (9m in cored drillhole NTGS 96/1 at 18o24'55"S, 134o14'40"E). Other age determinations include Ar40/Ar39 plagioclase separates: 508 +/- 2 Ma and 505 +/- 2 Ma (average 507 +/- 2 Ma) by Glass and Phillips (2006).|511 +/- 12 Ma (K-Ar; Bultitude, 1972).|Kalkarindji Suite.|Muckaty Sandstone Member.|Unconformably overlies South Nicholson Group. Is overlain disconformably by Gum Ridge, Wonarah Formations and Top Springs Limestone.|Widespread sub-aerial basaltic lavas.|12-JUL-16
8256|Helen Springs Volcanics|69561|6|Mentioned|p33 fig 2|Cambrian|Cambrian|||||Overlain by Thorntonia Limestone||
8256|Helen Springs Volcanics|69673|6|Mentioned|p39, p40, p58, p112, p136|||||Kalkarindji Suite|Includes Muckaty Sandstone Member|Unconformably overlies Bukalara Sandstone||
8256|Helen Springs Volcanics|70380|5|Briefly described|p745|Early Cambrian|Early Cambrian|Kalkarindji Large Igneous Province. Forms basement to central and northern Georgina Basin.||||||
8256|Helen Springs Volcanics|70968|5|Briefly described|p93, p100-101, p105, p108, p115|||Has a high-frequency magnetic expression.||Kalkarindji Suite.|Muckaty Sandstone Member.|Unconformably overlies Baralandji, Powell, Wiernty Formations (Renner Group).||
8256|Helen Springs Volcanics|72526|5|Briefly described|p6 Fig.1.2.|Cambrian|Cambrian|Shown with Colless Volcanics.||||||
8256|Helen Springs Volcanics|72527|6|Mentioned|p5 Fig.1.2.|Cambrian|Cambrian|||||||
8256|Helen Springs Volcanics|72919|6|Mentioned|p77|Cambrian|Cambrian|Georgina Basin. 101 m intersected in drillhole CRDD001.|||Overlain by Barkly Group.|||
8256|Helen Springs Volcanics|72967|6|Mentioned|p5|||Georgina Basin.||||||
8256|Helen Springs Volcanics|73083|6|Mentioned|p3, p47|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.|
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.||
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|
8291|Hermannsburg Sandstone|9199|5|Briefly described|Map legend|Devonian|Devonian|Of the Pertnjara Group.  Includes the Ljiltera Member.  Geological Province: Amadeus Basin.||||||04-NOV-04
8291|Hermannsburg Sandstone|9814|5|Briefly described|Map Legend|Devonian|Devonian|Pebbly sandstone, sandstone, rare conglomerate lenses. Of the Pertnjara Group.||||||
8291|Hermannsburg Sandstone|12891|5|Briefly described|p733 Fig. 2|Late Devonian|Middle Devonian|Geological province: Amadeus Basin.||||||07-FEB-11
8291|Hermannsburg Sandstone|22560|5|Briefly described|p3||Middle Devonian|||||||
8291|Hermannsburg Sandstone|22561|5|Briefly described|p23||Devonian|||||||
8291|Hermannsburg Sandstone|22562|6|Mentioned|p39|||||||||
8291|Hermannsburg Sandstone|22565|5|Briefly described|p70 & Table 1||Devonian|Approx thickness measured from seismic data - 900 meters||||||
8291|Hermannsburg Sandstone|22566|4|Described|p86|Devonian|Devonian|Of the Pertnjara Group.||||||20-OCT-05
8291|Hermannsburg Sandstone|22646|6|Mentioned|p 105|Devonian|Devonian|Of the Pertnjara Group.||||||26-SEP-06
8291|Hermannsburg Sandstone|22650|6|Mentioned|Fig 2 on p 157|Devonian|Devonian|Of the Pertnjara Group..||||||26-SEP-06
8291|Hermannsburg Sandstone|22656|6|Mentioned|p 284|Devonian|Devonian|||||||
8291|Hermannsburg Sandstone|22760|4|Described|p339|Late Devonian|Late Devonian|Of the Pertnjara Group.||||||20-OCT-05
8291|Hermannsburg Sandstone|22761|4|Described|p350|Late Devonian|Middle Devonian|Of the Pertnjara Group. Age is late Middle or early Late Devonian, constrained by the fossil ages in the underlying and overlying formations.||||||20-OCT-05
8291|Hermannsburg Sandstone|22762|6|Mentioned|p369|Late Devonian|Middle Devonian|Of the Pertnjara Group.  Age - Frasnian p373.||||||26-SEP-06
8291|Hermannsburg Sandstone|22763|5|Briefly described|p398||Late Devonian|Of the Pertnjara Group.||||||20-OCT-05
8291|Hermannsburg Sandstone|22804|5|Briefly described|p454||Devonian|Of the Pertnjara Group.||||||20-OCT-05
8291|Hermannsburg Sandstone|22805|5|Briefly described|p465||Middle Devonian|Of the Pertnjara Group.||||||20-OCT-05
8291|Hermannsburg Sandstone|22806|6|Mentioned|p478||Devonian|||||||
8291|Hermannsburg Sandstone|22824|5|Briefly described|p531|||||||||
8291|Hermannsburg Sandstone|22825|4|Described|p541-556|Devonian|Devonian|Of the Pertnjara Group.||||||20-OCT-05
8291|Hermannsburg Sandstone|22826|4|Described|p575|Devonian|Devonian|||||||
8291|Hermannsburg Sandstone|22828|6|Mentioned|p591|||||||||
8291|Hermannsburg Sandstone|23858|5|Briefly described|p915|Devonian|Devonian|Of Pertnjara Group. Geological Province: Amadeus Basin.||||||
8291|Hermannsburg Sandstone|24063|5|Briefly described|p223 Fig.6|||Geological Province: Amadeus Basin.||||||
8291|Hermannsburg Sandstone|24334|4|Described|p48 Tb.1, p51|Middle Devonian|Middle Devonian|Age: 367 - 381 Ma. Overlies the Parke Siltstone. Overlain by the Brewer Conglomerate. Geological Province: Amadeus Basin.||||||
8291|Hermannsburg Sandstone|29972|6|Mentioned|Table 1|||Carboniferous-Devonian||||||
8291|Hermannsburg Sandstone|30238|4|Described|p65|||Upper Devonian - Carboniferous age||||||
8291|Hermannsburg Sandstone|30544|6|Mentioned|p51|||Map legend on P51||||||
8291|Hermannsburg Sandstone|30615|6|Mentioned|p177|||Stratigraphic table Palm Valley -2||||||
8291|Hermannsburg Sandstone|31566|2|Defined|p238|Devonian|Devonian|See also p239.||||||26-SEP-06
8291|Hermannsburg Sandstone|31567|6|Mentioned|p285|||Pertnjara Group||||||
8291|Hermannsburg Sandstone|32209|6|Mentioned|Map legend|Devonian|Devonian|||||||
8291|Hermannsburg Sandstone|32640|6|Mentioned|p235|||||||||
8291|Hermannsburg Sandstone|32865|6|Mentioned|p482|||?Carb||||||
8291|Hermannsburg Sandstone|34111|5|Briefly described|Table 2|||Devonian - Carboniferous. See also pp16-18.||||||26-SEP-06
8291|Hermannsburg Sandstone|34442|5|Briefly described|Table 1|||Dev.- Carb.||||||
8291|Hermannsburg Sandstone|34579|4|Described|Table 3|||Devonian - Carboniferous||||||
8291|Hermannsburg Sandstone|35102|6|Mentioned|p7|||||||||
8291|Hermannsburg Sandstone|36821|6|Mentioned|p397|||||||||
8291|Hermannsburg Sandstone|38606|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
8291|Hermannsburg Sandstone|38885|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
8291|Hermannsburg Sandstone|39583|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
8291|Hermannsburg Sandstone|40740|3|Fully described|p60|||Mention p7.||||||26-SEP-06
8291|Hermannsburg Sandstone|40810|5|Briefly described|p12|||||||||
8291|Hermannsburg Sandstone|41018|6|Mentioned|p236|||||||||
8291|Hermannsburg Sandstone|41039|4|Described|p7|||||||||
8291|Hermannsburg Sandstone|41190|6|Mentioned|p267|||||||||
8291|Hermannsburg Sandstone|41270|6|Mentioned|p272|||||||||
8291|Hermannsburg Sandstone|41385|6|Mentioned|p366|||||||||
8291|Hermannsburg Sandstone|41492|6|Mentioned|Fig.10|||||||||
8291|Hermannsburg Sandstone|41708|5|Briefly described|p188|||||||||
8291|Hermannsburg Sandstone|41717|6|Mentioned|Fig.2|||||||||
8291|Hermannsburg Sandstone|41723|6|Mentioned|Map legend|Late Devonian||||||||
8291|Hermannsburg Sandstone|41820|6|Mentioned|Fig.3|||||||||
8291|Hermannsburg Sandstone|42037|5|Briefly described|Table 3 P79|||||||||
8291|Hermannsburg Sandstone|42049|5|Briefly described|p217|||||||||
8291|Hermannsburg Sandstone|42059|6|Mentioned|Fig.2 P131|||||||||
8291|Hermannsburg Sandstone|42082|6|Mentioned|Fig.3 P323|||||||||
8291|Hermannsburg Sandstone|42141|6|Mentioned|p568|||||||||
8291|Hermannsburg Sandstone|42504|5|Briefly described|p80|||||||||
8291|Hermannsburg Sandstone|42940|5|Briefly described|Plate 12|||||||||
8291|Hermannsburg Sandstone|43035|6|Mentioned|p23|||of Pertnjara Group||||||
8291|Hermannsburg Sandstone|43225|5|Briefly described|Map Legend|Devonian|Devonian|Of Pertnjara Group.||||||26-SEP-06
8291|Hermannsburg Sandstone|43503|6|Mentioned|11-17|Frasnian|Givetian|||||||
8291|Hermannsburg Sandstone|43646|6|Mentioned|Fig.3,p554|||||||||
8291|Hermannsburg Sandstone|43647|6|Mentioned|Fig.7,p538|||||||||
8291|Hermannsburg Sandstone|43648|6|Mentioned|Fig.13,p500|||||||||
8291|Hermannsburg Sandstone|43649|5|Briefly described|Fig.6,p460,463|||||||||
8291|Hermannsburg Sandstone|43666|6|Mentioned|p25|||||||||
8291|Hermannsburg Sandstone|43817|6|Mentioned|Fig.1,p42|||||||||
8291|Hermannsburg Sandstone|44335|5|Briefly described|p.11|Carboniferous|Devonian|Table 2. p.10, Dev-Carbon.||||||
8291|Hermannsburg Sandstone|44336|14|Not recorded|map legend|Carboniferous|Devonian|SG/53-3. Dev-Carbon, pt of Pertnjara Group.||||||
8291|Hermannsburg Sandstone|44342|6|Mentioned|p.7|||SG/53-5, fm of Pertnjara Group.||||||
8291|Hermannsburg Sandstone|44393|6|Mentioned|Fig.1|Carboniferous|Devonian|Part of Pertnjara Group. Dev-Carb.||||||
8291|Hermannsburg Sandstone|44395|14|Not recorded|p.9||Devonian|Of Pertnjara Group.||||||
8291|Hermannsburg Sandstone|44402|14|Not recorded|map legend|Carboniferous|Devonian|Part of Pertnjara Group. Dev. - Carb.||||||
8291|Hermannsburg Sandstone|44433|14|Not recorded|map legend|||Devonian to Carboniferous.||||||
8291|Hermannsburg Sandstone|44484|14|Not recorded|p.11, Tb. 1|Carboniferous|Devonian|Part of Pertnjara Group. Dev-Carb.||||||
8291|Hermannsburg Sandstone|44485|14|Not recorded|map legend|Carboniferous|Devonian|Part of Pertnjara Group. Dev-Carb. Defn on Tech.File F/53-13.||||||
8291|Hermannsburg Sandstone|44497|4|Described|p.12, Table 2|Carboniferous|Devonian|SF/53-13. Dev-Carb.||||||
8291|Hermannsburg Sandstone|44498|14|Not recorded|map legend|Carboniferous|Devonian|Part of Pertnjara Group. Dev-Carb.||||||
8291|Hermannsburg Sandstone|44505|14|Not recorded|p.5,8, Table 1|Carboniferous|Devonian|Of Pertnjara Group. Dev-Carb.||||||
8291|Hermannsburg Sandstone|44506|14|Not recorded|map legend|Carboniferous|Devonian|Devonian-Carboniferous.||||||
8291|Hermannsburg Sandstone|45041|4|Described|p98|||Dev.- L.Carb.||||||
8291|Hermannsburg Sandstone|45097|6|Mentioned|Fig.|||Correlation chart. Indeterminate.||||||
8291|Hermannsburg Sandstone|45168|6|Mentioned|p6|||||||||
8291|Hermannsburg Sandstone|45170|6|Mentioned|p8|||||||||
8291|Hermannsburg Sandstone|46928|6|Mentioned|Table 1|||||||||
8291|Hermannsburg Sandstone|47050|5|Briefly described|Fig.1|||||||||
8291|Hermannsburg Sandstone|60547|5|Briefly described|Map Legend|Devonian|Devonian|Of the Pertnjara Group. Sandstone. Geological Province: Amadeus Basin.||||||03-JUN-05
8291|Hermannsburg Sandstone|60674|5|Briefly described|Map legend|Devonian|Silurian|Of the Pertinjara Group.  Poorly bedded, poorly sorted lithic and feldspathic quartz sandstone.  Geological Province: Amadeus Basin.||||||12-JAN-05
8291|Hermannsburg Sandstone|61306|5|Briefly described|p40|||High-yielding aquifer rocks. Geological Province: northern Amadeus Basin.||||||26-SEP-06
8291|Hermannsburg Sandstone|61385|5|Briefly described|Map legend|Devonian|Devonian|Red-brown  sandstone, pebbly sandstone, minor siltstone.  Geological Province: Amadeus Basin.||||||20-OCT-05
8291|Hermannsburg Sandstone|61518|5|Briefly described|Map Legend|Devonian|Silurian|Poorly bedded, poorly sorted, lithic and feldspathic quartz sandstone. Geological Province: Amadeus Basin.||||||
8291|Hermannsburg Sandstone|62376|5|Briefly described|p18|Late Devonian|Late Devonian|Of the Pertnjara Group. Geological Province: Amadeus Basin.||||||09-FEB-10
8291|Hermannsburg Sandstone|62379|5|Briefly described|p7 Fig. 2|Devonian|Devonian|Of the Pertnjara Group. Geological Province: Amadeus Basin.||||||
8291|Hermannsburg Sandstone|64778|6|Mentioned|p13|Devonian|Devonian|Amadeus Basin.||||||
8291|Hermannsburg Sandstone|64809|5|Briefly described|p3 Fig.2,p6 Fig.4, p11 Fig.10, |Late Devonian|Late Devonian|Mis-spelt as Hermannsberg in Fig.4 and, more spectacularly, as Hermannsberg Siltstone in Fig.10.||Of the Pertnjara Group|Includes Ljiltera Member.|||
8291|Hermannsburg Sandstone|65233|4|Described|p3 Fig. 2|Late Devonian|Late Devonian|Of the Pertnjara Group. Max. thickness: 3000m. Geological province: Amadeus Basin. Syn-orogenic molasse of coalescing piedmont alluvial fans.||||||07-FEB-11
8291|Hermannsburg Sandstone|66767|5|Briefly described|p60|Devonian|Devonian|Amadeus Basin.||Pertnjara Group.||||
8291|Hermannsburg Sandstone|67028|6|Mentioned|p370 Fig.7, p371 Tb. 5|Devonian|Devonian|Magnetic information for unit concerning Mid-Paleozoic to Early Mesozoic pole positions for Australia are presented, sourced from the Global Palaeomagnetic Database (GPMDB; McElhinny & Lock 1993, 1996).|375-392 Ma magnetic age range|||||24-APR-12
8291|Hermannsburg Sandstone|67326|5|Briefly described|p2|Late Devonian|Late Devonian|Amadeus Basin.||Pertnjara Group.||Overlies Parke Siltstone. Is overlain by Brewer Conglomerate.||
8291|Hermannsburg Sandstone|67565|4|Described|p42, p52.|Devonian|Devonian|Estimated thickness is c.500 m. An important aquifer. ||Unit in Pertnjara Group.|Includes Ljiltera Member.|Conformably overlies Parke Siltstone.|Poorly bedded and poorly sorted, red-brown and chocolate-brown lithic-feldspathic quartz sandstone, with a silty matrix; thick to massive beds; locally calcareous with clasts of dolostone and limestone; local pebbly sandstone.|
8291|Hermannsburg Sandstone|67856|6|Mentioned|p338 fig 4-30|Late Devonian|Late Devonian|||Of Pertnjara Group.||||
8291|Hermannsburg Sandstone|68323|6|Mentioned|p4 Fig.2|Late Devonian|Late Devonian|Amadeus Basin.||Pertnjara Group.||||
8291|Hermannsburg Sandstone|69438|3|Fully described|p23:2-3, 7, 37-39, 48, 57|Late Devonian|Late Devonian|Wells et al. (1970). Jones (1972) recognised three Members. Amadeus Basin. Type area near Stokes Pass in the western MacDonnell Ranges. Up to c.1100m thick.||Pertnjara Group.|Ooraminna Sandstone, Owen Springs Sandstone, Ljiltera, Members.|Conformably overlies Mereenie Sandstone and Amulda Member (Parke Siltstone). Is overlain conformably (locally unconformably) by Brewer Conglomerate.|Poorly sorted red-brown to grey-brown lithofeldspathic quartz sandstone in repeated upward-fining fluvial cycles.|12-JUL-16
8291|Hermannsburg Sandstone|69673|5|Briefly described|p64 fig 53, p67|Late Devonian|Late Devonian|Maximum thickness of 1100m.|q|Pertnjara Group|Includes Ooraminna Sandstone Member, Owen Springs Sandstone Member, Ljiltera Member|Overlies Parke Siltstone, overlain by Brewer Conglomerate|Poorly sorted lithofeldspathic quartz sandstone.|13-SEP-18
8291|Hermannsburg Sandstone|71146|5|Briefly described|p6|Famennian|Frasnian|Amadeus Basin.||||Overlies the Parke Siltstone. Overlain by the Brewer Conglomerate.|Sandstone.|
8291|Hermannsburg Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
8291|Hermannsburg Sandstone|71279|5|Briefly described|p355 Fig.2,p360-361,p363-365,p376 Fig.26|Late Devonian|Late Devonian|See also p382 Tb.1. Amadeus Basin. Crops out in the Waterhouse Range. Magnetisation described. Modelled magnetic properties.||Pertnjara Group.|Ooraminna Sandstone Member, Ljiltera Member.|||
8291|Hermannsburg Sandstone|72369|4|Described|iii,p3-4,40-43|||Of Amadeus Basin. Widely distributed in the Amadeus Basin and typically exposed in prominent strike ridges with steep cliff faces. Paleomagnetic studies by McElhinny et al (2003) provided an age of c. 380-365 Ma. LA-ICP-MS U-Pb detrital zircon dating of sample HB15ND344 (quartz arenite) yielded an interpreted maximum depositional age of 545+\-5 Ma (youngest concordant zircon). Primary source(s) of the Neoproterozoic detritus is currently unknown. Mesoproterozoic detritus was most likely sourced from the Musgrave Province. Palaeoproterozoic detritus is most likely to have been recycled from the underlying strata and was probably originally sourced from the Aileron and Warumpi provinces. Sample locality, zircon description, SHRIMP results and analyses are discussed.||Unit of Pertnjara Group.|Includes Ooraminna Sandstone Member, Owen Springs Sandstone Member and Ljiltera Member.|Overlain by Brewer Conglomerate. Underlain confromably by Parke Siltstone.|Upward-fining fluvial cycles; poorly-sorted, red-brown to grey-brown lithofeldspathic quartz sandstone.|18-DEC-19
8291|Hermannsburg Sandstone|72374|4|Described|iii,p3-4,18,20,23-26|||Of Amadeus Basin. Widely distributed across the Amadeus Basin. Commonly exposed in prominent strike ridges with steep cliff faces. Paleomagnetic study by McElhinny et al 2003 suggested an age constrained between c. 380 and c. 365 Ma. Normington et al 2018 provided a max depositional age of c. 545 Ma, where detritus underwent significant recycling from underlying Amadeus Basin succession. Sample HB16ND368 (very fine-grained quartz arenite) yielded an interpreted maximum depositional age of 379+\-2 Ma. Zircons of c. 1450-800 Ma (c. 1127 peak) likely derived from Musgrave Province either directly, or recycled from underlying Amadeus Basin succession. Lesser groupings of c. 650-380 Ma, c. 1900-1500 Ma and c. 2850-2000 Ma zircon (Figure 30) were likely sourced from within underlying Amadeus Basin succession from the Aileron, Warumpi provinces as well as from distal sources within east Gondwana.||Unit of Pertnjara Group.||Underlain by Parke Siltstone.|Poorly-sorted, red-brown to grey-brown lithofeldspathic quartz sandstone, which exhibit fining-upward, fluvial cycles.|
8291|Hermannsburg Sandstone|73085|6|Mentioned|p1|late Devonian|late Devonian|||Pertnjara Group||Underlain by Parke Siltstone. Overlain by Brewer Conglomerate. Equivalent to Langra Formation (Finke Group).||
8291|Hermannsburg Sandstone|73279|5|Briefly described|p3, p15|Devonian|Devonian|Amadeus Basin. Middle part of the Pertnjara Group. Detrital zircons analysed for Hf isotopic composition [see article].||Pertnjara Group|||Includes sandstone.|
8293|Hermit Creek Metamorphics|9324|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Gneiss, metabasite, schist.||||||07-NOV-08
8293|Hermit Creek Metamorphics|9538|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Schist, gneiss, amphibolite, migmatite.||||||07-NOV-08
8293|Hermit Creek Metamorphics|9579|5|Briefly described|Map Sheet|Paleoproterozoic|Paleoproterozoic|Early Proterozoic age. Informally subdivided into four facies.||||||
8293|Hermit Creek Metamorphics|22479|5|Briefly described|fig1p2|Orosirian|Orosirian|Placed within Litchfield Province.  Part of the Pine Creek Inlier.||||||26-SEP-06
8293|Hermit Creek Metamorphics|22809|3|Fully described|21|Proterozoic|Proterozoic|||||||
8293|Hermit Creek Metamorphics|22810|5|Briefly described|Table2 P4|||||||||
8293|Hermit Creek Metamorphics|22813|5|Briefly described|Map|Paleoproterozoic|Paleoproterozoic|Gneiss, metabasite, schist.||||||07-NOV-08
8293|Hermit Creek Metamorphics|23714|4|Described|p8|Proterozoic|Proterozoic|See also page 8 Table 1. Litchfield Province.||||||
8293|Hermit Creek Metamorphics|23715|5|Briefly described|Map legend||Proterozoic|In the Litchfield Province||||||
8293|Hermit Creek Metamorphics|23733|5|Briefly described|p32 Fig. 19|||||||||
8293|Hermit Creek Metamorphics|23822|5|Briefly described|p305|Archean|Archean|Geological Province: Litchfield Province.||||||07-NOV-08
8293|Hermit Creek Metamorphics|24047|5|Briefly described|p5 Fig.4|Paleoproterozoic|Paleoproterozoic|Gneiss, schist, amphibolite.  Geological Province: Pine Creek Orogen.||||||07-NOV-08
8293|Hermit Creek Metamorphics|32170|6|Mentioned|Map legend|Archean|Archean|Prob. Archaean||||||07-NOV-08
8293|Hermit Creek Metamorphics|32171|4|Described|Table 1|||Archaean||||||
8293|Hermit Creek Metamorphics|32307|5|Briefly described|Table 1|||Archaean||||||
8293|Hermit Creek Metamorphics|32309|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
8293|Hermit Creek Metamorphics|32310|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
8293|Hermit Creek Metamorphics|32659|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
8293|Hermit Creek Metamorphics|32660|5|Briefly described|Table 2|||||||||
8293|Hermit Creek Metamorphics|32700|4|Described|Table 1|||Archaean? See p12.||||||26-SEP-06
8293|Hermit Creek Metamorphics|33376|6|Mentioned|Map legend|Paleoproterozoic|Archean|Archaean and/or Lower Proterozoic||||||07-NOV-08
8293|Hermit Creek Metamorphics|33377|6|Mentioned|Table 1|||Stratigraphy||||||
8293|Hermit Creek Metamorphics|35140|6|Mentioned|Fig.1|||||||||
8293|Hermit Creek Metamorphics|36473|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
8293|Hermit Creek Metamorphics|37579|5|Briefly described|Regional setting map legend|Paleoproterozoic|Paleoproterozoic|Schist, amphibolite, migmatite.||||||07-NOV-08
8293|Hermit Creek Metamorphics|38884|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
8293|Hermit Creek Metamorphics|39563|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
8293|Hermit Creek Metamorphics|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
8293|Hermit Creek Metamorphics|39801|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Schist, gneiss, amphibolite, migmatite.||||||07-NOV-08
8293|Hermit Creek Metamorphics|39889|4|Described|p489|||See also p485.||||||26-SEP-06
8293|Hermit Creek Metamorphics|40168|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Schist, gneiss, amphibolite, migmatite.||||||07-NOV-08
8293|Hermit Creek Metamorphics|40223|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Schist, gneiss, amphibolite, migmatite.||||||07-NOV-08
8293|Hermit Creek Metamorphics|40765|6|Mentioned|p3|||||||||
8293|Hermit Creek Metamorphics|40808|5|Briefly described|Table 2|||||||||
8293|Hermit Creek Metamorphics|40823|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
8293|Hermit Creek Metamorphics|41304|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
8293|Hermit Creek Metamorphics|41305|5|Briefly described|Fig.4|||||||||
8293|Hermit Creek Metamorphics|41407|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
8293|Hermit Creek Metamorphics|41586|6|Mentioned|Map legend|||||||||
8293|Hermit Creek Metamorphics|41645|3|Fully described|p3|||||||||
8293|Hermit Creek Metamorphics|41646|6|Mentioned|Map legend|Paleoproterozoic||Pelitic and semi-pelitic schist and gneiss; phyllite; quartz-mica schist; sillimanite-andalusite-muscovite schist; andalusite-cordierite hornfels; minor quartzite.||||||07-NOV-08
8293|Hermit Creek Metamorphics|41660|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Low to high grade metamorphic rocks, retrogressed pelitic and psammitic gneiss and schist, with quartz and feldspar and +/- following: biotite, sillimanite, garnet, muscovite, chlorite and sericite; metabasite.||||||07-NOV-08
8293|Hermit Creek Metamorphics|41661|3|Fully described|p4|||Mention p16.||||||26-SEP-06
8293|Hermit Creek Metamorphics|41980|4|Described|p570|||See also p576.||||||26-SEP-06
8293|Hermit Creek Metamorphics|42014|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
8293|Hermit Creek Metamorphics|43187|5|Briefly described|p2|||||||||
8293|Hermit Creek Metamorphics|43595|5|Briefly described|p353|||Metamorphism approx.1870 Ma||||||
8293|Hermit Creek Metamorphics|45022|5|Briefly described|p.23||Archean|On many pages.||||||07-NOV-08
8293|Hermit Creek Metamorphics|45058|6|Mentioned|Fig. 8|||Archaean||||||
8293|Hermit Creek Metamorphics|45112|4|Described|p48|||||||||
8293|Hermit Creek Metamorphics|46675|5|Briefly described|Map legend for regional setting...|Paleoproterozoic|Paleoproterozoic|Schist, gneiss, amphibolite, migmatite.  Geological Province: Pine Creek Geosyncline.||||||07-NOV-08
8293|Hermit Creek Metamorphics|46676|14|Not recorded|p.6||Archean|||||||07-NOV-08
8293|Hermit Creek Metamorphics|47047|6|Mentioned|p219|||||||||
8293|Hermit Creek Metamorphics|48942|3|Fully described|p8|||||||||
8293|Hermit Creek Metamorphics|50586|6|Mentioned|p3.1|||Intruded by Allia Suite.||||||
8293|Hermit Creek Metamorphics|60526|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Schist, gneiss, amphibolite, migmatite.||||||
8293|Hermit Creek Metamorphics|62375|5|Briefly described|p10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Gneiss, schist, amphibolite. Geological Province: Pine Creek Orogen.||||||11-FEB-10
8293|Hermit Creek Metamorphics|63866|4|Described|p105, p107|Orosirian|Orosirian|Litchfield Province, Pine Creek Orogen. Protoliths for these rocks included semi-pelitic sedimentary and intercalated mafic igneous rocks. Metamorphism of this unit has been dated on monazites at 1856 +/- 2 Ma and 1854 +/- 4 Ma.|ca. 1876-1861 Ma (Maximum depositional ages)||||Amphibolite and granulite grade metamorphic rocks.|
8293|Hermit Creek Metamorphics|64698|4|Described|lithinterp table|Orosirian|Paleoproterozoic|Age ~1850-2500Ma.Misspelt as Hermit Creek Metamorphics. Massive to banded metabasite; Magnetic schist and amphibolite intersected in drillholes, seen on aeromag images, but generally non-outcropping; Semi-pelitic gneiss; schist,  hornfels, minor qtzite;||||||17-SEP-14
8293|Hermit Creek Metamorphics|64722|5|Briefly described|p10|||Of Litchfield Province of Pine Creek Region. Underwent medium to high grade metamorphism at ~1855 Ma. This unit plus Fog Bay and Welltree Metamorphics are correlated with Finniss River Group.||||||11-APR-12
8293|Hermit Creek Metamorphics|64730|6|Mentioned|p125 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of Litchfield Province. Shown as lateral equivalent of Finniss River Group.||||||03-MAY-12
8293|Hermit Creek Metamorphics|64731|4|Described|p145, 149, 154-158, 159-160, p163-164|Paleoproterozoic|Paleoproterozoic|Of Litchfield Province. Divided into three unnamed mappable subunits. May be high-grade equivalent to, or may unconformably underlie, Finniss River Group. Petrologic description given. Peak or near-peak high-grade metamorphism dated at 1855 +/- 2 Ma.||||||12-APR-12
8293|Hermit Creek Metamorphics|64956|4|Described|p2 Tb. 20, p83-86|Paleoproterozoic|Paleoproterozoic|Max. depositional ages: 1875+/-4Ma, 1868+/-5Ma. Geological province: Pine Creek Orogen. Sample is a garnet-biotite-quartz-plagioclase-K-feldspar gneiss; migmatitic (p53)||||||07-FEB-11
8293|Hermit Creek Metamorphics|65232|5|Briefly described|p6 Fig. 5|Palaeoproterozoic|Palaeoproterozoic|Gneiss, schist, amphibolite. General lithology given for three units including Hermit Creek, Fog Bay and Welltree Metamorphics. On figure, presented as Hermit Creek and Fog Bay Metamorphics.||||||09-FEB-10
8293|Hermit Creek Metamorphics|65556|3|Fully described|p2 Tb.1, p4, p9-13, p45, p51|||Litchfield Province. Composite package of undeformed, granulite-facies, migmatitic, semi-pelitic, pelitic and psammitic metasedimentary rocks; highly deformed amphibolite-facies, pelitic and psammitic ferruginous schist; amphibolite; and subordinate calc-silicate and fine-grained cordierite hornfels. Exposed sporadically across ~100 square km in the Daly River region. Outcrop of sampled migmatite occurs as sparse fresh boulders and subcrop. SHRIMP U-Pb monazite metamorphic age of 1855+/-2 Ma and 1853+/-4 Ma.||||||
8293|Hermit Creek Metamorphics|67167|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Unit in Cosmo Supergroup.|||Psammitic gneiss, biotite quartzite, pelitic and semi-pelitic schist and gneiss, quartz-mica schist, sillimanite-andalusite-muscovite schist, andalusite-cordierite hornfels, minor quartzite.|
8293|Hermit Creek Metamorphics|67186|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Psammitic gneiss; biotite quartzite; massive to banded amphibolite; pelitic and semi-pelitic schist and gneiss; quartz-mica schist; sillimanite-andalusite-muscovite schist; andalusite-cordierite hornfels; minor quartzite.|23-NOV-11
8293|Hermit Creek Metamorphics|67232|4|Described|p3, p4, p5. |Paleoproterozoic|Paleoproterozoic|Litchfield Province, Pine Creek Orogen. Mid-amphibolite to granulite facies, peaking at 1855 Ma (Carson et al. 2008). Exposed in southern part of the Province. Correlated with younger detrital zircon spectra in Burrell Creek Formation.|Max. deposition 1868 +/- 4 Ma (Worden 2008a).|||Probably intruded by Wangi Basics (now Woolianna Gabbro).|Granulite-facies pelitic and psammitic schist, amphibolite, cordierite migmatite and rare calc-silicate rocks.|21-NOV-11
8293|Hermit Creek Metamorphics|67564|5|Briefly described|p9 Fig.4.|Paleoproterozoic|Paleoproterozoic|Litchfield Province, Pine Creek Orogen.|||||Gneiss, schist, amphibolite.|
8293|Hermit Creek Metamorphics|67779|5|Briefly described|p5 Fig.4(b).|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||Unit in Cosmo Supergroup.||||
8293|Hermit Creek Metamorphics|68733|6|Mentioned|p184|||Litchfield Province. Has nearly identical Nd isotopic values with Inverway Metamorphics, suggesting a contiguous Paleoproterozoic low-grade-metamorphic basement between Pine Creek and Tanami regions.||||||05-DEC-17
8293|Hermit Creek Metamorphics|69383|6|Mentioned|p38|Paleoproterozoic||Pine Creek Orogen, Litchfield Domain. Low?pressure, high-temperature metamorphism commenced ~1855 Ma.||||||
8293|Hermit Creek Metamorphics|69420|4|Described|p5:2, 4-7, 13, 26-27, 117|Paleoproterozoic|Paleoproterozoic|Litchfield Domain, Pine Creek Orogen. Monazite dating of metamorphism gives 1855 +/- 2 Ma and 1853 +/- 4 Ma. Appears as Hermit Creek Volcanics on p 5:117, where it is presumed to be the parent body for boulders of corundum.||Cosmo Supergroup.||Correlated with Burrell Creek Formation (Finniss River Group).|Sillimanite gneiss, garnet-cordierite gneiss, biotite-quartz schist, metamorphosed mafic igneous rocks. Shows no significant fabric development; commonly preserves primary bedding structures.|12-JUL-16
8293|Hermit Creek Metamorphics|69435|6|Mentioned|p20:3|||||||Is overlain unconformably by Moyle River Formation.||12-JUL-16
8293|Hermit Creek Metamorphics|69933|5|Briefly described|v, p1, p4-p7, p26-27|Orosirian|Orosirian|Petrography, zircon characteristics, SHRIMP analyses and results are provided.|1860 +/-3 Ma (Max dep, SHRIMP U-Pb)||||Medium-grained, compositionally layered, high-grade metasedimentary rock with semi-pelitic and psammitic layers.|
8293|Hermit Creek Metamorphics|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. The undivided unit (under cover) and the three facies are all mapped separately.||Cosmo Supergroup.|||Granulite-facies (semi-)pelitic schist and gneiss, sillimanite gneiss and schist, garnet-cordierite gneiss, quartz-mica schist, andalusite-cordierite hornfels, minor quartzite; amphibolite-facies ferruginous schist, rare calc-silicate; amphibolite.|
8293|Hermit Creek Metamorphics|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||gneiss, schist|
8293|Hermit Creek Metamorphics|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen. Metamorphosed at 1853 +/- 4 Ma.|||||Cordierite-bearing migmatite.|
8293|Hermit Creek Metamorphics|73089|5|Briefly described|p32-33|||Pine Creek Orogen, western; Litchfield Domain. Appears to be a higher-metamorphic-grade correlative of the upper Cosmo Supergroup. Dominantly Paleoproterozoic detritus; protolith deposited after 1868 +/- 5 Ma. Experienced high-temperature, low-pressure metamorphism at 1855-1853 Ma and were intruded by granitic rocks at a similar time (1863-1850 Ma) in an interpreted extensional setting.|||||Amphibolite to granulite facies metamorphic rocks.|
8362|Hillsoak Bore Metamorphics|41510|6|Mentioned|Map legend|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
8362|Hillsoak Bore Metamorphics|50246|5|Briefly described|p9, p20 Fig. 2|Paleoproterozoic|Paleoproterozoic|Predominantly metasediments, including calcareous units and rare marbles, and amphibolites.||||||07-FEB-11
8362|Hillsoak Bore Metamorphics|62595|5|Briefly described|p9, p29 Fig.6, p31 Fig.9.|||Part of the Alice Springs Arltungs Nappe Complex, a south-directed thrusting event c.430-300 Ma. With Heavitree Quartzite, hosts the Arltunga goldfield deposit. Written as Hill Soak Bore Metamorphics in Fig.6 and as Hillsoak Bore metamorphics in Fig.9.|||||Predominantly metasediments, including calcareous units and rare marbles, andalusite schist and amphibolites.|
8362|Hillsoak Bore Metamorphics|66860|6|Mentioned|p1|||Hosts the Goat Camp Dam base metal prospect. Probably deposited in shallow-water prior to deposition of most of Strangways Metamorphic Complex.||||||
8362|Hillsoak Bore Metamorphics|69427|5|Briefly described|p12:9, 16, 57-58|Paleoproterozoic|Paleoproterozoic|Strangways Range region, Aileron Province. Crops out in the W part of the White Range Nappe within the Arltunga Nappe Complex, S and W of Paddys Plain. Hosts gold deposits in the Arltunga goldfield.|||||Marble, calc-silicate rock, andalusite schist, amphibolite, quartzite, biotite-muscovite schists, granitic gneiss, biotite gneiss (with garnets to 10cm), sillimanite-bearing metapelite and felsic gneiss.|12-JUL-16
8388|Hobblechain Rhyolite|22432|5|Briefly described|p22|Statherian|Statherian|Age 1725+/- 2Ma.||||||26-SEP-06
8388|Hobblechain Rhyolite|22538|6|Mentioned|App1 P722||Statherian|||||||
8388|Hobblechain Rhyolite|22665|5|Briefly described|Table1 P222, P225||Statherian|Age of unit is 1725+/-2 Ma||||||
8388|Hobblechain Rhyolite|23363|5|Briefly described|352 Tab.3|Statherian|Statherian|Age: 1725+/-2Ma.||||||26-SEP-06
8388|Hobblechain Rhyolite|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|Of Tawalla Group.||||||07-NOV-08
8388|Hobblechain Rhyolite|23395|5|Briefly described|p389|||||||||
8388|Hobblechain Rhyolite|23396|5|Briefly described|p407 Fig.2|Statherian|Statherian|Of Tawallah Group.  Age: 1725+/-2Ma.||||||26-SEP-06
8388|Hobblechain Rhyolite|23398|5|Briefly described|p436|Statherian|Statherian|Age: 1725+/-2Ma.||||||26-SEP-06
8388|Hobblechain Rhyolite|23776|5|Briefly described|p705 Fig 2.|Statherian|Statherian|Age: 1725+/-2 Ma. Of Tawallah Group.||||||26-SEP-06
8388|Hobblechain Rhyolite|24048|6|Mentioned|p36|||Geological Province: McArthur Basin.||||||
8388|Hobblechain Rhyolite|24050|6|Mentioned|p27|||||||||
8388|Hobblechain Rhyolite|24197|5|Briefly described|p29|Paleoproterozoic|Paleoproterozoic|Of the Fagan Suite. Rocks of lava domes and flows. Coarse porphyritic quartz-feldspar rhyolite.||||||07-FEB-11
8388|Hobblechain Rhyolite|24419|5|Briefly described|p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Of the Tawallah Group.  Geological Province: McArthur Basin, Murphy Province.||||||07-NOV-08
8388|Hobblechain Rhyolite|24432|6|Mentioned|p570 Fig.10|||||||||
8388|Hobblechain Rhyolite|32519|6|Mentioned|p341|||||||||
8388|Hobblechain Rhyolite|32904|6|Mentioned|p95|||||||||
8388|Hobblechain Rhyolite|35114|6|Mentioned|Fig.5|||||||||
8388|Hobblechain Rhyolite|36012|6|Mentioned|p16|||||||||
8388|Hobblechain Rhyolite|37371|6|Mentioned|p368|||||||||
8388|Hobblechain Rhyolite|38042|6|Mentioned|p167|||||||||
8388|Hobblechain Rhyolite|40105|6|Mentioned|Fig.7|||||||||
8388|Hobblechain Rhyolite|40691|5|Briefly described|p11|||Mention Fig.4||||||
8388|Hobblechain Rhyolite|41721|3|Fully described|p25|||Of the Tawallah Group. Conformably overlies Gold Creek Volcanics; overlain by McArthur Group. Porphyrytic rhyolite. Geological province: McArthur Basin.||||||18-FEB-08
8388|Hobblechain Rhyolite|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
8388|Hobblechain Rhyolite|41957|6|Mentioned|p68|||||||||
8388|Hobblechain Rhyolite|42385|5|Briefly described|p14|||||||||
8388|Hobblechain Rhyolite|42639|6|Mentioned|p17|||Calvert Hills, Robinson River||||||
8388|Hobblechain Rhyolite|42812|5|Briefly described|p27, Fig.5|||||||||
8388|Hobblechain Rhyolite|42873|5|Briefly described|Fig.1, P110|||||||||
8388|Hobblechain Rhyolite|43010|5|Briefly described|Fig.6||Mesoproterozoic|of "Mid Proterozoic" age.||||||
8388|Hobblechain Rhyolite|43036|6|Mentioned|Fig.5|||||||||
8388|Hobblechain Rhyolite|43715|6|Mentioned|p27|||||||||
8388|Hobblechain Rhyolite|44112|6|Mentioned|p43|||||||||
8388|Hobblechain Rhyolite|44436|5|Briefly described|p.10|||(E53-4).||||||02-DEC-04
8388|Hobblechain Rhyolite|45162|2|Defined|p43|||||||||
8388|Hobblechain Rhyolite|50591|5|Briefly described|p1.3, 4.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Of the Fagan Supersuite. Geological Province: Arnhem Block/McArthur Basin. Age: 1725 +/- 2Ma (Shrimp).||||||07-NOV-08
8388|Hobblechain Rhyolite|60483|5|Briefly described|p7 Fig. 5|Paleoproterozoic|Paleoproterozoic|Of the Tawallah Group. Age: 1725+/-2Ma. Geological Province: McArthur Basin.||||||07-NOV-08
8388|Hobblechain Rhyolite|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Tawallah Group. Underlain by Gold Creek Volcanics.||||||03-JUN-09
8388|Hobblechain Rhyolite|60574|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Tawallah Group. Intrudes the Pungalina Member.||||||07-NOV-08
8388|Hobblechain Rhyolite|63112|6|Mentioned|p1192 Tb.1|||Calvert Superbasin. May have been fed by a fissure feeder of Packsaddle Microgranite. <100 m thick.|1725 +/- 2 Ma.||||Porphyritic rhyolite with quartz phenocrysts and micropoikilitic texture.|
8388|Hobblechain Rhyolite|63866|5|Briefly described|p54|||||Prize Supersequence||||
8388|Hobblechain Rhyolite|64726|6|Mentioned|p86 Table 1.|||Sampled for paleomagnetic reconstruction of Australian and Laurentian Apparent Polar Wander Path.|1725 +/- 2 Ma.|||||
8388|Hobblechain Rhyolite|64817|6|Mentioned|p353 Fig.4, p355 Fig.5|Statherian|Statherian||1725 +/- 2 Ma.|Of the Tawallah Group.||||
8388|Hobblechain Rhyolite|65228|5|Briefly described|p22, p25, Figs.02, 06, 07, 10.|Statherian|Statherian|McArthur Basin. Felsic.|1725 +/- 2 Ma.|Unit in Tawallah Group.||Overlies Gold Creek Volcanics. Is overlain by Pungalina Member.||
8388|Hobblechain Rhyolite|65337|6|Mentioned|p15, p17.|||Southeastern McArthur Basin.|c.1725 Ma.|||||
8388|Hobblechain Rhyolite|65340|4|Described|p11, p.13 Table 4, pp39-46, p52, p69.|||Named by Yates (1963); included adjacent epiclastic deposits which are now considered part of Pungalina Member of Echo Sandstone. Consistent 70 - 100 m thickness. Mineralogy, microstructure, fabric and contact relationships are described in detail. Hosts Cu mineralisation in chlorite-altered rhyolite breccia at Camel Creek.|1725 +/- 2 Ma (Page and Sweet 1998).|Unit in Tawallah Group.||Disconformably overlies Gold Creek Volcanics. Contiguous and co-magmatic with Packsaddle Microgranite. Is overlain by Upper Pungalina Member.|Pink, porphyritic (K-feldspar-quartz), massive to flow-banded, spherulitic to microgranophyric rhyolite with local lithophysae, autobreccia, peperite and chlorite alteration.|
8388|Hobblechain Rhyolite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Paleoproterozoic|Paleoproterozoic|Calvert Superbasin.||Tawallah Group|||Rhyolite, reddish brown, porphyritic.|
8388|Hobblechain Rhyolite|67352|6|Mentioned|p14  Tb.2|||||||Is overlain unconformably by Masterton Sandstone.||
8388|Hobblechain Rhyolite|69430|4|Described|p15:3, 9-10, 12, 48|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin. 70-100m thick. Lava flow with talus-lined margin. Comagmatic with Packsaddle Microgranite. A typographical error in 15:10 has the age at 1752 +/- 2 Ma.|1725 +/- 2 Ma (Page and Sweet, 1998).|Tawallah Group.||Disconformably overlies Gold Creek Volcanics. Is overlain conformably by Pungalina Member (Warramana Sandstone).|Pink, porphyritic (K-feldspar-quartz), massive to flow-banded, spherulitic to microgranophyric rhyolite.|12-JUL-16
8388|Hobblechain Rhyolite|69591|5|Briefly described|p56|||Camooweal-Murphy Domain, Mount Isa Province. Part of Tawallah Supersequence. Subaerial (?) deposits.||Tawallah Group.|||Reddish-brown, porphyritic rhyolite.|
8388|Hobblechain Rhyolite|69673|5|Briefly described|p16 fig 13, p17 fig 14||||1725 Ma|Tawallah Group||Overlain by Pungalina Member, Warramana Sandstone, overlies Gold Creek Volcanics|Rhyolite.|
8388|Hobblechain Rhyolite|70849|5|Briefly described|Map legend.|Statherian|Statherian|McArthur Basin.||Tawallah Group.||Overlies Gold Creek Volcanics. Is overlain by Masterton Sandstone (McArthur Group).|Reddish-brown, porphyritic rhyolite.|
8388|Hobblechain Rhyolite|71592|5|Briefly described|Appendix A.|||McArthur Basin.|1725+/-2 Ma (crystallisation: U-Pb zircon SHRIMP)||||Rhyolite.|
8388|Hobblechain Rhyolite|71606|5|Briefly described|p135,137|||McArthur Basin. SHRIMP data givers 1710-1700 Ma age, associated with Fagan Phase magmatism of Rawlings 1994.||Unit of Tawallah Group.||Hosted in the uppermost Tawallah Group.||
8388|Hobblechain Rhyolite|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Southeastern McArthur Basin. U-Pb zircon igneous crystallisation age.|1725 +/-2 Ma|Tawallah Group||Overlies Gold Creek Volcanics and is partially laterally equivalent to Pungalina Member and Warramana Sandstone.||
8388|Hobblechain Rhyolite|72718|6|Mentioned|p7|Statherian|Statherian|Southern McArthur Basin.|1725 +/- [?] Ma|Tawallah Group||Underlaing by Gold Creek Volcanics. Partly overlain by Warramana Sandstone[?] and Pungalina Member. Equivalent to Packsaddle Microgranite.||
8388|Hobblechain Rhyolite|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Southeastern McArthur Basin. U-Pb zircon igneous crystallisation age given.|1725 +/- 2 Ma|Tawallah Group||Overlies Gold Creek Volcanics and is laterally equivalent to Pungalina Member.||
8388|Hobblechain Rhyolite|73042|6|Mentioned|p4|Statherian|Statherian|Southern McArthur Basin, Calvert Superbasin. Geochronology is a U-Pb zircon igneous crystallisation age.|1725 +/- 2 Ma (see Fig.1.2)|Tawallah Group||Underlain by Gold Creek Volcanics. Overlain by Echo Sandstone.||
8388|Hobblechain Rhyolite|73083|6|Mentioned|p40|||||||||
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.|
8468|Hooker Creek Formation|12891|5|Briefly described|p732, p733 Fig. 2|Late Cambrian|Middle Cambrian|Overlies Montejinni Limestone; overlain by Lothari Hill Sandstone. Max. thickness: ~170m. Geological province: Wiso Basin. Dolomitic siltstone, siltstone and silty dolomite; black shales contain Gloeocapsamorpha sp, an oil-prone kerogen.||||||07-FEB-11
8468|Hooker Creek Formation|31412|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
8468|Hooker Creek Formation|31413|6|Mentioned|Map legend|Cambrian|Cambrian|Middle||||||
8468|Hooker Creek Formation|31637|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
8468|Hooker Creek Formation|34810|5|Briefly described|p8|||Does not crop out in sheet area.||||||09-AUG-06
8468|Hooker Creek Formation|35125|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
8468|Hooker Creek Formation|35224|4|Described|Table 1|||See also p5.||||||26-SEP-06
8468|Hooker Creek Formation|35227|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
8468|Hooker Creek Formation|35229|4|Described|Table.1|||||||||
8468|Hooker Creek Formation|35231|4|Described|Table.1|||||||||
8468|Hooker Creek Formation|36335|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|Middle Cambrian(Ordian).||||||
8468|Hooker Creek Formation|42059|5|Briefly described|p130|||See also Fig.2||||||
8468|Hooker Creek Formation|42504|5|Briefly described|Table 54 P79|||||||||
8468|Hooker Creek Formation|45148|6|Mentioned|p2|||Formerly part of Winnecke Creek Tableland formation.||||||
8468|Hooker Creek Formation|45155|6|Mentioned|Fig.8|||||||||
8468|Hooker Creek Formation|60672|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Dolomitic silstone, silstone, sandy siltstone, dolostone, claystone.||||||11-JAN-05
8468|Hooker Creek Formation|60684|2|Defined|p49 Appendix, p17|Middle Cambrian|Middle Cambrian|Formerly included in Chewings' (1931) Winnecke Creek Tablelands formation and in Merrina Beds (Milligan et al 1966). Conformably overlies Montejinni Lst;conformably overlain by Lothari Hill Sst. Max. thick:161.5m in type section (Green Swamp Well 6).||||||28-APR-05
8468|Hooker Creek Formation|62787|6|Mentioned|p82 Fig. 3|Cambrian|Cambrian|Geological Province: Wiso Basin (NT).||||||07-FEB-11
8468|Hooker Creek Formation|64068|6|Mentioned|p225|||Wiso Basin. Correlated with Narpa Group.||||||
8468|Hooker Creek Formation|64443|6|Mentioned|p40.|||Of Wiso Basin. Correlative of Barkly Group, Georgina Basin.||||||
8468|Hooker Creek Formation|65239|5|Briefly described|p3 Fig. 4|Middle Cambrian|Middle Cambrian|Geological province: Wiso Basin. Restricted marine deposits.||||||04-JUN-09
8468|Hooker Creek Formation|65338|6|Mentioned|p71.|Middle Cambrian|Middle Cambrian|Scattered outcrops of Wiso Basin rocks occur in LANDER RIVER area.||||||
8468|Hooker Creek Formation|65345|5|Briefly described|pp3-4, p6 Fig.5, p7. |Cambrian|Cambrian|Wiso Basin. Over 160 m thick. Waterbore RN020989 contains two intervals of ore-grade phosphate at shallow depths. Restricted marine deposits.||||Overlies Montejinni Limestone. Is overlain by Lothari Hill Sandstone.|Interbedded siltstone and shale, with thin dolostone interbeds more abundant towards the base of the Formation.|
8468|Hooker Creek Formation|69437|5|Briefly described|p22:10-11, 15-16|Series 2|Series 2|Wiso Basin, Centralian B Superbasin. Sequence 1. Peritidal and restricted shallow-marine deposits. Has good petroleum reservoir potential.||||Overlies Montejinni Limestone. Is overlain by Lothari Hill Sandstone.|Fine-grained siliciclastic rocks and lesser dolomitic limestone.|12-JUL-16
8468|Hooker Creek Formation|69443|6|Mentioned|p28:21|||Wiso Basin.||||Correlated with Barkly Group.||12-JUL-16
8468|Hooker Creek Formation|69446|6|Mentioned|p31:3|||Wiso Basin. Strong species-level similarity with correlative faunas of Tindall Limestone (Daly Basin).||||||12-JUL-16
8468|Hooker Creek Formation|69447|3|Fully described|p32:2-5, 7-8|Middle Cambrian|Middle Cambrian|Kennewell and Huleatt (1980). Wiso Basin. Peritidal to restricted marine deposits. Up to 161.5m thick, in the type section in BMR Green Swamp Well-6. Exposed as low rises or thin caps on scarps. Has strong species-level similarity to correlative faunas of Linnekar Limestone and Panton Formation (Ord Basin) and Tindall Limestone (Daly Basin). Associated with the Kunayangku and Lady Judith phosphate prospects. Associated with economically insignificant copper occurrences. Has produced good groundwater flows locally; may form an effective petroleum reservoir. Intraformational siltstone and claystone may provide seals.||||Conformably and gradationally overlies Montejinni Limestone. Is overlain gradationally by Lothari Hill Sandstone and unconformably by Point Wakefield beds or Buchanan Hills beds.|Maroon-green siltstone, minor limestone, quartz sandstone; limestone beds fossiliferous (trilobites including Redlichia, brachiopods, hyoliths, echinoderm plates).|12-JUL-16
8468|Hooker Creek Formation|69448|6|Mentioned|p33:3|||Wiso Basin.||||Correlated with Negri Subgroup (Ord Basin) in part.||12-JUL-16
8468|Hooker Creek Formation|69673|5|Briefly described|x, p142, p145|Cambrian|Cambrian |161.5m thick.||||Overlies the Montejinni Limestone|Laminated, bioturbated micaceous siltstone and grey dolomitic mudstone with minor marine dolomitic limestone beds and dolomitic quartz sandstone.|
8468|Hooker Creek Formation|70380|6|Mentioned|p745|Stage 5|Stage 4|Wiso Basin.||||||
8468|Hooker Creek Formation|70854|5|Briefly described|Map legend.|Cambrian|Cambrian|Wiso Basin.|||||Dolomitic siltstone, siltstone, sandy siltstone, dolostone, claystone.|
8468|Hooker Creek Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, siltstone, dolostone|
8468|Hooker Creek Formation|73083|6|Mentioned|p38, p49||||||||Mostly siliciclastics with lesser dolomite (4 to 1 ratio).|
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.||||||
8504|Horseshoe Bend Shale|22760|5|Briefly described|p340|||Parent - Finke Group.  Age - may be Famennian.||||||
8504|Horseshoe Bend Shale|22826|6|Mentioned|p576|Devonian|Devonian|||||||
8504|Horseshoe Bend Shale|23858|5|Briefly described|p916|Late Devonian|Middle Devonian|Of Finke Group. Overlying Unit Idracowra Sandstone. Underlying Unit Langra Conglomerate. Geological Province: Amadeus Basin.||||||
8504|Horseshoe Bend Shale|24301|4|Described|p22, p7 Tb. 2|Devonian|Devonian|Of Finke Group. Overlies Langra Formation, underlies Idacowra Sandstone. Maximum thickness: 566m. Geological Province: Amadeus Basin.||||||
8504|Horseshoe Bend Shale|30544|6|Mentioned|Fig.5|||||||||
8504|Horseshoe Bend Shale|31566|6|Mentioned|p244|||Devonian.||||||
8504|Horseshoe Bend Shale|31567|3|Fully described|p285|||Refers Wells et al. (1966).||||||
8504|Horseshoe Bend Shale|33844|6|Mentioned|Table 1|||||||||
8504|Horseshoe Bend Shale|33971|3|Fully described|p30|||Refers Wells et al. (1966).||||||
8504|Horseshoe Bend Shale|34111|5|Briefly described|Table 2|||Devonian - Carboniferous||||||
8504|Horseshoe Bend Shale|34580|4|Described|Table 1|||Devonian - Carboniferous||||||
8504|Horseshoe Bend Shale|35102|6|Mentioned|Fig.17|||||||||
8504|Horseshoe Bend Shale|41125|6|Mentioned|p40|||||||||
8504|Horseshoe Bend Shale|42504|6|Mentioned|p81|||||||||
8504|Horseshoe Bend Shale|42699|5|Briefly described|map legend|Devonian||||||||
8504|Horseshoe Bend Shale|42940|6|Mentioned|Plate 5|||||||||
8504|Horseshoe Bend Shale|43035|5|Briefly described|p25|||of Finke Group||||||
8504|Horseshoe Bend Shale|44133|5|Briefly described|p44|Carboniferous?|Late Devonian|Of the Finke Group. Conformably overlies Mereenie Sandstone.||||||
8504|Horseshoe Bend Shale|44323|14|Not recorded|map legend|Carboniferous|Devonian|SG/53-6. Dev-Carb. pt. of Finke Group.||||||
8504|Horseshoe Bend Shale|44342|4|Described|p.7, Table 2|Carboniferous|Devonian|SG/53-5. Dev-Carbon.||||||
8504|Horseshoe Bend Shale|44343|14|Not recorded|map legend|Carboniferous|Devonian|Dev-Carbon.||||||
8504|Horseshoe Bend Shale|44393|4|Described|p.6,7,8,Tb.1,Fig.1|Carboniferous|Devonian|Part of Finke Group. Dev-Carb.||||||
8504|Horseshoe Bend Shale|44433|14|Not recorded|map legend|||Devonian to Carboniferous.||||||
8504|Horseshoe Bend Shale|45041|4|Described|p104|||Devonian||||||
8504|Horseshoe Bend Shale|48865|2|Defined|p.4,5,Fig.33||Paleozoic|On many figures. Fig.4,21,27,38,29,31,32,36,39,41,52,Pl.5,10,11. Unit of Finke Group. (G53-3,6).||||||07-NOV-08
8504|Horseshoe Bend Shale|48890|4|Described|p.52|Carboniferous|Devonian|Pt. Finke Gp. Dev-Carb.||||||
8504|Horseshoe Bend Shale|50372|5|Briefly described|Map Legend|Devonian|Devonian|Of Finke Group. Geological Province: Amadeus Basin. C||||||10-AUG-06
8504|Horseshoe Bend Shale|65309|4|Described|p6 Table 1, pp13-14, p19.|Devonian|Devonian|Very distinctive unit, with isolated exposures in northeast map area. Most outcrops only a few metres thick. Contains a relative abundance of halite pseudomorphs and detrital biotite, implying arid conditions during deposition.||Unit in Finke Group.||Is overlain by Idracowra Sandstone.|Fine to very fine, chocolate-brown, biotitic quartz sandstone or siltstone.|
8504|Horseshoe Bend Shale|65342|6|Mentioned|p10.|||Pedirka Basin. Max. thickness at least 86 m.  Seen as having potential as an insulating layer for geothermal energy.||||Overlies Langra Sandstone. Is overlain by Idracowra Sandstone.||
8504|Horseshoe Bend Shale|65489|6|Mentioned|p63|||Potential to act as a seal.||||||
8504|Horseshoe Bend Shale|69438|3|Fully described|p23:2-3, 40-41|Late Devonian|Late Devonian|Wells et al. (1966). Amadeus Basin. Most widespread unit of the Group, but most poorly exposed. Is 92m thick at the type locality N of Horseshoe Bend homestead. Up to 310m thick elsewhere. Lithology described in some detail. Appears as Horshoe Bend Shale on 23:3.||Finke Group.||Conformably overlies Langra Formation. Is overlain transitionally by Idracowra Sandstone.|Red-brown and lesser green siltstone, with minor thin interbeds of fine sandstone.|12-JUL-16
8504|Horseshoe Bend Shale|69449|5|Briefly described|p34:5|Devonian|Devonian|||Finke Group.||Overlies Langra Formation. Is overlain by Idracowra Sandstone.||12-JUL-16
8504|Horseshoe Bend Shale|69673|6|Mentioned|p64 fig 53, p149|||||Finke Group||Overlies Langra Formation||
8504|Horseshoe Bend Shale|71279|5|Briefly described|p355 Fig.2|Late Devonian|Late Devonian|Amadeus Basin.||Finke Group.||||
8504|Horseshoe Bend Shale|73085|6|Mentioned|p1|late Devonian|late Devonian|[Unclear relationship with Idracowra Sandstone].||Finke Group||Underlain by Langra Formation. Equivalent to Brewer Conglomerate (Pertnjara Group).||
8558|Hugh River Shale|9199|5|Briefly described|Map legend|Cambrian|Cambrian|Of the Pertaoorrta Group.  Siltstone, shale, limestone, dolomite.  Geological Province: Amadeus Basin.||||||04-NOV-04
8558|Hugh River Shale|9814|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Pertaoorrta Group. Shale, limestone, silty sandstone, siltstone.||||||
8558|Hugh River Shale|22442|6|Mentioned|p54|||Amadeus Basin||||||
8558|Hugh River Shale|22561|5|Briefly described|p21|Neoproterozoic|Neoproterozoic|||||||03-DEC-15
8558|Hugh River Shale|22566|6|Mentioned|Fig 2 on p77, &p87|Late Cambrian|Middle Cambrian|Of the Pertaoorrta Group.||||||27-SEP-06
8558|Hugh River Shale|22650|6|Mentioned|p 159|Cambrian|Cambrian|||||||
8558|Hugh River Shale|22651|5|Briefly described|p 171|Middle Cambrian|Middle Cambrian|Of the Pertaoorrta Group.  Informally divided into upper and lower Hugh River Shale p 171.||||||27-SEP-06
8558|Hugh River Shale|22653|6|Mentioned|p 242|||||||||
8558|Hugh River Shale|22654|6|Mentioned|p 246|||||||||
8558|Hugh River Shale|22656|6|Mentioned|p 277||Middle Cambrian|||||||
8558|Hugh River Shale|22804|6|Mentioned|Fig 2 on p432|Cambrian|Cambrian|Of the Pertaoorrta Group.||||||27-SEP-06
8558|Hugh River Shale|22826|6|Mentioned|Fig 2 on p565|Cambrian|Cambrian|||||||
8558|Hugh River Shale|23361|5|Briefly described|16 Fig.4|Cambrian|Neoproterozoic III|||||||
8558|Hugh River Shale|24334|5|Briefly described|p48 Tb.1|Middle Cambrian|Early Cambrian|Age: 505 - 535 Ma.||||||
8558|Hugh River Shale|29721|6|Mentioned|Table 44|||||||||
8558|Hugh River Shale|29972|6|Mentioned|Table 1|||Middle Cambrian||||||
8558|Hugh River Shale|30544|6|Mentioned|p48|||On map legend||||||
8558|Hugh River Shale|30659|6|Mentioned|p87|||Lower-Middle Cambrian age||||||
8558|Hugh River Shale|30660|6|Mentioned|Table 1|||Middle Cambrian age||||||
8558|Hugh River Shale|30661|6|Mentioned|Table 1|||||||||
8558|Hugh River Shale|30662|6|Mentioned|p188|||Palaeomagnetic dates||||||
8558|Hugh River Shale|33307|6|Mentioned|Fig.6|||||||||
8558|Hugh River Shale|33625|6|Mentioned|Table 2|||||||||
8558|Hugh River Shale|34442|5|Briefly described|Table 1|||Cambrian||||||
8558|Hugh River Shale|34579|4|Described|Table 2|||Cambrian. see p16.||||||27-SEP-06
8558|Hugh River Shale|35088|6|Mentioned|Fig.8|||||||||
8558|Hugh River Shale|35102|6|Mentioned|Fig.2|||||||||
8558|Hugh River Shale|36198|6|Mentioned|Fig.III.2|||||||||
8558|Hugh River Shale|37818|6|Mentioned|Table 2|||||||||
8558|Hugh River Shale|38606|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
8558|Hugh River Shale|38885|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
8558|Hugh River Shale|39210|6|Mentioned|Fig.11|||||||||
8558|Hugh River Shale|39213|6|Mentioned|Fig.6|||Amadeus Basin Succession||||||
8558|Hugh River Shale|39583|6|Mentioned|Map legend|Middle Cambrian|Early Cambrian|Early to Middle CambrianE - M||||||
8558|Hugh River Shale|40254|6|Mentioned|Fig.7|||||||||
8558|Hugh River Shale|40740|3|Fully described|p42|||Mention p5.||||||27-SEP-06
8558|Hugh River Shale|40810|4|Described|p6|||||||||
8558|Hugh River Shale|41115|6|Mentioned|Fig.2|||||||||
8558|Hugh River Shale|41190|6|Mentioned|Fig.4|||||||||
8558|Hugh River Shale|41224|6|Mentioned|Fig.2|||||||||
8558|Hugh River Shale|41270|6|Mentioned|Table 1|||||||||
8558|Hugh River Shale|41717|6|Mentioned|Fig.2|||||||||
8558|Hugh River Shale|42082|6|Mentioned|Fig.3 P323|||||||||
8558|Hugh River Shale|42504|5|Briefly described|Fig. 23 P103|||||||||
8558|Hugh River Shale|42940|5|Briefly described|Plate 12|||||||||
8558|Hugh River Shale|43225|5|Briefly described|Map Legend||Cambrian|Of Pertaoorrta Group.||||||27-SEP-06
8558|Hugh River Shale|43503|6|Mentioned|12-50|Mindyallan|Boomerangian|||||||
8558|Hugh River Shale|43648|6|Mentioned|p491|||||||||
8558|Hugh River Shale|43649|6|Mentioned|p457|||||||||
8558|Hugh River Shale|44133|5|Briefly described|p4 Fig. 7.2, 42|Early Cambrian|Early Cambrian|Geological Province: Western Warburton Basin.||||||
8558|Hugh River Shale|44402|5|Briefly described|map legend||Cambrian|Part of Pertaoorrta Group.||||||02-DEC-04
8558|Hugh River Shale|44497|4|Described|p.9, Table 1||Cambrian|SF/53-13.||||||
8558|Hugh River Shale|44498|14|Not recorded|map legend||Cambrian|Part of Pertaoorrta Group.||||||
8558|Hugh River Shale|45041|5|Briefly described|p53|||M.- U. Camb.||||||
8558|Hugh River Shale|46928|6|Mentioned|Table 1|||||||||
8558|Hugh River Shale|48639|14|Not recorded|p.17|||||||||
8558|Hugh River Shale|48838|2|Defined|p.15, Tb.1||Cambrian|L & M Cam.||||||
8558|Hugh River Shale|48862|14|Not recorded|p.16-20|||Name now superseded by Hugh River Shale Member. (F52-15).||||||
8558|Hugh River Shale|48863|14|Not recorded|p.22|||Prob.partly equiv.to Illara Sandstone.||||||
8558|Hugh River Shale|48865|14|Not recorded|Fig.4,opp.p.10||Cambrian|Unit of Pertaoorrta Gp. (F53-13).||||||
8558|Hugh River Shale|48890|4|Described|p.41||Cambrian|See also Tables, Figs, Plates. pt. Pertaoorrta Gp. Defn. on Tech.File F/53-13.||||||
8558|Hugh River Shale|48963|6|Mentioned|Fig.3|||||||||
8558|Hugh River Shale|60547|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Pertaoorrta Group. Siltstone, shale, limestone, dolomite. Geological Province: Amadeus Basin.||||||03-JUN-05
8558|Hugh River Shale|60674|5|Briefly described|Map legend|Cambrian|Cambrian|Of the Pertaoorrta Group.  Red-brown, fine calcareous siltstone and sandstone. Geological Province: Amadeus Basin.||||||
8558|Hugh River Shale|61309|5|Briefly described|p16 Fig. 4|||Geological Province: Amadeus Basin.||||||06-FEB-08
8558|Hugh River Shale|61518|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Pertaoorta Group. Red-brown fine grained calcareous siltstone and sandstone. Geological Province: Amadeus Basin.||||||
8558|Hugh River Shale|61732|5|Briefly described|p99|Cambrian|Cambrian|Together with other Cambrian units overlies the Arumbera Sandstone.||||||07-FEB-11
8558|Hugh River Shale|62376|5|Briefly described|p18|Late Cambrian|Middle Cambrian|Of the Pertaoorrta Group. Geological Province: Amadeus Basin.||||||09-FEB-10
8558|Hugh River Shale|62379|5|Briefly described|p7 Fig. 2, p17|Late Cambrian|Middle Cambrian|Of the Pertaoorrta Group. Geological Province: Amadeus Basin. Siltstone, shale, carbonate.||||||
8558|Hugh River Shale|64068|5|Briefly described|p62, 65, 225|||Amadeus Basin. Lower part correlated with Arthur Creek Formation, Beetle Creek Formation. In part correlated with Steamboat Sandstone.||||||
8558|Hugh River Shale|64778|6|Mentioned|p13|Cambrian|Cambrian|Amadeus Basin.||||||
8558|Hugh River Shale|64809|6|Mentioned|p3 Fig.2, p6 Fig.4, p11 Fig.10.   |Late Cambrian|Middle Cambrian|See also p13 Fig.13 .||Unit in Pertaoorrta Group.||||
8558|Hugh River Shale|65233|5|Briefly described|p3 Fig. 2, p8|Late Cambrian|Middle Cambrian|Of the Pertaoorrta Group. Interfingers in N and E of basin with Tempe Formation. Geological province: Amadeus Basin.||||||07-FEB-11
8558|Hugh River Shale|65342|6|Mentioned|p4.|||Amadeus Basin. Max. thickness at least 258 m.||||Overlies Giles Creek Dolostone. Is overlain by Shannon Formation.||
8558|Hugh River Shale|67326|5|Briefly described|p2, p5|Late Cambrian|Middle Cambrian|Amadeus Basin.||Pertaoorrta Group.||Overlies Chandler Formation. Is overlain by Jay Creek Limestone and Goyder Formation.||
8558|Hugh River Shale|67565|4|Described|p40, p47.|Cambrian|Cambrian|Not shown on the map; outcrops poorly north of the Idirriki Range. Lateral equivalent of Tempe and Deception Formations, and the Illara and Petermann Sandstones. Thickness of c.450 m. Deposited in two distinct episodes.||||Grades laterally into Cleland Sandstone.|Red-brown, fine-grained calcareous sandstone and siltstone.|03-DEC-15
8558|Hugh River Shale|67856|6|Mentioned|p338 fig 4-30|Cambrian|Cambrian|||Of Pertaoorta Group.||||
8558|Hugh River Shale|68316|6|Mentioned|p778 Fig.1|||||||||
8558|Hugh River Shale|68323|6|Mentioned|p4 Fig.2|Late Cambrian|Middle Cambrian|Amadeus Basin.||Pertaoorrta Group.||||
8558|Hugh River Shale|69437|5|Briefly described|p22:10-11|Series 2|Series 2|Amadeus Basin. Nearshore to shallow-marine deposits.||||Overlies Chandler Formation. Is overlain by Jay Creek Limestone, Goyder Formation.|Shale and siltstone, with lesser dolostone and sandstone.|12-JUL-16
8558|Hugh River Shale|69438|3|Fully described|p23:2-3, 7, 24, 28-31|Late Cambrian|Middle 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, and included in the Pertaoorrta Group, by Ranford et al. (1965). Amadeus Basin. Poorly exposed. c.500m thick. Relationship to other units in the Group is geographically variable. Facies change into Tempe Formation. Fossils indicate an Ordian age. A lateral equivalent of the Illara Sandstone-Deception Formation-Petermann Sandstone succession. Part-equivalent to Giles Creek Dolostone; Tempe, Shannon Formations; and Cleland Sandstone.||Pertaoorrta Group.||Disconformably overlies Chandler Formation and Arumbera Sandstone. Is overlain conformably by Jay Creek Limestone and Goyder Formation.|Red-brown and grey-brown siltstone and shale, with minor thin beds of dolostone, limestone, sandstone and chert.|12-JUL-16
8558|Hugh River Shale|69439|6|Mentioned|p24:10|||Amadeus Basin.||||Lower part is correlated with the Bloodwood Formation (Ngalia Basin).||12-JUL-16
8558|Hugh River Shale|69449|6|Mentioned|p34:2 Fig.34.2|Cambrian|Cambrian|Eastern Amadeus Basin. Has equivalent rocks in the western Warburton Basin.||||||12-JUL-16
8558|Hugh River Shale|69673|4|Described|p65, p80, p82,  p149 fig 120|||Potential source rock. Estimated thickness of 500m.||||Disconformably overlies Chandler Formation, overlain by Jay Creek Limestone|Disconformably overlies Chandler Formation, overlain by Jay Creek Limestone|
8558|Hugh River Shale|71114|5|Briefly described|p171-4, p176, p178-180|Drumian||Amadeus Basin. Deposited between ~511 and 490 Ma, in a shallow marine environment during sea level lowstand and contains trilobite fragments, but lacking biostratigraphic correlation. 151m thick in Dingo 1 well. Includes up to 16% anhydrite in Dingo 2, and 25% in Alice 1.||||Overlies Giles Creek Dolostone. Is overlain by Shannon Formation.||14-FEB-18
8558|Hugh River Shale|71279|5|Briefly described|p355 Fig.2, p365|Late Cambrian|Middle Cambrian|Amadeus Basin.||Pertaoorrta Group.||||
8558|Hugh River Shale|72358|6|Mentioned|p118|Series 3|Series 3|Of Amadeus Basin.||||||
8558|Hugh River Shale|72516|6|Mentioned|p92|Cambrian|Cambrian|Amadeus Basin.||||Equivalent to the Arthur Creek Formation and the Steamboat Sandstone.||03-JUN-21
8558|Hugh River Shale|73085|6|Mentioned|p1|late Cambrian|middle Cambrian|Partly equivalent to Deception Sandstone, Illara Sandstone, Tempe Formation, Shannon Formation, Giles Creek Dolostone.||Pertaoorrta Group [and equivalents?]||Underlain by Chandler Formation. Overlain and partly equivalent to Jay Creek Limestone and lower Goyder Formation. [See comments].||
8558|Hugh River Shale|73281|6|Mentioned|Appendix (DIP)|||See DIP034_Welldata.xlsx.||||||
8560|Hughie Sandstone|14019|5|Briefly described|p4 Fig. 3|||Of the Wattie Group. Conformably overlies the Burtawurta Formation, Wickham Formation. Conformably overlain by the Mount Sanford Formation. Fine to medium quartz sandstone. Max. Thickness: 90m. Geological Province: Victoria Basin.||||||
8560|Hughie Sandstone|24122|5|Briefly described|p4 Fig.3|||Of Wattie Group.  Geological Province: Victoria Basin.||||||
8560|Hughie Sandstone|24297|3|Fully described|p6|Proterozoic|Proterozoic|Of Wattie Group. Conformably overlain by Mount Sanford Formation, conformably overlies Burtawurta Formation. Maximum thickness: 87m.  See also p5 Tb. 2.||||||
8560|Hughie Sandstone|24298|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Wattle Group. Quartz sandstone.||||||27-SEP-06
8560|Hughie Sandstone|24441|5|Briefly described|p1 Fig. 1|Mesoproterozoic|Mesoproterozoic|Of the Wattie Group. Overlies Burtawurta Formation; overlain by Mount Sanford Formation. Geological Province: Victoria Basin.||||||08-AUG-05
8560|Hughie Sandstone|24442|5|Briefly described|p50 Fig. 1|||Of the Wattie Group. Geological Province: Victoria Basin.||||||
8560|Hughie Sandstone|28255|3|Fully described|p35, Tb. 11 (opp. p8)|Adelaidean|Adelaidean|Of the Wattie Group.  Fine- to medium-grained quartz sandstone. Conformably overlain by Mount Sanford Formation.; conformably overlies Burtawurta Formation. Max. thickness: 130m.||||||
8560|Hughie Sandstone|30003|4|Described|p8, p12|||Of the Wattie Group. Max. thickness: 132m.||||||19-APR-05
8560|Hughie Sandstone|30004|6|Mentioned|Map legend|Proterozoic|Proterozoic|Carpentarian or Adelaidean||||||
8560|Hughie Sandstone|32172|4|Described|Table 1|||Carpentarian or Adelaidean||||||
8560|Hughie Sandstone|32173|5|Briefly described|Map legend|Adelaidean|Carpentarian|Of the Wattie Group.  Fine to medium quartz sandstone.  Carpentarian or Adelaidean (per legend).||||||16-NOV-04
8560|Hughie Sandstone|32175|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Wattie Group.  Massive fine and medium quartz sandstone.||||||02-DEC-04
8560|Hughie Sandstone|32660|5|Briefly described|Table 6|||||||||
8560|Hughie Sandstone|33374|6|Mentioned|p7|||Stratigraphy.||||||
8560|Hughie Sandstone|33375|5|Briefly described|p7, p9 Tb. 1|||Of the Wattie Group. Overlain by Mount Sanford Formation.||||||26-APR-05
8560|Hughie Sandstone|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
8560|Hughie Sandstone|33378|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Wattie Group. Massive quartz sandstone.||||||27-APR-05
8560|Hughie Sandstone|45112|5|Briefly described|Table 9|||||||||
8560|Hughie Sandstone|48943|2|Defined|p45|Adelaidean|Adelaidean|||||||
8560|Hughie Sandstone|60589|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Wattie Group.  Quartz sandstone.  Geological Province: Victoria Basin.||||||
8560|Hughie Sandstone|60672|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Quartz sandstone. Overlies Burtawurta Formation. Overlain by Mount Sanford Formation. Of Wattie Group. Geological Province: Victoria Basin.||||||11-JAN-05
8560|Hughie Sandstone|60685|4|Described|p4 Fig. 3 , p6||Paleoproterozoic|Of the Wattie Group. Fine to medium sandstone. Conformable on Burtawurta Formation, Wickham Formation; conformable below Mount Sanford Formation. Max. thickness: 87m. Geological Province: Victoria Basin.||||||07-NOV-08
8560|Hughie Sandstone|65342|6|Mentioned|p11 Fig.13. |||Victoria Basin.||Unit in Wattie Group.||Overlies Burtawurta Formation. Is overlain by Mount Sanford Formation.||
8560|Hughie Sandstone|67151|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Birindudu Basin.||Unit in Wattie Group.||Overlies Burtawurta Formation. Is overlain by Mount Sanford Formation.|Massive quartz sandstone.|
8560|Hughie Sandstone|68733|5|Briefly described|p177 Fig.2, p179 Tb.1, p185-186|||Previously included in the Victoria Basin by Cutovinos et al. (2002). Now included in the Birrindudu Basin due to a recent subdivision by the NGTS (Dunster and Ahmad 2013). Sm-Nd isotope data tabulated.||Of the Wattie Group.||||05-DEC-17
8560|Hughie Sandstone|69432|5|Briefly described|p17:2, 9|||Birrindudu Basin. Shallow-marine and near marine deposits including minor subaerial exposure.||Wattie Group.||Conformably overlies Burtawurta or Wickham Formations. Is overlain conformably by Mount Sanford Formation.|Cross-bedded and ripple marked, fine to medium, immature quartz sandstone.|12-JUL-16
8560|Hughie Sandstone|69673|6|Mentioned|p48 fig 35|||||Wattie Group||Overlies Burtawurta Formation, overlain by Mount Sanford Formation||
8560|Hughie Sandstone|70655|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Birindudu Basin.||Wattie Group.||Overlies Burtawurta Formation. Is overlain by Mount Sanford Formation.|Massive quartz sandstone.|24-JAN-22
8560|Hughie Sandstone|70854|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Wattie Group.||Overlies Burtawurta Formation. Is overlain by Mount Sanford Formation.|Quartz sandstone.|
8560|Hughie Sandstone|70855|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Wattie Group.||Overlies Burtawurta Formation. Is overlain by Mount Sanford Formation.|Quartz sandstone.|
8560|Hughie Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
8560|Hughie Sandstone|71302|4|Described|p1,6-7,15-21,72,74||Paleoproterozoic|Of Birindudu Basin. Forms low, weakly terraced hills adjacent to Wattie Creek in central-eastern LIMBUNYA 1: 250 000 sheet (Cutovinos et al., 2002). Up to 90m thick; deposited in transgressive, shallow marine and near marine conditions that included minor subaerial exposure. Sample GA 1956888 (quartz sandstone) yielded an interpreted (weighted mean 207Pb/206Pb) maximum depositional age of 1675+\-17 Ma. Major zircon provenance peaks at c. 1700-1950 Ma (maxima c. 1770-1780 Ma), smaller peaks c. 1590-1640 Ma, subordinate clusters at c. 1900-2000 Ma and 2500-2550 Ma. Sample location, description, zircon description, SHRIMP analyses and results are discussed.||Unit of Wattie Group.||Overlain by Mount Sanford Formation. Underlain conformably by Burtawurta Formation.|Cross-bedded and ripple marked, fine- to medium-grained, immature to mature quartz sandstone, locally ferruginous (reduction spots).|09-DEC-19
8560|Hughie Sandstone|72718|6|Mentioned|p7|||Birrindudu Basin.||Wattie Group||Underlain by Burtawurta Formation. Overlain by Mount Sanford Formation.||
8560|Hughie Sandstone|73083|6|Mentioned|p31|||||||||
8643|Idracowra Sandstone|22826|6|Mentioned|Fig 2 on p565|Devonian|Devonian|||||||
8643|Idracowra Sandstone|23858|5|Briefly described|p916||Late Devonian|Of Finke Group. Underlain by Horseshoe Bend Shale. Geological Province: Amadeus Basin.||||||27-SEP-06
8643|Idracowra Sandstone|30544|6|Mentioned|p51|||On map legend||||||
8643|Idracowra Sandstone|31566|6|Mentioned|p244|||Devonian.||||||
8643|Idracowra Sandstone|31567|3|Fully described|p288|||Refers Wells et al. (1966).||||||
8643|Idracowra Sandstone|33971|3|Fully described|p30|||Refers Wells et al. (1966)||||||
8643|Idracowra Sandstone|34580|4|Described|Table 1|||Devonian - Carboniferous||||||
8643|Idracowra Sandstone|35102|6|Mentioned|Fig.17|||||||||
8643|Idracowra Sandstone|42504|5|Briefly described|p81|||||||||
8643|Idracowra Sandstone|42699|5|Briefly described|map legend|Devonian||||||||
8643|Idracowra Sandstone|43035|5|Briefly described|p26|||Of Finke Group.||||||27-SEP-06
8643|Idracowra Sandstone|44133|6|Mentioned|p44|||||||||
8643|Idracowra Sandstone|44323|14|Not recorded|map legend|Carboniferous|Devonian|SG/53-6. Dev-Carb. Part of Finke Group.||||||27-SEP-06
8643|Idracowra Sandstone|44342|4|Described|p.7, Table 2|Carboniferous|Devonian|SG/53-5. Dev-Carbon.||||||
8643|Idracowra Sandstone|44343|14|Not recorded|map legend|Carboniferous|Devonian|Dev-Carb.||||||
8643|Idracowra Sandstone|44393|6|Mentioned|Fig.1|Devonian|Cambrian|Correlates with Santo Sandstone. Dev-Camb.||||||
8643|Idracowra Sandstone|45041|4|Described|p105|||Of the Finke Group.||||||27-SEP-06
8643|Idracowra Sandstone|48865|2|Defined|p.5.Fig.34|Carboniferous|Devonian|On many figures. Fig.4,21,29,33,35,Pl.10,11. Unit of Finke Group. Devn.Carb. (G53-5,6).||||||
8643|Idracowra Sandstone|48890|14|Not recorded|Tb.3,p.51,53|||Defn. on Tech.File E/53-8.||||||
8643|Idracowra Sandstone|50372|5|Briefly described|Map Legend|Devonian|Devonian|Of Finke Group. Geological Province: Amadeus Basin. Fine to medium grained quartz sandstone.||||||
8643|Idracowra Sandstone|65309|4|Described|p6 Table 1, pp13-14. |Devonian|Devonian|Commonly exposed below Mesozoic sediments in basal parts of mesas. Usually less than 6m thick, but up to 50m in bores.||Unit in Finke Group.||Overlies Horseshoe Bend Shale. Is overlain disconformably by Algebuckina Sandstone.|Fine to medium quartz sandstone, white to pale yellow; thinly bedded, weakly kaolinitic.|
8643|Idracowra Sandstone|65342|6|Mentioned|p10.|||Pedirka Basin. Max. thickness at least 245 m.||||Overlies Horseshoe Bend Shale. Is overlain by Crown Point Formation.||
8643|Idracowra Sandstone|69438|3|Fully described|p23:2-3, 40-42|Late Devonian|Late Devonian|Wells et al. (1966). Includes the lateral equivalent, Santo Sandstone, which name has been abandoned. Amadeus Basin. It is 52m thick at the type section, 6.5km SSW of Idracowra Station; reaches 280m thick at Mount Hakea. Sediment supply was from the NW, unlike a SW source for the lower Finke Group.||Finke Group.||Transitionally overlies Horseshoe Bend Shale (locally disconformably).|Dominated by sedimentary cycles, average 2m thick, of typically white to pale grey medium-grained sandstone, some of which is pebbly. Contains mudclasts, current lineations and mudcracks.|12-JUL-16
8643|Idracowra Sandstone|69449|5|Briefly described|p34:5|Devonian|Devonian|||Finke Group.||Overlies Horseshoe Bend Shale and (disconformably) Langra Formation.|Sandstone and claystone.|12-JUL-16
8643|Idracowra Sandstone|69673|6|Mentioned|p64 fig 53, p149|||||Finke Group||Overlies Langra Formation||
8643|Idracowra Sandstone|71279|5|Briefly described|p355 Fig.2|Late Devonian|Late Devonian|Amadeus Basin.||Finke Group.||||
8643|Idracowra Sandstone|73085|6|Mentioned|p1|late Devonian|late Devonian|[Unclear relationship with Horseshoe Bend Shale].||Finke Group||Underlain by Langra Formation. Equivalent to Brewer Conglomerate (Pertnjara Group).||
8643|Idracowra Sandstone|73281|6|Mentioned|Appendix (DIP)|||See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
8653|Illara Sandstone|22561|5|Briefly described|p21|Neoproterozoic|Neoproterozoic|||||||
8653|Illara Sandstone|22646|6|Mentioned|p 100|||||||||
8653|Illara Sandstone|22650|6|Mentioned|p 159|Cambrian|Cambrian|||||||
8653|Illara Sandstone|22651|4|Described|p 187|Late Cambrian|Middle Cambrian|Of the Pertaoorrta Group.||||||27-SEP-06
8653|Illara Sandstone|22653|6|Mentioned|p 241|||||||||
8653|Illara Sandstone|22654|5|Briefly described|p 249|||||||||
8653|Illara Sandstone|22763|6|Mentioned|Table 1 on p386|Cambrian|Cambrian|Of the Pertaoorrta Group.||||||27-SEP-06
8653|Illara Sandstone|22804|6|Mentioned|Fig 2 on p432|Cambrian|Cambrian|Of the Pertaoorrta Group.||||||27-SEP-06
8653|Illara Sandstone|22826|6|Mentioned|Fig 2 on p565|Cambrian|Cambrian|||||||
8653|Illara Sandstone|23250|5|Briefly described|p1124 Fig.2||Middle Cambrian|Correlate of Lake Frome Group.||||||
8653|Illara Sandstone|23361|5|Briefly described|16 Fig.4|Cambrian|Neoproterozoic III|||||||
8653|Illara Sandstone|29721|6|Mentioned|Table 44|||||||||
8653|Illara Sandstone|33307|6|Mentioned|Fig.6|||||||||
8653|Illara Sandstone|34442|5|Briefly described|Table 1|||Cambrian||||||
8653|Illara Sandstone|35102|6|Mentioned|Fig.2|||||||||
8653|Illara Sandstone|36198|6|Mentioned|p294|||See also Fig.III.2||||||
8653|Illara Sandstone|39213|6|Mentioned|Fig.6|||Amadeus Basin Succession||||||
8653|Illara Sandstone|40254|6|Mentioned|Fig.7|||||||||
8653|Illara Sandstone|40740|3|Fully described|p43|||||||||
8653|Illara Sandstone|40810|5|Briefly described|p13|||Mention p3.||||||27-SEP-06
8653|Illara Sandstone|41190|6|Mentioned|Fig.4|||||||||
8653|Illara Sandstone|41224|6|Mentioned|Fig.2|||||||||
8653|Illara Sandstone|41233|6|Mentioned|Fig.3|||||||||
8653|Illara Sandstone|41270|6|Mentioned|Table 1|||||||||
8653|Illara Sandstone|41717|6|Mentioned|Fig.2|||||||||
8653|Illara Sandstone|41723|6|Mentioned|Map legend|Neoproterozoic||||||||
8653|Illara Sandstone|42082|6|Mentioned|Fig.3 P323|||||||||
8653|Illara Sandstone|42940|5|Briefly described|Plate 12|||||||||
8653|Illara Sandstone|43225|5|Briefly described|Map Legend||Cambrian|Of Pertaoorrta Group.||||||27-SEP-06
8653|Illara Sandstone|43503|6|Mentioned|12-50|Undillan|Floran|||||||
8653|Illara Sandstone|43649|6|Mentioned|p457|||||||||
8653|Illara Sandstone|44395|14|Not recorded|p.8||Cambrian|Correlates with Cleland Sandstone.||||||
8653|Illara Sandstone|44402|5|Briefly described|map legend||Cambrian|Part of Pertaoorrta Group.||||||02-DEC-04
8653|Illara Sandstone|44484|14|Not recorded|p.10, Tb.1||Cambrian|Part of Pertaoorrta Group.||||||
8653|Illara Sandstone|44485|14|Not recorded|map legend||Cambrian|Part of Pertaoorrta Group.||||||
8653|Illara Sandstone|44497|4|Described|p.10, Table 1||Cambrian|SF/53-13.||||||
8653|Illara Sandstone|44498|14|Not recorded|map legend||Cambrian|Part of Pertaoorrta Group.||||||
8653|Illara Sandstone|44505|14|Not recorded|p.7, Table 1||Cambrian|Of Pertaoorrta Group.||||||
8653|Illara Sandstone|44506|14|Not recorded|map legend||Cambrian|||||||
8653|Illara Sandstone|45041|5|Briefly described|p53|||M.Camb.||||||
8653|Illara Sandstone|45155|6|Mentioned|p34|||||||||
8653|Illara Sandstone|45170|6|Mentioned|Table 3|||||||||
8653|Illara Sandstone|48863|2|Defined|p.22||Middle Cambrian|Tb.1. opp.p.7,9,19,20,Pl.10,15,16. Middle Cambrian. (G52-4,G53-1).||||||
8653|Illara Sandstone|48865|14|Not recorded|Fig.4,opp.p.10||Cambrian|(G52-4,F53-13). Unit of Pertaoorrta Gp.||||||
8653|Illara Sandstone|48963|6|Mentioned|Fig.3|||||||||
8653|Illara Sandstone|61309|5|Briefly described|p16 Fig. 4|||Geological Province: Amadeus Basin.||||||06-FEB-08
8653|Illara Sandstone|61385|5|Briefly described|Map legend|Cambrian|Cambrian|Red brown sandstone, silty sandstone.  Geological Province: Amadeus Basin.||||||
8653|Illara Sandstone|61732|5|Briefly described|p99|Cambrian|Cambrian|Together with other Cambrian units overlies the Arumbera Sandstone.||||||07-FEB-11
8653|Illara Sandstone|62376|5|Briefly described|p18|Middle Cambrian|Middle Cambrian|Of the Pertaoorrta Group. Geological Province: Amadeus Basin.||||||09-FEB-10
8653|Illara Sandstone|62379|5|Briefly described|p7 Fig. 2, p17|Middle Cambrian|Middle Cambrian|Of the Pertaoorrta Group. Geological Province: Amadeus Basin.||||||
8653|Illara Sandstone|64068|6|Mentioned|p65, 225|||Amadeus Basin. Correlated with Steamboat Sandstone.||||||
8653|Illara Sandstone|64778|6|Mentioned|p15-16, 18, 22|Cambrian|Cambrian|Amadeus Basin. Thermal history summarised. Max. palaeotemperature analysis summary.|530-525 Ma.|||||
8653|Illara Sandstone|64809|6|Mentioned|p3 Fig.2 |Middle Cambrian|Middle Cambrian|||Unit in Pertaoorrta Group.||||
8653|Illara Sandstone|65233|5|Briefly described|p3 Fig. 2, p8|Middle Cambrian|Middle Cambrian|Of the Pertaoorrta Group. Conformably overlies the Tempe Formation, but this study suggests 'Illara Sandstone' should be included within Tempe Formation and its name made redundant. Geological province: Amadeus Basin.||||||07-FEB-11
8653|Illara Sandstone|67326|5|Briefly described|p2, p4|Middle Cambrian|Middle Cambrian|Amadeus Basin.||Pertaoorrta Group.||Overlies Tempe Formation. Is overlain by Deception Sandstone.||
8653|Illara Sandstone|67565|4|Described|p40, p47.|Cambrian|Cambrian|Restricted to the Gardiner Anticline. Type locality in the Gardiner Range. c.200 m thick. Lateral equivalent of Hugh River Shale. Correlates with the lower Shannon Formation in the eastern Amadeus Basin.||||Conformably overlies Tempe Formation. Is overlain conformably by Deception Formation.|Fine- and medium-grained micaceous and feldspathic sandstone, with minor interbeds of micaceous siltstone and calcareous sandstone; moderately sorted and cross-bedded, convolute bedding and slumped cross-beds common.|
8653|Illara Sandstone|67856|6|Mentioned|p338 fig 4-30|Cambrian|Cambrian|||Of Pertaoorta Group.||||
8653|Illara Sandstone|68323|6|Mentioned|p4 Fig.2|Middle Cambrian|Middle Cambrian|Amadeus Basin.||Pertaoorrta Group.||||
8653|Illara Sandstone|69437|5|Briefly described|p22:10|Series 3|Series 3|Amadeus Basin.||||Overlies Tempe Formation. Is overlain by Petermann Sandstone, Deception Formation.||12-JUL-16
8653|Illara Sandstone|69438|4|Described|p23:2-3, 24, 29-30, 59|Middle Cambrian|Middle Cambrian|Wells et al. (1965). Carmichael Sub-basin, Amadeus Basin. Forms prominent strike ridges. c.200m thick. The Illara Sandstone-Deception Formation-Petermann Sandstone succession is a lateral equivalent of both Cleland Sandstone and Hugh River Shale. Hydrocarbon source rock intervals may be present.||Pertaoorrta Group.||Disconformably overlies Tempe Formation. Is overlain conformably by Deception Formation. Equivalent to upper Hugh River Shale, lower Cleland Sandstone and Shannon Formation.|Red-brown, fine- to medium-grained, feldspathic and micaceous quartz sandstone, with minor layers of micaceous siltstone and shale.|12-JUL-16
8653|Illara Sandstone|69673|5|Briefly described|p64 fig 53, p66, p80, p82, p88, p91|||up to 200m thick.||||Disconformably overlies Tempe Formation, overlain by Deception Sandstone|Fine to medium grained, feldspathic and micaceous quartz sandstone with minor layers of micaceous siltstone and shale.|
8653|Illara Sandstone|71114|4|Described|p171, p170 fig 1b, p175-177, p179-180|Drumian|Stage 5|Amadeus Basin western succession. Deposited between ~511 and 490 Ma. Deposited in a restricted, partly lacustrine nearshore setting with detrital input from the hinterland. ||||Overlies Tempe Formation. Is overlain by Deception Formation..|Fluvially-dominated sandstone with occasional lacustrine incursions.|14-FEB-18
8653|Illara Sandstone|71279|5|Briefly described|p355 Fig.2|Middle Cambrian|Middle Cambrian|Amadeus Basin.||Pertaoorrta Group.||||
8653|Illara Sandstone|71898|5|Briefly described|p9, p11|||Amadeus Basin.||||Disconformably overlies the Tempe Formation. Conformably overlain by the Deception Formation.||
8653|Illara Sandstone|72358|6|Mentioned|p118|Series 3|Series 3|Of Amadeus Basin.||||||
8653|Illara Sandstone|72374|4|Described|iii,p3-4,14-17|Cambrian|Cambrian|Of Amadeus Basin. Restricted in outcrop to the Gardiner Range, Petermann Creek and Parana Hill anticlines; forming laterally continuous 'ribs' of outcropping sandstone with intervening, ~1 m thick recessive intervals that suggest an alternation between sandstone and siltstone or shale. Sample HB16ND231 (sandstone) yielded an interpreted maximum depositional age of 566+\-5 Ma. Detrital zircon provenance indicate significant recycling from underlying Amadeus Basin succession. Detrital zircons of c. 1400-900 Ma (c. 1258 Ma and c. 1086 Ma peak) likely sourced from Warumpi Province. C. 1800-1430 Ma zircons likely derived from the Aileron and Warumpi provinces to the north, and Musgrave Province to the south. Neoarchean-Paleoproterozoic (c. 2710-2000 Ma) and Neoproterozoic-Cambrian zircons (c. 685-500 Ma) likely sourced from east Gondwana.||Unit of Pertaoorrta Group.||Partially laterally equivalent to Petermann Sandstone and Deception Formation.|Red-brown, fine- to mediumgrained, feldspathic and micaceous quartz sandstone, together with minor micaceous siltstone and shale.|11-OCT-19
8653|Illara Sandstone|72516|6|Mentioned|p92|Cambrian|Cambrian|Amadeus Basin.||||Equivalent to the Steamboat Sandstone.||03-JUN-21
8653|Illara Sandstone|73085|4|Described|piii, p1, p3-7, p9-11|middle Cambrian|middle Cambrian|Amadeus Basin. 73 m thick in drillhole LA05DD01. Upper lithology is more feldspathic than the overlying Petermann Sandstone.||Pertaoorrta Group [and equivalents?]||Underlain by Tempe Formation. Overlain by Petermann Sandstone and Deception Sandstone. Equivalent to Cleland Sandstone and Hugh River Shale.|Dark red to brown, finely laminated to massive, fine- to medium-grained feldspathic, micaceous sandstone and red to dark orange, fine-grained, finely laminated, clay cemented silty sandstone.|
8675|Inca Formation|22954|6|Mentioned|Fig3p9|Middle Cambrian|Middle Cambrian|||||||
8675|Inca Formation|23031|6|Mentioned|17|||Geol Province Georgina Basin||||||
8675|Inca Formation|23393|5|Briefly described|p22, p23 Fig. 6|Middle Cambrian|Middle Cambrian|||||||
8675|Inca Formation|24034|6|Mentioned|p48|||Clay-rich litology.||||||06-MAY-09
8675|Inca Formation|30239|5|Briefly described|p1193|||||||||
8675|Inca Formation|30242|6|Mentioned|Fig.2|||||||||
8675|Inca Formation|30479|6|Mentioned|Fig.5|||See also Fig.6,Fig.7. stratigraphic relationships||||||
8675|Inca Formation|30775|6|Mentioned|p1|||||||||
8675|Inca Formation|30778|6|Mentioned|p1,Fig.5|||||||||
8675|Inca Formation|30914|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
8675|Inca Formation|31289|6|Mentioned|Fig. 1|||Middle Cambrian||||||
8675|Inca Formation|31342|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
8675|Inca Formation|31396|6|Mentioned|Fig.3|||||||||
8675|Inca Formation|31465|6|Mentioned|p418|||Trilobite content||||||
8675|Inca Formation|32576|5|Briefly described|p49|||||||||
8675|Inca Formation|32948|6|Mentioned|p111|||||||||
8675|Inca Formation|32952|4|Described|p1188|||M.-U.Cambrian. See also pp1189-1194,1203-1213.||||||27-SEP-06
8675|Inca Formation|33111|4|Described|p36|||Mention Fig.4||||||
8675|Inca Formation|33368|6|Mentioned|p5|||Bituminous limestone||||||
8675|Inca Formation|33482|6|Mentioned|Fig.2|||Cambrian||||||
8675|Inca Formation|34287|6|Mentioned|Fig.3|||||||||
8675|Inca Formation|34395|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
8675|Inca Formation|34543|6|Mentioned|p98|||||||||
8675|Inca Formation|34754|6|Mentioned|p42|||||||||
8675|Inca Formation|34903|6|Mentioned|p582|||||||||
8675|Inca Formation|35001|6|Mentioned|Fig.45|||||||||
8675|Inca Formation|35004|6|Mentioned|Fig.60|||||||||
8675|Inca Formation|35054|6|Mentioned|Table 23|||||||||
8675|Inca Formation|35121|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
8675|Inca Formation|35139|4|Described|Table.2|||||||||
8675|Inca Formation|35553|6|Mentioned|p10|||See also Appendix 2, description of Agnostid localities.||||||
8675|Inca Formation|35556|6|Mentioned|Plate 4|||||||||
8675|Inca Formation|35939|6|Mentioned|p633|||||||||
8675|Inca Formation|36234|3|Fully described|p168|||||||||
8675|Inca Formation|36243|6|Mentioned|Table 1A|||||||||
8675|Inca Formation|36645|5|Briefly described|p314|||Fig.2.||||||
8675|Inca Formation|36818|6|Mentioned|p203|||||||||
8675|Inca Formation|37413|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
8675|Inca Formation|37572|4|Described|p158|||See also Fig.7||||||
8675|Inca Formation|38444|5|Briefly described|p105|||||||||
8675|Inca Formation|38446|6|Mentioned|Table 23|||||||||
8675|Inca Formation|38608|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
8675|Inca Formation|39445|5|Briefly described|Table 4|||See also p62.||||||27-SEP-06
8675|Inca Formation|39690|6|Mentioned|Table 1|||||||||
8675|Inca Formation|39797|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
8675|Inca Formation|39943|6|Mentioned|Table 2C|||||||||
8675|Inca Formation|40004|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
8675|Inca Formation|40221|4|Described|p20|||||||||
8675|Inca Formation|40386|6|Mentioned|p440|||||||||
8675|Inca Formation|40686|5|Briefly described|p407|||||||||
8675|Inca Formation|40852|6|Mentioned|p37|||||||||
8675|Inca Formation|40855|6|Mentioned|p345|||||||||
8675|Inca Formation|40856|5|Briefly described|p315|||||||||
8675|Inca Formation|40857|5|Briefly described|p268|||||||||
8675|Inca Formation|40858|5|Briefly described|p132|||||||||
8675|Inca Formation|41129|6|Mentioned|Fig.8|||||||||
8675|Inca Formation|41240|6|Mentioned|Fig.1|||||||||
8675|Inca Formation|41298|6|Mentioned|Map legend|Middle Cambrian||||||||
8675|Inca Formation|41388|6|Mentioned|p552|||||||||
8675|Inca Formation|41639|6|Mentioned|p3|||||||||
8675|Inca Formation|42139|6|Mentioned|Fig.12 P78|||||||||
8675|Inca Formation|42575|5|Briefly described|Fig.2 P335|||||||||
8675|Inca Formation|43105|6|Mentioned|p16|||||||||
8675|Inca Formation|43807|6|Mentioned|Fig.2,p347|||||||||
8675|Inca Formation|44091|14|Not recorded|p16,Tb.1,18||Middle Cambrian|||||||
8675|Inca Formation|44205|14|Not recorded|p69,78,89|||||||||
8675|Inca Formation|44210|2|Defined|map,p6,13,Tb.2|||Overlies Beetle Creek Formation or Pilpah Sandstone.||||||
8675|Inca Formation|44211|14|Not recorded|p95-98,100-103|||||||||
8675|Inca Formation|44213|14|Not recorded|Map Legend||Middle Cambrian|||||||
8675|Inca Formation|44275|14|Not recorded|Map Legend|||||||||
8675|Inca Formation|44276|14|Not recorded|p20,22,Tb.2,map|||||||||
8675|Inca Formation|44277|14|Not recorded|Map Legend||Middle Cambrian|||||||
8675|Inca Formation|44757|14|Not recorded|p155||Middle Cambrian|Divided into Upper Limestone, and Lower Shale members.||||||
8675|Inca Formation|44788|14|Not recorded|p27|||||||||
8675|Inca Formation|44882|14|Not recorded|p177||Cambrian|In French||||||
8675|Inca Formation|44989|14|Not recorded|p.122|||||||||
8675|Inca Formation|45052|3|Fully described|p92|||M.Camb. See also p32.||||||27-SEP-06
8675|Inca Formation|45054|6|Mentioned|p6|||Fossil locality||||||
8675|Inca Formation|45062|6|Mentioned|p7|||||||||
8675|Inca Formation|45079|4|Described|p30|||Cambrian age||||||
8675|Inca Formation|45119|6|Mentioned|p4|||||||||
8675|Inca Formation|45166|5|Briefly described|Table 15|||||||||
8675|Inca Formation|47024|6|Mentioned|Table 1|||||||||
8675|Inca Formation|47058|5|Briefly described|p125|||||||||
8675|Inca Formation|49027|6|Mentioned|p7|||||||||
8675|Inca Formation|50100|5|Briefly described|p22|Early Ordovician|Early Cambrian|Predominantly shallow-marine, clastic, calcareous, dolomitic, cherty and phosphatic sedimentary rocks.  Overlies the Beetle Creek Formation.; passes laterally into Roaring Siltstone.  ||||||
8675|Inca Formation|60122|6|Mentioned|p57 Appendix|||Correlated with parts of the arthur Creek Formation. Geological Province: eastern Georgina Basin and Burke River Structural Belt.||||||
8675|Inca Formation|60264|5|Briefly described|p575 Fig. 1|Middle Cambrian|Middle Cambrian|See also Inca Shale.||||||
8675|Inca Formation|60359|5|Briefly described|Map Legend|Cambrian|Cambrian|Siltstone, shale, sandstone, chert, limestone.||||||
8675|Inca Formation|63450|4|Described|p81|Middle Cambrian|Middle Cambrian|Contains a shale member ~100m thick - probably the Inca Shale mentioned in Fig. 5 (p78). Overlain by Devoncourt Limestone but with hiatus between.||||||07-FEB-11
8675|Inca Formation|64068|4|Described|p63, p59, 62, p114|Middle Cambrian|Middle Cambrian|Potential oil source. Contains diverse fauna. Correlated with Arthur Creek Formation, Blazan Shale, Currant Bush Limestone, Age Creek Formation.||Of Narpa Group.||Disconformably overlies Beetle Creek Formation or Thorntonia Limestone. Conformably overlain by Currant Bush Limestone, V Creek Limestone, Roaring Silstone, Devoncourt Limestone.|Laminated pyritic siliceous shale and siltstone, chert, dark foetid limestone.|05-APR-12
8675|Inca Formation|64443|6|Mentioned|p40.|||Correlative of Wonarah Formation.||||||
8675|Inca Formation|67127|6|Mentioned|p78|||Primary host for phosphorite REE deposits.||||||
8675|Inca Formation|67323|5|Briefly described|GIS attrib tbl; p83, p92 Fig.12.2|Cambrian|Cambrian|Georgina Basin.||Narpa Group.||Overlies Beetle Creek Formation, locally unconformably. Is overlain by Currant Bush Limestone and (unconformably) by Roaring Siltstone and Devencourt Limestone.|Siliceous shale and chert with limestone interbeds.|
8675|Inca Formation|67352|6|Mentioned|p69|||||||||
8675|Inca Formation|67402|6|Mentioned|p215, p217|||||||Overlies the Thorntonia Limestone||
8675|Inca Formation|69443|5|Briefly described|p28:16, 20, 2223|Middle Cambrian|Middle Cambrian|Georgina Basin.||Narpa Group.||Disconformably overlies Thorntonia Limestone. Is overlain by and partially interfingers with Currant Bush Limestone. Correlated with Anthony Lagoon, Wonarah Formations.||12-JUL-16
8675|Inca Formation|69573|6|Mentioned|p659|||Contains Drumian Stage [Cambrian] fossil sites.||||||
8675|Inca Formation|69591|4|Described|p87-89, p91-92, p96-97, p98 Fig.2.91|Cambrian|Cambrian|Burke River Structural Belt, Georgina Basin. Exposed in low rolling hills, mesas, cliffs and creek banks along the Basin margin. Up to 150m thick. Contains a rich agnostoid trilobite fauna. Is in part laterally equivalent to Currant Bush Limestone and Gowers Formation. Is lithologically identical to Blazan Shale. Is also lithologically identical to Roaring Siltstone, which is considered to be its northern younging extension; they are distinguished by fossil fauna (named).||Narpa Group.||Conformably overlies Beetle Creek Formation and Thorntonia Limestone. Is overlain by Currant Bush Limestone, and unconformably by Roaring Siltstone and Devoncourt Limestone.|Laminated siliceous shale and siltstone (bituminous when fresh) with bands of chert and large lenses of impure flaggy and ellipsoidal limestone varying from 3 to 150m thick and pinching out to the N.|
8675|Inca Formation|70723|5|Briefly described|p21-29, p31|Cambrian|Cambrian|Georgina Basin. Deposited in a marine environment under anoxic conditions. Oil-prone source rock. Kerogen type and biomarker compositions discussed in detail.||Narpa Group||Overlies Beetle Creek Formation, overlain by Currant Bush Limestone|Laminated pyritic and calcareous shale and siltstone, interbedded with limestone that contains abundant organic matter.|
8675|Inca Formation|70864|6|Mentioned|p74 Fig 2||Paleozoic|Shown as a combined unit with Beetle Creek Formation.||||||
8675|Inca Formation|72297|5|Briefly described|p747, p752|Cambrian|Cambrian|Georgina Basin. TOC value of 2.82% reported.|||||Contains thin oil shale beds.|
8675|Inca Formation|72321|6|Mentioned|Fig 2|Drumian|Wulian|Burke River Structural Belt, Georgina Basin. Australian stages:  Floran to Undillan. Undilla Sub-basin, Georgina Basin.  Australian Stages: Templetonian to Undillan. ||of Narpa Group.||||
8675|Inca Formation|72516|6|Mentioned|p92|Cambrian|Cambrian|Eastern Georgina Basin.||||Equivalent to the Arthur Creek Formation.||03-JUN-21
8675|Inca Formation|73418|5|Briefly described|p3, p4 Fig.3|Miaolingian|Miaolingian|Georgina Basin, Burke River Structural Belt and Undilla Sub-basin.||Narpa Group||Overlies Beetle Creek Formation, underlies Currant Bush Limestone, lateral equivalent of Blazan Shale and Roaring Siltstone.|Shale/siltstone/chert sequence.|
8703|Ingula Migmatite|40079|6|Mentioned|p87|||||||||
8703|Ingula Migmatite|69427|4|Described|p12:9-10|||Shaw et al. (1979). Strangways Range region, Aileron Province. Large areas mapped as Ingula Migmatite NW of Saltbush Bore by Shaw et al. (1979) have been reinterpreted as Wuluma Granite by Collins et al. (1989).|1810-1800 inferred from fig 12.9|Strangways Metamorphic Complex.||Has faulted and gradational contacts with Erontonga Metamorphics. Grades into Wuluma Granite.|Migmatite and felsic gneiss with lesser mafic granulite, cordierite gneiss and sillimanite gneiss.|29-JAN-18
8769|Irindina Gneiss|9199|5|Briefly described|Map legend|||Biotite-plagioclase-garnet-quartz gneiss, muscovite schist.  Geological Province: Arunta Block.||||||04-NOV-04
8769|Irindina Gneiss|9394|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block (Division 2). Of the Harts Range Group. Garnet-biotite gneiss, sillimanite gneiss.||||||
8769|Irindina Gneiss|9694|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block (Division Two). Of the Harts Range Group. Gneiss, schist, marble.||||||
8769|Irindina Gneiss|22524|6|Mentioned|p41,p42|||Of Maidment 2005, Buick et al. 2005. ? In part now Yambla Gneiss?||||||02-FEB-19
8769|Irindina Gneiss|23844|5|Briefly described|p44|||Of the Harts Range Group. Garnet quartzofeldspathic gneiss, amphibolite, gneiss and marble.||||||27-SEP-06
8769|Irindina Gneiss|23983|5|Briefly described|p27|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
8769|Irindina Gneiss|23984|5|Briefly described|p3 Fig.2|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
8769|Irindina Gneiss|24540|6|Mentioned|p6|||Hosts a sodic pegmatite suite. Geological Province: Arunta region.||||||07-FEB-11
8769|Irindina Gneiss|33103|6|Mentioned|p14|||Probably contains outcrops mapped as Harts Range Group.||||||27-SEP-06
8769|Irindina Gneiss|34488|6|Mentioned|p8|||||||||
8769|Irindina Gneiss|38885|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
8769|Irindina Gneiss|39552|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
8769|Irindina Gneiss|39583|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob. Early Proterozoic||||||19-JUN-13
8769|Irindina Gneiss|39610|6|Mentioned|p6|||||||||
8769|Irindina Gneiss|39887|6|Mentioned|Fig.3|||||||||
8769|Irindina Gneiss|39898|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Harts Range Group. Schistose garnet-biotite-quartz-plagioclase gneiss, biotite gneiss, quartzofeldspathic gneiss, layered and massive amphibolite. Geological Province: Amadeus Basin.||||||07-NOV-08
8769|Irindina Gneiss|39931|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic. Of the Harts Range Group.||||||07-NOV-08
8769|Irindina Gneiss|40100|5|Briefly described|p258|||||||||
8769|Irindina Gneiss|40538|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Block.||||||07-NOV-08
8769|Irindina Gneiss|40906|4|Described|p8|||||||||
8769|Irindina Gneiss|40977|5|Briefly described|p296|||||||||
8769|Irindina Gneiss|41083|6|Mentioned|Fig.3|||||||||
8769|Irindina Gneiss|41967|6|Mentioned|p248|||||||||
8769|Irindina Gneiss|42504|6|Mentioned|Plate 8 P27|||||||||
8769|Irindina Gneiss|44114|5|Briefly described|p321|||Central Arunta Inlier. Shallow-marine sedimentary rocks.|>1750 Ma (Mortimer et al., 1987).||||Pelitic and calcareous rocks, amphibolite.|
8769|Irindina Gneiss|44327|14|Not recorded|Tb.I,p.7,map||Archean|(F53-11).||||||07-NOV-08
8769|Irindina Gneiss|44328|14|Not recorded|map legend||Archean|Archaean.||||||07-NOV-08
8769|Irindina Gneiss|44964|14|Not recorded|p.38|||||||||
8769|Irindina Gneiss|46730|4|Described|p6, 11, 12|||Of Harts Range Group. Geological Province: Arunta Block.||||||
8769|Irindina Gneiss|46740|14|Not recorded|p.188|||||||||
8769|Irindina Gneiss|46830|6|Mentioned|p23|||Refs Joklik 1955||||||
8769|Irindina Gneiss|46868|6|Mentioned|p77|||||||||
8769|Irindina Gneiss|48844|14|Not recorded|p.1,10,15,Pl.8|||(F53-11).||||||
8769|Irindina Gneiss|48880|4|Described|p.11,12||Archean|p.9,10. Archaean. Ref. to Joklik 1955.||||||07-NOV-08
8769|Irindina Gneiss|48992|6|Mentioned|p12|||||||||
8769|Irindina Gneiss|49036|6|Mentioned|p13|||||||||
8769|Irindina Gneiss|60525|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block (Division 2). Garnet-biotite-quartz-plagioclase gneiss; amphibolite.||||||
8769|Irindina Gneiss|60547|5|Briefly described|Map Legend|Precambrian|Precambrian|Of the Harts Range group. Biotite-plagioclase-garnet-quartz gneiss, muscovite schist.||||||
8769|Irindina Gneiss|60549|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Harts Range Group.  Quartzofeldspathic gneiss, biotite gneiss, quartzite, layered amphibolite, minor garnet-bearing biotite gneiss.  Probably Paleoproterozoic?||||||07-NOV-08
8769|Irindina Gneiss|60668|5|Briefly described|p12|||Of the Harts Range Group.  Associated laterally with mafic sheets of Riddock Amphibolite. ||||||
8769|Irindina Gneiss|62595|4|Described|p4 Table 2, p11, p13, p34 Fig.14.|Middle Cambrian|Early Cambrian|Age from detrital zircons. Deposition within a deeper extensional sub-basin between the Amadeus and Georgina Basins, coeval with partial melting of underlying Harts Range Group. Relative probability plots of detrital zircon data are shown.|<520-510 Ma.|Unit in Harts Range Group.|||Thick sequence of garnet-biotite-plagioclase +/- sillimanite schist and gneiss, with minor layers of marble, calc-silicate and quartzite; locally migmatitic, with garnets to 15cm; intercalated with amphibolite of Harts Range Meta-Igneous Complex.|
8769|Irindina Gneiss|64337|4|Described|pp374-376|||Contains garnet-bearing leucosomes. Recent geochronological results are discussed.||Of Harts Range Complex.|Includes Riddock Amphibolite and Naringa Calcsilicate.|Structurally underlies Brady Gneiss.|Fe-rich metapelites and metapsammites.|
8769|Irindina Gneiss|65358|5|Briefly described|p14|Neoproterozoic|Neoproterozoic|Of Harts Range Group. Dominant lithologies include schistose garnet-biotite gneiss, sillimanite gneiss and biotite gneiss.||||||
8769|Irindina Gneiss|66767|5|Briefly described|p59|||Irindina Province.||||Overlies Stanovos Gneiss.|A thick package of biotite-garnet-quartz-plagioclase +/- sillimanite schist, with locally interlayered marble, calc-silicate, mafic amphibolite and quartzite.|
8769|Irindina Gneiss|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Arunta Block.|1747 +/- 11 Ma.|||||
8769|Irindina Gneiss|68316|5|Briefly described|p777, p778, p779, p780, p783 Fig.4, p785||Series 2|Contains detrital zircon spectra similar to Amadeus Basin units. Age constrained by the Harts Range Meta-Igneous Complex. Probability distribution diagram (Fig. 4) for ages of detrital zircons, 2 samples (1 from this study and other from Buick et al. 2001).||Lowermost unit of the Harts Range Meta-Igneous Complex.|Includes Naringa Calccareous Member.|Overlain by the Brady Gneiss.|Metapelite-dominated.|10-APR-17
8769|Irindina Gneiss|68517|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Arunta Block. Early Proterozoic? age.||Of the Harts Range Group.|Includes Stanovos Gneiss Member and Riddock Amphibolite Member.||Schistose garnet-biotite-quartz-plagioclase gneiss, biotite gneiss, quartzofeldspathic gneiss, layered and massive amphibolite, calc-silicate rock, and marble.|
8769|Irindina Gneiss|68697|6|Mentioned|p22, p24, p46|||||Harts Range Metamorphic Complex.||||
8769|Irindina Gneiss|69031|5|Briefly described|p5|Statherian|Statherian|The oldest gneiss dated in the northern Harts Range, Irindina Province.|1745 +/- 6 Ma (SHRIMP U-Pb zircon: Maidment, 2005)|Harts Range Metamorphic Complex.|||Megacrystic gneiss.|
8769|Irindina Gneiss|69383|6|Mentioned|p58|||Replaced in part by Bruna Gneiss.||||||
8769|Irindina Gneiss|69418|6|Mentioned|p3:21|||Arunta Region. Hosts the Molyhil W-Mo skarn deposit (described).||||||12-JUL-16
8769|Irindina Gneiss|69427|4|Described|p12:37|Statherian|Neoproterozoic|Harts Range. Megacrystic gneisses, with SHRIMP ages 1745 +/- 6 Ma and 1746 +/- 6 Ma  are interleaved with Irindian Gneiss and distinguished from Bruna Granitic Gneiss by the presence of garnet and absence of hornblende. SHRIMP U-Pb zircon ages (both Maidment, 2005)|1745 +/- 6 Ma and 1746 +/- 6 Ma.|||Interleaved with the Harts Range Metamorphic Complex.|Granitic gneiss and megacrystic gneiss containing K-feldspar (with coarse phenocrysts preserved in low-strain domains), quartz, plagioclase, biotite and minor garnet.|18-DEC-19
8769|Irindina Gneiss|69437|6|Mentioned|p22:6|||Irindina Province.|||Stanovos Gneiss Member.|||12-JUL-16
8769|Irindina Gneiss|69444|4|Described|p29:1-4, 9|Cambrian|Neoproterozoic|Shaw et al. (1982). Irindina Province. Dominant detrital zircon ages of c.1750 Ma for the lower part of this unit indicate sediment source was Bruna Granitic Gneiss. Is asssociated with the Tibbs gold-tungsten-copper prospect.||Harts Range Metamorphic Complex.|Riddock Amphibolite, Naringa Calcareous, Stanovos Gneiss, Members.|Is overlain by Brady Gneiss. Is intruded by Lloyd gabbro.|Dominated by a thick package of garnet- and biotite-rich psammopelitic schist; reworked into a biotite gneiss with porphyroblasts of garnet and K-feldspar; localised layers of marble, calc-silicate rock and quartzite.|12-JUL-16
8769|Irindina Gneiss|69917|6|Mentioned|p169, 170, 180, 190, 192|||'lower Irindina Gneiss' replaced by Yambla Gneiss. 'upper Irindina Gneiss' replaced by Spriggs Gneiss.  Part of  Irindina Gneiss possibly replaced by Stanovos Gneiss.||||||28-JUL-15
8769|Irindina Gneiss|69928|6|Mentioned|p210|||Arunta Inlier.||Harts Range Complex.|||Mafic metapelite; amphibolite facies.|
8769|Irindina Gneiss|69937|6|Mentioned|p25|||Zircon provenance signature is very similar to Gaylad Sandstone and virtually identical to that of Heavitree Quartzite.||Harts Range Metamorphic Complex.||||
8769|Irindina Gneiss|70094|5|Briefly described|p76-78, 80-81, 83-86|||Northern Harts Range. Mineralogy detailed. Calculated P - T pseudosections.||Harts Range Group.|Naringa Calcareous Member, Stanovos Gneiss Member, Harts Range Meta-Igneous Complex.|Is interleaved with the Harts Range Meta-Igneous Complex. Is overlain by Brady Gneiss.|Metapelites: garnet-sillimanite-biotite gneiss.|
8769|Irindina Gneiss|70744|5|Briefly described|p944-945|Early Cambrian|Early Cambrian|Detrital zircon age distribution graph.||Harts Range Group.|||Metasedimentary rocks.|
8769|Irindina Gneiss|70809|6|Mentioned|p24, p27|||||||||
8769|Irindina Gneiss|71592|5|Briefly described|Appendix A.|||Arunta Orogen. More than 30 age determinations given with enormous range of crystallisation and metamorphism ages.|c.1750 Ma to c.320 Ma (SHRIMP U-Pb zircon).||||Metapelite, pegmatite, metapsammite, metabasite.|
8769|Irindina Gneiss|71621|6|Mentioned|p48|||||||||
8769|Irindina Gneiss|72375|5|Briefly described|p25|||Geological province: Irindina Province.||Unit of Harts Range Metamorphic Complex.||||
8769|Irindina Gneiss|72516|5|Briefly described|p7, p78|||Irindina Province. Previously considered to be a part of the Harts Range Metamorphic Complex. [unclear if this unit still in use or obsolete, although use on p7 in Fig 12 implies currency]||Harts Range Metamorphic Complex|Includes the Stanovos Gneiss Member, Naringa Calcareous Member and the Riddock Amphibolite Member.|Overlain by the Brady Gneiss.||16-JUN-21
8769|Irindina Gneiss|72524|6|Mentioned|p8.||Cambrian [age inconsistent with parent Yambla Gniess]|Replaced by Yambla Gniess. Has a detrital zircon spectra dominated by a unimodal peak at ca. 1750 Ma and a maximum deposition age of ca. 530 Ma (Scrimgeour 2013, Buick et al 2005, Maidment 2005, Beyer et al 2013).|c. 530 max depositional age|||||
8769|Irindina Gneiss|73184|6|Mentioned|p196-197|||Arunta Inlier. Contains a 980 Ma spike in detrital zircons, potential source of Neoproterozoic detrital zircons in the Grant Group.|||||Includes metapelite.|
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
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].||||||
8892|Jay Creek Limestone|9199|5|Briefly described|Map legend|Cambrian|Cambrian|Of the Pertaoorrta Group.  Limestone, shale, dolomite; fossiliferous.  Geological Province: Amadeus Basin.||||||04-NOV-04
8892|Jay Creek Limestone|9814|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Pertaoorrta Group. Fossiliferous dolomitic limestone and shale.||||||
8892|Jay Creek Limestone|22561|5|Briefly described|p27|Neoproterozoic|Neoproterozoic|||||||
8892|Jay Creek Limestone|22646|6|Mentioned|p 104|||||||||
8892|Jay Creek Limestone|22650|6|Mentioned|p 159|Cambrian|Cambrian|||||||
8892|Jay Creek Limestone|22651|5|Briefly described|p 171|Late Cambrian|Middle Cambrian|Of the Pertaoorrta Group.||||||28-SEP-06
8892|Jay Creek Limestone|22653|6|Mentioned|p 241|||||||||
8892|Jay Creek Limestone|22654|5|Briefly described|p 245|||||||||
8892|Jay Creek Limestone|22655|5|Briefly described|p 261|||||||||
8892|Jay Creek Limestone|22760|6|Mentioned|p337|Cambrian|Cambrian|||||||
8892|Jay Creek Limestone|22804|6|Mentioned|Fig 2 on p432|Cambrian|Cambrian|Parent - Pertaoorrta Group.||||||
8892|Jay Creek Limestone|22826|4|Described|p572|Cambrian|Cambrian|||||||
8892|Jay Creek Limestone|23361|5|Briefly described|16 Fig.4|Cambrian|Neoproterozoic III|||||||
8892|Jay Creek Limestone|29721|6|Mentioned|Table 44|||||||||
8892|Jay Creek Limestone|29972|6|Mentioned|Table 1|||Middle Cambrian||||||
8892|Jay Creek Limestone|30544|6|Mentioned|p48|||On map legend||||||
8892|Jay Creek Limestone|32469|6|Mentioned|p531|||||||||
8892|Jay Creek Limestone|32720|6|Mentioned|Table 1|||Of Pertaoorta Group.||||||28-SEP-06
8892|Jay Creek Limestone|32721|6|Mentioned|p74|||Mid.Camb.||||||
8892|Jay Creek Limestone|32722|6|Mentioned|Fig.3|||Stromatolite||||||
8892|Jay Creek Limestone|32854|6|Mentioned|p354|||||||||
8892|Jay Creek Limestone|33307|6|Mentioned|Fig.6|||||||||
8892|Jay Creek Limestone|34111|5|Briefly described|Table 2|||Cambrian. See also pp6,15,18.||||||28-SEP-06
8892|Jay Creek Limestone|34579|4|Described|Table 2|||Cambrian. See p16.||||||28-SEP-06
8892|Jay Creek Limestone|34925|6|Mentioned|p125|||||||||
8892|Jay Creek Limestone|35064|6|Mentioned|p208|||||||||
8892|Jay Creek Limestone|35102|6|Mentioned|Fig.2|||||||||
8892|Jay Creek Limestone|36198|6|Mentioned|Fig.III.2|||||||||
8892|Jay Creek Limestone|38606|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
8892|Jay Creek Limestone|38885|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
8892|Jay Creek Limestone|39210|5|Briefly described|p38|||||||||
8892|Jay Creek Limestone|39213|6|Mentioned|Fig.6|||Amadeus Basin Succession||||||
8892|Jay Creek Limestone|39583|6|Mentioned|Map legend|Middle Cambrian|Early Cambrian|Late to Middle Cambrian||||||
8892|Jay Creek Limestone|40740|3|Fully described|p42|||Mention p5.||||||28-SEP-06
8892|Jay Creek Limestone|40810|4|Described|p6|||||||||
8892|Jay Creek Limestone|41203|5|Briefly described|p31|||||||||
8892|Jay Creek Limestone|41224|6|Mentioned|Fig.2|||||||||
8892|Jay Creek Limestone|41270|6|Mentioned|p278|||||||||
8892|Jay Creek Limestone|42354|5|Briefly described|Fig.3 P5|||||||||
8892|Jay Creek Limestone|42504|5|Briefly described|Fig. 23 P103|||||||||
8892|Jay Creek Limestone|42940|5|Briefly described|Plate 12|||||||||
8892|Jay Creek Limestone|43225|5|Briefly described|Map Legend||Cambrian|Of Pertaoorrta Group.||||||28-SEP-06
8892|Jay Creek Limestone|43503|6|Mentioned|12-50|Mindyallan|Undillan|||||||
8892|Jay Creek Limestone|43648|6|Mentioned|Fig.27,p509|||||||||
8892|Jay Creek Limestone|44433|14|Not recorded|map legend||Cambrian|||||||
8892|Jay Creek Limestone|44484|14|Not recorded|p.10, Tb.1|||(Cambrian).||||||
8892|Jay Creek Limestone|44485|14|Not recorded|map legend||Cambrian|Part of Pertaoorrta Group.||||||
8892|Jay Creek Limestone|44497|4|Described|p.9, Table 1||Cambrian|SF/53-13.||||||
8892|Jay Creek Limestone|44498|14|Not recorded|map legend||Cambrian|Part of Pertaoorrta Group.||||||
8892|Jay Creek Limestone|45041|5|Briefly described|p58|||M.Camb.||||||
8892|Jay Creek Limestone|46740|14|Not recorded|p.187,188|||M.Cam-early U.Cam.galena.||||||
8892|Jay Creek Limestone|46928|6|Mentioned|Table 1|||||||||
8892|Jay Creek Limestone|48639|14|Not recorded|p.5,13||Middle Cambrian|See also page, 1,4,6,7,11,17,Pl.1,Sh.2,3,Pl.2,Sh.1. M.Cambrian. (F53-14,G55-2).||||||
8892|Jay Creek Limestone|48838|2|Defined|p.15, Tb.1|||||||||
8892|Jay Creek Limestone|48862|14|Not recorded|p.16-17|||Name now superseded by Jay Creek Limestone Member. (F52-15).||||||
8892|Jay Creek Limestone|48863|2|Defined|p.19||Cambrian|Tb.1. opp.p.7,9,16,18,22,23,39,40,Pl.2,3,9,10,16. Middle-Upper Cambrian. (G53-1).||||||
8892|Jay Creek Limestone|48865|14|Not recorded|p.45,23,Fig.4||Cambrian|Unit of Pertaoorrta Gp. (F53-13).||||||
8892|Jay Creek Limestone|48890|4|Described|p.42||Cambrian|See also Tables, Figs and Plates. Part of Pertaoorrta Group.||||||28-SEP-06
8892|Jay Creek Limestone|48963|6|Mentioned|p29|||||||||
8892|Jay Creek Limestone|60547|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Pertaoorrta Group. Limestone, shale, dolomite; fossiliferous. Geological Province: Amadeus Basin.||||||
8892|Jay Creek Limestone|61309|5|Briefly described|p16 Fig. 4|||Geological Province: Amadeus Basin.||||||06-FEB-08
8892|Jay Creek Limestone|61732|5|Briefly described|p99|Cambrian|Cambrian|Together with other Cambrian units overlies the Arumbera Sandstone.||||||07-FEB-11
8892|Jay Creek Limestone|62376|5|Briefly described|p18|Late Cambrian|Middle Cambrian|Of the Pertaoorrta Group. Geological Province: Amadeus Basin.||||||09-FEB-10
8892|Jay Creek Limestone|62379|5|Briefly described|p7 Fig. 2, p14|Late Cambrian|Middle Cambrian|Of the Pertaoorrta Group. Geological Province: Amadeus Basin.||||||
8892|Jay Creek Limestone|64068|6|Mentioned|p65,67, 69, 70, 225|||Amadeus Basin. Correlated with Chabalowe Formation,  Arrinthrunga Formation, Georgina Limestone, Selwyn Range Limestone, southern Georgina Basin.||||||
8892|Jay Creek Limestone|64809|6|Mentioned|p3 Fig.2, p6 Fig.4, p11 Fig.10 |Late Cambrian|Middle Cambrian|||Unit in Pertaoorrta Group.||||
8892|Jay Creek Limestone|65233|5|Briefly described|p3 Fig. 2, p8|Late Cambrian|Middle Cambrian|Of the Pertaoorrta Group. Lower portion interfingers with Tempe Formation. Geological province: Amadeus Basin.||||||07-FEB-11
8892|Jay Creek Limestone|67326|5|Briefly described|p2|Late Cambrian|Middle Cambrian|Amadeus Basin.||Pertaoorrta Group.||Overlies Hugh River Shale and Shannon Formation. Is overlain by Goyder Formation.||
8892|Jay Creek Limestone|67856|6|Mentioned|p338 fig 4-30|Cambrian|Cambrian|||Of Pertaoorta Group.||||
8892|Jay Creek Limestone|68316|6|Mentioned|p778 Fig.1|||||||||
8892|Jay Creek Limestone|68323|6|Mentioned|p4 Fig.2|Late Cambrian|Middle Cambrian|Amadeus Basin.||Pertaoorrta Group.||||
8892|Jay Creek Limestone|69437|6|Mentioned|p22:10|Series 3|Series 3|Amadeus Basin.||||||12-JUL-16
8892|Jay Creek Limestone|69438|3|Fully described|p23:2-3, 7, 24, 30-32, 53-54|Late Cambrian|Middle Cambrian|Pritchard and Quinlan (1962). Amadeus Basin. 50m thick at its type section in Jay Creek; thickens to the S to 425m. Also appears as Jay Creek Dolostone in the text on 23:24. Stromatolites are more abundant in this Formation than in any other unit in the Basin. With the Goyder Formation, hosts the Owen Springs uneconomic Cu-Pb-Zn occurrences. Also hosts Mn mineralisation at Area 2.||Pertaoorrta Group.||Conformably overlies, and locally is equivalent to, upper Hugh River Shale. Is flanked by Shannon Formation. Is overlain conformably by, and is partly laterally equivalent to, Goyder Formation.|Grey and light yellow-brown, locally foetid, stromatolitic and thrombolitic boundstone, ooid and peloid grainstone and calcareous mudstone; siltstone; shale; lesser calcareous sandstone.|12-JUL-16
8892|Jay Creek Limestone|69673|5|Briefly described|p64 fig 53, p66, p80, p83|||Potential source rock. Up to 425m thick in places. Girvanella fossils, inarticulate brachiopods, molluscs and trilobite fragments.||||Overlies Hugh River Shale|Limestone, siltstone, shale and lesser calcareous sandstone.|
8892|Jay Creek Limestone|71114|5|Briefly described|p171, p170 fig 1b, p173-174, p178, p180|Guzhangian||Amadeus Basin. Deposited between ~511 and 490 Ma, in the intertidal to subtidal zone. Age refined to Guzhangian in the upper part of the succession.||||Overlies, and is equivalent to upper part of, Shannon Formation. Is overlain by Goyder Formation.|Characterised by oolitic, stromatolitic limestones.|14-FEB-18
8892|Jay Creek Limestone|71279|5|Briefly described|p355 Fig.2, p363, p365, p382 Tb.1|Late Cambrian|Middle Cambrian|Amadeus Basin. Modelled magnetic properties.||Pertaoorrta Group.||||
8892|Jay Creek Limestone|72358|5|Briefly described|p117-124|Series 3|Series 3|Of Amadeus Basin. Transgressive systems tract. Equivalent to Arrinthrunga Formation in the Georgina Basin. Deposited in intertidal and subtidal environments.||||Equivalent to the Shannon Formation and the Petermann Sandstone.|Limestone and dolostone with minor siltstone and shale interbeds.|10-JAN-20
8892|Jay Creek Limestone|72489|6|Mentioned|p4|Cambrian|Cambrian|Correlations of the upper Shannon Fm. with the Jay Creek Limestone have been used to bracket the Shannon Formation to between ca. 502 to 497 Ma.||||Correlated with upper part of Shannon Formation.|Includes limestone.|
8892|Jay Creek Limestone|72516|6|Mentioned|p93|Cambrian|Cambrian|Amadeus Basin.||||Equivalent to the Arrinthrunga Formation.||08-JUN-21
8892|Jay Creek Limestone|73085|6|Mentioned|p1|late Cambrian|middle Cambrian|||Pertaoorrta Group [and equivalents?]||Underlain by and partly equivalent to Hugh River Shale. Partly equivalent to Shannon Formation and lower Goyder Formation. Unconformably overlain by upper Goyder Formation.||
8949|Jessie Gap Gneiss|9199|5|Briefly described|Map legend|Precambrian|Precambrian|Of the Hayes Complex.  Biotite-quartz-feldspar granitic gneiss.  Geological Province: Arunta Block.||||||03-NOV-04
8949|Jessie Gap Gneiss|23363|5|Briefly described|352 Tab.3|Statherian|Statherian|Age: 1747+/-9Ma.||||||28-SEP-06
8949|Jessie Gap Gneiss|23733|5|Briefly described|p34 Fig.20|||Age: 1747Ma.||||||
8949|Jessie Gap Gneiss|24197|5|Briefly described|p60 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Age: 1747Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
8949|Jessie Gap Gneiss|39888|6|Mentioned|Fig.8|||||||||
8949|Jessie Gap Gneiss|50369|5|Briefly described|p1.4, 14.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Jessie Gap Suite. Age: 1747 +/- 9Ma (Shrimp).||||||07-NOV-08
8949|Jessie Gap Gneiss|60547|5|Briefly described|Map Legend|Precambrian|Precambrian|Of the Hayes Complex. Geological Province: Arunta Block. Biotite-quartz-feldspar granitic gneiss.||||||
8949|Jessie Gap Gneiss|69427|5|Briefly described|p12:14-15, 30, 36|Statherian|Statherian|Wigley Domain, Aileron Province. SHRIMP U-Pb zircon age. Mis-spelt as Jessie Gap Gniess on 12:30.|1747 +/- 9 Ma (Zhao and Bennett, 1995).||||Typically an equigranular to porphyritic, medium-grained, foliated leucocratic granite that is locally interlayered with gneissic and metasedimentary rocks.|12-JUL-16
8949|Jessie Gap Gneiss|69925|5|Briefly described|p18, 21-22, 25, 27-28, 36, 39|||Southern Arunta Province, Arunta Inlier. Ion probe U-Pb isotope analyses tabulated.|1747 +/- 9 Ma; U-Pb crystallisation age|||Is overlain nonconformably by Heavitree Quartzite. Is intruded by Stuart Dyke Swarm.|Biotite-feldspar granitic gneiss. Main phase slightly porphyritic gneissic granite.|
8949|Jessie Gap Gneiss|69931|6|Mentioned|p269, 273-274, 280, 296|Paleoproterozoic|Paleoproterozoic|Arunta Inlier. REE analyses, Sm-Nd isotopic analyses, tabulated.||Jessie Gap Suite.|||Fine- to coarse-grained, foliated granite.|
8949|Jessie Gap Gneiss|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen.|1747+/-9 Ma (crystallisation: U-Pb zircon SHRIMP)||||Felsic gneiss.|
8956|Jim Jim Granite|9534|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Intruded by Oenpelli Dolerite.||||||07-NOV-08
8956|Jim Jim Granite|9691|5|Briefly described|Map Legend|||Altered pink biotite granite, anomalously radioactive, commonly with north trending quartz filled shears: anatectic granite.||||||
8956|Jim Jim Granite|9701|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Altered pink biotite granite, anomalously radioactive, commonly with north trending quartz filled shears: anatectic granite.||||||02-JUN-05
8956|Jim Jim Granite|9733|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Altered pink biotite granite, anomalously radioactive; commonly with north trending quartz filled shears; anatectic granites.||||||
8956|Jim Jim Granite|23363|5|Briefly described|351 Tab.1|Orosirian|Orosirian|Age: 1838+/-7Ma.||||||28-SEP-06
8956|Jim Jim Granite|23867|6|Mentioned|p4|||||||||
8956|Jim Jim Granite|24197|5|Briefly described|p28, p106 Tb. 15.1|Paleoproterozoic|Paleoproterozoic|Of the Jim Jim Suite. Age: ~1825Ma. Geological Province: Pine Creek Inlier.||||||07-FEB-11
8956|Jim Jim Granite|30832|5|Briefly described|p318|||||||||
8956|Jim Jim Granite|30863|6|Mentioned|p50|||||||||
8956|Jim Jim Granite|31347|6|Mentioned|p135|||||||||
8956|Jim Jim Granite|31833|6|Mentioned|Table 2|||||||||
8956|Jim Jim Granite|32397|6|Mentioned|p399|||Intrusive. Uranium field.||||||
8956|Jim Jim Granite|32660|5|Briefly described|Table 2|||||||||
8956|Jim Jim Granite|33186|4|Described|p291|||Re origin.||||||28-SEP-06
8956|Jim Jim Granite|33278|6|Mentioned|Fig.7|||||||||
8956|Jim Jim Granite|35465|6|Mentioned|Fig.1|||Geology of Pine Creek Geosyncline||||||
8956|Jim Jim Granite|36085|6|Mentioned|p495|||||||||
8956|Jim Jim Granite|36535|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
8956|Jim Jim Granite|36635|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
8956|Jim Jim Granite|37462|4|Described|Table 4.II|||||||||
8956|Jim Jim Granite|37815|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
8956|Jim Jim Granite|39518|6|Mentioned|p3|||||||||
8956|Jim Jim Granite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
8956|Jim Jim Granite|41146|6|Mentioned|p858|||||||||
8956|Jim Jim Granite|41406|6|Mentioned|Map legend|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
8956|Jim Jim Granite|43624|6|Mentioned|p13|||Of Pine Creek Plutonic Complex.||||||28-SEP-06
8956|Jim Jim Granite|44399|14|Not recorded|map legend||Paleoproterozoic|Biotite granite.||||||07-NOV-08
8956|Jim Jim Granite|45022|4|Described|p.134,238. Pl.28.||Carpentarian|||||||
8956|Jim Jim Granite|46639|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Age: 1732+/-11Ma. Coarse white to pink even-grained to porphyritic biotie leucogranite, hornblende biotite granite. Commonly strongly altered.||||||07-NOV-08
8956|Jim Jim Granite|46824|6|Mentioned|Table 1|||See also p322.||||||28-SEP-06
8956|Jim Jim Granite|48962|6|Mentioned|Fig.15|||||||||
8956|Jim Jim Granite|50545|5|Briefly described|p115||Orosirian|Age: 1838+/-7 Ma. Of Jim Jim Suite.||||||17-DEC-07
8956|Jim Jim Granite|50586|5|Briefly described|p1.1, 5.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Of the Jim Jim Suite. Age: 1838 +/- 7Ma (Shrimp).||||||07-NOV-08
8956|Jim Jim Granite|60550|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Altered pink biotite granite, anomalously radioactive, commonly with north trending quartz filled shears: anatectic granites.||||||
8956|Jim Jim Granite|60680|5|Briefly described|Map legend|Orosirian|Orosirian|Of the Jim Jim Suite.  White to pink, coarse, evenly-grained to porphyritic biotite leucogranite and hornblende-biotite granite.  Age: 1838Ma.||||||
8956|Jim Jim Granite|61206|5|Briefly described|p516, p517 Fig.1|Early Proterozoic|Early Proterozoic|||||Intrudes Myra Falls Metamorphics.|K-U-Th-rich granites|
8956|Jim Jim Granite|63866|5|Briefly described|p110|Orosirian|Orosirian|Central Domain, Pine Creek Orogen. |1838 +/- 7 Ma (Page, OZCHRON)|David Suite||||
8956|Jim Jim Granite|64677|6|Mentioned|p6||||c.1838 Ma.|||||
8956|Jim Jim Granite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Of Jim Jim Suite. Age 1838Ma SHRIMP U/Pb.  I-type. White to pink, coarse, evenly-grained to porphyritic biotite leucogranite and hornblende-biotite granite. Intrudes Nourlangie Schist, Burrell Creek Formation and Zamu Dolerite.||||||07-JAN-09
8956|Jim Jim Granite|64956|6|Mentioned|p93|||Intrudes Nourlangie Schist.||||||07-FEB-11
8956|Jim Jim Granite|65232|5|Briefly described|p24, p22 Fig. 12, p42|||Post-orogenic granitoids, including Jim Jim Granite, Tin Camp Creek Granite and Nabarlek Granite, intruded during period 1840 - 1820 Ma (OZCHRON).||||||09-FEB-10
8956|Jim Jim Granite|67057|6|Mentioned|p463.|Paleoproterozoic|Paleoproterozoic||1732 +/- 11 Ma.|||||
8956|Jim Jim Granite|67564|3|Fully described|p7 Table 2, p19, pp36-37, p85.|Paleoproterozoic|Paleoproterozoic|Eastern Pine Creek Orogen. 530 km2 in area. A total rock Rb-Sr model age of 1732 +/- 11 Ma (Page et al. 1980) may be related to hydrothermal activity associated with Oenpelli Dolerite intrusion.|1838 +/- 7 Ma (SHRIMP U - Pb zircon).|Unit in David Suite.||Intrudes Nourlangie Schist, Zamu Dolerite and Burrell Creek Formation. Is intruded by Oenpelli Dolerite. Is overlain nonconformably by Mamadawerre Sandstone.|Coarse, equigranular; hornblende-biotite and porphyritic biotite granites; biotite leucogranite, porphyritic and even-grained, with local muscovite and tourmaline enrichment.|
8956|Jim Jim Granite|69420|5|Briefly described|p5:18, 21, 23, 67, 79|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Mineralogy and petrology/geochemistry summarised.|1838 +/- 7 Ma : SHRIMP U-Pb zircon.|Jim Jim Suite.|||Granite, leucogranite, porphyritic granite and granophyric granite.|12-JUL-16
8956|Jim Jim Granite|69577|6|Mentioned|p117 Fig.6|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.|c.1825 Ma.|||||
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.||
9110|Kakadu Group|9534|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes Munmarlary Quartzite, Mount Basedow Gneiss, Kudjumarndi Quartzite and Mount Howship Gneiss.||||||07-NOV-08
9110|Kakadu Group|9538|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Leucogneiss, quartzite, schist.  Conformably overlain by the Cahill Formation; conformably overlies the Nanambu Complex.||||||07-NOV-08
9110|Kakadu Group|9691|5|Briefly described|Map Legend|||||||||
9110|Kakadu Group|9701|5|Briefly described|Map Legend|Proterozoic|Archean|||||||07-NOV-08
9110|Kakadu Group|9733|5|Briefly described|Map Legend|Proterozoic|Proterozoic|||||||
9110|Kakadu Group|22479|5|Briefly described|fig1p2|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
9110|Kakadu Group|22810|5|Briefly described|Table2 P5|||Maximum thickness 2000m.||||||04-OCT-06
9110|Kakadu Group|23216|6|Mentioned|Fig3p5||Paleoproterozoic|||||||07-NOV-08
9110|Kakadu Group|23714|5|Briefly described|p6 Fig 4|Proterozoic|Proterozoic|||||||
9110|Kakadu Group|24047|5|Briefly described|p5 Fig.4|Paleoproterozoic|Paleoproterozoic|Quartzite, gneiss, schist.  Geological Province: Pine Creek Orogen.  See also p6 Fig. 5.||||||07-NOV-08
9110|Kakadu Group|24181|5|Briefly described|p84|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Unconformably overlies Archaean basement. Overlain by Cahill Formation.||||||07-NOV-08
9110|Kakadu Group|35140|6|Mentioned|Fig.2|||||||||
9110|Kakadu Group|36635|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
9110|Kakadu Group|37462|4|Described|Table 4.II|||||||||
9110|Kakadu Group|37579|5|Briefly described|Regional setting map legend|Paleoproterozoic|Paleoproterozoic|Leucogneiss, quartzite, schist.||||||07-NOV-08
9110|Kakadu Group|37815|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
9110|Kakadu Group|38239|6|Mentioned|Fig.2|||||||||
9110|Kakadu Group|38349|4|Described|p5|||||||||
9110|Kakadu Group|38351|4|Described|p5|||||||||
9110|Kakadu Group|38884|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
9110|Kakadu Group|39069|5|Briefly described|Table 1|||||||||
9110|Kakadu Group|39357|6|Mentioned|p3|||||||||
9110|Kakadu Group|39563|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
9110|Kakadu Group|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
9110|Kakadu Group|39801|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Leucogneiss, quartzite, schist.||||||07-NOV-08
9110|Kakadu Group|40104|6|Mentioned|p331|||||||||
9110|Kakadu Group|40168|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Leucogneiss, quartzite. schist.||||||07-NOV-08
9110|Kakadu Group|40223|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Leucogneiss, quartzite, schist.||||||07-NOV-08
9110|Kakadu Group|40243|6|Mentioned|Fig.1|||||||||
9110|Kakadu Group|40493|6|Mentioned|p21|||||||||
9110|Kakadu Group|40808|6|Mentioned|Table 2|||||||||
9110|Kakadu Group|40823|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
9110|Kakadu Group|40852|6|Mentioned|p25|||||||||
9110|Kakadu Group|41125|6|Mentioned|Fig.6|||||||||
9110|Kakadu Group|41304|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
9110|Kakadu Group|41309|6|Mentioned|p3|||||||||
9110|Kakadu Group|41311|6|Mentioned|p5|||||||||
9110|Kakadu Group|41397|6|Mentioned|p6|||||||||
9110|Kakadu Group|41406|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
9110|Kakadu Group|41407|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
9110|Kakadu Group|41586|6|Mentioned|Map legend|||||||||
9110|Kakadu Group|42012|6|Mentioned|Fig.3 P3|||||||||
9110|Kakadu Group|42372|5|Briefly described|p16|||||||||
9110|Kakadu Group|42927|5|Briefly described|p428|||see also Fig.1 p429.||||||04-OCT-06
9110|Kakadu Group|43187|5|Briefly described|p7|||||||||
9110|Kakadu Group|43595|5|Briefly described|p351|||||||||
9110|Kakadu Group|43624|6|Mentioned|Table 1,p9|Paleoproterozoic|Archean|||||||07-NOV-08
9110|Kakadu Group|43832|6|Mentioned|11,14|||Age 2000-2200 Ma||||||
9110|Kakadu Group|46639|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes Mount Basedow Gneiss, Munmarlary Quartzite, Mount Howship Gneiss and Kudjumarndi Quartzite.||||||07-NOV-08
9110|Kakadu Group|46658|6|Mentioned|p548|||||||||
9110|Kakadu Group|46675|5|Briefly described|Map legend for regional setting...|Paleoproterozoic|Paleoproterozoic|Leucogneiss, quartzite, schist.  Conformably overlain by the Cahill Formation;  conformably overlies the Nanambu Complex.  Geological Province: Pine Creek Geosyncline.||||||07-NOV-08
9110|Kakadu Group|46700|5|Briefly described|P7, Table1 P12||Proterozoic|||||||
9110|Kakadu Group|47049|6|Mentioned|Fig.2|||||||||
9110|Kakadu Group|60526|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Leucogneiss, quartzite, schist.||||||
9110|Kakadu Group|60550|5|Briefly described|Map Legend|Proterozoic|Proterozoic|||||||
9110|Kakadu Group|60680|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes: Munmarlary Quartzite, Mount Basedow Gneiss.  Geological Province: Pine Creek Orogen.||||||07-NOV-08
9110|Kakadu Group|61206|5|Briefly described|p516, p517 Fig.1|Early Proterozoic|Early Proterozoic|||||Overlies the Nanambu Complex and is overlain by the Cahill Formation and the Nourlangie Schist.|Arkosic metasedimentary rocks|
9110|Kakadu Group|61827|5|Briefly described|p158 Fig. 4|||||||||
9110|Kakadu Group|62375|5|Briefly described|p8 Table 1, 9 table 2, 10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Sandstone, arkose, siltstone, conglomerate, quartzite, schist, gneiss. Thickness: <1000m. Geological Province: Pine Creek Orogen.||||||11-FEB-10
9110|Kakadu Group|63866|5|Briefly described|p111|||Nimbuwah Domain, Pine Creek Orogen. Deposited as locally derived fluviatile to shallow marine sedimentary rocks.||||Conformably overlain by the Cahill Formation.|Meta-arkose, quartzite and quartzofeldspathic gneiss.|
9110|Kakadu Group|64698|5|Briefly described|lithinterp table|Orosirian|Paleoproterozoic|Includes Munmarlary Quartzite, Mount Basedow Gneiss, Kudjurmarndi Quartzite.||||||07-JAN-09
9110|Kakadu Group|64730|6|Mentioned|p124, 142|Paleoproterozoic|Paleoproterozoic|Significantly older than the overlying South Alligator Group, with a stratigraphic break of up to 160 millions years.||||Underlies South Alligator Group.||03-MAY-12
9110|Kakadu Group|64956|5|Briefly described|p87|||Contains Kudjumarndi Quartzite (top unit). Geological province: Pine Creek Orogen.||||||07-FEB-11
9110|Kakadu Group|65232|5|Briefly described|p7, p23, p6 Fig. 5, p5 Fig. 4|Palaeoproterozoic|Palaeoproterozoic|Includes Kudjumarandi Quartzite (missp), Munmaliary Quartzite (missp) and Mount Basedow Gneiss. Quartzite, gneiss, schist. Geol. Prov: Pine Creek Orogen. Presumed unconformably overlies Nanambu Complex; conformably underlies Cahill Formation.||||||09-FEB-10
9110|Kakadu Group|65390|6|Mentioned|p27 Fig. 6|Orosirian|Orosirian|Pine Creek Inlier. Figure 6 infers age is between about 2000 and 1870 Ma.||||||
9110|Kakadu Group|66683|5|Briefly described|pp368-369, p372. |Paleoproterozoic|Paleoproterozoic|||Unit in Woodcutters Supergroup.|Comprises Kudjumarndi Quartzite, Munmarlary Quartzite and Mount Basedow Gneiss.||Metaconglomerate, quartzite; minor psammitic to pelitic schist.|
9110|Kakadu Group|67057|6|Mentioned|p454. |||Nimbuwah Domain.||||||
9110|Kakadu Group|67355|6|Mentioned|p6, 10, 26|||Nanambu Shelf.||Woodcutters Supergroup||Correlated with the Manton Group.|Includes a radioactive arenite unit(s).|25-JAN-17
9110|Kakadu Group|67479|6|Mentioned|p33||||||Includes the Kudjumarndi Quartzite.|||
9110|Kakadu Group|67564|4|Described|p8 Table 2, p9 Fig.4, p10 Fig.5, p11.|Paleoproterozoic|Paleoproterozoic|Oldest rocks in the Pine Creek Orogen. Deformed and metamorphosed to greenschist facies during the 1860 - 1850 Ma Nimbuwah Event.|2200 Ma?||Includes Munmarlary and Kudjumarndi Quartzites, Mount Howship and Mount Basedow Gneisses.|Unconformably overlies Nanambu Complex. Is overlain by Namoona Group.|Meta-arkose, quartzofeldspathic gneiss, quartzite.|
9110|Kakadu Group|67779|5|Briefly described|p4, p6 Fig.5, p7, pp14-16, p104.|Paleoproterozoic|Paleoproterozoic|Nimbuwah Domain, Pine Creek Orogen. Deposition age based on stratigraphic correlation with Woodcutters Supergroup.|2020 Ma.||Includes Mount Basedow Gneiss, Munmarlary and Kudjumarndi Quartzites.|||14-MAY-18
9110|Kakadu Group|69419|5|Briefly described|p4:6,|Paleoproterozoic|Paleoproterozoic|Part of the metamorphosed basement to the McArthur Basin.|||||Amphibolite-facies psammitic and pelitic rocks.|12-JUL-16
9110|Kakadu Group|69420|5|Briefly described|p5:2, 4, 6-7, 23-24, 67, 82|Paleoproterozoic|Paleoproterozoic|Forms the oldest Paleoproterozoic strata in the Nimbuwah Domain, Pine Creek Orogen. Has strong similarities in (detrital zircon) provenance with the Manton and Mount Partridge Groups.||Woodcutters Supergroup.|Mount Basedow, Mount Howship Gneisses; Munmarlary, Kudjumarndi Quartzites.||Gneiss, schist, orthoquartzite.|12-JUL-16
9110|Kakadu Group|69917|6|Mentioned|p24, 42||||||Includes Munmarlary Quartzite, Kudjumarndi Quartzite.|||29-JUL-15
9110|Kakadu Group|70853|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||Kudjumarndi Quartzite.|||
9156|Kamarga Volcanics|22438|5|Briefly described|p545-547, Fig.12|||Possibly equivalent to Eastern Creek Volcanics||||||
9156|Kamarga Volcanics|22457|6|Mentioned|Fig29 P30|||Shown as Kamarga Volcs.||||||
9156|Kamarga Volcanics|22680|6|Mentioned|85|||||||||
9156|Kamarga Volcanics|23031|6|Mentioned|28|||||||||
9156|Kamarga Volcanics|23198|6|Mentioned|p873, 875|||||||||
9156|Kamarga Volcanics|23363|5|Briefly described|344 Fig.3|||||||||
9156|Kamarga Volcanics|23393|5|Briefly described|p18, p16 Fig.4|Proterozoic|Proterozoic|Intruded by Yeldham Granite.  Geological Province: Lawn Hill Sub-province.||||||
9156|Kamarga Volcanics|23406|5|Briefly described|p601 Fig.3|||||||||
9156|Kamarga Volcanics|23408|6|Mentioned|p515, p516 Fig. 5|||Onlapped by Torpedo Creek Quartzite. Includes igneous rocks.||||||15-JUN-09
9156|Kamarga Volcanics|23409|5|Briefly described|p535 Fig.2|||||||||
9156|Kamarga Volcanics|23767|5|Briefly described|p1954 Fig. 1a|||Geological Province: Mount Isa Superbasin.||||||
9156|Kamarga Volcanics|23958|5|Briefly described|p1133|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
9156|Kamarga Volcanics|23964|5|Briefly described|p1265|||Geological Province: Mount Isa Inlier.||||||
9156|Kamarga Volcanics|24308|5|Briefly described|p999, p987 Fig. 2|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
9156|Kamarga Volcanics|24309|6|Mentioned|p1012 Fig. 1|||||||||
9156|Kamarga Volcanics|24419|5|Briefly described|p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: Western Fold Belt, Lawn Hill Subprovince.||||||07-NOV-08
9156|Kamarga Volcanics|24432|6|Mentioned|p565 Fig.4|||||||||
9156|Kamarga Volcanics|36548|2|Defined|p513|Precambrian|Precambrian|||||||
9156|Kamarga Volcanics|37459|6|Mentioned|p427|||||||||
9156|Kamarga Volcanics|38237|6|Mentioned|Fig.3|||||||||
9156|Kamarga Volcanics|38291|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
9156|Kamarga Volcanics|38310|6|Mentioned|p237|||||||||
9156|Kamarga Volcanics|38348|4|Described|p4|||||||||
9156|Kamarga Volcanics|38584|6|Mentioned|p22|||||||||
9156|Kamarga Volcanics|39445|5|Briefly described|Table 2|||See also p35 and p40.||||||04-OCT-06
9156|Kamarga Volcanics|39497|6|Mentioned|Fig.4|||||||||
9156|Kamarga Volcanics|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
9156|Kamarga Volcanics|39925|6|Mentioned|p334|||||||||
9156|Kamarga Volcanics|39944|6|Mentioned|p229|||||||||
9156|Kamarga Volcanics|40840|6|Mentioned|Map legend|||||||||
9156|Kamarga Volcanics|41979|5|Briefly described|p518|||||||||
9156|Kamarga Volcanics|42565|5|Briefly described|Table 1 P6, P2|||||||||
9156|Kamarga Volcanics|45166|4|Described|p17|||||||||
9156|Kamarga Volcanics|49041|5|Briefly described|Table 1|||||||||
9156|Kamarga Volcanics|50536|6|Mentioned|p4.1|||Geological Province: Mount Isa Inlier.||||||
9156|Kamarga Volcanics|50550|5|Briefly described|p1146 Fig.9, p1152 Fig.13|||Geological Province: Western Fold Belt.||||||19-DEC-07
9156|Kamarga Volcanics|50624|5|Briefly described|p234 Fig.2||Paleoproterozoic|||||||07-NOV-08
9156|Kamarga Volcanics|60558|5|Briefly described|p5 Fig. 4, p9 Fig. 7|||Age: ~1740 - 1730Ma.||||||03-JUN-09
9156|Kamarga Volcanics|63109|6|Mentioned|p1112|||||||||
9156|Kamarga Volcanics|63866|5|Briefly described|p57||||||||Lower greenschist-facies basalts and feldspathic sandstones of unknown age.|
9156|Kamarga Volcanics|64250|6|Mentioned|p23|||||||||
9156|Kamarga Volcanics|64575|6|Mentioned|p656|||Correlated with Eastern Creek Volcanics.||||||
9156|Kamarga Volcanics|65337|6|Mentioned|p5. |||Leichhardt Superbasin; Lawn Hill Platform.||||||
9156|Kamarga Volcanics|65396|6|Mentioned|p196|||Kamarga Dome, NW Mount Isa Inlier.||||Correlated (possibly) with Eastern Creek Volcanics.||
9156|Kamarga Volcanics|67323|5|Briefly described|GIS attrib tbl, p10, p39, p107|Paleoproterozoic|Paleoproterozoic|See also Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Post-Barramundi basement to Century Domain, Mount Isa Inlier. Is directly overlain by the Isa Superbasin sequence.|Pre-1810 Ma.|||Intruded by Yeldham Granite.|Vesicular, amygdaloidal and massive basalt; flow top breccias common; interbeds of feldspathic and conglomeratic sandstone|
9156|Kamarga Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province.||||||
9156|Kamarga Volcanics|69591|5|Briefly described|p29-30, p32, p58|Paleoproterozoic|Paleoproterozoic|Century Domain, Mount Isa Province. Crops out in the Kamarga Dome, E of Century Mine. Subaerial, local fluvial environment.||||Is intruded by Yeldham Granite.|Vesicular, massive and amygdaloidal basalt; flow-top breccias common; interbeds of feldspathic and conglomeratic sandstone.|
9156|Kamarga Volcanics|72526|5|Briefly described|p6 Fig.1.2,|Paleoproterozoic|Paleoproterozoic|||||||
9156|Kamarga Volcanics|72889|6|Mentioned|p6 Fig.i.|||||||||
9156|Kamarga Volcanics|73413|6|Mentioned|p3|||Mount Isa Inlier, Western Fold Belt, Lawn Hill Platform.||||||
9312|Katherine River Group|9534|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Includes the McKay Sandstone and Kombolgie Formation.||||||
9312|Katherine River Group|9538|5|Briefly described|Map legend|Proterozoic|Proterozoic|Contains the Kombolgie Formation.  Age is Middle Proterozoic.||||||28-OCT-04
9312|Katherine River Group|9691|5|Briefly described|Map Legend|||||||||
9312|Katherine River Group|9701|5|Briefly described|Map Legend|Proterozoic|Proterozoic|||||||02-JUN-05
9312|Katherine River Group|9733|5|Briefly described|Map Legend|Carpentarian|Carpentarian|||||||
9312|Katherine River Group|22479|5|Briefly described|fig4, pg10|Statherian|Statherian|||||||
9312|Katherine River Group|22536|4|Described|p9|Proterozoic|Proterozoic|||||||
9312|Katherine River Group|22538|4|Described|P713, P715|Statherian|Statherian|||||||
9312|Katherine River Group|22574|5|Briefly described|map|Proterozoic|Proterozoic|||||||
9312|Katherine River Group|22600|6|Mentioned|Map legend|||||||||
9312|Katherine River Group|22748|6|Mentioned|p235 Fig.1|||||||||
9312|Katherine River Group|22808|6|Mentioned|7 fig 4|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
9312|Katherine River Group|23119|5|Briefly described|p433|||||||||
9312|Katherine River Group|23216|5|Briefly described|Fig3p5,19,39,50-1||Paleoproterozoic|||||||07-NOV-08
9312|Katherine River Group|23374|3|Fully described|Tb2p10,8,9,5,6,18,20,26,29,30,34,35||Statherian|Component units: Kombolgie Subgroup, Cottee Formation, Shadforth Sandstone, McCaw Formation, Gundi Sandstone. Of McArthur Basin.||||||04-OCT-06
9312|Katherine River Group|23384|5|Briefly described|p26|||||||||
9312|Katherine River Group|23395|5|Briefly described|p382|||||||||
9312|Katherine River Group|23396|5|Briefly described|p 407 fig.2|||||||||
9312|Katherine River Group|23714|4|Described|p36|Proterozoic|Proterozoic|See also page 7 Table 1. Geological Province: Rum Jungle Region. Max. thickness: 2000 m.||||||
9312|Katherine River Group|23733|5|Briefly described|p32 Fig. 19|||||||||
9312|Katherine River Group|23867|3|Fully described|p2|Paleoproterozoic|Paleoproterozoic|Geological Province: McArthur Basin.  See also Table 1 and Figs. 3 and 30.||||||07-NOV-08
9312|Katherine River Group|23937|5|Briefly described|p7, p25 Tb. 2|Statherian|Statherian|In the Calvert Superbasin.  Geological Province: McArthur Basin.||||||
9312|Katherine River Group|24047|5|Briefly described|p5 Fig.4|Paleoproterozoic|Paleoproterozoic|Age: 1815-1710Ma.  Geological Province: Pine Creek Orogen.  See also p6 Fig. 5 and p12 Fig.10.||||||07-NOV-08
9312|Katherine River Group|24048|6|Mentioned|p6|||||||||
9312|Katherine River Group|24049|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|In regional setting map legend.||||||07-NOV-08
9312|Katherine River Group|24050|3|Fully described|p12, p9 Tb. 2|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
9312|Katherine River Group|24051|5|Briefly described|Map Legend|Statherian|Statherian|Geological Province: McArthur Basin.||||||23-DEC-09
9312|Katherine River Group|24197|6|Mentioned|p103|||Geological Province: Pine Creek Inlier.||||||07-FEB-11
9312|Katherine River Group|29599|5|Briefly described|p30|||||||||
9312|Katherine River Group|30680|6|Mentioned|p309|||||||||
9312|Katherine River Group|30831|6|Mentioned|p4|||Also mention Fig.9.||||||
9312|Katherine River Group|31439|6|Mentioned|p293|||||||||
9312|Katherine River Group|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
9312|Katherine River Group|32660|4|Described|Table 4|||||||||
9312|Katherine River Group|33278|6|Mentioned|Fig.1|||||||||
9312|Katherine River Group|34287|6|Mentioned|p34|||||||||
9312|Katherine River Group|35114|6|Mentioned|p204|||||||||
9312|Katherine River Group|35465|6|Mentioned|Fig.1|||Geology of Pine Creek Geosyncline||||||
9312|Katherine River Group|35495|6|Mentioned|p340|||||||||
9312|Katherine River Group|36473|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
9312|Katherine River Group|36535|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
9312|Katherine River Group|36635|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
9312|Katherine River Group|37217|6|Mentioned|p650|||||||||
9312|Katherine River Group|37462|4|Described|Table4.IV|||||||||
9312|Katherine River Group|37565|6|Mentioned|Fig.5, P11|||||||||
9312|Katherine River Group|37568|6|Mentioned|p78|||||||||
9312|Katherine River Group|37579|5|Briefly described|Map legend|Carpentarian|Carpentarian|Includes the Kombolgie Formation.||||||10-OCT-05
9312|Katherine River Group|37815|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
9312|Katherine River Group|38042|6|Mentioned|p160|||||||||
9312|Katherine River Group|38349|4|Described|p16|||||||||
9312|Katherine River Group|38351|4|Described|p12|||See also Table 1.||||||04-OCT-06
9312|Katherine River Group|38884|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
9312|Katherine River Group|39210|6|Mentioned|p50|||||||||
9312|Katherine River Group|39357|4|Described|p15|||||||||
9312|Katherine River Group|39563|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
9312|Katherine River Group|39679|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
9312|Katherine River Group|39801|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Sandstone, minor limestone, siltstone and conglomerate. Interbedded intermediate to basic volcanics.||||||04-OCT-05
9312|Katherine River Group|40105|6|Mentioned|p321|||||||||
9312|Katherine River Group|40168|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Sandstone, minor limestone, siltstone and conglomerate. Interbedded intermediate to basic volcanics.||||||18-OCT-05
9312|Katherine River Group|40223|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Sandstone, minor limestone, siltstone, conglomerate. Interbedded intermediate to basic volcanics.||||||19-OCT-05
9312|Katherine River Group|40248|4|Described|p225|||||||||
9312|Katherine River Group|40823|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
9312|Katherine River Group|40957|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
9312|Katherine River Group|41019|6|Mentioned|p243|||||||||
9312|Katherine River Group|41125|6|Mentioned|p15|||See also Fig.6||||||
9312|Katherine River Group|41294|6|Mentioned|Map legend|Mesoproterozoic||||||||
9312|Katherine River Group|41295|4|Described|p15|||||||||
9312|Katherine River Group|41304|6|Mentioned|Map legend|Mesoproterozoic||||||||
9312|Katherine River Group|41305|6|Mentioned|Fig.4|||||||||
9312|Katherine River Group|41309|4|Described|p7|||||||||
9312|Katherine River Group|41311|4|Described|p22|||||||||
9312|Katherine River Group|41397|4|Described|p19|||||||||
9312|Katherine River Group|41406|6|Mentioned|Map legend|Mesoproterozoic||||||||
9312|Katherine River Group|41407|6|Mentioned|Map legend|Proterozoic||||||||
9312|Katherine River Group|41586|6|Mentioned|Map legend|Mesoproterozoic||||||||
9312|Katherine River Group|41878|6|Mentioned|p34|||||||||
9312|Katherine River Group|42014|5|Briefly described|Map legend|Mesoproterozoic||||||||
9312|Katherine River Group|42812|6|Mentioned|p10|||||||||
9312|Katherine River Group|43010|2|Defined|p92||Paleoproterozoic|Of Statherian age.||||||07-NOV-08
9312|Katherine River Group|43140|5|Briefly described|p4||Mesoproterozoic|||||||
9312|Katherine River Group|43149|5|Briefly described|Map Legend||Paleoproterozoic|of Statherian age.||||||07-NOV-08
9312|Katherine River Group|43187|5|Briefly described|p7|||||||||
9312|Katherine River Group|43292|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
9312|Katherine River Group|43595|6|Mentioned|p438|||||||||
9312|Katherine River Group|43624|6|Mentioned|Table 1, p9||Paleoproterozoic|||||||07-NOV-08
9312|Katherine River Group|43720|5|Briefly described|p4|Mesoproterozoic|Paleoproterozoic|Late Palaeoproterozoic - Mesoproterozoic||||||07-NOV-08
9312|Katherine River Group|43726|6|Mentioned|p2|||||||||
9312|Katherine River Group|43832|5|Briefly described|25-28,Table7 p27, 97||Paleoproterozoic|Upper constituent units not present in area. Known to belong to McArthur Basin. Underlain by Edith River Group.||||||07-NOV-08
9312|Katherine River Group|44112|5|Briefly described|p1,11,43|Statherian|Orosirian|Poorly constrained Max Age: ~1840 Ma. Part of Supersequence 1(B); Mid-upper units 1(C); upper units 1(D)||||||
9312|Katherine River Group|44201|14|Not recorded|p.7|||||||||
9312|Katherine River Group|44299|6|Mentioned|p.11|||SD/53-7,8.||||||
9312|Katherine River Group|44338|14|Not recorded|opp.p.6|||(C53-14).||||||
9312|Katherine River Group|44339|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
9312|Katherine River Group|44399|5|Briefly described|map legend||Neoproterozoic|Includes the Diljin and Kombolgie Formations and the Edith River Volcanics.||||||04-OCT-06
9312|Katherine River Group|44400|2|Defined|p.4,6-8,11,Tb.1||Paleoproterozoic|Contains West Branch Volcanics, Gundi Greywacke, McCaw Formation, Shadforth Sandstone, Cottee Formation, McKay Sandstone, Kombolgie Formation, Nungbalgarri Volcanic Member. L.Prot. Mt.Marumba Sheet (D53-6), opp.p.6, map.||||||06-NOV-20
9312|Katherine River Group|44401|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
9312|Katherine River Group|44471|14|Not recorded|p.7,9,13,opp.7, map|||(D53-10).||||||
9312|Katherine River Group|44472|5|Briefly described|map legend||Paleoproterozoic|Includes the Diamond Creek Formation, Gundi Greywacke and the West Branch Volcanics.||||||07-NOV-08
9312|Katherine River Group|45022|3|Fully described|p.55||Carpentarian|On many pages.||||||
9312|Katherine River Group|45064|5|Briefly described|p14|||||||||
9312|Katherine River Group|46163|2|Defined|p168-171||Mesoproterozoic|||||||14-MAY-18
9312|Katherine River Group|46639|5|Briefly described|Map legend||Paleoproterozoic|Includes the Kombolgie Formation.||||||07-NOV-08
9312|Katherine River Group|46658|6|Mentioned|Fig.5 P548|||||||||
9312|Katherine River Group|46675|5|Briefly described|Map legend for regional setting...|Mesoproterozoic|Mesoproterozoic|Sandstone, minor limestone, siltstone and conglomerate; interbedded intermediate to basic volcanics.   Geological Province: Pine Creek Geosyncline.||||||
9312|Katherine River Group|46676|14|Not recorded|p.6||Neoproterozoic|U.Proterozoic; includes Kombolgie Formation.||||||
9312|Katherine River Group|46678|5|Briefly described|Table 1|Proterozoic|Proterozoic|Contains the Diljin Hill and Kombolgie Formations, and Edith River Volcanics.  Max. thickness:  9,000 feet.||||||
9312|Katherine River Group|46679|14|Not recorded|map legend||Neoproterozoic|Upper Proterozoic.||||||
9312|Katherine River Group|46700|5|Briefly described|P29, Table1 P8||Carpentarian|||||||
9312|Katherine River Group|46861|6|Mentioned|p5|||||||||
9312|Katherine River Group|47049|6|Mentioned|p237|||||||||
9312|Katherine River Group|48867|14|Not recorded|p.1-20||Mesoproterozoic|map. M.Proterozoic.||||||
9312|Katherine River Group|50225|5|Briefly described|p406 Fig. 10, p407|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine CreekMcArthur Basin.||||||07-FEB-11
9312|Katherine River Group|50545|5|Briefly described|p115||Paleoproterozoic|Overlain by Roper Group. Thickness:~1980 m.||||||07-NOV-08
9312|Katherine River Group|50586|6|Mentioned|p1.1, 2.1|||||||||
9312|Katherine River Group|50623|5|Briefly described|p260 Fig.3, p261|Statherian|Statherian|Correlated with Depot Creek Sandstone.||||||07-DEC-04
9312|Katherine River Group|60483|6|Mentioned|p8, p27|||Geological Province: northern McArthur Basin. Contiguous with Tawallah Group in southern part of basin. Contains thin basalt sections in lower part of unit.||||||
9312|Katherine River Group|60526|5|Briefly described|Map Legend|Carpentarian|Carpentarian|Sandstone; minor limestone, siltstone and conglomerate. Interbedded intermediate to basic volcanics.||||||
9312|Katherine River Group|60550|5|Briefly described|Map Legend|Carpentarian|Carpentarian|||||||
9312|Katherine River Group|60571|5|Briefly described|Map legend|Statherian|Statherian|Geological Province: McArthur Basin.||||||19-NOV-04
9312|Katherine River Group|60573|5|Briefly described|Map legend|Orosirian|Orosirian|Includes the West Branch Volcanics, Gundi Sandstone, Diamond Creek Volcanics and McCaw Formation.  Do not outcrop in the Roper River mapsheet area.||||||14-FEB-05
9312|Katherine River Group|60574|5|Briefly described|Map Legend|||Geological Province: McArthur Basin.||||||
9312|Katherine River Group|60680|5|Briefly described|Map legend|Statherian|Statherian|Includes the Kombolgie Subgroup.  Geological Province: McArthur Basin.||||||13-JAN-05
9312|Katherine River Group|61206|5|Briefly described|p516-517|||Forms spectacular cliffs bordering Kakadu National Park to the east.|||Includes Kombolgie subgroup.|Includes the Kombolgie subgroup.||
9312|Katherine River Group|61390|5|Briefly described|Map Legend|Statherian|Statherian|||||||
9312|Katherine River Group|61403|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|In regional setting map legend.||||||07-NOV-08
9312|Katherine River Group|61572|5|Briefly described|p666|||Rocks deformed by the Gulpuliyul impact structure. Geological Province: McArthur Basin. See also p671 Tb. 1||||||
9312|Katherine River Group|61861|6|Mentioned|Fig.2.|||Pine Creek.||||Unconformably overlies Edith River Group.||
9312|Katherine River Group|62375|5|Briefly described|p8 Table 1, 9 table 2, 10 Fig. 3|Neoproterozoic|Paleoproterozoic|Sandstone, conglomerate, minor greywacke, siltsotne, interbedded volcanics and pyroclastics. Age: 1780-1700Ma. Thickness: 3000-4500m. Geological Province: Pine Creek Orogen.||||||09-FEB-10
9312|Katherine River Group|63866|5|Briefly described|p107, p112-p114, p123|||A maximum depositional age range of 1860-1810 Ma (Page, OZCHRON) is derived from the Kombolgie Subgroup. The lower part of this group is equivalent to the Dhunganda Formation of the Donydji Group. Intruded by the Jimbu Microgranite and Oenpelli Dolerite.  |||Includes the basal Kombolgie Subgroup and West Branch Volcanics.|Unconformably overlain by the Mount Rigg Group. Equivalent to the Tolmer Group, Donydji Group, Spencer Creek Group, Tawallah Group and the Groote Eylandt Group.||
9312|Katherine River Group|64677|5|Briefly described|p4, p6|||Overlies Pine Creek Orogen basement.|>1720 Ma.|||Overlies Nabarlek Granite nonconformably.||
9312|Katherine River Group|64698|5|Briefly described|lithinterp table|Statherian|Orosirian|McArthur Basin. Incl. Shadforth Sandstone, Nungbalgarri Volcanics, McKay Sandstone, McCaw Formation, Marlgowa Sandstone, Mamadewerre Sandstone, Gundi Sandstone, Gumarrirnbang Sandstone, Diamond Creek Volcanics, Cottee Formation, Bonanza Creek Formation.||||||07-JAN-09
9312|Katherine River Group|64722|5|Briefly described|p22||Paleoproterozoic|Of Pine Creek region of North Australian Craton.|||Includes Kombolgie Subgroup at its base.|Overlies Edith River and El Sherana Groups.||11-APR-12
9312|Katherine River Group|64724|5|Briefly described|p45 Fig.5, p46|Statherian|Statherian|Lower part of this group of the Leichhardt Superbasin, deposited during the Leichhardt Extension (1800-1750 Ma). Upper part during Calvert Extension (1730-1690), Pine Creek Inlier.||||||
9312|Katherine River Group|64725|6|Mentioned|p61.|Mesoproterozoic|Paleoproterozoic|McArthur Basin. Subhorizontal platform clastic rocks.||||||
9312|Katherine River Group|64730|6|Mentioned|p126-7|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. Unconformably overlies Nimbuwah Domain, possible correlate of Tolmer Group in the Litchfield Province (Needham et al. 1988).||||||03-MAY-12
9312|Katherine River Group|64816|6|Mentioned|p2 Fig.1 |||||||||
9312|Katherine River Group|64817|6|Mentioned|p352 Fig.3, p353 Fig.4, p354 |||Arnhem Shelf, McArthur Basin.|||Includes West Branch and Diamond Creek Volcanics; Gundi and Shadforth Sandstones; Jimbu Microgranite; McCaw, Bonanza Creek and Cottee Formations and Kombolgie Subgroup.|||
9312|Katherine River Group|64956|6|Mentioned|p77, p93|||Overlies Nanambu Complex; unconformably overlies Nourlangie Schist.||||||07-FEB-11
9312|Katherine River Group|65228|6|Mentioned|p7|||McArthur Basin.|||Includes McCaw Formation.|||
9312|Katherine River Group|65232|5|Briefly described|p7-8, p6 Fig. 5, p24, p5 Fig. 4|Palaeoproterozoic|Palaeoproterozoic|Incl: Kombolgie Subgroup, Mackay Ss, Cottee Fm, Shadforth Sst, Bonanza Creek Fm, McCaw Fm, Gundi Ss, West Branch Volcanics. Unconf: over Edith River Group; under Mount Rigg Group. Sandstone, conglom., mafic volcanics. Geol. Prov: eastern Pine Creek Orogen||||||09-FEB-10
9312|Katherine River Group|65339|6|Mentioned|p4.|||Unconformably overlies Pine Creek Orogen rocks.||||||
9312|Katherine River Group|65340|6|Mentioned|p74.|||Central Arnhem Land. Radial deformation of this unit has been attributed to gravity sliding following uplift caused by the intrusion of Jimbu Microgranite. A similar explanation is offered for deformation of Gold Creek Volcanics and Pungalina Member around the Packsaddle Microgranite. Contemporaneous with Tawallah, Donydji and Spencer Creek Groups.||||||
9312|Katherine River Group|67057|5|Briefly described|p454. |Paleoproterozoic|Paleoproterozoic||1822 +/- 5  to 1720 +/- 7 Ma (Sweet et al. 1999a).||Includes Kombolgie Subgroup.|Overlies Plum Tree Creek Volcanics. Is intruded by Jimbu Microgranite and Oenpelli Dolerite.||
9312|Katherine River Group|67355|6|Mentioned|p6, p7 Tb.2, p14|||The El Sherana and Edith River Groups were previously part of this Group.|||Kombolgie Subgroup.|Upper part correlated with the Tolmer Group.||25-JAN-17
9312|Katherine River Group|67564|3|Fully described|p6 Table 2, p9 Fig.4, pp38-50, p86.|Paleoproterozoic|Paleoproterozoic|McArthur Basin. Largely undeformed, dipping gently (2 - 5 degrees) to E and SE;  mixed sedimentary-mafic volcanic succession, some 2600 m thick. Correlative of Tolmer Group to the west.|1825 - 1705 Ma.||Includes Kombolgie Subgroup; Cottee, Bonanza Creek and McCaw Formations; Shadforth and Gundi Sandstones.|Overlies David Suite. Is intruded by Oenpelli Dolerite.|Dominantly quartz arenite; mudstone, glauconitic sandstone, minor stromatolitic dolostone and rare basalt and dolerite sills in upper parts.|
9312|Katherine River Group|67779|5|Briefly described|p4, p7, pp31-38.|Mesoproterozoic|Paleoproterozoic|Originally defined by Walpole et al. (1968); revised by Plumb and Roberts (1992). Basal group of the McArthur Basin sequence on the Arnhem Plateau. Up to 5000 m of platform sediments and volcanic rocks deposited in braided rivers.|||Includes Kombolgie Subgroup.||Relatively undeformed conglomerate, sandstone, siltstone, dolostone and volcanic units.|
9312|Katherine River Group|69018|6|Mentioned|p450 Fig.1a|||Of McArthur Basin.||||||
9312|Katherine River Group|69417|6|Mentioned|p2:5|Statherian|Statherian|McArthur Basin.||||||12-JUL-16
9312|Katherine River Group|69420|5|Briefly described|p5:6, 26, 39, 52, 62, 64, 67, 78-79, 84|Paleoproterozoic|Paleoproterozoic|Nimbuwah Domain, Pine Creek Orogen. Has no auriferous veins. Associated with numerous U deposits.|||Kombolgie Subgroup, Marlgowa, Gumarrirnbang, Mamadawerre Sandstones.|||12-JUL-16
9312|Katherine River Group|69430|4|Described|p15:2-4, 6-9, 30|||Walpole (1958) originally recognised two Formations: Edith River Volcanics and Kombolgie Formation; the former has since been raised to Group status in the underlying Pine Creek Orogen succession. Ruker (1959) and Randal (1963) subdivided the Katherine River Group into several units, which were revised by Walpole et al. (1968). Carson et al (1999) identified three sandstone Formations and volcanic Members within the Kombolgie Formation, which they upgraded to Subgroup rank. NW McArthur Basin.|>1710 Ma.||Kombolgie Subgroup; Cottee, Bonanza Creek, McCaw, Formations; Shadforth, Gundi Sandstones; Diamond Creek, West Branch Volcanics; Jimbu Microgranite.|Equivalent to Tawallah (and probably contiguous with it) and Donydji Groups. Is intruded by Jimbu Microgranite (up to and including Gundi Sandstone).|Sandstone with volcanic intervals in the lower part; sandstone, minor dolostone and mudstone in the upper.|12-JUL-16
9312|Katherine River Group|69432|6|Mentioned|p17:5|||McArthur Basin. A likely correlative of Tolmer Group (Birrindudu Basin).||||||12-JUL-16
9312|Katherine River Group|69455|6|Mentioned|p39:1|Proterozoic|Proterozoic|These rocks form the SW part of the Arnhem Land Plateau.||||||12-JUL-16
9312|Katherine River Group|69673|6|Mentioned|p3 fig 2, p15, p17, p49|Statherian|Statherian|Northwestern McArthur Basin.|1710 Ma||Includes West Branch Volcanics, Gundi Sandstone, Jimbu Microgranite, Diamond Creek Volcanics, McCaw Formation, Bonanza Creek Formation, Shadforth Sandstone, Cottee Formation, Kombolgie Subgroup|||
9312|Katherine River Group|70853|5|Briefly described|Map legend.|Statherian|Statherian||||Kombolgie Subgroup.|||
9312|Katherine River Group|70866|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|McArthur Basin.|||Includes Kombolgie Subgroup.|Overlies Geolsec Formation. Is overlain unconformably by Uniya Formation.||01-MAR-18
9312|Katherine River Group|70968|6|Mentioned|p2 Fig.3|||||||||
9312|Katherine River Group|71059|6|Mentioned|p2|Paleoproterozoic|Paleoproterozoic|McArthur Basin.||||||
9312|Katherine River Group|71374|6|Mentioned|p2|||northern McArthur Basin.||||Broadly equivalent to the Tawalah Group.||
9312|Katherine River Group|71592|5|Briefly described|Appendix A.|||McArthur Basin.|||||Andesite.|
9312|Katherine River Group|71606|5|Briefly described|p135,137-138|Statherian|Statherian|West Arnhem Shelf, McArthur Basin. Arenite-bimodal volcanic-lutite-carbonate sequence.|||Includes West Branch Volcanics.|Underlain unconformably by Pine Creek Granites and Edith River Group. Correlable to Tawallah Group.||
9312|Katherine River Group|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin. Informally divided in to lower and upper parts.||||||06-MAR-20
9312|Katherine River Group|72373|5|Briefly described|p2|Paleoproterozoic|Paleoproterozoic|Broadly equivalent to Redbank package, Tawallah Group (central/southern McArthur Basin), Birrindudu and Tolmer groups (Birrindudu Basin) and Tomkinson Creek and Hatches Creek groups (Tomkinson Province).||||||
9312|Katherine River Group|72377|5|Briefly described|p12|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin.|||Includes West Branch Volcanics.|||
9312|Katherine River Group|72718|6|Mentioned|p5 Tb.1|||McArthur Basin. Calvert/Leichhardt Superbasin of Jackson et al. (1999, 2000). Redbank package.||||||
9325|Katipiri Formation|23054|6|Mentioned|p30|||||||||
9325|Katipiri Formation|24175|5|Briefly described|p43|Quaternary|Quaternary|Overlies both Kutjitara and Tirari Formations.||||||
9325|Katipiri Formation|24321|5|Briefly described|Map legend|Pleistocene|Pleistocene|||||||
9325|Katipiri Formation|29673|6|Mentioned|p330|||||||||
9325|Katipiri Formation|31699|6|Mentioned|p132|||Pleistocene. Preferable name to Katipiri Sands (re lithology)||||||
9325|Katipiri Formation|42124|6|Mentioned|p43|||||||||
9325|Katipiri Formation|42375|4|Described|p50-55|||Originally named Katipiri Sand. Amended herein. Lake Eyre Basin. Variation of Katipiri Formation,SA.||||||
9325|Katipiri Formation|42543|6|Mentioned|p4|||||||||
9325|Katipiri Formation|42746|5|Briefly described|Fig.9 P14|||Synonym for Katipiri Sand? See also p22.||||||01-SEP-20
9325|Katipiri Formation|42784|6|Mentioned|p487|||||||||
9325|Katipiri Formation|42883|6|Mentioned|p6|||||||||
9325|Katipiri Formation|43041|5|Briefly described|p589|||||||||
9325|Katipiri Formation|43042|5|Briefly described|p596|||||||||
9325|Katipiri Formation|44133|5|Briefly described|p245, 244 Table 11.3|Late Pleistocene|Middle Pleistocene|Maximum Thickness: 5m. ||||||
9325|Katipiri Formation|61119|5|Briefly described|p124, p128, p131, p137, p144, pp146-147||Pleistocene|Youngest unit discussed in this paper. Meandering river and, possibly saline, lake deposits. Detailed descriptions of Lungfish fossil assemblages included.||||||28-MAR-12
9325|Katipiri Formation|61155|5|Briefly described|p17|Pleistocene|Pleistocene|Overlies the Kutjitara Formation; underlies the Kootaburra [Kootaberra]  Formation. Age: <1.5Ma. Geological Province: Lake Eyre Basin.||||||01-SEP-20
9325|Katipiri Formation|66131|5|Briefly described|p240, p243, p244 Fig.4, p246-247|Pleistocene|Pleistocene|Paleochannels underlying dunefields and cut into Tirari and Kutjitara Formations.||||Overlies Kutjitara Formation. Disconformably overlies Etadunna Formation. Correlative unit of the Eurinilla Formation.|Fluviolacustrine sediments and recessional shoreline dunes.|
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.|
9375|Keepera Group|9394|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Georgina Basin. Includes: Oorabra Arkose.||||||
9375|Keepera Group|9694|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Includes: Oorabra Arkose. Geological Province: Georgina Basin.||||||
9375|Keepera Group|22762|6|Mentioned|p362|||Geological Province - Georgina Basin.||||||
9375|Keepera Group|37462|4|Described|Table 4.IX|||||||||
9375|Keepera Group|37928|6|Mentioned|Fig.5|||||||||
9375|Keepera Group|37929|5|Briefly described|p526|||||||||
9375|Keepera Group|38157|6|Mentioned|Table IX|||||||||
9375|Keepera Group|39445|6|Mentioned|p56|||||||||
9375|Keepera Group|40538|6|Mentioned|Map legend|Adelaidean|Adelaidean|Geological Province: Georgina Basin.||||||15-NOV-05
9375|Keepera Group|40906|4|Described|p18|||||||||
9375|Keepera Group|42504|5|Briefly described|Table 4 P73|||||||||
9375|Keepera Group|43595|5|Briefly described|p548,Fig.5-33,549||Adelaidean|||||||
9375|Keepera Group|45155|6|Mentioned|Fig.7|||||||||
9375|Keepera Group|48990|2|Defined|p17|Adelaidean|Adelaidean|||||||
9375|Keepera Group|60122|5|Briefly described|p5, p11|Neoproterozoic|Neoproterozoic|Includes the Black Stump Arkose and Wonnadinna Dolostone.  Gological Province: Georgina Basin.||||||17-MAY-05
9375|Keepera Group|60551|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Includes: Oorabra Arkose. Geological province: Georgina Basin.||||||
9375|Keepera Group|60590|5|Briefly described|Map legend|Cryogenian|Cryogenian|Includes Black Stump Arkose and Wonnadinna Dolostone.||||||
9375|Keepera Group|61404|5|Briefly described|Map legend|Cryogenian|Cryogenian|Includes: Boko Formation, Ooraba Arkose, Wonnadinna Dolostone, and Black Stump Arkose.  Geological Province: southern Georgina Basin.||||||13-OCT-05
9375|Keepera Group|62642|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Georgina/Ngalia Basin.||||||
9375|Keepera Group|64068|3|Fully described|p223-224 App 1, pp45-48, p7, 35, p viii|Ediacaran|Cryogenian|Intended as redefinition. Disconformably overlies Aroota Group after c.650 Ma uplift.|||Now includes Sun Hill, Black Stump and Oorabra Arkoses, Little Burke Tillite, Boko Formation (correlated with Marinoan glaciation) and Wonnadinna Dolostone.|Disconformably overlies Aroota Group.||04-APR-12
9375|Keepera Group|65338|6|Mentioned|pp60-63.|||Named by Walter (1980); redefined by Kruse in Dunster et al. (2007). |||Includes Black Stump, Oorabra and Sun Hill Arkoses, Wonnadinna Dolostone, Little Burke Tillite and Boko Formation.|||
9375|Keepera Group|65341|6|Mentioned|p4, pp12-15. |Cryogenian|Cryogenian||||Includes Boko Formation and Oorabra Arkose.|||
9375|Keepera Group|66767|5|Briefly described|p58|Neoproterozoic|Neoproterozoic|Georgina Basin. Over 450m thick. Glacial units are tentatively attributed to the Marinoan glaciation.|||||Glacial sedimentary rocks and intertidal to deeper marine dolostone.|
9375|Keepera Group|67164|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Georgina/Ngalia Basins.|||Includes Boko Formation.|||
9375|Keepera Group|67870|6|Mentioned|p43|Neoproterozoic|Neoproterozoic|Georgina Basin.||||||
9375|Keepera Group|67892|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic||||Includes Boko Formation.|||
9375|Keepera Group|69437|5|Briefly described|p22:7|||Southern Georgina Basin. Centralian A Superbasin. Supersequence 3.|||Black Stump, Sun Hill, Oorabra Arkoses; Boko Formation; Little Burke Tillite.|Is overlain by Wonnadinna Dolostone.|Glacial outwash deposits.|12-JUL-16
9375|Keepera Group|69443|5|Briefly described|p28:2-3, 7-10, 31|Ediacaran|Cryogenian|Walter (1980); redefined by Kruse in Dunster et al. (2007). Southern Georgina Basin. Deposition followed uplift associated with the Rinkabeena Movement. Glacigene and post-glacial deposits. Equivalent to Olympic Formation, Pioneer Sandstone, middle to upper Inindia beds, Boord Formation and Mount Doreen Formation.|||Boko Formation; Oorabra, Black Stump, Sun Hill Arkoses; Little Burke Tillite; Wonnadinna Dolostone.|Disconformably overlies Aroota Group; overlain unconformably or disconformably by Shadow Group.||12-JUL-16
9375|Keepera Group|69673|6|Mentioned|p111, p114 fig 92, p115|Neoproterozoic|Neoproterozoic||||Includes Black Stump Arkose, Oorabra Arkose, Boko Formation, Wonnadinna Dolostone|||
9375|Keepera Group|72515|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Jervois Range Special Map Sheet. Georgina Basin.|||Includes the Oorabra Arkose.|Disconformably overlain by the Mopunga Group. Disconformably overlies the Aroota Group.||20-APR-22
9375|Keepera Group|72516|5|Briefly described|p13, p21, p85-87, p135, p171, p176|Ediacaran|Ediacaran|Georgina Basin.|||Includes the Oorabra Arkose.|Disconformably overlain by the Mopunga Group.||20-APR-22
9375|Keepera Group|72711|6|Mentioned|p3 Fig.2.|||Shown only on p3 Fig.2. From the interpretive geology map of the Jervois Range Special (modified from Weisheit et al 2019). Shown as part of the Georgina Basin.||||||
9394|Kelly Creek Formation|8187|5|Briefly described|Map legend|Ordovician|Ordovician|Sandstone, siltstone.||||||
9394|Kelly Creek Formation|10116|5|Briefly described|Map Legend|Early Ordovician|Early Ordovician|Quartzose sandstone and dolomite.||||||
9394|Kelly Creek Formation|12891|5|Briefly described|p733 Fig. 2|Middle Ordovician|Middle Ordovocian|Geological province: SW Georgina Basin.||||||07-FEB-11
9394|Kelly Creek Formation|12951|5|Briefly described|p143 fig 4, p145 fig 6, p151|Early Ordovician|Early Ordovician|Georgina Basin.||||||
9394|Kelly Creek Formation|13995|6|Mentioned|p99|||Georgina Basin.||||||
9394|Kelly Creek Formation|22646|6|Mentioned|Fig 5 on p 105|Early Ordovician|Early Ordovician|Georgina Basin.||||||
9394|Kelly Creek Formation|22954|6|Mentioned|Fig3p9|Early Ordovician|Early Ordovician|||||||
9394|Kelly Creek Formation|24065|4|Described|p235|Early Ordovician|Late Cambrian|Geological Province: Georgina Basin.  Maximum thickness: ~170m.||||||
9394|Kelly Creek Formation|24442|5|Briefly described|p49|Early Cambrian|Early Cambrian|Overlain by Coolibah Formation.  On TOBERMORY sheet.||||||
9394|Kelly Creek Formation|30914|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
9394|Kelly Creek Formation|30983|6|Mentioned|p70|||||||||
9394|Kelly Creek Formation|31572|6|Mentioned|p21|||Correlation chart||||||
9394|Kelly Creek Formation|33111|4|Described|p37|||Mention Fig.9||||||
9394|Kelly Creek Formation|33738|6|Mentioned|p49|||||||||
9394|Kelly Creek Formation|34454|5|Briefly described|Table 2|||p16.||||||04-OCT-06
9394|Kelly Creek Formation|34847|6|Mentioned|Table 1|||Stratigraphy and hydrocarbon prospects.||||||04-OCT-06
9394|Kelly Creek Formation|35121|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
9394|Kelly Creek Formation|35139|4|Described|Table.2|||||||||
9394|Kelly Creek Formation|36234|3|Fully described|p170|||||||||
9394|Kelly Creek Formation|36243|6|Mentioned|Table 1A|||||||||
9394|Kelly Creek Formation|36473|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian to Ordovician||||||
9394|Kelly Creek Formation|36580|6|Mentioned|Fig.3|||||||||
9394|Kelly Creek Formation|37572|4|Described|p162|||See also Fig.8||||||
9394|Kelly Creek Formation|38532|4|Described|Fig.1|||||||||
9394|Kelly Creek Formation|38832|6|Mentioned|p157|||||||||
9394|Kelly Creek Formation|39445|5|Briefly described|Table 4|||Disconformity within. See also p64 and Fig.5.||||||04-OCT-06
9394|Kelly Creek Formation|39921|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
9394|Kelly Creek Formation|39943|6|Mentioned|Table 2B|||||||||
9394|Kelly Creek Formation|40136|5|Briefly described|p29|||||||||
9394|Kelly Creek Formation|40906|6|Mentioned|Fig.11|||||||||
9394|Kelly Creek Formation|41524|6|Mentioned|Fig.3|||||||||
9394|Kelly Creek Formation|42059|6|Mentioned|Fig.2 P131|||||||||
9394|Kelly Creek Formation|42060|6|Mentioned|Fig.5 P140|||||||||
9394|Kelly Creek Formation|42643|6|Mentioned|p32|||||||||
9394|Kelly Creek Formation|43105|5|Briefly described|Fig.4,p9.|||||||||
9394|Kelly Creek Formation|43803|6|Mentioned|Fig.5,p71|||||||||
9394|Kelly Creek Formation|43808|5|Briefly described|p294|||||||||
9394|Kelly Creek Formation|44233|14|Not recorded|Fig.1||Early Ordovician|||||||
9394|Kelly Creek Formation|44308|14|Not recorded|p10,11,Tb.1||Early Ordovician|||||||
9394|Kelly Creek Formation|44309|2|Defined|Tb.1,p11,12,17,map||Ordovician|||||||
9394|Kelly Creek Formation|44312|14|Not recorded|Map Legend||Early Ordovician|||||||
9394|Kelly Creek Formation|44326|14|Not recorded|Map Legend||Early Ordovician|||||||
9394|Kelly Creek Formation|44358|5|Briefly described|p10,19|||similar lithologically and stratigraphically to Swift Formation.||||||
9394|Kelly Creek Formation|44469|2|Defined|p.9,19,Tb.I|||(F53-12). See also p.13-16,Tb.II. Conformably overlies Ninmaroo Fm.;Overlain by Coolibah Fm. Laterally equiv.to lower part of Tomahawk Beds. Similar lithology to Swift Fm.Fossils Good aquifer.||||||04-OCT-06
9394|Kelly Creek Formation|44470|5|Briefly described|map legend|||Upper Proterozoic to Lower Cambrian.||||||02-DEC-04
9394|Kelly Creek Formation|44848|14|Not recorded|p111|||||||||
9394|Kelly Creek Formation|44852|14|Not recorded|p71||Early Ordovician|||||||
9394|Kelly Creek Formation|44920|14|Not recorded|Map Legend,Sheet 4||Early Ordovician|||||||
9394|Kelly Creek Formation|45052|2|Defined|p124|Early Ordovician|Early Ordovician|See also p37.||||||04-OCT-06
9394|Kelly Creek Formation|45155|6|Mentioned|Fig.8|||||||||
9394|Kelly Creek Formation|46887|6|Mentioned|p251|||||||||
9394|Kelly Creek Formation|46897|6|Mentioned|Fig.3|||||||||
9394|Kelly Creek Formation|46956|6|Mentioned|p160|||||||||
9394|Kelly Creek Formation|46958|6|Mentioned|p195|||See also Fig.2.||||||
9394|Kelly Creek Formation|46959|6|Mentioned|p213|||||||||
9394|Kelly Creek Formation|47024|6|Mentioned|p2|||||||||
9394|Kelly Creek Formation|48901|14|Not recorded|Not recorded|Early Ordovician|Late Cambrian|U.Camb-L.Ord.||||||
9394|Kelly Creek Formation|49027|4|Described|p16|||||||||
9394|Kelly Creek Formation|60122|3|Fully described|p27, p4, p10 Tb. 1, p28 Fig. 33|Early Ordovician|Early Ordovician|Conformable on Tomahawk and Ninmaroo Fms; disconformable on Ninmaroo Fm and Georgina Lst; unconformable beneath Nora Fm, conformable below Coolibah Fm; also unconformably overlain by Austral Downs Lst. . Max. thickness: 290m. Geol. Prov: Georgina Basin.||||||17-MAY-05
9394|Kelly Creek Formation|60590|5|Briefly described|Map legend|Early Ordovician|Early Ordovician|Quartzose and dolomitic quartz sandstone, siltstone, dolostone, partially dolomitised limestone, minor conglomerate.  Overlies the Arrinthrunga and Ninmaroo Formations.||||||
9394|Kelly Creek Formation|61404|5|Briefly described|Map legend|Early Ordovician|Early Ordovician|Of the Toko Group. Quartzose and dolomitic quartz sandstone, siltstone, dolostone, partially dolomitised limestone, minor conglomerate. Geological Province: southern Georgina Basin.||||||12-OCT-05
9394|Kelly Creek Formation|63450|5|Briefly described|p76, p78 Fig. 5|Arenig|Arenig|Overlies Ninmaroo Formation; overlain by conformably by Coolibah Formation. Max. thickness: 290m. Geological province: Georgina Basin, West Toko Syncline. Lower section predominantly sandstone; upper part is dolostone and dolomitised limestone.||||||07-FEB-11
9394|Kelly Creek Formation|63562|6|Mentioned|p338 fig 3, p352 Fig.10|Early Ordovician|Early Ordovician|Of Georgina Basin.||||Overlies Tomahawk Formation. Is overlain by Nora Formation.||
9394|Kelly Creek Formation|64068|3|Fully described|p75-76, p71,73,78, 82, 226|Early Ordovician|Late Cambrian|Established by Casey in Smith (1965).Parts formerly included in Dulcie Sandstone (Joklik 1955), Ninmaroo Formation (Prichard 1960), Tomahawk Formation (Smith 1964), Tarlton Formation (Smith 1965).||Of Toko Group.||Conformably overlies Tomahawk Formation and conformably to disconformably overlies Ninmaroo Formation. Conformably overlain by Coolibah Formation or Nora Formation.|Sandstones, dolostone, siltstone, minor conglomerate and coquinite; overlain by dolostone, sandstone, dolomudstone, dolomitic limestone, minor conglomerate. Contains surficial manganocrete.|04-APR-12
9394|Kelly Creek Formation|64778|6|Mentioned|p13|Ordovician|Ordovician|Dulcie Syncline, Southern Georgina Basin.||||||
9394|Kelly Creek Formation|64812|5|Briefly described|p237 Fig. 2|Middle Ordovician|Middle Ordovician|Geological Province: southern Georgina Basin.||||||07-FEB-11
9394|Kelly Creek Formation|64813|5|Briefly described|p256 Fig. 3|Middle Ordovician|Middle Ordovician|Geological Province: southern Georgina Basin.||||||11-FEB-09
9394|Kelly Creek Formation|65237|5|Briefly described|p4 Fig. 7, p10|Ordovician||Conformably overlies Tomahawk beds; disconformably overlain by Dulcie Sandstone. Geological province: southern Georgina Basin/Dulcie Syncline. Comprises fresh water/aeolian clastic rocks.||||||07-FEB-11
9394|Kelly Creek Formation|65341|6|Mentioned|p2 Fig.2. |Ordovician|Ordovician|||||||
9394|Kelly Creek Formation|65342|5|Briefly described|p6.|||Georgina Basin. |||||Quartzose and glauconitic sandstone; minor dolostone, mudstone, and conglomerate; upper part dominantly limestone with lesser interbedded sandstone, marl at top.|
9394|Kelly Creek Formation|65489|5|Briefly described|p125-128|Ordovician|Early Ordovician|Georgina Basin. A thick and relatively homogeneous dolostone reservoir exists in this unit. Hosts the Ethabuka 1 gas discovery.||||Overlies Ninmaroo Formation. Is overlain by Coolibah Formation.||
9394|Kelly Creek Formation|66767|5|Briefly described|p59|Ordovician|Ordovician|Southern Georgina Basin.||Toko Group.|||Dolomitic quartz sandstone and dolostone.|
9394|Kelly Creek Formation|67323|5|Briefly described|p81, p83, p88, p90, p92 Fig.12.2|Early Ordovician|Early Ordovician|See also GIS attrib tbl, Solid Geology Map. Toko Syncline, Georgina Basin. Age: Ordovician? A petroleum target in the underexplored Georgina Basin. An aquifer supplying water bores.||Toko Group.||Overlies Ninmaroo Formation. Is overlain by Nora Formation unconformably and Coolibah Formation conformably.|Sandstone, dolomite, siltstone, coquinite|
9394|Kelly Creek Formation|67402|6|Mentioned|p25, p25 tbl RRM3|Chewtonian|Bendigonian|Georgina Basin, West Toko Syncline. Maximum thickness of 290m. Potential reservoir for carbon dioxide storage. Sealed by the Nora Formation. See also p165 tbl LPB1, p213 fig GRG3, p214, p215, p217.  ||||Overlies the Ninmaroo Formation. Overlain by the Coolibah or Nora Formations.|Predominantly sandstone overlain by dolostone and dolomitised limestone.|
9394|Kelly Creek Formation|68553|6|Mentioned|Map legend; schematic diagram.|Ordovician|Ordovician|Georgina Basin. This unit, as well as the Toko Group and Coolibah Formation, are all mapped under the symbol, Ot.||||||
9394|Kelly Creek Formation|69437|5|Briefly described|p22:10, 15|Ordovician|Ordovician|Southern Georgina Basin. Hosts surficial manganocrete and pisolitic manganiferous lag.||||Overlies Tomahawk, Ninmaroo Formations. Is overlain by Coolibah Formation.||12-JUL-16
9394|Kelly Creek Formation|69443|4|Described|p28:7, 26-28, 30, 44, 46|Early Ordovician|Early Ordovician|Casey in Smith (1965). Southern Georgina Basin. Forms prominent hills, scarps and dissected plateaux. Contains a varety of sedimentary structures (listed). 92-290m thick. Sparse fossil assemblage. Peritidal to unrestricted open-marine deposits. Hosts uneconomic manganese deposits at the Halfway Dam prospect. Potential petroleum reservoir. Flowed gas from Ethabuka-1 in Qld.||Toko Group.||Overlies Tomahawk and Ninmaroo Formations, conformably to locally disconformably. Is overlain conformably by Coolibah or Nora Formations, or unconformably by Dulcie Sandstone.|Lower interval of calcareous and dolomitic sandstones, dolostone, siltstone, minor conglomerate and coquinite, overlain by an upper interval of dolostone, dolomitic quartz sandstone, dolomudstone, quartzose dolomitic limestone and minor conglomerate.|12-JUL-16
9394|Kelly Creek Formation|69591|5|Briefly described|p87, p93-95, p97|Ordovician|Ordovician|West Toko Syncline, Georgina Basin. This unit is here removed from the otherwise clastic-dominated Toko Group and assigned to the carbonate-dominated Cockroach Group. Up to 168m thick. Contains a diverse and abundant fauna (listed).||Cockroach Group.||Conformably/disconformably overlies Ninmaroo Formation. Is overlain disconformably by Coolibah Formation and Nora Formation.|Includes quartz and calcareous sandstones, siltstone, dolomite, calcarenite and silicified coquinite with lenses of white chert.|
9394|Kelly Creek Formation|69673|4|Described|p118, p120, p127, p129, p135, p137, p140|Ordovician|Ordovician|92m thick. Potential source rocks present.||Toko Group||Conformably overlain by Coolibah Formation, conformably overlies Tomahawk Formation, Ninmaroo Formation|Calcareous and dolomitic sandstone, dolostone, siltstone, dolomudstone, limestone and minor conglomerate and coquinite.|
9394|Kelly Creek Formation|70380|6|Mentioned|p745|Floian|Tremadocian|Southern Georgina Basin.||||||
9394|Kelly Creek Formation|71800|6|Mentioned|p26 fig 3|Early Ordovician|Early Ordovician|Georgina Basin.||||Overlies the Tomahawk Formation. Overlain by the Nora Formation.||
9394|Kelly Creek Formation|72516|6|Mentioned|p11, p94|||Georgina Basin.||||Conformably overlies the Tomahawk Formation.||
9394|Kelly Creek Formation|73591|6|Mentioned|p40|||Georgina Basin.||||||
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|
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.||
9550|Kilgour Sandstone Member|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
9550|Kilgour Sandstone Member|40691|6|Mentioned|Fig.4|||||||||
9550|Kilgour Sandstone Member|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
9550|Kilgour Sandstone Member|44287|14|Not recorded|opp.11|||Member of Mainoru Fm (Roper Gp.).||||||
9550|Kilgour Sandstone Member|44288|14|Not recorded|map legend|||Sandstone, siltstone. Upper (?) Proterozoic.||||||
9550|Kilgour Sandstone Member|45162|6|Mentioned|Table 7|||See also Fig.4||||||
9550|Kilgour Sandstone Member|70897|6|Mentioned|Fig.1.7.6|||Appears simply as Kilgour. McArthur Basin.||||||
9550|Kilgour Sandstone Member|70968|5|Briefly described|p29, p131|Calymmian|Calymmian|Of Smith (1964) for a sandstone-dominated interval cropping out as a 50m-high cuesta on the SE side of the Abner Range in southern BAUHINIA DOWNS sheet. Exposure is too small to depict at 1:250 000 scale; there is no type area/section; and it has never been properly defined. These authors therefore regard it as informal. See references for Kilgour sandstone member (p17, p20, 29-30).||||||
9550|Kilgour Sandstone Member|71779|5|Briefly described|p2, Fig. 1|||Bauhinia Downs Region, McArthur Basin.||Of Mainoru Formation.||||
9589|Kinevans Sandstone|28255|3|Fully described|p77, Tb. 11 (opp. p8)|||Almost entirely consists of sandstone. Conformably overlain by Antrim Plateau Volcanics; unconformably overlies rocks of the Auvergne and Duredin Groups. Overlies Angalarri Siltstone near Kildurk Homestead. Age is Proterozoic or Cambrian. Max. thick; 45m.||||||14-JUN-05
9589|Kinevans Sandstone|33375|6|Mentioned|p10|||Reddish brown medium sst; up to 30% grains of feldspar and sedimentary rocks; minor calcareous sst. Unconformably overlies Angalarri Siltstone, Ranford Fm. and Moonlight Valley Tillite. Age is Late Adelaidean or Early Cambrian.  Max. thickness: 45m.||||||27-APR-05
9589|Kinevans Sandstone|33376|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
9589|Kinevans Sandstone|33378|5|Briefly described|Map legend|||Reddish brown medium sandstone, minor calcareous sandstone.  Age is either Late Adelaidean or Early Cambrian.||||||27-APR-05
9589|Kinevans Sandstone|45112|4|Described|p46|||p46-47.||||||05-OCT-06
9589|Kinevans Sandstone|48943|2|Defined|p86|Early Cambrian|Neoproterozoic|Upper Prot. or Lower Camb.||||||
9589|Kinevans Sandstone|65337|6|Mentioned|p94.|||||Unit in Kalkarindji Volcanic Group.||Is overlain by Antrim Plateau Volcanics.||
9589|Kinevans Sandstone|67151|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Wolfe Basin.||||Unconformably overlies Ranford Formation. Is unconformably overlain by Antrim Plateau Volcanics.|Red-brown medium sandstone; minor calcareous sandstone.|
9589|Kinevans Sandstone|69437|5|Briefly described|p22:4-5|Ediacaran|Ediacaran|Undated. Unassigned to a Group or a Basin. May be equivalent to Mount Forster Sandstone (Wolfe Basin, WA).||||||12-JUL-16
9589|Kinevans Sandstone|69442|5|Briefly described|p27:6|||Mapped in 1st Edition of WATERLOO map, but unassigned to any Group or Basin. Recent NTGS mapping suggests it may be equivalent to Mount Forster Sandstone (Albert Edward Group) of the Wolfe Basin in WA. Undated.|||||Red-brown medium-grained sandstone with subordinate calcareous cement locally.|12-JUL-16
9589|Kinevans Sandstone|69445|5|Briefly described|p30:3-4|||Sweet et al. (1974). Included in the Kalkarindji Volcanic Group of Kruse (in Rawlings et al., 2008). Victoria River region.||||Is overlain conformably by Antrim Plateau Volcanics.||12-JUL-16
9589|Kinevans Sandstone|70655|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Wolfe Basin.||||Overlies Angalarri Siltstone, Saddle Creek Formation, Moonlight Valley Tillite unconformably. Is unconformably overlain by Antrim Plateau Volcanics.|Red-brown medium sandstone; minor calcareous sandstone.|24-JAN-22
9589|Kinevans Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
9589|Kinevans Sandstone|73083|6|Mentioned|p48|||||||Overlain by Kalkarindji Suite.||
9589|Kinevans Sandstone|73255|6|Mentioned|p533 Fig.1, p534 Fig.2, p535|early Cambrian|early Cambrian|||Albert Edward Group||Disconformably overlies the Ranford Formation and Flat Rock Sandstone. Underlies the Antrim Plateau Basalt.||
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|
9771|Koolatong Siltstone|22538|6|Mentioned|Fig3 P708|||||||||
9771|Koolatong Siltstone|22600|4|Described|Map legend|Statherian|Statherian|||||||
9771|Koolatong Siltstone|24048|3|Fully described|p53|Mesoproterozoic|Paleoproterozoic|Of the Balma Group.  Max. thickness: 1000m.  Geological Province: McArthur Basin.||||||07-NOV-08
9771|Koolatong Siltstone|24049|5|Briefly described|Map Legend|Statherian|Statherian|Of Balma Group. Mudstone: sometimes dolomitic, evaporite pseudomorphs and dessication cracks; sandstone: fine-grained, thin-bedded, interbedded with mudstone; dolostone and limestone cycles; most of formation very recessive. Geol. Prov: McArthur Basin.||||||11-OCT-05
9771|Koolatong Siltstone|32660|5|Briefly described|Table 4|||||||||
9771|Koolatong Siltstone|42597|5|Briefly described|Map Legend|Carpentarian||||||||
9771|Koolatong Siltstone|43010|2|Defined|p108||Paleoproterozoic|Of McArthur Group. Of Statherian age.||||||07-NOV-08
9771|Koolatong Siltstone|44112|4|Described|p49,52-55,58|||||||||
9771|Koolatong Siltstone|44299|4|Described|p.12|||SD/53-7,8. Lower(?) Proterozoic. Table 1.||||||
9771|Koolatong Siltstone|44300|14|Not recorded|map legend|||SD/53-7,8. Lower (?) Proterozoic.||||||
9771|Koolatong Siltstone|45162|6|Mentioned|p45|||||||||
9771|Koolatong Siltstone|61403|5|Briefly described|Map Legend|Statherian|Statherian|Of Balma Group. Mudstone: sometimes dolomitic, evaporite pseudomorphs and dessication cracks; sandstone: fine-grained, thin-bedded, interbedded with m udstone; dolostone and limestone cycles; most of formation very recessive. Geol. Prov: McArthur Basin.||||||
9771|Koolatong Siltstone|64817|6|Mentioned|p353 Fig.4 |||||Of the Balma Group.||||
9771|Koolatong Siltstone|67323|6|Mentioned|Eastern Australia Time-Space Plot|||McArthur region.||||||
9771|Koolatong Siltstone|69430|4|Described|p15:3, 13, 21-22|Statherian|Statherian|Walker Fault Zone, northern McArthur Basin. Over 500m thick. Shallow-water low-energy, locally emergent or evaporitic, sediments; some high-energy storm-influenced facies.||Basal Balma Group.||Conformably and gradationally overlies Fleming Sandstone. Is overlain by Strawbridge Breccia (contact not exposed).|Khaki green to red mudstone, sometimes dolomitic, local evaporite pseudomorphs; fine-grained, thinly bedded sandstone interbedded with mudstone; grey to buff, microbial-laminated, stromatolitic, intraclastic dolostone and limestone cycles with ooids.|12-JUL-16
9771|Koolatong Siltstone|69673|6|Mentioned|p16 fig 13|Mesoproterozoic|Paleoproterozoic|Walker Fault Zone||Balma Group||Overlain by Strawbridge Breccia||
9771|Koolatong Siltstone|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.||Lower Balma Group.||||
9771|Koolatong Siltstone|72373|5|Briefly described|p6,9|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin.||Unit of Balma Group.||||
9772|Koolendong Granite|24197|5|Briefly described|p105|Paleoproterozoic|Paleoproterozoic|Of the Wagait Suite. Age: ~1850Ma. Geological Province: Pine Creek Inlier.||||||07-FEB-11
9772|Koolendong Granite|32307|4|Described|Table 1|||Carpentarian||||||
9772|Koolendong Granite|32310|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
9772|Koolendong Granite|32701|6|Mentioned|p7|||L.Prot.||||||
9772|Koolendong Granite|33376|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
9772|Koolendong Granite|33377|6|Mentioned|Table 1|||Strat.||||||
9772|Koolendong Granite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
9772|Koolendong Granite|45112|5|Briefly described|Table 4|||||||||
9772|Koolendong Granite|48942|2|Defined|p28|Carpentarian|Carpentarian|||||||
9772|Koolendong Granite|50586|5|Briefly described|p1.1, 6.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Of the Wagait Suite.||||||07-NOV-08
9772|Koolendong Granite|63866|5|Briefly described|p105|Orosirian|Orosirian|Litchfield Province, Pine Creek Orogen. |1860 +/-5 Ma (Worden et al, in review)|||||
9772|Koolendong Granite|64677|5|Briefly described|v, p1, p12-14, p46|||Pine Creek Orogen.|1859.9 +2.2/-4.8 Ma.|||Intrudes Burrell Creek Formation. Is overlain nonconformably by Moyle River Formation.||
9772|Koolendong Granite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Wagait Suite. Age 1860Ma SHRIMP U/Pb. I-type. Granodiorite. Coarse, equigranular and porphyritic granite and granodiorite. Intrudes Burrell Creek Formation and Chilling Sandstone.||||||07-JAN-09
9772|Koolendong Granite|67167|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Unit in Wagait Suite.|||Coarse, equigranular and porphyritic granite and granodiorite.|
9772|Koolendong Granite|69420|5|Briefly described|p5:18, 28-29|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Mineralogy described. SHRIMP U-Pb zircon age.|1860 +2/-5 Ma: Worden et al. (2008).|Wagait Suite.||Intrudes the Burrell Creek Formation.|A biotite-hornblende granodiorite and leucocratic porphyritic quartz monzonite; quartz and pegmatite veins are abundant.|12-JUL-16
9772|Koolendong Granite|69435|6|Mentioned|p20:3|||||||Is overlain unconformably by Moyle River Formation.||12-JUL-16
9772|Koolendong Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granite|
9772|Koolendong Granite|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|1860+/-3.5 Ma crystallisation: U-Pb zircon SHRIMP||||Altered granite.|
9863|Kudjumarndi Quartzite|9534|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Kakadu Group.  Coarse orthoquartzite, muscovite quartzite, minor gneissic biotite quartzite; feldspar-quartz gneiss.||||||07-NOV-08
9863|Kudjumarndi Quartzite|9691|5|Briefly described|Map Legend|||Of the Kakadu Group. Coarse orthoquartzite.||||||
9863|Kudjumarndi Quartzite|9701|5|Briefly described|Map Legend|Proterozoic|Archean|Of the Kakadu Group. Coarse orthoquartzite.||||||07-NOV-08
9863|Kudjumarndi Quartzite|22810|5|Briefly described|Table2 P5|||Maximum thickness 150m.||||||09-OCT-06
9863|Kudjumarndi Quartzite|35140|6|Mentioned|Fig.2|||||||||
9863|Kudjumarndi Quartzite|36535|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
9863|Kudjumarndi Quartzite|36635|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
9863|Kudjumarndi Quartzite|37462|6|Mentioned|Fig.4.8|||||||||
9863|Kudjumarndi Quartzite|37815|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
9863|Kudjumarndi Quartzite|38239|6|Mentioned|Fig.2|||||||||
9863|Kudjumarndi Quartzite|38884|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
9863|Kudjumarndi Quartzite|39069|5|Briefly described|Table 1|||||||||
9863|Kudjumarndi Quartzite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
9863|Kudjumarndi Quartzite|40493|5|Briefly described|Table 1|||||||||
9863|Kudjumarndi Quartzite|40808|5|Briefly described|Table 2|||||||||
9863|Kudjumarndi Quartzite|41146|5|Briefly described|Fig.2|||||||||
9863|Kudjumarndi Quartzite|43187|5|Briefly described|p2|||||||||
9863|Kudjumarndi Quartzite|46639|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Kakadu Group. Underlain by Mount Howship Gneiss (of Kakadu Group).  Coarse orthoquartzite, muscovite quartzite, minor gneissic biotite quartzite.||||||07-NOV-08
9863|Kudjumarndi Quartzite|46700|5|Briefly described|P7, Table1 P12||Proterozoic|Equivalent to Mount Howship Gneiss||||||
9863|Kudjumarndi Quartzite|60550|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Kakadu Group. Coarse orthoquartzite, muscovite quartzite, minor gneissic biotite quartzite.||||||
9863|Kudjumarndi Quartzite|64956|4|Described|p2 Tb. 21, p86-88|Paleoproterozoic|Paleoproterozoic|Upper unit of the Kakadu Group. Conformable on Mount Howship Gneiss. Max. depositional age: 2404+/-16ma.  Lateral equivalent of Mummarlary Quartzite. Geological province: Pine Creek Orogen. Sample is muscovite-bearing quartzite.||||||07-FEB-11
9863|Kudjumarndi Quartzite|65232|6|Mentioned|p23|||With Mount Howship Gneiss, underlies Myra Falls Metamorphics in the Myra Falls Inlier and are correlated with Kakadu Group. See also misspelt Kudjumarandi Quartzite.||||||09-FEB-10
9863|Kudjumarndi Quartzite|66683|5|Briefly described|pp368-369, p372. |Paleoproterozoic|Paleoproterozoic|Outcrop pattern controlled by kilometre-scale F2/F3 structures. Exposure lies parallel to a regional positive gravity anomaly, interpreted as Oenpelli Dolerite emplaced at base of Kakadu Group.||Unit in Kakadu Group.||||
9863|Kudjumarndi Quartzite|67479|5|Briefly described|p29, p33, p37, p55|Paleoproterozoic|Paleoproterozoic|||Of the Kakadu Group.||Underlain by the Kukalak Gneiss and the Njibinjibinj Gneiss.|Metasedimentary rocks.|
9863|Kudjumarndi Quartzite|67564|6|Mentioned|p11.|Paleoproterozoic|Paleoproterozoic|||Unit in Kakadu Group.||||
9863|Kudjumarndi Quartzite|67779|3|Fully described|p10 Table 1, pp15-16, pp43-47, p89.|Paleoproterozoic|Paleoproterozoic|Nimbuwah Domain, Pine Creek Orogen. Forms low ridges. Up to 150 m thick. Correlated with Munmarlary Quartzite and Mount Partridge Group. Age is based on this latter correlation. Outcrops in Myra Falls Inlier; rests on Neoarchean gneiss basement. Detrital zircons indicate the sediments were derived from underlying Arrarra and Kukalak Gneisses. Structures and geochronology are described in detail.|Deposition c.2020 Ma.|Unit in Kakadu Group.||Unconformably overlies Kukalak and Arrarra Gneisses. Is thrust-faulted over Mamadawerre Sandstone. Is overlain by the Cahill Formation.|Massive orthoquartzite, locally muscovite- or biotite-bearing, rare cross-beds; meta-arkose, locally interlayered with foliated amphibolite.|14-MAY-18
9863|Kudjumarndi Quartzite|68697|6|Mentioned|p36|||||||||
9863|Kudjumarndi Quartzite|69420|4|Described|p5:4, 6-7, 24, 67|Paleoproterozoic|Paleoproterozoic|Nimbuwah Domain, Pine Creek Orogen. Forms ridges in the Myra Falls Inlier. c.150m thick. Fluvial to shallow-marine deposits. Detrital zircon age peaks at c.2673-2572 Ma and c.2530-2483 Ma.||Kakadu Group.|||Orthoquartzite, ranging from monomineralic to micaceous, hornblende-rich and feldspathic types; gneiss; minor schist.|12-JUL-16
9863|Kudjumarndi Quartzite|69917|5|Briefly described|p24, 42|Paleoproterozoic|Paleoproterozoic|Has similar detrital zircon spectrum to Munmalary Quartzite.||Of Kakadu Group||Overlies Kukalak Gneiss.||
9863|Kudjumarndi Quartzite|70853|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||<2400 Ma.|Kakadu Group.|||Massive orthoquartzite: locally muscovite- or biotite-bearing; rare cross-beds.|
9863|Kudjumarndi Quartzite|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|2404+/-16 Ma (MDA: U-Pb zircon SHRIMP)||||Muscovite-bearing quartzite.|
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.||||||
9910|Kunja Siltstone|14019|4|Described|p8-9, 28|Paleoproterozoic|Paleoproterozoic|Of the Limbunya Group. Mudstone and siltstone, rare dolostone and tuffite. Conformably on Mallabah Dolostone, conformably overlain by Farquharson Sandstone. Age: 1635 +/- 19Ma. Type section 61m. Geological Province: Birrindudu Basin.||||||07-NOV-08
9910|Kunja Siltstone|24122|5|Briefly described|p4 Fig.3|||Of Limbunya Group.  Geological Province: Birrindudu Basin.||||||
9910|Kunja Siltstone|24297|5|Briefly described|p4 Fig.3|Proterozoic|Proterozoic|Of Limbunya Group.  Geological Province: Birrindudu Basin.||||||
9910|Kunja Siltstone|24441|5|Briefly described|p1 Fig. 1|||Of the Limbunya Group. Overlies Mallabah Dolostone;  overlain by Farquharson Sandstone. Geological Province: Birrindudu Basin.||||||
9910|Kunja Siltstone|24442|5|Briefly described|p50 Fig. 1|||Of the Limbunya Group.  Geological Province: Birrindudu Basin.||||||
9910|Kunja Siltstone|28255|3|Fully described|p19-20, Tb. 11 (opp. p8)|||Of the Limbunya Group. Comprises siltstone, shale and silty dolomite; poorly outcropping. Overlain by Farquharson Fm; underlain by Mallabah Dolomite.  Age is Adeaidean or Carpentarian. Max. thickness: 60m. See also p121 Appendix.||||||
9910|Kunja Siltstone|30003|4|Described|p9|||Of the Limbunya Group. Fissile green fine siltstone; minor flaggy to fissile grey, pink and brown dolomite.Max. thickness: 64m.||||||19-APR-05
9910|Kunja Siltstone|30004|6|Mentioned|Map legend|Proterozoic|Proterozoic|Carpentarian or Adelaidean||||||
9910|Kunja Siltstone|32172|4|Described|Table 1|||Carpentarian or Adelaidean||||||
9910|Kunja Siltstone|32173|5|Briefly described|Map legend|Adelaidean|Carpentarian|Of the Limbunya Group.  Purple and green siltstone and silty dolomite.  Conformably overlain by Farquharson Sandstone; conformably overlies the Mallabah Dolomite.  Carpentarian or Adelaidean (per legend).||||||17-NOV-04
9910|Kunja Siltstone|32660|5|Briefly described|Table 6|||||||||
9910|Kunja Siltstone|33375|6|Mentioned|p9|||Of the Limbunya Group. Age is Carpentarian or Adelaidean. Siltstone, dolomitic siltstone. Conformable on Mallabah Dolomite. Max. thickness: ~50m.||||||26-APR-05
9910|Kunja Siltstone|33376|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
9910|Kunja Siltstone|33378|5|Briefly described|Map legend|||Of the Limbunya Group. Siltstone, dolomitic siltstone.Age is Carpentarian or Adelaidean.||||||27-APR-05
9910|Kunja Siltstone|45112|5|Briefly described|Table 7|||||||||
9910|Kunja Siltstone|48943|2|Defined|p22|Proterozoic|Proterozoic|Strat. section p130.||||||09-OCT-06
9910|Kunja Siltstone|60589|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Limbunya Group.  Mudstone, siltstone, minor orange water-laid tuffite and carbonaceous mudstone.  Conformably overlies the Mallabah Formation; conformably overlain by Farquharson Sandstone.  Geological Province: Birrindudu Basin.||||||07-NOV-08
9910|Kunja Siltstone|60672|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Siltstone, dolomitic siltstone, mudstone. Of Limbunya Group. Overlain by Farquharson Sandstone. Overlies Mallabah Dolostone. Geological Province: Birrindudu Basin.||||||07-NOV-08
9910|Kunja Siltstone|60685|5|Briefly described|p4 Fig. 3|||Of the Limbunya Group. Geological Province: Birrindudu Basin.||||||
9910|Kunja Siltstone|65342|6|Mentioned|p11 Fig.13. |||Birrindudu Basin.||Unit in Limbunya Group.||Overlies Mallabah Dolostone. Is overlain by Farquharson Sandstone.||
9910|Kunja Siltstone|67151|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Birindudu Basin.||Unit in Limbunya Group.||Overlies Mallabah Dolostone. Is overlain by Farquharson Sandstone.|Siltstone, dolomitic siltstone, mudstone, minor tuffite.|
9910|Kunja Siltstone|68733|5|Briefly described|p177 Fig.2, p186|Statherian|Statherian|Birrindudu Basin.|ca. 1640 Ma, tuff (Cutovinos et al. 2002)|Of the Limbunya Group.||||
9910|Kunja Siltstone|69429|6|Mentioned|p14:2 Fig.14.2|Paleoproterozoic|Paleoproterozoic|||Limbunya Group.||||12-JUL-16
9910|Kunja Siltstone|69432|4|Described|p17:2, 7, 13-14|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin. Up to 60m thick. Interpreted as a maximum flooding surface. Exploration target for base metals; contains pyritic shale units but has not been extensively explored. Has poor to excellent hydrocarbon source potential. SHRIMP U-Pb zircon age; misprinted as 1653 +/- 19 Ma on 17:2.|1635 +/- 19 Ma (Fanning, 1991).|Limbunya Group.||Is overlain conformably by Farquharson Sandstone.|Homogeneous succession of laminated mudstone and fissile siltstone bounded by silty dolostone. Includes thin beds of water-lain tuff. Contains basal carbonaceous material (TOC 2.2%) which is weakly anomalous in Pb and Zn.|12-JUL-16
9910|Kunja Siltstone|69673|6|Mentioned|p48 fig 35, p50|||Carbonaceous material intersected in drillhole.||Limbunya Group||Overlies Mallabah Dolostone, overlain by Farquharson Sandstone||
9910|Kunja Siltstone|70655|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Birindudu Basin.||Limbunya Group||Overlies Mallabah Dolostone. Is overlain by Farquharson Sandstone.|Siltstone, dolomitic siltstone, mudstone, minor tuffite.|07-NOV-16
9910|Kunja Siltstone|70854|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin. Maximum depositional age.|<1635 +/- 18 Ma (SHRIMP zircon age).|Limbunya Group.||Overlies Mallabah Dolostone. Is overlain by Farquharson Sandstone.|Siltstone, dolomitic siltstone, mudstone.|
9910|Kunja Siltstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone|
9910|Kunja Siltstone|71302|5|Briefly described|p6|Paleoproterozoic|Paleoproterozoic|Of Birindudu Basin. Contains 1635+\-19 Ma tuffs (Fanning, 1991; Smith, 2001), proposed to have been sourced from reworking of upper Limbunya Group rocks (Smith 2001).||Unit of Limbunya Group.||Overlain by Farquharson Sandstone. Underlain by Mallabah Dolostone.||
9910|Kunja Siltstone|71374|6|Mentioned|p36|Statherian|Statherian|SHRIMP dates are derived from waterlain tuffs.|1635 +/- 19 Ma (SHRIMP U-Pb)|||Conformably overlain by the Farquharson Sandstone.||
9910|Kunja Siltstone|71592|5|Briefly described|Appendix A.|||Birrindudu Basin.|1635+/-19 Ma (MDA: zircon).||||Orange waterlain tuffite horizon.|
9910|Kunja Siltstone|72718|6|Mentioned|p7|Statherian|Statherian|Birrindudu Basin.|1653 +/- 19 Ma|Limbunyah Group||Underlain by Mullabah Dolostone. Overlain by Farquharson Sandstone.||
9910|Kunja Siltstone|73280|6|Mentioned|p1, p4-5, App.1A|||McArthur Basin. Sampled for XRD mineralogy to investigate brittleness and Kubler indices [see report].||||||
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.||
9937|Kurrundie Sandstone|23384|6|Mentioned|Fig 27|||Of Needham and Stuart-Smith (1985).||||||
9937|Kurrundie Sandstone|23867|5|Briefly described|Fig. 3|||Of Edith River Group.  Geological Province: McArthur Basin.||||||
9937|Kurrundie Sandstone|30831|6|Mentioned|Fig.1|||||||||
9937|Kurrundie Sandstone|39357|4|Described|p14|||||||||
9937|Kurrundie Sandstone|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
9937|Kurrundie Sandstone|40248|4|Described|p224|||||||||
9937|Kurrundie Sandstone|40823|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
9937|Kurrundie Sandstone|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
9937|Kurrundie Sandstone|41125|6|Mentioned|Fig.15|||||||||
9937|Kurrundie Sandstone|41311|4|Described|p14|||||||||
9937|Kurrundie Sandstone|41397|4|Described|p16|||||||||
9937|Kurrundie Sandstone|41407|6|Mentioned|Map legend|Proterozoic||||||||
9937|Kurrundie Sandstone|43140|4|Described|p3||Paleoproterozoic|||||||07-NOV-08
9937|Kurrundie Sandstone|43187|5|Briefly described|p2|||||||||
9937|Kurrundie Sandstone|43832|4|Described|24, Table6 p22||Paleoproterozoic|Max. age: 1870 Ma (base of Edith River Group, p21)||||||07-NOV-08
9937|Kurrundie Sandstone|46658|6|Mentioned|p557|||||||||
9937|Kurrundie Sandstone|47049|5|Briefly described|Table|||Elevation to formation from member status; placed in Edith River Group.||||||
9937|Kurrundie Sandstone|49744|5|Briefly described|Fig.3|||||||||
9937|Kurrundie Sandstone|60680|5|Briefly described|Map legend|Orosirian|Orosirian|Of the Edith River Group. Coarse to pebbly lithic quartz sandstone with massive interbeds of polymictic pebble to boulder conglomerate.||||||07-JAN-09
9937|Kurrundie Sandstone|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1800-1825Ma. Of Edith River Group.  Max. thickness 350m. Purple to brown, thickly bedded to massive, coarse to pebbly lithic quartz sandstone with massive interbeds of polymictic pebble to boulder conglomerate; minor planar-laminated siltstone.||||||07-JAN-09
9937|Kurrundie Sandstone|64817|5|Briefly described|p355 Fig.5,|||Arnhem Shelf, McArthur Basin.||Of the Edith River Group.|||Sandstone and conglomerate.|04-JUN-18
9937|Kurrundie Sandstone|65232|6|Mentioned|p45, p44 Fig. 29|||Of Edith River Group. Basal polymict conglomerate and sandstone.||||||09-FEB-10
9937|Kurrundie Sandstone|67564|3|Fully described|p2, p7 Table 2, p26 Fig.17, pp29-30.|Paleoproterozoic|Paleoproterozoic|Component of Arnhem Land Plateau. Forms prominent strike ridges and pavements. 350 m of juvenile braidplain deposits. Most of the conglomerate clasts are from the underlying El Sherana Group. Includes rocks previously mapped by Walpole (1963) as Kurrundie Member. Is correlated with Phillips Creek and Hindrance Sandstones.|c.1825 Ma.|Unit in Edith River Group.||Unconformably overlies Big Sunday Formation. Is overlain conformably by Plum Tree Creek Volcanics.|Thickly bedded to massive, coarse to pebbly lithic quartz sandstone with interbeds of polymictic pebble to boulder conglomerate; minor siltstone.|
9937|Kurrundie Sandstone|67779|5|Briefly described|p6 Fig.5.|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen.||Unit in Edith River Group.||||
9937|Kurrundie Sandstone|69420|4|Described|p5:4, 7, 15, 79|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen. South Alligator region. c.350m thick. Fluviatile: juvenile braidplain deposits.||Basal Edith River Group.||Overlies Hindrance Creek Sandstone and (unconformably) Big Sunday Formation. Is overlain by Phillips Creek Sandstone.|Thickly bedded to massive, purple to brown, coarse to pebbly lithic quartz sandstone with interbeds of polymictic pebble to boulder conglomerate; minor siltstone.|12-JUL-16
9937|Kurrundie Sandstone|70293|5|Briefly described|p598-599, p615|Orosirian|Orosirian|Coronation Hill area.||Edith River Group||Is overlain unconformably by Plum Tree Creek Volcanics. Unconformably overlies Big Sunday Formation (El Sherana Group). Is intruded by Malone Creek Granite.|Basal lithic quartz sandstone and polymictic conglomerate.|
