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
21096|Abarungkwa Sandstone|22538|6|Mentioned|Fig3 p708|||||||||04-JUN-18
21096|Abarungkwa Sandstone|22600|4|Described|Map legend|Orosirian|Orosirian|||||||
21096|Abarungkwa Sandstone|22808|2|Defined|29|Orosirian|Orosirian|Parent Bustard Subgroup. Overlying unit Bickerton Rhyolite, underlying unit Grindall Formation||||||
21096|Abarungkwa Sandstone|24048|3|Fully described|p15|Statherian|Orosirian|Parent Bustard Group.  Max. thickness: 150m.  Geological Province: McArthur Basin.||||||
21096|Abarungkwa Sandstone|24049|5|Briefly described|Map Legend|Orosirian|Orosirian|Of Bustard Subgroup, Groote Eylandt Group. Sandstone: pebbly, quartz-rich (lithic at base); granule conglomerate, quartz-rich; pebble to cobble conglomerate, polymict; quartz sandstone. Geol. Prov: McArthur Basin.||||||13-OCT-05
21096|Abarungkwa Sandstone|43292|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
21096|Abarungkwa Sandstone|44112|6|Mentioned|Fig11p30|||||||||
21096|Abarungkwa Sandstone|61403|5|Briefly described|Map Legend|Orosirian|Orosirian|Of Bustard Subgroup, Groote Eylandt Group. Sandstone: pebbly, quartz-rich (lithic at base); granule conglomerate, quartz-rich; pebble to cobble conglo merate, polymict; quartz sandstone. Geol. Prov: McArthur Basin.||||||
21096|Abarungkwa Sandstone|64817|5|Briefly described|p353 Fig.4, p355 Fig.5 |||Caledon Shelf South, McArthur Basin. Age range shown is for whole of Bustard Subgroup.|1820-1790 Ma.|Of the Bustard Subgroup.|||Sandstone and conglomerate.|04-JUN-18
21096|Abarungkwa Sandstone|69430|4|Described|p15:3, 5|||NE McArthur Basin. Estimated thickness up to 150m. High-energy braided fluvial deposits.||Bustard Subgroup.||Overlies Erringkarri Rhyolite ?disconformably and Grindall Formation unconformably. Is overlain conformably by Bickerton Rhyolite or unconformably by Milyakburra Formation.|White, coarse- to very coarse-grained, cross-bedded pebbly quartz-rich sandstone, lithic at base; quartz-rich granule conglomerate; polymictic pebble and cobble conglomerate; minor medium-grained quartz sandstone.|12-JUL-16
21096|Abarungkwa Sandstone|69673|6|Mentioned|p16 fig 13|||Northeastern McArthur Basin.||Bustard Subgroup||Overlain by Bickerton Rhyolite, overlies Erringkarri Rhyolite||04-JUN-18
21122|Alyangula Subgroup|22538|6|Mentioned|p714, Fig3 p208||Statherian|||||||17-JUL-06
21122|Alyangula Subgroup|22600|4|Described|Map legend|Orosirian|Orosirian|||||||
21122|Alyangula Subgroup|22808|2|Defined|31|Statherian|Statherian|Of the Groote Eylandt Group. Underlying unit: Milyema Formation||||||17-JUL-06
21122|Alyangula Subgroup|24047|5|Briefly described|p12 Fig. 10|Paleoproterozoic|Paleoproterozoic|Age: 1800-1740Ma.  Geological Province: McArthur Basin.||||||04-MAR-20
21122|Alyangula Subgroup|24048|3|Fully described|p19|Paleoproterozoic|Paleoproterozoic|Of the Groote Eylandt Group.  Geological Province: McArthur Basin.||||||07-NOV-08
21122|Alyangula Subgroup|24049|5|Briefly described|Map Legend|Orosirian|Orosirian|Of Groote Eylandt Group. Includes Dalumbu Sandstone, Bartalumba Basalt, Woodah Sandstone, and Alyinga Sandstone. Geol. Prov: McArthur Basin.||||||13-OCT-05
21122|Alyangula Subgroup|43292|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
21122|Alyangula Subgroup|44112|6|Mentioned|p10,43|||Part of Supersequence 1(B)||||||
21122|Alyangula Subgroup|61403|5|Briefly described|Map Legend|Orosirian|Orosirian|Of Groote Eylandt Group. Includes Dalumbu Sandstone, Bartalumba Basalt, Woodah Sandstone, and Alyinga Sandstone. Geol. Prov: McArthur Basin.||||||
21122|Alyangula Subgroup|63866|5|Briefly described|p115|||Leichhardt/Calvert Superbasin.||Groote Eylandt Group|Includes the Alyinga Sandstone.|||
21122|Alyangula Subgroup|64817|5|Briefly described|p353 Fig.4, p355 Fig.5 |||Caledon Shelf South, McArthur Basin.||Of the Groote Eylandt Group.|Includes Dalumbu Sandstone, Bartalumba Basalt, Woodah Sandstone and Alyinga Sandstone.|Disconformably overlies Bustard Subgroup.|Sandstone and conglomerate; mafic volcanics.|04-JUN-18
21122|Alyangula Subgroup|69430|4|Described|p15:3-6|||NE McArthur Basin. Forms most of Groote Eylandt, Connexion Island and the SE part of Bickerton Island.||Groote Eylandt Group.|Woodah, Alyinga, Dalumbu Sandstones; Bartalumba Basalt.||Fluvial sandstone, conglomerate and basaltic volcanic rocks.|12-JUL-16
21122|Alyangula Subgroup|69673|6|Mentioned|p16 fig 13, p17|||Part of the lower redbank package, a 2-4km thick succession of fluvial to intertidal sandstone with intervening flood basalt unit and an upper shallow marine shale-carbonate unit. Northeastern McArthur Basin.||Groote Eylandt Group|Includes Dalumbu Sandstone, Bartalumba Basalt, Woodnah Sandstone, Anyinga Sandstone|||
21122|Alyangula Subgroup|70302|5|Briefly described|iv, p5, p7|Statherian|Statherian|McArthur Basin.||Groote Eylandt Group.|Woodah Sandstone.|||
21122|Alyangula Subgroup|71374|5|Briefly described|p24|||McArthur Basin.||Groote Eylandt Group||Unconformably overlain by the Coast Range Sandstone.||04-MAY-18
21122|Alyangula Subgroup|71606|5|Briefly described|p137|Statherian|Statherian|South Caledon Shelf, McArthur Basin.||Unit of Groote Eylandt Group.||Upper unit of Groote Eylandt Group. Underlain conformably to unconformably by Bustard Subgroup.||
21122|Alyangula Subgroup|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.||Upper Groote Eylandt Group.|||Quartzose sandstone; subordinate conglomerate, mudstone; basaltic volcanics.|04-MAR-20
21122|Alyangula Subgroup|72377|5|Briefly described|p6|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin.||Unit of Groote Eylandt Group.||Overlain unconformably by Coast Range Sandstone.||
21123|Alyinga Sandstone|22538|6|Mentioned|Fig3 P708|||||||||
21123|Alyinga Sandstone|22600|4|Described|Map legend|Statherian|Statherian|||||||
21123|Alyinga Sandstone|22808|2|Defined|31|Statherian|Statherian|Of the Alyangula Subgroup. Overlying unit: Bartalumba Basalt, underlying unit: Milyema Formation||||||17-JUL-06
21123|Alyinga Sandstone|24047|5|Briefly described|p49|Paleoproterozoic|Paleoproterozoic|Pebbly quartz sandstone.  See also p50 Fig. 41.||||||07-NOV-08
21123|Alyinga Sandstone|24048|3|Fully described|p21|Paleoproterozoic|Paleoproterozoic|Of the Alyangula Subgroup.  Max. thickness: 300m.  Geological Province: McArthur Basin.||||||07-NOV-08
21123|Alyinga Sandstone|24049|5|Briefly described|Map Legend|Orosirian|Orosirian|Of Alyangula Subgroup, Groote Eylandt Group. Thin basal granule to boulder conglomerate and pebbly to cobbly sandstone, polymict; sandstone: locally pebbly, quartz-rich, trough cross-beds in lower part, ripple horizons at top. Geol. Prov: McArthur Basin.||||||13-OCT-05
21123|Alyinga Sandstone|43292|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
21123|Alyinga Sandstone|44112|6|Mentioned|Fig11p30|||||||||
21123|Alyinga Sandstone|61403|5|Briefly described|Map Legend|Orosirian|Orosirian|Of Alyangula Subgroup, Groote Eylandt Group. Thin basal granule to boulder conglomerate and pebbly to cobbly sandstone, polymict; sandstone: locally p ebbly, quartz-rich, trough cross-beds in lower part, ripple horizons at top. Geol. Prov: McArthur Basin.||||||
21123|Alyinga Sandstone|63866|5|Briefly described|p115|||Leichhardt/Calvert Superbasin.||Alyangula Subgroup||Equivalent to the Woodah Sandstone.||
21123|Alyinga Sandstone|64817|6|Mentioned|p353 Fig.4, p355 Fig.5 |||Caledon Shelf South, McArthur Basin.||Of the Alyangula Subgroup.||Disconformably overlies Milyema Formation.|Sandstone and conglomerate.|04-JUN-18
21123|Alyinga Sandstone|69430|4|Described|p15:3, 5-6|||NE McArthur Basin. c.300m thick in type area. Mostly high-energy braided fluvial, with minor marginal marine deposits. Appears as Anyinga Sandstone in 15:3.||Alyangula Subgroup.||Apparently disconformably overlies Milyema Formation. Lateral equivalent of Woodah Sandstone.|Medium- to coarse-grained sandstone, with very large trough cross-beds in lower part. Basal polymict granule to boulder conglomerate and pebbly and cobbly sandstone.|12-JUL-16
21123|Alyinga Sandstone|69455|6|Mentioned|p39:10|Paleoproterozoic|Paleoproterozoic|Groote Eylandt.||||||12-JUL-16
21126|Ambalindum Sandstone Member|43565|4|Described|p424-444|||||||||
21126|Ambalindum Sandstone Member|43748|5|Briefly described|p10, Fig. 4,7, Tb 1|Middle Eocene|Late Cretaceous|55m thick in Alice Springs 2.||Of Hale Formation.|||Argillaceous, poorly sorted sandstone and pebble conglomerate.|19-DEC-11
21126|Ambalindum Sandstone Member|65194|5|Briefly described|p53 Fig.4.7.|||Unit in Hale Formation. Unconformably overlies Arunta Complex. Is overlain by Claraville Mudstone Member. Sandstone, lesser conglomerate.||||||
21126|Ambalindum Sandstone Member|69458|5|Briefly described|p42:7-8|||Hale Basin. High-energy fluvial deposits. c.55m thick.||Basal Hale Formation.||Is overlain conformably by Delaney Mudstone Member.|Shaly, poorly sorted sandstone (locally yellow and weathered) with intercalations of granule and pebble conglomerate.|12-JUL-16
21137|Andrew Young Igneous Complex|7821|5|Briefly described|p47-48, 57, 59-61, 64, 66|||Central Province of Arunta Inlier; south of Ngalia Basin. Corresponds with a marked magnetic high. Zircon analyses tabulated. The gabbro host rock has been dated at 1625 Ma (U-Pb zircon: Fanning, unpubl. data). Undeformed; post-Strangways Orogeny.|1635 +/- 9 Ma (granite).||||Mainly gabbroic to tonalitic rocks, with lesser small bodies of granite and pegmatite.|
21137|Andrew Young Igneous Complex|23844|6|Mentioned|p14, 15|||Geological Province: Arunta Province. Of Young et al (1995a, b). Age: ~1635 +/- 9Ma||||||
21137|Andrew Young Igneous Complex|24197|5|Briefly described|p61 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Age: 1635Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
21137|Andrew Young Igneous Complex|43275|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
21137|Andrew Young Igneous Complex|43749|6|Mentioned|Fig.1,p6||Mesoproterozoic|Age: approx 1635 Ma||||||
21137|Andrew Young Igneous Complex|44158|4|Described|p16, Table.1|Paleoproterozoic|Paleoproterozoic|Age: granite 1635+/- 9 Ma, gabbronorite ~1625 Ma, U-Pb zircon age dates. of Arunta Inlier.||||||05-MAY-10
21137|Andrew Young Igneous Complex|50369|5|Briefly described|p1.5, 20.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Andrew Young Suite. Age: 1635 +/- 9Ma.||||||07-NOV-08
21137|Andrew Young Igneous Complex|60674|6|Mentioned|Solid Geology legend|||Geological Province: Aileron Province.||||||
21137|Andrew Young Igneous Complex|61387|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|All undifferentiated intrusive rock including porphyritic biotite granite, with variable magnetic intensity. Age: ~1640Ma. In the Arunta region.||||||07-NOV-08
21137|Andrew Young Igneous Complex|61518|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Gabbronorite, tonalite, granite, extremely magnetic. Geological Province: Aileron Province.||||||07-NOV-08
21137|Andrew Young Igneous Complex|61519|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Porphyritic biotite granite, fine grained quartz diorite, undifferentiated norite, diorite and minor biotite granite, anorthosite and calc-silicate rock, orthopyroxene norite, olivine bearing norite and gabbronorite. Geological Province: Aileron Province.||||||07-NOV-08
21137|Andrew Young Igneous Complex|61660|5|Briefly described|p23, p24.  |Proterozoic|Proterozoic|Intrudes the North Australian Craton. Is spatially associated with localised high-T, low-P granulite facies metamorphism in surrounding metasedimentary rocks. The authors propose this resulted from the accretion of the Warumpi Province onto the North Australian Craton, with consequent hairpin bend in the apparent polar wander path.|1635 +/- 9 Ma (Young et al. 1995).||||Largely gabbro and tonalite.|
21137|Andrew Young Igneous Complex|64722|6|Mentioned|p11|Statherian|Statherian|Intruded during the Liebig Event.|1640 - 1630 Ma.|||||11-APR-12
21137|Andrew Young Igneous Complex|65329|5|Briefly described|Map legend|Palaeoproterozoic|Palaeoproterozoic|Shown as older than Yaloolgarrie and Wabudali Granites, younger than Waluwiya Suite. Gabbronorite, hornblende-pyroxene tonalite, minor hornblende-biotite granite, orthopyroxene norite, olivine-bearing norite; high gravity and magnetic response;||||||
21137|Andrew Young Igneous Complex|65330|5|Briefly described|Map legend|Palaeoproterozoic|Palaeoproterozoic|Shown as older than Yaloolgarrie and Wabudali Granites, younger than Waluwiya Suite. Gabbronorite, hornblende-pyroxene tonalite, minor hornblende-biotite granite, orthopyroxene norite, olivine-bearing norite; high gravity and magnetic response;||||||
21137|Andrew Young Igneous Complex|65358|5|Briefly described|p11|Statherian|Statherian|Post-tectonic. Mafic to intermediate. Emplaced at ~1635 Ma.||||||
21137|Andrew Young Igneous Complex|66800|6|Mentioned|p929.|||Mentioned as an example of rocks with comparably low SiO2 (vis-a-vis Etheridge Group leucogabbro) containing cogenetic zircon (Young et al.1995).||||||11-MAY-12
21137|Andrew Young Igneous Complex|67323|5|Briefly described|p35|Paleoproterozoic|Paleoproterozoic|Arunta Inlier. See also Andrew Young Complex (Eastern Australia Time-Space Plot).|~1640 Ma.||||Orthopyroxene and olivine norite, gabbronorite, diorite, porphyritic biotite granite, anorthosite and calc-silicate rock.|
21137|Andrew Young Igneous Complex|67565|5|Briefly described|p3, p5 Fig.3, p48, p50, p64.|||Arunta Region. Includes large mafic igneous bodies which induced low-pressure granulite facies metamorphism in turbiditic metasedimentary rocks north of the Central Australian Suture. Strong magnetic response. Has high Ni-Cu-Co sulfide prospectivity. Intruded at a similar time to the Papunya Igneous Complex, but is geochemically distinct.||||||
21137|Andrew Young Igneous Complex|68150|5|Briefly described|p12|||Aileron Province.|1633 +/- 3 Ma, Claoue-Long and Hoatson 2005|||||
21137|Andrew Young Igneous Complex|68832|4|Described|p46-52, 23, 55|||Aileron Province, Arunta Region. SHRIMP U-Pb zircon geochronology.  Weakly foliated biotite syenogranite sampled. Crystallisation age given.|1640+/-6 Ma|||Intrudes Lander Rock beds.|Includes isolated outcrops of undeformed to weakly foliated porphyritic biotite granite that is interpreted to intrude at least some mafic phases of the Complex.|12-JAN-17
21137|Andrew Young Igneous Complex|68994|6|Mentioned|p5|||Emplaced in Aileron Province (Mount Rennie, Northern Territory) north of Central Australian Suture at 1640+/-6 Ma, with associated low-pressure, high-temperature metamorphism of host Nyirripi beds (Cross et al. 2005)|1640+/-6 Ma (intrusion).|||Intrudes Nyirripi beds.|Gabbronorite to tonalite intrusion.|13-JAN-17
21137|Andrew Young Igneous Complex|69427|5|Briefly described|p12:3, 5, 25, 40 Fig.12.34; 12:42, 59|Statherian|Statherian|Young et al. (1995). Andrew Young Hills, and small bouldery outcrops 5-10 km ENE of Sandy Blight Junction, Aileron Province. A complex of gabbronorite and mafic tonalite, with minor granite and aplite. Geochemistry suggests varying degrees of crustal contamination. Intrusion by this unit is associated with granulite-facies metamorphism of the Nyirripi beds. May have potential for Ni-Cu-Co sulfide mineralisation. SHRIMP U-Pb zircon ages by Claoue-Long and Hoatson (2005) and Young et al. (1995) respectively.|1633 +/- 5 Ma and 1635 +/- 9 Ma.||||Non-foliated, fine- to medium-grained gabbronorite, magnetite gabbronorite, biotite gabbronorite, gabbro, hornblende tonalite and diorite; also various norites, microdiorite, anorthosite and biotite granite.|12-JUL-16
21137|Andrew Young Igneous Complex|69428|6|Mentioned|p13:12|||Aileron Province. Synchronous with a period of extension (c.1633 Ma) which saw intrusion by the Ilpilli Dolerite in the Warumpi Province to the S.||||||12-JUL-16
21137|Andrew Young Igneous Complex|69508|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region, Aileron Province. Four un-named subunits are mapped separately.|||||Gabbronorite, hornblende-pyroxene tonalite, minor hornblende-biotite granite, orthopyroxene norite, olivine-bearing norite.|
21137|Andrew Young Igneous Complex|69937|5|Briefly described|p19|||Possible source of (some) zircons in the Olympic Formation.|~1635 Ma.|||||
21137|Andrew Young Igneous Complex|71348|6|Mentioned|p201|Calymmian|Statherian|Geological province: Aileron Province, Arunta Region.||||||
21137|Andrew Young Igneous Complex|71592|5|Briefly described|Appendix A.|||Arunta Orogen.|1640+/-5.9 Ma (U-Pb zircon: SHRIMP)||||Granite, gabbro.|
21137|Andrew Young Igneous Complex|72071|6|Mentioned|p1303|||Geological province: Arunta region. Mafic and felsic magmatism related to Isan Orogeny and accretion of Warumpi Province along eastern and southern margins of the North Australian Craton respectively.||||||
21137|Andrew Young Igneous Complex|72360|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Geological province: Aileron Province.|||||Porphyritic biotite granite; fine grained quartz diorite; undifferentiated norite, diorite and minor biotite granite, anorthosite and calc-silicate rock; orthopyroxene norite; olivine bearing norite and gabbronorite.|09-SEP-19
21137|Andrew Young Igneous Complex|72711|6|Mentioned|p6, p12.|||Formation related to mineralisation dated at c. ca 1670 Ma at Bumblebee and Grapple prospects. (Table 1; Reno et al 2018, Kositcin et al 2019, McGloin et al 2019a).|ca. 1670 Ma.|||||
21137|Andrew Young Igneous Complex|72894|5|Briefly described|piii, p5, p8, p10|Statherian|Statherian|Gabbronorite of the Andrew Young Igneous Complex has a SHRIMP U-Pb age of 1633 +/- 3 Ma (Claoue-Long and Hoatson, 2005)|ca 1635 Ma||||Undeformed/unmetamorphosed layered mafic igneous rock|
21141|Annaburroo Volcanic Member|50586|6|Mentioned|p6.1|||Of the Wildman Siltstone (Gerowie Suite). Geological Province: Pine Creek Inlier.||||||
21185|Balma Group|22479|5|Briefly described|fig4, pg10|Statherian|Statherian|||||||
21185|Balma Group|22538|4|Described|P710, Fig4, P717|Calymmian|Statherian|Part of the Glyde package.||||||20-DEC-06
21185|Balma Group|22600|4|Described|Map legend|Statherian|Statherian|||||||
21185|Balma Group|22808|6|Mentioned|7 fig 4|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
21185|Balma Group|23374|6|Mentioned|Fig3p5,6,34|||Of McArthur Basin.||||||20-JUL-06
21185|Balma Group|23937|5|Briefly described|p50 Fig. 26|||Part of the Glyde package of Rawlings (1999).  Geological Province: McArthur Basin.  See also p4 Fig. 4 and  p9.||||||27-OCT-04
21185|Balma Group|24047|5|Briefly described|p12 Fig. 10, p11|Paleoproterozoic|Paleoproterozoic|Age: 1670-1600Ma.  Together with the Habgood Group overlies the Parsons Range Group.  Geological Province: McArthur Basin.||||||07-NOV-08
21185|Balma Group|24048|2|Defined|p98 App.1|Mesoproterozoic|Paleoproterozoic|See also p52.  Proposer: P.W. Haines. Previously mapped as McArthur Group.  Overlain by Balbirini Dolomite.  Underlain by Fleming Sandstone.  Max. thickness: 4500m.  Geological Province: McArthur Basin||||||07-NOV-08
21185|Balma Group|24049|5|Briefly described|Map legend|Statherian|Statherian|Includes Bath Range, Baiguridji and Conway Formations, Yarrawirrie Formation (includes Ngilipitji Conglomerate Member), Zamia Creek and Koolatong Siltstones, Vaughton Siltstone, and Strawbridge Breccia. Geol. Prov: McArthur Basin.||||||13-OCT-05
21185|Balma Group|43292|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
21185|Balma Group|43645|6|Mentioned|p561|||U-Pb zircon age: 1599+/-11 Ma.||||||16-NOV-06
21185|Balma Group|44112|3|Fully described|p10,37,49,53-54|Statherian|Statherian|Part of Supersequence 3.||||||20-DEC-06
21185|Balma Group|60573|6|Mentioned|Regional Setting legend|Paleoproterozoic|Paleoproterozoic|Overlain by Nathan Group rocks.||||||07-NOV-08
21185|Balma Group|60574|5|Briefly described|Map Legend|||Geological Province: McArthur Basin.||||||
21185|Balma Group|61403|5|Briefly described|Map legend|Statherian|Statherian|Includes Bath Range, Baiguridji and Conway Formations, Yarrawirrie Formation (includes Ngilipitji Conglomerate Member), Zamia Creek and Koolatong Silt stones, Vaughton Siltstone, and Strawbridge Breccia. Geol. Prov: McArthur Basin.||||||
21185|Balma Group|63866|5|Briefly described|p114, p116, p123|||Isa Superbasin. Partially equivalent to the Vizard Group.|||Includes the Yarrawirrie Formation and the Bath Range Formation.|Conformably overlies the Parsons Range Group.|Evaporitic and stromatolitic dolostyone and fine-grained siliciclastic rocks.|
21185|Balma 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)||||||
21185|Balma Group|64817|6|Mentioned|p352 Fig.3, p353 Fig.4 ||||||Includes Bath Range Formation, Baiguridgi Formation, Yarrawirrie Formation, Zamia Creek Siltstone, Conway Formation, Vaughton Siltstone, Strawbridge Breccia, Koolatong Siltstone.|||
21185|Balma Group|65228|5|Briefly described|p18, p23|||c.1620 Ma. Evidence of fault-controlled sedimentation.||||Overlies Parsons Range Group.||
21185|Balma Group|65340|6|Mentioned|p10 Fig.5.|||||||||
21185|Balma Group|69417|6|Mentioned|p2:5|Statherian|Statherian|McArthur Basin.||||||12-JUL-16
21185|Balma Group|69421|6|Mentioned|p6:6|||McArthur Basin.||||||12-JUL-16
21185|Balma Group|69430|4|Described|p15:2-4, 13-14, 20-23|Statherian|Statherian|Haines (1994) used this term for units in the southern Walker Fault Zone originally mapped (Plumb and Roberts, 1965) as McArthur Group. The Group was defined by Haines et al. (1999), who preferred a correlation with the nearby Habgood Group rather than the McArthur Group. Northern McArthur Basin. Up to c.4.5 km thick. Shallow-water and locally evaporitic sediments. Has more siliciclastic, and less carbonate, sediments than McArthur Group. May correlate with Jalma Formation. There are two internal hiatuses. SHRIMP zircon ages of tuffaceous sediments (Haines et al., 1999). Ages of surrounding units also given.|1620 +/- 21 Ma; 1599 +/- 11 Ma.||Koolatong, Vaughton, Zamia Creek Siltstones; Strawbridge Breccia; Conway, Yarrawirrie, Baiguridgi, Bath Range Formations.|Conformably overlies Fleming Sandstone (Parsons Range Group). Locally  overlies conformably [?]  Donydji Group, and possibly unconformably by Balbirini Dolostone (Nathan Group).|A thick succession of mainly mudstone, carbonate and sandstone, with minor tuffaceous components in some Formations.|07-JUL-20
21185|Balma Group|69673|6|Mentioned|p3 fig 2, p15, p17, p46, p47|Mesoproterozoic|Paleoproterozoic|Walker Fault Zone|||Includes Bath Range Formation, Baiguridgi Formation, Yarrawirrie Formation, Zamia Creek Siltstone, Conway Formation, Vaughton Siltstone, Strawbridge Breccia, Koolatong Siltstone|||
21185|Balma Group|70968|6|Mentioned|p2 Fig.3|||||||||
21185|Balma Group|71059|6|Mentioned|p2|Paleoproterozoic|Paleoproterozoic|McArthur Basin.||||||
21185|Balma Group|71374|5|Briefly described|iii, p2, p12, p15, p26-p28, p30, p33|||northern McArthur Basin. May correlate with the Yarawoi Formation (Habgood Group).|||Includes the Yarrawirrie Formation, Vaughton Siltstone, Conway Formation and Zamia Creek Siltstone.|Overlain by the Nathan Group.||
21185|Balma Group|71606|5|Briefly described|p135,137-138|Statherian|Statherian|Central Walker Trough, McArthur Basin. Evaporite-carbonate sequence. Top of balma Group c. 1600 Ma.|||Includes Yarrawirrie Formation.|Overlain unconformably by Nathan Group. Underlain by Parsons Range Group. Correlable to Habgood Group and Vizard Formation.||
21185|Balma Group|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin. Informally subdivided into Lower, Middle and Upper parts.||||||04-MAR-20
21185|Balma Group|72373|5|Briefly described|iii,p1-2,6,9,11,15,17,24|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. Broadly equivalent to Glyde Package, McArthur and Vizard groups (McArthur Basin) and Limbunya group (Birrindude Basin).|||Includes Koolatong Siltstone, Strawbridge Breccia, Bath Range and Baiguridji formations.|Overlain by Nathan Group.||02-OCT-19
21185|Balma Group|72377|5|Briefly described|p13, 15|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. Rawlings et al (1997) suggested that Mount Bonner Sandstone may be an attenuated lateral facies variant of the Balma Group, deposited on the higher-relief flanks of the main depositional areas for this group.||||||10-OCT-19
21185|Balma Group|72718|6|Mentioned|p5 Tb.1|||McArthur Basin. Isa Superbasin of Jackson et al. (1999, 2000). Glyde package.||||||
21201|Bartalumba Basalt|22538|6|Mentioned|Fig3 P708|||||||||
21201|Bartalumba Basalt|22600|4|Described|Map legend|Statherian|Statherian|||||||
21201|Bartalumba Basalt|22808|2|Defined|32|Statherian|Statherian|Of Alyangula Subgroup. Max thickness 400 m. Overlying unit: Dalumbu Sandstone; underlying unit: Alyinga Sandstone||||||20-JUL-06
21201|Bartalumba Basalt|23018|6|Mentioned|p303|||||||||
21201|Bartalumba Basalt|23363|5|Briefly described|344 Fig.3|||||||||
21201|Bartalumba Basalt|23374|5|Briefly described|p14|||Equivalent to Nungbalgarri Volcanics. Geol. Prov:  McArthur Basin.||||||20-JUL-06
21201|Bartalumba Basalt|24047|5|Briefly described|p49|Paleoproterozoic|Paleoproterozoic|Vesicular and amygdaloidal basalt and microdiorite.  Conformably overlain by Dalumbu Sandstone; overlies Alyinga Sandstone;  also overlies Milyema Formation.  Max. thickness: 400m.  See also p50 Fig. 41.||||||07-NOV-08
21201|Bartalumba Basalt|24048|3|Fully described|p22|Paleoproterozoic|Paleoproterozoic|Of Alyangula Subgroup.  Max. thickness: 400m.  Geological Province: McArthur Basin.||||||07-NOV-08
21201|Bartalumba Basalt|24049|5|Briefly described|Map Legend|Statherian|Statherian|Of Alyangula Subgroup (Groote Eylandt Group). Basalt: amgdaloidal; micro-dolerite. Geol. Prov: McArthur Basin.||||||20-JUL-06
21201|Bartalumba Basalt|43292|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
21201|Bartalumba Basalt|43680|6|Mentioned|p303|||||||||
21201|Bartalumba Basalt|44112|6|Mentioned|Fig11p30|||||||||
21201|Bartalumba Basalt|61403|5|Briefly described|Map Legend|Statherian|Statherian|Of Alyangula Subgroup, Groote Eylandt Group. Basalt: amgdaloidal; micro-dolerite. Geol. Prov: McArthur Basin.||||||
21201|Bartalumba Basalt|63866|6|Mentioned|p117|||||||||
21201|Bartalumba Basalt|64817|5|Briefly described|p353 Fig.4, p355 Fig.5 |||Caledon Shelf South, McArthur Basin.||Of the Alyangula Subgroup.|||Mafic volcanics.|04-JUN-18
21201|Bartalumba Basalt|69430|4|Described|p15:3, 5-6|||NE McArthur Basin. 200-400m thick. Subaerial lava flows.||Alyangula Subgroup.||Conformably overlies Alyinga Sandstone. Is overlain conformably by Dalumbu Sandstone.|Deeply weathered, red and black, massive to vesicular and amygdaloidal basalt and microdolerite.|12-JUL-16
21201|Bartalumba Basalt|69455|6|Mentioned|p39:10|Paleoproterozoic|Paleoproterozoic|Groote Eylandt.||||||12-JUL-16
21201|Bartalumba Basalt|69673|6|Mentioned|p16 fig 13|||Northeastern McArthur Basin.||Alyangula Subgroup||Overlain by Dalumbu Sandstone, overlies Woodnah Sandstone, Anyinga Sandstone||
21201|Bartalumba Basalt|73083|6|Mentioned|p13|||Finely checkered dark grey and white magnetic appearance.||||||
21279|Boggy Hole Gneiss|24197|5|Briefly described|p61 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Of Madderns Yard Suite. Age: 1680Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
21279|Boggy Hole Gneiss|44114|6|Mentioned|p339||||1650 Ma (Zhao and Bennett, 1995).|||||
21279|Boggy Hole Gneiss|50369|5|Briefly described|p1.5, 19.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Madderns Yard Suite. Age: 1648 +/- 10Ma (SHRIMP).||||||06-JAN-12
21279|Boggy Hole Gneiss|69428|5|Briefly described|p13:2-4, 7|Paleoproterozoic|Paleoproterozoic|Eastern Haasts Bluff Domain, Warumpi Province. Youngest dated meta-igneous rock in the parent Complex: may be genetically distinct.|1648 +/- 10 Ma (SHRIMP U-Pb zircon).|Madderns Yard Metamorphic Complex.||Intruded by Ellery Granitic Complex.|Includes porphyritic garnet-bearing gneissic granite.|12-JUL-16
21279|Boggy Hole Gneiss|69925|5|Briefly described|p18, 21, 23, 25, 29-31|||Southern Arunta Province, Arunta Inlier. Probable basement to Chewings Range metasediments. Deformed and metamorphosed during the Chewings phase of the Aileron Event at 1585 +/- 70 Ma. Ion probe U-Pb isotope analyses tabulated.|1648 +/- 10 Ma (crystallisation).|||Is intruded by Stuart Dyke Swarm.|Quartzofeldspathic gneiss, porphyroblastic granitic gneiss, leucocratic gneiss and laminated granitic gneiss; all garnet-bearing.|
21279|Boggy Hole Gneiss|69931|6|Mentioned|p269, 273-274, 280, 296|Paleoproterozoic|Paleoproterozoic|Arunta Inlier. REE analyses, Sm-Nd isotopic analyses, tabulated. Is basement to Simpsons Gap Metasediments.||Boggy Hole Suite.|||Porphyritic granite.|
21279|Boggy Hole Gneiss|71592|5|Briefly described|Appendix A.|||Warumpi Province, Arunta Orogen.|1648+/-10 Ma (crystallisation: U-Pb zircon SHRIMP)||||Felsic gneiss.|
21329|Brinkley Bluff Gneiss|24197|5|Briefly described|p61 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Of the Iwupataka ?Suite (name presented on its own). Age: 1605Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
21329|Brinkley Bluff Gneiss|43225|5|Briefly described|Map Legend||Paleoproterozoic|Of the Iwupataka Metamorphic Complex.||||||07-NOV-08
21329|Brinkley Bluff Gneiss|43503|2|Defined|8,25,78|||||||||
21329|Brinkley Bluff Gneiss|50369|5|Briefly described|p1.5, 22.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Iwupataka Suite. Age: 1605 +/- 6Ma (Shrimp).||||||07-NOV-08
21329|Brinkley Bluff Gneiss|69428|5|Briefly described|p13:07|||Crops out within and along the N side of the Chewings Range.|||||Foliated biotite-rich granite.|12-JUL-16
21329|Brinkley Bluff Gneiss|69932|6|Mentioned|p302-303, 306-307|||Southern Province, Arunta Inlier. Sm-Nd data tabulated. Presented as Brinkley Granite Gneiss (p302), Brinkley Granitic Gneiss (p303, 306), and Brinkley Augen Gneiss (p309): all invalid names.|1605 Ma.||||Biotite-rich, fine-grained augen gneiss of adamellite composition.|
21342|Brumbreu Formation|23410|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Flynn Subgroup, Churchills Head Group. Lithic and volcanic arenite; heavy mineral-bearing quartz arenite; granule and pebble beds; felsic tuff. Arenite, fine to coarse grained; thin to medium bedded.||||||07-NOV-08
21342|Brumbreu Formation|23733|3|Fully described|p6, p4 Tb.1|Proterozoic|Proterozoic|Of the Flynn Group. Confomably overlies Wundirgi Formation, overlain by Hayward Creek Formation.||||||02-AUG-06
21342|Brumbreu Formation|23809|5|Briefly described|p27 Fig. 25|||Of the Flynn Group.  Geological Province: Tennant Inlier.||||||
21342|Brumbreu Formation|24172|2|Defined|p22, p7 Tb.1|Paleoproterozoic|Paleoproterozoic|Of the Flynn Subgroup. Conformably overlain by Hayward Creek Fm; conformably underlain by Wundirgi Formation. Geological Prov: Tennant Creek Inlier. Max.Thick.: 900m in type section. Originally the Warramunga Group, now included in the Flynn Subgroup.||||||07-NOV-08
21342|Brumbreu Formation|24294|5|Briefly described|p1168 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of the Flynn Subgroup (Churchills Head Group). Age: ~1860-1840 Ma. Geological Province: Tennant Creek Inlier.||||||07-NOV-08
21342|Brumbreu Formation|24303|5|Briefly described|p3|Proterozoic|Proterozoic|Of the Flynn Group. Overlain by the Tomkinson Creek Group.||||||
21342|Brumbreu Formation|43223|5|Briefly described|Map Legend||Paleoproterozoic|of Flynn Subgroup||||||07-NOV-08
21342|Brumbreu Formation|43224|5|Briefly described|Map legend||Proterozoic|of Flynn Subgroup||||||
21342|Brumbreu Formation|50353|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Flynn Group. Lithic volcanic arenite; heavy mineral-bearing quartz arenite; granule and pebble beds; felsic tuff. Arenite, fine to course grained; thin to medium bedded.||||||07-NOV-08
21342|Brumbreu Formation|60684|4|Described|p11, p6 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Flynn Subgroup (Churchills Head Group). Lithic arenite and volcanic litharenite; magnetite-bearing qtz arenite; granule,pebble beds; felsic tuff (chert). Conformable(transitional) below Hayward Creek Formation and over Wundirgi Formation.||||||07-NOV-08
21342|Brumbreu Formation|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Ooradidgee Group.  Lithic/volcanilithic arenite; heavy mineral-bearing sandstone; felsic tuff. Overlies the Wundirgi Formation. In Tennant Creek region.||||||07-NOV-08
21342|Brumbreu Formation|65209|5|Briefly described|p35 Fig.1, p36|Paleoproterozoic|Paleoproterozoic|||Ooradidgee Group.||Conformable and apparently transitional over Wundirgi Formation.||05-JAN-17
21342|Brumbreu Formation|65338|6|Mentioned|p19.|||May partly fill the time interval between first and second felsic volcanic episodes of this Group, i.e. c.1840 - 1810 Ma.||Unit in Ooradidgee Group.||||
21342|Brumbreu Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Tennant Creek/Davenport area.||Ooradidgee Group.||||
21342|Brumbreu Formation|69187|5|Briefly described|p53 Fig.2, p54 Fig.3|||Warramunga Province.||Ooradidgee Group||||
21342|Brumbreu Formation|69424|4|Described|p9:3, 5, 14-16, 19,22,26,28, 39 Fig.9.24|Paleoproterozoic|Paleoproterozoic|Warramunga Province. c.600-1500m thick [?text is inconsistent: states on 9:19 it is 900m thick at type section, which is the same comment for Bernborough Formation]. Marginal marine to fluviatile. Minimum age from un-named monzodiorite/dolerite sills.|>1821 +/- 8 Ma.|Ooradidgee Group.||Conformably (transitionally) overlies Wundirgi Formation. Is overlain conformably (locally unconformably or faulted) by Hayward Creek Formation.|Lithic and volcanilithic sandstone; magnetite-bearing quartz sandstone; granule and pebble beds; felsic tuff (chert); sandstone is fine- to coarse-grained and thinly to medium bedded.|12-JUL-16
21342|Brumbreu Formation|69431|6|Mentioned|p16:4, 6-7|||||Ooradidgee Group.||Is overlain by Manga Mauda Member (Hayward Creek Formation) conformably, disconformably and unconformably.||12-JUL-16
21342|Brumbreu Formation|72379|5|Briefly described|p5|Paleoproterozoic|Paleoproterozoic|Geological province: Warramunga Province.||||||
21342|Brumbreu Formation|73124|6|Mentioned|p2 Fig.1|||||Ooradidgee Group||Underlain by Wundirgi Formation.||
21342|Brumbreu Formation|73125|5|Briefly described|p2|Palaeoproterozoic|Palaeoproterozoic|Warramunga Province.||Ooradidgee Group.||||
21342|Brumbreu Formation|73460|6|Mentioned|p2|||Warramunga Province.||Ooradidgee Group||Underlain by Wundirgi Formation and Bernborough Formation.||
21342|Brumbreu Formation|73590|6|Mentioned|p2|||||Ooradidgee Group||Underlain by Wundirgi Formation and Bernborough Formation.||
21352|Buger Creek Granite|43631|3|Fully described|p14,15||Paleoproterozoic|Age: approx. 1780.||||||07-NOV-08
21356|Bukudal Granite|22538|6|Mentioned|P713|||||||||
21356|Bukudal Granite|22600|4|Described|Map legend|Orosirian|Orosirian|||||||
21356|Bukudal Granite|22808|6|Mentioned|5|||Geol. province: Arnhem Inlier.||||||02-AUG-06
21356|Bukudal Granite|24048|3|Fully described|p13|Mesoproterozoic|Paleoproterozoic|Previously included in the Myaoola and Caledon Granites.  Intrudes the Bradshaw Complex.  Age: 1840Ma.  Geological Province: Arnhem Inlier.||||||07-NOV-08
21356|Bukudal Granite|24049|5|Briefly described|Map Legend|Orosirian|Orosirian|Granite: massive, white to pink, medium to coarse-grained, equigranular, granophyric, fayalite-bearing; miarolitic cavities and mafic clots; intruded by microgranite dykes and sills. Geol. Prov: McArthur Basin, Arnhem Inlier.||||||13-OCT-05
21356|Bukudal Granite|24197|5|Briefly described|p29, p54|Paleoproterozoic|Paleoproterozoic|Of the Giddy Suite. Geological Province: Arnhem Block.||||||07-FEB-11
21356|Bukudal Granite|43292|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
21356|Bukudal Granite|44112|2|Defined|p1,7,13,23-24||Orosirian|Max Age: 1835-37 (+/-) 4 Ma. Replaces 'Caledon Granite'.||||||02-AUG-06
21356|Bukudal Granite|50591|5|Briefly described|p1.3, 3.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Of the Giddy Suite. Geological Province: Arnhem Block/McArthur Basin. Age: 1837-1835 +/- 4Ma (Shrimp).||||||07-NOV-08
21356|Bukudal Granite|61403|5|Briefly described|Map Legend|Orosirian|Orosirian|Granite: massive, white to pink, medium to coarse-grained, equigranular, granophyric, fayalite-bearing; miarolitic cavities and mafic clots; intruded by microgranite dykes and sills. Geol. Prov: McArthur Basin, Arnhem Inlier.||||||
21356|Bukudal Granite|63866|4|Described|p115|Orosirian|Orosirian|Arnhem Inlier, Northern Caledon Shelf.|1836 +/- 5 Ma; 1835 +/- 4 Ma (Page, OZCHRON)|Giddy Suite|||A-type granites.|
21356|Bukudal Granite|69421|4|Described|p6:1-3, 5-7|Orosirian|Orosirian|Rawlings et al. (1997), who revised the Giddy and Caledon Granites of Dunnet (1965): the latter being superseded. Arnhem Province. Coeval with Garrthalala and Giddy Granites. Geochemistry briefly described.|1837 +/- 4 Ma (SHRIMP U-Pb zircon).|Giddy Suite.||Intrudes Grindall Formation and Bradshaw Complex.|Granite, massive, white to pink, equigranular, medium- to coarse-grained; contains fayalite; locally sheared; distinctive reddened spherical inclusions. High-level emplacement: has miarolitic cavities and granophyric intergrowths. A-type.|12-JUL-16
21356|Bukudal Granite|69430|6|Mentioned|p15:5-6|||||||Is overlain unconformably by Woodah Sandstone.||12-JUL-16
21356|Bukudal Granite|70719|4|Described|iv, p1, p5, p13-15, p17, p24|Orosirian|Orosirian|Exposed over a wide area in eastern Arnhem Province as boulders and tors. Three previous SHRIMP U-Pb zircon ages between 1835 Ma and 1837 Ma (all by Page, 1996).|1825 +/- 5 Ma (magmatic crystallisation age)|Giddy Suite.||Intrudes Grindall Formation and Bawaka granite. Correlated with Giddy, Garrthalala and Dhalinybuy Granites.|Coarse-grained, equigranular, unmetamorphosed fayalite-bearing biotite granite. A-type.|06-FEB-18
21356|Bukudal Granite|71374|6|Mentioned|p24|||Arnhem Province.|c. 1825 Ma|||||
21356|Bukudal Granite|71592|5|Briefly described|Appendix A.|||Arnhem Province.|1836+/-4 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
21356|Bukudal Granite|71606|5|Briefly described|p135|Paleoproterozoic|Paleoproterozoic|McArthur Basin. Based on field relationships, likely to be older, at least pre-dating upper Groote Eylandt Group.||||||
21356|Bukudal Granite|71620|6|Mentioned|p11|||Arnhem Province. A sample now recognised as Melville Bay Metamorphics was previously assigned to this unit.||||||
21402|Bustard Subgroup|22538|6|Mentioned|P714, Fig3 P208|||||||||
21402|Bustard Subgroup|22600|4|Described|Map legend|Orosirian|Orosirian|||||||
21402|Bustard Subgroup|22808|2|Defined|29|Orosirian|Orosirian|Arnhem Inlier||||||
21402|Bustard Subgroup|24047|5|Briefly described|p12 Fig. 10|Paleoproterozoic|Paleoproterozoic|Age: ~1800Ma.  Geological Province: McArthur Basin.||||||07-NOV-08
21402|Bustard Subgroup|24048|3|Fully described|p15|Statherian|Orosirian|Of the Groote Eylandt Group.  Geological Province: McArthur Basin||||||02-AUG-06
21402|Bustard Subgroup|24049|5|Briefly described|Map Legend|Orosirian|Orosirian|Of Groote Eylandt Group. Includes Milyakburra Formation, Milyema Formation,Bickerton Rhyolite, Abarungkwa Sandstone, and Erringkarri Rhyolite. Geol. Prov: McArthur Basin.||||||13-OCT-05
21402|Bustard Subgroup|43292|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
21402|Bustard Subgroup|44112|4|Described|p10|||Part of Supersequence 1(A)||||||
21402|Bustard Subgroup|50591|6|Mentioned|p3.2|||Geological Province: Arnhem Block/McArthur Basin.||||||
21402|Bustard Subgroup|61403|5|Briefly described|Map Legend|Orosirian|Orosirian|Of Groote Eylandt Group. Includes Milyakburra Formation, Milyema Formation,Bickerton Rhyolite, Abarungkwa Sandstone, and Erringkarri Rhyolite. Geol. Prov: McArthur Basin.||||||02-AUG-06
21402|Bustard Subgroup|63866|4|Described|p115|Orosirian|Orosirian|Leichhardt/Calvert Superbasin. Age constrained by a crystallisation age for the Bickerton Rhyolite.||Groote Eylandt Group|Includes the Bickerton Rhyolite.|||
21402|Bustard Subgroup|64817|5|Briefly described|p353 Fig.4, p355 Fig.5, p367 Tb.2 |||Caledon Shelf South, McArthur Basin.|1820-1790 Ma.|Of the Groote Eylandt Group.|Includes the Milyakburra and Milyema Formations; Bickerton and Erringkarri Rhyolite; and Abarungkwa Sandstone.||Felsic volcanics, sandstone and conglomerate.|04-JUN-18
21402|Bustard Subgroup|69430|4|Described|p15:3-5|||NE McArthur Basin.|1815 Ma.|Groote Eylandt Group.|Erringkarri, Bickerton Rhyolites; Abarungkwa Sandstone; Milyakburra, Milyema Formations.|Is overlain disconformably by Alyangula Subgroup.|Fluvial sandstone, conglomerate and subaerial felsic volcanic rocks.|12-JUL-16
21402|Bustard Subgroup|69673|6|Mentioned|p16 fig 13|Orosirian|Orosirian|Northeastern McArthur Basin.|1815 Ma|Groote Eylandt Group|Includes Milyakburra Formation, Milyema Formation, Bickerton Rhyolite, Abarungkwa Sandstone, Erringkarri Rhyolite|||
21402|Bustard Subgroup|71606|5|Briefly described|p137|Statherian|Orosirian|South Caledon Shelf, McArthur Basin.||Unit of Groote Eylandt Group.||Lower unit of Groote Eylandt Group. Overlain conformably to unconformably by Alyangula Subgroup. Underlain by Arnhem Granites.||
21402|Bustard Subgroup|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.||Lower Groote Eylandt Group.|||Lithic and quartzose sandstone, conglomerate; rhyolitic volcanics.|04-MAR-20
21470|Cato Volcanics|22538|6|Mentioned|Fig3 P708||Statherian|Age of unit is 1717+/-11 Ma.||||||03-AUG-06
21470|Cato Volcanics|22600|4|Described|Map legend|Statherian|Statherian|||||||
21470|Cato Volcanics|23363|5|Briefly described|352 Tab.3|Statherian|Statherian|Age: 1717+/-11Ma.||||||03-AUG-06
21470|Cato Volcanics|24048|5|Briefly described|p14 Fig. 5|||Geological Province: McArthur Basin.||||||
21470|Cato Volcanics|24049|5|Briefly described|Map Legend|Statherian|Statherian|Of Spencer Creek Group. Rhyolite: pink to brown, porphyritic with phenocrysts of K-feldspar, quartz, plagioclase and pyroxene. Geol. Prov: McArthur Basin.||||||12-OCT-05
21470|Cato Volcanics|44112|2|Defined|p44,47-48,105||Statherian|Max Age: 1717 (+/-) 11 Ma||||||
21470|Cato Volcanics|50591|5|Briefly described|p1.3, 4.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Of the Fagan Supersuite. Geological Province: Arnhem Block/McArthur Basin. Age: 1717 +/- 11Ma (SHRIMP).||||||06-JUN-18
21470|Cato Volcanics|61403|5|Briefly described|Map Legend|Statherian|Statherian|Of Spencer Creek Group. Rhyolite: pink to brown, porphyritic with phenocrysts of K-feldspar, quartz, plagioclase and pyroxene. Geol. Prov: McArthur Basin.||||||06-JUN-18
21470|Cato Volcanics|63866|5|Briefly described|p114-p117|Statherian|Statherian|Northern Caledon Shelf.|1717 +/- 10 Ma (Page, OZCHRON)|||Unconformably overlain by the Rorruwuy Sandstone and the Mount Bonner Sandstone. Potentially equivalent ot the Parsons Range Group.||
21470|Cato Volcanics|64817|6|Mentioned|p353 Fig.4, p355 Fig.5 |Statherian|Statherian|Caledon Shelf North, McArthur Basin.|1717+/-11 Ma|Of the Spencer Creek Group.||||
21470|Cato Volcanics|69430|5|Briefly described|p15:3|||NE McArthur Basin.|1717 +/- 11 Ma.|Spencer Creek Group.||||12-JUL-16
21470|Cato Volcanics|69673|6|Mentioned|p16 fig 13|||Northeastern McArthur Basin.|1717 +/- 11 Ma|Spencer Creek Group||Overlies Yuduyudu Formation||
21470|Cato Volcanics|71592|5|Briefly described|Appendix A.|||Caledon Shelf, Arnhem Province.|1717+/-11 Ma (crystallisation: U-Pb zircon SHRIMP)||||Dacite.|
21470|Cato Volcanics|72377|5|Briefly described|p12|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. Page (1996d) reported SHRIMP U-Pb zircon age of 1717+\-11 Ma, interpreted as magmatic crystallisation age, which is within uncertainty with the magmatic crystallisation age of the Haddon Volcanics (1712+\-12 Ma; this record).|1717+\-11 Ma (magmatic)|Unit of Spencer Creek Group.||||
21509|Coast Range Sandstone|22538|6|Mentioned|P715|||Part of the Goyder package||||||
21509|Coast Range Sandstone|22600|4|Described|Map legend|Statherian|Statherian|||||||
21509|Coast Range Sandstone|22808|6|Mentioned|7 fig 4|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
21509|Coast Range Sandstone|23374|5|Briefly described|Fig3p5||Paleoproterozoic|of McArthur Basin.||||||07-NOV-08
21509|Coast Range Sandstone|24048|3|Fully described|p99 App. 1|Statherian|Statherian|See also p50.  Proposer: P.W. Haines.  Overlain by Jalma Formation; underlain by Grindall Formation.  Previously mapped as trhe former "Groote Eylandt Beds".  Max. Thickness: 40m.||||||
21509|Coast Range Sandstone|24049|5|Briefly described|Map Legend|Statherian|Statherian|Quartz sandstone: white, medium to coarse-grained, thick-bedded, commonly pebbly: lenticular basal pebble or cobble conglomerate. Geol. Prov: McArthur Basin.||||||13-OCT-05
21509|Coast Range Sandstone|43292|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
21509|Coast Range Sandstone|44112|6|Mentioned|p10,98|||||||||
21509|Coast Range Sandstone|60573|6|Mentioned|Regional Setting legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
21509|Coast Range Sandstone|61403|5|Briefly described|Map Legend|Statherian|Statherian|Quartz sandstone: white, medium to coarse-grained, thick-bedded, commonly pebbly: lenticular basal pebble or cobble conglomerate. Geol. Prov: McArthur Basin.||||||
21509|Coast Range Sandstone|63866|5|Briefly described|p114, p116|||Isa Superbasin. Partially equivalent to the Vizard Group.||||Conformably overlies the Parsons Range Group. Unconformably overlain by the Jalma Formation.|Evaporitic and stromatolitic dolostyone and fine-grained siliciclastic rocks.|
21509|Coast Range Sandstone|64817|6|Mentioned|p353 Fig.4|||||||||
21509|Coast Range Sandstone|69430|4|Described|p15:3, 7, 13-14|Statherian|Statherian|Haines et al. (1999). Previously, most outcrops were mapped (Plumb and Roberts, 1965) as part of the Groote Eylandt beds (now Groote Eylandt Group). NE McArthur Basin. 20-40m thick. High-energy transgressive deposit with some fluvial facies. Possible equivalent to Parsons Range Group.||||Unconformably overlies Grindall Formation, Bradshaw Complex, and apparently Gadabara Volcanics and Woodah Sandstone. Is overlain unconformably by Jalma Formation.|White, medium- to coarse-grained, thickly bedded quartz sandstone, commonly pebbly; lenticular basal pebble or cobble conglomerate.|12-JUL-16
21509|Coast Range Sandstone|69673|6|Mentioned|p16 fig 13|||Possibly equivalent to Parsons Range Group.||||||
21509|Coast Range Sandstone|71374|3|Fully described|iii, p1 tbl 1, p24-p27, p55-p56|Statherian|Statherian|McArthur Basin. The type section occurs between 590500mE 8518000mN and 590200mE 8518000mN across the northern part of the Coast Range (Haines et al, 1999). SHRIMP age is interpreted as the maximum depositional age for this formation. Based on age is interpreted as a probable correlative of the Parsons Range Group. Sampling site provided along with zircon description and SHRIMP analytical discussion. Age correlated with the Parsons Range Group.|1670 +/- 10 Ma (SHRIMP U-PB)|||Unconformably overlies the Alyangula Subgroup (Groote Eylandt Group). Unconformably overlain by the Jalma Formation.|Fine-grained quartz sandstone.|
21509|Coast Range Sandstone|71605|5|Briefly described|p19, p35|||McArthur Basin. SHRIMP age interpreted as a maximum depositional age of this unit and derived from Kositicin et al, in press.|1670 +/- 10 Ma (SHRIMP U-Pb)|||Unconformably overlies the Gadabara Volcanics.||
21509|Coast Range Sandstone|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.|||||Quartzose sandstone, conglomerate.|
21509|Coast Range Sandstone|72377|4|Described|iii,p1,6-7,10-11,13|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. Type section: Located between 590500mE, 8518000mN and 590200mE, 8518000mN across the northern part of the Coast Range (Haines et al 1999). Exposures restricted to northeastern BLUE MUD BAY mapsheet. intruded by thin NW-trending mafic dykes along the central Coast Range (Haines et al 1999). Kositcin et al (2017) reported interpreted maximum depositional age of 1670+\-10 Ma (SHRIMP U-Pb zircon dating). Sample BM16TJM029 (fine-grained quartz sandstone; 588160E 8510265N): MC-LA-ICP-MS zircon Hf studies yielded dominant age populations between c. 1868 to c. 1838 Ma with Hf isotope values consistent with zircons of the same age from Arnhem Province basement.|1670+\-10 Ma (max dep age)|||Overlain by Jalma Formation. Underlain unconformably by Gadabara Volcanics or Haddon Volcanics or Alyangula Subgroup/Groote Eylandt Group.|Lenticular basal conglomerate, middle unit of lenticular, pebbly, coarse-grained sandstone to granule conglomerate, and upper unit of medium to thickly bedded, fine- to coarse-grained sandstone.|
21611|Dalumbu Sandstone|22538|6|Mentioned|Fig3 P708|||||||||
21611|Dalumbu Sandstone|22600|4|Described|Map legend|Statherian|Statherian|||||||
21611|Dalumbu Sandstone|22808|2|Defined|32|Statherian|Statherian|Of the Alyangula Subgroup. Max thickness 1000 m.||||||08-AUG-06
21611|Dalumbu Sandstone|23018|6|Mentioned|p303||Proterozoic|||||||
21611|Dalumbu Sandstone|24047|5|Briefly described|p49|Paleoproterozoic|Paleoproterozoic|Well-jointed, cross-bedded quartz arenite, dominating rock outcrops on Groote Eylandt.  Conformably overlies Bartalumba Basalt.  Max. thickness: 1000m.  See also p12 Fig. 10 and p50 Fig. 41.||||||07-NOV-08
21611|Dalumbu Sandstone|24048|3|Fully described|p22|Paleoproterozoic|Paleoproterozoic|Of Alyangula Subgroup.  Max. thickness: 1000m.  Geological Province: McArthur Basin.||||||07-NOV-08
21611|Dalumbu Sandstone|24049|5|Briefly described|Map Legend|Statherian|Statherian|Of Alyangula Subgroup, Groote Eylandt Group. Sandstone: white, coarse-grained, cross-bedded, pebbly (mainly quartz), granule lenses, quartz-rich; sandstone: white to pink, medium-grained, cross-bedded, quartz-rich. Geol. Prov: McArthur Basin.||||||13-OCT-05
21611|Dalumbu Sandstone|43292|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
21611|Dalumbu Sandstone|43680|5|Briefly described|p303||Proterozoic|||||||
21611|Dalumbu Sandstone|44112|6|Mentioned|Fig11p30|||||||||
21611|Dalumbu Sandstone|60573|5|Briefly described|Map legend|Orosirian|Orosirian|Of the Groote Eylandt Group.  Quartz sandstone: white, coarse-grained, pebbly, local granule lenses; white to pink quartz sandstone, medium-grained, cross-bedded.||||||
21611|Dalumbu Sandstone|61403|5|Briefly described|Map Legend|Statherian|Statherian|Of Alyangula Subgroup, Groote Eylandt Group. Sandstone: white, coarse-grained, cross-bedded, pebbly (mainly quartz), granule lenses, quartz-rich; sand stone: white to pink, medium-grained, cross-bedded, quartz-rich. Geol. Prov: McArthur Basin.||||||
21611|Dalumbu Sandstone|64817|6|Mentioned|p353 Fig.4, p355 Fig.5 |||Caledon Shelf South, McArthur Basin.||Of the Alyangula Subgroup.||||
21611|Dalumbu Sandstone|69430|4|Described|p15:3, 5|||NE McArthur Basin. 500-1000m thick exposure. Mostly braided fluvial, with minor marine incursion, deposits; thin subaerial basalt lava flow.||Alyangula Subgroup.||Conformably overlies Bartalumba Basalt.|White, coarse-grained, cross-bedded, pebbly (mainly quartz) quartz-rich sandstone with granule lenses; white to pink, medium-grained, cross-bedded quartz-rich sandstone; basalt, very weathered and ferruginised.|12-JUL-16
21611|Dalumbu Sandstone|69455|6|Mentioned|p39:10-13|Paleoproterozoic|Paleoproterozoic|Groote Eylandt. Forms a series of WNW-trending ridges.||||||12-JUL-16
21611|Dalumbu Sandstone|69673|6|Mentioned|p16 fig 13|||Northeastern McArthur Basin.||Alyangula Subgroup||Overlies Bartalumba Basalt||
21620|Dashwood Gabbro Complex|43225|5|Briefly described|Map Legend||Mesoproterozoic|Of Arunta Block.||||||08-AUG-06
21620|Dashwood Gabbro Complex|43503|2|Defined|8,26,80|||||||||
21620|Dashwood Gabbro Complex|69428|5|Briefly described|p13:05|||Warren and Shaw (1995). Southwest of Mount Ziel. Undated.||||Intrudes the Glen Helen Metamorphics.|Altered gabbro, dolerite and ultramafic rocks surrounded by leucocratic rocks that are interpreted as locally derived melt.|12-JUL-16
21635|Delaney Mudstone Member|43565|5|Briefly described|p424-440|||||||||
21635|Delaney Mudstone Member|43748|5|Briefly described|Table 1|||Locally developed. ?Equivalent to Claraville Mudstone Member (shown in same stratigraphic position& with same description and map symbol, see p10)||Of Hale Formation.|||Olive green mudstone and siltstone.|07-OCT-15
21635|Delaney Mudstone Member|69458|5|Briefly described|p42:7-8|||Claraville Sub-basin, eastern Hale Basin.||Hale Formation.||Conformably overlies Ambalindum Sandstone Member. Lateral equivalent of Ulgnamba Lignite Member.|Olive-green mudstone and siltstone.|12-JUL-16
21653|Dhalinybuy Granite|22538|6|Mentioned|P715||Orosirian|||||||
21653|Dhalinybuy Granite|22600|4|Described|Map legend|Orosirian|Orosirian|||||||
21653|Dhalinybuy Granite|24048|6|Mentioned|p8|||Geological Province: Arnhem Inlier.||||||
21653|Dhalinybuy Granite|24049|5|Briefly described|Map Legend|Orosirian|Orosirian|Granite: pink to green, medium to coarse-grained, equigranular to porphyritic, locally sheared and foliated, local mylonite. Geol. Prov: McArthur Basin, Arnhem Inlier.||||||09-AUG-06
21653|Dhalinybuy Granite|24197|5|Briefly described|p29|Paleoproterozoic|Paleoproterozoic|Of the Giddy Suite. Geological Province: Arnhem Block.||||||07-FEB-11
21653|Dhalinybuy Granite|43292|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
21653|Dhalinybuy Granite|44112|2|Defined|p1,7,13,25,105|Statherian|Statherian|Max Age: ~1870 Ma; Min Age: ~1710 Ma||||||
21653|Dhalinybuy Granite|50591|5|Briefly described|p3.1|Paleoproterozoic|Paleoproterozoic|Of the Giddy Suite. Geological Province: Arnhem Block/McArthur Basin. See also Dhalinbuy Granite.||||||07-NOV-08
21653|Dhalinybuy Granite|61403|5|Briefly described|Map Legend|Orosirian|Orosirian|Granite: pink to green, medium to coarse-grained, equigranular to porphyritic, locally sheared and foliated, local mylonite. Geol. Prov: McArthur Basi n, Arnhem Inlier..||||||
21653|Dhalinybuy Granite|69421|4|Described|p6:1-3, 6-7|Orosirian|Orosirian|Rawlings et al. (1997), who revised the Giddy and Caledon Granites of Dunnet (1965): the latter being superseded. Arnhem Province. Exposed as rounded tors and boulders. Undated; a minimum age of c.1710 Ma is from the overlying Yanungbi Volcanics.|c.1835 Ma.|Giddy Suite.||?Intrudes Bradshaw Complex. Is intruded by Yanungbi Volcanics. Is overlain unconformably or nonconformably by Yanungbi Volcanics or Gove Sandstone (Spencer Creek Group).|Granite, pink to green, medium- to coarse-grained, equigranular to K-feldspar porphyritic; variably deformed from massive to locally sheared and foliated, to local proto-mylonite.|12-JUL-16
21653|Dhalinybuy Granite|70302|6|Mentioned|p7|||Arnhem Province.||||Is overlain unconformably by Yanungbi Volcanics.||
21653|Dhalinybuy Granite|70719|6|Mentioned|p13, p15|||||||Correlated with Bukudal, Giddy Granites.||
21654|Dhunganda Formation|22538|5|Briefly described|P715||Statherian|||||||
21654|Dhunganda Formation|22600|4|Described|Map legend|Statherian|Statherian|||||||
21654|Dhunganda Formation|23363|5|Briefly described|344 Fig.3|||||||||
21654|Dhunganda Formation|24048|3|Fully described|p23|Statherian|Paleoproterozoic|Of Donydji Group.  Includes the lower half of former "Ritarango beds".  Max. thickness: >500m.  Geological Province: McArthur Basin.||||||07-NOV-08
21654|Dhunganda Formation|24049|5|Briefly described|Map Legend|Statherian|Statherian|Of Donydji Group. Mudstone and fine-grained sandstone; felsic, mafic and minor hybrid igneous rocks; volcaniclastic breccia, conglomerate and sandstone; sheared rocks. Geol. Prov: McArthur Basin.||||||21-OCT-05
21654|Dhunganda Formation|44112|2|Defined|p10,31-32,34,106|Statherian|Orosirian|Part of Supersequence 1(C). Max Age: ~1870 Ma; Min Age: ~1710 Ma||||||
21654|Dhunganda Formation|50591|5|Briefly described|p5.1|Paleoproterozoic|Paleoproterozoic|Of the Donydji Group.  Geological Province: Arnhem Block/McArthur Basin.||||||07-NOV-08
21654|Dhunganda Formation|61403|5|Briefly described|Map Legend|Statherian|Statherian|Of Donydji Group. Mudstone and fine-grained sandstone; felsic, mafic and minor hybrid igneous rocks; volcaniclastic breccia, conglomerate and sandston e; sheared rocks. Geol. Prov: McArthur Basin.||||||21-OCT-05
21654|Dhunganda Formation|63866|5|Briefly described|p114, p117|||Leichhardt/Calvert Superbasins. Mistakenly called the Dhonganda Formation on p114.||Donydji Group||Unconformably overlain by the Ritarango Formation and the Fagan Volcanics. Equivalent to the Katherine River Group and the Woodah Sandstone.||
21654|Dhunganda Formation|64817|6|Mentioned|p353 Fig.4, p355 Fig.5 |||Walker Fault Zone, McArthur Basin.||Of the Donydji Group.||||
21654|Dhunganda Formation|65340|6|Mentioned|p92.|||Northern McArthur Basin. Tentatively correlated with Aquarium Formation on the basis of similar lithofacies.||||||
21654|Dhunganda Formation|69421|6|Mentioned|p6:3 Tb.6.1|||McArthur Basin.||Donydji Group.||Probably overlies unconformably the Mirarrmina Complex.||12-JUL-16
21654|Dhunganda Formation|69430|4|Described|p15:3, 6-7|Statherian|Statherian|Walker Fault Zone, northern McArthur Basin. Over 500m thick. Lower part fluvial to shallow-water deltaic deposits; upper part ranges from alluvial to moderately deep-water lacustrine deposits.||Donydji Group.||Overlies Mirarrmina Complex apparently unconformably. Is overlain by Ritarango Formation possibly unconformably.|Strongly deformed sandstone, mudstone, felsic-mafic-hybrid igneous rocks, volcaniclastic rocks.|12-JUL-16
21654|Dhunganda Formation|69673|6|Mentioned|p16 fig 13|||||Donydji Group||||
21654|Dhunganda Formation|72377|4|Described|iii,p1,8-9|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. Minimum age constraint is provided by interpreted volcanic ages from two samples of rhyolite (c. 1706 Ma) in the overlying Fagan Volcanics (Page 1996a,b). Sample AB15AWE013 (altered felsic volcanic rock; 561150E 8596380N): LA-ICP-MS zircon dating yielded 1726+\-6 Ma, representing timing of volcanism. Likely time-equivalent with Wollogorang Formation.|1726+\-6 Ma (magmatic)|Unit of Donydji Group.||Overlain unconformably by Ritarango Formation. Underlain unconformably by Mirrarrmina Complex.|Lower sandstone overlain by an upper recessive package with intervals of mudstone and sandstone, felsic, mafic and hybrid igneous rocks, and volcaniclastic and sheared rocks.|07-OCT-19
21655|Dhupuwamirri Member|22538|6|Mentioned|Fig3 P708||Statherian|Age of unit is 1706+/-10 Ma.||||||09-AUG-06
21655|Dhupuwamirri Member|22600|4|Described|Map legend|Statherian|Statherian|||||||
21655|Dhupuwamirri Member|23363|5|Briefly described|344 Fig.3|Statherian|Statherian|Age: ~1707Ma.||||||09-AUG-06
21655|Dhupuwamirri Member|24048|3|Fully described|p32|Statherian|Statherian|Of the Fagan Volcanics.  Age: 1706+/-10Ma (SHRIMP U-Pb).  Max. thickness: 450m.  Geological Province: McArthur Basin.||||||09-AUG-06
21655|Dhupuwamirri Member|24049|5|Briefly described|Map Legend|Statherian|Statherian|Of Fagan Volcanics, Donydji Group. Rhyolite: porphyritic with phenocrysts of K-feldspar, quartz and albite, massive to flow banded; volcaniclastic mudstone, sandstone and breccia; dolerite, basalt and hybrid rocks. Geol. Prov: McArthur Basin.||||||13-OCT-05
21655|Dhupuwamirri Member|44112|2|Defined|p29,31,41-43,106|Statherian|Statherian|Max Age: 1706 (+/-) 10 Ma.||||||09-AUG-06
21655|Dhupuwamirri Member|61403|5|Briefly described|Map Legend|Statherian|Statherian|Of Fagan Volcanics, Donydji Group. Rhyolite: porphyritic with phenocrysts of K-feldspar, quartz and albite, massive to flow banded; volcaniclastic mud stone, sandstone and breccia; dolerite, basalt and hybrid rocks. Geol. Prov: McArthur Basin.||||||
21655|Dhupuwamirri Member|64817|6|Mentioned|p353 Fig.4 |Statherian|Statherian||1706 +/- 10 Ma.|Of the Fagan Volcanics.||||
21655|Dhupuwamirri Member|69430|4|Described|p15:3, 6-7, 13|Statherian|Statherian|Walker Fault Zone, northern McArthur Basin. 450-550m thick. Shallow-water, low-energy sediments; extrusive and high-level intrusive igneous rocks. SHRIMP U-Pb zircon age.|1706 +/- 10 Ma (Page et al., 2000).|Fagan Volcanics.||Conformably overlies Sheridan Member. Is overlain conformably by Mattamurta Sandstone.|Rhyolite; volcaniclastic mudstone, sandstone and breccia; dolerite, basalt and hybrid igneous rocks.|12-JUL-16
21655|Dhupuwamirri Member|69673|6|Mentioned|p16 fig 13|||||Fagan Volcanics||Overlain by Mattamurta Sandstone, overlies Sheridan Member||
21655|Dhupuwamirri Member|72377|5|Briefly described|p8,12, 19|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. Page (1996 a,b; discussed in Rawlings et al 1997) reported SHRIMP 207Pb/206Pb zircon age of 1706+\-10 Ma, interpreted to record timing of volcanism in the Donydji Group.|1706+\-10 Ma (Pb/Pb; volcanism)|Unit of Fagan Volcanics.|||Rhyolite.|10-OCT-19
21680|Donydji Group|22479|5|Briefly described|fig4, pg10|Statherian|Statherian|||||||
21680|Donydji Group|22538|4|Described|Fig4, p710, p714|Statherian|Statherian|||||||04-MAY-18
21680|Donydji Group|22600|4|Described|Map legend|Statherian|Statherian|||||||
21680|Donydji Group|22808|6|Mentioned|7 fig 4|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
21680|Donydji Group|23374|5|Briefly described|Fig3 p5,6,34||Paleoproterozoic|Of the McArthur Basin.||||||04-MAY-18
21680|Donydji Group|23937|5|Briefly described|p4 Fig. 4|||Part of the Redbank package of Rawlings (1999).  Geological Province: McArthur Basin.||||||27-OCT-04
21680|Donydji Group|24048|3|Fully described|p23|Statherian|Paleoproterozoic|Previously informally referred to as "Mitchell Ranges Formation" and "Cypress Creek Formation".  Max. thickness: 3000m.  Geological Province: McArthur Basin||||||07-NOV-08
21680|Donydji Group|24049|5|Briefly described|Map Legend|Statherian|Statherian|Includes Fagan Volcanics (including Dhupuwamirri Member, Sheridan Member, and Maidjunga Member), Ritarango Formation, and Dhunganda Formation. Geol. Prov: McArthur Basin.||||||13-OCT-05
21680|Donydji Group|43292|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
21680|Donydji Group|44112|3|Fully described|p10,11,29,31,43,107|Statherian|Orosirian|Poorly constrained Max Age: ~1870 Ma; Min Age: ~1710 Ma. Part of Supersequence 1||||||
21680|Donydji Group|50591|6|Mentioned|p5.1|||Includes: Dhunganda Formation.||||||
21680|Donydji Group|60573|6|Mentioned|Regional Setting legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
21680|Donydji Group|60574|5|Briefly described|Map Legend|||Geological Province: McArthur Basin.||||||
21680|Donydji Group|61403|5|Briefly described|Map Legend|Statherian|Statherian|Includes Fagan Volcanics (including Dhupuwamirri Member, Sheridan Member, and Maidjunga Member), Ritarango Formation, and Dhunganda Formation. Geol. P rov: McArthur Basin.||||||
21680|Donydji Group|63866|5|Briefly described|p112, p114, p123|||Walker Fault Zone.|||Includes the Dhonganda Formation, Ritarango Formation and the Fagan Volcanics.|Unconformably overlies the Mirrarrmina Complex. Conformably overlain by the Parsons Range Group. Equivalent to the Katherine River Group.|Coarse-grained siliciclastic rocks and bimodal volcanics.|
21680|Donydji Group|64817|6|Mentioned|p352-355 Figs.3,4,5; p367 Tb.2 |||Walker Fault Zone, McArthur Basin.|||Includes Fagan Volcanics, Ritarango Formation and Dhunganda Formation.|||
21680|Donydji Group|65337|6|Mentioned|p15.|||McArthur Basin. Resembles Mitchiebo Volcanics.||||||
21680|Donydji Group|65340|6|Mentioned|p7.|||Walker Fault Zone, McArthur Basin. Contemporaneous with Tawallah, Katherine River and Spencer Creek Groups.||||||
21680|Donydji Group|67323|5|Briefly described|Eastern Australia Time-Space Plot|||McArthur region.|1706 +/- 10 Ma.|||||
21680|Donydji Group|69417|6|Mentioned|p2:5|Statherian|Statherian|McArthur Basin.||||||12-JUL-16
21680|Donydji Group|69421|6|Mentioned|p6:3 Tb.6.1, 6:5-6|||McArthur Basin.|||Fagan Volcanics, Dhunganda Formation.|||12-JUL-16
21680|Donydji Group|69430|4|Described|p15:2-4, 6-7, 13-14, 22|Statherian|Statherian|Walker Fault Zone, northern McArthur Basin. Crops out only in the Mitchell Ranges. Thickness probably 2000-3000m; calculation is complicated by structural repetition of some Formations. A localised episode of wrench faulting and thrusting has caused significant ductile and brittle deformation. An age of 1710 Ma (Rawlings et al., 1997) is also given.|>1706 +/- 10 Ma.||Dhunganda, Ritarango Formations; Fagan Volcanics.|Inferred to overlie unconformably the Mirarrmina Complex. Is overlain conformably by the Parsons Range Group and (locally) Balma Group.|A succession of dominantly fluviatile to shallow-water, coarse-grained, siliciclastic sedimentary rocks with felsic and mafic igneous rocks.|12-JUL-16
21680|Donydji Group|69673|6|Mentioned|p3 fig 2, p15,p16 fig 13, p17 |Statherian|Statherian||1710 Ma||Includes Fagan Volcanics, Ritarango Formation, Dhuganda Formation|Overlain by Parsons Range Group||
21680|Donydji Group|70968|6|Mentioned|p2 Fig.3|||||||||
21680|Donydji Group|71059|6|Mentioned|p2|Paleoproterozoic|Paleoproterozoic|McArthur Basin.||||||
21680|Donydji Group|71374|6|Mentioned|p2, p24|||northern McArthur Basin.|||Includes the Fagan Volcanics.|Broadly equivalent to the Tawalah Group.||
21680|Donydji Group|71606|5|Briefly described|p135,137|Statherian|Statherian|Central Walker Trough, McArthur Basin. Lower part of Donydji Group probabyl represent attenuated equivalent of main Tawallah Group.|||Includes Fagan Volcanics and Latram Granite and Ritarango beds.|Overlain by Parsons Range Group. Underlain unconformably by Mirarrmina Complex.||
21680|Donydji Group|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.|||||Lithic and quartzose sandstone, mudstone; minor conglomerate; synsedimentary rhyolitic sills and volcanics with minor basalt; dolerite sills and dykes.|
21680|Donydji 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).||||||
21680|Donydji Group|72377|5|Briefly described|iii,p8-9, 19|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin.|||Includes Dhunganda Formation and Fagan Volcanics.|||10-OCT-19
21680|Donydji Group|72718|6|Mentioned|p5 Tb.1|||McArthur Basin. Calvert/Leichhardt Superbasin of Jackson et al. (1999, 2000). Redbank package.||||||
21695|Drimmie Head Granite|22600|4|Described|Map legend|Orosirian|Orosirian|||||||
21695|Drimmie Head Granite|24047|5|Briefly described|p75 Fig. 60|Paleoproterozoic|Paleoproterozoic|Of the Bradshaw Complex.  Geological Province: Carpentaria Basin.||||||07-NOV-08
21695|Drimmie Head Granite|24048|5|Briefly described|p10|||Of Bradshaw Complex.  Geological Province: Arnhem Inlier.||||||09-AUG-06
21695|Drimmie Head Granite|24049|5|Briefly described|Map Legend|Orosirian|Orosirian|Leucogranite: cordierite-garnet-bearing, white, medium to coarse-grained, massive and foliated; granulite facies metasedimentary and mafic enclaves. Geol. Prov: McArthur Basin, Arnhem Inlier.||||||13-OCT-05
21695|Drimmie Head Granite|44112|2|Defined|p13,18-20,107||Orosirian|Previously known as 'Drimmie Head type'. Max Age: 1867 (+/-) 12 Ma.||||||28-NOV-22
21695|Drimmie Head Granite|50591|5|Briefly described|p1.3, 2.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Of the Bradshaw Suite. Geological Province: Arnhem Block/McArthur Basin.||||||07-NOV-08
21695|Drimmie Head Granite|61403|5|Briefly described|Map Legend|Orosirian|Orosirian|Leucogranite: cordierite-garnet-bearing, white, medium to coarse-grained, massive and foliated; granulite facies metasedimentary and mafic enclaves. G eol. Prov: McArthur Basin, Arnhem Inlier.||||||
21695|Drimmie Head Granite|69421|4|Described|p6:2-4|||Rawlings et al. (1997). NE Arnhem Province. Exposed as sheets and plutons. A syn-metamorphic leucogranite probably derived from inhomogeneous melting of a metasedimentary protolith including the Melville Bay Metamorphics, which it intrudes.|1867 +/- 12 Ma.|Bradshaw Complex.||Intrudes Melville Bay Metamorphics.|Garnetiferous leucogranite and granitic gneiss, medium- to coarse-grained, massive to foliated; abundant enclaves including psammitic and pelitic gneiss, calc-silicate hornfels and mafic granulite.|12-JUL-16
21695|Drimmie Head Granite|69455|6|Mentioned|p39:7 Fig.39.8|Paleoproterozoic|Paleoproterozoic|Part of the basement in the Gove area (Arnhem Province).||||||12-JUL-16
21695|Drimmie Head Granite|70719|4|Described|iv, p1, p7-10, p21|Orosirian|Orosirian|Bremer Island and Melville Bay area. The type locality is Drimmie Head Peninsula in northern GOVE sheet area. Crops out as sheets and plutons. Derived by partial melting of Melville Bay Metamorphics. Previous age determination was 1867 +/- 12 Ma (Page, 1995).|1862 +/- 4 Ma (magmatic crystallisation age)|||Intrudes Melville Bay Metamorphics.|Cordierite-garnet (S-type) leucogranite with variable amounts of biotite and occasional feldspar megacrysts, and abundant xenoliths of granulite-facies metasedimentary and mafic rocks.|06-FEB-18
21695|Drimmie Head Granite|71592|5|Briefly described|Appendix A.|||Arnhem Province.|1862+/-4 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
21695|Drimmie Head Granite|71605|5|Briefly described|iii, p9, p12, p25||Orosirian|Arnhem Province. S-type granite, interpreted to have been derived from the sedimentary rocks that were metamorphosed to the Melville Bay Metamorphics.|1862 +/- 4 Ma, SHRIMP U-Pb, Kositicin et al 2015a|||Intrudes the Melville Bay Metamorphics.|Garnet-cordierite-biotite granite.|
21695|Drimmie Head Granite|71620|4|Described|iv, p6-p7, p13, p16, p18, p22-p23, p28|Orosirian|Orosirian|Arnhem Province. SHRIMP age interpreted as the igneous crystallisation age of this unit. LA-ICPMS ages from Reno et al (2017) include 1886 +/- 9 Ma and 1873 +/- 9 Ma and are interpreted to record melt-formation and crystallisation of this unit. Derived from melting of the Melville Bay Metamorphics.|1862 +/- 4 Ma (SHRIMP Pb/Pb Kositcin et al, 2015)||||S-type granite.|28-NOV-22
21695|Drimmie Head Granite|72365|4|Described|iii,p1,6-7,12-14,20,25-27,29,31-33,36|Orosirian|Orosirian|Geological province: Arnhem Province. Exposed as sheets and plutons around Melville Bay and on Gove Peninsula in the northeast Arnhem Province. Type locality: in situ boulders and tors located at Drimmie Head Peninsula in northern GOVE. Syn-metamorphic leucogranite (S-type granite) formed from partial melts of Melville Bay Metamorphics between c. 1880 Ma and ca. 1859 Ma (see Summary section for references). Includes xenoliths of garnet-cordierite migmatitic gneiss that resemble the Melville Bay Metamorphics. Previous geochron analysis include 1867+\-12 Ma (Page et al., 1995) and 1862+\-4 (Kositcin et al 2015) as interpreted crystallisation ages. Sample GV14SKR033 (granite; 684611E 8649840N) yields two ages: 1886+\-9 Ma, interpreted to record timing of zircon growth during initial melt formation; and 1873+\-9 Ma, interpreted as granite crystallisation age. Garnets formed as a solid product from intial melting of Melville Bay Metamorphics, and then entrained in the melt during migration within and extraction from Melville Bay Metamorphics. Overlain by Cretaceous and Cenozoic sediments and Quaternary alluvium.||||Intrudes Melville Bay Metamorphics.|Garnetiferous leucogranite with abundant xenoliths of granulite-facies metasedimentary and mafic rocks.|09-JAN-20
21695|Drimmie Head Granite|72377|5|Briefly described|p10|Paleoproterozoic|Paleoproterozoic|Geological province: Arnhem Province. Interpreted to be co-magmatic with Bawaka Granite, and Orunyah Granite.|c. 1862 Ma|||||
21715|Durabudboi beds|22538|6|Mentioned|Fig3 P708|||||||||
21715|Durabudboi beds|22600|4|Described|Map legend|Calymmian|Calymmian|||||||
21715|Durabudboi beds|23374|5|Briefly described|Fig3p5|Mesoproterozoic|Paleoproterozoic|Of McArthur Basin.||||||07-NOV-08
21715|Durabudboi beds|24048|6|Mentioned|p5 Fig. 3|||||||||
21715|Durabudboi beds|24049|5|Briefly described|Map Legend|Calymmian|Statherian|Mudstone: laminated, weathered, yellow, purple and white, probably dolomitic at depth; minor chert (silicified carbonate) and leached carbonate: relict stromatolite, arenite and evaporite textures. Geol. Prov: McArthur Basin.||||||13-OCT-05
21715|Durabudboi beds|44112|2|Defined|p67,107-108||Paleoproterozoic|||||||07-NOV-08
21715|Durabudboi beds|61403|5|Briefly described|Map Legend|Calymmian|Statherian|Mudstone: laminated, weathered, yellow, purple and white, probably dolomitic at depth; minor chert (silicified carbonate) and leached carbonate: relic t stromatolite, arenite and evaporite textures. Geol. Prov: McArthur Basin.||||||
21715|Durabudboi beds|63866|5|Briefly described|p116-p117|||||||Unconformably overlies the Rorruwuy Sandstone. Equivalent to the Mount Bonner Sandstone.||
21715|Durabudboi beds|69430|5|Briefly described|p15:3, 14, 23|||NE McArthur Basin. These rocks were previously assigned to the Cretaceous succession. It was suggested that these rocks may be part of the lower Roper Group.||||Is overlain by the Roper Group. Is correlated with the Habgood Group.|Mainly laminated mudstone and minor dolomitic rocks.|12-JUL-16
21715|Durabudboi beds|71374|4|Described|iii, p1 tbl 1, p33-p35, p61-p62|Calymmian|Calymmian|McArthur Basin. Informal name. SHRIMP age is interpreted as the maximum depositional age. Possible musgrave zircon provenenance. A reference locality of Haines and Pietsch in Rawlings et al (1997) is mentioned. Sampling site provided along with zircon description and SHRIMP analytical discussion.|1571 +/- 14 Ma (SHRIMP U-Pb)||||Weathered and ferruginised, thinly bedded, laminated and flaggy mudstone which was probably originally dolomitic, minor leached and silicified carbonate rock and rare fine-grained sandstone.|
21715|Durabudboi beds|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.|||||Dolomitic mudstone; minor stromatolitic-evaporitic chert.|
21753|Erringkarri Rhyolite|22538|6|Mentioned|Fig3 P708|||||||||
21753|Erringkarri Rhyolite|22600|4|Described|Map legend|Orosirian|Orosirian|||||||
21753|Erringkarri Rhyolite|22808|2|Defined|29|Orosirian|Orosirian|Of the Bustard Subgroup. Overlying unit Abarungkwa Sandstone||||||16-AUG-06
21753|Erringkarri Rhyolite|23363|5|Briefly described|344 Fig.3|||||||||
21753|Erringkarri Rhyolite|24048|3|Fully described|p15|Statherian|Orosirian|Rhyolite, dark red, variably porphyritic (K-feldspar).  Of the Bustard Group.  Max. thickness: >20m.  Geological Province: McArthur Basin.||||||16-AUG-06
21753|Erringkarri Rhyolite|24049|5|Briefly described|Map Legend|Orosirian|Orosirian|Of Bustard Subgroup, Groote Eylandt Group. Rhyolite: dark red, variably porphyritic (K-feldspar). Geol. Prov: McArthur Basin.||||||13-OCT-05
21753|Erringkarri Rhyolite|43292|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
21753|Erringkarri Rhyolite|44112|6|Mentioned|Fig11p30|||||||||
21753|Erringkarri Rhyolite|50591|5|Briefly described|p5.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arnhem Block/McArthur Basin. Of the Bickerton Suite. Unconformably overlies: Giddy Suite.||||||07-NOV-08
21753|Erringkarri Rhyolite|61403|5|Briefly described|Map Legend|Orosirian|Orosirian|Of Bustard Subgroup, Groote Eylandt Group. Rhyolite: dark red, variably porphyritic (K-feldspar). Geol. Prov: McArthur Basin.||||||
21753|Erringkarri Rhyolite|64817|5|Briefly described|p353 Fig.4, p355 Fig.5 |||Caledon Shelf South, McArthur Basin. Age is of whole Bustard Subgroup.|1820-1790 Ma|Of the Bustard Subgroup.|||Felsic volcanics.|04-JUN-18
21753|Erringkarri Rhyolite|69430|4|Described|p15:3, 5|||NE McArthur Basin. Over 20m thick. Large subaerial domes and coulees. A short period of weathering and erosion preceded burial.||Bustard Subgroup.||Inferred to overlies Grindall Formation unconformably. Is overlain by Abarungkwa Sandstone ?disconformably.|Dark red, variably K-feldspar-phyric rhyolite; locally aphanitic.|12-JUL-16
21753|Erringkarri Rhyolite|69673|6|Mentioned|p16 fig 13|||Northeastern McArthur Basin.||Bustard Subgroup||Overlain by Abarungkwa Sandstone||
21755|Ethel Creek Granite|43275|5|Briefly described|Map Legend||Mesoproterozoic|Of Southwark Granite Suite.||||||18-SEP-06
21755|Ethel Creek Granite|43631|3|Fully described|p15|||Palaeoproterozoic or Mesoproterozoic||||||
21755|Ethel Creek Granite|44158|4|Described|p20 Table.1|Mesoproterozoic|Mesoproterozoic|Of Southwark Granitic Suite. Age: Probably around 1570Ma. Intrudes Lander Rock beds.||||||05-MAY-10
21755|Ethel Creek Granite|61385|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Arunta Complex. Sparsely megacrystic biotite granite.||||||20-OCT-05
21755|Ethel Creek Granite|65329|5|Briefly described|Map legend|Palaeoproterozoic|Palaeoproterozoic|Of Southwark Granite Suite. Shown as older than Vaughan Springs Quartzite, younger than Yaloolgarrie and Wabudali Granites. Sparsely megacrystic muscovite-biotite granite; low gravity response; low to moderate granitic magnetic response [Mesoproterozoic is missing from map key]||||||19-DEC-12
21755|Ethel Creek Granite|65330|5|Briefly described|Map legend|Palaeoproterozoic|Palaeoproterozoic|Of Southwark Granite Suite. Shown as older than Vaughan Springs Quartzite, younger than Yaloolgarrie and Wabudali Granites. Sparsely megacrystic muscovite-biotite granite; low gravity response; low to moderate granitic magnetic response [Mesoproterozoic is missing from map key]||||||19-DEC-12
21755|Ethel Creek Granite|69427|5|Briefly described|p12:44|||Young et al. (1995). Immediately N of Ngalia Basin, Aileron Province.||Southwark Suite.||||12-JUL-16
21824|Gadabara Volcanics|22538|6|Mentioned|P713, Table1||Statherian|Part of the Redbank package.||||||19-SEP-06
21824|Gadabara Volcanics|22600|4|Described|Map legend|Statherian|Statherian|||||||
21824|Gadabara Volcanics|23363|5|Briefly described|344 Fig.3|||||||||
21824|Gadabara Volcanics|24048|2|Defined|p99|Statherian|Statherian|See also p36.  Previously included as part of "Bickerton Volcanics".  Max. thickness: 50m.  Geological Province: McArthur Basin.||||||
21824|Gadabara Volcanics|24049|5|Briefly described|Map Legend|Statherian|Statherian|Felsic igneous rock: pink to brown, coherent and banded; volcanic breccia. Geol. Prov: McArthur Basin.||||||13-OCT-05
21824|Gadabara Volcanics|24050|6|Mentioned|p30|||||||||
21824|Gadabara Volcanics|43292|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
21824|Gadabara Volcanics|44112|6|Mentioned|p43,49,73|||||||||
21824|Gadabara Volcanics|50591|5|Briefly described|p1.3, Table 1.1|Paleoproterozoic|Paleoproterozoic|Of the Fagan Supersuite. Geological Province: Arnhem Block/McArthur Basin.||||||07-NOV-08
21824|Gadabara Volcanics|61403|5|Briefly described|Map Legend|Statherian|Statherian|Felsic igneous rock: pink to brown, coherent and banded; volcanic breccia. Geol. Prov: McArthur Basin.||||||
21824|Gadabara Volcanics|63866|5|Briefly described|p114-p115, p117|||Southern Caledon Shelf. Misspelt as the Gadabra Volcanics on p117.||||Overlies the Woodah Sandstone.||
21824|Gadabara Volcanics|64817|6|Mentioned|p353 Fig.4, p355 Fig.5|||Caledon Shelf Central/South, McArthur Basin.||||Shown as equivalent to Cato Volcanics.||06-JUN-18
21824|Gadabara Volcanics|67779|6|Mentioned|p32.|||Northeastern Arnhem Land. Included by Rawlings (1999) in his Redbank Package, with Katherine River Group, Spencer Creek Group, Donji Group, Groote Eylandt Group and Tawallah Group.||||||
21824|Gadabara Volcanics|69430|4|Described|p15:3, 7, 13|Statherian|Statherian|NE McArthur Basin. 50m thick. High-energy, braided fluviatile deposits: shallow-marine in the upper part.||||Disconformably overlies and intrudes Woodah Sandstone. Is overlain unconformably by Coast Range Sandstone.|Felsic igneous rock; volcanic sandstone and breccia.|12-JUL-16
21824|Gadabara Volcanics|71605|5|Briefly described|iv, p1, p35|||Arnhem Province. Intrudes all units of the Arnhem Province, including unnamed units. Disconformably overlies the Woodah Sandstone. Unconformably overlain by the Coast Range Sandstone.||||Intrudes the Wonga Orthogneiss, Melville Bay Metamorphics, Bawaka Granite, Drimmie Head Granite, Bradshaw Complex and the Grindall Formation.|Fine-grained, porphyritic to glomerophyric rhyolite.|
21824|Gadabara Volcanics|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.|||||Alkaline intermediate volcanics.|
21824|Gadabara Volcanics|72377|5|Briefly described|iii,p1,9-10|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. Intrudes into all units of the Arnhem Province, including Melville Bay Metamorphics and Grindall Formation. Interpreted to be correlable with Yanungbi Volcanics (Rawlings et al., 1997). Sample BM16KAW076 (quartz-bearing trachyte; 631900E 8535045N): LA-ICP-MS zircon dating was not possible because no zircon was found in sample. Age constrained by overlying Coast Range Sandstone (max dep age  1670+/-10 Ma); underlying Woodah Sandstone (max.dep. age 1815+/-13 Ma); and intrusion into unnamed pegmatite (1807+/-11 Ma).||||Overlain unconformably by Coast Range Sandstone. Underlain unconformably by, and intrudes into Woodah Sandstone.||09-OCT-19
21856|Glen Helen Metamorphics|1490|6|Mentioned|p7-8, 10-11|||Migmatitic basement to Southern Province of the Arunta Inlier. New U-Th-Pb analyses and age determinations tabulated.|1660 +/- 4 Ma.|||Is intruded by Teapot granitoid.|Foliated, highly migmatised felsic gneiss of tonalitic composition.|
21856|Glen Helen Metamorphics|7837|6|Mentioned|p94|||||||||
21856|Glen Helen Metamorphics|24197|5|Briefly described|p61 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Of Madderns Yard Suite. Age: 1680Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
21856|Glen Helen Metamorphics|24608|6|Mentioned|p986|||||||||
21856|Glen Helen Metamorphics|43225|5|Briefly described|Map Legend||Paleoproterozoic|Of Madderns Yard Metamorphic Complex.||||||07-NOV-08
21856|Glen Helen Metamorphics|43503|2|Defined|7, 21, 77|||Dated at 1660-1680 Ma.||||||19-SEP-06
21856|Glen Helen Metamorphics|44114|5|Briefly described|p321|||Southern Arunta Inlier. Felsic magmatic rocks.|1680 Ma (Black and Shaw, 1995).||||Banded quarzofeldspathic gneisses, minor amphibolite.|
21856|Glen Helen Metamorphics|50369|5|Briefly described|p1.5, 19.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Madderns Yard Suite. Age: 1660-1680 +/- 13Ma (U-Pb, Sm-Nd, Shrimp).||||||07-NOV-08
21856|Glen Helen Metamorphics|60674|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Madderns Yard Metamorphic Complex.  Felsic migmatite, strained biotite granite, amphibolite, minor pelitic metasediment.||||||07-NOV-08
21856|Glen Helen Metamorphics|61518|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Felsic migmatite, strained biotite granite, amphibolite, minor metasediment, moderatly magnetic. Of the Madderns Yard Metamorphic Complex. Geological Province: Haasts Bluff Domain.||||||07-NOV-08
21856|Glen Helen Metamorphics|61660|4|Described|p3, p4, p10, pp13-18, p23.   |Proterozoic|Proterozoic|Haasts Bluff Domain. These SHRIMP U-Pb zircon ages are interpreted as magmatic (Black and Shaw, 1992, 1995). An igneous protolith sample has an age of 1688 +/- 16 Ma.|1678 +/- 6 Ma and 1663 +/- 13 Ma.|Unit in Madderns Yard Metamorphic Complex.|||Upper amphibolite facies migmatitic orthogneiss and rare metapelites.|
21856|Glen Helen Metamorphics|64809|6|Mentioned|p13 Fig.13|||||||||
21856|Glen Helen Metamorphics|65272|6|Mentioned|p318 fig 2.|||Haasts Bluff Domain.||||||
21856|Glen Helen Metamorphics|67565|4|Described|pp4-8, p11, pp27-28, p29, p31, p34.|Paleoproterozoic|Paleoproterozoic|Haasts Bluff Domain, Warumpi Province. Upper amphibolite facies from the 1640-1635 Ma Liebig Orogeny. Metamorphic effects and geochemistry are detailed. Kinny (2002) provides a second age (similar method) of 1661 +/- 8 Ma.|1688 +/- 16 Ma (SHRIMP U-Pb zircon).|Unit in Madderns Yard Metamorphic Complex.|||Felsic migmatitic orthogneiss, foliated granite, rare amphibolite, pelite, psammite; biotite-sillimanite +/- garnet pelite, psammite, minor amphibolite.|
21856|Glen Helen Metamorphics|68832|5|Briefly described|p14-19, 26|Statherian|Statherian|Warumpi Province, Arunta Region. SHRIMP U-Pb zircon geochronology. Biotite granodiorite sampled. Crystallisation age given. Previous ages for other samples of this unit: 1688+/-16 Ma (Kinny 2002), 1660+/-4 Ma (Black and Shaw 1992) and 1678+/-6 Ma (Black and Shaw 1995), all crystallisation ages.|1661+/-8 Ma|||Relationship with nearby Ikuntji Metamorphics unclear.|Migmatitic felsic orthogneiss, with abundant porphyritic biotite granite, and less common metasedimentary rock and amphibolite.|
21856|Glen Helen Metamorphics|69428|4|Described|p13:2, 4-5, 7, 14, 16, 18|Paleoproterozoic|Paleoproterozoic|Warren and Shaw (1995), Scrimgeour et al. (2005). Eastern Haasts Bluff Domain, Warumpi Province. Formerly included metasedimentary rocks hosting the Stokes Yard base metal prospect; now reassigned to the Iwupataka Metamorphic Complex. SHRIMP U-Pb protolith core zircon. Metamorphism during the Liebig Orogeny is briefly described. Metamorphic zircon rim overgrowths are dated at c.1660 Ma. Various other ages are given.|1688 +/- 16 Ma (Scrimgeour et al., 2005).|Madderns Yard Metamorphic Complex.||Is intruded by Dashwood Gabbro Complex, Cumming Leucogabbro, Ormiston Pound Granite, Teapot Granite Complex.|Biotite-bearing migmatitic felsic orthogneiss, with abundant porphyritic biotite granite, and less common metasedimentary rock and amphibolite.|12-JUL-16
21856|Glen Helen Metamorphics|69932|6|Mentioned|p302-303, 306-307, 310|||Southern Province, Arunta Inlier. Part of the basement. Sm-Nd data tabulated. Migmatised c.1660 Ma and c.1136 Ma.|1678 +/- 6 Ma (Black and Shaw, 1995).||||Migmatised, foliated tonalitic gneiss. Probably a metavolcanic complex.|
21856|Glen Helen Metamorphics|71592|5|Briefly described|Appendix A.|||Warumpi Province, Arunta Orogen.|1678+/-6 Ma (crystallisation: U-Pb zircon SHRIMP)||||Felsic gneiss.|
21894|Gove Sandstone|22538|6|Mentioned|Fig3 P708|||||||||
21894|Gove Sandstone|22600|4|Described|Map legend|Statherian|Statherian|||||||
21894|Gove Sandstone|24048|5|Briefly described|p36|||Of Spencer Creek Group.||||||21-SEP-06
21894|Gove Sandstone|24049|5|Briefly described|Map Legend|Statherian|Statherian|Of Spencer Creek Group. Sandstone: white to pink, fine to very coarse-grained, quartzose, locally common quartz pebbles, trough cross-bedded. Geol. Prov: McArthur Basin.||||||12-OCT-05
21894|Gove Sandstone|44112|2|Defined|p25,46-47,108-109||Statherian|Part of Supersequence 1(C). Max Age: ~1710 Ma||||||
21894|Gove Sandstone|61403|5|Briefly described|Map Legend|Statherian|Statherian|Of Spencer Creek Group. Sandstone: white to pink, fine to very coarse-grained, quartzose, locally common quartz pebbles, trough cross-bedded. Geol. Pr ov: McArthur Basin.||||||
21894|Gove Sandstone|64817|6|Mentioned|p353 Fig.4, p355 Fig.5 |||Caledon Shelf North, McArthur Basin.||Of the Spencer Creek Group.||Shown as base of Spencer Creek Group in Fig5, underlain by Yanungbi Volcanics in Fig 4. Overlain by Yuduyudu Formation.|Shown as sandstone and conglomerate.|06-JUN-18
21894|Gove Sandstone|69421|6|Mentioned|p6:6|||||Spencer Creek Group.||Overlies Dhalinybuy Granite.||12-JUL-16
21894|Gove Sandstone|69430|6|Mentioned|p15:3|||NE McArthur Basin.||Spencer Creek Group.||||12-JUL-16
21894|Gove Sandstone|69673|6|Mentioned|p16 fig 13|||Northeastern McArthur Basin.||Spencer Creek Group||Overlain by Yuduyudu Formation, overlies Yanungbi Volcanics, Latram Granite||
21914|Grindall Formation|22479|5|Briefly described|fig4, pg10|Orosirian|Orosirian|||||||
21914|Grindall Formation|22538|6|Mentioned|P713|||||||||
21914|Grindall Formation|22600|4|Described|Map legend|Orosirian|Orosirian|||||||
21914|Grindall Formation|22808|2|Defined|28|Paleoproterozoic|Paleoproterozoic|Geol province Arnhem Inlier||||||07-NOV-08
21914|Grindall Formation|23374|5|Briefly described|Fig3p5||Paleoproterozoic|||||||07-NOV-08
21914|Grindall Formation|24048|3|Fully described|p8|Paleoproterozoic||Originally named "Grindall Metamorphics".  Intruded by Bradshaw Complex and Bukudal Granite. Max. thickness: >1000m.  Geological Province: Arnhem Inlier.||||||07-NOV-08
21914|Grindall Formation|24049|5|Briefly described|Map Legend|Orosirian|Orosirian|Sandstone: red-brown to grey-green, fine to medium-grained, thin to thick-bedded, graded; interbedded with red-brown to grey-green mudstone. Locally metamorphosed. Geol. Prov: McArthur Basin, Arnhem Inlier.||||||13-OCT-05
21914|Grindall Formation|43292|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
21914|Grindall Formation|44112|3|Fully described|p7,13,98|Orosirian||Thought to be at least a partial protolith for the Bradshaw Complex.||||||21-SEP-06
21914|Grindall Formation|60573|6|Mentioned|Regional Setting legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
21914|Grindall Formation|61403|5|Briefly described|Map Legend|Orosirian|Orosirian|Sandstone: red-brown to grey-green, fine to medium-grained, thin to thick-bedded, graded; interbedded with red-brown to grey-green mudstone. Locally metamorphosed. Geol. Prov: McArthur Basin, Arnhem Inlier.||||||
21914|Grindall Formation|63866|5|Briefly described|p115, p117|||Arnhem Inlier, Northern Caledon Shelf.||||Intruded by the Bradshaw Complex.|Turbiditic sedimentary rocks.|
21914|Grindall Formation|69417|5|Briefly described|p2:5|Orosirian|Orosirian|Arnhem Orogen.||||Is intruded by Bradshaw Complex.||12-JUL-16
21914|Grindall Formation|69421|4|Described|p6:1-5|||Originally Grindall Metamorphics (Plumb and Roberts, 1992). Arnhem Province. Turbidite-dominated. Thickness estimated at over 1000m. Minimum age (intrusion). Lithologically similar to Burrell Creek Formation.|>1837 +/- 4 Ma.|||Is intruded by Bradshaw Complex and Bukudal Granite. Correlated tentatively with Burrell Creek Formation.|A deformed and locally metamorphosed turbidite succession of interbedded red-brown to grey-green fine- to medium-grained sandstone and mudstone.|12-JUL-16
21914|Grindall Formation|69430|6|Mentioned|p15:5, 13|||||||Is overlain unconformably by Coast Range Sandstone. Inferred to underlie Woodah Sandstone, Erringkarri Rhyolite and Abarungkwa Sandstone unconformably.||12-JUL-16
21914|Grindall Formation|69673|6|Mentioned|p3 fig 2|Orosirian|Orosirian|||||||
21914|Grindall Formation|70302|5|Briefly described|iv, p5, p7|||Arnhem Province.||||Is overlain unconformably by Woodah Sandstone.|Interlayered sandstone and mudstone.|
21914|Grindall Formation|70719|4|Described|iv, p1, p5-7, p19-20|Orosirian|Orosirian|Southern Arnhem Province. Oldest stratigraphic unit in the Province. Interpreted as unmetamorphosed equivalent of Melville Bay Metamorphics. Was tentatively correlated with Burrell Creek Formation, but their detrital age spectra are markedly different. There are some similarities in age spectra with Cahill Formation and Nourlangie Schist of Nimbuwah Domain, Pine Creek Orogen. Interpreted by Haines et al 1999 to represent a turbidite succession deposited within a rapidly subsiding submarine basin.|1934 +/- 47 Ma (maximum depositional age).|||Is overlain unconformably by Woodah Sandstone. Is intruded by Bukudal Granite. Correlative of Cosmo Supergroup.|Deformed but largely unmetamorphosed siliciclastic (turbidite) succession of interlayered fine-grained sandstone, siltstone and lesser mudstone.|06-FEB-18
21914|Grindall Formation|71374|6|Mentioned|p27|||Arnhem Province.||||Locally overlain by the Jalma Formation.||
21914|Grindall Formation|71592|5|Briefly described|Appendix A.|||Arnhem Province.|1934+/-47 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
21914|Grindall Formation|71605|5|Briefly described|iii-iv, p1, p18-p20, p35|||Arnhem Province. SHRIMP ages of detrital zircons range from 2877-1956 Ma with the youngest 12 grains being those presented here and interpreted as maximum depositional ages.|1986 +/- 8 Ma (SHRIMP U-Pb)||||Sericite-bearing metasandstone.|
21914|Grindall Formation|71606|5|Briefly described|p137|Orosirian|Orosirian|Central and South Caledon Shelf, McArthur Basin.||||Overlain by Arnhem Granites.||
21914|Grindall Formation|71620|6|Mentioned|p5|||||||Unconformably overlies the Melville Bay Metamorphics.||
21914|Grindall Formation|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Basement to McArthur Basin.||||||05-MAR-20
21914|Grindall Formation|72377|5|Briefly described|p9, 10, 13, 19|Paleoproterozoic|Paleoproterozoic|Geological province: Arnhem Province. Interpreted maximum depositional ages of 1986+\-8 Ma and 1934+\-47 Ma were reported from Kositcin et al (2018) and Kositcin et al (2015a) respectively, based on SHRIMP U-Pb zircon dating.||||Overlain by Jalma Formation. Intruded by sub-volcanic dykes of the Gadabara Volcanics.||09-OCT-19
21914|Grindall Formation|73089|6|Mentioned|p32, p34|Orosirian|Orosirian|Arnhem Province. Does not contain zircon age components younger than c. 1930 Ma.|1862-1830 Ma||||Turbiditic rocks.|
21994|Illyabba Metamorphics|23361|5|Briefly described|31|||||||||
21994|Illyabba Metamorphics|24197|5|Briefly described|p59 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Of the Narwietooma Suite. Age: ~1880Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
21994|Illyabba Metamorphics|43225|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
21994|Illyabba Metamorphics|43503|2|Defined|6,19,76|||||||||
21994|Illyabba Metamorphics|50369|5|Briefly described|p1.3, 3.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Narwietooma Suite.||||||07-NOV-08
21994|Illyabba Metamorphics|61309|6|Mentioned|p31|||Tonalitic/granodioritic rocks.||||||06-FEB-08
21994|Illyabba Metamorphics|69427|5|Briefly described|p12:14-15|||Warren and Shaw (1995). Wigley Domain, Aileron Province. Occurs between the Redbank and Charles River Thrusts. Appears as Ilyabba in Fig.12.12.|||||Mainly migmatitic orthogneisses of a tonalitic to granodioritic composition, with small mafic pods, and lesser cordierite-bearing and garnet-biotite-sillimanite metapelitic gneiss.|12-JUL-16
10002|Lady Loretta Formation|22438|4|Described|p539, Fig.3 p537|||Youngest unit in Fiery Creek Dome region. See also Fig.10a p546||||||
10002|Lady Loretta Formation|22453|5|Briefly described|p 11  Fig 10|||||||||
10002|Lady Loretta Formation|22585|6|Mentioned|P739, Fig2, Fig3|||||||||
10002|Lady Loretta Formation|22680|6|Mentioned|83,85,87|||||||||
10002|Lady Loretta Formation|22681|5|Briefly described|89,90|Proterozoic|Proterozoic|Max thickness 2000 m. Underlain by Esperanza Formation.||||||09-OCT-06
10002|Lady Loretta Formation|23031|3|Fully described|40|||Geological province: Lawn Hill Subprovince. Of the McNamara Group. Overlain by Shady Bore Quartzite.||||||09-OCT-06
10002|Lady Loretta Formation|23072|5|Briefly described|p754|||||||||
10002|Lady Loretta Formation|23362|5|Briefly described|339|||||||||
10002|Lady Loretta Formation|23363|5|Briefly described|351 Tab.1|Statherian|Statherian|||||||
10002|Lady Loretta Formation|23387|6|Mentioned|p18 fig.19|||Of McNamara Group.||||||
10002|Lady Loretta Formation|23393|4|Described|p19, p20|Paleoproterozoic|Paleoproterozoic|Of McNamara Group.  Overlies the Esperanza Formation ; underlies Shady Bore Quartzite.||||||07-NOV-08
10002|Lady Loretta Formation|23396|5|Briefly described|p407 Fig.2|Statherian|Statherian|Of McNamara Group. Age: 1647+/-4Ma.||||||09-OCT-06
10002|Lady Loretta Formation|23397|5|Briefly described|p469|||||||||
10002|Lady Loretta Formation|23398|4|Described|p449|Statherian|Statherian|Of McNamara Group.  Age: 1647+/-4Ma.||||||09-OCT-06
10002|Lady Loretta Formation|23399|5|Briefly described|p503|||Of McNamara Group..||||||09-OCT-06
10002|Lady Loretta Formation|23406|5|Briefly described|p606, p612|Statherian|Statherian|Of McNamara Group. Age: 1647+/-4Ma. Geological province: Lawn Hill Platform. Contains a basal breccia layer.||||||16-JUN-09
10002|Lady Loretta Formation|23408|5|Briefly described|p511, p513 Fig. 2, p523|||Of McNamara Group. Includes a basal breccia which is interpreted to form the basal unconformity of the Lady Loretta Supersequence.||||||15-JUN-09
10002|Lady Loretta Formation|23409|4|Described|p539 Tab.1|Statherian|Statherian|Age: 1647+/-4Ma.||||||09-OCT-06
10002|Lady Loretta Formation|23466|5|Briefly described|p272 Fig.6|Statherian|Statherian|||||||
10002|Lady Loretta Formation|23767|5|Briefly described|p1956 Fig. 2|||Geological Province: Western Fold Belt. See also p1957 Fig.3.||||||
10002|Lady Loretta Formation|23958|5|Briefly described|p1134|Mesoproterozoic|Paleoproterozoic|Of McNamara Group.||||||07-NOV-08
10002|Lady Loretta Formation|23964|5|Briefly described|p1265|Proterozoic|Proterozoic|Of McNamara Group.  Geological Province: Mount Isa Inlier.  Maximum thicknees: 2000m.||||||
10002|Lady Loretta Formation|23965|5|Briefly described|p1297|Mesoproterozoic|Paleoproterozoic|Of McNamara Group. Geological Province: Mount Isa Inlier.||||||07-NOV-08
10002|Lady Loretta Formation|24308|5|Briefly described|p987 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of the McNamara Group.   Geological Province:  Mount Isa Superbasin||||||07-NOV-08
10002|Lady Loretta Formation|24309|5|Briefly described|p1018|Proterozoic|Proterozoic|Of the McNamara Group.||||||09-OCT-06
10002|Lady Loretta Formation|24432|4|Described|p560 Tb.1, p562 Fig.2|Statherian|Statherian|Of McNamara Group. Age: 1647+/-4 Ma. Carbonaceous, pyritic, dolomitic and sideritic siltstone and shale. Geological Province: Lawn Hill Platform.||||||
10002|Lady Loretta Formation|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10002|Lady Loretta Formation|36937|6|Mentioned|p229|||||||||
10002|Lady Loretta Formation|37459|1|Redefined|p430|Mesoproterozoic|Mesoproterozoic|Age is more specifically Carpentarian||||||
10002|Lady Loretta Formation|37568|6|Mentioned|p84|||||||||
10002|Lady Loretta Formation|37569|6|Mentioned|p93|||||||||
10002|Lady Loretta Formation|38237|4|Described|p129|||||||||
10002|Lady Loretta Formation|38291|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10002|Lady Loretta Formation|38348|4|Described|p12|||||||||
10002|Lady Loretta Formation|38584|6|Mentioned|p22|||||||||
10002|Lady Loretta Formation|39445|5|Briefly described|Table 2|||||||||
10002|Lady Loretta Formation|39497|6|Mentioned|Fig.4|||||||||
10002|Lady Loretta Formation|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the McNamara Group.||||||15-JUN-06
10002|Lady Loretta Formation|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10002|Lady Loretta Formation|39925|6|Mentioned|Fig.9|||||||||
10002|Lady Loretta Formation|39943|6|Mentioned|Table 1A|||||||||
10002|Lady Loretta Formation|39944|6|Mentioned|p228|||||||||
10002|Lady Loretta Formation|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10002|Lady Loretta Formation|40179|5|Briefly described|p306|||||||||
10002|Lady Loretta Formation|40221|3|Fully described|p18|||||||||
10002|Lady Loretta Formation|40394|6|Mentioned|Fig.2|||||||||
10002|Lady Loretta Formation|41298|6|Mentioned|Map legend|Carpentarian||||||||
10002|Lady Loretta Formation|42166|6|Mentioned|p111|||||||||
10002|Lady Loretta Formation|43235|5|Briefly described|p9,Fig.10.|||Of McNamara Group.||||||09-OCT-06
10002|Lady Loretta Formation|43615|6|Mentioned|p13|||||||||
10002|Lady Loretta Formation|45166|5|Briefly described|p30|||||||||
10002|Lady Loretta Formation|47083|3|Fully described|p17||Proterozoic|Previously part of Paradise Creek Formation of Carter and others (1961). Of McNamara Gp. Overlain by Shady Bore Quartzite; underlain by Esperanza Fm. Max thickness: 1800 m.||||||09-OCT-06
10002|Lady Loretta Formation|50550|5|Briefly described|p1139 Fig.2||Statherian|Age: >1647 Ma, <1657 Ma. Conformably overlies Esperanze Formation, conformably overlain by Shady Bore Quartzite. Geological Province: Western Fold Belt.||||||17-DEC-07
10002|Lady Loretta Formation|50600|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the McNamara Group.  Laminated and massive dolomite; intraclastic, oolitic and stromatolitic dolomite; ferruginous chert breccia, flaggy siltstone and fine sandstone.  Overlies Esperanza Formation; overlain by Shady Bore Quartzite.||||||28-JUN-04
10002|Lady Loretta Formation|60558|5|Briefly described|p5 Fig. 4|||Of McNamara Group. Overlain by Shady Bore Quartzite, underlain by Esperanza Formation.||||||
10002|Lady Loretta Formation|61936|5|Briefly described|p194 Fig. 6|||Geological Province: Lawn Hill Platform, Western Fold Belt, Mount Isa Inlier.||||||
10002|Lady Loretta Formation|62084|5|Briefly described|p936 Fig.5|||Isa Superbasin. Lawn Hill. Hosts Lady Loretta deposit (Zn-Pb-Ag stratiform). Shown as Lady Loretta Fm.||McNamara Group|||Platform carbonates.|
10002|Lady Loretta Formation|62535|5|Briefly described|p672|Statherian|Statherian|Lawn Hill Platform.|1647 +/- 4 Ma.|McNamara Group.||||
10002|Lady Loretta Formation|63109|6|Mentioned|p1108 Fig. 3|||Geological Province: Isa Superbasin.||||||30-SEP-08
10002|Lady Loretta Formation|63111|5|Briefly described|p1164 Tb. 1, p1163 Fig. 3|Statherian|Statherian|Of Loretta Supersequence. Age: 1647+/-4Ma and 1649+/-7Ma. Geological Province: Isa Superbasin. Laminated fine-grained sandstone and siltstones, peloid-dolograinstones, dolomudstone and carbonates.||||||07-FEB-11
10002|Lady Loretta Formation|63113|6|Mentioned|p1214,1219,1220,1225: Figs.2,8,9,13. |||Part of Loretta supersequence.|1647 Ma.|Of the McNamara Group||Is overlain by Riversleigh Siltstone or ?unconformably by Shady Bore Quartzite.||
10002|Lady Loretta Formation|63114|5|Briefly described|p1253 Fig.2. |||Isa superbasin.||Of the Loretta supersequence||Is overlain by Shady Bore Quartzite.||
10002|Lady Loretta Formation|63115|6|Mentioned|p1279 Fig.4.|||Isa superbasin.||||||
10002|Lady Loretta Formation|63116|6|Mentioned|p1297 Fig.2, p1299 Tb.1, p1300 |||Isa superbasin. Material properties detailed.||||||
10002|Lady Loretta Formation|63866|5|Briefly described|p57|Statherian|Statherian|Isa Superbasin.|1647 +/- 4 Ma|Loretta Supersequence||||
10002|Lady Loretta Formation|64250|6|Mentioned|p11 fig 3||||1647 +/- 4 Ma|Unit in McNamara Group.||||
10002|Lady Loretta Formation|64575|6|Mentioned|p665|||||||||
10002|Lady Loretta Formation|65228|5|Briefly described|p26, Fig.04.|Statherian|Statherian|Part of Loretta Supersequence.|1647 +/- 4 Ma (SHRIMP).|||Equivalent to Loretta Supersequence.||
10002|Lady Loretta Formation|65337|6|Mentioned|p33 Fig.27.|||Correlates with upper Brumby Formation.||||Overlies Esperanza Formation. Is overlain by Shady Bore Quartzite.||
10002|Lady Loretta Formation|65396|5|Briefly described|p82, p175, p195, p241|Statherian|Statherian|Isa Superbasin. Cover Sequence 3. Lawn Hill Platform. Detrital zircon sources listed.|1647 +/- 4 Ma|McNamara Group||Overlies Esperanza Formation; overlain by Shady Bore Quartzite.||03-APR-17
10002|Lady Loretta Formation|66844|5|Briefly described|p245,268, 269|Mesoproterozoic|Statherian|Lawn Hill and Gunpowder region. Age from SHRIMP dating.|1647+\-3 Ma|Within Loretta Supersequence.||Underlain unconformably by Esperanza Formation. Overlain by upper McNamara Group.|Basal breccia, marine carbonates and siliciclastics.|
10002|Lady Loretta Formation|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map, p60|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Mount Isa Inlier, Isa Superbasin.|1647 +/- 4 Ma (maximum depositional age).|McNamara Group.|||Laminated stromatolitic and intraclastic dolomite, dolomitic siltstone, limestone, shale|
10002|Lady Loretta Formation|68542|6|Mentioned|p6|||||Lower McNamara Group||Overlies Esperanza Formation||
10002|Lady Loretta Formation|68576|5|Briefly described|Q_2: p6-7|||Lawn Hill Platform, Mount Isa Inlier. Hosts the exceptionally high-grade, sediment-hosted Lady Loretta Zn-Pb-Ag deposit (described in detail).||Lower McNamara Group.|||Basal interbedded dolomitic siltstone and sandstone; then interbedded pyrite, argillaceous siltstone and minor sandstone; banded to massive sulfides, locally baritic; massive siltstone locally pyritic; interbedded siltstone, sandstone and sulfides.|
10002|Lady Loretta Formation|68732|5|Briefly described|p162, p165 Fig.3|Statherian|Statherian|Of the Loretta Supersequence. Sedimentary depositional age.|1647 +/- 4 Ma|Of the McNamara Group.||||
10002|Lady Loretta Formation|69591|4|Described|p42, p43-44, p54|||Isa Superbasin. Thins to the NNW. Deposited on a shallow carbonate platform: subtidal/inner shelf/outer ramp deposits. Loretta Supersequence.|~1647 Ma (Betts et al., 1999).|McNamara Group.||Overlies Esperanza Formation.|Laminated stromatolitic and intraclastic dolomite, dolomitic siltstone, limestone, shale.|
10002|Lady Loretta Formation|70864|5|Briefly described|p75, 74 Fig 2, p78, p80, 81, 84, 100|Mesoproterozoic||||McNamara Group|||Stromatolitic dolostones, dolomitic siltstone and carbonaceous pyritic shale.|
10002|Lady Loretta Formation|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1648+/-13 Ma (crystallisation: U-Pb zircon SHRIMP)||||Tuffite or shale.|
10002|Lady Loretta Formation|72526|5|Briefly described|p1, p8 Fig.1.3, p10, p85.|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 based on the age of tuffaceous intervals (Page and Sweet, 1998; Page et al., 2000; Carson et al., 2011b). Age given as U-Pb zircon sedimentary depositional age.|1647 +/-4 Ma.|McNamara Group||Overlies Esperanza Formation and conformably underlies Shady Bore Quartzite.||
10002|Lady Loretta Formation|72912|4|Described|p5 Fig.3, p15, p33 Fig.12.|Statherian|Statherian|Shown as being located in the Queensland part of the McNamara Group. Located in the Lawn Hill Platform of the Mount Isa Province, and the East part of the South Nicholson Basin. U-Pb zircon sedimentary depositional age [?] given.|1647 +/- 4 Ma|McNamara Group||Overlies Esperanza Formation and underlies Shady Bore Quartzite.|Includes dolomitic siltstone.|
10002|Lady Loretta Formation|72913|5|Briefly described|p4,p7,  p8, p9 Tb.1, p22, p26.|Paleoproterozoic|Paleoproterozoic|Shown as being in the eastern and Lawn Hill Platform part of the Isa Superbasin. Identified in Argyle Creek 1 in this study.  Mineral composition shows majority quartz and dolomite.|1647 +/- 4 Ma|McNamara Group||Overlies Esperanza Formation and underlies Shady Bore Quartzite.|Includes dolomitic siltstone.|
10002|Lady Loretta Formation|72967|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|Lawn Hill Platform.||McNamara Group||||
10002|Lady Loretta 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).|1647 +/- 4 Ma (see Fig.1.2)|McNamara Group||Underlain by Esperanza Formation. Overlain by Shady Bore Quartzite unconformably in part.||
10002|Lady Loretta Formation|73144|6|Mentioned|p8-9|Statherian|Statherian|Isa Superbasin. Loretta Supersequence. Aquifer. Includes oil show. Deposited in subtidal tempestite cycles (Southgate et al., 2000).||McNamara Group||Underlain by Esperanza Formation. Unconformably overlain by Riversleigh Siltstone.|Dolomudstone.|
10002|Lady Loretta Formation|73525|6|Mentioned|p4-5 Fig.2|||Mount Oxide-(Ardmore-May Downs) Domain.|||||Carbonates.|
10097|Lalngang Sandstone|22547|5|Briefly described|p24|||Of Fitzmaurice Group. Overlain by Legune Formation. Correlates with Stonewall Sandstone||||||12-OCT-06
10097|Lalngang Sandstone|32307|4|Described|Table 2|||Proterozoic||||||
10097|Lalngang Sandstone|32310|6|Mentioned|Map legend|Adelaidean|Carpentarian|Adelaidean/Carpentarian.||||||12-OCT-06
10097|Lalngang Sandstone|32660|5|Briefly described|Table 6|||||||||
10097|Lalngang Sandstone|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Fitzmaurice Group.  Quartz sandstone, grit, conglomerate, minor siltstone.||||||02-DEC-04
10097|Lalngang Sandstone|32701|4|Described|Table 1|||Fitzmaurice Gp. Adelaidean||||||
10097|Lalngang Sandstone|32728|6|Mentioned|Fig.14|||||||||
10097|Lalngang Sandstone|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
10097|Lalngang Sandstone|37462|6|Mentioned|Fig.4.13|||||||||
10097|Lalngang Sandstone|45112|6|Mentioned|p34|||||||||
10097|Lalngang Sandstone|48938|2|Defined|p16|Adelaidean|Adelaidean|||||||
10097|Lalngang Sandstone|48942|3|Fully described|p36|||Strat. section.||||||
10097|Lalngang Sandstone|60006|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: ? Halls Creek Orogen. Of Fitzmaurice Group. Silica cemented quartz sandstone, conglomerate, minor siltstone.||||||19-JUL-04
10097|Lalngang Sandstone|60682|4|Described|p5|Mesoproterozoic|Mesoproterozoic|Of Fitzmaurice Group. Thickness: >1400m. Conformably/disconformably overlies Goobaieri Formation. Grades conformably up into Legune Formation. Geological Province Halls Creek Orogen. Quartz sandstone, conglomerate and minor siltstone.||||||
10097|Lalngang Sandstone|64698|6|Mentioned|lithinterp table|||Also misspelt as Lalngang Sndstone, Laingang Formation, & Lalngang Formation.||||||
10097|Lalngang Sandstone|65331|5|Briefly described|Map legend|Mesoproterozic|Mesoproterozic|Of Fitzmaurice Group, ?Halls Creek Orogen. Silica cenemnted quartz sandstone, conglomerate, minor siltstone||||||
10097|Lalngang Sandstone|65417|5|Briefly described|p158 Fig.2, p159, pp162-163.|Mesoproterozoic|Mesoproterozoic|Fitzmaurice Mobile Zone. Correlated with the Stonewall Sandstone of the Carr Boyd Group (Halls Creek Orogen).||Unit in Fitzmaurice Group.||Is overlain conformably by Legune Formation.||
10097|Lalngang Sandstone|69435|4|Described|p20:2-4|||Sweet et al. (1974). Fitzmaurice Basin. Exposed over a large area. 1400m thick at the type area.||Fitzmaurice Group.||Conformably (?regionally disconformably) overlies Goobaieri Formation. Is overlain gradationally by Legune Formation. Is intruded by Ti Tree Granophyre.|Silica-cemented quartz sandstone, commonly thickly bedded with locally abundant cross-beds and ripple marks; conglomerate, and minor siltstone. Becomes more argillaceous to the NW.|12-JUL-16
10097|Lalngang Sandstone|69673|5|Briefly described|p59, p60 fig 48|||1400m thick.||Fitzmaurice Group||Overlain by Legune Formation, overlies Goobaieri Formation|Silica cemented quartz sandstone, conglomerate and minor siltstone.|
10097|Lalngang Sandstone|70206|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Fitzmaurice Basin.||Fitzmaurice Group|||Silica cemented quartz sandstone, conglomerate and minor siltstone.|
10097|Lalngang Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, sandstone|
10134|Lancewood Shale|30479|6|Mentioned|p22|||See also Fig.3||||||
10134|Lancewood Shale|30914|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
10134|Lancewood Shale|35054|6|Mentioned|Table 23|||||||||
10134|Lancewood Shale|37572|5|Briefly described|p158|||||||||
10134|Lancewood Shale|38446|6|Mentioned|Table 23|||||||||
10134|Lancewood Shale|39445|5|Briefly described|Table 4|||See also p61, p62.||||||09-DEC-08
10134|Lancewood Shale|44211|14|Not recorded|p101|||||||||
10134|Lancewood Shale|44274|14|Not recorded|Tb.1,opp.p7,11|||Overlies Currant Bush Limestone, possibly equivalent to upper part of Currant Bush Limestone.||||||
10134|Lancewood Shale|44482|14|Not recorded|p.11||Middle Cambrian|(E53-12). Middle Cambrian.||||||09-DEC-08
10134|Lancewood Shale|44926|5|Briefly described|Map Legend|Permian|Late Carboniferous|||||||
10134|Lancewood Shale|45052|5|Briefly described|p93|||Middle Cambrian.||||||09-DEC-08
10134|Lancewood Shale|45079|5|Briefly described|p30|||Cambrian age||||||
10134|Lancewood Shale|64068|6|Mentioned|p225|||Of Opik (1960). In part replaced by Narpa Group.||||||
10134|Lancewood Shale|65337|5|Briefly described|p64.|||Named by Opik (1960). Included in upper Currant Bush Limestone by Smith and Roberts (1963). Reinstated as Lancewood Shale by Shergold et al. (1985). Back as 'provisionally adopted' Currant Bush Limestone in this study.|||||Minor friable sandstone, leached and deeply lateritised siltstone and shale.|
10134|Lancewood Shale|69573|6|Mentioned|p659|||Georgina Basin. Contains Drumian Stage [Cambrian] fossil sites.||||||
10134|Lancewood Shale|69591|6|Mentioned|p96||||||||Siltstone, shale, chert.|
10161|Langfield Group|13194|4|Described|p390 Tb. 4-16, p382 fig 4-59, p399|Tournaisian|Tournaisian|||||Overlies Ningbing Group. Part equivalent to Bonaparte Formation.||
10161|Langfield Group|13234|6|Mentioned|p250 Fig.2, p252 Fig.4,p260 Tb.1, |Early Carboniferous|Early Carboniferous|Potential reservoir.|||||Includes dolomites.|
10161|Langfield Group|14228|5|Briefly described|p6 fig3|Tournaisian|Famennian|Southern Bonaparte Basin.||||Overlies Ningbing Group.||05-OCT-16
10161|Langfield Group|22663|5|Briefly described|W97 8 to 10 fig.2||Carboniferous|||||||01-MAR-10
10161|Langfield Group|23377|6|Mentioned|p212 Fig.5|Carboniferous|Devonian|Of Vulcan Sub-basin.||||||12-OCT-06
10161|Langfield Group|23858|5|Briefly described|p919|||Geological Province: Bonaparte Basin.  Max. thickness: 2000 m.||||||
10161|Langfield Group|24390|5|Briefly described|p2 Fig. 2|Early Carboniferous|Late Devonian|Geological Province: Bonaparte Basin.||||||
10161|Langfield Group|24503|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Sandstone, limestone, shale and siltstone.  Geological Province: Bonaparte Basin.||||||
10161|Langfield Group|24569|5|Briefly described|p248 Fig. 3|Tournaisian|Late Devonian|Geological Province: Petrel Sub-basin.||||||
10161|Langfield Group|40993|2|Defined|p10|Tournaisian|Tournaisian|||||||
10161|Langfield Group|41459|6|Mentioned|Fig.2|||||||||
10161|Langfield Group|41532|6|Mentioned|p292|||||||||
10161|Langfield Group|41598|6|Mentioned|p412|||||||||
10161|Langfield Group|41731|5|Briefly described|p519|||See also p574.||||||12-OCT-06
10161|Langfield Group|41864|4|Described|p101|||Formerly "Eight Mile Creek Group" then "Keep River Group"||||||
10161|Langfield Group|41865|6|Mentioned|Map legend||Tournaisian|||||||
10161|Langfield Group|42442|5|Briefly described|Fig.6 P9|||Same unit as Langfield Group in WA.||||||12-OCT-06
10161|Langfield Group|43236|6|Mentioned|p14,Fig.13.||Tournaisian|||||||
10161|Langfield Group|43661|6|Mentioned|Fig.3|||||||||
10161|Langfield Group|50085|5|Briefly described|p2 Fig. 2|Early Carboniferous|Late Devonian|Geological Province: Bonaparte Basin.||||||
10161|Langfield Group|60006|5|Briefly described|Map Legend|Tournaisian|Tournaisian|Geological Province: Bonaparte Basin. Unconformably overlies Ningbing Group. Sandstone, siltstone, shale, limestone, dolostone.||||||22-JUL-04
10161|Langfield Group|60364|4|Described|p184|Tournaisian|Tournaisian|Alternating calcarenite and sandstone. Overlain by Milligans Formation. Thickness: 900m. Geological Province: Bonaparte Basin.||||||12-OCT-06
10161|Langfield Group|60682|4|Described|piii, 22 Table 5|Tournaisian|Tournaisian|Mixed carbonate/siliciclastic shallow marine deposits. Unconformably overlain by Weaber Group. Max. thickness 900m. Contains 5 formations.||||||31-JUL-15
10161|Langfield Group|61023|5|Briefly described|p2 Fig. 2|Carboniferous|Devonian|Geological Province: Bonaparte Basin.||||||11-APR-08
10161|Langfield Group|61542|5|Briefly described|p277 Fig. 2, p283|Tournaisian|Tournaisian|Includes Bonaparte and Burt Range Formations, Enga Sandstone, Septimus Limestone and Zimmermann Sandstone. Overlies Ningbing Group; unconformably underlies Weaber Group. Geological province: onshore Bonapart Basin/Petrel-Sub-basin.||||||07-FEB-11
10161|Langfield Group|62837|5|Briefly described|Stratigraphic columns|Visean|Tournaisian|Includes the Bonaparte Formation.  Age: <355->345Ma. Geological Province:  Petrel Sub-basin (offshore).||||||01-MAR-10
10161|Langfield Group|64159|5|Briefly described|p93|Carboniferous|Carboniferous|Contains the Burt Range Formation. Geological Province: Bonaparte Basin.||||||
10161|Langfield Group|64580|4|Described|map legend|Tournaisian|Tournaisian|Undivided; sandstone, limestone,shale and siltstone; includes BONAPARTE (subsurface only) and BURT RANGE FORMATIONS, ENGA and ZIMMERMAN SANDSTONES, and SEPTIMUS LIMESTONE.||||||09-DEC-08
10161|Langfield Group|64689|5|Briefly described|p14, p20|||Gorter et al. (2004) suggest this unit is the source of oil discoveries at Turtle-1 and Barnett-1 (previously thought to be Milligans Formation).||||Overlain unconformably by Milligans Formation.||
10161|Langfield Group|64694|5|Briefly described|p231-233, p234 Fig.2, p236, p238 Tb.1|Visean|Late Tournaisian|See also p239, p241, p242 Tb.4, p243, p246-249.|||Includes Burt Range Formation, Upper Bonaparte Formation, Enga Sandstone, Septimus Limestone and Zimmermann Sandstone.|Overlies Ningbing Group. Overlain by the Weaber Group unconformably.||
10161|Langfield Group|65331|5|Briefly described|Map legend + overview geology map legend|Tournasian|Tournasian|Of Bonaparte Basin. Includes Zimmerman Sandstone, Septimus Limestone, Enga Sandstone, Burt Range Formation. Sandstone, siltstone, shale, limestone, dolostone||||||
10161|Langfield Group|67167|5|Briefly described|Map legend.|Carboniferous|Carboniferous||||||Undivided: shale, siltstone, limestone.|
10161|Langfield Group|67186|5|Briefly described|Map legend.|Carboniferous|Carboniferous||||||Shale, sandstone, limestone.|23-NOV-11
10161|Langfield Group|69099|4|Described|500k_geologyp08_lut.csv|Tournasian|||||Includes Bonaparte (subsurface only) and Burt Range Formations, Enga and Zimmermann Sandstones, and Septimus Limestone.||Sandstone, limestone,shale and siltstone.|31-JUL-15
10161|Langfield Group|69165|4|Described|500k_geologyp08_lut.csv|Tournaisian|Tournaisian||||Includes Bonaparte Formation, Burt Range Formation, Enga Sandstone, Zimmerman Sandstone||Undivided; sandstone, limestone, shale and siltstone|
10161|Langfield Group|69422|6|Mentioned|p7:2 Fig.7.2|Carboniferous|Carboniferous|Bonaparte Basin.||||||12-JUL-16
10161|Langfield Group|69452|4|Described|p36:4, 6-7, 9, 11-13, 15, 18, 23, 28|Early Carboniferous|Late Devonian|Beere and Mory (1986). Petrel Sub-basin, Bonaparte Basin. Up to 900m thick. Non-commercial discoveries of oil and/or gas in the southern part of the Sub-basin are probably sourced from older units of this Group.|||Enga, Zimmerman Sandstones; Burt Range, Bonaparte Formations; Septimus Limestone.|Overlies Ningbing Group conformably or disconformably. Is overlain unconformably by Weaber Group and by Border Creek and Keep Inlet Formations (Kulshill Group).||12-JUL-16
10161|Langfield Group|69634|5|Briefly described|500k_geologyp08_lut.csv|Tournaisian|Tournaisian||||Includes Bonaparte and Burt Range formations, Enga and Zimmerman sandstones, and Septimus Limestone.|||
10161|Langfield Group|69653|5|Briefly described|p10, 14|Carboniferous|Carboniferous|Petrel Sub-basin. Shallow-marine to non-marine settings.||||Overlies Ningbing Group. Is overlain by Weaber Group.|Fine-grained clastic and carbonate sediments.|
10161|Langfield Group|69673|5|Briefly described|p167, p170 fig 142, p171, p177,|Early Carboniferous|Late Devonian|Conventional petroleum potential, sealed by the Milligans Formation, forms a seal for the underlying Ningbing Group. Maximum thickness of 900m.|||Includes Enga Sandstone, Bonaparte Formation, Burt Range Formation, Septimus Limestone, Zimmerman Sandstone|Overlies Ningbing Group, Buttons Formation, overlain by Milligans Formation|Marine sandstone, limestone and shale.|
10161|Langfield Group|70061|5|Briefly described|Petrel Sub-basin; Fig.3, p2|||See also Regional geology: Fig.8, p5, p8-9, p11-12, p16. An equivalent unit in the Petrel Sub-basin includes the upper (Tournaisian) part of the Bonaparte Formation; oil- and gas-prone mudstones, previously assigned to the Milligans Formation.|||Burt Range, Ningbing Limestones.|Is overlain by Milligans Formation.||12-JUL-16
10161|Langfield Group|70154|5|Briefly described|500k_interpgeop14_lut.csv|Tournaisian|Tournaisian||346-358 Ma||||Sandstone, limestone, shale, and siltstone|
10161|Langfield Group|70206|5|Briefly described|Map Legend, cross-sect.|Carboniferous|Carboniferous|Bonaparte Basin.|||Includes Zimmerman Sandstone, Septimus Limestone, Enga Sandstone, Burt Range Formation.|Unconformably overlies Ningbing Group. Unconformably overlain by Weaber Group.||
10161|Langfield Group|70812|6|Mentioned|p30|||||||||
10161|Langfield Group|70826|6|Mentioned|p6 tbl 3|Carboniferous|Carboniferous|Southern Bonaparte Basin.||||||
10161|Langfield Group|70851|6|Mentioned|p17|||||||||
10161|Langfield Group|71146|5|Briefly described|p6,  p43 fig 33|Tournaisian|Famennian|Bonaparte Basin.||||Overlies the Buttons Formation. Unconformably overlain by the Weaber Group.|Sandstone and carbonate.|
10161|Langfield Group|71267|5|Briefly described|1M_geologyp12_lut.csv|Tournaisian|Tournaisian|Of Southern Bonaparte Basin. Events: Alice Springs Orogeny (450-295 Ma); Eclipse Movement (340-300 Ma). See 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|358.9-346.7 Ma (biostrat-inferred)||Includes Burt Range Formation, Enga Sandstone, Hardman Formation, Septimus Limestone, Zimmermann Sandstone.|||
10161|Langfield Group|72034|5|Briefly described|500k_interpgeop16_lut|Tournaisian|Tournaisian|Southern Bonaparte Basin. Max  age from biostratigraphy, min age inferred.|||||Sandstone, limestone, shale, and siltstone.|
10163|Langford Gneiss|33103|4|Described|Table 2|||||||||
10163|Langford Gneiss|33104|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
10163|Langford Gneiss|50369|6|Mentioned|p26.2|||||||||
10163|Langford Gneiss|65341|6|Mentioned|p2 Fig.2. |Paleoproterozoic|Paleoproterozoic|||||||19-JUN-13
10163|Langford Gneiss|69917|5|Briefly described|p96-98|Statherian|Orosirian|Central Arunta Region, Aileron Province. U/Pb LA-ICPMS zircon dating. Shown and described on p96 as Langford Granite. 1801+/-8 Ma is interpreted as the igneous crystallisation age of the granite. Sample also shows inheritance from Bleechmore Metamorphics.||||Inferred to intrude Bleechmore Metamorphics|Granitic orthogneiss.|
10170|Langra Formation|22562|6|Mentioned|p39|||||||||
10170|Langra Formation|22760|5|Briefly described|p340|||Of the Finke Group.||||||13-OCT-06
10170|Langra Formation|22826|4|Described|p576|Devonian|Devonian|Of the Finke Group.||||||13-OCT-06
10170|Langra Formation|24301|5|Briefly described|p22|||Geological Province: Amadeus Basin||||||
10170|Langra Formation|30544|6|Mentioned|Fig.5 P51|||Map legend||||||
10170|Langra Formation|31566|6|Mentioned|p244|||Devonian||||||
10170|Langra Formation|31567|3|Fully described|p280|||Refers Wells et al. (1966).||||||
10170|Langra Formation|33971|3|Fully described|p30|||Refers Wells et al. (1966).||||||
10170|Langra Formation|34111|5|Briefly described|Table 2|||See also pp16-19. Devonian - Carboniferous.||||||13-OCT-06
10170|Langra Formation|34580|4|Described|Table 1|||Devonian - Carboniferous||||||
10170|Langra Formation|35102|6|Mentioned|Fig.17|||||||||
10170|Langra Formation|42699|5|Briefly described|map legend|Devonian||||||||
10170|Langra Formation|42940|6|Mentioned|Plate 5|||||||||
10170|Langra Formation|43035|5|Briefly described|p24|||Of Finke Group.||||||13-OCT-06
10170|Langra Formation|44133|5|Briefly described|p44|Carboniferous?|Late Devonian|Of the Finke Group. Conformably overlies Mereenie Sandstone. Overlain by Horseshoe Bend Shale.||||||
10170|Langra Formation|44323|14|Not recorded|map legend|Carboniferous|Devonian|SG/53-6, Dev-Carb pt of Finke Group.||||||
10170|Langra Formation|44393|4|Described|p.3,7,8,Tb.1,Fig.1|Carboniferous|Devonian|Part of Finke Group. Dev-Carb.||||||
10170|Langra Formation|44433|14|Not recorded|map legend|||Devonian to Carboniferous.||||||
10170|Langra Formation|45041|4|Described|p104|||Devonian||||||
10170|Langra Formation|48865|2|Defined|p.4,10,Fig.29|Carboniferous|Devonian|On many figures. Fig.4,11,21,28,36,39,51,53,55,Pl.3,4,5,11. Unit of Finke Gp.Devn-Carb. (G53-6)||||||
10170|Langra Formation|48890|4|Described|p.51|Carboniferous|Devonian|See also, Tb.2,Tb.3,Fig.4. p.52, Pl.9. pt. Finke Gp. Dev-Carb.||||||
10170|Langra Formation|50372|5|Briefly described|Map Legend|Devonian|Devonian|Of Finke Group. Geological Province: Amadeus Basin. Weathered fine to medium grained crossbedded quartz sandstone with rare conglomeritic lenses with basement clasts.||||||
10170|Langra Formation|65233|5|Briefly described|p13|||Interfingers with pertnjara Group.||||||07-FEB-11
10170|Langra Formation|65309|4|Described|p6 Table 1, pp13-14, pp19-20.|Devonian|Devonian|Most exposures thin and consist of upper part of sequence. Drilling shows thickness ranges from 0 to 130m. Includes angular clasts of Stairway Sandstone. Type area at Polly Corner.||Unit in Finke Group.||Partly overlies, and partly a distal equivalent of, Polly Conglomerate.|Very weathered, fine to medium, cross-bedded quartz sandstone; rare conglomeratic lenses with basement clasts; red and blue clayey shale encountered in drillholes.|
10170|Langra Formation|65489|6|Mentioned|p63|||Amadeus Basin. Contains potential reservoir beds. The middle unit could act as a seal.||||||
10170|Langra Formation|69438|4|Described|p23:2-3, 10, 20, 40-41|Late Devonian|Late Devonian|Wells et al. (1966). Amadeus Basin. Up to 527m thick. Becomes finer-grained northwards and up-section. Fluvial: mainly point-bar deposits.||Finke Group.||Conformably/gradationally overlies Polly Conglomerate. Unconformably overlies Larapinta Group, Parke Siltstone, Winnall beds, Bitter Springs Formation. Is overlain conformably by Horseshoe Bend Shale.|Cycles of massive conglomerate beds overlain by sandstone and an upper sandy siltstone, overlain by pebbly cross-bedded sandstone; then sandy micaceous siltstone; topped by fine- to medium-grained sandstone succession with few pebbly intervals.|12-JUL-16
10170|Langra Formation|69449|5|Briefly described|p34:5|Devonian|Devonian|||Finke Group.||Overlies Polly Conglomerate. Is overlain by Horseshoe Bend Shale.|Massive sandstone with minor claystone.|12-JUL-16
10170|Langra Formation|69673|6|Mentioned|p64 fig 53, p149|||||Finke Group||Overlies Polly Conglomerate, overlain by Horseshoe Bend Shale, Idracowra Sandstone||
10170|Langra Formation|71279|5|Briefly described|p355 Fig.2|Late Devonian|Late Devonian|Amadeus Basin.||Finke Group.||||
10170|Langra Formation|73085|6|Mentioned|p1|late Devonian|late Devonian|||Finke Group||Underlain by Polly Conglomerate. Overlain by Horseshoe Bend Shale / Idracowra Sandstone. Equivalent to Hermannsburg Sandstone (Pertnjara Group).||
10170|Langra Formation|73281|6|Mentioned|Appendix (DIP)|||See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
10184|Larapinta Group|9199|5|Briefly described|Map legend|Ordovician|Cambrian|Includes the Pacoota Sandstone.  Geological Province: Amadeus Basin.||||||
10184|Larapinta Group|9814|5|Briefly described|Map Legend|Ordovician|Ordovician|||||||
10184|Larapinta Group|13995|5|Briefly described|p69|Ordovician|Ordovician|Amadeus Basin.|||Stairway Sandstone.|||
10184|Larapinta Group|22561|6|Mentioned|p11|||||||||
10184|Larapinta Group|22563|6|Mentioned|p47||Ordovician|||||||
10184|Larapinta Group|22566|5|Briefly described|p76|Devonian|Late Cambrian|||||||
10184|Larapinta Group|22650|6|Mentioned|Fig 2 on p 157|Ordovician|Cambrian|||||||
10184|Larapinta Group|22651|6|Mentioned|p 189|||||||||
10184|Larapinta Group|22655|6|Mentioned|p 255|||informally divided in to upper and lower Larapinta Group, p255.||||||17-JAN-07
10184|Larapinta Group|22656|6|Mentioned|Fig 4 on p 282|Ordovician|Cambrian|||||||
10184|Larapinta Group|22760|5|Briefly described|p339|||||||||
10184|Larapinta Group|22761|6|Mentioned|Fig 2 on p351|Ordovician||||||||
10184|Larapinta Group|22763|6|Mentioned|p394|Late Ordovician|Cambrian|||||||
10184|Larapinta Group|22804|4|Described|p451|Early Devonian|Late Cambrian|||||||
10184|Larapinta Group|22805|6|Mentioned|p471|||||||||
10184|Larapinta Group|22806|6|Mentioned|p485||Ordovician|||||||
10184|Larapinta Group|22807|6|Mentioned|Fig 3 on p495|Late Ordovician|Early Ordovician|||||||
10184|Larapinta Group|22824|5|Briefly described|p525|Ordovician|Cambrian|||||||
10184|Larapinta Group|22826|6|Mentioned|Fig 4 on p567|||||||||
10184|Larapinta Group|23858|6|Mentioned|p914|||Geological Province: Amadeus Basin.||||||
10184|Larapinta Group|24063|5|Briefly described|p220|Ordovician|Cambrian|Geological Province: Amadeus Basin.||||||
10184|Larapinta Group|24064|5|Briefly described|p229 Fig.7|Ordovician|Ordovician|Geological Province: Amadeus Basin.||||||
10184|Larapinta Group|24111|6|Mentioned|p214 Fig. 9|||Geological Province: Amadeus Basin.||||||24-MAR-05
10184|Larapinta Group|24301|5|Briefly described|p20|Ordovician|Ordovician|Includes Stairway Sandstone, Stokes Siltstone and Carmichael Sandstone.   Geological Province: Amadeus Basin||||||
10184|Larapinta Group|24302|5|Briefly described|Map Legend|Ordovician|Ordovician|Includes the Stairway Sandstone, Stokes Siltstone and Carmichael Sandstone. Geological Province: Amadeus Basin.||||||16-JUL-13
10184|Larapinta Group|29721|6|Mentioned|Table 44|||||||||
10184|Larapinta Group|29972|6|Mentioned|p4|||Upper Cambrian- Ordovician||||||
10184|Larapinta Group|30238|4|Described|p64|||Cambrian - Ordovician age.||||||17-JAN-07
10184|Larapinta Group|30258|6|Mentioned|Fig.2|||Ordovician age||||||
10184|Larapinta Group|30544|6|Mentioned|p49|||||||||
10184|Larapinta Group|30817|6|Mentioned|p14|||||||||
10184|Larapinta Group|31566|6|Mentioned|p230|||Ordovician||||||
10184|Larapinta Group|31567|6|Mentioned|p280|||Unconformably overlain by Langra Formation.||||||17-JAN-07
10184|Larapinta Group|31707|4|Described|p50|||Discussed.||||||17-JAN-07
10184|Larapinta Group|32208|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
10184|Larapinta Group|32209|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
10184|Larapinta Group|33192|6|Mentioned|p20|||||||||
10184|Larapinta Group|33307|6|Mentioned|Fig.6|||||||||
10184|Larapinta Group|33738|6|Mentioned|p52|||||||||
10184|Larapinta Group|33761|6|Mentioned|p146|||Ord.- Sil? - Dev.||||||
10184|Larapinta Group|33971|5|Briefly described|p28|||Strat. section Fig.15.||||||
10184|Larapinta Group|34111|5|Briefly described|Table 2|||Cambrian - Ordovician. See also pp15-18.||||||13-OCT-06
10184|Larapinta Group|34186|6|Mentioned|Fig.4|||Ordovician||||||
10184|Larapinta Group|34442|5|Briefly described|Table 1|||Cambrian - Ordovician. See also pp8,9,10,11.||||||13-OCT-06
10184|Larapinta Group|34488|6|Mentioned|p11|||||||||
10184|Larapinta Group|34579|4|Described|Table 2|||Cambrian - Ordovician. See pp10,15,16.||||||13-OCT-06
10184|Larapinta Group|34580|4|Described|Table 1|||Ordovician||||||
10184|Larapinta Group|35102|6|Mentioned|p4|||||||||
10184|Larapinta Group|36198|6|Mentioned|Fig.III.2|||||||||
10184|Larapinta Group|36473|6|Mentioned|Map legend|Ordovician|Adelaidean|Adelaidean to Ordovician||||||
10184|Larapinta Group|36643|6|Mentioned|p65|||||||||
10184|Larapinta Group|36818|6|Mentioned|p203|||||||||
10184|Larapinta Group|36821|6|Mentioned|p397|||||||||
10184|Larapinta Group|38329|6|Mentioned|p210|||||||||
10184|Larapinta Group|38606|6|Mentioned|Map legend|Early Ordovician|Late Cambrian|Late Cambrian to Early Ordovician||||||
10184|Larapinta Group|38885|6|Mentioned|Map legend|Early Ordovician|Late Cambrian|Late Cambrian - Early Ordovician||||||
10184|Larapinta Group|39565|6|Mentioned|p33|||||||||
10184|Larapinta Group|39583|6|Mentioned|Map legend|Early Ordovician|Late Cambrian|Late Cambrian to Early Ordovician||||||
10184|Larapinta Group|39931|6|Mentioned|Map legend|Early Ordovician|Late Cambrian|Late Cambrian to Early Ordovician||||||
10184|Larapinta Group|40136|5|Briefly described|p29|||||||||
10184|Larapinta Group|40201|5|Briefly described|Table 1|||||||||
10184|Larapinta Group|40740|3|Fully described|p46|||Mention p6.||||||13-OCT-06
10184|Larapinta Group|40810|4|Described|p7|||||||||
10184|Larapinta Group|41018|6|Mentioned|p236|||||||||
10184|Larapinta Group|41039|6|Mentioned|Fig.2|||||||||
10184|Larapinta Group|41115|6|Mentioned|p1400|||||||||
10184|Larapinta Group|41190|6|Mentioned|p267|||||||||
10184|Larapinta Group|41203|5|Briefly described|p4|||||||||
10184|Larapinta Group|41224|5|Briefly described|p430|||||||||
10184|Larapinta Group|41270|6|Mentioned|p272|||||||||
10184|Larapinta Group|41385|6|Mentioned|Fig.3|||||||||
10184|Larapinta Group|41621|5|Briefly described|Map legend|Late Ordovician|Late Cambrian|||||||
10184|Larapinta Group|41711|6|Mentioned|p259|||||||||
10184|Larapinta Group|41717|6|Mentioned|Fig.2|||||||||
10184|Larapinta Group|41723|6|Mentioned|Map legend|Ordovician||||||||
10184|Larapinta Group|41801|5|Briefly described|p212|||||||||
10184|Larapinta Group|41819|6|Mentioned|Map legend|Late Ordovician|Late Cambrian|||||||
10184|Larapinta Group|41820|5|Briefly described|p7|||||||||
10184|Larapinta Group|42060|6|Mentioned|Fig.5 P140|||||||||
10184|Larapinta Group|42082|6|Mentioned|p322|||||||||
10184|Larapinta Group|42141|6|Mentioned|Fig.3 P570|||||||||
10184|Larapinta Group|42354|5|Briefly described|p3, p6|||Defined by Prichard and Quinlan (1962).||||||17-JAN-07
10184|Larapinta Group|42504|6|Mentioned|p77|||||||||
10184|Larapinta Group|42699|5|Briefly described|map legend|Ordovician||||||||
10184|Larapinta Group|42940|5|Briefly described|Plate 2|Ordovician|Ordovician|Siltstone, sandstone, limestone, dolostone, phosphorite; marine fossils.  Age: 500-440Ma. Geological province: Amadeus Basin.||||||23-JAN-08
10184|Larapinta Group|43035|5|Briefly described|p21|||||||||
10184|Larapinta Group|43105|5|Briefly described|Fig.3,p8.|||||||||
10184|Larapinta Group|43225|5|Briefly described|Map Legend||Ordovician|In the Amadeus Basin.||||||17-JAN-07
10184|Larapinta Group|43503|6|Mentioned|32-50|Silurian|Late Cambrian|||||||
10184|Larapinta Group|43631|6|Mentioned|p26|||||||||
10184|Larapinta Group|43647|6|Mentioned|Fig.4,533|||||||||
10184|Larapinta Group|43648|5|Briefly described|Fig.1,p488|||||||||
10184|Larapinta Group|43649|5|Briefly described|fig.1,p454-455,459|||||||||
10184|Larapinta Group|43817|6|Mentioned|Fig.1,p42|||||||||
10184|Larapinta Group|44133|5|Briefly described|p43|||Includes: Stairway Sandstone.||||||
10184|Larapinta Group|44323|14|Not recorded|map legend||Ordovician|SG/53-6. Ordovician.||||||
10184|Larapinta Group|44342|4|Described|p.6, Table 2||Ordovician|SG/53-5. U-M Ordovician.||||||
10184|Larapinta Group|44343|14|Not recorded|map legend||Late Ordovician|U.Ordovician.||||||
10184|Larapinta Group|44393|6|Mentioned|p.7|||refs Wells et al 1968.||||||
10184|Larapinta Group|44395|14|Not recorded|p.8,9,12,13, Tb.2|||||||||
10184|Larapinta Group|44402|5|Briefly described|map legend|Ordovician|Cambrian|Includes Stokes Siltstone, Stairway Sandstone, Horn Valley Siltstone, Pacoota Sandstone. Camb-Ord.||||||02-DEC-04
10184|Larapinta Group|44433|14|Not recorded|map legend|||Cambrian to Ordovician.||||||
10184|Larapinta Group|44484|14|Not recorded|p.3,5,10,Fig.4,Tb.1|Ordovician|Cambrian|Camb-Ord. See also p.12,14, for more details.||||||
10184|Larapinta Group|44485|14|Not recorded|map legend|Ordovician|Cambrian|Includes Pacoota Sandstone, Horn Valley Siltstone, Stairway Sandstone, Carmichael Sandstone, Stokes Siltstone. Camb-Ord.||||||
10184|Larapinta Group|44493|4|Described|p.11||Ordovician|BLOODS RANGE sheet (G53-3). See p.8,13, for details.||||||22-DEC-09
10184|Larapinta Group|44494|14|Not recorded|map legend||Ordovician|||||||
10184|Larapinta Group|44497|4|Described|p.10-11, Table 2|Ordovician|Cambrian|SF/53-13. Cambrian-Ord.||||||
10184|Larapinta Group|44498|14|Not recorded|map legend|Ordovician|Cambrian|Camb-Ord.||||||
10184|Larapinta Group|44505|14|Not recorded|p.2,7,8,10,11, Fig 1|Ordovician|Cambrian|Camb-Ord.||||||
10184|Larapinta Group|44506|14|Not recorded|map legend|Ordovician|Cambrian|Cambrian-Ordovician.||||||
10184|Larapinta Group|45036|6|Mentioned|p3|||Upper Cambrian - Upper Ordovician age||||||
10184|Larapinta Group|45041|4|Described|p61|||See also pp62-86. Ordovician.||||||13-OCT-06
10184|Larapinta Group|45118|6|Mentioned|p3|||||||||
10184|Larapinta Group|45155|6|Mentioned|p36|||See also Fig.37||||||
10184|Larapinta Group|45170|6|Mentioned|Fig.8|||||||||
10184|Larapinta Group|46829|6|Mentioned|Fig.2|||||||||
10184|Larapinta Group|46856|6|Mentioned|p279|||||||||
10184|Larapinta Group|46928|6|Mentioned|Table 1|||||||||
10184|Larapinta Group|47050|6|Mentioned|Fig.2|||||||||
10184|Larapinta Group|47052|6|Mentioned|p261|||||||||
10184|Larapinta Group|48639|14|Not recorded|p.16,opp.p.1|Ordovician|Cambrian|Ord-Cam. (G55-2).||||||
10184|Larapinta Group|48838|2|Defined|p.18,22, Tb.1,2|||||||||
10184|Larapinta Group|48862|14|Not recorded|p.1,18,24-29,39-42|||(F52-15). Pl.10,11.||||||
10184|Larapinta Group|48863|14|Not recorded|p.30||Ordovician|Tb.1. opp.p.7,p.2,7,12,24,30,31,37,39-42,Pl.11,13,15,16. (G52-4,G53-1).||||||
10184|Larapinta Group|48864|2|Defined|p.32||Ordovician|Tb.1. On many pages. p.2,9,10,27,38,30,34,37,47,50,Pl.11. (G52-3). Ord.||||||
10184|Larapinta Group|48865|4|Described|p.23||Ordovician|Includes: Pacoota Sandstone, Horn Valley Fm, Stokes Fm, Stairway Sandstone. Ord. On many pages. p.20,21,27,45-47,50,Pl.8.||||||
10184|Larapinta Group|48880|14|Not recorded|p.20,33,Pl.10,11||Ordovician|(F53-13,F53-14). Ord.||||||
10184|Larapinta Group|48890|4|Described|p.44-47|Ordovician|Cambrian|See also Tables, Figs and Plates. Camb-Ord.||||||13-OCT-06
10184|Larapinta Group|48963|6|Mentioned|p2|||p22||||||13-OCT-06
10184|Larapinta Group|50098|5|Briefly described|p1|Ordovician|Late Cambrian|Includes the Pacoota Sandstone, Horn Valley Siltstone, Stairway Sandstone, Stokes Siltstone and Carmichael Sandstone. Geological Province: Amadeus Basin.||||||
10184|Larapinta Group|50286|5|Briefly described|Map Legend|Ordovician|Ordovician|Geological Province: Amadeus Basin.||||||
10184|Larapinta Group|60547|5|Briefly described|Map Legend|Ordovician|Cambrian|Geological Province: Amadeus Basin.||||||
10184|Larapinta Group|60572|5|Briefly described|Map legend|Ordovician|Ordovician|White sandstone, locally bioturbated, minor siltstone, and conglomeratic sandstone.  Geological Province: Amadeus Basin.||||||23-DEC-09
10184|Larapinta Group|60674|5|Briefly described|Map legend|Ordovician|Cambrian|Includes: Pacoota Sandstone, Horn Valley and Stokes Siltstones, and Carmicahel Sandstone.  Geological Province: Amadeus Basin.||||||27-MAY-09
10184|Larapinta Group|60678|5|Briefly described|Map legend|Ordovician|Ordovician|White sandstone, locally bioturbated; minor siltstone and conglomeratic sandstone.  Geological Province: Amadeus Basin.||||||
10184|Larapinta Group|60679|5|Briefly described|Map Legend|Ordovician|Ordovician|Sandstone, minor siltstone and conglomeratic sandstone. Geological Province: Amadeus Basin.||||||
10184|Larapinta Group|60683|4|Described|p26, p9 Tb. 1|Ordovician|Ordovician|White sandstone, locally bioturbated, with minor siltstone and conglomeratic sandstone. Geological Province: Musgave Block/ Amadeus Basin.||||||16-JUN-09
10184|Larapinta Group|60904|5|Briefly described|p790 Fig. 16|Middle Ordovician|Late Cambrian|Marine sediments.||||||
10184|Larapinta Group|61386|5|Briefly described|Map legend|Cambrian|Cambrian|White sandstone, locally bioturbated, minor siltstone and conglomeratic sandstone. Geological Province: Amadeus Basin.||||||23-DEC-09
10184|Larapinta Group|61387|5|Briefly described|Map legend|Ordovician|Ordovician|Includes the Pacoota Sandstone, Horn Valley Siltstone, Stairway and Carmichael Sandstones. Geological Province: Amadeus Basin.||||||17-JAN-07
10184|Larapinta Group|61518|5|Briefly described|Map Legend|Ordovician|Cambrian|Geological Province: Amadeus Basin.||||||
10184|Larapinta Group|61519|5|Briefly described|Map Legend|Ordovician|Ordovician|Geological Province: Amadeus Basin.||||||
10184|Larapinta Group|62376|5|Briefly described|p18|Early Devonian|Late Cambrian|Geological Province: Amadeus Basin.||||||09-FEB-10
10184|Larapinta Group|62379|5|Briefly described|p7 Fig. 2|Devonian|Late Cambrian|Geological Province: Amadeus Basin.||||||
10184|Larapinta Group|62609|5|Briefly described|Map Legend|Ordovician|Cambrian|Siltstone, sandstone, limestone, dolomite, phosphorite. Underlies: Mereenie Sandstone. Overlies: Pertaoorrta Group.||||||14-AUG-06
10184|Larapinta Group|62620|5|Briefly described|Map Legend|Ordovician|Cambrian|Siltstone, sandstone, limestone, dolomite, phosphorite.||||||
10184|Larapinta Group|62794|5|Briefly described|p288, p289 Fig.2, p290|Ordovician|Late Cambrian|In Amadeus Basin, southern Northern Territory. Over 2100 m thick. Comprises (in ascending order) Pacoota Sandstone, Horn Valley Siltstone, Stairway Sandstone, Stokes Siltstone, Carmichael Sandstone.||||||
10184|Larapinta Group|62982|5|Briefly described|p7|Late Ordovician|Late Cambrian|Includes the Pacoota Sandstone at its base. Thick marine deposits. Geological Province: Amadeus Basin. Hosts two producing oil and gas fields.||||||16-JAN-07
10184|Larapinta Group|63562|6|Mentioned|p348-349|Middle Ordovician|Late Cambrian|Of Amadeus Basin.|||Includes Pacoota and Stairway Sandstones, and Horn Valley and Stokes Siltstones.|||
10184|Larapinta Group|64334|5|Briefly described|p37, 40, 42, 45, 47|Ordovician|Late Cambrian|Prichard and Quinlan (1962). Originally the Larapintine Series of Tate (1896), using the Aboriginal name for the Finke River. Mostly shallow-marine. Up to 2300m thick.|||Pacoota, Carmichael Sandstones; Horn Valley, Stairway, Stokes Siltstones.|Unconformably overlies Pertaoorrta Group.||
10184|Larapinta Group|64778|6|Mentioned|p12-13|Ordovician|Ordovician|Amadeus Basin. Post-Delamerian Orogeny sediments; thickening to N; over 2000m.||||||
10184|Larapinta Group|64809|6|Mentioned|p3 Fig.2, p6 Fig.4 |Early Devonian|Proterozoic||||Includes the Stairway Sandstone, Horn Valley Siltstone and Pacoota Sandstone.|||
10184|Larapinta Group|64970|6|Mentioned|p719 Fig. 2|Silurian|Ordovician|Geological Province: Amadeus Basin.||||||27-MAY-09
10184|Larapinta Group|65102|6|Mentioned|p363, Figure 4-38|Paleozoic|Paleozoic|Amadeus Basin.||||||
10184|Larapinta Group|65233|3|Fully described|p3 Fig. 2, p9|Silurian|Late Cambrian|Informally divided into Lower - Upper Larapinta Groups; upper comprises Carmichael and Mereenie Sandstones; lower consists of Pacoota and Stairway Sandstone, and Horn Valley and Stokes Siltstones. Unconformably overlies Goyder Formation. In Amadeus Basin.||||||16-JUL-13
10184|Larapinta Group|65256|5|Briefly described|p6 Tb.1, p24, p16, p19|Ordovician|Ordovician|White to red sandstone, locally bioturbated, minor siltstone, conglomeratic sandstone and limestone interbeds; fossiliferous. Onlaps Dean Quartzite; unconformably overlies Pottoyu Granite Suite; may directly overlie basement; locally overlies Winnall beds. Some sections contain angular clasts of Dean Quartzite. Includes Stokes Siltstone. >10m thick.||||||
10184|Larapinta Group|65272|6|Mentioned|p319, p320 Fig.3|Ordovician|Cambrian|Northern Amadeus Basin. Thick marine sequences coeval with the Larapinta Event.||||||
10184|Larapinta Group|65489|5|Briefly described|p125|Ordovician|Cambrian|Amadeus Basin.|||Includes Pacoota, Stairway and Carmichael Sandstones; Horn Valley and Stokes Siltstones.|Overlies Pertaoorrta Group.||
10184|Larapinta Group|66767|5|Briefly described|p60|Ordovician|Ordovician|NE Amadeus Basin.|||Horn Valley Siltstone.|Overlies Pertaoorta Group. Is overlain by Mereenie Sandstone.|Predominantly siliciclastic sedimentary rocks.|
10184|Larapinta Group|67326|5|Briefly described|p2-3|Early Devonian|Late Cambrian|Amadeus Basin.|||Pacoota, Stairway, Carmichael, Mereenie Sandstones; Horn Valley, Stokes Siltstones.|Overlies Pertaoorrta Group. Is overlain by Pertnjara Group.||
10184|Larapinta Group|67565|5|Briefly described|p5 Fig.3, pp41-42.|||Amadeus Basin.|||Includes Pacoota Sandstone, Horn Valley Siltstone, Stairway Sandstone, Stokes Siltstone, Carmichael Sandstone.|||03-DEC-15
10184|Larapinta Group|67856|5|Briefly described|p338 fig 4-30|Late Ordovician|Late Cambrian||||Includes Pacoota Sandstone, Horn Valley Siltstone, Stairway Sandstone, Stokes Siltstone, Carmichael Sandstone.|||
10184|Larapinta Group|68316|6|Mentioned|p779, p785|Ordovician|Ordovician|Amadeus Basin.||||||
10184|Larapinta Group|68323|6|Mentioned|p4 Fig.2|Early Devonian|Late Cambrian|Amadeus Basin.|||Pacoota, Stairway, Carmichael, Mereenie Sandstones; Horn Valley, Stokes Siltstones.|||
10184|Larapinta Group|69438|5|Briefly described|p23:2-5, 7-8, 20, 32-39, 46, 50, 60|Late Ordovician|Late Cambrian|Defined, as were its constituent Formations, by Pritchard and Quinlan (1962); after the Larapintine Series of Tate (1896). They included sandstone of the Carmichael Sandstone in the upper Stokes Siltstone (others mapped it as lower Mereenie Sandstone). Amadeus Basin.|||Pacoota, Stairway, Carmichael Sandstones; Horn Valley, Stokes Siltstones.|Is overlain disconformably by Dare Siltstone Member (Parke Siltstone).||12-JUL-16
10184|Larapinta Group|69444|6|Mentioned|p29:6|Ordovician|Ordovician|Amadeus Basin. Deposition was coincident with tectonism (the Larapinta Event) with peaks at 475 Ma and 460 Ma.||||||12-JUL-16
10184|Larapinta Group|69449|5|Briefly described|p34:4|Ordovician|Ordovician|Amadeus Basin.|||Pacoota Sandstone.|||12-JUL-16
10184|Larapinta Group|69458|6|Mentioned|p42:8|Ordovician|Ordovician|Amadeus Basin.||||||12-JUL-16
10184|Larapinta Group|69606|5|Briefly described|p4 fig 2|Ordovician|Cambrian|Misspelling of the Larapinta Group. Amadeus Basin. The carbonate shales and muds are potential source and seal rocks whilst the sandstones are potential reservoir rocks.||||Unconformably overlies the Upper Pertaoorta Group. Overlain by the Carmichael Sandstone.|Interbedded sandstone, carbonate, shale and marl.|
10184|Larapinta Group|69673|6|Mentioned|p66, p102, p103||||||Includes Pacoota Sandstone, Horn Valley Siltstone, Stairway Sandstone, Stokes Siltstone, Carmichael Sandstone|||
10184|Larapinta Group|70749|6|Mentioned|p54|||Amadeus Basin.|||Pacoota Sandstone.|||
10184|Larapinta Group|71146|5|Briefly described|p6|Wenlock|Cambrian|Amadeus Basin.|||Includes the Pacoota Sandstone, Horn Valley Siltstone, Stairway Sandstone, Stokes Siltstone and the Carmichael Sandstone.|Unconformably overlies the Pertaoorrta Group.|Sandstone, carbonate, mudstone and coal.|
10184|Larapinta Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, sandstone|
10184|Larapinta Group|71268|5|Briefly described|1m_geologyp12_lut.csv||||||||Marine sediments. White sandstone, locally bioturbated; minor siltstone and conglomeratic sandstone.|
10184|Larapinta Group|71279|5|Briefly described|p355 Fig.2, p363, p365, p374, p382 Tb.1|Early Devonian|Late Cambrian|Amadeus Basin. Modelled magnetic properties.|||Pacoota, Stairway, Carmichael, Mereenie Sandstones; Horn Valley, Stokes Siltstones.|||
10184|Larapinta Group|71898|5|Briefly described|iii, p1, p3, p17, p20-p22|||Amadeus Basin. Outcrops on the PALM VALLEY Sheet (5440) of the HENBURY Sheet (SG 53-01).|||Includes the Horn Valley Siltstone and the Pacoota Sandstone.|Overlies the Pertaoorrta Group.||19-NOV-18
10184|Larapinta Group|71965|6|Mentioned|p911|||Of Amadeus Basin.||||Correlable to Warratta Group.||
10184|Larapinta Group|72360|5|Briefly described|Map legend|Ordovician|Cambrian|Of Amadeus Basin.|||Includes Carmichael Sandstone, Stairway Sandstone, Horn Valley Siltstone and Pacoota Sandstone.|||09-SEP-19
10184|Larapinta Group|72369|5|Briefly described|iii,26,37|Devonian|Ordovician|Of Amadeus Basin.|||Includes Pacoota and Stairway sandstones, Stokes Siltstone, and the Carmichael and Mereenie sandstones, Parke Siltstone, Horn Valley Siltstone.|||
10184|Larapinta Group|72374|5|Briefly described|iii,p3,17|||Of Amadeus Basin.|||Layout implies includes Carmichael and Mereenie sandstones.|||11-OCT-19
10184|Larapinta Group|72476|6|Mentioned|p36 Fig.9|||Amadeus Basin. Time-temperature thermal history diagram.||||||
10184|Larapinta Group|73085|6|Mentioned|p1, p4|early Devonian|late Cambrian||||Mereenie Sandstone, Carmichael Sandstone, Stokes Siltstone, Stairway Sandstone, Horn Valley Siltstone, Pacoota Sandstone.|||
10184|Larapinta Group|73119|6|Mentioned|piii, p19|||Amadeus Basin, western.|||Stairway Sandstone|||
10184|Larapinta Group|73279|6|Mentioned|p10-14|Ordovician|Cambrian|Amadeus Basin.|||Pacoota Sandstone, Stairway Sandstone, Stokes Siltstone, Carmichael Sandstone|||
10184|Larapinta Group|73437|6|Mentioned|p152|||Apatite fission track cooling age of 341+/-58 Ma from Tingate, (1990).||||||
10261|Lawn Hill Formation|22453|6|Mentioned|p 12|||Geological Province: McArthur Basin.||||||13-OCT-06
10261|Lawn Hill Formation|22665|5|Briefly described|Table1 P222, P227||Calymmian|Actually spelt Lawn Hill Fmn.||||||13-OCT-06
10261|Lawn Hill Formation|22680|6|Mentioned|83,87|||Geol province Mount Isa Basin. Parent McNamara Group||||||
10261|Lawn Hill Formation|22747|5|Briefly described|p8||Precambrian|Conformably overlies Ploughed Mountain Beds||||||
10261|Lawn Hill Formation|23031|6|Mentioned|40|||Geol province Lawn Hill Subprovince. Of McNamara Group.||||||13-OCT-06
10261|Lawn Hill Formation|23072|5|Briefly described|p753-754||Proterozoic|||||||
10261|Lawn Hill Formation|23075|5|Briefly described|p730|||Of the McNamara Group.||||||
10261|Lawn Hill Formation|23362|6|Mentioned|339 Fig.2|||||||||
10261|Lawn Hill Formation|23363|5|Briefly described|351 Tab.1|Calymmian|Statherian|Ages: 1595+/-6Ma, 1593+/-8Ma.||||||13-OCT-06
10261|Lawn Hill Formation|23387|6|Mentioned|p18 fig.19|||Of McNamara Group.||||||
10261|Lawn Hill Formation|23393|4|Described|p21|Paleoproterozoic|Paleoproterozoic|Of McNamara Group.  Overlies the Termite Range Formation.  Geological Province: Lawn Hill Sub-province.||||||07-NOV-08
10261|Lawn Hill Formation|23396|4|Described|p421|||Of McNamara Group.||||||13-OCT-06
10261|Lawn Hill Formation|23397|5|Briefly described|p473|||||||||
10261|Lawn Hill Formation|23398|4|Described|p452|Calymmian|Statherian|Age: 1591+/-10Ma.||||||13-OCT-06
10261|Lawn Hill Formation|23405|4|Described|p566|Statherian|Statherian|Of McNamara Group. Age: 1593+/-8Ma.||||||13-OCT-06
10261|Lawn Hill Formation|23406|5|Briefly described|p606,p607 Fig. 8,  p616, p617|Statherian|Statherian|Of McNamara Group. Age: 1591+/-10Ma.||||||16-JUN-09
10261|Lawn Hill Formation|23407|5|Briefly described|p632|||||||||
10261|Lawn Hill Formation|23408|5|Briefly described|p513 Fig.2|||Of McNamara Group.||||||13-OCT-06
10261|Lawn Hill Formation|23409|5|Briefly described|p535 Fig.2|||Of McNamara Group.||||||13-OCT-06
10261|Lawn Hill Formation|23448|4|Described|p479|||Of McNamara Group.||||||13-OCT-06
10261|Lawn Hill Formation|23466|5|Briefly described|p272 Fig.6|Calymmian|Statherian|||||||
10261|Lawn Hill Formation|23958|3|Fully described|p1135|Mesoproterozoic|Paleoproterozoic|Of McNamara Group. Maximum thickness: 2200m.||||||07-NOV-08
10261|Lawn Hill Formation|23964|5|Briefly described|p1265|Proterozoic|Proterozoic|Of McNamara Group.  Geological Province: Mount Isa Inlier.  Maximum thicknees: 2200m.||||||
10261|Lawn Hill Formation|24308|5|Briefly described|p987 Fig. 2|Mesoproterozoic|Paleoproterozoic|Of the McNamara Group.   Geological Province:  Mount Isa Superbasin||||||07-NOV-08
10261|Lawn Hill Formation|24309|5|Briefly described|p1013|Proterozoic|Proterozoic|Of the McNamara Group.||||||13-OCT-06
10261|Lawn Hill Formation|24432|4|Described|p560 Tb.1, p562 Fig.2|Statherian|Statherian|Of McNamara Group. Overlies Termite Range Formation. Age: 1595+/-6 Ma. Siliclastic, carbonaceous and sideritic shale and siltstone. Geological Province: Lawn Hill Platform.||||||
10261|Lawn Hill Formation|24442|5|Briefly described|p23 Fig. 2|Mesoproterozoic|Mesoproterozoic|Of the McNamara Group.  Age: ~1590Ma.||||||
10261|Lawn Hill Formation|26310|4|Described|p4 Table 1|Proterozoic|Proterozoic|Sandstone, greywacke, shale. Maximum Thickness: 5000 feet. Underlies: Constance Sandstone (unconformably).||||||
10261|Lawn Hill Formation|30508|6|Mentioned|p94|||Stratigraphy||||||
10261|Lawn Hill Formation|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
10261|Lawn Hill Formation|31420|6|Mentioned|p216|||||||||
10261|Lawn Hill Formation|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10261|Lawn Hill Formation|32660|5|Briefly described|Table 5|||||||||
10261|Lawn Hill Formation|32959|6|Mentioned|Fig.21|||||||||
10261|Lawn Hill Formation|33387|4|Described|p350|||||||||
10261|Lawn Hill Formation|33900|5|Briefly described|p15|||||||||
10261|Lawn Hill Formation|35074|6|Mentioned|Fig.2|||||||||
10261|Lawn Hill Formation|35114|6|Mentioned|Fig.5|||||||||
10261|Lawn Hill Formation|36003|6|Mentioned|Fig.8|||||||||
10261|Lawn Hill Formation|37459|1|Redefined|p432|Mesoproterozoic|Mesoproterozoic|Age is more specifically Carpentarian.||||||23-DEC-08
10261|Lawn Hill Formation|37568|5|Briefly described|p84|||||||||
10261|Lawn Hill Formation|37569|5|Briefly described|p90|||||||||
10261|Lawn Hill Formation|38237|4|Described|p131|||See also Fig.3.||||||
10261|Lawn Hill Formation|38276|6|Mentioned|Fig.1|||||||||
10261|Lawn Hill Formation|38291|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10261|Lawn Hill Formation|38348|4|Described|p22|||||||||
10261|Lawn Hill Formation|38528|6|Mentioned|Fig.1|||||||||
10261|Lawn Hill Formation|38584|6|Mentioned|p22|||||||||
10261|Lawn Hill Formation|39422|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the McNamara Group.  Includes the Widdallion Sandstone Member.  Blocky to massive, thick-bedded, micaceous, cross-bedded medium quartz sandstone.  Conformably overlies the Plain Creek Formation; unconformably overlain by Constance Sandstone.||||||10-JAN-05
10261|Lawn Hill Formation|39445|5|Briefly described|Table 2|||||||||
10261|Lawn Hill Formation|39497|4|Described|p14|||See also Fig.4.||||||13-OCT-06
10261|Lawn Hill Formation|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10261|Lawn Hill Formation|39925|4|Described|p331|||||||||
10261|Lawn Hill Formation|42819|6|Mentioned|p312|||||||||
10261|Lawn Hill Formation|43611|6|Mentioned|p39||Mesoproterozoic|||||||
10261|Lawn Hill Formation|43615|6|Mentioned|p13|||||||||
10261|Lawn Hill Formation|43652|6|Mentioned|p388|||||||||
10261|Lawn Hill Formation|44210|14|Not recorded|p11|||||||||
10261|Lawn Hill Formation|44213|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
10261|Lawn Hill Formation|44238|14|Not recorded|p.221, Fig.1||Precambrian|Defn on Tech.File E/54-9.||||||
10261|Lawn Hill Formation|44271|2|Defined|p36,39,44,57,58|||Conformably overlies Ploughed Mountain Beds. Significant Pb-Zn mineralisation.||||||
10261|Lawn Hill Formation|44274|2|Defined|Tb.2,p9|||||||||
10261|Lawn Hill Formation|44275|14|Not recorded|Map Legend|||||||||
10261|Lawn Hill Formation|44280|14|Not recorded|p6|||||||||
10261|Lawn Hill Formation|44281|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
10261|Lawn Hill Formation|44290|14|Not recorded|p438,439|||Precambrian possibly Palaeoproterozoic.||||||
10261|Lawn Hill Formation|44305|14|Not recorded|p.8|||(E53-8).||||||
10261|Lawn Hill Formation|44482|14|Not recorded|p.6|||(E53-12).||||||
10261|Lawn Hill Formation|44521|14|Not recorded|p8|||Upper Paleoproterozoic.||||||
10261|Lawn Hill Formation|44765|14|Not recorded|p14|||||||||
10261|Lawn Hill Formation|44919|14|Not recorded|p596 (Tb.),p600|||Top of Carpentarian||||||
10261|Lawn Hill Formation|44922|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of McNamara Group.||||||
10261|Lawn Hill Formation|44989|2|Defined|p.110-112|||Tb. III,IV. On many pages. Underlies Ploughed Mountain Beds. May be roughly equivalent to Cliffdale Volcanics. 2000-5000?' (E54-9).||||||
10261|Lawn Hill Formation|45079|6|Mentioned|p9|||Precambrian age. Map legend P9||||||
10261|Lawn Hill Formation|45166|5|Briefly described|p30|||||||||
10261|Lawn Hill Formation|45287|14|Not recorded|p.225-7,229|||Overlain by Constance Sandstone.||||||
10261|Lawn Hill Formation|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
10261|Lawn Hill Formation|46919|6|Mentioned|p218|||||||||
10261|Lawn Hill Formation|50550|5|Briefly described|p1139 Fig.2||Statherian|Age: 1595-1630 Ma.Conformably overlies Termite Range Formation. Geological Province: Western Fold Belt.||||||17-DEC-07
10261|Lawn Hill Formation|50600|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the McNamara Group.  Sandstone and conglomeratic sandstone; flaggy tuff and tuffaceous siltstone; carbonaceous shale, micaceous siltstone.||||||
10261|Lawn Hill Formation|60558|5|Briefly described|p5 Fig. 4|||Of McNamara Group. Underlain by Termite Range Formation.||||||03-JUN-09
10261|Lawn Hill Formation|61904|5|Briefly described|p132 Fig. 2|Proterozoic|Proterozoic|Youngest member of the McNamara Group. Includes Bulmung Sandstone Member. Laminated siltstone. Geological Province: Western Fold Belt of Mt. Isa Inlier.||||||
10261|Lawn Hill Formation|61936|5|Briefly described|p194 Fig. 6|||Geological Province: Calvert Superbasin, Western Fold Belt, Mount Isa Inlier.||||||
10261|Lawn Hill Formation|62084|4|Described|p936 Fig.5, p945-946, p949|Proterozoic|Proterozoic|Isa Superbasin. Lawn Hill. Hosts Century deposit (Zn-Pb-Ag stratiform). Age: 1595+/-6 Ma, U-Pb SHRIMP (Page and Sweet 1998). Shown as Lawn Hill Fm. Thickness: 1800-2200 m. Six sedimentary units H1-H6, where H4 is 300 m-thick mineralised sequence.|1611+/-4 U-Pb SHRIMP (after Page et al. 2000)|McNamara Group|||Variably dolomitic organic siltstones and shales. Shale, siltstone, sandstone, tuffaceous rocks, and minor dolomite.|
10261|Lawn Hill Formation|62659|5|Briefly described|Map Legend|Calymmian|Statherian|Of the McNamara Group. Interlaminated and thinly interbedded red, grey and brown siltstone and fine grained sandstone; green to grey shale and siltstone, dolomitic siltstone, dolostone.||||||
10261|Lawn Hill Formation|63109|6|Mentioned|p1108 Fig. 3|||Geological Province: Isa Superbasin. Consists of shale.||||||30-SEP-08
10261|Lawn Hill Formation|63110|6|Mentioned|p1141 Fig. 17|Statherian|Calymmian|Age: ~ 1629-1580Ma. Geological Province: Isa Superbasin.||||||11-JUN-08
10261|Lawn Hill Formation|63111|5|Briefly described|p1164 Tb. 1, p1163 Fig. 3|Calymmian|Statherian|Of Doom Supersequence.Age: ca. 1575Ma. Thickness: 600-1050m. Geological Province: Isa Superbasin. Consists of volcanic detritus arkose, mudstone, sandstone siltstone, and silty shales.||||||07-FEB-11
10261|Lawn Hill Formation|63113|5|Briefly described|p1214 Fig.2, p1219 Fig.8, p1225 Fig.13. |||Part of Lawn, Wide and Doom supersequences.|c.1615-1589 Ma.|Of the McNamara Group||Overlies Termite Range Formation or Riversleigh Siltstone. Is overlain by Allaru Mudstone.||
10261|Lawn Hill Formation|63114|5|Briefly described|p1253 Fig.2, p1254, p1258. |Proterozoic|Proterozoic|Isa Superbasin. Hosts the stratiform Century Zn-Pb-Ag deposit/Watson's lode.|1595 Ma.|Of the Term, Lawn, Wide and Doom supersequences|||Includes a 45m-thick interlayered black shale and siltstone sequence.|06-APR-17
10261|Lawn Hill Formation|63115|6|Mentioned|p1279 Fig.4.|||Isa superbasin.||||||
10261|Lawn Hill Formation|63116|6|Mentioned|p1297 Fig.2, p1299 Tb.1, p1300|||Isa superbasin. Material properties detailed.||||||
10261|Lawn Hill Formation|63866|5|Briefly described|p57|Statherian|Statherian|Isa Superbasin. Subdivided into two units in the Term Supersequence and transitional between the Term and Lawn Supersequences.|c. 1636-1611 Ma|||||
10261|Lawn Hill Formation|64250|6|Mentioned|p11 fig 3, p20||||1611 +/- 4 Ma - 1595 +/- 6 Ma|Unit in McNamara Group.||||
10261|Lawn Hill Formation|64317|5|Briefly described|p588 Fig. 1, p589, p595|Mesoproterozoic|Mesoproterozoic|Age for upper section of unit: 1593+/-8Ma. Mainly quartzite, carbonaceous shale and silt/mudstone. Also refers to the 'upper Lawn Hill Formation' which hosts the Century mine.||||||23-SEP-08
10261|Lawn Hill Formation|64575|5|Briefly described|p655, p656 Fig. 1, p657, p664, p665|Proterozoic|Proterozoic|Thickness: >850m. Thick sequence of siltstone, shale and sandstone. Host Century mineralisation.||||||
10261|Lawn Hill Formation|65228|5|Briefly described|p35, Fig.04.|||Lower part of this unit is in the Term Supersequence in the southern Lawn Hill Platform. The upper part is in the Wide Supersequence.||||Overlies Termite Range Formation.||
10261|Lawn Hill Formation|65337|3|Fully described|p9 Fig.5, p29, p33.|Paleoproterozoic|Paleoproterozoic|Formerly Bluff Range beds (Smith and Roberts 1963). 125 - 2600 m of storm-dominated shelf deposits. In Queensland, hosts the world-class Century Zn-Pb-Ag deposit.|c.1616 - c.1595 Ma.|Unit in McNamara Group.|Includes Bulmung and Widdallion Sandstone Members.|Overlies Plain Creek Formation. Is overlain by Playford Sandstone.|Interlaminated and thinly interbedded red, grey and brown siltstone and fine-grained sandstone; green to grey shale and siltstone, dolomitic siltstone, laminated and intraclastic dolostone; distinctive sandstone unit at top.|13-APR-17
10261|Lawn Hill Formation|65396|5|Briefly described|p82, p175, p188, p241|Calymmian|Statherian|Isa Superbasin. Cover Sequence 3. Lawn Hill Platform.|1611 +/- 4 Ma, 1595 +/- 6 Ma|McNamara Group||Overlies Termite Range Formation.||04-APR-17
10261|Lawn Hill Formation|66843|5|Briefly described|p36, p38 Fig.10, p39|||||McNamara Group.|||Includes a basal feldspathic sandstone.|
10261|Lawn Hill Formation|67323|4|Described|Solid Geology Map, p10|Calymmian|Statherian|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Camooweal-Murphy and Century Domains, Mount Isa Inlier. Youngest unit in Isa Superbasin sequence. Hosts Zn-Pb Century Mine.|1616 +/- 5 Ma and 1595 +/- 6 Ma.|McNamara Group.|Bulmung Sandstone Member, Widdallion Sandstone Member.||Siltstone, shale, tuff, minor sandstone and dolomite.|
10261|Lawn Hill Formation|68542|5|Briefly described|p4, p6 |||Lawn Hill Platform.|1595 Ma|Upper McNamara Group|||Carbonaceous shale, siltstone and sandstone.|
10261|Lawn Hill Formation|68576|4|Described|Q_2: p4, p6|||Lawn Hill Platform, Mount Isa Inlier. Hosts the Century Zn deposit (described in detail), and the Zinc Hills Lodes Zn-Pb-Ag deposit.|1595 Ma.|Upper McNamara Group.||Overlies Termite Range Formation. Is overlain unconformably by South Nicholson Group.|A sequence of shale, siltstone and sandstone.|
10261|Lawn Hill Formation|68732|6|Mentioned|p165 Fig.3|||Lawn Hill Platform, Western Fold Belt. Of the Doom Supersequence, Wide Supersequence, Lawn Supersequence, and Term Supersequence. Sedimentary depositional ages.|1595 +/- 6, 1611 +/- 4, 1616 +/- 5 Ma|||||
10261|Lawn Hill Formation|69430|5|Briefly described|p15:39|Proterozoic|Proterozoic|Turbiditic siliciclastic black shale and siderite-rich siltstone host the stratiform Zn-Pb-Ag Century deposit.|||||A succession of shale, siltstone and sandstone.|12-JUL-16
10261|Lawn Hill Formation|69433|4|Described|p18:2, 6, 10|Statherian|Statherian|Sweet (1984); previously mapped as Bluff Range beds (Smith and Roberts, 1963). Southern succession, Lawn Hill Platform. 175-2970m thick, thinning to the N. Marine shelf, mainly below wave-base, deposits. Hosts the world-class Century Zn-Pb-Ag deposit in Qld.; the unit's extension into NT should be considered prospective.||Topmost McNamara Group.|Widdallion Sandstone Member.|Conformably overlies Plain Creek Formation. Is overlain by South Nicholson Group disconformably or locally unconformably.|Recessive, interlaminated and thinly interbedded, grey, green, and red, variably leached, shale, siltstone, very fine-grained sandstone, dolostone and dolomitic siltstone.|12-JUL-16
10261|Lawn Hill Formation|69443|5|Briefly described|p28:19|||Lawn Hill Platform.||McNamara Group.||Is overlain unconformably by Border Waterhole Formation.||12-JUL-16
10261|Lawn Hill Formation|69591|4|Described|p43 Fig.2.31, p47, p54|||Camooweal-Murphy and Century Domains, Isa Superbasin. Constitutes the Lawn, Wide and Doom Supersequences, separated by disconformities. Deep-marine and proximal submarine fan deposits. Grades downwards into coarser-grained turbidites of Termite Range Formation.|Lower: 1611 +/- 4 Ma (Page et al., 2000).|McNamara Group.||Overlies Termite Range Formation.|Dominantly fine-grained: siltstone, shale, tuff, minor sandstone and dolomite.|
10261|Lawn Hill Formation|69673|4|Described|p52 fig 42, p54, p55|||Up to 2600m thick. Deposited in a marine shelf environment, mainly below wave base. High enough TOC in QLD to be considered valid source rock. Unconventional petroleum potential.||McNamara Group|||Shale, siltstone, very fine grained sandstone, dolostone and dolomitic siltstone.|
10261|Lawn Hill Formation|70897|5|Briefly described|p39-40, Fig.1.7.7|Mesoproterozoic|Mesoproterozoic|Carrara Range region. Age for the H4s siltstone member. Source of abundant reworked sediment, as well as 1591 +/- 10 Ma detrital zircons, in overlying Constance Sandstone.|1595 +/- 6 Ma (Page and Sweet, 1998).|||Is overlain by Constance Sandstone with an angular unconformity (locally disconformably).||
10261|Lawn Hill Formation|71369|5|Briefly described|p4, p8, p13|Calymmian||Age derived from Page et al (2000) who interprets it as the depositional age of tuffs in this unit.|1591 +/- 10 Ma (U-Pb zircon)||Widdallion Sandstone Member.|Is overlain unconformably by Hedleys Sandstone. Is locally overlain by Burangoo Sandstone.||20-FEB-18
10261|Lawn Hill Formation|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1595+/-6 Ma (crystallisation: U-Pb zircon SHRIMP)||||Siltstone, tuffaceous siltstone.|
10261|Lawn Hill Formation|71863|6|Mentioned|p2|Proterozoic|Proterozoic|Isa Superbasin.||||||
10261|Lawn Hill Formation|72408|4|Described|map sheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet.||Unit of McNamara Group.|Includes Widdallion Sandstone Member, Bulmung Sandstone Member.||Siltstone, shale, tuf, minor sandstone, dolomite.|
10261|Lawn Hill Formation|72414|4|Described|map sheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.||Unit of McNamara Group.|Includes Widdallion Sandstone Member, Bulmung Sandstone Member.||Siltstone, shale, tuf, minor sandstone, dolomite.|
10261|Lawn Hill Formation|72415|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.||Unit of McNamara Group.|Includes Widdallion Sandstone Member, Bulmung Sandstone Member.||Siltstone, shale, tuf, minor sandstone, dolomite.|
10261|Lawn Hill Formation|72416|4|Described|map sheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet Geological Compilation Series.||Unit of McNamara Group.|Includes Widdallion Sandstone Member, Bulmung Sandstone Member.||Siltstone, shale, tuf, minor sandstone, dolomite.|
10261|Lawn Hill Formation|72418|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet.||Unit of McNamara Group.|Incldues Widdallion Sandstone Member, Bulmung Sandstone Member.||Siltstone, shale, tuff, minor sandstone and dolomite|
10261|Lawn Hill Formation|72421|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.||Unit of McNamara Group.|Incldues Widdallion Sandstone Member, Bulmung Sandstone Member.||Siltstone, shale, tuff, minor sandstone and dolomite|
10261|Lawn Hill Formation|72422|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.||Unit of McNamara Group.|Incldues Widdallion Sandstone Member, Bulmung Sandstone Member.||Siltstone, shale, tuff, minor sandstone and dolomite|
10261|Lawn Hill Formation|72423|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet Geological Compilation Series. Lithology of numerous other outcrops provided.||Unit of McNamara Group.|Incldues Widdallion Sandstone Member, Bulmung Sandstone Member.||Siltstone, shale, tuff, minor sandstone and dolomite|18-MAR-20
10261|Lawn Hill Formation|72526|5|Briefly described|p8 Fig.1.3.|Calymmian|Statherian|Shown as located in the Lawn Hill Platform of the Mount Isa Province and the east part of the South Nicholson Basin. Three ages given as U-Pb zircon sedimentary depositional ages determined from lower and upper parts of the unit in Qld. Base of formation shown as older in NT than Qld.|1615 +/- Ma to 1595 +/- 6 Ma|McNamara Group||Overlies Plain Creek Formation, Termite Range Formation.||
10261|Lawn Hill Formation|72527|5|Briefly described|p7 Fig.1.4, p10, p27, p119, p132.|Paleoproterozoic|Paleoproterozoic|A tuff from the uppermost part of this unit yielded an interpreted magmatic age of 1595 ± 6 Ma. i.e. a minimum age for Lawn Hill Formation. See also p140, p194.|min age from tuff: 1595+/-6 Ma.|McNamara Group||Overlies Plain Creek Formation and underlies Widdallion Sandstone Member. Underlies South Nicholson Group.|Includes tuffs.|
10261|Lawn Hill Formation|72912|4|Described|p5 Fig.3, p14, p32, p33 Fig.12.|Statherian|Statherian|Shown as being located in both Queensland and Northern Territory. Base of unit shown as older in NT. Located in the Lawn Hill Platform of the Mount Isa Province, and the East part of the South Nicholson Basin.  Three U-Pb zircon sedimentary depositional ages [?] given, also including 1615+/-5 Ma (lower). See also p45-46.|1595+/-6 Ma (upper), 1611+/-4 Ma (lower)|McNamara Group||Overlies Plain Creek Formation (NT) and overlies Termite Range Formation (Qld). Partially equivalent to Doomadgee Formation and Mount Les Siltstone.|Includes organic rich siltstone.|
10261|Lawn Hill Formation|72913|5|Briefly described|p4,7,8, 9 Tb.1, p18, 19 Fig.11, p20,26.|Paleoproterozoic|Paleoproterozoic|Shown as being in the eastern and Lawn Hill Platform part of the Isa Superbasin. Identified in 6 wells in this study. Associated with a gas discovery (Egilabria 2). Mineral composition shows majority quartz, microcline, muscovite, calcite and dolomite.|1611 +/- 4 Ma|McNamara Group||Overlies Termite Range Formation.|Include organic rich siltstone.|
10261|Lawn Hill Formation|72919|6|Mentioned|p5|Paleoproterozoic|Paleoproterozoic|||McNamara Group||Underlain by Plain Creek Formation. Probably includes Widdallion Sandstone Member.||
10261|Lawn Hill Formation|72967|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|Lawn Hill Platform.||McNamara Group||||
10261|Lawn Hill Formation|73042|6|Mentioned|p4, p13-14||Statherian|South Nicholson Basin region and Mount Isa Province, Isa Superbasin. Geochronology is a U-Pb zircon sedimentary depositional age (?maximum depositional age) (see Fig.1.2).|ca 1615-1595 Ma|McNamara Group||Underlain by Plain Creek Formation and Termite Range Formation. Overlain by(?) Widdallion Sandstone Member and unconformably by South Nicholson Group.||
10261|Lawn Hill Formation|73043|6|Mentioned|p15 Fig.8|Paleoproterozoic|Paleoproterozoic|||||||
10261|Lawn Hill Formation|73098|6|Mentioned|p4, p7, p33|||Lawn Hill Platform. Organic petrolography performed on three samples from the Amoco DDH 83-2 well. [See report for bitumen/maceral description].|||||Includes dark grey shale.|
10261|Lawn Hill Formation|73144|6|Mentioned|p8-9|Calymmian|Statherian|Isa Superbasin. Split across the Doom, Wide, Lawn and Term supersequences. Includes aquifers, partial aquifers, leaky aquitards and aquitards. Includes potential shale gas/oil plays and potential tight gas/oil. Includes oil show and gas discovery in subunit denoted as lower Pmh 4.||McNamara Group|Widdallion Sandstone Member, Bulmung Sandstone Member|Underlain by Termite Range Formation.||14-OCT-22
10289|Ledan Schist|9394|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block (Division 3). Biotite-muscovite-quartz schist, minor metaconglomerate.||||||
10289|Ledan Schist|23732|5|Briefly described|p28 Fig.26|Mesoproterozoic|Paleoproterozoic|Geological Province: Arunta Province.||||||07-NOV-08
10289|Ledan Schist|23733|5|Briefly described|p34 Fig.20|||||||||
10289|Ledan Schist|23868|5|Briefly described|p753 Fig. 10|Proterozoic|Proterozoic|Geological Province: Arunta Inlier.||||||21-SEP-09
10289|Ledan Schist|24047|5|Briefly described|p7 Fig. 6|Paleoproterozoic|Paleoproterozoic|Age: 1770Ma.  Geological Province: Arunta Province.||||||07-NOV-08
10289|Ledan Schist|33102|5|Briefly described|p440|||||||||
10289|Ledan Schist|33103|4|Described|Table 1|||Mention p14.||||||13-OCT-06
10289|Ledan Schist|33104|6|Mentioned|Map legend|Precambrian|Precambrian|||||||
10289|Ledan Schist|39887|6|Mentioned|Fig.5|||||||||
10289|Ledan Schist|39888|6|Mentioned|Appendix|||Published isotopic ages.||||||
10289|Ledan Schist|40538|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Block.||||||07-NOV-08
10289|Ledan Schist|40906|4|Described|p11|||||||||
10289|Ledan Schist|42643|4|Described|p5, Table 1 p10|||||||||
10289|Ledan Schist|42644|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Quartz-mica schist, metamorphosed rhyolite-dacite, quartzite, minor cherty tuff, minor conglomerate, amphibolite. Geological Province: Arunta Inlier.||||||07-NOV-08
10289|Ledan Schist|43568|6|Mentioned|Fig.4,p506|||||||||
10289|Ledan Schist|48992|6|Mentioned|p63|||||||||
10289|Ledan Schist|48997|6|Mentioned|Fig.2|||||||||
10289|Ledan Schist|61208|5|Briefly described|p208, p207 Fig. 1|Late Neoproterozoic|Paleoproterozoic|Predominantly coarse-grained musc+qtz +/-bio schist, minor qtzite and amphibolite, overlying basal conglomerate. Unconformably overlies Delny Gneiss and Delmore Metamorphics; underlies (disconformably?) Utopia Quartzite. Geol. Prov: eastern Arunta Inlier.||||||23-DEC-08
10289|Ledan Schist|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|In Tennant Creek region.||||||07-NOV-08
10289|Ledan Schist|62636|6|Mentioned|Map Legend|||Possible equivalent to a pelitic migmatite in Mount Theo sheet area. Solid Geology legend.||||||
10289|Ledan Schist|64068|5|Briefly described|p32|||Bundled in with Mendip Metamorphics and Utopia Quartzite as the 1770-1740 Ma Ledan package.||||||
10289|Ledan Schist|64574|6|Mentioned|p704 Fig. 1|Paleoproterozoic|Paleoproterozoic|||||||
10289|Ledan Schist|64738|6|Mentioned|p250 Table 1.|Paleoproterozoic|Paleoproterozoic|Pegmatite crystallisation 1730 +/- 4 Ma.||||||
10289|Ledan Schist|65209|6|Mentioned|p35 Fig.1|Paleoproterozoic|Paleoproterozoic|Encompassed by informal Lower Wauchope Subgroup.||Wauchope Subgroup||||05-JAN-17
10289|Ledan Schist|65341|5|Briefly described|p2 Fig.2, p7. |Paleoproterozoic|Paleoproterozoic|Considered part of same sedimentary package as Mendip Metamorphics and Utopia Quartzite.|Detrital zircon c.1780 Ma (Maidment et al. 2005).|||Is overlain by Utopia Quartzite.||19-JUN-13
10289|Ledan Schist|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.|||||Quartz-mica schist, metamorphosed rhyodacitic volcanics; quartzite; minor cherty tuff and conglomerate; amphibolite.|
10289|Ledan Schist|67181|5|Briefly described|p631|Statherian|Statherian|Aileron Province, North Australian Craton|1770-1730 Ma (Maidment et al. 2005)|Unit in Ledan Package||||
10289|Ledan Schist|67323|6|Mentioned|Eastern Australia Time-Space Plot|||Arunta Block.||||||
10289|Ledan Schist|68150|5|Briefly described|p11 Tb.3.2|||Age: SHRIMP, MSWD 1, 24 analyses, Maidment et al. (2005).|1730 +/- 4 Ma, pegmatite crystallisation|||||
10289|Ledan Schist|69383|4|Described|p81-82, 67, 70, 73||Paleoproterozoic|Arunta region, Aileron Province. SHRIMP U-Pb and Hf geochronology analyses.  Max deposition age poorly constrained.|ca 1775 Ma (Maidment 2005)|Of Ledan Package.||Overlain by Utopia Quartzite. Correlative of Mendip Metamorphics.|Coarse-grained muscovite +quartz +/- biotite schist, with minor quartzite and amphibolite. Quartzite sampled.|
10289|Ledan Schist|69417|6|Mentioned|p2:5|Statherian|Statherian|S and E Aileron Province.||||||12-JUL-16
10289|Ledan Schist|69427|4|Described|p12:3, 33-34|Statherian|Statherian|Shaw and Warren (1975). Crops out in a NW-trending belt between Mount Tops and Delmore Downs homestead, N of the Delny Shear Zone, Aileron Province. Poorly defined maximum depositional age: SHRIMP U-Pb detrital zircons.|< c.1780-1770 Ma (Maidment et al., 2005).|||Unconformably overlies Delny Metamorphics. Is overlain disconformably by Utopia Quartzite.|Upper greenschist to lower amphibolite facies succession of muscovite-quartz +/- biotite schist, with lesser quartzite, tourmaline-rich quartzite, amphibolite and a basal conglomerate.|12-JUL-16
10289|Ledan Schist|69431|6|Mentioned|p16:1|||Arunta Region. Possible correlative of Hatches Creek Group and, by inference, Tomkinson Creek Group.||||||12-JUL-16
10289|Ledan Schist|69554|6|Mentioned|p139|||Aileron Province, Arunta Region, Northern Australian Craton. Contains detrital zircons aged c.1920 Ma.||||||
10289|Ledan Schist|71348|6|Mentioned|p201|Statherian|Statherian|Geological province: Aileron Province, Arunta Region.||||||
10289|Ledan Schist|71592|5|Briefly described|Appendix A.|||Arunta Orogen.|||||Schist.|
10289|Ledan Schist|72516|6|Mentioned|p9, p192|||Aileron Province. Maximum depositional age ca 1810 Ma (Reno pers comm)||||Possible age equivalent to Bonya Metamorphics.||27-MAY-21
10289|Ledan Schist|73083|6|Mentioned|p11|Statherian|Statherian|Deposited between ca 1770-1750 Ma. Not equivalent to Ooradidgee Group, Lander Rock Formation, or Hatches Creek Group.|1770-1750 Ma|||||
10289|Ledan Schist|73591|6|Mentioned|p33-34|||||Deep Bore Metamorphics|||Schist.|
10294|Lees Sandstone|30914|6|Mentioned|Map legend|Cretaceous|Jurassic|Jurassic - Cretaceous||||||
10294|Lees Sandstone|33164|6|Mentioned|p87|||Correlation. Refers Skwarko (1966).||||||13-OCT-06
10294|Lees Sandstone|33165|6|Mentioned|Chart|||Correlation chart only||||||
10294|Lees Sandstone|39445|5|Briefly described|Table 10|||||||||
10294|Lees Sandstone|39523|6|Mentioned|p96|||||||||
10294|Lees Sandstone|44213|14|Not recorded|Map Legend||Late Jurassic|||||||
10294|Lees Sandstone|44989|14|Not recorded|Not recorded|||||||||
10294|Lees Sandstone|45011|4|Described|p9,19,20,22,30|Aptian|Neocomian|On QLD and NT cards. Underlies Polland Shale. Outcrops from Qld border to Pine Creek and beyond.||||||
10294|Lees Sandstone|67323|6|Mentioned|GIS attrib tbl; p106|||informally grouped with Mullaman beds.||||||
10294|Lees Sandstone|68135|5|Briefly described|p52 fig 2b|Early Cretaceous|Tithonian|Carpentaria Basin. Contains plant macrofossils.||||Overlies Hampstead Sandstone|Cross-bedded sandstone.|14-SEP-17
10294|Lees Sandstone|68553|6|Mentioned|Map legend; schematic diagram.|Early Cretaceous|Jurassic|Carpentaria Basin. This unit is mapped with Mullaman beds, and unnamed sedimentary units, under the symbol, JKm.||||||
10294|Lees Sandstone|69056|6|Mentioned|Reference images sheet.|||Shown on the simplified surface geology maps of the Quamby Project area; mapped as one unit with Mullaman beds and unnamed sediments.||||||
10294|Lees Sandstone|69594|6|Mentioned|p522|||Occurs on the CAMOOWEAL and MOUNT ISA 250k sheets. Known from the NT. Overlies Precambrian and Cambrian basement. Non-marine.||||||
10294|Lees Sandstone|73137|6|Mentioned|p6|Early Cretaceous|Jurassic|||||||
10303|Legune Formation|22547|5|Briefly described|p24|||Of Fitzmaurice Group. Overlies Lalngang Formation. Correlates with Pincombe Formation||||||13-OCT-06
10303|Legune Formation|32307|4|Described|Table 2|||Proterozoic||||||
10303|Legune Formation|32310|6|Mentioned|Map legend|Adelaidean|Carpentarian|Adelaidean/Carpentarian||||||
10303|Legune Formation|32660|5|Briefly described|Table 6|||||||||
10303|Legune Formation|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Fitzmaurice Group.  Quartz sandstone and siltstone.||||||02-DEC-04
10303|Legune Formation|32701|4|Described|Table 1|||Adelaidean. See also p7. Of Fitzmaurice Gp.||||||13-OCT-06
10303|Legune Formation|32728|6|Mentioned|Fig.14|||||||||
10303|Legune Formation|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
10303|Legune Formation|37462|6|Mentioned|Fig.4.13|||||||||
10303|Legune Formation|39827|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
10303|Legune Formation|40494|4|Described|p11|||||||||
10303|Legune Formation|41645|6|Mentioned|p15|||||||||
10303|Legune Formation|45112|6|Mentioned|Table 16|||||||||
10303|Legune Formation|48938|2|Defined|p19|Proterozoic|Proterozoic|See also pp20-21. Measured section p88.||||||13-OCT-06
10303|Legune Formation|48942|3|Fully described|p37|||||||||
10303|Legune Formation|60006|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: ? Halls Creek Orogen. Of Fitzmaurice Group. Silica cemented quartz sandstone, siltstone.||||||
10303|Legune Formation|60682|4|Described|p5|Mesoproterozoic|Mesoproterozoic|Of Fitzmaurice Group. Thickness: >600m. Overlies Lalngang Formation (conformable) and Whitewater Volcanics (unconformable). Geological Province: Halls Creek Orogen. Medium grained quartz sandstone, siltstone, fine grained sandstone.||||||04-MAY-05
10303|Legune Formation|64698|4|Described|lithinterp table|||Age ~1150-1250Ma (Stenian) but age name given as Statherian.Of Fitzmaurice Group. Max. thickness 600m. Silica cemented quartz sandstone, siltstone. Conformably overlies Lalngang Sandstone (and other misspellings).||||||07-JAN-09
10303|Legune Formation|65331|5|Briefly described|Map legend|Mesoproterozic|Mesoproterozic|Of Fitzmaurice Group, ?Halls Creek Orogen. Silica cemented quartz sandstone, siltstone||||||
10303|Legune Formation|65417|5|Briefly described|p158 Fig.2, p159, pp162-163.|Mesoproterozoic|Mesoproterozoic|Fitzmaurice Mobile Zone. Correlated with the Pincombe Formation of the Carr Boyd Group (Halls Creek Orogen).||Topmost unit in Fitzmaurice Group.||Conformably overlies Lalngang Sandstone.||
10303|Legune Formation|69435|4|Described|p20:2-6|||Sweet et al. (1974). Fitzmaurice Basin. Exposed over a large area.||Fitzmaurice Group.||Conformably and gradationally overlies Lalngang Sandstone. Unconformably overlies Whitewater Volcanics.|Generally consists of monotonous medium-grained silica-cemented quartz sandstone / quartzite. Some beds can be traced up to 20km; others show lateral facies variations. Localised ferruginous phases are associated with groundwater movement.|12-JUL-16
10303|Legune Formation|69452|6|Mentioned|p36:10 Fig.36.7|Mesoproterozoic|Paleoproterozoic|Fitzmaurice Basin. Minimum age given as ?Mesoproterozoic.||||||12-JUL-16
10303|Legune Formation|69673|5|Briefly described|p59, p60 fig 48|||Up to 600m thick.||Fitzmaurice Group||Overlies Lalngang Sandstone|Silica cemented quartz sandstone or quartzite.|
10303|Legune Formation|70206|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Fitzmaurice Basin.||Fitzmaurice Group|||Silica cemented quartz sandstone, siltstone.|
10303|Legune Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, sandstone|
10303|Legune Formation|73083|6|Mentioned|p8|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||||||
10337|Lena Quartzite Member|23031|6|Mentioned|24|Paleoproterozoic|Paleoproterozoic|Geol. province: Mount Isa Fold Belt. Of the Eastern Creek Volcanics.||||||07-NOV-08
10337|Lena Quartzite Member|23073|6|Mentioned|p745|||||||||
10337|Lena Quartzite Member|23395|5|Briefly described|p386 Fig.3|||Of Eastern Creek Volcanics.||||||13-OCT-06
10337|Lena Quartzite Member|23399|5|Briefly described|p501|||||||||
10337|Lena Quartzite Member|23965|5|Briefly described|p1296|Paleoproterozoic|Paleoproterozoic|Of Eastern Creek Volcanics.  Geological Province: Mount Isa Inlier.||||||07-NOV-08
10337|Lena Quartzite Member|24033|5|Briefly described|p5|||Of Eastern Creek Volcanics. Includes quartzite, feldspathic quartzite and siltstone.||||||
10337|Lena Quartzite Member|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Eastern Creek Volcanics. Overlies the Cromwell Metabasalt Member; underlies the Pickwick Metabasalt Member.||||||01-OCT-08
10337|Lena Quartzite Member|30534|2|Defined|p303|Carpentarian|Carpentarian|||||||
10337|Lena Quartzite Member|33900|5|Briefly described|p11|||||||||
10337|Lena Quartzite Member|34499|6|Mentioned|Table 11|||||||||
10337|Lena Quartzite Member|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10337|Lena Quartzite Member|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10337|Lena Quartzite Member|38232|6|Mentioned|p84|||||||||
10337|Lena Quartzite Member|38233|5|Briefly described|Table 1|||||||||
10337|Lena Quartzite Member|38234|6|Mentioned|p103|||||||||
10337|Lena Quartzite Member|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10337|Lena Quartzite Member|38560|6|Mentioned|p113|||||||||
10337|Lena Quartzite Member|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Eastern Creek Volcanics. Feldspathic quartzite, orthoquartzite.||||||15-JUN-06
10337|Lena Quartzite Member|39622|6|Mentioned|Appendix|||||||||
10337|Lena Quartzite Member|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
10337|Lena Quartzite Member|39934|6|Mentioned|p317|||||||||
10337|Lena Quartzite Member|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10337|Lena Quartzite Member|40221|3|Fully described|p7|||||||||
10337|Lena Quartzite Member|40598|6|Mentioned|Fig.2|||||||||
10337|Lena Quartzite Member|40623|5|Briefly described|p98|||||||||
10337|Lena Quartzite Member|41298|6|Mentioned|Map legend|Carpentarian||||||||
10337|Lena Quartzite Member|42782|6|Mentioned|p469|||Same as Lena Quartzite, Lena Member.||||||13-OCT-06
10337|Lena Quartzite Member|45161|6|Mentioned|p11|||||||||
10337|Lena Quartzite Member|45166|5|Briefly described|p15|||||||||
10337|Lena Quartzite Member|46801|6|Mentioned|p115|||See also Fig. 14.||||||13-OCT-06
10337|Lena Quartzite Member|47083|4|Described|p5-6||Proterozoic|Of Eastern Creek Volcanics (Haslingden Group). Maximum thickness: 200 m.||||||30-JAN-07
10337|Lena Quartzite Member|49009|6|Mentioned|p49|||Member of Eastern Creek Volcanics.||||||
10337|Lena Quartzite Member|50100|5|Briefly described|p17|||Of the Eastern Creek Volcanics.||||||
10337|Lena Quartzite Member|62873|5|Briefly described|p692 Fig. 1|||Also referred to as Lena Quartzite. Separates the Pickwick Metabasalt and Cromwell Metabasalt Members of Eastern Creek Volcanics (above and below respectively).||||||28-NOV-06
10337|Lena Quartzite Member|63023|5|Briefly described|p1025 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of Eastern Creek Volcanics (Haslingden Group). Geological Province: Leichardt Superbasin. See also Lena Quartzite (abbrev.).||||||07-NOV-08
10337|Lena Quartzite Member|63111|5|Briefly described|p1164 Tb. 1, p1165|Statherian|Statherian|Of Eastern Creek Volcanics. Overlain by Pickwick Metabasalt Member, underlain by Cromwell Metabasalt Member. Age: 1779+/-4Ma. Thickness: 750m. Geol Prov: Leichhardt Superbasin. Poorly-sorted, coarse-grained to well-sorted, fine-grained sandstone.||||||07-FEB-11
10337|Lena Quartzite Member|67323|4|Described|GIS attrib tbl, p13|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Leichhardt Superbasin. Leichhardt River Domain, Mount Isa Inlier. The rank {Member] is absent in the Eastern Australia Time-Space Plot.|1779 +/- 4 Ma ( MDA: Neumann et al. 2006, 2007).|Eastern Creek Volcanics.||Overlies Cromwell Metabasalt Member and is overlain by Pickwick Metabasalt Member.|Feldspathic quartzite, orthoquartzite with rare pebbles.|
10337|Lena Quartzite Member|68732|5|Briefly described|p161, p165 Fig.3|Statherian|Statherian|Of the Prize Supersequence. Maximum sedimentary depositional age.|1779 +/- 4 Ma|||||
10337|Lena Quartzite Member|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Eastern Creek Volcanics.||Overlies Cromwell Metabasalt Member. Is overlain by Pickwick Metabasalt Member.|Feldspathic quartzite and orthoquartzite with rare pebbles.|
10337|Lena Quartzite Member|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Eastern Creek Volcanics.||Overlies Cromwell Metabasalt Member. Is overlain by Pickwick Metabasalt Member.|Feldspathic quartzite and orthoquartzite with rare pebbles.|
10337|Lena Quartzite Member|71592|5|Briefly described|Appendix A.|||Leichhardt River Domain, Mount Isa Orogen.|1773+/-2 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
10337|Lena Quartzite Member|71799|5|Briefly described|p150 fig 2, p152|Statherian|Statherian|Lawn Hill. 750m thick. Maximum depositional age is derived from Neumann et al, 2006.|1779 +/- 4 Ma (Max. dep. Age)|Eastern Creek Volcanics||Overlies the Cromwell Metabasalt Member. Overlain by the Pickwick Metabasalt Member.|Quartzite, sandstone and greywacke.|
10337|Lena Quartzite Member|71980|5|Briefly described|map legend sheet 1|Proterozoic|Proterozoic|||Of Eastern Creek Volcanics|||feldspathic sandstone, fluvial - coastal.|
10363|Lewis Granite|22446|6|Mentioned|p20|Statherian|Statherian|||||||
10363|Lewis Granite|24197|5|Briefly described|p7, p26|Proterozoic|Proterozoic|Probably part of the Granites Supersuite. Geological province: Granites-Tanami Block. See also p82.||||||07-FEB-11
10363|Lewis Granite|29809|6|Mentioned|Table 1|||||||||
10363|Lewis Granite|29813|6|Mentioned|p7|||||||||
10363|Lewis Granite|35205|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10363|Lewis Granite|36532|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
10363|Lewis Granite|36887|5|Briefly described|p206|||||||||
10363|Lewis Granite|38335|6|Mentioned|p1735|||||||||
10363|Lewis Granite|39559|6|Mentioned|Table 1|||||||||
10363|Lewis Granite|39888|6|Mentioned|Fig.8|||||||||
10363|Lewis Granite|41465|6|Mentioned|p13|||||||||
10363|Lewis Granite|42504|5|Briefly described|Table 3 P60|||||||||
10363|Lewis Granite|42754|6|Mentioned|p3|||||||||
10363|Lewis Granite|43832|6|Mentioned|Table 17 p90||Paleoproterozoic|||||||07-NOV-08
10363|Lewis Granite|44998|14|Not recorded|p.17|||||||||
10363|Lewis Granite|45140|1|Redefined|p12-13, p15-16, p22, p24-25, p32-35|Paleoproterozoic|Paleoproterozoic|See also p37-38, p47, p74, Appx.p10-11. Modified after Casey and Wells (1964). The Granites-Tanami Block. Named after Lewis Range. Previously included rocks now mapped as Slatey Creek Granite; now restricted to outcrops N and E of the Lewis Range (the original type locality) in the Lucas sheet area. A more precise type area is nominated in this study: a 40m high hill 1km WNW of Point Nelligan at 20 deg 11'30"S, 128 deg 38'00"E. Crops out mostly as gently sloping aprons of coarse granitic sand; also as tors, low rubbly mounds and flat-topped hills capped by laterite. Chemically, is essentially identical to Slatey Creek and The Granites Granites; geochemistry detailed.|1720+/-8 Ma (Rb-Sr whole-rock, Page et al. 1976).|||Intrudes the Killi Killi Beds (Tanami Complex). Is overlain by Gardiner and Lewis Range Sandstones.|Pinkish to pale grey muscovite or muscovite-biotite adamellite; local biotite adamellite and granodiorite. Cross-cutting sheets of pegmatite and aplite are common; local quartz veins, slickensides and fine-grained biotite-rich xenoliths.|
10363|Lewis Granite|46788|4|Described|p8|||||||||
10363|Lewis Granite|46864|6|Mentioned|p37|||Re age dates||||||
10363|Lewis Granite|48826|2|Defined|p.14||Paleoproterozoic|Tb.III, p.14,15,33,Pl.1. Granite of Lamboo Complex. Intrudes Halls Creek Metamorphics. Overlain by Phillipson Beds. ?L.Proterozoic. (E52-13,F52-2).||||||07-NOV-08
10363|Lewis Granite|50589|5|Briefly described|p1.4, 2.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Granites-Tanami Block. Of the Granites Suite/Supersuite. Age: 1684 +/- 8Ma (Rb-Sr).||||||07-NOV-08
10363|Lewis Granite|62580|5|Briefly described|p47|||Of the Frederick Suite. Contains Orion Granodiorite (part of the composite Lewis Granite) analysed to show it consists of fine- to medium-grained, equigranular biotite granodiorite.||||||07-FEB-11
10363|Lewis Granite|63261|6|Mentioned|p16|||Included in the Grimwade Suite.||||||07-FEB-11
10363|Lewis Granite|64277|5|Briefly described|Map ledgend|Paleoproterozoic|Paleoproterozoic|Age: 1795Ma. Muscovite and biotite monzogranite; locally porphyritic; minor biotite granodiorite.||||||10-MAY-21
10363|Lewis Granite|64580|4|Described|map legend||Paleoproterozoic|Muscovite and biotite monzogranite; locally porphyritic; minor biotite granodiorite.||||||09-DEC-08
10363|Lewis Granite|66129|5|Briefly described|p213, p214, p215 Fig.2, p216, p217|Statherian|Statherian|9000 sq. km, number of separate lobes. 1795 Ma. Monzogranite and granodiorite; medium to coarse grained quartz, white euhedral K-feldspar, plagioclase, primary muscovite, biotite. Accessory minerals: apatite, allanite, titanite, fluorite, pyrite, tourmaline, zircon.||||||
10363|Lewis Granite|66468|6|Mentioned|p17 Fig.3, p18 Fig.5, p20-21|Paleoproterozoic|Paleoproterozoic|See also p25-26 Figs.8,9; p27. Marked negative gravity anomalies and weakly magnetic.||||||
10363|Lewis Granite|68474|6|Mentioned|p573|Palaeoproterozoic|Palaeoproterozoic|Granites-Tanami Orogen.|ca. 1795 Ma||||Monzogranite, granodiorite.|
10363|Lewis Granite|68656|5|Briefly described|GEOL_LUT_CSV/100k_interpgeop_lut|Paleoproterozoic|Paleoproterozoic|See also 100k_maginterpgeop_lut.csv; 500k_geologyp08_lut; and GEOCHRON. Granites-Tanami Complex. High gravity; non- to highly magnetic.|1792 +/- 5 Ma (Wingate et al., 2007).|Frederick Suite|||Muscovite and biotite monzogranite; locally porphyritic; minor biotite granodiorite, diorite and/or gabbro.|
10363|Lewis Granite|69253|5|Briefly described|p759, p760-761 Figs.14-15, p762, p763|||Petrophysical properties described. Undergone ~6 km right-lateral displacement by Trans-Tanami Fault. See also p766, p767.||Unit in Frederick Suite.||Intrudes Dead Bullock Formation.||
10363|Lewis Granite|69426|6|Mentioned|p11:10, 11:12|||Blake et al. (1979).||Grimwade Suite.||||08-OCT-18
10363|Lewis Granite|69587|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Geological province: Granites-Tanami Orogen, North Australian Craton. Sample GSWA 184802 (monzogranite) yielded a weighted mean 207Pb*/206Pb* date of 1792+\-5 Ma, interpreted as the age of magmatic crystallization of the monzogranite. Events: Alice Springs Orogeny; Tanami Orogeny D1t. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|1815-1790 Ma (inferred)|Unit of Granites Supersuite.|||Muscovite and biotite monzogranite; locally porphyritic; minor biotite granodiorite|
10363|Lewis Granite|70129|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|c.1796 Ma (Bagas et al., 2010).||||Muscovite and biotite monzogranite, locally porphyritic; minor biotite granodiorite.|
10363|Lewis Granite|70130|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen. The two facies are mapped separately.|c.1796 Ma (Bagas et al., 2010).||||Muscovite and biotite monzogranite, locally porphyritic, minor biotite granodiorite; magnetite-bearing monzogranite.|
10363|Lewis Granite|70142|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|1820-1790 Ma.||||Muscovite and biotite monzogranite, locally porphyritic; minor biotite granodiorite.|
10363|Lewis Granite|70143|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|1820-1790 Ma.||||Muscovite and biotite monzogranite, locally porphyritic; minor biotite granodiorite.|
10363|Lewis Granite|71080|6|Mentioned|p6|||At base of type section of Lewis Range Sandstone, 1.5 km southwest of Point Nelligan.||||Unconformably underlies Lewis Range Sandstone.||
10363|Lewis Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||pegmatite, aplite, granodiorite, monzogranite|
10363|Lewis Granite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen. Age inferred.|1796+/-16 Ma.||||Muscovite and biotite monzogranite; locally porphyritic; minor biotite granodiorite. Magnetite-bearing monzogranite.|
10363|Lewis Granite|73089|4|Described|p3, p8-9, p13, p18-20, p38-39, p44|Orosirian|Orosirian|Granites-Tanami Orogen. A large composite body comprising magnetic and non-magnetic phases, which appears to reflect distinct magma batches emplaced during the same magmatic event. Assigned to the Frederick and Grimwade Suites. [See report for geochon details from six samples]. May be associated with the 1810-1790 Ma Stafford Event.|1807-1800 Ma|Frederick and Grimwade Suites||Intrudes Killi Killi Formation and Stubbins Formation.|Fine to medium grained monzogranites to granodiorites with rare mafic and fine-grained granitic xenoliths.|
10363|Lewis Granite|73445|5|Briefly described|p7|||Crowe and Muhling (1977). A corresponding biotite monzogranite in the Granites-Tanami Orogen has a U-Pb zircon age of 1825-1719 Ma.||||||
10365|Lewis Range Sandstone|22496|6|Mentioned|p9||Mesoproterozoic|Unconformably overlies the Gardiner Sandstone.||||||12-AUG-04
10365|Lewis Range Sandstone|23314|6|Mentioned|336|||||||||
10365|Lewis Range Sandstone|23621|5|Briefly described|p33|||Geological Province: Birrindudu Basin.||||||
10365|Lewis Range Sandstone|24173|5|Briefly described|p24|Neoproterozoic|Neoproterozoic|Of the Redcliff Pound Group. Geological Province: Birrindudu Basin. Part of extensive sand blanket including Mount Kinahan Sandstone, Vaughan Springs Quartzite, Heavitree Quartzite and Townsend Quartzite||||||06-APR-05
10365|Lewis Range Sandstone|29813|4|Described|Table 2|||||||||
10365|Lewis Range Sandstone|29817|6|Mentioned|p10|||||||||
10365|Lewis Range Sandstone|29818|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
10365|Lewis Range Sandstone|31360|6|Mentioned|Table 1|||||||||
10365|Lewis Range Sandstone|35205|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
10365|Lewis Range Sandstone|36532|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
10365|Lewis Range Sandstone|42504|5|Briefly described|Table 3 P60|||||||||
10365|Lewis Range Sandstone|45140|2|Defined|p13, p23-25, p40-41, p43, p46-48, p50-51|||See also p53, p55, p57, p75, Appx.p25-26. Crowe and Muhling (1977); Blake et al. (1977). Most of this unit was previously mapped as parts of Phillipson Beds and Kearney Beds (Well, 1962; Casey and Wells, 1964). Birrindudu Basin. Named after the Lewis Range: caps the NW-trending line of cuestas. 400m thick, up to 1000m. The type section is 1.5km SW of Point Nelligan, at 20deg 13'00"S, 128deg 38'00"E. Lateral equivalent of Munyu and Muriel Range Sandstones; ?correlated with Denison Beds. Mainly flat-lying or very gently dipping, except near faults.||Basal Redcliff Pound Group.||Unconformably overlies Killi Killi Beds, Gardiner Sandstone, Lewis and Slatey Creek Granites and ?Baines Beds. Is overlain conformably by Murraba Formation.|Friable, locally silicified, well-sorted, medium- to fine-grained quartz arenite; subordinate poorly-sorted sublithic arenite, quartz arenite, conglomerate and rare siltstone.|
10365|Lewis Range Sandstone|46788|6|Mentioned|p8|||||||||
10365|Lewis Range Sandstone|46864|4|Described|p38|||||||||
10365|Lewis Range Sandstone|62453|6|Mentioned|p16|||Geological Province: Murraba (formerly Birrindudu) Basin.||||||
10365|Lewis Range Sandstone|62580|6|Mentioned|p10|||||||||07-FEB-11
10365|Lewis Range Sandstone|64277|5|Briefly described|Map ledgend|Neoproterozoic|Neoproterozoic|Of Redcliffe Pound Group. Geological Province: Murraba Basin, Centralian Superbasin. Cross-bedded quartz sandstone, ripple marks locally; minor sandstone, conglomerate, and siltstone.||||||24-JUN-08
10365|Lewis Range Sandstone|65074|4|Described|p351 fig 4-37, p353, p356 Tb. 4-12|Neoproterozoic|Neoproterozoic|Of North/Centre Birrindudu Basin. 400 m (up to 1km) thick. Type section is 1.5 km SW of Point Nelligan in the Lewis Range.||Redcliff Pound Group||Overlain by Murraba Formation (conformably). Equivalent to Munyu Sandstone and Muriel Range Sandstone.|Quartz arenite, shale, siltstone, limestone, chert.|
10365|Lewis Range Sandstone|68656|5|Briefly described|GEOL_LUT_CSV/100k_interpgeop_lut|Neoproterozoic|Neoproterozoic|Murraba Basin. See also GEOCHRON.csv which gives two U-Pb zircon ages: 1021 +/- 33 Ma and 1067 +/- 20 Ma (both Blake et al., 2000).|1021 +/- 33 Ma (Pb/Pb).|Redcliff Pound Group||Unconformably overlies Slatey Creek Granite.|Cross-bedded quartz sandstone, with ripple marks, minor sandstone, conglomerate, and siltstone; chert, sublithic sandstone, siltstone, limestone; glauconitic sandstone, siltstone and shale, minor dolomitic sandstone.|
10365|Lewis Range Sandstone|68733|6|Mentioned|p188|Neoproterozoic|Neoproterozoic|Age shown as Neoproterozoic(?).||Redcliff Pound Group.||||05-DEC-17
10365|Lewis Range Sandstone|68994|6|Mentioned|p20|||Murraba Basin.||||Equivalent to Munyu Sandstone.||13-JAN-17
10365|Lewis Range Sandstone|69099|4|Described|GEOL_LUT_CSV files + geochron files|Cryogenian|Cryogenian|Murraba Basin||Redcliff Pound Group|||Cross-bedded quartz sandstone, with ripple marks; minor sandstone, conglomerate, and siltstone.|31-JUL-15
10365|Lewis Range Sandstone|69440|5|Briefly described|p25:1-2|Cryogenian|Cryogenian|Crops out in LUCAS and BILLILUNA map areas. Lithologically similar to Denison beds.||||Correlated with Munyu Sandstone and (probably) Denison beds.|Well-sorted, medium- to fine-grained quartz arenite, sublithic arenite, conglomerate and rare siltstone.|12-JUL-16
10365|Lewis Range Sandstone|69587|4|Described|GEOL_LUT_CSV files + geochron files|Cryogenian|Cryogenian|Of Murraba Basin and Birrindudu Basin, Centralian Superbasin. Events: Alice Springs Orogeny. Sample GSWA 178851 (mature qtz-rich sandstone) yielded weighted mean 207Pb*/206Pb* dates of 1021+\-33 Ma, interpreted as maximum depositional age of the sandstone. Sample GSWA 178852 (qtz-rich sandstone) yielded weighted mean 207Pb*/206Pb* dates of 1067+\-20 Ma, interpreted as maximum depositional age of the sandstone. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv.|830-810 Ma (inferred)|Unit of Redcliff Pound Group.||Basal unit of Redcliff Plain Group. Underlain unconformably by Slatey Creek Granite.|Cross-bedded quartz sandstone with ripple marks; glauconitic sandstone, conglomerate, siltstone, chert, limestone.|
10365|Lewis Range Sandstone|69634|4|Described|100k_interpgeop_lut.csv|Cryogenian|Cryogenian|Of Murraba Basin, Centralian Superbasin. Events: Alice Springs Orogeny.|830-810 Ma (Inferred)|Unit of Redcliff Pound Group.|||Cross-bedded quartz sandstone with ripple marks; minor sandstone, conglomerate, and siltstone|
10365|Lewis Range Sandstone|70129|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Murraba Basin, Centralian Superbasin.||Redcliff Pound Group.|||Cross-bedded quartz sandstone with ripple marks; minor sandstone, conglomerate and siltstone.|
10365|Lewis Range Sandstone|70130|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Murraba Basin, Centralian Superbasin.||Redcliff Pound Group.||Is ovelain by Murraba Formation.|Cross-bedded quartz sandstone with ripple marks; minor sandstone, conglomerate and siltstone.|
10365|Lewis Range Sandstone|70141|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Murraba Basin, Centralian Superbasin.||Redcliff Pound Group.||Overlies Birrindudu Group.|Cross-bedded quartz sandstone with ripple marks; minor sandstone, conglomerate and siltstone. Separately mapped sub-units: chert, sublithic sandstone, siltstone and limestone; glauconitic sandstone, siltstone and shale, minor dolomitic sandstone.|
10365|Lewis Range Sandstone|70142|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Murraba Basin, Centralian Superbasin.|830-810 Ma.|Redcliff Pound Group.||Overlies Slatey Creek Granite.|Cross-bedded quartz sandstone, with ripple marks; minor sandstone, conglomerate and siltstone.|
10365|Lewis Range Sandstone|70143|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Murraba Basin, Centralian Superbasin. Unclear if age range refers to the Group or just the Lewis Range Sandstone.|830-810 Ma.|Redcliff Pound Group.|||Cross-bedded quartz sandstone with ripple marks; minor sandstone, conglomerate and siltstone.|
10365|Lewis Range Sandstone|70154|4|Described|100k_interpgeop_lut.csv|Cryogenian|Neoproterozoic||810-1000 Ma|Redcliff Pound Group|||Cross-bedded quartz sandstone with ripple marks; minor sandstone, conglomerate, and siltstone|
10365|Lewis Range Sandstone|71080|4|Described|p8-11 23, 25-26, 27, 28, 29, 31, 32, 36|Tonian|Tonian|Basal unit, northern Murraba Basin. Type section discussed. Named for Lewis Range on LUCAS. Basal unit in the northern Murraba Basin. 20-400 m thick. Extent of unit in Kearney Range questioned. Previously included as the basal unit in the Redcliff Pound Group. Different detrital zircon spectra suggest younger age than Munyu Sandstone and/or different provenance. Part of the succession in the Kearney Range are more like Birrindudu Group rocks of the Birrindudu Basin and may be equivalnet to Hidden Basin beds. See also p4, 5, 6, 7,|detrital Zr max dep age 916 +/-43 Ma|||Unconformably overlies Lewis Granite at type section, Slatey Creek Granite. Previously considered a lateral equivalent of Munyu Sandstone, to Sth and Muriel Range Sandstone NT.|Dominated by well-sorted, fine- to medium grained, thin- to medium-bedded quartz arenite, with subordinate, poorly sorted, sublithic arenite, quartz arenite and conglomerate. Minor siltstone present locally.|04-FEB-19
10365|Lewis Range Sandstone|71267|4|Described|GEOL_LUT_CSV files|Tonian|Tonian|Of Murraba Basin, Centralian Superbasin. Events: Alice Springs Orogeny (450-295 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv and geochron files.|1000-810 Ma (inferred)|Unit of Redcliff Pound Group.|||Cross bedded and rippled medium to fine grained quartz sandstone with shale pellet layers in places; minor shale, siltstone, limestone and chert with conglomerate and sublithic sandstone near the base|
10365|Lewis Range Sandstone|73086|6|Mentioned|p18, p30, p39|||Murraba Basin, southern.||||Potentially correlates to Bitter Springs Group.||
10365|Lewis Range Sandstone|73445|5|Briefly described|p7, 10, 12-14|||Whole-rock chemistry tabulated.||Redcliff Pound Group.||Is overlain by Murraba Formation. Equivalent to Munyu and Muriel Range Sandstones.|Fine-grained sandstone.|
10414|Limbunya Group|14019|4|Described|p4-6|Paleoproterozoic|Paleoproterozoic|Dolostone, siltstone, sandstone, tuffite. Unconformably overlies Inverway Metamorphics and Birrindudu Group; unconformably overlain by the Wattie Group. Max. thickness: 1300m. Geological Province: Birrindudu Basin.||||||07-NOV-08
10414|Limbunya Group|22446|5|Briefly described|p20|Calymmian|Calymmian|||||||
10414|Limbunya Group|23314|5|Briefly described|329|||||||||
10414|Limbunya Group|23809|5|Briefly described|p47|Proterozoic|Proterozoic|Correlated with McArthur Group and possible with Namerinni Group (Tennant Inlier), and with Bungle Bungle Dolomite (Osmond Basin, W.A.). Geological Province: Birrindudu Basin.||||||30-MAR-05
10414|Limbunya Group|24122|5|Briefly described|p4 Fig.3|||Geological Province: Birrindudu Basin.||||||
10414|Limbunya Group|24297|5|Briefly described|p4 Fig.3, p15|Proterozoic|Proterozoic|Geological Province: Birrindudu Basin.||||||
10414|Limbunya Group|24298|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Dolomite, siltstone, sandstone, chert.||||||19-OCT-05
10414|Limbunya Group|24441|5|Briefly described|p1 Fig. 1|||Unconformably overlies Birrindudu Group;  unconformably overlain by Wattie Group. Geological Province: Birrindudu Basin.||||||
10414|Limbunya Group|24442|5|Briefly described|p3, p50 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: 1640-1635Ma.  Geological Province: Victoria-Birrindudu Basin.||||||07-NOV-08
10414|Limbunya Group|28255|3|Fully described|p10-11, Tb.11 (opp. p8)|||Now includes the former "Kirkimbie Beds". Subdivided into 11 formations. Extensive sequence of dolomite, siltstone and sandstone. Unconformably overlies Inverway metamorphics and Bunda Grit; unconformably overlain by the Wattie Group. Max. thick: >1300m.||||||22-DEC-08
10414|Limbunya Group|29804|6|Mentioned|p418|||||||||
10414|Limbunya Group|29805|4|Described|Table 1|||||||||
10414|Limbunya Group|29809|6|Mentioned|p418|||||||||
10414|Limbunya Group|30003|4|Described|p6, p9|||Predominantly dolomite, silty dolomite and siltstone, with subordinate sandstone and chert.  Age is Carpentarian or Adelaidean. Unconformably overlain by by the Wattie Group.||||||19-APR-05
10414|Limbunya Group|30004|6|Mentioned|Map legend|Proterozoic|Proterozoic|Carpentarian or Adelaidean||||||
10414|Limbunya Group|31361|6|Mentioned|Table 1|||||||||
10414|Limbunya Group|32172|4|Described|p6|||Carpentarian or Adelaidean||||||
10414|Limbunya Group|32173|5|Briefly described|Map legend|Adelaidean|Carpentarian|Carpentarian or Adelaidean||||||16-NOV-04
10414|Limbunya Group|32175|5|Briefly described|Map legend|Adelaidean|Carpentarian|Dolomite, siltstone, sandstone, chert.||||||02-DEC-04
10414|Limbunya Group|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10414|Limbunya Group|32660|4|Described|Table 6|||||||||
10414|Limbunya Group|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Massive dark grey dolomite, chert.||||||02-DEC-04
10414|Limbunya Group|32701|4|Described|Table 1|||Adelaidean. See also p7.||||||30-OCT-06
10414|Limbunya Group|32728|6|Mentioned|p16|||||||||
10414|Limbunya Group|33374|6|Mentioned|p6|||Stratigraphy.||||||
10414|Limbunya Group|33375|4|Described|p7, p9 Tb. 1|||Carpentarian or Adelaidean.||||||26-APR-05
10414|Limbunya Group|33376|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10414|Limbunya Group|33377|5|Briefly described|Table 2|||Strat.||||||
10414|Limbunya Group|33378|5|Briefly described|Map legend|||Age is Carpentarian or Adelaidean.||||||27-APR-05
10414|Limbunya Group|35950|6|Mentioned|p311|||||||||
10414|Limbunya Group|36473|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10414|Limbunya Group|36532|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10414|Limbunya Group|37462|4|Described|Table 4.V|||||||||
10414|Limbunya Group|38243|6|Mentioned|Fig.2|||||||||
10414|Limbunya Group|42504|6|Mentioned|p68|||Birrindudu Basin||||||
10414|Limbunya Group|45112|3|Fully described|p17|||p17-18||||||30-OCT-06
10414|Limbunya Group|45140|2|Defined|p12-13, p39-42, p53, p62, p74, Appx.p19|||Sweet et al. (1974). Birrindudu Basin. Named after Limbunya pastoral lease. Forms low strike ridges and undulating terrain. Over 400m thick. Folded about NW-trending axes. Mainly shallow-marine deposits.||||Unconformably overlies Bunda Grit and Inverway Metamorphics. Correlated with Birrindudu Group. Is overlain unconformably by Antrim Plateau Volcanics and Wattie Group.|Silicified medium- to fine-grained sublithic arenite and quartz arenite; cross-bedded, locally with ripple marks. Some beds contain shale pellets. Carbonate rocks.|
10414|Limbunya Group|46864|6|Mentioned|p38|||||||||
10414|Limbunya Group|48938|4|Described|p21|||Measured section p89.||||||30-OCT-06
10414|Limbunya Group|48943|2|Defined|p14|Adelaidean|Carpentarian|Carp. or Adel.||||||
10414|Limbunya Group|48950|3|Fully described|p38|||||||||
10414|Limbunya Group|50225|5|Briefly described|p406 Fig. 10, p407|Mesoproterozoic|Paleoproterozoic|Geological Province: Birrindudu Basin.||||||07-FEB-11
10414|Limbunya Group|60006|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Birrindudu Basin. Includes: Blue Hole Formation, Campbell Springs Dolostone, Fraynes Formation. Dolostone, siltstone, sandstone, tuffite.||||||07-NOV-08
10414|Limbunya Group|60589|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes eleven named units and undivided rocks.  Consists of dolostone, siltstone, sandstone, tuffite.  Geological Province: Birrindudu Basin.||||||07-NOV-08
10414|Limbunya Group|60672|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Mainly dolostone, sandstone and siltstone. Geological Province: Birrindudu Basin.||||||07-NOV-08
10414|Limbunya Group|60682|5|Briefly described|piii, 7|Statherian|Statherian|Geological Province: Birrindudu Basin.||||||
10414|Limbunya Group|60685|5|Briefly described|p4 Fig. 3|Proterozoic|Proterozoic|Unconformably overlain by Wickham Formation (Wattie Group). Geological Province: Birrindudu Basin.||||||
10414|Limbunya Group|63261|5|Briefly described|p17, p24|Paleoproterozoic|Paleoproterozoic|Interpreted to overlie Birrindudu Group to the north (drill hole evidence). Age: 1640-1635Ma (SHRIMP U-Pb, tuffaceous rock, Smith et al 2001).|Age: 1640-1635Ma|||||07-FEB-11
10414|Limbunya Group|64662|5|Briefly described|p44|Statherian|Statherian|Age: ~1.64Ga. Overlies Birrindudu Group in the Victoria River Basin.||||||07-FEB-11
10414|Limbunya Group|64722|5|Briefly described|Fig. 2 p3-6, p10|Statherian|Statherian|Age of 1640-1635 Ma given after Cutovinos et al. (2002).||||Overlies Birrindudu Group.||11-APR-12
10414|Limbunya Group|64724|5|Briefly described|p45 Fig.5, p46|Statherian|Statherian|Victoria River and Birrindudu Basin unit deposited as part of sedimentation in the Isa Superbasin (1660-1590 Ma)||||||
10414|Limbunya Group|64737|4|Described|p232 Fig.2, p233, p243|Statherian|Statherian|Of Victoria River Basin. Ages from volcanics within the unit (Cutovinos et al., 2002).|1636 +/- 5 and 1639 +/- 7 Ma.||Includes Bluehole Formation and Campbell Springs Dolostone.|Overlies Gardiner Sandstone.|Interlayered siliciclastic and hypersaline carbonate rocks which include stromatolites and other features interpreted as shallow to very shallow marine deposition.|30-APR-12
10414|Limbunya Group|65074|6|Mentioned|p349, p351 fig 4-37, p352|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||||||
10414|Limbunya Group|65331|5|Briefly described|Map legend + overview geology map legend|Palaeoproterozoic|Palaeoproterozoic|Of Birrindudu Basin. Includes Fraynes Formation, Campbell Springs Dolostone, Blue Hole Formation. Dolostone, siltstone, sandstone, tuffite||||||
10414|Limbunya Group|65342|5|Briefly described|pp10-11.|||Birrindudu Basin.|||Includes Stirling, Kunja and Farquharson Sandstones; Margery, Amos Knob, Blue Hole, Fraynes and Killaloc Formations; Pear Tree, Mallabah and Campbell Springs Dolostones.|Unconformably overlies Birrindudu and Tolmer Groups.|Mainly carbonate and siliciclastic rocks.|
10414|Limbunya Group|67151|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Birindudu Basin.|||Includes Stirling and Farquharson Sandstones; Margery, Amos Knob, Blue Hole, Killaloc and Fraynes Formations; Pear Tree, Mallabah and Campbell Springs Dolostones; and Kunja Siltstone.|Is unconformably overlain by Wattie Group.||
10414|Limbunya Group|67269|6|Mentioned|p20-21 Fig.19|||Birrindudu Basin.|||Pear Tree Dolomite.|||
10414|Limbunya Group|68280|6|Mentioned|p26 fig 24|||Birrindudu Basin.|||Includes Pear Tree Dolomite|||
10414|Limbunya Group|68733|4|Described|p176-179, p181, p184-187, p193|Statherian|Statherian|Birrindudu Basin. Age constraints provided by four intercalated tuffs in the upper parts (Smith 2001; Cutovinos et al. 2002). No longer marks the subdivision between Birrindudu and Victoria Basins; replaced by top-Tijunna Group unconformity. Uncertain correlation with Birrindudu Group discussed.|ca. 1640 - 1635 Ma||Includes Killaloc, Fraynes, Blue Hole, Amos Knob and Margery Formations; Campbell Springs, Pear Tree, and Mallabah Dolostones; Faraquharson Sandstone and Stirling (basal) Sandstones; Kunja Siltstone.|Unconformably overlain by the Wickham Formation.  Unconformably underlain by the Birrindudu Group.|Carbonate dominated.|05-DEC-17
10414|Limbunya Group|69417|5|Briefly described|p2:5-6|Statherian|Statherian|Southern Birrindudu Basin.|c.1650-1630 Ma.|||||12-JUL-16
10414|Limbunya Group|69425|6|Mentioned|p10:4|||Mentioned as possible correlative of Hatches Creek Group, based on geochronological grounds.||||||12-JUL-16
10414|Limbunya Group|69429|5|Briefly described|p14:2|Paleoproterozoic|Paleoproterozoic||||Stirling, Farquharson Sandstones; Margery, Amos Knob, Blue Hole Formations; Pear Tree, Mallabah, Campbell Springs Dolostones; Kunja Siltstone.|Unconformably overlies Inverway Metamorphics.||12-JUL-16
10414|Limbunya Group|69430|5|Briefly described|p15:19|Statherian|Statherian|Birrindudu Basin. Has tuffaceous units with similar ages to tuffaceous units dated at 1639 +/- 3 Ma in the HYC Pyritic Shale Member of the Barney Creek Formation (McArthur Group), McArthur Basin.||||||12-JUL-16
10414|Limbunya Group|69432|4|Described|p17:1-3, 5-9, 12-13|Paleoproterozoic|Paleoproterozoic|Assigned to the Birrindudu Basin by Dunster et al. (2000). Previously assigned to the Victoria Basin. Composite thickness of c.1300m. Generally dips at very low angles; has locally developed broad gentle folds. Exploration target for base metals.|||Stirling, Farquharson Sandstones; Margery, Amos Knob, Blue Hole, Fraynes, Killaloc Formations; Mallabah, Pear Tree, Campbell Springs Dolostones.|Unconformably overlies Birrindudu and Tolmer Groups. Is overlain unconformably by Wattie Group.|A succession of cyclic carbonate and siliciclastic rocks. Minor subaqueous tuffaceous beds.|12-JUL-16
10414|Limbunya Group|69435|5|Briefly described|p20:1|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin. Possible correlative of the Fitzmaurice Group.|c.1640 Ma.||||Predominantly carbonates and evaporites.|12-JUL-16
10414|Limbunya Group|69448|5|Briefly described|p33:8|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin.|||Stirling Sandstone.|||12-JUL-16
10414|Limbunya Group|69673|6|Mentioned|p3 fig 2, p47, p48 fig 35, p188|Statherian|Statherian|Approximately 1300m thick. Age ranging from 1830-1638 Ma. Also includes the Kunja Siltstone, Farquharson Sandstone, Blue Hole Formation, Campbell Springs Dolostone, Fraynes Formation, Killaloc Formation.|||Includes Stirling Sandstone, Margery Formation, Pear Tree Dolostone, Amos Knob Formation, Mallabah Dolostone|Unconformably overlies Birrindudu Group, unconformably overlain by Wattie Group|Dolostone and dolomitic siliciclastic rocks.|
10414|Limbunya Group|70206|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Birindudu Basin [misspelling of Birrindudu Basin].|||Includes Fraynes Formation, Campbell Springs Dolostone, Blue Hole Formation.|||18-JUL-16
10414|Limbunya Group|70655|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Birindudu Basin.|||Includes Fraynes, Killaloc, Blue Hole, Amos Knob, Margery Formations, Campbell Springs, Mallabah Dolostones, Farquharson Sandstone, Kunja Siltstone,  Pear Tree Dolostone, Stirling Sandstone.|Is unconformably overlain by Wattie Group.||
10414|Limbunya Group|70848|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin.|||Stirling Sandstone, Margery Formation.|||
10414|Limbunya Group|70854|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.|||Pear Tree, Mallabah, Campbell Springs Dolostones; Amos Knob, Blue Hole, Fraynes Formations; Kunja Siltstone; Farquharson Sandstone.|Is overlain unconformably by Wattie Group.|Dolostone, siltstone, sandstone, shale, chert.|
10414|Limbunya Group|70855|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin. No outcrop in map area: shown in Section only.|||Fraynes, Killaloc Formations.|Is overlain unconformably by Wickham Formation (Wattie Group).|Dolostone, siltstone, sandstone, chert.|
10414|Limbunya Group|70968|6|Mentioned|p6|||Birrindudu Basin.||||Is overlain unconformably by Roper Group.||
10414|Limbunya Group|71169|5|Briefly described|p71|Statherian|Statherian|North Australian Craton.|c. 1650 Ma|||||
10414|Limbunya Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||dolostone, siltstone|
10414|Limbunya Group|71302|5|Briefly described|p2-3,6,72-74|Paleoproterozoic|Paleoproterozoic|Of Birindudu Basin. Also includes Amos Knob Formation, Pear Tree Dolostone, Margery Formation, Stirling Sandstone.|||Includes Killaloc Formation, Fraynes Formation, Campbell Springs Dolostone, Blue Hole Formation, Farquharson Sandstone, Kunja Siltstone, Mallabah Dolostone.|Overlain by Wattie Group. Underlain by Birrindudu Group or Tolmer Group.||
10414|Limbunya Group|71374|5|Briefly described|iii, p1 tbl 1, p2, p36|Mesoproterozoic|Palaeoproterozoic|Birrindudu Basin.|||Includes the Farquharson Sandstone.|||
10414|Limbunya Group|72373|5|Briefly described|p2|Paleoproterozoic|Paleoproterozoic|Of Birrindudu Basin. Broadley equivalent to Glyde package, and Habgood, Balma, McArthur and Vizard groups (McArthur Basin).||||||
10414|Limbunya Group|73083|6|Mentioned|p30-31|||[Also written as Limbunya group].||||Unconformably overlain by Wickham Formation (Wattie Group).||
10424|Limmen Sandstone|22538|6|Mentioned|Fig3 P708|||||||||
10424|Limmen Sandstone|22600|4|Described|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
10424|Limmen Sandstone|22853|3|Fully described|26|Proterozoic|Proterozoic|Of the Roper Group. Max thickness 80m. Overlain by Mainoru Formation, underlain by McArthur Group and Nathan Group.||||||30-OCT-06
10424|Limmen Sandstone|23216|5|Briefly described|p30,33-4|||||||||
10424|Limmen Sandstone|23404|5|Briefly described|p639 Fig.2|||Of Roper Group.||||||
10424|Limmen Sandstone|23776|5|Briefly described|p705 Fig 2.|||Of Roper Group||||||
10424|Limmen Sandstone|23937|2|Defined|p83 App. 1|Calymmian|Calymmian|Of Collara Subgroup. Previously mapped as Mallison Sst and lower Wigram Fm of Malay Road Group. Conformably overlain by Gibb Mbr; overlies Mantungula Fm with erosive contact.  Thickness in Roper area: 100m: 330m In TANUMBIRINI. Geol.Prov: McArthur Basin.||||||01-NOV-04
10424|Limmen Sandstone|24048|4|Described|p70|Mesoproterozoic|Paleoproterozoic|Of the Roper Group.  Geological Province: McArthur Basin.||||||07-NOV-08
10424|Limmen Sandstone|24049|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Roper Group. Does not crop out in BLUE MUD BAY map sheet. Subdivided into two units: first, quartz arenite, and second, upper part: sandstone with lower part: mudstone. Geol. Prov: McArthur Basin.||||||13-OCT-05
10424|Limmen Sandstone|24050|3|Fully described|p41, P9 Tb. 2|Mesoproterozoic|Mesoproterozoic|Of Roper Group.  Granule- and pebble-rich quartz sandstone overlain by fine- to medium-grained quartz sandstone.  Overlies Dook Creek Formation; underlies Mainoru Formation.  Max. thickness: 60m.||||||30-OCT-06
10424|Limmen Sandstone|24051|5|Briefly described|Map Legend|Calymmian|Calymmian|Of Roper Group. Geological Province: McArthur Basin.||||||23-DEC-09
10424|Limmen Sandstone|24303|5|Briefly described|p60 Appendix|Mesoproterozoic|Mesoproterozoic|Of the Roper Group. Geological Province: McArthur Basin. Correlative of upper part of Sweetwater Member (Baralandji Formation). See also p24 Tb.4.||||||
10424|Limmen Sandstone|32660|5|Briefly described|Table 4|||||||||
10424|Limmen Sandstone|39210|6|Mentioned|p51|||||||||
10424|Limmen Sandstone|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
10424|Limmen Sandstone|40691|6|Mentioned|p64|||Mention Fig.4||||||
10424|Limmen Sandstone|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
10424|Limmen Sandstone|41220|6|Mentioned|Fig.3|||||||||
10424|Limmen Sandstone|41268|5|Briefly described|Fig.4|||Mention p290.||||||30-OCT-06
10424|Limmen Sandstone|41531|6|Mentioned|p167|||||||||
10424|Limmen Sandstone|42385|4|Described|p26|||See also Table 5 p25.||||||30-OCT-06
10424|Limmen Sandstone|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
10424|Limmen Sandstone|42597|5|Briefly described|Map Legend|Adelaidean||||||||
10424|Limmen Sandstone|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.||Lower Roper Group (Roper Group).||In schematic section, underlies Mainoru Formation; overlies Mantungula Formation.|Ridge forming: structureless quartzarenite interbedded with micaceous siltstone; sandstone, pebbly sandstone; basal regolith structure. Detailed lithology given.|25-AUG-14
10424|Limmen Sandstone|42639|4|Described|p38|||||||||
10424|Limmen Sandstone|42700|5|Briefly described|map legend|Mesozoic|Early Cretaceous|||||||
10424|Limmen Sandstone|42739|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Of the Lower Roper Group. Predominantly fine to medium grained, thin to medium bedded quartzarenite with thin interbeds of micaceous mudstone.||||||19-OCT-05
10424|Limmen Sandstone|42812|3|Fully described|p45, Table 5|||Of Roper Group.||||||30-OCT-06
10424|Limmen Sandstone|42846|5|Briefly described|p503, Fig.1 p502|||Basal unit of Roper Group.||||||09-MAY-05
10424|Limmen Sandstone|43010|6|Mentioned|p145|||||||||
10424|Limmen Sandstone|43036|4|Described|p57|||Of Roper Group.||||||30-OCT-06
10424|Limmen Sandstone|43149|5|Briefly described|Map Legend||Mesoproterozoic|Of Roper Group. Of Calymmian age.||||||30-OCT-06
10424|Limmen Sandstone|43652|6|Mentioned|p386|||||||||
10424|Limmen Sandstone|44112|3|Fully described|Table12p68,69|||||||||
10424|Limmen Sandstone|44287|14|Not recorded|p.12, opp.11|||(E53-3).||||||
10424|Limmen Sandstone|44288|14|Not recorded|map legend|||Quartz sandstone, sandstone, siltstone Conglomerate. Upper (?) Proterozoic.||||||
10424|Limmen Sandstone|44299|4|Described|p.13|||SD/53-7,8. U(?) Proterozoic. Table 1.||||||
10424|Limmen Sandstone|44300|14|Not recorded|map legend|||SD/53-7,8. Upper (?) Proterozoic.||||||
10424|Limmen Sandstone|44332|14|Not recorded|p.7,opp.6,map|||(D53-14).||||||
10424|Limmen Sandstone|44333|14|Not recorded|map legend|||Upper(?) Proterozoic.||||||
10424|Limmen Sandstone|44400|2|Defined|p.9,12,Tb.1,opp.p.6|||Mt. Marumba (D53-6), map.||||||
10424|Limmen Sandstone|44401|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
10424|Limmen Sandstone|44434|14|Not recorded|p.7,8, opp.p.6, map|||||||||
10424|Limmen Sandstone|44435|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
10424|Limmen Sandstone|44436|5|Briefly described|p.10-13,opp. p.7,map|||(E53-4).||||||02-DEC-04
10424|Limmen Sandstone|44437|5|Briefly described|map legend|Precambrian|Precambrian|Of the Roper Group.  Massive fine- to medium-grained quartz sandstone, micaceous siltstone.  Conformably overlies the Karns Dolomite; conformably overlain by Mainoru Formation. Upper (?) Proterozoic.||||||08-DEC-04
10424|Limmen Sandstone|44459|14|Not recorded|p.8,9,opp.p.6, map|||(E53-2).||||||
10424|Limmen Sandstone|44460|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
10424|Limmen Sandstone|44471|14|Not recorded|p.9, opp.p.7, map|||(D53-10).||||||
10424|Limmen Sandstone|44472|5|Briefly described|map legend|||Of the Roper Group.  Massive and flaggy silicified quartz sandstone,micaceous quartz greywacke; basal quartz pebble conglomerate.  Upper (?) Proterozoic.||||||02-DEC-04
10424|Limmen Sandstone|44473|14|Not recorded|p.10, opp. p.7|||(E53-7). Basal Formation of Roper Group.||||||
10424|Limmen Sandstone|44474|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
10424|Limmen Sandstone|44530|14|Not recorded|p.11,14, opp.12|||(D53-15).||||||
10424|Limmen Sandstone|44531|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
10424|Limmen Sandstone|45022|5|Briefly described|p.80||Adelaidean|Of Roper Group. Tb.11. Pl.28.||||||
10424|Limmen Sandstone|45162|4|Described|p151, p4 Fig.4, p105|Proterozoic|Proterozoic|||Of Roper Group||||26-MAR-18
10424|Limmen Sandstone|46861|6|Mentioned|Fig.2|||||||||
10424|Limmen Sandstone|60483|5|Briefly described|p7 Fig. 5, p32|||Of the Roper Group. Geological Province: McArthur Basin.||||||05-OCT-07
10424|Limmen Sandstone|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Roper Group. Overlain by Mainoru Formation, underlain by Mantungula Formation.||||||
10424|Limmen Sandstone|60573|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Roper Group.  Quartz sandstone: thick to very thick bedded, fine-to coarse-grained, graniule to pebble-rich towards base; minor micaceous siltstone. Overlies Mantungula Formation; underlies Mainoru Formation.||||||15-FEB-05
10424|Limmen Sandstone|60574|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Roper Group. Overlies the Mantungula Formation. Overlain by the Mainoru Formation. Pink to white fine-grained quartzose sandstone with current lineation.||||||
10424|Limmen Sandstone|61390|5|Briefly described|Map Legend|Ectasian|Calymmian|Of the Collara Subgroup. Quartz sandstone: thick to very thick bedded, fine to very coarse grained, granule to pebble rich towards base, planar and trough cross bedded, current ripples; minor micaceous siltstone.||||||
10424|Limmen Sandstone|61403|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Roper Group. Does not crop out in BLUE MUD BAY map sheet. Subdivided into two units: first, quartz arenite, and second, upper part: sandstone with lower part: mudstone. Geol. Prov: McArthur Basin.||||||
10424|Limmen Sandstone|61566|5|Briefly described|p622|Proterozoic|Proterozoic|Oldest unit of the Roper Group. Morphologically prominent mature quartzite and sandstone deposits; exhibits shatter cones related to the Strangways impact event, and occasionally monomict brecciation. Geological Province: McArthur Basin.||||||26-APR-06
10424|Limmen Sandstone|62376|5|Briefly described|p38|Mesoproterozoic|Mesoproterozoic|Of the Roper Group. Geological Province: Beetaloo Sub-Basin.||||||09-FEB-10
10424|Limmen Sandstone|64784|5|Briefly described|p2 Fig.2 |Proterozoic|Proterozoic|Beetaloo Basin.||Unit in Roper Group.||Is overlain by Mainoru Formation.||
10424|Limmen Sandstone|64815|6|Mentioned|p5 Fig.3, p17  |||||Of the Roper Group.||||
10424|Limmen Sandstone|64816|6|Mentioned|p2 Fig.1 |||||Unit in Roper Group.||||
10424|Limmen Sandstone|64817|6|Mentioned|p353 Fig.4 |||||Of the Roper Group.||||
10424|Limmen Sandstone|64975|6|Mentioned|p162 Fig.6.|Mesoproterozoic|Mesoproterozoic|||Unit in Roper Group.||||
10424|Limmen Sandstone|65228|5|Briefly described|Figs.02, 24.|||McArthur Basin.||Unit in Roper Group.||Overlies Mantungula Formation and Dungaminnie Formation. Is overlain by Mainoru Formation.||
10424|Limmen Sandstone|65236|5|Briefly described|p3 Fig. 3|Mesoproterozoic|Mesoproterozoic|Of the Roper Group. Geological province: Beetaloo Sub-basin.||||||04-JUN-09
10424|Limmen Sandstone|65340|4|Described|p62, pp66-67. |Mesoproterozoic|Mesoproterozoic|Forms a broad north-striking resistant ridge in western ROBINSON RIVER. Outcrops as large, rounded boulders. Occasional planar and trough crossbeds; rare asymmetric ripples. Interpreted as marine shelf deposits, above fair-weather wave base. Forms a concentrically striking outcrop around a 6 km diameter circular outcrop of Bukalara Sandstone at the Foelsche impact structure.||Unit in Roper Group.||Overlies Mantungula Formation; locally unconformably overlies Karns Dolomite. Is overlain by Mainoru Formation.|White to pale pink or maroon, strongly silicified, medium to thickly bedded, fine quartzose sandstone; characteristic fine parallel lamination; poorly bedded to massive; thin brown iron oxide weathered carapace.|
10424|Limmen Sandstone|65342|6|Mentioned|p8.|||McArthur Basin. Max. thickness at least 39 m.||Unit in Roper Group.||Overlies Mantungula Formation. Is overlain by Mainoru Formation.||
10424|Limmen Sandstone|67144|5|Briefly described|Map legend.|Calymmian|Calymmian|Ridge-forming.||Unit in Roper Group.||Overlies Balbirini Dolostone. Is overlain by Mainoru Formation.|Fine-grained structureless quartz arenite with clay clast imprints, minor ripples and cross-beds; interbedded with grey micaceous siltstone; very fine-grained sandstone and iron-stained, poorly-sorted pebbly sandstone; local basal regolith breccia.|
10424|Limmen Sandstone|67352|4|Described|p13 Tb.2, p58|Calymmian|Calymmian|McArthur Basin. 1350m thick.||Roper Group||Overlies (unconformably) Nathan or McArthur Groups. Overlain conformably by Mainoru Formation.|Fine- to medium-grained quartz arenite, commonly equant and intensely silicified; local tabular micaceous or pebbly sandstone, siltstone, limestone; basal beds conglomeratic or silty.|
10424|Limmen Sandstone|69018|5|Briefly described|p450 Fig.1b|Calymmian|Calymmian|||Of Roper Group.||||
10424|Limmen Sandstone|69430|4|Described|p15:3, 24-27, 30, 34, 43, 48, 62|Calymmian|Calymmian|McArthur Basin. 20-100m thick. Fluvial to shallow-marine shoreline sandstone.||Basal Collara Subgroup.||Overlies Dook Creek Formation (Mount Rigg Group) unconformably and Mantungula Formation ?disconformably (erosive contact). Is overlain conformably by Gibb Member (Mainoru Formation).|Fine to very coarse and granule-rich quartz sandstone; minor micaceous siltstone.|12-JUL-16
10424|Limmen Sandstone|69673|6|Mentioned|p16 fig 13|||McArthur Basin.||Collara Subgroup||Overlain by Mainoru Formation, Unconformably? Overlies Dook Creek Formation||
10424|Limmen Sandstone|70734|5|Briefly described|p16 Fig. 2|||McArthur Basin. Tidal platform sandstone.||Of Collara Subgroup.||Overlies Mantungula Formation, overlain by Mainoru Formation.||
10424|Limmen Sandstone|70822|5|Briefly described|p102 fig 1 (A)|Mesoproterozoic|Mesoproterozoic|||Roper Group.||Overlies Mantungula Formation; overlain by Gibb Member (Mainoru Formation).|Sandstone.|
10424|Limmen Sandstone|70897|5|Briefly described|p43, Fig.1.7.6,9|Mesoproterozoic|Mesoproterozoic|McArthur Basin.||Roper Group.||Overlies Dungaminnie Formation unconformably and Mantungula Formation conformably.|Fine- to medium-grained quartz sandstone; commonly with pebbles of chertified carbonates at the base.|
10424|Limmen Sandstone|70968|2|Defined|p6, p10-17, p21-23, p25, p124, p126-129|Calymmian|Calymmian|See also p131, p138-140, p143-144. Sweet in Abbott et al. (2001) after Dunn (1963). Originally mapped as Canopy Rock Sandstone (Ruker, 1959); also mapped as Mallison Sandstone and lower Wigram Formation of the Malay Road Group, and as part of Baralminar beds: all these names are superseded. Previously included rocks now part of Mantungula Formation; and the upper part near Roper Bar has been reassigned to the Gibb and Wadjeli Sandstone Members of Mainoru Formation. Named after Limmen Bight River. Type section is near Mission Gorge, from 477100mE 8378900mN (base) to 478100mE 8381000mN in URAPUNGA sheet. Forms mesas, cuestas or narrow ridges. Very widespread. Represents basal Roper Group locally. Lithology described and illustrated in detail. Shallow marine deposits. Thickness c.130m to estimated maximum of c.300m. Detrital zircon diagram.||Collara Subgroup.||Overlies Mantungula Formation conformably; Dook Creek Formation (Mount Rigg Group), McArthur and Nathan Groups unconformably; Urapunga Granite nonconformably. Conformably underlies Mainoru Formation.|Indurated, white, thickly bedded, medium- to very coarse-grained quartz sandstone, minor pebbly sandstone and conglomerate; overlain by fine- to medium-grained, well sorted quartz sandstone with thin interbeds of micaceous sandstone and siltstone.|
10424|Limmen Sandstone|71059|4|Described|p3|Mesoproterozoic|Mesoproterozoic|McArthur Basin. 15 - 130+ m thick. Coastal tidal platform, possibly some fluvial, deposits.||Collara Subgroup.||Conformably overlies Mantungula Formation. Is overlain conformably by Gibb Member, and locally disconformably by Nullawun Member, (Mainoru Formation).|Fine to very coarse and granule-rich quartz sandstone; minor micaceous siltstone.|
10424|Limmen Sandstone|71488|5|Briefly described|p141 fig 1b|||||Collara Subgroup||Overlies the Mantungula Formation. Overlain by the Mainoru Formation.||
10424|Limmen Sandstone|71494|4|Described|p2-p4, p7-p8, p17-p19, p22-p23, p26|||20-100m thick. Deposited in a fluvial to shallow marine or shoreline environment. Referred to as the Limmen Formation on p23.||||Unconformably overlies the Mantungula Formation. Conformably overlain by the Gibb member; disconformably overlain by the Nullawun Member.|Fine to very coarse and granule-rich quartz sandstone; minor micaceous siltstone.|
10424|Limmen Sandstone|71779|5|Briefly described|p2 Fig. 1|||Urapunga, Beetaloo Sub-basin and Bauhinia Downs Regions, McArthur Basin.||Collara Subgroup||||24-SEP-18
10424|Limmen Sandstone|71893|3|Fully described|iii, p2-p5, p8, p13-p15|Calymmian|Calymmian|McArthur Basin. A type section occurs near Mission Gorge in the Collara Mountains about 10km northeast of Ngukurr in central-northern Urapunga. Zircon description, description at type section, sample locality, LAICPMS U-Pb and Hf analysis, results and interpretation are provided. The youngest individual date obtained was 1615 +/- 50 Ma a maximum depositional age of 1629 +/- 23 Ma was obtained. 5-10m thick. Age is constrained to be between 1589 +/- 3 Ma to 1492 +/- 4 Ma on the basis of dating of the underlying Nathan Group and overlying Showell Member respectively.||Collara Subgroup||Disconformably (probably) overlies the Mantungula Formation. Unconformably overlies the McArthur and Nathan groups. Conformably (locally disconformably) overlain by the Mainoru Formation.|Thickly- to very thickly-bedded, medium- to very coarse-grained or granule rich fluvial quartz sandstone overlain by a medium to thickly bedded, fine-grained quartz sandstone.|
10424|Limmen Sandstone|72526|5|Briefly described|p8 Fig.1.3.|Calymmian|Calymmian|Shown as located in the Urapunga Fault Zone, Beetaloo Sub-basin, Batten Fault Zone and Southeastern McArthur Basin. Minimum age from overlying Mainoru Formation.||Collara Subgroup||Overlies Mantungula Formation and underlies Mainoru Formation.||
10424|Limmen Sandstone|72718|6|Mentioned|p7|||Southern McArthur Basin.||Collara Subgroup, Roper Group||Partly underlain by Mantungula Formation. Overlain by Mainoru Formation.||
10424|Limmen Sandstone|72912|5|Briefly described|p5 Fig.3.|Mesoproterozoic|Mesoproterozoic|Located in the Urapunga Fault Zone, Beetaloo Sub-basin and the Batten Fault Zone in the Southern McArthur Basin.||Collara Subgroup||Overlies Mantungula Formation and underlies Mainoru Formation.||
10424|Limmen Sandstone|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|Southern McArthur Basin, Roper Superbasin.||Collara Subgroup, Roper Group||Underlain by Mantungula Formation. Overlain by Mainoru Formation.||
10424|Limmen Sandstone|73083|6|Mentioned|p40|||||||||
10424|Limmen Sandstone|73242|5|Briefly described|p39|||||Collara Subgroup, Roper Group||Underlain by Mantungula Formation. Overlain by Gibb Member, Mainoru Formation.|Includes tidal Sandstone.|
10424|Limmen Sandstone|73280|6|Mentioned|p1, p4-5, App.1A, App.1C|||McArthur Basin. Sampled for XRD mineralogy to investigate brittleness and Kubler indices [see report].||||||
10424|Limmen Sandstone|73412|5|Briefly described|p4, 8|||Southern McArthur Basin.||Collara Subgroup.||Unconformably overlies upper Balbirini Dolostone (Nathan Group). Is overlain by Mainoru Formation.||
10441|Linnekar Limestone|14019|5|Briefly described|p21|Middle Cambrian|Middle Cambrian|Of the Negri Subgroup (Goose Hole Group).  Geological Province: Ord Basin.||||||
10441|Linnekar Limestone|22537|5|Briefly described|40|||||||||
10441|Linnekar Limestone|23821|5|Briefly described|p244|Middle Cambrian|Middle Cambrian|Of Negri Group. Geological Province: Ord Basin.  Maximum thickness: 40m.||||||
10441|Linnekar Limestone|24303|6|Mentioned|p63 Appendix|||Geological Province: Ord Basin. Correlative of Gum Ridge Formation.||||||
10441|Linnekar Limestone|28255|3|Fully described|p97, Tb. 9 (before p83), p144 App.|Late Cambrian|Cambrian|Of the Negri Group. Grey, flaggy, crystalline limestone with interbedded siltstone and shale; chert nodules abundant; fossiliferous. Conformably overlies Nelson Shale; conformably underlies Panton Formation. Max. thickness: 20m. Geol.Prov: Hardman Basin.||||||03-DEC-12
10441|Linnekar Limestone|32172|4|Described|Table 2|||Middle Cambrian. Negri Gp.||||||
10441|Linnekar Limestone|32173|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Of the Negri Group.  Grey, flaggy, fossiliferous limestone, minor siltstone interbeds.  Conformably underlies the Panton Formation; conformably overlies the Nelson Shale.||||||17-NOV-04
10441|Linnekar Limestone|32648|6|Mentioned|p32|||M. Camb.||||||
10441|Linnekar Limestone|33376|6|Mentioned|Map legend|Early Ordovician|Middle Cambrian|Middle Cambrian to Lower Ordovician||||||
10441|Linnekar Limestone|36551|6|Mentioned|Table 16|||||||||
10441|Linnekar Limestone|36890|3|Fully described|p397|||||||||
10441|Linnekar Limestone|39210|6|Mentioned|p48|||||||||
10441|Linnekar Limestone|40993|6|Mentioned|Fig.1|||||||||
10441|Linnekar Limestone|40996|6|Mentioned|p403|||||||||
10441|Linnekar Limestone|41840|3|Fully described|p42|||||||||
10441|Linnekar Limestone|41864|4|Described|p18|||||||||
10441|Linnekar Limestone|41865|5|Briefly described|Map legend||Early Cambrian|||||||
10441|Linnekar Limestone|41866|5|Briefly described|Map legend|Early Cambrian||||||||
10441|Linnekar Limestone|42070|6|Mentioned|Fig.9 P12|||||||||
10441|Linnekar Limestone|42477|5|Briefly described|p68|||||||||
10441|Linnekar Limestone|42771|6|Mentioned|p15|||||||||
10441|Linnekar Limestone|44230|5|Briefly described|Map Legend||Middle Cambrian|||||||
10441|Linnekar Limestone|44317|4|Described|Table 4||Cambrian|||||||
10441|Linnekar Limestone|44318|14|Not recorded|map legend||Middle Cambrian|Mid.Cambrian.||||||
10441|Linnekar Limestone|44363|5|Briefly described|p.6,18,21||Middle Cambrian|Middle Cambrian (Negri Group).||||||
10441|Linnekar Limestone|44364|14|Not recorded|map legend|||||||||
10441|Linnekar Limestone|44868|5|Briefly described|Map Legend|Boomerangian|Ordian|||||||
10441|Linnekar Limestone|44965|14|Not recorded|Not recorded|||||||||
10441|Linnekar Limestone|45055|6|Mentioned|p10|||Fossil locality||||||
10441|Linnekar Limestone|45062|6|Mentioned|p74|||||||||
10441|Linnekar Limestone|48943|3|Fully described|p109|||Strat. table p140.||||||30-OCT-06
10441|Linnekar Limestone|60419|3|Fully described|p1, 3 Fig.2, p6-7|Middle Cambrian|Middle Cambrian|Of Negri Subgroup. Conformably overlies Nelson Shale. Conformably overlain by Panton Formation. Max. thickness: 40m. Thinly bedded calcimudstone, marl and mudstone, and thicker bioclast wackestone. Contains Ordian fauna. Geological Province: Ord Basin.||||||
10441|Linnekar Limestone|60519|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Negri Subgroup (Goose Hole Group). Laminated micritic limestone, shale and calcareous shale; contains chert, stromatolites, and macrofossils locally. Geological Province: Ord Basin.||||||03-NOV-04
10441|Linnekar Limestone|60589|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Of the Negri Subgroup (Goose Hole Group).  Stromatolitic and fossiliferous limestone and calcareous shale, local chert. Conformably overlies the Nelson Shale; conformably overlain by Panton Formation.  Geological Province: Ord Basin.||||||15-DEC-08
10441|Linnekar Limestone|62789|6|Mentioned|p133|Cambrian|Cambrian|In Ord Basin. Contains Redlichia forresti assemblage of very low diversity.||||||
10441|Linnekar Limestone|64580|6|Mentioned|map legend|||Of Goose Hole Group.||||||15-DEC-08
10441|Linnekar Limestone|67352|6|Mentioned|p20|Middle Cambrian|Middle Cambrian|Ord Basin. Contains a widespread (NT-SA-Antarctica) fossil fauna.||||||
10441|Linnekar Limestone|67860|4|Described|p417 fig 4-85, p419 Tb. 4-18, p421|Middle Cambrian|Middle Cambrian|8-24 m thick. Type section details given. Fossiliferous.||Negri Subgroup||Conformably overlies Nelson Shale. Is overlain conformably by Panton Formation.|Basal micritic limestone with chert nodules; middle trilobitic shale; upper limestone and shale.|
10441|Linnekar Limestone|69099|4|Described|GEOL_LUT_CSV files + geochron files|Series 3||Ord Basin||Negri Subgroup|||Basal micritic limestone; middle trilobitic shale; upper limestone and shale.|31-JUL-15
10441|Linnekar Limestone|69165|5|Briefly described|100k_interpgeop_lut.csv|Cambrian|Cambrian|See also 500k_geologyp08_lut.csv.||Negri Subgroup|||Basal micritic limestone; middle trilobitic shale; upper limestone and shale.|
10441|Linnekar Limestone|69437|5|Briefly described|p22:10-11|Series 3|Series 2|Ord Basin, Centralian B Superbasin. Sequence 1.||Negri Subgroup.||Overlies Nelson Shale. Is overlain by Panton Formation.||12-JUL-16
10441|Linnekar Limestone|69446|6|Mentioned|p31:3|||Ord Basin. Strong species-level similarity with correlative faunas of Tindall Limestone (Daly Basin).||||||12-JUL-16
10441|Linnekar Limestone|69447|6|Mentioned|p32:2|||Ord Basin. Has strong species-level correlative faunas with Montejinni Limestone and Hooker Creek Formation (Wiso Basin).||||||12-JUL-16
10441|Linnekar Limestone|69448|4|Described|p33:2-6, 8|Middle Cambrian|Middle Cambrian|Traves (1955); Playford et al. (1975). Ord Basin. Up to 40m thick; generally 8-31m. Peritidal to shallow subtidal deposits. Appears as Linnekar Sandstone in Fig.33.3. Ordian age. Hosts a number of uneconomic base metal anomalies.||Negri Subgroup.||Conformably overlies Nelson Shale. Is overlain conformably and gradationally by Panton Formation.|Microbial, bioclast and oncoid limestone, alternating with fossiliferous grey to olive-brown mudstone and marl. Low-diversity fauna of trilobite Redlichia forresti, hyolith Guduguwan hardmani, and brachiopods.|12-JUL-16
10441|Linnekar Limestone|69634|4|Described|GEOL_LUT_CSV files|Series 3|Series 3|Geological province: Halls Creek Orogen. Of Ord Basin. Events: Alice Springs Orogeny. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|505-497 Ma (Inferred)|Unit of Negri Subgroup.|||Basal micritic limestone; middle trilobitic shale; upper limestone and shale|
10441|Linnekar Limestone|69673|5|Briefly described|p142, p192, p193|Cambrian|Cambrian|40m thick.||Negri Subgroup||Overlain by Panton Formation, overlies Nelson Shale|Microbial, bioclast and oncoid limestones alternating with fossiliferous mudstone and marl.|
10441|Linnekar Limestone|70154|5|Briefly described|100k_interpgeop_lut.csv|Cambrian|Cambrian||497-505 Ma|Negri Subgroup|||Basal micritic limestone; middle trilobitic shale; upper limestone and shale.|
10441|Linnekar Limestone|71267|4|Described|GEOL_LUT_CSV files|Series 3|Series 3|Geological province: Halls Creek Orogen. Of Ord Basin. Events: Alice Springs Orogeny (450-295 Ma); Pertnjara-Brewer Movements (Alice Springs Orogeny phase 2) (390-360 Ma); Rodingan Movement (Alice Springs Orogeny phase 1) (450-420 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|505-497 Ma (inferred)|Unit of Negri Subgroup.|||Basal micritic limestone; middle trilobitic shale; upper limestone and shale|
10441|Linnekar Limestone|71800|5|Briefly described|p25-p26|Middle Cambrian|Middle Cambrian|Ord Basin.||Negri Subgroup||Overlies the Nelson Shale. Overlain by the Panton Formation.||
10441|Linnekar Limestone|73255|6|Mentioned|p534 Fig.2|Cambrian|Cambrian|||Goose Hole Group||Overlies the Nelson Shale, underlies the Panton Formation.||
10466|Litchfield Complex|9538|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Granite, granodiorite, pegmatite, migmatite.||||||07-NOV-08
10466|Litchfield Complex|23714|6|Mentioned|p14|||||||||
10466|Litchfield Complex|32170|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10466|Litchfield Complex|32171|4|Described|Table 1|||Carpentarian p8.||||||30-OCT-06
10466|Litchfield Complex|32307|4|Described|Table 1|||Carpentarian||||||
10466|Litchfield Complex|32309|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10466|Litchfield Complex|32310|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10466|Litchfield Complex|32659|6|Mentioned|Map legend|Paleoproterozoic|Archean|Archaean or Lower Proterozoic||||||07-NOV-08
10466|Litchfield Complex|32660|5|Briefly described|Table 2|||||||||
10466|Litchfield Complex|32700|4|Described|Table 1|||See also p13. Age: 1820 my.||||||30-OCT-06
10466|Litchfield Complex|32819|6|Mentioned|p36|||||||||
10466|Litchfield Complex|33076|6|Mentioned|Map legend|Paleoproterozoic|Archean|Archaean to Lower Proterozoic||||||07-NOV-08
10466|Litchfield Complex|33093|4|Described|Table 2|||||||||
10466|Litchfield Complex|33278|6|Mentioned|Fig.7|||||||||
10466|Litchfield Complex|33376|6|Mentioned|Map legend|Paleoproterozoic|Archean|Archaean and/or Lower Proterozoic||||||07-NOV-08
10466|Litchfield Complex|33377|6|Mentioned|Table 1|||Strat.||||||
10466|Litchfield Complex|35061|6|Mentioned|p143|||||||||
10466|Litchfield Complex|35140|6|Mentioned|Fig.1|||||||||
10466|Litchfield Complex|35465|6|Mentioned|Fig.2|||Summary of positions of magnetic units in the Lower Proterozoic||||||
10466|Litchfield Complex|35495|6|Mentioned|Fig.2|||||||||
10466|Litchfield Complex|35950|6|Mentioned|Fig.1|||||||||
10466|Litchfield Complex|36473|6|Mentioned|Map legend|Proterozoic|Archean|Archaean to Proterozoic||||||07-NOV-08
10466|Litchfield Complex|37462|6|Mentioned|p220|||||||||
10466|Litchfield Complex|37579|5|Briefly described|Regional setting map legend|Paleoproterozoic|Paleoproterozoic|Granite, granodiorite, pegmatite, migmatite.||||||07-NOV-08
10466|Litchfield Complex|38066|6|Mentioned|Fig.9|||p53.||||||30-OCT-06
10466|Litchfield Complex|38884|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
10466|Litchfield Complex|39563|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
10466|Litchfield Complex|39801|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Granite, granodiorite, pegmatite, migmatite.||||||07-NOV-08
10466|Litchfield Complex|39889|4|Described|p485|||||||||
10466|Litchfield Complex|40168|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Granite, granodiorite, pegmatite, migmatite.||||||07-NOV-08
10466|Litchfield Complex|40223|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Granite, granodiorite, pegmatite, migmatite.||||||07-NOV-08
10466|Litchfield Complex|40823|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
10466|Litchfield Complex|41407|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
10466|Litchfield Complex|41586|6|Mentioned|Map legend|||||||||
10466|Litchfield Complex|43595|5|Briefly described|p229||Paleoproterozoic|||||||07-NOV-08
10466|Litchfield Complex|43624|6|Mentioned|Table 1,p9|Paleoproterozoic|Archean|||||||07-NOV-08
10466|Litchfield Complex|44314|2|Defined|p.9,10,map|||(D52-4). Darwin Sheet.||||||
10466|Litchfield Complex|44315|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
10466|Litchfield Complex|45003|14|Not recorded|p18|||||||||
10466|Litchfield Complex|45022|3|Fully described|p.132,133||Precambrian|On many pages. Age given as L.Precambrian, what does it mean?||||||
10466|Litchfield Complex|45112|5|Briefly described|Table 4|||||||||
10466|Litchfield Complex|46163|14|Not recorded|p.171|||||||||
10466|Litchfield Complex|46658|5|Briefly described|p555|||||||||
10466|Litchfield Complex|46675|5|Briefly described|Map legend for regional setting...|Paleoproterozoic|Paleoproterozoic|Granite, granodiorite, pegmatite, migmatite.  Geological Province: Pine Creek Geosyncline.||||||07-NOV-08
10466|Litchfield Complex|46676|14|Not recorded|p.9|||||||||
10466|Litchfield Complex|48916|6|Mentioned|p.13|||||||||
10466|Litchfield Complex|48942|3|Fully described|p24|||||||||
10466|Litchfield Complex|60526|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Granite, granodiorite, pegmatite, migmatite.||||||
10466|Litchfield Complex|64730|6|Mentioned|p123|Paleoproterozoic|Paleoproterozoic|Used in 'province' sense.|||||Amphibolite to granulite facies metasedimentary rocks and granites.|03-MAY-12
10515|Ljiltera Member|9199|5|Briefly described|Map legend|Devonian|Devonian|Of the Hermansburg Sandstone (Pertnjara Group).  Pebbly sandstone and sandstone.  Geological Province: Amadeus Basin.||||||
10515|Ljiltera Member|9814|5|Briefly described|Map Legend|Devonian|Devonian|Of the Hermannsburg Sandstone. Sandstone.||||||
10515|Ljiltera Member|22760|4|Described|p341|Late Devonian|Late Devonian|Of  Hermannsburg Sandstone.||||||30-OCT-06
10515|Ljiltera Member|22825|6|Mentioned|p543|||||||||
10515|Ljiltera Member|30544|6|Mentioned|p51|||Map legend||||||
10515|Ljiltera Member|31566|2|Defined|p240|Devonian|Devonian|||||||
10515|Ljiltera Member|31567|6|Mentioned|Fig. 3|||Diagrammatic cross section||||||
10515|Ljiltera Member|35102|6|Mentioned|p7|||||||||
10515|Ljiltera Member|38606|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
10515|Ljiltera Member|38885|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
10515|Ljiltera Member|39583|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
10515|Ljiltera Member|40740|5|Briefly described|Fig.30|||||||||
10515|Ljiltera Member|41018|6|Mentioned|p236|||||||||
10515|Ljiltera Member|41385|6|Mentioned|Fig.12|||||||||
10515|Ljiltera Member|41708|6|Mentioned|p198|||||||||
10515|Ljiltera Member|43225|5|Briefly described|Map Legend||Devonian|Of Pertnjara Group.||||||30-OCT-06
10515|Ljiltera Member|43503|6|Mentioned|16-43|Late Devonian|Middle Devonian|||||||
10515|Ljiltera Member|43649|6|Mentioned|p465|||||||||
10515|Ljiltera Member|60547|5|Briefly described|Map Legend|Devonian|Devonian|Of the Hermannsburg Sandstone. Pebbly sandstone and sandstone. Geological Province: Amadeus Basin.||||||
10515|Ljiltera Member|64809|6|Mentioned|p6 Fig.4 |Late Devonian|Late Devonian|||Of the Hermannsburg Sandstone.||||
10515|Ljiltera Member|67565|5|Briefly described|p42.|Devonian|Devonian|Reflects increased rates of uplift in the source area during deposition.||Unit in Hermannsburg Sandstone.|||An upper unit of medium- to coarse-grained pebbly sandstone.|
10515|Ljiltera Member|69438|3|Fully described|p23:7, 39-40|Devonian|Devonian|Jones (1972). Amadeus Basin. Type section is at Glen Helen Gorge where it forms 480m of orange to red-brown lithic and sublithic sandstones. Thins rapidly to the S.||Hermannsburg Sandstone.||Conformably overlies Ooraminna Sandstone, and Owen Springs Sandstone, Members. Is locally overlain transitionally by, or interdigitates with, Undandita Member (Brewer Conglomerate).|Pebbly and conglomeratic sandstones, becoming more conglomeratic towards the top with cobbles to 15cm common.|12-JUL-16
10515|Ljiltera Member|69673|6|Mentioned|p67|||||Hermannsburg Sandstone||Overlies Owen Springs Sandstone Member||
10515|Ljiltera Member|71279|6|Mentioned|p365|||||Hermannsburg Sandstone.||||
10515|Ljiltera Member|72369|5|Briefly described|p40|||Of Amadeus Basin.||Unit of Hermannsburg Sandstone.||||
10524|Lloyd Creek Formation|14019|5|Briefly described|p4 Fig. 3|||Of the Auvergne Group.  Geological Province: Victoria Basin.||||||
10524|Lloyd Creek Formation|24122|5|Briefly described|p4 Fig.3|||Of Auvergne Group.  Geological Province: Victoria Basin.||||||
10524|Lloyd Creek Formation|24297|5|Briefly described|p4 Fig.3|||Of Auvergne Group.  Geological Province: Victoria Basin.||||||
10524|Lloyd Creek Formation|24441|5|Briefly described|p1 Fig. 1|Mesoproterozoic|Mesoproterozoic|Of the Auvergne Group. Overlies Pinkerton Sandstone; overlain by Spencer Sandstone. Geological Province: Victoria Basin.||||||25-JAN-06
10524|Lloyd Creek Formation|24442|5|Briefly described|p50 Fig. 1|||Of the Auvergne Group.  Geological Province: Victoria Basin.||||||
10524|Lloyd Creek Formation|32170|6|Mentioned|Map legend|Adelaidean|Carpentarian|Adelaidean or Carpentarian||||||
10524|Lloyd Creek Formation|32307|4|Described|Table 2|||Proterozoic||||||
10524|Lloyd Creek Formation|32310|6|Mentioned|Map legend|Adelaidean|Carpentarian|Adelaidean/Carpentarian||||||
10524|Lloyd Creek Formation|32660|5|Briefly described|Table 6|||||||||
10524|Lloyd Creek Formation|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Auvergne Group.  Dolomite, oolitic and stromatolitic; sandy and silty dolomite; siltstone.||||||02-DEC-04
10524|Lloyd Creek Formation|32700|4|Described|Table 1|||Lithology p14. Re: Randal (1962).||||||30-OCT-06
10524|Lloyd Creek Formation|32701|4|Described|Table 1|||Adelaidean. Auvergne Gp. See p9.||||||30-OCT-06
10524|Lloyd Creek Formation|32728|6|Mentioned|Fig.14|||||||||
10524|Lloyd Creek Formation|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
10524|Lloyd Creek Formation|45112|6|Mentioned|Table 6|||||||||
10524|Lloyd Creek Formation|48938|2|Defined|p47|Proterozoic|Proterozoic|Measured section p96. ?Adelaidean||||||30-OCT-06
10524|Lloyd Creek Formation|48942|3|Fully described|p71|||||||||
10524|Lloyd Creek Formation|60006|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Victoria Basin. Of Auvergne Group. Overlies Pinkerton Sandstone. Overlain by Spencer Sandstone. Oolitic and microbial dolostone, quartzic and silty dolostone, sandstone, dolomitic siltstone.||||||
10524|Lloyd Creek Formation|60682|4|Described|p9 Table 2, 10|Cryogenian|Cryogenian|Of Auvergne Group. Conformably overlies Pinkerton Sandstone. Conformably overlain by Spencer Sandstone. Max. thickness: 162m. Geological Province: Victoria Basin. Dolostone, dololutite, dolarenite, dolomitic siltstone, quartz sandstone.||||||
10524|Lloyd Creek Formation|60685|5|Briefly described|p4 Fig. 3|Mesoproterozoic|Mesoproterozoic|Of the Auvergne Group. Geological Province: Victoria Basin.||||||
10524|Lloyd Creek Formation|65331|5|Briefly described|Map legend|Neoproterozoic |Neoproterozoic|Of Auvergne Group, Victoria Basin. Ooidal and microbial dolostone, quartzic and silty dolostone, sandstone, dolomitic siltstone||||||
10524|Lloyd Creek Formation|65342|6|Mentioned|p11 Fig.13. |||Victoria Basin.||Unit in Auvergne Group.||Overlies Pinkerton Sandstone. Is overlain by Spencer Sandstone.||
10524|Lloyd Creek Formation|67167|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|||Unit in Auvergne Group.|||Ooidal and microbial dolostone, quartzitic and silty dolostone, sandstone, dolomitic siltstone.|
10524|Lloyd Creek Formation|68733|6|Mentioned|p177 Fig.2, p189 Fig.8|Cryogenian|Cryogenian|Victoria Basin.||Of the Auvergne Group.||||05-DEC-17
10524|Lloyd Creek Formation|69437|5|Briefly described|p22:4-5|Cryogenian|Cryogenian|Victoria/Wolfe Basins, Centralian A Superbasin. Supersequence 1.||||Overlies Pinkerton Sandstone. Is overlain by Spencer Sandstone.||12-JUL-16
10524|Lloyd Creek Formation|69441|5|Briefly described|p26:2-5|Neoproterozoic|Neoproterozoic|Typically <90m thick, up to 162m locally. Shallow-marine, mixed carbonate/siliciclastic with wave action, storm deposits and brine-logging of sediments.||Auvergne Group.||Conformably overlies Pinkerton Sandstone. Is overlain conformably by Spencer Sandstone.|Dolostone (oolitic and microbial), quartzose and silty dolostone, dololutite, dolarenite, dolomitic siltstone, quartz sandstone. Rare glauconite grains.|12-JUL-16
10524|Lloyd Creek Formation|69673|5|Briefly described|p188|||162m thick.||Auvergne Group|||Oolitic and stromatolitic dolostone interbedded with dolarenite, quartzic dolostone and rippled quartz sandstone.|
10524|Lloyd Creek Formation|70206|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Victoria Basin.||Auvergne Group|||Oolitic and microbial dolostone, quartzic and silty dolostone, sandstone, dolomitic siltstone.|
10524|Lloyd Creek Formation|71302|5|Briefly described|p6|Neoproterozoic|Neoproterozoic|Of Victoria Basin.||Unit of Auvergne Group.||Overlain by Spencer Sandstone. Underlain by Pinkerton Sandstone.||
10524|Lloyd Creek Formation|73083|6|Mentioned|p8|||||||||
10558|Lochness Formation|22438|6|Mentioned|p549, Fig.12|||||||||
10558|Lochness Formation|22457|5|Briefly described|P31|||Of the Haslingden Group.||||||30-OCT-06
10558|Lochness Formation|22585|5|Briefly described|Fig2 P737, Fig3|||Actually spelt Lochness Fm. in text.||||||30-OCT-06
10558|Lochness Formation|23031|5|Briefly described|24|||Geol province: Mount Isa Fold Belt. Of the Myally Subgroup. Overllain by Torpedo Creek Quartzite, Suprise Creek Formation, Quilalar Formation; underlain by Withworth Quartzite.||||||19-DEC-07
10558|Lochness Formation|23395|5|Briefly described|p386 Fig.3|||Of Myally Subgroup.||||||30-OCT-06
10558|Lochness Formation|23396|4|Described|p418|Statherian|Statherian|of Myally Subgroup (Haslingden Group).||||||30-OCT-06
10558|Lochness Formation|23397|6|Mentioned|p464 Fig.3|||||||||
10558|Lochness Formation|23518|4|Described|p11|Proterozoic|Proterozoic|Of Myally Subgroup.  Geological Province: Western Fold Belt.||||||
10558|Lochness Formation|30534|2|Defined|p304|Carpentarian|Carpentarian|||||||
10558|Lochness Formation|33900|4|Described|p12|||||||||
10558|Lochness Formation|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10558|Lochness Formation|38232|6|Mentioned|p84|||||||||
10558|Lochness Formation|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10558|Lochness Formation|39445|5|Briefly described|Table 2|||See also p40.||||||30-OCT-06
10558|Lochness Formation|39556|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||
10558|Lochness Formation|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Myally Subgroup (Haslingden Group).  Overlies the Whitworth Quartzite; underlies the Quilalar Formation.||||||30-OCT-06
10558|Lochness Formation|39622|6|Mentioned|Fig.2|||See also Appendix||||||
10558|Lochness Formation|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10558|Lochness Formation|40221|3|Fully described|p10|||||||||
10558|Lochness Formation|41277|5|Briefly described|p83|||||||||
10558|Lochness Formation|41298|6|Mentioned|Map legend|Carpentarian||||||||
10558|Lochness Formation|41307|4|Described|p11|||||||||
10558|Lochness Formation|42676|5|Briefly described|Fig.2 P41|||||||||
10558|Lochness Formation|42818|4|Described|p211, Table 1 p209|||Of Myally Subgroup.||||||30-OCT-06
10558|Lochness Formation|45166|5|Briefly described|p14|||||||||
10558|Lochness Formation|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
10558|Lochness Formation|46960|6|Mentioned|p222|||||||||
10558|Lochness Formation|47083|4|Described|p7|||Youngest member of Myally Subgp (Haslingden Gp). Contains 3 informal members. Intruded by Weberra Granite. Conformably overlain by Quilalar Fm; conformably underlain by Whitworth Quartzite.||||||30-OCT-06
10558|Lochness Formation|50332|6|Mentioned|p17|Proterozoic|Proterozoic|Of the Myally Subgroup.||||||07-FEB-11
10558|Lochness Formation|50550|6|Mentioned|p1144 Fig.7||Statherian|Geological Province: Western Fold Belt.||||||19-DEC-07
10558|Lochness Formation|62988|5|Briefly described|p34|||Redbed playa facies. Geological Province: Mount Isa Inlier.||||||25-JAN-07
10558|Lochness Formation|63023|5|Briefly described|p1025 Fig. 2|||Of Myally Subgroup (Haslingden Group). Overlies Whitworth Quartzite; unconformably overlain by Quilalar Formation. Geological Province: Leichardt Superbasin.||||||
10558|Lochness Formation|63109|6|Mentioned|p1108 Fig. 3|||Overlain by Quilalar Formation, underlain by Whitworth Quartzite. Geological Province: Leichhardt Superbasin. Consists of siltstone.||||||
10558|Lochness Formation|63111|5|Briefly described|p1163 Fig. 3|Statherian|Statherian|Of Myally Subgroup. Overlain by Quilalar Formation, underlain by Whitworth Quartzite. Geological Province: Leichhardt Superbasin. Consists mostly of sandstone.||||||07-FEB-11
10558|Lochness Formation|63113|5|Briefly described|p1214 Fig.2, p1225 Fig.13.|||||Of the Myally Subgroup||Overlies Whitworth Quartzite. Is overlain by Quilalar Formation.||
10558|Lochness Formation|63114|5|Briefly described|p1253 Fig.2. |||||Of the Myally Subgroup||Overlies Whitworth Quartzite. Is overlain by Quilalar Formation.||
10558|Lochness Formation|63115|6|Mentioned|p1279 Fig.4.|||Leichhardt superbasin.||||||
10558|Lochness Formation|63116|6|Mentioned|p1297 Fig.2,p1299 Tb.1, |||Leichhardt superbasin. Material properties detailed.||||||
10558|Lochness Formation|64726|6|Mentioned|p87.||||c.1775-1755 Ma.|||||
10558|Lochness Formation|64834|5|Briefly described|p13 Fig.2|||Leichhardt Superbasin. Western Succession of Mount Isa Basin.||Myally Subgroup|||Sandstone.|
10558|Lochness Formation|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.||Myally Subgroup.|||Dolomitic feldspathic sandstone and siltstone, laminated ferruginous sandstone.|
10558|Lochness Formation|68021|5|Briefly described|p135|Statherian|Statherian|Towards top of Myally Supersequence. May represent excursion into evaporitic or shallow marine conditions.|||||Red beds with minor amounts of intercalated dolostone.|13-DEC-16
10558|Lochness Formation|68732|5|Briefly described|p160-162, p165 Fig.3|||Deposition in ephemeral playa and sandflat/dry mudflat environments. Of the Myally Supersequence.||Haslingden Group.|||Red siltstones and shales with desiccation cracks and weathering profiles, interpreted as paleosols, occur in this Formation.|01-DEC-17
10558|Lochness Formation|69591|5|Briefly described|p33, p57|||Mount Oxide and Leichhardt River Domains, Leichhardt Superbasin. Part of Myally Supersequence. Near shore/fluvial deposits.|||Myally Subgroup.|Overlies Alsace Quartzite.|Dolomitic feldspathic sandstone and siltstone, laminated ferruginous sandstone (redbeds).|
10558|Lochness Formation|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Myally Subgroup.||Overlies Whitworth Quartzite.|Dolomitic, feldspathic sandstone and siltstone and laminated ferruginous sandstone.|
10558|Lochness Formation|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Myally Subgroup.||Overlies Whitworth Quartzite.|Dolomitic, feldspathic sandstone and siltstone and laminated ferruginous sandstone.|
10558|Lochness Formation|71799|5|Briefly described|p154|||Leichardt Superbasin.|ca. 1750 Ma||||Stromatolite bearing dolostones.|
10558|Lochness 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 Bortala Formation and underlies Whitworth Quartzite.||
10558|Lochness 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 Bortala Formation and underlies Whitworth Quartzite.||
10558|Lochness Formation|72919|6|Mentioned|p63|||||Myally Subgroup, Myally Supersequence||||
10558|Lochness Formation|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Mount Isa Province, Leichhardt Superbasin.||Myally Subgroup||Underlain by Bortala Formation. Overlain by Whitworth Quartzite.||
10558|Lochness Formation|73525|6|Mentioned|p4-5 Fig.2, p19 Fig.13|||Leichhardt River Domain.|||||Clastics.|
10640|Longsight Sandstone|29591|6|Mentioned|Table 72|||||||||
10640|Longsight Sandstone|29961|4|Described|p12|||Cretaceous||||||
10640|Longsight Sandstone|30021|6|Mentioned|p87|||||||||
10640|Longsight Sandstone|30102|4|Described|p26|||See also P17,27,28,29.||||||
10640|Longsight Sandstone|30461|6|Mentioned|p100|||||||||
10640|Longsight Sandstone|30914|6|Mentioned|Map legend|Cretaceous|Jurassic|Jurassic - Cretaceous||||||
10640|Longsight Sandstone|31572|4|Described|Fig. 1|||L.Cretaceous||||||
10640|Longsight Sandstone|32275|6|Mentioned|p8|||Refers Casey (1959)||||||
10640|Longsight Sandstone|32576|6|Mentioned|p51|||||||||
10640|Longsight Sandstone|33073|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10640|Longsight Sandstone|33075|6|Mentioned|p451|||Refers Casey (1959)||||||
10640|Longsight Sandstone|33111|4|Described|p43|||Mention P6.||||||
10640|Longsight Sandstone|33164|6|Mentioned|Fig.4|||||||||
10640|Longsight Sandstone|33165|6|Mentioned|Chart|||Correlation chart only||||||
10640|Longsight Sandstone|33414|6|Mentioned|p212-214,Tb.||Neocomian|||||||
10640|Longsight Sandstone|33638|6|Mentioned|p10|||||||||
10640|Longsight Sandstone|33825|6|Mentioned|p10|||Correlation table||||||
10640|Longsight Sandstone|33964|6|Mentioned|p6|||Refers Casey (1968) & Yeates (1971).||||||
10640|Longsight Sandstone|34454|5|Briefly described|Table 2|||L.Cret.||||||
10640|Longsight Sandstone|34619|6|Mentioned|p.160, Pl.22||Cretaceous|||||||08-APR-13
10640|Longsight Sandstone|34847|6|Mentioned|p37|||||||||
10640|Longsight Sandstone|35121|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10640|Longsight Sandstone|35139|4|Described|Table.2|||||||||
10640|Longsight Sandstone|35811|6|Mentioned|p556|||Exploration carried out.||||||
10640|Longsight Sandstone|39211|6|Mentioned|p26|||||||||
10640|Longsight Sandstone|39445|5|Briefly described|Table 10|||||||||
10640|Longsight Sandstone|41125|6|Mentioned|p42|||||||||
10640|Longsight Sandstone|41247|6|Mentioned|p126|||||||||
10640|Longsight Sandstone|42397|6|Mentioned|Fig.2 P3|||||||||
10640|Longsight Sandstone|42447|6|Mentioned|p5 + Fig. 17|||Part equivalent to Westbourne Formation.||||||
10640|Longsight Sandstone|42474|5|Briefly described|p26|||||||||
10640|Longsight Sandstone|42749|5|Briefly described|p31|||see also Fig.2 P27||||||
10640|Longsight Sandstone|43105|5|Briefly described|Fig.9,p15|||||||||
10640|Longsight Sandstone|43122|5|Briefly described|p23|||see also Fig. 2.||||||
10640|Longsight Sandstone|43883|14|Not recorded|p18 Fig.4-3|||||||||
10640|Longsight Sandstone|43985|4|Described|p8,10-13,Fig.3,Pl.2|||||||||
10640|Longsight Sandstone|44031|14|Not recorded|p5,8|Cretaceous|Jurassic|||||||
10640|Longsight Sandstone|44082|6|Mentioned|Table p34||Aptian|Mention on correlation table of Queensland Cretaceous sediments.||||||
10640|Longsight Sandstone|44087|14|Not recorded|p4,7,opp.7|||||||||
10640|Longsight Sandstone|44119|14|Not recorded|Map Legend|Early Cretaceous|Late Jurassic|||||||
10640|Longsight Sandstone|44120|14|Not recorded|Map Legend|Early Cretaceous|Late Jurassic|||||||
10640|Longsight Sandstone|44121|14|Not recorded|p5-6,10-12|Early Cretaceous|Late Jurassic|||||||
10640|Longsight Sandstone|44122|2|Defined|p318-323,Fig.48|||||||||
10640|Longsight Sandstone|44168|4|Described|Tb.1,6,5,10,map|||||||||
10640|Longsight Sandstone|44212|14|Not recorded|p110|||Not on white card.||||||
10640|Longsight Sandstone|44276|4|Described|p25,Tb.2,map|||Aquifer.||||||
10640|Longsight Sandstone|44277|14|Not recorded|Map Legend||Early Cretaceous|||||||
10640|Longsight Sandstone|44291|2|Defined|Tb.1,p6,8,13,14,map||Early Cretaceous|Equivalent to upper part of Blythesdale Group.||||||
10640|Longsight Sandstone|44308|14|Not recorded|p2,11,13,Tb.2||Early Cretaceous|||||||
10640|Longsight Sandstone|44309|2|Defined|Tb.1,p7,13,14,map|||||||||
10640|Longsight Sandstone|44310|14|Not recorded|Map Legend||Early Cretaceous|||||||
10640|Longsight Sandstone|44312|14|Not recorded|Map Legend||Early Cretaceous|||||||
10640|Longsight Sandstone|44326|14|Not recorded|Map Legend||Early Cretaceous|||||||
10640|Longsight Sandstone|44346|14|Not recorded|p4,5,10|||||||||
10640|Longsight Sandstone|44361|14|Not recorded|Map Legend||Early Cretaceous|||||||
10640|Longsight Sandstone|44362|4|Described|p11,Tb.1||Early Cretaceous|||||||
10640|Longsight Sandstone|44376|14|Not recorded|p4,5|||||||||
10640|Longsight Sandstone|44406|14|Not recorded|p4,opp.p6|||||||||
10640|Longsight Sandstone|44408|14|Not recorded|p4,opp.p6|||||||||
10640|Longsight Sandstone|44469|2|Defined|opp.p.6,p.12, Tb.I||Cretaceous|(F53-12). Rhizocorallium, wood.||||||
10640|Longsight Sandstone|44470|5|Briefly described|map legend||Cretaceous|||||||02-DEC-04
10640|Longsight Sandstone|44543|2|Defined|p34,36||Early Cretaceous|Underlies Wilgunyah Formation.||||||
10640|Longsight Sandstone|44611|14|Not recorded|p22|||||||||
10640|Longsight Sandstone|44634|14|Not recorded|p30|||||||||
10640|Longsight Sandstone|44920|14|Not recorded|Map Legend,Sheet 4||Cretaceous|||||||
10640|Longsight Sandstone|45004|14|Not recorded|p.8,20,32,36,38-63|||On many pages.||||||
10640|Longsight Sandstone|45051|6|Mentioned|Fig.2A|||Lower Cretaceous. See also Fig.5A, 3.||||||
10640|Longsight Sandstone|45052|5|Briefly described|p134|||Cretaceous||||||
10640|Longsight Sandstone|45094|6|Mentioned|p9|||Cret.||||||
10640|Longsight Sandstone|45103|6|Mentioned|p5|||||||||
10640|Longsight Sandstone|48906|14|Not recorded|p5,Tb.2,App.C,Pl.1|Early Cretaceous|Late Jurassic|||||||
10640|Longsight Sandstone|48908|14|Not recorded|Tb.1||Early Cretaceous|||||||
10640|Longsight Sandstone|49027|5|Briefly described|p21|||||||||
10640|Longsight Sandstone|60122|5|Briefly described|p35|Cretaceous|Cretaceous|Subsumed into Hooray Sandstone, together with the Tarlton Formation (Mond and Harrison, in Senior et al 1978).||||||
10640|Longsight Sandstone|63450|5|Briefly described|p83|Cretaceous|Jurassic|As defined by Casey (1959) contained two distinct facies, a lower fluvial facies and upper glauconitic marine facies. The latter may be equivalent to Cadna-owie Formation.||||||08-APR-13
10640|Longsight Sandstone|66915|5|Briefly described|p9, p11 Fig.7|||Western Eromanga Basin.||||Is overlain by Wallumbilla Formation on western margin of Eromanga Basin, at C-horizon boundary.||
10640|Longsight Sandstone|67323|5|Briefly described|GIS attrib tbl, p92 Fig.12.2|Cretaceous|Jurassic|See also Solid Geology Map. Galilee/Eromanga/Carpentaria Basins.||||Overlies Ethabuka Sandstone. Is overlain by Wallumbilla Formation.|Sandstone, ferruginous sandstone, conglomerate, some siltstone.|
10640|Longsight Sandstone|67402|6|Mentioned|p214|Cretaceous|Cretaceous|Aquifer unit.||||||
10640|Longsight Sandstone|68553|6|Mentioned|Map legend; schematic diagram.|Early Cretaceous|Jurassic|Surat Basin. This unit, as well as Bungil, Orallo and Southlands Formations; Gubberamunda, Hooray and Mooga Sandstones, and Kumbarilla beds, are all mapped under the symbol, JKb.||||||
10640|Longsight Sandstone|69457|5|Briefly described|p41:6|||This name was applied (Smith 1963, 1965; Mond and Harrison in Senior et al. 1978) to outliers of Eromanga Basin strata in TOBERMOREY and HAY RIVER map areas. Some were remapped as undifferentiated Jurassic-Cretaceous by Kruse et al. (2002). They are most probably equivalents of the Algebuckina Sandstone (and possibly the Cadna-owie Formation).|||||Mesa-forming planar to cross-bedded, medium-coarse sandstone and minor mudstone, siltstone and conglomerate.|12-JUL-16
10640|Longsight Sandstone|69594|5|Briefly described|p526, p528|Barremian|Callovian|NW Eromanga Basin. Includes outliers of nominally Mesozoic sedimentary rocks that overlie elements of the Georgina Basin and Precambrian Mount Isa Province. Has been correlated with all units ranging from Hutton Sandstone to Wallumbilla Formation.||||Is overlain by Wallumbilla Formation.||
10647|Looking Glass Formation|22538|6|Mentioned|Fig3 P709|||Formation actually spelt Fmn in text.||||||30-OCT-06
10647|Looking Glass Formation|22664|6|Mentioned|46|Paleoproterozoic|Paleoproterozoic|Of the Batten Subgroup. In McArthur Basin||||||07-NOV-08
10647|Looking Glass Formation|22853|3|Fully described|23|Proterozoic|Proterozoic|Of Batten Subgroup. Max thickness 140 m, Overlain by Nathan Group; underlain by Stretton Sandstone.||||||30-OCT-06
10647|Looking Glass Formation|23397|5|Briefly described|p475|||||||||
10647|Looking Glass Formation|23405|5|Briefly described|p590|||||||||
10647|Looking Glass Formation|23406|5|Briefly described|p617|||Overlain by Amos Formation. Geological province: McArthur Basin. Part of the Term Supersequence. Has an extensively silicified top.||||||24-JUN-09
10647|Looking Glass Formation|23407|5|Briefly described|p627 Fig.2|||||||||
10647|Looking Glass Formation|23776|5|Briefly described|p705 Fig 2.|||Of Batten Subgroup.||||||
10647|Looking Glass Formation|23902|4|Described|p1568 Fig.2|||Of the Batten Subgroup. Overlies the Stretton Sandstone. Geological Province: McArthur Basin||||||
10647|Looking Glass Formation|23937|6|Mentioned|p13|||||||||
10647|Looking Glass Formation|23963|5|Briefly described|p1239 Fig.2|||Geological Province: McArthur Basin. Of the Batten Subgroup||||||
10647|Looking Glass Formation|30344|6|Mentioned|Fig.4|||Part of Batten Subgroup||||||
10647|Looking Glass Formation|32658|3|Fully described|Table 2|||See also Fig. 3.||||||30-OCT-06
10647|Looking Glass Formation|32660|5|Briefly described|Table 4|||||||||
10647|Looking Glass Formation|33666|6|Mentioned|Table 1|||||||||
10647|Looking Glass Formation|35261|6|Mentioned|Fig.2|||||||||
10647|Looking Glass Formation|38582|6|Mentioned|Fig.3|||||||||
10647|Looking Glass Formation|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
10647|Looking Glass Formation|40259|6|Mentioned|Table 1|||||||||
10647|Looking Glass Formation|40691|6|Mentioned|p61|||||||||
10647|Looking Glass Formation|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
10647|Looking Glass Formation|41220|4|Described|p368|||||||||
10647|Looking Glass Formation|41268|6|Mentioned|p296|||||||||
10647|Looking Glass Formation|41277|6|Mentioned|Fig.2|||||||||
10647|Looking Glass Formation|42385|4|Described|p23|||See also Table 4 p16.||||||30-OCT-06
10647|Looking Glass Formation|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
10647|Looking Glass Formation|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.||Of Batten Subgroup (McArthur Group).||In schematic section, underlies combined Balbirini Dolomite and Smythe Sandstone; overlies Stretton Sandstone.|Stromatolitic dolostone; dolarenite and sandy dolarenite. Detailed lithology given.|11-NOV-11
10647|Looking Glass Formation|42639|4|Described|p33, Table 5 p20|||||||||
10647|Looking Glass Formation|42812|6|Mentioned|Fig.5|||Of Batten Subgroup?||||||30-OCT-06
10647|Looking Glass Formation|42846|5|Briefly described|Fig.1 p502|||Of McArthur Group. Geological Province: McArthur Basin.||||||09-MAY-05
10647|Looking Glass Formation|42935|6|Mentioned|p529 Fig.2|||Of Batten Subgroup||||||30-OCT-06
10647|Looking Glass Formation|43010|6|Mentioned|p129|||||||||
10647|Looking Glass Formation|43036|6|Mentioned|Fig.5|||Of McArthur Group||||||30-OCT-06
10647|Looking Glass Formation|44287|14|Not recorded|p.10, opp.9|||Top fm of Batten Subgroup (McArthur Group). (E53-3).||||||
10647|Looking Glass Formation|44288|14|Not recorded|map legend|||Chert, chert-breccia, minor sandstone dolomitic siltstone. Lower (?) Proterozoic.||||||
10647|Looking Glass Formation|44530|14|Not recorded|p.10|||(D53-15).||||||
10647|Looking Glass Formation|45162|2|Defined|p130|Proterozoic|Proterozoic|Type section location given.||||||06-APR-18
10647|Looking Glass Formation|46915|6|Mentioned|Fig.1|||Stratigraphic section through McArthur Group.||||||
10647|Looking Glass Formation|46968|4|Described|p302|||See also Fig.3.||||||30-OCT-06
10647|Looking Glass Formation|46998|6|Mentioned|p290|||||||||
10647|Looking Glass Formation|60483|5|Briefly described|p7 Fig. 5, p30|||Of Batten Subgroup (McArthur Group). Geological Province: McArthur Basin.||||||05-OCT-07
10647|Looking Glass Formation|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Batten Subgroup. Underlain by Stretton Sandstone.||||||03-JUN-09
10647|Looking Glass Formation|63112|6|Mentioned|p1191 Fig.2|||Isa Superbasin; southern McArthur Basin. Age approximated from Fig.2.|c.1620-1615 Ma.|Unit in Term Supersequence.||||
10647|Looking Glass Formation|64815|6|Mentioned|p4 Fig.2, p5 Fig.3|||||Of the Batten Subgroup.||||
10647|Looking Glass Formation|64816|6|Mentioned|p2 Fig.1 |||||Unit in McArthur Group.||||
10647|Looking Glass Formation|64817|6|Mentioned|p353 Fig.4 |||||Of Batten Subgroup.||||
10647|Looking Glass Formation|65228|5|Briefly described|p35, Figs.02, 04, 23, 27.|||Part of Term Supersequence in McArthur River Region. Gamma ray log, lithofacies detailed. Measured section.||Unit in Batten Subgroup.||Overlies Stretton Sandstone.||
10647|Looking Glass Formation|66843|5|Briefly described|p24, p37, p38 Fig.10|||McArthur Basin. Has an erosional surface. These authors propose a significant time and stratigraphic break here.||McArthur Group.||Overlies Stretton Sandstone. Is overlain by Amos Formation.|Shallow-water carbonates c.100m thick that are everywhere (outcrop and drill hole) intensely silicified.|
10647|Looking Glass Formation|69018|5|Briefly described|p450 Fig.1b|Statherian|Statherian|Of McArthur Basin.||Of McArthur Group.||||
10647|Looking Glass Formation|69430|4|Described|p15:3, 16, 19, 34, 61-62|Statherian|Statherian|Southern McArthur Basin. 30-70m thick. Peritidal-shallow marine sediments. Fair to good conventional hydrocarbon reservoirs occur.||Batten Subgroup.||Conformably overlies Stretton Sandstone. Is overlain disconformably by Amos Formation.|Intensely silicified, commonly stromatolitic dolostone, dolarenite and sandy dolarenite; thin intervals of intraclast conglomerate.|12-JUL-16
10647|Looking Glass Formation|69673|6|Mentioned|p16 fig 13, p32, p40|||Batten Fault Zone. Reservoir rock. 30-70m thick.||Batten Subgroup||Conformably overlies Stretton Sandstone, disconformably overlain by Amos Formation|Silicified stromatolitic dolostone, sandy dolomudstone, sandy dolostone and dolomitic quartz sandstone with thin intervals of intraclastic conglomerate.|
10647|Looking Glass Formation|71374|6|Mentioned|p18|||||||Unconformably overlain by the Smythe Sandstone.||
10647|Looking Glass Formation|72248|5|Briefly described|p147|||Of McArthur Basin.||Unit of Batten Subgroup.||||
10647|Looking Glass Formation|72373|5|Briefly described|p14,22|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin.||||Underlain conformably by Stretton Sandstone.||
10647|Looking Glass Formation|72523|6|Mentioned|p2 Fig.2.|Statherian|Statherian|||Batten Subgroup||Overlies Stretton Sandstone and underlies Amos Formation.||
10647|Looking Glass Formation|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the southern part of the Batten Fault Zone.||Batten Subgroup||Overlies Stretton Sandstone and is shown to be unconformably underlying Smythe Sandstone.||
10647|Looking Glass Formation|72718|6|Mentioned|p7|||Southern McArthur Basin. Batten Fault Zone (north).||Batten Sub-group, McArthur Group||Underlain by Stretton Sandstone. Unconformably overlain [?] by Smythe Sandstone. Equivalent to Amos Formation. Partly equivalent to lower Balbirini Dolostone.||
10647|Looking Glass Formation|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Batten Fault Zone of the Southern McArthur Basin.||Batten Subgroup||Overlies Stretton Sandstone and unconformably underlies Nathan Group.||
10647|Looking Glass Formation|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin, Isa Superbasin.||Batten Subgroup, McArthur Group||Underlain by Stretton Sandstone. Unconformably overlain(?) by Smythe Sandstone.||
10647|Looking Glass Formation|73412|5|Briefly described|p4, 8|||Southern McArthur Basin.||Batten Subgroup.||Overlies Stretton Sandstone. Is overlain unconformably by Smythe Sandstone (Nathan Group).||
10668|Lothari Hill Sandstone|12891|5|Briefly described|p732, p733 Fig. 2|Late Cambrian|Middle Cambrian|Confusingly referred to as L.H.Fm and L.H.Sandstone - both probably misnomers! Overlies Hooker Creek Fm. Geol.prov: Wiso Basin.Fine-gr.silty quartz sst+rare siltstone; but in MT SOLITAIRE area, is mostly fine-gr. with claystone+rare sst beds outcropping.||||||07-FEB-11
10668|Lothari Hill Sandstone|31412|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
10668|Lothari Hill Sandstone|31413|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
10668|Lothari Hill Sandstone|31637|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
10668|Lothari Hill Sandstone|34810|5|Briefly described|p8|||Do not crop out in sheet area.||||||
10668|Lothari Hill Sandstone|35125|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
10668|Lothari Hill Sandstone|35224|4|Described|Table 1|||See also p5.||||||30-OCT-06
10668|Lothari Hill Sandstone|35227|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
10668|Lothari Hill Sandstone|35229|4|Described|Table.1|||||||||
10668|Lothari Hill Sandstone|35231|4|Described|Table.1|||||||||
10668|Lothari Hill Sandstone|36335|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|Middle Cambrian(Ordian).||||||
10668|Lothari Hill Sandstone|41204|6|Mentioned|p14|||||||||
10668|Lothari Hill Sandstone|42059|5|Briefly described|p130|||See also Fig.2||||||
10668|Lothari Hill Sandstone|45148|2|Defined|p14|Middle Cambrian|Middle Cambrian|Part of Winnecke Creek Tableland Formation.See p2.||||||30-OCT-06
10668|Lothari Hill Sandstone|45155|6|Mentioned|Fig.8|||||||||
10668|Lothari Hill Sandstone|60684|5|Briefly described|p49-50 Appendix, p14|Middle Cambrian|Middle Cambrian|Formerly included in Chewings' (1931) Winnecke Creek Tablelands formation and in Merrina Beds (Milligan et al 1966).||||||28-APR-05
10668|Lothari Hill Sandstone|62637|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Wiso Basin. Red-brown laminated claystone; white fine-grained angular sandstone.||||||23-DEC-09
10668|Lothari Hill Sandstone|64068|6|Mentioned|p225|||Wiso Basin. Correlated with Narpa Group.||||||
10668|Lothari Hill Sandstone|64443|6|Mentioned|p40.|||Of Wiso Basin. Correlative of Barkly Group, Georgina Basin.||||||
10668|Lothari Hill Sandstone|65239|5|Briefly described|p3 Fig. 4|Middle Cambrian|Middle Cambrian|Geological province: Wiso Basin. Deposits from a tidal environment.||||||04-JUN-09
10668|Lothari Hill Sandstone|65345|5|Briefly described|p4, p6 Fig.5.|Cambrian|Cambrian|Wiso Basin. Over 95 m thick. Tidal deposits.||||Overlies Hooker Creek Formation. Is unconformably overlain by Point Wakefield beds.||
10668|Lothari Hill Sandstone|69432|5|Briefly described|p17:2|Cambrian|Cambrian|Wiso Basin.||||Unconformably overlies Gardiner Sandstone.|Flat-lying chert and minor sandstone.|12-JUL-16
10668|Lothari Hill Sandstone|69437|5|Briefly described|p22:10-11|Series 2|Series 2|Wiso Basin, Centralian B Superbasin. Sequence 1. Peritidal deposits.||||Overlies Hooker Creek Formation. Is overlain by Point Wakefield beds.|Sandstone-dominated sediments.|12-JUL-16
10668|Lothari Hill Sandstone|69439|6|Mentioned|p24:10|||Wiso Basin. The interval Montejinni Limestone-Lothari Hill Sandstone is correlated with the Walbiri Dolostone of the Ngalia Basin.||||||12-JUL-16
10668|Lothari Hill Sandstone|69443|6|Mentioned|p28:21|||Wiso Basin.||||Correlated with Barkly Group.||12-JUL-16
10668|Lothari Hill Sandstone|69447|3|Fully described|p32:2-3, 5, 9|Middle Cambrian|Middle Cambrian|Wiso Basin. Intertidal to ?shoreface deposits. Up to 93.9m thick, in the type section in BMR Green Swamp Well-4. Best exposed as scarps surrounding low rises. Unfossiliferous. Poor to fair hydrocarbon reservoir potential; intraformational siltstone and claystone may provide seals.||||Gradationally overlies Hooker Creek Formation. Is overlain unconformably by Point Wakefield beds, Lake Surprise Sandstone, or Buchanan Hills beds.|Pale- to red-brown, fine quartz sandstone, locally micaceous or dolomitic; minor claystone, dolostone; dessication cracks, vertical ?burrows, minor low-angle cross-beds, symmetric ripples.|12-JUL-16
10668|Lothari Hill Sandstone|69673|5|Briefly described|p142, p143, p145|Cambrian|Cambrian|93.9m thick.|||||Locally dolomitic quartz sandstone and minor claystone, dolostone and chert.|
10668|Lothari Hill Sandstone|70380|6|Mentioned|p745|Stage 5|Stage 4|Wiso Basin.||||||
10668|Lothari Hill Sandstone|73083|6|Mentioned|p24|||||||||
10840|Lucas Formation|22446|6|Mentioned|p20|Mesozoic|Mesozoic|||||||
10840|Lucas Formation|29809|6|Mentioned|Table 1|||||||||
10840|Lucas Formation|29810|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
10840|Lucas Formation|29812|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
10840|Lucas Formation|29817|5|Briefly described|p7|||||||||
10840|Lucas Formation|29819|6|Mentioned|Map legend|Late Paleozoic|Late Paleozoic|||||||07-NOV-08
10840|Lucas Formation|31360|4|Described|Table 1|||||||||
10840|Lucas Formation|31362|4|Described|Table 1|||||||||
10840|Lucas Formation|35205|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
10840|Lucas Formation|36473|6|Mentioned|Map legend|Permian|Permian|||||||
10840|Lucas Formation|36532|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
10840|Lucas Formation|41883|6|Mentioned|p65|||||||||
10840|Lucas Formation|42504|5|Briefly described|Table 4 P73|||||||||
10840|Lucas Formation|43631|6|Mentioned|p27|||||||||
10840|Lucas Formation|45140|2|Defined|p13-14, p26, p40, p46, p49, p61-64, p68|Paleozoic|Paleozoic|See also p75, p83, Appx.p42-43. Hodgson (1976). Previously the Lucas Beds (Casey and Wells, 1964). Named after Lake Lucas. Flat or gently-dipping. Type section (described in some detail) is a low cliff at 20deg 53'30"S, 28deg 56'00"E in the Lucas sheet area. Casey and Wells (1964) chose the bed of Lake Dennis as the "nominate" exposure, but no rocks of the Formation are exposed as they are covered by salt and alluvium. Estimated 1000m thick. Unfossiliferous: probably lacustrine. Local calcrete and laterite cappings. Source of salty water from bores. Correlated with Pertnjara Group; suggested correlation with Noonkanbah Formation is dubious. Possibly Devonian.||||Inferred to overlie Muriel Range Sandstone and Erica Sandstone unconformably. Is overlain unconformably by Pedestal Beds.|Purplish to grey, medium- to fine-grained friable calcareous sandstone; medium- to coarse-grained non-calcareous sandstone (lithic to sublithic arenite); thin-bedded to laminated siltstone and mudstone; local thin limestone beds and sandy dolomite.|
10840|Lucas Formation|45155|6|Mentioned|p42|||||||||
10840|Lucas Formation|46864|4|Described|p38|||||||||
10840|Lucas Formation|50315|5|Briefly described|Map Legend|Devonian|Devonian|Calcareous and non-calcareous sandstone, siltstone and mudstone.  Age: <410Ma.||||||09-JUN-04
10840|Lucas Formation|50374|5|Briefly described|Map Legend|Devonian|Devonian|Calcareous and non-calcareous sandstone, siltstone and mudstone.||||||
10840|Lucas Formation|50376|5|Briefly described|Map Legend|Devonian|Devonian|Calcareous and non-calcareous sandstone, siltstone and mudstone; minor limestone.||||||19-APR-06
10840|Lucas Formation|60676|5|Briefly described|Map legend|Devonian|Devonian|Calcareous and non calcareous sandstone, siltstone and mudstone; minor limestone.||||||19-JAN-05
10840|Lucas Formation|61861|5|Briefly described|p4, Map 1|Devonian|Devonian|Flat-lying siliciclastic rocks.||||Overlies Antrim Plateau Volcanics.||03-APR-12
10840|Lucas Formation|62377|5|Briefly described|p15|||Overlies the Dead Bullock Formation.||||||
10840|Lucas Formation|62628|5|Briefly described|Map Legend|Paleozoic|Paleozoic|Geological Province: Canning Basin. Calcareous and non-calcareous sandstone, siltstone and mudstone; minor limestone.||||||07-NOV-08
10840|Lucas Formation|64580|4|Described|map legend||Paleozoic|Sandstone, in part calcareous, siltstone, mudstone; minor limestone and conglomerate.||||||09-DEC-08
10840|Lucas Formation|64675|6|Mentioned|p10, Map 1|||||||||19-MAR-14
10840|Lucas Formation|65074|4|Described|p350 fig 4-36, p351, p358-360, p362|Paleozoic|Paleozoic|See also p353, p359 fig 4-13, p360, p362. Of Birrindudu Basin. 1000 m thick. Non-fossiliferous; possibly Devonian. Type section is a cliff exposure along E shore of Lake Dennis, 20o54'S, 128o56'E.||||Overlain by Pedestal beds (unconformably). Overlies Redcliff Pound Group (unconformably). Probably correlates with Pertnjara Group.|Sandstone (calcareous or not), siltstone, mudstone; minor dolomite, limestone.|
10840|Lucas Formation|65324|6|Mentioned|Map legend|Devonian|Devonian|Not shown on map||||||
10840|Lucas Formation|65349|6|Mentioned|Map legend|Devonian|Devonian|Not shown on map||||||
10840|Lucas Formation|65350|6|Mentioned|Map legend|Devonian|Devonian|Not shown on map||||||
10840|Lucas Formation|65351|6|Mentioned|Map legend|Devonian|Devonian|Not shown on map||||||
10840|Lucas Formation|68656|5|Briefly described|GEOL_LUT_CSV/100k_interpgeop_lut|Paleozoic|Paleozoic|Canning Basin. See also 500k_geologyp08_lut.csv.|||||Sandstone (partly calcareous), siltstone, and mudstone; minor limestone and conglomerate.|
10840|Lucas Formation|69432|6|Mentioned|p17:2|||Canning Basin.||||Overlies Birrindudu Group.||12-JUL-16
10840|Lucas Formation|69440|5|Briefly described|p25:2|Devonian|Devonian|Canning Basin.||||Unconformably overlies Erica Sandstone.||12-JUL-16
10840|Lucas Formation|69453|5|Briefly described|p37:1|Devonian|Devonian|Lucas Outlier, Canning Basin. Deposition in a fluvio-lacustrine environment. Estimated thickness of 1000m. Age inferred from correlation with Pertnjara Group (Amadeus Basin).||||Unconformably overlies (inferred) Redcliff Pound Group. Is inferred to be overlain unconformably by Pedestal beds. (Inferred) correlative of Pertnjara Group.|Flat-lying to gently-dipping, medium- to fine-grained calcareous to non-calcareous sandstone, interbedded with siltstone and mudstone, which are locally calcareous. No marine fossils.|12-JUL-16
10840|Lucas Formation|69587|4|Described|GEOL_LUT_CSV files|Paleozoic|Paleozoic|Of Canning Basin. Events: Alice Springs Orogeny. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|541-252.17 Ma (inferred)||||Sandstone (partly calcareous), siltstone, and mudstone; minor limestone and conglomerate|
10840|Lucas Formation|69673|5|Briefly described|p200|||Approximately 1000m thick.|||||Medium to fine grained calcareous to non-calcareous sandstone interbedded with siltstone and mudstone, which are locally calcareous.|
10840|Lucas Formation|70130|5|Briefly described|Map legend|Paleozoic|Paleozoic|Canning Basin.|||||Sandstone (partly calcareous), siltstone and mudstone; minor limestone and conglomerate.|
10840|Lucas Formation|70826|6|Mentioned|p6 tbl 3, p11|Paleozoic|Paleozoic|eastern Canning Basin.||||||20-MAY-20
10840|Lucas Formation|70852|5|Briefly described|Map legend.|Paleozoic|Paleozoic|Canning Basin.|||||Calcareous and non-calcareous sandstone, siltstone and mudstone; minor limestone.|
10840|Lucas Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, sandstone|
10840|Lucas Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleozoic|Paleozoic|Canning Basin. Age inferred.|||||Sandstone (partly calcareous), siltstone, and mudstone; minor limestone and conglomerate|
10840|Lucas Formation|73445|5|Briefly described|p3, 6, 8, 10, 24, 35, 37-38, 41-43|Paleozoic|Paleozoic|See also p65-118. Canning Basin. Regolith chemistry tabulated. Bedrock appears to control regolith chemistry in this unit.|||||Thin-bedded calcareous sandstone, siltstone, mudstone, minor limestone and conglomerate.|
10891|Lynott Formation|22453|6|Mentioned|p 12|||McArthur Basin||||||
10891|Lynott Formation|22538|6|Mentioned|P717|||||||||
10891|Lynott Formation|22664|6|Mentioned|33-35,37,39,40 fig 5|Paleoproterozoic|Paleoproterozoic|Batten Subgroup, McArthur Basin. Also on pages 42,46-48||||||07-NOV-08
10891|Lynott Formation|22853|5|Briefly described|22|Proterozoic|Proterozoic|Of the Batten Subgroup.||||||30-OCT-06
10891|Lynott Formation|23387|6|Mentioned|p18 fig.19|||Of Batten Subgroup.||||||
10891|Lynott Formation|23396|4|Described|p413|Statherian|Statherian|Of McArthur Group. Age: 1636+/-4Ma.||||||30-OCT-06
10891|Lynott Formation|23397|5|Briefly described|p473|||||||||
10891|Lynott Formation|23398|4|Described|p443|Statherian|Statherian|U/Pb SHRIMP depostional age: 1636+/-4Ma.Tuffaceous mudstone in Hot Springs Member was dated. this is in ~ the middle of the Formation.||||||09-SEP-14
10891|Lynott Formation|23409|5|Briefly described|p533|||Of McArthur Group.||||||30-OCT-06
10891|Lynott Formation|23776|5|Briefly described|p705 Fig 2.|Statherian|Statherian|AGe: 1636+/-4 Ma. Of Batten Subgroup.||||||30-OCT-06
10891|Lynott Formation|23902|4|Described|p1568 Fig.2|||Of the Batten Subgroup. Overlain by the Yalco Formation. Geological Province: McArthur Basin||||||
10891|Lynott Formation|23910|5|Briefly described|p292 Fig. 2|||Of Batten Subgroup.  Geological Province: McArthur Basin.||||||30-OCT-06
10891|Lynott Formation|23937|4|Described|p9, p25 Tb. 2|Statherian|Statherian|Of the Batten Subgroup (McArthur Group).  Overlain by Yalco Formation.  Age: 1636Ma.  Geological Province: McArthur Basin.||||||30-OCT-06
10891|Lynott Formation|23963|5|Briefly described|p1239 Fig.2|||Geological Province: McArthur Basin. Of the Batten Subgroup.||||||30-OCT-06
10891|Lynott Formation|24048|6|Mentioned|p57|||Of the Batten Subgroup.||||||30-OCT-06
10891|Lynott Formation|24179|5|Briefly described|p83, p84 Fig. 2|Paleoproterozoic|Paleoproterozoic|Age: 1636 +/- 4 Ma.  Overlies the Reward Formation.  Overlain by the Yalco Formation.  Geological Province:  McArthur Basin.||||||07-NOV-08
10891|Lynott Formation|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Of Battten Subgroup. Overlain by Yalco Formation. Carbonate. Geological Province: Southern McArthur Basin.||||||
10891|Lynott Formation|30344|6|Mentioned|Fig.4|||Part of Batten Subgroup||||||
10891|Lynott Formation|32658|3|Fully described|Table 2|||See also Fig. 3||||||
10891|Lynott Formation|32660|5|Briefly described|Table 4|||||||||
10891|Lynott Formation|33665|6|Mentioned|Fig.2|||||||||
10891|Lynott Formation|33666|6|Mentioned|p528|||Table 1||||||
10891|Lynott Formation|35261|6|Mentioned|Fig.2|||||||||
10891|Lynott Formation|37568|4|Described|p79|||||||||
10891|Lynott Formation|38042|6|Mentioned|p167|||||||||
10891|Lynott Formation|38143|6|Mentioned|p21|||||||||
10891|Lynott Formation|38582|4|Described|p226|||||||||
10891|Lynott Formation|39561|6|Mentioned|Fig.5|||||||||
10891|Lynott Formation|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
10891|Lynott Formation|40259|6|Mentioned|Table 1|||||||||
10891|Lynott Formation|40691|5|Briefly described|p12|||||||||
10891|Lynott Formation|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
10891|Lynott Formation|41220|6|Mentioned|p367|||||||||
10891|Lynott Formation|41268|6|Mentioned|p295|||||||||
10891|Lynott Formation|41277|6|Mentioned|Fig.2|||||||||
10891|Lynott Formation|42385|5|Briefly described|p22|||See also Table 4 p16.||||||30-OCT-06
10891|Lynott Formation|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
10891|Lynott Formation|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.||Of Batten Subgroup (McArthur Group).|Donnegan Member over Hot Spring Member over Caranbirini Member.|In schematic section, Donnegan Member underlies Yalco Formation; Caranbirini Member overlies combined Teena Dolomite, Barney Creek Formation and Reward Dolomite.||11-NOV-11
10891|Lynott Formation|42639|4|Described|p31, Table 5 p20|||||||||
10891|Lynott Formation|42700|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
10891|Lynott Formation|42739|5|Briefly described|map legend|Statherian|Statherian|Of the Batten Subgroup.||||||19-OCT-05
10891|Lynott Formation|42812|3|Fully described|p40, Table 4|||Of Batten Subgroup.||||||30-OCT-06
10891|Lynott Formation|42846|5|Briefly described|Fig.1 p502|||Of McArthur Group. Geological Province: McArthur Basin.||||||09-MAY-05
10891|Lynott Formation|42935|6|Mentioned|p529 Fig.2|||of Batten Subgroup||||||
10891|Lynott Formation|43010|5|Briefly described|Fig.6||Mesoproterozoic|of "Mid Proterozoic" age.||||||
10891|Lynott Formation|43036|4|Described|p53|||Of Batten Subgroup.||||||30-OCT-06
10891|Lynott Formation|44287|14|Not recorded|p.6,9-11, opp.9|||Fore-reef seds. (E53-3).||||||
10891|Lynott Formation|44288|14|Not recorded|map legend|||Siltstone, sandstone, dolomite chert, chert-breccia, dolomite-breccia. Lower (?) Proterozoic.||||||
10891|Lynott Formation|44434|14|Not recorded|p.7, opp. p.6, map|||Basal fm of Batten Subgroup (McArthur Group). (D53-11,12).||||||
10891|Lynott Formation|44435|14|Not recorded|map legend|||Lower (?) Proterzoic.||||||
10891|Lynott Formation|44530|14|Not recorded|p.10, opp.10|||(D53-15).||||||
10891|Lynott Formation|44531|14|Not recorded|map legend|||Lower (?) Proterozoic.||||||
10891|Lynott Formation|45162|2|Defined|p108-120|Proterozoic|Proterozoic|||||||06-APR-18
10891|Lynott Formation|46915|6|Mentioned|Fig.1|||Stratigraphic section through McArthur Group.||||||
10891|Lynott Formation|46968|6|Mentioned|Fig.2|||||||||
10891|Lynott Formation|47008|6|Mentioned|p330|||||||||
10891|Lynott Formation|60483|5|Briefly described|p7 Fig. 5, p8|||Of Batten Subgroup (McArthur Group). Contains the Caranbirini, Hot Spring and Donnegan Members. Geological Province: McArthur Basin.||||||05-OCT-07
10891|Lynott Formation|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Batten Subgroup. Includes Donnegan, Hot Spring and Caranbirini Members. Overlian by Yalco Formation, underlain by Umbolooga Subgroup.||||||
10891|Lynott Formation|60573|5|Briefly described|Map legend|Statherian|Statherian|Of the McArthur Group. Silicified siltstone and dolomitic siltstone; laminated to thinly bedded, brown to grey, small-scale bedding convolution.||||||
10891|Lynott Formation|61390|5|Briefly described|Map Legend|Statherian|Statherian|Of the McArthur Group. Silicified siltstone and dolomitic siltstone.||||||
10891|Lynott Formation|62084|6|Mentioned|p936 Fig.5|||Isa Superbasin. McArthur Basin. Shown as Lynott Fm.||McArthur Group|||Platform carbonates.|
10891|Lynott Formation|63112|6|Mentioned|p1191 Fig.2|||Isa Superbasin; southern McArthur Basin. Age approximated from Fig.2.|c.1635-1630 Ma.|Unit in River Supersequence.||||
10891|Lynott Formation|63866|5|Briefly described|p54|Statherian|Statherian|Isa Superbasin.|1636 +/- 4 Ma (Page et al., 2000)|River Supersequence||||
10891|Lynott Formation|64726|6|Mentioned|p86 Table 1.|||Sampled for paleomagnetic reconstruction of Australian and Laurentian Apparent Polar Wander Path.|1636 +/- 4 Ma.|||||
10891|Lynott Formation|64815|6|Mentioned|p4 Fig.2, p5 Fig.3|||||Of the Batten Subgroup.|Includes Caranbirini, Hot Spring, Donnegan Members.|||
10891|Lynott Formation|64816|6|Mentioned|p2 Fig.1 |||||Unit in McArthur Group.||||
10891|Lynott Formation|64817|6|Mentioned|p353 Fig.4 |Statherian|Statherian||1636 +/- 4 Ma.|Of the Batten Subgroup.|Includes the Donnegan Member, Hot Spring Member and Caranbirini Member.|||
10891|Lynott Formation|65228|4|Described|p32, p33, p35, Table 1, Figs.02,04,22. |Statherian|Statherian|Part of River Supersequence.|1636 +/- 4 Ma.|Unit in Batten Subgroup.|Includes Caranbirini, Hot Spring, Donnegan Members.|Unconformably overlies Reward Dolomite. Is overlain by Yalco Formation.||
10891|Lynott Formation|66843|6|Mentioned|p38 Fig.10|||Shown only as Lynott.||||||12-SEP-19
10891|Lynott Formation|69018|5|Briefly described|p450 Fig.1b|Statherian|Statherian|Of McArthur Basin.|1636+/-3 Ma.|Of McArthur Group.||||
10891|Lynott Formation|69418|6|Mentioned|p3:36|||McArthur Basin. Good potential hydrocarbon source rocks.||||||12-JUL-16
10891|Lynott Formation|69430|4|Described|p15:3,14, 16,19, 22-23, 30, 34,40-41,61|Statherian|Statherian|Southern McArthur Basin. 50-600m thick. Correlated with Nagi Formation and part of Zamia Creek Siltstone. Potential hydrocarbon source rock.|1636 +/- 4 Ma.|Batten Subgroup.|Caranbirini, Hot Spring, Donnegan Members.|Overlies the Reward Dolostone possibly unconformably. Is overlain conformably by Yalco Formation.|An evaporite-rich unit of mainly dolomitic siltstone, dolarenite, stromatolitic dolostone and lesser dolomitic sandstone.|12-JUL-16
10891|Lynott Formation|69673|4|Described|p24, p27, p34, p40, p42, p44, p47|||Batten Fault Zone. Potential source rock. Thickness ranges from 50-600m .|1636 +/- 4 Ma|Batten Subgroup|Includes Hot Spring Member, Donnegan Member, Caranbirini Member|Unconformably overlies Reward Dolostone, conformably overlain by Yalco Formation|Evaporite rich unit of mainly dolomitic siltstone, sandy dolostone, stromatolitic dolostone and lesser dolomitic sandstone.|
10891|Lynott Formation|71374|6|Mentioned|p9|||McArthur Basin.|||Includes the Donnegan Member and Hot Spring Member.|Conformably overlain by  Yalco Formation.||04-MAY-18
10891|Lynott Formation|71592|5|Briefly described|Appendix A.|||McArthur Basin.|1636+/-4 Ma (MDA: U-Pb zircon SHRIMP)||||Includes a 2 cm-thick pink tuff layer and a silt layer below the pink tuff.|
10891|Lynott Formation|71606|5|Briefly described|p138|Statherian|Statherian|Batten Trough, McArthur Basin.||Unit of Batten Subgroup.||Underlain by Umbolooga Subgroup.||
10891|Lynott Formation|72248|5|Briefly described|p147|||Of McArthur Basin.||Unit of Batten Subgroup.|Includes Donnegan and Hot Spring members [and Caranbirini Mmeber?] .|||13-SEP-19
10891|Lynott Formation|72373|5|Briefly described|p17|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. Dated at 1636+\-4 Ma; partially overlaps in age with Baiguridji Formation (Ahmad et al 2013).||Unit of upper McArthur Group.||||02-OCT-19
10891|Lynott Formation|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Batten Fault Zone of the Southern McArthur Basin. Age given as U-Pb zircon sedimentary depositional age.|1636 +/-4 Ma|Batten Subgroup|Includes Hot Springs Member.|Unconformably overlies Reward Dolostone and underlies Yalco Formation.||
10891|Lynott Formation|72718|6|Mentioned|p7|||Southern McArthur Basin. Batten Fault Zone. [May include the Caranbirini Member but this is not clear in Fig.6]||Batten Sub-group, McArthur Group|Donnegan Member, Hot Spring Member, Caranbirini Member|Partly underlain by Caranbirini Member[?]. Partly underlain by Reward Dolostone (Umbolooga Sub-group) unconformably[?]. Overlain by Yalco Formation.||
10891|Lynott Formation|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Batten Fault Zone of the Southern McArthur Basin. U-Pb zircon sedimentary depositional age (Ma).|1636 +/- 4 Ma|Batten Subgroup|Includes Hot Springs Member.|Unconformably overlies Reward Dolostone and underlies Yalco Formation.||
10891|Lynott Formation|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin, Isa Superbasin.||Batten Subgroup, McArthur Group|Hot Springs Member|Unconformably underlain by Reward Dolostone. Overlain by Yalco Formation.||
10891|Lynott 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].|||Caranbirini Member, Hot Springs Member|||
10891|Lynott Formation|73412|5|Briefly described|p4, 8, 12, 19|||Southern McArthur Basin.||Batten Subgroup.|Hot Spring, Caranbirini Members.|Unconformably overlies Reward Dolostone. Is overlain by Yalco Formation.||
10952|Mackunda Formation|12597|5|Briefly described|p492 Tb.1, p500|Cenomanian|Cenomanian|Eromanga Basin. 60m thick.|||||Marginal marine sequence; labile sandstone, siltstone and mudstone, calcareous in part, containing bivalves, ammonites, belemnites, polyzoans and sharks' teeth.|
10952|Mackunda Formation|13497|5|Briefly described|p115 fig 6.33, p146, p149-p154, |Early Cretaceous|Early Cretaceous|Eromanga Basin. Mis-spelt as the Macunda Formation on p146.||Marree Subgroup||Overlies the Allaru Mudstone and the Oodnadatta Formation. Overlain by the Winton Formation.||
10952|Mackunda Formation|13516|6|Mentioned|p167 fig 10, p169 fig 11, p171 fig 12|Late Cretaceous|Late Cretaceous|In Eromanga Basin.||||||
10952|Mackunda Formation|22857|5|Briefly described|p296-7 Tb.22.1|Cenomanian|Albian|Of the Rolling Downs Group. Geological Province: Eromanga Basin.||||||
10952|Mackunda Formation|22865|5|Briefly described|Table22.1p296-7|Cenomanian|Albian|||||||
10952|Mackunda Formation|22883|5|Briefly described|Fig2 P30||Late Cretaceous|Overlying unit is Winton Formation, underlying unit is Allura Mudstone||||||
10952|Mackunda Formation|22912|5|Briefly described|33|||Geol province Eromanga Basin||||||
10952|Mackunda Formation|23056|6|Mentioned|12 table 2|||||||||
10952|Mackunda Formation|23154|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Geological Province - Eromanga Basin. Of the Neales River Group.||||||20-FEB-07
10952|Mackunda Formation|23155|4|Described|p33|Early Cretaceous|Early Cretaceous|Determination of the spore-pollen assemblage indicate an Early Cretaceous (Albian) age. The unit conformably overlies both the Allaru Mudstone and Oodnadatta Formation on STRZELECKI.||||||11-NOV-13
10952|Mackunda Formation|23183|6|Mentioned|p223||Albian|||||||
10952|Mackunda Formation|23188|6|Mentioned|p283,287||Albian|||||||
10952|Mackunda Formation|23375|4|Described|Fig2 p265|Cenomanian|Albian|In the Eromanga Basin.||||||31-OCT-06
10952|Mackunda Formation|23425|5|Briefly described|Plate 10.2|||In the Eromanga Basin Province.||||||20-FEB-07
10952|Mackunda Formation|23430|4|Described|p524 Table 14.7|||Eromanga Basin Province. Maximum thickness <275 m.||||||
10952|Mackunda Formation|23818|6|Mentioned|p141 Fig.65|||Geological Province: Great Artesian Basin. Of the Manuka Sub-Group.||||||
10952|Mackunda Formation|23883|5|Briefly described|p129 Fig. 11.2|Cretaceous|Cretaceous|Of Rolling Downs Group. Geological Province: Great Australian Superbasin.||||||
10952|Mackunda Formation|23911|5|Briefly described|p97 Fig. 11|Cretaceous|Cretaceous|Geological Province: Eromanga Basin.  Of the Rolling Downs Group.||||||
10952|Mackunda Formation|23982|5|Briefly described|p35 Fig.7|Cretaceous|Cretaceous|Of Rolling Downs Group. Geological Province: Great Artesian Basin.||||||
10952|Mackunda Formation|24092|5|Briefly described|p5|Cretaceous|Cretaceous|Geological Province: Great Artesian Basin.||||||
10952|Mackunda Formation|24175|3|Fully described|p28, p17 Fig. 3|Cenomanian|Albian|Overlain by Winton Formation; overlies Allaru Mudstone. Max. thickness: 57m. Geological Province: Eromanga Basin.||||||11-NOV-13
10952|Mackunda Formation|24204|5|Briefly described|p263 Fig.4, p267|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||
10952|Mackunda Formation|24210|5|Briefly described|p133 Fig. 2|Late Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||
10952|Mackunda Formation|24251|5|Briefly described|p234 Fig.1, p245|Albian|Albian|Underlain by Allaru Formation. Geological Province: Eromanga Basin||||||20-FEB-07
10952|Mackunda Formation|24321|5|Briefly described|Map legend|Cenomanian|Albian|Of the Neales River Group.||||||31-OCT-06
10952|Mackunda Formation|29591|6|Mentioned|p71|||||||||
10952|Mackunda Formation|30019|6|Mentioned|p2|||Upper Albian||||||
10952|Mackunda Formation|30020|6|Mentioned|p35|||||||||
10952|Mackunda Formation|30103|5|Briefly described|p9|||Unit of Rolling Downs Group. Table 3 on p9.||||||31-OCT-06
10952|Mackunda Formation|30104|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|30691|4|Described|p17|||See also p22,Table 4,6. Lower-Upper Cretaceous.||||||31-OCT-06
10952|Mackunda Formation|30804|6|Mentioned|p10|||||||||
10952|Mackunda Formation|30853|5|Briefly described|Table 3|||Albian age||||||
10952|Mackunda Formation|30854|4|Described|Table 4|||Albian||||||
10952|Mackunda Formation|30855|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|Rolling Downs Group||||||
10952|Mackunda Formation|30856|6|Mentioned|p10|||||||||
10952|Mackunda Formation|31098|6|Mentioned|p10|||||||||
10952|Mackunda Formation|31144|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|31145|5|Briefly described|Table 1|||Lower Cretaceous||||||
10952|Mackunda Formation|31208|6|Mentioned|Fig. 7|||||||||
10952|Mackunda Formation|31425|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|31430|5|Briefly described|Table 1|||L.Cretaceous||||||
10952|Mackunda Formation|31431|5|Briefly described|Table 3|||Lower Cretaceous.||||||
10952|Mackunda Formation|31432|4|Described|Table 1|||L.Cretaceous||||||
10952|Mackunda Formation|31434|6|Mentioned|p8|||||||||
10952|Mackunda Formation|31436|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|31438|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|31441|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|31553|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|31572|4|Described|Fig. 1|||L.Cretaceous||||||
10952|Mackunda Formation|32277|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower Cretaceous - Upper Cretaceous.||||||
10952|Mackunda Formation|32314|6|Mentioned|Fig. 4|||||||||
10952|Mackunda Formation|32395|6|Mentioned|p7|||Correlation||||||
10952|Mackunda Formation|32396|6|Mentioned|p9|||Correlated with Normanton Fm.||||||
10952|Mackunda Formation|32553|4|Described|p38|||||||||
10952|Mackunda Formation|32796|6|Mentioned|p303|||||||||
10952|Mackunda Formation|33016|6|Mentioned|p1|||Table on P1||||||
10952|Mackunda Formation|33067|4|Described|Table 1|Early Cretaceous|Early Cretaceous|Of the Rolling Downs Group.||||||07-JUL-04
10952|Mackunda Formation|33069|4|Described|p7|||L.-U.Cret.||||||
10952|Mackunda Formation|33073|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|33075|6|Mentioned|Table 1|||||||||
10952|Mackunda Formation|33078|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|33079|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|33082|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|33083|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|33086|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower to Upper Cretaceous||||||
10952|Mackunda Formation|33087|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|33088|4|Described|Table 3|||Of the Rolling Downs Group.||||||20-FEB-07
10952|Mackunda Formation|33089|4|Described|Table 2|||L.Cret.||||||
10952|Mackunda Formation|33165|6|Mentioned|Chart|||Correlation chart only||||||
10952|Mackunda Formation|33176|6|Mentioned|p171|||||||||
10952|Mackunda Formation|33182|6|Mentioned|p200|||L.Cret. See also Table 1||||||
10952|Mackunda Formation|33368|6|Mentioned|p25|||Strat.table.||||||
10952|Mackunda Formation|33372|6|Mentioned|Table 1|||||||||
10952|Mackunda Formation|33414|6|Mentioned|p211|||||||||
10952|Mackunda Formation|33561|6|Mentioned|p102|||||||||
10952|Mackunda Formation|33638|5|Briefly described|Table 1|||||||||
10952|Mackunda Formation|33639|5|Briefly described|Table 2|||L.Cret.||||||
10952|Mackunda Formation|33640|4|Described|Table 2|||L.Cret.||||||
10952|Mackunda Formation|33642|6|Mentioned|p144-5,147-8,Tb.1,|||Refers Vine & Day (1965). Figs. 1 & 2.||||||
10952|Mackunda Formation|33643|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|33647|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|33648|6|Mentioned|p19|||Stratigraphy.||||||
10952|Mackunda Formation|33825|6|Mentioned|p10|||Correlation table||||||
10952|Mackunda Formation|33832|5|Briefly described|p11|||Stratigraphy and correlation.||||||31-OCT-06
10952|Mackunda Formation|33964|4|Described|p6|||||||||
10952|Mackunda Formation|34065|4|Described|p6|||L.Cret.||||||
10952|Mackunda Formation|34091|5|Briefly described|Table 1|||L.Cret||||||
10952|Mackunda Formation|34174|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
10952|Mackunda Formation|34217|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|34218|4|Described|Table 1|||Lower Cretaceous. See also Table 2.||||||
10952|Mackunda Formation|34356|6|Mentioned|p21|||Albian.||||||
10952|Mackunda Formation|34485|4|Described|Table 1|||Lower - Upper Cretaceous||||||
10952|Mackunda Formation|34486|4|Described|Table 1|||Lower - Upper Cretaceous||||||
10952|Mackunda Formation|34487|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|34611|6|Mentioned|Fig.65|||Correlation chart||||||
10952|Mackunda Formation|34619|3|Fully described|p.160. Pl.22||Adelaidean|||||||
10952|Mackunda Formation|35139|4|Described|Table.2|||||||||
10952|Mackunda Formation|35239|6|Mentioned|Fig.4|||||||||
10952|Mackunda Formation|35560|6|Mentioned|Fig.3|||||||||
10952|Mackunda Formation|35793|6|Mentioned|Fig.3|||||||||
10952|Mackunda Formation|35811|5|Briefly described|Table 3|||||||||
10952|Mackunda Formation|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
10952|Mackunda Formation|36229|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
10952|Mackunda Formation|36243|6|Mentioned|Table 6A|||||||||
10952|Mackunda Formation|36552|6|Mentioned|Fig.25|||||||||
10952|Mackunda Formation|36571|6|Mentioned|p101|||See also Table 4.||||||
10952|Mackunda Formation|37263|6|Mentioned|p319|||||||||
10952|Mackunda Formation|37451|6|Mentioned|Table 2|||||||||
10952|Mackunda Formation|37608|3|Fully described|Table 1|||||||||
10952|Mackunda Formation|38226|6|Mentioned|Table 1|||||||||
10952|Mackunda Formation|38373|6|Mentioned|p621|||||||||
10952|Mackunda Formation|38779|6|Mentioned|p4|||||||||
10952|Mackunda Formation|38814|6|Mentioned|Table 1|||||||||
10952|Mackunda Formation|39070|4|Described|p366|||||||||
10952|Mackunda Formation|39211|5|Briefly described|Fig.3|||See also Figs 4,7,11,13 etc. Correlation||||||
10952|Mackunda Formation|39445|5|Briefly described|Table 11|||||||||
10952|Mackunda Formation|39478|6|Mentioned|Table 1|||||||||
10952|Mackunda Formation|39846|6|Mentioned|Fig.2|||||||||
10952|Mackunda Formation|39847|5|Briefly described|p40|||||||||
10952|Mackunda Formation|39943|6|Mentioned|Table 8A|||||||||
10952|Mackunda Formation|40121|6|Mentioned|Table 1|||||||||
10952|Mackunda Formation|40199|6|Mentioned|Fig.2|||||||||
10952|Mackunda Formation|40220|6|Mentioned|Fig.2|||||||||
10952|Mackunda Formation|40249|6|Mentioned|p41|||||||||
10952|Mackunda Formation|40675|6|Mentioned|Table 8A|||||||||
10952|Mackunda Formation|40681|6|Mentioned|Fig.2|||||||||
10952|Mackunda Formation|40687|3|Fully described|p419|||||||||
10952|Mackunda Formation|40801|6|Mentioned|p42|||||||||
10952|Mackunda Formation|40910|6|Mentioned|p17|||||||||
10952|Mackunda Formation|40926|6|Mentioned|p19|||||||||
10952|Mackunda Formation|41060|6|Mentioned|p2|||Generalized stratigraphy||||||
10952|Mackunda Formation|41062|6|Mentioned|Fig.5|||||||||
10952|Mackunda Formation|41063|6|Mentioned|p40|||||||||
10952|Mackunda Formation|41064|6|Mentioned|p62|||||||||
10952|Mackunda Formation|41084|5|Briefly described|Fig.2|||||||||
10952|Mackunda Formation|41085|6|Mentioned|p89|||||||||
10952|Mackunda Formation|41086|3|Fully described|p98, Fig.3|||||||||
10952|Mackunda Formation|41088|6|Mentioned|Fig.2|||||||||
10952|Mackunda Formation|41097|6|Mentioned|Table 1|||||||||
10952|Mackunda Formation|41099|6|Mentioned|Fig.9|||||||||
10952|Mackunda Formation|41165|5|Briefly described|p363|||Mention Fig.15||||||
10952|Mackunda Formation|41176|6|Mentioned|Table 2|||||||||
10952|Mackunda Formation|41177|6|Mentioned|Fig.2|||||||||
10952|Mackunda Formation|41182|5|Briefly described|Fig.2|||||||||
10952|Mackunda Formation|41183|6|Mentioned|Fig.3 p308|||||||||
10952|Mackunda Formation|41187|6|Mentioned|Fig.2|||||||||
10952|Mackunda Formation|41198|6|Mentioned|Table 1|||||||||
10952|Mackunda Formation|41214|6|Mentioned|Fig.3|||||||||
10952|Mackunda Formation|41216|6|Mentioned|Fig.18|||||||||
10952|Mackunda Formation|41266|6|Mentioned|Fig.3|||||||||
10952|Mackunda Formation|41523|3|Fully described|p282|||See also p277.||||||31-OCT-06
10952|Mackunda Formation|41707|6|Mentioned|Fig.8|||||||||
10952|Mackunda Formation|41724|6|Mentioned|p383|||||||||
10952|Mackunda Formation|41950|5|Briefly described|Fig.2 P3|||||||||
10952|Mackunda Formation|42061|4|Described|Fig,11 P159|||||||||
10952|Mackunda Formation|42067|4|Described|Appendix 2|||See also Fig.2 p309.||||||31-OCT-06
10952|Mackunda Formation|42071|6|Mentioned|p117|||||||||
10952|Mackunda Formation|42084|6|Mentioned|Fig.3 P356|||||||||
10952|Mackunda Formation|42085|6|Mentioned|Fig.2 P374|||||||||
10952|Mackunda Formation|42395|5|Briefly described|Fig.13 P83|||||||||
10952|Mackunda Formation|42397|6|Mentioned|Fig.2 P3|||||||||
10952|Mackunda Formation|42429|6|Mentioned|Figs.6 & 9 P156|||||||||
10952|Mackunda Formation|42446|4|Described|p14|||||||||
10952|Mackunda Formation|42447|6|Mentioned|Fig. 1|||||||||
10952|Mackunda Formation|42477|5|Briefly described|p166|||||||||
10952|Mackunda Formation|42496|5|Briefly described|p136, Fig.3 p132|||||||||
10952|Mackunda Formation|42520|5|Briefly described|p6|||||||||
10952|Mackunda Formation|42673|5|Briefly described|Fig.2, P184|||||||||
10952|Mackunda Formation|42746|5|Briefly described|p12|||See also Fig.6||||||
10952|Mackunda Formation|42749|6|Mentioned|Fig.2 P27|||||||||
10952|Mackunda Formation|42999|5|Briefly described|Table 2,p90||Late Cretaceous|||||||
10952|Mackunda Formation|43002|5|Briefly described|Fig.2,p135|||||||||
10952|Mackunda Formation|43004|5|Briefly described|Table 1,p179|||||||||
10952|Mackunda Formation|43053|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marginal marine sandstone and siltstone. Includes Mount Howie Sandstone.||||||25-MAY-05
10952|Mackunda Formation|43105|6|Mentioned|p15|||||||||
10952|Mackunda Formation|43114|5|Briefly described|p16|||||||||
10952|Mackunda Formation|43122|5|Briefly described|Fig.2.|||||||||
10952|Mackunda Formation|43258|5|Briefly described|Map Legend||Cretaceous|||||||
10952|Mackunda Formation|43298|5|Briefly described|Map Legend||Cretaceous|||||||
10952|Mackunda Formation|43591|6|Mentioned|p40|||||||||
10952|Mackunda Formation|43628|6|Mentioned|Fig.3|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|44016|14|Not recorded|Map Legend||Early Cretaceous|||||||
10952|Mackunda Formation|44017|14|Not recorded|Map Legend|||||||||
10952|Mackunda Formation|44018|14|Not recorded|Map Legend||Early Cretaceous|||||||
10952|Mackunda Formation|44019|14|Not recorded|Map Legend||Early Cretaceous|||||||
10952|Mackunda Formation|44020|14|Not recorded|p10,Tb.1,2||Early Cretaceous|Of roling Dwons Grouop.||||||
10952|Mackunda Formation|44031|14|Not recorded|p3,5,8,9||Cretaceous|||||||
10952|Mackunda Formation|44033|14|Not recorded|map,p4,5,8,9||Cretaceous|||||||
10952|Mackunda Formation|44034|4|Described|Tb.1,p2,4-6,9,10|||||||||
10952|Mackunda Formation|44042|14|Not recorded|Map Legend||Early Cretaceous|||||||
10952|Mackunda Formation|44067|14|Not recorded|Map Legend||Early Cretaceous|||||||
10952|Mackunda Formation|44082|6|Mentioned|p6,12,26,28,Tb.p34||Albian|Mentioned with respect to Qld Cretaceous fossils which are either of stratigraphic significance or are illustrative of the occurrence of a particular group.||||||
10952|Mackunda Formation|44089|4|Described|Tb.1,p3,4,8,9,map||Early Cretaceous|||||||
10952|Mackunda Formation|44091|14|Not recorded|p60|||||||||
10952|Mackunda Formation|44133|4|Described|p122-123, 104 Fig. 9.11|Early Cenomanian|Late Albian|Geological Province: Eromanga Basin. Conformably overlies Oodnadatta Formation and Allaru Mudstone. Contains sediments from the now superseded Mount Alexander Sandstone Member and Blanchewater Formation.||||||
10952|Mackunda Formation|44361|14|Not recorded|Map Legend||Early Cretaceous|||||||
10952|Mackunda Formation|44362|4|Described|p12,Tb.1||Early Cretaceous|||||||
10952|Mackunda Formation|44374|14|Not recorded|p12||Cretaceous|early Late Albian sandstone,siltstone indicating shoaling of seas throughout Eromanga Basin.||||||
10952|Mackunda Formation|44376|14|Not recorded|p6|||||||||
10952|Mackunda Formation|44410|14|Not recorded|Map Legend||Early Cretaceous|||||||
10952|Mackunda Formation|44414|14|Not recorded|p110-112|||Sandstone, mudstone characterised by marine fossils overlain by Winton Formation.||||||
10952|Mackunda Formation|44417|2|Defined|p416,419-420|||Formerly called Mackunda Beds. Overlies Wilgunya Formation. Albian fossils. Unit of Rolling Downs Group.||||||31-OCT-06
10952|Mackunda Formation|44418|14|Not recorded|Map Legend||Early Cretaceous|||||||
10952|Mackunda Formation|44573|14|Not recorded|p98||Cretaceous|||||||
10952|Mackunda Formation|44807|14|Not recorded|unknown (p1-16)|||Allaru Mudstone, correlated with Normanton Formation.||||||
10952|Mackunda Formation|44915|14|Not recorded|p18|||Ref. to Vine and Day 1965. Comparable to lower part of Blanchewater Formation in South Australia.||||||
10952|Mackunda Formation|44920|14|Not recorded|Map Legend,Sheet 4||Cretaceous|||||||
10952|Mackunda Formation|45052|5|Briefly described|p134|||Mesozoic||||||
10952|Mackunda Formation|45103|6|Mentioned|p8|||||||||
10952|Mackunda Formation|45110|6|Mentioned|p147|||See also Table 18.||||||
10952|Mackunda Formation|45168|6|Mentioned|p6|||||||||
10952|Mackunda Formation|46791|5|Briefly described|p48|||||||||
10952|Mackunda Formation|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
10952|Mackunda Formation|48920|3|Fully described|p62|||||||||
10952|Mackunda Formation|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
10952|Mackunda Formation|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
10952|Mackunda Formation|50100|5|Briefly described|p23|Cretaceous|Cretaceous|Of the Rolling Downs Group.  Geological Province: Eromanga Basin.||||||
10952|Mackunda Formation|60331|5|Briefly described|p34 Fig.3|Albian|Albian|Overlies Allaru Mudstone. Overlain by Winton Formation. Geological Province: Eromanga Basin.||||||
10952|Mackunda Formation|60717|5|Briefly described|p40 Fig. 2|Early Cretaceous|Early Cretaceous|Overlies Allaru Mudstone and Oodnadatta Formation, with which it also interfingers laterally. Overlain by Winton Formation. Geological Province: Eromanga Basin.||||||31-JAN-08
10952|Mackunda Formation|60953|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marginal marine sandstone and siltstone.||||||
10952|Mackunda Formation|61312|5|Briefly described|p64, p79 Table E2|Cretaceous|Cretaceous|Of the Rolling Downs Group. Siltstone, sandstone, minor shale. Geological Province: Eromanga Basin (absent in NSW).||||||
10952|Mackunda Formation|61611|6|Mentioned|p265 Fig. 3|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||13-MAR-09
10952|Mackunda Formation|61613|6|Mentioned|p282 Fig. 2|Late Cretaceous|Late Cretaceous|Geological Province: Eromanga Basin.||||||07-FEB-11
10952|Mackunda Formation|61614|6|Mentioned|p290 Fig. 2|Late Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||17-MAR-09
10952|Mackunda Formation|61615|6|Mentioned|p302 Fig. 2|Late Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||07-FEB-11
10952|Mackunda Formation|62028|5|Briefly described|p10 Fig. 1|||||||||
10952|Mackunda Formation|62029|5|Briefly described|p15 Fig. 4|Cretaceous|Cretaceous|||||||
10952|Mackunda Formation|62046|5|Briefly described|p125 Fig. 2|Cretaceous|Cretaceous|Geological Province: Cooper-Eromanga Basins.||||||14-APR-08
10952|Mackunda Formation|62376|5|Briefly described|p84|Early Cretaceous|Early Cretaceous|Geological Province: Pedirka Basin.||||||09-FEB-10
10952|Mackunda Formation|62537|6|Mentioned|p191 Fig.2. |Late Cretaceous|Late Cretaceous|Eromanga Basin.||||Overlies Oodnadatta and Allaru Formations. Is overlain by Winton Formation.||
10952|Mackunda Formation|62730|5|Briefly described|p352 Fig. 1|Late Cretaceous|Late Cretaceous|Geological Province: Eromanga Basin.||||||21-APR-08
10952|Mackunda Formation|63979|2|Defined|p53, Fig. 44|Cenomanian|Albian|Previously Mackunda Beds (Vine 1964). Of Manuka Subgroup (Rolling Downs Gp). Conformable on Allaru Mudstone. Conformable below Winton Fm. Max. thick: 150m. Interbedded sandstone, siltstone and mudstone and lesser mudclast intraformational conglomerate.||||||07-FEB-11
10952|Mackunda Formation|64048|6|Mentioned|p64 Tb. 2, p72|||Geological Province: Eromanga Basin.||||||07-FEB-11
10952|Mackunda Formation|64197|6|Mentioned|p625 Fig.1c, p630 Figs.6,7|Cretaceous|Cretaceous|Eromanga Basin.||||Overlies Allaru Mudstone (Marree Subgroup); is overlain by Winton Formation.||10-DEC-15
10952|Mackunda Formation|64665|6|Mentioned|p62.|Cretaceous|Cretaceous|Eromanga Basin.||||||
10952|Mackunda Formation|65238|5|Briefly described|p7 Fig. 8|Early Cretaceous|Early Cretaceous|Geological province: Eromanga Basin. Transgressive marine deposits.||||||
10952|Mackunda Formation|65376|5|Briefly described|p9 Fig.1.2. |Cretaceous|Cretaceous||||||Marginal marine to fluvial mudstone and siltstone.|
10952|Mackunda Formation|65385|5|Briefly described|pS134 Fig.7|Late Cretaceous|Early Cretaceous|Of Eromanga Basin. Overlies Allaru Mudstone and Oodnadatta Formation. Overlain by Winton Formation.||||||08-MAR-12
10952|Mackunda Formation|65489|5|Briefly described|p49, p55, p58, p61, p96, p155|Early Cretaceous|Early Cretaceous|Eromanga Basin. 200m thick. Regional seal.||||Overlies Allaru Mudstone. Is overlain by Winton Formation.||
10952|Mackunda Formation|65925|5|Briefly described|Appendix 2.||||||||Calcareous sandstone; siltstone; shale.|
10952|Mackunda Formation|66518|6|Mentioned|p19 Fig.4.|Cretaceous|Cretaceous|Eromanga Basin.||||Overlies Oodnadatta Formation.||06-FEB-14
10952|Mackunda Formation|66529|6|Mentioned|p12 Fig.5, p16  |||||Unit in Rolling Downs Group.||Overlies Oodnadatta Formation and Allaru Mudstone. Is overlain by Winton Formation.||
10952|Mackunda Formation|66623|6|Mentioned|pp264-265.|||Partly equivalent to Allaru Mudstone in Koonenberry Belt, NSW.||||Overlies Allaru Mudstone.||
10952|Mackunda Formation|67323|5|Briefly described|p87, p92, p93 Fig.12.3, p95 Fig.12.5|Cretaceous|Cretaceous|See also GIS attrib tbl, Solid Geology Map. Eromanga/Carpentaria Basins.||||Overlies Allaru Mudstone. Is overlain by Winton Formation.|Feldspathic sandstone, siltstone.|
10952|Mackunda Formation|67402|4|Described|p26 tbl RRM4|Cenomanian|Albian|Eromanga Basin. Deposited in shallow marine or paralic environments. Maximum thickness of 100m. Estimated porosity of 10-25% with unknown permeability. See also p108, p109, p115 tbl ERO2.||||Overlies the Allaru Mudstone. Overlain by the Winton Formation.|Very fine to fine-grained sandstone, with laminations of siltstone and mudstone and lesser mud-clast intraformational conglomerate.|
10952|Mackunda Formation|67784|5|Briefly described|p25-26, p28-32|Albian|Albian|Northern Eromanga Basin. 90-275m thick.||||Overlies Allaru Formation, overlain by Winton Formation|Contains labeceratid ammonites.|08-FEB-18
10952|Mackunda Formation|68068|5|Briefly described|Map legend|Albian|Albian|Eromanga Basin. Marginal marine to paralic; a marine regression. Fossiliferous: molluscs, forams, wood, diverse microflora, fish and vertebrates.||Unit in Neales River Group.||Conformably overlies Oodnadatta Formation. Is overlain conformably by Winton Formation.|Bimodal cross-bedded, yellow-brown fine to medium sand interbedded with greenish to grey silt and silty clay; then pale grey-green, interbedded, cross-bedded, glauconitic, sand-silt-shale and calcareous shales, mud and clay intraclasts common.|
10952|Mackunda Formation|68131|5|Briefly described|p2 Fig.1|Cretaceous|Cretaceous|Marginal marine to fluvial sediments. Mapped with Mackunda Formation as one unit.|||||Mudstone and siltstone.|
10952|Mackunda Formation|68206|6|Mentioned|p31-33|Albian|Albian|NE Eromanga Basin.||||Overlies Allaru Formation.||
10952|Mackunda Formation|68279|6|Mentioned|p18|||Galilee Basin stratigraphic cross-sections, and mineralogy tables.||||||
10952|Mackunda Formation|68553|6|Mentioned|Map legend; schematic diagram.|Cretaceous|Cretaceous|Eromanga and Carpentaria Basins.||Unit in Rolling Downs Group.||Conformably overlies Allaru Mudstone. Is overlain conformably by Winton Formation.||
10952|Mackunda Formation|68713|5|Briefly described|p22|Cretaceous|Cretaceous|||Of the Neales River Group.||||
10952|Mackunda Formation|68715|6|Mentioned|p30 Fig.7|Cenomanian|Albian|Eromanga Basin.||||||
10952|Mackunda Formation|68731|6|Mentioned|pp209-211|||||||||
10952|Mackunda Formation|68734|5|Briefly described|p218 Fig.2, p221 Fig.3|Cenomanian|Albian|Eromanga Basin (SW and NE). Marine to coastal paralic. Mis-spelt as Mackundra Formation in Fig.2.||Of the Rolling Downs Group.||||16-JAN-17
10952|Mackunda Formation|68821|5|Briefly described|p292 Fig.1, p296|Cretaceous|Cretaceous|Lower Cretaceous age. Parallic to marine sediments.||Of the Rolling Downs Group.||||
10952|Mackunda Formation|69019|4|Described|p83 Fig.20, p85, p99-101.|Cenomanian|Albian|Of Vine and Day (1965). Eromanga Basin; final Cretaceous marine deposition. Thickness from 0-192 m. Has developed a porcellanite horizon.||Unit in Neales River Group.||Overlies Oodnadatta Formation conformably; overlies Allaru Mudstone. Is overlain conformably by Winton Formation.|Pale grey-green, interbedded, glauconitic cross-bedded sand, silt; shale and calcareous shale, often as intraclasts in upper sand beds. Contains ovoidal limestone concretions to tabular limestone bodies.|
10952|Mackunda Formation|69023|5|Briefly described|p79, p86-87, p89 Fig.20, p93|Cenomanian|Albian|See also p105-106, p119, p122-123, p151, p191-192. Defined by Vine and Day (1965) in Queensland as the youngest marine to marginal marine unit within the Eromanga Basin. Thickness varies from <49 to ~82m. Marginal marine and paralic to deltaic. Diverse fauna listed. Weathering has formed porcellanite. Stratigraphic wells intersection data.||||Conformably overlies Oodnadatta Formation and Allaru Mudstone. Is overlain conformably by Winton Formation.|Pale grey-green, interbedded, glauconitic cross-bedded sand, silt, shale and calcareous shale. Local ferricrete capping.|
10952|Mackunda Formation|69457|4|Described|p41:2-3, 6-7, 10-12|Early Cretaceous|Early Cretaceous|Vine and Day (1965). Central and southern Eromanga Basin. Formerly part of the superseded Blanchewater Formation, used for the combined undifferentiated Mackunda-Winton Formations interval. Thickness is variable, from 74m to >150m. Marine; distinguished by its lack of coal. Contains a diverse fossil assemblage, from a dinosaur to microfossils.||Manuka Subgroup.||Conformably overlies Allaru Mudstone and Oodnadatta Formation. Is overlain conformably by Winton Formation.|Thinly interbedded labile very fine- to fine-grained lithic sandstone, laminated siltstone and mudstone with numerous plant remains, and lesser mud-clast intraformational conglomerate.|12-JUL-16
10952|Mackunda Formation|69562|6|Mentioned|p681-682|Mesozoic|Mesozoic|||Said to be a unit in Marree Subgroup.||||06-APR-22
10952|Mackunda Formation|69582|6|Mentioned|p65|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies the Allaru Mudstone. Overrlain by the Winton Formation.||
10952|Mackunda Formation|69594|5|Briefly described|p519, p526, p530-531, p574|Cenomanian|Albian|Vine (1964); Vine and Day (1965). Eromanga Basin. Mostly 75-100+ metres thick. Boundaries in drill holes are distinguished by various geophysical properties (described). Shallow-marine and paralic deposits with abundant volcanilithic sediments from the E. Contains a distinct marine fauna (listed) including the "iconic" Muttaburrasaurus.||||Conformably overlies Allaru Mudstone. Is overlain conformably by Winton Formation.|Labile volcanic lithic-feldspathic interbedded sandstone, siltstone, mudstone and minor impure coquinitic and cone-in-cone limestone and intraformational conglomerate.|
10952|Mackunda Formation|69599|6|Mentioned|p599|Cretaceous|Cretaceous|||||Is overlain unconformably by Moses Sandstone.||
10952|Mackunda Formation|69673|5|Briefly described|p155 fig 127|Cretaceous|Cretaceous|||Manuka Subgroup||Overlies Oodnadatta Formation, Allaru Mudstone, overlain by Winton Formation|Carbonaceous, pyritic shale with lesser interbedded sandstone.|
10952|Mackunda Formation|69797|5|Briefly described|p17 Fig.2|Early Cretaceous|Early Cretaceous|Geol. Prov: Eromanga Basin.||||||
10952|Mackunda Formation|69946|4|Described|p23, p26-28, p57, p94, p123|Late Cretaceous|Early Cretaceous|Vine and Day (1965). Type section is at the headwaters of Mackunda Creek on Gnalta Station. 60 - 120m thick. Wireline log correlations.||||Conformably overlies Allaru Mudstone and Oodnadatta Formation. Is overlain conformably by Winton Formation.|Interbedded, partly calcareous very fine-grained sandstone, siltstone and shale. Locally, transgressive mudstone units are interbedded with shoreface sandstones.|
10952|Mackunda Formation|69947|6|Mentioned|p13 Fig.7.2|Late Cretaceous|Early Cretaceous|Eromanga Basin.||||||
10952|Mackunda Formation|69948|6|Mentioned|Fig.4.18|||Eromanga Basin.||||Overlies Allaru Mudstone. Is overlain by Winton Formation.||
10952|Mackunda Formation|70383|5|Briefly described|p45|Albian|Albian|Eromanga Basin. Marginal marine deposits.||||||
10952|Mackunda Formation|70821|5|Briefly described|p21, p33, p79-80|Late Cretaceous|Late Cretaceous|Eromanga Basin. Absent in the southern Thomson region. 30.5m thick in Mirintu 1 petroleum well. Hydrochemistry mentioned.||Rolling Downs Group.||Conformably overlies Allaru Mudstone. Is overlain by Winton Formation.||
10952|Mackunda Formation|70823|5|Briefly described|p25-p27, p41, p43-p44,p78|Early Cretaceous|Early Cretaceous|Eromanga Basin. Age is minimum depositional age. Up to 200m thick.|c. 101 Ma|||Overlies the Allaru Formation and the Oodnadatta Formation. Overlain by the Winton Formation.||
10952|Mackunda Formation|70824|5|Briefly described|p9|Cretaceous|Cretaceous|Eromanga Basin.||||Overlies the Allaru Mudstone. Overlain by the Winton Formation.||
10952|Mackunda Formation|70836|6|Mentioned|p474|Albian|Albian|Eromanga Basin.||||||
10952|Mackunda Formation|70860|6|Mentioned|p281|||Great Artesian Basin.||||||
10952|Mackunda Formation|71321|6|Mentioned|p15|||Of Eromanga Basin.||||Overlain by Winton Formation. Underlain by Mount Alexander Sandstone Member or Allaru Mudstone.||
10952|Mackunda Formation|71342|3|Fully described|Ch 1 p6, Ch 1 p19, Ch4 p25,|Cenomanian|Albian|Eromanga Basin. Defined by Vine and Day (1965) who nominated the type section at the headwaters of Mackunda Creek on Gnalta Station. Hosts a major confined aquifer. Up to 120m thick. Dated on the basis of palynology and rare macrofossils.Sedimentology and palaeoenvironment are discussed. Spore-pollen zone is given in Ch5 p57.  See also Ch5 p23, Ch5 p26-p28, Ch5 p33, Ch5 p57, Ch5 p125, Ch6 p8, Ch6 p10, Ch7 p13.||||Conformably overlies the Allaru Mudstone and the Oodnadatta Formation. Conformably overlain by the Winton Formation.|Interbedded, partly calcareous, very fine-grained sandstone, siltstone and shale.|
10952|Mackunda Formation|71855|5|Briefly described|p27|||||||Overlies the Toolebuc Formation.||
10952|Mackunda Formation|71863|5|Briefly described|p5|Cenomanian|Albian|Eromanga Basin.||||Overlies the Allaru Mudstone. Overlain by the Winton Formation.||
10952|Mackunda Formation|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA,QLD,NSW). Note that it also appears as a unit in the Neales River Group. Upper part: confined aquifers, generally producing non-flowing artesian water bores.||Rolling Downs Group.||Overlies Oodnadatta FZ. Is overlain by Winton FZ.||
10952|Mackunda Formation|72456|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marree 1:250k map sheet.|||||Sandstone, calcareous; siltstone and shale.|
10952|Mackunda Formation|73167|6|Mentioned|p664 Fig. 2|Cretaceous|Cretaceous|Eromanga Basin.||||||
10952|Mackunda Formation|73249|6|Mentioned|p319|Cretaceous|Cretaceous|Eromanga Basin.||||Overlies the Allaru Mudstone, underlies the Winton Formation.||
10952|Mackunda Formation|73251|6|Mentioned|p36, p62|Early Cretaceous|Early Cretaceous|Eromanga Basin, Frome Embayment. Marginal thermal maturity. Marginal marine.||||Underlain by Allura Mudstone. Underlain by and equivalent to Oodnadatta Formation.||
10952|Mackunda Formation|73343|6|Mentioned|p337|Cretaceous|Cretaceous|Eromanga Basin.||||Underlain by Allaru Mudstone. Equivalent to Winton Formation.||
10952|Mackunda Formation|73479|5|Briefly described|p156 Fig.2, p159-160, p166, p175|Cretaceous|Cretaceous|Eromanga Basin. Fluvial-lacustrine depositional environment. Significantly eroded following exhumation (late Cretaceous).|ca 97 Ma|||Overlies Allaru Mudstone, unconformably underlies Eyre Formation||
11018|Mail Change Limestone|22954|6|Mentioned|Fig3p9|||||||||
11018|Mail Change Limestone|23031|5|Briefly described|28|||Geol province Georgina Basin. Underlying unit V-Creek Limestone||||||
11018|Mail Change Limestone|23393|5|Briefly described|p23 Fig. 6|Cambrian|Cambrian|||||||
11018|Mail Change Limestone|23408|6|Mentioned|p527|||Includes two-toned deeper-water ramp carbonates.||||||15-JUN-09
11018|Mail Change Limestone|30479|6|Mentioned|Fig.6|||See also Fig.7. Stratigraphic relationships||||||
11018|Mail Change Limestone|30914|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
11018|Mail Change Limestone|31396|6|Mentioned|Fig.3|||||||||
11018|Mail Change Limestone|33111|4|Described|p37|||Mention p27.||||||31-OCT-06
11018|Mail Change Limestone|34287|6|Mentioned|Fig.3|||||||||
11018|Mail Change Limestone|34395|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
11018|Mail Change Limestone|34659|6|Mentioned|p221|||||||||
11018|Mail Change Limestone|35054|6|Mentioned|Table 23|||||||||
11018|Mail Change Limestone|35121|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
11018|Mail Change Limestone|35139|4|Described|Table.2|||||||||
11018|Mail Change Limestone|35553|6|Mentioned|p175|||Appendix containing description of Agnostid localities.||||||
11018|Mail Change Limestone|37572|4|Described|p158|||See also Fig.7||||||
11018|Mail Change Limestone|38446|6|Mentioned|Table 23|||||||||
11018|Mail Change Limestone|39445|5|Briefly described|Table 4|||See also p62.||||||31-OCT-06
11018|Mail Change Limestone|39690|6|Mentioned|Table 1|||||||||
11018|Mail Change Limestone|40686|5|Briefly described|p407|||||||||
11018|Mail Change Limestone|40856|6|Mentioned|Fig.23.6|||||||||
11018|Mail Change Limestone|41129|6|Mentioned|Fig.8|||||||||
11018|Mail Change Limestone|41298|6|Mentioned|Map legend|Middle Cambrian||||||||
11018|Mail Change Limestone|41388|6|Mentioned|Fig.2|||||||||
11018|Mail Change Limestone|44091|14|Not recorded|p16,Tb.1,p18||Middle Cambrian|||||||
11018|Mail Change Limestone|44205|14|Not recorded|p51,155|||See also Lexicon.||||||
11018|Mail Change Limestone|44210|2|Defined|map,Tb.2,p13,14||Middle Cambrian|||||||
11018|Mail Change Limestone|44211|2|Defined|p101-107|||Overlain by Split Rock Sandstone and rests on V-Creek Limestone. Restricted to Undilla Basin.||||||
11018|Mail Change Limestone|44213|14|Not recorded|Map Legend||Middle Cambrian|||||||
11018|Mail Change Limestone|44275|14|Not recorded|Map Legend|||||||||
11018|Mail Change Limestone|44920|14|Not recorded|Map Legend,Sheet 2||Middle Cambrian|||||||
11018|Mail Change Limestone|45012|14|Not recorded|p338|||Fauna.||||||
11018|Mail Change Limestone|45052|3|Fully described|p94|||M.Camb.||||||
11018|Mail Change Limestone|45054|6|Mentioned|p6|||Fossil locality||||||
11018|Mail Change Limestone|45079|5|Briefly described|p34|||Cambrian age.||||||
11018|Mail Change Limestone|47058|6|Mentioned|p134|||||||||
11018|Mail Change Limestone|48906|14|Not recorded|Tb.1|||||||||
11018|Mail Change Limestone|60122|6|Mentioned|p57 Appendix|||Correlated with parts of Arthur Creek Formation.  Geological Province: eastern Georgina Basin.||||||31-OCT-06
11018|Mail Change Limestone|62791|6|Mentioned|p239|Middle Cambrian|Middle Cambrian|Source of the Type species of Treptotreta jucunda Henderson & MacKinnon 1981; Middle Cambrian (Goniagnostus nathorsti Biozone).||||||
11018|Mail Change Limestone|63450|5|Briefly described|p82|Middle Cambrian|Middle Cambrian|Geological Province: Undilla Sub-basin.||||||07-FEB-11
11018|Mail Change Limestone|64068|5|Briefly described|p62, 64, 225|||Eastern Georgina Basin. Correlated with Arthur Creek Formation, Roaring Siltstone, Devoncourt Limestone.||||||
11018|Mail Change Limestone|64443|6|Mentioned|p41|||Correlative of Ranken Limestone, Camooweal Dolostone.||||||
11018|Mail Change Limestone|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map; p83|Middle Cambrian|Middle Cambrian|Undilla Sub-basin, Georgina Basin.||Narpa Group.||Overlies V-Creek Limestone. Is overlain by Split Rock Sandstone.|Limestone, bituminous limestone, sandy limestone, calcilutite, minor arenite, chert nodules|
11018|Mail Change 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
11018|Mail Change Limestone|69573|6|Mentioned|p659|||Contains Drumian Stage [Cambrian] fossil sites.||||||
11018|Mail Change Limestone|69591|4|Described|p87-88, p90, p96-97, p98 Fig.2.91|Cambrian|Cambrian|Undilla Sub-basin, Georgina Basin. Up to 30m thick. Contains abundant brachiopods and rare trilobites. Supratidal or high intertidal deposits. Coeval with Camooweal Dolostone and upper Age Creek Formation.||Narpa Group.||Conformably overlies V Creek Limestone. Is overlain by and grades laterally into Split Rock Sandstone.|Blue-grey and yellow mottled, thick-bedded, fine muddy limestone; includes microbial firm ground in upper shoreface settings and ephemeral evaporite horizons.|
11018|Mail Change Limestone|70380|5|Briefly described|p757|Cambrian|Cambrian|Eastern Georgina Basin. The cyclic pattern of deposition, interpreted as parasequences, is comparable with the Briggs Member of Oolloo Dolostone (Daly Basin).|||||Contains cycles of alternating limestone (<2m thick) and calcareous siltstone interbeds (up to 8m thick).|
11018|Mail Change Limestone|72321|6|Mentioned|Fig 2|Drumian|Drumian|Undilla Sub-basin, Georgina Basin. Australian Stage: Undillan.||of Narpa Group.||||
11018|Mail Change Limestone|72516|6|Mentioned|p92|Cambrian|Cambrian|Eastern Georgina Basin.||||Equivalent to the Arthur Creek Formation.||03-JUN-21
11018|Mail Change Limestone|73418|5|Briefly described|p4 Fig.3|Miaolingian|Miaolingian|Georgina Basin, Undilla Sub-basin.||Narpa Group||Overlies V-Creek Limestone, underlies Split Rock Sandstone|Limestone.|
11034|Mainoru Formation|22538|6|Mentioned|Fig3 P708|||||||||
11034|Mainoru Formation|22600|4|Described|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
11034|Mainoru Formation|22853|3|Fully described|26|Proterozoic|Proterozoic|Of the Roper Group. Max thickness 200 m. Overlying unit Crawford Formation, underlying unit Limmen Sandstone||||||31-OCT-06
11034|Mainoru Formation|23216|5|Briefly described|Table1p8,34|||||||||
11034|Mainoru Formation|23374|5|Briefly described|p6||Calymmian|U/Pb Zircon age of 1494Ma. Of the Roper Group. In the McArthur Basin.||||||31-OCT-06
11034|Mainoru Formation|23404|5|Briefly described|p638|Calymmian|Calymmian|Age: 1492+/-4Ma.||||||31-OCT-06
11034|Mainoru Formation|23407|5|Briefly described|p633|||||||||
11034|Mainoru Formation|23733|5|Briefly described|p45 App.2|Mesoproterozoic|Mesoproterozoic|Of Roper Group.  Age: 1492+/-2Ma.  Geological Province: McArthur Basin.||||||
11034|Mainoru Formation|23776|5|Briefly described|p711|||Of Roper Group.||||||
11034|Mainoru Formation|23937|2|Defined|p84 App. 1, p30-36, p23-24, p27,26, p6|Calymmian|Calymmian|Of the Roper Group.  Conformably overlain by Crawford Formation.  Age: 1492+/-4 Ma; 1493+/-4Ma (Jackson et al, 1999).  Max. thickness: <100m.  Geological Province: McArthur Basin.  See also p30.||||||10-NOV-17
11034|Mainoru Formation|24047|6|Mentioned|p23|||Contains the Wadjeli Sandstone Member.  Geological Province: McArthur Basin.||||||
11034|Mainoru Formation|24048|4|Described|p70|Mesoproterozoic|Paleoproterozoic|Of the Roper Group.  Geological Province: McArthur Basin.||||||07-NOV-08
11034|Mainoru Formation|24049|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Roper Group. Siltstone: micaceous in places; interbedded with sandstone: fine-grained, thin to medium-bedded, glauconitic or pyritic in places, mudstone intraclasts; mudstone: carbonaceous, thin to very thin-bedded. Geol. Prov: McArthur Basin.||||||13-OCT-05
11034|Mainoru Formation|24050|3|Fully described|p42, p8 Tb. 2|Mesoproterozoic|Mesoproterozoic|Of the Roper Group.  Calcareous and non-calcareous mudstone; glauconitic and micaceous siltstone and sandstone; limestone.  Overlies Limmen Sandstone; underlies Crawford Formation.  Thickness: ~250m.||||||31-OCT-06
11034|Mainoru Formation|24051|5|Briefly described|Map Legend|Calymmian|Calymmian|Of Roper Group. Geological Province: McArthur Basin.||||||
11034|Mainoru Formation|24303|5|Briefly described|p59 Appendix|||Of the Roper Group. Geological Province: McArthur Basin. Age: 1492 +/- 4 Ma. Possible correlative of Grayling Member (Baralandji Formation) - see p61 Appendix.||||||
11034|Mainoru Formation|32660|5|Briefly described|Table 4|||||||||
11034|Mainoru Formation|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
11034|Mainoru Formation|40691|6|Mentioned|p65|||Mention Fig.4||||||
11034|Mainoru Formation|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
11034|Mainoru Formation|41220|6|Mentioned|Fig.3|||||||||
11034|Mainoru Formation|41268|6|Mentioned|p290|||||||||
11034|Mainoru Formation|41531|6|Mentioned|p167|||||||||
11034|Mainoru Formation|42385|4|Described|p26|||See also Table 5 p25.||||||31-OCT-06
11034|Mainoru Formation|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
11034|Mainoru Formation|42597|5|Briefly described|Map Legend|Adelaidean||||||||
11034|Mainoru Formation|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.||Lower Roper Group (Roper Group).||In schematic section, underlies Crawford Formation; overlies Limmen Sandstone.|Micaceous siltstone to sandstone, dolomitic siltstone, mudstone, micaceous siltstone to muddy siltstone, sandstone and siltstone. Detailed lithology given.|11-NOV-11
11034|Mainoru Formation|42639|4|Described|p38|||||||||
11034|Mainoru Formation|42700|5|Briefly described|map legend|Mesozoic|Early Cretaceous|||||||
11034|Mainoru Formation|42739|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Of the Lower Roper Group. Interbedded red-brown to purple mudstone and very fine to fine grained sandstone both commonly micaceous and glauconitic.||||||19-OCT-05
11034|Mainoru Formation|42812|3|Fully described|p47, Table 5|||Of the Roper Group.||||||31-OCT-06
11034|Mainoru Formation|42846|5|Briefly described|p503, Fig.1 p502|||Oof Roper Group. Fine-grained. Geological Province: McArthur Basin.||||||09-MAY-05
11034|Mainoru Formation|43010|5|Briefly described|p164|||||||||
11034|Mainoru Formation|43036|4|Described|p59|||Of Roper Group.||||||31-OCT-06
11034|Mainoru Formation|43149|5|Briefly described|Map Legend||Mesoproterozoic|Of Roper Group. Of Calymmian age.||||||31-OCT-06
11034|Mainoru Formation|43652|6|Mentioned|p386|||||||||
11034|Mainoru Formation|44112|3|Fully described|Table12p68,69-70|||||||||
11034|Mainoru Formation|44287|14|Not recorded|p.12, opp.11|||Glauconitic. (E53-3).||||||
11034|Mainoru Formation|44288|14|Not recorded|map legend|||Siltstone, glauconitic sandstone, feldspathic sandstone, shale. Upper (?) Proterozoic.||||||
11034|Mainoru Formation|44299|4|Described|p.13|||SD/53-7,8. U(?) Proterozoic. Table 1.||||||
11034|Mainoru Formation|44300|14|Not recorded|map legend||Neoproterozoic|SD/53-7,8. U.Proterozoic, pt of Roper Gp.||||||
11034|Mainoru Formation|44332|14|Not recorded|p.7,opp.6,map|||(D53-14).||||||
11034|Mainoru Formation|44333|14|Not recorded|map legend|||Upper(?) Proterozoic.||||||
11034|Mainoru Formation|44400|2|Defined|p.9,Tb.1,opp.p.6,map|||Mt.Marumba Sheet. (D53-6).||||||
11034|Mainoru Formation|44401|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
11034|Mainoru Formation|44434|14|Not recorded|p.7, opp. p.6, map|||Includes Wooden Duck Member. (D53-11,12).||||||
11034|Mainoru Formation|44435|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
11034|Mainoru Formation|44436|5|Briefly described|p.11, opp. p. 7, map|||(E53-4).||||||02-DEC-04
11034|Mainoru Formation|44437|5|Briefly described|map legend|Precambrian|Precambrian|Of the Roper Group.  Laminated micaceous siltstone and fine-grained sandstone.  Conformably overlies Limmen Sandstone; conformably overlain by Crawford Formation.  Upper (?) Proterozoic.||||||08-DEC-04
11034|Mainoru Formation|44459|14|Not recorded|P.8,opp.p.6, map|||(E53-2).||||||
11034|Mainoru Formation|44460|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
11034|Mainoru Formation|44471|14|Not recorded|p.9,11,15,opp.7, map|||(D53-10).||||||
11034|Mainoru Formation|44472|5|Briefly described|map legend|||Of the Roper Group.  Micaceous siltstone, blocky chert, pink to cream silicified siltstone.  Upper (?) Proterozoic.||||||02-DEC-04
11034|Mainoru Formation|44473|14|Not recorded|p.10, opp. p.7|||(E53-7). Formation of Roper Group.||||||
11034|Mainoru Formation|44474|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
11034|Mainoru Formation|44530|14|Not recorded|p.11, opp.12|||(D53-15).||||||
11034|Mainoru Formation|44531|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
11034|Mainoru Formation|45022|6|Mentioned|p.80||Adelaidean|Of Roper Group.  Tb.11.||||||
11034|Mainoru Formation|45162|6|Mentioned|Fig.4|||||||||
11034|Mainoru Formation|46861|6|Mentioned|Fig.2|||||||||
11034|Mainoru Formation|46968|6|Mentioned|p304|||||||||
11034|Mainoru Formation|60483|5|Briefly described|p7 Fig. 5, p9|||Of the Roper Group. Age: 1492+/-4ma SHRIMP, Jackson et al 1999). Geological Province: McArthur Basin. Carbonaceous unit.||||||
11034|Mainoru Formation|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Roper Group. Overlain by Crawford Formation, underlain by Limmen Sandstone.||||||
11034|Mainoru Formation|60573|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Roper Group.  Contains the Showell, Wooden Duck, Mountain Valley Limestone, Nullawun, Wadjeli Sandstone and Gibb Members.  Overlies Limmen Sandstone; underlies Crawford Fm.  Actual Mainoru Formation rocks are undifferentiated on this sheet area.||||||15-FEB-05
11034|Mainoru Formation|60574|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Roper Group. Overlies the Limmen Sandstone. Overlain by the Crawford Formation. Green to grey micaceous siltstone, shale and fine-grained glauconitic sandstone.||||||
11034|Mainoru Formation|61390|5|Briefly described|Map Legend|Ectasian|Calymmian|Of the Collara Subgroup.||||||
11034|Mainoru Formation|61403|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Roper Group. Siltstone: micaceous in places; interbedded with sandstone: fine-grained, thin to medium-bedded, glauconitic or pyritic in places, mud stone intraclasts; mudstone: carbonaceous, thin to very thin-bedded. Geol. Prov: McArthur Basin.||||||
11034|Mainoru Formation|61566|5|Briefly described|p622|Proterozoic|Proterozoic|Of the Roper Group. Mica-rich siltstone. Geological Province: McArthur Basin.||||||
11034|Mainoru Formation|61572|5|Briefly described|p666|Mesoproterozoic|Mesoproterozoic|Of the lower Roper Group. Age: 1493Ma.  Geological Province: McArthur Basin.||||||
11034|Mainoru Formation|62376|5|Briefly described|p38|Mesoproterozoic|Mesoproterozoic|Of the Roper Group. Geological Province: Beetaloo Sub-Basin.||||||09-FEB-10
11034|Mainoru Formation|63866|4|Described|p113, p116|Calymmian|Calymmian|McArthur basin.|1493 +/- 4 Ma (Jackson et al., 1999)|Roper Group|||Tuffite.|
11034|Mainoru Formation|64784|5|Briefly described|p2 Fig.2 |Proterozoic|Proterozoic|Beetaloo Basin.||Unit in Roper Group.||Overlies Limmen Sandstone. Is overlain by Crawford Formation.||
11034|Mainoru Formation|64815|6|Mentioned|p5 Fig.3 |||||Of the Roper Group.||||
11034|Mainoru Formation|64816|5|Briefly described|p2 Fig.1,p4  |Calymmian|cCalymmian||1492 +/- 4 Ma.|Unit in Roper Group.||||
11034|Mainoru Formation|64817|6|Mentioned|p353 Fig.4 |||||Of the Roper Group.||||
11034|Mainoru Formation|64975|6|Mentioned|p162 Fig.6.|Mesoproterozoic|Mesoproterozoic|||Unit in Roper Group.|Includes Wooden Duck Member.|||
11034|Mainoru Formation|65228|5|Briefly described|Fig.02.|||||Unit in Roper Group.||Overlies Limmen Sandstone. Is overlain by Crawford Formation.||
11034|Mainoru Formation|65236|5|Briefly described|p3 Fig. 3|Mesoproterozoic|Mesoproterozoic|Of the Roper Group. Geological province: Beetaloo Sub-basin.||||||04-JUN-09
11034|Mainoru Formation|65337|6|Mentioned|p7, p45.|||McArthur Basin. Storm shelf facies closely resembles that of Crow Formation.|1492 +/- 4 Ma (Jackson et al. 1999).|||||
11034|Mainoru Formation|65340|4|Described|p11, p62.|Mesoproterozoic|Mesoproterozoic|A thick recessive unit, rarely well-exposed. The cross-bedded lithofacies is identical to Crawford Formation and was partially mis-mapped by Yates (1963). Reflects a mainly subtidal, storm-wave-influenced marine shelf environment.|1492 +/- 4 Ma (Jackson et al. 1999).|Unit in Roper Group.||Overlies Limmen Sandstone. Is overlain by Crawford Formation.|Interbedded green to grey micaceous mudstone and tabular lithic, glauconitic fine sandstone with basal markings; also resistant intervals of grey, pseudokarstically weathering, thick bedded lithic fine sandstone with swaley crossbeds.|
11034|Mainoru Formation|65342|5|Briefly described|p8.|||McArthur Basin. Max. thickness at least 190 m.  Seen as having potential as an insulating layer for geothermal energy.||Unit in Roper Group.||Overlies Limmen Sandstone. Is overlain by Crawford Formation.|Siltstone, shale, fine sandstone.|
11034|Mainoru Formation|67144|5|Briefly described|Map legend.|Calymmian|Calymmian|Recessive.||Unit in Roper Group.||Overlies Limmen Sandstone. Is overlain by Crawford Formation.|Red-brown micaceous siltstone to very fine-grained sandstone; minor thin beds of dolomitic siltstone and light purple mudstone; minor glauconitic fine-grained sandstone and siltstone.|
11034|Mainoru Formation|67323|5|Briefly described|Mount Isa Block Time-Space Plot, p9|Mesoproterozoic|Mesoproterozoic|See also Eastern Australia Time-Space Plot. McArthur region (NT) and Camooweal-Murphy Domain, Mount Isa Inlier (QLD). Ages: 1492+/-4 Ma, 1493+/-4 Ma (Jackson et al. 1999).||||Correlated with South Nicholson Group||
11034|Mainoru Formation|67352|4|Described|p13, p47, p49|Calymmian|Calymmian|McArthur Basin. Over 1km thick.||Roper Group||Overlies Limmen Sandstone (conformably).  Overlain by Crawford Formation (conformably) or Buckalara Sandstone or Top Springs Limestone.|Siliceous siltstone and shale; micaceous siltstone and very finegrained sandstone: tabular to fissile and glauconitic; minor glauconitic fine-grained sandstone and siltstone.|
11034|Mainoru Formation|68146|6|Mentioned|p197|||Ages of tuffaceous layers; Jackson et al. (1999).|1492 +/- 4 Ma and 1493 +/- 4 Ma.|||||
11034|Mainoru Formation|69018|5|Briefly described|p450 Fig.1b|Calymmian|Calymmian||1492 +/- 4 Ma.|Of Roper Group.||||
11034|Mainoru Formation|69430|4|Described|p15:3, 26-27, 30, 34, 48, 62|Calymmian|Calymmian|McArthur Basin. Abbott et al. (2001) divided the Formation into six named Members based on lithology. SHRIMP U-Pb zircon age for a tuffaceous bed.|1492 +/- 4 Ma (Jackson et al., 1999).|Collara Subgroup.|Gibb, Wadjeli Sandstone, Nullawun, Mountain Valley Limestone, Wooden Duck, Showell, Members.|Conformably overlies Limmen Sandstone. Is ovelain conformably by Crawford Formation or disconformably by Jalboi Formation.|Red and green mudstone and siltstone, glauconitic and micaceous sandstone, micritic and intraclastic limestone, calcareous and non-calcareous mudstone.|12-JUL-16
11034|Mainoru Formation|69458|5|Briefly described|p42:21|||McArthur Basin.||Roper Group.||Is overlain unconformably by Annie Creek Limestone.||12-JUL-16
11034|Mainoru Formation|69591|5|Briefly described|p52||||1493 and 1492 +/- 4 Ma (Jackson et al., 1999).|||Corelated with the South Nicholson Group in Qld.||
11034|Mainoru Formation|69673|5|Briefly described|p16 fig 13, p31|||McArthur Basin. Unexplored source rock potential.|1492 +/- 4 Ma (SHRIMP)|Collara Subgroup||Overlain by Crawford Formation, Jalboi Formation, Overlies Limmen Sandstone|Tuffaceous bed.|
11034|Mainoru Formation|70734|5|Briefly described|p14, 16|||McArthur Basin.||Of Collara Subgroup.|Includes Gibb Member, Nullawun Member, Mountain Valley Limestone Member, Wooden Duck Member, Showell Creek Member.|||
11034|Mainoru Formation|70822|5|Briefly described|p102 fig 1 (A), p104|Mesoproterozoic|Mesoproterozoic|SHRIMP U-Pb zircon age from tuffs in Showell Mmeber.|1492 +/- 4 Ma (Southgate et al., 2000).|Roper Group.|Gibb, Nullawun, Mountain Valley Limestone, Wooden Duck, Showell Creek, Members.|Overlies Limmen Sandstone; overlain by Crawford Formation.||24-SEP-18
11034|Mainoru Formation|70897|5|Briefly described|p44, Fig.1.7.6,9|Mesoproterozoic|Mesoproterozoic|This age, and another at 1493 +/- 4 Ma, represent a maximum depositional age and effectively the actual deposition age.|1492 +/- 4 Ma.|Roper Group.|||Includes green claystone (?tuffs) from dark grey, laminated, low-energy (deep-water) shales.|
11034|Mainoru Formation|70968|2|Defined|p6, p13, p17-35, p44, p53, p69, p123|Calymmian|Calymmian|See also p126, p130-131, p143. Sweet in Abbott et al. (2001) after Dunn (1963). Named after Mainoru homestead. Originally mapped as middle part of Wigram Formation of Malay Road Group (Dunnet, 1965) and as upper part of Baralminar beds (Plumb and Roberts, 1992): these names are now superseded. Partially mismapped as Crawford Formation by Yates (1963) in ROBINSON RIVER sheet. Type section is SE of Mountain Valley homestead at 372100mE 8444000mN (base) through 373600mE 8437600mN then SE to 379600mE 8433200mN (top), in URAPUNGA sheet. The usefulness or otherwise of subdividing the Formation is discussed. Very recessive: forms rubble- and scree-covered valleys. Widely distributed. Variable thickness up to c.1000m. Fluvial floodplain to shallow-marine facies. Is intruded by Derim Derim Dolerite sills.|1492 +/- 4 Ma (Jackson et al., 1999).|Collara Subgroup.|Wadjeli Sandstone, Wooden Duck, Mountain Valley Limestone, Nullawun, Gibb, Showell, Members.|Overlies Limmen Sandstone and Mantungula Formation conformably (locally disconformably). Underlies Crawford Formation gradationally, and Buckingham Bay Sandstone or Jalboi Formation unconformably.|A complex unit dominated by red, green, grey and black shale and siltstone, with lesser glauconitic and micaceous sandstone, micritic and intraclastic limestone, and calcareous mudstone. Carbonates are minor and atypical of Roper Group.|
11034|Mainoru Formation|71059|4|Described|p3, p14-16, p18, p20, p24, p31|Mesoproterozoic|Mesoproterozoic|McArthur Basin. 270-1000m thick. TOC and Pyrolysis, elemental kerogen CHONS, X-ray diffraction, organic petrology reflectivity, data all detailed.||Collara Subgroup.|Gibb, Wadjeli Sandstone, Nullawun, Mountain Valley Limestone, Wooden Duck, Showell, Members.|Conformably overlies Limmen Sandstone. Is overlain conformably by Crawford Formation, and unconformably to disconformably by Jalboi Formation.|Non-calcareous and calcareous mudrocks, glauconitic and micaceous sandstone, micritic and intraclastic limestone.|
11034|Mainoru Formation|71369|6|Mentioned|p4|||Ages are U-Pb and interpreted as depositional ages for the tuffs of this formation.|1492 +/- 4 Ma and 1493 +/- 4 Ma|||||
11034|Mainoru Formation|71488|5|Briefly described|p141 fig 1b, p142|Calymmian|Calymmian|Dated at 1492 +/- 4 Ma and 1492 +/- 29 Ma by Jackson et al., 1999 and Southgate et al., 2000, respectively.|c. 1492 Ma (SHRIMP)|Collara Subgroup|Includes the Gibb Member, Nullawan Member, Mountain Valley Limestone Member, Wooden Duck Member and the Showell Creek Member.|Overlies the Limmen Sandstone. Overlain by the Crawford Formation.||
11034|Mainoru Formation|71494|4|Described|p2-p27|||Intersected by six HyLogged holes. Crops out in an ENE-trending belt in northwestern Urapunga. Originally defined by Abbott et al (2001) who also defined new members. Core log features presented in this volume.|||Includes the Mountain Valley Limestone Member, Wooden Duck Member, Nullawun Member and the Showell Member.||Comprises red, green grey and black shale and siltstone, glauconititc and micaceous sandstone, micritic and intraclastic limestone and calcareous mudstone.|
11034|Mainoru Formation|71592|5|Briefly described|Appendix A.|||McArthur Basin.|1492+/-4 Ma (crystallisation: U-Pb zircon).||||Tuffite, tuff.|
11034|Mainoru Formation|71779|5|Briefly described|p2, p23, p24, p26, 27|||Urapunga, Beetaloo Sub-basin and Bauhinia Downs Regions, McArthur Basin. SHRIMP U-Pb zircon age from tuffs in Showell Member.|1492 +/- 4 Ma, 1493+/-4 Ma (Jackson et al., 1999)|Collara Subgroup|Includes the Showell Member, Wooden Duck Member, Mountain Valley Limestone Member, Nullawun Member, Wadjeli Sandstone Member, Kilgour Sandstone Member, and Gibb Member.|||24-SEP-18
11034|Mainoru Formation|71893|4|Described|p5, p8-p9, p13, p17, p20, p25, p32|Calymmian|Calymmian|McArthur Basin.||Collara Subgroup|Includes the Showell Member.|Conformably (locally disconformably) overlies the Limmen Sandstone. Conformably overlain by the Crawford Formation.||
11034|Mainoru Formation|72526|5|Briefly described|p3, p8 Fig.1.3, p85,|Calymmian|Calymmian|Shown as located in the Urapunga Fault Zone, Beetaloo Sub-basin, Batten Fault Zone and Southeastern McArthur Basin. Includes tuffs dated at 1492 +/- 4 Ma and 1493 +/- 4 Ma.|1493 +/-4 Ma to 1492 +/-4 Ma|Collara Subgroup||Overlies Limmen Sandstone and underlies Crawford Formation.||
11034|Mainoru Formation|72527|5|Briefly described|p1, p10, p41, p56, p65.|Calymmian|Calymmian|Tuffs dated at 1492 +/- 4 Ma and 1493+/- 4 Ma (Jackson et al. 1999).|younger than c. 1492 Ma|Collara Subgroup|||Includes tuffs.|
11034|Mainoru Formation|72718|6|Mentioned|p7, p9|Calymmian|Calymmian|Southern McArthur Basin.|1492 +/- 4 Ma|Collara Subgroup, Roper Group|Showell Member|Partly underlain by Limmen Sandstone. Overlain by Crawford Formation.||
11034|Mainoru Formation|72912|5|Briefly described|p5 Fig.3, p20.|Mesoproterozoic|Mesoproterozoic|Located in the Urapunga Fault Zone, Beetaloo Sub-basin and the Batten Fault Zone in the Southern McArthur Basin. Age determined using volcanic tuff samples; ref Jackson et al., 1999. U-Pb zircon sedimentary depositional age (Ma).|1492 +/- 4 Ma, 1493 +/- 4 Ma|Collara Subgroup||Overlies Limmen Sandstone and underlies Crawford Formation.|Includes tuffs.|
11034|Mainoru Formation|73042|6|Mentioned|p4|Calymmian|Calymmian|Southern McArthur Basin, Roper Superbasin. Geochronology is a U-Pb zircon sedimentary depositional age (?maximum depositional age).|1492+/-4 Ma and 1493+/-4 Ma|Collara Subgroup, Roper Group||Underlain by Limmen Sandstone. Overlain by Crawford Formation.||
11034|Mainoru Formation|73083|6|Mentioned|p47|Mesoproterozoic|Mesoproterozoic|||||||
11034|Mainoru Formation|73242|5|Briefly described|p39|Calymmian|Calymmian||ca 1492 Ma|Collara Subgroup, Roper Group|Showell Member, Wooden Duck Member, Moutain Valley Limestone Memebr, Nullawun Member, Wadjeli Sandstone Member, Gibb Member|Underlain by Limmen Sandstone. Overlain by Crawford Formation. Intruded by Derim Derim Dolerite.|Includes felsic volcanic rocks, interbedded mudstone and fine sandstone, marine shelf sandstone, mudstone and shale, and limestone in mudstone.|
11034|Mainoru Formation|73280|6|Mentioned|p1, p4-5, App.1A, App.1B, App.1C|||McArthur Basin. Sampled for XRD mineralogy to investigate brittleness and Kubler indices [see report].||||||
11034|Mainoru Formation|73412|5|Briefly described|p4, 8|||Southern McArthur Basin.||Collara Subgroup.||Overlies Limmen Sandstone and Mantungula Formation. Is overlain by Crawford Formation.||
11103|Mallapunyah Formation|22453|5|Briefly described|p 11|||||||||
11103|Mallapunyah Formation|22538|6|Mentioned|App1 P722|||||||||
11103|Mallapunyah Formation|22664|5|Briefly described|Fig. 2 p34|||Of the Umbolooga Subgroup (McArthur Group).||||||31-OCT-06
11103|Mallapunyah Formation|22670|6|Mentioned|52, fig 1, 53,58|||Formation as 'Fmt' in text||||||
11103|Mallapunyah Formation|22720|6|Mentioned|p 174|||McArthur Basin||||||
11103|Mallapunyah Formation|22853|3|Fully described|15|Proterozoic|Proterozoic|Of the Umbolooga Subgroup. Max thickness 220 m. Overlain by Amelia Dolomite; underlain by Masterton Sandstone.||||||31-OCT-06
11103|Mallapunyah Formation|23363|5|Briefly described|351 Tab.1|Statherian|Statherian|Age: 1650+/-20Ma.||||||31-OCT-06
11103|Mallapunyah Formation|23387|6|Mentioned|p18 fig.19|||Of Umbolooga Subgroup.||||||
11103|Mallapunyah Formation|23396|6|Mentioned|p419|||||||||
11103|Mallapunyah Formation|23397|5|Briefly described|p469|||||||||
11103|Mallapunyah Formation|23398|4|Described|p440||Statherian|||||||
11103|Mallapunyah Formation|23776|5|Briefly described|p705 Fig 2.|||Of Umbolooga Subgroup.||||||
11103|Mallapunyah Formation|23902|4|Described|p1568 Fig.2|||Of the Umbolooga Subgroup. Overlain by the Amelia Dolomite. Overlies the Masterton Sandstone. Geological Province: McArthur Basin||||||
11103|Mallapunyah Formation|23910|5|Briefly described|p292 Fig. 3|||Of Umbolooga Subgroup.  Geological Province: McArthur Basin.||||||
11103|Mallapunyah Formation|23963|5|Briefly described|p1238, 1239 Fig.2|||Geological Province: McArthur Basin. Of the Umboloonga Subgroup||||||03-MAR-05
11103|Mallapunyah Formation|23968|6|Mentioned|p1362|||Geological Province: McArthur Basin.||||||
11103|Mallapunyah Formation|24047|5|Briefly described|p12 Fig. 10, p40|Paleoproterozoic|Paleoproterozoic|Age: ~1670Ma.  Geological Province: McArthur Basin.||||||07-NOV-08
11103|Mallapunyah Formation|24048|6|Mentioned|p55|||||||||
11103|Mallapunyah Formation|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Of Umbolooga Subgroup. Overlain by Amelia Dolomite. Carbonate. Geological Province: Southern McArthur Basin.||||||
11103|Mallapunyah Formation|30272|6|Mentioned|p5|||Stratigraphic table on p5.||||||31-OCT-06
11103|Mallapunyah Formation|30344|6|Mentioned|Fig.4|||Part of Umbolooga Formation||||||
11103|Mallapunyah Formation|30345|6|Mentioned|Table 1|||Lithology. Carpentarian age||||||
11103|Mallapunyah Formation|32339|5|Briefly described|p143|||||||||
11103|Mallapunyah Formation|32363|5|Briefly described|Table 1|||||||||
11103|Mallapunyah Formation|32479|6|Mentioned|Fig.2|||||||||
11103|Mallapunyah Formation|32658|3|Fully described|Table 2|||See also Fig. 3||||||
11103|Mallapunyah Formation|32660|5|Briefly described|Table 4|||||||||
11103|Mallapunyah Formation|33665|6|Mentioned|p368|||See also Fig.2||||||
11103|Mallapunyah Formation|33666|6|Mentioned|p528|||Table 1.||||||
11103|Mallapunyah Formation|35162|6|Mentioned|Table.1|||||||||
11103|Mallapunyah Formation|35261|6|Mentioned|Fig.2|||||||||
11103|Mallapunyah Formation|37568|6|Mentioned|p79|||||||||
11103|Mallapunyah Formation|39561|6|Mentioned|Fig.5|||||||||
11103|Mallapunyah Formation|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
11103|Mallapunyah Formation|40105|6|Mentioned|Fig.7|||||||||
11103|Mallapunyah Formation|40259|6|Mentioned|Table 1|||||||||
11103|Mallapunyah Formation|40691|5|Briefly described|p19|||||||||
11103|Mallapunyah Formation|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
11103|Mallapunyah Formation|41220|6|Mentioned|Fig.3|||||||||
11103|Mallapunyah Formation|41268|5|Briefly described|Fig.3|||||||||
11103|Mallapunyah Formation|41277|6|Mentioned|Fig.2|||||||||
11103|Mallapunyah Formation|42385|4|Described|p15|||See also Table 4 p17.||||||31-OCT-06
11103|Mallapunyah Formation|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
11103|Mallapunyah Formation|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.||Of Umbolooga Subgroup (McArthur Group).||In schematic section, underlies Amelia Dolomite; overlies Masterton Sandstone.|Shale and siltstone; sandstone interbeds; stromatolitic dolostone; botryoidal quartz nodules (cauliflower chert). Detailed lithology given.|11-NOV-11
11103|Mallapunyah Formation|42639|3|Fully described|p22, Table 5 p21|||||||||
11103|Mallapunyah Formation|42700|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
11103|Mallapunyah Formation|42739|5|Briefly described|map legend|Statherian|Statherian|Of the Umbolooga Subgroup. Interbedded red to purple dolomitic mudstone and variably dolomitic cross-bedded sandstone; stromatolitic dolostone, flat-pebble breccia, rare carbonaceous shale and pink tuffite.||||||19-OCT-05
11103|Mallapunyah Formation|42812|3|Fully described|p33, Table 4|||Of the Umbolooga Subgroup.||||||31-OCT-06
11103|Mallapunyah Formation|42935|6|Mentioned|p529 Fig.2|||of Umbolooga Subgroup||||||
11103|Mallapunyah Formation|43010|5|Briefly described|Fig.6||Mesoproterozoic|of "Mid Proterozoic" age.||||||
11103|Mallapunyah Formation|43036|3|Fully described|p45|||Of the Umbolooga Subgroup.||||||31-OCT-06
11103|Mallapunyah Formation|44112|6|Mentioned|p55|||||||||
11103|Mallapunyah Formation|44287|14|Not recorded|p.9-11,,19,opp.9|||(E53-3).||||||
11103|Mallapunyah Formation|44288|14|Not recorded|map legend|||Quartz sandstone, purple siltstone, dolomite, chert, siderite. Lower (?) Proterozoic.||||||
11103|Mallapunyah Formation|44473|14|Not recorded|p.9, opp. p.7|||(E53-7). Basal formation of McArthur Group.||||||
11103|Mallapunyah Formation|44474|14|Not recorded|map legend|||Lower (?) Proterozoic.||||||
11103|Mallapunyah Formation|44530|14|Not recorded|p.9,10, opp.10|||(D53-15).||||||
11103|Mallapunyah Formation|44531|14|Not recorded|map legend|||Lower (?) Proterozoic.||||||
11103|Mallapunyah Formation|45162|1|Redefined|p55-65|Proterozoic|Proterozoic|Mention p82.||||||28-MAR-18
11103|Mallapunyah Formation|46915|4|Described|p153|||Depositional environments discussed.||||||
11103|Mallapunyah Formation|46968|6|Mentioned|Fig.2|||||||||
11103|Mallapunyah Formation|60483|5|Briefly described|p7 Fig. 5, p30|||Of Umbolooga Subgroup (McArthur Group). Geological Province: McArthur Basin.||||||05-OCT-07
11103|Mallapunyah Formation|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Umbolooga Subgroup. Overlian by Amelia Dolomite, underlian by Masterton Sandstone.||||||
11103|Mallapunyah Formation|62084|5|Briefly described|p936 Fig.5|||Isa Superbasin. McArthur Basin. Shown as Mallapunyah Fm.||McArthur Group|||Hematitic siltstones.|
11103|Mallapunyah Formation|63112|6|Mentioned|p1191 Fig.2|||Isa Superbasin; southern McArthur Basin. Age approximated from Fig.2.|c.1655-1645 Ma.|Unit in Gun and Loretta Supersequences.||||
11103|Mallapunyah Formation|63866|5|Briefly described|p54|||Isa Superbasin.||Gun Supersequence||||
11103|Mallapunyah Formation|64815|6|Mentioned|p4 Fig.2, p5 Fig.3, p8 Tb.1, p18-19|||Mainly siliciclastic.||Of the Umbolooga Subgroup.||||
11103|Mallapunyah Formation|64817|6|Mentioned|p353 Fig.4 |||||Of the Umbolooga Subgroup.||||
11103|Mallapunyah Formation|65228|5|Briefly described|p24, p25, Table 1, Figs.02, 04, 11-12.|Statherian|Statherian|Part of Gun Supersequence, but upper parts are in Loretta Supersequence. Age from SHRIMP detrital zircon. Gamma ray log, lithology and facies detailed. Measured section.|Maximum age of 1653 +/- 9 Ma.|Unit in Umbolooga Subgroup.||Conformably overlies Masterton Sandstone. Is overlain by Amelia Dolomite.||
11103|Mallapunyah Formation|65340|5|Briefly described|p52.|||Western Foelsche Inlier.||Unit in McArthur Group.||Overlies Echo Sandstone.||
11103|Mallapunyah Formation|67144|5|Briefly described|Map legend.|Statherian|Statherian|Mainly recessive.||Unit in Umbolooga Subgroup.||Overlies Masterton Sandstone. Is overlain by Amelia Dolostone.|Red to purple dolomitic shale and siltstone; dolomitic cross-bedded sandstone interbeds; stromatolitic dolostone common in upper part; common botryoidal quartz nodules, ripples, dessication cracks, evaporite moulds and casts.|
11103|Mallapunyah Formation|67352|4|Described|p14 Tb.2, p58|Statherian|Statherian|McArthur Basin. Hosts copper ore at Kilgour Crossing. 450m thick.||Umbolooga Subgroup||Overlies (conformably) Masterton Sandstone. Overlain (conformably) by Amelia Dolostone.|Dolomitic siltstone and mudstone, dolomudstone, shale, sandstone, dolostone, chert; minor conglomerate.|
11103|Mallapunyah Formation|69430|4|Described|p15:3, 17, 22, 34, 55|Statherian|Statherian|Southern McArthur Basin. 100-c.450m thick. Continental and coastal sabkha deposits. Mainly recessive. Hosts several iron occurrences in the Tawallah Pocket area.||Umbolooga Subgroup.||Conformably and gradationally overlies Masterton Sandstone. Is overlain conformably by Amelia Dolostone.|Red to purple, dolomitic cross-bedded sandstone interbeds; stromatolitic dolostone, more prevalent in the upper part of the unit; common botryoidal quartz nodules (cauliflower chert), ripples, dessication cracks, gypsum and halite casts and moulds.|12-JUL-16
11103|Mallapunyah Formation|69673|6|Mentioned|p16 fig 13|||Batten Fault Zone||Umbolooga Subgroup||Overlies Masterton Sandstone, overlain by Amelia Dolostone||
11103|Mallapunyah Formation|71374|5|Briefly described|p6|||McArthur Basin.||||Conformably (transitional) overlies the Masterton Sandstone.||
11103|Mallapunyah Formation|71592|5|Briefly described|Appendix A.|||McArthur Basin.|1653+/-27 Ma (MDA: U-Pb zircon SHRIMP)||||Siltstone.|
11103|Mallapunyah Formation|72248|6|Mentioned|p147|||Of McArthur Basin.||Unit of Umbolooga Subgroup.||||
11103|Mallapunyah Formation|72373|6|Mentioned|p6,9,11|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin.||Of Umbolooga Subgroup.||||02-OCT-19
11103|Mallapunyah Formation|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Batten Fault Zone of the Southern McArthur Basin.||Umbolooga Subgroup||Overlies Masterton Sandstone and underlies Amelia Dolostone.||
11103|Mallapunyah Formation|72718|6|Mentioned|p7|||Southern McArthur Basin. Batten Fault Zone.||Umbolooga Sub-group, McArthur Group||Underlain by Masterton Sandstone. Overlain by Amelia Dolostone.||
11103|Mallapunyah Formation|72912|5|Briefly described|p5 Fig.3|Statherian|Statherian|Located in the Batten Fault Zone of the Southern McArthur Basin.||Umbolooga Subgroup||Overlies Masterton Sandstone and underlies Amelia Dolostone.||
11103|Mallapunyah Formation|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin, Isa Superbasin.||Umbolooga Subgroup, McArthur Group||Underlain by Masterton Sandstone. Overlain by Amelia Dolostone.||
11103|Mallapunyah Formation|73280|6|Mentioned|p1, p4-5, App.1A, App.1C|||McArthur Basin. Sampled for XRD mineralogy to investigate brittleness and Kubler indices [see report].||||||
11103|Mallapunyah Formation|73412|5|Briefly described|p2, 4, 8|||Southern McArthur Basin.|1653 +/- 17 Ma (MDA).|Umbolooga Subgroup.||Overlies Masterton Sandstone. Is overlain by Amelia Dolostone.||
11123|Malone Creek Granite|23363|5|Briefly described|351 Tab.1|||||||||
11123|Malone 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
11123|Malone Creek Granite|29599|6|Mentioned|p39|||||||||
11123|Malone Creek Granite|30830|5|Briefly described|p301|||||||||
11123|Malone Creek Granite|31347|6|Mentioned|p135|||||||||
11123|Malone Creek Granite|32660|5|Briefly described|Table 2|||||||||
11123|Malone Creek Granite|33278|6|Mentioned|Fig.7|||||||||
11123|Malone Creek Granite|34528|6|Mentioned|p18|||||||||14-NOV-06
11123|Malone Creek Granite|35061|6|Mentioned|p143|||||||||
11123|Malone Creek Granite|35140|6|Mentioned|p321|||||||||
11123|Malone Creek Granite|35465|6|Mentioned|Fig.1|||Geology of Pine Creek Geosyncline||||||
11123|Malone Creek Granite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
11123|Malone Creek Granite|40248|6|Mentioned|p222|||||||||
11123|Malone Creek Granite|41125|6|Mentioned|Fig.15|||||||||
11123|Malone Creek Granite|41397|4|Described|p18|||||||||
11123|Malone Creek Granite|41406|6|Mentioned|Map legend|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
11123|Malone Creek Granite|41407|6|Mentioned|Map legend|Proterozoic||||||||
11123|Malone Creek Granite|42324|5|Briefly described|p5|||||||||
11123|Malone Creek Granite|43624|6|Mentioned|p13|||Of Pine Creek Plutonic Complex.||||||
11123|Malone Creek Granite|43718|4|Described|Fig 1.1,p1,92|||||||||
11123|Malone Creek Granite|44399|5|Briefly described|map legend||Paleoproterozoic|Fine-grained granite.||||||07-NOV-08
11123|Malone Creek Granite|45022|4|Described|p.135||Carpentarian|On many pages.||||||31-OCT-06
11123|Malone Creek Granite|46658|6|Mentioned|p559|||||||||
11123|Malone Creek Granite|46678|6|Mentioned|p9|||Mount Evelyn, N.T., Sheet D.53/5. BMR 1:250,000 Geol.Ser.Explan.Notes.||||||
11123|Malone Creek Granite|46848|6|Mentioned|p167|||||||||
11123|Malone Creek Granite|47049|6|Mentioned|p237|||||||||
11123|Malone Creek Granite|48867|14|Not recorded|p.6,12,13,18,19||Paleoproterozoic|map. L.Proterozoic.; "a quartz-rich alkalic variety"; probably represents cupola from underlying Cullen Granite batholith.||||||07-NOV-08
11123|Malone Creek Granite|50545|5|Briefly described|p115||Orosirian|Age: 18320+/-8 Ma. Of Jim Jim Suite.||||||17-DEC-07
11123|Malone 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: 1823-1736 +/- 20Ma (Shrimp).||||||07-NOV-08
11123|Malone Creek Granite|60680|5|Briefly described|Map legend|Orosirian|Orosirian|Pink to greenish-pink, fine chloritised eveny grained alkali feldspar granite with abundant quartz and greisen veins.  Age: 1823Ma.||||||14-NOV-06
11123|Malone Creek Granite|63866|5|Briefly described|p110|Orosirian|Orosirian|Central Domain, Pine Creek Orogen.|1820 +/- 8 Ma (Page, OZCHRON)|David Suite||||
11123|Malone Creek Granite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Jim Jim Suite. Age 1823Ma SHRIMP U/Pb.  I-type. Pink to greenish-pink, fine chloritised evenly grained alkali feldspar granite with abundant quartz and greisen veins. Intrudes Burrell Creek Formation, Zamu Dolerite and El Sherana Group.||||||07-JAN-09
11123|Malone Creek Granite|65232|5|Briefly described|p60|||With Edith River Group described as late-tectonic volcanic rocks of South Alligator Mineral Field. See also Malone Granite.||||||09-FEB-10
11123|Malone Creek Granite|67564|3|Fully described|p7 Table 2, p17 Table 3, p27, p37, p85.|Paleoproterozoic|Paleoproterozoic|Eastern Pine Creek Orogen. Another SHRIMP U-Pb date gives 1808 +/- 20 Ma, while a biotite Rb-Sr date gives an age of 1736 +/- 5 Ma. Isolated pluton of 82 km2. Outcrops as a deeply dissected plateau.|1823 +/- 9 Ma (SHRIMP U - Pb zircon).|Unit in David Suite.||Intrudes Coronation Sandstone, Burrell Creek Formation, Zamu Dolerite and Pul Pul Rhyolite.|Three concentric gradational zones: inner fine to medium, slightly porphyritic alkali feldspar granite; fine to coarse, even-grained to porphyritic alkali feldspar granite; outer fine, even-grained, chloritised alkali feldspar granite.|
11123|Malone Creek Granite|69420|5|Briefly described|p5:17-18, 21, 23, 79|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Mineralogy and petrology/geochemistry summarised. Two other SHRIMP age determinations are given: 1808 +/- 20 Ma and 1736 +/- 5 Ma [!?].|1823 +/- 9 Ma: SHRIMP U-Pb zircon.|Jim Jim Suite.|||Porphyritic alkali-feldspar granite, equigranular medium-grained granite.|12-JUL-16
11123|Malone Creek Granite|70293|5|Briefly described|p597-599, p613|Orosirian|Orosirian||1823 +/- 9 Ma (OZCHRON).|||Intrudes Kurrundie Sandstone, Plum Tree Creek Volcanics||
11123|Malone Creek Granite|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|1808+/-20 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
11215|Manuka Subgroup|13516|6|Mentioned|p167 fig 10, p169 fig 11|Late Cretaceous|Late Cretaceous|Eromanga Basin.||Of Rolling Downs Group||||
11215|Manuka Subgroup|29591|6|Mentioned|p69|||||||||
11215|Manuka Subgroup|39445|6|Mentioned|Table 11|||||||||
11215|Manuka Subgroup|63979|5|Briefly described|p53|||Of Rolling Downs Group. Includes Mackunda and Winton Formations.||||||07-FEB-11
11215|Manuka Subgroup|69457|5|Briefly described|p41:6, 11-13|Early Cretaceous|Early Cretaceous|Vine et al. (1967). Eromanga Basin.||Rolling Downs Group.|Mackunda and Winton Formations.|Overlies Wilgunya and Marree Subgroups.||12-JUL-16
11215|Manuka Subgroup|69673|6|Mentioned|p156||||||Includes Mackunda Formation, Winton Formation|Overlies Wilgunya Subgroup||
11259|Marchinbar Sandstone|9534|5|Briefly described|Map legend||Cambrian|Of the Wessel Group.  Flaggy to massive thin-bedded sandstone.||||||07-JUL-04
11259|Marchinbar Sandstone|9691|5|Briefly described|Map Legend|||Of the Wessel Group. Flaggy to massive thin-bedded sandstone.||||||
11259|Marchinbar Sandstone|9701|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Wessel Group. Flaggy to massive thin-bedded sandstone.||||||02-JUN-05
11259|Marchinbar Sandstone|9733|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Wessel Group. Flaggy to massive thin bedded sandstone.||||||
11259|Marchinbar Sandstone|22600|4|Described|Map legend|Neoproterozoic|Neoproterozoic|||||||
11259|Marchinbar Sandstone|23374|3|Fully described|Tb3p22,20,21,27|Neoproterozoic|Neoproterozoic|Of the Wessel Group, Arafura Basin.||||||31-OCT-06
11259|Marchinbar Sandstone|24047|5|Briefly described|p11, p84|Neoproterozoic|Neoproterozoic|Of the Wessel Group.  Quartz sandstone.  Max. thickness: 240m.  Geological Province: Arafura Basin.  See also p86 Fig. 74.||||||
11259|Marchinbar Sandstone|24049|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Wessel Group. Sandstone: white, quartz-rich, fine to medium-grained, mostly medium-bedded, flat to trough cross-bedded, ripples. Geol. Prov: Arafura Basin.||||||13-OCT-05
11259|Marchinbar Sandstone|24442|6|Mentioned|p21|||||||||
11259|Marchinbar Sandstone|32660|5|Briefly described|Table 7|||||||||
11259|Marchinbar Sandstone|36535|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
11259|Marchinbar Sandstone|36635|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
11259|Marchinbar Sandstone|37815|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
11259|Marchinbar Sandstone|42058|5|Briefly described|p113|||||||||
11259|Marchinbar Sandstone|42597|5|Briefly described|Map Legend|Adelaidean||||||||
11259|Marchinbar Sandstone|43010|2|Defined|p180|Middle Cambrian|Early Cambrian|Of the Wessel Group.||||||31-OCT-06
11259|Marchinbar Sandstone|44112|4|Described|Table13p74,76,108|Neoproterozoic|Neoproterozoic|||||||12-MAY-06
11259|Marchinbar Sandstone|44338|14|Not recorded|p.7,opp.6|||Top fm of Wessel Group. (C53-14).||||||
11259|Marchinbar Sandstone|44339|14|Not recorded|map legend||Neoproterozoic|Upper Proterozoic, part of Wessel Group.||||||
11259|Marchinbar Sandstone|44475|2|Defined|p.8,9,opp.p.6, map|||(C53-15,16). See also Tb.1, for more details.||||||
11259|Marchinbar Sandstone|44476|14|Not recorded|map legend||Neoproterozoic|Upper Proterozoic.||||||
11259|Marchinbar Sandstone|46639|5|Briefly described|Map legend|Cambrian|Cambrian|Of the Wessel Group. Underlain by Raiwalla Shale. Flaggy to massive thin-bedded sandstone.||||||14-AUG-07
11259|Marchinbar Sandstone|46792|6|Mentioned|Fig.2|||||||||
11259|Marchinbar Sandstone|60550|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Wessel Group. Flaggy to massive thin-bedded sandstone.||||||
11259|Marchinbar Sandstone|60571|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of the Wessel Group. Sandstone: white, fine- to medium-grained, medium-bedded, horizontal planar laminations to planar cross-bedded. Geological Province: Arafura Basin.||||||30-NOV-04
11259|Marchinbar Sandstone|61403|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Wessel Group. Sandstone: white, quartz-rich, fine to medium-grained, mostly medium-bedded, flat to trough cross-bedded, ripples. Geol. Prov: Arafur a Basin.||||||
11259|Marchinbar Sandstone|62504|5|Briefly described|p2|Neoproterozoic|Neoproterozoic|Of the Wessel Group. Overlies: Raiwalla Shale. Underlies; Elcho Island Formation.||||||
11259|Marchinbar Sandstone|62505|4|Described|p3|Neoproterozoic|Neoproterozoic|Of the Wessel Group. Underlies: Elcho Island Formation. Overlies: Raiwalla Shale.||||||
11259|Marchinbar Sandstone|62788|5|Briefly described|p104.|Neoproterozoic|Neoproterozoic|Arafura Basin.||Of the Wessel Group.||Overlies Raiwalla Shale and underlies Elcho Island Formation.||03-DEC-12
11259|Marchinbar Sandstone|63062|5|Briefly described|p11|||Of the Wessel Group. Geological Province: Arafura and Money Shoal Basins.||||||07-FEB-11
11259|Marchinbar Sandstone|69418|6|Mentioned|p3:28|||Arafura Basin. Hosts several residual-type bauxite deposits (described).||||||12-JUL-16
11259|Marchinbar Sandstone|69437|6|Mentioned|p22:4-5|Ediacaran|Ediacaran|Arafura Basin.||||||12-JUL-16
11259|Marchinbar Sandstone|69451|3|Fully described|p35:3-6, 11-12|Neoproterozoic|Neoproterozoic|Plumb and Roberts (1992), who nominated a reference section on Marchinbar Island in WESSEL ISLANDS map area. Arafura Basin. Relatively high-energy, very shallow-marine deposits. 300m thick (onshore). Generally poor outcrop. No metazoan or trace fossils have been found. Age from stratigraphic position. Hosts significant bauxite deposits on Marchinbar and Elcho Islands.||Wessel Group.||Conformably and gradationally overlies Raiwalla Shale. Is overlain by Elcho Island Formation locally disconformably or possibly conformably.|Clean, white, quartz-rich, fine- to medium-grained sandstone, mostly medium bedded, with horizontal laminations, trough cross-beds, wave and current ripples, rare dessication cracks.|12-JUL-16
11259|Marchinbar Sandstone|69673|5|Briefly described|p195, p196|||estimated 300m thick.||Wessel Group|||Quartz sandstone.|
11259|Marchinbar Sandstone|73083|6|Mentioned|p28, p33|Neoproterozoic|Neoproterozoic|||||||
11259|Marchinbar Sandstone|73086|6|Mentioned|p133|||Arafura Basin.||||Correlates to Julie Formation.||
11295|Margaret Granite|23337|5|Briefly described|906 Fig.9|||||||||
11295|Margaret Granite|23714|4|Described|p27|||See also page 19 Table 4. Geological Province: Cullen Batholith.||||||
11295|Margaret Granite|23715|5|Briefly described|Map legend||Proterozoic|Predominantly I-type. In the Cullen Batholith, of the Rum Jungle and Central Regions.||||||
11295|Margaret Granite|24197|5|Briefly described|p106 Tb. 15.1|Paleoproterozoic|Paleoproterozoic|Of the Cullen Supersuite. Age: ~1825Ma. Geological Province: Pine Creek Inlier.||||||07-FEB-11
11295|Margaret Granite|24260|6|Mentioned|p1013 Fig.1|||Geological Province: Pine Creek Inlier.||||||06-AUG-08
11295|Margaret Granite|33278|6|Mentioned|Fig.7|||||||||
11295|Margaret Granite|35061|6|Mentioned|p143|||||||||
11295|Margaret Granite|35465|6|Mentioned|p59|||||||||
11295|Margaret Granite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
11295|Margaret Granite|40223|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Coarse porphyritic granite.||||||07-NOV-08
11295|Margaret Granite|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
11295|Margaret Granite|41309|4|Described|p9|||||||||
11295|Margaret Granite|41465|6|Mentioned|p8|||||||||
11295|Margaret Granite|42756|6|Mentioned|Fig.5 P6|||||||||
11295|Margaret Granite|42927|5|Briefly described|p428|||see also Fig.2 p430.||||||02-NOV-06
11295|Margaret Granite|43140|3|Fully described|p25||Paleoproterozoic|Of Cullen Batholith.||||||07-NOV-08
11295|Margaret Granite|43624|6|Mentioned|p10|||||||||
11295|Margaret Granite|43832|4|Described|Tb8 p42;46,49,55,65||Paleoproterozoic|Age 1860+-45 Ma; less accurate ages of 1784+-8 and 1780+-20 Ma (p53).||||||07-NOV-08
11295|Margaret Granite|44950|14|Not recorded|Not recorded|||||||||
11295|Margaret Granite|45022|3|Fully described|p.140,141||Carpentarian|On many pages.||||||02-NOV-06
11295|Margaret Granite|46658|6|Mentioned|p559|||||||||
11295|Margaret Granite|46675|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Coarse porphyritic adamellite.  Intrudes the Mount Partridge, South Alligator and Finniss River Groups.||||||07-NOV-08
11295|Margaret Granite|46676|14|Not recorded|p.9|||||||||
11295|Margaret Granite|50586|5|Briefly described|p1.1, 4.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Of the Cullen Supersuite. Age: 1860 +/- 25Ma (U-Pb).||||||07-NOV-08
11295|Margaret Granite|63866|5|Briefly described|p110|Orosirian|Orosirian|Central Domain, Pine Creek Orogen.|1860 +/- 45 Ma (ID-TIMS)|Cullen Supersuite||||
11295|Margaret Granite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1820-1850Ma. Of Cullen Supersuite.  I-type. Coarse porphyritic biotite granite||||||
11295|Margaret Granite|67564|6|Mentioned|p33 Fig.19.|Paleoproterozoic|Paleoproterozoic|Pluton within Cullen Batholith, Pine Creek Orogen.||||||
11295|Margaret Granite|69420|5|Briefly described|p5:17-18, 20|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Granite-dominated plutons; mineralogy and petrology/geochemistry summarised.|1860 +/- 25 Ma conventional U-Pb zircon (TIMS).|Margaret Suite.|||Medium- to coarse-grained porphyritic to equigranular quartz monzonite. I-type.|12-JUL-16
11295|Margaret Granite|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.|1860 +/- 25 Ma.||||Light grey to pink, medium- to coarse-grained, porphyritic to equigranular biotite-hornblende granite.|
11295|Margaret Granite|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|1860+/-45 Ma (crystallisation: U-Pb).||||Granite.|
11296|Margaret Hill Conglomerate|22538|6|Mentioned|Fig3 P708|||||||||
11296|Margaret Hill Conglomerate|23216|5|Briefly described|Fig5p20,25,30-1|||||||||
11296|Margaret Hill Conglomerate|23396|5|Briefly described|p 407 fig.2|||Of Mount Rigg Group||||||02-NOV-06
11296|Margaret Hill Conglomerate|32660|5|Briefly described|Table 4|||||||||
11296|Margaret Hill Conglomerate|43010|6|Mentioned|p106|||Also p140. Of Mount Rigg Group.||||||
11296|Margaret Hill Conglomerate|43149|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of Mount Rigg Group.Of Calymmian or Statherian age.||||||07-NOV-08
11296|Margaret Hill Conglomerate|44112|6|Mentioned|p67|||||||||
11296|Margaret Hill Conglomerate|44201|14|Not recorded|p.9||Neoproterozoic|U.Proterozoic.||||||
11296|Margaret Hill Conglomerate|44471|14|Not recorded|opp.7|||(D53-10).||||||
11296|Margaret Hill Conglomerate|45022|3|Fully described|p.75.||Carpentarian|Of Mount Rigg Group. Of many pages.||||||
11296|Margaret Hill Conglomerate|45162|6|Mentioned|Fig.152|||||||||
11296|Margaret Hill Conglomerate|46679|14|Not recorded|map legend||Neoproterozoic|Upper Proterozoic.||||||
11296|Margaret Hill Conglomerate|64817|6|Mentioned|p353 Fig.4 |||||Of the Mount Rigg Group.||||
11296|Margaret Hill Conglomerate|69430|4|Described|p15:3, 24-25, 30|||NW McArthur Basin. 0-300m thick. High-energy alluvial fan or proximal braided stream deposits.||Mount Rigg Group.||Unconformably overlies West Branch Volcanics. Is overlain conformably by Bone Creek Sandstone.|Thickly to very thickly bedded polymictic pebble, cobble and boulder conglomerate; purple lithic sandstone and granule conglomerate.|12-JUL-16
11296|Margaret Hill Conglomerate|69673|6|Mentioned|p16 fig 13|Paleoproterozoic|Paleoproterozoic|Northwestern McArthur Basin.||Mount Rigg Group||Overlain by Bone Creek Sandstone||
11378|Marshall Granite|9394|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block.||||||
11378|Marshall Granite|9694|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block. Hornblende granite, leucogranite, aplite.||||||
11378|Marshall Granite|22524|6|Mentioned|p41,p42|||||||||
11378|Marshall Granite|23732|5|Briefly described|p10, p24 Fig.23|Paleoproterozoic|Paleoproterozoic|Intrudes Deep Bore Metamorphics. Weakly foliated to massive hornblende granite.  Geological Province: Arunta Province.||||||07-NOV-08
11378|Marshall Granite|23868|5|Briefly described|p741 Fig. 2, p742|||Intrudes Deep Bore Metamorphics.  Geological Province: Arunta Inlier.||||||21-SEP-09
11378|Marshall Granite|24047|6|Mentioned|p105 Appendix 1|||Geological Province: Arunta province.||||||
11378|Marshall Granite|24197|5|Briefly described|p60 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Of the Alarinjela Suite. Age: ?1713Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
11378|Marshall Granite|40538|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Hornblende granite, slightly foliated, pink. Geological Province: Arunta Block.||||||07-NOV-08
11378|Marshall Granite|40906|4|Described|p12|||Mention p11.||||||02-NOV-06
11378|Marshall Granite|44327|14|Not recorded|Tb.I,p.6,map||Paleoproterozoic|(F53-11). Lower Proterozoic.||||||07-NOV-08
11378|Marshall Granite|44328|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
11378|Marshall Granite|46868|6|Mentioned|Fig.2|||||||||
11378|Marshall Granite|48844|2|Defined|p.11,13-15|||(New name). (F53-11). Pls. 2,8,17,25.||||||
11378|Marshall Granite|49036|6|Mentioned|p7|||||||||
11378|Marshall Granite|50369|5|Briefly described|p1.4, 16.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Alarinjela Suite.||||||07-NOV-08
11378|Marshall Granite|62595|5|Briefly described|p7, p13.|||Includes metasedimentary rafts which host the Molyhil Mo-W skarn deposit.|||||Medium-grained biotite granite that has been chloritised and sericitised along the S walls, and K-feldspar altered along the N and W walls, of the Molyhil open cut.|
11378|Marshall Granite|64068|6|Mentioned|p46|||||||Overlain nonconformably by Oorabra Arkose.||05-APR-12
11378|Marshall Granite|68150|5|Briefly described|p.vi Tb.i, p32-35|||On 100K mapsheet: DNEIPER 5952. Sample description: weakly foliated to massive, pink, medium-grained biotite-hornblende granite, containing pink K-feldspar, quartz, yellow-orange plagioclase and dark brown hornblende, with rare biotite and epidote; dykes and veins of aplite, pegmatite and quartz are common.|1791 +/- 3 Ma, igneous crystallis'n, SHRIMP Pb/Pb|||intrudes Cackleberry Metamorphics and Deep Bore Metamorphics|foliated biotite monzogranite|
11378|Marshall Granite|69227|6|Mentioned|p266|||||||||
11378|Marshall Granite|69418|6|Mentioned|p3:21|||Arunta Region. Hosts the Molyhil W-Mo skarn deposit (described).||||||12-JUL-16
11378|Marshall Granite|69427|5|Briefly described|p12:30, 40, 62|||Smith (1964). Aileron Province. Included in a group of 1730-1710 Ma granites, but was geochemically grouped with the 1771 Ma Dneiper Granite by Zhao and McCulloch (1995). Hosts the Molyhil Mo-W deposit (described in some detail) in metasedimentary rafts.|||||Weakly foliated hornblende granite, with lesser leucogranite, aplite and microgranite.|12-JUL-16
11378|Marshall Granite|69931|6|Mentioned|p269|Paleoproterozoic|Paleoproterozoic|Arunta Inlier. Presented as Marshall granite.||Dneiper suite.||||
11378|Marshall Granite|71592|5|Briefly described|Appendix A.|||Arunta Orogen.|1791+/-3 Ma (U-Pb zircon SHRIMP)||||Monzogranite.|
11378|Marshall Granite|71750|4|Described|p13,17|Statherian|Statherian|Geological province: Aileron Province. Emplacement age 1723+\-12 Ma (LA-ICP-MS zircon U-Pb; Beyer et al in prep), synchronous with Deep Bore Metamorphic zircon rim growth.||||Intrudes into Deep Bore Metamorphics.|Massive to weakly foliated hornblende-bearing granite.|20-NOV-22
11378|Marshall Granite|71839|4|Described|iii, p1, p21-22, p26-p29|Statherian|Statherian|Exposed in the pit wall of the Molyhil W-Mo deposit in central JINKA. 1720 +/- 18 Ma Pb-Pb is interpreted as the minimum magmatic crystallisation age of this unit. Interpreted to be derived from protolith of the Dinkum Orthogneiss. Sampling location and description there are described, additionally zircon morphology, U-Pb analyses and results are also provided.|1723 +/- 12 Ma (Beyer et al, in prep)|||Intrudes the Deep Bore Metamorphics.|Granite and aplite dykes.|21-MAR-23
11378|Marshall Granite|72367|5|Briefly described|p21,27|Statherian|Statherian|Geological province: Aileron Province. Considered to have formed from extensive partial melting of metasedimentary-metaigneous rocks in the Deep Bore Domain, and subsequently accummulation of generated melt. Beyer et al (in prep) recorded Pb/Pb age of 1723+\-12 Ma as an igneous crystallisation age.|1723+\-12 Ma (crystallisation)|||||
11378|Marshall Granite|72370|6|Mentioned|p29|||Geological province: Aileron Province. Part of a suite of granites emplaced in HUCKITTA map sheet at c. 1725-1715 Ma (along with Mount Swan Granite, Jinka Granite) (Hollis et al 2010, Weisheit et al in review, Beyer et al in prep).||||||
11378|Marshall Granite|72372|5|Briefly described|p24|Statherian|Statherian|Geological province: Aileron Province. Felsic magmatism in the NE Aileron Province, post-dating D2 and D3 deformation in the Bonya Hills area and associated with epigenetic mineralisation. Yields magmatic crystallisation zircon age of 1723+\-12 Ma (Beyer et al in prep).|1723+\-12 Ma (magmatic)|||||
11378|Marshall Granite|72711|6|Mentioned|p6|||Hosts rafts of Deep Bore Metamorphics.||||||
11378|Marshall Granite|72717|6|Mentioned|p5, p10|||Aileron Province. Variably deformed. Variably gneissic to mylonitic. Mylonitic version has a near-identical appearance to Dinkum Orthogneiss.||||||
11378|Marshall Granite|73123|5|Briefly described|piii, p5, p8, p10, p13|Statherian|Statherian|May include leucogranite and quartz-feldspar veins that cross-cut foliation in the Bacardi Granite [indicating relative timing postdating metamorphism]. These plutons are a product of extensive partial melting of the Deep Bore Domain; thus, emplacement age is interpreted to record cooling of the domain below solidus temperatures. Widespread and intimately associated with the Narbarloo Granite throughout the eastern Mopunga Range.|1720 +/- 18 Ma|||Intrudes Black Label Suite, Yam Gneiss and Narbarloo Granite.|Felsic intrusives.|
11378|Marshall Granite|73128|5|Briefly described|piii, p5-6, p8, p10|Statherian|Statherian|Aileron Province. Widespread plutons throughout the Deep Bore Domain. Geochron is concordia crystallisation age obtained from LA-ICP-MS apatite dating of a sample of brecciated and calcite-quartz-fluorite veined fine-grained K-feldspar-quartz granite (GA Sample ID: 2003087854U at Molyhil tungsten-molybdenum deposit). Matches previous age of 1720 +/- 18 Ma [zircon U-Pb?]. Resulted from extensive partial melting during the ca 1787-1717 Ma metamorphic cycle. Can include xenoliths of the Deep Bore Metamorphics and Yam Gneiss. Skarn-alteration and mineralisation at Molyhil deposit is associated with intrusion of this unit.|1732 +/- 8 Ma|||Intrudes Deep Bore Metamorphics and Yam Gneiss.||
11378|Marshall Granite|73551|6|Mentioned|p11-15|Statherian|Statherian|Intrusion is associated with alteration and mineralisation at the Molyhil deposit. A zircon igneous crystallisation age of 1720 +/- 18 Ma was reported by Kositcin et al. (2018).|1720 +/- 18 Ma|||Intrudes the Deep Bore Metamorphics and Yam Gneiss.||
11378|Marshall Granite|73591|4|Described|piii, p2, p11, p14-16, p29-30, p36, p40|||Aileron Province. Outcrops in the Mopunga Range. Derived from partial melting of the Dinkum Orthogneiss. Main body is crosscut by late phase dykes. Metamic zircons did not yield a magmatic age. An apatite LA-ICP-MS age of 1732 +/- 8 Ma at the Molyhil W-Mo deposit is interpreted to record timing of granite crystallisation (Reno et al 2021). Analysed for Lu-Hf isotopes. Outcrop 4.8 km south of Elkera No.2 Bore in eastern Dneiper (low blocky hill in the Mopunga Range) was previously interpreted as Marshall Granite but reinterpreted as Narboarloo Granite based on composition.|1732 +/- 8 Ma apatite LA-ICP-MS|Sainthill Suite||Cross-cuts Dinkum Orthogneiss and Deep Bore Metamorphics. Intrudes Narbarloo Granite.|Distinctive pink-coloured granite.|
11401|Marura Siltstone|22538|6|Mentioned|Fig3 P708|||||||||
11401|Marura Siltstone|22600|4|Described|Map legend|Statherian|Statherian|||||||
11401|Marura Siltstone|24048|4|Described|p49|||Of the Parsons Range Group.  Overlain by Fleming Sandstone; underlain by Badalngarrmirri Formation.  Max. thickness: 250m.  Geological Province: McArthur Basin.||||||02-NOV-06
11401|Marura Siltstone|24049|5|Briefly described|Map Legend|Statherian|Statherian|Of Parsons Range Group. Siltstone: thin to thick-bedded, laminated to massive; thin to medium interbeds of dolomitic siltstone, sandstone and dolostone; dessication cracks and halite casts; stromatolitic chert bed near base. Geol. Prov: McArthur Basin.||||||11-OCT-05
11401|Marura Siltstone|32660|5|Briefly described|Table 4|||||||||
11401|Marura Siltstone|42597|5|Briefly described|Map Legend|Carpentarian||||||||
11401|Marura Siltstone|43010|2|Defined|p89||Paleoproterozoic|Of Parsons Range Group. Of Statherian age.||||||07-NOV-08
11401|Marura Siltstone|44112|4|Described|p49,52|||Contacts presummed conformable or faulted but neither exposed||||||
11401|Marura Siltstone|44299|4|Described|p.11||Paleoproterozoic|SD/53-7,8. L.Proterozoic. Table 1.||||||07-NOV-08
11401|Marura Siltstone|44300|14|Not recorded|map legend||Paleoproterozoic|SD/53-7,8. L.Proterozoic.||||||07-NOV-08
11401|Marura Siltstone|61403|5|Briefly described|Map Legend|Statherian|Statherian|Of Parsons Range Group. Siltstone: thin to thick-bedded, laminated to massive; thin to medium interbeds of dolomitic siltstone, sandstone and doloston e; dessication cracks and halite casts; stromatolitic chert bed near base. Geol. Prov: McArthur Basin.||||||
11401|Marura Siltstone|64817|6|Mentioned|p353 Fig.4 |||||Unit in Parsons Range Group.||||
11401|Marura Siltstone|69430|4|Described|p15:3, 13-14|Statherian|Statherian|Walker Fault Zone, northern McArthur Basin. 100-250m thick. Supratidal mudflats, sabkha deposits. A silicified dolostone bed near the base shows selective silicification of small columnar stromatolites.||Parsons Range Group.||Overlies Badalngarrmirri Formation presumably conformably. Is overlain conformably by Fleming Sandstone.|Grey, green and purple, laminated to massive mudstone and siltstone; dololutite and sandstone interbeds; stromatolitic chert near base.|12-JUL-16
11401|Marura Siltstone|69673|6|Mentioned|p16 fig 13|||||||Overlain by Fleming Sandstone, overlies Badalingarrmirri Formation||
11438|Masson Formation|9534|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Namoona Group.  Quartz greywacke, carbonaceous siltstone, calcareous siltstone, conglomerate, limestone.  Intruded by part of the Zamu Dolerite.||||||07-NOV-08
11438|Masson Formation|9691|5|Briefly described|Map Legend|||Of the Namoona Group. Quartz greywacke, carbonaceous siltstone, calcareous siltstone, conglomerate, limestone.||||||
11438|Masson Formation|9701|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Namoona Group. Quartz greywacke, carbonaceous siltstone, calcareous siltstone, conglomerate, limestone.||||||02-JUN-05
11438|Masson Formation|9733|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Quartz greywacke, carbonaceous/calcareous siltstone, conglomerate.||||||
11438|Masson Formation|22479|5|Briefly described|fig1p2|||||||||
11438|Masson Formation|22810|5|Briefly described|Table2 p5, p13|||Maximum thickness 3000m, correlates with lower member of Cahill Formation.||||||02-NOV-06
11438|Masson Formation|23714|4|Described|p11|Proterozoic|Proterozoic|See also page 8 Table 1. Of Namoona Group.  Max. thickness: 1000 m.||||||
11438|Masson Formation|23715|5|Briefly described|Map legend||Proterozoic|Of the Namoona Group, in the  Central Region.||||||02-NOV-06
11438|Masson Formation|23733|5|Briefly described|p32 Fig. 19|||Of Namoona Group.||||||
11438|Masson Formation|24047|5|Briefly described|p5 Fig.4|Paleoproterozoic|Paleoproterozoic|Of Namoona Group.  Shale siltstone, quartzite, dolomite.  Geological Province: Pine Creek Orogen.  See also p30-31, p41 Fig. 36.||||||07-NOV-08
11438|Masson Formation|24442|6|Mentioned|p27|||||||||
11438|Masson Formation|29599|5|Briefly described|p30|||||||||
11438|Masson Formation|30317|5|Briefly described|p952|||||||||
11438|Masson Formation|30830|5|Briefly described|p301|||||||||
11438|Masson Formation|30831|6|Mentioned|p1|||||||||
11438|Masson Formation|31347|6|Mentioned|p135|||||||||
11438|Masson Formation|31435|6|Mentioned|p62|||||||||
11438|Masson Formation|32397|6|Mentioned|p397|||Oldest shale in Uranium field||||||
11438|Masson Formation|32660|5|Briefly described|Table 2|||||||||
11438|Masson Formation|32873|5|Briefly described|p36|||Lithology. See also Fig.1||||||
11438|Masson Formation|32875|6|Mentioned|Fig.2|||||||||
11438|Masson Formation|32958|5|Briefly described|p953|||||||||
11438|Masson Formation|32959|6|Mentioned|p3|||||||||
11438|Masson Formation|33186|4|Described|p287|||||||||
11438|Masson Formation|33278|6|Mentioned|Fig.1|||||||||
11438|Masson Formation|34528|6|Mentioned|p18|||Lower Proterozoic. See P19||||||
11438|Masson Formation|35140|6|Mentioned|Fig.2|||||||||
11438|Masson Formation|35247|6|Mentioned|Fig.2|||||||||
11438|Masson Formation|35465|6|Mentioned|Fig.2|||Summary of positions of magnetic units in the Lower Proterozoic||||||
11438|Masson Formation|36085|6|Mentioned|Fig.7|||||||||
11438|Masson Formation|36535|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
11438|Masson Formation|36635|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
11438|Masson Formation|37462|6|Mentioned|Fig.4.8|||||||||
11438|Masson Formation|37579|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Namoona Group. Shale (probably carbonaceous at depth), fine to coarse calcareous and volcanic quartz greywacke, dolarenite, sandstone, dolomite.||||||07-NOV-08
11438|Masson Formation|37815|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
11438|Masson Formation|38239|6|Mentioned|Fig.2|||||||||
11438|Masson Formation|38349|6|Mentioned|Table 4|||||||||
11438|Masson Formation|38351|6|Mentioned|Table 3|||||||||
11438|Masson Formation|38557|5|Briefly described|p287|||||||||
11438|Masson Formation|38884|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
11438|Masson Formation|39069|5|Briefly described|Table 1|||||||||
11438|Masson Formation|39117|6|Mentioned|p137|||||||||
11438|Masson Formation|39357|4|Described|p3|||||||||
11438|Masson Formation|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
11438|Masson Formation|40168|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Namoona Group. Carbonaceous phyllite, slate, silty phyllite, siltstone, sandy siltstone, minor laminated medium to coarse grey quartzite and feldspathic quartzite, and massive ironstone.||||||07-NOV-08
11438|Masson Formation|40223|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Namoona Group. Brown micaceous and carbonaceous siltstone, sandy siltstone, slate and phyllite, minor quartzite and rare calc-silicate hornfels.||||||07-NOV-08
11438|Masson Formation|40243|6|Mentioned|Fig.2|||||||||
11438|Masson Formation|40248|6|Mentioned|p221|||||||||
11438|Masson Formation|40493|5|Briefly described|Table 1|||||||||
11438|Masson Formation|40808|6|Mentioned|p12|||||||||
11438|Masson Formation|40823|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
11438|Masson Formation|40852|6|Mentioned|Fig.3.2|||||||||
11438|Masson Formation|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
11438|Masson Formation|41125|6|Mentioned|p26|||||||||
11438|Masson Formation|41309|4|Described|p3|||||||||
11438|Masson Formation|41311|4|Described|p5|||||||||
11438|Masson Formation|41397|4|Described|p7|||||||||
11438|Masson Formation|41407|6|Mentioned|Map legend|Proterozoic||||||||
11438|Masson Formation|41594|6|Mentioned|p22|||||||||
11438|Masson Formation|42190|6|Mentioned|p282|||||||||
11438|Masson Formation|43140|4|Described|p2||Paleoproterozoic|Of Namoona Group.||||||07-NOV-08
11438|Masson Formation|43187|5|Briefly described|p2|||||||||
11438|Masson Formation|43624|6|Mentioned|p8|||Of Namoona Group.||||||
11438|Masson Formation|43718|6|Mentioned|p28|||||||||
11438|Masson Formation|43720|5|Briefly described|p5|||||||||
11438|Masson Formation|43832|3|Fully described|11-14, 97||Paleoproterozoic|Maximum age: 2000 Ma.  Part of Namoona Group, overlain by Stag Creek Volcanics.||||||07-NOV-08
11438|Masson Formation|44314|2|Defined|p.5,8,10,11,14,map|||(D52-4). Darwin Sheet. Tb.1. pp.6-7||||||
11438|Masson Formation|44315|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
11438|Masson Formation|44399|5|Briefly described|map legend||Paleoproterozoic|Of the Goodparla Group.  Contains the Coirwong Greywacke Member.  Quartz greywacke, carbonaceous siltstone, calcareous siltstone, conglomerate.||||||07-NOV-08
11438|Masson Formation|45022|3|Fully described|p.31||Paleoproterozoic|On many pages.||||||07-NOV-08
11438|Masson Formation|45146|3|Fully described|Table 1|||See also p5.||||||21-SEP-06
11438|Masson Formation|46163|14|Not recorded|p.168-171,173-4|||||||||
11438|Masson Formation|46658|6|Mentioned|p549|||||||||
11438|Masson Formation|46676|14|Not recorded|p.6||Paleoproterozoic|L.Proterozoic; unit of Goodparla Group.||||||07-NOV-08
11438|Masson Formation|46678|5|Briefly described|Table 1|Proterozoic|Proterozoic|Of Goodparla Group.  Quartz, greywacke, siltstone, carbonaceous siltstone, inplaces pyritic and in places with silicified dolomite bands.  Max. thickness: 10,000 feet.||||||
11438|Masson Formation|46700|5|Briefly described|P14, Table1 P12||Proterozoic|||||||
11438|Masson Formation|46848|5|Briefly described|p167|||||||||
11438|Masson Formation|46877|6|Mentioned|Fig.1|||||||||
11438|Masson Formation|47049|6|Mentioned|Fig.2|||||||||
11438|Masson Formation|48866|14|Not recorded|p.3|||(D52-4,8).||||||
11438|Masson Formation|48981|6|Mentioned|Plate 1|||||||||
11438|Masson Formation|48982|5|Briefly described|p3|||||||||
11438|Masson Formation|49744|5|Briefly described|Fig.13 last page|||||||||
11438|Masson Formation|50586|6|Mentioned|p4.5|||Intruded by Cullen Supersuite.||||||
11438|Masson Formation|60550|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Namoona Group. Quartz greywacke, carbonaceous siltstone, calcareous siltstone, conglomerate, limestone.||||||
11438|Masson Formation|60680|5|Briefly described|Map legend|Rhyacian|Rhyacian|Of the Namoona Group.  Geological Province: Pine Creek Orogen. Carbonaceous-pyritic and dolomitic slate, phyllite and schist; carbonaceous pyritic doloutite; medium to coarse quartz meta-arenite.||||||16-JUN-05
11438|Masson Formation|62375|5|Briefly described|p10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of the Namoona Group. Geological Province: Pine Creek Orogen.||||||09-FEB-10
11438|Masson Formation|62378|5|Briefly described|p5, 16|||Geological Province: Pine Creek Orogen. Altered rhyolite tuff.||||||
11438|Masson Formation|64698|4|Described|lithinterp table|Orosirian|Paleoproterozoic|Age ~2050-2500Ma. Of Namoona Group. Max thick. 3000m. Carbonaceous-pyritic and dolomitic slate, phyllite, schist, dololutite; med/coarse quartz meta-arenite, coarse/very coarse, poorly sorted feldspathic-quartz metagreywacke, fine/coarse dolarenite.||||||07-JAN-09
11438|Masson Formation|64730|5|Briefly described|p125 Fig. 3|Paleoproterozoic|Paleoproterozoic|Age from the deposition age of conformably overlying Stag Creek Volcanics.|Min. deposition age 2021 +/- 10 Ma.|Of Namoona Group.||Conformably underlies Stag Creek Volcanics.||02-MAY-12
11438|Masson Formation|64956|5|Briefly described|p69|||Of the Namoona Group. Conformably overlies Stag Creek Volcanics.||||||07-FEB-11
11438|Masson Formation|65232|5|Briefly described|p45, p6 Fig. 5, p50, p65, App. 2|Palaeoproterozoic|Palaeoproterozoic|Base of Namoona Group. Underlies Stag Creek Volcanics. Shale, siltstone, quartzite, dolomite/dolostone. Hornfelsed adjacent to granite contact. Uranium mineralisation in tuffaceous shale at top of unit.||||||09-FEB-10
11438|Masson Formation|65339|6|Mentioned|p7.|||Correlated with Beestons Formation to the west.||||||
11438|Masson Formation|67355|5|Briefly described|p6, p7 Tb.2, p10, p35||Paleoproterozoic|The stratabound Namoona deposit (Zn-Pb-Ag) is hosted within carbonaceous pyritic shale of the Formation.||?Goodparla Group, Woodcutters Supergroup.|Acacia Gap Tongue.|Correlative to Beestons Formation and Celia Dolostone.||25-JAN-17
11438|Masson Formation|67564|3|Fully described|p8 Table 2, p9 Fig.4, p11, pp13-14.|Paleoproterozoic|Paleoproterozoic|Correlative of Beestons Formation and lower parts of Cahill Formation. >2800 m of mainly shallow marine (sub-wavebase) deposits. Outcrops as low, NW-trending strike ridges and rubbly rises. The Nimbuwah Event deformed and thrust this unit against Wildman Siltstone and Koolpin Formation. Hosts hydrothermal U vein deposits and stratabound Pb-Zn-Ag.|>2050 Ma (SHRIMP U-Pb zircon).|Unit in Namoona Group.||Is intruded by Minglo Granite and Goodparla Dolerite. Is overlain conformably by Stag Creek Volcanics and unconformably by Mundogie Sandstone, Edith River Group, or Petrel Formation.|Carbonaceous-pyritic and dolomitic slate, phyllite, schist and mudstone; meta-arenite; metagreywacke; quartzic intraclast dolostone; dolostone and marble; minor mafic volcaniclastic slate and rhyolitic tuff.|
11438|Masson Formation|67779|5|Briefly described|p6 Fig.5.|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen.||Unit in Namoona Group.||||
11438|Masson Formation|69418|6|Mentioned|p3:17|||Pine Creek Orogen. Hosts the Dam and Twin (Cleo) vein-type U deposit (described).||||||12-JUL-16
11438|Masson Formation|69420|4|Described|p5:4, 6, 8-9, 14, 16, 60, 65, 67, 79, 83|Paleoproterozoic|Paleoproterozoic|See also 86, 110, 112. South Alligator and central regions, Central Domain, Pine Creek Orogen. Up to 2800m thick. Mainly shallow-marine (sub-wavebase) deposits. Hosts the Dam and the Twin uranium deposits, and the George Creek Zn-Pb deposit. Also hosts the Frances Creek East iron ore deposit.||Namoona Group.||Is overlain conformably by Stag Creek Volcanics. Is intruded by Goodparla Dolerite.|Carbonaceous-pyritic and dolomitic shale, carbonaceous pyritic dolomudstone, quartz sandstone, feldspathic-quartz greywacke, dolostone, marble, minor mafic volcaniclastic shale and rhyolitic tuff.|12-JUL-16
11438|Masson Formation|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||Namoona Group.||Unconformably overlies Rum Jungle Complex. Is overlain unconformably by Mount Partridge Group.|Red-brown, carbonaceous-pyritic and dolomitic slate, phyllite and schist; carbonaceous pyritic dolomudstone; quartz metasandstone; coarse- to very coarse-grained poorly sorted feldspathic-quartz metagreywacke; dolograinstone.|
11438|Masson Formation|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|2400+/-110 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
11438|Masson Formation|73083|6|Mentioned|p5-6|||Rocks that compose a dome structure in the Alligator River 1:250K Sheet (SW) were reassigned to this unit from the Wildman Siltstone.||||Overlain by Mundogie Sandstone. Underlain by Nanambu Complex.|Greywacke, siltstone, conglomerate, and limestone.|
11455|Mattamurta Sandstone|22538|6|Mentioned|Fig3 P708|||||||||
11455|Mattamurta Sandstone|22600|4|Described|Map legend|Statherian|Statherian|||||||
11455|Mattamurta Sandstone|24048|3|Fully described|p38|||Of Parsons Range Group.  Max. thickness: 3000m.  Geological Province: McArthur Basin.||||||02-NOV-06
11455|Mattamurta Sandstone|24049|5|Briefly described|Map Legend|Statherian|Statherian|Of Parsons Range Group. Quartz  sandstone: medium to very thick-bedded, fine to coarse-grained, with granule-rich laminae and scattered pebbles; cross-bedding and ripples; local porphyritic K-feldspar-quartz rhyolite near base. Geol. Prov: McArthur Basin.||||||12-OCT-05
11455|Mattamurta Sandstone|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Of Parsons Range Group. Overlain by Badalngarrmirri Formation. Geological Province: Northern McArthur Basin.||||||
11455|Mattamurta Sandstone|32660|5|Briefly described|Table 4|||||||||
11455|Mattamurta Sandstone|42597|5|Briefly described|Map Legend|Carpentarian||||||||
11455|Mattamurta Sandstone|43010|2|Defined|p85||Paleoproterozoic|Of Parsons Range Group. Of Statherian age.||||||07-NOV-08
11455|Mattamurta Sandstone|44112|4|Described|p31,49-50|||||||||
11455|Mattamurta Sandstone|44299|4|Described|p.11||Paleoproterozoic|SD/53-7,8. L.Proterozoic. Table 1.||||||07-NOV-08
11455|Mattamurta Sandstone|44300|14|Not recorded|map legend||Paleoproterozoic|SD/53-7,8. L.Proterozoic.||||||07-NOV-08
11455|Mattamurta Sandstone|61403|5|Briefly described|Map Legend|Statherian|Statherian|Of Parsons Range Group. Quartz sandstone: medium to very thick-bedded, fine to coarse-grained, with granule-rich laminae and scattered pebbles; cross -bedding and ripples; local porphyritic K-feldspar-quartz rhyolite near base. Geol. Prov: McArthur Basin.||||||
11455|Mattamurta Sandstone|64817|6|Mentioned|p353 Fig.4|||||Unit in Parsons Range Group.||||
11455|Mattamurta Sandstone|65228|6|Mentioned|p23|||NW McArthur Basin.||||Is overlain by Badalngarrmirri Formation.||
11455|Mattamurta Sandstone|69430|4|Described|p15:3, 13-14|Statherian|Statherian|Walker Fault Zone, northern McArthur Basin. 2700-3000m thick. Previously thought to overlie Fagan Volcanics unconformably. Shallow-marine and possibly braided fluvial deposits. The porphyry resembles that in the Fagan Volcanics.||Parsons Range Group.||Conformably overlies Dhupuwamirri Member (Fagan Volcanics). Is overlain conformably by Mount Fawcett Member (Badalngarrmirri Formation).|Fine- to coarse-grained quartz sandstone; scattered granule and pebble layers; shallow sills of crystal-rich felsic porphyry (porphyritic rhyolite) in the lowermost 200m.|12-JUL-16
11455|Mattamurta Sandstone|69673|6|Mentioned|p16 fig 13|||||||Overlain by Badalingarrmirri Formation, overlies Dhupuwamirri Member||
11476|Maurice Formation|22716|6|Mentioned|table4,p231|Proterozoic|Proterozoic|||||||
11476|Maurice Formation|22804|6|Mentioned|Fig 2 on p432|Neoproterozoic|Neoproterozoic|||||||
11476|Maurice Formation|22826|6|Mentioned|Fig 2 on p565|Neoproterozoic|Neoproterozoic|||||||
11476|Maurice Formation|24301|5|Briefly described|p17|||Geological Province: Amadeus Basin||||||
11476|Maurice Formation|31914|6|Mentioned|p96|||||||||
11476|Maurice Formation|33588|6|Mentioned|p6|||||||||
11476|Maurice Formation|34442|6|Mentioned|p7|||Prot. See also p8. Equiv. Pertatataka Formation.||||||02-NOV-06
11476|Maurice Formation|35102|6|Mentioned|Fig.2|||||||||
11476|Maurice Formation|35127|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
11476|Maurice Formation|35222|4|Described|Table.2|||||||||
11476|Maurice Formation|35863|6|Mentioned|Table 1|||||||||
11476|Maurice Formation|36473|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
11476|Maurice Formation|36551|6|Mentioned|Table 13|||||||||
11476|Maurice Formation|36887|5|Briefly described|p211|||||||||
11476|Maurice Formation|37928|6|Mentioned|Fig.4|||||||||
11476|Maurice Formation|39210|6|Mentioned|Fig.10|||||||||
11476|Maurice Formation|40740|6|Mentioned|p1|||||||||
11476|Maurice Formation|41039|6|Mentioned|Fig.2|||||||||
11476|Maurice Formation|41852|6|Mentioned|Table 1|||||||||
11476|Maurice Formation|42940|5|Briefly described|Plate 2|Neoproterozoic|Neoproterozoic|Sandstone, quartzwacke, siltstone.  Geological province: Amadeus Basin.||||||23-JAN-08
11476|Maurice Formation|43503|6|Mentioned|50|||||||||
11476|Maurice Formation|44395|14|Not recorded|p.6,12, Tb.1||Proterozoic|Correlates with Winnall Beds and Pertatataka Formation.||||||
11476|Maurice Formation|44396|5|Briefly described|map legend|||(Proterozoic-Lower Palaeozoic). SF/52-15.||||||
11476|Maurice Formation|44439|2|Defined|p.7,8, Tb.1, map||Neoproterozoic|Upper Proterozoic-Cambrian. Age unclear. Probably equiv.to Cleland Sandstone (Cam.).||||||02-NOV-06
11476|Maurice Formation|44440|14|Not recorded|map legend|Cambrian|Neoproterozoic|Upper Proterozoic-Cambrian.||||||
11476|Maurice Formation|44499|14|Not recorded|opp.p.6, Tb.1|||Proterozoic to Lower Palaeozoic?||||||
11476|Maurice Formation|44500|5|Briefly described|map legend|||Proterozoic to Lower Palaeozoic?||||||
11476|Maurice Formation|45041|4|Described|p38|||Prot. Equiv. Winnall Beds||||||
11476|Maurice Formation|45149|6|Mentioned|Table 1|||Page 17.||||||
11476|Maurice Formation|48842|2|Defined|p.18-20|Early Paleozoic|Neoproterozoic|p.8,15,17-18-20,21-2,27,32,Pl.5,7,8. Tb.I. Overlies Ellis Sandstone and Sir Frederick Conglomerate. U.Prot.-L.Palae.||||||07-NOV-08
11476|Maurice Formation|48864|14|Not recorded|Tb.1,p.10,31,Pl.10|||Cambrian? (G52-2).||||||
11476|Maurice Formation|48963|6|Mentioned|Fig.2|||||||||
11476|Maurice Formation|61385|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Red, crossbedded sandstone; siltstone. Geological Province: Amadeus Basin.||||||
11476|Maurice Formation|61387|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Red, cross-bedded sandstone; siltstone.  Geological Province: Amadeus Basin.||||||
11476|Maurice Formation|61519|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Red, cross bedded sandstone; siltstone. Geological Province: Amadeus Basin.||||||
11476|Maurice Formation|62376|5|Briefly described|p18|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin.||||||09-FEB-10
11476|Maurice Formation|62379|5|Briefly described|p7 Fig. 2|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin.||||||
11476|Maurice Formation|62609|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Sandstone, quartz greywacke, siltstone. Overlies Sir Frederick Conglomerate and Ellis Sandstone.||||||14-AUG-06
11476|Maurice Formation|62620|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Sandstone, quartz greywacke, siltstone.||||||
11476|Maurice Formation|64580|4|Described|map legend||Neoproterozoic|Very fine to medium grained quartzose sandstone; cross-bedded; minor laminated, micaceous siltstone.||||||09-DEC-08
11476|Maurice Formation|64809|6|Mentioned|p3 Fig.2 |Proterozoic|Proterozoic|||||||
11476|Maurice Formation|65102|6|Mentioned|p363, Figure 4-38|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
11476|Maurice Formation|65233|5|Briefly described|p3 Fig. 2|Neoproterozoic|Neoproterozoic|Geological province: Amadeus Basin.||||||07-FEB-11
11476|Maurice Formation|67326|5|Briefly described|p2, p4, p8|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||Overlies Sir Frederick Conglomerate and Ellis Sandstone. Is overlain unconformably by Eninta Formation.||
11476|Maurice Formation|67856|4|Described|p340, 338 , 339, 335, 337, 344, 345|Neoproterozoic|Neoproterozoic|Of Wells et al., 1964, 1970. Type section: Maurice Hills, 23o54'S, 120o18'E. 1800m thick. Deltaic/paralic/shallow marine sediments. No age determination.||||Overlies Ellis Sandstone (conformably) and Sir Frederick Conglomerate (conformably). equivalent to upper part of Winnall beds.|Cross-bedded sandstone, quartz greywacke, micaceous sandstone, clay pellets, heavy mineral concentrations, chocolate-brown laminated siltstone.|
11476|Maurice Formation|68323|6|Mentioned|p4 Fig.2|Neoproterozoic|Neoproterozoic|Amadeus Basin.||Pertaoorrta Group.||||
11476|Maurice Formation|69003|6|Mentioned|p60|Cambrian|Cambrian|W Amadeus Basin.||||||
11476|Maurice Formation|69031|5|Briefly described|p4, p9|||Amadeus Basin. Deposited during the c.580-530 Ma Petermann Orogeny.||||Overlies Sir Frederick Conglomerate and Ellis Sandstone.||
11476|Maurice Formation|69437|5|Briefly described|p22:10|Cambrian|Cambrian|Idirriki Sub-basin, SW Amadeus Basin.||||Overlies Ellis Sandstone, Mount Currie Conglomerate and Mutitjulu Arkose.||12-JUL-16
11476|Maurice Formation|69438|4|Described|p23:2-4, 18, 20-21, 23|Early Cambrian|Ediacaran|Amadeus Basin. Up to 3600m thick in WA. Alternating fluvial and shallow-marine deposits. Sediments sourced from the S. Was previously considered equivalent to Pertatataka Formation.||Pertaoorrta Group.||Conformably overlies Ellis Sandstone and Sir Frederick Conglomerate. Lateral equivalent of upper parts of Arumbera Sandstone and Winnall beds. Is faulted against Bitter Springs Formation.|Medium- to thinly-bedded, cross-bedded, finely micaceous red sandstone and siltstone.|12-JUL-16
11476|Maurice Formation|69606|5|Briefly described|p1, p4 fig 2, p14, p17|Lower Cambrian|Upper Ediacaran|western Amadeus Basin. Deposited synchronously with the Petermann Orogeny. Potential reservoir and seal rock.||||Overlies the Ellis Sandstone and the Sir Frederick Conglomerate.|Shale, sandstone and siltstone.|
11476|Maurice Formation|69673|6|Mentioned|p64 fig 53, p65, p75|||||||Overlies Sir Frederick Conglomerate, Ellis Sandstone, correlated with Winnall beds||
11476|Maurice Formation|70416|5|Briefly described|p65 Fig.2|Early Cambrian|Early Cambrian|Amadeus Basin.||Top of Winnall Group.||Overlies Ellis Sandstone.||
11476|Maurice Formation|70793|4|Described|500k_interpgeop14_lut.csv|Series 2|Ediacaran|Of Amadeus Basin (Phase 1), Centralian Superbasin. Events: Areyonga Movement; Delamarian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma).|635-509 Ma (inferred)||||Lithic and feldspathic sandstone, very fine to medium grained; cross-bedded; minor laminated, micaceous siltstone; commonly silicified|
11476|Maurice Formation|70826|6|Mentioned|p5 tbl 2|||Supersequence 4, Centralian Superbasin.||||||21-JAN-22
11476|Maurice Formation|70839|4|Described|p325,329-333,335-340,344|Cambrian|Cambrian|Of Amadeus Basin. Part of Supersequence 4. Reaches up to 3600m thickness in the south, and thins significantly to the north (Haines et al., 2012). Conglomeratic clasts likely derived from Dean Quartzite and Kulail Sandstone, and Tjauwata Group (or Dixon Range beds; WA). SHRIMP U-Pb zircon geochronology samples and analysis on p331-334. Two samples, one each from lower and upper parts of the section. Lower Maurice maximum dep age: 831+\-13 Ma (207Pb/206Pb). Upper Maurice maximum dep age: 698+\-20 Ma (207Pb/206Pb). See p332-333 for zircon age spectrums.||||Overlain by Mu Formation. Underlain by Ellis Sandstone and Sir Frederick Conglomerate. Correlable to units 3 and 4 of the Winnall beds.|Immature fluvial sandstone, siltstone, and minor conglomerate. Clasts include quartzite, sandstone, and metasandstone lithologies.|
11476|Maurice Formation|71080|5|Briefly described|p30 fig 21|Cambrian|Cambrian|Amadeus Basin in WA. Supersequence 4.|||||Dominantly sandstone, some shale.|
11476|Maurice Formation|71088|4|Described|p1-p2, p7-p8, p12|Cambrian|Ediacaran|Amadeus Basin. Reassigned to Supersequence 4. Correlated with the Pertatataka Formation by Wells et al., 1970; Grey, 1990 and Lindsay and Korsch., 1991. This unit is very recessive and rarely exposed. This unit reaches a maximum thickness of 3600m exposed in the southern Wallace Hills. Samples dated in this study are described. Max depositional age from detrital zircon from lower Maurice Formation: 831+/-13 Ma. Max depositional age from detrital zircon from upper Maurice Formation: 698+/-20 Ma. See also p14, p16-p22, p24, p33.||||Overlies the Sir Frederick Conglomerate and the Ellis Sandstone. Unconformably overlain by the Mu Formation. Equivalent to the Winnall beds, Angas Hills Formation and Arumbera Sandstone.|Red-brown micaceous siltstone and very friable fine-grained sandstone. Red brown micaceous sandstone, lesser siltstone and local conglomeratic sandstone.|02-MAY-23
11476|Maurice Formation|71114|6|Mentioned|p170 fig 1b|Terreneuvian|Terreneuvian|SW Amadeus Basin.||||||14-FEB-18
11476|Maurice Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, sandstone|
11476|Maurice Formation|71268|4|Described|GEOL_LUT_CSV files|Series 2|Ediacaran|Of Amadeus Basin (Phase 1), Centralian Superbasin. Events: Delamarian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma). See 1m_geologyp12_lut.csv, 500k_interpgeop16_lut.csv.|635-510 Ma (inferred)||||Very fine to medium grained, cross bedded quartz sandstone; minor laminated micaceous siltstone and micaceous sandstone|
11476|Maurice Formation|71279|5|Briefly described|p355 Fig.2|Early Cambrian|Early Cambrian|Amadeus Basin.||Pertaoorrta Group.||||
11476|Maurice Formation|71592|5|Briefly described|Appendix A.|||Amadeus Basin.|698+/-20 Ma (MDA: U-Pb zircon SHRIMP)||||Medium- to coarse-grained quartz-lithic sandstone.|
11476|Maurice Formation|71800|5|Briefly described|p26-p27|Early Cambrian|Early Cambrian|Amadeus Basin.||||Overlies the Ellis Sandstone and the Sir Frederick Conglomerate. Overlain by the Mu Formation and Mount Currie Conglomerate.|Lithic sandstone.|
11476|Maurice Formation|71810|5|Briefly described|Map legend.|Cambrian|Ediacaran|Amadeus Basin (Phase 1), Centralian Superbasin.||||Overlies Ellis Sandstone. Is overlain by Paterson Formation.|Fine- to medium-grained, cross-bedded, poorly-sorted, friable, lithic, feldspathic and micaceous red-brown sandstone; micaceous red-brown siltstone (inferred to have been deposited during the Petermann Orogeny).|
11476|Maurice Formation|71841|5|Briefly described|p1|Early Cambrian|Ediacaran|Of Amadeus Basin.||Unit of Pertaoorrta Group.||Underlain by Sir Frederick Conglomerate or Ellis Sandstone. Grades into Winnall beds.||
11476|Maurice Formation|71842|5|Briefly described|p2-3|Early Cambrian|Early Cambrian|Of Amadeus Basin. Nomenclature after Haines and Allen 2010 (Western Amadeus, WA).||Unit of Pertaoorrta Group.||Underlain by Sir Frederick Conglomerate or Ellis Sandstone.||
11476|Maurice Formation|72034|5|Briefly described|500k_interpgeop16_lut|Series 2|Ediacaran|Amadeus Basin (Phase 1).|||||Lithic and feldspathic sandstone, very fine to medium grained; cross-bedded; minor laminated, micaceous siltstone; commonly silicified.|
11476|Maurice Formation|72358|6|Mentioned|p118|Series 2|Series 2|Of Amadeus Basin.||||||
11476|Maurice Formation|72360|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of Amadeus Basin.|||||Red, cross bedded sandstone; siltstone.|09-SEP-19
11476|Maurice Formation|72601|6|Mentioned|p3|Cambrian|Ediacaran|Amadeus Basin, western portion[?].||||||
11476|Maurice Formation|73180|6|Mentioned|p48 Fig.1|Early Cambrian|Early Cambrian|Amadeus Basin.||||Conformably overlies the Mount Currie Conglomerate.||
11512|McArthur Group|7071|5|Briefly described|p1|||Geological Province: McArthur Basin.||||||
11512|McArthur Group|14019|5|Briefly described|p4|Paleoproterozoic|Paleoproterozoic|Includes the Barney Creek Formation.  Geological Province: McArthur  Basin.||||||07-NOV-08
11512|McArthur Group|22479|5|Briefly described|fig4, pg10|Statherian|Statherian|||||||
11512|McArthur Group|22538|4|Described|p707, p717||Statherian|Part of the Glyde package||||||20-JUL-06
11512|McArthur Group|22600|6|Mentioned|Map legend|||||||||
11512|McArthur Group|22644|5|Briefly described|3,5,7,9|||Geol province McArthur Basin. Of Murphy Metamorphics (?). Underlying unit: Gold Creek Volcanics||||||20-JUL-06
11512|McArthur Group|22662|6|Mentioned|22,24,29,30|||Geol province McArthur Basin||||||
11512|McArthur Group|22664|3|Fully described|33,35,39,42,43,45|Paleoproterozoic|Paleoproterozoic|Geol.province: McArthur Basin. Also on pages 46 fig 14, 47,48.||||||07-NOV-08
11512|McArthur Group|22665|6|Mentioned|P219|||||||||
11512|McArthur Group|22670|6|Mentioned|53,54,58-60|||Geological province: McArthur Basin.||||||06-NOV-06
11512|McArthur Group|22808|6|Mentioned|7 fig 4|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
11512|McArthur Group|22853|5|Briefly described|14|Proterozoic|Proterozoic|Age 1690 +29 - 25 Ma. Max thickness 4 km||||||
11512|McArthur Group|23066|5|Briefly described|p807, Fig.1|Proterozoic|Proterozoic|In the McArthur Basin.||||||06-NOV-06
11512|McArthur Group|23195|6|Mentioned|p5|||Informally referred to "Lower" McArthur group sandstone aquifer.||||||
11512|McArthur Group|23197|6|Mentioned|Fig.1, p850|||Informally referred to a "Lower" McArthur Group.||||||
11512|McArthur Group|23216|6|Mentioned|p30|||||||||
11512|McArthur Group|23291|6|Mentioned|p24|||Geological Province: Georgetown Region.||||||08-JUL-15
11512|McArthur Group|23362|6|Mentioned|337|||||||||
11512|McArthur Group|23374|5|Briefly described|Fig3p5,34,35,6,29||Paleoproterozoic|Of McArthur Basin.||||||07-NOV-08
11512|McArthur Group|23387|6|Mentioned|p18 fig.19|||||||||
11512|McArthur Group|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: McArthur Basin.||||||07-NOV-08
11512|McArthur Group|23395|5|Briefly described|p382|||||||||
11512|McArthur Group|23397|5|Briefly described|p463|||||||||
11512|McArthur Group|23398|5|Briefly described|p440|||||||||
11512|McArthur Group|23405|6|Mentioned|p576|||||||||
11512|McArthur Group|23407|5|Briefly described|p626|||||||||
11512|McArthur Group|23408|6|Mentioned|p512|||Found to contain cauliflower-chert nodules in Palaeoproterozoic carbonates.||||||15-JUN-09
11512|McArthur Group|23409|5|Briefly described|p533|||||||||
11512|McArthur Group|23534|6|Mentioned|p2317|||Hosts the McArthur River deposit. Geological Province: McArthur Basin.||||||
11512|McArthur Group|23733|6|Mentioned|p31|||Geological Province: MacArthur Basin.  See also p32 Fig. 19.||||||
11512|McArthur Group|23776|5|Briefly described|p705 Fig 2|||||||||
11512|McArthur Group|23809|5|Briefly described|p47 Fig. 42|Proterozoic|Proterozoic|Geological Province: McArthur Basin.  Correlates with Namerinni Group (Ashburton Province), Lumbunya (Limbunya misspelt) Group (Birrindudu Basin) and Bungle Bungle Dolomite (Osmond Basin, WA).||||||30-MAR-05
11512|McArthur Group|23902|5|Briefly described|p1568 Fig. 2, p1571|||Max. Thickness: 4400m. Geological Province: McArthur Basin||||||
11512|McArthur Group|23910|4|Described|p290|Paleoproterozoic|Paleoproterozoic|Geological Province: McArthur Basin.||||||07-NOV-08
11512|McArthur Group|23937|5|Briefly described|p8, p25 Tb. 2|Statherian|Statherian|Restricted to Maria Island in ROPER RIVER.  On URAPUNGA these rocks are now divided into Vizard and Nathan Groups (Jackson et al, 1987).  Geological Province: Isa Superbasin.||||||
11512|McArthur Group|23957|5|Briefly described|p1120|Proterozoic|Proterozoic|Age: 1640 +/- 3Ma.  Geological Province: McArthur Basin.||||||
11512|McArthur Group|23961|6|Mentioned|p1191|||Geological Province: Mt Isa Inlier.||||||
11512|McArthur Group|23963|5|Briefly described|p1237, 1239 Fig.2|||Geological Province: McArthur Basin.||||||
11512|McArthur Group|23966|5|Briefly described|p1309|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier.   Age: 1640 +/- 7Ma.||||||
11512|McArthur Group|24047|5|Briefly described|p12 Fig. 10, p11|Paleoproterozoic|Paleoproterozoic|Age: 1670-1600Ma.  Geological Province: McArthur Basin.  See also p40.||||||07-NOV-08
11512|McArthur Group|24048|5|Briefly described|p3|||Geological Province: McArthur Basin||||||
11512|McArthur Group|24049|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|In regional setting map legend.||||||07-NOV-08
11512|McArthur Group|24050|5|Briefly described|p7|||||||||
11512|McArthur Group|24179|5|Briefly described|p82|||Overlies the Tallawah Group.  Overlain by the Nathan group.  Geological Province:  McArthur Basin.||||||
11512|McArthur Group|24303|6|Mentioned|p17|||Geological Province: McArthur Basin.||||||
11512|McArthur Group|24419|5|Briefly described|p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: McArthur Basin.||||||07-NOV-08
11512|McArthur Group|24432|5|Briefly described|p562 Fig.2|Calymmian|Statherian|Geological Province: Southern McArthur Basin.||||||28-JAN-05
11512|McArthur Group|24442|6|Mentioned|p14|||Equivalent of the Namerinni Group.  Geological Province: McArthur Basin.||||||
11512|McArthur Group|30272|6|Mentioned|p5|||Stratigraphic table on P5||||||
11512|McArthur Group|30318|6|Mentioned|p327|||||||||
11512|McArthur Group|30344|6|Mentioned|Fig.4|||See also P29.||||||
11512|McArthur Group|30345|6|Mentioned|Table 1|||Carpentarian age. Lithology||||||
11512|McArthur Group|30354|6|Mentioned|p20|||||||||
11512|McArthur Group|30363|6|Mentioned|p22|||||||||
11512|McArthur Group|30839|6|Mentioned|p29|||||||||
11512|McArthur Group|31824|6|Mentioned|p28|||U.Proterozoic||||||
11512|McArthur Group|32132|6|Mentioned|p820|||||||||
11512|McArthur Group|32144|6|Mentioned|p81|||Solvent extractable organic matter||||||
11512|McArthur Group|32339|6|Mentioned|p143|||||||||
11512|McArthur Group|32363|6|Mentioned|p330|||||||||
11512|McArthur Group|32479|6|Mentioned|p1393|||||||||
11512|McArthur Group|32658|3|Fully described|p103|||See also p104 -115. Nomenclature revised||||||20-JUL-06
11512|McArthur Group|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
11512|McArthur Group|32660|4|Described|Table 4|||||||||
11512|McArthur Group|32722|6|Mentioned|Fig.2|||Stromatolite||||||
11512|McArthur Group|32959|6|Mentioned|p19|||||||||
11512|McArthur Group|33214|6|Mentioned|Fig.1|||||||||
11512|McArthur Group|33550|6|Mentioned|p272|||||||||
11512|McArthur Group|33630|6|Mentioned|p908|||||||||
11512|McArthur Group|33665|6|Mentioned|p365|||||||||
11512|McArthur Group|33666|4|Described|p526|||Discussed throughout||||||
11512|McArthur Group|34287|6|Mentioned|p34|||See also PP36, 37, 55||||||
11512|McArthur Group|34754|6|Mentioned|p15|||||||||
11512|McArthur Group|34891|6|Mentioned|p240|||||||||
11512|McArthur Group|35114|6|Mentioned|p199|||||||||
11512|McArthur Group|35162|6|Mentioned|p1007|||||||||
11512|McArthur Group|35261|6|Mentioned|p316|||||||||
11512|McArthur Group|35950|6|Mentioned|p311|||||||||
11512|McArthur Group|36012|6|Mentioned|p16|||||||||
11512|McArthur Group|36473|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
11512|McArthur Group|36751|6|Mentioned|p472|||See also p479.||||||06-NOV-06
11512|McArthur Group|36796|6|Mentioned|p19|||||||||
11512|McArthur Group|37216|6|Mentioned|p558|||||||||
11512|McArthur Group|37217|6|Mentioned|p649|||||||||
11512|McArthur Group|37371|6|Mentioned|p368|||||||||
11512|McArthur Group|37462|4|Described|Table4.IV|||||||||
11512|McArthur Group|37565|5|Briefly described|p3|||See also Fig.5||||||
11512|McArthur Group|37569|6|Mentioned|p89|||See also P90||||||
11512|McArthur Group|38042|6|Mentioned|p160|||||||||
11512|McArthur Group|38156|6|Mentioned|Fig.1|||||||||
11512|McArthur Group|38243|6|Mentioned|p354|||||||||
11512|McArthur Group|38278|6|Mentioned|p7|||||||||
11512|McArthur Group|38504|6|Mentioned|p1177|||||||||
11512|McArthur Group|38529|6|Mentioned|p275|||||||||
11512|McArthur Group|38582|6|Mentioned|p215|||||||||
11512|McArthur Group|38902|6|Mentioned|p20|||||||||
11512|McArthur Group|39122|6|Mentioned|p154|||||||||
11512|McArthur Group|39210|4|Described|p50|||||||||
11512|McArthur Group|39445|6|Mentioned|p39|||Correlated with Fickling Group||||||
11512|McArthur Group|39558|6|Mentioned|Table 1|||||||||
11512|McArthur Group|39561|6|Mentioned|Fig.5|||||||||
11512|McArthur Group|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
11512|McArthur Group|39925|6|Mentioned|p337|||||||||
11512|McArthur Group|40088|6|Mentioned|p224|||||||||
11512|McArthur Group|40105|6|Mentioned|p310|||See also Fig.7||||||
11512|McArthur Group|40109|5|Briefly described|p302|||||||||
11512|McArthur Group|40259|6|Mentioned|Table 1|||||||||
11512|McArthur Group|40691|3|Fully described|p11|||||||||
11512|McArthur Group|40973|6|Mentioned|p193|||||||||
11512|McArthur Group|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
11512|McArthur Group|41019|5|Briefly described|p243|||||||||
11512|McArthur Group|41220|5|Briefly described|p367|||||||||
11512|McArthur Group|41268|4|Described|p284|||Mention p288||||||20-JUL-06
11512|McArthur Group|41277|5|Briefly described|p80|||||||||
11512|McArthur Group|41406|6|Mentioned|Map legend|Mesoproterozoic||||||||
11512|McArthur Group|41465|6|Mentioned|p12|||||||||
11512|McArthur Group|41649|6|Mentioned|p76|||||||||
11512|McArthur Group|41721|4|Described|p26|||Includes Karns Dolomite and Masterton Sandstone.  Geological Province: McArthur Basin.||||||11-JUN-08
11512|McArthur Group|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
11512|McArthur Group|41957|6|Mentioned|p68|||||||||
11512|McArthur Group|41970|6|Mentioned|p336|||||||||
11512|McArthur Group|41975|6|Mentioned|p437|||||||||
11512|McArthur Group|42058|6|Mentioned|p118|||||||||
11512|McArthur Group|42323|6|Mentioned|p4|||||||||
11512|McArthur Group|42365|5|Briefly described|p272|||||||||
11512|McArthur Group|42385|4|Described|p14|||See also Table 4 p16 and 17.||||||06-NOV-06
11512|McArthur Group|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
11512|McArthur Group|42504|6|Mentioned|p68|||Not misspelling of McArthur River Group?||||||
11512|McArthur Group|42597|5|Briefly described|Map legend|Carpentarian||||||||
11512|McArthur Group|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.|||Batten Subgroup (5 formations) overlying Umbolooga Subgroup (11 formations).|Underlies Nathan Group units; overlies Tawallah Group units.||07-NOV-11
11512|McArthur Group|42639|4|Described|p18, Table 5 p20,21|||||||||
11512|McArthur Group|42652|5|Briefly described|p306|||||||||
11512|McArthur Group|42700|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
11512|McArthur Group|42739|5|Briefly described|map legend|Statherian|Statherian|||||||19-OCT-05
11512|McArthur Group|42753|6|Mentioned|p2|||||||||
11512|McArthur Group|42812|4|Described|p28, Table 4|||||||||
11512|McArthur Group|42819|5|Briefly described|p307|||||||||
11512|McArthur Group|42846|5|Briefly described|p503, Fig.1 p502|||Geological Province: McArthur Basin.||||||09-MAY-05
11512|McArthur Group|42873|5|Briefly described|Fig.1, P110|||||||||
11512|McArthur Group|42935|5|Briefly described|p529 Fig.2|||||||||
11512|McArthur Group|43010|2|Defined|p107||Paleoproterozoic|Of Statherian age.||||||07-NOV-08
11512|McArthur Group|43036|4|Described|p39|||||||||
11512|McArthur Group|43069|5|Briefly described|p15|||||||||
11512|McArthur Group|43107|6|Mentioned|p9|||||||||
11512|McArthur Group|43115|6|Mentioned|p176|||||||||
11512|McArthur Group|43235|6|Mentioned|p8|||Proterozoic||||||
11512|McArthur Group|43292|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
11512|McArthur Group|43486|5|Briefly described|21|||||||||
11512|McArthur Group|43583|6|Mentioned|p2164|||Age 1690+/-27 Ma||||||
11512|McArthur Group|43595|4|Described|p437-8||Mesoproterozoic|Age: 1690+/-27 Ma.||||||06-NOV-06
11512|McArthur Group|43610|5|Briefly described|p20||Proterozoic|Age of tuffaceous beds: 1640+/-3 Ma (SHRIMP)||||||
11512|McArthur Group|43615|6|Mentioned|p14|||||||||
11512|McArthur Group|43664|6|Mentioned|p14|||||||||
11512|McArthur Group|43788|6|Mentioned|p13||Proterozoic|||||||
11512|McArthur Group|44111|6|Mentioned|p55|||Middle Proterozoic. Has for years been thought to be a correlative of Yeneena Group; more recent work puts this latter unit in Late Proterozoic.||||||
11512|McArthur Group|44112|5|Briefly described|p5,55|||Part of Supersequence 3||||||
11512|McArthur Group|44155|6|Mentioned|p252|||McArthur Basin. Probable part correlative of Mount Parker Sandstone and Bungle Bungle Dolomite.||||||
11512|McArthur Group|44287|14|Not recorded|p.6-19|||map. (E53-3).||||||
11512|McArthur Group|44288|14|Not recorded|map legend|||Lower (?) Proterozoic.||||||
11512|McArthur Group|44299|4|Described|p.11-13|||SD/53-7,8. Lower(?) Proterozoic. Table 1.||||||
11512|McArthur Group|44300|14|Not recorded|map legend|||SD/53-7,8. Lower (?) Proterozoic.||||||
11512|McArthur Group|44305|14|Not recorded|p.11,14,18|||(E53-8). opp.6,18.||||||
11512|McArthur Group|44306|14|Not recorded|map legend|||(?) Lower Proterozoic.||||||
11512|McArthur Group|44332|14|Not recorded|p.7,11,12,opp.6,map|||(D53-14).||||||
11512|McArthur Group|44333|14|Not recorded|map legend|||Lower(?) Proterozoic.||||||
11512|McArthur Group|44434|14|Not recorded|p.7,10, opp.p.6, map|||Includes in this area Kookaburra Creek Formation & Batten Subgroup. (D53-11,12).||||||
11512|McArthur Group|44435|14|Not recorded|map legend|||Lower (?) Proterzoic.||||||
11512|McArthur Group|44436|5|Briefly described|p.6,10,12,opp.7,map|||Includes Karns Dolomite. (E53-4).||||||02-DEC-04
11512|McArthur Group|44437|5|Briefly described|map legend|Precambrian|Precambrian|Includes the Karns Dolomite.  Lower (?) Proterozoic.  Overlain by the Roper Group.||||||08-DEC-04
11512|McArthur Group|44459|14|Not recorded|p.8,12,13|||(E53-2). Not found on E53-2 sheet area.||||||
11512|McArthur Group|44471|14|Not recorded|p.8-15, opp.p.7, map|||(D53-10).||||||
11512|McArthur Group|44472|5|Briefly described|map legend|||Includes the Vizard Formation, Mount Birch Sandstone and the Kookaburra Creek Formation.  Lower (?) Proterozoic.||||||02-DEC-04
11512|McArthur Group|44473|14|Not recorded|p.7-10,13-15|||(E53-7). Includes (Wallhallow sheet area) Billengarrah Formation, Emmerugga Dolomite, Bauhinia Downs Subgroup (q.v.), Amelia Dolomite & Mallapunya Formation (bottom).||||||
11512|McArthur Group|44474|14|Not recorded|map legend|||Lower (?) Proterozoic.||||||
11512|McArthur Group|44482|14|Not recorded|p.7,8,14,opp.p.6,map|||(E53-12).||||||
11512|McArthur Group|44483|5|Briefly described|map legend|||Lower (?) Proterozoic.||||||
11512|McArthur Group|44530|14|Not recorded|p.6-14, opp.12,16|||(D53-15).||||||
11512|McArthur Group|44531|14|Not recorded|map legend|||Lower (?) Proterozoic.||||||
11512|McArthur Group|45022|6|Mentioned|p.74||Carpentarian|||||||
11512|McArthur Group|45032|14|Not recorded|p9||Carpentarian|Tb.1, Pl.1.||||||
11512|McArthur Group|45112|6|Mentioned|p19|||||||||
11512|McArthur Group|45140|6|Mentioned|p12-13|||McArthur Basin region.||||||
11512|McArthur Group|45162|4|Described|p45|Proterozoic|Proterozoic|||||||
11512|McArthur Group|45167|5|Briefly described|Fig.27|||||||||
11512|McArthur Group|46861|6|Mentioned|p2|||||||||
11512|McArthur Group|46915|4|Described|p149|||Discussed throughout article.||||||
11512|McArthur Group|46955|6|Mentioned|p159|||||||||
11512|McArthur Group|46968|6|Mentioned|Fig.1|||See also Fig.2||||||
11512|McArthur Group|47004|6|Mentioned|p328|||||||||
11512|McArthur Group|47008|6|Mentioned|p330|||||||||
11512|McArthur Group|50225|5|Briefly described|p406 Fig. 10, p407|Paleoproterozoic|Paleoproterozoic|Geological Province: McArthur Basin.||||||07-FEB-11
11512|McArthur Group|60483|4|Described|p7 Fig. 5, p8, p30|||Subdivided into Umbolooga and Batten Subgroups. Unconformable over Tawallah Gp. Age: 1670-1600Ma. Thickness: ~4.5km. Geol.Prov: McArthur Basin. Interbedded stromatolitic and evaporitic dolostone, sandstone, mudstone, and minor tuffaceous mudstone.||||||
11512|McArthur Group|60553|5|Briefly described|p624, 625|||Lower McArthur Group carbonates overlain by the Barney Creek Formation.||||||06-APR-18
11512|McArthur Group|60558|5|Briefly described|p7, p8 Fig. 6|Proterozoic|Proterozoic|Inculdes Umbolooga and Batten Sub-groups. Dominated by shallow water to locally emergent, often evaporitic carbonates with minor associated fine-grained shallow water clastics.||||||
11512|McArthur Group|60573|5|Briefly described|Map legend|Statherian|Statherian|Includes the Stretton Sandstone, and Yalco and Lynott Formations.||||||
11512|McArthur Group|60574|5|Briefly described|Map Legend|||Geological Province: McArthur Basin.||||||
11512|McArthur Group|61390|5|Briefly described|Map Legend|Statherian|Statherian|||||||
11512|McArthur Group|61403|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|In regional setting map legend.||||||07-NOV-08
11512|McArthur Group|61541|6|Mentioned|p267.||||||Includes the Upper Barney Creek Formation.|||
11512|McArthur Group|61736|5|Briefly described|p674|Paleoproterozoic|Paleoproterozoic|Age (in middle section): 1640+/-3Ma (McArthur River deposit).||||||
11512|McArthur Group|62084|5|Briefly described|p936 Fig.5, p941 Fig.9, p942, p956-957|||Isa Superbasin. McArthur Basin. Shown as lower McArthur Group in Fig.9.|||Mallapunyah Formation, Amelia Dolomite, Tatoola Sandstone, Tooganinie Formation, Myrtle Shale, Emmerugga Dolomite, Teena Dolomite, Barney Creek Formation, Reward Dolomite, Lynott Formation|||
11512|McArthur Group|62285|6|Mentioned|p380|||||||||
11512|McArthur Group|62473|6|Mentioned|p75||Paleoproterozoic|Age at its HYC deposit: ca. 1640Ma.||||||17-JUN-09
11512|McArthur Group|62535|5|Briefly described|p674|||Hosts the McArthur River Pb-Zn-Ag deposit.|1640 +/- 3 Ma.|||||
11512|McArthur Group|63062|5|Briefly described|p38|||Includes Barney Creek Formation. Geological Province: McArthur Basin.||||||07-FEB-11
11512|McArthur Group|63110|6|Mentioned|p1141|||Underlian by Tawallah Group.||||||11-JUN-08
11512|McArthur Group|63112|6|Mentioned|p1190|||Southern McArthur Basin.||||||
11512|McArthur Group|64250|6|Mentioned|p25 fig 10|||Southern McArthur Basin.||||||
11512|McArthur 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)||||||
11512|McArthur Group|64777|6|Mentioned|p2|Palaeoproterozoic|Palaeoproterozoic|||||||
11512|McArthur Group|64784|6|Mentioned|p3 Fig.3 |||||||||
11512|McArthur Group|64815|5|Briefly described|p1, p3-6, p8 Tb.1, p10, p13-14    |||See also p15 Fig.9, p16-20. Hosts the HYC Zn-Pb-Ag deposit. Carbonate-dominated.|||Includes Umbolooga and Batten Subgroups.|Correlated with Fickling, McNamara and Mount Isa Groups. Is overlain unconformably by Nathan Group.||
11512|McArthur Group|64816|5|Briefly described|p1, p2 Fig.1, p4, p18 |||Contains hydrocarbon source and reservoir beds.|||Includes Emmerugga, Teena, Reward Dolomites; Barney Creek, Lynott, Yelco, Looking Glass and Amos Formations; Stretton Sandstone.|Underlies the Barney Creek Formation||
11512|McArthur Group|64817|6|Mentioned|p352 Fig.3, p353 Fig.4, p354 ||||||Includes the Batten and Umbolooga Subgroups.|||
11512|McArthur Group|64970|6|Mentioned|p726|||||||||
11512|McArthur Group|64975|6|Mentioned|p162 Fig.6.|Mesoproterozoic|Mesoproterozoic|||||||
11512|McArthur Group|65074|6|Mentioned|p352, p354 Tb. 4-11|||||||||
11512|McArthur Group|65209|6|Mentioned|p38|||||||correlates with Namerinni Group||
11512|McArthur Group|65228|5|Briefly described|p7, Fig.02. |Proterozoic||McArthur Basin. Contains cauliflower chert nodules and other ?evaporite pseudomorphs. Measured section.|||Includes Umbolooga and Batten Subgroups.|Unconformably overlies Tawallah Group. Is overlain unconformably by Nathan Group.||
11512|McArthur Group|65236|6|Mentioned|p4 Fig. 4|||Geological province: Beetaloo Sub-basin.||||||
11512|McArthur Group|65340|5|Briefly described|p11, p82.|||Possible partial correlation with Karns Dolomite. Faults, fractures and conduits within this unit are filled with magmatic kimberlite, bedded lapilli tuff and kimberlite breccia that host the Merlin diamond mine.|1670 - 1600 Ma.||Includes Masterton Sandstone.|Unconformably overlies Tawallah Group.||
11512|McArthur Group|66800|6|Mentioned|p928.|||||||||
11512|McArthur Group|66843|4|Described|p23-24, p37|||Southern McArthur Basin.|||Includes Stretton Sandstone, Looking Glass Formation, Amos Formation, Barney Creek Formation.|Unconformably overlies Tawallah Group. Is overlain unconformably by Nathan Group.|A succession of stromatolitic carbonates with minor sandstone and shale.|12-SEP-19
11512|McArthur Group|67144|5|Briefly described|Map legend.|Statherian|Statherian|McArthur Basin.|||Includes  Umbolooga Subgroup.|Overlies Tawallah Group. Is overlain by Nathan Group.||13-APR-12
11512|McArthur Group|67269|6|Mentioned|p20-21 Fig.19|||McArthur Basin.|||Amelia Dolomite.|||
11512|McArthur Group|67323|5|Briefly described|p35|Paleoproterozoic|Paleoproterozoic|McArthur Basin.|Deposition begins ~1660 Ma.||Masterton Sandstone.|||
11512|McArthur Group|67352|4|Described|p12-14, p41, p49 Tb.5, p51, p58-59|Statherian|Statherian|5km thick; carbonate dominated.|1670-1615 Ma||Umbolooga Subgroup, Batten Subgroup|Is overlain paraconformably by Nathan Group.||
11512|McArthur Group|67564|6|Mentioned|p51.|||Equivalent units are missing in this sheet area.||||||
11512|McArthur Group|68280|6|Mentioned|p26 fig 24|||McArthur Basin.|||Includes Amelia Dolomite|||
11512|McArthur Group|68732|6|Mentioned|p159|||||||||
11512|McArthur Group|68733|5|Briefly described|p186-187|Statherian|Statherian|McArthur Basin.|ca. 1640 Ma||Includes the Masterson Sandstone (basal unit), Teena Dolomite, Mount Les Silstone, and Barney Creek Formation.|||05-DEC-17
11512|McArthur Group|69018|5|Briefly described|p450 Fig.1a, b|Statherian|Statherian|Of McArthur Basin.|||Includes Velkerri Formation, Emmerugga Dolomite, Teena Dolomite, Barney Creek Formation, Reward Dolomite, Lynott Formation, Yelco Formation, Stretton Sandstone, Looking Glass, Amos Formations.|||
11512|McArthur Group|69417|6|Mentioned|p2:5|Statherian|Statherian|McArthur Basin.||||||12-JUL-16
11512|McArthur Group|69418|5|Briefly described|p3:36|Proterozoic|Proterozoic|McArthur Basin. Long-recognised as having petroleum potential, particularly in small fault-bounded sub-basins in the southern Batten Fault Zone.||||||12-JUL-16
11512|McArthur Group|69429|6|Mentioned|p14:3 Fig.14.4, 14:4|Paleoproterozoic|Paleoproterozoic|McArthur Basin.||||||12-JUL-16
11512|McArthur Group|69430|4|Described|p15:1-4, 9-10, 12, 14-23, 29-30, 34, 39|Statherian|Statherian|See also 15:42, 48, 56-57, 61-63. Exposures are confined to the Batten Fault Zone, southern McArthur Basin. Essentially horizontal, c.5 km thick succession. Upper part correlates with Nagi Formation (Vizard Group). Has petroleum potential; fair to good conventional reservoirs occur.|||Umbolooga, Batten Subgroups.|Unconformably overlies Echo Sandstone (Tawallah Group). Is overlain unconformably by Bukalara Sandstone.|Platformal stromatolitic dolostone and clastic sedimentary rocks with local pyritic carbonaceous siltstone units.|12-JUL-16
11512|McArthur Group|69431|6|Mentioned|p16:1, 25||||||Umbolooga Subgroup.|Correlated with Namerinni Group.||12-JUL-16
11512|McArthur Group|69433|6|Mentioned|p18:1, 10|||||||Equivalent to Fickling Group (Lawn Hill Platform).||12-JUL-16
11512|McArthur Group|69451|6|Mentioned|p35:13||||||Barney Creek Formation.|||12-JUL-16
11512|McArthur Group|69455|6|Mentioned|p39:14|Proterozoic|Proterozoic|McArthur Basin. Contains organic-rich shale and is relatively unmetamorphosed, making for good potential source rocks underlying the Carpentaria Basin.||||||12-JUL-16
11512|McArthur Group|69673|4|Described|p15, p17, p20, p32, p41, p45, p47, p58,|Statherian|Statherian|Batten Fault Zone. Has elevated potential for both conventional and unconventional petroleum. Up to 5 km thick. Deposited primarily in lacustrine to marine setting. Fair to good reservoir properties.|||Includes Umbolooga Subgroup, Batten Subgroup|Unconformably overlies Tawallah Group, unconformably overlain by Nathan Group, correlated with Fickling Group, Namerinni Group|Stromatolitic and evaporitic dolostone and clastic sedimentary rock with local pyritic carbonaceous siltstone.|
11512|McArthur Group|70822|5|Briefly described|p102 fig 1 (A), p103|Mesoproterozoic|Mesoproterozoic||1625 +/- 2 Ma; 1614 +/- 4 Ma.|||Overlies Tawallah Group; is overlain by Nathan Group.||
11512|McArthur Group|70849|5|Briefly described|Map legend.|Statherian|Statherian|McArthur Basin.|||Includes Masterton Sandstone, Karns Dolomite.|Overlies Tawallah Group.|Mainly sandstone and dolostone.|07-NOV-17
11512|McArthur Group|70897|5|Briefly described|p36, p42, p45|Paleoproterozoic|Paleoproterozoic|Mixed carbonate-clastic lithofacies.||||Isa Superbasin. Is overlain unconformably by Roper Group.|Tightly folded and faulted carbonate-rich succession.|
11512|McArthur Group|70968|6|Mentioned|p2 Fig.3, p6-7, p13, p17, p139|Paleoproterozoic|Paleoproterozoic|||||Is overlain unconformably by Limmen Sandstone (Roper Group).||
11512|McArthur Group|71059|5|Briefly described|iii, p2, p7|Paleoproterozoic|Paleoproterozoic|McArthur Basin.|||Includes Barney Creek Formation [in Umbolooga Subgroup].|Is overlain unconformably by Roper Group.||07-NOV-17
11512|McArthur Group|71374|4|Described|iii, p1 tbl 1, p2, p18-p19, p36|Palaeoproterozoic|Palaeoproterozoic|McArthur Basin. On the basis of SHRIMP ages is interpreted as broadly equivalent to the Habgood Group.|||Includes the Umbolooga Subgroup, Masterton Sandstone, Amos Formation and the Yalco Formation.|Overlain by the Nathan Group. Broadly equivalent to the Farquharson Sandstone.||
11512|McArthur Group|71606|5|Briefly described|p135,137-138|Statherian|Statherian|McArthur Basin. Evaporite-carbonate sequence.|||Includes Batten and Umbolooga subgroups.|||
11512|McArthur Group|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin. Informally subdivided into Lower, Middle and Upper parts||||||04-MAR-20
11512|McArthur Group|71779|5|Briefly described|p5|Palaeoproterozoic|Palaeoproterozoic|McArthur Basin.||||Disconformably or unconformably overlain by the Roper Group.||
11512|McArthur Group|71893|5|Briefly described|p13|Palaeoproterozoic|Palaeoproterozoic|McArthur Basin.||||Unconformably overlain by the Limmen Sandstone.||
11512|McArthur Group|72248|5|Briefly described|p145-148,156|||Of McArthur Basin. Thickness: ~5km. Carbonate-dominated sequence that is strongly fault controlled and constrained within Batten Fault Zone (Plumb and Wellman, 1987). Depositional environments: allvuvial and shallow marine at the top and base, deeper marine in the middle section.|||Includes Batten and Umbolooga subgroups.||Interbedded stromatolitic and evaporitic dolostone, sandstone, siltstone and shale.|13-SEP-19
11512|McArthur Group|72373|5|Briefly described|iii,p1-2,5,14,17,22,24,27,36,39|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin.|||Includes Umbolooga and Batten subgroups, Masterton Sandstone.|||02-OCT-19
11512|McArthur Group|72523|5|Briefly described|p1-2, p2 Fig.2, p8, p12.|Statherian|Statherian|Shown on p2 Fig.2 as extending south and north of the junction of Carpentaria Highway and Tablelands Highway.|||Includes Batten Subgroup, Umbolooga Subgroup.|Unconformably underlies Nathan Group.||
11512|McArthur Group|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Batten Fault Zone of the Southern McArthur Basin.|||Umbolooga Subgroup and Batten Subgroup|Overlies Tawallah Group and underlies Nathan Group and is shown as partially equivalent to Vizard Group.||
11512|McArthur Group|72527|6|Mentioned|p1, p194, p196.|Paleoproterozoic|Paleoproterozoic||1640-1650 Ma|||||
11512|McArthur Group|72711|6|Mentioned|p11, p11 Fig.8.|Statherian|Statherian|Mc Arthur Basin. Includes sulphate evaporites.|c. 1640 Ma.||||Includes pyrite.|
11512|McArthur Group|72718|6|Mentioned|piii, p2, p5-8, p20|Palaeoproterozoic|Palaeoproterozoic|Beetaloo Sub-basin, McArthur Basin. Isa Superbasin, Glyde package. Occurs within the Batten Fault Zone. Present as a veneer over the Daly Waters Fault Zone.|||Batten Sub-group, Umbolooga Sub-group and units therein|||
11512|McArthur Group|72912|4|Described|p5 Fig.3, p13, p18, p36, p48.|Paleoproterozic|Paleoproterozic|Located in the Batten Fault Zone of the Southern McArthur Basin.|||Umbolooga Subgroup and Batten Subgroup|Shown as unconformably overlying Tawallah Group, underlying Nathan Group and partially equivalent to Vizard Group.|Includes sandstone, shale and dolostone.|
11512|McArthur Group|72919|6|Mentioned|p98|Paleoproterozoic|Paleoproterozoic|||||||
11512|McArthur Group|72967|6|Mentioned|p2|Paleoproterozoic|Paleoproterozoic|||||||
11512|McArthur Group|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin, Isa Superbasin.|||Batten and Umbolooga subgroups, and units therein.|Unconformably overlain(?) by Smythe Sandstone (Nathan Group).||
11512|McArthur Group|73083|6|Mentioned|p37|Paleoproterozoic|Paleoproterozoic|||||||
11512|McArthur Group|73288|6|Mentioned|p708|Paleoproterozoic|Paleoproterozoic|McArthur Basin, NT. One of the main unconventional hydrocarbon targets in the Basin.||||||
11512|McArthur Group|73405|6|Mentioned|p241|Paleoproterozoic|Paleoproterozoic|Contains shallow-water or emergent sedimentary features.|||Barney Creek Formation.|||
11512|McArthur Group|73412|4|Described|p1-2, 4, 6-13, 15-21|||Southern McArthur Basin. Deposition followed a hiatus of c.30 m.y. Dry bulk density tabulated. Faults described in detail. Characterised by a prominent gravity high, very low magnetic susceptibility, and relatively uniform K-enriched radiometric signal.|c.1660-1610 Ma (SHRIMP: Munson, 2019).||Umbolooga and Batten Subgroups.|Unconformably overlies Tawallah Group. Is overlain unconformably by the Nathan Group.|A succession of carbonates, mudstones and sandstones. Shallow to moderately deep-water deposits.|
11530|McCaw Formation|22432|6|Mentioned|p20|||In the MacArthur Basin.||||||06-NOV-06
11530|McCaw Formation|22538|6|Mentioned|Fig3 P708|||||||||
11530|McCaw Formation|22748|6|Mentioned|p235 Fig.1|||||||||
11530|McCaw Formation|23216|5|Briefly described|Table1p9,24|||Previously mapped as Diamond Creek Member (Ruker, 1959).||||||
11530|McCaw Formation|23363|5|Briefly described|344 Fig.3|||||||||
11530|McCaw Formation|23374|3|Fully described|Tb2p10,17,18||Statherian|Unconformable below Gundi Sandstone. Of Katherine River Group, McArthur Basin.||||||06-NOV-06
11530|McCaw Formation|23396|5|Briefly described|p 407 fig.2|||Of Katherine River Group.||||||06-NOV-06
11530|McCaw Formation|23867|3|Fully described|p13|Paleoproterozoic|Paleoproterozoic|Of Katherine River Group.  Originally included in Diamond Creek Member of Diljin Hill Formation.  Max. thickness: 300m.  Geological Province: McArthur Basin.  See also Table 1 and Figs. 3 and 30.||||||07-NOV-08
11530|McCaw Formation|23937|4|Described|p7, p25 Tb. 2|Statherian|Statherian|Of the Katherine River Group.  Mapped as "Diamond Creek Formation" in URAPUNGA (Dunn, 1963a).  In KATHERINE they were subdivided into McCaw Fm and Diamond Creek Volcanics (Kruse et al, 1994).  Max. thick: 50m: 250m in KATHERINE. Geol.Prov: McArthur Basin.||||||03-NOV-04
11530|McCaw Formation|24048|5|Briefly described|p36|||Of the Katherine River Group..||||||06-NOV-06
11530|McCaw Formation|24050|2|Defined|p82 App. 1|Statherian|Statherian|Thickness estimated at ~200-250m (poor exposure).  Overlies Bonanza Creek Formation.  Considered to be stratigraphic equivalent of Wollogorang Formation.||||||23-DEC-09
11530|McCaw Formation|24051|5|Briefly described|Map Legend|Statherian|Statherian|Of Katherine River Group. Geological Province: McArthur Basin.||||||
11530|McCaw Formation|30318|6|Mentioned|p327|||||||||
11530|McCaw Formation|32660|5|Briefly described|Table 4|||||||||
11530|McCaw Formation|42597|5|Briefly described|Map Legend|Carpentarian||||||||
11530|McCaw Formation|43010|2|Defined|p103||Paleoproterozoic|Of Katherine River Group. Of Statherian age.||||||07-NOV-08
11530|McCaw Formation|43149|5|Briefly described|Map Legend||Paleoproterozoic|Of Katherine River Group. Of Statherian age.||||||07-NOV-08
11530|McCaw Formation|44112|6|Mentioned|p43,49|||||||||
11530|McCaw Formation|44400|2|Defined|p.8,Tb.1,opp.p.6,map|||Overlain by Gundi Greywacke. Mt.Marumba Sheet. (D53-6).||||||13-JAN-05
11530|McCaw Formation|44401|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
11530|McCaw Formation|45022|6|Mentioned|p.57,67,68.||Carpentarian|Of Katherine River Group.  Fig.15,16,17. Tb.3,4. Pl.28||||||
11530|McCaw Formation|60571|5|Briefly described|Map Legend|Statherian|Statherian|Of Katherine River Group. Sandstone: fine-grained, medium- to thick-bedded, massive, low angle trough cross bedded and planar laminations, lithic and feldspathic, minor glauconitic horizons; mudstone; dolomitic mudstone. Geol. Prov.: McArthur Basin.||||||30-NOV-04
11530|McCaw Formation|60680|5|Briefly described|Map legend|Statherian|Statherian|Of the Katherine River Group.  Interbedded deeply weathered and leached mudstone and thinly bedded dolostone. Geological Province: McArthur Basin. Overlies: Bananza Creek Formation. Underlies: Gundi Sandstone.||||||07-JAN-09
11530|McCaw Formation|61390|5|Briefly described|Map Legend|Statherian|Statherian|Of the Katherine River Group. Dolostone: fissile to flaggy, laminated to thin bedded; minor medium-coarse grained sandstone.||||||
11530|McCaw Formation|61572|5|Briefly described|p668 Fig. 3|||Siliciclastic and dolomitic rocks; some basalt and dolerite. Of Katherine River Group. Overlain by Gundi Sandstone; overlain by Bone Creek Sandstone. Max. thickness: 250m. Geological Province: McArthur Basin.||||||06-NOV-06
11530|McCaw Formation|64698|4|Described|lithinterp table|Statherian|Statherian|Age ~1720-1730Ma. McArthur Basin. Of Katherine River Group. Max. thickness 300m. Interbedded deeply weathered and leached mudstone and thinly bedded dolostone; thinly bedded, fine lithic and glauconitic sandstone.||||||07-JAN-09
11530|McCaw Formation|64817|6|Mentioned|p353 Fig.4, p355 Fig.5 |||Arnhem Shelf, McArthur Basin.||Of the Katherine River Group.|||Dolostone.|05-JUN-18
11530|McCaw Formation|65228|5|Briefly described|p7|||McArthur Basin. Contains distinctive carbonate lithofacies diagnostic of Wollogorang Formation, Tawallah Group.[ i.e. they are considered time-equivalents?]||Katherine River Group.||||13-DEC-17
11530|McCaw Formation|65232|5|Briefly described|p7 Fig. 6|||Of Katherine River Group. Underlies Gundi Sandstone; overlies Bonanza Creek Formation. 200-250m thick. Shallow-marine dololutite, carbonate.||||||09-FEB-10
11530|McCaw Formation|65340|6|Mentioned|pp92-93.|||Northern McArthur Basin. Correlated with Settlement Creek Dolerite and Lower Wollogorang Formation. Tentatively correlated with Aquarium Formation on the basis of similar lithofacies.||||||
11530|McCaw Formation|67564|3|Fully described|p6 Table 2, p10 Fig.5, p39 Fig.20, p49.|Paleoproterozoic|Paleoproterozoic|Contains rocks previously mapped by Walpole (1963) as the Diamond Creek Member of the now defunct Diljin Hill Formation. 300 m of marine shelf sediments. Poorly exposed.|1740 - 1720 Ma.|Unit in Katherine River Group.||Overlies Bonanza Creek Formation conformably. Is overlain ?unconformably by Gundi Sandstone.|Interbedded deeply weathered mudstone and thinly bedded dolostone; thinly bedded, lithic and glauconitic sandstone.|
11530|McCaw Formation|69430|4|Described|p15:3, 8-9, 30|||NW McArthur Basin. 250-300m thick. Shallow-marine shelf deposits. Contacts not observed.||Katherine River Group.||Overlies Bonanza Creek Formation probably conformably. Is overlain by Gundi Sandstone; also conformably by and interfingers with Diamond Creek Volcanics.|Medium to thick bedded, massive, planar laminated and trough cross-bedded feldspathic sandstone; minor glauconitic horizons and mudstone.|12-JUL-16
11530|McCaw Formation|69673|6|Mentioned|p16 fig 13|||Northwestern McArthur Basin.||Katherine River Group||Overlain by Gundi Sandstone, Jimbu Microgranite, Overlies Bonanza Creek Formation, Shadforth Sandstone||
11552|McKay Sandstone|9534|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Katherine River Group.||||||
11552|McKay Sandstone|9691|5|Briefly described|Map Legend|||Quartz sandstone, medium feldspathic sandstone, fine to medium ferruginous sandstone, greywacke, fine to medium siltstone. Of the Katherine River Group.||||||
11552|McKay Sandstone|9701|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Quartz sandstone, medium feldspathic sandstone, fine to medium ferruginous sandstone, greywacke, fine to medium siltstone. Of the Katherine River Group.||||||02-JUN-05
11552|McKay Sandstone|9733|5|Briefly described|Map Legend|Carpentarian|Carpentarian|Quartz sandstone, medium feldspathic sandstone, fine to medium ferruginous sandstone. Of the Katherine River Group.||||||
11552|McKay Sandstone|22538|6|Mentioned|Fig3 P708|||||||||
11552|McKay Sandstone|22748|6|Mentioned|p235 Fig.1|||||||||
11552|McKay Sandstone|23216|5|Briefly described|p20,22-3|||||||||
11552|McKay Sandstone|23363|5|Briefly described|344 Fig.3|||||||||
11552|McKay Sandstone|23374|3|Fully described|Tb2p10,16,17,27||Statherian|Part laterally equivalent to upper Marlgowa Sandstone. Of Kombolgie Subgroup, Katherine River Group, McArthur Basin.||||||06-NOV-06
11552|McKay Sandstone|23384|5|Briefly described|p26, Fig 27|||Of the Kombolgie Subgroup (Katherine River Group).||||||06-NOV-06
11552|McKay Sandstone|23396|5|Briefly described|p 407 fig.2|||Of Katherine River Group.||||||06-NOV-06
11552|McKay Sandstone|23867|3|Fully described|p7|Paleoproterozoic|Paleoproterozoic|Redefined by Brakel (1999).  Of Kombolgie Subgroup.  Max. thickness: 342m.  Geological Province: McArthur Basin.  See also Table 1, Figs. 3, 30 and p22 Appendix.||||||07-NOV-08
11552|McKay Sandstone|24050|2|Defined|p79 App. 1|Statherian|Statherian|Formerly mapped as parts of "Kombolgie Formation" and the "Diljin Hill Fm." (of Walpole, 1962).  Thickness at type section: 340m.  Overlies the Marlgowa Sandstone; underlies the Cottee Formation.  Probably correlates with Rosie Creek Sandstone.||||||23-DEC-09
11552|McKay Sandstone|24051|5|Briefly described|Map Legend|Statherian|Statherian|Of Kombolgie Subgroup, Katherine River Group. Geological Province: McArthur Basin.||||||
11552|McKay Sandstone|32660|5|Briefly described|Table 4|||||||||
11552|McKay Sandstone|36535|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
11552|McKay Sandstone|36635|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
11552|McKay Sandstone|37815|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
11552|McKay Sandstone|42597|5|Briefly described|Map Legend|Carpentarian||||||||
11552|McKay Sandstone|43010|2|Defined|p99||Paleoproterozoic|Of Katherine River Group. Of Statherian age.||||||07-NOV-08
11552|McKay Sandstone|43149|5|Briefly described|Map Legend||Paleoproterozoic|of Katherine River Group. Of Statherian age.||||||07-NOV-08
11552|McKay Sandstone|44400|2|Defined|p.7,Tb.1,opp.p.6,map|||Overlain by Cottee Formation. (D53-6).||||||06-NOV-06
11552|McKay Sandstone|44401|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
11552|McKay Sandstone|45022|4|Described|p.57,67,68.||Carpentarian|Of Katherine River Group.  Fig.15,16,17. Tb.3,4. Pl.28.||||||
11552|McKay Sandstone|50545|5|Briefly described|p114 Fig.1||Paleoproterozoic|Of Kombolgie Subgroup. Contains evaporites.||||||07-NOV-08
11552|McKay Sandstone|60550|5|Briefly described|Map Legend|Carpentarian|Carpentarian|Of the Katherine River Group. Quartz sandstone, medium feldspathic sandstone, fine to medium ferruginous sandstone, greywacke, siltstone.||||||
11552|McKay Sandstone|60571|5|Briefly described|Map legend|Statherian|Statherian|Of the Kombolgie Subgroup (Katherine River Group). Sandstone: white, red/brown to purple, fine- to medium grained, thin- to medium-bedded, trough cross-bedded, quartzose, lithic and/or ferruginous. Geological Province: McArthur Basin.||||||30-NOV-04
11552|McKay Sandstone|60680|5|Briefly described|Map legend|Statherian|Statherian|Of Kombolgie Subgroup (Katherine River Gp). Includes Snowdrop Sandstone Member.  Glauconitic quartz sandstone; thin grey-green laminated mudstone and siltstone interbeds. Geol.Prov: McArthur Basin. Overlies Marlgowa Sandstone. Underlies Cottee Formation||||||06-NOV-06
11552|McKay Sandstone|64698|4|Described|lithinterp table|Statherian|Statherian|Age ~1740-1780Ma. McArthur Basin. Of Katherine River Group. Max thick 250m. White to light grey-green, trough and hummocky cross-bedded, glauconitic qtz sandst; thin grey-green laminated mudst and siltst interbeds; minor fine pyritic lithic sandst.||||||07-JAN-09
11552|McKay Sandstone|64817|6|Mentioned|p353 Fig.4, p355 Fig.5 |||Arnhem Shelf, McArthur Basin.||Of the Kombolgie Subgroup.|||Sandstone and conglomerate.|04-JUN-18
11552|McKay Sandstone|65232|6|Mentioned|App. 2|||See also probable misspelling - Mackay Sandstone.||||||09-FEB-10
11552|McKay Sandstone|67057|6|Mentioned|p455.|||||Topmost unit in Kombolgie Subgroup.||Overlies Marlgowa Sandstone.||
11552|McKay Sandstone|67564|3|Fully described|p6 Table 2, p39 Fig.20, pp43-46, p86.|Paleoproterozoic|Paleoproterozoic|Roberts and Plumb (1965); included in Kombolgie Subgroup by Sweet et al. (1999). Walpole (1963) mapped rocks of this formation as lower Diljin Hill Formation (now defunct). Kruse et al. (1994) have mapped most of the McKay Sandstone in KATHERINE as part of Cottee Formation. 342 m of storm-dominated shelf to shoreline deposits. Brownish tones and subdued topography. Equivalent to Rosie Creek Member, southern McArthur Basin.||Unit in Kombolgie Subgroup.|Includes Snowdrop Sandstone Member.|Overlies Marlgowa Sandstone. Is overlain disconformably by Cottee Formation.|Glauconitic, fine to coarse sandstone; minor siltstone and mudstone.|
11552|McKay Sandstone|67779|6|Mentioned|p32.|Paleoproterozoic|Paleoproterozoic|||Topmost unit in Kombolgie Subgroup.||||
11552|McKay Sandstone|69430|4|Described|p15:3, 7-8|||NW McArthur Basin. This is shown as the topmost unit in Kombolgie Subgroup in 15:3, but elsewhere is treated as not part of the Subgroup. 340m thick. Shallow tidal marine deposits. Probably a lateral equivalent to the ferruginous facies in the upper Marlgowa Sandstone.||Katherine River Group.||Conformably and gradationally overlies Marlgowa Sandstone. Is overlain conformably by Cottee Formation.|White-grey, fine- to medium-grained, thin to medium bedded, trough cross-bedded quartz arenite; interbedded with red-brown to purple, recessive lithic and ferruginous sandstone.|12-JUL-16
11552|McKay Sandstone|69673|6|Mentioned|p16 fig 13|||Northwestern McArthur Basin.||Kombolgie Subgroup||Overlain by Cottee Formation, overlies Marlgowa Sandstone||
11575|McNamara Group|7071|5|Briefly described|p1|Mesoproterozoic|Paleoproterozoic|Geological Province: northern Mount Isa Inlier.||||||07-NOV-08
11575|McNamara Group|22438|6|Mentioned|p549, Fig.12|||||||||
11575|McNamara Group|22453|5|Briefly described|p 11|||NT and QLD||||||
11575|McNamara Group|22457|6|Mentioned|Fig29 P30|||||||||
11575|McNamara Group|22468|5|Briefly described|p 16, 17|||||||||
11575|McNamara Group|22585|6|Mentioned|Fig1 P736|||||||||
11575|McNamara Group|22644|5|Briefly described|5 fig 2|||Geol. province: Mount Isa Basin. Underlain by Fiery Creek Volcanics.||||||06-NOV-06
11575|McNamara Group|22665|6|Mentioned|P219, P227|||||||||
11575|McNamara Group|22680|5|Briefly described|83,85-87|Mesoproterozoic|Paleoproterozoic|Geol. province: Mount Isa Basin.||||||07-NOV-08
11575|McNamara Group|23031|5|Briefly described|21|Paleoproterozoic|Paleoproterozoic|Geological  province: Mount Isa Fold Belt.||||||07-NOV-08
11575|McNamara Group|23072|6|Mentioned|p754|||||||||
11575|McNamara Group|23073|5|Briefly described|p744|||||||||
11575|McNamara Group|23075|5|Briefly described|p730||Mesoproterozoic|Age: 1595+/-6 M yr.||||||06-NOV-06
11575|McNamara Group|23198|5|Briefly described|p873, 875||Paleoproterozoic|Age: Late Palaeoproterozoic. Informally referred to 'Lower McNamara Group".||||||07-NOV-08
11575|McNamara Group|23362|6|Mentioned|337|||||||||
11575|McNamara Group|23387|6|Mentioned|p18 fig.19|||||||||
11575|McNamara Group|23393|5|Briefly described|p11, p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Fold Belt.||||||07-NOV-08
11575|McNamara Group|23395|6|Mentioned|p383|||||||||
11575|McNamara Group|23396|5|Briefly described|p407 Fig.2|||||||||
11575|McNamara Group|23397|5|Briefly described|p463|||||||||
11575|McNamara Group|23398|5|Briefly described|p441|||||||||
11575|McNamara Group|23399|5|Briefly described|p487|||||||||
11575|McNamara Group|23405|4|Described|p566|||Lawn Hill Platform.||||||
11575|McNamara Group|23406|5|Briefly described|p601 Fig. 3, p603-4, p607 Fig. 8|||Includes 11 named formations (see p607 Fig. 8). Geological province: Isa Superbasin.  Lower part is of ramp carbonates and clastics; upper is clastics.||||||22-JUL-13
11575|McNamara Group|23408|5|Briefly described|p509, p513 Fig. 2|||Previous interpretations of this group are included. Comprises: Torpedo Ck. Quartzite, Gunpowder Ck., Paradise Ck., Esperanza, Lady Loretta Fms., Shady Bore Quartzite, Riversleigh and Lawn Hill Fms (Hutton et al 1981). On Lawn Hill Platform||||||15-JUN-09
11575|McNamara Group|23409|4|Described|p537|||Of Lawn Hill Platform.||||||21-SEP-06
11575|McNamara Group|23448|5|Briefly described|p479|||||||||
11575|McNamara Group|23466|5|Briefly described|p267|||||||||
11575|McNamara Group|23518|4|Described|p9 Fig. 3, p12|Proterozoic|Proterozoic|Geological Province: Western Fold Belt.||||||
11575|McNamara Group|23957|6|Mentioned|p1123|||||||||
11575|McNamara Group|23958|4|Described|p1132|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
11575|McNamara Group|23964|5|Briefly described|p1265|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier.||||||
11575|McNamara Group|23965|5|Briefly described|p1297|Mesoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier.||||||07-NOV-08
11575|McNamara Group|23986|5|Briefly described|p65|||||||||21-SEP-06
11575|McNamara Group|24034|5|Briefly described|p9|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier. Quartzite, siltstone, stromatolitic dolomite, laminated siltstone, dolomitic siltstone, orthoquartzite, shale and fine-grained sandstone.||||||
11575|McNamara Group|24308|5|Briefly described|p990, p987 Fig.2|Mesoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Superbasin||||||07-NOV-08
11575|McNamara Group|24309|5|Briefly described|p1013|||||||||
11575|McNamara Group|24419|5|Briefly described|p12 Fig.4, p13 Fig.5, p14, p17|Paleoproterozoic|Paleoproterozoic|Includes the Gunpowder Creek Formation. In URANDANGI 1:250 000 sheet area the McNamara Group is represented by the upper Gunpowder Creek Formation. Unconformably overlies Yaringa Metamorphics. Geol.Prov: Isa Superbasin.||||||07-NOV-08
11575|McNamara Group|24432|5|Briefly described|p562 Fig.2|Calymmian|Statherian|Geological Province: Lawn Hill Platform.||||||28-JAN-05
11575|McNamara Group|24442|6|Mentioned|p22, p23 Fig. 2|Mesoproterozoic|Mesoproterozoic|Includes Lawn Hill, Plain Creek, Formations, Shady Bore Quartzite and Musselbrook Formation.  Age: 1670-1600Ma.  Geological Province: McArthur Basin.||||||
11575|McNamara Group|30534|6|Mentioned|p300|||See also p305.||||||21-SEP-06
11575|McNamara Group|31342|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
11575|McNamara Group|33900|6|Mentioned|p4|||||||||
11575|McNamara Group|35074|6|Mentioned|Fig.2|||||||||
11575|McNamara Group|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
11575|McNamara Group|36548|6|Mentioned|p513|||||||||
11575|McNamara Group|37459|2|Defined|p426|Mesoproterozoic|Mesoproterozoic|Age is more specifically Carpentarian||||||
11575|McNamara Group|37462|4|Described|Table4.VII|||||||||
11575|McNamara Group|37565|6|Mentioned|Fig.5|||||||||
11575|McNamara Group|37568|4|Described|p84|||||||||
11575|McNamara Group|37569|6|Mentioned|p91|||||||||
11575|McNamara Group|37816|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
11575|McNamara Group|38232|6|Mentioned|p82|||||||||
11575|McNamara Group|38234|6|Mentioned|Fig.2|||||||||
11575|McNamara Group|38235|6|Mentioned|p117|||||||||
11575|McNamara Group|38237|4|Described|p127|||||||||
11575|McNamara Group|38276|6|Mentioned|Fig.1|||||||||
11575|McNamara Group|38278|6|Mentioned|Fig.1|||||||||
11575|McNamara Group|38291|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
11575|McNamara Group|38348|4|Described|p5|||||||||
11575|McNamara Group|38350|4|Described|p15|||||||||
11575|McNamara Group|38584|6|Mentioned|p17|||||||||
11575|McNamara Group|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
11575|McNamara Group|38835|6|Mentioned|p164|||||||||
11575|McNamara Group|38836|6|Mentioned|p165|||||||||
11575|McNamara Group|38919|6|Mentioned|p496|||||||||
11575|McNamara Group|39043|6|Mentioned|p10|||||||||
11575|McNamara Group|39338|6|Mentioned|p351|||See also Fig.1.||||||
11575|McNamara Group|39422|5|Briefly described|Map legend|Carpentarian|Carpentarian|Includes the Lawn Hill, Plain Creek and Musselbrook Formations.||||||10-JAN-05
11575|McNamara Group|39445|4|Described|p41|||Carp. Shallow marine. Lawn Hill Platform. See also pp36,55,56 and Table 2.||||||21-SEP-06
11575|McNamara Group|39492|6|Mentioned|p31|||||||||
11575|McNamara Group|39497|4|Described|p11|||||||||
11575|McNamara Group|39556|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||
11575|McNamara Group|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||15-JUN-06
11575|McNamara Group|39622|6|Mentioned|Fig.2|||||||||
11575|McNamara Group|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
11575|McNamara Group|39925|6|Mentioned|p329|||See also Fig.2.||||||
11575|McNamara Group|39934|6|Mentioned|p317|||See also Fig.3.||||||
11575|McNamara Group|39944|6|Mentioned|p228|||||||||
11575|McNamara Group|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
11575|McNamara Group|40221|3|Fully described|p13|||||||||
11575|McNamara Group|40394|6|Mentioned|Fig.2|||||||||
11575|McNamara Group|40840|6|Mentioned|Map legend|||||||||
11575|McNamara Group|41298|6|Mentioned|Map legend|Carpentarian||||||||
11575|McNamara Group|41307|5|Briefly described|p16|||||||||
11575|McNamara Group|41381|6|Mentioned|p325|||||||||
11575|McNamara Group|41862|6|Mentioned|p474|||||||||
11575|McNamara Group|41978|6|Mentioned|p502|||||||||
11575|McNamara Group|41979|5|Briefly described|p514|||||||||
11575|McNamara Group|42367|4|Described|p18||Proterozoic|Correlated with Mount Isa Group.||||||18-JAN-07
11575|McNamara Group|42565|5|Briefly described|Table 1 P5, P4|||||||||
11575|McNamara Group|42706|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Age: ~1870Ma. Dolomite, siltstone, chert, sandstone, conglomerate.||||||09-FEB-09
11575|McNamara Group|42766|5|Briefly described|p1|||||||||
11575|McNamara Group|42819|5|Briefly described|p312|||||||||
11575|McNamara Group|43107|6|Mentioned|p8|||||||||
11575|McNamara Group|43235|6|Mentioned|p8|||Proterozoic||||||
11575|McNamara Group|43486|5|Briefly described|21|||||||||
11575|McNamara Group|43608|6|Mentioned|Fig.11,p11|||||||||
11575|McNamara Group|43615|6|Mentioned|p13|||||||||
11575|McNamara Group|43616|6|Mentioned|p2|||||||||
11575|McNamara Group|43652|6|Mentioned|p388|||||||||
11575|McNamara Group|44195|6|Mentioned|p350|||||||||
11575|McNamara Group|44922|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
11575|McNamara Group|45161|4|Described|p12|||||||||
11575|McNamara Group|45166|4|Described|p29|||||||||
11575|McNamara Group|46598|5|Briefly described|p307|||||||||
11575|McNamara Group|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
11575|McNamara Group|46960|6|Mentioned|p216|||||||||
11575|McNamara Group|47083|3|Fully described|p14-18||Proterozoic|Age: 1470-1490 Ma upper age limit. Correlates with Mount Isa Group. Unconformably overlain by Thorntonia Fm; unconformably underlain by Surprise Crk Fm. Max thickness: 4000 m.||||||21-SEP-06
11575|McNamara Group|49018|6|Mentioned|p6|||||||||
11575|McNamara Group|49041|5|Briefly described|Table 1|||||||||
11575|McNamara Group|50225|5|Briefly described|p406 Fig. 10, p407|Paleoproterozoic|Paleoproterozoic|Geological Province: Isa Superbasin.||||||07-FEB-11
11575|McNamara Group|50536|5|Briefly described|p11.3|Paleoproterozoic|Paleoproterozoic|Age: ~1670Ma.||||||07-NOV-08
11575|McNamara Group|50550|6|Mentioned|p1140|||Geological Province: Western Fold Belt.||||||19-DEC-07
11575|McNamara Group|50624|5|Briefly described|p234 Fig.2|Calymmian|Statherian|U-Pb ages: Upper: 1595 +/-6 Ma, Lower: 1653 +/-7 Ma.||||||22-JUL-13
11575|McNamara Group|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Includes: Gunpowder Creek Formation, Torpedo Creek Quartzite.||||||
11575|McNamara Group|60558|5|Briefly described|p3, p5 Fig. 4|||Includes eight units.||||||03-JUN-09
11575|McNamara Group|61262|5|Briefly described|p455 Fig. 11|Mesoproterozoic|Paleoproterozoic|Geological Province: western Mount Isa Block.||||||07-NOV-08
11575|McNamara Group|61736|5|Briefly described|p673|Paleoproterozoic|Paleoproterozoic|Includes the Riversleigh Siltstone. Depositional age range: 1653+/-7Ma and 1658+/-3Ma for tuffaceous units.||||||
11575|McNamara Group|61904|5|Briefly described|p132 Fig. 2|Proterozoic|Proterozoic|Includes Lawn Hill Formation as youngest section. Max. thickness: 10km. Fine-grained clastic sediments and minor volcanic rocks hosting base metal deposits of Mt. Isa, Hilton, Hilton North and Lady Loretta.||||||
11575|McNamara Group|61913|5|Briefly described|p161|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
11575|McNamara Group|61922|5|Briefly described|p9 Fig. 3, p10|Mesoproterozoic|Paleoproterozoic|Age: ~1660-1595Ma.  Geological Province: Mount Isa Inlier. See also p21 Fig.13.||||||07-NOV-08
11575|McNamara Group|61929|5|Briefly described|p128 Fig. 2|Mesoproterozoic|Paleoproterozoic|Age: 1653+/-7 to 1595+/-6Ma.||||||07-NOV-08
11575|McNamara Group|61936|5|Briefly described|p194 Fig. 6|Mesoproterozoic|Paleoproterozoic|Age: >1650-1600Ma.Shown to include Walford Dolomite, Mount Les Siltstone and Doomadgee Formation in figure; these also included in the correlating Fickling Group in the southern Murphy Inlier. Geol.Prov: Lawn Hill Platform, Western F.B., Mount Isa Inlier||||||07-NOV-08
11575|McNamara Group|62084|5|Briefly described|p936 Fig.5, p938|||Isa Superbasin. Lawn Hill. Hosts Mount Isa, Hilton and George Fisher deposits (Zn-Pb-Ag mineralisation).|||Gunpowder Creek Formation, Paradise Creek Formation, Esperanza Formation, Lady Loretta Formation, Shady Bore Quartzite, Riversleigh Siltstone, Termite Range Formation, Lawn Hill Formation|||
11575|McNamara Group|62473|5|Briefly described|p75||Paleoproterozoic|Contains the Riversleigh Formation. Age: ca. 1640Ma.||||||17-JUN-09
11575|McNamara Group|62535|5|Briefly described|p672-674|Statherian|Statherian|Lawn Hill Platform. Age of redeposited tuffaceous unit in the lower part of the Group.|1658 +/- 3 Ma.||Torpedo Creek, Shady Bore Quartzites; Gunpowder, Paradise Creek, Esperanza, Lady Loretta Formations; Mount Les, Riversleigh Siltstones.|||
11575|McNamara Group|62592|5|Briefly described|p73.|||Mount Isa Inlier. Upper parts are equivalent to the presumed deposition of topmost Willyama Supergroup, subsequently removed.||||||
11575|McNamara Group|62659|5|Briefly described|Map Legend|Calymmian|Statherian|||||||
11575|McNamara Group|63023|5|Briefly described|p1025 Fig. 2|||Geological Province: Isa Superbasin.||||||
11575|McNamara Group|63113|5|Briefly described|p1214 Fig.2.|||Isa Superbasin.|c.1659-c.1589 Ma.||Includes Shady Bore and Torpedo Creek Quartzites; Riversleigh Siltstone; Lady Loretta, Esperanza, Paradise Creek, Gunpowder Creek, Termite Range and Lawn Hill Formations.|||
11575|McNamara Group|63114|6|Mentioned|p1252.|||Lawn Hill platform, Isa superbasin.|||||Carbonate, carbonaceous siltstone, shale.|
11575|McNamara Group|63593|5|Briefly described|p288 Fig.2, p291 Fig.3 and Tb.2.|||Western Fold Belt.|Between c.1700 and 1670 Ma.|||Is intruded by Sybella Granite.|Siltstone, sandstone, shale.|
11575|McNamara Group|63866|6|Mentioned|p52|||||||||
11575|McNamara Group|63884|5|Briefly described|p14|||Predominantly sideritic and locally carbonaceous shale, mudstone and sandstone.||||||
11575|McNamara Group|64137|6|Mentioned|p1544|||McArthur River area. Same age as Tarcoola Formation.||||||
11575|McNamara Group|64250|6|Mentioned|p25 fig 10, p19, p24|||Western Fold Belt, Mount Isa Inlier.|c.1660 Ma - 1595 +/- 6 Ma|||||
11575|McNamara Group|64317|6|Mentioned|p588, p601|||||||||
11575|McNamara Group|64724|5|Briefly described|p45 Fig.5, p46|Calymmian|Statherian|Lawn Hill Platform / Mt Isa Inlier unit deposited as part of sedimentation in the Isa Superbasin (1660-1590 Ma)||||||02-APR-12
11575|McNamara Group|64725|6|Mentioned|p58 Fig.2. |||Mount Isa Inlier.||||||
11575|McNamara Group|64743|6|Mentioned|p342. |Paleoproterozoic|Paleoproterozoic|Mount Isa Inlier. A sequence of sag-phase sediments up to c.8 km thick.|1650-1590 Ma.|||Equivalent to Paragon Group, Broken Hill Block.||
11575|McNamara Group|64744|5|Briefly described|p353 Fig.4, p354. ||Statherian|Mount Isa Basin.|||||Fluviatile to shallow marine sandstones, siltstones and dolostones; lesser intercalated black shale.|
11575|McNamara Group|64815|6|Mentioned|p3, |||||||||
11575|McNamara Group|65209|6|Mentioned|p38|||||||correlates with Namerinni Group||
11575|McNamara Group|65228|6|Mentioned|p8, p16|Proterozoic||Most complete stratigraphic sections in Lawn Hill Platform area. Contains cauliflower chert nodules and other ?evaporite pseudomorphs.||||||
11575|McNamara Group|65337|4|Described|p v, p6 Fig.3.  |Mesoproterozoic|Paleoproterozoic|Deposited in a variety of shallow-marine settings.|c.1670-1590 Ma.||Has Gunpowder Creek, Paradise Creek, Esperanza, Lady Loretta, Drummond, Brumby, Plain Creek, Termite Range, Lawn Hill Formations; Shady Bore Quartzite, Riversleigh Siltstone and Bullrush Conglomerate|Disconformably, locally unconformably, overlies Surprise Creek Formation.|Mixed succession of siliciclastic and carbonate rocks: shallow-marine sandstone, red-beds,stromatolitic and evaporitic dolostone and chert; fan delta sandstone and conglomerate; mudstone, siltstone and minor dolostone.|
11575|McNamara Group|65387|6|Mentioned|p85|||Widespread volcanism around 1690-1650 Ma is evident from tuff layers in this unit and the Mount Isa Group.||||||
11575|McNamara Group|65396|5|Briefly described|p82, p175, p188, p197, p241, p439|Calymmian|Statherian|Isa Superbasin: Western Fold Belt. Hosts giant shale-hosted Pb-Zn-Ag+/-Cu deposits.|1660 - 1595 +/- 6 Ma||Lower and Upper Gunpowder Creek Formation, Paradise Creek, Esperanza, Lady Loretta, Riversleigh, Termite Range, Lawn Hill Formations; Shady Bore Quartzite.|||04-APR-17
11575|McNamara Group|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).||||||
11575|McNamara Group|66824|6|Mentioned|p133, 148|||Local occurrence of Sybella Granite pebbles in basal conglomerate.||||Is faulted against and unconformably overlies Sybella Granite. Equivalent to Mount Isa Group.||
11575|McNamara Group|66843|6|Mentioned|p36||||||Includes Lawn Hill Formation.|||12-SEP-19
11575|McNamara Group|66844|5|Briefly described|p244-245|||Lawn Hill and Gunpowder region. This paper concentrates on the lower part of this Group. SE-thickening, characterised by extensional or transtentional faults, deposited in an intracratonic rift basin.|||Includes Prize, Gun, Loretta, River, Term, Lawn, Wide and Doom Supersequences.|Unconformably overlies Fiery Creek Formation.||
11575|McNamara Group|67323|4|Described|p10-11, p26, p34-36, p39, p60, p107|||See also GIS attrib tbl, Solid Geology Map. Century, Mount Oxide, Camooweal-Murphy and Ardmore-May Downs Domains, Mount Isa Inlier. Formally subdivided and informally subdivided to show altered rocks as separate unit. The upper part of the Group (deposited ~1620-1595 Ma) contains the Lawn, Wide and Doom Supersequences. CONSTITUENTS (continued): Plain Creek Formation, Riversleigh Siltstone, Shady Bore Quartzite, Termite Range Formation, Torpedo Creek Quartzite.|~1660-1595 Ma.||Includes  Esperanza Formation, Gun Supersequence, Gunpowder Creek Formation, Lady Loretta Formation, Lawn Hill Formation, Mount Oxide Chert Member, Paradise Creek Formation. See COMMENTS for more.|Geophysics show that Yeldham Granite underlies.|Includes altered carbonate rocks - some leached, porous beds, some silicified and/or ferruginised|
11575|McNamara Group|67499|6|Mentioned|p939|||Occurs about 220km northwest of Mt Isa.||||Stratigraphically equivalent to the Mt Isa Group. Overlain by the South Nicholson Group.||08-MAY-12
11575|McNamara Group|67539|6|Mentioned|p14|||||||Unconformably overlain by Constance Sandstone, South Nicholson Group.||
11575|McNamara Group|68021|6|Mentioned|p135 fig 4|Statherian|Statherian|Western Succession.||||Overlies Surprise Creek Formation.||
11575|McNamara Group|68146|6|Mentioned|p196|||||||Underlies South Nicholson Group.||
11575|McNamara Group|68542|6|Mentioned|p6|||Of Andrews (1998).|||Inclydes informal Lower and Upper McNamara Groups.|Is overlain unconformably by South Nicholson Group.||22-OCT-19
11575|McNamara Group|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province.||||||
11575|McNamara Group|68576|5|Briefly described|Q_2: p6|||Andrews (1998).|||Lower and Upper McNamara Groups.|Is overlain unconformably by South Nicholson Group.||
11575|McNamara Group|68732|5|Briefly described|p159-162||||||Includes the Paradise Creek Formation, Esperanza Formation, and Lady Loretta Formation.||Contains braided fluvial cross-stratified quartzites and pebbly quartzites at or near its base.|01-DEC-17
11575|McNamara Group|69222|5|Briefly described|p221|Calymmian|Statherian|Lawn Hill Platform; across the Western Fold Belt it is called the Mount Isa Group. Age range c.1653-1595 Ma.|1653 +/- 7 Ma|||Overlies Surprise Creek Formation, Correlated with Mount Isa Group||09-FEB-18
11575|McNamara Group|69370|6|Mentioned|p307 Fig.2|Calymmian|Statherian|Western Fold Belt, Mount Isa Block.||||Is intruded by Sybella Granite.||25-JAN-19
11575|McNamara Group|69417|6|Mentioned|p2:5-6|Statherian|Statherian|South Nicholson/Lawn Hill Basin.||||||12-JUL-16
11575|McNamara Group|69433|4|Described|p18:2-3, 5-6, 8-10|Statherian|Statherian|Sweet and Hutton (1982), Hutton et al. (1981). Southern succession, Lawn Hill Platform. Hosts the world-class Century Zn-Pb-Ag deposit, in Qld, 60km E of the border. The unit's extension into NT should be considered prospective.|c.1690-1595 Ma (Page et al., 2000).||Drummond, Brumby, Plain Creek, Lawn Hill Formations; Bullrush Conglomerate; Shady Bore Quartzite.|Overlies Carrara Range Group unconformably, and Surprise Creek Formation disconformably or unconformably. Correlated with Fickling Group.|Sandstone, conglomerate, siltstone, shale and various carbonate rocks, commonly silicified to chert in outcrop.|12-JUL-16
11575|McNamara Group|69434|5|Briefly described|p19:4, 6|Paleoproterozoic|Paleoproterozoic|Lawn Hill Platform. A possible correlative of Caulfield beds (South Nicholson Basin).||||Is overlain unconformably by Accident Subgroup (South Nicholson Group).||12-JUL-16
11575|McNamara Group|69443|6|Mentioned|p28:19|||Lawn Hill Platform.|||Lawn Hill Formation.|||12-JUL-16
11575|McNamara Group|69591|4|Described|p29, p41-44, p46, p54, p108|Paleoproterozoic|Paleoproterozoic|See also p109 Fig.2.106, p111. Lawn Hill Platform. Marks the onset of deposition in the Isa Superbasin.|~1650-1595 Ma.||Torpedo Creek, Shady Bore Quartzites; Gunpowder Creek, Paradise Creek, Esperanza, Lady Loretta, Lawn Hill, Termite Range, Plain Creek Formations; Riversleigh Siltstone.|Coeval with Mount Isa Group. The upper part is correlated with the Milo beds.|Arenites, argillites and carbonate platform rocks, followed by deepwater carbonaceous clastics. Uppermost sediments are fluvial.|
11575|McNamara Group|69673|6|Mentioned|p3 fig 2, p51|Calymmian|Statherian||1690-1595 Ma||Includes Widdallion Sandstone Member, Lawn Hill Formation, Plain Creek Formation, Shady Bore Quartzite, Bullrush Conglomerate, Brumby Formation, Drummond Formation|Correlated with Fickling Group|Sandstone, conglomerate, siltstone, shale and various carbonate rocks which are commonly silicified to chert.|
11575|McNamara Group|70864|5|Briefly described|p75, 74 Fig 2|Mesoproterozoic|Paleoproterozoic||||Includes Torpedo Creek Quartzite, Gunpowder Creek Formation, Paradise Creek Formation, Esperanza Formation, Lady Loretta Formation, Shady Bore Quartzite||Dolomitic and carbonaceous siltstones.|
11575|McNamara Group|70897|5|Briefly described|p36-37, p39, p41-42, p45|Paleoproterozoic|Paleoproterozoic|Mixed carbonate-clastic lithofacies. Source of 1680 Ma zircons in Mullera Formation. Uppermost units deposited c.1590 Ma.|c.1640 Ma.|||Isa Superbasin. Is overlain unconformably by South Nicholson Group.||
11575|McNamara Group|71369|5|Briefly described|p4, p10-11, p24, p33, p36, p49|||Underwent moderate folding but little metamorphism during the 1585-1500 Ma Mount Isa Orogeny. Basement for South Nicholson Group.||||Is overlain unconformably by South Nicholson Group.||20-FEB-18
11575|McNamara Group|71606|5|Briefly described|p137|Statherian|Statherian|South Nicholson Basin, and Lawn Hill Platform, Mount Isa Inlier.||||Underlain unconformably by Carrara Range Group. Equivalent to McNamara Group.||
11575|McNamara Group|71960|6|Mentioned|p85, p86 Fig. 8|||||||Shown as equivalent to Mount Isa Group.||
11575|McNamara Group|72408|4|Described|map sheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet.|||Includes Lawn Hill Formation.|||
11575|McNamara Group|72414|4|Described|map sheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.|||Includes Lawn Hill Formation.|||
11575|McNamara Group|72415|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.|||Includes Lawn Hill Formation, Termite Range Formation.|||
11575|McNamara Group|72416|4|Described|map sheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet Geological Compilation Series. Includes the Wide Supersequence, Lawn Supersequence and the Term Supersequence-3.|||Includes Lawn Hill Formation, Termite Range Formation.|||19-MAR-20
11575|McNamara Group|72418|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet.|||Includes Lawn Hill Formation, Terminte Range Formation, Plain Creek Formation, Riversleigh Siltstone.|||
11575|McNamara Group|72421|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.|||Includes Lawn Hill Formation, Terminte Range Formation, Plain Creek Formation, Riversleigh Siltstone.|||
11575|McNamara Group|72422|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.|||Includes Lawn Hill Formation, Terminte Range Formation, Plain Creek Formation, Riversleigh Siltstone.|||
11575|McNamara Group|72423|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet Geological Compilation Series. Incorporates the Wide Supersequence and the Term Supersequence 1-3.|||Includes Lawn Hill Formation, Terminte Range Formation, Plain Creek Formation, Riversleigh Siltstone.||Grey to brown, siltstone and shale, tuffaceous siltstone and sandstone, feldspathic, micaceous sandstone and siltstone interbeds, minor dolomite.|18-MAR-20
11575|McNamara Group|72526|5|Briefly described|p1, p4, p6, p8, p10, p85-86.|Calymmian|Statherian|Shown as located in the Lawn Hill Platform of the Mount Isa Province and the east part of the South Nicholson Basin. Shown p8 to be Statherian, but stated p1 to be late Paleoproterozoic to earliest Mesoproterozoic.Depositional ages from Page and Sweet, 1998; Page et al., 2000.|c. 1658 Ma to 1595 Ma dep. age from tuff (p4)||Gunpowder Creek, Paradise Creek, Esperanza, Lady Loretta, Termite Range, Lawn Hill, Drummond, Brumby, Plain Creek Formations; Shady Bore Quartzite, Riversleigh Siltstone, Bullrush Conglomerate.|Shown as partially overlying Sybella Granite and Gunpowder Creek Formation and shown as underlying South Nicholson Group.|Inlcudes quartzite and conglomerate.|
11575|McNamara Group|72527|4|Described|p1,p3, p5, p10, p12, p27, p87, p91, p98|Paleoproterozoic|Paleoproterozoic|See also p105, p112, p119-120, p132, p140, p147, p161, p193-196.|||Includes Widdallion Sandstone Member, Lawn Hill Formation, Plain Creek Formation, Shady Bore Quartzite, Brumby Formation, Bullrush Conglomerate, Drummond Formation, Paradise Creek Formation.|Unconformably underlies the South Nicholson Group. Possible correlation with Benmara Group.|Includes friable brown to purple lithic and micaceous fine to coarse-grained sandstone and minor laminated siltstone and claystone. Quartzite with abundant pebble lags and gritty lenses, bedded polymict granule, pebble to cobble conglomerate.|
11575|McNamara Group|72889|6|Mentioned|p6 Fig.i.|||||||||
11575|McNamara Group|72912|4|Described|p5 Fig.3, p13-14, p17, p24-25.|Paleoproterozic|Paleoproterozic|Part of Isa Superbasin. Shown as being located in both Queensland and Northern Territory. Located in the Lawn Hill Platform of the Mount Isa Province, and the East part of the South Nicholson Basin. Has potential to host shale gas deposits. See also p32, p33, p35, p45-47.|||Gunpowder Creek, Paradise Creek, Esperanza, Lady Loretta, Termite Range, Lawn Hill, Drummond, Brumby, Plain Creek Formations; Shady Bore Quartzite, Riversleigh Siltstone, Bullrush Conglomerate.|Shown as partially underlying South Nicholson Group.|Mixed clastic sediments and carbonates.|
11575|McNamara Group|72913|5|Briefly described|p7, p9 Tb.1.|Paleoproterozoic|Paleoproterozoic|Shown as being in the Lawn Hill Platform and eastern part of the Isa Superbasin.|||Includes Lawn Hill Formation, Termite Range Formation, Riversleigh Siltstone, Lady Loretta Formation, Shady Bore Quartzite, Esperanza Formation, Paradise Creek Formation, Gunpowder Creek Formation.|Shown as lateral equivalent to Fickling Group and underlying South Nicholson Group.|Include organic rich siltstone, dolomitic siltstone, sandstone, dolostone.|
11575|McNamara Group|72919|6|Mentioned|p3, p5, p25, p71, p98|Paleoproterozoic|Paleoproterozoic|Isa Superbasin.|||Lawn Hill Formation, Plain Creek Formation, Shady Bore Quartzite, Brumby Formation, Drummond Formation, Bullrush Conglomerate|Unconformably underlain by Surprise Creek Formation. Unconformably overlain by Wangalinji Member (Playford Sandstone, Wild Cow Subgroup, South Nicholson Group). Equivalent to Benmara Group.||
11575|McNamara Group|72949|6|Mentioned|p35|Calymmian|Statherian|Mount Isa Inlier, Western Fold Belt.||||||
11575|McNamara Group|72967|6|Mentioned|p2, p6|Paleoproterozoic|Paleoproterozoic|Lawn Hill Platform.|||Lawn Hill Formation, Termite Range Formation, Riversleigh Siltstone, Walford Dolostone*, Lady Loretta Formation|||
11575|McNamara Group|73042|6|Mentioned|p1, p3-4, p6, p11, p13|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin region and Mount Isa Province.|||Riversleigh Siltstone, Lawn Hill Formation and more (see p4 Fig.1.2).|||
11575|McNamara Group|73083|6|Mentioned|p35, p72|Paleoproterozoic|Paleoproterozoic|||||||
11575|McNamara Group|73137|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|||||||
11575|McNamara Group|73144|6|Mentioned|p8|Calymmian|Statherian|Isa Superbasin. [informal upper and lower are indicated in Fig.2]. Spans the Doom, Wide, Lawn, Term, River, Loretta, and Gun supersequences. Includes aquifers, partial aquifers, leaky aquitards and aquitards. Includes potential shale gas/oil plays and potential tight gas/oil.|||Lawn Hill Formation, Termite Range Formation, Riversleigh Siltstone, Lady Loretta Formation, Esperanza Formation, Paradise Creek Formation, Gunpowder Creek Formation, and members therein|||14-OCT-22
11575|McNamara Group|73413|6|Mentioned|p3|||Mount Isa Inlier, Western Fold Belt, Lawn Hill Platform.||||||
11575|McNamara Group|73418|6|Mentioned|p4|||Mount Oxide Domain.|||||Carbonaceous metasedimentary rocks.|
11649|Mendip Metamorphics|33103|4|Described|Table 1|||Mention p14.||||||06-NOV-06
11649|Mendip Metamorphics|33104|6|Mentioned|Map legend|Precambrian|Precambrian|||||||
11649|Mendip Metamorphics|39887|6|Mentioned|Table 1|||See also Fig.5||||||
11649|Mendip Metamorphics|39888|6|Mentioned|Table 1|||||||||
11649|Mendip Metamorphics|50369|6|Mentioned|p26.2|||||||||
11649|Mendip Metamorphics|61208|5|Briefly described|p208, p207 Fig. 1|Late Neoproterozoic|Paleoproterozoic|Consist of a sequence of quartzite (thickly bedded) and biotite gneiss with minor amounts of granule conglomerate, calc-silicate and amphibolite. Geological Province: eastern Arunta Inlier.||||||07-NOV-08
11649|Mendip Metamorphics|64068|5|Briefly described|p32|||Bundled in with Ledan Schist and Utopia Quartzite as the 1770-1740 Ma Ledan package.||||||
11649|Mendip Metamorphics|64574|6|Mentioned|p704 Fig. 1|Paleoproterozoic|Paleoproterozoic|||||||
11649|Mendip Metamorphics|64738|5|Briefly described|p248, p250, Table 1.|Paleoproterozoic|Paleoproterozoic|Subjected to two episodes of high-grade metamorphism: Strangways and Chewings events. Metamorphic zircon overgrowths range from c.1740-1680 Ma, averaging 1723 +/- 9 Ma. Intruded by a pegmatite aged 1730 +/- 4 Ma.||||||
11649|Mendip Metamorphics|65341|5|Briefly described|p2 Fig.2, p7. |Paleoproterozoic|Paleoproterozoic|Intruded by pegmatite at 1730 +/- 4 Ma and has metamorphic zircon rims aged 1723 +/- 9 Ma (Maidment et al. 2005). Considered part of same sedimentary package as Ledan Schist and Utopia Quartzite.|Max. deposition c.1760 Ma (Maidment et al. 2005).|||||19-JUN-13
11649|Mendip Metamorphics|67181|5|Briefly described|p631|Statherian|Statherian|Aileron Province, North Australian Craton|1770-1730 Ma (Maidment et al. 2005)|Unit in Ledan Package||||
11649|Mendip Metamorphics|68150|5|Briefly described|p11 Tb.3.2|||Age: SHRIMP, MSWD 0.8, 30 analyses, Maidment et al. (2005).|1723 +/- 9, metamorphism|||||
11649|Mendip Metamorphics|69227|5|Briefly described|p281|||Shaw and Warren (1975). Age unknown.||||Unconformably overlies the Bleechmore Granulite.|A sequence of lower- to mid-amphibolite facies metasediments.|
11649|Mendip Metamorphics|69383|5|Briefly described|p73, 75, 76, 70, 81|||Arunta region. Sample AC07LCV160 comes from an area previously mapped as Mendip Metamorphics, but analyses indicate it to be much younger Irindina Province (955+/-10 Ma).|1770-1730 Ma max dep age.|Of Ledan Package.||Correlative of Ledan Schist.||
11649|Mendip Metamorphics|69427|5|Briefly described|p12:28, 33-34, 44|Statherian|Statherian|Crops out S of the Delny Shear Zone, Aileron Province. Upper greenschist to lower amphibolite facies metamorphism. SHRIMP U-Pb maximum depositional age; metamorphic zircon overgrowths aged 1723 +/- 9 Ma, and late-stage high-U overgrowths at 1572 +/- 16 Ma (Chewings Orogeny). Cut by a pegmatite dyke aged 1730 +/- 4 Ma.|<1770 Ma (Maidment et al., 2005).|||Unconformably overlies Mount Bleechmore Granulite.|A succession of quartzite and quartz-biotite rock with minor granule conglomerate, amphibolite, calc-silicate rock and biotite-muscovite quartz schist; the quartzite is thickly-bedded and tightly folded with a steeply dipping schistosity.|12-JUL-16
11649|Mendip Metamorphics|69431|6|Mentioned|p16:1|||Arunta Region. Possible correlative of Hatches Creek Group and, by inference, Tomkinson Creek Group.||||||12-JUL-16
11649|Mendip Metamorphics|69747|6|Mentioned|p274|||Arunta Orogen. Metamorphosed to the amphibolite facies. Metamorphism was dated on zircon metamorphic overgrowths at 1723 +/- 9 Ma (Maidment et al., 2005).||||||
11649|Mendip Metamorphics|71348|5|Briefly described|p217|Paleoproterozoic|Paleoproterozoic|Geological province: Aileron Province, Arunta Region. Maximum depositional age c. 1770-1750 Ma (Maidment et al., 2005; Cross and Crispe, 2007; Hollis et al., 2013; Kositcin et al., 2015).|<1770-1750 Ma|||||
11649|Mendip Metamorphics|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen. Both ages are of metamorphism: U-Pb zircon SHRIMP.|1723+/-9 Ma and 1572+/-17 Ma.||||Quartzite.|
11649|Mendip Metamorphics|72516|6|Mentioned|p9|Statherian|Statherian|Aileron Province.|ca. 1790 Ma|||||
11667|Mereenie Sandstone|9199|5|Briefly described|Map legend|Devonian|Silurian|White cross-bedded sandstone.  Geological Province: Amadeus Basin.||||||
11667|Mereenie Sandstone|9814|5|Briefly described|Map Legend|Devonian|Devonian|White cross-bedded sandstone.||||||
11667|Mereenie Sandstone|12891|5|Briefly described|p733 Fig. 2|Early Devonian|Late Silurian|Geological province: Amadeus Basin.||||||07-FEB-11
11667|Mereenie Sandstone|22560|5|Briefly described|p3|||Age "mostly" Silurian,  Max and Min limits not specified||||||01-SEP-09
11667|Mereenie Sandstone|22561|4|Described|p22|Devonian|Early Cambrian|||||||
11667|Mereenie Sandstone|22564|4|Described|p60|||Age Siluro-Devonian.  Overlying unit - Pertnjara Group||||||
11667|Mereenie Sandstone|22565|5|Briefly described|p70 & Table 1||Silurian|Thickness at Areyonga Creek measured from surface expression - 700m thick.  Approx. thickness measured from seismic data 710m.||||||
11667|Mereenie Sandstone|22566|4|Described|p84|Early Devonian|Silurian|Of the Larapinta Group.||||||06-NOV-06
11667|Mereenie Sandstone|22646|5|Briefly described|p 107|Devonian|Silurian|Underlain by Harajica and Ooraminna Sandstones in different sections - p107.||||||06-NOV-06
11667|Mereenie Sandstone|22650|4|Described|p 163|Early Devonian||Age of base of Mereenie Sandstone is not known but may be as old as latest Ordovician.||||||
11667|Mereenie Sandstone|22651|6|Mentioned|Fig 10 btw p182-183|||Age Siluro-Devonian.||||||
11667|Mereenie Sandstone|22656|5|Briefly described|p 279|Devonian|Silurian|||||||
11667|Mereenie Sandstone|22760|4|Described|p337|Devonian||Origin - Aeolian Deposition.  Age - Siluro-Devonian.||||||
11667|Mereenie Sandstone|22761|4|Described|p349-350|Early Devonian|Late Ordovician|Age - Mostly Silurian.||||||06-NOV-06
11667|Mereenie Sandstone|22762|5|Briefly described|p369|Devonian|Silurian|||||||
11667|Mereenie Sandstone|22763|5|Briefly described|p394|Early Devonian|Silurian|||||||
11667|Mereenie Sandstone|22804|4|Described|p442|||Poorly constrained age but is generally assumed to be Silurian to Early Devonian.||||||06-NOV-06
11667|Mereenie Sandstone|22805|5|Briefly described|p465||Early Devonian|||||||
11667|Mereenie Sandstone|22806|6|Mentioned|Fig 6 on p481|||Age - Ordovician(?)-Devonian(?)||||||
11667|Mereenie Sandstone|22807|6|Mentioned|Fig 3 on p495|Devonian|Silurian|||||||
11667|Mereenie Sandstone|22824|5|Briefly described|p526|||||||||
11667|Mereenie Sandstone|22826|4|Described|p575|Early Devonian|Late Ordovician|||||||
11667|Mereenie Sandstone|23282|6|Mentioned|p83|||May correlate with Mimili Formation. In the Amadeus Basin.||||||06-NOV-06
11667|Mereenie Sandstone|23361|5|Briefly described|16 Fig.4|Early Devonian|Caradoc|Age: 450-400Ma.||||||06-NOV-06
11667|Mereenie Sandstone|23858|5|Briefly described|p914|Late Ordovician|Late Ordovician|Overlain by Pertnjara Group; underlain by Carmichael Sandstone. Geological Province: Amadeus Basin. Max. thickness: 1500 m.||||||06-NOV-06
11667|Mereenie Sandstone|24063|5|Briefly described|p220|Devonian|Silurian|Geological Province: Amadeus Basin. Maximum thicknes: >900m.||||||
11667|Mereenie Sandstone|24064|5|Briefly described|p229 Fig.7|Devonian|Silurian|Geological Province: Amadeus Basin.||||||
11667|Mereenie Sandstone|24111|5|Briefly described|p214 Fig. 9|Devonian|Devonian|Geological Province: Amadeus Basin.  See also p215 Fig. 11.||||||30-MAR-05
11667|Mereenie Sandstone|24301|5|Briefly described|p21|||Unconformably overlies Carmichael Sandstone.  Geological Province: Amadeus Basin||||||06-NOV-06
11667|Mereenie Sandstone|24334|4|Described|p43, p48 Tb.1|Early Devonian|Caradoc|Age: 391 - 458 Ma (?evidence for this precision?).  Overlies the Carmichael Sandstone.  Overlain by the Parke Siltstone.||||||01-SEP-09
11667|Mereenie Sandstone|29474|6|Mentioned|p10|||||||||
11667|Mereenie Sandstone|29591|5|Briefly described|Table 23|||||||||
11667|Mereenie Sandstone|29972|6|Mentioned|p5|||Silurian-Devonian||||||
11667|Mereenie Sandstone|30045|6|Mentioned|p343|||||||||
11667|Mereenie Sandstone|30075|6|Mentioned|p12|||||||||
11667|Mereenie Sandstone|30238|4|Described|p64|||Devonian age.||||||06-NOV-06
11667|Mereenie Sandstone|30544|5|Briefly described|p50|||See also p51.||||||06-NOV-06
11667|Mereenie Sandstone|30615|6|Mentioned|p177|||Stratigraphic table - Palm Valley -2||||||
11667|Mereenie Sandstone|30659|6|Mentioned|p89|||Devonian. Palaeomagnetism.||||||
11667|Mereenie Sandstone|30661|6|Mentioned|Table 1|||||||||
11667|Mereenie Sandstone|30662|6|Mentioned|p188|||Palaeomagnetic dates||||||
11667|Mereenie Sandstone|31566|5|Briefly described|p229|||? Silurian - Devonian. See also p230, 231, 233, 239 etc.||||||06-NOV-06
11667|Mereenie Sandstone|31707|6|Mentioned|Table 1|||See also Fig. 2||||||
11667|Mereenie Sandstone|31914|6|Mentioned|p97|||Equivalent? Lennis Sst. & of Wanna Beds.||||||
11667|Mereenie Sandstone|32208|6|Mentioned|Map legend|Devonian|Silurian|Silurian? and Devonian?||||||
11667|Mereenie Sandstone|32619|6|Mentioned|p465|||||||||
11667|Mereenie Sandstone|32648|6|Mentioned|p32|||Sil. - Dev.||||||
11667|Mereenie Sandstone|32865|6|Mentioned|p482|||Partly Dev.||||||
11667|Mereenie Sandstone|33307|6|Mentioned|Fig.6|||||||||
11667|Mereenie Sandstone|33326|6|Mentioned|p449|||||||||
11667|Mereenie Sandstone|33625|6|Mentioned|p185|||Table 2||||||
11667|Mereenie Sandstone|33761|6|Mentioned|p146|||Sil? - Dev.||||||
11667|Mereenie Sandstone|33832|6|Mentioned|p8|||Stratigraphy||||||
11667|Mereenie Sandstone|33844|6|Mentioned|Table 1|||||||||
11667|Mereenie Sandstone|33871|6|Mentioned|Fig.4|||||||||
11667|Mereenie Sandstone|33971|6|Mentioned|p34|||Lithology sim. to Crown Pt. Fm.||||||
11667|Mereenie Sandstone|34111|5|Briefly described|p12|||Silurian? - Devonian. See also pp14,16,18.||||||06-NOV-06
11667|Mereenie Sandstone|34433|6|Mentioned|p41|||||||||
11667|Mereenie Sandstone|34442|5|Briefly described|Table 1|||Silurian? - Devonian.||||||06-NOV-06
11667|Mereenie Sandstone|34579|4|Described|Table 2|||Silurian - Devonian. See also pp10,16,17.||||||06-NOV-06
11667|Mereenie Sandstone|35088|6|Mentioned|p98|||||||||
11667|Mereenie Sandstone|35102|6|Mentioned|Fig.2|||||||||
11667|Mereenie Sandstone|35223|6|Mentioned|p11|||||||||
11667|Mereenie Sandstone|35997|6|Mentioned|p577|||||||||
11667|Mereenie Sandstone|36473|6|Mentioned|Map legend|Carboniferous|Devonian|Between Carboniferous and Devonian||||||
11667|Mereenie Sandstone|36751|6|Mentioned|p489|||||||||
11667|Mereenie Sandstone|36821|6|Mentioned|p397|||||||||
11667|Mereenie Sandstone|36890|4|Described|p400|||Formerly Mareena Bluff Formation.||||||06-NOV-06
11667|Mereenie Sandstone|37727|4|Described|p72|||See also p14.||||||06-NOV-06
11667|Mereenie Sandstone|37818|6|Mentioned|p81|||||||||
11667|Mereenie Sandstone|38606|6|Mentioned|Map legend|Devonian|Devonian|||||||
11667|Mereenie Sandstone|38885|6|Mentioned|Map legend|Devonian|Devonian|||||||
11667|Mereenie Sandstone|39213|6|Mentioned|Fig.6|||Amadeus Basin Succession||||||
11667|Mereenie Sandstone|39565|6|Mentioned|Fig.14|||||||||
11667|Mereenie Sandstone|39583|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
11667|Mereenie Sandstone|40136|6|Mentioned|p36|||||||||
11667|Mereenie Sandstone|40201|5|Briefly described|Table 1|||||||||
11667|Mereenie Sandstone|40387|6|Mentioned|p146|||||||||
11667|Mereenie Sandstone|40642|6|Mentioned|p172|||||||||
11667|Mereenie Sandstone|40740|3|Fully described|p58|||Mention p6.||||||06-NOV-06
11667|Mereenie Sandstone|40810|5|Briefly described|p11|||||||||
11667|Mereenie Sandstone|40834|5|Briefly described|p138|||||||||
11667|Mereenie Sandstone|40906|6|Mentioned|p30|||Mention Fig.11||||||
11667|Mereenie Sandstone|40911|6|Mentioned|Map legend|Devonian|Devonian|Prob. Devonian||||||
11667|Mereenie Sandstone|40926|6|Mentioned|p12|||||||||
11667|Mereenie Sandstone|41018|6|Mentioned|p233|||||||||
11667|Mereenie Sandstone|41039|4|Described|p6|||||||||
11667|Mereenie Sandstone|41190|6|Mentioned|Fig.4|||||||||
11667|Mereenie Sandstone|41224|6|Mentioned|Fig.2|||||||||
11667|Mereenie Sandstone|41270|6|Mentioned|p270|||||||||
11667|Mereenie Sandstone|41276|6|Mentioned|p61|||||||||
11667|Mereenie Sandstone|41385|6|Mentioned|p363|||||||||
11667|Mereenie Sandstone|41409|6|Mentioned|p290|||||||||
11667|Mereenie Sandstone|41560|6|Mentioned|p551|||||||||
11667|Mereenie Sandstone|41621|5|Briefly described|Map legend|Middle Devonian|Late Ordovician|||||||
11667|Mereenie Sandstone|41717|6|Mentioned|Fig.2|||||||||
11667|Mereenie Sandstone|41723|6|Mentioned|Map legend|Late Ordovician|Early Devonian|||||||
11667|Mereenie Sandstone|41819|6|Mentioned|Map legend|Middle Devonian|Late Ordovician|||||||
11667|Mereenie Sandstone|41820|3|Fully described|p13|||||||||
11667|Mereenie Sandstone|42049|5|Briefly described|p217|||||||||
11667|Mereenie Sandstone|42058|6|Mentioned|p116|||||||||
11667|Mereenie Sandstone|42059|6|Mentioned|Fig.2 P131|||||||||
11667|Mereenie Sandstone|42060|6|Mentioned|Fig.5 P140|||||||||
11667|Mereenie Sandstone|42082|6|Mentioned|Fig.3 P323|||||||||
11667|Mereenie Sandstone|42140|6|Mentioned|p558|||||||||
11667|Mereenie Sandstone|42141|6|Mentioned|p568|||||||||
11667|Mereenie Sandstone|42504|5|Briefly described|p77|||||||||
11667|Mereenie Sandstone|42643|6|Mentioned|p32|||||||||
11667|Mereenie Sandstone|42699|5|Briefly described|map legend|Devonian|Silurian|||||||
11667|Mereenie Sandstone|42776|6|Mentioned|p305|||||||||
11667|Mereenie Sandstone|42940|5|Briefly described|Plate 2|Silurian|Silurian|Sandstone, minor conglomerate.  Age: 440-410Ma.  Geological province: Amadeus Basin.||||||23-JAN-08
11667|Mereenie Sandstone|43035|5|Briefly described|p23|||||||||
11667|Mereenie Sandstone|43105|5|Briefly described|Fig.3,p8.|||||||||
11667|Mereenie Sandstone|43225|5|Briefly described|Map Legend|Devonian|Ordovician|||||||
11667|Mereenie Sandstone|43503|6|Mentioned|11-39|Early Devonian|Silurian|||||||
11667|Mereenie Sandstone|43646|6|Mentioned|Fig.3,p554|Devonian|Silurian|||||||
11667|Mereenie Sandstone|43647|6|Mentioned|p530|||||||||
11667|Mereenie Sandstone|43648|5|Briefly described|Fig.1,p488|||||||||
11667|Mereenie Sandstone|43649|5|Briefly described|fig.1,p454-455,459|||||||||
11667|Mereenie Sandstone|43666|6|Mentioned|p20|||||||||
11667|Mereenie Sandstone|43749|6|Mentioned|p37|||||||||
11667|Mereenie Sandstone|43817|5|Briefly described|p61-63|||||||||
11667|Mereenie Sandstone|43869|5|Briefly described|p10|Silurian|Silurian|Wind-blown sand, very porous and stores large quatities of water; main source of groundwater for Alice Springs.  Deposited about 430my ago.||||||06-NOV-06
11667|Mereenie Sandstone|44133|4|Described|p42 Fig. 7.16, 44|Middle Paleozoic|Early Paleozoic|Geological Province: Amadeus Basin. Conformably underlies: Finke Group. May exceed 600m in Thickness in depressions. Conformably overlain by Polly Conglomerate, Langra Formation, Horseshoe Bend Shale.||||||07-NOV-08
11667|Mereenie Sandstone|44158|6|Mentioned|p33|||of Amadeus Basin.||||||
11667|Mereenie Sandstone|44220|14|Not recorded|p.67|||||||||
11667|Mereenie Sandstone|44335|4|Described|p.11|Devonian|Silurian|Table 2. p.10, Sil-Dev.||||||
11667|Mereenie Sandstone|44336|14|Not recorded|map legend|Devonian|Silurian|SG/53-3.  Silurian-Devonian.||||||
11667|Mereenie Sandstone|44342|6|Mentioned|p.5, Table 2|||SG/53-5. ?Silurian-Devonian.||||||
11667|Mereenie Sandstone|44343|14|Not recorded|map legend|Devonian|Silurian|Silurian-Devonian.||||||
11667|Mereenie Sandstone|44393|4|Described|p.3, Tb.1|||||||||
11667|Mereenie Sandstone|44394|14|Not recorded|map legend|||Silurian (?) to Devonian.||||||
11667|Mereenie Sandstone|44395|14|Not recorded|p.9,10,12, Tb.2||Late Ordovician|Upper Ordovician.||||||
11667|Mereenie Sandstone|44396|5|Briefly described|map legend|||(Sil?-Dev). SF/52-15.||||||
11667|Mereenie Sandstone|44402|5|Briefly described|map legend|||Silurian? - Dev.||||||02-DEC-04
11667|Mereenie Sandstone|44433|14|Not recorded|map legend|||Silurian? to Devonian.||||||
11667|Mereenie Sandstone|44439|2|Defined|p.7,8, Tb.1, map|Devonian|Ordovician|Ordovician-Devonian.||||||
11667|Mereenie Sandstone|44440|14|Not recorded|map legend|Devonian|Ordovician|Ordovician-Devonian.||||||
11667|Mereenie Sandstone|44484|14|Not recorded|p.5,8,9,11,Fig.4,Tb1|||(?Sil-Dev). See also p.11,12,14, for more details.||||||
11667|Mereenie Sandstone|44485|14|Not recorded|map legend|||Sil? - Dev.||||||
11667|Mereenie Sandstone|44493|4|Described|p.11, map|Devonian|Ordovician|Bloods Range sheet. (G53-3). Ord-Dev. See p.8,13, for details.||||||
11667|Mereenie Sandstone|44494|14|Not recorded|map legend|Devonian|Ordovician|Ordovician - Devonian.||||||
11667|Mereenie Sandstone|44495|4|Described|p.6, map|Devonian|Ordovician|See p.8-10, Tb.1, for details. (G52-8). Ord-Dev.||||||
11667|Mereenie Sandstone|44497|4|Described|p.11,12, Table 2|Devonian|Ordovician|SF/53-13. Ord-Dev.||||||
11667|Mereenie Sandstone|44498|14|Not recorded|map legend|Devonian|Ordovician|Ordovician-Devonian.||||||
11667|Mereenie Sandstone|44505|14|Not recorded|p.2,4,8,9,Fig 1,Tb.1|Devonian|Silurian|Sil-Dev. See also p.9,12, for more details.||||||
11667|Mereenie Sandstone|44506|14|Not recorded|map legend|||Silurian? to Devion.||||||
11667|Mereenie Sandstone|45036|6|Mentioned|p3|||||||||
11667|Mereenie Sandstone|45041|4|Described|p86|||See also pp87-89. U.Sil.- M.Dev.||||||06-NOV-06
11667|Mereenie Sandstone|45148|6|Mentioned|p20|||||||||
11667|Mereenie Sandstone|45155|6|Mentioned|Fig.8|||||||||
11667|Mereenie Sandstone|45168|6|Mentioned|p6|||||||||
11667|Mereenie Sandstone|45170|6|Mentioned|p8|||||||||
11667|Mereenie Sandstone|46829|6|Mentioned|Fig.2|||||||||
11667|Mereenie Sandstone|46928|6|Mentioned|Table 1|||||||||
11667|Mereenie Sandstone|47050|5|Briefly described|p240|||||||||
11667|Mereenie Sandstone|48639|4|Described|p.4|||See also p.1,5-7,16,Pl.1,Sh.1. ?Ord (Siln-Devn according to B.M.R.) F53-14,G55-2).||||||
11667|Mereenie Sandstone|48838|2|Defined|p.19,22-23, Tb.1|||||||||
11667|Mereenie Sandstone|48842|4|Described|p.20||Paleozoic|p.1,20,27,32,Pl.7. Tb.I.||||||07-NOV-08
11667|Mereenie Sandstone|48862|14|Not recorded|p.1,15,18,25,27-42|||(F52-15). Age uncertain, base at least is Ord. opp.8,9; Pl.4,5,9-11.||||||
11667|Mereenie Sandstone|48863|2|Defined|p.29|||Tb.1. opp.p.7,9,20,28,31,36,37-40,42,Pl.4,9,11,13-14,16. Ordovician-Devonian. (G52-4,G53-1).||||||
11667|Mereenie Sandstone|48864|2|Defined|p.34|Middle Devonian|Early Ordovician|Tb.1. On many pages. p.2,9,10,21,32,35,37,48,50,Pl.10,11,13. L.Ord-Lower or Middle Devonian. (G52-2,3,8).||||||
11667|Mereenie Sandstone|48865|2|Defined|p.4,Fig.26-27|||Many figures. Fig.4,21,25,42,47,51,Fig.14, Pl.8-10. = 'Marena red sandstone'. Upper Ordovician? (G52-8,G53-5).||||||06-NOV-06
11667|Mereenie Sandstone|48880|14|Not recorded|p.20,33,Pl.10,11,13|Devonian|Ordovician|(F53-13,14,G53-3).Ord-Devn.||||||
11667|Mereenie Sandstone|48890|4|Described|p.48, pl.12|Devonian|Silurian|See also Tables, Figs & Plates. Sil-Dev.||||||
11667|Mereenie Sandstone|48963|6|Mentioned|Fig.3|||||||||
11667|Mereenie Sandstone|50098|5|Briefly described|p1||Late Ordovician|Geological Province: Amadeus Basin.||||||
11667|Mereenie Sandstone|50244|6|Mentioned|p100|||||||||
11667|Mereenie Sandstone|60547|5|Briefly described|Map Legend|Devonian|Silurian|White cross-bedded sandstone. Geological Province: Amadeus Basin.||||||
11667|Mereenie Sandstone|60674|5|Briefly described|Map legend|Devonian|Silurian|Of the Pertnjara Group.  White to pale brown, fine, well-sorted quartz sandstone.  Geological Province: Amadeus Basin.||||||03-DEC-15
11667|Mereenie Sandstone|61306|5|Briefly described|p14, p40|||High-yielding aquifer rocks. Geological Province: northern Amadeus Basin||||||
11667|Mereenie Sandstone|61309|5|Briefly described|p16 Fig. 4, p25 Fig. 11|||Geological Province: Amadeus Basin.||||||06-FEB-08
11667|Mereenie Sandstone|61385|5|Briefly described|Map legend|Devonian|Silurian|White, crossbedded sandstone.  Geological Province: Amadeus Basin.||||||20-OCT-05
11667|Mereenie Sandstone|61387|5|Briefly described|Map legend|Devonian|Silurian|Of the Pertnjara Group. White sandstone, large-scale cross-bedding.  Geological Province: Amadeus Basin.||||||06-NOV-06
11667|Mereenie Sandstone|61518|5|Briefly described|Map Legend|Devonian|Silurian|White to pale brown fine grained, well sorted quartz sandstone. Geological Province: Amadeus Basin.||||||
11667|Mereenie Sandstone|61519|5|Briefly described|Map Legend|Silurian|Silurian|Of the Pertnjara Group. White sandstone, large scale cross bedding. Geological Province: Amadeus Basin.||||||
11667|Mereenie Sandstone|62359|6|Mentioned|p547 Fig. 7|||Geological Province: Amadeus Basin.||||||
11667|Mereenie Sandstone|62376|5|Briefly described|p18|Early Devonian|Silurian|Of the Larapinta Group. Geological Province: Amadeus Basin.||||||09-FEB-10
11667|Mereenie Sandstone|62379|5|Briefly described|p7 Fig. 2|Devonian|Silurian|Of the Larapinta Group. Geological Province: Amadeus Basin.||||||
11667|Mereenie Sandstone|62609|5|Briefly described|Map Legend|Devonian|Silurian|Sandstone, minor conglomerate. Underlies: Pertnjara Group. Overlies: Larapinta Group.||||||14-AUG-06
11667|Mereenie Sandstone|62620|5|Briefly described|Map Legend|Devonian|Silurian|Sandstone, minor  conglomerate.||||||
11667|Mereenie Sandstone|63562|5|Briefly described|p338 fig 3, p352 fig 10, p355|Devonian|Silurian|See also p347 fig 9, p350. Of Amadeus Basin. Up to 1.5 km thick package. Zircons similar to underlying sediments (mostly 0.63-0.49 Ga) thus presumed to be derived from them. Similar age spectrum as Stairway Sandstone.|c.435-405 Ma.|||Overlies Carmichael Sandstone conformably. Overlain by Pertnjara Group unconformably.|Aeolian, lesser fluvial, quartz arenites.|
11667|Mereenie Sandstone|64068|6|Mentioned|p78, 79, p7|Silurian|Silurian|Amadeus Basin. Correlated with Devonian Dulcie Sandstone, Cravens Peak beds, Georgina Basin.||||||
11667|Mereenie Sandstone|64334|5|Briefly described|p39, 42|Silurian|Silurian|Amadeus Basin. Deposition was probably in a foreland basin with highlands to the N.||||Unconformably overlies Carmichael Sandstone (Larapinta Group).|Aeolian, fluvial and locally marginal-marine deposits.|
11667|Mereenie Sandstone|64580|4|Described|map legend|Silurian|Ordovician|Quartz sandstone; minor siltstone; eolian.||||||09-DEC-08
11667|Mereenie Sandstone|64769|6|Mentioned|p29|||Dimension stone from this unit is called Ooraminna Sandstone.||||||06-MAY-09
11667|Mereenie Sandstone|64778|6|Mentioned|p13, 16-17, 20|Silurian|Silurian|Amadeus and Pedirka Basins. Max. palaeotemperature analysis summary.||||||
11667|Mereenie Sandstone|64809|5|Briefly described|p2, p3 Fig.2, p6 Fig.4, p11 Fig.10 |Early Devonian|Silurian|Aeolian and fluvial deposition.||||||
11667|Mereenie Sandstone|64970|6|Mentioned|p719 Fig. 2|Devonian|Silurian|Geological Province: Amadeus Basin.||||||27-MAY-09
11667|Mereenie Sandstone|65194|6|Mentioned|p30, p57, p59, p67|Paleozoic||Amadeus Basin. Misspelt as Meerenie on p67. Aquifer supplying Alice Springs.||||||
11667|Mereenie Sandstone|65233|4|Described|p3 Fig. 2, p10, p12-13|Early Devonian|Silurian|Of upper Larapinta Group. Gradational with Carmichael Sandstone below. Max.thickness:900m. Geol.prov: Amadeus Basin. Comprises 3 unnamed units - lower aeolian succession overlain by locally developed fluvial deposits, capped by an upper aeolian sandstone.||||||07-FEB-11
11667|Mereenie Sandstone|65272|6|Mentioned|p319, p320 Fig.3|Devonian|Silurian|||||||
11667|Mereenie Sandstone|65342|6|Mentioned|p3, p10.|||Amadeus and Eromanga Basins. Max. thickness at least 338 m.||||Overlies Stairway Sandstone. Is overlain by Pertnjara Group.||
11667|Mereenie Sandstone|65449|5|Briefly described|p34-35|Early Devonian|Late Ordovician|Amadeus Basin. Marginal marine to eolian deposits. Closely resembles Tandalgoo Formation lithologically.||||Time-correlative with Carribuddy Group and Worral Formation.||
11667|Mereenie Sandstone|65489|5|Briefly described|p56, p63-64, p125|Devonian|Devonian|Amadeus Basin. Exhibits particularly good reservoir properties at McDills 1.||||||
11667|Mereenie Sandstone|66767|5|Briefly described|p60|Devonian|Late Ordovician|Amadeus Basin. Up to 1000m thick.||||Overlies Larapinta Group. Is overlain unconformably by Pertnjara Group.|Shallow-marine to fluvial quartz sandstone.|
11667|Mereenie Sandstone|67028|6|Mentioned|p372 Tb. 5|Devonian|Ordovician|Magnetic information for unit concerning Mid-Paleozoic to Early Mesozoic pole positions for Australia is presented, sourced from the Global Palaeomagnetic Database (GPMDB; McElhinny & Lock 1993, 1996).|398-461 Ma magnetic age range|||||24-APR-12
11667|Mereenie Sandstone|67326|5|Briefly described|p2-3|Early Devonian|Silurian|Amadeus Basin.||Larapinta Group.||Overlies Carmichael Sandstone. Is overlain by Parke Siltstone.||
11667|Mereenie Sandstone|67565|5|Briefly described|p5 Fig.3, p42, p47, p52.|||Amadeus Basin. Widespread; occurs as prominent ridges. Shallow marine sands overlain  by aeolian dunes. Thickness from 220-1000 m. Devonian fish remains were recorded from its upper beds. An important aquifer.||||Overlies Carmichael Sandstone. Is overlain by Pertnjara Group.|White to pale brown, fine-grained, well-sorted quartz sandstone.|
11667|Mereenie Sandstone|67856|4|Described|p338 fig 4-30, p347 , 337, 346, 348|Early Devonian|Late Ordovician|Of Wells et al., 1964, 1970 etc. [Database says it is part of Pertnjara Group. This reference says there is unconformity between them] Type section West of Ellery Creek (NT). Shallow marine, eolian, fluviatile. Up to 100 m thick [p346, or 1000m p347]. 9 m exposed in WA.||||Overlies Carmichael Sandstone (unconformably).  Overlain gradationally in some parts and unconformably in others by Pertnjara Group (NT).|White to pale brown, cross-bedded pure quartz sandstone.|
11667|Mereenie Sandstone|68323|6|Mentioned|p4 Fig.2|Early Devonian|Early Devonian|Amadeus Basin.||Larapinta Group.||||
11667|Mereenie Sandstone|69438|3|Fully described|p23:2-5,7,21,32, 36-39, 46-48, 50, 55-57|Late Devonian|Silurian|Pritchard and Quinlan (1962); previously spelled as Mareenie Sandstone (Madigan, 1932). Originally Mereenie Bluff Formation of Chewings (1894) for sandstone at the George Gill Range, Amadeus Basin. Was formerly mapped (Ranford et al., 1965) as including rocks which were subsequently (Wells et al., 1970) assigned as a separate Formation (the Carmichael Sandstone). The type section is in the west MacDonnell Ranges, W of Ellery Creek; reference sections at Stokes Pass and Areyonga Creek further to the W. Up to c.1000m thick. Widespread unit: extends c.800km E-W and c.200km N-S. Is faulted against Carnegie Formation. Is overlain by Brewer Conglomerate unconformably. Age range of Late Ordovician?-Early Devonian? is due to absence of useful fossils. Has been quarried for dimension stone in the Ooraminna area.||Ungrouped.||Overlies Carmichael Sandstone conformably (unconformably in the E), and Pertaoorrta Group unconformably. Is overlain by Parke Siltstone or Hermannsburg Sandstone conformably.|Variably thinly to thickly bedded, white to pale brown very pure quartz sandstone; generally fine-grained, but is occasionally medium-grained, with grains well-rounded and well-sorted. Burrows and arthropod tracks occur.|27-APR-17
11667|Mereenie Sandstone|69439|5|Briefly described|p24:11|Silurian|Ordovician|Amadeus Basin. Possible correlative of Kerridy Sandstone (Ngalia Basin).||||||12-JUL-16
11667|Mereenie Sandstone|69449|5|Briefly described|p34:2 Fig.34.2; 34:5, 7|Devonian|Silurian|Eastern Amadeus Basin, with equivalents in the western Warburton Basin. Potential petroleum reservoir rocks.||||Is overlain by Polly Conglomerate (Finke Group).|Red-brown to orange, fine- to coarse-grained, friable sandstone, cross-bedded and locally calcareous.|12-JUL-16
11667|Mereenie Sandstone|69458|6|Mentioned|p42:8|Early Devonian|Late Ordovician|Amadeus Basin.||||||12-JUL-16
11667|Mereenie Sandstone|69606|5|Briefly described|p3, p4 fig 2|Devonian|Silurian|One outcrop found in WA. Deposited during the Alice Springs Orogeny. Amadeus Basin. Potential reservoir rock.||||Unconformably overlies the Carmichael Sandstone. Unconformably overlain by the Pertnjara Group.|Sandstone.|
11667|Mereenie Sandstone|69673|5|Briefly described|p64 fig 53, p67, p149, p149 fig 120|||1km thick.||||Overlies Carmichael Sandstone, overlain by Parke Siltstone|Fine grained, occasionally medium grained, very pure quartz sandstone.|
11667|Mereenie Sandstone|69982|6|Mentioned|p42|Devonian|Late Ordovician|Amadeus Basin.||||||
11667|Mereenie Sandstone|70793|4|Described|500k_interpgeop14_lut.csv|Early Devonian|Silurian|Of Amadeus Basin (Phase 2). Events: Alice Springs Orogeny (450-295 Ma); Rodingan Movement (Alice Springs Orogeny phase 1) (450-420 Ma). See 500k_interpgeop14_lut.csv, 2_5m_interpgeop15_lut.csv.|443.4-393.3 Ma (inferred)||||Quartz sandstone; minor siltstone; largely eolian|
11667|Mereenie Sandstone|70826|6|Mentioned|p7 tbl 3|Devonian|Silurian|Amadeus Basin.||||||24-APR-20
11667|Mereenie Sandstone|71080|6|Mentioned|p30 fig 21|Devonian|Silurian|Amadeus Basin.|||||Dominantly sandstone.|
11667|Mereenie Sandstone|71146|5|Briefly described|p6, p28|Pragian|Ludlow|Amadeus Basin. Hosts trace fossils including burrows, trails, scratch marks and tunnels similar to those found in the Tumblagooda Sandstone.||||Overlies the Carmichael Sandstone (Larapinta Group).|Sandstone.|
11667|Mereenie Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, sandstone|
11667|Mereenie Sandstone|71268|4|Described|GEOL_LUT_CSV files|Early Devonian|Silurian|Geological province: Paterson Orogen. Of Bentley Basin. Events: Rodingan Movement (Alice Springs Orogeny phase 1) (450-420 Ma). See 1m_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|443.4-393.3 Ma (inferred)|Unit of Pertnjara Group.|||Porous, white to pale-brown, fine grained, well sorted quartz sandstone, minor conglomerate|
11667|Mereenie Sandstone|71279|5|Briefly described|p355 Fig.2,p360,p363-365,p374,p382 Tb.1|Early Devonian|Silurian|Amadeus Basin. Crops out in the Waterhouse Range. Magnetisation described. Modelled magnetic properties.||Larapinta Group.||||
11667|Mereenie Sandstone|71342|6|Mentioned|Ch9 p16, Ch9 p20|||||||Unconformably overlies the Stairway Sandstone. Unconformably overlain by the Finke Group.||
11667|Mereenie Sandstone|71618|6|Mentioned|p130|Devonian|Silurian|Of Amadeus Basin.||||||
11667|Mereenie Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Early Devonian|Silurian|Amadeus Basin (Phase 2).|||||Quartz sandstone; minor siltstone; largely eolian.|
11667|Mereenie Sandstone|72360|5|Briefly described|Map legend|Silurian|Silurian|Of Amadeus Basin.|||||White sandstone, large scale cross bedding.|09-SEP-19
11667|Mereenie Sandstone|72369|4|Described|iii,p3-4-4,34-35,37-40|||Of Amadeus Basin. Widespread in the Amadeus Basin, covering ~800 km east-west and 200 km north-south (Owen in Kennard et al 1986). No previous geochronological analysis, but inferred age constraints provided by c. 480 MA MDA of underlying mereenie Sandstone (Maidment 2005), and paleomagnetic investigation by Li et al. (1991), providing possible Silurian age. LA-ICP-MS U-Pb detrital zircon dating of sample HB15VJN091 (medium-grained quartz arenite) yielded an interpreted maximum depositional age of 486+\-5 Ma (youngest concordant zircon). This age is within certainty of that provided by Maidment 2005, but inconsistent with paleomagnetic age of Li et al. (1991). Contains Meso- to Neoproterozoic detrital zircon age populations (c. 1235-915 Ma) likely sourced from Musgrave Province. Late Neoproterozoic to Cambrian (c. 750-485 Ma) zircons may have been derived from distal greater Gondwanan input, as there are no known Cambrian sources proximal to Amadeus Basin. Archean-Paleoproterozoic grains (c. 3125-1840 Ma) may have been recycled from North Australian Craton. Sample locality, zircon description, SHRIMP results and analyses are discussed.||Unit of Larapinta Group.||Overlain by parke Siltstone, or disconformably by Hermannsburg Sandstone. Underlain by Carmichael Sandstone.|Variably thinly- to thickly bedded, white to pale brown, quartz sandstone.|18-DEC-19
11667|Mereenie Sandstone|72374|4|Described|iii,p3-4,20-24,26|||Of Amadeus Basin. Depositional environment: shallow marine in the lower part, becoming aeolian in upper. Paleomagnetic investigation by Li et al 1991 suggested a Silurian (444-419 Ma) age. Provenance studies by Normington et al 2018 indicate recycling of detritus from underlying Amadeus Basin succession, as well as primary sources including Musgrave Province. Sample HB16ND358 (sandstone) yielded an interpreted maximum depositional age of 505+\-5 Ma. Zircons of c. 1300-800 Ma (c. 1209, 1158, 1183 and 1127 Ma peaks) likely derived from Musgrave Province either directly, or recycled from underlying Amadeus Basin succession. Lesser groupings of c. 700-500 Ma and c. 2050-1450 Ma likely sourced directly from Aileron, Warumpi and Musgrave provinces, or recycled from underlying Amadeus Basin succession.||Publication layout suggests this is a unit of Larapinta Group.|||Variably thinly- to thickly bedded, white to pale brown sandstone; well-rounded and well-sorted, fine- to medium-grained quartz arenite.|11-OCT-19
11667|Mereenie Sandstone|72476|6|Mentioned|p36 Fig.9|||Amadeus Basin. Time-temperature thermal history diagram.||||||
11667|Mereenie Sandstone|73085|6|Mentioned|p1, p4|early Devonian|Silurian|||Larapinta Group||Underlain by Carmichael Sandstone. Overlain by Parke Siltstone (Pertnjara Group).||
11667|Mereenie Sandstone|73119|5|Briefly described|piii, p1, p21-23, Appendix|Silurian|Silurian[?]|Amadeus Basin, widespread. Depositional environment ranges from shallow marine to fluvial to aeolian. Geochron is new SHRIMP U-Pb detrital zircon maximum depositional age, which is younger than the previous youngest age of 486 +/- 5 Ma (Normington et al., 2018), although still older than the Silurian age proposed using palaeomagnetism (Li et al., 1991). Detrital zircon age components are dominated by Palaeozoic to Neoproterozoic and early Mesoproterozoic zircons with only a small number of older Proterozoic-Archean grains. Sourced dominantly from the Musgrave Province with contributions probably from reworked underlying strata originally sourced from the Aileron and Warumpi provinces. [See article for provenance discussion].|473 +/- 7 Ma SHRIMP U-Pb||||Includes poorly-sorted, medium-grained sandstone.|
11667|Mereenie Sandstone|73279|5|Briefly described|p3, p14|Devonian|Ordovician|Amadeus Basin. Detrital zircons analysed for Hf isotopic composition [see article].||||Underlain by Larapinta Group [Carmichael Sandstone]. Overlain by Pertnjara Group.|Includes sandstone.|
11667|Mereenie Sandstone|73281|6|Mentioned|Appendix (DIP)|||See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
11835|Milingimbi Formation|23373|4|Described|p318||Early Ordovician|Of Goulburn Group.  In the Arafura Basin.||||||06-NOV-06
11835|Milingimbi Formation|23374|5|Briefly described|p23|||Of Goulburn Group.  In the Arafura Basin.||||||06-NOV-06
11835|Milingimbi Formation|42058|4|Described|p115|||||||||
11835|Milingimbi Formation|44112|6|Mentioned|p78|||||||||
11835|Milingimbi Formation|62510|5|Briefly described|p3|Orodvician|Orodvician|||||||
11835|Milingimbi Formation|63062|5|Briefly described|p9 Fig. 9, p14|Early Ordovician|Early Ordovician|Of the Goulburn Group. Geological Province: Arafura and Money Shoal Basins. Mixed carbonate and clastic rocks.||||||07-FEB-11
11835|Milingimbi Formation|69297|5|Briefly described|p283, p285|Lower Ordovician|Lower Ordovician|Arafura Basin. Deposited in a shallow marine shelf environment.||Goulburn Group||Overlies the Naningbura Dolomite. Overlain by the Mooroongga Formation.|Carbonate and clastic rocks.|
11835|Milingimbi Formation|69437|5|Briefly described|p22:10|Early Ordovician|Early Ordovician|Arafura Basin.||||Overlies Naningbura Dolomite. Is overlain by Mooroongga Formation.||12-JUL-16
11835|Milingimbi Formation|69451|3|Fully described|p35:3-4, 6-8; 35:13 Fig.35.9|Ordovician|Ordovician|Bradshaw et al. (1990); Nicoll (2006). Arafura Basin (offshore). Shallow-marine deposits. 169m thick in the type section in Arafura-1. Contains Tremadocian conodont faunas.||Goulburn Group.||Conformably overlies Naningbura Dolomite. Is overlain by Mooroongga Formation probably conformably, or by presumed Arafura Group unconformably.|Dolostone, limestone, glauconitic sandstone, shale; becomes more siliciclastic up-section; conodont faunas.|12-JUL-16
11835|Milingimbi Formation|69673|6|Mentioned|p197|||||||||
11835|Milingimbi Formation|70098|4|Described|p5|Early Ordovician|Furongian|The Lower Ordovician marine shelf mixed carbonate and clastic rocks of the Milingimbi and Mooroongga formations form the uppermost units of the Goulburn Group. See also misspelt Millingimbi Formation on p19 Fig.5||Goulburn Group||Overlies Naningbura Dolomite.|Marine shelf mixed carbonate and clastic rocks.|
11862|Milligans Formation|5256|5|Briefly described|p143, p144, p148.|Visean|Tournaisian|Bonaparte Basin. Type section: Milligans 1 (44-155m). Rare conodonts indicate age ~ Tournaisian - Visean boundary, but elsewhere stated as latest Tournaisian - late Visean. Widespread clastic marine unit. Wave protected, calm, shallow water environment||||||
11862|Milligans Formation|7142|6|Mentioned|p350 Fig.4.|Early Carboniferous|Early Carboniferous|Browse Basin.||||Overlies Bonaparte Formation. Is overlain by Tanmurra Formation.||
11862|Milligans Formation|13194|6|Mentioned|p390 Tb. 4-16; p382, 402 figs 4-59,-66|Visean|Tournaisian|Type Section: Milligans 1 well (44-155m); Reference section: Bonaparte 1 well (497-2280m).  300 to 2142m thick offshore marine deposits.||Weaber Group||Unconformably overlies Bonaparte Formation; Cockatoo, Ningbing and Langfield Groups; overlies Bonaparte Formation (conformably). Conformably underlies Utting Calcarenite and Waggon Creek Formation.|Shale; minor siltstone and sandstone.|
11862|Milligans Formation|13234|5|Briefly described|p248, p250-256, p260,262 Tbs.1,2; p265.|Early Carboniferous|Early Carboniferous|Source rock for oil at Turtle and Barnett reservoirs. Deposited during rapid deepening. Proven regional top seal.|||||Marine anoxic shales.|
11862|Milligans Formation|13354|6|Mentioned|p375 Fig.6.|Early Carboniferous|Early Carboniferous|Overlies Bonaparte Formation and underlies Tanmurra Formation.||62||||28-OCT-14
11862|Milligans Formation|14228|5|Briefly described|p6 fig3|Carboniferous|Carboniferous|Southern Bonaparte Basin.||||Overlain by Tanmurra Formation.||05-OCT-16
11862|Milligans Formation|22663|5|Briefly described|W97 8 to 10 p2 Fig.3||Carboniferous|||||||01-MAR-10
11862|Milligans Formation|23356|5|Briefly described|26 Tab.2|Early Carboniferous|Early Carboniferous|||||||
11862|Milligans Formation|23377|6|Mentioned|p212 Fig.5||Mississippian|In the Vulcan Sub-basin.||||||06-NOV-06
11862|Milligans Formation|24246|5|Briefly described|p7|Early Carboniferous|Early Carboniferous|Geological Province: Bonaparte Basin.||||||
11862|Milligans Formation|24378|5|Briefly described|p14|||Geological Province: Bonaparte Basin.||||||
11862|Milligans Formation|24390|5|Briefly described|p2 Fig. 2, p3 Table 1|Early Carboniferous|Early Carboniferous|Geological Province: Bonaparte Basin.||||||
11862|Milligans Formation|24569|5|Briefly described|p248 Fig. 3|Visean|Visean|Of the Weaber Group.Geological Province: Petrel Sub-basin.||||||02-MAR-05
11862|Milligans Formation|40792|5|Briefly described|p175|||Mention Fig.3.||||||06-NOV-06
11862|Milligans Formation|40993|6|Mentioned|p9|||Mention Fig.1||||||
11862|Milligans Formation|41459|6|Mentioned|p278|||||||||
11862|Milligans Formation|41532|5|Briefly described|p292|||||||||
11862|Milligans Formation|41690|6|Mentioned|p57|||||||||
11862|Milligans Formation|41731|6|Mentioned|p574|||||||||
11862|Milligans Formation|41839|4|Described|p31|||Formerly "Milligans Beds"||||||
11862|Milligans Formation|41864|3|Fully described|p123|||||||||
11862|Milligans Formation|41865|5|Briefly described|Map legend|late Visean|late Tournaisian|||||||
11862|Milligans Formation|41867|5|Briefly described|Map legend|late Visean|late Tournaisian|||||||
11862|Milligans Formation|42030|5|Briefly described|p750|||||||||
11862|Milligans Formation|42055|4|Described|Fig.1 P52|||||||||
11862|Milligans Formation|42056|6|Mentioned|p96|||||||||
11862|Milligans Formation|42175|5|Briefly described|p197|||||||||
11862|Milligans Formation|42442|3|Fully described|p11|Visean|Tournaisian|NT. Age latest Tournaisian to late Visean.||||||
11862|Milligans Formation|42547|4|Described|p101|||||||||
11862|Milligans Formation|43482|6|Mentioned|23||Early Carboniferous|||||||
11862|Milligans Formation|44159|6|Mentioned|Table p.38||Early Carboniferous|||||||
11862|Milligans Formation|49637|5|Briefly described|Fig. 6|Early Carboniferous|Early Carboniferous|Age: ~350Ma. Geological Province: Bonaparte Basin.||||||07-FEB-11
11862|Milligans Formation|50085|5|Briefly described|p2 Fig. 2, p3 Tb.1|Carboniferous||Shaly unit.  Geological Province: Bonaparte Basin.||||||11-MAY-04
11862|Milligans Formation|60006|5|Briefly described|Map Legend|Visean|Visean|Geological Province: Bonaparte Basin. Of the Weaber Group. Shale, siltstone, minor sandstone.||||||22-JUL-04
11862|Milligans Formation|60364|4|Described|p184, 189, 196|Visean|Tournaisian|Overlies Langfield Group and Bonaparte Formation (unconformable). Conformably overlain by Utting Calcarenite and Burvill Formation. Max. thickness: 2143m. Offshore shales and other marine clastics. Fossiliferous. Geological Province: Bonaparte Basin.||||||11-MAY-05
11862|Milligans Formation|60682|4|Described|p22 Table 5, 24|Visean|Tournaisian|Of Weabar Group. Unconformably overlies Langfield Group. Thickness: 2142m. Shale and siltstone, minor sandstone. Prograding delta and alluvial fan. Geological Province: Bonaparte Basin.||||||
11862|Milligans Formation|60701|5|Briefly described|p13|Early Carboniferous|Early Carboniferous|Contains oil in its marine shales.  Geological Province: Bonaparte Basin.||||||
11862|Milligans Formation|61023|5|Briefly described|p2 Fig. 2|Carboniferous|Carboniferous|Geological Province: Bonaparte Basin.||||||11-APR-08
11862|Milligans Formation|61250|6|Mentioned|p45|Carboniferous|Carboniferous|Unconformably overlies the Langford Group.  Geological Province: Bonaparte Basin.||||||
11862|Milligans Formation|61542|1|Redefined|p276, p277 Fig. 2|Visean|Tournaisian|Of Beere(1984). Gorter et al(2005) subdivided off part as Yow Fm.and relegated Waggon Creek Fm. to W.C. facies.Of Weaber Gp (basal) - fossiliferous shales and siltstone. Unconformable on Bonaparte Fm. Geol.province: onshore Bonapart Basin/Petrel-Sub-basin.||||||17-JUN-13
11862|Milligans Formation|62759|5|Briefly described|p1|Carboniferous|Carboniferous|Stated to unconformably overlie Langford Group - which should be Langfield Group.||||||
11862|Milligans Formation|62837|5|Briefly described|Stratigraphic columns|Visean|Tournaisian|Of the Weaber Group.  Age: <345-~328Ma. Geological Province:  Petrel Sub-basin (offshore).||||||01-MAR-10
11862|Milligans Formation|64580|6|Mentioned|map legend|||Of Weaber Group.||||||15-DEC-08
11862|Milligans Formation|64689|5|Briefly described|p16, p20 |Carboniferous|Carboniferous|Previously, thought to be the source of oil discoveries at Turtle-1 and Barnett-1; Gorter et al. (2004) suggest otherwise (the Langfield Group).||Basal unit in Weaber Group.||Overlies the Langfield Group unconformably.||
11862|Milligans Formation|64694|5|Briefly described|p231-241, p242 Tb.4, p243-244|Visean|Late Tournaisian|See also p245 Fig.9, p246-249, p252. Divided into a lower and an upper part by Lee and Gunn (1988). Previous to this study, marine shales in this unit were regarded as the source of Early Carboniferous to Permian-reservoired oils in the offshore Turtle and Barnett wells. The authors say that there is no compelling evidence that this unit contains oil-prone source beds where it has been sampled.||Unit in Weaber Group.||Unconformably overlies Bonaparte Formation and Langfield Group. Is overlain unconformably by Tanmurra Formation.||
11862|Milligans Formation|65331|5|Briefly described|Map legend|Visean|Visean|Of Bonaparte Basin. Of Weaber Group. Shale, siltstone, minor sandstone||||||
11862|Milligans Formation|67195|5|Briefly described|Appendix 2|||Bonaparte Basin.|||||Includes heterolithic fine-grained light grey sandstone and dark grey siltstone; slumping features; whispy siltstone in the sandstone.|
11862|Milligans Formation|67200|5|Briefly described|app 2 p8||||||||Heterolithic fine grained sandstone and siltstone; slumping features.|
11862|Milligans Formation|69099|6|Mentioned|500k_geologyp08_lut.csv|Pennsylvanian|Mississippian|||Weaber Group||||03-AUG-15
11862|Milligans Formation|69165|6|Mentioned|500k_geologyp08_lut.csv|Pennsylvanian|Mississippian|||Weaber Group||||
11862|Milligans Formation|69452|4|Described|p36:9, 11-16, 24-25, 28|Early Carboniferous|Early Carboniferous|Caye (1968); Gorter et al. (2005). Petrel Sub-basin, Bonaparte Basin. Moderately deep marine deposits. Up to 2143m thick. Offshore and onshore. Incorporates the former Waggon Creek Formation, now as a facies association. An upper interval, above a major sequence boundary, was assigned to the Yow Creek Formation by Gorter et al. (2005). Latest Tournaisian to early Visean. Significant gas flows obtained in Keep River-1 and Weaber-1, -2A. Acted as a seal to the mineralising brine which produced the Sandy Creek Zn-Pb-Ag deposit. Also appears as Milligans Shale in Fig.32.19. Has produced dry gas flows in most cases where it is intersected.||Weaber Group.||Unconformably overlies Septimus Limestone (Langfield Group) and (locally) Buttons Formation. Is overlain unconformably by Utting Calcarenite and Yow Creek Formation.|A recessive unit. Offshore: mostly fossiliferous silty shale. Onshore intersections also include interbedded sandstone, limestone (packstone and grainstone), and conglomerate of the Waggon Creek facies association. Abundant fauna and microflora.|12-JUL-16
11862|Milligans Formation|69634|5|Briefly described|500k_geologyp08_lut.csv|Carboniferous|Carboniferous|||Unit of Weaber Group.||||
11862|Milligans Formation|69653|6|Mentioned|p10|Carboniferous|Carboniferous|Petrel Sub-basin.||Weaber Group.||Overlies Bonaparte Formation. Is overlain by Yow Creek Formation.||
11862|Milligans Formation|69673|5|Briefly described|p168 fig 138, p171, p178, p181, p184|Early Carboniferous||Proven gas reservoir.||Weaber Group||Overlies Langfield Group, Buttons Formation, overlain by Yow Creek Formation|Fossiliferous silty shale and interbedded sandstone, limestone and conglomerates.|
11862|Milligans Formation|70061|5|Briefly described|Petrel Sub-basin; Fig.3, p2-3|Visean|Tournaisian|See also Regional geology: Fig.8, p8-9, p11-13, p16. Sandstones and shales filling in an incised channel system in the Bonaparte Formation. Hydrocarbon source and reservoir rocks and a regional seal. Oil- and gas-prone mudstones, previously attributed to this unit, are assigned to a Langfield Group equivalent. Hosts conventional and unconventional gas resources in the Weaber gas field and elsewhere.||Weaber Group.||Overlies Bonaparte Formation and Langfield Group. Is overlain by Yow Creek Formation.||12-JUL-16
11862|Milligans Formation|70206|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Bonaparte Basin.||Weaber Group|||Shale, siltstone, minor sandstone.|
11862|Milligans Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Weaber Group.|||Black and dark grey shale, partly calcareous; minor limestone; rare fine to medium-grained sandstone; thin to thick beds; diverse fauna|
11862|Milligans Formation|73117|6|Mentioned|p15|Visean|Visean|Bonaparte Basin, southern.||Weaber Group||Overlain by Yow Creek Formation.||
11911|Minglo Granite|23714|4|Described|p29|||See also page 19 Table 4. Geological Province: Cullen Batholith.||||||
11911|Minglo Granite|23715|5|Briefly described|Map legend||Proterozoic|Predominantly I-type. In the Cullen Batholith, of the Rum Jungle and Central Regions.||||||
11911|Minglo Granite|24197|5|Briefly described|p106 Tb. 15.1|Paleoproterozoic|Paleoproterozoic|Of the Cullen Supersuite. Age: ~1825Ma. Geological Province: Pine Creek Inlier.||||||07-FEB-11
11911|Minglo Granite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
11911|Minglo Granite|40168|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Cullen Batholith. Granite, leucogranite, granodiorite. Pink-green coarse porphyritic hornblende-biotite granite.||||||07-NOV-08
11911|Minglo Granite|40223|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Cullen Batholith. Coarse porphyritc pink and green granite.||||||07-NOV-08
11911|Minglo Granite|40823|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
11911|Minglo Granite|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
11911|Minglo Granite|41309|4|Described|p9|||||||||
11911|Minglo Granite|41311|4|Described|p18|||||||||
11911|Minglo Granite|42756|6|Mentioned|Fig.5 P6|||||||||
11911|Minglo Granite|42927|5|Briefly described|p428|||see also Fig.2 p430.||||||06-NOV-06
11911|Minglo Granite|43140|3|Fully described|p30||Paleoproterozoic|Of Cullen Batholith. Mapped as part of Cullen Granite by Noakes (1949) and Malone (1962).||||||07-NOV-08
11911|Minglo Granite|43624|6|Mentioned|p13|||Geological Province: Cullen Batholith.||||||
11911|Minglo Granite|43832|3|Fully described|Table8p40;49;Tb12p64||Paleoproterozoic|||||||07-NOV-08
11911|Minglo Granite|50586|5|Briefly described|p1.1, 4.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Of the Cullen Supersuite.||||||07-NOV-08
11911|Minglo Granite|60680|5|Briefly described|Map legend|Orosirian|Orosirian|Of the Cullen Supersuite.  Pink and green, coarse porphyritic hornblende-biotite granite; pink coarse porphyritic biotite granite; minor grey fine equigranular leucogranite in outer zone.  Age: 1825-1820Ma.||||||02-MAR-18
11911|Minglo Granite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1820-1840Ma. Of Fingerpost Suite, Cullen Supersuite. I-type. Pink and green, coarse porphyritic hornblende-biotite granite.||||||07-JAN-09
11911|Minglo Granite|65232|6|Mentioned|App. 2|||||||||09-FEB-10
11911|Minglo Granite|67564|3|Fully described|p7 Table 2, p13, pp33-34.|Paleoproterozoic|Paleoproterozoic|I-type. Pluton within Cullen Batholith, Pine Creek Orogen. 370 km2 in area.|1825 Ma.|Unit in Cullen Supersuite.||Intrudes Namoona, Mount Partridge, South Alligator and Finniss River Groups.|Massive, coarse, pink and green, porphyritic granite; minor peripheral fine, grey, equigranular leucogranites.|
11911|Minglo Granite|69420|5|Briefly described|p5:17-18, 20, 22|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Granite-dominated plutons; mineralogy and petrology/geochemistry summarised.||Fingerpost Suite.|||Coarse-grained porphyritic granite, monzonite and leucogranite. I-type.|12-JUL-16
11911|Minglo Granite|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||Fingerpost Suite.|||Pink and green, medium- to coarse-grained, porphyritic hornblende-biotite granite; pink, coarse-grained, porphyritic biotite granite; minor grey, fine-grained, equigranular leucogranite in outer zone.|
11983|Mitchiebo Volcanics|23363|5|Briefly described|344 Fig.3|||||||||
11983|Mitchiebo Volcanics|38237|6|Mentioned|Fig.3|||||||||
11983|Mitchiebo Volcanics|39338|5|Briefly described|p352|||||||||
11983|Mitchiebo Volcanics|39422|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of Carrara Range Gp.  Strongly altered vesicular and amygdaloidal basalt or trachyte; feldspathic and lithic sandstone; minor micaceous siltstone and shale.  Conformably overlies Don Creek Sst; unconformably overlain by Top Rocky Rhyolite, Musselbrook Fm.||||||10-JAN-05
11983|Mitchiebo Volcanics|39497|4|Described|p7|||||||||
11983|Mitchiebo Volcanics|39925|6|Mentioned|p337|||||||||
11983|Mitchiebo Volcanics|40811|6|Mentioned|p318|||||||||
11983|Mitchiebo Volcanics|45166|5|Briefly described|p27|||||||||
11983|Mitchiebo Volcanics|49018|2|Defined|p4|Carpentarian|Carpentarian|||||||
11983|Mitchiebo Volcanics|62659|5|Briefly described|Map Legend|Statherian|Statherian|Of the Carrara Range Group. Weathered or altered, massive to vesicular or microvesicular basalt and microdolerite; minor sandstone, mudstone and peperite.||||||
11983|Mitchiebo Volcanics|63866|5|Briefly described|p57|||Carrara Range, Leichhardt Superbasin.||||Overlain by the Top Rocky Rhyolite. Possibly equivalent to the Eastern Creek Volcanics.||
11983|Mitchiebo Volcanics|65337|4|Described|p6 Fig.3, p10 Table 3, p13.|||500-1000 m thick subaerial lava flows and shallow invasive flows. The upper sandstone part (Sweet 1984) is defined in this study as the new unit, Gator Sandstone. Resembles Seigal Volcanics, Eastern Creek Volcanics and Buddawadda Basalt. Highly magnetic.||Unit in Carrara Range Group.||Overlies Don Creek Sandstone. Is overlain by Gator Sandstone.|Weathered and/or altered, massive to vesicular or microvesicular basalt and microdolerite; lesser sandstone, mudstone and peperite.|
11983|Mitchiebo Volcanics|69433|4|Described|p18:2, 5-7|Statherian|Statherian|Southern succession, Lawn Hill Platform. 500-1000m thick. Is lithologically and geochemically indistinguishable from Seigal Volcanics (McArthur Basin). Is correlated with Seigal and Eastern Creek Volcanics and Buddawadda Basalt.||Carrara Range Group.||Conformably overlies Don Creek Sandstone. Is overlain by Gator Sandstone conformably, or Surprise Creek Formation and (locally) Top Rocky Rhyolite unconformably.|Weathered and/or altered, massive to vesicular or microvesicular basalt and microdolerite, with interbeds of sandstone, mudstone and peperite.|12-JUL-16
11983|Mitchiebo Volcanics|69673|4|Described|p52 fig 42,|||Up to 1km thick.||Carrara Range Group|||Basalt and microdolerite with interbeds of sandstone, mudstone and peperite.|
11983|Mitchiebo Volcanics|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.||Carrara Range Group||Overlies Don Creek Sandstone and underlies Gator Sandstone.||
11983|Mitchiebo Volcanics|72527|6|Mentioned|p7 Fig.1.4, p120, p169.|Paleoproterozoic|Paleoproterozoic|Rawlings et al. (2008) subdivided this unit creating the newly named Gator Sandstone at the top.||Carrara Range Group||Overlies Don Creek Sandstone and underlies Gator Sandstone.|Rhyolite clasts locally comprise as much as 10-15 percent of the total clast population; the remaining clasts are dominated by sandstone, siltstone, mudstone, layered chert, milky vein quartz and possibly small fragments of mafic volcanics.|
11983|Mitchiebo Volcanics|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the East part of the South Nicholson Basin and Lawn Hill Platform.||Carrara Range Group||Overlies Don Creek Sandstone and underlies Gator Sandstone.||
11983|Mitchiebo Volcanics|72919|6|Mentioned|p5|Paleoproterozoic|Paleoproterozoic|||Carrara Range Group||Underlain by Don Creek Sandstone. Overlain by Gator Sandstone.||
11983|Mitchiebo Volcanics|73043|6|Mentioned|p15 Fig.8|Paleoproterozoic|Paleoproterozoic|||||||
11984|Mithaka Formation|8187|5|Briefly described|Map legend|Ordovician|Ordovician|Siltstone, sandstone; mudstone.  Overlain by Cravens Peak beds.||||||21-JUN-04
11984|Mithaka Formation|8217|5|Briefly described|Map Legend|Ordovician|Ordovician|Siltstone, sandstone.||||||
11984|Mithaka Formation|10116|5|Briefly described|Map Legend|Middle Ordovician|Middle Ordovician|Of the Toko Group. Mudstone, quartzose sandstone.||||||19-AUG-04
11984|Mithaka Formation|12891|5|Briefly described|p733 Fig. 2|Late Ordovician|Late Ordovician|Geological province: SW Georgina Basin.||||||07-FEB-11
11984|Mithaka Formation|12951|6|Mentioned|p143 fig 4, p145 fig 6|Middle Ordovician|Early Ordovician|Georgina Basin.||||||
11984|Mithaka Formation|13995|6|Mentioned|p101|Middle Ordovician|Middle Ordovician|Georgina Basin.||||||
11984|Mithaka Formation|22646|6|Mentioned|Fig 5 on p 105|Late Ordovician|Early Ordovician|In the Georgina Basin.||||||06-NOV-06
11984|Mithaka Formation|22954|6|Mentioned|Fig3p9|Llanvirnian|Llanvirnian|||||||
11984|Mithaka Formation|23858|5|Briefly described|p924 Fig 8|Ordovician||||||||
11984|Mithaka Formation|24065|4|Described|p235|Middle Ordovician|Early Ordovician|Of Toko Group. Geological Province: Georgina Basin. Maximum thickness: 120m.||||||
11984|Mithaka Formation|24442|6|Mentioned|p49|||On TOBERMORY sheet.||||||
11984|Mithaka Formation|33111|4|Described|p38|||Mention Fig.9||||||
11984|Mithaka Formation|33738|6|Mentioned|p54|||||||||
11984|Mithaka Formation|34454|5|Briefly described|Table 2|||M.Ordovician||||||
11984|Mithaka Formation|34847|6|Mentioned|Table 1|||Stratigraphy and hydrocarbon prospects.||||||06-NOV-06
11984|Mithaka Formation|35121|6|Mentioned|Map legend|Middle Ordovician|Middle Ordovician|||||||
11984|Mithaka Formation|35139|4|Described|Table.2|||||||||
11984|Mithaka Formation|35146|6|Mentioned|p470|||||||||
11984|Mithaka Formation|36234|3|Fully described|p174|||||||||
11984|Mithaka Formation|36243|6|Mentioned|Table 1A|||||||||
11984|Mithaka Formation|36580|6|Mentioned|p469|||See also Fig.1.||||||06-NOV-06
11984|Mithaka Formation|37572|4|Described|p164|||See also Fig.8.||||||06-NOV-06
11984|Mithaka Formation|38832|6|Mentioned|p157|||||||||
11984|Mithaka Formation|39445|5|Briefly described|Table 4|||||||||
11984|Mithaka Formation|39921|6|Mentioned|Map legend|Middle Ordovician|Middle Ordovician|||||||
11984|Mithaka Formation|39943|6|Mentioned|Table 2A|||||||||
11984|Mithaka Formation|40136|5|Briefly described|p31|||||||||
11984|Mithaka Formation|40810|5|Briefly described|p15|||||||||
11984|Mithaka Formation|40906|6|Mentioned|Fig.11|||||||||
11984|Mithaka Formation|41524|6|Mentioned|Fig.3|||||||||
11984|Mithaka Formation|42059|6|Mentioned|Fig.2 P131|||||||||
11984|Mithaka Formation|42060|6|Mentioned|Fig.5 P140|||||||||
11984|Mithaka Formation|43105|5|Briefly described|Fig.4,p9.|||||||||
11984|Mithaka Formation|43236|6|Mentioned|p14||Ordovician|In the Georgina Basin.||||||06-NOV-06
11984|Mithaka Formation|43803|6|Mentioned|Fig.5,p71|||||||||
11984|Mithaka Formation|44308|14|Not recorded|p10,14,Tb.1||Early Ordovician|Of Toko Group.||||||
11984|Mithaka Formation|44309|2|Defined|Tb.1,p7,12-3,17,19,||Ordovician|Unit of Toko Group. Overlies Carlo Sandstone. Map.||||||
11984|Mithaka Formation|44312|14|Not recorded|Map Legend||Early Ordovician|(Middle Ordovician)||||||
11984|Mithaka Formation|44326|14|Not recorded|Map Legend||Early Ordovician|(Middle Ordovician)||||||
11984|Mithaka Formation|44334|14|Not recorded|map legend||Ordovician|Middle Ordovician.||||||
11984|Mithaka Formation|44358|2|Defined|App.p18|Early Ordovician|Early Ordovician|See also p10, Tb.1. (Middle-Middle Ordovician).||||||11-FEB-09
11984|Mithaka Formation|44469|2|Defined|p.10, Tb.I|Middle Ordovician|Middle Ordovician|(F53-12). Conformably overlies Carlo Sandstone. Of the Toko Group.  Fossils. See also p.16.||||||09-FEB-17
11984|Mithaka Formation|44470|5|Briefly described|map legend||Ordovician|Middle Ordovician.||||||02-DEC-04
11984|Mithaka Formation|44848|14|Not recorded|p111|||||||||
11984|Mithaka Formation|44852|14|Not recorded|p71||Ordovician|||||||
11984|Mithaka Formation|44920|14|Not recorded|Map Legend, Sheet 4||Ordovician|Middle Ordovician||||||
11984|Mithaka Formation|45052|3|Fully described|p130|||M.Ord. See also p38.||||||06-NOV-06
11984|Mithaka Formation|45118|6|Mentioned|p3|||||||||
11984|Mithaka Formation|45148|6|Mentioned|Fig.4|||In the Georgina Basin.||||||06-NOV-06
11984|Mithaka Formation|45155|6|Mentioned|Fig.8|||||||||
11984|Mithaka Formation|46841|6|Mentioned|p97|||||||||
11984|Mithaka Formation|46940|4|Described|p57|||||||||
11984|Mithaka Formation|46956|6|Mentioned|p160|||||||||
11984|Mithaka Formation|46959|6|Mentioned|Table 1|||||||||
11984|Mithaka Formation|46973|6|Mentioned|p52|||||||||
11984|Mithaka Formation|47024|6|Mentioned|Table 1|||||||||
11984|Mithaka Formation|49027|4|Described|p19|||Mention p20.||||||06-NOV-06
11984|Mithaka Formation|60122|3|Fully described|p33|Middle Ordovician|Middle Ordovician|Of the Toko Gp. Conformable on Carlo Sandstone; conformable beneath Ethabuka Sandstone and Poodyea Formation. Max. thickness: 156m. Geological province: Georgina Basin. See also p4-5, p10 Tb. 1.||||||18-MAY-05
11984|Mithaka Formation|60590|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Of the Toko Group.  Gypsiferous shale and siltstone, calcareous siltstone, quartz sandstone, glauconitic and micaceous quartz sandstone, minor coquinite and granule conglomerate.||||||
11984|Mithaka Formation|61404|5|Briefly described|Map legend|Middle Ordovician|Middle Ordovician|Of the Toko Group. Gypsiferous shale and siltstone, calcareous siltstone, quartz sandstone, glauconitic and micaceous quartz sandstone, minor coquinite and granule conglomerate. Geological Province: southern Georgina Basin.||||||12-OCT-05
11984|Mithaka Formation|64068|3|Fully described|p77-78, p19|Late Ordovician|Late Ordovician|Diverse fauna. Deposited inshore of Carlo Sandstone barrier.||Of Toko Group.||Conformably and gradationally overlies Carlo Sandstone. Conformably and gradationally overlain by Ethabuka Sandstone, or unconformably by Cravens Peak beds.|Gypsiferous green shale, calcareous siltstone; minor calcareous sandstone, coquinite and granule conglomerate.|04-APR-12
11984|Mithaka Formation|64778|6|Mentioned|p13|Ordovician|Ordovician|Toko Syncline, Southern Georgina Basin.||||||
11984|Mithaka Formation|64812|5|Briefly described|p237 Fig. 2|Middle Ordovician|Middle Ordovician|Geological Province: southern Georgina Basin.||||||07-FEB-11
11984|Mithaka Formation|64813|5|Briefly described|p256 Fig. 3|Middle Ordovician|Middle Ordovician|Geological Province: southern Georgina Basin.||||||11-FEB-09
11984|Mithaka Formation|65237|5|Briefly described|p4 Fig. 7, p10|Ordovician|Ordovician|Geological province: southern Georgina Basin.||||||07-FEB-11
11984|Mithaka Formation|65489|5|Briefly described|p125|Ordovician|Ordovician|Georgina Basin.||||Overlies Carlo Sandstone. Is overlain by Ethabuka Formation.||
11984|Mithaka Formation|67323|5|Briefly described|GIS attrib tbl, p83, p90, p92 Fig.12.2|Early Ordovician|Early Ordovician|See also Solid Geology Map. West Toko Syncline, Georgina Basin.||Toko Group.||Overlies Carlo Sandstone. Is overlain by Ethubuka Sandstone.|Siltstone, arenite, quartzose, arenite, shale|
11984|Mithaka Formation|67402|6|Mentioned|p25, p25 tbl RRM3|Darriwillian|Darriwillian|Georgina Basin. Assessed to be a potential unconventional seal for Carbon dioxide storage. Deposited in a tidal or lagoonal environment associated with a barrier island system. Maximum thickness of 156m. See also p213 fig GRG3, p215-p217.||||Conformably overlies the Carlo Sandstone. Overlain by the Ethabuka Sandstone.|Siltstone and fine sandstone.|
11984|Mithaka Formation|69437|5|Briefly described|p22:10|Ordovician|Ordovician|Southern Georgina Basin.||||Overlies Carlo Sandstone. Is overlain by Ethabuka Sandstone.||12-JUL-16
11984|Mithaka Formation|69443|4|Described|p28:7, 27, 29, 46|Late Ordovician|Late Ordovician|Casey in Smith (1963). Southern Georgina Basin. Poorly exposed. 20-156m thick. Mostly undescribed fossil fauna (listed). Late Gisbornian age. Low-energy marine lagoon deposits with limited tidal range. Potential seal for the Carlo Sandstone.||Toko Group.||Conformably and gradationally overlies Carlo Sandstone. Is overlain conformably and gradationally by Ethabuka Sandstone, or unconformably by Cravens Peak beds.|Thinly bedded gypsiferous shale, calcareous siltstone, minor calcareous, glauconitic and micaceous quartz sandstone, and minor coquinite and granule conglomerate.|12-JUL-16
11984|Mithaka Formation|69458|6|Mentioned|p42:20|||Georgina Basin.||||Is overlain unconformably by Poodyea Formation.||14-SEP-18
11984|Mithaka Formation|69591|5|Briefly described|p87, p95-96|Ordovician|Ordovician|West Toko Syncline, Georgina Basin. 60-120m thick. Contains a moderately diverse fauna (listed).||Toko Group.||Conformably and transitionally overlies Carlo Sandstone. Is overlain conformably by Ethabuka Sandstone.|Succession of brown and grey gypsiferous siltstone and sandstone, white glauconitic quartz sandstone, green gypsiferous shale, calcareous shale and thin coquinite. Sand increases up-section.|
11984|Mithaka Formation|69599|6|Mentioned|p600|||||||Is overlain unconformably by the Poodyea Formation.||
11984|Mithaka Formation|69673|5|Briefly described|p118, p119 fig 94, p128, p136|Ordovician|Ordovician|120m thick.||Toko Group||Overlies Carlo Sandstone, overlain by Ethabuka Sandstone|Gypsiferous shale, calcareous siltstone and minor calcareous, glauconitic and micaceous quartz sandstone.|
11984|Mithaka Formation|70380|6|Mentioned|p745|Katian|Sandbian|Southern Georgina Basin.||||||
11984|Mithaka Formation|72297|5|Briefly described|p748|||Forms suitable cap rocks in the Toko Syncline, Georgina Basin.|||||Siltstone and mudstone.|
11984|Mithaka Formation|72503|6|Mentioned|p33|||Georgina Basin. Contains typical shallow-water [conodont] forms (e.g., Aurilobodus leptosomatus and Tangshanodus sp.).||||||
11995|Mittiebah Sandstone|23328|5|Briefly described|1031 Fig.2|Proterozoic|Proterozoic|||||||07-SEP-09
11995|Mittiebah Sandstone|24442|5|Briefly described|p23 Fig. 2|Mesoproterozoic|Mesoproterozoic|||||||
11995|Mittiebah Sandstone|31396|6|Mentioned|p1190|||||||||
11995|Mittiebah Sandstone|32660|5|Briefly described|Table 5|||||||||
11995|Mittiebah Sandstone|37572|6|Mentioned|Fig.7|||||||||
11995|Mittiebah Sandstone|38444|6|Mentioned|p307|||||||||
11995|Mittiebah Sandstone|39497|6|Mentioned|p16|||||||||
11995|Mittiebah Sandstone|41721|4|Described|p29|||Conformably overlies Mullera Formation. Max. thickness: 2700m. Consists of quartz sandstone, feldspathic sandstone, and arkose.||||||02-AUG-07
11995|Mittiebah Sandstone|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
11995|Mittiebah Sandstone|43010|5|Briefly described|Fig.6||Mesoproterozoic|Of South Nicholson Group. Of "Mid Proterozoic" age.||||||06-NOV-06
11995|Mittiebah Sandstone|44283|14|Not recorded|p.7|||Outcrops to west of (E53-15).||||||
11995|Mittiebah Sandstone|44285|14|Not recorded|p.6||Adelaidean|Outcrops on RANKEN sheet (E53-16).||||||06-NOV-06
11995|Mittiebah Sandstone|44301|2|Defined|map, p.7||Neoproterozoic|BRUNETTE DOWNS map (E53-11). Upper Proterozoic.||||||06-NOV-06
11995|Mittiebah Sandstone|44302|14|Not recorded|map legend|||Crossbedded, ripple marked ferruginous quartz sandstone.||||||17-OCT-11
11995|Mittiebah Sandstone|44305|14|Not recorded|p.15|||(E53-8). opp.6,18.||||||
11995|Mittiebah Sandstone|44306|14|Not recorded|map legend|||(?) Upper Proterozoic.||||||
11995|Mittiebah Sandstone|44441|2|Defined|opp.p.6,7, Tb.1, map||Neoproterozoic|Upper Proterozoic. (E53-12,16).||||||
11995|Mittiebah Sandstone|44442|14|Not recorded|map legend||Neoproterozoic|Upper Proterozoic.||||||
11995|Mittiebah Sandstone|44473|14|Not recorded|p.9,10 opp. p.7|||(E53-7). Formation of South Nicholson Group.||||||
11995|Mittiebah Sandstone|44474|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
11995|Mittiebah Sandstone|44482|14|Not recorded|p.5,7, opp. p.6, map|||(E53-12). See also p.10,13, for more details.||||||
11995|Mittiebah Sandstone|44483|5|Briefly described|map legend|||Upper (?) Proterozoic.||||||
11995|Mittiebah Sandstone|45032|4|Described|p7,9||Adelaidean|See also Pl.1, p22,10,25,89. (E53-12,16).||||||
11995|Mittiebah Sandstone|45052|4|Described|p71|||Adelaidean.||||||06-NOV-06
11995|Mittiebah Sandstone|62657|5|Briefly described|Map Legend|Calymmian|Calymmian|Of the Wild Cow Subgroup. Medium to thick, fine to coarse grained, quartzose to lithic sandstone; minor interbeds of pebble or boulder conglomerate and siltstone.||||||
11995|Mittiebah Sandstone|62659|5|Briefly described|Map Legend|Calymmian|Calymmian|Of the Accident Subgroup. Medium to thick bedded, fine to coarse grained, quartzose to lithic sandstone; minor interbeds of pebble or cobble conglomerate and siltstone.||||||
11995|Mittiebah Sandstone|64443|4|Described|p2, p3-4, p5 Fig.3, p6 Tb.1.|Calymmian|Calymmian|Probable lateral relationship with Constance Sandstone; possibly conformably overlain by Mullera Formation; when Mullera Formation absent is unconformably overlain by Helen Springs Volcanics. Forms moderately prominent isolated ridges. 2200 m+ thick.||Of the Accident Subgroup.||Conformably or disconformably overlies the Crow Formation; unconformably overlain by Wonarah Formation.|Quartzose to sublithic sandstone, minor siltstone and conglomerate interbeds; fresh surfaces are pink-brown, weathered rocks are orange-, purple-, dark-brown.|14-MAY-14
11995|Mittiebah Sandstone|65336|5|Briefly described|Map Legend|Calymmian|Calymmian|Of Accident Subgroup, South Nicholson Group. Medium to thick, fine- to coarse- grained, quartzose to lithic sandstone; minor interbeds of pebble or cobble conglomerate and siltstone.||||||
11995|Mittiebah Sandstone|65337|3|Fully described|p54-57, p9 Fig.5, p38 Table 5.|Mesoproterozoic|Mesoproterozoic|Northwest MOUNT DRUMMOND area. Probable correlative of Constance Sandstone. Over 2200 m of alternating shallow storm-influenced marine and braided fluvial deposits. Strongly resistant unit. Fine parallel magnetic banding; ? heavy mineral concentrations.||||Overlies Crow Formation. Is probably overlain by Mullera Formation.|Fine- to coarse-grained, quartzose to lithic sandstone; minor interbeds of pebble or cobble conglomerate and siltstone.|15-MAY-17
11995|Mittiebah Sandstone|65344|5|Briefly described|p13, 16|Mesoproterozoic|Mesoproterozoic|Of the South Nicholson Group, South Nicholson Basin. See thin section descriptions for detail.||Of the South Nicholson Group.||||03-MAY-12
11995|Mittiebah Sandstone|67144|5|Briefly described|Map legend.|Calymmian|Calymmian|||Unit in South Nicholson Group.||Is unconformably overlain by Bukalara Sandstone.|Medium to thick, fine- to coarse-grained, quartzose to lithic sandstone; minor interbeds of pebble or cobble conglomerate and siltstone.|
11995|Mittiebah Sandstone|67150|5|Briefly described|Map legend.|Calymmian|Calymmian|South Nicholson Basin.||Unit in South Nicholson Group. May be part of Accident Subgroup.|||Medium to thick, fine- to coarse-grained, quartzose to lithic sandstone; minor interbeds of pebble or cobble conglomerate and siltstone.|17-OCT-11
11995|Mittiebah Sandstone|67352|4|Described|p4,p15-16,p23,p36,p40-41,p51,p60,p69|Calymmian|Calymmian|Over 2200 m thick in the Mittiebah Range. Aquifer for farms.||Accident Subgroup||Overlies Crow Formation conformably or disconformably. Overlain unconformably by Anthony Lagoon Formation, Wonarah Formation, Mullera Formation or Helen Springs Volcanics.|Fine to coarse, quartzose to sublithic sandstone, with minor interbeds of conglomerate and siltstone.|
11995|Mittiebah Sandstone|69434|4|Described|p19:2, 5-7|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin. Mapping of this unit by Smith and Roberts (1963) included rocks now assigned to the Crow Formation. 450-2200m thick. Alternating shallow storm-influenced marine and braided fluvial deposits. Tentatively correlated with Constance Sandstone.||Accident Subgroup.||Overlies Crow Formation conformably to disconformably. Is overlain probably conformably by Mullera Formation.|Fine to coarse, quartzic to lithic sandstone; minor interbeds of pebble or cobble conglomerate and siltstone.|12-JUL-16
11995|Mittiebah Sandstone|69443|6|Mentioned|p28:22|||South Nicholson Basin.||||May be unconformably overlain by Anthony Lagoon Formation (Georgina Basin).||12-JUL-16
11995|Mittiebah Sandstone|69673|6|Mentioned|p56|||Up to 2200m thick. Deposited in shallow storm influenced marine and braided fluvial settings.||Accident Subgroup|||Quartzose to lithic sandstone with minor interbeds of pebble or cobble conglomerate and siltstone.|
11995|Mittiebah Sandstone|70849|5|Briefly described|Map legend.|Calymmian|Calymmian|South Nicholson Basin.||South Nicholson Group.||Shown as overlying Mullera Formation. Is overlain unconformably by Bukalara Sandstone.|Quartz sandstone, feldspathic sandstone, arkose.|15-MAY-17
11995|Mittiebah Sandstone|70897|6|Mentioned|Fig.1.7.6|||Appears simply as Mittiebah. South Nicholson Basin.||||||
11995|Mittiebah Sandstone|70968|6|Mentioned|p131 Fig.118, p132|Calymmian|Calymmian|||Accident Subgroup.||||
11995|Mittiebah Sandstone|71369|6|Mentioned|p5|||Rawlings et al. (2008) showed this unit, previously interpreted to overlie the Mullera Formation, to be equivalent to the Constance Sandstone. South Nicholson Basin.||||Equivalent to the Constance Sandstone.||20-FEB-18
11995|Mittiebah Sandstone|72526|4|Described|p1-2, p4, 7, 8, 33, p56-75, p86,87.|Mesoproterozoic|Mesoproterozoic|Distinct U-Pb SHRIMP maximum depositional ages obtained from 2 samples: 1658+/-23 Ma from Brunette Downs sheet area, 1586+/-7 Ma from type locality in Mittiebah Range, Mt Drummond map sheet. Shown as being located in the west of the South Nicholson Basin. Possibly lateral correlative with Constance Sandstone. Comparison of detrital age spectra of Bowgan Sandstone, Crow Fomation, Wild Cow Subgroup and some Caulfield beds samples with the older 'Mittebah Sandstone' sample suggests there may be another older package of rocks in the area, equivalent to the McNamara Group.   For lithology and deposition ref Ahmad and Munson, 2013b. This unit is c. 450-2200m thick.|1586+/-7 Ma max dep age.|Accident Subgroup||Conformably to disconformably overlies Tobacco Member, Crow Formation and underlies Mullera Formation.|Includes fine to coarse-grained, quartz dominated to lithic sandstone with minor interbeds of siltstone and pebble to cobble conglomerate.|
11995|Mittiebah Sandstone|72527|6|Mentioned|p1, p7 Fig.1.4, p161, p196.|Mesoproterozoic|Mesoproterozoic|The assignment of Mittiebah Sandstone to the poorly outcropping sandstones in north-eastern BRUNETTE DOWNS map is provisional (GA 2676117; Anderson et al., 2019a).||Accident Subgroup||Unconformably overlies Tobacco Member and Crow Formation, underlies Mullera Formation and is unconformably laterally equivalent to Constance Sandstone.||
11995|Mittiebah Sandstone|72912|4|Described|p5 Fig.3, p25, p33 Fig.12, p48.|Mesoproterozoic|Mesoproterozoic|Located in the west part of the South Nicholson Basin||Accident Subgroup||Overlies Crow Formation and underlies Mullera Formation, and is equivalent to Bowthorne Member and Constance Sandstone.|Includes sandstone.|
11995|Mittiebah Sandstone|72919|4|Described|p. 1, 4-5, 47, 70-74, 77-81, 85, 95-97|Calymmian|Statherian|South Nicholson Basin, Lawn Hill Platform. Approximately 450-2200 m thick. Type locality is in the Mittiebah Range. Deposited in alternating shallow, storm-influenced marine and braided fluvial environments. Contact with overlying Mullera Formation is inferred to be conformable but is not exposed. Also unconformably overlain by Paleozoic Georgina Basin and/or Cenozoic strata. A maximum depositional age of 1586 +/- 7 Ma was reported for a sample (2676116) from the type area by Anderson et al. (2019). A new U-Pb SHRIMP zircon maximum depositional age of 1625 +/- 27 Ma was reported herein for a sample from rocks mapped as this unit (Mittiebah Formation) but may be from an unrelated late Paleoproterozoic unit, similar to sample 2676117 reported by Anderson et al. (2019) based on the absence of a Mesoproterozoic population in the detrital zircon spectra. New data herein finds that strata previously interpreted as Mittiebah Sandstone? in drillhole CRDD001 are more likely to represent the Bukalara Sandstone based on similar detrital zircon signatures (new U-Pb SHRIMP zircon maximum depositional age of 1316 +/- 27 Ma). Carson et al. (2020) proposed an expanded version of the Benmara Group that includes strata of [or equivalent to?] this unit (Mittiebah Formation) in the hanging wall of the Benmara Fault based on comparison of detrital zircon spectra with that of late Paleoproterozoic successions.|1625 +/- 27 Ma U-Pb SHRIMP|Accident Subgroup, South Nicholson Group|Tobacco Member|Conformably to disconformably overlies Tobacco Member (Crow Formation, Wild Cow Subgroup). Overlain by Mullera Formation. Equivalent to Constance Sandstone.|Fine- to coarse-grained, quartz-dominated to lithic sandstone with minor interbeds of siltstone and pebble to cobble conglomerate.|
11995|Mittiebah Sandstone|73042|6|Mentioned|p4|||The Mittiebah Sandstone is recorded in the Mesoproterozoic South Nicholson Group in the western portion of the South Nicholson Basin region, which corresponds to the formally accepted usage (see ASUD). It is also used in the Paleoproterozoic Benmara Group from the same region/province, written as Mittiebah* Formation, which might indicate tentative or uncertain use of this nomenclature, or the age of the unit. South Nicholson Basin region, Roper Superbasin (and Isa Superbasin for Mittiebah* Formation).||Accident Subgroup, South Nicholson Group||Underlain by Crow Formation, overlain by Mullera Formation. Partly underlain and equivalent to Caulfield beds.||
11995|Mittiebah Sandstone|73043|6|Mentioned|p7 Fig.2|Paleoproterozoic|Paleoproterozoic|||Benmara Group||||
11995|Mittiebah Sandstone|73083|6|Mentioned|p34-35, p39|||Three small ridges on the Mount Drummond map sheet were mapped as this unit but may have been misidentified.||South Nicholson Group||Equivalent to Constance Sandstone. Underlain by Mullera Formation.||
12097|Money Shoal beds|42056|5|Briefly described|Fig.6 p95|||||||||16-NOV-06
12126|Montara Formation|5952|5|Briefly described|p215 Fig. 5|||Appears as Montara in figure. Geological Province: Bonaparte Basin.||||||01-MAR-10
12126|Montara Formation|7142|6|Mentioned|p350 Fig.4.|Late Jurassic|Middle Jurassic|Browse Basin.||||Overlies Plover Formation. Is overlain by Lower Vulcan Formation.||
12126|Montara Formation|23377|6|Mentioned|p211|||In the Vulcan Sub-basin.||||||07-NOV-06
12126|Montara Formation|23378|6|Mentioned|p180 Fig.2|Late Jurassic|Middle Jurassic|Of the Swan Group.  In the Vulcan Sub-basin.||||||07-NOV-06
12126|Montara Formation|24427|5|Briefly described|p49 Fig.2|Late Jurassic|Middle Jurassic|Geological Province: Bonaparte Basin.||||||09-MAR-05
12126|Montara Formation|42053|4|Described|p40|||See also Fig.2||||||01-MAR-10
12126|Montara Formation|42395|5|Briefly described|p81|||||||||
12126|Montara Formation|43826|6|Mentioned|Fig.2,p163||Middle Jurassic|||||||01-MAR-10
12126|Montara Formation|61550|6|Mentioned|p495 Fig.2. |Callovian|Callovian|||Unit in Swan Group.||||
12126|Montara Formation|62837|5|Briefly described|Stratigraphic columns|Middle Jurassic|Middle Jurassic|Age: ~163-~156Ma. Geological Province:  Vulcan Sub-basin.||||||01-MAR-10
12126|Montara Formation|63358|5|Briefly described|p4 Fig. 1.3|Oxfordian|Callovian|||||||01-MAR-10
12126|Montara Formation|64689|5|Briefly described|p7 Fig.6, p14-15|Late Jurassic|Middle Jurassic|See also references to mis-spelt Montara Sandstone (p8-9). A near top reservoir reflector.||||||
12126|Montara Formation|64696|6|Mentioned|p125, p127 Fig.2, p131, p134, p136-137|Late Jurassic|Middle Jurassic|Deposition in fan-deltas and alluvial fans.|||||Sandstones, shales.|
12126|Montara Formation|64697|6|Mentioned|p89 |Late Jurassic|Late Jurassic|In 1988, BHPP encountered a 10 m oil leg below a 20 m gas column in its Montara-1 well.||||||
12126|Montara Formation|66187|5|Briefly described|p413 Fig.2, p414 Tb.1|Oxfordian|Oxfordian|Swan Group. Underlies the Lower Vulcan Formation, overlies the Plover Formation. Mount Ashmore Dome. Shallow marine sandstone. Mis-spelt as Montana in Fig.2.||||||
12126|Montara Formation|67195|5|Briefly described|Appendix 2|||Browse Basin.|||||Includes heterolithic fine-grained yellow/buff sandstone and dark grey siltstone; highly bioturbated; ocassional reddish brown nodules/diagenetic overprint?|
12126|Montara Formation|67200|5|Briefly described|app 2 p7||||||||Heterolithic fine grained sandstone and siltstone; highly bioturbated.|
12126|Montara Formation|68135|5|Briefly described|p51 fig 2a|Late Jurassic|Middle Jurassic|Browse Basin.||||Is overlain by Vulcan Formation.||14-SEP-17
12126|Montara Formation|69297|6|Mentioned|p303, p305, p308, p309|Upper Jurassic|Upper Jurassic|Barcoo and Seringapatam Sub-basins of the Browse Basin. Deposited in a fluvial to deltaic environment.||Swan Group||Unconformably overlies the Ashmore Volcanics and the Plover Formation. Overlain by the Lower Vulcan Formation.||
12126|Montara Formation|69452|5|Briefly described|p36:15, 21-22|Jurassic|Jurassic|Bonaparte Basin.||Swan Group.||Equivalent to Elang Formation.||12-JUL-16
12126|Montara Formation|69689|6|Mentioned|p16|Jurassic|Jurassic|Browse, Bonaparte Basins.||||Overlies Plover Formation.||
12126|Montara Formation|70061|5|Briefly described|Regional geology; Fig.7, p6, p12, p17|Oxfordian|Callovian|See also Vulcan: Fig.2, p1-2. Bonaparte Basin; commercial petroleum reservoir. Contains mature marine, oil- and gas-prone source rocks.||Swan Group.||Overlies Plover Formation. Is overlain by Lower Vulcan Formation.|Retrogradational deltaic sandstones and transgressive marine shales.|12-JUL-16
12126|Montara Formation|70064|5|Briefly described|Northern Fig.2; p1-2. Yampi: Fig.2|Oxfordian|Callovian|See also Regional: Fig. 6; p6, p8-10. Central: Fig.2; p2. Caswell-Barcoo Sub-basins, Browse Basin. Potential source rock, and potential reservoirs in horsts and tilted fault-blocks. Oil and gas shows occur locally. Apparently includes [an informal? unit called] the Ichthys Formation: appears in Northern: p2 as Montara (Ichthys) Formation.||Swan Group.||Overlies Plover Formation or Ashmore Volcanics. Is overlain by Lower Vulcan Formation.|Prograding fan-delta systems.|12-JUL-16
12130|Montejinni Limestone|12891|5|Briefly described|p731, p733 Fig. 2|Late Cambrian|Middle Cambrian|Overlain by Hooker Creek Formation. Geological province: Wiso Basin. Sampled for hydrocarbon shows (p735). Fractured and vuggy carbonates are present and may have enhanced permeability.||||||07-FEB-11
12130|Montejinni Limestone|14019|5|Briefly described|p20|Middle Cambrian|Middle Cambrian|Fossiliferous unit.  Overlies the Antrim Plateau Volcanics.||||||
12130|Montejinni Limestone|23328|5|Briefly described|1030|Middle Cambrian|Early Cambrian|||||||07-SEP-09
12130|Montejinni Limestone|23410|5|Briefly described|Map Legend|Ordian-Early Templetonia|Ordian-Early Templetonia|Bioclast, stylolitic, onkoid, mottled, ribbon and cryptomicrobial limestone and dolostone, minor siliciclastic and dolomitic mudstone; chert and evaporite nodules; local basal breccia; chertified at surface; fossiliferous. Geol. Prov: Wiso Basin.||||||02-NOV-05
12130|Montejinni Limestone|23733|5|Briefly described|p22, 23|Cambrian|Cambrian|||||||
12130|Montejinni Limestone|23770|5|Briefly described|p2 Fig. 1|Middle Cambrian|Middle Cambrian|Shallow marine to intertidal calcilutite, calcarentie, dolomite and clacareous siltstone.  Geological Province: Wiso Basin||||||
12130|Montejinni Limestone|23821|5|Briefly described|p244|||||||||14-NOV-06
12130|Montejinni Limestone|23981|6|Mentioned|p65|||Geological Province: South-eastern Wiso Basin.||||||14-FEB-07
12130|Montejinni Limestone|24122|3|Fully described|p13|Cambrian|Cambrian|Unconformably overlies Antrim Plateau Volcanics. Approximately 60m. thick.  Geological Province: Wiso Basin.||||||
12130|Montejinni Limestone|24297|4|Described|p19|Cambrian|Cambrian|Maximum thickness: 151m.  Unconformably overlies Antrim Plateau Volcanics. Geological Province: Wiso Basin.||||||
12130|Montejinni Limestone|24298|5|Briefly described|Map Legend|Cambrian|Cambrian|Limestone, dolostone, mudstone, breccia, calcilutite, calcarenite.||||||19-OCT-05
12130|Montejinni Limestone|24300|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Daly River Group.   Geological Province: Wiso Basin||||||07-NOV-06
12130|Montejinni Limestone|24303|3|Fully described|p39|Ordian-Early Templetonian|Ordian-Early Templetonian|Geological Province: Wiso Basin. Maximum Thickness: 151m. Correlates with the Tindall Limestone and Gum Ridge Formation. See also p63 Appendix.||||||04-DEC-12
12130|Montejinni Limestone|24304|5|Briefly described|Map legend|Cambrian|Cambrian|Limestone and dolostone; minor fine-grained sandstone and siliciclastic mudstone; fossiliferous; chert and nodular evaporitic pseudomorphs; silicified outcrop, recessive.||||||17-OCT-05
12130|Montejinni Limestone|28255|5|Briefly described|Summary|||Overlies Antrim Plateau Volcanics in the east. Correlated with Headleys Limestone. Geological Province: Daly River and Wiso Basins.||||||15-JUN-05
12130|Montejinni Limestone|29591|6|Mentioned|p107|||||||||
12130|Montejinni Limestone|30003|4|Described|p11, p14|Middle Cambrian|Middle Cambrian|Basal unit in the Wiso Basin.  Equivalent in part to Tindall Limestone in the Daly River Basin. Overlies the Antrim Plateau Volcanics.||||||19-APR-05
12130|Montejinni Limestone|30004|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
12130|Montejinni Limestone|31412|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
12130|Montejinni Limestone|31413|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
12130|Montejinni Limestone|31637|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
12130|Montejinni Limestone|31917|5|Briefly described|p32|||See Fig.3.||||||
12130|Montejinni Limestone|32175|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
12130|Montejinni Limestone|32775|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|||||||02-DEC-04
12130|Montejinni Limestone|33022|6|Mentioned|p271|||||||||
12130|Montejinni Limestone|33164|6|Mentioned|p87|||||||||
12130|Montejinni Limestone|33373|3|Fully described|Table 3|||p12.||||||07-NOV-06
12130|Montejinni Limestone|33374|4|Described|p13|||||||||
12130|Montejinni Limestone|33376|6|Mentioned|Map legend|Early Ordovician|Middle Cambrian|Middle Cambrian to Lower Ordovician||||||
12130|Montejinni Limestone|34051|5|Briefly described|Table 1|||L.- M.Camb. See also pp4,6 -11.||||||07-NOV-06
12130|Montejinni Limestone|34052|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
12130|Montejinni Limestone|34438|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
12130|Montejinni Limestone|34439|5|Briefly described|Table 1|||Middle Cambrian||||||
12130|Montejinni Limestone|34440|5|Briefly described|Table 1|||M.Camb.||||||
12130|Montejinni Limestone|34810|5|Briefly described|p8|||Does not outcrop in sheet area.||||||07-NOV-06
12130|Montejinni Limestone|35125|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
12130|Montejinni Limestone|35224|4|Described|Table 1|||See also p5.||||||07-NOV-06
12130|Montejinni Limestone|35227|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
12130|Montejinni Limestone|35229|4|Described|Table.1|||||||||
12130|Montejinni Limestone|35231|4|Described|Table.1|||||||||
12130|Montejinni Limestone|36335|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|Middle Cambrian(Ordian).||||||
12130|Montejinni Limestone|36473|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian to Ordovician||||||
12130|Montejinni Limestone|39210|6|Mentioned|p48|||||||||
12130|Montejinni Limestone|39523|6|Mentioned|p96|||||||||
12130|Montejinni Limestone|41864|6|Mentioned|p157|||In Wiso Basin||||||
12130|Montejinni Limestone|42059|4|Described|p135|||See also Fig.2||||||
12130|Montejinni Limestone|42504|6|Mentioned|p77|||||||||
12130|Montejinni Limestone|44113|5|Briefly described|p240|Middle Cambrian|Middle Cambrian|Of the Daly River Group. Geological Province: Daly River Basin. Maximum Thickness: 78m.||||||
12130|Montejinni Limestone|44411|14|Not recorded|map legend||Middle Cambrian|Middle Cambrian.||||||
12130|Montejinni Limestone|44965|14|Not recorded|Not recorded|||||||||25-JAN-18
12130|Montejinni Limestone|45022|6|Mentioned|p.102||Middle Cambrian|||||||
12130|Montejinni Limestone|45064|3|Fully described|Table 1|||See also p19.||||||07-NOV-06
12130|Montejinni Limestone|45148|2|Defined|p9|Middle Cambrian|Middle Cambrian|Also mentioned p2.||||||07-NOV-06
12130|Montejinni Limestone|45155|6|Mentioned|Fig.8|||||||||
12130|Montejinni Limestone|45168|6|Mentioned|p6|||||||||
12130|Montejinni Limestone|47044|6|Mentioned|p191|||||||||
12130|Montejinni Limestone|48942|6|Mentioned|p73|||Strat. table.||||||
12130|Montejinni Limestone|48950|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
12130|Montejinni Limestone|50353|5|Briefly described|Map Legend|Ordian-Early Templetonia|Ordian-Early Templetonia|Grey bioclast, styolitic, onkoid, mottled, ribbon and cryptomicrobial limestone and dolostone, minor maroon siliciclastic and yellow-grey dolomitic mudstone;chert and evaporite nodules; local basal breccia; chertified at surface, fossiliferous.||||||04-JUN-04
12130|Montejinni Limestone|60672|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Limestone, dolostone, calcareous mudstone and siltstone. Geological Province incorrectly shown as Ord Basin. Should be Wiso Basin||||||14-NOV-06
12130|Montejinni Limestone|60684|2|Defined|p48-49 Appendix, p16-17||Ordian-Early Templetonian|Unconformably overlies Antrim Plateau Volcanics; conformably overlain by Hooker Creek Formation and unconformably by Point Wakefield beds where former is absent. Age is probably Ordian- Early Templetonian. Max. thickness: 151.2m. Geol.Prov: Wiso Basin.||||||25-JAN-18
12130|Montejinni Limestone|60685|3|Fully described|p3 Fig. 2, p1|Cambrian|Cambrian|Consists of two limestone intervals seperated by mudstone. Overlies Antrim Plateau Volcanics. Max. Thickness: 151m. Geological Province: Wiso Basin. Lateral correlative of Tindall Limestone and Gum Ridge Formation.||||||
12130|Montejinni Limestone|60990|6|Mentioned|p85|Middle Cambrian|Middle Cambrian|Wiso Basin. Faunal links with Antarctica.||||||
12130|Montejinni Limestone|62787|6|Mentioned|p82 Fig. 3|Cambrian|Neoproterozoic|Geological Province: Wiso Basin (NT).||||||07-FEB-11
12130|Montejinni Limestone|62790|5|Briefly described|p207|Middle Cambrian|Middle Cambrian|Eastern Wiso Basin. Contains fossils of Bradoria alaris, and Parahoulongdongella? Sp. (Kruse, 1998, Fig.24), the only Ordian or early Templetonian representative of the Hipponicharionidae in Australia.||||||
12130|Montejinni Limestone|63569|6|Mentioned|p123|Cambrian|Cambrian|Wiso Basin. Contains lingulate brachiopods that correlate with Redlichia guizhouensis Zone of China.||||||
12130|Montejinni Limestone|64068|6|Mentioned|p225|||Wiso Basin. Correlated with Narpa Group.||||||
12130|Montejinni Limestone|64443|6|Mentioned|p40.|||Of Wiso Basin. Correlative of Barkly Group, Georgina Basin.||||||
12130|Montejinni Limestone|64780|5|Briefly described|p62 Fig.3 |Cambrian|Cambrian|||||||
12130|Montejinni Limestone|65239|5|Briefly described|p2-3|Middle Cambrian|Middle Cambrian|Conformably overlain by Point Wakefield beds. Geological province: Wiso Basin. Shallow, epeiric sea deposits.||||||04-JUN-09
12130|Montejinni Limestone|65337|5|Briefly described|p94.|Middle Cambrian|Middle Cambrian|Wiso Basin. Carbonates.||||Unconformably overlies Kalkarindji Volcanic Group.||
12130|Montejinni Limestone|65345|5|Briefly described|pp3-4, p6 Fig.5, p8. |Middle Cambrian|Middle Cambrian|Wiso Basin. Over 150 m thick. Contains a 15 m-thick phosphatic zone which is promising for further exploration. Shallow epeiric sea deposits.||||Is overlain by Hooker Creek Formation.|Limestone, dolostone, dolomitic limestone, calcareous mudstone and siltstone, commonly with abundant chert nodules.|
12130|Montejinni Limestone|67352|6|Mentioned|p19|Middle Cambrian|Middle Cambrian|Wiso Basin. Contains a widespread (NT-SA-Antarctica) fossil fauna.||||||
12130|Montejinni Limestone|69437|5|Briefly described|p22:10-11, 15-16|Series 2|Series 2|Wiso Basin, Centralian B Superbasin. Sequence 1. Shallow-marine and lesser peritidal deposits. Has potential as a petroleum source and reservoir rock.||||Is overlain by Hooker Creek Formation.|Limestone, dolostone and minor siliciclastic rocks.|12-JUL-16
12130|Montejinni Limestone|69438|5|Briefly described|p23:29|Middle Cambrian|Middle Cambrian|Wiso Basin. Correlation based on a distinct positive excursion in stable carbon and oxygen isotopes.||||Time-equivalent to Giles Creek Dolostone (Amadeus Basin).||12-JUL-16
12130|Montejinni Limestone|69439|6|Mentioned|p24:10|||Wiso Basin. The interval Montejinni Limestone-Lothari Hill Sandstone is correlated with the Walbiri Dolostone of the Ngalia Basin.||||||12-JUL-16
12130|Montejinni Limestone|69443|6|Mentioned|p28:21|||Wiso Basin.||||Correlated with Gum Ridge Formation.||12-JUL-16
12130|Montejinni Limestone|69445|5|Briefly described|p30:5, 11, 17|Middle Cambrian|Middle Cambrian|Randal and Brown (1967). Wiso Basin. Associated with the Crowsons Prospect copper occurrence.||||Unconformably overlies Antrim Plateau Volcanics (Kalkarindji Suite).||12-JUL-16
12130|Montejinni Limestone|69446|6|Mentioned|p31:2-3|||Wiso Basin. Probably continuous with Tindall Limestone under cover.||||||12-JUL-16
12130|Montejinni Limestone|69447|4|Described|p32:2-5, 7-9|Middle Cambrian|Middle Cambrian|Traves (1955). Oldest unit in the Wiso Basin. Peritidal to restricted marine deposits. Up to 151m thick. Crops out as a rugged dissected terrace flanking a plateau, and as isolated mesas or sparse low rises or boulder fields. The main producing aquifer in the western Wiso Basin. Fossiliferous: trilobites including Redlichia, bradoriides, brachiopods, hyoliths, molluscs, echinoderm plates, sponge spicules and chancelloriids. Has strong species-level similarity to correlative faunas of Linnekar Limestone and Panton Formation (Ord Basin) and Tindall Limestone (Daly Basin). Associated with the Kunayangku, Lady Judith and Warrego West phosphate prospects. The Crowsons (copper) Prospect occurs at/near the contact with Antrim Plateau Volcanics. Has fair to good petroleum source rock potential; hydrocarbon shows have been recorded. Has good potential as a reservoir.||||Unconformably overlies Antrim Plateau Volcanics. Is overlain conformably and gradationally by Hooker Creek Formation and unconformably by Point Wakefield beds.|Limestone and dolostone (including microbial (dolo)laminite and mottled, bioclast, oncoid and ribbon types), maroon-green siltstone; minor dolomitic quartz sandstone; local basal polymict breccia; nodular evaporites, hot and cold seep structures.|12-JUL-16
12130|Montejinni Limestone|69448|6|Mentioned|p33:3|||Wiso Basin.||||Correlated with Negri Subgroup (Ord Basin) in part.||12-JUL-16
12130|Montejinni Limestone|69458|5|Briefly described|p42:20|Middle Cambrian|Middle Cambrian|Wiso Basin.||||Overlies Antrim Plateau Volcanics. Is overlain unconformably by Camfield beds.||14-SEP-18
12130|Montejinni Limestone|69673|5|Briefly described|ix, p142, p145, p146 fig 117|Cambrian|Cambrian|Minor hydrocarbon shows have been noted in this unit. Up to 151m thick. Contains marine fossils and stromatolites.||||Overlain by the Hooker Creek Formation|Fractured and vuggy limestone, dolostone, siltstone and minor dolomitic quartz sandstone.|
12130|Montejinni Limestone|70380|6|Mentioned|p745|Stage 5|Stage 4|Wiso Basin.||||||
12130|Montejinni Limestone|70752|6|Mentioned|p129|||Wiso Basin. Brachiopod systematic palaeontological descriptions.||||||
12130|Montejinni Limestone|70850|5|Briefly described|Map legend.|Cambrian|Cambrian|Wiso Basin. The two facies are mapped separately.|||||Mudstone and argillaceous limestone, siliceous breccia at base; limestone, dolostone.|
12130|Montejinni Limestone|70854|5|Briefly described|Map legend.|Cambrian|Cambrian|Wiso Basin.|||||Limestone, dolostone, calcareous mudstone and siltstone.|
12130|Montejinni Limestone|70855|5|Briefly described|Map legend.|Cambrian|Cambrian|Wiso Basin.|||||Limestone, dolostone, calcareous mudstone and siltstone. Three facies are mapped separately: limestone, dolostone; mudstone and argillaceous limestone, siliceous breccia at base; calcilutite, calcarenite, dolostone.|
12130|Montejinni Limestone|70968|5|Briefly described|p112|Middle Cambrian|Middle Cambrian|Wiso Basin. Kennewell and Huleatt (1980) assigned the Lake Woods beds (at that stage mapped as Gum Ridge Formation) to this unit; subsequently reassigned to Renner Group by Hussey et al. (2001).||||Unconformably overlies Lake Woods beds.||
12130|Montejinni Limestone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, dolostone|
12130|Montejinni Limestone|71754|14|Not recorded|p199|||SF52-4.||||||
12130|Montejinni Limestone|73083|6|Mentioned|p12, p14, p24-25, p30, p38, p49|Cambrian|Cambrian|Wiso Basin.||||||
12151|Monument Formation|23410|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Flynn Subgroup, Churchills Head Group. Rhyolitic and rhyodacite tephra, tuffaceous sandstone and siltstone; chert; shale: thin to medium bedded; parallel-, or cross-laminated.||||||07-NOV-08
12151|Monument Formation|23733|5|Briefly described|p7 Fig.1|Paleoproterozoic|Paleoproterozoic|See also p32 Fig. 19.||||||07-NOV-08
12151|Monument Formation|23809|5|Briefly described|p29, l27 Fig. 25|Paleoproterozoic|Paleoproterozoic|Of the Flynn Group.  Appears to be intruded by the Tennant Creek Granite.  Age of felsic volcanics: 1853+/-5 Ma U/Pb SHRIMP crystallisation age.  Geological Province: Tennant Inlier.||||||24-FEB-23
12151|Monument Formation|24172|5|Briefly described|p17, p8 Tb.1, p67 Tb.9|Paleoproterozoic|Paleoproterozoic|Of Flynn Subgroup. Conformably overlain by Whippet Sandstone Member. Geological Province: Tennant Creek Inlier. Max. thickness: ~1000m in type area. Correlated with lower part of Wundirgi and Yungkulungu Fms. May be up tp ~3000m thick in the east.||||||07-NOV-08
12151|Monument Formation|32959|6|Mentioned|p21|||||||||
12151|Monument Formation|33307|5|Briefly described|p18|||Mention Fig.8.||||||
12151|Monument Formation|39213|5|Briefly described|p18|||See also Fig.8.||||||
12151|Monument Formation|43223|5|Briefly described|Map Legend||Paleoproterozoic|Of Flynn Subgroup.||||||07-NOV-08
12151|Monument Formation|46992|6|Mentioned|p254|||||||||
12151|Monument Formation|60684|4|Described|p11, p7 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of the Flynn Subgroup (Churchills Head Group). Siltstone, shale, chert and arenite, wacke. Conformably underlies Whippet Sandstone Member (Bernborough Fm); disconformably/unconformably overlies Warramunga Formation. Max. thickness: ~1000m (in type area).||||||07-NOV-08
12151|Monument Formation|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Ooradidgee Group. Rhyolitic and rhyodacitic tephra, tuffaceous sandstone, siltstone.  In the Tennant Creek region.||||||07-NOV-08
12151|Monument Formation|65209|6|Mentioned|p35 Fig.1, p36|Paleoproterozoic|Paleoproterozoic|||Ooradidgee Group||||
12151|Monument Formation|65222|5|Briefly described|p111|||Originally considered to be older than Warramunga Formation. Reassigned to Flynn Subgroup in 1991 (Donnellan).||Of Flynn Subgroup|||Volcaniclastic.|24-JAN-22
12151|Monument Formation|65338|6|Mentioned|p19.|||Undated, but broadly correlated with volcanic rocks of Yungkulungu and Bernborough Formations.||||||
12151|Monument Formation|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Ooradidgee Group.|||Rhyolitic and rhyodacitic tephra, tuffaceous sandstone, siltstone.|
12151|Monument Formation|69187|6|Mentioned|p53 Fig.2, p54 Fig.3|||Warramunga Province.||Ooradidgee Group||||
12151|Monument Formation|69424|3|Fully described|p9:3-5, 15-17, 19-20, 39 Fig.9.24|Paleoproterozoic|Paleoproterozoic|Warramunga Province. Type area is near Flynn's Monument (53K 416700mE 7850700mN). c.1000m thick in type section; may be up to 3000m in the east. Base not exposed. Moderately deep-water depositional environment, shallowing upwards. Subaqueous and subaerial components in the E. Minimum age constrained by overlying Bernborough Formation age of 1845+/-4 Ma.|1853 +/- 5 Ma (Smith, 1999).|Ooradidgee Group.||Is overlain conformably by Whippet Sandstone Member (Bernborough Formation). Correlated with Yungkulungu Formation - volcanic lithofacies.|Very thinly to thinly bedded, laminated or massive siltstone and chert; shale; fine- to medium-grained lithic sandstone and wacke. Thinly to medium bedded tuff, volcanilithic sandstone and siltstone in the east (probably near the top of the unit).|24-FEB-23
12151|Monument Formation|72910|6|Mentioned|p22.|Artinskian|Artinskian|Byro Sub-basin. Abandoned name, now believed to be, in part, equivalent to the Ballythanna Sandstone Member.||||||
12151|Monument Formation|73124|6|Mentioned|p2 Fig.1|||||Ooradidgee Group||Overlain by Bernborough Formation. Equivalent to Wundirgi Formation.||
12151|Monument Formation|73125|5|Briefly described|p2|Palaeoproterozoic|Palaeoproterozoic|Warramunga Province.||Ooradidgee Group.||||
12151|Monument Formation|73427|5|Briefly described|p4, p12-13|Orosirian|Orosirian|Part of the lowermost package of the Ooradidgee Group. Cogenetic with the Tennant Creek Supersuite.|1855-1845 Ma|Ooradidgee Group||||
12151|Monument Formation|73460|6|Mentioned|p2|||Warramunga Province.||Ooradidgee Group||Overlain by Bernborough Formation. Equivalent to Wundirgi Formation.||
12151|Monument Formation|73550|6|Mentioned|p4|Orosirian|Orosirian||ca 1850 Ma|Ooradidgee Group||||
12151|Monument Formation|73590|6|Mentioned|p1-2|Orosirian|Orosirian||ca 1850 Ma|Ooradidgee Group||Overlain by Bernborough Formation. Equivalent to Wundirgi Formation.||
12250|Moonkinu Sandstone|13194|4|Described|p384 Tb. 4-16, p396 fig 4-60|Late Cretaceous|Late Cretaceous|Mis-spelt as Mookinu on p384. Type section: Moonkinu Beach, Bathurst Is. 11o28'S 130o28'E. Reference section: Jacaranda 1 well (817-2848m). Only on East side of Bonaparte Basin and Money Shoals Basin.||||||
12250|Moonkinu Sandstone|23999|5|Briefly described|p8|Cretaceous|Cretaceous|Deltaic sediments. Overlies the Wangarlu Formation. Thickness: 400m.||||||07-FEB-11
12250|Moonkinu Sandstone|24047|5|Briefly described|p13, p63|Cretaceous|Cretaceous|Of the Bathurst Island Group.  Geological Province: Money Shoal Basin.||||||
12250|Moonkinu Sandstone|41532|3|Fully described|p306|||||||||
12250|Moonkinu Sandstone|42442|3|Fully described|p28|Cenomanian|Cenomanian|||||||27-JUL-06
12250|Moonkinu Sandstone|43699|6|Mentioned|Fig.6,p10||Late Cretaceous|||||||
12250|Moonkinu Sandstone|43739|6|Mentioned|Fig.5,p38||Late Cretaceous|||||||
12250|Moonkinu Sandstone|49637|5|Briefly described|Fig.3|Late Cretaceous|Late Cretaceous|Of the Bathurst Island Group. Geological Province: Darwin Shelf.||||||07-FEB-11
12250|Moonkinu Sandstone|69456|3|Fully described|p40:2; 40:3 Fig.40.4; 40:4, 6, 8|Cenomanian|Cenomanian|Mory (1988); formerly the Moonkinu Member of Hughes and Senior (1974), and the Puffin Formation Equivalent of McLennan et al. (1990). SW Money Shoal Basin, E Bonaparte Basin. Type section is the cliffs adjacent to Moonkinu Beach on Bathurst Island, where it is 18m thick. Maximum thickness c.400m in Tinganoo Bay-1. High-energy, shallow-marine environment. Sparsely fossiliferous.||Bathurst Island Group.||Conformably overlies Wangarlu Formation. Lateral equivalent of Wangarlu Formation in the Bonaparte Basin. Is overlain unconformably by Van Diemen Sandstone and Woodbine Group.|Grey to yellow, cross-bedded, fine-grained glauconitic sandstone and quartz sandstone, interbedded with lesser light to dark grey siltstone and mudstone.|12-JUL-16
12250|Moonkinu Sandstone|69673|6|Mentioned|p204|Cretaceous|Cretaceous|||Bathurst Island Group|||Cross bedded, fine grained, glauconitic sandstone and quartz sandstone, interbedded with lesser light to dark grey siltstone and mudstone.|
12250|Moonkinu Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
12250|Moonkinu Sandstone|73083|6|Mentioned|p11, p17, p33|Cretaceous|Cretaceous|Money Shoal Basin.||||||
12299|Mooroongga Formation|23373|4|Described|p318||Early Ordovician|Of the Goulburn Group.  In the Arafura Basin. Truncated by Late Devonian unconformity.||||||07-NOV-06
12299|Mooroongga Formation|23374|5|Briefly described|p23||Early Ordovician|Of the Goulburn Group.  In the Arafura Basin.||||||07-NOV-06
12299|Mooroongga Formation|42058|4|Described|p115|||||||||
12299|Mooroongga Formation|44112|6|Mentioned|p78|||||||||
12299|Mooroongga Formation|62505|4|Described|p3, 4 |Ordovician|Cambrian|Of the Goulburn Group. Overlies: Milingimbie Formation. Thickness: 201m+. Shale, limestone, sandstone.||||||
12299|Mooroongga Formation|62510|5|Briefly described|p3|Orodvician|Orodvician|||||||
12299|Mooroongga Formation|63062|5|Briefly described|p9 Fig. 9, p14|Early Ordovician|Early Ordovician|Of the Goulburn Group. Geological Province: Arafura and Money Shoal Basins. Mixed carbonate and clastic rocks, shaly sediments.||||||07-FEB-11
12299|Mooroongga Formation|69297|5|Briefly described|p283, p285|Lower Ordovician|Lower Ordovician|Arafura Basin. Deposited in a shallow marine shelf environment.||Goulburn Group||Overlies the Milingimbi Formation.|Carbonate and clastic rocks.|
12299|Mooroongga Formation|69437|5|Briefly described|p22:10|Early Ordovician|Early Ordovician|Arafura Basin.||||Overlies Milingimbi Formation.||12-JUL-16
12299|Mooroongga Formation|69451|4|Described|p35:3-4, 6-8; 35:13 Fig.35.9|Ordovician|Ordovician|Bradshaw et al. (1990); Nicoll (2006). Arafura Basin (offshore). Shallow-marine deposits. Up to 201m thick. Diverse fossil assemblage. Early Floian age from limited but diagnostic conodonts; similar age to Florina Formation (Daly Basin).||Goulburn Group.||Overlies Milingimbi Formation probably conformably. Is overlain unconformably by Djabura Formation (Arafura Group).|Shale, limestone, sandstone, glauconitic sandstone; minor chert, dolomitic in part; becomes more calcareous up-section; limited conodont faunas.|12-JUL-16
12299|Mooroongga Formation|69673|6|Mentioned|p197|||||||||
12299|Mooroongga Formation|70098|4|Described|p5, p19 Fig.5|Early Ordovician|Early Ordovician|The Lower Ordovician marine shelf mixed carbonate and clastic rocks of the Milingimbi and Mooroongga formations form the uppermost units of the Goulburn Group.||Goulburn Group||Overlies Milingimbi Formation. Is ?unconformably overlain by Djabura Formation.|Marine shelf mixed carbonate and clastic rocks.|
12299|Mooroongga Formation|73567|6|Mentioned|p68|Ordovician|Ordovician|Arafura Basin.||||||
12305|Mopunga Group|9394|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Includes: Elkera Formation, Grant Bluff Formation, Elyuah Formation. Geological Province: Georgina Basin.||||||
12305|Mopunga Group|9694|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Includes: Elkera Formation, Grant Bluff Formation, Elyuah Formation. Geological Province: Georgina Basin.||||||18-NOV-04
12305|Mopunga Group|12951|5|Briefly described|p143,  fig 4|Neoproterozoic|Neoproterozoic|Georgina Basin.|||Includes Elkera Formation at top.|||
12305|Mopunga Group|22649|6|Mentioned|p 137|||In the Georgina Basin.||||||07-NOV-06
12305|Mopunga Group|33103|6|Mentioned|p23|||||||||
12305|Mopunga Group|33111|5|Briefly described|p39|||Fauna.||||||
12305|Mopunga Group|35005|5|Briefly described|p145|||||||||
12305|Mopunga Group|36473|6|Mentioned|Map legend|Cambrian|Adelaidean|Adelaidean to Cambrian||||||
12305|Mopunga Group|37462|4|Described|Table 4.IX|||||||||
12305|Mopunga Group|37929|5|Briefly described|p526|||||||||
12305|Mopunga Group|38157|6|Mentioned|Table IX|||||||||
12305|Mopunga Group|38445|6|Mentioned|p102|||||||||
12305|Mopunga Group|39210|4|Described|p51|||||||||
12305|Mopunga Group|39445|6|Mentioned|p56|||||||||
12305|Mopunga Group|40538|5|Briefly described|Map legend|Adelaidean|Adelaidean|Geological Province: Georgina Basin.||||||15-NOV-05
12305|Mopunga Group|40906|4|Described|p21|||Mention Fig.9||||||
12305|Mopunga Group|41429|6|Mentioned|p247|||||||||
12305|Mopunga Group|42504|5|Briefly described|p85|||||||||
12305|Mopunga Group|42643|6|Mentioned|p21|||In the Georgina Basin||||||07-NOV-06
12305|Mopunga Group|42956|5|Briefly described|p31 Fig.4|||||||||
12305|Mopunga Group|43595|5|Briefly described|p548,Fig.5-33,549||Adelaidean|||||||
12305|Mopunga Group|44233|14|Not recorded|Fig.1|Early Cambrian|Adelaidean|Adelaidean-Lower Cambrian.||||||
12305|Mopunga Group|44327|14|Not recorded|Tb.I,p.4,7,8,map||Middle Cambrian|(F53-11). Mid.Camb. Consists of Elyuah, Grant Bluff and Mount Baldwin Formations.||||||07-NOV-06
12305|Mopunga Group|44328|14|Not recorded|map legend|Early Cambrian|Neoproterozoic|Lower Cambrian to Upper Proterozoic.||||||
12305|Mopunga Group|45052|4|Described|p68|||Adelaidean.||||||07-NOV-06
12305|Mopunga Group|45102|6|Mentioned|p43|||See also p45,49.||||||07-NOV-06
12305|Mopunga Group|45155|6|Mentioned|Fig.7|||||||||
12305|Mopunga Group|46957|6|Mentioned|p165|||||||||
12305|Mopunga Group|48844|2|Defined|p.1,8,20|Early Cambrian|Neoproterozoic|Pl.8. U.Proterozoic-L.Cam. Disconformably overlies Mount Cornish Formation. (F53-11).||||||07-NOV-06
12305|Mopunga Group|48901|14|Not recorded|Not recorded||Adelaidean|inc. Grant Bluff Formation, Elyuah Formation, Mount Cornish Formation, Field River Beds.||||||07-NOV-06
12305|Mopunga Group|48990|1|Redefined|p17|Adelaidean|Adelaidean|||||||
12305|Mopunga Group|60122|5|Briefly described|p12|Neoproterozoic|Neoproterozoic|Includes the Elyuah Formation, Gnalla-a-Gea Arkose and Grant Bluff Formation. Geological Province: Georgina Basin. See also p5.||||||
12305|Mopunga Group|60551|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Includes: Elkera Formation, Grant Bluff Formation, Elyuah Formation. Geological province: Georgina Basin.||||||17-NOV-04
12305|Mopunga Group|60590|5|Briefly described|Map legend|Cryogenian|Cryogenian|Includes the Elyuah and Grant Bluff Formations and Gnallan-a-Gea Arkose.||||||25-NOV-04
12305|Mopunga Group|61388|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Georgina Basin.||||||
12305|Mopunga Group|61404|5|Briefly described|Map legend|Adelaidean|Adelaidean|Includes: Elyuah Fm., Gnallan-a-Gea Arkose, Grant Bluff Fm., Central Mt. Stuart Fm., Elkera Formation and the Andagera Formation.  Age: Ediacaran.  Geological Province: southern Georgina Basin.||||||11-OCT-05
12305|Mopunga Group|61732|5|Briefly described|p106|||Includes: Elyuah, Grant Bluff, Elkera and Central Mount Stuart Formations.  Geological Province: Georgina Basin.||||||07-FEB-11
12305|Mopunga Group|62642|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Georgina/Ngalia Basin.||||||
12305|Mopunga Group|62789|6|Mentioned|p129|Neoproterozoic|Neoproterozoic|In southern Georgina Basin.||||Underlies the Mount Baldwin Formation.||28-MAR-12
12305|Mopunga Group|62790|5|Briefly described|p210|Neoproterozoic|Neoproterozoic|Southern Georgina Basin.||||Underlies the Neoproterozoic-Lower Cambrian Mount Baldwin Formation.||04-DEC-12
12305|Mopunga Group|62984|5|Briefly described|p13|Neoproterozoic III|Neoproterozoic III|Ediacaran package. Geological Province: Georgina Basin.||||||23-JAN-07
12305|Mopunga Group|63562|6|Mentioned|p344|Ediacaran|Ediacaran||||Includes Grant Bluff Formation.|||
12305|Mopunga Group|64068|3|Fully described|p224 App 1, pp49-54, p35, 55, p7|Ediacaran|Ediacaran|Intended as redefinition. Adds Andagera Formation to this Group. Redefined (Walter, 1980) to exclude the Mount Baldwin Formation.|||Includes Gnallan-a-Gea Arkose; Elyuah, Elkera, Central Mount Stuart, Andagera, and Grant Bluff Formations.|Overlies Keepera Group units disconformably. Is disconformably overlain by Shadow Group units or Thorntonia Limestone.|Siliciclastic sediments.|04-APR-12
12305|Mopunga Group|64778|6|Mentioned|p13|Neoproterozoic|Neoproterozoic|Southern Georgina Basin.||||||
12305|Mopunga Group|64812|5|Briefly described|p237 Fig. 2|Neoproterozoic|Neoproterozoic|Geological Province: southern Georgina Basin.||||||07-FEB-11
12305|Mopunga Group|64813|5|Briefly described|p256 Fig. 3|Neoproeterozoic|Neoproterozoic|Geological Province: southern Georgina Basin.||||||11-FEB-09
12305|Mopunga Group|65237|5|Briefly described|p5|Late Neoproterozoic|Late Neoproterozoic|Comprises Elyuah, Grant Bluff and Elkera Formations. Max. thickness: 800m. Geological province: southern Georgina Basin. Synorogenic sediments.||||||07-FEB-11
12305|Mopunga Group|65333|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Wiso Basin. Includes Central Mount Stuart Formation. Arkose, subarkose, quartz arenite and siltstone.||||||
12305|Mopunga Group|65334|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Wiso Basin. Subsurface only. Includes Central Mount Stuart Formation||||||
12305|Mopunga Group|65338|6|Mentioned|pp63-67.|Ediacaran|Ediacaran||||Includes Elyuah, Grant Bluff, Elkera, Central Mount Stuart and Andagera Formations and Gnallan-a-gea Arkose.|Overlies Wonnadinna Dolostone.||
12305|Mopunga Group|65341|6|Mentioned|p2 Fig.2, p5. |Ediacaran|Ediacaran|An unconformity-bound package.|||Includes Gnallan-a-Gea Arkose, Andagera, Central Mount Stuart, Grant Bluff, Elyuah and Elkera Formations.|||
12305|Mopunga Group|66767|5|Briefly described|p58|Ediacaran|Ediacaran|Georgina Basin.|||||Largely siliciclastic post-glacial sedimentary rocks.|
12305|Mopunga Group|67148|5|Briefly described|Map legend.|Ediacaran|Ediacaran||||Includes Andagera Formation.|||
12305|Mopunga Group|67164|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Georgina/Ngalia Basins.|||Includes Elyuah, Grant Bluff and Central Mount Stuart Formations.|||
12305|Mopunga Group|67352|4|Described|v, p17-18, p44 fig 48|Ediacaran|Ediacaran||||Andagera Formation|||
12305|Mopunga Group|67870|6|Mentioned|p43|Neoproterozoic|Neoproterozoic|Georgina Basin.||||||
12305|Mopunga Group|67892|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic||||Includes Elyuah, Grant Bluff and Central Mount Stuart Formations.|||
12305|Mopunga Group|68270|5|Briefly described|p680-681,683|Ediacaran|Ediacaran|Southern Georgina Basin.||||Underlain disconformably by Boko Formation.||
12305|Mopunga Group|69437|5|Briefly described|p22:7|||Southern Georgina Basin. Centralian A Superbasin. Supersequence 3.|||Elkera, Elyuah, Grant Bluff Formations; Gnallan-a-Gea Arkose.|||12-JUL-16
12305|Mopunga Group|69443|4|Described|p28:2-3, 7, 10-12, 14, 31|Ediacaran|Ediacaran|Noakes (1956); redefined by Kruse in Dunster et al. (2007). Southern Georgina Basin. Postglacial sediments deposited following the Toomba Movement. Correlated with the Amadeus Basin succession of Gaylad Sandstone-Pertatataka Formation-Julie Formation-uppermost Inindia beds-upper Boord Formation-lower Arumbera Sandstone; also with the Mount Doreen Formation and lower Yuendumu Sandstone of the Ngalia Basin.|||Elyuah, Grant Bluff, Elkera, Andagera, Central Mount Stuart Formations; Gnallan-a-gea Arkose.|Is overlain unconformably or disconformably by Shadow Group.||12-JUL-16
12305|Mopunga Group|69673|6|Mentioned|p111, p115|Neoproterozoic|Neoproterozoic||||Includes Gnallan-a-gea Arkose, Elyuah Formation, Grant Bluff Formation, Elkera Formation, Central Mt Stuart Formation, Andagera Formation|||
12305|Mopunga Group|70951|6|Mentioned|p1080|Proterozoic|Proterozoic|Part of basement geology to the Georgina Basin. Low reflectance measured.||||||
12305|Mopunga Group|72515|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Jervois Range Special Map Sheet. Georgina Basin.|||Includes the Elkera Formation, Grant Bluff Formation and the Elyuah Formation.|Unconformably overlain by the Shadow Group. Disconformably overlies the Keepera Group.||
12305|Mopunga Group|72516|5|Briefly described|p12-13, p21, p85, p88-90|Ediacaran|Ediacaran|Georgina Basin. Locally intruded by quartz veins. See also p96, p135, p158, p171, p176.|||Includes the Elkera Formation, Grant Bluff Formation and Elyuah Formation,|Disconformably overlies the Keepera Group.||21-APR-22
12305|Mopunga 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.||||||
12356|Morphett Creek Formation|23410|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Tomkinson Creek Subgroup, Churchills Head Group. Sublithic and lithic arenite; feldspathic litharenite; siltstone; dolostone and sandy dolostone. Arenite. Dolostone and siltstone, including cryptomicrobial dolostone.||||||07-NOV-08
12356|Morphett Creek Formation|23733|3|Fully described|p12|Paleoproterozoic|Paleoproterozoic|Of Tomkinson Creek Group. Conformably overlain by Short Range Sandstone and conformably overlies Hayward Creek Formation.  Max. thickness: ~1500m. See also p32 Fig. 19.||||||07-NOV-08
12356|Morphett Creek Formation|23809|5|Briefly described|p27 Fig. 25|||Of the Tomkinson Creek Group.  Geological Province: Tennant Inlier.||||||
12356|Morphett Creek Formation|24047|5|Briefly described|p7 Fig. 6, p9|Paleoproterozoic|Paleoproterozoic|Age: ~1780Ma.  Geological Province: Ashburton Province (Tennant Inlier).  See also p57 Fig. 49.||||||07-NOV-08
12356|Morphett Creek Formation|24172|3|Fully described|p29, p6 Tb,1, p65 Tb.9|Paleoproterozoic|Paleoproterozoic|Of the Tomkinson Creek Subgroup. Conformably overlain by Short Range Sandstone; conformably underlain by Hayward Creek Formation. Geological Province: Tennant Creek Inlier. Max. Thickness: 2500m.||||||07-NOV-08
12356|Morphett Creek Formation|24303|3|Fully described|p4 Tb.1, p6|Proterozoic|Proterozoic|Of the Tomkinson Creek Group. Overlain by the Short Range Sandstone and unconformably overlain by the Gleeson Formation. Disconformably overlies the Whittington Range Member. Max. Thickness: 3200m.||||||
12356|Morphett Creek Formation|24304|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Tomkinson Creek Group. Includes the Kuerschner and Mitty Members as well as undifferentiated rock. Comprises Kuerschner and Mitty Members and undifferentiated sandstone, pebbly sandstone, siliciclastic mudstone, silicified stromatolitic dolostone.||||||07-NOV-08
12356|Morphett Creek Formation|24442|5|Briefly described|p14|||Of the Tomkinson Creek Group.  Geological Province: Ashburton Province.||||||
12356|Morphett Creek Formation|32174|6|Mentioned|Map legend|Carpentarian|Paleoproterozoic|Early Proterozoic or Carpentarian||||||07-NOV-08
12356|Morphett Creek Formation|33307|6|Mentioned|Fig.8|||||||||
12356|Morphett Creek Formation|35125|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
12356|Morphett Creek Formation|35229|4|Described|Table.1|||||||||
12356|Morphett Creek Formation|35771|2|Defined|p24|early Carpentarian|early Carpentarian|Appendix.||||||
12356|Morphett Creek Formation|39213|6|Mentioned|Fig.8|||||||||
12356|Morphett Creek Formation|39624|6|Mentioned|Fig.3|||||||||
12356|Morphett Creek Formation|43223|5|Briefly described|Map Legend||Paleoproterozoic|Of Tomkinson Creek Subgroup.||||||07-NOV-08
12356|Morphett Creek Formation|43224|5|Briefly described|Map legend||Proterozoic|Of Tomkinson Creek Subgroup.||||||07-NOV-06
12356|Morphett Creek Formation|50353|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Tomkinson Creek Group.Unconformably overlies Hayward Creek Formation. Overlain by Short Range Sandstone.||||||07-NOV-08
12356|Morphett Creek Formation|60684|5|Briefly described|p5 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Tomkinson Cr. Subgp (Churchills Head Gp). Conglom., sublithic/ lithic and feldspathic arenite, siltstone, cryptomicrobial boundstone and quartz carbonate. Conformably unerlies Short Range Fm; conformably overlies Hayward Cr.Fm. Max. thick:~2500m.||||||07-NOV-08
12356|Morphett Creek Formation|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Tomkinson Creek Group. Sublithic/lithic arenite, feldspathic arenite, siltstone; dolostone, sandy dolostone; minor conglomerate. In the Tennant Creek region.||||||07-NOV-08
12356|Morphett Creek Formation|64780|5|Briefly described|p63 Fig.4 |Palaeoproterozoic|Palaeoproterozoic|||Of the Tomkinson Creek Group||||
12356|Morphett Creek Formation|64817|6|Mentioned|p367|||Tomkinson Creek Province.||||||
12356|Morphett Creek Formation|65209|5|Briefly described|p35 Fig.1, p37|Paleoproterozoic|Paleoproterozoic|||Tomkinson Creek Group|Deagan Member|lowermost sandstone interval of Morphett Creek Formation (Tomkinson Creek Group) correlates with Errolola Sandstone (Hatches Creek Group).||
12356|Morphett Creek Formation|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Tomkinson Creek Group.||Is overlain by Short Range Sandstone.|Sublithic/lithic arenite, feldspathic arenite, siltstone; dolostone, sandy dolostone; minor conglomerate.|
12356|Morphett Creek Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Tennant Creek/Davenport area.||Tomkinson Creek Group.||||
12356|Morphett Creek Formation|69424|6|Mentioned|p9:39 Fig.9.24|Paleoproterozoic|Paleoproterozoic|Tennant Creek area.||Tomkinson Creek Group.||||12-JUL-16
12356|Morphett Creek Formation|69425|5|Briefly described|p10:12|||Tomkinson Province.|||Kuerschner Member.|||12-JUL-16
12356|Morphett Creek Formation|69431|4|Described|p16:1, 3-6, 8-9, 13, 22-23|Paleoproterozoic|Paleoproterozoic|Tomkinson Province. c.3000-3200m thick. Fluvial to shallow-marine deposits: continental red beds, and marginal shallow-marine, including peritidal flats and sabkha deposits; some shallow-marine channels. Folding during the Davenport Event is discussed.||Tomkinson Creek Group.|Kuerschner, Mitty Members.|Disconformably overlies Whittington Range Member (Hayward Creek Formation). Is overlain by Short Range Sandstone conformably, and by Gleeson Formation unconformably.|Sandstone and pebbly sandstone; siltstone; thin to medium beds of intraformational conglomeratic sandstone; chertified laminated dolostone; stromatolites; pebble to cobble conglomerate; evaporite pseudomorphs; enterolitihc and nodular chert.|12-JUL-16
12356|Morphett Creek Formation|69673|6|Mentioned|p58|||||Tomkinson Creek Group||||
12476|Mount Baldwin Formation|9694|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Underlies Errarra Formation, Arthur Creek Formation; overlies Elkera Formation. Geological Province: Georgina Basin. Sandstone; rare siltstone.||||||07-NOV-06
12476|Mount Baldwin Formation|12891|5|Briefly described|p733 Fig. 2|Early Cambrian|Early Cambrian|Geological province: SW Georgina Basin. Written as Mt Baldwin Fm in text of figure.||||||07-FEB-11
12476|Mount Baldwin Formation|12951|5|Briefly described|p143, 145, 149, 155|Early Cambrian|Early Cambrian|Georgina Basin. Alluvial fan/ fan-delta setting.||||Laterally equivalent to Adam Shale. Unconformably overlies Elkera Formation.|Siliciclastic rocks.|
12476|Mount Baldwin Formation|22646|6|Mentioned|p 102|Early Cambrian||Situated in the Georgina Basin.  Mount is Mt in text.||||||07-NOV-06
12476|Mount Baldwin Formation|22954|6|Mentioned|Fig3p9|Early Cambrian||||||||
12476|Mount Baldwin Formation|24581|6|Mentioned|p817|Cambrian|Cambrian|Mount is Mt. in text. Geological Province: Georgina Basin.||||||
12476|Mount Baldwin Formation|33103|6|Mentioned|p23|||||||||
12476|Mount Baldwin Formation|33111|6|Mentioned|p38|||p39.||||||07-NOV-06
12476|Mount Baldwin Formation|33681|6|Mentioned|p137|||||||||
12476|Mount Baldwin Formation|35005|5|Briefly described|p145|||||||||
12476|Mount Baldwin Formation|35221|6|Mentioned|p14|||||||||
12476|Mount Baldwin Formation|35798|6|Mentioned|p307|||Early Cambrian. Correlative of Adam Shale and lower Red Heart Dolomite.||||||07-NOV-06
12476|Mount Baldwin Formation|37572|5|Briefly described|p154|||See also p156,165 and Fig.8.||||||07-NOV-06
12476|Mount Baldwin Formation|38157|6|Mentioned|Table IX|||||||||
12476|Mount Baldwin Formation|38445|6|Mentioned|p102|||||||||
12476|Mount Baldwin Formation|39210|4|Described|p51|||Age p53.||||||07-NOV-06
12476|Mount Baldwin Formation|40538|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Quartz arenite, medium to coarse grained, thin to thick bedded, dusky red. Geological Province: Georgina Basin.||||||15-NOV-05
12476|Mount Baldwin Formation|40642|6|Mentioned|p163|||||||||
12476|Mount Baldwin Formation|40810|5|Briefly described|p13|||||||||
12476|Mount Baldwin Formation|40906|4|Described|p21|||||||||
12476|Mount Baldwin Formation|41457|6|Mentioned|p24|||||||||
12476|Mount Baldwin Formation|41524|6|Mentioned|Fig.3|||||||||
12476|Mount Baldwin Formation|41801|6|Mentioned|p214|||||||||
12476|Mount Baldwin Formation|42059|6|Mentioned|Fig.2 P131|||||||||
12476|Mount Baldwin Formation|42504|5|Briefly described|p85|||||||||
12476|Mount Baldwin Formation|42643|6|Mentioned|p21|||In the HUCKITTA sheet area.||||||07-NOV-06
12476|Mount Baldwin Formation|42956|4|Described|p30|||see also Fig.4 p31.||||||07-NOV-06
12476|Mount Baldwin Formation|44320|14|Not recorded|p.7|||||||||
12476|Mount Baldwin Formation|44327|2|Defined|Tb.I,p.8-10,18,map||Middle Cambrian|(F53-11). Mid Camb.top fm. Of the Mopunga Group.||||||07-NOV-06
12476|Mount Baldwin Formation|44328|14|Not recorded|map legend|Early Cambrian|Neoproterozoic|Lower Cambrian to Upper Proterozoic.||||||
12476|Mount Baldwin Formation|44358|5|Briefly described|p8||Early Cambrian|In HUCKITTA sheet area.||||||07-NOV-06
12476|Mount Baldwin Formation|45052|2|Defined|p68|Adelaidean|Adelaidean|||||||
12476|Mount Baldwin Formation|45102|6|Mentioned|p4|||See also p45.||||||07-NOV-06
12476|Mount Baldwin Formation|45148|6|Mentioned|Fig.4|||In the Georgina Basin.||||||07-NOV-06
12476|Mount Baldwin Formation|45155|6|Mentioned|Fig.8|||||||||
12476|Mount Baldwin Formation|46957|4|Described|p166|||||||||
12476|Mount Baldwin Formation|47035|6|Mentioned|p85|||||||||
12476|Mount Baldwin Formation|48844|2|Defined|p.26-37||Early Cambrian|On many pages. p.1,16-7,20,26-37,39,41,43, F.26,58-9,65,67, Pl.8.(new name).Overlies Grant Bluff Formation. L.Cam.(F53-11). See also Fig.10, p26.||||||19-MAY-17
12476|Mount Baldwin Formation|48901|14|Not recorded|Not recorded||Early Cambrian|L.Cambrian.||||||
12476|Mount Baldwin Formation|48990|1|Redefined|p13|Adelaidean|Adelaidean|See also p11.||||||07-NOV-06
12476|Mount Baldwin Formation|49027|6|Mentioned|p7|||||||||
12476|Mount Baldwin Formation|60122|6|Mentioned|p9 P11 Tb. 1|||Within Supersequence 4. Disconformably overlain by Red Heart Dolostone. Geological Province: Georgina Basin. See also p44.||||||
12476|Mount Baldwin Formation|60551|5|Briefly described|Map Legend|Cambrian|Cambrian|Underlies Errarra Formation, Arthur Creek Formation; overlies Elkera Formation. Geological province: Georgina Basin. Thin to thick bedded, cross bedded sandstone, rare siltstone.||||||30-SEP-08
12476|Mount Baldwin Formation|61022|5|Briefly described|p15 Fig. 2|Early Cambrian|Early 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. Mount is MT in text.||||||20-APR-05
12476|Mount Baldwin Formation|61404|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Of the Shadow Group. Quartz arenite: medium to coarse.  Geological Province: southern Georgina Basin.||||||
12476|Mount Baldwin Formation|61732|6|Mentioned|p109, p113|||Overlies Elkera Formation. Formerly included a stromatolite section now in the upper part of the Elkera Formation.||||||07-FEB-11
12476|Mount Baldwin Formation|62376|5|Briefly described|p53|Early Cambrian|Neoproterozoic|Geological Province: Georgina Basin||||||09-FEB-10
12476|Mount Baldwin Formation|62595|6|Mentioned|p28 Fig.4.|Early Cambrian|Early Cambrian|Georgina Basin. Relative probability plots of detrital zircon data are shown.||||||
12476|Mount Baldwin Formation|62789|5|Briefly described|p128, p129 Fig. 2|Early Cambrian|Neoproterozoic|In southern Georgina Basin. 63 m thick at Pacific Oil & Gas Baldwin No. 1 exploration well.||||Underlies Lower Cambrian Red Heart Dolostone and overlies Mopunga Group.|Thickly bedded sandstone, lesser siltstone.|28-MAR-12
12476|Mount Baldwin Formation|62790|5|Briefly described|p208, 210|Early Cambrian|Neoproterozoic|Southern Georgina Basin. 63 m thick in Pacific Oil & Gas Baldwin No. 1 well.||||Overlies Mopunga Group and underlies Errarra Formation.|Thickly bedded sandstone, lesser siltstone.|28-MAR-12
12476|Mount Baldwin Formation|62984|5|Briefly described|p14|||Appears to conformably overlie the Elkera Formation. Geological Province: Georgina Basin.||||||23-JAN-07
12476|Mount Baldwin Formation|63562|4|Described|p338 fig 3, p345-8, p351, p352 fig 10|Early Cambrian|Early Cambrian|Of Georgina Basin. Zircons have several age clusters; possible source areas discussed.||||Correlated with Arumbera Sandstone.|Well-sorted, medium- to fine-grained quartz sandstone; contains earliest Cambrian trace fossils.|
12476|Mount Baldwin Formation|64068|3|Fully described|p55, p51, 54, p19, p ix|Early Cambrian|Early Cambrian|Potential hydrocarbon reservoir. Redefined (Walter 1980), to exclude upper dolostone now part of Red Heart Dolostone. Also removed from Mopunga Group in 1980. Correlations: Octy Formation, Neutral Junction Formation, Adam Shale, possibly Sylvester Sandstone.||Of Shadow Group.||Unconformably overlies Elkera Formation. Is unconformably overlain by Red Heart Dolostone.|Red to red-brown quartz arenite and sublitharenite, quartz greywacke, siltstone, shale; minor subarkose.|04-APR-12
12476|Mount Baldwin Formation|64778|6|Mentioned|p13|Cambrian|Cambrian|Dulcie Syncline, Southern Georgina Basin.||||||
12476|Mount Baldwin Formation|64812|5|Briefly described|p237 Fig. 2|Early Cambrian|Early Cambrian|Geological Province: southern Georgina Basin.||||||07-FEB-11
12476|Mount Baldwin Formation|64813|5|Briefly described|p256 Fig. 3|Early Cambrian|Early Cambrian|Unconformably overlies Elkera Formation; overlain by Red Heart Dolostone. Geological Province: southern Georgina Basin. Siliciclastic rocks.||||||11-FEB-09
12476|Mount Baldwin Formation|65237|5|Briefly described|p3 Fig. 4, p5|Early Cambrian|Early Cambrian|Unconformably on Elkera Fm in the south. Max.thickness: ~300m. Geol.prov: southern Georgina Basin. Full spectrum of alluvial fan-delta facies varying from proximal conglomeratic facies to distal siltstone/mudstone successions. Mount is Mt in places.||||||07-FEB-11
12476|Mount Baldwin Formation|65341|5|Briefly described|p14, p16. |||Previously (Smith 1964) included in Mopunga Group; later removed (Walter 1980) because of a local basal unconformity and Cambrian trace fossils. More recent field comparisons suggest that some outcrops mapped as Mount Baldwin Formation are likely laterally equivalent to parts of Central Mount Stuart Formation and Octy Formation and thus should be included in Mopunga Group.||||Overlies Elkera Formation.||
12476|Mount Baldwin Formation|66767|5|Briefly described|p59|Early Cambrian|Early Cambrian|Southern Georgina Basin.||||Is overlain by Red Heart Dolostone.|Fan-delta to marine sandstones.|
12476|Mount Baldwin Formation|69437|5|Briefly described|p22:10|Cambrian|Cambrian|Southern Georgina Basin.||||Is overlain by Red Heart Dolostone.||12-JUL-16
12476|Mount Baldwin Formation|69443|4|Described|p28:7, 11, 14-15, 45-46|Early Cambrian|Early Cambrian|K.G. Smith (1964), redefined by Walter (1980). Southern Georgina Basin. 60-320m thick. Basal beds are recessive; the rest of the Formation is ridge-forming. Has been modelled for unconformity-related uranium mineralisation.||Shadow Group.||Disconformably or unconformably overlies Elkera Formation. Is overlain unconformably by Red Heart Dolostone. Correlated with Octy and Neutral Junction Formations, Adam Shale and ?Sylvester Sandstone.|Quartz sandstone, sublithic sandstone, quartz greywacke, siltstone, shale and minor subarkose. Rare granule-bearing beds and pebble-sized claystone intraclasts; prominent cross-beds throughout; various ichnofossils.|12-JUL-16
12476|Mount Baldwin Formation|69561|6|Mentioned|p33 fig 2|Cambrian|Cambrian|||||Overlain by Red Heart Dolostone||
12476|Mount Baldwin Formation|69673|5|Briefly described|p116, p119 fig 94, p129, p136, p138|||||Shadow Group||Unconformably overlies Elkera Formation, unconformably overlain by Red Heart Dolostone, correlated with Octy Formation, Neutral Junction Formation|Quartz sandstone, sublithic sandstone, glauconitic and feldspathic sandstones, quartz greywacke, siltstone, shale and minor subarkose.|
12476|Mount Baldwin Formation|69917|6|Mentioned|p115|||Georgina Basin. Walter et al (1995) assigned this unit to Supersequence 4 of their Centralian Superbasin.||||||
12476|Mount Baldwin Formation|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.||||||
12476|Mount Baldwin Formation|70749|6|Mentioned|p52-53|||Georgina Basin. Detrital zircons indicate a range of ages and more complex source(s).||||||
12476|Mount Baldwin 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. 1.17 Ga; Maidment et al., 2007).||||||
12476|Mount Baldwin Formation|70951|6|Mentioned|p1077, 1082|||||||||
12476|Mount Baldwin Formation|71800|5|Briefly described|p26-p27|Early Cambrian|Early Cambrian|Georgina Basin.|||||Quartz sandstone.|
12476|Mount Baldwin Formation|72515|5|Briefly described|Map Legend|Cambrian|Cambrian|Jervois Range Special Map Sheet. Georgina Basin. Contains Ichnofossils.||Shadow Group||Unconformably overlain by the Red Heart Dolostone.|Quartz arenite, sublitharenite; medium-thick-bedded, cross bedded; minor quartzwacke, siltstone, shale, granule-bearing greywacke, sandstone and coarse grained subarkose.|
12476|Mount Baldwin Formation|72516|3|Fully described|p12-13, p15, p61, p89-90, p95-96|Terreneuvian|Terreneuvian|Georgina Basin. Type section is defined in the Elua Range in JINKA. Exposed northeast of the Lucy Creek Fault Zone, Elua Range in the Jervois and Johansen Ranges and is structurally emplaced in the Charlotte Fault Zone. The basal beds are recessive whereas the rest of it is ridge-forming. Contains ichnofossils. 100-320m thick in Jervois Range, 230m thick in Johannsen Range. Deposited in an alluvial fan delta. Interpreted to correlate with the Octy Formation, Junction Formation, Adam Shale and Sylvester Sandstone. Age correlative of Crossing Bore Schist, Atula calc-silicate, Arumbera Sandstone. Intruded by quartz-vein breccias in the Charlotte and Bonya fault zones. See also p99, p154-155, p173, p176, p186.|ca 670 Ma (max dep age)|Shadow Group||Overlies the Elkera Formation with angular unconformity and the Thring Granite. Unconformably overlain by the Red Heart Dolostone.|Quartz arenite, sublitharenite; medium-thick bedded, cross bedded. Minor quartzwacke, siltstone, shale, granule-bearing greywacke, sandstones with pebble-sized claystone intraclasts, coarse grained subarkose.|02-JUN-21
12501|Mount Basedow Gneiss|9534|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Kakadu Group.  Gneissic meta-arkose, quartzite, interbanded biotite gneiss and schist.  Transitional into the Nanambu Complex.||||||07-NOV-08
12501|Mount Basedow Gneiss|9691|5|Briefly described|Map Legend|||Of the Kakadu Group. Gneissic meta-arkose, quartzite.||||||
12501|Mount Basedow Gneiss|9701|5|Briefly described|Map Legend|Proterozoic|Archean|Of the Kakadu Group. Gneissic meta-arkose, quartzite.||||||07-NOV-08
12501|Mount Basedow Gneiss|9733|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Gneissic meta-arkose, quartzite, interbedded biotite gneiss and schist; transitional into Nanambu Complex.||||||
12501|Mount Basedow Gneiss|22810|5|Briefly described|Table2 P5|||Maximum thickness: 1500m.||||||07-NOV-06
12501|Mount Basedow Gneiss|35140|6|Mentioned|Fig.2|||||||||
12501|Mount Basedow Gneiss|35465|6|Mentioned|Fig.2|||Summary of positions of magnetic units in the Lower Proterozoic.||||||07-JAN-09
12501|Mount Basedow Gneiss|36535|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
12501|Mount Basedow Gneiss|36635|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
12501|Mount Basedow Gneiss|37462|6|Mentioned|Fig.4.8|||||||||
12501|Mount Basedow Gneiss|37815|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
12501|Mount Basedow Gneiss|38239|6|Mentioned|Fig.2|||||||||
12501|Mount Basedow Gneiss|38349|4|Described|p10|||||||||
12501|Mount Basedow Gneiss|38351|6|Mentioned|p5|||||||||
12501|Mount Basedow Gneiss|38884|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
12501|Mount Basedow Gneiss|39069|5|Briefly described|Table 1|||||||||
12501|Mount Basedow Gneiss|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
12501|Mount Basedow Gneiss|40493|5|Briefly described|Table 1|||||||||
12501|Mount Basedow Gneiss|40808|5|Briefly described|Table 2|||||||||
12501|Mount Basedow Gneiss|41146|5|Briefly described|Fig.2|||||||||
12501|Mount Basedow Gneiss|43187|5|Briefly described|p2|||||||||
12501|Mount Basedow Gneiss|46639|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Kakadu Group. Gneissic meta-arkose, quartzite, interbanded biotite gneiss and schist, transitional into the Nanambu Complex.||||||07-NOV-08
12501|Mount Basedow Gneiss|46700|5|Briefly described|P7, Table1 P12||Proterozoic|Equivalent to Mount Howship Gneiss.||||||07-NOV-06
12501|Mount Basedow Gneiss|60550|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of th Kakadu Group. Gneissic meta-arkose, quartzite, interbedded biotite gniess and schist; transitional into Nanambu Complex.||||||
12501|Mount Basedow Gneiss|60680|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Kakadu Group.  Well foliated and banded, fine to coarse gneissic meta-arkose, micaceous quartzite and feldspathic quartzite; cross-bedding is preserved in places; interbanded biotite-rich gneiss and schist.Geological Province: Pine Creek Orogen.||||||07-NOV-08
12501|Mount Basedow Gneiss|64698|4|Described|lithinterp table|Orosirian|Paleoproterozoic|Age ~2025-2500Ma. Of Kakadu Group. Max thick 500m. Foliated and banded, fine/coarse gneissic meta-arkose, micaceous qtzite and feldspathic qtzite; some cross-bedding preserved; interbanded biotite-rich gneiss and schist.||||||
12501|Mount Basedow Gneiss|64956|4|Described|p2 Tb. 22, p88-89|Paleoproterozoic|Paleoproterozoic|Basal unit of Kakadu Group; equiv. to Mount Howship Gneiss. Borders the Nanambu Complex. Max. depositional age: 2284+/-18ma. Geological province: Pine Creek Orogen. Sample is muscovite-bearing feldspathic quartzite.||||||07-FEB-11
12501|Mount Basedow Gneiss|65232|6|Mentioned|p22 Fig. 12|||Of Kakadu Group.||||||09-FEB-10
12501|Mount Basedow Gneiss|66683|6|Mentioned|p368.|Paleoproterozoic|Paleoproterozoic|||Unit in Kakadu Group.||||
12501|Mount Basedow Gneiss|67564|4|Described|p8, p11, p28, p62.|Paleoproterozoic|Paleoproterozoic|Formerly Mount Partridge Formation (Walpole 1963), now defunct. Mainly braided fluviatile depositional environment; crossbedding is locally preserved. Near Mount Basedow, meta-arkose of the Mount Basedow Gneiss grades into a leucogneiss of the Nanambu Complex, suggesting some of the latter's units are metamorphic products of sedimentary rocks. Has high Th and K radiometric counts.|Depositional age of ?2200 Ma.|Unit in Kakadu Group.|||Fine to coarse gneissic meta-arkose; micaceous or feldspathic quartzite; quartzite with interbanded biotite-rich gneiss and schist.|
12501|Mount Basedow Gneiss|67779|5|Briefly described|p6 Fig.5, p16.|Paleoproterozoic|Paleoproterozoic|Nimbuwah Domain, Pine Creek Orogen. Detrital zircons indicate the sediments were derived from underlying 2520 Ma Nanambu Complex. Possibly correlated with Kudjumarndi Quartzite.||Unit in Kakadu Group.||Is overlain by Munmarlary Quartzite.||
12501|Mount Basedow Gneiss|69420|5|Briefly described|p5:4, 6-7, 24, 67|Paleoproterozoic|Paleoproterozoic|Nimbuwah Domain, Pine Creek Orogen. Over 1500m thick. Fluvial to shallow-marine deposits. Detrital zircon age peaks at 2518 Ma.||Kakadu Group.|||Pink-grey, muscovite-biotite gneiss, granitoid gneiss, meta-arkose, meta-conglomerate (these last two are radioactive), quartzite; minor schist. Strongly foliated parallel to compositional layering. Cross-bedding preserved locally.|12-JUL-16
12501|Mount Basedow Gneiss|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|2518+/-3 Ma (MDA: U-Pb zircon SHRIMP)||||Muscovite-bearing feldspathic quartzite.|
12510|Mount Birch Sandstone|22853|5|Briefly described|24|||Overlain by Balbirini Dolomite.||||||10-SEP-19
12510|Mount Birch Sandstone|23937|2|Defined|p87 App. 1|Calymmian|Statherian|Of Nathan Group.  Conformably overlain by Knuckey Fm; unconformably overlies Nagi Fm, and nonconformably over Urapunga Granite.  Max. thickness: 100m.  Geol.Prov: McArthur Basin.||||||07-NOV-06
12510|Mount Birch Sandstone|24047|5|Briefly described|p12 Fig. 10, p40|Mesoproterozoic|Mesoproterozoic|Of the Nathan Group.  Overlies the McArthur Group as the basal unit of Nathan Group.  Also unconformably overlies the Mount Reid Volcanics.  Geological Province: McArthur Basin.||||||
12510|Mount Birch Sandstone|32658|3|Fully described|Table 2|||See also Fig. 3.||||||07-NOV-06
12510|Mount Birch Sandstone|32660|5|Briefly described|Table 4|||||||||
12510|Mount Birch Sandstone|37568|5|Briefly described|p79|||||||||
12510|Mount Birch Sandstone|40259|6|Mentioned|Table 1|||||||||
12510|Mount Birch Sandstone|41220|6|Mentioned|Fig.3|||||||||
12510|Mount Birch Sandstone|42639|6|Mentioned|p35|||Superseded by Smythe Sandstone.||||||
12510|Mount Birch Sandstone|44332|14|Not recorded|p.7,opp.6,map|||(D53-14).||||||
12510|Mount Birch Sandstone|44333|14|Not recorded|map legend|||Lower(?) Proterozoic.||||||
12510|Mount Birch Sandstone|44471|14|Not recorded|p.8, opp.p.7, map|||(D53-10). Formation of McArthur Group.||||||
12510|Mount Birch Sandstone|44472|5|Briefly described|map legend|||Of the McArthur Group.  White and brown feldspathic sandstone, calcareous near base.  Lower (?) Proterozoic.||||||02-DEC-04
12510|Mount Birch Sandstone|44530|14|Not recorded|p.9, opp.10|||(D53-15).||||||
12510|Mount Birch Sandstone|44531|14|Not recorded|map legend|||Lower (?) Proterozoic.||||||
12510|Mount Birch Sandstone|45162|6|Mentioned|p45|||||||||
12510|Mount Birch Sandstone|46968|6|Mentioned|p302|||||||||
12510|Mount Birch Sandstone|60483|5|Briefly described|p7 Fig. 5|||Of the Nathan Group. Geological Province: McArthur Basin. Mount is Mt in text.||||||
12510|Mount Birch Sandstone|60573|5|Briefly described|Map legend|Calymmian|Statherian|Of the Nathan Group. Feldspathic quartz sandstone, medium - to coarse-grained, cross-bedded, commonly dolomitic, scattered small pebbles and intraclasts; basal pebble to cobble conglomerate in type area. Mount is Mt in text of legend.||||||
12510|Mount Birch Sandstone|61390|5|Briefly described|Map Legend|Calymmian|Statherian|Of the Nathan Group. Feldspathic quartz sandstone: medium to coarse grained, cross bedded, commonly dolomitic.||||||
12510|Mount Birch Sandstone|64817|6|Mentioned|p353 Fig.4 |||||Of Nathan Group.||||
12510|Mount Birch Sandstone|69429|5|Briefly described|p14:4|||Hosts quartz hematite (ironstone) lenses (the Murphys Fe prospect) at the unconformable contact with the Mount Reid Rhyolite in the Urapunga Inlier vicinity.||Nathan Group.||||12-JUL-16
12510|Mount Birch Sandstone|69430|4|Described|p15:3, 22-24, 30, 51|||Abbott et al. (2001); formerly included within Balbirini Dolostone (Jackson et al., 1987). Urapunga Fault Zone, McArthur Basin. c.5-100m thick. Fluvial, braided stream deposits. Correlated with Smythe Sandstone and Bone Creek Sandstone elsewhere in the Basin. Hosts the Murphys iron ore prospect at the unconformity with Mount Reid Rhyolite.||Nathan Group.||Unconformably overlies Nagi Formation (Vizard Group), Urapunga Granite/Mount Reid Rhyolite. Is overlain conformably and gradationally by Knuckey Formation.|Dolomitic and quartz sandstone; lenticular conglomerate near base.|12-JUL-16
12510|Mount Birch Sandstone|69673|6|Mentioned|p16 fig 13|Paleoproterozoic|Paleoproterozoic|Urapunga Fault Zone||Nathan Group||Overlain by Knuckey Formation||
12510|Mount Birch Sandstone|72373|4|Described|iii,p1,24-25,27-33,35|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. Type section: 1 km south of Nagi Hill in southern URAPUNGA. About 80m thick at type section. Forms prominent ridges in outcrop. Has not been previously geochronologically dated. Two samples from the top and bottom of the formation, yielded interpreted max depositional ages of 1615+\-28 (Sample 2771375 (UR18TJM069: Silicified fine-grained quartz sandstone; URAPUNGA) and 1629+\-24 Ma (Sample 2771377 (UR18TJM077: Medium-grained, chertbearing quartz sandstone) respectively.|1629+\-24 Ma (max dep age)|Unit of Nathan Group.||Overlain gradationally by Knuckey Formation. Underlain unconformably by Nagi Formation or Mount Reid Rhyolite or Urapunga Granite. Correlable with Smythe Sandstone or Bone Creek Sandstone.|Dolomitic and quartz sandstone with a lenticular basal or near-basal conglomerate.|
12510|Mount Birch Sandstone|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as being located in the Urapunga Fault Zone in the Southern McArthur Basin.||Nathan Group||Shown as unconformably overlying Nagi Formation and underlies Knuckey Formation.||
12510|Mount Birch Sandstone|72718|6|Mentioned|p7|||Southern McArthur Basin. Urapunga Fault Zone.||Nathan Group||Unconformably underlain[?] by Nagi Formation (Vizard Group). Overlain by Knuckey Formation.||
12510|Mount Birch Sandstone|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Urapunga Fault Zone.||Nathan Group||Unconformably overlies Vizard Group and underlies Knuckey Formation. Partially equivalent to Smythe Sandstone.||
12510|Mount Birch Sandstone|73042|6|Mentioned|p4|Mesoproterozoic|Paleoproterozoic|Southern McArthur Basin, Isa Superbasin.||Nathan Group||Unconformably underlain(?) by Nagi Formation (Vizard Group). Overlain by Knuckey Formation.||
12516|Mount Birnie beds|32576|6|Mentioned|Fig.2|||||||||
12516|Mount Birnie beds|37816|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
12516|Mount Birnie beds|37930|6|Mentioned|p528|||||||||
12516|Mount Birnie beds|38350|6|Mentioned|p22|||||||||
12516|Mount Birnie beds|38608|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
12516|Mount Birnie beds|39029|5|Briefly described|Map legend|Cambrian|Cambrian|||||||25-AUG-04
12516|Mount Birnie beds|39425|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
12516|Mount Birnie beds|39496|6|Mentioned|p16|||||||||
12516|Mount Birnie beds|41306|6|Mentioned|p6|||||||||
12516|Mount Birnie beds|41801|6|Mentioned|p217|||||||||
12516|Mount Birnie beds|45162|6|Mentioned|p153|||||||||
12516|Mount Birnie beds|49027|6|Mentioned|p7|||||||||
12516|Mount Birnie beds|50100|5|Briefly described|p22|Early Cambrian|Early Cambrian|Predominantly shallow-marine, clastic, calcareous, dolomitic, cherty and phosphatic sedimentary rocks.  Disconformably overlain by Thorntonia Limestone.||||||
12516|Mount Birnie beds|63450|5|Briefly described|p78 Fig. 5, p80|Early Cambrian|Early Cambrian|Geological province: Georgina Basin, Burke River Structural Belt.||||||07-FEB-11
12516|Mount Birnie beds|64068|4|Described|p54, p46, 58|Early Cambrian|Early Cambrian|Correlations: Mount Baldwin Formation, Adam Shale, Octy Formation, Neutral Junction Formation, Riversdale Formation and possibly Sylvester Sandstone.||Of Shadow Group.||Unconformably overlies Little Burke Tillite. Is overlain unconformably by Thorntonia Limestone or Beetle Creek Formation.|Conglomerate, orthoquartzitic, silty and ferruginous sandstones, arkose, red and green micaceous shale, siltstone.|05-APR-12
12516|Mount Birnie beds|67127|6|Mentioned|p80|||||||||
12516|Mount Birnie beds|67323|5|Briefly described|GIS attrib tbl; p83|Cambrian|Cambrian|Burke River Structural Belt, Georgina Basin.||Shadow Group||Is overlain unconformably by Thorntonia Limestone.|Massive ferruginous sandstone, cross-bedded sandstone, conglomerate, red and green shale, mudstone, dolomite.|
12516|Mount Birnie beds|67870|5|Briefly described|p38-39, p43-46, p48, p50-53|Middle Cambrian|Middle Cambrian|Burke River Structural Belt, Georgina Basin. Basal sequence in the Basin.||||Is overlain unconformably by Thorntonia Limestone.|Sandstone, dolostone, organic-rich siltstone, shale.|
12516|Mount Birnie beds|68270|5|Briefly described|p681,683|Early Cambrian|Early Cambrian|Southern Georgina Basin.||||Underlain unconformably by Little Burke Tillite.||
12516|Mount Birnie beds|69377|5|Briefly described|map legend|Cambrian|Cambrian|||Shadow Group|||Massive ferruginous sandstone, cross-bedded sandstone, conglomerate, red and green shale, mudstone and dolomite; basal tillite|
12516|Mount Birnie beds|69443|5|Briefly described|p28:7, 14|Early Cambrian|Early Cambrian|Southern Georgina Basin.||Shadow Group.||||12-JUL-16
12516|Mount Birnie beds|69591|5|Briefly described|p87, p90-93, p96-97, p98 Fig.2.91|Cambrian|Cambrian|Burke River Structural Belt, Georgina Basin.||Shadow Group.||Is overlain unconformably by Thorntonia Limestone. A notional correlative of Riversdale Formation.|Basal tillite(20m); bedded dolomite(10m); massive dark ferruginous sandstone, thick-bedded and thin-bedded sandstone(40m); sandy, red or green micaceous shale and siltstone(100m); orthoquartzite and quartz conglomerate(20m); massive mudstone(20m).|
12516|Mount Birnie beds|72683|5|Briefly described|Map legend|Cambrian|Cambrian|Georgina Basin.||Shadow Group||Underlies Thorntonia Limestone.|Massive ferruginous sandstone, cross-bedded sandstone, conglomerate, red and green shale, mudstone and dolomite; basal tillite.|
12516|Mount Birnie beds|72684|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Georgina Basin. Overlies the Mitakoodi Domain. Shown as younger than the Isan Orogeny (1590-1500 Ma).||Shadow Group||Shown as unconformably underlying the Narpa Group.|Massive ferruginous sandstone, cross-bedded sandstone, conglomerate, red and green shale, mudstone and dolomite; basal tillite.|
12516|Mount Birnie beds|73553|5|Briefly described|p263|Cambrian|Neoproterozoic|Georgina Basin.||||Unconformably overlies Wimberu Granite||
12528|Mount Bonner Sandstone|22538|6|Mentioned|P715|||Part of the Glyde package||||||
12528|Mount Bonner Sandstone|22600|4|Described|Map legend|Statherian|Statherian|||||||
12528|Mount Bonner Sandstone|22808|6|Mentioned|7 fig 4|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
12528|Mount Bonner Sandstone|23374|5|Briefly described|Fig3p5||Paleoproterozoic|In the McArthur Basin.||||||07-NOV-08
12528|Mount Bonner Sandstone|24048|6|Mentioned|p101|||||||||
12528|Mount Bonner Sandstone|24049|5|Briefly described|Map Legend|Statherian|Statherian|Mount is Mt in text. Conglomerate: open to closed-framework, polymict; sandstone: pebbly, quartzose, large-scale trough cross-bedding. Geol. Prov: McArthur Basin.||||||12-OCT-05
12528|Mount Bonner Sandstone|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
12528|Mount Bonner Sandstone|32660|5|Briefly described|Table 4|||||||||
12528|Mount Bonner Sandstone|36473|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
12528|Mount Bonner Sandstone|37462|4|Described|Table4.IV|||||||||
12528|Mount Bonner Sandstone|37568|6|Mentioned|Fig.5|||||||||
12528|Mount Bonner Sandstone|41406|6|Mentioned|Map legend|Carpentarian||||||||
12528|Mount Bonner Sandstone|42597|5|Briefly described|Map legend|Carpentarian||||||||
12528|Mount Bonner Sandstone|43010|3|Fully described|p154|Mesoproterozoic|Paleoproterozoic|Of Statherian or Calymmian age. Only a reference area given. No Type Area nominated.||||||28-NOV-22
12528|Mount Bonner Sandstone|44112|3|Fully described|p10,63-65||Statherian|Max Age: 1717 (+/-) 11 Ma.||||||07-NOV-06
12528|Mount Bonner Sandstone|61403|5|Briefly described|Map Legend|Statherian|Statherian|Mount is Mt in text. Conglomerate: open to closed-framework, polymict; sandstone: pebbly, quartzose, large-scale trough cross-bedding. Geol. Prov: McA rthur Basin.||||||
12528|Mount Bonner Sandstone|63866|5|Briefly described|p116-p117|||||||Unconformably overlies the Cato Volcanics. Unconformably overlain by the Nathan Group. Equivalent to the Durabudboi beds.||
12528|Mount Bonner Sandstone|64817|6|Mentioned|p353 Fig.4 |||||||||
12528|Mount Bonner Sandstone|69430|4|Described|p15:3, 14, 23|||NE McArthur Basin. Previously included rocks which later (Rawlings et al., 1997) formed the Rorruwuy Sandstone.||||Unconformably overlies (most units in) the Spencer Creek Group. Is overlain unconformably by Balbirini Dolostone. Correlated with Jalma Formation.|Fluvial conglomerate and sandstone.|12-JUL-16
12528|Mount Bonner Sandstone|69673|6|Mentioned|p16 fig 13, p18|||||||||
12528|Mount Bonner Sandstone|71374|5|Briefly described|iii, p1 tbl 1, p27, p30-p33, p59-p60|Orosirian|Orosirian|McArthur Basin. SHRIMP age is interpreted as the maximum depositional age for this formation. An isolated younger age of 1729 +/- 14 Ma was returned for this unit also. Based on age is interpreted as a probable correlative of the Parsons Range Group. Approximately 150m thick. Sampling site provided along with zircon description and SHRIMP analytical discussion.|1815 +/- 9 Ma (SHRIMP U-Pb)|||Unconformably overlies the Yanungbi Volcanics. Unconformably overlain by the Balbirini Dolostone.|Basal conglomerate overlain by a fining-upwards succession of typically grey to white, silicified, fine- to medium- to very coarse-grained (locally pebbly) quartz sandstone.|
12528|Mount Bonner Sandstone|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.|||||Conglomerate, sandstone.|
12528|Mount Bonner Sandstone|72377|4|Described|iii,p1,13-16|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. Thickness: 150m. Rawlings et al (1997) suggested that Mount Bonner Sandstone may be an attenuated lateral facies variant of the Parsons Range, Habgood or Balma groups, deposited on the higher-relief flanks of the main depositional areas for these groups. Kositcin et al (2017) reported interpreted maximum depositional age of 1815+\-9 Ma. Sample GV16TJM004 (fine-grained quartz sandstone; 672547E 8663377N): interpreted maximum depositional age of c. 1815 Ma supports the supposition of a lateral correlation with the Parsons Range Group. MC-LA-ICP-MS zircon Hf studies yielded dominant age populations between c. 1868 to c. 1838 Ma with Hf isotope values consistent with zircons of the same age from Arnhem Province basement.|1815+\-9 Ma (max dep age)|||Underlain unconformably by Spencer Creek Group.|Thick, local basal conglomerate overlain by a fining-upwards succession of typically grey to white, silicified, fine- to medium- to very coarse-grained (locally pebbly) quartz sandstone.|
12554|Mount Bundey Granite|22658|6|Mentioned|p 270||Proterozoic|Geological Province - Pine Creek Inlier||||||
12554|Mount Bundey Granite|24047|5|Briefly described|p21, p39|||Part of the Mount Bundey igneous suite.||||||08-NOV-06
12554|Mount Bundey Granite|24197|5|Briefly described|p106 Tb. 15.1|Paleoproterozoic|Paleoproterozoic|Of the Cullen Supersuite. Age: ~1825Ma. Geological Province: Pine Creek Inlier.||||||07-FEB-11
12554|Mount Bundey Granite|32660|5|Briefly described|Table 2|||||||||
12554|Mount Bundey Granite|32958|4|Described|p956|||||||||
12554|Mount Bundey Granite|33278|6|Mentioned|Fig.7|||||||||
12554|Mount Bundey Granite|35465|6|Mentioned|p56|||||||||
12554|Mount Bundey Granite|39518|3|Fully described|p9|||||||||
12554|Mount Bundey Granite|39563|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
12554|Mount Bundey Granite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
12554|Mount Bundey Granite|41304|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
12554|Mount Bundey Granite|41305|4|Described|p19|||||||||
12554|Mount Bundey Granite|43624|6|Mentioned|p18,Fig.15,p20|||||||||
12554|Mount Bundey Granite|44314|14|Not recorded|p.9,10,map|||(D52-4).DARWIN Sheet.||||||08-NOV-06
12554|Mount Bundey Granite|44315|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
12554|Mount Bundey Granite|45022|4|Described|p.143||Carpentarian|Pet. Desc.on Tech-File D/52-4. On many pages.||||||08-NOV-06
12554|Mount Bundey Granite|45087|5|Briefly described|p24|||Chemical analyses.||||||
12554|Mount Bundey Granite|50586|5|Briefly described|p1.1, 4.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Of the Cullen Supersuite. Age: 1831 +/- 6Ma (U-Pb).||||||07-NOV-08
12554|Mount Bundey Granite|60526|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Coarse pink granite.||||||
12554|Mount Bundey Granite|60677|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Part of the Mount Bundey igneous suite.||||||08-NOV-06
12554|Mount Bundey Granite|62375|5|Briefly described|p26|||Age: 1831 +/- 6Ma. Intrudes the Mount Partridge and South Alligator Gps. Massive reddish-brown to pale pink granite and minor quartz monzonite. Feldspar, quartz, plagioclase, hornblende, biotite; minor zircon, epidote, magnetite, pyrite.||||||09-FEB-10
12554|Mount Bundey Granite|63866|4|Described|p110|Orosirian|Orosirian|Central Domain, Pine Creek Orogen. Numeric ages are derived from Page, OZCHRON. An additional numeric age of 1821 +/- 5 Ma is derived from Rasmussen et al., 2006. This unit has hornfelsed the Wildman Siltstone where they contact.|1831 +/- 6 Ma (SHRIMP)|Cullen Supersuite||Intrudes the Wildman Siltstone.||
12554|Mount Bundey Granite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Of Cullen Supersuite. Age 1831Ma U/Pb.  I-type. Pink porphyritic biotite granite, coarse biotite granite.||||||07-JAN-09
12554|Mount Bundey Granite|64730|6|Mentioned|p134|Orosirian|Orosirian||1831 +/- 6 Ma (Page 1996).|||Intrudes Gerowie Tuff.||03-MAY-12
12554|Mount Bundey Granite|65339|4|Described|p6 Table 1, pp12-13, p15. |||Has contact-metamorphosed Gerowie Tuff into a hard, cherty rock which is quarried at the Boral Mount Bundey quarry. With Mount Goyder Syenite, forms the Mount Bundey pluton; includes genetically associated K-rich shoshonitic lamprophyre (minette) and felsic dykes.|1831 +/- 6 Ma (Page in Sheppard 1995).|||Intrudes Wildman Siltstone and South Alligator Group.|Pink, medium to coarse biotite-hornblende monzogranite, with minor fine-grained porphyritic monzogranite.|
12554|Mount Bundey Granite|69420|4|Described|p5:14, 17-18, 20, 22, 45|Paleoproterozoic|Paleoproterozoic|Sheppard (1992). Granite-dominated plutons; mineralogy and petrology/geochemistry summarised. Is intruded by lamprophyre dykes at Toms Gully mine workings, where the Granite has caused development of andalusite-bearing hornfels in the Wildman Siltstone host.|1831 +/- 6 Ma conventional U-Pb zircon (TIMS).|Mount Bundey Suite.||Intrudes Mount Goyder Syenite.|Massive medium-grained granite. I-type, calc-alkaline.|12-JUL-16
12554|Mount Bundey Granite|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|1831+/-6.0 Ma (crystallisation: U-Pb).||||Granite.|
12580|Mount Chapple Metamorphics|23844|3|Fully described|p29|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Province. A component of the Narwietooma Metamorphic Complex (Warren and Shaw, 1995). See also Fig.11||||||07-NOV-08
12580|Mount Chapple Metamorphics|24197|5|Briefly described|p59 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Of the Narwietooma Suite. Age: ~1880Ma. Geological Province: Arunta Inlier. Mount is Mt in text.||||||07-FEB-11
12580|Mount Chapple Metamorphics|43225|5|Briefly described|Map Legend||Paleoproterozoic|Of the Narwietooma Metamorphic Complex.||||||07-NOV-08
12580|Mount Chapple Metamorphics|43503|1|Redefined|6,19,76|||||||||
12580|Mount Chapple Metamorphics|49831|5|Briefly described|p1, Fig.1 p15|||Defn crd with Convenor.  Variation on informal Mount Chapple granulite and Mount Chappell granulites.||||||08-NOV-06
12580|Mount Chapple Metamorphics|50369|5|Briefly described|p1.3, 3.1, table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Narwietooma Suite.||||||07-NOV-08
12580|Mount Chapple Metamorphics|60668|5|Briefly described|p7, p2 Tb. 1|||Large composite mafic-intermediate-felsic granulite body which is a component of the Narwietooma Metamorphic Complex. Dominated by mafic granulite. See also Fig. 17a||||||
12580|Mount Chapple Metamorphics|64738|5|Briefly described|pp247-248, p250 Table 1, pp252-253, 259|Paleoproterozoic|Paleoproterozoic|Subjected to two episodes of high-grade metamorphism: Strangways 1725 +/- 11 Ma, and Chewings 1591 +/- 6 Ma, events.|Protolith age of 1774 +/- 2 Ma.|||||
12580|Mount Chapple Metamorphics|67181|5|Briefly described|p631|Statherian|Statherian|Aileron Province, North Australian Craton. ca 1774 +/- 2 Ma from Claoue-Long and Hoatson (2005) and/or Hoatson et al. (2005)|ca 1774 +/- 2 Ma|||||
12580|Mount Chapple Metamorphics|67565|6|Mentioned|p5 Fig.3.|||Arunta Region.||||||
12580|Mount Chapple Metamorphics|68150|5|Briefly described|p11 Tb.3.2|||Age: SHRIMP, MSWD 1.8, 5 analyses, Claoue-Long and Hoatson, 2005.|1725 +/- 11 Ma, metamorphism|||||
12580|Mount Chapple Metamorphics|69427|4|Described|p12:3, 17-18, 29-32, 40, 44, 59|Statherian|Statherian|Aileron Province. Has less mafic rock, more felsic rock, and more abundant and variable metasedimentary rocks than Mount Hay Granulite, separated by the Harry Creek Shear Zone. SHRIMP U-Pb age of granulites; also evidence for high-grade metamorphism at 1725 +/- 11 Ma (Strangways Orogeny) and 1591 +/- 6 Ma (Chewings Orogeny). May have potential for Ni-Cu-Co mineralisation.|1774 +/- 2 Ma (Claoue-Long and Hoatson, 2005).|Narwietooma Metamorphic Complex.|||Mafic and felsic granulites; intermediate granulite and gneiss; quartzofeldspathic gneiss, felsic granulite with minor mafic granulite; gneissic charnockite; migmatitic metasedimentary rocks.|12-JUL-16
12580|Mount Chapple Metamorphics|70376|6|Mentioned|p834|Paleoproterozoic|Paleoproterozoic|Also ~1771 Ma felsic component (Claoue-Long & Hoatson 2005).|1774+/-2 Ma mafic component.|||||27-SEP-16
12580|Mount Chapple Metamorphics|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen. Metamorphosed at 1725 +/- 11 Ma and at 1591 +/- 6 Ma (both U-Pb zircon SHRIMP ages).|1774+/-2 Ma (crystallisation: U-Pb zircon SHRIMP)||||Mafic granulite, felsic granulite.|
12580|Mount Chapple Metamorphics|71858|6|Mentioned|p69|||Aileron Province.||||||
12580|Mount Chapple Metamorphics|72894|6|Mentioned|p19|||||Narwietooma Metamorphic Complex|||Dominated by quartzofeldspathic gneiss and felsic granulite|
12596|Mount Cornish Formation|9694|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Geological Province: Georgina Basin. Underlies: Oorabra Arkose. Blue-grey diamictite.||||||
12596|Mount Cornish Formation|33102|6|Mentioned|Fig.2|||||||||
12596|Mount Cornish Formation|33699|6|Mentioned|p445|||||||||
12596|Mount Cornish Formation|35005|5|Briefly described|p145|||||||||
12596|Mount Cornish Formation|36473|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
12596|Mount Cornish Formation|36898|6|Mentioned|p181|||||||||
12596|Mount Cornish Formation|37572|5|Briefly described|p154|||||||||
12596|Mount Cornish Formation|37929|4|Described|p525|||||||||
12596|Mount Cornish Formation|38157|6|Mentioned|Table IX|||||||||
12596|Mount Cornish Formation|39210|4|Described|p51|||||||||
12596|Mount Cornish Formation|40538|5|Briefly described|Map legend|Adelaidean|Adelaidean|Tillite; siltstone; varvite. Geological Province: Georgina Basin.||||||15-NOV-05
12596|Mount Cornish Formation|40906|4|Described|p18|||||||||
12596|Mount Cornish Formation|41005|6|Mentioned|Fig.2|||||||||
12596|Mount Cornish Formation|41405|6|Mentioned|p205|||||||||
12596|Mount Cornish Formation|42059|6|Mentioned|Fig.2 P131|||||||||
12596|Mount Cornish Formation|42504|5|Briefly described|p72|||In the Georgina Basin.||||||08-NOV-06
12596|Mount Cornish Formation|42643|6|Mentioned|Fig.4 P19|||||||||
12596|Mount Cornish Formation|44158|6|Mentioned|p29|||In the Georgina Basin.||||||08-NOV-06
12596|Mount Cornish Formation|44233|14|Not recorded|Fig.1||Adelaidean|||||||
12596|Mount Cornish Formation|44327|2|Defined|Tb.I,p.7,8,13,14,18||Neoproterozoic|(F53-11). U.Prot. may be correlated with Areyonga Formation. Map.||||||08-NOV-06
12596|Mount Cornish Formation|44328|14|Not recorded|map legend||Neoproterozoic|Upper Proterozoic.||||||
12596|Mount Cornish Formation|45041|6|Mentioned|p45|||Correlates with Olympic Member||||||
12596|Mount Cornish Formation|45052|2|Defined|p67|Adelaidean|Adelaidean|||||||
12596|Mount Cornish Formation|45155|6|Mentioned|Fig.7|||In theGeorgina Basin.||||||08-NOV-06
12596|Mount Cornish Formation|46865|6|Mentioned|p49|||||||||
12596|Mount Cornish Formation|48844|2|Defined|p.1,16-20,22-3|||F.26,57,58,67,Pl.8. (new name). Overlain by Elyuah orFormation. Glacial origin. (F53-11).||||||08-NOV-06
12596|Mount Cornish Formation|48990|1|Redefined|p13|Adelaidean|Adelaidean|||||||
12596|Mount Cornish Formation|60122|6|Mentioned|p9|||||||||
12596|Mount Cornish Formation|60551|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Underlies Oorabra Arkose; overlies Yackah beds. Geological province: Georgina Basin.  Diamictite, siltstone, varved beds.||||||08-NOV-06
12596|Mount Cornish Formation|61404|5|Briefly described|Map legend|Cryogenian|Cryogenian|Of the Aroota Group. Tillite, siltstone, varvite. Geological Province: southern Georgina Basin.||||||
12596|Mount Cornish Formation|63562|6|Mentioned|p338 fig 3, p352 fig 10|Cryogenian|Cryogenian|Of Georgina Basin.||||Correlated with Areyonga Formation.||
12596|Mount Cornish Formation|64068|3|Fully described|p45, p223, p viii|Cryogenian||Correlated with Yardida Tilite.||Of Aroota Group.||Disconformably overlies Yackah beds; is disconformably overlain by Oorabra Arkose.|Several hundred metres of blue-green diamictite with interbeds of varvite and siltstone; minor sandstone, arkose and dolostone.|04-APR-12
12596|Mount Cornish Formation|64103|6|Mentioned|p404|||Geological Province: Georgina Basin.||||||07-FEB-11
12596|Mount Cornish Formation|64778|6|Mentioned|p13|Neoproterozoic|Neoproterozoic|Dulcie Syncline, Southern Georgina Basin.||||||
12596|Mount Cornish Formation|68270|4|Described|p680-683,686-688|Cryogenian|Cryogenian|Southern Georgina Basin. Type section occurs 4km WSW to 4.8km SSW of Mount Cornish; lat. 22'49'S, long. 136'27'E. Less than 365m thick. Glacial and periglacial deposit. Correlative to Sturt Tillite. Lateral equivalent to Yardida Tillite. Related to Sturt glaciation.||||Overlain disconformably by Oorabra Arkose. Underlain disconformably by Yackah beds.|Poorly bedded blue-green diamictite with interbeds of green varve-like siltstone, minor sandstone, arkose and dolostone; possible lower marker cap dolomite.|03-JUL-19
12596|Mount Cornish Formation|69437|5|Briefly described|p22:4-5, 7|Cryogenian|Cryogenian|SE Georgina Basin, Centralian A Superbasin. Supersequence 2.||Aroota Group.|||Glacial sedimentary rocks.|12-JUL-16
12596|Mount Cornish Formation|69439|6|Mentioned|p24:7|||Georgina Basin.||||Correlated with Naburula Formation (Ngalia Basin).||12-JUL-16
12596|Mount Cornish Formation|69443|4|Described|p28:6-8, 32-33|Cryogenian|Cryogenian|K.G. Smith (1964). Mount Cornish, Georgina Basin. Unfossiliferous. Small discontinuous outcrops. Generally 12-34m thick; 680m in the type section. Glacial and periglacial deposits. Part of the hangingwall of the Ooomoolmilla and Lucy Creek Faults; interpreted as rift basin fill in half grabens.||Aroota Group.||Disconformably overlies Yackah beds. Is overlain disconformably by Oorabra Arkose. Correlated with Yardida Tillite.|Diamictite with interbeds of varvite and siltstone; minor sandstone, arkose and dolostone. Some diamictite clasts are faceted and striated.|12-JUL-16
12596|Mount Cornish Formation|69673|4|Described|p114 fig 92|Cryogenian|Cryogenian|Maximum thickness of 680m.||Aroota Group|||Diamictite with interbeds of varvite and siltstone; minor sandstone and dolostone.|
12596|Mount Cornish Formation|72515|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Jervois Range Special Map Sheet. Georgina Basin.||Aroota Group|||Diamictite, interbedded varvite, siltstone; minor sandstone, arkose and dolostone.|
12596|Mount Cornish Formation|72516|3|Fully described|p13, p72, p79, p85-87|Cryogenian|Cryogenian|Georgina Basin. Type section occurs 4km west-southwest of Mount Cornish in southeast JERVOIS RANGE SPECIAL; also exposed in the Elua Range in Jinka. Deposited in a glacial to periglacial environment. Maximum thickness of 680m in the type section, however structural repitition is interpreted; 12-34m thick in Jinka. Equivalent to the Yardida Tillite and Central Mount Stuart Formation. See also p96-97, p154, p186, p195, p218.||Aroota Group||Unconformably overlies the Boundary Igneous Complex. Disconformably overlies the Yackah beds. Disconformably overlain by the Oorabra Arkose.|Poorly sorted, medium to very thickly bedded, blue green diamictite interbedded with laminated varvite and siltstone, minor sandstone, arkose and dolostone layers.|
12596|Mount Cornish Formation|73086|6|Mentioned|p62, p158|||Georgina Basin.||||Correlates to Areyonga Formation.||
12609|Mount Currie Conglomerate|22566|5|Briefly described|p73|Early Cambrian|Neoproterozoic|Of the Pertaoorrta Group.||||||08-NOV-06
12609|Mount Currie Conglomerate|22650|4|Described|p 160|||Age - Cambrian p 159.||||||
12609|Mount Currie Conglomerate|22651|5|Briefly described|p 173|||Precise age uncertain,  suggested approx. age of 600-580 Ma.||||||08-NOV-06
12609|Mount Currie Conglomerate|22763|6|Mentioned|p400|||||||||
12609|Mount Currie Conglomerate|22804|5|Briefly described|p444||Neoproterozoic|Of the Pertaoorrta Group.||||||08-NOV-06
12609|Mount Currie Conglomerate|22826|6|Mentioned|p568|Cambrian|Neoproterozoic|||||||
12609|Mount Currie Conglomerate|24301|3|Fully described|p17, p7 Tb. 2|Cambrian|Neoproterozoic|Defined by Forman (1955). Is divided into three informal units. Maximum thickness: 6100m. Unconformably overlies Winnall Sandstone. Geological Province: Amadeus Basin||||||24-SEP-08
12609|Mount Currie Conglomerate|24302|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Amadeus Basin||||||
12609|Mount Currie Conglomerate|24496|5|Briefly described|p21 Tb.2|Cambrian|Cambrian|Geological Province: Amadeus Basin.||||||
12609|Mount Currie Conglomerate|24497|5|Briefly described|Map legend|Early Paleocene|Neoproterozoic|Geological Province: Amadeus Basin.||||||
12609|Mount Currie Conglomerate|24499|5|Briefly described|Map legend|||Mount is Mt. in text.  Geological Province: Amadeus Basin.||||||
12609|Mount Currie Conglomerate|30815|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
12609|Mount Currie Conglomerate|30817|4|Described|p9|||See also p14.||||||08-NOV-06
12609|Mount Currie Conglomerate|33307|6|Mentioned|Fig.6|||||||||
12609|Mount Currie Conglomerate|33478|6|Mentioned|Table 1|||||||||
12609|Mount Currie Conglomerate|33568|6|Mentioned|p45|||||||||
12609|Mount Currie Conglomerate|35102|6|Mentioned|Fig.2|||||||||
12609|Mount Currie Conglomerate|35308|6|Mentioned|p454|||||||||
12609|Mount Currie Conglomerate|36473|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
12609|Mount Currie Conglomerate|38157|6|Mentioned|Table VI|||||||||
12609|Mount Currie Conglomerate|39213|6|Mentioned|Fig.6|||Amadeus Basin Succession||||||
12609|Mount Currie Conglomerate|39565|6|Mentioned|p32|||||||||
12609|Mount Currie Conglomerate|40740|6|Mentioned|p1|||||||||
12609|Mount Currie Conglomerate|40910|6|Mentioned|p13|||||||||
12609|Mount Currie Conglomerate|41115|6|Mentioned|p1389|||||||||
12609|Mount Currie Conglomerate|41723|6|Mentioned|Map legend|Neoproterozoic|Early Cambrian|||||||
12609|Mount Currie Conglomerate|41852|6|Mentioned|Table 1|||||||||
12609|Mount Currie Conglomerate|41884|4|Described|p70|||||||||
12609|Mount Currie Conglomerate|42018|6|Mentioned|p540|||||||||
12609|Mount Currie Conglomerate|42504|5|Briefly described|p76|||||||||
12609|Mount Currie Conglomerate|42940|5|Briefly described|Plate 2|Cambrian|Cambrian|Conglomerate, arkose.  Age: 590-500Ma. Geological province: Amadeus Basin.||||||23-JAN-08
12609|Mount Currie Conglomerate|43035|4|Described|p20|||||||||
12609|Mount Currie Conglomerate|43503|6|Mentioned|50|Early Cambrian|Proterozoic|||||||
12609|Mount Currie Conglomerate|43756|6|Mentioned|p542|||||||||
12609|Mount Currie Conglomerate|43869|4|Described|p9, p10, p12|||Age: >550 Ma.  Geological Province: Amadeus Basin.||||||12-SEP-05
12609|Mount Currie Conglomerate|44109|5|Briefly described|p164|Cambrian|Cambrian|Thick, poorly sorted conglomerate and boulder lenses, with clasts up 1m across. Geological Province: Amadeus Basin.||||||
12609|Mount Currie Conglomerate|44439|14|Not recorded|p.7||Precambrian|Probably equivalent to Ellis Sandstone & Sir Frederick Conglomerate. Tentatively uppermost Precambrian. (G52-1).||||||
12609|Mount Currie Conglomerate|44493|4|Described|p.11, map|||BLOODS RANGE sheet. (G53-3). See p.8,10,12, for details.||||||08-NOV-06
12609|Mount Currie Conglomerate|44494|14|Not recorded|map legend||Cambrian|||||||
12609|Mount Currie Conglomerate|44495|4|Described|p.6, map||Cambrian|AYERS ROCK sheet (G52-8). See p.8,10 for details.||||||08-NOV-06
12609|Mount Currie Conglomerate|44496|5|Briefly described|map legend||Cambrian|Conglomerate; arkose at Ayers Rock possible lithological variant.||||||02-DEC-04
12609|Mount Currie Conglomerate|44505|14|Not recorded|p.3,7,8, Fig.1, Tb.1||Cambrian|||||||
12609|Mount Currie Conglomerate|44506|14|Not recorded|map legend||Proterozoic|||||||
12609|Mount Currie Conglomerate|45041|4|Described|p46|||L.Cambrian||||||
12609|Mount Currie Conglomerate|45170|5|Briefly described|p7|||||||||
12609|Mount Currie Conglomerate|48863|2|Defined|p.14|||Tb.1. opp. p.7,15. (G52-4) ?Cambrian.||||||
12609|Mount Currie Conglomerate|48864|2|Defined|p.29|||Tb.1. On many pages. p.1,9,10,24,27,38,31,42,47,Pl.11,13. (G52-3,7,8). ?Cambrian.||||||
12609|Mount Currie Conglomerate|48865|14|Not recorded|Fig.4.opp.p.10|||(G52-4).||||||
12609|Mount Currie Conglomerate|48963|6|Mentioned|Fig.3|||||||||
12609|Mount Currie Conglomerate|50286|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Amadeus Basin.||||||22-DEC-09
12609|Mount Currie Conglomerate|60572|5|Briefly described|Map legend|Cambrian|Cambrian|Geological Province: Amadeus Basin.||||||23-DEC-09
12609|Mount Currie Conglomerate|60660|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Non-magnetic molasse basin sediments.||||||22-FEB-05
12609|Mount Currie Conglomerate|60662|5|Briefly described|Map Legend|||Molasse basin sediments.||||||22-FEB-05
12609|Mount Currie Conglomerate|60678|5|Briefly described|Map legend|Cambrian|Cambrian|Conglomerate containing clasts of sandstone, quartzite, felsic and mafic volcanics, granite, gneiss, mafic intrusives.  Geological Province: Amadeus Basin.||||||11-JAN-05
12609|Mount Currie Conglomerate|60679|5|Briefly described|Map Legend|Cambrian|Cambrian|Conglomerate with clasts of volcanics, granite and basalt. Geological Province: Amadeus Basin.||||||
12609|Mount Currie Conglomerate|60683|4|Described|p25-26, p9 Tb. 1|Cambrian|Cambrian|Includes the Ampiara member.  Unconformably overlies the Winnall beds. Geological Province: Musgrave Block/Amadeus Basin.||||||20-APR-05
12609|Mount Currie Conglomerate|61154|5|Briefly described|p26, p29|||Molasse deposits in the Mulga Park Domain, containing metamorphic epidote and locally actinolite. Age: 1062+/-6Ma (for contained rhyolite clast from Musgrave Block: Kober Pb-Pb age).  Geological Province: Musgrave Block.||||||19-JUL-05
12609|Mount Currie Conglomerate|61306|5|Briefly described|p11, p24|Cambrian|Cambrian|At Kata Tjuta and Mount Currie - in the Kata Tjuta complex. Geological Province: Amadeus Basin. See also p30, p46 Fig. 12 and p78-82 Appendix figures.||||||
12609|Mount Currie Conglomerate|61386|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Contains the Ampiara member. Coarse conglomerate, with rounded clasts of fine-grained porphyritic and banded rhyolite and less abundant rhyodacite, granite, amygdaloidal basalt in an epidotised arkosic matrix. Geological Province: Amadeus Basin.||||||23-DEC-09
12609|Mount Currie Conglomerate|61732|6|Mentioned|p96|||Overlie Winnall beds.||||||07-FEB-11
12609|Mount Currie Conglomerate|62376|5|Briefly described|p18|Early Cambrian|Late Proterozoic|Of the Pertaoorrta Group. Geological Province: Amadeus Basin.||||||09-FEB-10
12609|Mount Currie Conglomerate|62379|5|Briefly described|p7 Fig. 2|Early Cambrian|Late Proterozoic|Of the Pertaoorrta Group. Geological Province: Amadeus Basin.||||||
12609|Mount Currie Conglomerate|62609|5|Briefly described|Map Legend|Cambrian|Proterozoic|Conglomerate, arkose at  Ayers Rock.||||||08-NOV-06
12609|Mount Currie Conglomerate|62620|5|Briefly described|Map Legend|Cambrian|Proterozoic|Conglomerate, arkose at Ayers Rock.||||||
12609|Mount Currie Conglomerate|64068|6|Mentioned|p224|||Amadeus Basin. Correlated with Shadow Group, Georgina Basin.||||||
12609|Mount Currie Conglomerate|64103|6|Mentioned|p401|Early Cambrian|Ediacaran|Geological Province: Amadeus Basin.||||||07-FEB-11
12609|Mount Currie Conglomerate|64809|5|Briefly described|p2, p3 Fig.2 |Early Cambrian|Late Proterozoic|Deposited in Mount Currie Sub-basin during Petermann Orogeny.||Unit in Pertaoorrta Group.||||
12609|Mount Currie Conglomerate|65194|5|Briefly described|p64 Fig.4.9|Cambrian|Cambrian|Bedrock outcrops around Uluru.||||||11-APR-16
12609|Mount Currie Conglomerate|65233|5|Briefly described|p3 Fig. 2, p7|Early Cambrian|Neoproterozoic|Of the Pertaoorrta Group. Geological province: Amadeus Basin. Coarse. Clastic rocks in SW of basin which probably interfinger with Arumbera Sandstone.||||||07-FEB-11
12609|Mount Currie Conglomerate|65256|4|Described|piii, p6 Tb.1, p11, p16, p19|Cambrian||Molasse-type sediments from Petermann Orogeny uplift. Up to 6-7 km thick. Pb-Pb Kober zircon date for a rhyolite clast 1062+/-6 Ma; likely sourced from Tjauwata Group.||||Unconformably overlies Pinyinna beds, Winnall beds; correlated with Arumbera Sandstone.|Well-rounded clasts of quartzite; lower section is oligomictic comprising sandstone clasts; becomes polymictic and dominated by porphyritic rhyolite clasts up-section; upper part grades into dominantly granitic clasts.|19-MAY-14
12609|Mount Currie Conglomerate|67128|5|Briefly described|p13, p29|||Appears as Mount Currie conglomerate on p13. Kober Pb evaporation age from a rhyolite clast.|<1062 +/- 6 Ma (Young et al., 2002).|||||
12609|Mount Currie Conglomerate|67326|5|Briefly described|p2, p4|Early Cambrian|Neoproterozoic|Amadeus Basin.||Pertaoorrta Group.||Overlies Eninta Formation. Is overlain by Cleland Sandstone and tempe Formation.||
12609|Mount Currie Conglomerate|67856|6|Mentioned|p338 fig 4-30|Early Cambrian|Neoproterozoic|||Of Pertaoorta Group.||||
12609|Mount Currie Conglomerate|68100|6|Mentioned|p27|||Amadeus Basin. Detrital zircon ages mentioned.||||||
12609|Mount Currie Conglomerate|68270|5|Briefly described|p683|Ediacaran|Ediacaran|Amadeus Basin.||||Underlain by Sir Fred Conglomerate and Ellis Sandstone.||
12609|Mount Currie Conglomerate|68323|6|Mentioned|p4 Fig.2|Early Cambrian|Neoproterozoic|Amadeus Basin.||Pertaoorrta Group.||||
12609|Mount Currie Conglomerate|68733|6|Mentioned|p189 Fig.8|Ediacaran|Ediacaran|Mount spelt as Mt in text. Shown as underlying (sic) the Winnall Beds.||||||05-DEC-17
12609|Mount Currie Conglomerate|69436|5|Briefly described|p21:4, 20|Paleozoic|Paleozoic|Mount Currie Sub-basin, Amadeus Basin. Coarse fluvial sediments deposited in a flexural downwarping produced by the Petermann Orogeny.||||||12-JUL-16
12609|Mount Currie Conglomerate|69437|5|Briefly described|p22:10|Cambrian|Cambrian|Idirriki Sub-basin, SW Amadeus Basin.||||Is overlain by Maurice Formation.||12-JUL-16
12609|Mount Currie Conglomerate|69438|4|Described|p23:2-4, 20-23, 26-27, 44|Early Cambrian|Ediacaran|Forman (1963). Amadeus Basin. Estimated thickness is 6100m; 650m is exposed at Mount Olga (Kata Tjuta). Previously correlated with the Arumbera Sandstone. Probably late syntectonic to post-tectonic with the later phases of the 580-530 Ma Petermann Orogeny. Metamorphosed to greenschist facies. Lithologies are described in some detail.||Pertaoorrta Group.||Unconformably overlies Winnall beds. Is correlated with the Mutitjulu Arkose.|A thick succession of coarse pebble, cobble and boulder conglomerate.|12-JUL-16
12609|Mount Currie Conglomerate|69443|6|Mentioned|p28:14|||Amadeus Basin.||||Correlated with (part of) the Shadow Group.||12-JUL-16
12609|Mount Currie Conglomerate|69673|6|Mentioned|p64 fig 53, p65|||||||||
12609|Mount Currie Conglomerate|70018|5|Briefly described|p234-235|Neoproterozoic|Neoproterozoic|Amadeus Basin. Of Supersequence 4 in the southern Amadeus Basin. Equivalent to Ayers Rock Arkose. Correlable to Arumbera Sandstone in the northern Amadeus Basin.||||Underlain by Winnall Beds.||
12609|Mount Currie Conglomerate|70839|4|Described|p324,329-330,341-345|Cambrian|Cambrian|Of the southern Amadeus Basin. Part of Supersequence 4. Estimated thickness: 6km (as base of unit is not exposed). Interpreted to represent local remnants of proximal foreland deposition from Petermann Orogeny (Forman, 1966; Wells et al., 1970; Lindsay and Korsch, 1991). Detrital zircon analysis suggest a Musgrave region source (Pitjantjatjara Supersuite; Camacho et al., 2002) and additional minor Warakurna Supersuite component. Metamorphosed to greenschist-facies (Edgoose et al., 2004) indicating significant burial. Juxtaposed in outcrop against Winnall Beds unit 4 at one locality on the AYERS ROCK 1:250,000 geological map sheet near Yulara (Forman, 1965; Young et al., 2002). Alternative possibility from this study suggests this unit dates from late in the development of c. 1.0 Ga Ngaanyatjarra Rift.||||Underlain unconformably by Winnall beds. Equivalent to Mutitjulu Arkose.|Thick boulder conglomerate. Clasts include fresh igneous and metamorphic rocks including granite, basalt, and other lithologies.|
12609|Mount Currie Conglomerate|71088|5|Briefly described|p1, p8-p10, p12, p25-p27|Cambrian|Cambrian|Amadeus Basin. Assigned by previous authors to Supersequence 4, a lack of zircons younger than c. 1 Ga warrants a reassessment of their stratigraphic and structural relationships (according to the authors). Potentially unconformably overlies the Winnall beds.||||Equivalent (assumed) to the Mutitjulu Arkose.||
12609|Mount Currie Conglomerate|71114|5|Briefly described|p170 fig 1b|Terreneuvian|Ediacaran|SW Amadeus Basin.||||Shown as lateral equivalent to Ellis Sandstone, Sir Frederick Conglomerate.||14-FEB-18
12609|Mount Currie Conglomerate|71170|5|Briefly described|p91, p95|||Metamorphic evidence suggests this unit was deeply buried.||||||
12609|Mount Currie Conglomerate|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||quartzite, sandstone|
12609|Mount Currie Conglomerate|71279|5|Briefly described|p355 Fig.2|Early Cambrian|Ediacaran|Amadeus Basin.||Pertaoorrta Group.||||
12609|Mount Currie Conglomerate|71592|5|Briefly described|Appendix A.|||Musgrave Province. Contains a rhyolite clast dated at 1062 +/- 6 Ma.|||||Includes clast of rhyolite.|
12609|Mount Currie Conglomerate|71800|5|Briefly described|p26-p27|Early Cambrian|Early Cambrian|Amadeus Basin.||||Overlies the Maurice Formation. Unconformably overlain by the Chandler Limestone.|Sandstone.|
12609|Mount Currie Conglomerate|71841|5|Briefly described|p1|Early Cambrian|Ediacaran|Of Amadeus Basin.||Unit of Pertaoorrta Group.||Surrounded by Winnall beds. Also grades into Ellis Sandstone.||
12609|Mount Currie Conglomerate|71842|5|Briefly described|p3|Early Cambrian|Ediacaran|Of Amadeus Basin.||Unit of Pertaoorrta Group.||Correlable to Ellis Sandstone, Sir Frederick Conglomerate and Winnall Beds.||
12609|Mount Currie Conglomerate|72358|6|Mentioned|p118|Series 1|Ediacaran|Of Amadeus Basin.||||||
12609|Mount Currie Conglomerate|72476|5|Briefly described|p26, 35-36|||Amadeus Basin. Early Paleozoic. Sediments derived from the Musgrave Block basement.|||||Thick (>4 km) packages.|
12609|Mount Currie Conglomerate|73180|6|Mentioned|p48 Fig.1|Early Cambrian|Early Cambrian|Amadeus Basin. Mount spelt as Mt in text.||||Disconformably overlies the Carnegie Formation, underlies the Maurice Formation.||
12627|Mount Davis Granite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
12627|Mount Davis Granite|40823|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
12627|Mount Davis Granite|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
12627|Mount Davis Granite|41311|4|Described|p20|||||||||
12627|Mount Davis Granite|42756|6|Mentioned|Fig.5 P6|||||||||
12627|Mount Davis Granite|43140|4|Described|p37||Paleoproterozoic|Within the Cullen Batholith.||||||07-NOV-08
12627|Mount Davis Granite|43624|6|Mentioned|p14|||||||||
12627|Mount Davis Granite|43832|4|Described|Table8p37;46,Tb12p63||Paleoproterozoic|||||||07-NOV-08
12627|Mount Davis Granite|45022|4|Described|p.137|||(= Cullen Granite).||||||
12627|Mount Davis Granite|50586|5|Briefly described|p1.1, 4.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Of the Cullen Supersuite.||||||07-NOV-08
12627|Mount Davis Granite|60680|5|Briefly described|Map legend|Orosirian|Orosirian|Of the Cullen Supersuite.  Pink medium to coarse equigranular biotite leucogranite and coarse porphyritic biotite leucogranite.  Age: 1810-1800Ma.||||||13-JAN-05
12627|Mount Davis Granite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1800-1820Ma. Of Cullen Supersuite.  I-type. Pink, medium to coarse equigranular biotite leucogranite and coarse porphyritic biotite leucogranite. Intrudes Burrell Creek Formation.||||||
12627|Mount Davis Granite|67564|3|Fully described|p7 Table 2, p24, p33 Fig.19, pp35-36.|Paleoproterozoic|Paleoproterozoic|I-type. 11 km by 5 km pluton within Cullen Batholith, Pine Creek Orogen. Greisens and vein quartz stockworks are common; some host copper mineralisation, e.g. Mount Davis mine.|1810 - 1800 Ma.|Unit in Cullen Supersuite.||Is intruded by Lewin Springs Syenite.|Pink, medium to coarse, equigranular biotite leucogranite; locally grades into coarse porphyritic biotite leucogranite.|
12627|Mount Davis Granite|69420|5|Briefly described|p5:17-20, 85-87|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Leucogranite-dominated plutons; mineralogy and petrology/geochemistry summarised. Also listed in Shoobridge Suite [?] p5:20. Hosts Cu-Pb deposits including 16 vein-type occurrences, eg Mount Davis.||Saunders Suite.|||Coarse-grained porphyritic leucogranite. I-type.|12-JUL-16
12639|Mount Doreen Formation|23314|5|Briefly described|331 Fig.2|||||||||
12639|Mount Doreen Formation|24064|4|Described|p226|Adelaidean|Adelaidean|Geological Province: Ngalia Basin. Maximum thicknes: 340m.||||||
12639|Mount Doreen Formation|24111|5|Briefly described|p216|Neoproterozoic|Neoproterozoic|Geological Province: Ngalia Basin. Mount is Mt in text.  See also p215 Fig. 11.||||||30-MAR-05
12639|Mount Doreen Formation|30258|6|Mentioned|p101|||Proterozoic age. See also FIg.2||||||
12639|Mount Doreen Formation|31454|6|Mentioned|Fig.2|||||||||
12639|Mount Doreen Formation|32442|5|Briefly described|p9|||||||||
12639|Mount Doreen Formation|33102|6|Mentioned|Fig.2|||||||||
12639|Mount Doreen Formation|33757|3|Fully described|p9|||See also Table 1. Adelaidean.||||||09-NOV-06
12639|Mount Doreen Formation|33760|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
12639|Mount Doreen Formation|33761|6|Mentioned|p145|||Adelaidean||||||
12639|Mount Doreen Formation|35863|6|Mentioned|p288|||||||||
12639|Mount Doreen Formation|36473|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
12639|Mount Doreen Formation|36898|6|Mentioned|p181|||||||||
12639|Mount Doreen Formation|37462|4|Described|Table 4.IX|||||||||
12639|Mount Doreen Formation|37537|5|Briefly described|Map legend|Adelaidean|Adelaidean|Basal diamictite, pink marker dolomite. Diamictite, dolomite and shale. Geological Province: Ngalia Basin.||||||14-FEB-06
12639|Mount Doreen Formation|37928|3|Fully described|p519|||See also p515.||||||09-NOV-06
12639|Mount Doreen Formation|38157|6|Mentioned|Table VII|||||||||
12639|Mount Doreen Formation|38945|4|Described|p131|||||||||
12639|Mount Doreen Formation|39565|6|Mentioned|p33|||||||||
12639|Mount Doreen Formation|40906|6|Mentioned|Fig.9|||||||||
12639|Mount Doreen Formation|41405|5|Briefly described|p205|||||||||
12639|Mount Doreen Formation|41429|6|Mentioned|p247|||||||||
12639|Mount Doreen Formation|41717|6|Mentioned|Fig.19|||||||||
12639|Mount Doreen Formation|42059|5|Briefly described|Fig.2 P131|||||||||
12639|Mount Doreen Formation|42504|5|Briefly described|p83|||||||||
12639|Mount Doreen Formation|42643|6|Mentioned|p21|||In the Ngalia Basin.||||||09-NOV-06
12639|Mount Doreen Formation|43275|5|Briefly described|Map Legend||Neoproterozoic|||||||
12639|Mount Doreen Formation|43595|5|Briefly described|p548,Fig.5-33,549||Adelaidean|||||||
12639|Mount Doreen Formation|43631|3|Fully described|p24,25||Neoproterozoic|||||||
12639|Mount Doreen Formation|43749|6|Mentioned|Fig.1,p6||Neoproterozoic|||||||
12639|Mount Doreen Formation|44158|4|Described|p29 Table.2|Neoproterozoic|Neoproterozoic|In the Ngalia Basin.||||||09-NOV-06
12639|Mount Doreen Formation|45155|2|Defined|p26|Adelaidean|Adelaidean|||||||
12639|Mount Doreen Formation|46865|4|Described|p52|||Mention p41.||||||09-NOV-06
12639|Mount Doreen Formation|46903|6|Mentioned|p54|||||||||
12639|Mount Doreen Formation|61385|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Tillite, dololutite, shale, sandstone.  Geological Province: Ngalia Basin.||||||
12639|Mount Doreen Formation|62085|6|Mentioned|p24|Ediacaran|Ediacaran|Ngalia Basin. Cap carbonate in this unit corresponds with the GSSP of Nuccaleena Formation.||||||
12639|Mount Doreen Formation|64068|6|Mentioned|p46|||Ngalia Basin.  Correlated with Sun Hill Arkose, Little Burke Tillite, Black Stump Arkose, Wonnadinna Dolostone, Oorabra Arkose, Boko Formation, southern Georgina Basin.||||||
12639|Mount Doreen Formation|65232|5|Briefly described|p70|||Disconformably overlies Rinkabeena Shale. Diamictite, dolostone, shale. Geol. Prov: Ngalia Basin.||||||09-FEB-10
12639|Mount Doreen Formation|65329|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of Ngalia Basin. Shown as younger than Rinkabeena Shale, older than Yuendumu Sandstone. Tillite, dololutite, shale, sandstone||||||
12639|Mount Doreen Formation|65330|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of Ngalia Basin. Shown as younger than Rinkabeena Shale, older than Yuendumu Sandstone. Tillite, dololutite, shale, sandstone||||||
12639|Mount Doreen Formation|65342|6|Mentioned|p6.|||Ngalia Basin. Max. thickness at least 149 m.||||Overlies Rinkabeena Shale. Is overlain by Djagamara Formation.|Green to red-brown siltstone.|
12639|Mount Doreen Formation|67872|5|Briefly described|p13, p15, p35|Neoproterozoic|Neoproterozoic|Ngalia Basin. Part of the M2 mega-sequence of Lindsay (2002).|||Wanapi Dolomite Member.|||17-APR-18
12639|Mount Doreen Formation|68244|6|Mentioned|p671|||Ngalia Basin.||||||
12639|Mount Doreen Formation|68270|4|Described|p680,682-683,686-687|Ediacaran|Cryogenian|Ngalia Basin.|||Includes Newhaven Shale Member, Wanapi Dolomite Member and Mount Davenport Diamictite Member.|||
12639|Mount Doreen Formation|68276|6|Mentioned|p73-74|||Ngalia Basin. The barite-rich horizon is overlain by the Red Shale Member.|||Red Shale Member.||Glaciogenic deposits, overlain by seafloor barite associated with ferruginous domal stromatolites.|
12639|Mount Doreen Formation|68277|6|Mentioned|p95|Neoproterozoic|Neoproterozoic|The rank is not given in the text.||||||
12639|Mount Doreen Formation|69437|5|Briefly described|p22:4-5, 7|Ediacaran|Cryogenian|Ngalia Basin, Centralian A Superbasin. Supersequence 3.|||||Diamictite, dolomudstone and shale.|12-JUL-16
12639|Mount Doreen Formation|69438|6|Mentioned|p23:17|||The diamictite member of this unit has been correlated with the Olympic Formation (Amadeus Basin).||||||12-JUL-16
12639|Mount Doreen Formation|69439|4|Described|p24:2-10, 13-14, 16, 18, 20-21|Ediacaran|Ediacaran|Well et al. (1968). Ngalia Basin, Centralian A Superbasin. Supersequence 3. Recessive unit. 100-?350m thick. A complete section is exposed in the Patmungala Syncline, Naburula Hills. Is overlain unconformably by Djagamara Formation and Mount Eclipse Sandstone. Hosts subeconomic amounts of fluorite c.1.6km N of Mount Djagamara. "Oily slicks" were reported from drilling mud during coring of this unit.|||Mount Davenport Diamictite, Wanapi Dolostone, Newhaven Shale, Members.|Unconformably overlies Albinia Formation, Eva Springs Member (Vaughan Springs Quartzite) and (probably) Naburula Formation. Overlies Rinkabeena Shale (probably) disconformably.|Glacial deposits: predominantly diamictite, with subordinate dolostone and shale.|12-JUL-16
12639|Mount Doreen Formation|69443|5|Briefly described|p28:8, 10|||Ngalia Basin. Glacigene and post-glacial deposits related to the Elatina (previously Marinoan) glaciation. Correlates with part of the Mopunga Group (Georgina Basin).||||Equivalent to Keepera Group (Georgina Basin).||12-JUL-16
12639|Mount Doreen Formation|69673|5|Briefly described|p106, p107 fig 85|||Up to 350m thick.|||Includes Mount Davenport Diamictite Member, Wanapi Dolostone Member, Newhaven Shale Member|Overlies Rinkabeena Shale, overlain by Yuendumu Sandstone|Diamictite with subordinate dolostone and shale.|
12639|Mount Doreen Formation|72516|6|Mentioned|p87|Ediacaran|Ediacaran|Ngalia Basin. Age assumed from equivalence with Oorabra Arkose.||||Equivalent to the Oorabra Arkose.||02-JUN-21
12639|Mount Doreen Formation|73086|6|Mentioned|p101, p113, p122, p167|||Ngalia Basin. Upper red shale member may correlate to Pertatataka Formation. Diamictite member correlates with Olympic Formation.||||Correlates to Olympic Formation and Pertatataka Formation.||
12672|Mount Eclipse Sandstone|9380|5|Briefly described|Map Legend|Paleozoic|Paleozoic|Geological Province: Ngalia Basin. Sandstone, pebbly sandstone, conglomerate.||||||07-NOV-08
12672|Mount Eclipse Sandstone|22650|6|Mentioned|p 166||Early Carboniferous|Geological Province - Ngalia Basin||||||09-NOV-06
12672|Mount Eclipse Sandstone|22760|5|Briefly described|p345|||Geological Provience - Ngalia Basin.  Mount spelt Mt in text.  Plant fossils are preserved in this unit.||||||
12672|Mount Eclipse Sandstone|22761|6|Mentioned|p359|Middle Devonian|Late Devonian|Geological Province - Ngalia Basin.||||||
12672|Mount Eclipse Sandstone|22804|5|Briefly described|p454|||||||||
12672|Mount Eclipse Sandstone|22824|6|Mentioned|p526|Carboniferous|Devonian|Geological Province - Ngalia Basin.  Mount is spelt Mt in text.||||||
12672|Mount Eclipse Sandstone|23270|5|Briefly described|Table 1, p3||Paleozoic|Late Devonian to Early Carboniferous plant fossil assemblage. of Ngalia Basin.||||||07-NOV-08
12672|Mount Eclipse Sandstone|23271|5|Briefly described|Map legend||Paleozoic|In the Ngalia Basin.||||||23-DEC-09
12672|Mount Eclipse Sandstone|23621|5|Briefly described|p36|||Geological Province: Ngalia Basin.||||||
12672|Mount Eclipse Sandstone|23858|5|Briefly described|p916|Carboniferous|Devonian|Mount is Mt. in text. Geological Province: Ngalia Basin.||||||
12672|Mount Eclipse Sandstone|24064|4|Described|p227|Carboniferous|Carboniferous|Geological Province: Ngalia Basin. Maximum thicknes: 2400m.||||||
12672|Mount Eclipse Sandstone|24111|5|Briefly described|p218|Carboniferous|Carboniferous|Geological Province: Ngalia Basin.  See also p215 Fig. 11.||||||
12672|Mount Eclipse Sandstone|24334|5|Briefly described|p48 Tb.1|Visean|Visean|Age: 350-339 Ma. Mount is Mt. in text.||||||09-NOV-06
12672|Mount Eclipse Sandstone|24424|5|Briefly described|p539 Tb.4|Visean|Visean|Age: 330-343 Ma. Palaeomagnetic poles given. Mount written Mt in text.||||||04-FEB-05
12672|Mount Eclipse Sandstone|30258|6|Mentioned|Fig.2|||Carboniferous age||||||
12672|Mount Eclipse Sandstone|30684|4|Described|p10|||Carboniferous age||||||
12672|Mount Eclipse Sandstone|31454|4|Described|p30|||Refers uranium mineralisation. See also p31-32.||||||09-NOV-06
12672|Mount Eclipse Sandstone|32469|6|Mentioned|p531|||See also p532.||||||09-NOV-06
12672|Mount Eclipse Sandstone|32640|6|Mentioned|p237|||||||||
12672|Mount Eclipse Sandstone|32865|6|Mentioned|p482|||Carb.||||||
12672|Mount Eclipse Sandstone|33757|3|Fully described|p9|||See also Table 2.||||||09-NOV-06
12672|Mount Eclipse Sandstone|33758|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
12672|Mount Eclipse Sandstone|33760|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
12672|Mount Eclipse Sandstone|33761|6|Mentioned|p145|||Carb. See also p148.||||||09-NOV-06
12672|Mount Eclipse Sandstone|36473|6|Mentioned|Map legend|Carboniferous|Devonian|Between Carboniferous and Devonian||||||
12672|Mount Eclipse Sandstone|37025|6|Mentioned|Map|||Map legend comments.||||||
12672|Mount Eclipse Sandstone|37537|5|Briefly described|Map legend|Carboniferous|Devonian|Arkosic, coarse, massive, red-brown sandstone; subgreywacke, cobble and boulder conglomerate; red and green micaceous siltstone and shale. Geological Province: Ngalia Basin.||||||14-FEB-06
12672|Mount Eclipse Sandstone|38277|6|Mentioned|p154|||||||||
12672|Mount Eclipse Sandstone|38557|5|Briefly described|p292|||||||||
12672|Mount Eclipse Sandstone|39565|6|Mentioned|p33|||||||||
12672|Mount Eclipse Sandstone|40906|6|Mentioned|Fig.11|||||||||
12672|Mount Eclipse Sandstone|41125|6|Mentioned|p38|||See also Fig.24||||||
12672|Mount Eclipse Sandstone|41270|6|Mentioned|p278|||||||||
12672|Mount Eclipse Sandstone|41492|6|Mentioned|Fig.10|||||||||
12672|Mount Eclipse Sandstone|41717|5|Briefly described|p361|||||||||
12672|Mount Eclipse Sandstone|42059|5|Briefly described|Fig.2 P131|||||||||
12672|Mount Eclipse Sandstone|42141|6|Mentioned|p568|||||||||
12672|Mount Eclipse Sandstone|42504|5|Briefly described|p84|||||||||
12672|Mount Eclipse Sandstone|42547|4|Described|P 59|||Mount is Mt in text.||||||09-NOV-06
12672|Mount Eclipse Sandstone|42775|6|Mentioned|p327|||||||||
12672|Mount Eclipse Sandstone|42783|5|Briefly described|p473|||||||||
12672|Mount Eclipse Sandstone|43275|5|Briefly described|Map Legend||Carboniferous|||||||
12672|Mount Eclipse Sandstone|43631|3|Fully described|p26,27|Carboniferous|Devonian|||||||
12672|Mount Eclipse Sandstone|43749|6|Mentioned|Fig.1,p6|Carboniferous|Late Devonian|||||||
12672|Mount Eclipse Sandstone|44158|4|Described|p33 Table.2|Carboniferous|Carboniferous|In the Ngalia Basin.||||||09-NOV-06
12672|Mount Eclipse Sandstone|45097|6|Mentioned|p28|||Plant fossils? Late Carb. Correlation chart||||||
12672|Mount Eclipse Sandstone|45148|6|Mentioned|p20|||||||||
12672|Mount Eclipse Sandstone|45155|2|Defined|p38|Carboniferous|Late Devonian|Devonian - Carboniferous||||||
12672|Mount Eclipse Sandstone|45168|6|Mentioned|p6|||||||||
12672|Mount Eclipse Sandstone|46830|6|Mentioned|p32|||||||||
12672|Mount Eclipse Sandstone|46849|6|Mentioned|p185|||||||||
12672|Mount Eclipse Sandstone|61385|5|Briefly described|Map legend|Carboniferous|Carboniferous|Arkosic sandstone and conglomeratic sandstone, greywacke, minor conglomerate; plant and trace fossils. Geological Province: unnamed Palaeozoic basin.||||||16-DEC-11
12672|Mount Eclipse Sandstone|61768|6|Mentioned|p81, p86||Visean|||||||
12672|Mount Eclipse Sandstone|64068|5|Briefly described|p8|Middle Carboniferous|Middle Carboniferous|Ngalia Basin. Unconformity at its top. A primary paleopole from this unit at 340 Ma immediately preceded a 90 degree turn in APWP.||||||
12672|Mount Eclipse Sandstone|65107|6|Mentioned|Fig 1, p276|Carboniferous|Carboniferous|Mount spelt Mt, This unit helped constrain the Late Paleozoic pole path for the New England orogen.||||||
12672|Mount Eclipse Sandstone|65232|5|Briefly described|p9, p70, p71 Fig. 43, App. 2|Lower Carboniferous|Upper Devonian|Age: 350-370 Ma marked start of deposition of the youngest unit preserved in the Ngalia Basin. Sandstone-type uranium mineralisation. Feldspathic sandstone, conglomerate lenses, carbonate cement, and carbonaceous material. Geol. Prov: Ngalia Basin.||||||09-FEB-10
12672|Mount Eclipse Sandstone|65233|5|Briefly described|p13|||Geological province: Ngalia Basin.  Synorogenic deposition.||||||07-FEB-11
12672|Mount Eclipse Sandstone|65329|5|Briefly described|Map legend|Palaeozoic|Palaeozoic|Of Ngalia Basin. Younger than Kerridy Sandstone. Arkosic sandstone, conglomerate, overlies undivided sedimentary rocks||||||02-FEB-10
12672|Mount Eclipse Sandstone|65330|5|Briefly described|Map legend|Palaeozoic|Palaeozoic|Of Ngalia Basin. Younger than Kerridy Sandstone. Arkosic sandstone, conglomerate, overlies undivided sedimentary rocks||||||02-FEB-10
12672|Mount Eclipse Sandstone|65338|6|Mentioned|p59.|||||||Unconformably overlies Vaughan Springs Quartzite.||
12672|Mount Eclipse Sandstone|65342|6|Mentioned|p6.|||Ngalia Basin. Max. thickness at least 997 m.||||Overlies Kerridy Sandstone.||
12672|Mount Eclipse Sandstone|65343|5|Briefly described|p3 Fig.4|Carboniferous|Carboniferous|Ngalia Basin.||||||
12672|Mount Eclipse Sandstone|65382|5|Briefly described|p711, 713, 715, p712 Fig.1,  p717 App. 2|Visean|latest Devonian|Ngalia Basin. Palynomorphs of the Anapiculatisporites largus Assemblage indicating a Visean age occur in the upper part of the formation. Correlated with Ducabrook Formation, Drummond Basin||||||
12672|Mount Eclipse Sandstone|66767|6|Mentioned|p61|Carboniferous|Carboniferous|Ngalia Basin. Foreland sedimentary rocks derived from the thrust-generated topography to the NW.||||||
12672|Mount Eclipse Sandstone|67028|6|Mentioned|p370 Fig.7, p371 Tb. 5|Carboniferous|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)|310-345 Ma magnetic age range|||||24-APR-12
12672|Mount Eclipse Sandstone|67565|6|Mentioned|p5 Fig.3.|||Ngalia Basin.||||||
12672|Mount Eclipse Sandstone|67872|4|Described|p8, p11, p13, p15-18, p35, p37, p39-61|Early Carboniferous|Late Devonian|See also p39-p66, p71-73, p85, p94. Wells and Moss (1983). Ngalia Basin. Deposited during the Alice Springs Orogeny. Fluvial channel and floodplain deposits: distal alluvial fans. Crops out as (sandstone) ridges separated by (mudstone) depressions. Part of the M6 mega-sequence of Lindsay (2002). Sourced from volcanic arc granites (Carrington Granitic Suite). Hosts Bigrlyi, Walbiri and Minerva uranium deposits: Bigrlyi described in great detail. Seismic interpretations. Appears as Mt Eclipse Formation on p40 and as Mt Eclipse Sandstones on p41. Sedimentological characteristics described in great detail. Drill core correlation. Petrology detailed: thin sections illustrated. C, O and Sr isotopes detailed.|||||Mainly medium- to coarse-grained arkosic sandstone and sub-greywacke with interbedded conglomerate and subordinate siltstones and shale. Carbonate-cemented sandstones are distributed heterogeneously throughout.|17-APR-18
12672|Mount Eclipse Sandstone|68295|6|Mentioned|p28-29 Fig. 2.2|Carboniferous|Carboniferous|Li et al. (1989).||||||
12672|Mount Eclipse Sandstone|68998|5|Briefly described|vi, p1, p28-31, Appendix Tb.10|Carboniferous|Late Devonian|Ngalia Basin. Contains a detrital zircon age spectrum from Archaean to Neoproterozoic. Diverse source areas listed. Geochronology is discussed.|562 +/- 6 Ma (maximum depositional age).||||Interbedded fine- to medium-grained sandstone, fine-grained sandstone to clay and medium- to coarse-grained, subarkosic laminated sandstone.|30-JUN-20
12672|Mount Eclipse Sandstone|69418|5|Briefly described|p3:17, 37|Carboniferous|Carboniferous|Ngalia Basin. Hosts the Malawiri, Minerva and Walbiri sandstone-type U deposits (described). A shallow gas flow has been recorded from this unit.||||||12-JUL-16
12672|Mount Eclipse Sandstone|69427|6|Mentioned|p12:48-49|Carboniferous|Carboniferous|Ngalia Basin. Sediment was derived from thrust-generated topography to the NW.||||||12-JUL-16
12672|Mount Eclipse Sandstone|69437|6|Mentioned|p22:15|||Ngalia Basin. May have petroleum source rock and reservoir potential.||||||12-JUL-16
12672|Mount Eclipse Sandstone|69438|5|Briefly described|p23:46, 48|Carboniferous|Devonian|Ngalia Basin. Foreland sedimentation deformed by the Eclipse Event.||||||12-JUL-16
12672|Mount Eclipse Sandstone|69439|4|Described|p24:2-6, 8, 10-14, 16-22|Carboniferous|Late Devonian|Widely exposed across the Ngalia Basin. Forms strike ridges and isolated cuestas and mesas. Over 3000m thick. Fluvial and piedmont foreland basin deposits. Deposition occurred during the Alice Springs Orogeny. Deformed during the Eclipse Event: strata are vertical to overturned in places. Contains palynomorphs and plant fossils (Lepidodendron sp and Triphyllopteris austrina Morris). Hosts uranium (-vanadium) occurrences (eg Bigrlyi, Walbiri, Minerva/Malawiri and others). Deposition of this unit possibly assisted hydrocarbon generation in the Basin. Possible hydrocarbon source rock: associated with very minor gas flows. Contains potential reservoirs.||||Overlies Eva Springs Member (Vaughan Springs Quartzite) conformably or disconformably, and Mount Doreen and Bloodwood Formations, and Kerridy Sandstone, unconformably.|Coarse-grained, poorly sorted, thinly bedded to massive arkosic sandstone; lesser subgreywacke, minor cobble and pebble conglomerate, rare thin lenses of dolomudstone; red or green siltstone and shale. Local significant carbonaceous material.|12-JUL-16
12672|Mount Eclipse Sandstone|69673|4|Described|p107 fig 85, p108, p109, p110|||Greater than 3000m thick, hosts uranium mineralisation throughout.||||Overlies Kerridy Sandstone|Arkosic sandstone, subgreywacke, minor cobble and pebble conglomerate, rare thin lenses of dolomudstone, siltstone and shale with conglomeratic lenses near the base of the formation.|
12672|Mount Eclipse Sandstone|69791|5|Briefly described|p1081-1093|Carboniferous|Late Devonian|Ngalia Basin. A basin-wide host to uranium  mineralisation. Thickness to c.2400m. Crops out vertically, forming ridges; the mudstones are commonly eroded into depressions. Mineralogy, petrography and diagenesis detailed. The grey sandstone unit which hosts the uranium is c.100m thick and is capped by a thick mudstone unit.|||||Immature, kaolinised, medium-grained subarkosic sandstones with patchy calcite cement; mudstones; basal boulder conglomerate.|
12672|Mount Eclipse Sandstone|69948|6|Mentioned|Fig.4.5|Carboniferous|Carboniferous|Haines et al. (2001). Ngalia Basin. Syn-orogenic.||||||
12672|Mount Eclipse Sandstone|71342|6|Mentioned|Ch4 p12|||||||||
12764|Mount Gordon Sandstone|14019|5|Briefly described|p4 Fig. 3|||Of the Bullita Group.  Geological Province: Victoria Basin.||||||
12764|Mount Gordon Sandstone|24122|5|Briefly described|p4 Fig.3|||Of Bullita Group. Mount is Mt. in text.  Geological Province: Victoria Basin.||||||
12764|Mount Gordon Sandstone|24441|5|Briefly described|p1 Fig. 1|Mesoproterozoic|Mesoproterozoic|Of the Bullita Group. Unconformably overlies Nero Siltstone and Bynoe Formation;  overlain by Battle Creek Formation. Geological Province: Victoria Basin. Mount is Mt in text.||||||25-JAN-06
12764|Mount Gordon Sandstone|24442|5|Briefly described|p50 Fig. 1|||Of the Bullita Group. Geological Province: Victoria Basin.  Mount is Mt in text of figure.||||||
12764|Mount Gordon Sandstone|30003|4|Described|p7, p13|||Blocky white to yellow medium-bedded fine to medium quartz sandstone. Conformably overlies the Nero Siltstone. Max. thickness: 11m.Carpentarian or Adelaidean.||||||19-APR-05
12764|Mount Gordon Sandstone|30004|6|Mentioned|Map legend|Proterozoic|Proterozoic|Carpentarian or Adelaidean||||||
12764|Mount Gordon Sandstone|32660|5|Briefly described|Table 6|||||||||
12764|Mount Gordon Sandstone|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
12764|Mount Gordon Sandstone|45112|5|Briefly described|Table 10|||||||||
12764|Mount Gordon Sandstone|48943|2|Defined|p68|Proterozoic|Proterozoic|?Adelaidean||||||
12764|Mount Gordon Sandstone|60672|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Blocky, medium quartz sandstone. Of Bullita Group. Geological Province: Victoria Basin.||||||
12764|Mount Gordon Sandstone|65342|6|Mentioned|p11 Fig.13. |||Victoria Basin.||Unit in Bullita Group.||Is overlain by Battle Creek Formation.||
12764|Mount Gordon Sandstone|69432|4|Described|p17:2, 11-12|||Birrindudu Basin. Described as "poorly documented". 11m thick. Contradictory relationships with the Nero Siltstone are given. Is a lithostratigraphic correlative of either the upper or lower Weaner Sandstone and is possibly synonymous with it.||Bullita Group.||Overlies Bynoe Formation unconformably and Nero Siltstone either "with apparent conformity" or "unconformably". Is overlain by Battle Creek Formation.|Blocky, white to yellow, medium-bedded, fine to medium quartz sandstone.|12-JUL-16
12764|Mount Gordon Sandstone|69673|6|Mentioned|p48 fig 35|||||Bullita Group||Unconformably overlies Nero Siltstone, Bynoe Formation, overlain by Battle Creek Formation||
12764|Mount Gordon Sandstone|70854|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Bullita Group.||Overlies Nero Siltstone. Is overlain unconformably by Wondoan Hill Formation (Tijunna Group).|Blocky, medium quartz sandstone.|
12764|Mount Gordon Sandstone|70968|5|Briefly described|p115|||||Bullita Group.||Is overlain unconformably by Wondoan Hill Formation.||
12764|Mount Gordon Sandstone|71302|5|Briefly described|p6||Paleoproterozoic|Of Birindudu Basin.||Unit of Bullita Group.||||
12780|Mount Harris Basalt|22561|4|Described|p15|Neoproterozoic|Neoproterozoic|||||||
12780|Mount Harris Basalt|22567|6|Mentioned|p91|||||||||
12780|Mount Harris Basalt|22804|6|Mentioned|Fig 2 on p432|||Mount spelt Mt in text.||||||
12780|Mount Harris Basalt|23361|5|Briefly described|16 Fig.4|Neoproterozoic|Neoproterozoic|||||||
12780|Mount Harris Basalt|24496|5|Briefly described|p15|Mesoproterozoic|Mesoproterozoic|Of Tjauwata Group. Mount written Mt in text. Geological Province: Musgrave Block.||||||
12780|Mount Harris Basalt|30389|6|Mentioned|p9|||Refers Forman(1966)||||||
12780|Mount Harris Basalt|30390|6|Mentioned|p195|||||||||
12780|Mount Harris Basalt|30817|6|Mentioned|p11|||||||||
12780|Mount Harris Basalt|31393|6|Mentioned|Pl.25|||||||||
12780|Mount Harris Basalt|31970|6|Mentioned|p15|||||||||
12780|Mount Harris Basalt|33307|6|Mentioned|Fig.6|||||||||
12780|Mount Harris Basalt|33478|6|Mentioned|Table 1|||||||||
12780|Mount Harris Basalt|35102|6|Mentioned|Fig.2|||||||||
12780|Mount Harris Basalt|35308|6|Mentioned|Table 1|||||||||
12780|Mount Harris Basalt|36473|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
12780|Mount Harris Basalt|36887|6|Mentioned|p208|||||||||
12780|Mount Harris Basalt|39210|6|Mentioned|p40|||See also Fig.10.||||||09-NOV-06
12780|Mount Harris Basalt|39213|6|Mentioned|Fig.6|||Amadeus Basin Succession.||||||09-NOV-06
12780|Mount Harris Basalt|42504|5|Briefly described|p67|||||||||
12780|Mount Harris Basalt|42940|5|Briefly described|Plate 2|Mesoproterozoic|Paleoproterozoic|In the south-west.  Greenschist, basalt, tuff, conglomerate, quartzite.  Geological province: Amadeus Basin.||||||07-NOV-08
12780|Mount Harris Basalt|43503|6|Mentioned|12-50||Proterozoic|||||||
12780|Mount Harris Basalt|44139|6|Mentioned|p284|||Of Forman, 1966. Later Mount Harris Volcanics (Daniels, 1974); see references p284-286.|| ||||05-MAR-18
12780|Mount Harris Basalt|44493|4|Described|p.7, map||Precambrian|BLOOD RANGE sheet (G53-3). See p.9-12,14, for details. PreC.||||||09-NOV-06
12780|Mount Harris Basalt|44494|14|Not recorded|map legend|||||||||
12780|Mount Harris Basalt|45041|5|Briefly described|p15|||Precambrian||||||
12780|Mount Harris Basalt|48863|14|Not recorded|p.13|||||||||
12780|Mount Harris Basalt|48864|2|Defined|p.9,11-12||Proterozoic|Tb.1. On many pages. p.1,14,18,20-23,37,41,42,47,50,Pl.2,11,12. Middle or Upper Proterozoic. (G52-3,7).||||||
12780|Mount Harris Basalt|48963|6|Mentioned|Fig.3|||||||||
12780|Mount Harris Basalt|50286|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Underlies Dean Quartzite.  Of the Tjauwata Group.||||||22-DEC-09
12780|Mount Harris Basalt|50321|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group.  Intruded by Walu Granite.||||||09-JUN-04
12780|Mount Harris Basalt|60678|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group.  Variably silicified and epidotised, amygdaloidal basalt.  Geological Province: Musgrave Block.||||||
12780|Mount Harris Basalt|60679|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Basalt. Geological Province: Musgrave Block. Of Tjauwata Group.||||||14-JAN-05
12780|Mount Harris Basalt|60683|6|Mentioned|p7|Mesoproterozoic|Mesoproterozoic|Age: 1070-1040Ma.  Geological Province: Musgrave Block. Mount may be Mt in text.||||||20-APR-05
12780|Mount Harris Basalt|61154|5|Briefly described|p16, p18 Fig. 10|Mesoproterozoic|Mesoproterozoic|Of Tjauwata Gp. Distinctively banded rock due to alternating layers silicified and epidotised amygdaloidal basalt with less altered basalt. Over Tjuninanta Fn; under Puntitjata Rhyolite. Intruded by veins of Walu Granite. Thick: 1-2km (est.). Mount is Mt||||||19-JUL-05
12780|Mount Harris Basalt|61309|5|Briefly described|p16 Fig. 4|||Geological Province: Amadeus Basin. Mount is Mt in text.||||||06-FEB-08
12780|Mount Harris Basalt|61386|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group. Variably silicified and epidotised amygdaloidal basalt with rare lenses of crystalline quartz sandstone.||||||23-DEC-09
12780|Mount Harris Basalt|62359|5|Briefly described|p547, p549|||Underlies Dean Quartzite. Geological Province: Amadeus Basin. Basaltic bimodal volcanics. Mount may be Mt in text.||||||
12780|Mount Harris Basalt|62609|5|Briefly described|Map Legend|Precambrian|Precambrian|Green Schist, basalt, tuff, conglomerate, quartzite.||||||
12780|Mount Harris Basalt|62620|5|Briefly described|Map Legend|Precambrian|Precambrian|Green schist, basalt, tuff, conglomerate, quartzite.||||||
12780|Mount Harris Basalt|62989|5|Briefly described|p39|Mesoproterozoic|Mesoproterozoic|Of Tjauwata Gp. Overlies Tjuninanta Fm. Max. thick:2km. Accumulated basalt flows. Geochemically similar to Mummawarrawarra Basalt (Tollu Group), Alcurra dolerite and Giles Complex rocks; interpreted as extrusive phase of the Giles Complex. Age: 1080Ma.||||||07-FEB-08
12780|Mount Harris Basalt|63562|6|Mentioned|p341|||Of Amadeus Basin. Part of the initial Basin fill.||Tjauwata Group||Correlated with Stuart Dyke Swarm.||
12780|Mount Harris Basalt|63866|5|Briefly described|p203, p208|||Mulga Park Domain, Musgrave Province.||Tjauwata Group||Overlain by the Puntitjata Rhyolite. Intruded by the Walu Granite.||
12780|Mount Harris Basalt|64580|4|Described|map legend||Mesoproterozoic|Of Tjauwata Group. Metamorphosed basalt, basaltic tuff, conglomerate, and quartzite.||||||09-DEC-08
12780|Mount Harris Basalt|65233|5|Briefly described|p2|Mesoproterozoic|Mesoproterozoic|Overlies Tjuninanta Formation; overlain by Bloods Range Formation. Age: 1080Ma. Max. thickness: 2km. Geological province: Amadeus Basin. Basaltic flows.||||||07-FEB-11
12780|Mount Harris Basalt|65256|1|Redefined|p3, p6 Tb.1, p9-11, p20, p27, p37-39|Stenian|Stenian|Redefined. Estimated to be 1-2 km thick minimum. Correlative of Mummawarrawarra Basalt; intruded by Walu Granite and Alcurra dolerite. Largely non-magnetic; associated with shallow Cenozoic and Quaternary soils; interpreted magmatic age of 1080 Ma. Similar in composition to Alcurra dolerite. Forms rounded low hills and peneplains.||Of the Tjauwata Group.||Overlies Tjuninanta Formation (gradational contact), and Karukali Quartzite. Overlain by Puntitjata Rhyolite or Bloods Range Formation.|Amygdaloidal basalt with layered altered (epidotised and silicified) and unaltered zones and with rare crystalline quartz sandstone interbeds; no quartz-feldspar porphyry subunit.|19-MAY-14
12780|Mount Harris Basalt|65906|6|Mentioned|p6|Mesoproterozoic|Mesoproterozoic|Unit in Tjauwata Group. A correlative of Mummawarrawarra Basalt.  Is intruded by  Walu Granite aged 1084 +/- 9 Ma (SHRIMP U-Pb zircon).||||||
12780|Mount Harris Basalt|67128|5|Briefly described|p12, p18|||||Tjauwata Group.||Is intruded by Walu Granite. Correlated (tentatively) with Mummawarrawarra Basalt.||
12780|Mount Harris Basalt|68995|6|Mentioned|p6|||||Tjauwata Group||||
12780|Mount Harris Basalt|69091|5|Briefly described|p70, p103 Fig.5.6|||These are basal units of Bentley Supergroup (Howard et al., 2011a; Evins et al., 2010).||Tjauwata Group||Equivalent to Mummawarrawarra Basalt (of Kunmarnara Group).||07-OCT-14
12780|Mount Harris Basalt|69153|5|Briefly described|500k_geologyp08_lut.csv||Mesoproterozoic|||Tjauwata Group|||Metamorphosed basalt, basaltic tuff, conglomerate, and quartzite|
12780|Mount Harris Basalt|69436|4|Described|p21:4, 11, 13-14, 19, 21|Mesoproterozoic|Mesoproterozoic|Forman (1966). Musgrave Province. Origin of magma discussed; similar geochemistry as Alcurra Dolerite suggests a common source. Very thick: estimated at 1-2 km. Is locally thrust over Dean Quartzite. Contains a quartz vein with Au, Ag and secondary lead and copper minerals.||Tjauwata Group.||Overlies Tjuninanta Formation. Is overlain by, or laterally equivalent to, Puntitjata Rhyolite. Is intruded by Walu Granite. Correlated with Mummawarrawarra Basalt.|Distinctively banded basalts, due to alternating layers of silicified and epidotised amygdaloidal basalt with less altered basalt. Fe-tholeiites.|12-JUL-16
12780|Mount Harris Basalt|69729|5|Briefly described|p79|||||Tjauwata Group.||Equivalent to the Mummawarrawarra Basalt.||
12780|Mount Harris Basalt|70018|4|Described|p233,235-237|Mesoproterozoic|Mesoproterozoic|Amadeus Basin. Minimum age provided by the 1084+\-9 Ma age of high level granites that intrude it (U-Pb on zircon; Close et al., 2003).||Unit of Tjauwata Group.||Overlain by, or laterally equivalent to Puntitjata Rhyolite. Underlain by Tjuninanta Formation.|Epidotised, silicified amygloidal basalt flows, rare quartz sandstone beds.|
12780|Mount Harris Basalt|70634|4|Described|500k_geolgyp08_lut.csv|Mesoproterozoic|Mesoproterozoic|||Tjauwata Group|||Metamorphosed basalt, basaltic tuff, conglomerate, and quartzite.|
12780|Mount Harris Basalt|70793|4|Described|500k_interpgeop14_lut.csv|Mesoproterozoic|Mesoproterozoic|Geological province: Paterson Orogen, Musgrave Province. Of Bentley Basin. Events: Giles Event (1085-1040 Ma); Areyonga Movement; Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Alice Springs Orogeny (450-295 Ma).|1085-1040 Ma (inferred)|Unit of Tjauwata Group.|||Metamorphosed siliciclastic sedimentary and volcanic rocks|
12780|Mount Harris Basalt|71210|6|Mentioned|p8|||||Tjauwata Group||||
12780|Mount Harris Basalt|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||greenschist facies rock, basalt|
12780|Mount Harris Basalt|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). See 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 1m_geologyp12_lut.csv, 500k_interpgeop16_lut.csv.|1084-1075 Ma (inferred)|Unit of Tjauwata Group.|||Metamorphosed basalt, basaltic tuff, conglomerate, and quartzite|
12780|Mount Harris Basalt|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Tjauwata Group|||Metamorphosed basalt, basaltic tuff, conglomerate, and quartzite.|
12780|Mount Harris Basalt|72094|5|Briefly described|p17|Neoproterozoic|Neoproterozoic|Bentley Basin.||Unit of Tjauwata Group.||Conformably underlain by Karukali Quartzite. Likely time and lateral equivalent to Mummawarrawarra Basalt.||
12786|Mount Hay Granulite|23361|6|Mentioned|13 Fig.2|||||||||
12786|Mount Hay Granulite|23844|3|Fully described|p32|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Province. Max Thickness: 3000m. Part of the Narwietooma Metamorphic Complex (Warren and Shaw, 1995). See also Fig.14, 16, 17||||||07-NOV-08
12786|Mount Hay Granulite|24197|5|Briefly described|p59 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Of the Narwietooma Suite. Age: ~1880Ma. Geological Province: Arunta Inlier. Mount is Mt in text.||||||07-FEB-11
12786|Mount Hay Granulite|39566|6|Mentioned|Table 1|||||||||
12786|Mount Hay Granulite|43225|5|Briefly described|Map Legend||Paleoproterozoic|Of the Narwietooma Metamorphic Complex.||||||07-NOV-08
12786|Mount Hay Granulite|43503|1|Redefined|6,19,75|||||||||
12786|Mount Hay Granulite|44114|5|Briefly described|p321|||Central Arunta Inlier. Felsic to mafic extrusives and possible intrusives.|? >1880 Ma (Shaw, 1994).||||Felsic, felsic-intermediate, mafic-intermediate and mafic granulites and gneisses.|
12786|Mount Hay Granulite|50369|5|Briefly described|p1.3, 3.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Narwietooma Suite.||||||07-NOV-08
12786|Mount Hay Granulite|60668|5|Briefly described|p9, p2 Tb. 1|||Comprises dominantly mafic granulite, felsic and intermediate granulite whilst the remainder consists of anorthosite, migmatitic metasediments and various felsic rocks. Faulted against the Anburla Anorthosite.||||||
12786|Mount Hay Granulite|61309|6|Mentioned|p13 Fig. 2|||||||||
12786|Mount Hay Granulite|64735|5|Briefly described|p216||||~1820-1800 Ma.|||Intrudes Lander Package.||30-APR-12
12786|Mount Hay Granulite|64738|6|Mentioned|p247 Fig.1, p250 Table 1, p252-253, 259|Paleoproterozoic|Paleoproterozoic|Metamorphosed 1700 +/- 17 Ma. Also called the Mount Hay mafic granulite.|Protolith age of 1803 +/- 5 Ma.|||||
12786|Mount Hay Granulite|65338|5|Briefly described|p40.|Statherian|Orosirian|HERMANNSBURG area.|1803 +/- 5 Ma (Claoue-Long and Hoatson 2005).||||Metagabbro.|
12786|Mount Hay Granulite|66526|5|Briefly described|p36.|Proterozoic|Proterozoic|Aileron Province. The granulite and associated gabbro intrusions were produced in the Mount Hay Event, ME 9 in the Proterozoic Mafic-Ultramafic Magmatic Event Series.|c.1810 Ma.|||||
12786|Mount Hay Granulite|68150|5|Briefly described|p11 Tb.3.2|||Age: SHRIMP, MSWD 1.3, 10 analyses, Claoue-Long and Hoatson, 2005.|1700 +/- 17 Ma, metamorphism|||||
12786|Mount Hay Granulite|69427|4|Described|p12:3, 17-18, 20, 23-24, 29, 40, 59|Orosirian|Orosirian|Aileron Province. SHRIMP U-Pb zircon age of intrusion (of mafic component). Other ages given for other lithologies in the unit range from c.1819 Ma to c.1783 Ma. Similar dating of zircon rims identified metamorphism at 1700 +/- 17 Ma (Strangways Orogeny) and 1590 Ma (Chewings Orogeny). May have potential for Ni-Cu-Co mineralisation.|1805 +/- 3 Ma (Claoue-Long and Hoatson, 2005).|Narwietooma Metamorphic Complex.||Is faulted against the Anburla Anorthosite.|Dominated by mafic granulite (60%); felsic to intermediate granulite, lesser anorthosite and migmatitic metasedimentary rock; minor charnockite, leucogranite and pegmatite.|12-JUL-16
12786|Mount Hay Granulite|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen. Metamorphosed at 1700 +/- 17 Ma (U-Pb zircon SHRIMP).|1803+/-5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Mafic granulite.|
12786|Mount Hay Granulite|72894|6|Mentioned|p19|||||Narwietooma Metamorphic Complex|||Dominated by mafic granulite|
12792|Mount Hendry Formation|22954|6|Mentioned|Fig3p9|Middle Cambrian|Early Cambrian|||||||
12792|Mount Hendry Formation|23031|4|Described|30|||Geological  province: Georgina Basin.||||||09-NOV-06
12792|Mount Hendry Formation|23393|5|Briefly described|p23 Fig. 6|Middle Cambrian|Early Cambrian|Mount is Mt. in text of figure.  Geological Province: Georgina Basin.||||||
12792|Mount Hendry Formation|23986|5|Briefly described|p68|||Mount is Mt. in text.||||||
12792|Mount Hendry Formation|30479|6|Mentioned|Fig.7|||Lower Cambrian age||||||
12792|Mount Hendry Formation|30914|6|Mentioned|Map legend|Early Cambrian|Proterozoic|Proterozoic - Early Cambrian||||||
12792|Mount Hendry Formation|33482|6|Mentioned|p6|||Lower Middle Cambrian||||||
12792|Mount Hendry Formation|35001|6|Mentioned|Fig.45|||||||||
12792|Mount Hendry Formation|35054|6|Mentioned|p246|||||||||
12792|Mount Hendry Formation|36448|6|Mentioned|Fig.1|||||||||
12792|Mount Hendry Formation|38209|5|Briefly described|Fig.1|||||||||
12792|Mount Hendry Formation|38446|6|Mentioned|p144|||||||||
12792|Mount Hendry Formation|39445|5|Briefly described|Table 4|||See also p61 and p62.||||||09-NOV-06
12792|Mount Hendry Formation|39690|6|Mentioned|Table 1|||||||||
12792|Mount Hendry Formation|40004|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
12792|Mount Hendry Formation|40221|4|Described|p19|||Mention p6.||||||09-NOV-06
12792|Mount Hendry Formation|40386|6|Mentioned|Fig.1|||||||||
12792|Mount Hendry Formation|40686|6|Mentioned|Fig.3|||||||||
12792|Mount Hendry Formation|40852|5|Briefly described|p38|||||||||
12792|Mount Hendry Formation|40855|6|Mentioned|Fig.24.1|||||||||
12792|Mount Hendry Formation|40856|6|Mentioned|Fig.23.6|||||||||
12792|Mount Hendry Formation|40858|5|Briefly described|p132|||||||||
12792|Mount Hendry Formation|41129|6|Mentioned|Fig.8|||||||||
12792|Mount Hendry Formation|41240|6|Mentioned|p112|||||||||
12792|Mount Hendry Formation|41388|6|Mentioned|Fig.2|||||||||
12792|Mount Hendry Formation|45079|5|Briefly described|p10|||Recommends term be discontinued. See p16.||||||09-NOV-06
12792|Mount Hendry Formation|47058|6|Mentioned|Fig.4 P124|||||||||
12792|Mount Hendry Formation|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Early Cambrian|Neoproterozoic|Georgina Basin||Narpa Group|||Conglomerate, arenite, arkose, shale, mudstone, dolomite|
12792|Mount Hendry Formation|69591|5|Briefly described|p97, p98 Fig.2.91|Cambrian|Cambrian|Basal clastics of the Georgina Basin.||||Overlain by ?Thorntonia Limestone.||
12798|Mount Hooper Sandstone|35140|6|Mentioned|Fig.2|||||||||
12798|Mount Hooper Sandstone|35465|6|Mentioned|Fig.2|||Summary of positions of magnetic units in the Lower Proterozoic||||||
12798|Mount Hooper Sandstone|37462|6|Mentioned|Fig.4.8|||||||||
12798|Mount Hooper Sandstone|38239|6|Mentioned|Fig.2|||||||||
12798|Mount Hooper Sandstone|39069|5|Briefly described|Table 1|||||||||
12798|Mount Hooper Sandstone|40493|5|Briefly described|Table 1|||||||||
12798|Mount Hooper Sandstone|47049|6|Mentioned|Fig.2|||||||||
12798|Mount Hooper Sandstone|60550|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Mount Partridge Group. Interbedded medium quartz sandstone, arkosic sandstone, siltstone, meta-siltstone, phyllite, coarse quartzite and feldspathic quartzite, pebbly in places, with minor conglomerate beds.||||||
12816|Mount Ida Granite|23733|5|Briefly described|p34 Fig.20|||Mount is Mt.in text of figure.||||||
12816|Mount Ida Granite|24197|5|Briefly described|p60 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Of the Jinka Suite. Age: 1713Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
12816|Mount Ida Granite|39888|6|Mentioned|Fig.8|||||||||
12816|Mount Ida Granite|42326|5|Briefly described|Table 2 P11|||||||||
12816|Mount Ida Granite|50369|5|Briefly described|p1.4, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Jinka Suite.||||||07-NOV-08
12816|Mount Ida Granite|65341|6|Mentioned|p2 Fig.2. |Paleoproterozoic|Paleoproterozoic|||||||
12816|Mount Ida Granite|69917|6|Mentioned|p103|Statherian|Statherian|Thought to have been emplaced during the early part of the 1730-1690 Ma Strangways Event.||||Intrudes Copia Granite.||29-JUL-15
12816|Mount Ida Granite|69925|6|Mentioned|p39|||Huckitta-Alcoota area, Arunta Inlier.||||Correlated with Mount Swan Granite.||
12816|Mount Ida Granite|69931|6|Mentioned|p269, 275, 296|Paleoproterozoic|Paleoproterozoic|Arunta Inlier. Sm-Nd isotopic analyses tabulated.||Mount Swan Suite.|||Granite.|
12822|Mount Isa Group|22453|5|Briefly described|p 11|||NT and QLD||||||
12822|Mount Isa Group|22468|5|Briefly described|p 17|||||||||
12822|Mount Isa Group|22483|6|Mentioned|Table 2 p416.|||||||||
12822|Mount Isa Group|22498|5|Briefly described|Fig2 P235, Fig5|||||||||
12822|Mount Isa Group|22644|5|Briefly described|5|||Geological province: Mount Isa Basin. Underlain by Fiery Creek Volcanics.Of the Yaringa Metamorphics. Mount as 'Mt' in text||||||09-NOV-06
12822|Mount Isa Group|22665|6|Mentioned|P219, P227|||Mount actually spelt Mt||||||
12822|Mount Isa Group|22680|6|Mentioned|83|||Mount as 'Mt' in text||||||
12822|Mount Isa Group|22747|6|Mentioned|Table1,p7|||Part of Ploughed Mountain Beds equivalent to Mount Isa Group||||||
12822|Mount Isa Group|22955|6|Mentioned|160||Paleoproterozoic|||||||07-NOV-08
12822|Mount Isa Group|23031|5|Briefly described|21|Paleoproterozoic|Paleoproterozoic|Geological province: Leichardt Sub Province.||||||07-NOV-08
12822|Mount Isa Group|23072|6|Mentioned|p754|||||||||
12822|Mount Isa Group|23291|6|Mentioned|p24|||Geological Province: Georgetown Region.||||||08-JUL-15
12822|Mount Isa Group|23313|6|Mentioned|319 Fig. 6|||||||||
12822|Mount Isa Group|23362|6|Mentioned|337|||||||||
12822|Mount Isa Group|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Fold Belt.||||||07-NOV-08
12822|Mount Isa Group|23395|6|Mentioned|p383|||Mount is spelt Mt. in text.||||||
12822|Mount Isa Group|23397|5|Briefly described|p463|||Mount is Mt. in text.||||||
12822|Mount Isa Group|23398|4|Described|p454|||||||||
12822|Mount Isa Group|23399|4|Described|p485|||||||||
12822|Mount Isa Group|23408|5|Briefly described|p509, p511, p513 Fig. 2|||Previous interpretations of this group are included. Comprises Surprise Ck. Beds, Warrina Pk Quartzite, Mondarra Siltstone, Breakaway Shale, Native Bee Siltstone, Urquhart Shale, Spear and Kennedy Siltstones, Magazine Shale (Cavaney 1975).||||||15-JUN-09
12822|Mount Isa Group|23409|5|Briefly described|p536|||Isa Superbasin||||||
12822|Mount Isa Group|23447|5|Briefly described|p436|Proterozoic|Proterozoic|||||||
12822|Mount Isa Group|23448|5|Briefly described|p479|Statherian|Statherian|Age: 1670Ma.||||||09-NOV-06
12822|Mount Isa Group|23466|5|Briefly described|p269|||||||||
12822|Mount Isa Group|23518|4|Described|p9 Fig. 3, p12|Proterozoic|Proterozoic|Geological Province: Western Fold Belt.||||||
12822|Mount Isa Group|23554|6|Mentioned|pB34|||Geological Province: Mt Isa Inlier.||||||
12822|Mount Isa Group|23767|5|Briefly described|p1954 Fig. 1a|||Geological Province: Mount Isa Superbasin||||||
12822|Mount Isa Group|23957|6|Mentioned|p1123|||||||||
12822|Mount Isa Group|23961|6|Mentioned|p1191|||Geological Province: Mt Isa Inlier.||||||
12822|Mount Isa Group|23966|5|Briefly described|p1309|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier.   Age: 1653 +/- 7Ma.||||||
12822|Mount Isa Group|23969|6|Mentioned|p1371 Fig.2|||Mount is Mt. in text. Geological Province: Mount Isa Inlier.||||||
12822|Mount Isa Group|24254|6|Mentioned|p21|||||||||
12822|Mount Isa Group|24419|5|Briefly described|p14, p17, p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Includes Warrina Park Quartzite (basal unit), Moondarra Siltstone, Breakaway Shale and Native Bee Siltstone. Overlies Surprise Creek Formation.  Geological Province: Isa Superbasin. Equivalent to lower McNamara Group in Lawn Hill Subprovince.||||||07-NOV-08
12822|Mount Isa Group|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Overlies Lena Quartzite. Geological Province: Leichardt River Fault Trough.||||||
12822|Mount Isa Group|29969|6|Mentioned|p392|||||||||
12822|Mount Isa Group|30354|6|Mentioned|p9|||Refers to micro palaeontology||||||
12822|Mount Isa Group|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||25-AUG-04
12822|Mount Isa Group|30530|6|Mentioned|p515|||||||||
12822|Mount Isa Group|30531|6|Mentioned|p15|||Also mention P20 and P22.||||||
12822|Mount Isa Group|30534|6|Mentioned|p300|||See also P305||||||
12822|Mount Isa Group|30535|1|Redefined|p404|Carpentarian|Carpentarian|||||||
12822|Mount Isa Group|30723|5|Briefly described|p340|||||||||
12822|Mount Isa Group|30724|6|Mentioned|p73|||||||||
12822|Mount Isa Group|30725|5|Briefly described|p574|||||||||
12822|Mount Isa Group|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
12822|Mount Isa Group|31207|6|Mentioned|p1414|||||||||
12822|Mount Isa Group|31342|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
12822|Mount Isa Group|31421|6|Mentioned|p509|||||||||
12822|Mount Isa Group|31704|6|Mentioned|p5|||Minor Copper in shale association||||||
12822|Mount Isa Group|31821|6|Mentioned|p1023|||||||||
12822|Mount Isa Group|32041|4|Described|p353|||||||||
12822|Mount Isa Group|32042|5|Briefly described|p38|||||||||
12822|Mount Isa Group|32100|6|Mentioned|p273|||||||||
12822|Mount Isa Group|32144|6|Mentioned|p116|||Organic matter||||||
12822|Mount Isa Group|32211|6|Mentioned|p12|||Lower Proterozoic||||||
12822|Mount Isa Group|32376|6|Mentioned|p1541|||||||||
12822|Mount Isa Group|32466|6|Mentioned|p316|||||||||
12822|Mount Isa Group|32479|6|Mentioned|Fig.1|||||||||
12822|Mount Isa Group|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
12822|Mount Isa Group|32660|4|Described|Table 5|||||||||
12822|Mount Isa Group|32818|5|Briefly described|p17|||Age||||||
12822|Mount Isa Group|32951|6|Mentioned|Table 1|||||||||
12822|Mount Isa Group|32959|6|Mentioned|p31|||||||||
12822|Mount Isa Group|33111|6|Mentioned|p5|||||||||
12822|Mount Isa Group|33214|5|Briefly described|p1279|||Age discussed||||||
12822|Mount Isa Group|33791|6|Mentioned|p373|||||||||
12822|Mount Isa Group|33893|6|Mentioned|Table 1|||||||||
12822|Mount Isa Group|33894|6|Mentioned|Table 2|||||||||
12822|Mount Isa Group|33896|6|Mentioned|Fig.1|||||||||
12822|Mount Isa Group|33897|6|Mentioned|p1280|||||||||
12822|Mount Isa Group|33900|4|Described|p13|||Mention p4.||||||09-NOV-06
12822|Mount Isa Group|34499|4|Described|p226|||See Table 11.||||||09-NOV-06
12822|Mount Isa Group|34891|6|Mentioned|p240|||||||||
12822|Mount Isa Group|35001|6|Mentioned|p261|||||||||
12822|Mount Isa Group|35004|6|Mentioned|p266|||||||||
12822|Mount Isa Group|35074|6|Mentioned|Fig.2|||||||||
12822|Mount Isa Group|35114|6|Mentioned|p199|||||||||
12822|Mount Isa Group|35115|6|Mentioned|Fig.1|||||||||
12822|Mount Isa Group|35116|4|Described|p181|||See also p177 and Table 4.||||||09-NOV-06
12822|Mount Isa Group|35261|6|Mentioned|Fig.1|||||||||
12822|Mount Isa Group|35286|6|Mentioned|p158|||||||||
12822|Mount Isa Group|35309|6|Mentioned|p373|||||||||
12822|Mount Isa Group|35369|6|Mentioned|PB5|||||||||
12822|Mount Isa Group|35495|6|Mentioned|p341|||||||||
12822|Mount Isa Group|35892|6|Mentioned|p369|||||||||
12822|Mount Isa Group|35932|6|Mentioned|p461|||||||||
12822|Mount Isa Group|35950|6|Mentioned|p305|||||||||
12822|Mount Isa Group|36012|6|Mentioned|p16|||||||||
12822|Mount Isa Group|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
12822|Mount Isa Group|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
12822|Mount Isa Group|36548|6|Mentioned|p513|||||||||
12822|Mount Isa Group|36584|6|Mentioned|p367|||||||||
12822|Mount Isa Group|37217|6|Mentioned|p649|||||||||
12822|Mount Isa Group|37413|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
12822|Mount Isa Group|37459|6|Mentioned|p423|||||||||
12822|Mount Isa Group|37462|4|Described|Table4.VII|||||||||
12822|Mount Isa Group|37464|6|Mentioned|p508|||||||||
12822|Mount Isa Group|37565|5|Briefly described|p2|||See also Fig.5||||||
12822|Mount Isa Group|37568|5|Briefly described|p84|||||||||
12822|Mount Isa Group|37569|6|Mentioned|p91|||||||||
12822|Mount Isa Group|37816|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
12822|Mount Isa Group|37862|6|Mentioned|p587|||||||||
12822|Mount Isa Group|38156|6|Mentioned|Fig.1|||||||||
12822|Mount Isa Group|38232|6|Mentioned|p82|||||||||
12822|Mount Isa Group|38234|6|Mentioned|Fig.2|||||||||
12822|Mount Isa Group|38235|6|Mentioned|p113|||||||||
12822|Mount Isa Group|38237|6|Mentioned|p132|||||||||
12822|Mount Isa Group|38276|6|Mentioned|Fig.1|||||||||
12822|Mount Isa Group|38278|6|Mentioned|Fig.1|||||||||
12822|Mount Isa Group|38345|6|Mentioned|p18|||||||||
12822|Mount Isa Group|38348|6|Mentioned|p6|||||||||
12822|Mount Isa Group|38350|4|Described|p15|||||||||
12822|Mount Isa Group|38442|5|Briefly described|Map legend|Proterozoic|Proterozoic|Contains the Breakaway Shale, Moondarra Siltstone and the Warrina Park Quartzite.||||||25-AUG-04
12822|Mount Isa Group|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
12822|Mount Isa Group|38584|6|Mentioned|p17|||||||||
12822|Mount Isa Group|38598|6|Mentioned|p197|||||||||
12822|Mount Isa Group|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
12822|Mount Isa Group|38833|6|Mentioned|p161|||||||||
12822|Mount Isa Group|38835|6|Mentioned|p164|||||||||
12822|Mount Isa Group|38836|6|Mentioned|p165|||||||||
12822|Mount Isa Group|38919|6|Mentioned|p493|||||||||
12822|Mount Isa Group|39043|6|Mentioned|p9|||||||||
12822|Mount Isa Group|39202|6|Mentioned|p242|||||||||
12822|Mount Isa Group|39362|6|Mentioned|p1468|||||||||
12822|Mount Isa Group|39445|4|Described|p41|||Shallow marine in parts-intermontane. See also p36, p40 and Table 2.||||||09-NOV-06
12822|Mount Isa Group|39492|6|Mentioned|p30|||||||||
12822|Mount Isa Group|39556|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||
12822|Mount Isa Group|39561|6|Mentioned|Fig.8|||||||||
12822|Mount Isa Group|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Includes: Warrina Park Quartzite, Moondarra Siltstone, Breakaway Shale and Native Bee Siltstone.||||||15-JUN-06
12822|Mount Isa Group|39602|6|Mentioned|p603|||||||||
12822|Mount Isa Group|39622|6|Mentioned|Fig.2|||||||||
12822|Mount Isa Group|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
12822|Mount Isa Group|39934|6|Mentioned|p317|||See Fig.3||||||
12822|Mount Isa Group|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
12822|Mount Isa Group|40105|6|Mentioned|p310|||||||||
12822|Mount Isa Group|40202|6|Mentioned|p719|||||||||
12822|Mount Isa Group|40221|4|Described|p19|||||||||
12822|Mount Isa Group|40394|6|Mentioned|Fig.2|||||||||
12822|Mount Isa Group|40598|6|Mentioned|p31|||||||||
12822|Mount Isa Group|40623|5|Briefly described|p95|||||||||
12822|Mount Isa Group|40788|6|Mentioned|p27|||||||||
12822|Mount Isa Group|40840|6|Mentioned|Map legend|||||||||
12822|Mount Isa Group|40984|5|Briefly described|p400|||||||||
12822|Mount Isa Group|41079|6|Mentioned|p296|||||||||
12822|Mount Isa Group|41248|5|Briefly described|p69|||||||||
12822|Mount Isa Group|41277|6|Mentioned|Fig.5|||||||||
12822|Mount Isa Group|41298|6|Mentioned|Map legend|Carpentarian||||||||
12822|Mount Isa Group|41307|5|Briefly described|p15|||||||||
12822|Mount Isa Group|41381|6|Mentioned|p323|||||||||
12822|Mount Isa Group|41466|6|Mentioned|p23|||||||||
12822|Mount Isa Group|41744|5|Briefly described|p407|||||||||
12822|Mount Isa Group|41791|6|Mentioned|p272|||||||||
12822|Mount Isa Group|41802|5|Briefly described|p530|||||||||
12822|Mount Isa Group|41975|6|Mentioned|p437|||||||||
12822|Mount Isa Group|41978|6|Mentioned|p502|||||||||
12822|Mount Isa Group|41979|6|Mentioned|Fig.2 P512|||||||||
12822|Mount Isa Group|42072|4|Described|p1615|||||||||
12822|Mount Isa Group|42234|6|Mentioned|Fig.2 P1055|||||||||
12822|Mount Isa Group|42323|6|Mentioned|p4|||||||||
12822|Mount Isa Group|42350|5|Briefly described|p542||Mesoproterozoic|See also Fig. 1 p543.||||||09-NOV-06
12822|Mount Isa Group|42365|5|Briefly described|p272|||||||||
12822|Mount Isa Group|42367|6|Mentioned|p18|||||||||
12822|Mount Isa Group|42503|5|Briefly described|p334|||||||||
12822|Mount Isa Group|42523|5|Briefly described|p372|||||||||
12822|Mount Isa Group|42565|5|Briefly described|Table 1 P5, P4|||||||||
12822|Mount Isa Group|42570|6|Mentioned|p548|||Actually spelt Mt. Isa Group.||||||
12822|Mount Isa Group|42766|6|Mentioned|p2|||||||||
12822|Mount Isa Group|42782|5|Briefly described|p458|||||||||
12822|Mount Isa Group|42818|5|Briefly described|p206, Fig.2 p205|||||||||
12822|Mount Isa Group|42819|5|Briefly described|p310|||||||||
12822|Mount Isa Group|43107|6|Mentioned|p8|||||||||
12822|Mount Isa Group|43486|5|Briefly described|21|||||||||
12822|Mount Isa Group|43583|6|Mentioned|p2164|||Age 1670+/-19 Ma||||||
12822|Mount Isa Group|43595|5|Briefly described|p353,441||Mesoproterozoic|Tuffs U-Pb zircon age:1670+/-19 Ma.||||||09-NOV-06
12822|Mount Isa Group|43608|6|Mentioned|Fig.11,p11|||||||||
12822|Mount Isa Group|43615|6|Mentioned|p13|||1653+/-7 Ma||||||
12822|Mount Isa Group|43616|6|Mentioned|p2|||||||||
12822|Mount Isa Group|43652|6|Mentioned|p388|||||||||
12822|Mount Isa Group|43664|6|Mentioned|p14|||||||||
12822|Mount Isa Group|43760|5|Briefly described|p431|||Tuff horizons dated at 1670 Ma.||||||09-NOV-06
12822|Mount Isa Group|43972|14|Not recorded|p7||Paleoproterozoic|||||||07-NOV-08
12822|Mount Isa Group|44195|6|Mentioned|p350|||||||||
12822|Mount Isa Group|44389|14|Not recorded|p33||Paleoproterozoic|||||||07-NOV-08
12822|Mount Isa Group|44517|2|Defined|p234,237,239,map||Paleoproterozoic|Replaces Mount Isa Shale. Consists of Moondarra Silstone, Breakaway Shale, Native Bee Siltstone, Urquhardt Shale, Spear Siltstone, Kennedy Siltstone and Magazine Shale.||||||07-NOV-08
12822|Mount Isa Group|44755|14|Not recorded|Fig.1,p90,93||Mesoproterozoic|||||||
12822|Mount Isa Group|44764|4|Described|p33|||15,000' thick.||||||
12822|Mount Isa Group|44765|14|Not recorded|p15,16,18|||In Western Geosyncline.||||||
12822|Mount Isa Group|44766|14|Not recorded|unknown (23-27)|||Not listed on white card.||||||
12822|Mount Isa Group|44816|14|Not recorded|p20|||||||||
12822|Mount Isa Group|44827|14|Not recorded|p359|||||||||
12822|Mount Isa Group|45072|5|Briefly described|p5|||Sedimentation||||||
12822|Mount Isa Group|45136|4|Described|Table 1|||Also mention p19.||||||09-NOV-06
12822|Mount Isa Group|45161|5|Briefly described|p13|||See also p27.||||||09-NOV-06
12822|Mount Isa Group|45162|6|Mentioned|p45|||||||||
12822|Mount Isa Group|45166|4|Described|p28|||||||||
12822|Mount Isa Group|46801|6|Mentioned|p115|||See also Table 1||||||
12822|Mount Isa Group|46919|6|Mentioned|p221|||||||||
12822|Mount Isa Group|46960|6|Mentioned|p215|||||||||
12822|Mount Isa Group|46962|4|Described|Table 1|||See also Fig.3.||||||
12822|Mount Isa Group|46996|6|Mentioned|p273|||||||||
12822|Mount Isa Group|47011|6|Mentioned|p331|||||||||
12822|Mount Isa Group|47083|4|Described|p18-19|||Age: 1670 Ma. Correlates with McNamara Group. Overlies Surprise Creek Formation.  Mount Isa Orogen. Max thickness: 4250 m.||||||18-JAN-07
12822|Mount Isa Group|49041|5|Briefly described|Table 1|||||||||
12822|Mount Isa Group|50100|5|Briefly described|p11, p13 Fig. 4|Statherian|Statherian|Age: ~1650Ma.||||||
12822|Mount Isa Group|50332|4|Described|p16, p50|Paleoproterozoic|Paleoproterozoic|Includes; Moondarra Siltstone, Breakaway Shale, Native Bee Siltstone, Urquhart Shale + Spear Siltstone. Age: ~1700-1640Ma. Geol Prov: Western Fold Belt Province. Fluvial and shallow marine/lacustrine sedimentary rocks and subordinate bimodal volcanics.||||||07-FEB-11
12822|Mount Isa Group|50536|6|Mentioned|p8.1|||Geological Province: Mount Isa Inlier.||||||
12822|Mount Isa Group|50550|6|Mentioned|p1141 Fig.4||Statherian|Geological Province: Western Fold Belt.||||||19-DEC-07
12822|Mount Isa Group|50624|4|Described|p235||Statherian|Lists contained units. Unconformably overlies Haslingden Group. Thickness: 4000m.||||||
12822|Mount Isa Group|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Meta-arenite, quartzite, siltstone, shale.||||||
12822|Mount Isa Group|60558|5|Briefly described|p3, p4 Fig. 3, p5 Fig. 4|Paleoproterozoic|Paleoproterozoic|Includes seven units. Geological Province: Western Fold Belt.||||||03-JUN-09
12822|Mount Isa Group|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Geological Province: western Mount Isa Block.||||||07-NOV-08
12822|Mount Isa Group|61732|6|Mentioned|p26|||||||||07-FEB-11
12822|Mount Isa Group|61735|5|Briefly described|p658|Paleoproterozoic|Paleoproterozoic|Age: ~1653Ma.||||||30-JUN-09
12822|Mount Isa Group|61736|5|Briefly described|p674|||Includes Native Bee Siltstone and Urquhart Shale.||||||
12822|Mount Isa Group|61922|5|Briefly described|p9 Fig. 3, p10|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. See also p19 Fig.11.||||||07-NOV-08
12822|Mount Isa Group|61923|5|Briefly described|p27, p28 Fig.1|||Includes the Warrina Park Quartzite, Moondarra Siltstone, Breakaway Shale and Native Bee Siltstone. Overlies Eastern Creek Volcanics. Geological Province: Mount Isa Inlier. Mount is Mt in text. See also p34 Fig.6.||||||
12822|Mount Isa Group|61924|6|Mentioned|p43 Fig.2B|||||||||
12822|Mount Isa Group|61933|6|Mentioned|p176|||Geological Province: Western Fold belt, Mount Isa Inlier.  Mount is Mt in text.||||||
12822|Mount Isa Group|61963|6|Mentioned|p776|||Hosts the Mount Isa Cu-Pb-Zn deposits.||||||23-MAR-06
12822|Mount Isa Group|62084|5|Briefly described|p936 Fig.5, p950 Fig.14|||Isa Superbasin. Mount Isa.|||Moondarra Siltstone, Breakaway Shale, Native Bee Siltstone, Urquhart Shale, Spear Siltstone, Kennedy Siltstone, Magazine Shale|||
12822|Mount Isa Group|62287|5|Briefly described|p130|Mesoproterozoic|Mesoproterozoic|Includes the Urquhart Shale.  Geological Province: Mount Isa Inlier.||||||09-NOV-06
12822|Mount Isa Group|62288|5|Briefly described|p122 Fig. 2|Paleoproterozoic|Paleoproterozoic|Age: 1655Ma.  Geological Province: Western Fold Belt/ Mount Isa Inlier.||||||07-NOV-08
12822|Mount Isa Group|62535|5|Briefly described|p672, p674|Statherian|Statherian|Leichhardt River Fault Trough.|||Warrina Park Quartzite; Moondarra, Native Bee, Spear Siltstones; Breakaway, Urquhart, Magazine Shales; Kennedy Formation.||Includes dominant rhythmically laminated siliciclastic facies.|
12822|Mount Isa Group|62536|5|Briefly described|p658|||Mount Isa, Qld. Deposition and syngenetic mineralisation was followed 50-100 m.y. later by major deformational events.|1653 Ma (deposition).|||||
12822|Mount Isa Group|62873|5|Briefly described|p692|||Includes the Urquhart Shale in upper section. Sequence of carbonaceous and dolomitic siltstones, mudstones and shales. Overlies the Haslingden Group. Max. thickness: 6km.||||||22-NOV-06
12822|Mount Isa Group|63023|6|Mentioned|p1026|||Mount is Mt in text.||||||
12822|Mount Isa Group|63114|6|Mentioned|p1252. |||Isa superbasin.|||||Carbonate, carbonaceous siltstone, shale.|
12822|Mount Isa Group|63593|5|Briefly described|p288 Fig.2, p291 Fig.3 and Tb.2, p294.  |Palaeoproterozoic|Palaeoproterozoic|Western Fold Belt. 4500 m thick.|ca 1670 Ma||||Dolomitic siltstone, shale.|
12822|Mount Isa Group|63866|6|Mentioned|p52|||||||||
12822|Mount Isa Group|63884|5|Briefly described|p14|||Metasedimentary rocks. Overlies Eastern Creek Volcanics. Mount is Mt in text.||||||
12822|Mount Isa Group|64137|6|Mentioned|p1544|||Mount Isa inlier. Same age as Tarcoola Formation.||||||
12822|Mount Isa Group|64250|5|Briefly described|p8, p25 fig 10, p11 fig.3, p19, p22, p24|||Detrital zircons age: 1730-1700 Ma probably from reworked material from NW. 1880-1850 Ma and ~ 1785 Ma are consistent with derivation from Murphy Inlier and Eastern Creek Volcanics.|1655 +/- 4 Ma||Breakaway, Urquhart, Magazine Shales; Moondarra, Native Bee, Spear-Kennedy Siltstones.||Mainly shales and siltstones.|
12822|Mount Isa Group|64367|5|Briefly described|p555  Fig. 1c|Paleoproterozoic|Paleoproterozoic|Overlies Eastern Creek Volcanics. Max. thickness: 6km. Carbonaceous and dolomitic siltstones, mudstones and shales depositied in shallow water conditions.||||||07-FEB-11
12822|Mount Isa Group|64725|6|Mentioned|p58 Fig.2. |||Mount Isa Inlier.||||||
12822|Mount Isa Group|64741|6|Mentioned|p310|||Temporal equivalents of upper parts of Willyama Supergroup.||||||07-FEB-11
12822|Mount Isa Group|64742|6|Mentioned|p334.|||||||||
12822|Mount Isa Group|64815|6|Mentioned|p3, |||||||||
12822|Mount Isa Group|65228|6|Mentioned|p9|||||||||
12822|Mount Isa Group|65337|6|Mentioned|p6.|||Isa Superbasin.||||||
12822|Mount Isa Group|65387|6|Mentioned|p85|||Widespread volcanism around 1690-1650 Ma is evident from tuff layers in this unit and the McNamara Group.||||||
12822|Mount Isa Group|65396|5|Briefly described|p16, p82, p173, p175, p188, p190, p193|Statherian|Statherian|See also p197, p241, p391, p439. Cover Sequence 3. Leichhardt River Fault Trough. Deposition mainly between c.1665 Ma and 1650 Ma. Hosts giant shale-hosted Pb-Zn-Ag+/-Cu deposits.|1655 +/- 4 Ma||Includes Moondarra Siltstone, Breakaway Shale, Native Bee Siltstone, Urquhart Shale, Spear-Kennedy Siltstone, Magazine Shale||Calcareous shales, pelites and mafic volcanics.|
12822|Mount Isa Group|66800|6|Mentioned|p928, p933.|||Western Fold Belt, Mount Isa Inlier. Hosts the Mount Isa and Hilton world-class, massive base-metal deposits.||||||
12822|Mount Isa Group|66824|6|Mentioned|p132, 135, 148-151|||Interpreted as a sag-phase sequence.||||Unconformably overlies Surprise Creek Formation. Equivalent to McNamara Group.|Includes laminated shales and dolomitic siltstones; tuff beds.|
12822|Mount Isa Group|66843|6|Mentioned|p35||||||includes Urquhart Shale.|||12-SEP-19
12822|Mount Isa Group|67026|4|Described|pp335-336.|Statherian|Statherian|4.5 - 6 km thick sequence of supracrustal volcanic and sedimentary rocks, deposited in a series of intracontinental extension-related basins.|1785 - 1650 Ma (Duncan et al. 2006).||Includes Urquhart Shale Formation.|Intruded by the Sybella Batholith c. 1660 Ma.|Sequence of carbonaceous and dolomitic siltstones, mudstones and shales.|24-APR-12
12822|Mount Isa Group|67323|4|Described|p8, p13, p15, p26, p34, p39, p72, p107|Paleoproterozoic|Paleoproterozoic|See also GIS attrib tbl, Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Leichhardt River Domain, Mount Isa Inlier. Isa Superbasin. Deposition began c.1670 Ma. Contains Ag anomalies.|~1675-1645 Ma.||Includes Breakaway Shale, Hero Formation, Kennedy Siltstone, Magazine Shale, Moondarra Siltstone, Native Bee Siltstone, Spear Siltstone, Urquhart Shale, Warrina Park Quartzite.|Unconformably overlies Oroopo Metabasalt.|Meta-arenite and quartzite, pyritic siltstone and shale; minor schist, micaceous metasiltstone|
12822|Mount Isa Group|67499|4|Described|p938-40, p941, p947, p948, p942 Fig.4|Statherian|Statherian|Equivalent to the McNamara Group - about 220km northwest of Mount Isa. Age estimated from p942 Fig.4.|1660 Ma||Includes Warrina Park Quartzite.|Stratigraphically equivalent to the McNamara Group.|Hosts important base-metal ores and consists of a basal silicified sandstone and conglomerate unit, overlain by several shale and siltstone units.|08-MAY-12
12822|Mount Isa Group|68020|6|Mentioned|p125, p126||||||Includes Urquhart Shale|Lower part correlated with Paradise Creek Formation.|Includes metasedimentary rocks.|
12822|Mount Isa Group|68021|6|Mentioned|p135 fig 4|Statherian|Statherian|Western Succession.||||Overlies Surprise Creek Formation.||
12822|Mount Isa Group|68542|6|Mentioned|p6|||Cavaney (1975). Leichhardt River Fault Trough, Mount Isa Inlier.|||Includes Warrina Park Quartzite; Moondarra, Native Bee, Spear, Kennedy Siltstones; Breakaway, Urquhart, Magazine Shales.|Overlies Surprise Creek Beds.||
12822|Mount Isa Group|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province.||||||
12822|Mount Isa Group|68576|5|Briefly described|Q_2: p6|||Cavaney (1975). Leichhardt River Fault Trough, Mount Isa Inlier.|||Warrina Park Quartzite; Moondarra, Native Bee, Spear, Kennedy Siltstones; Breakaway, Urquhart, Magazine Shales.|Overlies Surprise Creek Beds.||
12822|Mount Isa Group|68732|5|Briefly described|p159-163|||Mount spelt as Mt in text.|||Moondarra and Native Bee Siltstones, Urquhart Shale.||Includes cross-stratified quartzites and pebbly quartzites at or near the base.|01-DEC-17
12822|Mount Isa Group|69056|5|Briefly described|p54-56|||Isa Superbasin. Ore-bearing.|||Gun Supersequence.|Correlated with Tommy Creek Microgranite.||
12822|Mount Isa Group|69222|6|Mentioned|p221|Calymmian|Statherian|12-14km thick. Western Fold Belt; across the Lawn Hill Platform it is called the McNamara Group. Associated with the Mount Isa Rift Event. Age range c.1653-1595 Ma.|1652 +/- 7 Ma|||Overlies Surprise Creek Formation, Correlated with McNamara Group|Sag-related shale and dolomite rich sequences.|
12822|Mount Isa Group|69370|6|Mentioned|p307 Fig.2|Statherian|Statherian|Western Fold Belt, Mount Isa Block.||||Overlies Surprise Creek Formation. Is intruded by Sybella Granite.||25-JAN-19
12822|Mount Isa Group|69542|5|Briefly described|p132, p133 Fig.2, p140|Mesoproterozoic|Paleoproterozoic|Western Fold Belt.|||Includes Warrina Park Quartzite, Moondarra Siltstone, Breakaway Shale, Native Bee Siltstone, Urquhart Shale.||Laminated dolomitic and carbonaceous siltstone and shale.|
12822|Mount Isa Group|69591|4|Described|p29, p40, p42-45, p55, p108|Paleoproterozoic|Paleoproterozoic|Leichhardt River Domain, Isa Superbasin. Upper parts are mostly carbonaceous, and dolomitic argillites deposited in deeper water (deepwater rhythmites). Is coeval with 1653-1650 Ma Tommy Creek Microgranite.|~1660-1650 Ma (lower part).||Warrina Park Quartzite, Urquhart Shale, Moondarra Siltstone, Breakaway Shale, Native Bee Siltstone, Spear Siltstone, Kennedy Siltstone, Magazine Shale, Hero Formation.|Unconformably overlies Oroopo Metabasalt. Coeval with McNamara Group. Is faulted against Eastern Creek Volcanics and Myally Subgroup.|Dominated by carbonaceous and dolomitic siltstone and shale.|
12822|Mount Isa Group|70282|5|Briefly described|p544, p551|||Cover sequence 4, Mount Isa. Shallow-marine deposits.|> 1652 Ma||Urquhart Shale.|Overlies Surprise Creek Formation.|Siltstones and carbonate rocks.|13-FEB-18
12822|Mount Isa Group|70283|5|Briefly described|p25|Paleoproterozoic|Paleoproterozoic|Hosts the Mount Isa Cu and stratiform Pb-Zn-Ag deposits.|||Includes Surprise Creek Formation, Urquhart Shale|Overlies Haslingden Group|Metasediments: dolomitic siltstone, shale and carbonates, interbedded with minor tuff horizons, sulfates and minor halite evaporites.|14-FEB-18
12822|Mount Isa Group|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic||||Warrina Park Quartzite; Moondarra, Native Bee Siltstones; Breakaway Shale.|||
12822|Mount Isa Group|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic||||Warrina Park Quartzite; Moondarra, Native Bee Siltstones; Breakaway Shale.|||
12822|Mount Isa Group|70897|5|Briefly described|p36||||c.1640 Ma.|||||
12822|Mount Isa Group|71606|5|Briefly described|p137|Statherian|Statherian|Leichardt River Fault Trough, Mount Isa Inlier.||||Underlain by Surprise Creek Formation. Equivalent to Fickling and McNamara groups.||
12822|Mount Isa Group|71960|5|Briefly described|p85-87, p77, p78, 81, 83, 104, 105|Proterozoic|Proterozoic|Originally defined by Bennet (1965). Redefined by Derrick et al. (1976) as comprising 8 formations. Four lowest in study area form a fining upwards megasequence (lower Mount Isa Group). Provenance of lower part shown to be from west. Also shows early deformation.|||Includes from base,  Warrina Park Quartzite, Hero Formation, Moondarra Siltstone, Breakaway Shale, Native Bee Siltstone.|Unconformably overlies/truncates Eastern Creek Volcanics in Hero Syncline, and other parts of the Haslingden Group elsewhere. Shown as equivalent to McNamara Group in Fig 8 p86.||
12822|Mount Isa Group|71980|5|Briefly described|map legend sheets 1, 2|Proterozoic|Proterozoic|Paroo Range, Hero/Western Fault Zone.|||Includes Surprise Creek Formation, Warrina Park Quartzite, Hero Formation, Moondarra Siltstone, Breakaway Shale,|Unconformably overlies Haslingden Group.||03-APR-19
12822|Mount Isa Group|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Leichhardt River Fault Trough and the Kalkadoon-Leichhardt Belt of the Mount Isa Province.|||Magazine Shale, Spear-Kennedy Siltstone, Urquhart Shale, Native Bee Siltstone, Breakaway Shale and Moondarra Siltstone.|Shown as unconformably and partially overlying Torpedo Creek and Warrina Park Quartzites.|Includes shale and siltstone.|
12822|Mount Isa Group|72889|6|Mentioned|p6 Fig.i.|||||||||
12822|Mount Isa Group|72912|5|Briefly described|p5 Fig.3, p13.|Statherian|Statherian||||Magazine, Urquhart and Breakaway Shale, Spear-Kennedy, Native Bee and Moondarra Siltstone.|Shown as unconformably overlying Torpedo Creek and Warrina Park Quartzite. Laterally and partially equivalent to McNamara Group.|Includes carbonaceous and dolomitic siltstones andshales.","Located in the Leichhardt River Fault Trough and the Kalkadoon-Leichhardt Belt of the Isa Superbasin, Mount Isa Province.|
12822|Mount Isa Group|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Mount Isa Province, Isa Superbasin.|||Magazine Shale, Spear-Kennedy Siltstone, Urquhart Shale, Native Bee Siltstone, Breakaway Shale, Moondarra Siltstone.|||
12822|Mount Isa Group|73137|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|||||||
12822|Mount Isa Group|73413|6|Mentioned|p3|||Mount Isa Inlier.||||||
12840|Mount John Shale Member|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
12840|Mount John Shale Member|32660|6|Mentioned|p223|||||||||
12840|Mount John Shale Member|32728|6|Mentioned|Fig.3|||||||||
12840|Mount John Shale Member|36885|4|Described|p177|||||||||
12840|Mount John Shale Member|37371|6|Mentioned|p388|||||||||
12840|Mount John Shale Member|37462|4|Described|Table 4.VI|||||||||
12840|Mount John Shale Member|38157|6|Mentioned|Table X|||||||||
12840|Mount John Shale Member|44155|4|Described|p251-252|||200m thick.|1128 +/- 110 Ma (Dow and Gemuts, 1969).|Wade Creek Sandstone|||Khaki and some black shale and siltstone, minor quartz sandstone; some beds highly ferruginous.|
12840|Mount John Shale Member|44317|4|Described|Table 3||Adelaidean|||||||
12840|Mount John Shale Member|44318|14|Not recorded|map legend||Adelaidean|Adelaidean.||||||
12840|Mount John Shale Member|45047|2|Defined|p80|Adelaidean|Adelaidean|See also pp32,35.||||||28-MAY-15
12840|Mount John Shale Member|45112|6|Mentioned|p30|||||||||
12840|Mount John Shale Member|45140|5|Briefly described|p59||||1128 +/- 110 Ma (Dow and Gemuts, 1969).|Wade Creek Sandstone.|||A thick shale lens.|
12840|Mount John Shale Member|48938|5|Briefly described|p76|||Age. Refers Dow & Gemuts (1969).||||||
12840|Mount John Shale Member|67484|5|Briefly described|p294|Neoproterozoic||Kimberley Region. Previously, Sprigg (1949) named the possible fossil Protoniobia wadea from this unit and considered it to be related to the Ediacaran fauna from South Australia. The age and organic nature are questionable.||||Is overlain by Eliot Range Dolomite.||28-MAY-15
12840|Mount John Shale Member|69099|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Victoria River Basin||Wade Creek Formation|||Grey-green siltstone, mudstone, and fine- to coarse-grained sandstone.|03-AUG-15
12840|Mount John Shale Member|69165|5|Briefly described|100k_interpgeop_lut.csv|Mesoproterozoic|Mesoproterozoic|||Wade Creek Formation|||Grey-green siltstone, mudstone and fine to coarse grained sandstone.|
12840|Mount John Shale Member|69634|4|Described|100k_interpgeop_lut.csv|Mesoproterozoic|Mesoproterozoic|Geological province: Halls Creek Orogen. Of Victoria River Basin. Events:Alice Springs Orogeny; Yampi Orogeny D1/M1.|1600-1000 Ma (Inferred)|Unit of Wade Creek Formation.|||Grey-green siltstone, mudstone, and fine- to coarse-grained sandstone|
12840|Mount John Shale Member|70154|5|Briefly described|100k_interpgeop_lut.csv|Mesoproterozoic|Mesoproterozoic||1000-1600 Ma||||Siltstone, mudstone and fine to coarse grained sandstone.|
12840|Mount John Shale Member|71267|5|Briefly described|100k_interpgeop_lut.csv|Mesoproterozoic|Mesoproterozoic|Geological province: Halls Creek Orogen. Of Osmond Basin. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma).|1600-1000 Ma (inferred)|Unit of Wade Creek Formation.|||Grey-green siltstone, mudstone, and fine- to coarse-grained sandstone|
12840|Mount John Shale Member|73255|6|Mentioned|p534 Fig.2|Tonian|Tonian|Written as Mt John Shale Member in text.||Wade Sandstone||Interbedded in the Wade Sandstone.||
12886|Mount Les Siltstone|22453|6|Mentioned|p 12|||In the McArthur Basin.||||||09-NOV-06
12886|Mount Les Siltstone|22665|5|Briefly described|Table1, P229||Statherian|Mount actually spelt Mt, Age of unit is 1640+/-7 Ma.||||||09-NOV-06
12886|Mount Les Siltstone|22673|3|Fully described|63-66, 76,78|||Geological province: Mount Isa Basin. Mount as 'Mt' in text.||||||09-NOV-06
12886|Mount Les Siltstone|22680|6|Mentioned|83,85,87|||Geological province: Mount Isa Basin. Of the Fickling Group.||||||09-NOV-06
12886|Mount Les Siltstone|23031|6|Mentioned|27|||Of the Fickling Group.||||||09-NOV-06
12886|Mount Les Siltstone|23065|6|Mentioned|16|||Of the Fickling Group. Age 1640 +/- 7 Ma||||||09-NOV-06
12886|Mount Les Siltstone|23393|5|Briefly described|p21|Paleoproterozoic|Paleoproterozoic|Of Fickling Group.||||||07-NOV-08
12886|Mount Les Siltstone|23396|4|Described|p417|Statherian|Statherian|Of Fickling Group. Age: 1640+/-7Ma.||||||28-SEP-06
12886|Mount Les Siltstone|23397|5|Briefly described|p473|Statherian|Statherian|Age: 1640+/-7Ma.||||||09-NOV-06
12886|Mount Les Siltstone|23398|4|Described|p445|Statherian|Statherian|Age: 1640+/-7Ma.||||||28-SEP-06
12886|Mount Les Siltstone|23406|5|Briefly described|p606, p608 Fig. 9, p613|Statherian|Statherian|Of Fickling Group. Age: 1640+/-7Ma. Consists of interbedded, fine-grained sandstone, siltstone and shale with occasional thin dolostone beds.||||||16-JUN-09
12886|Mount Les Siltstone|23409|5|Briefly described|p533|||Of the Fickling Group.||||||09-NOV-06
12886|Mount Les Siltstone|24308|5|Briefly described|p1002, p987 Fig. 2|Paleoproterozoic|Paleoproterozoic|Mount is Mt. in text.  Of the Fickling Group.   Geological Province:  Mount Isa Superbasin||||||07-NOV-08
12886|Mount Les Siltstone|24432|4|Described|p562 Fig.2|Statherian|Statherian|Of McNamara Group. Age: 1640+/-7 Ma. Carbonaceous, dolomitic and pyritic shales and local talus breccias. Overlies Walford Dolomite. Geological Province: Lawn Hill Platform.||||||25-FEB-05
12886|Mount Les Siltstone|35640|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
12886|Mount Les Siltstone|36012|3|Fully described|Table 3|||See also p16.||||||28-SEP-06
12886|Mount Les Siltstone|36217|6|Mentioned|p206|||Published by Grimes & others 1979. Definition approved by Qld SNC.||||||
12886|Mount Les Siltstone|36439|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
12886|Mount Les Siltstone|36442|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
12886|Mount Les Siltstone|38237|6|Mentioned|p129|||||||||
12886|Mount Les Siltstone|38348|6|Mentioned|p13|||||||||
12886|Mount Les Siltstone|38584|4|Described|p17|||||||||
12886|Mount Les Siltstone|39445|5|Briefly described|Table 2|||See also p39.||||||09-NOV-06
12886|Mount Les Siltstone|39497|6|Mentioned|Fig.4|||||||||
12886|Mount Les Siltstone|39685|6|Mentioned|p407|||||||||
12886|Mount Les Siltstone|39925|6|Mentioned|Fig.9|||||||||
12886|Mount Les Siltstone|41721|4|Described|p28|||||||||
12886|Mount Les Siltstone|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
12886|Mount Les Siltstone|43010|5|Briefly described|Fig.6||Mesoproterozoic|Of the Fickling Group. Of "Mid Proterozoic" age.||||||09-NOV-06
12886|Mount Les Siltstone|45162|6|Mentioned|p146|||||||||
12886|Mount Les Siltstone|45166|5|Briefly described|p30|||||||||
12886|Mount Les Siltstone|49001|2|Defined|p10|Carpentarian|Carpentarian|||||||
12886|Mount Les Siltstone|60558|5|Briefly described|p5 Fig. 4|||Of Fickling Group. Overlian by Doomadgee Formation, underlain by Walford Dolomite.||||||
12886|Mount Les Siltstone|61936|5|Briefly described|p194 Fig. 6|||Age: <1640Ma. Geological Province: Lawn Hill Platform, Western Fold Belt, Mount Isa Inlier, Isa Superbasin.||||||15-MAR-07
12886|Mount Les Siltstone|62535|5|Briefly described|p672|Statherian|Statherian|Lawn Hill Platform.|1640 +/- 7 Ma.|McNamara Group.||||
12886|Mount Les Siltstone|63109|6|Mentioned|p1108 Fig. 3|||Mount is Mt in text. Overlain by Riversleigh Siltstone. Geological Province: Isa Superbasin. Consists of siltstone and shale.||||||30-SEP-08
12886|Mount Les Siltstone|63111|5|Briefly described|p1164 Tb. 1, p1163 Fig. 3|Statherian|Statherian|Of River Supersequence. Age: 1644+/-8 and 1640+/-7Ma. Geological Province: Isa Superbasin. Consists of conglomerates and fine-grained arenites.||||||07-FEB-11
12886|Mount Les Siltstone|63113|6|Mentioned|p1225 Fig.13, p1226. |||Isa Superbasin. River supersequence. The probable source of hydrocarbons deposited in Walford Dolomite.||||Overlies Walford Dolomite.||
12886|Mount Les Siltstone|63115|6|Mentioned|1279 Fig.4,p1281, |||Isa superbasin. Hosts the Walford Creek Cu-Zn-Pb-bearing stratiform pyrite lenses.||Unit in Fickling Group.|||Includes metalliferous dolomitic black shales.|
12886|Mount Les Siltstone|63116|6|Mentioned|p1297 Fig.2, |||Isa superbasin.||||||
12886|Mount Les Siltstone|63866|5|Briefly described|p56|Statherian|Statherian|Isa Superbasin.|1640 +/- 7 Ma|||Equivalent to the River Supersequence.||
12886|Mount Les Siltstone|65228|5|Briefly described|p33, Fig.04.|Statherian|Statherian|Mt Les in text. Only component of River Supersequence at the northern end of Lawn Hill Platform.|1640 +/- 7 Ma (SHRIMP).|||||
12886|Mount Les Siltstone|65337|6|Mentioned|p22 Table 4.|||||Unit in Fickling Group.||Is overlain by Doomadgee Formation.||
12886|Mount Les Siltstone|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Camooweal-Murphy Domain, Mount Isa Inlier. Isa Superbasin.|1640 +/- 7 Ma (maximum depositional age).|Fickling Group.|||Dolomitic siltstone and shale; flaggy dolomite interbeds|
12886|Mount Les Siltstone|68733|5|Briefly described|p186|Statherian|Statherian|||Of the McArthur Group.||||
12886|Mount Les Siltstone|69433|4|Described|p18:2-4|Statherian|Statherian|Northern succession, Lawn Hill Platform. Up to 90m thick. Evaporitic conditions in a supratidal environment. SHRIMP U-Pb zircon age from a tuffaceous bed, by Page and Sweet (1998), Page et al. (2000). Misspelt as Mount Less Siltstone in table 18.1, p18:4.|1640 +/- 7 Ma.|Fickling Group.||Conformably overlies Walford Dolostone. Is overlain disconformably by Doomadgee Formation.|Dolostone, siltstone, shale and minor interbeds of flaggy dolostone with gypsum and pyrite pseudomorphs.|23-APR-20
12886|Mount Les Siltstone|69591|4|Described|p43 Fig.2.31, p47|||Camooweal-Murphy Domain, Isa Superbasin. S of the Murphy Inlier. Part of the River Supersequence. Deep marine deposits.|1640 +/- 7 Ma (Page and Sweet, 1998).|Fickling Group.||Equivalent of the Riversleigh Siltstone.|Dolomitic siltstone and shale; flaggy dolomite interbeds.|
12886|Mount Les Siltstone|69673|4|Described|p52 fig 42, p53 , p54 |Statherian|Statherian||1640 +/- 7 Ma||||Dolostone, siltstone, shale and minor interbeds of flaggy dolostone with gypsum and pyrite pseudomorphs.|
12886|Mount Les Siltstone|70849|5|Briefly described|Map legend.|Statherian|Statherian|Lawn Hill Platform.||Fickling Group.||Overlies Walford Dolostone. Is overlain unconformably by Doomadgee Formation.|Dolomitic siltstone and shale; flaggy dolomite interbeds.|
12886|Mount Les Siltstone|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1641+/-7 Ma (crystallisation: U-Pb zircon SHRIMP)||||Ash tuff.|
12886|Mount Les Siltstone|72526|5|Briefly described|p8 Fig.1.3, p20.|Statherian|Statherian|Shown as being located in the central and west of the South Nicholson Basin. Age given as U-Pb zircon sedimentary depositional age.|1640 +/-7 Ma|Fickling Group||Overlies Walford Dolomite and disconformably underlies Doomadgee Formation.||
12886|Mount Les Siltstone|72912|5|Briefly described|p5 Fig.3, p32, p33 Fig.12, p45.|Statherian|Statherian|Located in the West and Central of the South Nicholson Basin. U-Pb zircon sedimentary depositional age given.|1640 +/- 7 Ma|Fickling Group||Overlies Walford Dolomite and unconformably underlies Doomadgee Formation. Partially equivalent to Lawn Hill Formation and Shady Bore Quartzite. Laterally equivalent to Plain Creek Formation.|Includes organic rich siltstone and shales.|
12886|Mount Les Siltstone|72913|5|Briefly described|p4, p7, p8, p9 Tb.1, p22, p24, p26.|Paleoproterozoic|Paleoproterozoic|Shown as being in the central part of the Isa Superbasin.  Identified in 3 wells in this study. Mineral composition shows majority quartz, microcline, muscovite and dolomite.|1640 +/- 7 Ma|Fickling Group||Overlies Walford Dolomite and unconformably underlies Doomadgee Formation.|Includes siltstone.|
12886|Mount Les Siltstone|72967|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|Lawn Hill Platform.||Fickling Group||||
12886|Mount Les Siltstone|73042|5|Briefly described|p1, p4, p6, p14, p17|Statherian|Statherian|Previous zircon U-Pb age data on a tuff interval yielded a depositional age of 1640+/-7 Ma (Page and Sweet, 1998). Mount Isa Province (Lawn Hill Platform) and South Nicholson Basin region, Isa Superbasin. Maximum thickness: <100m. Parent unit is said to be the Fickling Group throughout; however, is indicated as the McNamara Group on p18 (wrong parent?).|1640 +/- 7 Ma|Fickling Group||Conformably underlain by Walford Dolomite. Disconformably overlain by Doomadgee Formation.|Dolostone, siltstone and shale with minor occurrences of flaggy dolostone with gypsum and pyrite pseudomorphs.|
13010|Mount Parker Sandstone|22440|5|Briefly described|p4,5|Stenian|Stenian|Age 1200- 1000Ma.||||||09-NOV-06
13010|Mount Parker Sandstone|22496|6|Mentioned|p10||Neoproterozoic|Superseded by Mount Kinahan Sandstone.||||||09-NOV-06
13010|Mount Parker Sandstone|22547|5|Briefly described|p21|||In the Texas Downs Basin - mapped as Texas Downs Formation.||||||09-NOV-06
13010|Mount Parker Sandstone|22716|5|Briefly described|table4, p236|Mesoproterozoic|Mesoproterozoic|May be equivalent to part of the Birrindudu Group.||||||
13010|Mount Parker Sandstone|22754|5|Briefly described|p11 Tb. 3|Mesoproterozoic|Mesoproterozoic|||||||
13010|Mount Parker Sandstone|22764|4|Described|Table1,p7||Carpentarian|770 m. Unconformable on Olympio Formation and Lamboo Complex.||||||01-FEB-10
13010|Mount Parker Sandstone|23314|5|Briefly described|329|||Mount is Mt. in text.||||||
13010|Mount Parker Sandstone|23621|5|Briefly described|p31|Mesoproterozoic|Mesoproterozoic|Geological Province: Osmond Basin.||||||
13010|Mount Parker Sandstone|23809|5|Briefly described|p47 Fig. 42|Proterozoic|Proterozoic|Geological Province: Osmond Basin. Mount is Mt in text. Correlates with Campbell Springs Dolostone (Birrindudu Basin), Shillinglaw Formation (Tennant Creek Inlier) and Barney Creek Formation (McArthur Basin).||||||22-MAY-08
13010|Mount Parker Sandstone|28255|6|Mentioned|p11|||Age is probably Adelaidean or may be as old as Carpentarian. East Kimberley area (WA). Mount is Mt in text.||||||
13010|Mount Parker Sandstone|29805|6|Mentioned|p8|||||||||
13010|Mount Parker Sandstone|29809|6|Mentioned|p418|||||||||
13010|Mount Parker Sandstone|29813|4|Described|Table 2|||||||||
13010|Mount Parker Sandstone|29818|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
13010|Mount Parker Sandstone|30895|6|Mentioned|Map legend|Adelaidean|Carpentarian|Prob. Adelaidean||||||
13010|Mount Parker Sandstone|31393|6|Mentioned|Pl.25|||||||||
13010|Mount Parker Sandstone|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
13010|Mount Parker Sandstone|32660|5|Briefly described|Table 6|||||||||
13010|Mount Parker Sandstone|32728|5|Briefly described|p42|||||||||
13010|Mount Parker Sandstone|34230|6|Mentioned|Plate 8|Proterozoic|Proterozoic|||||||28-OCT-04
13010|Mount Parker Sandstone|35120|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
13010|Mount Parker Sandstone|35950|6|Mentioned|p311|||||||||
13010|Mount Parker Sandstone|36532|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
13010|Mount Parker Sandstone|36551|6|Mentioned|p26|||||||||
13010|Mount Parker Sandstone|36885|4|Described|p177|||||||||
13010|Mount Parker Sandstone|36898|6|Mentioned|Fig.2A|||||||||
13010|Mount Parker Sandstone|37299|6|Mentioned|Fig.1|||||||||
13010|Mount Parker Sandstone|37462|4|Described|Table 4.V|||||||||
13010|Mount Parker Sandstone|41811|6|Mentioned|p212|||||||||
13010|Mount Parker Sandstone|43631|6|Mentioned|p20|||||||||
13010|Mount Parker Sandstone|44140|5|Briefly described|p299|Mesoproterozoic|Mesoproterozoic|Of Birrindudu Basin.||||Correlated with Colombo Sandstone (Kimberley Basin).||
13010|Mount Parker Sandstone|44155|4|Described|p251-252|Mesoproterozoic|Mesoproterozoic|150-300m thick. Type locality at Mount Parker. Probable part correlative of Tawallah and McArthur Groups in McArthur Basin.||||Overlies Red Rock Beds and Fish Hole Dolerite unconformably. Overlain by Bungle Bungle Dolomite conformably. Correlated with Gardiner Sandstone.|Clean quartz sandstone, commonly with pebbly lenses; commonly ferruginous at top.|
13010|Mount Parker Sandstone|44317|4|Described|Table 2||Carpentarian|||||||
13010|Mount Parker Sandstone|44318|14|Not recorded|map legend|||Adelaidean or Carpentarian.||||||
13010|Mount Parker Sandstone|44324|14|Not recorded|p.10||Neoproterozoic|Tb.2 (Upper Proterozoic).||||||
13010|Mount Parker Sandstone|44325|14|Not recorded|map legend||Neoproterozoic|Up.Proterozoic.||||||
13010|Mount Parker Sandstone|44363|5|Briefly described|p.6,13,14,16,17|||Adelaidean or Carpentarian.||||||
13010|Mount Parker Sandstone|44364|14|Not recorded|map legend|||||||||
13010|Mount Parker Sandstone|45047|2|Defined|p74|early Adelaidean|late Carpentarian|See also pp31,35. Early Adelaidean or Late Carpentarian.||||||09-NOV-06
13010|Mount Parker Sandstone|45112|6|Mentioned|p15|||||||||
13010|Mount Parker Sandstone|45140|2|Defined|p12-13, p25, p39-41, p58, p60, p74|||See also Appx.p31. Dow and Gemuts (1969). Unnamed basin NW of Birrindudu Basin. Named after Mount Parker. Mapped as Kearney Beds by Casey and Wells (1964). The type section is in the Osmond Range, in the Dixon Range sheet area. Forms discontinuous strike ridges. 300m thick. In SW of Gordon Downs map area, this unit included rocks now assigned to Wade Creek Sandstone (Gemuts and Smith, 1968).||||Unconformably overlies Olympio Formation. Is overlain conformably by Bungle Bungle Dolomite. Probable equivalent to Birrindudu Group.|Well-sorted, medium-grained quartz arenite; lesser medium- to coarse-grained sublithic arenite and minor pebbly arenite, conglomerate and local siltstone. Cross-bedding common; some bedding planes are crowded with shale pellets.|
13010|Mount Parker Sandstone|46864|5|Briefly described|p40|||||||||
13010|Mount Parker Sandstone|48950|6|Mentioned|p36|||||||||
13010|Mount Parker Sandstone|50225|5|Briefly described|p406 Fig. 10, p407|Mesoproterozoic|Mesoproterozoic|Geological Province: Halls Creek Province.||||||07-FEB-11
13010|Mount Parker Sandstone|64104|6|Mentioned|p75, p76 fig 10|Neoproterozoic|Neoproterozoic|Osmond Basin. Part of Osmond Range succession. [this article changes the age of a number of units, including this one, without explanation]||||||19-MAY-15
13010|Mount Parker Sandstone|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.|||||Well sorted thinly bedded medium grained quartz sandstone, medium to coarse sublithic arenite and minor pebble conglomerate with siltstone locally near the base; low angle cross bedding is common, and clay pellets occur on bedding planes in places|
13010|Mount Parker Sandstone|73255|6|Mentioned|p534 Fig.2|Tonian|Tonian|Written as Mt Parker Sandstone in text.||Osmond Range Succession||Underlies the Bungle Bungle Dolomite.||
13012|Mount Partridge Group|9324|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Sandstone, siltstone, shale, marble, quartzite, conglomerate.||||||07-NOV-08
13012|Mount Partridge Group|9534|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes the Wildman Siltstone and Mundogie Sandstone.||||||07-NOV-08
13012|Mount Partridge Group|9538|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Sandstone, siltstone, shale, quartzite, arkose, conglomerate, dolomite; schist and gneiss in the east. Unconformably overlain by the South Alligator Gp; unconformably overlies the Namoona Gp.||||||07-NOV-08
13012|Mount Partridge Group|9579|5|Briefly described|Map Sheet|Paleoproterozoic|Paleoproterozoic|Early Proterozoic age.||||||
13012|Mount Partridge Group|9691|5|Briefly described|Map Legend|||||||||
13012|Mount Partridge Group|9701|5|Briefly described|Map Legend|Proterozoic|Proterozoic|||||||02-JUN-05
13012|Mount Partridge Group|22479|5|Briefly described|fig1p2|Orosirian|Orosirian|||||||
13012|Mount Partridge Group|22809|6|Mentioned|map|Proterozoic|Proterozoic|||||||
13012|Mount Partridge Group|22810|5|Briefly described|Table2 P4, P12|||Maximum thickness: 5000m||||||09-NOV-06
13012|Mount Partridge Group|22813|5|Briefly described|Map|Paleoproterozoic|Paleoproterozoic|.||||||07-NOV-08
13012|Mount Partridge Group|23216|6|Mentioned|Fig3p5||Paleoproterozoic|||||||07-NOV-08
13012|Mount Partridge Group|23714|4|Described|p9|Proterozoic|Proterozoic|See also page 12. Underlain by Namoona Group. Max. thickness: 1250 m.||||||09-NOV-06
13012|Mount Partridge Group|23715|5|Briefly described|Map legend||Proterozoic|In the Rum Jungle and Central Regions||||||
13012|Mount Partridge Group|23733|5|Briefly described|p32 Fig. 19|||Mount is Mt. in text of figure.||||||
13012|Mount Partridge Group|23999|5|Briefly described|p6 Fig. 3|||Mount is Mt in text of figure.||||||07-FEB-11
13012|Mount Partridge Group|24047|5|Briefly described|p5 Fig.4|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Orogen.  See also p6 Fig. 5.||||||07-NOV-08
13012|Mount Partridge Group|24181|5|Briefly described|p87 Fig.2|Paleoproterozoic|Paleoproterozoic|Unconformably overlies Namoona Group, unconformably overlain by South Alligator Group. Written Mt in text. Geological Province: Pine Creek Inlier.||||||07-NOV-08
13012|Mount Partridge Group|24260|6|Mentioned|p1013 Fig.1|||Geological Province: Pine Creek Inlier||||||
13012|Mount Partridge Group|24442|6|Mentioned|p30, p43|||Dolostone.  Of the Pine Creek Orogen. Unconformably overlain by the Geolsec Formation.  Intruded by the Zamu Dolerite.||||||
13012|Mount Partridge Group|36535|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13012|Mount Partridge Group|36635|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13012|Mount Partridge Group|37462|4|Described|Table 4.II|||||||||
13012|Mount Partridge Group|37579|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes the Wildman Siltstone and Mundogie Sandstone.||||||07-NOV-08
13012|Mount Partridge Group|37815|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13012|Mount Partridge Group|38239|6|Mentioned|Fig.2|||||||||
13012|Mount Partridge Group|38349|4|Described|p13|||||||||
13012|Mount Partridge Group|38884|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13012|Mount Partridge Group|39068|5|Briefly described|Map legend|Proterozoic|Proterozoic|Includes the Wildman Siltstone.||||||14-FEB-06
13012|Mount Partridge Group|39069|4|Described|p6|||||||||
13012|Mount Partridge Group|39320|6|Mentioned|Fig.1|||||||||
13012|Mount Partridge Group|39357|4|Described|p7|||||||||
13012|Mount Partridge Group|39518|4|Described|p3|||See also p6.||||||09-NOV-06
13012|Mount Partridge Group|39563|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13012|Mount Partridge Group|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13012|Mount Partridge Group|39801|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Sandstone, siltstone, shale, quartzite, arkose, conglomerate, dolomite; schist and gneiss in east.||||||07-NOV-08
13012|Mount Partridge Group|40104|6|Mentioned|p349|||||||||
13012|Mount Partridge Group|40168|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Sandstone, siltstone, shale, quartzite, arkose, conglomerate, dolomite; schist and gneiss in east.||||||07-NOV-08
13012|Mount Partridge Group|40223|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Sandstone, siltstone, shale, quartzite, arkose, conglomerate, dolomite; schist and gneiss in east.||||||07-NOV-08
13012|Mount Partridge Group|40243|6|Mentioned|Fig.2|||||||||
13012|Mount Partridge Group|40492|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13012|Mount Partridge Group|40493|4|Described|p6|||||||||
13012|Mount Partridge Group|40495|6|Mentioned|Fig.3|||||||||
13012|Mount Partridge Group|40765|6|Mentioned|Fig.3|||||||||
13012|Mount Partridge Group|40808|3|Fully described|p3|||||||||
13012|Mount Partridge Group|40809|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13012|Mount Partridge Group|40823|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13012|Mount Partridge Group|40852|5|Briefly described|p25|||||||||
13012|Mount Partridge Group|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13012|Mount Partridge Group|40973|6|Mentioned|p195|||||||||
13012|Mount Partridge Group|41125|6|Mentioned|Fig.6|||||||||
13012|Mount Partridge Group|41304|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
13012|Mount Partridge Group|41305|3|Fully described|p10|||||||||
13012|Mount Partridge Group|41309|4|Described|p3|||||||||
13012|Mount Partridge Group|41311|4|Described|p5|||||||||
13012|Mount Partridge Group|41397|4|Described|p7|||||||||
13012|Mount Partridge Group|41406|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
13012|Mount Partridge Group|41407|6|Mentioned|Map legend|Proterozoic||||||||
13012|Mount Partridge Group|41586|6|Mentioned|Map legend|||||||||
13012|Mount Partridge Group|41645|6|Mentioned|Fig.6|||||||||
13012|Mount Partridge Group|41661|6|Mentioned|p26|||See also Fig.6||||||
13012|Mount Partridge Group|41663|6|Mentioned|p14|||||||||
13012|Mount Partridge Group|41873|6|Mentioned|Fig.3|||||||||
13012|Mount Partridge Group|41874|6|Mentioned|Fig.7|||||||||
13012|Mount Partridge Group|41878|6|Mentioned|p34|||||||||
13012|Mount Partridge Group|41980|6|Mentioned|p585|||||||||
13012|Mount Partridge Group|42012|6|Mentioned|p10|||||||||
13012|Mount Partridge Group|42014|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
13012|Mount Partridge Group|42202|6|Mentioned|p510|||||||||
13012|Mount Partridge Group|42927|5|Briefly described|p428|||see also Fig.1 p429, Fig.2 p430.||||||09-NOV-06
13012|Mount Partridge Group|43115|5|Briefly described|p181|||Mount is Mt in text.||||||09-NOV-06
13012|Mount Partridge Group|43140|5|Briefly described|p2||Paleoproterozoic|||||||07-NOV-08
13012|Mount Partridge Group|43187|5|Briefly described|p4|||||||||
13012|Mount Partridge Group|43595|5|Briefly described|p351|||||||||
13012|Mount Partridge Group|43624|6|Mentioned|Table 1,p9||Paleoproterozoic|||||||07-NOV-08
13012|Mount Partridge Group|43720|5|Briefly described|p4||Paleoproterozoic|||||||07-NOV-08
13012|Mount Partridge Group|43832|3|Fully described|13-15,97||Paleoproterozoic|Minimum age 1890 Ma.  Within Pine Ck Geosyncline. Underlain by Namoona Gp, overlain by S AlligatorGp||||||07-NOV-08
13012|Mount Partridge Group|46639|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes Mundogie Sandstone and Wildman Siltstone.||||||07-NOV-08
13012|Mount Partridge Group|46658|6|Mentioned|p550|||||||||
13012|Mount Partridge Group|46675|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes Wildman Sltst, Whites Fm, Coomalie Dolomite and Crater Fm.  Unconformably overlain by South Alligator Gp; unconformably overlies the Namoona Gp. Intruded by Shoobridge, Burnside, Margaret, Fenton and Cullen Granites, and Zamu Dolerite.||||||07-NOV-08
13012|Mount Partridge Group|46700|6|Mentioned|Table1 P10|||||||||
13012|Mount Partridge Group|47049|6|Mentioned|Fig.2|||||||||
13012|Mount Partridge Group|50623|4|Described|p259 Fig.2|Paleoproterozoic|Paleoproterozoic|Unconformably overlies Manton Group, unconformably overlain by South Alligator Group.||||||07-NOV-08
13012|Mount Partridge Group|60526|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Includes: Wildman Siltstone, Mundogie Sandstone.||||||
13012|Mount Partridge Group|60550|5|Briefly described|Map Legend|Proterozoic|Proterozoic|||||||
13012|Mount Partridge Group|60575|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Includes the Wildman Siltstone, Whites Formation, Coomalie Dolomite and Crater Formation.||||||07-NOV-08
13012|Mount Partridge Group|60677|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Overlies Manton Group. Overlain by South Alligator Group.||||||11-JAN-05
13012|Mount Partridge Group|60680|5|Briefly described|Map legend|Orosirian|Orosirian|Includes: Wildman Siltstone and Mundogie Sandstone.  Geological Province: Pine Creek Orogen.||||||14-JAN-05
13012|Mount Partridge Group|61389|5|Briefly described|Map Legend|||||||||
13012|Mount Partridge Group|61827|5|Briefly described|p158 Fig. 4|||Mount is Mt in text.||||||
13012|Mount Partridge Group|61861|6|Mentioned|Fig.2.|||Pine Creek.||||Unconformably overlies Namoona Group. Is unconformably overlain by South Alligator Group.||
13012|Mount Partridge Group|62375|5|Briefly described|p8 Table 1, 9 table 2, 10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Sandstone, siltstone, arkose, shale, conglomerate, quartzite, carbonaceous siltstone and shale, dolostone, magnesite. Thickness: <5000m. Geological Province: Pine Creek Orogen.||||||09-FEB-10
13012|Mount Partridge Group|62378|5|Briefly described|p12|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Orogen.||||||07-NOV-08
13012|Mount Partridge Group|63866|5|Briefly described|p109|||Central Domain, Pine Creek Orogen.|||Includes the Wildman Siltstone.|||
13012|Mount Partridge Group|64676|6|Mentioned|v, p19||||||Wildman Siltstone.|||
13012|Mount Partridge Group|64698|5|Briefly described|lithinterp table|Orosirian|Paleoproterozoic|Age~ 1862-2500Ma. Includes Coomalie Dolostone, Crater Formation, Mundogie Sandstone, Whites Formation, Wildman Siltstone and unnamed conglomerate.||||||07-JAN-09
13012|Mount Partridge Group|64722|5|Briefly described|Fig. 2 p3-6, p9, 24|Orosirian|Orosirian|Part of an older component (2030-2020 Ma) of Central Domain of Pine Creek Orogen||||||
13012|Mount Partridge Group|64730|5|Briefly described|p125 Fig. 3, p126, p138, 139|Paleoproterozoic|Paleoproterozoic|5000m thick. Age from age of volcanics in Wildman Siltstone.|Min. deposition age 2019 +/- 4 Ma.||Includes Whites Formation, Coomalie Dolostone, Koolpinyah Dolostone, Crater Formation, Mundogie Sandstone and Wildman Siltstone.|Unconformably underlies South Alligator Group.||02-MAY-12
13012|Mount Partridge Group|64731|5|Briefly described|p147|Proterozoic|Proterozoic|Central Domain, Pine Creek Orogen.||||Unconformably overlain by South Alligator Group.||12-APR-12
13012|Mount Partridge Group|64956|6|Mentioned|p70|||Contains Mundogie Sandstone and Wildman Siltstone. Unconformably overlies Namoona and Manton Groups; unconformably overlain by South Alligator Group.||||||07-FEB-11
13012|Mount Partridge Group|65232|5|Briefly described|p45, p51-52, p7, p6 Fig. 5, p5 Fig. 4|Palaeoproterozoic|Palaeoproterozoic|Incl: Wildman Siltst, Mundogie Sst, Whites Fm, Coomalie Dolost, Crater Fm. Unconf: over Manton Gp; under Koolpin Fm. Thrust over Depot Creek Sst and Geolsec Fm. Fault: Rum Jungle Complex. Zamu Dolerite intrudes. Age: 2025Ma SHRIMP U-Pb zircon.||||||09-FEB-10
13012|Mount Partridge Group|65339|6|Mentioned|p5 Fig.4, p6 Table 1, pp8-12. ||||||Includes Crater and Whites Formations; Coomalie and Koolpinyah Dolostones; Wildman Siltstone.|||
13012|Mount Partridge Group|66683|5|Briefly described|p368, p377. |Paleoproterozoic|Paleoproterozoic|Formerly correlated with Cahill Formation; zircon detrital spectra are markedly dissimilar, suggesting different depocentres.||Unit in Woodcutters Supergroup.|Includes Whites Formation.|||11-OCT-11
13012|Mount Partridge Group|67127|6|Mentioned|p175|Proterozoic|Proterozoic|Prospective for U-REE mineralisation. Hosts known unconformity-related vein-type U-Au mineralisation.||||||
13012|Mount Partridge Group|67186|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Unit in Woodcutters Supergroup|Includes Crater and White's Formations, Coomalie Dolostone and Wildman Siltstone.|||23-NOV-11
13012|Mount Partridge Group|67232|5|Briefly described|p4. |||Central Domain, Pine Creek Orogen.|||Includes Wildman Siltstone.|||
13012|Mount Partridge Group|67355|5|Briefly described|p6, p7 Fig.5, p10, p12, p15, p47 Fig.38|Orosirian|Paleoproterozoic|Age from zircons in tuffaceous sediments. Synrift sedimentation. Possibly exposed subaerially prior to deposition of the South Alligator Group, via minor uplift or sea level fall.|2026 +/- 5 Ma (SHRIMP zircon)|Woodcutters Supergroup|Crater Formation, Coomalie Dolostone, Whites Formation and Wildman Siltstone.|||25-JAN-17
13012|Mount Partridge Group|67564|4|Described|p iv, p8 Table 2, p10 Fig.5, pp14-19.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Deformed and metamorphosed to greenschist facies during the 1860 - 1850 Ma Nimbuwah Event.|2050 - 1900? Ma.||Includes Mundogie Sandstone, Wildman Siltstone and Nourlangie Schist.|Unconformably overlies Namoona Group. Is disconformably overlain by South Alligator Group.|Siliciclastic sedimentary rocks.|
13012|Mount Partridge Group|67779|5|Briefly described|p5 Fig.4(b), p19.|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen. Previous correlations with Cahill Formation have been found to be erroneous, based on recent SHRIMP and LA-ICPMS U-Pb detrital zircon analyses.|2019 +/- 4 Ma (Worden et al. 2008a,b).|Upper unit in Woodcutters Supergroup.|Includes Crater and Whites Formations; Mundogie Sandstone; Coomalie and Koolpinyah Dolostones, and Wildman Siltstone.|||
13012|Mount Partridge Group|69419|5|Briefly described|p4:3 Fig.4.3, 4:5|Orosirian|Orosirian|W. Pine Creek Orogen. Appears as Upper Mount Partridge Group in Fig.4.3 but not in the Index; thus presumably not intended as a formal name.|c.2019 Ma.||Wildman Siltstone.|||12-JUL-16
13012|Mount Partridge Group|69420|3|Fully described|p5:2, 4, 6, 8-11, 15-16, 24-25, 31, 67|Paleoproterozoic|Paleoproterozoic|See also 79, 93, 103, 105, 116. Formerly Mount Partridge Formation (as cited in Walpole et al., 1968). Central Domain, Pine Creek Orogen. Lower greenschist facies. Maximum deposition ages of constituent units. A 160 m.y. hiatus followed the end of deposition. Deformation mentioned. Similar (detrital zircon) provenance with Kakadu and Manton Groups, but not with Cahill Formation and Nourlangie Schist: previous correlation with those units is not valid. Hosts Sn sulfide vein deposits.|2284 +/- 18 Ma to 2019 +/- 4 Ma.|Woodcutters Supergroup.|Crater, Whites Formations; Mundogie Sandstone; Wildman Siltstone; Coomalie, Koolpinyah Dolostones.|Unconformably overlies Manton and Namoona Groups. Is overlain unconformably by South Alligator Group.|A succession of fluvial to shallow-marine sandstones, succeeded by thick shales or local stromatolitic carbonate rock, followed by thick carbonaceous mud interbedded with dololutite.|12-JUL-16
13012|Mount Partridge Group|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. The undivided unit (under cover) and its constituents are mapped separately.||Of Woodcutters Supergroup.|Includes Wildman Siltstone, Whites Formation, Coomalie Dolostone, Crater Formation, Mundogie Sandstone.|Unconformably overlies Manton Group. Is overlain unconformably by South Alligator Group.||28-FEB-18
13012|Mount Partridge Group|71302|5|Briefly described|p73|Archean|Archean|Geological province: Pine Creek Orogen.|||Includes Crater Formation.|||
13012|Mount Partridge Group|72527|6|Mentioned|p192.|Orosirian|Orosirian|Of the central Pine Creek Orogen (Worden et al., 2008). Includes c. 2020 Ma tuffs.|||||Includes tuffs.|
13064|Mount Rigg Group|9538|5|Briefly described|Map legend|Proterozoic|Proterozoic|Pink and white flaggy quartz sandstone.||||||28-OCT-04
13064|Mount Rigg Group|22479|5|Briefly described|fig4, pg10|Calymmian|Calymmian|||||||
13064|Mount Rigg Group|22538|4|Described|P715, P718|||Mount actually spelt Mt. Part of the Favenc package.||||||09-NOV-06
13064|Mount Rigg Group|22600|4|Described|Map legend|Calymmian||||||||
13064|Mount Rigg Group|22808|6|Mentioned|7 fig 4|||||||||
13064|Mount Rigg Group|23216|4|Described|Fig3p5,Table1p8,30|Calymmian|Statherian|Consists of: Margaret Hill Comglomerate, Bone Creek Sandstone and Dook Creek Formation.||||||
13064|Mount Rigg Group|23374|3|Fully described|Tb2p10,18,19,5,6,20,30,34,35|Calymmian|Statherian|Age: 1615-1575Ma. Consists of Bone Creek Sandstone and Dook Creek Formation. Correlative of Nathan Group. In the McArthur Basin.||||||09-NOV-06
13064|Mount Rigg Group|23396|5|Briefly described|p 407 fig.2|||||||||
13064|Mount Rigg Group|23867|4|Described|p14|Mesoproterozoic|Paleoproterozoic|Geological  Province: McArthur Basin.  See also Table 1.||||||07-NOV-08
13064|Mount Rigg Group|23937|5|Briefly described|p24 Tb. 2, p13|Calymmian|Statherian|Of the Roper Group.  Includes Dook Creek Formation and Bone Creek Sandstone. Overlain by Limmen Sandstone; overlies the West Branch Volcanics.  Geological Province: McArthur Basin.||||||07-JAN-09
13064|Mount Rigg Group|24047|5|Briefly described|p12 Fig. 10|Mesoproterozoic|Mesoproterozoic|Geological Province: McArthur Basin.||||||
13064|Mount Rigg Group|24048|4|Described|p68|Calymmian|Calymmian|Geological Province: McArthur Basin.||||||
13064|Mount Rigg Group|24049|5|Briefly described|Map Legend|Calymmian|Calymmian|Mount is Mt in text. Includes Dook Creek Formation. Geol. Prov: McArthur Basin.||||||13-OCT-05
13064|Mount Rigg Group|24050|3|Fully described|p31, p9 Tb. 2|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
13064|Mount Rigg Group|24051|5|Briefly described|Map Legend|Calymmian|Statherian|Geological Province: McArthur Basin.||||||
13064|Mount Rigg Group|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
13064|Mount Rigg Group|32660|4|Described|Table 4|||||||||
13064|Mount Rigg Group|34287|6|Mentioned|p36|||See also p37.||||||09-NOV-06
13064|Mount Rigg Group|35114|6|Mentioned|Fig.5|||Originally entered as Qld unit. Probably a mistake [CEBAug95]||||||
13064|Mount Rigg Group|36473|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
13064|Mount Rigg Group|37462|4|Described|Table4.IV|||||||||
13064|Mount Rigg Group|37565|6|Mentioned|Fig.5|||||||||
13064|Mount Rigg Group|37568|6|Mentioned|p79|||||||||
13064|Mount Rigg Group|37569|6|Mentioned|p90|||||||||
13064|Mount Rigg Group|37579|5|Briefly described|Regional setting map legend|Carpentarian|Carpentarian|Sandstone, conglomerate, limestone.||||||10-OCT-05
13064|Mount Rigg Group|38243|6|Mentioned|p354|||||||||
13064|Mount Rigg Group|38884|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
13064|Mount Rigg Group|39210|6|Mentioned|p50|||||||||
13064|Mount Rigg Group|39563|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
13064|Mount Rigg Group|39801|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Sandstone, conglomerate, limestone.||||||05-OCT-05
13064|Mount Rigg Group|40105|6|Mentioned|p316|||||||||
13064|Mount Rigg Group|40168|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Sandstone, conglomerate, limestone.||||||18-OCT-05
13064|Mount Rigg Group|40223|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Sandstone, conglomerate, limestone.||||||19-OCT-05
13064|Mount Rigg Group|40823|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
13064|Mount Rigg Group|41019|5|Briefly described|p243|||||||||
13064|Mount Rigg Group|41406|6|Mentioned|Map legend|Mesoproterozoic||||||||
13064|Mount Rigg Group|41407|6|Mentioned|Map legend|Mesoproterozoic||||||||
13064|Mount Rigg Group|41586|6|Mentioned|Map legend|||||||||
13064|Mount Rigg Group|42597|5|Briefly described|Map Legend|Carpentarian||||||||
13064|Mount Rigg Group|43010|2|Defined|p139-148|Mesoproterozoic|Paleoproterozoic|Of Statherian or Calymmian age.||||||28-MAR-18
13064|Mount Rigg Group|43149|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|of Calymmian or Statherian age.||||||07-NOV-08
13064|Mount Rigg Group|43292|5|Briefly described|Map Legend||Mesoproterozoic|||||||
13064|Mount Rigg Group|44112|3|Fully described|p2,Table11p63,66-67|Calymmian|Calymmian|Age: between ~1600 and ~1430 Ma.||||||09-NOV-06
13064|Mount Rigg Group|44201|14|Not recorded|p.7||Neoproterozoic|U.Proterozoic.||||||
13064|Mount Rigg Group|44400|2|Defined|p.7,8,11,12,Tb.1|||Mt.Marumba. (D53-6), opp.p.6, map.||||||
13064|Mount Rigg Group|44401|14|Not recorded|map legend|||Lower (?) Proterozoic.||||||
13064|Mount Rigg Group|44471|14|Not recorded|p.7,8,13, opp.7, map|||(D53-10). Here includes Dook Creek and Bone Creek Formations.||||||09-NOV-06
13064|Mount Rigg Group|44472|5|Briefly described|map legend|||Includes the Dook Creek and Bone Creek Formations.  Mount is Mt in map legend.  Lower (?) Proterozoic.||||||02-DEC-04
13064|Mount Rigg Group|45022|4|Described|p.74||Carpentarian|On many pages.||||||09-NOV-06
13064|Mount Rigg Group|45064|5|Briefly described|p14|||||||||
13064|Mount Rigg Group|45162|6|Mentioned|p136|||||||||
13064|Mount Rigg Group|46163|14|Not recorded|p.168,170||Neoproterozoic|||||||
13064|Mount Rigg Group|46675|5|Briefly described|Map legend for regional setting...|Mesoproterozoic|Mesoproterozoic|Sandstone, conglomerate, limestone.   Geological Province: Pine Creek Geosyncline.||||||
13064|Mount Rigg Group|46679|14|Not recorded|map legend||Neoproterozoic|Upper Proterozoic.||||||
13064|Mount Rigg Group|46861|6|Mentioned|p5|||||||||
13064|Mount Rigg Group|50225|5|Briefly described|p406 Fig. 10, p407|Mesoproterozoic|Paleoproterozoic|Geological Province: McArthur Basin.  Mount is Mt. in text.||||||07-FEB-11
13064|Mount Rigg Group|60526|5|Briefly described|Map Legend|Carpentarian|Carpentarian|Sandstone, conglomerate, limestone.||||||
13064|Mount Rigg Group|60571|5|Briefly described|Map legend|Calymmian|Calymmian|Includes the Dook Creek Formation and Bone Creek Formation. Mount is Mt in map legend. Geological Province: McArthur Basin.||||||30-NOV-04
13064|Mount Rigg Group|60573|5|Briefly described|Map legend|Calymmian|Statherian|Includes Dook Creek Formation and Bone Creek Sandstone. Mount is Mt in text of legend. Do not outcrop in the ROPER RIVER mapsheet area.||||||09-NOV-06
13064|Mount Rigg Group|60574|5|Briefly described|Map Legend|||Geological Province: McArthur Basin.||||||
13064|Mount Rigg Group|60680|5|Briefly described|Map legend|Statherian|Statherian|Geological Province: McArthur  Basin.||||||
13064|Mount Rigg Group|61390|5|Briefly described|Map Legend|Calymmian|Statherian|||||||
13064|Mount Rigg Group|61403|5|Briefly described|Map Legend|Calymmian|Calymmian|Mount is Mt in text. Includes Dook Creek Formation. Geol. Prov: McArthur Basin.||||||
13064|Mount Rigg Group|61572|5|Briefly described|p667 Fig. 2|||Includes Dook Creek Formation and Bone Creek Sandstone. Rocks deformed by the Gulpuliyul impact structure. Overlies the Katherine River Group. Geological Province: McArthur Basin. Mount is Mt in text. See also p671 Tb. 1.||||||07-JAN-09
13064|Mount Rigg Group|63866|5|Briefly described|p113-p114|||Isa Superbasin.|<1710 Ma (unit relationships)|||Unconformably overlain by the Roper Group. Unconformably overlies the Katherine River Group and West Branch Volcanics. Equivalent to the Nathan Group.|Dolostones and sandstones.|
13064|Mount Rigg Group|64698|4|Described|lithinterp table|Calymmian|Statherian|Age ~1500-1705Ma. McArthur Basin. Max. thickness 520m. Succession of basal conglomerate followed by quartz sandstone, mudstone and laminated dolostone.||||||07-JAN-09
13064|Mount Rigg Group|64724|5|Briefly described|p46|Proterozoic|Proterozoic|McArthur Basin unit deposited as part of sedimentation in the Isa Superbasin (1660-1590 Ma)||||||
13064|Mount Rigg Group|64817|6|Mentioned|p352 Fig.3, p353 Fig.4 ||||||Includes the Dook Creek Formation, Bone Creek Sandstone, Margaret Hill Conglomerate.|||
13064|Mount Rigg Group|65232|5|Briefly described|p8, p5 Fig. 4|||Unconformably overlies Katherine River Group. Shallow-marine clastic sedimentary and carbonate rocks. Age: 1600 Ma. Presented as Nathan and Mount Rigg groups on figure. Geol. Prov: Pine Creek Orogen.||||||09-FEB-10
13064|Mount Rigg Group|65340|6|Mentioned|pp10-11.|||Arnhem Shelf, McArthur Basin.||||||
13064|Mount Rigg Group|67323|6|Mentioned|Eastern Australia Time-Space Plot|||McArthur region.||||||
13064|Mount Rigg Group|67564|4|Described|p iv, p6 Table 2, p10 Fig.5, p49, p51.|Paleoproterozoic|Paleoproterozoic|McArthur Basin. Largely undeformed sedimentary (mixed siliciclastic - dolomitic succession) and volcanic rocks. Correlative of Nathan Group in southern McArthur Basin.|1613 - 1590 Ma.||Includes Bone Creek Sandstone and Dook Creek Formation.|Disconformably overlies Katherine River Group.||
13064|Mount Rigg Group|69417|6|Mentioned|p2:5|Calymmian|Statherian|McArthur Basin.||||||12-JUL-16
13064|Mount Rigg Group|69430|5|Briefly described|p15:2-4, 8, 23-25, 30|||NW McArthur Basin. In Dunn (1963), this Group comprised the Bone Creek and Dook Creek Formations.|||Margaret Hill Conglomerate, Bone Creek Sandstone, Dook Creek Formation.|Unconformably overlies West Branch Volcanics (Katherine River Group). Is overlain unconformably by Roper Group.||12-JUL-16
13064|Mount Rigg Group|69673|6|Mentioned|p3 fig 2, p15, p19|Paleoproterozoic|Paleoproterozoic||||Includes Dook Creek Formation, Bone Creek Sandstone, Margaret Hill Conglomerate|||
13064|Mount Rigg Group|70897|5|Briefly described|p43|||Southern Arnhem Land. Eroded (500-1000m) and a regolith developed before being buried.||||Equivalent to Nathan Group. Is overlain disconformably by Roper Group.||
13064|Mount Rigg Group|70968|5|Briefly described|p2 Fig.3, p6, p13||||||Dook Creek Formation.|Is overlain unconformably by Limmen Sandstone (Roper Group).||
13064|Mount Rigg Group|71059|5|Briefly described|p1-2|Mesoproterozoic|Mesoproterozoic|McArthur Basin.||||Is overlain unconformably by Roper Group.||
13064|Mount Rigg Group|71374|6|Mentioned|p2|||northern McArthur Basin.||||Equivalent to the Bullita and Wattie Groups.||
13064|Mount Rigg Group|71606|5|Briefly described|p135,137-138|Calymmian|Calymmian|East Arnhem Shelf, McArthur Basin. Evaporite-carbonate sequence  deposited in a broad sag basin across most of the region with no evidence of tectonic control from previous rifts.||||Overlain unconformably by Roper Group. Underlain unconformably by Nimbuwah Complex. Correlable to Karns Dolomite and Nathan Group.||
13064|Mount Rigg Group|71632|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|McArthur Basin.|||||Cyclic coarse-grained chertified evaporitic-stromatolitic-ooidal dolostone, sandstone, siltstone.|
13064|Mount Rigg Group|71779|5|Briefly described|p5|Mesoproterozoic|Palaeoproterozoic|McArthur Basin.||||Disconformably or unconformably overlain by the Roper Group.||
13064|Mount Rigg Group|72373|5|Briefly described|p2,27|Mesoproterozoic|Mesoproterozoic|Of northern McArthur Basin. Broadly equivalent to Favenc package, Nathan Group and Karns Dolostone (McArthur Basin), Bullita and Wattie groups (Birrindudu Basin) and Namerinni Group (Tomkinson Province).|||Includes Bone Creek Sandstone, Dook Creek Formation.|||
13064|Mount Rigg Group|72718|6|Mentioned|p5 Tb.1|||McArthur Basin. Isa Superbasin of Jackson et al. (1999, 2000). Favenc package.||||||
13064|Mount Rigg Group|73242|6|Mentioned|p39|||||||Overlain by[?] Phelp Sandstone, Collara Subgroup, Roper Group.||
13087|Mount Sanford Formation|14019|4|Described|p19|||Of the Wattie Group. Siltstone, dolostone, sandstone, mudstone, chert, rare claystone and tuffite. Conformably overlies Hughie Sandstone; overlain by remnants of the Neave Sandstone. Max. thickness >200m. Geological Province: Victoria Basin.||||||
13087|Mount Sanford Formation|23809|5|Briefly described|p52|||Geological Province: Victoria River Basin.||||||
13087|Mount Sanford Formation|24122|5|Briefly described|p4 Fig.3|||Of Wattie Group.  Geological Province: Victoria Basin.||||||
13087|Mount Sanford Formation|24297|3|Fully described|p6|Proterozoic|Proterozoic|Of Wattie Group. Disconformably overlain by Neave Sandstone, conformably overlies Hughie Sandstone. Maximum thickness: 200m.  See also p5 Tb. 2.||||||
13087|Mount Sanford Formation|24298|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Mount in Mt in text. Of the Wattie Group. Dolomitic siltstone, dolostone, sandstone, minor chert.||||||09-NOV-06
13087|Mount Sanford Formation|24441|5|Briefly described|p1 Fig. 1|Mesoproterozoic|Mesoproterozoic|Of the Wattie Group. Unconformably overlies Hughie Sandstone;  unconformably overlain by Neave Sandstone. Geological Province: Victoria Basin.||||||
13087|Mount Sanford Formation|24442|5|Briefly described|p50 Fig. 1|||Of the Wattie Group. Geological Province: Victoria Basin.||||||
13087|Mount Sanford Formation|28255|3|Fully described|p36, Tb. 11 (opp. p8)|Adelaidean|Adelaidean|Of the Wattie Group. Siltstone, dolomite and claystone. Conformably overlain by Neave Sandstone; conformable over Hughie Sandstone. Max. thickness: 250m. Mount is Mt in text. See also p128 Appendix.||||||
13087|Mount Sanford Formation|30003|4|Described|p8, p12|||Of the Wattie Group. Overlain by the Neave Sandstone. Max. thickness: 49m. Carpentarian or Adelaidean||||||19-APR-05
13087|Mount Sanford Formation|30004|6|Mentioned|Map legend|Proterozoic|Proterozoic|Carpentarian or Adelaidean||||||
13087|Mount Sanford Formation|32172|4|Described|Table 1|||Carpentarian or Adelaidean.||||||09-NOV-06
13087|Mount Sanford Formation|32173|5|Briefly described|Map legend|Adelaidean|Carpentarian|Of the Wattie Group.  Purple and grey-green siltstone, dolomite; minor claystone and fine sandstone.  Carpentarian or Adelaidean (per legend).||||||16-NOV-04
13087|Mount Sanford Formation|32175|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Wattie Group.  Interbedded flaggy dolomitic siltstone, dolomite and fine sandstone; minor silicified claystone.  Mount is Mt in legend.||||||02-DEC-04
13087|Mount Sanford Formation|32660|5|Briefly described|Table 6|||||||||
13087|Mount Sanford Formation|33374|6|Mentioned|p7|||Stratigraphy.||||||
13087|Mount Sanford Formation|33375|5|Briefly described|p7, p8 Tb. 1|Adelaidean|Adelaidean|Of the Wattie Group. Overlain by the Neave Sandstone; overlies the Hughie Sandstone.||||||26-APR-05
13087|Mount Sanford Formation|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
13087|Mount Sanford Formation|33378|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Wattie Group. Chocolate and green siltstone, interbedded fine sandstone; minor dolomite and claystone mainly near the top.||||||27-APR-05
13087|Mount Sanford Formation|45112|6|Mentioned|p19|||||||||
13087|Mount Sanford Formation|48943|2|Defined|p46|Adelaidean|Adelaidean|||||||
13087|Mount Sanford Formation|60589|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Wattie Group.  Dolomitic siltstone, dolostone, sandstone and minor chert.  Geological Province: Victoria Basin.||||||
13087|Mount Sanford Formation|60672|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Dolomitic siltstone, dolostone with chert nodules interbedded with siltstone and sandstone, claystone. Of Wattie Group. Overlies Hughie Formation. Overlain by Neave Sandstone. Geological Province: Victoria Basin.||||||11-JAN-05
13087|Mount Sanford Formation|60685|4|Described|p4 Fig. 3, p6|Mesoproterozoic||Of the Wattie Group. Dolomitic siltstone, mudstone and fine sandstone; subordinate dolostone and chert. Conformable on Hughie Sandstone; disconformably below Neave Sandstone. Max. Thickness: >200m. Geological Province: Victoria Basin.||||||
13087|Mount Sanford Formation|65342|6|Mentioned|p11 Fig.13. |||Victoria Basin.||Unit in Wattie Group.||Overlies Hughie Sandstone. Is unconformably overlain by Neave Sandstone.||
13087|Mount Sanford Formation|67151|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Birindudu Basin.||Unit in Wattie Group.||Overlies Hughie Sandstone. Is overlain by Neave Sandstone, possibly unconformably.|Dolomitic siltstone, interbedded fine sandstone; minor dolostone and claystone, mainly near top.|
13087|Mount Sanford Formation|68733|5|Briefly described|p177 Fig.2, p182|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 Wattie Group.||Unconformably overlain by the Neave Sandstone.||
13087|Mount Sanford Formation|69432|4|Described|p17:2, 9, 14|||Birrindudu Basin. Has local and regional variations in content and thickness. Typically 20-50m thick, but may be over 200m to the N. Has local weak malachite mineralisation.||Wattie Group.||Conformably overlies Hughie Sandstone. Is overlain by Neave Sandstone conformably to locally unconformably.|Interbedded siltstone, dolostone (rarely stromatolitic), fine sandstone, dolomitic mudstone, chert, and rare claystone and tuff. Carbonate content increases up-section in the S.|12-JUL-16
13087|Mount Sanford Formation|69673|6|Mentioned|p48 fig 35|||||Wattie Group||Overlies Hughie Sandstone, unconformably overlain by Neave Sandstone||
13087|Mount Sanford Formation|70655|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Birindudu Basin.||Wattie Group.||Overlies Hughie Sandstone. Is overlain by Neave Sandstone, or Seale Sandstone, possibly unconformably.|Dolomitic siltstone, interbedded fine sandstone; minor dolostone and claystone, mainly near top.|
13087|Mount Sanford Formation|70854|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Wattie Group.||Overlies Hughie Sandstone. Is overlain unconformably? by Neave Sandstone.|Dolomitic siltstone, dolostone with chert nodules interbedded with siltstone and sandstone, claystone.|21-SEP-17
13087|Mount Sanford Formation|70855|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Wattie Group.||Overlies Hughie Sandstone. Is overlain ?unconformably by Neave Sandstone.|Dolomitic siltstone, dolostone, sandstone, minor  chert, claystone.|
13087|Mount Sanford Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||dolostone, siltstone|
13087|Mount Sanford Formation|71302|5|Briefly described|p6,15||Paleoproterozoic|Of Birindudu Basin.||Unit of Wattie Group.||Underlain by Hughie Sandstone.||
13087|Mount Sanford Formation|72718|6|Mentioned|p7|||Birrindudu Basin.||Wattie Group||Underlain by Hughie Sandstone. Unconformably[?] overlain by Neave Sandstone.||
13103|Mount Smith Metamorphics|8217|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block. Meta-arkose, calc-silicate gneiss, biotite schist.||||||
13103|Mount Smith Metamorphics|39921|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13103|Mount Smith Metamorphics|49027|6|Mentioned|p1|||||||||
13103|Mount Smith Metamorphics|69427|5|Briefly described|p12:3, 8, 27|||Warren (1981). Aileron Province. Lower- to  middle-amphibolite facies metamorphism. SHRIMP U-Pb detrital zircon maximum depositional age.|<1777 +/- 19 Ma (Carson et al., 2009).||||Biotite-muscovite metapelitic schist, semi-pelitic gneiss and meta-greywacke, with rare muscovite schist; locally contains andalusite and cordierite; rare fine fibrolite development.|12-JUL-16
13106|Mount Stafford Granite|7838|5|Briefly described|p69-70, 74, 77-78, 80, 82-83, 85, 87|||Emplaced during the first of two tectonic cycles in the northern Arunta Inlier. Zircon analyses tabulated and discussed. Occasionally presented as Mt. Stafford Granite.|1818 +/- 15 Ma.|||Intrudes Lander Rock beds.|Abundant K-feldspar megacrystic and foxy-red biotite granite; rare euhedral cordierite (now mostly recrystallised aggregates of muscovite and greenish biotite). S-type. Abundant xenoliths of country rock. Intruded as a series of sheet-like bodies.|
13106|Mount Stafford Granite|23733|5|Briefly described|p34 Fig.20|||Mount is Mt. in text of figure.  Age: 1818Ma.||||||
13106|Mount Stafford Granite|24047|5|Briefly described|p7 Fig. 6|Paleoproterozoic|Paleoproterozoic|Mount is Mt in text of figure.  Geological Province: Arunta Province.||||||07-NOV-08
13106|Mount Stafford Granite|42146|6|Mentioned|p652|||||||||
13106|Mount Stafford Granite|43749|6|Mentioned|p23|||Age: 1820 Ma.||||||09-NOV-06
13106|Mount Stafford Granite|64956|5|Briefly described|p15|||Previous/alternate name for Anmatjira Orthogeniss - not intended as a formal name. Intruded by Anmatjira Granite, also named Anmatjira Orthogneiss.||||||07-FEB-11
13106|Mount Stafford Granite|69226|5|Briefly described|p239-241|Orosirian|Orosirian|Reynolds-Anmatjira Ranges region.|1818 +/- 15 Ma (Collins and Williams, 1995).|||Intrudes Mount Stafford Beds.||
13106|Mount Stafford Granite|70376|5|Briefly described|p833|Paleoproterozoic|Paleoproterozoic|Formed up to granulite facies contact metamorphic aureole in the Mount Stafford Beds. Dated by Rubatto et al. 2006; Worden et al. 2008)|1802+/-3 Ma, 1795+/-4 Ma|||Intrudes Mt Stafford Beds.||
13106|Mount Stafford Granite|71592|5|Briefly described|Appendix A.|||Arunta Orogen.|1818+/-15 Ma (U-Pb zircon: SHRIMP)||||Granite.|
13125|Mount Swan Granite|9394|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block. Porphyritic granite, partly hornblende bearing.||||||
13125|Mount Swan Granite|23363|5|Briefly described|352 Tab.3|Statherian|Statherian|Age: 1713+/-7Ma.||||||09-NOV-06
13125|Mount Swan Granite|23732|5|Briefly described|p3, 21 Table. 1.|Paleoproterozoic|Paleoproterozoic|Age: 1713 +/- 7Ma (SHRIMP U-Pb; Zhao and Bennett, 1995). Mount is Mt. in text.||||||14-SEP-12
13125|Mount Swan Granite|23733|5|Briefly described|p34 Fig.20|||Mount is Mt. in text of figure.  Age: 1713Ma.||||||
13125|Mount Swan Granite|23844|5|Briefly described|p40|Statherian|Statherian|Age: 1800Ma.||||||09-NOV-06
13125|Mount Swan Granite|23868|5|Briefly described|p741|Paleoproterozoic|Paleoproterozoic|Age: 1713+/-7Ma.  Geological Province: Arunta Inlier.||||||07-NOV-08
13125|Mount Swan Granite|24197|5|Briefly described|p60 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Of the Jinka Suite. Age: 1713Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
13125|Mount Swan Granite|33103|4|Described|Table 2|||||||||
13125|Mount Swan Granite|33104|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
13125|Mount Swan Granite|39888|6|Mentioned|Fig.7|||||||||
13125|Mount Swan Granite|40538|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Hornblende biotite granite, porphyritic, pink. Geological Province: Arunta Block.||||||07-NOV-08
13125|Mount Swan Granite|40906|4|Described|p12|||||||||
13125|Mount Swan Granite|42326|5|Briefly described|Table 2 P11|||||||||
13125|Mount Swan Granite|44327|14|Not recorded|Tb.I,p.7,map||Paleoproterozoic|(F53-11). Lower Proterozoic.||||||07-NOV-08
13125|Mount Swan Granite|44328|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
13125|Mount Swan Granite|46868|6|Mentioned|p76|||||||||
13125|Mount Swan Granite|48844|2|Defined|p.1,14-15|||Pls. 2,8. (new name). Intrudes Brady Gneiss. (F53-11).||||||
13125|Mount Swan Granite|48997|5|Briefly described|p7|||||||||
13125|Mount Swan Granite|50369|5|Briefly described|p1.4, 15.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Jinka Suite.||||||07-NOV-08
13125|Mount Swan Granite|62595|5|Briefly described|p7.|Statherian|Statherian||c.1713 Ma (Zhao and Bennett 1995).|||||
13125|Mount Swan Granite|64068|6|Mentioned|p33|Statherian|Statherian|.|1713 +/- 7 Ma.|||||05-APR-12
13125|Mount Swan Granite|64738|6|Mentioned|p247 Fig.2, p249-250, 251, 253|Statherian|Statherian|Intrudes the Dneiper Granite.|Crystallised 1713 +/- 7 Ma.|||Intrudes Kanandra Granulite. Intrudes the Dneiper Granite.||23-APR-12
13125|Mount Swan Granite|65341|6|Mentioned|p2 Fig.2. |Paleoproterozoic|Paleoproterozoic|||||||
13125|Mount Swan Granite|66860|6|Mentioned|p91|||SHRIMP U-Pb zircon age; an age of 1700 Ma from Pb isotope analysis of K-feldspar compares favourably.|1713 +/- 7 Ma (Zhao and Bennett, 1995).|||||
13125|Mount Swan Granite|67323|6|Mentioned|Eastern Australia Time-Space Plot|||Arunta Block.||||||
13125|Mount Swan Granite|68150|5|Briefly described|p1, p10, p11 Tb.3.2|||Tb. 3.2 contains age measurements in Arunta Region, related to Strangways Event. Zhao and Bennett (1995) calculated 1713  +/-  7 Ma as age of Mount Swan Granite, however, individual measured ages are dispersed with an MSWD of 2.4 and an age range from ca. 1740 to 1680 Ma, with an unexplained outlier at ca. 1630 Ma. Aileron Province. See also Mount Swan Suite.|1724 +/- 6 Ma, Hollis et al., 2010|||||
13125|Mount Swan Granite|69383|5|Briefly described|p66-69, 63, 80|Statherian|Statherian|Arunta region, Aileron Province.  LA-ICPMS U-Pb and Hf geochronology analyses. Crystallisation age. Previously dated by zircon SHRIMP U?Pb analysis at 1713+/-7 Ma by Zhao et al (1995)|1724+/-6 Ma|||In faulted contact with, and intrudes, Kanandra Granulite.|Weakly to non-deformed porphyritic biotite granite.|15-JUL-15
13125|Mount Swan Granite|69417|5|Briefly described|p2:5|Statherian|Statherian|Aileron Province.|1730-1710 Ma.|||||12-JUL-16
13125|Mount Swan Granite|69427|4|Described|p12:3, 7, 40, 62|Statherian|Statherian|Smith (1964), Shaw et al. (1975). Aileron Province. LA-ICPMS U-Pb zircon age. Also 1713 +/- 7 Ma (SHRIMP U-Pb zircon age by Zhao and Bennett, 1995).|1724 +/- 6 Ma (Hollis et al., 2010).|||Intrudes Kanandra Granulite.|Pink, porphyritic, biotite-hornblende granite, characterised by coarse K-feldspar phenocrysts to 10cm long; generally undeformed (except near major faults); locally contains rafts of Perenti Metamorphics.|12-JUL-16
13125|Mount Swan Granite|69510|5|Briefly described|p15|||Magmatic crystallisation ages by SHRIMP U-Pb (Zhao and Bennett, 1995) and LA-ICPMS (Beyer et al., 2012) respectively.|1713 +/- 7 Ma; 1724 +/- 6 Ma.|||||
13125|Mount Swan Granite|69794|6|Mentioned|iv,p10|Statherian|Statherian|Geological province: Aileron Province. Of Arunta Region. Generally undeformed. Previously dated at 1713+\-7 Ma (Zhao and Bennett, 1995) and 1724+\-6 Ma (Hollis et al., 2010).||||||06-APR-20
13125|Mount Swan Granite|69917|6|Mentioned|p85|||||||||
13125|Mount Swan Granite|69925|5|Briefly described|p18, 21, 24-25, 34-35, 37, 39|||Northern Arunta Province, Arunta Inlier. Ion probe U-Pb isotope analyses tabulated. Post-Strangways Event.|1713 +/- 7 Ma (crystallisation).|||Intrudes Perenti Metamorphics and Dneiper Granite. Correlated (lithologically and geochemically) with Mount Ida Granite.|Pink, porphyritic to megacrystic with phenocrysts up to 100mm. Groundmass consists of quartz, orthoclase, plagioclase (An30), hornblende and accessory minerals. Not foliated.|
13125|Mount Swan Granite|69931|6|Mentioned|p269, 273, 282-283, 296|Paleoproterozoic|Paleoproterozoic|Arunta Inlier. REE analyses tabulated.||Mount Swan Suite.|||Megacrystic granite, pink porphyritic granite.|
13125|Mount Swan Granite|71592|5|Briefly described|Appendix A.|||Arunta Orogen.|1724+/-5.9 Ma (U-Pb zircon: LA-ICPMS).||||Granite, porphyroblastic granite.|
13125|Mount Swan Granite|71750|5|Briefly described|iii,p6|Statherian|Statherian|Geological province: Aileron Province. Surrounds and intrudes Perenti Metamorphics. LA-ICP-MS 207Pb/206Pb zircon age of 1724+\-6 Ma (Beyer et al 2013); SHRIMP 207Pb/206Pb zircon age of 1713+\-7 Ma (Zhao and Bennett 1995).|c. 1720 Ma|||Intrudes Perenti Metamorphics.||20-SEP-19
13125|Mount Swan Granite|72370|6|Mentioned|p29|||Geological province: Aileron Province.  Part of a suite of granites emplaced in HUCKITTA map sheet at c. 1725-1715 Ma (along with Marshall Granite, Jinka Granite) (Hollis et al 2010, Weisheit et al in review, Beyer et al in prep).||||||
13125|Mount Swan Granite|72516|6|Mentioned|p192|||Aileron Province.||||Intrudes the Perenti Metamorphics.||
13125|Mount Swan Granite|73591|6|Mentioned|p31|Statherian|Statherian|Includes xenoliths of the Perenti Metamorphics.|ca 1720 Ma|||||
13203|Mount Webb Granite|22716|6|Mentioned|p232|Statherian|Statherian|||||||
13203|Mount Webb Granite|23363|5|Briefly described|352 Tab.3|Statherian|Statherian|||||||
13203|Mount Webb Granite|23396|6|Mentioned|p426|||||||||
13203|Mount Webb Granite|24197|5|Briefly described|p33, p61 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Of Mount Webb Suite. Heterogeneous granite, of several types of unaltered granite, sodic-clacic altered granite, sericite-altered granite and aplite. Age: 1615Ma. Geol. Prov: western Arunta Block. See also p143, p146 for lith.detail.||||||30-JAN-17
13203|Mount Webb Granite|24567|5|Briefly described|p160 Tb. 2|Mesoproterozoic|Mesoproterozoic|Age: 1480Ma. Geological Province: Arunta Inlier. Name written as Mt Webb only under heading for GRANITE.||||||09-MAY-05
13203|Mount Webb Granite|29806|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
13203|Mount Webb Granite|29807|4|Described|Table 1|||||||||
13203|Mount Webb Granite|35201|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
13203|Mount Webb Granite|35223|4|Described|Table.2|||||||||
13203|Mount Webb Granite|36532|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
13203|Mount Webb Granite|39559|6|Mentioned|Table 1|||||||||
13203|Mount Webb Granite|39888|6|Mentioned|Fig.9|||||||||
13203|Mount Webb Granite|41465|6|Mentioned|p13|||||||||
13203|Mount Webb Granite|42504|5|Briefly described|p61|||||||||
13203|Mount Webb Granite|44194|4|Described|p2|Paleoproterozoic|Paleoproterozoic|Co-magmatic with Pollock Hills Formation Felsic Volcanics. SHRIMP ages given 1639+/-5 Ma.||||||07-NOV-08
13203|Mount Webb Granite|45140|2|Defined|p12-13, p22, p26, p28-38, p60-61, p74|Calymmian|Calymmian|See also Appx.p14-15. Blake (1977). Arunta Block. Named after a prominent hill (Mount Webb). Forms scattered groups of spherical boulders and tors up to 30m high; one of these is the type locality, at 22deg 50'00"S, 127deg 50'30"E. A preferred age given is 1526 +/- 25 Ma (Page et al., 1976). Geochemistry detailed.|1520 +/- 40 Ma (Rb-Sr; Page et al., 1976).|||Intrudes Arunta Complex, also (and probably co-magmatic with lavas in) the Pollock Hills Formation. Is overlain unconformably by Heavitree Quartzite.|Pink to grey, medium- to coarse-grained biotite adamellite, locally with hornblende. Locally has a gneissic texture. Cut by rare aplite veins <1m wide, by quartz veins, and by later unfoliated basic dykes.|
13203|Mount Webb Granite|46788|4|Described|p7|||||||||
13203|Mount Webb Granite|50369|5|Briefly described|p1.5, 21.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Mount Web Suite. Age: 1486 +/- 40Ma.||||||07-NOV-08
13203|Mount Webb Granite|61660|5|Briefly described|p23. |Proterozoic|Proterozoic|Western extension of the Warumpi Province.|1639 +/- 5 Ma.|||||
13203|Mount Webb Granite|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Monzogranite; syenogranite, granodiorite, and tonalite.||||||09-DEC-08
13203|Mount Webb Granite|64726|6|Mentioned|p84.|Paleoproterozoic|Paleoproterozoic|||||||
13203|Mount Webb Granite|65074|4|Described|p351, p354 Tb. 4-11, p360-362|Mesoproterozoic|Mesoproterozoic|Type section 32 km WNW of Mount Webb. Probably comagmatic with acid lavas of Pollock Hills Formation.|1520 +/- 40 Ma (Page et al., 1976).|||Intrudes Pollock Hills Formation. Overlain by Heavitree Quartzite unconformably.|Even-grained adamellite.|
13203|Mount Webb Granite|67323|5|Briefly described|p35|Paleoproterozoic|Paleoproterozoic|Arunta Inlier.|~1640 Ma.||||Heterogeneous granite, hornblende-biotite granite, sodic-calcic altered granite, sericite-altered granite, aplite.|
13203|Mount Webb Granite|68994|4|Described|p1, p4-9, p11, p17-18, p23, p26-27|||Warumpi Province. Magmatic crystallisation age. Similar age determinations given. Hf analyses detailed.|1640+/-7 Ma (Kirkland et al. 2009).||||Felsic magmatic rocks. Sample analysed is coarse-grained, foliated, biotite-hornblende metamonzogranite.|13-JAN-17
13203|Mount Webb Granite|69003|5|Briefly described|p5, p32|Paleoproterozoic|Paleoproterozoic|Warumpi Province, West Arunta Orogen. Associated with the c.1640-1635 Ma Liebig Orogeny.|c.1640 Ma.|||Intrudes Ininti Granite.||
13203|Mount Webb Granite|69031|5|Briefly described|p4, p6, p7-8, p12, p15, p27,p43,p59,p67|Statherian|Statherian|Warumpi Province, Arunta Orogen. Previously thought to be coeval with Pollock Hills Formation; geochronology establishes a c.30 m.y. separation. Several similar age determinations given. A large gold (and numerous other metals) anomaly occurs in regolith within this unit's area. Magnetic susceptibility data. Distance to this unit was used as a predictor in modelling for U sources and orogenic Au systems.|1640 +/- 7 Ma (Kirkland et al., 2009).||||Granite, granodiorite, aplite, albitite, porphyry, tonalite. Has undergone local extensive magmatic sodic-calcic and sericitic alteration.|
13203|Mount Webb Granite|70762|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Warumpi Province, Arunta Orogen, North Australian Craton.|||||Metamonzogranite, metasyenogranite, metagranodiorite and metatonalite.|
13203|Mount Webb Granite|70826|6|Mentioned|p10|Paleoproterozoic|Paleoproterozoic|||||||
13203|Mount Webb Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
13203|Mount Webb Granite|71592|5|Briefly described|Appendix A.|||Warumpi Province, Arunta Orogen.|1640+/-7 Ma (crystallisation: U-Pb zircon SHRIMP)||||Monzogranite.|
13203|Mount Webb Granite|71810|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Warumpi Province, Arunta Orogen, North Australian Craton.|c.1640 Ma.||||Metamonzogranite; locally metasyenogranite, metagranodiorite, and metatonalite.|
13203|Mount Webb Granite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Warumpi Province, Arunta Orogen.|Max age 1647+/-7 Ma, min 1633+/-7 Ma.||||Metamonzogranite; metasyenogranite, metagranodiorite, and metatonalite.|
13237|Mount Winnecke Formation|22446|4|Described|p19|Orosirian|Orosirian|||||||
13237|Mount Winnecke Formation|22716|6|Mentioned|table4,p231|Proterozoic|Proterozoic|||||||
13237|Mount Winnecke Formation|23621|5|Briefly described|p39|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13237|Mount Winnecke Formation|23809|5|Briefly described|p3 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of the Mount Winnecke Group.  Age: 1824+/-5Ma.||||||07-NOV-08
13237|Mount Winnecke Formation|24197|5|Briefly described|p26, p82|||Part of the Granites Supersuite; formed from altered and greisenised comagmatic volcanics of the Winnecke Granophyre. Age: 1810Ma. Geological province: The Granites-Tanami Block. See also p82 Tb. 10.1.||||||07-FEB-11
13237|Mount Winnecke Formation|29804|4|Described|Table 1|||||||||
13237|Mount Winnecke Formation|29805|4|Described|Table 1|||||||||
13237|Mount Winnecke Formation|29809|5|Briefly described|p417|||||||||
13237|Mount Winnecke Formation|29811|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13237|Mount Winnecke Formation|29813|6|Mentioned|Table 2|||||||||
13237|Mount Winnecke Formation|31361|4|Described|Table 2|||||||||
13237|Mount Winnecke Formation|31362|6|Mentioned|Table 1|||||||||
13237|Mount Winnecke Formation|31412|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13237|Mount Winnecke Formation|31413|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13237|Mount Winnecke Formation|32659|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13237|Mount Winnecke Formation|33102|6|Mentioned|Fig.2|||||||||
13237|Mount Winnecke Formation|35224|4|Described|Table 1|||See also p5.||||||09-NOV-06
13237|Mount Winnecke Formation|35231|4|Described|Table.1|||||||||
13237|Mount Winnecke Formation|35950|6|Mentioned|p303|||||||||
13237|Mount Winnecke Formation|36308|6|Mentioned|p212|||||||||
13237|Mount Winnecke Formation|36473|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13237|Mount Winnecke Formation|36532|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13237|Mount Winnecke Formation|37462|6|Mentioned|p234,p279|||||||||
13237|Mount Winnecke Formation|39571|6|Mentioned|p130|||||||||
13237|Mount Winnecke Formation|39887|6|Mentioned|p453|||||||||
13237|Mount Winnecke Formation|39888|6|Mentioned|Appendix|||Published isotopic ages.||||||
13237|Mount Winnecke Formation|41204|6|Mentioned|p10|||||||||
13237|Mount Winnecke Formation|41465|5|Briefly described|p9|||||||||
13237|Mount Winnecke Formation|41883|5|Briefly described|p65|||Shown as Mount Winnecke Formation in Fig.49||||||
13237|Mount Winnecke Formation|41961|6|Mentioned|Table 1 P39|||||||||
13237|Mount Winnecke Formation|41970|6|Mentioned|p336|||||||||
13237|Mount Winnecke Formation|42504|5|Briefly described|p59|||||||||
13237|Mount Winnecke Formation|42643|6|Mentioned|p5|||||||||
13237|Mount Winnecke Formation|43595|5|Briefly described|p353|||Dated (Rb-Sr) at 1764+/-15 Ma.||||||09-NOV-06
13237|Mount Winnecke Formation|43631|6|Mentioned|p10|||||||||
13237|Mount Winnecke Formation|45140|2|Defined|p12-15, p18, p20-23, p29-30, p32-34, p36|Paleoproterozoic|Paleoproterozoic|See also p38-39, p41, p54, p73-74, p82, Appx.p6-7. Blake et al. (1975). Named after Mount Winnecke. The Granites-Tanami Block. Mapped as Mount Winnecke Sandstone by Traves (1955); renamed because of the voluminous acid volcanics in the sequence. The type section is from 18deg 37'55"S, 130deg 21'20"E to 18deg 42'40"S, 130deg 27'10"E. Over 4800m thick. Possibly overlies Mount Charles Beds unconformably. Resistant beds of sublithic arenite form strike ridges and plateaus. Lithologies described; geochemistry detailed.|1808 +/- 15 Ma (Page et al., 1976).|||Unconformably overlies the Tanami Complex. Underlies unconformably Gardiner Sandstone and conformably Supplejack Downs Sandstone. Intruded by (probably co-magmatic with) Winnecke Granophyre.|Medium to thick-bedded, deep maroon to purplish sublithic arenite with common grit and pebble beds; iron-stained acid lava; tuffaceous sandstone and siltstone; conglomerate, locally interbedded with sandstone; water-laid acid tuff; rare agglomerate.|
13237|Mount Winnecke Formation|45167|5|Briefly described|Fig.27|||||||||
13237|Mount Winnecke Formation|46788|4|Described|p2|||||||||
13237|Mount Winnecke Formation|46797|5|Briefly described|p80|||Dates given||||||
13237|Mount Winnecke Formation|46864|5|Briefly described|p37|||||||||
13237|Mount Winnecke Formation|48950|2|Defined|p23|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13237|Mount Winnecke Formation|50589|5|Briefly described|p1.4, 2.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Of the Granites Suite/Supersuite. Geological Province: Granites-Tanami Block. Age: 1824-1770 +/- 15Ma (Shrimp, Rb-Sr).||||||07-NOV-08
13237|Mount Winnecke Formation|61056|6|Mentioned|p778|||Mount is Mt in text.||||||
13237|Mount Winnecke Formation|61861|6|Mentioned|p3 Table 1, p19 |Paleoproterozoic|Paleoproterozoic|Of Blake et al (1979). Raised to Group status.||||||
13237|Mount Winnecke Formation|63261|3|Fully described|p9 Fig. 5, p12|Paleoproterozoic|Paleoproterozoic|Of the Ware Group. Superseded Mount Winnecke Sandstone when Blake et al (1975) recognised 3 main lithologies: rhyolite lava, sublithic arenite+ tuffaceous sed. rock. Overlain by Nanny Goat Volcanics. Age of rhyolite: 1824+/-5Ma. Geol.prov: Tanami Region.||||||07-FEB-11
13237|Mount Winnecke Formation|64662|5|Briefly described|p29 Fig. 2, p30 Fig. 3, p43|Orosirian|Orosirian|Of the Ware Group. Age: ca.1824+/-5Ma - based on a rhyolite sample. Geological Province: Tanami region.||||||07-FEB-11
13237|Mount Winnecke Formation|64675|6|Mentioned|p9, p24, Fig.37|||Misspelt as Mount winnecke formation in Fig.2.||||Unconformably underlain by the Tanami Complex.||
13237|Mount Winnecke Formation|64725|5|Briefly described|p63 Fig.7.|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|c.1825 Ma.|Unit in Ware Group.||||
13237|Mount Winnecke Formation|64730|5|Briefly described|p142, Fig.11|Paleoproterozoic|Paleoproterozoic|Tanami region. Age is crystallisation age of  included rhyolite.|1824 +/- 5 Ma.|?Of Ware Group.||||02-MAY-12
13237|Mount Winnecke Formation|64733|6|Mentioned|p170 Fig.2|Orosirian|Orosirian||~1825 Ma.|Of Ware Group.||Overlain by Nanny Goat Volcanics.||20-APR-12
13237|Mount Winnecke Formation|64734|5|Briefly described|p186 Fig.1|Orosirian||Ca. 1825 Ma. Of Ware Group.||||||14-SEP-09
13237|Mount Winnecke Formation|64956|5|Briefly described|p7|||Of the Ware Group.||||||07-FEB-11
13237|Mount Winnecke Formation|65074|6|Mentioned|p349, p351 fig 4-37|Proterozoic|Proterozoic|Of North/Centre Birrindudu Basin. Early Proterozoic. c.1500 m thick.|1808 +/- 15 Ma (Page et al., 1976).|||Unconformably overlain by Gardiner Sandstone.|Acid volcanics and clastic-sedimentary rocks.|
13237|Mount Winnecke Formation|65338|6|Mentioned|p21.|||Tanami Region. Previously, correlated with Reynolds Range Group (Blake et al. 1979).||||||
13237|Mount Winnecke Formation|65359|4|Described|p1-38.|Orosirian|Orosirian|Tanami Region. Ware Group. Is intruded by Winnecke Granophyre, which is comagmatic with this unit's volcanic component. 3 sub units: tuffaceous sandstone, sublithic arenite, porphyritic and non-porphyritic acid lava. Arenite composed of fluviatile, probable braidplain to shallow marine. Geochemistry and lithology described in great detail. 1824+/-5 Ma SHRIMP U-Pb zircon age from rhyolite (Ozchron).||||||
13237|Mount Winnecke Formation|66129|6|Mentioned|p214 Fig.1|Orosirian|Orosirian|1825 Ma. Unit in Ware Group.||||||
13237|Mount Winnecke Formation|67824|6|Mentioned|p385 Fig.2, p387|||Ozchron database, Geoscience Australia.|1824 +/- 5 Ma (SHRIMP U-Pb, #87495029).|Unit in Ware Group.||||
13237|Mount Winnecke Formation|67826|6|Mentioned|p401 Fig.2|Orosirian|Orosirian||~ 1825 Ma|Of the Ware Group.||||
13237|Mount Winnecke Formation|68474|6|Mentioned|p572|Palaeoproterozoic|Palaeoproterozoic|Granites-Tanami Orogen.|ca. 1825 Ma|Ware Group||||
13237|Mount Winnecke Formation|69426|4|Described|p11:3-5, 7-8, 11|Orosirian|Orosirian|The definition by Vandenberg and Crispe (in prep) includes the former Mount Winnecke Sandstone (Traves, 1955), parts of the former Nongra Beds and the former Helena Creek Beds (Blake et al. , 1975). Subaerial to subaqueous caldera-type structures. Lithofacies described in some detail. Maximum depositional ages from detrital zircons are 1819 +/- 13 Ma, 1818 +/- 5 Ma and 1816 +/- 18 Ma.|1824 +/- 5 Ma rhyolite crystallisation; Page, 1998|Ware Group.||Is intruded by Winnecke Granophyre.|Coarse-grained quartz sandstone and granular conglomerate, dacites, rhyolites, mudstones and breccias.|12-JUL-16
13237|Mount Winnecke Formation|70291|4|Described|p178,181|Orosirian|Orosirian|Geological province: Tanami. Age constraint based on interbedded rhyolite.|ca. 1825 Ma|Unit of Ware Group.|||Coarse-grained quartz sandstone and granular conglomerate, interbedded with rhyolite.|
13237|Mount Winnecke Formation|70848|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region. Three facies are mapped separately.|c.1824-1816 Ma.|Ware Group.|||Quartz-lithic sandstone, granule conglomerate. Dacites, rhyolites, pebbly mudstone, pebbly sandstone, brecciated rhyodacite. Rhyolite, granule conglomerate, quartz-lithic sandstone, interbedded sandstone and mudstone, purple mudstone, breccia.|
13237|Mount Winnecke Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||felsic facies: rhyodacite, sedimentary facies: sandstone, arenite|
13237|Mount Winnecke Formation|71592|5|Briefly described|Appendix A.|||Tanami Orogen.|1824+/-5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Felsic volcanics.|
13237|Mount Winnecke Formation|73083|6|Mentioned|p23-24|||Intruded by granite of the Tanami Orogen.||||||
13237|Mount Winnecke Formation|73089|6|Mentioned|p8|||||Ware Group||Intruded by Winnecke Granophyre.||
13270|Mountain Valley Limestone Member|23216|5|Briefly described|Table1p8,34|||||||||
13270|Mountain Valley Limestone Member|23404|5|Briefly described|p638|||Of Mainoru Formation.||||||
13270|Mountain Valley Limestone Member|23937|2|Defined|p87 App. 1, p34|Calymmian|Calymmian|Of the Mainoru Formation.  Conformably overlain by Wooden Duck Member; conformably overlies the Nullawun Member.  Age: >1493Ma.  Max. thickness: 80m.  Geological Province: McArthur Basin.||||||03-NOV-04
13270|Mountain Valley Limestone Member|24050|4|Described|p44, p8 Tb. 2|Mesoproterozoic|Mesoproterozoic|Interbedded green mudstone, finely crystalline limestone and dolostone.  Of the Mainoru Formation.   Max. thickness: >50m.||||||13-NOV-06
13270|Mountain Valley Limestone Member|24051|5|Briefly described|Map Legend|Calymmian|Calymmian|Of Mainoru Formation (Roper Group). Geological Province: McArthur Basin.||||||13-NOV-06
13270|Mountain Valley Limestone Member|40691|6|Mentioned|Fig.4|||||||||
13270|Mountain Valley Limestone Member|43149|5|Briefly described|Map Legend||Mesoproterozoic|Of Mainoru Formation. Of Calymmian age.||||||13-NOV-06
13270|Mountain Valley Limestone Member|44471|14|Not recorded|p.9,11, opp.p.7, map|||(D53-10). Glauconitic Member of Mainoru Formation (Roper Group).||||||
13270|Mountain Valley Limestone Member|44472|5|Briefly described|map legend|||Of the Mainoru Formation (Roper Group).  Grey flaggy limestone, brown marl, glauconitic in places.  Upper (?) Proterozoic.||||||02-DEC-04
13270|Mountain Valley Limestone Member|45162|6|Mentioned|Table 7|||See also Fig.4||||||
13270|Mountain Valley Limestone Member|60573|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Mainoru Formation (Roper Group).  Together with other members, appears as Mountain Valley Limestone only in map legend.  Does not outcrop in the ROPER RIVER mapsheet area||||||13-NOV-06
13270|Mountain Valley Limestone Member|61390|5|Briefly described|Map Legend|Ectasian|Calymmian|Of the Mainoru Formation. Green laminated mudstone with thin to medium interbeds of intraclastic limestone.||||||
13270|Mountain Valley Limestone Member|69430|4|Described|p15:26-27, 30|Calymmian|Calymmian|Abbott et al. (2001). McArthur Basin. 55-80m thick. Shallow-marine, tidal flat sediments.||Mainoru Formation.||Conformably ovelies Nullawun Member. Is overlain conformably by Wooden Duck Member.|Lithologically distinctive: green laminated mudstone interbedded with intraclast limestone.|12-JUL-16
13270|Mountain Valley Limestone Member|70734|5|Briefly described|p16 Fig. 2|||McArthur Basin. Shown as Mtn Valley Lst. Mbr. Limestone and calcareous siltstone.||Of Mainoru Formation.||Overlies Nullawun member. Overlain by Wooden Duck Member.||
13270|Mountain Valley Limestone Member|70822|5|Briefly described|p102 fig 1 (A)|Mesoproterozoic|Mesoproterozoic|||Mainoru Formation||Overlies Nullawan Member; overlain by Wooden Duck Member.|Limestone.|
13270|Mountain Valley Limestone Member|70968|2|Defined|p17-18, p20, p25, p27-30, p131, p138|Calymmian|Calymmian|See also p140, p143-144. Sweet in Abbott et al. (2001) after Dunn (1963). Named after Mountain Valley pastoral lease and homestead. Recessive and poorly exposed: forms low terraced rises and hills. Without the limestone, it is hard to distinguish from the rest of the Formation. An interval of glauconitic rocks was reassigned to the overlying Wooden Duck Member by Abbott et al. (2001). The type section is from 374100mE 8442100mN (base) to 374500mE 8442000mN in URAPUNGA sheet. A reference section in Urapunga-1 drillhole is from 204.1m (base) to 126.2m. Thickness ranges from c.20-88m; 55m at the type section. Shallow-water, intertidal environment. Lithology described and illustrated.||Mainoru Formation.||Disconformably overlies Limmen Sandstone locally. Overlies Nullawun Member gradationally. Is overlain conformably by Wooden Duck Member.|Mainly laminated green to red-brown mudrocks (shale and mudstone); also includes interbedded calcareous sandstone and minor carbonate rocks (limestone and dolostone).|
13270|Mountain Valley Limestone Member|71059|4|Described|p3|Mesoproterozoic|Mesoproterozoic|McArthur Basin. 55-88m thick. Shallow-marine, tidal-flat deposits.||Mainoru Formation.||Conformably overlies Nullawun Member. Is overlain conformably by Wooden Duck Member.|Green laminated mudrocks interbedded with intraclast limestone.|
13270|Mountain Valley Limestone Member|71488|5|Briefly described|p141 fig 1b|||||Mainoru Formation||Overlies the Nullawan Member. Overlain by the Wooden Duck Member.||
13270|Mountain Valley Limestone Member|71494|4|Described|p2-p4, p6-p9, p12-p13, p15, p18, p26|||Thickness ranges from 55 to 80 metres. Deposited in a shallow marine, tidal flat environment. Limestone beds have dessication features and intraclasts and probably represent shallowest depositional setting. Core log features presented in this volume.||Mainoru Formation||Conformably overlies the Nullawan Member. Overlain conformably by the Wooden Duck Member.|Green laminated mudstone interbedded with intraclast limestone.|
13270|Mountain Valley Limestone Member|71779|5|Briefly described|p2 Fig. 1|||Urapunga Region, McArthur Basin.||Mainoru Formation||||24-SEP-18
13270|Mountain Valley Limestone Member|73242|5|Briefly described|p39|||||Mainoru Formation, Collara Subgroup, Roper Group||Underlain by Nullawun Member. Overlain by Wooden Duck Member.|Includes limestone in mudstone.|
13287|Moyle River Formation|9579|5|Briefly described|Map Sheet|Mesoproterozoic|Mesoproterozoic|Middle Proterozoic age.||Of the Fitzmaurice Group.||||
13287|Moyle River Formation|22547|6|Mentioned|Fig4,p25|||Of the Fitzmaurice Group. Overlain by Goobaieri Formation.||||||14-NOV-06
13287|Moyle River Formation|23822|5|Briefly described|p299|Proterozoic|Proterozoic|Geological Province: Litchfield Province.||||||
13287|Moyle River Formation|32171|4|Described|Table 1|||Carpentarian/Adelaidean||||||
13287|Moyle River Formation|32307|4|Described|Table 2|||Proterozoic||||||
13287|Moyle River Formation|32309|6|Mentioned|Map legend|Adelaidean|Carpentarian|Carpentarian/Adelaidean||||||
13287|Moyle River Formation|32310|6|Mentioned|Map legend|Adelaidean|Carpentarian|Adelaidean/Carpentarian||||||
13287|Moyle River Formation|32660|5|Briefly described|Table 6|||||||||
13287|Moyle River Formation|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Fitzmaurice Group.  Quartz sandstone; minor siltstone, grit and pebble conglomerate.||||||02-DEC-04
13287|Moyle River Formation|32701|4|Described|Table 1|||Adelaidean. Fitzmaurice Group.||||||13-NOV-06
13287|Moyle River Formation|32728|6|Mentioned|Fig.14|||||||||
13287|Moyle River Formation|33076|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
13287|Moyle River Formation|33093|4|Described|Table 2|||||||||
13287|Moyle River Formation|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
13287|Moyle River Formation|35140|6|Mentioned|p322|||||||||
13287|Moyle River Formation|37462|6|Mentioned|Fig.4.13|||||||||
13287|Moyle River Formation|39889|6|Mentioned|p485|||||||||
13287|Moyle River Formation|40495|6|Mentioned|p12|||||||||
13287|Moyle River Formation|40764|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
13287|Moyle River Formation|40765|3|Fully described|p10|||||||||
13287|Moyle River Formation|41645|4|Described|p135|||||||||
13287|Moyle River Formation|41646|6|Mentioned|Map legend|Mesoproterozoic||Of the Fitzmaurice Group. Quartzarenite, fine to medium grained, poorly sorted, thickly bedded to massive, with abundant cross bedding; basal conglomerate; stromatolitic dolomite; dolomite; siltstone.||||||17-OCT-05
13287|Moyle River Formation|41661|6|Mentioned|p16|||||||||
13287|Moyle River Formation|45112|6|Mentioned|Table 16|||||||||
13287|Moyle River Formation|47047|6|Mentioned|p220|||||||||
13287|Moyle River Formation|48938|2|Defined|p15|Adelaidean|Adelaidean|||||||
13287|Moyle River Formation|48942|3|Fully described|p32|||Strat. section p108.||||||13-NOV-06
13287|Moyle River Formation|60006|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: ? Halls Creek Orogen. Of Fitzmaurice Group. Silica-cemented quartz sandstone, minor siltstone and pebble conglomerate.||||||07-JAN-09
13287|Moyle River Formation|60682|4|Described|p5|Mesoproterozoic|Mesoproterozoic|Of Fitzmaurice Group. Thickness: ~100m. Unconformably overlies Bow River Granite. Conformably overlain by Goobaieri Formation. Geological Province: Halls Creek Orogen. Quartz sandstone, minor siltstone and conglomerate.||||||
13287|Moyle River Formation|63866|4|Described|p108|Statherian|Statherian|Litchfield Province, Pine Creek Orogen.|c. 1635 Ma (Carson, C.J., unpublished)|Fitzmaurice Group||Intruded by the Murrenja Dolerite.||
13287|Moyle River Formation|64677|5|Briefly described|p13|||Pine Creek Orogen.||Fitzmaurice Group.||Nonconformably overlies Koolendong Granite.||
13287|Moyle River Formation|64698|4|Described|lithinterp table|||Age ~1150-1250Ma (Stenian) but age name given as Statherian. Victoria - Birrindudu Basin. Of Fitzmaurice Group. Max. thickness 3000m. Silica cemented quartz sandstone, minor siltstone and pebble conglomerate.||||||07-JAN-09
13287|Moyle River Formation|64956|6|Mentioned|p66|||Overlies the Wagait Granite.||||||07-FEB-11
13287|Moyle River Formation|65331|5|Briefly described|Map legend|Mesoproterozic|Mesoproterozic|Of Fitzmaurice Group, ?Halls Creek Orogen. Silica cemented quartz sandstone, minor siltstone and pebble conglomerate||||||
13287|Moyle River Formation|65417|5|Briefly described|p158 Fig.2.|Mesoproterozoic|Mesoproterozoic|Fitzmaurice Mobile Zone.||Basal unit in Fitzmaurice Group.||Is overlain conformably by Goobaieri Formation.||
13287|Moyle River Formation|67167|5|Briefly described|Map legend.|||||Unit in Fitzmaurice Group.|||Quartz sandstone, fine- to medium-grained, poorly sorted, thickly bedded to massive, with abundant cross-beds, basal conglomerate; dolostone, siltstone.|
13287|Moyle River Formation|67186|5|Briefly described|Map legend.|||||Unit in Fitzmaurice Group.|||Quartz sandstone, fine- to medium-grained, poorly-sorted, thickly-bedded to massive, with abundant cross-beds; basal conglomerate; dolostone; siltstone.|23-NOV-11
13287|Moyle River Formation|69420|6|Mentioned|p5:105||||||||Arenite and intraformational conglomerate.|12-JUL-16
13287|Moyle River Formation|69435|4|Described|p20:2-5|||Sweet et al. (1974). Fitzmaurice Basin. Thickness estimated at about 5,000m; it is not possible to determine the true thickness of this unit: previous estimates are briefly discussed. Has developed a weak to moderate foliation adjacent to faults in the north. Is intruded by Murrenja Dolerite.|<1640 Ma (detrital zircons).|Fitzmaurice Group.||Unconformably overlies Bow River and Koolendong Granites, Murra-Kamangee Granodiorite, Hermit Creek Metamorphics and Henschke Breccia. Is overlain conformably by Goobaieri Formation.|Fine- to coarse-grained quartz sandstone; minor siltstone and pebble to cobble conglomerate. Local;ly contains small lenses of volcanic rocks, dolostone (with stromatolites) and conglomerate.|12-JUL-16
13287|Moyle River Formation|69673|5|Briefly described|p59, p60 fig 48|Statherian|Statherian|Up to 5000m thick.|1640 Ma|Fitzmaurice Group||Overlain by Goobaieri Formation|Fine to coarse grained quartz sandstone, minor siltstone and conglomerate.|
13287|Moyle River Formation|70206|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Fitzmaurice Basin.||Fitzmaurice Group|||Silica cemented quartz sandstone, minor siltstone and pebble conglomerate.|
13287|Moyle River Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
13287|Moyle River Formation|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|1638+/-20 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
13301|Mud Tank Carbonatite|9199|5|Briefly described|Map legend|||Zircon-apatite-magnetite-ilmenite.  Geological Province: Arunta Block.||||||04-NOV-04
13301|Mud Tank Carbonatite|22524|6|Mentioned|p37|Cryogenian|Cryogenian|||||||
13301|Mud Tank Carbonatite|22804|6|Mentioned|p443|||Geological Province - Arunta Block.  Age - 735+/-5 Ma.||||||
13301|Mud Tank Carbonatite|23844|5|Briefly described|p43|Neoproterozoic|Neoproterozoic|Age: 732 +/- 5Ma (U-Pb zircon, Black and Gulson 1978)||||||
13301|Mud Tank Carbonatite|24047|5|Briefly described|p10|Neoproterozoic|Neoproterozoic|Age: 730Ma.  Geological Province: Arunta province.||||||
13301|Mud Tank Carbonatite|33307|4|Described|p6|||||||||
13301|Mud Tank Carbonatite|35216|6|Mentioned|p51|||||||||
13301|Mud Tank Carbonatite|35521|5|Briefly described|p39|||Chemical analysis.||||||13-NOV-06
13301|Mud Tank Carbonatite|38885|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
13301|Mud Tank Carbonatite|39213|3|Fully described|p6|||||||||
13301|Mud Tank Carbonatite|39552|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
13301|Mud Tank Carbonatite|39583|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
13301|Mud Tank Carbonatite|39610|4|Described|p14|||See also p7.||||||13-NOV-06
13301|Mud Tank Carbonatite|39621|3|Fully described|p12|||||||||
13301|Mud Tank Carbonatite|39887|6|Mentioned|Fig.3|||||||||
13301|Mud Tank Carbonatite|39888|6|Mentioned|Table 1|||||||||
13301|Mud Tank Carbonatite|40811|4|Described|p320|||||||||
13301|Mud Tank Carbonatite|41509|6|Mentioned|p4|||||||||
13301|Mud Tank Carbonatite|41830|6|Mentioned|p549|||||||||
13301|Mud Tank Carbonatite|42481|6|Mentioned|Fig.1 P183|||||||||
13301|Mud Tank Carbonatite|46830|6|Mentioned|p23|||||||||
13301|Mud Tank Carbonatite|46868|6|Mentioned|p79|||||||||
13301|Mud Tank Carbonatite|46884|4|Described|p227|||||||||
13301|Mud Tank Carbonatite|48992|2|Defined|p38|Neoproterozoic|Neoproterozoic|||||||
13301|Mud Tank Carbonatite|49444|14|Not recorded|?|||||||||
13301|Mud Tank Carbonatite|50246|5|Briefly described|p6, p7, p19 Fig. 1|||Name also presented as the informal Mud Tank carbonatite. Age: 732+/-5Ma. Potassic alkaline igneous suite that hosts orthomagmatic PGE-Au-Cu-Ni deposits. Also referred to as the Mud Tank carbonatite complex.||||||07-FEB-11
13301|Mud Tank Carbonatite|60525|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block. Carbonatite, eluvium containing magnetite, apatite and zircon.||||||
13301|Mud Tank Carbonatite|60547|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Internediate to ultrabasic. Zircon-apatite-magnetite-illmenite-phlogopite carbonatite.||||||
13301|Mud Tank Carbonatite|65341|6|Mentioned|p2 Fig.2. |||||||||
13301|Mud Tank Carbonatite|66860|6|Mentioned|p2 fig 2|||||||||
13301|Mud Tank Carbonatite|67127|6|Mentioned|p98, p100, p107, p109, p172|Neoproterozoic|Neoproterozoic|Located near the Woolanga Lineament in a zone that also features the Nolans Bore deposit; however it should be noted a recent date for the host veins of 1244 +/- 10 Ma (Korsch et al, 2009; U-Pb) suggests the mineralisation is not related to this unit. 52km north-northwest of the Mordor Complex.|732 +/- 5 Ma (U-Pb; Black and Gulson, 1978)||||Features significantly higher Cu, Ni and Cr contents and lower Sr, Zr, Nb, Mo, La and Ce contents than average carbonatites. Occurs near the Woolanga Lineament.|
13301|Mud Tank Carbonatite|69418|6|Mentioned|p3:31, 34|||Arunta Region. Hosts gem quality garnet, zircon and apatite at Gemtree (Harts Range area), and vermiculite at Mud Tank (described).||||||12-JUL-16
13301|Mud Tank Carbonatite|69427|4|Described|p12:40 Fig.12.34; 12:46, 64|Neoproterozoic|Neoproterozoic|Shaw et al. (1979), Crohn and Moore (1984), Currie et al. (1992). Near the N margin of the Strangways Range, Aileron Province. Deformed carbonatite with steeply-dipping to subvertical foliation/layering. Vermiculite has been mined since 1996, with reserves providing a mine life of ~20 years; fossicking for coarse zircons occurs. Age by TIMS conventional U-Pb method on zircon separates.|732 +/- 5 Ma (Black and Gulson, 1978).|||Intrudes Yambah Granulite.|Crystalline carbonate rocks; foliated micaceous carbonate rocks, rich in pale brown phlogopite; feldspathic carbonate rocks with variable amounts of sodic plagioclase, clinopyroxene, amphibole and biotite. Significant vermiculite occurs.|12-JUL-16
13301|Mud Tank Carbonatite|69585|6|Mentioned|p6-7|||Mentioned as a standard for zircon dating.||||||
13301|Mud Tank Carbonatite|69729|5|Briefly described|p66, p85|Neoproterozoic|Neoproterozoic|Black and Gulson (1978). Underlies Amadeus Basin. Less formally presented as the Mud Tank carbonatite complex on p85.|c.732 Ma.|||||
13301|Mud Tank Carbonatite|69929|6|Mentioned|p243|||NW Gough Dam Shear Zone, Arunta Block. Has well-foliated margins, and gradational contacts with enveloping pelitic schists and mylonites.|732 +/- 5 Ma (U-Pb; Black and Gulson, 1978).|||||
13301|Mud Tank Carbonatite|70789|5|Briefly described|p320|||Apatite from this unit was used as an in-house secondary standard for LA-ICP-MS.||||||
13301|Mud Tank Carbonatite|70825|6|Mentioned|p41|||||||||
13301|Mud Tank Carbonatite|71858|6|Mentioned|p69|||Aileron Province.|ca. 732 Ma|||||
13318|Mudginberri Phonolite|9534|5|Briefly described|Map legend|Adelaidean|Adelaidean|Part of a phonolite dyke swarm.||||||
13318|Mudginberri Phonolite|9691|5|Briefly described|Map Legend|||Phonolite dyke swarm.||||||
13318|Mudginberri Phonolite|9701|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Phonolite dyke swarm.||||||02-JUN-05
13318|Mudginberri Phonolite|9733|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Phonolite dyke swarm.||||||
13318|Mudginberri Phonolite|23374|5|Briefly described|p20||Ectasian|Age: Rb-Sr 1316+/-40Ma. Within the Nimbuwah Complex.||||||13-NOV-06
13318|Mudginberri Phonolite|33186|6|Mentioned|p293|||||||||
13318|Mudginberri Phonolite|36535|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
13318|Mudginberri Phonolite|36635|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
13318|Mudginberri Phonolite|37815|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
13318|Mudginberri Phonolite|38349|4|Described|p17|||||||||
13318|Mudginberri Phonolite|38351|6|Mentioned|p13|||||||||
13318|Mudginberri Phonolite|38884|6|Mentioned|Map legend|Adelaidean|Adelaidean|Prob. Adelaidean||||||
13318|Mudginberri Phonolite|39620|5|Briefly described|p9|||||||||
13318|Mudginberri Phonolite|41146|6|Mentioned|p858|||||||||
13318|Mudginberri Phonolite|43715|6|Mentioned|p28|||||||||
13318|Mudginberri Phonolite|46639|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Age: 1316+/-40Ma. Fine grey-green to weathered pink equigranular to strongly porhyritic K-feldspar, nepheline and pyroxene phonolite, phonolitic tephrite, and minor trachybasalt; peralkaline dyke swarms.||||||
13318|Mudginberri Phonolite|46700|5|Briefly described|P7, Table1 P8||Adelaidean|Intrudes Nanambu Complex.  Age of unit is 1316 Ma.||||||13-NOV-06
13318|Mudginberri Phonolite|60550|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Phonolite dyke swarms.||||||
13318|Mudginberri Phonolite|62375|5|Briefly described|p8 Table 1|Neoproterozoic|Paleoproterozoic|Phonolite dykes. Age: 1200 +/- 35Ma. Thickness: 1m. Geological Province: Pine Creek Orogen.||||||09-FEB-10
13318|Mudginberri Phonolite|63866|6|Mentioned|p117|||||||||
13318|Mudginberri Phonolite|67779|5|Briefly described|pp40-41, p103.|||A peralkaline dyke swarm.|1316 +/- 40 Ma (Rb-Sr: Page et al. 1980).|||Intrudes Nanambu Complex.||
13318|Mudginberri Phonolite|73242|6|Mentioned|p46|Ectasian|Ectasian|Pine Creek Orogen, eastern; Nimbuwah Domain. Peralkaline. Geochron from Page et al. (1980).|1316 +/- 40 Ma Rb-Sr|||||
13380|Mullaman beds|23374|5|Briefly described|p25|Cenomanian|Aptian|Subdivided into Walker River and Yirrkala Formations in eastern Arnhem Land.||||||
13380|Mullaman beds|23425|5|Briefly described|p381|||||||||
13380|Mullaman beds|24050|5|Briefly described|p53|Albian|Neocomian|Previuosly the Mullaman Group.||||||
13380|Mullaman beds|31268|6|Mentioned|Table 1|||||||||
13380|Mullaman beds|36335|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
13380|Mullaman beds|36439|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
13380|Mullaman beds|36442|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
13380|Mullaman beds|38291|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late and/or Early Cretaceous||||||
13380|Mullaman beds|38348|6|Mentioned|p25|||||||||
13380|Mullaman beds|38350|6|Mentioned|p22|||||||||
13380|Mullaman beds|38584|4|Described|p21|||||||||
13380|Mullaman beds|39422|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Clayey sandstone, claystone, conglomerate.  Unconformably overlies rocks of the South Nicholson Group, and over the Camooweal Dolomite.||||||10-MAR-05
13380|Mullaman beds|39497|6|Mentioned|p16|||||||||
13380|Mullaman beds|39523|6|Mentioned|p96|||||||||
13380|Mullaman beds|39797|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
13380|Mullaman beds|39925|6|Mentioned|Fig.2|||||||||
13380|Mullaman beds|41268|6|Mentioned|Fig.15|||||||||
13380|Mullaman beds|41406|6|Mentioned|Map legend|Early Cretaceous||||||||
13380|Mullaman beds|42821|5|Briefly described|p66|||||||||
13380|Mullaman beds|43630|6|Mentioned|p8||Mesozoic|Old name no longer in use||||||
13380|Mullaman beds|44112|6|Mentioned|p79,82|||Subdivided into newly defined 'Walker River Formation' and 'Yirrkala Formation' based on work by Krassey (1994a,b)||||||
13380|Mullaman beds|44922|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|Quartzose sandstone, claystone, siltstone, minor conglomerate.||||||01-JUL-04
13380|Mullaman beds|45148|3|Fully described|p20|||Briefly described p5.||||||07-OCT-22
13380|Mullaman beds|47083|6|Mentioned|p19|||||||||
13380|Mullaman beds|50600|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|Quartz sandstone and siltstone.||||||
13380|Mullaman beds|61155|5|Briefly described|p16|||Age is pre-Cainozoic. Geological region: South Alligator Valley, East Arnhem Land and Barkly Tableland.||||||
13380|Mullaman beds|65239|5|Briefly described|p3 Fig. 4|Cretaceous|Cretaceous|Geological province: Wiso Basin. Fluvial deposits.||||||
13380|Mullaman beds|65345|5|Briefly described|p7 Fig.6. |Cretaceous|Cretaceous|Wiso Basin. Fluvial deposits.||||||
13380|Mullaman beds|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map; p106|Early Cretaceous|Late Jurassic|Eromanga/Carpentaria Basins.|||||Quartz sandstone and conglomerate, sandy claystone and siltstone|
13380|Mullaman beds|67564|5|Briefly described|p51.|Middle Aptian|Middle Aptian|Defined by Skwarko (1966). Correlated with parts of the Petrel and Darwin Formations; now defunct. Earliest marine sediments of the Dunmarra Basin coastal belt. Forms the Bulademo Tableland.||||||
13380|Mullaman beds|68553|6|Mentioned|Map legend; schematic diagram.|Early Cretaceous|Jurassic|Carpentaria Basin. This unit is mapped with Lees Sandstone, and unnamed sedimentary units, under the symbol, JKm.||||||
13380|Mullaman beds|69056|6|Mentioned|Reference images sheet.|||Shown on the simplified surface geology map of the Quamby Project area; mapped as one unit with Lees Sandstone and unnamed sediments.||||||
13380|Mullaman beds|69594|5|Briefly described|p521-522|Early Cretaceous|Early Cretaceous|Western Gulf Sub-basin (NT), Carpentaria Basin. Occurs on WESTMORELAND and LAWN HILL 250K sheets. In NT, where the type region is located, this name has been replaced by Walker River Formation and Yirrkala Formation (Krassay, 1994; after Skwarko, 1966), "thus leaving the Mullaman beds as an anachronism" [?but not yet obsolete]. Age is poorly constrained: possible equivalent units mentioned.|||||Thin, mesa-forming sandstones with overlying siltstone or claystone.|
13380|Mullaman beds|69673|6|Mentioned|p202|||Discontinued name.||||||
13380|Mullaman beds|71369|5|Briefly described|p45|Early Cretaceous|Late Jurassic|Swarko (1966). Scattered remnants in far NW Queensland and adjacent NT. Mainly flat-lying. Thickness varies from a few metres to 15-20m. Rocks at higher elevations invariably occur in a zone of deep weathering, with lateritic profiles developed in the claystones.|||||Basal sandstone and granule conglomerate, commonly ferruginous, overlain by claystone.|
13380|Mullaman beds|72414|4|Described|map sheet|Early Cretaceous|Late Jurassic|Of Geogina Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.||||Underlain unconformably nu Camooweal Dolomite.|Quartz sandstone and conglomerate, sandy claystone and siltstone.|
13380|Mullaman beds|72415|4|Described|mapsheet|Early Cretaceous|Late Jurassic|Of Geogina Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.||||Underlain unconformably nu Camooweal Dolomite.|Quartz sandstone and conglomerate, sandy claystone and siltstone.|
13380|Mullaman beds|72421|4|Described|mapsheet|Early Cretaceous|Late Jurassic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.|||||Quartz sandstone and conglomerate, sandy claystone and siltstone|
13380|Mullaman beds|72422|4|Described|mapsheet|Early Cretaceous|Late Jurassic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.|||||Quartz sandstone and conglomerate, sandy claystone and siltstone|
13380|Mullaman beds|73137|6|Mentioned|p6|Early Cretaceous|Jurassic|||||||
13391|Mullera Formation|23393|4|Described|p21|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Group.||||||
13391|Mullera Formation|23937|5|Briefly described|p76 App. 1|||Of the South Nicholson Group.  Overlies Constance Sandstone.||||||18-APR-05
13391|Mullera Formation|24047|5|Briefly described|p27|||Of the South Nicholson Group.  Geological Province: South Nicholson Basin.||||||
13391|Mullera Formation|24442|5|Briefly described|p23 Fig. 2|Mesoproterozoic|Mesoproterozoic|Of the South Nicholson Group.||||||
13391|Mullera Formation|26310|2|Defined|p1, 3, 4, 8, 10, Table 1|Proterozoic|Proterozoic|Maximum Thickness: 8,000 feet. Type section in text. Underlies Tidna Sandstone (conformably), Colless Volcanics (unconformably), Camooweal Dolomite (unconformably).  Overlies: Constance Sandstone (conformably). Siltstone, sandstone, shale, ironstone.||||||13-NOV-06
13391|Mullera Formation|31420|6|Mentioned|p216|||||||||
13391|Mullera Formation|32660|5|Briefly described|Table 5|||||||||
13391|Mullera Formation|36003|6|Mentioned|p1029|||See also Fig.8.||||||
13391|Mullera Formation|36012|6|Mentioned|p26|||||||||
13391|Mullera Formation|36439|6|Mentioned|Map legend|Adelaidean|Carpentarian|Carpentarian or Adelaidean||||||
13391|Mullera Formation|36442|6|Mentioned|Map legend|Adelaidean|Carpentarian|Carpentarian or Adelaidean.||||||13-NOV-06
13391|Mullera Formation|37462|6|Mentioned|p263|||||||||
13391|Mullera Formation|38291|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
13391|Mullera Formation|38348|6|Mentioned|p24|||||||||
13391|Mullera Formation|38584|4|Described|p20|||||||||
13391|Mullera Formation|39422|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the South Nicholson Group.  Contains the Middle Creek Sandstone Member.  Siltstone, shales, sandstone and ironstone.  Unconformably overlain by the Mullaman beds; conformably overlies Constance Sandstone.||||||22-JUL-13
13391|Mullera Formation|39445|5|Briefly described|Table 3|||300 million tonnes iron ore. Age: 1135 Ma - see p55.||||||13-NOV-06
13391|Mullera Formation|39497|4|Described|p15|||||||||
13391|Mullera Formation|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
13391|Mullera Formation|39925|6|Mentioned|Fig.2|||||||||
13391|Mullera Formation|41721|4|Described|p29|||||||||
13391|Mullera Formation|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
13391|Mullera Formation|43010|5|Briefly described|Fig.6||Mesoproterozoic|of South Nicholson Group. Of "Mid Proterozoic" age.||||||
13391|Mullera Formation|44091|14|Not recorded|p11||Neoproterozoic|||||||
13391|Mullera Formation|44271|2|Defined|p40,41,57,60,62|||Conformably overlies Constance Sandstone. Overlain by Camooweal Dolomite.||||||
13391|Mullera Formation|44274|2|Defined|Tb.2,p9,10,15,16,map|||||||||
13391|Mullera Formation|44275|14|Not recorded|Map Legend|||||||||
13391|Mullera Formation|44281|14|Not recorded|Map Legend||Neoproterozoic|||||||
13391|Mullera Formation|44290|2|Defined|p439||Paleoproterozoic|||||||07-NOV-08
13391|Mullera Formation|44301|14|Not recorded|p.7|||Occurs on MT DRUMMOND sheet. (E53-12).||||||13-NOV-06
13391|Mullera Formation|44305|14|Not recorded|p.15|||(E53-8). opp.6,18.||||||
13391|Mullera Formation|44306|14|Not recorded|map legend|||(?) Upper Proterozoic.||||||
13391|Mullera Formation|44441|14|Not recorded|p.7||Neoproterozoic|Overlain by Mittiebah Sandstone in E53-12 (Mt.Drummond). Upper Proterozoic.||||||13-NOV-06
13391|Mullera Formation|44482|14|Not recorded|p.5,7,9,opp.p.6, map|||(E53-12). See also p.10,13,15,16, for more details.||||||
13391|Mullera Formation|44483|5|Briefly described|map legend|||Upper (?) Proterozoic.||||||
13391|Mullera Formation|44521|14|Not recorded|p8||Neoproterozoic|||||||
13391|Mullera Formation|44920|14|Not recorded|Map Legend, Sheet 2||Adelaidean|||||||
13391|Mullera Formation|44922|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of South Nicholson Group.  Includes the Train Range Ironstone and Middle Creek Sandstone Members.||||||01-JUL-04
13391|Mullera Formation|44989|2|Defined|p.119,120|||Tb.II. (E53-4,8). On many pages.||||||
13391|Mullera Formation|45032|14|Not recorded|p7||Adelaidean|||||||
13391|Mullera Formation|45052|3|Fully described|p71|||Adelaidean||||||
13391|Mullera Formation|45079|6|Mentioned|p75|||Diagram on p75. Upper Proterozoic age.||||||13-NOV-06
13391|Mullera Formation|45166|5|Briefly described|p33|||||||||
13391|Mullera Formation|45287|14|Not recorded|p.223,226,229,231||Neoproterozoic|||||||
13391|Mullera Formation|48894|6|Mentioned|p24|||Age||||||
13391|Mullera Formation|62659|5|Briefly described|Map Legend|Calymmian|Calymmian|Of the Accident Subgroup. Green, grey and reddish brown to maroon, micaceous, locally ferruginous siltstone, shale and fine grained, lithic to quartzose sandstone.||||||
13391|Mullera Formation|64443|5|Briefly described|p3, p4, p6, p29|Calymmian|Calymmian|||Of the Accident Subgroup.||Possibly unconformably overlies Mittiebah Sandstone.|Typically comprises fine-coarse, quartzose to sublithic sandstone with minor interbeds of conglomerate and siltstone, medium-very thick bedding with scattered-entrained quartz granules and pebbles.|14-MAY-14
13391|Mullera Formation|65337|3|Fully described|p9 Fig.5, p38 Table 5, pp57-60.|Mesoproterozoic|Mesoproterozoic|Northwest MOUNT DRUMMOND area. Thickness over 1100 m. Distribution now substantially less than previous maps as many outcrops have been reassigned. Contains shale rich in hydrocarbons (TOC c.10%) with low thermal maturity.||Unit in Accident Subgroup.|Includes Middle Creek Sandstone Member.|Overlies Mittiebah and Constance Sandstones. Is overlain by Tidna Sandstone.|Green to maroon, micaceous, locally ferruginous siltstone, shale and fine-grained, lithic to quartzose sandstone; minor ironstone, organic-rich shale and medium-grained quartzose sandstone.|
13391|Mullera Formation|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map, p39|Neoproterozoic|Mesoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. South Nicholson Basin.||South Nicholson Group.|||Siltstone, shale, some sandstone and ironstone.|
13391|Mullera Formation|67352|6|Mentioned|p12, p16|Calymmian|Calymmian|||Accident Subgroup||||
13391|Mullera Formation|67539|5|Briefly described|p14, p15 Fig.8|||Thin ironstones of the Boodjamulla Formation were previously mapped as the Mullera Formation.||Of the South Nicholson Group.|Includes Train Range Ironstone Member and Middle Creek Sandstone Member.|Overlain by the Tidna Formation. Underlain by the Constance Sandstone.||
13391|Mullera Formation|68020|6|Mentioned|p128|||||?Of South Nicholson Group||||
13391|Mullera Formation|68146|5|Briefly described|p196|||||Accident Subgroup.|Middle Creek Sandstone Member, Train Range Ironstone Member.|Conformably overlies Elizabeth Sandstone Member. Is overlain by Tidna Sandstone.||
13391|Mullera Formation|68575|6|Mentioned|p28|||South Nicholson Basin.||||Is overlain conformably and gradationally by Tidna Sandstone.||
13391|Mullera Formation|69434|4|Described|p19:2, 4-8|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin. Mapping of this unit by Smith and Roberts (1963) included rocks now assigned to the Crow Formation. Over 1100m thick (in NT); up to 1800m thick (in Qld). Very recessive. A variety of sedimentary structures are listed. Shallow-marine shelf deposits, partly above storm wave-base and partly below. Several ironstone intervals in Qld, grouped as the Train Range Ironstone Member, were explored for iron. Hosts several "Clinton-type" oolitic iron ore occurrences (described) in NT. Has mixed indications, mostly negative, for petroleum potential. A whole-rock (shale) Rb-Sr date of 1510 +/- 120 Ma (Plumb and Derrick, 1975) is considered unreliable due to possible inherited material.||Accident Subgroup.|Middle Creek Sandstone Member, Train Range Ironstone Member.|Conformably overlies Constance Sandstone. Is overlain conformably by Tidna Sandstone (in Qld).|Green or red-brown to maroon, micaceous, locally ferruginous siltstone, shale and lithic to quartzic fine sandstone; minor ironstone, organic-rich shale and medium quartzic sandstone. Characteristically thinly-bedded.|12-JUL-16
13391|Mullera Formation|69445|6|Mentioned|p30:17|||||||Is overlain by Colless Volcanics.||12-JUL-16
13391|Mullera Formation|69591|4|Described|p52, p54, p88, p98, p111|Mesoproterozoic|Mesoproterozoic|Camooweal-Murphy Domain, South Nicholson Basin (Qld and NT). Mainly deep marine, locally shallowing, deposits.||Uppermost Accident Subgroup.|Train Range Ironstone Member, Middle Creek Sandstone Member.|Overlies Elizabeth Sandstone. Is overlain by Yidna Sandstone.|Predominantly deeper marine shales and siltstone, punctuated by shallower sandstone and oolitic ironstone units.|
13391|Mullera Formation|69673|6|Mentioned|p56, p57|||Up to 1100m thick. Deposited in shallow marine shelf environment.||Accident Subgroup|||Micaceous, locally ferruginous siltstone, shale and lithic to quartzose sandstone, organic rich shale and quartzose sandstone.|
13391|Mullera Formation|70849|5|Briefly described|Map legend.|Calymmian|Calymmian|South Nicholson Basin.||South Nicholson Group.||Overlies Constance Sandstone. Is overlain by Mittiebah Sandstone.|Fine- to coarse-grained quartz sandstone; greywacke and siltstone, commonly rich in iron oxides.|
13391|Mullera Formation|70897|5|Briefly described|p41-42, Fig.1.7.6,8|Mesoproterozoic|Mesoproterozoic|Results of dating of six samples' detrital zircons are tabulated and graphed. The youngest result is assumed to be the maximum depositional age.|1492 +/- 4 Ma (maximum depositional age).|South Nicholson Group.|||Green to grey, carbonaceous siltstone and shale; pyritic grey shale; pale green tuffaceous clay.|
13391|Mullera Formation|70968|5|Briefly described|p131 Fig.118, p132|Ectasian|Ectasian|May correlate with the Maiwok Subgroup.||Accident Subgroup.||||
13391|Mullera Formation|71369|4|Described|p1, p4-6, p22-23, p36-44, p48, p50|Mesoproterozoic|Mesoproterozoic|Mapped by Carter and Opik (1961); defined by them in Carter et al. (1961). Revised by Carter and Zimmerman (1960) [sic], who named the Tidna Sandstone as a separate Formation rather than the uppermost Member of this unit. South Nicholson Basin. Occupies a series of structural basins. 1020-2460m thick. Lithologies, particularly the ironstones, described in great detail. Age is derived from U-Pb zircon.|1569 +/- 19 Ma (maximum depositional age)|Accident Subgroup.|Train Range Ironstone Member, Middle Creek Sandstone Member.|Conformably overlies Elizabeth Sandstone. Is overlain conformably and gradationally by Tidna Sandstone.|Dominantly mudstone (shale and siltstone), punctuated by sandstone, ferruginous sandstone and ironstone, and minor conglomerate.|20-FEB-18
13391|Mullera Formation|71592|5|Briefly described|Appendix A.|||South Nicholson Basin. Sixteen age determinations are given, for MDAs and provenance clusters.|1569+/- 38 Ma (MDA: U-Pb zircon SHRIMP)||||Siltstone, shale.|
13391|Mullera Formation|71779|5|Briefly described|p23, p24, 26 p27|||South Nicholson Basin. Probably equivalent to the Velkerri Formation.||||||24-SEP-18
13391|Mullera Formation|72297|5|Briefly described|p749|||South Nicholson Basin. Poor source material; organic material has mostly reached an advanced stage of thermal maturity.|||||Includes shales.|
13391|Mullera Formation|72408|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet.||Unit of Accident Subgroup.|Includes Middle Creek Sandstone Member and Train Range Ironstone Member.||Siltstone, shale, sandstone and ironstone.|
13391|Mullera Formation|72414|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.||Unit of Accident Subgroup.|Includes Middle Creek Sandstone Member and Train Range Ironstone Member.||Siltstone, shale, sandstone and ironstone.|
13391|Mullera Formation|72415|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.||Unit of Accident Subgroup.|Includes Middle Creek Sandstone Member and Train Range Ironstone Member.||Siltstone, shale, sandstone and ironstone.|
13391|Mullera Formation|72416|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet Geological Compilation Series.||Unit of Accident Subgroup.|Includes Middle Creek Sandstone Member and Train Range Ironstone Member.||Siltstone, shale, sandstone and ironstone.|
13391|Mullera Formation|72418|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet.||Unit of Accident Subgroup.|Includes Middle Creek Sandstone Member, Train Range Sandstone Member.||Siltstone, shale, sandstone and ironstone|
13391|Mullera Formation|72421|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.||Unit of Accident Subgroup.|Includes Middle Creek Sandstone Member, Train Range Sandstone Member.||Siltstone, shale, sandstone and ironstone|
13391|Mullera Formation|72422|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series. Various additional lithologies are provided.||Unit of Accident Subgroup.|Includes Middle Creek Sandstone Member, Train Range Sandstone Member.||Siltstone, shale, sandstone and ironstone|10-DEC-19
13391|Mullera Formation|72423|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet Geological Compilation Series. Lithology of numerous other outcrops provided.||Unit of Accident Subgroup.|Includes Middle Creek Sandstone Member, Train Range Sandstone Member.||Siltstone, shale, sandstone and ironstone|18-MAR-20
13391|Mullera Formation|72526|5|Briefly described|p8 Fig.1.3, p33, p40, p46, p56|Mesoproterozoic|Mesoproterozoic|Shown as being located in the west of the South Nicholson Basin. Assumed to conformably overlie Mittiebah Sandstone but contact not exposed.||Accident Subgroup|Probably includes  Middle Creek Sandstone Member, Train Range Ironstone [Member].|Conformably overlies Constance Sandstone. Overlies Mittiebah Sandstone.||
13391|Mullera Formation|72527|6|Mentioned|p7 Fig.1.4.|Mesoproterozoic|Mesoproterozoic|South Nicholson Group.||Accident Subgroup|Includes Middle Creek Sandstone Member.|Overlies Mittiebah Sandstone and Constance Sandstone.|Includes sandstone.|
13391|Mullera Formation|72912|4|Described|p5 Fig.3, p23, p27-30, p32, p34.|Mesoproterozoic|Mesoproterozoic|Located in the west, central and east part of the South Nicholson Basin. This unit is considered to have good gas potential. See also p33 Fig.12, p34, p35 Fig.13, p37 Fig.14, p45.||Accident Subgroup|Middle Creek Sandstone Member, Train Range Ironstone Member|Overlies Mittiebah Sandstone, Constance Sandstone, underlies Tidna Sandstone.|Includes siltstone.|
13391|Mullera Formation|72913|5|Briefly described|p4, p7 Fig.2, p8, p9 Tb.1, p15, 16, 26|Mesoproterozoic|Mesoproterozoic|Shown as being in the west, central and eastern parts of the South Nicholson Basin. Mineral composition boxplots reveal dominant quartz, muscovite and kaolinite components. Identified in Amoco DDH 83-3 well.||Accident Subgroup|Middle Creek Sandstone Member, Train Range Ironstone.|Partially overlies Mittebah Sandstone, Bowthorn Member and Constance Sandstone and underlies Tidna Sandstone.|Includes siltstone, ironstone, sandstone.|
13391|Mullera Formation|72919|5|Briefly described|p5, p56-57, p70|Mesoproterozoic|Mesoproterozoic|Contact with underlying Mittiebah Sandstone is inferred to be conformably but is not exposed. Withnall and Hutton (2013) suggested the unit may be present in Morstone 1 as the portion containing glauconitic sandstones and finer units.||Accident Subgroup, South Nicholson Group|Middle Creek Sandstone Member, Train Range Ironstone Member|Underlain by Elizabeth Sandstone, Mittiebah Sandstone and Constance Sandstone, including Schultz Sandstone Member. Overlain by Tidna Sandstone and Bukalara Sandstone (unconformably).||
13391|Mullera Formation|72967|6|Mentioned|p5|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin.||South Nicholson Group||||
13391|Mullera Formation|73042|5|Briefly described|p4, p6, p9-11|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin region, Roper Superbasin. Maximum thickness: >1100m (Ahmad and Munson, 2013). Previous maximum depositional ages include 1550 +/- 51 Ma (Yang, 2019) and between ca 1750 and 1570 Ma elsewhere (Jones et al., 2018 and references therein). Present day hydrogen index suggests the unit has no present-day potential for hydrocarbon generation at the sampled locality (Jarrett et al., 2019). Re-Os sample 2777644 is tentatively interpreted as belonging to the Mullera Formation (?Mullera Formation), although a geologically permissible regression age could not be obtained. (Relationship between Mullera Formation and its possible constituents (Middle Creek Sandstone Member, Train Range Ironstone) is not clear in Fig.1.2.)||Accident Subgroup, South Nicholson Group|Middle Creek Sandstone Member, Train Range Ironstone.|Underlain by Constance Sandstone conformably and Mittiebah Sandstone. Partly overlain by Tidna Sandstone.|Siltstone, shale, sandstone, with minor ironstone.|
13391|Mullera Formation|73083|6|Mentioned|p34-35|Mesoproterozoic|Mesoproterozoic|Has numerous iron-bearing rock types, although mapped exposures have a bland, featureless, non-layered magnetic character.||||Overlain by Mittiebah Sandstone.|Includes siltstone (locally ferruginous), glauconitic sandstone with hematite 'dustings', ferruginous sandstone, ferruginous siltstone, and ironstone.|
13391|Mullera Formation|73098|6|Mentioned|p4, p7, p17|||South Nicholson Basin. Organic petrolography performed on four samples from the NTGS 00/1 well. Laminated component is characterised by alternations of bitumen-lean and bitumen-rich layers. [See report for bitumen/maceral description].|||||Includes grey to black shale and laminated brown to dark grey shale.|
13391|Mullera Formation|73144|6|Mentioned|p8|Calymmian|Calymmian|South Nicholson Basin. Aquitard with potential shale gas/oil play.||Accident Subgroup, South Nicholson Group|Middle Creek Sandstone Member, Train Range Ironstone|Underlain by Elizabeth Sandstone. Overlain by Tidna Sandstone.||
13399|Mulluk Mulluk Volcanics|9324|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Finniss River Group. Spherulitic rhyolite.||||||07-NOV-08
13399|Mulluk Mulluk Volcanics|22809|4|Described|10|Proterozoic|Proterozoic|Of the Finnis River Group.||||||13-NOV-06
13399|Mulluk Mulluk Volcanics|22810|5|Briefly described|Table2 P4|||Underlies Burrell Creek Formation.||||||13-NOV-06
13399|Mulluk Mulluk Volcanics|23715|5|Briefly described|Map legend||Proterozoic|Of the Finniss River Group. In the Litchfield Province.||||||13-NOV-06
13399|Mulluk Mulluk Volcanics|40808|5|Briefly described|Table 2|||||||||
13399|Mulluk Mulluk Volcanics|41645|6|Mentioned|p11|||||||||
13399|Mulluk Mulluk Volcanics|41661|6|Mentioned|p13|||||||||
13399|Mulluk Mulluk Volcanics|50586|6|Mentioned|p6.1|||Geological Province: Pine Creek Inlier. Of the Gerowie Suite.||||||
13399|Mulluk Mulluk Volcanics|64698|4|Described|lithinterp table|Orosirian|Orosirian|Finniss River Group. Age 1862Ma SHRIMP U/Pb. Max Thickness 2000m. Spherulitic rhyolite.||||||07-JAN-09
13399|Mulluk Mulluk Volcanics|65339|6|Mentioned|p13.|||Litchfield Province, Pine Creek Orogen.||Unit in Finniss River Group.||||
13399|Mulluk Mulluk Volcanics|67186|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Finniss River Group||Partial lateral equivalent to Burrell Creek Formation.|Metamorphosed spherulitic rhyolite.|23-NOV-11
13399|Mulluk Mulluk Volcanics|69420|4|Described|p5:6-7, 13, 87|Paleoproterozoic|Paleoproterozoic|Western region, Central Domain, Pine Creek Orogen. Unit in Finniss River Group. Comagmatic with Meeway and Berinka Volcanics, and Warrs Volcanic Member. See also reference to Mulluk Mulluk Volcanic Member (5:4). Up to 2000m thick. Aerial to subaqueous lavas.||Finniss River Group.||Is overlain conformably by, and interbedded with, basal Burrell Creek Formation.|Spherulitic rhyolite, rhyolitic tuff, rhyodacite and metadacite; typically shows strong sericitic alteration.|12-JUL-16
13468|Mungerebar Limestone|24065|5|Briefly described|p234|Late Cambrian|Late Cambrian|Geological Province: Georgina Basin.  Maximum thickness: 30m.||||||
13468|Mungerebar Limestone|30479|6|Mentioned|Fig.6|||Stratigraphic relationships||||||
13468|Mungerebar Limestone|31286|4|Described|p57|||Early Cambrian. Mindyallan Stage.||||||
13468|Mungerebar Limestone|33111|6|Mentioned|Fig.15|||||||||
13468|Mungerebar Limestone|35054|6|Mentioned|Table 23|||||||||
13468|Mungerebar Limestone|35121|6|Mentioned|Map legend|Late Cambrian|Middle Cambrian|Middle to Late Cambrian||||||
13468|Mungerebar Limestone|35139|4|Described|Table.2|||||||||
13468|Mungerebar Limestone|37275|6|Mentioned|p291|||||||||
13468|Mungerebar Limestone|37572|4|Described|p161|||See also p165 and Fig.8.||||||13-NOV-06
13468|Mungerebar Limestone|38446|6|Mentioned|Table 23|||||||||
13468|Mungerebar Limestone|38532|4|Described|Fig.1|||||||||
13468|Mungerebar Limestone|39445|5|Briefly described|Table 4|||See also p62.||||||13-NOV-06
13468|Mungerebar Limestone|39690|6|Mentioned|p88|||||||||
13468|Mungerebar Limestone|40038|6|Mentioned|p248|||||||||
13468|Mungerebar Limestone|41003|5|Briefly described|p196|||||||||
13468|Mungerebar Limestone|41810|6|Mentioned|p112|||||||||
13468|Mungerebar Limestone|42139|6|Mentioned|Fig.19 P74|||||||||
13468|Mungerebar Limestone|42994|6|Mentioned|p8|||||||||
13468|Mungerebar Limestone|44205|4|Described|p46,47|||||||||
13468|Mungerebar Limestone|44211|2|Defined|p91,95-96,100-104|||Rests on Steamboat Sandstone. Marks boundary against overlying Georgina Limestone.||||||
13468|Mungerebar Limestone|44309|2|Defined|Tb.1,p7,8-11,17|||Disconformably underlies Ninmaroo Formation.||||||
13468|Mungerebar Limestone|44326|14|Not recorded|Map Legend|Late Cambrian|Middle Cambrian|||||||
13468|Mungerebar Limestone|44543|2|Defined|p32,36|Late Cambrian|Middle Cambrian|||||||
13468|Mungerebar Limestone|44719|14|Not recorded|p143|||Lowermost Upper Cambrian. Conodonts present.||||||13-NOV-06
13468|Mungerebar Limestone|44920|14|Not recorded|Map Legend, Sheet 4|Late Cambrian|Middle Cambrian|||||||
13468|Mungerebar Limestone|45002|14|Not recorded|p23,24,43,72|||Late Cambrian fossils.||||||
13468|Mungerebar Limestone|45012|14|Not recorded|p84-86,92-107,111-15||Late Cambrian|p145-149,205-278,282-296,326-37,343-44,263-372,381-2. Mindyallan fauna.||||||
13468|Mungerebar Limestone|45052|3|Fully described|p102|||M.Camb. See also p33.||||||13-NOV-06
13468|Mungerebar Limestone|45053|6|Mentioned|p12|||||||||
13468|Mungerebar Limestone|45079|6|Mentioned|p36|||Cambrian age. Lithology||||||
13468|Mungerebar Limestone|45115|6|Mentioned|p6|||||||||
13468|Mungerebar Limestone|45130|6|Mentioned|p61|||||||||
13468|Mungerebar Limestone|46958|6|Mentioned|Fig.2|||||||||
13468|Mungerebar Limestone|48906|14|Not recorded|App.D.|||||||||
13468|Mungerebar Limestone|48971|6|Mentioned|p10|||See also p30.||||||13-NOV-06
13468|Mungerebar Limestone|60122|6|Mentioned|p18|||Conformably overlies Steamboat Sandstone.||||||
13468|Mungerebar Limestone|62790|6|Mentioned|p208, 217|Middle Cambrian|Middle Cambrian|Eastern Georgina Basin. Contains the comptalutid Aristaluta spicata Opik, 1967, in its lower (late Boomerangian) part. Also contains the svealutid Anabarochilina chummyensis (Hinz-Schallreuter, 1993c), the only known Mindyallan bradoriid.||||||28-MAR-12
13468|Mungerebar Limestone|62791|6|Mentioned|p233, p236, p239|Late Cambrian|Middle Cambrian|Source of Type species of Picnotreta debilis and Stilpnotreta magna both Henderson & MacKinnon 1981 (Mindyallan Stage).||||||04-DEC-12
13468|Mungerebar Limestone|64068|3|Fully described|p69, p65, 67, 69, 73|Late Cambrian|Middle Cambrian|Diverse fossil fauna. Correlated with Chabalowe Formation, Arrinthrunga Formation, Georgina Limestone, Selwyn Range Limestone, Cleland Sandstone. Trilobites indicate late Middle Cambrian (Boomerangian) Lejopyge laevigata Zone to early Late Cambrian (Mindyallan) Glyptagnostus stolidotus Zone (Shergold et al 1985, Shergold 1997)||Of Narpa Group.||Laterally interdigitates with and conformably overlies Steamboat Sandstone. Is overlain by Georgina Limestone conformably (Opik 1960) or Ninmaroo Formation disconformably.|Quartzic and ooid grainstone, dolomitic limestone, chert; dolostone and sandstone interbeds toward base.|21-MAR-16
13468|Mungerebar Limestone|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Middle Cambrian|Middle Cambrian|Georgina Basin.||Narpa Group|||Limestone, bituminous limestone, sandy limestone, calcilutite, minor arenite, chert nodules.|
13468|Mungerebar Limestone|69443|5|Briefly described|p28:16, 26|Middle Cambrian|Middle Cambrian|Georgina Basin.||Narpa Group.||Is overlain disconformably by Ninmaroo Formation.||12-JUL-16
13468|Mungerebar Limestone|69573|6|Mentioned|p659, 661, 669|||Georgina Basin.||||||
13468|Mungerebar Limestone|69591|5|Briefly described|p87, p91, p93, p96|Cambrian|Cambrian|Oban Sub-basin, Georgina Basin. Appears as Mungereebar Limestone on p87. Up to 30m thick. Lithologically very similar to Quita Formation. Trilobite and conodont faunas indicate Lejopyge laevigata Zone to Mindyallan.||||Transitionally overlies and interfingers with Steamboat Sandstone. Is overlain unconformably/disconformably by Ninmaroo Formation.|Thin-bedded limestone with thin chert layers and nodules; upper boundary is marked by a fine-grained dolomite.|
13468|Mungerebar Limestone|70723|5|Briefly described|p24 Fig. 2|Cambrian|Cambrian|Georgina Basin.||Narpa Group||Overlies Steamboat Sandstone. Is overlain by Georgina Limestone.|Limestone.|
13468|Mungerebar Limestone|72358|5|Briefly described|p125|||Of Georgina Basin. Includes G. stolidotus zone.||||Overlain by Georgina Limestone.||
13468|Mungerebar Limestone|72516|6|Mentioned|p93-94|Cambrian|Cambrian|Eastern Georgina Basin.||||Equivalent to the Arrinthrunga Formation and the Eurowie Sandstone Member.||08-JUN-21
13494|Munyu Sandstone|29806|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
13494|Munyu Sandstone|29807|4|Described|Table 1|||||||||
13494|Munyu Sandstone|29810|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
13494|Munyu Sandstone|29817|5|Briefly described|p9|||||||||
13494|Munyu Sandstone|29819|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
13494|Munyu Sandstone|31360|4|Described|Table 1|||||||||
13494|Munyu Sandstone|35205|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
13494|Munyu Sandstone|36532|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
13494|Munyu Sandstone|37299|6|Mentioned|Fig.1|||||||||
13494|Munyu Sandstone|45140|2|Defined|p13, p40, p43-46, p48, p56, p58 Fig.43|||See also p60, p75, p83, Appx.p23-24. Blake and Yeates (1977). Named after the Munyu Hills. Birrindudu Basin. Previously mapped as Gardiner Beds (Wells, 1962; Casey and Wells, 1964). 400m thick. The type section is across a strike ridge at 21deg 55'00"S, 128deg 55'00"E in Stansmore sheet area. Forms NE-trending strike ridges. Unconformably overlies Arunta Complex.||Basal Redcliff Pound Group.||Lateral equivalent of Muriel Range and Lewis Range Sandstones, and Vaughan Springs and Heavitree Quartzites. Is overlain by Murraba Formation conformably and Pedestal Beds unconformably.|Medium to thin-bedded, poorly sorted, medium- to very coarse-grained silicified quartz arenite; commonly with scattered pebbles and layers or lenses of grit and quartz-pebble conglomerate. Local limestone lenses and near-base sublithic arenite beds.|
13494|Munyu Sandstone|45155|6|Mentioned|p18|||||||||
13494|Munyu Sandstone|46864|4|Described|p38|||||||||
13494|Munyu Sandstone|62453|6|Mentioned|p16|||Geological Province: Murraba (formerly Birrindudu) Basin.||||||
13494|Munyu Sandstone|62580|6|Mentioned|p10|||||||||07-FEB-11
13494|Munyu Sandstone|62632|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of the Redcliff Pound Group. Geological Province: Murraba Basin. Quartz sandstone, planar crossbeds, asymmetric ripples; minor conglomerate and siltstone.||||||23-DEC-09
13494|Munyu Sandstone|62633|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of the Redcliff Pound Group. Geological Province: Murraba Basin. Medium to coarse grained sugary massive quartz sandstone; red-brown micaceous silty sandstone.||||||16-AUG-06
13494|Munyu Sandstone|64580|4|Described|map legend|Neoproterozoic|Neoproterozoic|Of Redcliff Pound Group. Quartz sandstone, conglomerate.||||||09-DEC-08
13494|Munyu Sandstone|65074|4|Described|p351 fig 4-37, p353, p356 Tb.4-12|Neoproterozoic|Neoproterozoic|Of SW Birrindudu Basin. 400m thick. Type section is on southeast STANMORE sheet; details given.||Redcliff Pound Group||Overlain by Murraba Formation (conformably). Equivalent to Muriel Range Sandstone and Lewis Range Sandstone.|Quartz arenite, grit, conglomerate, breccia, shale, siltstone, limestone, chert.|
13494|Munyu Sandstone|65332|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Redcliff Pound Group, Murraba Basin. Shown as equivalent age to Vaughan Springs Quartzite, Ngalia Basin. Medium- to coarse-grained sugary massive quartz sandstone; red-brown micaceous silty sandstone||||||02-FEB-10
13494|Munyu Sandstone|65338|6|Mentioned|p59.|||Murraba Basin. Correlated with Vaughan Springs Quartzite.||||||
13494|Munyu Sandstone|67163|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Murraba Basin. See also misspelt Munya Sandstone.||Unit in Redcliff Pound Group.||Is overlain by Murraba Formation.|Quartz sandstone: planar crossbeds, asymmetric ripples, reverse and normal grading; minor conglomerate and siltstone; weakly folded.|19-OCT-11
13494|Munyu Sandstone|68994|4|Described|p1, p8-10, p20, p22, p25, p27|Neoproterozoic|Neoproterozoic|Murraba Basin. Conservative max depositional age of 1155+/-14 Ma, although age of deposition known to be much younger based on correlation with Lewis Range Sandstone. Detrital zircon U-Pb ages listed and Hf analyses detailed. Misspelt as Munya sandstone in Fig.5.|c.1040-820 Ma (Kirkland et al. 2009).|Redcliff Pound Group||Unconformably overlies Lander Rock Formation. Equivalent to Lewis Range Sandstone, Muriel Range Sandstone  and Vaughan Springs Quartzite.|Quartz sandstone, micaceous siltstone, and minor conglomerate.|13-JAN-17
13494|Munyu Sandstone|69031|4|Described|p8|Neoproterozoic|Neoproterozoic|Murraba Basin, west Arunta Orogen. Exposed in the Alec Ross Range, where they are locally folded and faulted. Geochronology by Kirkland et al. (2009).|1155 +/- 14 Ma (maximum depositional age).|Redcliff Pound Group.||Unconformably overlies Lander Rock Formation.|Coarse-grained to pebbly sandstones.|
13494|Munyu Sandstone|69288|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Murraba Basin.||Redcliff Pound Group.|||Quartz sandstone with planar crossbeds, asymmetric ripples, and reverse and normal grading; minor conglomerate and siltstone; weakly folded.|
13494|Munyu Sandstone|69437|5|Briefly described|p22:4-6|Cryogenian|Cryogenian|Murraba Basin, Centralian A Superbasin. Supersequence 1.||Redcliff Pound Group.||Is overlain by Murraba Formation.||12-JUL-16
13494|Munyu Sandstone|69440|5|Briefly described|p25:1-2|Cryogenian|Cryogenian|Murraba Basin. Estimated thickness c.200-400m. Age is poorly constrained; inferred to correlate with Dean and Heavitree Quartzites (Amadeus Basin) and Vaughan Springs Quartzite (Ngalia Basin).||Basal Redcliff Pound Group.||Unconformably overlies Lander Rock Formation and Grimwade Suite. Is overlain conformably by Murraba Formation. Correlates with Denison beds (WA). Equivalent to Muriel Range and Lewis Range Sandstones.|Medium to thickly bedded, fine to coarse quartz sandstone; minor pebble conglomerate; rare thin beds of sublithic siltstone. Local interbedded non-fossiliferous limestone lenses near the top.|12-JUL-16
13494|Munyu Sandstone|69673|5|Briefly described|p187|||Estimated total thickness of 400m.||Redcliff Pound Group||Conformably overlain by Murraba Formation|Quartz sandstone with minor conglomerate and rare sublithic siltstone.|
13494|Munyu Sandstone|70762|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Murraba Basin, Centralian Superbasin.|<1099 Ma.||||Quartz sandstone and conglomerate.|07-NOV-16
13494|Munyu Sandstone|71080|4|Described|p4, 5-p10, 23, p27-p29, 31,36|Tonian|Tonian|Basal unit, southern Murraba Basin. Type section location on Stansmore sheet given. Named after the Munyu Hills in the NT. Outcrops on WEBB, STANSMORE and HIGHLAND ROCKS where it forms strike ridges.Max thickness 400m (Blake et al. 1979). Age inferred from correlations.  Detrital zircon maximum depositional age (1099+/-40 Ma) is similar to that for correlated units, but some of them have other constraints. Previously included in Redcliff Pound Group.The unit closely resembles the Heavitree Formation of the basal Amadeus Basin, with which it has long been correlated. No basal contact with Arunta Orogen basement is exposed in southern Stansmore map sheet area. Appears to be in fault contact with a younger carbonate unit.|Detrital zircon max dep age 1099 +/-40 Ma|||Correlated with Heavitree Formation, Dean Quartzite, Kulail Sandstone of Amadeus Basin; Vaughan Springs Quartzite Ngalia Basin.|Typically a medium-grained, well-sorted quartz sandstone, varying from thin bedded and flaggy, to more commonly thick bedded and blocky. Fine-grained quartz-pebble conglomerate occurs locally.|04-FEB-19
13494|Munyu Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sedimentary breccia, shale, sandstone, conglomerate, siltstone|
13494|Munyu Sandstone|71592|5|Briefly described|Appendix A.|||Murraba Basin.|1155+/-14 Ma (MDA: U-Pb zircon SHRIMP)||||Coarse- to very coarse-grained sandstone.|
13494|Munyu Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Tonian|Tonian|Murraba Basin.|||||Quartz sandstone and conglomerate.|
13494|Munyu Sandstone|73086|6|Mentioned|p9|||Murraba Basin, southern.||||Correlates to Heavitree Formation.||
13494|Munyu Sandstone|73445|5|Briefly described|p3, 6-8, 12-14, 24, 35, 38, 41, 43|Mesoproterozoic|Mesoproterozoic|See also p46 Fig.29, p65-118. Murraba Basin, west Arunta Orogen. Over 400m thick. Whole-rock and regolith chemistries tabulated.|1155 +/- 14 Ma (MDA: Kirkland et al., 2009).|Redcliff Pound Group.||Unconformably overlies Lake McKay Quartzite. Equivalent to Muriel Range and Lewis Range Sandstones.|Silicified quartz arenite, conglomerate, minor limestone.|
13518|Muriel Range Sandstone|29812|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
13518|Muriel Range Sandstone|29817|6|Mentioned|p10|||||||||
13518|Muriel Range Sandstone|31360|6|Mentioned|Table 1|||||||||
13518|Muriel Range Sandstone|31362|4|Described|Table 1|||||||||
13518|Muriel Range Sandstone|35205|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
13518|Muriel Range Sandstone|36532|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
13518|Muriel Range Sandstone|45140|2|Defined|p13, p22, p40, p43, p46, p48, p75|||See also Appx.p24-25. Hodgson (1976). Named after Muriel Range. Birrindudu Basin. Mapped as Phillipson Beds by Casey and Wells (1964). Forms cuestas and strike ridges. The type section across the Inningarra Range is SW of Mongrel Downs homestead, from 20deg 45'10"S, 129deg 38'45"E to 20deg 47'00"S, 129deg 54'30"E where the unit has its maximum thickness of c.450m. Lithologies described in some detail. Lateral equivalent of Munyu and Lewis Range Sandstones; distinguished by its thin to very thin beds and abundant shale pellets.||Basal Redcliff Pound Group.||Unconformably overlies Pargee Sandstone, Killi Killi and Mount Charles Bed, and The Granites Granite. Is overlain conformably by Murraba Formation, unconformably by Lucas Formation and Pedestal Beds.|Predominantly sublithic arenite and quartz arenite; minor siltstone, shale, arkose, conglomerate and breccia.|
13518|Muriel Range Sandstone|46864|4|Described|p38|||||||||
13518|Muriel Range Sandstone|50315|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of the Redcliff Pound Group. Sublithic arente, quartz arenite, minor siltstone, shale, conglomerate, arkose, breccia. Age: ~800Ma.||||||02-MAY-07
13518|Muriel Range Sandstone|50374|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Redcliff Pound Group.||||||13-NOV-06
13518|Muriel Range Sandstone|50376|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Redcliff Pound Group. Sublithic arenite, quartz arenite, minor siltstone, shale, conglomerate, arkose, breccia.||||||19-APR-06
13518|Muriel Range Sandstone|60676|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of Redcliff Pound Group. Sublithic arenite, quartz arenite, minor siltstone, shale, conglomerate, arkose, breccia.||||||19-JAN-05
13518|Muriel Range Sandstone|61861|5|Briefly described|p4, p10, 12|||Loosely correlated with Heavitree Quartzite, basal Amadeus Basin. Neoproterozoic?||Unit in Redcliff Pound Group.||Unconformably overlies Dead Bullock Formation, Killi Killi Formation.|Quartz arenite.|
13518|Muriel Range Sandstone|62377|5|Briefly described|p15|||Overlies the Dead Bullock Formation.||||||
13518|Muriel Range Sandstone|62580|6|Mentioned|p10|||||||||07-FEB-11
13518|Muriel Range Sandstone|62628|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of the Redcliff Pound Group. Geological Province: Murraba Basin. Sublithic arenite, quartz arenite, minor siltstone, shale, conglomerate, arkose breccia.||||||
13518|Muriel Range Sandstone|65074|4|Described|p351 fig 4-37, p353, p357 Tb. 4-12|Neoproterozoic|Neoproterozoic|Of North/Centre Birrindudu Basin. 450m thick. Type section is in the Inningarra Range; details given.||Redcliff Pound Group||Equivalent to Lewis Range Sandstone and Munyu Sandstone.|Quartz arenite, grit, conglomerate, breccia, shale, siltstone, limestone, chert.|
13518|Muriel Range Sandstone|65194|5|Briefly described|p89 Table 4.3|||Proterozoic sedimentary rocks. Average yield from water bores shown.||||||11-APR-16
13518|Muriel Range Sandstone|65323|5|Briefly described|Map legend, cross sect.|Neoproterozoic|Neoproterozoic|Not present on map; Of the Redcliff Pound Group; arenite, siltstone, shale, conglomerate, arkose, breccia; non-magnetic||||||10-DEC-12
13518|Muriel Range Sandstone|65324|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|Not shown on map; of the Redcliff Pound Group||||||
13518|Muriel Range Sandstone|65326|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Not shown on map; of the Redcliff Pound Group||||||12-APR-10
13518|Muriel Range Sandstone|65327|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Not shown on map; of the Redcliff Pound Group||||||12-APR-10
13518|Muriel Range Sandstone|65328|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Not shown on map; of the Redcliff Pound Group||||||12-APR-10
13518|Muriel Range Sandstone|65349|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|Not shown on map; of the Redcliff Pound Group||||||
13518|Muriel Range Sandstone|65350|5|Briefly described|Map legend|Cryogenian|Cryogenian|Of Redcliff Pound Group; sublithic arenite, quartz arenite, minor siltstone, shale, conglomerate, arkose, breccia. Age given as 800 Ma?||||||
13518|Muriel Range Sandstone|65351|5|Briefly described|Map legend|Cryogenian|Cryogenian|Of the Redcliff Pound Group; sublithic arenite, quartz arenite, minor siltstone, shale, conglomerate, arkose, breccia. Age given as 800 Ma?||||||02-MAR-10
13518|Muriel Range Sandstone|65352|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Not shown on map; Of the Redcliff Pound Group||||||12-APR-10
13518|Muriel Range Sandstone|65353|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Not shown on map; Of the Redcliff Pound Group||||||12-APR-10
13518|Muriel Range Sandstone|65354|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Not shown on map; of the Redcliff Pound Group||||||12-APR-10
13518|Muriel Range Sandstone|65355|5|Briefly described|cross section|Neoproterozoic|Neoproterozoic|Not shown on map; Of the Redcliff Pound Group||||||10-DEC-12
13518|Muriel Range Sandstone|65356|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Not shown on map; Of the Redcliff Pound Group||||||12-APR-10
13518|Muriel Range Sandstone|67168|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|||Unit in Redcliff Pound Group.||Unconformably overlies Tanami Group, Inningarra Suite and Pargee Sandstone. Is unconformably overlain by Antrim Plateau Volcanics.|Arenite, siltstone, shale, conglomerate, arkose, breccia.|
13518|Muriel Range Sandstone|68994|6|Mentioned|p20|||Murraba Basin.||||Equivalent to Munyu Sandstone.||13-JAN-17
13518|Muriel Range Sandstone|69440|5|Briefly described|p25:1-2|Cryogenian|Cryogenian|SE Tanami Region; mainly THE GRANITES map area. Maximum thickness of c.450m.||||Correlated with Munyu Sandstone.|Predominantly sublithic arenite and quartz arenite; minor siltstone, shale, arkose, conglomerate and breccia.|12-JUL-16
13518|Muriel Range Sandstone|69673|5|Briefly described|p187|||450m thick.||Redcliff Pound Group|||Sublithic arenite and quartz arenite, minor siltstone, shale, arkose, conglomerate and breccia.|
13518|Muriel Range Sandstone|70852|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Murraba Basin.||Redcliff Pound Group.|||Sublithic sandstone, quartz sandstone, minor siltstone, shale, conglomerate, arkosic breccia.|
13518|Muriel Range Sandstone|71080|5|Briefly described|p5-7, p4, p5, p27, 36|||Of Hodgson, 1976, Blake et al. 1979. Up to 450 m thick. Distinguished from its correlatives by its very thin to thin bedding and the abundance of shale pellets. In NT, so not reassessed in this GSWA study. Lies unconformably on Granites-Tanami Orogen and Tanami Basin rocks.||Previously Of Redcliff Pound Group.||Correlated with both the Lewis Range Sandstone and Munyu Sandstone (Blake et al., 1979).|Predominantly sublithic arenite and quartz arenite, but also includes minor siltstone, shale, arkose, conglomerate, and breccia.|04-FEB-19
13518|Muriel Range Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, sedimentary breccia, shale, siltstone, arenite, sandstone|
13518|Muriel Range Sandstone|73445|5|Briefly described|p7|||||Redcliff Pound Group.||Equivalent to Munyu and Lewis Range Sandstones.||
13528|Murphy Metamorphics|22457|6|Mentioned|Fig29 P30|||||||||
13528|Murphy Metamorphics|22479|5|Briefly described|fig4, pg10|Orosirian|Orosirian|||||||
13528|Murphy Metamorphics|22673|6|Mentioned|64|||Geological province: Mount Isa Basin. Overlain by Kalkadoon Granite, Leichardt Volcanics||||||13-NOV-06
13528|Murphy Metamorphics|23065|5|Briefly described|11|||||||||
13528|Murphy Metamorphics|23066|5|Briefly described|p807, Fig.1|Proterozoic|Proterozoic|||||||
13528|Murphy Metamorphics|23395|6|Mentioned|p390|||||||||
13528|Murphy Metamorphics|23405|5|Briefly described|p565|Statherian||Age: >1900Ma.||||||13-NOV-06
13528|Murphy Metamorphics|24419|6|Mentioned|p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: Murphy Province, Lawn Hill Subprovince (north); South Nicholson Basin.||||||07-NOV-08
13528|Murphy Metamorphics|24442|5|Briefly described|p23 Fig. 2|Paleoproterozoic|Paleoproterozoic|Age: ~1850Ma.  Geological Province: McArthur Basin.  See also p22 Fig. 1.||||||07-NOV-08
13528|Murphy Metamorphics|31348|6|Mentioned|p343|||||||||
13528|Murphy Metamorphics|31421|6|Mentioned|p507|||||||||
13528|Murphy Metamorphics|32659|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13528|Murphy Metamorphics|32660|5|Briefly described|Table 2|||||||||
13528|Murphy Metamorphics|33900|6|Mentioned|p7|||Redate||||||
13528|Murphy Metamorphics|35114|6|Mentioned|Table.1|||||||||
13528|Murphy Metamorphics|35950|6|Mentioned|p304|||||||||
13528|Murphy Metamorphics|36439|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13528|Murphy Metamorphics|36442|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13528|Murphy Metamorphics|36473|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13528|Murphy Metamorphics|37462|5|Briefly described|p234|||||||||
13528|Murphy Metamorphics|37565|6|Mentioned|Fig.5|||||||||
13528|Murphy Metamorphics|38066|6|Mentioned|Fig.9|||p53.||||||13-NOV-06
13528|Murphy Metamorphics|38584|4|Described|p4|||||||||
13528|Murphy Metamorphics|39338|6|Mentioned|p351|||||||||
13528|Murphy Metamorphics|39422|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Phyllite and quartz-sericite schist, quartzite, sandstone, siltstone, chert, ironstone (pyrite graphite schist below).  Unconformably overlain by Don Creek Sandstone (Carrara Range Group).  Probably Early Proterozoic.||||||07-NOV-08
13528|Murphy Metamorphics|39497|4|Described|p5|||See also p17.||||||13-NOV-06
13528|Murphy Metamorphics|39685|6|Mentioned|Fig.1|||||||||
13528|Murphy Metamorphics|39925|6|Mentioned|Fig.9|||||||||
13528|Murphy Metamorphics|40489|6|Mentioned|p88|||||||||
13528|Murphy Metamorphics|40491|6|Mentioned|p79|||||||||
13528|Murphy Metamorphics|40840|6|Mentioned|Map legend|||||||||
13528|Murphy Metamorphics|41125|6|Mentioned|p35|||See also Fig.23||||||
13528|Murphy Metamorphics|41319|6|Mentioned|p195|||||||||
13528|Murphy Metamorphics|41381|6|Mentioned|p325|||||||||
13528|Murphy Metamorphics|41406|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
13528|Murphy Metamorphics|41721|3|Fully described|p2, p6|Paleoproterozoic|Paleoproterozoic|Overlain by Cliffdale Volcanics. Intruded by Nicholson Granite Complex. Geol.Prov: Murphy Inlier. Sequence of shale, siltstone, greywacke and volcanics, metamorphosed into greenschist facies quartz-albite-muscovite-biotite schist and gneiss.||||||07-NOV-08
13528|Murphy Metamorphics|41722|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
13528|Murphy Metamorphics|41757|6|Mentioned|p207|||||||||
13528|Murphy Metamorphics|44305|14|Not recorded|p.6,8,9,10,15,17,18|||(E53-8). opp.6,18.||||||
13528|Murphy Metamorphics|44306|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
13528|Murphy Metamorphics|44482|14|Not recorded|p.6,9, opp. p.6, map|||(E53-12). See also p.13,14, for more details.||||||
13528|Murphy Metamorphics|44483|5|Briefly described|map legend||Paleoproterozoic|Defn. on Tech.File E/53-12. Lower Proterozoic.||||||07-NOV-08
13528|Murphy Metamorphics|45032|14|Not recorded|p9||Paleoproterozoic|Lower ?Proterozoic. Tb.1, Pl.1.||||||07-NOV-08
13528|Murphy Metamorphics|45052|4|Described|p69|||L.Prot. See also Table 9.||||||13-NOV-06
13528|Murphy Metamorphics|45140|6|Mentioned|p12-13|||McArthur Basin region.||||Possible correlative of Tanami Complex.||
13528|Murphy Metamorphics|45166|4|Described|p8|||||||||
13528|Murphy Metamorphics|45167|5|Briefly described|Fig.27|||||||||
13528|Murphy Metamorphics|46804|6|Mentioned|p153|||Stratigraphy||||||
13528|Murphy Metamorphics|49001|6|Mentioned|p1|||||||||
13528|Murphy Metamorphics|49018|6|Mentioned|p4|||||||||
13528|Murphy Metamorphics|50536|6|Mentioned|p3.2|||Intruded by Nicholson Suite.||||||
13528|Murphy Metamorphics|62659|5|Briefly described|Map Legend|Orosirian|Orosirian|Purple micaceous metasiltstone (phyllite), metagreywacke and quartz-mica schist with locally abundant quartz veins; minor metaquartzite, banded ironstone and calc-silicate rock.||||||
13528|Murphy Metamorphics|63866|5|Briefly described|p56||||||||Metasedimentary rocks, volcanics and migmatites.|
13528|Murphy Metamorphics|64575|6|Mentioned|p656|||Age: 1890Ma.||||||
13528|Murphy Metamorphics|65232|5|Briefly described|p9, p66, App. 2|||Unconformably underlies Cliffdale Volcanics. Intruded by  Nicholson Granite Complex. Deformed and metamorphosed succession of shale, siltstone, greywacke and volcanic rocks of Barramundi Orogeny at 1860-1845 Ma. U mineralisation. Geol Prov: Murphy Inlier.||||||09-FEB-10
13528|Murphy Metamorphics|65337|4|Described|p v, p6 Fig.3,  p10 Table 3. |Paleoproterozoic|Paleoproterozoic|Oldest exposed basement rocks in MOUNT DRUMMOND map area. Flysch sediments, metamorphosed and deformed during Barramundi Orogeny c.1870 Ma.|c.2100-1880 Ma.|||Is overlain by Connelly Volcanics, probably unconformably, and unconformably by Benmara and South Nicholson Groups.|Mainly turbiditic succession. Ferruginised outcrop and float of red-brown to purple or yellow, finely-laminated micaceous metasiltstone, metagreywacke and quartz-mica schist; minor metaquartzite and calc-silicate rock; local 5m thick horizon of BIF.|
13528|Murphy Metamorphics|65340|5|Briefly described|p7, p82.|Paleoproterozoic|Paleoproterozoic|Metasedimentary bedrock; multiple deformation and metamorphism to greenschist facies during the Barramundi Orogeny. Hosts abundant non-transported microdiamonds.|?2100 - 1845 Ma.||||Turbidites.|
13528|Murphy Metamorphics|66529|5|Briefly described|p20-21 |Paleoproterozoic|Paleoproterozoic|||||Unconformably overlain by the Cliffdale Volcanics.|Quartz-feldspar-mica schists and gneisses.|
13528|Murphy Metamorphics|67323|5|Briefly described|Mount Isa Block Time-Space Plot|Paleoproterozoic|Paleoproterozoic|See also p9, p29, Eastern Australia Time-Space Plot. Pre-Barramundi basement to Camooweal - Murphy Domain, Mount Isa Inlier. Protoliths of this unit were metamorphosed during the ~1870-1850 Ma Barramundi Orogeny.|1853 +/- 4 Ma (maximum depositional age).|||Intruded by Nicholson Granite. Overlain by Cliffdale Volcanics.||
13528|Murphy Metamorphics|68998|5|Briefly described|vi, p34-37|||Murphy Province.||||Is intruded by the Nicholson Granite Complex.||
13528|Murphy Metamorphics|69383|5|Briefly described|p38-43, 44|Paleoproterozoic|Paleoproterozoic|Murphy Inlier. LA-ICPMS U-Pb geochronology analyses. Max deposition age. Previously dated samples (Hanley 1996) were a little older: ~1870 Ma.|1853+/- 4 Ma|||Overlain by Westmoreland Conglomerate.|Immature ferruginous meta-greywacke (lower greenschist facies) sampled.|
13528|Murphy Metamorphics|69417|5|Briefly described|p2:4-5, 9|Orosirian|Orosirian|Murphy Province. Maximum depositional age.|1853 Ma (Hollis et al., 2009).|||Is intruded by Nicholson Granite Complex. Is overlain unconformably by Cliffdale Volcanics.||12-JUL-16
13528|Murphy Metamorphics|69423|4|Described|p8:1-5, 7|Orosirian|Orosirian|Murphy Inlier, Murphy Province. Possible stratigraphic equivalent of Finniss River Group (Pine Creek Orogen) and Warramunga Formation (Warramunga Province). Isoclinally folded; dips vertically or steeply to N. LA-ICPMS detrital zircon maximum deposition age; Hollis et al. (2010). Minimum depositional age of c.1850 Ma from stratigraphic relationships. Hosts the Coanjula microdiamond occurrence; also minor uranium occurrences in the W of the Inlier near the contact with the Nicholson Granite Complex.|<1853 +/- 4 Ma to c.1850 Ma.|||Is overlain unconformably by Cliffdale Volcanics. Is intruded by Nicholson Granite Complex.|A succession of greenschist-facies metamorphosed shale and greywacke: phyllite, schist and quartzite. A 5m-thick banded ironstone is present locally. Numerous quartz veins. Banded chert and hematitic ironstone, pyritic and graphitic at depth.|12-JUL-16
13528|Murphy Metamorphics|69430|5|Briefly described|p15:11, 51|||Hosts minor U mineralisation associated with faults and fractures.||||Is overlain unconformably by Westmoreland Conglomerate (Tawallah Group).||12-JUL-16
13528|Murphy Metamorphics|69433|5|Briefly described|p18:2, 4-5|||Murphy Province. Basement to the Lawn Hill Platform succession.||||Is overlain unconformably by Carrara Range and Benmara Groups (Lawn Hill Platform).||12-JUL-16
13528|Murphy Metamorphics|69434|5|Briefly described|p19:1, 4-5|Paleoproterozoic|Paleoproterozoic|Murphy Inlier. A source of siliciclastic sediments for the Caulfield beds, South Nicholson Basin.||||Is overlain unconformably by Crow Formation (South Nicholson Group).||12-JUL-16
13528|Murphy Metamorphics|69510|5|Briefly described|piii, p17-19, 21|||SHRIMP U-Pb zircon maximum depositional age. The intrusion at 1846 +/- 6 Ma provides a minimum depositional age for the sedimentary protolith. Previous age determinations (c.1870 Ma and c.1853 Ma) are mentioned.|1864.3 +/- 5.0 Ma (Kositcin et al., 2014).|||Is intruded by the Nicholson Granite.|Includes lithic greywacke interlayered with minor banded shale and quartzwacke.|
13528|Murphy Metamorphics|69591|5|Briefly described|p30-31, p58|||Camooweal-Murphy Domain. Does not crop out in Qld, but is inferred in the subsurface of the Murphy Tectonic Ridge. Considered part of the same depositional package as the Murphy and Yaringa Metamorphics. Minimum age (Page et al., 2000) from intrusion.|>1856 Ma.|||Is intruded by Nicholson Granite.|Quartz-albite-muscovite-biotite schist; gneiss, phyllite and migmatite.|
13528|Murphy Metamorphics|69673|6|Mentioned|p3 fig 2, p51|Orosirian|Orosirian|||||||
13528|Murphy Metamorphics|70849|5|Briefly described|Map legend.|Orosirian|Orosirian|Murphy Province.||||Is overlain unconformably by Wire Creek Sandstone (Tawallah Group equivalent). Is intruded by Nicholson Granite Complex.|Undivided: metasedimentary rocks, commonly sheared and brecciated; quartz-albite-mica schist. Separately mapped: metasiltstone and metashale; immature metasandstone, poorly sorted, fine- to coarse-grained, micaceous.|
13528|Murphy Metamorphics|71592|5|Briefly described|Appendix A.|||Murphy Region.|1853+/-4 Ma (MDA: U-Pb zircon LA-ICPMS).||||Greywacke.|
13528|Murphy Metamorphics|71606|5|Briefly described|p137|Orosirian|Orosirian|Murphy Tectonic Ridge and South Nicholson Basin.||||Overlain unconformably by Cliffdale Volcanics and Wire Creek Sandstone, and Nicholson Granite. Equivalent to Yaringa Metamorphics.||
13528|Murphy Metamorphics|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Basement to McArthur Basin.||||||05-MAR-20
13528|Murphy Metamorphics|72526|5|Briefly described|p8 Fig.1.3, p6 Fig.1.2.|Orosirian|Orosirian|Shown as being located in the west and central part of the South Nicholson Basin and the Southeastern McArthur Basin.||||Shown as underlying Cliffdale Volcanics.||
13528|Murphy Metamorphics|72527|4|Described|p3, p5, p7, 9, 161, 181, p184-191, p192|Paleoproterozoic|Paleoproterozoic|Murphy Province. Sample gives 1874+/-7 Ma max.dep.age. Previous detrital zircon geochronology results: 1867+/-7 Ma, 1864+/-5 Ma, 1852+/-4 Ma. Minimum age constrained by overlying and intruding units. Considered to represent a succession of turbidites prior to metamorphism. The siliclastic detritus generated by this unit is thought to contribute to the Caulfield beds. Correlated with Burrell Creek Formation, Yaringa Metamorphics, Inverway Metamorphics, Lander Rock Formation. See also p193 Fig.9.1, p194.|Depositional age 1867-1845 Ma.|||Unconformably underlies Wire Creek Sandstone, Cliffdale Volcanics. Extensively intruded by Nicholson Granite complex.|Greenschist-facies shales, schists, meta-siltstones, meta-arenites, meta-greywackes, meta-volcanics and rare banded ironstone.|
13528|Murphy Metamorphics|72912|5|Briefly described|p5 Fig.3, p20.|Orosirian|Orosirian|Basement rocks located in the west part of the South Nicholson Basin and the Southeastern McArthur Basin.|c. 1850 Ma|||Shown as underlying Cliffdale Volcanics. Faulted against South Nicholson Group at Benmara Fault.||15-MAR-21
13528|Murphy Metamorphics|72919|6|Mentioned|p5-7, p11, p16|Paleoproterozoic|Paleoproterozoic|Murphy Province, North Australian Craton.||||Intruded by Nicholson Granite Complex. Unconformably overlain by Cliffdale Volcanics.||
13528|Murphy Metamorphics|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin and South Nicholson Basin region.||||||
13528|Murphy Metamorphics|73043|6|Mentioned|p7 Fig.2|Paleoproterozoic|Paleoproterozoic|Geological Province: Murphy Province.||||||
13528|Murphy Metamorphics|73089|5|Briefly described|p32, p34|||Murphy Province. Contains dominant detrital zircon age components of 1867 +/- 7 and 1853 +/- 4 Ma, with a smaller proportion of early Paleoproterozoic to Neoarchean grains. Unconformably overlain by 1851 +/- 3 Ma felsic volcanic rocks.|||||Turbiditic shale and greywacke with lesser ironstone, quartzite and chert.|
13528|Murphy Metamorphics|73427|4|Described|p3, p5-6, p12-14, App.A|Orosirian|Orosirian|North Australian Craton, Murphy Inlier/Murphy Province. Also exposed in the Carrara Range Inlier. Represents turbidity flows and chemical sediments deposited in a deep marine or shelf setting. Previous maximum depositional ages include 1874 +/- 7 Ma (Kositcin and Carson, 2019) and 1867 +/- 7 Ma (Hanley, 1996). Sampled for monazite U-Pb dating to constrain deformation and metamorphism. Deformed and metamorphosed during the Murphy Event (D1/M1: 1860-1855 Ma); isoclinally folded about east-trending axes and dip steeply to the north; greenschist-facies metamorphism. A second episode of ductile deformation and metamorphism (D2/M2) occurred during the waning stage of, or after, 1855-1845 Ma igneous activity.|ca 1860 Ma|||Crosscut by Nicholson Granite.|Shale, siltstone, greywacke, schist and felsic volcanic rocks, with rare banded ironstone and calc-silicate rock.|
13528|Murphy Metamorphics|73525|6|Mentioned|p4-5 Fig.2, p19 Fig.13|||Mount Oxide-(Ardmore-May Downs) and Leichhardt River Domains.|||||Metamorphics.|
13529|Murraba Formation|22496|6|Mentioned|p10|||||||||
13529|Murraba Formation|23314|5|Briefly described|336|||||||||
13529|Murraba Formation|29806|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
13529|Murraba Formation|29807|4|Described|Table 1|||||||||
13529|Murraba Formation|29810|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
13529|Murraba Formation|29813|4|Described|Table 2|||||||||
13529|Murraba Formation|29817|5|Briefly described|p9|||||||||
13529|Murraba Formation|29818|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
13529|Murraba Formation|29819|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
13529|Murraba Formation|31360|4|Described|Table 1|||||||||
13529|Murraba Formation|35205|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
13529|Murraba Formation|36532|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
13529|Murraba Formation|45140|2|Defined|p13, p40, p43-45, p47-48, p50-51, p55-56|||See also p58 Fig.43, Appx.p26-27. Blake and Yeates (1977). Named after Murraba Ranges. Birrindudu Basin. Mapped as Gardiner Beds and Phillipson Beds by Casey and Wells (1964). Forms subdued strike ridges and low cuestas. 800m thick; only 350m at the type section at 21deg 36'30"S, 128deg 46'30"E. Folded into gentle curves.||Redcliff Pound Group.||Conformably overlies Munyu and Lewis Range Sandstones. Is overlain by Hazlett Beds, and conformably by Erica Sandstone. Probable correlative of Jawilga Beds and Bitter Springs Formation.|Interbedded chert-granule conglomerate, sublithic arenite, quartz arenite, siltstone, shale, mudstone, pebble conglomerate and dolomite. Beds are mainly thin to laminated.|
13529|Murraba Formation|46864|4|Described|p38|||||||||
13529|Murraba Formation|62632|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of the Redcliff Pound Group. Geological Province: Murraba Basin. Conglomerate, rounded to subangular coarse grained sand to pebbles, quartz and chert clasts, minor arenite.||||||23-DEC-09
13529|Murraba Formation|65074|4|Described|p351 fig 4-37, p353, p356 Tb. 4-12, p362|Neoproterozoic|Neoproterozoic|Of  Birrindudu Basin. 20-800m thick. Type section is at Redcliff Pound.||Redcliff Pound Group||Overlies Munyu and Lewis Range Sandstones conformably. Equivalent to Jawilga beds. Overlain conformably by Erica Sandstone.|Chert-granule conglomerate, arenite, siltstone, shale, mudstone, pebble conglomerate, dolomite.|
13529|Murraba Formation|67163|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Murraba Basin.||Unit in Redcliff Pound Group.||Overlies Munyu Sandstone. Is overlain by Erica Sandstone.|Conglomerate: rounded to subangular coarse-grained sand to pebbles, quartz and chert clasts; minor arenite.|19-OCT-11
13529|Murraba Formation|69288|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Murraba Basin.||Redcliff Pound Group.|||Conglomerate with rounded to subangular coarse-grained sand to pebbles, quartz and chert clasts, minor arenite.|
13529|Murraba Formation|69437|5|Briefly described|p22:4-6|Cryogenian|Cryogenian|Murraba Basin, Centralian A Superbasin. Supersequence 1.||Redcliff Pound Group.||Overlies Munyu Sandstone. Is overlain by Erica Sandstone.||12-JUL-16
13529|Murraba Formation|69440|4|Described|p25:1-3|Cryogenian|Cryogenian|Murraba Basin. Most extensive exposures are in WA; some outcrops occur in the Sydney Margaret Range. Up to 800m thick. Interpreted to have been deposited in fluvial to less-common shallow-marine environments and at times was emergent.||Redcliff Pound Group.||Conformably overlies Munyu and Lewis Range Sandstones. Is overlain conformably by Erica Sandstone. Correlates with Jawilga beds (WA).|Conglomerate, sublithic and quartz sandstone; rare mudstone and dolostone.|12-JUL-16
13529|Murraba Formation|69673|5|Briefly described|p187|||800m thick (in WA).||Redcliff Pound Group||Conformably overlies Munyu Sandstone, conformably overlain by Erica Sandstone|Conglomerate and sublithic sandstone, quartz sandstone, with rare mudstone and dolostone.|
13529|Murraba Formation|70129|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Murraba Basin, Centralian Superbasin.||Redcliff Pound Group.|||Chert-clast granule and pebble conglomerate, sandstone, siltstone and mudstone; minor limestone; thin-bedded (section only).|
13529|Murraba Formation|70130|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Murraba Basin, Centralian Superbasin.||Redcliff Pound Group.||Overlies Lewis Range Sandstone. Is overlain by Erica Sandstone.|Chert-clast granule and pebble conglomerate, sandstone, siltstone and mudstone; minor limestone; thin-bedded.|
13529|Murraba Formation|71080|4|Described|p11-p18, 21, 27, 28, 29, 32,36-37|Ediacaran|Ediacaran|Murraba Basin. Named for the Murraba Ranges on STANSMORE. 350 m thick in type section. Definition needs revision. Cenozoic cover obscures previously inferred relationships in Stansmore map sheet area. Picking boundary with overlying Erica Sandstone is problematic. Thickness estimated at 220m at western end of Phillipson Range. Includes Arumberia and tubular body fossils. See also p4, 5,||Redcliff Pound Group||Basal unconformity inferred. Conformably overlain by Erica Formation.|Interbedded chert-granule conglomerate, sublithic arenite, quartz arenite, siltstone, shale, pebble conglomerate and dolomite.|04-FEB-19
13529|Murraba Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, siltstone, shale, conglomerate|
13529|Murraba Formation|73445|5|Briefly described|p7-8, 10|||The boundary with Erica Sandstone is time-transgressive.||Redcliff Pound Group.||Overlies Lewis Range Formation. Is overlain by Erica Sandstone.|Siliciclastic sedimentary rocks.|
13596|Musgrave Complex|22506|6|Mentioned|p129|||||||||
13596|Musgrave Complex|22635|6|Mentioned|p492||Mesoproterozoic|||||||
13596|Musgrave Complex|22806|5|Briefly described|p484||Precambrian|||||||
13596|Musgrave Complex|22824|6|Mentioned|Fig 1 on p530|||||||||
13596|Musgrave Complex|22826|6|Mentioned|Fig 1 on p564|||||||||
13596|Musgrave Complex|23205|6|Mentioned|p302|Proterozoic|Proterozoic|||||||
13596|Musgrave Complex|23463|6|Mentioned|p240|||||||||
13596|Musgrave Complex|23571|5|Briefly described|p4 Fig. 2, p7|||Geological Province: Officer Basin. Overlain by Townsend Quartzite (unconformable)||||||13-NOV-06
13596|Musgrave Complex|23590|6|Mentioned|p4|||||||||
13596|Musgrave Complex|23745|5|Briefly described|p15|Mesoproterozoic|Mesoproterozoic|Also called Wingelina complex. Age: c.1550-1200 Ma.||||||
13596|Musgrave Complex|23758|6|Mentioned|p5|||||||||
13596|Musgrave Complex|23760|6|Mentioned|p5|||||||||
13596|Musgrave Complex|24115|6|Mentioned|p28|Mesoproterozoic|Mesoproterozoic|||||||
13596|Musgrave Complex|24390|6|Mentioned|p9|||||||||
13596|Musgrave Complex|24410|6|Mentioned|p36, p37|||Name used in structural context.||||||
13596|Musgrave Complex|24535|6|Mentioned|p16, p19 Fig.15|Mesoproterozoic|Mesoproterozoic|Text uses this name as a geological province. Fig 15 shows includes bimodal magmatism 1090 - 1049 Ma.||||||
13596|Musgrave Complex|38066|5|Briefly described|p50|||||||||
13596|Musgrave Complex|41190|6|Mentioned|p264|||||||||
13596|Musgrave Complex|41270|6|Mentioned|p267|||||||||
13596|Musgrave Complex|41594|5|Briefly described|p72|||||||||
13596|Musgrave Complex|41717|6|Mentioned|p248|||||||||
13596|Musgrave Complex|41852|5|Briefly described|p208|||||||||
13596|Musgrave Complex|42049|6|Mentioned|Fig.1 P216|||||||||
13596|Musgrave Complex|42730|4|Described|p16|||||||||
13596|Musgrave Complex|43442|6|Mentioned|Fig.5,p16|||Probably used as a geological province.||||||
13596|Musgrave Complex|49895|6|Mentioned|p5|||||||||
13596|Musgrave Complex|50008|6|Mentioned|p47 Fig.4|||||||||
13596|Musgrave Complex|50085|6|Mentioned|p9|||Geological Province: Officer Basin.||||||
13596|Musgrave Complex|50127|6|Mentioned|p48 Fig. 2|||Structural term.||||||
13596|Musgrave Complex|50205|6|Mentioned|p60|||Includes the Tollu Volcanics.||||||
13596|Musgrave Complex|50222|6|Mentioned|p334 Tb. 2|Mesoproterozoic|Mesoproterozoic|Age: 1.06Ga.||||||
13596|Musgrave Complex|50228|5|Briefly described|p477|Mesoproterozoic|Mesoproterozoic|Geological Province: West Australian Craton.||||||
13596|Musgrave Complex|50544|6|Mentioned|p55, p60|||Intended as a structural term in this context.||||||
13596|Musgrave Complex|50621|6|Mentioned|p165 Fig.6, p167|||Geological Province Paterson Orogen.||||||
13596|Musgrave Complex|60470|6|Mentioned|p5|Mesoproterozoic|Mesoproterozoic|Includes zircon-bearing rocks of ~1070 Ma. Possible source material for Throssell Range and Lamil Group rocks.||||||
13596|Musgrave Complex|61023|6|Mentioned|p13|||||||||
13596|Musgrave Complex|61064|5|Briefly described|p5, p12|Neoproterozoic|Mesoproterozoic|See also pages 38 and 49.||||||
13596|Musgrave Complex|61272|5|Briefly described|p123 Fig.4|||Unconformably overlain by the Townsend Quartzite.||||||
13596|Musgrave Complex|61306|6|Mentioned|p11|Proterozoic|Proterozoic|Geological Province: Amadeus Basin.||||||
13596|Musgrave Complex|61564|6|Mentioned|p589 Fig. 1|||Structural term in this context.||||||
13596|Musgrave Complex|61732|6|Mentioned|p36, p56, p84|||Structural term in this context. See also p90.||||||07-FEB-11
13596|Musgrave Complex|61733|5|Briefly described|p55|||Discussion of crustal material required for Nd isotopic signature.|||||Felsic gneisses.|
13596|Musgrave Complex|62453|5|Briefly described|p4|Mesoproterozoic|Mesoproterozoic|||||||
13596|Musgrave Complex|62986|6|Mentioned|p18|||||||||
13596|Musgrave Complex|62987|6|Mentioned|p30|||||||||
13596|Musgrave Complex|63465|6|Mentioned|p553 Fig. 2|||Includes granulites.||||||
13596|Musgrave Complex|63869|6|Mentioned|p3 Fig.1|||||||||
13596|Musgrave Complex|64283|6|Mentioned|p55|||||||||07-FEB-11
13596|Musgrave Complex|64325|6|Mentioned|p80, p84, p85|Mesoproterozoic|Mesoproterozoic|||||||
13596|Musgrave Complex|64577|6|Mentioned|p605|||||||||
13596|Musgrave Complex|64635|6|Mentioned|p2 Fig.1|||||||||
13596|Musgrave Complex|64777|6|Mentioned|p1 Fig.1, p3, p7-8|||||||||
13596|Musgrave Complex|64793|6|Mentioned|p282 Fig.1|||||||||
13596|Musgrave Complex|64943|6|Mentioned|p2|Mesoproterozoic|Mesoproterozoic|Of central Australia (Williams and Myers 1990). Considered part of the Paterson Orogen.||||||
13596|Musgrave Complex|65363|6|Mentioned|p4.|||||||||
13596|Musgrave Complex|65410|6|Mentioned|p73 Fig.2.|Proterozoic|Proterozoic|Officer and Amadeus Basins.||||||
13596|Musgrave Complex|65416|5|Briefly described|pp135-137, p145.|Mesoproterozoic|Paleoproterozoic|Western Officer Basin. Metasedimentary and meta-igneous rocks, overlain by Mission and Cassidy Groups. Post-Cambrian movement saw this unit stepped further to the south than the Rudall Complex.||||||
13596|Musgrave Complex|65454|6|Mentioned|p12|||||||||
13596|Musgrave Complex|65487|6|Mentioned|p9|||Potentially contiguous with the Albany-Fraser Orogen to the SW.||||||
13596|Musgrave Complex|65826|6|Mentioned|p5. |Proterozoic|Proterozoic|Paterson Orogen rocks outcrop in this part of central Australia. Name used in 'geological province' sense.||||||23-MAY-16
13596|Musgrave Complex|65833|4|Described|p1-18|Neoproterozoic|Mesoproterozoic|Includes Wirku Metamorphics.||||||
13596|Musgrave Complex|66256|6|Mentioned|p2|||Of Myers et al. (1996). Term now replaced by Musgrave Province.||||||
13596|Musgrave Complex|66427|6|Mentioned|p40 Fig.1|||Mafic magmatism c.1.06 Ga.||||||
13596|Musgrave Complex|67581|6|Mentioned|p44 Fig.8|||||||||
13596|Musgrave Complex|70125|6|Mentioned|p403, p408|||Central Australia.||||||
13596|Musgrave Complex|70634|6|Mentioned|174558.1.pdf|||Used interchangeably as a geological province.|||Includes Pitjantjatjara Supersuite, Wirku Metamorphics|||
13596|Musgrave Complex|72476|6|Mentioned|p36|||Detrital zircon ages suggest the Musgrave Block was exhumed 590 Ma and 420 Ma.||||||
13635|Myally Subgroup|22438|4|Described|p535, Fig.3 p537|||See also Fig.10a p546||||||
13635|Myally Subgroup|22585|5|Briefly described|P739, Fig1|||||||||
13635|Myally Subgroup|22644|5|Briefly described|5|||Geological province: Mount Isa Basin. Overlain by Quilalar Formation||||||18-JAN-07
13635|Myally Subgroup|23031|5|Briefly described|24|||Geological province: Mount Isa Fold Belt. Underlain by Leander Quartzite, Eastern Creek Volcanics.||||||13-NOV-06
13635|Myally Subgroup|23073|5|Briefly described|p744 (fig 2), p748|||||||||
13635|Myally Subgroup|23393|5|Briefly described|p18, p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|Of Haslingden Group.  Geological Province: Mount Isa Fold Belt.||||||07-NOV-08
13635|Myally Subgroup|23395|4|Described|p384 Fig.2|||Of the Haslingden Group.||||||13-NOV-06
13635|Myally Subgroup|23396|5|Briefly described|p407 Fig.2|||Of the Haslingden Group.||||||13-NOV-06
13635|Myally Subgroup|23397|6|Mentioned|p467|||||||||
13635|Myally Subgroup|23399|5|Briefly described|p500|||||||||
13635|Myally Subgroup|23408|6|Mentioned|p511, p515|||Underlies Torpedo Creek Quartzite.||||||15-JUN-09
13635|Myally Subgroup|23466|5|Briefly described|p265|||||||||
13635|Myally Subgroup|23518|4|Described|p9 Fig. 3, p11|Proterozoic|Proterozoic|Geological Province: Western Fold Belt. Of the Haslingden Group.||||||
13635|Myally Subgroup|23767|5|Briefly described|p1954 Fig. 1a|||Maximum thickness: ~2500m.   Geological Province: Leichhardt Superbasin. See also p1955.||||||
13635|Myally Subgroup|23965|4|Described|p1296|Paleoproterozoic|Paleoproterozoic|Of Haslingden Group. Geological Province: Mount Isa Inlier.||||||07-NOV-08
13635|Myally Subgroup|23969|6|Mentioned|p1371 Fig.2|||Geological Province: Mount Isa Inlier. Of the Haslingden Group.||||||
13635|Myally Subgroup|24308|5|Briefly described|p991, p987 Fig.2|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13635|Myally Subgroup|24419|5|Briefly described|p16, p13 Fig. 5, p12 Fig. 4|Proterozoic|Proterozoic|Formerly the Judenan beds. Of the Haslingden Group.  Conformably overlies Mount Guide Quartzite and Eastern Creek Volcanics. Geological Province: Leichardt River Subprovince and Lawn Hill Subprovince. See also p15 Fig. 6.||||||18-JAN-07
13635|Myally Subgroup|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Overlies Eastern Creek Volcanics. Overlain by Quilalar Formation.||||||
13635|Myally Subgroup|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Haslingden Group.||||||25-AUG-04
13635|Myally Subgroup|30534|6|Mentioned|p303|||Revision of name||||||
13635|Myally Subgroup|30535|6|Mentioned|p403|||||||||
13635|Myally Subgroup|33900|4|Described|p12|||Mention p10.||||||13-NOV-06
13635|Myally Subgroup|35074|6|Mentioned|Fig.2|||||||||
13635|Myally Subgroup|35286|6|Mentioned|Fig.17|||||||||
13635|Myally Subgroup|35295|6|Mentioned|Fig.2|||||||||
13635|Myally Subgroup|35369|6|Mentioned|Table 1|||Stratigraphy||||||
13635|Myally Subgroup|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
13635|Myally Subgroup|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
13635|Myally Subgroup|36548|6|Mentioned|p513|||||||||
13635|Myally Subgroup|37459|6|Mentioned|p423|||||||||
13635|Myally Subgroup|37462|6|Mentioned|p266|||||||||
13635|Myally Subgroup|37568|5|Briefly described|p81|||See also p85.||||||13-NOV-06
13635|Myally Subgroup|37569|6|Mentioned|p91|||||||||
13635|Myally Subgroup|38232|6|Mentioned|p84|||||||||
13635|Myally Subgroup|38233|5|Briefly described|Table 1|||||||||
13635|Myally Subgroup|38235|6|Mentioned|p113|||||||||
13635|Myally Subgroup|38237|6|Mentioned|p132|||||||||
13635|Myally Subgroup|38276|6|Mentioned|Fig.1|||||||||
13635|Myally Subgroup|38350|6|Mentioned|p10|||||||||
13635|Myally Subgroup|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
13635|Myally Subgroup|38560|6|Mentioned|p113|||||||||
13635|Myally Subgroup|38919|6|Mentioned|p494|||||||||
13635|Myally Subgroup|39362|6|Mentioned|Fig.1|||||||||
13635|Myally Subgroup|39445|5|Briefly described|p35|||See also p40 and Table 2.||||||13-NOV-06
13635|Myally Subgroup|39556|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||
13635|Myally Subgroup|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Haslingden Group.  Includes: Alsace Quartzite, Bortala Fm., Whitworth Quartzite and Lochness Formation.||||||15-JUN-06
13635|Myally Subgroup|39622|6|Mentioned|p21|||||||||
13635|Myally Subgroup|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
13635|Myally Subgroup|39925|6|Mentioned|Fig.9|||||||||
13635|Myally Subgroup|39934|6|Mentioned|Fig.3|||||||||
13635|Myally Subgroup|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
13635|Myally Subgroup|40202|6|Mentioned|p719|||||||||
13635|Myally Subgroup|40221|3|Fully described|p8|||||||||
13635|Myally Subgroup|40394|6|Mentioned|p284|||||||||
13635|Myally Subgroup|40598|6|Mentioned|Fig.1|||||||||
13635|Myally Subgroup|40623|5|Briefly described|p98|||||||||
13635|Myally Subgroup|40840|6|Mentioned|Map legend|||||||||
13635|Myally Subgroup|41277|6|Mentioned|p83|||||||||
13635|Myally Subgroup|41298|6|Mentioned|Map legend|Carpentarian||||||||
13635|Myally Subgroup|41307|4|Described|p9|||||||||
13635|Myally Subgroup|41978|6|Mentioned|p501|||||||||
13635|Myally Subgroup|41979|6|Mentioned|Fig.2 P512|||||||||
13635|Myally Subgroup|42234|5|Briefly described|p1056|||||||||
13635|Myally Subgroup|42367|6|Mentioned|p17|||Part of Haslingden Group||||||
13635|Myally Subgroup|42503|6|Mentioned|p336|||||||||
13635|Myally Subgroup|42523|5|Briefly described|p372|||||||||
13635|Myally Subgroup|42565|5|Briefly described|Table 1 P5, P2|||||||||
13635|Myally Subgroup|42676|5|Briefly described|Fig.2 P41|||||||||
13635|Myally Subgroup|42706|5|Briefly described|map legend|Proterozoic|Proterozoic|Upper part of the Haslingden Group.||||||09-FEB-09
13635|Myally Subgroup|42782|5|Briefly described|p458|||||||||
13635|Myally Subgroup|42818|4|Described|p211, Table 1 p208|||Of the Haslingden Group.||||||13-NOV-06
13635|Myally Subgroup|43608|6|Mentioned|Fig.11,p11|||||||||
13635|Myally Subgroup|43616|6|Mentioned|p3|||||||||
13635|Myally Subgroup|43760|5|Briefly described|p431|||||||||
13635|Myally Subgroup|43788|6|Mentioned|p20|||||||||
13635|Myally Subgroup|43928|6|Mentioned|23|||||||||
13635|Myally Subgroup|44195|6|Mentioned|p356 Fig.9|||||||||
13635|Myally Subgroup|45136|4|Described|Table 1|||||||||
13635|Myally Subgroup|45161|6|Mentioned|p12|||||||||
13635|Myally Subgroup|45166|4|Described|p16|||||||||
13635|Myally Subgroup|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
13635|Myally Subgroup|46960|6|Mentioned|p215|||||||||
13635|Myally Subgroup|46962|4|Described|Table 1|||See also Fig.3.||||||
13635|Myally Subgroup|46995|5|Briefly described|p268|||||||||
13635|Myally Subgroup|46996|6|Mentioned|p273|||||||||
13635|Myally Subgroup|47083|4|Described|p6-10||Proterozoic|Of Haslingden Group. Overlain by Quilalar Fm - conformable. Underlain by Eastern Creek Volcanics.||||||13-NOV-06
13635|Myally Subgroup|50100|5|Briefly described|p16|Proterozoic|Proterozoic|Of the Haslingden Group.  Unconformably overlies the Leichhardt Volcanics; conformably overlies the Eastern Creek Volcanics.||||||
13635|Myally Subgroup|50332|5|Briefly described|p17, p70|Proterozoic|Proterozoic|Includes; Alsace Quartzite, Bortala Formation, Whitworth Quartzite and Lochness Formation. Conformably overlies Eastern Creek Volcanics. Consists of feldspathic and quartz sandstones, with minor dolomitic and calcareous beds and felsic volcanics.||||||07-FEB-11
13635|Myally Subgroup|50536|6|Mentioned|p8.4|||Geological Province: Mount Isa Inlier. Intruded by Sybella Suite.||||||
13635|Myally Subgroup|50550|5|Briefly described|p1139 Fig.2||Statherian|Age: 1756 Ma, 1742 Ma. Conformably overlies Eastern Creek Volcanics. Geological Province: Western Fold Belt.||||||19-DEC-07
13635|Myally Subgroup|50624|5|Briefly described|p234 Fig.2||Paleoproterozoic|Of the Haslingden Group.||||||07-NOV-08
13635|Myally Subgroup|60558|5|Briefly described|p4 Fig. 3|Paleoproterozoic|Paleoproterozoic|Geological Province: Western Fold Belt.||||||03-JUN-09
13635|Myally Subgroup|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: >1750Ma. Geological Province: western Mount Isa Block.||||||07-NOV-08
13635|Myally Subgroup|61922|5|Briefly described|p8, p9 Fig. 3|||An immature ferruginous quartz arenite. Discordantly overlies the Eastern Creek Volcanics. Geological Province: Mount Isa Inlier/Western Fold Belt.  See also p19 Fig.11,  p21 Fig.13..||||||
13635|Myally Subgroup|61923|5|Briefly described|p29 Fig.2, p30|||Upper section of the Haslingden Group. Generally a sandstone series consisting of either mature, silica-cemented white quartzite or immature, orange weathering ferruginous sandstone. Geological Province: Mount Isa Inlier.||||||
13635|Myally Subgroup|61929|5|Briefly described|p128 Fig. 2|||Includes Alsace Quartzite, Bortala Formation and Whitworth Quartzite.||||||
13635|Myally Subgroup|61936|5|Briefly described|p193|||Overlies Eastern Creek Volcanics; overlain by Quilalar Formation. Geological Province: Leichhardt Superbasin, Western Fold Belt, Mount Isa Inlier.||||||
13635|Myally Subgroup|62084|6|Mentioned|p936 Fig.5|||Leichhardt Superbasin.||||||
13635|Myally Subgroup|62288|5|Briefly described|p122 Fig. 2, p34|Paleoproterozoic|Paleoproterozoic|Geological Province: Western Fold Belt/ Mount Isa Inlier.||||||07-NOV-08
13635|Myally Subgroup|62988|5|Briefly described|p34|Paleoproterozoic|Paleoproterozoic|Included in the Myally Supersequence spanning the interval ~1780-1765Ma. Geological Province: Mount Isa Inlier.||||||07-NOV-08
13635|Myally Subgroup|63023|5|Briefly described|p1025 Fig. 2|||Geological Province: Leichhardt Superbasin.||||||22-JUL-13
13635|Myally Subgroup|63111|5|Briefly described|p1163 Fig. 3, p1164 Tb. 1|Statherian|Statherian|Includes; Alsace Quartzite, Bortalla Formation, Whitworth Quartzite, Lochness Formation. Overlain by Quilalar Formation, underlain by Mount Guide Quartzite. Thickness: 4000m. Geological Province: Leichhardt Superbasin.||||||07-FEB-11
13635|Myally Subgroup|63113|5|Briefly described|p1214 Fig.2.||||||Includes the Whitworth Quartzite; Lochness, Quilalar, Fiery Creek and Surprise Creek Formations.|||
13635|Myally Subgroup|63114|5|Briefly described|p1253 Fig.2. |||Leichhardt superbasin.|||Includes the Lochness Formation, Whitworth Quartzite, Bortala Formation and Alsace Quartzite.|Overlies Eastern Creek Volcanics. Is overlain by Quilalar Formation.||
13635|Myally Subgroup|63593|5|Briefly described|p288 Fig.2, p291 Fig.3 and Tb.2.|||Western Fold Belt. 4000 m thick.|||||Mainly sandstone, minor siltstone.|
13635|Myally Subgroup|63884|5|Briefly described|p14|||Siliciclastic; quartzite, sandstone and siltstone.||||||
13635|Myally Subgroup|64250|5|Briefly described|p11 fig 3, p19, p22, p23, p27|||Western Fold Belt, Mount Isa Inlier. Forms a single Supersequence with the Eastern Creek Volcanics.|1773 +/- 2 Ma|Haslingden Group||||
13635|Myally Subgroup|64367|5|Briefly described|p555  Fig. 1c|Paleoproterozoic|Paleoproterozoic|Topmost rocks of Eastern Creek Volcanics. Age: ca.1775Ma.||||||07-FEB-11
13635|Myally Subgroup|64725|6|Mentioned|p58 Fig.2. |||Mount Isa Inlier.||||||
13635|Myally Subgroup|64744|6|Mentioned|p353 Fig.4. |Statherian|Statherian|Mount Isa Basin.||||Overlies Eastern Creek Volcanics.||
13635|Myally Subgroup|64832|5|Briefly described|p1154, p1155 Figs. 2, 3|Paleoproterozoic|Paleoproterozoic|Of the Haslingden Group. Age: ca.1775Ma. Geological Province: Mt Isa Inlier. Consists of quartz-feldspathic sandstones.||||||07-FEB-11
13635|Myally Subgroup|64834|5|Briefly described|p13 Fig.2, p31-32|||Leichhardt Superbasin. Western Succession of Mount Isa Basin.|||Lochness Formation, Whitworth Formation, Bortalla Formation, Alsace Quartzite|||
13635|Myally Subgroup|65337|6|Mentioned|p5. |||Leichhardt Superbasin; Leichhardt River Fault Trough.||Unit in Haslingden Group.||||
13635|Myally Subgroup|65396|6|Mentioned|p16, p82, p175, p187, p190, p193-194|Statherian|Statherian|See also p196, p241. Leichhardt Superbasin. Cover Sequence 2. Lawn Hill Platform, Leichhardt River Fault Trough. Predominantly continental to shallow restricted marine deposits.|1773 +/- 2 Ma (Neumann et al., 2005).|Haslingden Group||Overlies Eastern Creek Volcanics; overlain by Quilalar Formation.||
13635|Myally Subgroup|65505|6|Mentioned|979, Fig 9|Proterozoic|Proterozoic|||||||
13635|Myally Subgroup|66529|5|Briefly described|p32, p34 |||Leichhardt Superbasin.||||Overlies Eastern Creek Volcanics.|Coarse-to-medium-grained siliciclastics.|
13635|Myally Subgroup|66824|6|Mentioned|p135|||||||||
13635|Myally Subgroup|67026|6|Mentioned|p336 Fig.3. |Proterozoic|Proterozoic|||Unit in Haslingden Group.||||
13635|Myally Subgroup|67323|4|Described|p11-12, p24, p31, p39, p107|Paleoproterozoic|Paleoproterozoic|See also GIS attrib tbl, Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Leichhardt Superbasin. Widespread throughout the Mount Isa Inlier.|Deposition ~1775-1760 Ma.|Haslingden Group.|Includes Alsace Quartzite, Bortala Formation, Lochness Formation, Whitworth Quartzite.|Unconformably overlain by Surprise Creek Formation. Geophysics suggests may be underlain by Eastern Creek Volcanics.|Variably feldspathic and lithic sandstone, siltstone and minor conglomerate.|
13635|Myally Subgroup|67499|5|Briefly described|p938|||Of Derrick (1982), Blake and Stewart (1992). See also Myally Group, Fig. 3.||Of the Haslingden Group.||Underlain by the Eastern Creek Volcanics.||
13635|Myally Subgroup|67539|6|Mentioned|p2|||Includes sandstones. Shown as Myally Sub Group in Fig. 3, p4. Previously considered to unconformably overlie Ewen Granite.||||Intruded by Ewen Granite.||
13635|Myally Subgroup|68020|6|Mentioned|p126||||||Includes Whitworth Quartzite.|||
13635|Myally Subgroup|68021|5|Briefly described|p135 fig 4|Statherian|Statherian|Part of Myally Supersequence, Leichhardt Superbasin, Western Succession.||||Overlies Eastern Creek Volcanics, unconformably overlain by Quilalar Formation. Part equivalent to Marraba Volcanics?||
13635|Myally Subgroup|68542|6|Mentioned|p12|||||||||
13635|Myally Subgroup|68575|6|Mentioned|p1, p37, p78, p112, p124|||A 500m thick sandstone sequence, between Argylla Formation and overlying Ballara Quartzite, may be an equivalent of this unit.||||||
13635|Myally Subgroup|68576|5|Briefly described|Q_2: p12|||Western Succession, Mount Isa region.||||Is overlain by Mary Kathleen Group (equivalents).||
13635|Myally Subgroup|69056|6|Mentioned|p2 |||||||||
13635|Myally Subgroup|69222|5|Briefly described|p221, p222 Fig.2|||Leichhardt River Fault Trough. Post-rift subsidence deposits.|||Includes Pickwick Metabasalt, Alsace Quartzite, Bortala Formation, Whitworth Quartzite|Overlies Eastern Creek Volcanics, overlain by Quilalar Formation||09-FEB-18
13635|Myally Subgroup|69370|6|Mentioned|p307 Fig.2|Statherian|Statherian|Western Fold Belt, Mount Isa Block.||Unit in Haslingden Group.||Is overlain by Quilalar Formation.||25-JAN-19
13635|Myally Subgroup|69542|6|Mentioned|p133 Fig.2|Mesoproterozoic|Paleoproterozoic|Western Fold Belt.||||||
13635|Myally Subgroup|69591|4|Described|p33, p38, p45-46, p49, p57, p88, p105|||Leichhardt Superbasin. Probably absent N of the Murphy Tectonic Ridge. Part of Myally Supersequence. E-W-trending normal faults (from north-south extension) were active during deposition.|~1773 Ma (Neumann et al., 2006).|Haslingden Group.|Alsace, Whitworth Quartzites; Bortala, Lochness Formations.|Overlies Eastern Creek Volcanics. Is overlain unconformably by Gunpowder Creek Formation. Is faulted against Mount Isa Group.|Siliciclastic sediments.|
13635|Myally Subgroup|70282|5|Briefly described|p544 table 1|||Cover sequence 2, Mount Isa.|1790-1760 Ma (or 1720 Ma)|||Overlies Eastern Creek Volcanics.|Clastic sediments and carbonates.|13-FEB-18
13635|Myally Subgroup|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Haslingden Group.|Alsace, Whitworth Quartzites; Bortala, Lochness Formations.|Overlies Eastern Creek Volcanics.||
13635|Myally Subgroup|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Haslingden Group.|Alsace, Whitworth Quartzites; Bortala, Lochness Formations.|Overlies Eastern Creek Volcanics.||
13635|Myally Subgroup|71606|5|Briefly described|p137|Statherian|Statherian|Lawn Hill Platform and Leichardt River Fault Trough, Mount Isa Inlier.||||Overlain by Bigie Formation and Quilalar Formation. Underlain by Eastern Creek Volcanics and Haslingden Group.||
13635|Myally Subgroup|71799|5|Briefly described|p150 fig 2, p153 tbl 1, p153|Statherian|Statherian|Lawn Hill. Source of age not provided. Referred to as the Myally Supersequence on p153 and also Myally Supergroup.|1773 +/- 3 Ma (SHRIMP)||Includes the Alsace Quartzite.|Overlies the Eastern Creek Volcanics. Overlain by the Quilalar Formation.||
13635|Myally Subgroup|71960|6|Mentioned|p77, 86|||Provenance shown to be from west.||Of Haslingden Group.||||
13635|Myally Subgroup|71980|5|Briefly described|map legend sheet 1|Proterozoic|Proterozoic|||Of Haslingden Group|Includes Alsace Quartzite, Bortala Formation, Whitworth Quartzite.|Overlies Eastern Creek Volcanics.||
13635|Myally Subgroup|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. Age given as U-Pb zircon sedimentary depositional age. [material dated not stated]|1773 +/-2 Ma||Whitworth Quartzite, Lochness Formation, Bortala Formation and Alsace Quartzite|Overlies Eastern Creek and shown as partially underlying Quilarlar Formation and Don Creek Sandstone.||
13635|Myally Subgroup|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Leichhardt River Domain.||Haslingden Group||Overlies Eastern Creek Volcanics.|Variably feldspathic and lithic sandstone, siltstone and minor conglomerate.|
13635|Myally Subgroup|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Leichhardt River Domain.||Haslingden Group||Overlies Eastern Creek Volcanics.|Variably feldspathic and lithic sandstone, siltstone and minor conglomerate.|
13635|Myally Subgroup|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. U-Pb zircon sedimentary depositional age given [but no indication of what unit dated, or where the sample sits stratigraphically].|1773 +/- 2 Ma||Whitworth Quartzite, Lochness Formation, Bortala Formation and Alsace Quartzite.|Shown as underlying Carrara Range Group.||
13635|Myally Subgroup|72919|5|Briefly described|p56, p63-64|||Mount Isa Province. Previously Myally beds.||Myally Supersequence|Alsace Quartzite, Bortala Formation, Whitworth Quartzite, Lochness Formation|||
13635|Myally Subgroup|73042|6|Mentioned|p4|Statherian|Statherian|Mount Isa Province, Leichhardt Superbasin. Geochronology is a U-Pb zircon sedimentary depositional age (?maximum depositional age).|1773 +/- 2 Ma (see Fig.1.2)||Whitworth Quartzite, Lochness Formation, Bortala Formation, Alsace Quartzite.|Underlain by Eastern Creek Volcanics. Partly overlain(?) by Quilalar Formation.||
13635|Myally Subgroup|73525|5|Briefly described|p4-5 Fig.2, p19 Fig.13, p20|Statherian|Statherian|Mount Oxide-(Ardmore-May Downs) and Leichhardt River Domains.|1768+/-8 Ma, 1773+/-2 Ma maximum depositional ages||||Clastics.|
13641|Myaoola Granite|24048|6|Mentioned|p13|||||||||
13641|Myaoola Granite|32659|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13641|Myaoola Granite|32660|5|Briefly described|Table 2|||||||||
13641|Myaoola Granite|36473|6|Mentioned|Map legend|Proterozoic|Archean|Archaean to Proterozoic||||||07-NOV-08
13641|Myaoola Granite|41406|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
13641|Myaoola Granite|42597|5|Briefly described|Map Legend|Archean||||||||07-NOV-08
13641|Myaoola Granite|43010|2|Defined|p40||Paleoproterozoic|Of Orosirian age.||||||07-NOV-08
13641|Myaoola Granite|44299|5|Briefly described|p.8||Archean|SD/53-7,8. Archaean. Table 1.||||||07-NOV-08
13641|Myaoola Granite|44300|14|Not recorded|map legend||Archean|SD/53-7,8. Archaean.||||||07-NOV-08
13660|Myrtle Shale|22538|6|Mentioned|Fig3 P709|||||||||
13660|Myrtle Shale|22662|5|Briefly described|30|Proterozoic|Proterozoic|Geological province: McArthur Basin.||||||13-NOV-06
13660|Myrtle Shale|22664|5|Briefly described|Fig. 2 p34|||Of the Umbolooga Subgroup (McArthur Group).||||||13-NOV-06
13660|Myrtle Shale|22853|4|Described|19|Proterozoic|Proterozoic|Of the Umbolooga Subgroup. Overain by Emmerugga Dolomite; underlain by Leila Sandstone and Tooganinie Formation.||||||13-NOV-06
13660|Myrtle Shale|23387|6|Mentioned|p18 fig.19|||Of Umbolooga Subgroup.||||||
13660|Myrtle Shale|23396|5|Briefly described|p407 Fig.2|||Of the McArthur Group.||||||13-NOV-06
13660|Myrtle Shale|23397|5|Briefly described|p473|||||||||
13660|Myrtle Shale|23409|5|Briefly described|p533|||Of the McArthur Group.||||||13-NOV-06
13660|Myrtle Shale|23776|5|Briefly described|p705 Fig 2.|||Of Umbolooga Subgroup||||||
13660|Myrtle Shale|23902|4|Described|p1568 Fig.2|||Of the Umbolooga Subgroup. Overlain by the Emmerugga Dolomite. Overlies the Leila Sandstone and the Tooganinie Formation. Geological Province: McArthur Basin.||||||05-OCT-07
13660|Myrtle Shale|23910|5|Briefly described|p292 Fig. 3|||Of Umbolooga Subgroup.  Geological Province: McArthur Basin.||||||
13660|Myrtle Shale|23963|5|Briefly described|p1239 Fig.2|||Geological Province: McArthur Basin. Of the Umbolooga Subgroup.||||||
13660|Myrtle Shale|24432|6|Mentioned|p570 Fig.10|Statherian|Statherian|||||||28-JAN-05
13660|Myrtle Shale|30272|6|Mentioned|p5|||Stratigraphic table||||||
13660|Myrtle Shale|35162|6|Mentioned|Table.1|||||||||
13660|Myrtle Shale|36796|6|Mentioned|Fig.3|||||||||
13660|Myrtle Shale|38582|6|Mentioned|p219|||||||||
13660|Myrtle Shale|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
13660|Myrtle Shale|40691|4|Described|p38|||||||||
13660|Myrtle Shale|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
13660|Myrtle Shale|41268|5|Briefly described|Fig.3|||||||||
13660|Myrtle Shale|42385|4|Described|p19|||See also Table 4 p17.||||||
13660|Myrtle Shale|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
13660|Myrtle Shale|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.||Of Umbolooga Subgroup (McArthur Group).||In schematic section, underlies Mara Dolomite Member (Emmerugga Dolomite); overlies Leila Sandstone.|Dolomitic siltstone, shale, dolulitite, sandstone, halite casts. Detailed lithology given.|11-NOV-11
13660|Myrtle Shale|42639|4|Described|p25, Table 5 p21|||||||||
13660|Myrtle Shale|42812|6|Mentioned|p36|||Of the Tooganinie Formation?||||||13-NOV-06
13660|Myrtle Shale|42935|6|Mentioned|p529 Fig.2|||Of the Umbolooga Subgroup.||||||13-NOV-06
13660|Myrtle Shale|43010|5|Briefly described|Fig.6||Mesoproterozoic|of "Mid Proterozoic" age.||||||
13660|Myrtle Shale|43036|5|Briefly described|p48|||||||||
13660|Myrtle Shale|43486|5|Briefly described|21|||||||||
13660|Myrtle Shale|45162|2|Defined|p83|Proterozoic|Proterozoic|||||||
13660|Myrtle Shale|60483|5|Briefly described|p7 Fig. 5, p30|||Of Umbolooga Subgroup (McArthur Group). Geological Province: McArthur Basin.||||||05-OCT-07
13660|Myrtle Shale|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Umbolooga Subgroup. Overlian by Emmerugga Dolomite, underlian by Leila Sandstone.||||||
13660|Myrtle Shale|62084|5|Briefly described|p936 Fig.5|||Isa Superbasin. McArthur Basin.||McArthur Group|||Hematitic siltstones.|
13660|Myrtle Shale|63112|6|Mentioned|p1191 Fig.2|||Isa Superbasin; southern McArthur Basin. Age approximated from Fig.2.|c.1640 Ma.|Unit in River Supersequence.||||
13660|Myrtle Shale|64815|6|Mentioned|p4 Fig.2, p5 Fig.3, p8 Tb.1, p14 Tb.5|||||Of the Umbolooga Subgroup.||||
13660|Myrtle Shale|64817|6|Mentioned|p353 Fig.4 |||||Of the Umbolooga Subgroup.||Shown as partial lateral equivalent of Tooganinie Formation, and overlying Leila Sandstone.||14-JUN-18
13660|Myrtle Shale|65228|4|Described|p30, Table 1, Figs.02, 04, 11-12, 18-19.|||In upper part of Loretta Supersequence (cf. Southgate et al 2000 who regarded it as basal River Supersequence). Gamma ray log, lithology and facies detailed. Measured section.||Unit in Umbolooga Subgroup.||Overlies Leila Sandstone. Is overlain by Emmerugga Dolomite.|Red beds with evaporitic stromatolitic cycles.|
13660|Myrtle Shale|67144|5|Briefly described|Map legend.|Statherian|Statherian|Recessive.||Unit in Umbolooga Subgroup.||Overlies Leila Sandstone. Is overlain by Emmerugga Dolostone.|Thinly-bedded to laminated, commonly dolomitic siltstone, shale, dololutite (in places stromatolitic) and fine-grained sandstone; halite casts common.|
13660|Myrtle Shale|67352|4|Described|p14 Tb.2|Statherian|Statherian|McArthur Basin. 60 m thick.||Umbolooga Subgroup||Overlies Leila Sandstone and Tooganinie Formation (conformably).  Overlain by Mara Dolostone Member (conformably).|Siltstone, shale and fine-grained sandstone: thinly bedded to laminated, commonly dolomitic; dolomudstone.|
13660|Myrtle Shale|69430|4|Described|p15:3, 17, 34|Statherian|Statherian|Jackson et al. (1987); previously Myrtle Shale Member of Tooganinie Formation (Plumb and Brown, 1973). Southern McArthur Basin. 40-60m thick. Lagoonal and/or low-gradient alluvial plain sediments.||Umbolooga Subgroup.||Conformably and gradationally overlies Leila Sandstone. Is overlain conformably and gradationally by Mara Dolostone Member (Emmerugga Dolostone).|Thinly bedded to laminated, commonly dolomitic siltstone, shale and fine-grained sandstone (halite casts common); dololutite (in places stromatolitic).|12-JUL-16
13660|Myrtle Shale|69673|6|Mentioned|p16 fig 13|||Batten Fault Zone||Tooganinie Formation||Overlies Leila Sandstone||
13660|Myrtle Shale|72248|6|Mentioned|p147|||Of McArthur Basin.||Unit of Umbolooga Subgroup.||||
13660|Myrtle Shale|72373|5|Briefly described|p11|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin.||Unit of Umbolooga Subgroup.||Underlain by Leila Sandstone.||
13660|Myrtle Shale|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the southern part of the Batten Fault Zone.||Umbolooga Subgroup.||Overlies Leila Sandstone and underlies Mara Dolostone Member, Emmerugga Dolostone.||
13660|Myrtle Shale|72718|6|Mentioned|p7|||Southern McArthur Basin. Batten Fault Zone (south).||Umbolooga Sub-group, McArthur Group||Underlain by Leila Sandstone. Overlain by Myrtle Shale. Equivalent to Tooganinie Formation.||
13660|Myrtle Shale|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the South part of the Batten Fault Zone of the Southern McArthur Basin.||Umbolooga Subgroup||Overlies Leila Sandstone and underlies Mara  Dolostone Member and is partly equivalent to Tooganinie Formation.||
13660|Myrtle Shale|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin, Isa Superbasin.||Umbolooga Subgroup, McArthur Group||Underlain by Leila Sandstone. Overlain by Mara Dolostone Member. May be equivalent to Tooganinie Formation.||
13660|Myrtle Shale|73412|5|Briefly described|p4, 8|||Southern McArthur Basin.||Umbolooga Subgroup.||Overlies Leila Sandstone. Is overlain by Emmerugga and Teena Dolostones.||
13665|N'Dahla Member|9199|5|Briefly described|Map legend|Ordovician|Cambrian|Of the Pacoota Sandstone (Larapinta Group).   Purplish-brown sandstone and siltstone.  Geological Province: Amadeus Basin.||||||
13665|N'Dahla Member|22760|5|Briefly described|p340|||Of the Parke Siltstone.  Contains a sparse fish fauna known from the Cleland Hills, Dare Plain and Ross River.||||||20-NOV-06
13665|N'Dahla Member|22762|6|Mentioned|p364|||||||||
13665|N'Dahla Member|22804|5|Briefly described|p454||Devonian|Of the Parke Siltstone.  Age - Tentatively placed near the Early - Middle Devonian boundary (ie. Emsian-Eifelian) based on fish fauna.||||||20-NOV-06
13665|N'Dahla Member|31572|6|Mentioned|Fig.|||Correlation chart. L.Ord.||||||
13665|N'Dahla Member|34579|4|Described|Table 2|||Cambrian - Ordovician||||||
13665|N'Dahla Member|38606|6|Mentioned|Map legend|Early Ordovician|Late Cambrian|Late Cambrian to Early Ordovician||||||
13665|N'Dahla Member|38885|6|Mentioned|Map legend|Early Ordovician|Late Cambrian|Late Cambrian - Early Ordovician||||||
13665|N'Dahla Member|39583|6|Mentioned|Map legend|Early Ordovician|Late Cambrian|Late Cambrian to Early Ordovician||||||
13665|N'Dahla Member|40136|5|Briefly described|p33|||||||||
13665|N'Dahla Member|40740|4|Described|p76|||||||||
13665|N'Dahla Member|40810|6|Mentioned|p8|||||||||
13665|N'Dahla Member|41018|4|Described|Fig.3|||||||||
13665|N'Dahla Member|42354|5|Briefly described|p4, p7|Devonian||Member of Parke Siltstone (Pertnjarra Group) since 1987. Formerly part of Pacoota Sandstone.||||||20-NOV-06
13665|N'Dahla Member|43649|6|Mentioned|p459|||||||||
13665|N'Dahla Member|45041|4|Described|p67|||U.Camb. Mb. Pacoota Sst||||||
13665|N'Dahla Member|48890|2|Defined|p.45||Cambrian|Tb.2, Fig.4, pt. Pacoota Sandstone. Defn. on Tech.File F/53-15.||||||
13665|N'Dahla Member|50246|5|Briefly described|p20 Fig. 2|Carboniferous|Devonian|Of the Pertnjara Group. Silty sandstone, fossiliferous, glauconitic and brown.||||||07-FEB-11
13665|N'Dahla Member|60547|5|Briefly described|Map Legend|Ordovician|Cambrian|Of the Pacoota Sandstone. Purplish-brown sandstone and siltstone. Geological Province: Amadeus Basin.||||||03-JUN-05
13665|N'Dahla Member|62595|5|Briefly described|p29 Fig.6.|Carboniferous|Devonian|Ross River area.||Unit in Pertnjara Group.|||Silty sandstone, fossiliferous, glauconitic and brown.|
13665|N'Dahla Member|63562|6|Mentioned|p346 fig 8|||||Pertnjara Group||||
13665|N'Dahla Member|69438|4|Described|p23:8, 38|Devonian|Devonian|Young et al. (1987), who recognised Devonian fish scales and bones, and placed this unit in the Pertnjara Group. Only known from the Ross River Syncline, Amadeus Basin. Originally mapped (Wells et al., 1967) as Pacoota Sandstone. Appears as N'dahla Member on 23:8.||Parke Siltstone.||Unconformably overlies the Pacoota Sandstone. Probable equivalent of Deering Siltstone Member.|Dark red-brown, medium- to coarse-grained, poorly sorted sandstone and pebbly sandstone, glauconitic in places. Occasional conglomerate intervals and thin layers of limestone occur.|12-JUL-16
13665|N'Dahla Member|69673|6|Mentioned|p67|||||Parke Siltstone||||
13671|Nabarlek Granite|9534|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Altered pink biotite granite.||||||07-NOV-08
13671|Nabarlek Granite|9691|5|Briefly described|Map Legend|||Altered pink biotite granite, anomalously radioactive, commonly with north trending quartz filled shears: anatectic granite.||||||
13671|Nabarlek 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
13671|Nabarlek Granite|9733|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Altered pink biotite granite, anomalously radioactive; commonly with north trending quartz filled shears; anatectic granites.||||||
13671|Nabarlek 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
13671|Nabarlek Granite|31833|6|Mentioned|Table 2|||||||||
13671|Nabarlek Granite|36085|6|Mentioned|p502|||Name intended as informal.||||||20-NOV-06
13671|Nabarlek Granite|36535|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13671|Nabarlek Granite|36635|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13671|Nabarlek Granite|37815|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13671|Nabarlek Granite|38884|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
13671|Nabarlek Granite|39048|6|Mentioned|p824|||||||||
13671|Nabarlek Granite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13671|Nabarlek Granite|40489|6|Mentioned|p88|||||||||
13671|Nabarlek Granite|41406|6|Mentioned|Map legend|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
13671|Nabarlek Granite|41649|5|Briefly described|p75|||||||||
13671|Nabarlek Granite|46639|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Age: 1780+/-13Ma. Altered pink biotite granite, anomalously radioactive.||||||07-NOV-08
13671|Nabarlek Granite|46700|5|Briefly described|P28, Table1 P10||Statherian|Age of unit is 1780 Ma.||||||20-NOV-06
13671|Nabarlek Granite|46824|6|Mentioned|Table 1|||See also p322.||||||20-NOV-06
13671|Nabarlek Granite|50545|5|Briefly described|p113||Paleoproterozoic|Intrudes Myra Falls Metamorphics. Of Jim Jim Suite.||||||07-NOV-08
13671|Nabarlek 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
13671|Nabarlek Granite|60550|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Altered pink biotite granite, anomalously radioactive, commonly with north trending quartz filled shears: anatectic granites.||||||08-JUN-05
13671|Nabarlek Granite|61206|5|Briefly described|p516, p517 Fig.1|Early Proterozoic|Early Proterozoic|||||Intrudes Myra Falls Metamorphics.|K-U-Th-rich granites.|
13671|Nabarlek Granite|63866|5|Briefly described|p112|Orosirian|Orosirian|Nimbuwah Domain, Pine Creek Orogen. Numeric age is interpreted as the age of igneous crystallisation.|1818 +/- 7 Ma (Worden et al, 2006b)|David Suite||||
13671|Nabarlek Granite|64677|5|Briefly described|p1, p6-7, p40|||Pine Creek Orogen.|1818 +/- 8 Ma.|Jim Jim Suite.||Intrudes Myra Falls Metamorphics. Is overlain nonconformably by Katherine River Group.|Medium-grained granite.|
13671|Nabarlek Granite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1820-1850Ma.  I-type. Altered pink biotite granite.||||||07-JAN-09
13671|Nabarlek Granite|65232|5|Briefly described|p24, 42|||Post-orogenic granitoids, including Jim Jim Granite, Tin Camp Creek Granite and Nabarlek Granite, intruded during period 1840 - 1820 Ma (OZCHRON).||||||09-FEB-10
13671|Nabarlek Granite|66683|6|Mentioned|p368 Fig.3, p369.||||1818 +/- 8 Ma.|||Is unconformably overlain by Kombolgie Subgroup.||
13671|Nabarlek Granite|67057|5|Briefly described|p454. |Paleoproterozoic|Paleoproterozoic|Post-orogenic intrusion.|1818 +/- 7 Ma (Worden 2006).|||||
13671|Nabarlek Granite|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Pine Creek area.|1818 +/- 8 Ma.|||||
13671|Nabarlek Granite|67564|5|Briefly described|p85.|Paleoproterozoic|Paleoproterozoic|Eastern Pine Creek Orogen.|1818 +/- 7 Ma (SHRIMP U - Pb zircon).|Unit in David Suite.||||
13671|Nabarlek Granite|67779|3|Fully described|p6 Fig.5, p8 Table 1, pp30-31, p64, p86.|Paleoproterozoic|Paleoproterozoic|Nimbuwah Domain, Pine Creek Orogen. Small, low-lying outcrops. Their ages suggest that this unit, the Cullen Supersuite granites and the Edith River Group formed as part of the same thermal event. Anomalously high U and Th radiometric responses. Geochemistry is described in detail.|1818 +/- 8 Ma (Worden et al. 2006b).|Unit in Jim Jim Suite.||Intrudes Nimbuwah Complex. Is overlain unconformably by Mamadawerre Sandstone.|Altered medium- to coarse-grained, pink to green biotite granite; accessory zircon, allanite and fluorite; commonly with north-trending quartz-filled shears; anatectic granite.|
13671|Nabarlek Granite|69420|4|Described|p5:18, 21, 23, 25, 69-70|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Mineralogy and petrology/geochemistry summarised. Very high U content. Intersected 450m below the Nabarlek orebody. Late-orogenic. Geochronology by Worden et al. (2006).|1818 +/- 8 Ma; SHRIMP U-Pb zircon.|Jim Jim Suite.||Intrudes Cahill Formation.|Pink, coarse-grained granite consisting mainly of plagioclase, quartz, orthoclase, biotite, rare opaques. Extensively altered, and significantly more radioactive than typical granitoids.|12-JUL-16
13671|Nabarlek Granite|69577|6|Mentioned|p117 Fig.6|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||||||
13671|Nabarlek Granite|70853|5|Briefly described|Map legend.|Orosirian|Orosirian||1818 Ma.||||Altered pale pink biotite granite: anomalously radioactive, commonly with north-trending quartz-filled shears; anatectic granite.|
13671|Nabarlek Granite|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|1818+/-7 Ma (crystallisation: U-Pb zircon SHRIMP)||||Medium-grained granite.|
13676|Naburula Formation|23270|5|Briefly described|Table 1, p4||Proterozoic|In the Ngalia Basin. Age: Late Proterozoic.||||||20-NOV-06
13676|Naburula Formation|23271|5|Briefly described|Map legend||Proterozoic|In the Ngalia Basin. Age: Late Proterozoic.||||||03-MAY-10
13676|Naburula Formation|24111|5|Briefly described|p215 Fig. 11|Neoproterozoic|Neoproterozoic|Appears as Naburula only in text of figure.  Geological Province: Ngalia Basin.  See also Nabarula Formation (p216).||||||
13676|Naburula Formation|36898|6|Mentioned|p181|||||||||
13676|Naburula Formation|37462|4|Described|Table 4.IX|||||||||
13676|Naburula Formation|37537|5|Briefly described|Map legend|Adelaidean|Adelaidean|Shale; dark grey to black, minor siltstone; diamictite, polmictic, subrounded, faceted and striated erratics; green-brown matrix, poorly sorted siltstone; green-grey and dark brown, fine, thin-bedded dolomite. Geological Province: Ngalia Basin.||||||
13676|Naburula Formation|37928|3|Fully described|p518|||See also p515.||||||20-NOV-06
13676|Naburula Formation|38157|6|Mentioned|Table VII|||||||||
13676|Naburula Formation|39565|6|Mentioned|p33|||See also p38.||||||20-NOV-06
13676|Naburula Formation|40906|6|Mentioned|Fig.9|||||||||
13676|Naburula Formation|41405|6|Mentioned|p205|||||||||
13676|Naburula Formation|41717|6|Mentioned|Fig.19|||||||||
13676|Naburula Formation|42059|5|Briefly described|Fig.2|||See also p133.||||||20-NOV-06
13676|Naburula Formation|42504|5|Briefly described|Table 4 P73|||||||||
13676|Naburula Formation|42643|6|Mentioned|Fig.4 P19|||||||||
13676|Naburula Formation|43595|5|Briefly described|p548,Fig.5-33,549||Adelaidean|||||||
13676|Naburula Formation|44158|4|Described|p27 Table.2|Neoproterozoic|Neoproterozoic|In the Ngalia Basin.||||||20-NOV-06
13676|Naburula Formation|45155|2|Defined|p22|Adelaidean|Adelaidean|||||||
13676|Naburula Formation|46865|2|Defined|p53|late Adelaidean|late Adelaidean|||||||
13676|Naburula Formation|46903|6|Mentioned|Fig.5|||Correlation chart||||||
13676|Naburula Formation|61385|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Dark grey shale, minor siltstone and dololutite, basal tillite. Geological Province: Ngalia Basin.||||||
13676|Naburula Formation|64068|6|Mentioned|p45, 223|||Ngalia Basin. Correlated with Yardida Tillite, southern Georgina Basin.||||||
13676|Naburula Formation|64103|6|Mentioned|p404|||Geological Province: Ngalia Basin.||||||07-FEB-11
13676|Naburula Formation|65232|5|Briefly described|p70|||With Rinkabeena Shale, both overlie both Albinia Formation and Mount Vaughan Quartzite [misspelling of Vaughan Springs Quartzite]. Diamictite. Geol. Prov: Ngalia Basin.||||||09-FEB-10
13676|Naburula Formation|65338|5|Briefly described|p59.|||||||Probably unconformably overlies Vaughan Springs Quartzite.|Diamictite.|
13676|Naburula Formation|68270|4|Described|p680,682-683,685,687-688|Cryogenian|Cryogenian|Ngalia Basin. Type section occurs in Eastern Naburula Hills, lat. 22'17'30"S, long. 131'19'30"E.  [Misspelt as Nabarula on p683 Fig 67.2]. Less than 8m thick. Subglacial, shallow-marine ice proximal deposit. Related to Sturt glaciation. Correlative to Sturt Tillite.||||Overlain by Rinkabeena Shale. Underlain unconformably by basement, Patmungula beds, Vaughan Springs Quartzite.|Basal diamictite (2-3m; poorly sorted mudstone matrix), overlain by interbedded shale-siltstone and a overlying cap dolomite.|03-JUL-19
13676|Naburula Formation|68277|6|Mentioned|p95|Neoproterozoic|Neoproterozoic|The rank is not given in the text.||||||
13676|Naburula Formation|69437|5|Briefly described|p22:4-5, 7|Cryogenian|Cryogenian|Ngalia Basin, Centralian A Superbasin. Supersequence 2.||||Is overlain by Rinkabeena Shale.|Basal diamictite succeeded by shale and dolomudstone at the top of the Formation.|12-JUL-16
13676|Naburula Formation|69439|3|Fully described|p24:2-4, 7-8, 13-14, 18, 20-21|Cryogenian|Cryogenian|Wells in Preiss et al. (1978). Previously (Wells et al., 1968) regarded this as part of Mount Doreen Formation. Ngalia Basin, Centralian A Superbasin. Supersequence 2. Naburula Hills area (the type area) and Vaughan Springs Syncline. 8m thick in the type area. Correlated with Areyonga Formation, Sturt Tillite, Mount Cornish Formation and lower Yardida Tillite. An 8m-thick black shale interval has excellent hydrocarbon source rock potential.||||Unconformably overlies Vaughan Springs Quartzite and ?Albinia Formation, and Patmungala beds (basement). Is overlain (probably unconformably) by Mount Doreen Formation.|Dark grey to black mudstone, shale and minor siltstone, interbeds of green-grey and brown dolostone, and a basal green diamictite with erratics up to 1m across. A marker bed at the top has weathered, green-grey, laminated dolomudstone.|12-JUL-16
13676|Naburula Formation|69443|6|Mentioned|p28:8|||Ngalia Basin.||||Equivalent to the Aroota Group.||12-JUL-16
13676|Naburula Formation|69673|5|Briefly described|p106, p107 fig 85|Neoproterozoic|Neoproterozoic|Thin unit, up to 8m thick. Source rock potential.||||Overlies Albinia Formation, overlain by Rinkabeena Shale|Mudstone, shale and minor siltstone and dolomudstone, interbeds of dolostone and basal diamictite.|
13676|Naburula Formation|72516|6|Mentioned|p86|Cryogenian|Cryogenian|Ngalia Basin.||||Equivalent to the Mount Cornish Formation.||02-JUN-21
13676|Naburula Formation|72601|6|Mentioned|p5|||Ngalia Basin.||||||
13676|Naburula Formation|73086|6|Mentioned|p158|||[Variation of published name; probably a misspelling of Nabarula Formation]. Ngalia Basin.||||Correlates to Areyonga Formation[?].||
13724|Namoona Group|9324|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Shale, sandstone, arkose, conglomerate, dolomite.||||||07-NOV-08
13724|Namoona Group|9534|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes the Masson Formation.||||||07-NOV-08
13724|Namoona Group|9538|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Calcareous and carbonaceous shale, sandstone, limestone, dolomite, magnesite, arkose, conglomerate; schist and marble in the east.  Unconformably overlain by the Mount Partridge Group; unconformably overlies the Rum Jungle and Waterhouse Complexes.||||||07-NOV-08
13724|Namoona Group|9579|5|Briefly described|Map Sheet|Paleoproterozoic|Paleoproterozoic|Early Proterozoic age.||||||
13724|Namoona Group|9691|5|Briefly described|Map Legend|||||||||
13724|Namoona Group|9701|5|Briefly described|Map Legend|Proterozoic|Proterozoic|||||||10-JUN-05
13724|Namoona Group|22479|5|Briefly described|fig1p2|||||||||
13724|Namoona Group|22809|6|Mentioned|Map|Proterozoic|Proterozoic|||||||
13724|Namoona Group|22810|5|Briefly described|Table2 P5, P11|||Maximum thickness: 3500m.||||||20-NOV-06
13724|Namoona Group|22813|5|Briefly described|Map|Paleoproterozoic|Paleoproterozoic|Shale, sandstone, arkose, conglomerate, dolomite.||||||07-NOV-08
13724|Namoona Group|23216|6|Mentioned|Fig3p5||Paleoproterozoic|||||||07-NOV-08
13724|Namoona Group|23714|4|Described|p9|Proterozoic|Proterozoic|See also page 11. Overlain by Mount Partridge Group; underlain by Rum Jungle complex. Geological Province: Rum Jungle Region.||||||20-NOV-06
13724|Namoona Group|23715|5|Briefly described|Map legend||Proterozoic|In the Rum Jungle and Central Regions||||||
13724|Namoona Group|23733|5|Briefly described|p32 Fig. 19|||||||||
13724|Namoona Group|24047|5|Briefly described|p5 Fig.4|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Orogen.  See also p6 Fig. 5, p30 Fig. 23.||||||07-NOV-08
13724|Namoona Group|24181|5|Briefly described|p87 Fig.2|Paleoproterozoic|Paleoproterozoic|Unconformably overlies Archaean basement. Unconformably overlain by Mount Partridge Group. Geological Province: Pine Creek Inlier.||||||07-NOV-08
13724|Namoona Group|35140|6|Mentioned|Fig.2|||||||||
13724|Namoona Group|36535|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13724|Namoona Group|36635|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13724|Namoona Group|37462|4|Described|Table 4.II|||||||||
13724|Namoona Group|37579|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes the Masson Formation and Stag Creek Volcanics.||||||07-NOV-08
13724|Namoona Group|38239|6|Mentioned|p9|||See also Fig.2.||||||
13724|Namoona Group|38884|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13724|Namoona Group|39069|5|Briefly described|Table 1|||See also Fig.4.||||||
13724|Namoona Group|39357|4|Described|p3|||||||||
13724|Namoona Group|39518|6|Mentioned|p3|||||||||
13724|Namoona Group|39563|6|Mentioned|Map legend|Paleoproterozoic|Archean|Early Proterozoic to Archaean||||||07-NOV-08
13724|Namoona Group|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13724|Namoona Group|39801|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Calcareous and carbonaceous shale, sandstone, limestone, dolomite, magnesite, arkose, conglomerate; schist and marble in east.||||||07-NOV-08
13724|Namoona Group|40104|6|Mentioned|p349|||||||||
13724|Namoona Group|40168|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Calcareous and carbonaceous shale, sandstone, limestone, dolomite, magnesite, arkose, conglomerate; schist and marble in east.||||||07-NOV-08
13724|Namoona Group|40223|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Calcareous and carbonaceous shale, sandstone, limestone, dolomite, magnesite, arkose, conglomerate; schist and marble in east.||||||07-NOV-08
13724|Namoona Group|40243|6|Mentioned|Fig.2|||||||||
13724|Namoona Group|40492|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
13724|Namoona Group|40493|6|Mentioned|p21|||||||||
13724|Namoona Group|40765|6|Mentioned|Fig.3|||||||||
13724|Namoona Group|40808|6|Mentioned|p3|||||||||
13724|Namoona Group|40809|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13724|Namoona Group|40823|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13724|Namoona Group|40852|6|Mentioned|p25|||||||||
13724|Namoona Group|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13724|Namoona Group|40973|6|Mentioned|p195|||||||||
13724|Namoona Group|41125|6|Mentioned|Fig.14|||See also Fig.6||||||
13724|Namoona Group|41304|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
13724|Namoona Group|41305|2|Defined|p5|Paleoproterozoic||||||||07-NOV-08
13724|Namoona Group|41309|4|Described|p3|||||||||
13724|Namoona Group|41311|4|Described|p5|||||||||
13724|Namoona Group|41397|4|Described|p6|||||||||
13724|Namoona Group|41406|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
13724|Namoona Group|41407|6|Mentioned|Map legend|Proterozoic||||||||
13724|Namoona Group|41465|6|Mentioned|p5|||||||||
13724|Namoona Group|41586|6|Mentioned|Map legend|||||||||
13724|Namoona Group|41663|6|Mentioned|p8|||||||||
13724|Namoona Group|42012|6|Mentioned|p33|||||||||
13724|Namoona Group|42014|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
13724|Namoona Group|42927|5|Briefly described|p428|||see also Fig.1 p429.||||||20-NOV-06
13724|Namoona Group|43140|5|Briefly described|p2||Paleoproterozoic|||||||07-NOV-08
13724|Namoona Group|43561|6|Mentioned|p1434|||||||||
13724|Namoona Group|43595|5|Briefly described|p351|||||||||
13724|Namoona Group|43624|6|Mentioned|Table 1,p9||Paleoproterozoic|||||||07-NOV-08
13724|Namoona Group|43720|5|Briefly described|p4||Paleoproterozoic|||||||07-NOV-08
13724|Namoona Group|43832|3|Fully described|11-14||Paleoproterozoic|Maximum age: 2000 Ma. Within Pine Creek Geosyncline.  Overlain by Mount Partridge Group.||||||04-DEC-08
13724|Namoona Group|46658|5|Briefly described|p548|||||||||
13724|Namoona Group|46675|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes the Celia Dolomite and Beestons Formation. Unconformably overlain by the Mount Partridge Group.  Overlies unconformably the Rum Jungle and Waterhouse Complexes.||||||12-APR-12
13724|Namoona Group|46700|5|Briefly described|p14, Table1 p12||Proterozoic|||||||12-JUL-16
13724|Namoona Group|47049|6|Mentioned|Fig.2|||||||||
13724|Namoona Group|60526|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Calcareous and carbonaceous shale, sandstone, limestone, dolomite, arkose, conglomerate; schist and marble in east.||||||
13724|Namoona Group|60550|5|Briefly described|Map Legend|Proterozoic|Proterozoic|||||||
13724|Namoona Group|60575|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes the Celia Dolomite and the Beestons Formation.||||||07-NOV-08
13724|Namoona Group|60680|5|Briefly described|Map legend|Orosirian|Orosirian|Includes: Stag Creek Volcanics and Masson Formation.  Geological Province: Pine Creek Orogen.||||||
13724|Namoona Group|61827|5|Briefly described|p158 Fig. 4|||||||||
13724|Namoona Group|61861|6|Mentioned|Fig.2.|||Pine Creek.||||||
13724|Namoona Group|62375|5|Briefly described|p8 Table 1, 9 table 2, 10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Pyritic carbonaceous shale and siltstone, calcareous in places, calcareous sandstone, tuff, agglomerate. Thickness: 3000m. Geological Province: Pine Creek Orogen.||||||09-FEB-10
13724|Namoona Group|63866|5|Briefly described|p108|||Central Domain, Pine Creek Orogen.||||Overlain by the Stag Creek Volcanics. Equivalent to the Manton Group.||
13724|Namoona Group|64698|5|Briefly described|lithinterp table|Orosirian|Neoarchean|Age ~1865-2600Ma. Includes Cahill Formation (~1865-2500Ma), Masson Formation, Stag Creek Volcanics.||||||07-JAN-09
13724|Namoona Group|64722|5|Briefly described|Fig. 2 p3-6, p9, 24|Orosirian|Orosirian|Part of an older component (2030-2020 Ma) of Central Domain of Pine Creek Orogen.||||||11-APR-12
13724|Namoona Group|64730|5|Briefly described|p124, 125 Fig. 3, p138|Paleoproterozoic|Paleoproterozoic|includes Stag Creek Volcanics at top which has maximum deposition age of 2021 +/- 10 Ma.|||Includes Masson Formation and Stag Creek Volcanics.|Unconformably underlies Mundogie Sandstone of Mount Partridge Group.||02-MAY-12
13724|Namoona Group|64731|5|Briefly described|p147|Proterozoic|Proterozoic|Central Domain, Pine Creek Orogen.||||||
13724|Namoona Group|64956|5|Briefly described|p69, p72|||Contains the Masson Formation. Unconformably overlain by Mount Partridge Group.||||||07-FEB-11
13724|Namoona Group|65232|5|Briefly described|p45, p7, p6 Fig. 5, p5 Fig. 4|Palaeoproterozoic|Palaeoproterozoic|Includes Masson Formation (at base) and Stag Creek Volcanics. Unconformable lower contact with Archaean basement complexes. Intruded by Zamu Dolerite. Geol. Prov: Pine Creek Orogen.||||||09-FEB-10
13724|Namoona Group|65339|6|Mentioned|p7. |||Eastern equivalent of Manton Group.||||||
13724|Namoona Group|67355|6|Mentioned|p6, p7 Tb.2, p10, p15, p46 Fig.37||Paleoproterozoic|Synrift sedimentation. Possible influence of synrift faults.||Woodcutters Supergroup||Correlative to Manton Group. Underlies the Crater Formation, indicated as unconformable.||25-JAN-17
13724|Namoona Group|67564|5|Briefly described|p iv, p8 Table 2, p9 Fig.4, p11. |Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Correlative of Celia Dolostone and Cahill Formation. Deformed and metamorphosed to greenschist facies during the 1860 - 1850 Ma Nimbuwah Event.|||Includes Cahill and Masson Formations and Stag Creek Volcanics.|Overlies Kakadu Group. Is overlain unconformably by Mount Partridge Group, Nourlangie Schist and Katherine River Group.||
13724|Namoona Group|67779|5|Briefly described|p5 Fig.4(b), p6 Fig.5, p19.|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen.|c.2020 Ma.|Unit in Woodcutters Supergroup.|Includes Masson Formation and Stag Creek Volcanics.|||
13724|Namoona Group|69420|5|Briefly described|p5:2,4,6, 8-10, 15-16, 24, 31, 67,79,93|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen. Deformation mentioned.||Woodcutters Supergroup.|Masson Formation, Stag Creek Volcanics.|Is overlain unconformably by the Mount Partridge Group.||12-JUL-16
13724|Namoona Group|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||Probably part of Woodcutters Supergroup.|Includes Masson Formation.|Unconformably overlies Rum Jungle Complex. Is overlain unconformably by Mount Partridge Group.||01-MAR-18
13724|Namoona Group|72527|6|Mentioned|p192.|Orosirian|Orosirian|Of the central Pine Creek Orogen (Worden et al., 2008). Includes c. 2020 Ma tuffs.|c. 2020 Ma||||Includes tuffs.|
13823|Nappamerri Group|13497|4|Described|iv, v, x, xi, xii, p63-p65, p69 fig 6.1|Late Triassic|Late Permian|Cooper Basin. Maximum thickness of 600m. Previously the Nappamerri Formation before being elevated to Group status by Channon and Wood (1989) and Powis (1989). Widespread and best developed in the Nappamerri and Patchawarra troughs where it is over 500m thick. See also p70, p104, p132 tbl 8.1, p133, p141, p144 fig 9.2, p146, p148-p153, p170, p189, p204, p216.|||Includes the Arrabury Formation, Tinchoo Formation and the Cuddapan Formation.|Conformably overlies the Toolachee Formation and the Gidgealpa Group.||
13823|Nappamerri Group|13516|6|Mentioned|p147 fig 5, p163, p171 fig 12|Triassic|Late Permian|From Cooper Basin||||||
13823|Nappamerri Group|22883|6|Mentioned|P31|Middle Triassic|Late Permian|||||||
13823|Nappamerri Group|23154|6|Mentioned|Map Legend|Triassic|Permian|Geological Province - Cooper Basin.||||||
13823|Nappamerri Group|23155|4|Described|p23|Triassic|Late Permian|Underlying unit on STRZELECKI - Gidgealpa Group (disconformity).||||||
13823|Nappamerri Group|23340|5|Briefly described|12|Triassic|Triassic|||||||
13823|Nappamerri Group|23375|6|Mentioned|p293, 294|||In the Cooper Basin..||||||20-NOV-06
13823|Nappamerri Group|23731|5|Briefly described|p71|Triassic|Triassic|Geological Province: Cooper Basin.||||||
13823|Nappamerri Group|23982|5|Briefly described|p58 Fig.18|||Geological Province: Eromanga Basin.||||||
13823|Nappamerri Group|24092|5|Briefly described|p8 Fig.3|||||||||17-JAN-08
13823|Nappamerri Group|24204|5|Briefly described|p262, 270|||Equivalent to Walkandi Group. Geological Province: Cooper Basin.||||||17-DEC-04
13823|Nappamerri Group|24210|5|Briefly described|p133 Fig. 2|Middle Triassic|Late Permian|Overlies the Toolachee Formation.  Geological Province: Cooper Basin.  See also p132.||||||
13823|Nappamerri Group|42008|1|Redefined|p269|Carnian|Tatarian|See also Fig.2, Fig.3, Fig.4||||||
13823|Nappamerri Group|42085|6|Mentioned|Fig.2 P374|||||||||
13823|Nappamerri Group|42395|5|Briefly described|Fig.13 P83|||In Qld, SA.||||||
13823|Nappamerri Group|42746|5|Briefly described|Fig.2 P4|||||||||
13823|Nappamerri Group|42999|5|Briefly described|Table 2,p90||Middle Triassic|||||||
13823|Nappamerri Group|43105|5|Briefly described|Fig.7,p13|||||||||
13823|Nappamerri Group|43570|6|Mentioned|Fig.2,p535|Scythian|Tatarian|||||||
13823|Nappamerri Group|43628|6|Mentioned|Fig.3|Late Triassic|Early Triassic|||||||
13823|Nappamerri Group|44133|4|Described|p78-79, 85|Middle Triassic|Late Permian|Geological Province: Cooper Basin. Overlies: Gidgealpa Group. Consists of: Arrabury Formation, Tinchoo Formation. Overlain by the Cuddapan Formation. Thickness:>550m.||||||17-JAN-08
13823|Nappamerri Group|60717|5|Briefly described|p40, p41|Middle Triassic|Late Permian|Includes Arrabury and Tinchoo Formations. Overlies the Gidgealpa Group. Max.  Thickness: 500m. Geological Province: Cooper Basin. See also Figure 2.||||||17-JUL-14
13823|Nappamerri Group|61015|6|Mentioned|p45|Triassic|Triassic|||||||19-APR-05
13823|Nappamerri Group|61613|6|Mentioned|p282, p282 Fig. 2|Triassic|Late Permian|Includes Arrabury and Tinchoo Formation. Geological Province: Cooper and Simpson Basins.||||||07-FEB-11
13823|Nappamerri Group|61614|6|Mentioned|p294, p295, p290 Fig. 2|Middle Triassic|Late Permian|Includes Tinchoo and Arrabury Formations. Geological Province: Cooper Basin.||||||17-MAR-09
13823|Nappamerri Group|61615|5|Briefly described|p302, p303, p302 Fig. 2, p304, p305|Late Triassic|Late Permian|Includes; Arrabury and Tinchoo Formations, Callamburra, Paning and Wimma Sandstone Members. Conformably overlies Toolachee Formation. Geological Province: Cooper Basin. Fluvial and lacustrine environments.||||||07-FEB-11
13823|Nappamerri Group|61616|6|Mentioned|p330 Fig. 2|Early Triassic|Late Permian|Includes Arrabury and Tinchoo Formations. Geological Province: Cooper Basin.||||||
13823|Nappamerri Group|62046|5|Briefly described|p125 Fig. 2|Triassic|Permian|Geological Province: Cooper-Eromanga Basins.||||||14-APR-08
13823|Nappamerri Group|62537|6|Mentioned|p191 Fig.2. |Late Triassic|Early Triassic|Cooper Basin.|||Includes Arrabury and Tinchoo Formations and Wimma Sandstone.|Overlies Gidgealpa Group.||
13823|Nappamerri Group|62730|5|Briefly described|p351, p352 Fig. 1|Late Triassic|Late Permian|Includes the Arrabury and Tinchoo Formations. Geological Province: Cooper Basin.||||||21-APR-08
13823|Nappamerri Group|63832|6|Mentioned|p131 fig 2|Changhsingian|Changhsingian|Of Cooper Basin.||||||14-MAR-14
13823|Nappamerri Group|63978|2|Defined|p7, p18, Fig. 3|Early Triassic|Late Permian|Supersedes Nappamerri Fm. Contains the Arrabury and Tinchoo Fms. Max. thick: 450m. Conformable on Toolachee Fm (Gidgealpa Gp). Unconformably overlain by Poolawanna Fm and Hutton Sandstone (Eromanga Basin), and by Cuddapan Fm. in places. In Cooper Basin.||||||07-FEB-11
13823|Nappamerri Group|63979|6|Mentioned|p31|||||||||07-FEB-11
13823|Nappamerri Group|64048|5|Briefly described|p65|Triassic|Early Triassic|Includes the Tinchoo Formation. Member units act as a seal for the Toolachee Formation reservoirs.||||||07-FEB-11
13823|Nappamerri Group|64197|6|Mentioned|p625 Fig.1c|Middle Triassic|Late Permian|Cooper Basin.|||Includes the Arrabury and Tinchoo Formations|Overlies Toolachee Formation.||
13823|Nappamerri Group|64631|6|Mentioned|p44 Fig.2.||Changhsingian|Cooper Basin. Some biostratigraphic age control.||||Overlies Toolachee Formation.||
13823|Nappamerri Group|65489|5|Briefly described|p24-25, p42, p48, p96, p130-132, p158|Middle Triassic|Permian|Cooper Basin. Reservoir for economic oil and gas. The best source rocks are thin, laterally discontinuous coals in the upper part of the unit. Also regarded as a regional seal to the Cooper Basin.|||Includes Arrabury and Tinchoo Formations.|Overlies Gidgealpa Group unconformably (?) and Toolachee Formation conformably.||
13823|Nappamerri Group|65925|5|Briefly described|p16 Fig.2.3, Appendix 2.|Triassic|Triassic|Cooper Basin.|||||Red beds; mudstone; siltstone; sandstone; lithic sandstone.|
13823|Nappamerri Group|66529|6|Mentioned|p12 Fig.5|||Eromanga Basin.||||Is unconformably overlain by Poolowanna Formation.||
13823|Nappamerri Group|67402|6|Mentioned|p90, p90 fig CPR4, p95|Middle Triassic|Late Permian|See also p96, p98, p100, p105.|||Includes the Arrabury Formation and Tinchoo Formation.|Overlies the Gidgealpa Group.||
13823|Nappamerri Group|68731|5|Briefly described|p200 Fig 3.110, p204, p205, p207|Middle Triassic|Lopingian|Nomenclatural history and subdivision of this group is outlined by Gray and McKellar (2002). Introduced by Papalia (1969, p.108). Raised to Group status by Powis (1989). Thickest in the Windorah and Arrabury troughs.|||Includes the Tinchoo Formation and Arrabury Formation (basal).|Unconformably overlain by the Poolawanna Formation and Hutton Sandstone or the Cuddapan Formation.|Contains distinct redbed characteristics.|17-JUL-14
13823|Nappamerri Group|69019|5|Briefly described|p82.|Middle Triassic|Permian|Southern Cooper Basin.|||||Dominated by fluvial sands.|
13823|Nappamerri Group|69023|5|Briefly described|p81-82, p151|Middle Triassic|Permian|Cooper Basin. Eroded by Middle Triassic tectonic activity causing tilting to the NE. Rocks of this unit are not known in the CALLABONNA sheet area.||||Conformably overlies Gidgealpa Group.||
13823|Nappamerri Group|69454|5|Briefly described|p38:4|Ladinian|Changhsingian|Cooper Basin.|||Arrabury, Tinchoo Formations.|Overlies Gidgealpa Group.||12-JUL-16
13823|Nappamerri Group|69673|6|Mentioned|p153 fig 125||||||Includes Arrabury Formation, Tinchoo Formation|||
13823|Nappamerri Group|69728|6|Mentioned|p285|Late Triassic|Permian|Cooper Basin.|||Arrabury, Tinchoo Formations.|||
13823|Nappamerri Group|69797|5|Briefly described|p17 Fig.2, p18|Middle Triassic|Early Triassic|Geol. Prov: Cooper Basin.|||Tinchoo Formation, Arrabury Formation|||
13823|Nappamerri Group|69946|5|Briefly described|p9, p52, p54|Late Triassic|Permian|Cooper Basin.|||Includes Arrabury and Tinchoo Formations.|Conformably overlies Gidgealpa Group. Is overlain unconformably by Cuddapan Formation.||
13823|Nappamerri Group|69947|5|Briefly described|p13 Fig.7.2, p16-17 Figs.7.5-6|Middle Triassic|Late Carboniferous|See also p21 Fig.7.10. Cooper Basin.|||Arrabury, Tinchoo Formations.|Overlies Gidgealpa Group. Is overlain unconformably by Cuddapan Formation.||
13823|Nappamerri Group|69948|6|Mentioned|p3-4|Early Triassic|Permian|Cooper Basin. Basement to Eromanga Basin in the southern Cooper region.||||||
13823|Nappamerri Group|70317|6|Mentioned|p33|Middle Triassic|Late Permian|Cooper Basin.|||Arrabury, Tinchoo Formations.|Overlies Gidgealpa Group. Is overlain unconformably by Cuddapan Formation.||
13823|Nappamerri Group|70823|4|Described|iv, p14, p25-p27|Middle Triassic|Lower Triassic|Cooper Basin. Seismic reflection and outcrop characteristics briefly discussed. This group has an average thickness of ~200m and is thickest in the Nappamerri Trough. This group is generally regarded as sealing the Gidgealpa Group. See also p39, p41, p49-p50, p70, p75-p77, p82.|||Includes the Arrabury Formation and the Tinchoo Formation.|Conformably overlies the Gidgealpa Group.||
13823|Nappamerri Group|70824|4|Described|p1, p5, p8, p37, p104-p107, p113, p123|Middle Triassic|Lower Triassic|Cooper Basin. Typically deposited as organically lean fluvial deposits. Areal extent and source rock geochemistry is discussed. This group reaches a maximum thickness close to 600m in the Nappamerri, Patchawarra and Arrabury troughs.|||Includes the Arrabury Formation and the Tinchoo Formation.|||
13823|Nappamerri Group|70946|5|Briefly described|p1087, p1089|Middle Triassic|Late Permian|Cooper Basin.|||Arrabury, Tinchoo Formations.|||08-OCT-18
13823|Nappamerri Group|71265|5|Briefly described|p589|Induan|Olenekian|Cooper Basin.|||Arrabury Formation.|Overlies Gidgealpa Group.||
13823|Nappamerri Group|71321|6|Mentioned|p15|||Of Patchawarra and Nappamerri troughs, Cooper Basin.||||||
13823|Nappamerri Group|71342|5|Briefly described|Ch4 p3-p4, Ch5 p9,  Ch5 p30|Early Triassic|Late Permian|Cooper Basin. See also Ch5 p52, Ch7 p13, Ch7 p16, Ch7 p21, Ch10 tbl 10.1, Ch10 p14, Ch10 p17, Ch10 p19-p20, Ch13 p7.|||Includes the Arrabury Formation and the Tinchoo Formation.|Overlies the Toolachee Formation. Unconformably overlain by the Hutton Sandstone.||
13823|Nappamerri Group|71701|5|Briefly described|p155|Olenekian|Induan|Cooper Basin.|||Includes the Arrabury Formation.|Overlies the Gidgealpa Group.||
13823|Nappamerri Group|72297|5|Briefly described|p742|||Cooper Basin. Has gas reservoirs at Marama and at Epsilon.||||||
13823|Nappamerri Group|72298|5|Briefly described|p801|Triassic||Eromanga Basin (SA,QLD).||||Is overlain unconformably by Poolowanna FZ.||
13823|Nappamerri Group|73167|5|Briefly described|p662, p664|Triassic|Triassic|Cooper Basin. Up to 500m of Nappamerri Group sediments uplifted and eroded along pre-existing faults in the Late Triassic E-W-compressional Hunter-Bowen Event, regional unconformity. Constituent units in Fig. 2, p664 confirmed in ASUD.|||Callamurra Member, Panning Member, Wimma Sandstone Member, Tinchoo Formation|Overlies the Toolachee Formation.|Floodplain, lacustrine and fluvial channel sediments.|
13823|Nappamerri Group|73244|6|Mentioned|p86|Triassic|Triassic|Cooper Basin. Floodplain, lacustrine, fluvial channels.||||||
13823|Nappamerri Group|73251|6|Mentioned|p62|Middle Triassic|Permian|Cooper Basin. Non-marine depositional environments.|||Tinchoo Formation, Arrabury Formation, Wimma Sandstone Member, Paning Member, Callamurra Member|Underlain by Toolachee Formation (Gidgealpa Group).||
13823|Nappamerri Group|73343|5|Briefly described|p337-338|Triassic|Triassic|Cooper Basin. Reflects floodplain, lacustrine, and fluvial channel settings. Incised during the Late Triassic Hunter-Bowen Event.|||Tinchoo Formation, Wimma Sandstone Member, Panning Member, Callamurra Member|Underlain by Toolachee Formation.||
13823|Nappamerri Group|73479|5|Briefly described|p156 Fig.2, p159, p163, p166|Triassic|Triassic|Cooper Basin. Floodplain, lacustrine, fluvial channels depositional environment. Highly efficient regional seal. Up to 500 m thickness was exhumed and eroded in Hunter-Bowen Event.|||Callamurra Member, Panning Member, Wiumma Sandstone Member, Tinchoo Formation|Overlies Toolachee Formation, unconformably underlies Cuddapan Formation||
13823|Nappamerri Group|73495|6|Mentioned|p498|Middle Triassic|Lower Triassic|Cooper Basin. Up to 550 m thick.||||||
13859|Naringa Calcareous Member|9199|5|Briefly described|Map legend|||Of the Irindina Gneiss.  Flaggy biotite quartzite, calc-silicate rock, marble.  Geological Province: Arunta Block.||||||04-NOV-04
13859|Naringa Calcareous Member|23844|5|Briefly described|Fig.26|||Of the Irindina Gneiss. Biotite quartzite, calc-silicate rock, biotite gneiss and marble.||||||20-NOV-06
13859|Naringa Calcareous Member|38885|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
13859|Naringa Calcareous Member|39583|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
13859|Naringa Calcareous Member|39887|6|Mentioned|Fig.3|||||||||
13859|Naringa Calcareous Member|39931|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic. Of the Irindina Gneiss (Harts Range Group).||||||07-NOV-08
13859|Naringa Calcareous Member|40100|5|Briefly described|p258|||||||||
13859|Naringa Calcareous Member|46730|4|Described|p6, 11|||Of Irindina Gneiss. Geological Province: Arunta Block.||||||
13859|Naringa Calcareous Member|46868|6|Mentioned|p77|||||||||
13859|Naringa Calcareous Member|49036|6|Mentioned|p13|||||||||
13859|Naringa Calcareous Member|60547|5|Briefly described|Map Legend|Precambrian|Precambrian|Of the Irindina Gneiss. Flaggy biotite quartzite, calc-silicate rock, marble.||||||
13859|Naringa Calcareous Member|62595|6|Mentioned|p28 Fig.4.|||Relative probability plots of detrital zircon data are shown. See also Naringa Gneiss p4 Table2.||||||19-JUN-13
13859|Naringa Calcareous Member|68316|5|Briefly described|pp777-784|Early Devonian|Mesoproterozoic|Amadeus Basin. Age range determined from quartzite within the Naringa Calcareous Member.|1.27 Ga-405 Ma|Of the Irindina Gneiss.|||Comprises quartzite and marble.|
13859|Naringa Calcareous Member|69444|5|Briefly described|p29:1-3|||Crops out in western Harts Range. Similar detrital zircon population to the lower part of Stanovos Gneiss Member; may be correlative.||Irindina Gneiss.|||Calc-silicate rock, calcareous quartzofeldspathic gneiss, marble, biotite gneiss and quartzite.|12-JUL-16
13859|Naringa Calcareous Member|70094|6|Mentioned|p76, 80|||||Irindina Gneiss.||||
13859|Naringa Calcareous Member|71592|5|Briefly described|Appendix A.|||Arunta Orogen.  SHRIMP U-Pb zircon metamorphism ages.|452+/-5.7 Ma and 484+/-13 Ma.||||Quartzite.|
13859|Naringa Calcareous Member|72516|6|Mentioned|p7, p78, p86|||Irindina Province. [unclear if this unit still in use or obsolete]||Irindina Gneiss||Equivalent to the Yackah beds.||16-JUN-21
13949|Neave Sandstone|14019|4|Described|p15-16|||Of the Wattie Group. Quartz sandstone with feldspar, chert, clay and rock fragments. Disconformably overlies Mount Sanford Formation. Thickness: 12m. Geological Province: Victoria Basin.||||||
13949|Neave Sandstone|24122|5|Briefly described|p4 Fig.3|||Of Wattie Group.  Geological Province: Victoria Basin.||||||
13949|Neave Sandstone|24297|3|Fully described|p7|Proterozoic|Proterozoic|Of Wattie Group. Conformably overlain by Gibbie Formation, disconformably overlies Mount Sanford Formation. Maximum thickness: 20m.  See also p5 Tb. 2.||||||20-NOV-06
13949|Neave Sandstone|24298|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Wattie Group. Pebbly sandstone, quartz sandstone.||||||20-NOV-06
13949|Neave Sandstone|24441|5|Briefly described|p1 Fig. 1|Mesoproterozoic|Mesoproterozoic|Of the Wattie Group. Unconformably overlies Mount Sanford Formation;  overlain by Gibbie Formation. Geological Province: Victoria Basin.||||||25-JAN-06
13949|Neave Sandstone|24442|5|Briefly described|p50 Fig. 1|||Of the Wattie Group. Geological Province: Victoria Basin.||||||
13949|Neave Sandstone|28255|3|Fully described|p38, Tb. 11 (opp. p8)|Adelaidean|Adelaidean|Of the Wattie Group. Consists of flaggy, blocky and massive quartz sandstone. Conformably overlies [??] Gibbie Formation. Max. thickness: 21m; ~12m in type section.||||||31-OCT-11
13949|Neave Sandstone|30003|4|Described|p8, p12|||Of the Wattie Group. Overlies the Mount Sanford Formation.  Carpentarian or Adelaidean.  Thickness at Neave Creek: 12m.||||||19-APR-05
13949|Neave Sandstone|30004|6|Mentioned|Map legend|Proterozoic|Proterozoic|Carpentarian or Adelaidean||||||
13949|Neave Sandstone|32172|4|Described|Table 1|||Carpentarian or Adelaidean||||||
13949|Neave Sandstone|32173|5|Briefly described|Map legend|Adelaidean|Carpentarian|Of the Wattie Group.  Fine and medium sandstone.  Carpentarian or Adelaidean (per legend).||||||16-NOV-04
13949|Neave Sandstone|32175|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Wattie Group.  Blocky, fine and medium quartz sandstone; minor pebbly beds near base.||||||02-DEC-04
13949|Neave Sandstone|32660|5|Briefly described|Table 6|||||||||
13949|Neave Sandstone|33374|6|Mentioned|p7|||Strat.||||||
13949|Neave Sandstone|33375|4|Described|p7, p8 Tb. 1|Adelaidean|Adelaidean|Of the Wattie Group. Overlain by the Gibbie Formation; overlies the Mount Sanford Formation.||||||26-APR-05
13949|Neave Sandstone|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
13949|Neave Sandstone|33378|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Wattie Group. Fine and medium quartz; minor conglomeratic sandstone.||||||27-APR-05
13949|Neave Sandstone|45112|5|Briefly described|Table 9|||||||||
13949|Neave Sandstone|48943|2|Defined|p47|Adelaidean|Adelaidean|||||||
13949|Neave Sandstone|60589|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Wattie Group.  Pebbly sandstone and quartz sandstone.  Geological Province: Victoria Basin.||||||
13949|Neave Sandstone|60672|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Fine and medium quartz sandstone, minor conglomeritic sandstone. Overlies Mount Sanford Formation. Overlain by Gibbie Formation. Of Wattie Group. Geological Province: Victoria Basin.||||||11-JAN-05
13949|Neave Sandstone|60685|4|Described|p4 Fig. 3, p7|Mesoproterozoic|Mesoproterozoic|Of the Wattie Group. Sandstone, minor conglomerate. Disconformably on Mount Sanford Formation; conformable below Gibbie Formation. Max. thickness: 10m. Geological Province: Victoria Basin.||||||
13949|Neave Sandstone|65342|6|Mentioned|p11 Fig.13. |||Victoria Basin.||Unit in Wattie Group.||Unconformably overlies Mount Sanford Formation. Is overlain by Gibbie Formation.||
13949|Neave Sandstone|67151|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Birindudu Basin.||Unit in Wattie Group.||Overlies, possibly unconformably, Mount Sanford Formation. Is overlain by Gibbie Formation.|Fine and medium quartz sandstone, minor conglomeratic sandstone.|
13949|Neave Sandstone|68733|4|Described|p177-180, p182-186||Statherian|Sweet et al. (1974). Previously included in the Victoria Basin by Cutovinos et al. (2002). Now included in the Birrindudu Basin due to a recent subdivision by the NGTS (Dunster and Ahmad 2013). ~ 12-20m thick. Maximum depositional age of ca. 1617 +/- 39 Ma. Sm-Nd isotope data tabulated.|Maximum depositional age of ca. 1617 +/- 39 Ma.|Of the Wattie Group.||Unconformably overlies Mount Sanford Formation. Conformably overlain by the Gibbie Formation.|Comprises cross-bedded fine- to medium grained feldspathic sandstone with locally abundant pebbly beds, mud flakes and lithic fragments.|05-DEC-17
13949|Neave Sandstone|69432|4|Described|p17:2, 9|||Birrindudu Basin. Rarely over 20m thick. Probably shallow-marine littoral deposits. Detrital zircon maximum depositional age; similar provenance to Wickham Formation.|1622 +/- 32 Ma (Carson, 2010).|Wattie Group.||Overlies Mount Sanford Formation conformably to locally unconformably. Is overlain conformably by Gibbie Formation.|Grey-purple, fine to medium quartz sandstone containing feldspar, chert, clay and rock fragments; basal conglomerate contains chert and quartzite clasts.|17-AUG-18
13949|Neave Sandstone|69673|6|Mentioned|p48 fig 35|||||Wattie Group||Unconformably overlies Mount Sanford Formation, overlain by Gibble Formation||
13949|Neave Sandstone|70655|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Birindudu Basin.||Wattie Group.||Overlies Mount Sanford Formation, possibly unconformably. Is overlain by Gibbie Formation.|Fine and medium quartz sandstone; minor conglomeratic sandstone.|24-JAN-22
13949|Neave Sandstone|70854|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Wattie Group.||?Unconformably overlies Mount Sanford Formation. Is overlain by Gibbie Formation.|Fine and medium quartz sandstone, minor conglomeratic sandstone.|21-SEP-17
13949|Neave Sandstone|70855|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Wattie Group.||Overlies Mount Sanford Formation ?unconformably. Is overlain by Gibbie Formation.|Pebbly sandstone, quartz sandstone.|
13949|Neave Sandstone|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||sandstone|
13949|Neave Sandstone|71302|5|Briefly described|p6,72,74||Paleoproterozoic|Of Birindudu Basin. Maximum depositional age: 1617+\-39 Ma (Carson, 2013; Munson, 2016 and Munson, in prep). Contain small c > 1560-1640 Ma age populations.||Unit of Wattie Group.||Overlain by Gibbie Formation. Underlain by Mount Sanford Formation.||
13949|Neave Sandstone|71592|5|Briefly described|Appendix A.|||Victoria River Region.|1617+/- 39 Ma (MDA: Pb/Pb zircon).||||Volcaniclastic rock.|
13949|Neave Sandstone|72718|6|Mentioned|p7|Calymmian|Statherian|Birrindudu Basin.|1622 +/- 32 Ma|Wattie Group||Unconformably[?] underlain by Mount Sanford Formation. Overlain by Gibbie Formation.||
13990|Nelson Shale|14019|5|Briefly described|p21|Middle Cambrian|Middle Cambrian|Of the Negri Subgroup (Goose Hole Group).  Geological Province: Ord Basin.||||||
13990|Nelson Shale|22547|4|Described|p30||Early Cambrian|Of the Negri Subgroup. Geological province: Ord Basin. Thickness: 180 m. Overlies Headley Limestone.||||||14-NOV-06
13990|Nelson Shale|23621|5|Briefly described|p36|Late Cambrian|Middle Cambrian|See also page 9 Table 1. Of Negri Subgroup. Geological Province: Ord Basin. Max. thickness: 18 m.||||||
13990|Nelson Shale|23622|5|Briefly described|Map Legend|Cambrian|Cambrian|Of Goose Hole Group. Geological Province: Ord Basin.||||||
13990|Nelson Shale|23821|5|Briefly described|p244|Middle Cambrian|Middle Cambrian|Of Negri Group. Geological Province: Ord Basin.  Maximum thickness: 180m.||||||
13990|Nelson Shale|28255|3|Fully described|p96|Cambrian|Cambrian|Grey and red, calcareous and gypsiferous shales and mudstone; minor limestone. Conformably overlies Headleys Limestone; conformably underlies Linnekar Limestone. Max. thickness: 165m. See also Table 9 (before p83) and p143 Appendix.||||||
13990|Nelson Shale|32172|4|Described|Table 2|||Middle Camb.||||||
13990|Nelson Shale|32173|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Of the Negri Group.  Grey and red calcareous shales with gypsum bands and mudstone.  Conformably overlies Headleys Limestone; conformably overlain by the Linnekar Limestone.||||||20-NOV-06
13990|Nelson Shale|32648|6|Mentioned|p32|||M.Camb.||||||
13990|Nelson Shale|33376|6|Mentioned|Map legend|Early Ordovician|Middle Cambrian|Middle Cambrian to Lower Ordovician||||||
13990|Nelson Shale|36551|6|Mentioned|Table 16|||||||||
13990|Nelson Shale|36890|3|Fully described|p396|||||||||
13990|Nelson Shale|39210|5|Briefly described|Fig.18|||||||||
13990|Nelson Shale|40993|6|Mentioned|Fig.1|||||||||
13990|Nelson Shale|41840|2|Defined|p41|Middle Cambrian||||||||
13990|Nelson Shale|41864|3|Fully described|p18|||||||||
13990|Nelson Shale|41865|5|Briefly described|Map Legend|Middle Cambrian||||||||
13990|Nelson Shale|41866|5|Briefly described|Map legend|Middle Cambrian||||||||
13990|Nelson Shale|42070|6|Mentioned|Fig.9 P12|||||||||
13990|Nelson Shale|43299|5|Briefly described|Map Legend||Cambrian|Of the Negri Subgroup.||||||20-NOV-06
13990|Nelson Shale|43853|5|Briefly described|Map Legend||Ordian|||||||
13990|Nelson Shale|44230|5|Briefly described|Map Legend||Middle Cambrian|||||||
13990|Nelson Shale|44317|4|Described|Table 4||Cambrian|||||||
13990|Nelson Shale|44318|14|Not recorded|map legend||Middle Cambrian|Mid.Cambrian.||||||
13990|Nelson Shale|44363|5|Briefly described|p.6,18,20||Middle Cambrian|Middle Cambrian, Negri Group.||||||
13990|Nelson Shale|44364|14|Not recorded|map legend|||||||||
13990|Nelson Shale|44868|5|Briefly described|Map Legend|Boomerangian|Ordian|||||||
13990|Nelson Shale|44965|14|Not recorded|Not recorded|||||||||
13990|Nelson Shale|45047|6|Mentioned|p126|||||||||
13990|Nelson Shale|48943|3|Fully described|p108|||Strat. table p139.||||||20-NOV-06
13990|Nelson Shale|60419|3|Fully described|p1, p3 Fig.2, p5|Middle Cambrian|Middle Cambrian|Of Negri Subgroup. Conformably overlies Headleys Limestone. Conformably overlain by Linnekar Limestone. Max. thickness: 183 m. Maroon gypsiferous shale and mudstone. Geological Province: Ord Basin.||||||
13990|Nelson Shale|60519|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Negri Subgroup (Goose Hole Group). Purple siltstone and mudstone; minor feldspathic sandstone. Geological Province: Ord Basin.||||||03-NOV-04
13990|Nelson Shale|60589|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Of the Negri Subgroup (Goose Hole Group).  Maroon and grey gypsiferous shale and mudstone, minor sandstone, laminated limestone.  Conformably overlies Headleys Limestone; conformably overlain by the Linnekar Limestone. Geological Province: Ord Basin.||||||24-NOV-04
13990|Nelson Shale|64580|6|Mentioned|map legend|||Of Goose Hole Group.||||||15-DEC-08
13990|Nelson Shale|67860|4|Described|p417 Fig4-85, p420 Tb.4-18, p421 fig4-86|Middle Cambrian|Middle Cambrian|100-183 m thick. Type section details given. Contains rare Girvanella fossils.||Negri Subgroup||Conformably overlies Headleys Limestone or Antrim Plateau Volcanics. Is conformably overlain by Linnekar Limestone.|Purple gypsiferous siltstone and sandstone; minor micritic limestone.|
13990|Nelson Shale|69099|4|Described|GEOL_LUT_CSV files + geochron files|Series 3|Series 3|Ord Basin||Negri Subgroup|||gypsiferous siltstone and mudstone; minor micritic limestone|
13990|Nelson Shale|69165|5|Briefly described|100k_interpgeop_lut.csv|Cambrian|Cambrian|See also 500k_geologyp08_lut.csv.||Negri Subgroup|||Gypsiferous siltstone and mudstone; minor micritic limestone.|
13990|Nelson Shale|69437|5|Briefly described|p22:10-11|Series 3|Series 2|Ord Basin, Centralian B Superbasin. Sequence 1.||Negri Subgroup.||Overlies Headleys Limestone. Is overlain by Linnekar Limestone.||12-JUL-16
13990|Nelson Shale|69448|4|Described|p33:2-5, 8-9|Middle Cambrian|Middle Cambrian|Traves (1955). Ord Basin. 100-183m thick. Intertidal to supratidal deposits. Recessive unit: widely distributed but poorly exposed. Ordian age. Associated with uneconomic stratabound copper at contact with Headleys Limestone.||Negri Subgroup.||Conformably overlies Headleys Limestone or (locally) Antrim Plateau Volcanics unconformably. Is overlain conformably by Linnekar Limestone.|Maroon to grey, gypsiferous and pyritic shale and mudstone, minor fine sandstone, rare laminated limestone; unfossiliferous except for calcimicrobe Girvanella.|12-JUL-16
13990|Nelson Shale|69634|4|Described|GEOL_LUT_CSV files|Series 3|Series 3|Geological province: Halls Creek Orogen. Of Ord Basin. Events: Alice Springs Orogeny. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|505-497 Ma (Inferred)|Unit of Negri Subgroup.|||Gypsiferous siltstone and mudstone; minor micritic limestone|
13990|Nelson Shale|69673|5|Briefly described|p192, p193|Cambrian|Cambrian|183m thick.||Negri Subgroup||Overlain by Linnekar Limestone, overlies Headleys Limestone|Gypsiferous and pyritic shale and mudstone with minor sandstone and rare laminated limestone, deposited under peritidal conditions.|
13990|Nelson Shale|70154|5|Briefly described|100k_interpgeop_lut.csv|Cambrian|Cambrian||497-505 Ma|Negri Subgroup|||Gypsiferous siltstone and mudstone; minor micritic limestone.|
13990|Nelson Shale|71267|4|Described|GEOL_LUT_CSV files|Series 3|Series 3|Geological province: Halls Creek Orogen. Of Ord Basin. Events: Alice Springs Orogeny (450-295 Ma); Pertnjara-Brewer Movements (Alice Springs Orogeny phase 2) (390-360 Ma); Rodingan Movement (Alice Springs Orogeny phase 1) (450-420 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|505-497 Ma (inferred)|Unit of Negri Subgroup.|||Maroon and grey gypsiferous shale and mudstone, minor sandstone, laminated limestone.|
13990|Nelson Shale|71800|5|Briefly described|p25-p26|Middle Cambrian|Middle Cambrian|Ord Basin.||Negri Subgroup||Overlies the Headleys Limestone. Overlain by the Linnekar Limestone.||
13990|Nelson Shale|73255|6|Mentioned|p534 Fig.2|Cambrian|Cambrian|||Goose Hole Group||Overlies the Headleys Limestone, underlies the Linnekar Limestone.||
14123|Nicholson Granite Complex|22673|6|Mentioned|64|||Geological province: Mount Isa Basin.||||||14-NOV-06
14123|Nicholson Granite Complex|22680|6|Mentioned|85|||||||||
14123|Nicholson Granite Complex|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
14123|Nicholson Granite Complex|23405|6|Mentioned|p565|||||||||
14123|Nicholson Granite Complex|23406|6|Mentioned|p608|||Parts contained as clasts in the Fish River Formation.||||||16-JUN-09
14123|Nicholson Granite Complex|24419|5|Briefly described|p17, p18|Paleoproterozoic|Paleoproterozoic|Includes the Cliffdale Volcanics.  Geological Province: Lawn Hill Subprovince (north).||||||07-NOV-08
14123|Nicholson Granite Complex|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
14123|Nicholson Granite Complex|31421|6|Mentioned|p507|||||||||
14123|Nicholson Granite Complex|35640|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
14123|Nicholson Granite Complex|35950|6|Mentioned|p304|||||||||
14123|Nicholson Granite Complex|36012|3|Fully described|Table 1|||See also p8.||||||14-NOV-06
14123|Nicholson Granite Complex|36439|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
14123|Nicholson Granite Complex|36442|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
14123|Nicholson Granite Complex|37462|5|Briefly described|p234|||||||||
14123|Nicholson Granite Complex|38042|6|Mentioned|Fig.1|||||||||
14123|Nicholson Granite Complex|38237|6|Mentioned|p130|||||||||
14123|Nicholson Granite Complex|38335|6|Mentioned|p1727|||||||||
14123|Nicholson Granite Complex|38584|4|Described|p4|||||||||
14123|Nicholson Granite Complex|38900|6|Mentioned|p66|||||||||
14123|Nicholson Granite Complex|39123|6|Mentioned|p157|||||||||
14123|Nicholson Granite Complex|39445|5|Briefly described|Table 2|||See also p38.||||||14-NOV-06
14123|Nicholson Granite Complex|39685|6|Mentioned|Fig.1|||||||||
14123|Nicholson Granite Complex|39925|6|Mentioned|p337|||||||||
14123|Nicholson Granite Complex|40489|6|Mentioned|p88|||Also Mention on p89.||||||14-NOV-06
14123|Nicholson Granite Complex|40491|6|Mentioned|p79|||||||||
14123|Nicholson Granite Complex|40840|6|Mentioned|Map legend|||||||||
14123|Nicholson Granite Complex|41125|6|Mentioned|p35|||||||||
14123|Nicholson Granite Complex|41319|6|Mentioned|p195|||||||||
14123|Nicholson Granite Complex|41406|6|Mentioned|Map legend|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
14123|Nicholson Granite Complex|41721|3|Fully described|p4|||Includes the Norris and Nicholson granites of Roberts et al (1963). Comprises non-equigranular, coarse- to medium-grained hornblende and/or biotite-bearing granite, adamellite and granodiorite.||||||01-AUG-07
14123|Nicholson Granite Complex|41722|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
14123|Nicholson Granite Complex|41757|4|Described|p207|||||||||
14123|Nicholson Granite Complex|42754|6|Mentioned|p3|||||||||
14123|Nicholson Granite Complex|43595|6|Mentioned|p353|||Rb-Sr date: 1804+/-83 Ma.||||||14-NOV-06
14123|Nicholson Granite Complex|45162|6|Mentioned|p11|||||||||
14123|Nicholson Granite Complex|45166|5|Briefly described|p8|||||||||
14123|Nicholson Granite Complex|46804|6|Mentioned|p154|||||||||
14123|Nicholson Granite Complex|49001|2|Defined|p1|Carpentarian|Carpentarian|||||||
14123|Nicholson Granite Complex|49002|6|Mentioned|p1|||||||||
14123|Nicholson Granite Complex|61936|5|Briefly described|p193, p194 Fig. 6|||Geological Province: Lawn Hill Platform, Eastern Fold Belt, Mount Isa Inlier.||||||
14123|Nicholson Granite Complex|65228|5|Briefly described|p20.|Orosirian|Orosirian|SE McArthur Basin. Felsic; geochemically similar to Scrutton Volcanics. Ages from different phases of the granite (Page et al. 2000).|1856 +/- 3 Ma; 1845 +/- 3 Ma.|||Intrudes Murphy Metamorphic complex.||
14123|Nicholson Granite Complex|65232|5|Briefly described|p9, p8 Fig. 7|||Comagmatic I-type granitoids intrude Murphy Metamorphics. Age: 1856 Ma, 1845 Ma. Biotite +/- muscovite granite and hornblende-biotite granodiorite. Geol Prov: Murphy Inlier. See also Nicholson Granite, p67-68.||||||09-FEB-10
14123|Nicholson Granite Complex|65337|6|Mentioned|p50.||||||||K-feldspar rich granite.|
14123|Nicholson Granite Complex|66529|5|Briefly described|p20 Fig.7, p21  |||Also shortened to Nicholson Granite on p20.|~1840 Ma (M. Ahmad, NTGS, pers.comm.)|||Intrudes the Murphy Metamorphics and Cliffdale Volcanics.|Biotite +/-  muscovite granite and hornblende-biotite granodiorite.|
14123|Nicholson Granite Complex|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map, p29|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Camooweal-Murphy Domain, Mount Isa Inlier. Nicholson Igneous Event. Informally subdivided into 6 or 7 units. See also Nicholson Granite (p9).|1845 +/- 3 Ma.|Nicholson Suite.||Intrudes Cliffdale Volcanics.|Xenolithic porphyritic hornblende-biotite and biotite granite, microgranite, greisen.|
14123|Nicholson Granite Complex|68998|5|Briefly described|vi, p34-37|||Murphy Province. This name is used interchangeably with Nicholson Granite. Contains inherited grains aged up to c.2500 Ma, matching the detrital spectrum of the Murphy Metamorphics. This age determination substantiates the "Barramundi" age commonly assumed for granites in the Murphy Province. Most outcrops are moderately to deeply weathered. Intruded by microgranite dykes. Additional ages are derived from Page et al (2000) and include 1856 +/- 3 Ma and 1845 +/- 3 Ma (SHRIMP U-Pb).|1846 +/- 6 Ma (magmatic crystallisation).|||Intrudes (cross-cuts) the Murphy Metamorphics.|Deeply weathered, deep red to white, generally megacrystic (feldspar phenocrysts to 10cm) felsic granite.|30-JUN-20
14123|Nicholson Granite Complex|69417|5|Briefly described|p2:5|Orosirian|Orosirian|Murphy Orogen.||||Intrudes Murphy Metamorphics.||12-JUL-16
14123|Nicholson Granite Complex|69418|6|Mentioned|p3:21|||Murphy Province. Hosts the Crystal Hill greisen Sn-W deposit (described).||||||12-JUL-16
14123|Nicholson Granite Complex|69423|4|Described|p8:1, 3-5|Orosirian|Orosirian|Sweet and Slater (1975), Ahmad and Wygralak (1989). Murphy Inlier, Murphy Province. Comagmatic with Connellys and Cliffdale Volcanics. Eight lithological varieties (Gardner, 1978) were simplified into two groups by Ahmad (1987). SHRIMP U-Pb zircon ages of two samples. Hosts copper and several small tin +/- tungsten occurrences (eg Crystal Hill).|1856 +/- 3 Ma & 1845 +/- 3 Ma (Page et al., 2000)||Norris, Nicholson Granites.|Intrudes Murphy Metamorphics.|Group A: inequigranular, coarse- to medium-grained hornblende- and/or biotite-bearing granite, quartz monzonite and granodiorite; common mafic xenoliths and K-feldspar phenocrysts. Group B: equigranular quartz monzonite, granite and alkali granite.|12-JUL-16
14123|Nicholson Granite Complex|69430|5|Briefly described|p15:11, 49-51|||Appears as Nicholson Granite in the text as often as it appears as Nicholson Granite Complex in diagrams.||||Is overlain unconformably by Westmoreland Conglomerate (Tawallah Group).|Includes hornblende-biotite granodiorite and biotite-muscovite granite.|12-JUL-16
14123|Nicholson Granite Complex|69433|5|Briefly described|p18:2|||Probable source of 1847 +/- 13 Ma sediment (zircons) for Wire Creek Sandstone.||||Is overlain unconformably by Wire Creek Sandstone.||12-JUL-16
14123|Nicholson Granite Complex|69434|6|Mentioned|p19:1, 4|||Murphy Inlier. A source of siliciclastic sediments for the Caulfield beds, South Nicholson Basin.||||||12-JUL-16
14123|Nicholson Granite Complex|69591|5|Briefly described|p30-31, p60|||Camooweal-Murphy Domain. Is coeval with the Kalkadoon Granodiorite to the S.|1845 +/- 3 Ma (Geoscience Australia unpub. data).|||Intrudes Cliffdale Volcanics.|Xenolithic porphyritic hornblende-biotite and biotite granite, microgranite, greisen.|
14123|Nicholson Granite Complex|69673|6|Mentioned|p3|||||||||
14123|Nicholson Granite Complex|70849|5|Briefly described|Map legend.|Orosirian|Orosirian|Murphy Province.||||Intrudes Murphy Metamorphics and Cliffdale Volcanics.|Hornblende-biotite adamellite and granodiorite, medium- to coarse-grained, inequigranular. Biotite + muscovite granite and adamellite, medium- to fine-grained, equigranular.|
14123|Nicholson Granite Complex|71369|6|Mentioned|p47|||Basement rocks of the South Nicholson Basin.||||||
14123|Nicholson Granite Complex|71592|5|Briefly described|Appendix A.|||Murphy Region.|1846+/-6 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
14123|Nicholson Granite Complex|72526|5|Briefly described|p8 Fig.1.3.|Orosirian|Orosirian|3 U-Pb SHRIMP igneous crystallisation ages given. Shown as being located in the west and central part of the South Nicholson Basin and the Southeastern McArthur Basin. See also South Nicholson Granite Complex p6.|1845+/-3 Ma, 1856+/-6 Ma|||Probably overlain by Westmoreland Conglomerate and Wire Creek Sandstone.||
14123|Nicholson Granite Complex|72912|5|Briefly described|p5 Fig.3.|Orosirian|Orosirian|Located in the west part of the South Nicholson Basin and the Southeastern McArthur Basin. Three U-Pb zircon igneous crystallisation ages (Ma) shown. See also Nicholson Granite p19.|1856 +/- 6 Ma to 1845 +/- 3 Ma.|||Shown as overlying Cliffdale Volcanics, Murphy Metamorphics. Unconformably underlies Westmoreland Conglomerate.||
14123|Nicholson Granite Complex|72919|4|Described|p1, p4-9, p11, p93|Orosirian|Orosirian|Murphy Province, North Australian Craton. Two varieties have been described; Group A, a coarse- to medium-grained massive porphyritic hornblende +/-biotite granite-granodiorite, characterised by large K-feldspar crystals and abundant mafic xenoliths, and Group B, characterised as an equigranular biotite +/-muscovite granite-adamellite with rare hornblende and xenoliths. New U-Pb SHRIMP zircon magmatic crystallisation age of 1855 +/- 5 Ma. Previously reported geochronology yielded ages of 1856 +/- 3 Ma, 1845 +/- 3 Ma, and 1846 +/- 6 Ma (Page et al., 2000; Kositcin et al., 2013). Broadly coeval with Connellys Volcanics and Cliffdale Volcanics.|1855 +/- 5 Ma U-Pb SHRIMP|||Intrudes Murphy Metamorphics.|Includes biotite granite, coarse- to medium-grained massive porphyritic granite-granodiorite, and equigranular granite-adamellite.|
14123|Nicholson Granite Complex|73042|6|Mentioned|p4|Orosirian|Orosirian|Southern McArthur Basin and South Nicholson Basin region. Geochronology is a U-Pb zircon igneous crystallisation age.|1856+/-6 Ma, 1845+/-3 Ma, 1846+/-6 Ma|||||
14123|Nicholson Granite Complex|73427|6|Mentioned|p3|Orosirian|Orosirian|North Australian Craton, Murphy Inlier.|1855-1845 Ma|||||
14166|Ningbing Group|13194|4|Described|p382 fig 4-59, p399, p402 fig 4-66|Devonian|Devonian|171-1166m thick Famennian reef complex.|||Buttons Formation, Garimala Limestone, Wungabal Limestone, Kamilili Formation, Djilirri Limestone.|In part equivalent to Bonaparte Formation.  Overlies Cockatoo Group.||
14166|Ningbing Group|13234|6|Mentioned|p253,p260 Tb.1, |Famennian|Famennian|Lack porosity-enhancing stromatoporoids. Is similar to fractured algal boundstones of Nullara Formation in Canning Basin.||||||
14166|Ningbing Group|14228|5|Briefly described|p6 fig3|Devonian|Devonian|Southern Bonaparte Basin.||||Overlies Cockatoo Group. Overlain by Langfield Group.||05-OCT-16
14166|Ningbing Group|22814|5|Briefly described|fig2|Early Carboniferous|Late Devonian|||||||
14166|Ningbing Group|23377|6|Mentioned|p212 Fig.5|Carboniferous|Devonian|Of Vulcan Sub-basin.||||||28-MAY-08
14166|Ningbing Group|23858|5|Briefly described|p919|||Geological Province: Bonaparte Basin.||||||
14166|Ningbing Group|24390|5|Briefly described|p2 Fig. 2, p3 Table 1|Late Devonian|Late Devonian|Geological Province: Bonaparte Basin.||||||
14166|Ningbing Group|24503|5|Briefly described|Map legend|Devonian|Devonian|Limestone reef complexes; cyanobacterial limestone, limestone breccia, shale and sandstone. Geological Province: Bonaparte Basin.||||||11-APR-08
14166|Ningbing Group|24569|5|Briefly described|p248 Fig. 3|Late Devonian|Late Devonian|Geological Province: Petrel Sub-basin.||||||
14166|Ningbing Group|40993|4|Described|p7|||Previously defined as Ningbing Limestone.||||||20-NOV-06
14166|Ningbing Group|41459|6|Mentioned|Fig.2|||||||||
14166|Ningbing Group|41532|6|Mentioned|p292|||||||||
14166|Ningbing Group|41731|5|Briefly described|p578|||See also p574.||||||20-NOV-06
14166|Ningbing Group|41864|4|Described|p85|||||||||
14166|Ningbing Group|41865|6|Mentioned|Map legend||Famennian|||||||
14166|Ningbing Group|41867|6|Mentioned|Map legend||Famennian|||||||
14166|Ningbing Group|42030|6|Mentioned|p748|||||||||
14166|Ningbing Group|42175|5|Briefly described|Fig.2 P200|||||||||
14166|Ningbing Group|42442|5|Briefly described|Fig.6 P9|||In WA and NT.||||||20-NOV-06
14166|Ningbing Group|43236|6|Mentioned|p14,Fig.13.||Late Devonian|||||||
14166|Ningbing Group|43661|6|Mentioned|Fig.3|||||||||
14166|Ningbing Group|50085|5|Briefly described|p2 Fig. 2, p3 Tb. 1||Devonian|Geological Province: Bonaparte Basin.||||||
14166|Ningbing Group|60006|5|Briefly described|Map Legend|||Geological Province: Bonaparte Basin. Unconformably overlain by Langfield Group.||||||
14166|Ningbing Group|60364|4|Described|p184|Famennian|Famennian|Equivalent to part of Buttons Formation. Geological Province: Bonaparte Basin.||||||
14166|Ningbing Group|61023|5|Briefly described|p2 Fig. 2|Late Devonian|Late Devonian|Geological Province: Bonaparte Basin.||||||17-MAR-08
14166|Ningbing Group|61542|5|Briefly described|p277 Fig. 2|Famennian|Famennian|Overlain by Langfield Group. Geological Province: onshore Bonapart Basin/Petrel-Sub-basin.||||||07-FEB-11
14166|Ningbing Group|64159|5|Briefly described|p93|Late Devonian|Late Devonian|Hosts minor dolomite-mineralisation within the limestone reef complex.||||||
14166|Ningbing Group|64580|4|Described|map legend||Late Devonian|Limestone reef complexes; cyanobacterial limestone, limestone breccia, shale, and sandstone; includes DJILLIRI, WUNGABAL, and GARIMALA LIMESTONES, and KAMILILI and BUTTONS FORMATIONS.||||||09-DEC-08
14166|Ningbing Group|64694|6|Mentioned|p232, p234 Fig.2, p245 Fig.9|Late Devonian|Devonian||||Includes Wungabal and Garimala Limestones, and Buttons Formation.|Is overlain by Milligans Formation.||
14166|Ningbing Group|65331|6|Mentioned|cross-section only|||Shown only as subsurface on cross-section, in Devonian colour.||||||
14166|Ningbing Group|69099|4|Described|500k_geologyp08_lut.csv|Late Devonian|Late Devonian||||Includes Djilliri, Wungabal,and Garimala Limestones, and Kamilili And Buttons Formations||Limestone reef complexes; cyanobacterial limestone, limestone breccia, shale, and sandstone.|03-AUG-15
14166|Ningbing Group|69165|4|Described|500k_geologyp08_lut.csv|Famennian|Frasnian||||Includes Djilliri Limestone, Wungabal Limestone, Garimala Limestone, Kamilili Formation, Buttons Formation||Undivided; limestone reef complexes; cyanobacterial limestone, limestone breccia, shale and sandstone.|
14166|Ningbing Group|69452|4|Described|p36:4; 36:6 Fig.36.5; 36:7-13, 15|Late Devonian|Late Devonian|Mory and Beere (1988); equivalent to Buttons Beds-Ningbing Limestone interval of Veevers and Roberts (1968). Divided into 5 Formations in WA; only Buttons Formation is recognised in NT where the Group is entirely subsurface; the rest is undivided. Thickness varies: 171m to 1166m; 1024m onshore (NT). Carbonate rocks deposited as a reef complex, similar to those in the Canning Basin. Lateral equivalent in part of Bonaparte Formation.|||Djilirri, Wungabal, Garimala Limestones; Kamilili, Buttons Formations.|Overlies Cockatoo Group conformably or disconformably, and Antrim Plateau Volcanics disconformably. Is overlain by Langfield Group conformably or disconformably, or by Weaber Group disconformably.|Undivided: fine-grained and lesser medium-grained limestone and dolostone with authigenic quartz; overlain by bioclastic and mottled limestone containing algal bioherms and abundant bioclastic fragments.|12-JUL-16
14166|Ningbing Group|69634|5|Briefly described|500k_geologyp08_lut.csv||Late Devonian||||Includes Djilliri Limestone, Wungubal Limestone, Garimala Limestone, Kamilili Formation and Buttons Formation.|||
14166|Ningbing Group|69653|6|Mentioned|p10, 14|Late Devonian|Late Devonian|Petrel Sub-basin. Shallow-marine to non-marine settings.||||Overlies Cockatoo Group. Is overlain by Langfield Group.|Fine-grained clastic and carbonate sediments.|
14166|Ningbing Group|69673|5|Briefly described|p167, p169, p170, p175, p177|Famennian|Famennian|Conventional petroleum potential. Sealed by Langfield Group.|||Includes Djilirri Limestone, Kamilili Formation, Wungabal Limestone, Garimala Limestone, Buttons Formation|Overlain by Langfield Group, conformably (or disconformably) overlies Cockatoo Group, disconformably overlies Antrim Plateau Volcanics|Limestone and dolostone with authigenic quartz and fossil fragments. Bioclastic and mottled limestone.|
14166|Ningbing Group|70061|5|Briefly described|Petrel Sub-basin; Fig.3|Devonian|Devonian|See also Regional geology: Fig.8, p8, p11, p13, p16. An equivalent unit in the Petrel Sub-basin includes the middle (Famennian) part of the Bonaparte Formation. Oil shows occur in onshore Bonaparte Basin. Hosts gas in Vienta 1.||||||12-JUL-16
14166|Ningbing Group|70154|5|Briefly described|500k_interpgeop14_lut.csv|Famennian|Famennian||359-372 Ma||||Limestone reef complexes; cyanobacterial limestone, limestone breccia, shale, and sandstone|
14166|Ningbing Group|70206|5|Briefly described|cross-section only|||||||Unconformably overlain by Weaber Group.||
14166|Ningbing Group|70812|6|Mentioned|p30, p38|||||||||
14166|Ningbing Group|70826|6|Mentioned|p7 tbl 3|Devonian|Devonian|Southern Bonaparte Basin.||||||
14166|Ningbing Group|70851|6|Mentioned|p17|||||||||
14166|Ningbing Group|71146|5|Briefly described|p6|Famennian|Frasnian|Bonaparte Basin.||||Overlies the Cockatoo Group. Overlain by the Buttons Formation.|Carbonates.|
14166|Ningbing Group|71267|4|Described|GEOL_LUT_CSV files|Famennian|Famennian|Of Southern Bonaparte Basin. Events: Alice Springs Orogeny (450-295 Ma); Eclipse Movement (340-300 Ma); Pertnjara-Brewer Movements (Alice Springs Orogeny phase 2) (390-360 Ma). See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|372.2-358.9 Ma (biostrat)||||Limestone reef complexes; cyanobacterial limestone, limestone breccia, shale and sandstone.|
14166|Ningbing Group|72034|5|Briefly described|500k_interpgeop16_lut|Famennian|Famennian|Southern Bonaparte Basin.  Age from biostratigraphy.|||||Limestone reef complexes; cyanobacterial limestone, limestone breccia, shale, and sandstone.|
14173|Ninmaroo Formation|8187|5|Briefly described|Map legend|Cambrian|Cambrian|Dolostone, limestone, (ooid, petoidal and echinoderm grainstone, cryptalgal boundstone, flat pebble conglomerate), dolomitic sandstone.  Overlies Georgina Limestone.||||||21-JUN-04
14173|Ninmaroo Formation|8217|5|Briefly described|Map Legend|Ordovician|Cambrian|Dolomite, minor limestone-crystalline dolostone, algal boundstone, grainstone.||||||
14173|Ninmaroo Formation|10116|5|Briefly described|Map Legend|Early Ordovician|Early Ordovician|Dolomite, micrite, grainstones, conglomerate, boundstones, limestone, sandstone.||||||
14173|Ninmaroo Formation|12891|5|Briefly described|p733 Fig. 2|Early Ordovician|Middle Cambrian|Geological province: SW Georgina Basin.||||||07-FEB-11
14173|Ninmaroo Formation|12951|5|Briefly described|p143 fig 4, p145 fig 6, p148|Early Ordovician|Late Cambrian|Georgina Basin.||||Tomahawk beds interfingers.||
14173|Ninmaroo Formation|13995|5|Briefly described|p75-76, p79|||Druce et al. (1982). Georgina Basin. Contains rostroconches (listed) in beds of Datsonian (latest Cambrian) age, and a tentative nautiloid.||||||
14173|Ninmaroo Formation|22646|6|Mentioned|p 104|Early Ordovician|Early Ordovician|Georgina Basin||||||
14173|Ninmaroo Formation|22954|4|Described|Fig1p6,p10-1,17-8|Warendan|Payntonian|Consists of Unbunmaroo, Jiggamore, Mort, Corrie and Datson Members.||||||30-JAN-07
14173|Ninmaroo Formation|23553|5|Briefly described|p2276|Ordovician|Cambrian|Geological Province: Georgina Basin.||||||
14173|Ninmaroo Formation|24065|4|Described|p235|Early Ordovician|Late Cambrian|Geological Province: Georgina Basin.  Maximum thickness: 1000m.||||||
14173|Ninmaroo Formation|24334|5|Briefly described|p48 Tb.1|Arenig|Middle Cambrian|Age: 500-485 Ma. Formation is Fmn. in text. Geological Privince: Georgina Basin.||||||20-NOV-06
14173|Ninmaroo Formation|24442|5|Briefly described|p45|Ordovician|Cambrian|Interfingers with Tomahawk Formation.||||||
14173|Ninmaroo Formation|30479|6|Mentioned|p16|||Ordovician age. See also Fig.3||||||
14173|Ninmaroo Formation|30598|6|Mentioned|p50|||||||||
14173|Ninmaroo Formation|31287|6|Mentioned|p424|||||||||
14173|Ninmaroo Formation|31572|4|Described|Fig. 1|||L.Ord.||||||
14173|Ninmaroo Formation|32576|6|Mentioned|p50|||Potential aquifer||||||
14173|Ninmaroo Formation|32952|4|Described|p1188|||Ordovician. See also pp92 and 93.||||||20-NOV-06
14173|Ninmaroo Formation|33111|4|Described|p39|||||||||
14173|Ninmaroo Formation|33482|2|Defined|Fig.4||Ordovician|||||||
14173|Ninmaroo Formation|33657|6|Mentioned|p1|||||||||
14173|Ninmaroo Formation|34252|6|Mentioned|Po.10|||Fossils||||||
14173|Ninmaroo Formation|34287|6|Mentioned|p76|||||||||
14173|Ninmaroo Formation|34454|5|Briefly described|Table 2|||Cambrian - Ordovician||||||
14173|Ninmaroo Formation|34847|6|Mentioned|Table 1 P31|||Stratigraphy and hydrocarbon prospects.||||||20-NOV-06
14173|Ninmaroo Formation|35032|6|Mentioned|p117|||||||||
14173|Ninmaroo Formation|35121|6|Mentioned|Map legend|Early Ordovician|Late Cambrian|||||||
14173|Ninmaroo Formation|35139|4|Described|Table.2|||||||||
14173|Ninmaroo Formation|35146|6|Mentioned|p469|||||||||
14173|Ninmaroo Formation|35936|6|Mentioned|p614|||||||||
14173|Ninmaroo Formation|36234|3|Fully described|p169|||See also Fig.1.||||||
14173|Ninmaroo Formation|36243|6|Mentioned|Table 1A|||||||||
14173|Ninmaroo Formation|36473|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian to Ordovician||||||
14173|Ninmaroo Formation|36580|6|Mentioned|Fig.3|||||||||
14173|Ninmaroo Formation|36645|6|Mentioned|p312|||||||||
14173|Ninmaroo Formation|37572|4|Described|p161|||See also p162 and Figs.7 and 8.||||||20-NOV-06
14173|Ninmaroo Formation|38444|5|Briefly described|p106|||||||||
14173|Ninmaroo Formation|38446|5|Briefly described|p152|||||||||
14173|Ninmaroo Formation|38532|4|Described|p231|||||||||
14173|Ninmaroo Formation|38608|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
14173|Ninmaroo Formation|39445|5|Briefly described|Table 4|||See also p61, p64 andFig.5. Included Georgina Lst on map.||||||20-NOV-06
14173|Ninmaroo Formation|39690|6|Mentioned|Fig.2|||||||||
14173|Ninmaroo Formation|39921|6|Mentioned|Map legend|Early Ordovician|Late Cambrian|Late Cambrian to Early Ordovician||||||
14173|Ninmaroo Formation|39943|6|Mentioned|Table 2B|||||||||
14173|Ninmaroo Formation|40127|6|Mentioned|p8|||||||||
14173|Ninmaroo Formation|40136|5|Briefly described|p34|||||||||
14173|Ninmaroo Formation|40810|5|Briefly described|p14|||||||||
14173|Ninmaroo Formation|40830|6|Mentioned|p12|||||||||
14173|Ninmaroo Formation|40852|6|Mentioned|Fig.3.7|||||||||
14173|Ninmaroo Formation|40906|6|Mentioned|Fig.11|||||||||
14173|Ninmaroo Formation|41524|6|Mentioned|Fig.3|||||||||
14173|Ninmaroo Formation|42058|6|Mentioned|p115|||||||||
14173|Ninmaroo Formation|42059|5|Briefly described|Fig.2 P131|||See also p134.||||||20-NOV-06
14173|Ninmaroo Formation|42060|6|Mentioned|Fig.5 P140|||||||||
14173|Ninmaroo Formation|42354|6|Mentioned|p9|Datsonian||In the Georgina Basin.||||||20-NOV-06
14173|Ninmaroo Formation|42643|6|Mentioned|p32|||Georgina Basin||||||
14173|Ninmaroo Formation|43105|5|Briefly described|Fig.4,p9.|||||||||
14173|Ninmaroo Formation|43807|6|Mentioned|Fig.2,p347|||||||||
14173|Ninmaroo Formation|43883|14|Not recorded|p18 Fig.4-3|||||||||
14173|Ninmaroo Formation|44091|14|Not recorded|p17,Tb.1,p19,21||Late Cambrian|Trempealeauan.||||||
14173|Ninmaroo Formation|44121|14|Not recorded|p5|Early Ordovician|Late Cambrian|||||||
14173|Ninmaroo Formation|44210|14|Not recorded|p7|||||||||
14173|Ninmaroo Formation|44212|2|Defined|p110,112|||||||||
14173|Ninmaroo Formation|44233|14|Not recorded|Fig.1|Early Ordovician|Late Cambrian|U.Camb-L.Ord.||||||
14173|Ninmaroo Formation|44273|14|Not recorded|Map Legend||Early Ordovician|||||||
14173|Ninmaroo Formation|44276|2|Defined|p20,27,Tb.2|||||||||
14173|Ninmaroo Formation|44291|14|Not recorded|p7|||||||||
14173|Ninmaroo Formation|44308|14|Not recorded|p5,10,Tb.1|Late Carboniferous|Tremadocian|||||||
14173|Ninmaroo Formation|44309|2|Defined|Tb.1,p9-12,16-7,map|Ordovician|Cambrian|Rests disconformably on Georgina Limestone and Mungerebar Limestone.||||||20-NOV-06
14173|Ninmaroo Formation|44310|14|Not recorded|Map Legend||Early Cambrian|||||||
14173|Ninmaroo Formation|44312|14|Not recorded|Map Legend|Ordovician|Cambrian|||||||
14173|Ninmaroo Formation|44326|14|Not recorded|Map Legend|Ordovician|Cambrian|||||||
14173|Ninmaroo Formation|44351|14|Not recorded|p15|||||||||
14173|Ninmaroo Formation|44358|6|Mentioned|p10|||||||||
14173|Ninmaroo Formation|44361|14|Not recorded|Map Legend|Ordovician|Cambrian|||||||
14173|Ninmaroo Formation|44362|4|Described|p10,Tb.1|Ordovician|Cambrian|||||||
14173|Ninmaroo Formation|44457|2|Defined|p.8, Tb.1, map|Early Ordovician|Late Cambrian|Upper Cambrian-L.Ord. SANDOVER RIVER map (F53-8).||||||20-NOV-06
14173|Ninmaroo Formation|44458|5|Briefly described|map legend|Early Ordovician|Late Cambrian|Grey dolomite, algal dolomite; pelletal dolarenite, quartzose, with some ooltihs; some sandstone and siltstone.||||||16-NOV-04
14173|Ninmaroo Formation|44469|2|Defined|p.9, Tb.I|||(F53-12). See also p.8,12-14,16. Tb.II. Overlies Arrinthrunga Fm. Laterally equivalent to lower part of Tomahawk Beds. Fossils; good aquifers.||||||30-JAN-07
14173|Ninmaroo Formation|44470|5|Briefly described|map legend|||Upper Cambrian - Lower Ordovician.||||||02-DEC-04
14173|Ninmaroo Formation|44543|2|Defined|p32-34,46|Early Ordovician|Late Cambrian|Overlies Chatsworth Limestone. Name changed from Ninmaroo Limestone to Ninmaroo Formation as dolomite becomes as prevelant as limestone and some sandstone occurs to the west of Glenormiston.||||||30-JAN-07
14173|Ninmaroo Formation|44620|14|Not recorded|p88||Tremadocian|Conodonts.||||||
14173|Ninmaroo Formation|44852|14|Not recorded|p71||Early Ordovician|||||||
14173|Ninmaroo Formation|44882|14|Not recorded|p265,287||Tremadocian|In French||||||
14173|Ninmaroo Formation|44920|14|Not recorded|Map Legend, Sheet 4|Early Ordovician|Late Cambrian|||||||
14173|Ninmaroo Formation|45002|14|Not recorded|p16,24|||Late Cambrian fossils.||||||
14173|Ninmaroo Formation|45051|5|Briefly described|p6|||Upper Cambrian - Ordovician. See also p1,4,10.||||||20-NOV-06
14173|Ninmaroo Formation|45052|2|Defined|p18|Ordovician|Cambrian|Cambrian - Ordovician||||||
14173|Ninmaroo Formation|45058|6|Mentioned|p8|||See also P23. Correlation with Pander Greensand.||||||
14173|Ninmaroo Formation|45079|6|Mentioned|p12|||Map legend on p12.||||||20-NOV-06
14173|Ninmaroo Formation|45094|3|Fully described|p11|||||||||
14173|Ninmaroo Formation|45115|6|Mentioned|p6|||||||||
14173|Ninmaroo Formation|45130|6|Mentioned|p3|||||||||
14173|Ninmaroo Formation|45166|5|Briefly described|Table 15|||||||||
14173|Ninmaroo Formation|45168|6|Mentioned|Table 1, P6|||||||||
14173|Ninmaroo Formation|46887|6|Mentioned|p251|||||||||
14173|Ninmaroo Formation|46897|6|Mentioned|p351|||See also Fig.2||||||
14173|Ninmaroo Formation|46956|6|Mentioned|p160|||||||||
14173|Ninmaroo Formation|46958|4|Described|p183|||||||||
14173|Ninmaroo Formation|46959|6|Mentioned|Table 1|||||||||
14173|Ninmaroo Formation|47024|6|Mentioned|p1|||||||||
14173|Ninmaroo Formation|47057|6|Mentioned|p554|||||||||
14173|Ninmaroo Formation|48901|14|Not recorded|Not recorded||Early Ordovician|L.Ordovician.||||||
14173|Ninmaroo Formation|48906|14|Not recorded|Tb.1,App.D|||||||||
14173|Ninmaroo Formation|48971|6|Mentioned|p42|||||||||
14173|Ninmaroo Formation|49027|4|Described|p12|||||||||
14173|Ninmaroo Formation|50100|5|Briefly described|p22|Early Ordovician|Early Ordovician|Comprises micritic limestone, intraformational breccia, dolomite, chert, mudstone and minor cross-stratified dolomitic limestone; highly fossiliferous.  Overlain by Swift Formation.||||||30-JAN-07
14173|Ninmaroo Formation|50244|5|Briefly described|p88, p89 Fig. 1, p90, p92 Fig. 3, p95|Ordovician|Cambrian|Includes; Datson, Corrie, Mort, Jiggamore and Unbunmaroo Members. Geological Province: Georgina Basin. Dolomitic. On p100 Fig. 7 also.||||||
14173|Ninmaroo Formation|60122|3|Fully described|p4-5, p24-25|Early Ordovician|Late Cambrian|Supersedes N. Limestones and N.Series (Whitehouse 1936). Includes 5 formal members not recognised in TOBERMORY. Conformable over Chatsworth Lst (absent in TOBERMORY); disconformable over Arrinthrunga Fm; interfingers with Tomahawk Fm. Max. thick: 795m.||||||19-MAY-05
14173|Ninmaroo Formation|60123|4|Described|p5|Ordovician|Cambrian|Limestone, dolostone, minor quartz sandstone. Disconformably underlies Austral Downs Limestone. Disconformably overlies: Arrinthrunga Formation. Thickness: 795m.||||||28-APR-05
14173|Ninmaroo Formation|60359|5|Briefly described|Map Legend|Ordovician|Cambrian|Calcarenite, calcilutite, breccia, limestone, marl.||||||
14173|Ninmaroo Formation|60590|5|Briefly described|Map legend|Early Ordovician|Late Cambrian|Dolostone, limestone, minor quartz sandstone.  Time equivalent of Tomahawk Formation.  Overlies the Arrinthrunga Formation; overlain by Kelly Creek Formation.||||||25-NOV-04
14173|Ninmaroo Formation|60675|5|Briefly described|Map legend|Early Ordovician|Late Cambrian|Dolostone, limestone, minor quartz sandstone.||||||
14173|Ninmaroo Formation|61404|5|Briefly described|Map legend|Early Ordovician|Late Cambrian|Of the Cockroach Group. Dolostone, limestone, minor quartz sandstone. Geological Province: southern Georgina Basin.||||||
14173|Ninmaroo Formation|62793|6|Mentioned|p272|Early Ordovician|Late Cambrian|The C. lindstromi Assemblage Zone 8 occupies an interval from 404 to 563 m above the base of Ninmaroo Formation, defining the base of the Ordovician in the Black Mountain section.|||Includes Unbunmaroo Member.|Overlies Chatsworth Limestone.||21-MAR-12
14173|Ninmaroo Formation|63450|4|Described|p76, p78 Fig. 5, p82, p83|Ordovician|Late cambrian|Conformable on Chatsworth Lst (Burke River Struct.Belt), unconformable on Arrinthrunga Fm. in W. Toko Syncline, on Georgina Fm.in E. Overlain by Swift Fm (karstified); and by Kelly Ck. Fm. Max .thickness: 950m. In Georgina Basin, East Toko Syncline.||||||07-FEB-11
14173|Ninmaroo Formation|64068|4|Described|pp72-73, p69, 71, 75, p8, 19|Early Ordovician|Late Cambrian|795 m thick in type section. Paleopoles from this and other units define a major change in APWP. Conformably and gradationally overlies and may interdigitate with Chatsworth Limestone. Laterally interdigitates with Tomahawk Formation. Conformably to disconformably overlain by Kelly Creek Formation. Formerly (Prichard 1960) included rocks now in Kelly Creek Formation.||Of Cockroach Group.|Includes Unbunmaroo, Jiggamore, Mort, Corrie and Datson Members.|Disconformably overlies Georgina Limestone, Mungerebar Limestone, Arrinthrunga Fm. Conformably overlain by Swift Formation.|Mixed-lithology limestones, dolostones; minor quartz sandstone, conglomerate. Surficial manganocrete.|05-APR-12
14173|Ninmaroo Formation|64443|6|Mentioned|p18||Late Cambrian|||||Disconformably overlies Arrinthrunga Formation.||14-MAY-14
14173|Ninmaroo Formation|64812|5|Briefly described|p237 Fig. 2|Middle Ordovician|Late Cambrian|Geological Province: southern Georgina Basin.||||||07-FEB-11
14173|Ninmaroo Formation|64813|5|Briefly described|p256 Fig. 3|Middle Ordovician|Late Cambrian|Geological Province: southern Georgina Basin. Lateral equivalent is the Tomahawk beds.||||||11-FEB-09
14173|Ninmaroo Formation|65489|5|Briefly described|p123, p125-127|Ordovician|Cambrian|Georgina Basin. Contains traces of bitumen.||||Overlies Chatsworth Limestone (conformably), and Arrinthrunga Formation and Georgina Limestone (unconformably). Is overlain by Kelly Creek Formation.||
14173|Ninmaroo Formation|67028|6|Mentioned|p371 Tb. 5|Devonian|Cambrian|Listed with Chatswood Limestone, magnetic information for unit concerning Mid-Paleozoic to Early Mesozoic pole positions for Australia is presented, sourced from the Global Palaeomagnetic Database (GPMDB; McElhinny & Lock 1993, 1996).|398-495 Ma magnetic age range|||||10-AUG-15
14173|Ninmaroo Formation|67323|5|Briefly described|GIS attrib tbl, p83, p90, p92 Fig.12.2|Ordovician|Cambrian|See also Solid Geology Map. Georgina Basin. Appears as Nimaroo Formation on p83.||Cockroach Group.||Unconformably overlies Arrinthrunga Formation and Georgina Limestone; overlies Chatsworth Limestone conformably. Is overlain by Kelly Creek Formation and Swift Formation.|Calcarenite, dolomite, limestone, oolitic and algal limestone, calcilutite.|
14173|Ninmaroo Formation|67402|5|Briefly described|p25, p25 tbl RRM3, p165 tbl LPB1|Bendigonian|Late Cambrian|Georgina Basin, Toko Syncline. Maximum thickness of 950m. Potential carbon dioxide storage reservoir, sealed by the Nora Formation. Gas has been observed in fractures from this unit. Deposited in sub-tidal to supra-tidal environments. See also p213 fig GRG3, p213 fig GRG5, p214, p215, p217.||||Unconformably overlies the Arrinthrunga Formation. Overlain by the Kelly Creek Formation.|Predominantly limestone.|
14173|Ninmaroo Formation|67870|6|Mentioned|p39, p43|Ordovician|Cambrian|Georgina Basin.||||||
14173|Ninmaroo Formation|69377|5|Briefly described|map legend|Early Ordovician|Late Cambrian|||Cockroach Group|||Calcarenite and dolomite, oolitic and algal limestone and calcilutite|
14173|Ninmaroo Formation|69437|5|Briefly described|p22:10, 15|Early Ordovician|Cambrian|Southern Georgina Basin. Hosts surficial manganocrete and pisolitic manganiferous lag.||||Overlies Arrinthrunga Formation. Is overlain by Kelly Creek Formation.||12-JUL-16
14173|Ninmaroo Formation|69443|3|Fully described|p28:7, 19, 25-27, 44|Early Ordovician|Late Cambrian|Casey (1959) after Whitehouse (1936). Southern Georgina Basin. Forms extensive tracts of smooth rounded hills to isolated low rises. Has five Members in the type section in BOULIA map area (Shergold and Druce, 1980), but these have not been identified in the NT. Up to 795m thick (in the type section). Contains a diverse fossil fauna (listed). Interdigitates with Tomahawk Formation. Open to restricted marine and emergent evaporitic carbonate sedimentation. Contains numerous sedimentary structures. Has returned locally significant manganese assay results.||Cockroach Group.||Overlies Chatsworth Limestone conformably and Arrinthrunga Formation, Georgina or Mungereba Limestones disconformably. Is overlain by Swift or Kelly Creek Formations.|Ooid, peloid, bioclast, intraclast, microbial and mixed-lithology limestone and dolostone; minor quartz sandstone and conglomerate. Microbial carbonate rocks include microbial dololaminite, stromatolitic doloboundstone and stromatolitic biostromes.|12-JUL-16
14173|Ninmaroo Formation|69458|6|Mentioned|p42:20|||||||Is overlain by Austral Downs Limestone.||14-SEP-18
14173|Ninmaroo Formation|69561|6|Mentioned|p33 fig 2|Datsonian|Payntonian|||||||
14173|Ninmaroo Formation|69591|3|Fully described|p87, p91, p93-94|Ordovician|Cambrian|Widespread unit in SE Georgina Basin. Deposited on a regional unconformity, except in the Burke River Structural Belt. Whitehouse (1936) included the thick succession of limestone at Black Mountain, Mount Ninmaroo and Mount Datson as Ninmaroo Limestone; Casey (1959) separated the lower part of the Black Mountain section as the Chatsworth Limestone, and renamed the remainder the Ninmaroo Formation to recognise the varied lithologies elsewhere. Up to 950m thick; thins westwards. Contains a rich and varied fauna (listed). Upper part is laterally equivalent to the Swift Formation which unconformably overlies it locally.||Cockroach Group.||Overlies Mungerebar, Georgina Limestones disconformably, Mount Birnie beds unconformably, and Chatsworth Limestone conformably (diachronous boundary). Conformably underlies Kelly Creek Formation.|Limestone (including oolitic, algal and echinodermal) and dolomite banks with marly, shaly, sandy and brecciated interbeds.|
14173|Ninmaroo Formation|69673|4|Described|p114 fig 92, p117, p118, p135|Ordovician|Cambrian|795m thick. Fossils includes conodonts which are the basis for age constraints. Some reservoir potential.||Cockroach Group||Conformably overlain by Kelly Creek Formation, overlies Chabalowe Formation, Arrinthrunga Formation|Ooid, peloid, bioclast, intraclast, microbial limestone and dolostone with minor quartz sandstone and conglomerate.|
14173|Ninmaroo Formation|70380|5|Briefly described|p745-746, p758-759|Tremadocian|Furongian|Southern Georgina Basin. Contains a conodont fauna very similar to that collected in Oolloo Dolostone in the Claravale area, leading to reappraisal of the age of the latter unit. Is lithologically similar to, and of an equivalent age to, the Florina Formation (Daly Basin).||||Interdigitates with Tomahawk Formation.||
14173|Ninmaroo Formation|70749|6|Mentioned|p54|||Georgina Basin, Centralian Superbasin.||Cockroach Group.||||
14173|Ninmaroo Formation|71284|5|Briefly described|p489, p492|||Black Mountain area, western Queensland.|||Unbunmaroo Member.|||
14173|Ninmaroo Formation|72297|5|Briefly described|p747-748|||Georgina Basin.|||||Includes dolomite; where exposed at the surface, is karstified.|
14173|Ninmaroo Formation|72516|6|Mentioned|p94|Ordovician|Cambrian|HAY RIVER map sheet. Georgina Basin.||||Equivalent to the Tomahawk Formation.||09-JUN-21
14173|Ninmaroo Formation|73083|6|Mentioned|p75|Early Ordovician|Late Cambrian|||||Underlain by Camooweal Dolostone.||
14235|Nora Formation|8187|5|Briefly described|Map legend|Ordovician|Ordovician|Limonitic coquina limestone, siltstone, sandstone.||||||
14235|Nora Formation|9394|5|Briefly described|Map Legend|Early Ordovician|Early Ordovician|Geological Province: Georgina Basin. Siltstone, dolomite, oolitic ironstone, sandstone. Overlies Tomahawk beds.||||||21-NOV-06
14235|Nora Formation|9694|5|Briefly described|Map Legend|Early Ordovician|Early Ordovician|Underlies Dulcie Sandstone. Overlies Tomahawk beds. Geological Province: Georgina Basin. Siltstone, dolomite, oolitic ironstone, sandstone.||||||21-NOV-06
14235|Nora Formation|10116|5|Briefly described|Map Legend|Middle Ordovician|Early Ordovician|Of the Toko Group. Siltstone, sandstone, limestone.||||||
14235|Nora Formation|12891|5|Briefly described|p733 Fig. 2|Middle Ordovician|Middle Ordovocian|Geological province: SW Georgina Basin.||||||07-FEB-11
14235|Nora Formation|12951|6|Mentioned|p143 fig 4, p145 fig 6|Middle Ordovician|Early Ordovician|Georgina Basin.||||||
14235|Nora Formation|13995|5|Briefly described|p67, p74, p76-77, p79-80, p83, p101-102|Ordovician|Ordovician|Georgina Basin. Comparatively shallow-water deposits. Three brachiopod genera are recorded, but are in need of reassessment. Contains Middle Ordovician pelecypods and gastropods, and nautiloids. Has a rich trilobite fauna (described).||||Part-equivalent to Stairway Sandstone.|Mainly interbedded siltstones, minor sandstones and limestones (coquinites).|
14235|Nora Formation|22646|6|Mentioned|p 105|Early Ordovician|Early Ordovician|In the Georgina Basin.||||||21-NOV-06
14235|Nora Formation|22954|6|Mentioned|Fig3p9|Ordovician|Ordovician|||||||
14235|Nora Formation|23214|5|Briefly described|p123|||Maggs (1963).||||||
14235|Nora Formation|23858|5|Briefly described|p924 Fig 8|Ordovician||||||||
14235|Nora Formation|24047|6|Mentioned|p105 Appendix 1|||Geological Province: Georgina Basin.||||||
14235|Nora Formation|24065|4|Described|p235|Middle Ordovician|Early Ordovician|Of Toko Group. Geological Province: Georgina Basin. Maximum thickness: 120m.||||||
14235|Nora Formation|24442|5|Briefly described|p49|||On TOBERMORY sheet.||||||
14235|Nora Formation|30983|5|Briefly described|p70|||||||||
14235|Nora Formation|31572|6|Mentioned|p21|||||||||
14235|Nora Formation|33657|6|Mentioned|p1|||||||||
14235|Nora Formation|33738|6|Mentioned|p54|||||||||
14235|Nora Formation|34252|6|Mentioned|Po.2|||Fossils.||||||21-NOV-06
14235|Nora Formation|34454|6|Mentioned|Table 2|||L.Ordovician||||||
14235|Nora Formation|34847|6|Mentioned|Table 1|||Stratigraphy and hydrocarbon prospects.||||||21-NOV-06
14235|Nora Formation|35121|6|Mentioned|Map legend|Middle Ordovician|Middle Ordovician|||||||
14235|Nora Formation|35139|4|Described|Table.2|||||||||
14235|Nora Formation|35146|6|Mentioned|p470|||||||||
14235|Nora Formation|36234|3|Fully described|p173|||||||||
14235|Nora Formation|36243|6|Mentioned|Table 1A|||||||||
14235|Nora Formation|36580|6|Mentioned|p469|||See also Fig.1||||||
14235|Nora Formation|37572|4|Described|p163|||See also p169 and Fig.8.||||||21-NOV-06
14235|Nora Formation|37727|6|Mentioned|Fig.1|||||||||
14235|Nora Formation|38832|6|Mentioned|p157|||||||||
14235|Nora Formation|39445|5|Briefly described|Table 4|||||||||
14235|Nora Formation|39921|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
14235|Nora Formation|39943|6|Mentioned|Table 2A|||||||||
14235|Nora Formation|40136|5|Briefly described|p34|||||||||
14235|Nora Formation|40538|5|Briefly described|Map legend|Early Ordovician|Early Ordovician|Siltstone; minor sandstone; oolitic ironstone. Geological Province: Georgina Basin.||||||15-NOV-05
14235|Nora Formation|40810|5|Briefly described|p14|||||||||
14235|Nora Formation|40855|6|Mentioned|p329|||||||||
14235|Nora Formation|40906|4|Described|p27|||Mention Fig.9||||||
14235|Nora Formation|41385|6|Mentioned|Fig.4|||||||||
14235|Nora Formation|41524|6|Mentioned|Fig.3|||||||||
14235|Nora Formation|42059|5|Briefly described|Fig.2 P131|||See also p134.||||||21-NOV-06
14235|Nora Formation|42060|6|Mentioned|Fig.5 P140|||||||||
14235|Nora Formation|42354|6|Mentioned|p10|||||||||
14235|Nora Formation|42504|5|Briefly described|Table 54 P79|||||||||
14235|Nora Formation|43105|5|Briefly described|Fig.4,p9.|||||||||
14235|Nora Formation|43803|6|Mentioned|Fig.5,p71|||||||||
14235|Nora Formation|43808|5|Briefly described|p294|||||||||
14235|Nora Formation|44308|14|Not recorded|p10,Tb.1||Early Ordovician|Of Toko Group.||||||
14235|Nora Formation|44309|2|Defined|Tb.1,p7,12,17,19,map|||Conformably overlies Coolibah Formation.||||||
14235|Nora Formation|44312|14|Not recorded|Map Legend||Early Ordovician|(Middle Ordovician)||||||
14235|Nora Formation|44326|14|Not recorded|Map Legend||Early Ordovician|(Middle Ordovician)||||||
14235|Nora Formation|44327|2|Defined|Tb.I,p.11,14-16,map|||(F53-11). Conformably overlies Tomahawk Beds.||||||21-NOV-06
14235|Nora Formation|44328|14|Not recorded|map legend||Ordovician|Middle Ordovician.||||||
14235|Nora Formation|44334|14|Not recorded|map legend||Ordovician|Middle Ordovician.||||||
14235|Nora Formation|44358|2|Defined|App.p18|Early Ordovician|Early Ordovician|See also p10, Tb.1. (Middle-Middle Ordovician).||||||31-MAR-09
14235|Nora Formation|44469|2|Defined|p.10, Tb.I|||(F53-12). See also p.12,13,15,16,Tb.II. Contains phosphatic beds. Fossils.||||||
14235|Nora Formation|44470|5|Briefly described|map legend||Ordovician|Middle Ordovician.||||||02-DEC-04
14235|Nora Formation|44852|14|Not recorded|p71||Ordovician|Middle Ordovician.||||||
14235|Nora Formation|44920|14|Not recorded|Map Legend, Sheet 4||Ordovician|Middle Ordovician||||||
14235|Nora Formation|45052|2|Defined|p128|Middle Ordovician|Middle Ordovician|Unit of Toko Group.||||||
14235|Nora Formation|45115|6|Mentioned|p6|||||||||
14235|Nora Formation|45118|6|Mentioned|p2,3|||||||||
14235|Nora Formation|45148|6|Mentioned|Fig.4|||In the Georgina Basin.||||||21-NOV-06
14235|Nora Formation|45155|6|Mentioned|Fig.8|||||||||
14235|Nora Formation|46841|4|Described|p104|||Also mention p97.||||||21-NOV-06
14235|Nora Formation|46897|6|Mentioned|Fig.3|||||||||
14235|Nora Formation|46956|6|Mentioned|p160|||||||||
14235|Nora Formation|46959|6|Mentioned|Table 1|||||||||
14235|Nora Formation|47024|6|Mentioned|Table 1|||||||||
14235|Nora Formation|48844|2|Defined|p.50-3||Ordovician|On many pages. p.2,16,17,47,48,50-3, F.26,58,59-62,68,69, Pl.8. M.Ordovician. (F53-11).||||||
14235|Nora Formation|48901|14|Not recorded|Not recorded||Ordovician|Middle Ordovician.  Part of Toko Group.||||||21-NOV-06
14235|Nora Formation|49027|4|Described|p17|||||||||
14235|Nora Formation|50091|6|Mentioned|p407, p413 Tb. 1|||Panderodus nogamii (conodont) found  - in Toko Range area (Qld).  Geological Province: Georgina Basin.||||||04-NOV-04
14235|Nora Formation|60122|3|Fully described|p31-32, p10 Tb. 1, p28 Fig. 33|Early Ordovician|Early Ordovician|Of Toko Group. Conformable on Kelly Cr. and Coolibah Fms; conformable below Carlo Sst and unconformable below Poodyea Fm. Max. thick: 250m. Geol.Prov: Georgina Basin.||||||21-NOV-06
14235|Nora Formation|60551|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological province: Georgina Basin.||||||
14235|Nora Formation|60590|5|Briefly described|Map legend|Early Ordovician|Early Ordovician|Of the Toko Group.  Micaceous and glauconitic siltstone, claystone, sandstone, minor dolostone; basal coquinite.  Overlies the Coolibah Formation; overlain by Carlo Sandstone.||||||21-NOV-06
14235|Nora Formation|61404|5|Briefly described|Map legend|Early Ordovician|Early Ordovician|Of the Toko Group. Micaceous and glauconitic siltstone, claystone, sandstone, minor dolostone; basal coquinite. Geological Province: southern Georgina Basin.||||||
14235|Nora Formation|62794|6|Mentioned|p289, 298, p303, 336|Early Ordovician|Early Ordovician|Georgina Basin. Overlies Coolibah Formation. Likely correlation exists between basal Nora Formation and upper Horn Valley Siltstone in Amadeus Basin, based on trilobites.||||||
14235|Nora Formation|63450|4|Described|p78 Fig. 5, p82|Arenig|Arenig|Conformably overlies Coolibah Formation; overlain conformably by Carlo Sandstone. Max. thickness: 250m. Geological province: Georgina Basin, West Toko Syncline. Basal coquinite with remainder being siltstone, mudstone and sandstone with minor dolostone.||||||07-FEB-11
14235|Nora Formation|63562|6|Mentioned|p338 fig 3, p349, p352 fig 10|Early Ordovician|Early Ordovician|Of Georgina Basin.||||Overlies Kelly Creek Formation.|Siliciclastics.|
14235|Nora Formation|64068|3|Fully described|p77, 75, 78, p19|Middle Ordovician|Middle Ordovician|Very diverse fauna.||Of Toko Group.||Conformably overlies Coolibah and Kelly Creek Formations. Conformably overlain by Carlo Sandstone or unconformably by Dulcie Sandstone.|Thin-bedded micaceous and glauconitic siltstone, claystone, fine sandstone, minor dolostone; basal bioclast grainstone-rudstone.|04-APR-12
14235|Nora Formation|64778|6|Mentioned|p13|Ordovician|Ordovician|Dulcie Syncline, Southern Georgina Basin.||||||
14235|Nora Formation|64812|5|Briefly described|p237 Fig. 2|Middle Ordovician|Middle Ordovician|Geological Province: southern Georgina Basin.||||||07-FEB-11
14235|Nora Formation|64813|5|Briefly described|p256 Fig. 3|Middle Ordovician|Middle Ordovician|Geological Province: southern Georgina Basin.||||||11-FEB-09
14235|Nora Formation|65237|5|Briefly described|p4 Fig. 7, p10|Ordovician|Ordovician|Geological province: southern Georgina Basin.||||||07-FEB-11
14235|Nora Formation|65489|5|Briefly described|p123, p125-126|Ordovician|Ordovician|Georgina Basin. Contains bitumen.||||Is overlain by Carlo Sandstone.||
14235|Nora Formation|67323|5|Briefly described|p81, p83, p90, p92 Fig.12.2|Early Ordovician|Early Ordovician|See also GIS attrib tbl, Solid Geology Map. Toko Syncline, Georgina Basin. Contains Pb, Zn and Pb-Zn anomalies 50-75km NE of Camooweal.||Toko Group||Overlies Kelly Creek Formation unconformably and Coolibah Formation conformably. Is overlain by Carlo Sandstone.|Dolomite, siltstone, fine arenite.|
14235|Nora Formation|67402|4|Described|p25 tbl RRM3, p213 fig GRG3|Castlemanian|Chewtonian|Georgina Basin. Deposited in shallow subtidal to intertidal environment or offshore below wave base. Gas has been observed from fractures of this unit. Maximum thickness of 235m. See also p213 fig GRG5, p214, p215, p216, p217, p219.||||Is laterally equivalent to or conformably overlies the Coolibah Formation. Overlain by the Carlo Sandstone.|Basal coquinite with an upper section of siltstone, mudstone and sandstone with minor dolomite.|
14235|Nora Formation|69437|5|Briefly described|p22:10|Ordovician|Ordovician|Southern Georgina Basin.||||Overlies Coolibah Formation. Is overlain by Carlo Sandstone.||12-JUL-16
14235|Nora Formation|69443|4|Described|p28:7, 27-30|Middle Ordovician|Early Ordovician|Casey in Smith (1963). Southern Georgina Basin. A recessive unit, poorly exposed. 42-250m thick. Lower part is richly fossiliferous (fauna listed). Floian to early Darriwilian age.||Toko Group.||Conformably overlies Kelly Creek and Coolibah Formations. Is overlain conformably by Carlo Sandstone, or unconformably by Dulcie Sandstone.|Thinly bedded, micaceous and glauconitic siltstone, claystone, fine sandstone and minor dolostone, with a basal bioclast grainstone-rudstone. Some siliciclastic units are rippled and cross-laminated.|12-JUL-16
14235|Nora Formation|69458|6|Mentioned|p42:20|||Georgina Basin.||||Is overlain unconformably by Poodyea Formation.||14-SEP-18
14235|Nora Formation|69591|4|Described|p87, p94-95|Ordovician|Ordovician|West Toko Syncline, Georgina Basin. Up to 120m thick. Contains a diverse fossil assemblage (listed).||Toko Group.||Overlies Coolibah Formation conformably and Kelly Creek Formation disconformably. Is overlain conformably and transitionally by Carlo Sandstone.|Sandstone and siltstone with thin grey limestone in the lower part, dark brown and grey limonitic limestone in the middle, succeeded by olive, yellow, purple and grey siltstones and green and brown fine glauconitic sandstones.|
14235|Nora Formation|69599|6|Mentioned|p600|||||||Is overlain unconformably by the Poodyea Formation.||
14235|Nora Formation|69673|4|Described|p114 fig 92, p118, p119 fig 94, p128|Ordovician|Ordovician|250m thick.||Toko Group||Overlies Coolibah Formation, overlain by Carlo Sandstone|Siltstone, claystone, sandstone and minor dolostone with a basal bioclast grainstone-rudstone.|
14235|Nora Formation|70380|6|Mentioned|p745|Darriwilian|Darriwilian|Southern Georgina Basin.||||||
14235|Nora Formation|71800|6|Mentioned|p26 fig 3|Early Ordovician|Early Ordovician|Georgina Basin.||||Overlies the Kelly Creek Formation.||
14235|Nora Formation|72297|5|Briefly described|p748|||Forms suitable cap rocks in the Toko Syncline, Georgina Basin.|||||Siltstone and mudstone.|
14235|Nora Formation|72503|6|Mentioned|p28|||Georgina Basin, Toko Ranges, far western Queensland. Histiodella serrata [conodont?] is recognised from this unit (originally referred to as Histiodella sinuosa).||||||
14253|Normanton Formation|22747|6|Mentioned|p15|||||||||
14253|Normanton Formation|23065|5|Briefly described|4, 18|||Of Rolling Downs Group.  In the Carpentaria Basin.||||||21-NOV-06
14253|Normanton Formation|23393|5|Briefly described|p24|Early Cretaceous|Early Cretaceous|Of Rolling Downs Group.||||||
14253|Normanton Formation|23425|4|Described|p378|||Of Rolling Downs Group. Underlain by Allaru Mudstone. In the Carpentaria Basin Province.||||||21-NOV-06
14253|Normanton Formation|23431|5|Briefly described|p543|||||||||
14253|Normanton Formation|23518|5|Briefly described|p13|Mesozoic|Mesozoic|Of Rolling Downs Group.  Geological Province: Carpentaria Basin.||||||
14253|Normanton Formation|23982|5|Briefly described|p58 Fig.18|||Geological Province: Carpentaria Basin.||||||
14253|Normanton Formation|24047|5|Briefly described|p11|Cretaceous|Cretaceous|Geological Province: Carpentaria Basin.||||||
14253|Normanton Formation|24073|5|Briefly described|p378 Table 2|Early Cretaceous|Early Cretaceous|Of Rolling Downs Group. Maximum thickness: 250m.  Geological Province: Carpentaria Basin.||||||
14253|Normanton Formation|24092|5|Briefly described|p8 Fig.3|||Geological Province: Carpentaria Basin.||||||
14253|Normanton Formation|30020|6|Mentioned|Fig.1|||||||||
14253|Normanton Formation|30095|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
14253|Normanton Formation|30584|4|Described|Table 1|||Also mentioned p6.||||||21-NOV-06
14253|Normanton Formation|30585|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
14253|Normanton Formation|30914|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
14253|Normanton Formation|31164|6|Mentioned|Fig. 1|||Refers Rivereau (1966).||||||
14253|Normanton Formation|31165|6|Mentioned|Table 1|||||||||
14253|Normanton Formation|31168|6|Mentioned|p10|||||||||
14253|Normanton Formation|31208|6|Mentioned|Fig. 7|||||||||
14253|Normanton Formation|31433|5|Briefly described|p6|||L.Cretaceous. Paralic||||||
14253|Normanton Formation|31434|3|Fully described|Table 1|||See also p8.||||||21-NOV-06
14253|Normanton Formation|31437|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
14253|Normanton Formation|31440|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
14253|Normanton Formation|32314|6|Mentioned|Fig. 4|||||||||
14253|Normanton Formation|32392|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
14253|Normanton Formation|32393|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
14253|Normanton Formation|32395|6|Mentioned|p6|||Stratigraphic table||||||
14253|Normanton Formation|32396|6|Mentioned|p8,9,18||Early Cretaceous|Shallow marine and paralic, correlated with Mackunda Formation.||||||
14253|Normanton Formation|33150|4|Described|p8|||L.Cret.||||||
14253|Normanton Formation|33151|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
14253|Normanton Formation|33165|6|Mentioned|Chart|||Correlation chart only||||||
14253|Normanton Formation|33175|6|Mentioned|p284|||||||||
14253|Normanton Formation|33176|6|Mentioned|p171|||||||||
14253|Normanton Formation|33177|5|Briefly described|Table 1|||||||||15-JUL-04
14253|Normanton Formation|33178|6|Mentioned|p11|||||||||
14253|Normanton Formation|33182|6|Mentioned|Fig.1|||L.Cret.||||||
14253|Normanton Formation|33183|3|Fully described|p227|||Name revised and restricted.||||||21-NOV-06
14253|Normanton Formation|33184|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
14253|Normanton Formation|33185|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
14253|Normanton Formation|33561|6|Mentioned|p102|||||||||
14253|Normanton Formation|33642|6|Mentioned|p144|||Named by Laing and Power (1959) in the Carpentaria Basin.||||||21-NOV-06
14253|Normanton Formation|33772|6|Mentioned|p13|||||||||
14253|Normanton Formation|33773|4|Described|Table 1|||See also p17.||||||21-NOV-06
14253|Normanton Formation|34356|6|Mentioned|p2|||See also p20,21,32. Lower Cretaceous.||||||21-NOV-06
14253|Normanton Formation|34811|4|Described|Table 1|||||||||
14253|Normanton Formation|35253|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
14253|Normanton Formation|35640|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
14253|Normanton Formation|35811|5|Briefly described|Table 3|||||||||
14253|Normanton Formation|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
14253|Normanton Formation|36012|3|Fully described|Table 5|||See also p18, 20.||||||21-NOV-06
14253|Normanton Formation|36228|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
14253|Normanton Formation|37608|3|Fully described|Table 1|||||||||
14253|Normanton Formation|38143|6|Mentioned|p20|||||||||
14253|Normanton Formation|39211|5|Briefly described|p36|||Fossils. Age||||||
14253|Normanton Formation|39445|5|Briefly described|Table 11|||||||||
14253|Normanton Formation|39556|5|Briefly described|Map legend|Cretaceous|Cretaceous|||||||
14253|Normanton Formation|39797|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
14253|Normanton Formation|39899|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
14253|Normanton Formation|40648|6|Mentioned|p12|||||||||
14253|Normanton Formation|41064|6|Mentioned|p62|||||||||
14253|Normanton Formation|41266|6|Mentioned|Fig.3|||||||||
14253|Normanton Formation|41307|6|Mentioned|p5|||See also p20.||||||21-NOV-06
14253|Normanton Formation|42061|5|Briefly described|p157|||See also Fig.11||||||
14253|Normanton Formation|42637|5|Briefly described|p11|||||||||
14253|Normanton Formation|43105|6|Mentioned|p16|||||||||
14253|Normanton Formation|43630|6|Mentioned|p70|||also fig.4||||||
14253|Normanton Formation|43883|14|Not recorded|p18 Fig.4-3|||||||||
14253|Normanton Formation|44031|14|Not recorded|p3,Tb.1||Cretaceous|||||||
14253|Normanton Formation|44082|6|Mentioned|p18,Tb.p34||Albian|Mentioned with respect to Qld Cretaceous fossils which are either of stratigraphic significance or are illustrative of the occurrence of a particular group.||||||
14253|Normanton Formation|44112|6|Mentioned|p82||Cenomanian|||||||
14253|Normanton Formation|44251|14|Not recorded|p4||Albian|||||||
14253|Normanton Formation|44346|14|Not recorded|opp.p5|||Equivalent of Allaru Member of Wilgunya Formation.||||||
14253|Normanton Formation|44515|2|Defined|p28||Albian|Overlain by Lynd Formation. Correlated with Kamileroi Limestone. No fossils.||||||
14253|Normanton Formation|44656|2|Defined|p325,328,Fig.48,T.10||Albian|||||||
14253|Normanton Formation|44747|14|Not recorded|p5,8,9||Albian|Contains Magoura Member (lower) Wernadinga Siltstone Member (upper). (late Albian)||||||
14253|Normanton Formation|44807|4|Described|p8-10,map||Early Cretaceous|||||||
14253|Normanton Formation|45004|14|Not recorded|p.8,14,15,28|||||||||
14253|Normanton Formation|45145|3|Fully described|Table 5|||See also p25 and Table 4.||||||21-NOV-06
14253|Normanton Formation|46791|6|Mentioned|Table 2|||||||||
14253|Normanton Formation|46872|6|Mentioned|p105|||||||||
14253|Normanton Formation|46937|6|Mentioned|Fig.10|||||||||
14253|Normanton Formation|49010|6|Mentioned|Fig.4|||In the Carpentaria Basin.||||||21-NOV-06
14253|Normanton Formation|49011|6|Mentioned|Fig.3|||In the Carpentaria Basin.||||||21-NOV-06
14253|Normanton Formation|50044|6|Mentioned|p197|||Mentioned only as a time equivalent in the Gulf of Carpentaria region.||||||
14253|Normanton Formation|62837|5|Briefly described|Stratigraphic columns|Cenomanian|Cenomanian|Of the Rolling Downs Group.  Age: ~94-~91Ma. Geological Province: Carpentaria, Bamaga and Karumba Basins.||||||01-MAR-10
14253|Normanton Formation|64820|5|Briefly described|pS6 Fig. 4, pS9|Cenomanian|Albian|Top unit of Rolling Downs Group. Underlies the bauxite of the Bulimba Formation. Med.-fine-grained glauconitic sandstone with carbonaceous intercalated phases, and siltstone. Geological province: Weipa Sub-basin, Carpentaria Basin.||||||27-AUG-18
14253|Normanton Formation|66529|6|Mentioned|p12 Fig.5, p16  |||Carpentaria Basin.||Unit in Rolling Downs Group.||Overlies Allaru Mudstone.||
14253|Normanton Formation|66915|5|Briefly described|p6 Fig.3|Late Cretaceous|Early Cretaceous|Carpentaria Basin.||||||
14253|Normanton Formation|67323|5|Briefly described|GIS attrib tbl,  p86-87, p94 Fig.12.4|Cretaceous|Cretaceous|See also Solid Geology Map. Eromanga/Carpentaria Basins. Marginal-marine sediments.||||Overlies Allaru Mudstone.|Labile sandstone, siltstone, minor mudstone and cone-in-cone limestone.|
14253|Normanton Formation|67402|5|Briefly described|p177 tbl CRP/KRM1, p181|Cenomanian|Cenomanian|Carpentaria Basin. Deposited in a paralic to shallow marine environment. Approximately 150m thick.||||Overlies the Allaru Mudstone. Overlain by the Bulimba Formation.|Glauconitic sandstone and siltstone.|
14253|Normanton Formation|67784|5|Briefly described|p26|Albian|Albian|Carpentaria Basin. Age infered from Aptian belemnites and ammonites in underlying Wallumbilla Fm||Wilgunya Subgroup.||Overlies Allaru Mudstone.||27-AUG-18
14253|Normanton Formation|68553|6|Mentioned|Map legend; schematic diagram.|Cretaceous|Cretaceous|Carpentaria Basin.||Unit in Rolling Downs Group.||Conformably overlies Polland Waterhole Shale.||
14253|Normanton Formation|68734|6|Mentioned|p221 Fig.3|Cretaceous|Cretaceous|||||||
14253|Normanton Formation|68821|6|Mentioned|p292 Fig.1|Cretaceous|Cretaceous|Lower Cretaceous age.||Of the Rolling Downs Group.||||
14253|Normanton Formation|69297|5|Briefly described|p273, p274 fig 4. 3|Upper Cretaceous|Upper Jurassic|||Rolling Downs Group||Overlies the Allaru Mudstone.|Lithic glauconitic sandstones.|
14253|Normanton Formation|69455|6|Mentioned|p39:2, 39:4 Fig.39.3|Cretaceous|Cretaceous|||||Is correlated with the onshore Yirrkala Formation.||12-JUL-16
14253|Normanton Formation|69582|6|Mentioned|p22|Upper Cretaceous|Upper Cretaceous|Eromanga Basin. Deposited in a paralic, fluvial and lacustrine environment.||||Overlies the Allaru Mudstone.||
14253|Normanton Formation|69591|6|Mentioned|p101 Fig.2.96|||||||Overlies Allaru Formation. Is overlain unconformably by Armraynald Beds.||
14253|Normanton Formation|69594|5|Briefly described|p518, p521-522, p574|Cenomanian|Aptian|Youngest deposits in the Carpentaria Basin. Upper marine to paralic deposits. Thins markedly from NE to S and W. Faunal control on age limits discussed.||Rolling Downs Group.||Conformably overlies Allaru Mudstone.||
14253|Normanton Formation|69599|5|Briefly described|p601|Cretaceous|Cretaceous|One of the hosts of the world's largest deposit of bauxite on the west coast of Cape York. Formation of the bauxite discussed.||Rolling Downs Group.|||Medium- to fine-grained glauconitic sand with common carbonaceous intercalations; deeply weathered with a typical lateritic profile containing loose, free-running pisoliths of bauxite with little or no matrix.|
14253|Normanton Formation|71863|6|Mentioned|p4-p5|Cenomanian|Albian|Carpentaria Basin. Deposited during a marine incursion.||Rolling Downs Group||||
14253|Normanton Formation|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Carpentaria Basin.||Rolling Downs Group.||Overlies Allaru Mudstone.||
14253|Normanton Formation|72799|6|Mentioned|p27|||||||||
14253|Normanton Formation|73083|6|Mentioned|p51, p54, p56, p62, p65, p68|Cretaceous|Cretaceous|Carpentaria Basin, Canobie Depression.||Rolling Downs Group|||Includes sandstone and conglomerate.|
14253|Normanton Formation|73137|6|Mentioned|p6|Cretaceous|Cretaceous|||||||
14253|Normanton Formation|73144|6|Mentioned|p8, p13|Cretaceous|Cretaceous|Carpentaria Basin. Partial aquifer. Capped by an unconformity.||Rolling Downs Group||Underlain by Allaru Mudstone.||
14253|Normanton Formation|73147|5|Briefly described|p129||Albian|||Rolling Downs Group.||Overlies Allaru Mudstone.||
14253|Normanton Formation|73553|6|Mentioned|p7|Cretaceous|Cretaceous|||||||
14401|Nungbalgarri Volcanics|22444|5|Briefly described|p 8||Archean|Age 1.72Ga.   Thermomagnetic curve shown||||||07-NOV-08
14401|Nungbalgarri Volcanics|22538|6|Mentioned|p713, Fig3 p708|||||||||22-SEP-18
14401|Nungbalgarri Volcanics|23059|5|Briefly described|639|||||||||
14401|Nungbalgarri Volcanics|23363|5|Briefly described|344 Fig.3|||||||||
14401|Nungbalgarri Volcanics|23374|1|Redefined|Tb2p10,11,41,42,27,28,32,33,36,45||Statherian|Rb-Sr age of 1648+/-29Ma. Of the Kombolgie Subgroup (Katherine River Group)  In the McArthur Basin.||||||21-NOV-06
14401|Nungbalgarri Volcanics|23384|5|Briefly described|Fig 27|||||||||
14401|Nungbalgarri Volcanics|23733|5|Briefly described|p32 Fig. 19|||Of Kombolgie Subgroup (Katherine River Group).||||||
14401|Nungbalgarri Volcanics|23867|3|Fully described|p4|Paleoproterozoic|Paleoproterozoic|Of Kombolgie Subgroup.  Includes the former Mount Callanan and Birdie Creek Volcanic Members.  Massive amygdaloidal basaltic lava, minor tuff, siltstone.  Max. thickness: 200m.   Geological Province: McArthur Basin.  See also Table1 and Figs. 3 and 30.||||||07-NOV-08
14401|Nungbalgarri Volcanics|24050|3|Fully described|p13, p10|||Of the Kombolgie Subgroup.  Vesicular and amygdaloidal basalt.  Overlies Mamadawerre Sandstone.  Overlain disconformably by Gumarrirnband Sandstone.||||||21-NOV-06
14401|Nungbalgarri Volcanics|24051|5|Briefly described|Map Legend|Statherian|Statherian|Of Kombolgie Subgroup (Katherine River Group). Geological Province: McArthur Basin.||||||21-NOV-06
14401|Nungbalgarri Volcanics|24432|5|Briefly described|p562 Fig.2|||Of the Lower Katherine River Group. Overlies Yiyintyi Sandstone. Mafic. Geological Province: Northern McArthur Basin.||||||28-JAN-05
14401|Nungbalgarri Volcanics|41957|6|Mentioned|p67|||||||||
14401|Nungbalgarri Volcanics|50545|5|Briefly described|p114 Fig.1||Paleoproterozoic|Of Kombolgie Subgroup.||||||07-NOV-08
14401|Nungbalgarri Volcanics|60571|5|Briefly described|Map legend|Statherian|Statherian|Of the Kombolgie Subgroup (Katherine River Group). Vesicular and amygdaloidal basalt. Geological Province: McArthur Basin.||||||30-NOV-04
14401|Nungbalgarri Volcanics|60680|5|Briefly described|Map legend|Statherian|Statherian|Of the Kombolgie Subgroup (Katherine River Group).  Weathered and hydrothermally altered massive and amygdaloidal basalt basalt flows. Geological Province: McArthur Basin. Overlies Mamadawerre Sandstone. Underlies Gumarrimbang Sandstone.||||||21-NOV-06
14401|Nungbalgarri Volcanics|61206|6|Mentioned|p516|||||||Overlies Mamadawerre Sandstone. Is overlain by Gumarrimbang Sandstone.|Mafic volcanic flow.|
14401|Nungbalgarri Volcanics|63866|5|Briefly described|p112, p117|||||||Equivalent to the McAddens Creek Volcanic member.||
14401|Nungbalgarri Volcanics|64698|4|Described|lithinterp table|Statherian|Orosirian|Age ~1750-1810Ma. McArthur Basin. Of Katherine River Group. Max Thickness 200m.Weathered and hydrothermally altered massive and amygdaloidal basalt flows; minor tuff and siltstone.||||||07-JAN-09
14401|Nungbalgarri Volcanics|64817|6|Mentioned|p353 Fig.4, p355 Fig.5 |||Arnhem Shelf, McArthur Basin.||Of the Kombolgie Subgroup.|||Mafic volcanics.|04-JUN-18
14401|Nungbalgarri Volcanics|65232|5|Briefly described|p7 Fig. 6, p58, p69|||Of Kombolgie Subgroup (Katherine River Group). Overlies Mamadawerre Sandstone. Altered amygdaloidal basalt. Mineralisation at Devils Elbow Prospect (U, Au and Pd) is related to fractures within.||||||09-FEB-10
14401|Nungbalgarri Volcanics|65337|6|Mentioned|p13.|||McArthur Basin. Resembles Mitchiebo Volcanics.||||||
14401|Nungbalgarri Volcanics|67057|5|Briefly described|p455 Figs.1 & 2, p462.|Paleoproterozoic|Paleoproterozoic||1780 - 1760 Ma.|Unit in Kombolgie Subgroup.||Overlies Mamadawerre Sandstone. Is overlain by Gumarrirnbang Sandstone.||
14401|Nungbalgarri Volcanics|67323|5|Briefly described|Eastern Australia Time-Space Plot|||McArthur region.||Lower Katherine River Group.||||
14401|Nungbalgarri Volcanics|67564|3|Fully described|p6 Table 2, p39 Fig.20, pp41-42.|Paleoproterozoic|Paleoproterozoic|Of Sweet et al. (1999); formerly Nungbalgarri Volcanic Member (Roberts and Plumb 1965). Includes the former Mount Callanan and Birdie Creek Volcanic Members, both of which names are now abandoned. 200 m of subaerial flows over fluviatile sediments. Has a distinctive high-K radiometric signature. Hosts U-Au-Pd at Devils Elbow, western MILINGIMBI.||Unit in Kombolgie Subgroup.||Overlies Mamadawerre Sandstone conformably. Is overlain unconformably by Gumarrirnbang Sandstone.|Altered massive and amygdaloidal basalt flows; minor tuff and siltstone.|
14401|Nungbalgarri Volcanics|67779|3|Fully described|p6 Fig.5, p8, p32, pp34-36, pp69-71.|Paleoproterozoic|Paleoproterozoic|McArthur Basin. 100-200 m thick. Subaerial volcanism; locally subaqueous. Intensely weathered; forms distinctive red-brown soils, recognisable from satellite imagery. Equivalent to McAddens Creek and Birdie Creek Volcanic Members. Has a high K-U radiometric response. Geochemistry is discussed in some detail.||Unit in Kombolgie Subgroup.||Overlies Mamadawerre Sandstone conformably. Is overlain unconformably by Gumarrirnbang Sandstone.|Trachybasalt, dacite and rhyodacite: massive flows, vesicular and amygdaloidal near top; columnar jointing: rare pillow structures; rare porphyritic olivine dolerite dykes; minor interbedded sandstone and tuffaceous siltstone.|14-MAY-18
14401|Nungbalgarri Volcanics|67873|6|Mentioned|p21|||Strongly altered in places. Would have formed a cap/seal on fluid flow.||Kombolgie Subgroup||||20-APR-18
14401|Nungbalgarri Volcanics|69420|6|Mentioned|p5:79|Paleoproterozoic|Paleoproterozoic|||Katherine River Group.||||12-JUL-16
14401|Nungbalgarri Volcanics|69430|4|Described|p15:3, 7-8, 51-52|||NW McArthur Basin. Recessive. Thickness is stated as 92m but also as "estimated to be 60m". Hosts U-Au-PGE mineralisation in fractures.||Kombolgie Subgroup.||Conformably overlies Mamadawerre Sandstone. Is overlain conformably by Gumarrirnbang Sandstone. Intruded by Oenpelli Dolerite.|Dominantly a fine-grained, equigranular, vesicular and amygdaloidal basalt; largely subaerial but with local pillows.|12-JUL-16
14401|Nungbalgarri Volcanics|69673|6|Mentioned|p16 fig 13|||Northwestern McArthur Basin.||Kombolgie Subgroup||Overlain by Gumarrirnbang Sandstone, overlies Mamadawerre Sandstone, Oenpelli Dolerite||
14401|Nungbalgarri Volcanics|70293|5|Briefly described|p597-599|||||Kombolgie Subgroup||Overlies Mamadawerre Sandstone|Mafic rocks.|
14401|Nungbalgarri Volcanics|70853|5|Briefly described|Map legend.|Statherian|Statherian|||Kombolgie Subgroup.|||Trachybasalt, dacite and rhyodacite: massive flows, vesicular and amygdaloidal near top; columnar jointing; rare pillow structures; rare porphyritic olivine dolerite dykes; minor interbedded sandstone and tuffaceous siltstone.|
14401|Nungbalgarri Volcanics|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|2474+/-16 Ma (MDA: U-Pb zircon SHRIMP)||||Basalt.|
14422|Nyanantu Formation|22538|6|Mentioned|App1 P723|||||||||
14422|Nyanantu Formation|23395|5|Briefly described|p401|||In the McArthur Basin.||||||21-NOV-06
14422|Nyanantu Formation|23396|5|Briefly described|p407 Fig.2|||Of the Tawallah Group.||||||21-NOV-06
14422|Nyanantu Formation|23398|4|Described|p440|Statherian|Statherian|Age: 1708+/-5Ma.||||||21-NOV-06
14422|Nyanantu Formation|23963|5|Briefly described|p1239 Fig.2|||Geological Province: McArthur Basin. Of the Tawallah Group.||||||21-NOV-06
14422|Nyanantu Formation|24050|6|Mentioned|p27|||Geological Province: McArthur Basin.||||||
14422|Nyanantu Formation|42700|5|Briefly described|map legend|Paleoproterozoic||Variation on Nyanantu beds.||||||07-NOV-08
14422|Nyanantu Formation|42739|5|Briefly described|map legend|Statherian|Statherian|Coarse grained pebbly sandstone and cobble boulder conglomerate; immature, poorly sorted.||||||19-OCT-05
14422|Nyanantu Formation|42812|2|Defined|p80|Proterozoic||Probable age 1713 +/- 6Ma. See also p27.||||||21-NOV-06
14422|Nyanantu Formation|43036|3|Fully described|p37|||||||||
14422|Nyanantu Formation|44112|6|Mentioned|p35|||||||||
14422|Nyanantu Formation|60483|5|Briefly described|p7 Fig. 5, p29|Paleoproterozoic|Paleoproterozoic|Of the Tawallah Group. Age: 1708+/-5Ma. Geological Province: McArthur Basin.||||||07-NOV-08
14422|Nyanantu Formation|63112|6|Mentioned|p1191 Fig.2, p1192 Tb.1|||Calvert Superbasin.|1708 +/- 5 Ma.|Unit in Big Supersequence.|||Polymict conglomerate, lithic sandstones, and coarse volcaniclastics.|
14422|Nyanantu Formation|63866|5|Briefly described|p54|||||Prize Supersequence||||
14422|Nyanantu Formation|64815|6|Mentioned|p4 Fig.2, p5 Fig.3 |||||Of the Tawallah Group.||||
14422|Nyanantu Formation|64817|6|Mentioned|p353 Fig.4, p355 Fig.5 |Statherian|Statherian||1708 +/- 5 Ma.|Of the Tawallah Group.||||
14422|Nyanantu Formation|65228|5|Briefly described|p23, Figs.02, 04, 05, 07, 10.|Statherian|Statherian|Mis-spelt as Nynantu on p23. Southern McArthur Basin. Epiclastics associated with Tanumbirini Rhyolite. Fig.02 implies this unit should no longer be part of Tawallah Group.|1708 +/- 5 Ma.|||Overlies Tanumbirini Rhyolite and Warramana Sandstone.||08-JAN-18
14422|Nyanantu Formation|65340|5|Briefly described|p12, p53 Fig.51. |||Variety of depositional environments including alluvial and debris flow, local braid-delta and proximal braided fluviatile..|1708 +/- 5 Ma detrital age.|Unit in Tawallah Group.||Overlies Tanumbirini Rhyolite and, unconformably, Warramana Sandstone. Is overlain by Burash Sandstone.||
14422|Nyanantu Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||McArthur region.|1708 +/- 5 Ma (maximum depositional age).|||||
14422|Nyanantu Formation|69430|4|Described|p15:3, 9-10, 13|||Southern McArthur Basin. 450m thick. Fluvial and alluvial fans deposits. Is correlated with Echo Sandstone. SHRIMP U-Pb detrital zircon maximum deposition age.|1708 +/- 5 Ma (Page et al., 2000).|Tawallah Group.||Conformably or disconformably overlies Warramana Sandstone and (is also interbedded with) Tanumbirini Rhyolite. Is overlain conformably by Burash Sandstone and ?disconformably by Masterton Sandstone.|Lithic conglomeratic sandstone with numerous pebble- and cobble-rich intervals.|12-JUL-16
14422|Nyanantu Formation|69673|6|Mentioned|p16 fig 13, p17 fig 14|||Coarse clastic sedimentary rock.||Tawallah Group||Overlain by Burash Sandstone, overlies Tanumbirini Rhyolite, Warramana Sandstone||
14422|Nyanantu Formation|71592|5|Briefly described|Appendix A.|||McArthur Basin.|1708+/-5 Ma (MDA: U-Pb zircon SHRIMP)||||Conglomerate.|
14422|Nyanantu Formation|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Urapunga Fault Zone, Beetaloo Sub-basin, Batten Fault Zone and Southeastern McArthur Basin.||Tawallah Group|Diagram suggests includes Tanumbinini Rhyolite.|Partially overlies Warramana Sandstone and Pungalina Member and underlies Burash Sandstone.||
14422|Nyanantu Formation|72718|6|Mentioned|p7|||Southern McArthur Basin.||Tawallah Group||Partly overlain by Burash Sandstone. Partly underlain by Warramana Sandstone. Partly underlain by and equivalent to Tanumbirini Rhyolite. Equivalent to Echo Sandstone.||
14422|Nyanantu Formation|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Beetaloo Sub-basin and the Batten Fault Zone in the Southern McArthur Basin. U-Pb zircon sedimentary depositional age (Ma).|1708+/-5 Ma.|Tawallah Group|Tanumbinini Rhyolite ?|Overlies Warramana Sandstone and partially overlies Pungalina Member, underlies Burash Sandstone and partially equivalent to Echo Sandstone.||
14422|Nyanantu Formation|73042|6|Mentioned|p4|Statherian|Statherian|Southern McArthur Basin, Calvert Superbasin. Geochronology is a U-Pb zircon sedimentary depositional age (?maximum depositional age).|1708 +/- 5 Ma (see Fig.1.2)|Tawallah Group||Partly(?) underlain by Warramana Sandstone and Tanumbinini Rhyolite. Partly overlain by Burash Sandstone.||
14422|Nyanantu Formation|73412|5|Briefly described|p2, 4, 8|||Southern McArthur Basin. Appears mis-spelt as Nyantu Formation on p2.|1708 +/- 5 Ma (SHRIMP: Page and Sweet, 1998).|||Overlies Tanumbirini Rhyolite and Warramana Sandstone. Is overlain unconformably by Masterton Sandstone (McArthur Group).||
14496|Oenpelli Dolerite|9534|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Porphyritic olivine dolerite, ophitic dolerite, granophyric dolerite, serpentinite. Intrudes the Nourlangie Schist.||||||17-JUN-09
14496|Oenpelli Dolerite|9538|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Olivine dolerite and differentiates. Age: >1650Ma.||||||17-JUN-09
14496|Oenpelli Dolerite|9691|5|Briefly described|Map Legend|||Porphyritic olivine dolerite, ophitic dolerite, granophyric dolerite and differentiates; serpentinite.||||||
14496|Oenpelli Dolerite|9701|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Porphyritic olivine dolerite, ophitic dolerite, granophyric dolerite and differentiates; serpentinite.||||||02-JUN-05
14496|Oenpelli Dolerite|9733|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Porphyritic olivine dolerite, olivine dolerite, quartz dolerite, granophyric dolerite and granophyre.||||||
14496|Oenpelli Dolerite|22538|6|Mentioned|P713||Statherian|Age of unit is 1688+/-13 Ma.||||||21-NOV-06
14496|Oenpelli Dolerite|22600|6|Mentioned|Map legend|||||||||
14496|Oenpelli Dolerite|22808|6|Mentioned|7 fig 4|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
14496|Oenpelli Dolerite|23374|3|Fully described|p19-20, Fig3p5,9,27,28,32,33,35,36,46||Statherian|Age: 1688+/-13Ma. In the McArthur Basin.||||||28-MAR-18
14496|Oenpelli Dolerite|23867|5|Briefly described|p3|Paleoproterozoic|Paleoproterozoic|Age: 1688+/-13Ma.||||||07-NOV-08
14496|Oenpelli Dolerite|23937|6|Mentioned|p47|Statherian|Statherian|Age: 1688Ma (Carson et al, 1999).||||||
14496|Oenpelli Dolerite|24048|6|Mentioned|p5 Fig. 3|||||||||
14496|Oenpelli Dolerite|24049|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|In regional setting map legend.||||||07-NOV-08
14496|Oenpelli Dolerite|24050|3|Fully described|p30, p9 Tb. 2|Paleoproterozoic|Paleoproterozoic|Fine- to coarse-grained dolerite. Intrudes the Marlgowa Sandstone.||||||28-MAR-18
14496|Oenpelli Dolerite|24051|5|Briefly described|Map Legend|Statherian|Statherian|Geological Province: McArthur Basin.||||||
14496|Oenpelli Dolerite|24181|5|Briefly described|p83|Statherian|Statherian|N-NE trending mafic dykes. Age: ~1690 Ma. Geological Province: Pine Creek Inlier.||||||
14496|Oenpelli Dolerite|24197|5|Briefly described|p132|||Continental tholeiite. Age: <1870Ma. Geological province: Pine Creek Inlier.||||||07-FEB-11
14496|Oenpelli Dolerite|24340|5|Briefly described|p148|Mesoproterozoic|Mesoproterozoic|Age: 1688 +/- 13 Ma. Geological Province: Pine Creek Inlier.||||||
14496|Oenpelli Dolerite|29423|5|Briefly described|p305|||||||||
14496|Oenpelli Dolerite|30142|6|Mentioned|p13|||Fig. on this page.||||||
14496|Oenpelli Dolerite|30863|6|Mentioned|p50|||||||||
14496|Oenpelli Dolerite|31833|6|Mentioned|Table 2|||||||||
14496|Oenpelli Dolerite|32959|6|Mentioned|PP1|||Stratigraphy||||||
14496|Oenpelli Dolerite|33084|4|Described|Table 1|||||||||
14496|Oenpelli Dolerite|33085|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
14496|Oenpelli Dolerite|33186|4|Described|p292|||Re lithology||||||
14496|Oenpelli Dolerite|35114|6|Mentioned|p204|||||||||
14496|Oenpelli Dolerite|35140|6|Mentioned|p320|||||||||
14496|Oenpelli Dolerite|35165|6|Mentioned|Fig.2|||||||||
14496|Oenpelli Dolerite|35465|6|Mentioned|p54|||Stratigraphy||||||
14496|Oenpelli Dolerite|35950|6|Mentioned|p303|||||||||
14496|Oenpelli Dolerite|36085|6|Mentioned|p502|||Intended as informal.||||||
14496|Oenpelli Dolerite|36473|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
14496|Oenpelli Dolerite|36475|6|Mentioned|p59|||||||||
14496|Oenpelli Dolerite|36535|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
14496|Oenpelli Dolerite|36635|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
14496|Oenpelli Dolerite|37462|4|Described|Table 4.II|||||||||
14496|Oenpelli Dolerite|37579|5|Briefly described|Map legend|Carpentarian|Carpentarian|Olivine dolerite, commonly porphyritic; minor quartz dolerite and granophyre.||||||10-OCT-05
14496|Oenpelli Dolerite|37815|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
14496|Oenpelli Dolerite|38239|6|Mentioned|p9|||||||||
14496|Oenpelli Dolerite|38349|4|Described|p15|||||||||
14496|Oenpelli Dolerite|38351|4|Described|p12|||||||||
14496|Oenpelli Dolerite|38557|6|Mentioned|p287|||||||||
14496|Oenpelli Dolerite|38884|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
14496|Oenpelli Dolerite|39048|6|Mentioned|p824|||||||||
14496|Oenpelli Dolerite|39357|4|Described|p17|||||||||
14496|Oenpelli Dolerite|39563|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
14496|Oenpelli Dolerite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
14496|Oenpelli Dolerite|39801|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Olivine dolerite and differentiates.||||||07-NOV-08
14496|Oenpelli Dolerite|39924|6|Mentioned|p349|||||||||
14496|Oenpelli Dolerite|40104|6|Mentioned|p336|||||||||
14496|Oenpelli Dolerite|40105|6|Mentioned|p321|||See also Fig.7||||||
14496|Oenpelli Dolerite|40168|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Olivine dolerite and differentiates.||||||07-NOV-08
14496|Oenpelli Dolerite|40223|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Olivine dolerite and differentiates.||||||07-NOV-08
14496|Oenpelli Dolerite|40243|6|Mentioned|p139|||||||||
14496|Oenpelli Dolerite|40248|6|Mentioned|p221|||||||||
14496|Oenpelli Dolerite|40823|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
14496|Oenpelli Dolerite|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
14496|Oenpelli Dolerite|41125|6|Mentioned|p15|||||||||
14496|Oenpelli Dolerite|41146|5|Briefly described|p858|||||||||
14496|Oenpelli Dolerite|41147|5|Briefly described|p1153|||||||||
14496|Oenpelli Dolerite|41295|6|Mentioned|p5|||||||||
14496|Oenpelli Dolerite|41304|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
14496|Oenpelli Dolerite|41305|5|Briefly described|Fig.4|||||||||
14496|Oenpelli Dolerite|41311|4|Described|p21|||||||||
14496|Oenpelli Dolerite|41397|4|Described|p18|||||||||
14496|Oenpelli Dolerite|41406|6|Mentioned|Map legend|Mesoproterozoic||||||||
14496|Oenpelli Dolerite|41407|6|Mentioned|Map legend|Proterozoic||||||||
14496|Oenpelli Dolerite|41465|6|Mentioned|p12|||||||||
14496|Oenpelli Dolerite|41586|6|Mentioned|Map legend|||||||||
14496|Oenpelli Dolerite|41594|5|Briefly described|p74|||||||||
14496|Oenpelli Dolerite|41601|6|Mentioned|p42|||||||||
14496|Oenpelli Dolerite|41649|5|Briefly described|p66|||||||||
14496|Oenpelli Dolerite|41957|5|Briefly described|p67|||||||||
14496|Oenpelli Dolerite|42012|6|Mentioned|p30|||||||||
14496|Oenpelli Dolerite|42110|5|Briefly described|p131|||||||||
14496|Oenpelli Dolerite|42372|5|Briefly described|p18|||||||||21-NOV-06
14496|Oenpelli Dolerite|43010|6|Mentioned|p41|||||||||
14496|Oenpelli Dolerite|43187|5|Briefly described|p2|||||||||
14496|Oenpelli Dolerite|43292|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
14496|Oenpelli Dolerite|43595|6|Mentioned|p75|||Emplaced at 1.69 Ga.||||||21-NOV-06
14496|Oenpelli Dolerite|43624|6|Mentioned|Fig.32,p38|||Age: 1680 Ma||||||
14496|Oenpelli Dolerite|43719|5|Briefly described|p31|||||||||
14496|Oenpelli Dolerite|43832|4|Described|66,69,97||Mesoproterozoic|Age: 1690 Ma (rb-Sr). Occurs as dykes and lopoliths.||||||17-JUN-09
14496|Oenpelli Dolerite|44112|6|Mentioned|Fig3p8|||||||||
14496|Oenpelli Dolerite|45121|6|Mentioned|p7|||||||||
14496|Oenpelli Dolerite|46639|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Age: 1688+/-13Ma. Porphyritic to ophitic olivine dolerite, quartz dolerite, granophyric dolerite and differentiates.||||||07-NOV-08
14496|Oenpelli Dolerite|46658|6|Mentioned|p559|||||||||
14496|Oenpelli Dolerite|46675|5|Briefly described|Map legend for regional setting...|Paleoproterozoic|Paleoproterozoic|Olivine dolerite and differentiates. Age: >1650Ma. Geological Province: Pine Creek Geosyncline.||||||17-JUN-09
14496|Oenpelli Dolerite|46700|5|Briefly described|P28, Table1 P8||Carpentarian|Age of unit is 1688 Ma.||||||21-NOV-06
14496|Oenpelli Dolerite|46824|6|Mentioned|Table 1|||See also p321.||||||21-NOV-06
14496|Oenpelli Dolerite|46874|3|Fully described|p125|||||||||
14496|Oenpelli Dolerite|47049|6|Mentioned|Fig.3|||||||||
14496|Oenpelli Dolerite|50545|4|Described|p113||Paleoproterozoic|Age: 1723+/-6 Ma. 220-250 m thick sheet intrudes Myra Falls Metamorphics and separates Lower Schist from the Footwall Amphibolite.||||||17-JUN-09
14496|Oenpelli Dolerite|50586|6|Mentioned|p2.1|||Intrudes: Nimbuwah Complex.||||||
14496|Oenpelli Dolerite|60526|5|Briefly described|Map Legend|Carpentarian|Carpentarian|Olivine dolerite and differentiates.||||||
14496|Oenpelli Dolerite|60550|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Porphyritic olivine dolerite, ophitic dolerite, granophyric dolerite and differentiates.||||||
14496|Oenpelli Dolerite|60571|5|Briefly described|Map legend|Statherian|Statherian|Medium- to coarse-grained ophitic dolerite, minor felsic differentiates. Geological Province: McArthur Basin.||||||30-NOV-04
14496|Oenpelli Dolerite|60573|6|Mentioned|Regional Setting legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
14496|Oenpelli Dolerite|60680|5|Briefly described|Map legend|Statherian|Statherian|Fine to coarse, porphyritic and equigranular olivine dolerite, ophitic dolerite.  Age: 1723Ma.  Geological Province: McArthur  Basin.||||||13-JAN-05
14496|Oenpelli Dolerite|61206|5|Briefly described|p516, p517 Fig.1|Early Proterozoic|Early Proterozoic|Appears as Oenpelli dolerite in Fig.2.|1720 Ma (Kyser et al., 2000).||||A very extensive gabbroic intrusion; sills to 250 m thick.|
14496|Oenpelli Dolerite|61403|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|In regional setting map legend.||||||07-NOV-08
14496|Oenpelli Dolerite|61561|5|Briefly described|p531|Paleoproterozoic|Paleoproterozoic|Intrudes the Gumarrirnbang Sandstone. Age: 1688+/-13Ma.||||||07-NOV-08
14496|Oenpelli Dolerite|62375|5|Briefly described|p8 Table 1, 9 table 2.|Neoproterozoic|Paleoproterozoic|Layered tholeiitic dolerite lopoliths. Age: 1720Ma. Thickness: <250m. Geological Province: Pine Creek Orogen.||||||09-FEB-10
14496|Oenpelli Dolerite|63866|5|Briefly described|p112, p124||||1723 +/- 6 ma (Page, OZCHRON)|||Intrudes the Katherine River Group.||
14496|Oenpelli Dolerite|64698|4|Described|lithinterp table|Statherian|Statherian|Age 1720Ma SHRIMP U/Pb. Max thickness 175m. Fine to coarse, porphyritic and equigranular olivine dolerite, ophitic dolerite.||||||07-JAN-09
14496|Oenpelli Dolerite|64725|5|Briefly described|p74.|Paleoproterozoic|Paleoproterozoic||c.1690 Ma (Hein 2002).||||Mafic dykes.|
14496|Oenpelli Dolerite|64730|6|Mentioned|p126|Statherian|Statherian|Marks close of the Top End Orogeny of Needham et al. (1988).|1723 +/- 6 Ma (Page 1996).|||||03-MAY-12
14496|Oenpelli Dolerite|64817|6|Mentioned|p353 Fig.4, p354 |Statherian|Statherian||1730 Ma (SHRIMP zircon: Kyser et al., 2000).|Of the Kombolgie Subgroup.||||
14496|Oenpelli Dolerite|64956|6|Mentioned|p64, p93|||Intrudes Nourlangie Schist. Faulted against by Tin Camp Granite.||||||07-FEB-11
14496|Oenpelli Dolerite|65232|5|Briefly described|p24, p7-8|Statherian|Statherian|Several large lopolithic sills and dykes of olivine dolerite, quartz dolerite and granophyre intruded orogenic rocks and Kombolgie Subgroup at 1725 - 1720 Ma (OZCHRON, Kyser et al 2001 and 2000) causing hornsfelsing. Thickness of sills: up to 250m.||||||09-FEB-10
14496|Oenpelli Dolerite|65339|6|Mentioned|p5 Fig.4. ||||||||Mafic intrusive rocks.|
14496|Oenpelli Dolerite|65340|6|Mentioned|p93.|||Northern Arnhem Shelf. Interpreted deeper-level feeder of the stratigraphically-higher Settlement Creek Dolerite.||||||
14496|Oenpelli Dolerite|66526|5|Briefly described|p36.|Proterozoic|Proterozoic|Pine Creek Province. Produced in the Oenpelli Event, ME 12 in the Proterozoic Mafic-Ultramafic Magmatic Event Series.|c.1720 Ma.|||||
14496|Oenpelli Dolerite|66683|5|Briefly described|p368 Fig.3, p369.|||Series of flat-lying sills and laccoliths emplaced into Paleoproterozoic strata and Kombolgie Subgroup.|c.1723 Ma.|||||
14496|Oenpelli Dolerite|67057|5|Briefly described|p454, p455 Fig.1, p457, p463. |Paleoproterozoic|Paleoproterozoic|Is prevalent in the King River uranium prospect in the Nimbuwah Domain.|1723 +/- 6 Ma (Edgecombe et al. 2002).|||Intrudes Katherine River Group.||
14496|Oenpelli Dolerite|67323|5|Briefly described|Eastern Australia Time-Space Plot, p34|Paleoproterozoic|Paleoproterozoic|Pine Creek area.|Emplaced 1688 +/- 13 Ma.|||||
14496|Oenpelli Dolerite|67355|6|Mentioned|p5, p23, p40|Statherian|Statherian|Date from OZCHRON database.|1723 +/- 6 Ma (conventional U-Pb baddeleyite)||||Dolerite lopolith intrusion.|25-JAN-17
14496|Oenpelli Dolerite|67564|3|Fully described|p iv, p6 Table 2, p10 Fig.5, p50.|Statherian|Statherian|A thick (to 175 m) symmetrically differentiated, layered, lopolithic sill. Forms prominent ridges to 150 m high; elsewhere forms distinctive red-brown soils with dense vegetation. High magnetic susceptibility. Type locality is a prominent ridge along Graveside Gorge.|1723 +/- 6 Ma.|||Intrudes Katherine River Group, Jim Jim Granite, Nourlangie Schist, Mount Bonnie Formation, Burrell Creek Formation, Zamu Dolerite.|Equigranular, ophitic subalkaline olivine dolerite, porphyritic at margins.|
14496|Oenpelli Dolerite|67779|3|Fully described|p6 Fig.5, p8 Table 1, p20, pp38-40, p108|Paleoproterozoic|Paleoproterozoic|Nimbuwah Domain, Pine Creek Orogen. Type section is a prominent ridge along Graveside Gorge. Up to 250 m thick. Thought to consist of four major and one minor lopoliths. Includes porphyritic gabbroic rocks intruding the former Myra Falls Metamorphics, described by Dunn (1962), and mafic rocks in the Oenpelli area (Bryan, 1962); the name was introduced provisionally by Needham et al. (1974). Geochemistry is discussed in some detail.|1723 +/- 6 Ma (Ferenczi and Sweet, 2005).|||Intrudes Nourlangie Schist.|Porphyritic olivine doleritic sills, ophitic dolerite, granophyric dolerite, serpentinite; textures vary from massive, equigranular, fine-grained dolerite to coarse-grained gabbroic assemblages.|
14496|Oenpelli Dolerite|69420|5|Briefly described|p5:5, 26, 67, 69-71, 79, 81, 90|Paleoproterozoic|Paleoproterozoic|Lopoliths emplaced at 1-2km depth in rocks which had previously been buried to mid-to-deep crustal levels during the c.1865 Ma Nimbuwah Event. Continuous over tens of kilometres, and are 500-1500m thick. Brief discussion of reliability of this U-Pb baddeleyite age.|1723 +/- 6 Ma (Ferenczi and Sweet, 2005).||||A series of sub-alkaline and differentiated sills of porphyritic to ophitic olivine dolerite, minor olivine-plagioclase cumulates that locally define rhythmic layering, and narrow discontinuous granophyric dolerite within zones of quartz dolerite.|12-JUL-16
14496|Oenpelli Dolerite|69430|4|Described|p15:3, 7-9, 51-52|||Defined by Needham et al. (1975); later formalised and described in detail by Smart et al. (1974, 1975) and Stuart-Smith and Ferguson (1978). NW McArthur Basin. Zoned sills and lopoliths. Represents continental tholeiite. Previously thought to be overlain unconformably by Kombolgie Subgroup. Page et al. (1980) determined a Rb-Sr age of 1688 +/- 13 Ma. A more recent determination gives intrusion at 1725-1720 Ma (OZCHRON, Polito et al., 2004).|1725-1720 Ma.|Kombolgie Subgroup.||Intrudes Nungbalgarri Volcanics, Marlgowa Sandstone (Kombolgie Subgroup) and Nimbuwah Complex.|Fine- to coarse-grained olivine dolerite, commonly porphyritic; quartz dolerite, granophyre.|12-JUL-16
14496|Oenpelli Dolerite|69577|6|Mentioned|p113-114|Paleoproterozoic|Paleoproterozoic||1723 +/- 6 Ma (Page, 1996).|||Intrudes Kombolgie Subgroup.||
14496|Oenpelli Dolerite|69673|6|Mentioned|p16 fig 13|||||Kombolgie Subgroup||Overlain by Nungbalgarri Volcanics||
14496|Oenpelli Dolerite|70284|6|Mentioned|p1258|||||||||
14496|Oenpelli Dolerite|70293|6|Mentioned|p620|Statherian|Statherian|Intrudes the Kombolgie Sub-basin.|1720 Ma.|||||
14496|Oenpelli Dolerite|70853|5|Briefly described|Map legend.|Statherian|Statherian||||||Medium- to coarse-grained porphyritic olivine dolerite sills, ophitic dolerite, granophyric dolerite, serpentinite.|
14496|Oenpelli Dolerite|71374|5|Briefly described|p34|Statherian|Statherian|Pine Creek Orogen. Isotopic age is interpreted as the crystallisation age for this unit.|1735 +/- 3 Ma (TIMS U-Pb Baddeleyite)|||||
14496|Oenpelli Dolerite|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|1723.0+/-6 Ma (crystallisation: baddeleyite U-Pb).||||Dolerite.|
14496|Oenpelli Dolerite|71632|5|Briefly described|Map legend.|||McArthur Basin.||Lower Katherine River Group.|||Dolerite sills and dykes.|
14496|Oenpelli Dolerite|72706|6|Mentioned|p4, p17|||From drillhole 19NBDD002  located at MGA94 (Zone 53) 317944mE 8638644mN, south of the Nabarlek Mine. Drilled to test an IP anomaly and also designed to test lower contact of the Oenpelli Dolerite. Stratigraphy not explicitly logged.|||||Pyroxene-plagioclase-chlorite dolerite-gabbro in this hole.|
14550|Oliver Formation|5952|5|Briefly described|p214 Fig. 4, p215 Fig. 5, p229|Pliocene|Miocene|In figure, Fm = Formation. Includes Oliver Sand Member. Geological Province: Bonaparte Basin. Composed of firm to moderately hard calcarenites with abundant skeletal material.||||||01-MAR-10
14550|Oliver Formation|7142|6|Mentioned|p350 Fig.4.|Neogene|Neogene|Browse Basin.||||Overlies Cartier Formation. Is overlain by Barracouta Formation.||
14550|Oliver Formation|13353|6|Mentioned|p401 Fig.2.|Neogene|Neogene|||||Overlies Cartier Formation. Is overlain by Barracouta Formation.||
14550|Oliver Formation|13354|6|Mentioned|p375 Fig.6.|Neogene|Neogene|Unit of Woodbine Group. Overlies Cartier Formation and underlies Barracouta Formation.||86||||28-OCT-14
14550|Oliver Formation|22663|5|Briefly described|AC97 1-4 Fig.4||Miocene|Of the Woodbine Group.||||||01-MAR-10
14550|Oliver Formation|23377|4|Described|p212 Fig.5; p218|Quaternary|Miocene|In the Vulcan Sub-basin. Unconformable base.||||||21-NOV-06
14550|Oliver Formation|24171|5|Briefly described|p722 Fig. 3|Tertiary|Tertiary|Geological Province : Vulcan Sub-Basin.||||||01-MAR-10
14550|Oliver Formation|24218|5|Briefly described|p847|Early Miocene|Early Miocene|Geological Province: Bonaparte Basin.||||||
14550|Oliver Formation|42053|5|Briefly described|Fig.2 P29|||See also Fig.2||||||01-MAR-10
14550|Oliver Formation|42066|5|Briefly described|Fig.3 P199|||||||||01-MAR-10
14550|Oliver Formation|60634|6|Mentioned|p1168 Fig.3. |Miocene|Miocene|||Unit in Woodbine Group.||Overlies Prion Formation. Is overlain by Barracouta Formation.||
14550|Oliver Formation|61548|6|Mentioned|p480 Fig.3|Miocene|Miocene|Northern Bonaparte Basin.||||||
14550|Oliver Formation|61550|6|Mentioned|p495 Fig.2. |||||Unit in Woodbine Group.||Is overlain by Barracouta Formation.||
14550|Oliver Formation|62837|5|Briefly described|Stratigraphic columns|Late Miocene|Oligocene|Contains the Oliver Sand Member. Age: ~25-~7.0Ma. Geological Province: Western Bonaparte Basin and Northern Bonaparte Basin.||||||01-MAR-10
14550|Oliver Formation|63358|5|Briefly described|p4 Fig. 1.3|Miocene|Miocene|||||||01-MAR-10
14550|Oliver Formation|64695|5|Briefly described|p260-262  |Miocene|Miocene|Northern Bonaparte Basin.|||Includes Oliver Sandstone Member.|Unconformably overlies Prion and Hibernia Formations. Is overlain by Barracouta Formation.||
14550|Oliver Formation|64697|5|Briefly described|p84 Fig.2 |Miocene|Miocene|||||||
14550|Oliver Formation|65680|6|Mentioned|p709 Fig.2.|Messinian|Aquitanian|Host to an interpreted dish-shaped, multiringed impact structure, about 2.5 km diameter, formed by collision of a meteorite or small asteroid with unconsolidated, water-saturated shallow-marine shelf carbonate, in mid- to late-Serravallian.|||Includes Oliver Sandstone Member.|Overlies Cartier Formation. Is unconformably overlain by Barracouta Formation.||
14550|Oliver Formation|66187|5|Briefly described|p413 Fig.2, p414 Tb.1, p421, p423|Miocene|Oligocene|Unit in Woodbine Group. Underlies Barracouta Formation (WA), overlies the Prion Formation unconformably. In the Mount Ashmore Dome. Mainly limestone and dolomite.||||||
14550|Oliver Formation|68223|6|Mentioned|p178 Fig.3, p179 Fig.4, p184 Fig.9|Miocene|Miocene|In Fig. 9, the base of Pliocene is indicated by the Top Oliver Formation.||||||
14550|Oliver Formation|69297|6|Mentioned|p305|Messinian|Chattian|Caswell, Barcoo and Seringapatam Sub-basins of the Browse Basin.||Woodbine Group||Overlies the Cartier Formation. Overlain by the Barracouta Shoal Formation.||
14550|Oliver Formation|69452|5|Briefly described|p36:15, 22|Neogene|Neogene|Bonaparte Basin.||Woodbine Group.||||12-JUL-16
14550|Oliver Formation|69673|6|Mentioned|p174|||||||||
14550|Oliver Formation|70061|5|Briefly described|Regional geology; Figs.6-7, p12|Miocene|Oligocene|See also Sahul: Fig.2, p2. Vulcan: Fig.2, p2. Reservoir. Sealed by intraformational carbonates or the overlying Barracouta Shoal Formation.||Woodbine Group.|Oliver Sandstone Member.|Overlies Cartier Formation. Is overlain by Barracouta Shoal Formation.||12-JUL-16
14550|Oliver Formation|70064|5|Briefly described|Regional Fig. 6. Central: Fig.2|Miocene|Oligocene|See also Northern: Fig.2. Yampi: Fig.2. Browse Basin.||Woodbine Group.|Oliver Sandstone Member.|Overlies Cartier Formation. Is overlain by Barracouta Shoal Formation.||12-JUL-16
14563|Olympic Formation|14019|6|Mentioned|p19|||Geological Province: Amadeus Basin.  Correlated with Fargoo Tillite (Grey and Corkeran, 1998).||||||
14563|Olympic Formation|22506|6|Mentioned|p130 Fig.4|Neoproterozoic III|Cryogenian|||||||
14563|Olympic Formation|22560|6|Mentioned|p2|||||||||
14563|Olympic Formation|22561|5|Briefly described|p24|Neoproterozoic|Neoproterozoic|||||||
14563|Olympic Formation|22566|4|Described|p81|Neoproterozoic|Neoproterozoic|Stratigraphic relations described from a number of localities - p81.  Type section mentioned, thickness and distribution discused - p81.||||||
14563|Olympic Formation|22567|6|Mentioned|Fig 1 on p92|||||||||
14563|Olympic Formation|22646|6|Mentioned|Fig 1 on p 98|Neoproterozoic|Neoproterozoic|||||||
14563|Olympic Formation|22648|4|Described|p 127 - 132|Neoproterozoic|Neoproterozoic|||||||13-NOV-06
14563|Olympic Formation|22649|4|Described|p 143|Neoproterozoic|Neoproterozoic|At the type section for the Gaylad Sandstone the Olympic Formation is 36 meters thick,  the Olympic Formation is overlain by Gaylad Sandstone and underlain by the Loves Creek Member of the Bitter Springs Formation.||||||21-NOV-06
14563|Olympic Formation|22651|6|Mentioned|Fig 11 btw p182-183|Proterozoic|Proterozoic|||||||
14563|Olympic Formation|22762|5|Briefly described|p374|Neoproterozoic|Neoproterozoic|||||||
14563|Olympic Formation|22804|5|Briefly described|p440|Neoproterozoic|Neoproterozoic|||||||
14563|Olympic Formation|22816|5|Briefly described|p10 Fig. 4|Neoproterozoic|Neoproterozoic|In the Amadeus Basin.||||||21-NOV-06
14563|Olympic Formation|22826|4|Described|p570|Neoproterozoic|Neoproterozoic|||||||
14563|Olympic Formation|23250|5|Briefly described|p1124  Fig.2||Cryogenian|Correlate of Whyalla Sandstone and Wilmington Formation equivalent and Elatina Formation, Yaltipena Formation and Trezona Formation (Umberatana Group). Geological province: Amadeus Basin.||||||21-NOV-06
14563|Olympic Formation|23287|6|Mentioned|Fig.4|||Age: Upper Cryogenian. In the Amadeus Basin.||||||21-NOV-06
14563|Olympic Formation|23314|5|Briefly described|333 Fig.4|Neoproterozoic III||Geological province: Amadeus Basin.||||||16-NOV-06
14563|Olympic Formation|23361|5|Briefly described|16 Fig.4|Neoproterozoic III|Cryogenian|||||||
14563|Olympic Formation|23557|5|Briefly described|p95 Fig.1|Neoproterozoic III|Neoproterozoic III|Geological Province: Amadeus Basin.||||||
14563|Olympic Formation|23806|5|Briefly described|p1122 Fig. 1|Neoproterozoic|Neoproterozoic|||||||
14563|Olympic Formation|24111|5|Briefly described|p216|Neoproterozoic|Neoproterozoic|Geological Province: Amadeus Basin. See also p215 Fig. 11.||||||
14563|Olympic Formation|24442|6|Mentioned|p38|||Geological Province: Centralian Superbasin.||||||
14563|Olympic Formation|35805|5|Briefly described|p36|||See also Fig.3.||||||
14563|Olympic Formation|35863|6|Mentioned|Table 1|||||||||
14563|Olympic Formation|36898|6|Mentioned|p181, p195 Fig. 4, p198|||Red, silty, dolomitic. Geological province: eastern Amadeus Basin.||||||16-NOV-06
14563|Olympic Formation|37462|4|Described|Table 4.IX|||||||||
14563|Olympic Formation|37928|3|Fully described|p517|||||||||
14563|Olympic Formation|37929|6|Mentioned|Fig.2|||||||||
14563|Olympic Formation|38157|6|Mentioned|Table VI|||||||||
14563|Olympic Formation|38885|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
14563|Olympic Formation|38945|6|Mentioned|p130|||Includes diamictites. Geological Province: Amadeus Basin (NT).||||||16-NOV-06
14563|Olympic Formation|39565|6|Mentioned|p32|||||||||
14563|Olympic Formation|39583|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
14563|Olympic Formation|39898|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Diamictite, overlain by green shale with scattered boulders. Geological Province: Amadeus Basin.||||||14-FEB-06
14563|Olympic Formation|40740|4|Described|p12|||||||||
14563|Olympic Formation|40810|6|Mentioned|p3|||||||||
14563|Olympic Formation|40852|6|Mentioned|p24 Fig. 3.2, p29|Adelaidean|Adelaidean|Geological province: Amadeus Basin.  Correlation with Wilpena Group in the Adelaide Geosyncline is suggested (Preiss et al 1978).||||||16-NOV-06
14563|Olympic Formation|40906|6|Mentioned|Fig.9|||||||||
14563|Olympic Formation|41005|6|Mentioned|p419 Fig.2|||Age: Marinoan. Geological Province: Amadeus Basin in NT.||||||16-NOV-06
14563|Olympic Formation|41039|6|Mentioned|Fig.2|||||||||
14563|Olympic Formation|41190|6|Mentioned|Fig.4|||||||||
14563|Olympic Formation|41270|6|Mentioned|Table 1|||||||||
14563|Olympic Formation|41405|5|Briefly described|p205|||Capped by laminated pink dolomite identical to that of Nuccaleena Fm. Incl: upper lenticular boulder tillite, gritty pebbly dolomite; lower red siltstone with interbedded lenses of dark limestone and gritty to pebbly limestone. Geol. prov: Amadeus Basin.||||||16-NOV-06
14563|Olympic Formation|41429|5|Briefly described|p246|||Thin laminated pink to buff dolomite capping Marinoan tillites.  Geological province: Amadeus Basin.  Equivalent to Nuccaleena Formation.||||||16-NOV-06
14563|Olympic Formation|41618|6|Mentioned|Fig.2|||Glacigenic unit. geological province: Amadeus Basin.||||||22-NOV-06
14563|Olympic Formation|41717|6|Mentioned|Fig.2|||||||||
14563|Olympic Formation|41801|6|Mentioned|Fig.4|||||||||
14563|Olympic Formation|41852|6|Mentioned|p210|||||||||
14563|Olympic Formation|42059|6|Mentioned|Fig.2 P131|||||||||
14563|Olympic Formation|42082|6|Mentioned|Fig.3 P323|||||||||
14563|Olympic Formation|42504|5|Briefly described|p72|||||||||
14563|Olympic Formation|42643|6|Mentioned|p21|||In the Amadeus Basin.||||||21-NOV-06
14563|Olympic Formation|42845|6|Mentioned|Fig.3 P498|||||||||
14563|Olympic Formation|42886|5|Briefly described|Fig.2 P219|||see also Fig.1 p218.||||||21-NOV-06
14563|Olympic Formation|42940|5|Briefly described|Plate 2|Neoproterozoic|Neoproterozoic|Diamictite, sandstone, shale, limestone.  Geological province: Amadeus Basin.||||||23-JAN-08
14563|Olympic Formation|43105|5|Briefly described|Fig.3,p8|||||||||
14563|Olympic Formation|43503|6|Mentioned|11-50|||from Ediacaran to||||||
14563|Olympic Formation|43595|5|Briefly described|p548, p549 Fig5-33|Adelaidean|Adelaidean|Age: 660-680 Ma. Geological province: Amadeus Basin.||||||16-NOV-06
14563|Olympic Formation|43756|6|Mentioned|p542|||||||||
14563|Olympic Formation|44111|6|Mentioned|p.58 Fig. 2|||in Amadeus Basin, presented as "Olympic" only in Fig. 2.||||||
14563|Olympic Formation|46865|6|Mentioned|p43|||Upgraded p51.||||||21-NOV-06
14563|Olympic Formation|46903|6|Mentioned|p54|||||||||
14563|Olympic Formation|49796|4|Described|p1 & Sections|||||||||
14563|Olympic Formation|60549|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Diamictite overlain by green shale.||||||
14563|Olympic Formation|60682|5|Briefly described|p19|Neoproterozoic|Neoproterozoic|Geological Province: Amadeus Basin.||||||03-MAY-05
14563|Olympic Formation|61309|5|Briefly described|p16 Fig. 4|||Geological Province: Amadeus Basin.||||||06-FEB-08
14563|Olympic Formation|61732|3|Fully described|p4 Fig. 3, p91-92.|Cryogenian|Cryogenian|Glacigenic rocks orginally defined as Olympic Member (Pertatataka Fm), but now upgraded to formation status. Unconformably on Aralka Fm. Max. thickness: 300m. Geol.Prov: Amadeus Basin. See also p5 Tb. 1, p31, p87.||||||07-FEB-11
14563|Olympic Formation|62085|6|Mentioned|p24|Ediacaran|Ediacaran|Amadeus Basin. The base of the cap carbonate at the top of this unit corresponds with the Ediacaran GSSP.||||Intertongues with Gaylad Sandstone.||
14563|Olympic Formation|62376|5|Briefly described|p18|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin.||||||09-FEB-10
14563|Olympic Formation|62453|5|Briefly described|p12 Fig. 8|Ediacaran|Cryogenian|Geological Province: Amadeus Basin.||||||
14563|Olympic Formation|62903|5|Briefly described|p729, p730|||Amadeus Basin. Very thin stratigraphic thickness of Aralka Formation preserved in Wallara-1 (~27m) may be a lacuna unconformity between the Aralka and Olympic Formations. Presented as Olympic in figure.||||overlies hiatus overlying Aralka Formation, abrupt contact in drillcore; interpreted as Marinoan (Yerelina Subgroup) equivalent (Walter et al. 2000).|glacial|
14563|Olympic Formation|62984|5|Briefly described|p13|Cryogenian|Cryogenian|Geological Province: Amadeus Basin. Representative of the Marinoan glacial episode.||||||23-JAN-07
14563|Olympic Formation|63458|6|Mentioned|p873, p897 Fig.19, p900. |Cryogenian|Cryogenian|Amadeus Basin.||||Overlies Aralka Formation. Correlated with Fargoo Tillite.||
14563|Olympic Formation|63562|5|Briefly described|p338 fig 3, p343-344, p352 fig 10|Ediacaran|Ediacaran|Of Amadeus Basin.|||||Includes (Marinoan) diamictites.|
14563|Olympic Formation|64068|6|Mentioned|p46|||Amadeus Basin.  Correlated with Sun Hill Arkose, Little Burke Tillite, Black Stump Arkose, Wonnadinna Dolostone, Oorabra Arkose, Boko Formation, southern Georgina Basin.||||||
14563|Olympic Formation|64103|6|Mentioned|p404|||Geological Province: Amadeus Basin.||||||07-FEB-11
14563|Olympic Formation|64625|5|Briefly described|p243, p245, p247, p252, p256-257|||Amadeus Basin. Correlated with Marinoan glacial event. Lithology, C and O isotopes detailed.||||Overlies Bitter Springs Formation, and Aralka Formation unconformably. Unconformably overlain by Gaylad Sandstone.|Green mudstone, pebbly sandstone and conglomerate, breccia, dolomite beds and diamictite; thin-bedded sandstone and dolomite, massive chert-bearing dolomite.|
14563|Olympic Formation|64778|6|Mentioned|p13|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
14563|Olympic Formation|64797|6|Mentioned|p153 Fig.2, p164 Fig.11|Ediacaran|Ediacaran|Amadeus Basin. Rank not shown in diagram; shown as Olympic Boord.||||||
14563|Olympic Formation|64809|5|Briefly described|p3 Fig.2, p15 Fig.15 |Proterozoic|Proterozoic||||||Dolostone, conglomerate, sandstone.|
14563|Olympic Formation|65233|3|Fully described|p3 Fig. 2, p6|Neoproterozoic|Neoproterozoic|Tog. with Pioneer Sst. disconformably overlies Aralka Fm.Max. thickness: 190m. Geol.prov: Amadeus Basin. Lenticular units of sst., siltst., conglom/diamictite, shale+dolostone in NE of basin. Lateral equiv. is Pioneer Sandstone.||||||07-FEB-11
14563|Olympic Formation|65272|6|Mentioned|p320 Fig.3||Ediacaran|||||||
14563|Olympic Formation|65365|5|Briefly described|p10 Fig. 4|Ediacaran|Cryogenian|Amadeus Basin||||||
14563|Olympic Formation|65366|5|Briefly described|p23 Fig. 3|Ediacaran|Cryogenian|Amadeus Basin||||||
14563|Olympic Formation|65410|6|Mentioned|p74.|Neoproterozoic|Neoproterozoic|Amadeus Basin. Part of Supersequence 3.||||||
14563|Olympic Formation|66767|5|Briefly described|p60|Neoproterozoic|Neoproterozoic|NE Amadeus Basin. 190m thick. The diamictite is associated with the Marinoan glaciation.||||Disconformably overlies Aralka Formation. Is overlain unconformably by Gaylad Sandstone.|Red and green siltstone and sandstone, pebbly arkose and conglomerate, and dark red-brown diamictite.|
14563|Olympic Formation|67326|5|Briefly described|p2|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||Overlies Aralka Formation. Is overlain by Pioneer Sandstone.||
14563|Olympic Formation|67484|6|Mentioned|p294 Tb.1|Cryogenian|Cryogenian|Amadeus Basin.||||Overlain by the Pertatataka Formation. Underlain by the Aralka Formation.||
14563|Olympic Formation|67565|6|Mentioned|p5 Fig.3.|||Amadeus Basin.||||||
14563|Olympic Formation|67620|6|Mentioned|p5|Cryogenian|Cryogenian|Amadeus Basin.||||Overlies Aralka Formation. Is overlain by Pertatataka Formation.||
14563|Olympic Formation|67856|5|Briefly described|p338 fig 4-30, p345|Neoproterozoic|Neoproterozoic|Shown as equivalent to Pioneer Sandstone.||||Underlies Pertatataka Formation.||
14563|Olympic Formation|68244|6|Mentioned|p671|||Amadeus Basin.||||||
14563|Olympic Formation|68270|4|Described|p679,682-683,685-688|Cryogenian|Cryogenian|Amadeus Basin. Type section occurs 8 km SE of Ringwood Homestead; lat. 23'54"S, long.,134'59"E. Restricted to the NE Amadeus Basin. Less than 200m thick. Periglacial: fluvial to marginal marine deposit. Clasts are mainly fine-coarse pebbles, range up to boulder size in the upper parts of the formation. Clasts are mostly rounded and consist of quartzite, granite, gneiss, carbonate and basalt; some are faceted. Includes a paraconformable, up to 30m thick (4m in type section) "upper marker cap dolomite" intersected in type area, and is related to Elatina glaciation. Correlable to Elatina Formation, Nuccaleena Formation.||||Overlain by Pertatataka Formation, Underlain disconformably by Aralka Formation.|Red and green mudstone and siltstone with intercalated sandstone, diamictite, siltstone, conglomerate and dolomite (which generally overlie conglomerate).|03-JUL-19
14563|Olympic Formation|68276|5|Briefly described|p68, 73|Neoproterozoic|Neoproterozoic|Amadeus Basin. The ""Formation"" is omitted.",,||||Is overlain conformably by Pertatataka Formation.|Glaciogenic deposits, overlain by seafloor barite associated with ferruginous domal stromatolites.|
14563|Olympic Formation|68277|6|Mentioned|p95|Neoproterozoic|Neoproterozoic|The rank is not given in the text.||||||
14563|Olympic Formation|68323|6|Mentioned|p4 Fig.2|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
14563|Olympic Formation|68473|6|Mentioned|p531|||Amadeus Basin.||||||
14563|Olympic Formation|68733|5|Briefly described|p188, p189 Fig.8|Cryogenian|Cryogenian|Amadeus Basin.|||||Diamictites.|05-DEC-17
14563|Olympic Formation|69031|6|Mentioned|p4, p9|||Amadeus Basin. Formerly part of Boord Formation (name discontinued).||||||
14563|Olympic Formation|69437|5|Briefly described|p22:4-5, 7|Cryogenian|Cryogenian|NE Amadeus Basin, Centralian A Superbasin. Supersequence 3.||||Overlies Aralka Formation. Is overlain by Gaylad Sandstone. Is equivalent to Pioneer Sandstone.|Diamictite, siliciclastic rocks and dolostone.|12-JUL-16
14563|Olympic Formation|69438|4|Described|p23:2-5, 16-19, 43|Ediacaran|Cryogenian|Priess et al. (1978); previously the Olympic Member of the Pertatataka Formation (Wells et al., 1967). Amadeus Basin. Up to 190m thick. Has been correlated with the diamictite member of the Mount Doreen Formation (Ngalia Basin); Oorabra Arkose, Boko Formation, Black Stump Arkose (Georgina Basin); Chambers Bluff Tillite (Officer Basin). The "cap dolostone" has been correlated with the Nuccaleena Dolostone (Adelaide Fold Belt).||||Disconformably overlies Aralka Formation. Lateral equivalent of Pioneer Sandstone. Is overlain disconformably by Pertatataka Formation.|Lenticular units of sandstone, siltstone, conglomerate, diamictite, shale and dolostone. Near the top is a pale brown and pink gritty dolostone ("upper marker cap dolomite") which is a laminated, thinly bedded interval up to 30m thick.|12-JUL-16
14563|Olympic Formation|69439|6|Mentioned|p24:8|||Amadeus Basin.||||Correlated with Mount Davenport Diamictite Member.||12-JUL-16
14563|Olympic Formation|69441|6|Mentioned|p26:1|||Amadeus Basin.||||Correlated with Moonlight Valley Tillite (Wolfe Basin).||12-JUL-16
14563|Olympic Formation|69442|6|Mentioned|p27:4|||Amadeus Basin.||||Correlated with Fargoo Tillite (Wolfe Basin).||12-JUL-16
14563|Olympic Formation|69443|5|Briefly described|p28:8|||Adelaide Fold Belt. Glacigene and post-glacial deposits related to the Elatina (previously Marinoan) glaciation.||||Equivalent to Keepera Group (Georgina Basin).||12-JUL-16
14563|Olympic Formation|69606|5|Briefly described|p1, p4 fig 2, p5, p6 fig 3, p7 fig 4|Cryogenian|Cryogenian|Supersequence 3. <100m thick. Potential reservoir and seal rock. Amadeus Basin. Poorly exposed. Glacigene origin, inferred to have been deposited during the Elatina glaciation. Previously the Olympic Member of Wells et al, 1967.  See also p12, p13 fig 7, p14, p19.||||Overlies the Aralka Formation, overlain by the Pertatataka Formation. Inferred to be equivalent to the Pioneer Sandstone.|The dominant lithology is siltstone with interbedded sandstone, while conglomerate, lesser dolostone and reddish glacial diamictite with striated and faceted clasts as smaller components.|
14563|Olympic Formation|69673|5|Briefly described|p63, p64 fig 53, p88, p91|||Potential reservoir rock.||||Overlain by Pioneer Sandstone, disconformably overlies Aralka Formation|Diamictite, siliciclastic rocks and dolostone.|
14563|Olympic Formation|69937|4|Described|v Fig.1, vi, p3 Tb.1, p17-19, p22, p26|Neoproterozoic|Neoproterozoic|See also p45-46. NE Amadeus Basin. Formerly the Olympic Member of Pertatataka Formation (Wells et al., 1967). A potential equivalent to the Pioneer Sandstone. Correlated with the ~640 Ma to ~580 Ma Elatina glacial succession. Likely zircon provenance discussed.|690 +/- 14 Ma (maximum depositional age).|||Disconformably overlies Areyonga and Aralka Formations. Is overlain unconformably by Waldo Pedlar Member (Pertatataka Formation). Lateral equivalent of Pioneer Sandstone.|Lenticular units of sandstone, siltstone, conglomerate, diamictite, shale and dolostone.|
14563|Olympic Formation|70018|5|Briefly described|p235|Neoproterozoic|Neoproterozoic|Amadeus Basin. Of Supersequence 3 in the northern Amadeus Basin. Equivalent to Pioneer Sandstone. Correlable to Inindia Beds in the southern Amadeus Basin.||||Overlain by Pertatataka Formation. Underlain by Aralka Formation.||
14563|Olympic Formation|70416|5|Briefly described|p63, p65, p68, p72, p74, p80|Cryogenian|Cryogenian|Deposited during the Elatina Glaciation. Contains reworked stromatolite Tungussia inna from the underlying Aralka Formation.||||Unconformably overlies Aralka Formation. Is overlain by Pertatataka Formation. Laterally equivalent to Pioneer Sandstone.||
14563|Olympic Formation|70839|5|Briefly described|p329|Neoproterozoic|Neoproterozoic|Of Amadeus Basin.||||Overlain by Pertatataka Formation. Underlain by Aralka Formation. Equivalent to Pioneer Sandstone.||
14563|Olympic Formation|71001|5|Briefly described|p18 Fig.2, p19-21, 23, 27-28|Cryogenian|Cryogenian|Amadeus Basin. Glacial deposits. Cap carbonate is dominated by manganiferous dolomite. Carbon isotope correlation graph.||||Overlies Aralka Formation. Is overlain by Gaylad Sandstone.|Glacial sandstone; cap carbonate.|
14563|Olympic Formation|71080|5|Briefly described|p27, p29 fig 20, p30|Cryogenian|Cryogenian|Amadeus Basin. Supersequence 3. Includes glacial diamictites?|||||Diamictite, sandstone and lesser conglomerate.|
14563|Olympic Formation|71088|6|Mentioned|p8|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
14563|Olympic Formation|71279|5|Briefly described|p355 Fig.2, p382 Tb.1|Ediacaran|Cryogenian|Amadeus Basin. Modelled magnetic properties.||||||
14563|Olympic Formation|71344|5|Briefly described|p1094, 1096-1100, 1102-3|||Amadeus Basin.  Glaciogenic succession. Top commonly marked by a pink cap carbonate that in some places contains small columnar stromatolites.||Of Inindia Package.||Unconformably overlies the Aralka Formation. Equivalent to Pioneer Sandstone. Is overlain conformably by Pertatataka Formation.|Conglomerates, diamictites, sandstones, shales and carbonates.|10-NOV-17
14563|Olympic Formation|71592|5|Briefly described|Appendix A.|||Amadeus Basin.|690+/-14 Ma (MDA: U-Pb zircon SHRIMP)||||Coarse-grained feldspathic sandstone.|
14563|Olympic Formation|71801|6|Mentioned|p230-p231, p237|Ediacaran|Ediacaran|Amadeus Basin.||||Overlies the Aralka Formation.||
14563|Olympic Formation|71810|5|Briefly described|Map legend.|Ediacaran|Cryogenian|Amadeus Basin (Phase 1), Centralian Superbasin.|||||Diamictite, sandstone, conglomerate, and siltstone; large erratics; common glacially faceted and striated clasts.|
14563|Olympic Formation|71841|5|Briefly described|p1|Ediacaran|Cryogenian|Of Amadeus Basin.||||Equivalent to Pioneer Sandstone. Grades into Inindia beds.||
14563|Olympic Formation|71842|5|Briefly described|p1-3,9|Ediacaran|Ediacaran|Of Amadeus Basin. Nomenclature after Edgoose 2013 (NE Amedeus, NT). Generally confined to the NE Amadeus Basin, and disappears from outcrop westward from central northern margin.||||Equivalent with Pioneer Formation. Overlain by Pertatataka Formation. Underlain by Aralka Formation. Correlable with Winnall beds.||
14563|Olympic Formation|72369|5|Briefly described|p7,9-10|||Of Amadeus Basin.||||Underlain disconformably by Aralka Formation.||
14563|Olympic Formation|72375|4|Described|p1-2,19-23,25|Neoproterozoic|Neoproterozoic|Of Amadeus Basin. Formerly known as Olympic Member of the Pertatataka Formation (Wells et al., 1967). Redefined (Priess et al 1978). Restricted to the NE Amadeus Basin, and can be correlated with Elatina glacial successions of the Adelaide Rift Complex and the Georgina, Ngalia and Officer basins (Lindsay 1993, Walter et al 1995). SHRIMP U-Pb zircon analyses by Kositcin et al., 2015 yielded an interpreted maximum depositional age (pooled 238U/206Pb) of 690+\-14 Ma. LA-ICP-MS Hf isotopic signatures for the zircon age populations from NTGS RD13CJE001 (feldpsathic quartz sandstone) suggest they crystallised in magmas derived from a range of crustal sources (see p21-22 for Hf isotopic results and interpretations). Sample location and description is provided.||||Overlain unconformably by Gaylad Sandstone or Pertatataka Formation. Underlain disconformably by Aralka Formation. Laterally correlable (interfingers with) to Pioneer Sandstone.|Lenticular units of sandstone, siltstone, conglomerate, diamictite, shale and dolostone.|04-DEC-19
14563|Olympic Formation|72489|5|Briefly described|p3, p4 Fig.3|Cryogenian|Cryogenian|Amadeus Basin.||||Unconformably overlying Aralka Formation.|Includes glacial deposits and also stromatolitic bioherms, oolitic grainstone, intraclast breccia, and packstone.|
14563|Olympic Formation|72601|5|Briefly described|p: 1, 3-5, 7-8, 11-12, 14, 16, 19, 24-25|Cryogenian|Cryogenian|Amadeus Basin. Deposition was coeval with the Elatina glaciation. Renamed from the Olympic Member. Previously part of the Pertatataka Formation prior to redefinition by Preiss et al. (1978).||||Unconformably underlain by Aralka Formation. Overlain by Pertatataka Formation. Equivalent to Pioneer Sandstone. Correlates to Cottons Breccia.||
14563|Olympic Formation|73085|6|Mentioned|p1, p27|Ediacaran|Ediacaran|Previously thought to occur in drillhole BR05DD01 as what is now considered Areyonga Formation. [Unclear relationship with Pioneer Sandstone].||||Underlain by Aralka Formation. Partly overlain by[?] Pertatataka Formation unconformably. Partly overlain by[?] and equivalent to[?] Gaylad Sandstone. Equivalent to Inindia beds.||
14563|Olympic Formation|73086|1|Redefined|[See comments].|Cryogenian|Cryogenian|[Redefined herein. See also definition card, ASUD]. Added type area. Glaciogenic. Amadeus Basin. Part of Supersequence III. Diamictite includes intrabasinal clasts (i.e., Heavitree Formation, Bitter Springs Group, Aralka Formation, Areyonga Formation and less basement rock clasts than seen in Areyonga Formation diamictite). Can be difficult to distinguish from the Areyonga Formation based on lithology alone. When the diamictite is absent, it is difficult to differentiate from the Waldo Pedlar Member of the Pertatataka Formation. Cap carbonate is not ubiquitous. Lateral equivalent of the Pioneer Sandstone; less widely recognised in the subsuface than Pioneer Sandstone. Previously a member of the Pertatataka Formation. Age constrained by correlation with Chambers Bluff Tillite (Rb-Sr age of 651 +/- 87 Ma) and the ca 660-635 Ma Marinoan glaciation, supported by a 690 +/- 14 Ma detrital zircon maximum depositional age. No known fossils other than poorly preserved stromatolites. May preserve the Cryogenian-Ediacaran boundary. Partly overlain by [and equivalent to?] Gaylad Sandstone. Correlates with Mount Doreen Formation, Elatina Formation, Nuccaleena Formation, Oorabra Arkose, Black Stump Arkose, Boko Formation, Chambers Bluff Tillite, Pioneer Sandstone. p: 3, 5-6, 27-28, 53-54, 63, 67, 71-72, 79, 91, ~99-114, 118-123, 143, 160, 167-169, App 2.|ca. 650 Ma|||Unconformably underlain by Gillen and Johnnys Creek formations (Bitter Springs Group) and Aralka Formation. Unconformably overlain by Pertatataka Formation. [See comments for more].|Glacial deposits including lenticular diamictite, sandstone, siltstone, conglomerate, boulder clay, and dolostone in varying proportions with rapid lateral variation in thickness and lithology.|
14563|Olympic Formation|73088|6|Mentioned|p1|Cryogenian|Cryogenian|Amadeus Basin, northeast.||||Unconformably underlain by Aralka Formation. Overlain by Gaylad Sandstone. Equivalent to Pioneer Sandstone.||
14563|Olympic Formation|73180|4|Described|p47-48 p52-54|Neoproterozoic|Neoproterozoic|Amadeus Basin. Defined by Preiss et al (1978). Elatina glacial/post-glacial sequences. Outcrop limited to the northeast of the basin and the Boord Ridges. Disconformable contact with Bitter Springs Group in the north and northeast of the basin from erosion by a grounded ice sheet, deposition of thin sandstones and conglomerates from localised high-energy deposition, likely glacial outwash.||||Equivalent to the Pioneer Sandstone, disconformably overlies the Aralka Formation, conformably underlies the Pertatataka Formation.|Glaciogenic suite of lenticular diamictites, polymict conglomerates, pebbly arkosic sandstones, siltstones and mudstones with interbedded and overlying pink, commonly stromatolitic dolostones. Includes reworked carbonates.|
14590|One Tree 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
14590|One Tree Granite|37413|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
14590|One Tree Granite|37862|4|Described|p584|||||||||
14590|One Tree Granite|38310|6|Mentioned|p237|||||||||
14590|One Tree Granite|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
14590|One Tree Granite|38900|6|Mentioned|p55|||||||||
14590|One Tree Granite|39445|5|Briefly described|Table 2|||||||||
14590|One Tree Granite|40840|6|Mentioned|Map legend|||||||||
14590|One Tree Granite|45161|4|Described|p27|||||||||
14590|One Tree Granite|45166|6|Mentioned|p10|||||||||
14590|One Tree Granite|49009|2|Defined|p31|Paleoproterozoic|Paleoproterozoic|Previously mapped as Kalkadoon Granite (Carter and Opik,1963).||||||07-NOV-08
14590|One Tree Granite|49041|5|Briefly described|Table 2|||||||||
14590|One Tree Granite|50100|5|Briefly described|p16|Proterozoic|Proterozoic|Of the Kalkadoon Batholith.  Overlain unconformably by Leichhardt Volcanics.||||||
14590|One Tree Granite|50536|5|Briefly described|p1.4 Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Kalkadoon Suite.||||||07-NOV-08
14590|One Tree Granite|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Pale to dark biotite granite, commonly porphyritic and foliated.||||||
14590|One Tree Granite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map., p14|Paleoproterozoic|Paleoproterozoic|Kalkadoon Igneous Event. Kalkadoon-Leichhardt Domain, central Mount Isa Block.||Kalkadoon Suite or Supersuite|||Medium to coarse biotite granite, locally porphyritic, minor microgranite, aplite, pegmatite. Massive to strongly foliated.|
14590|One Tree Granite|69591|5|Briefly described|p31, p60|||Kalkadoon Batholith, Kalkadoon-Leichhardt Domain, Mount Isa Province.||Kalkadoon Suite.|||Medium to coarse biotite granite, locally porphyritic, minor microgranite, aplite, pegmatite; massive to strongly foliated.|
14590|One Tree Granite|73137|6|Mentioned|p1, p90, p93|Orosirian|Orosirian|Similar in age to Plum Mountain Gneiss and a sample tentatively assigned[?] to the Birds Well Granite [ca. 1863 Ma].|1860 Ma|||||
14590|One Tree Granite|73413|6|Mentioned|p5-6, p9-10, p21|Orosirian|Orosirian|[Also written as One Tree granite]. New U-Pb zircon age of 1857 +/- 5 Ma reported herein. A remnant was identified immediately west of Tick Hill[?].|1857 +/- 5 Ma|Kalkadoon Supersuite|||Includes granitic gneiss.|
14590|One Tree Granite|73553|6|Mentioned|p6, p8 Fig.1.2.3, p253-254|||Kalkadoon-Leichhardt Domain. Interpreted to intrude Plum Mountain Gneiss.||Kalkadoon Suite||||
14591|Ongeva Granulite|9199|5|Briefly described|Map legend|Precambrian|Precambrian|Of the Strangways Metamorphic Complex.  Interlayered felsic gneiss and mafic granulites.  Geological Province: Arunta Block.||||||03-NOV-04
14591|Ongeva Granulite|39566|6|Mentioned|Table 1|||||||||
14591|Ongeva Granulite|44114|5|Briefly described|p321, 339|||Central Arunta Inlier. Bimodal extrusives.|1780 Ma (Black and Shaw, 1995).||||Felsic and mafic granulites.|
14591|Ongeva Granulite|60547|5|Briefly described|Map Legend|Precambrian|Precambrian|Interlayered felsic and mafic granulites. Of the Strangways Metamorphic Complex. Geological Province: Arunta Block.||||||06-JUN-05
14591|Ongeva Granulite|64366|5|Briefly described|p605|Paleoproterozoic|Paleoproterozoic|Occurs in the eastern part of the Strabgways metamorphic Complex.  Age: Exhibits evidence of Early Strangways Orogeny which occurred at 1.79Ga.||||||07-NOV-08
14591|Ongeva Granulite|66860|6|Mentioned|p8|||||Strangways Metamorphic Complex|||Contains felsic intrusive unit(s).|
14591|Ongeva Granulite|69427|4|Described|p12:9-11, 37-38, 41|||Shaw et al. (1979). Eastern Strangways Range, Aileron Province. Metamorphism described in some detail.||Strangways Metamorphic Complex.||Is structurally overlain by Cadney Metamorphics. Is intruded by Anamarra Granite.|Interlayered mafic and felsic granulite, with less abundant migmatitic quartzofeldspathic gneiss and cordierite granulite. Migmatitic garnet-biotite-sillimanite metapelitic rocks also occur.|12-JUL-16
14595|Oolbra Orthogneiss|39887|6|Mentioned|Fig.3|||||||||
14595|Oolbra Orthogneiss|39888|6|Mentioned|Fig.8|||||||||
14595|Oolbra Orthogneiss|60547|5|Briefly described|Map Legend|Precambrian|Precambrian|Porphyroblastic schistose, granitic gneiss.||||||
14595|Oolbra Orthogneiss|69427|5|Briefly described|p12:9, 14-15, 30-31|||Strangways Range region, Ankala Domain, Aileron Province. A typo in 12:31 says this unit "includes" [instead of intrudes] Sliding Rock Metamorphics and Narbib Granulite.||||Intrudes Sliding Rock Metamorphics and Narbib Granulite.|Schistose porphyritic orthogneiss. In the type location, contains biotite, garnet and hornblende, with coarse K-feldspar phenocrysts.|12-JUL-16
14595|Oolbra Orthogneiss|69931|6|Mentioned|p274, 296|Paleoproterozoic|Paleoproterozoic|Arunta Inlier. Sm-Nd isotopic analyses tabulated.|||||Granite.|
14599|Oonagalabi Gneiss Complex|41242|5|Briefly described|p239|||||||||
14599|Oonagalabi Gneiss Complex|64337|6|Mentioned|p374 Fig. 1|Proterozoic|Proterozoic|Proterozoic basement.||||||
14610|Oorabra Arkose|9394|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Georgina Basin. Of the Keepera Group. Arkose, minor conglomerate.||||||
14610|Oorabra Arkose|9694|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Keepera Group. Geological Province: Georgina Basin. Underlies Elyuah Formation. Overlies Mount Cornish Formation. Arkose, sedimentary breccia, dolomite.||||||21-NOV-06
14610|Oorabra Arkose|37572|6|Mentioned|p164|||||||||
14610|Oorabra Arkose|37929|5|Briefly described|p526|||||||||
14610|Oorabra Arkose|38157|6|Mentioned|Table IX|||||||||
14610|Oorabra Arkose|40538|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Keepera Group. Arkose, locally with block sized intraclasts; siltstone; conglomerate; rare dolostone; sandstone. Geological Province: Georgina Basin.||||||15-NOV-05
14610|Oorabra Arkose|40906|4|Described|p18|||Mention Plate 7.||||||21-NOV-06
14610|Oorabra Arkose|41405|6|Mentioned|p205|||||||||
14610|Oorabra Arkose|42059|6|Mentioned|Fig.2 P131|||||||||
14610|Oorabra Arkose|42504|6|Mentioned|p85|||||||||
14610|Oorabra Arkose|42643|6|Mentioned|Fig.4 P19|||||||||
14610|Oorabra Arkose|44327|14|Not recorded|p.8|||(F53-11) Interfingers with sh. of Elyuah Fm.||||||21-NOV-06
14610|Oorabra Arkose|44328|14|Not recorded|map legend|Early Cambrian|Neoproterozoic|Lower Cambrian to Upper Proterozoic.||||||
14610|Oorabra Arkose|44964|14|Not recorded|p.33|||||||||
14610|Oorabra Arkose|45155|6|Mentioned|Fig.7|||In the Georgina Basin.||||||21-NOV-06
14610|Oorabra Arkose|46865|6|Mentioned|p49|||||||||
14610|Oorabra Arkose|48844|14|Not recorded|p.8,22-25|||F.7, Pls.3,8.||||||
14610|Oorabra Arkose|48990|4|Described|p13|||||||||
14610|Oorabra Arkose|49036|6|Mentioned|p5|||||||||
14610|Oorabra Arkose|60122|5|Briefly described|p9, p11 Tb. 1|||Formerly of the Elyuah Formation as the Oorabra Arkose Member.  Redefinition of the formation excluded this member. Disconformably overlain by Elyuah Formation.||||||01-JUN-05
14610|Oorabra Arkose|60551|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Keepera Group. Geological province: Georgina Basin.  Underlies Elyuah Formation. Overlies Mount Cornish Formation. Arkose, sharpstone, conglomerate, dolomite; basal tillite.||||||21-NOV-06
14610|Oorabra Arkose|61388|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Coarse-grained to granular and pebbly red-brown arkose, cobble conglomerate, red-brown feldspathic sandstone and mudstone. Geological Province: Georgina Basin.||||||13-OCT-05
14610|Oorabra Arkose|61404|5|Briefly described|Map legend|Cryogenian|Cryogenian|Of the Keepera Group. Arkose: locally with block-sized clasts; siltstone, conglomerate; rare dolostone, sandstone.  Geological Province: southern Georgina Basin.||||||
14610|Oorabra Arkose|61732|6|Mentioned|p108 Fig 40|||Formerly part of Elyuah Formation but excluded by Walter (1980).||||||07-FEB-11
14610|Oorabra Arkose|62984|5|Briefly described|p13|Cryogenian|Cryogenian|Overlies Boko Formation locally.  Geological Province: Georgina Basin. Representative of the Marinoan glacial episode.||||||23-JAN-07
14610|Oorabra Arkose|63562|5|Briefly described|p338 fig 3, p343-5, p352 Fig.10.|Ediacaran|Ediacaran|Of Georgina Basin.||||Is overlain by Elyuah Formation.||
14610|Oorabra Arkose|64068|3|Fully described|p46-47, p162, p19, p viii|Cryogenian||High NTGS gamma radiometric readings, presumably reflecting immature sediments from nearby granite basement.||Of Keepera Group.||Disconformably overlies Mount Cornish Formation, or various Palaeoproterozoic units. Possibly conformable over Boko Formation. Disconformably overlain by Elyuah Formation.|Proximal fluvial glacial outwash: arkoses, micaceous siltstone, shale, conglomerate; minor dolostone, sandstone.|04-APR-12
14610|Oorabra Arkose|64778|6|Mentioned|p13|Neoproterozoic|Neoproterozoic|Dulcie Syncline, Southern Georgina Basin.||||||
14610|Oorabra Arkose|65237|5|Briefly described|p5|Neooproterozoic|Neoproterozoic|Unconformably overlies Amesbury Quartzite. Geological province: southern Georgina Basin. Glacial diamictite (probably representing the younger "Marinoan" glacial episode).||||||07-FEB-11
14610|Oorabra Arkose|65338|5|Briefly described|p60, pp63-64.|||Fluvioglacial deposits.||Unit in Keepera Group.|||Includes conglomerate, pebbly arkose, arkose, silltstone and shale; arkosic sandstone locally includes a wide range of phenoclast lithologies; basal conglomerate facies locally has faceted and striated faces.|
14610|Oorabra Arkose|65341|4|Described|p2 Fig.2, pp12-14. |||Lenticular, discontinuous unit.||Unit in Keepera Group.||Conformably or disconformably overlies Boko Formation. Unconformably overlies Utopia Quartzite. Is overlain, probably unconformably, by Elyuah Formation.|Massive, poorly sorted, coarse to granular and pebbly red-brown arkose, conglomerate; matrix of angular clasts;  red-brown feldspathic sandstone, mudstone.|
14610|Oorabra Arkose|68270|4|Described|p680-683,686,688|Cryogenian|Cryogenian|Southern Georgina Basin. Type section occurs 0.8km NNE of Grant Bluff, Elua Range; lat.22'41.5'S,  long. 135'46'E. Less than 1165m thick. Proximal fluvial and glacial outwash deposit related to Elatina glaciation. Correlative to Elatina Formation. Laterally equivalent to Sun Hill Arkose and Black Stump Arkose.||||Overlain disconformably by Mopunga Group. Underlain by Boko Formation, disconformably by Mount Cornish Formation, possibly locally by Boko Formation.|Poorly sorted, medium- to coarse-grained and pebbly arkose, with interbedded sandstone, laminated micaceous siltstone and shale and conglomerate. Includes a basal conglomerate with faceted and striated clasts.|03-JUL-19
14610|Oorabra Arkose|69418|6|Mentioned|p3:30|Neoproterozoic|Neoproterozoic|||||||12-JUL-16
14610|Oorabra Arkose|69437|5|Briefly described|p22:4-5, 7|Cryogenian|Cryogenian|SE Georgina Basin, Centralian A Superbasin. Supersequence 3.||Keepera Group.||||12-JUL-16
14610|Oorabra Arkose|69438|6|Mentioned|p23:17|||Georgina Basin.||||Correlated with the Olympic Formation (Amadeus Basin).||12-JUL-16
14610|Oorabra Arkose|69443|4|Described|p28:7-9, 32-33, 35|Cryogenian|Cryogenian|Joklik (1955). Georgina Basin. Unfossiliferous. Forms rugged outcrops with tors. Highly variably thickness: 17-1165m. Glacial outwash deposit. Part of the hangingwall of the Ooomoolmilla and Lucy Creek Faults; interpreted as rift basin fill in half grabens.||Keepera Group.||Overlies Mount Cornish Formation disconformably, and possibly Boko Formation conformably. Is overlain disconformably or slightly unconformably by Elyuah Formation.|Medium-grained to pebbly arkose to lithic arkose, micaceous siltstone, shale and conglomerate; minor dolostone and sandstone. Local basal conglomerate has glacially faceted and striated clasts.|12-JUL-16
14610|Oorabra Arkose|69673|5|Briefly described|p114 fig 92, p115|Cryogenian|Cryogenian|Maximum thickness of 1165m.||Keepera Group|||Arkose, micaceous siltstone, shale and conglomerate.|
14610|Oorabra Arkose|72515|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Jervois Range Special Map Sheet. Georgina Basin.||Keepera Group|||Arkose; laminated micaceous siltstone, shale and conglomerate with lithic arkose lenses; minor dolostone, sandstone, local basal conglomerate.|
14610|Oorabra Arkose|72516|3|Fully described|p13, 15, 16, p61, p63, p86-88|Ediacaran|Ediacaran|Georgina Basin. 17-1165m thick. Type section occcurs 800m north-northeast of the Grant Bluff in the Elyuah Range in Jinka. Restricted to a few outcrops in the JERVOIS RANGE SPECIAL map sheet. Deposited in a rapid erosion, mass-transport, proximal deposition in a fluvial, glacial environment. Faulted against the Elkera Formation. Interpreted to correlate with Sun Hill Arkose, Black Stump Arkose, Boko Formation, Pioneer Sandstone and the Mount Doreen Formation. Nonconformably overlies the Thring Granite. Disconformably overlies the Mount Cornish Formation.||Keepera Group||Disconformably overlain by the Elyuah Formation. Nonconformably overlies Thring Granite.Unconformably overllies the Attutra Metagabbro and possibly Unca Granite.|Arkose; laminated micaceous siltstone, shale and conglomerate with lithic arkose lenses; minor dolostone, sandstone, local basal conglomerate.|26-APR-22
14610|Oorabra Arkose|73086|6|Mentioned|p101, p167|||Georgina Basin.||||Correlates to Olympic Formation.||
14614|Ooraminna Sandstone Member|9199|5|Briefly described|Map legend|Devonian|Devonian|Of the Hermansburg Sandstone (Pertnjara Group). Cross-bedded quartz sandstone.  Geological Province: Amadeus Basin.||||||
14614|Ooraminna Sandstone Member|22646|6|Mentioned|p 107|||Of the Hermannsburg Sandstone.  Overlies Mareenie Sandstone p107.||||||21-NOV-06
14614|Ooraminna Sandstone Member|22760|4|Described|p338|||Of the Hermannsburg Sandstone.||||||21-NOV-06
14614|Ooraminna Sandstone Member|22761|5|Briefly described|p351|Late Devonian|Middle Devonian|Of the Hermannsberg Sandstone.||||||21-NOV-06
14614|Ooraminna Sandstone Member|22762|6|Mentioned|p373||Devonian|||||||
14614|Ooraminna Sandstone Member|31566|2|Defined|p239|Devonian|Devonian|||||||
14614|Ooraminna Sandstone Member|35102|6|Mentioned|p39|||||||||
14614|Ooraminna Sandstone Member|41018|6|Mentioned|p236|||||||||
14614|Ooraminna Sandstone Member|41385|6|Mentioned|p366|||||||||
14614|Ooraminna Sandstone Member|60547|5|Briefly described|Map Legend|Devonian|Devonian|Of the Hermannsburg Sandstone. Cross-bedded quartz sandstone. Geological Province: Amadeus Basin.||||||
14614|Ooraminna Sandstone Member|69438|3|Fully described|p23:39|Devonian|Devonian|Jones (1972). Originally described as the Orange Creek Member (Pearce, 1968). Waterhouse-Ooraminna Anticlines and Camel Flat Syncline areas, NE Amadeus Basin. Type section is 315m thick along Orange Creek at the E end of the Waterhouse Anticline.||Hermannsburg Sandstone.||Disconformably overlies Mereenie Sandstone.|A uniform succession of planar bedded, cross-stratified, medium-grained quartzic sandstone, with rare siltstone and pebbly intervals.|12-JUL-16
14614|Ooraminna Sandstone Member|69673|6|Mentioned|p67|||||Hermannsburg Sandstone||Overlain by Owen Springs Sandstone Member||
14614|Ooraminna Sandstone Member|71279|6|Mentioned|p360, p364|||Magnetisation briefly described.||Hermannsburg Sandstone.||||27-OCT-17
14669|Osprey Formation|5952|5|Briefly described|p214 Fig. 4, p215 Fig. 5|Middle Triassic|Middle Triassic|Of Sahul Group. In figure, Fm = Formation. Geological Province: Bonaparte Basin.||||||01-MAR-10
14669|Osprey Formation|7142|6|Mentioned|p350 Fig.4.|Middle Triassic|Early Triassic|Browse Basin.||||Overlies Mount Goodwin Formation. Is overlain by Pollard Formation.||
14669|Osprey Formation|13194|6|Mentioned|p386 Tb. 4-16|Anisian|Anisian|Type Section: Osprey 1 well (1318-1834m). Up to 516m thick shallow marine deposits.||Sahul Group||Overlies Mount Goodwin Formation (conformably). Overlain by Pollard Formation.|Interbedded shale and sandstone; minor carbonate.|
14669|Osprey Formation|13222|6|Mentioned|p229 Fig.2.|||||Unit in Sahul Group.||||
14669|Osprey Formation|13242|5|Briefly described|p225|||Unconformably overlies Upper Mount Goodwin Formation in the west. Includes sandstones.||||||07-FEB-11
14669|Osprey Formation|13354|6|Mentioned|p375 Fig.6, p376 Fig.7.|Triassic|Late Permian|Bonaparte Basin. Unit of Sahul Group. Overlies Mount Goodwin Formation and underlies Pollard Formation. Equivalent to Erskine Sandstone of onshore Canning Basin.||161||||28-OCT-14
14669|Osprey Formation|22663|5|Briefly described|AC97 1-4 Fig.4||Middle Triassic|Of the Sahul Group.||||||01-MAR-10
14669|Osprey Formation|23378|6|Mentioned|p180 Fig.2|Middle Triassic|Early Triassic|Of the Sahul Group.  In the Vulcan Sub-basin.||||||21-NOV-06
14669|Osprey Formation|24171|5|Briefly described|p722 Fig. 3|Triassic|Triassic|Geological Province : Vulcan Sub-Basin.||||||01-MAR-10
14669|Osprey Formation|24207|5|Briefly described|p209 Fig. 5|Middle Triassic|Middle Triassic|||||||01-MAR-10
14669|Osprey Formation|41532|2|Defined|p302|Middle Triassic|Early Triassic|||||||
14669|Osprey Formation|42053|5|Briefly described|Fig.2 P29|||||||||01-MAR-10
14669|Osprey Formation|42066|5|Briefly described|Fig.3 P199|||||||||01-MAR-10
14669|Osprey Formation|42442|2|Defined|p21|Anisian|Scythian|NT and WA. Age: Early to Middle Triassic (late Scythian to Anisian).||||||14-APR-08
14669|Osprey Formation|43826|6|Mentioned|Fig.2,p163||Middle Triassic|||||||01-MAR-10
14669|Osprey Formation|60634|6|Mentioned|p1168 Fig.3. |Middle Triassic|Middle Triassic|||Unit in Sahul Group.||Overlies Mount Goodwin Formation. Is overlain by Pollard Formation.||
14669|Osprey Formation|61550|6|Mentioned|p495 Fig.2.|||||Unit in Sahul Group.||Overlies Mount Goodwin Formation. Is overlain by Pollard Formation.||09-NOV-12
14669|Osprey Formation|63358|5|Briefly described|p4 Fig. 1.3|Anisian|nammalian|||||||01-MAR-10
14669|Osprey Formation|63929|6|Mentioned|p131 Fig.2.|Early Triassic|Early Triassic|Ashmore Platform (east), Sahul Platform. Includes marine and non-marine sediments.||||Overlies Mount Goodwin Formation. Is overlain by Pollard Formation.||
14669|Osprey Formation|66124|5|Briefly described|p171 Fig.2|Anisian|Anisian|Ashmore Platform (East). Marine. Underlies Pollard Formation and overlies Mount Goodwin Formation.||||||
14669|Osprey Formation|66187|5|Briefly described|p413 Fig.2|Middle Triassic|Early Triassic|Sahul Group. Underlies the Pollard Formation, overlies the Mount Goodwin Formation. Mount Ashmore Dome.||||||
14669|Osprey Formation|67370|6|Mentioned|p313 Fig.2, p323 Fig.14. |Triassic|Triassic|||||Overlies Mount Goodwin Subgroup. Is overlain by Crane Formation.||
14669|Osprey Formation|68223|6|Mentioned|p178 Fig.3|Ladian|Scythian|||||||
14669|Osprey Formation|69297|6|Mentioned|p305|Ladinian|Anisian|Caswell, Barcoo and Seringapatam Sub-basins of the Browse Basin.||Sahul Group||Overlies the Kinmore Group. Overlain by the Pollard Formation.|Siltstone and mudstone.|
14669|Osprey Formation|69452|5|Briefly described|p36:15, 21|Triassic|Triassic|Bonaparte Basin.||Sahul Group.||Equivalent to lower part of Cape Londonderry Formation.||12-JUL-16
14669|Osprey Formation|69653|6|Mentioned|p10|Middle Triassic|Middle Triassic|Petrel Sub-basin.||Troughton Group.||Equivalent to Lower Cape Londonderry Formation.||
14669|Osprey Formation|69689|6|Mentioned|p16|Triassic|Triassic|Browse, Bonaparte Basins.||||||
14669|Osprey Formation|70061|5|Briefly described|Petrel Sub-basin; Fig.2|Anisian|Anisian|See also Regional geology: Figs.6-7. Vulcan: Fig.2. Equivalent to the lower part of Cape Londonderry Formation.||Sahul Group.||Overlies Fishburn Formation (Mount Goodwin Subgroup). Is overlain by Pollard Formation.||12-JUL-16
14669|Osprey Formation|70064|5|Briefly described|Regional Fig. 6. Central: Fig.2|Ladinian|Anisian|See also Northern: Fig.2. Yampi: Fig.2. Caswell-Barcoo Sub-basins, Browse Basin.||Sahul Group.||Overlies Kinmore Group. Is overlain by Pollard Formation.||12-JUL-16
14669|Osprey Formation|71146|5|Briefly described|p6|Middle Triassic|Early Triassic|Bonaparte Basin.||||Overlies the Mount Goodwin Subgroup. Overlain by the Sahul Group.|Mudstone.|
14703|Owen Springs Sandstone Member|22760|5|Briefly described|p345|||Of the Hermannsburg Sandstone.||||||21-NOV-06
14703|Owen Springs Sandstone Member|22825|6|Mentioned|p543|||||||||
14703|Owen Springs Sandstone Member|31566|2|Defined|p240|Devonian|Devonian|||||||
14703|Owen Springs Sandstone Member|35102|6|Mentioned|p39|||||||||
14703|Owen Springs Sandstone Member|41385|6|Mentioned|Fig.12|||||||||
14703|Owen Springs Sandstone Member|41708|6|Mentioned|p198|||||||||
14703|Owen Springs Sandstone Member|69438|3|Fully described|p23:39|Devonian|Devonian|Jones (1972). Amadeus Basin. c.220m thick at the type section on the N flank of the James Range. Thins to c.100m near its extremities.||Hermannsburg Sandstone.||Conformably/transitionally overlies Ooraminna Sandstone Member. Is overlain conformably/transitionally by Ljiltera Member.|White, cross-bedded, medium- to coarse-grained sandstone with some pebble-sized clasts (probably of Mereenie Sandstone).|12-JUL-16
14703|Owen Springs Sandstone Member|69673|6|Mentioned|p67|||||Hermannsburg Sandstone||Overlies Ooraminna Sandstone Member, overlain by Ljiltera Member||
14703|Owen Springs Sandstone Member|72369|5|Briefly described|p40|||Of Amadeus Basin.||Unit of Hermannsburg Sandstone.||||
14735|Packsaddle Microgranite|23065|6|Mentioned|13|Proterozoic|Proterozoic|||||||
14735|Packsaddle Microgranite|23363|5|Briefly described|352 Table 3|Statherian|Statherian|Age: 1724+/-4Ma.||||||26-MAR-18
14735|Packsaddle Microgranite|23395|6|Mentioned|p395|||||||||
14735|Packsaddle Microgranite|23396|6|Mentioned|p423 Fig.17|||||||||
14735|Packsaddle Microgranite|23397|6|Mentioned|p464 Fig.3|||||||||
14735|Packsaddle Microgranite|23398|4|Described|p437|Statherian|Statherian|Age: 1724+/-4Ma.||||||22-NOV-06
14735|Packsaddle Microgranite|24048|6|Mentioned|p36|||Geological Province: McArthur Basin.||||||
14735|Packsaddle Microgranite|24050|6|Mentioned|p30|||||||||
14735|Packsaddle Microgranite|32519|6|Mentioned|p341|||||||||
14735|Packsaddle Microgranite|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
14735|Packsaddle Microgranite|32660|6|Mentioned|p222|||||||||
14735|Packsaddle Microgranite|32904|6|Mentioned|p95|||||||||
14735|Packsaddle Microgranite|34811|6|Mentioned|Fig.2|||||||||
14735|Packsaddle Microgranite|35114|6|Mentioned|p204|||||||||
14735|Packsaddle Microgranite|35640|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
14735|Packsaddle Microgranite|35776|4|Described|p819|||||||||
14735|Packsaddle Microgranite|35950|6|Mentioned|p312|||||||||
14735|Packsaddle Microgranite|36012|6|Mentioned|Fig.2|||||||||
14735|Packsaddle Microgranite|36473|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
14735|Packsaddle Microgranite|37217|6|Mentioned|p650|||||||||
14735|Packsaddle Microgranite|37371|6|Mentioned|p368|||||||||
14735|Packsaddle Microgranite|37462|6|Mentioned|p244|||||||||
14735|Packsaddle Microgranite|37565|6|Mentioned|p11|||||||||
14735|Packsaddle Microgranite|39445|5|Briefly described|Table 2|||Age p39. See also p36.||||||22-NOV-06
14735|Packsaddle Microgranite|40691|5|Briefly described|p11|||||||||
14735|Packsaddle Microgranite|40811|6|Mentioned|p318|||||||||
14735|Packsaddle Microgranite|41406|6|Mentioned|Map legend|Mesoproterozoic||||||||
14735|Packsaddle Microgranite|41721|3|Fully described|p25||Paleoproterozoic|Of the Tawallah Group. Overlain by McArthur Group rocks. Intrudes Wollogorong Formation and Gold Creek Volcanics. Age: 1690Ma.  Porphyritic microgranite.||||||07-NOV-08
14735|Packsaddle Microgranite|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
14735|Packsaddle Microgranite|41957|6|Mentioned|p68|||||||||
14735|Packsaddle Microgranite|43715|6|Mentioned|p28|||||||||
14735|Packsaddle Microgranite|44112|6|Mentioned|p43|||||||||
14735|Packsaddle Microgranite|44305|14|Not recorded|p.13,18|||(E53-8). opp.6,18.||||||
14735|Packsaddle Microgranite|44306|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
14735|Packsaddle Microgranite|44436|5|Briefly described|p.12-13,opp. p.7,map|||Intrusive equivalent of Hobblechain Rhyolite Member. (E53-4).||||||02-DEC-04
14735|Packsaddle Microgranite|44437|5|Briefly described|map legend|Precambrian|Precambrian|Porphyritic microgranite.||||||08-DEC-04
14735|Packsaddle Microgranite|45087|5|Briefly described|p16|||Chemical analyses||||||
14735|Packsaddle Microgranite|45162|2|Defined|p44|Proterozoic|Proterozoic|Reference area location given.||||||22-FEB-18
14735|Packsaddle Microgranite|46919|6|Mentioned|p221|||||||||
14735|Packsaddle Microgranite|48894|6|Mentioned|p24|||Age: 1520my.||||||22-NOV-06
14735|Packsaddle Microgranite|50591|5|Briefly described|p1.3, 4.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Of the Fagan Supersuite. Geological Province: Arnhem Block/McArthur Basin.||||||07-NOV-08
14735|Packsaddle Microgranite|60483|5|Briefly described|p7 Fig. 5|||Of the Tawallah Group. Geological Province: McArthur Basin.||||||05-OCT-07
14735|Packsaddle Microgranite|60574|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Red, porphyritic (K-feldspar-quartz), microgranophyric to spherulitic microgranite. Intrudes the Gold Creek Volcanics.||||||07-NOV-08
14735|Packsaddle Microgranite|63112|6|Mentioned|p1192 Tb.1|||Calvert Superbasin. May have been feeder fissure for Hobblechain Rhyolite.|1724 +/- 4 Ma.||||Porphyritic rhyolite with quartz phenocrysts and microgranophyric to spherulitic texture.|
14735|Packsaddle Microgranite|64817|6|Mentioned|p370|||||||||
14735|Packsaddle Microgranite|65228|5|Briefly described|Figs.06, 07, 10.|Statherian|Statherian|Southern McArthur Basin.|1724 +/- 4 Ma (Page et al.2000).|||Intrudes Tawallah Group.||
14735|Packsaddle Microgranite|65337|6|Mentioned|p17.|||Southeastern McArthur Basin.|c.1725 Ma.|||||
14735|Packsaddle Microgranite|65340|3|Fully described|p11, p13 Table 4, pp46-47.|||A small (70 sq. km. outcrop) high-level, elongate northwest-striking laccolith. Chemically indistinguishable from the central, massive portion of Hobblechain Rhyolite, for which it was probably the feeder.|1724 +/- 4 Ma (Page et al. 2000).|Unit in Tawallah Group.||Intrudes Wollogorang Formation and Gold Creek Volcanics. Contiguous and co-magmatic with Hobblechain Rhyolite.|Red or pink, porphyritic (K-feldspar-quartz), microgranophyric to spherulitic rhyolite and microgranite. Quartz veins common.|26-MAR-18
14735|Packsaddle Microgranite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map, p107|Paleoproterozoic|Paleoproterozoic|Weberra Igneous Event. Shown informally as Packsaddle microgranite on p9.|||||Feldspar porphyry|
14735|Packsaddle Microgranite|67352|6|Mentioned|p14 Tb.2|||||||Intrudes Gold Creek Volcanics.||
14735|Packsaddle Microgranite|69430|4|Described|p15:9-10, 48|||Southern McArthur Basin. High-level laccolith: comagmatic with Hobblechain Rhyolite. Mineralised breccia pipes in the Running Creek area are contemporaneous with this unit.|1725 +/- 2 Ma (Page and Sweet, 1998).|Tawallah Group.||Intrudes Wollogorang Formation and Gold Creek Volcanics. Contiguous with Hobblechain Rhyolite.|Red or pink, porphyritic (K-feldspar-quartz), microgranophyric to spherulitic rhyolite and microgranite.|12-JUL-16
14735|Packsaddle Microgranite|69591|5|Briefly described|p38, p59|||N of the Murphy Tectonic Ridge. Has chemical and lithological similarities to the Peters Creek Volcanics.|1724 +/- 4 Ma.||||Feldspar porphyry.|
14735|Packsaddle Microgranite|70849|5|Briefly described|Map legend.|Statherian|Statherian|McArthur Basin.||Tawallah Group.|||Pink, porphyritic microgranite.|
14735|Packsaddle Microgranite|71592|5|Briefly described|Appendix A.|||McArthur Basin.|1724+/-4 Ma (crystallisation: U-Pb zircon SHRIMP)||||Quartz-feldspar microgranite, ferruginised.|
14735|Packsaddle Microgranite|72526|5|Briefly described|p6 Fig.1.2.|Paleoproterozoic|Paleoproterozoic|||||||
14735|Packsaddle Microgranite|72718|6|Mentioned|p7|||Southern McArthur Basin (southeastern).||Tawallah Group||Underlain by Gold Creek Volcanics. Overlain by Warramana Sandstone[?]. Equivalent to Hobblechain Rhyolite and Pungalina Member.||
14735|Packsaddle Microgranite|73083|6|Mentioned|p37, p40|||A tiny intrusion that intrudes the McArthur Basin sequence.||||||
14744|Pacoota Sandstone|9199|5|Briefly described|Map legend|Ordovician|Cambrian|Contains the N'Dahla Member.  Fossiliferous sandstone and silty sandstone.  Geological Province: Amadeus Basin.||||||04-NOV-04
14744|Pacoota Sandstone|9814|5|Briefly described|Map Legend|Ordovician|Ordovician|Of the Larapinta Group. Fossiliferous sandstone, silty sandstone, siltstone.||||||
14744|Pacoota Sandstone|12891|6|Mentioned|p734|||Geological province: Amadeus Basin. See also the misspelt Pakoota Sandstone.||||||07-FEB-11
14744|Pacoota Sandstone|13995|5|Briefly described|p75-76, p81-82, p91, p95|Ordovician|Cambrian|Shergold et al. (1991). Amadeus Basin. Platform deposits associated with Delamerian Orogeny. Contains rostroconchs (named) in beds of Datsonian (latest Cambrian) age. The oldest known diverse fauna of pelecypods in the world occurs in Warendian (Tremadocian) beds of this unit: species listed. Contains microvertebrate remains.|||||Coarse siliciclastics.|
14744|Pacoota Sandstone|22560|5|Briefly described|p3|||||||||
14744|Pacoota Sandstone|22561|4|Described|p28|Neoproterozoic|Neoproterozoic|Horn Valley Siltstone overlies this unit.||||||22-NOV-06
14744|Pacoota Sandstone|22565|5|Briefly described|p71 & Table 1|||Thickness at Areyonga Creek measured from surface expression - 560m thick.  Approx. thickness measured from seismic data - 350m.||||||
14744|Pacoota Sandstone|22566|4|Described|p84|Early Devonian|Late Cambrian|Of the Larapinta Group.||||||22-NOV-06
14744|Pacoota Sandstone|22646|5|Briefly described|p 105|Ordovician|Cambrian|informal division - lower Pacoota Sandstone refered to p 104||||||
14744|Pacoota Sandstone|22650|4|Described|p 160|Ordovician|Cambrian|Of the Larapinta Group.||||||22-NOV-06
14744|Pacoota Sandstone|22651|5|Briefly described|p 174||Late Cambrian|A major sequence boundary lies at the base of the Pacoota Sandstone which overlies the Pertaoorrta Group.||||||
14744|Pacoota Sandstone|22655|5|Briefly described|p 253|||||||||
14744|Pacoota Sandstone|22656|4|Described|p 277|Early Ordovician|Late Cambrian|||||||
14744|Pacoota Sandstone|22657|4|Described|p 285|Early Ordovician|Late Cambrian|Subdivided into p1-4.||||||22-NOV-06
14744|Pacoota Sandstone|22758|4|Described|p303-307|||Informally divided into upper and lower Pacoota Sandstone. The upper Pacoota Sandstone is Early Arenig in Age. The Pacoota Sandstone contains oolitic ironstones in the Henbury and Lake Amadeus Regions.||||||06-FEB-08
14744|Pacoota Sandstone|22759|5|Briefly described|p317|||Age Cambro-Ordovician.||||||
14744|Pacoota Sandstone|22760|6|Mentioned|p338|||||||||
14744|Pacoota Sandstone|22762|5|Briefly described|p364|Early Ordovician|Late Cambrian|||||||
14744|Pacoota Sandstone|22763|6|Mentioned|p398|Early Ordovician|Cambrian|Of the Larapinta Group.||||||22-NOV-06
14744|Pacoota Sandstone|22804|5|Briefly described|p452|Early Ordovician|Late Cambrian|Of the Larapinta Group.||||||22-NOV-06
14744|Pacoota Sandstone|22805|4|Described|p463-471|Early Ordovician|Late Cambrian|Capable of sustaining economic hydrocarbon flows p468.||||||
14744|Pacoota Sandstone|22806|4|Described|p486 & Tab 3 @p488|||Age - Cambro-Ordovician p481.  Informally devided into subunits p1-4, p480.||||||22-NOV-06
14744|Pacoota Sandstone|22807|4|Described|p499 & p500-503|Early Ordovician|Late Cambrian|Of the Larapinta Group.  The Pacoota Sandstone has been divided into four subunits, from top to bottom p1-3 and p4;  see also p499.||||||22-NOV-06
14744|Pacoota Sandstone|22824|4|Described|p526-530|Early Ordovician|Late Cambrian|Of the Larapinta Group.  Age - late Payntonian to early Arenigian, this correlates to an age range of 508-480 Ma.  See p526.||||||22-NOV-06
14744|Pacoota Sandstone|22825|6|Mentioned|p543|Early Ordovician|Early Ordovician|||||||
14744|Pacoota Sandstone|22826|4|Described|p572|Ordovician|Late Cambrian|Of the Larapinta Group.||||||22-NOV-06
14744|Pacoota Sandstone|22828|6|Mentioned|p591|||||||||
14744|Pacoota Sandstone|23250|5|Briefly described|p1124  Fig.2||Late Cambrian|Correlate of Lake Frome Group.||||||
14744|Pacoota Sandstone|23282|6|Mentioned|p81|||Probably equivalent to Mount Chandler Sandstone in Officer Basin. In the Amadeus Basin.||||||22-NOV-06
14744|Pacoota Sandstone|23361|5|Briefly described|16 Fig.4|Cambrian|Cambrian|||||||
14744|Pacoota Sandstone|23373|6|Mentioned|p318||Early Ordovician|In the Amadeus Basin.||||||22-NOV-06
14744|Pacoota Sandstone|23818|6|Mentioned|p111|||Correlated with Mount Chandler Sandstone. Geological Province: Amadeus Basin.||||||
14744|Pacoota Sandstone|23858|5|Briefly described|p915|Ordovician|Cambrian|Geological Province: Amadeus Basin.||||||
14744|Pacoota Sandstone|24047|5|Briefly described|p60|Late Cambrian|Late Cambrian|Geological Province: Amadeus Basin.||||||
14744|Pacoota Sandstone|24063|5|Briefly described|p220|Ordovician|Cambrian|Geological Province: Amadeus Basin.||||||
14744|Pacoota Sandstone|24064|5|Briefly described|p229 Fig.7|Ordovician|Ordovician|Of Larapinta Group. Geological Province: Amadeus Basin.||||||
14744|Pacoota Sandstone|29591|5|Briefly described|Table 23|||||||||
14744|Pacoota Sandstone|29721|6|Mentioned|p46|||||||||
14744|Pacoota Sandstone|29972|6|Mentioned|Table 1|||||||||
14744|Pacoota Sandstone|30045|6|Mentioned|p344|||||||||
14744|Pacoota Sandstone|30238|4|Described|p68|||Cambrian - Ordovician age||||||
14744|Pacoota Sandstone|30258|6|Mentioned|Fig.2|||Ordovician age. Part of Larapinta Group||||||
14744|Pacoota Sandstone|30540|6|Mentioned|p61|||Possibly source rock||||||
14744|Pacoota Sandstone|30544|6|Mentioned|p49|||Ordovician age||||||
14744|Pacoota Sandstone|30598|6|Mentioned|p51|||||||||
14744|Pacoota Sandstone|30615|6|Mentioned|p177|||Ordovician Formation damage||||||
14744|Pacoota Sandstone|31566|6|Mentioned|p231|||See also Fig. 2||||||
14744|Pacoota Sandstone|31572|6|Mentioned|p21|||U.Camb. - L.Ord. Correlation chart 1||||||
14744|Pacoota Sandstone|31707|4|Described|p50|||Lithology||||||
14744|Pacoota Sandstone|32712|6|Mentioned|Table 1|||||||||
14744|Pacoota Sandstone|32715|6|Mentioned|p1177|||Oil||||||
14744|Pacoota Sandstone|33307|6|Mentioned|Fig.6|||||||||
14744|Pacoota Sandstone|33491|6|Mentioned|p55|||||||||
14744|Pacoota Sandstone|33738|6|Mentioned|p47|||||||||
14744|Pacoota Sandstone|33761|6|Mentioned|p146|||Ord. Of the Larapinta Group.||||||22-NOV-06
14744|Pacoota Sandstone|33971|6|Mentioned|p26|||Refers gas production.||||||
14744|Pacoota Sandstone|34111|5|Briefly described|Table 2|||See also pp15,18. Cambrian - Ordovician||||||22-NOV-06
14744|Pacoota Sandstone|34280|6|Mentioned|p10|||||||||
14744|Pacoota Sandstone|34287|6|Mentioned|p79|||||||||
14744|Pacoota Sandstone|34433|6|Mentioned|p17|||||||||
14744|Pacoota Sandstone|34442|5|Briefly described|Table 1|||Cambrian - Ordovician||||||
14744|Pacoota Sandstone|34579|4|Described|Table 2|||See also pp16,17. Cambrian - Ordovician.||||||22-NOV-06
14744|Pacoota Sandstone|34612|6|Mentioned|p111|||Correlation||||||
14744|Pacoota Sandstone|35102|6|Mentioned|Fig.2|||||||||
14744|Pacoota Sandstone|35628|6|Mentioned|Table 3|||||||||
14744|Pacoota Sandstone|35805|6|Mentioned|Fig.3|||||||||
14744|Pacoota Sandstone|36096|6|Mentioned|p219|||||||||
14744|Pacoota Sandstone|36128|6|Mentioned|p13|||||||||
14744|Pacoota Sandstone|36198|6|Mentioned|Fig.III.2|||||||||
14744|Pacoota Sandstone|36331|6|Mentioned|p6|||See also p30,36,44,53.||||||22-NOV-06
14744|Pacoota Sandstone|36643|6|Mentioned|p65|||||||||
14744|Pacoota Sandstone|36818|6|Mentioned|p203|||||||||
14744|Pacoota Sandstone|38329|6|Mentioned|p209|||||||||
14744|Pacoota Sandstone|38606|6|Mentioned|Map legend|Early Ordovician|Late Cambrian|Late Cambrian to Early Ordovician||||||
14744|Pacoota Sandstone|38885|6|Mentioned|Map legend|Early Ordovician|Late Cambrian|Late Cambrian - Early Ordovician||||||
14744|Pacoota Sandstone|39213|6|Mentioned|Fig.6|||Amadeus Basin Succession||||||
14744|Pacoota Sandstone|39214|6|Mentioned|p10|||||||||
14744|Pacoota Sandstone|39583|6|Mentioned|Map legend|Early Ordovician|Late Cambrian|Late Cambrian to Early Ordovician||||||
14744|Pacoota Sandstone|39931|6|Mentioned|Map legend|Early Ordovician|Late Cambrian|Late Cambrian to Early Ordovician||||||
14744|Pacoota Sandstone|40136|5|Briefly described|p36|||See also p23, p32||||||22-NOV-06
14744|Pacoota Sandstone|40740|3|Fully described|p50|||Mention p6.||||||22-NOV-06
14744|Pacoota Sandstone|40810|4|Described|p7|||||||||
14744|Pacoota Sandstone|40830|6|Mentioned|p12|||||||||
14744|Pacoota Sandstone|40852|6|Mentioned|p34|||||||||
14744|Pacoota Sandstone|40906|6|Mentioned|Fig.11|||||||||
14744|Pacoota Sandstone|41018|4|Described|Fig.3|||Mention Fig.2||||||
14744|Pacoota Sandstone|41039|4|Described|p3|||||||||
14744|Pacoota Sandstone|41115|6|Mentioned|Fig.2|||||||||
14744|Pacoota Sandstone|41123|6|Mentioned|p181|||||||||
14744|Pacoota Sandstone|41190|5|Briefly described|p267|||||||||
14744|Pacoota Sandstone|41203|5|Briefly described|p14|||||||||
14744|Pacoota Sandstone|41224|5|Briefly described|p433|||||||||
14744|Pacoota Sandstone|41270|6|Mentioned|p274|||See also p276||||||22-NOV-06
14744|Pacoota Sandstone|41385|6|Mentioned|Fig.2|||||||||
14744|Pacoota Sandstone|41409|6|Mentioned|p290|||||||||
14744|Pacoota Sandstone|41560|6|Mentioned|p551|||||||||
14744|Pacoota Sandstone|41621|5|Briefly described|Map legend|Early Ordovician|Late Cambrian|||||||
14744|Pacoota Sandstone|41639|6|Mentioned|p17|||||||||
14744|Pacoota Sandstone|41708|6|Mentioned|p198|||||||||
14744|Pacoota Sandstone|41711|6|Mentioned|p259|||||||||
14744|Pacoota Sandstone|41723|6|Mentioned|Map legend|Early Ordovician|Late Cambrian|||||||07-DEC-12
14744|Pacoota Sandstone|41820|3|Fully described|p8|||||||||
14744|Pacoota Sandstone|42037|5|Briefly described|Table 3 P79|||||||||
14744|Pacoota Sandstone|42049|5|Briefly described|p216|||||||||
14744|Pacoota Sandstone|42059|5|Briefly described|p130|||See also Fig.2||||||
14744|Pacoota Sandstone|42060|6|Mentioned|Fig.5 P140|||||||||
14744|Pacoota Sandstone|42082|4|Described|p322|||||||||
14744|Pacoota Sandstone|42354|2|Defined|p2-12|Bendigonian|Payntonian|Type section - Fig.2 p4.||||||22-NOV-06
14744|Pacoota Sandstone|42504|4|Described|p77|||||||||
14744|Pacoota Sandstone|42643|6|Mentioned|p32|||In the Amadeus Basin.||||||22-NOV-06
14744|Pacoota Sandstone|42940|6|Mentioned|Plate 5|||||||||
14744|Pacoota Sandstone|43035|6|Mentioned|p38|||||||||
14744|Pacoota Sandstone|43105|5|Briefly described|p8|||||||||
14744|Pacoota Sandstone|43225|5|Briefly described|Map Legend|Ordovician|Cambrian|Of Larapinta Group.||||||22-NOV-06
14744|Pacoota Sandstone|43230|6|Mentioned|p9||Ordovician|Reservoir target.||||||
14744|Pacoota Sandstone|43503|6|Mentioned|11-50|Bendigonian|Payntonian|||||||
14744|Pacoota Sandstone|43646|6|Mentioned|Fig.3,p554|Bendigonian|Payntonian|||||||
14744|Pacoota Sandstone|43647|6|Mentioned|p535|||||||||
14744|Pacoota Sandstone|43648|6|Mentioned|p491|||||||||
14744|Pacoota Sandstone|43649|5|Briefly described|p457|||||||||
14744|Pacoota Sandstone|43781|6|Mentioned|p4|||||||||
14744|Pacoota Sandstone|43803|6|Mentioned|Fig.5,p71|||||||||
14744|Pacoota Sandstone|43809|6|Mentioned|Fig.3,p215|||||||||
14744|Pacoota Sandstone|43817|5|Briefly described|p61-63|||||||||
14744|Pacoota Sandstone|43869|6|Mentioned|p10||Cambrian|||||||
14744|Pacoota Sandstone|43883|14|Not recorded|p11|||||||||
14744|Pacoota Sandstone|44133|5|Briefly described|p40, 43, 4 Fig. 7.2|Early Ordovician|Early Ordovician|Geological Province: Western Warburton Basin.||||||
14744|Pacoota Sandstone|44158|6|Mentioned|p33|||In the Amadeus Basin..||||||22-NOV-06
14744|Pacoota Sandstone|44395|14|Not recorded|p.8,10,12, Tb.2|||Camb-Ord.||||||
14744|Pacoota Sandstone|44396|5|Briefly described|map legend|||(Camb-Ord). Of Larapinta Group.||||||22-NOV-06
14744|Pacoota Sandstone|44402|5|Briefly described|map legend|Ordovician|Cambrian|Part of Larapinta Group. Camb-Ord.||||||02-DEC-04
14744|Pacoota Sandstone|44433|14|Not recorded|map legend|||Cambrian to Ordovician.||||||
14744|Pacoota Sandstone|44484|14|Not recorded|p.11,12,13,Tb.1,2|||Part Of Larapinta Group. (Camb-Ord).||||||
14744|Pacoota Sandstone|44485|14|Not recorded|map legend|Ordovician|Cambrian|Part of Larapinta Group. Camb-Ord. Defn on Tech.File F/53-13.||||||
14744|Pacoota Sandstone|44497|4|Described|p.10, Table 2|Ordovician|Cambrian|SF/53-13. Cambrian-Ord.||||||
14744|Pacoota Sandstone|44498|14|Not recorded|map legend|Ordovician|Cambrian|Part of Larapinta Group. Cambrian-Ord.||||||
14744|Pacoota Sandstone|44505|14|Not recorded|p.8,11, Table 1,2|Ordovician|Cambrian|Of Larapinta Group. Camb-Ord.||||||
14744|Pacoota Sandstone|44506|14|Not recorded|map legend|||Cambrian to Ordovician.||||||07-DEC-12
14744|Pacoota Sandstone|45036|6|Mentioned|p3|||||||||
14744|Pacoota Sandstone|45041|4|Described|p62|||See also pp63-68. U.Camb. - L.Ord.||||||22-NOV-06
14744|Pacoota Sandstone|45115|6|Mentioned|p7|||||||||
14744|Pacoota Sandstone|45118|6|Mentioned|p1,3|||||||||
14744|Pacoota Sandstone|45148|6|Mentioned|Fig.4|||In the Amadeus Basin.||||||22-NOV-06
14744|Pacoota Sandstone|45153|6|Mentioned|App.1-2|||||||||
14744|Pacoota Sandstone|45155|6|Mentioned|Fig.8|||||||||
14744|Pacoota Sandstone|45168|6|Mentioned|p6|||||||||
14744|Pacoota Sandstone|45170|6|Mentioned|p8|||||||||
14744|Pacoota Sandstone|46730|5|Briefly described|p7|Ordovician|Cambrian|Underlain by Pertaoorrta Group. Geological Province: Amadeus Basin||||||22-NOV-06
14744|Pacoota Sandstone|46826|5|Briefly described|p345|||||||||
14744|Pacoota Sandstone|46928|6|Mentioned|Table 1|||||||||
14744|Pacoota Sandstone|47050|6|Mentioned|p240|||||||||
14744|Pacoota Sandstone|48639|14|Not recorded|pages not known|||||||||
14744|Pacoota Sandstone|48838|2|Defined|p.19, Tb.1|||||||||
14744|Pacoota Sandstone|48862|14|Not recorded|p.8-18,23-25,40,41|||Basal unit of Larapinta Group. (F52-15). Pl.3,8-11.||||||22-NOV-06
14744|Pacoota Sandstone|48863|2|Defined|p.24,25|Early Ordovician|Late Cambrian|Tb.1. opp.p.7,9,14,20,29,30,36,37,39-41, Pl.3,4,9,10,11,13,15,16. Upper Cambrian-Lower Ordovician. (G52-4,G53-1).||||||
14744|Pacoota Sandstone|48864|14|Not recorded|p.10(Tb),31-33||Ordovician|||||||
14744|Pacoota Sandstone|48865|14|Not recorded|Fig.4,p.23,24|||(G52-4,F53-13)(Larapinta Gp.).||||||
14744|Pacoota Sandstone|48890|4|Described|p.44|Ordovician|Cambrian|See also Tables, Figs and Plates. Part of Larapinta Group. Camb-Ord.||||||22-NOV-06
14744|Pacoota Sandstone|48963|6|Mentioned|p5|||Fig.3||||||
14744|Pacoota Sandstone|50089|5|Briefly described|p430 Fig. 5|Ordovician|Ordovician|Geological Province: Amadeus Basin.||||||
14744|Pacoota Sandstone|50097|5|Briefly described|p44|Bendigonian|Lancefieldian|Geological Province: Amadeus Basin.||||||07-FEB-11
14744|Pacoota Sandstone|50098|5|Briefly described|p1|Ordovician||Of the Larapinta Group. Geological Province: Amadeus Basin.||||||
14744|Pacoota Sandstone|50246|5|Briefly described|p20 Fig. 2|Ordovician|Cambrian|Sandstone, siltstone - fossiliferous.||||||07-FEB-11
14744|Pacoota Sandstone|60287|5|Briefly described|p384|Ordovician|Cambrian|Thickness: 200 m.||||||
14744|Pacoota Sandstone|60547|5|Briefly described|Map Legend|Ordovician|Cambrian|Fossiliferous sandstone and silty sandstone. Of the Larapinta Group. Geological Province: Amadeus Basin.||||||03-JUN-05
14744|Pacoota Sandstone|60674|5|Briefly described|Map legend|Ordovician|Cambrian|Of the Larapinta Group. Medium cross-bedded quartz sandstone; minor coarse sandstone and pebbly beds. Geological Province: Amadeus Basin.||||||
14744|Pacoota Sandstone|61306|5|Briefly described|p14, p40|||High-yielding aquifer rocks. Geological Province: northern Amadeus Basin.||||||22-NOV-06
14744|Pacoota Sandstone|61309|5|Briefly described|p16 Fig. 4|||Geological Province: Amadeus Basin.||||||06-FEB-08
14744|Pacoota Sandstone|61385|5|Briefly described|Map legend|Ordovician|Cambrian|Sandstone, conglomeratic sandstone; marine fossils.   Geological Province: Ngalia Basin [?check map].||||||20-OCT-10
14744|Pacoota Sandstone|61387|5|Briefly described|Map legend|Ordovician|Ordovician|Of the Larapinta Group. Sandstone; marine fossils. Geological Province: Amadeus Basin.||||||04-OCT-05
14744|Pacoota Sandstone|61518|5|Briefly described|Map Legend|Ordovician|Cambrian|Of the Larapinta Group. Medium grained cross bedded quartz sandstone; minor coarse grained sandstone and pebbly beds. Geological Province: Amadeus Basin.||||||
14744|Pacoota Sandstone|61519|5|Briefly described|Map Legend|Ordovician|Ordovician|Of the Larapinta Group. Sandstone; marine fossils. Geological Province: Amadeus Basin.||||||14-FEB-06
14744|Pacoota Sandstone|62359|5|Briefly described|p542, p546|Ordovician|Ordovician|Overlain by Horn Valley Siltstone. Forms the reservoir for main hydrocarbon-producing system of the basin.  Geological Province: Amadeus Basin. See also p546-547 Figs. 6 and 7.||||||
14744|Pacoota Sandstone|62376|5|Briefly described|p18|Early Ordovician|Late Cambrian|Of the Larapinta Group. Geological Province: Amadeus Basin.||||||09-FEB-10
14744|Pacoota Sandstone|62379|5|Briefly described|p7 Fig. 2|Ordovician|Late Cambrian|Of the Larapinta Group. Geological Province: Amadeus Basin.||||||
14744|Pacoota Sandstone|62595|5|Briefly described|p9, p29 Fig.6, p30 Fig.8.|Ordovician|Cambrian|Widespread unit; the principal hydrocarbon reservoir in the Amadeus Basin. Contains 600-500 Ma detrital zircons with no apparent Central Australian source.|||||Mainly marine siliciclastics: fossiliferous sandstone and siltstone.|
14744|Pacoota Sandstone|62794|5|Briefly described|p288, p289 Fig.2, p290-291|Early Ordovician|Late Cambrian|Basal unit of Larapinta Group. Resistant quartzose sandstone, siltstone. Overlain by Horn Valley Siltstone. The boundary between these units has been revised several times (Prichard & Quinlan 1962; Wells et al.1970; Huckaba 1970; Gorter 1984,1991).||||||
14744|Pacoota Sandstone|62982|5|Briefly described|p7|Early Ordovician|Late Cambrian|Of the Larapinta Group. Thick shallow marine deposits with fluvial interludes. Overlain by Horn Valley Siltstone. Geological Province: Amadeus Basin. Main reservoir of Larapinta Group is in upper section of this unit.||||||05-FEB-08
14744|Pacoota Sandstone|63121|6|Mentioned|p231|||||||||
14744|Pacoota Sandstone|63562|4|Described|p338 fig 3, p341, p352 fig 10|Early Ordovician|Late Cambrian|See also p353 fig 11, p346-9. Of Amadeus Basin. Marine/locally fluvial, widespread siliciclastic unit. Zircon ages very mixed. Principal hydrocarbon reservoir in the Basin.||Larapinta Group||Overlies Goyder Formation. Is overlain by Horn Valley Siltstone. Correlated with Tomahawk Formation.|Medium-grained quartz sandstone.|
14744|Pacoota Sandstone|64068|6|Mentioned|p71, 72, 73, 75|||Amadeus Basin. Basal part may correlate with Chatsworth Limestone. Correlated with Ninmaroo Formation, Tomahawk Formation, Kelly Creek Formation, Georgina Basin.||||||
14744|Pacoota Sandstone|64334|5|Briefly described|p39-43, 45-46|Ordovician|Cambrian|Amadeus Basin. Is notably cyclic on several scales, shallowing-upward. Reservoir rock.||Larapinta Group.||Unconformably overlies Pertaoorrta Group. Is overlain by Horn Valley Siltstone.||
14744|Pacoota Sandstone|64778|6|Mentioned|p13|Ordovician|Ordovician|Amadeus Basin.||||||
14744|Pacoota Sandstone|64809|5|Briefly described|p2, p3 Fig.2, p6 Fig.4, p11 Fig.10.|Early Ordovician|Late Cambrian|See also p13 Fig.13. Marine transgression.||Of the Larapinta Group||||
14744|Pacoota Sandstone|65233|4|Described|p3 Fig. 2, p9-10|Early Ordovician|Late Cambrian|Basal unit of Larapinta Group. Gradational with upper Goyder Fm below. Max. thickness: 800m. Geological province: Amadeus Basin. An important oil reservoir in mainly shallow marine deposits - further lithological details included.||||||07-FEB-11
14744|Pacoota Sandstone|65342|6|Mentioned|p4.|||Amadeus Basin. Max. thickness at least 384 m.||||Overlies Goyder Formation. Is overlain by Horn Valley Siltstone.||
14744|Pacoota Sandstone|65489|5|Briefly described|p125|Ordovician|Cambrian|Amadeus Basin. Hosts Mereenie oil field and the Palm Valley and West Walker gas fields.||Unit in Larapinta Group.||Overlies Goyder Formation (Pertaoorrta Group). Is overlain by Horn Valley Siltstone.||
14744|Pacoota Sandstone|66589|6|Mentioned|p178|Early Ordovician|Early Ordovician|Case studies cited; not visited in the field by the authors of this study.||||||
14744|Pacoota Sandstone|67326|4|Described|p2-6, p12-13, Appx.2|Early Ordovician|Late Cambrian|Amadeus Basin. The lower part of this unit was intersected by stratigraphic drillhole LA05DD01. Up to 800m thick; thins to the S. Mainly shallow-marine deposits. Unmetamorphosed. Cored section photograph. Contains viable reservoir-quality sandstone. Cu sulfides present in basal part. Composite log.||Larapinta Group.||Overlies Goyder Formation, and Petermann Sandstone ?disconformably. Is overlain by Horn Valley Siltstone.|Off-white to pink, occasionally red-yellow, cross-bedded, locally bioturbated and strongly limonitic, quartzose sandstone; minor metasedimentary, acid volcanic and kaolinitic clasts.|
14744|Pacoota Sandstone|67565|5|Briefly described|p40, p41, p50, p52.|Early Ordovician|Late Cambrian|Shallow marine environment. Forms prominent peaks and ridges. Is an important aquifer and oil and gas reservoir; it is the reservoir rock at the Mereenie oil/gas field. Up to 640 m thick. Hosts a significant manganese occurrence at the Wangatinya Prospect. An important aquifer.||||Conformably overlies Cleland Sandstone and Goyder Formation. Is overlain conformably by Horn Valley Siltstone.|Mainly a medium-grained, cross-bedded quartz sandstone, with minor coarse sandstone and pebbly beds; local prominent glauconitic bed.|
14744|Pacoota Sandstone|67856|6|Mentioned|p338 fig 4-30|Early Ordovician|Late Cambrian|||Of Larapinta Group.||||
14744|Pacoota Sandstone|68297|5|Briefly described|p177|Bendigonian|Bendigonian|Amadeus Basin. Includes disarticulated vertebrate fossils.||||||
14744|Pacoota Sandstone|68316|6|Mentioned|pp778-780, pp782-784|Early Ordovician|Early Ordovician|Amadeus Basin.|< c. 490 Ma, detrital zircon|||||
14744|Pacoota Sandstone|68323|5|Briefly described|p1-6, p8-10, p12-13, p15|Early Ordovician|Late Cambrian|Mineralogy detailed: dominated by quartz and kaolinite. The mineralogy is uniform across the logged boundary with the underlying unit.||Larapinta Group.||Overlies Petermann Sandstone, probably conformably.|Largely quartzose; minor metasedimentary, acid volcanic and kaolinitic clasts.|
14744|Pacoota Sandstone|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 (tight gas).||||||12-JUL-16
14744|Pacoota Sandstone|69437|5|Briefly described|p22:10, 15|Early Ordovician|Furongian|Amadeus Basin. Hosts the Wangatinya manganese prospect; currently uneconomic. Has considerable unconventional petroleum potential: tight gas.||||Overlies Goyder Formation. Is overlain by Horn Valley Siltstone.||12-JUL-16
14744|Pacoota Sandstone|69438|3|Fully described|p23:2-3,7-8,30,32-34,38,46,53-57,59-61|Early Ordovician|Late Cambrian|Pritchard and Quinlan (1962). Best exposed in prominent strike ridges and high escarpments in the MacDonnell, Idirriki and James Ranges and Johnny Creek Anticline, Amadeus Basin. 700-800m thick. Informally subdivided into four sequences (see Lithology), with a diverse fossil fauna at a number of levels. Sediment was sourced from the west and the east. Mapped (Wells et al., 1967) as including rocks subsequently assigned to N'Dahla Member (of Parke Siltstone) by Young et al. (1987). Hosts the Wangatinya manganese mineralisation. Contains oolitic ironstone beds with little economic significance. One of the main hydrocarbon reservoirs for the Basin, sealed by thick shales of the Horn Valley Siltstone.||Larapinta Group.||Overlies Cleland Sandstone conformably and Goyder Formation unconformably. Is overlain by N'Dahla Member unconformably and Horn Valley Siltstone probably unconformably.|Deeply incised, coarse-grained channel sandstone; strongly bioturbated sandstones with well-developed Skolithos ichnofacies; sandstones, glauconitic shale with dolostone layers; shales interbedded with sandstones rich in ichnofossils.|12-JUL-16
14744|Pacoota Sandstone|69439|5|Briefly described|p24:10|Ordovician|Ordovician|Amadeus Basin. Mentioned as having a similar fossil assemblage to the Bloodwood Formation (Ngalia Basin) which was nevertheless dated as Cambrian. Possible correlative of Djagamara Formation.||||||12-JUL-16
14744|Pacoota Sandstone|69443|6|Mentioned|p28:26-27|||Amadeus Basin.||||Correlated with Cockroach and Toko Groups.||12-JUL-16
14744|Pacoota Sandstone|69444|6|Mentioned|p29:2 Fig.29.3|||Amadeus Basin. Detrital zircon probability distribution diagram.||||||12-JUL-16
14744|Pacoota Sandstone|69449|5|Briefly described|p34:2 Fig.34.2; 34:4|Ordovician|Cambrian|Eastern Amadeus Basin.||Larapinta Group.||Probable correlative of Innamincka Formation.||12-JUL-16
14744|Pacoota Sandstone|69458|6|Mentioned|p42:33 Fig.42.37|||Amadeus Basin. Forms steeply-dipping strata in west MacDonnell Ranges with bevelled crests, interpreted as a preservation of an earlier upland surface.||||||12-JUL-16
14744|Pacoota Sandstone|69673|4|Described|p66, p87, p92, p93, p96,  p103, p149,|Ordovician|Cambrian|Deposited in shallow marine and paralic environments. 700-800m thick.||Larapinta Group||Unconformably overlies upper Goyder Formation, conformably overlain by Horn Valley Siltstone|Strongly bioturbated sandstones, sandstones overlain by glauconitic shale and dolostones. Black shales and siltstone interbeds.|
14744|Pacoota 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.||||||
14744|Pacoota Sandstone|70749|6|Mentioned|p52, p54|||Amadeus Basin.||Larapinta Group.||||
14744|Pacoota Sandstone|71114|6|Mentioned|p170 fig 1b, p172-6. ||Furongian|Across entire Amadeus Basin. Downhole logs of petroleum wells Alice 1 and East Mereenie 4.||||Shown as overlying Goyder Formation.||14-FEB-18
14744|Pacoota Sandstone|71146|5|Briefly described|p6|Early Ordovician|Cambrian|Amadeus Basin.||Larapinta Group||Unconformably overlies the Pertaoorrta Group. Overlain by the Horn Valley Siltstone.|Sandstone.|
14744|Pacoota Sandstone|71171|6|Mentioned|p2|||Amadeus Basin.||||||
14744|Pacoota Sandstone|71279|5|Briefly described|p353, p355 Fig.2, p359, p366, p382 Tb.1|Early Ordovician|Late Cambrian|Amadeus Basin. Modelled magnetic properties.|<510 Ma (maximum depositional age).|Larapinta Group.|||Quartzite.|27-OCT-17
14744|Pacoota Sandstone|71283|6|Mentioned|p472, p478|Early Ordovician|Early Ordovician|Amadeus Basin. Trilobite species mentioned.||||||
14744|Pacoota Sandstone|71342|6|Mentioned|Ch9 p3, Ch9 p7, Ch9 p9, Ch9 p11, Ch9 p21|Palaeozoic|Palaeozoic|||||||
14744|Pacoota Sandstone|71800|5|Briefly described|p26-p27|Early Ordovician|Late Cambrian|Amadeus Basin.||||Unconformably overlies the Goyder Formation. Overlain by the Horn Valley Siltstone.|Sandstone and quartz sandstone.|
14744|Pacoota Sandstone|71898|5|Briefly described|p17|||Amadeus Basin.||Larapinta Group||Unconformably overlies the Goyder Formation. Conformably to unconformably overlain by the Horn Valley Siltstone.||19-NOV-18
14744|Pacoota Sandstone|72358|5|Briefly described|p118-119,121-126|Furongian|Furongian|Of Amadeus Basin. Contact with underlying Goyder Formation is brecciated and deformed, associated with anticlinal structural architecture of Waterhouse Range (Austin et al., 2017). This contact is described as a 2nd-order regressive sequence boundary in this study, marking a disconformity and erosional surface.||||Underlain by Goyder Formation.||10-JAN-20
14744|Pacoota Sandstone|72360|5|Briefly described|Map legend|Ordovician|Cambrian|Of Amadeus Basin.||Unit of Larapinta Group.|||Sandstone; marine fossils.|09-SEP-19
14744|Pacoota Sandstone|72369|4|Described|iii,p3-4,26-29|||Of Amadeus Basin. Outcrops extensively across the Amadeus Basin, and most well exposed as prominent strike ridges in the MacDonnell, Idirriki and James ranges, and in the Johnnys Creek Anticline. LA-ICP-MS U-Pb detrital zircon dating of sample HB15VJN345 (quartz arenite) yielded an interpreted maximum depositional age of 522+\-5 Ma (youngest concordant zircon), but does not further constrained the depositional age of the Pacoota Sandstone, as it pre-dates the c. 508-480 Ma age provided by fossils (see Shergold et al 1991), and the c. 488-486 Ma MDA provided by Maidment (2005). Contains detrital zircons sourced from Aileron and Warumpi provinces (c. 2000-1430 Ma age spectrum). Detrital zircons between c. 1255-850 Ma and c. 750-520 Ma are interpreted to have been sourced distally from east Gondwana as there are no known proximal Neoproterozoic-Cambrian sources to the Amadeus Basin. Diverse zircon age spectra and large proportion of rounded zircon grains, indicate at least partial derivation from intra-basinal recycling from older lithostratigraphic units.||Unit of Larapinta Group.||Unconformably overlain by Horn Valley Siltstone. Basal unit of Larapinta Group. Unconformably overlies the Goyder Formation.|Variably fine- to coarse-grained quartz sandstone.|18-DEC-19
14744|Pacoota Sandstone|72516|6|Mentioned|p94|Ordovician|Cambrian|Amadeus Basin.||||Equivalent to the Tomahawk Formation.||09-JUN-21
14744|Pacoota Sandstone|73085|4|Described|piii, p1, p3-8|early Ordovician|late Cambrian|Amadeus Basin. 62.5 m thick in drillhole LA05DD01. Basal contact with Petermann Sandstone is sharp.||Larapinta Group||Underlain by Pertermann Sandstone and Goyder Formation (Pertaoorrta Group and equivalents). Overlain by Horn Valley Siltstone.|White to brown, medium- to coarse-grained sandstone with occasional fine-grained, thinly laminated beds. Bedding and lamina planes are defined by red or orange Fe-oxide minerals. Cross-bedding was also observed in a short interval of core.|
14744|Pacoota Sandstone|73279|5|Briefly described|p3, p10|Ordovician[?]|Cambrian|Amadeus Basin. Lowermost part of the Larapinta Group. Detrital zircons analysed for Hf isotopic composition [see article].||Larapinta Group|||Includes sandstone.|
14744|Pacoota Sandstone|73346|6|Mentioned|p18|Early Ordovician|Furongian|Amadeus Basin. Includes the arandaspid Porophoraspis sp.||||||
14839|Panton Formation|14019|5|Briefly described|p21|Middle Cambrian|Middle Cambrian|Of the Negri Subgroup (Goose Hole Group).  Includes the Shady Camp and Corby Limestone Members.  Geological Province: Ord Basin.||||||
14839|Panton Formation|23821|5|Briefly described|p244|Middle Cambrian|Middle Cambrian|Of Negri Group. Geological Province: Ord Basin.||||||
14839|Panton Formation|24303|6|Mentioned|p63 Appendix|||Geological Province: Ord Basin. Correlative Of Gum Ridge Formation.||||||
14839|Panton Formation|28255|3|Fully described|p98|Middle Cambrian|Middle Cambrian|Of the Negri Group. Consists of a lower siltstone, middle fossiliferous limestone and an upper limestone; minor shale and gypsum. Conformably overlies Linnekar Limestone; conformably underlies Hudson Fm. Max. thickness: 190m. See also Table 9 (before p83)||||||
14839|Panton Formation|32172|4|Described|Table 2|||Middle Camb.||||||
14839|Panton Formation|32173|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Of the Negri Group.  Purple and green siltstone, minor shale, gypsum bands, fossiliferous limestone.  Conformably overlain by the Hudson Formation; conformably overlies the Linnekar Limestone.||||||17-NOV-04
14839|Panton Formation|32648|6|Mentioned|p32|||M.Camb.||||||
14839|Panton Formation|33376|6|Mentioned|Map legend|Early Ordovician|Middle Cambrian|Middle Cambrian to Lower Ordovician||||||
14839|Panton Formation|36551|6|Mentioned|Table 16|||||||||
14839|Panton Formation|36890|3|Fully described|p397|||Formerly Panton Shale.||||||14-NOV-06
14839|Panton Formation|40993|6|Mentioned|Fig.1|||||||||
14839|Panton Formation|40996|6|Mentioned|p405|||||||||
14839|Panton Formation|41840|1|Redefined|p42|Middle Cambrian||Incorporates the former Panton Shale, Shady Camp Limestone, Negri River Shale, Corby Limestone, Hudson Sh.||||||14-NOV-06
14839|Panton Formation|41864|4|Described|p19|||Includes units formerly known as Panton, Negri River, Hudson Shales, Corby Shady Camp Lsts.||||||
14839|Panton Formation|41865|5|Briefly described|Map legend|Middle Cambrian||||||||
14839|Panton Formation|41866|5|Briefly described|Map legend|Middle Cambrian||||||||
14839|Panton Formation|42070|6|Mentioned|p4|||||||||
14839|Panton Formation|44230|5|Briefly described|Map Legend||Middle Cambrian|||||||
14839|Panton Formation|44317|4|Described|Table 4||Cambrian|||||||
14839|Panton Formation|44318|14|Not recorded|map legend||Middle Cambrian|Mid.Cambrian||||||
14839|Panton Formation|44363|5|Briefly described|p.6,18,21||Middle Cambrian|Middle Cambrian.||||||
14839|Panton Formation|44364|14|Not recorded|map legend|||||||||
14839|Panton Formation|44868|5|Briefly described|Map Legend|Boomerangian|Ordian|||||||
14839|Panton Formation|45047|6|Mentioned|p126|||See also p128.||||||14-NOV-06
14839|Panton Formation|48943|3|Fully described|p110|||||||||
14839|Panton Formation|60419|3|Fully described|p1, p3 Fig.2|Middle Cambrian|Middle Cambrian|Of Negri Subgroup. Conformably overlies Linnekar Limestone. Conformably overlain by Eagle Hawk Sandstone. Max. thickness: 308 m. Maroon gypsiferous siltstone and shale, with two limestone members. Peritidal. Geological Province: Ord Basin.||||||
14839|Panton Formation|60519|5|Briefly described|Map Legend|Late Cambrian|Middle Cambrian|Of the Negri Subgroup (Goose Hole Group). Siltstone and mudstone; minor feldspathic sandstone, and limestone. Geological Province: Ord Basin.||||||03-NOV-04
14839|Panton Formation|60589|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Of the Negri Subgroup (Goose Hole Group).  Includes two members: Corby Limestone and Shady Camp Limestone Members.  Conformably overlies the Linnekar Limestone; conformably overlain by Eagle Hawk Sandstone.  Geological Province: Ord Basin.||||||24-NOV-04
14839|Panton Formation|62789|5|Briefly described|p133|Cambrian|Cambrian|Ord Basin. Contains Xystridura negrina assemblage of moderate diversity including trilobites, brachiopods, hyoliths, molluscs, adrioasteroid ossicles and a ptychoparioid.|||Includes Shady Camp and Corby Limestone Members.|||28-MAR-12
14839|Panton Formation|64580|6|Mentioned|map legend|||Of Goose Hole Group.||||||15-DEC-08
14839|Panton Formation|67352|6|Mentioned|p21|Middle Cambrian|Middle Cambrian|Ord Basin. Contains a widespread (NT-SA-Antarctica) fossil fauna.||||||
14839|Panton Formation|67860|4|Described|p417 fig 4-85, p419 Tb. 4-18, p421|Middle Cambrian|Middle Cambrian|105-308 m thick. Type section details given. Fossiliferous. Said to include "Hudson Formation" of Dow et al. (1964) [??].||Negri Subgroup|Includes Corby and Shady Camp, Limestone Members.|Conformably overlies Linnekar Limestone. Is overlain conformably by Eagle Hawk Sandstone.|Purple siltstone with sandstone and mudstone; minor limestone.|
14839|Panton Formation|69099|4|Described|GEOL_LUT_CSV files + geochron files|Series 3||Ord Basin||Negri Subgroup|||Purple siltstone; interbedded sandstone and mudstone; minor limestone.|04-AUG-15
14839|Panton Formation|69165|5|Briefly described|100k_interpgeop_lut.csv|Cambrian|Cambrian|See also 500k_geologyp08_lut.csv.||Negri Subgroup|||Purple siltstone; interbedded sandstone and mudstone; minor limestone.|
14839|Panton Formation|69437|5|Briefly described|p22:10-11|Series 3|Series 2|Ord Basin, Centralian B Superbasin. Sequence 1.||Negri Subgroup.||Overlies Linnekar Limestone. Is overlain by Eagle Hawk Sandstone.||12-JUL-16
14839|Panton Formation|69446|6|Mentioned|p31:3|||Ord Basin. Strong species-level similarity with correlative faunas of Tindall Limestone (Daly Basin).||||||12-JUL-16
14839|Panton Formation|69447|6|Mentioned|p32:2|||Ord Basin. Has strong species-level correlative faunas with Montejinni Limestone and Hooker Creek Formation (Wiso Basin).||||||12-JUL-16
14839|Panton Formation|69448|4|Described|p33:2-6, 8|Middle Cambrian|Middle Cambrian|Redefined by Mory and Beere (1985) to include five superseded Formation-rank units of Traves (1955). The upper part was formerly the Hudson Formation. Ord Basin. 308m thick. Peritidal deposits; restricted shallow subtidal between named Members. Widely distributed but poorly exposed. Typically forms sandy vertosol ("black soil") plains. Unfossiliferous except for the medial interval bracketed by named Members, which contains trilobites (including Redlichia and Xystridura), brachiopods, hyoliths, molluscs, disarticulated echinoderms, chancelloriids and sponge spicules. Hosts a number of uneconomic base metal anomalies.||Negri Subgroup.|Shady Camp, Corby, Limestone Members.|Conformably and gradationally overlies Linnekar Limestone. Is overlain conformably by Eagle Hawk Sandstone.|Maroon gypsiferous siltstone, mudstone, minor feldspathic sandstone and limestone; limestone, marl and thin sandstone beds between named Members.|12-JUL-16
14839|Panton Formation|69634|4|Described|GEOL_LUT_CSV files|Series 3|Series 3|Geological province: Halls Creek Orogen. Of Ord Basin. Events: Alice Springs Orogeny. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|505-497 Ma (Inferred)|Unit of Negri Subgroup.|||Purple siltstone; interbedded sandstone and mudstone; minor limestone|
14839|Panton Formation|69673|5|Briefly described|p142, p192, p193|Cambrian|Cambrian|308m thick.||Negri Subgroup|Includes Shady Camp Limestone Member, Corby Limestone Member|Overlies Linnekar Limestone, overlain by Eagle Hawk Sandstone|Gypsiferous siltstone and mudstone, fossiliferous limestone and marl and minor thin sandstone beds.|
14839|Panton Formation|70154|5|Briefly described|100k_interpgeop_lut.csv|Cambrian|Cambrian||497-505 Ma|Negri Subgroup|||Siltstone; interbedded sandstone, mudstone and minor limestone.|
14839|Panton Formation|70752|6|Mentioned|p131|||Ord Basin. Contains a fragment of brachiopod Westonia-like ornamentation of limited comparative value.||||||
14839|Panton Formation|71267|4|Described|GEOL_LUT_CSV files|Series 3|Series 3|Geological province: Halls Creek Orogen. Of Ord Basin. Events: Alice Springs Orogeny (450-295 Ma); Pertnjara-Brewer Movements (Alice Springs Orogeny phase 2) (390-360 Ma); Rodingan Movement (Alice Springs Orogeny phase 1) (450-420 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|505-497 Ma (inferred)|Unit of Negri Subgroup.|||Purple siltstone; interbedded sandstone and mudstone; micritic and oncolitic limestone|
14839|Panton Formation|71800|4|Described|p25-p27|Middle Cambrian|Middle Cambrian|Ord Basin. Hosts age diagnostic fossils such as the brachiopod Billingsella and Wimanella, girvanellids and stromatolites.||Negri Subgroup|Includes the Shady Camp Limestone Member and the Corby Limestone Member.|Overlies the Linnekar Limestone. Conformably (gradationally) overlain by the Eagle Hawk Sandstone.|Purple siltstone, flaggy sandstone and limestone.|
14839|Panton Formation|73255|6|Mentioned|p534 Fig.2|Cambrian|Cambrian|||Goose Hole Group||Overlies the Linnekar Limestone, underlies the Eagle Hawk Sandstone.||
14857|Paradise Creek Formation|22438|3|Fully described|p539, Fig.3 p537|Statherian|Statherian|Age of unit 1653+/-7 Ma. See also Fig.10a p546.||||||22-NOV-06
14857|Paradise Creek Formation|22453|6|Mentioned|p 11|||NT and QLD.||||||22-NOV-06
14857|Paradise Creek Formation|22468|5|Briefly described|p 16|Statherian|Statherian|Age: 1653 +/- 7 Ma SHRIMP U/Pb detrital zircons.||||||16-MAR-18
14857|Paradise Creek Formation|22585|6|Mentioned|P739, Fig2, Fig3|||||||||
14857|Paradise Creek Formation|22665|6|Mentioned|P221, Table1||Statherian|Age of unit is 1653+/-7 Ma.||||||22-NOV-06
14857|Paradise Creek Formation|22680|6|Mentioned|84|||Geological province: Mount Isa Basin. Of the McNamara Group.||||||22-NOV-06
14857|Paradise Creek Formation|22747|6|Mentioned|Table1,p7|||With Gunpowder Creek Formation correlates with Suprise Creek Beds and Ploughed Mountain Beds||||||
14857|Paradise Creek Formation|23031|5|Briefly described|53|||Geological province: Lawn Hill Subprovince. Of the McNamara Group. Overlain byEsperanza Formation; underlain by Gunpowder Creek Formation||||||22-NOV-06
14857|Paradise Creek Formation|23073|5|Briefly described|p744 (Fig 2), p745|||||||||
14857|Paradise Creek Formation|23198|6|Mentioned|p873|||||||||
14857|Paradise Creek Formation|23387|6|Mentioned|p18 fig.19|||Of McNamara Group.||||||
14857|Paradise Creek Formation|23393|4|Described|p19, p20|Paleoproterozoic|Paleoproterozoic|Includes the Mount Oxide Chert Member.  Of McNamara Group.||||||07-NOV-08
14857|Paradise Creek Formation|23396|4|Described|p420|Statherian|Statherian|Of the McNamara Group.  Age: 1658+/-3Ma.||||||22-NOV-06
14857|Paradise Creek Formation|23397|5|Briefly described|p469|Statherian|Statherian|||||||
14857|Paradise Creek Formation|23398|4|Described|p447|Statherian|Statherian|Of McNamara Group.  Age: 1659-1653Ma.||||||22-NOV-06
14857|Paradise Creek Formation|23399|5|Briefly described|p493 Fig.3|||Of the McNamara Group.||||||22-NOV-06
14857|Paradise Creek Formation|23405|5|Briefly described|p589|||||||||
14857|Paradise Creek Formation|23406|5|Briefly described|p611|||Geological province: Lawn Hill Platform. Includes deep to shallow marine carbonates.||||||16-JUN-09
14857|Paradise Creek Formation|23407|5|Briefly described|p632|||||||||
14857|Paradise Creek Formation|23408|4|Described|p512|||Of the McNamara Group. Contains numerous reworked tuffaceous beds, which may correlate with upper Mount Isa Group; and also, rhythmically laminated distal tempestite facies, dolomudstone and dolosiltstone.||||||30-MAY-14
14857|Paradise Creek Formation|23409|5|Briefly described|p535 Fig.2|||Of the McNamara Group||||||22-NOV-06
14857|Paradise Creek Formation|23466|5|Briefly described|p267|||||||||
14857|Paradise Creek Formation|23767|5|Briefly described|p1956 Fig. 2|||Geological Province: Western Fold Belt. See also p1957 Fig.3.||||||
14857|Paradise Creek Formation|23958|5|Briefly described|p1134 Fig.2|Mesoproterozoic|Paleoproterozoic|Of McNamara Group.||||||07-NOV-08
14857|Paradise Creek Formation|23964|5|Briefly described|p1265|Proterozoic|Proterozoic|Of McNamara Group.  Geological Province: Mount Isa Inlier.  Maximum thicknees: 500m.||||||
14857|Paradise Creek Formation|23965|5|Briefly described|p1297|Mesoproterozoic|Paleoproterozoic|Of McNamara Group. Geological Province: Mount Isa Inlier.||||||07-NOV-08
14857|Paradise Creek Formation|23986|5|Briefly described|p65|Proterozoic|Proterozoic|Of McNamara Group.||||||
14857|Paradise Creek Formation|24033|6|Mentioned|p25|||||||||
14857|Paradise Creek Formation|24156|5|Briefly described|p18, p19, p22|||Forms plateaux, rises and pediments with lateritic duricrust, mottled zone and ferruginous saprolite.|||||Dolomitic siltstone, minor sandstone and chert.|
14857|Paradise Creek Formation|24308|5|Briefly described|p1002, p987 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of the McNamara Group.   Geological Province:  Mount Isa Superbasin.||||||07-NOV-08
14857|Paradise Creek Formation|24309|5|Briefly described|p1018|Proterozoic|Proterozoic|Of the McNamara Group.||||||22-NOV-06
14857|Paradise Creek Formation|24419|6|Mentioned|p18|||Includes Mount Oxide Chert Member.||||||09-MAR-05
14857|Paradise Creek Formation|24432|4|Described|p562 Fig.2|Statherian|Statherian|Of McNamara Group. Overlain by Esperanza Formation. Age: c. 1658 Ma. Geological Province: Lawn Hill Platform.||||||
14857|Paradise Creek Formation|29969|5|Briefly described|p392|||||||||
14857|Paradise Creek Formation|30354|6|Mentioned|p9|||Refers to micropalaeontology.||||||
14857|Paradise Creek Formation|30535|6|Mentioned|p404|||Refers de Keyser(1958)||||||
14857|Paradise Creek Formation|30778|6|Mentioned|Fig.3|||||||||
14857|Paradise Creek Formation|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
14857|Paradise Creek Formation|31207|6|Mentioned|p1414|||||||||
14857|Paradise Creek Formation|31342|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
14857|Paradise Creek Formation|31396|6|Mentioned|p1188|||||||||
14857|Paradise Creek Formation|31704|6|Mentioned|p4|||Favourable horizon for copper||||||
14857|Paradise Creek Formation|31821|5|Briefly described|p1024|||||||||
14857|Paradise Creek Formation|31877|5|Briefly described|p378|||||||||
14857|Paradise Creek Formation|32264|5|Briefly described|p383|||||||||
14857|Paradise Creek Formation|32287|6|Mentioned|Fig. 1|||||||||
14857|Paradise Creek Formation|32478|6|Mentioned|p223|||||||||
14857|Paradise Creek Formation|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
14857|Paradise Creek Formation|32660|5|Briefly described|Table 5|||||||||
14857|Paradise Creek Formation|32722|6|Mentioned|Fig.2|||Carpentarian. Stromatolite||||||
14857|Paradise Creek Formation|32959|6|Mentioned|Fig.21|||||||||
14857|Paradise Creek Formation|33111|6|Mentioned|p28|||||||||
14857|Paradise Creek Formation|33900|5|Briefly described|p15|||||||||
14857|Paradise Creek Formation|34395|6|Mentioned|Map legend|Early Paleozoic|Early Paleozoic|||||||07-NOV-08
14857|Paradise Creek Formation|34754|6|Mentioned|p42|||||||||
14857|Paradise Creek Formation|34891|6|Mentioned|p240|||||||||
14857|Paradise Creek Formation|35001|6|Mentioned|Fig.45|||||||||
14857|Paradise Creek Formation|35004|6|Mentioned|p266|||||||||
14857|Paradise Creek Formation|35032|6|Mentioned|p117|||||||||
14857|Paradise Creek Formation|35074|6|Mentioned|Fig.2|||||||||
14857|Paradise Creek Formation|35115|6|Mentioned|p207|||||||||
14857|Paradise Creek Formation|35261|6|Mentioned|p338|||||||||
14857|Paradise Creek Formation|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
14857|Paradise Creek Formation|36715|6|Mentioned|p13|||||||||
14857|Paradise Creek Formation|37371|6|Mentioned|p368|||||||||
14857|Paradise Creek Formation|37459|1|Redefined|p428|Mesoproterozoic|Mesoproterozoic|Age is more specifically Carpentarian||||||
14857|Paradise Creek Formation|37555|6|Mentioned|p2|||||||||
14857|Paradise Creek Formation|37569|5|Briefly described|p91|||||||||
14857|Paradise Creek Formation|37572|6|Mentioned|Fig.7|||||||||
14857|Paradise Creek Formation|38232|6|Mentioned|p89|||||||||
14857|Paradise Creek Formation|38237|4|Described|p128|||||||||
14857|Paradise Creek Formation|38243|6|Mentioned|p354|||||||||
14857|Paradise Creek Formation|38276|6|Mentioned|Fig.1|||||||||
14857|Paradise Creek Formation|38291|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
14857|Paradise Creek Formation|38348|4|Described|p10|||||||||
14857|Paradise Creek Formation|38444|5|Briefly described|p105|||||||||
14857|Paradise Creek Formation|38446|4|Described|p186|||||||||
14857|Paradise Creek Formation|38584|6|Mentioned|p22|||||||||
14857|Paradise Creek Formation|39125|6|Mentioned|p163|||||||||
14857|Paradise Creek Formation|39210|6|Mentioned|Table 3|||||||||
14857|Paradise Creek Formation|39445|5|Briefly described|Table 2|||See also p41.||||||22-NOV-06
14857|Paradise Creek Formation|39492|6|Mentioned|p31|||||||||
14857|Paradise Creek Formation|39497|6|Mentioned|Fig.4|||||||||
14857|Paradise Creek Formation|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of McNamara Gp. Includes Mount Oxide Chert Member at base. Stromatolitic dolomite, dolomitic siltstone, some some limestone interbeds, dolomite with chert nodules after.... Overlain by Esperanza Formation; overlies Gunpowder Creek Fm.||||||15-JUN-06
14857|Paradise Creek Formation|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
14857|Paradise Creek Formation|39925|6|Mentioned|Fig.9|||||||||
14857|Paradise Creek Formation|39943|6|Mentioned|Table 1A|||||||||
14857|Paradise Creek Formation|39944|3|Fully described|p238|||||||||
14857|Paradise Creek Formation|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
14857|Paradise Creek Formation|40221|3|Fully described|p15|||||||||
14857|Paradise Creek Formation|40394|6|Mentioned|p285|||||||||
14857|Paradise Creek Formation|40623|5|Briefly described|p96|||||||||
14857|Paradise Creek Formation|40858|6|Mentioned|p136|||||||||
14857|Paradise Creek Formation|41298|6|Mentioned|Map legend|Carpentarian||||||||
14857|Paradise Creek Formation|41862|6|Mentioned|p474|||||||||
14857|Paradise Creek Formation|42166|6|Mentioned|p108|||||||||
14857|Paradise Creek Formation|43235|5|Briefly described|p9,Fig.10.|||Of the McNamara Group.||||||22-NOV-06
14857|Paradise Creek Formation|44091|14|Not recorded|p10||Mesoproterozoic|||||||
14857|Paradise Creek Formation|44115|14|Not recorded|p17|||||||||
14857|Paradise Creek Formation|44210|2|Defined|Tb.1,p9,map|||||||||
14857|Paradise Creek Formation|44213|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
14857|Paradise Creek Formation|44216|14|Not recorded|p385|||Dolomite and dolomitic sandstone.||||||
14857|Paradise Creek Formation|44271|2|Defined|p35,36,41|||Overlies Gunpowder Creek Formation.||||||
14857|Paradise Creek Formation|44275|14|Not recorded|Map Legend|||||||||
14857|Paradise Creek Formation|44279|14|Not recorded|Tb.1|||||||||
14857|Paradise Creek Formation|44290|2|Defined|p438,439|||Precambrian probably Palaeoproterozoic.||||||
14857|Paradise Creek Formation|44521|14|Not recorded|p8,21,map|||upper Early Proterozoic.||||||
14857|Paradise Creek Formation|44526|14|Not recorded|p253|||Probably contemporaneous in part with Mount Isa Shale.||||||
14857|Paradise Creek Formation|44552|14|Not recorded|p9|||||||||
14857|Paradise Creek Formation|44587|14|Not recorded|p381|||Affected by laterisation.||||||
14857|Paradise Creek Formation|44751|14|Not recorded|p302|||Dolomitic, with numerous stromatolites. A little younger than the 1st main deformation of the area.||||||
14857|Paradise Creek Formation|44788|14|Not recorded|p9|||||||||
14857|Paradise Creek Formation|44989|2|Defined|p.35,39,42,53-255|||Tb.II,III. On many pages. (E54-13,F54-1). Pl.15,22.||||||
14857|Paradise Creek Formation|45287|14|Not recorded|p.225,226||Paleoproterozoic|||||||07-NOV-08
14857|Paradise Creek Formation|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
14857|Paradise Creek Formation|47083|3|Fully described|p15-16||Proterozoic|Equivalent to Paradise Fm of Cavaney (1975). Of McNamara Gp. Overlain by Esperanza Fm; underlain by Gunpowder Creek Fm. Max. thickness 750 m.||||||22-NOV-06
14857|Paradise Creek Formation|50332|6|Mentioned|p21|Proterozoic|Proterozoic|Includes the Mount Oxide Chert Member.||||||07-FEB-11
14857|Paradise Creek Formation|50550|5|Briefly described|p1139 Fig.2, p1143 Fig.6||Statherian|Age: 1659 Ma, 1657Ma. Overlies Mount Oxide Chert conformably. Conformably overlain by Esperanza Formation. Geological Province: Western Fold Belt.||||||19-DEC-07
14857|Paradise Creek Formation|50600|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the McNamara Group.  Laminated dolomite and silicified siltstone.  Overlies Gunpowder Creek Formation; overlain by Esperanza Formation.||||||28-JUN-04
14857|Paradise Creek Formation|60558|5|Briefly described|p5 Fig. 4|||Of McNamara Group. Overlain by Esperanza Formation, underlain by Gunpowder Creek Formation.||||||
14857|Paradise Creek Formation|61732|5|Briefly described|p25|||Superseded by Esperanza Formation.  Contains microfossils in stromatolites. In the Mount Isa region.||||||07-FEB-11
14857|Paradise Creek Formation|61936|5|Briefly described|p194 Fig. 6|||Geological Province: Lawn Hill Platform, Western Fold Belt, Mount Isa Inlier.||||||
14857|Paradise Creek Formation|62084|4|Described|p936 Fig.5|||Isa Superbasin. Lawn Hill. Shown as Paradise Ck Fm.|1658+/-3 Ma U-Pb SHRIMP (after Page et al. 2000)|McNamara Group|||Platform carbonates.|
14857|Paradise Creek Formation|62535|5|Briefly described|p672|Statherian|Statherian|Lawn Hill Platform. Two other similar ages are given.|1654 +/- 4 Ma.|McNamara Group.||||
14857|Paradise Creek Formation|63023|6|Mentioned|p1037|Paleoproterozoic|Paleoproterozoic|Age: ca 1660-1655Ma. Of the Gun Supersequence.||||||07-NOV-08
14857|Paradise Creek Formation|63109|6|Mentioned|p1108 Fig. 3|||Geological Province: Isa Superbasin.||||||30-SEP-08
14857|Paradise Creek Formation|63111|5|Briefly described|p1163 Fig. 3|Statherian|Statherian|Of Gun Supersequence. Ages: 1668 - 1653Ma. Geological Province: Isa Superbasin. Laminated fine-grained sanstone and siltstones, dolomudstones, laminated carbonates.||||||07-FEB-11
14857|Paradise Creek Formation|63113|6|Mentioned|p1214 Fig.2, p1225 Fig.13. |||Part of Gun supersequence. Appears in Fig.2 only as Par. Ck.|c.1657 Ma.|Of the McNamara Group||||
14857|Paradise Creek Formation|63114|5|Briefly described|p1253 Fig.2. |||Isa superbasin.||||||
14857|Paradise Creek Formation|63115|6|Mentioned|p1279 Fig.4.|||Isa superbasin.||||||
14857|Paradise Creek Formation|63116|6|Mentioned|p1297 Fig.2, p1299 Tb.1, p1300 |||Isa superbasin. Material properties detailed.||||||
14857|Paradise Creek Formation|63866|5|Briefly described|p57-p58|Statherian|Statherian|Isa Superbasin.|1657 +/- 3 Ma (Page et al., 2000)|Gun Supersequence||||
14857|Paradise Creek Formation|63884|5|Briefly described|p14|||Mainly dolomitic. In contact with Gunpowder Creek Formation. Equivalent to Urquhart Shale.||||||
14857|Paradise Creek Formation|64250|6|Mentioned|p11 fig 3||||1658 +/- 3 Ma - 1653 +/- 7 Ma.|Unit in McNamara Group.||||
14857|Paradise Creek Formation|64575|6|Mentioned|p665|||||||||
14857|Paradise Creek Formation|65337|6|Mentioned|p30, p33.||||> c.1654 Ma.|||Overlies Gunpowder Creek Formation. Is overlain by Esperanza Formation.||
14857|Paradise Creek Formation|65396|5|Briefly described|p82, p175, p195, p241|Statherian|Statherian|Isa Superbasin. Cover Sequence 3. Lawn Hill Platform. Detrital zircon sources listed.|1654 +/- 3 Ma|McNamara Group||Overlies Upper Gunpowder Creek Formation; overlain by Esperanza Formation.||04-APR-17
14857|Paradise Creek Formation|66844|5|Briefly described|p243-244,251-254, 267-268,271,273|||Lawn Hill Platform. SHRIMP zircon ages of 1653+\-7, 1654+\-3, 1658+\-3 and 1659+\-3 Ma. Lower part coincides with decline in accommodation rates and reduction of siliciclastic influx, leading to carbonate facies deposition from Gun 1.5. Stromatolites, present at specific horizons, are dominantly domal-columnar, indicative of shallow sub-tidal and peritidal environments.||Of lower McNamara Group; Within Gun supersequences.|Informally subdivided into upper and lower parts.||Includes quartz peloid grainstone; intraclast grainstone; quartz arenite-intraclast grainstone; microbial laminite; domal stromatolites with quartz peloid grainstone and dolomudstone.|
14857|Paradise Creek Formation|67323|5|Briefly described|GIS attrib tbl,  p26, p34, p60|Paleoproterozoic|Paleoproterozoic|See also Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Mount Isa Inlier, Isa Superbasin.|1659 +/- 3 Ma to 1653 +/- 7 Ma.|Of McNamara Group.|||Stromatolitic dolomite, dolomitic siltstone, some limestone interbeds, dolomite with chert nodules after anhydrite; minor pink to grey fine tuff.|
14857|Paradise Creek Formation|68020|6|Mentioned|p125|||Includes Lady Annie and Mount Kelly group of Cu +/- Au deposits.||||Correlated with lower Mount Isa Group.||
14857|Paradise Creek Formation|68542|5|Briefly described|p6|||||Lower McNamara Group||Overlain by Esperanza Formation, overlies Gunpowder Creek Formation|Dolomitic siltstone and sandstone.|
14857|Paradise Creek Formation|68576|5|Briefly described|Q_2: p6-7|||Lawn Hill Platform, Mount Isa Inlier.||Lower McNamara Group.||Overlies Gunpowder Creek Formation. Is overlain by Esperanza Formation.|Dolomitic siltstone and sandstone.|
14857|Paradise Creek Formation|68732|6|Mentioned|p162, p163, p165 Fig.3, p168 Fig.5, p169|Statherian|Statherian|Of the Gun Supersequence. Ages for pinkites in this formation range from 1658 +/- 3 Ma to 1654 +/- 3 Ma. Sedimentary depositional ages.|1658 +/- 3, 1653 +/- 7, 1654 +/- 4, 1657 +/- 3 Ma|Of the McNamara Group.|||Contains stromatolitic bioherms and biostromes.|01-DEC-17
14857|Paradise Creek Formation|69591|4|Described|p42-45, p54, p88|||Isa Superbasin. Deposited on a shallow carbonate platform: deep marine/tempestites to peritidal deposits. Contains Conophytons. Part of Gun Supersequence.|1657 +/- 3 Ma (MDA: Page et al., 2000).|McNamara Group.||Overlies Gunpowder Creek Formation. Is overlain by Esperanza Formation.|Stromatolitic dolomite, dolomitic siltstone, some limestone interbeds, dolomite with chert nodules after anhydrite; minor pink to grey fine tuff.|
14857|Paradise Creek Formation|70864|5|Briefly described|p75, 74 Fig 2, p77, 78, 80,81,82,84,100|Mesoproterozoic||Breccia hosted Fe and Cu Sulphide mineralization.||McNamara Group|||Stromatolitic dolostone, dolomitic and carbonaceous siltstone, chert and sandstones.|
14857|Paradise Creek Formation|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1653+/-7 Ma (crystallisation: U-Pb zircon SHRIMP)||||Ash tuff.|
14857|Paradise Creek 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. 4 sedimentary depositional ages listed for this unit. Oldest and youngest listed in age field.|1658 +/- 3 Ma to 1653 +/- 7 Ma|McNamara Group||Overlies upper Gunpowder Formation and underlies Esperanza Formation.||
14857|Paradise Creek Formation|72527|6|Mentioned|p91, p105.|Statherian|Statherian|In Lawn Hill 1:250 K sheet area. Depositional age suggested as being simliar to Drummond Formation.|1658-1653 Ma (Page et al., 2000)|McNamara Group||Suggested to be laterally equivalent with Brumby and Drummond Formation.||
14857|Paradise Creek 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. Four U-Pb zircon sedimentary depositional ages given for this unit on p5 are shown for the overlying Esperanza Formation on p33.|1658 +/- 3 Ma to 1653 +/- 7 Ma|McNamara Group||Overlies Gunpowder Creek Formation and underlies Esperanza Formation.|Includes dolostone.|
14857|Paradise Creek 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.||McNamara Group||Overlies Gunpowder Creek Formation and underlies Esperanza Formation.|Includes dolostone.|
14857|Paradise Creek Formation|72919|6|Mentioned|p56, p63|||Mount Isa Province. Tuff crystallisation age of ca. 1658 Ma reported by Page et al. (2000).||||||
14857|Paradise Creek 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, 1654+/-3, 1653+/-7, 1658+/-3 Ma|McNamara Group||Underlain by Gunpowder Formation. Overlain by Esperanza Formation.||
14857|Paradise Creek Formation|73144|6|Mentioned|p8-9|Statherian|Statherian|Isa Superbasin. Part of the Gun Supersequence. Partial aquifer.||McNamara Group||Underlain by Gunpowder Creek Formation. Overlain by Esperanza Formation.||
14857|Paradise Creek Formation|73525|5|Briefly described|p4-5 Fig.2|Statherian|Statherian|Mount Oxide-(Ardmore-May Downs) Domain.|1658+/-3 Ma, 1657+/-3 Ma, 1653+/-7 Ma||||Carbonates.|
14869|Pargee Sandstone|22446|5|Briefly described|p20|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
14869|Pargee Sandstone|23809|4|Described|p9, p4|Paleoproterozoic|Paleoproterozoic|Interbedded conglomerate, quartz arenite and minor siltstone. Overlain by Gardiner Sandstone; unconformably overlies Killi Killi Formation.  Age: 1835Ma (inferred by Blake et al, 1999); <1845-1840Ma (Cooper and Ding, 1997).||||||07-NOV-08
14869|Pargee Sandstone|29809|6|Mentioned|Table 1|||||||||
14869|Pargee Sandstone|29811|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
14869|Pargee Sandstone|29812|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
14869|Pargee Sandstone|29813|4|Described|Table 2|||||||||
14869|Pargee Sandstone|29818|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
14869|Pargee Sandstone|31361|4|Described|Table 2|||||||||
14869|Pargee Sandstone|31362|4|Described|Table 1|||||||||
14869|Pargee Sandstone|33102|6|Mentioned|Fig.2|||||||||
14869|Pargee Sandstone|36473|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
14869|Pargee Sandstone|36532|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
14869|Pargee Sandstone|36902|6|Mentioned|p12|||||||||
14869|Pargee Sandstone|37462|6|Mentioned|p279|||||||||
14869|Pargee Sandstone|39887|6|Mentioned|p452|||||||||
14869|Pargee Sandstone|41125|6|Mentioned|p30|||||||||
14869|Pargee Sandstone|41883|5|Briefly described|p65|||||||||
14869|Pargee Sandstone|42643|6|Mentioned|p5|||||||||
14869|Pargee Sandstone|43631|6|Mentioned|p10|||||||||
14869|Pargee Sandstone|45112|6|Mentioned|p17|||||||||
14869|Pargee Sandstone|45140|2|Defined|p12-15, 17-18, p20, p22, p39, p41, p43|Paleoproterozoic|Paleoproterozoic|See also p54, p73, Appx.p8. Blake et al. (1975). The Granites-Tanami Block. Named after Pargee Range. The type section runs for 800m along a gully between 19deg 38'20"S, 129deg 12'30"E and 19deg 38'30"S, 129deg 12'15"E, Tanami sheet area. 1500m thick. Crops out as strike ridges up to 30m high, most extensively W and S of Pargee Range. Mainly steeply-dipping to overturned and tightly folded.|c.1800 Ma.|||Unconformably overlies Killi Killi and Mount Charles Beds (Tanami Complex). Is overlain unconformably by Gardiner and Muriel Range Sandstones.|Interbedded sublithic, lithic, and quartz arenite, conglomerate and greywacke. Arenites are mainly poorly sorted and medium-coarse grained; beds about 1m thick with common cross-bedding and ripple marks.|
14869|Pargee Sandstone|45167|5|Briefly described|Fig.27|||||||||
14869|Pargee Sandstone|46830|6|Mentioned|p29|||||||||
14869|Pargee Sandstone|46864|5|Briefly described|p37|||||||||
14869|Pargee Sandstone|48950|2|Defined|p22|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
14869|Pargee Sandstone|50315|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Conglomerate, sandstone and siltstone; sublithic and lithic arenite, quartz arenite; cream, pink, purple; sandstone poorly sorted, medium- to coarse-grained; conglomerate contains jasper clasts.||||||07-NOV-08
14869|Pargee Sandstone|50374|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Conglomerate, sandstone and siltstone; sublithic and lithic arenite, quartz arenite.||||||07-NOV-08
14869|Pargee Sandstone|50376|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
14869|Pargee Sandstone|50589|6|Mentioned|p2.1|||||||||
14869|Pargee Sandstone|60676|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Conglomerate, sandstone and siltstone: sublithic and lithic arenite, quartz arenite.||||||07-NOV-08
14869|Pargee Sandstone|61056|5|Briefly described|p777|||Overlies the Tanami Group.||||||
14869|Pargee Sandstone|61861|3|Fully described|p15-17, 3, 4,10,12,23, Figs.23-28, Map 1|Orosirian|Orosirian|Deposited in small extensional basins on top of deformed MacFarlane Peak and Tanami Groups. Non- to weakly magnetic. Deposition post-dates folding of Tanami Group, hence age is less than 1840 Ma. Tentatively correlated with Moola Bulla Formation.|1835 Ma inferred from correlation|||Unconformably overlies Dead Bullock Formation, Killi Killi Formation. Unconformably overlain by the Gardiner Sandstone, Birrindudu Group.|Dominated by interbedded thick-bedded quartz and lithic arenites and conglomerate. Pebbly sandstone and conglomerate are prominent at base. Most clasts are subrounded vein quartz, greywacke, siltstone and jasper derived from Killi Killi Formation.|
14869|Pargee Sandstone|62377|4|Described|p5, 7|Paleoproterozoic|Paleoproterozoic|Unconformably overlies Tanami Group. Quartz sandstone, lithic arenite and conglomerate. Unconformably overlain by Birrindudu Group. Overlies Killi Killi Formation and Dead Bullock Formation. Age : 1734 +/- 25Ma.||||||07-NOV-08
14869|Pargee Sandstone|62580|6|Mentioned|p10, p21|||Shallow marine sediments.||||||07-FEB-11
14869|Pargee Sandstone|62628|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Birrindudu Basin. Sandstone, conglomerate, siltstone: sublithic and lithic arenite, quartz arenite, jasperlitic conglomerate.||||||07-NOV-08
14869|Pargee Sandstone|63261|3|Fully described|p9 Fig. 5, p16|Paleoproterozoic|Paleoproterozoic|Unconformably overlain by Gardiner Sst (Birrindudu Gp); unconformable on Killi Killi Sst. Max dep age: 1768+/-14Ma. Thick succession of interbedded conglomerate, pebbly sandstone, quartz arenite + minor siltstone - more lith.detail included.||||||07-FEB-11
14869|Pargee Sandstone|63866|6|Mentioned|p99|||||||||
14869|Pargee Sandstone|64277|5|Briefly described|Map ledgend|Paleoproterozoic|Paleoproterozoic|Age: <1760Ma. Siltstone and mudstone; minor fine-grained, micaceous quartz sandstone. Conglomerate, cross-bedded sandstone and quartz sandstone and shale; minor dolomitic sandstone.||||||
14869|Pargee Sandstone|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Sandstone; minor conglomerate.||||||09-DEC-08
14869|Pargee Sandstone|64662|5|Briefly described|p28, p30 Fig. 3, p40, 44|Statherian|Statherian|Age: ~1.77 - 1.64 Ga, based on combo of youngest detrital zircons dates, diagenetic xenotime growth, age of Limbunya Group rocks (which overlie Birrindudu Group). Sandstone and conglomerate. Unconformably overlain by Gardiner Sandstone. Tanami region.||||||07-FEB-11
14869|Pargee Sandstone|64675|5|Briefly described|p9, p10, Fig.2, p16, Fig.24, p17, p24|Paleoproterozoic|Paleoproterozoic|Forms a prominent north-northeast orientated strike ridge east of the Pargee Fault. A high energy molasse deposit consistent with sedimentation in response to active deformation and uplift of underlying basement groups (Hendrickx et al 2000). See also Map 1.||||Unconformably underlain by the Tanami Complex. Unconformably underlain by the Killi Killi Formation.|Fines rapidly upward from thick bedded pebbly conglomerate (with vein quartz, chert and red jasper clasts) to quartz gritstone and medium to fine grained sandstone and siltstone.|19-MAR-14
14869|Pargee Sandstone|64722|5|Briefly described|Fig. 2 p3-6, p10|Statherian|Statherian|Maximum age from youngest detrital zircon (Cross and Crispe, 2007). Minimum age from Limbunya Group which lies stratigraphically above it. Interpreted as a platformal cover succession.|1768 +/- 14 Ma maximum.|||Unconformably overlain by Birrindudu Group.||11-APR-12
14869|Pargee Sandstone|64725|5|Briefly described|p63 Fig.7.|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|<1735 Ma.|||||
14869|Pargee Sandstone|64733|5|Briefly described|p170 Fig.2, p172 Fig.4, p175|Statherian|Statherian||~1765-1630 Ma.|||Unconformably overlies Mount Charles Formation and unconformably overlain by Birrindudu Group.||20-APR-12
14869|Pargee Sandstone|64734|5|Briefly described|p186 Fig.1||Statherian|<1735 Ma||||||14-SEP-09
14869|Pargee Sandstone|64956|6|Mentioned|p7|||In Tanami region.||||||07-FEB-11
14869|Pargee Sandstone|65074|6|Mentioned|p349, p351 fig 4-37|Proterozoic|Proterozoic|Of North/Centre Birrindudu Basin. Early Proterozoic. 1500 m thick.||||Unconformably overlain by Gardiner Sandstone.|Arenites, pebbly conglomerates.|
14869|Pargee Sandstone|65323|5|Briefly described|Map legend|Orosirian|Orosirian|Conglomerate, sandstone, siltstone; non to weakly magnetic||||||02-FEB-10
14869|Pargee Sandstone|65324|6|Mentioned|Map legend|Orosirian|Orosirian|Not shown on map||||||
14869|Pargee Sandstone|65326|6|Mentioned|Map legend|Orosirian|Orosirian|Not shown on map||||||02-FEB-10
14869|Pargee Sandstone|65327|6|Mentioned|Map legend|Orosirian|Orosirian|Not shown on map||||||
14869|Pargee Sandstone|65328|6|Mentioned|Map legend|Orosirian|Orosirian|Not shown on map||||||
14869|Pargee Sandstone|65338|6|Mentioned|p21.|||Tanami Region. Previously, correlated with Reynolds Range Group (Blake et al. 1979).||||||
14869|Pargee Sandstone|65349|6|Mentioned|Map legend|Orosirian|Orosirian|Not shown on map||||||
14869|Pargee Sandstone|65350|6|Mentioned|Map legend|Orosirian|Orosirian|Not shown on map||||||
14869|Pargee Sandstone|65351|6|Mentioned|Map legend|Orosirian|Orosirian|Not shown on map||||||
14869|Pargee Sandstone|65352|5|Briefly described|Map legend|Orosirian|Orosirian|Conglomerate, sandstone, siltstone; non to weakly magnetic||||||
14869|Pargee Sandstone|65353|5|Briefly described|Map legend|Orosirian|Orosirian|Conglomerate, sandstone, siltstone; non to weakly magnetic||||||02-FEB-10
14869|Pargee Sandstone|65354|6|Mentioned|Map legend|Orosirian|Orosirian|Not shown on map||||||
14869|Pargee Sandstone|65355|6|Mentioned|Map legend|Orosirian|Orosirian|Not shown on map||||||
14869|Pargee Sandstone|65356|5|Briefly described|Map legend|Orosirian|Orosirian|Not shown on map||||||
14869|Pargee Sandstone|65358|5|Briefly described|p7|Statherian|Statherian|In Tanami Region. Quartz sandstone, lithic arenite and conglomerate. Represents syn-tectonic sedimentation during the 1730 Ma Strangways Orogeny.||||||
14869|Pargee Sandstone|66129|5|Briefly described|p213, p214 Fig.1, p216 Fig.3|Statherian|Statherian|1758-1700 Ma. Unconformably underlies Birrindudu Group, unconformably overlies Ware Group.||||||
14869|Pargee Sandstone|66468|5|Briefly described|p16-17 Figs.2-4, p19, p21 Fig.6, p22|Statherian|Statherian|<1735 Ma. 1760 Ma (detrital zircon) to 1632 +/-3 Ma (diagenetic xenotime). ~1300m thick. Underlies Birrindudu Group unconformably.||||||
14869|Pargee Sandstone|66860|6|Mentioned|p6 Tb.1|||Tanami Region. Coeval with deposition of Ledan and (?) Oonagalabi packages (Arunta Region), and Hanlon Subgroup and upper parts of Tomkinson Creek Group (Tennant Region).||||||
14869|Pargee Sandstone|67168|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||||Unconformably overlies Tanami Group units. Is unconformably overlain by Gardiner Sandstone and Muriel Range Sandstone.|Conglomerate, sandstone, siltstone.|
14869|Pargee Sandstone|67824|6|Mentioned|p385 Fig.2|Paleoproterozoic|Orosirian||< 1735 Ma|||||
14869|Pargee Sandstone|67826|6|Mentioned|p401 Fig.2, p403|Statherian|Statherian|Relatively flat-lying sedimentary rocks.|~ 1770-1640 Ma|||||
14869|Pargee Sandstone|68474|6|Mentioned|p572|Palaeoproterozoic|Palaeoproterozoic|Granites-Tanami Orogen.|<1735 Ma|||||
14869|Pargee Sandstone|68656|5|Briefly described|GEOL_LUT_CSV/100k_interpgeop_lut|Paleoproterozoic|Paleoproterozoic|See also 500k_geologyp08_lut.|||||Siltstone and mudstone; minor fine-grained, micaceous quartz sandstone; conglomerate; cross-bedded sandstone; minor dolomitic sandstone.|
14869|Pargee Sandstone|68733|6|Mentioned|p186, p187 Fig.6|||Tanami region.||||Unconformably overlain by the Birrindudu Group. Unconformably underlain by the Mount Charles Formation.||05-DEC-17
14869|Pargee Sandstone|69099|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic||||||Sandstone; minor conglomerate.|04-AUG-15
14869|Pargee Sandstone|69253|5|Briefly described|p747 Fig.1, p748-749|Paleoproterozoic|Paleoproterozoic||< 1735 Ma.|||Unconformably overlies Tanami Group. Is overlain unconformably by Birrindudu Group.|Sandstone and conglomerate.|
14869|Pargee Sandstone|69383|6|Mentioned|p70|||Tanami Region. Detrital zircon spectra compared to Utopia Quartzite spectra.||||||
14869|Pargee Sandstone|69426|5|Briefly described|p11:3, 5, 7, 10, 14|||Crops out on W side of Coomarie Dome. SHRIMP U-Pb (detrital) zircon maximum depositional age.|<1768 +/- 14 Ma (Cross and Crispe, 2007).|||Unconformably overlies Killi Killi Formation. Is overlain unconformably by Gardiner Sandstone.|Interbedded shallow-marine to fluvial conglomerate, quartz sandstone and minor siltstone.|12-JUL-16
14869|Pargee Sandstone|69431|6|Mentioned|p16:1|||Tanami Region. Possible correlative of Hatches Creek Group and, by inference, Tomkinson Creek Group.||||||12-JUL-16
14869|Pargee Sandstone|69432|5|Briefly described|p17:2|||Youngest detrital zircon maximum depositional age.|1768 +/- 14 Ma (Cross and Crispe, 2007).|||Is overlain unconformably by the Birrindudu Group.||12-JUL-16
14869|Pargee Sandstone|69587|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: North Australian Craton. Events: Alice Springs Orogeny. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|1760-1735 Ma (inferred)||||Siltstone and mudstone; minor fine-grained, micaceous quartz sandstone, cross-bedded sandstone, conglomerate, minor dolomitic sandstone, shale.|
14869|Pargee Sandstone|69618|6|Mentioned|p90|Paleoproterozoic|Paleoproterozoic||<1735 Ma.|||||
14869|Pargee Sandstone|69747|5|Briefly described|p263||Paleoproterozoic|Geological province: Tanami Block, North Australian Craton.|< 1735 Ma|||||
14869|Pargee Sandstone|69917|6|Mentioned|p87|||Tanami Region. One of a number of North Australian Craton sources of zircons older than 1900 Ma.||||||
14869|Pargee Sandstone|70141|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|These three facies are mapped separately.|1760-1735 Ma.||||Conglomerate, cross-bedded sandstone and quartz sandstone, siltstone and shale; minor dolomitic sandstone. Siltstone and mudstone; minor fine-grained, micaceous quartz sandstone. Quartz sandstone.|
14869|Pargee Sandstone|70143|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic||||||Conglomerate; cross-bedded sandstone and quartz sandstone, siltstone and shale; minor dolomitic sandstone.|
14869|Pargee Sandstone|70154|5|Briefly described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic||1735-1760 Ma||||Sandstone; minor conglomerate|
14869|Pargee Sandstone|70291|4|Described|p178,180-181|Paleoproterozoic|Paleoproterozoic|Geological province: Tanami. Maximum depositional age of ~1735 Ma (but also suggested to be 1758+\-15 Ma; cross and Crispe, 2006?). Also constrained by a 1632+\-3 Ma age of xenotime associated with epigenetic REE-Th-U mineralisation (Vallini et al. 2006). Coeval with Fiddler Lake Granite emplacement.|<1735 Ma|||Overlain unconformably by Birrindudu Group.|Interbedded conglomerate, quartz arenite and minor siltstone|
14869|Pargee Sandstone|70852|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region.|||||Sandstone, conglomerate, siltstone; sublithic and lithic sandstone, quartz sandstone, conglomerate with jasperlitic and volcanic clasts.|
14869|Pargee Sandstone|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Events: North Australian Craton events (2500-250 Ma); Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Kalkarindji Supersuite Magmatic Event (511-511 Ma); Yampi Orogeny (1000-800 Ma). See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|1760-1735 Ma (inferred)||||Cross bedded, medium to coarse and locally pebbly sublithic sandstone with minor conglomerate|
14869|Pargee Sandstone|71348|5|Briefly described|p217|Paleoproterozoic|Paleoproterozoic|Geological province: Tanami Region, North Australian Craton. Maximum depositional age c. 1780 Ma Maidment et al., 2005; Cross and Crispe, 2007; Hollis et al., 2013; Kositcin et al., 2015).|< 1780 Ma.|||||
14869|Pargee Sandstone|71349|5|Briefly described|p724-725, p737|Paleoproterozoic|Paleoproterozoic|Tanami Region. Relatively flat-lying sedimentary rocks. Contains zircons aged c.3.1 Ga (significance explained).|1758-1700 Ma.|||||
14869|Pargee Sandstone|71397|6|Mentioned|p5|Statherian|Statherian|Geological province: Granites-Tanami Orogen.||||||
14869|Pargee Sandstone|71592|5|Briefly described|Appendix A.|||Tanami Orogen.|1768+/-14 Ma (MDA: U-Pb zircon SHRIMP)||||Quartz arenite.|
14869|Pargee Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic||||||Sandstone; minor conglomerate.|
14869|Pargee Sandstone|73083|6|Mentioned|p24|||Intruded by granite of the Tanami Orogen.||||||
14869|Pargee Sandstone|73089|4|Described|p3, p6-10, p29-31|Statherian|Statherian|Restricted area west of Coomarie Dome. 1.5 km thick. High energy shallow marine to fluvial depositional setting. Broadly coarsens up sequence. Post-dates granitic magmatism.|< c.1768 Ma|||Unconformably underlain by Killi Killi Formation. Unconformably overlain by Gardiner Sandstone.|Thickly bedded quartz arenite, lithic arenite, conglomerate, minor siltstone. Interbedded quartz-rich to lithic sandstone, conglomerate and minor siltstone.|
14883|Parke Siltstone|9814|5|Briefly described|Map Legend|Devonian|Devonian|Of the Pertnjara Group. Sandstone, siltstone.||||||
14883|Parke Siltstone|12891|5|Briefly described|p733 Fig. 2|Middle Devonian|Middle Devonian|Geological province: Amadeus Basin.||||||07-FEB-11
14883|Parke Siltstone|22560|5|Briefly described|p3||Middle Devonian|||||||
14883|Parke Siltstone|22561|5|Briefly described|p23||Devonian|Of the Pertnjara Group.||||||22-NOV-06
14883|Parke Siltstone|22565|6|Mentioned|p71 in Table 1|||Approx. thickness measured from seismic data - 400m.||||||
14883|Parke Siltstone|22566|5|Briefly described|p73|Devonian|Devonian|Of the Pertnjara Group.||||||22-NOV-06
14883|Parke Siltstone|22646|6|Mentioned|p 105|Devonian|Devonian|Of the Pertnjara Group.||||||22-NOV-06
14883|Parke Siltstone|22650|6|Mentioned|Fig 2 on p 157|Devonian|Devonian|Of the Pertnjara Group.||||||22-NOV-06
14883|Parke Siltstone|22656|6|Mentioned|p 281|Devonian|Devonian|||||||
14883|Parke Siltstone|22760|5|Briefly described|p339|||Of the Pertnjara Group.||||||22-NOV-06
14883|Parke Siltstone|22761|4|Described|p350|Middle Devonian|Early Devonian|Of the Pertnjara Group.||||||22-NOV-06
14883|Parke Siltstone|22763|6|Mentioned|Table 1 on p386||Late Devonian|Of the Pertnjara Group.||||||22-NOV-06
14883|Parke Siltstone|22804|6|Mentioned|p454|Late Devonian|Middle Devonian|Of the Pertnjara Group.||||||22-NOV-06
14883|Parke Siltstone|22805|5|Briefly described|p465||Middle Devonian|Of the Pertnjara Group.||||||22-NOV-06
14883|Parke Siltstone|22806|6|Mentioned|Fig 11 on p485|||||||||
14883|Parke Siltstone|22807|6|Mentioned|Fig 3 on p495|||Of the Pertnjara Group.  Age - (?)Middle Devonian-(?)Late Devonian.||||||22-NOV-06
14883|Parke Siltstone|22824|5|Briefly described|p526|||||||||
14883|Parke Siltstone|22825|6|Mentioned|Fig 1 on p542|||Of the Pertnjara Group.||||||22-NOV-06
14883|Parke Siltstone|22826|6|Mentioned|p575|Devonian|Devonian|||||||
14883|Parke Siltstone|23361|5|Briefly described|16 Fig.4|Early Carboniferous|Early Devonian|Age: 400-350Ma.||||||22-NOV-06
14883|Parke Siltstone|23858|5|Briefly described|p915|Devonian|Devonian|Of Pertnjara Group. Geological Province: Amadeus Basin.||||||
14883|Parke Siltstone|23979|5|Briefly described|p210|Frasnian|Givetian|||||||
14883|Parke Siltstone|24063|5|Briefly described|p223|||Geological Province: Amadeus Basin.||||||
14883|Parke Siltstone|24334|4|Described|p48 Tb.1, p51|Middle Devonian|Early Devonian|Age: 377 - 391 Ma. Overlies the Mereenie Sandstone. Overlain by the Hermannsburg Sandstone. Geological Province: Amadeus Basin.||||||
14883|Parke Siltstone|24424|5|Briefly described|p539 Tb.4|Middle Devonian|Middle Devonian|Age: 369-384 Ma. Palaeomagnetic poles given.||||||
14883|Parke Siltstone|29972|6|Mentioned|Table 1|||||||||
14883|Parke Siltstone|30238|4|Described|p64|||Upper Devonian - Carboniferous age.||||||22-NOV-06
14883|Parke Siltstone|30544|6|Mentioned|p51|||On map legend||||||
14883|Parke Siltstone|30659|6|Mentioned|p88|||||||||
14883|Parke Siltstone|31566|2|Defined|p231|Devonian|Devonian|See also p232-238.||||||22-NOV-06
14883|Parke Siltstone|31567|6|Mentioned|p280|||Conformable on Langra Formation.||||||22-NOV-06
14883|Parke Siltstone|32208|6|Mentioned|Map legend|Devonian|Devonian|||||||
14883|Parke Siltstone|32209|6|Mentioned|Map legend|Devonian|Devonian|||||||
14883|Parke Siltstone|32640|6|Mentioned|p235|||||||||
14883|Parke Siltstone|32865|6|Mentioned|p482|||U.Dev.||||||
14883|Parke Siltstone|34111|5|Briefly described|Table 2|||Devonian - Carboniferous.||||||22-NOV-06
14883|Parke Siltstone|34442|5|Briefly described|Table 1|||Devonian - Carboniferous.||||||22-NOV-06
14883|Parke Siltstone|35102|6|Mentioned|p22|||||||||
14883|Parke Siltstone|36821|6|Mentioned|p397|||||||||
14883|Parke Siltstone|40740|3|Fully described|p60|||Mention p97. Briefly described p6.||||||22-NOV-06
14883|Parke Siltstone|40810|5|Briefly described|p12|||||||||
14883|Parke Siltstone|41018|6|Mentioned|p234|||||||||
14883|Parke Siltstone|41039|4|Described|p7|||||||||
14883|Parke Siltstone|41190|6|Mentioned|Fig.4|||||||||
14883|Parke Siltstone|41270|6|Mentioned|p277|||||||||
14883|Parke Siltstone|41276|6|Mentioned|p74|||||||||
14883|Parke Siltstone|41385|6|Mentioned|p364|||||||||
14883|Parke Siltstone|41492|6|Mentioned|p119|||||||||
14883|Parke Siltstone|41708|6|Mentioned|Fig.1|||||||||
14883|Parke Siltstone|41717|6|Mentioned|Fig.2|||||||||
14883|Parke Siltstone|41723|6|Mentioned|Map legend|Late Devonian||||||||
14883|Parke Siltstone|42037|5|Briefly described|Table 3 P79|||||||||
14883|Parke Siltstone|42049|5|Briefly described|p217|||||||||
14883|Parke Siltstone|42059|6|Mentioned|Fig.2 P131|||||||||
14883|Parke Siltstone|42082|6|Mentioned|Fig.3 P323|||||||||
14883|Parke Siltstone|42141|6|Mentioned|Fig.3 P570|||||||||
14883|Parke Siltstone|42351|6|Mentioned|p46|||In the Amadeus Basin.||||||22-NOV-06
14883|Parke Siltstone|42354|6|Mentioned|p7|||||||||
14883|Parke Siltstone|42504|5|Briefly described|p80|||||||||
14883|Parke Siltstone|42564|6|Mentioned|p12|||In the Amadeus Basin.||||||22-NOV-06
14883|Parke Siltstone|42940|5|Briefly described|Plate 12|||||||||
14883|Parke Siltstone|43035|6|Mentioned|p23|||Of the Pertnjara Group.||||||22-NOV-06
14883|Parke Siltstone|43225|5|Briefly described|Map Legend||Devonian|Of the Pertnjara Group.||||||22-NOV-06
14883|Parke Siltstone|43503|6|Mentioned|11-17||Emsian|younger age: Ekelian||||||
14883|Parke Siltstone|43646|6|Mentioned|Fig.3,p554|||||||||
14883|Parke Siltstone|43647|6|Mentioned|Fig.7,p538|||||||||
14883|Parke Siltstone|43648|6|Mentioned|Fig.13,p500|||||||||
14883|Parke Siltstone|43649|5|Briefly described|Fig.1,p454-55,458-9|||||||||
14883|Parke Siltstone|44133|5|Briefly described|p44|Devonian|Devonian|Of the Pertnjara Group.||||||
14883|Parke Siltstone|44342|6|Mentioned|p.7|||SG/53-5. Unit of Pertnjara Group.||||||22-NOV-06
14883|Parke Siltstone|44393|6|Mentioned|Fig.1|||||||||
14883|Parke Siltstone|44395|14|Not recorded|p.9|||Of Pertnjara Group, late Middle or early Upper Devonian.||||||
14883|Parke Siltstone|44402|5|Briefly described|map legend|Carboniferous|Devonian|Part of Pertnjara Group. Dev-Carb.||||||02-DEC-04
14883|Parke Siltstone|44433|14|Not recorded|map legend|||Devonian to Carboniferous.||||||
14883|Parke Siltstone|44484|14|Not recorded|p.11, Tb.1|Carboniferous|Devonian|Part of Pertnjara Group. Dev-Carb.||||||
14883|Parke Siltstone|44485|14|Not recorded|map legend|Carboniferous|Devonian|Part of Pertnjara Group. Dev-Carb. Defn on Tech.File F/53-13.||||||
14883|Parke Siltstone|44497|4|Described|p.12, Table 2|Carboniferous|Devonian|SF/53-13. Dev-Carb.||||||
14883|Parke Siltstone|44498|14|Not recorded|map legend|Carboniferous|Devonian|Part of Pertnjara Group. Dev-Carb.||||||
14883|Parke Siltstone|44505|14|Not recorded|p.4,8, Table 1|Carboniferous|Devonian|Of Pertnjara Group. Dev-Carb.||||||
14883|Parke Siltstone|44506|14|Not recorded|map legend|||Devonian-Carboniferous.||||||
14883|Parke Siltstone|45041|4|Described|p95|||See also p96-98. Devonian. Of the Pertnjara Group.||||||22-NOV-06
14883|Parke Siltstone|45097|6|Mentioned|p27|||See also p28 ?entirely U.Devonian.||||||22-NOV-06
14883|Parke Siltstone|45140|5|Briefly described|p64|Devonian|Devonian|Amadeus Basin. Lacustrine deposits, similar lithology to the Lucas Formation.||Basal Pertnjara Group.||||
14883|Parke Siltstone|45170|6|Mentioned|Table 3|||||||||
14883|Parke Siltstone|46864|6|Mentioned|p40|||||||||
14883|Parke Siltstone|46928|6|Mentioned|Table 1|||||||||
14883|Parke Siltstone|47050|5|Briefly described|Fig.1|||||||||
14883|Parke Siltstone|60674|5|Briefly described|Map legend|Devonian|Silurian|Of the Pertinjara Group.  Micaceous siltstone; minor limestone and fine sandstone.  Geological Province: Amadeus Basin.||||||
14883|Parke Siltstone|61309|5|Briefly described|p16 Fig. 4|||Geological Province: Amadeus Basin.||||||06-FEB-08
14883|Parke Siltstone|61385|5|Briefly described|Map legend|Devonian|Devonian|Siltstone, calcareous siltstone, fine silty sandstone interbeds.  Geological Province: Amadeus Basin.||||||20-OCT-05
14883|Parke Siltstone|61518|5|Briefly described|Map Legend|Devonian|Silurian|Micaceous siltstone; minor limestone. Geological Province: Amadeus Basin.||||||
14883|Parke Siltstone|62376|5|Briefly described|p18|Late Devonian|Late Devonian|Of the Pertnjara Group. Geological Province: Amadeus Basin.||||||09-FEB-10
14883|Parke Siltstone|62379|5|Briefly described|p7 Fig. 2|Devonian|Devonian|Of the Pertnjara Group. Geological Province: Amadeus Basin.||||||
14883|Parke Siltstone|64068|6|Mentioned|p78, 79 |||Amadeus Basin. Correlated with Dulcie Sandstone, Cravens Peak beds, Georgina Basin.||||||
14883|Parke Siltstone|64778|6|Mentioned|p13|Devonian|Devonian|Amadeus Basin.||||||
14883|Parke Siltstone|64783|6|Mentioned|p101|||Amadeus Basin.||||||15-NOV-17
14883|Parke Siltstone|64809|5|Briefly described|p3 Fig.2, p6 Fig.4, p11 Fig.10.  |Late Devonian|Late Devonian|See also p13 Fig.13. Deposited in localised lacustrine conditions.||Of the Pertnjara Group|Includes Harajica Sandstone Member.|||
14883|Parke Siltstone|65233|3|Fully described|p3 Fig. 2, p13|Late Devonian|Late Devonian|Of the Pertnjara Group. Max. thickness: 1000m. Geological province: Amadeus Basin. Comprises immature siltstone and sandstone, mainly fluvial with some lacustrine influence - coarsens upwards into litho-feldspathic quartz sandstone.||||||07-FEB-11
14883|Parke Siltstone|66127|5|Briefly described|p441.|Frasnian|Givetian|||||||
14883|Parke Siltstone|66767|5|Briefly described|p60|Devonian|Devonian|Amadeus Basin.||Pertnjara Group.||||
14883|Parke Siltstone|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 is presented, sourced from the Global Palaeomagnetic Database (GPMDB; McElhinny & Lock 1993, 1996).|375-392 Ma magnetic age range|||||10-AUG-15
14883|Parke Siltstone|67326|5|Briefly described|p2|Late Devonian|Late Devonian|Amadeus Basin.||Pertnjara Group.||Overlies Mereenie Sandstone. Is overlain by Hermannsburg Sandstone.||
14883|Parke Siltstone|67565|5|Briefly described|p42, p45.|||Thickness c.500 m.||Unit in Pertnjara Group.|Includes Deering Siltstone, Harajica Sandstone, Dare Siltstone, and Amulda, Members.|Is overlain conformably by Hermannsburg Sandstone.|Recessive brown, purple and green micaceous siltstone with local thin interbeds of micaceous sandstone and thin limestone near the base.|
14883|Parke Siltstone|67856|6|Mentioned|p338 fig 4-30|Late Devonian|Late Devonian|||Of Pertnjara Group.||||
14883|Parke Siltstone|68297|5|Briefly described|p183|Devonian|Devonian|Amadeus Basin. Includes vertebrate bone beds.||||||
14883|Parke Siltstone|68298|5|Briefly described|p226|||Amadeus Basin?||Of Pertnjara Group?|Includes Harajica Sandstone member and basal Deering Siltstone member.|||
14883|Parke Siltstone|68323|6|Mentioned|p4 Fig.2|Late Devonian|Late Devonian|Amadeus Basin.||Pertnjara Group.||||
14883|Parke Siltstone|69438|2|Defined|p23:2-3, 7-8, 37-39, 48, 56-57|Late Devonian|Late Devonian|Wells et al. (1970). Divided into four Members by Jones (1972); Young et al. (1987) added a fifth, the N'Dahla Member. Amadeus Basin. Type section is on the Dare Plain: some constituent Members have type sections elsewhere. Up to c.1000m thick. Poorly outcropping. Deposition was initiated by the Pertnjara Event.||Basal Pertnjara Group.|N'Dahla, Deering Siltstone, Harajica Sandstone, Dare Siltstone, Amulda, Members.|Conformably and gradationally overlies Mereenie Sandstone. Is overlain conformably by Hermannsburg Sandstone.|Brown, purple and green micaceous siltstone, with thin interbeds of lithofeldspathic quartz sandstone. A thin dolomitic limestone occurs locally near the base. In the western MacDonnell Ranges, sandstone dominates the lower half of the succession.|12-JUL-16
14883|Parke Siltstone|69673|4|Described|p64 fig 53|||1km thick.||Pertnjara Group|Includes Deering Siltstone Member, N'Dahla Member, Harajica Sandstone Member, Dare Siltstone Member, Amulda Member|Overlies Mereenie Sandstone, overlain by Hermannsburg Sandstone|Micaceous siltstone with thin interbeds of lithofeldspathic quartz sandstone.|
14883|Parke Siltstone|71146|5|Briefly described|p6|Frasnian|Emsian|Amadeus Basin.||||Overlain by the Hermannsburg Sandstone.|Siltstone and mudstone.|
14883|Parke Siltstone|71279|5|Briefly described|p355 Fig.2, p365|Late Devonian|Late Devonian|Amadeus Basin.||Pertnjara Group.||||
14883|Parke Siltstone|72369|5|Briefly described|p37|||Of Amadeus Basin.||Unit of Larapinta Group.||Underlain conformably by Mereenie Sandstone.||
14883|Parke Siltstone|72374|6|Mentioned|p23|||Of Amadeus Basin.||||Conformably overlain by Hermannsburg Sandstone.||11-OCT-19
14883|Parke Siltstone|73085|6|Mentioned|p1|late Devonian|late Devonian|||Pertnjara Group||Underlain by Mereenie Sandstone (Larapinta Group). Overlain by Hermannsburg Sandstone. Equivalent to Polly Conglomerate (Finke Group).||
14948|Patmungala beds|7821|5|Briefly described|p45-48, 51-54, 64-66|||Arunta Inlier. Tightly folded during (and thus predates) the Strangways Orogeny; folded by Wabudali Tectonic Phase. Estimated thickness 1,100 m. Zircon analyses tabulated. This c.1799 Ma age is discussed and ""further analytical work is needed"".|1799 +/- 10 Ma.|||Is faulted against Lander Rock beds.|Arenaceous sediments (sandstones), felsic volcanics and fine-grained volcaniclastic rocks.|
14948|Patmungala beds|23733|5|Briefly described|p34 Fig.20|||Age: 1799Ma.||||||
14948|Patmungala beds|23868|5|Briefly described|p752|Paleoproterozoic|Paleoproterozoic|Age: 1799+/-7Ma.  Geological Province: Arunta Inlier.||||||07-NOV-08
14948|Patmungala beds|37537|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Sandstone and quartzite; siltstone, chert, pebble conglomerate and recrystalised tuff. Geological Province: Arunta Block.||||||07-NOV-08
14948|Patmungala beds|39887|6|Mentioned|p452|||||||||
14948|Patmungala beds|39888|6|Mentioned|Fig.9 P468|||||||||
14948|Patmungala beds|43275|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
14948|Patmungala beds|43749|6|Mentioned|Fig.1,p6,12||Paleoproterozoic|||||||07-NOV-08
14948|Patmungala beds|44114|5|Briefly described|p323-324|||Mount Doreen-Yuendumu region, central Arunta Inlier.|||||Quartzose, platform-like rocks. Intruded by granitoids.|
14948|Patmungala beds|44158|3|Fully described|p11, Table.1|Paleoproterozoic|Paleoproterozoic|Intruded by Yarunganyi Granite. Age: 1799+/-9 Ma, U-Pb zircon date. In the Arunta Inlier.||||||05-MAY-10
14948|Patmungala beds|45155|4|Described|Table 1 P10|||||||||
14948|Patmungala beds|50369|6|Mentioned|p24.2|||Intruded by Southwark Suite.||||||
14948|Patmungala beds|61385|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Arunta Complex. Sandstone, minor siltstone, kaolinitic sandstone; rare banded ironstone: and, felsic volcaniclastic siltstone.||||||07-NOV-08
14948|Patmungala beds|65329|5|Briefly described|Map legend|Palaeoproterozoic|Paleoproterozoic|Shown as older than Nalurbindi orthogneiss, Yulyupunyu granitic gneiss, younger than Lander Rock formation, Ngadarunga Granite, same age as Reynolds Range Group. Felsic volcaniclastic siltstone, sandstone, rare banded ironstone; low to high gravity response; low magnetic response, except ironstone||||Shown as equivalent to Reynolds Range Group||19-DEC-12
14948|Patmungala beds|65330|5|Briefly described|Map legend|Palaeoproterozoic|Paleoproterozoic|Shown as older than Nalurbindi orthogneiss, Yulyupunyu granitic gneiss, younger than Lander Rock Formation, Ngadarunga Granite. Felsic volc'clastic siltst, sandst, rare banded ironstone; low to high gravity response; dominantly low magnetic response||||Shown as equivalent to Reynolds Range Group||19-DEC-12
14948|Patmungala beds|65342|5|Briefly described|p6.|||Basement to Ngalia Basin. Max. thickness at least 40 m.||||Is overlain by Rinkabeena Shale.|Quartzite, siltstone, metatuff, chert conglomerate.|10-MAR-16
14948|Patmungala beds|67565|6|Mentioned|p5 Fig.3.|||Aileron Province.||||||
14948|Patmungala beds|68270|5|Briefly described|p680|Tonian|Tonian|Ngalia Basin.||||Overlain unconformably by Naburula Formation.||
14948|Patmungala beds|69427|5|Briefly described|p12:8, 13|Statherian|Orosirian|Young et al. (1995). N margin of Ngalia Basin. SHRIMP U-Pb age from a volcaniclastic rock.|1799 +/- 9 Ma (Young et al., 1995).||||Steeply dipping and tightly folded sandstone, generally coarse-grained and thickly-bedded to massive, minor siltstone and fine-grained volcaniclastic rock. A local 200m-long lens of banded ironstone.|12-JUL-16
14948|Patmungala beds|69439|5|Briefly described|p24:7|||Aileron Province, Arunta Region. Basement to Ngalia Basin.||||Is overlain unconformably by Naburula Formation and Rinkabeena Shale.||12-JUL-16
15005|Pedlar Gabbro|41308|6|Mentioned|p12|||||||||
15005|Pedlar Gabbro|44944|4|Described|p.19||Neoproterozoic|Upper Proterozoic.||||||
15005|Pedlar Gabbro|69424|6|Mentioned|p9:55|||Hatches Creek tungsten field. This unit includes blocks of Kurinelli Sandstone with auriferous quartz veins at the Crystal Hill gold mine. Appears inexplicably as Pedlar gabbro on the same page.||||||12-JUL-16
15005|Pedlar Gabbro|72379|5|Briefly described|p7,9|Paleoproterozoic|Paleoproterozoic|Geological province: Warramunga Province. Shown in all caps p7 fig 5, but as Pedlar gabbro p7, p9. Correlable to the informally named Last Hope dolerite (of Donnellan in review, see this record).|||||Gabbro, dolerite.|03-OCT-19
15091|Pertaoorrta Group|1842|5|Briefly described|p3|Early Cambrian|Ediacaran|Of Amadeus Basin.|||Includes Maurice Formation, Sir Frederick Conglomerate, Ellis Sandstone, Mount Currie Conglomerate, Carnegie Formation, Winnall beds, Namatjira Formation, Todd River Dolostone and Arumbera Sandstone.|||
15091|Pertaoorrta Group|9199|5|Briefly described|Map legend|Cambrian|Cambrian|Including undivided rocks of sandstone, siltstone, shale, dolomite, limestone, evaporites.  Geological Province: Amadeus Basin.||||||
15091|Pertaoorrta Group|9814|5|Briefly described|Map Legend|Cambrian|Cambrian|||||||
15091|Pertaoorrta Group|22561|5|Briefly described|p9|||||||||
15091|Pertaoorrta Group|22564|6|Mentioned|p60|Cambrian|Neoproterozoic|||||||
15091|Pertaoorrta Group|22566|4|Described|p76|Late Cambrian|Neoproterozoic|||||||
15091|Pertaoorrta Group|22650|6|Mentioned|Fig 2 on p 157|Cambrian||||||||
15091|Pertaoorrta Group|22651|4|Described|p 173|Cambrian|Neoproterozoic|Five major depositional sequences are recognised in the Pertaoorrta Group and described.||||||17-JUL-13
15091|Pertaoorrta Group|22652|6|Mentioned|p 195|Late Cambrian|Neoproterozoic|||||||
15091|Pertaoorrta Group|22654|6|Mentioned|p 252|||||||||
15091|Pertaoorrta Group|22655|6|Mentioned|p 255|||Informally divided in to upper and lower Pertaoorrta Groups, p255.||||||22-NOV-06
15091|Pertaoorrta Group|22657|6|Mentioned|p 285|||||||||
15091|Pertaoorrta Group|22760|6|Mentioned|p339|||||||||
15091|Pertaoorrta Group|22804|6|Mentioned|p445|Late Cambrian|Neoproterozoic|||||||
15091|Pertaoorrta Group|22807|6|Mentioned|Fig 3 on p495|Late Cambrian|Early Cambrian|||||||
15091|Pertaoorrta Group|22824|6|Mentioned|Fig 7 on p536|||||||||
15091|Pertaoorrta Group|22826|6|Mentioned|Fig 4 on p567|||||||||
15091|Pertaoorrta Group|24063|5|Briefly described|p218 Fig.2|Proterozoic|Proterozoic|Geological Province: Amadeus Basin.||||||
15091|Pertaoorrta Group|24064|5|Briefly described|p229 Fig.7|Cambrian|Cambrian|Geological Province: Amadeus Basin.||||||
15091|Pertaoorrta Group|24111|6|Mentioned|p214 Fig. 9|||Geological Province: Amadeus Basin.||||||30-MAR-05
15091|Pertaoorrta Group|29972|6|Mentioned|Table 1|||||||||
15091|Pertaoorrta Group|30238|4|Described|p64|||Cambrian age||||||
15091|Pertaoorrta Group|30258|6|Mentioned|Fig.2|||Cambrian age||||||
15091|Pertaoorrta Group|31566|6|Mentioned|p230|||Cambrian||||||
15091|Pertaoorrta Group|31707|6|Mentioned|Table 1|||See also Fig. 2||||||
15091|Pertaoorrta Group|31973|6|Mentioned|p3|||Correlation||||||
15091|Pertaoorrta Group|33307|6|Mentioned|Fig.6|||||||||
15091|Pertaoorrta Group|33761|6|Mentioned|p146|||See also Fig.3. Adel.- Camb.||||||
15091|Pertaoorrta Group|33971|6|Mentioned|p28|||Stratigraphic section Fig.15.||||||
15091|Pertaoorrta Group|34111|5|Briefly described|Table 2|||Cambrian. See also pp6,14-19.||||||22-NOV-06
15091|Pertaoorrta Group|34442|5|Briefly described|Table 1, p8,10|||Cambrian||||||03-JUL-17
15091|Pertaoorrta Group|34488|4|Described|Table 1|||See also Table 2. Cambrian||||||
15091|Pertaoorrta Group|34579|4|Described|Table 2|||Cambrian. See also pp15,17, Fig.2.||||||22-NOV-06
15091|Pertaoorrta Group|35102|6|Mentioned|p3|||||||||
15091|Pertaoorrta Group|36473|6|Mentioned|Map legend|Ordovician|Adelaidean|Adelaidean to Ordovician||||||
15091|Pertaoorrta Group|38445|6|Mentioned|p102|||||||||
15091|Pertaoorrta Group|38606|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
15091|Pertaoorrta Group|38885|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
15091|Pertaoorrta Group|39565|6|Mentioned|Fig.14|||||||||
15091|Pertaoorrta Group|39583|6|Mentioned|Map legend|Late Cambrian|Neoproterozoic|Late Cambrian to Late Proterozoic||||||
15091|Pertaoorrta Group|39931|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
15091|Pertaoorrta Group|40740|3|Fully described|p67|||Described p13.||||||22-NOV-06
15091|Pertaoorrta Group|40810|6|Mentioned|p3|||||||||
15091|Pertaoorrta Group|40910|6|Mentioned|p13|||||||||
15091|Pertaoorrta Group|40911|6|Mentioned|Map legend|Cambrian|Cambrian|Prob. Cambrian||||||
15091|Pertaoorrta Group|40998|6|Mentioned|p431|||||||||
15091|Pertaoorrta Group|41018|6|Mentioned|p240|||||||||
15091|Pertaoorrta Group|41039|6|Mentioned|Fig.2|||||||||
15091|Pertaoorrta Group|41115|6|Mentioned|p1400|||||||||
15091|Pertaoorrta Group|41224|6|Mentioned|p430|||||||||
15091|Pertaoorrta Group|41270|6|Mentioned|Table 1|||||||||
15091|Pertaoorrta Group|41385|6|Mentioned|Fig.3|||||||||
15091|Pertaoorrta Group|41621|6|Mentioned|Map legend|Cambrian||||||||
15091|Pertaoorrta Group|41717|6|Mentioned|Fig.2|||||||||
15091|Pertaoorrta Group|41723|6|Mentioned|Map legend|Neoproterozoic|Early Cambrian|||||||
15091|Pertaoorrta Group|41801|5|Briefly described|p212|||||||||
15091|Pertaoorrta Group|41819|6|Mentioned|Map legend|Cambrian||||||||
15091|Pertaoorrta Group|41820|5|Briefly described|p7|||||||||
15091|Pertaoorrta Group|42060|6|Mentioned|Fig.5 P140|||||||||
15091|Pertaoorrta Group|42082|6|Mentioned|Fig.3 P323|||||||||
15091|Pertaoorrta Group|42354|6|Mentioned|p6|||||||||
15091|Pertaoorrta Group|42504|6|Mentioned|Plate 11 P42|||||||||
15091|Pertaoorrta Group|42940|5|Briefly described|Plate 2|Cambrian|Cambrian|Sandstone, siltstone, shale, limestone, dolostone, conglomerate; marine fossils. Age: 590-500Ma.  Geological province: Amadeus Basin.||||||23-JAN-08
15091|Pertaoorrta Group|43035|5|Briefly described|p20|||||||||
15091|Pertaoorrta Group|43225|5|Briefly described|Map Legend||Cambrian|In the Amadeus Basin.||||||22-NOV-06
15091|Pertaoorrta Group|43503|6|Mentioned|32-50|Late Cambrian|Proterozoic|||||||
15091|Pertaoorrta Group|44133|5|Briefly described|p42|||Geological Province: Amadeus Basin.||||||
15091|Pertaoorrta Group|44335|4|Described|p.11||Cambrian|Table 2. p.10.||||||
15091|Pertaoorrta Group|44336|14|Not recorded|map legend||Cambrian|SG/53-3.||||||
15091|Pertaoorrta Group|44342|4|Described|p.5, Table 2||Cambrian|SG/53-5.||||||
15091|Pertaoorrta Group|44343|14|Not recorded|map legend||Cambrian|||||||
15091|Pertaoorrta Group|44393|4|Described|p.3,7,Tb.1||Early Cambrian|L.Cambrian.||||||
15091|Pertaoorrta Group|44394|14|Not recorded|map legend||Cambrian|||||||
15091|Pertaoorrta Group|44395|14|Not recorded|p.8|||Correlates with Cleland Sandstone (Cambrian?).||||||
15091|Pertaoorrta Group|44402|5|Briefly described|map legend||Cambrian|||||||02-DEC-04
15091|Pertaoorrta Group|44433|14|Not recorded|map legend||Cambrian|||||||
15091|Pertaoorrta Group|44484|14|Not recorded|p.10,12,Tb.1,2,Fig.4|||(Cambrian).||||||
15091|Pertaoorrta Group|44485|14|Not recorded|map legend||Cambrian|Includes Quandong Conglomerate, Eninta Sandstone, Chandler Limestone, Tempe Formation, Jay Creek Limestone,  Illara Sandstone, Deception Formation, Petermann Sandstone, Goyder Formation.||||||
15091|Pertaoorrta Group|44495|4|Described|p.6, map||Cambrian|AYERS ROCK sheet (G52-8). See p.8,10, for details.||||||22-NOV-06
15091|Pertaoorrta Group|44496|5|Briefly described|map legend||Cambrian|||||||02-DEC-04
15091|Pertaoorrta Group|44497|4|Described|p.6, Table 1||Cambrian|SF/53-13.||||||
15091|Pertaoorrta Group|44498|14|Not recorded|map legend||Cambrian|||||||
15091|Pertaoorrta Group|44505|14|Not recorded|p.5,7,8, Fig. 1||Cambrian|||||||
15091|Pertaoorrta Group|44506|14|Not recorded|map legend||Cambrian|||||||
15091|Pertaoorrta Group|45036|6|Mentioned|p3|||||||||
15091|Pertaoorrta Group|45041|4|Described|p49|||See also p50-60. Camb.||||||22-NOV-06
15091|Pertaoorrta Group|45170|6|Mentioned|p23|||||||||
15091|Pertaoorrta Group|46730|5|Briefly described|p7|Cambrian|Proterozoic|Overlain by Pacoota Sandstone. Geological Province: Amadeus Basin||||||22-NOV-06
15091|Pertaoorrta Group|46829|6|Mentioned|Fig.2|||||||||
15091|Pertaoorrta Group|46928|6|Mentioned|Table 1|||||||||
15091|Pertaoorrta Group|46957|6|Mentioned|p165|||||||||
15091|Pertaoorrta Group|48639|14|Not recorded|opp.p.1,map|Ordovician|Cambrian|Ord-Cam.||||||
15091|Pertaoorrta Group|48838|1|Redefined|p.14, Tb.1|||||||||
15091|Pertaoorrta Group|48862|14|Not recorded|p.16-24,31|||Now redefined as Pertaoorrta Formation. (F52-15).||||||22-NOV-06
15091|Pertaoorrta Group|48863|2|Defined|p.15||Early Ordovician|Tb.1. opp.p.7,p.5,10,11,16,18,19,26,40-42,Pl.9,10,15,15. Lower Ordovician. (G52-4,G53-1).||||||
15091|Pertaoorrta Group|48864|14|Not recorded|p.32|||Now called Pertaoorrta Formation.||||||
15091|Pertaoorrta Group|48865|2|Defined|p.10,Fig.20||Cambrian|Many figures. Fig.4,11,12,23,42,45,47,49,Fig.14,Pl.7,8. (G53-5,G52-8).||||||
15091|Pertaoorrta Group|48880|14|Not recorded|p.20,33,Pl.10,12,13||Cambrian|(F53-13,15,G53-3).||||||
15091|Pertaoorrta Group|48890|14|Not recorded|p.31,43|||Includes, Todd River Dolomite, Shannon Fm, Jay Ck Lm, Hugh River Shale, Giles Ck - Dolomite, Goyder Fm-, Chandler Ls, Arumbera Sandstone.||||||
15091|Pertaoorrta Group|48963|6|Mentioned|p22|||||||||
15091|Pertaoorrta Group|60547|5|Briefly described|Map Legend|Cambrian|Cambrian|Sandstone, siltstone, shale, dolomite, limestone, evaporites. Geological Province: Amadeus Basin.||||||03-JUN-05
15091|Pertaoorrta Group|60674|5|Briefly described|Map legend|Cambrian|Cambrian|Includes: Cleland Sandstone, Tempe, Illara, Deception and Petermann Formations, Hugh River Shale and the Goyder Formation.  Geological Province: Amadeus Basin.||||||12-JAN-05
15091|Pertaoorrta Group|62376|5|Briefly described|p18|Late Cambrian|Late Proterozoic|Geological Province: Amadeus Basin.||||||09-FEB-10
15091|Pertaoorrta Group|62379|5|Briefly described|p7 Fig. 2|Late Cambrian|Late Proterozoic|Geological Province: Amadeus Basin.||||||
15091|Pertaoorrta Group|62609|5|Briefly described|Map Legend|Cambrian|Cambrian|Sandstone, siltstone, shale, limestone, dolomite, some conglomerate. Marine fossils. Underlies Larapinta Group.||||||14-AUG-06
15091|Pertaoorrta Group|62620|5|Briefly described|Map Legend|Cambrian|Cambrian|Sandstone, siltstone, shale, limestone, dolomite, some conglomerate.||||||
15091|Pertaoorrta Group|62794|5|Briefly described|p289 Fig.2, p290|Late Cambrian|Late Cambrian|Amadeus Basin. Underlies Late Cambrian-Early Ordovician Larapinta Group. Includes Goyder Formation.||||||
15091|Pertaoorrta Group|64334|5|Briefly described|p39-40|Cambrian|Cambrian|Amadeus Basin.||||Is overlain unconformably by Larapinta Group.|Sandstone, limestone, dolostone.|
15091|Pertaoorrta Group|64443|6|Mentioned|p40.|||Of Amadeus Basin. Correlative of Barkly Group, Georgina Basin in part.||||||
15091|Pertaoorrta Group|64778|6|Mentioned|p11, 13|Cambrian|Cambrian|Amadeus Basin. Several thousand meters thick. Appears as Pertaoorta Group on p11.||||||
15091|Pertaoorrta Group|64809|5|Briefly described|p3 Fig.2 |Late Cambrian|Late Proterozoic|Mis-spelt as Pertaoort in Fig.4.|||Includes Mount Currie Cong.; Eninta, Chandler, Tempe, Shannon, Petermann, Goyder Formations; Arumbera, Illara, Cleland Sandstones; Todd River, Giles Creek Dolostones; Hugh River Shale; Jay Creek Lst.|||
15091|Pertaoorrta Group|64970|6|Mentioned|p719 Fig. 2|Cambrian|Neoproterozoic|Geological Province: Amadeus Basin.||||||27-MAY-09
15091|Pertaoorrta Group|65102|6|Mentioned|p363, Figure 4-38|Paleozoic|Neoproterozoic|Amadeus Basin.||||||
15091|Pertaoorrta Group|65233|4|Described|p3 Fig. 2, p7|Early Cambrian|Neoproterozoic|Geological province: Amadeus Basin.||||||07-FEB-11
15091|Pertaoorrta Group|65489|5|Briefly described|p125|Cambrian|Cambrian|Amadeus Basin.|||Includes Todd River Dolomite; Chandler, Giles Creek, Tempe, Shannon and Goyder Formations.|Overlies Arumbera Formation. Is overlain by Larapinta Group.||
15091|Pertaoorrta Group|67326|5|Briefly described|p2|Late Cambrian|Neoproterozoic|Amadeus Basin. Also includes Mount Currie Conglomerate; Todd River, Giles Creek Dolostones. The stratigraphic diagram is not clear: the Group may also include Sir Frederick Conglomerate, Ellis Sandstone, Winnall beds, and Pertatataka and Julie Formations.|||Arumbera, Cleland, Illara, Deception, Petermann Sandstones; Maurice, Eninta, Chandler, Tempe, Shannon, Goyder Formations; Jay Creek Limestone; Hugh River Shale. See Comments for more.|Is overlain by Larapinta Group.||
15091|Pertaoorrta Group|67565|5|Briefly described|p5 Fig.3, p39-41|||Amadeus Basin.|||Includes Arumbera Sandstone, Tempe Formation, Hugh River Shale, Illara Formation, Deception Formation, Petermann sandstone, Cleland Sandstone, Goyder Formation.|||03-DEC-15
15091|Pertaoorrta Group|68323|6|Mentioned|p4 Fig.2|Late Cambrian|Neoproterozoic|Amadeus Basin. Other constituents include Todd River, Giles Creek Dolostones; Hugh River Shale; Jay Creek Limestone.|||Maurice, Eninta, Chandler, Tempe, Shannon, Goyder FZs; Sir Frederick, Mount Currie Conglomerates; Arumbera, Cleland, Illara, Deception, Petermann Sandstones. See Comments for more.|||
15091|Pertaoorrta Group|69438|4|Described|p23:2-4, 23-32, 34, 37, 53|Late Cambrian|Ediacaran|?Ranford et al. (1965). Previously Pertaaoorrta Formation of Wells et al. (1965). Amadeus Basin. Other constituents are Hugh River Shale; Mutitjulu Arkose; Todd River, Giles Creek Dolostones; Jay Creek Limestone; Winnall beds. See also references to mis-spelt Pertaoorta Group (23:4-5, 7-8, 47, 50). Hosts malachite pellets at the Alalgara Cu occurrence.|||Arumbera, Ellis, Eninta, Cleland, Illara, Petermann Sandstones; Namatjira, Chandler, Maurice, Tempe, Deception, Goyder, Shannon Formations; Quandong, Mount Currie Conglomerates; see Comments for more|Is overlain unconformably by Stairway Sandstone (Larapinta Group) and Mereenie Sandstone.||12-JUL-16
15091|Pertaoorrta Group|69443|6|Mentioned|p28:21|||Amadeus Basin.||||Correlated with Barkly Group.||12-JUL-16
15091|Pertaoorrta Group|69449|6|Mentioned|p34:4|Cambrian|Cambrian|Amadeus Basin. Has equivalent rocks in western Warburton Basin in SA, but not yet described from any NT drillholes.||||||12-JUL-16
15091|Pertaoorrta Group|69673|5|Briefly described|p65, p66, p79|Cambrian|Ediacaran||||Includes Arumbera Sandstone,|Unconformably overlain by Stairway Sandstone|Carbonates and siliciclastic rocks.|
15091|Pertaoorrta Group|70749|6|Mentioned|p54|||Amadeus Basin.|||Goyder Formation.|||
15091|Pertaoorrta Group|70752|5|Briefly described|p125|Cambrian|Proterozoic|Amadeus Basin.|||Todd River, Giles Creek Dolostones; Arumbera Sandstone; Shannon, Goyder Formations.|||
15091|Pertaoorrta Group|70839|5|Briefly described|p329|Cambrian|Ediacaran|Of Amadeus Basin. Part of Supersequence 4.|||Includes Arumbera Sandstone.|Underlain by Julie Formation or Arumbera Sandstone.||
15091|Pertaoorrta Group|71088|6|Mentioned|p8, p33|Cambrian|Cambrian|Amadeus Basin.||||Equivalent to the Mu Formation.||
15091|Pertaoorrta Group|71146|5|Briefly described|p6|Cambrian|Cambrian|Amadeus Basin.||||Unconformably overlain by the Pacoota Sandstone (Larapinta Group).|Sandstone, carbonate, mudstone and evaporite.|
15091|Pertaoorrta Group|71268|5|Briefly described|1m_geologyp12_lut.csv||||||Includes Cleland Sandstone.|||
15091|Pertaoorrta Group|71279|5|Briefly described|p355 Fig.2, p382 Tb.1|Late Cambrian|Ediacaran|Amadeus Basin. Other constituents include: Winnall Beds; Todd River, Giles Creek Dolostones; Hugh River Shale; Jay Creek Limestone. Modelled magnetic properties.|||Carnegie, Maurice, Namatjira, Chandler, Deception, Shannon, Goyder Formations; Ellis, Arumbera, Cleland, Illara, Petermann Sandstones; Sir Frederick, Mount Currie Conglomerates. See Comments for more.|||
15091|Pertaoorrta Group|71841|5|Briefly described|p1|Early Cambrian|Ediacaran|Of Amadeus Basin.|||Includes Maurice Formation, Winnall Beds, Sir Frederick Conglomerate, Ellis Sandstone, Mount Currie Conglomerate, Carnegie Formation, Namatjira Formation, Todd Rover Dolostone and Arumbera Sandstone.|Underlain by Boord Formation or Inindia beds or Julie Formation.||
15091|Pertaoorrta Group|71842|5|Briefly described|p3|Early Cambrian|Ediacaran|Of Amadeus Basin.|||Includes Maurice Formation, Sir Frederick Conglomerate, Ellis Sandstone, Mount Currie Conglomerate, Carnegie Formation, Winnall beds, Namatjira Formation, Todd River Dolostone and Arumbera Sandstone.|||
15091|Pertaoorrta Group|71898|4|Described|iii, p1, p6, p8-p9, p11, p14, p17-p18|Late Cambrian|Early Cambrian|Amadeus Basin. Previously the Pertaoorrta Formation of Wells et al, 1965. Outcrops in the AREYONGA (5439) map sheet of HENBURY. Hosts a significant amount of detrital zircons ranging from ca 650-490 Ma.|||Includes the Tempe Formation, Deception Formation, Petermann Sandstone and the Goyder Formation.|Overlain by the Pacoota Sandstone (Larapinta Group).||19-NOV-18
15091|Pertaoorrta Group|72360|5|Briefly described|Solid Geology map|||Of Amadeus Basin.||||||
15091|Pertaoorrta Group|72369|5|Briefly described|p15,20,23,37|Cambrian|Cambrian|Of Amadeus Basin.|||Includes Arumbera and Eninta sandstones.|Underlain by Winnall Group.||
15091|Pertaoorrta Group|72374|5|Briefly described|iii,p3,12,15|Cambrian|Ediacaran|Of Amadeus Basin.|||Includes Eninta Sandstone, Illara Sandstone.|||
15091|Pertaoorrta Group|73085|6|Mentioned|p1|late Cambrian|Ediacaran||||[Unclear]|||
15091|Pertaoorrta Group|73119|6|Mentioned|piii, p14, p16|||Amadeus Basin, western. Dominant detrital zircon age components are Mesoproterozoic, with a major peak between ca 1170 - 1150 Ma and other minor peaks. [See article for provenance discussion].|||Cleland Sandstone, Tempe Formation|||
15094|Pertatataka Formation|9199|5|Briefly described|Map legend|Proterozoic|Proterozoic|Siltstone and shale with lenses of sandstone, limestone, dolomite, conglomerate.  Geological Province: Amadeus Basin.||||||
15094|Pertatataka Formation|9814|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Siltstone, shale.||||||
15094|Pertatataka Formation|22506|6|Mentioned|p130 Fig.4|Neoproterozoic III|Neoproterozoic III|||||||
15094|Pertatataka Formation|22560|5|Briefly described|p2|||||||||
15094|Pertatataka Formation|22561|4|Described|p24|Neoproterozoic|Neoproterozoic|||||||
15094|Pertatataka Formation|22562|6|Mentioned|p39|||||||||
15094|Pertatataka Formation|22564|5|Briefly described|p59||Neoproterozoic|||||||
15094|Pertatataka Formation|22566|5|Briefly described|p73|Neoproterozoic|Neoproterozoic|In the north of the Ooraminna depocentre, the Pertatataka Fromation overlies the lower subunits of the Olympic Formation at this Type Section - p81.||||||
15094|Pertatataka Formation|22567|5|Briefly described|p91|||Age: 730+/-45 Ma Rb-Sr data (Compston and Taylor, 1969).||||||04-SEP-14
15094|Pertatataka Formation|22646|4|Described|p 99|Neoproterozoic|Neoproterozoic|informal name - lower Pertatataka Formation is mentioned on p 101||||||
15094|Pertatataka Formation|22649|5|Briefly described|p 152|Neoproterozoic|Neoproterozoic|Underlain by Gaylad Sandstone.||||||22-NOV-06
15094|Pertatataka Formation|22651|6|Mentioned|Fig 10 btw p182-183|Proterozoic|Proterozoic|||||||
15094|Pertatataka Formation|22652|6|Mentioned|p 222|||||||||
15094|Pertatataka Formation|22653|6|Mentioned|Fig 14 on p 236|||||||||
15094|Pertatataka Formation|22746|5|Briefly described|p513, p529|||||||||
15094|Pertatataka Formation|22761|6|Mentioned|p358|||||||||
15094|Pertatataka Formation|22762|5|Briefly described|p378|Neoproterozoic|Neoproterozoic|||||||
15094|Pertatataka Formation|22763|5|Briefly described|p398|Neoproterozoic|Neoproterozoic|||||||
15094|Pertatataka Formation|22804|6|Mentioned|p440|Neoproterozoic|Neoproterozoic|||||||
15094|Pertatataka Formation|22805|5|Briefly described|p464|Neoproterozoic|Neoproterozoic|||||||
15094|Pertatataka Formation|22816|5|Briefly described|p10 Fig. 4|Neoproterozoic|Neoproterozoic|In the Amadeus Basin.||||||22-NOV-06
15094|Pertatataka Formation|22823|4|Described|p517-518|Proterozoic|Proterozoic|||||||
15094|Pertatataka Formation|22826|4|Described|p570|Neoproterozoic|Neoproterozoic|||||||
15094|Pertatataka Formation|22901|6|Mentioned|78|||Geological  province: Amadeus Basin.||||||22-NOV-06
15094|Pertatataka Formation|22921|6|Mentioned|39|||Geological province: Amadeus Basin.||||||17-APR-13
15094|Pertatataka Formation|23250|5|Briefly described|p1124  Fig.2||Neoproterozoic III|Correlate of Tent Hill Formation and Yarloo Shale, and Bunyeroo Formation, ABC Range Quartzite and Brachina Formation.||||||
15094|Pertatataka Formation|23282|6|Mentioned|p89|||In the Amadeus Basin.||||||22-NOV-06
15094|Pertatataka Formation|23287|6|Mentioned|p104 Fig.4|||Age: Ediacarian. In the Amadeus Basin.||||||22-NOV-06
15094|Pertatataka Formation|23314|5|Briefly described|333 Fig.4|Neoproterozoic III|Neoproterozoic III|||||||
15094|Pertatataka Formation|23356|5|Briefly described|26 Tab.2|Neoproterozoic|Neoproterozoic|Age: ~600Ma.||||||22-NOV-06
15094|Pertatataka Formation|23806|5|Briefly described|p1122 Fig. 1|Neoproterozoic|Neoproterozoic|||||||
15094|Pertatataka Formation|24064|5|Briefly described|p229 Fig.7|Adelaidean|Adelaidean|Geological Province: Amadeus Basin.||||||
15094|Pertatataka Formation|24111|5|Briefly described|p216|Neoproterozoic|Neoproterozoic|Geological Province: Amadeus Basin. See also p215 Fig. 11.||||||
15094|Pertatataka Formation|24301|5|Briefly described|p17|Neoproterozoic|Neoproterozoic|Geological Province: Amadeus Basin||||||
15094|Pertatataka Formation|24442|6|Mentioned|p38|||Geological Province: Centralian Superbasin.||||||
15094|Pertatataka Formation|29721|6|Mentioned|Table 44|||||||||
15094|Pertatataka Formation|29972|6|Mentioned|Table 1|||Proterozoic||||||
15094|Pertatataka Formation|30220|6|Mentioned|p244|||||||||
15094|Pertatataka Formation|30258|6|Mentioned|Fig.2|||About 730m.y.||||||
15094|Pertatataka Formation|30544|6|Mentioned|p48|||On map legend||||||
15094|Pertatataka Formation|31026|6|Mentioned|p61|||||||||
15094|Pertatataka Formation|31566|6|Mentioned|p230|||Proterozoic||||||
15094|Pertatataka Formation|31645|6|Mentioned|Table 2|||Correlation||||||
15094|Pertatataka Formation|32144|6|Mentioned|p81|||Organic matter||||||
15094|Pertatataka Formation|32376|6|Mentioned|p1541|||||||||
15094|Pertatataka Formation|32442|6|Mentioned|p9|||||||||
15094|Pertatataka Formation|32469|6|Mentioned|p531|||||||||
15094|Pertatataka Formation|32720|6|Mentioned|Table 1|||||||||
15094|Pertatataka Formation|32722|6|Mentioned|Fig.3|||Adelaidean. Stromatolite||||||
15094|Pertatataka Formation|33025|6|Mentioned|p928|||Minimum age 800 m.y.||||||
15094|Pertatataka Formation|33102|6|Mentioned|Fig.2|||||||||
15094|Pertatataka Formation|33103|6|Mentioned|p23|||||||||
15094|Pertatataka Formation|33630|6|Mentioned|p906|||||||||
15094|Pertatataka Formation|33655|6|Mentioned|p101|||||||||
15094|Pertatataka Formation|33761|6|Mentioned|p146|||Adelaidean. Contains Olympic Member||||||
15094|Pertatataka Formation|34111|4|Described|Table 1|||Precambrian. See also Table 4, pp11,14,17,19.||||||22-NOV-06
15094|Pertatataka Formation|34186|6|Mentioned|Fig.3|||Late Precambrian. See also Fig.4.||||||
15094|Pertatataka Formation|34202|6|Mentioned|p1058|||||||||
15094|Pertatataka Formation|34287|6|Mentioned|p41|||See also p42.||||||22-NOV-06
15094|Pertatataka Formation|34442|5|Briefly described|Table 1|||Proterozoic||||||
15094|Pertatataka Formation|34488|4|Described|Table 1|||Proterozoic. See also pp10,14,16.||||||22-NOV-06
15094|Pertatataka Formation|34579|5|Briefly described|Table 1|||See also pp15,17, Fig.2.||||||22-NOV-06
15094|Pertatataka Formation|34580|4|Described|Table 1|||||||||
15094|Pertatataka Formation|35064|6|Mentioned|p208|||||||||
15094|Pertatataka Formation|35088|6|Mentioned|p92|||||||||
15094|Pertatataka Formation|35102|6|Mentioned|Fig.2|||||||||
15094|Pertatataka Formation|35136|6|Mentioned|p140|||||||||
15094|Pertatataka Formation|35798|6|Mentioned|p307|||||||||
15094|Pertatataka Formation|35805|5|Briefly described|p36|||See also Fig.3.||||||
15094|Pertatataka Formation|35863|6|Mentioned|Table 1|||||||||
15094|Pertatataka Formation|36198|6|Mentioned|Fig.III.2|||||||||
15094|Pertatataka Formation|36473|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
15094|Pertatataka Formation|36898|6|Mentioned|p198|||||||||
15094|Pertatataka Formation|37371|6|Mentioned|p382|||||||||
15094|Pertatataka Formation|37462|4|Described|Table 4.IX|||||||||
15094|Pertatataka Formation|37572|6|Mentioned|p153|||||||||
15094|Pertatataka Formation|37928|6|Mentioned|p517|||||||||
15094|Pertatataka Formation|37929|6|Mentioned|Fig.2|||||||||
15094|Pertatataka Formation|38157|6|Mentioned|Table VI|||||||||
15094|Pertatataka Formation|38606|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
15094|Pertatataka Formation|38885|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
15094|Pertatataka Formation|38945|6|Mentioned|p134|||||||||
15094|Pertatataka Formation|39210|4|Described|p37|||||||||
15094|Pertatataka Formation|39213|6|Mentioned|Fig.6|||Amadeus Basin Succession||||||
15094|Pertatataka Formation|39558|6|Mentioned|Table 2|||||||||
15094|Pertatataka Formation|39565|6|Mentioned|p32|||||||||
15094|Pertatataka Formation|39583|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
15094|Pertatataka Formation|39898|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Laminated siltstone and shale, sandstone. Geological Province: Amadeus Basin.||||||14-FEB-06
15094|Pertatataka Formation|39931|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
15094|Pertatataka Formation|40105|6|Mentioned|p311|||||||||
15094|Pertatataka Formation|40201|5|Briefly described|Table 1|||||||||
15094|Pertatataka Formation|40740|3|Fully described|p12|||||||||
15094|Pertatataka Formation|40810|6|Mentioned|p3|||||||||
15094|Pertatataka Formation|40852|6|Mentioned|p29|||||||||
15094|Pertatataka Formation|40856|5|Briefly described|p316|||||||||
15094|Pertatataka Formation|41005|6|Mentioned|Fig.2|||||||||
15094|Pertatataka Formation|41039|6|Mentioned|Fig.2|||||||||
15094|Pertatataka Formation|41115|6|Mentioned|p1389|||||||||
15094|Pertatataka Formation|41190|6|Mentioned|Fig.4|||||||||
15094|Pertatataka Formation|41203|6|Mentioned|p5|||||||||
15094|Pertatataka Formation|41224|6|Mentioned|Fig.2|||||||||
15094|Pertatataka Formation|41270|6|Mentioned|Table 1|||||||||
15094|Pertatataka Formation|41429|5|Briefly described|p246|||||||||
15094|Pertatataka Formation|41618|6|Mentioned|Fig.2|||||||||
15094|Pertatataka Formation|41717|5|Briefly described|p355|||||||||
15094|Pertatataka Formation|41801|6|Mentioned|p218|||||||||
15094|Pertatataka Formation|41852|6|Mentioned|p209|||||||||
15094|Pertatataka Formation|42059|6|Mentioned|Fig.2 P131|||||||||
15094|Pertatataka Formation|42060|6|Mentioned|Fig.5 P140|||||||||
15094|Pertatataka Formation|42082|6|Mentioned|Fig.3 P323|||||||||
15094|Pertatataka Formation|42504|5|Briefly described|p72|||||||||
15094|Pertatataka Formation|42643|6|Mentioned|Fig.4 P19|||||||||
15094|Pertatataka Formation|42845|6|Mentioned|Fig.3 P498|||||||||
15094|Pertatataka Formation|42886|4|Described|p223|||see also Fig.2 p219.||||||22-NOV-06
15094|Pertatataka Formation|42940|5|Briefly described|Plate 2|Neoproterozoic|Neoproterozoic|Shale, siltstone.  Geological province: Amadeus Basin.||||||04-SEP-14
15094|Pertatataka Formation|43011|6|Mentioned|Table 2,p12|||||||||
15094|Pertatataka Formation|43057|5|Briefly described|p68|||||||||
15094|Pertatataka Formation|43105|5|Briefly described|Fig.3,p8|||||||||
15094|Pertatataka Formation|43225|5|Briefly described|Map Legend||Neoproterozoic|||||||
15094|Pertatataka Formation|43503|6|Mentioned|11-50|||from Ediacaran to||||||
15094|Pertatataka Formation|43595|5|Briefly described|p548,Fig.5-33,549||Adelaidean|||||||
15094|Pertatataka Formation|43622|6|Mentioned|p39|||||||||
15094|Pertatataka Formation|43647|6|Mentioned|Fig.4,533|||||||||
15094|Pertatataka Formation|43648|6|Mentioned|p491|||||||||
15094|Pertatataka Formation|43649|5|Briefly described|p457|||||||||
15094|Pertatataka Formation|43756|6|Mentioned|p542|||||||||
15094|Pertatataka Formation|43817|6|Mentioned|Fig.1,p42|||||||||
15094|Pertatataka Formation|44261|14|Not recorded|p7-19|||Not recorded on white card.||||||
15094|Pertatataka Formation|44262|14|Not recorded|p3-21|||Not listed on white card.||||||
15094|Pertatataka Formation|44335|4|Described|p.7||Proterozoic|Tb.1. p.8.||||||
15094|Pertatataka Formation|44342|14|Not recorded|p.5|||SG/53-5, correlated with Winnall Beds.||||||
15094|Pertatataka Formation|44395|14|Not recorded|p.6|||Correlates with Ellis Sandstone and Maurice Formation.||||||22-NOV-06
15094|Pertatataka Formation|44402|5|Briefly described|map legend||Proterozoic|||||||02-DEC-04
15094|Pertatataka Formation|44433|14|Not recorded|map legend||Proterozoic|||||||
15094|Pertatataka Formation|44484|14|Not recorded|p.10, Fig.4, Tb.1||Proterozoic|||||||
15094|Pertatataka Formation|44485|14|Not recorded|map legend||Proterozoic|||||||
15094|Pertatataka Formation|44497|4|Described|p.6, Table 1||Proterozoic|SF/53-13.||||||
15094|Pertatataka Formation|44498|14|Not recorded|map legend||Proterozoic|||||||
15094|Pertatataka Formation|44505|14|Not recorded|p.7, Fig.1, Table 1||Proterozoic|||||||
15094|Pertatataka Formation|44506|14|Not recorded|map legend||Proterozoic|||||||
15094|Pertatataka Formation|45041|4|Described|p32|||Proterozoic||||||
15094|Pertatataka Formation|45052|6|Mentioned|p67|||||||||
15094|Pertatataka Formation|45079|6|Mentioned|p16|||||||||
15094|Pertatataka Formation|46730|5|Briefly described|p7|||Underlain by Pioneer Sandstone. Geological Province: Amadeus Basin||||||22-NOV-06
15094|Pertatataka Formation|46829|6|Mentioned|Fig.2|||||||||
15094|Pertatataka Formation|46865|4|Described|p51|||||||||
15094|Pertatataka Formation|46903|6|Mentioned|Fig.3|||Magnetic polarity sequences||||||
15094|Pertatataka Formation|46928|6|Mentioned|Table 1|||||||||
15094|Pertatataka Formation|47035|6|Mentioned|Fig.1|||||||||
15094|Pertatataka Formation|48639|14|Not recorded|p.13,opp.p.1||Neoproterozoic|See also page, 11. Pl.2,Sh.2. U.Prot. (G55-2,15,G53-3).||||||
15094|Pertatataka Formation|48838|2|Defined|p.13, Tb.1|||||||||
15094|Pertatataka Formation|48844|14|Not recorded|p.8|||||||||
15094|Pertatataka Formation|48862|14|Not recorded|p.8|||On many pages. p.1,8,13,16,18,21,34,38,41,43; opp.8,9; Pl.2,7,10. (F52-15).||||||
15094|Pertatataka Formation|48863|2|Defined|p.12|||Tb.1. opp.p.7,9,11,17,38-40, Pl.15,16. ?Upper Proterozoic, or Lower Cambrian. (G52-4,G53-1).||||||
15094|Pertatataka Formation|48864|14|Not recorded|Tb.1,p.1,26,31|||||||||
15094|Pertatataka Formation|48865|14|Not recorded|Fig.4,p.20,45|||(F53-13).||||||
15094|Pertatataka Formation|48880|14|Not recorded|p.20,20,33,Pl.10-13||Neoproterozoic|U.Prot. 750 m.y. (F53-13,14).||||||
15094|Pertatataka Formation|48890|4|Described|p.22-31|||See also Tables, Figs and Plates. Includes: Ringwood Member, Olympic Member, Limbla Member, Julie Member, Cyclops Member. Defn on Tech.File F/53-13.||||||22-NOV-06
15094|Pertatataka Formation|48963|6|Mentioned|p5|||||||||
15094|Pertatataka Formation|48990|6|Mentioned|p11|||||||||
15094|Pertatataka Formation|49796|5|Briefly described|Sect C BDF 28|||||||||
15094|Pertatataka Formation|50246|5|Briefly described|p20 Fig. 2|Proterozoic|Proterozoic|Includes the Cyclops Member.||||||07-FEB-11
15094|Pertatataka Formation|60547|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Siltstone and shale with lenses of sandstone, limestone, dolomite, conglomerate. Geological Province: Amadeus Basin.||||||07-JUN-05
15094|Pertatataka Formation|60549|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Contains the Waldo Pedlar Member.  Laminated siltstone and shale, some sandstone.||||||02-FEB-05
15094|Pertatataka Formation|60674|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|White to yellow-brown, laminated and thinly-bedded fine kaolinitic sandstone with interbeds of laminated micaceous siltstone.  Geological Province: Amadeus Basin.||||||
15094|Pertatataka Formation|61385|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Siltstone, shale, sandstone; limestone with stromatolites. Geological Province: Amadeus Basin.||||||
15094|Pertatataka Formation|61387|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Laminated and thin-bedded, fine kaolinitic sandstone, with interbeds of micaceous siltstone. Geological Province: Amadeus Basin.||||||04-OCT-05
15094|Pertatataka Formation|61518|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Laminated and thin bedded fine grained kaolinitic sandstone with interbeds of micaceous siltstone. Geological Province: Amadeus Basin.||||||
15094|Pertatataka Formation|61519|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Laminated and thin bedded, fine kaolinitic sandstone with interbeds of micaceous siltstone. Geological Province: Amadeus Basin.||||||
15094|Pertatataka Formation|61732|3|Fully described|p4 Fig. 3, p94-95|Marinoan|Marinoan|Formerly incl. six members: Limbla and Ringwood Members and Olympic and Julie "Members" all now redefined; but retains Cyclops and Waldo Pedlar Members. Max. thickness: 570m. Geol.Prov: Amadeus Basin. See also p5 Tb. 1.||||||10-SEP-14
15094|Pertatataka Formation|62085|6|Mentioned|p15 Fig.1, p20  |||Amadeus Basin. Contains distinctive acritarch assembly: Appendisphaera barbata.|||||Marine siltstone.|
15094|Pertatataka Formation|62376|5|Briefly described|p18|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin.||||||09-FEB-10
15094|Pertatataka Formation|62379|5|Briefly described|p7 Fig. 2, p26|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin. Thickness: 600m. Black shale. Lateral equivalent of Winnall beds.||||||
15094|Pertatataka Formation|62428|5|Briefly described|p351 Tb. 6|Early Cambrian|Neoproterozoic III|Palaeomagnetic data.||||||10-FEB-09
15094|Pertatataka Formation|62453|5|Briefly described|p12 Fig. 8|Ediacaran|Ediacaran|Geological Province: Amadeus Basin.||||||
15094|Pertatataka Formation|62595|5|Briefly described|p29 Fig.6.|Proterozoic|Proterozoic|Ross River area.|||Includes Cyclops Member.||Sandstone, fine-grained, undulose to flat and laminated and fissile.|
15094|Pertatataka Formation|62620|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Siltstone, shale, limestone, calcarenite, dolomite, some sandstone and tillitic conglomerate.||||||
15094|Pertatataka Formation|62903|6|Mentioned|p730 Fig.1|||Amadeus Basin. Presented in figure as Pertatataka, and Pertatataka Fm.||||overlies Cap Dolomite; is overlain by Julie Formation.||
15094|Pertatataka Formation|63458|6|Mentioned|p897 Fig.19. |Ediacaran|Ediacaran|Amadeus Basin.||||Is overlain by Julie Formation.||
15094|Pertatataka Formation|63562|5|Briefly described|p338 fig 3, p343, 344, p352 fig 10|Ediacaran|Ediacaran|Of Amadeus Basin. Coarsens to the S, implying source in Musgrave Inlier.||||Overlies Pioneer Sandstone.|Deep-water turbidites and pelagic sediments.|
15094|Pertatataka Formation|63811|6|Mentioned|p503,505, p519-527 App A|Ediacaran|Ediacaran|Of Amadeus Basin. Has acritarch fossils in common with Ungoolya Group, Officer Basin, and Doushantuo Formation, South China. Also correlated with Khamaka and Kursov Formations, Siberia.||||||28-MAR-12
15094|Pertatataka Formation|64068|6|Mentioned|p49, 51, 224|||Amadeus Basin. Lower part correlated with Gnallan-a-Gea Arkose, Elyuah Formation, medial to upper part with Grant Bluff Formation, southern Georgina Basin.||||||
15094|Pertatataka Formation|64625|5|Briefly described|p243-257|Neoproterozoic|Neoproterozoic|Amadeus Basin. Has a basal "cap carbonate".|||Includes Cyclops Member|Overlies Gaylad Sandstone, Pioneer Sandstone. Is overlain gradationally by Julie Formation.|Siltstone and shale, sandstone.|
15094|Pertatataka Formation|64724|5|Briefly described|p49 Fig. 7|Ediacaran|Ediacaran|Deposited in the Amadeus Basin during the Centralian 3 event (~600-544 Ma)||||||
15094|Pertatataka Formation|64778|6|Mentioned|p13, 18|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
15094|Pertatataka Formation|64794|6|Mentioned|p238 fig 2|Ediacaran|Ediacaran|||||||
15094|Pertatataka Formation|64797|5|Briefly described|p152, p153 Fig.2, p157-159 |||See also p164 Fig.11, p167 Tb.10, p168 Tb.11, p176-177. Of Amadeus Basin. S-isotope data.||||Correlated with Brachina Formation (Adelaide Rift Complex).||
15094|Pertatataka Formation|64809|5|Briefly described|p2, p3 Fig.2, p6 Fig.4, p11 Fig.10.|Proterozoic|Proterozoic|See also p13 Fig.13, p15 Fig.15. Widespread transgressive deposits.|||Includes Cyclops Member.||Fine marine siliciclastics (siltstone, shale).|
15094|Pertatataka Formation|64970|6|Mentioned|p719 Fig. 2|Neproterozoic|Neoproterozoic|Geological Province: Amadeus Basin.||||||27-MAY-09
15094|Pertatataka Formation|65233|3|Fully described|p3 Fig. 2, p6|Neoproterozoic|Neoproterozoic|Formerly Winnall beds. Disconformable on Bitter Springs Fm; disconform.or conform.on Olympic Fm; below Julie Fm. Max.thick: 500m. Amadeus Basin.Thick extensive marine shales in succession of mainly fine-gr.clastics, predom'l red/green shale+ fine-gr. sst||||||07-FEB-11
15094|Pertatataka Formation|65256|6|Mentioned|p19|||Stratigraphic correlative of the Winnall beds.||||||
15094|Pertatataka Formation|65272|6|Mentioned|p320 Fig.3||Ediacaran|||||||
15094|Pertatataka Formation|65338|5|Briefly described|p64.|||Amadeus Basin. Correlative with Elyuah Formation.|||||Predominantly micaceous siltstone and shale with thinly interbedded sandstone; rare limestone.|
15094|Pertatataka Formation|65342|5|Briefly described|p4.|||Amadeus Basin. Max. thickness at least 19 m.||||Is overlain by Julie Formation.|Fine kaolinitic sandstone.|
15094|Pertatataka Formation|65365|5|Briefly described|p10 Fig. 4|Ediacaran|Ediacaran|Amadeus Basin. Includes Acanthomorph acritarchs.||||||
15094|Pertatataka Formation|65366|5|Briefly described|p23 Fig. 3|Ediacaran|Ediacaran|Amadeus Basin||||||
15094|Pertatataka Formation|65410|6|Mentioned|p74.|Neoproterozoic|Neoproterozoic|Amadeus Basin. Part of Supersequence 3. Contains distinctive, well-documented and well-constrained palynomorph assemblages of biostratigraphic significance, including acritarchs.||||||
15094|Pertatataka Formation|65416|6|Mentioned|p141, p146.|||Amadeus Basin. Tentatively correlated with Boondawari Formation (Officer Basin). Suggested by Perincek (1996) to pre-date the Petermann Ranges Orogeny.||||||
15094|Pertatataka Formation|65489|5|Briefly described|p125|Proterozoic|Proterozoic|Amadeus Basin.||||Overlies Aralka Formation. Is overlain by Arumbera Formation.||
15094|Pertatataka Formation|65892|6|Mentioned|p35.|Late Neoproterozoic|Late Neoproterozoic|Amadeus Basin. Contains same acritarchs as Bunyeroo and lower Wonoka Formations, Adelaide Geosyncline.||||||
15094|Pertatataka Formation|66767|5|Briefly described|p60|Neoproterozoic|Neoproterozoic|NE Amadeus Basin. 350m thick in its type section; locally up to 1400m thick. Deep-water, pelagic deposits.|||||Predominantly red and green siltstone, shale and feldspathic sandstone.|
15094|Pertatataka Formation|67326|4|Described|p2, p7-10, Appx.2|Neoproterozoic|Neoproterozoic|Amadeus Basin. Intersected by stratigraphic drillhole BRD05DD01. Over 450m thick. South of the Angas Lineament Zone (previously the Central Ridge), the Winnall beds are widespread and 400-500m thick; the authors state that the term is redundant, and the rocks subsumed into the Pertatataka Formation. Probable source of gas in the Dingo gas field; a potential source rock for dry gas over wide areas of the Basin. Rockeval Pyrolysis results discussed. Core section photographs. Composite log.||||Conformably to disconformably overlies Olympic or Bitter Springs Formations. Is overlain by Julie Formation.|Red-brown to occasionally grey siltstone and mudstone, becoming evaporitic towards the top. Occasional upward-fining cycles representing turbidity current deposits.|
15094|Pertatataka Formation|67484|6|Mentioned|p294 Tb.1|Ediacaran|Ediacaran|Amadeus Basin.||||Overlain by the Julie Formation. Underlain by the Olympic Formation.||
15094|Pertatataka Formation|67565|5|Briefly described|p5 Fig.3, p39, p46.|Ediacaran|Ediacaran|Amadeus Basin. Deep water siliciclastic sediments. Forms strike ridges. 350 m thick, increasing to the west.||||Is overlain unconformably by the Arumbera Sandstone.|White to yellow-brown, laminated and thinly-bedded, fine-grained kaolinitic sandstone; poorly exposed interbeds of laminated micaceous siltstone.|
15094|Pertatataka Formation|67620|6|Mentioned|p5, 22|Ediacaran|Ediacaran|Amadeus Basin. Contains abundant organic laminae (microbial mats).||||Overlies Olympic Formation. Is overlain by Julie Formation.||
15094|Pertatataka Formation|67856|5|Briefly described|p338 fig 4-30, p337, p345 |Neoproterozoic|Neoproterozoic|||||Underlain by Olympic Formation.||
15094|Pertatataka Formation|67912|6|Mentioned|p12, 25-27|||Amadeus Basin. Contains diverse assemblages of complex, large acritarchs.||||||
15094|Pertatataka Formation|68270|5|Briefly described|p679,683-684|Ediacaran|Ediacaran|Amadeus Basin.||||Overlain by Julie Formation. Underlain by Pioneer Sandstone and Olympic Formation.||
15094|Pertatataka Formation|68271|6|Mentioned|p696|||Adelaide Rift Complex.||||||
15094|Pertatataka Formation|68275|6|Mentioned|p61|||Variations in the Ediacaran sulfur-isotope record world-wide are briefly discussed.||||||
15094|Pertatataka Formation|68276|6|Mentioned|p71, 73-74|||Amadeus Basin. The ""Formation"" is omitted.",,||||Conformably overlies Olympic Formation.|Reddish-grey laminated siltstone with limestone turbidites.|
15094|Pertatataka Formation|68323|6|Mentioned|p4 Fig.2|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
15094|Pertatataka Formation|68473|6|Mentioned|p531|||Amadeus Basin.||||||
15094|Pertatataka Formation|68733|6|Mentioned|p189 Fig.8|Ediacaran|Ediacaran|Amadeus Basin.||||||
15094|Pertatataka Formation|69031|6|Mentioned|p4, p9|||Amadeus Basin. Formerly part of Boord Formation (name discontinued).||||||
15094|Pertatataka Formation|69437|5|Briefly described|p22:4-5, 7|Ediacaran|Ediacaran|NE Amadeus Basin, Centralian A Superbasin. Supersequence 3.||||Overlies Pioneer and Gaylad Sandstones. Is overlain by Julie Formation.|Siltstone and shale.|12-JUL-16
15094|Pertatataka Formation|69438|2|Defined|p23:2-5, 7-8, 10, 17-21, 27,43,47, 59-60|Ediacaran|Ediacaran|Pritchard and Quinlan (1962). The type section is 5km W of Ellery Creek and c.350m thick. Originally defined with two clastic units separated by a dolomite layer. Only the lower clastic unit remains to constitute the Formation; the other units are now the Olympic and Julie Formations. Amadeus Basin. Up to 1400m thick. Generally recessive; the Cyclops Member forms low ridges in places. Previously correlated with Winnall beds, but that unit is now correlated with Carnegie Formation and Arumbera Sandstone. One of the most likely oil- and/or gas-prone units in the Basin. Thick shales form seals over older reservoirs.|||Cyclops, Waldo Pedlar Members.|Disconformably overlies Olympic Formation, Pioneer Sandstone or Bitter Springs Formation. Is overlain conformably by Julie Formation.|Mainly (320m) red and green siltstone and shale, with flaser bedding, small-scale cross-laminations and thin interbeds of fine-grained sandstone; overlain by 1.5m of grey medium-grained feldspathic silicified sandstone and 30m of red siltstone.|12-JUL-16
15094|Pertatataka Formation|69443|6|Mentioned|p28:10|||Amadeus Basin. Correlates with part of the Mopunga Group (Georgina Basin).||||||12-JUL-16
15094|Pertatataka Formation|69606|4|Described|p1, p4 fig 2, p5, p6 fig 3, p7 fig 4, |Early Ediacaran|Early Ediacaran|c. 300m thick. Potential source and seal rock. Amadeus Basin. Type area In north-central Amadeus Basin mentioned. Contact with the Julie Formation is poorly exposed. See also  p14, p15 fig 8, p16, p18, p19.||||Overlies the Pioneer Sandstone and the Olympic Formation. Conformably (gradational) overlain by the Julie Formation.|Red and green siltstone, shale and minor sandstone.|
15094|Pertatataka Formation|69673|5|Briefly described|p63, p74, p80, p81, p86, p88, p90, p97,|Neoproterozoic|Neoproterozoic|Up to 1400m thick. Potential source rock and unconventional gas potential.|||Includes Cyclops Member, Waldo Pedlar Member|Overlain by Julie Formation, conformably overlies Gaylad Sandstone, overlies Pioneer Sandstone, correlated with Winnall beds|Siltstone, shale and feldspathic sandstone.|
15094|Pertatataka Formation|69937|5|Briefly described|v Fig.1, vi, p3 Tb.1, p14, p20, p23|Neoproterozoic|Neoproterozoic|See also p25-31, p51-54. Amadeus Basin. Inferred depositional age of ~575 Ma.|||Cyclops, Waldo Pedlar Members.|Overlies Olympic Formation unconformably and Gaylad Sandstone conformably. Is overlain conformably by Julie Formation.|Mainly grey-green and purple-brown laminated, micaceous siltstone and shale with thin interbeds of sandstone and limestone.|
15094|Pertatataka Formation|70018|5|Briefly described|p235|Neoproterozoic|Neoproterozoic|Amadeus Basin. Of Supersequence 3 in the northern Amadeus Basin. Correlable to Inindia Beds in the southern Amadeus Basin.||||Overlain by Julie Formation. Underlain by Pioneer Sandstone.||
15094|Pertatataka Formation|70416|5|Briefly described|p63-65, p80|Ediacaran|Ediacaran|Amadeus Basin. Earlier definitions included rocks subsequently assigned to Aralka Formation.|||Waldo Pedlar, Cyclops Members.|Overlies Olympic Formation and Pioneer Sandstone. Is overlain by Julie Formation.||
15094|Pertatataka Formation|70839|5|Briefly described|p329|Ediacaran|Ediacaran|Of Amadeus Basin.|||Includes Gaylad Sandstone.|Overlain by Julie Formation. Underlain by Olympic Formation or Pioneer Sandstone.||
15094|Pertatataka Formation|71001|5|Briefly described|p18 Fig.2, p20, 23, 27-28|Ediacaran|Ediacaran|Amadeus Basin. Marine deposits. Carbon isotope correlation graph.|||Waldo Pedlar, Cyclops Members.|Overlies Gaylad Sandstone. Is overlain by Julie Formation.|Dominantly marine pyritic shale.|
15094|Pertatataka Formation|71080|6|Mentioned|p29 fig 20, p30, 31|Ediacaran|Ediacaran|Amadeus Basin. Supersequence 3. Probable source rock for Dingo Field in eastern Amadeus.|||||Dominantly shale in WA. Includes carbonate and sandstone in NT.|
15094|Pertatataka Formation|71088|5|Briefly described|p2, p8, p15|lower Ediacaran|lower Ediacaran|Northern and eastern Amadeus Basin. The lower part of this formation was correlated with the Ellis Sandstone, Sir Frederick Conglomerate and the Maurice Formation by Wells et al., 1970; Grey, 1990; Lindsay and Korsch, 1991.||||||
15094|Pertatataka Formation|71279|5|Briefly described|p353, p355 Fig.2, p365-368, p370, p382|Ediacaran|Ediacaran|Amadeus Basin. Contains interbedded reduced and oxidised iron-rich layers. Contains zircons aged c.1.3 to 0.8 Ga sourced from Tjauwata Group (Musgrave Province). Magnetisation discussed in detail. Modelled magnetic properties.|||||Highly weathered grey-green shale and salty dolomite.|
15094|Pertatataka Formation|71288|6|Mentioned|p146|||Implications of a c.540 Ma paleopole position from this unit discussed.||||||
15094|Pertatataka Formation|71344|4|Described|p1092, 1094, 1095, 1096-1103|Ediacaran||Amadeus Basin. Includes acritarch assemblages that give depositional age constraints (Zhou et al., 2007). Deposited under marine conditions. 300-550 m thick.|635 - 582 Ma|Of Pertaoorta Package.|Includes Waldo Pedlar Member, Cyclops Member.|Conformably overlies the Olympic Formation, Gaylad Sandstone and is succeeded by the Julie Formation.|Red, green to dark green shales and siltstones. Lower and middle part dominated by laminated, dark grey, pyritic siltstone and shale.|10-NOV-17
15094|Pertatataka Formation|71800|6|Mentioned|p26 fig 3|Ediacaran|Ediacaran|Amadeus Basin.||||Overlain by the Julie Formation.||
15094|Pertatataka Formation|71801|6|Mentioned|p230-p231|Ediacaran|Ediacaran|Amadeus Basin.||||Overlain by the Julie Formation.||
15094|Pertatataka Formation|71810|5|Briefly described|Map legend.|Ediacaran|Cryogenian|Amadeus Basin (Phase 1), Centralian Superbasin.|||||Siltstone, shale, and minor sandstone; very poorly exposed.|
15094|Pertatataka Formation|71841|5|Briefly described|p1-2,13|Ediacaran|Ediacaran|Of Amadeus Basin. Original stratigraphy based on McKinnon-Matthews (2009): CPD003: 181.3-219m EOH. Revised stratigraphy in drill core: not intersected.|||Includes Cyclops and Waldo Pedlar members.|Overlain by Julie Formation. Underlain by Pioneer Sandstone or Gaylad Sandstone. Grades into Inindia beds.||
15094|Pertatataka Formation|71842|5|Briefly described|p1-3,9|Ediacaran|Ediacaran|Of Amadeus Basin. Nomenclature after Edgoose 2013 (NE Amedeus, NT).|||Includes Cyclops Member and Waldo Pedlar Member.|Overlain by Julie Formation. Underlain unconformably by Olympic/Pioneer Formation. Correlable with Winnall beds.||
15094|Pertatataka Formation|71898|5|Briefly described|p6|||Amadeus Basin.||||Unconformably (possibly) overlain by the Quandong Conglomerate.||
15094|Pertatataka Formation|72360|5|Briefly described|Solid Geology map|||Of Amadeus Basin.||||||
15094|Pertatataka Formation|72369|4|Described|iii,p3-4,11,14-p15|||Of Amadeus Basin. Originally of Pritchard and Quinlan, 1962. Maidment (2005) provided an inferred depositional age of 575 Ma; further inferred age constraint provided by its stratigraphic position above the Gaylad Sandstone that was deposited during the c. 640-580 Ma Elatina Glaciation (Walter et al 1995). LA-ICP-MS U-Pb detrital zircon dating of sample HB15ND364 (very coarse- to coarse grained sandstone) yielded an interpreted maximum depositional age of 822+\-11 Ma (youngest concordant zircon) does not further constrained the depositional age of the Pertatataka Formation as it is significantly older than the 575 Ma inferred depositional age of Maidment (2005). Contains significant proportion of detrital zircons derived from Musgrave Province (between c. 1500 Ma and c. 970 Ma age spectrum), and Aileron and Warumpi provinces (c. 1810 to c. 1625 Ma age spectrum), and minor Archean-Plaeoproterozoic (>c. 1780 Ma) and Neoproterozoic zircons indicate potential distal sources from the Amadeus Basin. Sample locality, zircon description, SHRIMP results and analyses are discussed.|||Includes Waldo Pedlar and Cyclops members.|Overlain by Winnall Group. Overlies the Gaylad Sandstone.|Red and green siltstone, shale, and fine to medium-grained feldspathic sandstone. Fine to medium-grained, red-brown quartz sandstone.|18-DEC-19
15094|Pertatataka Formation|72374|5|Briefly described|p14|||Of Amadeus Basin. Provenance spectra of Waldo Pedlar Member dominated by Musgrave Province-sourced zircon with lesser zircon sourced from Aileron and Warumpi provinces.|||Includes Waldo Pedlar Member.|||11-OCT-19
15094|Pertatataka Formation|72375|4|Described|p1-2,19-20,23,25,27,29,31|Neoproterozoic|Neoproterozoic|Of Amadeus Basin. Nomenclature of Pritchard and Quinlan 1962. Intepreted maximum depositional age of c. 575 Ma (Maidment 2005). Deep water depositional environment.|||Includes Waldo Pedlar Member, Cyclops Member.|Overlain conformably by Julie Formation. Underlain unconformably by Gaylad Sandstone.|Grey-green and purple-brown laminated, micaceous siltstone and shale with thin interbeds of sandstone and limestone.|
15094|Pertatataka Formation|72489|6|Mentioned|p4 Fig.3, p4|Ediacaran|Ediacaran|Located in the Amadeus Basin.|>548.8 +/- 1 Ma|||Overlain by Julie Formation.||
15094|Pertatataka Formation|72516|6|Mentioned|p88-89|Ediacaran|Ediacaran|Amadeus Basin.|||Includes the Cyclops Member.|Lower part equivalent to the Elyuah Formation. Cyclops Member equivalent to Grant Bluff Formation.||02-JUN-21
15094|Pertatataka Formation|72601|5|Briefly described|p3-4, p7-9, p11-12, p17, p25|Ediacaran|Ediacaran|Amadeus Basin. Preiss et al. (1978) subdivided the original Pertatataka Formation into five formations; Aralka Formation, Olympic Formation (former Olympic Member), Pioneer Sandstone, the revised Pertatataka Formation, and Julie Formation.||||Underlain by Olympic Formation and Pioneer Sandstone. Overlain by Julie Formation.||
15094|Pertatataka Formation|73085|4|Described|piii, p1, p3, p15-16, p18-19, p26-27|Ediacaran|Ediacaran|Amadeus Basin. Lithology is here described from a 136-metre-thick equivalent in drillhole BR05DD01. Sharp contact with underlying Aralka Formation marked by abrupt lithological change.|||Cyclops Member, Waldo Pedlar Member|Unconformably underlain by Aralka Formation, Pioneer Sandstone [/ Olympic Formation] and Gaylad Sandstone. Overlain by Julie Formation. Equivalent to Inindia beds.|Red-brown calcareous siltstone and fine-grained sandstone, micaceous, becoming green-grey siltstone with fine-grained sandstone intervals, calcareous.|
15094|Pertatataka Formation|73086|1|Redefined|[See comments].|Ediacaran|Ediacaran|[Defined herein. No revised definition card]. Post-glacial transgressive unit. Characterised by red and green siltstone with localised conglomerate. Amadeus Basin. Part of Supersequence III. Named was first used by Madigan (1932) from a dictionary of the Arunta language meaning red rock. Type section: Ellery Creek. Key locality: Olympic Bore. Distribution: extends across most of the eastern and central parts of the basin although it is generally poorly exposed (typically only several metres thick); exposures are best in the northeast. Type section thickness: 350 m. Maximum thickness: 1800 m. Originally included several units that were later separately defined such as Ringwood Member, Limbla Member, Aralka Formation, Olympic Formation, Julie Formation. Undivided Pertatataka Formation siltstones referred to as lower, middle or upper Pertatataka Formation according to position relative to formal members, or as undivided Pertatataka Formation where specific level is uncertain or referring to the unit as a whole. Can be difficult to distinguish the unit from siltstones of the Aralka Formation and non-diamictite lithologies of the Olympic Formation. No known macrofossils; large sphaeromorph and acanthomorph acritarch assemblages found in this unit; used to correlate with Rodda beds. Inferred depositional age of 575 Ma (Maidment, 2005). A detrital zircon maximum depositional age of ca 807 Ma is significantly older than the inferred true depositional age. Thinly bedded siltstone represents a quiet, marine depositional setting. Also correlates to Rodda beds, Elyuah Formation, Grant Bluff Formation, Gnallan-a-gea Arkose, Cox Formation, Bukalara Formation, Buckingham Bay Sandstone, Raiwalla Shale, Mount Doreen Formation, Bunyeroo Formation, Brachina Formation, ABC Range Quartzite. p: 3, 5-6, 53, 71-72, 75, 78-79, 90-91, 99-101, 107, ~113-118, 121-135, 143, 160, 163-169, 171.|ca 570 Ma||Cyclops Member, Waldo Pedlar Member|Conformably underlain by Pioneer Sandstone, Olympic Formation, Gaylad [Sandstone]. Overlain by Julie Formation. Correlates to upper Inindia beds and more [see comments].|Red and green siltstone with lenticular bedding, small-scale cross-laminations, and thin interbeds of sandstone overlain by grey, medium-grained, silicified, feldspathic sandstone, which in turn is overlain by red siltstone with sandstone laminae.|
15094|Pertatataka Formation|73088|6|Mentioned|p1|Ediacaran|Ediacaran|Amadeus Basin, northeast.|||Cyclops Member, Waldo Pedlar Member|Unconformably underlain by Pioneer Sandstone and Gaylad Sandstone. Overlain by Julie Formation.||
15094|Pertatataka Formation|73180|4|Described|p47-49, p51 Fig.6, p52|Neoproterozoic|Neoproterozoic|Amadeus Basin.|||Cyclops Member and Waldo Pedlar Members|Conformably overlies the Olympic Formation and Pioneer Sandstone, conformably underlies the Julie Formation.|Primarily red, brown and green shales, siltstones and fine sandstones.|
15094|Pertatataka Formation|73279|5|Briefly described|p3, p6-7|Ediacaran|Ediacaran|Amadeus Basin, eastern. Detrital zircons analysed for Hf isotopic composition [see article].||||May be equivalent to Gloaming Formation.|Includes sandstone.|
15099|Pertnjara Group|9199|5|Briefly described|Map legend|Devonian|Devonian|Includes the Brewer Conglomerate and Hermannsburg Sandstone.  Geological Province: Amadeus Basin.||||||04-NOV-04
15099|Pertnjara Group|9814|5|Briefly described|Map Legend|Devonian|Devonian|||||||
15099|Pertnjara Group|22560|5|Briefly described|p3|Late Devonian|Middle Devonian|||||||
15099|Pertnjara Group|22561|4|Described|p26||Early Devonian|||||||
15099|Pertnjara Group|22564|4|Described|p60||Devonian|Min age - ? Carboniferous.  Underlain by Mereenie Sandstone.||||||22-NOV-06
15099|Pertnjara Group|22566|5|Briefly described|p84|Carboniferous|Early Devonian|||||||12-APR-12
15099|Pertnjara Group|22646|6|Mentioned|p 105|||||||||
15099|Pertnjara Group|22650|5|Briefly described|p 165|Carboniferous|Devonian|||||||
15099|Pertnjara Group|22651|6|Mentioned|Fig 10 btw p182-183||Devonian|||||||
15099|Pertnjara Group|22655|5|Briefly described|p 255|||||||||
15099|Pertnjara Group|22656|6|Mentioned|p 277||Devonian|||||||
15099|Pertnjara Group|22657|6|Mentioned|p 297|Devonian|Devonian|||||||
15099|Pertnjara Group|22760|4|Described|p333-337|Late Devonian|Middle Devonian|||||||
15099|Pertnjara Group|22761|6|Mentioned|p350|Late Devonian|Early Devonian|||||||
15099|Pertnjara Group|22762|5|Briefly described|p377||Devonian|Distal equivalent to the Finke Group p376.||||||
15099|Pertnjara Group|22763|6|Mentioned|p394||Late Devonian|||||||
15099|Pertnjara Group|22804|4|Described|p442|Carboniferous|Middle Devonian|||||||
15099|Pertnjara Group|22805|5|Briefly described|p465||Middle Devonian|||||||
15099|Pertnjara Group|22807|6|Mentioned|Fig 3 on p495|||Age - (?)Middle Devonian-(?)Late Devonian.||||||
15099|Pertnjara Group|22824|5|Briefly described|p525|||||||||
15099|Pertnjara Group|23282|6|Mentioned|p83|||May correlate with Mimili Formation. In the Amadeus Basin.||||||22-NOV-06
15099|Pertnjara Group|23361|5|Briefly described|15|Devonian|Devonian|||||||
15099|Pertnjara Group|23732|5|Briefly described|p31|Late Devonian|Devonian|Geological Province: Amadeus Basin.||||||
15099|Pertnjara Group|23858|5|Briefly described|p913|Devonian||Underlain by Mereenie Sandstone. Geological Province: Amadeus Basin.||||||22-NOV-06
15099|Pertnjara Group|24063|5|Briefly described|p220|Early Carboniferous|Late Devonian|Geological Province: Amadeus Basin. Maximum thicknes: 3650m.||||||
15099|Pertnjara Group|24064|5|Briefly described|p229 Fig.7|Carboniferous|Devonian|Geological Province: Amadeus Basin.||||||
15099|Pertnjara Group|24111|6|Mentioned|p214 Fig. 9|||Geological Province: Amadeus Basin.||||||
15099|Pertnjara Group|29442|6|Mentioned|p103|||||||||
15099|Pertnjara Group|29721|6|Mentioned|Table 44|||||||||
15099|Pertnjara Group|29807|6|Mentioned|p13|||||||||
15099|Pertnjara Group|29817|6|Mentioned|p13|||||||||
15099|Pertnjara Group|29972|6|Mentioned|p4|||Devonian-Carboniferous||||||
15099|Pertnjara Group|30238|4|Described|p68|||Upper Devonian to Carboniferous age||||||
15099|Pertnjara Group|30258|6|Mentioned|Fig.2|||Devonian - ?Carboniferous||||||
15099|Pertnjara Group|30544|6|Mentioned|p51|||||||||
15099|Pertnjara Group|30659|6|Mentioned|p87|||||||||
15099|Pertnjara Group|31566|4|Described|p230|||See also p231. Refers Wells et al. (1970).||||||22-NOV-06
15099|Pertnjara Group|31567|6|Mentioned|p273|||Refers Finke Group.||||||22-NOV-06
15099|Pertnjara Group|31707|6|Mentioned|Table 1|||||||||
15099|Pertnjara Group|31991|4|Described|p294|||Struct. geol. and geol.history.||||||22-NOV-06
15099|Pertnjara Group|32208|6|Mentioned|Map legend|Devonian|Devonian|||||||
15099|Pertnjara Group|32209|6|Mentioned|Map legend|Devonian|Devonian|||||||
15099|Pertnjara Group|32640|6|Mentioned|p235|||||||||
15099|Pertnjara Group|32865|6|Mentioned|p482|||||||||
15099|Pertnjara Group|33103|6|Mentioned|p25|||||||||
15099|Pertnjara Group|33306|6|Mentioned|p206|||||||||
15099|Pertnjara Group|33307|6|Mentioned|Fig.6|||||||||
15099|Pertnjara Group|33326|6|Mentioned|p449|||Fauna.||||||
15099|Pertnjara Group|33761|6|Mentioned|p146|||Devonian - Carb?||||||
15099|Pertnjara Group|33971|6|Mentioned|p30|||Refers stratigraphy.||||||
15099|Pertnjara Group|34111|5|Briefly described|Table 2|||Devonian - Carboniferous. See also pp5,6,14,16.||||||22-NOV-06
15099|Pertnjara Group|34186|6|Mentioned|Fig.3|||Devonian - Permian. See also Figs 4,8.||||||
15099|Pertnjara Group|34442|5|Briefly described|Table 1|||Devonian - Carboniferous||||||
15099|Pertnjara Group|34579|4|Described|Table 3|||Devonian - Carboniferous. See also pp16,17.||||||22-NOV-06
15099|Pertnjara Group|34580|4|Described|Table 1|||||||||
15099|Pertnjara Group|34810|6|Mentioned|p9|||Re ages.||||||
15099|Pertnjara Group|35102|6|Mentioned|Fig.2|||||||||
15099|Pertnjara Group|35628|6|Mentioned|Table 3|||||||||
15099|Pertnjara Group|36473|6|Mentioned|Map legend|Carboniferous|Devonian|Between Carboniferous and Devonian||||||
15099|Pertnjara Group|38319|6|Mentioned|p328|||||||||
15099|Pertnjara Group|38606|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
15099|Pertnjara Group|38885|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
15099|Pertnjara Group|39213|6|Mentioned|p15|||Molasse conglomerate. Fig.6||||||
15099|Pertnjara Group|39565|6|Mentioned|Fig.14|||||||||
15099|Pertnjara Group|39583|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
15099|Pertnjara Group|40201|5|Briefly described|p691|||||||||
15099|Pertnjara Group|40740|3|Fully described|p60|||Briefly described p6.||||||22-NOV-06
15099|Pertnjara Group|40810|5|Briefly described|p12|||||||||
15099|Pertnjara Group|40906|6|Mentioned|Fig.11|||||||||
15099|Pertnjara Group|41018|6|Mentioned|p234|||||||||
15099|Pertnjara Group|41039|6|Mentioned|Fig.2|||||||||
15099|Pertnjara Group|41125|6|Mentioned|p40|||See also fig.24.||||||
15099|Pertnjara Group|41190|6|Mentioned|p267|||||||||
15099|Pertnjara Group|41204|6|Mentioned|p14|||||||||
15099|Pertnjara Group|41224|6|Mentioned|Fig.2|||||||||
15099|Pertnjara Group|41270|6|Mentioned|p268|||||||||
15099|Pertnjara Group|41385|6|Mentioned|p363|||See also Fig.12||||||
15099|Pertnjara Group|41492|6|Mentioned|p158|||||||||
15099|Pertnjara Group|41708|6|Mentioned|Fig.1|||||||||
15099|Pertnjara Group|41717|6|Mentioned|Fig.2|||||||||
15099|Pertnjara Group|41723|6|Mentioned|Map legend|Late Devonian||||||||
15099|Pertnjara Group|41820|6|Mentioned|p6|||See also Fig.3||||||
15099|Pertnjara Group|42060|6|Mentioned|Fig.5 P140|||||||||
15099|Pertnjara Group|42141|6|Mentioned|Fig.3 P570|||||||||
15099|Pertnjara Group|42351|6|Mentioned|p46|||In the Amadeus Basin.||||||22-NOV-06
15099|Pertnjara Group|42354|6|Mentioned|p7|||||||||
15099|Pertnjara Group|42504|6|Mentioned|p80|||||||||
15099|Pertnjara Group|42564|6|Mentioned|p12|||In the Amadeus Basin.||||||22-NOV-06
15099|Pertnjara Group|42643|6|Mentioned|p32|||||||||
15099|Pertnjara Group|42699|5|Briefly described|map legend|Devonian||||||||
15099|Pertnjara Group|42845|5|Briefly described|p496|||||||||
15099|Pertnjara Group|42940|5|Briefly described|Plate 2|Devonian|Devonian|Sandstone, siltstone, conglomerate, limestone; fish fossils.  Age: 410-360Ma. Geological province: Amadeus Basin.||||||23-JAN-08
15099|Pertnjara Group|43035|4|Described|p23|||||||||
15099|Pertnjara Group|43105|5|Briefly described|Fig.3,p8.|||||||||
15099|Pertnjara Group|43225|5|Briefly described|Map Legend||Devonian|In the Amadeus Basin.||||||22-NOV-06
15099|Pertnjara Group|43503|6|Mentioned|32-50|Late Devonian|Middle Devonian|||||||
15099|Pertnjara Group|43631|6|Mentioned|p27|||||||||
15099|Pertnjara Group|43646|6|Mentioned|p553||Devonian|||||||
15099|Pertnjara Group|43647|6|Mentioned|p530|||||||||
15099|Pertnjara Group|43648|5|Briefly described|Fig.1,p488|||||||||
15099|Pertnjara Group|43649|5|Briefly described|fig.1,p454-455,459|||||||||
15099|Pertnjara Group|43749|6|Mentioned|p37|||||||||
15099|Pertnjara Group|43817|6|Mentioned|Fig.1,p62|||||||||
15099|Pertnjara Group|44133|5|Briefly described|p44|Devonian|Devonian|Includes: Parke Siltstone.||||||
15099|Pertnjara Group|44342|4|Described|p.6, Table 2|Carboniferous|Devonian|SG/53-5. Dev-Carbon.||||||
15099|Pertnjara Group|44343|14|Not recorded|map legend|Carboniferous|Devonian|Dev. to Carbon.||||||
15099|Pertnjara Group|44393|6|Mentioned|p.6,7,8,Fig.1|||Correlated with Finke Group.||||||
15099|Pertnjara Group|44395|14|Not recorded|p.9,10,12, Tb.2|||Devonian?||||||
15099|Pertnjara Group|44402|5|Briefly described|map legend|Carboniferous|Devonian|Includes Hermannsburg Sandstone and Parke Siltstone. Dev-Carb.||||||02-DEC-04
15099|Pertnjara Group|44433|14|Not recorded|map legend|||Devonian to Carboniferous.||||||
15099|Pertnjara Group|44484|14|Not recorded|p.5,8,9,11,Tb.1,Fig4|Carboniferous|Devonian|Defn on Tech.File F/53-13. Dev-Carb.||||||
15099|Pertnjara Group|44485|14|Not recorded|map legend|Carboniferous|Devonian|Includes Parke Silstone, Hermannsburg Sandstone. Dev-Carb.||||||
15099|Pertnjara Group|44493|4|Described|p.13, map|Carboniferous|Devonian|BLOODS RANGE sheet (G53-3). Dev-Carb.||||||22-NOV-06
15099|Pertnjara Group|44494|14|Not recorded|map legend|Carboniferous|Devonian|Devonian-Carboniferous.||||||
15099|Pertnjara Group|44495|4|Described|p.9, map|Carboniferous|Devonian|AYERS ROCK sheet (G52-8). Devonian-Carb.||||||22-NOV-06
15099|Pertnjara Group|44496|5|Briefly described|map legend|Carboniferous|Devonian|Red-brown siltstone.  Devonian-Carboniferous.||||||22-NOV-06
15099|Pertnjara Group|44497|4|Described|p.11, Table 2|Carboniferous|Devonian|SF/53-13. Dev-Carb.||||||
15099|Pertnjara Group|44498|14|Not recorded|map legend|Carboniferous|Devonian|Dev-Carb.||||||
15099|Pertnjara Group|44505|14|Not recorded|p.2,8, Fig.11|Carboniferous|Devonian|Dev-Carb.||||||
15099|Pertnjara Group|44506|14|Not recorded|map legend|Carboniferous|Devonian|Devonian-Carboniferous.||||||
15099|Pertnjara Group|45041|4|Described|p94|||See also ppP95-102. U.Dev. to L.Carb.||||||22-NOV-06
15099|Pertnjara Group|45097|6|Mentioned|p27|||See also p28. Brachiopods.||||||22-NOV-06
15099|Pertnjara Group|45140|5|Briefly described|p13-14, p64-65|Early Carboniferous|Devonian|Wells et al. (1970). Amadeus Basin. Non-marine: broad alluvial plain deposits. Similar lithology to Pedestal Beds. Equivalent to Angas Hills Beds.|||Parke Siltstone.|Correlated with Lucas Formation.||
15099|Pertnjara Group|45148|6|Mentioned|p20|||||||||
15099|Pertnjara Group|45153|6|Mentioned|p55|||||||||
15099|Pertnjara Group|45155|6|Mentioned|Fig.8|||||||||
15099|Pertnjara Group|45170|6|Mentioned|p9|||||||||
15099|Pertnjara Group|46829|6|Mentioned|Fig.2|||||||||
15099|Pertnjara Group|46830|6|Mentioned|p24|||||||||
15099|Pertnjara Group|46864|6|Mentioned|p40|||||||||
15099|Pertnjara Group|46928|6|Mentioned|Table 1|||||||||
15099|Pertnjara Group|47050|5|Briefly described|p240|||||||||
15099|Pertnjara Group|48890|4|Described|p.49|Carboniferous|Devonian|Ref on wrong card! Pertnjara Formation. See also Tables, Figs and Plates.||||||22-NOV-06
15099|Pertnjara Group|48963|6|Mentioned|p22|||||||||
15099|Pertnjara Group|50246|5|Briefly described|p20 Fig. 2|Carboniferous|Devonian|Includes the N'Dhala Member.||||||07-FEB-11
15099|Pertnjara Group|60547|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Amadeus Basin.||||||03-JUN-05
15099|Pertnjara Group|61154|6|Mentioned|p34|||Geological Province: Amadeus Basin.||||||
15099|Pertnjara Group|61309|6|Mentioned|p15, p17|Devonian|Devonian|Deposited during the Alice Springs Orogeny. Geological Province: northern margin of Amadeus Basin. See also p25 Fig. 11.||||||06-FEB-08
15099|Pertnjara Group|61387|5|Briefly described|Map legend|Devonian|Silurian|Includes Mereenie Sandstone and undifferentiated rocks.  Geological Province: Amadeus Basin.||||||
15099|Pertnjara Group|61519|5|Briefly described|Map Legend|Devonian|Silurian|Geological Province: Amadeus Basin.||||||
15099|Pertnjara Group|62359|5|Briefly described|p544 Fig. 4a, p545||Devonian|Foreland basin unit. Geological Province: Amadeus Basin. See also p546 Fig. 6.||||||
15099|Pertnjara Group|62376|5|Briefly described|p18|Late Devonian|Late Devonian|Geological Province: Amadeus Basin.||||||09-FEB-10
15099|Pertnjara Group|62379|5|Briefly described|p7 Fig. 2|Devonian|Devonian|Geological Province: Amadeus Basin.||||||
15099|Pertnjara Group|62595|5|Briefly described|p29 Fig.6.|Carboniferous|Devonian|Ross River area.|||Includes N'Dahla Member.|||
15099|Pertnjara Group|62609|5|Briefly described|Map Legend|Carboniferous|Devonian|Sandstone, siltstone, conglomerate, some limestone. Overlies Mereenie Sandstone.||||||14-AUG-06
15099|Pertnjara Group|62620|5|Briefly described|Map Legend|Carboniferous|Devonian|Sandstone, siltstone, conglomerate, some limestone.||||||
15099|Pertnjara Group|63562|5|Briefly described|p338 fig 3, p352 fig 10, p350|Devonian|Devonian|Of Amadeus Basin. Upward-coarsening lacustrine, fluvial and alluvial fan deposits; thickening northwards.||||Overlies Mereenie Sandstone unconformably. Correlated to Dulcie Sandstone and Ethabuka Sandstone.|Upward-coarsening succession of lacustrine, fluvial and alluvial fan deposits.|
15099|Pertnjara Group|64334|5|Briefly described|p42|Devonian|Devonian|Deposition was synchronous with the main phase of the Alice Springs Orogeny.|||||Thick wedges of generally coarsening-upward non-marine clastic sediments.|
15099|Pertnjara Group|64778|6|Mentioned|p12-13, 33|Devonian|Devonian|N Amadeus Basin margin. Up to 3000m of clastics following the 375-340 Ma Pertnjara Movement (Alice Springs Orogeny).||||||
15099|Pertnjara Group|64809|5|Briefly described|p3, p6 Fig.4 |Late Devonian|Late Devonian||||Includes the Brewer Conglomerate, Hermannsburg Sandstone and Parke Siltstone.|||
15099|Pertnjara Group|64970|6|Mentioned|p719 Fig. 2|Devonian|Silurian|Geological Province: Amadeus Basin.||||||27-MAY-09
15099|Pertnjara Group|65074|6|Mentioned|p360|Devonian|Devonian|Amadeus Basin.||||Probably correlated with Lucas Formation and Pedestal beds (of Birrindudu Basin).||
15099|Pertnjara Group|65232|5|Briefly described|p72, p10 Fig 9.||Late Devonian|Includes Brewer Conglomerate at top. Thick succession of Late Devonian terrestrial sediments. Geol.Prov: Amadeus Basin.||||||09-FEB-10
15099|Pertnjara Group|65233|4|Described|p3 Fig. 2, p13|Late Devonian|Middle Devonian|Unconformable on Mereenie Sandstone. Geological province: Amadeus Basin. Written only as Pertnjara. Upward-coarsening foreland basin succession forming a thick clastic wedge - details incl.||||||07-FEB-11
15099|Pertnjara Group|65272|6|Mentioned|p319, p320 Fig.3|Late Devonian|Late Devonian|Deformed by the Alice Springs Orogeny.||||||
15099|Pertnjara Group|65309|5|Briefly described|p13, p16, pp18-19. |Devonian|Devonian|Central and northern Amadeus Basin. Interfingers with Finke Group. Ongoing uplift resulted in deposition of thicker and more extensive (than Finke Group), upward-coarsening sequence.|||Includes Parkes Siltstone.|||
15099|Pertnjara Group|65342|5|Briefly described|p3.|||Amadeus Basin. Max. thickness at least 194 m.||||Overlies Mereenie Sandstone.|Sandstone, siltstone, conglomerate, some limestone.|
15099|Pertnjara Group|65382|6|Mentioned|p711|Late Devonian|Middle Devonian|||||||
15099|Pertnjara Group|65489|6|Mentioned|p125|Devonian|Devonian|Amadeus Basin.||||||
15099|Pertnjara Group|66498|6|Mentioned|p45|||Amadeus Basin, central Australia.||N'Dhala Member.||||
15099|Pertnjara Group|66589|6|Mentioned|p180|Famennian|Givetian|Case studies cited; not visited in the field by the authors of this study.||||||
15099|Pertnjara Group|66767|5|Briefly described|p60|Devonian|Devonian|Amadeus Basin. Consists of a series of lacustrine, braided and meandering fluviatile and alluvial fan deposits during the Alice Springs Orogeny.|||Parke Siltstone, Hermannsburg Sandstone, Brewer Conglomerate.|Unconformably overlies Mereenie Sandstone.||
15099|Pertnjara Group|67326|5|Briefly described|p2|Late Devonian|Late Devonian|Amadeus Basin.|||Parke Siltstone, Hermannsburg Sandstone, Brewer Conglomerate.|Overlies Larapinta Group.||
15099|Pertnjara Group|67565|5|Briefly described|p5 Fig.3, p42.|||Amadeus Basin.|||Includes Parke Siltstone and Hermannsburg Sandstone.|Overlies Mereenie Sandstone.||03-DEC-15
15099|Pertnjara Group|67856|5|Briefly described|p338, 348|Late Devonian|Late Devonian||||Includes Parke Siltstone, Hermannsburg Sandstone, Brewer Conglomerate.|Unconformably overlies Mereenie Sandstone in N and E of basin.||
15099|Pertnjara Group|68298|6|Mentioned|p226|||Amadeus Basin. Unfossiliferous. Said to be similar age to Aztec Siltstone fauna, Antarctica.||||||
15099|Pertnjara Group|68323|6|Mentioned|p4 Fig.2|Late Devonian|Late Devonian|Amadeus Basin.|||Parke Siltstone, Hermannsburg Sandstone, Brewer Conglomerate.|||
15099|Pertnjara Group|69031|6|Mentioned|p9|Devonian|Devonian|Eastern Amadeus Basin.||||||
15099|Pertnjara Group|69427|6|Mentioned|p12:47-48|||Amadeus Basin. Synorogenic successions in this unit were progressively tilted as a result of S-directed thrusting in the Devonian.||||||12-JUL-16
15099|Pertnjara Group|69438|4|Described|p23:2-8, 37-40, 42, 46, 48, 50|Famennian|Givetian|Pritchard and Quinlan (1962). Northwest and north-central Amadeus Basin. Thins to the S. Devonian (Givetian- Frasnian)  fish fossils occur at several localities in basal Parke Siltstone. Min age constrained by Famennian spores in Brewer Conglomerate. Deposition was initiated by the Pertnjara Event, and the Group was mildly deformed, uplifted and eroded by the Brewer Event.|||Parke Siltstone, Hermannsburg Sandstone, Brewer Conglomerate.|Unconformably overlies Mereenie Sandstone. Correlative of, and interdigitates with, Finke Group.|A series of lacustrine, braided and meandering fluvial, and alluvial fan deposits.|13-SEP-18
15099|Pertnjara Group|69439|5|Briefly described|p24:11-12|Devonian|Devonian|Amadeus Basin. This unit's lithofacies resembles that of the Kerridy Sandstone (Ngalia Basin).|||Brewer Conglomerate.|||12-JUL-16
15099|Pertnjara Group|69449|6|Mentioned|p34:2 Fig.34.2|Devonian|Devonian|Eastern Amadeus Basin.||||||12-JUL-16
15099|Pertnjara Group|69453|6|Mentioned|p37:1|||Amadeus Basin.||||Stratigraphic equivalent to Pedestal beds.||12-JUL-16
15099|Pertnjara Group|69458|6|Mentioned|p42:8|Devonian|Devonian|Amadeus Basin.||||||12-JUL-16
15099|Pertnjara Group|69606|5|Briefly described|p4 fig 2|Carboniferous|Devonian|Deposited during the Alice Springs Orogeny. Amadeus Basin. Potential seal rock.||||Unconformably overlies the Mereenie Sandstone.|Shale, sandstone and conglomerate.|
15099|Pertnjara Group|69673|6|Mentioned|p67, p149 fig 120||||||Includes Parke Siltstone, Hermannsburg Sandstone, Brewer Conglomerate|Correlated with Finke Group||
15099|Pertnjara Group|69948|6|Mentioned|Fig.4.4|||Amadeus, Georgina and Wiso Basins. Syn-orogenic (Pertnjara Movement/Tabberabberan Orogeny).||||||
15099|Pertnjara Group|71088|6|Mentioned|p17-18|Devonian|Devonian|Amadeus Basin. This unit is locally folded and exposed near the type area of the Ligertwood beds.||||||03-MAY-23
15099|Pertnjara Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, sandstone|
15099|Pertnjara Group|71268|5|Briefly described|1m_geologyp12_lut.csv||||||Includes Mereenie Sandstone.|||
15099|Pertnjara Group|71279|5|Briefly described|p355 Fig.2, p363, p374, p382 Tb.1|Late Devonian|Late Devonian|Amadeus Basin. Modelled magnetic properties.|||Parke Siltstone, Hermannsburg Sandstone, Brewer Conglomerate.|||
15099|Pertnjara Group|72360|5|Briefly described|Map legend|Devonian|Devonian|Of Amadeus Basin.|||Includes Brewer Conglomerate.||Includes calcareous siltstone, siltstone, sandstone.|09-SEP-19
15099|Pertnjara Group|72369|5|Briefly described|iii,p40|Late Devonian|Late Devonian|Of Amadeus Basin.|||Includes Hermannsburg Sandstone.|||
15099|Pertnjara Group|72374|5|Briefly described|iii,p3,23|||Of Amadeus Basin.|||Includes Hermannsburg Sandstone.|||
15099|Pertnjara Group|72476|6|Mentioned|p36 Fig.9|||Amadeus Basin. Time-temperature thermal history diagram.||||||
15099|Pertnjara Group|73085|6|Mentioned|p1|late Devonian|late Devonian||||Brewer Conglomerate, Hermannsburg Sandstone, Parke Siltstone|Underlain by Mereenie Sandstone. Equivalent to Finke Group (Larapinta Group).||
15099|Pertnjara Group|73279|6|Mentioned|p14-15|Devonian|Devonian|Amadeus Basin.|||Hermannsburg Sandstone|||
15112|Petermann Sandstone|22561|5|Briefly described|p21|Neoproterozoic|Neoproterozoic|||||||
15112|Petermann Sandstone|22565|6|Mentioned|p71 in Table 1|||||||||
15112|Petermann Sandstone|22650|6|Mentioned|p 159|Cambrian|Cambrian|||||||
15112|Petermann Sandstone|22651|5|Briefly described|p 187|Late Cambrian|Middle Cambrian|Of the Pertaoorrta Group.||||||22-NOV-06
15112|Petermann Sandstone|22763|6|Mentioned|Table 1 on p386|Cambrian|Cambrian|Of the Pertaoorrta Group.||||||22-NOV-06
15112|Petermann Sandstone|22804|6|Mentioned|Fig 2 on p432|Cambrian|Cambrian|Of the Pertaoorrta Group.||||||22-NOV-06
15112|Petermann Sandstone|22826|6|Mentioned|Fig 2 on p565|Cambrian|Cambrian|||||||
15112|Petermann Sandstone|23250|5|Briefly described|p1124  Fig.2||Late Cambrian|Correlate of Lake Frome Group.||||||
15112|Petermann Sandstone|23361|5|Briefly described|16 Fig.4|Cambrian|Neoproterozoic III|||||||
15112|Petermann Sandstone|29721|6|Mentioned|Table 44|||||||||
15112|Petermann Sandstone|33307|6|Mentioned|Fig.6|||||||||
15112|Petermann Sandstone|34442|5|Briefly described|Table 1|||Cambrian||||||
15112|Petermann Sandstone|35102|6|Mentioned|Fig.2|||||||||
15112|Petermann Sandstone|36198|6|Mentioned|p294|||See also Fig.III.2||||||
15112|Petermann Sandstone|39213|6|Mentioned|Fig.6|||Amadeus Basin Succession||||||
15112|Petermann Sandstone|40740|3|Fully described|p43|||Mention p5.||||||22-NOV-06
15112|Petermann Sandstone|40810|6|Mentioned|p3|||||||||
15112|Petermann Sandstone|41115|6|Mentioned|Fig.2|||||||||
15112|Petermann Sandstone|41190|6|Mentioned|Fig.4|||||||||
15112|Petermann Sandstone|41224|6|Mentioned|Fig.2|||||||||
15112|Petermann Sandstone|41717|6|Mentioned|Fig.2|||||||||
15112|Petermann Sandstone|41723|6|Mentioned|Map legend|Neoproterozoic||||||||
15112|Petermann Sandstone|42082|6|Mentioned|Fig.3 P323|||||||||
15112|Petermann Sandstone|42940|5|Briefly described|Plate 8|||||||||
15112|Petermann Sandstone|43225|5|Briefly described|Map Legend||Cambrian|Of the Pertaoorrta Group.||||||22-NOV-06
15112|Petermann Sandstone|43503|6|Mentioned|12-50|Mindyallan|Boomerangian|||||||
15112|Petermann Sandstone|43649|6|Mentioned|p457|||||||||
15112|Petermann Sandstone|44395|14|Not recorded|p.8||Cambrian|Correlates with Cleland Sandstone.||||||
15112|Petermann Sandstone|44402|5|Briefly described|map legend||Cambrian|Part of Pertaoorrta Group.||||||02-DEC-04
15112|Petermann Sandstone|44484|14|Not recorded|p.10, Tb.1||Cambrian|Part of Pertaoorrta Group.||||||
15112|Petermann Sandstone|44485|14|Not recorded|map legend||Cambrian|Part of Pertaoorrta Group.||||||
15112|Petermann Sandstone|44497|5|Briefly described|p.10, Table 1||Cambrian|SF/53-13.||||||
15112|Petermann Sandstone|44498|14|Not recorded|map legend||Cambrian|Part of Pertaoorrta Group.||||||
15112|Petermann Sandstone|44505|14|Not recorded|Table 1, opp.p.4|||Of Pertaoorrta Group.||||||
15112|Petermann Sandstone|44506|14|Not recorded|map legend||Cambrian|||||||
15112|Petermann Sandstone|45041|5|Briefly described|p53|||M-U Camb. Of the Pertaoorrta Group.||||||22-NOV-06
15112|Petermann Sandstone|45155|6|Mentioned|p34|||||||||
15112|Petermann Sandstone|45170|6|Mentioned|Table 3|||||||||
15112|Petermann Sandstone|48863|2|Defined|p.23||Cambrian|Tb.1. opp.p.7,9,20,22,Pl.10,15,16. (G52-4,G53-1).||||||
15112|Petermann Sandstone|48865|14|Not recorded|Fig.4,opp.p.10||Cambrian|(G52-4,F53-13). Unit of Pertaoorrta Group.||||||
15112|Petermann Sandstone|48963|6|Mentioned|Fig.3|||||||||
15112|Petermann Sandstone|61309|5|Briefly described|p16 Fig. 4|||Geological Province: Amadeus Basin.||||||06-FEB-08
15112|Petermann Sandstone|61385|5|Briefly described|Map legend|Cambrian|Cambrian|Red-brown sandstone, silty sandstone. Geological Province: Amadeus Basin.||||||06-FEB-08
15112|Petermann Sandstone|61732|5|Briefly described|p99|Cambrian|Cambrian|Together with other Cambrian units overlies the Arumbera Sandstone.||||||07-FEB-11
15112|Petermann Sandstone|62379|5|Briefly described|p14|||||||||
15112|Petermann Sandstone|64068|6|Mentioned|p65,67, 69, 70, 225|||Amadeus Basin. Correlated with Steamboat Sandstone, Chabalowe Formation,  Arrinthrunga Formation, Georgina Limestone, Selwyn Range Limestone.||||||
15112|Petermann Sandstone|64778|6|Mentioned|p18|||Amadeus Basin. Thermal and maturation history modelling.||||||
15112|Petermann Sandstone|67326|4|Described|p2-6, p12-13, Appx.2|Late Cambrian|Middle Cambrian|Amadeus Basin. Intersected by stratigraphic drillhole LA05DD01, in which this unit appears to be genetically related to the Deception Siltstone via progradation of a fan-delta/braid-plain succession. Cored section photograph. Contains viable reservoir-quality sandstone. Cu sulfides present. Composite log.||Pertaoorrta Group.||Overlies Deception and Cleland Sandstones. Is overlain by Goyder Formation, and ?disconformably by Pacoota Sandstone. Equivalent to Deception Siltstone, Cleland Sandstone and Shannon Formation.|Red to red-brown, quartz sandstone with haematite-clay matrix; silty mudstone increasing towards the bottom; rare carbonate and glauconite. Unmetamorphosed.|
15112|Petermann Sandstone|67565|5|Briefly described|p40, p47.|||c.250 m thick. Lateral equivalent of Hugh River Shale to the east, and the Cleland Sandstone to the west.||||Conformably overlies Deception Formation. Is overlain conformably by Goyder Formation.|A succession of red-brown and white, fine- and medium-grained, thinly-bedded, cross-bedded and rippled, ferruginous and micaceous sandstone; heavy mineral bands and clay pellets are common.|
15112|Petermann Sandstone|67856|6|Mentioned|p338 fig 4-30|Cambrian|Cambrian|||Of Pertaoorta Group.||||
15112|Petermann Sandstone|68323|5|Briefly described|p1-6, p8-10, p12-15|Late Cambrian|Middle Cambrian|Mineralogy detailed: dominated by quartz and kaolinite. The mineralogy is uniform across the logged boundary with the overlying unit.||Pertaoorrta Group.||Overlies Tempe Formation. Is overlain by Pacoota Sandstone probably conformably.|More lithic and volcanogenic than quartzose.|
15112|Petermann Sandstone|69437|5|Briefly described|p22:10|Series 3|Series 3|Amadeus Basin.||||Overlies Illara Sandstone. Is overlain by Goyder Formation.||12-JUL-16
15112|Petermann Sandstone|69438|4|Described|p23:2-3, 24, 30, 59|Late Cambrian|Middle Cambrian|Wells et al. (1965). Carmichael Sub-basin, Amadeus Basin. Forms prominent red-brown strike ridges. Up to 250m 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.||Conformably overlies and interfingers with Deception Formation. Is overlain gradationally by, and interfingers with, Goyder Formation. Equivalent to upper Hugh River Shale.|Red-brown, fine- to medium-grained, thinly bedded micaceous sandstone, with common cross-beds and ripple marks.|12-JUL-16
15112|Petermann Sandstone|69673|5|Briefly described|p64 fig 53, p80, p82, p83|||Potential source rock. Up to 250m thick.||||Overlies Deception Sandstone, gradationally overlain by lower Goyder Formation|Fine to medium grained, thinly bedded micaceous sandstone with common cross beds and ripple marks,|
15112|Petermann Sandstone|71114|5|Briefly described|p171, p170 fig 1b, p175-177, p180|Guzhangian||Amadeus Basin western succession. Deposited between ~511 and 490 Ma. Deposited in an evolved deltaic complex containing large stream mouth bars.||||Overlies Deception Formation. Is overlain by Goyder Formation.||14-FEB-18
15112|Petermann Sandstone|71279|5|Briefly described|p355 Fig.2|Late Cambrian|Middle Cambrian|Amadeus Basin.||Pertaoorrta Group.||||
15112|Petermann Sandstone|71898|4|Described|iii, p1, p3, p11, p14-p17|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. Interpreted to represent part of a prograding fluvial-deltaic system. This unit has a maximum thickness of 250m.|511 +/- 18 Ma (SHRIMP U-Pb)|Pertaoorrta Group||Conformably overlies and interfingers with the Deception Formation. Conformably (transitionally) overlain by the Goyder Formation.|Fine- to medium-grained micaceous sandstone.|
15112|Petermann Sandstone|72358|5|Briefly described|p117-119,121-124|Series 3|Series 3|Of Amadeus Basin. Nearshore succession, deposited in an evolved deltaic complex with large stream mouth bars.||||Overlain gradationally by Jay Creek Limestone. Correlable to Shannon Formation and the Jay Creek Limestone.||10-JAN-20
15112|Petermann Sandstone|72374|6|Mentioned|p15|||Of Amadeus Basin.||||Partially laterally equivalent to Illara Sandstone.||
15112|Petermann Sandstone|72516|6|Mentioned|p92-93|Cambrian|Cambrian|Amadeus Basin.||||Equivalent to the Steamboat Sandstone and the Arrinthrunga Formation.||03-JUN-21
15112|Petermann Sandstone|73085|4|Described|piii, p1, p3-9, p11|late Cambrian|middle Cambrian|Amadeus Basin. 227 m thick in drillhole LA05DD01. Capped by ~1 m of red, massive siltstone to fine-grained sandstone. Basal contact with Illara Sandstone is sharp and probably erosional.||Pertaoorrta Group [and equivalents?]||Underlain by Illara Sandstone. Underlain by and equivalent to Deception Sandstone. Overlain by Pacoota Sandstone and lower Goyder Formation. Equivalent to Cleland Sandstone.|Red to red-brown, medium- to coarse-grained sandstone, characterised by feldspar and mica with occasional clasts of metasedimentary and volcanic rocks, and hematite-clay matrix. Intervals of siltstone and buff to pink sandstone are common.|
15114|Peters Creek Volcanics|22457|4|Described|P29, Fig29, Fig30|||Shown as Upper and Lower Peters Creek Volcanics Fig29 p30.||||||22-NOV-06
15114|Peters Creek Volcanics|22479|5|Briefly described|fig4, pg10|Statherian|Statherian|||||||
15114|Peters Creek Volcanics|22644|6|Mentioned|5 fig 2|||Geol province Mount Isa Basin. Volcanics as 'V' in text||||||
15114|Peters Creek Volcanics|22665|5|Briefly described|P221, Table1|Statherian|Statherian|Ages of unit are 1726+/-2 Ma (lower) and 1724+/-2 Ma (upper)||||||
15114|Peters Creek Volcanics|22673|6|Mentioned|64,65,79|||Geol province Mount Isa Basin. Overlying unit Fickling Group||||||
15114|Peters Creek Volcanics|22680|6|Mentioned|85|||||||||
15114|Peters Creek Volcanics|23065|6|Mentioned|16|Proterozoic|Proterozoic|Geol province Lawn Hill Subprovince. Age ~1725 Ma. Underlying unit is Wire Creek Sandstone.||||||21-FEB-18
15114|Peters Creek Volcanics|23363|5|Briefly described|352 Tab.3|Statherian|Statherian|||||||
15114|Peters Creek Volcanics|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
15114|Peters Creek Volcanics|23395|4|Described|p384 Fig.2|||||||||
15114|Peters Creek Volcanics|23396|4|Described|p415|||||||||
15114|Peters Creek Volcanics|23397|5|Briefly described|p466|||||||||
15114|Peters Creek Volcanics|23398|4|Described|p437|Statherian|Statherian|U/Pb SHRIMP pooled age: 1729+/-4Ma.||||||09-SEP-14
15114|Peters Creek Volcanics|23406|5|Briefly described|p601 Fig. 3, p603, p604 Fig. 6|||Age: 1730-1710Ma. Stated to be of a basal "rift" package. Forms an igneous dome. Parts contained as clasts in the Fish River Formation. Thickest at Hedleys Creek.  See also p600 Fig. 2.||||||16-JUN-09
15114|Peters Creek Volcanics|23409|5|Briefly described|p535|||Of Lawn Hill Platform.||||||11-JUN-08
15114|Peters Creek Volcanics|24197|5|Briefly described|p95 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Of the Fiery Supersuite. Age: 1710Ma. Geological Province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1. See also the possibly misspelt Peter Creek Volcanics (although both names may be in use?)||||||07-FEB-11
15114|Peters Creek Volcanics|24308|5|Briefly described|p998, p987 Fig. 2|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
15114|Peters Creek Volcanics|24419|5|Briefly described|p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: Lawn Hill Subprovince (north).||||||07-NOV-08
15114|Peters Creek Volcanics|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Age: 1725+/-3 Ma. Geological Province: Lawn Hill Platform.||||||28-JAN-05
15114|Peters Creek Volcanics|26310|5|Briefly described|p7 Fig. 2, Table 1.|Neoproterozoic|Neoproterozoic|Acidic to basic, generally intermediate lavas, with interbedded sediments.||||||09-AUG-04
15114|Peters Creek Volcanics|29966|6|Mentioned|p398|||||||||
15114|Peters Creek Volcanics|30318|6|Mentioned|p328|||||||||
15114|Peters Creek Volcanics|31348|6|Mentioned|p344|||||||||
15114|Peters Creek Volcanics|31421|6|Mentioned|p509|||||||||
15114|Peters Creek Volcanics|32660|5|Briefly described|Table 4|||||||||
15114|Peters Creek Volcanics|33214|6|Mentioned|Fig.1|||||||||
15114|Peters Creek Volcanics|35114|6|Mentioned|p200|||||||||
15114|Peters Creek Volcanics|35640|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
15114|Peters Creek Volcanics|36012|3|Fully described|Table 3|||See also p11,16.||||||22-NOV-06
15114|Peters Creek Volcanics|36439|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
15114|Peters Creek Volcanics|36442|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
15114|Peters Creek Volcanics|37462|4|Described|Table4.VII|||||||||
15114|Peters Creek Volcanics|37565|6|Mentioned|Fig.5|||||||||
15114|Peters Creek Volcanics|37568|6|Mentioned|Fig.5|||||||||
15114|Peters Creek Volcanics|38237|6|Mentioned|p126|||||||||
15114|Peters Creek Volcanics|38557|5|Briefly described|p293|||||||||
15114|Peters Creek Volcanics|38584|4|Described|p15|||||||||
15114|Peters Creek Volcanics|38835|6|Mentioned|p164|||||||||
15114|Peters Creek Volcanics|39445|5|Briefly described|Table 2|||See also P36 & P39||||||
15114|Peters Creek Volcanics|39497|6|Mentioned|p8|||See also Fig.4||||||
15114|Peters Creek Volcanics|39685|6|Mentioned|Fig.1|||||||||
15114|Peters Creek Volcanics|39925|6|Mentioned|p334|||||||||
15114|Peters Creek Volcanics|39944|6|Mentioned|Fig.5|||||||||
15114|Peters Creek Volcanics|40105|6|Mentioned|p310|||||||||
15114|Peters Creek Volcanics|40491|6|Mentioned|p79|||||||||
15114|Peters Creek Volcanics|40811|6|Mentioned|p318|||||||||
15114|Peters Creek Volcanics|40840|6|Mentioned|Map legend|||||||||
15114|Peters Creek Volcanics|41125|6|Mentioned|Fig.21|||||||||
15114|Peters Creek Volcanics|41319|6|Mentioned|Fig.1|||||||||
15114|Peters Creek Volcanics|41406|6|Mentioned|Map legend|Mesoproterozoic||||||||
15114|Peters Creek Volcanics|41721|3|Fully described|p27|||Originally mapped by Roberts et al (1963). Lower part is replaced by Seigal Volcanics.||||||01-AUG-07
15114|Peters Creek Volcanics|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
15114|Peters Creek Volcanics|42639|5|Briefly described|p8|||Lawn Hill Platform||||||
15114|Peters Creek Volcanics|42812|6|Mentioned|p65|||||||||
15114|Peters Creek Volcanics|43010|5|Briefly described|Fig.6||Mesoproterozoic|of "Mid Proterozoic" age.||||||
15114|Peters Creek Volcanics|43788|6|Mentioned|p14|||||||||
15114|Peters Creek Volcanics|44271|2|Defined|p39,44,57|||||||||
15114|Peters Creek Volcanics|44272|14|Not recorded|Map Legend||Neoproterozoic|||||||
15114|Peters Creek Volcanics|44274|14|Not recorded|p8,Tb.2|||||||||
15114|Peters Creek Volcanics|44275|14|Not recorded|Map Legend|||||||||
15114|Peters Creek Volcanics|44280|2|Defined|p5,Tb.1,map||Neoproterozoic|||||||
15114|Peters Creek Volcanics|44287|14|Not recorded|p.8, opp.7|||(E53-3).||||||
15114|Peters Creek Volcanics|44288|14|Not recorded|map legend||Paleoproterozoic|Amygdoloidal basalt, minor trachyte. Lower Proterozoic.||||||07-NOV-08
15114|Peters Creek Volcanics|44305|14|Not recorded|p.6,11,19,20||Neoproterozoic|(E53-8). opp.p.6,18. Includes Carolina Sandstone Member. U.Prot.||||||
15114|Peters Creek Volcanics|44306|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
15114|Peters Creek Volcanics|44473|14|Not recorded|p.8, opp. p.7|||(E53-7). Formation of Tawallah Group.||||||
15114|Peters Creek Volcanics|44474|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
15114|Peters Creek Volcanics|44530|14|Not recorded|p,4,8, opp.8|||(D53-15).||||||
15114|Peters Creek Volcanics|44531|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
15114|Peters Creek Volcanics|44806|14|Not recorded|p297|||Petrographic description.||||||
15114|Peters Creek Volcanics|44989|2|Defined|p.115-7|||Tb.II. On many pages. Pl.8. Overlies Cliffdale Volcanics, Westmoreland Conglomerate; underlies Wollogorang Formation (E54-5).||||||12-AUG-08
15114|Peters Creek Volcanics|45162|6|Mentioned|p14|||Mention P27||||||
15114|Peters Creek Volcanics|45166|5|Briefly described|p26|||See also P50||||||
15114|Peters Creek Volcanics|45287|14|Not recorded|p.223,226|||||||||
15114|Peters Creek Volcanics|46804|6|Mentioned|p154|||||||||
15114|Peters Creek Volcanics|46919|6|Mentioned|p221|||||||||
15114|Peters Creek Volcanics|48867|14|Not recorded|p.7|||Equivalent to part of Kombolgie Formation.||||||
15114|Peters Creek Volcanics|49001|6|Mentioned|p4|||||||||
15114|Peters Creek Volcanics|49002|6|Mentioned|p1|||||||||
15114|Peters Creek Volcanics|50224|6|Mentioned|p380 Fig. 6|||||||||07-FEB-11
15114|Peters Creek Volcanics|50536|5|Briefly described|p1.4, 7.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Fiery Supersuite. Age: 1724-1726 +/- 2Ma (Shrimp).||||||07-NOV-08
15114|Peters Creek Volcanics|50591|5|Briefly described|p5.1|Paleoproterozoic|Paleoproterozoic|Age: ~1725Ma.||||||07-NOV-08
15114|Peters Creek Volcanics|60558|6|Mentioned|p5 Fig. 4|||||||||
15114|Peters Creek Volcanics|61936|5|Briefly described|p194 Fig. 6|Paleoproterozoic|Paleoproterozoic|Age: 1730-1725Ma. Geological Province: Lawn Hill Platform, Western Fold Belt, Mount Isa Inlier.||||||07-NOV-08
15114|Peters Creek Volcanics|63109|5|Briefly described|p1109, p1108 Fig. 3|||Overlain by Surprise Creek Formation, underlain by Bigie Formation. Felsic rocks. Geological Province: Murphy Inlier.||||||08-MAR-13
15114|Peters Creek Volcanics|63110|6|Mentioned|p1141, p1141 Fig. 17|Statherian|Statherian|Geological Province: Calvert Superbasin.||||||11-JUN-08
15114|Peters Creek Volcanics|63113|6|Mentioned|p1214 Fig.2, 1225 Fig.13.||||c.1729-1724 Ma.|||Overlies ?unconformably Buddawadda Basalt.||
15114|Peters Creek Volcanics|63115|6|Mentioned|1279 Fig.4, p1281, p1290. |||Calvert superbasin.||||||
15114|Peters Creek Volcanics|63116|6|Mentioned|p1297 Fig.2, |||Calvert superbasin.||||||
15114|Peters Creek Volcanics|63866|5|Briefly described|p56|Statherian|Statherian|Murphy Inlier, Calvert Superbasin. Numeric dates derived from Page and Sweet, 1998 and Page et al., 2000.|1729 +/- 4 Ma and 1724 +/- 2 Ma|||||
15114|Peters Creek Volcanics|64250|6|Mentioned|p11 fig 3, p24, p19|||Of far NW of Mt Isa Inlier. May be intrusive.|1729 +/- 4 Ma - 1725 +/- 2 Ma||||Bimodal volcanics: basalt, rhyolite.|
15114|Peters Creek Volcanics|64575|6|Mentioned|p656|||Geological Province: Murphy Inlier.||||||
15114|Peters Creek Volcanics|64726|6|Mentioned|p86 Table 1.|||Sampled for paleomagnetic reconstruction of Australian and Laurentian Apparent Polar Wander Path.|1724 +/- 2 Ma.|||||
15114|Peters Creek Volcanics|64738|6|Mentioned|pp260-261.|Statherian|Statherian|Dated and used in identifying a right-angle bend in the earliest defined segment of northern Australia's Apparent Polar Wander Path.|c.1730 Ma.|||||
15114|Peters Creek Volcanics|64748|6|Mentioned|p276 Fig. 9|Paleoproterozoic|Paleoproterozoic|Basalt. Palaeomag results shown on polar wander path||||||
15114|Peters Creek Volcanics|64817|6|Mentioned|p351 Fig.2|||||||||
15114|Peters Creek Volcanics|65228|5|Briefly described|Figs.04, 07.|Statherian|Statherian|Southern McArthur Basin. Part of the Big Supersequence.|1729 +/- 4 Ma and 1724 +/- 2 Ma.||Includes Buddawarra Basalt.|Overlies Wire Creek Sandstone.||
15114|Peters Creek Volcanics|65337|5|Briefly described|p5. |||Leichhardt Superbasin; Lawn Hill Platform. Correlative of Carrara Range Group.|1729 +/- 4 Ma.||||Includes intrusive rhyodacites.|
15114|Peters Creek Volcanics|65340|6|Mentioned|p35, p93.|||Murphy Inlier. Part-correlated with Settlement Creek Dolerite and Gold Creek Volcanics.||||||
15114|Peters Creek Volcanics|65396|5|Briefly described|p82, p175, p187, p192-193, p195, p197|Statherian|Statherian|See also p241. Calvert Superbasin, far NW of Mount Isa Inlier. Cover Sequence 2. Formations with detrital zircons from this unit are listed.|1729 +/- 4 Ma, 1725 +/- 2 Ma||||Basalt and rhyolite.|
15114|Peters Creek Volcanics|66529|6|Mentioned|p3|||Calvert Superbasin.|~1730-1720 Ma|||||
15114|Peters Creek Volcanics|67323|5|Briefly described|GIS attrib tbl,  p9-10, p33, p107|Statherian|Statherian|See also Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Northern Camooweal-Murphy Domain, Mount Isa Inlier, Calvert Superbasin. Ages: 1729+/-4 Ma, 1724+/-4 Ma (1998, 2000), significantly older than Fiery Creek Volcanics.|1724+/-4 Ma||Includes Buddawadda Basalt Member, and 12 unnamed subdivisions.||Basalt, rhyolite, sandstone and conglomerate.|
15114|Peters Creek Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|McArthur Basin, Mount Isa Province.||||Conformably overlies Tawallah Group.||
15114|Peters Creek Volcanics|68575|6|Mentioned|p11|||||||Is overlain by Fickling Group.||
15114|Peters Creek Volcanics|69423|6|Mentioned|p8:4 Fig.8.7|Paleoproterozoic|Paleoproterozoic|Lawn Hill Platform.||||||12-JUL-16
15114|Peters Creek Volcanics|69430|6|Mentioned|p15:1|||||||||12-JUL-16
15114|Peters Creek Volcanics|69433|4|Described|p18:1-5|Statherian|Statherian|Northern succession, Lawn Hill Platform. Exposed in SW corner of CALVERT HILLS map area, but more completely in Qld. Forming a 10x50km belt. Geochemically distinct from Buddycurrawa Volcanics. The basalts in the lower part of the unit are probably equivalent to Seigal Volcanics. SHRIMP U-Pb zircon ages (Page and Sweet, 1998).|1726 +/- 2 Ma and 1724 +/- 2 Ma.|||Overlies probably conformably Wire Creek Sandstone. Is overlain unconformably by Fish River Formation (Fickling Group). Equivalent to upper Tawallah Group (McArthur Basin) and Carrara Range Group.|Vesicular and massive basaltic lavas with fine to medium sandstone interbeds; rhyolite, rhyodacite, tuff, shale, siltstone, dolostone and conglomerate.|12-JUL-16
15114|Peters Creek Volcanics|69591|4|Described|p29, p34, p38, p56, p106|Paleoproterozoic|Paleoproterozoic|Camooweal-Murphy Domain, Calvert Superbasin. Part of the Big Supersequence. Mostly high-level intrusives, with chemical and lithological similarities to Packsaddle Microgranite; also, sedimentary units (shallow-marine) have similarities to the Wollogorang Formation.|1726 +/- 2 Ma (Page and Sweet, 1998).||Buddawadda Basalt Member.|Is overlain by the Bigie Formation.|Basalt, rhyolite, sandstone, conglomerate.|
15114|Peters Creek Volcanics|69673|5|Briefly described|p51|Statherian|Statherian|Considered to be equivalent to the Tawallah Group of the McArthur Basin. Total thickness of 2km.|1726 +/- 2 Ma|||Unconformably overlain by Fickling Group|Vesicular and massive basaltic lavas with sandstone interbeds.|
15114|Peters Creek Volcanics|70849|5|Briefly described|Map legend.|Statherian|Statherian|Lawn Hill Platform.||Tawallah Group equivalent.||Overlies Wire Creek Sandstone. Is overlain unconformably by Fish River Formation (Fickling Group).|Alternating sequence of basalt, rhyolite and rhyodacite; some intermediate volcanics, possibly trachyte and andesite; minor tuff, shale, siltstone, sandstone, dolomite and conglomerate.|21-FEB-18
15114|Peters Creek Volcanics|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1726+/-2 Ma (crystallisation: U-Pb zircon SHRIMP)||||Ignimbrite, rhyolite.|
15114|Peters Creek Volcanics|71606|5|Briefly described|p137|Statherian|Statherian|South Nicholson Basin.||||Overlain unconformably by Fickling Group. Underlain by Wire Creek Sandstone.||
15114|Peters Creek Volcanics|71632|6|Mentioned|Map legend.|Paleoproterozoic|Paleoproterozoic|Shown elsewhere in map key as Lower Peters Creek Volcanics and Upper Peters Creek Volcanics. Unit evidently expanded in this map to include Wire Creek Sandstone, but this change appears to be a one off, not used again].||||||
15114|Peters Creek Volcanics|71799|5|Briefly described|p150 fig 2, p153 tbl 1|Statherian|Statherian|McArthur Basin. 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.|1730-1720 Ma||||Basalt, dolerite, gabbro or amphibolite.|
15114|Peters Creek Volcanics|72526|5|Briefly described|p6 Fig.1.2, p8 Fig.1.3.|Statherian|Statherian|U-Pb SHRIMP igneous crystallisation ages given. Shown as being located in the west of the South Nicholson Basin.|1725+/-2 Ma, 1729+/-4 Ma|||Overlies Wire Creek Sandstone and shown as partially underlying Benmara Group and Fickling Group.||
15114|Peters Creek Volcanics|72527|4|Described|p2, p7 Fig.1.4, p9, p87, p89, p176-177.|Paleoproterozoic|Paleoproterozoic|Insufficient zircon yield to enable meaningful date results. One of three units considered to represent c. 1725 Ma felsic volcanism in the region, including Top Rocky Rhyolite and Hobblechain Volcanics. See also p192, p194 and p196.|c. 1725 Ma (Page et al., 2000)|Tawallah Group||Unconformably overlies Wire Creek Sandstone and is laterally equivalent to Top Rocky Rhyolite.||
15114|Peters Creek Volcanics|72912|5|Briefly described|p5 Fig.3, p13, p17.|Statherian|Statherian|Calvert Superbasin. Located in the west part of the South Nicholson Basin. Three U-Pb zircon igneous crystallisation ages (Ma) shown.|1729 +/- 4 Ma to 1725 +/- 2 Ma||||Bimodal volcanics.|
15114|Peters Creek Volcanics|73042|6|Mentioned|p4|Statherian|Statherian|South Nicholson Basin region, Calvert Superbasin. Geochronology is a U-Pb zircon igneous crystallisation age.|1729+/-4 Ma, 1726+/-2 Ma, 1725+/-2 Ma|||||
15114|Peters Creek Volcanics|73083|6|Mentioned|p77|||||||||
15114|Peters 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.||||||
15114|Peters Creek Volcanics|73413|6|Mentioned|p3|||Mount Isa Inlier, Western Fold Belt, Lawn Hill Platform.||||||
15139|Phillips Creek Sandstone|23216|5|Briefly described|p12-4||Paleoproterozoic|||||||07-NOV-08
15139|Phillips Creek Sandstone|23384|6|Mentioned|Fig 27|||Of Needham and Stuart-Smith (1985).||||||
15139|Phillips Creek Sandstone|23867|5|Briefly described|Fig. 3|||Of Edith River Group.  Geological Province: McArthur Basin.||||||
15139|Phillips Creek Sandstone|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
15139|Phillips Creek Sandstone|40248|4|Described|p224|||||||||
15139|Phillips Creek Sandstone|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
15139|Phillips Creek Sandstone|41294|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
15139|Phillips Creek Sandstone|41295|4|Described|p12|||||||||
15139|Phillips Creek Sandstone|41586|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
15139|Phillips Creek Sandstone|43140|4|Described|p3||Paleoproterozoic|Of Edith River Group.||||||07-NOV-08
15139|Phillips Creek Sandstone|43187|5|Briefly described|p2|||||||||
15139|Phillips Creek Sandstone|43832|4|Described|24-25,Table6 p22.||Paleoproterozoic|||||||07-NOV-08
15139|Phillips Creek Sandstone|46658|6|Mentioned|p557|||||||||
15139|Phillips Creek Sandstone|47049|5|Briefly described|Table|||Elevation to formation from member status.||||||
15139|Phillips Creek Sandstone|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1825-1829Ma. Of Edith River Group. Poorly sorted lithic and tuffaceous sandstone, purple medium to coarse grained arkose and greywacke, conglomerate, sedimentary breccia, minor siltstone and phyllite.||||||07-JAN-09
15139|Phillips Creek Sandstone|64730|5|Briefly described|p125 Fig. 3|Paleoproterozoic|Paleoproterozoic|Age from overlying Plum Tree Creek Volcanics (Page 1996).|Min. deposition age of 1825 +/- 4 Ma.|Of Edith River Group.||Underlies Plum Tree Creek Volcanics.||02-MAY-12
15139|Phillips Creek Sandstone|67564|6|Mentioned|p29.|||In Needham and Stuart-Smith (1985); formerly Phillip Creek Member (Roberts and Plumb 1965). Is correlated with Kurrundie Sandstone.||Unit in Edith River Group.||||
15139|Phillips Creek Sandstone|67779|5|Briefly described|p6 Fig.5.|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen.||Unit in Edith River Group.||||
15139|Phillips Creek Sandstone|69420|5|Briefly described|p5:4, 15|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen.||Edith River Group.||Overlies Kurrundie Sandstone and (with angular unconformity) Tollis Formation. Is overlain unconformably by Plum Tree Creek Volcanics.|Interbedded, labile and tuffaceous, poorly sorted sandstone, arkose, conglomerate and minor siltstone.|12-JUL-16
15163|Pickwick Metabasalt Member|23031|6|Mentioned|24|Paleoproterozoic|Paleoproterozoic|Geological province: Mount Isa Fold Belt. Of the Eastern Creek Volcanics.||||||07-NOV-08
15163|Pickwick Metabasalt Member|23395|5|Briefly described|p386 Fig.3|||Of the Eastern Creek Volcanics.||||||23-NOV-06
15163|Pickwick Metabasalt Member|23518|4|Described|p11|Proterozoic|Proterozoic|Of Eastern Creek Volcanics.  Geological Province: Western Fold Belt.||||||
15163|Pickwick Metabasalt Member|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Eastern Creek Volcanics.  Overlies the Lena Quartzite Member.||||||25-AUG-04
15163|Pickwick Metabasalt Member|30534|2|Defined|p303|Carpentarian|Carpentarian|||||||
15163|Pickwick Metabasalt Member|33900|5|Briefly described|p11|||||||||
15163|Pickwick Metabasalt Member|35295|6|Mentioned|Fig.2|||||||||
15163|Pickwick Metabasalt Member|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
15163|Pickwick Metabasalt Member|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
15163|Pickwick Metabasalt Member|37568|5|Briefly described|p81|||||||||
15163|Pickwick Metabasalt Member|38232|6|Mentioned|p84|||||||||
15163|Pickwick Metabasalt Member|38233|5|Briefly described|Table 1|||||||||
15163|Pickwick Metabasalt Member|38234|6|Mentioned|p103|||||||||
15163|Pickwick Metabasalt Member|38236|6|Mentioned|p120|||||||||
15163|Pickwick Metabasalt Member|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
15163|Pickwick Metabasalt Member|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Eastern Creek Volcanics. Grey-green metabasalt, red-brown trachybasalt, orthoquartzite, feldspathic quartzite.||||||23-NOV-06
15163|Pickwick Metabasalt Member|39622|6|Mentioned|p30|||See also Appendix||||||
15163|Pickwick Metabasalt Member|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
15163|Pickwick Metabasalt Member|39924|6|Mentioned|p348|||||||||
15163|Pickwick Metabasalt Member|39934|6|Mentioned|p317|||||||||
15163|Pickwick Metabasalt Member|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
15163|Pickwick Metabasalt Member|40221|3|Fully described|p7|||||||||
15163|Pickwick Metabasalt Member|40598|6|Mentioned|Fig.2|||||||||
15163|Pickwick Metabasalt Member|41298|6|Mentioned|Map legend|Carpentarian||||||||
15163|Pickwick Metabasalt Member|45136|4|Described|p47|||||||||
15163|Pickwick Metabasalt Member|45166|5|Briefly described|p15|||||||||
15163|Pickwick Metabasalt Member|46801|6|Mentioned|p123|||||||||
15163|Pickwick Metabasalt Member|47083|4|Described|p5 + p6|||Youngest member of Eastern Creek Volcanics. Of Eastern Creek Volcanics of the Haslingden Group. Conformably overlain by Alsace Quartzite. Maximum thickness: 250 m.||||||23-NOV-06
15163|Pickwick Metabasalt Member|49041|6|Mentioned|Table 4|||||||||
15163|Pickwick Metabasalt Member|50100|5|Briefly described|p17|Proterozoic|Proterozoic|Of the Eastern Creek Volcanics.||||||
15163|Pickwick Metabasalt Member|62873|5|Briefly described|p692, p704|Paleoproterozoic|Paleoproterozoic|Of the Eastern Creek Volcanics.  Overlies the Lena Quartzite Member.||||||07-NOV-08
15163|Pickwick Metabasalt Member|63023|5|Briefly described|p1025 Fig. 2|||Of Eastern Creek Volcanics (Haslingden Group). Geological Province: Leichardt Superbasin.||||||
15163|Pickwick Metabasalt Member|63111|5|Briefly described|p1164 Tb. 1|Statherian|Statherian|Of Eastern Creek Volcanics. Overlain by Lena Quartzite Member. Geological Province: Leichhardt Superbasin. Tholeiitic mafic intrusions comprising metabasalts, sediments and tuffs.||||||07-FEB-11
15163|Pickwick Metabasalt Member|64367|5|Briefly described|p555  Fig. 1b|Paleoproterozoic|Paleoproterozoic|See also Pickwick Member. The abbreviated version of the name is used throughout the text - all relevant details are therefore attached to that version of the name. Also referred to as the Pickwick basalts. Of Eastern Creek Volcanics.||||||07-FEB-11
15163|Pickwick Metabasalt Member|64832|5|Briefly described|p1154, p1155 Figs. 2, 3|Paleoproterozoic|Paleoproterozoic|Of the Eastern Creek Volcanics. Geological Province: Mt Isa Inlier. Has lower titanium content than Cromwell Metabasalt Member, but extremely high Cu concentrations in its upper section - detailed geochemistry included. Referred to throughout paper.||||||07-FEB-11
15163|Pickwick Metabasalt Member|67323|5|Briefly described|GIS attrib tbl, p13|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot. Leichhardt River Domain, Mount Isa Inlier. Leichhardt Superbasin.||Eastern Creek Formation.||Overlies Lena Quartzite Member.|Grey-green metabasalt, red-brown trachybasalt, orthoquartzite, feldspathic quartzite, amygdaloidal metabasalt, flow-top breccia, tuff|
15163|Pickwick Metabasalt Member|67499|6|Mentioned|p938|||||Of the Eastern Creek Volcanics.||||08-MAY-12
15163|Pickwick Metabasalt Member|69591|6|Mentioned|p33|||Mount Oxide and Leichhardt River Domains, Leichhardt Superbasin.||||||
15163|Pickwick Metabasalt Member|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Eastern Creek Volcanics.||Overlies Lena Quartzite Member. Is overlain by Alsace Quartzite (Myally Subgroup).|Grey-green metabasalt, red-brown trachybasalt, orthoquartzite, feldspathic quartzite, amygdaloidal metabasalt, flow-top breccia and tuff. (Separately mapped) quartzite, feldspathic sandstone and epidosite.|
15163|Pickwick Metabasalt Member|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Eastern Creek Volcanics.||Overlies Lena Quartzite Member. Is overlain by Alsace Quartzite (Myally Subgroup).|Grey-green metabasalt, red-brown trachybasalt, orthoquartzite, feldspathic quartzite, amygdaloidal metabasalt, flow-top breccia and tuff. (Separately mapped) quartzite, feldspathic sandstone and epidosite.|
15163|Pickwick Metabasalt Member|71799|4|Described|p150 fig 2, p152, p156, p157-p158|Statherian|Statherian|Lawn Hill.|ca. 1775 Ma|Eastern Creek Volcanics||Overlies the Lena Quartzite Member. Overlain by the Alsace Quartzite.|Peperite, hyaloclastite and basalts.|03-OCT-18
15163|Pickwick Metabasalt Member|71980|5|Briefly described|map legend sheet 1|Proterozoic|Proterozoic|||Of Eastern Creek Volcanics|||metabasalt; fluviolacustrine sandstone between basalt flows.|
15163|Pickwick Metabasalt Member|73553|5|Briefly described|p231 Fig.7.1.7|||Western Succession.||Eastern Creek Volcanics||||
15228|Pincombe Formation|22547|5|Briefly described|p24|Cryogenian|Stenian|Of the Carr Boyd Group.  Age: 891 +/- 149 Ma.||||||14-NOV-06
15228|Pincombe Formation|22754|5|Briefly described|p11 Tb. 3|Mesoproterozoic|Mesoproterozoic|Of the Carr Boyd Group.||||||23-NOV-06
15228|Pincombe Formation|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
15228|Pincombe Formation|32660|5|Briefly described|Table 6|||||||||
15228|Pincombe Formation|32664|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
15228|Pincombe Formation|32701|6|Mentioned|p7|||||||||
15228|Pincombe Formation|32728|5|Briefly described|Table 6|||See also p47.||||||23-NOV-06
15228|Pincombe Formation|36551|6|Mentioned|Table 12|||||||||
15228|Pincombe Formation|37462|6|Mentioned|Fig.4.13|||||||||
15228|Pincombe Formation|40792|6|Mentioned|Fig.5|||||||||
15228|Pincombe Formation|41158|6|Mentioned|p19|||||||||
15228|Pincombe Formation|42175|5|Briefly described|Fig.2 P200|||||||||
15228|Pincombe Formation|44155|5|Briefly described|p250 Tb.3-10|||Up to 2500m thick.||Carr Boyd Group||Gradational contact with underlying Stonewall Sandstone.|Red and green siliceous siltstone, and fine sandstone, blocky quartz sandstone; minor micaceous shale.|
15228|Pincombe Formation|45047|6|Mentioned|Plate 17|||||||||
15228|Pincombe Formation|45112|6|Mentioned|Table 16|||||||||
15228|Pincombe Formation|48938|6|Mentioned|p76|||Equiv. Legune Fm.||||||
15228|Pincombe Formation|65417|5|Briefly described|pp156-159, pp162-163.|Mesoproterozoic|Mesoproterozoic|Halls Creek Orogen. Age from Bofinger (1967) recalculated by Plumb et al. (1981). Correlated with Legune Formation of the Fitzmaurice Group (NT). Braided-delta progradation and retreat.|891 +/- 149 Ma (Rb-Sr whole rock).|Topmost unit in Carr Boyd Group.||Conformably overlies Stonewall Sandstone.||
15228|Pincombe Formation|69435|5|Briefly described|p20:3|||Carr Boyd Basin. A previous correlation  with the Legune Formation (Fitzmaurice Group, NT) is called into question.||Carr Boyd Group.||Overlies Stonewall Sandstone.||12-JUL-16
15228|Pincombe Formation|69673|6|Mentioned|p60 fig 48|||||Carr Boyd Group||Overlies Stonewall Sandstone||
15228|Pincombe Formation|71267|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Carr Boyd Group.|||Siliceous siltstone and fine-grained sandstone, micaceous shale, quartz sandstone|
15264|Pinkerton Sandstone|14019|5|Briefly described|p4 Fig. 3|||Of the Auvergne Group. Geological Province: Victoria Basin.||||||12-SEP-11
15264|Pinkerton Sandstone|23937|6|Mentioned|p76 App. 1|||Of the Auvergne Group.||||||02-NOV-04
15264|Pinkerton Sandstone|24122|3|Fully described|p10, p5 Tb.1|Proterozoic|Proterozoic|Of Auvergne Group.  Conformably overlies Saddle Creek Formation.  Approximately 30m thick.  Geological Province: Victoria Basin.||||||
15264|Pinkerton Sandstone|24297|5|Briefly described|p4 Fig.3|||Of Auvergne Group. Geological Province: Victoria Basin.||||||12-SEP-11
15264|Pinkerton Sandstone|24300|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of the Auvergne Group. Geological Province: Victoria Basin.||||||12-SEP-11
15264|Pinkerton Sandstone|24441|5|Briefly described|p1 Fig. 1|Mesoproterozoic|Mesoproterozoic|Of the Auvergne Group. Overlies Saddle Creek Formation; overlain by Lloyds Creek Formation. Geological Province: Victoria Basin.||||||12-SEP-11
15264|Pinkerton Sandstone|24442|5|Briefly described|p50 Fig. 1|||Of the Auvergne Group. Geological Province: Victoria Basin.||||||12-SEP-11
15264|Pinkerton Sandstone|28255|4|Described|p67, Tb. 11 (opp. p8)|Adelaidean|Adelaidean|Of the Auvergne Group. Massive quartz sandstone. Conformably overlain by Lloyd Creek Formation; conformably overlies Saddle Creek Formation. Max. thickness100m. See also p68 Tb. 6.||||||
15264|Pinkerton Sandstone|32170|6|Mentioned|Map legend|Adelaidean|Carpentarian|Adelaidean or Carpentarian||||||
15264|Pinkerton Sandstone|32307|4|Described|Table 2|||Proterozoic||||||
15264|Pinkerton Sandstone|32310|6|Mentioned|Map legend|Adelaidean|Carpentarian|Adelaidean/Carpentarian||||||
15264|Pinkerton Sandstone|32660|5|Briefly described|Table 6|||||||||
15264|Pinkerton Sandstone|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Auvergne Group. Massive quartz sandstone, siltstone, minor mudstone.||||||12-SEP-11
15264|Pinkerton Sandstone|32700|4|Described|Table 1|||Lithology p14. Refers Randal (1962).||||||23-NOV-06
15264|Pinkerton Sandstone|32701|4|Described|Table 1|||Adelaidean. Auvergne Group. See p9.||||||23-NOV-06
15264|Pinkerton Sandstone|32728|6|Mentioned|Fig.14|||||||||
15264|Pinkerton Sandstone|32775|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Auvergne Group. Quartz sandstone, minor siltstone.||||||12-SEP-11
15264|Pinkerton Sandstone|33373|3|Fully described|p10|||Table 2.||||||
15264|Pinkerton Sandstone|33375|6|Mentioned|p11 Tb. 1, p13|Adelaidean|Adelaidean|Of the Auvergne Group. Fine and medium blocky quartz sandstone. Conformable on Saddle Creek Formation. Max. thickness: ~50m.||||||28-APR-05
15264|Pinkerton Sandstone|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
15264|Pinkerton Sandstone|33378|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Auvergne Group. Fine and medium quartz sandstone.||||||27-APR-05
15264|Pinkerton Sandstone|41660|5|Briefly described|Map legend|Mesoproterozoic||Of Auvergne Group. Quartz arenite, flaggy to well bedded, cross-bedded. Min thickness: up to at least 40m.||||||07-OCT-05
15264|Pinkerton Sandstone|41661|5|Briefly described|Table 1|||||||||
15264|Pinkerton Sandstone|45112|6|Mentioned|Table 6|||||||||
15264|Pinkerton Sandstone|48938|2|Defined|p43|Proterozoic|Proterozoic|Measured section p96. ?Adelaidean.||||||23-NOV-06
15264|Pinkerton Sandstone|48942|3|Fully described|p68|||||||||
15264|Pinkerton Sandstone|48943|4|Described|p76|||||||||
15264|Pinkerton Sandstone|60006|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Victoria Basin. Of Auvergne Group. Overlies Saddle Creek Formation. Overlain by Lloyd Creek Formation. Silica cemented quartz sandstone, minor siltstone and mudstone.||||||21-JUL-04
15264|Pinkerton Sandstone|60682|4|Described|p9 Table 2|Cryogenian|Cryogenian|Of Auvergne Group. Conformably overlies Saddle Creek Formation. Conformably overlain by Lloyd Creek Formation. Max. thickness: 375m. Quartz sandstone, minor siltstone and mudstone. Geological Province: Victoria Basin.||||||23-NOV-06
15264|Pinkerton Sandstone|60685|5|Briefly described|p4 Fig. 3|Mesoproterozoic|Mesoproterozoic|Of the Auvergne Group. Geological Province: Victoria Basin.||||||
15264|Pinkerton Sandstone|65331|5|Briefly described|Map legend|Neoproterozoic |Neoproterozoic|Of Auvergne Group, Victoria Basin. Silica cemented quartz sandstone, minor siltstone and mudstone||||||
15264|Pinkerton Sandstone|65342|6|Mentioned|p11 Fig.13. |||Victoria Basin.||Unit in Auvergne Group.||Overlies Saddle Creek Formation. Is overlain by Lloyd Creek Formation.||
15264|Pinkerton Sandstone|67151|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Victoria Basin.||Unit in Auvergne Group.||Overlies Saddle Creek Formation.|Fine and medium quartz sandstone.|
15264|Pinkerton Sandstone|67167|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|||Unit in Auvergne Group.|||Silica cemented quartz sandstone, minor siltstone and mudstone.|
15264|Pinkerton Sandstone|68733|5|Briefly described|p177 Fig.2, p179, p185, p189 Fig.8, p192|Cryogenian|Cryogenian|Victoria Basin. Sm-Nd isotope data tabulated.||Of the Auvergne Group.||||05-DEC-17
15264|Pinkerton Sandstone|69437|5|Briefly described|p22:4-5|Cryogenian|Cryogenian|Victoria/Wolfe Basins, Centralian A Superbasin. Supersequence 1.||||Overlies Saddle Creek Formation. Is overlain by Lloyd Creek Formation.||12-JUL-16
15264|Pinkerton Sandstone|69441|4|Described|p26:2-6|Neoproterozoic|Neoproterozoic|Forms a resistant capping on the main escarpments and plateaux of the Pinkerton and Yambarra Ranges. Typically 100-200m thick, up to 375m locally. Marine transgression, rare periods of brine-logging. Offset by Pinkerton Range Fault.||Auvergne Group.||Conformably overlies Saddle Creek Formation. Is overlain conformably by Lloyd Creek Formation.|Basal medium-grained silica-cemented quartz sandstone up to 30m thick; overlain by mudstone, siltstone and sandstones. Dolomitic phases present.|12-JUL-16
15264|Pinkerton Sandstone|69673|5|Briefly described|p188|||375m thick.||Auvergne Group|||Quartz sandstone, mudstone, siltstone and fine grained sandstone.|
15264|Pinkerton Sandstone|70206|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Victoria Basin.||Auvergne Group|||Silica cemented quartz sandstone, minor siltstone and mudstone.|
15264|Pinkerton Sandstone|70655|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Victoria Basin.||Auvergne Group||Overlies Saddle Creek Formation. Is overlain by Moonlight Valley Tillite.|Fine and medium quartz sandstone.|21-JAN-22
15264|Pinkerton Sandstone|70850|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Victoria Basin.||Auvergne Group.||Conformably overlies Saddle Creek Formation.|Silica-cemented quartz sandstone, minor siltstone and mudstone.|
15264|Pinkerton Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
15264|Pinkerton Sandstone|71302|4|Described|p1,6-7,58-64,72-74|Neoproterozoic|Neoproterozoic|Of Victoria Basin. Forms a resistant cap on main escarpments and dissected plateauz on AUVERGNE 1:250 000 map sheet (Sweet et al., 1974a, b; Dunster et al., 2000), reaching up to 375m thick. Deposited in high-energy nearshore conditions with more terrigenous clastic input than underlying Saddle Creek Formation or overlying Lloyd Creek Formation (Dunster et al., 2000; Dunster and Ahmed, 2013b). Sample GA 1957134 (quartz sandstone) yielded an interpreted (weighted mean 238U/206Pb) maximum depositional age of 973+\-14 Ma. Sample description, locality, zircon description, SHRIMP analyses and results are discussed.||Unit of Auvergne Group.||Overlain by Lloyd Creek Formation. Underlain conformably by Saddle Creek Formation.|Mudstone, siltstone, fine-grained, ferruginous, feldpsathic quartz sandstone and dolomitic phases.|09-DEC-19
15264|Pinkerton Sandstone|73083|6|Mentioned|p8|||||||||
15279|Pinyinna beds|22506|6|Mentioned|p130 Fig.4|Cryogenian|Cryogenian|||||||
15279|Pinyinna beds|22647|6|Mentioned|Fig 1 on p 113|||||||||
15279|Pinyinna beds|22804|5|Briefly described|p441|Neoproterozoic|Neoproterozoic|||||||
15279|Pinyinna beds|22826|4|Described|p568|Neoproterozoic|Neoproterozoic|The Pinyinna beds are time equivalents of the Bitter Springs Formation in the southwest of the Basin.||||||
15279|Pinyinna beds|24301|4|Described|p14|Neoproterozoic|Neoproterozoic|Also referred to as Pinyinna Beds on p7 Tb.2 and p15. Lithology: siltstone and dolostone.  Geological Province: Amadeus Basin.||||||16-JUN-09
15279|Pinyinna beds|24302|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Grey to purple muscovite-quartz phyllite, thinly laminated; crenulated in places. Geological Province: Amadeus Basin.||||||16-JUN-09
15279|Pinyinna beds|24496|5|Briefly described|p21 Tb.2|Neoproterozoic|Neoproterozoic|Geological Province: Amadeus Basin.||||||
15279|Pinyinna beds|24497|5|Briefly described|Map legend|Early Paleocene|Neoproterozoic|Geological Province: Amadeus Basin.||||||
15279|Pinyinna beds|36701|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
15279|Pinyinna beds|41884|6|Mentioned|p70|||||||||
15279|Pinyinna beds|42940|6|Mentioned|p 1|||||||||
15279|Pinyinna beds|45155|6|Mentioned|p47|||||||||
15279|Pinyinna beds|45170|6|Mentioned|p5|||||||||
15279|Pinyinna beds|50286|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Amadeus Basin. Overlies Dean Quartzite.  Underlies Winnall beds, Inindia beds.||||||22-DEC-09
15279|Pinyinna beds|50321|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Amadeus Basin. Overlies Dean Quartzite. Underlies Inindia beds, Winnall beds.||||||23-NOV-06
15279|Pinyinna beds|60572|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Grey, quartz-muscovite phyllite.   Geological Province: Amadeus Basin.||||||23-DEC-09
15279|Pinyinna beds|60660|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Deformed basal sediments of Amadeus Basin.||||||22-FEB-05
15279|Pinyinna beds|60678|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Grey quartz-muscovite phyllite, crystalline dolostone, fine-grained sandstone,red, green and pale grey fissile siltstone, dolomitic siltstone.  Geological Province: Amadeus Basin.||||||11-JAN-05
15279|Pinyinna beds|60679|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Quartz-muscovite phyllite. Geological Province: Amadeus Basin.||||||
15279|Pinyinna beds|60683|4|Described|p25, p9 Tb. 1|Neoproterozoic|Neoproterozoic|Sequence of siltstone and dolomite - grey quartz-muscovite phyllite, crystalline dolostone.  Conformably overlie Pottoyu Granite and Dean Quartzite. Age: probably c.820Ma. Thickness: >100m. Geol. Prov: Amadeus Basin. Equiv. to Bitter Springs Formation.||||||20-APR-05
15279|Pinyinna beds|61154|5|Briefly described|p18, p5 Tb. 1|Neoproterozoic|Neoproterozoic|Grey to purple quartz-muscovite phyllite; crystalline dolostone; fine sst; red, green and pale fissile sltst; dolomitic sltst.  Dominated by phyllite, interlayered with dolostone and minor schists in the north and Petermann Ranges. Typ sect.thickness:250m||||||19-JUL-05
15279|Pinyinna beds|61306|5|Briefly described|p32|Proterozoic|Proterozoic|Geological Province: Amadeus Basin.||||||
15279|Pinyinna beds|61386|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Pinyinna  Geological Province: Amadeus Basin.||||||23-NOV-06
15279|Pinyinna beds|62376|5|Briefly described|p18|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin.||||||09-FEB-10
15279|Pinyinna beds|62379|5|Briefly described|p7 Fig. 2|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin.||||||
15279|Pinyinna beds|62989|6|Mentioned|p40|||Geological Province: Amadeus Basin.||||||07-FEB-08
15279|Pinyinna beds|65233|5|Briefly described|p3 Fig. 2|Neoproterozoic|Neoproterozoic|Geological province: Amadeus Basin.||||||07-FEB-11
15279|Pinyinna beds|65256|4|Described|piii, p5, p6 Tb.1, p8, p16-18, p21, p29|Cryogenian|Stenian|[Formerly Pinyinna Beds (in Forman 1966)]. Probably ~800-820 Ma. Sourced from local 1040-1080 Ma granites and volcanics. Phyllitic to schistose in character. >100m thick.||||Disconformably underlies Winnall beds, Inindia beds, Mount Currie Conglomerate; conformably overlies Dean Quartzite; correlative of the Bitter Springs Formation.|Red and grey shales, grey phyllite, crystalline brown and grey, foetid, stromatolitic dolostone.|19-MAY-14
15279|Pinyinna beds|67326|5|Briefly described|p2|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||Overlies Dean Quartzite. Is overlain unconformably by Boord Formation.||
15279|Pinyinna beds|67856|4|Described|p341 tab 4-8, p338, 335, 337, 344, 348|Neoproterozoic|Neoproterozoic|Type section: Pinyinna Range 24o35'S, 129o51'E.  Stromatolites poorly preserved; age unknown. Misspelt as Pinnyinna beds in fig 4-30 p338.||||Overlain by Mount Currie Conglomerate (unconformably). equivalent to Bitter Springs Formation. Overlies Dean Quartzite (unconformably).|Sandstone, siltstone, limestone.|
15279|Pinyinna beds|68270|4|Described|p679,683|Tonian|Tonian|Amadeus Basin.||||Overlain unconformably by Inindia beds.||03-JUL-19
15279|Pinyinna beds|68323|6|Mentioned|p4 Fig.2|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
15279|Pinyinna beds|69436|5|Briefly described|p21:4, 17-19|Neoproterozoic|Neoproterozoic|Olia Chain, Amadeus Basin. Involved in thin- and thick-skinned deformation by the Petermann Orogeny. At the top of this unit is a decollement surface below which basement and basal Amadeus Basin rocks were structurally interleaved.||||Is structurally interleaved with Dean Quartzite.||12-JUL-16
15279|Pinyinna beds|69437|5|Briefly described|p22:4-6|Cryogenian|Cryogenian|SW Amadeus Basin, Centralian A Superbasin. Supersequence 1.||||Overlies Dean Quartzite. Lateral equivalent of Bitter Springs Formation.||12-JUL-16
15279|Pinyinna beds|69438|2|Defined|p23:2-4, 9-10, 14-15, 18, 44, 52|Cryogenian|Cryogenian|Forman (1966), who described it as a metamorphosed equivalent of Bitter Springs Formation. SW Amadeus Basin. Type area in the Pinyinna Range, where it is over 200m thick. Appears as Pinyinna Beds on 23:4. Part of Supersequence 1 of the Centralian A Superbasin. Metamorphosed to amphibolite-grade facies, decreasing to greenschist facies to the N. Detrital zircon age populations suggest provenance from the Musgrave Province. Maximum age from SHRIMP U-Pb analyses of detrital zircons (Close et al., 2004); minimum age from intrusive dyke. Hosts uneconomic base metal occurrences.|Between 1058 +/- 31 Ma and c.820 Ma.|||Conformably (gradationally) overlies Dean Quartzite. Lateral equivalent of Bitter Springs Formation. Is intruded by an Amata Dolerite [equivalent] dyke.|Grey, brown and white, laminated micaceous siltstone, overlain by grey and pink laminated dolostone, sometimes stromatolitic, and grey limestone. Typically unmetamorphosed, but locally to lower amphibolite grade.|12-JUL-16
15279|Pinyinna beds|69673|5|Briefly described|p63, p80, p84, p88, p91|Neoproterozoic|Neoproterozoic|||||Overlies Dean Quartzite, correlated with Bitter Springs Formation|Micaceous siltstone overlain by laminated dolostone, sometimes stromatolitic; some limestone.|
15279|Pinyinna beds|70416|6|Mentioned|p65 Fig.2|Cryogenian|Cryogenian|Amadeus Basin.||||||
15279|Pinyinna beds|71088|6|Mentioned|p8|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
15279|Pinyinna beds|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||dolostone, sandstone, siltstone, phyllite|
15279|Pinyinna beds|71268|5|Briefly described|1m_geologyp12_lut.csv||||||||Grey quartz-muscovite phyllite, crystalline dolostone, fine-grained sandstone, red, green and pale grey fissile siltstone, dolomitic siltstone. Dominated by phyllite, interlayered with dolostone and minor schists in the north and Petermann Ranges.|
15279|Pinyinna beds|71841|5|Briefly described|p1|Cryogenian|Cryogenian|Of Amadeus Basin.||||||
15279|Pinyinna beds|73085|6|Mentioned|p1|Tonian|Tonian|[Written as PINYINNA BEDS].||||Underlain by Dean Quartzite. Equivalent to Bitter Springs Group.||
15279|Pinyinna beds|73086|5|Briefly described|p: 3, 7, 15, 18, 30, 39, 148, 151, 154|||Amadeus Basin. Part of Supersequence I; deposited during the early sag phase of basin development. Restricted to sporadic exposures in the southwest of the basin. May correlate specifically with the Gillen Formation because of the conformable to transitional basal boundary with quartzite units.||||Correlates to Bitter Springs Group. Conformably underlain by Dean Quartzite|Shale and grey, crystalline, laminated, foetid and stromatolitic dolostone.|
15284|Pioneer Sandstone|9814|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Sandstone, dolomite, minor conglomerate.||||||
15284|Pioneer Sandstone|22506|6|Mentioned|p130 Fig.4|Neoproterozoic III|Cryogenian|||||||
15284|Pioneer Sandstone|22560|6|Mentioned|p2|||||||||
15284|Pioneer Sandstone|22561|6|Mentioned|p16|Neoproterozoic|Neoproterozoic|||||||
15284|Pioneer Sandstone|22566|5|Briefly described|p81|||See Pioneer Formation - p81.||||||23-NOV-06
15284|Pioneer Sandstone|22646|6|Mentioned|Fig 1 on p 98|Neoproterozoic|Neoproterozoic|||||||
15284|Pioneer Sandstone|22648|4|Described|p 135|||Type section in Ellery Creek p 127.  Overlain by [??check!] Areyonga Formation, p135.||||||18-APR-18
15284|Pioneer Sandstone|22649|4|Described|p 145|Neoproterozoic|Neoproterozoic|||||||
15284|Pioneer Sandstone|22804|6|Mentioned|Fig 2 on p432|Neoproterozoic|Neoproterozoic|||||||
15284|Pioneer Sandstone|22816|5|Briefly described|p10 Fig. 4|Neoproterozoic|Neoproterozoic|In the Amadeus Basin.||||||17-JAN-07
15284|Pioneer Sandstone|22826|4|Described|p570|Neoproterozoic|Neoproterozoic|||||||
15284|Pioneer Sandstone|22901|6|Mentioned|75|||Geological province: Amadeus Basin.||||||23-NOV-06
15284|Pioneer Sandstone|22907|6|Mentioned|42|||||||||
15284|Pioneer Sandstone|23287|6|Mentioned|Fig.4|||Age: Upper Cryogenian. of Amadeus Basin.||||||
15284|Pioneer Sandstone|23314|5|Briefly described|333 Fig.4|Neoproterozoic III||In the Amadeus Basin.||||||16-NOV-06
15284|Pioneer Sandstone|23361|5|Briefly described|16 Fig.4|Neoproterozoic III|Cryogenian|||||||
15284|Pioneer Sandstone|24111|5|Briefly described|p216|Neoproterozoic|Neoproterozoic|Geological Province: Amadeus Basin.  See also p215 Fig. 11.||||||
15284|Pioneer Sandstone|24301|5|Briefly described|p16|||Geological Province: Amadeus Basin||||||
15284|Pioneer Sandstone|35805|6|Mentioned|Fig.3|||||||||
15284|Pioneer Sandstone|35863|6|Mentioned|Table 1|||||||||
15284|Pioneer Sandstone|37928|5|Briefly described|p516|||||||||
15284|Pioneer Sandstone|37929|6|Mentioned|Fig.2|||||||||
15284|Pioneer Sandstone|38157|6|Mentioned|Table VI|||||||||
15284|Pioneer Sandstone|38606|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
15284|Pioneer Sandstone|38885|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
15284|Pioneer Sandstone|38945|6|Mentioned|p130|||||||||
15284|Pioneer Sandstone|39583|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
15284|Pioneer Sandstone|39898|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Sandstone, feldspathic sandstone; minor granule conglomerate. Geological Province: Amadeus Basin.||||||14-FEB-06
15284|Pioneer Sandstone|39931|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
15284|Pioneer Sandstone|40740|3|Fully described|p88|||Described p12.||||||23-NOV-06
15284|Pioneer Sandstone|40906|6|Mentioned|Fig.9|||||||||
15284|Pioneer Sandstone|41405|6|Mentioned|p205|||||||||
15284|Pioneer Sandstone|41852|6|Mentioned|p220|||||||||
15284|Pioneer Sandstone|42059|6|Mentioned|Fig.2 P131|||||||||
15284|Pioneer Sandstone|42504|5|Briefly described|p72|||||||||
15284|Pioneer Sandstone|42643|6|Mentioned|Fig.4 P19|||||||||
15284|Pioneer Sandstone|42886|6|Mentioned|p217|||Of Preiss (1978). Upper part of Areyonga Formation of Prichard and Quinlan (1962). Correlated with Olympic Formation.||||||17-JAN-07
15284|Pioneer Sandstone|42940|5|Briefly described|Plate 9|||||||||
15284|Pioneer Sandstone|43225|5|Briefly described|Map Legend||Neoproterozoic|||||||
15284|Pioneer Sandstone|43503|6|Mentioned|12-50|||Age from Ediacaran.||||||23-NOV-06
15284|Pioneer Sandstone|43756|6|Mentioned|p542|||||||||
15284|Pioneer Sandstone|44111|6|Mentioned|p.58, Fig. 2|||in Amadeus Basin. Presented as "Pioneer" only in Fig. 2.||||||
15284|Pioneer Sandstone|45155|6|Mentioned|p28|||Correlation||||||
15284|Pioneer Sandstone|46730|5|Briefly described|p7|||Overlain by Pertatataka Formation. Underlain by Bitter Springs Formation. Geological Province: Amadeus Basin||||||17-JAN-07
15284|Pioneer Sandstone|46865|2|Defined|p57|late Adelaidean|late Adelaidean|||||||
15284|Pioneer Sandstone|49796|5|Briefly described|p1 & Sections|||||||||
15284|Pioneer Sandstone|50246|5|Briefly described|p20 Fig. 2|Proterozoic|Proterozoic|Pebble to cobble conglomerate with carbonate matrix.||||||07-FEB-11
15284|Pioneer Sandstone|61309|5|Briefly described|p16 Fig. 4|||Geological Province: Amadeus Basin.||||||06-FEB-08
15284|Pioneer Sandstone|61732|3|Fully described|p4 Fig. 3, p92-93, p102|Cryogenian|Cryogenian|Of Olympic Fm. Unconformable on Bitter Springs Fm; elsewhere overlies or interfingers with Olympic Fm. Cap dolostone rocks (or 'upper cap dolomite' of Preiss et al (1978)) are overlain by the Pertatataka Fm. See also p5 Tb. 1, p31, p87.||||||07-FEB-11
15284|Pioneer Sandstone|62376|5|Briefly described|p18|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin.||||||09-FEB-10
15284|Pioneer Sandstone|62379|5|Briefly described|p7 Fig. 2|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin.||||||
15284|Pioneer Sandstone|62453|5|Briefly described|p12 Fig. 8|Ediacaran|Cryogenian|Geological Province: Amadeus Basin.||||||
15284|Pioneer Sandstone|62595|5|Briefly described|p29 Fig.6.|Proterozoic|Proterozoic|Ross River area.|||||Pebble to cobble conglomerate with carbonate matrix.|
15284|Pioneer Sandstone|63562|6|Mentioned|p338 fig 3,p343, p346 fig 8,p352 fig 10|Ediacaran|Ediacaran|Of Amadeus Basin. Called Pioneer Formation on p343.||||Is overlain by Pertatataka Formation.|Conglomerates and arkosic sandstones interpreted as glacial outwash deposits.|
15284|Pioneer Sandstone|64068|6|Mentioned|p46|||Amadeus Basin. Correlated with Sun Hill Arkose, Little Burke Tillite, Black Stump Arkose, Wonnadinna Dolostone, Oorabra Arkose, Boko Formation, southern Georgina Basin.||||||
15284|Pioneer Sandstone|64103|6|Mentioned|p404|||Geological Province: Amadeus Basin.||||||07-FEB-11
15284|Pioneer Sandstone|64625|5|Briefly described|p243-245, p248-253, p256-258|Neoproterozoic|Neoproterozoic|Amadeus Basin. Near-shore deposits. Lithology, C and O isotopes detailed.||||Unconformably overlies Aralka Formation. Disconformably overlies Bitter Springs Formation. Unconformably overlain by Gaylad Sandstone, overlain by Pertatataka Formation|Fenestrate-carbonate clast breccia, dolomitic quartz sandstone and chert pebble conglomerate.|
15284|Pioneer Sandstone|64778|6|Mentioned|p18|||Amadeus Basin. Thermal and maturation history modelling.||||||
15284|Pioneer Sandstone|64794|6|Mentioned|p238 fig 2|Ediacaran|Ediacaran|||||||
15284|Pioneer Sandstone|64809|6|Mentioned|p3 Fig.2, p6 Fig.4, p11 Fig.10.|Proterozoic|Proterozoic|See also p13 Fig.13.||||||
15284|Pioneer Sandstone|65233|3|Fully described|p3 Fig. 2, p6|Neoproterozoic|Neoproterozoic|Tog. with lateral equiv.Olympic Fm. disconformable on Aralka Fm. Geol.prov: Amadeus Basin. Consists of intertidal sandstone capped by 'marker' dolostone in western part of basin - correlated with Marinoan Nucaleena Dolostone in Adelaide Geosyncline.||||||07-FEB-11
15284|Pioneer Sandstone|65272|6|Mentioned|p320 Fig.3||Ediacaran|||||||
15284|Pioneer Sandstone|65365|5|Briefly described|p10 Fig. 4|Ediacaran|Cryogenian|Amadeus Basin||||||
15284|Pioneer Sandstone|65366|5|Briefly described|p23 Fig. 3|Ediacaran|Cryogenian|Amadeus Basin||||||
15284|Pioneer Sandstone|65410|6|Mentioned|p74.|Neoproterozoic|Neoproterozoic|Amadeus Basin. Part of Supersequence 3.||||||
15284|Pioneer Sandstone|67326|5|Briefly described|p2|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||Overlies Olympic Formation. Is overlain unconformably by Pertatataka Formation.||
15284|Pioneer Sandstone|67856|6|Mentioned|p345 fig 4-34, p337, p338 fig 4-30|Neoproterozoic|Neoproterozoic|Shown as equivalent to Olympic Formation.||||||
15284|Pioneer Sandstone|68270|4|Described|p679,682-688|Cryogenian|Cryogenian|Amadeus Basin. Type section occurs in Ellery Creek, 1.0-1.3 km south of contact with basement; lat. 23'47'24"S, long.133'04'12"E. Crops out mainly in the N-NE Amadeus Basin (Preiss et al. 1978; Shaw & Wells 1983; Field 1991; Freeman et al. 1991; Williams et al. 2007), but a 9 m section was intersected in Wallara 1 in the central part of the basin (Indigo Oil & Sirgo Exploration 1990), real extent is unknown. Less than 170m thick. Glacial outwash fan deposit. Includes a paraconformable "upper marker cap dolomite" that resembles that in Wahlgu Formation and is related to Elatina glaciation. Contains columnar stromatolite Anabaria = Kotuikania juvensis (Elleria minuta), and could be used a straitgraphic marker in central Austtralian basins. Correlable to Elatina Formation, Nuccaleena Formation.||||Overlain by Pertatataka Formation, Underlain disconformably by Aralka Formation.|Mostly of feldspathic, medium- to coarse-grained, cross-bedded sandstone and conglomerate; dolomite and chert; minor lodestones.|03-JUL-19
15284|Pioneer Sandstone|68316|6|Mentioned|p778 Fig.1|||||||||
15284|Pioneer Sandstone|68323|6|Mentioned|p4 Fig.2|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
15284|Pioneer Sandstone|68733|6|Mentioned|p188, p189 Fig.8|Cryogenian|Cryogenian|Amadeus Basin.|||||Peri-glacial arkosic sandstone.|
15284|Pioneer Sandstone|69031|6|Mentioned|p4|||Amadeus Basin.||||||
15284|Pioneer Sandstone|69437|5|Briefly described|p22:4-5, 7|Cryogenian|Cryogenian|NE Amadeus Basin, Centralian A Superbasin. Supersequence 3.||||Overlies Aralka Formation. Is overlain by Pertatataka Formation. Is equivalent to Olympic Formation.|Conglomerate and sandstone.|12-JUL-16
15284|Pioneer Sandstone|69438|3|Fully described|p23:2-5, 7-8, 10, 15, 17-19, 55, 60|Ediacaran|Ediacaran|Priess et al. (1978). Central-northern Amadeus Basin. About 170m thick at the type section at Ellery Creek. Priess et al. (1978) reassigned the upper Member of the Areyonga Formation (Pritchard and Quinlan, 1962) to this unit. Drillhole Ooraminna-2 targeted this unit for gas.||||Disconformably overlies Areyonga Formation and Bitter Springs Formation. Lateral equivalent of Olympic Formation. Is overlain ?disconformably by Pertatataka Formation.|Cross-bedded medium- to coarse-grained feldspathic and arkosic sandstone, grading up-section to c.1m of pink-grey dolostone with red-brown chert nodules. The top is irregular with columnar stromatolites, pebbly sandstone and conglomerate.|12-JUL-16
15284|Pioneer Sandstone|69443|5|Briefly described|p28:8|||Adelaide Fold Belt. Glacigene and post-glacial deposits related to the Elatina (previously Marinoan) glaciation.||||Equivalent to Keepera Group (Georgina Basin).||12-JUL-16
15284|Pioneer Sandstone|69606|5|Briefly described|p3, p4 fig 2, p12, p14|Cryogenian|Cryogenian|Amadeus Basin. Potential reservoir and seal rock. Inferred to have been deposited during the Elatina glaciation.||||Overlies the Aralka Formation, inferred to be equivalent to the Olympic Formation.|Sandstone, conglomerate and diamictite.|
15284|Pioneer Sandstone|69673|5|Briefly described|p63, p65, p81, p84, p88, p91, p98, p101|||Reservoir rock, hosts Ooraminna gas field.||||Overlain by Gaylad Sandstone, Pertatataka Formation, overlies Olympic Formation, disconformably overlies Areyonga Formation|Cross bedded, medium to coarse grained feldspathic and arkosic sandstone, grading into thin dolostone with chert nodules.|
15284|Pioneer Sandstone|69937|5|Briefly described|v Fig.1, vi, p3 Tb.1, p17, p20-22,p47-48|Neoproterozoic|Neoproterozoic|Central-northern Amadeus Basin. A potential equivalent to the Olympic Sandstone. Shallow-marine to tidal deposits. Likely zircon provenance discussed. Estimated age between ~640 Ma and ~580 Ma, based on correlations with other glacial successions, is considerably younger than the youngest detrital zircon.|709 +/- 15 Ma (maximum depositional age).|||Is overlain unconformably by Gaylad Sandstone. Lateral equivalent of Olympic Formation.|Medium- to coarse-grained, feldspathic and arkosic sandstone with common sedimentary structures. Dolomitic in upper parts. Pink dolostone and columnar stromatolites at top.|
15284|Pioneer Sandstone|70018|5|Briefly described|p234-235|Neoproterozoic|Neoproterozoic|Amadeus Basin. Of Supersequence 3 in the northern Amadeus Basin. Equivalent to Olympic Formation. Correlable to Inindia Beds in the southern Amadeus Basin.||||Overlain by Pertatataka Formation. Underlain by Aralka Formation.||
15284|Pioneer Sandstone|70416|5|Briefly described|p63, p65, p68, p72-73|Cryogenian|Cryogenian|Deposited during the Elatina Glaciation. Contains erratics of Aralka Formation with stromatolites (described in great detail).||||Unconformably overlies Aralka Formation. Is overlain by Pertatataka Formation. Laterally equivalent to Olympic Formation.||
15284|Pioneer Sandstone|70839|5|Briefly described|p329|Neoproterozoic|Neoproterozoic|Of Amadeus Basin.||||Overlain by Pertatataka Formation. Underlain by Aralka Formation. Equivalent to Olympic Formation.||
15284|Pioneer Sandstone|71080|5|Briefly described|p29 fig 20, p30, 31|Cryogenian|Cryogenian|Amadeus Basin. Supersequence 3. Significant gas flows in Ooraminna 1 and 2.|||||Diamictite, sandstone and lesser conglomerate?|
15284|Pioneer Sandstone|71088|6|Mentioned|p8|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
15284|Pioneer Sandstone|71279|5|Briefly described|p355 Fig.2, p365-368|Ediacaran|Ediacaran|Amadeus Basin.|||||Highly silicified sandstone, shale, dolostone.|
15284|Pioneer Sandstone|71344|6|Mentioned|p1094|||Amadeus Basin. Glacial.||||Equivalent to Olympic Formation.||10-NOV-17
15284|Pioneer Sandstone|71592|5|Briefly described|Appendix A.|||Amadeus Basin.|709+/-15 Ma (MDA: U-Pb zircon SHRIMP)||||Medium-grained sandstone.|
15284|Pioneer Sandstone|71841|5|Briefly described|p1|Ediacaran|Ediacaran|Of Amadeus Basin.||||Overlain by Gaylad Sandstone or Pertatataka Formation. Equivalent to Olympic Formation. Grades into Inindia beds.||
15284|Pioneer Sandstone|72375|4|Described|p1-2,20,22-23,25|Neoproterozoic|Neoproterozoic|Of Amadeus Basin. Nomenclature of Preiss et al., 1978. Extends across the north and northcentral Amadeus Basin, and can be correlated with Elatina glacial successions of the Adelaide Rift Complex and the Georgina, Ngalia and Officer basins (Lindsay 1993, Walter et al 1995). Interpreted to have been deposited in a shallow marine to tidal setting restricted to central-northern part of the Amadeus Basin (Preiss et al., 1978). Stratigraphic top of Pioneer Sandstone is characterised by irregular erosional surface containing erosional scours and filled with pink dolomite with columnar stromatolites (Normington et al., 2015). SHRIMP U-Pb zircon analysis by Kositcin et al., 2015 yielded an interpreted maximum depositional age (weighted mean 238U/206Pb) of 709+\-15 Ma, which is older that the inferred depositional age of c. 640 to 580 Ma (see Williams 1998, Grey et al., 2011) based on stratigraphic equivalence to Olympic Formation. LA-ICP-MS Hf isotopic signatures for the zircon age populations from NTGS AS13CJE031 (quartz sandstone) suggest they crystallised in magmas derived from a range of crustal sources (see p24 for Hf isotopic results and interpretations).||||Overlain unconformably by Gaylad Sandstone. Laterally correlable (interfingers with) to Olympic Formation.|Quartz sandstone, typically medium- to coarse-grained, feldspathic and arkosic with common sedimentary structures; overlain by dolomitic sandstone with abundant tabular cross-beds and, in parts, contains discrete dolostone.|
15284|Pioneer Sandstone|72516|6|Mentioned|p87|Ediacaran|Ediacaran|Amadeus Basin. Age implied from equivalence with Oorabra Arkose.||||Equivalent to the Oorabra Arkose.||02-JUN-21
15284|Pioneer Sandstone|72601|5|Briefly described|p3-5, p7-8, p11, p17|Cryogenian|Cryogenian|Amadeus Basin. Deposition was coeval with the Elatina glaciation. Previously part of the Pertatataka Formation prior to redefinition by Preiss et al. (1978).||||Unconformably underlain by Aralka Formation. Overlain by Pertatataka Formation. Equivalent to Olympic Formation. Correlated to Cottons Breccia.||
15284|Pioneer Sandstone|73085|6|Mentioned|p1|Ediacaran|Ediacaran|[Unclear relationship with Olympic Formation].||||Underlain by[?] Aralka Formation. Partly overlain by Pertatataka Formation unconformably. Partly overlain by and equivalent to Gaylad Sandstone. Equivalent to Inindia beds.||
15284|Pioneer Sandstone|73086|2|Defined|[See comments].|Cryogenian|Cryogenian|[Defined herein. No revised definition card]. Glaciogenic. Amadeus Basin. Part of Supersequence III. Lateral equivalent of the Olympic Formation; more extensively recognised in the subsurface than Olympic Formation. Primarily a feldspathic and pebbly sandstone with common conglomerate low in the unit and dolostone higher in the unit; capped by pink, stromatolite-bearing dolostone (Elleria minuta). Named after Pioneer Creek. Type section: Ellery Creek (sometimes obscured by alluvium). Key localities: Ringwood (Gaylad Syncline); Hidden Valley (Ross River Syncline). Distribution: confined to the northeast and north central margin of the basin as thin, discontinuous intervals. Previously described as a member of the Areyonga Formation. Type section thickness: 170 m. Where visible, sandstone is poorly sorted and weakly cross-bedded including herringbone cross-beds in the upper portion. Clear and distinctive cap carbonate. Correlated with Marinoan glacial successions. Geochron from detrital zircon maximum depositional ages; also constrained by the ca 660-635 Ma Marinoan glaciation. Interpreted to be an intraglacial glacial outwash or periglacial facies that probably correlates with the Olympic Formation. Partly correlates to upper Inindia beds. Possibly correlates to Mount Doreen, Elatina, and Nuccaleena formations. Partly equivalent to 'Undoolya Sequence'. p: 3, 5-6, 18, 62-63, 79, 99-101, 112-118, 122-123, 143, 151, 157, 167.|709 +/- 14 Ma SHRIMP U-Pb|||Equivalent to Olympic Formation. Unconformably underlain by Bitter Springs Group, Areyonga and Aralka formations. Overlain by [and equivalent to?] Gaylad Sandstone. Overlain by Pertatataka Formation.|Dominantly white to brown, friable, medium- to coarse-grained, cross-bedded, feldspathic sandstone capped by pink stromatolite-bearing dolostone.|
15284|Pioneer Sandstone|73088|6|Mentioned|p1|Cryogenian|Cryogenian|Amadeus Basin, northeast.||||Unconformably underlain by Aralka Formation. Unconformably overlain by Pertatataka Formation. Equivalent to Gaylad Sandstone and Olympic Formation.||
15284|Pioneer Sandstone|73180|4|Described|p47-48, p51 Fig.6, p52-54|Neoproterozoic|Neoproterozoic|Amadeus Basin. Elatina glacial/post-glacial sequences. Outcrops around Mount Connor. Disconformable contact with Bitter Springs Group in the north and northeast of the basin from erosion by a grounded ice sheet, deposition of thin sandstones and conglomerates from localised high-energy deposition, likely glacial outwash. [Descriptions of the Olympic Formation were also applied to the Pioneer Sandstone in text].||||Equivalent to the Olympic Formation, disconformably overlies the Aralka Formation, conformably underlies the Pertatataka Formation.|Glacial/periglacial clastic deposits including diamictite and reworked carbonates interbedded and capped by a distinctive pink to buff dolostone in proximal glaciogenic deposits, commonly bearing diagnostic stromatolites.|
15284|Pioneer Sandstone|75070|5|Briefly described|p175, 178-184|Middle Ordovician|Middle Ordovician|Western Tasmania. Detrital zircon signature discussed. Detrital zircon graph. Hf isotope diagram.|||||Sandstone.|
15306|Plain Creek Formation|24442|5|Briefly described|p23 Fig. 2|Mesoproterozoic|Mesoproterozoic|Of the McNamara Group.  Age: >1590Ma.||||||
15306|Plain Creek Formation|38237|6|Mentioned|Fig.3|||||||||
15306|Plain Creek Formation|38348|6|Mentioned|p18|||||||||
15306|Plain Creek Formation|39422|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of McNamara Gp.  Fissile to flaggy, micaceous sltst. and shale with thin interbeds of ripple laminate sst; thicker interbeds of flaggy to blocky, well-sorted sst. with thin grit and pebbly bands. Overlies massive orthoquarzite within the McNamara Group.||||||10-JAN-05
15306|Plain Creek Formation|39497|4|Described|p11|||||||||
15306|Plain Creek Formation|39925|6|Mentioned|p334|||||||||
15306|Plain Creek Formation|45166|5|Briefly described|p76|||||||||
15306|Plain Creek Formation|49018|2|Defined|p8|Carpentarian|Carpentarian|||||||
15306|Plain Creek Formation|62659|5|Briefly described|Map Legend|Statherian|Statherian|Of the McNamara Group. Micaceous siltstone and shale, fine to coarse grained lithic and sublithic sandstone; minor pebble conglomerate, graded sandstone beds, pebble to boulder bearing mudstone.||||||
15306|Plain Creek Formation|65337|3|Fully described|p9 Fig.5, pp27-28, p96.|Paleoproterozoic|Paleoproterozoic|Redefined; mapped in First Edition as part of Bluff Range beds. 400 - 1000 m of shallow to deep marine basin sediments including fan deltas. Manganese and iron oxide films and veins are common.|1647 +/- 8 to 1630 +/- 5 Ma.|Unit in McNamara Group.||Overlies Bullrush Conglomerate and Shady Bore Quartzite. Is overlain by Lawn Hill Formation and, unconformably, by Constance Sandstone.|Micaceous siltstone and shale, fine- to coarse-grained lithic and sublithic sandstone; minor pebble conglomerate, graded sandstone beds, and pebble- to boulder-bearing mudstone-turbidite and mass flow sediments.|
15306|Plain Creek Formation|67323|5|Briefly described|GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|Isa Superbasin.||McNamara Group|||Siltstone, shale, sandstone.|
15306|Plain Creek Formation|69433|4|Described|p18:2, 5-6, 9-10|Statherian|Statherian|Southern succession, Lawn Hill Platform. 400-1000m thick. A variety of facies is represented. Surficial manganese is common as a weathering crust; unlikely to extend deep into the host rock.||McNamara Group.||Conformably overlies Shady Bore Quartzite and (probably) Bullrush Conglomerate. Is overlain conformably by Lawn Hill Formation. Correlative of Buddycurrawa Volcanics (?).|Dominantly micaceous siltstone and shale, with several sandstone units. These sediments are arranged in cycles, a few metres thick, of stacked, upward-thickening and -coarsening beds. Thin films of manganese and iron oxides common throughout.|12-JUL-16
15306|Plain Creek Formation|69591|5|Briefly described|p54|||Camooweal-Murphy Domain, Isa Superbasin. Marine deposits.||McNamara Group.|||Siltstone, shale, sandstone.|
15306|Plain Creek Formation|69673|5|Briefly described|p52 fig 42, p53, p54, p55|||1km thick. Unconventional petroleum potential.||McNamara Group||Correlated with Riversleigh Siltstone, Termite Range Formation|Micaceous siltstone and shale, contains several sandstone units.|
15306|Plain Creek Formation|72418|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet.||Unit of McNamara Group.|||Siltstone, shale, sandstone|
15306|Plain Creek Formation|72421|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.||Unit of McNamara Group.|||Siltstone, shale, sandstone|
15306|Plain Creek Formation|72422|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.||Unit of McNamara Group.|||Siltstone, shale, sandstone|
15306|Plain Creek Formation|72423|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet Geological Compilation Series.||Unit of McNamara Group.|||Siltstone, shale, sandstone|
15306|Plain Creek Formation|72526|5|Briefly described|p8 Fig.1.3, p10.|Statherian|Statherian|Shown as being located in the central part of the South Nicholson Basin.||McNamara Group||Overlies Shady Bore Quartzite and underlies Lawn Hill Formation.||
15306|Plain Creek Formation|72527|4|Described|p1, 8, 112, 119, p132-139, p193, 194.|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin. Characterised by 'interbeds' of shale, siltstone and sandstone  ranging in thickness from 400m to 1000m.|1635+/-13 max dep age c. 1647-1630|McNamara Group||Overlies Shady Bore Quartzite, Bullrush Conglomerate.  Underlies Lawn Hill Formation (presumed conformably) or Constance Sandstone (unconformably). Equivalent to Riversleigh Formation (or Siltstone).|Commonly cycles of feldspathetic and fine-grained flaggy sandstones and laminated siltstones. Also includes micaceous siltstone.|
15306|Plain Creek Formation|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Shown as being located in the Northern Territory part of the McNamara Group.||McNamara Group||Overlies Shady Bore Quartzite and underlies Lawn Hill Formation. Laterally equivalent to Mount Les Siltstone, Riversliegh Siltstone.||
15306|Plain Creek Formation|72919|6|Mentioned|p5|Paleoproterozoic|Paleoproterozoic|||McNamara Group||Underlain by Shady Bore Quartzite. Overlain by Lawn Hill Formation. Equivalent to Bullrush Conglomerate.||
15306|Plain Creek Formation|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin region, Isa Superbasin.||McNamara Group||Partly underlain by Bullrush Conglomerate and Shady Bore Quartzite. Overlain by Lawn Hill Formation.||
15330|Plover Formation|5952|5|Briefly described|p214 Fig. 4, p215 Fig. 5, p216|Middle Jurassic|Early Jurassic|In figure, Fm = Formation. Geological Province: Bonaparte Basin.||||||01-MAR-10
15330|Plover Formation|7142|6|Mentioned|p350 Fig.4.|Middle Jurassic|Early Jurassic|Browse Basin.||||Overlies Nome Formation. Is overlain by Lower Vulcan and Montara Formations.||
15330|Plover Formation|12466|6|Mentioned|p177 Fig.10.|||||||Overlies Mount Goodwin Formation. Is overlain by Flamingo Group.||
15330|Plover Formation|13194|4|Described|p385 Tb. 4-16, p396 fig 4-60|Callovian|Jurassic|Type Section: Petrel 1 well (1820-2229m). 200-672m thick non-marine to marginal marine sediments.||Troughton Group||Overlies Malita Formation. Overlies Cape Londonderry Formation (disconformably). Overlain by Frigate Shale (uncf).|Coarse grained sandstone; minor shale, coal and limestone.|
15330|Plover Formation|13222|6|Mentioned|p234.|Early Jurassic|Early Jurassic|This unit was not involved in compressive structures, and truncates older structures within the Triassic. Hence folding (and formation of anticlinal traps) is constrained to late Triassic-Early Jurassic.||||||
15330|Plover Formation|13224|5|Briefly described|p484|Oxfordian|Pliensbachian|||||||
15330|Plover Formation|13234|5|Briefly described|p250 Fig.2, p260, p263 Tb.4. |Middle Jurassic|Middle Jurassic|Coastal plain deposits at the top of this unit provide reservoir facies.||||Is overlain by Flamingo Group.|Includes fluvial and paralic sands.|
15330|Plover Formation|13267|5|Briefly described|pp273-286.|Middle Jurassic|Middle Jurassic|Sahul Platform, Bonaparte Basin. Fair to excellent hydrocarbon reservoir quality. Variable oil shows observed. Hydrocarbon-charged fluid entering the lower part of this fluvio-deltaic unit was silica-rich (oil inclusions).||||Is overlain by Elang Formation.|Quartzose, medium- to coarse-grained, moderately well-sorted sandstone with minor amounts of clay allowing extensive quartz overgrowth, reducing porosity; minor coal.|
15330|Plover Formation|13310|6|Mentioned|p295.|Middle Jurassic|Middle Jurassic|Presence of a single palaeo-oil column from Octavius 2 exploration well, Vulcan Sub-basin.|||||Sandstones.|
15330|Plover Formation|13353|6|Mentioned|p401 Fig.2.|||||||Is overlain by Lower Vulcan and Montara Formations.||
15330|Plover Formation|13354|6|Mentioned|p375 Fig.6.|Middle Jurassic|Early Jurassic|Unit of Troughton Group. Overlies Nome Formation and underlies Lower Vulcan Formation.||86||||28-OCT-14
15330|Plover Formation|22663|5|Briefly described|NT97 -1-4 Fig.3||Jurassic|||||||01-MAR-10
15330|Plover Formation|23376|4|Described|p229 Fig.2;p227-9,235,240,244-5|Callovian|Hettangian|In the Bonaparte Basin.||||||23-NOV-06
15330|Plover Formation|23377|4|Described|p212 Fig.5; p211, 223|Late Jurassic|Early Jurassic|Unconformities at top and base. In the Vulcan Sub-basin.||||||23-NOV-06
15330|Plover Formation|23378|4|Described|p180 Fig.2, p177-179|Middle Jurassic|Early Jurassic|In the Vulcan Sub-basin.||||||01-MAR-10
15330|Plover Formation|24047|5|Briefly described|p13|Jurassic|Jurassic|Geological Province: Money Shoal Basin.||||||
15330|Plover Formation|24171|5|Briefly described|p722 Fig. 3|Jurassic|Jurassic|Geological Province : Vulcan Sub-Basin||||||01-MAR-10
15330|Plover Formation|24207|5|Briefly described|p209 Fig. 5, p210 Fig. 6|Toarcian|Toarcian|||||||01-MAR-10
15330|Plover Formation|24234|5|Briefly described|p287 Fig.3|Jurassic|Jurassic|Overlain by the Elang Formation. Geological Province: Bonaparte Basin.||||||17-MAR-05
15330|Plover Formation|24235|5|Briefly described|p298, p299|Jurassic|Jurassic|See also Plover formation. Geological Province: Bonaparte Basin.||||||
15330|Plover Formation|24427|5|Briefly described|p48, p49 Fig.2|Middle Jurassic|Early Jurassic|Geological Province: Bonaparte Basin.||||||09-MAR-05
15330|Plover Formation|24569|5|Briefly described|p248 Fig. 3|Oxfordian|Early Jurassic|Of the Troughton Group. Geological Province: Petrel Sub-basin.||||||17-MAR-05
15330|Plover Formation|41459|6|Mentioned|Fig.2|||||||||
15330|Plover Formation|41532|3|Fully described|p304|||||||||
15330|Plover Formation|41690|5|Briefly described|p6|||See also p57.||||||23-NOV-06
15330|Plover Formation|41731|6|Mentioned|Fig.3|||||||||
15330|Plover Formation|41733|6|Mentioned|Fig.3|||||||||
15330|Plover Formation|41759|6|Mentioned|p270|||||||||
15330|Plover Formation|42034|4|Described|Fig.4 P11|||||||||
15330|Plover Formation|42053|5|Briefly described|Fig.2 P29|||||||||01-MAR-10
15330|Plover Formation|42056|4|Described|p98|||||||||
15330|Plover Formation|42057|4|Described|p75|||See also p79.||||||23-NOV-06
15330|Plover Formation|42066|6|Mentioned|Fig.3 P199|||||||||
15330|Plover Formation|42081|5|Briefly described|Fig.2 P291|||||||||
15330|Plover Formation|42151|6|Mentioned|Fig.3 P57|||||||||
15330|Plover Formation|42442|3|Fully described|p24|Callovian|Pliensbachian|NT and WA.||||||23-NOV-06
15330|Plover Formation|42861|5|Briefly described|p3|||||||||
15330|Plover Formation|43230|5|Briefly described|p9|Middle Jurassic|Early Jurassic|||||||03-SEP-14
15330|Plover Formation|43661|6|Mentioned|Fig.3|||||||||
15330|Plover Formation|43699|5|Briefly described|p3-4|Middle Jurassic|Early Jurassic|||||||
15330|Plover Formation|43739|6|Mentioned|p10||Middle Jurassic|||||||
15330|Plover Formation|43825|6|Mentioned|p147||Jurassic|||||||
15330|Plover Formation|43826|6|Mentioned|Fig.2,p163|Middle Jurassic|Early Jurassic|||||||01-MAR-10
15330|Plover Formation|43828|6|Mentioned|p206|||||||||
15330|Plover Formation|43829|5|Briefly described|Fig.2,p225||Middle Jurassic|In the Sahul Syncline.||||||23-NOV-06
15330|Plover Formation|49637|5|Briefly described|Fig.3|Middle Jurassic|Middle Jurassic|Of the Troughton Group. Geological Province: Londonderry High.||||||07-FEB-11
15330|Plover Formation|50027|5|Briefly described|p10|Middle Jurassic|Early Jurassic|Fluviodeltaic sands.  Geological Province: Browse Basin.||||||
15330|Plover Formation|60378|4|Described|p95-101, 104-120|Middle Jurassic|Early Jurassic|Marine to terrestrial sediments including coal-rich layers. Petroleum reservoir. Thickness variations and distribution discussed.|||||Fluvial to deltaic sandstone.|
15330|Plover Formation|60386|6|Mentioned|p300, 302, 314|Middle Jurassic|Early Jurassic|Browse Basin/Bonaparte Basin. Non-marine, deltaic-nearshore-shelf.||||||
15330|Plover Formation|60634|5|Briefly described|p1166, p1167 Fig.2,  p1168 Fig.3.|Late Jurassic|Early Jurassic|Hydrocarbon reservoir sealed by Early Cretaceous calcareous shales. Leakage from the Skua oil field is primarily controlled by a fault intersection.||Unit in Troughton Group.||Unconformably overlies Nome Formation. Is overlain by Vulcan Formation.|Sandstones.|
15330|Plover Formation|61250|5|Briefly described|p45|Middle Jurassic|Early Jurassic|The dominant source for the Laminaria and Corallina Oil fields.||||||
15330|Plover Formation|61548|6|Mentioned|p480 Fig.3|Middle Jurassic|Late Triassic|Northern Bonaparte Basin.||||||
15330|Plover Formation|61550|5|Briefly described|p494, p495 Fig.2, p505.|Middle Jurassic|Early Jurassic|Vulcan Sub-basin. Fluvio-deltaic mudstones. Contains oils and condensates for the Montara and Bilyara wells, modelled to have had late oil generation and charge in the Pliocene (5 Ma to present).||||Unconformably overlies Sahul Group. Is overlain unconformably by Swan Group.|Fluvio-deltaic mudstones.|
15330|Plover Formation|62837|5|Briefly described|Stratigraphic columns|Middle Jurassic|Early Jurassic|Of the Troughton Group.  Age: ~203-~154Ma. Geological Province:  Northern Bonaparte Basin, Petrel Sub-basin (offshore) and Money Shoals Basin.||||||01-MAR-10
15330|Plover Formation|63062|4|Described|p9 Fig. 9, p33|Middle Jurassic|Early Jurassic|Represents youngest component of the Troughton Group in the study area. Geological Province: Bonaparte, Arafura and Money Shoal Basins. Fine- to coarse-grained sandstones with interbedded siltstones and claystones, and minor coal; fluvial in origin.||||||07-FEB-11
15330|Plover Formation|63358|5|Briefly described|p4 Fig. 1.3|Callovian|Sinemurian|See also p16 Fig. 3.1, p133 Fig. 3.71 and p172 Appendix Table A1.11.||||||01-MAR-10
15330|Plover Formation|64689|5|Briefly described|p3-18 |Middle Jurassic|Early Jurassic|Established as a regional oil and gas-liquids source rock: the dominant source for the Laminaria and Corallina oil fields; also as a target reservoir. Upper surface is the Callovian Unconformity.||||Unconformably overlies Nome Formation. Is overlain unconformably by Lower Vulcan Formation.||
15330|Plover Formation|64695|6|Mentioned|p265, p266, p267-269 Figs.12-14||||||||Sandstones.|
15330|Plover Formation|64696|5|Briefly described|p125; 127-128 Figs.2,3,4|Middle Jurassic|Early Jurassic|See also p129-131, p134-140. Bonaparte Basin. A key pre-rift reservoir/source unit.||||Unconformably overlies Nome Formation. Unconformably underlies the Vulcan Formation.|Basal red-bed succession of upward-fining channel sandstones capped by red/grey-green shales and siltstones; massive sandstones; coastal plain/deltaic shales; massive sheet-like sandstones.|
15330|Plover Formation|64697|5|Briefly described|p85, p86, p88, p96|Middle Jurassic|Early Jurassic|||||||
15330|Plover Formation|66187|5|Briefly described|p413 Fig.2|Middle Jurassic|Early Jurassic|Underlies the Montara Formation, overlies the Nome Formation. Mount Ashmore Dome.||||||
15330|Plover Formation|67195|5|Briefly described|Appendix 2|||Browse Basin.|||||Includes yellow fine-grained sandstone; grey siltstone, mottled (bioturbated).|04-JAN-23
15330|Plover Formation|67200|5|Briefly described|app 2 p7||||||||Fine grained sandstone and siltstone; bioturbated.|
15330|Plover Formation|67370|6|Mentioned|p323 Fig.14.|Jurassic|Jurassic|Southeastern Bonaparte Basin. Type section in Petrel-1 between 2,229 - 2471 m.||||Overlies Malita Formation.||
15330|Plover Formation|68054|6|Mentioned|p41, 44, 49|Middle Jurassic|Early Jurassic|Bonaparte Basin. Penetrated by the Sunrise-2 and Sunset West-1 well; palynomorphs therein are a focus of this article. Abundant photographs; systematic palaeontology of dinoflagellate cysts.|||||Fluvial sandstones dominate the lower pars of this unit; shallow-marine sandstones in the upper.|
15330|Plover Formation|68135|5|Briefly described|p51, p61|Middle Jurassic|Early Jurassic|Bonaparte and Browse Basins.||Troughton Group.||Overlies Malita Formation.||14-SEP-17
15330|Plover Formation|68223|6|Mentioned|p178 Fig.3, p179 Fig.4|Middle Jurassic|Early Triassic|||||||06-SEP-18
15330|Plover Formation|69297|4|Described|p283,  p285, p289|Middle Jurassic|Lower Jurassic|Money Shoal Basin and Barcoo and Seringapatam Sub-basins of the Browse Basin. Deposited in a fluvial-deltaic environment. Potential oil and gas source rocks. See also p303, p305, p307, p308, p309, p311, p320, p322, p324.||Troughton Group||Unconformably overlain by the Flamingo Group or the Montara Formation.|Coarsening upwards sandstones, interbedded with fine-grained beds of siltstone and shale.|
15330|Plover Formation|69418|6|Mentioned|p3:24, 26|||Pine Creek Orogen. Appears as ?Plover Formation eq. Identified as Petrel Formation in Sullivan (1970), hosts the Daly River Road surficial Fe deposit (described). Similarly identified as Petrel Formation in Ferenczi (2001), hosts the McLeans surficial-type Mn deposit (briefly described).||||||12-JUL-16
15330|Plover Formation|69452|5|Briefly described|p36:8, 15, 21, 28-29|Middle Jurassic|Early Jurassic|Petrel Sub-basin, Bonaparte Basin. Up to 500m thick (offshore). Drillhole Jabiru-1A intersected a 57m gross oil column in this unit and basal Flamingo Group, starting the Jabiru oil field. Also contained seven reservoir units in the Skua oil field.||Troughton Group.||||12-JUL-16
15330|Plover Formation|69455|6|Mentioned|p39:5|||||||Is overlain by Darwin Formation.||12-JUL-16
15330|Plover Formation|69456|4|Described|p40:1-5, 15|Early Cretaceous?|Early Jurassic|Bonaparte and Money Shoal Basins. In the NT, rocks of this unit are consistently referred to as "Plover Formation equivalent" (to the Bonaparte Basin succession). Onshore exposures were previously referred to as Petrel Formation (eg Pietsch and Stuart-Smith, 1987); that name was abandoned by Mory (1991) as it included an unconformity. Thickness is up to 564m offshore, where its age is given as late Early to late Middle Jurassic; and a queried assignation of up to 5m onshore, where its age is Jurassic to early Cretaceous. Fluvial braided-river systems to shallow-marine. Fair to very good petroleum source potential. Reservoir for gas accumulations in the E Bonaparte Basin.||Troughton Group.||Unconformably overlies Kulshill, Arafura and Goulburn Groups. Is overlain unconformably by Flamingo and Bathurst Island Groups.|(Offshore): Fine- to coarse-grained sandstone interbedded with siltstone and claystone, and minor coal. ?(Onshore): friable, poorly sorted, commonly limonitic sandstone and minor conglomerate.|12-JUL-16
15330|Plover Formation|69653|5|Briefly described|p1, 6, 8, 10, 15, 17-18, 37, 39, 43, 76|Middle Jurassic|Early Jurassic|Petrel Sub-basin. Suitable for CO2 storage; sealed by Frigate Shale. Delta plain- shoreface and fluvial deposits. Composite well diagram. Photomicrographs. See also p45-47, 50, 53, 63-64, 74.||Troughton Group.||Overlies Malita Formation. Is overlain by Elang Formation.|Mudstone; siltstone interbedded with fine-grained sandstone; massive pebbly sandstone; fine- to coarse-grained sandstone; very fine- to fine-grained sandstone. Facies described in detail.|
15330|Plover Formation|69673|5|Briefly described|p173||||||||Sandstone, siltstone and shale.|
15330|Plover Formation|69689|6|Mentioned|p16|Jurassic|Jurassic|Browse, Bonaparte Basins.||||Overlies Nome Formation. Is overlain by Montara Formation.||
15330|Plover Formation|70061|5|Briefly described|Petrel Sub-basin; Fig.2|Middle Jurassic|Early Jurassic|See also Regional geology: Figs.6-7, p5, p9-10, p12-15, p18-19. Sahul: Fig.2, p1-3. Vulcan: Fig.2, p1-2. Thick, widespread succession of fluvial and coastal plain sediments across most of the Bonaparte Basin (except the Ashmore Platform and the crest of the Londonderry High). A major source and productive (Skua and Jabiru fields) reservoir unit in the N Bonaparte Basin. Source and reservoir rocks in Sahul Syncline and Vulcan Sub-basin, and intraformational seal in the former.||Troughton Group.||Overlies Malita Formation. Is overlain by Elang Formation.|Includes local, thin, high-quality coals and pro-delta shales with high source potential.|12-JUL-16
15330|Plover Formation|70064|5|Briefly described|Northern Fig.2;p1-3. Yampi: Fig.2;p1-2|Bathonian|Hettangian|See also Regional: Fig. 6; p4-10. Central: Fig.2; p1-2. Browse Basin. Contains organic-rich rocks with fair to moderate oil potential, as well as gas-prone, high-quality coals and pro-delta shales. Potential reservoirs in horsts and tilted fault-blocks; sealed by Lower Vulcan Formation. Hosts gas in the Crux structure within the Heywood Graben. Has potential for intraformational seals.||Troughton Group.||Overlies Nome Formation (Sahul Group). Is overlain by Lower Vulcan Formation or Montara Formation (Swan Group).|Syn-rift sediments comprising fine- to very fine-grained sandstones, interbedded with occasional medium- to coarse-grained sandstones, siltstones, claystones and minor coals. Some local tuffaceous volcanics.|12-JUL-16
15330|Plover Formation|70098|5|Briefly described|p19 Fig.5|Middle Jurassic|Early Jurassic|||Troughton Group||Overlies Kulshill Group (and equivalent?). Is overlain by Flamingo Group, Lower (Flamingo Group).||
15334|Plum Tree Creek Volcanics|9538|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Edith River Group.  Includes the Fanny Rhyolite and Ironbark Members.  Massive to poorly layered red to reddish-brown xenolithic, porphyritic, ignimbrite, glassy in places; finely porphyritic and minor glassy, red-pink rhyolite.||||||28-OCT-04
15334|Plum Tree Creek Volcanics|23216|5|Briefly described|p3,Table1p10,13-4|Orosirian|Orosirian|Age: 1857-1822 Ma. Consists of: Ironbark Member, Fanny Rhyolite Member and Mount Shepherd Rhyolite Member.||||||
15334|Plum Tree Creek Volcanics|23384|6|Mentioned|Fig 27|||Of Needham and Stuart-Smith (1985).||||||
15334|Plum Tree Creek Volcanics|23733|5|Briefly described|p32 Fig. 19|||Age: 1822Ma.||||||
15334|Plum Tree Creek Volcanics|23867|5|Briefly described|p3|Paleoproterozoic|Paleoproterozoic|Of Edith River Group. Overlain unconformably by Mamadawerre Sandstone.  Age: ~1822Ma.  Geological Province: McArthur Basin.  See also Fig. 3.||||||07-NOV-08
15334|Plum Tree Creek Volcanics|24050|5|Briefly described|p11 Tb. 3|Orosirian|Orosirian|Same as Plum Tree Volcanics?  Ignimbrite.  Age: 1828+/-5m.y. (SHRIMP U-Pb zircon).||||||
15334|Plum Tree Creek Volcanics|30831|6|Mentioned|p6|||||||||
15334|Plum Tree Creek Volcanics|39357|4|Described|p14|||||||||
15334|Plum Tree Creek Volcanics|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
15334|Plum Tree Creek Volcanics|40248|4|Described|p225|||||||||
15334|Plum Tree Creek Volcanics|40823|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
15334|Plum Tree Creek Volcanics|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
15334|Plum Tree Creek Volcanics|41125|6|Mentioned|Fig.15|||||||||
15334|Plum Tree Creek Volcanics|41294|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
15334|Plum Tree Creek Volcanics|41295|4|Described|p12|||||||||
15334|Plum Tree Creek Volcanics|41311|4|Described|p14|||||||||
15334|Plum Tree Creek Volcanics|41397|4|Described|p17|||||||||
15334|Plum Tree Creek Volcanics|41407|6|Mentioned|Map legend|Proterozoic||||||||
15334|Plum Tree Creek Volcanics|41586|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
15334|Plum Tree Creek Volcanics|43140|5|Briefly described|p3|||Misspelt in description as Phillips Creek Volcanics.||||||
15334|Plum Tree Creek Volcanics|43149|5|Briefly described|Map Legend||Paleoproterozoic|Of the Edith River Group. Of Orosirian age.||||||07-NOV-08
15334|Plum Tree Creek Volcanics|43187|5|Briefly described|p2|||||||||
15334|Plum Tree Creek Volcanics|43718|5|Briefly described|p99|||||||||
15334|Plum Tree Creek Volcanics|43720|6|Mentioned|Appendix,p6|||||||||
15334|Plum Tree Creek Volcanics|43832|4|Described|25,Table6 p22.||Paleoproterozoic|||||||07-NOV-08
15334|Plum Tree Creek Volcanics|46658|6|Mentioned|p558|||||||||
15334|Plum Tree Creek Volcanics|46678|6|Mentioned|p9|||Mount Evelyn, N.T., Sheet D.53/5. BMR 1:250,000 Geol.Ser.Explan.Notes. Different to Table 1 entry of Plum Tree Volcanics.||||||
15334|Plum Tree Creek Volcanics|47049|5|Briefly described|Table|||Elevation to formation from member status. See also. Fig.3.||||||
15334|Plum Tree Creek Volcanics|49744|5|Briefly described|Fig.3|||||||||
15334|Plum Tree Creek Volcanics|50545|5|Briefly described|p115||Paleoproterozoic|Underlies Kombolgie Subgroup.||||||07-NOV-08
15334|Plum Tree Creek Volcanics|50586|5|Briefly described|p1.1, 4.5, 5.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Of the Jim Jim Suite/Edith River Group. Age: 1858-1825 +/- 43Ma (U-Pb).||||||07-NOV-08
15334|Plum Tree Creek Volcanics|60680|5|Briefly described|Map legend|Orosirian|Orosirian|Of the Edith River Group (Jim Jim Suite).  Massive, reddish-brown, porphyritic rhyodacitic ignimbrite, glassy pink rhyolite, flow-banded ignimbrite, green-grey amygdaloidal basaltic andesite, crystal tuff.  Age: 1822Ma. Underlies Mamadawerre Sandstone.||||||23-NOV-06
15334|Plum Tree Creek Volcanics|62375|5|Briefly described|p22|Paleoproterozoic|Paleoproterozoic|Of the Edith River Group. Unconformably underlies Kombolgie Subgroup. Geological Province: Pine Creek Orogen.||||||09-FEB-10
15334|Plum Tree Creek Volcanics|63866|5|Briefly described|p110|Orosirian|Orosirian|Central Domain, Pine Creek Orogen. Age is interpreted as the age of igneous crystallisation.|1825 +/- 4 Ma (Page, OZCHRON)|||Overlies the Edith River Group.||
15334|Plum Tree Creek Volcanics|64698|4|Described|lithinterp table|Orosirian|Orosirian|Of Edith River Group. Age 1825Ma SHRIMP U/Pb. Max thick. 900m. Massive porphyritic rhyodacitic ignimbrite, glassy rhyolite, flow-banded ignimbrite, amygdaloidal basaltic andesite, crystal tuff; minor lenses of qtz sandst and pebbly lithic qtz sandst.||||||
15334|Plum Tree Creek Volcanics|64730|5|Briefly described|p125 Fig. 3, p126, p142|Paleoproterozoic|Paleoproterozoic|Age is of extrusion/crystallisation. Caps Edith River Group.|1825 +/- 4 Ma SHRIMP zircon (Page 1996).|Of Edith River Group.|||Extensive ignimbrite sheet.|02-MAY-12
15334|Plum Tree Creek Volcanics|64748|4|Described|p275, p276 Fig.9, p278|Orosirian|Orosirian|1822 Ma; in the Pine Creek Orogen||||||
15334|Plum Tree Creek Volcanics|65232|5|Briefly described|p45, p44 Fig. 29, App. 2|Orosirian|Orosirian|Of Edith River Group. Age: 1822 +/- 6 Ma (SHRIMP U-Pb zircon). Ignimbrite and minor basalt.||||||09-FEB-10
15334|Plum Tree Creek Volcanics|65339|6|Mentioned|p5 Fig.4. ||||||||Felsic volcanic rocks.|
15334|Plum Tree Creek Volcanics|67027|6|Mentioned|p350.|Paleoproterozoic|Paleoproterozoic|Said to include the previously termed Edith River Volcanics.|c.1.88 Ga.|||||
15334|Plum Tree Creek Volcanics|67057|5|Briefly described|p454. |Paleoproterozoic|Paleoproterozoic||1822 +/- 5 Ma (Sweet et al. 1999a).|||Is overlain by Katherine River Group.||
15334|Plum Tree Creek Volcanics|67564|3|Fully described|p7 Table 2, p25, p28, pp30-31, p86.|Orosirian|Orosirian|900 m of subaerial felsic ignimbrite and mafic volcanic rocks, comagmatic with David Suite plutons; and minor braided fluviatile sediments. Includes rocks in the Turnoff Creek area, mapped as Big Sunday Formation by Stuart-Smith et al. (1988b); as well as 'Dinner Creek Volcanics' (BMR 1955), Plum Tree Creek Volcanic Member, undivided Edith River Volcanics and Grace Creek Granite (Walpole 1963). Is mineralogically and geochemically similar to Grace Creek Granite; the contact is gradational. Records the last volcanic episode in the Pine Creek Orogen; represents an extrusive event of the felsic Cullen Igneous Event.|1825 +/- 4 Ma (SHRIMP U - Pb zircon).|Unit in Edith River Group.||Overlies Kurrundie Sandstone; unconformably overlies South Alligator and Finniss River Groups. Intruded by Grace Creek Granite, Lewin Springs Syenite. Unconformably overlain by Mamadawerre Sandstone.|Massive, porphyritic rhyodacitic ignimbrite, glassy rhyolite, amygdaloidal andesite; minor lenses of pebbly quartz sandstone.|
15334|Plum Tree Creek Volcanics|67779|5|Briefly described|p6 Fig.5, p30.|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen.|1825 +/- 4 Ma (Page 1996a).|Topmost unit in Edith River Group.||||
15334|Plum Tree Creek Volcanics|69420|4|Described|p5:4, 7, 14-15, 17, 79|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen. South Alligator region. c.900m thick. Subaerial (volcanic rocks); minor braided fluviatile (sedimentary rocks). Compositionally similar, and geographically related, to Grace Creek Granite; shown as a unit in Jim Jim Suite. Another age is 1822 +/- 6 Ma (Kruse et al., 1994); both SHRIMP zircon extrusion age. Two more determinations are given.|1825 +/- 4 Ma (Page, 1996).|Edith River Group.||Conformably overlies Kurrundie, Phillips Creek and Hindrance Creek Sandstones and Maud Dolerite.|Massive, porphyritic rhyodacitic ignimbrite, glassy rhyolite, interbedded amygdaloidal basalt and andesite; minor clastic lenses of pebbly quartz sandstone, volcaniclastic pebble conglomerate, micaceous sandy siltstone and tuffaceous siltstone.|12-JUL-16
15334|Plum Tree Creek Volcanics|70293|5|Briefly described|p598-599, p601, p612-613, p615|Orosirian|Orosirian|Abbreviated to Plum Creek Volcanics on p598.|1825 +/- 4 Ma (U-Pb zircon: Page, 1997).|Edith River Group||Unconformably overlies Kurrundie Sandstone. Is unconformably overlain by Mamadawerre Sandstone. Is intruded by Malone Creek Granite.|Felsic and minor mafic volcanic rocks with lenses of quartz sandstone.|
15334|Plum Tree Creek Volcanics|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|1825+/-4 Ma (crystallisation: U-Pb zircon SHRIMP)||||Ignimbrite.|
15384|Point Wakefield beds|23410|5|Briefly described|Map Legend|Cambrian|Cambrian|Brown and white claystone, red to white micaceous sandstone, red-brown and white micaceous siltstone and claystone; minor local conglomerate; fossiliferous. Geol. Prov: Wiso Basin.||||||01-NOV-05
15384|Point Wakefield beds|23733|6|Mentioned|p22|||||||||
15384|Point Wakefield beds|36335|6|Mentioned|Map legend|Late Cambrian|Middle Cambrian|Middle Cambrian(Templetonian) to Late Cambrian.||||||
15384|Point Wakefield beds|45148|6|Mentioned|p2|||Formerly part of Winnecke Creek Tableland formation.||||||
15384|Point Wakefield beds|45155|6|Mentioned|Fig.8|||||||||
15384|Point Wakefield beds|45168|6|Mentioned|p6|||||||||
15384|Point Wakefield beds|50353|5|Briefly described|Map Legend|Late Templetonian-Floran|Late Templetonian-Floran|Brown and white claystone, red to white micaceous sandstone, red-brown and white micaceous siltstone and claystone; minor conglomerate; fossiliferous.||||||
15384|Point Wakefield beds|60684|2|Defined|p50 Appendix, p17||Late Templetonian-Floran|Formerly included in Chewings' (1931) Winnecke Creek Tablelands formation and in Merrina Beds (Milligan et al 1966). Brown/white calcareous claystone + interbedded well-sorted sandstone/ laminated claystone, with silicified linked bulbous stromatolites...||||||28-APR-05
15384|Point Wakefield beds|64068|6|Mentioned|p225|||Wiso Basin. Correlated with Narpa Group.||||||
15384|Point Wakefield beds|64443|6|Mentioned|p40.|||Of Wiso Basin. Correlative of Barkly Group, Georgina Basin.||||||
15384|Point Wakefield beds|65345|5|Briefly described|p6 Fig.5. |Middle Cambrian|Middle Cambrian|Wiso Basin.||||Unconformably overlies Lothari Hill Sandstone.||
15384|Point Wakefield beds|69437|5|Briefly described|p22:10-11|Series 3|Series 3|Wiso Basin, Centralian B Superbasin. Sequence 2. Shallow-marine deposits.||||Overlies Lothari Hill Sandstone. Equivalent to (lower) Wonarah Formation.|Fine-grained siliciclastic rocks.|12-JUL-16
15384|Point Wakefield beds|69439|6|Mentioned|p24:10|||Wiso Basin.||||Correlated with the Bloodwood Formation (Ngalia Basin).||12-JUL-16
15384|Point Wakefield beds|69443|6|Mentioned|p28:21|||Wiso Basin.||||Correlated with Barkly Group.||12-JUL-16
15384|Point Wakefield beds|69446|6|Mentioned|p31:4|||Wiso Basin.||||||12-JUL-16
15384|Point Wakefield beds|69447|4|Described|p32:2-3, 5, 9|Middle Cambrian|Middle Cambrian|Wiso Basin. Shallow marine to ?fluviatile deposits. Over 41.1m thick. Typically poorly exposed as rubble-strewn slopes and small scarps. Contains late Templetonian to Floran age trilobites which also occur in the Wonarah Formation (Georgina Basin). Broadly correlated with Anthony Lagoon and Wonarah Formations (Georgina Basin), Jinduckin Formation (Daly Basin) and Eagle Hawk Sandstone (Ord Basin). May have potential for hydrocarbon reservoirs (in vuggy dolostone) or seals (interbedded claystone).||||Unconformably overlies Lothari Hill Sandstone, Hooker Creek Formation and Montejinni Limestone. Is overlain gradationally or unconformably [!] by Hanson River beds.|White and brown, locally calcareous claystone, ?overlain by interbedded claystone and sandstone; fossiliferous (trilobites, brachiopods, sponge spicules, stromatolites); cross-beds in sandstone.|12-JUL-16
15384|Point Wakefield beds|69673|6|Mentioned|p143, p145|Cambrian|Cambrian|Informal name. Up to 41m thick.|||||Calcareous claystone, vuggy dolostone, sandstone and laminated claystone.|
15384|Point Wakefield beds|70380|6|Mentioned|p745|Stage 5|Stage 5|Wiso Basin.||||||
15384|Point Wakefield beds|73083|6|Mentioned|p25, p38, p49|||Wiso Basin.|||||Siliciclastics.|
15400|Police Creek Siltstone Member|30534|2|Defined|p305|Carpentarian|Carpentarian|||||||
15400|Police Creek Siltstone Member|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
15400|Police Creek Siltstone Member|39622|6|Mentioned|Fig.2|||||||||
15400|Police Creek Siltstone Member|42676|5|Briefly described|Fig.2, P41|||||||||
15400|Police Creek Siltstone Member|45166|5|Briefly described|p16|||||||||
15400|Police Creek Siltstone Member|67323|5|Briefly described|GIS attrib tbl.|Paleoproterozoic|Paleoproterozoic|Leichhardt Superbasin.||Myally Subgroup.|||Siltstone, phyllite, rhyolitic tuff|
15411|Pollock Hills Formation|24197|5|Briefly described|p141, p143|||Comagmatic felsic volcanics with Mount Webb Granite. See also the misspelt Polloch Hills Formation. See p143, p146 for lithological detail.||||||07-FEB-11
15411|Pollock Hills Formation|29806|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
15411|Pollock Hills Formation|29807|4|Described|Table 1|||||||||
15411|Pollock Hills Formation|35201|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
15411|Pollock Hills Formation|35223|4|Described|Table.2|||||||||
15411|Pollock Hills Formation|36532|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
15411|Pollock Hills Formation|37299|6|Mentioned|Fig.1|||||||||
15411|Pollock Hills Formation|39887|6|Mentioned|p452|||||||||
15411|Pollock Hills Formation|39888|6|Mentioned|Fig.9|||||||||
15411|Pollock Hills Formation|42504|5|Briefly described|Table 3 P60|||||||||
15411|Pollock Hills Formation|44194|4|Described|p3|Proterozoic|Proterozoic|Felsic volcanics co-magmatic with Mount Webb Granite. SHRIMP dating done but no satisfactory igneous crystallisation age obtained.||||||
15411|Pollock Hills Formation|45140|2|Defined|p12-13, p26, p28-34, p36-38, p60, p74|Calymmian|Calymmian|See also Appx.p14-15. New name: Blake (1977). Arunta Block. Named after the Pollock Hills, in which is the type section, from 22deg 50'S, 127deg 40'E to 22deg 49'S, 127deg 38'E. Over 1000m thick. Lithologies detailed. A preferred age given is 1526 +/- 25 Ma (Page et al., 1976). Geochemistry detailed.|1510+/-240 Ma (Rb-Sr whole-rock: Page et al.1976)|||Unconformably overlies Arunta Complex. Is intruded by (and probably co-magmatic with) Mount Webb Granite. Is overlain unconformably by Heavitree Quartzite.|Unmetamorphosed acid lavas and associated sedimentary rocks. At the type section, porphyritic acid lava (unknown thickness) is overlain by 600m of interbedded, medium- to thin-bedded lithic arenite, sublithic arenite and tuffaceous sandstone.|
15411|Pollock Hills Formation|46788|4|Described|p6|||||||||
15411|Pollock Hills Formation|50369|5|Briefly described|p1.5, 21.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Mount Webb Suite. Age: ignimbrite 1643 +/- 13, Ma, SHRIMP, 1478 +/- 240Ma Rb/Sr.||||||28-SEP-12
15411|Pollock Hills Formation|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Dacite, rhyodacite, and volcaniclastic sedimentary rock.||||||09-DEC-08
15411|Pollock Hills Formation|65074|4|Described|p349-350, p352-353, p354 Tb.4-11, p360|Mesoproterozoic|Mesoproterozoic|See also p362. Of SW Birrindudu Basin. Type locality is in the Pollock Hills: details given. 1-1.5 km thick. Lava units are probably comagmatic with Mount Webb Granite. Whole-rock Rb-Sr dating of acid lavas. An Rb-Sr isochron age is also given of 1526 +/- 25 Ma.|1510 +/- 240 Ma (Page et al., 1976).|||Intruded by Mount Webb Granite. Is overlain unconformably by Heavitree Quartzite.|Dacitic lavas and tuffs, arenite, tuffaceous sandstone, conglomerate, lapilli tuff, agglomerate.|
15411|Pollock Hills Formation|68994|4|Described|p1, p4-11, p16, p23-27|Statherian|Statherian|Warumpi Province. Magmatic crytallisation age of dacite. Detrital zircon U-Pb ages listed and Hf analyses detailed (Wingate et al. 2012). Volcanic age based on single youngest zircon analysis, 1643+/-13 Ma (Wyborn et al. 1998).|1677+/-6 Ma.|||Is overlain unconformably by Kiwirrkurra Formation.|Consists mainly of altered, black porphyritic metadacite and metarhyodacite, overlain by volcaniclastic sedimentary rocks.|13-JAN-17
15411|Pollock Hills Formation|69003|5|Briefly described|p5, p32|Paleoproterozoic|Paleoproterozoic|West Arunta Orogen.|c.1670 Ma.|||Overlies Ininti Granite.|Volcaniclastic rocks.|
15411|Pollock Hills Formation|69031|5|Briefly described|p4, p7-8, p15|Statherian|Statherian|Warumpi Province, Arunta Orogen. Previously thought to be coeval with Mount Webb Granite; geochronology establishes a c.30 m.y. separation. Source of sediment for Kiwirrkura Formation. Magnetic susceptibility data.|c.1670 Ma (U-Pb zircon: Wingate, 2012).|||Is intruded by Ininti Granite.|Includes chert, tuff, lavas including rhyodacite.|
15411|Pollock Hills Formation|70762|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Warumpi Province, Arunta Orogen, North Australian Craton.|||||Metadacite, metarhyodacite, and volcaniclastic metasedimentary rock.|
15411|Pollock Hills Formation|70826|6|Mentioned|p10|Paleoproterozoic|Paleoproterozoic|||||||
15411|Pollock Hills Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, ash tuff, agglomerate, sandstone|
15411|Pollock Hills Formation|71592|5|Briefly described|Appendix A.|||Arunta Orogen.|||||Ignimbrite.|
15411|Pollock Hills Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Warumpi Province, Arunta Orogen.|1677+/-6 Ma||||Metadacite, metarhyodacite, and volcaniclastic metasedimentary rock.|
15428|Poodyea Formation|22954|6|Mentioned|Fig3p9|||||||||
15428|Poodyea Formation|24442|6|Mentioned|p49|Cenozoic|Cenozoic|Fluviatile deposits.||||||
15428|Poodyea Formation|38832|2|Defined|p160|Tertiary|Tertiary|||||||
15428|Poodyea Formation|39495|6|Mentioned|p142|||||||||
15428|Poodyea Formation|39921|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
15428|Poodyea Formation|49027|4|Described|p22|||||||||
15428|Poodyea Formation|60122|5|Briefly described|p36|Cenozoic|Cenozoic|Cobble and boulder conglomerate, pebbly sandstone.  Unconformable on Nora Formation, Carlo Sandstone, Mithaka Formation and Ethabuka Sandstone. Max. thickness: 10m. Geol.Prov: Georgina Basin. See also p4-5, p10 Tb. 1.||||||19-NOV-08
15428|Poodyea Formation|60590|5|Briefly described|Map legend|Cenozoic|Cenozoic|Cobble and boulder conglomerate, pebbly sandstone.||||||19-NOV-08
15428|Poodyea Formation|61155|5|Briefly described|p16|Early Miocene|Early Miocene|Overlain by Mount Coley Sinter. Age: 21-17Ma. Thickness: 6m. Geological Province: Georgina Basin.||||||
15428|Poodyea Formation|61404|5|Briefly described|Map legend|Neogene||Cobble and boulder conglomerate, pebbly sandstone.  Geological Province: southern Georgina Basin.||||||
15428|Poodyea Formation|63450|5|Briefly described|p78 Fig. 5|Tertiary|Tertiary|Geological province: Georgina Basin, West Toko Syncline.||||||07-FEB-11
15428|Poodyea Formation|64068|3|Fully described|p79,p42, p ix|Miocene|Miocene|Proposed Radke (1983). Overlies Georgina Basin rocks. Formerly included in Cravens Peak beds (Reynolds in Smith 1965), Mithaka Formation, Carlo Sandstone (Smith 1965, and others).||||Unconformably overlies Cravens Peak beds, Ethabuka and Carlo Sandstones, Mithaka and Nora Formations.|Cobble and boulder conglomerate, pebbly sandstone. Fluviatile channel deposits.|04-APR-12
15428|Poodyea Formation|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Neogene|Paleogene|Age: Tertiary.|||||Boulder conglomerate, cross-stratified sandy conglomerate and pebbly sandstone.|
15428|Poodyea Formation|67870|6|Mentioned|p43|Cenozoic|Cenozoic|Georgina Basin.||||||
15428|Poodyea Formation|68553|6|Mentioned|Map legend|Neogene|Paleogene|This unit, as well as Elliott and Mueller Formations; Austral Downs, Horse Creek and Noranside Limestones; Mount Coley Sinter, Pomona beds and unnamed sedimentary units, are all mapped under the symbol, Tm.||||||
15428|Poodyea Formation|69458|5|Briefly described|p42:20|Neogene|Paleogene|Toko Syncline. Overlies SE Georgina Basin. 10m thick. Fluvial channel deposits. Pre-Quaternary Cenozoic age is likely; is overlain by Quaternary cover.||||Unconformably overlies Nora, Mithaka Formations; Carlo, Ethabuka Sandstones; Cravens Peak beds.|Sinuous outcrops of cobble and boulder conglomerate, cross-stratified conglomerate and pebbly sandstone. Some clasts are of the Carlo Sandstone.|14-SEP-18
15428|Poodyea Formation|69591|6|Mentioned|p96|||(Some?) rocks of this unit, along the Toomba Range SW of Boulia, were originally mapped as Cravens Peak beds.||||||
15428|Poodyea Formation|69599|5|Briefly described|p580, p584, p600|Miocene|Miocene|Radke et al. (1983). Straddles the QLD-NT border: occupies a series of small, discontinuous, linear outcrops in, and to the W and SW of, the Toko Range. Up to 10m thick. High-energy fluvial deposits. Age control is poor. RELATED UNITS (continued): Also correlated (at least partly) with Horse Creek, Noranside, Austral Downs Limestones.||||Unconformably overlies Nora and Mithaka Formations and Carlo and Ethabuka Sandstones. Correlated with Whitula and Doonbara Formations; Mount Coley Sinter; see COMMENTS for more.|Locally derived conglomerate and pebbly sandstone.|
15442|Poolowanna Formation|12597|5|Briefly described|p498-499, p501|||NW Eromanga Basin. 200m thick. Appears as Poolawanna Formation on p501.||||Grades laterally into, and is overlain by, Algebuckina Sandstone. Is conformably overlain by Hutton Sandstone.|Mainly fluvial sequence of interbedded fine-grained sub-labile sandstone, siltstone and mudstone, with minor coal seams generally <0.5m thick.|
15442|Poolowanna Formation|13497|5|Briefly described|p89, p104, p112, p114|Early Jurassic|Early Jurassic|Eromanga Basin. Deposited in a high-sinuosity fluvial, overbank or lacustrine environment. Oil and gas reservoir. See also p115 fig 6.33, p119, p130, p138 fig 8.17, p141, p149-p151, p153,  p167, p170, p216.||||Overlies the Patchawarra Formation. Unconformably overlies the Tinchoo Formation. Disconformably overlain by the Cuddapan Formation.  Overlain by the Hutton Sandstone.|Sandstones, siltstone, shale and minor coal.|
15442|Poolowanna Formation|13516|6|Mentioned|p167 fig 10, p171 fig 12, p172|Middle Jurassic|Early Jurassic|In Eromanga Basin.||||||
15442|Poolowanna Formation|22839|6|Mentioned|P33|||||||||
15442|Poolowanna Formation|22883|5|Briefly described|P31, Fig2||Early Jurassic|Overlying unit is Algebuckina Sandstone||||||
15442|Poolowanna Formation|23054|6|Mentioned|Fig5p22|Aalenian|Sinemurian|||||||
15442|Poolowanna Formation|23154|5|Briefly described|Map Legend|Early Jurassic|Early Jurassic|Geological Province - Eromanga Basin.||||||
15442|Poolowanna Formation|23155|4|Described|p25|Early Jurassic|Early Jurassic|Early Jurassic in age from palynological evidence. Unit contains coal seams (<1m typically) and has carbonised plant fossils preserved on bedding surfaces.  On STRZELECKI the unit is overlain by Hutton Sandstone (conformity).||||||16-SEP-08
15442|Poolowanna Formation|23375|4|Described|Fig2 p265|Aalenian|Sinemurian|In the Eromanga Basin.||||||17-JAN-08
15442|Poolowanna Formation|23982|5|Briefly described|p58 Fig.18|||Geological Province: Eromanga Basin.||||||
15442|Poolowanna Formation|24092|5|Briefly described|p8 Fig.3|||Geological Province: Eromanga Basin.||||||
15442|Poolowanna Formation|24204|5|Briefly described|p266, 263 Fig.4, p266 Fig.7|Early Jurassic|Early Jurassic|Overlain unconformably by Algebuckina Formation. Geological Province: Eromanga Basin.||||||
15442|Poolowanna Formation|24210|5|Briefly described|p132, p133 Fig. 2|Middle Jurassic|Early Jurassic|Comprises fluvial sandstones, interbedded with shales and discontinuous, thin coals. Geological Province: Eromanga Basin.||||||16-SEP-08
15442|Poolowanna Formation|24372|6|Mentioned|p21|||Geological Province: Cooper Basin.||||||
15442|Poolowanna Formation|24482|5|Briefly described|p44|||Geological Province: Eromanga Basin.||||||
15442|Poolowanna Formation|37776|6|Mentioned|Fig.2|||||||||
15442|Poolowanna Formation|40670|6|Mentioned|Fig.9|||||||||
15442|Poolowanna Formation|40926|6|Mentioned|Table 2|||||||||
15442|Poolowanna Formation|41060|6|Mentioned|p2|||See also Fig.5||||||
15442|Poolowanna Formation|41061|6|Mentioned|p20|||||||||
15442|Poolowanna Formation|41063|2|Defined|p46|Middle Jurassic|Early Jurassic|||||||
15442|Poolowanna Formation|41084|5|Briefly described|Fig.2|||||||||
15442|Poolowanna Formation|41175|6|Mentioned|Fig.1|||||||||
15442|Poolowanna Formation|41176|6|Mentioned|Table 2|||||||||
15442|Poolowanna Formation|41183|6|Mentioned|p310|||||||||
15442|Poolowanna Formation|41187|6|Mentioned|Fig.2|||||||||
15442|Poolowanna Formation|41216|6|Mentioned|p300|||||||||
15442|Poolowanna Formation|41724|6|Mentioned|p381|||||||||
15442|Poolowanna Formation|42008|5|Briefly described|p266|||||||||
15442|Poolowanna Formation|42357|6|Mentioned|p11|||||||||
15442|Poolowanna Formation|42463|6|Mentioned|Fig.4 P171|||||||||
15442|Poolowanna Formation|42520|5|Briefly described|p6|||||||||
15442|Poolowanna Formation|42746|4|Described|p10|||See also Fig.6.||||||17-JAN-08
15442|Poolowanna Formation|43052|5|Briefly described|Table 2.1|||||||||
15442|Poolowanna Formation|43628|6|Mentioned|Fig.3|Early Jurassic|Early Jurassic|||||||
15442|Poolowanna Formation|44133|4|Described|p105|Jurassic|Early Jurassic|Previously known as 'Cuttapirie beds', 'basal Hutton', and 'basal Jurassic'. Maximum Thickness in type section 206m. Intertongues with and is overlain by the Algebuckina Sandstone and Hutton Sandstone.||||||17-JAN-08
15442|Poolowanna Formation|60386|6|Mentioned|p299|Early Jurassic|Early Jurassic|Cooper/Eromanga Basin. Non-marine.||||||
15442|Poolowanna Formation|60717|5|Briefly described|p40 Fig. 2, p42|Middle Jurassic|Early Jurassic|Unconformity at base, over the Cuddapan Formation. Overlain by Hutton Sandstone. Geological Province: Eromanga Basin.||||||31-JAN-08
15442|Poolowanna Formation|61015|6|Mentioned|p44, p45|Early Jurassic|Early Jurassic|||||||19-APR-05
15442|Poolowanna Formation|61613|6|Mentioned|p282 Fig. 2|Middle Jurassic|Early Jurassic|Geological Province: Eromanga Basin.||||||07-FEB-11
15442|Poolowanna Formation|61614|6|Mentioned|p289, p297, p290 Fig. 2|Early Jurassic|Early Jurassic|Geological Province: Eromanga Basin. Contain coals and shales.||||||17-MAR-09
15442|Poolowanna Formation|61615|5|Briefly described|p302, p302 Fig. 2, p305, p306, p307|Middle Jurassic|Jurassic|Geological Province: Eromanga Basin. Comprises fluvial sandstones interbedded with shales and discontinuous, thin coals.||||||09-MAY-13
15442|Poolowanna Formation|62046|5|Briefly described|p125 Fig. 2|Jurassic|Jurassic|Geological Province: Cooper-Eromanga Basins.||||||14-APR-08
15442|Poolowanna Formation|62376|5|Briefly described|p84|Middle Jurassic|Late Triassic|Geological Province: Pedirka Basin.||||||09-FEB-10
15442|Poolowanna Formation|62537|6|Mentioned|p191 Fig.2, p192.|Middle Jurassic|Early Jurassic|Eromanga Basin. Significant hydrocarbon source potential.||||Is overlain by Hutton and Algebuckina Sandstones.||
15442|Poolowanna Formation|62730|5|Briefly described|p352 Fig. 1|Early Jurassic|Early Jurassic|Geological Province: Eromanga Basin.||||||14-APR-08
15442|Poolowanna Formation|63979|2|Defined|p32, Fig. 44|Toarcian|Pleinsbachian|Supersedes "Poolowanna beds". Unconformable on Cuddapan Fm; conformable below Hutton Sandstone. Max.thick: 165m.Comprises lower dominantly sandstone subunit + upper dominantly mudstone subunit - more lithology available.Geol. Prov.Eromanga Basin.||||||07-FEB-11
15442|Poolowanna Formation|64048|5|Briefly described|p64 Tb. 2, p69|||Geological Province: Eromanga Basin. Possesses hydrocarbon source potential.||||||07-FEB-11
15442|Poolowanna Formation|64197|6|Mentioned|p625 Fig.1c|Early Jurassic|Early Jurassic|Overlies the Nappamerri Unconformity.||||Underlies the Hutton Sandstone.||
15442|Poolowanna Formation|64232|5|Briefly described|p12|Jurassic|Jurassic|Geological Province: Eromanga Basin. Coal occurs in deeper parts of the basin in this unit.||||||24-JUL-08
15442|Poolowanna Formation|64665|5|Briefly described|p53 Fig.2, p61.|Early Jurassic|Early Jurassic|Eromanga Basin. Lateral equivalent of Precipice Sandstone and Evergreen Formation in the Surat Basin. Hosts thin (to 0.5 m thick) uneconomic coal seams.||||Is overlain by Hutton Sandstone.||
15442|Poolowanna Formation|64778|6|Mentioned|p13, 21, 28|Jurassic|Jurassic|Pedirka and Simpson Desert Basins. Appears as Poolawanna Formation on p13.  Potential hydrocarbon source.||||Is overlain by Algebuckina Formation.||
15442|Poolowanna Formation|65238|5|Briefly described|p3, p7 Fig. 8|Jurassic|Jurassic|Overlies Purni Formation. Geological province: Eromanga Basin. Meandering and anastomosing fluvial-floodplain deposits. See also p10, p14 Fig. 17.||||||16-FEB-10
15442|Poolowanna Formation|65385|5|Briefly described|pS134 Fig.7|Early Jurassic|Early Jurassic|Of Eromanga Basin. Overlain by Hutton Sandstone.||||||08-MAR-12
15442|Poolowanna Formation|65489|5|Briefly described|p15, p24, p26, p45, p47,p49, p53, p55-62|Early Jurassic|Early Jurassic|See also p91, p96, p137, p151-152, p154-160. Eromanga Basin. 130-290m thick. Hydrocarbon source rock. Stratigraphic and structural trapping of Permian generated oil. Gas and oil reservoir accounting for 6.3% and 5% respectively of the Basin's production. Intraformational shale seal.||||Overlies Cuddapan Formation unconformably. Is overlain by Algebuckina Sandstone.|Includes meandering fluvial sandstones and organic-rich shales.|
15442|Poolowanna Formation|65925|5|Briefly described|Appendix 2.||||||||White to pale grey, fine- to medium-grained, crossbedded sandstone, ripple cross laminated; dark grey siltstone; shale; coal seams and breccias.|
15442|Poolowanna Formation|66529|6|Mentioned|p12 Fig.5|||Eromanga Basin.||||Unconformably overlies Nappamerri Group. Is overlain by Algebuckina Sandstone and Hutton Sandstone.||
15442|Poolowanna Formation|66915|5|Briefly described|p6 Fig.3|Early Jurassic|Early Jurassic|Eromanga Basin.||||||
15442|Poolowanna Formation|67323|5|Briefly described|p87-88, p95 Fig.12.5|Early Jurassic|Early Jurassic|Eromanga/Galilee Basins. Hydrocarbon exploration target in the Eromanga Basin.||||Is overlain by Hutton Sandstone.||
15442|Poolowanna Formation|67402|6|Mentioned|p114 fig ERO13, p117|||Seel also the Poolowanna Formation, Lower and Poolowanna Formation, Upper.||||||
15442|Poolowanna Formation|68731|6|Mentioned|p208, pp209-211|Jurassic|Jurassic|See also Poolawanna Formation.||||Unconformably overlies Tinchoo Formation (Nappamerri Group).||17-JUL-14
15442|Poolowanna Formation|69001|6|Mentioned|p16|Early Cretaceous|Jurassic|Recent interpretations by the NSW DPI broadly group this unit within the Algebuckina Sandstone and equivalent units.||||||
15442|Poolowanna Formation|69019|5|Briefly described|p85 Fig.21.|Early Jurassic|Early Jurassic|Southern Eromanga Basin.||||Is overlain by Algebuckina and Hutton Sandstones.||
15442|Poolowanna Formation|69023|6|Mentioned|p86, p89 Fig.20, p90|Middle Jurassic|Early Jurassic|||||||
15442|Poolowanna Formation|69454|5|Briefly described|p38:3, 7 Fig.38.6; 38:12-13, 14 Fig.38.9|Early Jurassic|Early Jurassic|Eromanga Basin. Sandstones have fair to good reservoir potential, sealed by intra-formational shales.||||Unconformably overlies Peera Peera Formation. Is overlain by Algebuckina Sandstone.||12-JUL-16
15442|Poolowanna Formation|69457|4|Described|p41:2-4; 41:5 Fig.41.4; 41:15-17|Early Jurassic|Early Jurassic|Moore (1986); formerly Poolowanna beds of Wiltshire (1978). Eromanga Basin; entirely subsurface. 205m thick; thins to the W. Fluvial and lacustrine deposits. Pliensbachian-Toarcian age. The coal is black, dull and shaly and the thin (0.5m thick) seams are uneconomic. Contains confirmed oil source rocks with TOCs up to 15%. Thermal maturity, prospects and leads discussed in some detail. Lacustrine shales might form a regional seal. Contains the deepest reservoir units in the Eromanga Basin succession.||||Unconformably overlies Cuddapan Formation. Is overlain conformably by/intertongues with Hutton Sandstone and Algebuckina Sandstone. Lateral equivalent of Precipice Sandstone and Evergreen Formation.|Sandstone, siltstone and coaly shale, arranged in two upward-fining cycles. Thin discontinuous coal seams.|12-JUL-16
15442|Poolowanna Formation|69582|6|Mentioned|p65|Early Jurassic|Early Jurassic|Eromanga Basin.||||Overlain by the Hutton Sandstone.||
15442|Poolowanna Formation|69594|4|Described|p519, p524, p526, p531-532, p535, p545|Early Jurassic|Early Jurassic|See also p572. Eromanga Basin. Originally defined in the Poolowanna Trough in SA (Wiltshire, 1978; Moore, 1986); the type section is in DIO Poolowanna 1. Maximum thickness is 165m. Represents cyclic fluvio-lacustrine deposition. Palynofloras in QLD are Pliensbachian-Toarcian and are generally correlated with those of upper Precipice Sandstone-Evergreen Formation. Is a minor hydrocarbon reservoir; has hydrocarbon source potential. RELATED UNITS (continued): Passes laterally into Precipice Sandstone. Equivalent to Evergreen Formation.||||Unconformably overlies Cuddapan, Tinchoo, Toolachee and Patchawarra Formations. Is overlain conformably by Hutton Sandstone (and intertongues with it) and Algebuckina Sandstone. See COMMENTS for more.||
15442|Poolowanna Formation|69633|6|Mentioned|p14|||Eromanga Basin.||||||
15442|Poolowanna Formation|69673|5|Briefly described|p154, p154 fig 126, p159, p160, p161|Jurassic|Jurassic|Up to 205m thick. Confirmed oil source rock.||||Unconformably (or disconformably) overlain by Algebuckina Sandstone, Hutton Sandstone, overlies Walkandi Formation, unconformably overlies Peera Peera Formation|Interbedded sandstone that fines upwards into coaly shale and siltstone.|
15442|Poolowanna Formation|69790|6|Mentioned|p1063 Fig.2|Early Jurassic|Early Jurassic|Eromanga Basin.||||||
15442|Poolowanna Formation|69797|5|Briefly described|p17 incl Fig.2|Middle Jurassic|Early Jurassic|The best petroleum source rocks in Jurassic-Cretaceous sequence of Eromanga Basin are the highly carbonaceous shales of Poolowanna Formation, the coals and carbonaceous shales of Birkhead Formation, and organic-rich shales and siltstones of Murta Formation. Age approximated from figure. Geol. Prov: Eromanga Basin.||||||17-JAN-17
15442|Poolowanna Formation|69946|3|Fully described|p10-11, p51, p57-60, p74-82|Middle Jurassic|Early Jurassic|Eromanga Basin. Moore (1986); formerly Poolowanna beds (Wiltshire, 1978). Type section remains that of Wiltshire (1978), viz. the interval 2387 - 2593m in Poolowanna 1; not the interval 2422-2476m in Cuttapirrie 1 which has also been called Poolowanna Formation and 'Cuttapirrie beds' in SA. Up to 205m thick. Wireline log correlations.||||Intertongues with, and is overlain by, Algebuckina and Hutton Sandstones.|Interbedded grey to brown carbonaceous siltstone; pale grey to buff, very fine- to medium-grained sandstone; rare coal seams.|
15442|Poolowanna Formation|69947|5|Briefly described|p3-5, p13 Fig.7.2, p16-21 Figs.7.5-10|Early Jurassic|Early Jurassic|See also p23 Fig.7.12. Eromanga Basin. First deposits above the basal Eromanga Basin unconformity. Amalgamated channel sands and infilled palaeovalleys; no laterally extensive sand sheets. Facies described in some detail.||||Unconformably overlies Cuddapan Formation. Is overlain by Hutton Sandstone.|Sandstone, minor shale and thin coal seams.|
15442|Poolowanna Formation|69948|6|Mentioned|Fig.4.18|||Eromanga Basin.||||Unconformably overlies Peera Peera and Purni Formations. Is overlain by Algebuckina Sandstone.||
15442|Poolowanna Formation|69982|6|Mentioned|p49-50|Early Jurassic|Early Jurassic|The Sturt 7 oil well was re-perforated in this unit after extracting Mooracoochie Volcanics oil, extending production by almost one-half.||||||
15442|Poolowanna Formation|70823|4|Described|p25-p27, p43-p44, p78|Early Jurassic|Early Jurassic|Eromanga Basin. Deposited in a meandering-anastomosing fluvial or lacustrine or overbank environments. Up to 130m thick. This unit forms a source rock that hosts an oil and gas discovery.||||Unconformably overlies the Cuddapan Formation. Overlain by the Hutton Sandstone.|Sandstone, siltstone, shale and coal.|
15442|Poolowanna Formation|70824|5|Briefly described|p9|Jurassic|Jurassic|Eromanga Basin.||||Overlies the Cuddapan Formation. Overlain by the Hutton Sandstone.||
15442|Poolowanna Formation|71321|6|Mentioned|p15|||Of Eromanga Basin.||||Overlies the Peera Peera Formation. Overlain by the Algebuckina Sandstone.||24-OCT-19
15442|Poolowanna Formation|71342|3|Fully described|Ch 1 p3, Ch4 p25,  Ch5 p10-p12, Ch5 p30|Aalenian|Hettangian|Eromanga Basin. Source of significant production of gas in the Eromanga Basin. Originally the Poolowanna beds of Wiltshire (1978) before being raised to formation status by Moore (1986). This unit has also been previously referred to as the 'basal Hutton Sandstone', 'Cuttapirrie beds' (in South Australia or as the 'basal Jurassic' (in Queensland). A type section is mentioned in Poolowanna 1. Petrography is discussed in some detail. Spore-pollen zone is given in Ch5 p57. Reaches a maximum thickness of 205m in Poolowanna 1. Interpreted to have been deposited in fluvial channels meandering across a floodplain with minor coal swamps. Sequence stratigraphy discussed in detail (Ch7) as is source rock potential and hydrocarbon geochemistry (Ch8). See also Ch5 p51, Ch5 p57-p59, Ch5 p74, Ch6 p5-p6, Ch7 p3-p5, Ch7 p10, Ch7 p13, Ch7 p16-p17, Ch7 p20, Ch8 p2, Ch8 p8, Ch8 p10-p11, Ch9 p5, Ch9 p11, Ch9 p18, Ch10 p3, Ch10 tbl 10.1, Ch10 p6, Ch10 p14, Ch10 p17, Ch11 p2, Ch11 p7-p8, Ch11 p13, Ch12 p2p3, Ch12 tbl 12.1, Ch12 p6, Ch12 p9, Ch12 p11-p14, Ch13 p3, Ch13 p8, Ch14 p2-p7.||||Unconformably overlies the Peera Peera and Cuddapan Formations. Overlain by the Algebuckina and Hutton sandstones.|Interbedded carbonaceous siltstone, sandstone and rare coal seams. Sandstones range from very fine to medium grained and contain minor pebbles and granules of quartzite and reworked basement.|
15442|Poolowanna Formation|71805|5|Briefly described|p75-p76|Toarcian|Pleinsbachian|Eromanga Basin. This unit is temporally equivalent to the Precipice Sandstone.||||Overlain by the Hutton Sandstone.||16-MAY-19
15442|Poolowanna Formation|71863|5|Briefly described|p4|||Eromanga Basin. Potential petroleum source (although the majority is derived from the underlying Cooper Basin units).||||||
15442|Poolowanna Formation|72297|5|Briefly described|p739, p742-743|||Eromanga Basin. Petroleum reservoir, with source rock potential.||||||
15442|Poolowanna Formation|72298|5|Briefly described|p801|Jurassic|Jurassic|Eromanga Basin (SA,QLD).||||Unconformably overlies Nappamerri Group. Is overlain by Algebuckina, Hutton Sandstones.||
15442|Poolowanna Formation|72476|6|Mentioned|p36 Fig.9, p37|||Eromanga Basin. Time-temperature thermal history diagram. Only <1 km thickness preserved.||||||
15442|Poolowanna Formation|73167|6|Mentioned|p664 Fig. 2|Jurassic|Jurassic|Eromanga Basin. Contains oil.||||||
15442|Poolowanna Formation|73249|6|Mentioned|p319|Cretaceous|Jurassic|Eromanga Basin.||||||
15442|Poolowanna Formation|73251|6|Mentioned|p49, p55-56, p62|Early Jurassic|Early Jurassic|Eromanga Basin. Meandering-anastomosing fluvial depositional setting. Hydrocarbon source rock that contains[?] gas and oil.||||Overlain by Hutton Sandstone.||
15442|Poolowanna Formation|73281|6|Mentioned|p1, Appendix (DIP)|Early Jurassic|Early Jurassic|Eromanga Basin. Petroleum source rocks. See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx. Also written as Poolowanna Formation, lower.||||||
15442|Poolowanna Formation|73343|6|Mentioned|p337|Jurassic|Jurassic|Eromanga Basin. Hosts oil.||||Overlain by Hutton Sandstone.||
15442|Poolowanna Formation|73479|5|Briefly described|p156 Fig.2, p159, p179|Jurassic|Jurassic|Eromanga Basin. Fluvial depositional environment.|ca 200-180 Ma|||Unconformably overlies Cuddapan Formation, underlies Hutton Sandstone||
15573|Prices Creek Group|7433|5|Briefly described|p25 Fig.2, p28 Fig.5, p29. |Ordovician|Ordovician|Canning Basin. Marine carbonates.||||Grades laterally into Carranya beds.|Shallow marine, fine clastic and carbonate deposits.|
15573|Prices Creek Group|22741|5|Briefly described|P21, Table3 P18||Ordovician|||||||
15573|Prices Creek Group|23903|5|Briefly described|p1597 Fig.2|Ordovician|Ordovician|Geological Province: Canning Basin.||||||27-NOV-06
15573|Prices Creek Group|30983|4|Described|p73|||||||||
15573|Prices Creek Group|31870|6|Mentioned|p8|||||||||
15573|Prices Creek Group|32648|6|Mentioned|p32|||Camb.-Ord.||||||
15573|Prices Creek Group|32979|6|Mentioned|p38|||Correlation with basins in India.||||||
15573|Prices Creek Group|35104|6|Mentioned|Fig.2|||||||||
15573|Prices Creek Group|35119|4|Described|p460|||See also p448.||||||27-NOV-06
15573|Prices Creek Group|36225|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
15573|Prices Creek Group|36890|6|Mentioned|p321|||||||||
15573|Prices Creek Group|38878|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
15573|Prices Creek Group|40136|5|Briefly described|p37|||||||||
15573|Prices Creek Group|40810|5|Briefly described|p14|||||||||
15573|Prices Creek Group|41854|6|Mentioned|p94|||||||||
15573|Prices Creek Group|41894|6|Mentioned|p2|||||||||
15573|Prices Creek Group|43563|6|Mentioned|p4|Early Ordovician|Early Ordovician|(E.Ord-M.Ord)||||||
15573|Prices Creek Group|43803|6|Mentioned|p65||Ordovician|||||||
15573|Prices Creek Group|43818|6|Mentioned|Fig.2.p39||Early Ordovician|||||||
15573|Prices Creek Group|43819|6|Mentioned|p31||Arenig|||||||
15573|Prices Creek Group|43876|14|Not recorded|p553||Ordian|||||||
15573|Prices Creek Group|44143|6|Mentioned|p.426, p441 Tb. 4-19|Ordovician|Ordovician|Lennard Shelf. Includes Gap Creek and Emanuel Formations. Shallow marine carbonates and siliciclastics. Correlated with Nambeet and Willara Formations.||||||
15573|Prices Creek Group|44309|14|Not recorded|p12|||Fauna correlated with Coolibah Formation.||||||
15573|Prices Creek Group|44397|14|Not recorded|p.12|||||||||
15573|Prices Creek Group|44403|6|Mentioned|p.8||Ordovician|||||||
15573|Prices Creek Group|44404|14|Not recorded|map legend||Ordovician|||||||
15573|Prices Creek Group|44998|2|Defined|p18, map.|||||||||
15573|Prices Creek Group|45153|6|Mentioned|App.1-14|||||||||
15573|Prices Creek Group|45158|3|Fully described|p28|||||||||
15573|Prices Creek Group|48826|14|Not recorded|Tb.III|||||||||
15573|Prices Creek Group|48874|14|Not recorded|p.3|||||||||
15573|Prices Creek Group|63938|4|Described|p48, p52 Fig.4|Middle Ordovician|Early Ordovician|Unconformably overlain by Cadjebut Formation in the Emanuel Range.||||||10-NOV-08
15573|Prices Creek Group|64334|5|Briefly described|p39-40|Ordovician|Ordovician|Eastern Lennard Shelf, Canning Basin. Tremadoc-Arenig.|||Gap Creek, Emanuel Formations; Kudata Dolomite; Kunian Sandstone.|Correlates with Nambeet and Willara Formations.||
15573|Prices Creek Group|64502|5|Briefly described|p765 Fig.2, p768 Fig.5|Ordovician||||||||
15573|Prices Creek Group|64580|4|Described|map legend|Middle Ordovician|Early Ordovician|Siltstone, shale, limestone, and dolomitic sandstone; includes KUNIAN SANDSTONE, KUDATA DOLOMITE, EMANUEL and GAP CREEK FORMATIONS.||||||09-DEC-08
15573|Prices Creek Group|64643|4|Described|p3 Fig. 2, p33, 37|Middle Ordovician|Lower Ordovician|||||||
15573|Prices Creek Group|65301|5|Briefly described|p5 Fig. 4|Middle Ordovician|Early Ordovician|Geological province: Canning Basin.||||||
15573|Prices Creek Group|65449|6|Mentioned|p6|Middle Ordovician|Early Ordovician|||||||
15573|Prices Creek Group|65486|5|Briefly described|p6-7,9,17; Figs.5,67,19; Plate 1.|Ordovician|Ordovician|Dolomite, shale, and siltstone, Canning Basin. Unconformably underlies Pillara Limestone, Cadjebut Formation, Carolyn Formation (Grant Group).||||||
15573|Prices Creek Group|66127|5|Briefly described|pp19-21, p24, p68, Plates 4,5,7,8.|Middle Ordovician|Early Ordovician|Unconformably overlies Proterozoic rocks.|||Includes Emanuel and Gap Creek Formations.|Unconformably underlies Cadjebut Formation.|Dolomite, shale and siltstone.|
15573|Prices Creek Group|68007|6|Mentioned|p4|Ordovician|Ordovician|Canning Basin.||||||
15573|Prices Creek Group|68902|6|Mentioned|p9 fig 5|Ordovician|Ordovician||||Includes Carranya Formation|||
15573|Prices Creek Group|69099|4|Described|500k_geologyp08_lut.csv|Middle Ordovician|Early Ordovician||||Includes Kunian Sandstone, Kudata Dolomite, Emanuel and Gap Creek Formations||Siltstone, shale, limestone, and dolomitic sandstone.|04-AUG-15
15573|Prices Creek Group|69165|4|Described|500k_geologyp08_lut.csv|Ordovician|Ordovician||||Includes Kunian Sandstone, Kudata Dolomite, Emanuel Formation, Gap Creek Formation||Undivided; siltstone, shale, limestone and dolomitic sandstone|
15573|Prices Creek Group|69182|6|Mentioned|Ch4 p9-p12, Ch4 p40-p41|||Canning Basin. See also Ch4 p45,Ch4 p47, Ch4 p50-p58, Ch4 p74, Ch4 p79-p82, Ch4 p92, Ch4 p94.||||||
15573|Prices Creek Group|69883|5|Briefly described|p4-p5|Arenig|Tremadocian|Canning Basin. Conodont zones and supersequences provided.|||Includes the Kunian Sandstone, Kudata Dolomite, Emanuel Formation and Gap Creek Formation.|||
15573|Prices Creek Group|70154|5|Briefly described|500k_interpgeop14_lut.csv|Middle Ordovician|Lower Ordovician||458-485 Ma||||Siltstone, shale, limestone, and dolomitic sandstone|
15573|Prices Creek Group|70774|5|Briefly described|p4|Middle Ordovician|Early Ordovician|Fitzroy Trough and Lennard Shelf, Canning Basin.||||||06-FEB-20
15573|Prices Creek Group|70826|6|Mentioned|p7 tbl 3|Silurian|Ordovician|Canning Basin.||||||
15573|Prices Creek Group|71146|6|Mentioned|p24, p26|||Canning Basin.|||Includes the Kudata Dolomite and the Kunian Sandstone.|||
15573|Prices Creek Group|71171|5|Briefly described|p1-p2, p4|||Canning Basin.|||Includes the Kunian Sandstone, Carranya Formation, Kudata Dolomite, Emanuel Formation, Gap Creek Formation, Nambeet Formation and Willara Formation.|||
15573|Prices Creek Group|71267|4|Described|GEOL_LUT_CSV files|Middle Ordovician|Early Ordovician|Of Canning Basin. Events: Point Moody Extension (300-242 Ma); Red Bluffs Extension (372.2-360 Ma); Van Emmerick Extension (382.7-372.2 Ma); Samphire Marsh Extension (485-480 Ma). See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv.|485.4-458.4 Ma (bistrat)||Includes Emanuel Formation, Gap Creek Formation.||Siltstone, shale, limestone, and dolomitic sandstone|
15573|Prices Creek Group|71870|5|Briefly described|p5|||Canning Basin.||||Equivalent to the Nambeet Formation.||
15573|Prices Creek Group|71894|5|Briefly described|p4|Lower Ordovician|Lower Ordovician|Canning Basin.||||Overlies the Carranya Formation.|Cabonate and shale.|
15573|Prices Creek Group|72034|5|Briefly described|500k_interpgeop16_lut|Middle Ordovician|Early Ordovician|Canning Basin.  Age from biostratigraphy.|||||Siltstone, shale, limestone, and dolomitic sandstone.|
15573|Prices Creek Group|72499|5|Briefly described|p7 Fig.6.|Middle Ordovician|Early Ordovician|Located in the Fitzroy Trough.||||Overlies Carranya Formation.|Includes carbonate shales.|
15573|Prices Creek Group|72503|6|Mentioned|p26|||Canning Basin. Crops out along the Lennard Shelf.||||||
15573|Prices Creek Group|73117|5|Briefly described|p3|Lower Ordovician|Lower Ordovician|Canning Basin. Lower boundary marked by a major unconformity[?] [related to the Samphire Marsh Movement?].||||Unconformably overlain by[?] Carranya Formation.|Dominantly carbonate-shale, marl.|
15573|Prices Creek Group|73344|5|Briefly described|p2-4, p6, p41, p50-51, p53, p56, p62-65|Middle Ordovician|Early Ordovician|Canning Basin, Lennard Shelf. Known from the subsurface and outcrops. Part of supersequence A.|||Gap Creek Formation, Emanuel Formation, Kudata Dolomite, Kunian Sandstone|Equivalent to Nambeet Formation and Willara Formation.||07-DEC-22
15573|Prices Creek Group|73346|6|Mentioned|p1-3|Ordovician|Ordovician|Canning Basin, Lennard Shelf. Outcrops in the Emanuel Range as a small inlier.||||||
15573|Prices Creek Group|73567|6|Mentioned|p62|Ordovician|Ordovician|Canning Basin, Lennard Shelf.|||Emanuel Formation, Gap Creek Formation|Equivalent to the Nambeet and Willara formations.||
15576|Prices Springs Granite|24197|5|Briefly described|p106 Tb. 15.1|Paleoproterozoic|Paleoproterozoic|Of the Cullen Supersuite. Age: ~1825Ma. Geological Province: Pine Creek Inlier.||||||07-FEB-11
15576|Prices Springs Granite|24260|6|Mentioned|p1013 Fig.1|||Geological Province: Pine Creek Inlier.||||||27-NOV-06
15576|Prices Springs Granite|31435|6|Mentioned|p61|||||||||
15576|Prices Springs Granite|35140|6|Mentioned|p321|||||||||
15576|Prices Springs Granite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
15576|Prices Springs Granite|40168|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Pink-green or grey coarse equigranular to porphyritic granite.||||||07-NOV-08
15576|Prices Springs Granite|40223|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Coarse even-grained to porphyritic granite.||||||07-NOV-08
15576|Prices Springs Granite|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
15576|Prices Springs Granite|41309|4|Described|p9|||||||||
15576|Prices Springs Granite|41311|6|Mentioned|p17|||||||||
15576|Prices Springs Granite|41465|6|Mentioned|p8|||||||||
15576|Prices Springs Granite|42756|6|Mentioned|Fig.5 P6|||||||||
15576|Prices Springs Granite|42927|5|Briefly described|p428|||see also Fig.2 p430.||||||27-NOV-06
15576|Prices Springs Granite|43140|3|Fully described|p37||Paleoproterozoic|Of the Cullen Batholith. U-Pb age 1780 Ma.||||||07-NOV-08
15576|Prices Springs Granite|43624|6|Mentioned|p14|||||||||
15576|Prices Springs Granite|43832|4|Described|41,46,49,53,55,65||Paleoproterozoic|Age 1804+-50 Ma; less accurate 1780-1790 Ma (p53).||||||07-NOV-08
15576|Prices Springs Granite|45003|14|Not recorded|p52|||||||||
15576|Prices Springs Granite|45022|3|Fully described|p.140.||Carpentarian|On many pages. Pet Desc.on Tech.File D/52-8||||||27-NOV-06
15576|Prices Springs Granite|46658|6|Mentioned|p559|||||||||
15576|Prices Springs Granite|46676|14|Not recorded|p.9|||||||||
15576|Prices Springs Granite|50586|5|Briefly described|p1.1, 4.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Of the Cullen Supersuite. Age: 1804 +/- 50Ma (U-Pb).||||||07-NOV-08
15576|Prices Springs Granite|63866|5|Briefly described|p110|Orosirian|Orosirian|Central Domain, Pine Creek Orogen.|1804 +/- 50 Ma (ID-TIMS)|Cullen Supersuite||||
15576|Prices Springs Granite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1820-1850Ma. Of Cullen Supersuite.  I-type. Coarse biotite-hornblende granite, fine biotite granite. Intrudes South Alligator Group, Burrell Creek Formation.||||||07-JAN-09
15576|Prices Springs Granite|67564|6|Mentioned|p33 Fig.19.|Paleoproterozoic|Paleoproterozoic|Pluton within Cullen Batholith, Pine Creek Orogen.||||||
15576|Prices Springs Granite|69420|5|Briefly described|p5:17-18, 20|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Granite-dominated plutons; mineralogy and petrology/geochemistry summarised.|1804 +/- 50 Ma conventional U-Pb zircon (TIMS).|Margaret Suite.|||Medium- to coarse-grained porphyritic granite. I-type.|12-JUL-16
15576|Prices Springs Granite|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.|1804 +/- 50 Ma.||||Light grey, coarse-grained biotite-hornblende granite; fine- to medium-grained biotite granite.|
15576|Prices Springs Granite|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|1804+/-50 Ma (crystallisation: U-Pb).||||Granite.|
15604|Prion Formation|5952|5|Briefly described|p214 Fig. 4, p215 Fig. 5, p228|Eocene|Eocene|Pattillo and Nicholls (1990). In figure, Fm = Formation. Geological Province: Bonaparte Basin.||||||01-MAR-10
15604|Prion Formation|7142|6|Mentioned|p350 Fig.4.|Neogene|Paleogene|Browse Basin.||||Overlies Bassett Formation. Is overlain by Cartier Formation.||
15604|Prion Formation|13353|6|Mentioned|p401 Fig.2.|Paleogene|Paleogene|||||Overlies Bassett Formation. Is overlain by Cartier Formation.||
15604|Prion Formation|13354|6|Mentioned|p375 Fig.6.|Neogene|Palaeogene|Unit of Woodbine Group. Overlies Bassett Formation and underlies Cartier Formation.||83||||28-OCT-14
15604|Prion Formation|22663|5|Briefly described|AC97 1-4 Fig.4|Oligocene|Eocene|Of the Woodbine Group.||||||01-MAR-10
15604|Prion Formation|23378|6|Mentioned|p180 Fig.2||Eocene|Of the Woodbine Group. In the Vulcan Sub-basin.||||||27-NOV-06
15604|Prion Formation|24171|5|Briefly described|p722 Fig. 3|Tertiary|Tertiary|Geological Province: Vulcan Sub-Basin.||||||20-SEP-14
15604|Prion Formation|24218|5|Briefly described|p850|Eocene|Eocene|Geological Province: Bonaparte Basin.||||||
15604|Prion Formation|42053|5|Briefly described|Fig.2 P29|||||||||01-MAR-10
15604|Prion Formation|42066|5|Briefly described|Fig.3 P199|||||||||
15604|Prion Formation|60634|6|Mentioned|p1168 Fig.3. |Oligocene|Eocene|||Unit in Woodbine Group.||Overlies Hibernia Formation. Is overlain by Oliver Formation.||
15604|Prion Formation|61548|6|Mentioned|p480 Fig.3|Eocene|Eocene|Northern Bonaparte Basin.||||||
15604|Prion Formation|61550|6|Mentioned|p495 Fig.2. |Eocene|Eocene|||Unit in Woodbine Group.||Overlies Hibernia Formation.||
15604|Prion Formation|62837|5|Briefly described|Stratigraphic columns|Oligocene|Eocene|Age: ~41-~33Ma. Geological Province: Western Bonaparte Basin and Northern Bonaparte Basin.||||||01-MAR-10
15604|Prion Formation|63358|5|Briefly described|p4 Fig. 1.3|Oligocene|Eocene|||||||01-MAR-10
15604|Prion Formation|64695|5|Briefly described|p260, p262|Eocene|Eocene|Northern Bonaparte Basin.||||Overlies Hibernia Formation. Is overlain unconformably by Oliver Formation.||
15604|Prion Formation|66187|5|Briefly described|p413 Fig.2|Eocene||Unit in the Woodbine Group. Underlies the Oliver Formation unconformably; overlies the Hibernia Formation. Mount Ashmore Dome.||||||
15604|Prion Formation|68223|6|Mentioned|p178 Fig.3, p179 Fig.4|Eocene|Eocene|||||||
15604|Prion Formation|69452|5|Briefly described|p36:15, 22|Paleogene|Paleogene|Bonaparte Basin.||Woodbine Group.||||12-JUL-16
15604|Prion Formation|69673|6|Mentioned|p174|||||||||
15604|Prion Formation|70061|5|Briefly described|Regional geology; Figs.6-7|Eocene|Eocene|See also Sahul: Fig.2. Vulcan: Fig.2.||Woodbine Group.||Overlies Hibernia Formation. Is overlain by Cartier Formation.||12-JUL-16
15646|Puffin Formation|5952|5|Briefly described|p215 Fig. 5, p223|Late Cretaceous|Late Cretaceous|Appears as Puffin in figure. Geological Province: Bonaparte Basin.||||||01-MAR-10
15646|Puffin Formation|7142|6|Mentioned|p350 Fig.4.|Late Cretaceous|Late Cretaceous|Browse Basin.||||Is overlain by Bassett Formation.||
15646|Puffin Formation|13194|4|Described|p383 Tb. 4-16, p396 fig 4-60|Cretaceous|Cretaceous|Type section Grebe 1 well (2098-2630m). Up to 570m thick. Oil reservoir on Ashmore Platform.||Bathurst Island Group||Overlies Vee Formation (conformably but diachronous). Grades into Turnstone Formation and Brown Gannet Limestone.|Sandstone interbedded with lesser shale and marl. Petroleum.|
15646|Puffin Formation|13353|6|Mentioned|p401 Fig.2.|Late Cretaceous|Late Cretaceous|||||Is overlain by Bassett Formation.||
15646|Puffin Formation|13354|6|Mentioned|p375 Fig.6.|Late Cretaceous|Late Cretaceous|Unit of Bathurst Island Group. Overlies Fenelon and Gibson Formations, and underlies Bassett Formation of the Woodbine Group.||125||||28-OCT-14
15646|Puffin Formation|22663|5|Briefly described|AC97 1-4 Fig.4||Late Cretaceous|Of the Bathurst Island Group.||||||01-MAR-10
15646|Puffin Formation|23377|6|Mentioned|p211|||In the Vulcan Sub-basin.||||||27-NOV-06
15646|Puffin Formation|23378|5|Briefly described|p180 Fig.2||Cretaceous|Of the Bathurst Island Group. In the Vulcan Sub-basin.||||||01-MAR-10
15646|Puffin Formation|24171|5|Briefly described|p722 Fig. 3|Cretaceous|Cretaceous|Geological Province : Vulcan Sub-Basin.||||||01-MAR-10
15646|Puffin Formation|24207|6|Mentioned|p210 Fig. 6|||Referred to as Puffin only in Figure 6.||||||
15646|Puffin Formation|41459|6|Mentioned|Fig.2|||Reserved as Puffin.||||||27-NOV-06
15646|Puffin Formation|41532|2|Defined|p308|Late Cretaceous||||||||
15646|Puffin Formation|41731|6|Mentioned|Fig.3|||||||||
15646|Puffin Formation|42053|4|Described|p45|||See also Fig. 2 p29.||||||01-MAR-10
15646|Puffin Formation|42066|5|Briefly described|Fig.3 P199|||||||||
15646|Puffin Formation|42442|3|Fully described|p29|Danian|Campanian|Age: Late Cretaceous to early Paleocene. Type section in Grebe 1 between 2125 and 2630 m. Restricted to eastern Ashmore Platform and Vulcan Sub-basin. Max thickness 570 m.|||||lenticular sandstones interbedded with shale|01-NOV-12
15646|Puffin Formation|42861|6|Mentioned|p4|||||||||
15646|Puffin Formation|43661|6|Mentioned|Fig.3|||||||||
15646|Puffin Formation|43699|6|Mentioned|Fig.6,p10||Late Cretaceous|||||||
15646|Puffin Formation|43739|6|Mentioned|Fig.5,p38|||||||||
15646|Puffin Formation|43826|6|Mentioned|Fig.2,p163||Late Cretaceous|||||||01-MAR-10
15646|Puffin Formation|49637|5|Briefly described|Fig.3|Late Cretaceous|Late Cretaceous|Of the Bathurst Island Group. Geological Province: Ashmore Platform / Vulcan Sub-basin.||||||07-FEB-11
15646|Puffin Formation|60378|5|Briefly described|p95, fig 2, p96, 98, 106|Late Cretaceous|Late Cretaceous|Includes interpreted deep marine fan sediments considered to be a reservoir facies.|||||Includes sandstone.|
15646|Puffin Formation|60634|6|Mentioned|p1167 Fig.2,  p1168 Fig.3.|Late Cretaceous|Late Cretaceous|||Unit in Bathurst Island Group.||Overlies Jamieson and Fenelon Formations. Is overlain by Johnson Formation.||
15646|Puffin Formation|61550|6|Mentioned|p495 Fig.2. |Late Cretaceous|Late Cretaceous|||Unit in Bathurst Island Group.||Overlies Fenelon Formation. Is overlain by Johnson Formation.||
15646|Puffin Formation|62837|5|Briefly described|Stratigraphic columns|Paleocene|Late Cretaceous|Age: ~80-65Ma. Geological Province: Arafura and Money Shoals Basin.||||||01-MAR-10
15646|Puffin Formation|63358|5|Briefly described|p4 Fig. 1.3|Masstrichtian|Campanian|See also p133 Fig. 3.71.||||||01-MAR-10
15646|Puffin Formation|64697|5|Briefly described|p84 Fig.2, p88 |Late Cretaceous|Late Cretaceous|||||||
15646|Puffin Formation|66187|5|Briefly described|p413 Fig.2, p414 Tb.1|Maastrichtian|Maastrichtian|Bathurst Island Group. Underlies the Johnson Formation, overlies the Fenelon Formation. Mount Ashmore Dome. Interbedded deep-water marine sandstone and claystone.||||||
15646|Puffin Formation|69297|6|Mentioned|p305|Maastrichtian|Campanian|Caswell, Barcoo and Seringapatam Sub-basins of the Browse Basin.||Bathurst Island Group||Overlies the Fenelon Formation. Overlain by the Bassett Formation.||
15646|Puffin Formation|70061|5|Briefly described|Regional geology; Figs.6-7, p6, p12|Maastrichtian|Campanian|See also Vulcan: Fig.2, p2. Productive petroleum reservoir. Regionally-developed sandstones form high-quality reservoirs; commonly sealed by Johnson Formation carbonates. Potential gas reservoir in Vulcan Sub-basin.||Bathurst Island Group.||Overlies Wangarlu Formation. Is overlain by Johnson Formation. Correlates with Turnstone Formation.|Lowstand fan sandstones.|12-JUL-16
15646|Puffin Formation|70064|5|Briefly described|Regional Fig. 6; p6. Central: Fig.2; p2|Maastrichtian|Campanian|See also Northern: Fig.2: p1, p3. Yampi: Fig.2. Browse Basin. Gas show in Abalone 1 and Abalone Deep 1 wells. Potential reservoirs in horsts and tilted fault-blocks in submarine fan sandstones. Potential intraformational seals.||Bathurst Island Group.||Overlies Fenelon Formation. Is overlain by Johnson Formation.||12-JUL-16
15650|Pul Pul Rhyolite|9534|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Rhyolite, ignimbrite.||||||07-NOV-08
15650|Pul Pul Rhyolite|9691|5|Briefly described|Map Legend|||Of the Edith River Group. Rhyolite, ignimbrite.||||||
15650|Pul Pul Rhyolite|9701|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Edith River Group. Rhyolite, ignimbrite.||||||02-JUN-05
15650|Pul Pul Rhyolite|22429|4|Described|P23|Orosirian|Orosirian|Age of unit is 1828.6+/-5.1 Ma.||||||27-NOV-06
15650|Pul Pul Rhyolite|23363|5|Briefly described|344 Fig.3|||||||||
15650|Pul Pul Rhyolite|23384|6|Mentioned|Fig 27|||Of Needham and Stuart-Smith (1985).||||||
15650|Pul Pul Rhyolite|23733|5|Briefly described|p32 Fig. 19|||Of the Coronation Sandstone (El Sherana Group).||||||
15650|Pul Pul Rhyolite|23867|5|Briefly described|Fig. 3|||Of El Sherana Group.  Formerly Pul Pul Rhyolite Member (Edith River Volcanics).  Geological Province: McArthur Basin.||||||
15650|Pul Pul Rhyolite|24050|5|Briefly described|p11 Tb. 3|Orosirian|Orosirian|Ignimbrite.  Age: 1828+/-5m.y. (SHRIMP U-Pb zircon).||||||
15650|Pul Pul Rhyolite|24197|5|Briefly described|p105 Tb. 15.1|Paleoproterozoic|Paleoproterozoic|Of the El Sherana Suite. Age: ~1865Ma. Geological Province: Pine Creek Inlier.||||||07-FEB-11
15650|Pul Pul Rhyolite|24340|5|Briefly described|p147 Fig. 4|||Overlain by the Gimbat Ignimbrite Member. Geological Province: Pine Creek Inlier.||||||27-NOV-06
15650|Pul Pul Rhyolite|34528|6|Mentioned|p18|||Upper Proterozoic. See also pp19,20.||||||27-NOV-06
15650|Pul Pul Rhyolite|38349|6|Mentioned|p14|||||||||
15650|Pul Pul Rhyolite|39357|4|Described|p14|||||||||
15650|Pul Pul Rhyolite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
15650|Pul Pul Rhyolite|40248|4|Described|p222|||||||||
15650|Pul Pul Rhyolite|40823|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
15650|Pul Pul Rhyolite|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
15650|Pul Pul Rhyolite|41125|6|Mentioned|Fig.15|||||||||
15650|Pul Pul Rhyolite|41311|4|Described|p13|||||||||
15650|Pul Pul Rhyolite|41397|4|Described|p15|||||||||
15650|Pul Pul Rhyolite|41407|6|Mentioned|Map legend|Proterozoic||||||||
15650|Pul Pul Rhyolite|41594|6|Mentioned|p20|||||||||
15650|Pul Pul Rhyolite|42324|4|Described|p4-5|||||||||
15650|Pul Pul Rhyolite|43140|4|Described|p3||Paleoproterozoic|Of the El Sherana Group.||||||07-NOV-08
15650|Pul Pul Rhyolite|43187|5|Briefly described|p2|||||||||
15650|Pul Pul Rhyolite|43718|6|Mentioned|p2|||||||||
15650|Pul Pul Rhyolite|43720|5|Briefly described|p12|||||||||
15650|Pul Pul Rhyolite|43832|4|Described|21-23, Table6 p22||Paleoproterozoic|Age ~1870 Ma.||||||07-NOV-08
15650|Pul Pul Rhyolite|46163|14|Not recorded|p171|||Radioactive member of Edith River Volcanics.  Contains traces of Uranium.||||||27-NOV-06
15650|Pul Pul Rhyolite|46658|6|Mentioned|p556|||||||||
15650|Pul Pul Rhyolite|47049|5|Briefly described|Table|||Elevation to formation from member status; redefined.||||||
15650|Pul Pul Rhyolite|49744|5|Briefly described|Fig.3|||||||||
15650|Pul Pul Rhyolite|50586|5|Briefly described|p1.1, 6.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Of the El Sherana Suite.||||||07-NOV-08
15650|Pul Pul Rhyolite|60680|5|Briefly described|Map legend|Orosirian|Orosirian|Of the El Sherana Group (Jim Jim Suite).  Age: 1829Ma. Of the Edith River Group.  Purple to pink, felsic, welded vitric ignimbrite and non-welded ignimbrite; polymictic volcaniclastic granule to boulder conglomerate, massive volcaniclastic sandstone.||||||27-NOV-06
15650|Pul Pul Rhyolite|63866|5|Briefly described|p110|Orosirian|Orosirian|Central Domain, Pine Creek Orogen. Numeric age is derived from Jagodzinski, 1998.|1829 +/- 5 Ma (crystallisation)|El Sherana Group||||
15650|Pul Pul Rhyolite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Of El Sherana Group. Age 1829Ma SHRIMP U/Pb. Max thick. 1300m. Felsic welded vitric, and non-welded ignimbrite; polymictic volcaniclast. granule to boulder conglom., volcaniclast. sandst; Massive rhyolitic porphyry and non-vesicular rhyolite intrusives.||||||
15650|Pul Pul Rhyolite|64730|5|Briefly described|p125 Fig. 3, p126, p142|Paleoproterozoic|Paleoproterozoic|Age is of extrusion/crystallisation.|1829 +/- 5 Ma SHRIMP zircon (Jagodzinski 1998).|Of El Sherana Group.|||Massive pink rhyolitic ignimbrite.|02-MAY-12
15650|Pul Pul Rhyolite|65232|6|Mentioned|p46, p44 Fig. 29, App. 2|Orosirian|Orosirian|Of El Sherana Group. Faulted against Coronation Sandstone and Koolpin Formation. Massive rhyolite, ignimbrite, quartz feldspar porphyry and basalt. Age: 1828.6 +/- 5.1 Ma (SHRIMP U-Pb).||||||09-FEB-10
15650|Pul Pul Rhyolite|67564|3|Fully described|p7 Table 2, p17 Table 3, pp27-29, p86.|Paleoproterozoic|Paleoproterozoic|Jawoyn Sub-basin. 1300 m of subaerial and intrusive volcanic rocks, comagmatic with David Suite plutons; minor fluviatile sediments. Contains rocks previously mapped as Pul Pul Rhyolite Member (Walpole et al. 1960) and Edith River Volcanics (Walpole 1963). May have had a common subaerial volcanic source as Big Sunday Formation.|1828 +/- 4 Ma (SHRIMP U - Pb zircon).|Unit in El Sherana Group.||Overlies Gerowie Tuff and Burrell Creek Formations unconformably and Coronation Sandstone disconformably. Is disconformably overlain by Big Sunday Formation.|A succession of amalgamated felsic ignimbrite and volcaniclastic rocks, with partially intrusive rhyolite porphyry and rhyolite lava.|
15650|Pul Pul Rhyolite|67779|5|Briefly described|p6 Fig.5.|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen.|1829 +/- 5 Ma (Jagodzinski 1998).|Unit in El Sherana Group.||Overlies Coronation Sandstone. Is overlain by Big Sunday Formation.||
15650|Pul Pul Rhyolite|69420|4|Described|p5:4, 7, 15, 17, 79|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen. South Alligator region. Up to 1300m thick. Subaerial and intrusive (volcanic rocks); minor fluviatile (sedimentary rocks) deposits. SHRIMP U-Pb zircon extrusion age of a rhyolite porphyry. Other (similar) ages are mentioned.|1829 +/- 5 Ma (Jagodzinski, 1998).|El Sherana Group.||Unconformably overlies Coronation Sandstone. Is overlain by Big Sunday Formation with local disconformity.|Felsic welded vitric and non-welded ignimbrite, polymictic volcaniclastic conglomerate, massive volcaniclastic sandstone, intrusive massive rhyolite porphyry; minor siltstone lenses.|12-JUL-16
15650|Pul Pul Rhyolite|70293|5|Briefly described|p597-599, p613, p615|Orosirian|Orosirian|Jawoyn Sub-basin.|1829 +/- 5 Ma (Jagodzinski, 1992, 1998).|El Sherana Group||Overlies Coronation Sandstone, overlain by Big Sunday Formation|Ignimbrite, intrusive porphyry and rhyolite.|24-FEB-17
15650|Pul Pul Rhyolite|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|1869+/-44 Ma (crystallisation: U-Pb zircon SHRIMP)||||Metasomatite.|
15661|Pungalina Member|22538|2|Defined|App1 p722||Statherian|Previously not differentiated from Masterton Sandstone.||||||23-MAR-18
15661|Pungalina Member|23395|6|Mentioned|p400|||||||||
15661|Pungalina Member|23776|5|Briefly described|p705 Fig 2.|||Of Tawallah Group.||||||
15661|Pungalina Member|32904|6|Mentioned|p91|||||||||
15661|Pungalina Member|41721|3|Fully described|p25|||Separates Masterton Formation above from Gold Creek Volcanics below (Tawallah Group). Originally included in the Masterton Sandstone (Yeates (1963) and Roberts (unpub.). Siltstone and fine sandstone.||||||01-AUG-07
15661|Pungalina Member|42385|6|Mentioned|Fig.5 P8|||||||||
15661|Pungalina Member|42812|6|Mentioned|p24|||Of the Gold Creek Volcanics.||||||27-NOV-06
15661|Pungalina Member|43010|5|Briefly described|Fig.6||Mesoproterozoic|Of the Tawallah Group. Of "Mid Proterozoic" age.||||||27-NOV-06
15661|Pungalina Member|43036|6|Mentioned|Fig.5|||||||||
15661|Pungalina Member|44436|5|Briefly described|p.9,10, opp. p.7,map|||Topmost member of Masterton Formation (Tawallah Group). (E53-4).||||||27-NOV-06
15661|Pungalina Member|44437|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Of the Masterton Formation (Tawallah Group).  Red-brown, flaggy, fine-grained sandstone and siltstone.||||||07-NOV-08
15661|Pungalina Member|45162|2|Defined|p43|Proterozoic|Proterozoic|Briefly described Table 5.||||||27-NOV-06
15661|Pungalina Member|60483|5|Briefly described|p7 Fig. 5|||Of the Warramana Sandstone. Geological Province: McArthur Basin.||||||22-FEB-08
15661|Pungalina Member|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Tawallah Group. Underlain by Gold Creek Volcanics.||||||03-JUN-09
15661|Pungalina Member|60574|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Echo Sandstone. Overlies the Gold Creek Volcanics. Intruded by the Hobblechain Rhyolite.||||||07-NOV-08
15661|Pungalina Member|63112|5|Briefly described|p1192 Tb.1, p1194, p1198, p1201, p1205|||<10 to 70 m thick.||Unit in Echo Sandstone.|||Basal, pebbly sandstones, and conglomerates overlain by interbedded lithic sandstones and mudstones.|
15661|Pungalina Member|64817|6|Mentioned|p353 Fig.4, p370  |||Interpreted as an evolving volcanic apron that records the emplacement, denudation and burial of a high-relief volcanic landscape.||Appears to be shown as unit in Warramana Sandstone.||||07-JUN-18
15661|Pungalina Member|65228|5|Briefly described|p22, Figs.02, 06, 07, 10.|||McArthur Basin. Mis-spelt as Pungalena in Fig.07.||Basal unit of Echo Sandstone.||Overlies Gold Creek Volcanics and Hobblechain Rhyolite. Correlated with Warramana Sandstone.||
15661|Pungalina Member|65337|6|Mentioned|p15.|||Southern McArthur Basin.||||||
15661|Pungalina Member|65340|3|Fully described|pp28-29, pp44-48, p66.|||An epiclastic apron adjacent to the lava front of the Hobblechain Rhyolite, formed by collapse and rapid erosion of loose talus breccia; subsequently covered by lacustrine sediments. Defined by Yates (1963) as member of now-redundant Masterton Formation; included as member of Gold Creek Volcanics by Jackson et al. (1987); assigned to Echo Sandstone and redefined by Rawlings (1999, 2002). Large-scale folds and dome-and-basin structures are interpreted to have formed by gravity sliding after intrusion by Packsaddle Microgranite.|1725 - 1720 Ma.|Unit in Echo Sandstone.|Includes Lower and Upper Members.|Overlies Gold Creek Volcanics and, locally, Hobblechain Rhyolite. Unconformably overlies Wollogorang Formation. Is overlain by undifferentiated Echo Sandstone.|Talus and alluvial conglomerate, comprising 100% rhyolite clasts, immediately adjacent to Hobblechain Rhyolite; sandstone and mudstone.|
15661|Pungalina Member|69430|4|Described|p15:3, 10, 12, 48|||[Frustratingly inconsistent treatment of this unit's parentage!] It is stated as a Member of the Echo Sandstone, but its position as shown in pages 15:3 and 15:10 clearly imply a connection with Warramana Sandstone. Southern McArthur Basin. Up to 200m thick. Alluvial and debris flows, restricted marine or lacustrine deposits.||Echo Sandstone.||Overlies Hobblechain Rhyolite conformably and Gold Creek Volcanics conformably to disconformably. Is overlain conformably by Echo Sandstone.|Cobble-boulder conglomerate, pebbly sandstone; minor siltstone, ferruginous-lithic mudstone.|13-DEC-17
15661|Pungalina Member|69673|6|Mentioned|p16 fig 13, p17 fig 14|||Coarse clastic sedimentary rock.||Appears to be shown as part of Warramana Sandstone||Overlies Gold Creek Volcanics, Hobblechain Rhyolite||07-JUN-18
15661|Pungalina Member|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the southern part of the Batten Fault zone and the Southeastern McArthur Basin.||Tawallah Group||Overlies Gold Creek Volcanics and partially underlies Nyanantu Formation and is laterally equivalent to Warramana Sandstone and Hobblechain Rhyolite.||
15661|Pungalina Member|72718|6|Mentioned|p7|||Southern McArthur Basin.||Of Warramana Sandstone?, Tawallah Group||Underlain by Gold Creek Volcanics. Overlain by and equivalent to Warramana Sandstone. Equivalent to and partly underlain by Hobblechain Rhyolite. Partly equivalent to Packsaddle Microgranite.||
15661|Pungalina Member|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.||Not clear, Tawallah Group||Overlies Gold Creek Volcanics and shown to partially underlie Nyanantu Formation and is equivalent to Warramana Sandstone and Hobblechain Rhyolite.||
15661|Pungalina Member|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin, Calvert Superbasin. (Relationship between the Echo Sandstone and Pungalina Member is not clear in Fig.1.2.)||Echo Sandstone(?), Tawallah Group||Underlain by Gold Creek Volcanics. May be equivalent to Warramana Sandstone.||
15684|Purni Formation|13516|6|Mentioned|p147, fig 5|Early Permian|Early Permian|From Pedirka Basin||||||
15684|Purni Formation|22883|6|Mentioned|P29|Early Permian|Late Carboniferous|Underlying unit is Crown Point Formation.||||||27-NOV-06
15684|Purni Formation|23982|6|Mentioned|p96 Appendix 13|||Geological Province: Great Artesian Basin.||||||
15684|Purni Formation|24204|5|Briefly described|p262, 263 Fig.4, p266 Fig.7|Early Permian|Early Permian|Geological Province: Pedirka Basin.||||||
15684|Purni Formation|30514|6|Mentioned|p100|||Permian age||||||
15684|Purni Formation|30540|6|Mentioned|p67|||Similar to Patchawarra Formation of Cooper Basin||||||
15684|Purni Formation|30544|5|Briefly described|p52|||In the Pedirka Basin.||||||27-NOV-06
15684|Purni Formation|30825|6|Mentioned|p37|||||||||
15684|Purni Formation|33523|6|Mentioned|Fig.13|||||||||
15684|Purni Formation|33525|6|Mentioned|p5|||||||||
15684|Purni Formation|33824|6|Mentioned|p7|||||||||
15684|Purni Formation|33832|5|Briefly described|p7|||Stratigraphy||||||
15684|Purni Formation|33844|3|Fully described|p36|||||||||
15684|Purni Formation|33971|4|Described|p33|||||||||
15684|Purni Formation|33976|2|Defined|p5|Permian|Permian|||||||
15684|Purni Formation|35845|6|Mentioned|Fig.25|||||||||
15684|Purni Formation|36733|6|Mentioned|p14|||||||||
15684|Purni Formation|36922|6|Mentioned|p188|||||||||
15684|Purni Formation|37065|6|Mentioned|p30|||||||||
15684|Purni Formation|37776|6|Mentioned|Fig.2|||||||||
15684|Purni Formation|37855|6|Mentioned|Fig.2|||||||||
15684|Purni Formation|37917|4|Described|p470|||||||||
15684|Purni Formation|38958|5|Briefly described|p491|||||||||
15684|Purni Formation|39265|6|Mentioned|Fig. 3|||||||||
15684|Purni Formation|40637|6|Mentioned|Fig.2|||||||||
15684|Purni Formation|40910|6|Mentioned|p14|||||||||
15684|Purni Formation|40911|6|Mentioned|Map legend|Permian|Carboniferous|||||||
15684|Purni Formation|40925|6|Mentioned|Map legend|Permian|Carboniferous|Carboniferous to Permian||||||
15684|Purni Formation|40926|3|Fully described|p13|||||||||
15684|Purni Formation|41063|6|Mentioned|p40|||||||||
15684|Purni Formation|41183|6|Mentioned|p314|||||||||
15684|Purni Formation|41270|6|Mentioned|p279|||||||||
15684|Purni Formation|41491|6|Mentioned|p180|||||||||
15684|Purni Formation|41689|6|Mentioned|Table 1|||||||||
15684|Purni Formation|42463|6|Mentioned|Fig.4 P171|||||||||
15684|Purni Formation|42504|5|Briefly described|p81|||||||||
15684|Purni Formation|42547|4|Described|p82|||||||||
15684|Purni Formation|42746|5|Briefly described|p6, Fig.2 p4|||In the Pedirka Basin.||||||27-NOV-06
15684|Purni Formation|43052|5|Briefly described|Table 2.1|||||||||
15684|Purni Formation|44133|5|Briefly described|p65 Fig. 8.3, 90|Permain|Permain|Geological Province: Pedirka Basin. Probably conformably overlies Crown Point Formation.||||||
15684|Purni Formation|61250|5|Briefly described|p43|Permian|Early Permian|Includes a glacigene sandstone at base. Important oil source rock - contains petroleum systems. Geological Province: Perdika Basin. Correlates with Patchawarra Formation and Tirrawarra Sandstone.||||||18-AUG-05
15684|Purni Formation|62376|5|Briefly described|p84|Early Permain|Early Permian|Geological Province: Pedirka Basin.||||||09-FEB-10
15684|Purni Formation|62759|5|Briefly described|p1|Early Permian|Early Permian|Important oil source rock. Geological Province: Perdika/Eromanga Basins. Correlates with Patchewarra Formation in the Cooper Basin.||||||05-FEB-08
15684|Purni Formation|64232|5|Briefly described|p12|||Geological Province: Perdika Basin. Sub-bituminous coal seams are well-developed at suitable depths for CSM exploration in Mount Hammersley area.||||||24-JUL-08
15684|Purni Formation|64778|6|Mentioned|p13, 15-21, 23, 28, 33|Permian|Permian|Pedirka Basin. Thermal history summarised. Max. palaeotemperature analysis summary. Potential hydrocarbon source rock.|285-270 Ma.|||||
15684|Purni Formation|65238|5|Briefly described|p3, p5 Fig. 6, p7 Fig. 8|Permian|Permian|Conformably overlies Crown Point Fm; overlain by Poolowanna Fm. Geol.province: Pedirka Basin. Lacustrine, meander, fluvial-swamp deposits. Lithological details of three unnamed members included on p8 - total max.thickness being 350m. See also p14 Fig. 17||||||09-APR-13
15684|Purni Formation|65489|5|Briefly described|p13, p17, p55-61, p63-64, p91, p137-139|Permian|Permian|See also p143, p151. Pedirka Basin. 350m thick. Contains very thick coal sequences, and a well, drilled for coal bed methane, has been successful (CBM93001). Fair to exellent hydrocarbon source and reservoir potential.||||Overlies Crown Point Formation. Is correlated with Patchawarra Formation (Cooper Basin).|Alternating shale, coal and siltstones of lacustrine, swamp and floodplain deposition; also point-bar and other channel-derived sands.|
15684|Purni Formation|69418|5|Briefly described|p3:34|Permian|Permian|Pedirka Basin. Contains coal seams over 30m thick, extending over 70km along strike.||||||12-JUL-16
15684|Purni Formation|69454|4|Described|p38:3-4, 6-8, 10-15|Guadalupian|Asselian|Youngs (1975). Widespread in W Pedirka Basin. 564.3m thick in Blamore-1. Four sub-units ("facies suites") are described in some detail; the authors suggest possibly elevating the Formation to Group status and defining the subdivisions as Formations (depending on further study). Glaciofluvial outwash, flood plain/overbank, fluvial and paludal depositional environments. Considered to be lateral equivalent of the Patchawarra Formation and younger Gidgealpa Group units (Cooper Basin). Hosts significant coal-bearing intervals (detailed) with potential also for coal gasification or coal-to-liquid processing, as well as fair to good petroleum source potential. Sandstones have some reservoir potential, with intra-formational shale seals, while basal shale could seal underlying Tirrawarra Sandstone reservoirs.||||Conformably overlies Tirrawarra Sandstone or Crown Point Formation. Is overlain unconformably by Walkandi, Peera Peera Formations. Lateral equivalent of Stuart Range and Mount Toondina Formations.|Sandstone (locally pyritic), siltstone, shale, carbonaceous shale, coal, minor conglomerate.|12-JUL-16
15684|Purni Formation|69457|6|Mentioned|p41:5 Fig.41.4; 41:16-17|Permian|Permian|Fair to good source rocks.||||||12-JUL-16
15684|Purni Formation|69673|5|Briefly described|p151, p152, p159, p160, p161, p162, p164|Permian|Permian|greater than 550m thick. Contains five unnamed units. Source rock potential.||||Conformably overlies Crown Point Formation, overlies Tirrawarra Sandstone, unconformably overlain by Walkandi Formation, Peera Peera Formation, Algebuckina Sandstone|Sandstone, siltstone, shale, coal and minor conglomerate.|
15684|Purni Formation|69946|4|Described|p5, p7-8, p36, p44-45, p48-51|Artinskian|Asselian|Pedirka Basin. Defined by Youngs (1975) after informal references by Jacque (1966). Type section is the interval 1417 - 1698m in Purni 1. Up to 350m thick.||||Disconformably overlies Crown Point and Mount Toondina Formations.|Basal interbeds of grey shale and fine- to medium-grained sandstone, minor conglomerate and coal stringers; cross-bedded sandstone with interbeds of siltstone, shale and minor coal; silty sandstone, carbonaceous shale interbeds, abundant coal seams.|
15684|Purni Formation|69948|6|Mentioned|Fig.4.18|||Pedirka Basin.||||Unconformably overlies Mount Toondina, Stuart Range and Crown Point Formations. Is overlain unconformably by Algebuckina Sandstone and (locally) Walkandi, Peera Peera and Poolowanna Formations.||
15684|Purni Formation|71342|4|Described|Ch4 p25, Ch5 p5, Ch5 p7-p8|Early Permian|Early Permian|Pedirka Basin. Formally defined by Youngs (1975) following informal references by Jacque (1966) in the Mokari 1 well completion report. A type section in Purni 1 is mentioned. This unit is subdivided into three members at the type section, these are described further in Ch5 p7. A maximum thickness of 350m is recorded in Mokari 1. See also  Ch5 p30, Ch5 p36, Ch5 p44-p45, Ch5 p49-p51, Ch8 p28, Ch9 p16, Ch9 p18, Ch9 p20-p21, Ch11 p6, Ch14 p5-p7.||||Disconformably overlies the Crown Point Formation. Unconformably overlies the Finke Group.|Interbedded grey shale and fine to medium-grained sandstone with minor conglomerate and coal stringers.|
15684|Purni Formation|72476|6|Mentioned|p26, p36 Fig.9|Permian|Carboniferous|Perdika Basin. Time-temperature thermal history diagram.||||||
15684|Purni Formation|73281|6|Mentioned|p1, Appendix (DIP)|Permian|Permian|Pedirka Basin. Coal-rich. Petroleum source rocks. Data included in digital information package (DIP) 034. See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx. Also written as Purni Formation, lower.||||||
15725|Quandong Conglomerate|22654|6|Mentioned|Fig 1 on p 246|||||||||
15725|Quandong Conglomerate|30238|4|Described|p65|||Cambrian age||||||
15725|Quandong Conglomerate|35102|6|Mentioned|Fig.9|||||||||
15725|Quandong Conglomerate|40810|6|Mentioned|p3|||||||||
15725|Quandong Conglomerate|40852|6|Mentioned|Fig.3.7|||||||||
15725|Quandong Conglomerate|41115|6|Mentioned|p1389|||||||||
15725|Quandong Conglomerate|44484|14|Not recorded|p.6,10, Tb.1|||Part of Pertaoorrta Group. (Cambrian). Defn on Tech.File G/53-1.||||||
15725|Quandong Conglomerate|44485|14|Not recorded|map legend||Cambrian|Part of Pertaoorrta Group.||||||
15725|Quandong Conglomerate|45041|4|Described|p52|||Cambrian. Of the Pertaoorrta Group.||||||27-NOV-06
15725|Quandong Conglomerate|48863|2|Defined|p.16|||Tb.1. opp.p.7,9,15,17,18,40,Pl.15, ?Lower Cambrian. (G53-1).||||||
15725|Quandong Conglomerate|64068|6|Mentioned|p224|||Amadeus Basin. Correlated with Shadow Group, Georgina Basin.||||||
15725|Quandong Conglomerate|69437|6|Mentioned|p22:10|Cambrian|Cambrian|Amadeus Basin.||||||12-JUL-16
15725|Quandong Conglomerate|69438|4|Described|p23:3, 24, 27|Early Cambrian|Early Cambrian|Ranford et al. (1965). Gardiner Range and James Range anticlines, central Amadeus Basin. Thickness from <20m to c.160m. Appears as Quandong Formation on 23:24.||Pertaoorrta Group.||Overlies Areyonga and Pertatataka Formations, probably unconformably. Is overlain conformably by Pertaoorrta Group. Lateral equivalent of Arumbera Sandstone.|A succession of conglomerate, conglomeratic sandstone and sandstone. Conglomerate clasts are generally 2cm but range up to 30cm, and consist mainly of chert, sandstone and quartzite.|12-JUL-16
15725|Quandong Conglomerate|69443|6|Mentioned|p28:14|||Amadeus Basin.||||Correlated with (part of) the Shadow Group.||12-JUL-16
15725|Quandong Conglomerate|71898|4|Described|iii, p1, p3, p6-p8|Late Neoproterozoic|Late Neoproterozoic|Amadeus Basin. This unit was defined by Ranford et al (1965) Outcrops on the PALM VALLEY Sheet (5440) in the core of the Walker Creek and James Range anticlines. SHRIMP age is interpeted to be a maximum depositional age supporting a late Neoproterozoic age for this unit. This unit has an estimated maximum thickness of 160m but can be less than 20m thick in places. Sample location, description at location, zircon morphology, SHRIMP analysis, results and methods are discussed.|629 +/- 18 Ma (SHRIMP U-Pb)|||Overlies the Areyonga and Pertatataka formations. Overlain by the Winnall Group.|Pebble conglomerate, conglomeratic (pebble) sandstone and medium- to coarse-grained sandstone.|
15725|Quandong Conglomerate|72369|6|Mentioned|p23|||Of Amadeus Basin.||||||
15725|Quandong Conglomerate|72374|6|Mentioned|p12|||Of Amadeus Basin.||||||
15764|Quilalar Formation|22438|4|Described|p535, Fig.3 p537|||See also Fig.10a p546. Quartz-carbonate formation.||||||27-NOV-06
15764|Quilalar Formation|22457|5|Briefly described|P31|||||||||
15764|Quilalar Formation|22498|6|Mentioned|Fig2 P235|||||||||
15764|Quilalar Formation|22585|4|Described|P739, Fig1, Fig2|||||||||
15764|Quilalar Formation|22644|5|Briefly described|5 fig 2|||Geological  province: Mt Isa Basin.||||||18-JAN-07
15764|Quilalar Formation|22665|6|Mentioned|P220||Statherian|||||||
15764|Quilalar Formation|23031|5|Briefly described|21|Paleoproterozoic|Paleoproterozoic|Geological province: Mount Isa Fold Belt. Overlain by Bigie Formation.||||||07-NOV-08
15764|Quilalar Formation|23363|5|Briefly described|351 Tab.1|Statherian|Statherian|Age: 1780+/-20Ma.||||||27-NOV-06
15764|Quilalar Formation|23393|4|Described|p18, p16 Fig. 4|Paleoproterozoic|Paleoproterozoic|Geological Province: Lawn Hill Sub-province.||||||07-NOV-08
15764|Quilalar Formation|23395|6|Mentioned|p383|||||||||
15764|Quilalar Formation|23396|5|Briefly described|p407 Fig.2|||||||||
15764|Quilalar Formation|23399|6|Mentioned|p489|||||||||
15764|Quilalar Formation|23406|5|Briefly described|p601 Fig.3|||||||||
15764|Quilalar Formation|23466|5|Briefly described|p267|||||||||
15764|Quilalar Formation|23518|4|Described|p9 Fig. 3, p11|Proterozoic|Proterozoic|Geological Province: Western Fold Belt.||||||
15764|Quilalar Formation|23767|5|Briefly described|p1954 Fig. 1a|||Geological Province: Leichhardt Superbasin.||||||02-APR-07
15764|Quilalar Formation|23965|5|Briefly described|p1297|||||||||
15764|Quilalar Formation|24308|5|Briefly described|p991, p987 Fig.2|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
15764|Quilalar Formation|24419|5|Briefly described|p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Erroneously included in the Haslingden Group?  Geological Province: Western Fold Belt, Lawn Hill Subprovince and Leichardt River Subprovince (Mount Isa Orogen).||||||07-NOV-08
15764|Quilalar Formation|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|Reserved as Quilalar.||||||27-NOV-06
15764|Quilalar Formation|36548|6|Mentioned|p517|||||||||
15764|Quilalar Formation|36937|6|Mentioned|p229|||||||||
15764|Quilalar Formation|37459|6|Mentioned|p423|||||||||
15764|Quilalar Formation|37462|4|Described|Table4.VII|||||||||
15764|Quilalar Formation|37568|5|Briefly described|p83|||See also p85.||||||27-NOV-06
15764|Quilalar Formation|38232|6|Mentioned|p81|||See also p85.||||||27-NOV-06
15764|Quilalar Formation|38235|6|Mentioned|p113|||||||||
15764|Quilalar Formation|38237|6|Mentioned|p125|||||||||
15764|Quilalar Formation|38276|6|Mentioned|Fig.1|||||||||
15764|Quilalar Formation|38348|6|Mentioned|p7|||||||||
15764|Quilalar Formation|38350|6|Mentioned|p15|||||||||
15764|Quilalar Formation|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
15764|Quilalar Formation|38560|6|Mentioned|p115|||||||||
15764|Quilalar Formation|38835|6|Mentioned|p164|||||||||
15764|Quilalar Formation|38836|6|Mentioned|p165|||||||||
15764|Quilalar Formation|38900|6|Mentioned|p55|||||||||
15764|Quilalar Formation|38919|6|Mentioned|p496|||||||||
15764|Quilalar Formation|39202|6|Mentioned|p242|||||||||
15764|Quilalar Formation|39362|6|Mentioned|p1468|||||||||
15764|Quilalar Formation|39445|5|Briefly described|Table 2|||Probably continuous with Ballara Quartzite. See also p36 and p40.||||||27-NOV-06
15764|Quilalar Formation|39556|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||
15764|Quilalar Formation|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Myally Subgroup (Haslingden Group).  Overlies the Lochness Formation.||||||15-JUN-06
15764|Quilalar Formation|39622|6|Mentioned|Fig.2|||See also Appendix||||||
15764|Quilalar Formation|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
15764|Quilalar Formation|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
15764|Quilalar Formation|39925|6|Mentioned|Fig.9|||||||||
15764|Quilalar Formation|39934|6|Mentioned|Fig.3|||||||||
15764|Quilalar Formation|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
15764|Quilalar Formation|40221|3|Fully described|p11|||||||||
15764|Quilalar Formation|40840|6|Mentioned|Map legend|||||||||
15764|Quilalar Formation|40984|6|Mentioned|p389|||||||||
15764|Quilalar Formation|41277|6|Mentioned|Fig.5|||||||||
15764|Quilalar Formation|41307|4|Described|p11|||||||||
15764|Quilalar Formation|41381|6|Mentioned|p328|||||||||
15764|Quilalar Formation|41791|6|Mentioned|p269|||||||||
15764|Quilalar Formation|41978|6|Mentioned|p494|||||||||
15764|Quilalar Formation|41979|6|Mentioned|p522|||||||||
15764|Quilalar Formation|42234|4|Described|p1055|||||||||
15764|Quilalar Formation|42523|5|Briefly described|p372|||||||||
15764|Quilalar Formation|42565|4|Described|Table 1 P5, P2|||||||||
15764|Quilalar Formation|42676|5|Briefly described|Fig.2 P41|||||||||
15764|Quilalar Formation|42706|5|Briefly described|map legend|Proterozoic|Proterozoic|Sandstone, siltstone, shale: commonly calcareous.||||||09-FEB-09
15764|Quilalar Formation|42812|6|Mentioned|p65|||||||||
15764|Quilalar Formation|42818|5|Briefly described|p212|||see also Fig.2 p205.||||||27-NOV-06
15764|Quilalar Formation|43608|6|Mentioned|Fig.11,p11|||||||||
15764|Quilalar Formation|43616|6|Mentioned|p4|||||||||
15764|Quilalar Formation|44195|6|Mentioned|p356 Fig.9|||||||||
15764|Quilalar Formation|45161|6|Mentioned|p27|||||||||
15764|Quilalar Formation|45166|4|Described|p17|||||||||
15764|Quilalar Formation|46960|2|Defined|p221|Proterozoic|Proterozoic|||||||
15764|Quilalar Formation|46962|4|Described|Table 1|||See also Fig.3.||||||
15764|Quilalar Formation|46995|5|Briefly described|p268|||||||||
15764|Quilalar Formation|46996|6|Mentioned|p273|||||||||
15764|Quilalar Formation|47083|4|Described|p10-11||Proterozoic|Previously included as part of 'Surprise Creek Beds'.  Equivalent to Corella Formation. Overlain by Bigie Formation, Fiery Creek Volcanics, Surprise Ceek Formation; conformably underlain by Myally Subgroup.||||||27-NOV-06
15764|Quilalar Formation|49041|5|Briefly described|Table 1|||||||||
15764|Quilalar Formation|50100|5|Briefly described|p11, p13 Fig. 4|Statherian|Statherian|Unconformably overlies the Leichhardt Volcanics.  Age: ~1750Ma.  Geological Province: Western Fold Belt Province.||||||27-NOV-06
15764|Quilalar Formation|50332|5|Briefly described|p16, p17, p18|Paleoproterozoic|Paleoproterozoic|Age: 1755-1740Ma. Unconformably overlain by Bigie Formation, in western area conformably unberlain by Myally Subgroup, in other parts is unconformably underlain by Leichhardt Volcanics.||||||07-FEB-11
15764|Quilalar Formation|50550|5|Briefly described|p1139 Fig.2||Statherian|Conformably overlies Myally Subgroup. Overlain by Bigie Formation at an angular unconformity.||||||19-DEC-07
15764|Quilalar Formation|50624|5|Briefly described|p234 Fig.2||Paleoproterozoic|||||||07-NOV-08
15764|Quilalar Formation|60558|5|Briefly described|p4 Fig. 3|Paleoproterozoic|Paleoproterozoic|Geological Province: Western Fold Belt.||||||03-JUN-09
15764|Quilalar Formation|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: ~1750Ma. Geological Province: western Mount Isa Block.||||||07-NOV-08
15764|Quilalar Formation|61922|5|Briefly described|p8, p9 Fig. 3|||Together with the Mitakoodi Quartzite and Ballara Quartzite a part of this unit forms a marker horizon within the cover sequence 2.  Geological Province: Mount Isa Inlier/Eastern Fold Belt.||||||
15764|Quilalar Formation|61925|5|Briefly described|p64|||Correlates with Mitakoodi Quartzite and Ballara Formation in the Eastern Fold Belt. Geological Province: Western Fold Belt, Mount Isa Inlier.||||||
15764|Quilalar Formation|61929|5|Briefly described|p128 Fig. 2|||||||||
15764|Quilalar Formation|61936|5|Briefly described|p193|Paleoproterozoic|Paleoproterozoic|A shallow marine quartzite-carbonate succession. Overlies the Myally Group. Age: ca1755Ma. Geological Province: Leichhardt Superbasin, Western Fold Belt, Mount Isa Inlier.||||||07-NOV-08
15764|Quilalar Formation|62084|5|Briefly described|p936 Fig.5|||Leichhardt Superbasin. Shown as Quilalar Fm.|1755+/-3 Ma U-Pb SHRIMP (after Page et al. 2000)|||||
15764|Quilalar Formation|62288|5|Briefly described|p122 Fig. 2|Paleoproterozoic|Paleoproterozoic|Geological Province: Western Fold Belt/ Mount Isa Inlier.||||||07-NOV-08
15764|Quilalar Formation|62988|5|Briefly described|p34|Paleoproterozoic|Paleoproterozoic|Included in the Quilalar Supersequence spanning the interval ~1755-1740Ma (in the Western Succession). Geological Province: Mount Isa Inlier.||||||07-NOV-08
15764|Quilalar Formation|63023|5|Briefly described|p1024 Fig. 1, p1025 Fig. 2|Paleoproterozoic|Paleoproterozoic|Ages: 1763+/-8Ma,1759+/-5Ma,1748+/-4Ma. Max.thick: 2km. Unconformable on Lochness Fm (Myally Subgp). Geol.Prov: Calvert Superbasin. Quartzite, very fine-gr.hummocky sandstone, siltstone, variably carbonaceous shale, dolostone. See also p1027 Tb.1, p1030||||||07-NOV-08
15764|Quilalar Formation|63109|6|Mentioned|p1108 Fig. 3|||Underlain by Lochness Formation. Geological Province: Leichhardt Superbasin. Consists of dolostone and dolomitic siltstone and shale.||||||30-SEP-08
15764|Quilalar Formation|63111|5|Briefly described|p1162, p1163 Fig. 3, p1164 Tb. 1|Statherian|Statherian|Overlain by Bigie Formation, underlain by Myally Subgroup. Thickness:~ 2000m. Age: 1748+/-4Ma. Geological Province: Leichhardt Superbasin. Consists of sandstone with siltstone, shale and very fine sandstone and undifferentiated dolostone.||||||07-FEB-11
15764|Quilalar Formation|63113|5|Briefly described|p1214 Fig.2, p1225 Fig.13.|||||Of the Myally Subgroup||Overlies Lochness Formation. Is overlain ?unconformably by Bigie Formation.||
15764|Quilalar Formation|63114|5|Briefly described|p1253 Fig.2. |||Leichhardt superbasin.||||Overlies Lochness Formation (Myally Subgroup). Is overlain by Bigie Formation.||
15764|Quilalar Formation|63115|6|Mentioned|p1279 Fig.4.|||Leichhardt superbasin.||||||
15764|Quilalar Formation|63116|6|Mentioned|p1297 Fig.2, |||Leichhardt superbasin. Material properties detailed.||||||
15764|Quilalar Formation|63593|5|Briefly described|p288 Fig.2, p291 Fig.3 and Tb.2.|||Western Fold Belt. 2000 m thick.|||||Sandstone, siltstone, shale, commonly calcareous.|
15764|Quilalar Formation|63866|5|Briefly described|p54, p56, p58|Statherian|Statherian|Leichhardt Superbasin.|1748 +/- 3 Ma (Neumann et al., 2006)|||Overlies the Bortala Formation.||
15764|Quilalar Formation|64248|6|Mentioned|p38 Fig.5|||Kalkadoon-Leichhardt Belt. Equivalent to Corella Formation and Ballara and Mitakoodi Quartzites.||||||11-DEC-17
15764|Quilalar Formation|64250|5|Briefly described|p25 fig 10, p11 fig 3, p22|||Widespread across Mt Isa Inlier deposited in NW-SE trending basin open to SE.  Detrital zircons consistent with Argylla and Bottletree Formations origin or from the NW, Nicholson Granite, Cliffdale Volcanics and Kamarga Volcanics.|<1748 +/- 4 Ma|||Overlies Haslingden Group, Myally Subgroup.  Correlated with Ballara Quartzite and Mitakoodi Quartzite.|Variably calcareous.|
15764|Quilalar Formation|64367|5|Briefly described|p555  Fig. 1c|Paleoproterozoic|Paleoproterozoic|Ages: 1763+/-8Ma, 1748+/-4Ma.||||||07-FEB-11
15764|Quilalar Formation|64725|6|Mentioned|p58 Fig.2. |||Mount Isa Inlier.||||||
15764|Quilalar Formation|64726|6|Mentioned|p83 Fig.2.|||||||||
15764|Quilalar Formation|64744|6|Mentioned|p353 Fig.4. |Statherian|Statherian|Mount Isa Basin.||||||
15764|Quilalar Formation|64834|5|Briefly described|p13 Fig.2|||Leichhardt Superbasin. Western Succession of Mount Isa Basin.|||||Sandstone; siltstone, shale, very fine sandstone; undifferentiated dolostone.|
15764|Quilalar Formation|65337|6|Mentioned|p5. |||Leichhardt Superbasin; Leichhardt River Fault Trough.||||||
15764|Quilalar Formation|65396|5|Briefly described|p16, p82, p175, p187, p190, p193-196|Statherian|Statherian|See also p201, p241. Leichhardt Superbasin. Cover Sequence 2. Leichhardt River Fault Trough, Kalkadoon Leichhardt Belt. Detrital zircon sources listed. Shallow-marine deposits.|1748 +/- 4 Ma (Neumann et al., 2005).|||Overlies Myally Subgroup (Haslingden Group). Correlated with Ballara and Mitakoodi Quartzites and Corella Formation.|Calcareous metasediments, sandstone, mafic and felsic volcanics.|
15764|Quilalar Formation|65505|6|Mentioned|980|Proterozoic|Proterozoic|Age: c.1750 Ma.||||||
15764|Quilalar Formation|66529|6|Mentioned|p32 |||Uppermost unit in Leichhardt Superbasin.|||||Fine-grained siliciclastics and dolostone.|
15764|Quilalar Formation|67026|6|Mentioned|p336 Fig.3.|Statherian|Statherian||1755 +/- 3 Ma (Page et al. 2000).|||||24-APR-12
15764|Quilalar Formation|67323|5|Briefly described|p11, p15, p24, p31, p39, p107|Paleoproterozoic|Paleoproterozoic|See also GIS attrib tbl, Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Leichhardt Superbasin. Mount Oxide, Leichhardt River and Century Domains, Mount Isa Inlier. The lower part is a clastic succession deposited during extension; the upper part is a sag-phase carbonate succession.|~1775-1750 Ma (lower); ~1750-1740 Ma (upper).|||Unconformably overlain by Surprise Creek Formation, Bigie Formation. Equivalent to Ballara Quartzite, Mitakoodi Quartzite and Corella Formation. Intruded by Kalkadoon Granite?|Feldspathic quartzite, orthoquartzite, conglomerate, feldspathic grit, shale, siltstone.|
15764|Quilalar Formation|68021|5|Briefly described|p135 fig 4, p138|Statherian|Statherian|Quilalar Supersequence, Leichhardt Superbasin, Western Succession. Fluviatile to shallow marine sediments.|~1755 - ~1740 Ma|||Overlies Myally Subgroup unconformably, overlain by Fiery Creek Volcanics, Bigie Formation unconformably. Intruded by Weberra Granite?|Clean, well-sorted quartzite, well-bedded stromatolitic limestones, redeposited calcareous sandstones.|
15764|Quilalar Formation|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province.||||||
15764|Quilalar Formation|68575|6|Mentioned|p107-108|||||||Nonconformably overlies Kalkadoon Granite.||
15764|Quilalar Formation|68732|5|Briefly described|p159-163, p165-167, p169, p171|Statherian|Statherian|Contains flat rhythmites. Of the Quilalar Supersequence. Rocks characterised by a transgressive-regressive cycle. Maximum sedimentary depositional ages.|1763 +/- 8, 1748 +/- 4 Ma||||Includes fine- to coarse-grained quartzites and arenites, fining upwards into thinly bedded sandstones; very fine-grained arkosic sandstones. Also sandstone-siltstone-shale laminae and thin beds (rhythmites).|01-DEC-17
15764|Quilalar Formation|69056|6|Mentioned|p2|||||||||
15764|Quilalar Formation|69222|5|Briefly described|p221, p222 Fig.2|Statherian|Statherian|Leichhardt River Fault Trough. Post-rift subsidence deposits.||||Overlies Myally Subgroup, overlain by Bigie Formation, Fiery Creek Volcanics||09-FEB-18
15764|Quilalar Formation|69370|6|Mentioned|p307 Fig.2|Statherian|Statherian|Western Fold Belt, Mount Isa Block.||||Overlies Myally Subgroup.||25-JAN-19
15764|Quilalar Formation|69591|5|Briefly described|p29, p33-34, p38, p40, p57, p105-106|Paleoproterozoic|Paleoproterozoic|Part of the Quilalar Supersequence. Leichhardt River Domain. Probably absent N of the Murphy Tectonic Ridge. Shelf-fluvial shoreline deposits.|1748 +/- 4 Ma (MDA: Neumann et al., 2006).|||Equivalent to Corella Formation. ?Intruded by Augustus Igneous Complex.|Feldspathic quartzite, orthoquartzite, conglomerate, feldspathic grit, shale, siltstone.|
15764|Quilalar Formation|70282|6|Mentioned|p544 Tb.1|||Cover sequence 2, Mount Isa.|1790-1760 Ma (or 1720 Ma)|||||13-FEB-18
15764|Quilalar Formation|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Nine facies are mapped separately.|||||Feldspathic to quartzose sandstone, conglomerate, shale and siltstone, and minor limestone and dolomite.|
15764|Quilalar Formation|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Nine facies are mapped separately.|||||Feldspathic to quartzose sandstone, conglomerate, shale and siltstone, and minor limestone and dolomite.|
15764|Quilalar Formation|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1780+/-20 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone, basaltic andesite.|
15764|Quilalar Formation|71606|5|Briefly described|p137|Statherian|Statherian|Lawn Hill Platform, Mount Isa Inlier.||||Overlain unconformably by Bigie Formation. Underlain  by Myally Subgroup.||
15764|Quilalar Formation|71799|5|Briefly described|p150 fig 2|Statherian|Statherian|Lawn Hill.|ca. 1750 Ma|||Overlies the Myally Supergroup.|Sandstone, greywacke, dolomite and calc-silicate rocks.|
15764|Quilalar Formation|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Leichhardt River Fault Trough and the Kalkadoon-Leichhardt Belt of the Mount Isa Province.||||Shown as overlying Whitworth Formation and Argylla Formation.||
15764|Quilalar Formation|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Leichhardt River Domain and the Kalkadoon-Leichhardt Domain. Shown as older than the the Wonga-Burstall Event (c. 1740 Ma).||||Shown as equivalent to Stanbroke Sandstone, Mary Kathleen Group.|Feldspathic to quartzose sandstone, conglomerate, shale and siltstone, and minor limestone and dolomite.|
15764|Quilalar Formation|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Leichhardt River Domain and the Kalkadoon-Leichhardt Domain. Shown as older than the the Wonga-Burstall Event (c. 1740 Ma).||||Shown as equivalent to Stanbroke Sandstone, Mary Kathleen Group.|Feldspathic to quartzose sandstone, conglomerate, shale and siltstone, and minor limestone and dolomite.|
15764|Quilalar Formation|72889|6|Mentioned|p6 Fig.i.|||||||||
15764|Quilalar Formation|72912|5|Briefly described|p5 Fig.3, p12.|Statherian|Statherian|Located in the Leichhardt River Fault Trough and the Kalkadoon-Leichhardt Belt of the Mount Isa Province.||||Correlated with Corella and Doherty Formations.||
15764|Quilalar Formation|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Mount Isa Province, Leichhardt Superbasin.||||Underlain by(?) Whitworth Quartzite (Myally Subgroup).||
15764|Quilalar Formation|73137|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|||||||
15764|Quilalar Formation|73413|6|Mentioned|p3|||Mount Isa Inlier.||||||
15764|Quilalar Formation|73525|5|Briefly described|p4-5 Fig.2, p19 Fig.13, p20|Statherian|Statherian|Mount Oxide-(Ardmore-May Downs) and Leichhardt River Domains.|1776+/-7 Ma, 1763+/-8 Ma, 1748+/-4 Ma MDA||||Clastics, includes mafic extrusives, carbonates.|
15774|Quita Formation|24419|5|Briefly described|p18|Late Cambrian|Middle Cambrian|Sequence of thin-bedded to laminated bituminous limestone with some irregular chert laminae and nodules. Erosional contact with overlying Steamboat Sandstone. Interfingers with the Blazan Shale. Geological Province: Georgina Basin.||||||
15774|Quita Formation|30242|6|Mentioned|Fig.2|||||||||
15774|Quita Formation|30479|6|Mentioned|Fig.6|||See also p19. Name should be dropped.||||||27-NOV-06
15774|Quita Formation|30914|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
15774|Quita Formation|33111|6|Mentioned|Fig.15|||||||||
15774|Quita Formation|34287|6|Mentioned|Fig.3|||||||||
15774|Quita Formation|35054|6|Mentioned|Table 23|||||||||
15774|Quita Formation|35139|6|Mentioned|p46|||||||||
15774|Quita Formation|35553|6|Mentioned|p47|||||||||
15774|Quita Formation|36234|6|Mentioned|p168|||||||||
15774|Quita Formation|37572|4|Described|p158|||See also Fig.8 and p165.||||||27-NOV-06
15774|Quita Formation|38442|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|||||||25-AUG-04
15774|Quita Formation|38446|6|Mentioned|Table 23|||||||||
15774|Quita Formation|38608|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
15774|Quita Formation|39445|5|Briefly described|Table 4|||See also p62.||||||27-NOV-06
15774|Quita Formation|39690|6|Mentioned|p88|||||||||
15774|Quita Formation|40038|6|Mentioned|p248|||||||||
15774|Quita Formation|44211|2|Defined|p93,96,100-107|||Rests on eroded surface of Middle Cambrian rocks.||||||
15774|Quita Formation|44273|14|Not recorded|Map Legend||Middle Cambrian|||||||
15774|Quita Formation|44275|14|Not recorded|Map Legend|||||||||
15774|Quita Formation|44920|14|Not recorded|Map Legend, Sheet 4||Middle Cambrian|||||||
15774|Quita Formation|45012|14|Not recorded|p26,307|||Fauna.||||||
15774|Quita Formation|45052|3|Fully described|p100|||M.Camb.||||||
15774|Quita Formation|45054|6|Mentioned|p5|||Fossil locality||||||
15774|Quita Formation|45079|4|Described|p34|||Cambrian age||||||
15774|Quita Formation|45166|5|Briefly described|Table 15|||||||||
15774|Quita Formation|60122|6|Mentioned|p11 Tb. 1, p18|||Possibly disconformably overlain by Steamboat Sandstone?||||||
15774|Quita Formation|60123|5|Briefly described|p5|||Possibly disconformably underlies Steamboat Sandstone.||||||
15774|Quita Formation|60359|5|Briefly described|Map Legend|Cambrian|Cambrian|Bituminous limestone, marl, mudstone; minor chert, sandstone.||||||
15774|Quita Formation|64068|4|Described|p63-64, 62, 65|Middle Cambrian|Middle Cambrian|Formerly included in Steamboat Sandstone (Reynolds, 1965). Contains trilobites, hyoliths, molluscs. Correlated with Arthur Creek Formation, Blazan Shale, Inca Formation, Roaring Siltstone, Devoncourt Limestone, Currant Bush Limestone, Age Creek Formation, Camooweal Dolostone.||Of Narpa Group.||Conformably overlies or interdigitates with Blazan Shale. Disconformable over Beetle Creek Formation or Thorntonia Limestone. Conformably (or disconformably?) overlain by Steamboat Sandstone.|Siliceous shale, marly and quartzic limestone with nodular chert.|05-APR-12
15774|Quita Formation|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Middle Cambrian|Middle Cambrian|Georgina Basin.||Narpa Group.|||Limestone, bituminous limestone, sandy limestone, calcilutite, minor arenite, chert nodules.|
15774|Quita Formation|69443|5|Briefly described|p28:16|Middle Cambrian|Middle Cambrian|Georgina Basin.||Narpa Group.||||12-JUL-16
15774|Quita Formation|69573|6|Mentioned|p659, 665|||Georgina Basin. Contains Drumian Stage [Cambrian] fossil sites. High energy, inner shelf setting.||||||
15774|Quita Formation|69591|5|Briefly described|p87, p91, p96|Cambrian|Cambrian|Ardmore/Quita Creek area, Oban Sub-basin, Georgina Basin. 60-70m thick.||||Disconformably overlies Blazan Shale. Is overlain by Steamboat Sandstone transitionally.|Light-grey to dark-grey, bituminous, thin-bedded to laminate limestone (fine calcarenite, calcilutite or oolitic), with regressive interbeds of grey to yellowish marl and mudstone with some irregular chert laminae and nodules.|
15774|Quita Formation|70723|5|Briefly described|p24 Fig. 2|Cambrian|Cambrian|Georgina Basin.||Narpa Group||Overlies Blazan Shale. Is overlain by Steamboat Sandstone.||
15774|Quita Formation|72321|6|Mentioned|Fig 2|Guzhangian|Drumian|Toko Syncline, Georgina Basin.  Australian stages: Undillan to Boomerangian.||of Narpa Group.||||
15774|Quita Formation|72516|6|Mentioned|p92|||Eastern Georgina Basin.||||Equivalent to the Arthur Creek Formation.||
15830|Ranford Formation|22496|3|Fully described|p11||Neoproterozoic|Of the Duerdin Group. Conformably overlies the Moonlight Valley Tillite.  Inferred to be conformable on the Redbank Yard Formation to the south.  Geological Province:  Wolfe Basin.||||||16-AUG-04
15830|Ranford Formation|22537|5|Briefly described|37|Proterozoic|Proterozoic|||||||
15830|Ranford Formation|22547|4|Described|p28||Neoproterozoic III|Of the Duerdin Group. Geological province:  Wolfe Creek Basin. Thickness: 600 m. Overlies Moonlight Valley Tillite.||||||14-NOV-06
15830|Ranford Formation|22649|6|Mentioned|p 143|||Rb-Sr age: 672+/-70 Ma,   p143.||||||27-NOV-06
15830|Ranford Formation|22777|5|Briefly described|Map|||Of the Duerdin Group.  In the Wolfe Basin.||||||27-NOV-06
15830|Ranford Formation|23621|4|Described|p33|Neoproterozoic|Neoproterozoic|See also page 9 table 1. Of Duerdin Group. Geological Province: Wolfe Basin.  Max. thickness: 500 m.||||||
15830|Ranford Formation|23622|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Duerdin Group. Geological Province: Wolfe Basin.||||||
15830|Ranford Formation|23806|5|Briefly described|p1122 Fig. 1|Neoproterozoic|Neoproterozoic|Of Duerdin Group.||||||
15830|Ranford Formation|24173|4|Described|p25, p11 Tb.2|Neoproterozoic III|Neoproterozoic III|Of the Duerdin Group. Conformably overlain by Mount Forster Sandstone; conformably overlies Moonlight Valley Tillite; overlies the Illjara Sandstone disconformably. Geological Province: Wolfe Basin. Max Thickness: 500m.||||||09-MAR-05
15830|Ranford Formation|28255|3|Fully described|p76, Tb. 11 (opp. p8), p110|Adelaidean|Adelaidean|Of Duerdin Gp. Includes Jarrad Sst and Johnny Cake Sst Mbrs. Subdivided by Pontifex et al (1968): Bucket Spring, Beasly Knob and Ernie Lagoon Members. Ferruginous and laminated siltstones/sandstones sequence; claystone, "zebra-stone". Max. thick: >60m.||||||27-NOV-06
15830|Ranford Formation|29813|4|Described|Table 2|||||||||
15830|Ranford Formation|29818|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
15830|Ranford Formation|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
15830|Ranford Formation|31645|6|Mentioned|p4|||See also Table 1||||||
15830|Ranford Formation|32660|5|Briefly described|Table 6|||||||||
15830|Ranford Formation|32664|6|Mentioned|Map legend|Adelaidean|Adelaidean|Briefly described in notes||||||
15830|Ranford Formation|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Duerdin Group.  Includes three members: Jarrad Sandstone, Bucket Spring and Ernie Lagoon Members.||||||02-DEC-04
15830|Ranford Formation|32701|4|Described|Table 1|||Adelaidean. Duerdin Group. See p14.||||||27-NOV-06
15830|Ranford Formation|32728|6|Mentioned|Table 7|||See Fig.16||||||
15830|Ranford Formation|33375|6|Mentioned|p11 Tb. 1, p13|Adelaidean|Adelaidean|Of the Duerdin Group.  Fissile to massive purple ferruginous siltstone, white siltstone and claystone; minor sandstone. Conformable on Moonlight Valley Tillite. Max. thickness: 40m. Contains "zebra stone" in basal beds.||||||27-APR-05
15830|Ranford Formation|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
15830|Ranford Formation|33378|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Duerdin Group. Purple ferruginous siltstone, white siltstone and claystone; minor sandstone.||||||27-APR-05
15830|Ranford Formation|34230|6|Mentioned|p67|Proterozoic|Proterozoic|Contains zebra rock, a striking red and white banded rock - now submerged in the Ord River reservoir.||||||27-NOV-06
15830|Ranford Formation|36048|6|Mentioned|p381|||||||||
15830|Ranford Formation|36532|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
15830|Ranford Formation|36551|6|Mentioned|Table 12|||||||||
15830|Ranford Formation|36888|4|Described|p215|||||||||
15830|Ranford Formation|36898|5|Briefly described|Table 1|||See also p181.||||||27-NOV-06
15830|Ranford Formation|37577|6|Mentioned|p70|||||||||
15830|Ranford Formation|37927|5|Briefly described|p507|||||||||
15830|Ranford Formation|38157|6|Mentioned|Table X|||||||||
15830|Ranford Formation|39210|5|Briefly described|p49|||Age||||||
15830|Ranford Formation|39827|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
15830|Ranford Formation|40494|4|Described|p13|||||||||
15830|Ranford Formation|41429|6|Mentioned|p247|||||||||
15830|Ranford Formation|42047|6|Mentioned|p201|||||||||
15830|Ranford Formation|43299|5|Briefly described|Map Legend||Neoproterozoic|Of the Duerdin Group.||||||27-NOV-06
15830|Ranford Formation|43303|5|Briefly described|Map Legend||Neoproterozoic|Of the Duerdin Group.||||||27-NOV-06
15830|Ranford Formation|43853|5|Briefly described|Map Legend||Proterozoic|||||||
15830|Ranford Formation|43855|5|Briefly described|Map Legend||Proterozoic|||||||
15830|Ranford Formation|44140|4|Described|p301 fig 4-7, p302 Tb. 4-2|Neoproterozoic|Neoproterozoic|Of East Kimberley area. 564 m thick.||Duerdin Group|Jarrad Sandstone Member, Johnny Cake Shale Member.|Overlies Moonlight Valley Tillite. Is overlain unconformably by Mount Forster Sandstone (Albert Edward Group).|Thinly bedded khaki sandstone and fine quartz sandstone.|08-MAR-18
15830|Ranford Formation|44230|5|Briefly described|Map Legend||Proterozoic|||||||
15830|Ranford Formation|44317|4|Described|Table 3, p.7||Adelaidean|||||||
15830|Ranford Formation|44318|14|Not recorded|map legend||Adelaidean|Adelaidean.||||||
15830|Ranford Formation|44324|14|Not recorded|p.10||Adelaidean|Tb.2 (Adelaidean) Of the Duerdin Group.||||||27-NOV-06
15830|Ranford Formation|44325|14|Not recorded|map legend||Adelaidean|Adelaidean.||||||
15830|Ranford Formation|44363|5|Briefly described|p.6,14,20|||(Adelaidean) Of the Duerdin Group.||||||27-NOV-06
15830|Ranford Formation|44364|14|Not recorded|map legend|||||||||
15830|Ranford Formation|44868|5|Briefly described|Map Legend||Phanerozoic|||||||
15830|Ranford Formation|45047|2|Defined|p89|Adelaidean|Adelaidean|See p36.||||||07-NOV-16
15830|Ranford Formation|45112|4|Described|p40|||||||||
15830|Ranford Formation|45140|2|Defined|p13, p59, Appx.p34-35|||Dow and Gemuts (1969). Named after Mount Ranford. Unnamed basin NW of Birrindudu Basin. Mapped as Kearney Beds by Casey and Wells (1964). The type section is [in] Moonlight Valley, Dixon Range sheet area. Forms low strike ridges. Up to 200m thick. No fossils known.||Duerdin Group.||Conformably overlies Redbank Yard Formation. Is overlain unconformably by Mount Forster Sandstone.|Thin-bedded to laminated micaceous siltstone and shale; flaggy, well-sorted, fine-grained sublithic arenite; dolomitic sandstone.|
15830|Ranford Formation|48927|6|Mentioned|Table 1|||Refers Dow and Gemuts (1969).||||||27-NOV-06
15830|Ranford Formation|48938|4|Described|p70|||||||||
15830|Ranford Formation|48943|3|Fully described|p84|||||||||
15830|Ranford Formation|60006|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Wolfe Creek Basin. Of Duerdin Group.||||||
15830|Ranford Formation|60519|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Duerdin Group. Geological Province: Wolfe Creek Basin. Includes: Jarrad Sandstone Member. Siltstone and mudstone, greywacke, lithic sandstone, quartz sandstone, dolomitic quartz sandstone and dolomite.||||||05-NOV-04
15830|Ranford Formation|60682|5|Briefly described|p17 Table 4, 19|Neoproterozoic|Neoproterozoic|Of Duerdin Group. Geological Province: Wolfe Creek Basin.||||||
15830|Ranford Formation|63458|5|Briefly described|p873 Fig.2, p886-889, p897 Fig.19.|Ediacaran|Ediacaran|East Kimberley district.||Unit in Duerdin Group.|Includes Jarrad, and Johnny Cake, Sandstone Members.|Overlies Moonlight Valley Tillite.|Laminated siltstone (Texas/Mabel Downs); sandstone and dolomite (Palm Springs).|12-JUN-15
15830|Ranford Formation|64104|4|Described|p62-63, p66 fig 3, p68 Fig.5, p71-72|Neoproterozoic|Neoproterozoic|In the Purnululu area, parts of this unit have been reinterpreted as belonging to Frank River Sandstone.|||Includes Jarrad Sandstone Member and Johnny Cake Shale Member.|Overlies Moonlight Valley Formation conformably. Is overlain unconformably by Mount Forster Sandstone.|Marine siltstone and sandstone.|
15830|Ranford Formation|65331|5|Briefly described|Map legend|Neoproterozoic |Neoproterozoic|Of Duerdin Group, Wolfe Creek Basin. Includes Ernie Lagoon, Beasly Knob, Bucket Springs and Jarrad Sandstone Members. Quartz sandstone, siltstone, conglomerate||||||
15830|Ranford Formation|67151|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Wolfe Basin.||Unit in Duerdin Group.|Includes Jarrad Sandstone Member.|Overlies Moonlight Valley Tillite. Is unconformably overlain by Kinevans Sandstone.|Ferruginous siltstone, siltstone and claystone; minor sandstone.|
15830|Ranford Formation|67484|4|Described|p293-299|Ediacaran||East Kimberley. The upper part is a correlative of the Elatina and Nuccaleena Formations. A new Ediacara-type fossil Palaeopascichnus has been identified in the constituent Johnny Cake Shale Member. If correlation with the early Ediacara units in SA is accepted, this represents the earliest identifiable member of the Ediacara biota, and the first Ediacara-type fossil in the Kimberley.||Of the Duerdin Group.|Includes Johnny Cake Shale, Jarrad Sandstone, Members.|Underlain by the Moonlight Valley Tillite. Overlain by the Mount Forster Sandstone. Upper part correlates with Brachina Formation.|Upper part consists of claystone, dolomitic siltstone and fine sandstone.|27-MAY-15
15830|Ranford Formation|67620|5|Briefly described|p5|Ediacaran|Ediacaran|East Kimberley region.||Duerdin Group.|Jarrad Sandstone Member, Johnny Cake Shale Member.|Overlies Moonlight Valley Formation. Is overlain by Mount Forster Sandstone (Albert Edward Group).||
15830|Ranford Formation|68138|5|Briefly described|p153, 155-156|Neoproterozoic|Neoproterozoic|East Kimberley region.||Duerdin Group.||Overlies Moonlight Valley Formation.|Shale, silt/sandstones.|
15830|Ranford Formation|68244|4|Described|p660,668,670|Neoproterozoic|Neoproterozoic|East Kimberly area, Kimberley region. Nomenclature of Dow and Gemuts 1963, reinterpreted by Corkeron 2008 to be part of Moonlight Valley Formation and Frank River Sandstone.||Unit of Duerdin Group.||Uppermost unit of Duerdin Group. Overlain unconformably by Mount Forster Sandstone. Underlain by Moonlight Valley Formation.||
15830|Ranford Formation|68473|6|Mentioned|p529, 531-532, p534, p547|||||Duerdin Group|Includes the Johnny Cake Shale Member, Jarrad Sandstone Member and the Beasly Knob Member.|Equivalent to the Throssell Shale.||
15830|Ranford Formation|69099|4|Described|GEOL_LUT_CSV files + geochron files|Ediacaran||Wolfe Creek Basin||Duerdin Group|Includes Johnny Cake Shale Member, Jarrad Sandstone Member.||Green to reddish purple siltstone, locally micaceous; minor thin-bedded, fine-grained quartz sandstone and mudstone.|04-AUG-15
15830|Ranford Formation|69165|4|Described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran|See also 100k_xsecgeop_lut.csv.||Duerdin Group|Includes Johnny Cake Shale Member, Jarrad Sandstone Member||Undivided; green to reddish purple siltstone, locally micaceous; minor thin bedded, fine grained quartz sandstone and mudstone.|
15830|Ranford Formation|69437|5|Briefly described|p22:4-5, 7|Ediacaran|Ediacaran|Victoria/Wolfe Basins, Centralian A Superbasin. Supersequence 3.||Duerdin Group.||Overlies Moonlight Valley Tillite and Uniya Formation.||12-JUL-16
15830|Ranford Formation|69442|5|Briefly described|p27:1, 3-4, 6-7|||Wolfe Basin. Widespread in WA, where its thickness reaches 600m. Contains a leached white siltstone with locally-developed red to black Fe-oxide stripes, commercially exploited and marketed as 'zebrastone', mainly in WA.||Duerdin Group.|Ernie Lagoon, Beasly Knob, Bucket Spring, Jarrad Sandstone, Members.|||12-JUL-16
15830|Ranford Formation|69634|4|Described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran|Geological province: Halls Creek Orogen. Of Wolfe Basin, Centralian Superbasin. Events: Alice Springs Orogeny; King Leopold Orogeny D1/M1.|635-541 Ma (Inferred)|Unit of Duerdin Group.|Includes Jarrad Sandstone Member and Johnny Cake Shale Member.||Green to reddish purple siltstone, locally micaceous; minor thin-bedded, fine-grained quartz sandstone and mudstone|
15830|Ranford Formation|69673|5|Briefly described|p190|Neoproterozoic|Neoproterozoic|||Duerdin Group|Includes Jarrad Sandstone Member, Bucket Spring Member, Beasly Knob Member, Ernie Lagoon Member|||
15830|Ranford Formation|70154|4|Described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran||541-635 Ma|Duerdin Group|||Green to reddish purple siltstone, locally micaceous; minor thin-bedded, fine-grained quartz sandstone and mudstone.|
15830|Ranford Formation|70655|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Wolfe Basin||Duerdin Group.|Includes Jarrad Sandstone Member.|Shown as overying Moonlight Valley Tillite. May be unconformably overlain by Kinevans Sandstone relationship not clear on map.|Ferruginous siltstone, siltstone and claystone; minor sandstone.|
15830|Ranford Formation|71267|4|Described|GEOL_LUT_CSV files|Ediacaran|Ediacaran|Geological province: Halls Creek Orogen. Of Wolfe Basin, Centralian Superbasin. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|635-541 Ma (inferred)|Unit of Duerdin Group.|Includes Jarrod Sandstone Member, Johnny Cake Shale Member, Moonlight Valley Tillite.||Green to reddish purple siltstone, locally micaceous; minor thin-bedded, fine-grained quartz sandstone and mudstone|
15830|Ranford Formation|73255|4|Described|p532-535, p537-539, p543-546, p548-550|Ediacaran|Ediacaran|Contains Palaeopascichnus and Yangtziramulus fossils. Trough cross-bedded dolomitic sandstone facies deposited in fluvial paleochannels. Interbedded red-green siltstone facies includes gypsum rosettes, desiccation cracks, claystone breccias, planar and wavy bedding, suggested deposition in shallow lacustrine environment. Interbedded red siltstone and sandstone facies with planar/wavy bedding, ripple marks, claystone breccias and Rivularites repertus microbial trace fossil interpreted as fluvial levee, associated with paleochannel facies and eolian reworking. Red sandstone with dolomitic nodules facies represents well drained floodplain environments. Evidence of paleosols comparable with gypsids and calcids. Contains zebra rock in the Johnny Cake Member. Common early burial alterations include gleisation. Specific locations in text include p533 Fig.1, p538 Fig.5, p539 Fig.6 and p541.||Duerdin Group|Johnny Cake Member, Jarrad Member|Conformably overlies the Moonlight Valley Tillite, disconformably underlies the Kinevans Sandstone, and Mount Forster Sandstone, underlies the Albert Edward Group.|Dolomitic sandstones in lower part. Includes trough cross-bedded dolomitic sandstone, finely interbedded red-green siltstone, medium to coarse sandstone with interbedded fine grained sandstone and siltstone, red sandstones with dolomitic nodules.|
15983|Redcliff Pound Group|23621|6|Mentioned|p32|||||||||
15983|Redcliff Pound Group|24173|6|Mentioned|p24|Neoproterozoic|Neoproterozoic|Probable correlative of Ruby Plains Group (in the Billiluna 1:250,000 sheet area||||||
15983|Redcliff Pound Group|29806|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
15983|Redcliff Pound Group|29807|6|Mentioned|Table 1|||||||||
15983|Redcliff Pound Group|29809|6|Mentioned|Table 1|||||||||
15983|Redcliff Pound Group|29810|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
15983|Redcliff Pound Group|29812|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
15983|Redcliff Pound Group|29813|4|Described|Table 2|||||||||
15983|Redcliff Pound Group|29817|6|Mentioned|p7|||||||||
15983|Redcliff Pound Group|29818|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
15983|Redcliff Pound Group|29819|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
15983|Redcliff Pound Group|31360|6|Mentioned|Table 1|||||||||
15983|Redcliff Pound Group|31362|6|Mentioned|p8|||||||||
15983|Redcliff Pound Group|32660|6|Mentioned|p243|||||||||
15983|Redcliff Pound Group|33102|6|Mentioned|Fig.2|||||||||
15983|Redcliff Pound Group|33965|6|Mentioned|p7|||||||||
15983|Redcliff Pound Group|35205|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
15983|Redcliff Pound Group|35222|6|Mentioned|p10|||||||||
15983|Redcliff Pound Group|36473|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
15983|Redcliff Pound Group|36551|6|Mentioned|Table 12|||||||||
15983|Redcliff Pound Group|37299|6|Mentioned|Fig.1|||Misspelling? [No. Redcliffe Pound Group is the misspelling. CEBApr95]||||||
15983|Redcliff Pound Group|37462|6|Mentioned|Table 4.V|||||||||
15983|Redcliff Pound Group|42504|5|Briefly described|Table 4 P73|||||||||
15983|Redcliff Pound Group|43175|5|Briefly described|p6||Proterozoic|||||||
15983|Redcliff Pound Group|43631|6|Mentioned|p20|||||||||
15983|Redcliff Pound Group|45112|5|Briefly described|p29|||||||||
15983|Redcliff Pound Group|45140|2|Defined|p12-14, p17-18, p22, p26, p28, p39-40|Neoproterozoic|Neoproterozoic|See also p42-46, p48, p51-53, p56-60, p63-64, p66-67, p74-75, Appx.p23. Hodgson (1976); Blake and Yeates (1977). Named after Redcliff Pound. Birrindudu Basin. Generally gently dipping. Maximum exposed thickness is c.1300m; true thickness may be well over 2000m. No mineralisation yet been found. Younger than 1076 +/- 50 Ma (age of migmatite underlying Heavitree Quartzite). Is overlain by Hidden Basin Beds, and unconformably by Lucas Formation, Hazlett Beds and Knobby Sandstone.|||Lewis Range, Muriel Range, Munyu, Erica Sandstones; Murraba Formation.|Unconformably overlies Killi Killi and Mount Charles Beds, Arunta Complex, Birrindudu Group. Correlated with Heavitree Quartzite, Bitter Springs Formation, Vaughan Springs Quartzite, Limbunya Group.||
15983|Redcliff Pound Group|46788|6|Mentioned|p8|||||||||
15983|Redcliff Pound Group|46864|4|Described|p38|||||||||
15983|Redcliff Pound Group|50315|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Includes: Muriel Range Sandstone.  Age: <800Ma.||||||09-JUN-04
15983|Redcliff Pound Group|50374|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Includes Muriel Range Sandstone||||||
15983|Redcliff Pound Group|50376|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Includes the Muriel Range Sandstone.||||||22-JUN-04
15983|Redcliff Pound Group|60676|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Includes Muriel Range Sandstone. Sublithic arenite, quartz arenite, minor siltstone, shale, conglomerate, arkose, breccia.||||||19-JAN-05
15983|Redcliff Pound Group|61861|6|Mentioned|p4, p23, Map 1|Paleozoic|Neoproterozoic|Neoproterozoic?|||Includes Muriel Range Sandstone.|||
15983|Redcliff Pound Group|62580|5|Briefly described|p10|Neoproterozoic|Neoproterozoic|Part of a thick sequence of predominantly sublithic and quartz arenite in the Tanami region.||||||07-FEB-11
15983|Redcliff Pound Group|62628|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Murraba Basin.||||||15-AUG-06
15983|Redcliff Pound Group|62632|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Murraba Basin.||||||23-DEC-09
15983|Redcliff Pound Group|62633|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Murraba Basin.||||||
15983|Redcliff Pound Group|64580|4|Described|map legend||Neoproterozoic|Quartz sandstone and wacke; minor conglomerate, siltstone, shale, limestone, dolomite, chert, and glauconitic sandstone.||||||09-DEC-08
15983|Redcliff Pound Group|64635|6|Mentioned|p2 Fig.1|||||||||
15983|Redcliff Pound Group|64675|6|Mentioned|p10, Fig.21, Map 1|||||||||19-MAR-14
15983|Redcliff Pound Group|64724|5|Briefly described|p49 Fig. 7||Cryogenian|Age very poorly constrained. May be as young as Ediacaran||||||
15983|Redcliff Pound Group|64733|6|Mentioned|p169 Fig.1|Neoproterozoic|Neoproterozoic|||||||
15983|Redcliff Pound Group|65074|6|Mentioned|p350-351, p353, p356-357 Tb.4-12|Neoproterozoic|Neoproterozoic|See also p358, p360, p362. Of North/Centre Birrindudu Basin. Over 2 km thick. Deposition from c.1000 Ma.|||Lewis Range, Muriel Range, Munyu, Erica Sandstones; Murraba Formation.|Is overlain unconformably by Lucas Formation.||
15983|Redcliff Pound Group|65323|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|Not present on map; Includes the Muriel Range Sandstone. Age given as 800 Ma?||||||02-FEB-10
15983|Redcliff Pound Group|65324|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|Not shown on map; Includes the Muriel Range Sandstone; Age given as 800 Ma?||||||
15983|Redcliff Pound Group|65326|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Not shown on map; Includes the Muriel Range Sandstone;||||||12-APR-10
15983|Redcliff Pound Group|65327|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Not shown on map; Includes the Muriel Range Sandstone;||||||12-APR-10
15983|Redcliff Pound Group|65328|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Not shown on map; Includes the Muriel Range Sandstone;||||||12-APR-10
15983|Redcliff Pound Group|65332|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Murraba Basin. Includes Munyu Sandstone||||||02-FEB-10
15983|Redcliff Pound Group|65349|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|Not shown on map; Includes the Muriel Range Sandstone; Age given as 800 Ma?||||||
15983|Redcliff Pound Group|65350|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Includes the Muriel Range Sandstone. Age given as 800 Ma?||||||
15983|Redcliff Pound Group|65351|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Includes the Muriel Range Sandstone. Age given as 800 Ma?||||||
15983|Redcliff Pound Group|65352|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Not shown on map; Includes the Muriel Range Sandstone||||||12-APR-10
15983|Redcliff Pound Group|65353|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Not shown on map; Includes the Muriel Range Sandstone.||||||11-DEC-12
15983|Redcliff Pound Group|65354|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Not shown on map; Includes the Muriel Range Sandstone;||||||12-APR-10
15983|Redcliff Pound Group|65355|5|Briefly described|cross section|Neoproterozoic|Neoproterozoic|Not shown on map; Includes the Muriel Range Sandstone. Age given as 800 Ma?||||||10-DEC-12
15983|Redcliff Pound Group|65356|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Not shown on map; Includes the Muriel Range Sandstone||||||12-APR-10
15983|Redcliff Pound Group|67163|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Murraba Basin.|||Includes Erica and Munyu Sandstones and Murraba Formation.|Unconformably overlies Reynolds Range Group.||19-OCT-11
15983|Redcliff Pound Group|67168|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||Includes Muriel Range Sandstone.|Unconformably overlies Tanami Group, Inningarra Suite and Pargee Sandstone. Is unconformably overlain by Antrim Plateau Volcanics.||
15983|Redcliff Pound Group|68656|5|Briefly described|GEOL_LUT_CSV/500k_geologyp08_lut|Neoproterozoic|Neoproterozoic|Murraba Basin. See also 500k_interpgeop_lut.csv and GEOCHRON. Is mysteriously referred to as Redcliffe Plain Group, Redcliff Plain Group and Redcliff Pound Group in Geochronology dataset 743, which locates  it in the Birrindudu Basin.|||||Undivided; quartz sandstone and wacke; minor conglomerate, siltstone, shale, limestone, dolomite, chert and glauconitic sandstone.|
15983|Redcliff Pound Group|68733|6|Mentioned|p176 Fig.1, p188|||Murraba Basin.|||Includes the Munya and Lewis Range Sandstones (basal units).|||05-DEC-17
15983|Redcliff Pound Group|68994|4|Described|p20|Neoproterozoic|Neoproterozoic|Murraba Basin.|||Manyu Sandstone at base|Unconformably overlies Aileron Province rocks.||
15983|Redcliff Pound Group|69003|6|Mentioned|p5, p61|||Murraba Basin, Granites-Tanami Orogen.||||||
15983|Redcliff Pound Group|69031|6|Mentioned|p4, p6 Fig.4, p8|||Murraba Basin.|||Munyu Sandstone.|||
15983|Redcliff Pound Group|69099|4|Described|GEOL_LUT_CSV files + geochron files|Cryogenian|Cryogenian|Murraba Basin|||Includes Lewis Range Sandstone.||Quartz sandstone and wacke; minor conglomerate, siltstone, shale, limestone, dolomite, chert, and glauconitic sandstone.|04-AUG-15
15983|Redcliff Pound Group|69288|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Murraba Basin.|||Munyu, Erica Sandstones; Murraba Formation.|||
15983|Redcliff Pound Group|69432|5|Briefly described|p17:2, 13|Neoproterozoic|Neoproterozoic|Murraba Basin. Generally shallow-dipping.||||Overlies Birrindudu Group.||12-JUL-16
15983|Redcliff Pound Group|69437|5|Briefly described|p22:6|Cryogenian|Cryogenian|Murraba Basin, Centralian A Superbasin. Supersequence 1.|||Munyu, Erica Sandstones; Murraba Formation.||Almost exclusively siliciclastic sedimentary rocks.|12-JUL-16
15983|Redcliff Pound Group|69440|5|Briefly described|p25:1|||Murraba Basin. Siliciclastic sediments. Probably over 2000m thick.|||Munyu, Erica Sandstones; Murraba Formation.|||12-JUL-16
15983|Redcliff Pound Group|69453|6|Mentioned|p37:1|||Murraba Basin.||||Is inferred to be overlain unconformably by Lucas Formation.||12-JUL-16
15983|Redcliff Pound Group|69508|5|Briefly described|Map legend.|Neoproterozoic|Paleoproterozoic|Murraba Basin.|||Munya Sandstone.|||
15983|Redcliff Pound Group|69587|4|Described|GEOL_LUT_CSV files + geochron files|Cryogenian|Cryogenian|Of Murraba Basin, Centralian Superbasin. Events: Alice Springs Orogeny. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|830-810 Ma (inferred)||Includes Lewis Range Sandstone.||Quartz sandstone and wacke; minor conglomerate, siltstone, shale, limestone, dolomite, chert, and glauconitic sandstone|
15983|Redcliff Pound Group|69634|4|Described|GEOL_LUT_CSV files||Neoproterozoic|Of Murraba Basin, Centralian Superbasin. Events: Alice Springs Orogeny. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 500k_interpgeop_lut.csv.|830-810 Ma (Inferred)||Includes Lewis Range Sandstone.||Undivided; quartz sandstone and wacke; minor conglomerate, siltstone, shale, limestone, dolomite, chert, and glauconitic sandstone|
15983|Redcliff Pound Group|69673|6|Mentioned|p187|||More than 2000m thick.|||Includes Munyu Sandstone, Muriel Range Sandstone, Murraba Formation, Erica Sandstone|||
15983|Redcliff Pound Group|70129|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Murraba Basin, Centralian Superbasin.|||Lewis Range Sandstone, Murraba Formation.|||
15983|Redcliff Pound Group|70130|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Murraba Basin, Centralian Superbasin.|||Lewis Range, Erica Sandstones; Murraba Formation.||Dominantly sandstones; also conglomerate, siltstone and mudstone; minor limestone.|
15983|Redcliff Pound Group|70141|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Murraba Basin, Centralian Superbasin.|830-810 Ma.||Lewis Range Sandstone.|Overlies Birrindudu Group.||
15983|Redcliff Pound Group|70142|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Murraba Basin, Centralian Superbasin.|830-810 Ma.||Lewis Range Sandstone.|||
15983|Redcliff Pound Group|70143|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Murraba Basin, Centralian Superbasin. Unclear if age range refers to the Group or just the Lewis Range Sandstone.|830-810 Ma.||Lewis Range Sandstone.|||
15983|Redcliff Pound Group|70154|4|Described|100k_interpgeop_lut.csv|Cryogenian|Neoproterozoic|See also 500k_interpgeop_lut.csv.|810-1000 Ma||Includes Lewis Range Sandstone||Quartz sandstone and wacke; minor conglomerate, siltstone, shale, limestone, dolomite, chert, and glauconitic sandstone.|
15983|Redcliff Pound Group|70826|6|Mentioned|p5 tbl 2|||Centralian Superbasin.||||||20-APR-20
15983|Redcliff Pound Group|70851|6|Mentioned|p19|||||||||
15983|Redcliff Pound Group|70852|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Murraba Basin.|||Muriel Range Sandstone.|||
15983|Redcliff Pound Group|71080|1|Redefined|p1, p4, 6, 20, 27-28,  29, 31,32  36-38|Cambrian|Ediacaran|Murraba Basin. Previously believed to be Tonian.The term was first used by Blake et al (1973) and subsequently defined in Blake et al (1979). Originally this group contained the Lewis Range, Muriel Range and Munyu sandstone overlain by Murraba Formation and the Erica Sandstone. Outcrop is restricted to eastern STANSMORE and southeastern LUCAS 1;250k map sheets. Is expressed in outcrop as low strike ridges and strike valleys. This group is gently to tightly folded and faulted but not metamorphosed. At least 2000 m thick, as originally defined. Now restricted to Redcliff Pound area - c 1500 m thick, and supersequences 3 & 4 of the Centralian Superbasin.  Age inferred for regional correlations. Hosts Arumberia and probable tubular body fossils. Distinguishing and identifying features are discussed.|||Includes Murraba Formation, Erica Sandstone.|Unconformable over mostly concealed, unnamed units (likely supersequence 1-2 ). Unconformably overlain by Paleozoic outliers of Canning Basin in WA and Antrim Plateau Volcanics in NT.|Murraba Formation: Sandstone, siltstone, and minor carbonate and conglomerate deposited in shallow marine to deltaic environments. Erica Sandstone: predominantly sandstone deposited in deltaic, fluvial and eolian environments.|04-FEB-19
15983|Redcliff Pound Group|71267|4|Described|GEOL_LUT_CSV files|Cambrian|Cryogenian|Of Murraba Basin, Centralian Superbasin. Events: Alice Springs Orogeny (450-295 Ma). See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv.|650-510 Ma (inferred)||Includes Erica Sandstone, Lewis Range Sandstone.||Abundantly cross bedded and rippled medium grained quartz sandstone, minor sublithic sandstone, shale, siltstone, conglomerate, arkose, breccia; some convolute lamination and disturbed cross beds|
15983|Redcliff Pound Group|72034|5|Briefly described|500k_interpgeop16_lut|Cambrian|Cryogenian|Murraba Basin.|||||Quartz sandstone; minor conglomerate, siltstone, shale, carbonate and glauconitic sandstone.|
15983|Redcliff Pound Group|73445|5|Briefly described|p3, 6-8, 10, 12, 23-24, 29, 34-35|Cambrian|Neoproterozoic|See also p37-38, 41-47, 56, 65-118. Murraba Basin. Over 2,000m thick. Multi-element spider diagram. Regolith chemistry tabulated.|||Munyu, Lewis Range, Muriel Range, Erica Sandstones; Murraba Formation.|Unconformably overlies the Killi Killi Formation. Correlated with Heavitree Quartzite.|Sandstone, wacke; minor conglomerate, siltstone, shale, limestone, dolomite, chert, and glauconitic sandstone.|
16061|Reynolds Range Group|7821|5|Briefly described|p45-48, 61, 66|||Arunta Inlier. Tightly folded by the Wabudali Tectonic Phase (of the Strangways Orogeny). Exposed in narrow, major synclines.||||Unconformably overlies the Lander Rock beds. Is intruded by Yarunganyi Granite.|Shelf-type sediments.|
16061|Reynolds Range Group|7838|5|Briefly described|p70-71, 80-81, 83, 85-87|||Northern Arunta Inlier. Metamorphosed to granulite facies in the SE of the Range. Contains a lithic sandstone dated at 1785 +/- 15 Ma. Platform-style sediments; possibly a continental rift-related sequence.|1818 +/- 15 Ma to 1785 +/- 22 Ma.|||Overlies the Lander Rock beds basement. Is intruded by Warimbi Granite and Napperby Gneiss.||
16061|Reynolds Range Group|8222|5|Briefly described|Map Legend|||||||||
16061|Reynolds Range Group|9380|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block. Includes: Pine Hill Formation, Mount Thomas Quartzite.||||||
16061|Reynolds Range Group|11884|5|Briefly described|Map Legend|||Lower Proterozoic. Includes porphyry sills.|||Includes Pine Hill Formation and its Algamba Dolomite Member, Woodforde River Beds, and Mount Thomas Quartzite.|Unconformably overlies the Lander Rock Beds and Wickstead Creek Beds ?||
16061|Reynolds Range Group|22524|5|Briefly described|p35,table1p38|Statherian|Statherian|||||||
16061|Reynolds Range Group|22723|6|Mentioned|p259||Proterozoic|||||||
16061|Reynolds Range Group|22733|5|Briefly described|p301-4||Proterozoic|||||||
16061|Reynolds Range Group|22791|5|Briefly described|p54|||||||||
16061|Reynolds Range Group|23205|6|Mentioned|p318|Proterozoic|Proterozoic|Of the Arunta Complex.||||||28-NOV-06
16061|Reynolds Range Group|23316|5|Briefly described|p355|||Includes metamorphosed quartzites, pelites, marls and marbles.||||||07-FEB-07
16061|Reynolds Range Group|23361|6|Mentioned|10 Tab.1|||||||||
16061|Reynolds Range Group|23546|5|Briefly described|p573.|||||||||
16061|Reynolds Range Group|23556|5|Briefly described|p459|||||||||
16061|Reynolds Range Group|23733|5|Briefly described|p34 Fig.20|||Age: 1820-1780Ma.||||||
16061|Reynolds Range Group|23809|5|Briefly described|p41 Tb. 5, p45|||Intruded by the Coniston Schist.  Geological Province: Arunta Province.||||||
16061|Reynolds Range Group|24047|5|Briefly described|p7 Fig. 6, p9|Paleoproterozoic|Paleoproterozoic|Unconformably overlies the Lander Rock Beds.  Age: <1820Ma.  Geological Province: Arunta Province.||||||07-NOV-08
16061|Reynolds Range Group|24442|6|Mentioned|p3|||Geological Province: Arunta Province (north).||||||
16061|Reynolds Range Group|32480|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
16061|Reynolds Range Group|33102|4|Described|p439|||||||||
16061|Reynolds Range Group|33103|6|Mentioned|p14|||||||||
16061|Reynolds Range Group|35221|4|Described|Table.1|||||||||
16061|Reynolds Range Group|36473|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
16061|Reynolds Range Group|37058|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
16061|Reynolds Range Group|37462|5|Briefly described|Tab.4.VIII|||||||||
16061|Reynolds Range Group|39855|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
16061|Reynolds Range Group|39887|6|Mentioned|Fig.5|||||||||
16061|Reynolds Range Group|39888|6|Mentioned|Table 1|||||||||
16061|Reynolds Range Group|41964|5|Briefly described|p177|||||||||
16061|Reynolds Range Group|42146|5|Briefly described|p655|||||||||
16061|Reynolds Range Group|42217|4|Described|p409|||See also Fig.1||||||27-OCT-10
16061|Reynolds Range Group|42278|6|Mentioned|p42|||||||||
16061|Reynolds Range Group|42326|4|Described|p10|||||||||
16061|Reynolds Range Group|42401|5|Briefly described|p642|||||||||
16061|Reynolds Range Group|42504|5|Briefly described|p65|||||||||
16061|Reynolds Range Group|42643|6|Mentioned|p5|||||||||
16061|Reynolds Range Group|43275|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
16061|Reynolds Range Group|43568|6|Mentioned|p507|||||||||
16061|Reynolds Range Group|43631|3|Fully described|p9,10||Paleoproterozoic|Age: 1830-1800 Ma.||||||07-NOV-08
16061|Reynolds Range Group|43697|6|Mentioned|p27|||||||||
16061|Reynolds Range Group|43749|6|Mentioned|Fig.1,p6||Paleoproterozoic|||||||07-NOV-08
16061|Reynolds Range Group|44114|5|Briefly described|p317-318, 320-321|||Northern Arunta Inlier. Intertidal and subtidal sedimentary rocks. Metamorphosed at 1780-1770 Ma.|1820-1780 Ma; Collins and Williams,1995||||Platform-style sediments: quartzite-shale-carbonate successions; granulite facies metamorphism = orthoquartzite, calc-silicate rock, pelitic schist.|
16061|Reynolds Range Group|44158|4|Described|p11, Table.1|Paleoproterozoic|Paleoproterozoic|In the Arunta Inlier. Age: 1820 - 1790Ma. Includes Woodforde River beds, Pine Hill Formation and Mount Thomas Quartzite. Unconformably overlies Lander Rock beds; intruded by late granites.||||||05-MAY-10
16061|Reynolds Range Group|45148|6|Mentioned|p8|||||||||
16061|Reynolds Range Group|46864|6|Mentioned|p40|||||||||
16061|Reynolds Range Group|48992|1|Redefined|p45|Proterozoic|Proterozoic|||||||
16061|Reynolds Range Group|50369|5|Briefly described|p5.1, 24.2|||Intruded by Warimbi granite.||||||
16061|Reynolds Range Group|60681|5|Briefly described|Map legend|Statherian|Statherian|Quartzites, pelites, psammites, minor calcsilicates, minor basalts.  Age: 1805-1785Ma.  Geological Province: Aileron Province.||||||11-JAN-05
16061|Reynolds Range Group|60714|5|Briefly described|p121.|Statherian|Orosirian||c 1800 Ma|||Correlated with Hatches Creek Group.|Poorly sorted, matrix supported, polymict conglomerate 1-15 m thick; followed by transgressive quartzarenite facies 500m thick.|
16061|Reynolds Range Group|61208|6|Mentioned|p208|||||||||
16061|Reynolds Range Group|61309|6|Mentioned|p13 Fig. 2|||||||||
16061|Reynolds Range Group|61405|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes Mount Thomas Quartzite, Pine Hill Formation and undivided constituents. Geological Province: Arunta region - Aileron Province.||||||07-NOV-08
16061|Reynolds Range Group|62378|6|Mentioned|p23|Paleoproterozoic||||||||07-NOV-08
16061|Reynolds Range Group|62632|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Tanami/Arunta Region-Aileron Province.||||||23-DEC-09
16061|Reynolds Range Group|62633|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Region - Aileron Province||||||07-NOV-08
16061|Reynolds Range Group|62636|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Region - Aileron Province.|||Includes Pine Hill Formation and Mount Thomas Quartzite.|||15-APR-11
16061|Reynolds Range Group|62642|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Region - Aileron Province.||||||07-NOV-08
16061|Reynolds Range Group|63866|5|Briefly described|p93, p99|||Aileron Province.||||Unconformably overlies the Lander Package.||
16061|Reynolds Range Group|64068|5|Briefly described|p31-32|Paleoproterozoic|Paleoproterozoic|Northern Arunta Region.|1780 Ma.||||A shallow-marine to intertidal succession of quartzite, grading up into pelite and minor calc-silicate rock.|05-APR-12
16061|Reynolds Range Group|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Quartzite, quartz-mica schist.||||||09-DEC-08
16061|Reynolds Range Group|64722|5|Briefly described|Fig. 2 p3-6, p11|Statherian|Statherian|Siliciclastic rocks. Intruded by 1780 Ma granites. Metamorphosed to granulite facies from 1600-1580 Ma.||||Unconformably overlies Lander Package. Intruded by Napperby Gneiss, Coniston Schist.||11-APR-12
16061|Reynolds Range Group|64736|6|Mentioned|p222, p228|Statherian|Statherian|||||Overlies Lander Rock Formation unconformably.||30-APR-12
16061|Reynolds Range Group|64737|5|Briefly described|p231-2, Fig.2, p233 Fig.3, p238, p240-3||Orosirian|In Aileron Province. Interpreted to have been deposited in a shallow marine environment.|||Includes Mount Thomas Quartzite.||Package of quartzite, pelitic and psammitic schist, minor calc-silicate rock and rare basalt.|01-MAY-12
16061|Reynolds Range Group|64748|5|Briefly described|p277|Paleoproterozoic|Paleoproterozoic|~1800Ma; commences with a 1-15m thick matrix-supported polymict conglomerate||||||
16061|Reynolds Range Group|64956|6|Mentioned|p26|||||||||07-FEB-11
16061|Reynolds Range Group|65329|5|Briefly described|Map legend|Palaeoproterozoic|Palaeoproterozoic|Shown as older than Carrington Suite, Yulyupunyu granitic gneiss, younger than Lander Rock Formation, Ngadarunga Granite,  same age as Patmungala beds. Includes Pine Hill Formation, Woodforde River beds, Mount Thomas Quartzite||||||19-DEC-12
16061|Reynolds Range Group|65330|5|Briefly described|Map legend|Palaeoproterozoic|Palaeoproterozoic|Shown as older than Carrington Suite, Yulyupunyu granitic gneiss, younger than Lander Rock Formation, Ngadarunga Granite,  same age as Patmungala beds. Includes Pine Hill Formation, Woodforde River beds, Mount Thomas Quartzite||||||19-DEC-12
16061|Reynolds Range Group|65332|5|Briefly described|Map Legend|Palaeoproterozoic|Palaeoproterozoic|Includes Pine Hill Formation, Mount Thomas Quartzite. Shown as equivalent age to Nicker beds, older than Carrington Suite granites, younger than Lander Rock Formation.||||||02-FEB-10
16061|Reynolds Range Group|65335|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Aileron Province. Includes Pine Hill Formation and Mount Thomas Quartzite. Age: older than Yambah Event (1770-1760 Ma).||||||
16061|Reynolds Range Group|65338|5|Briefly described|p iv, pp20-21.|Paleoproterozoic|Paleoproterozoic|Probably correlates with Hatches Creek Group; close lithological comparison with succession of sandstone, stromatolitic carbonate and basalt in upper Wauchope Subgroup.|||Includes Mount Thomas Quartzite, Pine Hill Formation and Woodforde River Beds.|Overlies Lander Rock Formation.||
16061|Reynolds Range Group|65341|5|Briefly described|p2 Fig.2, p3. |Paleoproterozoic|Paleoproterozoic|Also includes Anira, Delmore, Mendip, Aileron and Nolans Dam Metamorphics; Wickstead Creek beds.|1780 Ma.||Includes Lander Rock Formation; Woolla, Bruna, Langford, Aloolya and Delny Gneisses; Ledan and Mount Freeling Schists; Utopia Quartzite; see Comments for remaining units.|||
16061|Reynolds Range Group|65343|5|Briefly described|p3 Fig.4|Paleoproterozoic|Paleoproterozoic|Arunta Region.||||||
16061|Reynolds Range Group|65358|5|Briefly described|p11, p13, p17-18|Statherian|Statherian|Shelf sediments and minor basalt. Unconformably overlies Lander Rock Formation. Dated at ~1780 Ma. In NW of Arunta Region; Aileron Province.||||||
16061|Reynolds Range Group|66767|5|Briefly described|p57|||Aileron Province.|c.1780 Ma.|||Correlated with Hatches Creek Group.||
16061|Reynolds Range Group|67163|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region; Aileron Province.|||Includes Mount Thomas Quartzite.|||20-OCT-11
16061|Reynolds Range Group|67164|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region; Aileron Province.|||Includes Mount Thomas Quartzite and Pine Hill Formation.|||
16061|Reynolds Range Group|67323|5|Briefly described|Eastern Australia Time-Space Plot; p30|||Arunta Inlier.|1798 +/- 2 Ma (maximum depositional age).||||Dominantly metamorphosed siliciclastic sedimentary successions intercalated with minor carbonates and calc-silicates.|
16061|Reynolds Range Group|67430|5|Briefly described|p9-10|Paleoproterozoic|Paleoproterozoic|Aileron Province.|~1785 (MDA) - ~1780 (minimum age) Ma.|||Unconformably overlies Lander Rock beds.|Metaquartzite, slate, schist and marble.|
16061|Reynolds Range Group|67565|6|Mentioned|p5 Fig.3.|||Aileron Province.||||||
16061|Reynolds Range Group|67892|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Arunta Region; Aileron Province.|||Includes Mount Thomas Quartzite and Pine Hill Formation.|||
16061|Reynolds Range Group|68316|6|Mentioned|p782, p783 Fig.4|Paleoproterozoic|Paleoproterozoic|Amadeus Basin. Geochronology by Williams et al (1996); Rubatto et al. (2001).|c. 1.80-1.78 Ga|||||
16061|Reynolds Range Group|68832|5|Briefly described|p55|||Aileron Province, Arunta Region.|~1780 Ma|||May be similar age to Nyirripi beds.||
16061|Reynolds Range Group|68998|5|Briefly described|p13-14|||Several maximum depositional ages given.|||Mount Thomas Quartzite.|Is intruded by Coniston Schist.||
16061|Reynolds Range Group|69003|6|Mentioned|p31|Paleoproterozoic|Paleoproterozoic|May correlate with Lake McKay Quartzite (Aileron Province, WA).|< 1798 +/- 10 Ma (maximum deposition age).|||||
16061|Reynolds Range Group|69031|5|Briefly described|p4, p7|||Aileron Province, Arunta Orogen. Geochronology by Claoue-Long et al. (2008).|1798 +/- 10 Ma (maximum depositional age).|||May correlate with Lake Mackay Quartzite.||
16061|Reynolds Range Group|69226|4|Described|p239-254|Statherian|Orosirian|Reynolds-Anmatjira Ranges region. Metamorphism detailed. Deformations described.|c.1812-1785 Ma.||Mount Thomas Quartzite.|Overlies Lander Rock, and Mount Stafford, Beds. Intruded by Warimbi and Coniston Schists and Napperby Gneiss.|A variably metamorphosed, shallow-marine succession of a basal conglomerate and quartz sandstones, siltstones, arkoses and carbonates.|
16061|Reynolds Range Group|69228|5|Briefly described|p358-359, p361-370, p372, p374-375|Paleoproterozoic|Paleoproterozoic|Arunta Inlier. Intruded by granites. Contact metamorphosed at 1.78 Ga. Lithology, fluid flow and metamorphism described in detail.|<1.80 Ga.|||Is intruded by Napperby Gneiss.|Basal quartzite; a lower unit of dominantly calc-pelites, a unit of pelitic and psammitic rocks, and an upper discontinuous calc-silicate unit dominated by marble.|
16061|Reynolds Range Group|69288|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region, Aileron Province.|||Includes Mount Thomas Quartzite.|||30-NOV-16
16061|Reynolds Range Group|69417|6|Mentioned|p2:5|Orosirian|Orosirian|N and W Aileron Province.||||||12-JUL-16
16061|Reynolds Range Group|69425|6|Mentioned|p10:4|||Proposed part-correlation with the Hatches Creek Group has been questioned by Claoue-Long.||||||12-JUL-16
16061|Reynolds Range Group|69427|4|Described|p12:2-3, 8, 13, 18, 25-28, 32-33, 41|Statherian|Statherian|Aileron Province. Best exposed in Reynolds and Wabudali Ranges. Fig.12.24 presents the Woodforde River and Wickstead Creek beds, Mount Dunkin and Mount Freeling Schists, also as Members of this unit. Various detrital zircon ages given. Is intruded by Napperby Gneiss and Coniston Schist which have identical SHRIMP U-Pb age of 1780 +/- 10 Ma (Collins and Williams, 1995; Smith, 2001). Monazite and metamorphic zircon ages are consistently in the range 1590-1560 Ma.|c.1780 Ma.||Mount Thomas Quartzite; Pine Hill Formation; Woodforde River, Wickstead Creek beds.|Unconformably overlies Lander Rock Formation. Is intruded by Carrington Suite, Wabudali Granite, Napperby Gneiss and Coniston Schist.||12-JUL-16
16061|Reynolds Range Group|69431|5|Briefly described|p16:1|||Arunta Region. Possible correlative of Hatches Creek Group and, by inference, Tomkinson Creek Group.||||Age-equivalent of Birrindudu Group.||12-JUL-16
16061|Reynolds Range Group|69508|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region, Aileron Province. Six un-named subunits are mapped separately.|||Mount Thomas Quartzite.||Undivided sedimentary rocks comprising muscovite schist, muscovite-biotite schist, quartzite, muscovite-biotite-andalusite schist, amphibolite, minor calc-silicate.|
16061|Reynolds Range Group|69917|6|Mentioned|p117|||||||||
16061|Reynolds Range Group|69937|6|Mentioned|p27, p30|||Possible source of some zircons in the Cyclops and Waldo Pedlar Members of the Pertatataka Formation.|c.1780 Ma.|||||
16061|Reynolds Range Group|70301|5|Briefly described|p7, p11, p16, p22|||Mentioned as having ages typical of 2394-1974 Ma zircons occurring in Wangala Granite. [But] on p22 the authors state that their age of 1773 +/- 4 Ma (for Wickstead Creek beds) is similar to those recorded from Reynolds Range Group: c.1785 Ma, 1798 Ma and 1779 Ma.||||Is intruded by Wangala Granite.|Metasedimentary rocks.|
16061|Reynolds Range Group|70376|5|Briefly described|p832, p833, p833 fig 2, p847, p849-850|Paleoproterozoic|Paleoproterozoic|Shallow marine metasediments. Forms a covering sequence over ca 1800 Ma magmatics. Deposition associated with back arc basin development. Grouped with informal Cadney metamorphics in Fig 1.|1799 Ma - 1778 Ma||Includes Mount Thomas Quartzite.|Unconformably overlies Lander Rock Formation, intruded by Napperby Gneiss|Schist, slate, siltstone, quartzite, amphibolite, calc-silicate; syn-depositional felsic units interpreted to be rhyolitic flows.|
16061|Reynolds Range Group|70554|6|Mentioned|p798|Paleoproterozoic|Paleoproterozoic|Geologial province: Aileron province. Age from Claoue-Long et al., 2008). Underwent high-grade (to granulite-facies) metamorphism during Chewnings Orogeny and emplacement of late-metamorphic pegmatites (Collins and Williams, 1995).|~1785 Ma|||||
16061|Reynolds Range Group|70739|6|Mentioned|p540||||1810-1780 Ma.|||||
16061|Reynolds Range Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
16061|Reynolds Range Group|71348|5|Briefly described|p201,217|Orosirian|Orosirian|Geological province: Aileron Province, Arunta Region. Maximum depositional age c. 1780 Ma (Hollis et al., 2013; Scrimgeour, 2013; Rosel et al.,2014).|< 1780 Ma.|||Underlain unconformably by Lander Rock Formation.||
16061|Reynolds Range Group|71350|6|Mentioned|p7|||Aileron Province.|||Includes the Mount Thomas Quartzite.|||
16061|Reynolds Range Group|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen.|||Pine Hill FZ.||Amphibolite- to granulite-facies metapelite, migmatitic granulite, pelitic gneiss.|
16061|Reynolds Range Group|71858|4|Described|p5-p6, p30, p69|||Aileron Province. Outcrops intermittently from the Reynolds Range in NAPPERBY to LAKE MACKAY.|ca. 1780 Ma||Includes the Wickstead Creek beds, Pine Hill Formation and the Mount Thomas Quartzite.|Unconformably overlies the Lander Rock Formation. Intruded by the Wangala Granite.||
16061|Reynolds Range Group|72516|6|Mentioned|p7|||Aileron Province.||||||
16061|Reynolds Range Group|73399|6|Mentioned|p2-4, p7, p9-11, App.E|Statherian|Statherian|Protolith reflects a shallow marine setting. May have undergone a single, long-lived (190 Myr) metamorphic event.|ca. 1800 to 1780 Ma||Pine Hill Formation|Unconformably underlain by the Lander Rock Formation.|May include quartzite, orthoquartzite, and shale.|
16061|Reynolds Range Group|74204|5|Briefly described|p2|Statherian|Orosirian||1810-1780 Ma||||Primarily quartzite, calc-silicate, and pelite units.|
16087|Riddock Amphibolite|23844|3|Fully described|p44|Cambrian|Neoproterozoic III|Of the Harts Range Group. Geological Province: Arunta Province. Max Thickness: <2000m. Name used interchangeably with Riddock Amphibolite Member in this study. See also Fig.26||||||28-NOV-06
16087|Riddock Amphibolite|34488|6|Mentioned|p8|||||||||28-FEB-11
16087|Riddock Amphibolite|36308|6|Mentioned|p211|||||||||
16087|Riddock Amphibolite|44964|14|Not recorded|p.39,49|||||||||
16087|Riddock Amphibolite|45003|14|Not recorded|p260|||See also Lexicon.||||||28-NOV-06
16087|Riddock Amphibolite|48880|14|Not recorded|Not recorded|||||||||
16087|Riddock Amphibolite|50246|5|Briefly described|p8, p11|||Age: 734+/-44Ma (zircon). High grade metamorphic rocks - garnetiferous amphibolite interlayered with garnet quartz-feldspathic gneiss, biotite gneiss, garnet-biotite gneiss, sillimanite gneiss and plagioclase-rich gneiss. Max.||||||07-FEB-11
16087|Riddock Amphibolite|60668|5|Briefly described|p12, p2 Tb. 1|||Volcano-sedimentary sequence comprising folded concordant mafic sheets within laterally continuous pelitic, calcareous and quartzose schists and gneisses of the Irindina Gneiss. Thickness of bodies range up to 2km.||||||
16087|Riddock Amphibolite|62595|4|Described|p15, p38 Figs.23 & 24.|Cryogenian|Cryogenian|E-W folds resulted from N-S shortening associated with Alice Springs Orogeny. Age based on analysis of zircon cores; rims have an age of 461 +/- 6 Ma reflecting the Larapinta Event.|734 +/- 44 Ma (Claoue-Long and Hoatson 2005).|Unit in Harts Range Meta-Igneous Complex.|||Garnetiferous para-amphibolite interlayered with garnet quartzofeldspathic gneiss, biotite gneiss, garnet-biotite gneiss, sillimanite gneiss and plagioclase-rich gneiss.|
16087|Riddock Amphibolite|64337|5|Briefly described|pp374-375|||Recent geochronological results are discussed. See also Mount Riddock Amphibolite (p375 Fig. 2).||Of Irindina Gneiss.|||Major thick metabasic rocks.|
16087|Riddock Amphibolite|64574|6|Mentioned|p705 Fig. 2|Paleozoic|Paleozoic|||||||
16087|Riddock Amphibolite|69917|4|Described|p198-199, 175, 178, 184, 190, 195, 196|Ordovician|Cambrian|Eastern Arunta Region, Irindina Province. U/Pb LA-ICPMS zircon dating, Hf analytical data. Dating gave 206Pb/238U age of 451+/-3 Ma, which is interpreted to reflect metamorphic zircon growth and/or complete recrystallization of zircon during the early Alice Springs Orogeny.|451+/-3 Ma metamorphic|||Cross cut by Entire Gneiss. Intimately associated with Leprechaun Gneiss. Intrudes Spriggs Gneiss.|Includes voluminous tholeiitic, metagabbroic, metadoleritic and meta-ultramafic rocks. Metagabbro sampled.|
16087|Riddock Amphibolite|71592|5|Briefly described|Appendix A.|||Arunta Orogen.|476+/-3.8 Ma (SHRIMP U-Pb zircon).||||Metabasite, metapelite, composite amphibolite belt.|
16104|Ringwood Member|9199|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Pertatataka Formation.  Dolomite, calcarenite, siltstone.  Geological Province: Amadeus Basin.||||||
16104|Ringwood Member|22506|6|Mentioned|p130 Fig.4|Cryogenian|Cryogenian|||||||
16104|Ringwood Member|22649|6|Mentioned|p 152|Neoproterozoic|Neoproterozoic|Of the Aralka Formation.||||||28-NOV-06
16104|Ringwood Member|22762|6|Mentioned|p378|Neoproterozoic|Neoproterozoic|Of the Aralka Formation.||||||28-NOV-06
16104|Ringwood Member|23250|5|Briefly described|p1124  Fig.2||Cryogenian|Of Aralka Formation. Correlate of Brighton Limestone and Sunderland Formation.||||||28-NOV-06
16104|Ringwood Member|30258|6|Mentioned|Fig.2|||Proterozoic. Member of Pertatataka Formation.||||||28-NOV-06
16104|Ringwood Member|31022|6|Mentioned|Fig. 4|||||||||
16104|Ringwood Member|32720|6|Mentioned|Table 1|||Of the Pertatataka Fm.||||||28-NOV-06
16104|Ringwood Member|32722|6|Mentioned|Fig.3|||Adelaidean. Stromatolitic member.||||||28-NOV-06
16104|Ringwood Member|34111|5|Briefly described|Table 1|||See also Table 4. Precambrian||||||
16104|Ringwood Member|34202|6|Mentioned|p1058|||||||||
16104|Ringwood Member|34488|5|Briefly described|Table 1|||Proterozoic. See p10.||||||28-NOV-06
16104|Ringwood Member|34579|4|Described|Table 1|||||||||
16104|Ringwood Member|35102|6|Mentioned|p19|||||||||
16104|Ringwood Member|35805|6|Mentioned|Fig.3|||||||||
16104|Ringwood Member|38157|6|Mentioned|p272|||See also Table VI.||||||
16104|Ringwood Member|38885|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
16104|Ringwood Member|39210|6|Mentioned|p37|||||||||
16104|Ringwood Member|39583|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
16104|Ringwood Member|39898|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of the Aralka Formation. Calcarenite; limestone and dolomite, both oolitic and stromatolitic in part. Geological Province: Amadeus Basin.||||||14-FEB-06
16104|Ringwood Member|40740|5|Briefly described|p12|||||||||
16104|Ringwood Member|40852|6|Mentioned|Fig.3.2|||||||||
16104|Ringwood Member|40906|6|Mentioned|Fig.9|||||||||
16104|Ringwood Member|41190|6|Mentioned|Fig.4|||||||||
16104|Ringwood Member|41270|6|Mentioned|Table 1|||||||||
16104|Ringwood Member|41717|6|Mentioned|Fig.2|||||||||
16104|Ringwood Member|41957|6|Mentioned|p73|||||||||
16104|Ringwood Member|42082|6|Mentioned|Fig.3 P323|||||||||
16104|Ringwood Member|42504|5|Briefly described|Table 4 p73|||||||||03-DEC-18
16104|Ringwood Member|42886|5|Briefly described|Fig.2 p219|||Of the Aralka Formation.||||||03-DEC-18
16104|Ringwood Member|42940|5|Briefly described|Plate 9|||||||||
16104|Ringwood Member|43595|6|Mentioned|p550|||||||||
16104|Ringwood Member|44335|4|Described|p.7||Proterozoic|Table 1. p.8.||||||
16104|Ringwood Member|44336|14|Not recorded|map legend||Proterozoic|SG/53-3. Member of Pertatataka Formation.||||||28-NOV-06
16104|Ringwood Member|44433|14|Not recorded|map legend||Proterozoic|||||||
16104|Ringwood Member|45041|4|Described|p37|||Proterozoic. Of the Pertatataka Formation.||||||28-NOV-06
16104|Ringwood Member|46865|6|Mentioned|Table.1|||||||||
16104|Ringwood Member|48890|2|Defined|p.26,27||Neoproterozoic|See also Tb.1,Tb.2,Fig.4, Pl.10. Part of Pertatataka Formation. U.Proterozoic.||||||28-NOV-06
16104|Ringwood Member|48963|6|Mentioned|Fig.2|||||||||
16104|Ringwood Member|60547|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Pertatataka Formation. Geological Province: Amadeus Basin. Dolomite, calcarenite, siltstone.||||||
16104|Ringwood Member|60549|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of the Aralka Formation.  Calcarenite; limestone, dolomite (some oolitic or stromatolitic).||||||
16104|Ringwood Member|61732|5|Briefly described|p94|||Formerly part of the Pertatataka Formation, now redefined within the Aralka Formation.||||||07-FEB-11
16104|Ringwood Member|62379|6|Mentioned|p29|||||||||
16104|Ringwood Member|62428|5|Briefly described|p351 Tb. 6|Early Cambrian|Neoproterozoic III|Palaeomagnetic data.||||||10-FEB-09
16104|Ringwood Member|62903|6|Mentioned|p730 Fig.1|||Amadeus Basin. Presented in figure as Ringwood.||Aralka Formation||||
16104|Ringwood Member|64797|5|Briefly described|p156 Fig.6, p157, p168 Tb.11|||||Unit in Aralka Formation.||||
16104|Ringwood Member|69438|5|Briefly described|p23:16, 52|Cryogenian|Cryogenian|Amadeus Basin. The same "clast-supported" stromatolites occur in Inindia beds near Mount Conner. Mentioned as Ringwood member of Pertatataka Formation in ILLOGWA CREEK map area.||Aralka Formation.|||Dominated by dolostone and limestone that is in part pisolitic and stromatolitic. Contains the columnar stromatolite Tungussia inna Walter, and distinctive and diagnostic  "clast-supported" stromatolites.|12-JUL-16
16104|Ringwood Member|69606|6|Mentioned|p12|||||||||
16104|Ringwood Member|69673|5|Briefly described|p74|||||Aralka Formation|||Dominated by dolostone and limestone that is partly pisolitic and stromatolitic.|
16104|Ringwood Member|69937|5|Briefly described|p14|Neoproterozoic|Neoproterozoic|Amadeus Basin.||Aralka Formation.|||Mainly limestone and dolostone with distinctive stromatolites.|
16104|Ringwood Member|70416|5|Briefly described|p64, p65 Fig.2, p72, p74, p77, p80|Cryogenian|Cryogenian|Defined as part of Aralka Formation by Preiss et al. (1978). Locally recognized. Contains the holotype S357 of the stromatolite Tungussia inna, described (Walter, 1972) when this unit was included in the Pertatataka Formation.||Aralka Formation.|||Stromatolitic dolostone and calcarenite.|
16104|Ringwood Member|71001|6|Mentioned|p18 Fig.2|Cryogenian|Cryogenian|Amadeus Basin. Marine deposits.||Aralka Formation.||||
16104|Ringwood Member|71344|6|Mentioned|p1093 Fig 1|Cryogenian|Cryogenian|||Of Aralka Formation.||||
16104|Ringwood Member|71801|6|Mentioned|p230, p232, p234-p235, p237|Cryogenian|Cryogenian|Amadeus Basin.||Aralka Formation||Overlies the Areyonga Formation. Overlain by the Limbla Member.||
16104|Ringwood Member|71841|5|Briefly described|p1|Cryogenian|Cryogenian|Of Amadeus Basin.||Unit of Aralka Formation.||||
16104|Ringwood Member|71842|4|Described|iii,p2-3,5,7|Cryogenian|Cryogenian|Of Amadeus Basin. Nomenclature after Edgoose 2013 (NE Amedeus, NT). Occurs as small discrete exposures amongst recent colluvium, alluvium and calcrete between the Conner Member (Areyonga Formation) and Mount Conner. Contains large domal stromatolite  bioherms (Atilanya fennensis; Allen et al 2015) ~1.5m across; diagnostic of the Ringwood Member and acts as an important bisotratigraphic marker.||||Unit within lower part of Aralka Formation.|Well laminated, buff, stromatolitic dolostone, interbedded with lenticular intraclast breccia.|
16104|Ringwood Member|72369|5|Briefly described|p10|||Of Amadeus Basin.||Unit of Aralka Formation.|||Limestone and dolostone, and has distinctive stromatolites.|
16104|Ringwood Member|72375|4|Described|p19|Neoproterozoic|Neoproterozoic|Of Amadeus Basin. Contains distinctive stromatolite forms Tungussia inna (Walter 1972) and Atilyana fennensis (Allen et al 2015).||Unit of Aralka Formation.||Overlain by Limbla Member. Underlain by Areyonga Formation.|Limestone and dolostone.|
16104|Ringwood Member|72489|5|Briefly described|p3, p5 Fig.4, p6, p7-p9, p12|Cryogenian|Cryogenian|Located in the eastern Amadeus Basin. Non-glacial interval.||Aralka Formation||Overlain by Limbla Member.|Includes limestone.|
16104|Ringwood Member|72601|5|Briefly described|p3-5, p7, p17|Cryogenian|Cryogenian|Amadeus Basin. Defined by Wells et al. (1967). Verdel and Campbell (2017) referred to all of the Aralka Formation beneath the Limbla Member (including a cap carbonate directly overlying the Areyonga Formation) as the Ringwood Member; however, this convention was not adopted in the current publication. Possibly correlates with Brighton Limestone in the Adelaide Rift Complex, but this inference is tenuous.||Aralka Formation||Underlain and overlain by undifferentiated Aralka Formation siltstone.|Carbonate dominated and commonly stromatolitic.|
16104|Ringwood Member|73085|5|Briefly described|piii, p1, p3, p5, p15-16, p19, p26-27|Cryogenian|Cryogenian|Amadeus Basin. Contains diagnostic stromatolite taxa. Has a basin-wide distribution[?]. Lithology is here described from a 37.1-metre-thick equivalent in drillhole BR05DD01. Recognised [in drillhole BR05DD01] based on the presence of carbonate interbeds and Tungussia inna stromatolites.||Aralka Formation|||Dark grey to black siltstone and mudstone with buff to grey calcareous siltstone and carbonate intervals with planar and wavy laminae; carbonate intervals are variably stromatolitic.|
16104|Ringwood Member|73086|1|Redefined|[See comments].|Cryogenian|Cryogenian|[Redefined herein. See also definition card, ASUD]. Re definition of unit. Characterised by the occurrence of lenticular intraclast breccia, clast supported stromatolites. Amadeus Basin. Type section: Halfway Dam. Key localities: Waldo Pedlar Bore, Limbla Syncline. Clast-supported stromatolites are a diagnostic feature of the unit. Previously part of the Pertatataka Formation. Commonly exhibits 'tramline' outcrop expression. Substantially lesser siliciclastic component than Limbla Member. Disconformably underlain by Wallara Formation in places. Transitional from underlying Areyonga Formation in places. p: 5-6, 56-57, 61-62, 71-91, 93, 96, 98, 122, 143, 160-166, App 2.|658 +/- 5 Ma, 657.2 +/- 5.4 Ma Re-Os|Aralka Formation||Transitional boundaries with the parant unit (Aralka Formation). Correlates to Brighton Limestone, Rinkabeena Shale, Inindia Beds[beds?] and possibly the Boord Formation.|Dominated by dolostone and limestone that is stromatolitic and pisolitic in part. Beds of calcarenite and lenticular intraclast breccia dolostone are common, minor siltstone was also observed.|
16104|Ringwood Member|73088|6|Mentioned|p1|Cryogenian|Cryogenian|Amadeus Basin, northeast.||Aralka Formation||||
16104|Ringwood Member|73180|6|Mentioned|p48 Fig.1|Neoproterozoic|Neoproterozoic|Amadeus Basin.||Aralka Formation||Conformably underlies the Limbla Member.||
16107|Rinkabeena Shale|24111|5|Briefly described|p216|Neoproterozoic|Neoproterozoic|Overlies the Nabarula Formation (Naburula). Geological Province: Ngalia Basin.  See also p215 Fig. 11.||||||19-DEC-12
16107|Rinkabeena Shale|36898|6|Mentioned|Fig.4|||||||||
16107|Rinkabeena Shale|37462|4|Described|Table 4.IX|||||||||
16107|Rinkabeena Shale|37537|5|Briefly described|Map legend|Adelaidean|Adelaidean|Green shale; interbedded siltstone. Geological Province: Ngalia Basin.||||||14-FEB-06
16107|Rinkabeena Shale|37928|6|Mentioned|Fig.4|||||||||
16107|Rinkabeena Shale|38157|6|Mentioned|Table VII|||||||||
16107|Rinkabeena Shale|38733|6|Mentioned|Table 4|||||||||
16107|Rinkabeena Shale|38945|6|Mentioned|Fig.1|||||||||
16107|Rinkabeena Shale|39565|6|Mentioned|p33|||||||||
16107|Rinkabeena Shale|40906|6|Mentioned|Fig.9|||||||||
16107|Rinkabeena Shale|41717|6|Mentioned|Fig.19|||||||||
16107|Rinkabeena Shale|42059|5|Briefly described|Fig.2|||See also p133.||||||28-NOV-06
16107|Rinkabeena Shale|42504|5|Briefly described|Table 4 P73|||||||||
16107|Rinkabeena Shale|42643|6|Mentioned|Fig.4 P19|||||||||
16107|Rinkabeena Shale|43275|5|Briefly described|Map Legend||Neoproterozoic|||||||
16107|Rinkabeena Shale|43595|5|Briefly described|p548,Fig.5-33,549||Adelaidean|||||||
16107|Rinkabeena Shale|43631|6|Mentioned|p25|||||||||
16107|Rinkabeena Shale|43749|6|Mentioned|Fig.1,p6||Neoproterozoic|||||||
16107|Rinkabeena Shale|44158|4|Described|p29 Table.2|Neoproterozoic|Neoproterozoic|In the Ngalia Basin.||||||28-NOV-06
16107|Rinkabeena Shale|45155|2|Defined|p26|Adelaidean|Adelaidean|||||||
16107|Rinkabeena Shale|46865|2|Defined|p52|late Adelaidean|late Adelaidean|||||||
16107|Rinkabeena Shale|46903|6|Mentioned|Fig.5|||Correlation chart||||||
16107|Rinkabeena Shale|61385|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Green to grey shale, minor siltstone.  Geological Province: Ngalia Basin.||||||
16107|Rinkabeena Shale|65232|5|Briefly described|p70|||With Naburula Formation, both overlie both Albinia Formation and Mount Vaughan Quartzite [misspelling of Vaughan Springs Quartzite]. Disconformably underlies Mount Doreen Formation. Shale and siltstone. Geol. Prov: Ngalia Basin.||||||09-FEB-10
16107|Rinkabeena Shale|65329|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of Ngalia Basin. Shown as younger than Nabarula Formation, older than Mount Doreen Formation. Green to grey shale, minor siltstone||||||28-SEP-11
16107|Rinkabeena Shale|65330|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of Ngalia Basin. Shown as younger than Nabarula Formation, older than Mount Doreen Formation. Green to grey shale, minor siltstone||||||28-APR-10
16107|Rinkabeena Shale|65342|6|Mentioned|p6.|||Ngalia Basin. Max. thickness at least 448 m. Seen as having potential as an insulating layer for geothermal energy.||||Overlies Patmungala beds. Is overlain by Mount Doreen Formation.||
16107|Rinkabeena Shale|67872|5|Briefly described|p13, p15|Neoproterozoic|Neoproterozoic|Ngalia Basin. Part of the M2 mega-sequence of Lindsay (2002).||||||
16107|Rinkabeena Shale|68270|5|Briefly described|p680,683|Cryogenian|Cryogenian|Ngalia Basin.||||Underlain by Naburula Formation.||
16107|Rinkabeena Shale|69437|5|Briefly described|p22:4-5, 7, 16|Cryogenian|Cryogenian|Ngalia Basin, Centralian A Superbasin. Supersequence 2. May have petroleum source rock potential.||||Overlies Naburula Formation.|Shale and minor siltstone.|12-JUL-16
16107|Rinkabeena Shale|69439|3|Fully described|p24:2-4, 7-8, 13-14, 16, 18, 20-21|Cryogenian|Cryogenian|Preiss et al. (1978). Previously (Wells, 1972) included in Mount Doreen Formation. Ngalia Basin, Centralian A Superbasin. Supersequence 2. 100m thick in the type section in the headwaters of Patmungala Creek in the Naburula Hills. Has some hydrocarbon source rock potential; possibly a post-mature source for gas. Contains potential reservoirs. Has potential for likely seals for Vaughan Springs Quartzite reservoirs.||||Overlies Patmungala beds (basement). Is overlain (probably) disconformably by Mount Doreen Formation. Equivalent to the Aralka Formation.|Distinctive green and grey-green, thinly bedded, partly micaceous shale and minor siltstone, and local thin beds of pale dolomitic shale. Locally pyritic and cut by thin calcite and quartz veins.|12-JUL-16
16107|Rinkabeena Shale|69673|5|Briefly described|p106, p107 fig 85|Neoproterozoic|Neoproterozoic|Up to 450m thick. Source rock potential.||||Overlies Naburula Formation, overlain by Mount Doreen Formation|Thinly bedded, partly micaceous shale and minor siltstone and local thin beds of pale dolomitic shale.|
16107|Rinkabeena Shale|71080|5|Briefly described|p31|||Ngalia Basin. Locally more than 900 m thick. Flared gas from Davis 1.||||Correlated with Aralka Formation, Amadeus Basin.|Grey to black shale.|
16107|Rinkabeena Shale|72601|6|Mentioned|p5, p8|||Correlative[?] with Aralka Formation.||||||
16107|Rinkabeena Shale|73086|6|Mentioned|p72, p78, p91, p161, p164-165|||Ngalia Basin.||||Correlates to Aralka Formation.|Includes cap dolostone.|
16118|Rising Sun Conglomerate|22954|6|Mentioned|Fig3p9|Early Cambrian|Early Cambrian|||||||
16118|Rising Sun Conglomerate|23410|5|Briefly described|Map Legend|Early Cambrian|Neoproterozoic|Conglomerate and sandstone; monomictic and polymictic orthoconglomerate; channel cross-bedded. Quartz arenite; predominantly medium bedded, parallel-, or cross-bedded.||||||02-NOV-05
16118|Rising Sun Conglomerate|23733|5|Briefly described|p31|Cambrian|Neoproterozoic|Geological Province: Georgina Basin.  See also p32 Fig. 19.||||||
16118|Rising Sun Conglomerate|23809|6|Mentioned|p27 Fig. 25|||Geological Province: Tennant Inlier.||||||29-NOV-04
16118|Rising Sun Conglomerate|24172|3|Fully described|p53|Cambrian|Neoproterozoic|Max. thickness: ~60m. Represents proximally eroded remnants of Hatches Creek Group or Tomkinson Creek Subgroup stratigraphy. Correlated with Andagera Formation (Georgina Basin) according to Stidolph et al (1988).||||||28-NOV-06
16118|Rising Sun Conglomerate|24303|6|Mentioned|p60 Appendix|||Possible correlative of Gleeson Formation.||||||
16118|Rising Sun Conglomerate|30320|4|Described|p422|||||||||
16118|Rising Sun Conglomerate|31735|6|Mentioned|Fig. 1|||||||||
16118|Rising Sun Conglomerate|32174|6|Mentioned|Map legend|Adelaidean|Adelaidean|Prob. Adelaidean||||||
16118|Rising Sun Conglomerate|33307|6|Mentioned|Fig.8|||||||||
16118|Rising Sun Conglomerate|35771|6|Mentioned|p9|||||||||
16118|Rising Sun Conglomerate|39213|6|Mentioned|Fig.8|||||||||
16118|Rising Sun Conglomerate|39624|4|Described|p42|||||||||
16118|Rising Sun Conglomerate|42956|5|Briefly described|p31 Fig.4|||||||||
16118|Rising Sun Conglomerate|43224|5|Briefly described|Map legend|Paleozoic|Neoproterozoic|||||||07-NOV-08
16118|Rising Sun Conglomerate|44960|14|Not recorded|Not recorded|||||||||
16118|Rising Sun Conglomerate|45052|4|Described|p67|||Adelaidean ?||||||
16118|Rising Sun Conglomerate|45167|5|Briefly described|Fig.27|||||||||
16118|Rising Sun Conglomerate|46842|6|Mentioned|p115|||||||||
16118|Rising Sun Conglomerate|47058|6|Mentioned|Fig.3 P123|||||||||
16118|Rising Sun Conglomerate|48860|2|Defined|p.15,16||Proterozoic|On many pages. p.1,5,7,9,32,57,58,69, Pl.6. (E53-14/Tennant Creek).||||||
16118|Rising Sun Conglomerate|50353|5|Briefly described|Map Legend|Early Cambrian|Neoproterozoic|Conglomerate and sandstone; monomictic and polymictic orthoconglomerate; channel cross-bedded. Quartz arenite; predominantly medium bedded, parallel or cross-bedded.||||||
16118|Rising Sun Conglomerate|60684|5|Briefly described|p13|Early Cambrian|Neoproterozoic III|Probably correlates with Andagerra Formation.||||||28-APR-05
16118|Rising Sun Conglomerate|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|In Tennant Creek region. Lithology not presented.||||||07-NOV-08
16118|Rising Sun Conglomerate|65209|5|Briefly described|p35 Fig.1, p38|Paleoproterozoic|Paleoproterozoic|Presented, in Fig.1 legend, as Rising Sun Congl. (in part). Limited geographical distribution and apparently confined to a largely fault-bounded block in TENNANT CREEK. Variously correlated with: Blanche Creek Member; sedimentary rocks of Epenarra Volcanics and Unimbra Sandstone, together with unconformably overlying Andagerra Formation; and Andagerra Formation and Helen Springs Volcanics. Likely Tomkinson Creek Group/Hatches Creek Group provenance. Possible correlation of Rising Sun Conglomerate with Jeromah Formation or Gleeson Formation possible, but not considered very probable.|||||Polymictic conglomerate, sandstone, and (probable tuffaceous) siltstone.|05-JAN-17
16118|Rising Sun Conglomerate|65237|6|Mentioned|p5|Early Cambrian|Early Cambrian|Mentioned by authors in listing "a plethora of stratigraphic names applied to early Cambrian sediments in the literature, which need rationalizing" - in the Georgina Basin.||||||07-FEB-11
16118|Rising Sun Conglomerate|65338|6|Mentioned|p6. |||A probable local erosional remnant of Hatches Creek Group-aged strata within Warramunga Province.||||||
16118|Rising Sun Conglomerate|67175|6|Mentioned|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||||||
16118|Rising Sun Conglomerate|69424|4|Described|p9:5, 17, 22, 26-27, 39 Fig.9.24|Paleoproterozoic|Paleoproterozoic|Of Crohn and Aldershaw (1965). Outcrop is mostly confined to the Rising Sun Ridge, c.15km ESE of Tennant Creek. Warramunga Province. Probably includes representatives of several Formations mapped elsewhere; the unit needs further work and redefinition. Tentatively assigned to Hatches Creek Group. Previous descriptions and correlations are detailed. Possible correlatives include Gleeson Formation, Blanche Creek and Manga Mauda Members (of Hayward Creek Formation), and Unimbra Sandstone.||Hatches Creek Group.||Unconformably overlies Yungkulungu Formation.|Three intervals of conglomerate separated by pebble- and cobble-bearing, very coarse-grained quartz sandstone (total 25m thick), overlain by up to 60m of ripple marked, cross-bedded quartz sandstone with abundant mudstone clasts.|12-JUL-16
16118|Rising Sun Conglomerate|69425|6|Mentioned|p10:13|||Warramunga Province.||||Correlated in part with Unimbra Sandstone.||12-JUL-16
16118|Rising Sun Conglomerate|69431|6|Mentioned|p16:5, 7|||Warramunga Province.||||Possible correlate of Blanche Creek Member.||12-JUL-16
16118|Rising Sun Conglomerate|69437|6|Mentioned|p22:4-5|Ediacaran|Ediacaran|Tennant Region. Of uncertain age or affinities, or not included in Centralian A Superbasin.||||||12-JUL-16
16118|Rising Sun Conglomerate|70968|6|Mentioned|p94|||Some or all of the outcrops assigned to this unit in TENNANT CREEK sheet may belong to the Gleeson Formation.||||||
16135|Riversdale Formation|30242|6|Mentioned|Fig.2|||||||||
16135|Riversdale Formation|30479|6|Mentioned|Fig.6|||||||||
16135|Riversdale Formation|30914|6|Mentioned|Map legend|Early Cambrian|Proterozoic|Proterozoic - Early Cambrian||||||
16135|Riversdale Formation|33111|6|Mentioned|p38|||||||||
16135|Riversdale Formation|33900|6|Mentioned|p19|||||||||
16135|Riversdale Formation|35054|6|Mentioned|p246|||||||||
16135|Riversdale Formation|35074|6|Mentioned|Fig.2|||||||||
16135|Riversdale Formation|37572|6|Mentioned|p157|||See also Fig.8||||||
16135|Riversdale Formation|37816|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
16135|Riversdale Formation|38350|6|Mentioned|p22|||||||||
16135|Riversdale Formation|38442|5|Briefly described|Map legend|Cambrian|Cambrian|||||||25-AUG-04
16135|Riversdale Formation|38446|6|Mentioned|p144|||||||||
16135|Riversdale Formation|38608|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
16135|Riversdale Formation|39445|5|Briefly described|Table 4|||See also p61 and p62.||||||28-NOV-06
16135|Riversdale Formation|39690|6|Mentioned|Table 1|||||||||
16135|Riversdale Formation|40038|6|Mentioned|Fig.1|||||||||
16135|Riversdale Formation|40856|6|Mentioned|Fig.23.6|||||||||
16135|Riversdale Formation|44211|14|Not recorded|p96,102|||Rests on basement and forms residuals below Thorntonia Limestone.||||||
16135|Riversdale Formation|44271|14|Not recorded|p21-62|||Not listed on white card.||||||
16135|Riversdale Formation|44273|14|Not recorded|Map Legend||Neoproterozoic|||||||
16135|Riversdale Formation|44275|14|Not recorded|Map Legend|||||||||
16135|Riversdale Formation|44309|2|Defined|Tb.1,opp.p7,7-9,map|||No fossils. Overlies Precambrian unconformably.||||||
16135|Riversdale Formation|44326|14|Not recorded|Map Legend||Early Cambrian|||||||
16135|Riversdale Formation|44920|14|Not recorded|Map Legend, Sheet 4||Early Cambrian|||||||
16135|Riversdale Formation|44989|4|Described|p.125|||Tb.II. (F54-5).||||||
16135|Riversdale Formation|45012|14|Not recorded|p26,27||Early Cambrian|||||||
16135|Riversdale Formation|45052|5|Briefly described|p74|||L.Camb.||||||
16135|Riversdale Formation|45079|5|Briefly described|p10|||Precambrian age. See also p16,p28,p29. Term to be discontinued.||||||28-NOV-06
16135|Riversdale Formation|45166|5|Briefly described|Table 15|||||||||
16135|Riversdale Formation|45287|14|Not recorded|p.223||Cambrian|||||||
16135|Riversdale Formation|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
16135|Riversdale Formation|46955|6|Mentioned|p159|||||||||
16135|Riversdale Formation|47058|6|Mentioned|Fig.8 P129|||||||||
16135|Riversdale Formation|60359|5|Briefly described|Map Legend|Cambrian|Cambrian|Sandstone, sandy dolomite, siltstone, mudstone, conglomerate.||||||
16135|Riversdale Formation|64068|4|Described|p54, 58, 225|Early Cambrian|Early Cambrian|To 30 m thick. Forms mesa cappings and low scarps. Correlations depend on boundary relations.||Of Shadow Group.||Is overlain by Thorntonia Limestone either unconformably or conformably and gradationally.|Conglomerate, red sandstone and red quartzic dolostone.|05-APR-12
16135|Riversdale Formation|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Early Cambrian|Neoproterozoic|Georgina Basin||Shadow Group|||Conglomerate, arenite, arkose, shale, mudstone, dolomite|
16135|Riversdale Formation|69443|5|Briefly described|p28:7, 14, 16|Early Cambrian|Early Cambrian|Southern Georgina Basin.||Shadow Group.||Is overlain by Thorntonia Limestone unconformably or gradationally[?].||12-JUL-16
16135|Riversdale Formation|69591|5|Briefly described|p90, p97, p98 Fig.2.91|Cambrian|Neoproterozoic|Oban Sub-basin, Georgina Basin. Crops out only in the Ardmore outlier as erosional residuals up to 30m thick.||Shadow Group.||Is overlain conformably by Thorntonia Limestone. Notional correlative of Mount Birnie beds.|Red sandstone, with several conglomerate bands in the lower part and red sandy dolomite above. Unfossiliferous.|
16164|Roaring Siltstone|9830|5|Briefly described|Map Legend|Cambrian|Cambrian|Siltstone, fine sandstone, chert. Underlies: Devoncourt Limestone, O'Hara Shale. Overlies: Thorntonia Limestone.||||||27-AUG-04
16164|Roaring Siltstone|22954|6|Mentioned|Fig3p9|Boomerangian|Undillan|||||||
16164|Roaring Siltstone|30479|6|Mentioned|Fig.5|||Stratigraphic relationships||||||
16164|Roaring Siltstone|30914|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
16164|Roaring Siltstone|31396|6|Mentioned|Fig.3|||||||||
16164|Roaring Siltstone|32952|6|Mentioned|p1188|||See also p1189. M.-U. Camb.||||||28-NOV-06
16164|Roaring Siltstone|33111|4|Described|p41|||Mention p6.||||||28-NOV-06
16164|Roaring Siltstone|33113|6|Mentioned|Fig.1|||Middle Camb.||||||
16164|Roaring Siltstone|33482|6|Mentioned|Fig.4|||Middle - Upper Cambrian||||||
16164|Roaring Siltstone|34903|6|Mentioned|p582|||||||||
16164|Roaring Siltstone|35054|6|Mentioned|Table 23|||||||||
16164|Roaring Siltstone|35121|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
16164|Roaring Siltstone|35139|4|Described|Table.2|||||||||
16164|Roaring Siltstone|35553|6|Mentioned|p153|||||||||
16164|Roaring Siltstone|35939|6|Mentioned|p633|||||||||
16164|Roaring Siltstone|36234|6|Mentioned|p168|||||||||
16164|Roaring Siltstone|37275|6|Mentioned|p290|||||||||
16164|Roaring Siltstone|37413|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
16164|Roaring Siltstone|37572|4|Described|p159|||See also Fig.8||||||
16164|Roaring Siltstone|37816|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
16164|Roaring Siltstone|38350|6|Mentioned|p22|||||||||
16164|Roaring Siltstone|38444|6|Mentioned|p139|||||||||
16164|Roaring Siltstone|38446|6|Mentioned|Table 23|||||||||
16164|Roaring Siltstone|38608|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
16164|Roaring Siltstone|39029|5|Briefly described|Map legend|Cambrian|Cambrian|Overlain by O'Hara Shale.||||||25-AUG-04
16164|Roaring Siltstone|39445|5|Briefly described|Table 4|||See also p62.||||||28-NOV-06
16164|Roaring Siltstone|39690|6|Mentioned|Table 1|||See also Fig.2||||||
16164|Roaring Siltstone|40852|6|Mentioned|Fig.3.7|||||||||
16164|Roaring Siltstone|40856|5|Briefly described|p313|||||||||
16164|Roaring Siltstone|41306|6|Mentioned|p4|||||||||
16164|Roaring Siltstone|41388|6|Mentioned|Fig.2|||||||||
16164|Roaring Siltstone|42139|6|Mentioned|Fig.18 P90|||||||||
16164|Roaring Siltstone|44205|2|Defined|p9-13,26-7,31-7,40-7||Middle Cambrian|p51-9,74-87,135,164,180-85. Overlies Mount Birnie Beds. Overlain by Devoncourt Limestone.||||||
16164|Roaring Siltstone|44211|14|Not recorded|p96,104,107|||||||||
16164|Roaring Siltstone|44275|14|Not recorded|Map Legend|||||||||
16164|Roaring Siltstone|44276|2|Defined|p21,Tb.2,map|||||||||
16164|Roaring Siltstone|44277|14|Not recorded|Map Legend||Middle Cambrian|||||||
16164|Roaring Siltstone|44278|14|Not recorded|Tb.1|||||||||
16164|Roaring Siltstone|44757|6|Mentioned|p155|||Probable stratigraphic equivalent of Beetle Creek Formation.||||||
16164|Roaring Siltstone|44882|14|Not recorded|p201||Cambrian|In French.||||||28-NOV-06
16164|Roaring Siltstone|45052|2|Defined|p101|Middle Cambrian|Middle Cambrian|||||||
16164|Roaring Siltstone|45079|5|Briefly described|p30|||Cambrian age||||||
16164|Roaring Siltstone|45166|5|Briefly described|Table 15|||||||||
16164|Roaring Siltstone|47058|6|Mentioned|Fig.4 P124|||||||||
16164|Roaring Siltstone|48633|14|Not recorded|p99|||Ref. to Opik 1961.||||||
16164|Roaring Siltstone|50100|5|Briefly described|p22|Early Ordovician|Early Cambrian|Finely laminated siltstone, siliceous shale and fine-grained sandstone.  Disconformably overlies Thorntonia Limestone; overlain conformably by (and passes laterally into) Devoncourt Limestone.||||||
16164|Roaring Siltstone|60122|6|Mentioned|p57 Appendix|||Geological Province: Burke River Structural Belt. Correlated with parts of the Arthur Creek Formation.||||||
16164|Roaring Siltstone|60359|5|Briefly described|Map Legend|Cambrian|Cambrian|Siltstone, sandstone; minor chert, shale.||||||
16164|Roaring Siltstone|63450|5|Briefly described|p78 Fig. 5|Middle Cambrian|Middle Cambrian|Geological province: Georgina Basin, Burke River Structural Belt.||||||07-FEB-11
16164|Roaring Siltstone|64068|3|Fully described|p64, 62, 63|Middle Cambrian|Middle Cambrian|Contains trilobites, brachiopods, molluscs, sponges and archaeocopides. Correlations: Age Creek Formation, V Creek Limestone, Mail Change Limestone, Split Rock Sandstone, Currant Bush Limestone, Devoncourt Limestone in part, Blazan Shale, Quita Formation, Camooweal Dolostone, upper Arthur Creek Formation.||Of Narpa Group.||Conformably overlies Inca Formation. Disconformable over Beetle Creek Formation or Thorntonia Limestone. Interdigitates with and is overlain by Devoncourt Limestone.|Siliceous shale, siltstone, sandstone; local basal conglomerate.|04-APR-12
16164|Roaring Siltstone|64443|6|Mentioned|p41|||Undilla Sub-basin. Correlative of Ranken Limestone, Camooweal Dolostone.||||||
16164|Roaring Siltstone|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map; p83|Middle Cambrian|Middle Cambrian|Burke River Structural Belt, Georgina Basin.||Narpa Group.||Unconformably overlies Inca Formation. Is overlain by Devencourt Limestone.|Siltstone, sandstone; minor chert, silicified shale.|
16164|Roaring Siltstone|67870|6|Mentioned|p43|Middle Cambrian|Middle Cambrian|Burke River Structural Belt, Georgina Basin.||||||
16164|Roaring Siltstone|69377|5|Briefly described|map legend|Cambrian|Cambrian|||Narpa Group|||Siltstone and sandstone; minor chert and silicified shale|
16164|Roaring Siltstone|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
16164|Roaring Siltstone|69573|6|Mentioned|p659, 661, 666, 668|||Georgina Basin. Deeper water, mid-outer shelf and slope settings.||||Grades laterally and vertically into Devoncourt Limestone.||
16164|Roaring Siltstone|69591|5|Briefly described|p87, p92, p96-97, p98 Fig.2.91|Cambrian|Cambrian|Burke River Structural Belt, Georgina Basin. Up to 70m thick. Lithologically identical to Inca Formation; considered to be its northern younging extension. They are distinguished by fossil fauna (named).||||Unconformably overlies Thorntonia Limestone. Is overlain conformably by, and passes laterally into, Devoncourt Limestone.|Thin-bedded, silty, siliceous shale with minor thin chert and fine sandstone and some bituminous calcilutites.|
16164|Roaring Siltstone|72321|6|Mentioned|Fig 2|Guzhangian|Drumian|Burke River Structural Belt, Georgina Basin. Australian stages:  Undillan to Boomerangian.||of Narpa Group.||||
16164|Roaring Siltstone|72516|6|Mentioned|p92|Cambrian|Cambrian|Eastern Georgina Basin.||||Equivalent to the Arthur Creek Formation.||03-JUN-21
16164|Roaring Siltstone|72683|5|Briefly described|Map legend|Cambrian|Cambrian|Georgina Basin.||Narpa Group||Underlies and is equivalent to Devoncourt Limestone. Unconformably overlies Thorntonia Limestone.|Siltstone and sand stone; minor chert and silicified shale.|
16164|Roaring Siltstone|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 Thorntonia Limestone and underlies Devoncourt Limestone.|Siltstone and sandstone; minor chert and silicified shale.|
16164|Roaring Siltstone|73418|5|Briefly described|p3, p4 Fig.3|Miaolingian|Miaolingian|Georgina Basin, Burke River Structural Belt.||Narpa Group||Lateral equivalent of Inca Formation, underlies Selwyn Range Limestone, Devoncourt Limestone|Siltstone.|
16267|Rolling Downs Group|730|6|Mentioned|p24, p25.|||Marine.||||||11-NOV-14
16267|Rolling Downs Group|9250|5|Briefly described|Map legend|Cretaceous|Cretaceous|Sandstone, siltstone and claystone., porcellaneous in part.||||||
16267|Rolling Downs Group|12575|5|Briefly described|p781. |Albian|Albian|Uppermost unit in Laura Basin. Vitrinite reflectance data are detailed.|124-97 Ma.||Includes Wollena Claystone.||Glauconitic open marine shale.|
16267|Rolling Downs Group|13516|5|Briefly described|p167 fig 10, p169 fig 11|Late Cretaceous|Early Cretaceous|In Surat Basin, Eromanga Basin.|||Includes Wilgunya Subgroup, Manuka Subgroup|||14-NOV-12
16267|Rolling Downs Group|22757|5|Briefly described|p7|||Also Table6, p11. Surat Basin.||||||28-NOV-06
16267|Rolling Downs Group|22780|5|Briefly described|map|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|22781|4|Described|p41|Early Cretaceous|Early Cretaceous|In the Carpentaria Basin.||||||02-APR-07
16267|Rolling Downs Group|22857|5|Briefly described|p294, p544 App.1 Tb.A1.12|Cenomanian|Aptian|Includes the Wallumbilla Formation, Surat Siltstone, Griman Creek Formation, and Winton Formation. Geological Province: Surat and Eromanga Basins. See also p296-7 Tb.22.1, p315 Fig. 22.8, p552 App.1 Tb.A1.13.||||||
16267|Rolling Downs Group|22865|4|Described|p294,Table22.1p296-7|Cenomanian|Aptian|||||||
16267|Rolling Downs Group|23053|4|Described|p8,11,28,30-1|Albian|Aptian|||||||
16267|Rolling Downs Group|23056|6|Mentioned|6|||Geological province: Eromanga Basin.||||||28-NOV-06
16267|Rolling Downs Group|23065|5|Briefly described|18|||Geological province: Carpentaria Basin.||||||28-NOV-06
16267|Rolling Downs Group|23183|6|Mentioned|p217||Aptian|||||||
16267|Rolling Downs Group|23220|6|Mentioned|p16|||||||||
16267|Rolling Downs Group|23224|5|Briefly described|p3|||Of McMinn 1981. Hosts the Wallumbilla Formation. Great Australian Basin.||||||07-MAR-06
16267|Rolling Downs Group|23291|4|Described|p80 Tb. 3.6|Early Cretaceous|Early Cretaceous|Age: Early Cretaceous. Conformably overlies Coffin Hill Member. Thickness: <10m. Geological Province: Georgetown Region.||||||26-NOV-08
16267|Rolling Downs Group|23336|5|Briefly described|p5|Cretaceous|Cretaceous|Overlies Mulga Downs Group.||||||28-NOV-06
16267|Rolling Downs Group|23393|5|Briefly described|p24|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|23420|6|Mentioned|p 131|||||||||
16267|Rolling Downs Group|23423|5|Briefly described|p267||Cretaceous|||||||
16267|Rolling Downs Group|23425|3|Fully described|p394 Table 9.7.|||Also see p378. Geological Province Carpentaria Basin.||||||03-APR-12
16267|Rolling Downs Group|23426|3|Fully described|p403 + Table 10.4 p407|Albian|Aptian|Formerly Battle Camp Shale and Wolena Claystone. Conformably underlain by Gilbert River Formation. Geological province: Laura Basin Province.||||||26-APR-07
16267|Rolling Downs Group|23427|5|Briefly described|Table 11.2 p418.|||||||||
16267|Rolling Downs Group|23428|5|Briefly described|p422|||||||||
16267|Rolling Downs Group|23430|5|Briefly described|p522|||Formerly Battle Camp Shale and Wolena Claystone. Basal shale is marine, variably calcareous and galuconitic, with minor siltstone and conglom. beds; overlain by marine silty/sandy claystone with calc.concretions. Geol. Prov: Laura Basin.||||||30-NOV-06
16267|Rolling Downs Group|23431|5|Briefly described|p544|||||||||
16267|Rolling Downs Group|23496|6|Mentioned|p59|||||||||
16267|Rolling Downs Group|23510|5|Briefly described|Map Legend||Early Cretaceous|||||||
16267|Rolling Downs Group|23511|5|Briefly described|Map Legend|Cretaceous|Middle Jurassic|||||||
16267|Rolling Downs Group|23512|5|Briefly described|Map Legend|Cretaceous|Middle Jurassic|||||||
16267|Rolling Downs Group|23518|5|Briefly described|p13|Mesozoic|Mesozoic|Geological Province: Carpentaria Basin.||||||
16267|Rolling Downs Group|23833|5|Briefly described|p256 Table 1|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|23879|6|Mentioned|p18|||||||||
16267|Rolling Downs Group|23883|5|Briefly described|p129 Fig. 11.2|Cretaceous|Cretaceous|Geological Province: Great Australian Superbasin.||||||
16267|Rolling Downs Group|23911|5|Briefly described|p97 Fig. 11|Albian|Aptian|Geological Province: Eromanga Basin.||||||
16267|Rolling Downs Group|23982|5|Briefly described|p2|Cretaceous|Cretaceous|Geological Province: Great Artesian Basin. See also page 35 Fig.7.||||||
16267|Rolling Downs Group|24047|5|Briefly described|p11-12|||Geological Province: Western Gulf Sub-basin.||||||
16267|Rolling Downs Group|24048|6|Mentioned|p76|||Geological Province: Carpentaria Basin.||||||
16267|Rolling Downs Group|24070|5|Briefly described|p303|Cretaceous|Cretaceous|Geological Province: Coonamble Embayment.||||||
16267|Rolling Downs Group|24073|5|Briefly described|p378 Table 2|Early Cretaceous|Early Cretaceous|Geological Province: Carpentaria Basin.||||||
16267|Rolling Downs Group|24089|5|Briefly described|Student Activites|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|24092|5|Briefly described|p8 Fig.3|||Geological Province: Eromanga Basin.||||||
16267|Rolling Downs Group|24243|5|Briefly described|p3 Fig.2|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|24393|5|Briefly described|p152 Tb. 1|Mesozoic|Mesozoic|Shallow marine deposits <50m. thick.||||||
16267|Rolling Downs Group|29591|6|Mentioned|p69|||||||||
16267|Rolling Downs Group|29961|6|Mentioned|p12|||||||||
16267|Rolling Downs Group|29991|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|30019|6|Mentioned|p2|||||||||
16267|Rolling Downs Group|30021|6|Mentioned|p87|||||||||
16267|Rolling Downs Group|30095|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|30102|5|Briefly described|p34|||Cretaceous age. See also p17.||||||28-NOV-06
16267|Rolling Downs Group|30103|5|Briefly described|p9|||Lower Cretaceous age. Table 3 on p9. See also Fig.2.||||||28-NOV-06
16267|Rolling Downs Group|30104|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|30133|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|30510|6|Mentioned|p103|||||||||
16267|Rolling Downs Group|30582|6|Mentioned|p4|||||||||
16267|Rolling Downs Group|30584|4|Described|Table 1|||||||||
16267|Rolling Downs Group|30585|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|30587|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|30691|4|Described|p6|||See also p15-17,20,Table 4,Fig.2. Lower Cretaceous age.||||||28-NOV-06
16267|Rolling Downs Group|30692|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|30696|6|Mentioned|p16|||||||||
16267|Rolling Downs Group|30697|6|Mentioned|p34|||Minor aquifer present.||||||28-NOV-06
16267|Rolling Downs Group|30699|6|Mentioned|p53|||Stratigraphy. Early Cretaceous||||||
16267|Rolling Downs Group|30701|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|30702|4|Described|p48|||See also p51,52,Fig.1. Stratigraphic table.||||||28-NOV-06
16267|Rolling Downs Group|30853|5|Briefly described|Table 3|||Cretaceous||||||
16267|Rolling Downs Group|30854|4|Described|Table 4|||Lower to Upper Cretaceous age||||||
16267|Rolling Downs Group|30855|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|30856|4|Described|Table 3|||Lower Cretaceous age||||||
16267|Rolling Downs Group|30857|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|30905|6|Mentioned|p147|||||||||
16267|Rolling Downs Group|30910|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|30914|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|31097|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|31098|5|Briefly described|Table 1|||||||||
16267|Rolling Downs Group|31109|6|Mentioned|p40|||See also P42, 44, 46, 50, 52, 54, 56, 58 & Map 62.||||||
16267|Rolling Downs Group|31110|5|Briefly described|p6|||See also p8-26. Terrain classification.||||||28-NOV-06
16267|Rolling Downs Group|31144|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
16267|Rolling Downs Group|31145|5|Briefly described|Table 1|||L. - U. Cretaceous||||||
16267|Rolling Downs Group|31164|6|Mentioned|p8|||Lower Cretaceous||||||
16267|Rolling Downs Group|31165|5|Briefly described|Table.1.|||||||||
16267|Rolling Downs Group|31166|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|31376|5|Briefly described|p4|||Mention p2.||||||28-NOV-06
16267|Rolling Downs Group|31422|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Includes the Wallumbilla Formation, Toolebuc Limestone and Allaru Mudstone.||||||02-DEC-04
16267|Rolling Downs Group|31425|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|31430|4|Described|Table 1|||||||||
16267|Rolling Downs Group|31431|5|Briefly described|Table 3|||L.U.Cretaceous||||||
16267|Rolling Downs Group|31432|4|Described|Table 1|||L.Cretaceous||||||
16267|Rolling Downs Group|31433|5|Briefly described|p7|||Lower Cretaceous||||||
16267|Rolling Downs Group|31434|4|Described|Table 1|||Lower Cretaceous. See also p8.||||||28-NOV-06
16267|Rolling Downs Group|31436|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower Cretaceous - Upper Cretaceous||||||
16267|Rolling Downs Group|31437|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|31438|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|31440|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|31441|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
16267|Rolling Downs Group|31443|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|31553|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|32274|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
16267|Rolling Downs Group|32275|4|Described|p8|||||||||
16267|Rolling Downs Group|32276|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|32277|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
16267|Rolling Downs Group|32314|6|Mentioned|Fig.4|||||||||
16267|Rolling Downs Group|32392|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|32393|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|32395|6|Mentioned|p6|||Stratigraphic table.||||||28-NOV-06
16267|Rolling Downs Group|32396|6|Mentioned|p8|||L.Cretaceous||||||
16267|Rolling Downs Group|32413|6|Mentioned|p87|||||||||
16267|Rolling Downs Group|32563|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|32671|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|32705|6|Mentioned|p183|||See also Fig.2||||||
16267|Rolling Downs Group|32706|4|Described|Table 1|||Mention p8.||||||28-NOV-06
16267|Rolling Downs Group|32796|4|Described|p301|||See also p302-303||||||28-NOV-06
16267|Rolling Downs Group|32918|4|Described|p18|||||||||11-JAN-10
16267|Rolling Downs Group|33011|6|Mentioned|p214|||||||||
16267|Rolling Downs Group|33016|6|Mentioned|p1|||||||||
16267|Rolling Downs Group|33017|6|Mentioned|p8|||||||||
16267|Rolling Downs Group|33067|4|Described|Table 1|Early Cretaceous|Early Cretaceous|Includes Winton, Mackunda and Wallumbilla Formations and Allaru Mudstone and Toolebuc Limestone.||||||07-JUL-04
16267|Rolling Downs Group|33068|6|Mentioned|p476|||Cret.||||||
16267|Rolling Downs Group|33069|4|Described|p7|||L.-U.Cret.||||||
16267|Rolling Downs Group|33070|4|Described|Table 2|||L.Cret.||||||
16267|Rolling Downs Group|33072|4|Described|Table 1|||L.Cret.||||||
16267|Rolling Downs Group|33073|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33075|6|Mentioned|p452|||||||||
16267|Rolling Downs Group|33078|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
16267|Rolling Downs Group|33079|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
16267|Rolling Downs Group|33080|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33082|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
16267|Rolling Downs Group|33083|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
16267|Rolling Downs Group|33086|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33087|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|33088|4|Described|Table 3|||L.Cret.||||||
16267|Rolling Downs Group|33089|4|Described|Table 2|||L.-U.Cret.||||||
16267|Rolling Downs Group|33090|4|Described|Table 4|||L.Cret.||||||
16267|Rolling Downs Group|33091|6|Mentioned|p9|||Strat.||||||
16267|Rolling Downs Group|33092|6|Mentioned|p8|||Strat. table||||||
16267|Rolling Downs Group|33094|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33095|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33096|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33150|4|Described|p8|||L.Cret.||||||
16267|Rolling Downs Group|33151|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33176|6|Mentioned|p175|||||||||
16267|Rolling Downs Group|33177|5|Briefly described|Table 1|||||||||15-JUL-04
16267|Rolling Downs Group|33178|5|Briefly described|p11|||||||||
16267|Rolling Downs Group|33181|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33182|6|Mentioned|p193|||||||||
16267|Rolling Downs Group|33184|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33185|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33226|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33372|6|Mentioned|Table 1|||||||||
16267|Rolling Downs Group|33448|4|Described|Table 1|||L.Cret.||||||11-JAN-10
16267|Rolling Downs Group|33449|4|Described|Table 1|||L.-U.Cret.||||||
16267|Rolling Downs Group|33451|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33452|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33528|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33529|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33561|6|Mentioned|p102|||||||||
16267|Rolling Downs Group|33638|5|Briefly described|Table 1|||See also p10.||||||28-NOV-06
16267|Rolling Downs Group|33639|5|Briefly described|p11|||L.Cret.||||||
16267|Rolling Downs Group|33640|4|Described|Table 2|||L.-U.Cret.||||||
16267|Rolling Downs Group|33642|6|Mentioned|p144,147,148|||Refers Vine & Day.(1965). Ref. to Whitehouse 1954. Subgroups. Ref to Jack 1886.||||||
16267|Rolling Downs Group|33643|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33644|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33646|5|Briefly described|p8|||Strat. table.||||||
16267|Rolling Downs Group|33647|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper? Cretaceous||||||
16267|Rolling Downs Group|33648|6|Mentioned|p19|||||||||
16267|Rolling Downs Group|33676|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|33709|6|Mentioned|p110|||Cretaceous.||||||
16267|Rolling Downs Group|33772|4|Described|p13|||||||||
16267|Rolling Downs Group|33773|4|Described|Table 1|||||||||
16267|Rolling Downs Group|33825|6|Mentioned|p10|||Correlation table||||||
16267|Rolling Downs Group|33832|5|Briefly described|p11|||Strat. and correlation.||||||28-NOV-06
16267|Rolling Downs Group|33882|4|Described|Table 1|||Mention p7,8.||||||28-NOV-06
16267|Rolling Downs Group|33883|6|Mentioned|p17|||||||||
16267|Rolling Downs Group|33884|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|34065|4|Described|p6|||L.Cret.||||||
16267|Rolling Downs Group|34091|5|Briefly described|Table 1|||Cret. See also pp4,8.||||||28-NOV-06
16267|Rolling Downs Group|34174|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|34217|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower to Upper Cretaceous||||||
16267|Rolling Downs Group|34218|5|Briefly described|Table 1|||Lower Cretaceous.||||||28-NOV-06
16267|Rolling Downs Group|34254|6|Mentioned|p481|||||||||
16267|Rolling Downs Group|34282|6|Mentioned|p96|||Cret.||||||
16267|Rolling Downs Group|34287|6|Mentioned|p186|||Cret.||||||
16267|Rolling Downs Group|34469|6|Mentioned|p107|||Cretaceous. See also pp117,118.||||||28-NOV-06
16267|Rolling Downs Group|34487|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|34550|5|Briefly described|Table 2.1|||Cretaceous||||||
16267|Rolling Downs Group|34811|4|Described|Table 1|||||||||
16267|Rolling Downs Group|34931|5|Briefly described|p320|||||||||
16267|Rolling Downs Group|35187|6|Mentioned|p53|||||||||
16267|Rolling Downs Group|35204|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|35220|4|Described|p16|||||||||
16267|Rolling Downs Group|35253|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|35559|4|Described|Table 1|||||||||
16267|Rolling Downs Group|35560|6|Mentioned|p289|||||||||
16267|Rolling Downs Group|35601|6|Mentioned|p144|||Geothermal gradients correlate with contours of base of R.D.Group||||||
16267|Rolling Downs Group|35640|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|35663|6|Mentioned|Table 1|||Biostratigraphy.||||||
16267|Rolling Downs Group|35793|6|Mentioned|p241|||Weathered profiles.||||||
16267|Rolling Downs Group|35811|5|Briefly described|Table 3|||||||||
16267|Rolling Downs Group|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
16267|Rolling Downs Group|36012|3|Fully described|Table 5|||||||||
16267|Rolling Downs Group|36056|6|Mentioned|p11|||||||||
16267|Rolling Downs Group|36228|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|36229|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|36473|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|36570|6|Mentioned|p46|||||||||
16267|Rolling Downs Group|36571|6|Mentioned|Table 4|||||||||
16267|Rolling Downs Group|36751|6|Mentioned|p488|||||||||
16267|Rolling Downs Group|36910|6|Mentioned|p61|||||||||
16267|Rolling Downs Group|36914|6|Mentioned|p87|||||||||
16267|Rolling Downs Group|36961|6|Mentioned|Table 1|||||||||
16267|Rolling Downs Group|37116|6|Mentioned|p310|||||||||
16267|Rolling Downs Group|37608|3|Fully described|Table 1|||See also Table 2||||||
16267|Rolling Downs Group|37995|4|Described|Table 1|||||||||
16267|Rolling Downs Group|38064|5|Briefly described|p42|||Contain opal deposits of White Cliffs and Lightning Ridge.||||||
16267|Rolling Downs Group|38226|6|Mentioned|Table 1|||||||||
16267|Rolling Downs Group|38374|6|Mentioned|p602|||||||||
16267|Rolling Downs Group|39211|6|Mentioned|p5|||Fig. 3,7,9,22,26 etc. Correlation||||||
16267|Rolling Downs Group|39315|6|Mentioned|Fig.5|||||||||
16267|Rolling Downs Group|39445|5|Briefly described|Table 11|||||||||
16267|Rolling Downs Group|39478|6|Mentioned|Table 1|||||||||
16267|Rolling Downs Group|39494|6|Mentioned|Fig.5|||||||||
16267|Rolling Downs Group|39556|5|Briefly described|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|39627|6|Mentioned|p269|||||||||
16267|Rolling Downs Group|39666|6|Mentioned|p110|||||||||
16267|Rolling Downs Group|39708|6|Mentioned|p478|||||||||
16267|Rolling Downs Group|39899|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|39942|6|Mentioned|p468|||||||||
16267|Rolling Downs Group|40030|6|Mentioned|Fig.5|||||||||
16267|Rolling Downs Group|40199|6|Mentioned|Fig.2|||||||||
16267|Rolling Downs Group|40544|6|Mentioned|Fig.6|||||||||
16267|Rolling Downs Group|40584|6|Mentioned|p434|||||||||
16267|Rolling Downs Group|40595|6|Mentioned|Fig.7|||||||||
16267|Rolling Downs Group|40623|5|Briefly described|p88|||||||||
16267|Rolling Downs Group|40648|3|Fully described|p12|||||||||
16267|Rolling Downs Group|40766|5|Briefly described|p25|||||||||
16267|Rolling Downs Group|40801|6|Mentioned|p79|||||||||
16267|Rolling Downs Group|40926|6|Mentioned|Table 2|||||||||
16267|Rolling Downs Group|41012|6|Mentioned|p137|||||||||
16267|Rolling Downs Group|41022|6|Mentioned|p279|||||||||
16267|Rolling Downs Group|41061|6|Mentioned|p19|||See also Fig.6. Generalized stratigraphy.||||||28-NOV-06
16267|Rolling Downs Group|41064|6|Mentioned|p55|||||||||
16267|Rolling Downs Group|41086|3|Fully described|p98|||See also Fig.3||||||
16267|Rolling Downs Group|41087|6|Mentioned|Fig.2|||||||||
16267|Rolling Downs Group|41088|6|Mentioned|p143|||||||||
16267|Rolling Downs Group|41097|6|Mentioned|Table 1|||||||||
16267|Rolling Downs Group|41117|6|Mentioned|Fig.2|||||||||
16267|Rolling Downs Group|41177|6|Mentioned|Fig.2|||||||||
16267|Rolling Downs Group|41188|6|Mentioned|Fig.3|||||||||
16267|Rolling Downs Group|41210|5|Briefly described|Fig.3|||||||||
16267|Rolling Downs Group|41247|6|Mentioned|Fig.7|||||||||
16267|Rolling Downs Group|41266|6|Mentioned|Fig.3|||||||||
16267|Rolling Downs Group|41307|4|Described|p17|||||||||
16267|Rolling Downs Group|41568|4|Described|p15|||||||||
16267|Rolling Downs Group|41642|6|Mentioned|p217|||||||||
16267|Rolling Downs Group|41681|6|Mentioned|p2|||||||||
16267|Rolling Downs Group|41725|6|Mentioned|Fig.2|||||||||
16267|Rolling Downs Group|41992|4|Described|Fig.2 P183|||See also p186.||||||28-NOV-06
16267|Rolling Downs Group|42007|6|Mentioned|Fig.2 P182|||||||||
16267|Rolling Downs Group|42061|5|Briefly described|Fig.4 P151|||||||||
16267|Rolling Downs Group|42121|6|Mentioned|Fig.1 P97|||||||||
16267|Rolling Downs Group|42346|4|Described|p81, Fig.4 p82|Early Cretaceous||||||||
16267|Rolling Downs Group|42364|5|Briefly described|Fig. 1 P196|||||||||
16267|Rolling Downs Group|42460|5|Briefly described|Fig.1 P206|||||||||
16267|Rolling Downs Group|42464|6|Mentioned|p8|||||||||
16267|Rolling Downs Group|42467|5|Briefly described|Map Legend|||||||||
16267|Rolling Downs Group|42596|5|Briefly described|Fig. 1 P24|||||||||
16267|Rolling Downs Group|42637|5|Briefly described|p10, 23|||||||||
16267|Rolling Downs Group|42650|4|Described|p16|||Conformably overlies/overlaps the Gilbert River Formation.||||||28-NOV-06
16267|Rolling Downs Group|42653|5|Briefly described|p318|||Terrain pattern description||||||
16267|Rolling Downs Group|42673|6|Mentioned|p195|||||||||
16267|Rolling Downs Group|43000|5|Briefly described|Fig.5,p112|||||||||
16267|Rolling Downs Group|43085|6|Mentioned|p8|||||||||
16267|Rolling Downs Group|43090|5|Briefly described|Map legend||Cretaceous|||||||
16267|Rolling Downs Group|43276|5|Briefly described|Map Legend||Early Cretaceous|||||||
16267|Rolling Downs Group|43277|5|Briefly described|Map Legend||Early Cretaceous|In the Great Australian Basin.||||||28-NOV-06
16267|Rolling Downs Group|43366|14|Not recorded|Map Legend|||||||||22-DEC-09
16267|Rolling Downs Group|43367|14|Not recorded|Map Legend|||||||||11-JAN-10
16267|Rolling Downs Group|43368|14|Not recorded|Map Legend|||||||||
16267|Rolling Downs Group|43369|14|Not recorded|Map Legend|||||||||
16267|Rolling Downs Group|43371|14|Not recorded|Map Legend|||||||||11-JAN-10
16267|Rolling Downs Group|43383|14|Not recorded|p26-28, diag||Cretaceous|||||||
16267|Rolling Downs Group|43384|14|Not recorded|Map Legend||Cretaceous|||||||
16267|Rolling Downs Group|43386|14|Not recorded|Map Legend||Cretaceous|||||||
16267|Rolling Downs Group|43390|14|Not recorded|p15,16,27-34|||Divided into Winton,Tambo,Roma Formations||||||
16267|Rolling Downs Group|43402|14|Not recorded|Map Legend||Cretaceous|||||||
16267|Rolling Downs Group|43403|14|Not recorded|Map Legend||Cretaceous|||||||
16267|Rolling Downs Group|43404|14|Not recorded|p11-15,20,23-33||Cretaceous|Table p9,Table p11||||||
16267|Rolling Downs Group|43405|14|Not recorded|Map Legend||Cretaceous|(Provisional Edition)||||||
16267|Rolling Downs Group|43410|14|Not recorded|Map Legend||Cretaceous|(Provisional Edition)||||||
16267|Rolling Downs Group|43411|14|Not recorded|Map Legend|||||||||
16267|Rolling Downs Group|43436|14|Not recorded|Map Legend||Cretaceous|(Provisional Edition)||||||
16267|Rolling Downs Group|43452|5|Briefly described|Map Legend||Cretaceous|Includes: Roma Formation, Tambo Formation, Winton Formation.||||||14-FEB-05
16267|Rolling Downs Group|43454|14|Not recorded|Map Legend||Cretaceous|||||||
16267|Rolling Downs Group|43459|14|Not recorded|p315-6|||||||||
16267|Rolling Downs Group|43487|5|Briefly described|20|||||||||
16267|Rolling Downs Group|43501|14|Not recorded|Map Legend||Cretaceous|(Provisional Edition) Inc. Yalpunga Beds, Oornoo Beds, Wittabrenna Beds||||||
16267|Rolling Downs Group|43542|14|Not recorded|Map Legend||Cretaceous|lithology||||||
16267|Rolling Downs Group|43596|4|Described|p40, p39 Tb. 4|Albian|Aptian|Max. thickness: 600m. Largely comprises mudstone, with beds and lenses of glauconitic, labile, white to buff quartzose fine sandstone; fossiliferous and with  concretionary limestone at base; shallow marine deposits.||||||15-JAN-09
16267|Rolling Downs Group|43602|5|Briefly described|Fig3 p194|||In Surat Basin/Eromanga Basin||||||
16267|Rolling Downs Group|43625|6|Mentioned|p47|||||||||
16267|Rolling Downs Group|43630|6|Mentioned|p69|||||||||
16267|Rolling Downs Group|43714|6|Mentioned|p8||Early Cretaceous|||||||
16267|Rolling Downs Group|43730|5|Briefly described|p24,29|||||||||
16267|Rolling Downs Group|43738|6|Mentioned|p5|||||||||
16267|Rolling Downs Group|43810|6|Mentioned|Fig.4,p209,210||Cretaceous|||||||
16267|Rolling Downs Group|43820|5|Briefly described|Map Legend||Early Cretaceous|||||||
16267|Rolling Downs Group|43881|14|Not recorded|p79,80|Cretaceous|Late Jurassic|See also Lexicon.||||||
16267|Rolling Downs Group|43995|14|Not recorded|Tb.p9,20 Fig.9||Cretaceous|Inc. Roma Formation, Tambo Formation and Winton Formation in the Eromanga Sub-Basin.||||||
16267|Rolling Downs Group|44020|14|Not recorded|p10,Tb.1|Late Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|44033|14|Not recorded|Tb.1,opp.p4|||||||||
16267|Rolling Downs Group|44034|6|Mentioned|Tb.1,p2|||||||||
16267|Rolling Downs Group|44041|6|Mentioned|Fig.1|||||||||
16267|Rolling Downs Group|44087|14|Not recorded|p4|||||||||
16267|Rolling Downs Group|44089|14|Not recorded|Tb.1||Early Cretaceous|||||||
16267|Rolling Downs Group|44091|14|Not recorded|p60||Cretaceous|||||||
16267|Rolling Downs Group|44093|6|Mentioned|p68 (photo)|||Associated with Gum Vale beds.||||||
16267|Rolling Downs Group|44099|14|Not recorded|Map Legend|Late Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|44112|6|Mentioned|p82|||||||||
16267|Rolling Downs Group|44121|14|Not recorded|p8|||||||||
16267|Rolling Downs Group|44122|14|Not recorded|p322|||||||||
16267|Rolling Downs Group|44207|14|Not recorded|p116|||||||||
16267|Rolling Downs Group|44269|14|Not recorded|p16||Cretaceous|||||||
16267|Rolling Downs Group|44291|14|Not recorded|p5|||||||||
16267|Rolling Downs Group|44346|14|Not recorded|p4|||||||||
16267|Rolling Downs Group|44375|14|Not recorded|p313|||||||||
16267|Rolling Downs Group|44406|14|Not recorded|p4|||||||||
16267|Rolling Downs Group|44408|14|Not recorded|p4|||||||||
16267|Rolling Downs Group|44415|14|Not recorded|p22,Fig.2,p23|||||||||
16267|Rolling Downs Group|44417|2|Defined|p417-421|Albian|Aptian|Contains: Winton, Mackunda and Wilgunya Formations. Overlies Gilbert River Formation. Probably Cenomanian.||||||
16267|Rolling Downs Group|44739|14|Not recorded|p19|||||||||
16267|Rolling Downs Group|44740|14|Not recorded|p29,39-42,47,48,52,|||p55,56,77||||||
16267|Rolling Downs Group|44744|14|Not recorded|p106-113|||||||||
16267|Rolling Downs Group|44800|14|Not recorded|p16,22,map||Cretaceous|||||||
16267|Rolling Downs Group|44819|14|Not recorded|p89|Albian|Aptian|Shaley basal formation is Roma Formation.||||||
16267|Rolling Downs Group|44836|14|Not recorded|p5,11,Figs.1-5||Cretaceous|||||||
16267|Rolling Downs Group|44852|14|Not recorded|p78||Early Cretaceous|||||||
16267|Rolling Downs Group|44989|14|Not recorded|p.125,126|||(E54-14).||||||
16267|Rolling Downs Group|45004|14|Not recorded|p.8|||Tb.1.||||||
16267|Rolling Downs Group|45011|14|Not recorded|p18,20|||Whitehouse correlated sediments in Polland Shale with Rolling Downs Group.||||||
16267|Rolling Downs Group|45110|6|Mentioned|p6|||||||||
16267|Rolling Downs Group|45145|3|Fully described|Table 5|||See also p23.||||||31-OCT-06
16267|Rolling Downs Group|46791|4|Described|p44|||Refers Galloway (1967)||||||
16267|Rolling Downs Group|46802|6|Mentioned|p131|||||||||
16267|Rolling Downs Group|46812|5|Briefly described|p241|||||||||
16267|Rolling Downs Group|46854|6|Mentioned|Fig.1|||||||||
16267|Rolling Downs Group|46872|6|Mentioned|p108|||||||||
16267|Rolling Downs Group|46881|6|Mentioned|Table 2|||||||||
16267|Rolling Downs Group|46911|6|Mentioned|Fig.1|||Geological map and distribution of weathered profiles.||||||
16267|Rolling Downs Group|46937|6|Mentioned|Fig.10|||||||||
16267|Rolling Downs Group|46939|6|Mentioned|Fig.1|||||||||
16267|Rolling Downs Group|47042|6|Mentioned|p171|||||||||
16267|Rolling Downs Group|47083|5|Briefly described|p20||Mesozoic|Carpentaria Basin.||||||
16267|Rolling Downs Group|48908|14|Not recorded|Tb.1||Cretaceous|||||||
16267|Rolling Downs Group|48920|3|Fully described|p56|||Cretaceous||||||
16267|Rolling Downs Group|48951|6|Mentioned|Table 1|||||||||
16267|Rolling Downs Group|50100|5|Briefly described|p23|Cretaceous|Cretaceous|Comprises Wallumbilla and Toolebuc Formations, Allaru Mudstone and Mackunda Formation.  Overlies the Gilbert River Formation.  Geological Province:  Eromanga Basin.||||||
16267|Rolling Downs Group|60087|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Includes Allaru Mudstone, Toolebuc Limestone, and Wallumbilla Formation.||||||
16267|Rolling Downs Group|61312|5|Briefly described|p66, p73|Albian|Aptian|Supersedes "Rolling Downs Formation". Comprises Wallumbilla and Toolebuc Formations, and Allaru Mudstone and Winton Formation. Geological Province: Eromanga Basin.||||||
16267|Rolling Downs Group|61377|5|Briefly described|p148 Tb. SU1|Early Cretaceous|Early Cretaceous|Includes the Griman Creek Formation, Surat Siltstone and Wallumbilla Formation. Green silty mudstone, minor sandstone. Geological Province: Surat Basin. See also p149 Fig. SU8.||||||07-FEB-11
16267|Rolling Downs Group|61823|5|Briefly described|p118|||Part of a marine transgressive sequence; overlies Gum Vale and Cadna-Owie Formations. Geological Province: Eromanga Basin.||||||
16267|Rolling Downs Group|62837|5|Briefly described|Stratigraphic columns|Late Cretaceous|Early Cretaceous|Includes Wallumbilla Formation, Allaru Mudstone and Normanton Formation.  Age: ~114-91Ma. Geological Province: Northern Gulf of Carpentaria, Southern Cape York and Burketown Depression.||||||01-MAR-10
16267|Rolling Downs Group|63450|5|Briefly described|p83|Cretaceous|Jurassic|Overlies Hooray Sandstone/Cadna-owie Formation. Marine deposits.||||||07-FEB-11
16267|Rolling Downs Group|63789|5|Briefly described|Map Legend|Cretaceous|Late Jurassic|Includes Hooray Sandstone. Subaerial scree and slope debris deopsits on fossil hill slopes and valley walls containing dislodged angular blocks of underlying bedrock. Commonly with pebbly sand infill and silcrete cement.||||||08-DEC-08
16267|Rolling Downs Group|63790|5|Briefly described|Map Legend|Cretaceous|Late Jurassic|Includes Hooray Sandstone. Beach pebble, cobble and boulder deposits formed from white quartzose sandstone. Commonly with silcrete cement.||||||08-DEC-08
16267|Rolling Downs Group|63793|6|Mentioned|p10.|Cretaceous|Jurassic|Eromanga Basin.||||||
16267|Rolling Downs Group|63979|6|Mentioned|p51-52|||Includes the Wilgunyah Subgroup.||||||07-FEB-11
16267|Rolling Downs Group|64061|6|Mentioned|p66|Cretaceous|Cretaceous|Contains the Griman Creek Formation. Geological Province: Surat Basin.||||||24-APR-08
16267|Rolling Downs Group|64570|5|Briefly described|p858|Early Cretaceous|Early Cretaceous|Volcanogenic sedimentary rocks and are rich in volcanic lithics.||||||22-DEC-08
16267|Rolling Downs Group|64665|5|Briefly described|p53 Fig.2, p62.|Early Cretaceous|Early Cretaceous|Laura Basin.||||Overlies Gilbert River Formation.|Dominantly marine shales and siltstones.|
16267|Rolling Downs Group|64679|5|Briefly described|Map legend|Cretaceous|Cretaceous|Conglomerate (pebbles of rounded white vein quartz and quartzite), quartz sandstone, siltstone and claystone; commonly silicified or ferruginised.||||||27-NOV-08
16267|Rolling Downs Group|64681|5|Briefly described|p2, p3 Fig. 1|Cretaceous|Cretaceous|Geological province: Eromanga Basin. Sandstone, siltstone, claystone.||||||
16267|Rolling Downs Group|64682|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Feldspathic and lithic sandstone, siltstone and mudstone; strongly kaolinised, mottled and ferruginised, locally containes exotic ?drop? boulders.||||||
16267|Rolling Downs Group|64683|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Includes Hooray Sandstone. Rounded waterworn white vein quartz and quartzite conglomerate, quartzose sandstones, siltstones and claystones deposited on undulating topography in underlying bedrock.||||||
16267|Rolling Downs Group|64820|4|Described|pS9, pS6 Fig. 4|Late Cretaceous|Middle Jurassic|Contains Garroway Sandstone, Gilbert River, Wallumbilla and Toolbeuc Formations, Allaru Mudstone and Normanton Formation. Overlain by Bulimba Formation.||||||
16267|Rolling Downs Group|64821|5|Briefly described|pS18, pS20-21, pS40|Cretaceous|Cretaceous|Discussed in relation to its saprolite zone in the East Weipa and Andoom areas where lenses of weakly lithified sandstone, clay and siltstone dominate. Unconformably overlain by the Bulimba Formation.||||||02-FEB-09
16267|Rolling Downs Group|64822|5|Briefly described|pS88, pS99|||Together with the overlying Bulimba Fm, hosted the development of the Weipa bauxite deposit - composed of a transported blanket of bauxite overlying a lateritic weathering profile. Geol.prov: Weipa Sub-basin, Carpentaria Basin.||||||02-FEB-09
16267|Rolling Downs Group|66529|6|Mentioned|p12 Fig.5|||Eromanga, Carpentaria, Surat Basins and Coonamble Embayment.|||Includes Wallumbilla, Toolebuc, Mackunda, Winton, Griman Creek Formations; Surat Siltstone; and Allaru Mudstone.|||
16267|Rolling Downs Group|66623|3|Fully described|p108, pp238-245, pp256-267.|Late Cretaceous|Early Cretaceous|Widespread throughout Eromanga Basin. Thickness c.600 m. Generally poor outcrops. Has fair hydrocarbon reservoir (no source) potential, and good local seal potential. Porous sandstone units provide groundwater resources.|||Includes Wilgunya Subgroup (in Queensland), Wallumbilla Formation (at base), Allaru Mudstone and Winton Formation (at top).|Overlies Cadna-owie Formation. Is unconformably overlain by Eyre Formation. Unconformably overlies Yancannia Formation.|Alternation of sandstone-poor and sandstone-rich intervals deposited in a marine environment; ice-rafted dropstone boulders in lower units.|07-JUN-13
16267|Rolling Downs Group|66915|5|Briefly described|p4-5, p15-17|||In later Rolling Downs Group units, the Toolebuc Formation is the only distinct and laterally persistent seismic reflection for correlation and is widespread in the Eromanga Basin.|||Wallumbilla Formation, Toolebuc Formation|||12-JAN-17
16267|Rolling Downs Group|66917|5|Briefly described|Map legend|Cretaceous|Cretaceous||||Includes Namur Sandstone.||Rounded, waterworn, white vein quartz, quartzite, conglomerate, quartzose sandstones, siltstones and claystones; overall upward-fining sequence with sparse marine fossils and large, rounded, quartzite dropstones.|
16267|Rolling Downs Group|66918|5|Briefly described|Map legend|Cretaceous|Cretaceous||||||Rounded, waterworn, white vein quartz and quartzite; conglomerate; quartzose sandstone; siltstones and claystones; overall upward-fining sequence with sparse marine fossils and large, rounded quartzite dropstones.|
16267|Rolling Downs Group|66920|5|Briefly described|Map legend|Cretaceous|Cretaceous||||Includes Wallumbilla Formation.||Rounded, waterworn, white vein quartz, quartzite, conglomerate, quartzose sandstones, siltstones and claystones; overall upward-fining sequence with sparse marine fossils and large, rounded, quartzite dropstones.|
16267|Rolling Downs Group|66921|6|Mentioned|Map legend|Cretaceous|Cretaceous||||Includes Cadna-owie Formation.|||
16267|Rolling Downs Group|67105|6|Mentioned|p661|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|67207|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||Includes Wallumbilla Formation.||Rounded, waterworn, white vein quartz, quartzite, conglomerate, quartzose sandstones, siltstones and claystones; overall upward-fining sequence with sparse marine fossils and large, rounded quartzite dropstones.|
16267|Rolling Downs Group|67208|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||||Rounded, waterworn, white vein quartz, quartzite, conglomerate, quartzose sandstones, siltstones and claystones; overall upward-fining sequence with sparse marine fossils and large, rounded quartzite dropstones.|
16267|Rolling Downs Group|67209|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||Includes Wallumbilla Formation and Allaru Mudstone.|Overlies Cadna-owie Formation. Is overlain by Cordillo Silcrete.|Rounded, waterworn, white vein quartz, quartzite, conglomerate, quartzose sandstones, siltstones and claystones; overall upward-fining sequence with sparse marine fossils and large, rounded, quartzite dropstones.|
16267|Rolling Downs Group|67210|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||||Overlies Yancannia Formation. Unconformably overlies Warratta Group. Is overlain by Eyre Formation.|Marine white claystones, siltstones and fine-grained quartzose sandstones with bioturbation.|
16267|Rolling Downs Group|67211|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||Includes Wallumbilla Formation and Allaru Mudstone.|Overlies Bunker Creek Formation and Warratta Group.|Rounded, waterworn, white vein quartz, quartzite, conglomerate, quartzose sandstones, siltstones and claystones; overall upward-fining sequence with sparse marine fossils and large, rounded, quartzite dropstones.|
16267|Rolling Downs Group|67402|4|Described|p179, p226-p230, p232, p309|Cenomanian|Aptian|Proven hydrocarbon seal in the Eromanga Basin with a combined thickness of up to 1500m; also present in the Laura Basin. Formerly the Battle Camp Shale and the Wolena Claystone.|||Includes the Allaru Mudstone, Toolebuc Formation and the Wallumbilla Formation|Overlies the Gilbert River Formation|Basal shale with minor silty and conglomeratic beds that is overlain by silty or sandy claystone with calcareous concretions.|
16267|Rolling Downs Group|67669|5|Briefly described|p11|Early Cretaceous|Early Cretaceous|Of Bowen Basin.|||Includes Wallumbilla Formation.|Underlain by Blythesdale Group.||
16267|Rolling Downs Group|68003|5|Briefly described|p52, p57 Fig.3-n, pp70-71, p127.|Early Cretaceous|Early Cretaceous|Surat Basin. Deposited in a major marine transgression-regression cycle.|||Includes Wallumbilla Formation, Surat Siltstone and Griman Creek Formation.|Overlies Bungil Formation and Drildool beds conformably.|Semiconsolidated clays and claystone with minor fine clayey quartz sandstone; coal and calcareous clay and calcarenite occur near the base; rare conglomerate and gravel.|
16267|Rolling Downs Group|68004|6|Mentioned|p131, p205.|Early Cretaceous|Early Cretaceous|Hosts the Lightning Ridge Opal Field. Mineral potential tracts and levels of certainty are discussed.||||||
16267|Rolling Downs Group|68069|5|Briefly described|Map legend, p2.|Cretaceous|Cretaceous|Surat Basin.|||Includes Wallumbilla Formation, Surat Siltstone and Griman Creek Formation.|||
16267|Rolling Downs Group|68553|6|Mentioned|Map legend; schematic diagram.|Cretaceous|Cretaceous|Surat, Laura, Carpentaria and Eromanga Basins.|||Includes Wallumbilla, Griman Creek, Toolebuc, Normanton, Mackunda and Winton Formations, and Allaru Mudstone.|||
16267|Rolling Downs Group|68593|5|Briefly described|p3-4|Early Cretaceous|Early Cretaceous|See individual units.|||Purlawaugh, Griman Creek Formations; Surat Siltstone.|Overlies Bungil Formation.||
16267|Rolling Downs Group|68734|5|Briefly described|p218 Fig.2|Albian|Barremian|Eromanga Basin (SW and NE) and Surat Basin.|||Includes Winton, Mackunda, Oodnadatta, Toolebuc, Wallumbilla, and Griman Creek Formations; Coorikiana Sandstone; Bulldog Shale; Allaru Mudstone; and Surat Siltstone.|||16-JAN-17
16267|Rolling Downs Group|68821|5|Briefly described|p292 Fig.1, p295|Cretaceous|Cretaceous|Lower Cretaceous age. Includes both marine and fluvial sedimentary rocks. Thick fluvial to coastal plain sequence.|||Includes Winton Formation, Mackunda Formation, Griman Creek Formation, Allaru Formation, Toolebuc Formation, Surat Siltstone, and Bulldog Shale.||Comprises carbonaceous and pyritic shale, siltstone, and coarse volcaniclastic sandstone with minor coal layers.|
16267|Rolling Downs Group|68901|6|Mentioned|p7 Fig. ii|||Eromanga Basin.|||Includes the Winton and Wallumbilla Formations.|||27-SEP-18
16267|Rolling Downs Group|69001|6|Mentioned|p2 Fig.1B, p30|Cretaceous|Cretaceous||||Includes the Doncaster Member.|||
16267|Rolling Downs Group|69297|6|Mentioned|p274 fig 4.3|Cenomanian|Early Cretaceous||||Includes the Wallumbilla Formation, Allaru Mudstone, Toolebuc Formation and the Normanton Formation.|||
16267|Rolling Downs Group|69455|6|Mentioned|p39:2, 39:4 Fig.39.3|Cretaceous|Cretaceous|Central Carpentaria Basin.||||||12-JUL-16
16267|Rolling Downs Group|69457|5|Briefly described|p41:2, 6, 8, 12|||Whitehouse (1955). Applies to the succession in SW Eromanga Basin, from the top of the (ungrouped) Cadna-owie Formation to the top of the Winton Formation. Up to c.1700m thick.|||Wilgunya, Manuka, Marree Subgroups.|Overlies Cadna-owie Formation.||12-JUL-16
16267|Rolling Downs Group|69555|6|Mentioned|p46||||||Includes Winton Formation|||
16267|Rolling Downs Group|69591|6|Mentioned|p29|Cretaceous|Jurassic|||||||
16267|Rolling Downs Group|69594|4|Described|p521-522, p540, p573-574|Late Cretaceous|Aptian|Carpentaria, Laura Basins. Source of lateritic bauxite (at Weipa) and kaolin, formed by deep weathering during the Late Cretaceous regression. The Group acts as the confining beds for the main aquifers in the Basin. Not subdivided in the Laura Basin, where it is up to 212m thick and is equivalent to the Wallumbilla Formation in the Eromanga Basin. Coeval with Allaru Mudstone. Youngest deposit in the Laura Basin.|||Wallumbilla, Toolebuc Formations; Allaru Mudstone; Normanton Formation.|Conformably overlies Gilbert River Formation. Is equivalent to upper Battle Camp Formation, Wolena Claystone.|Undivided: basal marine unit of calcareous and glauconitic shales with minor siltstone and conglomerate, overlain by silty and sandy marine claystones with carbonate concretions.|
16267|Rolling Downs Group|69599|5|Briefly described|p601-602|Cretaceous|Cretaceous|Lateritisation of this unit produced the world's largest bauxite deposit at Weipa.|||Normanton Formation.|||
16267|Rolling Downs Group|69673|6|Mentioned|p156||||||Includes Wilgunya Subgroup, Manuka Subgroup|||
16267|Rolling Downs Group|69682|5|Briefly described|p93 Fig.1|Cretaceous|Cretaceous|Eromanga and Surat Basins.||||||
16267|Rolling Downs Group|69952|5|Briefly described|p16|Cretaceous|Cretaceous|Eromanga Basin.|||Includes Winton and Wallumbilla Formations.|||
16267|Rolling Downs Group|69961|5|Briefly described|Map legend|Cretaceous|Cretaceous||||Includes Namur Sandstone?||Rounded, waterworn white vein quartz, quartzite, conglomerate, quartzose sandstones, siltstones and claystones; sparse marine fossils; large quartzite dropstones. Bioturbated marine white claystones, siltstones and fine-grained quartzose sandstones.|16-SEP-15
16267|Rolling Downs Group|70036|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Surat Basin. Included in a mapped unit of a marine sequence of semi-consolidated clay and claystone, minor fine quartz sandstone, coal and calcareous clay.||||||
16267|Rolling Downs Group|70207|6|Mentioned|p74|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|70345|6|Mentioned|p3|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|70352|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous||||Wilgunya Subgroup.|||
16267|Rolling Downs Group|70354|5|Briefly described|Map legend|Cretaceous|Cretaceous||||Wallumbilla, Toolebuc Formations; Allaru Mudstone.|||
16267|Rolling Downs Group|70572|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous||||Includes Wilgunya Subgroup.|||
16267|Rolling Downs Group|70648|5|Briefly described|Map Legend|Cretaceous|Cretaceous|2 un-named units: Marine white claystone, siltstone and fine-grained quartzose sandstone with bioturbation. Silicified variant.|||Includes 2 un-named units.||Rounded, waterworn, white vein quartz, quartzite, conglomerate, quartzose sandstone, siltstone and claystone; overall upward-fining sequence with sparse marine fossils and large, rounded quartzite dropstones.|
16267|Rolling Downs Group|70649|5|Briefly described|Map Legend|Cretaceous|Cretaceous||||Includes Winton Formation, Allaru Mudstone, Wallumbilla Formation.||Rounded, waterworn, white vein quartz, quartzite, conglomerate, quartzose sandstone, calcareous sandstone, siltstone and claystone; overall upward-fining sequence with sparse marine fossils and large, rounded quartzite dropstones.|
16267|Rolling Downs Group|70650|5|Briefly described|Map Legend|Cretaceous|Cretaceous||||||Rounded, waterworn, white vein quartz quartzite, conglomerate, quartzose sandstone, siltstone and claystone; overall upward-fining sequence with sparse marine fossils and large, rounded quartzite dropstones.|
16267|Rolling Downs Group|70651|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Includes unnamed sub-unit of marine white claystone, siltstone and fine-grained quartzose sandstone with bioturbation.|||Includes unnamed unit.||Rounded, waterworn, white vein quartz, quartzite, conglomerate, quartzose sandstone, siltstone and claystone; overall upward fining sequence with sparse marine fossils and large rounded quartzite dropstones.|
16267|Rolling Downs Group|70652|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Rounded quartz-rich gravel sourced from Namur Sandstone. Residual lag regolith and unconsolidated sediments also described.|||Includes Wallumbilla Formation.||Rounded, waterworn, white vein quartz, quartzite, conglomerate, quartzose sandstone, calcareous sandstone, siltstone and claystone; overall upward-fining sequence with sparse marine fossils and large, rounded quartzite dropstones.|
16267|Rolling Downs Group|70673|6|Mentioned|p7|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|70821|5|Briefly described|p21, p30-31, p33, p80, p109, p113-114|Late Cretaceous|Early Cretaceous|Eromanga, Surat Basins; Coonamble Embayment. Formerly included Hooray Sandstone. Sediments locally occupy palaeovalleys (eg Gongolgon).|||Wallumbilla, Toolebuc, Mackunda, Griman Creek, Winton Formations; Surat Siltstone; Allaru Mudstone.|Overlies Bungil or Cadna-owie Formations and Drildool beds. Is overlain unconformably by Glendower Formation.||
16267|Rolling Downs Group|70836|6|Mentioned|p474|||Lightning Ridge area, Surat Basin.|||Griman Creek Formation.|||
16267|Rolling Downs Group|70860|6|Mentioned|p280-281|Cretaceous|Cretaceous|The main confining layer in the Great Artesian Basin.|||||A thick argillaceous marine sequence; mostly shallow-marine mudstone and siltstone.|
16267|Rolling Downs Group|71262|6|Mentioned|p9 Fig 7|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|71342|6|Mentioned|Ch6 p12|||Originally subdivided by Whitehouse in 1926 who also subdivided this groups constituents into three sets of bed based on ammonite fauna. This scheme however was called into question by Casey (1960) and Day (1969). The validity of the Roma and Tambo Series was demonstrated by later workers (Dickins, 1960; Ludbrook, 1966; Day; 1969 and Morgan, 1980).|||Includes the Morven Bed, Roma Series, Maryborough Beds and the Tambo Series.|||
16267|Rolling Downs Group|71409|5|Briefly described|p1058-1059, p1061|Cretaceous|Cretaceous|Carpentaria Basin. Likely proximal source rocks for heavy minerals in central Cape York Peninsula. Outcrops in the northern tip of the Cape York Peninsula.||||Is overlain locally by Bulimba Formation.|Siltstones and claystones; deeply weathered and bauxitised.|23-APR-18
16267|Rolling Downs Group|71415|5|Briefly described|p11-p12|Late Cretaceous|Early Cretaceous|Geological province: SW Thomson Orogen. Of the Kooneberry Belt; of Eromanga Basin. Represents sedimentation from Early to Late Cretaceous before marine regression and closure of the Eromanga Basin (Exon and Senior 1976; Greenfield, Gilmore and Mills 2010).||||Uppermost unit of the Eromanga Basin. Underlain by Cadna-owie Formation.|Alternating sandstone, mudstone and calcareous units.|19-AUG-19
16267|Rolling Downs Group|71601|6|Mentioned|p121|||Geological province: Surat Basin.|||Includes Griman Creek Formation.|||
16267|Rolling Downs Group|71792|4|Described|p57-p58|Late Cretaceous|Early Cretaceous|Carpentaria Basin.|||||Grey mudstone, siltstone and fine sandstone, minor glauconitic sandstone.|
16267|Rolling Downs Group|71849|6|Mentioned|p8, p195|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|71853|5|Briefly described|Map legend.|Late Cretaceous|Early Cretaceous|The two facies are mapped separately.|||||Siltstone and mudstone; minor glauconitic sandstone. Deeply weathered siltstone and mudstone; minor glauconitic sandstone.|
16267|Rolling Downs Group|71854|5|Briefly described|Map legend.|Late Cretaceous|Early Cretaceous||||||Siltstone and mudstone with minor glauconitic sandstone; Deeply weathered siltstone and mudstone with minor glauconitic sandstone.|08-MAY-19
16267|Rolling Downs Group|71855|6|Mentioned|p20, p30|||Structure is briefly discussed.|||Includes the Toolebuc Formation.|||
16267|Rolling Downs Group|71863|5|Briefly described|p4|Late Cretaceous|Middle Jurassic|Carpentaria Basin. Deposited during a marine incursion.|||Includes the Wallumbilla Formation, the Toolebuc Formation, Allaru Mudstone and Normanton Formation.|||01-MAY-19
16267|Rolling Downs Group|71864|6|Mentioned|p13|||First described by Isbell (1957).|||Includes the Wallumbilla Formation.|||
16267|Rolling Downs Group|71890|6|Mentioned|p7|||Surat Basin.|||Includes the Wallumbilla Formation.|||
16267|Rolling Downs Group|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA,QLD,NSW), Carpentaria Basin, Surat Basin (QLD,NSW), Coonamble Embayment (NSW).|||Wallumbilla, Toolebuc, Mackunda, Winton, Normanton, Griman Creek FZs; Surat Siltstone; Allaru Mudstone.|Overlies Cadna-owie, Gilbert River, or Bungil FZ.||
16267|Rolling Downs Group|72914|6|Mentioned|p12|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|72915|6|Mentioned|p12, p26|Mesozoic|Mesozoic|Sedimentary rocks in the Congararra 1 borehole are attributed to the Rolling Downs Group (map symbol suggests Cretaceous age), and may represent source-proximal Wallumbilla Formation (after Hawke and Cramsie, 1984). Represented in the Congararra 1 borehole by 41.15 m TVD thickness of interbedded claystone, siltstone, sandstone and arkose where the top portion is an indurated silcrete (to 23.53 m TVD), and is weathered to ~42 m TVD, before becoming fresh gravelly sand.|||||Interbedded claystone, siltstone, sandstone and arkose|
16267|Rolling Downs Group|72967|6|Mentioned|p5|||Carpenteria Basin.|||Allaru Mudstone, Toolebuc Formation, Wallumbilla Formation, Gilbert River Formation|||
16267|Rolling Downs Group|72983|6|Mentioned|p15|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|73083|6|Mentioned|p51, p60-61, p68-69, p73|Mesozoic|Mesozoic|[Misspelt as Rolling Downs group on p61].|||Normanton Formation|||
16267|Rolling Downs Group|73144|6|Mentioned|p8|Cretaceous|Cretaceous|Carpentaria Basin. Contains units that constitute aquifers, partial aquifers, leaky aquitards and aquitards as well as host potential shale gas/oil plays and tight gas/oil.|||Normanton Formation, Allaru Mudstone, Toolebuc Formation, Wallumbilla Formation.|Underlain by Gilbert River Formation.||17-OCT-22
16267|Rolling Downs Group|73147|5|Briefly described|p128-129|Albian|Aptian|Marine.|||Wallumbilla, Toolebuc, Normanton Formations; Allaru Mudstone.|||
16267|Rolling Downs Group|73177|5|Briefly described|p1112|Late Jurassic|Late Jurassic|Relatively undeformed; gives a minimum age for the Alice Springs Orogeny.||||Unconformably overlies Ravendale Formation.||
16319|Roper Group|22479|5|Briefly described|fig4, pg10|Calymmian|Calymmian|||||||
16319|Roper Group|22538|4|Described|P710, Fig4, P718|Calymmian|Calymmian|Part of the Wilton package||||||
16319|Roper Group|22600|4|Described|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
16319|Roper Group|22644|6|Mentioned|4,7,9|||Geol province McArthur Basin||||||
16319|Roper Group|22662|6|Mentioned|22,23 fig 2|Mesoproterozoic|Mesoproterozoic|Geol province McArthur Basin||||||
16319|Roper Group|22664|6|Mentioned|Fig. 1 p34|||In the McArthur Basin.||||||28-NOV-06
16319|Roper Group|22670|6|Mentioned|51,55-57,59,60|||Geol province McArthur Basin||||||
16319|Roper Group|22673|6|Mentioned|65|||Geol province McArthur Basin||||||
16319|Roper Group|22808|6|Mentioned|7 fig 4|||||||||
16319|Roper Group|22853|3|Fully described|24|Proterozoic|Proterozoic|Min age: 1280 Ma; max age: 1430 Ma. Max thickness: 5 km. Underlain by McArthur Group and Nathan Group.||||||28-NOV-06
16319|Roper Group|23115|5|Briefly described|p462|||||||||
16319|Roper Group|23216|4|Described|Fig3p5,Table1p7,33,51|Calymmian|Calymmian|Min Age: 1429 Ma. Previously: Flying Fox Group (Ruker, 1959).||||||
16319|Roper Group|23328|5|Briefly described|1031 Fig.2|Proterozoic|Proterozoic|||||||07-SEP-09
16319|Roper Group|23362|6|Mentioned|339 Fig.2|||||||||
16319|Roper Group|23363|6|Mentioned|369|||||||||
16319|Roper Group|23374|5|Briefly described|Fig3p5,6,20,29,30,34,35||Mesoproterozoic|In the McArthur Basin.||||||28-NOV-06
16319|Roper Group|23393|5|Briefly described|p17 Fig. 5|Mesoproterozoic|Mesoproterozoic|Geological Province: McArthur Basin.||||||
16319|Roper Group|23396|6|Mentioned|p425|||||||||
16319|Roper Group|23404|4|Described|p637|||||||||
16319|Roper Group|23406|6|Mentioned|p606|||Age at base: 1493+/-4Ma (SHRIMP U-Pb, Page et al 2000).||||||16-JUN-09
16319|Roper Group|23407|5|Briefly described|p626 Fig.1|||||||||
16319|Roper Group|23409|6|Mentioned|p536|||||||||
16319|Roper Group|23733|6|Mentioned|p31|||Geological Province: MacArthur Basin.  See also p32 Fig. 19.||||||
16319|Roper Group|23776|5|Briefly described|p709|Calymmian|Calymmian|Age: 1500-1425 Ma.||||||28-NOV-06
16319|Roper Group|23809|5|Briefly described|p47 Fig. 42|Proterozoic|Proterozoic|Geological Province: McArthur Basin.  Correlates with Helicopter Sandstone and Ahern Formation, and  Auvergne Group (Victoria Basin) and Renner Group (Ashburton Province).||||||29-NOV-04
16319|Roper Group|23867|6|Mentioned|p2|||||||||
16319|Roper Group|23902|6|Mentioned|p1568 Fig.1|||Geological Province: McArthur Basin||||||
16319|Roper Group|23910|6|Mentioned|p291|||Geological Province: McArthur Basin.||||||
16319|Roper Group|23937|2|Defined|p91 App. 1, p22-23|Calymmian|Calymmian|Formerly the Flying Fox Group of Ruker (1959).  Age: 1490Ma (upper). Subdivided into 2 subgroups: Collara (lower part) and Maiwok (upper part) Subgps.  Overlies rocks of McArthur, Nathan and Mount Rigg Gps. Geol.Prov: McArthur Basin/Roper Superbasin.||||||02-NOV-04
16319|Roper Group|23963|6|Mentioned|p1238|||Geological Province: McArthur Basin.||||||10-MAR-05
16319|Roper Group|24047|5|Briefly described|p12 Fig. 10|Mesoproterozoic|Mesoproterozoic|Age: <1490Ma.  Geological Province: McArthur Basin.||||||
16319|Roper Group|24048|3|Fully described|p68|||Geological Province: McArthur Basin.||||||
16319|Roper Group|24049|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Includes Bessie Creek Sandstone, Corcoran Formation, Hodgson Sandstone, Jalboi Formation, Arnold Sandstone, Crawford Formation, Mainoru Formation and Limmen Sandstone. Geol. Prov: McArthur Basin.||||||13-OCT-05
16319|Roper Group|24050|3|Fully described|p40, p8 Tb. 2|Mesoproterozoic|Mesoproterozoic|Formerly the Flying Fox Group.||||||
16319|Roper Group|24051|5|Briefly described|Map Legend|Calymmian|Calymmian|Geological Province: McArthur Basin.||||||
16319|Roper Group|24169|5|Briefly described|p674|||Geological Province : McArthur Basin.  See also Roper River Group.||||||
16319|Roper Group|24179|5|Briefly described|p90|Mesoproterozoic|Mesoproterozoic|Overlies the Nathan group.  Geological Province:  McArthur Basin.||||||
16319|Roper Group|24303|5|Briefly described|p24|Mesoproterozoic|Mesoproterozoic|Correlates with Renner Group.||||||
16319|Roper Group|24419|5|Briefly described|p13 Fig.5|Mesoproterozoic|Mesoproterozoic|Geological Province: McArthur Basin||||||
16319|Roper Group|24442|6|Mentioned|p23|||||||||
16319|Roper Group|24522|6|Mentioned|p80 Fig. 2|||Geological Province: McArthur Basin/Mount Isa Inlier.||||||
16319|Roper Group|29550|6|Mentioned|Pl.6|||||||||
16319|Roper Group|30258|6|Mentioned|p104|||||||||
16319|Roper Group|30344|6|Mentioned|p29|||See also Fig.4||||||
16319|Roper Group|30345|6|Mentioned|Table 1|||Adelaidean age. Lithology||||||
16319|Roper Group|32144|6|Mentioned|p81|||Solvent extractable organic matter||||||
16319|Roper Group|32479|6|Mentioned|Fig.1|||||||||
16319|Roper Group|32658|6|Mentioned|p103|||See also Fig.3||||||
16319|Roper Group|32659|6|Mentioned|Map legend|Adelaidean|Carpentarian|Carpentarian or Adelaidean||||||
16319|Roper Group|32660|4|Described|Table 4|||||||||
16319|Roper Group|33665|6|Mentioned|p365|||||||||
16319|Roper Group|33900|6|Mentioned|p19|||||||||
16319|Roper Group|34053|6|Mentioned|p10|||Prot.||||||
16319|Roper Group|34287|6|Mentioned|p41|||||||||
16319|Roper Group|34438|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
16319|Roper Group|34439|5|Briefly described|Table 1|||Adelaidean. See also pp6,11.||||||28-NOV-06
16319|Roper Group|34440|6|Mentioned|p9|||||||||
16319|Roper Group|34754|6|Mentioned|p15|||||||||
16319|Roper Group|35114|6|Mentioned|p203|||||||||
16319|Roper Group|35162|6|Mentioned|Table.1|||||||||
16319|Roper Group|35261|6|Mentioned|Fig.1|||||||||
16319|Roper Group|35495|6|Mentioned|p341|||||||||
16319|Roper Group|35950|6|Mentioned|p311|||||||||
16319|Roper Group|36003|5|Briefly described|p1029|||||||||
16319|Roper Group|36473|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
16319|Roper Group|37217|6|Mentioned|p650|||||||||
16319|Roper Group|37371|6|Mentioned|p368|||||||||
16319|Roper Group|37462|4|Described|Table4.IV|||||||||
16319|Roper Group|37565|5|Briefly described|p3|||See also p11.||||||28-NOV-06
16319|Roper Group|37568|4|Described|p79|||||||||
16319|Roper Group|38042|6|Mentioned|p160|||||||||
16319|Roper Group|38156|6|Mentioned|Fig.1|||||||||
16319|Roper Group|38348|6|Mentioned|p8|||||||||
16319|Roper Group|38529|6|Mentioned|p275|||||||||
16319|Roper Group|38582|6|Mentioned|p215|||||||||
16319|Roper Group|38902|6|Mentioned|p20|||||||||
16319|Roper Group|39122|6|Mentioned|p154|||||||||
16319|Roper Group|39210|6|Mentioned|p50|||||||||
16319|Roper Group|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
16319|Roper Group|40105|6|Mentioned|p315|||||||||
16319|Roper Group|40109|5|Briefly described|p302|||||||||
16319|Roper Group|40259|6|Mentioned|Table 1|||||||||
16319|Roper Group|40691|3|Fully described|p11|||||||||
16319|Roper Group|40701|5|Briefly described|p41|||||||||
16319|Roper Group|40973|6|Mentioned|p193|||||||||
16319|Roper Group|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
16319|Roper Group|41019|5|Briefly described|p243|||||||||
16319|Roper Group|41220|5|Briefly described|p371|||||||||
16319|Roper Group|41268|3|Fully described|p289|||||||||
16319|Roper Group|41277|6|Mentioned|Fig.2|||||||||
16319|Roper Group|41406|6|Mentioned|Map legend|Mesoproterozoic||||||||
16319|Roper Group|41531|5|Briefly described|p165|||||||||
16319|Roper Group|41594|6|Mentioned|p73|||||||||
16319|Roper Group|41721|6|Mentioned|p27|||Its sediments unconformably cover Karns Dolomite in the northern part of CALVERT HILLS SHEETS.||||||01-AUG-07
16319|Roper Group|42058|6|Mentioned|p118|||||||||
16319|Roper Group|42060|6|Mentioned|p139|||||||||
16319|Roper Group|42343|6|Mentioned|p28|||||||||
16319|Roper Group|42385|4|Described|p24|||See also Table 5 p25.||||||28-NOV-06
16319|Roper Group|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
16319|Roper Group|42395|5|Briefly described|Fig.26 P86|||Age 1429 +/- 31Ma Rb/Sr.||||||28-NOV-06
16319|Roper Group|42597|5|Briefly described|Map legend|Adelaidean||||||||
16319|Roper Group|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.|||Maiwok Subgroup (2 formations) overlying Lower Roper Group (6 formations).|Overlies Nathan Group.||11-NOV-11
16319|Roper Group|42639|4|Described|p37, Table 7 p39|||||||||
16319|Roper Group|42700|5|Briefly described|map legend|Mesozoic|Early Cretaceous|||||||
16319|Roper Group|42739|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|||||||19-OCT-05
16319|Roper Group|42775|6|Mentioned|Fig.13 P323|||||||||
16319|Roper Group|42812|4|Described|p45, Table 5|||||||||
16319|Roper Group|42846|4|Described|p503, Fig.1 p502|||Geological Province: McArthur Basin.||||||09-MAY-05
16319|Roper Group|42935|6|Mentioned|p527|||||||||
16319|Roper Group|43010|4|Described|p157|||see also Table 30.||||||
16319|Roper Group|43036|4|Described|p57|||||||||
16319|Roper Group|43149|5|Briefly described|Map Legend||Mesoproterozoic|Of Calymmian age.||||||
16319|Roper Group|43292|5|Briefly described|Map Legend||Mesoproterozoic|||||||
16319|Roper Group|43561|5|Briefly described|Fig.3,1434,1438-39|||Age: approx 1430 Ma.||||||28-NOV-06
16319|Roper Group|43595|5|Briefly described|p438||Mesoproterozoic|||||||
16319|Roper Group|43645|5|Briefly described|p561||Mesoproterozoic|||||||
16319|Roper Group|43652|6|Mentioned|p386|Neoproterozoic|Mesoproterozoic|||||||
16319|Roper Group|43788|6|Mentioned|p13||Proterozoic|||||||
16319|Roper Group|44112|3|Fully described|p2,11,68,73,97|Calymmian||Part of Supersequence 5. Overlies all older basin packages with regional unconformity; may be equivalent with Nathan Group. Min Age: 1429 (+/-) 31 Ma.||||||
16319|Roper Group|44201|14|Not recorded|p.7||Neoproterozoic|U.Proterozoic.||||||
16319|Roper Group|44287|14|Not recorded|p.6-19|||(E53-3).||||||
16319|Roper Group|44288|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
16319|Roper Group|44299|4|Described|p.13|||SD/53-7,8. Upper(?) Proterozoic. Table 1.||||||
16319|Roper Group|44300|14|Not recorded|map legend|||SD/53-7,8. Upper (?) Proterozoic.||||||
16319|Roper Group|44305|14|Not recorded|p.14|||(E53-8).||||||
16319|Roper Group|44332|14|Not recorded|p.7-12,opp.6,map|||(D53-14).||||||
16319|Roper Group|44333|14|Not recorded|map legend|||Upper(?) Proterozoic.||||||
16319|Roper Group|44338|14|Not recorded|opp.p.6|||(C53-14).||||||
16319|Roper Group|44400|2|Defined|p.9,11,12|||See also p.4,5,7,Tb.1,opp.p.6,map.||||||
16319|Roper Group|44401|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
16319|Roper Group|44434|14|Not recorded|p.7-11,opp. p.6, map|||Here includes Limmen Sandstone, Mainoru Formation (1 member), Crawford Formation, Abner Sandstone (2 members), Corcoran Formation, Bessie Creek Sandstone (top). (D53-11,12).||||||
16319|Roper Group|44435|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
16319|Roper Group|44436|5|Briefly described|p.6,10-11,opp.7,map|||(E53-4).||||||02-DEC-04
16319|Roper Group|44437|5|Briefly described|map legend|Precambrian|Precambrian|Includes the Abner and Limmen Sandstones, and the Crawford and Mainoru Formations.  Overlies the McArthur Group.||||||08-DEC-04
16319|Roper Group|44459|14|Not recorded|p.7-11, opp.p.6, map|||(E53-2). In Tanumbirini sheet area includes: Limmen Sandstone, Mainoru Formation, Crawford Formation, Abner Sandstone (3 members), Corcoran Formation, Bessie Creek Sandstone & Cobanbirini Formation (top).||||||
16319|Roper Group|44460|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
16319|Roper Group|44471|14|Not recorded|p.8-13, opp.p.7, map|||(D53-10).||||||
16319|Roper Group|44472|5|Briefly described|map legend|||Includes the Maiwok Sub-Group.  Upper (?) Proterozoic.||||||02-DEC-04
16319|Roper Group|44473|14|Not recorded|p.7,10,13,15,opp.p.7|||(E53-7). Includes in Wallhallow sheet area Limmen Sandstone, Mainoru Formation, Crawford Formation & Arnold Sandstone Member (Abner Sandstone) at top of group.||||||
16319|Roper Group|44474|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
16319|Roper Group|44475|14|Not recorded|p.7|||(C53-15,16). Tentatively correlated with Malay Road Group.||||||
16319|Roper Group|44482|14|Not recorded|p.7|||(E53-12).||||||
16319|Roper Group|44530|14|Not recorded|p.6-17|||(D53-15).||||||
16319|Roper Group|44531|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
16319|Roper Group|45022|4|Described|p.79.||Adelaidean|On many pages.||||||28-NOV-06
16319|Roper Group|45032|14|Not recorded|p9||Adelaidean|Tb.1, Pl.1.||||||
16319|Roper Group|45064|5|Briefly described|p14|||||||||
16319|Roper Group|45112|5|Briefly described|p29|||||||||
16319|Roper Group|45140|6|Mentioned|p13|||McArthur Basin region.|~1400 Ma.|||||
16319|Roper Group|45162|3|Fully described|p148|||||||||
16319|Roper Group|45166|5|Briefly described|p33|||||||||
16319|Roper Group|46679|14|Not recorded|map legend||Neoproterozoic|Upper Proterozoic.||||||
16319|Roper Group|46792|6|Mentioned|p53|||Dates||||||
16319|Roper Group|46861|6|Mentioned|Fig.2a|||||||||
16319|Roper Group|46915|6|Mentioned|Fig.1|||Stratigraphic section through McArthur Group.||||||
16319|Roper Group|46968|6|Mentioned|Fig.1|||See also Fig.2.||||||
16319|Roper Group|46975|6|Mentioned|p86|||||||||
16319|Roper Group|49001|6|Mentioned|p15|||||||||
16319|Roper Group|49482|14|Not recorded|?|||Not a publication.||||||
16319|Roper Group|50225|5|Briefly described|p406 Fig. 10, p407|Mesoproterozoic|Mesoproterozoic|Geological Province: Roper Superbasin.||||||07-FEB-11
16319|Roper Group|50545|5|Briefly described|p116||Ectasian|Overlies Katherine River Group.||||||17-DEC-07
16319|Roper Group|60483|4|Described|p7 Fig. 5, p9|||Includes Maiwok Subgroup as well as 9 formations. Unconformable on Nathan Group. Thickness: up to 5km. Geological Province: McArthur Basin. Cyclic succession of fine- to coarse-grained silicilcastic rocks.||||||
16319|Roper Group|60558|5|Briefly described|p7, p8 Fig. 6|Proterozoic|Proterozoic|Includes nine units and Maiwok Subgroup. Consists of cyclic marine shelf sandstones and mudstones.||||||03-JUN-09
16319|Roper Group|60573|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
16319|Roper Group|60574|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: McArthur Basin. Includes: Mantungula Formation, Limmen Sandstone, Mainoru Formation, Crawford Formation, Abner Sandstone.||||||
16319|Roper Group|61390|5|Briefly described|Map Legend|Ectasian|Calymmian|Includes the Maiwok Subgroup and the Collara Subgroup.||||||
16319|Roper Group|61403|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Includes Bessie Creek Sandstone, Corcoran Formation, Hodgson Sandstone, Jalboi Formation, Arnold Sandstone, Crawford Formation, Mainoru Formation and Limmen Sandstone. Geol. Prov: McArthur Basin.||||||
16319|Roper Group|61566|5|Briefly described|p622|Cretaceous|Cretaceous|Alternating succession of greywacke, mica-rich siltstone (Mainoru and Corcoran Formations) and mature quartzite and sandstones (Limmen, Abner and Bessie Creek Sandstones). Geological Province: McArthur Basin.||||||26-APR-06
16319|Roper Group|61572|5|Briefly described|p667 Fig. 2|Mesoproterozoic|Mesoproterozoic|Quartz sandstone units alternate with units of fine sandstone, mudstone and siltstone. Unconformably overlies Mount Rigg Group.  Age: ca 1493-1430Ma. Max. thickness: 900m. Geological Province: McArthur Basin. See also p671 Tb. 1||||||
16319|Roper Group|62376|5|Briefly described|p38|Mesoproterozoic|Mesoproterozoic|Geological Province: Beetaloo Sub-Basin.||||||09-FEB-10
16319|Roper Group|63062|5|Briefly described|p38|||Includes Velkerri Formation. Geological Province: McArthur Basin. Marine deposits with source rock potential for petroleum.||||||07-FEB-11
16319|Roper Group|63112|6|Mentioned|p1190|||Southern McArthur Basin.||||||
16319|Roper Group|63245|5|Briefly described|p8, p15|Mesoproterozoic|Mesoproterozoic|Includes the Velkerri Formation. Age: ~1.45Ga. Geological Province: McArthur Basin.||||||31-JAN-08
16319|Roper Group|63866|4|Described|p113, p115, p116, p123|Calymmian|Calymmian|McArthur basin. Crops out in the Northern Caledon Shelf.|ca 1429-1493 Ma (unit relationship)||Includes the Mainoru Formation and the McMinn Formation.|Unconformably overlies the Mount Rigg Group and the Nathan Group.|Fine- and coarse-grained siliciclastic rocks.|
16319|Roper Group|64443|6|Mentioned|p3|Calymmian|Calymmian|In the McArthur Basin, correlative of the South Nicholson Group.||||||
16319|Roper Group|64698|4|Described|lithinterp table|Ectasian|Calymmian|Age stated to be Statherian (1800-1600Ma) but given as ~1200-1500Ma. McArthur Basin. Max thick. 900m. Sequence of mudstone, sandstone, subordinate limestone and conglomerate.||||||07-JAN-09
16319|Roper Group|64724|5|Briefly described|p45 Fig.5, p46, 47,48|Calymmian|Calymmian|McArthur Basin. Deposited between ~1500-1430 Ma.||||||
16319|Roper Group|64784|6|Mentioned|p1-7     |Proterozoic|Proterozoic|Lanigan et al. (1994) estimated the age to be at least 1430 Ma. Beetaloo Basin. ~3000 mt hick.|>1430 Ma|||||
16319|Roper Group|64815|5|Briefly described|p3, p5-6, p11-13, p15 Fig.9  |Ectasian|Calymmian|See also p16-18 Figs.10-12, p19. Thickens westward. Rb-Sr dating of glauconite in the Roper Group gives a minimum age of 1390 Ma (McDougall et al, 1965). Diagenetic illite Rb-Sr age of 1429 +/- 31 Ma from the top of the Group (Kralik 1982) extends the depositional age.|Minimum age 1280 Ma (dyke).||Includes Mantungula, Mainoru, Crawford, Corcoran, Bessie Creek, McMinn Formations; Limmen, Abner Sandstones.|Unconformably overlies McArthur and Nathan Groups.|Mainly composed of quartz sandstone with micaceous siltstone.|
16319|Roper Group|64816|4|Described|p1-2, p4, p5, p16, p18, p20   |Mesoproterozoic|Mesoproterozoic|Contains widespread live oils and hydrocarbon shows. Contains hydrocarbon source and reservoir beds. Experienced multiple episodes of oil and brine migration involving hydrocarbons of different molecular compositions. Age constrained by radiometric dating of the Mainoru and McMinn Formations.|ca. 1430 Ma (Jackson et al.,1998)||Includes Limmen, Abner, Bessie Creek Sandstones; Mainoru, Crawford, Corcoran, Velkerri, McMinn, Chambers River Formations.|Unconformably overlies McArthur and Nathan Groups.|Five depositional cycles: quartz arenite, siltstone and shale; minor carbonate intervals and laminated shelf mudstone.|
16319|Roper Group|64817|6|Mentioned|p352 Fig.3, p353 Fig.4 ||||||Includes Maiwok Subgroup; Chambers River, Corcoran, Crawford, Mantungula and Mainoru Formations; Limmen, Bessie Creek and Abner Sandstones.|||
16319|Roper Group|64970|6|Mentioned|p726|Mesoproterozoic|Mesoproterozoic|Age: 1600-1000 Ma. Geological Province: McArthur Basin.||||||27-MAY-09
16319|Roper Group|64975|6|Mentioned|p162 Fig.6.|Mesoproterozoic|Mesoproterozoic||||Includes Mantungula, Limmen, Arnold, Hodgson, Bessie Creek Sandstones; Mainoru, Crawford, Corcoran, Velkerri, McMinn Formations; Jalboi and Munji Members.|||
16319|Roper Group|65228|4|Described|p7, p38, Figs.02, 28.|||McArthur Basin.|||Includes Mantungula, Mainoru, Crawford, Corcoran Formations; Limmen, Abner, Bessie Creek Sandstones; Maiwok Subgroup.|Unconformably overlies Nathan Group. Overlies ?unconformably the Lawn Supersequence.||
16319|Roper Group|65236|5|Briefly described|p1-3|Neoproterozoic|Mesoproterozoic|Comprises 14 named units. Geological province: Beetaloo Sub-basin. Unconformably overlain by relatively thin sheets of Cambrian volcanics.||||||04-JUN-09
16319|Roper Group|65337|5|Briefly described|p6, p8, p36.|||Roper Superbasin. 2 - 5 km thick. Correlated with South Nicholson Group. The tidal platform sandstone facies is very similar to the trough cross-bedded sandstone facies in No Mans Sandstone Member.|1492 +/- 4 Ma.||Includes McMinn Formation.|||
16319|Roper Group|65340|4|Described|p57, pp61-62, p84.|Mesoproterozoic|Mesoproterozoic|Youngest unit of McArthur Basin. Shallow-marine nearshore to shelf settings.|1500 - 1400 Ma.||Includes Mantungula, Mainoru and Crawford Formations, and Limmen and Abner Sandstones.|Unconformably overlies Karns Dolomite.|Cyclic, fine to medium glauconitic sandstone and mudstone.|
16319|Roper Group|65342|6|Mentioned|p9.||||||Includes Mantungula,  Mainoru, Corcoran and Kyalla Formations; and Limmen, Abner, Moroak and Jamieson Sandstones.|||
16319|Roper Group|65344|5|Briefly described|p13|Calymmian|Calymmian|McArthur Basin. Correlated with Renner Group, Tennant Creek region and South Nicholson Group, South Nicholson Basin.||||||03-MAY-12
16319|Roper Group|66843|5|Briefly described|p23-24, p30, p34, p39|||Youngest tectonic-stratigraphic package in the southern McArthur Basin. Tentative SHRIMP age.|c.1494 Ma.|||Unconformably overlies Nathan Group.|Clastic rocks.|
16319|Roper Group|67057|6|Mentioned|p463.|||McArthur Basin. Renewed subsidence and volcanism occurred at 1493 +/- 4 Ma (Abbott and Sweet 2000).||||||
16319|Roper Group|67144|5|Briefly described|Map legend.|Calymmian|Calymmian|McArthur Basin.|||Includes Limmen and Abner Sandstones; Mainoru and Crawford Formations.|Overlies Nathan Group.||13-APR-12
16319|Roper Group|67352|4|Described|v, p12, p13, p49, p51|Calymmian|Calymmian|McArthur Basin rocks. Thickens westward to maximum of c. 5 km in Beetaloo Sub-basin.|1500-1450 Ma||Abner Sandstone, Crawford Formation, Mainoru Formation, Limmen Sandstone.|Overlies Nathan Group (unconformably) or McArthur Group.|Marine siliciclastics: alternating quartz sandstone and micaceous siltstone units.|
16319|Roper Group|67564|6|Mentioned|p51, p59.|||||||||
16319|Roper Group|67779|5|Briefly described|p40, p48.|||Underwent only slight displacement along the Bulman Fault, suggesting it was a long-lived basement fault reactivated after deposition of the Kombolgie Subgroup.||||Is intruded by Derim Derim Dolerite.||
16319|Roper Group|68146|5|Briefly described|p2, p197-198|||This age is used as the currently accepted, tentative age of the South Nicholson Group. A minimum age of c.1324 Ma comes from intrusions.|c.1500-1400 Ma.||Mainoru Formation.|Correlated with the South Nicholson Group. Is intruded by Derim Derim Dolerite.||
16319|Roper Group|69003|5|Briefly described|p48 Fig.57|Mesoproterozoic|Mesoproterozoic|Included as a contributing unit to Australia's Apparent Polar Wander Path through the Proterozoic.|1324 Ma.|||||
16319|Roper Group|69018|5|Briefly described|p448, 449, 450, 459, 460, 461||Calymmian|Of Roper Superbasin, McArthur Basin. Eukaryotic-like fossils have been detected in the Roper Group.|~1430 Ma.|||||
16319|Roper Group|69417|6|Mentioned|p2:5|Calymmian|Calymmian|McArthur Basin.||||||12-JUL-16
16319|Roper Group|69418|6|Mentioned|p3:36|||McArthur Basin. Long-recognised as having petroleum potential, particularly in the Beetaloo Sub-basin.||||||12-JUL-16
16319|Roper Group|69429|6|Mentioned|p14:3 Fig.14.4, 14:4|Mesoproterozoic|Mesoproterozoic|McArthur Basin.||||||12-JUL-16
16319|Roper Group|69430|4|Described|p15:2-4, 22, 24-31, 34, 42, 61-63|Calymmian|Calymmian|McArthur Basin. The upper part (mudstone dominated) was named the Maiwok Subgroup by Dunn (1963); the (tidal-platform sandstones) units from the base to the top of the Hodgson Sandstone were named the Collara Subgroup by Abbott et al. (2001). Has an areal extent of 145,000 km2. Essentially flat-lying; usually 1500m thick (over 3000m in the S). Has petroleum potential.|1492-1429 Ma.||Collara, Maiwok Subgroups.|Unconformably overlies Mount Rigg Group and Nathan Group. Correlated with South Nicholson and Renner Groups.|An upward-coarsening six-cycle succession of mainly marine mudstone alternating with sandstone; minor pedogenic sedimentary breccia, fluvial sandstone, micritic and intraclastic limestone, and ooidal limestone. Post-deposition mafic sills and dykes.|12-JUL-16
16319|Roper Group|69431|6|Mentioned|p16:1, 18, 22|||||||Correlated with Renner Group. Is intruded by Derim Derim Dolerite.||12-JUL-16
16319|Roper Group|69434|5|Briefly described|p19:1, 4, 6|||McArthur Basin. Correlated with the South Nicholson Basin succession. Zircons from tuffaceous material: Jackson et al. (1999).|1492 +/- 4 Ma and 1493 +/- 4 Ma.|||Correlated with South Nicholson Group.||12-JUL-16
16319|Roper Group|69443|6|Mentioned|p28:12|Calymmian|Calymmian|||||Is overlain unconformably by Bukalara Sandstone.||12-JUL-16
16319|Roper Group|69446|5|Briefly described|p31:2|Mesoproterozoic|Mesoproterozoic|McArthur Basin.||||Is overlain unconformably by Tindall Limestone (Daly River Group).||12-JUL-16
16319|Roper Group|69451|6|Mentioned|p35:13||||||Velkerri Formation.|||12-JUL-16
16319|Roper Group|69455|6|Mentioned|p39:14|Proterozoic|Proterozoic|McArthur Basin. Contains organic-rich shale and is relatively unmetamorphosed, making for good potential source rocks underlying the Carpentaria Basin.||||||12-JUL-16
16319|Roper Group|69458|5|Briefly described|p42:21, 38|||McArthur Basin.|||Mainoru Formation.|Is intruded by Derim Derim Dolerite.|Sedimentary rocks.|12-JUL-16
16319|Roper Group|69545|6|Mentioned|p104|||McArthur Basin.|ca. 1400 Ma|||||
16319|Roper Group|69591|5|Briefly described|p53, p111|||Deformed c. 1424 Ma.||||Correlated with the South Nicholson Group.||
16319|Roper Group|69673|4|Described|p15, p20, p21, p32, p40, p46, p58|Mesoproterozoic|Mesoproterozoic|Petroleum occurences are within Beetaloo Sub-basin. Northwestern and Southern McArthur Basin. 1500 to >3km thick in Beetaloo Sub-basin.|||Includes Collara Subgroup, Maiwok Subgroup|Unconformably overlies Nathan Group, unconformably overlain by Jamison sandstone and Hayfield mudstone (informal names) correlated with South Nicholson Group, Renner Group|Mudstone alternating with sandstone; includes minor pedogenic sedimentary breccia, fluvial sandstone, micritic and intraclastic limestone and ooidal ironstone.|
16319|Roper Group|70380|5|Briefly described|p746|Mesoproterozoic|Mesoproterozoic|McArthur Basin.||||Is overlain unconformably by Tindall Limestone (Daly Basin).||
16319|Roper Group|70734|5|Briefly described|p13-17, p24-p25|Mesoproterozoic||McArthur Basin. Youngest and final episode of sedimentation in basin. Hosts microfossils which are briefly discussed.|||Includes Collara and Maiwok Subgroups|||10-JUL-18
16319|Roper Group|70822|5|Briefly described|p101-104, p106, p109, p112 |Mesoproterozoic|Mesoproterozoic|Greater McArthur Basin. Thickness varies laterally from 1 to >5 km. Depositional models discussed.|c.1.4 Ga.||Phelp, Limmen, Arnold, Hodgson, Bessie Creek, Moroak Sandstones; Mantungula, Mainoru, Crawford, Jalboi, Corcoran, Velkerri, Kyalla, Bukalorkmi, C[h]ambers River Formations; Sherwin Ironstone.|Unconformably overlies Nathan Group. Correlated with South Nicholson Group.||03-MAR-17
16319|Roper Group|70897|4|Described|p36-48, Fig.1.7.6,9|Mesoproterozoic|Mesoproterozoic|McArthur Basin and northern Lawn Hill Platform. Shows remarkable lateral consistency and continuity over 14 000 km2 of the NT. Thickens SW to c.5000m. High-energy, current-and wave-affected shallow-marine, and lower energy, inner to outer shelf, environments. Previous age determinations (c.1429 Ma to c.1280 Ma) described. The basal unconformity represents a break of 80-90 m.y., probably the period of regional deformation and erosion associated with the Isan Orogeny.|c.1490 Ma.||Limmen Sandstone; Mantungula, McMinn, Mainoru Formations; Sherwin Ironstone Member.|Roper Superbasin. Unconformably overlies McArthur and Nathan Groups. Broadly correlated with South Nicholson Group.|About 15 alternating Formations/Members of clean quartz sandstone and shale; internally concordant and conformable.|
16319|Roper Group|70968|3|Fully described|v-vi, p2-86, p88, p91-94, p115, p120|Ectasian|Calymmian|See also p123-135, p137-140, p143-144. McArthur Basin. Randal (1963), after Dunn (1963); all units defined by Abbott et al. (2001). Formerly mapped as Flying Fox Group (Ruker, 1959). Named after Roper River. Crops out as strike ridges, mesas and plateaux. Up to c.3000m thick. Part of the Wilton package. Lithologies are laterally continuous over vast areas. Six facies associations listed and described. The rarity of limestone is distinctive. Intruded by Derim Derim Dolerite dykes.|c.1500-1324 Ma.||Collara, Maiwok Subgroups.|Disconformably or unconformably overlies Nathan, Mount Rigg, McArthur, Wattie, Bullita and Limbunya Groups and Urapunga Granite. Correlated with Renner and Tijunna Groups. Underlies Kalkarindji Suite.|Siliciclastic succession: alternating mudrock-rich and cross-bedded sandstone Formations; minor calcareous siltstone, limestone, pedogenic breccia, conglomerate and oolitic ironstone.|24-FEB-17
16319|Roper Group|71059|4|Described|iii, p1-61|Mesoproterozoic|Mesoproterozoic|McArthur Basin. Of exploration interest for unconventional shale oil and gas. The restricted marine basin depositional environment has been likened to present-day Black Sea.|||Maiwok, Collara Subgroups.|Unconformably overlies Wattie, Bullita, McArthur, Mount Rigg and Nathan Groups.|A regionally-extensive, upward-coarsening cyclic succession of mainly marine mudrocks alternating with sandstones; minor pedogenic sedimentary breccia, fluvial sandstone, micritic and intraclastic limestone, and ooidal ironstone.|
16319|Roper Group|71169|6|Mentioned|p82|||McArthur Basin.||||||
16319|Roper Group|71369|6|Mentioned|p2, p4, p49||||< 1324 Ma.|||Correlated with South Nicholson Group.||20-FEB-18
16319|Roper Group|71374|5|Briefly described|iii, p1 tbl 1, p2, p18, p21-p22, p33|Mesoproterozoic|Mesoproterozoic|McArthur Basin.|||Includes the Chambers River Formation.|Broadly equivalent to the Tijunna Group and Renner Group. Overlies the McArthur Group.||
16319|Roper Group|71488|4|Described|p140-142, p147, p150-p153|Mesoproterozoic|Mesoproterozoic|McArthur Basin. Stratigraphically thickest in the Beetaloo Sub-basin. Deposited in a shallow-water dominantly marine environment. High organic content shales in the upper part of this group is of interest for unconventional petroleum.|||Includes the Maiwok and Collara Subgroups.|Unconformably overlies the Nathan Group.|Siliciclastic succession of alternating mudrock-rich and cross-bedded sandstone formations. The upper part of the group is rich in high organic carbon shales.|
16319|Roper Group|71494|6|Mentioned|p1-p2, p4||||||Includes the Limmen Sandstone, Mainoru Formation.|||03-MAY-18
16319|Roper Group|71606|5|Briefly described|p135,137-138|Calymmian|Calymmian|McArthur Basin. Arenite-lutite sequence. Represents a broad sag basin extending across most of the basin. Upper part of the group has Rb-Sr minimum age of 1430 Ma.|>1430 Ma (Rb-Sr)||Includes Malay Road Group, Wilberforce beds and Baralminar beds.|Underlain unconformably by Mount Rigg Group, Nathan Group and Karns Dolomite.||
16319|Roper Group|71632|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|McArthur Basin.||||||
16319|Roper Group|71779|3|Fully described|iii, p2, p5-p6, p23, 24, 25, 26|Mesoproterozoic|Mesoproterozoic|McArthur Basin. Exposed from Arnhem Bay in the north to Katherine in the west, to northern Wallhallow and to Robinson River in the south. The most extensive outrcrops occur in the Urapunga region. Outcrop is expressed as strike ridges, mesas and plateaux of sandstone, separated by valleys that are underlain by poorly exposed mudrock-rich units. Frogtech Geoscience estimates the maximum thickness to be between ca 4000-6000 m. Largely deposited in a restricted or partly restricted or anoxic, mostly marine depositional environment subject to fluctuating salinities.|||Includes the Maiwok Subgroup and Collara Subgroup.|Disconformably or unconformably overlies the Urapunga Granite, Nathan, McArthur and Mount Rigg Groups. Equivalent to the Tijunna Group. Intruded by the Derim Derim Dolerite.|Dominantly siliciclastic succession characterised by alternating mudrock-rich and cross-bedded sandstone formations. Minor lithologies include calcareous siltstone, limestone, pedogenic breccia, conglomerate and oolitic ironstone.|24-SEP-18
16319|Roper Group|71857|6|Mentioned|iii,|Mesoproterozoic|Mesoproterozoic|McArthur Basin.|||Include Velkerri, Kyalla Formations.|||04-FEB-19
16319|Roper Group|71893|4|Described|iii, p1-p4, p8-p11, p13, p15|Mesoproterozoic|Mesoproterozoic|McArthur Basin. See also  p19, p23-p24, p26-p27, p30, p34, p37, p39, p64.|||Includes the Collara and Maiwok subgroups.|Unconformably overlain by the Jamison sandstone and Hayfield mudstone.||
16319|Roper Group|72248|5|Briefly described|p146,148|||Of McArthur Basin.|||||Quartz sandstone and fine-grained clastics.|
16319|Roper Group|72297|6|Mentioned|p749|||McArthur Basin. Live oil was encountered in the upper unit of the Group.||||||
16319|Roper Group|72373|5|Briefly described|p2|Mesoproterozoic|Mesoproterozoic|Of McArthur Basin. Broadly equivalent to Wilton package, Tijunna Group (Birrindudu Basin) and Renner Group (Tomkinson Province).||||||01-OCT-19
16319|Roper Group|72381|5|Briefly described|p771-773,777,780|Mesoproterozoic|Mesoproterozoic|Of Beetaloo Sub-basin, McArthur Basin. Deposited on a stable shelf environment (enclosed marine basin; see p773 for references). Contains six upward-coarsening cyclic sequences and is divided into two subgroups. Combined U-Pb data from the Bessie Creek Sandstone (Altree-2 drillhole), to Velkerri Formation, Moroak Sandstone and Kyalla Formation show an up-section trend of decreasing 1600-1500 Ma sources replaced by 1800-1700 Ma sources, representing a gradual change from eastern sources to southern sources (e.g. Arunta region) for upper Roper Group in the Beetaloo Sub-basin, supported by hafnium isotopic data.|||Includes Maiwok and Collara subgroups.|Intruded by Derim Derim Dolerite.||
16319|Roper Group|72523|6|Mentioned|p1-2.|Mesoproterozoic|Mesoproterozoic|||||Unconformably overlies Nathan Group.||
16319|Roper Group|72526|5|Briefly described|p3, p8 Fig.1.3, p85-86.|Ectasian|Calymmian|Shown as located in the Urapunga Fault Zone, Beetaloo Sub-basin and northern part of the Batten Fault Zone. Age constraints based on tuffs in Mainoru Fm, lower Roper Group, and Derim Derim Dolerite, which intrudes both subgroups.|c. 1500 Ma to 1313 Ma||Maiwok Subgroup and Collara Subgroup|Shown as unconformably overlying Nathan Group. Intruded by Derim Derim Dolerite. South Nicholson Group inferred age to be equivalent to this Group. Overlain by Jamison sandstone and Hayfield mudstone.||
16319|Roper Group|72527|5|Briefly described|p10, p27, p41, p56, p65, p78.|Mesoproterozoic|Mesoproterozoic|Situated in the McArthur Basin. Age  range of c. 1500 - 1313 Ma, from Mainoru Formation tuffs (lower Roper Group) 1492+/-4 Ma  (Jackson et al., 1999, de Vries et al., 2008; Rawlings et al., 2008; Ahmad and Munson, 2013; Sweet, 2017) and intruded by Derim Derim Dolerite (1312.9+/-0.7 Ma) as dykes and sills.|c. 1500-1313 Ma||Includes Mainoru Formation, Collara Subgroup, Bukalorkmi Sandstone, Maiwok Subgroup.|Intruded by the Derim Derim Dolerite. Correlated with South Nicholson Group.|Includes tuffs.|
16319|Roper Group|72711|6|Mentioned|p1.|Calymmian|Calymmian|McArthur Basin.|c. 1500 Ma. to c. 1400 Ma.|||||
16319|Roper Group|72718|6|Mentioned|piii, p1-2, p5-7, p9, p12, p20|Mesoproterozoic|Mesoproterozoic|Beelatoo Sub-basin, McArthur Basin. Roper Superbasin, Wilton package. Uppermost portion of the group has noted potential for unconventional and conventional petroleum resources. Principally deposited within the Beetaloo Sub-basin. More constituents include the Bukalorkmi Sandstone, Kyalla Formation, Sherwin Formation, Moroak Sandstone, Velkerri Formation, Bessie Creek Sandstone, Corcoran Formation, Hodgson Sandstone, Jalboi Formation, Arnold Sandstone, Abner Sandstone, Crawford Formation, Mainoru Formation, Showell Member, Limmen Sandstone, Mantungula Formation, and Phelp Sandstone.|||Collara Subgroup, Maiwok Subgroup, and units therein including Kyalla Formation|Partly underlain by Walmudga Formation (Nathan Group), Upper Balbirni Dolostone, Dungaminnie Formation, and Karns Dolostone unconformably. Overlain by Derim Derim Dolerite.|Lithologies are predominantly marine mudrocks alternating with shoreline sandstone, but minor calcareous mudstone, fluvial sandstone and conglomerate have also been observed.|
16319|Roper Group|72912|4|Described|p5 Fig.3, p18-22, p36, p48.|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. Crawford and Mainoru Formation and Limmen Sandstone being located in the South part of the Batten Fault Zone and the Southeastern McArthur Basin.|||Includes Collara Subgroup, Maiwok Subgroup.|Intruded by the Derim Derim Dolerite.|Includes sandstone and shales.|15-MAR-21
16319|Roper Group|72919|6|Mentioned|p1, p32, p95|||McArthur Basin. Temporally correlated with South Nicholson Group.|||Hodgson Sandstone, Arnold Sandstone|||
16319|Roper Group|72967|6|Mentioned|p2|Mesoproterozoic|Mesoproterozoic|||||||
16319|Roper Group|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|Southern McArthur Basin, Roper Superbasin.|||Maiwok and Collara subgroups.|Unconformably underlain by Nathan Group. Overlain by Jamison Sandstone.||
16319|Roper Group|73083|6|Mentioned|p11, p40-41, p45, p47, p49|Mesoproterozoic|Mesoproterozoic|McArthur Basin.|||Collara Subgroup, Kyalla Formation|Overlain by the Bradshaw Complex and Wessel Group.|Siliciclastics.|
16319|Roper Group|73144|6|Mentioned|p13, p19|Ectasian|Calymmian|May be similar in age to the South Nicholson Group.|1500-1400 Ma|||||
16319|Roper Group|73242|5|Briefly described|p36-37, p39-40, p44, p46|Mesoproterozoic|Mesoproterozoic|McArthur Basin. Excellent potential for both unconventional and conventional petroleum.|||Collara Subgroup, Maiwok Subgroup and units therein|Intruded by Derim Derim Dolerite.||
16319|Roper Group|73280|6|Mentioned|piii|||||||||
16319|Roper Group|73288|6|Mentioned|p708|Paleoproterozoic|Paleoproterozoic|McArthur Basin, NT. One of the main unconventional hydrocarbon targets in the Basin.||||||
16319|Roper Group|73412|4|Described|p2-4, 6, 8-13, 15-19, 21|||Southern McArthur Basin. Deposition followed a 70 m.y. hiatus (related to the Isan Orogeny). Dry bulk density tabulated. Faults described. Low gravity response; magnetic response is high where volcanic units (dykes and sills) are preserved; non-conductive unit.|c.1500-1324 Ma.||Collara, Maiwok Subgroups; McMinn Formation.|Unconformably overlies Nathan Group and, locally, Tawallah Group. Lateral equivalent of South Nicholson Group.|Part of an extremely widespread deposition of laterally continuous siliciclastic succession.|
16356|Rosie Creek Sandstone Member|22538|6|Mentioned|Fig3 P709|||||||||
16356|Rosie Creek Sandstone Member|22853|4|Described|10|Proterozoic|Proterozoic|Geological province: McArthur Basin. Of the Sly Creek Sandstone. Max thickness 160 m.||||||28-NOV-06
16356|Rosie Creek Sandstone Member|23776|5|Briefly described|p705 Fig 2.|||Of Tawallah Group.||||||
16356|Rosie Creek Sandstone Member|23867|5|Briefly described|Fig. 30|||Of Sly Creek Sandstone (Tawallah Group).  Geological Province: McArthur Basin.||||||
16356|Rosie Creek Sandstone Member|24050|5|Briefly described|p16|||Of the Tawallah Group.  Geological Province: McArthur Basin.||||||28-NOV-06
16356|Rosie Creek Sandstone Member|42385|4|Described|p10, p8 Fig. 5, p9 Tb. 3|Mesoproterozoic|Mesoproterozoic|Of Sly Creek Sandstone.  Variation of Rosie Creek Formation? Max. thickness: 160m. Comprises a range of clastic lithologies including feldspathic, arkosic, ferruginous and glauconitic sandstones and thin siltstone and shale beds.||||||18-SEP-07
16356|Rosie Creek Sandstone Member|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.||Of Sly Creek Sandstone (Tawallah Group).||In schematic section, underlies Aquarium Formation; member at top of Sly Creek Sandstone.|Sandstone (including conglomeratic), siltstone and shale. Detailed lithology given.|11-NOV-11
16356|Rosie Creek Sandstone Member|42639|4|Described|p10 Table 4 p11|||Of Sly Creek Sandstone.||||||28-NOV-06
16356|Rosie Creek Sandstone Member|42700|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
16356|Rosie Creek Sandstone Member|42739|5|Briefly described|map legend|Statherian|Statherian|Of the Sly Creek Sandstone. Sandstone, very fine to very coarse grained and rarely conglomeratic; generally moderatly to poorly sorted, sometimes bimodally sorted.||||||19-OCT-05
16356|Rosie Creek Sandstone Member|42812|3|Fully described|p17, Table 3|||Of Sly Creek Sandstone.||||||28-NOV-06
16356|Rosie Creek Sandstone Member|43036|3|Fully described|p19|||Of the Sly Creek Sandstone.||||||28-NOV-06
16356|Rosie Creek Sandstone Member|60483|5|Briefly described|p7 Fig. 5|||Of Sly Creek Sandstone (Tawallah Group). Geological Province: McArthur Basin.||||||05-OCT-07
16356|Rosie Creek Sandstone Member|60558|5|Briefly described|p8 Fig. 6, p12|Proterozoic|Proterozoic|Of Sly Creek Sandstone.||||||03-JUN-09
16356|Rosie Creek Sandstone Member|64817|6|Mentioned|p353 Fig.4, p367 Tb.2 |||||Unit in Sly Creek Sandstone.||||
16356|Rosie Creek Sandstone Member|65228|5|Briefly described|Figs.02, 05, 07.|||Shown as Rosie Creek Sandstone (ie Formation rank implied) in Figs. 05 and 07.||Top of Sly Creek Sandstone.||Is overlain by Wununmantyala Sandstone.||08-JAN-18
16356|Rosie Creek Sandstone Member|65340|6|Mentioned|p12 Fig.6. |||||Unit in Sly Creek Sandstone.||||
16356|Rosie Creek Sandstone Member|69430|5|Briefly described|p15:3, 12|||Southern McArthur Basin. Correlated with upper part of Seigal Volcanics. With the parent unit, forms an up to 900m thick succession of shallow-marine sandstone. Mis-spelt as Rosi Creek Sandstone Member on 15:12.||Sly Creek Sandstone.||||12-JUL-16
16356|Rosie Creek Sandstone Member|69673|6|Mentioned|p16 fig 13, p17 fig 14|||Coarse clastic sedimentary rock.||Sly Creek Sandstone||Conformably overlain by McDermott Formation, overlies Seigal Volcanics||
16356|Rosie Creek Sandstone Member|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Urapunga Fault Zone, Beetaloo Sub-basin, Batten Fault Zone and Southeastern McArthur Basin.||[Sly Creek Sandstone,]Tawallah Group||Overlie Sly Creek Sandstone and underlies McDermott Formation.||
16356|Rosie Creek Sandstone Member|72718|6|Mentioned|p7|||Southern McArthur Basin.||McDermott Formation?, Tawallah Group||Partly underlain by Sly Creek Sandstone and Seigal Volcanics. Overlain by McDermott Formation.||
16356|Rosie Creek Sandstone Member|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Beetaloo Sub-basin and the Batten Fault Zone in the Southern McArthur Basin.||Tawallah Group||Overlies Sly Creek Sandstone and Seigal Volcanics and underlies McDermott Formation.||
16356|Rosie Creek Sandstone Member|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin, Leichhardt Superbasin. No parent formation is shown.||Tawallah Group||Partly underlain by Sly Creek Sandstone and Seigal Volcanics. Overlain by McDermott Formation.||
16439|Rum Jungle Complex|9324|5|Briefly described|Map Legend|Archean|Archean|Granite, gneiss, schist, metasediments.||||||07-NOV-08
16439|Rum Jungle Complex|9538|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Gneiss, granite, schist, metasediments.  Unconformably overlain by the Namoona Group.||||||07-NOV-08
16439|Rum Jungle Complex|9579|5|Briefly described|Map Sheet|Archean|Archean|||||||
16439|Rum Jungle Complex|22446|6|Mentioned|p19||Archean|||||||07-NOV-08
16439|Rum Jungle Complex|22479|5|Briefly described|fig1p2|Archean|Archean|Age: 2500Ma. Located in the Rum Jungle Region.||||||07-NOV-08
16439|Rum Jungle Complex|22810|5|Briefly described|P5, P9||Archean|||||||07-NOV-08
16439|Rum Jungle Complex|22813|5|Briefly described|Map|Archean|Archean|Granite, gneiss, schist.||||||07-NOV-08
16439|Rum Jungle Complex|23714|4|Described|p5|||||||||
16439|Rum Jungle Complex|23715|5|Briefly described|Map legend||Archean|||||||07-NOV-08
16439|Rum Jungle Complex|23733|5|Briefly described|p32 Fig. 19|||||||||
16439|Rum Jungle Complex|24047|5|Briefly described|p5 Fig.4|Archean|Archean|Granite, gneiss, schist.  Age: 2500Ma.  Geological Province: Pine Creek Orogen.||||||07-NOV-08
16439|Rum Jungle Complex|24442|5|Briefly described|p3, p30|Neoarchean|Neoarchean|An Archaean dome surrounded by Palaeoproterozoic metasediments and minor volcanics - comprises schist, granite gneiss, BIF and granite.  See also p42-44.||||||07-NOV-08
16439|Rum Jungle Complex|27449|14|Not recorded|?|||||||||
16439|Rum Jungle Complex|29552|6|Mentioned|p36|||||||||
16439|Rum Jungle Complex|30559|6|Mentioned|p283|||||||||
16439|Rum Jungle Complex|30838|6|Mentioned|p272|||||||||
16439|Rum Jungle Complex|31347|6|Mentioned|p135|||||||||
16439|Rum Jungle Complex|31824|6|Mentioned|p25|||See also P26.||||||
16439|Rum Jungle Complex|32397|6|Mentioned|p397|||2400my||||||
16439|Rum Jungle Complex|32659|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
16439|Rum Jungle Complex|32660|5|Briefly described|Table 2|||||||||
16439|Rum Jungle Complex|32819|6|Mentioned|p33|||||||||
16439|Rum Jungle Complex|32874|6|Mentioned|p179|||||||||
16439|Rum Jungle Complex|32875|6|Mentioned|p278|||||||||
16439|Rum Jungle Complex|33225|6|Mentioned|p20|||||||||
16439|Rum Jungle Complex|33278|4|Described|p167|||||||||
16439|Rum Jungle Complex|34287|6|Mentioned|p27|||See also P30||||||
16439|Rum Jungle Complex|35055|6|Mentioned|p222|||||||||
16439|Rum Jungle Complex|35061|6|Mentioned|p143|||||||||
16439|Rum Jungle Complex|35140|6|Mentioned|Fig.1|||||||||
16439|Rum Jungle Complex|35247|6|Mentioned|Fig.2|||||||||
16439|Rum Jungle Complex|35465|6|Mentioned|Fig.2|||Summary of positions of magnetic units in the Lower Proterozoic||||||
16439|Rum Jungle Complex|35495|6|Mentioned|p343|||||||||
16439|Rum Jungle Complex|35950|5|Briefly described|p299|||||||||
16439|Rum Jungle Complex|36473|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
16439|Rum Jungle Complex|37462|4|Described|p220|||See also Table 4.II||||||
16439|Rum Jungle Complex|37579|5|Briefly described|Regional setting map legend|Paleoproterozoic|Paleoproterozoic|Gneiss, granite, schist, metasediments.||||||07-NOV-08
16439|Rum Jungle Complex|38066|5|Briefly described|p50|||||||||
16439|Rum Jungle Complex|38239|6|Mentioned|Fig.2|||||||||
16439|Rum Jungle Complex|38557|6|Mentioned|p287|||||||||
16439|Rum Jungle Complex|38884|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
16439|Rum Jungle Complex|39069|6|Mentioned|Table 1|||||||||
16439|Rum Jungle Complex|39320|6|Mentioned|Fig.1|||||||||
16439|Rum Jungle Complex|39357|6|Mentioned|p3|||||||||
16439|Rum Jungle Complex|39518|6|Mentioned|p3|||||||||
16439|Rum Jungle Complex|39563|6|Mentioned|Map legend|Paleoproterozoic|Archean|Early Proterozoic to Archaean||||||07-NOV-08
16439|Rum Jungle Complex|39566|6|Mentioned|p49|||||||||
16439|Rum Jungle Complex|39679|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
16439|Rum Jungle Complex|39801|6|Mentioned|Map legend|Archean|Archean|Gneiss, granite, schist, metasediments.||||||07-NOV-08
16439|Rum Jungle Complex|39889|6|Mentioned|Fig.1|||||||||
16439|Rum Jungle Complex|40168|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Gneiss, granite, schist, metasediments.||||||07-NOV-08
16439|Rum Jungle Complex|40223|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Gneiss, granite, schist, metasediments.||||||07-NOV-08
16439|Rum Jungle Complex|40243|6|Mentioned|Fig.2|||||||||
16439|Rum Jungle Complex|40492|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
16439|Rum Jungle Complex|40493|6|Mentioned|Table 1|||||||||
16439|Rum Jungle Complex|40495|6|Mentioned|Fig.5|||||||||
16439|Rum Jungle Complex|40765|6|Mentioned|Fig.3|||||||||
16439|Rum Jungle Complex|40808|3|Fully described|p3|||||||||
16439|Rum Jungle Complex|40809|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
16439|Rum Jungle Complex|40823|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
16439|Rum Jungle Complex|41125|6|Mentioned|p24|||See also Fig.6||||||
16439|Rum Jungle Complex|41304|6|Mentioned|Map legend|Archean||||||||07-NOV-08
16439|Rum Jungle Complex|41305|3|Fully described|p3|||||||||
16439|Rum Jungle Complex|41309|6|Mentioned|p3|||||||||
16439|Rum Jungle Complex|41311|6|Mentioned|p5|||||||||
16439|Rum Jungle Complex|41397|6|Mentioned|p6|||||||||
16439|Rum Jungle Complex|41407|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
16439|Rum Jungle Complex|41465|6|Mentioned|p4|||||||||
16439|Rum Jungle Complex|41586|6|Mentioned|Map legend|||||||||
16439|Rum Jungle Complex|41645|6|Mentioned|Fig.5|||||||||
16439|Rum Jungle Complex|41661|6|Mentioned|Fig.3|||||||||
16439|Rum Jungle Complex|41663|4|Described|p3|||See also p7.||||||28-NOV-06
16439|Rum Jungle Complex|41980|6|Mentioned|Fig.2 P545|||||||||
16439|Rum Jungle Complex|42014|5|Briefly described|Map legend|Archean||||||||07-NOV-08
16439|Rum Jungle Complex|42202|6|Mentioned|p510|||||||||
16439|Rum Jungle Complex|43187|5|Briefly described|p2|||||||||
16439|Rum Jungle Complex|43561|6|Mentioned|p1434|||||||||
16439|Rum Jungle Complex|43595|5|Briefly described|p229|||||||||
16439|Rum Jungle Complex|43624|6|Mentioned|Table 1,p9||Archean|||||||07-NOV-08
16439|Rum Jungle Complex|43832|6|Mentioned|11||Archean|||||||07-NOV-08
16439|Rum Jungle Complex|44112|6|Mentioned|p7|||||||||
16439|Rum Jungle Complex|45022|3|Fully described|p.124.||Late Precambrian|On many pages.||||||28-NOV-06
16439|Rum Jungle Complex|45087|5|Briefly described|p13|||See also p214, 216, 221, 222. Chemical analyses.||||||28-NOV-06
16439|Rum Jungle Complex|45112|5|Briefly described|p50|||||||||
16439|Rum Jungle Complex|46658|6|Mentioned|Fig.4 P546|||||||||
16439|Rum Jungle Complex|46675|5|Briefly described|Map legend|Archean|Archean|Unconformably overlain by the Namoona Group.||||||07-NOV-08
16439|Rum Jungle Complex|46991|6|Mentioned|p245|||||||||
16439|Rum Jungle Complex|47049|6|Mentioned|Fig.2|||||||||
16439|Rum Jungle Complex|48866|2|Defined|p.1-9,Fig.1|||Granitic. Occupies core of eroded dome of metaseds, which are not intruded but granite rests unconf. on older rocks. 6 units in complex.||||||19-FEB-13
16439|Rum Jungle Complex|60526|5|Briefly described|Map Legend|Proterozoic|Archean|Gneiss, granite, schist, metasediments.||||||07-NOV-08
16439|Rum Jungle Complex|60575|5|Briefly described|Map legend|Archean|Archean|||||||07-NOV-08
16439|Rum Jungle Complex|60677|5|Briefly described|Map Legend|Archean|Archean|15 subdivisions shown. Mainly granites, with some gneiss, schist and diorite.||||||07-NOV-08
16439|Rum Jungle Complex|61056|6|Mentioned|p785|||||||||
16439|Rum Jungle Complex|61389|5|Briefly described|Map Legend|||Schists, gneiss, granite. Has been informally subdivided by geophysical characteristics.||||||
16439|Rum Jungle Complex|62375|5|Briefly described|p7, 8 Table 1, 10 Fig. 3|Archean|Archean|Granite, granodiorite, quartz-monzonite, quartz monzodiorite, rare tonalite and monzonite. Intrude earlier metasediments. Age: 2525-2535Ma. Geological Province: Pine Creek Orogen.||||||09-FEB-10
16439|Rum Jungle Complex|62378|5|Briefly described|p12|Paleoproterozoic|Paleoproterozoic|Age 2500Ma. Granite.||||||07-NOV-08
16439|Rum Jungle Complex|63866|4|Described|p108, p117|Neoarchean|Neoarchean|Central Domain, Pine Creek Orogen. Numeric ages are rough crystallisation ages.|c. 2425-2520|||Intercalated with the Stanley Metamorphics.|Granite and granite-gneisses.|
16439|Rum Jungle Complex|64329|6|Mentioned|p20|||Three throium prospects have been recognised - including the Crater prospect on the SE margin of the Rum Jungle Dome.||||||
16439|Rum Jungle Complex|64662|5|Briefly described|p44|Archean|Archean|Earliest phase of granite intrusion occurred at ~2.53Ga (Cross et al 2005a). Possible source of Archean detrital zircons in Ferdies Member, Dead Bullock Formation, Tanami region. Unconformably overlain by Beestons Formation.||||||07-FEB-11
16439|Rum Jungle Complex|64676|5|Briefly described|v, p1-18|Neoarchean|Neoarchean|Crops out c.60 km S of Darwin. Comprises two basement domes (Rum Jungle and Waterhouse), unconformably overlain by basal units of the Pine Creek Orogen. Six samples (each described in detail) gave SHRIMP U-Pb zircon ages in the range 2545 +/- 4 Ma to 2521 +/- 4 Ma.||||Is overlain unconformably by Beestons Formation.|Includes granites, typically porphyritic, non-foliated biotite granites, and diorite.|
16439|Rum Jungle Complex|64698|4|Described|lithinterp table||Neoarchean|Age 2525Ma SHRIMP U/Pb. I and S-type granitoids. Granite gneiss, banded gneiss; granite and granodiorite, various textural varieties with complex cross-cutting relationships. Includes Stanley Metamorphics.||||||07-JAN-09
16439|Rum Jungle Complex|64722|5|Briefly described|Fig. 2 p. 3-6, p7|Neoarchean|Neoarchean|Include granites and some metasedimentary rocks of the Pine Creek Orogen.||||||
16439|Rum Jungle Complex|64730|5|Briefly described|p124, 138, 139|Neoarchean|Neoarchean|Includes granites of 2545-2520 Ma SHRIMP zircon emplacement age, intercalated with minor metasedimentary rocks and iron-formations of Stanley Metamorphics.||||||
16439|Rum Jungle Complex|64731|6|Mentioned|p147|Neoarchean|Neoarchean|||||||12-APR-12
16439|Rum Jungle Complex|64956|6|Mentioned|p78, p90|||||||||07-FEB-11
16439|Rum Jungle Complex|65232|5|Briefly described|p6 Fig. 5, p5 Fig. 4, p2, p51-52|Archaean|Archaean|Granitic phases intrude Stanley Metamorphics. Underlies Manton Group (unconform). Fault bounded with lower Mount Partridge Group rocks. Age: 2500 Ma. With Waterhouse Complex: granite, gneiss, schist. Anomalously high avg U. Geol. Prov: Pine Creek Orogen.||||||09-FEB-10
16439|Rum Jungle Complex|65339|4|Described|p4, p5 Fig.4, p7, p6 Table 1.|Neoarchean|Neoarchean|Northwestern Pine Creek Orogen. Forms part of the granitic basement. Formerly Rum Jungle Granite (Malone 1962a, b); renamed and described by Fisher and Sullivan (1954); lately includes Waterhouse Complex (Ahmad et al. in prep.). Exposed as a faulted dome. The granitic rocks are anomalously high in uranium and thorium. Metamorphism reached amphibolite grade.|>2525 Ma.|||Intrudes Stanley Metamorphics.|Metasedimentary rocks and banded ironstone, schist and gneiss, granite-gneiss and migmatite, metadiorite, coarse to medium granite, large-feldspar granite, leucocratic granite.|
16439|Rum Jungle Complex|65455|6|Mentioned|p6 Fig. 3|Neoarchean|Neoarchean|Contains significant U enrichments.||||||09-MAY-12
16439|Rum Jungle Complex|66683|5|Briefly described|pp365-367, pp376-378.|Neoarchean|Neoarchean|Felsic crystalline basement exposed near Batchelor. Polymetallic mineralisation developed in overlying carbonaceous sedimentary rocks.|c.2545-c.2521 Ma.||||Weakly foliated to massive granite, leucogranite, and metadiorite; with enclaves of metasedimentary mica schist, feldspathic gneiss, and banded iron formation.|
16439|Rum Jungle Complex|67186|5|Briefly described|Map legend.|Neoarchean|Neoarchean||||||Large-feldspar granite, coarse granite, granite gneiss, leucocratic granite, schist, gneiss, porphyritic granite.|23-NOV-11
16439|Rum Jungle Complex|67232|5|Briefly described|p2. |Archean|Archean|Part of the basement to the Central Domain, Pine Creek Orogen.|2545 - 2521 Ma.|||||
16439|Rum Jungle Complex|67355|5|Briefly described|p1, p4, p10, p15-17, p25, p36, p69|Paleoproterozoic|Neoarchean|First defined by Rhodes (1965).|2400 Ma (Rb-Sr, U-Pb), 2538-2525 Ma (SHRIMP U-Pb)|||Unconformably underlies the Beestons Formation.|Includes granitic rocks, schist, gneiss and banded ironstone.|25-JAN-17
16439|Rum Jungle Complex|67479|6|Mentioned|p56|Archean|Archean|||||||
16439|Rum Jungle Complex|67564|5|Briefly described|p9 Fig.4.|Archean|Archean|Rum Jungle Region, Pine Creek Orogen.|2500 Ma.||||Granite, gneiss, schist.|
16439|Rum Jungle Complex|67779|5|Briefly described|p6 Fig.5, p14, p16, p66, p83, p117.|Archean|Archean|Central Domain, Pine Creek Orogen. Correlated with similar-aged Kukalak Gneiss and Nanambu Complex.|2545-2521 Ma (Cross et al. 2005).|||Is overlain unconformably by the Manton Group.||
16439|Rum Jungle Complex|68697|5|Briefly described|p46|Neoarchean|Neoarchean|Central Domain, Pine Creek Orogen. Probably related to Nanambu Complex and Kukalak Gneiss.|2545-2521 Ma.|||||
16439|Rum Jungle Complex|68998|6|Mentioned|p33|Neoarchean|Neoarchean|Pine Creek Orogen.||||||
16439|Rum Jungle Complex|69003|6|Mentioned|p2|||||||||
16439|Rum Jungle Complex|69031|6|Mentioned|p3|||North Australian Craton.||||||
16439|Rum Jungle Complex|69419|5|Briefly described|p4:1-6, 8|Neoarchean|Neoarchean|Rhodes (1965); included six units. Later, Lally (2002) expanded the Complex to fifteen units, incorporating the Waterhouse Complex of Johnson (1974). Pine Creek Orogen. Hosts vein quartz-hosted Au mineralisation at the Giants Reef prospect.|c.2535-2520 Ma.|||Is overlain nonconformably by Beestons Formation. Intrudes Stanley Metamorphics.|Granite gneiss, metadiorite, a wide variety of granite types intruded by pegmatites, dolerite and quartz tourmaline veins; metasedimentary schist, gneiss and banded ironstone. I- and S-types.|12-JUL-16
16439|Rum Jungle Complex|69420|5|Briefly described|p5:4,6,8, 11, 16, 29, 38, 64, 66, 75, 81|Neoarchean|Neoarchean|See also 85, 100, 105, 111, 115. Part of the basement to the Central Domain of the Pine Creek Orogen. SHRIMP zircon emplacement age.|2545-2520 Ma (Cross et al., 2005).||||Weakly deformed granitoids. Granite, gneiss and schist.|12-JUL-16
16439|Rum Jungle Complex|69537|6|Mentioned|p6|Archean|Archean|Pine Creek Orogen.|c.2545-2521 Ma.|||||
16439|Rum Jungle Complex|69554|6|Mentioned|p139|||Pine Creek Orogen.|2545-2520 Ma (Cross et al., 2005).|||||
16439|Rum Jungle Complex|69917|5|Briefly described|p22-24, 45, 47|Neoarchean|Neoarchean|Pine Creek Orogen, Central Domain. U/Pb SHRIMP zircon dating, Hf, O analytical data. Age interpretation uncertain. Crystallisation may have been at 2535+/-7 Ma, or this may be another inherited component. Metamorphic recrystallisation may be  ~2230-2055 Ma or younger.|||||Pinkish-brown, equigranular, non-foliated fine-grained granite.|
16439|Rum Jungle Complex|70866|5|Briefly described|Map legend.|Neoarchean|Neoarchean|Pine Creek Orogen. The Rum Jungle Dome (2525-2521 Ma) and the Waterhouse Dome (2545-2535 Ma) are mapped separately. The former comprises granitic gneiss, migmatite, metadiorite, granites, metasedimentary rocks and banded ironstone. The latter consists of granites, amphibolite, migmatite and metasedimentary rocks.||||Is overlain unconformably by Manton and Namoona Groups.||
16439|Rum Jungle Complex|71256|5|Briefly described|p17-p18, 20-23|Neoarchean|Neoarchean|Of Pine Creek Orogen. Discussion on low delta18 O values in zircon grains.|~2545-2521 Ma||Includes enclaves of amphibolite-facies Stanley Metamorphics.||Syenogranite, monzogranite, and quartz monzonite intruded by pegmatites, dolerite, and quartz tourmaline veins.|28-MAY-19
16439|Rum Jungle Complex|71349|5|Briefly described|p736-737|Archean|Archean|Pine Creek Orogen.|2545-2521 Ma.|||||
16439|Rum Jungle Complex|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|2525+/-5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Undeformed non-foliated granites: fine-grained equigranular; coarse-grained porphyritic biotite-rich; K-feldspar-phyric biotite; medium-grained pink non-porphyritic. Non-foliated medium-grained equigranular biotite diorite.|
16445|Rumbalara Shale|22566|5|Briefly described|p79|Mesozoic|Mesozoic|Of the Finke Group.||||||28-NOV-06
16445|Rumbalara Shale|22826|6|Mentioned|p576|Early Cretaceous|Early Cretaceous|Geological Province - Eromanga Basin.||||||
16445|Rumbalara Shale|23818|6|Mentioned|p141 Fig.65|||Geological Province: Great Artesian Basin.||||||
16445|Rumbalara Shale|33165|6|Mentioned|Chart|||Correlation chart only||||||
16445|Rumbalara Shale|33832|5|Briefly described|p11|||Correlation and strat.||||||28-NOV-06
16445|Rumbalara Shale|33844|6|Mentioned|Table 1|||||||||
16445|Rumbalara Shale|33939|6|Mentioned|p412|||Lithology.  L.Cret.||||||
16445|Rumbalara Shale|33971|5|Briefly described|p26|||||||||
16445|Rumbalara Shale|34111|5|Briefly described|Table 3|||Cretaceous. See also pp16,18,19.||||||28-NOV-06
16445|Rumbalara Shale|34580|4|Described|Table 1|||Lower Cretaceous||||||
16445|Rumbalara Shale|34611|6|Mentioned|Fig.65|||Correlation chart.||||||
16445|Rumbalara Shale|34971|6|Mentioned|p296|||||||||
16445|Rumbalara Shale|36751|6|Mentioned|p490|||||||||
16445|Rumbalara Shale|40926|6|Mentioned|p17|||||||||
16445|Rumbalara Shale|42504|5|Briefly described|p83|||||||||
16445|Rumbalara Shale|42940|6|Mentioned|p2|||||||||
16445|Rumbalara Shale|43035|6|Mentioned|p26|||||||||
16445|Rumbalara Shale|44222|14|Not recorded|p107|||||||||
16445|Rumbalara Shale|44323|14|Not recorded|map legend||Early Cretaceous|SG/53-6. L.Cretaceous.||||||
16445|Rumbalara Shale|44335|4|Described|p.13||Cretaceous|Tb.3. p.14. L.Cretaceous.||||||
16445|Rumbalara Shale|44336|14|Not recorded|map legend||Early Cretaceous|SG/53-3. L.Cretaceous.||||||
16445|Rumbalara Shale|44342|5|Briefly described|p.8 Table 8||Early Cretaceous|SG/53-5.. L.Cretaceous.||||||
16445|Rumbalara Shale|44343|14|Not recorded|map legend||Early Cretaceous|L.Cretaceous.||||||
16445|Rumbalara Shale|44393|4|Described|p.6,7,10,Tb.1,Fig.1||Aptian|||||||
16445|Rumbalara Shale|44394|14|Not recorded|map legend||Early Cretaceous|Lower Cretaceous.||||||
16445|Rumbalara Shale|44433|14|Not recorded|map legend||Cretaceous|||||||
16445|Rumbalara Shale|44946|14|Not recorded|Not recorded|||||||||
16445|Rumbalara Shale|45011|4|Described|p9-13,15|||Same age as Roma and Lower Wilgunya Formations.||||||
16445|Rumbalara Shale|45041|4|Described|p114|||L. Cret.||||||
16445|Rumbalara Shale|46740|14|Not recorded|p.187||Cretaceous|||||||
16445|Rumbalara Shale|48639|14|Not recorded|opp.p.1,map||Cretaceous|Cret.||||||
16445|Rumbalara Shale|48865|2|Defined|p.39||Early Cretaceous|Many figures. Fig.4,37,38,41,Fig.13,51,53,Pl.6,10,11. Lower Cretaceous. (G53-3,6).||||||
16445|Rumbalara Shale|48880|14|Not recorded|p.17,20,Pl.13||Early Cretaceous|L.Cret.(G53-3).||||||
16445|Rumbalara Shale|48890|2|Defined|p.56||Early Carboniferous|See also Tb.2,3,Fig.4,p.26,27. Pl.10. Lower Carboniferous.||||||
16445|Rumbalara Shale|48963|6|Mentioned|Plate 5|||||||||
16445|Rumbalara Shale|50372|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Geological Province: Eromanga Basin. Very fine grained siltstone, commonly silicified to porcellanite.||||||
16445|Rumbalara Shale|61155|5|Briefly described|p16|||Age is pre-Cainozoic. Geological Province: East Amadeus Basin.||||||
16445|Rumbalara Shale|62609|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Siltstone, porcellanite, some sandstone. Overlies: De Souza Sandstone.||||||14-AUG-06
16445|Rumbalara Shale|62620|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Siltstone, porcellanite, some sandstone.||||||
16445|Rumbalara Shale|65309|6|Mentioned|p14.|||Probable correlative of Bulldog Shale in South Australia.||||Overlies Algebuckina Sandstone.||
16445|Rumbalara Shale|65342|6|Mentioned|p10.|||Pedirka Basin. Max. thickness at least 407 m.  Seen as having potential as an insulating layer for geothermal energy.||||Overlies Cadna-owie Formation.||
16445|Rumbalara Shale|68734|6|Mentioned|p221 Fig.3|Cretaceous|Cretaceous|||||||
16445|Rumbalara Shale|69457|5|Briefly described|p41:3-4, 8, 10, 14-15|Early Cretaceous|Early Cretaceous|Wells (1969). Described as a "local" name in the western Eromanga Basin (NT) for fine-grained exposures at a similar stratigraphic level that, in the FINKE map area, were later assigned to the Bulldog Shale? by Edgoose et al. (2002). They are here referred to as unassigned Wilgunya Subgroup, or as Bulldog Shale/Wallumbilla Formation, and the unit's name appears to be obsolete. c.275m thick. Hosts the Rumbalara Ochre Mine, mined between 1939 and 1951 for paint pigment.||||Disconformably/unconformably overlay De Souza Sandstone.||12-JUL-16
16445|Rumbalara Shale|69458|6|Mentioned|p42:16|||Eromanga Basin. Some rocks of the Wilgunya Subgroup in HALE RIVER, McDILLS map areas are mapped under this name.||||||12-JUL-16
16445|Rumbalara Shale|71321|6|Mentioned|p27|||||||Equivalent to Bulldog Shale.||
16445|Rumbalara Shale|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (NT).||||Overlies DeSouza Sandstone. Is overlain by Winton FZ.||
16445|Rumbalara Shale|73281|6|Mentioned|Appendix (DIP)|||See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
16493|Sadadeen Range Gneiss|9199|5|Briefly described|Map legend|Precambrian|Precambrian|Of the Hayes Complex.  Biotite-quartz-feldspar augen gneiss.  Geological Province: Arunta Block.||||||03-NOV-04
16493|Sadadeen Range Gneiss|41665|4|Described|p9|||||||||
16493|Sadadeen Range Gneiss|41816|4|Described|p7|||||||||
16493|Sadadeen Range Gneiss|50369|6|Mentioned|p26.4|||||||||
16493|Sadadeen Range Gneiss|60547|5|Briefly described|Map Legend|Precambrian|Precambrian|Of the Hayes Complex. Geological Province: Arunta Block. Biotite-quartz-feldspar augen gneiss.||||||
16494|Saddle Creek Formation|14019|5|Briefly described|p4 Fig. 3|||Of the Auvergne Group.  Geological Province: Victoria Basin.||||||
16494|Saddle Creek Formation|23937|6|Mentioned|p78 App. 1|||Of the Auvergne Group.||||||
16494|Saddle Creek Formation|24122|3|Fully described|p10, p5 Tb.1|Proterozoic|Proterozoic|Of Auvergne Group.  Conformably overlies Angalarri Siltstone, conformably overlain by Pinkerton Formation.  Maximum thickness 50m.  Geological Province: Victoria Basin.||||||
16494|Saddle Creek Formation|24297|5|Briefly described|p4 Fig.3|||Of Auvergne Group.  Geological Province: Victoria Basin.||||||
16494|Saddle Creek Formation|24300|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Parent: Auvergne Group.   Geological Province: Victoria Basin||||||
16494|Saddle Creek Formation|24441|5|Briefly described|p1 Fig. 1|Mesoproterozoic|Mesoproterozoic|Of the Auvergne Group. Overlies Angalarri Siltstone;  overlain by Pinkerton Sandstone. Geological Province: Victoria Basin.||||||
16494|Saddle Creek Formation|24442|5|Briefly described|p50 Fig. 1|||Of the Auvergne Group.  Geological Province: Victoria Basin.||||||
16494|Saddle Creek Formation|28255|5|Briefly described|p67, Tb. 11 (opp. p8)|Adelaidean|Adelaidean|Of the Auvergne Group. Consists of oolitic dolomite with minor sandstone and siltstone. Max. thickness: >150m. See also p68 Tb. 6.||||||
16494|Saddle Creek Formation|32170|6|Mentioned|Map legend|Adelaidean|Carpentarian|Adelaidean or Carpentarian||||||
16494|Saddle Creek Formation|32307|4|Described|Table 2|||Proterozoic||||||
16494|Saddle Creek Formation|32310|6|Mentioned|Map legend|Adelaidean|Carpentarian|Adelaidean/Carpentarian||||||
16494|Saddle Creek Formation|32660|5|Briefly described|Table 6|||||||||
16494|Saddle Creek Formation|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Auvergne Group.  Basal crossbedded sandstone; upper siltstone and oolitic dolomite.||||||02-DEC-04
16494|Saddle Creek Formation|32700|4|Described|Table 1|||Previously mapped as Yambarra Beds (Randal, 1962).||||||29-NOV-06
16494|Saddle Creek Formation|32701|4|Described|Table 1|||Adelaidean. Of the Auvergne Group.||||||29-NOV-06
16494|Saddle Creek Formation|32728|6|Mentioned|Fig.14|||||||||
16494|Saddle Creek Formation|32775|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Auvergne Group.  Basal crossbedded sandstone, overlain by siltstone with minor shale and dolomite.||||||02-DEC-04
16494|Saddle Creek Formation|33373|3|Fully described|p10|||p10.||||||29-NOV-06
16494|Saddle Creek Formation|33375|6|Mentioned|p11 Tb. 1, p13|Adelaidean|Adelaidean|Of the Auvergne Group. Blocky white quartz sandstone overlain by brown oolitic dolomite. Conformable on Angalarri Siltstone.  Max. thickness: ~50m.||||||26-APR-05
16494|Saddle Creek Formation|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
16494|Saddle Creek Formation|33378|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Auvergne Group. Basal blocky quartz sandstone, brown oolitic dolomite.||||||27-APR-05
16494|Saddle Creek Formation|39827|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
16494|Saddle Creek Formation|40494|4|Described|p11|||||||||
16494|Saddle Creek Formation|41660|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of Auvergne Group. Quartz arenite, flaggy to thickly bedded, with large scale cross-bedding, ripple marks and slump structures (up to at least 210m).||||||07-OCT-05
16494|Saddle Creek Formation|41661|5|Briefly described|Table 1|||||||||
16494|Saddle Creek Formation|45112|4|Described|Table 15|||||||||
16494|Saddle Creek Formation|48938|2|Defined|p40|Adelaidean|Adelaidean|||||||
16494|Saddle Creek Formation|48942|3|Fully described|p68|||||||||
16494|Saddle Creek Formation|48943|4|Described|p76|||||||||
16494|Saddle Creek Formation|60006|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Victoria Basin. Of Auvergne Group. Overlies Angalarri Siltstone. Overlain by Pinkerton Sandstone. Basal sandstone, upper siltstone, minor oolitic dolostone and dolarenite||||||21-JUL-04
16494|Saddle Creek Formation|60682|4|Described|p8, 9 Table 2|Cryogenian|Cryogenian|Of Auvergne Group. Conformably overlies Angalarri Siltstone. Conformably overlain by Pinkerton Formation. Max. thickness: >222m. Basal sandstone, upper siltstone and minor oolitic dolostone and dolarenite. Geological Province: Victoria Basin.||||||11-MAY-05
16494|Saddle Creek Formation|60685|5|Briefly described|p4 Fig. 3|Mesoproterozoic|Mesoproterozoic|Of the Auvergne Group. Geological Province: Victoria Basin.||||||
16494|Saddle Creek Formation|65331|5|Briefly described|Map legend|Neoproterozoic |Neoproterozoic|Of Auvergne Group, Victoria Basin. Basal sandstone, upper siltstone, minor dolostone and dolarenite||||||
16494|Saddle Creek Formation|65342|6|Mentioned|p11 Fig.13. |||Victoria Basin.||Unit in Auvergne Group.||Overlies Angalarri Siltstone. Is overlain by Pinkerton Sandstone.||
16494|Saddle Creek Formation|67151|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Victoria Basin.||Unit in Auvergne Group.||Overlies Angalarri Siltstone. Is overlain by Pinkerton Sandstone.|Basal quartz sandstone, brown oolitic dolostone, dolomitic sandstone and upper siltstone.|
16494|Saddle Creek Formation|67167|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|||Unit in Auvergne Group.|||Basal sandstone, upper siltstone, minor ooidal dolostone and dolarenite.|
16494|Saddle Creek Formation|68733|5|Briefly described|p177 Fig.2, p179, p185, p189 Fig.8, p192|Cryogenian|Cryogenian|Victoria Basin. Sm-Nd isotope data tabulated. Appears as Saddle Creek Sst in Fig.8.||Of the Auvergne Group.||||06-DEC-17
16494|Saddle Creek Formation|69418|6|Mentioned|p3:31|||Victoria Basin. Hosts barite at the Saddle Creek deposit (briefly described).||||||12-JUL-16
16494|Saddle Creek Formation|69437|5|Briefly described|p22:4-5|Cryogenian|Cryogenian|Victoria/Wolfe Basins, Centralian A Superbasin. Supersequence 1.||||Overlies Angalarri Siltstone. Is overlain by Pinkerton Sandstone.||12-JUL-16
16494|Saddle Creek Formation|69441|5|Briefly described|p26:2-6|Neoproterozoic|Neoproterozoic|Typically <160m thick; over 222m locally. Very shallow to emergent, high-energy clastic phases with brine-logging, ooid shoals; argillaceous phases are slightly deeper water. Pods and veins of barite occur, but no commercial exploitation has been reported.||Auvergne Group.||Conformably (locally unconformably) overlies Angalarri Siltstone. Is overlain conformably by Pinkerton Sandstone.|Basal sandstone less than 10m thick; overlain by siltstone, oolitic dolostone, silica-cemented quartz sandstone, dolarenite and minor shale. Numerous sedimentary structures.|12-JUL-16
16494|Saddle Creek Formation|69442|5|Briefly described|p27:2-5|||||Auvergne Group.||Is overlain unconformably by Uniya Formation and Skinner Sandstone. Is onlapped unconformably by Beasly Knob Member (Ranford Formation).||12-JUL-16
16494|Saddle Creek Formation|69673|5|Briefly described|p188|||222m thick.||Auvergne Group|||Basal sandstone overlain by siltstone, oolitic dolostone, silica cemented quartz sandstone, dolarenite and minor shale.|
16494|Saddle Creek Formation|70206|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Victoria Basin.||Auvergne Group|||Basal sandstone, upper siltstone, minor oolitic dolostone and dolarenite.|
16494|Saddle Creek Formation|70655|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Victoria Basin.||Auvergne Group||Overlies Angalarri Siltstone. Is overlain by Pinkerton Sandstone, Moonlight Valley Tillite, Kinevans Sandstone, Antrim Plateau Volcanics.|Basal quartz sandstone, brown oolitic dolostone, dolomitic sandstone and upper siltstone.|
16494|Saddle Creek Formation|70850|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Victoria Basin.||Auvergne Group.||Conformably overlies Angalarri Siltstone. Is overlain conformably by Pinkerton Sandstone.|Basal sandstone, upper siltstone, minor oolitic dolostone and dolarenite.|
16494|Saddle Creek Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
16494|Saddle Creek Formation|71302|4|Described|p1,6-7,50-57,72,74|Neoproterozoic|Neoproterozoic|Of Victoria Basin. Typically less than 160m thick, but reaches 222m maximum thickness in AUVERGNE 1:250 000 map sheet (Dunster et al., 2000). probably deposited in very shallow to emergent conditions, with high energy clastic phases and slightly deeper stable conditions (Dunster et al., 2000; Cutovinos et al., 2002). Sample GA 1957133 (quartz sandstone) yielded an interpreted (weighted mean 238U/206Pb) maximum depositional age of 1049+\-20 Ma. Dominated by detritus in the range 1550-1650 Ma, and have very little pre-1800 Ma zircon.||Unit of Auvergne Group.||Overlain by Pinkerton Sandstone. nderlain conformably, to locally unconformably by Angallari Siltstone.|Basal sandstone overlain by siltstone, oolitic dolostone, silica-cemented quartz sandstone, dolarenite and minor shale.|
16494|Saddle Creek Formation|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|1053+/-14 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
16494|Saddle Creek Formation|73083|6|Mentioned|p7||||||||Siltstone, shale, minor dolostone, sandstone, and dolarenite.|
16515|Sahul Group|5952|5|Briefly described|p215|Triassic|Triassic|Includes Mount Goodwin, Osprey, Pollard, Challis and Nome Formations. Geological Province: Bonaparte Basin.||||||01-MAR-10
16515|Sahul Group|13194|4|Described|p386 Tb. 4-16, p396 fig 4-60|Rhaetian|Triassic|~2200m thick.||||Overlies Kinmore Group; equivalent to Cape Londonderry Formation and units of Troughton Group.|Interbedded sandstone, limestone, dolomite and shale; minor coal, evaporite and volcanics.|
16515|Sahul Group|13222|6|Mentioned|p229 Fig.2.||||||Includes Benalla, Osprey, Pollard, Challis and Nome Formations.|||
16515|Sahul Group|13224|6|Mentioned|p485 fig 3|Rhaetian|Anisian|||||||
16515|Sahul Group|13354|6|Mentioned|p375 Fig.6.|Triassic|Late Permian|Comprises, in ascending order, Mount Goodwin, Osprey, Pollard, Challis and Nome Formations.||91||||28-OCT-14
16515|Sahul Group|22663|5|Briefly described|W97 -1-7 p3||Triassic|||||||01-MAR-10
16515|Sahul Group|23377|6|Mentioned|p211|||In the Vulcan Sub-basin.||||||29-NOV-06
16515|Sahul Group|23378|4|Described|p180 Fig.2|Late Triassic|Early Permian|In the Vulcan Sub-basin.||||||01-MAR-10
16515|Sahul Group|41532|3|Fully described|p301|||||||||
16515|Sahul Group|41690|5|Briefly described|p3|||||||||
16515|Sahul Group|41716|6|Mentioned|p334|||||||||
16515|Sahul Group|41759|6|Mentioned|p270|||||||||
16515|Sahul Group|42034|4|Described|Fig.4 P11|||||||||
16515|Sahul Group|42053|5|Briefly described|Fig.15 P46|||||||||01-MAR-10
16515|Sahul Group|42057|6|Mentioned|Fig.3 P70|||||||||
16515|Sahul Group|42066|5|Briefly described|Fig.3 P199|||||||||
16515|Sahul Group|42075|5|Briefly described|Fig.4 P245|||||||||
16515|Sahul Group|42442|3|Fully described|p21|||Occurs in NT and WA.||||||29-NOV-06
16515|Sahul Group|42861|5|Briefly described|p3|||||||||
16515|Sahul Group|43699|6|Mentioned|Fig.6,p10||Middle Triassic|||||||
16515|Sahul Group|43707|5|Briefly described|Fig.3,p4||Triassic|||||||
16515|Sahul Group|49637|5|Briefly described|Fig. 3|Late Triassic|Middle Triassic|Geological Province: Vulcan Sub-basin.||||||07-FEB-11
16515|Sahul Group|60386|6|Mentioned|p300|Late Triassic|Early Triassic|Browse Basin/Bonaparte Basin. Non-marine, deltaic-nearshore-shelf, limestone nearshore-shelf.||||||
16515|Sahul Group|60634|6|Mentioned|p1168 Fig.3. |Triassic|Triassic||||Includes Mount Goodwin, Osprey, Pollard, Challis and Nome Formations.|Overlies Kinmore Group. Is overlain by Troughton Group.||
16515|Sahul Group|61550|6|Mentioned|p495 Fig.2. |Rhaetian|Nammalian||||Includes the Nome, Challis, Pollard and Osprey Formations.|Overlies Mount Goodwin Formation. Is overlain by Plover Formation.||
16515|Sahul Group|62837|5|Briefly described|Stratigraphic columns|Early Jurassic|Early Triassic|Includes the Pollard, Benella (possibly misspelt and should be Benalla?), Osprey, Challis and Nome Formations.  Age: 245-~203Ma. Geological Province:  Western Bonaparte Basin.||||||01-MAR-10
16515|Sahul Group|66187|5|Briefly described|p413 Fig.2|Norian|Early Triassic|Mount Ashmore Dome, Bonaparte Basin. Includes the Nome, Challis, Pollard and Osprey Formations.||||||
16515|Sahul Group|68223|6|Mentioned|p179 Fig.4||Permian|||||||
16515|Sahul Group|69297|6|Mentioned|p305, p322|Rhaetian|Anisian|Caswell, Barcoo and Seringapatam Sub-basins of the Browse Basin.|||Includes the Osprey Formation, Pollard Formation, Challis Formation and the Nome Formation.|Overlies the Kinmore Group. Overlain by the Troughton Group.||
16515|Sahul Group|69452|5|Briefly described|p36:15|Triassic|Triassic|Bonaparte Basin.|||Nome, Osprey, Challis, Benalla, Pollard Formations.|Overlies Mount Goodwin Subgroup (Kinmore Group). Is overlain by Plover Formation (Troughton Group).||12-JUL-16
16515|Sahul Group|70061|5|Briefly described|Regional geology; Figs.6-7. Vulcan:Fig.2|Rhaetian|Anisian||||Benalla, Osprey, Pollard, Challis and Nome Formations.|Overlies Kinmore Group. Is overlain by Troughton Group.||12-JUL-16
16515|Sahul Group|70064|5|Briefly described|Regional Fig. 6. Central: Fig.2|Rhaetian|Carnian|See also Northern: Fig.2. Yampi: Fig.2. Browse Basin.|||Osprey, Pollard, Challis and Nome Formations.|Overlies Kinmore Group. Is overlain by Troughton Group.||12-JUL-16
16515|Sahul Group|71146|5|Briefly described|p6|Middle Triassic|Middle Triassic|Bonaparte Basin.||||Overlies the Osprey Formation.|Sandstone.|
16619|Santo Sandstone|22826|6|Mentioned|Fig 2 on p565|Devonian|Devonian|||||||
16619|Santo Sandstone|29591|5|Briefly described|Table 23|||||||||
16619|Santo Sandstone|31566|6|Mentioned|p244|||||||||
16619|Santo Sandstone|31567|5|Briefly described|p274|||Refers Wells et al. (1967). Of the Finke Group.||||||29-NOV-06
16619|Santo Sandstone|34111|5|Briefly described|Table 2|||Devonian - Carboniferous. See also pp6,16.||||||29-NOV-06
16619|Santo Sandstone|42504|6|Mentioned|p100|||||||||
16619|Santo Sandstone|44393|6|Mentioned|Fig.1|||Dev-Carb. Equivalent to Idracowra Sandstone of the Finke Group.||||||29-NOV-06
16619|Santo Sandstone|44433|14|Not recorded|map legend|||Devonian to Carboniferous.||||||
16619|Santo Sandstone|45041|4|Described|p105,103|||||||||27-OCT-06
16619|Santo Sandstone|48890|2|Defined|p.50,52,58|Carboniferous|Devonian|Tb.2, Fig.4, Pl.8,9. Devonian to Carboniferous. Defn. on Tech.File F/53-15.||||||
16619|Santo Sandstone|69438|6|Mentioned|p23:41|||Wells et al. (1967). Previously considered a lateral equivalent of Idracowra Sandstone although not included in the Finke Group (Jones, 1972). The rocks have been assigned to the Idracowra Sandstone and the name has been abandoned.||||||12-JUL-16
16670|Schaber Hornblende Granite|34579|4|Described|Table 1|||||||||
16670|Schaber Hornblende Granite|44964|14|Not recorded|p.43|||||||||
16670|Schaber Hornblende Granite|45041|6|Mentioned|Fig.5|||Precambrian||||||
16670|Schaber Hornblende Granite|48880|4|Described|p.12||Precambrian|p.10,Pl.11. (F53-14)||||||
16675|Scinto Breccia|23384|6|Mentioned|Fig 27|||Of Needham and Stuart-Smith (1985).||||||
16675|Scinto Breccia|23867|5|Briefly described|Fig. 3|||Of El Sherana Group.  Formerly Scinto Breccia Member (Edith River Volcanics).  Geological Province: McArthur Basin.||||||
16675|Scinto Breccia|29599|6|Mentioned|Fig.2|||||||||
16675|Scinto Breccia|34528|6|Mentioned|p18|||Upper Proterozoic. See also P19.||||||
16675|Scinto Breccia|40248|4|Described|p222|||||||||
16675|Scinto Breccia|40861|6|Mentioned|p122|||||||||
16675|Scinto Breccia|41397|4|Described|p13|||||||||
16675|Scinto Breccia|41407|6|Mentioned|Map legend|Proterozoic||||||||
16675|Scinto Breccia|41594|6|Mentioned|Fig.8|||||||||
16675|Scinto Breccia|43187|5|Briefly described|p2|||||||||
16675|Scinto Breccia|43718|6|Mentioned|p4|||||||||
16675|Scinto Breccia|43720|6|Mentioned|Appendix,p6|||||||||
16675|Scinto Breccia|46658|5|Briefly described|p556|||||||||
16675|Scinto Breccia|47049|6|Mentioned|p237|||||||||
16675|Scinto Breccia|60680|5|Briefly described|Map legend|Orosirian|Orosirian|Of the El Sherana Group (Jim Jim Suite). Quartz-haematite polymictic pebble breccia, commonly phosphatic; minor haematitic sandstone.||||||14-JAN-05
16675|Scinto Breccia|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1829-1845Ma. Of El Sherana Group.  Max thickness 100m. Pinkish-brown, quartz-haematite polymictic pebble breccia, commonly phosphatic; minor haematitc sandstone. Lenses at base of Coronation Sandstone.||||||
16675|Scinto Breccia|65232|6|Mentioned|p50, p49 Fig. 32, App. 2|||Haematitic breccia.||||||09-FEB-10
16675|Scinto Breccia|67564|3|Fully described|p7 Table 2, pp25-26.|Paleoproterozoic|Paleoproterozoic|Jawoyn Sub-basin. Irregular distribution; discontinuous outcrops of strike ridges and rubbly hills. 100 m thick subaerial talus deposits. Formerly (Walpole et al. 1960) the Scinto Breccia Member. Commonly contains elevated levels of Th, U, Cu, Ni, As and locally Au. Hosts secondary uranium mineralisation.||Unit in El Sherana Group.||Unconformably overlies Koolpin Formation and Mount Bonnie Formation. Is overlain conformably by Coronation Sandstone.|Pinkish-brown, quartz-hematite polymictic pebble breccia, commonly phosphatic;  minor hematitic sandstone.|
16675|Scinto Breccia|69420|5|Briefly described|p5:7, 15, 80, 116|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen. South Alligator region. c.100m thick. Subaerial talus. Hosts phosphate rock deposits.||Basal El Sherana Group.||Is interbedded with Coronation Sandstone.|Pink-brown, quartz-haematite, polymictic pebble breccia, commonly phosphatic; minor haematitic sandstone.|12-JUL-16
16675|Scinto Breccia|70293|6|Mentioned|p598|Orosirian|Orosirian|Jawoyn Sub-basin.||El Sherana Group||||
16698|Scrutton Volcanics|22479|5|Briefly described|fig4, pg10|Orosirian|Orosirian|||||||
16698|Scrutton Volcanics|22644|5|Briefly described|5 fig 2|||Geological province: McArthur Basin. Overlain by Yiyinti (Formation) - name presented only as Yiyinti in figure. Also spelt as Yinintyi Sandstone in text (p5).||||||29-NOV-06
16698|Scrutton Volcanics|22662|6|Mentioned|23 fig 2|||Geological province: McArthur Basin.||||||29-NOV-06
16698|Scrutton Volcanics|22670|6|Mentioned|56,58,59|||Geological province: McArthur Basin.||||||29-NOV-06
16698|Scrutton Volcanics|23115|5|Briefly described|p461||Proterozoic|Age: Early Proterozoic.||||||
16698|Scrutton Volcanics|23363|5|Briefly described|344 Fig.3|Orosirian|Orosirian|Age: ~1851Ma.||||||29-NOV-06
16698|Scrutton Volcanics|23395|6|Mentioned|p388|||||||||
16698|Scrutton Volcanics|23398|5|Briefly described|p434|Orosirian|Orosirian|Age: 1851+/-7Ma.||||||29-NOV-06
16698|Scrutton Volcanics|23733|5|Briefly described|p32 Fig. 19|||Age: 1851Ma.||||||
16698|Scrutton Volcanics|23910|5|Briefly described|p292 Fig. 3|||Geological Province: McArthur Basin.||||||
16698|Scrutton Volcanics|23937|6|Mentioned|p88 App. 1|||Geological Province: McArthur Basin.||||||03-NOV-04
16698|Scrutton Volcanics|23963|6|Mentioned|p1238|||Geological Province: McArthur Basin.||||||10-MAR-05
16698|Scrutton Volcanics|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
16698|Scrutton Volcanics|32660|5|Briefly described|Table 2|||||||||
16698|Scrutton Volcanics|36473|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
16698|Scrutton Volcanics|41406|6|Mentioned|Map legend|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
16698|Scrutton Volcanics|42385|4|Described|p3|Paleoproterozoic|Paleoproterozoic|Overlain by Yiyintyi Sandstone in eastern Tawallah Ranges. Min. age: 1857+/-30 Ma.||||||07-NOV-08
16698|Scrutton Volcanics|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
16698|Scrutton Volcanics|42638|5|Briefly described|Map legend|Paleoproterozoic||Age: Early Proterozoic.|1857 +/- 30 Ma.|||Not shown in schematic sections.|Dacitic to rhyolitic pyroclastics and lavas; rare basaltic-doleritic lavas, sills, dykes. Tuffaceous, feldspathic sandstone. Detailed lithology given.|11-NOV-11
16698|Scrutton Volcanics|42639|4|Described|p6|Paleoproterozoic||Age: 1857+/-30Ma (U-Pb).||||||07-NOV-08
16698|Scrutton Volcanics|42739|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Rhyolitic to dacitic volcanics, volcaniclastic sandstone and mudstone, minor basalt.||||||07-NOV-08
16698|Scrutton Volcanics|42812|1|Redefined|p80|Proterozoic||U-Pb age: 1851 +/- 7 Ma. See also Table 3.||||||29-NOV-06
16698|Scrutton Volcanics|43010|5|Briefly described|Fig.6||Paleoproterozoic|of Early Proterozoic age.||||||07-NOV-08
16698|Scrutton Volcanics|43036|4|Described|p10|||Age: 1851 +/- 7 Ma.||||||29-NOV-06
16698|Scrutton Volcanics|43788|6|Mentioned|p13||Proterozoic|||||||
16698|Scrutton Volcanics|44287|14|Not recorded|p.7,15-16|||Fine-med. grained porphyritic dacite + minor vesicular basalt, lenses of feldspathic sandstone, silstone, shale, tuff. Minor intrusions of qtz gabbro, dolerite. (E53-3).||||||
16698|Scrutton Volcanics|44288|14|Not recorded|map legend||Paleoproterozoic|Porphyritic dacite, basalt, sandstone siltstone, shale, tuff, basic intrusives. Lower Proterozoic.||||||07-NOV-08
16698|Scrutton Volcanics|44530|14|Not recorded|p.7-16|||?L.Proterozoic. (D53-15).||||||
16698|Scrutton Volcanics|44531|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
16698|Scrutton Volcanics|45162|6|Mentioned|p11|||Mention Fig.7||||||
16698|Scrutton Volcanics|46915|6|Mentioned| Fig.2|||||||||
16698|Scrutton Volcanics|48867|14|Not recorded|p.7|||Resemble Edith River Volcanics.||||||
16698|Scrutton Volcanics|50591|5|Briefly described|p5.1|Paleoproterozoic|Paleoproterozoic|Age: 1851 +/- 7Ma (Shrimp). Geological Province: Arnhem Block/McArthur Basin.||||||07-NOV-08
16698|Scrutton Volcanics|60483|5|Briefly described|p3 Fig. 2|||Geological Province: McArthur Basin.||||||05-OCT-07
16698|Scrutton Volcanics|60558|5|Briefly described|p9 Fig. 7, p12|||Age: 1851Ma (SHRIMP). Geological Province: McArthur Basin.||||||03-JUN-09
16698|Scrutton Volcanics|63112|6|Mentioned|p1190|||Part of basement to southern McArthur Basin.||||||
16698|Scrutton Volcanics|63866|5|Briefly described|p54|Orosirian|Orosirian|Southern McArthur Basin.|1851 +/- 7 Ma (Page et al., 2000)|||Equivalent to the Kalkadoon Suite.||
16698|Scrutton Volcanics|64815|5|Briefly described|p3, p4 Fig.2, p5 Fig.3, p15 Fig.9 |Orosirian|Orosirian|Forms basement to the McArthur Basin in this study area.|1857 +/- 30 Ma (Pietsch et al.,1991)||||Thick pyroclastic sheets of K-rich dacitic and rhyodacitic composition, with minor felsic and mafic lavas.|
16698|Scrutton Volcanics|65228|5|Briefly described|p20, Fig.05.|Orosirian|Orosirian|McArthur River area. 1,000 m+ thick succession. U-Pb zircon age. May correlate with Leichhardt Volcanics.|1851 +/- 7 Ma (Page et al. 2000).||||Rhyolitic to dacitic ignimbrites with minor mafic flows and intrusions, with volcaniclastic sandstones.|
16698|Scrutton Volcanics|69429|4|Described|p14:2-3|Paleoproterozoic|Paleoproterozoic|Smith (1964); Haines et al. (1993). A few small areas of silicic and minor mafic volcanic rocks and interbedded sedimentary rocks; constitute the Scrutton Inlier within the McArthur Basin. Base not exposed; estimated minimum thickness of 1000m. U-Pb zircon age.|1851 +/- 7 Ma (Page et al., 2000).|||Is overlain unconformably by the Yiyintyi Sandstone (Tawallah Group). Age-equivalent to Cliffdale Volcanics (Murphy Province).|Massive pink, purple-grey and green-brown porphyritic volcanic rocks of rhyolitic to dacitic composition; abundant broken crystals and fiamme indicate ignimbrites; rhyodacitic air-fall tuffs; interbedded sandstone and mudstone; local basalt.|12-JUL-16
16698|Scrutton Volcanics|69430|6|Mentioned|p15:10, 12|||Underlies southern McArthur Basin succession.||||Is overlain unconformably by Yiyintyi Sandstone.||12-JUL-16
16698|Scrutton Volcanics|70284|6|Mentioned|p1245|||||||||
16698|Scrutton Volcanics|71592|5|Briefly described|Appendix A.|||Arnhem Province.|1851+/-7 Ma (crystallisation: U-Pb zircon SHRIMP)||||Ignimbrite.|
16698|Scrutton Volcanics|71606|5|Briefly described|p137|Orosirian|Orosirian|Batten Trough, McArthur Basin.||||Overlain unconformably by Tawallah Group.||
16698|Scrutton 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 and shallow intrusions, tuff, sandstone.|
16698|Scrutton Volcanics|72526|5|Briefly described|p8 Fig.1.3.|Orosirian|Orosirian|Shown as located in the Urapunga Fault Zone, Beetaloo Sub-basin, Batten Fault Zone and Southeastern McArthur Basin. U-Pb zircon igneous crystallisation age.|1851 +/-7 Ma|||Shown as unconformably underlying Tawallah Group.||
16698|Scrutton Volcanics|72718|6|Mentioned|p6|Orosirian|Orosirian|Scrutton Inlier. See Page et al. (2000). Provides maximum depositional age for overlying Redbank package.|1851 +/- 7 Ma SHRIMP U-Pb|||||
16698|Scrutton Volcanics|72912|5|Briefly described|p5 Fig.3.|Orosirian|Orosirian|Located in the Urapunga Fault Zone, Beetaloo Sub-basin and the Batten Fault Zone in the Southern McArthur Basin. U-Pb zircon igneous crystallisation age (Ma) shown.|1851+/-7 Ma U/Pb zircon|||Shown as unconformably underlying Yiyintyi Sandstone and probably and partially equivalent to Cliffdale Volcanics and Murphy Metamorphics.||
16698|Scrutton Volcanics|72919|5|Briefly described|p11|Orosirian|Orosirian|Scrutton Inlier. An age of 1851 +/- 7 Ma was reported by Page et al. (2000). Considered coeval with the Cliffdale Volcanics.|1851 +/- 7 Ma|||||
16698|Scrutton Volcanics|73042|6|Mentioned|p4|Orosirian|Orosirian|Southern McArthur Basin. Geochronology is a U-Pb zircon igneous crystallisation age.|1851 +/- 7 Ma (see Fig.1.2)|||||
16698|Scrutton Volcanics|73412|5|Briefly described|p2, 4, 8, 12, 14|||Basement to southern McArthur Basin. Crops out adjacent to the Rosie and Lorella Faults.|1850 Ma (Pietsch et al., 1991).|||Is overlain unconformably by Tawallah Group.||
16726|Seigal Volcanics|22538|6|Mentioned|P714||Statherian|||||||
16726|Seigal Volcanics|22644|5|Briefly described|p5 Fig. 2|||Geol province McArthur Basin. Underlain by Yiyinti Sandstone.||||||29-NOV-06
16726|Seigal Volcanics|22853|4|Described|5 & 6|Proterozoic|Proterozoic|Geological province: McArthur Basin. Of the Tawallah Group. Max thickness: 400 m. Overlain by Sly Creek Sandstone.||||||29-NOV-06
16726|Seigal Volcanics|23065|6|Mentioned|15|||Geological province: McArthur Basin. Of the Tawallah Group.||||||29-NOV-06
16726|Seigal Volcanics|23066|5|Briefly described|p808|||||||||
16726|Seigal Volcanics|23363|5|Briefly described|344 Fig.3|||||||||
16726|Seigal Volcanics|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|Of Tawallah Group.||||||07-NOV-08
16726|Seigal Volcanics|23395|6|Mentioned|p385|||||||||
16726|Seigal Volcanics|23396|5|Briefly described|p407 Fig.2|||Of Tawallah Group.||||||29-NOV-06
16726|Seigal Volcanics|23733|5|Briefly described|p32 Fig. 19|||Of Tawallah Group.  Geological Province: MacArthur Basin.||||||
16726|Seigal Volcanics|23776|5|Briefly described|p705 Fig 2.|||Of Tawallah Group.||||||
16726|Seigal Volcanics|23867|5|Briefly described|Fig. 30|||Of Tawallah Group. Correlates with Nungbalgarri Volcanics of the Kombolgie Subgroup (Katherine River Group).||||||
16726|Seigal Volcanics|23910|5|Briefly described|p292 Fig. 3|||Of Tawallah Group.  Geological Province: McArthur Basin.||||||
16726|Seigal Volcanics|23963|5|Briefly described|p1239 Fig.2|||Geological Province: McArthur Basin. Of the Tawallah Group||||||
16726|Seigal Volcanics|24419|5|Briefly described|p13 Fig.5|Paleoproterozoic|Paleoproterozoic|Of the Tawallah Group. Geological Province: McArthur Basin; Murphy Province||||||07-NOV-08
16726|Seigal Volcanics|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Mafic. Geological Province: Southern McArthur Basin.||||||
16726|Seigal Volcanics|31421|6|Mentioned|p507|||See also p509.||||||29-NOV-06
16726|Seigal Volcanics|35114|6|Mentioned|p200|||||||||
16726|Seigal Volcanics|35640|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
16726|Seigal Volcanics|36012|3|Fully described|Table 2|||See also p11 and p16.||||||29-NOV-06
16726|Seigal Volcanics|36439|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
16726|Seigal Volcanics|36442|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
16726|Seigal Volcanics|37568|5|Briefly described|p78|||||||||
16726|Seigal Volcanics|38584|4|Described|p11, p12|||||||||
16726|Seigal Volcanics|38902|6|Mentioned|p28|||||||||
16726|Seigal Volcanics|39445|5|Briefly described|Table 2|||See also p36.||||||29-NOV-06
16726|Seigal Volcanics|39497|6|Mentioned|Fig.4|||||||||
16726|Seigal Volcanics|39685|6|Mentioned|Fig.1|||||||||
16726|Seigal Volcanics|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
16726|Seigal Volcanics|40489|6|Mentioned|p89|||||||||
16726|Seigal Volcanics|40491|6|Mentioned|p79|||||||||
16726|Seigal Volcanics|40691|5|Briefly described|p9|||||||||
16726|Seigal Volcanics|40811|6|Mentioned|p318|||||||||
16726|Seigal Volcanics|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
16726|Seigal Volcanics|41125|6|Mentioned|p35|||See also fig.21, fig.22.||||||
16726|Seigal Volcanics|41319|6|Mentioned|Fig.1|||||||||
16726|Seigal Volcanics|41406|6|Mentioned|Map legend|Mesoproterozoic||||||||
16726|Seigal Volcanics|41721|3|Fully described|p16|||Of Tawallah Group. Represents lower part of Peters Creek Volcanics (as mapped by Roberts et al,1963).Conformably overlie Westmoreland Conglomerate; underlies Mcdermott  Formation.Thickness:1500m. Geol.prov: McArthur Basin. Basalt and tuff; minor sandstone||||||01-AUG-07
16726|Seigal Volcanics|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
16726|Seigal Volcanics|42385|4|Described|p5-6|Mesoproterozoic|Mesoproterozoic|Conformable over Yiyintyi Sandstone; underlies Sly Creek Sandstone.  Max. thickness: up to 400m. Typically occur as amygdaloidal basalt flows with fine-grained, chilled bases and vesicular tops.||||||18-SEP-07
16726|Seigal Volcanics|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
16726|Seigal Volcanics|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.||||In schematic section, underlies Sly Creek Sandstone; overlies Yiyintyi Sandstone.|Amygdaloidal basalt lava.|11-NOV-11
16726|Seigal Volcanics|42639|4|Described|p8, Table 4 p11|||||||||
16726|Seigal Volcanics|42700|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
16726|Seigal Volcanics|42739|5|Briefly described|map legend|Statherian|Statherian|Of the Tawallah Group. Basalt lava, amygaloidal and massive, in part hyaloclastic.||||||19-OCT-05
16726|Seigal Volcanics|42812|3|Fully described|p11, Table 3|||Of Tawallah Group.||||||29-NOV-06
16726|Seigal Volcanics|43010|5|Briefly described|Fig.6||Mesoproterozoic|Of Tawallah Group. Of "Mid Proterozoic" age.||||||29-NOV-06
16726|Seigal Volcanics|43036|3|Fully described|p15|||Of the Tawallah Group.||||||29-NOV-06
16726|Seigal Volcanics|43788|6|Mentioned|p14|||||||||
16726|Seigal Volcanics|45162|2|Defined|p14|Proterozoic|Proterozoic|||||||
16726|Seigal Volcanics|45166|5|Briefly described|p28|||||||||
16726|Seigal Volcanics|46804|6|Mentioned|p154|||||||||
16726|Seigal Volcanics|49001|2|Defined|p4|Carpentarian|Carpentarian|||||||
16726|Seigal Volcanics|60483|5|Briefly described|p7 Fig. 5, p27|||Of the Tawallah Group. Includes Carolina Sandstone Member. Geological Province: McArthur Basin.||||||05-OCT-07
16726|Seigal Volcanics|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Tawallah Group. Includes Carolina Sandstone Member. Overlain by Sly Creek Sandstone, underlain by Yiyintyi Sandstone and Westmoreland Conglomerate.||||||
16726|Seigal Volcanics|63112|6|Mentioned|p1191 Fig.2, p1192 Tb.1, p1195, p1206 |||Leichhardt Superbasin. One of the mafic rock units that may have been the source of metals in the basin. Age approximated from Fig.2. 300-400 m thick. Mis-spelt as Siegal on p.1206.|c.1775-1780 Ma.||Includes Carolina Sandstone Member.||Amygdaloidal basalt lava; dolerite sills (a lower basalt-dominated one and an upper mixed basalt-sediment one) separated by fine-grained sandstone.|
16726|Seigal Volcanics|63866|5|Briefly described|p54, p56|||||Myally Supersequence||Overlies the Yiyintyi Sandstone. Equivalent to the Eastern Creek Volcanics and the Buddawadda Basalt.|Mafic volcanic rocks with continental tholeiite affinities.|
16726|Seigal Volcanics|64250|6|Mentioned|p25 fig 10|||Southern McArthur Basin. Contemporaneous with volcanism in Mount Isa Inlier.|c.1780 Ma|Unit in Tawallah Group.|||Mafic volcanic rocks.|
16726|Seigal Volcanics|64815|6|Mentioned|p4 Fig.2, p5 Fig.3 |||||Of the Tawallah Group.||||
16726|Seigal Volcanics|64817|6|Mentioned|p353 Fig.4, p355 Fig.5 |||||Of the Tawallah Group.|Includes Carolina Sandstone Member.|||
16726|Seigal Volcanics|65228|5|Briefly described|Figs.02, 05-07, 09.|||McArthur Basin.||Unit in Tawallah Group.|Includes Carolina Sandstone Member.|Overlies Yiyintyi Sandstone and Westmoreland Conglomerate. Is overlain by Sly Creek Sandstone and McDermott Formation.||
16726|Seigal Volcanics|65232|6|Mentioned|p9, p8 Fig. 7, p66, App. 2|||Of Tawallah Group. Conformably overlies Westmoreland Conglomerate. Thickness: up to 1600 m. Basalt flows and minor tuff beds and thin interbeds of siltstone and sandstone. Uranium mineralisation. Geol. Prov: McArthur Basin.||||||09-FEB-10
16726|Seigal Volcanics|65337|6|Mentioned|p13.|||Southern McArthur Basin. Some parts of Mitchiebo Volcanics resemble this unit.||||||
16726|Seigal Volcanics|65340|5|Briefly described|p12 Fig.6, p22, 93.|||A flood basalt unit from 0.1 to 1.6 km thick.||Unit in Tawallah Group.|Includes Carolina Sandstone Member.|Overlies Westmoreland Conglomerate and Yiyintyi Sandstone. Is overlain by Sly Creek Sandstone.||23-MAR-18
16726|Seigal Volcanics|66529|5|Briefly described|p20 Fig.7, p21  |||||||Conformably overlies the Westmoreland Conglomerate. Is overlain by Tawallah Group.|Basalt.|
16726|Seigal Volcanics|67057|6|Mentioned|p462.|Paleoproterozoic|Paleoproterozoic||1780 - 1760 Ma.|||||
16726|Seigal Volcanics|67144|5|Briefly described|Map legend.|Statherian|Statherian|||Unit in Tawallah Group.||Overlies Westmoreland Conglomerate. Is overlain by McDermott Formation.|Amygdaloidal basalt.|
16726|Seigal Volcanics|67323|4|Described|GIS attrib tbl, Solid Geology Map, p31|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. McArthur Basin, Leichhardt Superbasin. Camooweal-Murphy Domain, Mount Isa Inlier.|~1790 Ma.|Tawallah Group.|Carolina Sandstone Member.|Is overlain by Sly Creek Sandstone.|Vesicular and amygdaloidal basalt; massive non-vesicular basalt; thin siltstone; sandstone and tuff interbeds with scattered basalt bombs or cobbles.|
16726|Seigal Volcanics|67352|4|Described|p15 Tb.2|Statherian|Statherian|McArthur Basin. 1600 m thick.||Tawallah Group||Conformably overlies Yiyintyi Sandstone or Westmoreland Conglomerate. Overlain by McDermott Formation (conformably).|Altered basic lava flows: massive, amygdaloidal, vesicular, brecciate, haematitic; minor siltstone, feldspathic sandstone.|
16726|Seigal Volcanics|68020|6|Mentioned|p127|||||||Unconformably overlies Westmoreland Conglomerate.||
16726|Seigal Volcanics|69383|5|Briefly described|p48|Paleoproterozoic|Paleoproterozoic|McArthur Basin.|||Includes Carolina Sandstone Member.||A series of basaltic flows and brecciated volcanic facies; flaggy to massive, fine-grained sandstone.|
16726|Seigal Volcanics|69418|6|Mentioned|p3:19|||McArthur Basin. Hosts U in Westmoreland-Murphy-type deposits (described).||||||12-JUL-16
16726|Seigal Volcanics|69423|5|Briefly described|p8:4 Fig.8.7, 5-6|Paleoproterozoic|Paleoproterozoic|McArthur Basin. Hosts a number of uranium +/- gold occurrences.||Tawallah Group.||||12-JUL-16
16726|Seigal Volcanics|69430|4|Described|p15:3, 10-12, 44, 49-50|||Southern McArthur Basin. 225-1500m thick. Mostly subaerial lava. Upper part is correlated with Sly Creek Sandstone (and Rosie Creek Sandstone Member). Is pierced by a Cu-bearing volcanic plug, and hosts economically insignificant vein-type Cu occurrences. Hosts small U-Au deposits (described in some detail).||Tawallah Group.|Carolina Sandstone Member.|Overlies Westmoreland Conglomerate conformably, and Yiyintyi Sandstone conformably or sharply unconformably [?]. Is overlain conformably by McDermott Formation and Sly Creek Sandstone.|Amygdaloidal basalt flows 5-30m thick; thin siltstone and tuffaceous interbeds in upper part. Includes a prominent sandstone bed (Carolina Sandstone Member). Several feeder dykes are known; is intruded by a plug of volcanic breccia.|12-JUL-16
16726|Seigal Volcanics|69433|5|Briefly described|p18:2, 6|||McArthur Basin. Is lithologically and geochemically indistinguishable from the Mitchiebo Volcanics (Lawn Hill Platform).||Tawallah Group.||Probably equivalent to Peters Creek Volcanics (Lawn Hill Platform). Correlated with Mitchiebo Volcanics.||12-JUL-16
16726|Seigal Volcanics|69591|5|Briefly described|p33-34, p58|||Camooweal-Murphy Domain, Leichhardt Superbasin. Correlations with Eastern Creek Volcanics and Buddawadda Basalt Member (Peters Creek Volcanics) are speculative.||Tawallah Group.||Overlies Westmoreland Conglomerate.|Vesicular and amygdaloidal basalt; massive non-vesicular basalt; thin siltstone; sandstone and tuff interbeds with scattered basalt bombs or cobbles.|
16726|Seigal Volcanics|69673|6|Mentioned|p16 fig 13, p17 fig 14|||||Tawallah Group|Includes Carolina Sandstone Member|Overlain by Sly Creek Sandstone, Rosie Creek Sandstone Member, overlies Yiyintyi Sandstone||
16726|Seigal Volcanics|70284|5|Briefly described|p1244, p1245-1247, p1250-1253, 1257|Statherian|Statherian|McArthur Basin, Leichhardt Superbasin. Generally <20m thick, but may be up to 1600m thick. Geochemistry suggests dolerite dykes in region may be feeders.||||Conformably overlies Westmoreland Conglomerate.|Basaltic lava flows.|14-DEC-16
16726|Seigal Volcanics|70849|5|Briefly described|Map legend.|Statherian|Statherian|McArthur Basin.||Tawallah Group.|Carolina Sandstone Member.|Overlies Westmoreland Conglomerate. Is overlain by McDermott Formation.|Vesicular and amygdaloidal basalt; massive non-vesicular basalt; thin siltstone, sandstone and tuff interbeds.|
16726|Seigal Volcanics|71799|5|Briefly described|p150 fig 2, p156, p157 fig 5, p158|Statherian|Statherian|McArthur Basin.|ca. 1780 Ma|||Overlies the Westmoreland Conglomerate.|Basalt, dolerite, gabbro or amphibolite.|
16726|Seigal Volcanics|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Urapunga Fault Zone, Beetaloo Sub-basin, Batten Fault Zone and Southeastern McArthur Basin.||Tawallah Group||Partially overlies Yiyintyi Sandstone and Westmoreland Conglomerate and partially underlies Rosie Creek Sandstone Member and underlies and is laterally equivalent to Sly Creek Sandstone.||
16726|Seigal Volcanics|72718|6|Mentioned|p7|||Southern McArthur Basin. Incorporates[?] Carolina Sandstone Member.||Tawallah Group|Carolina Sandstone Member|Partly underlain by Yiyintyi Sandstone and Westmoreland Conglomerate. Partly overlain by and equivalent to Sly Creek Sandstone. Partly overlain by Rosie Creek Sandstone Member.||
16726|Seigal Volcanics|72912|5|Briefly described|p5 Fig.3, p19, p31 Fig.11.|Statherian|Statherian|Located in the Beetaloo Sub-basin and the Batten Fault Zone in the Southern McArthur Basin.||Tawallah Group||Overlies Yiyintyi Sandstone and Westmoreland Conglomerate, and underlies Sly Creek Sandstone and Rosie Creek Sandstone Member.||
16726|Seigal Volcanics|72919|6|Mentioned|p12|||[Written as Seigal Volcanics?]. Possibly intersected in drillhole BEN-SD60.|||||May include andesitic volcanics.|
16726|Seigal Volcanics|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin, Leichhardt Superbasin.  Partly overlain by Sly Creek Sandstone and Rosie Creek Sandstone Member.||Tawallah Group||Partly underlain by Yiyintyi Sandstone and Westmoreland Conglomerate.||
16726|Seigal Volcanics|73083|6|Mentioned|p35, p77|||||Tawallah Group||||
16726|Seigal Volcanics|73412|5|Briefly described|p2, 4, 8-9, 12, 20|||Southern McArthur Basin. Characterised by a magnetic low; ?reversely magnetised.||Tawallah Group.||Overlies Yiyintyi Sandstone and Westmoreland Conglomerate. Is overlain by Sly Creek Sandstone.||
16750|Sentinel beds|42699|5|Briefly described|map legend|Mesoproterozoic||Not related to Sentinel Range Igneous Complex, Qld.||||||
16750|Sentinel beds|43035|4|Described|p17|||||||||
16750|Sentinel beds|69436|5|Briefly described|p21:6|||Edgoose et al. (1993). Informal name for numerous ridges of quartzite in the Mulga Park area, Musgrave Province.|||||Foliated quartzite and quartz-muscovite schist containing minor garnet and/or biotite; locally intercalated with granite, pegmatite and amphibolite.|12-JUL-16
16758|Septimus Limestone|13194|4|Described|p390 Tb. 4-16, p402 fig 4-66|Middle Tournaisian||Type Section: Mount Septimus 15o43'S 128o59'E. 25-300m thick marine shelf, shoreface and foreshore deposits.||Langfield Group||Overlies Enga Sandstone (conformably). Overlain by Zimmerman[n] Sandstone (conformably).|Limestone and sandy limestone; minor marl and calcareous sandstone.|19-JUL-16
16758|Septimus Limestone|13234|5|Briefly described|p252 |||Includes traces of oil.||||Correlated with the Ningbing Limestone.||
16758|Septimus Limestone|23820|5|Briefly described|p202 Fig.2|Early Carboniferous|Early Carboniferous|Geological Province: Bonaparte Gulf Basin.||||||
16758|Septimus Limestone|31519|6|Mentioned|p917|||||||||
16758|Septimus Limestone|31714|6|Mentioned|p32|||||||||
16758|Septimus Limestone|32648|6|Mentioned|p32|||Tournaisian||||||
16758|Septimus Limestone|32664|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|Briefly described in notes||||||
16758|Septimus Limestone|32699|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|Limestone, minor calcareous sandstone.||||||02-DEC-04
16758|Septimus Limestone|32701|4|Described|Table 2|||L.Carb. See p16.||||||30-NOV-06
16758|Septimus Limestone|32870|5|Briefly described|p46|||||||||
16758|Septimus Limestone|34085|6|Mentioned|Cor.chart|||Tournaisian||||||
16758|Septimus Limestone|34155|6|Mentioned|p94|||||||||
16758|Septimus Limestone|36257|6|Mentioned|Table 2.1|||||||||
16758|Septimus Limestone|36473|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
16758|Septimus Limestone|36551|6|Mentioned|Table 16|||||||||
16758|Septimus Limestone|36890|3|Fully described|p379|||Formerly Mount Septimus Limestone.||||||30-NOV-06
16758|Septimus Limestone|36904|5|Briefly described|p9|||||||||
16758|Septimus Limestone|39827|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
16758|Septimus Limestone|40494|4|Described|p17|||||||||
16758|Septimus Limestone|40792|6|Mentioned|p175|||||||||
16758|Septimus Limestone|40993|6|Mentioned|p10|||||||||
16758|Septimus Limestone|41712|6|Mentioned|Fig.14|||||||||
16758|Septimus Limestone|41839|4|Described|p28|||Formerly "Mount Septimus Limestone".||||||30-NOV-06
16758|Septimus Limestone|41864|3|Fully described|p108|||Formerly called "Mount Septimus Series", "Mount Septimus Limestone".||||||30-NOV-06
16758|Septimus Limestone|41865|5|Briefly described|Map legend||middle Tournaisian|||||||
16758|Septimus Limestone|42175|5|Briefly described|Fig.2 P200|||||||||
16758|Septimus Limestone|42547|4|Described|p101|||||||||
16758|Septimus Limestone|42933|5|Briefly described|Fig.94 p258|||||||||
16758|Septimus Limestone|42994|6|Mentioned|p13|||||||||
16758|Septimus Limestone|43385|14|Not recorded|p176|||||||||
16758|Septimus Limestone|44159|6|Mentioned|Table p.38||Early Carboniferous|||||||
16758|Septimus Limestone|44965|14|Not recorded|Not recorded|||||||||
16758|Septimus Limestone|44993|14|Not recorded|p.7|||Camaratoechia.||||||
16758|Septimus Limestone|44994|6|Mentioned|p15|||Fig.6 Correlation.||||||
16758|Septimus Limestone|44998|14|Not recorded|App.3 p277-9|||Overlies Enga Sandstone.||||||
16758|Septimus Limestone|45015|6|Mentioned|p66|||Can be correlated with Moogooree Limestone. Geological Province: Bonaparte Gulf Basin.||||||01-JUN-06
16758|Septimus Limestone|45038|2|Defined|p.82||Early Carboniferous|See also Plates and Figures. L.Carb.||||||
16758|Septimus Limestone|45039|6|Mentioned|p1|||Lower Carboniferous. See also pp5,6,7,8,14 etc.||||||30-NOV-06
16758|Septimus Limestone|45050|6|Mentioned|p46|||See also pp50,51,57 etc. Late Tournaisian.||||||30-NOV-06
16758|Septimus Limestone|45063|6|Mentioned|p8|||See also pp18, 25 & Fig. 3. Tournaisian.||||||30-NOV-06
16758|Septimus Limestone|45097|6|Mentioned|Fig.|||Refers Mamet and Bedford (1968 p345).||||||30-NOV-06
16758|Septimus Limestone|45133|6|Mentioned|Fig.13|||||||||
16758|Septimus Limestone|45169|4|Described|p4|||||||||
16758|Septimus Limestone|46803|6|Mentioned|p147|||||||||
16758|Septimus Limestone|47040|6|Mentioned|Fig.3|||||||||
16758|Septimus Limestone|48635|14|Not recorded|Fig.1||Early Carboniferous|(D/52-10,11,14,15). Lower Carboniferous.||||||
16758|Septimus Limestone|48831|14|Not recorded|p.60|||||||||
16758|Septimus Limestone|48886|14|Not recorded|Map||Early Carboniferous|Lower Carboniferous.||||||
16758|Septimus Limestone|48971|6|Mentioned|p15|||See also p31, p32, p35, p36, p37, p39, p40, p41.||||||30-NOV-06
16758|Septimus Limestone|60006|5|Briefly described|Map Legend|Tournaisian|Tournaisian|Geological Province: Bonaparte Basin. Of Langfield Group. Dolomitic and calcareous sandstone, minor limestone||||||22-JUL-04
16758|Septimus Limestone|60364|4|Described|p184, 187, 194|Tournaisian|Tournaisian|Of Langfield Gp. Overlies Enga Sst. Disconform.overlain by Zimmermann Sst and Border Creek Fm. Thickness at type section: 180m. Skeletal sandy calcarenite, and minor dolomitic quartz sandstone. Abundant brachiopods. Geological Province: Bonaparte Basin||||||30-NOV-06
16758|Septimus Limestone|60682|4|Described|p22 Table 5, 24|Tournaisian|Tournaisian|Of Langfield Group. Conformably overlies Enga Sandstone. Conformably overlain by Zimmerman Sandstone. Max. thickness: <100m. Dolomitic and calcareous sandstone. Geological Province: Bonaparte Basin.||||||11-MAY-05
16758|Septimus Limestone|61542|5|Briefly described|p277 Fig. 2|Tournaisian|Tournaisian|Of the Langfield Group. Geological Province: onshore Bonapart Basin/Petrel-Sub-basin.||||||07-FEB-11
16758|Septimus Limestone|64580|6|Mentioned|map legend|||Of Langfield Group.||||||15-DEC-08
16758|Septimus Limestone|64694|5|Briefly described|p233, p239, p247, p254 Fig.12|Tournaisian|Tournaisian|Burt Range Shelf, Onshore Bonaparte Basin.||Unit in Langfield Group.||Overlies Enga Sandstone. Is overlain disconformably by Zimmermann Sandstone.||
16758|Septimus Limestone|65331|5|Briefly described|Map legend|Tournasian|Tournasian|Of Langfield Group, Bonaparte Basin. Dolomitic and calcareous sandstone, minor limestone||||||
16758|Septimus Limestone|69099|5|Briefly described|500k_geologyp08_lut.csv|Tournasian|Tournasian|||Langfield Group||||
16758|Septimus Limestone|69165|6|Mentioned|500k_geologyp08_lut.csv|Tournaisian|Tournaisian|||Langfield Group||||
16758|Septimus Limestone|69452|3|Fully described|p36:6 Fig.36.5; 36:9, 12-14|Tournaisian|Tournaisian|Veevers and Roberts (1968). Equivalent to Mount Septimus Limestone of Noakes et al. (1952). Petrel Sub-basin, Bonaparte Basin. Type section at Mount Septimus where it is 300m thick; thins rapidly away from this area. Main outcrops in Burt Range (WA). High-energy shallow-marine deposits. Onshore.||Langfield Group.||Conformably overlies Enga Sandstone. Is overlain conformably by Zimmermann Sandstone, and unconformably by Keep Inlet and Milligans Formations.|Limestone, quartzose limestone and calcareous sandstone. The sparse NT exposures consist of thinly bedded fine-grained dolomitic and calcareous feldspathic sandstone. Diverse fossil assemblage.|12-JUL-16
16758|Septimus Limestone|69634|5|Briefly described|500k_geologyp08_lut.csv|Tournaisian|Tournaisian|||Unit of Langfield Group.||||
16758|Septimus Limestone|69673|5|Briefly described|p171, p179, p180|||300m thick. Potential as a reservoir rock.||Langfield Group|||Limestone, quartzose limestone and calcareous sandstone.|
16758|Septimus Limestone|70206|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Bonaparte Basin.||Langfield Group|||Dolomitic and calcareous sandstone, minor limestone.|
16758|Septimus Limestone|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Langfield Group.|||Dolomitic and calcareous sandstone, minor limestone|
16787|Shady Bore Quartzite|22438|6|Mentioned|p549, Fig.12|||||||||
16787|Shady Bore Quartzite|22453|6|Mentioned|p 12|||||||||
16787|Shady Bore Quartzite|22680|6|Mentioned|83,85-87|||Geological province: Mount Isa Basin. Of the McNamara Group.||||||30-NOV-06
16787|Shady Bore Quartzite|23031|6|Mentioned|40|||Geological province: Lawn Hill Subprovince. Of the McNamara Group.||||||30-NOV-06
16787|Shady Bore Quartzite|23072|5|Briefly described|p754|||||||||
16787|Shady Bore Quartzite|23387|6|Mentioned|p18 fig.19|||Of McNamara Group.||||||
16787|Shady Bore Quartzite|23393|4|Described|p19, p20|Paleoproterozoic|Paleoproterozoic|Of McNamara Group.  Overlies Lady Loretta Formation.||||||07-NOV-08
16787|Shady Bore Quartzite|23396|5|Briefly described|p407 Fig.2|||Of McNamara Group.||||||30-NOV-06
16787|Shady Bore Quartzite|23397|5|Briefly described|p471|||||||||
16787|Shady Bore Quartzite|23398|5|Briefly described|p447|||Of McNamara Group.||||||
16787|Shady Bore Quartzite|23405|5|Briefly described|p565 Fig.2|||Of McNamara Group.||||||
16787|Shady Bore Quartzite|23406|5|Briefly described|p606|||Of Fickling Group?||||||24-JUN-09
16787|Shady Bore Quartzite|23408|5|Briefly described|p513 Fig.2|||Of McNamara Group||||||30-NOV-06
16787|Shady Bore Quartzite|23409|4|Described|p541|||Of McNamara Group.||||||30-NOV-06
16787|Shady Bore Quartzite|23466|5|Briefly described|p272 Fig.6|Statherian|Statherian|||||||
16787|Shady Bore Quartzite|23958|3|Fully described|p1134|Paleoproterozoic|Paleoproterozoic|Of McNamara Group.  Max. thickness: 460m.||||||07-NOV-08
16787|Shady Bore Quartzite|23964|5|Briefly described|p1265|Proterozoic|Proterozoic|Of McNamara Group.  Geological Province: Mount Isa Inlier.  Maximum thickness: 590m.||||||13-MAY-14
16787|Shady Bore Quartzite|23965|5|Briefly described|p1297|Mesoproterozoic|Paleoproterozoic|Of McNamara Group. Geological Province: Mount Isa Inlier.||||||07-NOV-08
16787|Shady Bore Quartzite|24033|6|Mentioned|p25, p26 Fig. 10|||||||||
16787|Shady Bore Quartzite|24308|5|Briefly described|p987 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of the McNamara Group.   Geological Province: Mount Isa Superbasin.||||||07-NOV-08
16787|Shady Bore Quartzite|24309|5|Briefly described|p1024|Proterozoic|Proterozoic|Of the McNamara Group.||||||30-NOV-06
16787|Shady Bore Quartzite|24432|4|Described|p562 Fig.2|Statherian|Statherian|Of McNamara Group. Overlain by Riversleigh Siltstone. Age: c.1647 Ma. Geological Province: Lawn Hill Platform.||||||
16787|Shady Bore Quartzite|24442|5|Briefly described|p23 Fig. 2|Mesoproterozoic|Mesoproterozoic|Of the McNamara Group.  Age: >1590Ma.||||||
16787|Shady Bore Quartzite|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
16787|Shady Bore Quartzite|36937|6|Mentioned|p229|||||||||
16787|Shady Bore Quartzite|37459|1|Redefined|p431|Mesoproterozoic|Mesoproterozoic|Age is more specifically Carpentarian.||||||30-NOV-06
16787|Shady Bore Quartzite|37568|5|Briefly described|p84|||||||||
16787|Shady Bore Quartzite|38237|4|Described|p129|||||||||
16787|Shady Bore Quartzite|38291|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
16787|Shady Bore Quartzite|38348|4|Described|p13|||||||||
16787|Shady Bore Quartzite|38584|6|Mentioned|p22|||||||||
16787|Shady Bore Quartzite|39445|5|Briefly described|Table 2|||||||||
16787|Shady Bore Quartzite|39497|6|Mentioned|p14|||See also Fig.4||||||
16787|Shady Bore Quartzite|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the McNamara Group.  Overlies Lady Loretta Formation.||||||15-JUN-06
16787|Shady Bore Quartzite|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
16787|Shady Bore Quartzite|39925|6|Mentioned|Fig.9|||||||||
16787|Shady Bore Quartzite|39944|6|Mentioned|Fig.1|||||||||
16787|Shady Bore Quartzite|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
16787|Shady Bore Quartzite|40221|3|Fully described|p18|||||||||
16787|Shady Bore Quartzite|41298|6|Mentioned|Map legend|Carpentarian||||||||
16787|Shady Bore Quartzite|43486|5|Briefly described|21|||||||||
16787|Shady Bore Quartzite|45166|5|Briefly described|p30|||||||||
16787|Shady Bore Quartzite|47083|4|Described|p18||Proterozoic|Of McNamara Group. Overlain by Riversleigh Siltstone; underlain by Lady Loretta Fm. Maximum thickness: 250 m.||||||30-NOV-06
16787|Shady Bore Quartzite|50550|5|Briefly described|p1139 Fig.2||Statherian|Age: >1644 Ma, <1647 Ma. Conformably overlies Lady Loretta Formation, conformably overlain by Riversleigh Siltstone. Geological Province: Western Fold Belt.||||||19-DEC-07
16787|Shady Bore Quartzite|50600|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the McNamara Group.  White, flaggy to massive, medium orthoquartzite, siltstone and dolomite.  Overlies Lady Loretta Formation; overlain by Riversleigh Siltstone.||||||28-JUN-04
16787|Shady Bore Quartzite|60558|5|Briefly described|p5 Fig. 4|||Of McNamara Group. Overlain by Riversleigh Siltstone, underlain by Lady Loretta Formation.||||||
16787|Shady Bore Quartzite|61913|6|Mentioned|p161|||||||||
16787|Shady Bore Quartzite|61936|5|Briefly described|p194 Fig. 6|||Geological Province: Lawn Hill Platform, Western Fold Belt, Mount Isa Inlier.||||||
16787|Shady Bore Quartzite|62084|5|Briefly described|p936 Fig.5|||Isa Superbasin. Lawn Hill. Shown as Shady Bore Qzit.||McNamara Group|||Rift phase clastics.|
16787|Shady Bore Quartzite|62535|5|Briefly described|p672|Statherian|Statherian|Lawn Hill Platform. Lithology not specified.||McNamara Group.||||
16787|Shady Bore Quartzite|62659|5|Briefly described|Map Legend|Statherian|Statherian|Of the McNamara Group. White, very fine to medium grained lithic and sublithic sandstone with wave rippled bedding surfaces.||||||
16787|Shady Bore Quartzite|63109|6|Mentioned|p1108 Fig. 3|||Overlain by Riversleigh Siltstone. Geological Province: Isa Superbasin. Consists of sandstone and conglomerate.||||||30-SEP-08
16787|Shady Bore Quartzite|63111|5|Briefly described|p1162, p1163 Fig. 3|Statherian|Statherian|Of River Supersequence. Age: 1644+/-8 and 1640+/-7Ma. Geological Province: Isa Superbasin. Consists of conglomerates and fine-grained arenites.||||||07-FEB-11
16787|Shady Bore Quartzite|63113|6|Mentioned|p1214 Fig.2, p1225 Fig.13. |||Part of River supersequence.|Between 1647 Ma and 1644 Ma.|Of the McNamara Group||Overlies ?unconformably Lady Loretta Formation. Is overlain by Riversleigh Siltstone.||
16787|Shady Bore Quartzite|63114|5|Briefly described|p1253 Fig.2. |||Isa superbasin. Appears only as Shady Bore.||Of the River supersequence.||Overlies Lady Loretta Formation.||
16787|Shady Bore Quartzite|63115|6|Mentioned|p1279 Fig.4.|||Isa superbasin.||||||
16787|Shady Bore Quartzite|63116|6|Mentioned|p1297 Fig.2,p1299 Tb.1,p1300, |||Isa superbasin. Material properties detailed. Basal unit of River supersequence. Shows well-developed quartz cements and stylolites subparallel to bedding; probably an initial aquifer but became an aquiclude early in the history of the basin.||||||
16787|Shady Bore Quartzite|64250|6|Mentioned|p11 fig 3|||||Unit in McNamara Group.||||
16787|Shady Bore Quartzite|64575|6|Mentioned|p665|||||||||
16787|Shady Bore Quartzite|65337|4|Described|p9 Fig.5, pp21-22, p26.|Paleoproterozoic|Paleoproterozoic|Southeast MOUNT DRUMMOND area. Up to 50 m of shallow marine deposits.||Unit in McNamara Group.||Overlies Brumby Formation and Lady Loretta Formation. Is overlain by Plain Creek Formation and Riversleigh Siltstone.|White, very fine- to medium-grained lithic and sublithic sandstone; prominently wave-rippled bedding surfaces.|
16787|Shady Bore Quartzite|65396|5|Briefly described|p82, p175, p241|||Isa Superbasin. Cover Sequence 3. Lawn Hill Platform.||McNamara Group||Overlies Lady Loretta Formation; overlain by Riversleigh Formation.||04-APR-17
16787|Shady Bore Quartzite|66843|6|Mentioned|p38 Fig.10|||shown only as Shady Bore.||||||12-SEP-19
16787|Shady Bore Quartzite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map|Paleoproterozoic|Paleoproterozoic|See also , Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Mount Isa Inlier, Isa Superbasin.||McNamara Group.|||Flaggy to massive medium orthoquartzite; interbeds of fine sandstone, siltstone, and dolomite|
16787|Shady Bore Quartzite|68542|6|Mentioned|p6|||||Upper McNamara Group||Overlain by Riversleigh Siltstone|Basal, coarse clastics fining upwards into a thick sequence of dolomitic siltstone.|
16787|Shady Bore Quartzite|68576|5|Briefly described|Q_2: p6|||Lawn Hill Platform, Mount Isa Inlier.||Upper McNamara Group.||Overlies Lady Loretta Formation. Is overlain by Riversleigh Siltstone.||
16787|Shady Bore Quartzite|68732|6|Mentioned|p165 Fig.3|||Presented as Shady Bore in figure. Of the River Supersequence.||||||
16787|Shady Bore Quartzite|69433|4|Described|p18:2, 5-6, 9|Statherian|Statherian|Southern succession, Lawn Hill Platform. Up to 50m thick. Wave-dominated marine shoreline deposits in a series of upward-shallowing cycles.|c.1640 Ma.|McNamara Group.||Conformably overlies Brumby Formation. Is overlain conformably and transitionally by Plain Creek Formation. Correlative of Breakfast Sandstone (?).|White, thinly to thickly bedded, fine- and medium-grained lithic and sublithic sandstone; features cross-beds and prominent wave ripple marks on bedding surfaces.|12-JUL-16
16787|Shady Bore Quartzite|69591|5|Briefly described|p43 Fig.2.31, p47, p54|||Camooweal-Murphy and Century Domains, Isa Superbasin. Part of the River Supersequence. High energy fluvial/shallow marine deposits.||McNamara Group.|||Flaggy to massive medium orthoquartzite; interbeds of fine sandstone, siltstone and dolomite.|
16787|Shady Bore Quartzite|69673|5|Briefly described|p52 fig 42, p53 |||40-50m thick. Deposited in a wave dominated marine shoreline environment in a series of upward shallowing cycles.||McNamara Group|||Lithic and sublithic sandstones.|
16787|Shady Bore Quartzite|70864|5|Briefly described|p75, 74 Fig 2|Mesoproterozoic||||McNamara Group|||Quartz sandstone, siltstones and dolomite.|
16787|Shady Bore Quartzite|70897|6|Mentioned|Fig.1.7.7|||Isa Superbasin.||||||
16787|Shady Bore Quartzite|72526|4|Described|p1-2, p4, p7 Tb.1.1, p8, p10-19|Statherian|Statherian|Shown as located in the Lawn Hill Platform of the Mount Isa Province and the east part of the South Nicholson Basin. Maximum depositional age reported here from Lawn Hill, Qld sample: 1694+/-17 Ma. Depositional age already constrained by age from tuffs in underlying Lady Loretta Formation. Previous MDA reported  from Mount Drummond, NT: 1635+/-8 Ma (Kositcin and Carson, 2019). Base of unit shown as older in NT than Qld, p8. Qld sample displays bedding surfaces with wave ripples and tabular moulds of probable rip-up mud clasts.See also p85, p87.|1647 Ma to 1635+/-8 Ma.|McNamara Group||Conformably overlies Lady Loretta Formation, Brumby Formation.Conformably underlies Riversleigh Siltstone, Plain Creek Formation.|White very fine to medium-grained sandstone with cross-beds and wave ripples in NT.  Flaggy to massive orthoquartzite with sandstone, some recessive siltstone + dolostone beds,+ with minor mud cracks, mudflake conglomerates + halite casts in QLD.|
16787|Shady Bore Quartzite|72527|4|Described|p1, 7, 8, 105, p112-118, p120, 132, 193|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin. 40-50 m thick.  Sampled from Mount Drummond sheet area. Previous geochron sample from Lawn Hill, Qld. See also p194.|1635+/-7 Ma max depositional age|McNamara Group||Conformably overlies Brumby Formation and conformably underlies Plain Creek Formation. Shown as laterally equivalent to Bullrush Conglomerate.|Mapped as massive white fine-grained well-sorted quartzite. Sample is a clean white medium-graned quartz sandstone with rare muscovite.|
16787|Shady Bore Quartzite|72912|5|Briefly described|p5 Fig.3, p33 Fig.12.|Statherian|Statherian|Shown as being located in both Queensland and Northern Territory, but older base in NT. Located in the Lawn Hill Platform of the Mount Isa Province, and the East part of the South Nicholson Basin.||McNamara Group||Overlies Brumby Formation (NT) and Lady Loretta Formation (Qld) and underlies Plain Creek Formation and is partially equivalent to Bullrush Conglomerate, Mount Les Siltstone and Walford Dolomite.|Includes sandstone.|
16787|Shady Bore Quartzite|72913|5|Briefly described|p7 Fig.2.|Paleoproterozoic|Paleoproterozoic|Shown as being in the eastern and Lawn Hill Platform part of the Isa Superbasin.||McNamara Group||Overlies Lady Loretta Formation and underlies Riversleigh Siltstone.|Includes quartzite, sandstone.|
16787|Shady Bore Quartzite|72919|6|Mentioned|p5|Paleoproterozoic|Paleoproterozoic|||McNamara Group||Underlain by Brumby Formation. Overlain by Plain Creek Formation. Equivalent to Bullrush Conglomerate.||
16787|Shady Bore Quartzite|73042|6|Mentioned|p4, p11|Paleoproterozoic|Paleoproterozoic|Mount Isa Province (Lawn Hill Platform) and South Nicholson Basin region, Isa Superbasin. Overlain by Plain Creek Formation.||McNamara Group||Unconformably underlain by Lady Loretta Formation and the Brumby Formation. Conformably overlain by the Riversleigh Siltstone.||
16787|Shady Bore Quartzite|73043|6|Mentioned|p15 Fig.8|Paleoproterozoic|Paleoproterozoic|||||||
16787|Shady Bore Quartzite|73144|6|Mentioned|p8-9|Statherian|Statherian|Isa Superbasin. Part of the River Supersequence. Overlies Lady Loretta Formation and overlain by Riversliegh Siltstone, but absent in Lawn Hill Platform area.||||||14-OCT-22
16787|Shady Bore Quartzite|73525|6|Mentioned|p4-5 Fig.2|||Mount Oxide-(Ardmore-May Downs) Domain.|||||Siliciclastics.|
16797|Shannon Formation|9199|5|Briefly described|Map legend|Cambrian|Cambrian|Of the Pertaoorrta Group.  Siltstone, shale, limestone, dolomite; fossiliferous.  Geological Province: Amadeus Basin.||||||04-NOV-04
16797|Shannon Formation|12891|5|Briefly described|p732|Middle Cambrian|Middle Cambrian|Geological province: Amadeus Basin. Lithology possibly analogous with Point Wakefield beds in Wiso Basin.||||||07-FEB-11
16797|Shannon Formation|22561|5|Briefly described|p21|Neoproterozoic|Neoproterozoic|In the Ooraminna Sub-basin.||||||30-NOV-06
16797|Shannon Formation|22566|5|Briefly described|p85|Late Cambrian|Middle Cambrian|Of the Pertaoorrta Group.  Informally divided into upper and lower Shannon Formation.||||||30-NOV-06
16797|Shannon Formation|22646|6|Mentioned|p 104|Cambrian|Cambrian|||||||
16797|Shannon Formation|22650|6|Mentioned|p 159|Cambrian|Cambrian|of the Pertaoorrta Group.||||||30-NOV-06
16797|Shannon Formation|22651|4|Described|p 186 - 187|Late Cambrian|Middle Cambrian|Of the Pertaoorrta Group.  Informally divided into upper and lower Shannon Formation p 171.||||||30-NOV-06
16797|Shannon Formation|22655|5|Briefly described|p 257|||||||||
16797|Shannon Formation|22656|5|Briefly described|p 281||Middle Cambrian|||||||
16797|Shannon Formation|22762|5|Briefly described|p369|Cambrian|Cambrian|Informally divided into upper and lower Shannon Formation.||||||30-NOV-06
16797|Shannon Formation|22804|6|Mentioned|Fig 2 on p432|Cambrian|Cambrian|Of the Pertaoorrta Group.||||||30-NOV-06
16797|Shannon Formation|22805|6|Mentioned|p464||Early Cambrian|||||||
16797|Shannon Formation|22826|4|Described|p572|Late Cambrian|Late Cambrian|||||||
16797|Shannon Formation|23361|5|Briefly described|16 Fig.4|Cambrian|Neoproterozoic III|||||||
16797|Shannon Formation|29721|6|Mentioned|Table 44|||||||||
16797|Shannon Formation|30258|6|Mentioned|Fig.2|||Part of Pertaoorta Group.||||||
16797|Shannon Formation|30544|6|Mentioned|p48|||Map legend||||||
16797|Shannon Formation|31572|6|Mentioned|Fig.|||Correlation chart. U.Camb.||||||
16797|Shannon Formation|33307|6|Mentioned|Fig.6|||||||||
16797|Shannon Formation|33761|6|Mentioned|p146|||Cambrian. Of the Pertaoorrta Formation.||||||30-NOV-06
16797|Shannon Formation|34111|5|Briefly described|Table 2|||Cambrian||||||
16797|Shannon Formation|34579|4|Described|Table 2|||Cambrian||||||
16797|Shannon Formation|35088|6|Mentioned|Fig.2|||||||||
16797|Shannon Formation|35102|6|Mentioned|Fig.2|||||||||
16797|Shannon Formation|35805|6|Mentioned|Fig.3|||||||||
16797|Shannon Formation|36198|6|Mentioned|p294|||See also Fig.III.2 and also p277.||||||30-NOV-06
16797|Shannon Formation|38606|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
16797|Shannon Formation|38885|6|Mentioned|Map legend|Late Cambrian|Late Cambrian|||||||
16797|Shannon Formation|39210|5|Briefly described|p38|||||||||
16797|Shannon Formation|39213|6|Mentioned|Fig.6|||Amadeus Basin Succession||||||
16797|Shannon Formation|39583|6|Mentioned|Map legend|Late Cambrian|Late Cambrian|||||||
16797|Shannon Formation|39931|6|Mentioned|Map legend|Cambrian|Cambrian|Of Pertaoorrta Group.||||||
16797|Shannon Formation|40254|6|Mentioned|Fig.7|||||||||
16797|Shannon Formation|40740|3|Fully described|p40|||Mention p5.||||||30-NOV-06
16797|Shannon Formation|40810|4|Described|p6|||||||||
16797|Shannon Formation|40906|6|Mentioned|Fig.11|||||||||
16797|Shannon Formation|40998|6|Mentioned|Fig.1|||||||||
16797|Shannon Formation|41018|6|Mentioned|Fig.2|||||||||
16797|Shannon Formation|41039|6|Mentioned|Fig.2|||||||||
16797|Shannon Formation|41115|6|Mentioned|Fig.2|||||||||
16797|Shannon Formation|41190|6|Mentioned|Fig.4|||||||||
16797|Shannon Formation|41224|6|Mentioned|Fig.2|||||||||
16797|Shannon Formation|41270|6|Mentioned|p274|||See also Table 1||||||
16797|Shannon Formation|41717|6|Mentioned|Fig.2|||||||||
16797|Shannon Formation|42059|6|Mentioned|Fig.2 P131|||||||||
16797|Shannon Formation|42060|6|Mentioned|p145|||||||||
16797|Shannon Formation|42082|6|Mentioned|Fig.3 P323|||||||||
16797|Shannon Formation|42354|5|Briefly described|Fig.4 P7|||||||||
16797|Shannon Formation|42504|5|Briefly described|p84|||In the Amadeus Basin.||||||30-NOV-06
16797|Shannon Formation|42886|5|Briefly described|Fig.1 P218|||||||||
16797|Shannon Formation|42940|5|Briefly described|Plate 12|||||||||
16797|Shannon Formation|43503|6|Mentioned|11-50|Mindyallan|Floran|||||||
16797|Shannon Formation|43646|6|Mentioned|Fig.3,p554||Middle Cambrian|||||||
16797|Shannon Formation|43781|6|Mentioned|p4||Late Cambrian|||||||
16797|Shannon Formation|43817|5|Briefly described|p61-63|||||||||
16797|Shannon Formation|44335|4|Described|p.11||Cambrian|Table 2. p.10.||||||
16797|Shannon Formation|44336|14|Not recorded|map legend||Cambrian|SG/53-3. Part of the Pertaoorrta Group.||||||30-NOV-06
16797|Shannon Formation|44433|14|Not recorded|map legend||Cambrian|||||||
16797|Shannon Formation|45041|4|Described|p57|||M-U Cambrian. Refers Wells et al. (1967)||||||
16797|Shannon Formation|45148|6|Mentioned|Fig.4|||In the Amadeus Basin.||||||30-NOV-06
16797|Shannon Formation|48890|2|Defined|p.40||Cambrian|See also Tables, Figs and Plates. Of the Pertaoorrta Group.||||||30-NOV-06
16797|Shannon Formation|48963|6|Mentioned|Fig.3|||||||||
16797|Shannon Formation|50246|5|Briefly described|p20 Fig. 2|Cambrian|Cambrian|Siltstone, shale, limestone and dolostone, well-interbedded, fossiliferous and stromatolitic.||||||07-FEB-11
16797|Shannon Formation|60547|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Pertaoorrta Group. Siltstone, shale, limestone, dolomite; fossiliferous. Geological Province: Amadeus Basin.||||||03-JUN-05
16797|Shannon Formation|61732|5|Briefly described|p99|Cambrian|Cambrian|Together with other Cambrian units overlies the Arumbera Sandstone.||||||07-FEB-11
16797|Shannon Formation|62376|5|Briefly described|p18|Late Cambrian|Middle Cambrian|Of the Pertaoorrta Group. Geological Province: Amadeus Basin.||||||09-FEB-10
16797|Shannon Formation|62379|5|Briefly described|p7 Fig. 2, p15|Late Cambrian|Middle Cambrian|Of the Pertaoorrta Group. Geological Province: Amadeus Basin. Siltstone, limestone, dolostone.||||||
16797|Shannon Formation|62595|5|Briefly described|p29 Fig.6.|Cambrian|Cambrian|Ross River area.|||||Siltstone, shale, limestone and dolostone, well interbedded, fossiliferous and stromatolitic.|
16797|Shannon Formation|63562|6|Mentioned|p338 fig 3,p346 fig 8, p348,p352 fig 10|Late Cambrian|Middle Cambrian|Of Amadeus Basin.||||Overlies Giles Creek Dolomite. Correlated with Arrinthrunga Formation. Is overlain by Goyder Formation.||
16797|Shannon Formation|64068|6|Mentioned|p65,67, 69, 70, 225|||Amadeus Basin. In part correlated with Steamboat Sandstone, Selwyn Range Limestone. Upper part correlated with Chabalowe Formation, Arrinthrunga Formation, Georgina Limestone.||||||
16797|Shannon Formation|64625|5|Briefly described|p244-245, p251|Cambrian|Cambrian|Amadeus Basin||||Overlies Giles Creek Dolomite|Siltstone, limestone and dolostone.|
16797|Shannon Formation|64778|6|Mentioned|p13|Cambrian|Cambrian|Amadeus Basin.||||||
16797|Shannon Formation|64809|5|Briefly described|p2, p3 Fig.2, p15 Fig.15 |Late Cambrian|Middle Cambrian|||Unit in Pertaoorrta Group.|||Siltstone, shale, limestone.|
16797|Shannon Formation|65233|3|Fully described|p3 Fig. 2, p8|Late Cambrian|Middle Cambrian|Of Pertaoorrta Gp. Conformable on/gradational with Giles Creek Dolostone. Max.thick: >700m, thinning to N and W. Geol.prov: Amadeus Basin. Lower part is silty shale with siltstone/dolostone thin interbeds; upper part is carbonate-rich - more lith. incl.||||||07-FEB-11
16797|Shannon Formation|65342|6|Mentioned|p4.|||Amadeus Basin. Max. thickness at least 400 m.||||Overlies Hugh River Shale. Is overlain by Goyder Formation.||
16797|Shannon Formation|65489|5|Briefly described|p125|Cambrian|Cambrian|Amadeus Basin.||Unit in Pertaoorrta Group.||Is overlain by Goyder Formation.||
16797|Shannon Formation|67326|5|Briefly described|p2, p4|Late Cambrian|Middle Cambrian|Amadeus Basin.||Pertaoorrta Group.||Overlies Giles Creek Dolostone. Is overlain by Jay Creek Limestone and Goyder Formation. Equivalent to Petermann Sandstone.||
16797|Shannon Formation|67565|6|Mentioned|p40.|||Eastern Amadeus Basin. The lower part is correlated with Illara Sandstone in the Gardiner Range.||||||
16797|Shannon Formation|67856|6|Mentioned|p338 fig 4-30|Cambrian|Cambrian|||Of Pertaoorta Group.||||
16797|Shannon Formation|68323|6|Mentioned|p4 Fig.2|Late Cambrian|Middle Cambrian|Amadeus Basin.||Pertaoorrta Group.||||
16797|Shannon Formation|69437|5|Briefly described|p22:10|Series 3|Series 3|Amadeus Basin.||||Overlies Giles Creek Dolostone. Is overlain by Goyder Formation.||12-JUL-16
16797|Shannon Formation|69438|4|Described|p23:2-3, 8, 24-25, 28, 30-32, 43, 59|Late Cambrian|Middle Cambrian|Wells et al. (1967). Amadeus Basin. Over 700m thick, thinning to the N and W. Hydrocarbon source rock intervals may be present.||Pertaoorrta Group.||Para/disconformably overlies Giles Creek Dolostone. Is overlain conformably by Goyder Formation. Equivalent to Illara Sandstone and upper Hugh River Shale. Flanks the Jay Creek Limestone.|Lower part is 270m of silty shale with interbeds of thin siltstone and dolostone; upper part is ribboned carbonate and mudstone, grainstone and thrombolites, stromatolites and evaporites.|12-JUL-16
16797|Shannon Formation|69449|6|Mentioned|p34:2 Fig.34.2|Cambrian|Cambrian|Eastern Amadeus Basin.||||||12-JUL-16
16797|Shannon Formation|69673|5|Briefly described|p64 fig 53, p66, p80, p81, p102, p103|Cambrian|Cambrian|Potential source rock and potential for unconventional petroleum. Greater than 700m thick.||||Disconformably overlies Giles Creek Dolostone, conformably overlain by lower Goyder Formation, correlated with Arrinthrunga Formation|Silty shale with interbeds of thin siltstone and dolostone.|
16797|Shannon Formation|70752|5|Briefly described|p126 Fig.1|Cambrian|Cambrian|||Pertaoorrta Group.|||Siltstone and shale; fossiliferous and stromatolitic limestone and dolostone.|
16797|Shannon Formation|71114|4|Described|p171, p170 fig 1b, p172-4, p176-180|Guzhangian||Amadeus Basin. Deposited between ~511 and 490 Ma, in the intertidal to subtidal zone on a carbonate platform/shelf under intermittent evaporitic conditions. 391m thick in Dingo 1 well.||||Overlies Hugh River Shale. Is overlain by Goyder Formation or Jay Creek Limestone. Upper part equivalent to Jay Creek Limestone.|Characterised by oolitic, stromatolitic limestones. Lower part is dominated by silty shale with dolostone interbeds. Upper part transgresses into a carbonate-rich succession during sea level rise.|14-FEB-18
16797|Shannon Formation|71279|5|Briefly described|p355 Fig.2, p363, p382 Tb.1|Late Cambrian|Middle Cambrian|Amadeus Basin. Modelled magnetic properties.||Pertaoorrta Group.||||
16797|Shannon Formation|71800|6|Mentioned|p26 fig 3|Late Cambrian|Middle Cambrian|Amadeus Basin.||||Overlies the Giles Creek Dolomite. Overlain by the Goyder Formation.||
16797|Shannon Formation|72358|5|Briefly described|p117-119,121, 123, 126|Series 3|Series 3|Of Amadeus Basin. Deposited in the supratidal to subtidal zone on carbonate platform/shelf with intermittent evaporitic conditions (Kennard, 1994; Schmid, 2017). The upper section is sometimes (incorrectly?) referred to as Jay Creek Limestone, but referred to this study as Jay Creek Limestone equivalent. Contains evidence of microbial communities included Girvanella (calcareous green algae) at Ross River (Kennard, 1994).||||Overlain by the Goyder Formation. Correlable to Petermann Sandstone.|Oolitic and stromatolitic limestones.|10-JAN-20
16797|Shannon Formation|72489|5|Briefly described|p3, p4, p5, p7 Fig.6, p8, p9,p12|Late Cambrian|Late Cambrian|Located in the Amadeus Basin. Age bracketted between ca. 502 to 497 Ma through correlation.||||Upper part correlated with Jay Creek Limestone.|Stromatolitic  and oolitic limestones.|
16797|Shannon Formation|72516|6|Mentioned|p92, 93|Cambrian|Cambrian|Amadeus Basin.||||Equivalent to the Steamboat Sandstone. Upper part equivalent to Arrinthrunga Formation.||08-JUN-21
16797|Shannon Formation|72570|6|Mentioned|p8|Cambrian|Cambrian|Amadeus Basin.||||||
16797|Shannon Formation|73085|6|Mentioned|p1|late Cambrian|middle Cambrian|||Pertaoorrta Group [and equivalents?]||Underlain by Giles Creek Dolostone. Overlain by lower Goyder Formation. Partly equivalent to Jay Creek Limestone and Hugh River Shale.||
16839|Shoal Reach Formation|14019|5|Briefly described|p4 Fig. 3|||Of the Auvergne Group.  Geological Province: Victoria Basin.||||||
16839|Shoal Reach Formation|24122|5|Briefly described|p4 Fig.3|||Of Auvergne Group.  Geological Province: Victoria Basin.||||||
16839|Shoal Reach Formation|24297|5|Briefly described|p4 Fig.3, p21|||Of Auvergne Group.  Geological Province: Victoria Basin.||||||
16839|Shoal Reach Formation|24441|5|Briefly described|p1 Fig. 1|Mesoproterozoic|Mesoproterozoic|Of Auvergne Group. Overlies Spencer Creek Formation. Geological Province: Victoria Basin.||||||
16839|Shoal Reach Formation|24442|5|Briefly described|p50 Fig. 1|||Of the Auvergne Group.  Geological Province: Victoria Basin.||||||
16839|Shoal Reach Formation|32170|6|Mentioned|Map legend|Adelaidean|Carpentarian|Adelaidean or Carpentarian||||||
16839|Shoal Reach Formation|32307|6|Mentioned|p10|||Proterozoic||||||
16839|Shoal Reach Formation|32310|6|Mentioned|Map legend|Adelaidean|Carpentarian|Adelaidean/Carpentarian||||||
16839|Shoal Reach Formation|32660|5|Briefly described|Table 6|||||||||
16839|Shoal Reach Formation|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Auvergne Group.  Dolomite, sandy and silty; minor siltstone and intraformational breccia.||||||02-DEC-04
16839|Shoal Reach Formation|32700|4|Described|Table 1|||Lithology p14. Refers Randal (1962)||||||30-NOV-06
16839|Shoal Reach Formation|32701|4|Described|Table 1|||Auvergne Group. See p9.||||||30-NOV-06
16839|Shoal Reach Formation|32728|6|Mentioned|Fig.14|||||||||
16839|Shoal Reach Formation|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
16839|Shoal Reach Formation|45112|4|Described|Table 15|||||||||
16839|Shoal Reach Formation|48938|2|Defined|p52|Proterozoic|Proterozoic|Measured section p98.||||||30-NOV-06
16839|Shoal Reach Formation|48942|3|Fully described|p71|||||||||
16839|Shoal Reach Formation|60006|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Victoria Basin. Of Auvergne Group. Overlies Spencer Sandstone. Unconformably overlain by Bullo River Sandstone, Black Point Sandstone Member and Moonlight Valley Tillite.||||||21-JUL-04
16839|Shoal Reach Formation|60682|4|Described|p9 Table 2, 13|Cryogenian|Cryogenian|Of Auvergne Group. Conformably overlies Spencer Sandstone. Unconformably overlain by Bullo River Sandstone. Max. thickness: <110m.  Dolostone, dololutite, dolarenite, dolostone, sandstone, minor siltstone and shale. Geological Province: Victoria Basin.||||||30-NOV-06
16839|Shoal Reach Formation|60685|5|Briefly described|p4 Fig. 3, p2|Mesoproterozoic|Mesoproterozoic|Of the Auvergne Group. Overlain by the former Bardia Chert Member, which is now remapped as silcrete/duricrust. Geological Province: Victoria Basin.||||||17-JUN-13
16839|Shoal Reach Formation|65331|5|Briefly described|Map legend|Neoproterozoic |Neoproterozoic|Of Auvergne Group, Victoria Basin.  Dolostone, sandstone, minor siltstone, and shale||||||
16839|Shoal Reach Formation|65342|6|Mentioned|p11 Fig.13. |||Victoria Basin.||Unit in Auvergne Group.||Overlies Spencer Sandstone.||
16839|Shoal Reach Formation|68733|5|Briefly described|p177 Fig.2, p183, p189 Fig.8|Cryogenian|Cryogenian|Victoria Basin.||Of the Auvergne Group.||Unconformably overlain by the Black Point Sandstone Member (Bullo River Sandstone).||06-DEC-17
16839|Shoal Reach Formation|69437|5|Briefly described|p22:4-5|Cryogenian|Cryogenian|Victoria/Wolfe Basins, Centralian A Superbasin. Supersequence 1.||||Overlies Spencer Sandstone.||12-JUL-16
16839|Shoal Reach Formation|69441|5|Briefly described|p26:2-3, 5|Neoproterozoic|Neoproterozoic|Thickness <100m, thins to NE. Poorly exposed. Mixed carbonate/siliciclastic platform.||Auvergne Group.||Conformably (gradationally) overlies Spencer Sandstone.|Quartzose and silty dolostone, dololutite, dolarenite, dolostone, sandstone; minor siltstone and shale; local intraformational conglomerate.|12-JUL-16
16839|Shoal Reach Formation|69442|6|Mentioned|p27:1, 3 Tb.27.1|||||Auvergne Group.||Is overlain by Bullo River Sandstone, mostly dis/unconformably but gradationally at one location.||12-JUL-16
16839|Shoal Reach Formation|69673|5|Briefly described|p188|||100m thick.||Auvergne Group|||Quartzic and silty dolostone, dololutite, dolarenite, siltstone sandstone and intraformational conglomerate.|
16839|Shoal Reach Formation|70206|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Victoria Basin.||Auvergne Group|||Silty and quartzic dolostone, dolostone, sandstone, minor siltstone and shale.|
16839|Shoal Reach Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||dolostone|
16839|Shoal Reach Formation|71302|5|Briefly described|p6|Neoproterozoic|Neoproterozoic|Of Victoria Basin.||Unit of Auvergne Group.||Overlain unconformably by Black Point Sandstone Member. Underlain by Spencer Sandstone.||
16942|Sir Frederick Conglomerate|22716|6|Mentioned|table4,p231|Proterozoic|Proterozoic|||||||
16942|Sir Frederick Conglomerate|22804|6|Mentioned|Fig 2 on p432|Neoproterozoic|Neoproterozoic|||||||
16942|Sir Frederick Conglomerate|22826|6|Mentioned|Fig 2 on p565|Neoproterozoic|Neoproterozoic|||||||
16942|Sir Frederick Conglomerate|24301|5|Briefly described|p17|||Geological Province: Amadeus Basin||||||
16942|Sir Frederick Conglomerate|33588|6|Mentioned|p6|||||||||
16942|Sir Frederick Conglomerate|34442|6|Mentioned|p7|||See also P8. Proterozoic. Equiv. Pertatataka Formation||||||
16942|Sir Frederick Conglomerate|35102|6|Mentioned|Fig.2|||||||||
16942|Sir Frederick Conglomerate|36551|6|Mentioned|Table 13|||||||||
16942|Sir Frederick Conglomerate|36887|5|Briefly described|p211|||||||||
16942|Sir Frederick Conglomerate|37928|6|Mentioned|Fig.4|||||||||
16942|Sir Frederick Conglomerate|39210|6|Mentioned|Fig.10|||||||||
16942|Sir Frederick Conglomerate|40740|6|Mentioned|p1|||||||||
16942|Sir Frederick Conglomerate|41852|6|Mentioned|p209|||||||||
16942|Sir Frederick Conglomerate|42940|5|Briefly described|Plate 2|Neoproterozoic|Neoproterozoic|Written as Sir Fred. Cong.  Conglomerate, sandstone.  Geological province: Amadeus Basin.||||||17-JUL-13
16942|Sir Frederick Conglomerate|43503|6|Mentioned|50|||||||||
16942|Sir Frederick Conglomerate|44109|5|Briefly described|p164|||Thick, poorly sorted conglomerate and boulder lenses, with clasts up 1m across. Geological Province: Amadeus Basin.||||||
16942|Sir Frederick Conglomerate|44439|2|Defined|p.7,8, Tb.1, map|Cambrian|Neoproterozoic|U.Prot.-Cambrian. Age unclear. Lateral equiv.to Ellis Sandstone. Probably equiv.to Mt. Currie Conglomerate in NT (G52-1) (G52-2).||||||30-NOV-06
16942|Sir Frederick Conglomerate|44440|14|Not recorded|map legend|Cambrian|Neoproterozoic|Upper Proterozoic-Cambrian.||||||
16942|Sir Frederick Conglomerate|44499|14|Not recorded|opp.p.6, Tb.1|Early Paleozoic|Proterozoic|Proterozoic to Lower Palaeozoic.||||||07-NOV-08
16942|Sir Frederick Conglomerate|45041|4|Described|p39|||Proterozoic. Equiv. Winnall Beds||||||
16942|Sir Frederick Conglomerate|48842|2|Defined|p15-16|Early Paleozoic|Neoproterozoic|p.8,17,18,21,27,32,Pl.5,7,8. Tb.I. Conformably overlain by Maurice Formation; lenses into Ellis Sandstone. Sequence of pebble, cobble and boulder conglomerate with kaolinitic sandstone matrix and thin beds and lenses of sandstone and pebbly sandstone.||||||07-NOV-08
16942|Sir Frederick Conglomerate|48864|14|Not recorded|Tb.1.,p.10,Pl.10||Cambrian|(G52-2).||||||
16942|Sir Frederick Conglomerate|48963|6|Mentioned|Fig.2|||||||||
16942|Sir Frederick Conglomerate|62376|5|Briefly described|p18|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin.||||||09-FEB-10
16942|Sir Frederick Conglomerate|62379|5|Briefly described|p7 Fig. 2|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin.||||||
16942|Sir Frederick Conglomerate|62609|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Conglomerate, some sandstone. Underlies: Maurice Formation. Overlies: Carnegie Formation.||||||14-AUG-06
16942|Sir Frederick Conglomerate|62620|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Conglomerate, some sandstone.||||||
16942|Sir Frederick Conglomerate|64809|6|Mentioned|p3 Fig.2 |Proterozoic|Proterozoic|||||||
16942|Sir Frederick Conglomerate|65102|6|Mentioned|p363, Figure 4-38|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
16942|Sir Frederick Conglomerate|65233|5|Briefly described|p3 Fig. 2|Neoproterozoic|Neoproterozoic|Geological province: Amadeus Basin.||||||07-FEB-11
16942|Sir Frederick Conglomerate|65256|6|Mentioned|p19|||Stratigraphic correlative of the Winnall beds.||||||
16942|Sir Frederick Conglomerate|67326|5|Briefly described|p2|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||Is overlain by Maurice Formation.||
16942|Sir Frederick Conglomerate|67856|4|Described|p340 tab 4-8, p338, 337, 339, 344, 345|Neoproterozoic|Neoproterozoic|Of Wells et al., 1964, 1970. ~1200m thick. Type sction: Gillespie Hills 24o16'S, 124o42'E.||||Conformably overlain by Maurice Formation. Interfingers with and equivalent to Ellis Sandstone, also equivalent to Winnall beds. Unconformably overlies Carnegie Formation.|Piedmont conglomerate. Boulder, cobble and pebble conglomerate; sandstone lenses, quartz phenoclasts of silicified sandstone; metaquartzite and mica schist.|
16942|Sir Frederick Conglomerate|68270|5|Briefly described|p683|Ediacaran|Ediacaran|Amadeus Basin. Appears as Sir Fred Conglomerate on p683.||||Overlain by Mount Currie Conglomerate. Underlain by Boord Formation.||03-JUL-19
16942|Sir Frederick Conglomerate|68323|6|Mentioned|p4 Fig.2|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
16942|Sir Frederick Conglomerate|69003|6|Mentioned|p60|Cambrian|Cambrian|W Amadeus Basin.||||||
16942|Sir Frederick Conglomerate|69031|5|Briefly described|p4, p9|||Amadeus Basin. Deposited during the c.580-530 Ma Petermann Orogeny.||||Overlies Carnegie Formation. Is overlain by Maurice Formation.||
16942|Sir Frederick Conglomerate|69438|5|Briefly described|p23:2, 18, 20-21, 23|Early Cambrian|Ediacaran|Amadeus Basin.||Pertaoorrta Group.||Overlies Carnegie Formation. Interfingers with Ellis Sandstone and is a correlative of (in part) Winnall beds. Is overlain by Maurice Formation.||12-JUL-16
16942|Sir Frederick Conglomerate|69606|5|Briefly described|p4 fig 2|Cambrian|Cambrian|Deposited during the Petermann Orogeny. Potential reservoir rock. Amadeus Basin.||||Overlies the Carnegie Formation, overlain by the Maurice Formation.|Sandstone and conglomerate.|
16942|Sir Frederick Conglomerate|69673|6|Mentioned|p64 fig 53|||||||Overlies Carnegie Formation, overlain by Maurice Formation||
16942|Sir Frederick Conglomerate|70416|6|Mentioned|p65 Fig.2|Early Cambrian|Early Cambrian|Amadeus Basin. Obsolete.||||||
16942|Sir Frederick Conglomerate|70793|4|Described|500k_interpgeop14_lut.csv|Series 2|Ediacaran|Of Amadeus Basin (Phase 1), Centralian Superbasin. Events: Areyonga Movement; Delamarian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma).|635-509 Ma (inferred)||||Cobble to boulder conglomerate; lesser interbedded sandstone.|
16942|Sir Frederick Conglomerate|70826|6|Mentioned|p5 tbl 2|||Supersequence 4, Centralian Superbasin.||||||20-APR-20
16942|Sir Frederick Conglomerate|70839|4|Described|p329-333,335,337-340,345|Ediacaran|Ediacaran|Of Amadeus Basin. Part of Supersequence 4. Restricted to local depocentres, reaching estimated thicknesses of up to 2000m. SHRIMP U-Pb zircon geochronology samples and analysis on p331-334. Concordant dates range between c. 1.06 and c. 2.7 Ga; two zircons older than c. 1.92 Ga. Dominant age component between c. 1.32 and c. 1.05 Ga, with minor components at c. 1.47, 1.57 and 1.76 Ga.|Max dep age: 1059+\-57 Ma (207Pb/206Pb)|||Overlain by Maurice Formation. Underlain by Carnegie Formation. Equivalent to Ellis Sandstone. Correlable to unit 2 of the Winnall beds.|Cobble and boulder conglomerate; clasts include quartzite, sandstone, and metasandstone lithologies.|
16942|Sir Frederick Conglomerate|71080|5|Briefly described|p30 fig 21|Cambrian||Amadeus Basin in WA. Supersequence 4.|||||Dominantly sandstone, some conglomerate.|
16942|Sir Frederick Conglomerate|71088|4|Described|p1-p2, p7-p8, p15, p17-p21, p24, p33|Neoproterozoic|Neoproterozoic|Restricted to the southern half of the Amadeus Basin. Reassigned to Supersequence 4. Potentially equivalent to the Ellis Sandstone. Correlated with the Pertatataka Formation by Wells et al., 1970; Grey, 1990 and Lindsay and Korsch., 1991. The dominant clasts of this unit are derived from the Dean Quartzite, Kulail Sandstone and Dixon Range beds.||||Overlain by the Maurice Formation. Unconformably overlain by the Mu Formation. Overlies the Carnegie Formation. Equivalent to the Winnall beds.|Clast-supported cobble to boulder conglomerate with well rounded clasts consisting of quartzite, sandstone and metasandstone.|
16942|Sir Frederick Conglomerate|71114|5|Briefly described|p170 fig 1b|Terreneuvian|Ediacaran|Appears (for reasons of space) as Sir Fred Cgl. SW Amadeus Basin.||||Shown as lateral equivalent to Ellis Sandstone, Mount Currie Conglomerate.||14-FEB-18
16942|Sir Frederick Conglomerate|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, conglomerate|
16942|Sir Frederick Conglomerate|71268|4|Described|GEOL_LUT_CSV files|Series 2|Ediacaran|Of Amadeus Basin (Phase 1), Centralian Superbasin. Events: Delamarian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma). See 1m_geologyp12_lut.csv, 500k_interpgeop16_lut.csv.|635-510 Ma (inferred)||||Sequence of pebble, cobble and boulder conglomerate with kaolinitic sandstone matrix and thin beds and lenses of sandstone and pebbly sandstone.|
16942|Sir Frederick Conglomerate|71279|5|Briefly described|p355 Fig.2|Early Cambrian|Ediacaran|Amadeus Basin.||Pertaoorrta Group.||||
16942|Sir Frederick Conglomerate|71800|5|Briefly described|p26-p27|Ediacaran|Ediacaran|Amadeus Basin.||||Overlies the Carnegie Formation. Overlain by the Maurice Formation.|Lithic sandstone.|
16942|Sir Frederick Conglomerate|71810|5|Briefly described|Map legend.|Cambrian|Ediacaran|Amadeus Basin (Phase 1), Centralian Superbasin.|||||Cobble to boulder conglomerate with predominantly sedimentary clasts and friable, sandy matrix; interbedded unit of red-brown, poorly sorted lithic sandstone in Mu Hills (inferred to have been deposited during the Petermann Orogeny).|
16942|Sir Frederick Conglomerate|71841|5|Briefly described|p1|Early Cambrian|Ediacaran|Of Amadeus Basin.||Unit of Pertaoorrta Group.||Overlain by Maurice Formation. Underlain by Carnegie Formation. Grades into Ellis Sandstone.||
16942|Sir Frederick Conglomerate|71842|5|Briefly described|p2-3, p9|Early Cambrian|Ediacaran|Of Amadeus Basin. Nomenclature after Haines and Allen 2010 (Western Amadeus, WA).||Unit of Pertaoorrta Group.||Overlain by Maurice Formation. Underlain by Carnegie Formation. Grades into Ellis Sandstone. Correlable to Arumbera Sandstone or Winnall beds.||08-JAN-20
16942|Sir Frederick Conglomerate|72034|5|Briefly described|500k_interpgeop16_lut|Series 2|Ediacaran|Amadeus Basin (Phase 1).|||||Cobble to boulder conglomerate; lesser interbedded sandstone.|
16942|Sir Frederick Conglomerate|72358|6|Mentioned|p118|Series 1|Ediacaran|Of Amadeus Basin.||||||
16978|Skull Creek Formation|14019|5|Briefly described|p4 Fig. 3|||Of the Bullita Group.  Geological Province: Victoria Basin.||||||
16978|Skull Creek Formation|24122|3|Fully described|p4, p5 Tb.1|Proterozoic|Proterozoic|Of Bullita Group. Includes Supplejack Dolostone Member. Conformably overlain by Bynoe Formation and conformably overlies Timber Creek Formation. Maximum thickness: >220m.  Geological Province: Victoria Basin.||||||
16978|Skull Creek Formation|24297|3|Fully described|p10|Proterozoic|Proterozoic|Of Bullita Group.  Conformably overlain by Bynoe Formation, conformably overlies Timber Creek Formation. Maximum thickness: 229m.   Geol. Prov: Victoria Basin.  See also p5 Tb. 2.||||||
16978|Skull Creek Formation|24298|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Bullita Group. Silty and quartzic dolostone, dolostone, dolomitic sandstone, dolomitic siltstone, sandstone, minor dolarenite.||||||30-NOV-06
16978|Skull Creek Formation|24300|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Bullita Group.   Geological Province: Victoria Basin||||||30-NOV-06
16978|Skull Creek Formation|24441|4|Described|p1 Fig. 1, p7, Appendix 2-1:5|Mesoproterozoic|Mesoproterozoic|Of Bullita Gp. Interbedded fine to medium sst, dolarenite, microbial dolostone and minor dololutite...... . Overlies Timber Creek Fm; overlain by Nero Sltst. Thickness: 229m.  Geol.Prov: Victoria Basin.||||||25-JAN-06
16978|Skull Creek Formation|24442|5|Briefly described|p50 Fig. 1|||Of the Bullita Group. Geological Province: Victoria Basin.||||||
16978|Skull Creek Formation|28255|3|Fully described|p45-46, Tb. 11 (opp. p8)|Adelaidean|Adelaidean|Of Bullita Gp. Supersedes "Skull Creek Limestone". Dolomite and dolomitic siltstone. Contains Bardia Chert and Supplejack Dolomite Mbrs. Conformably overlies Timber Cr.Fm; underlies Bynoe Fm. Max. thickness: 165m. See also p132-134 Appendix.||||||15-JUN-05
16978|Skull Creek Formation|30003|4|Described|p7, p12|||Of the Bullita Group. Overlies the Timber Creek Formation. Carpentarian or Adelaidean. Max. thickness: >50m.||||||19-APR-05
16978|Skull Creek Formation|30004|6|Mentioned|Map legend|Proterozoic|Proterozoic|Carpentarian or Adelaidean||||||
16978|Skull Creek Formation|32170|6|Mentioned|Map legend|Adelaidean|Carpentarian|Adelaidean or Carpentarian||||||
16978|Skull Creek Formation|32175|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Bullita Group.  Contains the Bardia Chert and Supplejack Dolomite Members.  Massive and blocky grey fine and medium crystalline dolomite; minor dolomitic siltstone and sandstone, chert.||||||02-DEC-04
16978|Skull Creek Formation|32660|5|Briefly described|Table 6|||||||||
16978|Skull Creek Formation|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Bullita Group.  Dolomite, dolmitic siltstone, silty dolomite, chert, minor sandstone.||||||08-AUG-05
16978|Skull Creek Formation|32700|5|Briefly described|Table 1|||See also p13. Of the Bullita Group.||||||30-NOV-06
16978|Skull Creek Formation|32701|4|Described|Table 1|||Adelaidean. Of the Bullita Gp.||||||30-NOV-06
16978|Skull Creek Formation|32775|5|Briefly described|Map legend|Adelaidean|Adelaidean|Includes the Bardia Chert and Supplejack Dolomite Members.||||||02-DEC-04
16978|Skull Creek Formation|33373|3|Fully described|p9|||On Table 2.||||||
16978|Skull Creek Formation|33375|6|Mentioned|p8 Tb. 1, p12|Adelaidean|Adelaidean|Of the Bullita Group. Interbedded dolomite and dolomitic siltstone; minor sandstone and chert, stromatolites in upper part. Max. thickness: 165m.||||||28-APR-05
16978|Skull Creek Formation|33377|6|Mentioned|p266|||||||||
16978|Skull Creek Formation|33378|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Bullita Group. Includes the Bardia Chert Member and Supplejack Dolomite Member.  Interbedded dolomite and dolomitic siltstone; minor sandstone and chert.||||||27-APR-05
16978|Skull Creek Formation|38243|6|Mentioned|p355|||||||||
16978|Skull Creek Formation|45112|6|Mentioned|Table 10|||||||||
16978|Skull Creek Formation|48938|2|Defined|p27|Adelaidean|Adelaidean|||||||
16978|Skull Creek Formation|48942|3|Fully described|p47|||Strat. section p110.||||||30-NOV-06
16978|Skull Creek Formation|48943|2|Defined|p55|Adelaidean|Adelaidean|Strat. section pp134,135.||||||30-NOV-06
16978|Skull Creek Formation|60006|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Victoria Basin. Of Bullita Group. Silty and quartzic dolostone, dolomitic sandstone, dolostone, dolarenite||||||
16978|Skull Creek Formation|60672|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Silty and quartzic dolostone, dolomitic sandstone, quartz sandstone, dolostone. Overlies Timber Creek Formation. Overlain unconformably by Antrim Plateau Volcanics. Of Bullita Group. Geological Province: Victoria Basin.||||||30-NOV-06
16978|Skull Creek Formation|60682|4|Described|piii, 8|Mesoproterozoic|Mesoproterozoic|Of Bullita Group. Gradationally overlies Timber Creek Formation. Unconformably overlain by Jasper Gorge Sandstone. Thickness: >100m. Geological Province: Victoria Basin. Dololutite, sandstone, dolomitic fine grained sandstone, dolarenite, dolostone.||||||30-NOV-06
16978|Skull Creek Formation|60685|4|Described|pp4 Fig. 3, p1|Mesoproterozoic|Mesoproterozoic|Of the Bullita Group. Sandstone, dolarenite, stromatolitic dolostone. Conformable on Timber Creek Formation; conformable below Bynoe Formation. Max. Thickness: 229m.  Geological Province: Victoria Basin.||||||19-MAY-05
16978|Skull Creek Formation|65331|5|Briefly described|Map legend|Mesoproterozic|Mesoproterozic|Of Bullita Group, Victoria Basin.  Includes Supplejack Dolostone Member. Silty and quartzic dolostone, dolomitic sandstone, dolostone, dolarenite||||||
16978|Skull Creek Formation|65342|6|Mentioned|p11 Fig.13. |||Victoria Basin.||Unit in Bullita Group.||Overlies Timber Creek Formation. Is overlain by Nero Siltstone and Bynoe Formation.||
16978|Skull Creek Formation|67151|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Birindudu Basin.||Unit in Bullita Group.|Includes Supplejack Dolostone Member.|Overlies Timber Creek Formation. Is overlain by Bynoe Formation.|Silty and quartzic dolostone, dolomitic sandstone, sandstone, dolostone.|
16978|Skull Creek Formation|68733|6|Mentioned|p177 Fig.2, p179 Tb.1, p184-186|||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.||||06-DEC-17
16978|Skull Creek Formation|69432|4|Described|p17:2, 10-11, 14-15|||Birrindudu Basin. 160-230m thick. Commonly contains pinolitic prisms of diagenetic siderite, and edgewise plate and flake breccias. Has local weak malachite mineralisation and visible galena, copper and manganese mineralisation. Minor barite occurs in carbonate rocks. Contains biologically degraded bitumen and pyrobitumen.||Bullita Group.|Supplejack Dolostone Member.||Interbedded fine to medium sandstone and dolarenite, biostromal dolostone and minor dolomitic siltstone, oolitic grainstone, dolorudite and chert. Sandstone is more prevalent in the lower parts; carbonate content increases up-section.|12-JUL-16
16978|Skull Creek Formation|69441|5|Briefly described|p26:3 Tb. 26.1|||Birrindudu Basin.||Bullita Group.||Is overlain unconformably by Jasper Gorge Sandstone (Auvergne Group).||12-JUL-16
16978|Skull Creek Formation|69673|6|Mentioned|p48 fig 35, p50|||||Bullita Group||Overlies Timber Creek Formation, overlain by Nero Siltstone, Bynoe Formation||
16978|Skull Creek Formation|70206|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Birindudu Basin [misspelling of Birrindudu Basin].||Bullita Group|Includes Supplejack Dolostone Member.||Silty and quartzic dolostone, dolostone, dolomitic sandstone, dolomitic siltstone, sandstone and minor dolarenite.|18-JUL-16
16978|Skull Creek Formation|70655|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Birindudu Basin.||Bullita Group.|Includes Supplejack Dolostone Member.|Overlies Timber Creek Formation. Is overlain by Bynoe Formation.|Silty and quartzic dolostone, dolomitic sandstone, sandstone, dolostone.|
16978|Skull Creek Formation|70850|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Bullita Group.|Supplejack Dolostone Member.|Conformably overlies Timber Creek Formation. Is overlain conformably by Bynoe Formation.|Silty and quartzic dolostone, dolostone, dolomitic sandstone, dolomitic siltstone, sandstone, minor dolarenite.|
16978|Skull Creek Formation|70854|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Bullita Group.||Overlies Timber Creek Formation. Is overlain by Nero Siltstone and the Antrim Plateau Volcanics.|Silty and quartzic dolostone, dolomitic sandstone, quartz sandstone, dolostone.|21-SEP-17
16978|Skull Creek Formation|70855|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Bullita Group.|Supplejack Dolostone Member.|Overlies Timber Creek Formation. Is overlain by Bynoe Formation, and unconformably by Jasper Gorge Sandstone.|Silty and quartzic dolostone, dolostone, dolomitic sandstone, dolomitic siltstone, sandstone, minor dolarenite.|
16978|Skull Creek Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, dolostone|
16978|Skull Creek Formation|71302|4|Described|p1,6-7,28-34,72,74||Paleoproterozoic|Of Birindudu Basin. Widely distributed, defined by Sweet et al. (1974a, b) and best exposed in central and western VICTORIA RIVER DOWNS 1: 250 000 mapsheet (Beier et al., 2002; Dunster and Ahmad, 2013a). Ranges in thickness between 160-230m. Likely deposited mostly in high-energy marine conditions but with intermittent evaporitic depositional conditions that included subaerial exposure and minor open-water settings (Dunster and Ahmad, 2013a). Sample GA 1957129 (dolomitic sandstone) yielded an interpreted (weighted mean 207Pb/206Pb) maximum depositional age of 1609+\-8 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 and SHRIMP analyses are discussed.||Unit of Bullita Group.|||Interbedded, fine- to medium-grained sandstone and dolarenite, biostromal dolostone and minor dolomitic siltstone, oolitic grainstone, dolorudite and chert.|09-DEC-19
16978|Skull Creek Formation|72718|6|Mentioned|p7|||Birrindudu Basin.||Bullita Group||Underlain by Timber Creek Formation. Overlain by Nero Siltstone and Bynoe Formation.||
16999|Sliding Rock Metamorphics|9199|5|Briefly described|Map legend|||Hornblende gneiss, garnet-amphibolite gneiss, felsic gneiss.  Geological Province: Arunta Block.||||||30-NOV-06
16999|Sliding Rock Metamorphics|39552|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
16999|Sliding Rock Metamorphics|43503|6|Mentioned|15|||||||||
16999|Sliding Rock Metamorphics|60547|5|Briefly described|Map Legend|Precambrian|Precambrian|Hornblende gneiss, garnet-amphibolite gneiss, felsic gneiss.||||||
16999|Sliding Rock Metamorphics|69427|5|Briefly described|p12:9, 14-15|||Strangways Range region, Ankala Domain, Aileron Province.||||Is intruded by Oolbra Orthogneiss.|Migmatitic felsic gneiss, biotite-bearing migmatite with minor sillimanite-bearing gneiss and amphibolite.|12-JUL-16
17000|Slippery Creek Siltstone|22538|6|Mentioned|Fig3 P708|||||||||
17000|Slippery Creek Siltstone|22600|4|Described|Map legend|Statherian|Statherian|||||||
17000|Slippery Creek Siltstone|24048|6|Mentioned|p55|||||||||
17000|Slippery Creek Siltstone|24049|5|Briefly described|Map Legend|Statherian|Statherian|Of Habgood Group. Mudstone: red, purple and dark green, distinctive graded silt laminae, weathered outcrops ferruginised; minor fine-grained sandstone and silty dololutite; large concretions common in places. Geol. Prov: McArthur Basin.||||||04-DEC-06
17000|Slippery Creek Siltstone|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Of Habgood Group. Overlain by Yarawoi Formation. Geological Province: Northern McArthur Basin.||||||
17000|Slippery Creek Siltstone|32660|5|Briefly described|Table 4|||||||||
17000|Slippery Creek Siltstone|42597|5|Briefly described|Map Legend|Carpentarian||||||||
17000|Slippery Creek Siltstone|43010|2|Defined|p131||Paleoproterozoic|Of Habgood Group. Of Statherian age.||||||07-NOV-08
17000|Slippery Creek Siltstone|44112|4|Described|p49,54,57-58|||||||||
17000|Slippery Creek Siltstone|61403|5|Briefly described|Map Legend|Statherian|Statherian|Of Habgood Group. Mudstone: red, purple and dark green, distinctive graded silt laminae, weathered outcrops ferruginised; minor fine-grained sandston e and silty dololutite; large concretions common in places. Geol. Prov: McArthur Basin.||||||04-DEC-06
17000|Slippery Creek Siltstone|64817|6|Mentioned|p353 Fig.4 |||||Of the Habgood Group.||||
17000|Slippery Creek Siltstone|67323|5|Briefly described|Eastern Australia Time-Space Plot; p35|Paleoproterozoic|Paleoproterozoic|McArthur Basin. Appears as Slippery Creek Siltstone Member (of the Habgood Group) on p35: accidental capitalisation?|~1660-1650 Ma.|Habgood Group.|||Siltstone and mudstone.|
17000|Slippery Creek Siltstone|69430|4|Described|p15:3, 13, 20, 22|||Walker Fault Zone, northern McArthur Basin. Subtidal, below wave base deposits.||Basal Habgood Group.||Conformably overlies Kurala Sandstone. Is overlain by Yarawoi Formation.|Predominantly red, purple and dark green laminated micaceous mudstone and minor fine-grained sandstone and muddy dololutite; some beds are pyritic, mainly near the base. Large concretions common locally. Weathered outcrop is ferruginised.|12-JUL-16
17000|Slippery Creek Siltstone|69673|6|Mentioned|p16 fig 13|||Walker Fault Zone||Habgood Group||Overlain by Yarawoi Formation, overlies Kurala Sandstone||
17000|Slippery Creek Siltstone|71374|6|Mentioned|p12|||||||Conformably overlain by the Yarawoi Formation.||
17000|Slippery Creek Siltstone|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.||Lower Habgood Group.|||Mudstone; minor dololutite and sandstone.|04-MAR-20
17000|Slippery Creek Siltstone|72373|5|Briefly described|p6,9,11|Paleoproterozoic|Paleoproterozoic|Of northern McArthur Basin. Associated with northern Walker Fault Zone.||Unit of Habgood Group.||||
17019|Smythe Sandstone|22538|6|Mentioned|Fig3 P709|||||||||
17019|Smythe Sandstone|22664|6|Mentioned|46|Paleoproterozoic|Paleoproterozoic|Geol province: McArthur Basin.||||||07-NOV-08
17019|Smythe Sandstone|22853|4|Described|24|Proterozoic|Proterozoic|Of the Nathan Group. Max thickness: 250 m.||||||04-DEC-06
17019|Smythe Sandstone|23387|6|Mentioned|p18 fig.19|||Of Nathan Group.||||||
17019|Smythe Sandstone|23407|5|Briefly described|p626|||||||||
17019|Smythe Sandstone|23776|5|Briefly described|p705 Fig 2.|||Of Nathan Group.||||||
17019|Smythe Sandstone|23937|5|Briefly described|p88 App. 1|||Supersedes Smythe Sandstone Member of Jackson et al (1987) which replaced original name of Mount Birch Sandstone, without definition,  of Dunn (1963c).||||||03-NOV-04
17019|Smythe Sandstone|24048|5|Briefly described|p64|Calymmian|Calymmian|Of the Nathan Group.  Geological Province: McArthur Basin.||||||04-DEC-06
17019|Smythe Sandstone|30344|6|Mentioned|Fig.4|||||||||
17019|Smythe Sandstone|32658|3|Fully described|Table 2|||See also Fig.3||||||
17019|Smythe Sandstone|32660|5|Briefly described|Table 4|||||||||
17019|Smythe Sandstone|33666|6|Mentioned|Table 1|||||||||
17019|Smythe Sandstone|35162|6|Mentioned|Table.1|||||||||
17019|Smythe Sandstone|35261|6|Mentioned|Fig.2|||||||||
17019|Smythe Sandstone|37462|4|Described|Table4.IV|||||||||
17019|Smythe Sandstone|37568|5|Briefly described|p79|||||||||
17019|Smythe Sandstone|40259|6|Mentioned|Table 1|||||||||
17019|Smythe Sandstone|42385|3|Fully described|p24, p8 Fig. 5|Mesoproterozoic|Mesoproterozoic|Of Nathan Gp. Thickness: 250m. Ridge-forming sst +conglom. - originally mapped as "Smythe Sandstone" on BAUHINIA DOWNS (Smith 1964) and "Mount Birch Sandstone"; has also been called "Smythe Sandstone Member".||||||26-MAR-18
17019|Smythe Sandstone|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
17019|Smythe Sandstone|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.||Of Nathan Group.||In schematic section, underlies Balbirini Dolomite; overlies Stretton Sst, and Looking Glass Formation (with Balbirini Dolomite); overlies Warramana Sandstone.|Polymict conglomerate; pebbly lithic sandstone, sandstone. Detailed lithology given.|09-NOV-11
17019|Smythe Sandstone|42639|4|Described|p35, Table 6|||||||||
17019|Smythe Sandstone|42700|5|Briefly described|map legend|Mesozoic|Early Cretaceous|||||||
17019|Smythe Sandstone|42739|5|Briefly described|map legend|Calymmian|Calymmian|Of the Nathan Group. Massive coarse polymict conglomerate, pebbly lithic sandstone, dolomitic sandstone and dolarenite; typically poorly sorted and trough cross-bedded.||||||19-OCT-05
17019|Smythe Sandstone|42812|3|Fully described|p43, Table 4|||Of the Nathan Group.||||||04-DEC-06
17019|Smythe Sandstone|43036|4|Described|p55|||Of Nathan Group.||||||04-DEC-06
17019|Smythe Sandstone|44112|6|Mentioned|p65-6|||||||||
17019|Smythe Sandstone|44287|14|Not recorded|p.10, opp.9|||Formation of the McArthur Group. (E53-3). Defn. on Tech.File E/53-3.||||||04-DEC-06
17019|Smythe Sandstone|44288|14|Not recorded|map legend|||Quartz sandstone, feldspathic sandstone, pebble to cobble conglomerate. Lower (?) Proterozoic.||||||
17019|Smythe Sandstone|45162|6|Mentioned|p45|||||||||
17019|Smythe Sandstone|46968|6|Mentioned|p302|||||||||
17019|Smythe Sandstone|60483|5|Briefly described|p7 Fig. 5|||Of the Nathan Group. Geological Province: McArthur Basin.||||||05-OCT-07
17019|Smythe Sandstone|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Nathan Group. Overlain by Balbirini Dolomite.||||||03-JUN-09
17019|Smythe Sandstone|63112|6|Mentioned|p1191 Fig.2|||Isa Superbasin; southern McArthur Basin. Age approximated from Fig.2.|c.1615-1610 Ma.|Unit in Lawn Supersequence.||||
17019|Smythe Sandstone|64815|5|Briefly described|p3, p5 Fig.3  |||||Unit in Nathan Group.|||Contains polymict conglomerate and pebbly lithic (chert) sandstone.|26-MAR-18
17019|Smythe Sandstone|64817|6|Mentioned|p353 Fig.4 |||||Of the Nathan Group.||||
17019|Smythe Sandstone|65228|5|Briefly described|Fig.02.|||McArthur Basin. Also appears in Figs.24 and 27 as Smythe Sandstone Member (of Balbirini Dolomite).||Unit in Nathan Group.||Is overlain by Balbirini Dolomite.||
17019|Smythe Sandstone|65340|6|Mentioned|p57, p59.|||Batten Fault Zone. Possibly a lateral equivalent to the lithologically similar basal Karns Dolomite.||||||
17019|Smythe Sandstone|67352|5|Briefly described|p12, p13 Tb.2|||||Unit in Nathan Group.||Overlain (conformably) by Balbirini Dolostone.|Pebbly lithic sandstone.|08-JAN-15
17019|Smythe Sandstone|69430|4|Described|p15:3, 23-25|||Batten Fault Zone, southern McArthur Basin. <100-250m thick. Terrestrial deposits: mainly fluvial (alluvial fan and debris flow). Correlated with Mount Birch Sandstone.||Nathan Group.||Unconformably overlies Batten Subgroup. Is overlain conformably and gradationally by Balbirini Dolostone, and unconformably by Roper Group.|Massive, coarse polymict conglomerate, pebbly lithic (chert) sandstone, typically poorly sorted and prominently cross-bedded; sandstone, minor sandy dolarenite. Conglomerate clasts were derived from the underlying McArthur Group.|12-JUL-16
17019|Smythe Sandstone|69673|6|Mentioned|p16 fig 13|Paleoproterozoic|Paleoproterozoic|Interlayered with Balbirini Dolostone (Upper and Lower packages)||Nathan Group||Overlain by Balbirini Dolostone||
17019|Smythe Sandstone|71374|3|Fully described|iii, p1 tbl 1, p18-p20, p51-p52|Calymmian|Statherian|McArthur Basin. The type section is located along a minor tributary of Clarke Creek about 26km west-southwest of the junction of Ryan Bend Road and Carpentaria Highway in central-eastern BATTEN. The type section was originally defined by Jackson et al (1987). SHRIMP age is interpreted as the maximum depositional age for this sample, but   comes from the top of the formation.  Tuffs in overlying Balbirini Dolostone have been dated at 1613 +/- 4Ma which is within the error of the MDA for Smythe Sandstone top.Possible Musgrave zircon provenenance. Sampling site provided along with zircon description and SHRIMP analytical discussion. Previously the Smythe Sandstone Member of Jackson et al (1987).Conformably overlain by the Balbirini Dolostone. Unconformably overlain by the Roper Group.|1605 +/- 14 Ma (SHRIMP U-Pb)|basal Nathan Group||Overlies the McArthur Group. Unconformably overlies the Looking Glass Formation, Stretton Sandstone and the Yalco Formation.|Basal, massive, coarse polymictic conglomerate, overlain by a thick succession of poorly sorted and prominently cross-bedded, fine- to medium-grained, pebbly lithic (chert) sandstone, quartz sandstone and minor sandy dolarenite.|09-MAY-18
17019|Smythe Sandstone|72373|5|Briefly described|p27-28|Paleoproterozoic|Paleoproterozoic|Of southern McArthur Basin.||||Correlable with Mount Birch Sandstone.||
17019|Smythe Sandstone|72523|5|Briefly described|piii, p1, p8-9, p12.|Early Mesoproterozoic|Early Mesoproterozoic|Type section location in northern Bauhinia Downs map sheet area. This unit is recognised in MOUNT YOUNG and in northern and southeastern BAUHINIA DOWNS, but it is absent in the vicinity of the Abner Range area in southern BAUHINIA DOWNS. Maximum depositional age for this unit (1605+/-14 Ma), overlaps with the older Balbirini Dolostone sample analysed here (1625+/-14 Ma).|1605 +/- 14 Ma maximum depositional age|Base of Nathan Group in Batten Fault Zone area.||Underlies Balbirini Dolostone.|Includes sandstone.|
17019|Smythe Sandstone|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Urapunga Fault Zone, Beetaloo Sub-basin, Batten Fault Zone and Southeastern McArthur Basin.||Nathan Group||Shown as overlying Batten Subgroup and said to underlie Upper Balbirini Dolostone.||
17019|Smythe Sandstone|72718|6|Mentioned|p7|||Southern McArthur Basin. Southwestern McArthur Basin, and Batten Fault Zone.||||Partly underlain[?] by Stretton Sandstone, Looking Glass Formation, and lower Balbirini Dolostone (all of Batten Sub-group, McArthur Group) unconformably. Overlain by upper Balbirini Dolostone.||
17019|Smythe Sandstone|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Beetaloo Sub-basin and Batten Fault Zone of the Southern McArthur Basin.||Nathan Group||Unconformably overlies Vizard and McArthur Group. Equivalent to Mount Birch Sandstone and partially equivalent to Knuckey Formation. Equivalent to Karns Dolostone.||
17019|Smythe Sandstone|73042|6|Mentioned|p4|Mesoproterozoic|Paleoproterozoic|Southern McArthur Basin, Isa Superbasin.||Nathan Group||Unconformably underlain(?) by Looking Glass Formation and partly by Stretton Sandstone. Overlain by Upper Balbirini Dolostone.||
17019|Smythe Sandstone|73412|5|Briefly described|p4|||Southern McArthur Basin.||Nathan Group.||Unconformably overlies Looking Glass and Amos Formations and lower Balbirini Dolostone. Is overlain by upper Balbirini Dolostone.||
17092|Soldiers 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
17092|Soldiers Creek Granite|31435|6|Mentioned|p63|||||||||
17092|Soldiers Creek Granite|32170|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17092|Soldiers Creek Granite|32700|4|Described|Table 1|||See also p13.||||||04-DEC-06
17092|Soldiers Creek Granite|33278|6|Mentioned|Fig.7|||||||||
17092|Soldiers Creek Granite|33377|6|Mentioned|Table 1|||Strat.||||||
17092|Soldiers Creek Granite|34983|6|Mentioned|p32|||||||||
17092|Soldiers Creek Granite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17092|Soldiers Creek Granite|41660|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Muscovite leucogranite, coarse-grained with greisen veins; muscovite - tourmaline pegmatite with associated cassiterite mineralisation. Age: 1760 +/- 27 Ma Rb/Sr.||||||07-NOV-08
17092|Soldiers Creek Granite|41661|3|Fully described|p17|||||||||
17092|Soldiers Creek Granite|41980|5|Briefly described|Table 3 P575|||||||||
17092|Soldiers Creek Granite|45022|3|Fully described|p.147||Carpentarian|On many pages.||||||
17092|Soldiers Creek Granite|45112|5|Briefly described|Table 4|||||||||
17092|Soldiers Creek Granite|48942|3|Fully described|p27|||||||||
17092|Soldiers Creek Granite|50586|5|Briefly described|p1.1, 3.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Of the Allia Suite.||||||07-NOV-08
17092|Soldiers Creek Granite|63866|5|Briefly described|p107|||Litchfield Province, Pine Creek Orogen.||||||
17092|Soldiers Creek Granite|64956|4|Described|p2 Tb. 1, p62|Paleoproterozoic|Paleoproterozoic|Overlain by Tolmer Gp + Antrim Plateau Volcanics. Intrudes Burrell Creek Fm (contains enclaves of its rocks)+Wangi Basics. Max. intrusion age: 1876+/-12Ma. Geol.prov: Pine Creek Orogen. Sample is an altered and deformed K-feldspar two-mica granite. Emplacement of the Soldiers Creek Granite can be better constrained by recent geochronological studies of the Wangi Basics and Burrell Creek Formation.||||||25-NOV-11
17092|Soldiers Creek Granite|65232|6|Mentioned|App. 2|||||||||09-FEB-10
17092|Soldiers Creek Granite|67232|6|Mentioned|p35.|||||||Intrudes Lilyarba Mafics.||
17092|Soldiers Creek Granite|69420|5|Briefly described|p5:18-19, 28, 102, 109|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Mineralogy and petrology/geochemistry summarised. Associated with Burrell Creek Formation Sn-Ta-Nb pegmatite deposits. Age from a mafic sample entrained within the granite.|<1830 Ma: Worden et al. (2008).|Allia Creek Suite.|||Quartz monzonite and granodiorite: a medium-grained porphyritic muscovite leucogranite, associated with greisen veins. Numerous xenoliths to 30cm occur throughout.|12-JUL-16
17092|Soldiers Creek Granite|69442|6|Mentioned|p27:3 Tb.27.1; 5|||||||Is overlain unconformably by Uniya Formation.||12-JUL-16
17092|Soldiers Creek Granite|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|1872+/-12 Ma (crystallisation: U-Pb zircon SHRIMP)||||Altered and deformed K-feldspar(megacrysts)-biotite-muscovite granite.|
17111|South Alligator Group|9324|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Carbonaceous and ferruginous shale with chert bands, carbonate, tuff, banded iron formation.||||||07-NOV-08
17111|South Alligator Group|9534|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes Kapalga Formation, Gerowie Tuff and Koolpin Formation.||||||07-NOV-08
17111|South Alligator Group|9538|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Carbonaceous and ferruginous shale with: chert bands, carbonate tuff, andesite, banded iron formation.  Conformably overlain by the Finniss River Group; unconformably over Mount Partridge Group.||||||07-NOV-08
17111|South Alligator Group|9579|5|Briefly described|Map Sheet|Paleoproterozoic|Paleoproterozoic|Early Proterozoic age.||||||
17111|South Alligator Group|9691|5|Briefly described|Map Legend|||||||||
17111|South Alligator Group|9701|5|Briefly described|Map Legend|Proterozoic|Proterozoic|||||||02-JUN-05
17111|South Alligator Group|9733|5|Briefly described|Map Legend|Proterozoic|Proterozoic|||||||
17111|South Alligator Group|22479|5|Briefly described|fig1p2|Orosirian|Orosirian|||||||
17111|South Alligator Group|22809|6|Mentioned|map|||||||||
17111|South Alligator Group|22810|5|Briefly described|Table2 P4, P13|||Maximum thickness: 5000m.||||||04-DEC-06
17111|South Alligator Group|22813|5|Briefly described|Map|Paleoproterozoic|Paleoproterozoic|Carbonaceous and ferruginous shale with chert bands, carbonate, tuff, banded iron formation.||||||07-NOV-08
17111|South Alligator Group|23122|6|Mentioned|p410|||||||||
17111|South Alligator Group|23216|6|Mentioned|Fig3p5||Paleoproterozoic|||||||07-NOV-08
17111|South Alligator Group|23714|4|Described|p10|Proterozoic|Proterozoic|Max. thickness: 5000 m.||||||
17111|South Alligator Group|23715|5|Briefly described|Map legend||Proterozoic|In the Rum Jungle and Central Regions||||||
17111|South Alligator Group|23733|5|Briefly described|p32 Fig. 19|||||||||
17111|South Alligator Group|23999|5|Briefly described|p6 Fig. 3|||Sediments. Includes the Gerowie Tuff.||||||07-FEB-11
17111|South Alligator Group|24001|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Siltstone, shale, chert, silicified carbonate, white quartz, oolitic quartzite.||||||
17111|South Alligator Group|24047|5|Briefly described|p5 Fig.4|Paleoproterozoic|Paleoproterozoic|Shale, phyllite, greywacke.  Geological Province: Pine Creek Orogen.  See also p6 Fig. 5.||||||07-NOV-08
17111|South Alligator Group|24181|5|Briefly described|p87 Fig.2|Paleoproterozoic|Paleoproterozoic|Unconformably overlies Mount Partridge Group. Overlain by Burrell Creek Formation. Geological Province: Pine Creek Inlier.||||||07-NOV-08
17111|South Alligator Group|24260|6|Mentioned|p1013 Fig.1|||Geological Province: Pine Creek Inlier||||||
17111|South Alligator Group|24442|6|Mentioned|p30, p43|||Of the Pine Creek Orogen.  Intruded by the Zamu Dolerite.  On NOONAMAH sheet.||||||
17111|South Alligator Group|29599|6|Mentioned|Fig.2|||||||||
17111|South Alligator Group|30558|6|Mentioned|Table 3|||||||||
17111|South Alligator Group|30680|6|Mentioned|p309|||||||||
17111|South Alligator Group|30830|6|Mentioned|Fig.1|||||||||
17111|South Alligator Group|30831|6|Mentioned|p1|||||||||
17111|South Alligator Group|30832|5|Briefly described|p318|||||||||
17111|South Alligator Group|31268|6|Mentioned|p20|||||||||
17111|South Alligator Group|31347|6|Mentioned|p135|||||||||
17111|South Alligator Group|31824|6|Mentioned|p25|||Lithology||||||
17111|South Alligator Group|32144|6|Mentioned|p116|||Organic matter||||||
17111|South Alligator Group|32659|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17111|South Alligator Group|32660|4|Described|Table 2|||||||||
17111|South Alligator Group|33225|6|Mentioned|p20|||||||||
17111|South Alligator Group|35140|6|Mentioned|Fig.2|||||||||
17111|South Alligator Group|35165|6|Mentioned|p1420|||||||||
17111|South Alligator Group|36473|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17111|South Alligator Group|36535|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17111|South Alligator Group|36635|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17111|South Alligator Group|37462|4|Described|Table 4.II|||||||||
17111|South Alligator Group|37579|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes the Kapalga Formation.||||||07-NOV-08
17111|South Alligator Group|37815|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17111|South Alligator Group|38239|6|Mentioned|Fig.2|||||||||
17111|South Alligator Group|38349|6|Mentioned|p27|||||||||
17111|South Alligator Group|38351|6|Mentioned|Table 1|||||||||
17111|South Alligator Group|38884|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17111|South Alligator Group|39068|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||14-FEB-06
17111|South Alligator Group|39069|4|Described|p7|||||||||
17111|South Alligator Group|39320|6|Mentioned|Fig.1|||||||||
17111|South Alligator Group|39357|4|Described|p9|||See also p12.||||||18-SEP-06
17111|South Alligator Group|39518|4|Described|p5|||||||||
17111|South Alligator Group|39563|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17111|South Alligator Group|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17111|South Alligator Group|39801|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Carbonaceous and ferruginous shale with chert bands, carbonate tuff, andesite, banded iron formation.||||||07-NOV-08
17111|South Alligator Group|40104|6|Mentioned|p349|||||||||
17111|South Alligator Group|40168|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Carbonaceous and ferruginous shale with: chert bands, carbonate, andesite, tuff, banded iron formation.||||||07-NOV-08
17111|South Alligator Group|40223|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Carbonaceous and ferruginous shale, with chert bands, tuff, carbonate, andesite, bif.||||||07-NOV-08
17111|South Alligator Group|40243|6|Mentioned|Fig.2|||||||||
17111|South Alligator Group|40492|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17111|South Alligator Group|40493|4|Described|p12|||||||||
17111|South Alligator Group|40495|6|Mentioned|Fig.3|||||||||
17111|South Alligator Group|40765|6|Mentioned|Fig.3|||||||||
17111|South Alligator Group|40808|3|Fully described|p12|||Mention p13.||||||18-SEP-06
17111|South Alligator Group|40809|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17111|South Alligator Group|40823|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17111|South Alligator Group|40852|5|Briefly described|p25|||||||||
17111|South Alligator Group|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17111|South Alligator Group|40973|6|Mentioned|p195|||||||||
17111|South Alligator Group|41125|5|Briefly described|p55|||Mention Fig.6||||||
17111|South Alligator Group|41304|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
17111|South Alligator Group|41305|4|Described|p16|||||||||
17111|South Alligator Group|41309|4|Described|p5|||||||||
17111|South Alligator Group|41311|4|Described|p9|||||||||
17111|South Alligator Group|41397|4|Described|p8|||||||||
17111|South Alligator Group|41406|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
17111|South Alligator Group|41407|6|Mentioned|Map legend|Proterozoic||||||||
17111|South Alligator Group|41465|6|Mentioned|p6|||||||||
17111|South Alligator Group|41466|6|Mentioned|p23|||||||||
17111|South Alligator Group|41586|6|Mentioned|Map legend|||||||||
17111|South Alligator Group|41594|6|Mentioned|p20|||||||||
17111|South Alligator Group|41645|6|Mentioned|Fig.6|||||||||
17111|South Alligator Group|41660|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Carbonaceous and ferruginous shale with chert bands, carbonate, tuff, banded iron formation.||||||07-NOV-08
17111|South Alligator Group|41661|6|Mentioned|p26|||See also Fig.5||||||
17111|South Alligator Group|41860|6|Mentioned|p443|||||||||
17111|South Alligator Group|41873|6|Mentioned|p5|||||||||
17111|South Alligator Group|41874|6|Mentioned|p11|||||||||
17111|South Alligator Group|41875|6|Mentioned|p18|||||||||
17111|South Alligator Group|41876|6|Mentioned|p21|||||||||
17111|South Alligator Group|41878|5|Briefly described|p34|||||||||
17111|South Alligator Group|42012|4|Described|p4|||||||||
17111|South Alligator Group|42014|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
17111|South Alligator Group|42163|5|Briefly described|p61|||||||||
17111|South Alligator Group|42202|6|Mentioned|Fig.1 P511|||||||||
17111|South Alligator Group|42927|5|Briefly described|p428|||see also Fig.1 p429.||||||04-DEC-06
17111|South Alligator Group|43115|6|Mentioned|p181|||||||||
17111|South Alligator Group|43140|5|Briefly described|p3||Paleoproterozoic|||||||07-NOV-08
17111|South Alligator Group|43187|5|Briefly described|p7|||||||||
17111|South Alligator Group|43624|6|Mentioned|Table 1,p9||Paleoproterozoic|||||||07-NOV-08
17111|South Alligator Group|43718|6|Mentioned|p23|||||||||
17111|South Alligator Group|43720|5|Briefly described|p4||Paleoproterozoic|||||||07-NOV-08
17111|South Alligator Group|43832|3|Fully described|12,15-19,97||Paleoproterozoic|Age around 1885 Ma. Within Pine Creek Geosyncline. Mt Partridge Group underlies, Finniss River Gp overlies.||||||07-NOV-08
17111|South Alligator Group|44399|5|Briefly described|map legend||Paleoproterozoic|Includes the Fisher Creek Siltstone, Gerowie Chert and Koolpin Formation.||||||07-NOV-08
17111|South Alligator Group|45022|4|Described|p.48.||Paleoproterozoic|On many pages.||||||07-NOV-08
17111|South Alligator Group|45086|5|Briefly described|p26|||See also p27. Lower Prot. Lithology.||||||04-DEC-06
17111|South Alligator Group|46163|14|Not recorded|p.168-170||Paleoproterozoic|Includes Fisher Creek Siltstones. Gerowie Chert, Koolpin Formation.||||||07-NOV-08
17111|South Alligator Group|46639|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes Kapalga Formation.||||||07-NOV-08
17111|South Alligator Group|46658|4|Described|p550|||||||||
17111|South Alligator Group|46675|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes upper Mount Bonnie and lower Koolpin Fms and Gerowie Tuff between.  Conformably overlain by Finniss River Gp; unconformably overlies the Mount Partridge Gp.  Intruded by the Shoobridge, Burnside, Margaret and Cullen Granites, and Zamu Dolerite.||||||07-NOV-08
17111|South Alligator Group|46678|5|Briefly described|Table 1|Proterozoic|Proterozoic|Contains Fusher Creek Siltstone, Gerowie Chert and Koolpin Formation.  Overlies and folded with Goodparla Group.||||||
17111|South Alligator Group|46700|5|Briefly described|P14, Table1 P10||Proterozoic|||||||
17111|South Alligator Group|46824|6|Mentioned|p328|||||||||
17111|South Alligator Group|46877|6|Mentioned|Fig.4|||||||||
17111|South Alligator Group|47049|6|Mentioned|Fig.2|||||||||
17111|South Alligator Group|50623|4|Described|p259 Fig.2|Paleoproterozoic|Paleoproterozoic|Shows transition from shallow marine to deeper water sediments. Unconformably overlies Mount Partridge Group, conformably overlain by Finnis River Group.||||||07-NOV-08
17111|South Alligator Group|60526|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Includes: Mount Bonnie Formation, Gerowie Tuff, Koolpin Formation.||||||
17111|South Alligator Group|60550|5|Briefly described|Map Legend|Proterozoic|Proterozoic|||||||
17111|South Alligator Group|60575|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Includes Mount Bonnie Formation, Gerowie Tuff and Koolpin Formation.||||||
17111|South Alligator Group|60677|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Unconformably overlies Mount Partridge Group. Overlain by Finniss River Group.||||||
17111|South Alligator Group|60680|5|Briefly described|Map legend|Orosirian|Orosirian|Includes: Mount Bonnie Formation, Gerowie Tuff and Koolpin Formation. Geological Province: Pine Creek Orogen.||||||
17111|South Alligator Group|61389|5|Briefly described|Map Legend|||||||||
17111|South Alligator Group|61827|5|Briefly described|p158 Fig. 4|||||||||
17111|South Alligator Group|61861|6|Mentioned|p12, Fig.2.|||Pine Creek Orogen.|||Includes Koolpin Formation.|Unconformably overlies Mount Partridge Group. Is overlain by Finniss River Group.||
17111|South Alligator Group|62375|5|Briefly described|p8 Table 1, 9 table 2, 10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Pyritic black shale and siltstone, chert banded and nodular heamatitic siltstone and black shale. Thickness:<5000m. Age: 1885 +/- 3Ma. Geological Province: Pine Creek Orogen.||||||09-FEB-10
17111|South Alligator Group|62378|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Orogen. Age: 1885 +/- 2Ma. Unconformably overlies: Wildman Siltstone.||||||07-NOV-08
17111|South Alligator Group|63866|5|Briefly described|p109, p112, p123|||Central Domain, Pine Creek Orogen.|||Includes the Gerowie Tuff and the Mount Bonnie Formation.|Conformably overlain by the Finniss River Group.||
17111|South Alligator Group|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1850-2025Ma.Includes Gerowie Tuff (1863Ma), Koolpin Formation, Mount Bonnie Formation, Shovel Billabong Andesite. Max thickness 500m. Quartz-sericite and quartz-chlorite-sericite schist.||||||07-JAN-09
17111|South Alligator 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.||||Overlain by El Sherana and Edith River Groups.||11-APR-12
17111|South Alligator Group|64730|5|Briefly described|p125 Fig. 3, p126, 139, p142 Fig. 11|Paleoproterozoic|Paleoproterozoic|5000m thick. Age from dates of the Gerowie Tuff (middle unit in Group). Previous age: ID-TIMS zircon 1885 +/-2 Ma interpreted as end of Archean basement extension.|Deposition age 1863 +/- 2 Ma.||Includes Mount Bonnie Formation, Gerowie Tuff and Koolpin Formation.|Conformably underlies Finniss River Group; unconformably overlies Mount Partridge Group.||02-MAY-12
17111|South Alligator Group|64731|5|Briefly described|p147|Proterozoic|Proterozoic|Central Domain, Pine Creek Orogen.||||Unconformably overlies Mount Partridge Group. Conformably overlain by Finniss River Group.|Composed of tuff, chert, clastic and carbonaceous sediments.|12-APR-12
17111|South Alligator Group|64956|5|Briefly described|p72, p78|||Unconformably overlies Mount Partridge Group; conformably overlain by Finniss River Group.  Geological province: Pine Creek Orogen.||||||07-FEB-11
17111|South Alligator Group|65232|5|Briefly described|p45, p7, p6 Fig. 5, p5 Fig. 4|Palaeoproterozoic|Palaeoproterozoic|Includes Mount Bonnie Formation and Koolpin Formation (at base). Unconformable over Mount Partridge Group. Conformable under Burrell Creek Formation. Intruded by Zamu Dolerite. Age: 1863+/-2 Ma tuff (Worden et al. 2004). Geol. Prov: Pine Creek Orogen.||||||09-FEB-10
17111|South Alligator Group|65339|5|Briefly described|p5 Fig.4, p6 Table 1, pp12-13. |||Gradually thins westward towards Rum Jungle and Waterhouse Domes.|||Includes Koolpin and Mount Bonnie Formations and Gerowie Tuff.|Intruded and contact metamorphosed by Mount Bundey Granite and Mount Goyder Syenite.|Greywacke, shale, siltstone.|
17111|South Alligator Group|65556|6|Mentioned|p45|||Sedimentary rocks. Possibly correlated with Fog Bay Metamorphics.||||||
17111|South Alligator Group|67186|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Unit in Cosmo Supergroup.|Includes Koolpin and Mount Bonnie Formations and Gerowie Tuff.|||23-NOV-11
17111|South Alligator Group|67323|5|Briefly described|Eastern Australia Time-Space Plot; p29|||Pine Creek area. Deposition age.|~1870-1860 Ma.||Mount Bonnie Formation, Gerowie Tuff, Koolpin Formation.||Siltstone; schist, phyllite and chert; pitchstone and andesite.|
17111|South Alligator Group|67355|5|Briefly described|p5-7, p12-16, p21, p46-47 Figs.37-8, p69||Orosirian|Batchelor Shelf. A combined thickness of up to 5000 m.||Cosmo Howley Supergroup|Koolpin Formation, Gerowie Tuff, Mount Bonnie Formation.|Time equivalent to/underlies the Finniss River Group conformably. Overlies the Mount Partridge Group (unconformably).||25-JAN-17
17111|South Alligator Group|67479|5|Briefly described|p56|Orosirian|Orosirian|Detrital zircon age spectra (eg Worden et al. 2008, Hollis et al. 2009). Contains felsic ash-fall deposits coeval with the Nimbuwah Complex.|c. 1865-1860 Ma|||||24-JAN-17
17111|South Alligator Group|67564|3|Fully described|p iv, p7 Table 2, p9 Fig.4, pp19-23.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Characteristically low-energy, shallow-marine (intertidal to subtidal) deposition. Deformed (tight to isoclinal folds and extensive faults) and metamorphosed to greenschist facies during the 1860 - 1850 Ma Nimbuwah Event.|c.1863 Ma.||Includes Koolpin Formation, Shovel Billabong Andesite, Gerowie Tuff and Mount Bonnie Formation.|Disconformably overlies Mount Partridge Group. Is overlain conformably by Finniss River Group.|A distinct succession of iron-rich, tuffaceous and carbonate-bearing metasedimentary rocks.|
17111|South Alligator Group|67779|5|Briefly described|p5 Fig.4(b).|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen.||Unit in Cosmo Supergroup.|Includes Koolpin Formation, Gerowie Tuff and Mount Bonnie Formation.|Is overlain by Finniss River Group.||
17111|South Alligator Group|67824|5|Briefly described|p383|||Pine Creek Orogen.|||Includes Koolpin Formation.|Overlain by Finniss River Group.||
17111|South Alligator Group|69383|6|Mentioned|p34|Paleoproterozoic||||||Overlain by Burrell Creek Formation||
17111|South Alligator Group|69418|6|Mentioned|p3:17, 19, 33|||Pine Creek Orogen. Hosts the Thunderball vein-type U deposit (described). Also hosts the Quantum REE prospect, 20km SW of Hayes Creek, in drill intersections.||||||12-JUL-16
17111|South Alligator Group|69419|6|Mentioned|p4:3 Fig.4.3|||W. Pine Creek Orogen.||||||12-JUL-16
17111|South Alligator Group|69420|3|Fully described|p5:2, 4-6, 8, 11-12, 15-16, 30, 52, 55|Paleoproterozoic|Paleoproterozoic|See also 67, 78-79, 93, 99, 105, 116. Central Domain, Pine Creek Orogen. As cited in Walpole et al. (1968), this unit included Koolpin Formation, Gerowie Chert and Fisher Creek Siltstone. Deposition of this unit followed deformation and ended a 160 m.y. hiatus.|c.1863 Ma (Worden et al., 2008).|Cosmo Supergroup.|Koolpin, Mount Bonnie Formations; Gerowie Tuff; Shovel Billabong Andesite.|Unconformably overlies Mount Partridge Group. Is overlain by Finniss River Group and (unconformably) by El Sherana Group. Is intruded by Zamu Dolerite.|A succession of basal breccia overlain by iron-rich sedimentary rocks, tuff, carbonate rocks, shale, greywacke and siltstone.|12-JUL-16
17111|South Alligator Group|69577|6|Mentioned|p117 Fig.6|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||||||
17111|South Alligator Group|69917|5|Briefly described|p51,52|||Pine Creek Orogen, Central Domain.||||Conformably underlies Finniss River Group.||
17111|South Alligator Group|70293|5|Briefly described|p597-600, p615, p619|Paleoproterozoic|Paleoproterozoic|Basement to the Central Domain, Pine Creek Orogen. See also references to South Alligator River Group (p599, p612, p618, p620).|||Koolpin Formation, Gerowie Tuff, Shovel Billabong Andesite, Mount Bonney Formation.|Unconformably overlain by El Sherana Group. Is intruded by Zamu Dolerite sills.|Folded and metamorphosed sedimentary, volcanic and plutonic rocks.|
17111|South Alligator Group|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||Cosmo Supergroup.|Includes Mount Bonnie, Koolpin Formations; Gerowie Tuff.|Unconformably overlies Mount Partridge Group. Is overlain by Finniss River Group.||28-FEB-18
17111|South Alligator Group|73083|6|Mentioned|p5-6|||Allochthonous.||||||
17111|South Alligator Group|73089|6|Mentioned|p32|||Pine Creek Orogen, central.||||Overlain[?] by Burrell Creek Formation.||
17123|South Nicholson Group|22479|5|Briefly described|fig4, pg10|Calymmian|Calymmian|||||||
17123|South Nicholson Group|22644|5|Briefly described|5,7|||Geological province: McArthur Basin.||||||04-DEC-06
17123|South Nicholson Group|22673|6|Mentioned|65,79|||Max thickness: 1000 m.||||||04-DEC-06
17123|South Nicholson Group|22680|4|Described|86|||||||||
17123|South Nicholson Group|23065|5|Briefly described|17|||Geological province: South Nicholson Basin.||||||04-DEC-06
17123|South Nicholson Group|23066|5|Briefly described|p807, Fig.1|Proterozoic|Proterozoic|||||||
17123|South Nicholson Group|23393|4|Described|p21, p17 Fig. 5|Mesoproterozoic|Mesoproterozoic|Geological Province: Lawn Hill Sub-province.||||||
17123|South Nicholson Group|23396|6|Mentioned|p425|||||||||
17123|South Nicholson Group|23404|5|Briefly described|p638 Fig.1|||||||||
17123|South Nicholson Group|23405|5|Briefly described|p586|||||||||
17123|South Nicholson Group|23406|5|Briefly described|p600 Fig. 2|||Age: <1500Ma.||||||16-JUN-09
17123|South Nicholson Group|23407|5|Briefly described|p633|||||||||
17123|South Nicholson Group|23409|5|Briefly described|p535 Fig.2|Mesoproterozoic|Mesoproterozoic|Of Lawn Hill Platform.||||||04-DEC-06
17123|South Nicholson Group|23519|5|Briefly described|p138|Mesoproterozoic|Mesoproterozoic|See also page 137 Fig 7||||||
17123|South Nicholson Group|23937|6|Mentioned|p22|||Correlated with the Roper Group - see p76 Appendix 1.||||||
17123|South Nicholson Group|23958|5|Briefly described|p1133|Mesoproterozoic|Mesoproterozoic|||||||
17123|South Nicholson Group|24047|6|Mentioned|p27|||Geological Province: South Nicholson Basin.||||||
17123|South Nicholson Group|24303|5|Briefly described|p59 Appendix|||Geological Province: Nicholson Basin. Correlative of Renner Group.||||||
17123|South Nicholson Group|24308|5|Briefly described|p995 Fig. 8|||||||||
17123|South Nicholson Group|24309|6|Mentioned|p1012 Fig. 1|||||||||
17123|South Nicholson Group|24419|5|Briefly described|p13 Fig.5|Mesoproterozoic|Mesoproterozoic|Geological Province: Murphy Province, Lawn Hill Subprovince (north), South Nicholson Basin.||||||
17123|South Nicholson Group|24432|6|Mentioned|p565 Fig.4|||||||||
17123|South Nicholson Group|24442|5|Briefly described|p22, p23 Fig. 2|Mesoproterozoic|Mesoproterozoic|Age: 1500-1450Ma. Geological Province: McArthur Basin.||||||
17123|South Nicholson Group|30344|6|Mentioned|p29|||Age: 1,510 +- 120m.y.||||||04-DEC-06
17123|South Nicholson Group|30508|6|Mentioned|p94|||Stratigraphy||||||
17123|South Nicholson Group|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
17123|South Nicholson Group|32659|6|Mentioned|Map legend|Adelaidean|Carpentarian|Carpentarian or Adelaidean||||||
17123|South Nicholson Group|32660|4|Described|Table 5|||||||||
17123|South Nicholson Group|32959|6|Mentioned|p31|||||||||
17123|South Nicholson Group|33214|6|Mentioned|Fig.1|||||||||
17123|South Nicholson Group|33900|6|Mentioned|p19|||||||||
17123|South Nicholson Group|34287|6|Mentioned|p41|||||||||
17123|South Nicholson Group|35114|6|Mentioned|p202|||||||||
17123|South Nicholson Group|35640|6|Mentioned|Map legend|Adelaidean|Adelaidean|Carpentarian||||||
17123|South Nicholson Group|35950|6|Mentioned|p311|||||||||
17123|South Nicholson Group|36003|6|Mentioned|p1029|||||||||
17123|South Nicholson Group|36012|3|Fully described|Table 4|||See also p16.||||||06-NOV-06
17123|South Nicholson Group|36439|6|Mentioned|Map legend|Adelaidean|Carpentarian|Carpentarian or Adelaidean.||||||23-DEC-08
17123|South Nicholson Group|36442|6|Mentioned|Map legend|Adelaidean|Carpentarian|Carpentarian or Adelaidean||||||
17123|South Nicholson Group|36473|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
17123|South Nicholson Group|37371|6|Mentioned|p368|||||||||
17123|South Nicholson Group|37459|6|Mentioned|p433|||See also p427.||||||04-DEC-06
17123|South Nicholson Group|37462|4|Described|Table4.VII|||||||||
17123|South Nicholson Group|37565|6|Mentioned|p3|||||||||
17123|South Nicholson Group|37568|6|Mentioned|p86|||||||||
17123|South Nicholson Group|37572|6|Mentioned|p155|||See also Fig.4||||||
17123|South Nicholson Group|38237|6|Mentioned|p125|||||||||
17123|South Nicholson Group|38291|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17123|South Nicholson Group|38348|4|Described|p24|||||||||
17123|South Nicholson Group|38584|4|Described|p19|||||||||
17123|South Nicholson Group|39422|5|Briefly described|Map legend|Carpentarian|Carpentarian|Includes the Mullera Formation and Constance Sandstone.||||||10-JAN-05
17123|South Nicholson Group|39445|5|Briefly described|p56|||See Table 3||||||
17123|South Nicholson Group|39497|6|Mentioned|p4|||||||||
17123|South Nicholson Group|39685|6|Mentioned|Fig.1|||||||||
17123|South Nicholson Group|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17123|South Nicholson Group|39925|6|Mentioned|p329|||||||||
17123|South Nicholson Group|40105|6|Mentioned|p315|||||||||
17123|South Nicholson Group|40840|6|Mentioned|Map legend|||||||||
17123|South Nicholson Group|41406|6|Mentioned|Map legend|Mesoproterozoic||||||||
17123|South Nicholson Group|41721|6|Mentioned|p28|||Overlies the Doomadgee Formation and where this is missing it overlies Mount Les Siltstone or Walford Dolomite. Thickness: 300m+.  Geol. prov: South Nicholson Basin. Sandstone, siltstone and shale.||||||01-AUG-07
17123|South Nicholson Group|41722|6|Mentioned|Map legend|||||||||
17123|South Nicholson Group|41979|6|Mentioned|Fig.2 P512|||||||||
17123|South Nicholson Group|42385|5|Briefly described|Fig.4 P7|||||||||
17123|South Nicholson Group|42386|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
17123|South Nicholson Group|42638|6|Mentioned|Map legend|||Appears on Regional Setting map. Age: Middle Proterozoic.|||||Quartz sandstone, micaceous siltstone and sandstone, shale.|07-NOV-11
17123|South Nicholson Group|42639|5|Briefly described|Fig.4 P7|||||||||
17123|South Nicholson Group|42775|6|Mentioned|Fig.13 P323|||||||||
17123|South Nicholson Group|43010|5|Briefly described|Fig.6||Mesoproterozoic|of "Mid Proterozoic" age.||||||
17123|South Nicholson Group|43595|5|Briefly described|p440-1|||Shale Rb-Sr date at: 1480 Ma.||||||23-DEC-08
17123|South Nicholson Group|44287|14|Not recorded|p.12|||Equiv. of Roper Group. (E53-3).||||||
17123|South Nicholson Group|44305|14|Not recorded|p.14,15|||(E53-8). opp.p.6,18. Includes Mittiebah Sandstone, Mullera Formation, Constance Sandstone.||||||
17123|South Nicholson Group|44306|14|Not recorded|map legend|||(?) Upper Proterozoic.||||||
17123|South Nicholson Group|44473|14|Not recorded|p.9-10,15,opp. p.7|||(E53-7). Represented in Wallhallow area by Mittiebah Sandstone.||||||
17123|South Nicholson Group|44474|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
17123|South Nicholson Group|44482|14|Not recorded|p.7,8-10,opp.p.6,map|||(E53-12). See also p.14, for more details.||||||
17123|South Nicholson Group|44483|5|Briefly described|map legend|||Upper (?) Proterozoic.||||||
17123|South Nicholson Group|44922|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
17123|South Nicholson Group|45032|14|Not recorded|p9||Adelaidean|Tb.1, Pl.1.||||||
17123|South Nicholson Group|45052|4|Described|p69|||Adelaidean||||||
17123|South Nicholson Group|45166|4|Described|p33|||||||||
17123|South Nicholson Group|46804|6|Mentioned|p154|||||||||
17123|South Nicholson Group|46919|6|Mentioned|p221|||||||||
17123|South Nicholson Group|49001|6|Mentioned|p9|||||||||
17123|South Nicholson Group|50225|5|Briefly described|p406 Fig. 10, p407|Mesoproterozoic|Mesoproterozoic|Geological Province: Roper Superbasin.||||||07-FEB-11
17123|South Nicholson Group|60675|6|Mentioned|Map legend|||||||||
17123|South Nicholson Group|61904|5|Briefly described|p132 Fig. 1|||||||||
17123|South Nicholson Group|62657|5|Briefly described|Map Legend|Calymmian|Calymmian|||||||
17123|South Nicholson Group|62659|5|Briefly described|Map Legend|Calymmian|Calymmian|||||||
17123|South Nicholson Group|63113|6|Mentioned|p1212 Fig.1. |Mesoproterozoic|Mesoproterozoic|||||||
17123|South Nicholson Group|63114|6|Mentioned|p1270.|||Roper superbasin.||||||
17123|South Nicholson Group|64443|4|Described|iii, p3-5, p28, p40 |Calymmian|Calymmian|Basement to much of central Georgina Basin. Correlative of Renner Group and Roper Group; may unconformably underlie Barkly Group. Undivided South Nicholson Group contains lithologically undistinctive constituent units.|||Divided into Wild Cow and Accident Subgroups.|Is unconformably overlain by Wonarah Formation, Arthur Creek Formation, Thorntonia Limestone, Helen Springs Volcanics.||14-MAY-14
17123|South Nicholson Group|64575|6|Mentioned|p657|||||||||
17123|South Nicholson Group|64724|6|Mentioned|p45 Fig.5|Calymmian|Calymmian|South Nicholson Basin||||||
17123|South Nicholson Group|65336|5|Briefly described|Map Legend|Calymmian|Calymmian|Includes Accident Subgroup which includes Mittiebah Sandstone. Unconformably overlain by Kalkarindji Volcanic Group. Undifferentiated South Nicholson Group consists of quartz sandstone, mudstone, other sedimentary rocks.||||||
17123|South Nicholson Group|65337|4|Described|p6 Fig.3, p34, pp36-60.|Mesoproterozoic|Mesoproterozoic|Roper Superbasin. Occupies much of  MOUNT DRUMMOND outcrop area. To 6500 m thick, medial to proximal foreland basin deposits. Hosts several ironstone units, organic rich source rocks and potential reservoir formations.|c.1500-1400 Ma.||Includes Wild Cow and overlying Accident Subgroups.|Unconformably overlies Benmara and McNamara Groups. Is unconformably overlain by Bukalara Sandstone, Helen Springs Volcanics and Wonarah Formation.|Couplets of fine-grained shelf tempestites and shales, and coarse-grained fluvial and shallow-marine siliciclastic rocks.|
17123|South Nicholson Group|65340|5|Briefly described|p82.|||Unconformably overlies a group of diatremes of non-diamondiferous kimberlitic to lamproitic affinity at Coanjula.|1490 - 1430 Ma.|||||
17123|South Nicholson Group|65344|4|Described|p3, 5, 7,  9, 15-16, 21, Figs., Tables|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Underlies the Georgina Basin. Correlated with the Roper Group of the McArthur Basin. See well logs and thin section descriptions for detail.|||Includes the Mittiebah Sandstone.|Overlain by the Gum Ridge Formation, Thorntonia Limestone and Helen Springs Volcanics.|Mainly quartz sandstone.|
17123|South Nicholson Group|67144|5|Briefly described|Map legend.|Calymmian|Calymmian|South Nicholson Basin.|||Includes Mittiebah Sandstone.|Is unconformably overlain by Kiana Group.||13-APR-12
17123|South Nicholson Group|67149|5|Briefly described|Map legend.|Calymmian|Calymmian|South Nicholson Basin.||||Is overlain by Helen Springs Volcanics.|Quartzose, lithic, micaceous and sublithic glauconitic sandstone, micaceous and ferruginous siltstone, shale, claystone; minor conglomerate, ironstone (cross-section only).|
17123|South Nicholson Group|67150|5|Briefly described|Map legend.|Calymmian|Calymmian|South Nicholson Basin.|||Includes Accident Subgroup.|Is unconformably overlain by Helen Springs Volcanics and Gum Ridge Formation.|Quartzose, lithic, micaceous and sublithic glauconitic sandstone, micaceous and ferruginous siltstone, shale, claystone; minor conglomerate, ironstone (cross-section only).|
17123|South Nicholson Group|67323|5|Briefly described|GIS attrib tbl, p9, p11, p39, p107|Mesoproterozoic|Paleoproterozoic|See also Solid Geology Map, Mount Isa Block Time-Space Plot. South Nicholson Basin. Age uncertain but likely to be in ~1500 - 1400 Ma range. Overlies Lawn Hill Platform rocks. CONSTITUENTS (continued): Middle Creek Sandstone Member, Mullera Formation, Pandanus Formation, Schultz Sandstone Member, Tidna Sandstone, Train Range Ironstone Member, Wallis Formation.|||Includes Bowthorn Siltstone Member, Burangoo Sandstone, Constance Sandstone, Elizabeth Sandstone Member, Hedleys Sandstone Member. See COMMENTS for more.||Siltstone, shale, sandstone.|
17123|South Nicholson Group|67352|4|Described|v,p8,p11,p16-20,p31-32,p41-42,p46-49,p51|Calymmian|Calymmian|Smith and Roberts (1963). South Nicholson Basin. Floors much of the central Georgina Basin. Provisional age from correlation with Roper Group (McArthur Basin). 1552 +/- 165 Ma (Harding in Fisher, 1965).|c.1500 - c.1400 Ma.||Wild Cow and Accident Subgroups.|Overlain (unconformably) by Gum Creek Formation or Helen Springs Volcanics.  Equivalent to Renner Group; correlated with Roper Group.|Siliciclastic sedimentary rocks.|
17123|South Nicholson Group|67499|5|Briefly described|p940, p947, p942 Fig.4, p949|Calymmian|Calymmian|Age of basal units determined using SHRIMP U-Pb dating of zircons in tuff layers. Group said to be hematitic and iron rich.|1493 +/- 8 Ma||Includes Quamby Conglomerate?|Overlies McNamara Group.||
17123|South Nicholson Group|67539|5|Briefly described|p14, p15, p16||||||Includes Boodjamulla Formation, Hedleys Sandstone, Pandanus Siltstone, Burangoo Sandstone, Wallis Siltstone, Constance Sandstone, Mullera Formation, Tidna Sandstone.|Unconformably underlain by the McNamara Group.||
17123|South Nicholson Group|68020|5|Briefly described|p128|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin. Includes oolitic Fe deposits.|||?Includes Mullera Formation?|||
17123|South Nicholson Group|68146|5|Briefly described|p2, p5, p21, p28-29, p35, p196-198|Proterozoic|Proterozoic|Currently accepted (tentative) age is based on correlation with c.1500-1400 Ma Roper Group in NT. Age determinations in this study do not provide an improved understanding of the depositional ages of the Group.|||Wild Cow, Accident Subgroups.|Unconformably overlies Doomadgee Formation (Fickling Group). Correlated with the Roper Group.|Siliciclastic sediments.|
17123|South Nicholson Group|68542|6|Mentioned|p6|||||||Overlies Upper McNamara Group||
17123|South Nicholson Group|68553|6|Mentioned|Map legend; schematic diagram.|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin.||||||
17123|South Nicholson Group|68575|5|Briefly described|p3, p11, p19, p27-33, p125, p128|||South Nicholson Basin. Maximum depositional age of 1602 +/- 22 Ma (from basal Hedleys Sandstone), but post-dates the 1550-1500 Ma Isan Orogeny.|<1500 Ma.||Wild Cow Subgroup; Tidna, Hedleys Sandstones.|||
17123|South Nicholson Group|68576|5|Briefly described|Q_2: p6|||Lawn Hill Platform, Mount Isa Inlier.||||Unconformably overlies McNamara Group.||
17123|South Nicholson Group|69417|5|Briefly described|p2:5-6|Calymmian|Calymmian|South Nicholson/Lawn Hill Basin.|||||Predominantly shallow marine sandstones.|12-JUL-16
17123|South Nicholson Group|69423|6|Mentioned|p8:4 Fig.8.7|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin.||||||12-JUL-16
17123|South Nicholson Group|69430|5|Briefly described|p15:26|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin.||||Correlated with Roper Group (McArthur Basin).||12-JUL-16
17123|South Nicholson Group|69433|6|Mentioned|p18:4, 10|||South Nicholson Basin.||||Unconformably overlies Doomadgee Formation (Fickling Group), McNamara and Benmara Groups, Lawn Hill Platform.||12-JUL-16
17123|South Nicholson Group|69434|4|Described|p19:2-7|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin. Correlated with the Roper Group, dated at 1492 +/- 4 Ma.|1500-1400 Ma.||Accident and Wild Cow Subgroups.|Unconformably overlies Murphy Metamorphics, McNamara and (probably) Benmara Groups. Is overlain unconformably by Bukalara Sandstone, Wonarah Formation and Helen Springs Volcanics.||12-JUL-16
17123|South Nicholson Group|69443|5|Briefly described|p28:5, 12, 21-22|Calymmian|Mesoproterozoic|South Nicholson Basin.||||Is overlain unconformably by Bukalara Sandstone and Wonarah Formation /Barkly Group (also ?disconformably). Correlative of Renner Group.||12-JUL-16
17123|South Nicholson Group|69445|5|Briefly described|p30:5|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin.||||Overlain unconformably by Peaker Piker Volcanics (now Helen Springs Volcanics). Is overlain unconformably by Colless Volcanics.||12-JUL-16
17123|South Nicholson Group|69591|5|Briefly described|p27, p29, p52-54, p88, p111|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin, Mount Isa Province. Age is not certain: probably Calymmian to Ectasian. The correlate (Mainoru Formation) has been dated at 1492 +/- 4 Ma. Deformed into a series of domes and basins, and cut by E- to ENE-trending faults, with minor local thrusting.|||Wild Cow, Accident Subgroups.|Is overlain unconformably by Bukalara Sandstone. Correlated with Roper Group, and Mainoru Formation in NT.||
17123|South Nicholson Group|69673|6|Mentioned|p56, p57|||Age is based on correlation with Roper Group.|1500-1400 Ma||Includes Wild Cow Subgroup, Accident Subgroup|Correlated with Roper Group.||
17123|South Nicholson Group|69928|6|Mentioned|p224|Mesoproterozoic|Mesoproterozoic|Mount Isa region. Postulated deposition resulting from Anmatjira Event (1500-1400 Ma) in the Arunta Inlier.||||||
17123|South Nicholson Group|70822|6|Mentioned|p104|||||||Correlated with Roper Group||
17123|South Nicholson Group|70849|5|Briefly described|Map legend.|Calymmian|Calymmian|South Nicholson Basin.|||Constance, Mittiebah Sandstones; Mullera Formation.|Unconformably overlies Fickling Group. Is overlain unconformably by Bukalara Sandstone.|Sandstone, siltstone, greywacke.|
17123|South Nicholson Group|70897|4|Described|p36-48 and Figs.1.7.1-9|Mesoproterozoic|Mesoproterozoic|Preserved over c. 20 000 km2 in far NW QLD and adjacent NT. Highly variable thickness to over 2000m: evidence suggests positive basement relief during early stages of deposition of this unit. Thickens to S and SW.|||Constance Sandstone; Pandanus, Wallis, Bowthorn, Train Range Ironstone, Members.|Roper Superbasin. Unconformably overlies McNamara Group and all units of the Fickling Group. Broadly correlated with Roper Group.|Quartz sandstone interstratified with siltstone and shale. Mainly medium- to coarse-grained, fluvial and shallow-marine quartz sandstone in lower half; deeper marine, finer-grained lithologies (glauconitic sandstone, siltstone, shale) in upper half.|
17123|South Nicholson Group|70968|5|Briefly described|v, p2-3, p131 Fig.118, p132, p137|Ectasian|Calymmian|South Nicholson Basin. Not included in this study. Probable correlative of the Winton package (i.e. Roper, Tijunna and Renner Groups). Up to 6500m thick.|||Accident, Wild Cow Subgroups.|||
17123|South Nicholson Group|71059|6|Mentioned|p2|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin.||||Equivalent to the Roper Group.||
17123|South Nicholson Group|71369|4|Described|p1-p2, p4-8, p10, p12, p23, p46-50|Ectasian|Calymmian|South Nicholson Basin. Composite measured sections. Faulting and folding after ~1324 Ma described in some detail. Geologic history summarised.|||Wild Cow, Accident Subgroups.|Unconformably overlies McNamara and Fickling Groups. Correlated with Roper Group.|The lower half is predominantly thick-bedded, well-indurated sandstone; the upper half is mainly thinly-bedded or laminated mudstone.|20-FEB-18
17123|South Nicholson Group|71488|6|Mentioned|p142|||South Nicholson Basin.||||||
17123|South Nicholson Group|71502|6|Mentioned|p2|||||||||
17123|South Nicholson Group|71606|5|Briefly described|p137|Calymmian|Calymmian|South Nicholson Basin.||||Underlain unconformably by Fickling Group.||
17123|South Nicholson Group|71632|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin.|||||Quartzose sandstone, siltstone, shale.|
17123|South Nicholson Group|72297|5|Briefly described|p712|||South Nicholson Basin.|||Train Range Ironstone Member.|||
17123|South Nicholson Group|72408|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet.|||Includes Accident Subgroup and Wild Cow Subgroup.|||
17123|South Nicholson Group|72414|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.|||Includes Accident Subgroup and Wild Cow Subgroup.|||
17123|South Nicholson Group|72415|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.|||Includes Accident Subgroup and Wild Cow Subgroup.|||
17123|South Nicholson Group|72416|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet Geological Compilation Series.|||Includes Accident Subgroup and Wild Cow Subgroup.|||
17123|South Nicholson Group|72418|5|Briefly described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet.|||Includes Accident Subgroup, Wild Cow Subgroup.|||
17123|South Nicholson Group|72421|5|Briefly described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.|||Includes Accident Subgroup, Wild Cow Subgroup.|||
17123|South Nicholson Group|72422|5|Briefly described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.|||Includes Accident Subgroup, Wild Cow Subgroup.|||
17123|South Nicholson Group|72423|5|Briefly described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet Geological Compilation Series.|||Includes Accident Subgroup, Wild Cow Subgroup.|||
17123|South Nicholson Group|72526|5|Briefly described|p1-5, 8, 20, 33, 40, 46,56,67,p85-86|Mesoproterozoic|Mesoproterozoic|Shown as located in the South Nicholson Basin. Inferred to be same age as Roper Group. LA-ICP-MS maximum depositional ages from undifferentiated borehole samples range from 1540+/-14- Ma to 1510+/-51 Ma.|c. 1500 Ma to 1313 Ma inferred||Wild Cow Subgroup and Accident Subgroup|Shown as partially and unconformably overlying Benmara Group, Fickling Group and McNamara Group.||
17123|South Nicholson Group|72527|4|Described|p1, p3, p10-12, p20, p27, p34, p41.|Mesoproterozoic|Mesoproterozoic|No tuffs identified in this Group, so no direct age constraints, only maximum depositional ages. Maximum age from underlying units: 1589+/-3 Ma. Maximum depostional ages range between 1750 and 1570 Ma. Best estimates on depositional age range is 1500-1400 Ma. See also p49, p56, p63, p71, p78, p86, p119, p140, p161, p193, p195-196.|c. 1500-1400 Ma.||Accident Subgroup and Wild Cow Subgroup.|Unconformably overlies McNamara Group, Nathan Group, Fickling Group, Surprise Creek Formation.||
17123|South Nicholson Group|72889|6|Mentioned|p6 Fig.i.|||||||||
17123|South Nicholson Group|72912|4|Described|p5 Fig.3, p12-15, p20-26.|Mesoproterozoic|Mesoproterozoic|Present in the Carrara Sub-basin. Seismically imaged in Murphy Province, Calvert Superbasin equivalent and under Georgina Basin sediments. Considered to be part of the Roper Superbasin. See also p33 Fig.12, p34-35, p45-49.|||Accident Subgroup and Wild Cow Subgroup.|Shown as unconformably overlying Benmara and Fickling Groups,and overlying McNamara Group. Correlated with Roper Group.|Includes siltstone, sandstone, dolomitic siltstone, ironstone.|15-MAR-21
17123|South Nicholson Group|72913|5|Briefly described|p7, p9.|Mesoproterozoic|Mesoproterozoic|Shown as being in the west, central and eastern part of the South Nicholson Basin.|||Wildcow Subgroup and Accident Subgroup|Shown as overlying Fickling Group, McNamara Group.|Includes sandstone, siltstone,|
17123|South Nicholson Group|72919|6|Mentioned|p. 1, 3, 5, 24-25, 31-32, 34-36, 39...|Ectasian|Calymmian|There are considerable 'cross-border' discrepancies between stratigraphic frameworks for this unit in the NT and QLD. May include the Caufield beds. Deposition bracketed to between ca. 1483-1470 Ma and ca. 1266 Ma based on comprehensive SHRIMP U-Pb zircon and xenotime geochronology presented by Anderson et al. (2019a, b) and Kositcin and Carson (2019). This data supports temporal correlation with the Roper Group. Two new U-Pb SHRIMP zircon maximum depositional ages of 1605 +/- 18 Ma and 1610 +/- 35 Ma were presented herein for unnamed sandstones from undifferentiated intervals of this unit. These were interpreted a probably belonging to the Constance Sandstone or equivalent. More locations: p. 41-43, 47, 56-57, 63-64, 70, 77, 85-86, 93-95.|Between ca. 1483-1470 Ma and ca. 1266 Ma||Accident Subgroup, Wild Cow Subgroup and units therein|Unconformably underlain by Widdallion Sandstone Member (McNamara Group). Unconformably overlain by Bukalara Sandstone.||
17123|South Nicholson Group|72967|6|Mentioned|p2, p5|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin.|||Mullera Formation, Constance Sandstone, Mittebah Sandstone|||
17123|South Nicholson Group|73042|6|Mentioned|p1, p2, p4, p6-7, p9|Ectasian|Calymmian|South Nicholson Basin region, Roper Superbasin. Geochronological constraint based on U-Pb zircon and xenotime age data of Anderson et al. (2019) and Carson et al. (2020). See also p9, p11, p14.|ca 1483 Ma and ca 1266 Ma||Accident Subgroup and Wildcow Subgroup, and units therein.|Unconformably underlain by the Doomadgee Formation (Fickling Group).||23-JUN-22
17123|South Nicholson Group|73043|6|Mentioned|p7 Fig.2|Mesoproterozoic|Mesoproterozoic||||Includes Constance Sandstone, Top Lily Sandstone.|||
17123|South Nicholson Group|73083|6|Mentioned|p6, p9, p22, p34-35, p39, p44, p69, p71|||Extend southward beneath the Georgina Basin. Includes sedimentary iron occurrences of the 'Constance Range type' composed of hematite, chamosite, and siderite, in places enriched by lateritic weathering. Mostly of uniform and very low magnetisation.|||Wild Cow Subgroup, Crow Formation, Mittiebah Sandstone||Includes siliciclastics.|
17123|South Nicholson Group|73098|6|Mentioned|p5|||South Nicholson region. Overlies sedimentary package composed of the Paleoproterozoic Isa Superbasin.||||||
17123|South Nicholson Group|73144|6|Mentioned|p8, p13, p19, p23, p43-44, p47-49|Calymmian|Calymmian|South Nicholson Basin. Fluvial to shallow marine. May be similar in age to the Roper Group.|||Accident and Wild Cow subgroups, Tidna, Elizabeth, Constance, Burangoo, and Hedleys sandstones, Mullera, Wallis, and Pandanus formations, and members therein|||
17123|South Nicholson Group|73412|6|Mentioned|p3, 8, 18|||||||Lateral equivalent to the Roper Group.||
17150|Speewah Group|22547|4|Described|p21|Orosirian|Orosirian|Geological province: Speewah Basin. Previously part of Kimberley Basin, now redefined as Speewah Basin. Age: 1835- 1805 Ma. Thickness: 1500 m. Overlies Lamboo Complex, overlain by Kimberley Group||||||14-NOV-06
17150|Speewah Group|22716|5|Briefly described|table4, p232|Orosirian|Orosirian|Age: 1835Ma.||||||04-DEC-06
17150|Speewah Group|22754|4|Described|p10 Tb.2|Paleoproterozoic|Paleoproterozoic|Age: 1835-1830 Ma.||||||07-NOV-08
17150|Speewah Group|23125|5|Briefly described|Table.1|||||||||
17150|Speewah Group|23323|5|Briefly described|p455 Fig. 3, p456 Table 1|Orosirian|Orosirian|Age: 1834 +/- 3 Ma. In the Kimberley Craton/Western Zone.||||||07-FEB-07
17150|Speewah Group|23383|6|Mentioned|p18, p17|||Overlain by the Kimberley Group. Age 1834 Ma.  Geological Province: Speewah Basin.||||||25-JAN-05
17150|Speewah Group|23722|4|Described|p17|Proterozoic|Proterozoic|Early Proterozoic.   Thickness: 360m.   Geological Province: Kimberley Basin||||||
17150|Speewah Group|23751|4|Described|p20|Paleoproterozoic|Paleoproterozoic|Age: 1835-1830 Ma (SHRIMP U-Pb). Geological Province: Speewah Basin.||||||07-NOV-08
17150|Speewah Group|24173|5|Briefly described|p19|||Of the Halls Creek Orogen. Felsic volcanics. Overlies Whitewater Volcanics. Geological Province: Speewah Basin. Age: 1834 +/- 3Ma (AGSO/OZCHRON).||||||06-APR-05
17150|Speewah Group|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Sandstone, feldspathic sandstone, siltstone and mudstone; minor rhyolitic volcaniclastic sandstone. Age: c.1835Ma.  Geological Province: Speewah Basin.||||||07-NOV-08
17150|Speewah Group|24572|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Clastic sedimentary rocks.  Age: c.1835Ma.  Geological Province: Halls Creek Orogen.||||||07-NOV-08
17150|Speewah Group|29380|6|Mentioned|p8|||||||||
17150|Speewah Group|29845|6|Mentioned|p113|||||||||
17150|Speewah Group|30097|6|Mentioned|Fig.54|||Also Tables 23,24,25||||||
17150|Speewah Group|30525|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17150|Speewah Group|30533|5|Briefly described|p15|||On Table 2. Age between Whitewater and Carson Volcanics.||||||
17150|Speewah Group|30558|6|Mentioned|p36|||||||||
17150|Speewah Group|30878|6|Mentioned|p51|||Precambrian. Stratigraphic table||||||
17150|Speewah Group|30892|6|Mentioned|Table 1|||Carpentarian||||||
17150|Speewah Group|30893|5|Briefly described|p205|||Carpentarian. Lithology||||||
17150|Speewah Group|30894|4|Described|p249|||Carpentarian||||||
17150|Speewah Group|30895|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17150|Speewah Group|30896|4|Described|p13|||Carpentarian||||||
17150|Speewah Group|30897|6|Mentioned|p12|||Stratigraphy||||||
17150|Speewah Group|30898|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17150|Speewah Group|31226|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17150|Speewah Group|31393|6|Mentioned|Pl.25|||||||||
17150|Speewah Group|31404|6|Mentioned|p257|||||||||
17150|Speewah Group|31439|6|Mentioned|p293|||||||||
17150|Speewah Group|32108|6|Mentioned|p231|||||||||
17150|Speewah Group|32659|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17150|Speewah Group|32660|4|Described|Table 3|||||||||
17150|Speewah Group|32663|6|Mentioned|p10|||||||||
17150|Speewah Group|32664|6|Mentioned|Map legend|Carpentarian|Carpentarian|Mention in notes||||||
17150|Speewah Group|32728|6|Mentioned|Fig.3|||||||||
17150|Speewah Group|34137|6|Mentioned|p7|||||||||
17150|Speewah Group|34462|6|Mentioned|p8|||||||||
17150|Speewah Group|36003|6|Mentioned|p1028|||||||||
17150|Speewah Group|36551|6|Mentioned|Table 10|||||||||
17150|Speewah Group|36885|3|Fully described|p182|||||||||
17150|Speewah Group|36898|6|Mentioned|p183|||||||||
17150|Speewah Group|36902|6|Mentioned|p11|||||||||
17150|Speewah Group|37462|3|Fully described|p235|||||||||
17150|Speewah Group|38482|6|Mentioned|Table 1|||||||||
17150|Speewah Group|38988|6|Mentioned|Fig.4|||||||||
17150|Speewah Group|41158|6|Mentioned|p36|||See also p65.||||||04-DEC-06
17150|Speewah Group|41987|5|Briefly described|Fig.4 P74|||||||||
17150|Speewah Group|42149|5|Briefly described|Table 1 P709|||||||||
17150|Speewah Group|42710|5|Briefly described|map legend|Proterozoic||||||||
17150|Speewah Group|42811|4|Described|p20, Fig.5|||||||||
17150|Speewah Group|42814|4|Described|p12|||||||||
17150|Speewah Group|42815|5|Briefly described|map|Proterozoic||||||||
17150|Speewah Group|43281|5|Briefly described|Map legend||Proterozoic|||||||
17150|Speewah Group|43561|6|Mentioned|p1437|||||||||
17150|Speewah Group|43595|5|Briefly described|p442|||||||||
17150|Speewah Group|43631|6|Mentioned|p10|||Kimberley region||||||
17150|Speewah Group|43666|6|Mentioned|p52,Table 2||Neoproterozoic|||||||
17150|Speewah Group|43853|5|Briefly described|Map Legend||Proterozoic|||||||
17150|Speewah Group|43854|5|Briefly described|Map Legend||Proterozoic|||||||
17150|Speewah Group|43863|5|Briefly described|map legend|Proterozoic|Proterozoic|||||||
17150|Speewah Group|44140|4|Described|p293, p295-299, p304|Paleoproterozoic|Paleoproterozoic|Kimberley Basin. ~1 km thick.|>1762 +/- 15 Ma (Rb-Sr).||O'Donnell, Tunganary  Formations; Valentine, Luman Siltstones; Lansdowne Arkose.|Unconformable on the Lamboo Complex and Hooper Complex (also faulted over the latter), and Whitewater Volcanics. Is overlain "subconformably" (?) by Kimberley Group. Is intruded by Hart Dolerite.|Quartzose & feldspathic arenite, interbedded with mudstone & minor amounts of acid volcanics; fluvial sands grade into fluvial and shallow-marine, then into deep-water silts.|08-MAR-18
17150|Speewah Group|44155|6|Mentioned|p236 Fig.3-35, p240, p241 Tb.3-4, p250|Paleoproterozoic|Paleoproterozoic|See also p252, p254 Fig.3-40.|||Includes O'Donnell Formation.|Overlies Whitewater Volcanics.||
17150|Speewah Group|44230|5|Briefly described|Map Legend||Proterozoic|||||||
17150|Speewah Group|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Includes the O'Donnell and Tunganary Formations, Valentine Siltstone, Lansdowne Arkose, Luman Siltstone and Bedford Sandstone. Age: c.1835Ma. geological Province: Speewah Basin.||||||07-NOV-08
17150|Speewah Group|44317|14|Not recorded|p.6||Carpentarian|||||||
17150|Speewah Group|44318|14|Not recorded|map legend||Carpentarian|Carpentarian.||||||
17150|Speewah Group|44363|4|Described|p.3,7,8,9,12,13-28||Paleoproterozoic|Lower Proterozoic. units.||||||07-NOV-08
17150|Speewah Group|44364|14|Not recorded|map legend|||||||||
17150|Speewah Group|44366|14|Not recorded|p.11, Table 1||Carpentarian|||||||
17150|Speewah Group|44367|14|Not recorded|map legend|||(Reprinted 1971).||||||
17150|Speewah Group|44397|14|Not recorded|p.9,17,19, Table 2||Carpentarian|||||||
17150|Speewah Group|44867|5|Briefly described|Map Legend||Mesoproterozoic|||||||
17150|Speewah Group|44868|5|Briefly described|Map Legend||Proterozoic|||||||
17150|Speewah Group|45047|5|Briefly described|p28|||See also p29.||||||04-DEC-06
17150|Speewah Group|48931|4|Described|p45|||||||||
17150|Speewah Group|48950|6|Mentioned|p36|||||||||
17150|Speewah Group|50009|5|Briefly described|p34|Paleoproterozoic|Paleoproterozoic|Underlies the Kimberley Group unconformably and disconformably. Sedimentary rocks. Geological Province: Kimberley Basin.||||||07-NOV-08
17150|Speewah Group|50437|6|Mentioned|p4.1|||||||||
17150|Speewah Group|60533|5|Briefly described|p591, 592 Fig. 1, 593|Paleoproterozoic|Paleoproterozoic|Age: ca. 1835-1800Ma. Geological Province: Speewah Basin.||||||07-NOV-08
17150|Speewah Group|60714|6|Mentioned|p111|||Speewah Basin.|||Includes O'Donnell and Tunganary Formations, Valentine and Luman Siltstones, Landsdowne Arkose and Bedford Sandstone.|Unconformably overlies Hooper and Lamboo Complexes. Is intruded by Hart Dolerite. Is overlain unconformably by Kimberley Group.||
17150|Speewah Group|60724|5|Briefly described|p4, p5 Fig. 2|||Intruded by Hart Dolerite. Age: 1.83Ga.||||||
17150|Speewah Group|60844|5|Briefly described|pp15-16. |Late Paleoproterozoic|Late Paleoproterozoic|Speewah Basin. Exposed along the southeast and southwest margins of the Kimberley Region.|c.1835 - 1820 Ma.||Includes Bedford Sandstone.|Is overlain by Kimberley Group.||
17150|Speewah Group|63866|5|Briefly described|p127, p130, p133|||Western Zone, Halls Creek Orogen. Deposited in fluvial to shallow marine environments.|||Includes the Valentine Siltstone.|Unconformably overlies the Whitewater Volcanics. Disconformably overlain by the Kimberley Group. Intruded by the Hart Dolerite.|Pebbly conglomerate, sandstone and siltstone.|
17150|Speewah Group|64104|6|Mentioned|p76 fig 10|Paleoproterozoic|Paleoproterozoic|||||||
17150|Speewah Group|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Sandstone, feldspathic sandstone, siltstone, and mudstone; minor rhyolitic volcaniclastic sandstone.||||||09-DEC-08
17150|Speewah Group|64724|5|Briefly described|p45, Fig.5|Orosirian|Orosirian|Deposited onto the Kimberley Craton at ~1835 Ma during the early stages of the Halls Creek Orogeny.||||||
17150|Speewah Group|64748|5|Briefly described|p268, p269 Fig 2, p278|Late Paleoproterozoic|Orosirian|Unconformity surface at the top of unit; intruded by Hart Dolerite; includes O'Donnell Formation, Tunganary Formation, Valentine Siltstone, Lansdowne Arkose, Lumen Siltstone, Bedford Sandstone.||||||
17150|Speewah Group|66845|4|Described|p536 Fig.2, p537|Paleoproterozoic|Paleoproterozoic|Felsic volcanic unit dates indicate this unit was deposited at 1834+/-3 Ma (Page et al. 1994)|c. 1835 Ma|||Unconformably overlies Western zone of Lamboo Complex and contiguous Hooper Complex; with Lamboo Complex, is overlain by Kimberley Group and its equivalents|Low-grade metasedimentary and metavolcanic rocks|21-JUL-15
17150|Speewah Group|66846|6|Mentioned|p549 Fig.2|Orosirian|Orosirian|In the Western Zone of the Lamboo Complex.|||||Terriginous clastic rock.|
17150|Speewah Group|67563|5|Briefly described|p120 Fig.1|||Exposed as the lowest unit of the Kimberley Basin.|||Includes Bedford Sandstone, Luman Siltstone, Lansdowne Arkose, Valentine Siltstone, Tunganary Formation, and O'Donnell Formation.|Overlain by the Kimberley Group.||20-JAN-17
17150|Speewah Group|68078|4|Described|p1, p5, p8, p11, p14 figure 10, p17, p23|Paleoproterozoic|Paleoproterozoic|Age is from felsic volcanic unit within the group.|1835 +/- 3 Ma (SHRIMP)||Includes Valentine Siltstone, Bedford Sandstone, Lansdowne Arkose, Luman Siltstone, Tunganary Formation, O'Donnell Formation|Intruded by Hart Dolerite, unconformably/(disconformably?) overlain by Kimberley Group, unconformably overlies Marboo Formation, Whitewater Volcanics and Paperbark Supersuite|Felsic volcanic rocks, terriginous clastic rock. Formations within the group are comprised of quartz and lithic sandstone, feldspathic sandstone, arkose and interbedded siltstone.  Cross bedding present in sandstones. Around 1.5km thick on average.|13-SEP-22
17150|Speewah Group|68244|6|Mentioned|p661|||Mount House area, Kimberley region.||||||
17150|Speewah Group|68992|5|Briefly described|p498 Fig.1, p499|||Kimberley Basin.|||Includes Bedford Sandstone, Luman Siltstone, Lansdowne Arkose, Valentine Siltstone, Tunganary Formation, and O'Donnell Formation.|Unconformably underlain by the Hooper Complex and the Lamboo Complex. Overlain by the Kimberley Group.||
17150|Speewah Group|69003|5|Briefly described|p5, p18, p20|Paleoproterozoic|Paleoproterozoic|Speewah Basin. Halls Creek Orogen.|||||Mainly interbedded siltstones and quartz, lithic, and feldspathic sandstones; minor volcanic and volcaniclastic rocks.|
17150|Speewah Group|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Speewah Basin. ~1500m thick.|||Includes Bedford Sandstone, Luman Siltstone, Lansdowne Arkose, Valentine Siltstone, Tunganary Formation, O'Donnell Formation.||Sandstone, siltstone, and mudstone; minor rhyolitic volcaniclastic siltstone|21-JUL-15
17150|Speewah Group|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_geologyp08_lut.csv.|||Includes Bedford Sandstone, Luman siltstone, Lansdowne Arkose, Valentinte Siltstone, Tunganary Formation, O'Donnell Formation.||Undivided; sandstone, feldspathic sandstone, siltstone and mudstone; minor rhyolitic volcaniclastic sandstone.|
17150|Speewah Group|69435|6|Mentioned|p20:1|||Possible correlative of the Fitzmaurice Group.||||||12-JUL-16
17150|Speewah Group|69585|4|Described|p1-5, p7, p10-16, p27, p30-32|Orosirian|Orosirian|Overlies the western Lamboo Province; crops out along its eastern margin and west Kimberley. Fluvial and shallow-marine succession, deposited during and immediately after the 1835-1810 Ma Halls Creek Orogeny. Typically ~1.5km thick. The authors propose derivation largely from Paperbark Supersuite granites; deposition in a retro-arc foreland basin. Deformed during Yampi and King Leopold Orogenies. Age from Valentine Siltstone.|1835 +/- 3 Ma (Page and Sun, 1994).||O'Donnell, Tunganary Formations; Valentine, Luman Siltstones; Lansdowne Arkose; Bedford Sandstone.|Unconformably overlies Whitewater Volcanics and Paperbark Supersuite. Is overlain unconformably by Kimberley Group. Is intruded by Hart Dolerite.|Dominantly fluvial quartz and lithic sandstone, feldspathic sandstone and arkose, with interbedded siltstone.|
17150|Speewah Group|69597|6|Mentioned|p3, p4, p5 fig 2b|||1.5 km thick. Unconformably deposited in the 1835 Ma Speewah Basin during the Halls Creek Orogeny.||||Overlain by the Kimberley Group. Intruded by the Hart Dolerite.||
17150|Speewah Group|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Halls Creek Orogen. Of Speewah Basin. Thickness: 1500m. King Leopold Orogeny D1/M1; Yampi Orogeny D1/M1; King Leopold Orogeny D1/M1; Yampi Orogeny D1/M1. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 250k_geologyp_lut.csv, 500k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 100k_interpgeol_lut.csv and geochron files.|1850-1784 Ma (Inferred)||Includes Lansdowne Arkose, Luman Siltstone, Tunganary Formation, Valentine Siltstone, Bedford Sandstone, O'Donnell Formation.|Overlain unconformably by Kimberley Group. Underlain unconformably by Hooper Complex, Lamboo Complex.|Undivided; sandstone, feldspathic sandstone, siltstone, and mudstone; minor rhyolitic volcaniclastic sandstone|
17150|Speewah Group|69660|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Speewah Basin, Kimberley Craton.|||Includes O'Donnell and Tunganary Formations; Valentine and Luman Siltstones; Lansdowne Arkose.||Sandstone, siltstone, mudstone; minor conglomerate.|
17150|Speewah Group|70126|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Speewah Basin; North Australian Craton.|||O'Donnell, Tunganary Formations; Valentine, Luman Siltstones; Lansdowne Arkose.||Sandstones, siltstones, mudstones, arkose and conglomerate.|
17150|Speewah Group|70154|6|Mentioned|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 2_5m_geologyp98_lut.csv.|||Luman Siltstone, O'Donnell Formation, Lansdowne Arkose, Tunganary Formation, Valentine siltstone|||
17150|Speewah Group|70731|5|Briefly described|p268,270,272,274,276,278|Orosirian|Orosirian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton. Siliciclastic sedimentary and minor felsic volcanic rocks. In contact with Whitewater Volcanics. Provenance from the SE and W basin margins dominated by Paleoproterozoic 1880-1850 Ma detrital zircons (Hollis et al., 2014). Difference in provenance and regional unconformity with overlying Kimberley Group reflect major change in basin-forming processes (extensional collapse of lithsphere following Halls Creek Orogeny; Hollis et al., 2014).||||Overlain unconformably by Kimberley Group/King Leopold Sandstone. Intruded by Hart Dolerite.||
17150|Speewah Group|70812|4|Described|p3, p6, p9, p19, p27, p30, p43|Orosirian|Orosirian|Western Zone of the Halls Creek Orogen, Lamboo Province. This unit features no mineral deposits; however, base metal mineralisation associated with felsic volcanism appears towards the base of this unit.|c. 1850-1800 Ma||Includes the o'Donnell Formation, Valentine Sandstone, Tunganary Formation, Luman Sandstone, Bedford Sandstone.|Overlies the Paperbark Supersuite. Unconformably overlain by the Kimberley Group.|Sandstones, siliciclastic sedimentary rocks and minor felsic volcanics.|
17150|Speewah Group|70826|6|Mentioned|p5 tbl 2, p9, p10|||Speewah Basin.||||Is intruded by the Hart Dolerite.||
17150|Speewah Group|70851|4|Described|p4-p6, p12, p16-p20, p24, p29|Paleoproterozoic|Paleoproterozoic|Western Zone, Lamboo Province. Geophysical response is discussed.|c. 1850-1800 Ma||Includes the O'Donnell Formation, Valentine Sandstone, Tunganary Formation, Luman Sandstone and the Bedford Sandstone.|Unconformably overlain by the King Leopold Sandstone. Intruded by the Hart Dolerite.||27-MAR-23
17150|Speewah Group|71113|5|Briefly described|p101-102,110|Orosirian|Orosirian|Geological province: Western Zone, Lamboo Province, Halls Creek Orogen. Siliciclastic sedimentary rocks deposited on Western Zone rocks during Halls Creek Orogeny.||||Overlain unconformably by Kimberley Group.||
17150|Speewah Group|71140|6|Mentioned|p101-102, 110|Orosirian|Orosirian|Western Zone, Lamboo Province, Halls Creek Orogen. Deposited during the Halls Creek Orogeny.|||||Siliciclastic sedimentary rocks.|
17150|Speewah Group|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Halls Creek Orogen, King Leopold Orogen. Of Speewah Basin. Thickness: 1500m. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv, 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyp_lut.csv, 1m_interpgeop_lut.csv, 100k_interpgeol_lut.csv, 1m_geologyl12_lut.csv and geochron files.|1835+\-3 to 1979 Ma (isotopic-inferred)||Includes Bedford Sandstone, Lansdowne Arkose, Luman Siltstone, O'Donnell Formation, Tunganary Formation, Valentine Siltstone.|Overlain unconformably by Kimberley Group.|Lithic and feldspathic sandstone, quartz sandstone, chloritic and micaceous siltstone, shale; minor rhyolitic ashstone and tuff|
17150|Speewah Group|71281|4|Described|p419, p421-423, p425, p429-432|Paleoproterozoic|Paleoproterozoic|Speewah Basin. 1.5km thick succession. Poorly outcropping. Represents a fluviatile to marine, transgressive and regressive event. Zircons are dominated by grains from the Paperbark Supersuite.|||O'Donnell, Tunganary Formations; Valentine, Luman Siltstones; Lansdowne Arkose; Bedford Sandstone.|Unconformably overlies Whitewater Volcanics. Is overlain unconformably by the Kimberley Group. Is intruded by Hart Dolerite.|Predominantly low-grade metasedimentary siliciclastic rocks: conglomerates and rippled and cross-bedded fluviatile to marine deposits.|
17150|Speewah Group|71397|5|Briefly described|p5-6|Orosirian|Orosirian|Geological province: Western Zone, Lamboo Province, Halls Creek Orogen. Mylonites on the margins of Speewah Group likely associated with c. 1000-800 Ma Yampi Orogeny (Tyler and Griffin, 1990; Tyler et al., 1995).||||||
17150|Speewah Group|71784|6|Mentioned|p83-84||Proterozoic|||||||
17150|Speewah Group|71811|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, North Australian Craton.|||O'Donnell, Tunganary Formations; Valentine, Luman Siltstones; Lansdowne Arkose; Bedford Sandstone.|Is intruded by Hart Dolerite.||
17150|Speewah Group|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Speewah Basin.|Max age 1835+/-3 Ma, min ~1797 Ma.||||Sandstone, siltstone, and claystone; minor rhyolitic volcaniclastic siltstone.|
17150|Speewah Group|72437|5|Briefly described|P12, p113||||||Includes the Valentine Siltstone, O'Donnell Formation.||Contains a very minor component of felsic igneous rocks.|
17150|Speewah Group|72490|5|Briefly described|p1-6, p11, p13|Orosirian|Orosirian|Age is maximum age of deposition. Detrital zircons show a dominant ca. 1860 Ma age component that reflects derivation from the Paperbark Supersuite.|1814 +/- 10 Ma||Bedford Sandstone, Luman Siltstone, Lansdowne Arkose, Valentine Siltstone, Tunganary Formation, O'Donnell Formation|Intruded by Hart Dolerite.|Siliciclastic rocks.|
17150|Speewah Group|73255|6|Mentioned|p533 Fig.1|Paleoproterozoic|Paleoproterozoic|||||||
17153|Spencer Sandstone|14019|5|Briefly described|p4 Fig. 3|||Of the Auvergne Group.  Geological Province: Victoria Basin.||||||
17153|Spencer Sandstone|24122|5|Briefly described|p4 Fig.3|||Of Auvergne Group.  Geological Province: Victoria Basin.||||||
17153|Spencer Sandstone|24297|5|Briefly described|p4 Fig.3|||Of Auvergne Group.  Geological Province: Victoria Basin.||||||
17153|Spencer Sandstone|24441|5|Briefly described|p1 Fig. 1|Mesoproterozoic|Mesoproterozoic|Of the Auvergne Group. Overlies Lloyd Creek Formation; overlain by Shoal Reach Formation. Geological Province: Victoria Basin.||||||
17153|Spencer Sandstone|24442|5|Briefly described|p50 Fig. 1|||Of the Auvergne Group.  Geological Province: Victoria Basin.||||||
17153|Spencer Sandstone|32170|6|Mentioned|Map legend|Adelaidean|Carpentarian|Adelaidean or Carpentarian||||||
17153|Spencer Sandstone|32307|4|Described|Table 2|||Proterozoic||||||
17153|Spencer Sandstone|32310|6|Mentioned|Map legend|Adelaidean|Carpentarian|Adelaidean/Carpentarian||||||
17153|Spencer Sandstone|32660|5|Briefly described|Table 6|||||||||
17153|Spencer Sandstone|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Auvergne Group.  Quartz sandstone, silty sandstone, dolomitic sandstone.||||||02-DEC-04
17153|Spencer Sandstone|32700|4|Described|Table 1|||Lithology p14 Refers Randal (1962).||||||04-DEC-06
17153|Spencer Sandstone|32701|4|Described|Table 1|||Adelaidean. See p9. Of the Auvergne Group.||||||04-DEC-06
17153|Spencer Sandstone|32728|6|Mentioned|Fig.14|||||||||
17153|Spencer Sandstone|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
17153|Spencer Sandstone|45112|6|Mentioned|Table 6|||||||||
17153|Spencer Sandstone|48938|2|Defined|p50|Proterozoic|Proterozoic|Adelaidean? Measured section p97. See also p7.||||||04-DEC-06
17153|Spencer Sandstone|48942|3|Fully described|p71|||||||||
17153|Spencer Sandstone|60006|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Victoria Basin. Of Auvergne Group. Overlies Lloyd Creek Formation. Overlain by Shoal Reach Formation and unconformably overlain by Black Point Sandstone Member and Moonlight Valley Tillite.||||||21-JUL-04
17153|Spencer Sandstone|60682|4|Described|p9 Table 2, 10|Cryogenian|Cryogenian|Of Auvergne Group. Conformably overlies Lloyd Creek Formation. Conformably overlain by Shoal Reach Formation. Thickness: 140-170m. Quartz sandstone, silty sandstone, dolomitic sandstone. Geological Province: Victoria Basin.||||||
17153|Spencer Sandstone|60685|5|Briefly described|p4 Fig. 3|Mesoproterozoic|Mesoproterozoic|Of the Auvergne Group. Geological Province: Victoria Basin.||||||
17153|Spencer Sandstone|65331|5|Briefly described|Map legend|Neoproterozoic |Neoproterozoic|Of Auvergne Group, Victoria Basin. Quartz sandstone, silty sandstone, dolomitic sandstone||||||
17153|Spencer Sandstone|65342|6|Mentioned|p11 Fig.13. |||Victoria Basin.||Unit in Auvergne Group.||Ovelies Lloyd Creek Formation. Is overlain by Shoal Reach Formation.||
17153|Spencer Sandstone|67167|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|||Unit in Auvergne Group.|||Quartz sandstone, silty sandstone, dolomitic sandstone.|
17153|Spencer Sandstone|68733|5|Briefly described|p177 Fig.2, p179 Tb.1, p185, p189 Fig.8|Cryogenian|Cryogenian|See also p192. Victoria Basin. Sm-Nd isotope data tabulated.||Of the Auvergne Group.||||06-DEC-17
17153|Spencer Sandstone|69437|5|Briefly described|p22:4-5|Cryogenian|Cryogenian|Victoria/Wolfe Basins, Centralian A Superbasin. Supersequence 1.||||Overlies Lloyd Creek Formation. Is overlain by Shoal Reach Formation.||12-JUL-16
17153|Spencer Sandstone|69441|5|Briefly described|p26:2-3, 5-6|Neoproterozoic|Neoproterozoic|Typically 140-165m thick. Shallow-marine with periods of subaerial exposure. Offset by Pinkerton Range Fault.||Auvergne Group.||Conformably overlies Lloyd Creek Formation. Is overlain conformably/gradationally by Shoal Reach Formation.|Basal thinly-bedded, fine- or medium-grained quartz sandstone; silty sandstone; dolomitic sandstone typical of upper part. Includes halite casts and pseudomorphs.|12-JUL-16
17153|Spencer Sandstone|69442|6|Mentioned|p27:3 Tb.27.1|||||Auvergne Group.||Is overlain unconformably by Big Knob beds and Bullo River Sandstone.||12-JUL-16
17153|Spencer Sandstone|69673|5|Briefly described|p188|||165m thick.||Auvergne Group|||Sandstone, siltstone and dolomitic sandstone.|
17153|Spencer Sandstone|70206|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Victoria Basin.||Auvergne Group|||Quartz sandstone, silty sandstone and dolomitic sandstone.|
17153|Spencer Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
17153|Spencer Sandstone|71302|4|Described|p1,6-7,65-75|Neoproterozoic|Neoproterozoic|Of Victoria Basin. Exposed sporadically within a NE trending belt from the Pinkerton Range to the Victoria River Fault Zone on the  AUVERGNE 1:250 000 map sheet. Up to 165m thick. Probably deposited in a shallow-marine environment with periods of subaerial exposure (Dunster et al., 2000). Sample GA 1957135 (quartz sandstone) yielded an interpreted (weighted mean 207Pb/206Pb) maximum depositional age of 1101+\-11 Ma, and is dominated by detritus in the range ca 1000-1250 Ma. Sample description, locality, zircon description, SHRIMP analyses and results are discussed.||Unit of Auvergne Group.||Overlain by Shoal Reach Formation. Underlain conformably by Lloyd Creek Formation.|Quartz sandstone, silty sandstone and dolomitic sandstone; thinly-bedded, fine- to medium-grained in the lower sequence, and typically more dolomitic to the top.|09-DEC-19
17180|Split Rock Sandstone|22954|6|Mentioned|Fig3p9|||||||||
17180|Split Rock Sandstone|23031|4|Described|31|||Geological province: Georgina Basin. Underlain by Mail Change Limestone, V-Creek Limestone, Age Creek Formation.||||||04-DEC-06
17180|Split Rock Sandstone|23393|5|Briefly described|p23 Fig. 6|Cambrian|Cambrian|Geological Province: Georgina Basin.||||||
17180|Split Rock Sandstone|30479|6|Mentioned|Fig.7|||Stratigraphic relationships||||||
17180|Split Rock Sandstone|30914|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
17180|Split Rock Sandstone|31287|6|Mentioned|p430|||Refers Opik (1956).||||||04-DEC-06
17180|Split Rock Sandstone|31396|6|Mentioned|Fig.3|||||||||
17180|Split Rock Sandstone|33111|4|Described|p42|||Mention p28.||||||04-DEC-06
17180|Split Rock Sandstone|34287|6|Mentioned|Fig.3|||||||||
17180|Split Rock Sandstone|34395|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
17180|Split Rock Sandstone|35054|6|Mentioned|Table 23|||||||||
17180|Split Rock Sandstone|35553|6|Mentioned|p153|||||||||
17180|Split Rock Sandstone|37572|4|Described|p158|||See also Fig.7 and p165.||||||04-DEC-06
17180|Split Rock Sandstone|38444|6|Mentioned|p139|||||||||
17180|Split Rock Sandstone|38446|6|Mentioned|Table 23|||||||||
17180|Split Rock Sandstone|39445|5|Briefly described|Table 4|||See also p62.||||||04-DEC-06
17180|Split Rock Sandstone|39690|6|Mentioned|Table 1|||||||||
17180|Split Rock Sandstone|40856|6|Mentioned|Fig.23.6|||||||||
17180|Split Rock Sandstone|41129|6|Mentioned|Fig.8|||||||||
17180|Split Rock Sandstone|41298|6|Mentioned|Map legend|Middle Cambrian||||||||
17180|Split Rock Sandstone|44091|14|Not recorded|p16,Tb.1,p18||Middle Cambrian|||||||
17180|Split Rock Sandstone|44205|14|Not recorded|p51,155|||See also Lexicon.||||||
17180|Split Rock Sandstone|44206|14|Not recorded|p122|||Overlies Pilpah Sandstone.||||||
17180|Split Rock Sandstone|44210|2|Defined|map,p5,7,15,Tb.2||Middle Cambrian|||||||
17180|Split Rock Sandstone|44211|2|Defined|p92,101-107|||Erosional residuals in Undilla Basin partly covered by Polland Shale.||||||04-DEC-06
17180|Split Rock Sandstone|44213|14|Not recorded|Map Legend||Middle Cambrian|||||||
17180|Split Rock Sandstone|44275|14|Not recorded|Map Legend|||||||||
17180|Split Rock Sandstone|44920|14|Not recorded|Map Legend, Sheet 2||Middle Cambrian|||||||
17180|Split Rock Sandstone|44989|14|Not recorded|p.122|||Overlies Pipah Sandstone.||||||
17180|Split Rock Sandstone|45052|3|Fully described|p94|||M.Camb.||||||
17180|Split Rock Sandstone|45054|6|Mentioned|p5|||Fossil locality||||||
17180|Split Rock Sandstone|45079|5|Briefly described|p38|||Cambrian age||||||
17180|Split Rock Sandstone|45119|6|Mentioned|p3|||||||||
17180|Split Rock Sandstone|48906|14|Not recorded|Tb.1|||||||||
17180|Split Rock Sandstone|64068|5|Briefly described|p62, 64, 225|||Eastern Georgina Basin. Correlated with Arthur Creek Formation, Roaring Siltstone, Devoncourt Limestone.||||||
17180|Split Rock Sandstone|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map; p83|Middle Cambrian|Middle Cambrian|Undilla Sub-basin, Georgina Basin.||Narpa Group.||Overlies Age Creek Formation and Mail Change Limestone.|Fine-grained quartzose arenite, siltstone.|
17180|Split Rock Sandstone|69443|5|Briefly described|p28:16|Middle Cambrian|Middle Cambrian|Georgina Basin.||Narpa Group.||||12-JUL-16
17180|Split Rock Sandstone|69573|6|Mentioned|p659, 665|||Georgina Basin. Contains Drumian Stage [Cambrian] fossil sites. High energy, inner shelf setting.||||||
17180|Split Rock Sandstone|69591|5|Briefly described|p87, p90, p96-97|Cambrian|Cambrian|Undilla Sub-basin, Georgina Basin. Preserved as erosional residuals in the Undilla area. Contains trilobites.||Narpa Group.||Conformably overlies Age Creek Formation. Overlies Mail Change Limestone conformably, locally disconformably, or grades laterally into it. Is overlain unconformably by Polland Waterhole Formation.|Fine quartz sandstone with siltstone interbeds and local cross-bedding.|
17180|Split Rock Sandstone|72321|6|Mentioned|Fig 2|Drumian|Drumian|Undilla Sub-basin, Georgina Basin. Australian Stage: Undillan.||of Narpa Group.||||
17180|Split Rock Sandstone|72516|6|Mentioned|p92|Cambrian|Cambrian|Eastern Georgina Basin.||||Equivalent to the Arthur Creek Formation.||03-JUN-21
17180|Split Rock Sandstone|73418|5|Briefly described|p4 Fig.3|Miaolingian|Miaolingian|Georgina Basin, Undilla Sub-basin.||Narpa Group||Overlies Mail Change Limestone|Sandstone.|
17236|Stag Creek Volcanics|22810|5|Briefly described|Table2 P5|||Maximum thickness 1000m. Overlies Masson Formation.||||||04-DEC-06
17236|Stag Creek Volcanics|23205|6|Mentioned|p42|Paleoproterozoic|Paleoproterozoic|In the Pine Creek Inlier.||||||07-NOV-08
17236|Stag Creek Volcanics|23714|6|Mentioned|p87|||||||||
17236|Stag Creek Volcanics|24181|4|Described|p102|Paleoproterozoic|Paleoproterozoic|Tholeiitic volcanic breecias and lavas. Interfingers with Masoon Formation. Of Namoona Group. Geological Province: Pine Creek Inlier.||||||07-NOV-08
17236|Stag Creek Volcanics|29599|6|Mentioned|Fig.2|||||||||
17236|Stag Creek Volcanics|30558|6|Mentioned|Table 3|||Archaean age||||||
17236|Stag Creek Volcanics|30831|6|Mentioned|p1|||||||||
17236|Stag Creek Volcanics|32660|5|Briefly described|Table 2|||||||||
17236|Stag Creek Volcanics|32959|6|Mentioned|p1|||Re stratigraphy||||||
17236|Stag Creek Volcanics|33186|4|Described|p287|||||||||
17236|Stag Creek Volcanics|34528|6|Mentioned|p19|||Archaean||||||
17236|Stag Creek Volcanics|34834|6|Mentioned|p213|||||||||
17236|Stag Creek Volcanics|35140|6|Mentioned|Fig.2|||||||||
17236|Stag Creek Volcanics|35465|6|Mentioned|Fig.2|||Summary of positions of magnetic units in the Lower Proterozoic||||||
17236|Stag Creek Volcanics|36085|6|Mentioned|Fig.7|||||||||
17236|Stag Creek Volcanics|36473|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17236|Stag Creek Volcanics|37462|6|Mentioned|Fig.4.8|||||||||
17236|Stag Creek Volcanics|37579|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Namoona Group. Basic volcanic breccia, andesite, tough, tuffaceous shale, tuffaceous greywacke.||||||07-NOV-08
17236|Stag Creek Volcanics|38239|6|Mentioned|Fig.2|||||||||
17236|Stag Creek Volcanics|39069|5|Briefly described|Table 1|||||||||
17236|Stag Creek Volcanics|39357|4|Described|p6|||||||||
17236|Stag Creek Volcanics|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17236|Stag Creek Volcanics|40243|6|Mentioned|Fig.2|||||||||
17236|Stag Creek Volcanics|40493|5|Briefly described|Table 1|||||||||
17236|Stag Creek Volcanics|40808|5|Briefly described|Table 2|||||||||
17236|Stag Creek Volcanics|40823|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17236|Stag Creek Volcanics|40852|6|Mentioned|Fig.3.2|||||||||
17236|Stag Creek Volcanics|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17236|Stag Creek Volcanics|41125|6|Mentioned|p26|||||||||
17236|Stag Creek Volcanics|41311|4|Described|p5|||||||||
17236|Stag Creek Volcanics|41397|4|Described|p7|||||||||
17236|Stag Creek Volcanics|41407|6|Mentioned|Map legend|Proterozoic||||||||
17236|Stag Creek Volcanics|43140|5|Briefly described|p2||Paleoproterozoic|Of Namoona Group.||||||07-NOV-08
17236|Stag Creek Volcanics|43187|5|Briefly described|p2|||||||||
17236|Stag Creek Volcanics|43624|6|Mentioned|p8|||Of Namoona Group.||||||
17236|Stag Creek Volcanics|43720|6|Mentioned|Appendix,p23|||||||||
17236|Stag Creek Volcanics|43832|3|Fully described|13-14, 97||Paleoproterozoic|Part of Namoona Group. Underlain by Masson Formation.||||||07-NOV-08
17236|Stag Creek Volcanics|44399|5|Briefly described|map legend||Archean|Altered basalt and basalt-agglomerate (greenstone).||||||07-NOV-08
17236|Stag Creek Volcanics|45022|6|Mentioned|p.23.||Archean|On many pages.||||||07-NOV-08
17236|Stag Creek Volcanics|46658|6|Mentioned|p552|||||||||
17236|Stag Creek Volcanics|46678|5|Briefly described|Table 1|Archean|Archean|Altered basalt and basalt agglomerate.  Density: 3.0-3.1.||||||07-NOV-08
17236|Stag Creek Volcanics|46877|6|Mentioned|Fig.1|||||||||
17236|Stag Creek Volcanics|47049|6|Mentioned|Fig.2|||||||||
17236|Stag Creek Volcanics|48867|14|Not recorded|map||Archean|||||||07-NOV-08
17236|Stag Creek Volcanics|60680|5|Briefly described|Map legend|Orosirian|Orosirian|Of the Namoona Group.  Age: 2048Ma.  Geological Province: Pine Creek Orogen.||||||04-DEC-06
17236|Stag Creek Volcanics|62378|5|Briefly described|p16|Paleoproterozoic|Paleoproterozoic|Age: 2048 +/- 13Ma. In the Masson Formation.||||||07-NOV-08
17236|Stag Creek Volcanics|63866|4|Described|p108|Orosirian|Orosirian|Central Domain, Pine Creek Orogen. Zircons within this group have also been dated at 2048 +/- 13 Ma (Page, OZCHRON).|2021 +/- 10 Ma (Worden et al, in press)|||Overlies the Namoona Group.|Basaltic and andesitic volcanics.|
17236|Stag Creek Volcanics|64698|4|Described|lithinterp table|Orosirian|Rhyacian|Of Namoona Group. Age 2050Ma SHRIMP U/Pb. Max thick 1000m. Altered, massive, fine amygdaloidal and slightly porphyritic basalt and basaltic andesite, basaltic agglomerate, mafic volcaniclastic shale and arenite.||||||07-JAN-09
17236|Stag Creek Volcanics|64730|4|Described|p124, 125 Fig. 3, p127 Table 1, 2, p130|Paleoproterozoic|Paleoproterozoic|Age is the maximum age of extrusion. Previous studies gave ages of xenocrystic zircons ~2048 Ma.|2021 +/- 10 Ma U/Pb SHRIMP.|Top of Namoona Group.||Conformably overlies Masson Formation. Unconformably overlain by Mundogie Sandstone.|Subaqueous tholeiitic basaltic-andesitic flows, flow breccias and sediments.|02-MAY-12
17236|Stag Creek Volcanics|64956|5|Briefly described|p2 Tb. 12, p69|Paleoproterozoic|Paleoproterozoic|Conformable on Masson Fm; unconformable below Mundogie Sst. Cryst. age: 2021+/-10Ma. In Pine Creek Orogen. Sample is altered basaltic-intermediate agglom. from a seq.of interbedded subaqueous tholeiitic basaltic-andesitic flows, flow breccias+ed.rocks||||||07-FEB-11
17236|Stag Creek Volcanics|65232|5|Briefly described|p45, p5 Fig. 4, p50, App. 2|||Of Namoona Group. Overlies Masson Formation. Andesitic to basaltic tuff, flows, breccia and siltstone. Uranium mineralisation. Geol. Prov: Pine Creek Orogen.||||||09-FEB-10
17236|Stag Creek Volcanics|65339|6|Mentioned|p5 Fig.4. ||||||||Mafic volcanic rocks.|
17236|Stag Creek Volcanics|66526|5|Briefly described|p37.|Proterozoic|Proterozoic|Pine Creek Province. Includes basalts produced in the Stag Creek Event, ME 4 in the Proterozoic Mafic-Ultramafic Magmatic Event Series.|c.2015 Ma.|||||
17236|Stag Creek Volcanics|67564|3|Fully described|p8 Table 2, p9 Fig.4, pp13-14, p61.|Paleoproterozoic|Paleoproterozoic|Up to 1000 m, commonly 400 - 500 m, of submarine flows. Low-K tholeiite basaltic composition. Produces a gravity high.|2048 +/- 13 Ma (SHRIMP U-Pb).|Unit in Namoona Group.||Conformably overlies Masson Formation.|Altered, massive, fine amygdaloidal basalt and basaltic andesite; basaltic agglomerate; mafic volcaniclastic shale and arenite.|
17236|Stag Creek Volcanics|67779|5|Briefly described|p6 Fig.5, p19.|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen.|2021 +/- 10 Ma (Worden et al. 2008a).|Unit in Namoona Group.||||
17236|Stag Creek Volcanics|69383|5|Briefly described|p72|Orosirian|Orosirian|Pine Creek Orogen.|2021+/-10 Ma|||||
17236|Stag Creek Volcanics|69420|4|Described|p5:1, 4, 6, 8-10, 16, 67, 79, 94|Paleoproterozoic|Paleoproterozoic|South Alligator region, Central Domain, Pine Creek Orogen. Generally poor, discontinuous exposures. Up to 1000m thick. Rare pillow structures indicate submarine flows. Associated with the George Creek Zn-Pb prospect. SHRIMP xenocrystic zircon maximum deposition age.|<2021 +/- 10 Ma (Worden et al., 2008).|Namoona Group.||Conformably overlies Masson Formation.|Basalt, andesite, agglomerate, volcaniclastic shale and sandstone.|12-JUL-16
17236|Stag Creek Volcanics|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen. A provenance cluster is dated at 2048 +/- 13 Ma (U-Pb zircon SHRIMP).|||||Ash tuff, volcanic breccia.|
17256|Stanbroke Sandstone|37413|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
17256|Stanbroke Sandstone|37816|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17256|Stanbroke Sandstone|37862|4|Described|p583|||||||||
17256|Stanbroke Sandstone|38310|6|Mentioned|p237|||||||||
17256|Stanbroke Sandstone|38350|4|Described|p11|||||||||
17256|Stanbroke Sandstone|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
17256|Stanbroke Sandstone|39445|5|Briefly described|Table 2|||||||||
17256|Stanbroke Sandstone|40840|6|Mentioned|Map legend|||||||||
17256|Stanbroke Sandstone|42565|5|Briefly described|Table 1 P5|||||||||
17256|Stanbroke Sandstone|45161|4|Described|p26|||||||||
17256|Stanbroke Sandstone|45166|5|Briefly described|p17|||||||||
17256|Stanbroke Sandstone|46960|6|Mentioned|p216|||||||||
17256|Stanbroke Sandstone|46962|4|Described|Table 1|||See also Fig.3.||||||
17256|Stanbroke Sandstone|46996|6|Mentioned|p273|||||||||
17256|Stanbroke Sandstone|49009|2|Defined|p43|Proterozoic|Proterozoic|Previously mapped as part of the Argylla Formation (Carter and Opik 63).||||||02-APR-07
17256|Stanbroke Sandstone|49041|5|Briefly described|Table 1|||||||||
17256|Stanbroke Sandstone|50100|5|Briefly described|p13 Fig. 4, p19|Statherian|Statherian|Mainly quartzose to feldspathic sst., with local basal conglomerates containing volcanic detritus; includes some calcareous and dolomitic beds; extensively recrystallised.  Overlies Magna Lynn Metabasalt and Argylla Fm.  Geol.Prov: Kalkadoon-Ewen Prov.||||||04-DEC-06
17256|Stanbroke Sandstone|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Arenite, dolomite, limestone, siltstone, basal conglomerate.||||||
17256|Stanbroke Sandstone|64250|6|Mentioned|p8|||Omitted from stratigraphic chart because of limited exposure.||||||
17256|Stanbroke Sandstone|65396|6|Mentioned|p174|||Southern Kalkadoon-Leichhardt Belt. Small unit with limited exposure.||||(Possibly) Correlated with Ballara Quartzite.||
17256|Stanbroke Sandstone|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map, p107|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot. Kalkadoon-Leichhardt Domain, Mount Isa Inlier. Calvert Superbasin.|||||Quartz arenite, feldspathic arenite, calcareous arenite, limestone, greywacke, siltstone, local basal conglomerate.|
17256|Stanbroke Sandstone|69591|5|Briefly described|p38 Fig.2.22, p39-40, p55|||Kalkadoon-Leichhardt Domain, Calvert Superbasin. Age uncertain; considered part of the Prize and Gun Supersequences.|||||Quartz arenite, feldspathic arenite, calcareous arenite, limestone, greywacke, siltstone, local basal conglomerate.|
17256|Stanbroke Sandstone|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Kalkadoon-Leichhardt Domain. Broad age range. Shown as older than the the Wonga-Burstall Event (c. 1740 Ma). Shown as younger than the Argylla Formation.||||Shown as laterally equivalent to Mary Kathleen Group, Quilalar Formation.|Quartzose to feldspathic sandstone, calcareous sandstone, limestone, lithic sandstoneand siltstone, local basal conglomerate.|
17256|Stanbroke Sandstone|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Kalkadoon-Leichhardt Domain. Broad age range. Shown as older than the the Wonga-Burstall Event (c. 1740 Ma). Shown as younger than the Argylla Formation.||||Shown as laterally equivalent to the Mary Kathleen Group, Quilalar Formation.|Quartzose to feldspathic sandstone, calcareous sandstone, limestone, lithic sandstoneand siltstone, local basal conglomerate.|
17256|Stanbroke Sandstone|73525|6|Mentioned|p4-5 Fig.2|||Kalkadoon-Leichhardt Domain.|||||Clastics.|
17310|Steamboat Sandstone|12951|5|Briefly described|p143 fig 4, 148|Middle Cambrian|Middle Cambrian|Georgina Basin. Overlying Arthur Creek Formation or Member at top?||?of Arthur Creek Formation.|||Quartzitic dolostone and dolomitic sandstone.|
17310|Steamboat Sandstone|24419|5|Briefly described|p18, p19|Late Cambrian|Middle Cambrian|Cross-stratified, ripple marked sandstone with interbedded silty sandstone and siltstone and basal units of sandy limestone and limestone. Erosional contact with underlying Quita Formation. Geological Province: Georgina Basin.||||||
17310|Steamboat Sandstone|24442|5|Briefly described|p45, p49|Middle Cambrian|Middle Cambrian|Quartzic dolostone and quartz sandstone.  Overlies the Arthur Creek Formation.  On SANDOVER RIVER sheet.||||||
17310|Steamboat Sandstone|30242|6|Mentioned|Fig.2|||||||||
17310|Steamboat Sandstone|30479|6|Mentioned|Fig.6|||Stratigraphic relationships||||||
17310|Steamboat Sandstone|30914|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
17310|Steamboat Sandstone|31287|6|Mentioned|p430|||Refers Opik (1956)||||||
17310|Steamboat Sandstone|33111|6|Mentioned|Fig.15|||||||||
17310|Steamboat Sandstone|34287|6|Mentioned|Fig.3|||||||||
17310|Steamboat Sandstone|34847|6|Mentioned|p40|||Also Table 1, stratigraphy & hydrocarbon prospects.||||||
17310|Steamboat Sandstone|35054|6|Mentioned|Table 23|||||||||
17310|Steamboat Sandstone|35121|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
17310|Steamboat Sandstone|35139|4|Described|Table.2|||||||||
17310|Steamboat Sandstone|35553|6|Mentioned|p8|||See also Appendix 2, description of Agnostid localities.||||||
17310|Steamboat Sandstone|36234|6|Mentioned|p175|||||||||
17310|Steamboat Sandstone|37572|4|Described|p158|||See also Fig.8||||||
17310|Steamboat Sandstone|38442|5|Briefly described|Map legend|Late Cambrian|Middle Cambrian|Middle to Late? Cambrian||||||25-AUG-04
17310|Steamboat Sandstone|38446|6|Mentioned|Table 23|||||||||
17310|Steamboat Sandstone|38608|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
17310|Steamboat Sandstone|39445|5|Briefly described|Table 4|||See also P62||||||
17310|Steamboat Sandstone|44205|4|Described|p46,47|||=age of Roaring Siltstone and Devoncourt Limestone.||||||
17310|Steamboat Sandstone|44211|14|Not recorded|p93,95-97,101-107|||Rests with breakd on Quita Formation.||||||
17310|Steamboat Sandstone|44273|14|Not recorded|Map Legend||Middle Cambrian|||||||
17310|Steamboat Sandstone|44275|14|Not recorded|Map Legend|||||||||
17310|Steamboat Sandstone|44309|2|Defined|Tb.1,p7,8-10,17||Middle Cambrian|Interfingers with Mungerebar Limestone above.||||||
17310|Steamboat Sandstone|44326|14|Not recorded|Map Legend||Middle Cambrian|||||||
17310|Steamboat Sandstone|44920|14|Not recorded|Map Legend, Sheet 4||Middle Cambrian|||||||
17310|Steamboat Sandstone|45002|14|Not recorded|p24|||early Late Cambrian fossils deposited in agitated shallow water, food abundant. See also Lexicon.||||||
17310|Steamboat Sandstone|45012|14|Not recorded|p1-9,16,19,26,28,91,||Middle Cambrian|p133-35,173-77,300-304,332-366||||||
17310|Steamboat Sandstone|45052|3|Fully described|p101|||M.Camb.||||||
17310|Steamboat Sandstone|45054|6|Mentioned|p5|||Fossil locality||||||
17310|Steamboat Sandstone|45079|4|Described|p38|||Cambrian age||||||
17310|Steamboat Sandstone|45119|6|Mentioned|p4|||||||||
17310|Steamboat Sandstone|45166|5|Briefly described|Table 15|||||||||
17310|Steamboat Sandstone|45168|6|Mentioned|p6|||||||||
17310|Steamboat Sandstone|46959|6|Mentioned|Table 1|||||||||
17310|Steamboat Sandstone|47024|6|Mentioned|Table 1|||||||||
17310|Steamboat Sandstone|47058|6|Mentioned|p136|||||||||
17310|Steamboat Sandstone|48633|14|Not recorded|p96|||Ref. to Opik 1961.||||||
17310|Steamboat Sandstone|60122|4|Described|p18|Middle Cambrian|Middle Cambrian|Conformably on Arthur Creek Formation; conformable beneath Arrintrhunga Formation and Mungerebar Limestone. Possible disconformable on Quita Fm. in URANDANGI-GLENORMISTON. Max. thick: 80m. Geol.Prov: Georgina Basin. See also p405, p11 Tb. 1.||||||
17310|Steamboat Sandstone|60123|4|Described|p5|Cambrian|Cambrian|Thickness: 80m. Conformably underlies: Arrinthrunga Formation. Conformably overlies: Arthur Creek Formation. Possibly disconformably overlying Quita Formation.||||||08-MAR-23
17310|Steamboat Sandstone|60359|5|Briefly described|Map Legend|Cambrian|Cambrian|Sandstone, siltstone.||||||
17310|Steamboat Sandstone|60590|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Quartzose and calcareous/dolomitic quartz sandstone, quartzose dolostone.  Conformably overlies the Arthur Creek Formation; conformably overlain by Arrinthrunga Formation.||||||26-NOV-04
17310|Steamboat Sandstone|60675|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Quartzose and calcareous/dolomitic quartz sandstone, quartzic dolostone.||||||
17310|Steamboat Sandstone|61022|5|Briefly described|p14, p15||Cambrian|Near-shoreline (tidal channel and deltaic clastics) oolitic carbonate and quartz-rich sandstone. Potential to trap oil in sediments below. Geological Province: Georgina Basin.||||||20-APR-05
17310|Steamboat Sandstone|61250|5|Briefly described|p43|Middle Cambrian|Middle Cambrian|Contains petroleum systems - potential reservoirs up to 150m thick.  Geological Province: Georgina Basin.||||||18-AUG-05
17310|Steamboat Sandstone|61404|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Of the Narpa Group. Quartzose and calcareous/dolomitic quartz sandstone, quartzose dolostone. Geological Province: southern Georgina Basin.||||||11-OCT-05
17310|Steamboat Sandstone|62759|5|Briefly described|p1|||Overlies Arthur Creek Formation. Geological Province: Georgina Basin.||||||05-FEB-08
17310|Steamboat Sandstone|64068|4|Described|p64-65, p62, 63, 67, 69, p88-89, p ix|Middle Cambrian|Middle Cambrian|Diverse trilobite fauna. Correlated with Devoncourt Limestone, lower Georgina Limestone, Cleland Sandstone in part, Illara Sandstone, Hugh River Shale in part, Shannon Formation in part, Petermann Sandstone.||Of Narpa Group.||Overlies Quita and Arthur Creek Formations. Laterally interdigitates with and conformably overlain by Mungerebar Limestone, Arrinthrunga Formation.|Quartz and calcareous sandstones with interbeds of quartzic grainstone and quartz dolostone; minor siltstone.|05-APR-12
17310|Steamboat Sandstone|64443|6|Mentioned|p9, p17, p18|Late Cambrian||An uppermost portion of the Arthur Creek Formation may alternatively represent this unit; a probable correlative of the quartz sandstone Cmdz unit (uppermost Camooweal Dolostone).||||. Conformably underlies Arrinthrunga Formation.||14-MAY-14
17310|Steamboat Sandstone|64812|4|Described|p236, p241-2 Fig. 8, 9, p243, p247|Late Cambrian|Late Cambrian|The inner ramp facies caps/interfingers with upper Arthur Creek Fm middle ramp facies; may be unconformable with overlying Chabalow/Arerinthrunga Fms. Near-shoreline oolitic carbonate + quartz-rich sandstone - more lith.details. Geol.Prov:Georgina Basin.||||||07-FEB-11
17310|Steamboat Sandstone|64813|5|Briefly described|p254, p255, p256 Fig. 2|Middle Cambrian|Middle Cambrian|Overlies/interfingers with Arthur Creek Formation. Geological province: Georgina Basin. Near-shore quartz clastic rocks.||||||11-FEB-09
17310|Steamboat Sandstone|65237|4|Described|p3 Fig. 4, p8|Middle Cambrian|Middle Cambrian|Overlies Chabalowe and Arrinthrunga Formations, usually conformably. Max. thickness: 250m. Geol.prov: southern Georgina Basin.Near-shoreline calcareous/siliciclastic sandstone, interbedded with oolitic rocks which interfinger with upper Arthur Creek Fm.||||||07-FEB-11
17310|Steamboat Sandstone|65345|5|Briefly described|p6 Fig.5. |Middle Cambrian|Middle Cambrian|Southern Georgina Basin.||||Overlies Arthur Creek Formation.||
17310|Steamboat Sandstone|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Middle Cambrian|Middle Cambrian|Georgina Basin||Narpa Group|||Calcarenite, calcareous and quartzose arenite, calcilutite|
17310|Steamboat Sandstone|69437|5|Briefly described|p22:10|Series 3|Series 3|Southern Georgina Basin. Potential petroleum reservoir.||||Overlies Arthur Creek Formation. Is overlain by Arrinthrunga Formation.||12-JUL-16
17310|Steamboat Sandstone|69443|4|Described|p28:16-19, 31|Middle Cambrian|Middle Cambrian|Noakes et al. (1959). Southern Georgina Basin. Forms mesa caps and plains. 17-221m thick. Diverse trilobite fauna: Boomerangian age. Nearshore sand to shallow-marine platform-edge deposits.||Narpa Group.||Conformably overlies Arthur Creek and Quita Formations. Is overlain conformably by Arrinthrunga Formation and Mungerebar Limestone (with which it interdigitates).|Quartz sandstone and calcareous sandstone, with interbeds of quartzose grainstone and quartzose dolostone; minor siltstone.|12-JUL-16
17310|Steamboat Sandstone|69561|6|Mentioned|p33 fig 2|Boomerangian|Boomerangian|||||Overlain by Arrinthrunga Formation, overlies Arthur Creek Formation||
17310|Steamboat Sandstone|69573|6|Mentioned|p659, 661, 666|||Georgina Basin. Intertidal to subtidal environment.||||||
17310|Steamboat Sandstone|69591|5|Briefly described|p87, p91, p96|Cambrian|Cambrian|Oban Sub-basin, Georgina Basin. Up to 80m thick. Trilobite fauna indicates late middle Cambrian (Lejopyge laevigata Zone).||||Overlies Quita Formation transitionally. Is overlain by and interfingers with Mungerebar Limestone.|Calcareous and quartz sandstones with interbeds of sandy limestone and dolomite; locally, the upper 25m has leached sandstone and minor siltstone.|
17310|Steamboat Sandstone|69673|5|Briefly described|p116, p117, p127, p129, p133, p138|||Up to 221m thick. Trilobite fossils present. Potential as a reservoir rock.||Narpa Group||Conformably overlies Arthur Creek Formation, conformably overlain by Arrinthrunga Formation|Quartz sandstone and calcareous sandstone with interbeds of grainstone and quartzic dolostone with minor siltstone.|
17310|Steamboat Sandstone|70380|6|Mentioned|p745|Series 3|Series 3|Southern Georgina Basin.||||||
17310|Steamboat Sandstone|70723|5|Briefly described|p24 Fig. 2|Cambrian|Cambrian|Georgina Basin.||Narpa Group||Overlies Quita Formation and Arthur Creek Formation. Is overlain by Mungerebar Limestone, Arrinthrunga Formation.|Sandstone.|
17310|Steamboat Sandstone|70951|5|Briefly described|p1083|||Geological province: Georgina Basin.||||Underlain by Arthur Creek Formation. Overlain by Hagen Member.||
17310|Steamboat Sandstone|72321|5|Briefly described|Fig 2, p4, p6|Guzhangian|Guzhangian|Toko Syncline, Georgina Basin. New, younger age based on Boomerangian agnostid trilobites in underlying Arthur Creek Foramtion. Australian Stage: upper Boomerangian.||of Narpa Group.||Overlies Arthur Creek Formation in Toko Syncline. May correlate with Chabalowe Formation, Dulcie Syncline.||
17310|Steamboat Sandstone|72515|5|Briefly described|Map Legend|Cambrian|Cambrian|Jervois Range Special Map Sheet. Georgina Basin. Contains fossil trilobites.||Narpa Group||Overlain by the Arrinthrunga Formation including the Eurowie Sandstone Member. Overlies the Arthur Creek Formation.|Quartz sandstone, calcareous sandstone, interbeds of quartzitic grainstone, quartzitic dolostone and minor siltstone.|05-JUL-22
17310|Steamboat Sandstone|72516|3|Fully described|p11-12, p92-93|Cambrian Series 3|Cambrian Series 3|Georgina Basin. Previously included in the Arthur Creek Formation before being separated by Dunster et al (2007). Occurs on GLENORMISTON, URANDANGI, SANDOVER RIVER, TOBERMORY and HUCKITTA map sheets; subsurface occurences are known in MOUNT WHELAN. Outcrops on the Jervois Range Special occur north of the Johannsen Range and west of the Jervois Range where it forms mesa caps and plains. Contains fossil trilobites which indiacte an upper Series 3 Cambrian age. Deposited in a near-shore, shallow marine; possibly barrier bar system. 40m thick in the mapped area, 17-221m elsewhere. Part equivalent of the Cleland Sandstone, Illara Sandstone, Hugh River Shale, Shannon Formation and the Petermann Sandstone.||Narpa Group||Conformably and gradationally overlain by the Arrinthrunga Formation. Conformably overlies the Arthur Creek Formation. Equivalent to the Devoncourt Limestone and the Georgina Limestone.|Quartz sandstone, calcareous sandstone; interbeds of quartzitic grainstone, quartzitic dolostone, minor siltstone.|03-JUN-21
17310|Steamboat Sandstone|73083|6|Mentioned|p75|Late Cambrian|Middle Cambrian|||||||
17310|Steamboat Sandstone|73288|5|Briefly described|p702|||Southern Georgina Basin. Downhole (Hylogger) logs.||||Overlies Arthur Creek Formation. Is overlain by Hagen Member.||
17338|Stirling Sandstone|14019|3|Fully described|p6|||Of the Limbunya Group. Quartzarenite, sandstone, conglomerate. Unconformably overlies Inverway Metamorphics; disconformably overlain by Margery Formation. Type section 120m thick. Geological Province: Birrindudu Basin. Correlated with Masterton Sandstone.||||||
17338|Stirling Sandstone|24122|5|Briefly described|p4 Fig.3|||Of Limbunya Group.  Geological Province: Birrindudu Basin.||||||
17338|Stirling Sandstone|24297|5|Briefly described|p4 Fig.3|Proterozoic|Proterozoic|Of Limbunya Group.  Geological Province: Birrindudu Basin.||||||
17338|Stirling Sandstone|24441|5|Briefly described|p1 Fig. 1|||Of the Limbunya Group. Unconformably overlies Coomarie Sandstone and Hinde Dolostone; overlain by Margery Formation. Geological Province: Birrindudu Basin.||||||08-AUG-05
17338|Stirling Sandstone|24442|5|Briefly described|p50 Fig. 1|||Of the Limbunya Group.  Geological Province: Birrindudu Basin.||||||
17338|Stirling Sandstone|28255|6|Mentioned|p13, Tb. 11 (opp. p8)|||Of the Limbunya Group. Composed entirely of sandstone. Unconformable on Inverway Metamorphics and probably Bunda Grit also. Age is Adealidean or Carpentarian. Max. thickness: 120m.||||||
17338|Stirling Sandstone|32172|4|Described|Table 1|||Carpentarian or Adelaidean||||||
17338|Stirling Sandstone|32173|5|Briefly described|Map legend|Adelaidean|Carpentarian|Of the Limbunya Group.  White and brown quartz sandstone, basal grit and minor conglomerate.  Overlies the Inverway Metamorphics unconformably; conformably underlies the Margery Formation.  Carpentarian or Adelaidean (per legend).||||||17-NOV-04
17338|Stirling Sandstone|32660|5|Briefly described|Table 6|||||||||
17338|Stirling Sandstone|33375|6|Mentioned|p9 Tb. 1|||Of the Limbunya Group. Age is Carpentarian or Adelaidean.||||||26-APR-05
17338|Stirling Sandstone|33376|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17338|Stirling Sandstone|33378|5|Briefly described|Map legend|||Of the Limbunya Group. Age is Carpentarian or Adelaidean.||||||27-APR-05
17338|Stirling Sandstone|45112|6|Mentioned|p15|||||||||
17338|Stirling Sandstone|48943|2|Defined|p15|Proterozoic|Proterozoic|||||||
17338|Stirling Sandstone|60589|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Limbunya Group.  Quartz arenite, dolomitic sandstone, conglomerate.  Unconformably overlies the Inverway Metamorphics.  Geological Province: Birrindudu Basin.||||||07-NOV-08
17338|Stirling Sandstone|60685|5|Briefly described|p4 Fig. 3|||Of the Limbunya Group. Geological Province: Birrindudu Basin.||||||
17338|Stirling Sandstone|65342|6|Mentioned|p11 Fig.13. |||Birrindudu Basin.||Unit in Limbunya Group.||Unconformably overlies Coomarie Sandstone and Hinde Dolostone. Is overlain by Margery Formation.||
17338|Stirling Sandstone|67151|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Birindudu Basin.||Unit in Limbunya Group.||Is overlain by Margery Formation.|Quartz arenite, dolomitic sandstone, conglomerate (section only).|
17338|Stirling Sandstone|67479|5|Briefly described|p58|Orosirian|Orosirian|Maximum depositional age (LIMBUNYA; Carson, unpublished data) is similar to that of the Depot Creek Sandstone; implications mentioned.|c. 1830 Ma|||||24-JAN-17
17338|Stirling Sandstone|68733|5|Briefly described|p177-187, p193||Orosirian|Sweet et al. (1974). Birrindudu Basin. Sm-Nd isotope data tabulated.|Maximum depositional age of ca. 1830 +/- 13 Ma|Basal unit of the Limbunya Group.||Unconformably overlies Inverway Metamorphics. Correlated with Mount Charles Formation.|Comprises predominantly coarse- to medium-grained well-rounded silicified quartz sandstone.|06-DEC-17
17338|Stirling Sandstone|69429|6|Mentioned|p14:2|||||Basal Limbunya Group.||Unconformably overlies Inverway Metamorphics.||12-JUL-16
17338|Stirling Sandstone|69432|4|Described|p17:2, 5-6, 13|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin. 120m thick. Includes the former unit, the Bunda Grit, which was recognised as a facies variant of this unit; the name has been abandoned. Contains a synsedimentary fault-scarp conglomerate near its type section; activity on the Negri Fault was contemporaneous with deposition of the Sandstone. Detrital zircon maximum depositional age.|<1830 +/- 13 Ma (Carson, 2010).|Limbunya Group.||Unconformably overlies Inverway Metamorphics and Birrindudu Group.|Massive, thickly bedded, coarse quartz sandstone followed up-section by thinly to medium bedded, moderately sorted, medium to coarse quartz sandstone and minor thin conglomerate interbeds.|12-JUL-16
17338|Stirling Sandstone|69448|6|Mentioned|p33:8|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin. Contains evidence of a growth fault during deposition (the Negri Fault) which turned out to be long-lived, affecting Cambrian rocks in the overlying Ord Basin.||Limbunya Group.||||12-JUL-16
17338|Stirling Sandstone|69673|6|Mentioned|p48 fig 35|||||Limbunya Group||Unconformably overlies Coomarie Sandstone, Hinde Dolostone, overlain by Margery Formation||
17338|Stirling Sandstone|70655|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Birindudu Basin. Section only.||Shown as base of Limbunya Group.|||Quartz arenite, dolomitic sandstone, conglomerate.|
17338|Stirling Sandstone|70848|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin.||Limbunya Group.|||Conglomerate: medium-thick bedded, cobble-pebbly, polymictic, cross-stratified; quartz sandstone: ripple marked, chert nodules; minor thin siltstone, mudstone.|
17338|Stirling Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
17338|Stirling Sandstone|71302|5|Briefly described|p6,72-74|Paleoproterozoic|Paleoproterozoic|Of Birindudu Basin. Reported maximum depositional age: 1830+\-13 Ma (Carson, 2013; Munson, 2016 and Munson, in prep). Almost entirely composed of zircon >1800 Ma in age, with significant populations of Neoarchean detritus at c. 2520 Ma, and contain small c > 1560-1640 Ma age populations. Carson (2013) suggested restricted provenance fromm the eastern zone of Halls Creek Orogen (c. 1910-1900 Ma mafic and felsic magmatism; see Blake et al., 2000). Tentatively correlated to Mount Charles Formation (of Cross and Crispe, 2007; see Carson 2013).||Unit of Limbunya Group.||Overlain by Margery Formation. Underlain by Coomarie Sandstone or Hinde Dolostone.||
17338|Stirling Sandstone|71592|5|Briefly described|Appendix A.|||Victoria River Region.|1830+/-13 Ma (MDA: Pb/Pb zircon).||||Sandstone.|
17338|Stirling Sandstone|72718|6|Mentioned|p7|Statherian|Orosirian|Birrindudu Basin.|younger than 1830 +/- 13 Ma|Limbunyah Group||Overlain by Margery Formation.||
17338|Stirling Sandstone|73083|6|Mentioned|p31-32|||Birrindudu Basin, lowest unit.|||||Clean quartz sandstone.|
17363|Stokes Siltstone|9814|5|Briefly described|Map Legend|Ordovician|Ordovician|Of the Larapinta Group. Siltstone, shale, fossiliferous limestone.||||||
17363|Stokes Siltstone|12891|5|Briefly described|p733 Fig. 2|Late Ordovician|Middle Ordovocian|Geological province: Amadeus Basin.||||||07-FEB-11
17363|Stokes Siltstone|13995|5|Briefly described|p73, p75, p77, p89, p101, p103|Ordovician|Ordovician|Amadeus Basin. Contains Darriwilian bryozoans (the first in Australian successions), the brachiopod Dinorthis leviensis, and a rostroconch species. Contains Middle Ordovician pelecypods. Gastropod species, first decribed in the 1890s, are listed, but need reassessment. Contains the conodont Plectodina onychodenta, which has links to N China. Contains microvertebrate remains. May hold the oldest jawed vertebrate in the fossil record.||||Conformably overlies Stairway Sandstone. Is overlain conformably by Carmichael Sandstone.|Conglomerate, iron-rich dolomitised limestone, shallow subtidal mudstone.|
17363|Stokes Siltstone|22560|5|Briefly described|p5|Late Ordovician|Ordovician|||||||
17363|Stokes Siltstone|22561|5|Briefly described|p9|Neoproterozoic|Neoproterozoic|also see Stokes Formation p25||||||
17363|Stokes Siltstone|22565|5|Briefly described|p71 & Table 1||Ordovician|Thickness at Areyonga Creek measured from surface expression - 450m thick.  Approx. thickness measured from seismic data - 300m.||||||
17363|Stokes Siltstone|22566|5|Briefly described|p85|Ordovician|Ordovician|Of the Larapinta Group.||||||04-DEC-06
17363|Stokes Siltstone|22646|5|Briefly described|p105|Ordovician|Ordovician|also see Stokes Formation p107||||||
17363|Stokes Siltstone|22650|4|Described|p 160|Ordovician|Ordovician|Of the Larapinta Group.||||||04-DEC-06
17363|Stokes Siltstone|22651|6|Mentioned|Fig 10 btw p182-183|Ordovician|Ordovician|||||||
17363|Stokes Siltstone|22656|4|Described|p 279|Late Ordovician|Early Ordovician|||||||
17363|Stokes Siltstone|22761|6|Mentioned|Fig 2 on p351|Ordovician||Of the Larapinta Group.||||||04-DEC-06
17363|Stokes Siltstone|22763|6|Mentioned|Table 1 on p386||Late Ordovician|Of the Larapinta Group..||||||04-DEC-06
17363|Stokes Siltstone|22804|6|Mentioned|Fig 2 on p432|Late Ordovician|Early Ordovician|Of the Larapinta Group.||||||04-DEC-06
17363|Stokes Siltstone|22806|6|Mentioned|p486|Ordovician|Ordovician|||||||
17363|Stokes Siltstone|22825|6|Mentioned|p553|||||||||
17363|Stokes Siltstone|22826|6|Mentioned|p574|Ordovician|Ordovician|Of the Larapinta Group.||||||04-DEC-06
17363|Stokes Siltstone|23361|5|Briefly described|16 Fig.4|Ordovician|Ordovician|||||||
17363|Stokes Siltstone|23858|6|Mentioned|p914|||Overlain by Carmichael Sandstone. Geological Province: Amadeus Basin.||||||04-DEC-06
17363|Stokes Siltstone|24063|6|Mentioned|p222|||Geological Province: Amadeus Basin.||||||
17363|Stokes Siltstone|24064|5|Briefly described|p229 Fig.7|Ordovician|Ordovician|Of Larapinta Group. Geological Province: Amadeus Basin.||||||
17363|Stokes Siltstone|24301|4|Described|p21, p7 Tb. 2|Ordovician|Ordovician|Of Larapinta Group. Previously combined with Carmichael Sandstone as "Stokes Formation" (Prichard and Quinlan, 1962). Overlies Stairway Sandstone, underlies Carmichael Sandstone. Max. thickness: 650m. Geological Province: Amadeus Basin.||||||
17363|Stokes Siltstone|29972|6|Mentioned|Table 1|||Upper Ordovician||||||
17363|Stokes Siltstone|30238|4|Described|p68|||Cambrian - Ordovician age||||||
17363|Stokes Siltstone|30258|6|Mentioned|Fig.2|||Ordovician age. Part of Larapinta Group.||||||
17363|Stokes Siltstone|30544|6|Mentioned|p49|||||||||
17363|Stokes Siltstone|30615|6|Mentioned|p177|||Stratigraphic table - Palm Valley -2||||||
17363|Stokes Siltstone|31566|6|Mentioned|p231|||See also Fig. 2||||||
17363|Stokes Siltstone|31707|4|Described|p53|||Lithology||||||
17363|Stokes Siltstone|32208|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
17363|Stokes Siltstone|32209|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
17363|Stokes Siltstone|32648|6|Mentioned|p32|||U.Ord.||||||
17363|Stokes Siltstone|32854|6|Mentioned|p352|||||||||
17363|Stokes Siltstone|33307|6|Mentioned|Fig.6|||||||||
17363|Stokes Siltstone|33738|6|Mentioned|Fig.5|||||||||
17363|Stokes Siltstone|33761|6|Mentioned|p146|||Ordovician. Larapinta Group||||||
17363|Stokes Siltstone|34111|5|Briefly described|Table 2|||Cambrian - Ordovician. See p15.||||||04-DEC-06
17363|Stokes Siltstone|34442|5|Briefly described|Table 1|||Cambrian - Ordovician||||||
17363|Stokes Siltstone|35102|6|Mentioned|Fig.2|||||||||
17363|Stokes Siltstone|36821|6|Mentioned|p398|||||||||
17363|Stokes Siltstone|36890|4|Described|p400|||Formerly Stokes Formation.||||||04-DEC-06
17363|Stokes Siltstone|39213|6|Mentioned|Fig.6|||Amadeus Basin Succession||||||
17363|Stokes Siltstone|40128|6|Mentioned|p1|||||||||
17363|Stokes Siltstone|40136|5|Briefly described|p40|||||||||
17363|Stokes Siltstone|40740|3|Fully described|p55|||Mention p6.||||||04-DEC-06
17363|Stokes Siltstone|40810|4|Described|p11|||||||||
17363|Stokes Siltstone|41039|4|Described|p6|||||||||
17363|Stokes Siltstone|41224|6|Mentioned|p430|||Mention Fig.2||||||
17363|Stokes Siltstone|41621|5|Briefly described|Map legend|Late Ordovician||||||||
17363|Stokes Siltstone|41708|6|Mentioned|p206|||||||||
17363|Stokes Siltstone|41723|6|Mentioned|Map legend|Ordovician||||||||
17363|Stokes Siltstone|41819|6|Mentioned|Map legend|Late Ordovician||||||||
17363|Stokes Siltstone|41820|4|Described|p12|||||||||
17363|Stokes Siltstone|42037|5|Briefly described|Table 3 P79|||||||||
17363|Stokes Siltstone|42049|6|Mentioned|p220|||||||||
17363|Stokes Siltstone|42059|6|Mentioned|Fig.2 P131|||||||||
17363|Stokes Siltstone|42060|6|Mentioned|Fig.5 P140|||||||||
17363|Stokes Siltstone|42082|6|Mentioned|Fig.3 P323|||||||||
17363|Stokes Siltstone|42141|6|Mentioned|Fig.3 P570|||||||||
17363|Stokes Siltstone|42354|6|Mentioned|p6|||||||||
17363|Stokes Siltstone|42504|5|Briefly described|p77|||||||||
17363|Stokes Siltstone|42699|5|Briefly described|map legend|Ordovician||||||||
17363|Stokes Siltstone|42940|5|Briefly described|Plate 8|||||||||
17363|Stokes Siltstone|43035|5|Briefly described|p22|||Of Larapinta Group.||||||04-DEC-06
17363|Stokes Siltstone|43225|5|Briefly described|Map Legend||Ordovician|Of the Larapinta Group.||||||04-DEC-06
17363|Stokes Siltstone|43503|6|Mentioned|11-50|Eastonian|Darriwilian|||||||
17363|Stokes Siltstone|43646|6|Mentioned|p553||Early Ordovician|||||||
17363|Stokes Siltstone|43647|6|Mentioned|p531|||||||||
17363|Stokes Siltstone|43649|5|Briefly described|Fig.1,p454-55,458|||Maybe misspelling of Stokes Formation||||||
17363|Stokes Siltstone|43803|6|Mentioned|Fig.5,p71|||||||||
17363|Stokes Siltstone|44342|4|Described|p.6, Table 2||Ordovician|SG/53-5. U-M Ordovician.||||||
17363|Stokes Siltstone|44343|14|Not recorded|map legend||Late Ordovician|U.Ordovician.||||||
17363|Stokes Siltstone|44395|14|Not recorded|p.9,12, Tb.2|||Upper Ordovician?||||||
17363|Stokes Siltstone|44402|5|Briefly described|map legend|Ordovician|Cambrian|Part of Larapinta Group. Camb-Ord.||||||02-DEC-04
17363|Stokes Siltstone|44433|14|Not recorded|map legend|||Cambrian to Ordovician.||||||
17363|Stokes Siltstone|44484|14|Not recorded|p.11,12, Tb.1|Ordovician|Cambrian|Camb-Ord.||||||
17363|Stokes Siltstone|44485|14|Not recorded|map legend|Ordovician|Cambrian|Part of Larapinta Group. Camb-Ord.||||||
17363|Stokes Siltstone|44495|14|Not recorded|p.6, map||Ordovician|Ayers Rock sheet (G52-8).||||||
17363|Stokes Siltstone|44496|5|Briefly described|map legend||Ordovician|Shale and siltstone, some fossiliferous dolomite at base.||||||02-DEC-04
17363|Stokes Siltstone|44497|4|Described|p.11, Table 2|Ordovician|Cambrian|SF/53-13. Camb-Ord.||||||
17363|Stokes Siltstone|44498|14|Not recorded|map legend|Ordovician|Cambrian|Part of Larapinta Group. Camb-Ord.||||||
17363|Stokes Siltstone|44499|14|Not recorded|opp.p.6, Tb.1||Ordovician|||||||
17363|Stokes Siltstone|44505|14|Not recorded|p.8,11, Table 1|Ordovician|Cambrian|Of Larapinta Group. Camb-Ord.||||||
17363|Stokes Siltstone|44506|14|Not recorded|map legend|Ordovician|Cambrian|Cambrian to Ordovician.||||||
17363|Stokes Siltstone|45041|2|Defined|p78|Middle Ordovician|Middle Ordovician|See also pp79-80. Of the Larapinta Group.||||||04-DEC-06
17363|Stokes Siltstone|45118|6|Mentioned|p1,3|||||||||
17363|Stokes Siltstone|45148|6|Mentioned|Fig.4|||Geol. prov: Amadeus Basin.||||||04-DEC-06
17363|Stokes Siltstone|45155|6|Mentioned|Fig.8|||||||||
17363|Stokes Siltstone|45170|6|Mentioned|Table 3|||||||||
17363|Stokes Siltstone|46928|6|Mentioned|Table 1|||||||||
17363|Stokes Siltstone|47052|6|Mentioned|p261|||||||||
17363|Stokes Siltstone|48963|6|Mentioned|Fig.3|||||||||
17363|Stokes Siltstone|50089|5|Briefly described|p430 Fig. 5|Ordovician|Ordovician|Geological Province: Amadeus Basin.||||||
17363|Stokes Siltstone|50098|5|Briefly described|p1, p3 Fig. 2|Late Ordovician|Middle Ordovician|Of the Larapinta Group. Interbedded reddish and greenish shale and siltstone with thin beds of limestone. Max. thickness 650m. Geological Province: Amadeus Basin.||||||04-MAY-05
17363|Stokes Siltstone|60674|5|Briefly described|Map legend|Ordovician|Ordovician|Of the Larapinta Group.  Variegated siltstone; minor fine-grained silty sandstone and calc-arenite.  Geological Province: Amadeus Basin.||||||12-JAN-05
17363|Stokes Siltstone|61309|5|Briefly described|p16 Fig. 4|||Geological Province: Amadeus Basin.||||||06-FEB-08
17363|Stokes Siltstone|61385|5|Briefly described|Map legend|Ordovician|Ordovician|Siltstone, shale, limestone; fossiliferous. Geological Province: Amadeus Basin.||||||
17363|Stokes Siltstone|61518|5|Briefly described|Map Legend|Ordovician|Ordovician|Of the Larapinta Group. Geological Province: Amadeus Basin.||||||
17363|Stokes Siltstone|62376|5|Briefly described|p18|Late Ordovician|Early Ordovician|Of the Larapinta Group. Geological Province: Amadeus Basin.||||||09-FEB-10
17363|Stokes Siltstone|62379|5|Briefly described|p7 Fig. 2|Ordovician|Ordovician|Of the Larapinta Group. Geological Province: Amadeus Basin.||||||
17363|Stokes Siltstone|62794|5|Briefly described|p288, p289 Fig.2.|Ordovician|Ordovician|Unit of Larapinta Group, overlying Stairway Sandstone and underlying Carmichael Sandstone.||||||
17363|Stokes Siltstone|62982|5|Briefly described|p7|Ordovician|Ordovician|Of the Larapinta Group. Overlies Stairway Sandstone; overlain by Carmichael Sandstone. Geological Province: Amadeus Basin.||||||16-JAN-07
17363|Stokes Siltstone|63562|6|Mentioned|p338 fig 3, p348, p352 fig 10|Late Ordovician|Early Ordovician|Of Amadeus Basin.||Larapinta Group.||Overlies Stairway Sandstone. Is overlain by Carmichael Sandstone.||
17363|Stokes Siltstone|64068|6|Mentioned|p77, 78, 226|||Of Amadeus Basin. Correlated with Carlo Sandstone, Mithaka Formation, Georgina Basin.||||||
17363|Stokes Siltstone|64334|5|Briefly described|p39-40, 42|Ordovician|Ordovician|Amadeus Basin.||Larapinta Group.||Overlies Stairway Sandstone. Is overlain unconformably by Carmichael Sandstone.|Mudstones with carbonate interbeds.|
17363|Stokes Siltstone|64580|4|Described|map legend||Ordovician|Interbedded shale and siltstone; limestone; fine-grained sandstone.||||||09-DEC-08
17363|Stokes Siltstone|64778|6|Mentioned|p13|Ordovician|Ordovician|Amadeus Basin.||||||
17363|Stokes Siltstone|64809|5|Briefly described|p2, p3 Fig.2, p11 Fig.10, p13 Fig.13 |Middle Ordovician|Middle Ordovician|Deposition on an open shelf in well-oxygenated waters.||||||
17363|Stokes Siltstone|65233|4|Described|p3 Fig. 2, p10|Late Ordovician|Early Ordovician|Of lower Larapinta Group. Gradational over Stairway Sandstone. Age: Middle Llanvirnian. Max. thickness: 650m. Geological province: Amadeus Basin.  Succession of fine clastics dominated by shale and siltstone with occasional evaporites.||||||07-FEB-11
17363|Stokes Siltstone|65256|6|Mentioned|p19|Ordovician|Ordovician|Of the Larapinta Group.||||||
17363|Stokes Siltstone|65449|5|Briefly described|p34-35||Darriwilian|Amadeus Basin. The lower part of this unit is correlated with Nita Formation on the basis of conodonts.||||Is overlain disconformably by Carmichael Sandstone. Time-correlative with Carribuddy Group and Worral Formation.||
17363|Stokes Siltstone|65489|5|Briefly described|p63, p125|Ordovician|Ordovician|Amadeus Basin. Could act as a caprock due to its low permeability.||Unit in Larapinta Group.||Overlies Stairway Sandstone. Is overlain by Carmichael Sandstone.||
17363|Stokes Siltstone|67326|5|Briefly described|p2|Late Ordovician|Early Ordovician|Amadeus Basin.||Larapinta Group.||Overlies Stairway Sandstone. Is overlain by Carmichael Sandstone.||
17363|Stokes Siltstone|67565|5|Briefly described|p41, p51. |Late Ordovician|Middle Ordovician|A recessive unit, outcropping poorly on valley floors. Up to 461 m thick. A seal in the Mereenie oil/gas field. Contains halite pseudomorphs, brachiopods and pelecypods.|||||Variegated siltstone, fine-grained grey silty sandstone, and grey-brown and orange-brown thinly-bedded and highly fossiliferous  limestone.|
17363|Stokes Siltstone|67856|4|Described|p338 fig 4-30, p347 tab 4-9, p337, p346|Late Ordovician|Middle Ordovician|Of Wells et al., 1964, 1970 etc. Type section: near Stokes Pass 23o35'S 132o07'E. Up to 650m thick (north Amadeus Basin) thinning southwards to 20-100m. Fossiliferous. Represents a variety of depositional environments, the upper part may be of high salinity.||Of Larapinta Group.||Unconformably overlain by Mereenie Sandstone (in WA), elsewhere conformably overlain by Carmichael Sandstone. Conformably overlies Stairway Sandstone or Proterozoic rocks.|Fossiliferous calcarenite. Red or green interbedded shale and siltstone; limestone interbeds; fine-grained sandstone.|
17363|Stokes Siltstone|68297|5|Briefly described|p177|Ordovician|Ordovician|Amadeus Basin. Includes disarticulated vertebrate fossils.||||Younger than Stairway Sandstone||
17363|Stokes Siltstone|68323|6|Mentioned|p4 Fig.2|Late Ordovician|Early Ordovician|Amadeus Basin.||Larapinta Group.||||
17363|Stokes Siltstone|69437|5|Briefly described|p22:10|Ordovician|Ordovician|Amadeus Basin.||||Overlies Stairway Sandstone. Is overlain by Carmichael Sandstone.||12-JUL-16
17363|Stokes Siltstone|69438|3|Fully described|p23:2-3, 32, 36, 56-57, 60|Late Ordovician|Middle Ordovician|Redefined by Wells et al. (1970). Originally the Stokes Formation of Pritchard and Quinlan (1962). Was formerly mapped (Pritchard and Quinlan, 1962) as including rocks which were subsequently (Wells et al., 1970) assigned as a separate Formation (the Carmichael Sandstone). Type section is at Stokes Pass. Amadeus Basin. A recessive, valley forming unit, c.650m thick in the north-central part of the Basin, thinning southwards to 20m. Represents a range of depositional environments. Contains relatively few fossils (listed). Thick shales seal Stairway Sandstone reservoirs.||Larapinta Group.||Conformably and gradationally overlies Stairway Sandstone. Is overlain unconformably by Carmichael Sandstone.|A succession of interbedded shale and siltstone, with thin beds of silty-sandy limestone containing abundant fossil debris; red shale and lesser grey-green siltstone; and interbedded red to green shale, grey-green siltstone and fine sandstone.|12-JUL-16
17363|Stokes Siltstone|69443|6|Mentioned|p28:27|||Amadeus Basin.||||Correlated with Toko Group.||12-JUL-16
17363|Stokes Siltstone|69447|6|Mentioned|p32:5|||Amadeus Basin. Contains fossils with affinities to Hanson River beds (Wiso Basin).||||||12-JUL-16
17363|Stokes Siltstone|69449|6|Mentioned|p34:2 Fig.34.2|Ordovician|Ordovician|Eastern Amadeus Basin.||||||12-JUL-16
17363|Stokes Siltstone|69673|5|Briefly described|p64 fig 53, p66, p88, p89, p149 fig 120|Ordovician|Cambrian|650m thick. Deposited in shallow marine environment. Thick seal on the Stairway Sandstone.||Larapinta Group||Conformably overlies Stairway Sandstone, overlain by Carmichael Sandstone|Interbedded shale, sandstone and silstone, thin beds of fossiliferous limestone.|
17363|Stokes Siltstone|70793|4|Described|500k_interpgeop14_lut.csv|Late Ordovician|Middle Ordovician|Of Amadeus Basin (Phase 2). Events: Alice Springs Orogeny (450-295 Ma); Rodingan Movement (Alice Springs Orogeny phase 1) (450-420 Ma). See 500k_interpgeop14_lut.csv, 2_5m_interpgeop15_lut.csv.|470-443.4 Ma (biostrat)||||Interbedded shale and siltstone; limestone; fine-grained sandstone|
17363|Stokes Siltstone|70826|6|Mentioned|p7 tbl 3|Silurian|Ordovician|Amadeus Basin.||||||
17363|Stokes Siltstone|71146|5|Briefly described|p6,  p43 fig 33|Late Ordovician|Middle Ordovician|Amadeus Basin.||Larapinta Group||Overlies the Stairway Sandstone.|Carbonate, mudstone and siltstone.|
17363|Stokes Siltstone|71171|6|Mentioned|p2|||Amadeus Basin.||||||
17363|Stokes Siltstone|71268|4|Described|GEOL_LUT_CSV files|Late Ordovician|Middle Ordovician|Of Amadeus Basin (Phase 2). Events: Rodingan Movement (Alice Springs Orogeny phase 1) (450-420 Ma). See 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|470-443.4 Ma (biostrat)||||Interbedded shale and siltstone; limestone; fine-grained sandstone|
17363|Stokes Siltstone|71279|5|Briefly described|p355 Fig.2,p365,p370,p373-375,p382 Tb.1|Late Ordovician|Early Ordovician|Amadeus Basin. Linear magnetic anomalies discussed. Modelled magnetic properties.||Larapinta Group.||||
17363|Stokes Siltstone|71800|6|Mentioned|p26 fig 3|Late Ordovician|Middle Ordovician|Amadeus Basin.||||Overlies the Stairway Sandstone. Unconformably overlain by the Carmichael Sandstone.||
17363|Stokes Siltstone|72034|5|Briefly described|500k_interpgeop16_lut|Late Ordovician|Middle Ordovician|Amadeus Basin (Phase 2).  Age from biostratigraphy.|||||Interbedded shale and siltstone; limestone; fine-grained sandstone.|
17363|Stokes Siltstone|72369|4|Described|iii,p3-4,29,31-34|||Of Amadeus Basin. most poorly exposed unit of Larapinta Group, but laterally extensive. No previous geochronologcal constraint, however biostratigraphic age constraint provided by conodont macrofossils at early Gisbornian (460-456 Ma; Gibb et al 2009). LA-ICP-MS U-Pb detrital zircon dating of sample HB15ND553 (micaceous siltstone) yielded an interpreted maximum depositional age of 493+\-5 Ma (youngest concordant zircon), but does not further constrain the age of the formation as it predates macrofossil age constraints at c. 460-456 Ma (e.g. Giss et al., 2008; Nicoll in Kennard et al 1986, Zhang et al 2003). Contains small groupings of Mesoproterozoic age zircon populations likely derived from Musgrave province. Paleoproterozoic to early Mesoproterozoic zircons (c. 2200-1475 Ma) may have been recycled from buried Cambrian and Neoproterozoic stratigraphy, or reflect input from proximal Aileron, Warumpi and Musgrave provinces, or distal east Gondwanan input. Cambrian zircon populations (c. 580-490 Ma) may have been derived from distal east Gondwanan input, as there are no known Cambrian sources proximal to Amadeus Basin. Sample locality, zircon description, SHRIMP results and analyses are discussed.||Unit of Larapinta Group.||Overlain unconformably by Carmichael Sandstone. Underlain conformably by Stairway Sandstone.|Lower siltstone and limestone; sparsely fossiliferous succession, overlain by red and purple sandstone and shale.|18-DEC-19
17363|Stokes Siltstone|73085|6|Mentioned|p1|late Ordovician|early Ordovician|||||Underlain by Stairway Sandstone. Overlain by Carmichael Sandstone.||
17363|Stokes Siltstone|73119|6|Mentioned|p19|early Gisbornian|early Gisbornian|Age from Gibb et al. (2009).|460-456 Ma|||Conformably underlain by Stairway Sandstone.||
17363|Stokes Siltstone|73279|5|Briefly described|p3, p12|Ordovician|Ordovician|Amadeus Basin. Detrital zircons analysed for Hf isotopic composition [see article].||Larapinta Group||Underlain by Stairway Sandstone. Overlain by Carmichael Sandstone.|Includes siltstone.|
17363|Stokes Siltstone|73346|6|Mentioned|p18|Late Ordovician|Darriwilian|Amadeus Basin. Includes the arandaspids Areyongalepis oervigi, Apedolepis tomlinsonae, and Sacabambaspis sp.||||||
17367|Stonewall Sandstone|22547|5|Briefly described|p24|||Of the Carr Boyd Group. Overlies Glenhill Formation, overlain by Pincombe Formation.||||||14-NOV-06
17367|Stonewall Sandstone|22754|5|Briefly described|p11 Tb. 3|Mesoproterozoic|Mesoproterozoic|Of the Carr Boyd Group.||||||
17367|Stonewall Sandstone|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
17367|Stonewall Sandstone|32660|5|Briefly described|Table 6|||||||||
17367|Stonewall Sandstone|32664|6|Mentioned|Map legend|Adelaidean|Adelaidean|Briefly described in notes||||||
17367|Stonewall Sandstone|32728|5|Briefly described|Table 6|||||||||
17367|Stonewall Sandstone|36551|6|Mentioned|Table 12|||||||||
17367|Stonewall Sandstone|36885|4|Described|p179|||||||||
17367|Stonewall Sandstone|37462|6|Mentioned|Fig.4.13|||||||||
17367|Stonewall Sandstone|44155|5|Briefly described|p250 Tb.3-10|||300-450m thick.||Carr Boyd Group||Overlies Glenhill Formation unconformably or Kimberley Group unconformably. Is overlain gradationally by Pincombe Formation.|Subfriable medium- to coarse-grained quartz sandstone, subordinate argillaceous and feldspathic sandstone, granule sandstone, red shale.|
17367|Stonewall Sandstone|44230|5|Briefly described|Map Legend||Proterozoic|||||||
17367|Stonewall Sandstone|44363|5|Briefly described|p.6,14,16,17|||(Adelaidean) Of theCarr Boyd Group.||||||04-DEC-06
17367|Stonewall Sandstone|44364|14|Not recorded|map legend|||||||||
17367|Stonewall Sandstone|45047|4|Described|p35|||Of the Carr Boyd Group.||||||17-OCT-12
17367|Stonewall Sandstone|45112|6|Mentioned|p34|||||||||
17367|Stonewall Sandstone|65417|5|Briefly described|pp156-159, pp162-163.|Mesoproterozoic|Mesoproterozoic|Halls Creek Orogen. Correlated with Lalngang Sandstone of the Fitzmaurice Group (NT). Braided-delta progradation and retreat.||Unit in Carr Boyd Group.||Conformably overlies Glenhill Formation. Is overlain conformably by Pincombe Formation.||
17367|Stonewall Sandstone|69435|5|Briefly described|p20:3|||Carr Boyd Basin. A previous correlation  with the Lalngang Sandstone (Fitzmaurice group, NT) is called into question.||Carr Boyd Group.||Overlies Glenhill Formation. Is overlain by Pincombe Formation.||12-JUL-16
17367|Stonewall Sandstone|69673|6|Mentioned|p60 fig 48|||||Carr Boyd Group||Overlain by Pincombe Formation, overlies Glenhill Formation||
17367|Stonewall Sandstone|71267|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Carr Boyd Group.|||Quartz sandstone, feldspathic sandstone, shale|
17395|Strangways Metamorphic Complex|1490|6|Mentioned|p13|||Associated with the ~1780-1760 Ma Strangways Orogeny. Previously dated at 1790 +/- 35 (Rb-Sr: Black et al., 1983).|1760-1750 Ma.|||||
17395|Strangways Metamorphic Complex|9199|5|Briefly described|Map legend|Precambrian|Precambrian|Geological Province: Arunta Block.||||||03-NOV-04
17395|Strangways Metamorphic Complex|9694|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block (Division One). Includes: Kanandra Granulite.||||||
17395|Strangways Metamorphic Complex|22524|6|Mentioned|p39,43|||||||||
17395|Strangways Metamorphic Complex|23205|6|Mentioned|p42|Proterozoic|Proterozoic|Age: Early Proterozoic. of Arunta Block.||||||
17395|Strangways Metamorphic Complex|23361|5|Briefly described|12|||||||||
17395|Strangways Metamorphic Complex|23732|5|Briefly described|p2, 29|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Province.||||||07-NOV-08
17395|Strangways Metamorphic Complex|23733|5|Briefly described|p34 Fig.20|||Contains the Anuma schist.||||||
17395|Strangways Metamorphic Complex|23844|6|Mentioned|p40, 46|||See also Fig.26||||||
17395|Strangways Metamorphic Complex|23858|5|Briefly described|p921|||||||||
17395|Strangways Metamorphic Complex|23983|6|Mentioned|p42|||||||||
17395|Strangways Metamorphic Complex|23985|6|Mentioned|p1|||||||||
17395|Strangways Metamorphic Complex|24442|6|Mentioned|p3|||Geological Province: Arunta Province.||||||
17395|Strangways Metamorphic Complex|37462|5|Briefly described|Tab.4.VIII|||||||||
17395|Strangways Metamorphic Complex|38885|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
17395|Strangways Metamorphic Complex|38896|6|Mentioned|Table 1|||||||||
17395|Strangways Metamorphic Complex|39552|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
17395|Strangways Metamorphic Complex|39583|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
17395|Strangways Metamorphic Complex|39610|5|Briefly described|p4|||||||||
17395|Strangways Metamorphic Complex|39721|6|Mentioned|p28|||||||||
17395|Strangways Metamorphic Complex|39887|6|Mentioned|p453|||See also Fig.5||||||
17395|Strangways Metamorphic Complex|39888|6|Mentioned|Table 1|||||||||
17395|Strangways Metamorphic Complex|39898|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Block.||||||07-NOV-08
17395|Strangways Metamorphic Complex|39931|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
17395|Strangways Metamorphic Complex|40098|6|Mentioned|p224|||||||||
17395|Strangways Metamorphic Complex|40100|6|Mentioned|p255|||||||||
17395|Strangways Metamorphic Complex|40538|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Block.||||||07-NOV-08
17395|Strangways Metamorphic Complex|40906|4|Described|p6|||||||||
17395|Strangways Metamorphic Complex|41686|6|Mentioned|p64|||||||||
17395|Strangways Metamorphic Complex|41967|6|Mentioned|p235|||||||||
17395|Strangways Metamorphic Complex|42147|5|Briefly described|p670|||||||||
17395|Strangways Metamorphic Complex|42326|5|Briefly described|Table 2 P11|||||||||
17395|Strangways Metamorphic Complex|42770|5|Briefly described|p12, Fig.14|||see also Table 2, age of 1820-1800 Ma.||||||
17395|Strangways Metamorphic Complex|43225|5|Briefly described|Map Legend||Paleoproterozoic|of Arunta Block||||||07-NOV-08
17395|Strangways Metamorphic Complex|43503|5|Briefly described|6|||||||||
17395|Strangways Metamorphic Complex|43568|6|Mentioned|p505|||||||||
17395|Strangways Metamorphic Complex|44114|5|Briefly described|p317-320, 323, 327-332, 338-342|||Central Arunta province. Is presented as SMC after p318.|||Anamarra Granite.|Locally faulted against Harts Range Group.|Pelites and calc-silicate rocks, and quarzites.|
17395|Strangways Metamorphic Complex|46868|6|Mentioned|p76|||Variation of Strangways Range?||||||
17395|Strangways Metamorphic Complex|46884|6|Mentioned|p227|||||||||
17395|Strangways Metamorphic Complex|48992|1|Redefined|p49|Proterozoic|Proterozoic|||||||
17395|Strangways Metamorphic Complex|50246|5|Briefly described|p3|Paleoproterozoic|Paleoproterozoic|Age: 1820-1800Ma.||||||07-FEB-11
17395|Strangways Metamorphic Complex|50369|6|Mentioned|p8.1|||Geological Province: Arunta Inlier.||||||
17395|Strangways Metamorphic Complex|60525|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block (Division 1).||||||
17395|Strangways Metamorphic Complex|60547|5|Briefly described|Map Legend|Precambrian|Precambrian|Geological Province: Arunta Block.||||||06-JUN-05
17395|Strangways Metamorphic Complex|60551|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block.||||||
17395|Strangways Metamorphic Complex|60668|6|Mentioned|p11, p2 Tb. 1|||Includes Kanandra Granulite.||||||
17395|Strangways Metamorphic Complex|61208|5|Briefly described|p205|Paleoproterozoic|Paleoproterozoic|Consists of sedimentary, volcanic and intrusive rocks. Overlain by Mendip Metamorphics, Ledan Schist and Utopia Quartzite. Age: ca.1.81-ca.1.79Ga. Geological Province: Arunta Inlier.||||||07-NOV-08
17395|Strangways Metamorphic Complex|61309|6|Mentioned|p12|||Geological Province: western Arunta Inlier.||||||06-FEB-08
17395|Strangways Metamorphic Complex|62595|5|Briefly described|p1, p6, p11, p15, p17, p33 Fig.13.|Paleoproterozoic|Paleoproterozoic|Aileron Province. This unit includes the older rocks of the Province; younger units comprise the Oonagalabi Assemblage. The lower part of this unit is included in Scrimgeour's (2003) Ongeva package. Hosts Zn-Pb-Cu(Ag-Au) deposits.|1840-1800 Ma.||||Includes mylonitic mafic and felsic gneiss.|
17395|Strangways Metamorphic Complex|63261|6|Mentioned|p23|||Geological province: Arunta region.||||||07-FEB-11
17395|Strangways Metamorphic Complex|63562|6|Mentioned|p345 Fig.7.|Paleoproterozoic|Paleoproterozoic|Georgina Basin.||||||
17395|Strangways Metamorphic Complex|63866|5|Briefly described|p93|||Aileron Province.||||||
17395|Strangways Metamorphic Complex|64068|5|Briefly described|p31, 32|||Lower part bundled in with Deep Bore Metamorphics, Bonya Schist and Cackleberry Metamorphics as the Ongeva package; likely equivalent to lower Hatches Creek Group in Davenport Province. Upper part included in the 1780-1760 Ma Cadney package.||||||
17395|Strangways Metamorphic Complex|64337|6|Mentioned|p374|Paleoproterozoic|Paleoproterozoic|Granulite grade Proterozoic basement.||||||
17395|Strangways Metamorphic Complex|64366|5|Briefly described|p604, p605 Fig. 2|||This complex experienced two cycles of metamorphism and intense deformation that reworked the earlier metamorphic assemblages and structures - developing mylonitic fabrics and kilometre-long sheath folds that define the overall structural trend in the area||||||19-JUN-13
17395|Strangways Metamorphic Complex|64574|5|Briefly described|p703, p705, p706, p715, p716|Paleoproterozoic|Paleoproterozoic|Metasedimentary, volcanics and intrusive rocks dominated by granulite-facies.||||||
17395|Strangways Metamorphic Complex|64735|5|Briefly described|p216, p217|Orosirian|Orosirian|Arunta Region; produced by the Strangways Event of 1740 - 1690 Ma. Protoliths to this unit are called Ongeva Package: metamorphosed volcanics dated to 1810 - 1800 Ma.||||||30-APR-12
17395|Strangways Metamorphic Complex|64737|6|Mentioned|p231-2|||Metamorphosed Ongeva Package.||||||01-MAY-12
17395|Strangways Metamorphic Complex|64738|5|Briefly described|pp246-261.|Paleoproterozoic|Paleoproterozoic|A 40 km x 80 km SE-trending, fault-bound block of deformed granulite-facies metamorphics and migmatites.|Protoliths c.1810-1800 Ma.||||Protoliths include metamorphosed siliciclastic and carbonate sedimentary rocks, bimodal volcanic and volcaniclastic and intrusive rocks.|23-APR-12
17395|Strangways Metamorphic Complex|65341|5|Briefly described|p2 Fig.2, p3. |Paleoproterozoic|Paleoproterozoic||Deposition 1810 - 1800 Ma.||Includes Mapata Gneiss.|||
17395|Strangways Metamorphic Complex|65358|6|Mentioned|p17|||Aileron Province.||||||
17395|Strangways Metamorphic Complex|66767|6|Mentioned|p60|||Is juxtaposed against the Irindina Province by the Florence-Mueller Shear Zone.||||||
17395|Strangways Metamorphic Complex|66860|4|Described|p7-92 (as SMC)|||Abbreviated to SMC. Thick package of complexly folded mafic and felsic granulites and metasediments, with subordinate granitic bodies. Most is older than 1780 Ma, but it is possible that some is as young as 1745 Ma.|||Includes Wuluma Granite, Cadney and Erontonga Metamorphics, Utnalanama Granulite.|||15-DEC-16
17395|Strangways Metamorphic Complex|67114|5|Briefly described|p758|Proterozoic|Proterozoic|Aileron Province, North Australian Craton. After the first mention, it appears in the text generally as SMC. Granulite-facies metamorphism occurred between 1.78 and 1.69 Ga.||||Is intruded by Anamarra and Wuluma Granites.|Sedimentary and igneous rocks, metamorphosed to granulite facies.|
17395|Strangways Metamorphic Complex|67565|6|Mentioned|p5 Fig.3.|||Aileron Province.||||||
17395|Strangways Metamorphic Complex|68150|6|Mentioned|p.viii, p10|||High-grade metamorphic conditions appear to have prevailed from ca. 1740 to 1690 Ma.||||||
17395|Strangways Metamorphic Complex|68517|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Arunta Block. Early Proterozoic? age.|||Includes Bungitina metamorphics.|||
17395|Strangways Metamorphic Complex|69226|5|Briefly described|p238-239|||Produced by the Strangways Orogeny.|1780-1720 Ma.|||||
17395|Strangways Metamorphic Complex|69227|5|Briefly described|p263, p278-280, p282-283|Proterozoic|Proterozoic|Stewart et al. (1980). Metamorphosed during the 1780-1710 Ma Strangways Event. Contacts the Harts Range Group along the Florence-Muller Shear Zone. Abbreviated to Strangways Complex in places.|||Kanandra Granulite, Entia Gneiss.|||
17395|Strangways Metamorphic Complex|69383|6|Mentioned|p65, 81|||One source of zircons in the unnamed granite intruding Kanandra Granulite.||||Underlies rocks of the Ledan Package.||
17395|Strangways Metamorphic Complex|69417|5|Briefly described|p2:5, 8-9|Orosirian|Orosirian|S and E Aileron Province. Widespread volcanism, volcaniclastic sedimentation and VMS mineralisation in this Complex is attributed to a back-arc basin environment at 1810-1800 Ma.||||||12-JUL-16
17395|Strangways Metamorphic Complex|69425|6|Mentioned|p10:4|||Ongeva Package, Arunta Region. Mentioned as possible correlative of Hatches Creek Group.||||||12-JUL-16
17395|Strangways Metamorphic Complex|69427|3|Fully described|p12:3,8-14,18,20,23,31,34,37-38,47,50-53|||SE Aileron Province. Described in two parts, lower and upper, which have no nomenclatural significance. The package comprising Deep Bore, Cackleberry and Delmore Metamorphics and part of Bonya Schist may be equivalent to the lower part of the Strangways Metamorphic Complex. Significant 1810-1800 Ma tholeiitic mafic intrusions in the lower part (associated with Stafford Event). Metamorphism described in some detail, with two events at 1730-1720 Ma and 1700-1690 Ma. The Irindina Province was thrust over this Complex along the Florence-Mueller Shear Zone, during the Alice Springs Orogeny. Zircon overgrowths occurred at 443 +/- 6 Ma (Rodingan Event). Hosts several Pb-Zn-Cu(-Ag-Au) prospects, each of which is described in some detail.|1810-1780? Ma.||Erontonga, Cadney Metamorphics; Utnalanama, Yambah and Ongeva Granulites; Ingula Migmatite; Mapata Gneiss.||A thick package of complexly folded mafic and felsic granulites (after bimodal volcanics and/or intrusives) and metasedimentary rocks (pelites passing upwards into a siliciclastic and carbonate succession); subordinate granite bodies.|12-JUL-16
17395|Strangways Metamorphic Complex|69444|6|Mentioned|p29:6-7|Paleoproterozoic|Paleoproterozoic|Experienced little or no effects from the Larapinta Event (480-460 Ma) in the Irindina Province. Was juxtaposed against the Irindina Province along the Florence-Mueller Shear Zone by the Rodingan Event (450-440 Ma).||||||12-JUL-16
17395|Strangways Metamorphic Complex|69917|6|Mentioned|p70, 82, 87|||Intruded by north-striking mafic dykes at ca 1690 Ma.||||Broadly correlated with Delny Metamorphics.||
17395|Strangways Metamorphic Complex|69928|6|Mentioned|p210, 224|||||||||
17395|Strangways Metamorphic Complex|69929|6|Mentioned|p229-230, 232-234, 242-246|||Arunta Block. Parts of this Complex were uplifted and cooled through 500 degrees C at c.400 Ma.|||Cadney Metamorphics.||Mafic and felsic granulites; retrograded to schists in shear zones.|
17395|Strangways Metamorphic Complex|69931|6|Mentioned|p267|||Central Province, Arunta Inlier. Presented as Strangway Metamorphic Complex.|||||Multiply-folded mafic and felsic orthogneisses intercalated with and locally overlain by subordinate metasediments.|
17395|Strangways Metamorphic Complex|69937|6|Mentioned|p27, p30|||Possible source of some zircons in the Cyclops and Waldo Pedlar Members of the Pertatataka Formation.|1815-1780 Ma (protoliths).|||||
17395|Strangways Metamorphic Complex|70094|6|Mentioned|p77|||Basement to Harts Range Group.||||||
17395|Strangways Metamorphic Complex|70739|6|Mentioned|p538-541, 560-561, 563|||Southern Aileron Province, Arunta Region. Abbreviated in the text to SMC. Zircon rim growth occurred c.1720 Ma.|1810-1780 Ma (sedimentary protoliths).|||||
17395|Strangways Metamorphic Complex|70825|6|Mentioned|p39-42, 47, 49-52|Proterozoic|Proterozoic|Arunta Region, North Australian Craton. Abbreviated to SMC in most of the article. Deformed and partially hydrated during the 380-320 Ma Alice Springs Orogeny via shear zones (discussed in great detail).||||||
17395|Strangways Metamorphic Complex|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen. Bvoth ages are of crystallisation: U-Pb zircon SHRIMP.|1727+/-2 Ma and 1717+/-2 Ma.||||Concordant leucosome, discordant leucosome.|
17395|Strangways Metamorphic Complex|71840|5|Briefly described|p2|||Geological province: Aileron Province. U-Pb dating yield age of c. 1815-1780 Ma for protolith ages, based on zircon dating from probably volcaniclastic rocks (Hussey et al 2006, Scrimgeour 2013).||||||
17395|Strangways Metamorphic Complex|72091|6|Mentioned|p1, 8|||Aileron Province, Arunta Orogen. Protolith ages interpreted to range ca. 1815-1780 Ma based on zircon dating of probable volcaniclastic rocks (Hussey et al., 2006, Scrimgeour 2013).||||||
17395|Strangways Metamorphic Complex|72378|5|Briefly described|p6,15|Paleoproterozoic|Paleoproterozoic|Geological province: Aileron Province. Maximum depositional and magmatic crystallisation ages of c. 1.8 Ga (Hussey et al., 2006; Scrimgeour, 2013).||||Overlain by Cadney Metamorphics, Bungitina metamorphics.||
17395|Strangways Metamorphic Complex|72516|5|Briefly described|p8, p64|Paleoproterozoic|Paleoproterozoic|Aileron Province. Previously interpreted to be an age equivalent to the Bonya Metamorphics. See also Strangways Metamorphics p7, p9. Crops out primarily in the Strangways Ranges northeast of Alice Springs.|||||Granulite facies metasedimentary rocks and bimodal intrusive rocks.|27-MAY-21
17395|Strangways Metamorphic Complex|72711|6|Mentioned|p6.|||Text refers to image in Fig.4c at the Johnnies Reward prospect.|||||Granulite metapelitic/quartzofeldspathic gneiss, garnet schist, and marble. Biotite and garnet schist containing minor disseminated sulfides (including chalcopyrite and pyrite)|
17395|Strangways Metamorphic Complex|72894|6|Mentioned|p19|Statherian|Orosirian|Age from Scrimgeour (2013).|ca 1820-1790 Ma|||||
17395|Strangways Metamorphic Complex|73592|6|Mentioned|p9|||Hussey et al. (2006). Hosts Utnalanama-type metamorphosed VMS deposits aged c.2.1-1.8 Ga.||||||
17418|Stray Creek Sandstone|9324|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Tolmer Group. Quartz arenite, flaggy, micaceous, ripple marked.||||||
17418|Stray Creek Sandstone|14019|5|Briefly described|p4 Fig. 3|||Of the Tolmer Group.||||||
17418|Stray Creek Sandstone|22809|3|Fully described|15|||Of theTolmer Group. Underlain by Depot Creek Sandstone.||||||04-DEC-06
17418|Stray Creek Sandstone|22810|4|Described|Table3 P7, P18||Proterozoic|Conformably overlies Depot Creek Sandstone.||||||04-DEC-06
17418|Stray Creek Sandstone|22813|5|Briefly described|Map|Mesoproterozoic|Mesoproterozoic|Overlies Depot Creek Sandstone. Of the Tolmer Group. Laminated micaceous quartz sandstone and siltstone, commonly glauconitic and ripple marked.||||||04-DEC-06
17418|Stray Creek Sandstone|23714|5|Briefly described|p36|Proterozoic|Proterozoic|Of Tolmer Group. Overlain by Hinde Dolomite. Max. thickness: 450 m.||||||04-DEC-06
17418|Stray Creek Sandstone|24047|6|Mentioned|p107 Appendix 1|||Geological Province: Pine Creek Orogen.||||||
17418|Stray Creek Sandstone|24122|5|Briefly described|p4 Fig.3|||Of Tolmer Group.  Geological Province: Birrindudu Basin.||||||
17418|Stray Creek Sandstone|24297|5|Briefly described|p4 Fig.3|Proterozoic|Proterozoic|Of Tolmer Group.  Geological Province: Birrindudu Basin.||||||
17418|Stray Creek Sandstone|24441|5|Briefly described|p1 Fig. 1|||Of the Tolmer Group. Overlies Depot Creek Sandstone; overlain by Hinde Dolostone. Geological Province: Birrindudu Basin.||||||
17418|Stray Creek Sandstone|24442|5|Briefly described|p50 Fig. 1|||Of the Tolmer Group.  Geological Province: Birrindudu Basin.||||||
17418|Stray Creek Sandstone|39679|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
17418|Stray Creek Sandstone|40168|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Tolmer Group. Laminated to thinly bedded very fine brown quartzite, micaceous sandy siltstone, limonitic micaceous siltstone.||||||18-OCT-05
17418|Stray Creek Sandstone|40957|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
17418|Stray Creek Sandstone|41660|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of Tolmer Group. Quartz arenite, often micaceous, flaggy, ripple-marked and cross-bedded, siderite marker horizon. Thickness: ~ 800m.||||||07-OCT-05
17418|Stray Creek Sandstone|41661|3|Fully described|p19|||||||||
17418|Stray Creek Sandstone|41663|6|Mentioned|p42|||||||||
17418|Stray Creek Sandstone|42012|4|Described|p13|||||||||
17418|Stray Creek Sandstone|42014|5|Briefly described|Map legend|Cambrian|Mesoproterozoic|||||||
17418|Stray Creek Sandstone|43140|4|Described|p4||Mesoproterozoic|Of the Tolmer Group.||||||04-DEC-06
17418|Stray Creek Sandstone|43187|5|Briefly described|p2|||||||||
17418|Stray Creek Sandstone|43832|4|Described|29,Table7 p27, 97||Mesoproterozoic|||||||
17418|Stray Creek Sandstone|60685|5|Briefly described|p4 Fig. 3|||Of the Tolmer Group. Geological Province: Birrindudu Basin.||||||
17418|Stray Creek Sandstone|64698|4|Described|lithinterp table|Statherian|Orosirian|Age ~1700-1825Ma. Tolmer Group.  Max. thickness 800m. Quartz arenite, flaggy, micaeous, ripple marked. Conformably overlies Depot Creek Sandstone. Conformably overlain by Hinde Dolostone (misspelt as Hindrance Dolostone in this dataset).||||||07-JAN-09
17418|Stray Creek Sandstone|65232|6|Mentioned|App. 2|||||||||09-FEB-10
17418|Stray Creek Sandstone|65342|6|Mentioned|p11 Fig.13. |||Birrindudu Basin.||Unit in Tolmer Group.||Overlies Depot Creek Sandstone. Is overlain by Hinde Dolostone.||
17418|Stray Creek Sandstone|67167|5|Briefly described|Map legend.|||||Unit in Tolmer Group.|||Laminated quartz sandstone and siltstone, commonly glauconitic and ripple marked.|
17418|Stray Creek Sandstone|67186|5|Briefly described|Map legend.|||||Unit in Tolmer Group.||Overlies Depot Creek Sandstone. Is overlain by Hinde Dolostone.|Laminated quartz sandstone and siltstone, commonly glauconitic and ripple-marked.|23-NOV-11
17418|Stray Creek Sandstone|67479|6|Mentioned|p16|||||||Conformably underlain by the Depot Creek Sandstone.||
17418|Stray Creek Sandstone|67779|5|Briefly described|p6 Fig.5.|Paleoproterozoic|Paleoproterozoic|Litchfield Province, Pine Creek Orogen.||Unit in Tolmer Group.||||
17418|Stray 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. Typically c.180m thick; up to 300m. Paralic becoming tidal shallow-marine deposits.||Tolmer Group.||Conformably overlies Depot Creek Sandstone. Is overlain conformably by Hinde Dolostone.|Cross-bedded and ripple-marked, medium- to coarse-grained sandstone, conglomerate and orthoquartzite. Interbeds of siltstone and glauconitic siltstone, and minor sedimentary carbonate and distinctive 2-5m siderite intervals, in upper parts.|12-JUL-16
17418|Stray Creek Sandstone|69442|6|Mentioned|p27:3 Tb.27.1; 5-6|||||||Is overlain unconformably by Uniya Formation.||12-JUL-16
17418|Stray Creek Sandstone|69673|6|Mentioned|p48 fig 35|||||Tolmer Group||Overlain by Hinde Dolostone, overlies Depot Creek Sandstone||
17418|Stray Creek Sandstone|70866|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Tolmer Group.||Conformably overlies Depot Creek Sandstone. Is overlain conformably by Hinde Dolostone.|Laminated quartz sandstone and siltstone, commonly glauconitic and ripple-marked, dolomitic in places.|
17418|Stray Creek Sandstone|71302|5|Briefly described|p6|Paleoproterozoic|Paleoproterozoic|Of Birindudu Basin.||Unit of Tolmer Group.||||
17426|Stretton Sandstone|22453|6|Mentioned|p 12|||In the McArthur Basin.||||||06-NOV-06
17426|Stretton Sandstone|22538|6|Mentioned|P717||Statherian|Age of unit is 1625+/-2 Ma.||||||06-NOV-06
17426|Stretton Sandstone|22664|6|Mentioned|35|Paleoproterozoic|Paleoproterozoic|Batten Subgroup, McArthur Basin||||||07-NOV-08
17426|Stretton Sandstone|22853|3|Fully described|23|Proterozoic|Proterozoic|Of Batten Subgroup. Max thickness: 160 m. Overlying units: Smythe Sandstone and Looking Glass Formation;  underlain by Yalco Formation||||||05-DEC-06
17426|Stretton Sandstone|23387|6|Mentioned|p18 fig.19|||||||||
17426|Stretton Sandstone|23397|5|Briefly described|p474|Statherian|Statherian|Age: 1625+/-2Ma.||||||06-NOV-06
17426|Stretton Sandstone|23398|5|Briefly described|p445|Statherian|Statherian|Age: 1625+/-2Ma.||||||06-NOV-06
17426|Stretton Sandstone|23407|5|Briefly described|p627 Fig.2|Statherian|Statherian|Age: 1625+/-2Ma.||||||06-NOV-06
17426|Stretton Sandstone|23776|5|Briefly described|p705 Fig 2.|Statherian|Statherian|Age: 1625+/-2 Ma. Of Batten Subgroup.||||||20-JUL-06
17426|Stretton Sandstone|23902|4|Described|p1568 Fig.2|||Of the Batten Subgroup. Overlies the Lynott Formation. Overlain by Looking Glass Formation and Amos Formation. Geological Province: McArthur Basin.||||||05-OCT-07
17426|Stretton Sandstone|23910|5|Briefly described|p292 Fig. 2|||Of Batten Subgroup.  Geological Province: McArthur Basin.||||||06-NOV-06
17426|Stretton Sandstone|23937|5|Briefly described|p9, p25 Tb. 2|Statherian|Statherian|Of the Batten Subgroup (McArthur Group). Outcrops on Maria Island - of light grey to purple, medium bedded, fine quartz sandstone.  Age: 1625Ma.  Geological Province: McArthur Basin.||||||03-NOV-04
17426|Stretton Sandstone|23963|5|Briefly described|p1239 Fig.2|||Geological Province: McArthur Basin. Of the Batten Subgroup (McArthur Group).||||||06-NOV-06
17426|Stretton Sandstone|24048|5|Briefly described|p59|Statherian|Statherian|Age: 1625+/-2Ma.||||||
17426|Stretton Sandstone|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Of Batten Subgroup. Overlies Yalco Formation. Geological Province: Southern McArthur Basin.||||||
17426|Stretton Sandstone|30344|6|Mentioned|Fig.4|||Part of Batten Subgroup||||||
17426|Stretton Sandstone|32658|4|Described|Table 2|||See also Fig.3||||||
17426|Stretton Sandstone|32660|5|Briefly described|Table 4|||||||||
17426|Stretton Sandstone|33666|6|Mentioned|Table 1|||||||||
17426|Stretton Sandstone|35261|6|Mentioned|Fig.2|||||||||
17426|Stretton Sandstone|38582|6|Mentioned|Fig.3|||||||||
17426|Stretton Sandstone|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
17426|Stretton Sandstone|40259|6|Mentioned|Table 1|||||||||
17426|Stretton Sandstone|40691|5|Briefly described|p12|||||||||
17426|Stretton Sandstone|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
17426|Stretton Sandstone|41268|6|Mentioned|p297|||||||||
17426|Stretton Sandstone|41277|6|Mentioned|Fig.2|||||||||
17426|Stretton Sandstone|42385|4|Described|p23|||See also Table 4 p16.||||||06-NOV-06
17426|Stretton Sandstone|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
17426|Stretton Sandstone|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.||Of Batten Subgroup (McArthur Group).||In schematic section, underlies Smythe Sandstone, Amos Formation and Looking Glass Formation; overlies Yalco Formation.|Quartzarenite. Detailed lithology given.|09-NOV-11
17426|Stretton Sandstone|42639|4|Described|p33, Table 5 p20|||||||||
17426|Stretton Sandstone|42739|5|Briefly described|map legend|Statherian|Statherian|Of the Batten Subgroup. Very fine to medium grained, thin to medium bedded quartzarenite, in places micaceous or glauconitic.||||||19-OCT-05
17426|Stretton Sandstone|42812|4|Described|p42, Table 4|||Of Batten Subgroup.||||||05-DEC-06
17426|Stretton Sandstone|42846|5|Briefly described|Fig.1 p502|||Of McArthur Group. Geological Province: McArthur Basin.||||||09-MAY-05
17426|Stretton Sandstone|42935|6|Mentioned|p529 Fig.2|||Of the Batten Subgroup (McArthur Group).||||||06-NOV-06
17426|Stretton Sandstone|43010|6|Mentioned|p128|||||||||
17426|Stretton Sandstone|43036|6|Mentioned|Fig.5|||In the McArthur Group.||||||06-NOV-06
17426|Stretton Sandstone|43486|5|Briefly described|21|||||||||
17426|Stretton Sandstone|44287|14|Not recorded|p.10, opp.9|||(E53-3).||||||
17426|Stretton Sandstone|44288|14|Not recorded|map legend|||Flaggy quartz sandstone. Lower (?) Proterozoic.||||||
17426|Stretton Sandstone|44434|14|Not recorded|p.7, opp. p.6, map|||Top formation of Batten Subgroup (McArthur Group). (D53-11,12).||||||
17426|Stretton Sandstone|44435|14|Not recorded|map legend|||Lower (?) Proterozoic.||||||
17426|Stretton Sandstone|44530|14|Not recorded|p.10, opp.10|||(D53-15).||||||
17426|Stretton Sandstone|44531|14|Not recorded|map legend|||Lower (?) Proterozoic.||||||
17426|Stretton Sandstone|45162|2|Defined|p126-130|Proterozoic|Proterozoic|||||||06-APR-18
17426|Stretton Sandstone|46915|6|Mentioned|Fig.1|||Stratigraphic section through McArthur Group.||||||
17426|Stretton Sandstone|46968|6|Mentioned|Fig.2|||||||||
17426|Stretton Sandstone|60483|5|Briefly described|p7 Fig. 5, p8, p30|Paleoproterozoic|Paleoproterozoic|Of Batten Subgroup (McArthur Group). Age: 1625+/-2Ma. Geological Province: McArthur Basin.||||||07-NOV-08
17426|Stretton Sandstone|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Batten Subgroup. Overlian by Looking Glass Formation, underlain by Yalco Formation.||||||
17426|Stretton Sandstone|60573|5|Briefly described|Map legend|Statherian|Statherian|Of the McArthur Group. Hummocky cross stratified very fine sandstone.||||||
17426|Stretton Sandstone|61390|5|Briefly described|Map Legend|Statherian|Statherian|Of the McArthur Group. Hummocky cross-stratified very fine grained sandstone.||||||
17426|Stretton Sandstone|63112|6|Mentioned|p1191 Fig.2|||Isa Superbasin; southern McArthur Basin. Age approximated from Fig.2.|c.1630-1620 Ma.|Unit in Term Supersequence.||||
17426|Stretton Sandstone|63866|5|Briefly described|p56|Statherian|Statherian|Isa Superbasin.|1625 +/- 2 Ma|Term Supersequence||||
17426|Stretton Sandstone|64815|5|Briefly described|p3, p4 Fig.2, p5 Fig.3 |Statherian|Statherian||1625 +/- 2 Ma (SHRIMP zircon: Page et al, 2000).|Unit in Batten Subgroup.||||
17426|Stretton Sandstone|64816|6|Mentioned|p2 Fig.1|||||Unit in McArthur Group.||||
17426|Stretton Sandstone|64817|6|Mentioned|p353 Fig.4 |Statherian|Statherian||1625 +/- 2 Ma.|Unit in Batten Subgroup.||||
17426|Stretton Sandstone|65228|4|Described|p32,p35-36,Table 1,Figs.02,04,22-23,27|Statherian|Statherian|Basal unit of Term Supersequence, in McArthur River Region. Age from Page et al. (2000). Section and gamma logs detailed. Measured section.|1625 +/- 2 Ma (SHRIMP U-Pb zircon).|Unit in Batten Subgroup.||Overlies Yalco Formation. Is overlain by Looking Glass and Amos Formations.|Sandstone, lesser shale.|
17426|Stretton Sandstone|66843|5|Briefly described|p24, p34-35, p37, p38 Fig.10|||McArthur Basin.|1625 +/- 2 Ma (SHRIMP U-Pb zircon).|McArthur Group.||Is overlain by Looking Glass Formation.|Flaggy sandstone and siltstone with thinly laminated, slightly graded, pink to light brown felsic tuff beds.|
17426|Stretton Sandstone|69018|5|Briefly described|p450 Fig.1b|Statherian|Statherian|Of McArthur Basin.||Of McArthur Group.||||
17426|Stretton Sandstone|69430|4|Described|p15:2-3, 16, 19, 22, 30, 34, 61|Statherian|Statherian|Southern McArthur Basin. <5-270m thick. Shallow-marine to sub-wave base sediments. Fair to good conventional hydrocarbon reservoirs occur.|1625 +/- 2 Ma.|Batten Subgroup.||Conformably overlies Yalco Formation. Is overlain conformably by Looking Glass or Amos Formations. Correlated with Baiguridji (?and Yarrawirrie) Formations.|Green to grey-brown, fine- to medium-grained, thinly bedded quartzarenite; minor micaceous siltstone. Distinctive wavy bedding, small ripples, tool marks, mudclast casts, dessication cracks and convolute bedding.|12-JUL-16
17426|Stretton Sandstone|69673|6|Mentioned|p16 fig 13, p32, p34, p35, p40|||Batten Fault Zone. Reservoir rock with locally good primary intergranular porosity. Up to 270m thick.|1625 +/- 2 Ma|Batten Subgroup||Conformably overlies Yalco Formation, conformably overlain by Looking Glass Formation, Amos Formation|Flaggy, very fine to medium grained quartz sandstone and minor micaceous siltstone; local conglomerate-breccia.|
17426|Stretton Sandstone|71374|5|Briefly described|p9, p18|||McArthur Basin. Age is from GA 91779043, Geochron Delivery and derived from an interbedded tuff in this formation.|1625 +/- 2 Ma (SHRIMP U-Pb)|||Conformably overlies the Yalco Formation. Unconformably overlain by the Smythe Sandstone.||
17426|Stretton Sandstone|71592|5|Briefly described|Appendix A.|||McArthur Basin.|1625+/-2 Ma (crystallisation: U-Pb zircon SHRIMP)||||Ash tuff.|
17426|Stretton Sandstone|72248|5|Briefly described|p147|||Of McArthur Basin.||Unit of Batten Subgroup.||||
17426|Stretton Sandstone|72373|4|Described|iii,p1,14-17,20,24,27|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. Type section is in MALLAPUNYAH mapsheet. Well-exposed in BAUHINIA DOWNS, southern MOUNT YOUNG and on Maria Island in southern ROPER RIVER. Contains 1625+\-2 Ma tuff near base of the unit (Page et al., 2000). Sample 2709629 (BD16TJM065: Fine-grained quartz sandstone; BAUHINIA DOWNS) yielded interpreted max depositional age of 1634+\-18 Ma. Shows similar detrital zircon age spectra to Nagi Formation (Vizard Group), supporting previous interpretations that these formations (with Yalco Formation) are broadly equivalent, and potentially sources from the same or similar terranes.|1634+\-18 Ma (max dep age)|Unit of Batten Subgroup.||Overlain conformably by Looking Glass Formation. Underlain conformably by Yalco Formation. May be equivalent to Baiguridji Formation or underlying Yarrawirrie Formation,  and Ulunourwi Formation..|Very fine- to medium-grained quartz sandstone and minor micaceous siltstone.|01-OCT-19
17426|Stretton Sandstone|72523|5|Briefly described|piii, 1, p2 Fig.2, p8.|Statherian|Statherian|Has detrital zircon spectrum with similarities to that determined for the 'lower evaporitic unit ' sample from near the base of the Balbirini Dolostone, sugesting some common sediment source areas/sediment transport pathways.||Batten Subgroup, McArthur Group.||Underlies Looking Glass Formation and the Balbirini Dolostone.|Includes sandstone.|29-OCT-20
17426|Stretton Sandstone|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Batten Fault Zone of the Southern McArthur Basin. Age given as U-Pb zircon sedimentary depositional age.|1625 +/-2 Ma|Batten Subgroup||Overlies Yalco Formation and underlies Looking Glass Formation.||
17426|Stretton Sandstone|72718|6|Mentioned|p7|||Southern McArthur Basin. Batten Fault Zone. Partly equivalent to Catfish Conglomerate[?].||Batten Sub-group, McArthur Group||Partly underlain by Yalco Formation. Overlain by Looking Glass and Amos formations and lower Balbirini Dolostone. Unconformably overlain[?] by Smythe Sandstone.||
17426|Stretton Sandstone|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Batten Fault Zone of the Southern McArthur Basin. U-Pb zircon sedimentary depositional age (Ma).|1625 +/- 2 Ma|Batten Subgroup||Overlies Yalco Formation and underlies Looking Glass Formation.||
17426|Stretton Sandstone|73042|6|Mentioned|p4||Statherian|Southern McArthur Basin, Isa Superbasin. Geochronology is a U-Pb zircon sedimentary depositional age (?maximum depositional age).|1625 +/- 2 Ma (see Fig.1.2)|Batten Subgroup, McArthur Group||Underlain by Yalco Formation. Partly overlain by Looking Glass Formation and unconformably by(?) Smythe Sandstone.||
17426|Stretton Sandstone|73412|5|Briefly described|p4, 8|||Southern McArthur Basin.||Batten Subgroup.||Overlies Yalco Formation. Is overlain by Looking Glass and Amos Formations and lower Balbirini Dolostone.||
17454|Stubb Formation|14019|5|Briefly described|p4 Fig. 3|||Of the Tijunna Group.  Geological Province: Victoria Basin.||||||
17454|Stubb Formation|22547|6|Mentioned|Fig4,p25|||Geological province:  Victoria River Basin. Overlies Wondoan Hill Formation.||||||05-DEC-06
17454|Stubb Formation|23937|5|Briefly described|p76 App. 1|||Of the Auvergne Group?||||||03-NOV-04
17454|Stubb Formation|24122|3|Fully described|p8, p5 Tb.1|Proterozoic|Proterozoic|Of Tijunna Group. Conformably overlies Wondoan Hill Formation. Originally included in the Auvergne Group.  Max. thickness: 210m.  Geological Province: Victoria Basin.||||||
17454|Stubb Formation|24297|3|Fully described|p15|Mesoproterozoic|Mesoproterozoic|Of Tijunna Group. Conformably overlies Wondoan Hill Formation. Was included in Auvergne Group on the 1st edition of VICTORIA RIVER DOWNS 1:250k. Maximum thickness: 115m.  Geol. Prov:  Victoria Basin.  See also p5 Tb. 2.||||||05-DEC-06
17454|Stubb Formation|24298|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Tijunna Group. Siltstone, shale, minor sandstone.||||||05-DEC-06
17454|Stubb Formation|24300|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Tijunna Group.   Geological Province: Victoria Basin||||||14-MAR-18
17454|Stubb Formation|24441|5|Briefly described|p1 Fig. 1, Appendix 2-1:2|Mesoproterozoic|Mesoproterozoic|Of the Tijunna Group. Overlies Wondoan Hill Formation; unconformably overlain by Jasper Gorge Sandstone. Claystone and siltstone. Thickness: >67m.Geological Province: Victoria Basin.||||||25-JAN-06
17454|Stubb Formation|24442|5|Briefly described|p50 Fig. 1|||Of the Tijunna Group.   Geological Province: Victoria Basin.||||||
17454|Stubb Formation|28255|3|Fully described|p62, Tb. 11 (opp. p8)|Adelaidean|Adelaidean|Basal unit of Auvergne Gp. Deep water deposit - fissile, laminated, dark-grey to red-brown, micaceous shale and coarse sltst becoming coarser upwards. Unconformable over Wondoan Hill Fm; conformable below Jasper Gorge Sst. Max. thick: 115m. See also p68 .||||||
17454|Stubb Formation|32170|6|Mentioned|Map legend|Adelaidean|Carpentarian|Adelaidean or Carpentarian||||||
17454|Stubb Formation|32175|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Auvergne Group.  Interbedded dark grey shale and siltstone; massive quartz sandstone interbeds near top.||||||02-DEC-04
17454|Stubb Formation|32659|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
17454|Stubb Formation|32660|5|Briefly described|Table 6|||||||||
17454|Stubb Formation|32700|4|Described|Table 1|||Auvergne Group. See p14.||||||05-DEC-06
17454|Stubb Formation|32701|6|Mentioned|p9|||||||||
17454|Stubb Formation|32728|6|Mentioned|p16|||||||||
17454|Stubb Formation|32775|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Auvergne Group.||||||02-DEC-04
17454|Stubb Formation|33373|3|Fully described|p9|||On Table 2.||||||
17454|Stubb Formation|33374|6|Mentioned|p8|||Strat. table. See also p12.||||||05-DEC-06
17454|Stubb Formation|33375|6|Mentioned|p11 Tb. 1, p12|Adelaidean|Adelaidean|Fine sandstone and silty sandstone; manganese and iron staining in joints. Max. thickness: ~15m.||||||26-APR-05
17454|Stubb Formation|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
17454|Stubb Formation|33378|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Auvergne Group. Fine and silty sandstone.||||||27-APR-05
17454|Stubb Formation|37462|4|Described|Table 4.VI|||||||||
17454|Stubb Formation|45112|3|Fully described|p29|||See p29-30.||||||05-DEC-06
17454|Stubb Formation|45140|6|Mentioned|p13|||Victoria River region.||||||
17454|Stubb Formation|48942|2|Defined|p59|Adelaidean|Adelaidean|||||||
17454|Stubb Formation|48943|3|Fully described|p72|||||||||
17454|Stubb Formation|60685|3|Fully described|p4 Fig. 3, p1|Mesoproterozoic|Mesoproterozoic|Formerly of the Auvergne Group now in Tijunna Group. Interbedded claystone, siltstone, mudstone, sandstone. Conformable on Wondoan Hill Formation; unconforably overlain by Jasper Gorge Sandstone. Max. Thickness: 210m. Geological Province: Victoria Basin.||||||05-DEC-06
17454|Stubb Formation|65342|6|Mentioned|p11 Fig.13. |||Victoria Basin.||Unit in Tijunna Group.||Overlies Wondoan Hill Formation. Is unconformably overlain by Jasper Gorge Sandstone of Auvergne Group.||
17454|Stubb Formation|67151|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Birindudu Basin.||Unit in Tijunna Group.||Overlies Wondoan Hill Formation.|Fine silty sandstone, siltstone.|
17454|Stubb Formation|68733|5|Briefly described|p177 Fig.2, p179-186, p191-192|Cryogenian|Statherian|Sweet et al. (1974). Previously included in the Victoria Basin by Cutovinos et al. (2002). Now included in the Birrindudu Basin due to a recent subdivision by the NGTS (Dunster and Ahmad 2013). Maximum depositional age of ca. 1618 +/- 13 Ma. Sm-Nd isotope data tabulated.|Maximum depositional age of ca. 1618 +/- 13 Ma.|Uppermost unit of the Tijunna Group.||Conformably underlain by the Wondoan Hill Formation. Unconformably overlain by the Jasper Gorge Sandstone.|Dominated by laminated, micaeous shale and silstone, with intercalated quartz sandstone.|06-DEC-17
17454|Stubb Formation|69432|4|Described|p17:2, 12, 15|||Birrindudu Basin. Up to 210m thick. Thick shale may have some potential as petroleum source rock.||Tijunna Group.||Unconformably overlies Banyan Formation.|Lower part is grey shale and red-brown micaceous siltstone; a succession of interbedded micaceous claystone, siltstone, minor mudstone and sandstone.|12-JUL-16
17454|Stubb Formation|69673|6|Mentioned|p48 fig 35|||||Tijunna Group||Overlies Wondoan Hill Formation, unconformably overlain by Auvergne Group||
17454|Stubb Formation|70655|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Birindudu Basin.||Tijunna Group.||Shown as overlying Wondoan Hill Formation in map key.|Fine silty sandstone, siltstone.|
17454|Stubb Formation|70850|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Tijunna Group.||Conformably overlies Wondoan Formation. Is overlain unconformably by Jasper Gorge Sandstone (Auvergne Group).|Siltstone, shale, minor sandstone.|
17454|Stubb Formation|70855|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Tijunna Group.||Overlies Wondoan Hill Formation. Is overlain unconformably by Antrim Plateau Volcanics.|Siltstone, shale, minor sandstone.|
17454|Stubb Formation|70968|2|Defined|vi, p115-117, p120-122, p124, p126-127|Mesoproterozoic|Mesoproterozoic|See also p129, p131-132. Sweet et al. (1974). Originally included in the former Victoria River Group by Traves (1955), and in the former Coolibah Formation by Laing and Allen (1956). Placed in the Auvergne Group by Morgan et al. (1970) and Sweet (1972, 1973), but then excluded by Sweet et al. (1974). Included in Tijunna Group by Beier et al. (2002). Named after Stubb yard, 5km ESE of Victoria Road bridge. The type section is at 52 723532mE 8276218mN (Base) to 52 752241mE 8285144mN in DELAMARE. Variable exposures; crops out extensively from Delamere homestead to the Victoria River. Contains detrital zircons aged c.3100 Ma, derived from the Pilbara or a non-Australian source. Lithology well described and illustrated. Up to 210m thick; 190m in the type section. Represents a regressive sedimentary cycle. Various age determination attempts described. Detrital zircon diagram and discussion.|c.1618 Ma (maximum depositional age).|Tijunna Group.||Overlies Wondoan Hill Formation conformably or Bynoe Formation (Bullita Group) unconformably. Is overlain unconformably by Jasper Gorge Sandstone (Auvergne Group).|A lower interval has homogeneous green, fissile, laminated micaceous claystone and coarse-grained quartz siltstone that grades upward into white and brown medium-grained quartz sandstone. Local minor thin beds of hematitic sandstone breccia.|24-FEB-17
17454|Stubb Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||shale, siltstone|
17454|Stubb Formation|71302|5|Briefly described|p6,72-74||Paleoproterozoic|Of Birindudu Basin. Maximum depositional age: 1618+\-13 Ma (Carson, 2013; Munson, 2016 and Munson, in prep). Contain small c > 1560-1640 Ma age populations. Also contains small clusters of c. 3100 Ma zircons, interpreted to have been recycled from Pine Creek Orogen sequences (e.g. Crater Formation, Mount Partridge Group; Hollis et al., 2010).||Unit of Tijunna Group.||Overlain by Jasper Gorge Formation. Underlain by Wondoan Hill Formation.||
17454|Stubb Formation|71592|5|Briefly described|Appendix A.|||Victoria River Region.|1618+/-13 Ma (MDA: Pb/Pb zircon).||||Sandstone.|
17454|Stubb Formation|71893|4|Described|p7-p8, p68-p69|||Birrindudu Basin. A maximum depositional age of 1618 +/- 13 Ma was interpreted for this unit in addition to two younger analyses at ca 1485 Ma and 1307 Ma.||Tijunna Group||Conformably overlies the Wondoan Hill Formation.||
17454|Stubb Formation|72718|6|Mentioned|p7|||Birrindudu Basin.||Tijunna Group||Underlain by Wondoan Hill Formation.||
17454|Stubb Formation|73083|6|Mentioned|p18|||||||||
17519|Sun Hill Arkose|10116|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Arkose, feldspathic sandstone, micaceous sandstone, siltstone, arkosic conglomerates.||||||
17519|Sun Hill Arkose|22954|6|Mentioned|Fig3p9|||||||||
17519|Sun Hill Arkose|30914|6|Mentioned|Map legend|Early Cambrian|Proterozoic|Proterozoic - Early Cambrian||||||
17519|Sun Hill Arkose|31287|5|Briefly described|p430|||Refers to status||||||
17519|Sun Hill Arkose|33111|4|Described|p43|||Mention p18.||||||05-DEC-06
17519|Sun Hill Arkose|34454|6|Mentioned|p10|||L.Cambrian||||||
17519|Sun Hill Arkose|34847|6|Mentioned|p31|||||||||
17519|Sun Hill Arkose|35121|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
17519|Sun Hill Arkose|35139|4|Described|Table.2|||||||||
17519|Sun Hill Arkose|36234|3|Fully described|p166|||||||||
17519|Sun Hill Arkose|36243|6|Mentioned|Table 1A|||||||||
17519|Sun Hill Arkose|37572|6|Mentioned|p155|||See also Fig.8||||||
17519|Sun Hill Arkose|39445|5|Briefly described|Table 4|||See also p62 and Fig.5.||||||05-DEC-06
17519|Sun Hill Arkose|39921|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
17519|Sun Hill Arkose|42060|6|Mentioned|Fig.5 P140|||||||||
17519|Sun Hill Arkose|42956|5|Briefly described|p27|||||||||
17519|Sun Hill Arkose|44121|14|Not recorded|p5|Early Cambrian|Neoproterozoic|||||||
17519|Sun Hill Arkose|44211|14|Not recorded|p95,97,102,104|||||||||
17519|Sun Hill Arkose|44291|14|Not recorded|p8|||||||||
17519|Sun Hill Arkose|44308|14|Not recorded|p3,5,13,Tb.1||Cambrian|Equivalent to Mount Birnie Beds.||||||
17519|Sun Hill Arkose|44310|14|Not recorded|Map Legend||Early Cambrian|||||||
17519|Sun Hill Arkose|44312|14|Not recorded|Map Legend||Early Cambrian|||||||
17519|Sun Hill Arkose|44543|2|Defined|p31,36||Early Cambrian|Equivalent to Mount Birnie Beds.||||||
17519|Sun Hill Arkose|44920|14|Not recorded|Map Legend, Sheet 4||Adelaidean|||||||
17519|Sun Hill Arkose|44989|14|Not recorded|p.122|||||||||
17519|Sun Hill Arkose|45002|14|Not recorded|p16|||Early Late Cambrian fossils present.||||||05-DEC-06
17519|Sun Hill Arkose|45012|14|Not recorded|p29||Early Cambrian|||||||
17519|Sun Hill Arkose|45052|3|Fully described|p75|||Adelaidean ?||||||
17519|Sun Hill Arkose|45102|6|Mentioned|p43|||||||||
17519|Sun Hill Arkose|48906|14|Not recorded|Tb.1|||||||||
17519|Sun Hill Arkose|49027|5|Briefly described|p3|||||||||
17519|Sun Hill Arkose|60122|6|Mentioned|p9|||||||||
17519|Sun Hill Arkose|63450|5|Briefly described|p78 Fig. 5, p80|Neoproterozoic|Neoproterozoic|Geological province: Georgina Basin, East Toko Syncline.||||||07-FEB-11
17519|Sun Hill Arkose|64068|3|Fully described|p45-46, p54, p viii|Cryogenian||Basal glacial outwash. Is overlain by Sylvester Sandstone. Correlated with Black Stump Arkose on lithologic similarity. Also correlated with Wonnadinna Dolostone, Oorabra Arkose, Boko, Olympic Formations, Pioneer Sandstone, Mount Doreen Formation.||Of Keepera Group.||Is overlain by Sylvester Sandstone.|Arkose, arkosic sandstone, green shale, micaceous greywacke, siltstone, dolomitic siltstone, pebble conglomerate and arkosic dolostone. Basal glacial outwash.|04-APR-12
17519|Sun Hill Arkose|65338|6|Mentioned|p60.|||||Unit in Keepera Group.||||
17519|Sun Hill Arkose|65489|5|Briefly described|p125|Cambrian|Proterozoic|Georgina Basin.||||Overlies Field River Beds. Is overlain by Mount Binnie Beds and Sylvester Sandstone.||
17519|Sun Hill Arkose|67323|5|Briefly described|GIS attrib tbl, p92 Fig.12.2|Early Cambrian|Neoproterozoic|See also Solid Geology Map. Centralian Superbasin||||is overlain by Marqua Formation.|Conglomerate, arenite, arkose, shale, mudstone, dolomite|
17519|Sun Hill Arkose|67402|6|Mentioned|p215 fig GRG8/GRG9|||||||||
17519|Sun Hill Arkose|67870|6|Mentioned|p43|Neoproterozoic|Neoproterozoic|Georgina Basin.||||||
17519|Sun Hill Arkose|68270|4|Described|p681-683,686,688|Cryogenian|Cryogenian|Southern Georgina Basin.Type section occurs at Sun Hill and low hills to N, 19km SE of Glenormiston Homestead; lat 23'1.9'S, long. 138'52"E. Less than 300m thick. Glacial outwash deposit related to Elatina glaciation. Correlative to Elatina Formation. Laterally equivalent to Oorabra Arkose and Black Stump Arkose.||||Overlain unconformably by Sylvester Sandstone.|Arkose, arkosic sandstone, shale, siltstone, dolomitic siltstone, conglomerate and arkosic dolomite.|03-JUL-19
17519|Sun Hill Arkose|68553|6|Mentioned|Map legend; schematic diagram.|Early Paleozoic|Neoproterozoic|Georgina Basin. This unit, as well as Black Stump and Gnallan-a-gea Arkoses, Yardida and Little Burke Tillites, are all mapped under the symbol, -P-Cg.||||||
17519|Sun Hill Arkose|69437|5|Briefly described|p22:7|||Southern Georgina Basin. Centralian A Superbasin. Supersequence 3.||Keepera Group.|||Glacial outwash deposits.|12-JUL-16
17519|Sun Hill Arkose|69443|5|Briefly described|p28:7-8|Cryogenian|Cryogenian|Georgina Basin.||Keepera Group.||||12-JUL-16
17519|Sun Hill Arkose|69591|5|Briefly described|p94|||E of Toko Syncline in the Sylvester Creek drainage. Has a complicated history of interpretation (detailed) by various workers.||||Is overlain by Sylvester Sandstone.|Arkosic sandstone, conglomerate, siltstone and dolomite.|
17519|Sun Hill Arkose|72516|6|Mentioned|p87|Ediacaran|Ediacaran|Georgina Basin.||||Equivalent to the Oorabra Arkose.||02-JUN-21
17542|Supplejack Downs Sandstone|22446|5|Briefly described|p19|Statherian|Statherian|||||||
17542|Supplejack Downs Sandstone|29809|6|Mentioned|Table 1|||||||||
17542|Supplejack Downs Sandstone|29811|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17542|Supplejack Downs Sandstone|29813|6|Mentioned|Table 2|||||||||
17542|Supplejack Downs Sandstone|31361|4|Described|Table 1|||||||||
17542|Supplejack Downs Sandstone|31362|6|Mentioned|Table 1|||||||||
17542|Supplejack Downs Sandstone|36473|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17542|Supplejack Downs Sandstone|36532|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17542|Supplejack Downs Sandstone|39887|6|Mentioned|p452|||||||||
17542|Supplejack Downs Sandstone|41883|5|Briefly described|p65|||||||||
17542|Supplejack Downs Sandstone|42643|6|Mentioned|p5|||||||||
17542|Supplejack Downs Sandstone|45140|2|Defined|p12-15, p18, p20-22, p39, p41, p73|Paleoproterozoic|Paleoproterozoic|See also Appx.p7. Blake et al. (1975). Named after Supplejack Downs homestead. The Granites-Tanami Block. The type section is across the S end of a strike ridge 11km E of the homestead, at 19deg 16'50"S, 130deg 02'45"E. At least 1300m thick. Forms a group of sandstone ridges up to 30m high E of the Supplejack Range.|c.1800 Ma.|||Overlies Nanny Goat Creek Beds (Tanami Complex) unconformably and Mount Winnecke Formation ?conformably. Is overlain unconformably by Birrindudu Group and Antrim Plateau Volcanics.|Mainly sublithic arenite and quartz arenite, medium to thin-bedded, commonly close-jointed and cross-bedded, some with layers of shale pellets and rare conglomerate lenses; local shale and siltstone.|
17542|Supplejack Downs Sandstone|45167|5|Briefly described|Fig.27|||||||||
17542|Supplejack Downs Sandstone|46864|6|Mentioned|p37|||||||||
17542|Supplejack Downs Sandstone|48950|2|Defined|p28|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17542|Supplejack Downs Sandstone|50315|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Birrindudu Group. Sandstone - white to pale pink, sublithic arenite, quartz arenite, conglomerate, siltstone and shale, minor volcanogenic sandstone; fine- to coarse-grained, variably sorted.||||||07-NOV-08
17542|Supplejack Downs Sandstone|50374|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Birrindudu Group||||||07-NOV-08
17542|Supplejack Downs Sandstone|50376|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Birrindudu Group. Sandstone - white to pale pink, sublithic arenite, quartz arenite, conglomerate, siltstone, shale, minor volcanogenic sandstone; fine- to coarse-grained, variably sorted.||||||07-NOV-08
17542|Supplejack Downs Sandstone|60676|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Birrindudu Group. Sandstone: white to pale pink, sublithic arenite, quartz arenite, conglomerate, siltstone and shale, minor volcanogenic sandstone; fine to coarse grained, variably sorted.||||||07-NOV-08
17542|Supplejack Downs Sandstone|61861|4|Described|p24, 23, p3 Table 1, p20|Statherian|Statherian|Now included in the Birrindudu Group on basis of lithological and structural similarities with other constituents, particularly Gardiner Sandstone. This study suggests further mapping may rename it as Gardiner or Coomarie Sandstone. Previous possible conformable contact over Mount Winnecke Formation now discounted.||Unit in Birrindudu Group.||Now known to unconformably overlie (or is faulted against) Nanny Goat Volcanics.|Thick-bedded, medium- to coarse-grained quartz arenite and sublithic arenite; contains small clasts of feldspar-quartz ignimbrite just above the base.|03-APR-12
17542|Supplejack Downs Sandstone|63261|5|Briefly described|p12|||Previously assigned to Ware Group, now assigned to Birrindudu Group based on lithological and structural similiarities with Gardiner Sandstone (Birrindudu Group).||||||07-FEB-11
17542|Supplejack Downs Sandstone|64675|6|Mentioned|p9|||See also Supplejack Sandstone.||||Unconformably underlain by the Tanami Complex.||
17542|Supplejack Downs Sandstone|65074|6|Mentioned|p349, p351 fig 4-37|Proterozoic|Proterozoic|Of North/Centre Birrindudu Basin. Early Proterozoic. 1300 m thick.||||Unconformably overlain by Gardiner Sandstone.|Sublithic arenite with minor amounts of shale and siltstone.|
17542|Supplejack Downs Sandstone|65323|5|Briefly described|Map legend|Statherian|Statherian|Of the Birrindudu Group; non-magnetic sandstone;  shown as lateral equivalent of Coomarie Sandstone, Talbot Well Formation, Gardiner Sandstone and interfingering with Gardiner Sandstone||||||10-DEC-12
17542|Supplejack Downs Sandstone|65324|6|Mentioned|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||
17542|Supplejack Downs Sandstone|65326|5|Briefly described|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||12-APR-10
17542|Supplejack Downs Sandstone|65327|5|Briefly described|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||12-APR-10
17542|Supplejack Downs Sandstone|65328|5|Briefly described|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||12-APR-10
17542|Supplejack Downs Sandstone|65338|6|Mentioned|p21.|||Tanami Region. Previously, correlated with Reynolds Range Group (Blake et al. 1979).||||||
17542|Supplejack Downs Sandstone|65349|6|Mentioned|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||
17542|Supplejack Downs Sandstone|65350|6|Mentioned|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||
17542|Supplejack Downs Sandstone|65351|6|Mentioned|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||
17542|Supplejack Downs Sandstone|65352|5|Briefly described|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||12-APR-10
17542|Supplejack Downs Sandstone|65353|5|Briefly described|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||12-APR-10
17542|Supplejack Downs Sandstone|65354|5|Briefly described|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group. Shown as lateral equivalent of Coomarie Sandstone, Talbot Well Formation, Gardiner Sandstone and interfingering with Gardiner Sandstone||||||12-DEC-12
17542|Supplejack Downs Sandstone|65355|5|Briefly described|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||12-APR-10
17542|Supplejack Downs Sandstone|65356|5|Briefly described|Map legend|Statherian|Statherian|Of the Birrindudu Group; non-magnetic sandstone; shown as lateral equivalent of Coomarie Sandstone, Talbot Well Formation, Gardiner Sandstone and interfingering with Gardiner Sandstone||||||12-DEC-12
17542|Supplejack Downs Sandstone|67168|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Lateral equivalent to Gardiner and Coomarie Sandstones and Talbot Well Formation.||Unit in Birrindudu Group.||Unconformably overlies Tanami and Mount Winnecke Groups.||
17542|Supplejack Downs Sandstone|69426|6|Mentioned|p11:5 Fig.11.4|||In Blake et al. (1979).||Birrindudu Group.||||12-JUL-16
17542|Supplejack Downs Sandstone|69432|6|Mentioned|p17:4|||Blake et al. (1975). Subsequently included in the Gardiner Sandstone.||||||12-JUL-16
17542|Supplejack Downs Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, arenite|
17542|Supplejack Downs Sandstone|73083|6|Mentioned|p24|||Intruded by granite of the Tanami Orogen.||||||
17551|Surprise Creek Formation|22438|4|Described|p537, Fig.3 p537|||||||||
17551|Surprise Creek Formation|22457|6|Mentioned|Fig29 P30|||||||||
17551|Surprise Creek Formation|22498|6|Mentioned|Fig2 P235, Fig5|||||||||
17551|Surprise Creek Formation|22585|6|Mentioned|Fig1 P736, Fig3|||Actually spelt Surprise Creek Fm.||||||
17551|Surprise Creek Formation|22680|6|Mentioned|83,85|||||||||
17551|Surprise Creek Formation|23073|5|Briefly described|p744 (fig 2), p748|||||||||
17551|Surprise Creek Formation|23393|4|Described|p19, p16 Fig. 4|Paleoproterozoic|Paleoproterozoic|Geological Province: Lawn Hill Sub-province. See also p17 Fig. 5.||||||24-FEB-10
17551|Surprise Creek Formation|23395|6|Mentioned|p383|||||||||
17551|Surprise Creek Formation|23396|5|Briefly described|p407 Fig.2|||||||||
17551|Surprise Creek Formation|23397|5|Briefly described|p467 Fig.2|||||||||
17551|Surprise Creek Formation|23399|4|Described|p490|||||||||
17551|Surprise Creek Formation|23406|5|Briefly described|p603|||Geological province: Lawn Hill Platform.||||||16-JUN-09
17551|Surprise Creek Formation|23408|4|Described|p511, p513 Fig. 2, p514|||Not included by Hutton et al (1981) in their McNamara Group.||||||15-JUN-09
17551|Surprise Creek Formation|23466|5|Briefly described|p267|||||||||
17551|Surprise Creek Formation|23767|5|Briefly described|p1954 Fig. 1a|||Geological Province: Mount Isa Superbasin. See also p1956 Fig.2 and p1957 Fig.3.||||||
17551|Surprise Creek Formation|23965|5|Briefly described|p1297|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier.||||||07-NOV-08
17551|Surprise Creek Formation|24048|5|Briefly described|p38|||Geological Province: Mt. Isa Inlier.||||||
17551|Surprise Creek Formation|24308|5|Briefly described|p992, p987 Fig. 2|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17551|Surprise Creek Formation|24419|5|Briefly described|p16, p17, p13 Fig.5, p15 Fig.6|Paleoproterozoic|Paleoproterozoic|Correlates with Torpedo Creek Formation. Part of the Prize Supersequence. Western Fold Belt, Leichhardt River Subprovince; Lawn Hill Subprovince (Mount Isa Orogen).||||||07-NOV-08
17551|Surprise Creek Formation|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Overlain by Torpedo Creek Quartzite and Cromwell metabasalt.||||||
17551|Surprise Creek Formation|35286|6|Mentioned|Fig.17|||||||||
17551|Surprise Creek Formation|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17551|Surprise Creek Formation|36548|6|Mentioned|Fig.3|||||||||
17551|Surprise Creek Formation|37459|6|Mentioned|p426|||||||||
17551|Surprise Creek Formation|37462|4|Described|Table4.VII|||||||||
17551|Surprise Creek Formation|37568|5|Briefly described|p84|||||||||
17551|Surprise Creek Formation|37816|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17551|Surprise Creek Formation|37862|6|Mentioned|p583|||||||||
17551|Surprise Creek Formation|38232|6|Mentioned|p82|||||||||
17551|Surprise Creek Formation|38234|6|Mentioned|Fig.2|||||||||
17551|Surprise Creek Formation|38235|6|Mentioned|p115|||||||||
17551|Surprise Creek Formation|38237|4|Described|p126|||||||||
17551|Surprise Creek Formation|38276|6|Mentioned|Fig.1|||||||||
17551|Surprise Creek Formation|38348|6|Mentioned|p7|||||||||
17551|Surprise Creek Formation|38350|4|Described|p14|||||||||
17551|Surprise Creek Formation|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17551|Surprise Creek Formation|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
17551|Surprise Creek Formation|38833|6|Mentioned|p161|||||||||
17551|Surprise Creek Formation|38835|6|Mentioned|p164|||||||||
17551|Surprise Creek Formation|38836|6|Mentioned|p165|||||||||
17551|Surprise Creek Formation|38900|6|Mentioned|p55|||||||||
17551|Surprise Creek Formation|38919|6|Mentioned|p494|||||||||
17551|Surprise Creek Formation|39202|6|Mentioned|Fig.3|||||||||
17551|Surprise Creek Formation|39362|6|Mentioned|p1468|||||||||
17551|Surprise Creek Formation|39445|5|Briefly described|Table 2|||See also p36 and p41.||||||05-DEC-06
17551|Surprise Creek Formation|39556|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||
17551|Surprise Creek Formation|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Underlies the Torpedo Creek Quartzite.||||||15-JUN-06
17551|Surprise Creek Formation|39622|6|Mentioned|Fig.2|||||||||
17551|Surprise Creek Formation|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17551|Surprise Creek Formation|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
17551|Surprise Creek Formation|39925|6|Mentioned|p335|||See also p329.||||||05-DEC-06
17551|Surprise Creek Formation|39944|6|Mentioned|Fig.5|||||||||
17551|Surprise Creek Formation|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17551|Surprise Creek Formation|40221|3|Fully described|p12|||||||||
17551|Surprise Creek Formation|40623|5|Briefly described|p98|||||||||
17551|Surprise Creek Formation|40840|6|Mentioned|Map legend|||||||||
17551|Surprise Creek Formation|41248|6|Mentioned|Fig.2|||||||||
17551|Surprise Creek Formation|41277|6|Mentioned|Fig.5|||||||||
17551|Surprise Creek Formation|41298|6|Mentioned|Map legend|Carpentarian||||||||
17551|Surprise Creek Formation|41307|4|Described|p14|||||||||
17551|Surprise Creek Formation|41791|6|Mentioned|p272|||||||||
17551|Surprise Creek Formation|41978|6|Mentioned|p494|||||||||
17551|Surprise Creek Formation|41979|6|Mentioned|Fig.2 P512|||||||||
17551|Surprise Creek Formation|42234|6|Mentioned|Fig.2 P1055|||||||||
17551|Surprise Creek Formation|42503|5|Briefly described|Fig.1 P334|||||||||
17551|Surprise Creek Formation|42565|5|Briefly described|Table 1 P5, P4|||||||||
17551|Surprise Creek Formation|42706|5|Briefly described|map legend|Proterozoic|Proterozoic|Sandstone, siltstone, shale.||||||09-FEB-09
17551|Surprise Creek Formation|42818|5|Briefly described|Fig.2 P205|||||||||
17551|Surprise Creek Formation|43235|6|Mentioned|p9|||Proterozoic.||||||
17551|Surprise Creek Formation|43608|6|Mentioned|Fig.11,p11|||||||||
17551|Surprise Creek Formation|43616|6|Mentioned|p3|||||||||
17551|Surprise Creek Formation|45161|5|Briefly described|p27|||||||||
17551|Surprise Creek Formation|45166|5|Briefly described|p14|||||||||
17551|Surprise Creek Formation|46960|2|Defined|p222|Proterozoic|Proterozoic|||||||
17551|Surprise Creek Formation|46962|4|Described|Table 1|||See also Fig.3.||||||
17551|Surprise Creek Formation|47083|3|Fully described|p12-13||Proterozoic|Previously mapped as 'Surprise Creek Beds' and 'Ploughed Mountain Beds'. Informally divided into 4 units. Overlain by McNamara and Mt Isa Groups. Underlain by Bigie Formation, Fiery Creek Volcanics, Quilalar Formation and Myally Subgroup.||||||05-DEC-06
17551|Surprise Creek Formation|49041|5|Briefly described|Table 1|||||||||
17551|Surprise Creek Formation|50100|5|Briefly described|p11, p13 Fig. 4, p19|Statherian|Statherian|Disconformably, unconformably and nonconformably overlies Leichhardt Volcanics and Kalkadoon Granodiorite.  Geological Province: Kalkadoon-Ewen Province / Western Fold Belt Province.||||||
17551|Surprise Creek Formation|50332|4|Described|p16, p20|Paleoproterozoic|Paleoproterozoic|Disconformably, unconformably and nonconformably overlies the Bigie Formation, Leichhardt Volcanics + Kalkadoon Granodiorite. Age: ~1700-1640Ma.Geol Prov: Western Fold Belt Province. Sedimentary rocks and subordinate bimodal volcanics.||||||07-FEB-11
17551|Surprise Creek Formation|50550|5|Briefly described|p1139 Fig.2, p1141 Fig.4||Statherian|Overlies Fiery Creek Volcanics at a syn-rift unconformity. Conformably overlain by Torpedo Creek Quartzite. Geological Province: Western Fold Belt.||||||19-DEC-07
17551|Surprise Creek Formation|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Arenite; minor conglomerate, shale, siltstone.||||||
17551|Surprise Creek Formation|60558|5|Briefly described|p4 Fig. 3|Paleoproterozoic|Paleoproterozoic|Geological Province: Western Fold Belt.||||||03-JUN-09
17551|Surprise Creek Formation|61204|5|Briefly described|p538|||Geological Province: Mount Isa Inlier. Underlain by Eastern Creek Volcanics; unconformably overlies Haslingden Group. Siltstones; sandstones; conglomerates.||||||31-MAY-07
17551|Surprise Creek Formation|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: <1700Ma. Geological Province: western Mount Isa Block.||||||07-NOV-08
17551|Surprise Creek Formation|61736|5|Briefly described|p672 Fig. 7, p673|Paleoproterozoic|Paleoproterozoic|Ages: 1688+/-6Ma, 1687+/-5Ma and 1688+/-5Ma (SHRIMP, Jackson et al 2005) from tuffs or shallow level, peperitic units.||||||
17551|Surprise Creek Formation|61929|5|Briefly described|p128 Fig. 2|||||||||
17551|Surprise Creek Formation|61936|5|Briefly described|p194 Fig. 6|||Dominantly siliciclastic succession.||||||
17551|Surprise Creek Formation|62084|5|Briefly described|p936 Fig.5|||Calvert Superbasin. Shown as Surprise Ck Fm.|1694+/-3 Ma U-Pb SHRIMP (after Page et al. 2000)|||||
17551|Surprise Creek Formation|62535|5|Briefly described|p672-673|Statherian|Statherian|Several other (similar) ages are given.|1688 +/- 6 Ma.|||Unconformably overlies Bigie Formation.||
17551|Surprise Creek Formation|62659|5|Briefly described|Map Legend|Statherian|Statherian|Basal pebble to boulder conglomerate with clasts of quartz, quartzite and rhyolite in matrix of pink medium to coarse grained sublithic sandstone.||||||06-MAY-13
17551|Surprise Creek Formation|63023|5|Briefly described|p1024 Fig. 1, p1025 Fig. 2|Paleoproterozoic|Paleoproterozoic|Age: ~1709+/-3Ma. Geological Province: Calvert Superbasin.||||||07-NOV-08
17551|Surprise Creek Formation|63109|6|Mentioned|p1112, p1108 Fig. 3|||Geological Province: Calvert Superbasin. Consists of sandstone.||||||01-SEP-08
17551|Surprise Creek Formation|63111|5|Briefly described|p1162, p1163 Fig. 3, p1164 Tb. 1|Statherian|Statherian|Overlain by Torpedo Creek Quartzite, underlain by Fiery Creek Volcanics. Age: 1690+/-7Ma. Geological Province: Calvert Superbasin. Consists of sandstone with conglomerate at the base of formation.||||||07-FEB-11
17551|Surprise Creek Formation|63113|5|Briefly described|p1214 Fig.2, p1225 Fig.13.|||Calvert Superbasin. Part of Prize supersequence.|1709 Ma.|Of the Myally Subgroup||Overlies Fiery Creek Formation.||
17551|Surprise Creek Formation|63114|5|Briefly described|p1253 Fig.2. |||Calvert superbasin.||Of the Prize supersequence.||Overlies Fiery Creek Volcanics.||
17551|Surprise Creek Formation|63115|6|Mentioned|1279 Fig.4, p1281, |||Calvert superbasin.||||||
17551|Surprise Creek Formation|63116|6|Mentioned|p1297 Fig.2,p1299 Tb.1,p1300, |||Calvert superbasin. Material properties detailed.||||||
17551|Surprise Creek Formation|63866|5|Briefly described|p58|||||||Overlies the Bigie Formation.||
17551|Surprise Creek Formation|64250|5|Briefly described|p25 fig 10, p11 fig 3, p27, p18|||Western Fold Belt, Mount Isa Inlier. Deeper water facies carbonaceous siltstone. Cu mineralisation.|1700-1690|||Is overlain by Torpedo Creek Quartzite and Warrina Park Quartzite. Correlated with Mount Albert Group in Eastern Fold Belt.|Deeper water facies carbonaceous siltstone.|
17551|Surprise Creek Formation|64367|5|Briefly described|p555  Fig. 1c|Paleoproterozoic|Paleoproterozoic|Age: 1688+/-5Ma.||||||07-FEB-11
17551|Surprise Creek Formation|64725|6|Mentioned|p58 Fig.2. |||Mount Isa Inlier.||||||
17551|Surprise Creek Formation|64726|6|Mentioned|p83 Fig.2.|||||||||
17551|Surprise Creek Formation|64744|6|Mentioned|p353 Fig.4. |Statherian|Statherian|Mount Isa Basin.||||||
17551|Surprise Creek Formation|64834|5|Briefly described|p12, p13 Fig.2, p31-32|||Calvert Superbasin. Western Succession of Mount Isa Basin.||||Unconformably overlies Eastern Creek Volcanics.|Sandstone, with pebble conglomerate near base.|
17551|Surprise Creek Formation|65228|5|Briefly described|p21, p23, Figs.04, 09, 10.|||Leichhardt River Fault Trough. Studied in detail by Domagala et al. (2000).||||Unconformably overlies Bigie Formation, Myally Subgroup and Eastern Creek Volcanics.||
17551|Surprise Creek Formation|65337|4|Described|p v, pp19-20.|Calymmian|Statherian|Calvert Superbasin. Thin siliciclastic veneer, from zero to 2000 m thick, of braided fluvial deposits, with local alluvial fan deposits at base.|1700-1690 Ma.|||Unconformably overlies Carrara Range Group. Is unconformably overlain by Gunpowder Creek or Drummond Formations of the McNamara Group.|Basal conglomerates, poorly-sorted and matrix-supported, sub-rounded to well-rounded pebbles and cobbles of quartz, quartzite and quartz sandstone, some rhyolite clasts; under white to pink, medium- to coarse-grained, sublithic to quartz sandstone.|
17551|Surprise Creek Formation|65396|5|Briefly described|p16, p82, p175, p184, p190, p201, p241|Statherian|Statherian|Calvert Superbasin. Cover Sequence 2. Lawn Hill Platform, Leichhardt River Fault Trough, Kalkadoon-Leichhardt Belt.|1700 - 1690 Ma|||Overlain by Torpedo Creek Quartzite, Warrina Park Quartzite.|Sandstone, calcareous shales, pelites and mafic volcanics.|04-APR-17
17551|Surprise Creek Formation|66529|6|Mentioned|p34|||Calvert Superbasin. Hosts some uranium prospects.||||||
17551|Surprise Creek Formation|66824|6|Mentioned|p148|||||||Unconformably overlies Fiery Creek Volcanics. Is overlain unconformably by Mount Isa Group.||
17551|Surprise Creek Formation|67026|6|Mentioned|p336 Fig.3.|Statherian|Statherian||1694 +/- 3 Ma (Page et al. 2000).|||||24-APR-12
17551|Surprise Creek Formation|67323|5|Briefly described|p8, p11, p25, p34, 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. Widespread unit in the Mount Isa Inlier. Ages by Page et al. (2000); Jackson et al. (2005) respectively.|1694 +/-3 Ma; 1687.7 +/-4.6 Ma.|||Unconformably overlies Quilalar Formation, Fiery Creek Volcanics, Myally Subgroup, Eastern Creek Volcanics (locally).|Quartzite, sandstone, calcareous sandstone, conglomerate, siltstone, shale|
17551|Surprise Creek Formation|67499|6|Mentioned|p948|||||Of Mount Isa Group?||||
17551|Surprise Creek Formation|68021|5|Briefly described|p135 fig 4|Statherian|Statherian|Prize Supersequence,  Calvert Superbasin, Western Succession. Environment changing from near-shore to deltaic or shallow marine.||||Overlies Fiery Creek Volcanics unconformably, overlain by McNamara Group, Mount Isa Group unconformably. Intruded by Sybella Granite? Part Equivalent to Roxmere Quartzite.|?Several cycles of upward-fining mainly siliciclastic sedimentation and increasing amounts of thinly laminated carbonaceous shale or rhythmite towards top.|
17551|Surprise Creek Formation|68146|5|Briefly described|p3, p189, p199, p203|||Age of tuff beds within the unit.|c.1688 Ma; Jackson et al. (2005).|||Overlies Fiery Creek Volcanics. Is overlain by Bularnu Formation.||
17551|Surprise Creek Formation|68542|5|Briefly described|p7|||Surprise Creek beds.|||||Sandstone, quartzite and conglomerate.|
17551|Surprise Creek Formation|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province.||||||
17551|Surprise Creek Formation|68575|5|Briefly described|p3, p37, p127|||SHRIMP age of "shallow-level peperitic intrusives". Also has detrital zircon maximum deposition ages of 1745 +/- 6 Ma and 1731 +/- 12 Ma (Neumann et al., 2009).|1688 +/- 5 Ma (Jackson et al., 2005).|||||
17551|Surprise Creek Formation|68576|5|Briefly described|Q_2: p7||||||||Sandstone, quartzite, conglomerate.|
17551|Surprise Creek Formation|68732|5|Briefly described|p160-162, p165 Fig.3, p168 Fig.5|||Undulatory rhythmite facies common. Of the Prize Supersequence. Sedimentary depositional ages.|1688 +/- 5, 1688 +/- 6 Ma||||Mainly very fine-grained arkosic sandstones. Includes cross-stratified quartzites and pebbly quartzites at the base, and fine- to coarse-grained quartzites and arenites, fining upwards into thinly bedded sandstones.|01-DEC-17
17551|Surprise Creek Formation|69056|5|Briefly described|p54|||Mount Isa Western Succession; Calvert Superbasin.|||||Sandstone.|
17551|Surprise Creek Formation|69222|5|Briefly described|p221, p222 Fig.2|Statherian|Statherian|Western Fold Belt. Associated with the Mount Isa Rift Event.||||Overlies Carters Bore Rhyolite, overlain by Mount Isa Group, McNamara Group||09-FEB-18
17551|Surprise Creek Formation|69370|6|Mentioned|p307 Fig.2|Statherian|Statherian|Western Fold Belt, Mount Isa Block.||||Overlies Bigie Formation. Is intruded by Weberra Granite. Is overlain by Mount Isa Group.||25-JAN-19
17551|Surprise Creek Formation|69433|4|Described|p18:2-3, 5-9|Statherian|Statherian|Rawlings et al. (2008); previously mapped (Sweet, 1984) as part of now-obsolete Musselbrook Formation. Southern succession, Lawn Hill Platform. Widespread in the Mount Isa region. Up to 450m thick. Braided fluvial, with local alluvial fan at base, deposits.||||Unconformably overlies Carrara Range Group. Is overlain by Mount Isa and McNamara Groups conformably or disconformably.|Basal lenses and beds of sub- to well-rounded pebble to boulder conglomerate with a coarse lithic sandstone matrix, intertonguing with and overlain by white to pink, thickly to very thickly bedded, medium to coarse sublithic to quartz sandstone.|12-JUL-16
17551|Surprise Creek Formation|69591|5|Briefly described|p29, p37-40, p44, p56, p107|Paleoproterozoic|Paleoproterozoic|Mount Isa Province. Part of the Prize Supersequence. Locally there was a hiatus between the lower and upper parts of this unit. Fluvial-shallow-marine deposits. Shows abrupt thickness changes across normal faults, forming wedge-shaped stratal geometries.|1688 +/- 5 Ma (Jackson et al., 2005)..|||Is overlain by Moondarra Siltstone.|Basal quartzite grading upwards into siltstone and minor shale. Also described on p56 as quartzite, sandstone, calcareous sandstone, conglomerate, siltstone, shale.|
17551|Surprise Creek Formation|69673|5|Briefly described|p53|||Up to 450m thick.|||||Conglomerate and sandstone.|
17551|Surprise Creek Formation|70282|5|Briefly described|p544 Tb.1|||Cover sequence 4, Mount Isa. Alluvial fan or shallow-marine deposits.|> 1652 Ma|||Overlain by Mount Isa Group|Conglomerate, sandstone and siltstone,|13-FEB-18
17551|Surprise Creek Formation|70283|6|Mentioned|p25|Paleoproterozoic|Paleoproterozoic|||Mount Isa Group||Overlies Haslingden Group.||14-FEB-18
17551|Surprise Creek Formation|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Five facies associations are separately mapped.|||||Siltstone, sandstone, quartzite, shale, conglomerate, ferruginous oolite marker beds.|
17551|Surprise Creek Formation|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Five facies associations are separately mapped.|||||Siltstone, sandstone, quartzite, shale, conglomerate, ferruginous oolite marker beds.|
17551|Surprise Creek Formation|70864|5|Briefly described|p79, p74 Fig 2, p82|||||?McNamara Group?|Overlies Gunpowder Creek Formation|||14-FEB-18
17551|Surprise Creek Formation|71592|5|Briefly described|Appendix A.|||Kalkadoon-Leichhardt Domain, Mount Isa Orogen.|1691+/-6.9 Ma (MDA: U-Pb zircon SHRIMP)||||Chert, sandstone.|
17551|Surprise Creek Formation|71606|5|Briefly described|p137|Statherian|Statherian|Leichardt River Fault Trough, Mount Isa Inlier.||||Overlain by Mount Isa Group.||
17551|Surprise Creek Formation|71960|5|Briefly described|p85, p83, p87, 104, 105, 106|Proterozoic|Proterozoic|In Paroo Range overlies an unconformity. Herein added to lower Mount Isa Group. Wedges out to west and south.||Of Mount Isa Group.||Unconformably to conformably overlain by Warrina Park Quartzite. Unconformably overlies/truncates Haslingden Group rocks.||
17551|Surprise Creek Formation|71980|5|Briefly described|map legend sheets 1, 2|Proterozoic|Proterozoic|Paroo Range, Western Fault Zone. From base: heterolithic inshore to transitional marine; fan, distributive to coastal; channel fill.||Of Mount Isa Group|||Ferruginous sandstone, dolostone, stromatolite, chert; shale, siltstone, sandstone; feldspathic sandstone; channel-fill framework conglomerate.|
17551|Surprise Creek Formation|72526|5|Briefly described|p6 Fig.1.2, p8 Fig.1.3.|Statherian|Statherian|Age given as U-Pb zircon sedimentary depositional age. Shown as located in the Lawn Hill Platform, Leichhardt River Fault Trough and the Kalkadoon-Leichhardt Belt of the Mount Isa Province and the eastern part of the South Nicholson Basin.|1688 +/-5 Ma|||Shown as unconformably overlying Fiery Creek Volcanics and Bigie Formation and underlies Torpedo Creek Quartzite and Warrina Park Quartzite.||
17551|Surprise Creek Formation|72527|4|Described|p1, 3, 5, 7, 9, 91, p147-160, p193, 194|Statherian|Statherian|South Nicholson Basin. Previously included in the obsolete Musselbrook Formation. Two samples dated from Mt Druumond area, NT: both quartz sandstone, 1858+/-5 Ma, 1743+/-26 Ma, Pb/Pb SHRIMP. Previous studies in Qld established depositional age ~1690-1680 Ma. Uncertain or unassigned stratigraphic affinity. Up to 200 m thick. Type location in the Lawn Hill region, Qld c. 300km southeast of Mount Drummond. Depositional environment is probably a proximal braided fluvial system, with local alluvial fans.|1743+/-26 Ma, 1858 +/- 5 Ma max depositional ages|||Unconformably overlies Top Rocky Rhyolite and unconformably underlies McNamara Group (Drummond Formation).|Well-rounded pebble to boulder conglomerate (with rhyolite clasts near the base), interlayered with sub-lithic to quartz sandstone (displaying small scale trough beds and current lineations).|
17551|Surprise Creek Formation|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Leichardt River Domain and Kalkadoon-Leichhardt Domain. Shown as older than the Isan Orogeny (1590-1500 Ma).||||Shown as partially equivalent in age and older than Garden Creek Porphyry.|Convoluted fine sandstone and siltstone; ferruginous gossanous sandstone. Buff, pink, white, and pale bluish grey thin-bedded fine to medium labile and ferruginous feldspathic sandstone, conglomerate, mud flake-shale pellet beds and quartzite.|
17551|Surprise Creek Formation|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Leichardt River Domain and Kalkadoon-Leichhardt Domain. Shown as older than the Isan Orogeny (1590-1500 Ma).||||Shown as partially equivalent in age and older than Garden Creek Porphyry.|Convoluted fine sandstone and siltstone; ferruginous gossanous sandstone. Buff, pink, white, and pale bluish grey thin-bedded fine to medium labile and ferruginous feldspathic sandstone, conglomerate, mud flake-shale pellet beds and quartzite.|
17551|Surprise Creek Formation|72889|6|Mentioned|p6 Fig.i.|||||||||
17551|Surprise Creek Formation|72912|5|Briefly described|p5 Fig.3, p13.|Statherian|Statherian|Of Calvert Superbasin. 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 sedimentary depositional age (Ma).|1688 +/- 5 Ma|Of Prize supersequence.||Shown as unconformably overlying Fiery Creek Volcanics and Bigie Formation and underlies Torpedo Creek and Warrina Park Quartzite.||
17551|Surprise Creek Formation|72919|6|Mentioned|p5|Paleoproterozoic|Paleoproterozoic|||||Unconformably underlain by Top Rocky Rhyolite (Carrara Range Group). Unconformably overlain by Drummond Formation (McNamara Group).||
17551|Surprise Creek Formation|73042|6|Mentioned|p4|Statherian|Statherian|The Surprise Creek Formation is recorded at two different chronostratigraphic levels in the South Nicholson Basin region / Mount Isa Province, but there is no explanation. The unit is written as Surprise Creek Formation* in the older instance, in Carrara Range Group. South Nicholson Basin region and Mount Isa Province, Calvert Superbasin. Geochronology is a U-Pb zircon sedimentary depositional age (?maximum depositional age) from the chronostratigraphically higher of the two instances of the unit, further east,  in Fig.1.2. overlain by Torpedo Creek/Warrina Park Quartzite.|1688 +/- 5 Ma (see comments and Fig.1.2)|Nil and Carrara Range Group (see comments)||Drummond Formation overlies unconformably. Top Rocky Rhyolite, Fiery Creek Volcanics/Bigie Formation underlie unconformably.||
17551|Surprise Creek Formation|73043|6|Mentioned|p15 Fig.8|Paleoproterozoic|Paleoproterozoic|||||||
17551|Surprise Creek Formation|73083|6|Mentioned|p72|||||||||
17551|Surprise Creek Formation|73137|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|||||||
17551|Surprise Creek Formation|73144|6|Mentioned|p9-10|||Calvert Superbasin. Prize Supersequence. Deposited in a coastal plain, nearshore environment with some below storm wavebase deposits (Southgate et al., 2000).|||||Sandstone, conglomerate and siltstone.|
17551|Surprise Creek Formation|73525|5|Briefly described|p4-5 Fig.2|Statherian|Statherian|Mount Oxide-(Ardmore-May Downs) and Leichhardt River Domains.|1694+/-3 Ma, 1687+/-4 Ma, 1682+/-19 Ma||||Clastics, siliciclastics.|
17573|Swan Group|13353|6|Mentioned|p398. |||Name replaced by Swan Formation. Includes hydrocarbon source rocks.|||Includes (Lower and Upper) Vulcan Formation.|||
17573|Swan Group|13354|6|Mentioned|p375 Fig.6.|Early Cretaceous|Middle Jurassic|Comprises Lower and Upper Vulcan Formations.||44||||28-OCT-14
17573|Swan Group|22663|5|Briefly described|AC97 1-4 Fig.4|||||||||01-MAR-10
17573|Swan Group|23378|4|Described|p180 Fig.2|Early Cretaceous|Middle Jurassic|In the Vulcan Sub-basin.||||||01-MAR-10
17573|Swan Group|41733|6|Mentioned|Fig.3|||||||||
17573|Swan Group|42053|5|Briefly described|Fig.17 P47|||||||||01-MAR-10
17573|Swan Group|42066|5|Briefly described|Fig.3 P199|||||||||
17573|Swan Group|60634|6|Mentioned|p1168 Fig.3. |Early Cretaceous|Late Jurassic||||Includes the Vulcan Formation.|Overlies Troughton Group. Is overlain by Bathurst Island Group.||
17573|Swan Group|61550|6|Mentioned|p495 Fig.2. |Berriasian|Callovian||||Includes the Vulcan and Montara Formations.|Unconformably overlies Plover Formation. Is overlain by Bathurst Island Group.||
17573|Swan Group|66187|5|Briefly described|p413 Fig.2|Berriasian|Oxfordian|Mount Ashmore Dome, Bonaparte Basin. Includes the Upper and Lower Vulcan Formation and Montara Formation.||||||
17573|Swan Group|69297|6|Mentioned|p305|Berriasian|Callovian|Caswell, Barcoo and Seringapatam Sub-basins of the Browse Basin.|||Includes the Montara Formation, the Lower Vulcan Formation and the Upper Vulcan Formation.|Overlies the Troughton Group. Overlain by the Bathurst Island Group.||
17573|Swan Group|69452|5|Briefly described|p36:15|Early Cretaceous|Jurassic|Bonaparte Basin.|||Montara, Vulcan Formations.|||12-JUL-16
17573|Swan Group|70061|6|Mentioned|Regional geology Fig.7. Vulcan: Fig.2|Tithonian|Callovian||||Ashmore Volcanics, Lower and Upper Vulcan Formation, Montara Formation.|||12-JUL-16
17573|Swan Group|70064|5|Briefly described|Regional Fig. 6. Central: Fig.2|Valanginian|Callovian|See also Northern: Fig.2. Yampi: Fig.2. Browse Basin.|||Lower and Upper Vulcan, Montara Formations.|Overlies Troughton Group. Is overlain by Bathurst Island Group.||12-JUL-16
17583|Swift Formation|13995|5|Briefly described|p75|Middle Ordovician|Early Ordovician|Georgina Basin. Rostroconch species listed.||||||
17583|Swift Formation|22954|5|Briefly described|Fig1p6,Fig5p16,23-4|Tertiary|Warendan|Correlates with Digby Peaks Breccia.||||||
17583|Swift Formation|24065|4|Described|p235|Early Ordovician|Late Cambrian|Geological Province: Georgina Basin.  Maximum thickness: 20m.||||||
17583|Swift Formation|30914|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
17583|Swift Formation|31572|4|Described|Fig. 1|||L.Ord.||||||
17583|Swift Formation|32576|6|Mentioned|p50|||Potential aquifer||||||
17583|Swift Formation|33111|4|Described|p43|||||||||
17583|Swift Formation|33738|6|Mentioned|p49|||||||||
17583|Swift Formation|35121|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
17583|Swift Formation|35139|4|Described|Table.2|||||||||
17583|Swift Formation|35936|6|Mentioned|p614|||||||||
17583|Swift Formation|36645|6|Mentioned|p312|||||||||
17583|Swift Formation|37413|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
17583|Swift Formation|37572|4|Described|p162|||See also Fig.8||||||
17583|Swift Formation|38444|5|Briefly described|p118|||||||||
17583|Swift Formation|38532|4|Described|Fig.1|||||||||
17583|Swift Formation|38608|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
17583|Swift Formation|39445|5|Briefly described|Table 4|||See also p64.||||||05-DEC-06
17583|Swift Formation|39690|6|Mentioned|Fig.2|||||||||
17583|Swift Formation|40127|6|Mentioned|p8|||||||||
17583|Swift Formation|40136|5|Briefly described|p40|||||||||
17583|Swift Formation|42354|5|Briefly described|p11|||||||||
17583|Swift Formation|43807|6|Mentioned|Fig.3,p348|||||||||
17583|Swift Formation|44358|6|Mentioned|p19|||Boulia area.||||||
17583|Swift Formation|44361|14|Not recorded|Map Legend||Early Ordovician|||||||
17583|Swift Formation|44362|4|Described|p11,Tb.1||Early Ordovician|||||||
17583|Swift Formation|44469|14|Not recorded|p.19|||Similar to Kelly Creek Formation lithology.||||||05-DEC-06
17583|Swift Formation|44543|2|Defined|p33||Early Ordovician|Overlies Ninmaroo Formation.||||||
17583|Swift Formation|44920|14|Not recorded|Map Legend, Sheet 4||Early Ordovician|||||||
17583|Swift Formation|45051|6|Mentioned|p4|||See also p10.23,Fig.3. Lower Ordovician age.||||||05-DEC-06
17583|Swift Formation|45052|2|Defined|p126|Early Ordovician|Early Ordovician|See also p37.||||||05-DEC-06
17583|Swift Formation|45058|6|Mentioned|Fig. 11|||Correlation||||||
17583|Swift Formation|45079|6|Mentioned|p12|||Map legend on p12.||||||05-DEC-06
17583|Swift Formation|45115|6|Mentioned|p6|||||||||
17583|Swift Formation|45166|5|Briefly described|Table 15|||||||||
17583|Swift Formation|46897|6|Mentioned|Fig.2|||||||||
17583|Swift Formation|46958|6|Mentioned|p195|||See also Fig.2.||||||
17583|Swift Formation|50100|5|Briefly described|p22|Early Ordovician|Early Ordovician|Comprises chert with siltstone, sandstone, silicified coquinite, limestone and dolomite interbeds; highly fossiliferous.  Overlies the Ninmaroo Formation.||||||
17583|Swift Formation|60359|5|Briefly described|Map Legend|Ordovician|Ordovician|Siltstone, sandstone, chert.||||||
17583|Swift Formation|63450|5|Briefly described|p78 Fig. 5, p82|Arenig|Tremadoc|Overlies Ninmaroo Formation as a regolith derived from karstification of the Ninmaroo Formation. Geological province: Georgina Basin, Burke River Structural Belt.||||||07-FEB-11
17583|Swift Formation|64068|3|Fully described|p75, 74, 75|Early Ordovician|Early Ordovician|Diverse fauna. 20 m thick. Regolith preferentially developed over weathered surfaces of Corrie and Datson Members of Ninmaroo Formation. Correlated with Kelly Creek Formation.||Of Cockroach Group.|||Chert, siltstone, sandstone, silicified coquinite, limestone, dolostone.|04-APR-12
17583|Swift Formation|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map; p83|Ordovician|Ordovician|Burke River Structural Belt, Georgina Basin.||Cockroach Group.||Overlies Ninmaroo Formation.|Siltstone, sandstone, coquinite (all silicified in part) chert|
17583|Swift Formation|67870|6|Mentioned|p43|Ordovician|Ordovician|Burke River Structural Belt, Georgina Basin.||||||
17583|Swift Formation|69443|5|Briefly described|p28:7, 25-26|Early Ordovician|Early Ordovician|Southern Georgina Basin. Regarded as a subaerial regolith discordant on the uppermost Ninmaroo Formation.||Cockroach Group.||Conformably overlies Ninmaroo Formation.||12-JUL-16
17583|Swift Formation|69591|5|Briefly described|p87, p93-94|Ordovician|Ordovician|Burke River Structural Belt, Georgina Basin. About 20m thick. Contains trilobites, brachiopods and a Bendigonian-age graptolite. Has undergone considerable diagenesis; interpreted as the silicification product of the upper two members (encrinite and dolomite) of the Ninmaroo Formation.||||Is laterally equivalent to the upper part of Ninmaroo Formation; locally overlies it unconformably. Unconformably overlies Beetle Creek Formation.|Bedded chert with interbeds of siltstone, sandstone, silicified coquinite and limestone.|
17583|Swift Formation|69673|6|Mentioned|p114 fig 92|||||Cockroach Group||Overlain by Kelly Creek Formation, overlies Chabalowe Formation, Arrinthrunga Formation||
17589|Sybella Granite|22498|6|Mentioned|Fig1 P234||Statherian|||||||
17589|Sybella Granite|22644|6|Mentioned|19|||Geol province Mount Isa Basin||||||
17589|Sybella Granite|22692|6|Mentioned|p765|||||||||
17589|Sybella Granite|23363|5|Briefly described|344 Fig.3|||||||||
17589|Sybella Granite|23396|5|Briefly described|p419|Statherian|Statherian|Age: 1671+/-8Ma.||||||05-DEC-06
17589|Sybella Granite|23398|5|Briefly described|p449|Statherian|Statherian|Age: ~1670Ma.||||||05-DEC-06
17589|Sybella Granite|23408|5|Briefly described|p510 Fig.1, p513 Fig. 2, p527|||||||||15-JUN-09
17589|Sybella Granite|23458|6|Mentioned|p114, p127|||In the Eastern Fold Belt.||||||27-AUG-07
17589|Sybella Granite|23776|5|Briefly described|p707 Fig 4|Statherian|Statherian|Age: 1670+/-8 Ma||||||02-NOV-07
17589|Sybella Granite|23969|6|Mentioned|p1371 Fig.2|||Geological Province: Mount Isa Inlier.||||||
17589|Sybella Granite|23972|5|Briefly described|p1422|Mesoproterozoic|Mesoproterozoic|Geological Province: Mount Isa Inlier.  Age: ~1660Ma.||||||
17589|Sybella Granite|24033|6|Mentioned|p15|||||||||
17589|Sybella Granite|24197|5|Briefly described|p130|Paleoproterozoic|Paleoproterozoic|Of Sybella Suite. Geological province: Mount Isa Inlier.||||||07-FEB-11
17589|Sybella Granite|24253|5|Briefly described|p9|Proterozoic|Proterozoic|Age: 1660 Ma. Geological Province: Mount Isa Block.||||||
17589|Sybella Granite|24254|5|Briefly described|p17, p24|Proterozoic|Proterozoic|Geological Province: Mount Isa Block. Age: ca. 1660-1670 Ma.||||||
17589|Sybella Granite|24419|5|Briefly described|p17, p12 Fig.4, p15 Fig.6|Proterozoic|Proterozoic|Of the Sybella Suite.||||||
17589|Sybella Granite|24432|5|Briefly described|p564 Fig.4|Statherian|Statherian|Geological Province: Mount Isa Inlier.||||||
17589|Sybella Granite|30531|6|Mentioned|p22|||||||||
17589|Sybella Granite|30534|6|Mentioned|p300|||See also p302,305.||||||05-DEC-06
17589|Sybella Granite|30535|6|Mentioned|p404|||Refers age Warrina Park Quartzite||||||
17589|Sybella Granite|30536|6|Mentioned|p100|||||||||
17589|Sybella Granite|30721|5|Briefly described|p53|||See also p54.||||||05-DEC-06
17589|Sybella Granite|30723|4|Described|p340|||Rb/Sr 1655m.y. Isotopic plot p346. See also p348.||||||05-DEC-06
17589|Sybella Granite|30724|6|Mentioned|p74|||Age given||||||
17589|Sybella Granite|30725|4|Described|p576|||||||||
17589|Sybella Granite|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
17589|Sybella Granite|31342|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
17589|Sybella Granite|32041|4|Described|p353|||||||||
17589|Sybella Granite|32042|5|Briefly described|p36|||||||||
17589|Sybella Granite|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17589|Sybella Granite|32660|5|Briefly described|Table 5|||||||||
17589|Sybella Granite|32818|5|Briefly described|p17|||Age||||||
17589|Sybella Granite|32951|6|Mentioned|p1276|||Consists of several phases||||||
17589|Sybella Granite|32952|6|Mentioned|p1188|||Precambrian||||||
17589|Sybella Granite|32959|6|Mentioned|p31|||||||||
17589|Sybella Granite|33482|6|Mentioned|p6|||||||||
17589|Sybella Granite|33893|4|Described|p35|||||||||
17589|Sybella Granite|33896|5|Briefly described|p465|||Foliations discussed||||||
17589|Sybella Granite|33897|6|Mentioned|p1280|||||||||
17589|Sybella Granite|33898|6|Mentioned|p232|||||||||
17589|Sybella Granite|33900|5|Briefly described|p21|||||||||
17589|Sybella Granite|34955|6|Mentioned|p227|||Age dating.||||||
17589|Sybella Granite|35074|6|Mentioned|Fig.2|||||||||
17589|Sybella Granite|35114|6|Mentioned|p203|||||||||
17589|Sybella Granite|35121|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17589|Sybella Granite|35139|4|Described|Table.2|||See also p10.||||||05-DEC-06
17589|Sybella Granite|35146|6|Mentioned|p469|||||||||
17589|Sybella Granite|35167|6|Mentioned|p151|||||||||
17589|Sybella Granite|35286|6|Mentioned|p156|||||||||
17589|Sybella Granite|35950|6|Mentioned|p305|||||||||
17589|Sybella Granite|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17589|Sybella Granite|36548|6|Mentioned|Fig.3|||||||||
17589|Sybella Granite|37217|6|Mentioned|p650|||||||||
17589|Sybella Granite|37371|6|Mentioned|p368|||||||||
17589|Sybella Granite|37459|6|Mentioned|p423|||||||||
17589|Sybella Granite|37462|4|Described|Table4.VII|||||||||
17589|Sybella Granite|37565|6|Mentioned|Fig.5|||||||||
17589|Sybella Granite|37568|6|Mentioned|p85|||||||||
17589|Sybella Granite|37572|6|Mentioned|Fig.8|||||||||
17589|Sybella Granite|37816|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17589|Sybella Granite|37862|6|Mentioned|p586|||||||||
17589|Sybella Granite|38232|6|Mentioned|p83|||See also p89.||||||05-DEC-06
17589|Sybella Granite|38276|6|Mentioned|Fig.1|||||||||
17589|Sybella Granite|38350|4|Described|p20|||See also p10.||||||05-DEC-06
17589|Sybella Granite|38442|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||25-AUG-04
17589|Sybella Granite|38560|6|Mentioned|p115|||||||||
17589|Sybella Granite|38598|6|Mentioned|p208|||||||||
17589|Sybella Granite|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
17589|Sybella Granite|38919|6|Mentioned|p496|||||||||
17589|Sybella Granite|39362|6|Mentioned|p1468|||||||||
17589|Sybella Granite|39445|5|Briefly described|p41|||See also p36 and Table 2.||||||05-DEC-06
17589|Sybella Granite|39622|6|Mentioned|p24|||See also Appendix||||||
17589|Sybella Granite|39690|6|Mentioned|p98|||||||||
17589|Sybella Granite|39822|6|Mentioned|p220|||||||||
17589|Sybella Granite|39934|6|Mentioned|Fig.3|||||||||
17589|Sybella Granite|40623|5|Briefly described|p102|||||||||
17589|Sybella Granite|40840|6|Mentioned|Map legend|||||||||
17589|Sybella Granite|41298|6|Mentioned|Map legend|Carpentarian||||||||
17589|Sybella Granite|41465|6|Mentioned|p12|||||||||
17589|Sybella Granite|41791|6|Mentioned|p250|||||||||
17589|Sybella Granite|41862|6|Mentioned|p474|||||||||
17589|Sybella Granite|41958|6|Mentioned|p98|||||||||
17589|Sybella Granite|41978|6|Mentioned|Fig 2 P499|||||||||
17589|Sybella Granite|41979|6|Mentioned|p538|||||||||
17589|Sybella Granite|42367|4|Described|p18|||U-Pb zircon ages: 1610Ma and 1670Ma.||||||05-DEC-06
17589|Sybella Granite|42503|6|Mentioned|p334|||||||||
17589|Sybella Granite|42706|5|Briefly described|map legend|Paleoproterozoic|Palaeoproterozoic|Age: ~1670Ma. Biotite granite. commonly foliated and porphyritic.||||||09-FEB-09
17589|Sybella Granite|42830|6|Mentioned|p158|||||||||
17589|Sybella Granite|42879|6|Mentioned|p214|||||||||
17589|Sybella Granite|43607|6|Mentioned|p7|||||||||
17589|Sybella Granite|43608|6|Mentioned|Fig.11,p11|||||||||
17589|Sybella Granite|43760|6|Mentioned|p442|||||||||
17589|Sybella Granite|44210|14|Not recorded|p8-10,15|||||||||
17589|Sybella Granite|44257|14|Not recorded|p20,21|||Age: Rb-Sr.1540 Ma.||||||05-DEC-06
17589|Sybella Granite|44271|2|Defined|p41,46,48,52,53,60|||||||||
17589|Sybella Granite|44275|14|Not recorded|Map Legend|||||||||
17589|Sybella Granite|44290|14|Not recorded|p437|||||||||
17589|Sybella Granite|44309|2|Defined|Tb.1,opp.p7,map|||||||||
17589|Sybella Granite|44326|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
17589|Sybella Granite|44517|14|Not recorded|p234|||Intrudes Eastern Creek Volcanics and Judenan Beds.||||||
17589|Sybella Granite|44521|14|Not recorded|p14|||||||||
17589|Sybella Granite|44522|4|Described|p1,3-5,7,8,10-12|||Late Early Proterozoic.||||||05-DEC-06
17589|Sybella Granite|44552|14|Not recorded|p23|||||||||
17589|Sybella Granite|44751|14|Not recorded|p300||Precambrian|||||||
17589|Sybella Granite|44755|14|Not recorded|p91|||||||||
17589|Sybella Granite|44812|14|Not recorded|p7|||Soil.||||||
17589|Sybella Granite|44849|14|Not recorded|p69,74-5,82,87,94|||Age: 1780 Ma = approx age of Ewen Granite.||||||05-DEC-06
17589|Sybella Granite|44920|14|Not recorded|Map Legend, Sheet2,4||Carpentarian|||||||
17589|Sybella Granite|44989|2|Defined|p.149-152|||Tb.IV. = Templeton Group. (F54-1,5).||||||
17589|Sybella Granite|45003|14|Not recorded|p15,37|||||||||
17589|Sybella Granite|45052|5|Briefly described|p73|||K/Ar age||||||
17589|Sybella Granite|45072|6|Mentioned|p10|||Intrudes Eastern Creek. Volcanics.||||||05-DEC-06
17589|Sybella Granite|45079|6|Mentioned|p8|||Precambrian. Minimum age 1400 m.y.||||||
17589|Sybella Granite|45087|5|Briefly described|p14|||Chemical analyses.||||||
17589|Sybella Granite|45161|4|Described|p13|||||||||
17589|Sybella Granite|45166|5|Briefly described|p37|||||||||
17589|Sybella Granite|45287|14|Not recorded|p.228,231||Archean|||||||07-NOV-08
17589|Sybella Granite|46801|6|Mentioned|p115|||See also Fig. 14||||||
17589|Sybella Granite|46962|6|Mentioned|p251|||||||||
17589|Sybella Granite|46976|6|Mentioned|Fig.1|||||||||
17589|Sybella Granite|48894|6|Mentioned|p33|||Age. See also pp34,35,36.||||||05-DEC-06
17589|Sybella Granite|48906|14|Not recorded|p4,28|||||||||
17589|Sybella Granite|48997|6|Mentioned|Fig.3|||||||||
17589|Sybella Granite|49041|5|Briefly described|Table 1|||||||||
17589|Sybella Granite|50542|6|Mentioned|p96|Paleoproterozoic|Paleoproterozoic|||||||07-FEB-11
17589|Sybella Granite|50550|5|Briefly described|p1140 Fig.3, p1152 Fig.13|||Geological Province: Western Fold Belt.||||||19-DEC-07
17589|Sybella Granite|50624|6|Mentioned|236 Fig.3||Statherian|Sybella Batholith has age of 1660 Ma.||||||
17589|Sybella Granite|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Biotite granite.||||||
17589|Sybella Granite|60513|6|Mentioned|p281, p290, 288|||||||||
17589|Sybella Granite|61204|6|Mentioned|p544|Statherian|Statherian|Geological Province: Mount Isa Inlier. Age: ca. 1660 Ma (Page et al.,2000)||||||
17589|Sybella Granite|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: <1700Ma. Geological Province: western Mount Isa Block.||||||07-NOV-08
17589|Sybella Granite|61736|5|Briefly described|p672 Fig. 7, p673|Paleoproterozoic|Paleoproterozoic|Age: 1671+/-8Ma. Geological province: Broken Hill Domain. Felsic magmatism.||||||24-FEB-10
17589|Sybella Granite|61922|5|Briefly described|p19 Fig. 11|||See also p21 Fig.13.||||||
17589|Sybella Granite|61923|5|Briefly described|p28 Fig.1|Paleoproterozoic|Paleoproterozoic|Comprises a suite of sheet-like bodies - a composite of intrusive phases, coarse-grained granodiorite to alkali-feldspar granite in this study area. Intrudes the Haslingden Group. Age: 1660+/-4 Ma and 1655+/-5 Ma. Geological Province: Mount Isa Inlier.||||||07-NOV-08
17589|Sybella Granite|61924|6|Mentioned|p43B|||||||||
17589|Sybella Granite|61933|5|Briefly described|p169 Fig.1|Paleoproterozoic|Paleoproterozoic|Age: 1675-1655 Ma; ca 1670-1655 Ma. See also p171 Tb.1.||||||07-NOV-08
17589|Sybella Granite|61936|5|Briefly described|p191, p194 Fig. 6|Mesoproterozoic|Paleoproterozoic|Age: ca 1610+/-13Ma, 1544+/-12Ma and 1510+/-13Ma.||||||07-NOV-08
17589|Sybella Granite|61963|6|Mentioned|p776|||Part of batholic plutons emplaced near Mount Isa.||||||
17589|Sybella Granite|62084|6|Mentioned|p950 Fig.14|||Mt Isa district.||||||
17589|Sybella Granite|62535|6|Mentioned|p672-673|Statherian|Statherian||1671 +/- 8 Ma.|||||
17589|Sybella Granite|62873|6|Mentioned|p692 Fig. 1|||||||||
17589|Sybella Granite|62988|5|Briefly described|p34|Paleoproterozoic|Paleoproterozoic|Coeval with Carters Bore Rhyolite.  Age: ~1675-1670Ma. Geological Province: Mount Isa Inlier.||||||07-NOV-08
17589|Sybella Granite|63023|5|Briefly described|p1024 Fig. 1, p1035|||Of Sybella Suite. Age: ca 1670Ma. Geological Province: Western Fold Belt.||||||
17589|Sybella Granite|63110|6|Mentioned|p1141 Fig. 17|Statherian|Statherian|||||||
17589|Sybella Granite|63593|5|Briefly described|p285 Fig.1, p287, p288 Fig.2. |Palaeoproterozoic|Palaeoproterozoic|Western Fold Belt. 1600 km2. Appears as Sybella granite on p287. See also p291 Fig.3 and Tb.2.|ca. 1670 Ma|||Intrudes Carters Bore Rhyolite and McNamara Group.||
17589|Sybella Granite|64249|5|Briefly described|p82 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: 1675-1655Ma. Geological Province: Mount Isa Inlier.||||||22-APR-09
17589|Sybella Granite|64250|6|Mentioned|p8, p9 fig 1, p11 fig 3, p21-22|||Western Fold Belt, Mount Isa Inlier. Mention is also made of the Sybella Batholith, not a stratigraphic term.|1674 +/- 4 Ma - 1655 +/- 4 Ma.|||||
17589|Sybella Granite|64254|6|Mentioned|p171|||||||||
17589|Sybella Granite|64367|5|Briefly described|p555  Fig. 1b, p560, p561 Tb. 2|Paleoproterozoic|Paleoproterozoic|Of the Sybella Batholith. Age of batholith: 1675-1665Ma. Intruded the Eastern Creek Volcanics.||||||07-FEB-11
17589|Sybella Granite|64725|6|Mentioned|p58 Fig.2. |||Mount Isa Inlier.||||||
17589|Sybella Granite|64726|6|Mentioned|p83 Fig.2.|||||||||
17589|Sybella Granite|64744|5|Briefly described|p353 Fig.4, p355 Fig.5, pp358-359.|Statherian|Statherian|Mount Isa Basin. A suite of stacked, I-type granite sill-like bodies, with amphibolite facies metamorphic aureole. Magmatism was synkinematic: gneissic fabric and near-identical monazite ages in the aureole.|1670 +/- 3 Ma.||||Granitic sills intercalated with lesser gabbro and dolerite.|
17589|Sybella Granite|64769|6|Mentioned|p26|Proterozoic|Proterozoic|QLD.||||||06-MAY-09
17589|Sybella Granite|64832|5|Briefly described|p1155 Fig. 1|Paleoproterozoic|Paleoproterozoic|Part of the Sybella Batholith which intruded the Haslingden Group. Age of emplacement: 1675-1655Ma (SHRIMP U-Pb zircon; Connors and Page 1995; Page et al 2000; Neumann et al 2005).||||||07-FEB-11
17589|Sybella Granite|64834|5|Briefly described|p13, p15, p32|||Sybella Intrusion shown in Fig.2|1678+/-8 Ma|||||
17589|Sybella Granite|65228|5|Briefly described|pp20-21, Fig.04.|Statherian|Statherian|Mount Isa region. Emplaced c.1680 - 1670 Ma.|1671 +/- 8 Ma.|||||
17589|Sybella Granite|65387|6|Mentioned|p55-56, p82|||A sample of migmatised gneissic granite, mapped as a component of this unit, was dated at 1782 +/- 5 Ma, but the authors point out that this sample is "different from other mapped units of the Sybella Batholith with which it has been equated".||||||05-APR-18
17589|Sybella Granite|65396|6|Mentioned|p11, p82, p103-104, p161, p172, p175|Statherian|Statherian|See also p193, p195, p241, p262, p274, p319, p361, p440. Lawn Hill Platform. Formations with detrital zircons from this unit are listed.|1675 +/- 3 Ma, 1660 +/- 5 Ma, 1655 +/- 4 Ma|||||
17589|Sybella Granite|65755|6|Mentioned|p2|||||||||
17589|Sybella Granite|66529|5|Briefly described|p3, p33, p37, p41, p94 |Proterozoic|Proterozoic|Western Mount Isa Province. Highly uranium enriched. ~1670 Ma Schofield (2009)||||||
17589|Sybella Granite|66824|5|Briefly described|p133-140, 145-151|||Referred to in the text as the Sybella Batholith (not a stratigraphic term); Wyborn (1979). Problems with previous age determinations discussed.|1660 +/- 5 Ma; 1655 +/- 4 Ma.|||Intrudes Haslingden Group.|An extensive felsic igneous complex, largely comprising granodiorite and alkali feldspar granite. Metamorphosed, multiply deformed, and metasomatised (detailed).|
17589|Sybella Granite|66844|6|Mentioned|p245|Statherian|Statherian|Mount Isa region. Age from SHRIMP dating.|1671+\-8 Ma|||||
17589|Sybella Granite|67127|6|Mentioned|p168|||Associated spatially with outcrops of the Mica Creek pegmatites [not a stratigraphic name].||||||
17589|Sybella Granite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.,p12|Paleoproterozoic|Paleoproterozoic|Sybella Igneous Event. Fractionated I-type granite.|1675 - 1670 Ma|Sybella Suite|||Foliated coarse-grained porphyritic biotite granite|
17589|Sybella Granite|67497|6|Mentioned|p905|||Mount Isa Inlier||||||
17589|Sybella Granite|67539|6|Mentioned|p8, p9 Fig.7|Statherian|Statherian|Sybella Belt. Contains xenolithic material with randomly oriented fabrics. 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.|c. 1680 - 1670 Ma|||||
17589|Sybella Granite|68021|5|Briefly described|p135 fig 4, p136, p137, p138|Statherian|Statherian|Shown as Sybella granite p137.|1670 Ma|||Intrudes Eastern Creek Volcanics, Surprise Creek Formation.||
17589|Sybella Granite|68146|5|Briefly described|p1,p4,p6,p64, p106-112,p194,p201,p211|||Sybella Batholith, Mount Isa Region. Forms moderately well-exposed bouldery outcrops. Whole-rock Sm-Nd isotopic data tabulated.|1679 +/- 4 Ma.|||Adjacent to Big Toby Granite.|Pale orange, K-feldspar phyric (up to 3cm) foliated biotite granite.|
17589|Sybella Granite|68542|6|Mentioned|p10|||||||||
17589|Sybella Granite|68575|6|Mentioned|p53, p55|||At Yaringa Creek, along the W margin of the Sybella Batholith, the Big Toby Granite was mapped as this unit; the western edge of the Sybella Granite is farther east.||||||
17589|Sybella Granite|68576|5|Briefly described|QLD_D1: p5, p7, p17|||Near Mount Isa. Granite pavers of this unit are used in the Queen Street Mall.|||||Foliated porphyritic biotite granite with characteristic feldspar augen.|
17589|Sybella Granite|68732|5|Briefly described|p158 Fig.1, p165 Fig.3, p167, p168 Fig.5|Statherian|Statherian|Mount Isa Inlier. Igneous crystallisation ages.|1670 +/- 3, 1674 +/- 4, 1671 +/- 8 Ma|||||
17589|Sybella Granite|69222|6|Mentioned|p224 Fig.3, p225, p227|||Heat flow and production discussed; values given. Apperas as Sybella granite on p227.||||||
17589|Sybella Granite|69370|5|Briefly described|p306, p307 Fig.2 |Statherian|Statherian|Western Fold Belt, Mount Isa Block. Associated with rhyolites, dolerites, sandstones and mudstones of Cover Sequence 3. Age is 1671 Ma in Fig.1.|c.1680 Ma (Page and Bell, 1986).|||Intrudes Mount Isa and McNamara Groups.||25-JAN-19
17589|Sybella Granite|69542|6|Mentioned|p133 Fig.2, p134|Mesoproterozoic|Paleoproterozoic|Western Fold Belt. Mention is also made (p133) of the Sybella Batholith aged ~1665 Ma.||||||09-FEB-18
17589|Sybella Granite|69591|5|Briefly described|p32, p41-42, p59, p107|||Sybella Batholith. Coeval with extrusion of the Carters Bore Rhyolite.|1670 +/- 3 Ma (Neumann et al., 2006).|||Is surrounded by (?intrudes) Alpha Centauri Metamorphics.|Strongly foliated coarse-grained porphyritic biotite granite.|
17589|Sybella Granite|70283|5|Briefly described|p25 Fig.1|Paleoproterozoic|Paleoproterozoic|The Sybella batholith term seems to be preferred in this article; it intrudes the Haslingden Group, was emplaced at 1660 +/- 4 Ma to 1655 +/- 5 Ma, and is broadly contemporaneous with the Mount Isa Group.|||||Granite.|14-FEB-18
17589|Sybella Granite|70858|6|Mentioned|p29, 31, 33|Paleoproterozoic|Paleoproterozoic|Tommy Creek Block, Isan Superbasin. Regarded by the authors as a good candidate for 1.75 Ga and younger detrital zircons in the Wernecke Supersuite, Yukon.|1.67 Ga.|||||
17589|Sybella Granite|70897|6|Mentioned|p41|||Source of 1680 Ma zircons in Mullera Formation.||||||
17589|Sybella Granite|71369|6|Mentioned|p4|||||||||
17589|Sybella Granite|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen. Both ages are crystallisation: U-Pb zircon SHRIMP.|1795+/-5 Ma and 1679+/-4 Ma.||||Granite.|
17589|Sybella Granite|72297|5|Briefly described|p702, p726|||Near Mount Isa. Used as dimension stone; its granite tiles, slabs and stone pave the Queen Street Mall in Brisbane. The beryl crystal-bearing Mica Creek Pegmatite is a phase of this unit.||||||
17589|Sybella Granite|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. 6 ages given as U-Pb zircon igneous crystallisation ages. Range shown in age field.|1679 +/-4 Ma to 1655 +/-4 Ma|||||
17589|Sybella Granite|72889|5|Briefly described|p23-25.|Statherian|Statherian|Of Sybella Batholith. Four previous magmatic ages reported from Neumann et al. 2006, and Carson et al.2011. [Age with smallest error indexed].|1669.7+/-2.9 Ma|||Co-magmatic with dolerite reported herein.||
17589|Sybella Granite|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. Six U-Pb zircon igneous crystallisation ages (Ma) shown. Oldest and youngest recorded here.|1679 +/- 4 Ma to 1655 +/- 4 Ma|||Shown as overlying Carters Bore Rhyolite and underlying McNamara Group.||
17589|Sybella Granite|73042|6|Mentioned|p4|Statherian|Statherian|South Nicholson Basin region and Mount Isa Province, Isa Superbasin. Geochronology is a series of 6 U-Pb zircon igneous crystallisation ages (see Fig.1.2 for list of dates).|~1655+/-4 to1679+/-4 Ma|||||
17589|Sybella Granite|73413|6|Mentioned|p3|||Mount Isa Inlier, Western Fold Belt, Lawn Hill Platform.||||||
17605|Sylvester Sandstone|10116|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Silicified quartzose sandstone, green siltstone.||||||
17605|Sylvester Sandstone|22954|6|Mentioned|Fig3p9|||||||||
17605|Sylvester Sandstone|30914|6|Mentioned|Map legend|Early Cambrian|Proterozoic|Proterozoic - Early Cambrian||||||
17605|Sylvester Sandstone|31287|6|Mentioned|p430|||||||||
17605|Sylvester Sandstone|33111|6|Mentioned|p38|||||||||
17605|Sylvester Sandstone|34454|5|Briefly described|Table 2|||L.Cambrian||||||
17605|Sylvester Sandstone|34847|6|Mentioned|p31|||||||||
17605|Sylvester Sandstone|35121|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
17605|Sylvester Sandstone|35139|4|Described|Table.2|||||||||
17605|Sylvester Sandstone|36234|3|Fully described|p166|||||||||
17605|Sylvester Sandstone|36243|6|Mentioned|Table 1A|||||||||
17605|Sylvester Sandstone|37572|5|Briefly described|p155|||See also Fig.8||||||
17605|Sylvester Sandstone|39445|5|Briefly described|Table 4|||See also p62.||||||05-DEC-06
17605|Sylvester Sandstone|39921|6|Mentioned|Map legend|Middle Cambrian|Early Cambrian|Early to Middle CambrianE - M||||||
17605|Sylvester Sandstone|42060|6|Mentioned|Fig.5 P140|||||||||
17605|Sylvester Sandstone|42956|5|Briefly described|p31 Fig.4|||||||||
17605|Sylvester Sandstone|44121|14|Not recorded|p5|Early Cambrian|Neoproterozoic|||||||
17605|Sylvester Sandstone|44211|14|Not recorded|p97,102|||||||||
17605|Sylvester Sandstone|44291|14|Not recorded|p8|||||||||
17605|Sylvester Sandstone|44308|14|Not recorded|p3,5,Tb.1||Early Cambrian|Equivalent to Mount Birnie Beds.||||||
17605|Sylvester Sandstone|44312|14|Not recorded|Map Legend||Early Cambrian|||||||
17605|Sylvester Sandstone|44543|2|Defined|p31,32,36||Early Cambrian|Overlies Sun Hill Arkose. No fossils.||||||
17605|Sylvester Sandstone|44920|14|Not recorded|Map Legend, Sheet 4||Adelaidean|||||||
17605|Sylvester Sandstone|45052|3|Fully described|p75|||Adelaidean||||||
17605|Sylvester Sandstone|47058|6|Mentioned|Fig.8 P129|||||||||
17605|Sylvester Sandstone|49027|6|Mentioned|p3|||Mention p5.||||||05-DEC-06
17605|Sylvester Sandstone|63450|5|Briefly described|p78 Fig. 5, p80|Cambrian|Cambrian|Geological province: Georgina Basin, East Toko Syncline.||||||07-FEB-11
17605|Sylvester Sandstone|64068|3|Fully described|p54, 55, 225|Early Cambrian|Early Cambrian|360 m thick in type section. Presumed to be Cambrian but may be Neoproterozoic. Correlations: Mount Baldwin Formation, Adam Shale and Red Heart Dolostone (Shergold 1985: 7).||Of Shadow Group.||Presumed to unconformably overlie Sun Hill Arkose.|Silicified brown sandstone, green siltstone.|04-APR-12
17605|Sylvester Sandstone|65489|5|Briefly described|p125|Cambrian|Cambrian|Georgina Basin.||||Overlies Mount Birnie Beds and Sun Hill Arkose. Is overlain unconformably by Thorntonia Limestone.||
17605|Sylvester Sandstone|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map; p83|Early Cambrian|Neoproterozoic|East Toko Syncline, Georgina Basin.||Shadow Group.||Is overlain by Thorntonia Limestone.|Conglomerate, arenite, arkose, shale, mudstone, dolomite.|
17605|Sylvester Sandstone|67870|6|Mentioned|p43|Early Cambrian|Early Cambrian|Georgina Basin.||||||
17605|Sylvester Sandstone|68270|5|Briefly described|p681,683|Early Cambrian|Early Cambrian|Southern Georgina Basin.||||Underlain unconformably by Sun Hill Arkose.||
17605|Sylvester Sandstone|69443|5|Briefly described|p28:7, 14-15|Early Cambrian|Early Cambrian|Southern Georgina Basin.||Shadow Group.||Possible correlative of Octy, Neutral Junction and Mount Baldwin Formations.||12-JUL-16
17605|Sylvester Sandstone|69591|5|Briefly described|p87, p94|Cambrian|Cambrian|West Toko Syncline, Georgina Basin. The rather complicated history of interpretation of this unit is given.||||Overlies Sun Hill Arkose. Is overlain transitionally by Thorntonia Limestone.|Silicified sandstone and green siltstone.|
17605|Sylvester Sandstone|72516|6|Mentioned|p90|Cambrian|Cambrian|Georgina Basin.||||Equivalent to the Mount Baldwin Formation.||02-JUN-21
17668|Talbot Well Formation|14019|5|Briefly described|p4 Fig. 3|||Of the Birrindudu Group.  Geological Province: Birrindudu Basin.||||||
17668|Talbot Well Formation|22446|5|Briefly described|p20|Calymmian|Calymmian|||||||
17668|Talbot Well Formation|23314|5|Briefly described|336|||||||||
17668|Talbot Well Formation|24122|5|Briefly described|p4 Fig.3|||Of Birrindudu Group.  Geological Province: Birrindudu Basin.||||||
17668|Talbot Well Formation|24297|5|Briefly described|p4 Fig.3|Proterozoic|Proterozoic|Of Birrindudu Group.  Geological Province: Birrindudu Basin.||||||
17668|Talbot Well Formation|24441|5|Briefly described|p1 Fig. 1|||Of the Birrindudu Group. Overlies Gardiner Sandstone; overlain by Coomarie Sandstone. Geological Province: Birrindudu Basin.||||||25-JAN-06
17668|Talbot Well Formation|24442|5|Briefly described|p50 Fig. 1|||Of the Birrindudu Group.  Geological Province: Birrindudu Basin.||||||
17668|Talbot Well Formation|29804|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17668|Talbot Well Formation|29805|4|Described|Table 1|||||||||
17668|Talbot Well Formation|29809|5|Briefly described|p418|||||||||
17668|Talbot Well Formation|29811|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
17668|Talbot Well Formation|29812|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17668|Talbot Well Formation|29813|4|Described|Table 2|||||||||
17668|Talbot Well Formation|29818|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
17668|Talbot Well Formation|31361|4|Described|Table 1|||||||||
17668|Talbot Well Formation|31362|4|Described|Table 1|||||||||
17668|Talbot Well Formation|36532|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17668|Talbot Well Formation|36551|6|Mentioned|Table 12|||||||||
17668|Talbot Well Formation|38243|6|Mentioned|p354|||||||||
17668|Talbot Well Formation|42504|5|Briefly described|Table 3 P60|||||||||
17668|Talbot Well Formation|44155|6|Mentioned|p252|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||||Equivalent to Bungle Bungle Dolomite, Osmond Range area.||
17668|Talbot Well Formation|45140|2|Defined|p13, p39-43, p54, p58, p74, p83|||See also Appx.p17-18. Blake et al. (1975). Birrindudu Basin. The type section is on the W side of Supplejack Range, at 19deg 16'45"S, 129deg 54'00"E in the Tanami sheet area. Up to 300m thick. Forms low mounds partly covered with chert rubble; locally capped by laterite and silcrete. May correlate with Bungle Bungle Dolomite and part of Limbunya Group.|c.1600 Ma.|Birrindudu Group.||Conformably overlies Gardiner Sandstone. Is overlain conformably by Coomarie Sandstone; unconformably by Antrim Plateau Volcanics.|Typically chert, commonly stromatolitic, locally brecciated; also includes sublithic arenite, quartz arenite, and laminated siltstone and shale which are locally interlayered with chert, and cherty arenite and stromatolitic limestone.|
17668|Talbot Well Formation|46788|6|Mentioned|p10|||||||||
17668|Talbot Well Formation|46864|4|Described|p38|||||||||
17668|Talbot Well Formation|48950|2|Defined|p36|Neoproterozoic|Neoproterozoic|||||||
17668|Talbot Well Formation|50315|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Birrindudu Group. Stromatolitic chert, cherty arenite, siltstone, mudstone, limestone, quartz arenite, sublithic arenite.||||||07-NOV-08
17668|Talbot Well Formation|50374|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Birrindudu Group.  Stromatolitic chert, cherty arenite, siltstone, mudstone, limestone, quartz arenite, sublithic arenite.||||||07-NOV-08
17668|Talbot Well Formation|50376|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Birrindudu Group. Stromatolitic chert, cherty arenite, siltstone, mudstone, limestone, quartz arenite, sublithic arenite.||||||07-NOV-08
17668|Talbot Well Formation|60676|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Birrindudu Group. Stromatolitic chert, cherty arenite, siltstone, mudstone, limestone, quartz arenite, sublithic arenite.||||||07-NOV-08
17668|Talbot Well Formation|60685|5|Briefly described|p4 Fig. 3|||Of the Birrindudu Group. Geological Province: Birrindudu Basin.||||||19-MAY-05
17668|Talbot Well Formation|61861|6|Mentioned|p3 Table 1|Paleoproterozoic|Paleoproterozoic|See also Talbot Wells Formation (pp22-24).||Unit in Birrindudu Group.|||Recessive unit characterised by chert, conmmonly stromatolitic indicating it is silicified limestone or dolomite; also sublithic arenite, quartz arenite and laminated siltstone, shale and minor limestone.|04-APR-12
17668|Talbot Well Formation|62628|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Birrindudu Group. Geological Province: Birrindudu Basin. Stromatolitic chert, cherty arenite, minor siltstone, mudstone, limestone, quartz arenite.||||||07-NOV-08
17668|Talbot Well Formation|63261|5|Briefly described|p7, p9 Fig. 5, p17|||Of Birrindudu Group. Thickness: 500m. Geological province: Victoria-Birrindudu Basin. Sedimentary structures, stromatolites and dolostone present. See also p[17.||||||07-FEB-11
17668|Talbot Well Formation|64662|5|Briefly described|p30 Fig. 3|Statherian|Statherian|Of the Birrindudu Group. Geological Province: Tanami region.||||||07-FEB-11
17668|Talbot Well Formation|64675|6|Mentioned|Fig.2|||||||||
17668|Talbot Well Formation|65074|4|Described|p349, p351 fig 4-37, p352-353|Mesoproterozoic|Mesoproterozoic|See also p354 Tb. 4-11, p362. Of North/Centre Birrindudu Basin. 250m thick. Occurs as low mounds capped by chert rubble. Type section details given.||Birrindudu Group||Overlies Gardiner Sandstone (conformably). Overlain by Coomarie Sandstone (conformably).|Chert, arenite, siltstone, shale, limestone.|
17668|Talbot Well Formation|65323|5|Briefly described|Map legend|Statherian|Statherian|Of the Birrindudu Group; non-magnetic chert, arenite, siltstone, mudstone and limestone; underlies the Coomarie Sandstone, overlies the Gardiner Sandstone||||||02-FEB-10
17668|Talbot Well Formation|65324|6|Mentioned|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||
17668|Talbot Well Formation|65326|5|Briefly described|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||12-APR-10
17668|Talbot Well Formation|65327|5|Briefly described|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||12-APR-10
17668|Talbot Well Formation|65328|5|Briefly described|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||12-APR-10
17668|Talbot Well Formation|65342|6|Mentioned|p11 Fig.13. |||Birrindudu Basin.||Unit in Birrindudu Group.||Overlies Gardiner Sandstone. Is overlain by Coomarie Sandstone.||
17668|Talbot Well Formation|65349|6|Mentioned|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||
17668|Talbot Well Formation|65350|6|Mentioned|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||
17668|Talbot Well Formation|65351|6|Mentioned|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||
17668|Talbot Well Formation|65352|5|Briefly described|Map legend|Statherian|Statherian|Of the Birrindudu Group; non-magnetic chert, arenite, siltstone, mudstone and limestone; underlies the Coomarie Sandstone, overlies the Gardiner Sandstone||||||
17668|Talbot Well Formation|65353|5|Briefly described|Map legend|Statherian|Statherian|Of the Birrindudu Group; non-magnetic chert, arenite, siltstone, mudstone and limestone; underlies the Coomarie Sandstone, overlies the Gardiner Sandstone||||||
17668|Talbot Well Formation|65354|5|Briefly described|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||12-APR-10
17668|Talbot Well Formation|65355|5|Briefly described|Map legend|Statherian|Statherian|Of the Birrindudu Group; non-magnetic chert, arenite, siltstone, mudstone and limestone; underlies the Coomarie Sandstone, overlies the Gardiner Sandstone||||||
17668|Talbot Well Formation|65356|5|Briefly described|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group; underlies the Coomarie Sandstone, overlies the Gardiner Sandstone||||||
17668|Talbot Well Formation|67168|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Unit in Birrindudu Group.||Overlies Gardiner Sandstone. Is overlain by Coomarie Sandstone, and unconformably overlain by Antrim Plateau Volcanics.|Chert, arenite, siltstone, mudstone, limestone.|
17668|Talbot Well Formation|69426|6|Mentioned|p11:5 Fig.11.4|||In Blake et al. (1979).||Birrindudu Group.||||12-JUL-16
17668|Talbot Well Formation|69432|5|Briefly described|p17:2, 4, 13|Paleoproterozoic|Paleoproterozoic|Occurs along Coomarie and Supplejack Ranges and in structural basin between the Gardiner and Supplejack Ranges, Birrindudu Basin. Topographically subdued. 300-500m thick. Probably a silicified limestone or dolostone-dominated unit that was deposited on a carbonate platform.||Birrindudu Group.|||Stromatolitic chert, locally massive or brecciated and poorly bedded; sublithic sandstone, quartz sandstone, laminated siltstone, shale and minor limestone.|12-JUL-16
17668|Talbot Well Formation|69673|6|Mentioned|p48 fig 35|||||Birrindudu Group||Overlain by Coomarie Sandstone, overlies Gardiner Sandstone||
17668|Talbot Well Formation|70848|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin.||Birrindudu Group.||Overlies Gardiner Sandstone.|Stromatolitic chert; minor siltstone, mudstone, limestone, quartz sandstone, sublithic quartz sandstone.|
17668|Talbot Well Formation|70852|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin.||Birrindudu Group.|||Stromatolitic chert, cherty sandstone, minor siltstone, mudstone, limestone, quartz sandstone, sublithic sandstone.|
17668|Talbot Well Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Birrindudu Group.|||Shallow marine stromatolitic chert, thinly bedded sublithic sandstone, laminated siltstone, shale and limestone|
17668|Talbot Well Formation|71302|5|Briefly described|p6|Paleoproterozoic|Paleoproterozoic|Of Birindudu Basin.||Unit of Birrindudu Group.||||
17668|Talbot Well Formation|71349|5|Briefly described|p725|||||Birrindudu Group.|||Fine-grained and calcareous.|
17763|Tanami Group|23809|5|Briefly described|p3, p6 Tb. 3|||Overlies the MacFarlane Peak Group with inferred disconformity. Intruded by Repulse Aplite.||||||22-DEC-08
17763|Tanami Group|24197|5|Briefly described|p81|Paleoproterozoic|Paleoproterozoic|Part of the Tanami Complex? (names used interchangeably?). Age: ~2450Ma. Geological province: The Granites-Tanami Block.||||||07-FEB-11
17763|Tanami Group|24442|6|Mentioned|p29|||||||||
17763|Tanami Group|45112|6|Mentioned|p15|||||||||
17763|Tanami Group|50152|5|Briefly described|p71|||Includes; Dead Bullock Formation and Killi Killi Formation.||||||
17763|Tanami Group|50315|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Includes: Twigg Formation, Killi Killi Formation, Dead Bullock Formation. Age: ~1880-<1835Ma.||||||07-NOV-08
17763|Tanami Group|50374|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Includes Dead Bullock, Killi Killi and Twigg Formations.||||||07-NOV-08
17763|Tanami Group|50376|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Includes the Dead Bullock, Killi Killi and Twigg Formations. Mainly dolerite; siltstone, sandstone chert; jasperitic chert; sandstone; siltstone.||||||07-NOV-08
17763|Tanami Group|50589|5|Briefly described|p1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Granites-Tanami Block. Age: 2450Ma? (single zircon from granite sill intruding the Group) to 1815Ma. The names Tanami Group and Tanami Complex appear to be used interchangeably.||||||07-NOV-08
17763|Tanami Group|60676|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes Twigg Formation, Killi Killi Formation, Dead Bullock Formation. Undifferentiated mafic volcanics and meta-sediment; dolerite; undifferentiated Tanami Group; siltstone, sandstone, chert; jasperlitic chert.||||||07-NOV-08
17763|Tanami Group|60681|5|Briefly described|Map legend|Orosirian|Orosirian|Includes the Killi Killi and Dead Bullock Formations.  Age: 1860-1830Ma.||||||
17763|Tanami Group|61056|5|Briefly described|p777-778|Paleoproterozoic|Paleoproterozoic|Has been used to refer to Tanami Complex . Comprises basal quartzite, pelitic to semi-pelitic schists in the middle, and metamorphosed turbiditic sequence at the top. Overlain by Pargee Sandstone.||||||07-NOV-08
17763|Tanami Group|61246|5|Briefly described|p1, p22|Paleoproterozoic|Paleoproterozoic|Overlain by Ware Group. Age: 1850-1830 Ma. Lateral equivalent of Lander Rock beds.||||||07-NOV-08
17763|Tanami Group|61405|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes the Killi Killi Formation. Age: >1835Ma.  Geological Province: Arunta region - Aileron Province.||||||07-NOV-08
17763|Tanami Group|61861|5|Briefly described|p3 Table 1, p4, pp9-14, p23, Map 1|Paleoproterozoic|Paleoproterozoic|This name (of Blake et al 1973) reinstated after use of 'Tanami Complex' for some years. Interpreted as a transgressive passive margin sequence. Hosts gold deposits. Older than Mount Charles Formation.|||Now includes Dead Bullock, Killi Killi and Twigg Formations.|Unconformably overlain by Pargee Sandstone and Mount Charles Formation.||04-APR-12
17763|Tanami Group|62377|5|Briefly described|p5|Paleoproterozoic|Paleoproterozoic|Metasediments. Overlain by Ware Group.||||||07-NOV-08
17763|Tanami Group|62580|5|Briefly described|p9, p21, p54|Paleoproterozoic|Paleoproterozoic|Thick clastic sediments. Overlies MacFarlane Peak Group.||||||07-FEB-11
17763|Tanami Group|62628|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Tanami Inlier.||||||07-NOV-08
17763|Tanami Group|62632|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Tanami/Arunta Region-Aileron Province.||||||07-NOV-08
17763|Tanami Group|62636|6|Mentioned|Map Legend|||Solid Geology legend.|||Killi Killi Formation.|||15-APR-11
17763|Tanami Group|62637|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Tanami/Arunta Region - Aileron Province.||||||23-DEC-09
17763|Tanami Group|63261|4|Described|p9 Fig. 5, p10-12|Paleoproterozoic|Paleoproterozoic|Of Blake et al (1973). Also known as Tanami Complex (Blake et al 1975). Contains basal Dead Bullock Fm+overlying Killi Killi Fm. Age:1880-1830Ma. Metasedimentary succession. Geological province: Tanami Region.|Age:1880-1830Ma.||basal Dead Bullock Fm+overlying Killi Killi Fm|||07-FEB-11
17763|Tanami Group|63866|6|Mentioned|p99|||||||||
17763|Tanami Group|64277|6|Mentioned|Map ledgend|Paleoproterozoic|Paleoproterozoic|Includes Killi Killi Formation.||||||
17763|Tanami Group|64662|5|Briefly described|p28, p30 Fig. 3|Orosirian|Rhyacian|Contains the Dead Bullock and Killi Killi Formations. Group intruded by doleritic sills and deformed by the ~1830Ma Tanami Event. Geological Province: Tanami region.||||||07-FEB-11
17763|Tanami Group|64675|5|Briefly described|p10, Fig.2, p12, p13, p16, p22, p23, p24|Paleoproterozoic|Paleoproterozoic|Represents a passive margin sequence.|||Includes Killi Killi Formation, Twigg Formation and Dead Bullock Formation. See also Map 2|||19-MAR-14
17763|Tanami Group|64722|5|Briefly described|Fig. 2 p3-6,p10|Orosirian|Orosirian|Tanami Region. Age given by Blake et al. (1975) and Cross and Crispe (2007).|1840 Ma.||Contains Killi Killi Formation.|Unconformably overlies Stubbins Formation, unconformably overlain by Ware Group.|Siliciclastic-dominated metasedimentary rocks|11-APR-12
17763|Tanami Group|64725|6|Mentioned|p62|||Regionally intruded by pre-tectonic dolerite sills that locally have peperitic upper and lower margins.|||Includes Dead Bullock and Killi Killi Formations.|||
17763|Tanami Group|64730|5|Briefly described|p141-142|Paleoproterozoic|Paleoproterozoic|Callie Member includes a felsic tuff dated at 1838 +/- 6 Ma.|||Includes Callie Member [in Dead Bullock Formation].|Unconformably overlies Stubbins Formation.||02-MAY-12
17763|Tanami Group|64733|4|Described|p169, 170 Fig.2, p171, p172, p172 Fig.4|Orosirian|Orosirian|Spatially extensive. Subdivided by Crispe et al. (2007). Age (Crispe et al., 2007) of tuffaceous sandstone in Dead Bullock Formation, but some age uncertainty and may be slightly older than ~1840. Overlies Stubbins Formation. Unconformably overlain by Ware Formation. Intruded by dolerite sills|~1840-1835 from SHRIMP U-Pb zircon.||Includes Dead Bullock Formation and Killi Killi Formation.|Overlies Stubbins Formation. Unconformably overlain by Ware Group.||20-APR-12
17763|Tanami Group|64734|5|Briefly described|p187, p186 Fig.1|Orosirian||Includes Dead Bullock Formation, Killi Killi Formation; intruded by 1825-1790Ma granitic suites and numerous dolerite sills; ages poorly constrained; Au known in all units; largest individual gold deposits in the Group are known in Dead Bullock Formation||||||14-SEP-09
17763|Tanami Group|64735|5|Briefly described|p216 Fig15,|Orosirian|Orosirian|Correlated with Lander Package, Bullion Schist, Ooradidgee Group.||||||30-APR-12
17763|Tanami Group|64737|5|Briefly described|p232, p232 Fig.2, p244|||Intruded by 1820-1800 Ma granites.|~1840 Ma.||Includes Killi Killi Formation.|Overlies Stubbins Formation; unconformably overlain by Birrindudu Group.||01-MAY-12
17763|Tanami Group|65323|5|Briefly described|Map legend|Orosirian|Archean|Includes Twigg Formation, Killi Killi Formation and Dead Bullock Formation along with metadolerite sills and four unnamed units differentiated only on the basis of magnetic response which varies from non to highly magnetic||||||02-FEB-10
17763|Tanami Group|65324|5|Briefly described|Map legend|Orosirian|Orosirian|Includes Twigg Formation, Killi Killi Formation and Dead Bullock Formation along with two unnamed units not shown on the map||||||
17763|Tanami Group|65326|5|Briefly described|Map legend|Orosirian|Archean|Includes Twigg Formation, Killi Killi Formation and Dead Bullock Formation as well as moderate-highly magnetic metadolerite sills and four unnamed units differentiated only on the basis of magnetic response, which are not shown on this map||||||02-FEB-10
17763|Tanami Group|65327|5|Briefly described|Map legend|Orosirian|Archean|Includes Twigg Formation, Killi Killi Formation, Dead Bullock Formation, moderate-highly magnetic metadolerite sills and four unnamed units differentiated only on the basis of magnetic response; only one of which is shown on this map||||||
17763|Tanami Group|65328|5|Briefly described|Map legend|Orosirian|Archean|Includes Twigg Formation, Killi Killi Formation, Dead Bullock Formation, moderate-highly magnetic metadolerite sills and on this sheet, one of four unnamed units differentiated only on the basis of magnetic response||||||02-FEB-10
17763|Tanami Group|65335|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Aileron Province. Includes Killi Killi Formation. Age: older than Tanami Event (1835 Ma)||||||
17763|Tanami Group|65349|5|Briefly described|Map legend|Orosirian|Orosirian|Includes Twigg Formation, Killi Killi Formation, Dead Bullock Formation and two unnamed units one of which is not shown on this map. Mafic volcanics and meta-sediment; interbedded turbiditic sandstone and siltstone||||||
17763|Tanami Group|65350|5|Briefly described|Map legend|Orosirian|Orosirian|Includes Twigg Formation, Killi Killi Formation and Dead Bullock Formation as well as two unnamed units not shown on the map; undifferentiated Tanami Group: interbedded turbiditic sandstone and siltstone||||||02-MAR-10
17763|Tanami Group|65351|5|Briefly described|Map legend|Orosirian|Orosirian|Includes Twigg Formation, Killi Killi Formation, Dead Bullock Formation and 2 unnamed units one of which is not shown on the map. Undifferentiated Tanami Group: interbedded turbiditic sandstone and siltstone. Fine to medium grained metadolerite sills||||||02-MAR-10
17763|Tanami Group|65352|5|Briefly described|Map legend|Orosirian|Archean|Includes Twigg Formation, Killi Killi Formation, Dead Bullock Formation along with moderate-highly magnetic metadolerite sills and  3 of 4 unnamed units differentiated only on the basis of magnetic response which varies from non to highly magnetic||||||
17763|Tanami Group|65353|5|Briefly described|Map legend|Orosirian|Archean|Includes Twigg Formation, Killi Killi Formation, Dead Bullock Formation, moderate-highly magnetic metadolerite sills and four unnamed units differentiated only on the basis of magnetic response which varies from non to highly magnetic or complex||||||
17763|Tanami Group|65354|5|Briefly described|Map legend|Orosirian|Archean|Includes Twigg Formation, Killi Killi Formation and Dead Bullock Formation as well as moderate-highly magnetic metadolerite sills and four unnamed units, differentiated only on the basis of magnetic response, which are not shown on this map||||||02-FEB-10
17763|Tanami Group|65355|5|Briefly described|Map legend|Orosirian|Archean|Includes Twigg Formation, Killi Killi Formation, Dead Bullock Formation, moderate-highly magnetic metadolerite sills and 2 of 4 unnamed units differentiated only on the basis of magnetic response which varies from non to highly magnetic||||||
17763|Tanami Group|65356|5|Briefly described|Map legend|Orosirian|Archean|Includes Twigg Formation, Killi Killi Formation and Dead Bullock Formation along with moderate-highly magnetic metadolerite sills and four unnamed units differentiated only on the basis of magnetic response; unnamed units not shown on this map||||||
17763|Tanami Group|65358|4|Described|p6-7|Orosirian|Orosirian|In Tanami Region. Overlies Archean basement (Billabong Complex). Unconformably overlain by Ware Group. Includes basal Dead Bullock Formation. Thick metasedimentary succession. 1850-1830 Ma. Deformed during Tanami Event (1840-1825 Ma).||||||19-DEC-16
17763|Tanami Group|65359|6|Mentioned|p1  |||Includes sedimentary rocks of the former Nongra beds.||||||
17763|Tanami Group|66129|6|Mentioned|p214 Fig.1, p216 Fig.3|||Contains Killi Killi Formation and Dead Bullock Formation.||||||
17763|Tanami Group|66468|5|Briefly described|p16-17, p21, p23, p25-27|Orosirian|Orosirian|1864-1844 Ma. Includes Killi Killi and Dead Bullock Formations. Rift architecture. Is overlain by Ware Group.||||||
17763|Tanami Group|66860|6|Mentioned|p6 Tb.1|||Tanami Region. Deposition of lower parts of this unit was coeval with deposition of Lander Rock beds (Arunta Region) and of Warramunga Formation (Tennant Region). The upper parts were deposited at the same time as lower Strangways Metamorphic Complex protoliths and upper parts of Lander Rock beds (Arunta Region) and upper parts of Ooradidgee Group (Tennant Region).||||||
17763|Tanami Group|67163|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region.|||Includes Killi Killi and Dead Bullock Formations.|||
17763|Tanami Group|67165|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region, Aileron Province. Parts of this unit are mapped according to the strength of their magnetic responses.|||Includes Dead Bullock and Killi Killi Formations.|||
17763|Tanami Group|67168|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||Includes Dead Bullock, Killi Killi and Twigg Formations.|Overlies MacFarlane Peak Group. Intruded by Inningarra, Granites, Frederick, Coomarie, Bore Field Road Suites and Nanny Goat Volcanics. Is unconformably overlain by Birrindudu, Mount Winnecke Groups.||
17763|Tanami Group|67323|5|Briefly described|p29|||Granites-Tanami terrane.|~1850-1835 Ma|||Unconformably overlies Stubbins Formation.||
17763|Tanami Group|67824|5|Briefly described|p383-385, p387, p392-393, p395-396.|Orosirian|Orosirian|Age constrained by constituent Formations. Group thins towards the southeast.|||Includes Killi Killi Formation, Dead Bullock Formation.|Overlies Killi Killi Formation and Billabong Complex. Unconformably overlain by the Ware Group.||
17763|Tanami Group|67826|4|Described|p401 Fig.2, p402, p403||Orosirian|Intruded by extensive granitic magmatism ~ 1820-1790 Ma. Experienced greenschist facies metamorphism and multiple deformation events.|> 1820 Ma||Includes Killi Killi Formation, Dead Bullock Formation.|Unconformably overlain by the Ware Group.||18-SEP-14
17763|Tanami Group|68474|5|Briefly described|p572-574, p576|Palaeoproterozoic|Palaeoproterozoic|Granites-Tanami Orogen. See also Tanami Supergroup. Undergone alteration and greenschist to amphibolite facies metamorphism.|||Includes the Killi Killi Formation, Stubbins Formation and the Dead Bullock Formation.|||
17763|Tanami Group|68656|5|Briefly described|GEOL_LUT_CSV/100k_interpgeop_lut|Paleoproterozoic|Paleoproterozoic|See also 100k_maginterpgeop_lut.csv. Granites-Tanami Complex. Moderate gravity, moderate to highly magnetic.|c.1848-1840 Ma (Huston et al., in press).||Includes Killi Killi Formation.||Metasedimentary rock.|
17763|Tanami Group|68733|5|Briefly described|p186, p187 Fig.6|Statherian|Statherian|Tanami region.||||Uncomformably underlain by the Billabong Complex. Unconformably overlain by the Ware Group. Correlated with Inverway Metamorphics.||06-DEC-17
17763|Tanami Group|68994|6|Mentioned|p6||||||Killi Killi Formation|||
17763|Tanami Group|69003|5|Briefly described|p5, p16-17|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|||Dead Bullock, Killi Killi, Stubbins, Mount Charles Formations.|||
17763|Tanami Group|69253|5|Briefly described|p746-767|Orosirian|Orosirian|Deformation, particularly Trans-Tanami Fault, discussed in detail.|||Includes Dead Bullock and Killi Killi Formations.|Is overlain unconformably by Pargee Sandstone.||
17763|Tanami Group|69288|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region. Most outcrops are weathered to saprock: original textures and fabrics are preserved, but mineralogy has been predominantly replaced.|||Dead Bullock, Killi Killi Formations.|||
17763|Tanami Group|69417|6|Mentioned|p2:5|Orosirian|Orosirian|Tanami Orogen.||||||12-JUL-16
17763|Tanami Group|69419|6|Mentioned|p4:7,|||Greenschist facies metamorphism.||||||12-JUL-16
17763|Tanami Group|69426|4|Described|p11:1, 3-5, 7-8, 10-11, 13-14, 26-27|Orosirian|Orosirian|Blake et al. (1973); later changed to Tanami Complex (Blake et al., 1975) because of inability to determine the constituent units at that time. Cooper and Ding (1997) used the name Tanami Group for a succession of quartzite, two pelitic units, and metamorphosed turbidites; the quartzite being of sedimentary origin and unconformably overlying the Billabong Complex. Crispe et al. (2007) included the two pelitic units in the Dead Bullock and Killi Killi Formations. Crispe and Vandenberg (2005) regarded the quartzite as (non-sedimentary) thickened, sheared quartz veining. Maximum thickness of 10km in the NW, thinning southwards to 3km. Deformation described in some detail. Age range of 1840-c.1815 Ma is given on p13.|Between c.1864 Ma and c.1821 Ma.||Stubbins, Dead Bullock, Killi Killi Formations.|Is overlain (probably) unconformably by Nanny Goat Volcanics (Ware Group).||12-JUL-16
17763|Tanami Group|69427|6|Mentioned|p12:3|||Tanami Region. Direct stratigraphic correlatives occur in 1860-1830 Ma sedimentary protoliths of metasedimentary rocks in the Aileron Province.||||||12-JUL-16
17763|Tanami Group|69429|6|Mentioned|p14:2|||Tanami Region. A likely correlative of the Inverway Metamorphics (Birrindudu Basin).||||||12-JUL-16
17763|Tanami Group|69432|6|Mentioned|p17:2, 4|||||||Is overlain unconformably by the Birrindudu Group.||12-JUL-16
17763|Tanami Group|69587|5|Briefly described|GEOL_LUT_CSV files + geochron files|||Geological province: Granites-Tanami Orogen, North Australian Craton. Of Tanami Basin. Tanami Group deposition was terminated by regional deformation and greenschist to amphibolite-facies metamorphism during the Tanami Event at c. 1830 Ma (Bagas et al., 2007). Events: Alice Springs Orogeny; Tanami Orogeny D1t. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|||Includes Dead Bullock Fomation, Killi Killi Formation.|Overlain unconformably by Ware Group.||
17763|Tanami Group|69618|5|Briefly described|p89-93, p95-97, p101 Fig.11, p102 Fig.13|Paleoproterozoic|Paleoproterozoic|See also p107, p109. Was divided into Stubbins Formation (in the west) and Dead Bullock Formation (in the east). The former is now included within the latter. Spread of detrital zircon ages, from Archean to early Paleoproterozoic, is typical of this Group.|c.1840-1835 Ma (Crispe et al., 2007).||Includes Killi Killi, Stubbins, Dead Bullock and Mount Charles Formations.|||
17763|Tanami Group|69673|6|Mentioned|p3 fig 2|Orosirian|Orosirian|||||||
17763|Tanami Group|69747|5|Briefly described|p262,264,267,272|Paleoproterozoic|Paleoproterozoic|Geological province: Tanami Block, North Australian Craton. Most extensive unit across the Granites-Tanami Orogen. Deposited in a back-arc basin environment. Deposition is followed by subductionof the Tanami back-arc oceanic slab which produced enormous subduction-induced heat and resulted in up to amphibolite facies metamorphism in the group. Palaeoproterozoic (ca. 1864 Ma) mafic suites include massive basalt, pillow basalt, basalt breccia and dolerite sills. Also intruded by c. 1800 Ma mafic dykes.|||Includes Killi Killi Formation and Dead Bullock Formation.|||
17763|Tanami Group|69933|6|Mentioned|p11|||||||||
17763|Tanami Group|70024|6|Mentioned|p35|||Folded and sheared by the c.1795 Ma Tanami Orogeny.|c.1865 Ma.||Dead Bullock, Killi Killi Formations.|||
17763|Tanami Group|70129|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|||Stubbins Formation.|||
17763|Tanami Group|70130|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen. Also includes an un-named but separately-mapped unit of feldspathic metawacke, metasiltstone and metamudstone; minor quartzite, banded metachert, metabasalt, metadolerite and metagabbro.|||Stubbins, Killi Killi Formations.|||
17763|Tanami Group|70141|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|1840-1835 Ma.||Killi Killi Formation.||Wacke, feldspathic wacke, quartz sandstone, sandstone, siltstone, mudstone, banded chert, basalt, dolerite and gabbro: all metamorphosed.|
17763|Tanami Group|70142|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|1840-1835 Ma.||Killi Killi Formation.|Overlies Stubbins Formation.||
17763|Tanami Group|70143|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|||Killi Killi Formation.|||
17763|Tanami Group|70291|4|Described|p178-179,181|Paleoproterozoic|Paleoproterozoic|Geological province: Tanami. Figure 2 p178 suggests that Bald Hill Sequence is part of the Tanami Group, but not so in text. Affected by ~1830 Ma Tanami Event (D1-M1) associated with macrofolding and regional greenschist-amphibolite facies metamorphism.|1838+\-6 Ma||Includes Dead Bullock Formation, Killi Killi Formation, and ?Bald Hill Sequence.|Intruded by dorelite sills, some of which have peperitic contacts with enclosing sedimentary rocks.|Carbonaceous and Fe-rich units.|
17763|Tanami Group|70478|6|Mentioned|p2 Fig 1, 6,10-12|||Geological Province: Tanami.|||Includes unnamed dolerite, Killi Killi Formation and Dead Bullock Formation.||Metasedimentary rocks.|
17763|Tanami Group|70826|6|Mentioned|p6 tbl 2, p9|Paleoproterozoic|Paleoproterozoic|Tanami Basin, ?Aileron Province.||||||21-APR-20
17763|Tanami Group|70848|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region. Undivided: cross-section only; see constituents for further details.|||Dead Bullock, Killi Killi Formations.|Is overlain unconformably by Birrindudu Group.||
17763|Tanami Group|70852|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region.|||Dead Bullock, Killi Killi Formations.|||
17763|Tanami Group|71267|4|Described|GEOL_LUT_CSV files|||Geological province: Granites-Tanami Orogen. Events: Alice Springs Orogeny (450-295 Ma); Stafford Event (1810-1790 Ma); Tanami Event (1850-1830 Ma). See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|||Includes Killi Killi Formation, Stubbins Formation.||Metamorphosed siliciclastic sedimentary rock and volcanic rocks|
17763|Tanami Group|71349|5|Briefly described|p725|||Crispe et al. (2007).|||Dead Bullock, Killi Killi Formations.|Unconformably overlies Browns Range Metamorphics. Is overlain unconformably by the Ware Group (inferred: contact not exposed). Is intruded by Birthday, Frederick and Grimwade Suites.||
17763|Tanami Group|71397|5|Briefly described|p5,46-47|Orosirian|Orosirian|Geological province: Granites-Tanami Orogen. Broadly a deep-marine succession, dominantly turbiditic (Crispe et al., 2007; Lambeck et al., 2008, 2012; Bagas et al., 2014).|||Includes Killi Killi Formation, Stubbins Formation, Dead Bullock Formation.|Overlain unconformably by Ware Group.||
17763|Tanami Group|71592|5|Briefly described|Appendix A.|||Tanami Orogen.|1800+/-14 Ma (crystallisation: U-Pb zircon SHRIMP)||||Rhyolite.|
17763|Tanami Group|72034|6|Mentioned|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes Killi Killi Formation, Stubbins Formation.|||
17763|Tanami Group|73083|6|Mentioned|p23|||Tanami Orogen.|||||Includes metamorphosed rocks.|
17763|Tanami Group|73089|4|Described|p: 1, 3, 5, 7-11, 22-31, 37, 39, 41-44|Paleoproterozoic|Paleoproterozoic|Archean detritus dominates the lower part of the succession, and c. 1865 Ma detritus with a minor c. 2500 Ma component dominates the upper part. Probably also contains Mount Charles Formation. Intruded by granitic rocks. Includes deformation that pre-dates Ware Group. Pre-dates the Stafford Event and are of relatively low metamorphic grade, except near contacts with granitic rocks. Comparable to the Halls Creek Group in terms of lithostratigraphy, changes in provenance and thickness.|||Dead Bullock Formation (Ferdies Member, Callie Member), Killi Killi Formation (NT)|Underlain by Billabong Complex. Unconformably overlain by Ware Group.|Dominantly siliciclastic metasedimentary rocks and lesser chemical metasedimentary and volcanic rocks metamorphosed under greenschist to locally amphibolite facies conditions.|
17763|Tanami Group|73158|5|Briefly described|p2-3, p6 Fig.5, p9-11|Orosirian||Granites-Tanami Orogen. Intruded by multiple generations of dolerite dykes and sills. MacFarlane Peak Group was integrated into the Tanami Group by Ahmed et al., (2013).|>1840 Ma||Dead Bullock Formation, Killi Killi Formation, Stubbins Formation, Mount Charles Formation.||Magmatic and sedimentary rocks. Lower-greenschist metamorphic facies.|
17763|Tanami Group|73159|5|Briefly described|p2-3, p6 Fig.5, p9-11|Palaeoproterozoic|Palaeoproterozoic|Granites-Tanami Orogen. Hosts orogenic gold mineralisation. Intruded by multiple generations of  dolerite dykes and sills.|>1840 Ma.||Dead Bullock, Stubbins, Killi Killi, Mount Charles Formations.|Overlies MacFarlane Peak Group.|Magmatic and sedimentary rocks. Lower greenschist-facies metamorphism.|
17793|Tanmurra Formation|7142|6|Mentioned|p350 Fig.4.|Early Carboniferous|Early Carboniferous|Browse Basin.||||Overlies Milligans Formation. Is overlain by Point Spring Sandstone.||
17793|Tanmurra Formation|12466|5|Briefly described|p177 Fig.10.|||||||Is overlain by Point Spring Sandstone.||03-SEP-14
17793|Tanmurra Formation|13194|4|Described|p389 Tb. 4-16|Upper Carboniferous|Visean|Type Section: Bonaparte 1 well (194-497m). 100-465m thick deltaic to marine shelf deposits.||Weaber Group||Overlies Milligans Formation (conformably), Bonaparte Formation (unconformably). Part equivalent to Point Spring Sandstone and part equivalent to Burvill Formation.|Calcarenite, dolomite, oolite, sandstone, siltstone, and mudstone.|
17793|Tanmurra Formation|13234|6|Mentioned|p250,252 Figs.2,4; p254; p262 Tb.2 |Early Carboniferous|Early Carboniferous|Encouraging test results for oil fluid and filtrate. Potential reservoir and seal.|||||Includes limestones.|
17793|Tanmurra Formation|13354|6|Mentioned|p375 Fig.6.|Early Carboniferous|Early Carboniferous|Overlies Milligans Formation and underlies Point Spring Sandstone.||66||||28-OCT-14
17793|Tanmurra Formation|14228|6|Mentioned|p6 fig3|Visean|Visean|||||Overlies Millgans Formation||
17793|Tanmurra Formation|22663|5|Briefly described|W97 8 to 10 p2 Fig.3||Carboniferous|||||||01-MAR-10
17793|Tanmurra Formation|23377|6|Mentioned|p212 Fig.5||Mississippian|In the Vulcan Sub-basin.||||||05-DEC-06
17793|Tanmurra Formation|23820|5|Briefly described|p203|Early Carboniferous|Early Carboniferous|Geological Province: Bonaparte Gulf Basin.||||||
17793|Tanmurra Formation|24378|6|Mentioned|p15|||Geological Province: Bonaparte Basin.||||||
17793|Tanmurra Formation|24390|5|Briefly described|p2 Fig. 2|Carboniferous|Carboniferous|Geological Province: Bonaparte Basin.||||||
17793|Tanmurra Formation|24569|5|Briefly described|p248 Fig. 3|Namurian|Visean|Of the Weaber Group. Geological Province: Petrel Sub-basin.||||||02-MAR-05
17793|Tanmurra Formation|30550|6|Mentioned|Fig.7|||Lower Carboniferous age||||||
17793|Tanmurra Formation|32307|6|Mentioned|p10|||L.Carboniferous||||||
17793|Tanmurra Formation|32662|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
17793|Tanmurra Formation|32663|4|Described|Table 2|||L.Carb.||||||
17793|Tanmurra Formation|32664|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|Briefly described in notes||||||
17793|Tanmurra Formation|32870|5|Briefly described|p48|||||||||
17793|Tanmurra Formation|33621|6|Mentioned|Table 1|||Fossil Shells.||||||
17793|Tanmurra Formation|34085|6|Mentioned|Cor.chart|||Visean - Namurian||||||
17793|Tanmurra Formation|36890|3|Fully described|p381|||||||||
17793|Tanmurra Formation|36904|6|Mentioned|p9|||||||||
17793|Tanmurra Formation|40993|6|Mentioned|Fig.1|||||||||
17793|Tanmurra Formation|41459|6|Mentioned|Fig.2|||||||||
17793|Tanmurra Formation|41532|5|Briefly described|p292|||||||||
17793|Tanmurra Formation|41690|5|Briefly described|p5|||||||||
17793|Tanmurra Formation|41731|5|Briefly described|p573|||See also p519 and Fig.3.||||||05-DEC-06
17793|Tanmurra Formation|41839|4|Described|p32|||||||||
17793|Tanmurra Formation|41864|3|Fully described|p132|||||||||
17793|Tanmurra Formation|41865|5|Briefly described|Map legend|early Namurian|late Visean|||||||
17793|Tanmurra Formation|42055|4|Described|Fig.1 P52|||||||||
17793|Tanmurra Formation|42056|6|Mentioned|p96|||||||||
17793|Tanmurra Formation|42442|3|Fully described|p13|Namurian early|Visean late|||||||
17793|Tanmurra Formation|42547|4|Described|p104|||||||||
17793|Tanmurra Formation|42564|6|Mentioned|p47|||||||||
17793|Tanmurra Formation|43661|6|Mentioned|Fig.3|||||||||
17793|Tanmurra Formation|44159|6|Mentioned|Table p.38||Early Carboniferous|||||||
17793|Tanmurra Formation|45038|14|Not recorded|p119|||||||||
17793|Tanmurra Formation|45039|6|Mentioned|p6|||||||||
17793|Tanmurra Formation|45050|6|Mentioned|p57|||||||||
17793|Tanmurra Formation|45056|4|Described|p7|||U.Visean||||||
17793|Tanmurra Formation|45063|6|Mentioned|p8|Early Carboniferous|Early Carboniferous|See also pp22, 27 and Fig. 3.||||||05-DEC-06
17793|Tanmurra Formation|45097|6|Mentioned|p20|||See also correlation chart||||||
17793|Tanmurra Formation|45155|6|Mentioned|p42|||||||||
17793|Tanmurra Formation|45169|4|Described|p7|||||||||
17793|Tanmurra Formation|46849|6|Mentioned|p180|||||||||
17793|Tanmurra Formation|48635|14|Not recorded|Not recorded|||||||||
17793|Tanmurra Formation|48886|14|Not recorded|Not recorded|||||||||
17793|Tanmurra Formation|49637|5|Briefly described|Fig. 6|Late Carboniferous|Early Carboniferous|Geological Province: Bonaparte Basin.||||||07-FEB-11
17793|Tanmurra Formation|50085|5|Briefly described|p2 Fig. 2|Carboniferous|Carboniferous|Geological Province: Bonaparte Basin.||||||
17793|Tanmurra Formation|60006|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Geological Province: Bonaparte Basin. Of  Weaber Group. Overlies Milligans Formation. Overlain by Border Creek Member and unconformably overlain by Kuriyippi Formation.||||||
17793|Tanmurra Formation|60364|5|Briefly described|p190, p196|Namurian|Visean|Thickness: 301m. Carbonates and calcareous and dolomitic sandstone. Ostracods described.||||||11-MAY-05
17793|Tanmurra Formation|60682|4|Described|p22 Table. 5, p25|Namurian|Visean|Of Weaber Group. Conformably overlies Milligans Formation. May be equivalent to Point Spring Sandstone and/or Burvill Formation. Thickness: <260m. Sandstone, limestone and dolostone. Geological Province: Bonaparte Basin.||||||
17793|Tanmurra Formation|60701|5|Briefly described|p13|Early Carboniferous|Early Carboniferous|Consists of sandy limestones and calcareous sandstones; good oil shows recorded.  Geological Province: Bonaparte Basin.||||||
17793|Tanmurra Formation|61023|5|Briefly described|p2 Fig. 2|Carboniferous|Carboniferous|Geological Province: Bonaparte Basin.||||||10-APR-08
17793|Tanmurra Formation|61542|1|Redefined|p276, p277 Fig. 2, p285|Visean|Visean|Of Weaber Group. Mory's original shelf carbonates unit (1991) is redefined with the upper 26m placed separately in the Sunbird Formation. Unconformable on Kingfisher Shale. Geol.prov: Bonapart Basin/Petrel-Sub-basin.Calcareous and dolomitic sandstone.||||||07-FEB-11
17793|Tanmurra Formation|62837|5|Briefly described|Stratigraphic columns|Namurian|Visean|Of the Weaber Group.  Age: ~328-~322Ma. Geological Province:  Petrel Sub-basin (offshore).||||||01-MAR-10
17793|Tanmurra Formation|64580|6|Mentioned|map legend|||Of Weaber Group.||||||15-DEC-08
17793|Tanmurra Formation|64694|5|Briefly described|p234, p235, p238 Tb.1, p242 Tb.4, p244|Serpukhovian|Visean|See also p245 Fig.9, p249. Onshore Bonaparte Basin.||Unit in Weaber Group.||Overlies Bonaparte Formation and Upper Milligans Formation unconformably. Is overlain by Point Spring Sandstone or Kulshill Group.||
17793|Tanmurra Formation|65331|6|Mentioned|cross-section only|||?Of Weaber Group.?Carboniferous. Based on colour used. Shown only as subsurface on cross-section||||||
17793|Tanmurra Formation|65342|5|Briefly described|p14. |||Bonaparte Basin. Max. thickness at least 276 m.||||Overlies Milligan Formation. Is overlain by Kulshill Formation.|Sandy limestone, calcareous sandstone.|
17793|Tanmurra Formation|65382|6|Mentioned|p717 App. 2|Namurian|Visean|Bonaparte Basin. 327 Ma.||||||
17793|Tanmurra Formation|67195|5|Briefly described|Appendix 2|||Bonaparte Basin.|||||Includes grey siltstone.|
17793|Tanmurra Formation|67200|6|Mentioned|app 2 p8||||||||Siltstone.|
17793|Tanmurra Formation|69099|5|Briefly described|500k_geologyp08_lut.csv|Pennsylvanian|Mississippian|||Weaber Group||||
17793|Tanmurra Formation|69165|6|Mentioned|500k_geologyp08_lut.csv|Pennsylvanian|Mississippian|||Weaber Group||||
17793|Tanmurra Formation|69451|6|Mentioned|p35:9|||Bonaparte Basin. Previously (Petroconsultants, 1989) correlated with part of the Kulshill Group equivalent rocks in the Arafura Basin.||||||12-JUL-16
17793|Tanmurra Formation|69452|3|Fully described|p36:9, 11-12, 14-17|Early Carboniferous|Early Carboniferous|Caye (1968). Equivalent to Medusa Beds of Kemp et al. (1977). Petrel Sub-basin, Bonaparte Basin. The type section is in Bonaparte-1 where it is 277m thick. Transgressive, delta to shallow marine shelf deposits. Offshore and onshore (subsurface). Late Visean.||Weaber Group.||Unconformably overlies Kingfisher Shale and Burvill Formation. Is overlain unconformably by Sandbar and Point Spring Sandstones, Arco and Sunbird Formations.|Calcareous and dolomitic sandstone with minor limestone, siltstone and shale.|12-JUL-16
17793|Tanmurra Formation|69634|5|Briefly described|500k_geologyp08_lut.csv|Carboniferous|Carboniferous|||Unit of Weaber Group.||||
17793|Tanmurra Formation|69653|6|Mentioned|p10|Carboniferous|Carboniferous|Petrel Sub-basin.||Weaber Group.||Overlies Kingfisher Shale. Is overlain by Sandbar Sandstone.||
17793|Tanmurra Formation|69673|5|Briefly described|p168 fig 138, p171, p172, p181|Carboniferous|Carboniferous|277m thick.||Weaber Group||Overlies Kingfisher Shale, overlain by Kuriyippi Formation, Point Spring Sandstone|Calcareous and dolomitic sandstone with minor limestone, siltstone and shale.|
17793|Tanmurra Formation|70061|5|Briefly described|Petrel Sub-basin; Fig.3, p2-3|Visean|Visean|See also Regional geology: Fig.8, p9, p11-12. Includes hydrocarbon source and reservoir rocks.||Weaber Group.||Overlies Kingfisher Shale. Is overlain by Sandbar Sandstone.|Includes anoxic marine mudstones.|12-JUL-16
17793|Tanmurra Formation|70206|5|Briefly described|cross-section only|Carboniferous|Carboniferous|Age implied by surrounding units.||Weaber Group||||
17793|Tanmurra Formation|73117|6|Mentioned|p11, p15|Visean|Visean|Bonaparte Basin, southern.||Weaber Group||Underlain by Kingfisher Shale and Burvill Formation. Overlain by Sunbird Formation and Sandbar Sandstone.||
17800|Tanumbirini Rhyolite|22538|6|Mentioned|P714||Statherian|Age of unit is 1713+/-7 Ma.||||||05-DEC-06
17800|Tanumbirini Rhyolite|22665|6|Mentioned|P231||Statherian|Age of unit is 1713+/-7 Ma.||||||05-DEC-06
17800|Tanumbirini Rhyolite|22853|4|Described|14|Proterozoic|Proterozoic|Geological province: McArthur Basin. Of the Tawallah Group. Max thickness: 100 m. Overlain by Masterton Sandstone; underlain by Warramana Sandstone||||||05-DEC-06
17800|Tanumbirini Rhyolite|23363|5|Briefly described|352 Tab.3|Statherian|Statherian|Age: 1713+/-7Ma.||||||05-DEC-06
17800|Tanumbirini Rhyolite|23395|6|Mentioned|p401|||||||||
17800|Tanumbirini Rhyolite|23396|5|Briefly described|p407 Fig.2|Statherian|Statherian|Of the Tawallah Group. Age: 1713+/-7Ma.||||||05-DEC-06
17800|Tanumbirini Rhyolite|23398|4|Described|p440|Statherian|Statherian|Age: 1713+/-7Ma.||||||05-DEC-06
17800|Tanumbirini Rhyolite|23733|5|Briefly described|p32 Fig. 19|||||||||
17800|Tanumbirini Rhyolite|23776|5|Briefly described|p705 Fig 2.|Statherian|Statherian|Age: 1713+/-7 Ma. Of the Tawallah Group.||||||05-DEC-06
17800|Tanumbirini Rhyolite|23910|4|Described|p290|Paleoproterozoic|Paleoproterozoic|Age: 1713+/-7Ma.  Geological Province: McArthur Basin.||||||07-NOV-08
17800|Tanumbirini Rhyolite|23963|5|Briefly described|p1238, 1239 Fig.2|Paleoproterozoic|Paleoproterozoic|Geological Province: McArthur Basin. Age: 1725+/-40 Ma. Of the Tawallah Group||||||07-NOV-08
17800|Tanumbirini Rhyolite|24048|6|Mentioned|p36|||Geological Province: McArthur Basin.||||||
17800|Tanumbirini Rhyolite|24050|5|Briefly described|p27|||Of the Tawallah Group.  Geological Province: McArthur Basin.||||||05-DEC-06
17800|Tanumbirini Rhyolite|24179|5|Briefly described|p84 Fig. 2|Paleoproterozoic|Paleoproterozoic|Overlies the Gold Creek Volcanics.  Age: 1713 +/- 7 Ma.  Geological Province:  McArthur Basin.||||||07-NOV-08
17800|Tanumbirini Rhyolite|24197|5|Briefly described|p56 Tb. 3.1|Paleoproterozoic|Paleoproterozoic|Of the Fagan Suite. Age: ~1710Ma.||||||07-FEB-11
17800|Tanumbirini Rhyolite|42385|4|Described|p14, p9 Tb. 3|Paleoproterozoic|Paleoproterozoic|Variation of Tanumbirini Volcanic Member? Conformably overlies Warramana Sandstone; unconformably overlain by Masterton Sandstone. Thickness: ~100m. Very uniform massive, pink-brown, deeply weathered, porphyritic rhyolite, with phenocrysts of quartz and f||||||07-NOV-08
17800|Tanumbirini Rhyolite|42386|5|Briefly described|Map legend|Mesoproterozoic||Age: 1725 +/- 40 Ma.||||||05-DEC-06
17800|Tanumbirini Rhyolite|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.|1725 +/- 40.|Of Tawallah Group.||Not shown in schematic sections.|Porphyritic rhyolite lava. Detailed lithology given.|09-NOV-11
17800|Tanumbirini Rhyolite|42639|4|Described|p17, Table 4 p11|||Age: 1725 +/- 40Ma  U-Pb zircon age||||||
17800|Tanumbirini Rhyolite|42700|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
17800|Tanumbirini Rhyolite|42739|5|Briefly described|map legend|Statherian|Statherian|Of the Tawallah Group. Porphyritic rhyolite lava with phenocrysts of quartz and feldspar set in sperulitic groundmass.||||||19-OCT-05
17800|Tanumbirini Rhyolite|42812|3|Fully described|p27, Table 3|||Of the Tawallah Group.||||||05-DEC-06
17800|Tanumbirini Rhyolite|42873|5|Briefly described|Fig.1, P110|||||||||
17800|Tanumbirini Rhyolite|43036|3|Fully described|p36|||Of the Tawallah Group. Age of 1713 +/- 6 Ma.||||||05-DEC-06
17800|Tanumbirini Rhyolite|44112|6|Mentioned|p43|||||||||
17800|Tanumbirini 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: 1713 +/- 7Ma (Shrimp).||||||07-NOV-08
17800|Tanumbirini Rhyolite|60483|5|Briefly described|p7 Fig. 5, p29|Paleoproterozoic|Paleoproterozoic|Of the Tawallah Group. Age: 1713+/-7Ma. Geological Province: McArthur Basin.||||||07-NOV-08
17800|Tanumbirini Rhyolite|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Tawallah Group. Underlain by Warramana Sandstone.||||||03-JUN-09
17800|Tanumbirini Rhyolite|63112|6|Mentioned|p1192 Tb.1|||Calvert Superbasin.|1713 +/- 7 Ma.|Unit in Big Supersequence.|||Massive porphyritic rhyolite.|
17800|Tanumbirini Rhyolite|63866|5|Briefly described|p54|Statherian|Statherian||1713 +/- 7 Ma|Prize Supersequence||||
17800|Tanumbirini Rhyolite|64815|6|Mentioned|p4 Fig.2, p5 Fig.3, p16|||Often missing in stratigraphic successions.||Of the Tawallah Group.||||
17800|Tanumbirini Rhyolite|64817|6|Mentioned|p353 Fig.4, p355 Fig.5 |Statherian|Statherian||1713 +/- 7 Ma.|Of the Tawallah Group||||
17800|Tanumbirini Rhyolite|65228|5|Briefly described|p22, p23, Figs.02, 04, 05, 07, 10.|Statherian|Statherian|Associated with Nyanantu Formation epiclastics.|1713 +/- 7 Ma.|Unit in Tawallah Group.||Overlies Warramana Sandstone. Is overlain conformably by Burash Sandstone.||
17800|Tanumbirini Rhyolite|65337|6|Mentioned|p15.|||Southern McArthur Basin.||||||
17800|Tanumbirini Rhyolite|65340|5|Briefly described|pp11-12, p53 Fig.51. |||Correlated with part of Echo Sandstone.|1713 +/- 7 Ma (Page and Sweet 1998).|Unit in Tawallah Group.||Unconformably overlies Warramana Sandstone. Is overlain by Nyanantu Formation.||
17800|Tanumbirini Rhyolite|69430|4|Described|p15:3, 9-10, 12-13|||Southern McArthur Basin. Subaerial lava flows and domes. 100m thick. U-Pb zircon age.|1713 +/- 7 Ma (Page et al., 2000).|Tawallah Group.||Conformably overlies Warramana Sandstone. Is conformably or disconformably overlain by, and is interbedded with, Nyanantu Formation.|Massive, pink-brown weathered porphyritic rhyolite lava with phenocrysts of quartz and feldspar set in a spherulitic groundmass.|12-JUL-16
17800|Tanumbirini Rhyolite|69673|5|Briefly described|p16 fig 13, p17 fig 14|||||Tawallah Group||Overlain by Nyanantu Formation, overlies Warramana Sandstone|Rhyolite.|
17800|Tanumbirini Rhyolite|71374|5|Briefly described|p6|||McArthur Basin. Age derived from Page and Sweet, 1998.|1713 +/- 7 Ma (SHRIMP)|||||
17800|Tanumbirini Rhyolite|71592|5|Briefly described|Appendix A.|||McArthur Basin.|1713+/-7 Ma (crystallisation: U-Pb zircon SHRIMP)||||Rhyolite.|
17800|Tanumbirini Rhyolite|71606|5|Briefly described|p135,137|Statherian|Statherian|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.||
17800|Tanumbirini Rhyolite|72377|5|Briefly described|p12|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. Page et al (2000) reported SHRIMP U-Pb zircon age of 1712+\-6 Ma, interpreted as magmatic crystallisation age, which is within uncertainty with the magmatic crystallisation age of the Haddon Volcanics (1712+\-12 Ma; this record).|1712+\-6 Ma (magmatic)|||||
17800|Tanumbirini Rhyolite|72718|6|Mentioned|p6-7|Statherian|Statherian|Southern McArthur Basin. Redbank package (near the top). Provides age constraint near top of Redbank package.|1713 +/- 7 Ma SHRIMP U-Pb|Tawallah Group||Underlain by Warramana Sandstone. Overlain by and equivalent to Nyanantu Formation. Equivalent to Echo Sandstone.||
17800|Tanumbirini Rhyolite|73412|5|Briefly described|p2, 4, 8|||Southern McArthur Basin. Is mis-spelt as Tanunbirini Rhyolite on p4.|1713 +/- 7 Ma.|||Overlies Warramana Sandstone. Is overlain by Nyanantu Formation.||
17868|Tarrara Formation|13194|4|Described|p395 Tb. 4-16; p382, 399 figs 4-59,-63|Middle Cambrian|Early Cambrian|Type Section: Tarrara Bar 15o04'S 128o41'E. 60-400m thick shallow marine deposits. Includes Blatchford Formation"" (in part).||Unit in Carlton Group.||Overlies Antrim Plateau Volcanics (conformably). Overlain by Hart Spring Sandstone (conformably). Equivalent to Negri Subgroup (Ord Basin).|Siltstone; minor sandstone and limestone.|
17868|Tarrara Formation|14228|5|Briefly described|p6 fig3|Cambrian|Cambrian|Southern Bonaparte Basin.||||Overlain by Hart Spring Sandstone.||06-OCT-16
17868|Tarrara Formation|24390|5|Briefly described|p2 Fig. 2|Cambrian|Cambrian|Geological Province: Bonaparte Basin. Of the Carlton Group.||||||
17868|Tarrara Formation|32648|6|Mentioned|p32|||M.Camb.||||||
17868|Tarrara Formation|32664|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|Briefly described in notes.||||||11-DEC-06
17868|Tarrara Formation|32870|6|Mentioned|Fig.6|||Refers Kaulback and Veevers (1969).||||||11-DEC-06
17868|Tarrara Formation|36257|6|Mentioned|Table 2.1|||||||||
17868|Tarrara Formation|36551|6|Mentioned|Table 16|||||||||
17868|Tarrara Formation|36890|3|Fully described|p374|||||||||
17868|Tarrara Formation|40993|6|Mentioned|Fig.1|||||||||
17868|Tarrara Formation|41459|6|Mentioned|Fig.2|||||||||
17868|Tarrara Formation|41690|5|Briefly described|p3|||||||||
17868|Tarrara Formation|41731|6|Mentioned|Fig.3|||||||||
17868|Tarrara Formation|41864|3|Fully described|p30|||||||||
17868|Tarrara Formation|41865|5|Briefly described|Map Legend|Middle Cambrian||||||||
17868|Tarrara Formation|43661|6|Mentioned|Fig.3|||||||||
17868|Tarrara Formation|44230|5|Briefly described|Map Legend||Middle Cambrian|||||||
17868|Tarrara Formation|45038|14|Not recorded|Fig 21,23,36||Cambrian|||||||
17868|Tarrara Formation|45058|6|Mentioned|Fig. 3|||See also Fig. 4. Mid.Cambrian||||||
17868|Tarrara Formation|48886|2|Defined|p.36||Middle Cambrian|See also Figs and App.2, p.61. Middle Cambrian.||||||11-DEC-06
17868|Tarrara Formation|50085|5|Briefly described|p2 Fig. 2|Cambrian|Early Cambrian|Of the Carlton Group. Geological Province: Bonaparte Basin.||||||15-DEC-08
17868|Tarrara Formation|61023|5|Briefly described|p2 Fig. 2|Cambrian|Cambrian|Of the Carlton Group. Geological Province: Bonaparte Basin.||||||11-APR-08
17868|Tarrara Formation|64443|6|Mentioned|p40.|||Of Bonaparte Basin. Correlative of Barkly Group, Georgina Basin.||||||
17868|Tarrara Formation|64580|6|Mentioned|map legend|||Of Carlton Group.||||||15-DEC-08
17868|Tarrara Formation|65337|5|Briefly described|p94.|Middle Cambrian|Middle Cambrian|Bonaparte Basin. Carbonates.||||Unconformably overlies Kalkarindji Volcanic Group.||
17868|Tarrara Formation|67860|6|Mentioned|p419 Tb. 4-18|||Of Bonaparte Basin.||||||
17868|Tarrara Formation|69099|5|Briefly described|500k_geologyp08_lut.csv|Early Ordovician|Middle Cambrian|||Carlton Group||||
17868|Tarrara Formation|69165|6|Mentioned|500k_geologyp08_lut.csv|Early Ordovician|Middle Cambrian|||Carlton Group||||
17868|Tarrara Formation|69437|5|Briefly described|p22:10-11|Series 2|Series 2|Carlton Sub-basin, Bonaparte Basin, Centralian B Superbasin. Sequence 1.||Carlton Group.||Is overlain by Hart Spring Sandstone. Equivalent to Gum Ridge, Border Waterhole, Chandler Formations; Thorntonia, Tindall, Top Springs Limestones; Walbiri, Giles Creek Dolostones.||12-JUL-16
17868|Tarrara Formation|69443|6|Mentioned|p28:21|||Bonaparte Basin.||||Correlated with Barkly Group.||12-JUL-16
17868|Tarrara Formation|69445|5|Briefly described|p30:17|Middle Cambrian|Middle Cambrian|Bonaparte Basin.||||Unconformably overlies Kalkarindji Suite.||12-JUL-16
17868|Tarrara Formation|69448|6|Mentioned|p33:3|||Bonaparte Basin.||Carlton Group.||Correlated with Negri Subgroup (Ord Basin).||12-JUL-16
17868|Tarrara Formation|69452|5|Briefly described|p36:5|Stage 5|Stage 4|Carlton Sub-basin, SW Bonaparte Basin.||Carlton Group.||Unconformably overlies Antrim Plateau Volcanics. Is overlain conformably by Hart Spring Sandstone.||12-JUL-16
17868|Tarrara Formation|69634|5|Briefly described|500k_geologyp08_lut.csv|||||Unit of Carlton Group.||||
17868|Tarrara Formation|69673|6|Mentioned|p168 fig 139|Cambrian|Cambrian|||Carlton Group||Overlies Antrim Plateau Volcanics, overlain by Hart Spring Sandstone||
17896|Tatoola Sandstone|22453|5|Briefly described|p 11  Fig 10|||||||||
17896|Tatoola Sandstone|22538|6|Mentioned|Fig3 P709|||||||||
17896|Tatoola Sandstone|22664|6|Mentioned|35,47|Paleoproterozoic|Paleoproterozoic|Umbolooga Subgroup. In the McArthur Basin.||||||07-NOV-08
17896|Tatoola Sandstone|22853|3|Fully described|18|Proterozoic|Proterozoic|Of the Umbolooga Subgroup. Max thickness 200 m. Overlain by Tooganinie Formation; underlain by Amelia Dolomite||||||11-DEC-06
17896|Tatoola Sandstone|23387|6|Mentioned|p18 fig.19|||Of Umbolooga Subgroup.||||||
17896|Tatoola Sandstone|23396|5|Briefly described|p407 Fig.2|Statherian|Statherian|Of McArthur Group. 1650+/-3Ma.||||||11-DEC-06
17896|Tatoola Sandstone|23397|5|Briefly described|p471|Statherian|Statherian|Age: 1648+/-3Ma.||||||11-DEC-06
17896|Tatoola Sandstone|23398|4|Described|p442|Statherian|Statherian|U/Pb SHRIMP age: 1648+/-3Ma. Dark siliceous bed near base. Possible tuffaceous interval. Pristine magmatic zircon population.||||||09-SEP-14
17896|Tatoola Sandstone|23776|5|Briefly described|p705 Fig 2, 707 Fig 4.|Statherian|Statherian|Age: 1650+/-3 Ma. Of Umbolooga Subgroup.||||||05-APR-18
17896|Tatoola Sandstone|23902|4|Described|p1568 Fig.2|||Of the Umbolooga Subgroup. Overlain by the Tooganinie Formation. Overlies the Amelia Dolomite. Geological Province: McArthur Basin||||||
17896|Tatoola Sandstone|23910|5|Briefly described|p292 Fig. 3|||Of Umbolooga Subgroup.  Geological Province: McArthur Basin.||||||
17896|Tatoola Sandstone|23963|5|Briefly described|p1239 Fig.2|||Geological Province: McArthur Basin. Of the Umbolooga Subgroup||||||03-MAR-05
17896|Tatoola Sandstone|24048|6|Mentioned|p55|||Of the Umbolooga Subgroup.||||||11-DEC-06
17896|Tatoola Sandstone|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Of Umbolooga Subgroup. Overlain by Tooganinie Formation. Geological Province: Southern McArthur Basin.||||||
17896|Tatoola Sandstone|30272|6|Mentioned|p5|||On stratigraphic table.||||||
17896|Tatoola Sandstone|30344|6|Mentioned|Fig.4|||Part of Umbolooga Subgroup||||||
17896|Tatoola Sandstone|30345|6|Mentioned|Table 1|||Carpentarian age. Lithology||||||
17896|Tatoola Sandstone|32363|5|Briefly described|Table 1|||||||||
17896|Tatoola Sandstone|32479|6|Mentioned|Fig.2|||||||||
17896|Tatoola Sandstone|32658|3|Fully described|Table 2|||See also Fig.3||||||
17896|Tatoola Sandstone|32660|5|Briefly described|Table 4|||||||||
17896|Tatoola Sandstone|33665|6|Mentioned|Fig.2|||||||||
17896|Tatoola Sandstone|33666|6|Mentioned|Table 1|||||||||
17896|Tatoola Sandstone|35162|6|Mentioned|Table.1|||||||||
17896|Tatoola Sandstone|35261|6|Mentioned|Fig.2|||||||||
17896|Tatoola Sandstone|37568|5|Briefly described|p79|||||||||
17896|Tatoola Sandstone|38582|6|Mentioned|Fig.3|||||||||
17896|Tatoola Sandstone|39561|6|Mentioned|Fig.5|||||||||
17896|Tatoola Sandstone|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
17896|Tatoola Sandstone|40259|6|Mentioned|Table 1|||||||||
17896|Tatoola Sandstone|40691|4|Described|p47|||Mention Fig.4||||||
17896|Tatoola Sandstone|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
17896|Tatoola Sandstone|41220|6|Mentioned|Fig.3|||||||||
17896|Tatoola Sandstone|41268|5|Briefly described|Fig.3|||||||||
17896|Tatoola Sandstone|41277|6|Mentioned|Fig.2|||||||||
17896|Tatoola Sandstone|41406|6|Mentioned|Map legend|Mesoproterozoic||||||||
17896|Tatoola Sandstone|42385|4|Described|p18|||See also Table 4 p17.||||||11-DEC-06
17896|Tatoola Sandstone|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
17896|Tatoola Sandstone|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.||Of Umbolooga Subgroup (McArthur Group).||In schematic section, underlies Tooganinie Formation; overlies Amelia Dolomite.|Vuggy sandstone, commonly dolomitic and lithic. Detailed lithology given.|09-NOV-11
17896|Tatoola Sandstone|42639|4|Described|p23, Table 5 p21|||||||||
17896|Tatoola Sandstone|42700|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
17896|Tatoola Sandstone|42739|5|Briefly described|map legend|Statherian|Statherian|Of the Umbolooga Subgroup. Dominatly white flaggy fine-grained sandstone and lesser mudstone, in places dolomitic.||||||19-OCT-05
17896|Tatoola Sandstone|42812|3|Fully described|p35, Table 4|||Of Umbolooga Subgroup.||||||11-DEC-06
17896|Tatoola Sandstone|42935|6|Mentioned|p529 Fig.2|||of Umbolooga Subgroup||||||
17896|Tatoola Sandstone|43010|5|Briefly described|Fig.6||Mesoproterozoic|of "Mid Proterozoic" age.||||||
17896|Tatoola Sandstone|43036|3|Fully described|p47|||of Umbolooga Subgroup||||||
17896|Tatoola Sandstone|43486|5|Briefly described|21|||||||||
17896|Tatoola Sandstone|44112|6|Mentioned|p55|||||||||
17896|Tatoola Sandstone|44287|14|Not recorded|p.9,10, opp.9|||(E53-3).||||||
17896|Tatoola Sandstone|44288|14|Not recorded|map legend|||Quartz sandstone, dolomitic sandstone, feldspathic sandstone. Lower (?) Proterozoic.||||||
17896|Tatoola Sandstone|44473|2|Defined|p.8,9, opp. p.7|||(E53-7). Basal formation of Bauhinia Downs Subgroup (backreef seds. in McArthur Group).||||||
17896|Tatoola Sandstone|44474|14|Not recorded|map legend|||Lower (?) Proterozoic.||||||
17896|Tatoola Sandstone|44530|14|Not recorded|p.10, opp.10|||(D53-15).||||||
17896|Tatoola Sandstone|44531|14|Not recorded|map legend|||Lower (?) Proterozoic.||||||
17896|Tatoola Sandstone|45162|1|Redefined|p72|Proterozoic|Proterozoic|Mention p127.||||||11-DEC-06
17896|Tatoola Sandstone|46915|6|Mentioned| Fig.1|||Stratigraphic section through McArthur Group.||||||
17896|Tatoola Sandstone|46955|6|Mentioned|p159|||||||||
17896|Tatoola Sandstone|46968|6|Mentioned|Fig.2|||||||||
17896|Tatoola Sandstone|50224|6|Mentioned|p380 Fig. 6|||||||||07-FEB-11
17896|Tatoola Sandstone|60483|5|Briefly described|p7 Fig. 5, p8|Paleoproterozoic|Paleoproterozoic|Of Umbolooga Subgroup (McArthur Group). Age: 1648+/-3Ma, 1650+/-3Ma. Geological Province: McArthur Basin.||||||07-NOV-08
17896|Tatoola Sandstone|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Umbolooga Subgroup. Overlian by Tooganinie Formation, underlian by Amelia Dolomite.||||||
17896|Tatoola Sandstone|62084|4|Described|p936 Fig.5|||Isa Superbasin. McArthur Basin. Shown as Tatoola Sst.|1648+/-3 Ma U-Pb SHRIMP (after Page et al. 2000)|McArthur Group|||Rift phase clastics.|
17896|Tatoola Sandstone|63112|6|Mentioned|p1191 Fig.2|||Isa Superbasin; southern McArthur Basin. Age approximated from Fig.2.|c.1650 Ma.|Unit in Loretta Supersequence.||||
17896|Tatoola Sandstone|63866|4|Described|p54|Statherian|Statherian|Isa Superbasin.|1648 +/- 3 Ma (Page et al., 2000)|Loretta Supersequence|||Tuffaceous siltstone, sandstone.|
17896|Tatoola Sandstone|64726|6|Mentioned|p86 Table 1.|||Sampled for paleomagnetic reconstruction of Australian and Laurentian Apparent Polar Wander Path.|1648 +/- 3 Ma.|||||
17896|Tatoola Sandstone|64748|6|Mentioned|p276 Fig. 9|Paleoproterozoic|Paleoproterozoic|Palaeomag results shown on polar wander path||||||
17896|Tatoola Sandstone|64815|6|Mentioned|p4 Fig.2, p5 Fig.3, p8 Tb.1, p17  |||||Of the Umbolooga Subgroup.||||
17896|Tatoola Sandstone|64817|6|Mentioned|p353 Fig.4 ||||1650 +/- 3 Ma.|Of the Umbolooga Subgroup.||||
17896|Tatoola Sandstone|65228|4|Described|p23,p26-27,p31,Table 1, Figs.02,04,11-12|Statherian|Statherian|About 600 m higher up than Tanumbirini Rhyolite (of Tawallah Group) aged c.1713 Ma, suggesting a long hiatus and/or erosion. Age from tuff in lower parts of the unit. Appears to thin northwards. Gamma ray log, lithology and facies detailed. Measured section.|1648 +/- 3 Ma.|Unit in Umbolooga Subgroup.||Gradationally overlies Amelia Dolomite. Is overlain by Tooganinie Formation.|Very fine-grained silty sandstone grading to mudstone, coarsening upward.|
17896|Tatoola Sandstone|67144|5|Briefly described|Map legend.|Statherian|Statherian|Ridge-forming.||Unit in Umbolooga Subgroup.||Overlies Amelia Dolostone. Is overlain by Tooganinie Formation.|Medium-grained vuggy sandstone, commonly dolomitic and lithic, cross-bedded and rippled with shale clasts and evaporite moulds and casts; thinly-bedded fine-grained white quartz sandstone; several recessive dolomitic units.|
17896|Tatoola Sandstone|67352|4|Described|p14 Tb.2, p58|Statherian|Statherian|McArthur Basin. 350 m thick. Hosted Yah Yah copper deposit at the contact with underlying Amelia Dolostone.||Umbolooga Subgroup||Overlies Amelia Dolostone (conformably). Overlain by Tooganinie Formation (conformably).|Upper: medium to coarse-grained sandstone: thinly to medium bedded; dolostone, quartzic dolostone. Lower: very fine- to fine-grained quartz sandstone: thinly bedded; shale, siltstone (locally dolomitic, tuffaceous); basal very fine-grained sandstone|
17896|Tatoola Sandstone|69430|4|Described|p15:3, 17, 34|Statherian|Statherian|Southern McArthur Basin. 80-350m thick. Changing up-sequence from clastic peritidal to mixed carbonate/siliciclastic subtidal beach to peritidal sediments.|1648 +/- 3 Ma.|Umbolooga Subgroup.||Conformably and gradationally overlies Amelia Dolostone. Is overlain conformably and gradationally by Tooganinie Formation.|Flaggy, thin-bedded, fine-grained sandstone, shale and siltstone (locally dolomitic), very fine sandstone at base, several recessive dolomitic units; medium-grained, thinly to medium bedded sandstone with shale clasts and evaporite casts/moulds.|12-JUL-16
17896|Tatoola Sandstone|69673|6|Mentioned|p16 fig 13|||Batten Fault Zone|1648 +/- 3 Ma|Umbolooga Subgroup||Overlies Amelia Dolostone, overlain by Tooganinie Formation||
17896|Tatoola Sandstone|70897|5|Briefly described|p43|Statherian|Statherian||c.1650 Ma.|McArthur Group.||Is overlain by Roper Group.||
17896|Tatoola Sandstone|71374|5|Briefly described|p6|||McArthur Basin. SHRIMP age is derived from an interbedded tuff in this unit.|1650 +/- 3 Ma (SHRIMP U-Pb)|||||
17896|Tatoola Sandstone|71592|5|Briefly described|Appendix A.|||McArthur Basin.|1648+/-3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Siltstone.|
17896|Tatoola Sandstone|71799|5|Briefly described|p150 fig 2|Statherian|Statherian|McArthur Basin.|ca. 1650 Ma|||Overlies the Amelia Dolomite.|Sandstone and greywacke.|
17896|Tatoola Sandstone|72248|6|Mentioned|p147|||Of McArthur Basin.||Unit of Umbolooga Subgroup.||||
17896|Tatoola Sandstone|72373|4|Described|iii,p1,5-8,11,14,17,20,24,27,30,34|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. Type section: 46 km SE of Cape Crawford in northeastern KILGOUR map sheet. Exposures restricted to Batten Fault Zone in southern McArthur Basin, from southern MOUNT YOUNG, through BAUHINIA DOWNS to northern WALHALLOW. Contains a tuffaceous rock dated at 1648+\-3 Ma (Page et al 2000). Sample 2709632 (WW16TJM025B: Fine-grained quartz-lithic sandstone; WALHALLOW) yielded interpreted max depositional age of 1671+\-3 Ma. Detrital zircon age spectra indicate significant change in provenance, or sediment pathways, between Tatoola Sandstone and overlying Tooganinie Formation.|1671+\-3 Ma (max dep age)|Unit of Umbolooga Subgroup.||Overlain conformably by Tooganinie Formation. Underlain conformably by Amelia Dolostone.|Light coloured, predominantly sandstone unit, mainly consisting of a lower, fine-grained, thinly bedded facies and an upper, medium- to coarse-grained, more thickly bedded sandstone and dolostone facies.|
17896|Tatoola Sandstone|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Batten Fault Zone of the Southern McArthur Basin. Age given as U-Pb zircon sedimentary depositional age.|1648 +/-3 Ma|Umbolooga Subgroup||Overlies Amelia Dolostone and underlies Leila Sandstone and Tooganinie Formation.||
17896|Tatoola Sandstone|72718|6|Mentioned|p7|||Southern McArthur Basin. Batten Fault Zone.||Umbolooga Sub-group, McArthur Group||Underlain by Amelia Dolostone. Overlain by Tooganinie Formation.||
17896|Tatoola Sandstone|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Batten Fault Zone of the Southern McArthur Basin. U-Pb zircon sedimentary depositional age (Ma).|1648+/-3 Ma|Umbolooga Subgroup||Overlies Amelia Dolostone and underlies Tooganinie Formation and Leila Sandstone.||
17896|Tatoola Sandstone|73042|6|Mentioned|p4|Statherian|Statherian|Southern McArthur Basin, Isa Superbasin. Geochronology is a U-Pb zircon sedimentary depositional age (?maximum depositional age).|1648 +/- 3 Ma (see Fig.1.2)|Umbolooga Subgroup, McArthur Group||Underlain by Amelia Dolostone. Partly overlain by Tooganinie Formation and Leila Sandstone.||
17896|Tatoola Sandstone|73412|5|Briefly described|p2, 4, 8|||Southern McArthur Basin.|1648 +/- 3 Ma.|Umbolooga Subgroup.||Overlies Amelia Dolostone. Is overlain by Tooganinie Formation.||
17902|Tawallah Group|7071|5|Briefly described|p1|||Geological Province: McArthur Basin.||||||
17902|Tawallah Group|22432|5|Briefly described|p20|||In the McArthur Basin.||||||11-DEC-06
17902|Tawallah Group|22453|5|Briefly described|p 11|||||||||
17902|Tawallah Group|22479|5|Briefly described|fig4, pg10|Statherian|Statherian|||||||
17902|Tawallah Group|22538|4|Described|P707, P714|Statherian|Orosirian|Part of the Redbank package||||||06-JUN-18
17902|Tawallah Group|22644|5|Briefly described|3,4,7,9,12,13|||Geological province: McArthur Basin.||||||11-DEC-06
17902|Tawallah Group|22662|5|Briefly described|22,23 fig 2|Proterozoic|Proterozoic|Geological province: McArthur Basin.||||||11-DEC-06
17902|Tawallah Group|22664|6|Mentioned|35|Paleoproterozoic|Paleoproterozoic|Geological province: McArthur Basin.||||||07-NOV-08
17902|Tawallah Group|22665|6|Mentioned|P222|||||||||
17902|Tawallah Group|22670|6|Mentioned|53,54,56,58,59,60|||Geological province: McArthur Basin.||||||11-DEC-06
17902|Tawallah Group|22673|6|Mentioned|64|||Geological province: McArthur Basin.||||||11-DEC-06
17902|Tawallah Group|22853|4|Described|5|Proterozoic|Proterozoic|Geol province McArthur Basin.||||||11-DEC-06
17902|Tawallah Group|23065|6|Mentioned|11|Proterozoic|Proterozoic|Geological province: McArthur Basin.||||||11-DEC-06
17902|Tawallah Group|23066|5|Briefly described|p807, Fig.1|Proterozoic|Proterozoic|Geological province: McArthur Basin.||||||11-DEC-06
17902|Tawallah Group|23195|6|Mentioned|p5|||Informally referred to "Upper" Tawallah Group.||||||
17902|Tawallah Group|23197|6|Mentioned|Fig.1, p850|||Informally referred to as lower and upper Tawallah Group.||||||
17902|Tawallah Group|23374|6|Mentioned|p8,41,42,34,6,8,30||Statherian|Equivalent to Kombolgie Subgroup. Geological province: McArthur Basin.||||||11-DEC-06
17902|Tawallah Group|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: McArthur Basin.||||||07-NOV-08
17902|Tawallah Group|23395|4|Described|p384 Fig.2|||||||||
17902|Tawallah Group|23396|5|Briefly described|p407 Fig.2|||||||||
17902|Tawallah Group|23397|6|Mentioned|p471|||||||||
17902|Tawallah Group|23398|5|Briefly described|p436|Statherian|Statherian|||||||
17902|Tawallah Group|23406|5|Briefly described|p601 Fig.3|||||||||
17902|Tawallah Group|23407|5|Briefly described|p627 Fig.2|||||||||
17902|Tawallah Group|23733|5|Briefly described|p32 Fig. 19|||Geological Province: MacArthur Basin.||||||
17902|Tawallah Group|23776|5|Briefly described|p704|||||||||
17902|Tawallah Group|23809|5|Briefly described|p27|Proterozoic|Proterozoic|Geological Province: McArthur Basin.  Correlates with Tomkinson Creek Group (Ashburton Province) and Birrindudu Group (Birrindudu Basin), and the Wauchope and Hanlon Subgroups of Hatches Creek Group (Davenport Province).||||||
17902|Tawallah Group|23867|5|Briefly described|p14|||See also Fig. 30.  Geological  Province: McArthur Basin.||||||
17902|Tawallah Group|23910|4|Described|p290|Paleoproterozoic|Paleoproterozoic|Geological Province: McArthur Basin.||||||07-NOV-08
17902|Tawallah Group|23937|6|Mentioned|p4 Fig. 4, p51|||||||||
17902|Tawallah Group|23963|4|Described|p1237, 1239 Fig.2|Paleoproterozoic|Paleoproterozoic|Geological Province: McArthur Basin. Age: 1857+/-30 Ma. Overlies the Scrutton Volcanics.||||||07-NOV-08
17902|Tawallah Group|23968|6|Mentioned|p1346 Fig. 1|||Geological Province: McArthur Basin.||||||
17902|Tawallah Group|24047|5|Briefly described|p12 Fig. 10|Paleoproterozoic|Paleoproterozoic|Age: 1800-1700Ma.  Geological Province: McArthur Basin.||||||07-NOV-08
17902|Tawallah Group|24048|6|Mentioned|p6|||Geological Province: McArthur Basin||||||
17902|Tawallah Group|24050|6|Mentioned|p12|||Geological Province: McArthur Basin.||||||
17902|Tawallah Group|24197|6|Mentioned|p54|||Contains igneous suites of rocks which are either bimodal, dominantly felsic or dominantly mafic. Geological Province: McArthur Basin.||||||07-FEB-11
17902|Tawallah Group|24419|5|Briefly described|p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Includes Hobblechain Rhyolite, Selgal Volcanics and Westmoreland Conglomerate.   Geological Province: McArthur Basin, Murphy Province.||||||07-NOV-08
17902|Tawallah Group|24432|6|Mentioned|p559|||||||||
17902|Tawallah Group|30272|6|Mentioned|p5|||On stratigraphic table||||||
17902|Tawallah Group|30318|6|Mentioned|p327|||||||||
17902|Tawallah Group|30344|6|Mentioned|p29|||See also Fig.4||||||
17902|Tawallah Group|30345|6|Mentioned|Table 1|||Carpentarian age. Lithology||||||
17902|Tawallah Group|30508|6|Mentioned|p94|||Stratigraphy||||||
17902|Tawallah Group|30534|6|Mentioned|p306|||||||||
17902|Tawallah Group|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
17902|Tawallah Group|31824|6|Mentioned|p28|||Middle Proterozoic||||||
17902|Tawallah Group|32339|6|Mentioned|Fig.1|||||||||
17902|Tawallah Group|32479|6|Mentioned|Fig.1|||||||||
17902|Tawallah Group|32519|6|Mentioned|p340|||||||||
17902|Tawallah Group|32658|4|Described|Table 2|||See also Fig.3||||||
17902|Tawallah Group|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17902|Tawallah Group|32660|4|Described|Table 4|||||||||
17902|Tawallah Group|32904|6|Mentioned|p89|||||||||
17902|Tawallah Group|33214|6|Mentioned|Fig.1|||||||||
17902|Tawallah Group|33665|5|Briefly described|p366|||||||||
17902|Tawallah Group|34287|6|Mentioned|p34|||||||||
17902|Tawallah Group|34754|6|Mentioned|p15|||||||||
17902|Tawallah Group|35114|6|Mentioned|p203|||||||||
17902|Tawallah Group|35162|6|Mentioned|p1007|||||||||
17902|Tawallah Group|35261|6|Mentioned|Fig.1|||||||||
17902|Tawallah Group|35495|6|Mentioned|p340|||||||||
17902|Tawallah Group|35640|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17902|Tawallah Group|35776|6|Mentioned|p814|||See also Table 1.||||||
17902|Tawallah Group|35950|6|Mentioned|p311|||||||||
17902|Tawallah Group|36012|3|Fully described|Table 2|||||||||
17902|Tawallah Group|36439|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17902|Tawallah Group|36442|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17902|Tawallah Group|36473|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17902|Tawallah Group|37217|6|Mentioned|p650|||||||||
17902|Tawallah Group|37372|6|Mentioned|p2|||||||||
17902|Tawallah Group|37462|4|Described|Table4.IV|||||||||
17902|Tawallah Group|37565|5|Briefly described|p3|||See also Fig.5.||||||11-DEC-06
17902|Tawallah Group|37568|4|Described|p75|||||||||
17902|Tawallah Group|37569|6|Mentioned|p91|||||||||
17902|Tawallah Group|38042|6|Mentioned|p160|||||||||
17902|Tawallah Group|38156|6|Mentioned|Fig.1|||||||||
17902|Tawallah Group|38529|6|Mentioned|p275|||||||||
17902|Tawallah Group|38582|6|Mentioned|p215|||||||||
17902|Tawallah Group|38584|4|Described|p10|||||||||
17902|Tawallah Group|38902|6|Mentioned|p20|||||||||
17902|Tawallah Group|39122|6|Mentioned|p154|||||||||
17902|Tawallah Group|39210|5|Briefly described|p50|||||||||
17902|Tawallah Group|39445|6|Mentioned|p36|||See also p39.||||||11-DEC-06
17902|Tawallah Group|39497|6|Mentioned|Fig.4|||||||||
17902|Tawallah Group|39561|6|Mentioned|Fig.5|||||||||
17902|Tawallah Group|39685|6|Mentioned|Fig.1|||||||||
17902|Tawallah Group|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
17902|Tawallah Group|39925|6|Mentioned|p337|||||||||
17902|Tawallah Group|40105|6|Mentioned|p310|||See also Fig.7||||||
17902|Tawallah Group|40109|5|Briefly described|p302|||||||||
17902|Tawallah Group|40259|6|Mentioned|Table 1|||||||||
17902|Tawallah Group|40489|6|Mentioned|p89|||||||||
17902|Tawallah Group|40491|6|Mentioned|p79|||||||||
17902|Tawallah Group|40691|3|Fully described|p7|||||||||
17902|Tawallah Group|40840|6|Mentioned|Map legend|||||||||
17902|Tawallah Group|40973|6|Mentioned|p193|||||||||
17902|Tawallah Group|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
17902|Tawallah Group|41019|5|Briefly described|p243|||||||||
17902|Tawallah Group|41125|6|Mentioned|p35|||||||||
17902|Tawallah Group|41220|5|Briefly described|p366|||||||||
17902|Tawallah Group|41268|4|Described|p283|||||||||
17902|Tawallah Group|41277|6|Mentioned|Fig.2|||||||||
17902|Tawallah Group|41319|6|Mentioned|Fig.1|||||||||
17902|Tawallah Group|41406|6|Mentioned|Map legend|Mesoproterozoic||||||||
17902|Tawallah Group|41721|3|Fully described|p8|||Comprises 10 named units and is the oldest group in the McArthur Basin sequence. Overlies igneous and metamoprhic complexes of the Murphy Inlier; disconformably overlain by Masterton Sandstone. Geological province: McArthur Basin.||||||01-AUG-07
17902|Tawallah Group|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
17902|Tawallah Group|41957|6|Mentioned|p68|||||||||
17902|Tawallah Group|42385|3|Fully described|p5|Paleoproterozoic|Paleoproterozoic|Includes Yiyintyti Sst, Seigal Volc, Sly Creek Sst, Aquarium Fm, Wununmantyala Sst, Settlement Creek Volcs, Wollogorang Fm, Gold Creek Volcs, Warramana Sst and Tanumbirini Rhyolite. Age between 1857 +/- 30Ma and 1725 +/- 40 Ma. Composite thickness: >5km.||||||06-JUN-18
17902|Tawallah Group|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
17902|Tawallah Group|42395|6|Mentioned|Fig.26 P86|||||||||
17902|Tawallah Group|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.|||10 fm, 1 mbr. Yiyintyi Ss, Seigal Volcs, Sly Creek Ss (Rosie Creek Ss Mbr), Aquarium Fm, Wununmantyala Ss, Settlement Ck Volcs, Wollogorang Fm, Gold Ck Volcs, Warramana Ss, Tanumbirini Rhyolite.|Underlies McArthur Group.||06-OCT-11
17902|Tawallah Group|42639|3|Fully described|p8, Table 4 p11|Mesoproterozoic||||||||
17902|Tawallah Group|42700|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
17902|Tawallah Group|42739|5|Briefly described|map legend|Statherian|Statherian|Quartz sandstone, conglomerate, mudstone, basaltic and rhyolitic volcanics, minor dolostone.||||||19-OCT-05
17902|Tawallah Group|42753|6|Mentioned|p2|||||||||
17902|Tawallah Group|42812|4|Described|p10, Table 3|||||||||
17902|Tawallah Group|42846|5|Briefly described|p503|||Geological Province: McArthur Basin.||||||09-MAY-05
17902|Tawallah Group|42873|5|Briefly described|p109|||see also Fig.1, p110.||||||11-DEC-06
17902|Tawallah Group|42935|5|Briefly described|p527|||||||||
17902|Tawallah Group|43010|6|Mentioned|p91|||of "Mid Proterozoic" age.||||||
17902|Tawallah Group|43036|4|Described|p13|||||||||
17902|Tawallah Group|43107|6|Mentioned|p9|||||||||
17902|Tawallah Group|43292|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
17902|Tawallah Group|43595|4|Described|p438||Mesoproterozoic|||||||
17902|Tawallah Group|43615|6|Mentioned|p14|||||||||
17902|Tawallah Group|43788|6|Mentioned|p13||Proterozoic|||||||
17902|Tawallah Group|44112|6|Mentioned|p10,43|||Part of Supersequence 1(B); middle and upper units in 1(C); upper units in 1(D)||||||
17902|Tawallah Group|44155|6|Mentioned|p252|||McArthur Basin. Probable part correlative of Mount Parker Sandstone and Bungle Bungle Dolomite.||||||
17902|Tawallah Group|44287|14|Not recorded|p.6-16|||(E53-3).||||||
17902|Tawallah Group|44288|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
17902|Tawallah Group|44299|6|Mentioned|p.11|||SD/53-7,8.||||||
17902|Tawallah Group|44305|14|Not recorded|p.11-13,18|||(E53-8). opp.p.6,18.||||||
17902|Tawallah Group|44306|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
17902|Tawallah Group|44332|14|Not recorded|p.7,11,12,opp.6,map|||(D53-14).||||||
17902|Tawallah Group|44333|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
17902|Tawallah Group|44434|14|Not recorded|opp.p.6,map|||Correlated with Groote Eylandt Beds. (D53-11,12).||||||
17902|Tawallah Group|44435|14|Not recorded|map legend|||Lower (?) Proterozoic.||||||
17902|Tawallah Group|44436|5|Briefly described|p.6-10,opp.p.7,map|||(E53-4).||||||02-DEC-04
17902|Tawallah Group|44437|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Includes the Masterton, Wollogorang and Aquarium Formations, and the Settlement Creek Volcanics.||||||07-NOV-08
17902|Tawallah Group|44459|14|Not recorded|p.6,7,opp.p.6, map|||(E53-2). Here includes Rosie Creek Sandstone, Settlement Creek Volcanics, Wollogorang Formation, Masterton Formation (top). See p.12,13, for more details.||||||
17902|Tawallah Group|44460|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
17902|Tawallah Group|44471|14|Not recorded|p.7|||(D53-10).||||||
17902|Tawallah Group|44473|14|Not recorded|p.7-8,13-15,opp. p.7|||(E53-7).||||||
17902|Tawallah Group|44474|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
17902|Tawallah Group|44482|14|Not recorded|p.7|||(E53-12).||||||
17902|Tawallah Group|44530|14|Not recorded|p.4-17|||(D53-15).||||||
17902|Tawallah Group|44531|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
17902|Tawallah Group|45032|14|Not recorded|p9||Carpentarian|Tb.1, Pl.1.||||||
17902|Tawallah Group|45140|6|Mentioned|p12-13|||McArthur Basin region.|~1575 Ma.|||||
17902|Tawallah Group|45162|2|Defined|p11|Proterozoic|Proterozoic|||||||
17902|Tawallah Group|45166|6|Mentioned|p14|||||||||
17902|Tawallah Group|45167|5|Briefly described|Fig.27|||||||||
17902|Tawallah Group|46804|6|Mentioned|p154|||||||||
17902|Tawallah Group|46861|6|Mentioned|p2|||||||||
17902|Tawallah Group|46915|6|Mentioned|Fig.1|||Stratigraphic section through McArthur Group.||||||
17902|Tawallah Group|46955|6|Mentioned|p159|||||||||
17902|Tawallah Group|46968|6|Mentioned|Fig.2|||||||||
17902|Tawallah Group|49001|6|Mentioned|p4|||||||||
17902|Tawallah Group|50225|5|Briefly described|p407|||Geological Province: McArthur Basin.||||||07-FEB-11
17902|Tawallah Group|50591|5|Briefly described|p1.1|||Geological Province: McArthur Basin.||||||
17902|Tawallah Group|60483|4|Described|p6, p7 Fig. 5|Paleoproterozoic|Paleoproterozoic|Unconformable over basement units including Scrutton Volcanics, and McArthur Group. Max.age: ~1850Ma; min.age: 1713+/-7Ma. Geol.Prov: McArthur Basin. Dominated by shallow marine to fluvial sandstone, with lesser mudstone, dolostone, igneous rocks.||||||07-NOV-08
17902|Tawallah Group|60558|5|Briefly described|p7, p8 Fig. 6, p10, p12|Proterozoic|Proterozoic|Includes 14 units. Coarse-grained terrigenous to shallow marine clasticsand mafic volcanics, with lesser shallow water to shelf carbonates.||||||
17902|Tawallah Group|60573|6|Mentioned|Regional Setting legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17902|Tawallah Group|60574|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: McArthur Basin.||||||07-NOV-08
17902|Tawallah Group|62084|6|Mentioned|p956||||||||Mafic and felsic volcaniclastic rocks, clastic and minor volcanic rocks.|
17902|Tawallah Group|62285|6|Mentioned|p380, p381|||||||||
17902|Tawallah Group|63110|6|Mentioned|p1141|||Includes; Settlement Creek and Gold Creek Volcanics. Overlain by McArthur Group.||||||11-JUN-08
17902|Tawallah Group|63112|6|Mentioned|p1190, p1992 Tb.1 |||Southern McArthur Basin. Also includes Warramana, Wununmantyala, Rosie Creek, Sly Creek, Echo and Yiyintyi Sandstones and Westmoreland Conglomerate.|||Includes Tanumbirini, Hobblechain Rhyolites; Packsaddle Microgranite; Gold Creek, Settlement Creek, Seigal  Volcanics; Aquarium, McDermott, Nyanantu, Wollogorang Formations. NB: See Comments.|||
17902|Tawallah Group|63866|5|Briefly described|p112, p115|||Southern McArthur Basin.||||Equivalent to the Katherine River Group and the Spencer Creek Group.||
17902|Tawallah Group|64250|6|Mentioned|p25 fig 10|||Southern McArthur Basin. Contemporaneous with volcanism in Mount Isa Inlier.|~1795-1695 Ma.||Includes Seigal Volcanics, Gold Creek Volcanics.|||15-MAR-18
17902|Tawallah Group|64724|5|Briefly described|p45 Fig.5, p46|Statherian|Statherian|Lower part of this group of the Leichhardt Superbasin (McArthur Basin), deposited during the Leichhardt Extension (1800-1750 Ma). Upper part is part of the Calvert Superbasin, deposited during the Calvert Event (~1730-1690 Ma).||||||
17902|Tawallah Group|64815|5|Briefly described|p3, p4 Fig.2, p5 Fig.3, p6, p10-13|Statherian|Orosirian|See also p15 Fig.9, p16-18 Figs.10-12. Represents the Redbank package. The topmost units are often missing in stratigraphic successions. Appears as Subgroup in Figs.10-12.|Deposition from 1815-1705 Ma.||Includes Yiyintyi, Sly Creek, Warramana, Wununmantyala Sandstones; Seigal, Settlement Creek, Gold Creek, Volcanics; Aquarium, Wollogorang, Nyanantu Formations; Tanumbirini Rhyolite.|Unconformably overlies Scrutton Volcanics.|Composed of sandstone, with bimodal igneous intrusions and lavas, lutite, conglomerate and dolostone.|
17902|Tawallah Group|64817|5|Briefly described|p352 Fig.3, p353 Fig.4, p354, 355, 357|||Also includes Tanumbirini and Hobblechain Rhyolite; Gold Creek, Settlement Creek and Seigal Volcanics. A mid-Tawallah Group east-west compressional event deformed and uplifted older units of the Group.|Shown as ~1790 - <1705 Ma.||Includes Burash, Echo, Warramana, Wununmantyala, Sly Creek and Yiyintyi Sandstones; Westmoreland Conglomerate; Nyanantu, Wollogorang, Aquarium and McDermott Formations; and various volcanic units.|||06-JUN-18
17902|Tawallah Group|64975|6|Mentioned|p162 Fig.6.|Mesoproterozoic|Mesoproterozoic|||||||
17902|Tawallah Group|65228|4|Described|p7, p19, Fig.02|||McArthur Basin. c.5,000 m thick. Lower parts of this unit comprise the Leichhardt Superbasin. Also includes Hobblechain and Tanumbirini Rhyolites.|||Includes Yiyintyi, Sly Creek, Wununmantyala, Warramana Sandstones; Seigal, Settlement Creek, Gold Creek Volcanics; McDermott, Aquarium, Wollogorang Formations; Westmoreland Conglomerate and others.||Shallow water clastics; minor carbonate, shale and volcanic rocks.|
17902|Tawallah Group|65232|5|Briefly described|p9, p20, p78|||Includes Westmoreland Conglomerate at base, Seigal Volcanics, and Wollogorang Formation. Correlatives of Katherine River Group and Tolmer Group. Unconformably overlie northern margin of Murphy Inlier. Uranium deposits. Geol. Prov: McArthur Basin.||||||09-FEB-10
17902|Tawallah Group|65337|6|Mentioned|p6 Fig.3, p15.|||McArthur Basin. Correlative of Carrara Range Group.||||||
17902|Tawallah Group|65340|3|Fully described|p5,  p.13 Table 4, pp11-57, p 66.|||PhD thesis and related papers published (Rawlings 1998, 1999, 2002). Oldest, most areally extensive and voluminous unit in southern McArthur Basin. Forms a regionally extensive, mainly flat-lying platform 2.5 to 6 km thick. Resistant sandstone ranges and plateaux; very little deformation is due to its zone of tectonic stability as well as the structurally competent, thick homogeneous sandstone packages. Probably contiguous with Katherine River Group, Tennant Creek Inlier and Mount Isa Inlier. Contemporaneous with Katherine River, Donydji and Spencer Creek Groups.|||Westmoreland Conglomerate; Yiyintyi, Sly Creek, Wununmantyala, Warramana, Burash and Echo Sandstones; Seigal, Gold Creek and other Volcanics; McDermott, Wollogorang and Nyanantu Formations; and more.|Unconformably overlies Murphy and Scrutton Inliers. Is unconformably overlain by McArthur Group,and Karns Dolomite.|Dominated by shallow-marine and fluviatile sandstone, with lesser mudstone, dolostone and bimodal (basalt-rhyolite) volcanic and high-level intrusive rocks.|23-MAR-18
17902|Tawallah Group|66529|5|Briefly described|p21 |||||||Overlies Seigal Volcanics.|Dolomite, sandstone and mafic and felsic volcanic rocks.|
17902|Tawallah Group|66843|5|Briefly described|p23-24|||Oldest tectonic-stratigraphic package in the southern McArthur Basin.|1760 - 1710 Ma.|||Is overlain unconformably by McArthur Group.|Mainly quartz-rich sandstones and mafic to felsic igneous rocks.|
17902|Tawallah Group|67144|5|Briefly described|Map legend.|Statherian|Statherian|McArthur Basin.|||Includes Westmoreland Conglomerate; Seigal, Settlement Creek and Gold Creek Volcanics; McDermott and Wollogorang Formations; Sly Creek Sandstone.|Is overlain by McArthur Group.||13-APR-12
17902|Tawallah Group|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map; p107|||CONSTITUENTS (continued): Gold Creek, Seigal, Settlement Creek, Cliffdale Volcanics.|||Aquarium, McDermott, Wollogorang Formations; Carolina Sandstone Member; Westmoreland Conglomerate; Sly Creek, Wire Creek Sandstones; Hobblechain Rhyolite. See COMMENTS for more.|||
17902|Tawallah Group|67352|4|Described|v, p11-12, p14-15 Tb.2, p50|Statherian|Statherian|McArthur Basin (Calvert Superbasin). Up to 6 km thick.|1790-1705 Ma||Includes Gold Creek Volcanics, Wollogorang Formation, Settlement Creek Volcanics, Sly Creek Sandstone, McDermott Formation and Seigal Volcanics.|Overlain by McArthur Group (unconformably).|Shallow-marine to fluviatile sandstone and volcanigenic and shallow-intrusive rocks, together with minor lutite, conglomerate and dolostone.|08-JAN-15
17902|Tawallah Group|67564|6|Mentioned|p86.|||Southern McArthur Basin.|||Includes Sly Creek Sandstone.|||
17902|Tawallah Group|67779|5|Briefly described|p32, p36.|||Southern McArthur Basin. Included by Rawlings (1999) in his Redbank Package, with Katherine River Group, Spencer Creek Group, Gadabara Volcanics, Groote Eylandt Group and Donji Group.|||Includes Sly Creek Sandstone.|||
17902|Tawallah Group|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|McArthur Basin, Mount Isa Province.||||Is overlain conformably by Peters Creek Volcanics.||
17902|Tawallah Group|69417|6|Mentioned|p2:5|Statherian|Statherian|McArthur Basin.||||||12-JUL-16
17902|Tawallah Group|69418|6|Mentioned|p3:15||||||Gold Creek Volcanics.|||12-JUL-16
17902|Tawallah Group|69423|5|Briefly described|p8:4 Fig.8.7|Paleoproterozoic|Paleoproterozoic|McArthur Basin.|||Settlement Creek dolerite, Seigal Volcanics, Westmoreland Conglomerate.|||12-JUL-16
17902|Tawallah Group|69429|5|Briefly described|p14:3|||McArthur Basin.|||Yiyintyi Sandstone.|Unconformably overlies Scrutton Volcanics.||12-JUL-16
17902|Tawallah Group|69430|4|Described|p15:2-4, 9-14, 35, 39, 62|||Southern McArthur Basin. Also includes igneous units: Settlement Creek Dolerite; Hobblechain, Tanumbirini Rhyolites; Packsaddle Microgranite. Generally shallow dipping or flat-lying. May be contiguous with Tomkinson Creek Group (Tomkinson Creek Province) and Haslingden Group (Isa Superbasin). Mentioned as a source of metals for the McArthur River Zn-Pb-Ag deposit. Hosts a number of small U-Au deposits surrounding the Murphy Inlier (described in detail).|>1710 Ma.||Westmoreland Conglomerate; Yiyintyi, Sly Creek, Wununmantyala, Warramana, Echo, Burash Sandstones; Seigal, Gold Creek Volcanics; McDermott, Aquarium, Wollogorang, Nyanantu Formations.|Is overlain unconformably by the McArthur and Nathan Groups. Is correlated, and probably contiguous, with the Katherine River Group.|Shallow-marine and fluvial sandstone, with lesser mudstone, dolostone and mafic and felsic volcanic rocks, and coeval and younger intrusive bodies.|12-JUL-16
17902|Tawallah Group|69433|6|Mentioned|p18:1-2, 10|||McArthur Basin.||||Equivalent to Wire Creek Sandstone and Peters Creek Volcanics (Lawn Hill Platform).||12-JUL-16
17902|Tawallah Group|69591|5|Briefly described|p29, p39, p56, p58|Paleoproterozoic|Paleoproterozoic|Camooweal-Murphy Domain, Mount Isa Province. The only unit in the McArthur Basin succession N of the Murphy Tectonic Ridge in Qld.|||Westmoreland Conglomerate; Sly Creek, Wire Creek Sandstones; McDermott, Aquarium, Wollogorang Formations; Gold Creek, Seigal, Settlement Creek Volcanics; Hobblechain Rhyolite.|||
17902|Tawallah Group|69673|4|Described|p15, p17, p20, p22, p32, p40, p49, p51|Statherian|Statherian|Also includes Tanumbirini Rhyolite, Warramana Sandstone, Hobblechain Rhyolite, Gold Creek Volcanics, Wollogorang Formation, Settlemenet Creek Dolerite, Wununmantyala Sandstone, Aquarium Formation, McDermott Formation, Sly Creek Sandstone, Seigal Volcanics, Yiyintyi Sandstone, Westmoreland Conglomerate.|1710 Ma||Includes Burash Sandstone, Nyanantu Formation, Echo Sandstone|Correlated with Birrindudu Group|Extensively silicified arkosic or quartz rich sandstone that alternate with mafic volcanic rocks, shale and rare carbonate rocks.|
17902|Tawallah Group|70284|5|Briefly described|p1245|Statherian|Statherian|Leichhardt Superbasin. 1000-4000m thick. Age inferred from age of Leichhardt Superbasin.|||||Fluvial conglomeratic sandstones, mafic volcanics and marine and aeolian sediments.|
17902|Tawallah Group|70302|5|Briefly described|iv, p7|Statherian|Statherian|Southern McArthur Basin. Age is also derived from Page and Sweet, 1998.|c.1730 Ma (Page et al., 2000).|||Correlated with Woodah Sandstone.||05-FEB-18
17902|Tawallah Group|70822|5|Briefly described|p102 fig 1 (A), p103|Mesoproterozoic|Mesoproterozoic|Chronostratigraphy is adapted from Brasier and Lindsay (1998) and Southgate et al. (2000).|1729 +/- 4 Ma to 1713 +/- 7 Ma.|||Overlain by McArthur Group||06-JUN-18
17902|Tawallah Group|70849|5|Briefly described|Map legend.|Statherian|Statherian|McArthur Basin and 'Tawallah Group equivalent' on Lawn Hill Platform. Also includes Packsaddle Microgranite.|||Wire Creek, Sly Creek Sandstones; Peters Creek, Seigal, Settlement Creek, Gold Creek Volcanics; Westmoreland Conglomerate; McDermott, Aquarium, Wollogorang Formations; Hobblechain Rhyolite.|Unconformably overlies Murphy Metamorphics and Cliffdale Volcanics.|Conglomerate, sandstone, greywacke, dolostone; basalt, dolerite, rhyolite, rhyodacite, dacite, trachyte, microgranite.|21-FEB-18
17902|Tawallah Group|70968|6|Mentioned|p2 Fig.3|||||||||
17902|Tawallah Group|71059|6|Mentioned|p2|Paleoproterozoic|Paleoproterozoic|McArthur Basin.||||||
17902|Tawallah Group|71374|5|Briefly described|p2, p6|||southern McArthur Basin.|||Includes the Gold Creek Volcanics, Wollogorang Formation and Wununmantyala Sandstone.|Unconformably overlain by the McArthur Group. Equivalent to the lower Spencer Creek, Groote Eylandt, Donydji, Katherine River and Edith River groups.||
17902|Tawallah Group|71606|5|Briefly described|p135,137|Statherian|Statherian|Bauhinia Shelf, Batten Trough and Wearyan Shelf, McArthur Basin. Arenite-bimodal volcanic-lutite-carbonate sequence. Age is constrained by 1710-1700 Ma Fagan Phase.|||Includes Hobblechain and Tanumbirini Rhyolites.|Correlable to Groote Eylandt Group. Overlain unconformably by Nathan and McArthur groups, and Karns Dolomite. Correlable to Katherine River Group.||
17902|Tawallah Group|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin. Informally subdivided into lower and upper parts.||||||06-MAR-20
17902|Tawallah Group|72248|5|Briefly described|p146,148|||Of McArthur Basin.|||||Quartz sandstone with lesser conglomerate, dolostone, fine-grained clastics, and mafic and felsic volcanics.|
17902|Tawallah Group|72373|5|Briefly described|p2|Paleoproterozoic|Paleoproterozoic|Of northern McArthur Basin. Broadly equivalent to Redbank package, and Spencer Creek, Groote Eylandt, Donydji, Katherine River and Edith River groups (northern McArthur Basin), Birrindudu and Tolmer groups (Birrindudu Basin) and Tomkinson Creek and Hatches Creek groups (Tomkinson Province).||||||
17902|Tawallah Group|72377|5|Briefly described|iii,p12|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin.|||Includes Wollogorang Formation and Tanumbirini Rhyolite.|||
17902|Tawallah Group|72523|6|Mentioned|p1.|Palaeoproterozoic|Palaeoproterozoic|||||Unconformably underlies the  Nathan Group.||
17902|Tawallah Group|72526|5|Briefly described|p4, p6 Fig.1.2, p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Urapunga Fault Zone, Beetaloo Sub-basin, Batten Fault Zone and Southeastern McArthur Basin. This group also includes Settlement Creek Dolorite and Westmoreland Conglomerate.|||Burash, Warramana,  Sandstone, Echo, Wununmantyala, Sly Ck. and Yiyintyi Ss, Nyanantu, Wollogorang, Aquarium and McDermott Fms, Tanumbinini, Hobblechain Rhyolites, Gold Creek, Seigal Volcanics,|Shown as unconformably overlying Scrutton Volcanics, Cliffdale Volcanics and Nicholson Granite Complex and unconformably underlying McArthur Group.||
17902|Tawallah Group|72527|6|Mentioned|p1, p3, p5, p7, p176, 185, 193, 194.|Paleoproterozoic|Paleoproterozoic|This group is divided by an unconformity between the earlier Wire Creek Sandstone and Peters Creek Volcanics. Lithographically also contains rounded clasts of predominantly white vein quartz, quartzite, felsic volcanics and rarely, granite.|||Includes Peters Creek Volcanics and Wire Creek Sandstone|Shown as laterally equivalent to and unconformably underlying Carrara Range Group and partially and unconformably overlying Murphy Metamorphics.|Includes feldspathic coarse and coarse-grained, gritty quartz sst., occasionally cross-bedded, with pebble lags and local cobble to boulder congl. lenses.|
17902|Tawallah Group|72718|6|Mentioned|piii, p5, p7|Palaeoproterozoic|Palaeoproterozoic|Beetaloo Sub-basin, McArthur Basin. Calvert/Leichhardt Superbasin, Redbank package. More constituents include the Tanumbirini and Hobblechain rhyolites, Packsaddle Microgranite, Gold Creek and Seigal volcanics, and the Settlement Creek Dolerite.|||Burash, Echo, Warramana, Wununmantyala, Sly Creek, Yiyintyi sandstones; Nyanantu, Wollogorang, Aquarium, McDermott formations; Westmoreland Conglomerate [see comments].|Conformably overlain by Parsons Range Group. Unconformably overlain by McArthur River Group,Nathan Group, Roper Group.|Dominated by shallow-marine to fluvial sandstone, with lesser shale, conglomerate, dolostone and bimodal volcanic rocks.|
17902|Tawallah Group|72912|4|Described|p5 Fig.3, p18-19, p36, p48.|Statherian|Statherian|Located in the Beetaloo Sub-basin and the Batten Fault Zone in the Southern McArthur Basin. Age constraints from dating of basal Westmoreland Conglomerate at 1815+/-7 Ma (sedimentary depositional age) and Tanumbirini Rhyolite, near top at 1713+/-7 Ma. This group also includes Settlement Creek Dolorite and Westmoreland Conglomerate.|||Burash, Warramana, Echo, Wununmantyala, Sly Creek and Yiyintyi Sandstones, Nyanantu, Wollogorang, Aquarium and McDermott Formations, Tanumbinini, Hobblechain Rhyolites, Gold Creek, Seigal Volcanics,|Shown as unconformably overlying Scrutton Volcanics and partially Westmoreland Conglomerate. Shown as unconformably underlying Umbolooga Subgroup, McArthur Group.|Includes sandstone, conglomerate, rhyolite and dolerite.|
17902|Tawallah Group|72919|6|Mentioned|p3, p12|Paleoproterozoic|Paleoproterozoic||||Westmoreland Conglomerate|||
17902|Tawallah Group|72967|6|Mentioned|p2|Paleoproterozoic|Paleoproterozoic|||||||
17902|Tawallah Group|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin, Calvert and Leichhardt Superbasin. Constituents: Burash Sandstone, Echo Sandstone, Nyanantu Formation, Tanumbinini Rhyolite, Warramana Sandstone, Pungalina Member, Hobblechain Rhyolite, Gold Creek Volcanics, Settlement Creek Dolorite, Wununmantyala Sandstone, Wuraliwuntya Member, Aquarium Formation, McDermott Formation, Rosie Creek Sandstone Member, Sly Creek Sandstone, Seigal Volcanics, Yiyintyi Sandstone, Westmoreland Conglomerate.|||See comments.|||
17902|Tawallah Group|73083|6|Mentioned|p35, p37, p40|Paleoproterozoic|Paleoproterozoic||||Seigal Volcanics||Includes a basal sandstone.|
17902|Tawallah Group|73412|4|Described|p1-2, 4, 6-20|||Southern McArthur Basin. Dry bulk density tabulated. Essentially flat-lying stratigraphy. Faults described. Low gravity response; magnetic response is high where volcanic units are preserved; non-conductive unit. Exposed at the surface c.10 km W of the Emu Fault Zone. Mafic volcanics are thought to be the source of Zn and Pb.|1790-1700 Ma.||Yiyintyi Sandstone, Westmoreland Conglomerate, Seigal Volcanics, Wununmantyala Sandstone, Wollogorang Formation, Settlement Creek and Gold Creek Volcanics.|Is overlain unconformably by McArthur Group.|Widespread fluvial to intertidal sandstones and conglomerates and an anomalously thick (c.2 km) pile of mafic volcanics; overlain by shallow marine siliciclastics and carbonates, and volcanics.|
17941|Tempe Formation|22560|5|Briefly described|p2||Middle Cambrian|||||||
17941|Tempe Formation|22561|4|Described|p21|Neoproterozoic|Neoproterozoic|In the Carmichael Sub-basin.||||||11-DEC-06
17941|Tempe Formation|22566|6|Mentioned|Fig 2 on p77, &p87|Middle Cambrian|Middle Cambrian|Of the Pertaoorrta Group.||||||11-DEC-06
17941|Tempe Formation|22646|4|Described|p 100|Middle Cambrian|Middle Cambrian|Age - early Middle Cambrian to early Middle Cambrian||||||11-DEC-06
17941|Tempe Formation|22650|5|Briefly described|p 159|Cambrian|Cambrian|Of the Pertaoorrta Group.||||||11-DEC-06
17941|Tempe Formation|22651|4|Described|p 185|Middle Cambrian|Early Cambrian|Of the Pertaoorrta Group. Max. thickness: ~350m in the Carmichael sub-basin, and is 100-300m thick elsewhere (p185).  Retains fossils - brachiopods, trilobites, hyoliths, gastropods, small phosphatic shells and acritarchs.||||||11-DEC-06
17941|Tempe Formation|22653|5|Briefly described|p 241||Middle Cambrian|||||||
17941|Tempe Formation|22654|4|Described|p 245-252|Middle Cambrian|Middle Cambrian|Age based on a fauna of brachiopods, trilobites, hyoliths and gastropods p245.||||||
17941|Tempe Formation|22760|6|Mentioned|p344|||||||||
17941|Tempe Formation|22763|6|Mentioned|p398|Cambrian|Cambrian|Of the Pertaoorrta Group.||||||11-DEC-06
17941|Tempe Formation|22804|6|Mentioned|Fig 2 on p432|Cambrian|Cambrian|Of the Pertaoorrta Group.||||||11-DEC-06
17941|Tempe Formation|22805|6|Mentioned|p471||Cambrian|||||||
17941|Tempe Formation|22826|6|Mentioned|Fig 2 on p565|Cambrian|Cambrian|||||||
17941|Tempe Formation|23250|5|Briefly described|p1124  Fig.2||Middle Cambrian|Correlate of Lake Frome Group.||||||
17941|Tempe Formation|23356|5|Briefly described|26 Tab.2|Cambrian|Cambrian|||||||
17941|Tempe Formation|29721|6|Mentioned|Table 44|||||||||
17941|Tempe Formation|30238|4|Described|p68|||||||||
17941|Tempe Formation|31969|6|Mentioned|p10|||||||||
17941|Tempe Formation|33307|6|Mentioned|Fig.6|||||||||
17941|Tempe Formation|34186|6|Mentioned|Fig.3|||Middle Cambrian. See Fig.4||||||
17941|Tempe Formation|34442|5|Briefly described|Table 1|||Cambrian||||||
17941|Tempe Formation|35102|6|Mentioned|Fig.2|||||||||
17941|Tempe Formation|36198|6|Mentioned|p294|||See also Fig.III.2||||||
17941|Tempe Formation|39213|6|Mentioned|Fig.6|||Amadeus Basin Succession||||||
17941|Tempe Formation|40254|6|Mentioned|Fig.7|||||||||
17941|Tempe Formation|40740|3|Fully described|p32|||Mention p5.||||||11-DEC-06
17941|Tempe Formation|40810|4|Described|p5|||Briefly described p13.||||||11-DEC-06
17941|Tempe Formation|40852|6|Mentioned|p34|||||||||
17941|Tempe Formation|40856|5|Briefly described|p316|||||||||
17941|Tempe Formation|41115|6|Mentioned|Fig.2|||||||||
17941|Tempe Formation|41190|6|Mentioned|Fig.4|||||||||
17941|Tempe Formation|41203|6|Mentioned|p5|||||||||
17941|Tempe Formation|41224|6|Mentioned|Fig.2|||||||||
17941|Tempe Formation|41233|6|Mentioned|p17|||||||||
17941|Tempe Formation|41270|6|Mentioned|p274|||||||||
17941|Tempe Formation|41639|6|Mentioned|p15|||||||||
17941|Tempe Formation|41717|6|Mentioned|p355|||||||||
17941|Tempe Formation|41723|6|Mentioned|Map legend|Neoproterozoic||||||||
17941|Tempe Formation|42060|6|Mentioned|Fig.5 P140|||||||||
17941|Tempe Formation|42082|6|Mentioned|Fig.3 P323|||||||||
17941|Tempe Formation|42940|5|Briefly described|Plate 8|||||||||
17941|Tempe Formation|43225|5|Briefly described|Map Legend||Cambrian|Of the Pertaoorrta Group.||||||30-SEP-08
17941|Tempe Formation|43503|6|Mentioned|11-50|Ordian|Botoman|||||||
17941|Tempe Formation|43646|6|Mentioned|Fig.3,p554||Middle Cambrian|||||||
17941|Tempe Formation|43649|6|Mentioned|p457|||||||||
17941|Tempe Formation|44158|6|Mentioned|p32|||||||||
17941|Tempe Formation|44402|5|Briefly described|map legend||Cambrian|Part of Pertaoorrta Group.||||||02-DEC-04
17941|Tempe Formation|44484|14|Not recorded|p.10,12,13, Tb.1|||?Lower Camb. Part of Pertaoorrta Group.||||||
17941|Tempe Formation|44485|14|Not recorded|map legend||Cambrian|Part of Pertaoorrta Group.||||||
17941|Tempe Formation|44497|4|Described|p.10, Table 1||Cambrian|SF/53-13.||||||
17941|Tempe Formation|44498|14|Not recorded|map legend||Cambrian|Part of Pertaoorrta Group.||||||
17941|Tempe Formation|44505|14|Not recorded|p.7,11, Table 1||Cambrian|Of Pertaoorrta Group.||||||
17941|Tempe Formation|44506|14|Not recorded|map legend||Cambrian|||||||
17941|Tempe Formation|45041|4|Described|p53|||Middle Cambrian. Of the Pertaoorrta Group.||||||11-DEC-06
17941|Tempe Formation|45155|6|Mentioned|p33|||||||||
17941|Tempe Formation|45170|6|Mentioned|Table 3|||||||||
17941|Tempe Formation|48863|2|Defined|p.18,19||Middle Cambrian|Tb.1. opp.p.7,9,17,20,22,41,Pl.10,15,16. Middle Cambrian. (G52-4,G53-1).||||||
17941|Tempe Formation|48865|14|Not recorded|Fig.4,opp.p.10||Cambrian|Unit of Pertaoorrta Group. (G52-4,F53-13).||||||11-DEC-06
17941|Tempe Formation|48890|14|Not recorded|p.77|||||||||
17941|Tempe Formation|48963|6|Mentioned|p5|||See also Fig.3||||||
17941|Tempe Formation|60674|5|Briefly described|Map legend|Cambrian|Cambrian|Of the Pertaoorrta Group. Red and green sandstone; interbeds of sandy dolostone and calcareous sandstone. Geological Province: Amadeus Basin.||||||16-JUN-09
17941|Tempe Formation|61385|5|Briefly described|Map legend|Cambrian|Cambrian|Massive yellow-brown fossiliferous limestone. Geological Province: Amadeus Basin.||||||16-JUN-09
17941|Tempe Formation|61518|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Pertaoorta Group. Red and green sandstone, interbeds of sandy dolostone and calcareous sandstone. Geological Province: Amadeus Basin.||||||
17941|Tempe Formation|61732|5|Briefly described|p99|Cambrian|Cambrian|Together with other Cambrian units overlies the Arumbera Sandstone.||||||07-FEB-11
17941|Tempe Formation|62379|5|Briefly described|p7 Fig. 2, p21|Middle Cambrian|Middle Cambrian|Of the Pertaoorrta Group. Fine siliciclastic sediment. Geological Province: Amadeus Basin.||||||11-DEC-06
17941|Tempe Formation|64068|5|Briefly described|p62, 225|||Amadeus Basin. Correlated with Arthur Creek Formation,  Beetle Creek Formation.||||||
17941|Tempe Formation|64778|6|Mentioned|p18|||Amadeus Basin. Thermal and maturation history modelling.||||||
17941|Tempe Formation|64809|5|Briefly described|p2, p3 Fig.2 |Middle Cambrian|Middle Cambrian|Continental deposition. Mis-spelt as Temple in Fig.2.||Unit in Pertaoorrta Group.||||
17941|Tempe Formation|65233|3|Fully described|p8|Middle Cambrian|Middle Cambrian|Of Pertaoorrta Gp. Disconformable on Chandler Fm; conformably overlain by Illara Sandstone. Interfingers with Hugh River Shale in north and east, and with the lower Cleland Sst in the west. Max. thickness: >150m. Geol.prov: Amadeus Basin.||||||07-FEB-11
17941|Tempe Formation|65375|6|Mentioned|p30.|||Amadeus Basin. Correlative with Corrodgery Formation, Yorke Peninsula, on basis of acritarch assemblage.||||||
17941|Tempe Formation|65489|5|Briefly described|p125|Cambrian|Cambrian|Amadeus Basin.||Unit in Pertaoorrta Group.||||
17941|Tempe Formation|67326|4|Described|p2, p4-6, p13, Appx.2|Middle Cambrian|Middle Cambrian|Amadeus Basin. Intersected by stratigraphic drillhole LA05DD01. Up to 201m thick, average about 150m. Composite log.||Pertaoorrta Group.||Overlies Chandler Formation disconformably and Mount Currie Conglomerate. Is overlain by Illara and (disconformably?) Petermann Sandstones.|The lower part is siltstone with characteristic red-brown/pale green mottling, overlain by a silicified chert breccia.|
17941|Tempe Formation|67565|5|Briefly described|pp39-40, p47.|Middle Cambrian|Middle Cambrian|Gardiner Range. A recessive unit, 150 m thick. Upper part contains brachiopods, trilobites, hyoliths and gastropods. Lateral equivalent of Hugh River Shale.||||Overlies Arumbera Sandstone. Is overlain by Illara Sandstone.|Red and green sandstone with beds and lenses of quartzic dolostone and calcareous sandstone, locally glauconitic.|
17941|Tempe Formation|67856|6|Mentioned|p338 fig 4-30|Cambrian|Cambrian|||Of Pertaoorta Group.||||
17941|Tempe Formation|68323|5|Briefly described|p1-6, p8-10, p12-13, p15|Middle Cambrian|Middle Cambrian|Within this unit are alternating zones of kaolin minerals with carbonate minerals, marking changes in pH and possibly different depositional environments; these may be useful in regional correlation.||Pertaoorrta Group.||Overlies Arumbera Sandstone.Is overlain by Petermann Sandstone.|Red-brown siltstone with characteristic pale green mottling, overlain by silicified chert breccia at the top.|
17941|Tempe Formation|69437|5|Briefly described|p22:10-11|Series 3|Series 3|Amadeus Basin, Centralian B Superbasin. Sequence 2. Nearshore to shallow-marine deposits.||||Overlies Chandler Formation. Is overlain by Cleland, Illara Sandstones.|Shale and siltstone, with lesser dolostone and sandstone.|12-JUL-16
17941|Tempe Formation|69438|4|Described|p23:2-3, 24, 28-30, 59-60|Middle Cambrian|Middle Cambrian|Ranford et al. (1965). Carmichael Sub-basin, Amadeus Basin. Predominantly recessive unit: poorly exposed. Average thickness about 150m; thickens to the S and SW. Facies change into Hugh River Shale. Is equivalent to Hugh River Shale and upper Giles Creek Dolostone. Hydrocarbon source rock intervals may be present. Could provide a seal for Arumbera Formation or over karst porosity in older carbonate rocks.||Pertaoorrta Group.||Disconformably/unconformably overlies Arumbera Sandstone, Chandler, Bitter Springs and Areyonga Formations. Is overlain disconformably by Illara and Cleland Sandstones.|Mainly shale and siltstone over a persistent basal sandstone sheet, with lesser dolostone, sandy dolostone, calcareous sandstone and locally glauconitic sandstone or dolostone. Upper part contains brachiopods, trilobites, hyoliths and gastropods.|12-JUL-16
17941|Tempe Formation|69439|6|Mentioned|p24:10|||Amadeus Basin.||||Correlated with the Bloodwood Formation (Ngalia Basin).||12-JUL-16
17941|Tempe Formation|69673|4|Described|p64 fig 53, p65, p80, p82, p88, p89, p91|||Potential source rock. On average around 150m thick.||||Disconformably overlies Chandler Formation, overlain by Cleland Sandstone, disconformably overlies Illara Sandstone|Shale and siltstone with lesser dolostone, sandy dolostone, calcareous sandstone and locally glauconitic sandstone or dolostone.|
17941|Tempe Formation|70752|6|Mentioned|p125, p129, p140-141|Middle Cambrian|Middle Cambrian|Amadeus Basin. Contains Middle Cambrian (Stage 4) brachiopods (described).||||||
17941|Tempe Formation|71001|6|Mentioned|p23|||||||||
17941|Tempe Formation|71114|4|Described|p171; p170 fig 1b,c; p175-180|Cambrian||Oldest unit in the western succession of the Amadeus Basin. Deposited between ~511 and 490 Ma. Nearshore to shallow shelf environments with minor marine incursions during Series 2, Stage 4 (Smith et al., 2015a) based on trilobite biostratigraphy. 242m thick in East Mereenie 4 well.|Likely max age 511 Ma.|||Is overlain by Illara Sandstone. In part age equivalent to Chandler Formation.|More sandstone- and siltstone-dominated towards top.|14-FEB-18
17941|Tempe Formation|71279|5|Briefly described|p355 Fig.2|Middle Cambrian|Middle Cambrian|Amadeus Basin.||Pertaoorrta Group.||||
17941|Tempe Formation|71898|4|Described|iii, p1, p3, p8-p11|Middle Cambrian|Middle Cambrian|Amadeus Basin.  Outcrops in the AREYONGA (5439) map sheet in strike valleys in the Gardiner Range, Walter Creek, Petermann Creek and Parana Hill anticlines.SHRIMP age is interpeted to be a maximum depositional age and supports the middle Cambrian age derived from its fossil assemblage of brachiopods, trilobites and gastropods (Wells et al, 1970; Shergold, 1986). This unit is interpreted as a nearshore to shallow-water shelf succession and has an average thickness of 150m. Sample location, description at location, zircon morphology, SHRIMP analysis, results and methods are discussed.|518 +/- 8 Ma (SHRIMP U-Pb)|Pertaoorrta Group||Unconformably overlies the Loves Creek Formation. Disconformably overlain by the Illara Sandstone.|Shale and siltstone with lesser dolostone, sandy dolostone, calcareous sandstone and locally glauconitic sandstone or dolostone.|19-NOV-18
17941|Tempe Formation|72358|6|Mentioned|p118|Series 3|Series 2|Of Amadeus Basin.||||||
17941|Tempe Formation|72516|6|Mentioned|p92|Cambrian|Cambrian|Amadeus Basin.||||Equivalent to the Arthur Creek Formation.||03-JUN-21
17941|Tempe Formation|73085|4|Described|piii, p1, p3-4, p7, p10-13|middle Cambrian|middle Cambrian|Amadeus Basin. 120 m thick in drillhole LA05DD01. In this drillcore, the upper 31 m is highly altered, and the basal 21 m comprises silicified, altered sandstone breccia with clasts of siltstone and chert. This [latter] interval defines the base of the unit and the basal contact is sharp and unconformable[?]. Sandstone below the silicified, altered sandstone breccia that were previously assigned to the unit were revised to be Arumbera Sandstone equivalents.||Pertaoorrta Group [and equivalents?]||Unconformably[?] underlain by Arumbera Sandstone[?]. Overlain by Illara Sandstone. Equivalent to Cleland Sandstone and Hugh River Shale. Partly underlain by Winnall Group and Chandler Formation.|Red to brown and buff to grey interbedded siltstone to fine-grained sandstone; weathered and kaolinised towards the top[?]. Silicified, altered sandstone breccia.|
17941|Tempe Formation|73119|4|Described|piii, p1, p16-18, Appendix|middle Cambrian|middle Cambrian|Amadeus Basin, central-west (Carmichael sub-basin). Poorly exposed in strike valleys in the Gardiner Range, Walters Creek, Petermann Creek and Parana Hill anticlines. Averages ~150 m thickness. Interpreted as a nearshore to shallow-water shelf succession containing offshore, shoreface, tidal flat, and bay and lagoon sediments. Brachiopods, trilobites and gastropods in the upper portion indicate an early Middle Cambrian age. Geochron is a new detrital zircon maximum depositional age, which is identical to previous age of 518 +/- 8 Ma (Kositcin et al., 2018). The majority of detrital zircons range from ca 1300 Ma to ca 1000 Ma; interpreted as sourced from the Musgrave, Warumpi, and Aileron provinces, either directly and/or through recycling and reworking of the underlying succession. [See article for provenance discussion].|518 +/- 6 Ma SHRIMP U-Pb|Pertaoorrta Group|||Predominantly recessive unit dominated by shale and siltstone, with lesser dolostone, sandy dolostone, calcareous sandstone, and locally glauconitic sandstone or dolostone.|
17944|Temple Bar Sandstone Member|35102|6|Mentioned|p27|||||||||
17944|Temple Bar Sandstone Member|43503|6|Mentioned|29|||||||||
17944|Temple Bar Sandstone Member|48992|2|Defined|p25|Neoproterozoic|Neoproterozoic|||||||
17944|Temple Bar Sandstone Member|50246|5|Briefly described|p8|Neoproterozoic|Neoproterozoic|Of the Heavitree Quartzite.||||||07-FEB-11
17944|Temple Bar Sandstone Member|61309|5|Briefly described|p17|||Of the Heavitree Quartzite. Geological Province: Amadeus Basin.||||||06-FEB-08
17944|Temple Bar Sandstone Member|62595|5|Briefly described|p8. |||||Unit in Heavitree Quartzite.|||Upward-fining unit; conglomerate and arkose.|
17944|Temple Bar Sandstone Member|73086|3|Fully described|p7, p9, p144|||Amadeus Basin. Of Stewart et al (1980). Type area: Heavitree Gap (112 m thick). Widespread, occurring along the entire northern margin of the basin. Contact with the overlying Fenn Gap Conglomerate Member is locally disconformable. [Also written as Temple Bar Member on p7; see Wells, 1967].||Heavitree Formation||Conformably underlain by Undoolya Siltstone Member. Overlain by Fenn Gap Conglomerate Member.||
17951|Tennant Creek Granite|22645|6|Mentioned|Table3 P213||Orosirian|||||||
17951|Tennant Creek Granite|23410|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Granite: biotite-bearing; rapakivi texture, and blue ovoid quartz; foliated to sheared in part, locally gneissic; locally abundant porphyritic granite enclaves, minor metasediment, and dolerite xenoliths; marginal alteration.||||||07-NOV-08
17951|Tennant Creek Granite|23733|3|Fully described|p14|Paleoproterozoic|Paleoproterozoic|Previously referred to as Tennant Creek granite complex and Red Bluff granite. Description given from the Red Bluff area.||||||07-NOV-08
17951|Tennant Creek Granite|23809|5|Briefly described|p27 Fig. 25, p29|Paleoproterozoic|Paleoproterozoic|Of the Tennant Creek Supersuite. The 1848Ma phase appears to intrude the Monument Formation (lower Flynn Group).||||||14-APR-15
17951|Tennant Creek Granite|24172|3|Fully described|p38, p63-64|Paleoproterozoic|Paleoproterozoic|Age: 1796Ma (Rb-Sr - Black, 1977); subsequently 1870+/-20Ma (U-Pb - Black, 1984); 1858+/-12Ma (zircon - Compston, 1991). Intrudes Warramunga Formation and the Flynn Subgroup.||||||14-APR-15
17951|Tennant Creek Granite|24197|5|Briefly described|p22, p68 Tb. 6.1|Paleoproterozoic|Paleoproterozoic|Of Tennant Creek Supersuite. Age: ~1850Ma. Geological province: Tennant Creek Inlier.||||||07-FEB-11
17951|Tennant Creek Granite|24294|5|Briefly described|p1168 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of the Flynn Subgroup (Churchills Head Group). Geological Province: Tennant Creek Inlier.||||||07-NOV-08
17951|Tennant Creek Granite|24567|5|Briefly described|p160 Tb. 2|Paleoproterozoic|Paleoproterozoic|Age: 1850Ma. Geological Province: Tennant Creek Inlier. Name written as Tennant Creek only under heading for GRANITE.||||||07-NOV-08
17951|Tennant Creek Granite|29135|4|Described|p38|||Informal use of name. -Pgu, -Pgt & -Pgv on Tennant Creek 1:250k sheet.||||||
17951|Tennant Creek Granite|39571|4|Described|p124|||Isotopic data.||||||23-DEC-08
17951|Tennant Creek Granite|41465|5|Briefly described|p9|||||||||
17951|Tennant Creek Granite|41961|6|Mentioned|Table 1 P39|||||||||
17951|Tennant Creek Granite|41970|6|Mentioned|p332|||||||||
17951|Tennant Creek Granite|42504|5|Briefly described|p61|||||||||
17951|Tennant Creek Granite|42853|5|Briefly described|p593|||See also Fig.1 p592.||||||23-DEC-08
17951|Tennant Creek Granite|42936|5|Briefly described|p546 Fig.1|||||||||
17951|Tennant Creek Granite|43223|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
17951|Tennant Creek Granite|43224|5|Briefly described|Map legend||Paleoproterozoic|||||||07-NOV-08
17951|Tennant Creek Granite|43749|6|Mentioned|p31|||Age: approx. 1830-1840 Ma.||||||11-DEC-06
17951|Tennant Creek Granite|43751|6|Mentioned|Fig.2,p610|||||||||
17951|Tennant Creek Granite|43832|6|Mentioned|88||Paleoproterozoic|Age in the range 1880-1800 Ma.||||||07-NOV-08
17951|Tennant Creek Granite|43850|4|Described|p262||Proterozoic|Now includes Red Bluff Granite. U-Pb zircon age 1858+/-12 Ma.||||||
17951|Tennant Creek Granite|46842|6|Mentioned|p114|||||||||
17951|Tennant Creek Granite|46964|6|Mentioned|p269|||||||||
17951|Tennant Creek Granite|46992|6|Mentioned|p253|||||||||
17951|Tennant Creek Granite|48860|14|Not recorded|Not recorded|||||||||
17951|Tennant Creek Granite|50353|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of 'Early' granite.||||||07-NOV-08
17951|Tennant Creek 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: 1858-1849 +/- 12Ma (Shrimp).||||||07-NOV-08
17951|Tennant Creek Granite|60684|2|Defined|p51 Appendix, p13|Paleoproterozoic|Paleoproterozoic|Intrusive two-feldspar, biotite- to biotite-bearing granite, predominantly alkali feldspar (microcline and orthoclase), sodic plagioclase (oligoclase), strained qrtz, and red-brown biotite. Intrudes Warramunga Fm. Age: 1858+/-12Ma, 1850+/-7Ma, 1848+/-7Ma||||||14-APR-15
17951|Tennant Creek Granite|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Tennant Creek Supersuite. Biotite granite, seriate porphyritic to equigranular; rapakiv texture; blue ovoid quartz; locally abundant enclaves, minor xeniliths; foliated, sheared in part, and locally gneissic. In the Tennant Creek region.||||||14-APR-15
17951|Tennant Creek Granite|64559|6|Mentioned|p973, p975 Fig. 8|||Age: 1858+/-12Ma (U-Pb).||||||23-DEC-08
17951|Tennant Creek Granite|65209|5|Briefly described|p35 Fig.1, p37, p39|Paleoproterozoic|Paleoproterozoic|Presented, in Fig.1, as Tennant Ck Granite||Tennant Creek Supersuite|||Deformed.|05-JAN-17
17951|Tennant Creek Granite|65222|5|Briefly described|p108 Tb 1, p110, p116-119, 119-120, 125|Orosirian|Orosirian|Shown as intruding Warramunga Formation rocks in Fig 9 p125. Previous data: 1648+/-50 Ma Rb-Sr at Red Bluff; 1870+/-20 Ma U-Pb. Four zircon sample localities from 3 plutons. 1853 +/- 10 Ma and 1849+/-7 Ma at Red Bluff.|1848 +/- 7 Ma to 1858 +/- 12Ma U/Pb SHRIMP.||||I-type.|24-JAN-22
17951|Tennant Creek Granite|65345|6|Mentioned|p11 Fig.11. |||||||||
17951|Tennant Creek 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, blue ovoid quartz, locally abundant enclaves, minor xenoliths; foliated, sheared in part, and locally gneissic.|
17951|Tennant Creek Granite|69187|4|Described|p51-54(incl Fig.2 and 3), p58 Fig.11,p59|Orosirian|Orosirian|Warramunga Province. Large intrusive complex. This age is indistinguishable from 1858 +/- 12 Ma age obtained by Compston(1995) for a nearby sample of Tennant Creek Granite.|crystallis'n 1851.1+/-3.5 Ma Pb/Pb SHRIMP zircon|Tennant Creek Supersuite||intrudes Warramunga Formation and Flynn Subgroup|granite; rounded to euhedral phenocrysts of K-feldspar, quartz and plagioclase in a medium- to coarse-grained matrix of quartz, K-feldspar, plagioclase and biotite|
17951|Tennant Creek Granite|69424|4|Described|p9:3, 6, 11-14, 16, 30|Paleoproterozoic|Paleoproterozoic|Warramunga Province. Syntectonic with the Tennant Event; previously dated at 1858 +/- 12 Ma (Compston, 1995). Various other ages given, down to 1846 +/- 3 Ma. E-trending 10-20m wide zones of mylonitisation or strong foliation with stretched quartz.|1850 +/- 4 Ma (Maidment et al., 2006).|Tennant Creek Supersuite.||Intrudes Warramunga Formation and undivided Ooradidgee Group.|Medium-grained, equigranular to seriate porphyritic biotite to biotite-bearing granite (syeno- to monzogranite); minor rapakivi texture; ovoid autoliths of porphyritic granodiorite, quartz monzonite and quartz diorite. Abundant and varied enclaves.|12-JUL-16
17951|Tennant Creek Granite|69917|5|Briefly described|p131 - 132|Orosirian|Orosirian|Warramunga Province, Tennant Region. Age from Maidment et al (2006)|1850+/-4Ma|Of Tennant Creek Supersuite||||
17951|Tennant Creek Granite|71592|5|Briefly described|Appendix A.|||Tennant Creek Region.|1853+/-10 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
17951|Tennant Creek Granite|73083|6|Mentioned|p44|||||||||
17951|Tennant Creek Granite|73124|6|Mentioned|p2 Fig.1|||||Tennant Creek Supersuite||||
17951|Tennant Creek Granite|73125|5|Briefly described|p2|Palaeoproterozoic|Palaeoproterozoic|Warramunga Province.||Tennant Creek Supersuite.||||
17951|Tennant Creek Granite|73460|6|Mentioned|p2|||Warramunga Province.||Tennant Creek Supersuite||||
17951|Tennant Creek Granite|73550|6|Mentioned|p25|||||||||
17951|Tennant Creek Granite|73590|6|Mentioned|p2|||||Tennant Creek Supersuite||||
17968|Teppa Hill Metamorphics|9199|5|Briefly described|Map legend|Precambrian|Precambrian|Of the Hayes Complex.  Muscovite-biotite-quartz-feldspar gneiss, amphibolite, quartzite.  Geological Province: Arunta Block.||||||03-NOV-04
17968|Teppa Hill Metamorphics|39887|6|Mentioned|Fig.3|||||||||
17968|Teppa Hill Metamorphics|60547|5|Briefly described|Map Legend|Precambrian|Precambrian|Of the Hayes Complex. Geological Province: Arunta Block. Muscovite-biotite-quartz-feldspar gneiss, amphibolite, quartzite.||||||
17968|Teppa Hill Metamorphics|69427|5|Briefly described|p12:14-15|||Wigley Domain, Aileron Province.||Hayes Metamorphic Complex.||Is intruded by Sadadeen Gneiss.|Biotite-muscovite schist and metasandstone, muscovite schist, and minor amphibolite and quartz-rich calc-silicate rock.|12-JUL-16
17968|Teppa Hill Metamorphics|71592|5|Briefly described|Appendix A.|||Arunta Orogen.|1120+/-9.9 Ma (metamorphism: U-Pb monazite).||||Metapelite.|
17975|Termite Range Formation|22453|6|Mentioned|p 12|||||||||
17975|Termite Range Formation|22665|5|Briefly described|Table1 P222, P227||Statherian|Age of unit is 1605+/-5 Ma and 1636+/-10 Ma.  Actually written as Termite Range Fmn.||||||11-DEC-06
17975|Termite Range Formation|22680|6|Mentioned|84|||Geological province: Mount Isa Basin. Of the McNamara Group.||||||11-DEC-06
17975|Termite Range Formation|23031|6|Mentioned|40|||Geological province: Lawn Hill Subprovince. Of the McNamara Group. Overlain by Lawn Hill Formation; underlain by Riversleigh Siltstone.||||||11-DEC-06
17975|Termite Range Formation|23072|5|Briefly described|p754|||||||||
17975|Termite Range Formation|23363|5|Briefly described|351 Tab.1|Statherian|Statherian|Age: 1636+/-10Ma.||||||11-DEC-06
17975|Termite Range Formation|23387|6|Mentioned|p18 fig.19|||Of McNamara Group.||||||
17975|Termite Range Formation|23393|4|Described|p19, p21|Paleoproterozoic|Paleoproterozoic|Of McNamara Group.  Age: 1636+/-10Ma, 1630+/-5Ma (Page & Sweet, 1998). Overlies the Riversleigh Siltstone; underlies the Lawn Hill Formation.||||||07-NOV-08
17975|Termite Range Formation|23396|5|Briefly described|p407 Fig.2|Statherian|Statherian|Of the McNamara Group.||||||11-DEC-06
17975|Termite Range Formation|23397|5|Briefly described|p473|Statherian|Statherian|Age: 1636+/-10Ma.||||||11-DEC-06
17975|Termite Range Formation|23398|4|Described|p452|Statherian|Statherian|Of McNamara Group.||||||
17975|Termite Range Formation|23405|4|Described|p566|Statherian|Statherian|Of McNamara Group. 1636+/-10Ma.||||||11-DEC-06
17975|Termite Range Formation|23408|5|Briefly described|p513 Fig.2|||Of the McNamara Group.||||||11-DEC-06
17975|Termite Range Formation|23409|4|Described|p535 Fig.2|Statherian|Statherian|Age: 1636+/-10Ma.||||||11-DEC-06
17975|Termite Range Formation|23448|5|Briefly described|p479|||||||||
17975|Termite Range Formation|23466|5|Briefly described|p272 Fig.6|Statherian|Statherian|||||||
17975|Termite Range Formation|23958|3|Fully described|p1139|Mesoproterozoic|Paleoproterozoic|Of McNamara Group. Maximum thickness: 1300m.||||||07-NOV-08
17975|Termite Range Formation|23964|5|Briefly described|p1268|Proterozoic|Proterozoic|Of McNamara Group.  Geological Province: Mount Isa Inlier.  Maximum thicknees: 1100m. See also p1269 Table 1.||||||
17975|Termite Range Formation|24308|5|Briefly described|p987 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of the McNamara Group.   Geological Province:  Mount Isa Superbasin.||||||07-NOV-08
17975|Termite Range Formation|24309|5|Briefly described|p1013|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17975|Termite Range Formation|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Of McNamara Group. Overlies Riversleigh Siltstone. Overlain by Lawn Hill Formation. Age: 1636-1630 Ma. Geological Province: Lawn Hill Platform.||||||11-DEC-06
17975|Termite Range Formation|37459|2|Defined|p432|Mesoproterozoic|Mesoproterozoic|Age is more specifically Carpentarian||||||
17975|Termite Range Formation|38237|4|Described|p130|||||||||
17975|Termite Range Formation|38291|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17975|Termite Range Formation|38310|6|Mentioned|p237|||||||||
17975|Termite Range Formation|38348|4|Described|p19|||||||||
17975|Termite Range Formation|38584|6|Mentioned|p22|||||||||
17975|Termite Range Formation|39497|6|Mentioned|p14|||See also Fig.4||||||
17975|Termite Range Formation|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17975|Termite Range Formation|39925|6|Mentioned|Fig.9|||||||||
17975|Termite Range Formation|43652|6|Mentioned|Fig.15,p393|||||||||
17975|Termite Range Formation|44922|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of McNamara Group.||||||
17975|Termite Range Formation|45166|5|Briefly described|p30|||||||||
17975|Termite Range Formation|50550|5|Briefly described|p1139 Fig.2||Statherian|Age: 1636-1630 Ma. Conformably overlies Riversleigh Siltstone, conformably overlain by Lawn Hill Formation. Geological Province: Western Fold Belt.||||||19-DEC-07
17975|Termite Range Formation|50600|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the McNamara Group.  Lithic and clayey sandstone, massive greywacke interbedded with shale and siltstone;  dark grey flaggy siltstone.||||||
17975|Termite Range Formation|60558|5|Briefly described|p5 Fig. 4|||Of McNamara Group. Overlain by Lawn Hill Formation, underlain by Riversleigh Siltstone.||||||
17975|Termite Range Formation|61936|5|Briefly described|p194 Fig. 6|||Geological Province: Lawn Hill Platform, Western Fold Belt, Mount Isa Inlier.||||||
17975|Termite Range Formation|62084|5|Briefly described|p936 Fig.5, p946 Fig.11, p948 Fig.13|Proterozoic|Proterozoic|Isa Superbasin. Lawn Hill. Shown as Termite Range Fm.||McNamara Group|||Variably dolomitic organic siltstones and shales.|
17975|Termite Range Formation|63109|6|Mentioned|p1108 Fig. 3|||Geological Province: Isa Superbasin. Consists of sandstone and conglomerate.||||||30-SEP-08
17975|Termite Range Formation|63111|5|Briefly described|p1164 Tb. 1, p1163 Fig. 3|Statherian|Statherian|Age: 1630+/-5 and 1636+/-10Ma. Geological Province: Isa Superbasin. Basal pebbly sandstones and conglomerate overlain by interbedded feldspathic and lithic sandstones and mudstones.||||||07-FEB-11
17975|Termite Range Formation|63113|5|Briefly described|p1214 Fig.2, p1225 Fig.13.|||Part of Term supersequence.|1630 Ma.|Of the McNamara Group||Overlies ?unconformably Riversleigh Siltstone. Is overlain by Lawn Hill Formation.||
17975|Termite Range Formation|63114|5|Briefly described|p1253 Fig.2. |||Isa superbasin.||Of the Term supersequence.||||
17975|Termite Range Formation|63115|6|Mentioned|p1279 Fig.4.|||Isa superbasin.||||||
17975|Termite Range Formation|63116|6|Mentioned|p1297 Fig.2,p1299 Tb.1,p1300, |||Isa superbasin. Material properties detailed.||||||
17975|Termite Range Formation|64250|6|Mentioned|p11 Fig.3|Statherian|Statherian||1630 +/- 5 Ma|Unit in McNamara Group.||||13-MAY-14
17975|Termite Range Formation|64317|6|Mentioned|p588 Fig. 1|||Appears in Fig. 1 as the term 'Lawn Hill and Termite Range Formation' but there is no reference in text.  Associated with the Termite Range Fault and Lawn Hill impact structure.||||||18-SEP-08
17975|Termite Range Formation|64575|6|Mentioned|p656 Fig. 1, p665|Proterozoic|Proterozoic|||||||
17975|Termite Range Formation|65228|5|Briefly described|p35, Fig.04.|Statherian|Statherian|Part of Term Supersequence in southern Lawn Hill Platform. SHRIMP zircon ages.|1636 +/- 10 Ma and 1630 +/- 5 Ma.|||Is overlain by Lawn Hill Formation.||
17975|Termite Range Formation|65337|5|Briefly described|p30.|||Correlative with Plain Creek Formation.|1647 +/- 8 to 1630 +/- 5 Ma (Page et al. 2000).|||Overlies Riversleigh Siltstone. Is overlain by Lawn Hill Formation.||
17975|Termite Range Formation|65396|5|Briefly described|p82, p175, p241|Statherian|Statherian|Isa Superbasin. Cover Sequence 3. Lawn Hill Platform.|1630 +/- 5 Ma|McNamara Group||Overlies Riversleigh Formation; overlain by Lawn Hill Formation.||04-APR-17
17975|Termite Range Formation|66843|6|Mentioned|p38 Fig.10|||||||||
17975|Termite Range Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot.|Paleoproterozoic|Paleoproterozoic|See also GIS attrib tbl, Mount Isa Block Time-Space Plot. Camooweal-Murphy and Century Domains, Mount Isa Inlier. Isa Superbasin.|1630 +/- 10 Ma (maximum depositional age).|McNamara Group.|||White to light brown and grey, thick bedded, fine to coarse, poorly sorted sandstone and lithic greywacke interbedded with laminated siltstone|
17975|Termite Range Formation|68542|6|Mentioned|p6|||||Upper McNamara Group||Disconformably overlies Riversleigh Siltstone, overlain by Lawn Hill Formation||
17975|Termite Range Formation|68576|5|Briefly described|Q_2: p6|||Lawn Hill Platform, Mount Isa Inlier.||Upper McNamara Group.||Overlies Riversleigh Siltstone. Is overlain by Lawn Hill Formation.||
17975|Termite Range Formation|68732|6|Mentioned|p165 Fig.3|Statherian|Statherian|Of the Term Supersequence. Sedimentary depositional age.|1630 +/- 5, 1636 +/- 10 Ma|||||
17975|Termite Range Formation|69591|4|Described|p43 Fig.2.31, p47, p54|||Camooweal-Murphy and Century Domains, Isa Superbasin. Constitutes the Term Supersequence. Submarine fan deposits: a series of medium- to coarse-grained clastic turbidite packages.|1636 +/- 10 Ma (MDA: Page et al., 2000).|McNamara Group.||Grades upwards into Lawn Hill Formation.|White to light brown and grey, thick-bedded, fine- to coarse, poorly sorted sandstone and lithic greywacke interbedded with laminated siltstone.|
17975|Termite Range Formation|69673|6|Mentioned|p54|||||||Correlated with Plain Creek Formation||
17975|Termite Range Formation|70897|6|Mentioned|Fig.1.7.7|||||||||
17975|Termite Range Formation|71369|5|Briefly described|p28|||||McNamara Group.||Is overlain unconformably by Schultz Sandstone Member.||
17975|Termite Range Formation|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1630+/-5 Ma (MDA: U-Pb zircon SHRIMP)||||Greywacke, siltstone, sandstone.|
17975|Termite Range Formation|71863|6|Mentioned|p2|Proterozoic|Proterozoic|Isa Superbasin.||||||
17975|Termite Range Formation|72408|4|Described|map sheet|Mesoproterozoic|Paleoproterozoic|Equivalent to the Term Supersequence.||||||
17975|Termite Range Formation|72415|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.||Unit of McNamara Group.|||Thin to medium-bedded, light brown clayey siltstone and ferruginous, fine to medium-grained sandstone|
17975|Termite Range Formation|72416|4|Described|map sheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet Geological Compilation Series.||Unit of Lawn Hill Formation.|||Thin to medium-bedded, light brown clayey siltstone and ferruginous, fine to medium-grained sandstone|
17975|Termite Range Formation|72418|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet.||Unit of McNamara Group.|||White to light brown and grey, thick bedded, fine to coarse-grained, poorly-sorted quartzose to lithic, occasionally ferruginous sandstone interbedded with laminated siltstone|
17975|Termite Range Formation|72421|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.||Unit of McNamara Group.|||White to light brown and grey, thick bedded, fine to coarse-grained, poorly-sorted quartzose to lithic, occasionally ferruginous sandstone interbedded with laminated siltstone|
17975|Termite Range Formation|72422|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.||Unit of McNamara Group.|||White to light brown and grey, thick bedded, fine to coarse-grained, poorly-sorted quartzose to lithic, occasionally ferruginous sandstone interbedded with laminated siltstone|
17975|Termite Range Formation|72423|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet Geological Compilation Series.||Unit of McNamara Group.|||Thin to medium-bedded, light brown clayey siltstone and ferruginous, fine to medium-grained sandstone. Thick bedded, poorly sorted sandstone interbedded with siltstone.|18-MAR-20
17975|Termite Range 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. Ages given as U-Pb zircon sedimentary depositional ages for lower and upper parts of the unit.|1636 +/- 10 Ma to 1630 +/- 5 Ma|McNamara Group||Overlies Riversleigh Siltstone and underlies Lawn Hill Formation.||
17975|Termite Range Formation|72527|6|Mentioned|p 132.|Statherian|Statherian|Described as being correlative with Riversleigh Siltstone.|c. 1647-1630 Ma|||Correlative with Riversleigh Siltstone Formation, Plain Creek Formation.|Includes tuffaceous volcanic material.|
17975|Termite Range 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 Lawn Hill Platform of the Mount Isa Province, and the East part of the South Nicholson Basin. U-Pb zircon sedimentary depositional ages given.|1630+/-5 Ma (upper), 1636+/-10 Ma (lower)|McNamara Group||Overlies Riversleigh Siltstone and underlies Lawn Hill Formation.|Includes dolomitic siltstone.|
17975|Termite Range Formation|72913|5|Briefly described|p4, p7, p8, p9 Tb.1, p18, p19, p26.|Paleoproterozoic|Paleoproterozoic|Shown as being in the eastern and Lawn Hill Platform part of the Isa Superbasin.  Identified in 2 wells in this study. Mineral composition boxplots reveal dominant quartz, muscovite, albite and microcline components.|1630 +/- 5 Ma|McNamara Group||Overlies Riversleigh Siltstone and underlies Lawn Hill Formation.|Includes dolomitic siltstone.|
17975|Termite Range Formation|72967|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|Lawn Hill Platform.||McNamara Group||||
17975|Termite Range Formation|73042|6|Mentioned|p4, p12-13|Statherian|Statherian|South Nicholson Basin region and Mount Isa Province, Isa Superbasin. Geochronology is a U-Pb zircon sedimentary depositional ages See Fig 1.2, p4 (?maximum depositional age).|1630 +/- 5 Ma, 1636 +/- 10 Ma|McNamara Group||Underlain by the Riversleigh Siltstone. Overlain by Lawn Hill Formation.||
17975|Termite Range Formation|73098|6|Mentioned|p4, p7, p39|||Lawn Hill Platform. Organic petrolography performed on one sample from the Amoco DDH 83-2 well. Laminated component is characterised by alternations of bitumen-lean and bitumen-rich layers. [See report for bitumen/maceral description]|||||Includes laminated and non-laminated dark brown to dark grey shale.|
17975|Termite Range Formation|73144|6|Mentioned|p8-9|Statherian|Statherian|Isa Superbasin. Part of the Term Supersequence. Leaky aquitard. Potential tight gas/oil. Includes oil show and gas show.||McNamara Group||Underlain by Riversleigh Siltstone. Overlain by Lawn Hill Formation.||
18039|The Granites Granite|22716|6|Mentioned|table4, p232|Statherian|Statherian|Age: 1790 Ma.||||||22-DEC-08
18039|The Granites Granite|23363|5|Briefly described|351 Tab.2|Statherian|Orosirian|Age: 1795+/-6Ma.||||||21-SEP-06
18039|The Granites Granite|23599|6|Mentioned|p15|||Geological Province: Granites-Tanami Inlier.||||||22-DEC-08
18039|The Granites Granite|23809|6|Mentioned|p11, p13|Paleoproterozoic|Paleoproterozoic|Age: 1795+/-6Ma (Ozchron, AGSO).||||||07-NOV-08
18039|The Granites Granite|24197|5|Briefly described|p7, p26|Proterozoic|Proterozoic|Of The Granites Supersuite. Geological province: Granites-Tanami Block.||||||07-FEB-11
18039|The Granites Granite|24567|5|Briefly described|p160 Tb. 2|Paleoproterozoic|Paleoproterozoic|Age: 1820Ma. Geological Province: Tanami Inlier. Name written as The Granites only under heading for GRANITE.||||||07-NOV-08
18039|The Granites Granite|29812|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
18039|The Granites Granite|31362|4|Described|Table 1|||||||||
18039|The Granites Granite|34810|6|Mentioned|p4|||||||||
18039|The Granites Granite|35227|6|Mentioned|Map legend|early Carpentarian|early Carpentarian|||||||
18039|The Granites Granite|36532|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
18039|The Granites Granite|39559|6|Mentioned|Table 1|||||||||
18039|The Granites Granite|39888|6|Mentioned|Fig.7|||||||||
18039|The Granites Granite|41465|6|Mentioned|p13|||||||||
18039|The Granites Granite|45140|2|Defined|p12-13, p15, p22-23, p25, p32-35, p37-38|Paleoproterozoic|Paleoproterozoic|See also p46, p74, p78, p83, Appx.p9-10. Hodgson (1976). The Granites-Tanami Block. Named after the abandoned gold mining settlement of The Granites; the type area is 1km S of there at 20deg 34'30"S, 129deg 21'10"E. Generally friable and highly weathered; locally forms tors and spheroidal boulders. Geochemistry detailed. Source of potable borewater at The Granites.|1780 +/- 24 Ma; Rb-Sr whole-rock: Page et al. 1976|||Is overlain by Muriel Range Sandstone. Intrudes Mount Charles Beds (Tanami Complex).|Pink and grey, locally porphyritic, biotite adamellite and associated minor aplite and pegmatite; cross-cutting quartz veins common; local poikilitic alkali feldspar crystals over 1 cm across.|
18039|The Granites Granite|46788|4|Described|p10|||||||||
18039|The Granites Granite|46864|6|Mentioned|p37|||Re age dates||||||
18039|The Granites Granite|50589|5|Briefly described|p1.4, 2.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Of the Granites Suite/Supersuite. Geological Province: Granites-Tanami Block. Age: 1795-1742 +/- 24Ma (Shrimp, Rb-Sr).||||||07-NOV-08
18039|The Granites Granite|61056|5|Briefly described|p778, p779 Tb. 1|Paleoproterozoic|Paleoproterozoic|Age: 1780+/-24Ma (whole rock samples).||||||07-NOV-08
18039|The Granites Granite|61246|5|Briefly described|p3|||Of the Grimwade Suite (?). Foliated monzogranite.||||||11-DEC-06
18039|The Granites Granite|63261|6|Mentioned|p16|||Included in the Grimwade Suite.||||||07-FEB-11
18039|The Granites Granite|69426|5|Briefly described|p11:10, 13, 21, 24|Statherian|Statherian|Blake et al. (1979). SHRIMP U-Pb zircon magmatic crystallisation age. An age of 1975 +/- 6 Ma (Smith, 2000) is also given [probably a misprint of 1795 Ma].|1791 +/- 4 Ma (Smith, 2001).|||||12-JUL-16
18039|The Granites Granite|71592|5|Briefly described|Appendix A.|||Tanami Orogen.|1795+/-6 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite, foliated monzodiorite.|
18088|Thorntonia Limestone|8187|5|Briefly described|Map legend|Cambrian|Cambrian|Overlies Black Stump Arkose; underlies Georgina Limestone.||||||21-JUN-04
18088|Thorntonia Limestone|9830|5|Briefly described|Map Legend|Cambrian|Cambrian|Dolomitic limestone, dolomite, chert nodules. Underlies O'Hara Shale, Roaring Siltstone. Overlies Mount Birnie Beds.||||||01-FEB-07
18088|Thorntonia Limestone|10116|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Micrite, silicified limestone, black shale, sandstone, siltstone, minor coquinite.||||||
18088|Thorntonia Limestone|12951|4|Described|p143, 146, 149, 154-155, 157|Middle Cambrian|Middle Cambrian|Georgina Basin. Dolomitic beds. Previously called lower Hay River Formation, lower Arthur Creek Formation [in various parts of the Basin?]. Electric logs and core correlations have allowed reduction of names for rocks of this age and lithology to just Thorntonia Limestone.||||Overlies Red Heart Dolostone disconformably. Unconformably overlain by Arthur Creek Formation.|Grey dolostone, minor dolopackstone and dolograinstones. Nodular evaporite and dissolution structures are common. Interbeds of dark carbonaceous mudstone. Locally siliciclastic sandstone, siltstone at base.|
18088|Thorntonia Limestone|22954|6|Mentioned|Fig3p9|Ordian-Early Templetonia||||||||
18088|Thorntonia Limestone|23031|6|Mentioned|17|||Geological  province: Georgina Basin.||||||11-DEC-06
18088|Thorntonia Limestone|23072|5|Briefly described|p754|||||||||
18088|Thorntonia Limestone|23393|5|Briefly described|p22|Middle Cambrian|Middle Cambrian|||||||
18088|Thorntonia Limestone|23408|5|Briefly described|p513|Middle Cambrian|Middle Cambrian|Geological province: Georgina Basin. carbonates.||||||15-JUN-09
18088|Thorntonia Limestone|23448|4|Described|p480|Cambrian|Cambrian|||||||
18088|Thorntonia Limestone|24308|5|Briefly described|p995 Fig. 8|||||||||
18088|Thorntonia Limestone|24419|5|Briefly described|p18|Late Cambrian|Middle Cambrian|Regionally extensive layer of rubbly black to white banded and convoluted chert and chert breccia (Ardmore Chert Member). Overlies Riversdale Formation; conformably underlies & interfingers with Beetle Creek Formation. Geological Province: Georgina Basin.||||||13-APR-05
18088|Thorntonia Limestone|24432|6|Mentioned|p565 Fig.4|||||||||
18088|Thorntonia Limestone|24442|5|Briefly described|p45|Middle Cambrian|Middle Cambrian|Comprises predominantly dolostone, with local basal terrigenous sediments and a medial interval bearing pyritic-carbonaceous black shale interbeds.  Geological Province: Georgina Basin.||||||11-DEC-06
18088|Thorntonia Limestone|26310|4|Described|p9, Table 1|Middle Cambrian|Middle Cambrian|Maximum thickness: 150 feet.  Limestone and dolomite.||||||
18088|Thorntonia Limestone|29940|6|Mentioned|p169|||||||||
18088|Thorntonia Limestone|30239|5|Briefly described|p1193|||||||||
18088|Thorntonia Limestone|30242|6|Mentioned|Fig.2|||||||||
18088|Thorntonia Limestone|30914|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
18088|Thorntonia Limestone|31396|6|Mentioned|Fig.3|||||||||
18088|Thorntonia Limestone|32576|5|Briefly described|p49|||||||||
18088|Thorntonia Limestone|32952|4|Described|p1188|||See also pp1189-1194,1204,1209. M.-U. Cambrian.||||||11-DEC-06
18088|Thorntonia Limestone|33111|4|Described|p43|||||||||
18088|Thorntonia Limestone|33113|6|Mentioned|Fig.1|||Mid.Camb.||||||
18088|Thorntonia Limestone|33387|6|Mentioned|p349|||||||||
18088|Thorntonia Limestone|33482|6|Mentioned|Fig.2|||Early Middle Cambrian. Phosphate in.||||||
18088|Thorntonia Limestone|34287|6|Mentioned|Fig.3|||||||||
18088|Thorntonia Limestone|34543|6|Mentioned|p98|||||||||
18088|Thorntonia Limestone|34847|6|Mentioned|Table 1|||Stratigraphy & hydrocarbon prospects||||||
18088|Thorntonia Limestone|34935|6|Mentioned|p274|||||||||
18088|Thorntonia Limestone|35001|6|Mentioned|Fig.45|||||||||
18088|Thorntonia Limestone|35032|6|Mentioned|p117|||||||||
18088|Thorntonia Limestone|35054|6|Mentioned|Table 23|||||||||
18088|Thorntonia Limestone|35121|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
18088|Thorntonia Limestone|35139|4|Described|Table.2|||||||||
18088|Thorntonia Limestone|35538|6|Mentioned|Fig.2|||||||||
18088|Thorntonia Limestone|35553|6|Mentioned|p176|||Appendix containing description of Agnostid localities.||||||
18088|Thorntonia Limestone|36234|3|Fully described|p167|||See also p162.||||||11-DEC-06
18088|Thorntonia Limestone|36243|6|Mentioned|Table 1A|||||||||
18088|Thorntonia Limestone|36448|5|Briefly described|p395|||||||||
18088|Thorntonia Limestone|36644|6|Mentioned|p213|||||||||
18088|Thorntonia Limestone|36645|5|Briefly described|p314|||Fig.3,2.||||||
18088|Thorntonia Limestone|36818|6|Mentioned|p203|||See also Plate 57.||||||
18088|Thorntonia Limestone|37572|4|Described|p157|||See also Figs.7 and 8 and p165.||||||11-DEC-06
18088|Thorntonia Limestone|37816|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
18088|Thorntonia Limestone|38209|5|Briefly described|p175|||||||||
18088|Thorntonia Limestone|38291|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
18088|Thorntonia Limestone|38348|6|Mentioned|p24|||||||||
18088|Thorntonia Limestone|38350|6|Mentioned|p22|||||||||
18088|Thorntonia Limestone|38442|5|Briefly described|Map legend|Cambrian|Cambrian|||||||25-AUG-04
18088|Thorntonia Limestone|38444|5|Briefly described|p105|||||||||
18088|Thorntonia Limestone|38446|6|Mentioned|Table 23|||||||||
18088|Thorntonia Limestone|38608|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
18088|Thorntonia Limestone|39029|5|Briefly described|Map legend|Cambrian|Cambrian|||||||25-AUG-04
18088|Thorntonia Limestone|39425|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
18088|Thorntonia Limestone|39445|5|Briefly described|Table 4|||See also p62.||||||11-DEC-06
18088|Thorntonia Limestone|39496|6|Mentioned|p16|||||||||
18088|Thorntonia Limestone|39562|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Grey crystalline limestone.||||||15-JUN-06
18088|Thorntonia Limestone|39690|6|Mentioned|Table 1|||||||||
18088|Thorntonia Limestone|39797|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
18088|Thorntonia Limestone|39921|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
18088|Thorntonia Limestone|39943|6|Mentioned|Table 2A|||||||||
18088|Thorntonia Limestone|40004|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
18088|Thorntonia Limestone|40137|6|Mentioned|p188|||||||||
18088|Thorntonia Limestone|40221|4|Described|p20|||||||||
18088|Thorntonia Limestone|40386|6|Mentioned|p429|||||||||
18088|Thorntonia Limestone|40623|5|Briefly described|p96|||See also p112.||||||11-DEC-06
18088|Thorntonia Limestone|40686|5|Briefly described|p407|||||||||
18088|Thorntonia Limestone|40810|6|Mentioned|p5|||||||||
18088|Thorntonia Limestone|40852|6|Mentioned|p37|||||||||
18088|Thorntonia Limestone|40855|6|Mentioned|p329|||||||||
18088|Thorntonia Limestone|40857|5|Briefly described|Table 21.1|||||||||
18088|Thorntonia Limestone|40858|5|Briefly described|p132|||||||||
18088|Thorntonia Limestone|41129|6|Mentioned|p17|||See also Fig.8.||||||13-SEP-18
18088|Thorntonia Limestone|41240|4|Described|p111|||||||||
18088|Thorntonia Limestone|41306|6|Mentioned|p4|||||||||
18088|Thorntonia Limestone|41388|6|Mentioned|Fig.2|||||||||
18088|Thorntonia Limestone|41639|6|Mentioned|p3|||||||||
18088|Thorntonia Limestone|42060|6|Mentioned|Fig.5 P140|||||||||
18088|Thorntonia Limestone|42070|6|Mentioned|p4|||||||||
18088|Thorntonia Limestone|42575|5|Briefly described|Fig.2 P335|||||||||
18088|Thorntonia Limestone|42956|5|Briefly described|p31 Fig.4|||||||||
18088|Thorntonia Limestone|43105|5|Briefly described|Fig.4,p9.|||||||||
18088|Thorntonia Limestone|43807|6|Mentioned|Fig.2,p347|||||||||
18088|Thorntonia Limestone|43883|14|Not recorded|p18 Fig.4-3|||See also Lexicon.||||||
18088|Thorntonia Limestone|44091|14|Not recorded|p16,Tb.1,p18||Middle Cambrian|||||||
18088|Thorntonia Limestone|44098|14|Not recorded|p98||Cambrian|||||||
18088|Thorntonia Limestone|44209|14|Not recorded|p140,145-146||Cambrian|||||||
18088|Thorntonia Limestone|44211|2|Defined|p96-98,101-109|||||||||
18088|Thorntonia Limestone|44213|14|Not recorded|Map Legend||Middle Cambrian|||||||
18088|Thorntonia Limestone|44271|14|Not recorded|p41|||See also Lexicon. Overlies Camooweal Dolomite. (lower Middle Cambrian)||||||
18088|Thorntonia Limestone|44273|14|Not recorded|Map Legend||Middle Cambrian|||||||
18088|Thorntonia Limestone|44274|2|Defined|Tb.1,p6,9,10,12,map||Middle Cambrian|Overlies? Camooweal Dolomite at Ixion Creek.||||||01-FEB-07
18088|Thorntonia Limestone|44275|14|Not recorded|Map Legend|||||||||
18088|Thorntonia Limestone|44276|2|Defined|p20,22,Tb.2,map|||||||||
18088|Thorntonia Limestone|44277|14|Not recorded|Map Legend||Middle Cambrian|||||||
18088|Thorntonia Limestone|44281|14|Not recorded|Map Legend||Middle Cambrian|||||||
18088|Thorntonia Limestone|44285|14|Not recorded|p.7|||||||||
18088|Thorntonia Limestone|44290|14|Not recorded|p439||Middle Cambrian|||||||
18088|Thorntonia Limestone|44309|2|Defined|Tb.1,p7-9,map|||No fossils. Unconformably overlies Precambrian.||||||
18088|Thorntonia Limestone|44326|14|Not recorded|Map Legend||Middle Cambrian|||||||
18088|Thorntonia Limestone|44441|14|Not recorded|p.8||Middle Cambrian|Middle Cambrian. Lawn Hill sheet (E54-9).||||||
18088|Thorntonia Limestone|44757|6|Mentioned|p153,155|||||||||
18088|Thorntonia Limestone|44920|14|Not recorded|Map Legend, Sheet2,4||Middle Cambrian|||||||
18088|Thorntonia Limestone|44922|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Underlies the Camooweal Dolomite.  Thin-bedded to massive dolomite and dolomitic limestone, Girvanella limestone.||||||01-JUL-04
18088|Thorntonia Limestone|44989|14|Not recorded|p.102,110,118-202|||On many pages.||||||
18088|Thorntonia Limestone|45052|3|Fully described|p92|||M.Camb.||||||
18088|Thorntonia Limestone|45055|6|Mentioned|p9|||See also p20,25,29,34.||||||13-SEP-18
18088|Thorntonia Limestone|45079|3|Fully described|p18|||||||||
18088|Thorntonia Limestone|45102|6|Mentioned|p43|||||||||
18088|Thorntonia Limestone|45130|6|Mentioned|Fig.2|||||||||
18088|Thorntonia Limestone|45166|5|Briefly described|Table 15|||||||||
18088|Thorntonia Limestone|46955|6|Mentioned|p159|||||||||
18088|Thorntonia Limestone|46959|6|Mentioned|Table 1|||||||||
18088|Thorntonia Limestone|47024|6|Mentioned|p1|||||||||
18088|Thorntonia Limestone|47044|6|Mentioned|p191|||||||||
18088|Thorntonia Limestone|47058|5|Briefly described|p119|||||||||
18088|Thorntonia Limestone|47083|5|Briefly described|p19||Cambrian|||||||
18088|Thorntonia Limestone|48906|14|Not recorded|Tb.1|||||||||
18088|Thorntonia Limestone|49027|6|Mentioned|p3|||||||||
18088|Thorntonia Limestone|50100|5|Briefly described|p22|Middle Cambrian|Middle Cambrian|Typically consists of silicified and commonly brecciated dolomite and chert; contains sparse fossils.  Disconformably overlies the Mount Birnie beds; disconformably overlain by Beetle Creek Formation and Roaring Siltstone.||||||
18088|Thorntonia Limestone|50550|6|Mentioned|p1146 Fig.9|||Geological Province: Western Fold Belt.||||||19-DEC-07
18088|Thorntonia Limestone|50600|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Overlies Border Waterhole Formation. Grey crystalline limestone and dolomite, some chert interbeds.||||||13-SEP-18
18088|Thorntonia Limestone|60122|3|Fully described|p15, p4-5, p11 Tb. 1|Middle Cambrian|Middle Cambrian|Limestone, dolostone; medial pyritic-carbonaceous black shale interbeds; basal terriginous sst, greywacke. mudstone. Disconformable on Red Heart Dolostone; disconformable below Arthur Cr Fm; nonconformable on Mount Tietkens Gr.Complex. Max. thick: 103m.||||||23-MAY-05
18088|Thorntonia Limestone|60123|4|Described|p5|Cambrian|Cambrian|Thickness: 103m. Disconformably overlies Red Heart Dolostone. Limestone, dolostone, black shale interbeds.||||||01-FEB-07
18088|Thorntonia Limestone|60264|5|Briefly described|p575 Fig. 1|Middle Cambrian|Middle Cambrian|Disconformably overlain by Monastery Creek Formation.  Geological Province: Burke River Inlier (Georgina Basin).||||||02-AUG-04
18088|Thorntonia Limestone|60359|5|Briefly described|Map Legend|Cambrian|Cambrian|Chert.||||||
18088|Thorntonia Limestone|60419|5|Briefly described|p18|Middle Cambrian|Middle Cambrian|Geological Province: Georgina Basin. Contains fauna of Ordian age.||||||
18088|Thorntonia Limestone|60590|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Dolostone, limestone; medial pyritic-carbonaceous black shale interbeds; basal terrigenous sandstone.  Overlies the Red Heart Dolostone (Tarlton Range area); overlain by Arthur Creek Formation.||||||25-NOV-04
18088|Thorntonia Limestone|60675|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Underlies Arthur Creek Formation. Dolostone, limestone; medial pyritic-carbonaceous black shale interbeds; basal terrigenous sandstone.||||||
18088|Thorntonia Limestone|61022|5|Briefly described|p14, p15 Fig. 2|Middle Cambrian|Middle Cambrian|Unconformably overlain by the lower Arthur Creek Formation.  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.||||||01-FEB-07
18088|Thorntonia Limestone|61155|5|Briefly described|p4|Cambrian|Cambrian|In northwest Queensland.||||||
18088|Thorntonia Limestone|61250|5|Briefly described|p43|Middle Cambrian|Middle Cambrian|Contains petroleum systems. Geological Province: Georgina Basin.||||||
18088|Thorntonia Limestone|61404|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Of the Narpa Group. Dolostone, limestone; medial pyritic-carbobaceous black shale interbeds; basal terrigenous sandstone. Geological Province: southern Georgina Basin.||||||
18088|Thorntonia Limestone|61904|5|Briefly described|p132 Fig. 2|Cambrian|Cambrian|||||||
18088|Thorntonia Limestone|62376|5|Briefly described|p53|Middle Cambrian|Early Cambrian|Geological Province: Georgina Basin.||||||09-FEB-10
18088|Thorntonia Limestone|62759|5|Briefly described|p1|||Geological Province: Georgina Basin. Contains extremely rich, oil-prone microbial source rocks.||||||05-FEB-08
18088|Thorntonia Limestone|62789|5|Briefly described|p128, p129 Fig. 2, p132|Middle Cambrian|Middle Cambrian|In southern Georgina Basin. Fossiliferous. 58 m thick in Pacific Oil & Gas Baldwin No. 1 exploration well.||||Overlies Early Cambrian Red Heart Dolostone and underlies Middle Cambrian Arthur Creek Formation.||28-MAR-12
18088|Thorntonia Limestone|62790|5|Briefly described|p207, p209, p210, Fig. 2|Middle Cambrian|Middle Cambrian|Southern Georgina Basin. Thickness of 58.1 m in the Pacific Oil & Gas Baldwin No. 1 well. ?Superseded Yelvertoft Beds.||||Overlies Errarra Formation and is overlain by Arthur Creek Formation.||28-MAR-12
18088|Thorntonia Limestone|62983|6|Mentioned|p11|||Geological Province: Georgina Basin.||||||
18088|Thorntonia Limestone|63062|6|Mentioned|p41|||Age equivalent of Jigaimara Formation. Geological Province: Georgina Basin.||||||07-FEB-11
18088|Thorntonia Limestone|63450|5|Briefly described|p76, p78 Fig. 5, p80|Middle Cambrian|Middle Cambrian|Unconformable over Monastery Creek Member (Beetle Creek Formation). Max.thickness: 100m. Geol. province: Georgina Basin, East Toko Synline and Burke River Structural Belt. Limestone, dolostone, black shale and minor sandstone and mudstone. See also p81.||||||07-FEB-11
18088|Thorntonia Limestone|64068|3|Fully described|p57-59, p82-87, p61, 44, 53, 54|Middle Cambrian|Middle Cambrian|Widespread. Potential hydrocarbon source and reservoir rock. Potential host for epigenetic, stratiform, sediment-hosted Pb-Zn. Has been recognised in southern Georgina Basin outcrop and drillholes in which it was formerly assigned variously to the Arthur Creek Formation, lower Hay River Formation or upper Hay River Formation Member 1. Detailed petrography is provided. Diverse Ordian fauna including trilobites Redlichia and Xystridura.||Of Narpa Group.|Includes chertified dolostone of Yelvertoft Bed and 'Ardmore Chert Member', and dolomitic-phosphatic Bronco Stromatolith Bed, all at top.|Disconformably overlies Andagera Formation.|Grey limestone, dolostone, pyritic-carbonaceous dolostone, marl and mudstone; minor nodular chert, phosphorite.|22-FEB-16
18088|Thorntonia Limestone|64317|5|Briefly described|p587, p588-589, p597|Middle Cambrian|Middle Cambrian|Annular outcrop with ~18km diameter - the Lawn Hill impact structure coincides with its outer margin.  Age is Ordian: 520-510Ma. Thickness: <100m, but within annulus may be up to 400m? Geol. prov: Georgina Basin. Mainly dolostone and dolomitic limestone.||||||13-SEP-18
18088|Thorntonia Limestone|64443|5|Briefly described|iii, p5-9, p6 Tb.1, p40|Ordian|Ordian-Early Templetonian|In Undilla Sub-basin. Max 121m thick. Shows pervasive recrystallisation, nodular evaporite, hydrocarbons.||Of Narpa Group.||Unconformably overlies undivided South Nicholson Group. Disconformably underlies Wonarah Formation.|Dolosparstone; minor bioclast and oncoid dolosparstone and intraclast dolowackestone to dolograinstone; basal dolomitic quartz sandstone and conglomerate sourced from Mittiebah Sandstone.|13-SEP-18
18088|Thorntonia Limestone|64575|6|Mentioned|p656 Fig. 1|Cambrian|Cambrian|||||||
18088|Thorntonia Limestone|64676|6|Mentioned|p23, p25|Middle Cambrian|Middle Cambrian|Georgina Basin.||||||
18088|Thorntonia Limestone|64778|6|Mentioned|p13, 25-26|Cambrian|Cambrian|Southern Georgina Basin. Potential hydrocarbon source.||||||
18088|Thorntonia Limestone|64812|4|Described|p236, p241-4 (figures),  p246, p251|Middle Cambrian|Middle Cambrian|Unconformably overlain by Arthur Creek Formation. Geol.Prov: Georgina Basin. Basin-wide, upward shallowing platformal, dolomitised limestone sequence; contains organic-rich shales which are prospective, noted as "hot shale" (Fig. 2). Max. thickness: 900m.||||||07-FEB-11
18088|Thorntonia Limestone|64813|5|Briefly described|p254, p255, p256 Fig. 2|Middle Cambrian|Middle Cambrian|Basal sst, siltst.or quartzitic dolostone,followed by interbedded carbonaceous mudstone; then erosional activity+deepening marine conditions resulted in anoxic, pyritic + carbonaceous, partly dolomitic shale = basal 'hot shale' of Arthur Creek Fm. above.||||||13-SEP-18
18088|Thorntonia Limestone|65237|4|Described|p3 Fig. 4, p6|Middle Cambrian|Middle Cambrian|Max. thickness: 100m. Geological province: southern Georgina Basin. Sheet-like, dolomitised limestone, with subordinate black shale; top of unit is a regional unconformity marked by karstification. Further lith. detail included.||||||07-FEB-11
18088|Thorntonia Limestone|65239|5|Briefly described|p2|Middle Cambrian|Middle Cambrian|Unconformably underlies Arthur Creek Formation. Geological province: Georgina Basin.||||||
18088|Thorntonia Limestone|65336|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of Narpa Group. Unconformably overlies Helen Springs Volcanics of Kalkarindji Volcanic Group; unconformably underlies Wonorah Formation of Barkly Group. Dolostone, limestone; medial pyritic-carbonaceous black shale interbeds; basal terrigenous sandstone.||||||
18088|Thorntonia Limestone|65337|6|Mentioned|p65.|Middle Cambrian|Middle Cambrian|Undilla Sub-basin, central and eastern Georgina Basin.||Unit in Narpa Group.||Unconformably overlies Kalkarindji Volcanic Group.||
18088|Thorntonia Limestone|65344|5|Briefly described|p3 Fig. 2 , p13, 24|||See thin section description for detail.||||Overlies South Nicholson Group. Overlain by Wonarah Formation.||
18088|Thorntonia Limestone|65345|5|Briefly described|pp1-2, p6 Fig.5, p8. |Cambrian|Cambrian|Georgina Basin. Positive tests in 1965-1966 for phosphate identified this unit as a target.||||Is unconformably overlain by Wonarah and Arthur Creek Formations.||
18088|Thorntonia Limestone|65489|5|Briefly described|p124-125, p127|Middle Cambrian|Middle Cambrian|Georgina Basin. Reservoir unit. Hosts the Lake Nash 1 tar and minor oil and gas show.||||Unconformably overlies Sylvester Sandstone. Is overlain by Monastery Creek Member (of Beetle Creek Formation).|Platform carbonates (dolomite).|
18088|Thorntonia Limestone|66767|5|Briefly described|p59|Middle Cambrian|Middle Cambrian|Southern Georgina Basin.||Narpa Group.|||Marine bioclastic carbonate rocks.|
18088|Thorntonia Limestone|67323|5|Briefly described|GIS attrib tbl, p72, p83, p92 Fig.12.2|Middle Cambrian|Middle Cambrian|See also Solid Geology Map. Georgina Basin. Contains Pb, Zn and Pb-Zn anomalies 50-75km NE of Camooweal.||Narpa Group.||Overlies Sylvester Sandstone and (unconformably) Mount Birnie beds and Colless Volcanics. Is overlain by Beetle Creek Formation and (unconformably) by Georgina Limestone.|Grey crystalline limestone.|
18088|Thorntonia Limestone|67402|4|Described|p25 tbl RRM3|Templetonian|Ordian|Georgina Basin, East Toko Syncline. Maximum thickness of 100m. Deposited in a restricted marine environment. See also p213 fig GRG3, p214, p215, p217.||||Overlain by the Marqua beds, Arrinthrunga Formation, Inca Formation or Georgina Limestone. Unconformably overlies the Red Heart Dolomite.|Limestone, dolostone, black shale and minor sandstone and mudstone.|
18088|Thorntonia Limestone|67870|5|Briefly described|p38-39, p43-48, p50-54|Middle Cambrian|Early Cambrian|Georgina Basin. Identified as a pair of strong continuous seismic reflections. Potential hydrocarbon source rocks: 2% TOC, and reservoir. Detailed modelling showing transformation ratios, expulsion mass (bulk) and expulsions mass for oil and gas.||Narpa Group.||Unconformably overlies Mount Birnie beds. Is overlain unconformably by Beetle Creek Formation or Inca Shale.|Sandstone, organic-rich (3% TOC) shale; sections of chert.|
18088|Thorntonia Limestone|68020|6|Mentioned|p126|Cambrian|Cambrian|Includes phosphorite deposits.||||||
18088|Thorntonia Limestone|69206|6|Mentioned|p2|||Georgina Basin.||||||
18088|Thorntonia Limestone|69297|6|Mentioned|p288|Middle Cambrian|Early Cambrian|Age equivalent of the Jigaimara Formation.||||||
18088|Thorntonia Limestone|69377|5|Briefly described|map legend|Cambrian|Cambrian|||Narpa Group|||Thick-bedded dolomitic limestone and dolomite with layers and nodules of chert|
18088|Thorntonia Limestone|69418|5|Briefly described|p3:36|Middle Cambrian|Middle Cambrian|Georgina Basin. Contains potentially prolific marine source rocks.||||||12-JUL-16
18088|Thorntonia Limestone|69437|5|Briefly described|p22:9-10, 15-16|Series 2|Series 2|Western Undilla Sub-basin, and southern Georgina Basin, Centralian B Superbasin. Sequence 1. Peritidal to marine deposits. Potential petroleum source and reservoir rock.||||Overlies Helen Springs Volcanics. Is overlain by Wonarah, Arthur Creek Formations. Correlated with Border Waterhole Formation.|Limestone, dolostone, marl, phosphorite and some siliciclastic rocks.|12-JUL-16
18088|Thorntonia Limestone|69439|6|Mentioned|p24:10|||Georgina Basin.||||||12-JUL-16
18088|Thorntonia Limestone|69443|4|Described|p28:12,14,16-17,20-22, 1,38-40,43,45-47|Middle Cambrian|Middle Cambrian|Opik (1956). Widely distributed. The "Mount Hendry Formation" is said to be "probably basal Thorntonia Limestone". From 23 to >400m thick; usually <100m. Diverse fossil assemblage (listed). Peritidal to marine deposits, partly dysoxic to anoxic in the S and SW of the Basin. Exposed and karstified in Middle-Late Cambrian. Also overlies Riversdale Formation unconformably or gradationally. Is overlain by Beetle Creek Formation conformably to disconformably; by Arthur Creek, Inca, Gowers Formations and Bronco Stromatolith Bed disconformably; by Currant Bush Limestone and Barkly Group unconformably. Lateral equivalent of Border Waterhole Formation. Associated with minor Pb-Zn mineralisation in the Marqua-Boat Hill area, and hosts high-grade phosphorite in the Marqua and Ammaroo/Barrow Creek areas (Foss Hill and Ammaroo deposits). With basal Arthur Creek Formation, forms a reservoir-seal couplet. Has high hydrocarbon yields and is a potential source rock. Also a potential petroleum reservoir.||Basal Narpa Group.|Yelvertoft Bed, "Ardmore Chert Member".|Overlies Colless Volcanics and "Mount Hendry Formation" gradationally; Andagera Formation and Red Heart Dolostone disconformably; Shadow Group and Mount Birnie beds unconformably.|Mainly marine bioclastic carbonate rocks: limestone, partially dolomitised limestone, dolostone, pyritic-carbonaceous dolostone, marl and mudstone; minor nodular chert and phosphorite. Local thin basal quartz sandstone or arkosic conglomerate lag.|12-JUL-16
18088|Thorntonia Limestone|69445|5|Briefly described|p30:5, 17|Middle Cambrian|Middle Cambrian|Central and eastern Georgina Basin.||||Unconformably overlies Colless Volcanics (Kalkarindji Suite).||12-JUL-16
18088|Thorntonia Limestone|69446|6|Mentioned|p31:3|||Georgina Basin. Broadly age-equivalent to Daly River Group(Daly Basin).||||||12-JUL-16
18088|Thorntonia Limestone|69447|6|Mentioned|p32:2|||Georgina Basin.||||Age-equivalent to Montejinni Limestone, Hooker Creek Formation and Lothari Hill Sandstone (Wiso Basin).||12-JUL-16
18088|Thorntonia Limestone|69448|6|Mentioned|p33:3|||Georgina Basin.||||Correlated with Negri Subgroup (Ord Basin) in part.||12-JUL-16
18088|Thorntonia Limestone|69561|5|Briefly described|p33 fig 2, p34|Ordian|Ordian|Ordian age confirmed by trilobite fossil assemblage in siltstone of overlying Arthur Creek Formation.||||Overlies Helen Springs Volcanics, Overlain by Wonarah Formation, Arthur Creek Formation|Limestone.|
18088|Thorntonia Limestone|69591|4|Described|p87-91, p94, p96-97|Cambrian|Neoproterozoic|Georgina Basin. Rarely >20m thick, but may be up to 100m thick. RELATED UNITS (continued): Is overlain by Inca Formation conformably, by Currant Bush Limestone, Blazan Shale or Age Creek Formation disconformably, and by Gowers Formation paraconformably.||Narpa Group.|Bronco Stromatolith.|Overlies Sylvester Sandstone (transitionally), Mount Birnie beds and (conformably) Riversdale Formation. Is overlain conformably by/locally grades into Beetle Creek Formation. See COMMENTS for more.|Includes thick-bedded dolomitic limestone, dolomite, phosphatic dolostone and bedded limestone with layers and nodules of chert. In places the limestone grades into shale, siltstone or fine sandstone. Richly fossiliferous.|
18088|Thorntonia Limestone|69673|4|Described|p116, p120,  p129,  p137, p138, p142,|Cambrian|Cambrian|23m - greater than 400m thick. Age derived from fossil assemblage.  Source rock with potential as a reservoir rock also.||Narpa Group||Disconformably overlain by Arthur Creek Formation|Limestone, dolomitised limestone, dolostone, pyritic carbonaceous dolostone, mudstone and marl with minor nodular chert and phosphorite.|07-MAR-23
18088|Thorntonia Limestone|70098|5|Briefly described|p7|||Georgina Basin. Approximate age equivalent of Jigaimara Formation.||||||
18088|Thorntonia Limestone|70303|5|Briefly described|iv, p15|Middle Cambrian|Middle Cambrian|Georgina Basin.||||Nonconformably overlies the Mount Tietkens Granite Complex.||
18088|Thorntonia Limestone|70321|6|Mentioned|p154-155|Cambrian|Cambrian|Riversleigh region. Overlain, down-cut and/or framed by much younger (Cenozoic/Tertiary) freshwater limestones containing vertebrate fossils. Their geochemical analyses tabulated.|~500 Ma.||||An extensive marine dolostone (variably dolomitised limestone).|
18088|Thorntonia Limestone|70380|6|Mentioned|p745|Stage 5|Stage 4|Georgina Basin.||||||
18088|Thorntonia Limestone|70723|5|Briefly described|p21-29, p31|Cambrian|Cambrian|Georgina Basin. Defined at the Thorntonia Station in Qld; known informally as Hay River Formation. Organic-rich shales have ben targeted for hydrocarbons: oil- and gas-prone source rock. Deposited in peritidal to marine environments under dysoxic to anoxic conditions. Kerogen type and biomarker compositions discussed in detail. Series 2-3 age.||Narpa Group||Overlies Red Heart Dolostone. Overlain by Arthur Creek Formation, Blazan Shale or Beetle Creek Formation.|Vuggy, partially dolomitized limestone, pyritic-carbonaceous dolostone, marl and mudstone. Abundant phosphatic shell fragments and algal mats.|
18088|Thorntonia Limestone|70752|6|Mentioned|p129, p141|Middle Cambrian|Middle Cambrian|Georgina Basin. Ordian. Brachiopod systematic palaeontological descriptions.||||||
18088|Thorntonia Limestone|70951|5|Briefly described|p1069,1072,1074,1076-1077,1080-1084|||Geological province: Georgina Basin. Dolomite-dominated in both SWIR and TIR wavelengths.||Unit of Narpa Group.||Overlain by Arthur Creek Formation. Underlain by basement.||
18088|Thorntonia Limestone|71502|5|Briefly described|p1-2, p8|Cambrian|Cambrian|Generally weakly phosphatised, especially in shallower depositional zones. Some exposures are silcretised. Overlies Proterozoic units of the Lawn Hill Platform. [Also written as Precambrian in Fig.8].||||Unconformably overlain by Carl Creek Limestone.|Marine carbonates with interbedded cherty material. Contains phosphatised stromatolites, ovoid phosphate nodules and invertebrate fossils. Extensively dolomitised.|
18088|Thorntonia Limestone|71621|6|Mentioned|p25|Middle Cambrian|Middle Cambrian|Georgina Basin. Unconformably overlies unnamed orthogneiss reported to have an igneous crystallisation age of 1846 ± 6 Ma.||||||02-FEB-19
18088|Thorntonia Limestone|72297|5|Briefly described|p752|Cambrian|Cambrian|Georgina Basin.|||||Contains thin oil shale beds.|
18088|Thorntonia Limestone|72321|5|Briefly described|Fig 2, p3, 4, 7|Wulian|Wulian|Undilla Sub-basin, Georgina Basin. Type area in Undilla Sub-basin where age Cambrian Series 3, Stage 5. Redefined to exclude older rocks (now Hay River Formation), across southern portion of the basin. Australian Stage: Templetonian.||of Narpa Group.||Correlated with the lower Arthur Creek Formation in the Dulcie Syncline.||
18088|Thorntonia Limestone|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 gradationally by Camooweal Dolomite. Underlain gradationally by Border Waterhole Formation.|Thick-bedded, dolomitic limestone and dolomite with layers and nodules of chert|
18088|Thorntonia Limestone|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 gradationally by Camooweal Dolomite. Underlain gradationally by Border Waterhole Formation.|Thick-bedded, dolomitic limestone and dolomite with layers and nodules of chert|
18088|Thorntonia Limestone|72515|5|Briefly described|Map Legend|Cambrian|Cambrian|Jervois Range Special Map Sheet. Georgina Basin. Contains fossil trilobites, brachiopods, molluscs.||Narpa Group||Disconformably overlain by the Arthur Creek Formation.|Limestone, dolomitised limestones, dolostone, pyritic-carbonaceous dolostone, marl, mudstone; minor nodular chert; phosphorate; local basal conglomerate, sandstone, greywacke.|
18088|Thorntonia Limestone|72516|3|Fully described|p12, p90-92|Cambrian|Cambrian|Georgina Basin. Occurs in HUCKITTA, ELKEDRA, SANDOVER RIVER, TOBERMORY, HAY RIVER, URANDANGI, DUCHESS, GLENORMISTON and JERVOIS RANGE SPECIAL map sheets. Contains fossil trilobites, archaeocipides, brachiopods and molluscs. Fossil assemblage indicates a Series 2 and Series 3 age of the Cambrian. Deposited in a peritidal to marine, partly dysoxic to anoxic environment. Thickness ranges from 23 to over 400m thick in the mapped area. Intersected in NTGS Huckitta 1 drillcore. Equivalent to the Gum Ridge Formation, Top Springs Limestone, Border Waterhole Formation and the Bronco Stromatolith Bed. Age equivalent of the Chandler Formation and the Giles Creek Dolostone of the Amadeus Basin.||Narpa Group||Disconformably overlain by the Arthur Creek Formation. Disconformably overlies the Red Heart Dolostone.|Limestone, dolomitised limestone, dolostone, pyritic-carbonaceous dolostone, marl, mudstone; minor nodular chert; phosphorate; local basal conglomerate, sandstone, greywacke.|02-JUN-21
18088|Thorntonia Limestone|72683|5|Briefly described|Map legend|Cambrian|Cambrian|Georgina Basin.||Narpa Group|||Thick-bedded , dolomitic limestone and dolomite with layers and nodules of chert.|
18088|Thorntonia 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||Underlies Roaring Siltstone and unconformably overlies the Shadow Group.|Thick-bedded, dolomitic limestone and dolomite with layers and nodules of chert and chert breccia.|
18088|Thorntonia Limestone|72967|6|Mentioned|p5|||Georgina Basin.||Napa Group||||
18088|Thorntonia Limestone|73288|5|Briefly described|p697-700, 702-703, 705, 707, 709 Fig.10|Middle Cambrian|Middle Cambrian|Southern Georgina Basin. Peritidal to marine platform setting. Non-economic oil and gas shows have been recorded. Downhole (Hylogger) logs; scratch test results tabulated. See also p710, 713.||Narpa Group.||Is overlain unconformably by Arthur Creek Formation.||07-MAR-23
18088|Thorntonia Limestone|73418|5|Briefly described|p3, p4 Fig.3|Miaolingian|Miaolingian|Georgina Basin, Burke River Structural Belt and Undilla Sub-basin.||Narpa Group||Overlies Hay River Formation, underlies Beetle Creek Formation|Limestone, commonly phosphatic near the top.|
18111|Ti-Tree Granophyre|9324|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Granophyre.||||||
18111|Ti-Tree Granophyre|32170|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
18111|Ti-Tree Granophyre|32307|4|Described|Table 1|||Carpentarian / L.Proterozoic||||||
18111|Ti-Tree Granophyre|32310|6|Mentioned|Map legend|Carpentarian|Paleoproterozoic|Carpentarian or Lower Proterozoic||||||07-NOV-08
18111|Ti-Tree Granophyre|32700|4|Described|Table 1|||Carpentarian. See also p13.||||||11-DEC-06
18111|Ti-Tree Granophyre|33376|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
18111|Ti-Tree Granophyre|33377|6|Mentioned|Table 1|||Re stratigraphy||||||
18111|Ti-Tree Granophyre|39889|6|Mentioned|Fig.1|||||||||
18111|Ti-Tree Granophyre|41645|4|Described|p16|||||||||
18111|Ti-Tree Granophyre|41660|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Altered and sheared granophyre; granophyric adamellite.||||||07-OCT-05
18111|Ti-Tree Granophyre|41661|5|Briefly described|Table 1|||||||||
18111|Ti-Tree Granophyre|41980|5|Briefly described|Table 3 P575|||||||||
18111|Ti-Tree Granophyre|42014|5|Briefly described|Map legend|Mesoproterozoic||||||||
18111|Ti-Tree Granophyre|43187|5|Briefly described|p2|||||||||
18111|Ti-Tree Granophyre|45112|5|Briefly described|Table 4|||||||||
18111|Ti-Tree Granophyre|48942|2|Defined|p24|Carpentarian|Carpentarian|||||||
18111|Ti-Tree Granophyre|67167|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Altered and sheared granophyre; granophyric quartz monzonite.|
18111|Ti-Tree Granophyre|67232|5|Briefly described|p16, p28.|||Crops out immediately adjacent to Woolianna Gabbro in WINGATE MOUNTAINS in Pine Creek Orogen. Contamination of Woolianna Gabbro by this unit produces 'crust-like' geochemical signature.||||||
18130|Tickalara Metamorphics|22469|6|Mentioned|p18, fig 21||Paleoproterozoic|Halls Creek Province||||||07-NOV-08
18130|Tickalara Metamorphics|22474|5|Briefly described|p20|Orosirian|Orosirian|Age: 1865 Ma.||||||14-NOV-06
18130|Tickalara Metamorphics|22526|3|Fully described|P679, P681, Fig2||Orosirian|Maximum age of unit is 1865 Ma.||||||14-NOV-06
18130|Tickalara Metamorphics|22537|6|Mentioned|34|Proterozoic|Proterozoic|||||||
18130|Tickalara Metamorphics|22547|4|Described|p13||Orosirian|In the Lamboo Complex, Halls Creek Orogen. Age: 1865 Ma. Overlain by Koongie Park Formation.||||||14-NOV-06
18130|Tickalara Metamorphics|22661|6|Mentioned|p 312|||||||||
18130|Tickalara Metamorphics|22716|5|Briefly described|table4, p232|Orosirian|Orosirian|Occurs in the central zone of Lamboo Complex.||||||
18130|Tickalara Metamorphics|22754|4|Described|p3|Paleoproterozoic|Paleoproterozoic|In the Lamboo Complex.||||||07-NOV-08
18130|Tickalara Metamorphics|22809|6|Mentioned|3|||||||||
18130|Tickalara Metamorphics|23323|4|Described|p454 Fig.2, p457 Fig. 4|Orosirian|Orosirian|Age: 1870-1850Ma.||||||07-FEB-07
18130|Tickalara Metamorphics|23383|6|Mentioned|p9, p5 Tb. 1|||Rocks mapped on ANGELO now recognised as being part of Koongie Park Formation.  Age: c.1865.  Geological Province: Hooper Orogen.||||||25-JAN-05
18130|Tickalara Metamorphics|23599|4|Described|p10|Paleoproterozoic|Paleoproterozoic|Age: c.1865 Ma. Geological Province: Lamboo Complex.||||||07-NOV-08
18130|Tickalara Metamorphics|23601|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|In the Lamboo Complex.||||||07-NOV-08
18130|Tickalara Metamorphics|23751|4|Described|p6|Paleoproterozoic|Paleoproterozoic|Age: c.1865 Ma. Geological Province: Lamboo Complex.||||||07-NOV-08
18130|Tickalara Metamorphics|23897|4|Described|p376, p377 Fig.1|Paleoproterozoic|Paleoproterozoic|Intruded by Sally Malay mafi-ultramafic intrusion.  Geological Province: Halls Creek Orogen.||||||07-NOV-08
18130|Tickalara Metamorphics|23925|5|Briefly described|p220 Fig. 2|Orosirian|Orosirian|Age: c. 1865 Ma.  Geological Province: Halls Creek Orogen.||||||
18130|Tickalara Metamorphics|24173|5|Briefly described|p7, p15|||Possible correlative of Milba Formation and of Halls Creek Group||||||06-APR-05
18130|Tickalara Metamorphics|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Age: 1865-1850Ma.  In the Lamboo Complex.||||||07-NOV-08
18130|Tickalara Metamorphics|24572|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Metamorphosed sedimentary rocks.  Age: >1835Ma.  Geological Province: Halls Creek Orogen.||||||07-NOV-08
18130|Tickalara Metamorphics|30097|6|Mentioned|Table 23|||See also Tables 24,27 and Fig.54.||||||
18130|Tickalara Metamorphics|30759|6|Mentioned|p16|||Map of East Kimberley Region||||||
18130|Tickalara Metamorphics|30892|6|Mentioned|p96|||Metamorphosed equivalent of Halls Creek Group.||||||14-NOV-06
18130|Tickalara Metamorphics|30895|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
18130|Tickalara Metamorphics|31230|6|Mentioned|p182|||||||||
18130|Tickalara Metamorphics|31828|6|Mentioned|p44|||Copper mineralisation||||||
18130|Tickalara Metamorphics|32659|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
18130|Tickalara Metamorphics|32660|5|Briefly described|Table 1|||||||||
18130|Tickalara Metamorphics|32728|5|Briefly described|p23|||See also p19.||||||14-NOV-06
18130|Tickalara Metamorphics|33812|5|Briefly described|p2|||Refers Gemuts (1971)||||||
18130|Tickalara Metamorphics|34604|4|Described|p250|||Proterozoic. Metamorphic zoning.||||||
18130|Tickalara Metamorphics|36551|6|Mentioned|p41|||||||||
18130|Tickalara Metamorphics|36885|3|Fully described|p167|||Formerly Halls Creek Metamorphics.||||||14-NOV-06
18130|Tickalara Metamorphics|37462|4|Described|Table 4.I|||Also described p225.||||||14-NOV-06
18130|Tickalara Metamorphics|38460|5|Briefly described|p1567|||||||||
18130|Tickalara Metamorphics|41158|6|Mentioned|p19|||||||||
18130|Tickalara Metamorphics|41465|6|Mentioned|p5|||||||||
18130|Tickalara Metamorphics|41594|6|Mentioned|Fig.15|||||||||
18130|Tickalara Metamorphics|41645|6|Mentioned|p4|||||||||
18130|Tickalara Metamorphics|41976|4|Described|p461|||||||||
18130|Tickalara Metamorphics|41977|5|Briefly described|p473|||||||||
18130|Tickalara Metamorphics|41987|6|Mentioned|p70|||||||||
18130|Tickalara Metamorphics|42326|5|Briefly described|p9|||||||||
18130|Tickalara Metamorphics|42329|5|Briefly described|p5|||See also Fig.2 p6.||||||14-NOV-06
18130|Tickalara Metamorphics|42730|5|Briefly described|p19|||||||||
18130|Tickalara Metamorphics|42757|6|Mentioned|p10|||||||||
18130|Tickalara Metamorphics|42768|6|Mentioned|Fig.6|||||||||
18130|Tickalara Metamorphics|43010|5|Briefly described|p37|||||||||
18130|Tickalara Metamorphics|43853|5|Briefly described|Map Legend||Proterozoic|||||||
18130|Tickalara Metamorphics|43855|5|Briefly described|Map Legend||Proterozoic|||||||
18130|Tickalara Metamorphics|43863|5|Briefly described|map legend|Proterozoic|Proterozoic|||||||
18130|Tickalara Metamorphics|43931|5|Briefly described|p20||Orosirian|Age: 1865 Ma. Geological province: Halls Creek Province.||||||14-NOV-06
18130|Tickalara Metamorphics|44155|5|Briefly described|p234-237, p240, p249, p254 Fig.3-40|Paleoproterozoic|Paleoproterozoic|U-Pb zircon age from pegmatite.|1854 +/- 6 Ma (Page and Hancock, 1988).|Lamboo Complex||?High-grade equivalent to Halls Creek Group. Faulted against Halls Creek Group. Intruded by Bow River Granite.|Schist, paragneiss, granulite, amphibolite, calc-silicates.|
18130|Tickalara Metamorphics|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Quartz-muscovite-biotite-cordierite hornfels; migmatitic quartz-plagioclase-muscovite-biotite(-sillimanite)-andalusite-cordierite(-chlorite) pelite, and amphibolite. Age: c.1865Ma. In the Lamboo Complex central zone.||||||07-NOV-08
18130|Tickalara Metamorphics|44317|4|Described|Table 1||Proterozoic|||||||
18130|Tickalara Metamorphics|44318|14|Not recorded|map legend||Proterozoic|Proterozoic.||||||
18130|Tickalara Metamorphics|44324|14|Not recorded|p.7||Proterozoic|Tb.1, (Proterozoic).||||||
18130|Tickalara Metamorphics|44325|14|Not recorded|map legend||Proterozoic|Proterozoic.||||||
18130|Tickalara Metamorphics|44363|5|Briefly described|p.7,8,9,22||Paleoproterozoic|Lower Proterozoic.  In the Lamboo Complex.||||||07-NOV-08
18130|Tickalara Metamorphics|44364|14|Not recorded|map legend|||||||||
18130|Tickalara Metamorphics|44366|14|Not recorded|p.9, Table 1||Proterozoic|||||||
18130|Tickalara Metamorphics|44367|14|Not recorded|map legend||Proterozoic|(Reprinted 1971). Part of Lamboo Complex. Undifferentiated.||||||14-NOV-06
18130|Tickalara Metamorphics|44397|14|Not recorded|p.8, Table 1||Proterozoic|Lamboo Complex.||||||
18130|Tickalara Metamorphics|44398|14|Not recorded|map legend||Proterozoic|||||||
18130|Tickalara Metamorphics|44693|5|Briefly described|Map Legend||Proterozoic|||||||
18130|Tickalara Metamorphics|44694|5|Briefly described|Map Legend||Proterozoic|||||||
18130|Tickalara Metamorphics|44868|5|Briefly described|Map Legend||Proterozoic|||||||
18130|Tickalara Metamorphics|45047|4|Described|p13|||See also pp19-24.  Age.||||||14-NOV-06
18130|Tickalara Metamorphics|45048|4|Described|p10|||See also p11, 23-51. Lower Proterozoic||||||14-NOV-06
18130|Tickalara Metamorphics|45087|6|Mentioned|p186|||Chemical analyses. See also p187, 224, 228, 230, 234.||||||14-NOV-06
18130|Tickalara Metamorphics|45112|6|Mentioned|p47|||||||||
18130|Tickalara Metamorphics|45140|5|Briefly described|p25|||Higher-grade equivalent to the Halls Creek Group. Age given is of the regional metamorphism; maximum age probably 2200 Ma.|1961 +/- 27 Ma (Dow and Gemuts, 1969).|Lamboo Complex.||||
18130|Tickalara Metamorphics|46797|6|Mentioned|p80|||Dates||||||
18130|Tickalara Metamorphics|50437|5|Briefly described|p3.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Age: 1850-1852 +/- 2Ma (Shrimp).||||||07-NOV-08
18130|Tickalara Metamorphics|60283|5|Briefly described|p24-29|||Halls Creek Orogen. Crops out as relatively flat plains.||||Is intruded by the Panton Intrusion.|Turbidites metamorphosed to granulite facies: quartz-feldspar-muscovite-biotite schists and gneisses.|
18130|Tickalara Metamorphics|60498|5|Briefly described|p1016 Fig.1, p1017 Table 1.|Paleoproterozoic|Paleoproterozoic||||Includes Norton metagabbro.||Amphibolite and granulite facies rocks.|03-JAN-18
18130|Tickalara Metamorphics|60519|5|Briefly described|Map Legend|Proterozoic|Proterozoic|In the Lambo Complex (Central Zone). Includes: Monkey Yard Tonalite, Fletcher Creek Monzogranite, Dougalls Tonalite.||||||14-NOV-06
18130|Tickalara Metamorphics|60533|6|Mentioned|p592, 593 Fig. 2, 595 Fig. 4, 597|Paleoproterozoic|Paleoproterozoic|Geological Province: Halls Creek Orogen. Age: ca 1865Ma. Overlain unconformably by Red Rock Formation.||||||07-NOV-08
18130|Tickalara Metamorphics|60724|4|Described|p10, p5 Fig. 2|Proterozoic|Proterozoic|Proposed that definition be expanded. Within the Lamboo Complex.||||||
18130|Tickalara Metamorphics|63866|4|Described|p129, p131|||Central Zone, Halls Creek Orogen. Numeric ages are interpreted as the maximum depositional ages for the sedimentary protoliths of this unit. The sedimentary protoliths to these rocks include turbiditic mudstone, siltstone, quartz sandstone, greywacke, chert, carbonates, BIF, mafic volcanics and bimodal sheet-like felsic intrusives. Ages also appear in Bodorkos et al, 1999, 2000a.|Ca. 1865 Ma (Page, OZCHRON)|||(Presumably) overlies the Milba Formation. Intruded by the Rose Bore Granite, Fletcher Creek Monzogranite, Dougall Tonalite and the Dougalls Suite.|Amphibolite and low-pressure granulite facies metasedimentary rocks and meta-igneous rodcks.|
18130|Tickalara Metamorphics|64104|6|Mentioned|p76, p77|Paleoproterozoic|Paleoproterozoic|Possible source of some clasts in Duerdin Group.|||||Schists and calc-silicate rocks.|
18130|Tickalara Metamorphics|64572|6|Mentioned|p802 Fig. 4, p803 Fig. 5|Paleoproterozoic|Paleoproterozoic|Age: ~1865Ma. Geological Province: Kimberley Craton.||||||22-DEC-08
18130|Tickalara Metamorphics|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Foliated, metamorphosed tonalite and granodiorite, monzogranite, syenogranite; locally migmatitic; Amphibolite; dioritic to gabbroic granulite; migmatitic pelite and psammite, BIF, calc-silicate rock, marble; local volcanic textures, carbonate, hornfels.||||||09-DEC-08
18130|Tickalara Metamorphics|64722|6|Mentioned|p9,10|||Of Halls Creek Orogen. An island arc assemblage accumulated on the southern and southwestern margins of the Kimberley Block. Probably a correlative of the Wangi Basics of the Halls Creek Orogen.||||||
18130|Tickalara Metamorphics|64731|5|Briefly described|pp164-165|Paleoproterozoic|Paleoproterozoic|Central Zone of Halls Creek Orogen. High-grade metamorphism at 1854 +/- 4 Ma (Page & Hancock 1988).||||||12-APR-12
18130|Tickalara Metamorphics|65413|6|Mentioned|p105 Fig.1, p106 Fig.2.|Paleoproterozoic|Paleoproterozoic|||Unit in Lamboo Complex.||||
18130|Tickalara Metamorphics|66526|5|Briefly described|p37.|Proterozoic|Proterozoic|Kimberley Province. Hosts Bow River nickel deposit. Correlated with Wangi Basics in Pine Creek Province. Produced in the Bow River Event, ME 6 in the Proterozoic Mafic-Ultramafic Magmatic Event Series.|c.1870 Ma.|||||
18130|Tickalara Metamorphics|66845|4|Described|p536 Fig.2, p537, p538, p541|Paleoproterozoic|Paleoproterozoic|Central zone of Lamboo Complex. ?Interrelated with Dougalls suite. Protoliths of this unit were intruded by leucogranite sheets, named Rose Bore Granite and Fletcher Creek Monzogranite ("Eastern Leucocratic Granitoid" of Ogasawara, 1988).|1865-1850 Ma|||intruded by Mabel Downs Tonalite||
18130|Tickalara Metamorphics|66846|6|Mentioned|p549 Fig.2, p552, p554, p556, p558|Orosirian|Orosirian|In the Central Zone of the Lamboo Complex.|||||?mafic volcanics and turbidites.|
18130|Tickalara Metamorphics|67232|5|Briefly described|p30, p34.|Paleoproterozoic|Paleoproterozoic|Central zone of Halls Creek Orogen. Possible correlative of Woolianna Gabbro, Pine Creek Orogen. Low- to high-grade, depleted metabasalt, representing an oceanic island arc/back-arc basin tectonic setting (Sheppard et al. 1999).|c.1865 Ma (Sheppard et al. 1999).|||||
18130|Tickalara Metamorphics|67779|6|Mentioned|p106 Fig.129, p107.|||Arc-related mafic rocks.||||||
18130|Tickalara Metamorphics|68078|6|Mentioned|p5|Paleoproterozoic|Paleoproterozoic|Age is of volcanic and associated sedimentary protoliths.|1865 Ma||||Metasediments and metavolcanics.|
18130|Tickalara Metamorphics|68656|5|Briefly described|GEOL_LUT_CSV/500k_geologyp08_lut|Paleoproterozoic|Paleoproterozoic||||||Mafic granulite, amphibolite, medium- to high-grade (migmatitic) pelite and psammite, BIF, calc-silicate rock and marble; local pillows and fragmental volcanic textures with interstitial carbonate, and hornfels.|
18130|Tickalara Metamorphics|69003|5|Briefly described|p5, p18-19, p22|||Central zone, Lamboo Province, Halls Creek Orogen.|c.1865 Ma.|||Is intruded by the Savannah intrusion.|Volcanic and associated rocks.|
18130|Tickalara Metamorphics|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen. Rb/Sr age:1920+/-27 Ma. SHRIMP age data from OZCHRON1. Original comment: 'This metamorphic age is based on 17 high-U concordant zircons or zircon rims, and is in good agreement with the conventional zircon data (1851 Ma).'|Metamorphic age: 1852+/-2 Ma U/Pb SHRIMP||Includes Fletcher Creek Granite, Rose Bore Granite and 18 unnamed units.||Mafic extrusive and intrusive meta-igneous rock with interlayered metasedimentary rock; minor metagranitic rock; includes mylonitic rocks: amphibolite, mafic granulite, ultramafic schist, migmatitic pelitic gneiss|04-AUG-15
18130|Tickalara Metamorphics|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also GA_geochron.csv.|1733-1920 Ma||||Mylonitized granitic rocks, amphibolite. Mafic granulite, ultramafic schist, amphibolite with interlayered migmatitic, pelitic and psammitic gneiss. Metamudstone, metasiltstone, metasandstone, metacarbonate.|
18130|Tickalara Metamorphics|69422|5|Briefly described|p7:1|||Central Zone, Halls Creek Orogen. Deformed and metamorphosed between 1865 and 1856 Ma and at 1854-1850 Ma.|||||Metasedimentary and meta-igneous rocks.|12-JUL-16
18130|Tickalara Metamorphics|69585|5|Briefly described|p2, p4|Orosirian|Orosirian|Central Lamboo Province. Represents an oceanic island arc.|||||Medium- to high-grade metasedimentary and mafic metavolcanic and metavolcaniclastic rocks.|
18130|Tickalara Metamorphics|69587|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic||||||Mafic granulite, amphibolite, medium- to high-grade (migmatitic) pelite and psammite, banded iron-formation, calc-silicate rock, and marble; local pillows and fragmental volcanic textures with intersitial carbonate, and hornfels|
18130|Tickalara Metamorphics|69597|5|Briefly described|p3, p5 |Paleoproterozoic|Paleoproterozoic|Central Lamboo Province. Intruded by sheets of 1850-1845 Ma tonalite.|1865 Ma||||Deformed and metamorphosed mafic volcanic rocks, volcaniclastics, turbidites.|
18130|Tickalara Metamorphics|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2; Hooper Orogeny; Hooper Orogeny D1/M1 - Central Zone. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 500k_interpgeop_lut.csv, 100k_interpgeol_lut.csv.|1865-1863 Ma (Inferred)||Includes Fletcher Creek Granite, Rose Bore Granite.||Amphibolite; interlayered pelite, psammite, calc-silicate, metamorphosed BIF and marble, mylonite, mafic granulite, metagabbro, ultramafic schist, migmatitic pelitic gneiss, quartz meta-sandstone, -siltstone, -mudstone, metabasalt|
18130|Tickalara Metamorphics|69747|5|Briefly described|p272|Orosirian|Orosirian|Geological province: Halls Creek Orogen. SHRIMP U-Pb dating of detrital zircons yield maximum depositional age of 1867-1864 Ma; crystallisation age of 1857-1855 Ma. Peak metamorphic age from SHRIMP U-Pb dating of monazite and metamorphic zircons of 1845+\-3 Ma and 1845+\-4 Ma respectively. Geochronological dates are derived from Hoatson, 1997; Page et al 1995a.||||||25-JUN-19
18130|Tickalara Metamorphics|70154|4|Described|100k_interpgeol_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|1850-1865 Ma||||Amphibolite containing garnet or clinopyroxene; relict primary layering and gabbroic textures. Mylonitized granitic rocks, mafic granulite, ultramafic schist, migmatitic pelitic gneis,metamudstone, metasiltstone, metasandstone and metacarbonate.|
18130|Tickalara Metamorphics|70731|5|Briefly described|p268-273,277-278|Orosirian|Orosirian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton. [Misspelt Ticklara Metamorphics on p278]. Associated with oceanic arc development of the central Lamboo Province at c. 1865 Ma outboard of the NAC. Deformed and metamorphosed to amphibolite and granulite facies at 1865-1856 Ma, and 1850-1845 Ma during the Hooper Orogeny (Blake et al., 2000a; Bodorkos et al., 1999; Bodorkos and Reddy, 2004; Page et al., 2001). Underwent rifting c. 1845-1840 Ma, resulting in formation of the Koongie Park Formation. Median density: 2850 kg/m3.||||||
18130|Tickalara Metamorphics|70812|4|Described|p3, p6, p8-p9, p12, p14|Orosirian|Orosirian|Central Zone of the Halls Creek Orogen, Lamboo Province. Metamorphosed at high temperature, low pressure amphibolite to granulite facies at 1865-1856 and 1850-1845 Ma during the Hooper and Halls Creek orogenies. Mineralisation is described. See also p18, p20, p24-p25, p27-p28, p31, p43.|c. 1865 Ma|||Intruded by the Dougalls Suite and the McIntosh Suite.|Mafic volcanic and volcaniclastic rocks, granulite facies rocks and migmatites.|
18130|Tickalara Metamorphics|70826|6|Mentioned|p9|Paleoproterozoic|Paleoproterozoic|||||||
18130|Tickalara Metamorphics|70851|4|Described|p3-p5, p7, p11-p12|Paleoproterozoic|Paleoproterozoic|Central Zone, Lamboo Province. Deformed and metamorphosed to amphibolite and granulite facies  during the Hooper Orogeny. Intruded by the c. 1856 Ma Panton Intrusion. Rock properties are provided and geophysical response is discussed. See also p17-p19, p23, p28-p29, p35.|c. 1865 Ma|||Intruded by the Panton Intrusion.|Sedimentary, mafic volcanic and volcaniclastic rocks.|
18130|Tickalara Metamorphics|71113|4|Described|p95-100,102-103,108-112|Orosirian|Orosirian|Geological province: Central Zone, Lamboo Province, Halls Creek Orogen. Intruded and metamorphosed by Dougalls Suite at 1850 Ma in an island arc (Sheppard et al., 2001) or convergent continental margin setting (Sheppard et al., 1997). Underwent regional HTLP metamorphism at 1845+\-4 Ma (Bodorkos et al., 1999; Oliver and Barr, 1997; Oliver et al., 1999; Thornett, 1986). Exposed units metamorphosed to granulite-facies, in faulted contact with non-metamorphosed Sally Downs Supersuite. Underwent rifting at 1845-1840 Ma at the end of Hooper Orogeny. Protolith sedimentary and igneous rocks may have been formed in either (1) an oceanic island arc setting above E-dipping subduction zone outboard of Kimberley Craton, or in (2) an ensialic marginal basin located closer to the margin of Kimberley Craton above a W-dipping subduction (Sheppard et al., 1999b). Geochemical analysis of depleted and enriched metabasalts indicate depleted light REEs signatures of both oceanic island arc/back-arc and MORB affinities (Sheppard et al., 199b). Numerical models with an active continental margin setup show the development of an ensialic marginal basin for deposition of the protoliths to the Tickalara Metamorphics and successfully replicate the geological evolution of the Lamboo Province.|1865 Ma|||Overlain by Koongie Park Formation. Intruded by Dougalls Suite. In fault contact with Sally Downs Supersuite.|Mafic volcanic and turbiditic sedimentary rocks.|
18130|Tickalara Metamorphics|71140|5|Briefly described|p95-103, 108-111|Orosirian|Orosirian|Oldest rocks in the Central Zone, Lamboo Province, Halls Creek Orogen. Intruded and metamorphosed c.1850 Ma. Rifting occurred 1845-1840 Ma.|c.1865 Ma.|||Is intruded by Dougalls Suite. Is faulted against Sally Downs Supersuite.|Low- to high-grade (granulite facies) metamorphosed turbiditic sedimentary and mafic submarine volcanic and volcaniclastic protoliths.|
18130|Tickalara Metamorphics|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma); Hooper Orogeny D2/M2 - Western Zone (1864-1850 Ma); Hooper Orogeny (1870-1850 Ma); Hooper Orogeny D1/M1 - Western Zone (1870-1864 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv, 100k_interpgeol_lut.csv and geochron files.|1865-1850 Ma (inferred)|Unit of Dougalls Suite.|Includes Fletcher Creek Granite, Rose Bore Granite, Corkwood Tonalite, Dead Finish Tonalite, Dougalls Tonalite, Monkey Yard Tonalite.||Amphibolite; interlayered pelite, psammite, calc-silicate, metamorphosed BIF and marble, mylonite, mafic granulite, metagabbro, ultramafic schist, migmatitic pelitic gneiss, quartz meta-sandstone, -siltstone, -mudstone, metabasalt|
18130|Tickalara Metamorphics|71281|5|Briefly described|p422|||Central Zone, Lamboo Province.||||Is intruded by Sally Downs Supersuite.|Dominated by a medium- to high-grade succession of metaturbidites, hosting mafic metavolcanic and volcaniclastic rocks with oceanic island-arc geochemical affinities.|
18130|Tickalara Metamorphics|71397|5|Briefly described|p4-6,14,44,47|Orosirian|Orosirian|Geological province: Central Zone, Lamboo Province, Halls Creek Orogen. Deposited in either an oceanic islandarc/ back-arc setting or an ensialic basin margin outboard of Kimberley Craton during east-directed subduction (Sheppard et al., 1999b; Griffin et al., 2000a). Evidence of deformation includes layer-parallel foliation and isoclinal folding at c. 1863-1850 Ma, and subsequent folding and medium to high T, LP metamorphism at c. 1845 Ma. Bodorkos et al. (1999) provided a maximum depositional age of c. 1865 Ma for sedimentary protoliths.|c. 1865-1850 Ma||||Middle to upper amphibolite to granulite facies mafic volcanic and intrusive rocks with interlayered metasedimentary and volcaniclastic rocks; MORB-like composition in lower part.|
18130|Tickalara Metamorphics|71873|5|Briefly described|p426-427,430,432,434-435,439-445|Orosirian|Orosirian|Geological province: Lamboo Province. Dominant in the Central Zone and comprises mafic volcanic (pillowed) and intrusive rocks with interlayered metasedimentary rocks at upper amphibolite to granulite facies. Comprises clasts of metamorphic and graphitic rocks, indicating a continental source. Metamorphosed to greenschist facies; folded and then intruded by Kevins Dam Suite. Magmatic-textured detrital zircons yield maximum depositional ages of 1869+\-4 and 1869+\-6 Ma. Contains recrystallized magmatic grains and metamorphic rims dated at 1862+\-6, 1864+\-15 and 1838+\-13 Ma. the c. 1860 Ma ages may have formed shortly after sediment deposition and are likely to be detrital metamorphic zircons. The younger age may represent metamorphic zircon formed in-situ within the sediment.|c. 1870 Ma||Includes Rose Bore granite.|||
18130|Tickalara Metamorphics|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Halls Creek Orogen.|||||Mafic extrusive and intrusive meta-igneous rock with interlayered metasedimentary rock; minor metagranitic rock.|
18130|Tickalara Metamorphics|72437|5|Briefly described|p5-p7, p14, p24, p41-44|Palaeoproterozoic|Palaeoproterozoic|Protoliths are intruded by leucogranite sheets. Two analyses are provided, one of the migmatite and one of the metaturbidite. Intruded by a zoned alkaline plug referred to as the Copperhead Albitite 'Carbonatite' Complex.|c. 1870 Ma||||Mafic amphibolite, granulite, migmatite and metaturbidite.|
18130|Tickalara Metamorphics|73089|5|Briefly described|p32-33, p37|Orosirian|Orosirian|Lamboo Province, Central Zone. Dominantly Paleoproterozoic detritus in metasedimentary rocks. Mafic volcanic rocks have geochemical characteristics that can be interpreted in terms of a back-arc/ensialic rift setting, or an oceanic arc.|c. 1875-1855 Ma||||Includes metasedimentary units and mafic volcanic rocks.|
18130|Tickalara Metamorphics|73427|6|Mentioned|p3|||North Australian Craton, Lamboo Province. Basalts may have formed during convergent margin processes.||||||
18163|Timber Creek Formation|14019|5|Briefly described|p4 Fig. 3|||Of the Bullita Group.  Geological Province: Victoria Basin.||||||
18163|Timber Creek Formation|24122|3|Fully described|p3, p5 Tb.1|Proterozoic|Proterozoic|Of Bullita Group. Conformably overlain by Skull Creek Formation and conformably overlies Seale Sandstone. Maximum thickness: 306m (on VICTORIA RIVER DOWNS).  Geological Province: Victoria Basin.||||||
18163|Timber Creek Formation|24297|3|Fully described|p8|Proterozoic|Proterozoic|Of Bullita Group.  Conformably overlain by Skull Creek Formation, conformably overlies Seale Sandstone. Maximum thickness: 306m. (in WATERLOO).  Geological Province: Victoria Basin.  See also p5 Tb. 2.||||||
18163|Timber Creek Formation|24298|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Bullita Group. Dolomitic siltstone and sandstone, minor dolostone and chert.||||||11-DEC-06
18163|Timber Creek Formation|24300|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Bullita Group.   Geological Province: Victoria Basin||||||11-DEC-06
18163|Timber Creek Formation|24441|4|Described|p1 Fig. 1, p7|Mesoproterozoic|Mesoproterozoic|Of Bullita Gp. Thinly interbedded very fine to medium sst, dolarenite, dolostone, dolomitic mudstone, and subordinate silty and quartzic dolostone.....Conformably overlies Seale Sst; overlain by Skull Creek Fm. Thickness: 306m. Geol.Prov: Victoria Basin.||||||11-DEC-06
18163|Timber Creek Formation|24442|5|Briefly described|p50 Fig. 1|||Of the Bullita Group. Geological Province: Victoria Basin.||||||
18163|Timber Creek Formation|28255|3|Fully described|p43-44, Tb. 11 (opp. p8)|Adelaidean|Adelaidean|Of the Bullita Group. Supersedes "Wave Hill Beds". Dolomitic siltstone and sandstone, dolomite. Conformably overlies Seale Sandstone (Wattie Group); grades up into Skull Creek Formation. Max. thickness: >200m. See also p130-131 Appendix.||||||17-JUN-05
18163|Timber Creek Formation|30003|4|Described|p7, p12|||Of the Bullita Group. Overlies the Seale Sandstone (Wattie Group). Carpentarian or Adelaidean. Max. thickness: 200m.||||||19-APR-05
18163|Timber Creek Formation|30004|6|Mentioned|Map legend|Proterozoic|Proterozoic|Carpentarian or Adelaidean||||||
18163|Timber Creek Formation|32175|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Bullita Group.  Interbedded dolomite, dolomitic sandstone and siltstone.||||||02-DEC-04
18163|Timber Creek Formation|32660|5|Briefly described|Table 6|||||||||
18163|Timber Creek Formation|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Bullita Group.  Dolomitic siltstone, siltstone; fine sandstone, dolomite, minor chert.||||||11-DEC-06
18163|Timber Creek Formation|32701|4|Described|Table 1|||Adelaidean. See p9. Of the Bullita Group.||||||11-DEC-06
18163|Timber Creek Formation|32775|5|Briefly described|Map legend|Adelaidean|Carpentarian|Of the Bullita Group.  Adelaidean or Carpentarian||||||02-DEC-04
18163|Timber Creek Formation|33373|3|Fully described|p9|||On Table 2.||||||
18163|Timber Creek Formation|33374|6|Mentioned|p7|||Strat.||||||
18163|Timber Creek Formation|33375|6|Mentioned|p8 Tb. 1, p12|Adelaidean|Adelaidean|Of the Bullita Group.   Interbedded fine sandstone, dolomite siltstone and dolomite; ripple marks, mud cracks and halite casts. Max. thickness: ~200m.||||||26-APR-05
18163|Timber Creek Formation|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
18163|Timber Creek Formation|33378|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Bullita Group. Interbedded fine grain sandstone, dolomitic siltstone, dolomite.||||||27-APR-05
18163|Timber Creek Formation|45112|6|Mentioned|p14|||||||||
18163|Timber Creek Formation|48938|2|Defined|p26|Proterozoic|Proterozoic|Measured section p89.  ?Adelaidean.||||||11-DEC-06
18163|Timber Creek Formation|48942|3|Fully described|p47|||Strat. section p110.||||||11-DEC-06
18163|Timber Creek Formation|48943|2|Defined|p51|Adelaidean|Adelaidean|||||||
18163|Timber Creek Formation|60006|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Victoria Basin. Of Bullita Group. Silty dolostone, dolomitic siltstone, sandstone, minor dolarenite||||||
18163|Timber Creek Formation|60672|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Silty dolostone, dolomitic siltstone, sandstone, minor dolarenite and dolostone. Unconformably overlies Wattie Group. Overlain by Skull Creek Formation. Of Bullita Group. Geological Province: Victoria Basin.||||||11-JAN-05
18163|Timber Creek Formation|60682|4|Described|piii, 8|Mesoproterozoic|Mesoproterozoic|Of the Bullita Group. Overlies Wattie Group. Conformably grades up into Skull Creek Formation, unconformably overlain by Jasper Gorge Sandstone. Thickness: 110m. Dolostone, doloutite, siltstone, dolarenite and sandstone. Geol. Province: Victoria Basin.||||||
18163|Timber Creek Formation|60685|3|Fully described|p4 Fig. 3, p8|Mesoproterozoic|Mesoproterozoic|Of the Bullita Group. Sandstone, dolarenite, dolostone, dolomitic mudstone. Conformable on Seale Sandstone; conformable beneath Skull Creek Formation.  Max. Thickness: 306m. Geological Province: Victoria Basin.||||||
18163|Timber Creek Formation|65331|5|Briefly described|Map legend|Mesoproterozic|Mesoproterozic|Of Bullita Group, Victoria Basin.  Silty dolostone, dolomitic siltstone, sandstone, minor dolarenite||||||
18163|Timber Creek Formation|65342|6|Mentioned|p11 Fig.13. |||Victoria Basin.||Unit in Bullita Group.||Overlies Seale Sandstone of the Wattie Group. Is overlain by Skull Creek Formation.||
18163|Timber Creek Formation|67151|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Birindudu Basin.||Unit in Bullita Group.||Unconformably overlies Seale Sandstone. Is overlain by Skull Creek Formation.|Silty dolostone, dolomitic siltstone, sandstone; minor dolomitic sandstone and dolostone.|
18163|Timber Creek Formation|68733|5|Briefly described|p177 Fig.2|||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.||||
18163|Timber Creek Formation|69432|4|Described|p17:2, 10, 14-15|||Birrindudu Basin. Over 300m thick. Contains live oil (probably sourced from Wattie Group) and pyrobitumen; also diagenetic chert nodules, disseminated pyrite and locally epigenetic galena. Minor barite occurs in carbonate rocks.||Bullita Group.||Partial lateral equivalent of Skull Creek Formation.|Thinly interbedded siltstone, fine sandstone and dolostone. Generally the carbonate content increases up-section. Biohermal and biostromal stromatolites, cauliflower chert, gypsum pseudomorphs and halite casts common.|12-JUL-16
18163|Timber Creek Formation|69441|5|Briefly described|p26:3 Tb. 26.1|||Birrindudu Basin.||Bullita Group.||Is overlain unconformably by Jasper Gorge Sandstone (Auvergne Group).||12-JUL-16
18163|Timber Creek Formation|69673|6|Mentioned|p48 fig 35, p50|||"live" oil bleeds found in this formation.||Bullita Group||Overlies Seale Sandstone, overlain by Skull Creek Formation||
18163|Timber Creek Formation|70206|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Birindudu Basin [misspelling of Birrindudu Basin].||Bullita Group|||Dolomitic siltstone, silty dolostone and sandstone, minor dolostone and chert.|18-JUL-16
18163|Timber Creek Formation|70655|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Birindudu Basin.||Bullita Group.||Unconformably overlies Seale Sandstone. Is overlain by Skull Creek Formation, and unconformably by Jasper Gorge Sandstone.|Silty dolostone, dolomitic siltstone, sandstone; minor dolomitic sandstone and dolostone.|
18163|Timber Creek Formation|70850|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Bullita Group.||Is overlain conformably by Skull Creek Formation.|Dolomitic siltstone, silty dolostone and sandstone, minor dolostone and chert.|
18163|Timber Creek Formation|70854|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Bullita Group.||Unconformably overlies Seale Sandstone (Bullita Group). Is overlain by Skull Creek Formation and Antrim Plateau Volcanics.|Silty dolstone, dolomitic siltstone, sandstone, minor dolarenite and dolostone.|21-SEP-17
18163|Timber Creek Formation|70855|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Bullita Group.||Overlies Seale Sandstone (Wattie Group). Is overlain by Skull Creek Formation, and unconformably by Jasper Gorge Sandstone.|Dolomitic siltstone, silty dolostone and sandstone, minor dolostone and chert.|
18163|Timber Creek Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, dolostone|
18163|Timber Creek Formation|71302|5|Briefly described|p6,22||Paleoproterozoic|Of Birindudu Basin.||Unit of Bullita Group.||Underlain conformably by Seale Sandstone/Wattie Group.||
18163|Timber Creek Formation|72718|6|Mentioned|p7|||Birrindudu Basin.||Bullita Group||Underlain by Seale Sandstone (Wattie Group). Overlain by Skull Creek Formation.||
18189|Tin Camp Granite|9534|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Altered pink biotite granite.||||||07-NOV-08
18189|Tin Camp Granite|9691|5|Briefly described|Map Legend|||Altered pink biotite granite, anomalously radioactive, commonly with north trending quartz filled shears: anatectic granite.||||||
18189|Tin Camp 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
18189|Tin Camp Granite|9733|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Altered pink biotite granite, anomalously radioactive; commonly with north trending quartz filled shears; anatectic granites.||||||
18189|Tin Camp 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
18189|Tin Camp Granite|36085|6|Mentioned|p502|||||||||
18189|Tin Camp Granite|36535|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
18189|Tin Camp Granite|36635|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
18189|Tin Camp Granite|37815|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
18189|Tin Camp Granite|38884|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
18189|Tin Camp Granite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
18189|Tin Camp Granite|40489|6|Mentioned|p88|||||||||
18189|Tin Camp Granite|41146|6|Mentioned|p858|||||||||
18189|Tin Camp Granite|41406|6|Mentioned|Map legend|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
18189|Tin Camp Granite|46639|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Age: 1755+/-15Ma. Altered pink and cream biotite granite and trondhjemite, anomalously radioactive.||||||07-NOV-08
18189|Tin Camp Granite|46700|5|Briefly described|P28, Table1 P10||Statherian|Age of unit is 1755 Ma||||||
18189|Tin Camp Granite|46824|6|Mentioned|Table 1|||See also p322.||||||11-DEC-06
18189|Tin Camp 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: 1758 +/- 20Ma (Rb-Sr).||||||07-NOV-08
18189|Tin Camp Granite|60550|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Altered pink biotite granite, anomalously radioactive, commonly with north trending quartz filled shears: anatectic granites.||||||
18189|Tin Camp Granite|61206|5|Briefly described|p516, p517 Fig.1,|Early Proterozoic|Early Proterozoic|||||Intrudes Myra Falls Metamorphics.|K-U-Th-rich granites.|
18189|Tin Camp Granite|63866|5|Briefly described|p112|Orosirian|Orosirian|Nimbuwah Domain, Pine Creek Orogen. Numeric age is interpreted as the age of igneous crystallisation.|1846 +/- 13 Ma (Worden et al, in review)|David Suite||||
18189|Tin Camp Granite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1820-1850Ma. Of Cullen Supersuite. I-type. Altered pink biotite granite and trondjhemite. Intrudes Nimbuwah Complex and Cahill Formation.||||||07-JAN-09
18189|Tin Camp Granite|64956|5|Briefly described|p2 Tb. 7, p64|Paleoproterozoic|Paleoproterozoic|Intrudes Nimbuwah Complex grandiorite migmatites; faulted against Oenpelli Dolerite; unconformably overlain by Kombolgie Subgroup. Cryst. Age: 1846+/-13Ma. Geological province: Pine Creek Orogen. Pervasively altered biotite granite.||||||07-FEB-11
18189|Tin Camp Granite|66683|5|Briefly described|pp367-369.|||Unconformably overlain by Kombolgie Subgroup, basal McArthur Basin.|1846 +/- 13 Ma.|||||11-OCT-11
18189|Tin Camp Granite|67057|5|Briefly described|p454. |Paleoproterozoic|Paleoproterozoic|Post-orogenic intrusion.|1846 +/- 13 Ma (Worden et al. 2008b).|||||
18189|Tin Camp Granite|67564|6|Mentioned|p85.|Paleoproterozoic|Paleoproterozoic|Eastern Pine Creek Orogen.||Unit in David Suite.||||
18189|Tin Camp Granite|67779|4|Described|p6 Fig.5, p8 Table 1, pp26-31, p64, p107|Paleoproterozoic|Paleoproterozoic|Nimbuwah Domain, Pine Creek Orogen. Undeformed (ie post-collisional), A-type granite. Another age given is 1842 +/- 12 Ma (Pb/Pb: Hollis et al. in press). Has an exceptionally high Th and U radiometric response. Geochemistry and geochronology are detailed.|1844 +/- 9 Ma (Worden et al. 2008b).|Unit in Jim Jim Suite.||Intrudes Nimbuwah Complex and Kukalak Gneiss. Is faulted against Oenpelli Dolerite. Is overlain unconformably by Mamadawerre Sandstone.|Altered pale pink to cream biotite granite: anomalously radioactive, commonly with north-trending quartz-filled shears; anatectic granite; locally coarse-grained and perthitic.|
18189|Tin Camp Granite|69420|4|Described|p5:18, 21, 23, 25-26|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. A late-orogenic, undeformed granite. Mineralogy and petrology/geochemistry summarised. Geochronology (based on only 8 analyses) by Worden et al. (2008).|1846 +/- 13 Ma: SHRIMP U-Pb zircon.|Jim Jim Suite.||Intrudes Nimbuwah Complex. Is overlain unconformably by Kombolgie Subgroup.|Biotite granite, trondhjemite and porphyritic granite; pervasively altered and enriched in Th and U.|12-JUL-16
18189|Tin Camp Granite|69917|5|Briefly described|p40-41|Orosirian|Orosirian|Pine Creek Orogen, Nimbuwah Domain.  U/Pb LA-ICPMS zircon dating (herein) agrees with 1846+/-13 Ma SHRIMP U-Pb age reported by Worden et al 2008.|1842+/-12 Ma||||K-feldspar-rich perthitic granite.|
18189|Tin Camp Granite|70853|5|Briefly described|Map legend.|Orosirian|Orosirian||1844 Ma.||||Altered pale pink to cream biotite granite: anomalously radioactive, commonly with north-trending quartz-filled shears; anatectic granite; locally coarse-grained and perthitic.|
18189|Tin Camp Granite|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen. Age determination by U-Pb zircon LA-ICPMS.|1842+/-12 Ma (crystallisation).||||Coarse-grained K-feldspar-rich perthitic granite.|
18263|Toko Group|10116|5|Briefly described|Map Legend|Middle Ordovician|Early Ordovician|Includes: Nora Formation, Carlo Sandstone, Mithaka Formation, Ethabuka Sandstone.||||||
18263|Toko Group|13995|6|Mentioned|p77|||Georgina Basin.||||||
18263|Toko Group|24065|4|Described|p235|Middle Ordovician|Early Ordovician|Geological Province: Georgina Basin.||||||
18263|Toko Group|30914|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
18263|Toko Group|31714|6|Mentioned|Fig. 4|||||||||
18263|Toko Group|33111|6|Mentioned|p17|||||||||
18263|Toko Group|33738|6|Mentioned|p54|||||||||
18263|Toko Group|34252|6|Mentioned|Po.2|||Fossils||||||
18263|Toko Group|34454|5|Briefly described|Table 2|||Ordovician||||||
18263|Toko Group|35121|6|Mentioned|Map legend|Middle Ordovician|Middle Ordovician|||||||
18263|Toko Group|35139|6|Mentioned|p16|||||||||
18263|Toko Group|35146|6|Mentioned|p468|||||||||
18263|Toko Group|36234|6|Mentioned|Fig.1|||||||||
18263|Toko Group|36473|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian to Ordovician||||||
18263|Toko Group|36580|1|Redefined|p473|Middle Ordovician|Early Ordovician|Early to Middle Ordovician. See also Fig.1||||||
18263|Toko Group|37572|6|Mentioned|p164|||||||||
18263|Toko Group|37727|6|Mentioned|Fig.1|||||||||
18263|Toko Group|37735|6|Mentioned|p12|||Assigned to the wrong state.||||||
18263|Toko Group|38832|6|Mentioned|p157|||||||||
18263|Toko Group|39445|6|Mentioned|p61|||See also p64, Table 4 and Fig.5.||||||11-DEC-06
18263|Toko Group|40136|5|Briefly described|p41|||||||||
18263|Toko Group|43808|6|Mentioned|p293|||||||||
18263|Toko Group|44091|14|Not recorded|p19,Tb.1||Early Ordovician|||||||
18263|Toko Group|44211|14|Not recorded|p95-99,103|Llanvirnian|Arenigian|Rests unconformably on Ninmaroo Formation. (Arenigian and perhaps Llanvirian or younger)||||||
18263|Toko Group|44233|14|Not recorded|Fig.1||Ordovician|Lower-Middle Ordovician.||||||
18263|Toko Group|44308|14|Not recorded|p10||Ordovician|||||||
18263|Toko Group|44309|14|Not recorded|Tb.1,p11,12,map|||Consists of Nora Formation, Carlo Sandstone, Mithaka Formation, Coolibah Formation.||||||
18263|Toko Group|44310|14|Not recorded|Map Legend|||Not listed on white card.||||||
18263|Toko Group|44312|14|Not recorded|Map Legend||Early Ordovician|(Middle Ordovician)||||||
18263|Toko Group|44326|14|Not recorded|Map Legend|Early Ordovician|Early Ordovician|(Early-Middle Ordovician)||||||
18263|Toko Group|44358|3|Fully described|App.p19|Early Ordovician|Early Ordovician|See also p9-10, (Early-Middle Ordovician)||||||
18263|Toko Group|44469|14|Not recorded|p.10|||(F53-12).||||||
18263|Toko Group|44470|5|Briefly described|map legend|||||||||02-DEC-04
18263|Toko Group|44543|14|Not recorded|p34|||Ref. to Queensland Geological Map 1953. See also Lexicon.||||||
18263|Toko Group|44920|14|Not recorded|Map Legend, Sheet 4||Ordovician|Ordovician||||||
18263|Toko Group|45052|4|Described|p126|||Constituent formations||||||
18263|Toko Group|45118|6|Mentioned|p4|||||||||
18263|Toko Group|46940|6|Mentioned|p57|||||||||
18263|Toko Group|46973|6|Mentioned|p53|||||||||
18263|Toko Group|48901|14|Not recorded|Not recorded|||||||||
18263|Toko Group|48906|14|Not recorded|Tb.1|||||||||
18263|Toko Group|49027|6|Mentioned|p17|||||||||
18263|Toko Group|60122|5|Briefly described|p5, p29-30|Early Ordovician|Early Ordovician|Originated as Toko Series (Whitehouse 1936). Historically the group has included, then excluded, and now includes Kelly Creek Fm. Similarly Coolibah Fm. has been included, excluded and now remains included. Also Includes Nora Fm, Carlo Sst and Mithaka Fm.||||||24-MAY-05
18263|Toko Group|60590|5|Briefly described|Map legend|Middle Ordovician|Early Ordovician|Includes the Coolibah, Nora and Mithaka Formations and Carlo Sandstone.||||||26-NOV-04
18263|Toko Group|61404|5|Briefly described|Map legend|Middle Ordovician|Early Ordovician|Comprises: Kelly Creek, Coolobah, Nora Formations, Carlo Sandstone, Mithaka Formation and Ethabuka Sandstone. Geological Province: southern Georgina Basin.||||||
18263|Toko Group|62983|5|Briefly described|p11|Middle Ordovician|Early Ordovician|Marine siliciclastic sedimentation. Thickness: 370m. Geological Province: Georgina Basin.||||||
18263|Toko Group|63562|6|Mentioned|p349|Early Ordovician|Late Cambrian|Of Georgina Basin.|||||Carbonates and siliciclastics.|
18263|Toko Group|64068|1|Redefined|p226, pp75-78, p7, 38, p ix|Late Ordovician|Late Cambrian|Intended as a redefinition. Southern Georgina Basin.|||Includes Kelly Creek, Coolibah, Nora and Mithaka Formations, Carlo and Ethabuka Sandstones.|Overlies Tomahawk and Ninmaroo Formations. Is overlain unconformably by Dulcie Sandstone and Cravens Peak beds.|Marine siliciclastics.|22-MAR-16
18263|Toko Group|66767|5|Briefly described|p59|Late Ordovician|Early Ordovician|Southern Georgina Basin.|||Kelly Creek Formation.||Marine siliciclastic sedimentary rocks including dolomitic quartz sandstone and dolostone.|
18263|Toko Group|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.||||||Includes Carlo Sandstone, Coolibah Formation, Ethabuka Sandstone, Kelly Creek Formation, Mithaka Formation, Nora Formation|||
18263|Toko Group|67870|5|Briefly described|p43, p46-47, p50-53|Ordovician|Ordovician|Georgina Basin. Potential hydrocarbon reservoir.|||||Sandstone, shale, limestone (chalk), siltstone, glauconite.|
18263|Toko Group|68553|6|Mentioned|Map legend; schematic diagram.|Ordovician|Ordovician|Georgina Basin. This unit, as well as Kelly Creek and Coolibah Formations, are all mapped under the symbol, Ot.||||||
18263|Toko Group|69443|4|Described|p28:3-4, 7, 26-31|Late Ordovician|Early Ordovician|Casey in Smith (1963), after Whitehouse (1936). Southern Georgina Basin. Forms scarps, plateaux and hills. Combined maximum thickness of 1678m. Is correlated with Hanson River beds (Wiso Basin), Florina Formation (Daly Basin), the poorly dated Djagamara Formation and Kerridy Sandstone (Ngalia Basin), and Pacoota Sandstone, Horn Valley Siltstone, Stairway Sandstone, Stokes Siltstone and Carmichael Sandstone (Amadeus Basin).|||Kelly Creek, Coolibah, Nora, Mithaka Formations; Carlo, Ethabuka Sandstones.|Overlies Cockroach Group conformably to locally disconformably, or Georgina Limestone unconformably. Is overlain unconformably by Cravens Peak beds.||12-JUL-16
18263|Toko Group|69591|4|Described|p95, p112|Late Ordovician|Middle Ordovician|Crops out in the Toko Syncline which straddles the QLD/NT border. Originally the Toko Series of Whitehouse (1936), which included the upper part of the Nora Formation and the Carlo Sandstone. Casey (cited in Smith, 1963) applied the name Toko Group to Kelly Creek, Coolibah, Nora, Mithaka Formations and Carlo Sandstone, then revised it by removing Kelly Creek Formation (cited in Smith, 1965). Draper (1980) added the newly named Ethabuka Sandstone and removed the Coolibah Formation: this is the formulation used in this study. Webby et al. (1981) rejected this and included the Coolibah Formation and excluded the Ethabuka Sandstone. Kruse et al. (2002) and Kruse and Mohammed (2005) followed Casey (cited in Smith, 1963), including Kelly Creek and Coolibah Formations and Ethabuka Sandstone.|||Nora, Mithaka Formations; Carlo, Ethabuka Sandstones.||Clastic sediments, dominantly sandstone.|
18263|Toko Group|69673|6|Mentioned|p111, p114 fig 92, p118, p119 fig 94|Ordovician|Ordovician||||Includes Kelly Creek Formation, Coolibah Formation, Nora Formation, Carlo Sandstone, Mithaka Formation, Ethabuka Sandstone|||
18275|Tolmer Group|9324|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Sandstone, siltstone, dolomite.||||||
18275|Tolmer Group|9538|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Sandstone, dolomite, siltstone.   Age: >900Ma.||||||
18275|Tolmer Group|9579|5|Briefly described|Map Sheet|Mesoproterozoic|Mesoproterozoic|Middle Proterozoic age.||||||
18275|Tolmer Group|14019|5|Briefly described|p2 Fig. 1|||On the FERGUSSON RIVER  and PINE CREEK  sheets.  Geological Province: Birrindudu Basin.||||||
18275|Tolmer Group|22479|5|Briefly described|fig1p2|||Placed in Litchfied Province.||||||11-DEC-06
18275|Tolmer Group|22809|5|Briefly described|1|||Underlain by Burrell Creek Formation.||||||18-NOV-11
18275|Tolmer Group|22810|5|Briefly described|Table3 P7, P18||Proterozoic|Minimum age: 1200 Ma; maximum age 1780+/-80 Ma.||||||11-DEC-06
18275|Tolmer Group|22813|5|Briefly described|Map|Mesoproterozoic|Mesoproterozoic|Sandstone, siltstone, dolomite.||||||19-OCT-05
18275|Tolmer Group|23216|6|Mentioned|Fig3p5,33||Mesoproterozoic|||||||
18275|Tolmer Group|23714|4|Described|p36|Proterozoic|Proterozoic|See also page 7 Table 1. Geological Province: Litchfield Province. Max. thickness 1800 m.||||||
18275|Tolmer Group|24047|5|Briefly described|p5 Fig.4|Paleoproterozoic|Paleoproterozoic|Sandstone, dolomite, siltstone.  Geological Province: Litchfield Province (Pine Creek Orogen).  See also p6 Fig. 5.||||||07-NOV-08
18275|Tolmer Group|24122|5|Briefly described|p4 Fig.3|||Geological Province: Birrindudu Basin.||||||
18275|Tolmer Group|24260|6|Mentioned|p1015 Fig.3|||Geological Province: Pine Creek Inlier||||||
18275|Tolmer Group|24297|5|Briefly described|p4 Fig.3|Proterozoic|Proterozoic|||||||
18275|Tolmer Group|24441|5|Briefly described|p1 Fig. 1|||Unconformably overlies the Pine Creek Geosyncline.  Unconformably overlain by the Limbunya Group. Geological Province: Birrindudu Basin.||||||
18275|Tolmer Group|24442|5|Briefly described|p30, p43|||Includes: Depot Creek, Stray Creek Sandstones and Hinde Dolostone.  Marine sandstones mainly.  Overlies the Finniss River Group. See also p50 Fig. 1.||||||
18275|Tolmer Group|32170|6|Mentioned|Map legend|Adelaidean|Carpentarian|Adelaidean or Carpentarian||||||
18275|Tolmer Group|32659|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
18275|Tolmer Group|32660|4|Described|Table 6|||||||||
18275|Tolmer Group|32700|4|Described|p15|||Refers Randal (1962). Much now Bullita and Auvergne Groups.||||||11-DEC-06
18275|Tolmer Group|32728|6|Mentioned|p16|||||||||
18275|Tolmer Group|32873|6|Mentioned|Fig.1|||||||||
18275|Tolmer Group|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
18275|Tolmer Group|33377|6|Mentioned|Fig.|||||||||
18275|Tolmer Group|33729|6|Mentioned|p81|||Fauna.||||||
18275|Tolmer Group|34287|6|Mentioned|p41|||||||||
18275|Tolmer Group|35465|6|Mentioned|Fig.1|||Geology of Pine Creek Geosyncline||||||
18275|Tolmer Group|35495|6|Mentioned|p350|||||||||
18275|Tolmer Group|36473|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
18275|Tolmer Group|37462|4|Described|Table 4.VI|||||||||
18275|Tolmer Group|37579|5|Briefly described|Regional setting map legend|Adelaidean|Adelaidean|Sandstone, dolomite, siltstone. Probably  Adelaidean.||||||10-OCT-05
18275|Tolmer Group|38157|6|Mentioned|p284|||||||||
18275|Tolmer Group|38243|6|Mentioned|p355|||||||||
18275|Tolmer Group|38884|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
18275|Tolmer Group|39069|6|Mentioned|Fig.5|||||||||
18275|Tolmer Group|39210|5|Briefly described|p49|||||||||
18275|Tolmer Group|39320|6|Mentioned|Fig.1|||||||||
18275|Tolmer Group|39563|6|Mentioned|Map legend|Adelaidean|Adelaidean|Prob. Adelaidean||||||
18275|Tolmer Group|39679|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
18275|Tolmer Group|39801|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|Prob.Late Proterozoic. Sandstone, dolomite, siltstone.||||||05-OCT-05
18275|Tolmer Group|39803|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
18275|Tolmer Group|40105|6|Mentioned|p316|||See also Fig.3||||||
18275|Tolmer Group|40168|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Sandstone, dolomite, siltstone.||||||18-OCT-05
18275|Tolmer Group|40223|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|Sandstone, dolomite, siltstone.||||||19-OCT-05
18275|Tolmer Group|40495|6|Mentioned|p13|||||||||
18275|Tolmer Group|40765|6|Mentioned|Fig.3|||||||||
18275|Tolmer Group|40808|6|Mentioned|p17|||||||||
18275|Tolmer Group|40809|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
18275|Tolmer Group|40823|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
18275|Tolmer Group|40852|6|Mentioned|p25|||||||||
18275|Tolmer Group|40957|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
18275|Tolmer Group|41125|6|Mentioned|Fig.6|||||||||
18275|Tolmer Group|41304|6|Mentioned|Map legend|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
18275|Tolmer Group|41305|6|Mentioned|Fig.4|||||||||
18275|Tolmer Group|41407|6|Mentioned|Map legend|Mesoproterozoic||||||||
18275|Tolmer Group|41586|6|Mentioned|Map legend|Mesoproterozoic||||||||
18275|Tolmer Group|41645|6|Mentioned|Fig.4|||||||||
18275|Tolmer Group|41646|6|Mentioned|Map legend|Mesoproterozoic||Sandstone, siltstone, dolomite.||||||17-OCT-05
18275|Tolmer Group|41660|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Includes Hinde Dolomite, Stray Creek Sandstone and Depot Creek Sandstone. Sandstone, siltstone, dolomite.||||||07-OCT-05
18275|Tolmer Group|41661|3|Fully described|p18|||Mention p23 and Fig.5.||||||11-DEC-06
18275|Tolmer Group|41878|6|Mentioned|p34|||||||||
18275|Tolmer Group|41980|6|Mentioned|p585|||||||||
18275|Tolmer Group|42012|4|Described|p13|||||||||
18275|Tolmer Group|42014|5|Briefly described|Map legend|Mesoproterozoic||||||||
18275|Tolmer Group|43140|5|Briefly described|p4||Mesoproterozoic|||||||
18275|Tolmer Group|43187|5|Briefly described|p7|||||||||
18275|Tolmer Group|43624|6|Mentioned|Table 1, p9,37|Adelaidean|Carpentarian|||||||
18275|Tolmer Group|43832|5|Briefly described|29,Table7 p27, 97||Mesoproterozoic|"Middle Proterozoic Platform Cover". Underlain by Finniss River Group.||||||
18275|Tolmer Group|44113|5|Briefly described|p240|Adelaidean|Adelaidean|Geological Province: Daly River Basin.||||||11-DEC-06
18275|Tolmer Group|44314|2|Defined|p.6-7,map|||(D52-4). DARWIN Sheet.||||||11-DEC-06
18275|Tolmer Group|44315|14|Not recorded|map legend||Neoproterozoic|Upper Proterozoic.||||||
18275|Tolmer Group|45022|3|Fully described|p.91.||Adelaidean|On many pages.||||||11-DEC-06
18275|Tolmer Group|45064|5|Briefly described|p14|||||||||
18275|Tolmer Group|45102|6|Mentioned|p49|||||||||
18275|Tolmer Group|45112|3|Fully described|p24|||p24-29.||||||11-DEC-06
18275|Tolmer Group|46163|14|Not recorded|p.168,170,171|||||||||
18275|Tolmer Group|46658|6|Mentioned|p560|||||||||
18275|Tolmer Group|46675|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Includes the Waterbag Creek Formation, Hinde Dolomite, and Buldiva Sandstone. Sandstone, dolomite, siltstone. Unconformably overlain by the Daly River Group; unconformably overlies the Finniss River Group.   Geological Province: Pine Creek Geosyncline.||||||29-NOV-04
18275|Tolmer Group|46676|14|Not recorded|p.6||Neoproterozoic|U.Proterozoic; includes Buldiva Sandstone, Hind Dolomite & Waterbag Creek Formation.||||||
18275|Tolmer Group|47049|6|Mentioned|p237|||||||||
18275|Tolmer Group|48867|14|Not recorded|p.7|||map. Katherine-Darwin area.||||||
18275|Tolmer Group|48942|6|Mentioned|p43|||Refers Randal (1962) & Walpole et al. (1968).||||||
18275|Tolmer Group|50623|6|Mentioned|p259 Fig.2|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
18275|Tolmer Group|60526|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Sandstone, dolomite, siltstone.||||||
18275|Tolmer Group|60575|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Includes the Buldiva Sandstone.||||||
18275|Tolmer Group|60685|5|Briefly described|p4 Fig. 3|Proterozoic|Proterozoic|Correlated with Birrindudu Group. Geological Province: Birrindudu Basin.||||||
18275|Tolmer Group|61389|5|Briefly described|Map Legend|||||||||
18275|Tolmer Group|62375|5|Briefly described|p8 Table 1, 9 table 2, 10 Fig. 3|Neoproterozoic|Paleoproterozoic|Sandstone, dolostone, siltstone. Thickness: 1000m. Geological Province: Pine Creek Orogen.||||||09-FEB-10
18275|Tolmer Group|63261|5|Briefly described|p17, p24|||Correlative of Birrindudu Group. Unconformably overlies the western Pine Creek Orogen.||||||07-FEB-11
18275|Tolmer Group|63866|5|Briefly described|p106-p107, p117, p123|||Litchfield Province, Pine Creek Orogen.||||Unconformably overlies the Wangi Basics and Zamu Dolerite. Equivalent to the Katherine River Gorup.||
18275|Tolmer Group|64698|5|Briefly described|lithinterp table|Statherian|Orosirian|Age ~1700-1825Ma.  Includes Depot Creek Sandstone, Stray Creek Sandstone, Waterbag Creek Formation, Hinde Dolostone (here misspelt as Hindrance Dolostone).||||||07-JAN-09
18275|Tolmer Group|64722|6|Mentioned|p10|||Of western Pine Creek Orogen. Possible correlative of the Birrindudu Group.||||||12-APR-12
18275|Tolmer Group|64724|5|Briefly described|p45 Fig.5, p46|Statherian|Statherian|Birrindudu Basin unit deposited during the Calvert Event (~1730-1690 Ma)||||||
18275|Tolmer Group|64730|6|Mentioned|p127|Paleoproterozoic|Paleoproterozoic|in the Litchfield Province. Possible correlate of Katherine River Group, McArthur Basin.||||||
18275|Tolmer Group|64956|6|Mentioned|p62|Mesoproterozoic|Mesproterozoic|Overlies Soldiers Creek Granite.||||||07-FEB-11
18275|Tolmer Group|65232|5|Briefly described|p52, p6 Fig. 5, p5 Fig. 4, p78|Palaeoproterozoic|Palaeoproterozoic|With Katherine River Group are correlatives of Birrindudu, Hatches Creek, Tomkinson Creek, and Tawallah Groups. Sedimentary rocks: sandstone, dolomite, siltstone. Geol. Prov: western Pine Creek Orogen.||||||09-FEB-10
18275|Tolmer Group|65339|5|Briefly described|p4, p5 Fig.4, p14, p16.|||Unconformably overlies Pine Creek Orogen rocks.|||||Sandstone, conglomerate, greywacke.|
18275|Tolmer Group|65342|5|Briefly described|pp10-11.|||Birrindudu Basin.|||Includes Depot Creek and Stray Creek Sandstones and Hinde Dolostone.|Is unconformably overlain by Limbunya Group.|Mostly coarse siliciclastic sedimentary rocks.|
18275|Tolmer Group|67167|5|Briefly described|Map legend.|||Areas with different magnetic responses are indicated.|||Includes Depot Creek and Stray Creek Sandstones and Hinde Dolostone.|||18-NOV-11
18275|Tolmer Group|67186|5|Briefly described|Map legend.||||||Includes Depot Creek and Stray Creek Sandstones and Hinde Dolostone.|||23-NOV-11
18275|Tolmer Group|67269|5|Briefly described|p20-21 Fig.19|Statherian|Orosirian|Birrindudu Basin.|1825-1700 Ma.||Hinde Dolostone.|||
18275|Tolmer Group|67323|5|Briefly described|Eastern Australia Time-Space Plot; p32|||Pine Creek area.|~1760 Ma deposition.||||Sandstone, dolomite, siltstone.|
18275|Tolmer Group|67355|6|Mentioned|p7 Fig.5, p14, p26, p27 Fig.18, p68||Paleoproterozoic||||Depot Creek Sandstone.|Unconformably overlies the Whites Formation and Coomalie Dolostone.||25-JAN-17
18275|Tolmer Group|67479|6|Mentioned|p2 Tb.1, p15, p58||||||Includes the Depot Creek Sandstone.|||
18275|Tolmer Group|67564|5|Briefly described|p9 Fig.4.|Paleoproterozoic|Paleoproterozoic|Western Pine Creek Orogen. Correlative of Katherine River Group to the east.|||||Sandstone, dolostone, siltstone.|
18275|Tolmer Group|67779|5|Briefly described|p6 Fig.5, p32.|Paleoproterozoic|Paleoproterozoic|Litchfield Province, Pine Creek Orogen. Formerly Buldiva Quartzite of Hossfeld (1937). Correlated with Katherine River Group by Noakes (1949) who later (1956) revoked the correlation.|||Includes Depot Creek and Stray Creek Sandstones; Hinde Dolostone, and Waterbag Creek Formation.|||21-MAY-18
18275|Tolmer Group|68280|6|Mentioned|p26 fig 24|||Birrindudu Basin.|||Includes Hinde Dolostone|||
18275|Tolmer Group|68575|5|Briefly described|p125|||Western Pine Creek Orogen. Age distribution is remarkably similar to other basal McArthur Basin clastics (eg Kombolgie Subgroup; Westmoreland Conglomerate).|||Depot Creek Sandstone.|||
18275|Tolmer Group|68733|6|Mentioned|p186||||||Depot Creek Sandstone.|||06-DEC-17
18275|Tolmer Group|69383|5|Briefly described|p31|Mesoproterozoic|Mesoproterozoic|||||Overlies Burrell Creek Formation.||
18275|Tolmer Group|69417|5|Briefly described|p2:5-6|Statherian|Statherian|Northern Birrindudu Basin. Represents part of a single, large un-named superbasin linked at depth beneath overlying basins.||||||12-JUL-16
18275|Tolmer Group|69419|6|Mentioned|p4:3 Fig.4.3|||W. Pine Creek Orogen.||||||12-JUL-16
18275|Tolmer Group|69420|5|Briefly described|p5:14, 54, 64|||Birrindudu Basin. Associated with Au mineralisation in the underlying Coomalie Dolostone.|||Depot Creek Sandstone.|Unconformably overlies Coomalie Dolostone.||12-JUL-16
18275|Tolmer Group|69432|4|Described|p17:1-3, 5-6, 12-13|Paleoproterozoic|Paleoproterozoic|Noakes (1956), for a succession of sandstone, dolostone and shale unconformably overlying the Pine Creek Orogen and unconformably overlain by the Daly Basin succession. Birrindudu Basin. A likely correlative of the Katherine River Group.  1600-1800m thick. Unfolded: horizontal to gently dipping. Age poorly constrained: lacks reliable chronostratigraphic control. SHRIMP U-Pb detrital zircon maximum deposition age of 1837 +/- 15 Ma by Claoue-Long et al. (2001).|<1837 Ma.||Depot Creek, Stray Creek, Sandstones; Hinde Dolostone.|Unconformably overlies Inverway Metamorphics. Is overlain unconformably by Limbunya Group.||12-JUL-16
18275|Tolmer Group|69673|6|Mentioned|p3 fig 2, p47, p48 fig 35, p49|Statherian|Statherian|1600-1800m thick.|||Includes Depot Creek Sandstone, Stray Creek Sandstone, Hinde Dolostone, Waterbag Creek Formation|Unconformably overlain by Limbunya Group|Sandstone, dolostone and shale with minor conglomerate and siltstone packages. Parts of the succession are glauconitic, stromatolitic or dolomitic.|
18275|Tolmer Group|70866|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.|||Includes Waterbag Creek Formation; Hinde Dolostone; Stray Creek, Depot Creek Sandstones.|Is overlain by Uniya Formation.||01-MAR-18
18275|Tolmer Group|71302|5|Briefly described|p6|Paleoproterozoic|Paleoproterozoic|Of Birindudu Basin.|||Includes Hinde Dolostone, Stray Creek Sandstone, Depot Creek Sandstone.|Overlain by Limbunya Group. Underlain by Inverway Metamorphics. Equivalent to Birrindudu Group.||
18275|Tolmer Group|72373|5|Briefly described|p2|Paleoproterozoic|Paleoproterozoic|Of Birrindudu Basin. Broadly equivalent to Redbank package, and Spencer Creek, Groote Eylandt, Donydji, Katherine River and Edith River groups (northern McArthur Basin), Tawallah Group (central/southern McArthur Basin) and Tomkinson Creek and Hatches Creek groups (Tomkinson Province).||||||
18318|Tomkinson Creek Group|23733|3|Fully described|p9|Paleoproterozoic|Paleoproterozoic|Upgraded from Tomkinson Creek Subgroup. Includes Short Range Sandstone, Hayward Creek Formation and Morphett Creek Formation.  Age: <1784Ma.   See also p32 Fig. 19.||||||07-NOV-08
18318|Tomkinson Creek Group|23809|5|Briefly described|p27|||Correlates with the Tawallah Group (McArthur Basin) and Birrindudu Group (Birrindudu Basin). Geological Province: Ashburton Province.||||||14-APR-15
18318|Tomkinson Creek Group|24047|5|Briefly described|p7 Fig. 6, p9|Paleoproterozoic|Paleoproterozoic|Age: 1780Ma.  Geological Province: Ashburton Province (Tennant Inlier).||||||07-NOV-08
18318|Tomkinson Creek Group|24303|1|Redefined|p3, p55 Appendix|Statherian|Statherian|Overlies the Flynn Group. Geological Province: Ashburton province. Max. Thickness: 11km. Age: ca 1805-1710 Ma. Unconformably overlain by the Namerinni and Renner Groups. See also p4 Tb.1.||||||25-JAN-10
18318|Tomkinson Creek Group|24304|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes Carmilly, Bootu, Attack Creek and Morphett Creek Formations, and the Short Range Sandstone.||||||07-NOV-08
18318|Tomkinson Creek Group|24442|5|Briefly described|p14|Proterozoic|Proterozoic|Comprises Hayward Creek and Morphett Creek Formations, Short Range Sandstone, and Attack Creek, Bootu and Carmilly Formations.  Geological Province: Ashburton Province.  Unconformably overlain by the Namerinni and Renner Groups.||||||
18318|Tomkinson Creek Group|32959|6|Mentioned|p21|||||||||
18318|Tomkinson Creek Group|33307|6|Mentioned|Fig.8|||||||||
18318|Tomkinson Creek Group|37565|6|Mentioned|Fig.5|||||||||
18318|Tomkinson Creek Group|37572|5|Briefly described|p155|||||||||
18318|Tomkinson Creek Group|39213|6|Mentioned|Fig.8|||See p20 for structure.||||||18-OCT-05
18318|Tomkinson Creek Group|46842|6|Mentioned|p111|||||||||
18318|Tomkinson Creek Group|46864|6|Mentioned|p40|||||||||
18318|Tomkinson Creek Group|46919|6|Mentioned|p219|||||||||
18318|Tomkinson Creek Group|46992|6|Mentioned|p253|||||||||
18318|Tomkinson Creek Group|50353|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
18318|Tomkinson Creek Group|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes Morphett Creek Formation, Short Range Sandstone (with its Deagan Member), Attack Creek, Bootu and Camilly Fms; and Hayward Creek Fm (with Blanche Creek, Manga Mauda, Meerie, Coodna and Whittington Range Members). In the Tennant Creek region.||||||07-NOV-08
18318|Tomkinson Creek Group|61861|6|Mentioned|p23, Fig.2.|||Tennant Inlier. Correlated with Birrindudu Group of Tanami Region.||||||
18318|Tomkinson Creek Group|64724|5|Briefly described|p45 Fig.5, p46|Statherian|Statherian|Unit of the Northern Tennant Creek Province of the Leichhardt Superbasin deposited during the Leichhardt Extension (1800-1750 Ma)||||||
18318|Tomkinson Creek Group|64780|4|Described|p60, p61, p62 Fig.3, p63 Fig.4 |Palaeoproterozoic|Palaeoproterozoic|Shallow-marine and continental sedimentary rocks with minor mafic volcanic rocks in the lower part. Age range given as 1805-1710 Ma on p60: possibly a misprint?|1805-1790? Ma||Includes the Carmilly, Bootu, Attack Creek, Morphett Creek Formations and Short Range Sandstone.|Unconformably underlies the Namerinni and Renner Groups.|A thick succession of shallow-marine and continental sedimentary rocks, with minor mafic volcanic rocks in the lower part.|
18318|Tomkinson Creek Group|65209|5|Briefly described|p35 Fig.1, p37, p38, p39|Paleoproterozoic|Paleoproterozoic|Formerly Subgroup status. Redefined Tomkinson Creek Group. 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. Likely source of many pebbles and boulders in Rising Sun Conglomerate. Geol. Prov: Tomkinson Creek Province.|||Carmilly Formation, Bootu Formation, Attack Creek Formation, Short Range Sandstone, Morphett Creek Formation, Hayward Creek Formation.|||05-JAN-17
18318|Tomkinson Creek Group|65232|5|Briefly described|p78|||With Hatches Creek Group, are correlatives of Katherine River Group and Tolmer Group. Dominated by shallow-marine clastic and carbonate sedimentary rocks. Geol Prov: Tennant Province.||||||09-FEB-10
18318|Tomkinson Creek Group|65338|5|Briefly described|p6. |||Tomkinson Creek Province, northern Tennant Region. Lithostratigraphic correlative of Hatches Creek Group, although this unit has very little felsic volcanics and hence carbonates are more important.|||Includes Whittington Range Volcanic Member.|||
18318|Tomkinson Creek Group|66860|6|Mentioned|p6 Tb.1|||Tennant Region. Deposition of the upper parts of this unit was coeval with Pargee Sandstone (Tanami Region).||Strangways Metamorphic Complex||||
18318|Tomkinson Creek Group|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.|||Includes Hayward Creek, Morphett Creek, Attack Creek, Bootu and Carmilly Formations; and Short Range Sandstone.|||
18318|Tomkinson Creek Group|67323|4|Described|Eastern Australia Time-Space Plt,p31-32|||See also. Tennant Creek/Davenport area.|~1820-1800 Ma (lower); ~1760-1740 Ma (upper).||Attack Creek, Bootu, Carmilly, Morphett Creek Formations; Short Range Sandstone; Manga Mauda, Meerie, Coodna, Whittington Members (parent not named).|Overlies Ooradidgee group. Is overlain by Namerinni Group.|Volcanic packages in the lower part; marine sandstone, dolostone, limestone and siltstone in the upper part.|
18318|Tomkinson Creek Group|69187|5|Briefly described|p52|||Tomkinson Province. Lower part of Hatches Creek Group is distinguished from Tomkinson Creek Group by presence of felsic and mafic volcanic units.||||overlies Ooradidgee Group|shallow marine sedimentary rocks|
18318|Tomkinson Creek Group|69417|5|Briefly described|p2:5-6|Orosirian|Orosirian|Tomkinson Province. Represents part of a single, large un-named superbasin linked at depth beneath overlying basins.||||Correlated with Hatches Creek Group.|Dominantly sandstone and volcanic rocks.|12-JUL-16
18318|Tomkinson Creek Group|69424|5|Briefly described|p9:2, 4-5, 16, 19, 27-28,34,39 Fig.9.24|Paleoproterozoic|Paleoproterozoic|Tomkinson Province. Deformation during the (?1790-1770 Ma) Davenport Event is described.|||Short Range Sandstone; Hayward Creek, Morphett Creek Formations.|Unconformably overlies Ooradidgee Group. Correlated with Hatches Creek Group.||12-JUL-16
18318|Tomkinson Creek Group|69425|6|Mentioned|p10:1-2, 4, 18-19|||Tomkinson Province, northern Tennant Region.||||Correlated with Hatches Creek Group.||12-JUL-16
18318|Tomkinson Creek Group|69429|6|Mentioned|p14:3-4|||Hussey et al. (2001). Tomkinson 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
18318|Tomkinson Creek Group|69430|6|Mentioned|p15:9|||Tomkinson Creek Province.||||May be contiguous with Tawallah Group (McArthur Basin).||12-JUL-16
18318|Tomkinson Creek Group|69431|3|Fully described|p16:1-7, 12-15, 18, 20, 22-24|Statherian|Orosirian|Donnellan et al. (2001). Originally the Tomkinson Creek Beds (Randal and Brown, 1969); partly redefined as Tomkinson Creek Subgroup (Donnellan et al., 1995), who combined it with Flynn Subgroup to form the Churchills Head Group. Subsequently, Donnellan et al. (2001) included rocks of the Flynn Subgroup within the correlative Ooradidgee Group, and redefined the remainder of the succession as Tomkinson Creek Group. The Churchills Head Group was thus redundant and the name abandoned. Tomkinson Province. Forms major ridges alternating with recessive valleys. Has regional NW- and NNW-trending folds. Estimated thickness about 6,500-10,000m. Age is poorly constrained. Basal relationships discussed. Onset of sedimentation was contemporaneous with c.1815-1805 Ma Murchison Event.|||Hayward Creek, Morphett Creek, Attack Creek, Bootu and Carmilly Formations; Short Range Sandstone.|Overlies Ooradidgee Group, mainly unconformably, locally conformably. Is overlain unconformably by Namerinni and Renner Groups. Correlated with Hatches Creek Group.|Unmetamorphosed. Four cycles of thick, ridge-forming siliciclastic sedimentary rocks overlain by recessive, mixed siliciclastic-carbonate succession.|12-JUL-16
18318|Tomkinson Creek Group|69447|6|Mentioned|p32:1|Proterozoic|Proterozoic|Tennant Region. Forms part of the basement for the Wiso Basin.||||||12-JUL-16
18318|Tomkinson Creek Group|69673|6|Mentioned|p3 fig 2, p17, p57, p58, p141|Orosirian|Statherian|Between 6500m and 10000m.|||Includes Hayward Creek Formation, Morphett Creek Formation, Short Range Sandstone, Attack Creek Formation, Bootu Formation, Carmilly Formation|Correlated with Groote Eylandt Group, Hatches Creek Group, Unconformably overlain by Namerinni Group, Renner Group||
18318|Tomkinson Creek Group|70968|6|Mentioned|p92, p94-95, p98, p102, p138-139|||Tomkinson Province.||||Is overlain unconformably by Gleeson Formation (Renner Group).||
18318|Tomkinson 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).||||||
18318|Tomkinson Creek Group|72711|6|Mentioned|p11.|||Mentioned as part of Tomkinson Province (Donnellan 2013). Includes sulphate evaporites.||||||
18318|Tomkinson Creek Group|72718|6|Mentioned|p6, p12, p18|||Tomkinson Province.||||Overlain by Glyde package rocks, in places where Redbank package not seen.||
18318|Tomkinson Creek Group|73083|6|Mentioned|p42|Paleoproterozoic|Paleoproterozoic|||||||
18349|Tooganinie Formation|22453|6|Mentioned|p 12|||||||||
18349|Tooganinie Formation|22538|6|Mentioned|Fig3 P709|||||||||
18349|Tooganinie Formation|22664|6|Mentioned|35,47|Paleoproterozoic|Paleoproterozoic|Of theUmbolooga Subgroup.  In the McArthur Basin.||||||07-NOV-08
18349|Tooganinie Formation|22853|3|Fully described|19|Proterozoic|Proterozoic|Of the Umbolooga Subgroup. Max thickness: 200 m. Overlain by  Leila Sandstone: underlain by Tatoola Sandstone.||||||12-DEC-06
18349|Tooganinie Formation|23387|6|Mentioned|p18 fig.19|||Of Umbolooga Subgroup.||||||
18349|Tooganinie Formation|23396|5|Briefly described|p407 Fig.2|||Of the McArthur Group.||||||12-DEC-06
18349|Tooganinie Formation|23397|5|Briefly described|p471|||||||||
18349|Tooganinie Formation|23398|5|Briefly described|p442|||||||||
18349|Tooganinie Formation|23776|5|Briefly described|p706|||Umbolooga Subgroup.||||||
18349|Tooganinie Formation|23902|4|Described|p1568 Fig.2|||Of the Umbolooga Subgroup. Overlain by the Leila Sandstone and the Myrtle Shale. Overlies the Tatoola Sandstone. Geological Province: McArthur Basin||||||12-DEC-06
18349|Tooganinie Formation|23910|5|Briefly described|p292 Fig. 3|||Of Umbolooga Subgroup.  Geological Province: McArthur Basin.||||||
18349|Tooganinie Formation|23961|6|Mentioned|p1193 Fig. 4|||Geological Province: Mt Isa Inlier.||||||
18349|Tooganinie Formation|23963|5|Briefly described|p1239 Fig.2|||Geological Province: McArthur Basin. Of the Umbolooga Subgroup.||||||
18349|Tooganinie Formation|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Of Umbolooga Subgroup. Overlies Tatoola Sandstone. Siltstone. Geological Province: Southern McArthur Basin.||||||
18349|Tooganinie Formation|30272|6|Mentioned|p5|||Stratigraphic table||||||
18349|Tooganinie Formation|30344|6|Mentioned|Fig.4|||Part of Umbolooga Subgroup.||||||
18349|Tooganinie Formation|30345|6|Mentioned|Table 1|||Carpentarian age. Lithology||||||
18349|Tooganinie Formation|32363|5|Briefly described|Table 1|||||||||
18349|Tooganinie Formation|32658|3|Fully described|Table 2|||See also Fig.3||||||
18349|Tooganinie Formation|32660|5|Briefly described|Table 4|||||||||
18349|Tooganinie Formation|33665|6|Mentioned|Fig.2|||||||||
18349|Tooganinie Formation|33666|6|Mentioned|Table 1|||||||||
18349|Tooganinie Formation|35162|6|Mentioned|Table.1|||||||||
18349|Tooganinie Formation|35261|6|Mentioned|Fig.2|||||||||
18349|Tooganinie Formation|36796|6|Mentioned|Fig.3|||||||||
18349|Tooganinie Formation|37568|5|Briefly described|p79|||||||||
18349|Tooganinie Formation|38156|6|Mentioned|Fig.2|||||||||
18349|Tooganinie Formation|38582|6|Mentioned|Fig.3|||||||||
18349|Tooganinie Formation|39561|6|Mentioned|Fig.3|||||||||
18349|Tooganinie Formation|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
18349|Tooganinie Formation|40105|6|Mentioned|Fig.7|||||||||
18349|Tooganinie Formation|40259|6|Mentioned|Table 1|||||||||
18349|Tooganinie Formation|40691|6|Mentioned|Fig.4|||Misspelling of Tooganinnie?||||||
18349|Tooganinie Formation|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
18349|Tooganinie Formation|41268|5|Briefly described|Fig.3|||||||||
18349|Tooganinie Formation|41277|6|Mentioned|p80|||||||||
18349|Tooganinie Formation|42385|4|Described|p19|||See also Table 4 p17.||||||12-DEC-06
18349|Tooganinie Formation|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
18349|Tooganinie Formation|42570|5|Briefly described|p546|||||||||
18349|Tooganinie Formation|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.||Of Umbolooga Subgroup (McArthur Group).||In schematic section, underlies Myrtle Shale and Leila Sandstone; overlies Tatoola Sandstone.|Dololutite, stromatolitic dololutite, dolomictic shale and siltstone, dolarenite, sandy dolarenite and sandstone. Detailed lithology given.|09-NOV-11
18349|Tooganinie Formation|42639|3|Fully described|p24, Table 5 p21|||||||||
18349|Tooganinie Formation|42700|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
18349|Tooganinie Formation|42739|5|Briefly described|map legend|Statherian|Statherian|Of the Umbolooga Subgroup. Dololutite, stromatolitic dololutite, red-brown dolomitic mudstone.||||||19-OCT-05
18349|Tooganinie Formation|42812|3|Fully described|p36, Table 4|||Of the Umbolooga Subgroup.||||||12-DEC-06
18349|Tooganinie Formation|42935|6|Mentioned|p529 Fig.2|||Of the Umbolooga Subgroup.||||||12-DEC-06
18349|Tooganinie Formation|43010|5|Briefly described|Fig.6||Mesoproterozoic|of "Mid Proterozoic" age.||||||
18349|Tooganinie Formation|43036|3|Fully described|p48|||Of the Umbolooga Subgroup.||||||12-DEC-06
18349|Tooganinie Formation|44287|14|Not recorded|p.9,10,18, opp.9|||(E53-3).||||||
18349|Tooganinie Formation|44288|14|Not recorded|map legend|||Dolomitic siltstone and shale dolomitic sandstone, dolomite, algal dolomite, oolitic limestone. Lower (?) Proterozoic.||||||
18349|Tooganinie Formation|44473|2|Defined|p.8,9,15|||(E53-7). Upper formation of Bauhinia Downs Subgroup (backreef seds of McArthur Group); contains Leila Sandstone Member.||||||
18349|Tooganinie Formation|44474|14|Not recorded|map legend|||Lower (?) Proterozoic.||||||
18349|Tooganinie Formation|44530|14|Not recorded|p.10, opp.10|||(D53-15).||||||
18349|Tooganinie Formation|44531|14|Not recorded|map legend|||Lower (?) Proterozoic.||||||
18349|Tooganinie Formation|45162|1|Redefined|p77|Proterozoic|Proterozoic|Mention p159.||||||12-DEC-06
18349|Tooganinie Formation|46915|6|Mentioned| Fig.1|||Stratigraphic section through McArthur Group.||||||
18349|Tooganinie Formation|46968|6|Mentioned|Fig.2|||||||||
18349|Tooganinie Formation|60483|5|Briefly described|p7 Fig. 5, p30|||Of Umbolooga Subgroup (McArthur Group). Geological Province: McArthur Basin.||||||05-OCT-07
18349|Tooganinie Formation|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Umbolooga Subgroup. Overlian by Leila Sandstone and Emmerugga Dolomite, underlian by Tatoola Sandstone.||||||
18349|Tooganinie Formation|62084|5|Briefly described|p936 Fig.5|||Isa Superbasin. McArthur Basin. Shown as Tooganinie Fm.||McArthur Group|||Platform carbonates.|
18349|Tooganinie Formation|63112|6|Mentioned|p1191 Fig.2|||Isa Superbasin; southern McArthur Basin. Age approximated from Fig.2.|c.1650 Ma.|Unit in Loretta Supersequence.||||
18349|Tooganinie Formation|64815|6|Mentioned|p4 Fig.2, p5 Fig.3, p8 Tb.1, p14 Tb.5|||||Of the Umbolooga Subgroup.||||
18349|Tooganinie Formation|64817|6|Mentioned|p353 Fig.4 |||||Of the Umbolooga Subgroup.||||
18349|Tooganinie Formation|65228|4|Described|p12, p28, p29, p31, Table 1.|||Mis-spelt as Tooganinnie on p12 and as Tooganine in Table 1. Southern McArthur Basin. Characterised by thin shoaling cycles of "clean" stromatolitic dolostones (low count) and "dirty" siltstones (high count), producing a saw-tooth gamma ray log pattern. Middle of Loretta Supersequence. Gamma ray log, lithology and facies detailed. Measured section. See also Figs.04, 11-12, 15-19.||Unit in Umbolooga Subgroup.||Overlies Tatoola Sandstone. Is overlain unconformably by Leila Sandstone.|Cyclic dolostone and siltstone unit with green shales near the base.|
18349|Tooganinie Formation|67144|5|Briefly described|Map legend.|Statherian|Statherian|Generally recessive.||Unit in Umbolooga Subgroup.||Overlies Tatoola Sandstone. Is overlain by Leila Sandstone.|Dololutite, stromatolitic dololutite, dolomitic shale and siltstone, ripple and cross-bedded dolarenite, sandy dolarenite and sandstone, breccia beds and ooids in dolarenite, common dessication cracks and pseudomorphs after halite and gypsum.|
18349|Tooganinie Formation|67352|4|Described|p14 Tb.2|Statherian|Statherian|McArthur Basin. 500 m thick.||Umbolooga Subgroup||Overlies Tatoola Sandstone (conformably). Conformably overlain by Myrtle Shale.|Dolomudstone, dolomitic shale and siltstone, breccia.|
18349|Tooganinie Formation|69430|4|Described|p15:3, 17, 34, 42, 48|Statherian|Statherian|Southern McArthur Basin. c.200m thick. Peritidal marine to emergent shoreline deposits, possibly deepening to the south. Previously included two Members named by Plumb and Brown (1973) : the Leila Sandstone Member and the Myrtle Shale Member; these were raised to Formation status by Jackson et al. (1987).  Stromatolites occur as stratiform, domal, columnar and conical forms. Appears as Toonganinie Formation on 15:34. Hosts the Mariner and Great Scott base metal prospects, among others.||Umbolooga Subgroup.||Conformably and gradationally overlies Tatoola Sandstone. Is overlain conformably and gradationally by Leila Sandstone.|Dololutite, stromatolitic dololutite, dolomitic shale and siltstone, ripple-marked and cross-bedded dolarenite and sandstone; breccia beds and ooids in dolarenite; common dessication cracks and pseudomorphs after gypsum and halite.|12-JUL-16
18349|Tooganinie Formation|69673|6|Mentioned|p16 fig 13|||Batten Fault Zone||Umbolooga Subgroup|Includes Leila Sandstone, Myrtle Shale|Overlies Tatoola Sandstone, overlain by Emmerugga Dolostone||
18349|Tooganinie Formation|72248|6|Mentioned|p147|||Of McArthur Basin.||Unit of Umbolooga Subgroup.||||
18349|Tooganinie Formation|72373|4|Described|iii,p1,8-11|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. Exposures restricted to Batten Fault Zone in southern McArthur Basin, from southern MOUNT YOUNG, through BAUHINIA DOWNS to northern WALHALLOW. Reference section: 78/01 of Jackson et al (1987), in SW GLYDE. Previous age constraints provided by tuffs in underlying Tatoola Sandstone (1648+\-3 Ma) and tuff near the top of overlying Coxco Dolostone Member (1639+\-6 Ma; Page et al., 2000). Sample 2709630 (BD16TJM081; Medium-grained dolomitic quartz sandstone; BAUHINIA DOWNS) yielded interpreted max depositional age of 1758+\-41 Ma, youngest grain 1664+/-38 Ma. Similar detrital zircon spectra with Leila Sandstone, suggesting derivation from similar source areas and potentially in part laterally equivalent.|1758+\-41 Ma (max dep age,conservative)|Unit of Umbolooga Subgroup.||Overlain conformably by Leila Sandstone. Underlain conformably by Tatoola Sandstone.|Thick succession of dolostone and interbedded dolomitic sandstone, siltstone and shale.|25-SEP-19
18349|Tooganinie Formation|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the northern part of the Batten Fault Zone.||Umbolooga Subgroup||Overlies Tatoola Sandstone and underlies Emmerugga Dolostone. Laterally equivalent to Leila Sandstone + Myrtle Shale.||
18349|Tooganinie Formation|72718|6|Mentioned|p7|||Southern McArthur Basin. Batten Fault Zone.||Umbolooga Sub-group, McArthur Group||Underlain by Tatoola Sandstone. Overlain by Emmerugga Dolostone. Equivalent to Myrtle Shale and Leila Sandstone.||
18349|Tooganinie Formation|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the north of the Batten Fault Zone.||Umbolooga Subgroup||Overlies Tatoola Sandstone and underlies Emmerugga Dolostone and is unconformably laterally equivalent to Myrtle Shale and Leila Sandstone.||
18349|Tooganinie Formation|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin, Isa Superbasin.||Umbolooga Subgroup, McArthur Group||Underlain by Tatoola Sandstone. Overlain by Emmerugga Dolostone. May be equivalent to Myrtle Shale and Leila Sandstone.||
18349|Tooganinie 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].||||||
18349|Tooganinie Formation|73412|5|Briefly described|p4, 8, 12|||Southern McArthur Basin.||Umbolooga Subgroup.||Overlies Tatoola Sandstone. Is overlain by Emmerugga and Teena Dolostones.||
18375|Toolebuc Formation|12597|5|Briefly described|p492 Tb.1, p500|Albian|Albian|Eromanga Basin. 3-75m thick. Characteristic high gamma response. Contains abundant bivalves, fish skeletons and teeth, radiolarians, globigerinids and dinoflagellates.|||||Carbonaceous and calcareous mudstone and limestone with minor thin interbeds of fine-grained calcareous labile sandstone and siltstone; local 10m thick oil-shale horizon in N.|
18375|Toolebuc Formation|13497|5|Briefly described|p115, p115 fig 6.33, p146|Early Cretaceous|Early Cretaceous|Eromanga Basin.||Marree Subgroup||Overlies the Wallumbilla Formation. Overlain by the Allaru Mudstone.|Shale and siltstone with minor shoreface sandstone.|
18375|Toolebuc Formation|13516|6|Mentioned|p167 fig 10, p169 fig 11, p171 fig 12|Albian|Albian|In Eromanga Basin.||||||
18375|Toolebuc Formation|22464|5|Briefly described|p9||Early Cretaceous|In the Eromanga Basin. Overlies Wallumbilla Formation.||||||12-DEC-06
18375|Toolebuc Formation|22857|5|Briefly described|p295, p296-7 Tb.22.1, p314|Albian|Albian|Oil shales occur. Together with Allaru Mudstone thickness is ~100m. Geological Province: Eromanga Basin||||||
18375|Toolebuc Formation|22865|4|Described|p295,Table22.1p296-7|Cenomanian|Albian|||||||
18375|Toolebuc Formation|22883|5|Briefly described|Fig2 P30||Early Cretaceous|Overlain by Allaru Mudstone, underlain by Wallumbilla Formation.||||||01-FEB-07
18375|Toolebuc Formation|22912|5|Briefly described|33|||Geological province: Eromanga Basin.||||||12-DEC-06
18375|Toolebuc Formation|23031|5|Briefly described|31|||||||||
18375|Toolebuc Formation|23056|6|Mentioned|12 table 2|||||||||
18375|Toolebuc Formation|23154|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Geological Province - Eromanga Basin.  Of the Marree Subgroup (Neales River Group) - not clear in legend however.||||||14-DEC-06
18375|Toolebuc Formation|23155|4|Described|p32|Early Cretaceous|Early Cretaceous|The formation is restricted to the northern and western STRZELECKI.||||||
18375|Toolebuc Formation|23356|5|Briefly described|26 Tab.2|Albian|Albian|||||||
18375|Toolebuc Formation|23375|4|Described|Fig2 p265, 266||Albian|Laterally equivalent to lower Oodnadatta Formation. In the Eromanga Basin.||||||12-DEC-06
18375|Toolebuc Formation|23393|5|Briefly described|p24|Early Cretaceous|Early Cretaceous|Of Rolling Downs Group.||||||
18375|Toolebuc Formation|23425|4|Described|Table 9.7 p394||Albian|see also p378. Of Rolling Downs Group. Overlain by Allaru Mudstone; underlain by Wallumbilla Formation. Carpentaria Basin Province.||||||12-DEC-06
18375|Toolebuc Formation|23430|4|Described|p522 + p524 Table 14.7|||In the Eromanga Basin Province.||||||12-DEC-06
18375|Toolebuc Formation|23431|5|Briefly described|p543|||||||||
18375|Toolebuc Formation|23518|5|Briefly described|p13|Mesozoic|Mesozoic|Of Rolling Downs Group.  Geological Province: Carpentaria Basin.||||||
18375|Toolebuc Formation|23864|6|Mentioned|p128|Albian|Albian|||||||
18375|Toolebuc Formation|23883|5|Briefly described|p129 Fig. 11.2|Cretaceous|Cretaceous|Of Rolling Downs Group.  Geological Province: Great Australian Superbasin.||||||
18375|Toolebuc Formation|23911|5|Briefly described|p97 Fig. 11|Cretaceous|Cretaceous|Geological Province: Eromanga Basin.  Of the Rolling Downs Group.||||||
18375|Toolebuc Formation|23982|5|Briefly described|p12|Cretaceous|Cretaceous|Of the Rolling Downs Group. Geological Province: Eromanga Basin. See also page 35 Fig.7.||||||
18375|Toolebuc Formation|23986|5|Briefly described|p71|||||||||
18375|Toolebuc Formation|24048|5|Briefly described|p76|||||||||
18375|Toolebuc Formation|24085|5|Briefly described|p33, p36, p38|Albian|Albian|Geological Province: Eromanga Basin.||||||16-SEP-08
18375|Toolebuc Formation|24092|5|Briefly described|p8 Fig.3|||Of Rolling Downs Group. Geological Province: Eromanga Basin.||||||
18375|Toolebuc Formation|24175|5|Briefly described|p17 Fig. 3|Albian|Albian|Geological Province: Eromanga Basin.||||||
18375|Toolebuc Formation|24201|5|Briefly described|p379|Albian|Albian|Geological Province: Eromanga Basin.||||||
18375|Toolebuc Formation|24204|5|Briefly described|p263 Fig.4, p267, p282 Fig.21|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||17-DEC-04
18375|Toolebuc Formation|24210|5|Briefly described|p133 Fig. 2|Early Cretaceous|Early Cretaceous|Of the Marree Subgroup.  Geological Province: Eromanga Basin.||||||
18375|Toolebuc Formation|24226|5|Briefly described|p391|Albian|Albian|Age: Late Albian.||||||
18375|Toolebuc Formation|24243|5|Briefly described|p3 Fig.2|Cretaceous|Cretaceous|Of Rolling Downs Group.||||||
18375|Toolebuc Formation|24251|5|Briefly described|p234 Fig.1, p245|Albian|Albian|Overlying Unit: Allaru Formation. Underlying Unit: Wallumbilla Formation. Maximum Thickness: <35m. Geological Province: Eromanga Basin||||||
18375|Toolebuc Formation|29394|6|Mentioned|p145|||Cretaceous.||||||
18375|Toolebuc Formation|30584|4|Described|Table 1|||||||||
18375|Toolebuc Formation|30585|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
18375|Toolebuc Formation|31121|6|Mentioned|Table 2|||||||||
18375|Toolebuc Formation|31165|6|Mentioned|Table 1|||||||||
18375|Toolebuc Formation|31168|6|Mentioned|p10|||||||||
18375|Toolebuc Formation|32314|6|Mentioned|Fig. 4|||||||||
18375|Toolebuc Formation|32705|6|Mentioned|p188|||||||||
18375|Toolebuc Formation|33017|6|Mentioned|p1|||See also p8.||||||12-DEC-06
18375|Toolebuc Formation|33075|4|Described|p451|||Type section p455.||||||12-DEC-06
18375|Toolebuc Formation|33078|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
18375|Toolebuc Formation|33079|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
18375|Toolebuc Formation|33086|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower to Upper Cretaceous||||||
18375|Toolebuc Formation|33176|6|Mentioned|p175|||||||||
18375|Toolebuc Formation|33177|6|Mentioned|p12|||||||||
18375|Toolebuc Formation|33178|6|Mentioned|p11|||||||||
18375|Toolebuc Formation|33179|4|Described|p11|||||||||
18375|Toolebuc Formation|33368|6|Mentioned|p27|||Refers Smart (1972).||||||
18375|Toolebuc Formation|33414|6|Mentioned|p212,213,Tb.|||Part of Wilgunya Sub-group.||||||
18375|Toolebuc Formation|33772|6|Mentioned|p13|||||||||
18375|Toolebuc Formation|33773|6|Mentioned|p17|||||||||
18375|Toolebuc Formation|33900|6|Mentioned|p21|||||||||
18375|Toolebuc Formation|34811|4|Described|Table 1|||||||||
18375|Toolebuc Formation|35220|6|Mentioned|Table 2|||||||||
18375|Toolebuc Formation|35239|6|Mentioned|p258|||||||||
18375|Toolebuc Formation|35253|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
18375|Toolebuc Formation|35457|6|Mentioned|p623|||||||||
18375|Toolebuc Formation|35560|4|Described|p291|||||||||
18375|Toolebuc Formation|35640|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
18375|Toolebuc Formation|35663|6|Mentioned|Fig.2|||Subsurface correlations of the central basin rock units.||||||
18375|Toolebuc Formation|35793|6|Mentioned|Fig.3|||||||||
18375|Toolebuc Formation|35811|5|Briefly described|Table 3|||Uranium exploration discussed p556.||||||12-DEC-06
18375|Toolebuc Formation|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
18375|Toolebuc Formation|35936|6|Mentioned|p615|||||||||
18375|Toolebuc Formation|36012|3|Fully described|Table 5|||See also p18.||||||12-DEC-06
18375|Toolebuc Formation|36110|6|Mentioned|p47|||||||||
18375|Toolebuc Formation|36228|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
18375|Toolebuc Formation|36229|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
18375|Toolebuc Formation|36243|6|Mentioned|Table 6A|||||||||
18375|Toolebuc Formation|36251|4|Described|p3|||||||||
18375|Toolebuc Formation|36331|6|Mentioned|p92|||||||||
18375|Toolebuc Formation|36552|6|Mentioned|p61|||||||||
18375|Toolebuc Formation|36571|6|Mentioned|p95|||||||||
18375|Toolebuc Formation|36690|6|Mentioned|p47|||||||||
18375|Toolebuc Formation|36713|5|Briefly described|p361|||||||||
18375|Toolebuc Formation|36910|6|Mentioned|p61|||||||||
18375|Toolebuc Formation|36912|6|Mentioned|Fig.3|||||||||
18375|Toolebuc Formation|36922|6|Mentioned|Fig.3|||||||||
18375|Toolebuc Formation|37287|6|Mentioned|p36|||||||||
18375|Toolebuc Formation|37608|3|Fully described|Table 1|||||||||
18375|Toolebuc Formation|37776|6|Mentioned|Fig.2|||||||||
18375|Toolebuc Formation|38011|6|Mentioned|p126|||||||||
18375|Toolebuc Formation|38199|5|Briefly described|p426|||Palynology||||||
18375|Toolebuc Formation|38218|4|Described|p285|||||||||
18375|Toolebuc Formation|38226|6|Mentioned|Table 1|||||||||
18375|Toolebuc Formation|38325|4|Described|p265|||||||||
18375|Toolebuc Formation|38372|6|Mentioned|p647|||||||||
18375|Toolebuc Formation|38373|6|Mentioned|p618|||||||||
18375|Toolebuc Formation|38608|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
18375|Toolebuc Formation|38779|6|Mentioned|p7|||||||||
18375|Toolebuc Formation|38780|6|Mentioned|p17|||||||||
18375|Toolebuc Formation|38814|6|Mentioned|Table 1|||||||||
18375|Toolebuc Formation|39029|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Overlain by Allaru Mudstone.||||||25-AUG-04
18375|Toolebuc Formation|39070|4|Described|p365|||||||||
18375|Toolebuc Formation|39211|5|Briefly described|Fig.3|||See also Figs 4,7,9,12-16 etc. Correlation.||||||12-DEC-06
18375|Toolebuc Formation|39445|5|Briefly described|Table 11|||||||||
18375|Toolebuc Formation|39478|6|Mentioned|Table 1|||||||||
18375|Toolebuc Formation|39480|6|Mentioned|p188|||||||||
18375|Toolebuc Formation|39481|6|Mentioned|p180|||||||||
18375|Toolebuc Formation|39482|6|Mentioned|Fig.7|||||||||
18375|Toolebuc Formation|39556|5|Briefly described|Map legend|Cretaceous|Cretaceous|||||||
18375|Toolebuc Formation|39575|6|Mentioned|p103|||||||||
18375|Toolebuc Formation|39708|4|Described|p477|||||||||
18375|Toolebuc Formation|39754|6|Mentioned|p1690|||||||||
18375|Toolebuc Formation|39797|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
18375|Toolebuc Formation|39799|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
18375|Toolebuc Formation|39846|6|Mentioned|Fig.2|||||||||
18375|Toolebuc Formation|39847|5|Briefly described|p39|||||||||
18375|Toolebuc Formation|39899|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
18375|Toolebuc Formation|39914|6|Mentioned|p3|||||||||
18375|Toolebuc Formation|39942|6|Mentioned|p463|||||||||
18375|Toolebuc Formation|39943|6|Mentioned|Table 8A|||||||||
18375|Toolebuc Formation|39989|6|Mentioned|p426|||||||||
18375|Toolebuc Formation|40121|6|Mentioned|Table 1|||||||||
18375|Toolebuc Formation|40167|6|Mentioned|p156|||||||||
18375|Toolebuc Formation|40199|6|Mentioned|Fig.1|||||||||
18375|Toolebuc Formation|40249|6|Mentioned|p41|||||||||
18375|Toolebuc Formation|40322|6|Mentioned|Fig.3|||||||||
18375|Toolebuc Formation|40452|6|Mentioned|p2|||||||||
18375|Toolebuc Formation|40648|6|Mentioned|p12|||||||||
18375|Toolebuc Formation|40670|6|Mentioned|Fig.9|||||||||
18375|Toolebuc Formation|40675|6|Mentioned|Table 8A|||||||||
18375|Toolebuc Formation|40687|6|Mentioned|Table 3|||||||||
18375|Toolebuc Formation|40719|5|Briefly described|p61|||||||||
18375|Toolebuc Formation|40771|5|Briefly described|p429|||||||||
18375|Toolebuc Formation|40801|6|Mentioned|p46|||||||||
18375|Toolebuc Formation|40926|6|Mentioned|p18|||||||||
18375|Toolebuc Formation|41012|3|Fully described|p137|||||||||
18375|Toolebuc Formation|41036|6|Mentioned|p220|||||||||
18375|Toolebuc Formation|41052|6|Mentioned|p87|||||||||
18375|Toolebuc Formation|41060|6|Mentioned|p2|||Generalized stratigraphy||||||
18375|Toolebuc Formation|41061|6|Mentioned|p19|||Generalized stratigraphy||||||
18375|Toolebuc Formation|41062|6|Mentioned|Fig.5|||||||||
18375|Toolebuc Formation|41063|6|Mentioned|p40|||||||||
18375|Toolebuc Formation|41064|6|Mentioned|p62|||||||||
18375|Toolebuc Formation|41084|5|Briefly described|Fig.2|||||||||
18375|Toolebuc Formation|41086|3|Fully described|p101|||See also Fig.3||||||
18375|Toolebuc Formation|41087|3|Fully described|p121|||||||||
18375|Toolebuc Formation|41088|4|Described|p141|||||||||
18375|Toolebuc Formation|41089|6|Mentioned|p156|||||||||
18375|Toolebuc Formation|41097|6|Mentioned|p166|||||||||
18375|Toolebuc Formation|41117|4|Described|p434|||||||||
18375|Toolebuc Formation|41121|6|Mentioned|p179|||||||||
18375|Toolebuc Formation|41125|6|Mentioned|p12|||||||||
18375|Toolebuc Formation|41165|5|Briefly described|p362, p368|||Mention Fig.20||||||
18375|Toolebuc Formation|41174|4|Described|p117|||||||||
18375|Toolebuc Formation|41175|6|Mentioned|Fig.1|||||||||
18375|Toolebuc Formation|41176|6|Mentioned|p206|||See also Table 2||||||
18375|Toolebuc Formation|41177|6|Mentioned|Fig.2|||||||||
18375|Toolebuc Formation|41178|6|Mentioned|p241|||||||||
18375|Toolebuc Formation|41179|6|Mentioned|p255|||||||||
18375|Toolebuc Formation|41180|5|Briefly described|p267|||||||||
18375|Toolebuc Formation|41181|6|Mentioned|p273|||||||||
18375|Toolebuc Formation|41182|5|Briefly described|p300|||||||||
18375|Toolebuc Formation|41183|6|Mentioned|p310|||||||||
18375|Toolebuc Formation|41184|6|Mentioned|p328|||||||||
18375|Toolebuc Formation|41187|6|Mentioned|Fig.2|||||||||
18375|Toolebuc Formation|41196|6|Mentioned|Fig.1|||||||||
18375|Toolebuc Formation|41198|6|Mentioned|Table 1|||||||||
18375|Toolebuc Formation|41214|6|Mentioned|Fig.3|||||||||
18375|Toolebuc Formation|41216|6|Mentioned|Fig.18|||||||||
18375|Toolebuc Formation|41219|6|Mentioned|p338|||||||||
18375|Toolebuc Formation|41266|6|Mentioned|Fig.3|||||||||
18375|Toolebuc Formation|41306|6|Mentioned|p4|||||||||
18375|Toolebuc Formation|41307|6|Mentioned|p5|||||||||
18375|Toolebuc Formation|41464|6|Mentioned|Map legend|Early Cretaceous||||||||
18375|Toolebuc Formation|41482|6|Mentioned|p37|||||||||
18375|Toolebuc Formation|41483|6|Mentioned|p49|||||||||
18375|Toolebuc Formation|41523|3|Fully described|p279|||||||||
18375|Toolebuc Formation|41556|6|Mentioned|Map legend|Early Cretaceous||||||||
18375|Toolebuc Formation|41568|5|Briefly described|p15|||||||||
18375|Toolebuc Formation|41707|6|Mentioned|p164|||||||||
18375|Toolebuc Formation|41724|6|Mentioned|p383|||||||||
18375|Toolebuc Formation|42061|4|Described|p155|||||||||
18375|Toolebuc Formation|42067|4|Described|Appendix 2|||||||||
18375|Toolebuc Formation|42071|6|Mentioned|p117|||||||||
18375|Toolebuc Formation|42084|6|Mentioned|Fig.3 P356|||||||||
18375|Toolebuc Formation|42085|6|Mentioned|Fig.2 P374|||||||||
18375|Toolebuc Formation|42374|6|Mentioned|p435|Albian||||||||
18375|Toolebuc Formation|42397|6|Mentioned|Fig.2 P3|||||||||
18375|Toolebuc Formation|42402|5|Briefly described|p115, 116|||||||||
18375|Toolebuc Formation|42429|6|Mentioned|p156|||||||||
18375|Toolebuc Formation|42446|4|Described|p13|||||||||
18375|Toolebuc Formation|42447|6|Mentioned|Fig.1|||||||||
18375|Toolebuc Formation|42496|5|Briefly described|p136, Fig.3 p132|||||||||
18375|Toolebuc Formation|42520|5|Briefly described|p6|||||||||
18375|Toolebuc Formation|42538|5|Briefly described|Fig. 25.2 P325|||||||||
18375|Toolebuc Formation|42585|5|Briefly described|p79|||||||||
18375|Toolebuc Formation|42588|5|Briefly described|p115|||||||||
18375|Toolebuc Formation|42637|4|Described|p11|||||||||
18375|Toolebuc Formation|42673|5|Briefly described|Fig.2, P184|||||||||
18375|Toolebuc Formation|42746|6|Mentioned|Fig.6 P8|||||||||
18375|Toolebuc Formation|42749|6|Mentioned|Fig.2 P27|||||||||
18375|Toolebuc Formation|42804|5|Briefly described|p115|||||||||
18375|Toolebuc Formation|42999|5|Briefly described|Table 2,p90||Early Cretaceous|||||||
18375|Toolebuc Formation|43002|5|Briefly described|Fig.2,p135|||||||||
18375|Toolebuc Formation|43004|5|Briefly described|Table 1,p179|||||||||
18375|Toolebuc Formation|43105|6|Mentioned|p15|||||||||
18375|Toolebuc Formation|43114|5|Briefly described|p15|||||||||
18375|Toolebuc Formation|43122|5|Briefly described|p29|||see also Fig. 2.||||||
18375|Toolebuc Formation|43591|6|Mentioned|p40|||||||||
18375|Toolebuc Formation|43602|6|Mentioned|191|||In Eromanga Basin. Of the Rolling Downs Group.||||||12-DEC-06
18375|Toolebuc Formation|43630|6|Mentioned|p70|||also Fig.4||||||
18375|Toolebuc Formation|44112|6|Mentioned|p82|||||||||
18375|Toolebuc Formation|44133|5|Briefly described|p122, 104 Fig. 9.11|Late Albian|Middle Albian|Geological Province: Eromanga Basin.||||||
18375|Toolebuc Formation|44291|14|Not recorded|p14|||||||||
18375|Toolebuc Formation|45145|3|Fully described|Table 5|||||||||
18375|Toolebuc Formation|45161|6|Mentioned|p67|||||||||
18375|Toolebuc Formation|46791|4|Described|p47|||||||||
18375|Toolebuc Formation|46872|6|Mentioned|p105|||||||||
18375|Toolebuc Formation|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
18375|Toolebuc Formation|47042|4|Described|p171|||||||||
18375|Toolebuc Formation|47083|5|Briefly described|p20||Mesozoic|Of Rolling Downs Group.||||||
18375|Toolebuc Formation|48770|6|Mentioned|Fig.1|||||||||
18375|Toolebuc Formation|49010|6|Mentioned|Fig.4|||In the Eromanga Basin.||||||12-DEC-06
18375|Toolebuc Formation|49011|6|Mentioned|Fig.3|||In the Eromanga Basin.||||||12-DEC-06
18375|Toolebuc Formation|49254|14|Not recorded|?|||||||||
18375|Toolebuc Formation|49273|14|Not recorded|?|||||||||
18375|Toolebuc Formation|49278|14|Not recorded|?|||||||||
18375|Toolebuc Formation|49330|14|Not recorded|?|||||||||
18375|Toolebuc Formation|49338|14|Not recorded|?|||||||||
18375|Toolebuc Formation|50100|5|Briefly described|p23|Cretaceous|Cretaceous|Of the Rolling Downs Group.  Contains calcareous bituminous shale (oil shale).  Geological Province: Carpentaria and Eromanga Basins.||||||
18375|Toolebuc Formation|50332|5|Briefly described|p22, p93, p96|Mesozoic|Mesozoic|Geological Province: Carpentaria Basin. Main lithologies are mudstone, calcareous shale, limestone, sandstone and siltstone. Also contains calcareous bituminous shale (oil shale).||||||07-FEB-11
18375|Toolebuc Formation|60331|5|Briefly described|p34 Fig.3|Albian|Albian|Overlies Wallumbilla Formation. Overlain by Allaru Mudstone. Geological Province: Eromanga Basin.||||||
18375|Toolebuc Formation|60359|5|Briefly described|Map Legend|Mesozoic|Mesozoic|Limestone, calcareous sandstone.||||||
18375|Toolebuc Formation|60717|5|Briefly described|p40 Fig. 2|Early Cretaceous|Early Cretaceous|Overlies Wallumbilla Formation. Overlain by Allaru Mudstone. Lateral to Oodnadatta Formation. Geological Province: Eromanga  Basin.||||||31-JAN-08
18375|Toolebuc Formation|61312|5|Briefly described|p66, p73|Albian|Aptian|Of the Rolling Downs Group. In Queensland it consists of carbonaceous and bitumous shale and siltstone with limestone lenses. In Queensland, overlies Wallumbilla Formation and is overlain by Allaru Mudstone. Geological Province: Eromanga Basin.||||||16-JUN-06
18375|Toolebuc Formation|61544|5|Briefly described|p374.|Albian|Albian|Eromanga Basin. Contains marine oil shales which are geochemically similar to asphaltite strandings along the Bight coast.|||||Includes marine oil shales.|
18375|Toolebuc Formation|61611|6|Mentioned|p265 Fig. 3|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||13-MAR-09
18375|Toolebuc Formation|61613|6|Mentioned|p282 Fig. 2|Early Cretaceous|Early Cretaceous|Of Maree Subgroup. Geological Province: Eromanga Basin.||||||07-FEB-11
18375|Toolebuc Formation|61614|6|Mentioned|p290 Fig. 2|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||17-MAR-09
18375|Toolebuc Formation|62376|5|Briefly described|p84|Early Cretaceous|Early Cretaceous|Geological Province: Pedirka Basin.||||||09-FEB-10
18375|Toolebuc Formation|62537|6|Mentioned|p191 Fig.2. |Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Bulldog Shale. Is overlain by Allaru Formation.||
18375|Toolebuc Formation|62730|5|Briefly described|p352 Fig. 1|Cretaceous|Cretaceous|Geological Province: Eromanga Basin.||||||21-APR-08
18375|Toolebuc Formation|62837|5|Briefly described|Stratigraphic columns|Early Cretaceous|Early Cretaceous|Of the Rolling Downs Group. Age: ~101-~98Ma. Geological Province: Southern Cape York and Burketown Depression.||||||01-MAR-10
18375|Toolebuc Formation|63979|2|Defined|p50, Fig. 44|Albian|Albian|Previously Toolebuc Member (Wilgunya Fm). Conformable over Wallumbilla Fm; overlain by Allaru Mudstone. Max.thick: 65m. Predominantly mudstone with thin layers of siltstone, sandstone and conglomerate, towards top; also contains limestone (incl. coquinite)||||||09-APR-13
18375|Toolebuc Formation|64048|5|Briefly described|p64 Tb. 2|||Source of hydrocarbons - oil shale. Geological Province: Eromanga Basin.||||||07-FEB-11
18375|Toolebuc Formation|64197|6|Mentioned|p625 Fig.1c, p630 Figs.6,7|Cretaceous|Cretaceous|Eromanga Basin.||Unit in Marree Subgroup.||Underlies Allaru Mudstone; overlies Wallumbilla Formation.||11-DEC-15
18375|Toolebuc Formation|64665|6|Mentioned|p62.|Cretaceous|Cretaceous|Eromanga Basin.||||||
18375|Toolebuc Formation|64778|6|Mentioned|p13|Cretaceous|Cretaceous|Pedirka and Simpson Desert Basins.||||||
18375|Toolebuc Formation|64820|5|Briefly described|pS6 Fig. 4|Late Albian|Late Albian|Of the Rolling Downs Group. Carbonaceous to calcareous silt-claystone with minor sandstones. Geological province: Weipa Sub-basin, Carpentaria Basin.||||||
18375|Toolebuc Formation|65238|5|Briefly described|p7 Fig. 8|Early Cretaceous|Early Cretaceous|Geological province: Eromanga Basin. Transgressive marine deposits.||||||
18375|Toolebuc Formation|65342|5|Briefly described|p9.|||Eromanga Basin. Max. thickness at least 52 m. Seen as having potential as an insulating layer for geothermal energy.||||Overlies Bulldog Shale. Is overlain by Oodnadatta Shale.|Limestone, calcareous bituminous shale.|
18375|Toolebuc Formation|65385|5|Briefly described|pS134 Fig.7|Early Cretaceous|Early Cretaceous|Of Eromanga Basin. Overlies Wallumbilla Formation. Overlain by Allaru Mudstone.||||||08-MAR-12
18375|Toolebuc Formation|65489|5|Briefly described|p49, p55, p58, p96, p155|Early Cretaceous|Early Cretaceous|Eromanga Basin. 60m thick. Oil shale potential.||||Overlies Wallumbilla Formation. Is overlain by Allaru Mudstone.||
18375|Toolebuc Formation|66529|5|Briefly described|p10, p12, p16-17, p41, p92    |Mesozoic|Mesozoic|Eromanga Basin. Previously investigated for oil shale. An ideal in situ reductant for U systems.|c.107 Ma.|Unit in Rolling Downs Group.||Overlies Wallumbilla Formation. Is overlain by Allaru Mudstone.|Significant organic content. Black shale.|
18375|Toolebuc Formation|66623|6|Mentioned|p264.|||||||Is overlain by Allaru Mudstone.||
18375|Toolebuc Formation|66915|5|Briefly described|p6 Fig.3, p16|Cretaceous|Cretaceous|Eromanga and Carpentaria Basins. In later Rolling Downs Group units, the Toolebuc Formation is the only distinct and laterally persistent seismic reflection for correlation and is widespread in the Eromanga Basin.|||||Includes a thin competent unit of calcareous and bituminous shale, and limestone (a distinct and laterally persistent seismic reflection for correlation).|
18375|Toolebuc Formation|67323|5|Briefly described|p39, p81, p85-89, p93-94, p95 Fig.12.5|Early Cretaceous|Early Cretaceous|See also p96, GIS attrib tbl, Solid Geology Map. Eromanga/Carpentaria Basins. Oil shale was discovered in two wells (AAP Fermoy 1 and AAP Mayneside 1) in this unit by Australian Aquitaine Petroleum Pty Ltd in 1966. Attention shifted to outcrops in Julia Creek but activity ceased in 1969. Widespread shallow-marine deposits. Hydrocarbon exploration target in the Eromanga Basin; bituminous shale occurs throughout its extent. Considered prospective for U in the Carpentaria Basin.||||Overlies Wallumbilla Formation. Is overlain by Allaru Mudstone.|Calcareous bituminous shale, limestone.|
18375|Toolebuc Formation|67402|4|Described|p108, p109, p112|Albian|Albian|Eromanga Basin. Generally only between 20-45m thick but may be up to 65m thick. Deposited in a restricted marine environment. See also  p113 fig ERO12, p123, p176, p177, p179 fig CRP/KRM6, p180, p181.||Rolling Downs Group||Overlies the Wallumbilla Formation. Conformably overlain by the Allaru Mudstone.|Mudstone dominated succession that also contains limestone that is subordinate to calcareous, bituminous siltstone, labile sandstone and shale.|
18375|Toolebuc Formation|67561|6|Mentioned|p53 Fig.3|||||||||
18375|Toolebuc Formation|67784|5|Briefly described|p25-26, p28-29, p31-32, p34|Albian|Albian|6-25m thick. Carpentaria, northern Eromanga Basins. Appears as Toolebuc Limestone in Tb.1 (p28). Euxinic facies.||Wilgunya Subgroup.||Overlain by Allaru Mudstone. Overlies Ranmoor Member/Coreena Member (Wallumbilla Formation). Is correlated with Oodnadatta Formation|Contains distinctive Inoceramus coquinites and oil shale.|08-FEB-18
18375|Toolebuc Formation|67870|5|Briefly described|p46-47, p50-52|Late Cretaceous|Late Cretaceous|Hydrocarbon seal.|||||Shaly limestone, marl, organic-rich (10% TOC) limestone, sandstone.|
18375|Toolebuc Formation|68206|5|Briefly described|p31, 33|Albian|Albian|NE Eromanga Basin. See also reference to Toolebuc Limestone (p32).||||Overlies Ranmoor Member (Wallumbilla Formation). Is overlain by Allaru Formation.|Limestone; distinctive Inoceramus coquinites and oil shale.|
18375|Toolebuc Formation|68279|6|Mentioned|p19|||Galilee Basin stratigraphic cross-section, and mineralogy table.||||||
18375|Toolebuc Formation|68307|5|Briefly described|p92|Early Cretaceous|Early Cretaceous|Eromanga-Carpentaria Basin. Organic-rich. Forms a strong reflective seismic horizon.||||||
18375|Toolebuc Formation|68553|6|Mentioned|Map legend; schematic diagram.|Cretaceous|Cretaceous|Eromanga and Carpentaria Basins.||Unit in Rolling Downs Group.||Conformably overlies Wallumbilla Formation. Is overlain conformably by Allaru Mudstone.||
18375|Toolebuc Formation|68731|6|Mentioned|pp209-211|||||||||
18375|Toolebuc Formation|68734|5|Briefly described|p218 Fig.2|Albian|Albian|Eromanga Basin (NE). Shallow marine.||Of the Rolling Downs Group.||||
18375|Toolebuc Formation|68821|5|Briefly described|p292 Fig.1, p295, p296, p298|Cenomanian|Cenomanian|Lower Cretaceous age. Parallic to marine sediments. Contains ubiquitous disseminated pyrite. Equivalent in age to the Surat Siltstone.|101 - 98 Ma|Of the Rolling Downs Group.|||Dominantly organic-rich black shale with thin (< 3 cm) beds of limestone.|
18375|Toolebuc Formation|69019|5|Briefly described|p85 Fig.21.|Albian|Albian|Southern Eromanga Basin.||||Overlies Oodnadatta and Wallumbilla Formations. Is overlain by Allaru Mudstone.||
18375|Toolebuc Formation|69023|6|Mentioned|p89 Fig.20, p99|Albian|Albian|||||||
18375|Toolebuc Formation|69056|6|Mentioned|Reference images sheet.|||Shown on the simplified surface geology map of the Quamby Project area.||||||
18375|Toolebuc Formation|69206|6|Mentioned|p2|Cretaceous|Cretaceous||||||Immature oil shale.|
18375|Toolebuc Formation|69297|5|Briefly described|p273, p274 fig 4. 3, p275|Upper Albian|Upper Albian|Carpentaria Basin. The carbonaceous mudstones are the best potential source rocks in the basin.||Rolling Downs Group||Overlies the Wallumbilla Formation. Overlain by the Allaru Mudstone.|Carbonaceous mudstone, siltstone and claystone.|
18375|Toolebuc Formation|69454|6|Mentioned|p38:3|||Eromanga Basin.||||||12-JUL-16
18375|Toolebuc Formation|69455|6|Mentioned|p39:4 Fig.39.3|Early Cretaceous|Early Cretaceous|||||||12-JUL-16
18375|Toolebuc Formation|69457|3|Fully described|p41:2-3;41:5 Fig.41.4;41:6-8,10-12,15-18|Albian|Albian|Casey (1959). Eromanga, Carpentaria Basins. Widespread occurrence in drillholes. Shallow-marine deposits. Up to 65m thick. This unit and the Allaru Mudstone are together equivalent to the middle and upper part of Oodnadatta Formation. Has a distinctive, strong gamma signature in wireline logs. Regarded as an oil shale in the NE part of the Basin in Qld. A rich oil-gas source rock, the mudstone typically has a high TOC, generally 9-20%, locally 35%, derived from planktonic algae and cyanobacterial mats; it is an attractive oil shale and unconventional petroleum exploration target. Contains diverse fossil assemblages.||Wilgunya Subgroup.||Conformably overlies Wallumbilla Formation. Is overlain conformably by Allaru Mudstone.|Dark grey to black mudstone which may be carbonaceous, calcareous or pyritic, with thin layers of siltstone; subordinate labile sandstone, limestone, marl and conglomerate.|12-JUL-16
18375|Toolebuc Formation|69582|5|Briefly described|p22, p25-p26, p29, p65-p66|Lower Cretaceous|Lower Cretaceous|Eromanga Basin. Deposited in a marine depositional environment. Intersected in GSQ Longreach 2 drillhole.||||Overlies the Wallumbilla Formation. Overlain by the Allaru Mudstone.|Mudstone.|
18375|Toolebuc Formation|69591|6|Mentioned|p101 Fig.2.96|||||||Overlies Wallumbilla Formation. Is overlain by Allaru Formation.||
18375|Toolebuc Formation|69594|4|Described|p518-519, p521-522, p526, p529-530, p533|Albian|Albian|See also p574. Carpentaria, Eromanga Basins. A thin, isochronous unit up to 65m thick; generally 20-45m. Represents maximum marine conditions within an epeiric basin system. Early late Albian. Contains oil shales; may also be prospective for shale gas. Has a distinct and strong gamma signature. Contains spectacular vertebrate fossils (listed).||Rolling Downs Group.||Overlies Wallumbilla Formation. Is overlain conformably by Allaru Mudstone.|Coquinitic limestone, nodular limestone, oil shale, kerigenous shale, with minor siltstone and labile sandstone.|
18375|Toolebuc Formation|69673|6|Mentioned|p12 t5, p159, p160, p164, p165|||Prospective for unconventional hydrocarbons. Potential oil/gas source rock.||Wilgunya Subgroup||Overlain by Allaru Mudstone, overlies Wallumbilla Formation|Mudstone with thin layers of siltstone and subordinate labile sandstone, limestone, marl and conglomerate.|
18375|Toolebuc Formation|69797|5|Briefly described|p17 Fig.2|Early Cretaceous|Early Cretaceous|Geol. Prov: Eromanga Basin. Presented in figure as Toolebuc Fm.||||||
18375|Toolebuc Formation|69946|3|Fully described|p23-26, p57, p94|Albian|Albian|Originally Toolebuc Member (Casey, 1959) of the Wilgunya Formation. Later upgraded to Toolebuc Limestone (Vine et al., 1967), then defined as Toolebuc Formation by Senior et al. (1975). Casey's type section, outcrop on the Boulia-Winton Road 7 miles (11.3km) E of the Hamilton Hotel, was replaced because of poor outcrop by Senior et al. (1975) by the interval 25.3 - 35.8 m in BMR Boulia 3A. A reference section was also assigned to Boulia 3 (25 - 36m). High gamma ray response: its role in identifying Wallumbilla Formation mis-correlations from Qld into SA is discussed. Up to 50m thick. Wireline log correlations.||||Conformably overlies Wallumbilla Formation. Passes laterally into Oodnadatta Formation. Is overlain conformably by Allaru Mudstone.|Black calcareous and carbonaceous mudstone with abundant fish remains; dark grey fossiliferous mudstone with coquinite comprising large bivalve shells; dark grey mudstone. Bituminous shales in the type section; local oil shale origins.|
18375|Toolebuc Formation|69947|5|Briefly described|p13 Fig.7.2|Early Cretaceous|Early Cretaceous|Eromanga Basin.||Marree Subgroup.||||
18375|Toolebuc Formation|69948|6|Mentioned|Fig.4.18|||Eromanga Basin.||||Overlies Wallumbilla Formation. Is overlain by Allaru Mudstone.||
18375|Toolebuc Formation|70354|5|Briefly described|Map legend|Cretaceous|Cretaceous|||Rolling Downs Group.||Overlies Wallumbilla Formation. Is overlain by Allaru Mudstone.|Calcareous bituminous shale and limestone.|
18375|Toolebuc Formation|70572|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|||Wilgunya Subgroup|||Calcareous bituminous shale and limestone.|20-JAN-22
18375|Toolebuc Formation|70574|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|||Wilgunya Subgroup|||Calcareous bituminous shale and limestone.|18-JAN-22
18375|Toolebuc Formation|70821|5|Briefly described|p21, p33, p80|Early Cretaceous|Early Cretaceous|Eromanga Basin. Absent in the southern Thomson region.||Rolling Downs Group.||Overlies Oodnadatta and Wallumbilla Formations. Is overlain by Allaru Mudstone.||
18375|Toolebuc Formation|70823|5|Briefly described|p25-p27, p43-p44, p78|Early Cretaceous|Early Cretaceous|Eromanga Basin. Up to 60m thick. Deposited in a restricted, stratified and anoxic marine environment. Hosts an oil shale source rock.||||Overlies the Wallumbilla Formation. Overlain by the Allaru Formation.||
18375|Toolebuc Formation|70824|5|Briefly described|p9|Cretaceous|Cretaceous|Eromanga Basin. Hosts oil shale source rocks.||||Overlies the Wallumbilla Formation. Overlain by the Allaru Mudstone.||
18375|Toolebuc Formation|70836|6|Mentioned|p474|Albian|Albian|||||Coeval with Griman Creek Formation.||
18375|Toolebuc Formation|70860|6|Mentioned|p281|||Great Artesian Basin.||||||
18375|Toolebuc Formation|71059|6|Mentioned|p6 Fig.5|||Eromanga Basin.||||||
18375|Toolebuc Formation|71321|6|Mentioned|p15|||Of Eromanga Basin.||||Overlies the Wallumbilla Formation. Overlain by the Allaru Mudstone.||24-OCT-19
18375|Toolebuc Formation|71342|3|Fully described|Ch4 p25, Ch5 p23-p25|Late Albian|Middle Albian|Eromanga Basin. Originally named by Casey (1959) the Toolebuc Member of the Wilgunya Formation. Vine et al (1967) subsequently upgraded the member to formation status as the Toolebuc Limestone. Senior et al (1975) redefined the Limestone as the Toolebuc Formation. The type section for this unit was originally assigned to outcrop on the Boulia-Winton Road by Casey (1959). The BMR defined a new type section in Boulia 3A due to poor outcropping of the original section. A reference section was also given. Distribution and wireline log characteristics are given. A maximum thickness of 50m is recorded in Haddon Downs 1 in the northern Cooper region. Age derived from fossil assemblage and palynological studies. Interpreted to have been deposited in a restricted marine environment. Spore-pollen zone is given in Ch5 p57. See also Ch5 p57, Ch6 p9, Ch7 p13, Ch12 p12, Ch12 p14.||||Conformably overlies the Wallumbilla Formation. Conformably overlain by the Allaru Mudstone.|Black calcareous and carbonaceous mudstone with abundant fish remains, dark grey fossiliferous mudstone with coquinite containing abundant bivalves and bituminous shales.|
18375|Toolebuc Formation|71382|5|Briefly described|p4, p11, p13, p16-p17|||Eromanga Basin. Intersected in GSQ Julia 1 from 156.65m-199.87m for a total of 43.22m thickness. Deposited during widespread shallow marine conditions. Temp log and stratlog are provided. Lithology is described in detail on p21. See also p21, p23, p25, p27, App 3, 4.||||Overlies the Wallumbilla Formation. Overlain by the Allaru Mudstone.|Mudstone and calcareous mudstone.|
18375|Toolebuc Formation|71601|6|Mentioned|p120, p121|Albian|Albian|NW Qld. Includes dinosaur fossils provisionally assigned to Minmi.||||||
18375|Toolebuc Formation|71855|4|Described|p1-p2, p4-p6, p9-p11, p13, p15, p18, p20|Early Cretaceous|Early Cretaceous|Eromanga and Carpentaria basins. This unit has three distinct lithofacies which are described. In places the contact with the underlying Wallumbilla Formation is faulted or disconformable. This unit is highly organic rich and has good source rock charactersitcs. Wireline log responses were described for this unit including Gamma-ray, sonic transit time and resistivity. Structure, geochemistry and source rock potential are discussed. Typically greater than 15m thick. See also p22-p35, p42-p44, p47-p50, p52-p53, p56-p57, p61-p64, p66-p68, p73-p75.||Rolling Downs Group||Conformably (gradationally) overlies the Wallumbilla Formation. Conformably (gradationally) overlain by the Allaru Mudstone. Overlain by the Mackunda Formation.|Calcareous mudstone, coquinitic mudstone and organic-rich, slightly calcareous mudstone without calcite laminae.|
18375|Toolebuc Formation|71863|4|Described|p1-p18|Albian|Albian|Eromanga and Carpentaria basins. Originally defined as the Toolebuc Limestone by Vine et al. (1967). Subsequently this unit was redefined by Senior et al (1975) as the Toolebuc Formation due to recognition of significant mudstone component. The type section is defined in BMR Boulia 3A (Burger, 1974; Senior et al., 1975). Deposited during a marine incursion. Mudstone may contain laminae of carbonate form from bivalve remains Inoceramus and Aucellina (Ozimic, 1986). Deposited in a restricted, oxygen depleted marine environment. Wireline log characteristics, geochemistry, sedimentary facies, fossil assemblage, petroleum resources and mineralisation are discussed. Equivalent to the Wooldrige Limestone Member and Urisino beds.||Rolling Downs Group||Conformably overlies the Wallumbilla Formation. Conformably overlain by the Allaru Mudstone. Equivalent to the Wooldridge Limestone Member and Urisino beds.|Laminated calcareous and kerogenous mudstone, minor coquinite and limestone, labile sandstone and oil shale.|01-MAY-19
18375|Toolebuc Formation|72297|5|Briefly described|p712, p721, p728, p746, p751-753, p755|Early Cretaceous|Early Cretaceous|Eromanga and Carpentaria Basins. Julia Creek area; occurs north as far as 16 degrees S. Oxidised oil shales in the upper part produce soft oxide coquina, with associated large molybdenum and vanadium resources. Hosts a large gypsum deposit at Hughenden; other localities mentioned. An excellent though immature hydrocarbon source rock. Very high potential shale oil resources (perhaps the most extensive in Australia) despite very low grade; eg Julia Creek oil shale deposit (described).||||Conformably overlies the Ranmoor Member (Wallumbilla Formation). Is overlain conformably by the Allaru Mudstone.|A flat-lying unit comprising an upper, coarse limestone-clay-oil shale unit and a lower, fine carbonate-clay-oil shale unit. Contains mudstones rich in organic kerogenous material.|
18375|Toolebuc Formation|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA,QLD,NSW), Carpentaria Basin.||Rolling Downs Group.||Overlies Coreena and Ranmoor Members (Wallumbilla FZ). Is overlain by Allaru Mudstone.||
18375|Toolebuc Formation|72799|6|Mentioned|p27|||||||||
18375|Toolebuc Formation|72913|6|Mentioned|p8.|||Three wells intersected this cover unit.||||||
18375|Toolebuc Formation|72967|6|Mentioned|p5|||Carpenteria Basin.||Rolling Downs Group||||
18375|Toolebuc Formation|73083|6|Mentioned|p58, p62-63|||||||Underlain by the Wallumbilla Formation.|Includes shale and subordinate limestone.|
18375|Toolebuc Formation|73137|6|Mentioned|p6|Cretaceous|Cretaceous|||||||
18375|Toolebuc Formation|73144|6|Mentioned|p8, p13|Cretaceous|Cretaceous|Carpentaria Basin. Aquitard with potential shale gas/oil play.||Rolling Downs Group||Underlain by Wallumbilla Formation. Overlain by Allaru Mudstone.||
18375|Toolebuc Formation|73147|5|Briefly described|p129|Aptian|Aptian|||Rolling Downs Group.||Overlies Wallumbilla Formation. Is overlain by Allaru Mudstone.||
18375|Toolebuc Formation|73167|6|Mentioned|p664 Fig. 2|Cretaceous|Cretaceous|Eromanga Basin.||||||
18375|Toolebuc Formation|73249|5|Briefly described|p319, p321, p323|Albian|Albian|Eromanga Basin. Deposited in a marine environment.||||Overlies the Wallumbilla Formation, underlies the Allaru Mudstone, lateral equivalent of the Coorikiana Sandstone.|Mudstone.|
18375|Toolebuc Formation|73251|6|Mentioned|p62|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Underlain by Wallumbilla Formation. Overlain by Allaru Mudstone. Equivalent to Oodnadatta Formation.||
18375|Toolebuc Formation|73281|6|Mentioned|Appendix (DIP)|||See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
18375|Toolebuc Formation|73343|6|Mentioned|p337|Cretaceous|Cretaceous|Eromanga Basin.||||Underlain by Wallumbilla Formation. Overlain by Allaru Mudstone. Equivalent to Oodnadatta Formation.||
18375|Toolebuc Formation|73479|5|Briefly described|p156 Fig.2, p159|Cretaceous|Cretaceous|Eromanga Basin. Open shallow marine depositional environment.|ca 103 Ma|||Overlies Wallumbilla Formation, underlies Allaru Mudstone||
18375|Toolebuc Formation|73553|6|Mentioned|p7|Cretaceous|Cretaceous|||||||
18425|Top Rocky Rhyolite|23363|5|Briefly described|352 Tab.3|Statherian|Statherian|Age: 1725+/-3Ma.||||||12-DEC-06
18425|Top Rocky Rhyolite|23398|4|Described|p437|Statherian|Statherian|Age: 1725+/-3Ma.||||||12-DEC-06
18425|Top Rocky Rhyolite|24442|5|Briefly described|p22 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of the Carrara Range Group.  Geological Province: McArthur Basin.  See also p23 Fig. 2.||||||07-NOV-08
18425|Top Rocky Rhyolite|38237|6|Mentioned|p126|||||||||
18425|Top Rocky Rhyolite|39338|5|Briefly described|p352|||||||||
18425|Top Rocky Rhyolite|39422|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Carrara Range Group.  Massive reddish-brown feldspar porphyry, probably rhyolite; minor basalt or trachyte.  Unconformably overlies Mitchiebo Volcanics; unconformably overlain by Musselbrook Formation (McNamara Group).||||||12-DEC-06
18425|Top Rocky Rhyolite|39497|4|Described|p10|||||||||
18425|Top Rocky Rhyolite|39925|6|Mentioned|p331|||See also p337.||||||12-DEC-06
18425|Top Rocky Rhyolite|40811|6|Mentioned|p318|||||||||
18425|Top Rocky Rhyolite|45166|5|Briefly described|p27|||||||||
18425|Top Rocky Rhyolite|49018|2|Defined|p5|Carpentarian|Carpentarian|||||||
18425|Top Rocky Rhyolite|62659|5|Briefly described|Map Legend|Statherian|Statherian|Of the Carrara Range Group. Pink, porphyritic, massive to flow banded, spherulitic to microgranophyric rhyolite; local autobreccia, peperite and hyaloclastite.||||||
18425|Top Rocky Rhyolite|63109|6|Mentioned|p1109|||||||||
18425|Top Rocky Rhyolite|63866|5|Briefly described|p57|Statherian|Statherian|Carrara Range, Leichhardt Superbasin.|1725 +/- 3 Ma (Page et al., 2000)|||Overlies the Michiebo Volcanics. Possibly equivalent to the Eastern Creek Volcanics.||
18425|Top Rocky Rhyolite|65337|3|Fully described|p6 Fig.3, p10 Table 3, pp14-16. |||Thickness to 400 m of moderate-aspect-ratio lava flow(s) and marginal ephemeral alluvial and debris flows. Described in detail.|1725 +/- 3 Ma (Page et al. 2000).|Unit in Carrara Range Group.||Overlies Gator Sandstone. Is unconformably overlain by Surprise Creek Formation and, locally, by Bullrush Conglomerate.|Lower part: pink, quartz and K-feldspar porphyritic, massive to flow banded, spherulitic to microgranophyric rhyolite; local autobreccia, peperite and hyaloclastite. Upper part: poorly-sorted matrix-supported pebble to boulder conglomerate.|
18425|Top Rocky Rhyolite|69433|4|Described|p18:2, 6-9|Statherian|Statherian|Southern succession, Lawn Hill Platform. Up to 400m thick. SHRIMP U-Pb zircon age.|1725 +/- 3 Ma (Page et al., 2000).|Carrara Range Group.||Unconformably overlies Gator Sandstone and locally the Mitchiebo Volcanics. Is overlain unconformably by Surprise Creek Volcanics or Bullrush Conglomerate.|Coherent porphyritic rhyolite, overlain by matrix-supported conglomerate, with subangular to subrounded, locally imbricated clasts set in a pink lithic gravel-sand-mud matrix, and crudely horizontally stratified and ungraded.|12-JUL-16
18425|Top Rocky Rhyolite|69673|4|Described|p52 fig 42,|Statherian|Statherian|Up to 400m thick.|1725 +/- 3 Ma|Carrara Range Group|||Rhyolite overlain by matrix supported conglomerate with imbricated clasts set in a gravel-sand-mud matrix.|
18425|Top Rocky Rhyolite|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1725+/-3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Rhyolite.|
18425|Top Rocky Rhyolite|72526|5|Briefly described|p8 Fig.1.3.|Paleoproterozoic|Paleoproterozoic|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.|1725 +/-3 Ma|Carrara Range Group||Overlies Gator Sandstone and shown as underlying Fiery Creek Volcanics and Bigie Formation.||
18425|Top Rocky Rhyolite|72527|4|Described|p7, 87, 89, p119-120, p127-129, 194,196|Paleoproterozoic|Paleoproterozoic|One of three units considered to represent c. 1725 Ma felsic volcanism in the region, including Peters Creek Volcanics and Hobblechain Volcanics. Provides maximum age for overlying Bullrush Conglomerate.  See also p147-148, p154.|1725 +/- 3 Ma (Page et al 2000)|Top of Carrara Range Group||Unconformably overlies Gator Sandstone, unconformably underlies Surprise Creek Formation, Bullrush Conglomerate, and is laterally equivalent to Peters Creek Volcanics.||
18425|Top Rocky Rhyolite|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the East part of the South Nicholson Basin and the Lawn Hill Platform. U-Pb zircon igneous crystallisation age shown.|1725 +/- 3 Ma|Carrara Range Group||Overlies Gator Sandstone and is shown as unconformably underlying Fiery Creek Volcanics and Bigie Formation.||
18425|Top Rocky Rhyolite|72919|6|Mentioned|p5|Paleoproterozoic|Paleoproterozoic|||Carrara Range Group||Unconformably underlain by Gator Sandstone. Unconformably overlain by Surprise Creek Formation.||
18425|Top Rocky Rhyolite|73042|6|Mentioned|p4|Statherian|Statherian|South Nicholson Basin region, Calvert Superbasin. Geochronology is a U-Pb zircon igneous crystallisation age.|1725 +/- 3 Ma (see Fig.1.2)|Carrara Range Group||Underlain by Gator Sandstone. Unconformably overlain by Surprise Creek Formation*.||
18425|Top Rocky Rhyolite|73043|6|Mentioned|p15 Fig.8|Paleoproterozoic|Paleoproterozoic|Age determination from Page et al. (2000).|1725 +/- 3 Ma|||||
18426|Top Springs Limestone|23981|6|Mentioned|p65|||Geological Province:  western Georgina Basin (NT).||||||
18426|Top Springs Limestone|24303|6|Mentioned|p63 Appendix|||Correlative of Gum Ridge Formation.||||||
18426|Top Springs Limestone|34149|6|Mentioned|Map legend|Middle Cambrian|Early Cambrian|Lower or Middle Cambrian||||||
18426|Top Springs Limestone|34439|6|Mentioned|p9|||M.Camb.||||||
18426|Top Springs Limestone|36473|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian to Ordovician||||||
18426|Top Springs Limestone|39791|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
18426|Top Springs Limestone|41013|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
18426|Top Springs Limestone|41268|6|Mentioned|Fig.15|||||||||
18426|Top Springs Limestone|41406|6|Mentioned|Map legend|Ordovician|Cambrian|||||||
18426|Top Springs Limestone|42638|5|Briefly described|Map legend|Middle Cambrian||||||Not shown in schematic sections.|Sandstone; trace fossils.|09-NOV-11
18426|Top Springs Limestone|42639|2|Defined|p46, p75|Ordian|Ordian|Age: Ordian (early Middle Cambrian)||||||
18426|Top Springs Limestone|44287|14|Not recorded|p.14, opp.11|||Redlichia found. (E53-3).||||||
18426|Top Springs Limestone|44288|14|Not recorded|map legend||Cambrian|Massive limestone, laminated cherty limestone. Lower to Middle Cambrian.||||||
18426|Top Springs Limestone|44473|14|Not recorded|p.7,10-12,15,opp.p.7|||(E53-7). M. or L.Cambrian in age.||||||
18426|Top Springs Limestone|44474|14|Not recorded|map legend|||Middle or Lower Cambrian.||||||
18426|Top Springs Limestone|45032|14|Not recorded|p9|Middle Cambrian|Early Cambrian|Tb.1,12, Pl.1. Lower or Middle Cambrian.||||||
18426|Top Springs Limestone|45162|3|Fully described|p153|||Mention p152.||||||12-DEC-06
18426|Top Springs Limestone|46792|6|Mentioned|p53|||||||||
18426|Top Springs Limestone|60990|6|Mentioned|p85|Middle Cambrian|Middle Cambrian|Georgina Basin. Faunal links with Antarctica.||||||
18426|Top Springs Limestone|63569|6|Mentioned|p123|Cambrian|Cambrian|Georgina Basin. Contains lingulate brachiopods that correlate with Redlichia guizhouensis Zone of China.||||||
18426|Top Springs Limestone|64068|6|Mentioned|p59, 225|||Of northern Georgina Basin. Correlated with Thorntonia Limestone.||||||
18426|Top Springs Limestone|64443|6|Mentioned|p40.|Middle Cambrian||||Of Barkly Group.||||14-MAY-14
18426|Top Springs Limestone|64784|6|Mentioned|p2,3,6,8 Figs.2-6|Cambrian|Cambrian|Beetaloo Basin.||||Overlies Antrim Plateau Volcanics.||
18426|Top Springs Limestone|64815|6|Mentioned|p5|Cambrian|Cambrian|Georgina Basin. Blankets parts of McArthur Basin.||||||
18426|Top Springs Limestone|65337|5|Briefly described|p61.|Middle Cambrian|Middle Cambrian|Northern Georgina Basin. Carbonates.||||Overlies Bukalara Sandstone. Unconformably overlies Kalkarindji Volcanic Group.||
18426|Top Springs Limestone|67144|5|Briefly described|Map legend.|Middle Cambrian|Middle Cambrian|||Unit in Barkly Group.||Unconformably overlies Bukalara Sandstone. Is unconformably overlain by Anthony Lagoon Formation.|Pale grey micritic limestone, karstic-weathering; commonly vuggy, also oncolitic, pisolitic textures; surface commonly potholed; rare large domal stromatolites.|
18426|Top Springs Limestone|67352|4|Described|v, p4,19,20,23,46-47,49-51,59,69|Middle Cambrian|Middle Cambrian|Northern Georgina Basin. Underlies a generally flat erosion surface. On p50 the topmost Bukalara Sandstone is taken to be within it but its basal siliciclastic layer is indistinguishable from the underlying Mainoru Formation. 92 m thick. Contains varied fauna common to Daly, Wiso, Ord and Georgina Basins and even Antarctica.||Barkly Group||Disconformably overlies Bukalara Sandstone. Lateral equivalent of Gum Ridge Formation.|Partially dolomitised, mottled bioclast, peloid and oncoid limestone, minor brecciated limestone and microbial laminite, rare fenestral limestone. Evaporite lenses, nodules, veins, collapse breccias; dolomitised, peloidal calcimudstone matrix.|
18426|Top Springs Limestone|69430|6|Mentioned|p15:29, 62|Cambrian|Cambrian|||||Unconformably overlies Antrim Plateau Volcanics.||12-JUL-16
18426|Top Springs Limestone|69437|5|Briefly described|p22:9-10|Series 2|Series 2|Northern Georgina Basin, Centralian B Superbasin. Sequence 1. Shallow-marine to peritidal deposits.||||Is overlain by Anthony Lagoon Formation. Equivalent to Gum Ridge Formation.||12-JUL-16
18426|Top Springs Limestone|69443|3|Fully described|p28:16, 21-22|Middle Cambrian|Middle Cambrian|Plumb and Rhodes (1963, 1964). Northern Georgina Basin. Likely to be continuous under cover with Gum Ridge Formation. Crops out as karstified flat to undulating plains. 92m thick in the type section in cored drillhole DD86SC2 in central-northern WALHALLOW map area. Fossiliferous. Restricted marine shelf deposits.||Barkly Group.||Disconformably overlies Bukalara Sandstone. May be overlain conformably by Anthony Lagoon Formation. Is correlated with Narpa Group.|Partially dolomitised, mottled bioclast, peloid and oncoid limestone, minor brecciated limestone and microbial laminite, rare fenestral limestone; all prone to patchy silicification. Evaporite (mainly anhydrite) lenses, nodules and veins throughout.|12-JUL-16
18426|Top Springs Limestone|69445|5|Briefly described|p30:5, 17|Middle Cambrian|Middle Cambrian|Northern Georgina Basin.||||Unconformably overlies Helen Springs Volcanics (Kalkarindji Suite).||12-JUL-16
18426|Top Springs Limestone|69446|6|Mentioned|p31:3|||Georgina Basin. Broadly age-equivalent to Daly River Group(Daly Basin).||||||12-JUL-16
18426|Top Springs Limestone|69447|6|Mentioned|p32:2|||Georgina Basin.||||Age-equivalent to Montejinni Limestone, Hooker Creek Formation and Lothari Hill Sandstone (Wiso Basin).||12-JUL-16
18426|Top Springs Limestone|69448|6|Mentioned|p33:3|||Georgina Basin.||||Correlated with Negri Subgroup (Ord Basin) in part.||12-JUL-16
18426|Top Springs Limestone|69591|4|Described|p88|Cambrian|Cambrian|Undilla Sub-basin, Georgina Basin.||Barkly Group.||||
18426|Top Springs Limestone|69673|5|Briefly described|p117, p142|||||Barkly Group|||Dolomitised limestone, minor brecciated limestone, microbial laminite.|
18426|Top Springs Limestone|70380|6|Mentioned|p745|Stage 5|Stage 4|Northern Georgina Basin.||||||
18426|Top Springs Limestone|70752|6|Mentioned|p131, p141|Middle Cambrian|Middle Cambrian|Georgina Basin. Ordian. Brachiopod systematic palaeontological descriptions.||||||
18426|Top Springs Limestone|71632|5|Briefly described|Map legend.|||Georgina Basin. Mapped with Antrim Plateau Volcanics, Cox Formation, Nutwood Downs Volcanics and Bukalara Sandstone as a single unit.||||||
18426|Top Springs Limestone|72321|6|Mentioned|p4|||Of Barkly Sub-basin, NW Georgina Basin,||||Correlated with Hay River Formation, Gum Ridge Formation.||
18426|Top Springs Limestone|72516|6|Mentioned|p91|Cambrian|Cambrian|Georgina Basin.||||Equivalent to the Thorntonia Limestone.||02-JUN-21
18426|Top Springs Limestone|73083|6|Mentioned|p47-48|Cambrian|Cambrian|||||Unconformably underlain by Bukalara Sandstone.||
18438|Torpedo Creek Quartzite|22438|4|Described|p539, Fig.3 p537|||See also Fig.10a p546.||||||12-DEC-06
18438|Torpedo Creek Quartzite|22453|6|Mentioned|p 11|||||||||
18438|Torpedo Creek Quartzite|22585|6|Mentioned|Fig3 P738|||Actually spelt Torpedo Creek Qtz.||||||
18438|Torpedo Creek Quartzite|22680|6|Mentioned|85,86|||Of McNamara Group. Overlies Kamarga Volcanics, Yeldham Granite and Surprise Creek Formation.||||||
18438|Torpedo Creek Quartzite|23031|6|Mentioned|24|||Geological  province: Lawn Hill Subprovince. Of the McNamara Group.||||||12-DEC-06
18438|Torpedo Creek Quartzite|23073|5|Briefly described|p744 (Fig 2)|||||||||
18438|Torpedo Creek Quartzite|23198|6|Mentioned|p873|||||||||
18438|Torpedo Creek Quartzite|23387|6|Mentioned|p18 fig.19|||Of McNamara Group.||||||
18438|Torpedo Creek Quartzite|23393|4|Described|p18, p19|Paleoproterozoic|Paleoproterozoic|Of MacNamara Group. Overlain by Gunpowder Creek Formation.||||||07-NOV-08
18438|Torpedo Creek Quartzite|23396|5|Briefly described|p407 Fig.2|||Of the  McNamara Group.||||||12-DEC-06
18438|Torpedo Creek Quartzite|23397|5|Briefly described|p463|||Of the Mount Isa Group (?).||||||12-DEC-06
18438|Torpedo Creek Quartzite|23398|5|Briefly described|p447|||Of McNamara Group.||||||
18438|Torpedo Creek Quartzite|23399|4|Described|p493|||Of the McNamara Group.||||||12-DEC-06
18438|Torpedo Creek Quartzite|23406|6|Mentioned|p618|||Mentioned in terms of equivalents and correlatives.||||||
18438|Torpedo Creek Quartzite|23408|4|Described|p513 Fig. 2, p514, p15|||Of the  McNamara Group. Overlies Myally Subgroup.||||||15-JUN-09
18438|Torpedo Creek Quartzite|23466|5|Briefly described|p273|||||||||
18438|Torpedo Creek Quartzite|23518|4|Described|p12|Proterozoic|Proterozoic|Of McNamara Group.  Geological Province: Western Fold Belt.||||||
18438|Torpedo Creek Quartzite|23767|5|Briefly described|p1956 Fig. 2|||Geological Province: Western Fold Belt. See also p1957 Fig.3.||||||
18438|Torpedo Creek Quartzite|23958|5|Briefly described|p1134 Fig.2|Mesoproterozoic|Paleoproterozoic|Of McNamara Group.||||||07-NOV-08
18438|Torpedo Creek Quartzite|23965|5|Briefly described|p1297|Mesoproterozoic|Paleoproterozoic|Of McNamara Group. Geological Province: Mount Isa Inlier.||||||07-NOV-08
18438|Torpedo Creek Quartzite|24308|5|Briefly described|p987 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of the McNamara Group. Geological Province:  Mount Isa Superbasin||||||07-NOV-08
18438|Torpedo Creek Quartzite|24419|5|Briefly described|p16-17|Paleoproterozoic|Paleoproterozoic|Thin, widespread sandstone unit - polymictic conglomerate grading upwards into cross-bedded quartzose to feldspathic sandstone, siltstone and shale.  Conformably overlain by, and interfingers with Gunpowder Creek Fm.  Part of the Prize Supersequence.||||||26-FEB-18
18438|Torpedo Creek Quartzite|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Overlies Surprise Creek Formation.||||||
18438|Torpedo Creek Quartzite|30535|6|Mentioned|p403|||Refers Cavaney (1975).||||||12-DEC-06
18438|Torpedo Creek Quartzite|37459|2|Defined|p427|Mesoproterozoic|Mesoproterozoic|Age is more specifically Carpentarian.||||||01-OCT-08
18438|Torpedo Creek Quartzite|37568|5|Briefly described|p84|||||||||
18438|Torpedo Creek Quartzite|37816|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
18438|Torpedo Creek Quartzite|38232|6|Mentioned|p87|||||||||
18438|Torpedo Creek Quartzite|38237|4|Described|p127|||||||||
18438|Torpedo Creek Quartzite|38291|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
18438|Torpedo Creek Quartzite|38348|4|Described|p8|||||||||
18438|Torpedo Creek Quartzite|38350|4|Described|p15|||||||||
18438|Torpedo Creek Quartzite|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
18438|Torpedo Creek Quartzite|39445|5|Briefly described|Table 2|||See also p35.||||||12-DEC-06
18438|Torpedo Creek Quartzite|39497|6|Mentioned|Fig.4|||||||||
18438|Torpedo Creek Quartzite|39556|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||
18438|Torpedo Creek Quartzite|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the McNamara Group.  White medium orthoquartzite with gypsum pseudomorphs locally. Overlies the Surprise Formation; underlies the Gunpowder Creek Formation.||||||15-JUN-06
18438|Torpedo Creek Quartzite|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
18438|Torpedo Creek Quartzite|39925|6|Mentioned|Fig.9|||||||||
18438|Torpedo Creek Quartzite|39944|3|Fully described|p229|||||||||
18438|Torpedo Creek Quartzite|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
18438|Torpedo Creek Quartzite|40221|3|Fully described|p13|||||||||
18438|Torpedo Creek Quartzite|41298|6|Mentioned|Map legend|Carpentarian||||||||
18438|Torpedo Creek Quartzite|41307|4|Described|p16|||||||||
18438|Torpedo Creek Quartzite|42367|5|Briefly described|p18|||Of the McNamara Group.||||||12-DEC-06
18438|Torpedo Creek Quartzite|43235|5|Briefly described|p9,Fig.10.|||Of the McNamara Group.||||||12-DEC-06
18438|Torpedo Creek Quartzite|45161|5|Briefly described|Table 3|||||||||
18438|Torpedo Creek Quartzite|45166|5|Briefly described|p30|||||||||
18438|Torpedo Creek Quartzite|47083|3|Fully described|p14||Proterozoic|Previously included in Mammoth Formation. Of McNamara Gp. O'lying unit Gunpowder Crk Fm. U'lying unit Surprise Crk Fm. Maximum thickness 300 m.||||||
18438|Torpedo Creek Quartzite|49041|6|Mentioned|Table 4|||||||||
18438|Torpedo Creek Quartzite|50550|5|Briefly described|p1139 Fig.2||Statherian|Conformably overlies Surprise Creek Formation. Overlain by Gunpowder Creek Formation at a syn-rift unconformity. Geological Province: Western Fold Belt
.||||||20-JUN-22
18438|Torpedo Creek Quartzite|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the McNamara Group. Meta-arenite, quartzite; minor conglomerate.||||||
18438|Torpedo Creek Quartzite|61936|5|Briefly described|p194 Fig. 6|||Geological Province: Lawn Hill Platform, Western Fold Belt, Mount Isa Inlier.||||||23-FEB-20
18438|Torpedo Creek Quartzite|62535|5|Briefly described|p672|Statherian|Statherian|Lawn Hill Platform. Lithology not specified.||McNamara Group.||||
18438|Torpedo Creek Quartzite|63109|6|Mentioned|p1108 Fig. 3|||Geological Province: Calvert Superbasin. Consists of sandstone.||||||30-SEP-08
18438|Torpedo Creek Quartzite|63111|5|Briefly described|p1163 Fig. 3, p1171|Statherian|Statherian|Of Gun Supesequence. Age: ~ 1690+/-7Ma.  Geological Province: Calvert Superbasin. Consists of sandstone.||||||07-FEB-11
18438|Torpedo Creek Quartzite|63113|6|Mentioned|p1214 Fig.2, p1225 Fig.13. |||Part of Prize and Gun supersequences. Appears in Fig.2 only as Torp.|1659 Ma.|Of the McNamara Group||||
18438|Torpedo Creek Quartzite|63114|5|Briefly described|p1253 Fig.2. |||Appears only as Torpedo.||||||
18438|Torpedo Creek Quartzite|63115|6|Mentioned|p1279 Fig.4.|||Calvert and Isa superbasins.||||||
18438|Torpedo Creek Quartzite|63116|6|Mentioned|p1297 Fig.2, |||Calvert and Isa superbasins. Material properties detailed.||||||
18438|Torpedo Creek Quartzite|64250|6|Mentioned|p11 fig.3|||Western Fold Belt, Mount Isa Inlier.||||Overlies Surprise Creek Formation. Is overlain by Lower Gunpowder Creek Formation.||
18438|Torpedo Creek Quartzite|64834|5|Briefly described|p13 Fig.2|||Calvert Superbasin. Western Succession of Mount Isa Basin. Only shown as Torpedo in Fig.2.|||||Sandstone.|
18438|Torpedo Creek Quartzite|65337|5|Briefly described|p5, p33 Fig.27.|||Calvert Superbasin.||Unit in McNamara Group.||Overlies Surprise Creek Formation. Is overlain by Gunpowder Creek Formation.||
18438|Torpedo Creek Quartzite|65396|6|Mentioned|p82, p175, p241|||Calvert Superbasin. Cover Sequence 2. Lawn Hill Platform.||||Overlies Surprise Creek Formation; overlain by Lower Gunpowder Creek Formation||
18438|Torpedo Creek Quartzite|66844|5|Briefly described|p264-265,270|||Lawn Hill Platform. See also Torpedo Creek Formation [Names used interchangeably]. Abrupt thickness variations imply highly localised sediment sources and discrete depocentres.||Of lower McNamara Group; Prize Supersequence.||Basal unit within the Prize Supersequence. Overlain by lower Gunpowder Creek Formation.|Nonmarine and nearshore sandstone.|
18438|Torpedo Creek Quartzite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map; p34|Paleoproterozoic|Paleoproterozoic|Century and Mount Oxide Domains, Mount Isa Inlier. Isa (Calvert) Superbasin. See also reference to Torpedo Creek Formation (Mount Isa Block Time-Space Plot).|~1690-1670 Ma.|McNamara Group.|||White to medium orthoquartzite, with gypsum pseudomorphs locally.|
18438|Torpedo Creek Quartzite|68146|5|Briefly described|p84, p189, p199-200|||Mentioned in exactly the same context as Torpedo Creek Formation (p3, p86).||||Overlies Fiery Creek Volcanics. Lateral equivalent to Warrina Park Quartzite.||02-NOV-18
18438|Torpedo Creek Quartzite|68542|6|Mentioned|p6|||||Lower McNamara Group||Overlain by Gunpowder Creek Formation||
18438|Torpedo Creek Quartzite|68575|4|Described|p3, p6-7, p40, p52-60, p125, p127, p134|||Mount Isa Region. Other age determinations discussed: the authors favour 1697 +/- 12 Ma by Neumann et al. (2009). Has a provenance (detrital zircon populations) significantly different from Saint-Smith and Bularnu Formations. Whole rock Sm-Nd isotopic data and age (1757 Ma).|1756 +/- 16 Ma (maximum depositional age).|||Overlies Big Toby Granite and Surprise Creek Formation. Is overlain by Gunpowder Formation.|Well-sorted, medium-grained metamorphosed and silicified feldspathic sandstone.|
18438|Torpedo Creek Quartzite|68576|5|Briefly described|Q_2: p6|||Lawn Hill Platform, Mount Isa Inlier.||Lower McNamara Group.||Overlies Surprise Creek Beds. Is overlain by Gunpowder Creek Formation.||
18438|Torpedo Creek Quartzite|68732|6|Mentioned|p160, p168 Fig.5|||Prize Supersequence.|||||Siliciclastic sediments.|01-DEC-17
18438|Torpedo Creek Quartzite|69591|4|Described|p38 Fig.2.22, p40, p42-44, p54, p107|||Mount Oxide and Leichhardt River Domains, Calvert Superbasin. Part of Prize and Gun Supersequences. Fluvial/shoreface deposits. These maximum depositional ages, by Neumann et al. (2009), are for lower and upper parts respectively.|1697 +/- 12 Ma and ~1674 +/- 6 Ma.|Basal McNamara Group.||Unconformably overlies Yeldham Granite. Is overlain by Gunpowder Creek Formation.|White to medium orthoquartzite, with gypsum pseudomorphs locally. Basal quartzite and conglomerate unit.|
18438|Torpedo Creek Quartzite|70864|5|Briefly described|p75||Paleoproterozoic|||Base of McNamara Group|||Sandstone and conglomerate.|
18438|Torpedo Creek Quartzite|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1756+/-16 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
18438|Torpedo Creek Quartzite|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown, with Warrina Park Quartzite, as located in the Lawn Hill Platform, Leichhardt River Fault Trough and the Kalkadoon-Leichhardt Belt of the Mount Isa Province and the eastern part of the South Nicholson Basin.||||Overlies Surprise Creek Formation and partially underlies lower Gunpowder Creek Formation and is shown as unconformably underlying Mount Isa Group.||
18438|Torpedo Creek Quartzite|72912|5|Briefly described|p5 Fig.3, p13.|Statherian|Statherian|Of Calvert Superbasin. 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. Listed with Warrina Park Quartzite. Lateral equivalent? U-Pb zircon sedimentary depositional age of overlying 'lower Gunpowder Creek Formation' is 1694+/-3 Ma, and of underlying Surprise Creek Formation is 1688+/-5 Ma.||Of Prize supersequence.||Overlies Surprise Creek Formation and partially underlies Gunpowder Creek Formation, Lower. May unconformably underlie Moondarra Siltstone.||
18438|Torpedo Creek Quartzite|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin region and Mount Isa Province, Calvert Superbasin. Listed as Torpedo Creek/Warrina Park Quartzite in Fig.1.2; does not specify / distinguish between the two units.||||Uncertain distinction from Warrina Park Quartzite. Underlain by Surprise Creek Formation. Partly overlain by lower Gunpowder Creek Formation.||
18438|Torpedo Creek Quartzite|73144|6|Mentioned|p10|||Said to be part of the Prize Supersequence. Written as Torpedo Creek quartzite. [c.f. Torpedo Creek Formation p9, shown as part of the Gun Supersequence]||||||17-OCT-22
18438|Torpedo Creek Quartzite|73413|6|Mentioned|p3|||Mount Isa Inlier, Western Fold Belt, Lawn Hill Platform.||||||
18438|Torpedo Creek Quartzite|73525|5|Briefly described|p4-5 Fig.2|Statherian|Statherian|Mount Oxide-(Ardmore-May Downs) Domain.|1697+/-12 Ma maximum depositional age||||Siliciclastics.|
18529|Train Range Ironstone Member|23393|5|Briefly described|p21|Mesoproterozoic|Mesoproterozoic|Of Mullera Formation.||||||
18529|Train Range Ironstone Member|23937|5|Briefly described|p62|||Of the Mullera Formation (South Nicholson Group).  Geological Province: Roper Superbasin.  See also p93 Appendix 1.||||||
18529|Train Range Ironstone Member|24047|5|Briefly described|p27|||Equivalent to the Sherwin Formation.||||||
18529|Train Range Ironstone Member|38291|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
18529|Train Range Ironstone Member|38348|6|Mentioned|p24|||||||||
18529|Train Range Ironstone Member|39497|6|Mentioned|p15|||||||||
18529|Train Range Ironstone Member|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
18529|Train Range Ironstone Member|44922|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of Mullera Formation.||||||
18529|Train Range Ironstone Member|45166|5|Briefly described|p33|||||||||
18529|Train Range Ironstone Member|65337|5|Briefly described|p58.|||Several ironstone intervals in the lower Mullera Formation that were the focus of exploration: the Constance Range deposits. Mineralisation is due to primary depositional processes and local surficial supergene enrichment and fault-related fluid movement.||Unit in South Nicholson Group.|||Contains three or four ore-grade beds; mineralisation consists of oolitic hematite, siderite and chamosite beds: "Wabana type".|
18529|Train Range Ironstone Member|67323|5|Briefly described|GIS attrib tbl|Neoproterozoic|Mesoproterozoic|South Nicholson Basin.||South Nicholson Group|||Hematitic and limonitic sandstone; siderite and chamosite-rich at depth; siltstone and shale interbeds.|
18529|Train Range Ironstone Member|67539|6|Mentioned|p15, Fig.8|||||Of the Mullera Formation.||||
18529|Train Range Ironstone Member|68020|5|Briefly described|p128|||45-180m thick.||?Of Mullera Formation?|||Lenticular ironstone beds and thinly bedded alternating dark grey shales, siltstones and sandstones.|
18529|Train Range Ironstone Member|68146|6|Mentioned|p196|||||Mullera Formation||||02-NOV-18
18529|Train Range Ironstone Member|69434|5|Briefly described|p19:7|Mesoproterozoic|Mesoproterozoic|Carter and Zimmerman (1960), Harms (1965), Slater and Mond (1980). Explored for iron in Qld: fourteen separate iron ore deposits identified.||Mullera Formation.|||Ironstone beds.|12-JUL-16
18529|Train Range Ironstone Member|69591|5|Briefly described|p52|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin (Qld and NT).||Mullera Formation.|||Contains numerous low-grade to high-grade hematite/goethite/siderite deposits of the oolitic type.|
18529|Train Range Ironstone Member|70897|5|Briefly described|p39, Fig.1.7.6|Mesoproterozoic|Mesoproterozoic|Appears in Fig.1.7.6 as Train Range Fe. Described as member of South Nicholson Group p39. Diagram suggests is a member of the Mullera Formation.||Mullera Formation.||Identical with Sherwin Ironstone Member (Roper Group).|Shallow-water oolitic ironstone.|28-NOV-17
18529|Train Range Ironstone Member|71369|4|Described|p1, p5-6, p33, p37-42, p44, p50|Mesoproterozoic|Mesoproterozoic|Initially named and defined as Train Range iron-bearing member by Carter and Zimmerman (1960) [actually their name was the more formal Train Range Iron-bearing Member]. Later the Train Range Ironstone Formation of Harms (1965). Modified to Train Range Ironstone Member by Slater and Mond (1980) and Sweet and Hutton (1982), who saw it as better included within the Mullera Formation than as a separate Formation. South Nicholson Basin. 45-180m thick. Progradational deposits.||Mullera Formation.|||Comprises a series of ferruginous sandstone and ironstone beds which are laterally gradational. Ironstones are largely oolitic at depth.|20-FEB-18
18529|Train Range Ironstone Member|72297|5|Briefly described|p712|||Constance Range area west of Lawn Hill; South Nicholson Basin.||South Nicholson Group.|||Up to ten lenticular beds of oolitic iron formation, interbedded with shale, siltstone and sandstone.|
18529|Train Range Ironstone Member|72408|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet.||Unit of Mullera Formation.|||Hematitic and limonitic sandstone; hematitic, sideritic and chamosite-rich oolites at depth; siltstone and shale interbeds.|
18529|Train Range Ironstone Member|72414|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.||Unit of Mullera Formation.|||Hematitic and limonitic sandstone; hematitic, sideritic and chamosite-rich oolites at depth; siltstone and shale interbeds.|
18529|Train Range Ironstone Member|72415|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.||Unit of Mullera Formation.|||Hematitic and limonitic sandstone; hematitic, sideritic and chamosite-rich oolites at depth; siltstone and shale interbeds.|
18529|Train Range Ironstone Member|72416|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet Geological Compilation Series.||Unit of Mullera Formation.|||Hematitic and limonitic sandstone; hematitic, sideritic and chamosite-rich oolites at depth; siltstone and shale interbeds.|
18529|Train Range Ironstone Member|72418|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet.||Unit of Mullera Formation.|||Hematitic and limonitic sandstone; hematitic, sideritic and chamosite-rich oolites at depth; siltstone and shale interbeds|
18529|Train Range Ironstone Member|72421|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.||Unit of Mullera Formation.|||Hematitic and limonitic sandstone; hematitic, sideritic and chamosite-rich oolites at depth; siltstone and shale interbeds|
18529|Train Range Ironstone Member|72422|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.||Unit of Mullera Formation.|||Hematitic and limonitic sandstone; hematitic, sideritic and chamosite-rich oolites at depth; siltstone and shale interbeds|
18529|Train Range Ironstone Member|72423|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet Geological Compilation Series.||Unit of Mullera Formation.|||Hematitic and limonitic sandstone; hematitic, sideritic and chamosite-rich oolites at depth; siltstone and shale interbeds|
18529|Train Range Ironstone Member|72912|4|Described|p5 Fig.3, p23, p33 Fig.12.|Mesoproterozoic|Mesoproterozoic|Located in East and Central parts of the South Nicholson Basin. Name shown in full p23, but mostly abbreviated to Train Range Ironstone.||Mullera Formation||||
18529|Train Range Ironstone Member|72919|6|Mentioned|p5|Mesoproterozoic|Mesoproterozoic|||Mullera Formation, Accident Subgroup, South Nicholson Group||||
18576|Treuer Member|23270|5|Briefly described|Table 1, p4||Proterozoic|In the Ngalia Basin. Age: Late Proterozoic.||||||12-DEC-06
18576|Treuer Member|23271|5|Briefly described|Map legend||Proterozoic|In the Ngalia Basin.Age: Late Proterozoic.||||||23-DEC-09
18576|Treuer Member|24064|4|Described|p226|Adelaidean|Adelaidean|Geological Province: Ngalia Basin.||||||
18576|Treuer Member|30258|6|Mentioned|p102|||Member Vaughan Springs Qtz. Min.age 1280m.y. See Table 1, Fig.2.||||||26-SEP-11
18576|Treuer Member|30684|4|Described|p11|||Adelaidian age.Of the Vaughan Springs Quartzite||||||12-DEC-06
18576|Treuer Member|32442|4|Described|Table 1|||Adelaidean||||||
18576|Treuer Member|33103|4|Described|Table 4|||||||||
18576|Treuer Member|33104|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
18576|Treuer Member|33757|3|Fully described|p9|||See also Table 1. Refers Wells et al. (in prep.)||||||
18576|Treuer Member|33758|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
18576|Treuer Member|33759|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
18576|Treuer Member|33760|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
18576|Treuer Member|33761|6|Mentioned|p145|||Adelaidean||||||
18576|Treuer Member|34724|6|Mentioned|p343|||||||||
18576|Treuer Member|37537|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Vaughan Springs Quartzite. White to grey, thin to poorly bedded siltstone, grey chert nodules and evaporites. Geological Province: Ngalia Basin.||||||14-FEB-06
18576|Treuer Member|38157|6|Mentioned|Table VII|||||||||
18576|Treuer Member|43275|5|Briefly described|Map Legend||Neoproterozoic|Of Vaughan Springs Quartzite.||||||
18576|Treuer Member|44158|4|Described|p23 Table.2|Neoproterozoic|Neoproterozoic|Of the Vaughan Springs Quartzite.||||||12-DEC-06
18576|Treuer Member|45140|5|Briefly described|p61|||Ngalia Basin. Crops out 40km E and 5 km SE of Mount Carey. 1825m thick.||Vaughan Springs Quartzite.|||A sequence of shale, siltstone and glauconitic sandstone.|
18576|Treuer Member|45155|2|Defined|p20|Adelaidean|Adelaidean|||||||
18576|Treuer Member|61385|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of the Vaughan Springs Quartzite. Thinly bedded mudstone, shale, quartz sandstone, minor glauconitic sandstone. Geological Province: Ngalia Basin.||||||
18576|Treuer Member|62633|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Ngalia Basin. Of the Vaughan Springs Quartzite. Thin bedded to flaggy fine grained quartz sandstone, minor siltstone.||||||
18576|Treuer Member|65332|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Vaughan Springs Quartzite. Thinly bedded to flaggy fine-grained quartz sandstone, minor siltstone||||||02-FEB-10
18576|Treuer Member|65338|4|Described|pp57-58, 59|||Possible volcaniclastic siltstone in this unit has zircons with U-Pb ages of 1400 Ma and older. Orthoquartzite shows oscillation ripple marks and small-scale probable worm tracks. Has basal conglomerate where Bigrlyi Member is absent.||Unit in Vaughan Springs Quartzite.||Overlies Bigrlyi Member. Is overlain by Eva Springs Member.|Succession of siltstone and fine- to medium-grained, thinly bedded, flaggy sandstone, with a component of micaceous, haematitic and feldspathic grains, with some glauconitic sandstone and possible evaporites (gypsum).|
18576|Treuer Member|69439|4|Described|p24:1-2, 4-6, 15-16|Cryogenian|Cryogenian|Young et al. (1995). Ngalia Basin, Centralian A Superbasin. Supersequence 1. A decollement in evaporite zones of this unit is related to thin-skinned thrusting and folding by the Eclipse Event (late Alice Springs Orogeny) in the Basin. Diverse sedimentary structures listed. Seismic evidence suggests the presence of salt intervals. 50-700m thick, increasing to W. Approximate age from correlation with other Centralian A Superbasin units. Older Rb-Sr, K-Ar and detrital zircon ages are given.|c.900 Ma.|Vaughan Springs Quartzite.||Conformably overlies Bigrlyi Member. Is overlain conformably by Eva Springs Member.|Micaceous mudstone (halite pseudomorphs common), laminated shale, flaggy to thinly bedded quartz sandstone, minor glauconitic sandstone; rare lenses of dolomudstone with spotted ?volcaniclastic sandstone and siltstone, local basal conglomerate/grit.|12-JUL-16
18576|Treuer Member|69508|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Ngalia Basin.||Vaughan Springs Quartzite.|||Thinly-bedded to flaggy, fine-grained quartz sandstone, minor siltstone.|
18576|Treuer Member|69673|6|Mentioned|p105, p107 fig 85|||||Vaughan Springs Quartzite||Overlain by Eva Springs Member, overlies Bigrlyi Member||
18608|Troughton Group|13194|5|Briefly described|p385 Tb. 4-16, p396 fig 4-60|Jurassic|Triassic|Up to 1500m thick.||||Overlies Sahul Group, Kinmore Group (both conformably). Part equivalent to Sahul Group.||
18608|Troughton Group|13222|6|Mentioned|p229 Fig.2.||||||Includes Cape Londonderry Formation.|||
18608|Troughton Group|13354|6|Mentioned|p375 Fig.6.|Middle Jurassic|Early Jurassic|Comprises upper Nome Formation and Plover Formation.||52||||28-OCT-14
18608|Troughton Group|22663|5|Briefly described|AC97 1-4 Fig.4||Jurassic|||||||01-MAR-10
18608|Troughton Group|24569|5|Briefly described|p248 Fig. 3|Jurassic|Triassic|Includes Cape Londonderry, Malita and Plover Formations. Geological Province: Petrel Sub-basin.||||||02-MAR-05
18608|Troughton Group|41459|6|Mentioned|Fig.2|||Reserved as Troughton Formation||||||
18608|Troughton Group|41532|3|Fully described|p304|||||||||
18608|Troughton Group|41731|6|Mentioned|Fig.3|||||||||
18608|Troughton Group|42053|5|Briefly described|Fig.15 P46|||||||||01-MAR-10
18608|Troughton Group|42066|5|Briefly described|Fig.3 P199|||||||||
18608|Troughton Group|42075|5|Briefly described|Fig.4 P245|||||||||
18608|Troughton Group|42442|3|Fully described|p23|||Variation of Troughton Group, WA.||||||
18608|Troughton Group|43661|6|Mentioned|Fig.3|||||||||
18608|Troughton Group|43699|6|Mentioned|p3|Middle Jurassic|Early Jurassic|||||||
18608|Troughton Group|43707|5|Briefly described|Fig.3,p4||Jurassic|||||||
18608|Troughton Group|43739|6|Mentioned|p10|Jurassic|Triassic|||||||
18608|Troughton Group|49637|5|Briefly described|Fig.3|Middle Jurassic|Late Triassic|Includes the Malita and Plover Formations.||||||07-FEB-11
18608|Troughton Group|60634|6|Mentioned|p1168 Fig.3. |Middle Jurassic|Early Jurassic||||Includes Plover Formation.|Overlies Sahul Group. Is overlain by Swan Group.||
18608|Troughton Group|62837|5|Briefly described|Stratigraphic columns|Middle Jurassic|Middle Triassic|Includes Cape Londonderry, Malita and Plover Formations.  Age: ~240-~154Ma. Geological Province:  Petrel Sub-basin (offshore).||||||01-MAR-10
18608|Troughton Group|63062|5|Briefly described|p9 Fig. 9|Middle Jurassic|Early Jurassic|Included in terms of equivalents, and represented in the study area by only its youngest component, the Plover Formation. Geological Province: Arafura and Money Shoal Basins. See also pp32-33 Figs. 29 and 30.||||||07-FEB-11
18608|Troughton Group|67370|6|Mentioned|p313 Fig.2. |Triassic|Triassic|||||Overlies Kinmore Group.||
18608|Troughton Group|68135|5|Briefly described|p51 fig 2a|Middle Jurassic|Early Jurassic|Bonaparte Basin.|||Malita, Plover Formations.|Is overlain by Flamingo Group.||15-SEP-17
18608|Troughton Group|69297|6|Mentioned|p285, p289, p290, p305, p322|Middle Jurassic|Early Jurassic|Arafura Basin.|||Includes the Plover Formation and the Ashmore Volcanics.|Overlies the Sahul Group. Overlain by the Swan Group.||
18608|Troughton Group|69451|6|Mentioned|p35:2 Fig.35.2; 35:3 Fig.35.4;|Jurassic|Jurassic|||||||12-JUL-16
18608|Troughton Group|69452|4|Described|p36:4-5, 8, 15, 19, 21|Middle Jurassic|Middle Triassic|Gunn (1988). An offshore succession extending across much of the Bonaparte Basin. Fluvial braided-stream, continental, deltaic fluvial to coastal.|||Cape Londonderry, Malita, Plover Formations; Ashmore Volcanics.|Unconformably overlies Mount Goodwin Subgroup. Is overlain by Flamingo Group disconformably to unconformably.|Dominantly siliciclastic rocks.|12-JUL-16
18608|Troughton Group|69454|5|Briefly described|p38:4|Rhaetian|Anisian|Petrel Sub-basin, Bonaparte Basin.|||Cape Londonderry, Malita Formations.|Overlies Kinmore Group.||12-JUL-16
18608|Troughton Group|69456|5|Briefly described|p40:1-4, 15 Fig.40.16|Middle Jurassic|Early Jurassic|Gunn (1988); defined in the Bonaparte Basin. The NT and offshore occurrences are consistently referred to as "Troughton Group equivalent".|||Cape Londonderry, Malita and Plover Formations.|||12-JUL-16
18608|Troughton Group|69653|6|Mentioned|p6, 8, 10, 14-15|Middle Jurassic|Early Triassic|Petrel Sub-basin. Deltaic to fluvial sediments; increasing shallow-marine influence in mid-Jurassic.|||Malita, Plover, Cape Londonderry Formations.|Overlies Kinmore Group. Is overlain unconformably by Flamingo Group.|Local redbeds.|
18608|Troughton Group|69673|5|Briefly described|p153 fig 125, p166 fig 136, p173||||||Includes Cape Londonderry Formation, Malita Formation, Plover Formation|Unconformably overlies Mount Goodwin Subgroup, disconformably overlain by Flamingo Group||
18608|Troughton Group|70061|5|Briefly described|Petrel Sub-basin; Fig.2|Bathonian|Anisian|See also Regional geology: Figs.6-7. Sahul: Fig.2. Vulcan: Fig.2.|||Cape Londonderrry, Malita and Plover Formations; Ashmore Volcanics.|Overlies Kinmore Group. Is overlain by Flamingo Group.||12-JUL-16
18608|Troughton Group|70064|5|Briefly described|Regional Fig. 6. Central: Fig.2|Bathonian|Hettangian|See also Northern: Fig.2. Yampi: Fig.2. Browse Basin.|||Plover Formation; Ashmore Volcanics.|Overlies Sahul Group. Is overlain by Swan Group.||12-JUL-16
18608|Troughton Group|70098|5|Briefly described|p3, p18 Fig.4, p19 Fig.5|Middle Jurassic|Early Jurassic|Money Shoal Basin. Shown as Flamingo Group-Troughton Group, Early Cretaceous - Jurassic.|||Plover Formation|Overlies Kulshill Group (and equivalent?).||
18718|Turnstone Formation|5952|5|Briefly described|p214 Fig. 4, p215 Fig. 5, p223|Late Cretaceous|Late Creatceous|Mory (1988). In figure, Fm = Formation. Geological Province: Bonaparte Basin. Calcareous claystones and calciluties.  Also on p228 Fig. 18.||||||01-MAR-10
18718|Turnstone Formation|13194|4|Described|p384 Tb. 4-16, p396 fig 4-60|Maastrichtian|Campanian|150-200m thick, open marine shelf deposits, fossiliferous. Only in east Ashmore Platform. Type section: Turnstone 1 well (925-1120m).||Bathurst Island Group||Overlies Vee Formation (conformably but diachronous). Grades laterally into Puffin Formation. Equivalent to upper Wangarlu Formation.|Calcareous claystone; minor marl.|
18718|Turnstone Formation|24218|5|Briefly described|p853 Fig. 5|Late Cretaceous|Late Cretaceous|Geological Province: Bonaparte Basin.||||||
18718|Turnstone Formation|41532|2|Defined|p308|Late Cretaceous||||||||
18718|Turnstone Formation|42442|2|Defined|p29|Maastrichtian|Campanian|Variation of Turnstone formation, WA. Age Late Cretaceous (Campanian to Maastrichtian).||||||01-SEP-14
18718|Turnstone Formation|43699|6|Mentioned|Fig.6,p10||Late Cretaceous|||||||
18718|Turnstone Formation|43739|6|Mentioned|Fig.5,p38||Late Cretaceous|||||||
18718|Turnstone Formation|49637|5|Briefly described|Fig.3|Late Cretaceous|Late Cretaceous|Of the Bathurst Island Group. Geological Province: Vulcan Sub-basin.||||||07-FEB-11
18718|Turnstone Formation|60385|5|Briefly described|p270, p272 Fig 3|Maastrichtian|Campanian|Browse Basin.|||Includes Prudhoe Member, Puffin Member, Puffin Sandstone Member, Borde Marl Member||Mudstone, with sandstone and hemipelagic marl members.|
18718|Turnstone Formation|61548|6|Mentioned|p480 Fig.3|Maastrichtian|Campanian|Northern Bonaparte Basin.||||||
18718|Turnstone Formation|62837|5|Briefly described|Stratigraphic columns|Paleocene|Late Cretaceous|Age: ~77-~65Ma. Geological Province: Northern Bonaparte Basin.||||||01-MAR-10
18718|Turnstone Formation|64695|5|Briefly described|p262 Fig.8 |Late Cretaceous|Late Cretaceous|Northern Bonaparte Basin.||||Overlies Fenelon Formation. Is overlain by Johnson Formation.||
18718|Turnstone Formation|68223|6|Mentioned|p178 Fig.3|Maastrichtian|Campanian|||||||
18718|Turnstone Formation|69452|6|Mentioned|p36:15|||Bonaparte Basin.||Bathurst Island Group.||||12-JUL-16
18718|Turnstone Formation|70061|5|Briefly described|Regional geology; Figs.6-7|Maastrichtian|Campanian|See also Sahul: Fig.2, p2. Vulcan: Fig.2.||Bathurst Island Group.||Overlies Fenelon Formation. Is overlain by Johnson Formation.||12-JUL-16
18798|Ulunourwi Formation|22538|6|Mentioned|Fig3 P708|||||||||
18798|Ulunourwi Formation|22600|4|Described|Map legend|Statherian|Statherian|||||||
18798|Ulunourwi Formation|24048|6|Mentioned|p62|||Of the Habgood Group.||||||13-DEC-06
18798|Ulunourwi Formation|24049|5|Briefly described|Map Legend|Statherian|Statherian|Of Habgood Group. Mudstone: red, purple and green, dolomitic in part, laminated, dessication cracks, evaporite nodules; sandstone: fine to medium-grained; silty dololutite and dolostone, rarely stromatolitic. Geol. Prov: McArthur Basin.||||||13-OCT-05
18798|Ulunourwi Formation|32660|5|Briefly described|Table 4|||||||||
18798|Ulunourwi Formation|42597|5|Briefly described|Map Legend|Carpentarian||||||||
18798|Ulunourwi Formation|43010|2|Defined|p135||Paleoproterozoic|Of the Habgood Group. Of Statherian age.||||||07-NOV-08
18798|Ulunourwi Formation|44112|4|Described|p30,59-61|||||||||
18798|Ulunourwi Formation|61403|5|Briefly described|Map Legend|Statherian|Statherian|Of Habgood Group. Mudstone: red, purple and green, dolomitic in part, laminated, dessication cracks, evaporite nodules; sandstone: fine to medium-grai ned; silty dololutite and dolostone, rarely stromatolitic. Geol. Prov: McArthur Basin.||||||
18798|Ulunourwi Formation|64817|6|Mentioned|p353 Fig.4 |||||Of the Habgood Group.||||
18798|Ulunourwi Formation|69430|5|Briefly described|p15:3, 20|||Walker Fault Zone, northern McArthur Basin. Very shallow, periodically emergent sediments with evidence of deepening to subtidal, storm-dominated deposition near the top.||Habgood Group.||Overlies Darwarunga Sandstone possibly conformably. Is overlain disconformably by Gwakura Formation.|Thick succession of mudstone, lesser sandstone and carbonate rocks. Halite pseudomorphs in fine-grained sandstone interbeds. Cauliflower chert nodules after sulfate evaporites, and ovoid nodules of quartz, carbonate, chlorite and barite are common.|12-JUL-16
18798|Ulunourwi Formation|69673|6|Mentioned|p16 fig 13|||Walker Fault Zone||Habgood Group||Overlain by Gwakura Formation, overlies Darwarunga Sandstone||
18798|Ulunourwi Formation|71374|6|Mentioned|p15|||||Habgood Group. ||Overlies the Darwarunga Sandstone.||
18798|Ulunourwi Formation|72373|5|Briefly described|p15,18|Paleoproterozoic|Paleoproterozoic|Of northern McArthur Basin. Associated with northern Walker Fault Zone.||Unit of Habgood Group.||||
18802|Uluru Clay|42359|4|Described|p523|||See Chen 1989.  At least 5Ma old.||||||13-DEC-06
18802|Uluru Clay|42389|5|Briefly described|p59|||||||||
18802|Uluru Clay|42867|4|Described|p4|||||||||
18802|Uluru Clay|61155|5|Briefly described|p16|Pleistocene|Early Pliocene|Underlies the Winmatti beds. Age: >5-~1Ma. Thickness: 60m. Geological Province: East Amadeus Basin.||||||
18802|Uluru Clay|61306|5|Briefly described|p60|Pliocene|Pliocene|Thick sequence of uniform clays in Lake Amadeus.||||||06-SEP-10
18802|Uluru Clay|69458|5|Briefly described|p42:24|||Lake Amadeus. Up to 60m thick. Estimated age greater than 5 Ma. Deposited under shallow-water lacustrine conditions with frequent dry periods.||||Is overlain by Winmatti beds.|Uniform clays.|12-JUL-16
18813|Umbolooga Subgroup|22538|6|Mentioned|P717|||||||||
18813|Umbolooga Subgroup|22662|6|Mentioned|22|Proterozoic|Proterozoic|Geological province: McArthur Basin.||||||13-DEC-06
18813|Umbolooga Subgroup|22664|6|Mentioned|34|Paleoproterozoic|Paleoproterozoic|Of the McArthur Group.  In the McArthur Basin.||||||07-NOV-08
18813|Umbolooga Subgroup|22853|5|Briefly described|14|Proterozoic|Proterozoic|Of the McArthur Group. Overlain by Batten Subgroup.||||||13-DEC-06
18813|Umbolooga Subgroup|23387|6|Mentioned|p18 fig.19|||Of McArthur Group.||||||
18813|Umbolooga Subgroup|23398|5|Briefly described|p443|||Of McArthur Group||||||
18813|Umbolooga Subgroup|23776|5|Briefly described|p705 Fig 2|||Of McArthur Group.||||||
18813|Umbolooga Subgroup|23902|4|Described|p1568 Fig.2|||Of the McArthur Group. Overlain by the Batten Subgroup. Geological Province: McArthur Basin||||||
18813|Umbolooga Subgroup|23910|5|Briefly described|p291|Paleoproterozoic|Paleoproterozoic|Of McArthur Group.  Geological Province: McArthur Basin.||||||07-NOV-08
18813|Umbolooga Subgroup|23937|6|Mentioned|p9|||Upper parts correlated with the Vizard Group.  See also p95 Appendix 1.||||||18-APR-05
18813|Umbolooga Subgroup|23963|5|Briefly described|p1239 Fig.2|||Geological Province: McArthur Basin. Of the McArthur Group.||||||
18813|Umbolooga Subgroup|24048|6|Mentioned|p55|||||||||
18813|Umbolooga Subgroup|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Of McArthur Group. Geological Province: Southern McArthur Basin.||||||
18813|Umbolooga Subgroup|30272|6|Mentioned|p5|||Stratigraphic table||||||
18813|Umbolooga Subgroup|30344|5|Briefly described|p29|||Part of McArthur Group||||||
18813|Umbolooga Subgroup|32479|6|Mentioned|p1394|||||||||
18813|Umbolooga Subgroup|35261|6|Mentioned|Fig.2|||||||||
18813|Umbolooga Subgroup|37462|4|Described|Table4.IV|||||||||
18813|Umbolooga Subgroup|37568|5|Briefly described|p79|||See also Fig.5 and p84.||||||13-DEC-06
18813|Umbolooga Subgroup|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
18813|Umbolooga Subgroup|40691|6|Mentioned|Fig.4|||||||||
18813|Umbolooga Subgroup|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
18813|Umbolooga Subgroup|41268|5|Briefly described|Fig.3|||||||||
18813|Umbolooga Subgroup|41277|6|Mentioned|Fig.2|||||||||
18813|Umbolooga Subgroup|41406|6|Mentioned|Map legend|Mesoproterozoic||||||||
18813|Umbolooga Subgroup|42385|4|Described|p14|||See also Table 4 p16 and 17.||||||13-DEC-06
18813|Umbolooga Subgroup|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
18813|Umbolooga Subgroup|42638|5|Briefly described|Map legend|Mesoproterozoic||Includes: Reward Dolomite; Barney Creek Formation; Teena Dolomite (and Coxco Dolomite Member); Mitchell Yard Dolomite and Mara Dolomite Members (Emmerugga Dolomite); Myrtle Shale; Leila Sandstone; Tooganinie Formation; Tatoola Sandstone; Amelia Dolomite; Mallapunyah Formation; and, Masterton Sandstone. Age: Middle Proterozoic.||Of McArthur Group.|11 units including 3 members. See Comments field for unit names.|Underlies Batten Subgroup (McArthur Group).||24-OCT-11
18813|Umbolooga Subgroup|42639|4|Described|p18, Table 5 p20,21|||||||||
18813|Umbolooga Subgroup|42739|5|Briefly described|map legend|Statherian|Statherian|Of the McArthur Group. Cyclic dolostone, mudstone, sandstone, evaporite casts, tuffite.||||||19-OCT-05
18813|Umbolooga Subgroup|42753|6|Mentioned|p2|||||||||
18813|Umbolooga Subgroup|42812|4|Described|p29, Table 4|||Of the McArthur Group.||||||13-DEC-06
18813|Umbolooga Subgroup|42935|6|Mentioned|p528|||||||||
18813|Umbolooga Subgroup|43010|6|Mentioned|p128|||||||||
18813|Umbolooga Subgroup|43036|4|Described|p39|||Of the McArthur Group.||||||13-DEC-06
18813|Umbolooga Subgroup|43595|4|Described|p438|||||||||
18813|Umbolooga Subgroup|44112|6|Mentioned|p55|||||||||
18813|Umbolooga Subgroup|45162|4|Described|p45|Proterozoic|Proterozoic|||||||
18813|Umbolooga Subgroup|46915|6|Mentioned|Fig.1|||Stratigraphic section through McArthur Group.||||||
18813|Umbolooga Subgroup|46968|6|Mentioned|Fig.2|||||||||
18813|Umbolooga Subgroup|60483|5|Briefly described|p7 Fig. 5, p8|||Of the McArthur Group. Unconformably overlain by Batten Subgroup. Geological Province: McArthur Basin.||||||05-OCT-07
18813|Umbolooga Subgroup|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of McArthur Group. Includes eleven units.||||||03-JUN-09
18813|Umbolooga Subgroup|64815|5|Briefly described|p3, p5 Fig.3, p8 Tb.1, p11, p15 Fig.9|||See also p16-18 Figs.10-12, p17, p19. Contains a number of internal disconformities.||Unit in McArthur Group.|Includes Mallapunyah, Tooganinie, Barney Creek Formations; Amelia, Emmerugga, Teena, Reward Dolostones; Tatoola, Leila Sandstones; Myrtle Shale.||Fine-grained dolostone is most prevalent; lesser sandstone, mainly in lower portion.|
18813|Umbolooga Subgroup|64817|6|Mentioned|p353 Fig.4 |||||Of the McArthur Group. |Includes the Barney Creek, Tooganinie and Mallapunyah Formations; Reward, Teena, Emmerugga and Amelia Dolomites; Leila, Tatoola and Masterton Sandstones; Myrtle Shale.|||
18813|Umbolooga Subgroup|65228|4|Described|p32, Fig.02.|||Upper part constitutes lower part of River Supersequence.||Unit in McArthur Group.|Includes Masterton, Tatoola, Leila Sandstones; Mallapunyah, Tooganinie, Barney Creek Formations; Amelia, Emmerugga, Teena Dolomites; Myrtle Shale.|Is overlain by Batten Subgroup.||
18813|Umbolooga Subgroup|67144|5|Briefly described|Map legend.|Statherian|Statherian|||Unit in McArthur Group.|Includes Masterton, Tatoola and Leila Sandstones; Mallapunyah, Tooganinie and Barney Creek Formations; Amelia, Emmerugga, Teena and Reward Dolostones; Myrtle Shale.|||
18813|Umbolooga Subgroup|67323|5|Briefly described|Eastern Australia Time-Space Plot; p35|Paleoproterozoic|Paleoproterozoic|McArthur Basin.|1640 +/- 3 Ma.||Reward Dolomite, Teena Dolostone, Masterton Sandstone.||Dolostone, mudstone, sandstone, evaporite casts, tuffite.|
18813|Umbolooga Subgroup|67352|4|Described|p12, p13-14 Tb.2, p51|Statherian|Statherian|Isa Superbasin.|c.1635 Ma (minimum).|McArthur Group|Reward, Teena, Emmerugga, Amelia Dolostones; Myrtle Shale; Leila, Tatoola, Masterton Sandstones; Tooganinie, Barney Creek, Mallapunyah Formations.|Is overlain by Batten Subgroup.|Carbonates.|
18813|Umbolooga Subgroup|69430|4|Described|p15:3, 14, 16-19, 22, 34, 39|Statherian|Statherian|Southern McArthur Basin. Contains minor discordant Pb-Zn-Ag +/-Cu Mississippi Valley-style deposits.||McArthur Group.|Masterton, Tatoola, Leila Sandstones; Mallapunyah, Tooganinie, Barney Creek Formations; Amelia, Emmerugga, Teena, Reward Dolostones; Myrtle Shale.|Unconformably overlies Tawallah Group. Is overlain unconformably by Batten Subgroup.|Dolostone, sandstone, siltstone and shale.|12-JUL-16
18813|Umbolooga Subgroup|69431|6|Mentioned|p16:25|||An equivalent succession was recognised in the northern Tomkinson Province, hosting low-grade base metal mineralisation.||McArthur Group.||||12-JUL-16
18813|Umbolooga Subgroup|69673|6|Mentioned|p16 fig 13|||Batten Fault Zone. Upper parts of this subgroup contain units with particularly good petroleum potential.||McArthur Group|Includes Masterton Sandstone, Mallapunyah Formation, Amelia Dolostone, Tatoola Sandstone, Tooganinie Formation, Emmerugga Dolostone,Teena Dolostone, Barney Creek Formation, Reward Dolostone|Unconformably overlain by Batten Subgroup||
18813|Umbolooga Subgroup|71374|6|Mentioned|p9|||||McArthur Group||Overlain by the Yalco Formation.||
18813|Umbolooga Subgroup|71606|5|Briefly described|p137-138|Statherian|Statherian|Batten Trough, McArthur Basin.||Unit of McArthur Group.|Includes Barney Creek Formation.|Lower unit of McArthur Group. Overlain by Batten Subgroup. Underlain unconformably by Tawallah Group.||
18813|Umbolooga Subgroup|72248|5|Briefly described|p147-148|||Of McArthur Basin.||Unit of McArthur Group.|Includes Reward Dlt, Barney Creek Fm, Teena Dlt, Emmerugga Dlt, Myrtle Shale, Leila Sst, Tooganinie Fm, Tatoola Sst, Amelia Dlt, Mallapunyah Fm and Masterton Sst.|Overlain conformably to unconformably by Batten Subgroup.||13-SEP-19
18813|Umbolooga Subgroup|72373|5|Briefly described|iii,5-6,9,11,39|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin.||Unit of McArthur Group.|Includes Tatoola Sandstone, Tooganinie Formation, Leila Sandstone, Mallapunyah Formation and Emmerugga Dolostone.|||
18813|Umbolooga Subgroup|72523|6|Mentioned|p2 Fig.2.|||||Mc Arthur Group||Underlies Batten Subgroup.||
18813|Umbolooga 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|Tooganinie Formation, Myrtle Shale, Leila Sandstone, Tatoola Sandstone, Amelia Dolostone, Mallapunyah Formation and Masterton Sandstone.|Shown as unconformably overlying Tawallah Group and underlying Batten Subgroup.||
18813|Umbolooga Subgroup|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Batten Fault Zone of the Southern McArthur Basin.||McArthur Group|Tooganinie Formation, Myrle Shale, Leila Sandstone, Tatoola Sandstone, Amelia Dolostone, Mallapunyah Formation and Masterton Sandstone.|Unconformably overlies Tawallah Group and underlies Batten Subgroup.|Includes sandstone, dolostone and shale.|
18813|Umbolooga Subgroup|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin, Isa Superbasin.||McArthur Group|Tooganinie, Mallapunyah formations; Myrtle Shale; Leila, Tatoola, Masterton sandstones; Amelia Dolostone.|Overlain by Emmerugga Dolostone  including Mara Dolostone Member.||
18813|Umbolooga Subgroup|73412|5|Briefly described|p4, 8, 18|||Southern McArthur Basin.||McArthur Group.|Masterton, Tatoola, Leila Sandstones; Mallapunyah, Tooganinie, Barney Creek Formations; Amelia, Emmerugga, Teena, Reward Dolostones; Myrtle Shale.|Unconformably overlies Tawallah Group. Is overlain by Batten Subgroup.||
18815|Umbrawarra Leucogranite|14019|6|Mentioned|p4|Orosirian|Orosirian|Age: 1825+/-7Ma. Geological Province: Pine Creek Geosyncline.||||||
18815|Umbrawarra Leucogranite|24197|5|Briefly described|p106 Tb. 15.1|Paleoproterozoic|Paleoproterozoic|Of the Cullen Supersuite. Age: ~1825Ma. Geological Province: Pine Creek Inlier.||||||07-FEB-11
18815|Umbrawarra Leucogranite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
18815|Umbrawarra Leucogranite|40168|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Cullen Batholith. Light grey coarse porphyritic biotite leucogranite.||||||07-NOV-08
18815|Umbrawarra Leucogranite|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
18815|Umbrawarra Leucogranite|41586|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
18815|Umbrawarra Leucogranite|42756|6|Mentioned|Fig.5 P6|||||||||
18815|Umbrawarra Leucogranite|43832|4|Described|Table8p38;46,55,62||Paleoproterozoic|Age 1825+-7 Ma; less accurate 1805+-12 Ma (p53)||||||07-NOV-08
18815|Umbrawarra Leucogranite|50586|5|Briefly described|p1.1, 4.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Of the Cullen Supersuite. Age: 1825-1805 +/- 12Ma (SHRIMP, U-Pb).||||||02-MAR-18
18815|Umbrawarra Leucogranite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Of Cullen Supersuite. Age 1825Ma SHRIMP U/Pb. I-type. Light grey coarse biotite monzonite leucogranite. Intrudes Burrell Creek Formation.||||||07-JAN-09
18815|Umbrawarra Leucogranite|67564|6|Mentioned|p33 Fig.19.|||Pluton within Cullen Batholith, Pine Creek Orogen.||||||
18815|Umbrawarra Leucogranite|69420|5|Briefly described|p5:17-19|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Leucogranite-dominated plutons; mineralogy and petrology/geochemistry summarised. A SHRIMP U-Pb zircon age of 1825 +/- 7 Ma is also given.|1805 +/- 12 Ma conventional U-Pb zircon (TIMS).|Tennysons Suite.|||Coarse-grained porphyritic leucogranite. I-type.|12-JUL-16
18815|Umbrawarra Leucogranite|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.|1825 +/- 9 Ma.|Tennysons Suite.|||Light grey to pink, medium- to coarse-grained, porphyritic to equigranular biotite-muscovite monzonite leucogranite.|
18815|Umbrawarra Leucogranite|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|1825+/-7 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
18819|Unbunmaroo Member|22954|4|Described|Fig1p6,17-9,21|Datsonian|Payntonian|||||||
18819|Unbunmaroo Member|36217|6|Mentioned|p206|||Published by Druce 1978. Definition approved by Qld SNC.||||||
18819|Unbunmaroo Member|37572|5|Briefly described|p161|||||||||
18819|Unbunmaroo Member|38532|4|Described|p242|||||||||
18819|Unbunmaroo Member|40136|5|Briefly described|p41|||||||||
18819|Unbunmaroo Member|40810|5|Briefly described|p14|||||||||
18819|Unbunmaroo Member|42354|6|Mentioned|p11|||Of Ninmaroo Formation.||||||13-DEC-06
18819|Unbunmaroo Member|46897|6|Mentioned|Fig.2|||||||||
18819|Unbunmaroo Member|46958|6|Mentioned|p195|||||||||
18819|Unbunmaroo Member|50244|6|Mentioned|p89 Fig. 1, p100 Fig. 7|Ordovician|Cambrian|Of Ninmaroo Formation. Geological Province: Georgina Basin.||||||22-APR-09
18819|Unbunmaroo Member|62793|6|Mentioned|p272|Late Cambrian|Late Cambrian|Contains latest Cambrian index species Cordylodus proavus. In Black Mountain section, C. proavus Assemblage Zone (lower Datsonian) is now defined as occurring between 130 m  and 230 m above the base of the Unbunmaroo Member.||Unit of Ninmaroo Formation.||||21-MAR-12
18819|Unbunmaroo Member|64068|4|Described|p73-74|Late Cambrian|Late Cambrian|Thickness 165 m in type section. Diverse fauna.||Base of Ninmaroo Formation.||Conformably to disconformably overlies Chatsworth Limestone. Is overlain by Jiggamore Member.|Peloid, ooid, peloid-intraclast and quartzic peloid grainstone, stromatolite boundstone, calcimudstone with evaporites.|05-APR-12
18819|Unbunmaroo Member|67323|5|Briefly described|GIS attrib tbl|Early Ordovician|Late Cambrian|Georgina Basin.||Cockroach Group|||Medium- to thick-bedded limestone (intraclast and peloid grainstone, mudstone, stromatolitic boundstone), dolomite, calcareous siltstone.|
18819|Unbunmaroo Member|71284|5|Briefly described|p489|||Black Mountain area, western Queensland. Contains the conodont Cordylodus proavus, which had been used to mark the base of the Ordovician in Australia.||Ninmaroo Formation.||||
18837|Undoolya Siltstone Member|23361|5|Briefly described|17|Proterozoic|Proterozoic|of the Heavitree Quartzite.||||||13-DEC-06
18837|Undoolya Siltstone Member|35102|6|Mentioned|p27|||||||||
18837|Undoolya Siltstone Member|43503|6|Mentioned|29|||||||||
18837|Undoolya Siltstone Member|48992|2|Defined|p25|Neoproterozoic|Neoproterozoic|||||||
18837|Undoolya Siltstone Member|50246|5|Briefly described|p8|Neoproterozoic|Neoproterozoic|Of the Heavitree Quartzite.||||||07-FEB-11
18837|Undoolya Siltstone Member|61309|5|Briefly described|p17|||Of the Heavitree Quartzite.  Not consistently present in the parent unit. Geological Province: Amadeus Basin.||||||06-FEB-08
18837|Undoolya Siltstone Member|62595|5|Briefly described|p8. |||||Unit in Heavitree Quartzite.|||Buff to red mudstone/siltstone with minor fine-grained sandstone (channel-fill) lenses.|
18837|Undoolya Siltstone Member|73086|3|Fully described|p7-9, p144|||Amadeus Basin. Of Stewart et al (1980). Type area: Heavitree Gap (16 m thick). Has a more restricted and localised distribution than other members of the Heavitree Formation. Widespread to the east of Alice Springs but missing to the west. Probably deposited as infill in locally developed topographic lows on weathered basement. [Also written as Undoolya Member on p7; see Wells, 1967].||Heavitree Formation||Nonconformably underlain by Sadadeen Gniess. Conformably overlain by Temple Bar Sandstone Member.||
19017|Utnalanama Granulite|23363|5|Briefly described|351 Tab.2|Statherian|Statherian|Age: 1778+/-5Ma.||||||13-DEC-06
19017|Utnalanama Granulite|23844|6|Mentioned|p29|||||||||
19017|Utnalanama Granulite|39470|6|Mentioned|p42|||||||||
19017|Utnalanama Granulite|43503|6|Mentioned|15|||||||||
19017|Utnalanama Granulite|66860|6|Mentioned|p8|||May be an intrusive unit (one of several in the SMC). Age is for a metamorphosed diorite and is dubious.|1778 +/- 5 Ma (Black and Shaw, 1995).|Strangways Metamorphic Complex||Intruded by Johannsen Metagabbro. Is overlain by Erontonga Metamorphics.|A large, relatively homogeneous mass of felsic granulite.|
19017|Utnalanama Granulite|67181|5|Briefly described|p631|Statherian|Statherian|Of the Calcalkaline-trondhjemitic Group (geochemical grouping) Arunta Region, North Australian Craton.|1763 +/- 2 Ma (Black and Shaw 1992)|||||08-MAR-13
19017|Utnalanama Granulite|69427|4|Described|p12:9-10, 24, 31, 41|Statherian|Statherian|Shaw et al. (1979). Strangways Range region, Aileron Province. Previously thought to unconformably underlie Erontonga Metamorphics. Formerly interpreted as supracrustal, now considered to be felsic intrusions (metadiorite). SHRIMP U-Pb age.|1778 +/- 5 Ma (Black and Shaw, 1995).|Strangways Metamorphic Complex.||Intrudes Erontonga Metamorphics. Is intruded by Gumtree Granite, Harry Anorthositic Gabbro and Johannsen Metagabbro.|Relatively homogeneous felsic granulite, comprising orthopyroxene-bearing meta-tonalite and two-pyroxene meta-diorite, interlayered with lesser cordierite granulite.|12-JUL-16
19017|Utnalanama Granulite|69925|6|Mentioned|p38-39|||Arunta Inlier.|1763 +2/-1 Ma (Black and Shaw, 1992).||||Tonalitic.|
19017|Utnalanama Granulite|71839|5|Briefly described|p10|||Outcrops in ALICE SPRINGS.||Strangways Metamorphic Complex||Intruded by the Gumtree Granite.||
19019|Utopia Quartzite|9394|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block (Division 3). Metaquartzite with minor muscovite.||||||
19019|Utopia Quartzite|23733|5|Briefly described|p34 Fig.20|||||||||
19019|Utopia Quartzite|24047|5|Briefly described|p7 Fig. 6|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Province.||||||07-NOV-08
19019|Utopia Quartzite|33102|5|Briefly described|p440|||||||||
19019|Utopia Quartzite|33103|4|Described|Table 1|||Mention p14.||||||13-DEC-06
19019|Utopia Quartzite|33104|6|Mentioned|Map legend|Precambrian|Precambrian|||||||
19019|Utopia Quartzite|39887|6|Mentioned|Fig.5|||||||||
19019|Utopia Quartzite|40538|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Block.||||||07-NOV-08
19019|Utopia Quartzite|40906|4|Described|p12|||||||||
19019|Utopia Quartzite|43568|6|Mentioned|Fig.4,p506|||||||||
19019|Utopia Quartzite|46868|6|Mentioned|p77|||||||||
19019|Utopia Quartzite|48992|6|Mentioned|p63|||||||||
19019|Utopia Quartzite|48997|6|Mentioned|Fig.2|||||||||
19019|Utopia Quartzite|61208|5|Briefly described|p207 Fig. 1|Late Neoproterozoic|Paleoproterozoic|Unconformably overlain by Grant Bluff Formation. Geological Province: eastern Arunta Inlier.||||||07-NOV-08
19019|Utopia Quartzite|61388|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Purple, brown and white quartzite, meta-sandstone, ironstone. Geological Province: Arunta Region.||||||07-NOV-08
19019|Utopia Quartzite|64068|5|Briefly described|p32, p162|||Bundled in with Mendip Metamorphics and Ledan Schist as the 1770-1740 Ma Ledan package. Part of  basement in Mount Skinner area.||||||
19019|Utopia Quartzite|64574|6|Mentioned|p704 Fig. 1|Paleoproterozoic|Paleoproterozoic|||||||
19019|Utopia Quartzite|65338|6|Mentioned|p62.|||||||Is overlain by Boko Formation.||
19019|Utopia Quartzite|65341|4|Described|p2 Fig.2, p4, p7. |Paleoproterozoic|Paleoproterozoic|Considered part of same sedimentary package as Mendip Metamorphics and Ledan Schist. Distinctly low magnetic and radiometric responses.|1765 - 1730 Ma deposition.|||Overlies Ledan Schist. Is unconformably overlain by Boko Formation and Oorabra Arkose.|Deformed, massive to tabular, purple, brown and white clean quartzite; metasandstone; ironstone.|19-JUN-13
19019|Utopia Quartzite|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Arunta Block.|1820 +/- 15 Ma.|||||
19019|Utopia Quartzite|69383|4|Described|p67-73, 81||Paleoproterozoic|Arunta region, Aileron Province.  LA-ICPMS  U-Pb and Hf geochronology analyses.  Max deposition age. This older age contradicts stratigraphic relationships with Ledan Schist.|1820+/-15 Ma|Of Ledan Package.||Overlies Ledan Schist. Contact regionally conformable but with local disconformities and shearing.|Typically silicified and recrystallised pale grey quartzite, with poorly preserved bedding and rare cross?bedding lamination.|
19019|Utopia Quartzite|69427|5|Briefly described|p12:33-34|||Eastern Aileron Province.||||Disconformably overlies Ledan Schist.|Massive to flaggy clean crystalline quartzite; contains highly weathered ironstone layers.|12-JUL-16
19019|Utopia Quartzite|69431|6|Mentioned|p16:1|||Arunta Region. Possible correlative of Hatches Creek Group and, by inference, Tomkinson Creek Group.||||||12-JUL-16
19019|Utopia Quartzite|69443|6|Mentioned|p28:35|||||||||12-JUL-16
19019|Utopia Quartzite|69554|6|Mentioned|p139|||Aileron Province, Arunta Region, Northern Australian Craton. Contains detrital zircons aged c.1920 Ma.||||||
19019|Utopia Quartzite|71592|5|Briefly described|Appendix A.|||Arunta Orogen.|1820+/-15 Ma (MDA: U-Pb zircon LA-ICPMS).||||Quartzite.|
19019|Utopia Quartzite|72516|6|Mentioned|p192|||Aileron Province. Maximum depositional age 1820 +/- 15 Ma (Hollis et al 2010).||||Possible age equivalent to Bonya Metamorphics.||27-MAY-21
19019|Utopia Quartzite|73591|6|Mentioned|p33-34|||||Deep Bore Metamorphics|||Quartzite.|
19021|Utting Calcarenite|5256|5|Briefly described|p143, p148.|Visean|Visean|Bonaparte Basin. Type section is 120m thick, around Utting Gap, NW Carlton Shelf. Age: mid-Visean V2b - V3a (Holkerian). Richly fossiliferous shelf carbonates.||||||
19021|Utting Calcarenite|13194|4|Described|p389 Tb. 4-16, p402 fig 4-66|Visean|Visean|Type Section: Utting Gap 14o58'S 128o36'E. 36-64m thick marine shelf deposits.||||Overlies Milligans Formation (conformably). Overlain by Burvill Formation (conformably).|Sandy limestone, calcareous sandstone; minor sandstone.|
19021|Utting Calcarenite|23820|5|Briefly described|p202 Fig.2|Early Carboniferous|Early Carboniferous|Geological Province: Bonaparte Gulf Basin.||||||
19021|Utting Calcarenite|31519|6|Mentioned|p917|||||||||
19021|Utting Calcarenite|32662|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
19021|Utting Calcarenite|32663|4|Described|Table 2|||L.Carb.||||||
19021|Utting Calcarenite|32664|6|Mentioned|Map legend|Visean|Visean|||||||
19021|Utting Calcarenite|32867|6|Mentioned|p40|||||||||
19021|Utting Calcarenite|32868|6|Mentioned|p220|||||||||
19021|Utting Calcarenite|32870|5|Briefly described|p48|||See alsop53.||||||13-DEC-06
19021|Utting Calcarenite|33621|6|Mentioned|Table 1|||||||||
19021|Utting Calcarenite|34085|6|Mentioned|Cor.chart|||Visean||||||
19021|Utting Calcarenite|34155|6|Mentioned|p93|||Lower Visean. See also pp101,102.||||||13-DEC-06
19021|Utting Calcarenite|36890|3|Fully described|p380|||||||||
19021|Utting Calcarenite|36904|6|Mentioned|p9|||||||||
19021|Utting Calcarenite|40993|6|Mentioned|Fig.1|||||||||
19021|Utting Calcarenite|41839|4|Described|p31|||Formerly "Milligans Beds".||||||23-APR-08
19021|Utting Calcarenite|41864|3|Fully described|p306|||||||||
19021|Utting Calcarenite|41865|5|Briefly described|Map legend|late Visean|early Visean|||||||
19021|Utting Calcarenite|41867|5|Briefly described|Map legend|late Visean|early Visean|||||||
19021|Utting Calcarenite|42442|6|Mentioned|p11|||See also p12.||||||13-DEC-06
19021|Utting Calcarenite|42547|4|Described|p102|||||||||
19021|Utting Calcarenite|42994|6|Mentioned|p13|||||||||
19021|Utting Calcarenite|43236|6|Mentioned|p14|Visean|Tournaisian|In the Bonaparte Basin.||||||13-DEC-06
19021|Utting Calcarenite|44994|6|Mentioned|p14|||||||||
19021|Utting Calcarenite|45038|14|Not recorded|p.111||Early Carboniferous|See also Figures. L.Carb.||||||
19021|Utting Calcarenite|45039|6|Mentioned|p1|||Lower Carboniferous. See also pp6,7,8,14 etc.||||||13-DEC-06
19021|Utting Calcarenite|45040|14|Not recorded|p7||Carboniferous|(?Carboniferous).||||||
19021|Utting Calcarenite|45050|6|Mentioned|p46|||Early Visean. See also p57.||||||13-DEC-06
19021|Utting Calcarenite|45063|6|Mentioned|p8|||See also p20 & 26 and Fig. 3.||||||13-DEC-06
19021|Utting Calcarenite|45097|5|Briefly described|p13|||See p19,21. Refers Bruce (1969). Conodonts. Chart.||||||13-DEC-06
19021|Utting Calcarenite|45169|4|Described|p6|||||||||
19021|Utting Calcarenite|48886|14|Not recorded|Map||Early Carboniferous|Lower Carboniferous.||||||
19021|Utting Calcarenite|60364|4|Described|p189, 194|Visean|Visean|Conformably overlies Milligans Formation. Conformably overlain by Burvill Formation. Thickness: 120m. Open shelf carbonates. Richly fossiliferous including brachiopods, corals and trilobites. Ostracods described. Geological Province: Bonaparte Basin.||||||
19021|Utting Calcarenite|61542|4|Described|p276, p277 Fig. 2, p284|Visean|Visean|Of Weaber Gp. Overlies Yow Creek Fm (formerly mapped as Milligans Fm); parts underlie Kingfisher Shale and Burvill Fm.Geol.prov: Bonapart Basin/Petrel-Sub-basin.Fossiliferous sandy limestone, calcareous sandstone and minor fine-gr.sandstone; conodonts.||||||07-FEB-11
19021|Utting Calcarenite|64580|6|Mentioned|map legend|||Of Weaber Group.||||||15-DEC-08
19021|Utting Calcarenite|64694|6|Mentioned|p234 Fig.2, p238 Tb.1, p253|Visean|Visean|||Unit in Weaber Group.||Overlies Lower Milligans Formation. Is correlated with Upper Milligans Formation.||
19021|Utting Calcarenite|66498|6|Mentioned|p47-48|||Bonaparte Basin, WA.||Weaber Group.|||A highly fossiliferous unit (taxa described).|
19021|Utting Calcarenite|68297|5|Briefly described|p197|Visean|Visean|Bonaparte Basin. Includes shark faunas.||||||22-JAN-13
19021|Utting Calcarenite|69099|5|Briefly described|500k_geologyp08_lut.csv|Pennsylvanian|Mississippian|||Weaber Group||||
19021|Utting Calcarenite|69165|6|Mentioned|500k_geologyp08_lut.csv|Pennsylvanian|Mississippian|||Weaber Group||||
19021|Utting Calcarenite|69452|3|Fully described|p36:9, 11-12, 14-16|Visean|Visean|Veevers and Roberts (1968). Petrel Sub-basin, Bonaparte Basin. Marine deposits. Type area is in Utting Gap (WA). Up to 120m thick. Offshore and onshore (subsurface). Also appears as Utting Conglomerate on 36:14.||Weaber Group.||Unconformably overlies Yow Creek or Milligans Formations. Lateral equivalent of Burvill Formation. Is overlain conformably by Kingfisher Shale.|Fossiliferous sandy limestone (wackestone and packstone), calcareous sandstone, minor fine- to medium-grained sandstone. Richly fossiliferous.|12-JUL-16
19021|Utting Calcarenite|69634|5|Briefly described|500k_geologyp08_lut.csv|Carboniferous|Carboniferous|||Unit of Weaber Group.||||
19021|Utting Calcarenite|69653|6|Mentioned|p10|Carboniferous|Carboniferous|Petrel Sub-basin.||Weaber Group.||Overlies Yow Creek Formation. Is overlain by Kingfisher Shale.||
19021|Utting Calcarenite|69673|6|Mentioned|p168 fig 138, p171|Carboniferous|Carboniferous|||Weaber Group||Overlies Yow Creek Formation, overlain by Kingfisher Shale|Fossiliferous sandy limestone, calcareous sandstone and sandstone.|
19021|Utting Calcarenite|70061|5|Briefly described|Petrel Sub-basin; Fig.3|Visean|Visean|See also Regional geology: Fig.8, p11. Gas reservoir in Bonaparte 2.||Weaber Group.||Overlies Yow Creek Formation. Is overlain by Kingfisher Shale.||12-JUL-16
19021|Utting Calcarenite|73117|6|Mentioned|p15|Visean|Visean|Bonaparte Basin, southern.||Weaber Group||Underlain by Yow Creek Formation. Overlain by Kingfisher Shale. Overlain by and equivalent to Burvill Formation.||
19024|V-Creek Limestone|23031|5|Briefly described|19|||||||||
19024|V-Creek Limestone|23393|5|Briefly described|p23 Fig. 6|Cambrian|Cambrian|Geological Province: Georgina Basin.||||||
19024|V-Creek Limestone|23408|6|Mentioned|p527|||Includes two-toned deeper-water ramp carbonates.||||||15-JUN-09
19024|V-Creek Limestone|30242|6|Mentioned|Fig.2|||||||||
19024|V-Creek Limestone|30479|6|Mentioned|Fig.6|||See also Fig.7. Stratigraphic relationships||||||
19024|V-Creek Limestone|30914|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
19024|V-Creek Limestone|31396|6|Mentioned|Fig.3|||||||||
19024|V-Creek Limestone|33111|4|Described|p44|||||||||
19024|V-Creek Limestone|33482|6|Mentioned|Fig.5|||Middle Cambrian||||||
19024|V-Creek Limestone|34395|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
19024|V-Creek Limestone|35054|6|Mentioned|Table 23|||||||||
19024|V-Creek Limestone|35121|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
19024|V-Creek Limestone|35139|4|Described|Table.2|||||||||
19024|V-Creek Limestone|35553|6|Mentioned|p36|||See also Appendix 2, description of Agnostid localities.||||||
19024|V-Creek Limestone|35556|6|Mentioned|Plate 35|||||||||
19024|V-Creek Limestone|37275|6|Mentioned|p287|||||||||
19024|V-Creek Limestone|37572|4|Described|p158|||||||||
19024|V-Creek Limestone|38444|6|Mentioned|p106|||||||||
19024|V-Creek Limestone|38445|6|Mentioned|p105|||||||||
19024|V-Creek Limestone|38446|6|Mentioned|Table 23|||||||||
19024|V-Creek Limestone|39445|5|Briefly described|Table 4|||See also p62.||||||13-DEC-06
19024|V-Creek Limestone|39690|6|Mentioned|p88|||||||||
19024|V-Creek Limestone|40038|6|Mentioned|p248|||||||||
19024|V-Creek Limestone|40686|5|Briefly described|p407|||||||||
19024|V-Creek Limestone|40856|6|Mentioned|Fig.23.6|||||||||
19024|V-Creek Limestone|41298|6|Mentioned|Map legend|Middle Cambrian||||||||
19024|V-Creek Limestone|41388|6|Mentioned|Fig.2|||||||||
19024|V-Creek Limestone|44091|14|Not recorded|p16,Tb.1,18||Middle Cambrian|||||||
19024|V-Creek Limestone|44205|14|Not recorded|p50-1,61,67,140,155,|||p167,168||||||
19024|V-Creek Limestone|44210|2|Defined|map,Tb.2,p13,14|||||||||
19024|V-Creek Limestone|44211|14|Not recorded|p101,103,107|||Known only in Undilla Basin. See also Lexicon.||||||
19024|V-Creek Limestone|44213|14|Not recorded|Map Legend||Middle Cambrian|||||||
19024|V-Creek Limestone|44275|14|Not recorded|Map Legend|||||||||
19024|V-Creek Limestone|44920|14|Not recorded|Map Legend,||Middle Cambrian|||||||
19024|V-Creek Limestone|45012|14|Not recorded|p338|||||||||
19024|V-Creek Limestone|45054|6|Mentioned|p6|||Fossil locality||||||
19024|V-Creek Limestone|45079|5|Briefly described|p34|||Cambrian age||||||
19024|V-Creek Limestone|45119|6|Mentioned|p3|||||||||
19024|V-Creek Limestone|48633|14|Not recorded|p99|||Ref. to Opik 1961.||||||
19024|V-Creek Limestone|60122|6|Mentioned|p57 Appendix|||Correlated with parts of Arthur Creek Formation. Geological Province: eastern Georgina Basin.||||||
19024|V-Creek Limestone|63450|5|Briefly described|p82|Middle Cambrian|Middle Cambrian|Geological Province: Undilla Sub-basin.||||||07-FEB-11
19024|V-Creek Limestone|64068|6|Mentioned|p62, 193|||Northeastern Georgina Basin. Correlated with  Arthur Creek Formation, Blazan Shale, Roaring Siltstone.. [See also misspelling: V Creek Limestone, p63 etc] Hosts limestone suitable for metallurgical lime, quicklime and cement manufacture, but operations are not viable due to transport difficulties and excessive energy requirements.||||Conformably overlies Inca Formation.||05-APR-12
19024|V-Creek Limestone|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map; p83|Middle Cambrian|Middle Cambrian|Undilla Sub-basin, Georgina Basin.||Narpa Group.||Overlies Currant Bush Limestone. Is overlain by Mail Change Limestone.|Limestone, bituminous limestone, sandy limestone, calcilutite, minor arenite, chert nodules.|
19024|V-Creek 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
19024|V-Creek Limestone|69573|6|Mentioned|p659|||Contains Drumian Stage [Cambrian] fossil sites.||||||
19024|V-Creek Limestone|69591|5|Briefly described|p87|Cambrian|Cambrian|Undilla Sub-basin, Georgina Basin. Mostly appears as V Creek Limestone (p88, p90, p96-97, p98 Fig.2.91). Coeval with Camooweal Dolostone.||Narpa Group.||Overlies Currant Bush Limestone. Is overlain by Mail Change Limestone.||
19024|V-Creek Limestone|72321|6|Mentioned|Fig 2|Drumian|Drumian|Undilla Sub-basin, Georgina Basin. Australian Stages: Floran to Undillan.||of Narpa Group.||||
19024|V-Creek Limestone|72516|6|Mentioned|p92|Cambrian|Cambrian|Eastern Georgina Basin.||||Equivalent to the Arthur Creek Formation.||03-JUN-21
19024|V-Creek Limestone|72967|6|Mentioned|p5|||Georgina Basin.||Napa Group||||
19024|V-Creek Limestone|73418|5|Briefly described|p4 Fig.3|Miaolingian|Miaolingian|Georgina Basin, Undilla Sub-basin.||Narpa Group||Overlies Currant Bush Limestone, underlies Mail Change Limestone|Limestone.|
19044|Van Diemen Sandstone|24047|5|Briefly described|p13, p85|Tertiary|Tertiary|Geological Province: Money Shoal Basin.||||||
19044|Van Diemen Sandstone|31406|4|Described|Table 2|||Mention p4.||||||13-DEC-06
19044|Van Diemen Sandstone|31407|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
19044|Van Diemen Sandstone|31408|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
19044|Van Diemen Sandstone|31409|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
19044|Van Diemen Sandstone|31410|2|Defined|p10|Cenozoic|Cenozoic|||||||19-NOV-08
19044|Van Diemen Sandstone|32472|6|Mentioned|p3|||||||||
19044|Van Diemen Sandstone|41532|6|Mentioned|Fig.15|||||||||
19044|Van Diemen Sandstone|42442|6|Mentioned|Fig.3 P4 P5|||||||||
19044|Van Diemen Sandstone|45121|2|Defined|p51|Tertiary|Tertiary|||||||
19044|Van Diemen Sandstone|45168|6|Mentioned|p12|||||||||
19044|Van Diemen Sandstone|46902|6|Mentioned|p39|||||||||
19044|Van Diemen Sandstone|61155|5|Briefly described|p16|Middle Eocene|Middle Eocene|Max. thickness: 250m. Geological Province: Money Shoal Basin - north and south.||||||
19044|Van Diemen Sandstone|69456|4|Described|p40:2; 40:3 Fig.40.4; 40:4, 6, 8-9, 12|Eocene|Eocene|See also 40:15 Fig.40.16. Hughes and Senior (1974); Hughes (1978). Money Shoal Basin. Ungrouped. Less than 60m thick. Fluvial deposits. Widely exposed as sea cliffs, discontinuous low ridges and dissected plateaux. Paleogene units "of equivalent age" to this Sandstone occur in the Woodbine Group of the Bonaparte Basin. Source of heavy mineral sands deposits (Tiwi Islands). Hosts lateritic bauxite.||||Unconformably overlies onshore Bathurst Island Group (Moonkinu Sandstone). ?Is overlain unconformably by Woodbine Group.|White to yellow, cross-bedded, medium- to coarse-grained quartz sandstone, minor lenses of siltstone, mudstone (with plant fossils) and granular conglomerate. Inland exposures are strongly weathered and iron-stained.|12-JUL-16
19044|Van Diemen Sandstone|69458|6|Mentioned|p42:6|Neogene|Paleogene|Money Shoal Basin.||||||12-JUL-16
19044|Van Diemen Sandstone|69673|6|Mentioned|p204|Cretaceous|Cretaceous||||||Cross bedded, medium to coarse grained quartz sandstone with minor lenses of siltstone and granular conglomerate.|
19044|Van Diemen Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, siltstone|
19050|Vanderlin Limestone|37605|5|Briefly described|p385|||Age assumed to be Quaternary.  Occurs on the Sir Edward Pellew Islands, Gulf of Carpentaria.||||||
19050|Vanderlin Limestone|42812|6|Mentioned|p57|||||||||
19050|Vanderlin Limestone|61155|5|Briefly described|p16|Holocene|Pleistocene|Age: <1.5Ma. Together with Beatrice Islands Limestone thickness is 5m. Geological region: East Arnhem Land.||||||
19050|Vanderlin Limestone|69458|5|Briefly described|p42:21|||Smith (1962). Sir Edward Pellew Islands, southern Gulf of Carpentaria. These rocks are presently 40m asl; due to either tectonism (Smith, 1962) or wind deposition (Coventry et al., 1980).||||Correlated with the Beatrice Island Limestone.|Coarsely cross-bedded limestone, rich in gastropods and foraminifera, with fine oolitic layers in foreset beds; tabular cross-beds may be up to 5m thick, with a few thin bands of quartz sandstone in the foresets.|12-JUL-16
19064|Vaughan Springs Quartzite|8222|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Ngalia Basin. Includes Trever Member.||||||13-DEC-06
19064|Vaughan Springs Quartzite|9380|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Ngalia Basin.||||||
19064|Vaughan Springs Quartzite|11884|5|Briefly described|Map Legend|Cambrian|Mesoproterozoic|Adelaidean|||||Medium silicified quartz sandstone, basal cobble conglomerate.|
19064|Vaughan Springs Quartzite|22496|6|Mentioned|p10||Neoproterozoic|In the Ngalia Basin.||||||13-DEC-06
19064|Vaughan Springs Quartzite|22803|6|Mentioned|p424|||Geological Province - Ngalia Basin.||||||
19064|Vaughan Springs Quartzite|23270|5|Briefly described|Table 1, p4||Proterozoic|In the Ngalia Basin. Age: Late Proterozoic.||||||13-DEC-06
19064|Vaughan Springs Quartzite|23271|5|Briefly described|Map legend||Proterozoic|Of Ngalia Basin. Age: Late Proterozoic.||||||13-DEC-06
19064|Vaughan Springs Quartzite|23361|6|Mentioned|12 Fig.2|||||||||
19064|Vaughan Springs Quartzite|23621|5|Briefly described|p33|||Geological Province: Ngalia Basin.||||||
19064|Vaughan Springs Quartzite|23858|5|Briefly described|p916|Proterozoic|Proterozoic|Geological Province: Ngalia Basin.||||||
19064|Vaughan Springs Quartzite|24047|6|Mentioned|p106 Appendix 1|||Geological Province: Ngalia Basin.||||||
19064|Vaughan Springs Quartzite|24064|4|Described|p226|Adelaidean|Adelaidean|Geological Province: Ngalia Basin. Maximum thicknes: 2800m.||||||
19064|Vaughan Springs Quartzite|24111|5|Briefly described|p216|Neoproterozoic|Neoproterozoic|Geological Province: Ngalia Basin. See also p215 Fig. 11.||||||03-MAY-10
19064|Vaughan Springs Quartzite|24173|5|Briefly described|p24|Neoproterozoic|Neoproterozoic|Part of extensive sand blanket including Mount Kinahan Sandstone, Heavitree Quartzite and Lewis Range Sandstone (Redcliff Pound Group) and Townsend Quartzite. Geological Province: Ngalia Basin.||||||06-APR-05
19064|Vaughan Springs Quartzite|29817|6|Mentioned|p10|||||||||
19064|Vaughan Springs Quartzite|30258|6|Mentioned|p100|||Younger control age 790 m.y.||||||
19064|Vaughan Springs Quartzite|30684|4|Described|p10|||Adelaidean age||||||
19064|Vaughan Springs Quartzite|31454|6|Mentioned|Fig.2|||||||||
19064|Vaughan Springs Quartzite|31991|6|Mentioned|p298|||Correlation||||||
19064|Vaughan Springs Quartzite|32442|4|Described|Table 1|||Adelaidean||||||
19064|Vaughan Springs Quartzite|32480|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
19064|Vaughan Springs Quartzite|32722|6|Mentioned|p58|||Adelaidean||||||
19064|Vaughan Springs Quartzite|33102|6|Mentioned|Fig.2|||||||||
19064|Vaughan Springs Quartzite|33103|4|Described|Table 4|||Mention p14.||||||13-DEC-06
19064|Vaughan Springs Quartzite|33104|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
19064|Vaughan Springs Quartzite|33757|3|Fully described|p9|||Adelaidean. See also Table 1.||||||13-DEC-06
19064|Vaughan Springs Quartzite|33758|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
19064|Vaughan Springs Quartzite|33759|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
19064|Vaughan Springs Quartzite|33760|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
19064|Vaughan Springs Quartzite|33761|6|Mentioned|p145|||Adelaidean||||||
19064|Vaughan Springs Quartzite|34724|6|Mentioned|p343|||||||||
19064|Vaughan Springs Quartzite|35038|6|Mentioned|p368|||||||||
19064|Vaughan Springs Quartzite|35102|6|Mentioned|p27|||||||||
19064|Vaughan Springs Quartzite|35221|4|Described|Table.1|||||||||
19064|Vaughan Springs Quartzite|36473|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
19064|Vaughan Springs Quartzite|36526|6|Mentioned|p151|||||||||
19064|Vaughan Springs Quartzite|36532|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
19064|Vaughan Springs Quartzite|37025|6|Mentioned|Map|||Map legend comments.||||||
19064|Vaughan Springs Quartzite|37058|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
19064|Vaughan Springs Quartzite|37462|4|Described|Table 4.IX|||||||||
19064|Vaughan Springs Quartzite|37537|5|Briefly described|Map legend|Adelaidean|Adelaidean|Pink to white, massive to thick bedded orthoquartzite; white, friable, quartz arenite; pebble and boulder conglomerate; shale. Geological Province: Ngalia Basin.||||||14-FEB-06
19064|Vaughan Springs Quartzite|37928|6|Mentioned|Fig.4|||||||||
19064|Vaughan Springs Quartzite|38157|6|Mentioned|Table VII|||||||||
19064|Vaughan Springs Quartzite|39210|6|Mentioned|p38|||||||||
19064|Vaughan Springs Quartzite|39565|6|Mentioned|p31|||||||||
19064|Vaughan Springs Quartzite|40105|6|Mentioned|p313|||||||||
19064|Vaughan Springs Quartzite|40383|6|Mentioned|p288|||||||||
19064|Vaughan Springs Quartzite|40740|6|Mentioned|p8|||||||||
19064|Vaughan Springs Quartzite|40906|6|Mentioned|Fig.9|||||||||
19064|Vaughan Springs Quartzite|41405|6|Mentioned|p206|||||||||
19064|Vaughan Springs Quartzite|41717|6|Mentioned|Fig.19|||||||||
19064|Vaughan Springs Quartzite|42059|6|Mentioned|Fig.2 P131|||||||||
19064|Vaughan Springs Quartzite|42326|5|Briefly described|p10|||||||||
19064|Vaughan Springs Quartzite|42504|5|Briefly described|p68|||||||||
19064|Vaughan Springs Quartzite|42643|6|Mentioned|p20, Fig.4 p19|||||||||
19064|Vaughan Springs Quartzite|42776|6|Mentioned|Fig.2 P301|||||||||
19064|Vaughan Springs Quartzite|43275|5|Briefly described|Map Legend||Neoproterozoic|||||||
19064|Vaughan Springs Quartzite|43595|5|Briefly described|p548,Fig.5-33,549||Adelaidean|||||||
19064|Vaughan Springs Quartzite|43631|3|Fully described|p20||Neoproterozoic|Age: Min 1280 Ma from Treuer Member, maybe 850 Ma from correlated units.||||||
19064|Vaughan Springs Quartzite|43749|6|Mentioned|Fig.1,p6||Neoproterozoic|||||||
19064|Vaughan Springs Quartzite|44158|4|Described|p21 Table.2|Neoproterozoic|Neoproterozoic|In the Ngalia Basin.||||||13-DEC-06
19064|Vaughan Springs Quartzite|45140|3|Fully described|p12-14, p26, p46, p60-61, p75, Appx.p41|||Nicholas (1971); Wells et al. (1972). Named after Vaughan Springs at Mount Doreen homestead. No type section defined as yet. Basal unit in the Ngalia Basin succession. Up to 2750m thick. Folded about E to ENE-trending fold axes; gentle to moderate dips; not metamorphosed; no apparent mineralisation. An age of 1280 Ma from glauconite (Cooper et al., 1971) is discounted: suggested that the glauconite was detrital, not authigenic.|<1070+/- 50 Ma; probably <1000 Ma.||Treuer Member.|Unconformably overlies Arunta Complex. Correlated with Heavitree Quartzite and Redcliff Pound Group.|Predominantly cross-bedded and ripple-marked, generally silicified quartz arenite; local thin basal conglomerate, and a sequence of shale, siltstone and thin interbeds of glauconitic sandstone.|
19064|Vaughan Springs Quartzite|45155|4|Described|p20|||||||||
19064|Vaughan Springs Quartzite|46792|6|Mentioned|p53|||Dates||||||
19064|Vaughan Springs Quartzite|46830|6|Mentioned|p21|||||||||
19064|Vaughan Springs Quartzite|46865|6|Mentioned|p46|||||||||
19064|Vaughan Springs Quartzite|46903|6|Mentioned|p48|||||||||
19064|Vaughan Springs Quartzite|61309|5|Briefly described|p13 Fig. 2, p15|||Geological Province: Ngalia Basin. Correlated with Bitter Springs Formation in the Amadeus Basin.||||||06-FEB-08
19064|Vaughan Springs Quartzite|61385|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Includes the Eva Springs, Treuer and Bigrlyi Members. Thick bedded quartzite, interbedded pebbly sandstone and pebble conglomerate. Geological Province: Ngalia Basin.||||||
19064|Vaughan Springs Quartzite|62453|6|Mentioned|p16|||Geological Province: Ngalia Basin.||||||
19064|Vaughan Springs Quartzite|62633|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Ngalia Basin. Bedded to well bedded quartz sandstone and quartzite, locally pebbly.||||||
19064|Vaughan Springs Quartzite|62642|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Georgina/Ngalia Basin. Undifferentiated orthoquartzite.||||||
19064|Vaughan Springs Quartzite|64068|6|Mentioned|p45, 223|||Ngalia Basin. Correlated with Amesbury Quartzite, southern Georgina Basin.||||||
19064|Vaughan Springs Quartzite|64956|5|Briefly described|p3 Tb. 1, p26|Paleoproterozoic|Paleoproterozoic|Max. depositional age: 1632+/-12Ma from detrital zircons. Geological province: Arunta region. This rock sample is only tentatively assigned to Vaughan Springs Quartzite (see p26 for possible correlative situations).||||||26-SEP-11
19064|Vaughan Springs Quartzite|65074|6|Mentioned|p358|Neoproterozoic|Neoproterozoic|Ngalia Basin. Appears as superseded Vaughan Springs Formation in the following paragraph.||||||
19064|Vaughan Springs Quartzite|65232|5|Briefly described|p70, p71 Fig. 43|Neoproterozoic|Neoproterozoic|Shallow-marine sandstone, minor mudstone, shale. Geol. Prov: Ngalia Basin. See also misspelling - Mount Vaughan Quartzite.||||||09-FEB-10
19064|Vaughan Springs Quartzite|65329|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of Ngalia Basin. Shown as younger than Southwark Granite Suite, oldest unit in Ngalia Basin. Quartz sandstone, local conglomerate at base; lesser siltstone, thinly bedded fine quartz sandstone; low flat to sublinear magnetic response||||||
19064|Vaughan Springs Quartzite|65330|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of Ngalia Basin. Shown as younger than Southwark Granite Suite, oldest unit in Ngalia Basin. Quartz sandstone, local conglomerate at base; lesser siltstone, thinly bedded fine quartz sandstone; low flat to sublinear magnetic response||||||
19064|Vaughan Springs Quartzite|65332|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Shown as equivalent age to Munyu Sandstone, Murraba Basin. Includes Treuer Member. Bedded to well bedded quartz sandstone and quartzite, locally pebbly||||||02-FEB-10
19064|Vaughan Springs Quartzite|65338|3|Fully described|p7, p27, pp57-59.|Neoproterozoic|Neoproterozoic|Basal unit in Ngalia Basin succession. Max depositional age from detrital zircons. May be as young as 840 Ma (Supersequence 1 of Centralian Superbasin). Constitutes the Bau, Nanga and Yindjirbi Ranges. Correlated with Heavitree, Townsend and Amesbury Quartzites, and Munyu Sandstone. From 300 m to 2500 m thick. Alluvial fan then shallow-marine deposits.|Max. 1632 +/- 11 Ma (Worden et al. 2008).||Includes Bigrlyi, Treuer and Eva Springs Members.|Unconformably overlies Koonoonyeri Granite, Lander Rock Formation. Is unconformably overlain by Yuendumu Sandstone, Mount Eclipse Sandstone, and probably by Mount Doreen Sandstone, Naburula Formation|Massive to thickly-bedded and cross-bedded, medium-grained orthoquartzite; uppermost 1000m contains well sorted and well rounded fine- and coarse-grained sandstones; minor detrital tourmaline, zircon and sericite; basal conglomerate widespread.|
19064|Vaughan Springs Quartzite|65341|6|Mentioned|p2 Fig.2. |||||||||
19064|Vaughan Springs Quartzite|65343|5|Briefly described|p3 Fig.4|Neoproterozoic|Neoproterozoic|Ngalia Basin.||||||
19064|Vaughan Springs Quartzite|67164|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Georgina/Ngalia Basins. Three units are un-named but mapped separately.||May be in Plenty Group.|||Basal monomict orthoconglomerate with quartzite phenoclasts in a quartzite matrix; thin-bedded, intensely ripple-marked, fissile quartzite; thick-bedded/massive, granule-bearing quartzite with pebble conglomerate interbeds.|05-OCT-11
19064|Vaughan Springs Quartzite|67565|6|Mentioned|p5 Fig.3.|||Ngalia Basin.||||||
19064|Vaughan Springs Quartzite|67872|5|Briefly described|p11, p13, p35, p39|Neoproterozoic|Neoproterozoic|Ngalia Basin. Also appears as Vaughn Springs Quartzite on p11. Seismic interpretations.|c.850 Ma.|||Is overlain by Albinia Formation.||17-APR-18
19064|Vaughan Springs Quartzite|67892|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Three sub-units are mapped separately.|||||Basal monomictic orthoconglomerate; then orthoquartzite and muscovite/tourmaline-bearing quartzite, medium to thick-bedded/massive; then thin-bedded, fissile, muscovite-bearing quartzite, intensely ripple-marked and cross-bedded, sugary textured.|04-JUL-12
19064|Vaughan Springs Quartzite|68270|5|Briefly described|p680,683|Tonian|Tonian|Ngalia Basin.||||Overlain unconformably by Naburula Formation or Mount Davenport Diamictite Member.||
19064|Vaughan Springs Quartzite|68733|6|Mentioned|p190|||Ngalia Basin.||||||
19064|Vaughan Springs Quartzite|68994|6|Mentioned|p18|||||||Equivalent to Heavitree Quartzite (Amadeus Basin).||
19064|Vaughan Springs Quartzite|68998|5|Briefly described|p18|Neoproterozoic|Neoproterozoic|Ngalia Basin.||||Overlies Ennugan Mountains Granite.|Quartzites.|
19064|Vaughan Springs Quartzite|69437|5|Briefly described|p22:4-6, 16|Cryogenian|Cryogenian|Ngalia Basin, Centralian A Superbasin. Supersequence 1. Has potential as a petroleum reservoir.|||||A thin succession of sandstone.|12-JUL-16
19064|Vaughan Springs Quartzite|69439|3|Fully described|p24:1-6, 8-9, 13-18, 20-21|Cryogenian|Cryogenian|Wells and Moss (1983). Ngalia Basin, Centralian A Superbasin. Supersequence 1. Type section is in the Vaughan Springs Syncline. Forms prominent strike ridges on the N and S flanks of the Basin. Over 2500m thick, thinning to E to 300m. Severely eroded by subsequent uplift from the Vaughan Springs Movement. Provenance discussed. Detrital zircon maximum deposition age (Donnellan, 2008; Worden et al., 2008). Contains potential reservoirs possibly sealed by Rinkabeena Shale.|<1594 +/- 30 Ma.||Bigrlyi, Treuer, Eva Springs Members.|Underlies Albinia Formation (conformably or disconformably), Mount Doreen Formation and Yuendumu Sandstone (unconformably) and Mount Eclipse Sandstone. Correlative of Heavitree and Dean Quartzites.|Mainly well-bedded to massive, well-sorted quartz sandstone; local basal pebble conglomerate and iron-stained feldspathic conglomerate. Strongly brecciated in many places.|12-JUL-16
19064|Vaughan Springs Quartzite|69440|6|Mentioned|p25:2|||Ngalia Basin. Inferred to correlate with Munyu Sandstone (Murraba Basin).||||||12-JUL-16
19064|Vaughan Springs Quartzite|69443|6|Mentioned|p28:5|||Ngalia Basin.||||Correlated with Plenty Group.||12-JUL-16
19064|Vaughan Springs Quartzite|69508|5|Briefly described|Map legend.|Neoproterozoic|Paleoproterozoic|Ngalia Basin.|||Treuer Member.||Bedded to well-bedded quartz sandstone and quartzite, locally pebbly.|
19064|Vaughan Springs Quartzite|69673|5|Briefly described|p105, p107 fig 85, p110|||Up to 2500m thick. Sedimentation occurred within an alluvial fan, followed by intertidal and shallow marine deposition.|||Includes Bigrlyi Member, Treuer Member, Eva Springs Member||Quartz sandstone and local basal pebble conglomerate and iron stained feldspathic conglomerate.|
19064|Vaughan Springs Quartzite|69791|6|Mentioned|p1082-1084|Neoproterozoic|Neoproterozoic|Scree from this unit conceals the contact between Mount Eclipse Sandstone and underlying units.||||||
19064|Vaughan Springs Quartzite|70301|5|Briefly described|p26|Neoproterozoic|Neoproterozoic|Ngalia Basin.||||Nonconformably overlies Ennugan Mountains Granite.||
19064|Vaughan Springs Quartzite|70793|4|Described|500k_interpgeop14_lut.csv|Cryogenian|Neoproterozoic|Of Amadeus Basin (Phase 1), Centralian Superbasin. Events: Alice Springs Orogeny (450-295 Ma); Areyonga Movement; Delamarian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma). See 500k_interpgeop14_lut.csv, 2_5m_interpgeop15_lut.csv.|1000-800 Ma (inferred; biostrat).||||Quartz sandstone, sandstone, and conglomerate; kyanite schist locally|
19064|Vaughan Springs Quartzite|70826|6|Mentioned|p5 tbl 2|||Supersequence 1, Centralian Superbasin.||||||20-APR-20
19064|Vaughan Springs Quartzite|71080|6|Mentioned|p23|||Ngalia Basin.||||Correlated with Munyu Sandstone, Murraba Basin.||
19064|Vaughan Springs Quartzite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||quartzite, sandstone|
19064|Vaughan Springs Quartzite|71268|4|Described|GEOL_LUT_CSV files|Tonian|Tonian|Of Amadeus Basin (Phase 1), Centralian Superbasin. Events: Delamarian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma). See 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|1000-800 Ma (inferred)|||Correlable with Kulail Sandstone, Dean Quartzite, Heavitree Quartzite.|Quartz sandstone, sandstone, and conglomerate; kyanite schist locally|
19064|Vaughan Springs Quartzite|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen.|1632+/-11 Ma (MDA: U-Pb zircon SHRIMP)||||Quartzite.|
19064|Vaughan Springs Quartzite|71858|5|Briefly described|p44-45|||Aileron Province.||||||
19064|Vaughan Springs 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, Dean Quartzite, Heavitree Quartzite. Min age  from biostratigraphy.|||||Informal grouping description: Quartz sandstone, sandstone, and conglomerate; kyanite schist locally [probably only in Dean Quartzite].|
19064|Vaughan Springs Quartzite|72375|5|Briefly described|p5|||Of Ngalia Basin.||||Equivalent to Heavitree Formation.||
19064|Vaughan Springs Quartzite|72516|6|Mentioned|p86|||Ngalia Basin. Age correlative of the Yackah beds of the Georgina Basin.||||||
19064|Vaughan Springs Quartzite|73086|6|Mentioned|p9, p145|||Ngalia Basin. Basal unit.||||Correlates to Heavitree Formation.||
19064|Vaughan Springs Quartzite|73399|6|Mentioned|App.E||||||||Quartzite.|
19065|Vaughton Siltstone|22538|6|Mentioned|Fig3 P708|||||||||
19065|Vaughton Siltstone|22600|4|Described|Map legend|Statherian|Statherian|||||||
19065|Vaughton Siltstone|23937|6|Mentioned|p10|||Of the Balma Group.  See also p92 Appendix 1.||||||18-APR-05
19065|Vaughton Siltstone|24048|3|Fully described|p56|Mesoproterozoic|Paleoproterozoic|Of the Balma Group.  Overlain by Conway Formation; underlain by Strawbridge Breccia.  Max. thickness: 1000m.  Geological Province: McArthur Basin.||||||07-NOV-08
19065|Vaughton Siltstone|24049|5|Briefly described|Map Legend|Statherian|Statherian|Of Balma Group. Mudstone: khaki green to black, carbonaceous in part, generally massive; minor sandstone and dolostone interbeds; common siderite nodules; basal conglomerate with friable sandstone matrix; very recessive. Geol. Prov: McArthur Basin.||||||11-OCT-05
19065|Vaughton Siltstone|32660|5|Briefly described|Table 4|||||||||
19065|Vaughton Siltstone|42597|5|Briefly described|Map Legend|Carpentarian||||||||
19065|Vaughton Siltstone|43010|2|Defined|p113||Paleoproterozoic|Of the McArthur Group. Of Statherian age||||||07-NOV-08
19065|Vaughton Siltstone|44112|6|Mentioned|p30,58|||||||||
19065|Vaughton Siltstone|44299|4|Described|p.12|||SD/53-7,8. Lower(?) Proterozoic. Table 1.||||||
19065|Vaughton Siltstone|44300|14|Not recorded|map legend|||SD/53-7,8. Lower (?) Proterozoic.||||||
19065|Vaughton Siltstone|45162|6|Mentioned|p45|||||||||
19065|Vaughton Siltstone|61403|5|Briefly described|Map Legend|Statherian|Statherian|Of Balma Group. Mudstone: khaki green to black, carbonaceous in part, generally massive; minor sandstone and dolostone interbeds; common siderite nodu les; basal conglomerate with friable sandstone matrix; very recessive. Geol. Prov: McArthur Basin.||||||
19065|Vaughton Siltstone|64817|6|Mentioned|p353 Fig.4|||||Of the Balma Group.||||
19065|Vaughton Siltstone|67323|5|Briefly described|Eastern Australia Time-Space Plot; p35|Paleoproterozoic|Paleoproterozoic|McArthur Basin. Appears as Vaughton Formation on p35.|1645-1620 Ma.|||||
19065|Vaughton Siltstone|69430|4|Described|p15:3, 21-22|Statherian|Statherian|Walker Fault Zone, northern McArthur Basin. c.600-1000m thick. Very recessive unit. Mostly deep subtidal below wave base sediments; marginal ?marine transgressive/fluvial unit at base. May correlate with the economically important Barney Creek Formation.||Balma Group.||Disconformably overlies Strawbridge Breccia. Is overlain by Conway Formation conformably and gradationally, and by Yarrawirrie Formation unconformably.|Khaki green to black, partly carbonaceous, generally massive mudstone; minor sandstone and dolostone interbeds; common siderite nodules; basal conglomerate with friable sandstone matrix. Contains black carbonaceous shale with up to 10% pyrite.|12-JUL-16
19065|Vaughton Siltstone|69673|4|Described|p16 fig 13, p31, p46, p47|Mesoproterozoic|Paleoproterozoic|Walker Fault Zone, 600-1000m thick. Deposited primarily in a subtidal environment, below wave base.||Balma Group||Conformably overlain by Conway Formation, Unconformably overlain by Yarrawirrie Formation, disconformably overlies Strawbridge Breccia, (tentative) correlated with|Massive, partly carbonaceous mudstone with minor sandstone and dolostone interbeds and basal conglomerate; minor shale.|
19065|Vaughton Siltstone|71374|5|Briefly described|p12|Statherian|Statherian|May correlate with the Yarawoi Formation (Habgood Group).||Balma Group||||
19065|Vaughton Siltstone|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.||Middle Balma Group.||||
19065|Vaughton Siltstone|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].||||||
19070|Vee Formation|5952|6|Mentioned|p222|||Defined by Mory (1988).||||||05-MAY-09
19070|Vee Formation|13194|4|Described|p384 Tb. 4-16, p396 fig 4-60|Campanian|Cenomanian|100-250m thick open marine shelf deposits. Type section: Swift 1 (2140-2360m).||Bathurst Island Group||Grades into Brown Gannet Limestone. Coeval with Wangarlu Formation to eat. Overlain by Turnstone Formation.|Marl, calcilutite, calcareous claystone.|
19070|Vee Formation|23377|6|Mentioned|p212 Fig.5||Late Cretaceous|In the Vulcan Sub-basin..||||||13-DEC-06
19070|Vee Formation|41459|6|Mentioned|Fig.2|||||||||
19070|Vee Formation|41532|2|Defined|p306|Late Cretaceous||||||||
19070|Vee Formation|41731|6|Mentioned|Fig.3|||||||||
19070|Vee Formation|42442|2|Defined|p29|early Campanian|Cenomanian|Age: Late Cretaceous (Cenomanian to early Campanian).||||||13-DEC-06
19070|Vee Formation|43661|6|Mentioned|Fig.3|||||||||
19070|Vee Formation|43699|6|Mentioned|Fig.6,p10||Late Cretaceous|||||||
19070|Vee Formation|43739|6|Mentioned|Fig.5,p38||Late Cretaceous|||||||
19070|Vee Formation|49637|5|Briefly described|Fig.3|Late Cretaceous|Late Cretaceous|Of the Bathurst Island Group. Geological Province: Vulcan Sub-basin.||||||07-FEB-11
19074|Velkerri Formation|22538|6|Mentioned|Fig3 P708|||||||||
19074|Velkerri Formation|22823|6|Mentioned|p517|||Geological Province - McArthur Basin.||||||
19074|Velkerri Formation|23216|5|Briefly described|Table1p7,34-5|||||||||
19074|Velkerri Formation|23356|5|Briefly described|26 Tab.2|Mesoproterozoic|Mesoproterozoic|Age: ~1400Ma.||||||13-DEC-06
19074|Velkerri Formation|23404|5|Briefly described|p646|||Of Roper Group.||||||
19074|Velkerri Formation|23776|5|Briefly described|p705 Fig 2|||Of Maiwok Subgroup||||||
19074|Velkerri Formation|23937|2|Defined|p94 App. 1|Calymmian|Calymmian|Of the Roper Group, formerly of now abandoned Cobanbirini Fm. Disconformably overlain Moroak Fm; conformably overlies Bessie Creek Sst. Age: >1429+/-31Ma. Max. thick: 330m in type section.  Geol.Prov: McArthur Basin.||||||18-APR-05
19074|Velkerri Formation|24047|6|Mentioned|p28 Fig. 21|||||||||
19074|Velkerri Formation|24048|5|Briefly described|p71|||Of the Maiwok Subgroup.||||||13-DEC-06
19074|Velkerri Formation|24179|5|Briefly described|p90|||Lower part of the Roper Group.  Geological Province:  McArthur Basin.||||||
19074|Velkerri Formation|24303|5|Briefly described|p34, p62 Appendix|||Of the Roper Group. Geological Province: McArthur Basin. Probable correlative of Lake Woods beds.||||||
19074|Velkerri Formation|32660|6|Mentioned|Fig.7|||||||||
19074|Velkerri Formation|40691|4|Described|p84|||||||||
19074|Velkerri Formation|41220|6|Mentioned|Fig.3|||||||||
19074|Velkerri Formation|41268|4|Described|p296|||||||||
19074|Velkerri Formation|41531|5|Briefly described|p165|||||||||
19074|Velkerri Formation|42058|5|Briefly described|p122|||||||||
19074|Velkerri Formation|42385|6|Mentioned|Fig.5 P8|||||||||
19074|Velkerri Formation|42395|6|Mentioned|Fig.26 P86|||||||||
19074|Velkerri Formation|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.||Of Maiwok Subgroup (Roper Group).||In schematic section, underlies Moroak Sandstone Member (McMinn Formation); overlies Bessie Creek Formation.|Shale, silty mudstone, micaceous siltstone, minor sandstone. Detailed lithology given.|09-NOV-11
19074|Velkerri Formation|42639|4|Described|p44, Table 7 p39|||||||||
19074|Velkerri Formation|42739|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Of the Maiwok Subgroup. Flaggy, fine-grained sandstone and siltstone, commonly micaceous.||||||19-OCT-05
19074|Velkerri Formation|42812|3|Fully described|p54, Table 5|||Of the Maiwok Subgroup.||||||13-DEC-06
19074|Velkerri Formation|42846|5|Briefly described|Fig.1 p502|||Of the Roper Group.  Fine-grained. Geological Province: McArthur Basin.||||||13-DEC-06
19074|Velkerri Formation|43010|5|Briefly described|Fig.6||Mesoproterozoic|Of Maiwok Subgroup. Of "Mid Proterozoic" age.||||||13-DEC-06
19074|Velkerri Formation|43036|6|Mentioned|Fig.5|||Of the Roper Group.||||||13-DEC-06
19074|Velkerri Formation|43149|5|Briefly described|Map Legend||Mesoproterozoic|Of Maiwok Subgroup.Of Calymmian age.||||||13-DEC-06
19074|Velkerri Formation|44201|14|Not recorded|p.9||Neoproterozoic|U.Proterozoic.||||||
19074|Velkerri Formation|44332|14|Not recorded|p.8,opp.6,map|||(D53-14).||||||
19074|Velkerri Formation|44333|14|Not recorded|map legend|||Upper(?) Proterozoic.||||||
19074|Velkerri Formation|44471|14|Not recorded|p.10, opp.p.7, map|||(D53-10).||||||
19074|Velkerri Formation|44472|5|Briefly described|map legend|||Of the Maiwok Sub-Group (Roper Group).  Pink calcareous greywacke, calcareous siltstone, laminated shale.Upper (?) Proterozoic.||||||02-DEC-04
19074|Velkerri Formation|44530|14|Not recorded|opp.12|||(D53-15).||||||
19074|Velkerri Formation|44531|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
19074|Velkerri Formation|45022|5|Briefly described|p.81, Table 11.Pl.28||Adelaidean|Of Maiwok Subgroup.||||||
19074|Velkerri Formation|45162|6|Mentioned|p163|||||||||
19074|Velkerri Formation|46679|14|Not recorded|map legend||Neoproterozoic|Upper Proterozoic.||||||
19074|Velkerri Formation|46861|6|Mentioned|Fig.2|||||||||
19074|Velkerri Formation|60483|5|Briefly described|p7 Fig. 5|||Of Maiwok Subgroup (Roper Group). Geological Province: McArthur Basin. Carbonaceous unit.||||||
19074|Velkerri Formation|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Maiwok Subgroup. Overlain by McMinn Formation, underlain by Bessie Creek Sandstone.||||||04-JUN-09
19074|Velkerri Formation|60573|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Roper Group.  Mudstone and siltstone, variably grey to black, locally high in organic carbon content, minor interbeds of glauconitic fine sandstone.||||||14-FEB-05
19074|Velkerri Formation|61250|5|Briefly described|p43|Mesoproterozoic|Mesoproterozoic|Contains rich petroleum systems. Geological Province: Beetaloo Sub-basin.||||||27-MAY-06
19074|Velkerri Formation|61390|5|Briefly described|Map Legend|Ectasian|Calymmian|Of the Maiwok Subgroup. Mudstone and siltstone: variably grey to black, locally high organic carbon content, minor interbeds of glauconitic fine sandstone.||||||
19074|Velkerri Formation|62376|5|Briefly described|p38|Mesoproterozoic|Mesoproterozoic|Of the Roper Group. Geological Province: Beetaloo Sub-Basin.||||||09-FEB-10
19074|Velkerri Formation|63062|5|Briefly described|p38|||Of the Roper Group. Geological Province: McArthur Basin.||||||07-FEB-11
19074|Velkerri Formation|63245|5|Briefly described|p8, p19|Mesoproterozoic|Mesoproterozoic|Of the Roper Group. Age: 1.45Ga. Geological Province: McArthur Basin.||||||
19074|Velkerri Formation|64784|4|Described|p1-10     |Proterozoic|Proterozoic|Beetaloo Basin. One of two major economic hydrocarbon source units in the Basin; TOC levels commonly exceed 4% and occasionally reach 8%.||||Overlies the Bessie Creek Sandstone. Unconformably? underlies the Moroak Sandstone.|Coarsening-upward succession, with greenish, organic poor shale present in the lower and upper portion of the formation and the organically richest portions near the middle.|
19074|Velkerri Formation|64816|5|Briefly described|p1, p2, p4, p5, p8-10, p18-21       |Proterozoic|Proterozoic|The most likely source for the oil in this study. A major potential petroleum source rock.|Deposition age ca. 1430 Ma|Unit in Roper Group.|||Glauconitic marine shale; finely laminated claystone/mudstone.|
19074|Velkerri Formation|64817|6|Mentioned|p353 Fig.4 |||||Of the Maiwok Subgroup.||||
19074|Velkerri Formation|64975|6|Mentioned|p162 Fig.6.|Mesoproterozoic|Mesoproterozoic|||Unit in Roper Group.||||
19074|Velkerri Formation|65228|5|Briefly described|Fig.02.|||||Unit in Maiwok Subgroup.||Overlies Bessie Creek Sandstone. Is overlain by McMinn Formation.||
19074|Velkerri Formation|65236|5|Briefly described|p2, p[3 Fig. 3, p4 Fig. 4|Mesoproterozoic|Mesoproterozoic|Overlain by Moroak Sst. Max. thickness: 1150m. Age: 1.43Ga (Warren et al 1998). Geol.province: Beetaloo Sub-basin. Oldest petroleum source rock sub-basin. Interpreted as a tripartite subdivision of organic-rich sub-units (3 unnamed members).||||||09-JUN-09
19074|Velkerri Formation|65342|5|Briefly described|p12. |||Daly Basin. Max. thickness at least 836 m. Seen as having potential as an insulating layer for geothermal energy.|||||Carbonaceous mudstone and siltstone.|
19074|Velkerri Formation|69018|5|Briefly described|p449, 450, 451|Calymmian|Calymmian|Organic-rich. Likely source rock for hydrocarbons in Bessie Creek Sandstone and possibly Jamison Sandstone. Estimated maximum burial 2.5 km, corresponding to ~75 degrees C.||Of Roper Group.||Intruded by 1280-1220 Ma by dolerite sill at base, in places.Overlies Bessie Creek Sandstone.||
19074|Velkerri Formation|69206|6|Mentioned|p3|||McArthur Basin. Has potential for unconventional oil and shale gas.||||||
19074|Velkerri Formation|69418|6|Mentioned|p3:36|||McArthur Basin. Excellent hydrocarbon source rocks.||||||12-JUL-16
19074|Velkerri Formation|69430|3|Fully described|p15:3, 27, 29-30, 53, 61-63|Calymmian|Calymmian|McArthur Basin. 330m thick in the type section in BMR drillhole Urapunga-4. Attains a thickness of 880m in the Beetaloo Sub-basin to the S. Distal shelf sediments. Potential hydrocarbon source rock (up to 12% TOC); oil and gas shows are common. Has some conventional reservoir potential, as well as potential for unconventional reservoirs (basin-centred gas). May be source rock for Moroak Sandstone, and source rock and seal for Bessie Creek Sandstone.|c.1.43 Ga (Lanigan et al., 1994).|Maiwok Subgroup.||Conformably overlies Bessie Creek Sandstone. Is overlain disconformably by Moroak Sandstone.|Grey and black mudstone and siltstone, with calcite nodules and pyrite stringers; minor fine glauconitic sandstone.|12-JUL-16
19074|Velkerri Formation|69451|6|Mentioned|p35:13|||Potential petroleum source rock: TOC up to 12%.||Roper Group.||||12-JUL-16
19074|Velkerri Formation|69673|4|Described|p20, p24, p29, p31,p33, p37, p44, p46|||Shale oil and gas potential. Northwestern and Southern McArthur Basin.||Maiwok Subgroup||Overlain by McMinn Formation, unconformably overlain by Moroak Sandstone, conformably overlies Bessie Creek Sandstone|Claystone, mudstone and siltstone with calcite noduels and pyrite stringers; minor fine sandstone.|
19074|Velkerri Formation|70734|4|Described|p13-19, 21-25|Mesoproterozoic|Mesoproterozoic|McArthur Basin. 330-880 m thick. Thickest & gas prone in Beetaloo Sub-basin. Extends over ~80,000 km2. Essentially unmetamorphosed and undeformed. Lower and upper parts distinguished in age and geochem data, but not explained. Thermal maturity of organic matter ranges from marginally mature to highly mature. Age consistent with SHRIMP age from tuff in Wooden Duck Member of Mainoru Formation, lower in succession. Storm-dominated shelf. Sampled from BMR Urapunga 4. Whole rock and pyrite geochem. data reported and discussed.|Re-Os 1361+/-21 Ma upper, 1417+/-29 Ma lower pt.|Of Maiwok Subgroup.||Overlain by Moroak Sandstone. Overlies the Corcoran Formation and the Bessie Creek Sandstone. Intruded by dolerite sills.|Dominantly parallel-laminated grey to black carbonaceous mudstones, with minor grey siltstones and very fine-grained sandstones including calcite nodules, pyrite stringers and glauconitic siltstones.|10-JUL-18
19074|Velkerri Formation|70822|4|Described|p101, p102 fig 1 (A),  p104-112|Mesoproterozoic|Mesoproterozoic|Greater McArthur Basin. Up to 930m thick. Mineralogy, geochemistry and TOC described in detail; discussed under informal upper, middle and lower sections. Low (sub-greenschist) metamorphic grade. Hosts "live" hydrocarbon occurrences; potential as an unconventional gas play. Ages of bottom and top respectively (Kendall et al., 2009).|1417 +/- 29 Ma to 1361 +/- 21 Ma (Re- Os).|Roper Group||Overlies Bessie Creek Sandstone. Is overlain by Moroak Sandstone, and unconformably by Nutwood Downs Volcanics.|Exceptionally organic-rich sediments: dominantly black shales with mudstones and siltstones and minor sandstones.|
19074|Velkerri Formation|70897|6|Mentioned|Fig.1.7.6,9|||McArthur Basin.||||||28-NOV-17
19074|Velkerri Formation|70968|2|Defined|p50-51, p55, p59-66, p75, p123-124|Ectasian|Ectasian|See also p126-128, p130-131, p134, p138, p140-143. Sweet in Abbott et al. (2001); after Dunn (1963) who included it as the basal unit in the Maiwok Subgroup. Formerly mapped as part of Cobanbirini Formation of Paine (1963) and Smith (1964); this name has been abandoned. Also referred to (by Amoco APC) as Lansen Creek Member (of Cobanbirini Formation); this is a junior synonym of the Velkerri Formation and has also been abandoned, along with its variants (eg "Lansen Creek Shale" of Powell et al., 1987; Lansen Shale of Lindsey, 2001). Named after Velkerri Creek. Recessive: underlies valleys and broad plains. The type section is a complete intersection in drillhole Urapunga-4, from 372m to 42m depth, kept at Geoscience Australia. Notable for a middle section of organic-rich beds which are prime petroleum source rocks.  Lithology described and illustrated in great detail. Up to 880m thick. Marine, sub-tidal, sub-wave base deposits. Re-Os ages for lower and upper parts respectively. Detrital zircon diagram.|1417 +/- 29 Ma and 1361 +/- 21 Ma.|Maiwok Subgroup.||Conformably and gradationally overlies Bessie Creek Sandstone. Is overlain conformably by Moroak Sandstone. Is intruded by Derim Derim Dolerite sills.|Interlaminated and thinly interbedded claystone and siltstone, minor fine-grained sandstone (typically glauconitic), and rare thin dolomitised limestone. Calcite nodules and veins and pyrite are present throughout.|24-SEP-18
19074|Velkerri Formation|71059|4|Described|iii, p1, p3, p6-7, p9-12, p14-21, p23-24|Mesoproterozoic|Mesoproterozoic|See also p28-31, p42-61. McArthur Basin. Of exploration interest for unconventional shale oil and gas: the middle of this unit has an average TOC of 3.76 wt%. A shale gas discovery has been announced. Estimated shale/tight gas/shale oil and condensate resources detailed. <50 - 1483m thick. Shallow to distal marine shelf deposits. Has a unique thin carbonate marker bed at the base. Core photograph. TOC and Pyrolysis, elemental kerogen CHONS, X-ray diffraction, pore fluid saturations, organic petrology reflectivity, gas analysis, data all detailed.||Roper Group.||Conformably overlies Bessie Creek Sandstone. Is overlain conformably / locally disconformably by Moroak Sandstone.|Interlaminated and thinly interbedded grey and black mudrock and siltstone; minor fine glauconitic sandstone.|
19074|Velkerri Formation|71488|4|Described|p140-p153|Ectasian|Ectasian|Beetaloo Sub-basin. Ages are interpreted as maximum depositional ages. Demonstrated to host a major shale-gas resource (Close et al., 2017) -the oldest commercial hydrocarbons yet known. Re-Os ages of 1417 +/- 29 Ma from the base and 1361 +/- 21 Ma from the top of the unit are provided after Kendall et al., 2009. Also referred to as the Upper, upper, Middle and Lower, Velkerri Formation on p144. Zircon geochronology results are briefly discussed.|1308 +/- 41 Ma|Maiwok Subgroup||Conformably overlies the Bessie Creek Sandstone. Conformably overlain by the Moroak Sandstone. Unconformably overlain by the Jamison sandstone.|Black mudrock succession with minor sandstone.|
19074|Velkerri Formation|71779|1|Redefined|iii, p1-p4, p6-8, p10-19, p24-26|Mesoproterozoic|Mesoproterozoic|McArthur Basin. Redefinition by TJ Munson and D Revie. Name derived from Velkerri Creek in URAPUNGA. The type section is a complete intersection in drillhole BMR Urapunga-4 from 372m to 42m depth (see Sweet and Jackson 1986). Subdivisions are best distinguished by a combination of methods including lithology, organic geochemistry, chemostratigraphy, wireline logging, hyperspectral logs and palynology; the distinguishing features of all its subdivisions are discussed in some detail. Thickness in various drillholes provided. Originally mapped as the lower part of the Cobanbirini Formation of Paine (1963) and Smith (1964). This formation has also been described as the Lansen Creek Member of the Cobanbirini Formation; that name is a junior synonym of the Velkerri Formation and has been abandoned along with all of its variants. This unit is rarely exposed except as occasional small outcrops of buff to white-weathering laminated siltstone and mudstone. This unit typically underlies broad valleys and extensive plains. Exposure locations are provided on p6. This formation is intersected by numerous wells in URAPUNGA, LARRIMAH, BAUHINIA DOWNS and possibly BEETALOO. Petrography, sedimentary features, palynology discussed. See also  p12 fig 9, p14-p16, p20, p27.||Maiwok Subgroup|Includes the Kalala, Amungee and Wyworrie members.|Conformably overlies the Bessie Creek Sandstone. Conformably overlain by the Moroak Sandstone.|Interlaminated and thinly interbedded claystone and siltstone, minor fine-grained sandstone and rare thin dolomitised limestone.|24-SEP-18
19074|Velkerri Formation|71857|5|Briefly described|iii, p1-2, p8-14, p25-31, p33-49|Mesoproterozoic|Mesoproterozoic|McArthur Basin. Self-sourced, continuous petroleum reservoir with documented oil and gas shows in several wells. Only middle part of Velkerri Formation discussed. Details of  8 wells tabulated. Core data analyzed for potential hydrocarbon resources. Structure, isopach maps. Data tabulated and graphed in 5 Appendices, one each for the Gorrie, Beetaloo, OT Downs and Broadmere Sub-basins.||Roper Group.|||Includes black shale horizons.|04-FEB-19
19074|Velkerri Formation|71893|5|Briefly described|p5, p8, p17, p20, p25, p32, p36-p37, p40|||McArthur Basin.||Maiwok Subgroup|Includes the Kalala and Wyworrie members.|Conformably overlain by the Moroak Sandstone.  Unconformably overlain by the Jamison sandstone.||
19074|Velkerri Formation|72381|4|Described|p771-779|Mesoproterozoic|Mesoproterozoic|Of Beetaloo Sub-basin, McArthur Basin. Deposited in a marine, subtidal, sub-wave base and generally quiet environment, affected by regular current activity (Powell et al. 1987; Abbott et al. 2001; Munson 2016; Sheridan et al. 2018). Maximum depositional age constrained at 1308+\-41 Ma (Yang et al., 2018). Kendall et al (2009) reported Re-Os model age of 1361+\-21 Ma in the upper part of the formation. Deposition is coeval with post-orogenic Mount Ida Province exhumations (c. 1460 and 1390 Ma), nothern Gawler Craton magmatism and high-grade metamorphism c. 1540 (Morrissey et al., 2018) and eastern Gawler Craton exhumation (c. 1420 Ma; Foster and Ehlers 1998). Intersected in Elliott-1 drillhole, and U-Pb zircon dating and Hf isotopic analysis was undertaken (this study). U-Pb detrital zircon age spectra from the Wyworrie Member (Fanning 2012, Yang et al 2018) suggest upper Velkerri provenance from the Eastern Fold Belt (Mount Isa Province; Griffin et al. 2006), or based on Hf isotopic analysis (this study), from Georgetown Province (Condie et al. 2005; Murgulov et al. 2007), or the eastern Gawler-Curnamona terranes (Kromkhun et al. 2013; Armit et al. 2014).||Unit of Mailwok Subgroup.|Includes Wyworrie, Amungee and Kalala members.|Overlain by Moroak Formation. Underlain by Bessie Creek Sandstone. Intruded by Derim Derim Dolerite.|Black shales and minor sandstone-siltstones.|
19074|Velkerri Formation|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 Bessie Creek Sandstone and underlies Moroak Sandstone.||
19074|Velkerri Formation|72718|6|Mentioned|p7-13, p20|Ectasian|Calymmian|Southern McArthur Basin. Urapunga Fault Zone, southwestern McArthur Basin, and Batten Fault Zone (north). Ages from organic-rich shales from the lower and upper parts of the formation respectively.|1417 +/- 29 Ma, 1361 +/- 21 Ma Re-Os|Maiwok Subgroup, Roper Group||Underlain by Bessie Creek Sandstone. Overlain by Moroak Sandstone.||
19074|Velkerri Formation|72912|5|Briefly described|p5 Fig.3, p36, p37 Fig.14.|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. TOC is described. Described as one of the best source rocks in the McArthur Basin.||Maiwok Subgroup|Includes Amungee Member.|Overlies Bessie Creek Sandstone and underlies Moroak Sandstone.|Includes hydrocarbon bearing shales (Jackson et al., 1988).|15-MAR-21
19074|Velkerri Formation|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|Southern McArthur Basin, Roper Superbasin.||Maiwok Subgroup, Roper Group||Underlain by Bessie Creek Sandstone. Overlain by Moroak Sandstone.||
19074|Velkerri Formation|73098|6|Mentioned|p4, p7, p11|||McArthur Basin. Organic petrolography performed on two samples from the Alexander 1 well. One sample had low organic matter and bitumen; the other sample had higher bitumen. [See report for bitumen/maceral description].|||||Includes dark brown and dark grey shales.|
19074|Velkerri Formation|73242|5|Briefly described|p39|Ectasian|Ectasian|Geochron from black shales (Kendall et al., 2009). Unit also assigned a detrital zircon young age of 1308 +/- 41 Ma (Yang et al., 2018), although it is unclear whether this is a maximum depositional age.|1361 +/- 21 Ma, 1417 +/- 29 Ma Re-Os|Maiwok Subgroup, Roper Group|Wyworrie Member, Amungee Member, Kalala Member|Underlain by Bessie Creek Sandstone. Overlain by Moroak Sandstone.|Includes interbedded mudstone and fine sandstone with mudstone and shale.|
19074|Velkerri Formation|73280|6|Mentioned|piii, p1, p4-5, App.1A, App.1B|||McArthur Basin. Sampled for XRD mineralogy to investigate brittleness and Kubler indices [see report].|||Amungee Member, Kalala Member, Wyworrie Member|||
19074|Velkerri Formation|73412|5|Briefly described|p4, 8|||Southern McArthur Basin.||Maiwok Subgroup.||Overlies Bessie Creek Sandstone. Is overlain by Moroak Sandstone.||
19148|Vulcan Formation|5952|5|Briefly described|p215 Fig. 5|||Appears as Vulcan in figure. Geological Province: Bonaparte Basin.||||||01-MAR-10
19148|Vulcan Formation|23377|5|Briefly described|p223||Late Jurassic|In the Vulcan Sub-basin.||||||13-DEC-06
19148|Vulcan Formation|23378|5|Briefly described|p197,202|Early Cretaceous|Late Jurassic|In the Vulcan Sub-basin.||||||01-MAR-10
19148|Vulcan Formation|42053|4|Described|p42|||||||||01-MAR-10
19148|Vulcan Formation|42861|6|Mentioned|p4|||||||||
19148|Vulcan Formation|43826|6|Mentioned|Fig.2,p163|Early Cretaceous|Late Jurassic|||||||01-MAR-10
19148|Vulcan Formation|60378|6|Mentioned|p95|Late Jurassic|Late Jurassic|Includes interpreted deep marine fan sediments considered to be a reservoir facies.|||See also informal subdivisions: Lower Vulcan Formation, Upper Vulcan Formation.|||
19148|Vulcan Formation|61550|6|Mentioned|p494, p495 Fig.2. |Late Jurassic|Late Jurassic|Contains marine hydrocarbon source rocks.||Unit in Swan Group.||Overlies Montara Formation. Is overlain unconformably by Echuca Shoals Formation.||
19148|Vulcan Formation|64697|5|Briefly described|p84 Fig.2, p86, p87, p88, p91 |Early Cretaceous|Late Jurassic|||||||
19148|Vulcan Formation|65078|5|Briefly described|p35|Triassic|Triassic|Includes a clastic "basal transgressive sand" in both Lower Vulcan and Upper Vulcan Formations. Geological province: Vulcan Sub-basin.||||||05-MAY-09
19148|Vulcan Formation|68135|5|Briefly described|p51 fig 2a|Early Cretaceous|Middle Jurassic|Browse Basin.||||Overlies Montara Formation.||15-SEP-17
19148|Vulcan Formation|69452|5|Briefly described|p36:15|Early Cretaceous|Jurassic|Bonaparte Basin.||Swan Group.||||12-JUL-16
19148|Vulcan Formation|70061|5|Briefly described|Regional geology; p6, p10, p12-13, p17|Late Jurassic|Middle Jurassic|See also Vulcan: p1-3. Gas- and oil-prone source rocks produce all produced oils in the Vulcan Sub-basin. Forms a widespread, competent seal across the Vulcan Sub-basin. Potential gas reservoir in Vulcan Sub-basin.|||||Marine sediments including mudstones and submarine fan sandstones.|12-JUL-16
19148|Vulcan Formation|70064|5|Briefly described|Regional p4-8, p10. Central: p1-2|Valanginian|Callovian|See also Northern: p1-2. Yampi: p1-2. Contains organic-rich rocks with fair to moderate oil potential. Potential reservoirs in horsts and tilted fault-blocks. Is a potential regional seal.|||||Interbedded sandstones and shales.|12-JUL-16
19151|W-Fold Shale Member|22538|6|Mentioned|Fig3 P709|||Member actually spelt Mbr||||||
19151|W-Fold Shale Member|22662|6|Mentioned|21,24,30|Proterozoic|Proterozoic|Geological province: McArthur Basin.  Of the Barney Creek Formation.||||||19-DEC-06
19151|W-Fold Shale Member|22664|5|Briefly described|34,37|Paleoproterozoic|Paleoproterozoic|Of the Barney Creek Formation (Umbolooga Subgroup). In the McArthur Basin.||||||07-NOV-08
19151|W-Fold Shale Member|22853|5|Briefly described|21|Proterozoic|Proterozoic|Of the Barney Creek Formation. Overlain by HYC Pyritic Shale Member.||||||19-DEC-06
19151|W-Fold Shale Member|23902|4|Described|p1568 Fig.2|||Of the Barney Creek Formation (Umbolooga Subgroup). Overlain by the HYC Pyritic Shale Member. Overlies the Coxco Dolomite Member. Geological Province: McArthur Basin||||||
19151|W-Fold Shale Member|23910|5|Briefly described|p292 Fig. 3|||Of Barney Creek Formation.  Geological Province: McArthur Basin.||||||
19151|W-Fold Shale Member|23963|5|Briefly described|p1239 Fig.2|||Geological Province: McArthur Basin. Of the Barney Creek Formation.||||||
19151|W-Fold Shale Member|23968|6|Mentioned|p1345|||Geological Province: McArthur Basin.||||||
19151|W-Fold Shale Member|32363|6|Mentioned|p331|||||||||
19151|W-Fold Shale Member|32479|6|Mentioned|p1395|||||||||
19151|W-Fold Shale Member|32658|3|Fully described|Table 2|||See also Figs 3 and 4. Barney Ck. Fm.||||||
19151|W-Fold Shale Member|33665|6|Mentioned|p368|||See also Fig.2.||||||
19151|W-Fold Shale Member|35162|6|Mentioned|p1008|||||||||
19151|W-Fold Shale Member|35261|6|Mentioned|Fig.2|||||||||
19151|W-Fold Shale Member|38156|6|Mentioned|Fig.2|||||||||
19151|W-Fold Shale Member|38582|6|Mentioned|p218|||||||||
19151|W-Fold Shale Member|39561|6|Mentioned|Fig.3|||||||||
19151|W-Fold Shale Member|40691|6|Mentioned|Fig.4|||||||||
19151|W-Fold Shale Member|42385|4|Described|p21|||Member of Barny Creek Formation.||||||
19151|W-Fold Shale Member|42639|5|Briefly described|p28, Fig.8 p30|||Of the Barney Creek Formation.||||||19-DEC-06
19151|W-Fold Shale Member|42812|5|Briefly described|p38|||Of the Barney Creek Formation.||||||19-DEC-06
19151|W-Fold Shale Member|42935|5|Briefly described|p530|||Of the Barney Creek Formation.||||||19-DEC-06
19151|W-Fold Shale Member|43036|6|Mentioned|p52|||Of the Barney Creek Formation.||||||19-DEC-06
19151|W-Fold Shale Member|45162|5|Briefly described|p98, 99|||Type section location given, p98.||||||06-APR-18
19151|W-Fold Shale Member|60483|5|Briefly described|p7 Fig. 5|||Of Barney Creek Fm (Umbolooga Subgroup, McArthur Group). Geological Province: McArthur Basin.||||||05-OCT-07
19151|W-Fold Shale Member|62084|6|Mentioned|p941 Fig.9|||Contains HYC ore body in Fig.9. Shown as W-Fold Shale Fig.9 and W-Fold shale in text.||||Is overlain by HYC Pyritic Shale Member. Overlies Coxco Dolomite.||
19151|W-Fold Shale Member|64815|6|Mentioned|p4 Fig.2|||||Unit in Barney Creek Formation.||||
19151|W-Fold Shale Member|64817|6|Mentioned|p353 Fig.4|||||Unit in Barney Creek Formation.||||
19151|W-Fold Shale Member|65228|5|Briefly described|p32, Fig.02.|||Appears as W-Fold Member on p32 and W Fold Shale Member in Fig.02.||Unit in Barney Creek Formation.||Overlies Teena Dolomite. Is overlain by HYC Pyritic Shale Member.|Pink and green tuffs.|
19151|W-Fold Shale Member|69430|4|Described|p15:3, 18, 38|Statherian|Statherian|Southern McArthur Basin. Appears as W-Fold shale on 15:35.||Barney Creek Formation.||Is overlain by HYC Pyritic Shale Member.|Green and red dolomitic siltstone and shale, and green vitric tuff. Much of the siltstone appears to have undergone K-metasomatism.|12-JUL-16
19151|W-Fold Shale Member|69673|4|Described|p16 fig 13|||Batten Fault Zone||Barney Creek Formation||Overlain by HYC Pyritic Shale Member|Green and red dolomitic siltstone and shale and green vitric tuff.|
19151|W-Fold Shale Member|72248|5|Briefly described|p147,149|||Of McArthur Basin.||Unit of Barney Creek Formation.||||
19151|W-Fold Shale Member|72718|6|Mentioned|p7|||Southern McArthur Basin. Batten Fault Zone.||Barney Creek Formation?, Umbolooga Sub-group, McArthur Group||Underlain by Coxco Dolostone Member. Overlain by HYC Pyritic Shale Member. Equivalent to Cooley Dolostone Member.||
19212|Waite Formation|9199|5|Briefly described|Map legend|||Greenish and grey siltstone and mudstone; chalcedony in upper part.||||||
19212|Waite Formation|9394|5|Briefly described|Map Legend|Pliocene|Miocene|Siltstone, claystone, limestone (commonly silicified), sandstone.||||||
19212|Waite Formation|9694|5|Briefly described|Map Legend|Early Pliocene|Late Miocene|Chalcedonic limestone, red-brown sandstone, silty sandstone, clayey sandstone and sandy claystone.||||||
19212|Waite Formation|23844|6|Mentioned|p40|Cenozoic|Cenozoic|Chalcedonic limestone, sandstone, mudstone and sandy conglomerate. Equivalent to Mount Bleechmore Granulite on ALCOOTA||||||19-NOV-08
19212|Waite Formation|29673|6|Mentioned|p360|||||||||
19212|Waite Formation|30055|6|Mentioned|p153|||||||||
19212|Waite Formation|30582|6|Mentioned|p9|||Diprotodontid remains||||||
19212|Waite Formation|30638|6|Mentioned|p232|||Upper Miocene or Lower Pliocene||||||
19212|Waite Formation|33103|6|Mentioned|p15|||||||||
19212|Waite Formation|33104|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
19212|Waite Formation|34996|6|Mentioned|p145|||||||||
19212|Waite Formation|36213|6|Mentioned|p89|||||||||
19212|Waite Formation|38371|6|Mentioned|p666|||||||||
19212|Waite Formation|39087|6|Mentioned|p16|||||||||
19212|Waite Formation|39610|4|Described|p8|||||||||
19212|Waite Formation|39898|5|Briefly described|Map legend|Tertiary|Tertiary|Greenish-grey siltstone, chalcedony and limestone.||||||14-FEB-06
19212|Waite Formation|40538|5|Briefly described|Map legend|early Pliocene|late Miocene|Chalcedonic limestone, grey; rare sandy mudstone.||||||15-NOV-05
19212|Waite Formation|40906|6|Mentioned|p30|||||||||
19212|Waite Formation|41537|6|Mentioned|Fig.2|||||||||
19212|Waite Formation|42375|5|Briefly described|Table 1 P11|||In the Waite Basin.||||||14-DEC-06
19212|Waite Formation|42420|6|Mentioned|p256|late Miocene||||||||
19212|Waite Formation|42457|6|Mentioned|p171|||||||||
19212|Waite Formation|42504|6|Mentioned|Table 1 P4|||||||||
19212|Waite Formation|42562|6|Mentioned|p95|||||||||
19212|Waite Formation|42776|5|Briefly described|p299|||||||||
19212|Waite Formation|43225|5|Briefly described|Map Legend||Tertiary|||||||
19212|Waite Formation|43503|5|Briefly described|45|||||||||
19212|Waite Formation|43565|3|Fully described|p422,431-440|Early Pliocene|Late Miocene|||||||
19212|Waite Formation|43748|4|Described|p8,19, Tb 1, p11,15,17|Early Pliocene|Late Miocene|Waite Basin. Includes vertebrate fossil assemblage. Middle unit within informal 'Alcoota beds' succession. 40m crops out. Full thickness not known. Interbedded chalcedonic, calcarenitic limestone, sandstone, siltstone and minor sandy conglomerate.|||||Interbedded chalcedonic, calcarenitic limestone, sandstone, siltstone and minor sandy conglomerate.|19-DEC-11
19212|Waite Formation|44133|5|Briefly described|p190 Fig. 10.30|Early Pliocene|Late Miocene|Geological Province: Waite Basin.||||||
19212|Waite Formation|44223|14|Not recorded|Fig.2|||Correlation of fauna.||||||
19212|Waite Formation|44227|14|Not recorded|p.59,74,91|Early Pliocene|Late Miocene|Alcoota fauna in early Pliocene or late Miocene. Diprotodontids. (F53-10).||||||
19212|Waite Formation|44238|14|Not recorded|Fig.3|Pliocene|Miocene|||||||
19212|Waite Formation|45028|2|Defined|p10-12|Pliocene|Miocene|See also Fig.2,4, p1,8,13-17,22,45,108,125,139,149,161,162,175,176,187. late Miocene or early Pliocene. (F53-10).||||||
19212|Waite Formation|45041|5|Briefly described|p118|||Mid Tertiary||||||
19212|Waite Formation|45128|6|Mentioned|p40|||||||||
19212|Waite Formation|46800|6|Mentioned|p109|||||||||
19212|Waite Formation|60547|5|Briefly described|Map Legend|Tertiary|Tertiary|Greenish and grey siltstone and mudstone; chalcedony in upper part.||||||
19212|Waite Formation|60551|5|Briefly described|Map Legend|Pliocene|Miocene|Geological Province: Waite Basin. Chalcedonic limestone.||||||
19212|Waite Formation|60668|5|Briefly described|Fig. 22a|||Chalcedonic limestone, sandstone, mudstone and conglomerate.||||||
19212|Waite Formation|60703|5|Briefly described|p704 Fig. 2, p725 Fig.18|Pliocene|Late Miocene|Geological Province: Waite Basin.||||||12-APR-05
19212|Waite Formation|61155|5|Briefly described|p5, p16|Late Miocene|Early Miocene|Lacustrine siltstones and chalcedonic limestones of central Australia. Age: >10Ma. Thickness: 20m. Geological Province: Hale, Ti-Tree and Waite  Basins.||||||07-OCT-15
19212|Waite Formation|61388|5|Briefly described|Map Legend|Cenozoic|Cenozoic|Chalcedonic limestone, massive chalcedony.||||||19-NOV-08
19212|Waite Formation|61404|5|Briefly described|Map legend|Neogene|Paleogene|Limestone: chalcedonic; rare quartzic mudstone. Geological Province: southern Georgina Basin.||||||07-NOV-08
19212|Waite Formation|62082|5|Briefly described|p19, p52|Pliocene|Miocene|Forms caps on mesas where it is equivalent to Austral Downs Limestone and chert; often associated with duricrust. See also p53.||||||07-FEB-11
19212|Waite Formation|64068|3|Fully described|p80, 79, p42, p19|Pliocene|Miocene|Gastropods and vertebrates fossils. Overlies Cenozoic ferricrete. Is overlain by Quaternary alluvium. Lower part correlated with Poodyea Formation. Correlations: Austral Downs Limestone, Brunette Limestone, Arltunga beds.|||||Lacustrine green siltstone below fluviatile red siltstone, sandstone and conglomeratic sandstone, capped by pedogenic chalcedonic limestone.|04-APR-12
19212|Waite Formation|65194|5|Briefly described|p53, p71-72, p74|Early Pliocene|Late Miocene|Waite Basin. Equivalents occur in Ti-Tree Basin which coarsen upwards, representing a change from lacustrine to fluvial conditions; overlain by undifferentiated Cenozoic alluvial sediments.||||||08-APR-16
19212|Waite Formation|65341|5|Briefly described|p2 Fig.2, p5, p19.|Cenozoic|Cenozoic|Waite Basin. Lacustrine and fluvial deposition. Outcrops as isolated low hills and in palaeochannels. Locally contains a gastropod and vertebrate fossil fauna indicating Late Miocene or Early Pliocene age.|||||Chalcedony, chalcedonic limestone, overlying lacustrine siltstone, fluviatile siltstone, sandstone and conglomerate.|
19212|Waite Formation|66131|6|Mentioned|p242 Fig.2|Miocene|Miocene|Middle to Late Miocene in age (from Fig.2 - stratigraphic correlation chart).||||||
19212|Waite Formation|69458|5|Briefly described|p42:7-13|||Waite Basin. Forms the hard resistant summit caps of many low plateaux and mesas. From lacustrine to fluvial deposits. Contains vertebrate fossils at the Alcoota fossil site (described).||Alcoota beds.||Unconformably overlies Tug Sandstone Member (Hale Formation).|Lacustrine green-grey siltstone, followed by fluvial red siltstone, sandstone and conglomeratic sandstone, capped by pedogenic cream or white, chalcedonic calcarenitic limestone.|12-JUL-16
19212|Waite Formation|72515|5|Briefly described|Map Legend|Cenozoic|Cenozoic|Jervois Range Special Map Sheet. Waite Basin.||Alcoota beds|||Calcedonic limestone, calcite veins.|05-JUL-22
19212|Waite Formation|72516|3|Fully described|p11, p98|Pliocene|Miocene|Waite Basin. Type section occurs 6km south of Alcoota homestead. Intersected in drillhole BMR Alcoota 3. Outcrops as low plateaus and mesas peripheral to the margins of the Waite Basin on ALCOOTA and ALICE SPRINGS map sheets; equivalents are interpreted on HUCKITTA. Maximum thickness is >3m in the mapped area, 19-130m elsewhere. Deposited in a lacustrine or fluvial environment. Hosts late Miocene to early Pliocene verterbrate fossils. Interpreted to be an age correlative of the Austral Downs Limestone, Brunette Limestone and the Arltunga beds. Equivalents are interpreted in southern Huckitta.||Alcoota beds||Unconformably overlies the Denara Orthogneiss.|Chalcedonic limestone, calcite veins; recessive, lacustrine, green siltstone. Fluvial red silstone, sandstone, conglomeratic sandstone.|09-JUN-21
19228|Walford Dolomite|22453|6|Mentioned|p 12|||In the Mount Isa Basin.||||||14-DEC-06
19228|Walford Dolomite|22673|6|Mentioned|64,65,66|||||||||
19228|Walford Dolomite|22680|6|Mentioned|84,85|||Geological: province Mount Isa Basin. Of Fickling Group.||||||14-DEC-06
19228|Walford Dolomite|23031|6|Mentioned|27|||Of the Fickling Group.||||||21-SEP-06
19228|Walford Dolomite|23065|6|Mentioned|16|||Geological province: Lawn Hill Subprovince. Of the Fickling Group. Underlain by Fish River Formation.||||||14-DEC-06
19228|Walford Dolomite|23393|5|Briefly described|p20|Paleoproterozoic|Paleoproterozoic|Of Fickling Group.||||||07-NOV-08
19228|Walford Dolomite|23396|5|Briefly described|p407 Fig.2|||Of Fickling Group.||||||21-SEP-06
19228|Walford Dolomite|23398|4|Described|p445|Statherian|Statherian|Age: 1649+/-7Ma.||||||21-SEP-06
19228|Walford Dolomite|23406|4|Described|p611, p609 Fig. 9|Statherian|Statherian|Of Fickling Group. Age: 1649+/-7Ma. Geological province: Murphy Inlier. Included in the Loretta Supersequence.  Lithological details included in Fig. 9.||||||16-JUN-09
19228|Walford Dolomite|23466|5|Briefly described|p269|||||||||
19228|Walford Dolomite|24308|5|Briefly described|p987 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of the Fickling Group.   Geological Province:  Mount Isa Superbasin||||||07-NOV-08
19228|Walford Dolomite|24432|4|Described|p565 Fig.2, p566 Fig.5|Statherian|Statherian|Age: <1649+/-7 Ma. Overlain by Mount Les Siltstone. Geological Province: Lawn Hill Platform.||||||
19228|Walford Dolomite|35640|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
19228|Walford Dolomite|36012|3|Fully described|Table 3|||See also p16.||||||21-SEP-06
19228|Walford Dolomite|36217|6|Mentioned|p206|||Published by Grimes and others 1979. Definition approved by Qld SNC.||||||21-SEP-06
19228|Walford Dolomite|36439|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
19228|Walford Dolomite|36442|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
19228|Walford Dolomite|38237|6|Mentioned|p128|||||||||
19228|Walford Dolomite|38348|6|Mentioned|p11|||||||||
19228|Walford Dolomite|38584|4|Described|p17|||||||||
19228|Walford Dolomite|39445|5|Briefly described|Table 2|||See also p39.||||||21-SEP-06
19228|Walford Dolomite|39497|6|Mentioned|Fig.4|||||||||
19228|Walford Dolomite|39685|6|Mentioned|p407|||||||||
19228|Walford Dolomite|39925|6|Mentioned|Fig.9|||||||||
19228|Walford Dolomite|39944|6|Mentioned|Fig.5|||||||||
19228|Walford Dolomite|41721|4|Described|p28|||||||||
19228|Walford Dolomite|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
19228|Walford Dolomite|43010|5|Briefly described|Fig.6||Mesoproterozoic|Of Fickling Group. Of "Mid Proterozoic" age.||||||21-SEP-06
19228|Walford Dolomite|45162|6|Mentioned|p146|||||||||
19228|Walford Dolomite|45166|5|Briefly described|p30|||||||||
19228|Walford Dolomite|49001|2|Defined|p9|Carpentarian|Carpentarian|||||||
19228|Walford Dolomite|60558|5|Briefly described|p5 Fig. 4|||Of Fickling Group. Includes Basal Member. Overlain by Mount Les Siltstone, underlain by Fish River Formation.||||||
19228|Walford Dolomite|61936|5|Briefly described|p194 Fig. 6|Paleoproterozoic|Paleoproterozoic|Age: 1649+/-7Ma. Geological Province: Lawn Hill Platform, Western Fold Belt, Mount Isa Inlier, Isa Superbasin.||||||07-NOV-08
19228|Walford Dolomite|63111|5|Briefly described|p1164 Tb. 1, p1163 Fig. 3|Statherian|Statherian|Of Loretta Supersequence. Age: 1647+/-4Ma and 1649+/-7Ma. Geological Province: Isa Superbasin. Laminated fine-grained sandstone and siltstones, peloid-dolograinstones, dolomudstone and carbonates.||||||07-FEB-11
19228|Walford Dolomite|63113|5|Briefly described|p1211, p1216, p1225-1226; Figs.2,13.  |||Minerals associated with residual hydrocarbons were predominantly pyrite and elemental (?native) Zn, Cu and Ag; native Pb in veinlets and native Ni dispersed throughout the organic matrix. Appears as Walford Ck. Dolomite in Fig.13. Part of Loretta supersequence. Source of hydrocarbons in this unit was probably Mount Les Siltstone.||Of the Loretta supersequence||Is overlain by Mount Les Siltstone.||
19228|Walford Dolomite|63866|5|Briefly described|p56|Statherian|Statherian|Isa Superbasin.|1649 +/- 7 Ma (depositional age)|||Equivalent to the Loretta Supersequence.||
19228|Walford Dolomite|65228|5|Briefly described|p26, Fig.04.|Statherian|Statherian|Part of Loretta Supersequence.|1649 +/- 7 Ma (SHRIMP).|||||
19228|Walford Dolomite|65337|6|Mentioned|p30, p36.|||||Unit in Fickling Group.||||
19228|Walford Dolomite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Camooweal-Murphy Domain, Mount Isa Inlier. Isa Superbasin.|1649 +/- 7 Ma (maximum depositional age).|Fickling Group.|||Blocky grey oolitic, stromatolitic and intraclastic dolomite; minor dolomitic sandstone and shale.|
19228|Walford Dolomite|69591|5|Briefly described|p42, p43 Fig.2.31, p55|||Camooweal-Murphy Domain, Isa Superbasin. Part of Loretta Supersequence. Peritidal deposits.|1649 +/- 7 Ma (MDA: Page et al., 2000).|Fickling Group.|||Blocky grey oolitic, stromatolitic and intraclastic dolomite; minor dolomitic sandstone and shale.|
19228|Walford Dolomite|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1649+/-7 Ma (crystallisation: U-Pb zircon SHRIMP)||||Tuff.|
19228|Walford Dolomite|72526|5|Briefly described|p8 Fig.1.3, p20.|Statherian|Statherian|Shown as being located in the central and west of the South Nicholson Basin. Age given as U-Pb zircon sedimentary depositional age.|1649 +/-7 Ma|Fickling Group||Overlies Fish River Formation and underlies Mount Les Siltstone.||
19228|Walford Dolomite|72912|5|Briefly described|p5 Fig.3, p33 Fig.12.|Statherian|Statherian|Located in the West and Central of the South Nicholson Basin. U-Pb zircon sedimentary depositional age given.|1644 +/- 7 Ma|Fickling Group||Overlies Fish River Formation and underlies Mount Les Siltstone. Partially laterally equivalent with Bullrush Conglomerate and Shady Bore Quartzite.|Includes dolomitic siltstone.|
19228|Walford Dolomite|72913|5|Briefly described|p7 Fig.2.|Paleoproterozoic|Paleoproterozoic|Shown as being in the central part of the Isa Superbasin. See also Walford Dolostone, discussed in text.|1649 +/- 7 Ma|Fickling Group||Overlies Fish River Formation and underlies Mount Les Siltstone.|Includes dolomitic siltstone.|
19228|Walford Dolomite|73042|6|Mentioned|p4, p14, p17|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin region, Isa Superbasin. Geochronology is a U-Pb zircon sedimentary depositional age (?maximum depositional age).|1649 +/- 7 Ma|Fickling Group||Underlain by Fish River Formation. Conformably overlain by Mount Les Siltstone.||
19323|Wallumbilla Formation|9528|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Dark purplish grey to white, fine to medium lithic sandstone, feldspathic sandstone.||||||
19323|Wallumbilla Formation|12597|4|Described|p492 Tb.1, p497, p498, p499-500|Albian|Aptian|Eromanga Basin. Division into the two Members is not possible in the NW, where the sequence is more uniform.|||Includes Doncaster and Coreena Members.||Marine, largely argillaceous sequence with common mollusc, gastropod, scaphopod and belemnites fossils.|
19323|Wallumbilla Formation|13497|5|Briefly described|p115 fig 6.33, p138 fig 8.17|Early Cretaceous|Early Cretaceous|Eromanga Basin. See also p144 fig 9.2, p145, p146, p148-p151.||Marree Subgroup||Overlies the Cadna-owie Formation. Overlain by the Toolebuc Formation.||
19323|Wallumbilla Formation|13516|5|Briefly described|p167 fig 10, p169 fig 11, p171 fig 12|Early Cretaceous|Early Cretaceous|In Eromanga Basin.|||Includes Doncaster and Coreena Members|||
19323|Wallumbilla Formation|22464|5|Briefly described|p9||Early Cretaceous|Eromanga Basin. Overlain by Toolebuc Formation.||||||18-DEC-06
19323|Wallumbilla Formation|22744|5|Briefly described|Fig1, P12, Table4||Cretaceous|||||||
19323|Wallumbilla Formation|22747|6|Mentioned|p15||Mesozoic|||||||
19323|Wallumbilla Formation|22757|6|Mentioned|Table6,p11||Early Cretaceous|In the Surat Basin.||||||18-DEC-06
19323|Wallumbilla Formation|22857|4|Described|p296-7 Tb.22.1, p544 App.1 Tb.A1.12|Albian|Aptian|Of the Rolling Downs Group. Sequence of mudstone and siltstone. Contains the Coreena Member. Max. thickness: 600m. Geological Province: Surat and Eromanga Basins. See also p312-3 Fig. 22.6, p314-5, p544 App.1 Tb.A1.12.||||||
19323|Wallumbilla Formation|22865|4|Described|p314,Table22.1p296-7|Albian|Aptian|||||||
19323|Wallumbilla Formation|22883|5|Briefly described|P31, Fig2||Early Cretaceous|Overlying unit is Toolebuc Formation, underlying unit is Cadna-owie Formation||||||
19323|Wallumbilla Formation|22912|5|Briefly described|33|||Geological province: Eromanga Basin.||||||18-DEC-06
19323|Wallumbilla Formation|23031|5|Briefly described|31|||||||||
19323|Wallumbilla Formation|23050|5|Briefly described|p 82 Fig.17|Early Cretaceous|Early Cretaceous|Of Surat Basin.||||||18-DEC-06
19323|Wallumbilla Formation|23056|6|Mentioned|9|||Geol Province Eromanga Basin||||||
19323|Wallumbilla Formation|23065|5|Briefly described|18|||Geological  province: Carpentaria Basin. Of the Rolling Downs Group.||||||18-DEC-06
19323|Wallumbilla Formation|23071|6|Mentioned|p761|||||||||
19323|Wallumbilla Formation|23154|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Geological Province - Eromanga Basin.  Of the Marree Subgroup (Neales River Group).||||||18-DEC-06
19323|Wallumbilla Formation|23155|4|Described|p32|Early Cretaceous|Early Cretaceous|The unit is laterally equivalent to the Bulldog Shale and it is limited to the northern part of STRZELECKI.  Age Aptian-Albian.||||||
19323|Wallumbilla Formation|23183|6|Mentioned|p222||Aptian|||||||
19323|Wallumbilla Formation|23220|5|Briefly described|p16||Mesozoic|Of the Rolling Downs Group.||||||18-DEC-06
19323|Wallumbilla Formation|23224|5|Briefly described|p3|||Hosts the Doncaster Member which hosts the Opal Deposits. Of Rolling Downs Group. In the Great Australian Basin.||||||01-FEB-07
19323|Wallumbilla Formation|23291|4|Described|p80 Tb. 3.6|Early Cretaceous|Early Cretaceous|Age: early Cretaceous. Conformably overlies Coffin Hill Member. Geological Province: Georgetown Region.||||||08-JUL-15
19323|Wallumbilla Formation|23375|4|Described|Fig2 p265|Albian|Barremian|Laterally equivalent to Bulldog Shale. of Eromanga Basin.||||||
19323|Wallumbilla Formation|23393|5|Briefly described|p24|Early Cretaceous|Early Cretaceous|Of Rolling Downs Group.||||||
19323|Wallumbilla Formation|23425|4|Described|Table 9.7 p394|Aptian|Aptian|+ Plate 9.2 + p378. Of Rolling Downs Group. Conformably overlain by Toolebuc Formation; underlain by Gilbert River Formation. Geological Province Carpentaria Basin. Max. thickness 500 m.||||||18-DEC-06
19323|Wallumbilla Formation|23430|5|Briefly described|p455|||Eromanga Basin Province.||||||
19323|Wallumbilla Formation|23496|5|Briefly described|Table 4, p59|Albian|Aptian|of Rolling Downs Group. Previously Blackdown Formation (Laing and Power 1959), then Wilgunya Subgroup (Grimes & Whittaker 1977) then of Smart and Others 1972/1980.||||||01-FEB-07
19323|Wallumbilla Formation|23499|5|Briefly described|map legend|Early Cretaceous|Early Cretaceous|In the Eromanga Basin.||||||18-DEC-06
19323|Wallumbilla Formation|23510|5|Briefly described|Map Legend||Early Cretaceous|Of the Rolling Downs Group.||||||18-DEC-06
19323|Wallumbilla Formation|23518|5|Briefly described|p13|Mesozoic|Mesozoic|Of Rolling Downs Group.  Geological Province: Carpentaria Basin.||||||
19323|Wallumbilla Formation|23713|6|Mentioned|p39|||||||||
19323|Wallumbilla Formation|23818|6|Mentioned|p141 Fig.65|||Geological Province: Great Artesian Basin. Of the Wilunga Sub-Group.||||||
19323|Wallumbilla Formation|23883|5|Briefly described|p129 Fig. 11.2|Cretaceous|Cretaceous|Of Rolling Downs Group.  Contains the Coreena and Doncaster Members.  Geological Province: Great Australian Superbasin.||||||
19323|Wallumbilla Formation|23911|5|Briefly described|p90 Fig. 4|Cretaceous|Cretaceous|Geological Province: Eromanga Basin.  Of the Rolling Downs Group.||||||
19323|Wallumbilla Formation|23982|5|Briefly described|p35 Fig.7|Cretaceous|Cretaceous|Includes the Coreena and Doncaster Members. Geological Province: Great Artesian Basin.||||||
19323|Wallumbilla Formation|23986|5|Briefly described|p71|||||||||
19323|Wallumbilla Formation|24048|5|Briefly described|p76|||||||||
19323|Wallumbilla Formation|24068|4|Described|p270 Table 2|Early Cretaceous|Early Cretaceous|Geological Province: Surat Basin.  Maximum thickness: 310m.||||||
19323|Wallumbilla Formation|24073|5|Briefly described|p378 Table 2|Early Cretaceous|Early Cretaceous|Supersedes Balckdown Formation.  Of Rolling Downs Group. Maximum thickness: 200m.  Geological Province: Carpentaria Basin.||||||
19323|Wallumbilla Formation|24085|5|Briefly described|Not recorded|Albian|Aptian|Contains Doncaster Member. Geological Province: Eromanga Basin||||||16-MAR-05
19323|Wallumbilla Formation|24092|5|Briefly described|p5|Cretaceous|Jurassic|Geological Province: Great Artesian Basin.||||||
19323|Wallumbilla Formation|24175|5|Briefly described|p17 Fig. 3|Albian|Aptian|Geological Province: Eromanga Basin.||||||
19323|Wallumbilla Formation|24204|5|Briefly described|p263 Fig.4, p267, p282 Fig.21|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||
19323|Wallumbilla Formation|24210|5|Briefly described|p133 Fig. 2|Early Cretaceous|Early Cretaceous|Of the Marree Subgroup?  Geological Province: Eromanga Basin.||||||
19323|Wallumbilla Formation|24243|5|Briefly described|p3 Fig.2|Cretaceous|Cretaceous|Of Rolling Downs Group.||||||
19323|Wallumbilla Formation|24251|5|Briefly described|p234 Fig.1, p245|Albian|Albian|Overlying Unit: Toolebuc Formation. Geological Province: Eromanga Basin||||||
19323|Wallumbilla Formation|29387|6|Mentioned|Table 5|||||||||
19323|Wallumbilla Formation|29393|6|Mentioned|Table 4|||Cretaceous.||||||
19323|Wallumbilla Formation|29591|6|Mentioned|p71|||||||||
19323|Wallumbilla Formation|29651|6|Mentioned|p25|||||||||
19323|Wallumbilla Formation|29721|6|Mentioned|Table 246|||||||||
19323|Wallumbilla Formation|30019|6|Mentioned|p2|||||||||
19323|Wallumbilla Formation|30020|4|Described|p29|||||||||
19323|Wallumbilla Formation|30021|6|Mentioned|p89|||||||||
19323|Wallumbilla Formation|30022|6|Mentioned|p32|||||||||
19323|Wallumbilla Formation|30024|6|Mentioned|p331|||||||||
19323|Wallumbilla Formation|30042|4|Described|p4|||? glauconite.||||||
19323|Wallumbilla Formation|30095|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|30102|6|Mentioned|Table 4|Cretaceous|Jurassic|See also P17.||||||
19323|Wallumbilla Formation|30103|5|Briefly described|p9|||Table 3 on p9.||||||18-DEC-06
19323|Wallumbilla Formation|30104|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|30443|6|Mentioned|p2|||See also P4. Aptian age||||||
19323|Wallumbilla Formation|30446|6|Mentioned|p39|||||||||
19323|Wallumbilla Formation|30458|6|Mentioned|p7|||Cretaceous age||||||
19323|Wallumbilla Formation|30508|6|Mentioned|p92|||Stratigraphic drilling||||||
19323|Wallumbilla Formation|30584|4|Described|Table 1|||||||||
19323|Wallumbilla Formation|30585|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|30587|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|30691|4|Described|Table 4|||Lower-Upper Cretaceous age. Of Rolling Downs Group||||||
19323|Wallumbilla Formation|30692|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|30694|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|Lower Cretaceous age||||||
19323|Wallumbilla Formation|30695|4|Described|Table 4|||Lower Cretaceous age.||||||17-SEP-08
19323|Wallumbilla Formation|30696|4|Described|Table 4|||Aptian-Albian age||||||
19323|Wallumbilla Formation|30698|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|30700|6|Mentioned|p22|||Lower Cretaceous age. Map||||||
19323|Wallumbilla Formation|30701|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|30702|6|Mentioned|Table 1|||Stratigraphic table||||||
19323|Wallumbilla Formation|30804|6|Mentioned|Table 2|||||||||
19323|Wallumbilla Formation|30853|5|Briefly described|Table 3|||Aptian to Lower Albian age||||||
19323|Wallumbilla Formation|30854|4|Described|Table 4|||Lower Cretaceous age||||||
19323|Wallumbilla Formation|30855|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|Unit in Rolling Downs Group||||||
19323|Wallumbilla Formation|30856|4|Described|Table 3|||Lower Cretaceous age.||||||
19323|Wallumbilla Formation|30857|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|30914|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
19323|Wallumbilla Formation|30915|6|Mentioned|Table|||Shown on stratigraphic table||||||
19323|Wallumbilla Formation|31097|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|31098|5|Briefly described|Table 1|||L. Cretaceous||||||
19323|Wallumbilla Formation|31116|4|Described|p43|||See also Table 2. Cretaceous||||||
19323|Wallumbilla Formation|31120|6|Mentioned|Table|||||||||
19323|Wallumbilla Formation|31121|6|Mentioned|Table 1|||||||||
19323|Wallumbilla Formation|31144|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|31145|5|Briefly described|Table 1|||L. Cretaceous||||||
19323|Wallumbilla Formation|31164|5|Briefly described|p8|||Aptian - Lower Albian, See also P10.||||||
19323|Wallumbilla Formation|31165|6|Mentioned|Table 11|||||||||
19323|Wallumbilla Formation|31168|6|Mentioned|p10|||||||||
19323|Wallumbilla Formation|31208|6|Mentioned|Fig 36|||See also Table 1||||||
19323|Wallumbilla Formation|31209|4|Described|p159|||||||||
19323|Wallumbilla Formation|31376|6|Mentioned|p4|||||||||
19323|Wallumbilla Formation|31422|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Of the Rolling Downs Group.  Mudstone, minor limestone, glauconitic sandstone.||||||02-DEC-04
19323|Wallumbilla Formation|31425|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|31430|5|Briefly described|Table 1|||L.Cretaceous||||||
19323|Wallumbilla Formation|31431|5|Briefly described|Table 3|||L.Cretaceous||||||
19323|Wallumbilla Formation|31432|4|Described|Table 1|||L.Cretaceous||||||
19323|Wallumbilla Formation|31433|5|Briefly described|p6|||L.Cretaceous||||||
19323|Wallumbilla Formation|31434|3|Fully described|Table 1|||See also p8. L.Cretaceous.||||||17-SEP-08
19323|Wallumbilla Formation|31436|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|31437|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|31438|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|31440|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|31441|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|31443|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|31553|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|31832|6|Mentioned|Table 6|||||||||
19323|Wallumbilla Formation|32136|6|Mentioned|p3|||Continuously cored composite section||||||
19323|Wallumbilla Formation|32193|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|32274|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|32275|4|Described|p8|||||||||
19323|Wallumbilla Formation|32276|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|32313|6|Mentioned|p165|||||||||
19323|Wallumbilla Formation|32314|6|Mentioned|Fig. 4|||||||||
19323|Wallumbilla Formation|32392|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|32393|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|32395|6|Mentioned|p6|||Stratigraphic table||||||
19323|Wallumbilla Formation|32396|6|Mentioned|p8|||Stratigraphic table||||||
19323|Wallumbilla Formation|32490|6|Mentioned|p9|||Crops out W of Buchanan sheet||||||
19323|Wallumbilla Formation|32553|4|Described|p38|||||||||
19323|Wallumbilla Formation|32705|6|Mentioned|p188|||||||||
19323|Wallumbilla Formation|32796|6|Mentioned|p302|||||||||
19323|Wallumbilla Formation|32797|4|Described|Table 4|||L.Cret.||||||
19323|Wallumbilla Formation|33016|6|Mentioned|p1|||On table||||||
19323|Wallumbilla Formation|33017|6|Mentioned|p5|||||||||
19323|Wallumbilla Formation|33067|4|Described|Table 1|Early Cretaceous|Early Cretaceous|Of the Rolling Downs Group.  Mudstone, siltstone,minor sandstone.||||||07-JUL-04
19323|Wallumbilla Formation|33069|4|Described|p7|||L.Cret.||||||
19323|Wallumbilla Formation|33070|4|Described|Table 2|||L.Cret.||||||
19323|Wallumbilla Formation|33071|4|Described|p2|||L.Cret.||||||
19323|Wallumbilla Formation|33072|4|Described|Table 1|||L.Cret.||||||
19323|Wallumbilla Formation|33073|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33075|6|Mentioned|p445|||||||||
19323|Wallumbilla Formation|33078|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33079|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33080|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33082|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33083|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33086|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower to Upper Cretaceous||||||
19323|Wallumbilla Formation|33087|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33088|4|Described|Table 3|||||||||
19323|Wallumbilla Formation|33089|4|Described|Table 2|||L.Cret.||||||
19323|Wallumbilla Formation|33090|4|Described|Table 4|||L.Cret.||||||
19323|Wallumbilla Formation|33091|5|Briefly described|p9|||Stratigraphy||||||
19323|Wallumbilla Formation|33092|5|Briefly described|p6|||Strat. table||||||
19323|Wallumbilla Formation|33094|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33095|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33096|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33150|4|Described|p9|||L.Cret.||||||
19323|Wallumbilla Formation|33151|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33165|6|Mentioned|Chart|||Correlatin chart only||||||
19323|Wallumbilla Formation|33175|6|Mentioned|p280|||||||||
19323|Wallumbilla Formation|33176|5|Briefly described|p172|||||||||
19323|Wallumbilla Formation|33177|6|Mentioned|p12|||||||||
19323|Wallumbilla Formation|33178|6|Mentioned|p11|||||||||
19323|Wallumbilla Formation|33179|4|Described|Table 2|||||||||
19323|Wallumbilla Formation|33180|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33182|6|Mentioned|p190|||||||||
19323|Wallumbilla Formation|33183|6|Mentioned|p233|||||||||
19323|Wallumbilla Formation|33368|6|Mentioned|p24|||Geol.Map.||||||
19323|Wallumbilla Formation|33372|4|Described|p17|||See also p20. From QDM Aramac 1.||||||18-DEC-06
19323|Wallumbilla Formation|33414|6|Mentioned|p212-214,Tb.||Aptian|Part of Wilgunya Sub-Group..||||||
19323|Wallumbilla Formation|33448|4|Described|Table 1|||L.Cret.||||||11-JAN-10
19323|Wallumbilla Formation|33449|4|Described|Table 1|||L.Cret.||||||
19323|Wallumbilla Formation|33451|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33452|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33561|6|Mentioned|p102|||||||||
19323|Wallumbilla Formation|33638|5|Briefly described|Table 1|||||||||
19323|Wallumbilla Formation|33639|5|Briefly described|p11|||L.Cret.||||||
19323|Wallumbilla Formation|33640|4|Described|Table 2|||||||||
19323|Wallumbilla Formation|33642|1|Redefined|p148|Early Cretaceous|Early Cretaceous|Includes Doncaster, Jones Valley, Ranmoor and Coreena Members. Contains Roma and older part of Tambo fauna of Aptian and Albian (Lower Cret)||||||
19323|Wallumbilla Formation|33643|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33644|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33645|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33646|6|Mentioned|p8|||Strat. table.||||||
19323|Wallumbilla Formation|33647|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33648|6|Mentioned|p20|||||||||
19323|Wallumbilla Formation|33672|5|Briefly described|p44|||Lithology.||||||
19323|Wallumbilla Formation|33673|4|Described|p292|||||||||
19323|Wallumbilla Formation|33772|6|Mentioned|p17|||||||||
19323|Wallumbilla Formation|33773|6|Mentioned|p17|||||||||
19323|Wallumbilla Formation|33825|6|Mentioned|p10|||Correlation table||||||
19323|Wallumbilla Formation|33832|5|Briefly described|p11|||Strat. and correlation.||||||18-DEC-06
19323|Wallumbilla Formation|33900|6|Mentioned|p21|||||||||
19323|Wallumbilla Formation|33939|6|Mentioned|p412|||||||||
19323|Wallumbilla Formation|33964|4|Described|p6|||Refers Vine et al. (1967).||||||
19323|Wallumbilla Formation|34065|4|Described|p6|||L.Cret.||||||
19323|Wallumbilla Formation|34091|5|Briefly described|Table 1|||See also P4. L.Cret. Part of Rolling Downs Group.||||||
19323|Wallumbilla Formation|34174|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|34212|6|Mentioned|p2|||Cretaceous||||||
19323|Wallumbilla Formation|34217|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|34218|4|Described|Table 1|||See also Table 2. Lower Cretaceous||||||
19323|Wallumbilla Formation|34356|6|Mentioned|p13|||Lower Cretaceous.||||||
19323|Wallumbilla Formation|34485|5|Briefly described|Table 1,p10|||Lower Cretaceous||||||
19323|Wallumbilla Formation|34486|5|Briefly described|Table 1|||Lower Cretaceous. See also Table 2||||||
19323|Wallumbilla Formation|34487|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|34611|6|Mentioned|Fig.65|||Correlation chart.||||||
19323|Wallumbilla Formation|34613|4|Described|Table 4|||||||||
19323|Wallumbilla Formation|34811|4|Described|Table 1|||||||||
19323|Wallumbilla Formation|35121|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|35139|4|Described|Table.2|||||||||
19323|Wallumbilla Formation|35239|6|Mentioned|p258|||||||||
19323|Wallumbilla Formation|35253|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|35457|6|Mentioned|Fig.5|||Stratigraphic correlation||||||
19323|Wallumbilla Formation|35560|4|Described|p290|||||||||
19323|Wallumbilla Formation|35640|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|35663|6|Mentioned|Fig.2|||Subsurface correlations of the central basin rock units.||||||
19323|Wallumbilla Formation|35793|6|Mentioned|Fig.3|||||||||
19323|Wallumbilla Formation|35811|5|Briefly described|Table 3|||||||||
19323|Wallumbilla Formation|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
19323|Wallumbilla Formation|35936|6|Mentioned|p615|||||||||
19323|Wallumbilla Formation|35937|6|Mentioned|Fig.5|||||||||
19323|Wallumbilla Formation|36012|3|Fully described|Table 5|||See also p18.||||||18-DEC-06
19323|Wallumbilla Formation|36228|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|36243|6|Mentioned|Table 6A|||||||||
19323|Wallumbilla Formation|36251|4|Described|p3|||||||||
19323|Wallumbilla Formation|36570|5|Briefly described|p50|||See also p60.||||||18-DEC-06
19323|Wallumbilla Formation|36571|6|Mentioned|p101|||See also Table 4.||||||
19323|Wallumbilla Formation|36574|6|Mentioned|p602|||||||||
19323|Wallumbilla Formation|36580|6|Mentioned|Fig.2|||||||||
19323|Wallumbilla Formation|36581|6|Mentioned|p464|||||||||
19323|Wallumbilla Formation|36910|6|Mentioned|p61|||||||||
19323|Wallumbilla Formation|37117|5|Briefly described|p313|||||||||
19323|Wallumbilla Formation|37451|6|Mentioned|Table 2|||||||||
19323|Wallumbilla Formation|37597|6|Mentioned|p77|||||||||
19323|Wallumbilla Formation|37608|3|Fully described|Table 1 p316-319|||||||||
19323|Wallumbilla Formation|37995|4|Described|p66|||||||||
19323|Wallumbilla Formation|38199|5|Briefly described|p423|||Palynology||||||
19323|Wallumbilla Formation|38218|5|Briefly described|p289|||||||||
19323|Wallumbilla Formation|38226|6|Mentioned|Table 1|||||||||
19323|Wallumbilla Formation|38372|6|Mentioned|p651|||||||||
19323|Wallumbilla Formation|38373|6|Mentioned|p619|||||||||
19323|Wallumbilla Formation|38608|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
19323|Wallumbilla Formation|38779|6|Mentioned|p7|||||||||
19323|Wallumbilla Formation|38780|6|Mentioned|p17|||||||||
19323|Wallumbilla Formation|38814|6|Mentioned|Table 1|||||||||
19323|Wallumbilla Formation|39029|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Overlies Gilbert River Formation.||||||25-AUG-04
19323|Wallumbilla Formation|39070|4|Described|p364|||||||||
19323|Wallumbilla Formation|39211|5|Briefly described|Fig.3|||See also Figs 4,7,9,11-15 etc. Correlation||||||
19323|Wallumbilla Formation|39212|6|Mentioned|p18|||||||||
19323|Wallumbilla Formation|39216|6|Mentioned|p55|||||||||
19323|Wallumbilla Formation|39445|5|Briefly described|Table 11|||||||||
19323|Wallumbilla Formation|39478|6|Mentioned|Table 1|||||||||
19323|Wallumbilla Formation|39556|5|Briefly described|Map legend|Cretaceous|Cretaceous|||||||
19323|Wallumbilla Formation|39627|6|Mentioned|p269|||||||||
19323|Wallumbilla Formation|39708|6|Mentioned|p478|||||||||
19323|Wallumbilla Formation|39797|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|39799|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|39846|6|Mentioned|p44|||||||||
19323|Wallumbilla Formation|39847|5|Briefly described|p38|||||||||
19323|Wallumbilla Formation|39899|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
19323|Wallumbilla Formation|39917|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|39942|6|Mentioned|p468|||||||||
19323|Wallumbilla Formation|39943|6|Mentioned|Table 8A|||||||||
19323|Wallumbilla Formation|39988|6|Mentioned|p288|||||||||
19323|Wallumbilla Formation|39989|4|Described|p423|||||||||
19323|Wallumbilla Formation|40058|6|Mentioned|p2|||||||||
19323|Wallumbilla Formation|40121|6|Mentioned|Table 1|||||||||
19323|Wallumbilla Formation|40150|6|Mentioned|p81|||||||||
19323|Wallumbilla Formation|40199|6|Mentioned|Fig.1|||||||||
19323|Wallumbilla Formation|40218|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
19323|Wallumbilla Formation|40245|6|Mentioned|Table 2|||||||||
19323|Wallumbilla Formation|40249|6|Mentioned|p38|||Mention P41||||||
19323|Wallumbilla Formation|40250|6|Mentioned|Fig.1|||||||||
19323|Wallumbilla Formation|40452|6|Mentioned|p2|||||||||
19323|Wallumbilla Formation|40541|3|Fully described|p111|||||||||
19323|Wallumbilla Formation|40544|6|Mentioned|p159|||||||||
19323|Wallumbilla Formation|40623|5|Briefly described|p108|||||||||
19323|Wallumbilla Formation|40648|6|Mentioned|p12|||||||||
19323|Wallumbilla Formation|40659|6|Mentioned|p250|||||||||
19323|Wallumbilla Formation|40666|4|Described|p358|||||||||
19323|Wallumbilla Formation|40670|6|Mentioned|Fig.9|||||||||
19323|Wallumbilla Formation|40675|6|Mentioned|Table 8A|||||||||
19323|Wallumbilla Formation|40687|3|Fully described|p418|||||||||
19323|Wallumbilla Formation|40771|6|Mentioned|p429|||||||||
19323|Wallumbilla Formation|40801|6|Mentioned|p29|||See also P39||||||
19323|Wallumbilla Formation|40832|3|Fully described|p457|||||||||
19323|Wallumbilla Formation|40833|6|Mentioned|p468|||||||||
19323|Wallumbilla Formation|40926|6|Mentioned|p18|||||||||
19323|Wallumbilla Formation|40962|6|Mentioned|Table 1|||||||||
19323|Wallumbilla Formation|41012|5|Briefly described|p137|||||||||
19323|Wallumbilla Formation|41060|6|Mentioned|Fig.3|||Generalized stratigraphy||||||
19323|Wallumbilla Formation|41062|6|Mentioned|Fig.5|||||||||
19323|Wallumbilla Formation|41063|6|Mentioned|p40|||||||||
19323|Wallumbilla Formation|41064|6|Mentioned|p60|||||||||
19323|Wallumbilla Formation|41084|5|Briefly described|Fig.2|||||||||
19323|Wallumbilla Formation|41086|3|Fully described|p98, Fig.3|||Mentioned p101.||||||18-DEC-06
19323|Wallumbilla Formation|41087|6|Mentioned|p123|||||||||
19323|Wallumbilla Formation|41088|6|Mentioned|p141|||||||||
19323|Wallumbilla Formation|41097|6|Mentioned|p165|||||||||
19323|Wallumbilla Formation|41099|6|Mentioned|Fig.9|||||||||
19323|Wallumbilla Formation|41117|6|Mentioned|Fig.2|||||||||
19323|Wallumbilla Formation|41165|5|Briefly described|p362|||||||||
19323|Wallumbilla Formation|41175|6|Mentioned|Fig.1|||||||||
19323|Wallumbilla Formation|41176|6|Mentioned|Table 2|||||||||
19323|Wallumbilla Formation|41177|6|Mentioned|p225|||||||||
19323|Wallumbilla Formation|41178|6|Mentioned|p242|||||||||
19323|Wallumbilla Formation|41182|5|Briefly described|p289|||||||||
19323|Wallumbilla Formation|41183|6|Mentioned|p310|||||||||
19323|Wallumbilla Formation|41184|6|Mentioned|p347|||||||||
19323|Wallumbilla Formation|41186|6|Mentioned|p197|||||||||
19323|Wallumbilla Formation|41187|6|Mentioned|p227|||||||||
19323|Wallumbilla Formation|41196|6|Mentioned|Fig.1|||||||||
19323|Wallumbilla Formation|41198|6|Mentioned|Table 1|||||||||
19323|Wallumbilla Formation|41214|6|Mentioned|Fig.3|||||||||
19323|Wallumbilla Formation|41216|6|Mentioned|Fig.18|||||||||
19323|Wallumbilla Formation|41246|6|Mentioned|Map legend|Cretaceous||||||||
19323|Wallumbilla Formation|41266|6|Mentioned|Fig.3|||||||||
19323|Wallumbilla Formation|41286|6|Mentioned|p118|||||||||
19323|Wallumbilla Formation|41306|6|Mentioned|p4|||||||||
19323|Wallumbilla Formation|41307|6|Mentioned|p5|||||||||
19323|Wallumbilla Formation|41361|6|Mentioned|Fig.3|||||||||
19323|Wallumbilla Formation|41427|6|Mentioned|p84|||||||||
19323|Wallumbilla Formation|41464|6|Mentioned|Map legend|Early Cretaceous||||||||
19323|Wallumbilla Formation|41523|3|Fully described|p278|||||||||
19323|Wallumbilla Formation|41556|6|Mentioned|Map legend|Early Cretaceous||||||||
19323|Wallumbilla Formation|41568|5|Briefly described|p15|||||||||
19323|Wallumbilla Formation|41681|6|Mentioned|p11,p22|||||||||
19323|Wallumbilla Formation|41707|6|Mentioned|p164|||||||||
19323|Wallumbilla Formation|41992|4|Described|Fig.2 p183|||||||||26-APR-18
19323|Wallumbilla Formation|42007|5|Briefly described|p182|||||||||
19323|Wallumbilla Formation|42061|4|Described|p157|||See also Fig.11||||||
19323|Wallumbilla Formation|42067|5|Briefly described|p309|||See also Appendix 2||||||
19323|Wallumbilla Formation|42071|6|Mentioned|p117|||||||||
19323|Wallumbilla Formation|42084|6|Mentioned|Fig.3 P356|||||||||
19323|Wallumbilla Formation|42085|6|Mentioned|Fig.2 P374|||||||||
19323|Wallumbilla Formation|42369|5|Briefly described|Fig.10, P61|||||||||
19323|Wallumbilla Formation|42397|6|Mentioned|Fig.2 P3|||||||||
19323|Wallumbilla Formation|42429|5|Briefly described|Fig.3 P155|||||||||
19323|Wallumbilla Formation|42446|4|Described|p13|||||||||
19323|Wallumbilla Formation|42447|6|Mentioned|p16|||||||||
19323|Wallumbilla Formation|42474|5|Briefly described|p25|||||||||
19323|Wallumbilla Formation|42496|5|Briefly described|p136, Fig.3 p132|||||||||
19323|Wallumbilla Formation|42520|5|Briefly described|p6|||||||||
19323|Wallumbilla Formation|42634|6|Mentioned|Table 8 P34|||||||||
19323|Wallumbilla Formation|42637|4|Described|p10, 23|||||||||
19323|Wallumbilla Formation|42673|5|Briefly described|Fig.2, P184|||||||||
19323|Wallumbilla Formation|42746|6|Mentioned|Fig.6 P8|||||||||
19323|Wallumbilla Formation|42749|5|Briefly described|p31|||see also Fig.2 p27.||||||18-DEC-06
19323|Wallumbilla Formation|42804|5|Briefly described|p115|||||||||
19323|Wallumbilla Formation|42940|5|Briefly described|Plate 2|Mesozoic|Mesozoic|Siltstone, porcellanite, sandstone; marine fossils.  Geological province: Amadeus Basin.||||||23-JAN-08
19323|Wallumbilla Formation|42999|5|Briefly described|Table 2,p90||Early Cretaceous|||||||
19323|Wallumbilla Formation|43000|5|Briefly described|p114|||see also Fig.5,p112||||||
19323|Wallumbilla Formation|43002|5|Briefly described|Fig.2,p135|||||||||
19323|Wallumbilla Formation|43004|5|Briefly described|Table 1,p179|||||||||
19323|Wallumbilla Formation|43083|5|Briefly described|p185|Cretaceous|Cretaceous|Argillaceouis deposits.||||||17-JUN-09
19323|Wallumbilla Formation|43105|5|Briefly described|Fig.9,p15.|||||||||
19323|Wallumbilla Formation|43114|5|Briefly described|p14|||||||||
19323|Wallumbilla Formation|43122|5|Briefly described|p25|||see also Fig. 2.||||||
19323|Wallumbilla Formation|43254|5|Briefly described|map legend|Early Cretaceous|Late Jurassic|||||||
19323|Wallumbilla Formation|43285|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|||||||
19323|Wallumbilla Formation|43287|5|Briefly described|Map Legend||Early Cretaceous|||||||
19323|Wallumbilla Formation|43404|14|Not recorded|Table p11||Cretaceous|||||||
19323|Wallumbilla Formation|43564|6|Mentioned|p453||Aptian|(Late Aptian)||||||
19323|Wallumbilla Formation|43591|6|Mentioned|p40|||||||||
19323|Wallumbilla Formation|43602|4|Described|191|||In the Eromanga Basin. Of the Rolling Downs Group.||||||18-DEC-06
19323|Wallumbilla Formation|43625|6|Mentioned|p48,74|||||||||
19323|Wallumbilla Formation|43630|6|Mentioned|p69, fig.4|||||||||
19323|Wallumbilla Formation|43989|14|Not recorded|Map Legend||Early Cretaceous|||||||
19323|Wallumbilla Formation|44016|14|Not recorded|Map Legend||Early Cretaceous|||||||
19323|Wallumbilla Formation|44017|14|Not recorded|Map Legend||Early Cretaceous|||||||
19323|Wallumbilla Formation|44018|14|Not recorded|Map Legend||Early Cretaceous|||||||
19323|Wallumbilla Formation|44019|14|Not recorded|Map Legend||Early Cretaceous|||||||
19323|Wallumbilla Formation|44020|14|Not recorded|Tb.1,2||Early Cretaceous|Of Rolling Downs Group.||||||
19323|Wallumbilla Formation|44031|14|Not recorded|p3,8,9,11,12||Cretaceous|||||||
19323|Wallumbilla Formation|44034|4|Described|Tb.2,p2,5,7-10,Fig.1|||||||||
19323|Wallumbilla Formation|44042|14|Not recorded|Map Legend||Early Cretaceous|||||||
19323|Wallumbilla Formation|44082|6|Mentioned|p3,4,6,8,10-30,Tb.34||Early Cretaceous|Mentioned with respect to Qld Cretaceous fossils which are either of stratigraphic significance or are illustrative of the occurrence of a particular group.||||||
19323|Wallumbilla Formation|44091|14|Not recorded|p60,63||Cretaceous|||||||
19323|Wallumbilla Formation|44099|14|Not recorded|Map Legend||Early Cretaceous|(Rolling Downs Group)||||||
19323|Wallumbilla Formation|44112|6|Mentioned|p82|||||||||
19323|Wallumbilla Formation|44133|5|Briefly described|p104 Fig. 9.11|Cretaceous|Cretaceous|Geological Province: Eromanga Basin.||||||
19323|Wallumbilla Formation|44308|14|Not recorded|p11,|||||||||
19323|Wallumbilla Formation|44376|14|Not recorded|p3|||||||||
19323|Wallumbilla Formation|44410|14|Not recorded|Map Legend||Early Cretaceous|||||||
19323|Wallumbilla Formation|44637|14|Not recorded|p287-291||Cretaceous|||||||
19323|Wallumbilla Formation|44807|14|Not recorded|p9|||Correlated with Blackdown Formation.||||||
19323|Wallumbilla Formation|45022|6|Mentioned|p111|Albian|Aptian|||||||
19323|Wallumbilla Formation|45071|6|Mentioned|p79|||||||||
19323|Wallumbilla Formation|45110|6|Mentioned|p24|||See also Table 18.||||||
19323|Wallumbilla Formation|45132|6|Mentioned|Table 2|||See also Fig.1.||||||
19323|Wallumbilla Formation|45145|3|Fully described|Table 5|||||||||
19323|Wallumbilla Formation|45161|6|Mentioned|p67|||||||||
19323|Wallumbilla Formation|46791|4|Described|p44|||||||||
19323|Wallumbilla Formation|46881|6|Mentioned|p198|||||||||
19323|Wallumbilla Formation|46902|6|Mentioned|p36|||||||||
19323|Wallumbilla Formation|46937|6|Mentioned|Fig.10|||||||||
19323|Wallumbilla Formation|46939|6|Mentioned|Fig.2|||See also Fig.1.||||||
19323|Wallumbilla Formation|46984|6|Mentioned|Table 1|||||||||
19323|Wallumbilla Formation|47042|6|Mentioned|p171|||||||||
19323|Wallumbilla Formation|47083|5|Briefly described|p20||Mesozoic|Of Rolling Downs Group.||||||
19323|Wallumbilla Formation|48919|6|Mentioned|p71|||Cretaceous. See also P72||||||
19323|Wallumbilla Formation|48920|3|Fully described|p58|||Lower Cretaceous age||||||
19323|Wallumbilla Formation|48951|6|Mentioned|Table 1|||||||||
19323|Wallumbilla Formation|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
19323|Wallumbilla Formation|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
19323|Wallumbilla Formation|50100|5|Briefly described|p23|Cretaceous|Cretaceous|Of the Rolling Downs Group.  Geological Province: Eromanga Basin.||||||
19323|Wallumbilla Formation|50199|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|50332|5|Briefly described|p22, p78|Mesozoic|Mesozoic|Geological Province: Carpentaria Basin. Main lithologies are mudstone, calcareous shale, limestone, sandstone and siltstone.||||||07-FEB-11
19323|Wallumbilla Formation|50627|5|Briefly described|Map legend|Cretaceous|Cretaceous|Clay-rich mudstone, silty mudstone, sandy siltstone, and sandstone.||||||
19323|Wallumbilla Formation|60081|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Mudstone and quartz-poor sandstone, minor glauconitic sandstone.||||||
19323|Wallumbilla Formation|60087|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Of the Rolling Downs Group. Mudstone, minor labile and galuconitic sandstone, limestone.||||||
19323|Wallumbilla Formation|60281|5|Briefly described|p27|Early Cretaceous|Early Cretaceous|Geological Province: Clarence-Moreton Basin, Cecil Plains Sub-basin.||||||20-JAN-05
19323|Wallumbilla Formation|60331|5|Briefly described|p34 Fig.3|Albian|Aptian|Overlies Gilbert River Formation. Overlain by Toolebuc Formation. Geological Province: Eromanga Basin.||||||
19323|Wallumbilla Formation|60357|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Overlies: Coffin Hill Member (Gilbert River Formation). Mudstone and siltstone, minor sandstone. Geological Province: Carpentaria Basin.||||||20-AUG-04
19323|Wallumbilla Formation|60358|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Silty and sandy claystone, mudstone and siltstone, calcareous concretions; minor glauconitic sandstone. Geological Province: Laura Basin.||||||18-AUG-04
19323|Wallumbilla Formation|60359|5|Briefly described|Map Legend|Mesozoic|Mesozoic|Mudstone, siltstone.||||||
19323|Wallumbilla Formation|60524|5|Briefly described|p486 Fig. 1, p488|Albian|Aptian|Marine deposits; contains Viviparidae fossils.  Geological Province: Eromanga Basin.||||||
19323|Wallumbilla Formation|60717|5|Briefly described|p40 Fig. 2|Early Cretaceous|Early Cretaceous|Overlies Cadna-owie Formation. Overlain by Toolebuc Formation. Lateral to Bulldog Shale. Geological Province: Eromanga Basin.||||||31-JAN-08
19323|Wallumbilla Formation|61014|6|Mentioned|p533 Fig.2, p539. |Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Wyandra Sandstone Member. Is overlain by Allaru Mudstone.||
19323|Wallumbilla Formation|61312|4|Described|p64, p67 Fig. E5, p73-74|Early Cretaceous|Early Cretaceous|Of Rolling Downs Gp. Marine sediment sequence of mudstone and siltstone, with limestone, minor lenticular sandstone, and intraformational conglomerate. Overlies Cadna-owie Fm.; overlain by Toolebuc Fm in Qld. Thickness: 300m. Geol. Prov: Eromanga Basin.||||||
19323|Wallumbilla Formation|61377|5|Briefly described|p148 Tb. SU1|Early Cretaceous|Early Cretaceous|Of the Rolling Downs Group. Mudstone, siltstone, minor sandstone, coal, conglomerate. Overlies Pilliga Sandstone. Geological Province: Surat Basin.||||||07-FEB-11
19323|Wallumbilla Formation|61611|6|Mentioned|p265 Fig. 3|Early Cretaceous|Early Cretaceous|Geological Province: Surat Basin and Eromanga Basin.||||||13-MAR-09
19323|Wallumbilla Formation|61613|6|Mentioned|p282 Fig. 2|Early Cretaceous|Early Cretaceous|Of Maree Subgroup. Geological Province: Eromanga Basin.||||||07-FEB-11
19323|Wallumbilla Formation|61614|6|Mentioned|p290 Fig. 2|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||17-MAR-09
19323|Wallumbilla Formation|62028|5|Briefly described|p10 Fig. 1|||||||||
19323|Wallumbilla Formation|62029|5|Briefly described|p15|Cretaceous|Cretaceous|Siltstone and shale - impermeable and acts as reservoir seal. See also Fig. 4.||||||14-APR-08
19323|Wallumbilla Formation|62376|5|Briefly described|p84|Early Cretaceous|Early Cretaceous|Geological Province: Pedirka Basin.||||||09-FEB-10
19323|Wallumbilla Formation|62537|6|Mentioned|p191 Fig.2. |Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Cadna-owie Formation. Is overlain by Coorikiana Formation.||
19323|Wallumbilla Formation|62730|5|Briefly described|p352 Fig. 1|Cretaceous|Cretaceous|Geological Province: Eromanga Basin.||||||21-APR-08
19323|Wallumbilla Formation|62837|5|Briefly described|Stratigraphic columns|Early Cretaceous|Early Cretaceous|Of the Rolling Downs Group. Age: ~113-~98Ma. Geological Province: Northern Gulf of Carpentaria.||||||01-MAR-10
19323|Wallumbilla Formation|63218|6|Mentioned|p211 Fig.2. |Early Cretaceous|Early Cretaceous|Surat Basin.|||Includes Doncaster and Coreena Members.|Overlies Bungil Formation. Is overlain by Surat Siltstone.||
19323|Wallumbilla Formation|63979|1|Redefined|p48, Fig. 44|Albian|Barremian|Lower part of Wilgunya Subgp.Equates to Bulldog Shale, Coorikiana Sst.+lower part of Oodnadatta Fm in SA. Informally subdiv.into lower+upper Wallumbilla Fm.Contains Doncaster +Coreena Members.Conformable on Cadna-owie Fm. Thickness:350m.Detailed lith.||||||03-DEC-18
19323|Wallumbilla Formation|64048|5|Briefly described|p64 Tb. 2|Early Cretaceous|Early Cretaceous|Contains the Coreena Member. Geological Province: Eromanga Basin.||||||07-FEB-11
19323|Wallumbilla Formation|64197|6|Mentioned|p625 Fig.1c, p630 Figs.6,7|Cretaceous|Cretaceous|Eromanga and Surat Basins.||Unit in Marree Subgroup.||Eromanga Basin: underlies Toolebuc Formation; overlies Cadna-owie Formation. Surat Basin: underlies the Surat Siltstone, overlies the Bungil Formation.||11-DEC-15
19323|Wallumbilla Formation|64665|6|Mentioned|p62.|Cretaceous|Cretaceous|Eromanga Basin.||||||
19323|Wallumbilla Formation|64820|5|Briefly described|pS6 Fig. 4|Barremian|Albian|Of the Rolling Downs Group. Geological province: Weipa Sub-basin, Carpentaria Basin.||||||
19323|Wallumbilla Formation|64856|3|Fully described|p79, p98-101|Albian|Aptian|Named and defined in the Surat Basin by Vine et al. (1967), with the type section in Wallumbilla Creek, near Roma. Also in Eromanga Basin. Contains Doncaster and Coreena Members. Conformably overlies Bungil Formation. Age from pollen assemblages (units APK3, 4). Mudstone, siltstone, concretionary limestone, minor lenticular sandstone, conglomerate. Up to 475m thick.|| ||||29-NOV-17
19323|Wallumbilla Formation|64857|5|Briefly described|p113 Fig.3|||Overlies Bungil Formation, Surat Basin.||||||
19323|Wallumbilla Formation|64858|6|Mentioned|p181 Tb.1, p187-188|||Surat Basin.||||||30-NOV-09
19323|Wallumbilla Formation|65112|6|Mentioned|Fig 11 p324; Fig 16 p 328|Early Cretaceous|Early Cretaceous|Unit in the Surat Basin.|||Includes Doncaster and Coreena Members.|Overlies the Bungil Formation; underlies the Surat Siltstone.||22-MAR-12
19323|Wallumbilla Formation|65113|5|Briefly described|Fig 4 p340|Early Cretaceous|Early Cretaceous|Overlies the Bungil Formation, Surat Siltstone.||||||
19323|Wallumbilla Formation|65114|5|Briefly described|p385 Fig.3|Early Cretaceous||||||||
19323|Wallumbilla Formation|65116|5|Briefly described|Fig 2 p437|Early Cretaceous|Early Cretaceous|Includes Coreena Member, Doncaster Member. Underlies the Surat Siltstone, Overlies the Bungil Formation, Surat Basin.||||||
19323|Wallumbilla Formation|65119|5|Briefly described|p503, 504, fig 7-8 p514, Fig 16-19|Early Cretaceous|Early Cretaceous|Surat Basin. Marine shelf deposits of siltstone, mudstone and fine sandstone. Age: 111-117 Ma. Fission Track age: 87-109 Ma.||||||07-MAR-12
19323|Wallumbilla Formation|65238|5|Briefly described|p7 Fig. 8, p14 Fig. 17|Early Cretaceous|Early Cretaceous|Geological province: Eromanga Basin. Transgressive marine deposits.||||||
19323|Wallumbilla Formation|65384|6|Mentioned|S116, S118|||In Surat Basin? Includes Doncaster Member.||||||
19323|Wallumbilla Formation|65385|5|Briefly described|pS134 Fig.7|Early Cretaceous|Early Cretaceous|Of Eromanga Basin. Overlies Cadna-owie Formation. Overlain by Toolebuc Formation.||||||08-MAR-12
19323|Wallumbilla Formation|65489|5|Briefly described|p49, p55-56, p58, p61, p155|Early Cretaceous|Early Cretaceous|Eromanga Basin. 450m thick. Regional seal.||||Overlies Cadna-owie Formation. Is overlain by Toolebuc Formation.||
19323|Wallumbilla Formation|66529|6|Mentioned|p12 Fig.5|||||Unit in Rolling Downs Group.|Includes Doncaster, Coreena, Jones V and Ranmoor Members.|||
19323|Wallumbilla Formation|66623|3|Fully described|p239, pp242-245, pp256-259. |Albian|Aptian|Previously known as the Blackdown Formation in Queensland. c.360 m thick. Contains a wide range of fossils. Shoreline to deeper marine environment. Outcrops as low rolling hills. Hosts opals at White Cliffs; possible heavy mineral (magnetite and zircon) strandlines locally.||Unit in Rolling Downs Group.|Includes Coreena and Doncaster Members.|Conformably, but sharply overlies Wyandra Sandstone Member. Coreena Member is gradationally overlain by Allaru Mudstone. Doncaster Member disconformably overlies Cadna-owie Formation.|Muddy sandstone and siltstone with local large spherical calcareous concretions; black shale and minor sandstone with abundant dropstone boulders; pyritic and bioturbated mudstone, claystone and shale; calcareous and glauconitic sandstones.|05-JUN-13
19323|Wallumbilla Formation|66915|4|Described|p1-2, 4-6, p9, p11 Fig.7, p12, p16, p18|Cretaceous|Cretaceous|Carpentaria, Eromanga and Surat Basins. Base of Wallumbilla Formation (the "C-Horizon") and correlatives is the major bounding surface of the Great Artesian Basin.||Basal Rolling Downs Group|Coreena Member, Doncaster Member|Overlies Wyandra Sandstone Member (Cadna-owie Formation), Gilbert River and Bungil Formations.|Marine muds.|12-JAN-17
19323|Wallumbilla Formation|66920|5|Briefly described|Map legend|Cretaceous|Cretaceous|||Unit in Rolling Downs Group.|Includes Doncaster Member.||Marine grey mudstone and siltstone with minor interbeds of fine-grained glauconitic and calcareous sandstone, local thin micritic limestone beds and heavy mineral strandline accumulations; down-sequence glacial ice-rafted erratics.|
19323|Wallumbilla Formation|67133|5|Briefly described|p2, p5, p17-19|Early Cretaceous|Early Cretaceous|Samples of this unit were analysed by XRD and optical microscopy for this study. Consists of quartz (27-52%), feldspars (20-30%) with plagioclase dominant, minor (<8%) kaolinite and significant (13-26%) mixed-layer clays, mainly illite.|||Doncaster and Coreena Members.||Siltstones and mudstones with minor sandstones.|
19323|Wallumbilla Formation|67207|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||Unit in Rolling Downs Group.|Includes Doncaster and Coreena Members.||Marine grey mudstone and siltstone with minor interbeds of fine-grained glauconitic and calcareous sandstone, local thin micritic limestone beds and heavy mineral strandline accumulations; down-sequence glacial ice-rafted erratics.|
19323|Wallumbilla Formation|67209|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||Unit in Rolling Downs Group.|Includes Doncaster and Coreena Members.|Overlies Cadna-owie Formation. Is overlain by Allaru Mudstone.|Marine grey mudstone and siltstone with minor interbeds of fine-grained glauconitic and calcareous sandstone, local thin micritic limestone beds and heavy mineral strandline accumulations; down-sequence glacial ice-rafted erratics.|
19323|Wallumbilla Formation|67211|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||Unit in Rolling Downs Group.|Includes Doncaster and Coreena Members.|Overlies Easter Monday Formation.|Marine grey mudstone and siltstone with minor interbeds of fine-grained glauconitic and calcareous sandstone, local thin micritic limestone beds and heavy mineral strandline accumulations; down-sequence glacial ice-rafted erratics.|
19323|Wallumbilla Formation|67323|5|Briefly described|p86-87, p92 Fig.12.2, p93, p94 Fig.12.4|Early Cretaceous|Early Cretaceous|See also GIS attrib tbl, Solid Geology Map, p95 Fig.12.5, p96. Eromanga/Carpentaria Basins. Marine sediments.|||Includes Ranmoor Member.|Overlies Cadna-owie and Gilbert River Formations and Longsight Sandstone. Is overlain by Toolebuc Formation.|Mudstone and siltstone with calcareous concretions.|
19323|Wallumbilla Formation|67402|4|Described|p26, p26 tbl RRM4, p29|Albian|Aptian|Eromanga Basin. Deposited in a transgressive marine environment which was followed by paralic and fluvial deposition. Ranges from 200 to over 350m thick in the Eromanga Basin and up to 600m thick in the Carpentaria Basin. Proven regional seal for hydrocarbons. Misspelt as Wullumbilla on p265. See also p29 fig PSA4, PSA5, p108-p112, p113 fig ERO12, p115 tbl ERO2, p120, P123, p146 fig SRT3, p148, p156, p176, p177, p179 fig CRP/KRM6, p181, p265.||Rolling Downs Group||Overlies the Cadna-owie Formation and Gilbert River Formation. Overlain by the Allaru Mudstone and Toolebuc Formation.|Consists primarily of marine mudstone interbedded with sandy mudstone, siltstone, shale and limestone.|
19323|Wallumbilla Formation|67561|5|Briefly described|p51-60, p62 Fig.11, p67, p68|Aptian|Aptian|Eromanga Basin. Australian Spore-Pollen zonation: C.hughesi. Deposited on a shallow marine shelf during a cold climate transgression. Previously regarded as a lowstand section, but re-interpreted by Bron (2010) as a tsunami deposit generated by the (125 +/- 1 Ma) Tookoonooka impact.||||Correlative of the Bulldog Shale.|Contains glendonites, petrified wood, and ice-rafted boulders of exotic lithology.|20-JAN-17
19323|Wallumbilla Formation|67669|5|Briefly described|p11|Early Cretaceous|Early Cretaceous|Of Bowen Basin.||Unit of Rolling Downs Group.||Underlain by Bungil Formation.||
19323|Wallumbilla Formation|67784|6|Mentioned|p25, p26, p28-29, p31, p32|||185-253m thick. Northern Eromanga Basin.||Wilgunya Subgroup.|Includes Doncaster Member, Jones Valley Member, Ranmoor Member, Coreena Member|Overlies Gilbert River Formation, overlain by Toolebuc Formation||08-FEB-18
19323|Wallumbilla Formation|68003|5|Briefly described|p57 Fig.3-n.|||Bowen Basin.||Unit in Rolling Downs Group.||Overlies Bungil Formation. Is overlain by Surat Siltstone.||
19323|Wallumbilla Formation|68004|6|Mentioned|p175.|||A seal for reservoirs in the Hooray and Mooga Sandstones.||||||
19323|Wallumbilla Formation|68069|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Surat Basin. Shown on cross-sections and time-space plot and basement interpretation only.||Rolling Downs Group|Includes Coreena and Doncaster Members.|Overlies Bungil Formation. Is overlain conformably by Surat Siltstone.|Sandstone, claystone, siltstone and mudstone.|22-NOV-13
19323|Wallumbilla Formation|68117|5|Briefly described|p346|Early Cretaceous|Early Cretaceous|Surat Basin.|||Doncaster, Coreena Members.|||
19323|Wallumbilla Formation|68206|5|Briefly described|p31-33|Aptian|Aptian|Carpentaria, Eromanga Basins.|||Doncaster, Jones Valley, Ranmoor Members.|Is overlain by Toolebuc Formation.||
19323|Wallumbilla Formation|68279|6|Mentioned|p18-19|||Galilee Basin stratigraphic cross-sections, and mineralogy tables.||||||
19323|Wallumbilla Formation|68345|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Carpentaria Basin.||||Conformably overlies Coffin Hill Member (Gilbert River Formation).|Mudstone and siltstone with calcareous concretions.|
19323|Wallumbilla Formation|68349|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Carpentaria Basin.||||Conformably overlies Coffin Hill Member (Gilbert River Formation).|Mudstone and siltstone with calcareous concretions.|
19323|Wallumbilla Formation|68417|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Carpentaria Basin. No outcrop in map area: shown only in subsurface and rock relationship diagram.||||Conformably underlain by the Coffin Hill Member, Gilbert River Formation.|Mudstone and siltstone with calcareous concretions.|
19323|Wallumbilla Formation|68553|6|Mentioned|Map legend; schematic diagram.|Cretaceous|Cretaceous|Surat, Eromanga, Laura and Carpentaria Basins.||Unit in Rolling Downs Group.||Is overlain conformably by Griman Creek Formation and Toolebuc Formation.||
19323|Wallumbilla Formation|68576|5|Briefly described|Q_4: p3|Early Cretaceous|Early Cretaceous|Surat Basin.|||Doncaster, Coreena Members.|Overlies Bungil Formation. Is overlain by Surat Siltstone.||
19323|Wallumbilla Formation|68593|5|Briefly described|p4, p47|Early Cretaceous|Early Cretaceous|Mainly marine deposits.|||Doncaster and Coreena Members.|Overlies Bungil Formation. Is overlain by Surat Siltstone.|Siltstone, mudstone, minor conglomerate, rare coal.|
19323|Wallumbilla Formation|68731|6|Mentioned|pp209-211|||||||||
19323|Wallumbilla Formation|68734|5|Briefly described|p218 Fig.2, p221 Fig.3|Aptian|Barremian|Eromanga Basin (NE). Marine to coastal paralic and shallow marine.||Of the Rolling Downs Group.|Includes Coreena Member and Doncaster Member.|||16-JAN-17
19323|Wallumbilla Formation|68821|5|Briefly described|p292 Fig.1, p292, p295, p296, p298|Cretaceous|Cretaceous|Lower Cretaceous age. Equivalent to the Bulldog Shale Formation. Parallic to marine sediments. Contains ubiquitous disseminated pyrite.||Of the Rolling Downs Group.|||Consist of pyrite and carbonaceous-rich marine mudstones and siltstones interbedded with fine sandstones.|
19323|Wallumbilla Formation|68901|5|Briefly described|p7 Fig. ii|Upper Cretaceous|Lower Cretaceous|Eromanga Basin.||Rolling Downs Group|||Mudstone, siltstone, sandstone; calcareous in part.|27-SEP-18
19323|Wallumbilla Formation|69019|5|Briefly described|p85 Fig.21.|Albian|Aptian|Southern Eromanga Basin.||||Overlies Cadna-owie Formation. Is overlain by Toolebuc Formation.||
19323|Wallumbilla Formation|69023|6|Mentioned|p89 Fig.20, p99|Albian|Aptian|||||||
19323|Wallumbilla Formation|69297|5|Briefly described|p273, p274 fig 4. 3, p275|Upper Cretaceous|Upper Jurassic|Carpentaria Basin. Contains good TOC for hydrocarbon generation.||Rolling Downs Group||Overlies the Gilbert River Formation. Overlain by the Toolebuc Formation.|Lithic glauconitic sandstones, siltstone, claystone and limestone.|
19323|Wallumbilla Formation|69377|5|Briefly described|map legend|Early Cretaceous|Early Cretaceous||||||Mudstone and siltstone with calcareous concretions|
19323|Wallumbilla Formation|69379|5|Briefly described|map legend|Cretaceous|Cretaceous||||Doncaster Member|||
19323|Wallumbilla Formation|69454|6|Mentioned|p38:3, 13|||Eromanga Basin. Potential seal for Cadna-owie Formation sandstone reservoirs.||||||12-JUL-16
19323|Wallumbilla Formation|69455|5|Briefly described|p39:4 Fig.39.3; 39:14-15|Early Cretaceous|Early Cretaceous|Provides a seal to Gilbert River Formation sandstone reservoirs in the offshore Western Gulf Sub-basin. Organic-rich shale is a possible source rock.||||||12-JUL-16
19323|Wallumbilla Formation|69457|3|Fully described|p41:2-3; 41:5 Fig.41.4; 41:6-10, 14-16|Early Cretaceous|Early Cretaceous|Vine et al. (1967). Eromanga, Carpentaria and Surat Basins. Mostly subsurface; outcrops form mesas, buttes or low rounded duricrusted hills. Shallow-marine, nearshore to marginal marine, minor non-marine deposits. 143m to over 350m thick. Equivalent to the succession comprising Bulldog Shale, Coorikiana Sandstone and lower part of Oodnadatta Formation. The name Bulldog Shale has previously (and inappropriately) been used to describe this Formation in the NT (eg Questa, 1990; Ambrose and Heugh, 2010). Has fair to occasionally excellent petroleum source intervals. May seal Cadna-owie Formation reservoirs.||Wilgunya Subgroup.|Doncaster, Coreena, Jones Valley, Ranmoor Members.|Overlies Cadna-owie Formation conformably, and Algebuckina Sandstone disconformably/unconformably. Is overlain conformably by Toolebuc Formation.|Mudstone and siltstone; minor thin intervals of fine sandstone and limestone. Locally calcareous, and may contain glauconite; shell fragments common in places. Locally silicified to porcellanite. Contains diverse fossil assemblages.|12-JUL-16
19323|Wallumbilla Formation|69582|5|Briefly described|p22, p25-p26, p29, p36, p65-p66|Lower Cretaceous|Lower Cretaceous|Eromanga and Surat basins. Deposited in a marine depositional environment. Intersected in GSQ Longreach 2 drillhole.||||Overlain by the Toolebuc Formation and the Surat Siltstone. Overlies the Bungil Formation and the Cadna-owie Formation.|Sandstone.|
19323|Wallumbilla Formation|69591|6|Mentioned|p101 Fig.2.96|||||||Overlies Gilbert River Formation. Is overlain by Toolebuc Formation.||
19323|Wallumbilla Formation|69594|4|Described|p518-519, p521-522, p526, p528-530, p534|Aptian|Barremian|See also p538, p540, p550, p573. Vine et al. (1967). Carpentaria, Eromanga, Laura and northern Surat Basins. Much of the upper part was previously known as Blackdown Formation (Laing and Power, 1959; Woods, 1961). Up to 475m thick. Contains a rich marine fauna (listed). Members not always discernible. RELATED UNITS (continued): Equivalent to Rolling Downs Group in the Laura Basin, the Roma Formation and lower part of overlying Tambo Formation.||Wilgunya Subgroup.|Coreena, Doncaster, Jones Valley, Ranmoor, Trimble Members.|Conformably overlies Gilbert River, Cadna-owie, Bungil Formations, Longsight Sandstone, Ronlow and Helby beds. Is overlain by Toolebuc Formation, Surat Siltstone and Allaru Mudstone. See COMMENTS.|Volcanogenic. Dominated by thick successions of sporadically nodular siltstone with lesser glauconitic sandstone, volcanic crystal-lithic sandstone and silty limestone.|
19323|Wallumbilla Formation|69673|5|Briefly described|p155 fig 127, p156, p159, p161|Cretaceous|Cretaceous|||Wilgunya Subgroup|Includes Doncaster Member, Coreena Member|Overlies Mount Anna Sandstone Member, Cadna-owie Formation overlain by Toolebuc Formation, correlated with Bulldog Shale|Mudstone, shale and siltstone with minor thin interbeds of fine sandstone and limestone.|
19323|Wallumbilla Formation|69681|6|Mentioned|p74 Fig.3, p82|Early Cretaceous|Early Cretaceous||||Includes Doncaster and Coreena Members.|||
19323|Wallumbilla Formation|69797|5|Briefly described|p17 Fig.2|Early Cretaceous|Early Cretaceous|Geol. Prov: Eromanga Basin.||||||
19323|Wallumbilla Formation|69946|3|Fully described|p19, p21-25, p56-57, p94|Early Cretaceous|Early Cretaceous|Vine et al. (1967); formerly Roma Formation, used by the petroleum industry. Type section is 'Wallumbilla Creek, from Wallumbilla Township south for 12 miles [19.3km]'. Distribution is by definition controlled by Toolebuc Formation: where absent, Bulldog Shale is used. Lithology is identical to Bulldog Shale. Up to 596m thick. Early Aptian-Albian. Wireline log correlations.||||Conformably overlies Cadna-owie Formation. Is overlain conformably by Toolebuc Formation.|Grey mudstone and siltstone with minor interbeds of fine-grained sandstone. Local pebbly and muddy diamictite containing metamorphic and sedimentary clasts.|
19323|Wallumbilla Formation|69947|5|Briefly described|p9, p13 Fig.7.2, p29 Fig.7.18|Early Cretaceous|Early Cretaceous|See also p31 Fig.7.20. Eromanga Basin.||Marree Subgroup.||Overlies Wyandra Sandstone Member (Cadna-owie Formation).|Thick, fossiliferous mudstones and siltstones.|
19323|Wallumbilla Formation|69948|6|Mentioned|p4; Figs.4.2, 18|||Eromanga Basin (an intracratonic basin). Sediment thickness, sonic log, gamma ray log all shown in contrast with Otway Basin (a rift basin).||||Overlies Cadna-owie Formation. Is overlain by Toolebuc Formation.|Marine shales.|
19323|Wallumbilla Formation|69952|5|Briefly described|p16|Cretaceous|Cretaceous|Eromanga Basin.||Unit in Rolling Downs Group.|||Mudstone, siltstone, sandstone; calcareous in part.|
19323|Wallumbilla Formation|70207|6|Mentioned|p14, p74|Early Cretaceous|Early Cretaceous|Georgetown region.||||||
19323|Wallumbilla Formation|70345|6|Mentioned|p3|Cretaceous|Cretaceous|||||||
19323|Wallumbilla Formation|70352|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|||Wilgunya Subgroup.|||Mudstone and siltstone with calcareous concretions.|
19323|Wallumbilla Formation|70354|5|Briefly described|Map legend|Cretaceous|Cretaceous|||Rolling Downs Group.||Is overlain by Toolebuc Formation.|Mudstone and siltstone with calcareous concretions.|
19323|Wallumbilla Formation|70572|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|||Wilgunya Subgroup|||Mudstone and siltstone with calcareous concretions.|20-JAN-22
19323|Wallumbilla Formation|70649|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||Rolling Downs Group|Includes Coreena Member, Doncaster Member.||Marine grey mudstone and siltstone with minor interbeds of fine-grained glauconitic and calcareous sandstone, local thin micritic limestone beds and heavy mineral strandline accumulations; down-sequence glacial ice rafted erratics.|
19323|Wallumbilla Formation|70652|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Unconsolidated sediments also described.||Rolling Downs Group|Includes Coreena Member, Doncaster Member.|||
19323|Wallumbilla Formation|70673|6|Mentioned|p7|Cretaceous|Cretaceous|||||||
19323|Wallumbilla Formation|70720|6|Mentioned|p24-25|Early Cretaceous|Early Cretaceous||||Doncaster Member.|||
19323|Wallumbilla Formation|70821|4|Described|p21 Fig.2.6, p22 Fig.2.7, p23, p28|Early Cretaceous|Early Cretaceous|See also p30-31, p33, p79-80, p82, p85-88, p111-112, p117. Vine et al. (1967). The most widely distributed marine unit within the Great Australian Superbasin: Eromanga, Carpentaria, Laura and parts of Surat Basins. Varying thicknesses given from wells. Aptian to Albian age. Hydrochemistry mentioned; hydrostratigraphic properties. Equivalent to Bulldog Shale and Oodnadatta Formation.||Rolling Downs Group.|Doncaster, Coreena Members.|Overlies Cadna-owie and Bungil Formations, Hooray Sandstone and Drildool beds. Is overlain by Toolebuc Formation or Surat Siltstone; locally by Winton Formation (conformably).||
19323|Wallumbilla Formation|70823|5|Briefly described|p43-p44, p78|Early Cretaceous|Early Cretaceous|Eromanga Basin. Up to 450m thick. Deposited in open marine transgressive to regressive marine shoreface environments.||||Overlies the Cadna-owie Formation. Overlain by the Toolebuc Formation.||
19323|Wallumbilla Formation|70824|5|Briefly described|p9|Cretaceous|Cretaceous|Eromanga Basin.||||Overlies the Cadna-owie Formation. Overlain by the Toolebuc Formation.||
19323|Wallumbilla Formation|70836|6|Mentioned|p474|Early Cretaceous|Early Cretaceous|Lightning Ridge area, Surat Basin. Barremian-Albian.|||Coreena, Doncaster Members.|Overlies Bungil Formation. Is overlain by Surat Siltstone.||
19323|Wallumbilla Formation|70860|6|Mentioned|p281|||Great Artesian Basin.|||Coreena, Doncaster, Ranmoor, Jones Valley, Members.|||
19323|Wallumbilla Formation|71251|4|Described|p8, p11-13, p15, p17-20, p29|||First described by Isbell (1957). Eromanga Basin. 186m total thickness in Eulo 1 borehole; it was not possible to differentiate the two Members in this borehole. Natural gamma, magnetic susceptibility data tabulated. Conductivity data/diagram.||Rolling Downs Group.|Coreena and Doncaster Members.|Overlies Wyandra Sandstone Member (Cadna-owie Formation). Is overlain by Winton Formation.|Generally monotonous, glauconitic, marine, dark bluish-grey carbonaceous mudstone with some lignite plant fragments, some thin (estimated <1m) beds of siltstone and fine sandstone.|
19323|Wallumbilla Formation|71321|5|Briefly described|p15,27,65|Cenomanian|Cenomanian|Of Eromanga Basin. Previously known as Roma Formation. Regressivee depositional package following peak early Cretaceous marine transgression; marginal marine shoreface deposit.||||Equivalent to Bulldog Shale. Overlain by the Toolebuc Formation.||24-OCT-19
19323|Wallumbilla Formation|71342|3|Fully described|Ch4 p4, Ch4 p9, Ch4 p25|Albian|Aptian|Eromanga Basin. Formally defined by Vine et al (1967)  to replace the Roma Formation. Vine et al also defined the type section in "Wallumbilla Creek,from Wallumbilla Township south for 12 miles" in Queensland. This unit reaches a maximum thickness of 596m in Coonatie 1 in the Patchawarra Trough and 260m in the Poolowanna Trough. Age derived from palynology. Interpreted to have been deposited in a shallow epicontinental sea at cold high latitudes as debris flows. Spore-pollen zone is given in Ch5 p57. See also Ch5 p22, Ch5 p24-p25, Ch5 p30, Ch5 p57, Ch6 p8-p9, Ch7 p9, Ch7 p13, Ch10 p17, Ch11 p4-p5, Ch12 p12, Ch12 p14.||||Conformably overlies the Wyandra Sandstone Member (Cadna-owie Formation). Conformably overlain by the Toolebuc Formation.|Grey mudstone and siltstone with minor interbeds of fine-grained sandstone.|
19323|Wallumbilla Formation|71382|5|Briefly described|p4, p13, p16-p17, p19-p20|||Intersected in GSQ Julia 1 from 199.87m-310.49m for a total of 110.62m thickness. Temp log and stratlog are provided. Lithology is described in detail on p20. See also p23, p25, p27, App 3, 4.||||Overlies the Hooray Sandstone. Overlain by the Toolebuc Formation.|Interbedded mudstone and sandstone with minor calcareous mudstone.|
19323|Wallumbilla Formation|71855|4|Described|p2, p4-p6, p9-p10, p13|Jurassic|Jurassic|Eromanga and Carpentaria basins. In places the contact with the overlying Toolebuc Formation is disconformable or faulted. Wireline log responses were described for this unit including Gamma-ray, sonic transit time and resistivity. Structure is discussed. See also p15, p27, p33-p35, p50, p52-p53, p56-p57, p75.||||Conformably (gradationally) overlain by the Toolebuc Formation.|Glauconitic, smectite-rich mudstone, siltstone or fine-grained sandstone.|
19323|Wallumbilla Formation|71863|5|Briefly described|p4-p9|Albian|Aptian|Eromanga and Carpentaria basins. Deposited in a marine incursion.||Rolling Downs Group|Includes the Doncaster Member and the Coreena Member.|Overlies the Gilbert River Formation, Helby beds and the Cadna-owie Formation. Conformably overlain by the Toolebuc Formation.||
19323|Wallumbilla Formation|71864|4|Described|p8, p10, p13-p14, p16-p20|||Intersected in GSQ Eulo 2 borehole between 23-51m depth. Originally mapped in the area by Senior (1971). Described in Senior, 1971 as glauconitic marine siltstones and claystones. Gamma log characteristics and magnetic susceptibility is provided.||Rolling Downs Group|Includes the Coreena Member and the Doncaster Member.|Overlain by the Winton Formation. Overlies the Waihora Volcanics.|Dark blue to light grey siltstone with a distinctive layer producing carbonaceous flecks and a fine quartzose sandstone layer in addition to mudstone.|
19323|Wallumbilla Formation|71890|6|Mentioned|p7|||Surat Basin.||Rolling Downs Group||||
19323|Wallumbilla Formation|72297|5|Briefly described|p742, p746, p753|||Eromanga Basin. Acts as a regional seal. Potential hydrocarbon source rocks.|||Ranmoor Member.|Is overlain conformably by the Toolebuc Formation.|Shales and mudstones.|
19323|Wallumbilla Formation|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA,QLD,NSW), Carpentaria Basin, Surat Basin (QLD,NSW), Coonamble Embayment (NSW).||Rolling Downs Group.|Doncaster, Coreena, Jones Valley, Ranmoor Members.|Overlies Wyandra Sandstone Member (Cadna-owie FZ); Gilbert River and Bungil FZs; Ronlow, Helby, Albany Pass and Drildool beds. Is overlain by Toolebuc FZ or Surat Siltstone.||
19323|Wallumbilla Formation|72913|6|Mentioned|p8.|||Two wells intersected this cover unit.||||||
19323|Wallumbilla Formation|72914|5|Briefly described|p12, p14, p16, p18, p20-21, p29, App. I|Cretaceous|Cretaceous|In Tongo 1 [borehole], the unit is semi-monotonous consisting chiefly of marine siltstone and claystone, but can occasionally has washes of coarser-grained quartzose sediments derived from local basement highs. Natural gamma emissions are relatively subdued and monotonous.||||Underlain by the Wyandra Sandstone Member (Cadna-owie Formation).|Marine siltstone and claystone with occasional washes of coarser-grained quartzose material.|
19323|Wallumbilla Formation|72915|6|Mentioned|p16, p19, p27, p39 App E, App I|Mesozoic|Mesozoic|Sedimentary rocks in the Congararra 1 borehole are attributed to the Rolling Downs Group, and may represent source-proximal Wallumbilla Formation (after Hawke and Cramsie, 1984). Mineralogical changes from clay-rich to quartz-rich are reflected in natural gamma emissions [data]. Relatively non-magnetic in Congararra 1. No groundwater was made from this unit in Congararra 1.||||||
19323|Wallumbilla Formation|72967|6|Mentioned|p5|||Carpenteria Basin.||Rolling Downs Group||||
19323|Wallumbilla Formation|72983|6|Mentioned|p15|Cretaceous|Cretaceous|||||||
19323|Wallumbilla Formation|73083|6|Mentioned|p62-63|Cretaceous|Cretaceous|||||Overlain by the Toolebuc Formation.|Mudstone and siltstone.|
19323|Wallumbilla Formation|73113|5|Briefly described|p. 22-24, 36-37, 41, 69, 80, 88, 116...|||Surat Basin. Tight aquitard. More locations: p. 119, 146, 151-152, 168-172, 177-178, 191.||||||
19323|Wallumbilla Formation|73137|6|Mentioned|p6, p81|Cretaceous|Cretaceous|Carpentaria Basin. Intersected in drill hole GIDPDS5.||||||08-OCT-22
19323|Wallumbilla Formation|73144|6|Mentioned|p8, p13|Cretaceous|Cretaceous|Carpentaria Basin. Leaky aquitard.||Rolling Downs Group||Underlain by Gilbert River Formation. Overlain by Toolebuc Formation.||
19323|Wallumbilla Formation|73147|5|Briefly described|p129|Aptian|Aptian|||Rolling Downs Group.||Overlies Gilbert River Formation. Is overlain by Toolebuc Formation.||
19323|Wallumbilla Formation|73167|6|Mentioned|p664 Fig. 2|Cretaceous|Cretaceous|Eromanga Basin.||||||
19323|Wallumbilla Formation|73203|6|Mentioned|p653|Early Cretaceous|Early Cretaceous||||Doncaster Member||Includes interbedded sandy/silty claystone and interbedded fine sandstones.|
19323|Wallumbilla Formation|73249|5|Briefly described|p319, p321, p323|Albian|Aptian|North and east of the Eromanga Basin [shown as within the Eromanga Basin on p319 Fig.2]. Laterally equivalent to the Bulldog Shale.||||Lateral equivalent to the Bulldog Shale, overlies the Cadna-owie Formation, underlies the Toolebuc Formation.|Siltstone and mudstone dominated.|
19323|Wallumbilla Formation|73251|6|Mentioned|p62|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Underlain by Wyandra Sandstone Member (Cadna-owie Formation). Overlain by Toolebuc Formation. Equivalent to Coorikiana Sandstone and Bulldog Shale.||
19323|Wallumbilla Formation|73281|6|Mentioned|p1, Appendix (DIP)|||Eromanga Basin. See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
19323|Wallumbilla Formation|73343|6|Mentioned|p337|Cretaceous|Cretaceous|Eromanga Basin.||||Underlain by Wyandra Sandstone Member (Cadna-owie Formation). Overlain by Toolebuc Formation. Equivalent to Coorikiana Sandstone and Bulldog Shale.||
19323|Wallumbilla Formation|73472|6|Mentioned|p114|Cretaceous|Cretaceous|||||||
19323|Wallumbilla Formation|73479|5|Briefly described|p156 Fig.2, p159, p163, p164 Fig.7, p175|Cretaceous|Cretaceous|Eromanga Basin. Restricted open marine and shoreface depositional environment.|ca 125-104 Ma|||Overlies Wyandra Sandstone Member, underlies Toolebuc Formation||
19323|Wallumbilla Formation|73553|6|Mentioned|p7|Cretaceous|Cretaceous|||||||
19392|Wangarlu Formation|5952|5|Briefly described|p215 Fig. 5, p222, p223|||Appears as Wangarlu in figure. Geological Province: Bonaparte Basin.||||||01-MAR-10
19392|Wangarlu Formation|13194|4|Described|p384 Tb. 4-16|Cretaceous|Cretaceous|Type section: Cliffs at NW end of Wangarlu Bay, Cobourg Peninsula. 11o12'S 132o20'E.||Bathurst Island Group||Overlies Darwin Formation (conformably). Part coeval with Moonkinu Sandstone, Turnstone Formation, Vee Formation, Puffin Formation, Brown Gannet Limestone.|Micaceous mudstone, galuconitic siltstone; minor sandstone and carbonate.|
19392|Wangarlu Formation|23999|5|Briefly described|p8|Cretaceous|Cretaceous|Supersedes Wangarlu Mudstone Member. Conformably overlies Darwin Formation; overlain by Mookinu Sandstone. Thickness: 2000m.||||||07-FEB-11
19392|Wangarlu Formation|24001|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Kaolinitic to montmorillonitic claystone/mudstone.||||||18-DEC-06
19392|Wangarlu Formation|24047|5|Briefly described|p13, p63|Cretaceous|Cretaceous|Of the Bathurst Island Group.  Geological Province: Money Shoal Basin.||||||
19392|Wangarlu Formation|24218|5|Briefly described|p850|Late Cretaceous|Late Cretaceous|Geological Province: Bonaparte Basin.||||||
19392|Wangarlu Formation|24379|5|Briefly described|p17|Cretaceous|Cretaceous|Overlies Echuca Shoals Formation. Geological Province: North West shelf.||||||18-DEC-06
19392|Wangarlu Formation|24569|5|Briefly described|p248 Fig. 3|Santonian|Coniacian|Of the Bathurst Island Group. Geological Province: Petrel Sub-basin.||||||02-MAR-05
19392|Wangarlu Formation|41459|6|Mentioned|Fig.2|||||||||
19392|Wangarlu Formation|41532|3|Fully described|p306|||||||||
19392|Wangarlu Formation|41731|6|Mentioned|Fig.3|||||||||
19392|Wangarlu Formation|42056|4|Described|p100|||||||||
19392|Wangarlu Formation|42442|2|Defined|p28|Maastrichtian|Albian|NT and WA.||||||18-DEC-06
19392|Wangarlu Formation|42473|6|Mentioned|p56|||||||||
19392|Wangarlu Formation|43661|6|Mentioned|Fig.3|||||||||
19392|Wangarlu Formation|43699|6|Mentioned|Fig.6,p10||Early Cretaceous|||||||
19392|Wangarlu Formation|43739|6|Mentioned|Fig.5,p38|Late Cretaceous|Early Cretaceous|||||||
19392|Wangarlu Formation|49637|5|Briefly described|Fig.3|Early Cretaceous|Early Cretaceous|Of the Bathurst Island Group. Geological Province: Petrel Sub-basin.||||||07-FEB-11
19392|Wangarlu Formation|62837|5|Briefly described|Stratigraphic columns|Paleocene|Early Cretaceous|Of the Bathurst Island Group. Age: ~104-~65Ma. Geological Province: Petrel Sub-basin and Arafura and Money Shoals Basins.||||||01-MAR-10
19392|Wangarlu Formation|64695|5|Briefly described|p262 Fig.8, p265, p266-269 Figs.11-14|Late Cretaceous|Late Cretaceous|Northern Bonaparte Basin. A major vitrinite maturity jump at the base of this unit may have been caused by multiple diatreme intrusions.||||Is overlain by Johnson Formation.||
19392|Wangarlu Formation|69452|4|Described|p36:8, 15, 22|Campanian|Albian|Hughes and Senior (1974); Hughes (1978); redefined in Mory (1988). Money Shoal Basin; also Petrel Sub-basin, Bonaparte Basin, where the rocks are referred to as Wangarlu Formation equivalent. Ofshore; <2000m thick. Inner to distal marine shelf.||Bathurst Island Group.||Conformably overlies Darwin Formation.|Massive claystone with subordinate siltstone and minor sandstone, grading upward into claystone, calcimudstone and marl.|12-JUL-16
19392|Wangarlu Formation|69456|3|Fully described|p40:2; 40:3 Fig.40.4; 40:4, 6-8, 10|Cretaceous|Cretaceous|Mory (1988); formerly Wangarlu Mudstone Member of Hughes and Senior (1974). Western Money Shoal Basin, Bonaparte Basin and their offshore areas. Shallow marine environment. 287m thick, thinning to the S; over 2000m in the Malita Graben (offshore Bonaparte Basin). Marine; much of the shale is probably prodeltaic. Contains a relatively diverse, late Albian ammonite fauna. Local 20-30m deep laterite profile capped by ferricrete.||Bathurst Island Group.||Conformably overlies Darwin Formation. Is overlain conformably by Moonkinu Sandstone.|Micaceous mudstone, claystone; variable amounts of glauconitic siltstone, sandstone, marl and limestone. Pyrite, pyritic nodules, calcareous concretions and carbonaceous material are relatively common.|12-JUL-16
19392|Wangarlu Formation|69653|5|Briefly described|p6, 8, 10, 26-27, 30, 37-38, 41-43, 63|Cretaceous|Cretaceous|Petrel Sub-basin. Offshore marine shelf deposits. Schematic (gamma ray) well sections. Composite well diagram. See also p50-51, 53.||Bathurst Island Group.||Overlies Darwin Formation. Is overlain by Woodbine Group.|Fine- to coarse-grained sandstones, packstone limestone, glauconitic argillaceous siltstone, silty mudstone, massive mudstone. Facies described in detail.|
19392|Wangarlu Formation|69673|6|Mentioned|p204|Cretaceous|Cretaceous|||Bathurst Island Group|||Micaceous mudstone with variable amounts of glauconitic siltstone, sandstone, marl and limestone.|
19392|Wangarlu Formation|70061|5|Briefly described|Petrel Sub-basin; Fig.2|Maastrichtian|Albian|See also Regional geology: Fig.6, p12. Sahul: Fig.2, p3. Regionally-developed sandstones form high-quality reservoirs; commonly sealed by Johnson Formation carbonates. Shales and claystones form a regional seal in Sahul Syncline.||Bathurst Island Group.||Overlies Darwin Formation. Is overlain by Woolaston and Puffin Formations.||12-JUL-16
19392|Wangarlu Formation|73083|6|Mentioned|p17|Cretaceous|Cretaceous|Money Shoal Basin.||||||
19519|Warrego Granite|22446|5|Briefly described|p26|Statherian|Statherian|||||||
19519|Warrego Granite|22645|6|Mentioned|P212, Fig9, P213||Statherian|Age of unit is 1650 Ma.||||||18-DEC-06
19519|Warrego Granite|22658|5|Briefly described|p 275|Proterozoic|Proterozoic|||||||
19519|Warrego Granite|23204|6|Mentioned|p1363|||||||||
19519|Warrego Granite|23363|5|Briefly described|352 Tab.3|Statherian|Statherian|Age: ca 1645.||||||18-DEC-06
19519|Warrego Granite|23410|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Granite: Two-mica, corundum-bearing, granite and granodiorite; coarse grained, equigranular, massive. Pegmatitic segregations, greisenisation; quartz-biotite metamorphic aureole.||||||07-NOV-08
19519|Warrego Granite|23733|3|Fully described|p14|Paleoproterozoic|Paleoproterozoic|Included in the Devils Suite by Wyborn et al (1998 a). See also p 7 Fig. 1.||||||23-DEC-08
19519|Warrego Granite|23809|6|Mentioned|p27 Fig. 25|||Geological Province: Tennant Inlier.||||||30-NOV-04
19519|Warrego Granite|24047|6|Mentioned|p8 Fig. 7|||Includes the Devils Suite.  Geological Province: Tennant Inlier.||||||
19519|Warrego Granite|24172|6|Mentioned|p64|||||||||
19519|Warrego Granite|24197|6|Mentioned|p68 Tb. 6.1|Paleoproterozoic|Paleoproterozoic|Of the Devils Suite. Age: ~1710Ma. Geological Province: Tennant Creek/Davenport Province.||||||07-FEB-11
19519|Warrego Granite|24294|5|Briefly described|p1168 Fig.1|Paleoproterozoic|Paleoproterozoic|Age: 1700-1650 Ma. Geological Province: Tennant Creek Inlier.||||||07-NOV-08
19519|Warrego Granite|29135|4|Described|p36|||Informal use of name. -Pgw,-Pgy & -Pgx on Tennant Creek 1:250k sheet.||||||
19519|Warrego Granite|39571|6|Mentioned|p129|||||||||
19519|Warrego Granite|41465|6|Mentioned|p12|||||||||
19519|Warrego Granite|41879|6|Mentioned|p43|||||||||
19519|Warrego Granite|41970|6|Mentioned|p338|||||||||
19519|Warrego Granite|42853|5|Briefly described|p594|||see also Fig.1 p592.||||||18-DEC-06
19519|Warrego Granite|42936|5|Briefly described|p546 Fig.1|||||||||
19519|Warrego Granite|43832|6|Mentioned|Table 17 p90||Paleoproterozoic|||||||07-NOV-08
19519|Warrego Granite|43850|4|Described|p263|||Rb-Sr age 1662+/-20 Ma probably represents minimum age for crystalisation||||||
19519|Warrego Granite|46842|6|Mentioned|p114|||||||||
19519|Warrego Granite|46964|6|Mentioned|p269|||||||||
19519|Warrego Granite|46992|6|Mentioned|p253|||||||||
19519|Warrego Granite|50353|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of 'Late' granite. Two-mica, corundum-bearing granite and granodiorite; course grained, equigranular, massive. Pegmatite segregations, greisenisation; quartz-biotite metamorphic aureole.||||||07-NOV-08
19519|Warrego 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: 1677-1662 +/- 20Ma (Ar-Ar, Rb-Sr).||||||07-NOV-08
19519|Warrego Granite|60657|5|Briefly described|p13 Fig. 2|Paleoproterozoic|Paleoproterozoic|Age: 1680-1660Ma. Geological Province: Tennant Creek Inlier.||||||07-NOV-08
19519|Warrego Granite|60684|2|Defined|p54 Appendix, p1|Paleoproterozoic|Paleoproterozoic|Intrusive, massive, coarse-grained equigranular muscovite granite or granodiorite; S-type. Intrudes the Flynn Subgroup. Age: 1700-1650 Ma (Compston 1995). Geological Province: Tennant Creek province.||||||17-APR-15
19519|Warrego Granite|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Granite/granodiorite; muscovite-biotite and corundum-bearing; equigranular; pematitic segregations.  In the Tennant Creek region.||||||07-NOV-08
19519|Warrego Granite|64559|6|Mentioned|p973, p975 Fig. 8, p979, p980|||Age: 1662+/-20Ma (Rb-Sr). Unfoliated and U-rich.||||||23-DEC-08
19519|Warrego Granite|65209|6|Mentioned|p35 Fig.1, p37|Paleoproterozoic|Paleoproterozoic|||Devils Suite||||
19519|Warrego Granite|65455|6|Mentioned|p7|Paleoproterozoic|Paleoproterozoic|In the Tennant Creek region. It is noteworthy as a high-U igneous rock.||Devils Suite.||||09-MAY-12
19519|Warrego Granite|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Devils Suite.|||Granite/granodiorite; muscovite-biotite and corundum- bearing; equigranular; pegmatitic segregations.|
19519|Warrego Granite|67352|6|Mentioned|p8|||Uncertain age; may be 1650 Ma, which should probably exclude it from Devils Suite.||Devils Suite||||
19519|Warrego Granite|69187|5|Briefly described|p53 Fig.2, p54 Fig.3, p62|Statherian|Statherian|Warramunga Province.|1662 +/- 20 Ma Rb-Sr (Black 1981)|||||
19519|Warrego Granite|69424|4|Described|p9:3, 11, 14, 28-30, 32, 43, 51|Statherian|Statherian|Warramunga Province. Knotted quartz-muscovite schist forms a contact aureole up to 400m wide. Has contact metamorphosed the Warrego Au-Cu-Bi deposit, and thus was not the source of mineralisation. Age is uncertain; previous age analyses are described. They include an imprecise U-Pb igneous crystallisation age of c.1645 Ma (Compston, 1995) and a K-Ar muscovite age of 1684 +/- 17 Ma (Compston, 1994).|c.1645 Ma?|Devils Suite.||Intrudes Warramunga Formation and Ooradidgee Subgroup.|Massive, coarse-grained and equigranular, two-mica, corundum-bearing granite to granodiorite; locally greisenous. Contains metasedimentary xenoliths.|12-JUL-16
19519|Warrego Granite|71592|5|Briefly described|Appendix A.|||Tennant Creek Region.|||||Granite.|
19519|Warrego Granite|72380|5|Briefly described|p9|Paleoproterozoic|Paleoproterozoic|Geological province: Warramunga and Davenport provinces. Previously geochronological analysis yielded zircon ages ranging from c. 1857 Ma to c. 1650 Ma, and a 40Ar-39Ar muscovite age of 1677+\-4 Ma (Compston 1994, 1995; Donnellan 2013 and references therein; whole rock Rb-Sr age of 1662+\-20 Ma (Black 1977) and K-Ar muscovite ages of 1710+\-35 Ma and 1684+\-35 Ma (Compston and McDougall, 1994). These geochronological ages indicate a crystallisation age potentially as young as c. 1650 Ma, but a precise age remains uncertain.||||||
19519|Warrego Granite|73124|6|Mentioned|p2 Fig.1|||||||||
19519|Warrego Granite|73125|5|Briefly described|p2|Palaeoproterozoic|Palaeoproterozoic|Warramunga Province.||Devils Suite.||||
19519|Warrego Granite|73427|6|Mentioned|App.A|||Tennant Region.||||||
19519|Warrego Granite|73460|6|Mentioned|p2|||Warramunga Province.||||Equivalent to Devils Suite.||
19519|Warrego Granite|73590|6|Mentioned|p2|Statherian|Statherian||ca 1710-1700 Ma|||Equivalent to Devils Suite.||
19520|Warrego Volcanics|23410|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Flynn Subgroup, Churchills Head Group. Chert (silicified tuff?); tuff; white weathering siltstone and shale; fine grained sublithic arenite; thin to medium bedded; laminated.||||||07-NOV-08
19520|Warrego Volcanics|23733|3|Fully described|p6|Paleoproterozoic|Paleoproterozoic|Of the Flynn Group.  Thickness in type section: ~550m.||||||07-NOV-08
19520|Warrego Volcanics|23809|5|Briefly described|p27 Fig. 25|||Of the Flynn Group. Geological Province: Tennant Inlier.||||||14-APR-15
19520|Warrego Volcanics|24172|4|Described|p21, p7 Tb.1|Paleoproterozoic|Paleoproterozoic|Of the Flynn Subgroup. Underlain by Wundirgi Formation. Max. thickness: ~550m in type area. Originally included in the Warramunga Group, now part of the Flynn Subgroup. Correlates with Bernborough and upper parts of Wundirgi and Yungkulungu Formations.||||||07-NOV-08
19520|Warrego Volcanics|24197|5|Briefly described|p22, p28|Paleoproterozoic|Paleoproterozoic|Parts included in Tennant Creek Supersuite. Of the Devils Suite. Geological Province: Tennant Creek/Davenport Province.||||||07-FEB-11
19520|Warrego Volcanics|32174|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
19520|Warrego Volcanics|33307|6|Mentioned|Fig.8|||||||||
19520|Warrego Volcanics|35771|2|Defined|p21|Paleoproterozoic|Paleoproterozoic|Appendix.||||||07-NOV-08
19520|Warrego Volcanics|39213|6|Mentioned|Fig.8|||||||||
19520|Warrego Volcanics|43223|5|Briefly described|Map Legend||Paleoproterozoic|of Flynn Subgroup||||||07-NOV-08
19520|Warrego Volcanics|46991|6|Mentioned|p245|||||||||
19520|Warrego Volcanics|46992|6|Mentioned|Table 1|||||||||
19520|Warrego Volcanics|50353|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Flynn Group. Chert (silicified tuff?); tuff; white weathering siltstone and shale; and fine grained sublithic arenite; thin to medium bedded; laminated.||||||07-NOV-08
19520|Warrego Volcanics|60684|5|Briefly described|p6 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of the Flynn Subgp (Churchills Head Gp). White, pink, mauve, grey and green siltstone, chert and felsic tuff, and possible ignimbrite interbedded with fine- to medium-grained lithic arenite. Correlates with Bernborough Fm. Max. thick: ~550m. I-type section||||||14-APR-15
19520|Warrego Volcanics|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Ooradidgee Group. Chert (silicifed tuff), tuff; siltstone, shale, fine-grained lithic arenite/wacke.  In the Tennant Creek region.||||||14-APR-15
19520|Warrego Volcanics|65209|6|Mentioned|p35 Fig.1, p36|Paleoproterozoic|Paleoproterozoic|||Ooradidgee Group||Is overlain by Wundirgi Formation.||05-JAN-17
19520|Warrego Volcanics|65338|6|Mentioned|p19.|||Undated, but broadly correlated with volcanic rocks of Yungkulungu and Bernborough Formations.||||||
19520|Warrego Volcanics|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Ooradidgee Group.|||Chert (silicified tuff), tuff; siltstone, shale, fine-grained lithic arenite/wacke.|
19520|Warrego Volcanics|69187|5|Briefly described|p53 Fig.2, p54 Fig.3|||Warramunga Province.||Ooradidgee Group||||
19520|Warrego Volcanics|69424|4|Described|p9:3-5, 15-16, 19-20, 39 Fig.9.24|Paleoproterozoic|Paleoproterozoic|Warramunga Province. c.550m thick in type section. Subaerial pyroclastic rocks and waterlain (shallow marine?) reworked equivalents. Lateral equivalent of part of Wundirgi, Monument and Yungkulungu Formations. Age from correlation with Yungkulungu Formation volcanic lithofacies. Minimum age from geological correlation of marker bed overlying Warrego Volcanics being the same as marker bed underlying Bernborough Formation (age near base: 1845+/-4 Ma)|1849 +/- 5 Ma (Smith, 1999).|Ooradidgee Group.||Unconformably overlies Warramunga Formation. Is overlain conformably by Wundirgi Formation.|Siltstone, chert, felsic tuff and probable ignimbrite, interbedded with fine- to medium-grained lithic sandstone.|24-FEB-23
19520|Warrego Volcanics|73124|6|Mentioned|p2 Fig.1|||||Ooradidgee Group||||
19520|Warrego Volcanics|73125|5|Briefly described|p2|Palaeoproterozoic|Palaeoproterozoic|Warramunga Province. Included in Ooradidgee Group.||Tennant Creek Supersuite.||||
19520|Warrego Volcanics|73460|6|Mentioned|p2|||Warramunga Province.||Ooradidgee Group||||
19520|Warrego Volcanics|73590|6|Mentioned|p2|||||||||
19573|Waterbag Creek Formation|9324|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Tolmer Group. Red mudstone with thin arenite layers; abundant halite clasts.||||||
19573|Waterbag Creek Formation|22809|5|Briefly described|17|||||||||
19573|Waterbag Creek Formation|23714|4|Described|p7 Table 1|Proterozoic|Proterozoic|See also page 36. Of Tolmer Group. Litchfield Province. Max. thickness: 30 m.||||||
19573|Waterbag Creek Formation|23715|5|Briefly described|Map legend||Proterozoic|In the Litchfield Porvince||||||
19573|Waterbag Creek Formation|32170|6|Mentioned|Map legend|Adelaidean|Carpentarian|Adelaidean or Carpentarian||||||
19573|Waterbag Creek Formation|32660|5|Briefly described|Table 6|||||||||
19573|Waterbag Creek Formation|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
19573|Waterbag Creek Formation|33377|6|Mentioned|p267|||||||||
19573|Waterbag Creek Formation|39679|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
19573|Waterbag Creek Formation|40852|6|Mentioned|Fig.3.2|||||||||
19573|Waterbag Creek Formation|41661|6|Mentioned|p18|||||||||
19573|Waterbag Creek Formation|43624|6|Mentioned|p37|||Of Tolmer Group.||||||
19573|Waterbag Creek Formation|45022|3|Fully described|p.95||Adelaidean|Of Tolmer Group. On many pages.||||||18-DEC-06
19573|Waterbag Creek Formation|45112|5|Briefly described|Table 10|||||||||
19573|Waterbag Creek Formation|46675|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Tolmer Group.  Interbedded ferruginous sandstone, varicoloured siltstone, silicified limestone, marl; halite casts in sandstone and siltstone.  Conformably overlies Hinde Dolomite.||||||29-NOV-04
19573|Waterbag Creek Formation|46676|14|Not recorded|p.6||Neoproterozoic|U.Proterozoic; unit of Tolmer Group.||||||
19573|Waterbag Creek Formation|48942|3|Fully described|p43|||||||||
19573|Waterbag Creek Formation|64698|4|Described|lithinterp table|Statherian|Orosirian|Age ~1700-1825Ma. Tolmer Group. Max thick 500m. Red mudstone with thin arenite layers, abundant halite casts. Conformably overlies -Pth (Hindrance Dolostone - a misspelling of Hinde Dolostone).||||||07-JAN-09
19573|Waterbag Creek Formation|67779|5|Briefly described|p6 Fig.5.|Paleoproterozoic|Paleoproterozoic|Litchfield Province, Pine Creek Orogen.||Unit in Tolmer Group.||||
19573|Waterbag Creek Formation|69432|5|Briefly described|p17:6|||300-500m thick. Is probably a partial lateral equivalent of Hinde Dolostone. Widespread and locally abundant pseudomorphs of evaporites, and casts and moulds after halite, indicate brine-logged subaerial deposits.||||Conformably overlies Hinde Dolostone.|Dominated by red mudstone and interbedded shale, thinly to medium bedded siltstone, sandstone, dolomitic sandstone and dolostone. Locally contains interbedded ferruginous sandstone, varicoloured siltstone, silicified limestone, marl and siltstone.|12-JUL-16
19573|Waterbag Creek Formation|69673|6|Mentioned|p49|||||Tolmer Group||||
19573|Waterbag Creek Formation|70866|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Tolmer Group.||Conformably overlies Hinde Dolostone.|Red mudstone with thin sandstone layers, abundant halite casts.|
19609|Wattie Group|14019|4|Described|p14, 29|||Siliclastic sucession with subordinate carbonates. Unconformably overlies Limbunya Group; unconformably overlain by Auvergne Group. Max. thickness: 450m. Geological Province: Victoria Basin. Possibly correlated with Nathan Group.||||||
19609|Wattie Group|23216|6|Mentioned|Fig3p5||Mesoproterozoic|||||||
19609|Wattie Group|23809|5|Briefly described|p47 Fig. 42|||Correlates with the Nathan Group (McArthur Basin).  Geological Province: Victoria Basin.||||||
19609|Wattie Group|24122|5|Briefly described|p4 Fig.3|||Geological Province: Victoria Basin.||||||
19609|Wattie Group|24297|3|Fully described|p4|Proterozoic|Proterozoic|Maximum thickness: 450m.  Geological Province: Victoria Basin.   See also p5 Tb. 2.||||||
19609|Wattie Group|24441|5|Briefly described|p1 Fig. 1|Mesoproterozoic|Mesoproterozoic|Unconformably overlies the Limbunya Group (Birrindudu Basin); conformably overlain by Timber Creek Formation (Bullita Group). Geological Province: Victoria Basin.||||||
19609|Wattie Group|24442|5|Briefly described|p50 Fig. 1|||Divided into 7 units.  Geological Province: Victoria Basin.||||||
19609|Wattie Group|28255|3|Fully described|p31, Tb. 11 (opp. p8)|Adelaidean|Adelaidean|Comprises seven formations/units. Unconformably overlies Limbunya Group; conformably overlain by Timber Creek Formation of the Bullita Group. Max. thickness: 400m.||||||18-DEC-06
19609|Wattie Group|29809|6|Mentioned|p418|||||||||
19609|Wattie Group|30003|4|Described|p8, p12|||Characteristic feature of this group is the presence of 10-20% of white graines, clearly visible in hand specimens - composed of microcline and plagioclase crystals, chert, claystone and other rock fragments, and clay aggregates.||||||19-APR-05
19609|Wattie Group|30004|6|Mentioned|Map legend|Proterozoic|Proterozoic|Carpentarian or Adelaidean||||||
19609|Wattie Group|32172|4|Described|p9|||Carpentarian or Adelaidean. Table 1||||||
19609|Wattie Group|32173|5|Briefly described|Map legend|Adelaidean|Carpentarian|Carpentarian or Adelaidean (per legend).||||||17-NOV-04
19609|Wattie Group|32175|5|Briefly described|Map legend|Adelaidean|Adelaidean|||||||02-DEC-04
19609|Wattie Group|32659|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
19609|Wattie Group|32660|4|Described|Table 6|||||||||
19609|Wattie Group|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Sandstone, siltstone, minor dolomite.||||||02-DEC-04
19609|Wattie Group|32701|4|Described|Table 1|||Adelaidean. See p8.||||||18-DEC-06
19609|Wattie Group|32728|6|Mentioned|p16|||||||||
19609|Wattie Group|33374|6|Mentioned|p6|||||||||
19609|Wattie Group|33375|5|Briefly described|p7-8|Adelaidean|Adelaidean|See also Table 1 p8-9.||||||26-APR-05
19609|Wattie Group|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
19609|Wattie Group|33377|5|Briefly described|Table 2|||||||||
19609|Wattie Group|33378|5|Briefly described|Map legend|Adelaidean|Adelaidean|||||||27-APR-05
19609|Wattie Group|36473|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
19609|Wattie Group|37462|4|Described|Table 4.VI|||||||||
19609|Wattie Group|38157|6|Mentioned|p284|||||||||
19609|Wattie Group|42012|6|Mentioned|p13|||||||||
19609|Wattie Group|45112|3|Fully described|p18|||p18-19.||||||18-DEC-06
19609|Wattie Group|45140|6|Mentioned|p13, Appx.p19|||Victoria River region.||||Unconformably overlies Limbunya Group.||
19609|Wattie Group|46864|6|Mentioned|Fig.4|||||||||
19609|Wattie Group|48938|4|Described|p21|||||||||
19609|Wattie Group|48943|2|Defined|p39|Adelaidean|Adelaidean|||||||
19609|Wattie Group|60006|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Victoria Basin. Undifferentiated micaceous siltstone, sandstone, minor dolostone.||||||
19609|Wattie Group|60589|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Includes seven named units.  Consists of siltstone, sandstone, dolostone.    Geological Province: Victoria Basin.||||||24-NOV-04
19609|Wattie Group|60672|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Mainly dolostone, sandstone and siltstone. Unconformably overlies Limbunya Group. Overlain unconfromably by Bullita Group. Geological Province: Victoria Basin.||||||11-JAN-05
19609|Wattie Group|60682|4|Described|piii|Paleoproterozoic|Paleoproterozoic|Conformably overlain by Bullita Group. Age: 1610-1570Ma. Undifferentiated micaceous siltstone, sandstone and minor dolostone. Geological Province: Victoria Basin.||||||07-NOV-08
19609|Wattie Group|60685|4|Described|p4|Mesoproterozoic|Paleoproterozoic|Sandstone, siltstone, dolostone. Unconformably overlies Limbunya Group; conformable below Bullita Group. Age: 1.61-1.57Ga. Max. Thickness: 450m. Geological Province: Victoria Basin.||||||07-NOV-08
19609|Wattie Group|64724|5|Briefly described|p45 Fig.5, p46|Statherian|Statherian|Victoria River and Birrindudu Basin unit deposited as part of sedimentation in the Isa Superbasin (1660-1590 Ma)||||||
19609|Wattie Group|65331|5|Briefly described|Map legend + overview geology map legend|Mesoproterozic|Mesoproterozic|Of Victoria Basin. Micaceous siltstone, sandstone, minor dolostone||||||
19609|Wattie Group|65342|5|Briefly described|pp10-11.|||Victoria Basin.|||Includes Wickham, Burtawurta, Mount Sanford and Gibbie Formations; Hughie, Neave and Seale Sandstones.|Is overlain by Bullita Group.|Mainly a siliciclastic succession with minor carbonate intervals.|
19609|Wattie Group|67151|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Birindudu Basin.|||Includes Wickham, Burtawurta, Mount Sanford and Gibbie Formations; Hughie, Neave and Seale Sandstones.|Unconformably overlies Limbunya Group. Is unconformably overlain by Bullita Group.||
19609|Wattie Group|68733|5|Briefly described|p177-179, p181 Fig.3, p184, p185 Tb.4|||Previously included in the Victoria Basin by Cutovinos et al. (2002). Now included in the Birrindudu Basin due to a recent subdivision by the NGTS (Dunster and Ahmad 2013).|||Includes Seale, Neave, Hughie Sandstones; Gibbie, Mount Sanford, Burtawurta, Wickham Formations.|||06-DEC-17
19609|Wattie Group|69417|5|Briefly described|p2:5-6|Calymmian|Calymmian|Southern Birrindudu Basin.|||||Includes stromatolitic carbonate rocks and sandstone deposited in sag basins.|12-JUL-16
19609|Wattie Group|69432|4|Described|p17:1-3, 9, 13, 15|||Birrindudu Basin. The base of this unit was selected (by Dunster et al., 2000 and Cutovinos et al., 2002) as the break between the Birrindudu and Victoria Basins. This study places that boundary at the base of the Auvergne Group. A mostly recessive, siliciclastic succession with subordinate carbonate rocks. Age is poorly constrained. Total thickness over 450m, thickening to the E and N. Is gently folded into broad domes, anticlines and synclines 10-50km across. Exploration target for base metals. May have been the source of oil in Timber Creek Formation.|||Wickham, Burtawurta, Mount Sanford, Gibbie Formations; Hughie, Neave, Seale Sandstones.|Unconformably overlies Limbunya Group. Is overlain unconformably by Bullita Group.|Siliciclastic, with subordinate carbonate, rocks.|12-JUL-16
19609|Wattie Group|69441|6|Mentioned|p26:1|||The unconformity at the base of this unit used to mark the separation between the Birrindudu and overlying Victoria Basins (Dunster et al., 2000; Cutovinos et al., 2002). This study relocates the boundary between the Tijunna and Auvergne Groups.||||||12-JUL-16
19609|Wattie Group|69445|5|Briefly described|p30:4|Proterozoic|Proterozoic|Victoria River region, Birrindudu Basin.||||Is overlain unconformably by Antrim Plateau Volcanics.||12-JUL-16
19609|Wattie Group|69673|6|Mentioned|p3 fig 2, p47, p48 fig 35, p51|Paleoproterozoic|Paleoproterozoic||||Includes Wickham Formation, Burtawurta Formation, Hughie Sandstone, Mount Sanford Formation, Neave Sandstone, Gibble Formation, Seale Sandstone|Unconformably overlies Limbunya Group, unconformably overlain by Bullita Group||
19609|Wattie Group|70206|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Birindudu Basin [misspelling of Birrindudu Basin].|||||Micaceous siltstone, sandstone and minor dolostone.|18-JUL-16
19609|Wattie Group|70655|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Birindudu Basin.|||Includes Seale Sandstone, Gibbie Formation, Neave Sandstone, Mount Sandford Formation, Hughie Sandstone, Burtawurta Formation, Wickham Formation.|Unconformably overlies Limbunya Group. Is unconformably overlain by Bullita Group, Auvergne Group.|Micaceous siltstone, sandstone, minor dolostone.|
19609|Wattie Group|70848|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Victoria Basin.|||Wickham Formation.|||
19609|Wattie Group|70854|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.|||Wickham, Burtawurta, Mount Sanford, Gibbie Formations; Hughie, Neave, Seale Sandstones.|Unconformably overlies Limbunya Group. Is overlain unconformably by Bullita Group.|Sandstone, siltstone, claystone, chert, dolostone, conglomerate.|
19609|Wattie Group|70855|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.|||Wickham, Burtawurta, Mount Sanford, Gibbie Formations; Hughie, Neave, Seale Sandstones.|Unconformably overlies Limbunya Group. Is overlain by Timber Creek Formation (Bullita Group).|Sandstone, siltstone, claystone, dolostone, chert, conglomerate.|
19609|Wattie Group|70968|5|Briefly described|p6, p130, p132|||Birrindudu Basin.||||Is overlain unconformably by Roper Group. Equivalent of the Nathan Group.||
19609|Wattie Group|71059|5|Briefly described|p7|||Birrindudu Basin.||||Is overlain unconformably by Roper Group. Equivalent to Nathan Group (McArthur Basin).||
19609|Wattie Group|71169|5|Briefly described|p71|Calymmian|Calymmian|North Australian Craton.|c. 1550-1400 Ma|||||
19609|Wattie Group|71302|5|Briefly described|p1-3,6,15,22,72-74||Paleoproterozoic|Of Birindudu Basin.|||Includes Seale Sandstone, Gibbie Formation, Neave Sandstone, Mount Sanford Formation, Hughie Sandstone, Burtawurta Formation, Wickham Formation.|Overlain by Bullita Group. Underlain by Limbunya Group.||
19609|Wattie Group|71374|6|Mentioned|p2|||Birrindudu Basin.||||||
19609|Wattie Group|72373|5|Briefly described|p2,36,39|Mesoproterozoic|Mesoproterozoic|Of Birrindudu Basin. Broadly equivalent to Favenc package, Nathan, Mount Rigg, Balma groups and Karns Dolostone (McArthur Basin) and Namerinni Group (Tomkinson province).||||||
19609|Wattie Group|72718|6|Mentioned|p7, p9|||Birrindudu Basin. Equivalent to the Favenc package.|||Seale Sandstone, Gibbie Formation, Neave Sandstone, Mount Sanford Formation, Hughie Sandstone, Burtawurta Formation, Wickham Formation|Unconformably[?] underlain by Killaloc Formation (Limbunya Group). Overlain by Timber Creek Formation (Bullita Group).||
19609|Wattie Group|73083|6|Mentioned|p30||||||Wickham Formation|Unconformably underlain by Limbunya Group.||
19643|Weaber Group|13194|4|Described|p388 Tb. 4-16, p382 fig 4-59|Upper Carboniferous|Tournaisian|600-2400m thick upward coarsening and shallowing sequence.||||||
19643|Weaber Group|22814|5|Briefly described|fig2|Carboniferous|Carboniferous|||||||
19643|Weaber Group|23858|5|Briefly described|p919|||Geological Province: Bonaparte Basin.  Max. thickness: 2400 m.||||||22-DEC-06
19643|Weaber Group|24503|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Sandstone, limestone, and minor conglomerate, shale and siltstone.  Geological Province: Bonaparte Basin.||||||
19643|Weaber Group|24569|5|Briefly described|p248 Fig. 3|Namurian|Visean|Includes the Point Spring Sandstone, Tanmurra and Milligans Formations. Geological Province: Petrel Sub-basin.||||||02-MAR-05
19643|Weaber Group|32701|6|Mentioned|p17|||Refers Traves (1955)||||||
19643|Weaber Group|40993|6|Mentioned|Fig.1|||||||||
19643|Weaber Group|41459|6|Mentioned|Fig.2|||||||||
19643|Weaber Group|41532|4|Described|p292|||||||||
19643|Weaber Group|41598|6|Mentioned|p412|||||||||
19643|Weaber Group|41731|6|Mentioned|Fig.3|||||||||
19643|Weaber Group|41864|4|Described|p123|||||||||
19643|Weaber Group|41865|6|Mentioned|Map legend|Westphalian|late Tournaisian|||||||
19643|Weaber Group|42055|4|Described|Fig.1 P52|||||||||
19643|Weaber Group|42056|4|Described|p96|||||||||
19643|Weaber Group|42442|3|Fully described|p11|||||||||
19643|Weaber Group|42933|5|Briefly described|Fig.94 p258|||||||||
19643|Weaber Group|43236|6|Mentioned|p14,Fig.13.|Namurian|Visean|||||||
19643|Weaber Group|43661|6|Mentioned|Fig.3|||||||||
19643|Weaber Group|44965|14|Not recorded|Not recorded|||||||||
19643|Weaber Group|45038|14|Not recorded|p.27,30,78,86,94||Permian|Perm?||||||
19643|Weaber Group|48938|6|Mentioned|p75|||Refers Traves.||||||
19643|Weaber Group|60006|5|Briefly described|Map Legend|Namurian|Visean|Geological Province: Bonaparte Basin. Sandstone, siltstone, conglomerate, shale, limestone||||||22-JUL-04
19643|Weaber Group|60364|5|Briefly described|p184|Early Carboniferous|Early Carboniferous|Geological Province: Bonaparte Basin.||||||
19643|Weaber Group|60386|6|Mentioned|p297|Carboniferous|Carboniferous|Roebuck/Canning Basin. Deltaic - nearshore - shelf. Post Alice Springs Orogeny.||||||
19643|Weaber Group|60682|4|Described|piii|Carboniferous|Carboniferous|Unconformably overlies Langfield Group. Unconformably overlain by Kulshill Group. Max. thickness: >2400m. Geological Province: Bonaparte Basin. Shoreface, deltaic and fluvial deposits.||||||19-DEC-06
19643|Weaber Group|61542|1|Redefined|p276, p277 Fig. 2|Early Carboniferous|Early Carboniferous|Of Mory and Beere (1988).Originally incl: Milligans+Waggon Creek Fms, Utting Calcarenite, Burvill+Tanmurra Fms+Point Spring Sst. Here revised to exclude Pt Spring Sst; Waggon Ck Fm is relegated to a facies association (mbr). New subdivisions introduced.||||||07-FEB-11
19643|Weaber Group|62837|5|Briefly described|Stratigraphic columns|Namurian|Tournaisian|Includes Milligans and Tanmurra Formations and Point Spring Sandstone.  Age: <345-~311Ma. Geological Province:  Petrel Sub-basin (offshore).||||||01-MAR-10
19643|Weaber Group|64580|4|Described|map legend|Pennsylvanian|Mississippian|Undivided; siltstone, shale, sandstone, conglomerate; subordinate carbonate; includes TANMURRA, MILLIGANS, WAGGON CREEK and BURVILL FORMATIONS, UTTING CALCARENITE, and POINT SPRING SANDSTONE.||||||09-DEC-08
19643|Weaber Group|64630|5|Briefly described|p31 Fig.2|Serpukhovian|Visean|Province: Bonaparte Basin. Unconformably underlies the Wadeye Group. Palynology age: G. maculosa to S. ybertii.||||||18-JAN-10
19643|Weaber Group|64689|5|Briefly described|p16|Carboniferous|Carboniferous||||Includes the Milligans Formation.|||
19643|Weaber Group|64694|5|Briefly described|p231, p232, p233, p239, p249|Namurian|Tournaisian|Bonaparte Basin.||Unit in Weaber Group.|Includes Waggon Creek, Lower and Upper Milligans, Burvill, Tanmurra Formations; Utting Calcarenite; Point Spring Sandstone.|Overlies the Langfield Group unconformably.||
19643|Weaber Group|65331|5|Briefly described|Map legend + overview geology map legend|Bashkirian|Visean|Of Bonaparte Basin. Includes Point Spring Sandstone, Burvill Formation, Milligans Formation. Age shown as Visean to Namurian. Sandstone, siltstone, conglomerate, shale, limestone||||||
19643|Weaber Group|66498|6|Mentioned|p48|||Bonaparte Basin, WA.|||Utting Calcarenite.|||
19643|Weaber Group|67354|6|Mentioned|p73. ||||||Includes Wadeye Sub-Group and Sunbird Formation.|||
19643|Weaber Group|69099|4|Described|500k_geologyp08_lut.csv|Pennsylvanian|Mississippian||||Includes Tanmurra, Milligans, Waggon Creek and Burvill Formations, Utting Calcarenite, and Point Spring Sandstone||siltstone, shale, sandstone, conglomerate; subordinate carbonate;|
19643|Weaber Group|69165|4|Described|500k_geologyp08_lut.csv|Pennsylvanian|Mississippian||||Includes Tanmurra Formation, Milligans Formation, Burvill Formation, Waggon Creek Formation, Utting Calc-arenite, Point Spring Sandstone||Undivided; siltstone, shale, sandstone and conglomerate; subordinate carbonate.|
19643|Weaber Group|69422|6|Mentioned|p7:2 Fig.7.2|Carboniferous|Carboniferous|Bonaparte Basin.||||||12-JUL-16
19643|Weaber Group|69452|4|Described|p36:4, 7, 9, 11-17|Early Carboniferous|Early Carboniferous|Traves (1955); Gorter et al. (2005). Petrel Sub-basin, Bonaparte Basin. Onshore and offshore. c.2400m thick. Originally included Point Spring Sandstone as the topmost unit; since assigned to the Wadeye Group by Gorter et al. (2005). Latest Tournaisian to early Serpukhovian age.|||Milligans, Yow Creek, Burvill, Tanmurra, Sunbird Formations; Utting Calcarenite; Kingfisher Shale; Sandbar Sandstone.|Overlies Ningbing Group disconformably and Langfield Group unconformably. Is overlain unconformably by the Wadeye Group.|A complex succession of clastic and carbonate sedimentary rocks, separated by several unconformities.|12-JUL-16
19643|Weaber Group|69634|5|Briefly described|500k_geologyp08_lut.csv|Pennsylvanian|Mississippian||||Includes Tanmurra Formation, Milligans Formatrion, Waggon Creek Formation, Utting Calcarenite and Point Springs Sandstone.||Undivided; siltstone, shale, sandstone, conglomerate; subordinate carbonate|
19643|Weaber Group|69653|6|Mentioned|p10, 14-15|Carboniferous|Carboniferous|Petrel Sub-basin.|||Milligans, Yow Creek, Tanmurra, Sunbird Formations; Utting Calcarenite; Kingfisher Shale; Sandbar Sandstone.|Overlies Langfield Group. Is overlain by Kulshill Group.||
19643|Weaber Group|69673|6|Mentioned|p166 fig 136, p171, p179|Carboniferous|Carboniferous|Up to 2400m thick.|||Includes Milligans Formation, Yow Creek Formation, Utting Calcarenite, Kingfisher Shale, Tanmurra Formation, Sandbar Sandstone, Sunbird Formation|Overlain by Kinmore Group, Wadeye Group, unconformably overlies Langfield Group||
19643|Weaber Group|70061|5|Briefly described|Petrel Sub-basin; Fig.3|Serpukhovian|Tournaisian|See also Regional geology: Fig.8, p8. Intraformational seal.|||Milligans, Yow Creek, Tanmurra and Sunbird Formations; Utting Calcarenite; Kingfisher Shale; Sandbar Sandstone.|Overlies Bonaparte Formation. Is overlain by Wadeye Group.||12-JUL-16
19643|Weaber Group|70064|5|Briefly described|Regional Fig. 6|Bashkirian|Tournaisian|Caswell-Barcoo Sub-basins, Browse Basin.||||Is overlain by Kulshill Group.||12-JUL-16
19643|Weaber Group|70154|5|Briefly described|500k_interpgeop14_lut.csv|Pennsylvanian|Tournaisian||298-350 Ma||||Siltstone, shale, sandstone, conglomerate; subordinate carbonate|
19643|Weaber Group|70206|5|Briefly described|Map Legend, cross-sect.|Carboniferous|Carboniferous|Bonaparte Basin.|||Includes Point Spring Sandstone, Burvill Formation, Milligans Formation, Waggon Creek Formation, Tanmurra Formation.|Unconformably overlies Langfield Group.||
19643|Weaber Group|70826|6|Mentioned|p6 tbl 3|Carboniferous|Carboniferous|Southern Bonaparte Basin.||||||
19643|Weaber Group|70851|6|Mentioned|p17|||||||||
19643|Weaber Group|71146|5|Briefly described|p6, p34,  p43 fig 33|Visean|Tournaisian|Bonaparte Basin. Believed to be partially equivalent to the Williambury Formation.||||Unconformably overlies the Bonaparte Formation and the Langfield Group. Unconformably overlain by the Wadeye Group.|Mudstone, sandstone and carbonate.|
19643|Weaber Group|71267|4|Described|GEOL_LUT_CSV files|Pennsylvanian|Tournaisian|Of Burt Range Shelf; Carlton Shelf, Southern Bonaparte Basin. Events: Gondwana breakup-northern NW Shelf (320-138 Ma); Alice Springs Orogeny (450-295 Ma). See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv.|350-298.9 Ma (biostrat)||Includes Milligans Formation, Burvill Formation.||Quartz sandstone, siltstone, shale, minor limestone and conglomerate. Shoreface, deltaic and fluvial deposits|
19643|Weaber Group|72034|5|Briefly described|500k_interpgeop16_lut|Pennsylvanian|Tournaisian|Burt Range Shelf; Carlton Shelf, Southern Bonaparte Basin.  Age from biostratigraphy.|||||Siltstone, shale, sandstone, conglomerate; subordinate carbonate.|
19643|Weaber Group|73117|6|Mentioned|p15|Visean|Visean|Bonaparte Basin, southern.|||Sunbird Formation, Sandbar Sandstone, Tanmurra Formation, Kingfisher Shale, Burvill Formation, Utting Calcarenite, Yow Creek Formation, Milligans Formation.|||
19658|Weberra Granite|22438|3|Fully described|p545-547, Fig.12|Statherian|Statherian|Intrudes the uppermost sequences of the Leichhardt Superbasin.||||||19-DEC-06
19658|Weberra Granite|22585|6|Mentioned|Fig1 P736, Fig3||Statherian|||||||
19658|Weberra Granite|22665|6|Mentioned|P230|||||||||
19658|Weberra Granite|23031|5|Briefly described|24|Paleoproterozoic|Paleoproterozoic|Geological province: Mount Isa Fold Belt.||||||07-NOV-08
19658|Weberra Granite|23363|5|Briefly described|344 Fig.3|||||||||
19658|Weberra Granite|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Fold Belt.||||||07-NOV-08
19658|Weberra Granite|23396|6|Mentioned|p426|||||||||
19658|Weberra Granite|23398|5|Briefly described|p433 Fig.2|Statherian|Statherian|Age: 1698+/-24Ma.||||||19-DEC-06
19658|Weberra Granite|23408|6|Mentioned|p513 Fig. 2|||||||||
19658|Weberra Granite|23466|5|Briefly described|p275|||||||||
19658|Weberra Granite|23545|5|Briefly described|Fig 1 p604|||||||||
19658|Weberra Granite|23767|5|Briefly described|p1954 Fig. 1a|||Geological Province: Mount Isa Superbasin. See also p1955.||||||
19658|Weberra Granite|23776|5|Briefly described|p707 Fig 4|Statherian|Statherian|Age: 1698+/-24 Ma. Of McArthur Group.||||||19-DEC-06
19658|Weberra Granite|24197|5|Briefly described|p28, p95 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Of the Fiery Supersuite. Age: 1678Ma. Geological Province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
19658|Weberra Granite|24307|5|Briefly described|p978|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Block||||||07-NOV-08
19658|Weberra Granite|24308|5|Briefly described|p987 Fig. 2|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
19658|Weberra Granite|24419|5|Briefly described|p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Of the Fiery Suite.  Geological Province: Western Fold Belt, Lawn Hill Subprovince (Mount Isa Orogen).||||||07-NOV-08
19658|Weberra Granite|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
19658|Weberra Granite|32660|5|Briefly described|Table 5|||||||||
19658|Weberra Granite|32959|6|Mentioned|Fig.21|||||||||
19658|Weberra Granite|33387|6|Mentioned|p349|||||||||
19658|Weberra Granite|33900|5|Briefly described|p22|||||||||
19658|Weberra Granite|35074|6|Mentioned|Fig.2|||||||||
19658|Weberra Granite|36548|6|Mentioned|p513|||||||||
19658|Weberra Granite|37459|6|Mentioned|p423|||||||||
19658|Weberra Granite|37462|4|Described|Table4.VII|||||||||
19658|Weberra Granite|37568|6|Mentioned|p83|||||||||
19658|Weberra Granite|38232|6|Mentioned|p89|||||||||
19658|Weberra Granite|38348|6|Mentioned|p6|||||||||
19658|Weberra Granite|39445|5|Briefly described|Table 2|||See also p36 and p40.||||||19-DEC-06
19658|Weberra Granite|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Medium to coarse granite, leucogranite, medium graphic granite. May be partly coeval with Fiery Creek Volcanics.||||||15-JUN-06
19658|Weberra Granite|39944|6|Mentioned|p229|||||||||
19658|Weberra Granite|40840|6|Mentioned|Map legend|||||||||
19658|Weberra Granite|41465|6|Mentioned|p12|||||||||
19658|Weberra Granite|41862|6|Mentioned|p474|||||||||
19658|Weberra Granite|41978|6|Mentioned|p502|||||||||
19658|Weberra Granite|41979|4|Described|p522|||||||||
19658|Weberra Granite|42565|5|Briefly described|Table 2 P7|||||||||
19658|Weberra Granite|43010|5|Briefly described|p81|||||||||
19658|Weberra Granite|44213|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
19658|Weberra Granite|44257|14|Not recorded|p22|||||||||
19658|Weberra Granite|44271|14|Not recorded|p37,38,45,52,53|||Intrudes Ploughed Mountain Beds.||||||
19658|Weberra Granite|44274|14|Not recorded|Tb.2,p13,map||Paleoproterozoic|||||||07-NOV-08
19658|Weberra Granite|44275|14|Not recorded|Map Legend|||||||||
19658|Weberra Granite|44751|14|Not recorded|p30||Precambrian|||||||
19658|Weberra Granite|44989|2|Defined|p.154-6|||Tb.IV. On many pages. Intrudes Ploughed Mountain Beds. (E54-9,13).||||||
19658|Weberra Granite|45166|5|Briefly described|p33|||||||||
19658|Weberra Granite|45287|14|Not recorded|p.229|||||||||
19658|Weberra Granite|46960|6|Mentioned|p216|||||||||
19658|Weberra Granite|47083|4|Described|p21|||Previously included a pluton now mapped as Yeldham Granite. Comagmatic with Fiery Creek Volcanics. Intrudes Quilalar Formation and Myally Subgroup. A-type granite.||||||29-APR-16
19658|Weberra Granite|49041|5|Briefly described|Table 1|||Mention Table 4||||||
19658|Weberra Granite|50536|5|Briefly described|p1.4, 7.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Fiery Suite. Age: 1678-1698 +/- 24Ma (U-Pb).||||||07-NOV-08
19658|Weberra Granite|61929|5|Briefly described|p128 Fig. 2|||||||||
19658|Weberra Granite|61936|5|Briefly described|p194 Fig. 6|Paleoproterozoic|Paleoproterozoic|Age: ca1700Ma. See also p192 Fig. 5.||||||07-NOV-08
19658|Weberra Granite|62988|5|Briefly described|p34|Paleoproterozoic|Paleoproterozoic|Part of the ~1710Ma Fiery Event, together with Fiery Creek Volcanics. Geological Province: Mount Isa Inlier.||||||07-NOV-08
19658|Weberra Granite|63023|5|Briefly described|p1035|Paleoproterozoic|Paleoproterozoic|Age: ca 1700Ma. Geological Province: Western Fold Belt.||||||07-NOV-08
19658|Weberra Granite|63109|6|Mentioned|p1109|||Age: ~1710Ma (Hone et al., 1987).||||||
19658|Weberra Granite|63110|6|Mentioned|p1141 Fig. 17|Statherian|Statherian|Geological Province: Calvert Superbasin.||||||11-JUN-08
19658|Weberra Granite|63866|5|Briefly described|p57|Statherian|Statherian|Calvert Superbasin.|1711 +/-3 Ma (Neumann et al., 2006)|||||
19658|Weberra Granite|64250|6|Mentioned|p11 fig 3, p19, p21, p24|||Western Fold Belt, Mount Isa Inlier. Co-magmatic with Fiery Creek Volcanics.|1711 +/- 3 Ma|||||
19658|Weberra Granite|65228|5|Briefly described|Figs.04, 10.|Statherian|Statherian|Mount Isa area. Mis-spelt as Webbera in Fig.10. Poor time constraint. Probably coeval with Fiery Creek Volcanics (1709 +/- 3 Ma).|1698 +/- 24 Ma.|||||
19658|Weberra Granite|65396|6|Mentioned|p82, p175, p187, p193, p197, p241|Statherian|Statherian|Calvert Superbasin. Cover Sequence 2. Co-magmatic with 1709 +/- 3 Ma Fiery Creek Volcanics.|1698 +/- 24 Ma|||||
19658|Weberra Granite|66844|6|Mentioned|p245|Statherian|Statherian|Isa Superbasin. Age from SHRIMP dating.|1695+\-24 Ma|||||
19658|Weberra Granite|67323|5|Briefly described|GIS attrib tbl, p11, p24, p33, p41, p107|Paleoproterozoic|Paleoproterozoic|See also Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Weberra Igneous Event; initiation of Calvert Superbasin. Mount Oxide Domain, Mount Isa Inlier. Forms core of the Fiery Creek Dome. Included in a list of Suites on p41.|1711+/-3 Ma (Neumann et al. 2009).|||Coeval with Fiery Creek Volcanics.|Medium to coarse granite, leucogranite, medium graphic granite.|
19658|Weberra Granite|68021|5|Briefly described|p135 fig 4, p136|Statherian|Statherian||1710 Ma|||Intrudes Bigie Formation and possibly Quilalar Formation.||
19658|Weberra Granite|68542|6|Mentioned|p1 |||||||||
19658|Weberra Granite|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province.||||||
19658|Weberra Granite|68576|6|Mentioned|Q_2: p1|Paleoproterozoic|Paleoproterozoic|Mount Isa area.||||||
19658|Weberra Granite|68732|5|Briefly described|p165 Fig.3|Statherian|Statherian|Of the Big Supersequence. Igneous crystallisation age. Age assumed to be determined with SHRIMP.|1711 +/- 3 Ma|||||04-APR-18
19658|Weberra Granite|69222|6|Mentioned|p222 Fig.2, p225 Tb.2|Statherian|Statherian|Heat flow values given.|1698 +/- 24 Ma (Wyborn et al., 1998).|||||09-FEB-18
19658|Weberra Granite|69370|6|Mentioned|p307 Fig.2|Statherian|Statherian|Western Fold Belt, Mount Isa Block.||||Intrudes Surprise Creek Formation.||25-JAN-19
19658|Weberra Granite|69591|5|Briefly described|p28, p37-39, p59, p106|Paleoproterozoic|Paleoproterozoic|Mount Oxide Domain, Calvert Superbasin. Syn-extensional. Forms the northern exposure of a NE-trending belt of laccoliths in the footwall of the Fiery Creek Fault Zone. Coeval with the Fiery Creek Volcanics. Wyborn et al. (1998) dated this unit at 1698 +/- 28 Ma.|1710 Ma.||||Medium to coarse granite, leucogranite, medium graphic granite.|
19658|Weberra Granite|70858|6|Mentioned|p31|Paleoproterozoic|Paleoproterozoic|Calvert Superbasin.|1710 Ma.|||||
19658|Weberra Granite|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1711+/-3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
19658|Weberra Granite|71799|5|Briefly described|p154|Statherian|Statherian|Lawn Hill Platform.|1711 +/- 3 Ma (Neumann et al, 2006)|||||
19658|Weberra Granite|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as being located in the central part of the South Nicholson Basin. Age given as U-Pb zircon igneous crystallisation age.|1711 +/-3 Ma|||||
19658|Weberra Granite|72889|6|Mentioned|p6 Fig.i.|||||||||
19658|Weberra Granite|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|U-Pb zircon igneous crystallisation age (Ma) shown.|1711 +/- 3 Ma|||Shown as younger than Carrara Range Group.||
19658|Weberra Granite|73042|6|Mentioned|p4|Statherian|Statherian|South Nicholson Basin region, Calvert Superbasin. Geochronology is a U-Pb zircon igneous crystallisation age.|1711 +/- 3 Ma (see Fig.1.2)|||Partly overlain(?) by Surprise Creek Formation unconformably.||
19658|Weberra Granite|73413|6|Mentioned|p3|||Mount Isa Inlier, Western Fold Belt, Lawn Hill Platform. [Written as Weberra Granitte].||||||
19716|Welltree Metamorphics|9324|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Biotite gneiss, marble, para-amphibolite, calc-silicate gneiss.||||||07-NOV-08
19716|Welltree Metamorphics|9579|5|Briefly described|Map Sheet|Paleoproterozoic|Paleoproterozoic|Early Proterozoic age.||||||
19716|Welltree Metamorphics|22479|5|Briefly described|fig1p2|Orosirian|Orosirian|Placed in Litchfield province||||||
19716|Welltree Metamorphics|22632|5|Briefly described|p520,2|Neoproterozoic|Proterozoic|Sn-Ta pegmatite host||||||
19716|Welltree Metamorphics|22809|6|Mentioned|3|Proterozoic|Proterozoic|||||||
19716|Welltree Metamorphics|22810|4|Described|P15, Table2 P4|||Metamorphic equivalent of Burrell Creek Formation||||||
19716|Welltree Metamorphics|22813|5|Briefly described|Map|Paleoproterozoic|Paleoproterozoic|Biotite gneiss, marble, para-amphibolite, calcsilicate gneiss.||||||07-NOV-08
19716|Welltree Metamorphics|23714|4|Described|p9|Proterozoic|Proterozoic|See also page 7 Table 1. Litchfield Province.||||||
19716|Welltree Metamorphics|23715|5|Briefly described|Map legend||Proterozoic|In the Litchfield Province||||||
19716|Welltree Metamorphics|23733|5|Briefly described|p32 Fig. 19|||||||||
19716|Welltree Metamorphics|24001|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Quartz feldspar biotite gneiss, quartzite.||||||
19716|Welltree Metamorphics|24047|5|Briefly described|p5 Fig.4|Paleoproterozoic|Paleoproterozoic|Gneiss, schist, amphibolite.  Geological Province: Pine Creek Orogen.||||||07-NOV-08
19716|Welltree Metamorphics|39803|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
19716|Welltree Metamorphics|40492|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
19716|Welltree Metamorphics|40493|5|Briefly described|Table 1|||||||||
19716|Welltree Metamorphics|40495|4|Described|p9|||||||||
19716|Welltree Metamorphics|40764|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
19716|Welltree Metamorphics|40765|3|Fully described|p3|||Mention Fig.3||||||
19716|Welltree Metamorphics|40808|4|Described|p15|||Mention p3.||||||19-DEC-06
19716|Welltree Metamorphics|40809|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
19716|Welltree Metamorphics|41304|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
19716|Welltree Metamorphics|41305|4|Described|p18|||||||||
19716|Welltree Metamorphics|41980|4|Described|p571|||See also p576.||||||19-DEC-06
19716|Welltree Metamorphics|42014|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
19716|Welltree Metamorphics|50586|6|Mentioned|p3.3, 6.2|||Intruded by Allia Suite, Wagait Suite.||||||
19716|Welltree Metamorphics|62375|5|Briefly described|p10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Gneiss, schist, amphibolite. Geological Province: Pine Creek Orogen.||||||09-FEB-10
19716|Welltree Metamorphics|63866|5|Briefly described|p105, p107|Orosirian|Orosirian|Litchfield Province, Pine Creek Orogen. Psammopelitic rocks dominated the protoliths of these rocks. Monazites in this unit records a second phase of metamorphism in the province at 1812 +/- 3 Ma (Carson et al., in press).|ca. 1876-1861 Ma (Maximum depositional ages)|||||
19716|Welltree Metamorphics|64677|5|Briefly described|v, p1, p8-10, p42-43|||Pine Creek Orogen. Mid-upper amphibolite facies metasedimentary rocks. A conservative age: the youngest zircon was dated at 1825 +/- 32 Ma.|1865 +/- 4 Ma (protolith maximum deposition age).||||Pelitic schist with garnet porphyroblasts.|
19716|Welltree Metamorphics|64698|4|Described|lithinterp table|Orosirian|Paleoproterozoic|Age ~1860-2500Ma. Quartz-feldspar-biotite gneiss garnet sillimanite andalusite, quartzitic gneiss, quartzite, minor quartz-feldspar-muscovite gneiss; Graphitic ferruginous schist, gneiss and metaquartzite, common andalusite.||||||07-JAN-09
19716|Welltree Metamorphics|64722|5|Briefly described|p10|||Of Litchfield Province of Pine Creek Region. Underwent medium to high grade metamorphism at 1813 +/- 3 Ma. This unit plus Fog Bay and Hermit Creek Metamorphics are correlated with Finniss River Group.||||||11-APR-12
19716|Welltree Metamorphics|64730|6|Mentioned|p125 Fig. 3|Paleoproterozoic|Paleoproterozoic|In the Litchfield Province. Shown as lateral equivalent of Finniss River Group.||||||03-MAY-12
19716|Welltree Metamorphics|64731|4|Described|p145, p149-151, 158, 161-164|Paleoproterozoic|Paleoproterozoic|Of Litchfield Province. Timing of fabric development and peak (or near-peak) metamorphism of the Welltree Metamorphics: 1813+/-3 Ma.|||Includes Sweets Member.|In faulted contact with Fog Bay Metamorphics.||12-APR-12
19716|Welltree Metamorphics|64956|6|Mentioned|p65|||Intruded by Two Sisters Granite and Wagait Granite.||||||07-FEB-11
19716|Welltree Metamorphics|65232|5|Briefly described|p6 Fig. 5, App. 2|Palaeoproterozoic|Palaeoproterozoic|Gneiss, schist, amphibolite. General lithology given for three units including Hermit Creek, Fog Bay and Welltree Metamorphics.||||||09-FEB-10
19716|Welltree Metamorphics|65339|6|Mentioned|p5 Fig.4. ||||||||Gneiss, schist, para-amphibolite.|
19716|Welltree Metamorphics|65556|4|Described|p2 Tb.1, p4, p11, p13-14, p45, p53|||Litchfield Province, Pine Creek Orogen. Mid- to upper-amphibolite-facies, graphitic, garnet-feldspar-biotite+/-sillimanite+/-magnetite gneiss and quartzo-feldspathic mica schist, quartzitic gneiss and quartzite. SHRIMP U-Pb monazite age of 1813+/-3 Ma dates metamorphism. Poorly exposed east of Tom Turners Fault.||||||
19716|Welltree Metamorphics|67186|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Of Cosmo Supergroup? Shown as same age as Finniss River Group.|||||Quartz-feldspar-biotite gneiss; garnet-sillimanite-andalusite quartzitic gneiss; quartzite; marble, in places graphitic; para-amphibolite; calc-silicate gneiss; minor quartz-feldspar-muscovite gneiss.|23-NOV-11
19716|Welltree Metamorphics|67232|3|Fully described|p3, p4, p5, p35.|Paleoproterozoic|Paleoproterozoic|Litchfield Province, Pine Creek Orogen. Mid- to upper-amphibolite facies, peaking at 1813 Ma. Limited exposure east of the Tom Turners Fault in the NE of the Province. Correlated with younger detrital zircon spectra in Burrell Creek Formation. The age quoted is a U-Pb SHRIMP maximum depositional age for the sedimentary protolith to this unit.|1865 +/- 4 Ma (Worden et al. 2006a)/|||Possibly intruded by Keri Metamorphics.|Mid-upper amphibolite facies garnet gneiss, schist and quartzite.|
19716|Welltree Metamorphics|67564|5|Briefly described|p9 Fig.4.|Paleoproterozoic|Paleoproterozoic|Litchfield Province, Pine Creek Orogen.|||||Gneiss, schist, amphibolite.|
19716|Welltree Metamorphics|67779|5|Briefly described|p5 Fig.4(b).|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||Unit in Cosmo Supergroup.||||
19716|Welltree Metamorphics|69383|6|Mentioned|p38|Paleoproterozoic||Pine Creek Orogen, Litchfield Domain. Low?pressure, high-temperature metamorphism commenced ~1855 Ma.||||||
19716|Welltree Metamorphics|69418|6|Mentioned|p3:21|||Pine Creek Orogen (Litchfield Domain). Hosts the Labelle Sn-Ta-Nb pegmatite deposit (described).||||||12-JUL-16
19716|Welltree Metamorphics|69420|4|Described|p5:2, 4-7, 26-27, 102, 105, 117|Paleoproterozoic|Paleoproterozoic|NE Litchfield Domain, Pine Creek Orogen. Poorly exposed. Metamorphism at 1813 +/- 3 Ma (207Pb/206Pb monazite: Carson et al., 2008). Hosts the Labelle Sn-Ta-Nb deposit (briefly described).||Cosmo Supergroup.|Sweets Member.|Correlated with Burrell Creek Formation (Finniss River Group). Is faulted against Fog Bay Metamorphics.|Quartz-feldspar-muscovite schist and gneiss; minor quartzite, marble, graphitic schist, calc-silicate gneiss, marble. Has a well-developed ductile fabric.|12-JUL-16
19716|Welltree Metamorphics|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||Cosmo Supergroup.|Includes Sweets Member.||Quartz-feldspar-biotite gneiss, garnet-sillimanite-andalusite quartzitic gneiss, quartzite; minor quartz-feldspar-muscovite gneiss.|01-MAR-18
19716|Welltree Metamorphics|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||gneiss|
19716|Welltree Metamorphics|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|1865+/-4 Ma (MDA: U-Pb zircon SHRIMP)||||Garnet-sillimanite pelitic schist; biotite-garnet-sillimanite gneiss.|
19716|Welltree Metamorphics|73089|6|Mentioned|p32-33|||Pine Creek Orogen, western; Litchfield Domain. Appears to be a higher-metamorphic-grade correlative of the upper Cosmo Supergroup.|||||Amphibolite to granulite facies metamorphic rocks.|
19780|West Branch Volcanics|22538|4|Described|p715, p718||Statherian|||||||13-APR-18
19780|West Branch Volcanics|22665|6|Mentioned|P231||Statherian|Age of unit is 1705+/-6 Ma to 1712+/-6 Ma.||||||19-DEC-06
19780|West Branch Volcanics|22748|6|Mentioned|p235 Fig.1|||||||||
19780|West Branch Volcanics|23216|4|Described|Table1p8,19,25-6|Statherian|Statherian|Age: 1712-1705 Ma.||||||
19780|West Branch Volcanics|23363|5|Briefly described|352 Tab.3|Statherian|Statherian|||||||
19780|West Branch Volcanics|23374|5|Briefly described|p14||Statherian|Age: U/Pb zircon 1712 -1705 Ma. Of the Katherine River Group. In the McArthur Basin.||||||19-DEC-06
19780|West Branch Volcanics|23396|4|Described|p 409|Statherian|Statherian|Oof the Katherine River Group. Age:  ~1709Ma.||||||19-DEC-06
19780|West Branch Volcanics|23397|6|Mentioned|p464 Fig.3|||||||||
19780|West Branch Volcanics|23733|5|Briefly described|p32 Fig. 19|||Of Katherine River Group.||||||
19780|West Branch Volcanics|23867|5|Briefly described|p3|Paleoproterozoic|Paleoproterozoic|Of Katherine River Group.  Age: ~1705Ma.  See also Fig. 3.  Geological Province: McArthur Basin.||||||07-NOV-08
19780|West Branch Volcanics|23937|4|Described|p8, p25 Tb. 2|Statherian|Statherian|Of the Katherine River Group.  Unconformably overlain by Bone Creek Sandstone; disconformably overlies Gundi Sandstone. Age: 1712-1705Ma (Kruse et al, 1994).  Max. thickness: >70m.  Geological Province: McArthur Basin.||||||18-APR-05
19780|West Branch Volcanics|24048|6|Mentioned|p36|||Geological Province: McArthur Basin.||||||
19780|West Branch Volcanics|24050|3|Fully described|p27, p9 Tb. 2|Paleoproterozoic|Paleoproterozoic|Formerly included in the Diljin Hill Formation.  Of the Katherine River Group.  Overlies Gundi Sandstone; underlies Mount Rigg Group unconformably.  Max. thickness: >100m.||||||07-NOV-08
19780|West Branch Volcanics|24051|5|Briefly described|Map Legend|Statherian|Statherian|Of Katherine River Group. Geological Province: McArthur Basin.||||||
19780|West Branch Volcanics|24197|5|Briefly described|p29|Paleoproterozoic|Paleoproterozoic|Of the Fagan Suite. Rocks of lava domes and flows.||||||07-FEB-11
19780|West Branch Volcanics|24432|4|Described|p565 Fig.2|Statherian|Statherian|Of Upper Katherine River Group. Age: 1705 Ma. Geological Province: Northern McArthur Basin.||||||
19780|West Branch Volcanics|32660|5|Briefly described|Table 4|||||||||
19780|West Branch Volcanics|41406|6|Mentioned|Map legend|Mesoproterozoic||||||||
19780|West Branch Volcanics|42597|5|Briefly described|Map Legend|Carpentarian||||||||
19780|West Branch Volcanics|43010|3|Fully described|p106|||Of the Katherine River Group.||||||19-DEC-06
19780|West Branch Volcanics|43149|5|Briefly described|Map Legend||Paleoproterozoic|Of the Katherine River Group.Of Statherian age.||||||07-NOV-08
19780|West Branch Volcanics|44112|6|Mentioned|p43|||||||||
19780|West Branch Volcanics|44400|2|Defined|p.8,Tb.1,opp.p.6,map|||Mt.Marumba Sheet. (D53-6).||||||
19780|West Branch Volcanics|44401|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
19780|West Branch Volcanics|44471|14|Not recorded|p.7, opp.p.7, map|||(D53-10). Formation of Katherine River Group.||||||
19780|West Branch Volcanics|44472|5|Briefly described|map legend||Paleoproterozoic|Of the Katherine River Group.  Amygdaloidal basalt, tuff, interbedded with coarse greywacke and agglomerate; sandstone.||||||07-NOV-08
19780|West Branch Volcanics|45022|6|Mentioned|p.56.||Carpentarian|Of Katherine River Group. On many pages.||||||19-DEC-06
19780|West Branch Volcanics|50224|6|Mentioned|p380 Fig. 6|||||||||07-FEB-11
19780|West Branch Volcanics|50545|5|Briefly described|p136||Statherian|Age: 1705+/-11 Ma.||||||17-DEC-07
19780|West Branch Volcanics|50591|5|Briefly described|p1.3, 4.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Of the Fagan Supersuite. Geological Province: Arnhem Block/McArthur Basin. Age: 1712-1705 +/- 16Ma (SHRIMP).||||||09-SEP-14
19780|West Branch Volcanics|61390|5|Briefly described|Map Legend|Statherian|Statherian|Of the Katherine River Group. Basalt: massive and vesicular; peperite; pink microdolerite.||||||
19780|West Branch Volcanics|61572|5|Briefly described|p666|Paleoproterozoic|Paleoproterozoic|Mafic volcanic rocks; minor sandstone. Age: 1720+/-7Ma [or is this the age of the Jimbu Microgranite?]. Max. thickness: >100m. Geological Province: McArthur Basin. See also p671 Tb. 1||||||10-OCT-19
19780|West Branch Volcanics|63866|5|Briefly described|p112-p114, p117|Statherian|Statherian||1712-1705 Ma (Kruse et al., 1994)|Katherine River Group||Unconformably overlain by the Mount Rigg Group and the Nathan Group.||
19780|West Branch Volcanics|64698|4|Described|lithinterp table|Statherian|Statherian|McArthur Basin. Of Katherine River Group. Age 1705-1712Ma SHRIMP U/Pb. Max thick 2000m. Poorly sorted purple fine to coarse sandstone, vesicular mafic volcanics, minor quartz-feldspar porphyry, conglomerate at base. Conformably overlies Gundi Sandstone.||||||
19780|West Branch Volcanics|64726|6|Mentioned|p86 Table 1.|||Sampled for paleomagnetic reconstruction of Australian and Laurentian Apparent Polar Wander Path.|1709 +/- 10 Ma.|||||
19780|West Branch Volcanics|64738|6|Mentioned|pp260-261.|Statherian|Statherian|Dated and used in identifying a reversal in direction in the earliest defined segment of northern Australia's Apparent Polar Wander Path.|c.1710 Ma.|||||
19780|West Branch Volcanics|64748|6|Mentioned|p276 Fig. 9|Paleoproterozoic|Paleoproterozoic|Palaeomag results shown on polar wander path||||||
19780|West Branch Volcanics|64817|6|Mentioned|p353 Fig.4, p355 Fig.5 |Statherian|Statherian|Arnhem Shelf, McArthur Basin. As well as the 3 ages of 1705 Ma, a fourth age is given at 1712 +/- 6 Ma.|1705 +/- 6,11 and 16 Ma.|Of the Katherine River Group.|||Sandstone and conglomerate, mafic volcanics, felsic volcanics.|05-JUN-18
19780|West Branch Volcanics|65228|5|Briefly described|p23, Fig.10.|Statherian|Statherian|Northern McArthur Basin.|1705 +/- 6 Ma (Page et al. 2000).|||Is overlain by Parsons Range Group.||
19780|West Branch Volcanics|65232|5|Briefly described|p7 Fig. 6, p45||Statherian|Of Katherine River Group. Overlies Gundi Sandstone. Max Age: 1712 Ma.||||||09-FEB-10
19780|West Branch Volcanics|67323|5|Briefly described|Eastern Australia Time-Space Plot|||McArthur region.|1705 +/- 16 Ma.|Upper Katherine River Group.||||
19780|West Branch Volcanics|67564|5|Briefly described|p38, p39 Fig.20, p41, p46.|||Not present in this sheet area. Constrains the minimum age of the Katherine River Group.|1712 - 1705 Ma (Kruse et al. 1994).|||Overlies Gundi Sandstone.||
19780|West Branch Volcanics|69430|4|Described|p15:3, 8-9, 30|||NW McArthur Basin. 1500-2000m thick. Lacustrine sediments; intrusive semi-concordant sills and extrusive basalts. Age also given as "well-constrained" at 1710 Ma. The maximum constraining age of 1720 Ma is from the comagmatic Jimbu Microgranite which was emplaced concurrently with deposition of the underlying Gundi Sandstone.|1705 +/- 16 Ma.|Katherine River Group.||Overlies Gundi Sandstone conformably or locally disconformably. Is overlain unconformably by Mount Rigg Group.|Vesicular and amygdaloidal basalt, dolerite, peperite; fine-grained sandstone and mudstone; minor medium-grained and pebbly sandstone.|12-JUL-16
19780|West Branch Volcanics|69673|6|Mentioned|p16 fig 13|||Northwestern McArthur Basin.||Katherine River Group||Overlies Gundi Sandstone, Jimbu Microgranite||
19780|West Branch Volcanics|71592|5|Briefly described|Appendix A.|||McArthur Basin.|1712+/-6 Ma (crystallisation: U-Pb zircon SHRIMP)||||Rhyolite, agglomerate, sedimentary siliciclastics, conglomerate.|
19780|West Branch Volcanics|71606|5|Briefly described|p135,137|Statherian|Statherian|West Arnhem Shelf, McArthur Basin. SHRIMP data givers 1710-1700 Ma age, associated with Fagan Phase magmatism of Rawlings 1994.||Unit of Katherine River Group.||Hosted in the uppermost Katherine River Group.||
19780|West Branch Volcanics|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.||Upper Katherine River Group.||||
19780|West Branch Volcanics|72377|5|Briefly described|p12|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. Page et al (2000) reported SHRIMP U-Pb zircon age of 1715+\-16 Ma, interpreted as magmatic crystallisation age, which is within uncertainty with the magmatic crystallisation age of the Haddon Volcanics (1712+\-12 Ma; this record).|1705+\-16 Ma (magmatic)|Unit of Katherine River Group.||||10-OCT-19
19842|Westmoreland Conglomerate|22538|6|Mentioned|P714||Statherian|||||||
19842|Westmoreland Conglomerate|22644|5|Briefly described|5|||Geol province McArthur Basin. Parent Murphy Metamorphics||||||
19842|Westmoreland Conglomerate|23065|6|Mentioned|4|||||||||
19842|Westmoreland Conglomerate|23066|5|Briefly described|p808|||Overlying unit Seigal Volcanics.||||||
19842|Westmoreland Conglomerate|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|Of Tawallah Group.||||||07-NOV-08
19842|Westmoreland Conglomerate|23395|5|Briefly described|p395|||||||||
19842|Westmoreland Conglomerate|23776|5|Briefly described|p705 Fig 2.|||Of Tawallah Group.||||||
19842|Westmoreland Conglomerate|23867|5|Briefly described|Fig. 30|||Of Tawallah Group. Correlates with part of Mamadewerre Sandstone of the Kombolgie Subgroup (Katherine River Group).||||||
19842|Westmoreland Conglomerate|24419|5|Briefly described|p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Of the Tawallah Group.  Geological Province: McArthur Basin, Murphy Province.||||||07-NOV-08
19842|Westmoreland Conglomerate|26310|4|Described|p7, Fig. 2, Table 1|Proterozoic|Proterozoic|Sandstone and conglomerate. Maximum Thickness: 4000 feet.||||||
19842|Westmoreland Conglomerate|29961|6|Mentioned|Fig.1|||||||||
19842|Westmoreland Conglomerate|30318|6|Mentioned|p327|||||||||
19842|Westmoreland Conglomerate|30912|6|Mentioned|p364|||||||||
19842|Westmoreland Conglomerate|31348|4|Described|p345|||||||||
19842|Westmoreland Conglomerate|31421|6|Mentioned|p509|||||||||
19842|Westmoreland Conglomerate|31824|6|Mentioned|p28|||See also P32. U.Proterozoic||||||
19842|Westmoreland Conglomerate|32660|5|Briefly described|Table 4|||||||||
19842|Westmoreland Conglomerate|32758|6|Mentioned|p62|||||||||
19842|Westmoreland Conglomerate|33214|6|Mentioned|Fig.1|||||||||
19842|Westmoreland Conglomerate|33225|6|Mentioned|p24|||||||||
19842|Westmoreland Conglomerate|34006|6|Mentioned|p64|||||||||
19842|Westmoreland Conglomerate|35114|6|Mentioned|p200|||||||||
19842|Westmoreland Conglomerate|35495|6|Mentioned|p340|||||||||
19842|Westmoreland Conglomerate|35640|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
19842|Westmoreland Conglomerate|36012|3|Fully described|Table 2|||See also P11.||||||
19842|Westmoreland Conglomerate|36439|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
19842|Westmoreland Conglomerate|36442|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
19842|Westmoreland Conglomerate|37568|5|Briefly described|p77|||||||||
19842|Westmoreland Conglomerate|38557|5|Briefly described|p293|||||||||
19842|Westmoreland Conglomerate|38584|4|Described|p11|||||||||
19842|Westmoreland Conglomerate|38902|6|Mentioned|p28|||||||||
19842|Westmoreland Conglomerate|39445|5|Briefly described|Table 2|||||||||
19842|Westmoreland Conglomerate|39497|6|Mentioned|p7|||See also Fig.4||||||
19842|Westmoreland Conglomerate|39685|6|Mentioned|Fig.1|||||||||
19842|Westmoreland Conglomerate|39986|6|Mentioned|p75|||||||||
19842|Westmoreland Conglomerate|40489|6|Mentioned|p89|||||||||
19842|Westmoreland Conglomerate|40491|6|Mentioned|p79|||||||||
19842|Westmoreland Conglomerate|40675|6|Mentioned|Table 1A|||||||||
19842|Westmoreland Conglomerate|40691|6|Mentioned|p9|||||||||
19842|Westmoreland Conglomerate|41125|6|Mentioned|p35|||See also Fig.21||||||
19842|Westmoreland Conglomerate|41319|4|Described|p195|||||||||
19842|Westmoreland Conglomerate|41594|6|Mentioned|p50|||||||||
19842|Westmoreland Conglomerate|41721|3|Fully described|p9|Mesoproterozoic|Mesoproterozoic|Of Tawallah Group. Unconformably overlies Murphy Metamorphics (west), Nicholson Granite Complex (central area) and Cliffdale Volcanics (east). Conformably overlain by Seigal Volcanics. Thickness:1900m. Sandstone and conglomerate. Geol.prov: McArthur Basin||||||01-AUG-07
19842|Westmoreland Conglomerate|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
19842|Westmoreland Conglomerate|42385|6|Mentioned|p3|||||||||
19842|Westmoreland Conglomerate|42639|5|Briefly described|p8|||Stratigraphic equivalent to Yiyintyi Sandstone||||||
19842|Westmoreland Conglomerate|42812|5|Briefly described|p11|||see also Fig.5||||||
19842|Westmoreland Conglomerate|43010|5|Briefly described|Fig.6||Mesoproterozoic|of Tawallah Group. Of "Mid Proterozoic" age.||||||
19842|Westmoreland Conglomerate|43036|6|Mentioned|Fig.5|||||||||
19842|Westmoreland Conglomerate|43788|6|Mentioned|p14|||||||||
19842|Westmoreland Conglomerate|44271|2|Defined|p39,55,57||Paleoproterozoic|Overlies Cliffdale Volcanics and Nicholson Granite.||||||07-NOV-08
19842|Westmoreland Conglomerate|44272|14|Not recorded|Map Legend||Neoproterozoic|||||||
19842|Westmoreland Conglomerate|44275|14|Not recorded|Map Legend|||||||||
19842|Westmoreland Conglomerate|44280|2|Defined|p5-8,Tb.1,map|||||||||
19842|Westmoreland Conglomerate|44287|14|Not recorded|opp.p.7|||Equiv. of Yiyinti Sandstone. (E53-3).||||||
19842|Westmoreland Conglomerate|44305|14|Not recorded|p.6,8,11,19|||(E53-8). opp.6,18.||||||
19842|Westmoreland Conglomerate|44306|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
19842|Westmoreland Conglomerate|44473|14|Not recorded|p.7-8, opp. p.7|||(E53-7).||||||
19842|Westmoreland Conglomerate|44474|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
19842|Westmoreland Conglomerate|44521|14|Not recorded|p1,7,9,10,13-15,46||Neoproterozoic|||||||
19842|Westmoreland Conglomerate|44751|14|Not recorded|p302|||The unit if older than the Neoproterozoic Constance Sandstone.||||||
19842|Westmoreland Conglomerate|44989|2|Defined|p.114-115|||Tb.II. On many pages. (E54,5) + NT. Pl.8,15.||||||
19842|Westmoreland Conglomerate|45162|3|Fully described|p11|Proterozoic|Proterozoic|||||||21-FEB-18
19842|Westmoreland Conglomerate|45166|5|Briefly described|p77|||||||||
19842|Westmoreland Conglomerate|45287|14|Not recorded|p.223,226,228,231|||||||||
19842|Westmoreland Conglomerate|46804|6|Mentioned|p154|||Stratigraphy||||||
19842|Westmoreland Conglomerate|49001|6|Mentioned|p4|||||||||
19842|Westmoreland Conglomerate|50536|6|Mentioned|p3.2|||Overlies: Nicholson Suite.||||||19-JUL-04
19842|Westmoreland Conglomerate|60483|5|Briefly described|p7 Fig. 5|||Of the Tawallah Group. Geological Province: McArthur Basin.||||||05-OCT-07
19842|Westmoreland Conglomerate|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Tawallah Group. Overlain by Seigal Volcanics.||||||03-JUN-09
19842|Westmoreland Conglomerate|63109|6|Mentioned|p1111, p1108 Fig. 3, p1112|||Proximal fluvial sandstone. Geological Province: Leichhardt Superbasin.||||||30-SEP-08
19842|Westmoreland Conglomerate|63112|6|Mentioned|p1189-1191,p1193-1195,p1198,p1200-1206|||Leichhardt 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. <2000 m thick.|c.1795-1790 Ma.||||Proximal fluvial facies: poorly sorted and immature, coarse- to fine-grained.|
19842|Westmoreland Conglomerate|63113|6|Mentioned|p1225 Fig.13. |||Leichhardt Superbasin.||||||
19842|Westmoreland Conglomerate|63115|6|Mentioned|p1279 Fig.4.|||Base of Leichhardt superbasin. Potential aquifer sequence.||||||
19842|Westmoreland Conglomerate|63116|6|Mentioned|p1297 Fig.2, p1299-1306, p1309 |||Leichhardt superbasin. Material properties detailed. Aquifer.||||||
19842|Westmoreland Conglomerate|63866|5|Briefly described|p56|||||||(Possibly) equivalent to the Guide Supersequence.||
19842|Westmoreland Conglomerate|64817|6|Mentioned|p353 Fig.4, p355 Fig.5, p377  |||||Of the Tawallah Group.||||
19842|Westmoreland Conglomerate|65228|5|Briefly described|p7, Figs.02, 06, 07. |||Southern McArthur Basin.||Basal unit in Tawallah Group.||Is overlain by Seigal Volcanics. Equivalent to Yiyintyi Sandstone.||
19842|Westmoreland Conglomerate|65232|5|Briefly described|p9, p8 Fig. 7, p66-68, App. 2|Late Palaeoproterozoic|Late Palaeoproterozoic|At base of Tawallah Group. Conformably underlies Seigal Volcanics; unconformably over Cliffdale Volcanics. Thickness: up to 1800 m. Arenite, conglomerate, minor siltstone. Uranium mineralisation. Geol. Prov: McArthur Basin.||||||09-FEB-10
19842|Westmoreland Conglomerate|65337|6|Mentioned|pp12-13. |||Southern McArthur Basin. Correlative of Don Creek Sandstone.||||||
19842|Westmoreland Conglomerate|65340|5|Briefly described|p12 Fig.6, p84.|||McArthur Basin. Only occurs in the subsurface in this map area.||Unit at base of Tawallah Group.||Is overlain by Seigal Volcanics. Is shown as equivalent to Yiyintyi Sandstone.||23-MAR-18
19842|Westmoreland Conglomerate|66529|5|Briefly described|p20 Fig.7, p21  |||Basal unit in McArthur Basin. Over 1200 m thick. Hosts uranium deposits aged around 1655 Ma (Polito et al., 2005) along the Redtree dyke zone.||||Conformably overlain by the Seigal Volcanics.|Arkose, conglomerate and quartz arenites.|
19842|Westmoreland Conglomerate|67144|5|Briefly described|Map legend.|Statherian|Statherian|||Unit in Tawallah Group.||Is overlain by Seigal Volcanics.|Pebble and cobble conglomerate, lithic and quartz sandstone, red micaceous siltstone.|
19842|Westmoreland Conglomerate|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map, p9|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Camooweal-Murphy Domain, Mount Isa Inlier. Leichhardt Superbasin. Informally subdivided into 5 units. Max depositional age: 1814 +/-14 Ma (Magee et al in prep).|1865 +/- 7 Ma and 1843 +/- 4 Ma MDAs.|Tawallah Group.||Correlated with Wire Creek Sandstone and Mount Guide Quartzite.|Pebble to cobble conglomerate, white argillaceous sandstone and orthoquartzite.|
19842|Westmoreland Conglomerate|67352|6|Mentioned|p15 Tb.2|||||||Is overlain conformably by Seigal Volcanics.||
19842|Westmoreland Conglomerate|67479|5|Briefly described|p2 Tb.1, pp12-15, p61 Tb.4, p62 Tb.4|Orosirian|Orosirian|Maximum depositional age.|1830 +/- 7 Ma.||||Silicified altered fine-grained pink tuff.|24-JAN-17
19842|Westmoreland Conglomerate|68020|5|Briefly described|p127|||Hosts uranium mineralisation near contact with overlying Seigal Volcanics.||||Unconformably overlain by Seigal Volcanics.|Sandstone and conglomerate.|
19842|Westmoreland Conglomerate|68575|4|Described|p2, p6-7, p87-93, p125, p134|||Mount Isa Region. A major component of the basement terrane in the Duchess and Dajarra 1:100 000 sheet areas. Thin section analysis showed the clasts are quartzo-feldspathic siliciclastics; zircons have detrital morphology; thus the rock is not a peperite. This means the age is of maximum deposition, not emplacement/deposition. Age distribution is remarkably similar to other basal McArthur Basin clastics (eg Kombolgie Subgroup; Depot Creek Sandstone). Whole rock Sm-Nd isotopic data and age (1819 Ma).|1815 +/- 14 Ma (maximum deposition age).|Kurbayia Metamorphic Complex.|||Fine-grained, subangular to angular clasts to 10cm in a siltstone matrix.|
19842|Westmoreland Conglomerate|68733|6|Mentioned|p186||Orosirian|Maximum depositional age of ca. 1830 Ma. Basal eastern McArthur Basin.||||||
19842|Westmoreland Conglomerate|69383|4|Described|p43-48, 49|Paleoproterozoic|Paleoproterozoic|Base of McArthur Basin. Fluvial. Up to 1400 m thick. Four upward-fining cycles. LA-ICPMS U-Pb and Hf geochronology analyses.  2 samples. Max deposition age is further constrained by underlying Murphy Metamorphics.|1865+/-7; 1843+/-4 Ma|||Unconformable on Murphy Metamorphics. Conformably overlain by Carolina Sandstone Member.|Coarse pebbly sandstone from the youngest, fourth cycle of the formation; Coarse pebbly conglomeritic sandstone for top of unit; sampled.|
19842|Westmoreland Conglomerate|69418|5|Briefly described|p3:19|||McArthur Basin. Hosts U deposits in sub-horizontal and sub-vertical lenses adjacent to altered, sub-vertical dolerite dykes.||||Unconformably overlies Cliffdale Volcanics.||12-JUL-16
19842|Westmoreland Conglomerate|69423|5|Briefly described|p8:1, 2 Fig.8.3, 5-6|||Separated by the Tin Hole Hinge Line, a probable thrust fault, from the Murphy Inlier to the S. Hosts a number of uranium +/- gold occurrences, and appears to be the source of numerous stream sediment gold occurrences.||||Unconformably overlies Cliffdale Volcanics.||12-JUL-16
19842|Westmoreland Conglomerate|69430|4|Described|p15:3, 9-11, 49-51|||Southern McArthur Basin. Up to 1900m thick. Fluvial to alluvial fan deposits, derived from the NE. Hosts small U-Au deposits (described in some detail).||Tawallah Group.||Unconformably overlies Cliffdale Volcanics, Nicholson Granite Complex and Murphy Metamorphics. Is overlain conformably by Seigal Volcanics. Probably equivalent to lower Kombolgie Subgroup.|A thick succession of conglomerate, coarse argillaceous sandstone with scattered pebbles.|12-JUL-16
19842|Westmoreland Conglomerate|69433|5|Briefly described|p18:2, 5|||McArthur Basin. Fluvial braided river and alluvial fan deposits.||Basal Tawallah Group.||Correlated with Wire Creek and Don Creek Sandstones (Lawn Hill Platform).||12-JUL-16
19842|Westmoreland Conglomerate|69434|6|Mentioned|p19:4|||Basal McArthur Basin. A possible source of siliciclastic sediments for the Caulfield beds, South Nicholson Basin.||||||12-JUL-16
19842|Westmoreland Conglomerate|69591|4|Described|p33-34, p39, p58|||Camooweal-Murphy Domain, Leichhardt Superbasin. Fluvial deposits. Another maximum depositional age of 1843 +/- 4 Ma is by Carson et al. (2011).|1814 +/- 14 Ma (MDA: Magee et al. in press).|Basal Tawallah Group.||Is overlain by Seigal Volcanics. Correlated with Wire Creek Sandstone and Mount Guide Quartzite.|Pebble to cobble conglomerate, white argillaceous sandstone and orthoquartzite.|
19842|Westmoreland Conglomerate|69673|6|Mentioned|p16 fig 13, p17 fig 14|||Coarse clastic sedimentary rock.||Tawallah Group||Overlain by Seigal Volcanics||
19842|Westmoreland Conglomerate|69917|4|Described|p199-201|Paleoproterozoic|Paleoproterozoic|McArthur Basin. U/Pb LA-ICPMS zircon dating. 1851+/-7.2 Ma is interpreted to be a conservative estimate of the maximum depositional age of this rock. This is slightly older than the age (1843+/-4 Ma) reported for the upper unit of the conglomerate (Hollis et al 2010a).Carson et al 2011 reported an age of 1830+/-7 Ma for a silicified tuff that forms a layer within the basal Westmoreland Conglomerate. This implies that sedimentation began after the maximum depositional age reported here.||||Unconformably overlies Cliffdale Volcanics. Correlated with Kombolgie Subgroup.|coarse-grained sandstone composed of quartz grains in a kaolinite matrix. Bed bases are marked by cobble beds between 0.05 and 0.2 m thick.|
19842|Westmoreland Conglomerate|70284|5|Briefly described|p1243, p1245-1252, p1255-1258|Statherian|Statherian|McArthur Basin, Leichhardt Superbasin. Up to 1800m thick. Hosts uranium mineralization.|> 1680+/-18 Ma (fluid migration age)|||Conformably overlain by Seigal Volcanics. Cut by dolerite dykes.|Quartz, chert and felsic volcanic cobble conglomerate and medium-coarse grained, well sorted sandstone.|14-DEC-16
19842|Westmoreland Conglomerate|70849|5|Briefly described|Map legend.|Statherian|Statherian|McArthur Basin. Five facies are mapped separately.||Tawallah Group.||Unconformably overlies Cliffdale Volcanics. Is overlain by Seigal Volcanics.|Siltstone, conglomerate and talus breccia, sandstone; pebble and cobble conglomerate, sandstone; boulder and cobble conglomerate, greywacke, sandstone; conglomerate, sandstone, greywacke, siltstone.|
19842|Westmoreland Conglomerate|71592|5|Briefly described|Appendix A.|||McArthur Basin.|1830+/-7 Ma (MDA: U-Pb zircon SHRIMP)||||Coarse-grained sandstone, rhyodacite, coarse pebbly sandstone, volcanic rock.|
19842|Westmoreland Conglomerate|71799|5|Briefly described|p150 fig 2|Statherian|Orosirian|McArthur Basin.|ca. 1800 Ma|||Overlain by the Seigal Volcanics.|Sandstone, greywacke and conglomerate.|
19842|Westmoreland Conglomerate|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Orosirian|Shown as located in the Southeastern McArthur Basin. Age given as U-Pb zircon sedimentary depositional age. Shown on diagram as Statherian age but depositional ages listed are Orosirian.|1830 +/-7 Ma, to 1815 +/-7 Ma|Tawallah Group||Shown as unconformably overlying Nicholson Granite Complex and Cliffdale Volcanics and partially underlies Seigal Volcanics.||
19842|Westmoreland Conglomerate|72527|5|Briefly described|p161, p177, p194.|Paleoproterozoic|Paleoproterozoic|The siliclastic detritus generated by this unit is thought to contribute to the Caulfield beds.||||Equivalent to Wire Creek Sandstone.||
19842|Westmoreland Conglomerate|72718|6|Mentioned|p7|||Southern McArthur Basin (southeastern).||Tawallah Group||Overlain by Seigal Volcanics. Equivalent to Yiyintyi Sandstone.||
19842|Westmoreland Conglomerate|72912|5|Briefly described|p5 Fig.3, p19, p31 Fig.11.|Statherian|Statherian|Located in the Southeastern McArthur Basin, in the Southern McArthur Basin. Two U-Pb zircon sedimentary depositional ages given 1830+/-7 Ma, 1815+/-7 Ma.||Tawallah Group||Unconformably overlies Nicholson Granite Complex and Cliffdale Volcanics. Equivalent to Yiyintyi Sandstone.||
19842|Westmoreland Conglomerate|72919|6|Mentioned|p12|||Intersected in drillhole BEN-SD60.||Tawallah Group||||
19842|Westmoreland Conglomerate|73042|6|Mentioned|p4||Orosirian|Southern McArthur Basin, Leichhardt Superbasin. Geochronology is a U-Pb zircon sedimentary depositional age (?maximum depositional age).|1830 +/- 7 Ma, 1815 +/- 7 Ma (see Fig.1.2)|Tawallah Group||Partly unconformably underlain(?) by Nicholson Granite Complex. Overlain by Seigal Volcanics.||
19842|Westmoreland Conglomerate|73412|5|Briefly described|p2, 4, 8, 12|||The basal unit in the southern McArthur Basin. Smooth, non-magnetic response.||Tawallah Group.||Lateral equivalent to Yiyintyi Sandstone. Is overlain by Seigal Volcanics.||
19898|White Mountain Formation|23821|4|Described|p245|Miocene|Miocene|Geological Province: Ord Basin. Maximum thickness: 113m.||||||
19898|White Mountain Formation|30862|6|Mentioned|p26|||Middle Tertiary age||||||
19898|White Mountain Formation|31529|6|Mentioned|p95|||||||||
19898|White Mountain Formation|34548|6|Mentioned|p134|||See also p137. Miocene - Pliocene||||||19-DEC-06
19898|White Mountain Formation|36213|6|Mentioned|p86|||||||||
19898|White Mountain Formation|36257|6|Mentioned|Table 2.1|||||||||
19898|White Mountain Formation|36551|6|Mentioned|Table 16|||||||||
19898|White Mountain Formation|36890|3|Fully described|p398|||Formerly White Mount Series.||||||19-DEC-06
19898|White Mountain Formation|40605|6|Mentioned|p196|||||||||
19898|White Mountain Formation|41864|2|Defined|p153|Miocene||Formerly "White Mountain Series"||||||
19898|White Mountain Formation|41866|5|Briefly described|Map legend|Cenozoic||||||||19-NOV-08
19898|White Mountain Formation|42829|5|Briefly described|p148|||||||||
19898|White Mountain Formation|43606|5|Briefly described|p5||Early Miocene|||||||
19898|White Mountain Formation|44221|14|Not recorded|p.87, 88, 97, 102|||||||||
19898|White Mountain Formation|44222|14|Not recorded|p119|||||||||
19898|White Mountain Formation|44317|4|Described|Table 4||Cenozoic|||||||19-NOV-08
19898|White Mountain Formation|44318|14|Not recorded|map legend||Tertiary|Tertiary.||||||
19898|White Mountain Formation|45022|6|Mentioned|p.165.|Pliocene|Miocene|||||||
19898|White Mountain Formation|48925|6|Mentioned|p13|||Miocene ? Fauna||||||
19898|White Mountain Formation|60703|6|Mentioned|p725 Fig. 18|Tertiary|Tertiary|||||||12-APR-05
19898|White Mountain Formation|61155|5|Briefly described|p16|Middle Miocene|Early Miocene|Overlies detrital ferricrete; underlies Birdum Creek beds. Thickness: 120m. Geological Province: Ord and Wiso Basins.||||||
19898|White Mountain Formation|67860|5|Briefly described|p416 Fig.4-84, p417 fig 4-85|Miocene|Miocene|See also p418 Tb. 4-18, p422. 30-115 m thick in small outcrops. Type section details given. Contains the foraminifer Ammonia beccarii.|||||Fossiliferous chert, siltstone, sandstone, marl.|
19898|White Mountain Formation|71754|14|Not recorded|p200|Pliocene|Miocene|Ref to Traves, 1955.||||||
19928|Whitewater Volcanics|22474|5|Briefly described|p21||Orosirian|Age: 1855 +/- 5 Ma.||||||14-NOV-06
19928|Whitewater Volcanics|22526|6|Mentioned|Fig3 P682||Orosirian|||||||
19928|Whitewater Volcanics|22547|4|Described|p9||Orosirian|In the Lamboo Complex, Halls Creek Orogen. Age: 1850 +/- 5 Ma. Part of the Whitewater Volcanics reassigned to Castlereagh Hill Porphyry. Overlies Marboo Formation, overlain by O'Donnell Formation||||||08-MAY-15
19928|Whitewater Volcanics|22716|5|Briefly described|table4, p232|Orosirian|Orosirian|Intruded by Paperbark supersuite.||||||14-NOV-06
19928|Whitewater Volcanics|22741|5|Briefly described|P20, Table3 P19||Proterozoic|||||||
19928|Whitewater Volcanics|22754|4|Described|p6|Paleoproterozoic|Paleoproterozoic|Age c. 1855 Ma (Gellatly et al, 1975).||||||07-NOV-08
19928|Whitewater Volcanics|23125|5|Briefly described|Table.1|||||||||
19928|Whitewater Volcanics|23323|5|Briefly described|p454 Fig.2, p456 Tb. 1|Orosirian|Orosirian|Age: 1860-1850 Ma and 1855+/-5Ma.||||||07-FEB-07
19928|Whitewater Volcanics|23383|6|Mentioned|p8|||||||||
19928|Whitewater Volcanics|23621|5|Briefly described|p20|||||||||
19928|Whitewater Volcanics|23722|4|Described|p8|Orosirian|Orosirian|Age: 1850+/-5Ma (U-Pb zircon).   Geological Province: Hooper Complex||||||
19928|Whitewater Volcanics|23751|4|Described|p7|Paleoproterozoic|Paleoproterozoic|Age: 1855+/-5 Ma (SHRIMP U-Pb zircon). Dacitic to rhyolite ignimbrites. Geological Province: Lamboo Complex.||||||07-NOV-08
19928|Whitewater Volcanics|24173|5|Briefly described|p15, 19|||Overlain by Speewah Group; unconformably overlies Marboo Formation. Geological Province: Halls Creek Orogen. Age: 1880-1845Ma. Intruded by Mount Christine Granitoid||||||06-APR-05
19928|Whitewater Volcanics|24197|5|Briefly described|p23, p85|||Of the Paperbark Supersuite. Felsic and phenocryst-rich. Age: 1850-1860Ma. Geological province: Kimberley Province (East and West). See also p89-90 Tb. 11.1.||||||07-FEB-11
19928|Whitewater Volcanics|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Fine- to medium-grained quartz-feldspar rhyolite- to dacite-porphyry and welded ignimbrite; minor agglomerate, lapilli tuff and volcaniclastic rock.  Age: 1865-1850Ma.||||||07-NOV-08
19928|Whitewater Volcanics|24572|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Age: >1835Ma.  Geological Province: Halls Creek Orogen.||||||07-NOV-08
19928|Whitewater Volcanics|30097|6|Mentioned|Fig.54|||Also Tables 23,24,27||||||
19928|Whitewater Volcanics|30525|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
19928|Whitewater Volcanics|30526|6|Mentioned|p112|||||||||
19928|Whitewater Volcanics|30533|3|Fully described|p12|||On Table 1. Dated as 1830 or 1960m.y.||||||
19928|Whitewater Volcanics|30878|6|Mentioned|p51|||Precambrian. Stratigraphic table||||||
19928|Whitewater Volcanics|30892|5|Briefly described|p96|||||||||
19928|Whitewater Volcanics|30895|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
19928|Whitewater Volcanics|30896|4|Described|p12|||Lower Proterozoic||||||
19928|Whitewater Volcanics|30897|4|Described|p9|||||||||
19928|Whitewater Volcanics|30898|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
19928|Whitewater Volcanics|31226|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
19928|Whitewater Volcanics|31393|6|Mentioned|Pl.25|||||||||
19928|Whitewater Volcanics|32108|6|Mentioned|Fig.1|||||||||
19928|Whitewater Volcanics|32659|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
19928|Whitewater Volcanics|32660|5|Briefly described|Table 1|||||||||
19928|Whitewater Volcanics|32664|6|Mentioned|Map legend|Carpentarian|Carpentarian|Briefly described in notes||||||
19928|Whitewater Volcanics|32699|5|Briefly described|Map legend|Carpentarian|Carpentarian|Acid lava, tuff, intrusive quartz-feldspar porphyry.||||||02-DEC-04
19928|Whitewater Volcanics|32701|5|Briefly described|Table 1|||Carpentarian. Lamboo Complex||||||
19928|Whitewater Volcanics|32728|5|Briefly described|p27|||See also Fig.3||||||
19928|Whitewater Volcanics|33376|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
19928|Whitewater Volcanics|33377|6|Mentioned|Table 1|||Strat.||||||
19928|Whitewater Volcanics|33443|6|Mentioned|p260|||||||||
19928|Whitewater Volcanics|34462|6|Mentioned|p12|||?Subsurface||||||
19928|Whitewater Volcanics|34834|6|Mentioned|p213|||||||||
19928|Whitewater Volcanics|35950|6|Mentioned|p302|||||||||
19928|Whitewater Volcanics|36225|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
19928|Whitewater Volcanics|36308|6|Mentioned|p212|||||||||
19928|Whitewater Volcanics|36473|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
19928|Whitewater Volcanics|36551|6|Mentioned|p41|||||||||
19928|Whitewater Volcanics|36885|3|Fully described|p172|||||||||
19928|Whitewater Volcanics|36902|6|Mentioned|p11|||||||||
19928|Whitewater Volcanics|37299|6|Mentioned|Fig.1|||||||||
19928|Whitewater Volcanics|37462|4|Described|Table 4.I|||See also Fig.4.6||||||
19928|Whitewater Volcanics|38071|6|Mentioned|p104|||||||||
19928|Whitewater Volcanics|38482|6|Mentioned|Table 1|||||||||
19928|Whitewater Volcanics|39827|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
19928|Whitewater Volcanics|40494|4|Described|p9|||||||||
19928|Whitewater Volcanics|41158|6|Mentioned|p19|||||||||
19928|Whitewater Volcanics|41465|6|Mentioned|p6|||See also P12||||||
19928|Whitewater Volcanics|41557|6|Mentioned|p589|||||||||
19928|Whitewater Volcanics|41575|6|Mentioned|p592|||||||||
19928|Whitewater Volcanics|41961|6|Mentioned|Table 1 P39|||||||||
19928|Whitewater Volcanics|41976|4|Described|p461|||||||||
19928|Whitewater Volcanics|41977|4|Described|p471|||||||||
19928|Whitewater Volcanics|42149|6|Mentioned|p704|||||||||
19928|Whitewater Volcanics|42329|5|Briefly described|p5|||Age 1850 +/- 5 Ma. See also Fig.2 p6.||||||14-NOV-06
19928|Whitewater Volcanics|42342|5|Briefly described|p22|||||||||
19928|Whitewater Volcanics|42710|5|Briefly described|map legend|Proterozoic||||||||
19928|Whitewater Volcanics|42768|6|Mentioned|p7|||||||||
19928|Whitewater Volcanics|42811|4|Described|p7|||Of Hooper Complex.||||||14-NOV-06
19928|Whitewater Volcanics|42814|4|Described|p6|||||||||
19928|Whitewater Volcanics|42815|5|Briefly described|map|||||||||
19928|Whitewater Volcanics|43281|5|Briefly described|Map legend|Proterozoic|Proterozoic|Approx 1855 Ma.||||||
19928|Whitewater Volcanics|43561|6|Mentioned|Fig.6,p1437|||Emplaced approx. Age: 1865-1850 Ma.||||||14-NOV-06
19928|Whitewater Volcanics|43568|6|Mentioned|p506|||Dated at : 1850+/-5 Ma||||||
19928|Whitewater Volcanics|43586|6|Mentioned|Fig.1,p4|||||||||
19928|Whitewater Volcanics|43595|5|Briefly described|p350,351,443|||U-Pb zircon dates: 1850+/-5 Ma||||||
19928|Whitewater Volcanics|43632|6|Mentioned|p10|||||||||
19928|Whitewater Volcanics|43666|6|Mentioned|p6|Proterozoic|Mesoproterozoic|||||||
19928|Whitewater Volcanics|43749|6|Mentioned|p31|||||||||
19928|Whitewater Volcanics|43794|5|Briefly described|p319-320||Proterozoic|||||||
19928|Whitewater Volcanics|43819|6|Mentioned|Table 2,p33|||||||||
19928|Whitewater Volcanics|43853|5|Briefly described|Map Legend||Proterozoic|||||||
19928|Whitewater Volcanics|43854|5|Briefly described|Map Legend||Proterozoic|||||||
19928|Whitewater Volcanics|43863|5|Briefly described|map legend|Proterozoic|Proterozoic|||||||
19928|Whitewater Volcanics|43931|5|Briefly described|p21||Orosirian|Age: 1855 +/- 5 Ma.||||||14-NOV-06
19928|Whitewater Volcanics|44140|5|Briefly described|p295 Tb.4-1, p297, p299|||||||Is overlain disconformably by O'Donnell Formation (Speewah Group), and unconformably by Revolver Creek Formation.|Acid volcanics.|
19928|Whitewater Volcanics|44155|4|Described|p234 Tb.3-2, p236 Fig.3-35,p237|Paleoproterozoic|Paleoproterozoic|See also p240-243, p247-249, p253-254. Dow and Gemuts (1969). Comagmatic with Castlereagh Hills, Bickleys and Mount Disaster Porphyries. Up to 2km thick. Contains Woodward Dolerite cobbles near base. Zircon U-Pb age from a felsic volcanic. Page (1976) recalculated data of Bofinger (1967) to obtain a whole-rock Rb-Sr isochron age of 1764 +/- 35 Ma. Other ages given.|1850 +/- 5 Ma (Page and Hancock, 1988).|Lamboo Complex, Hooper Complex||Intrudes or unconformably overlies Halls Creek Group. Intruded by Castlereagh Hill and Little Gold River Porphyries; also by Bow River and Lennard Granites. Overlain by Speewah Group.|Rhyolitic to andesitic ashflow tuff; minor intercalations of agglomerate, siltstone, sandstone, conglomerate and chert near top of sequence; rare lavas.|
19928|Whitewater Volcanics|44230|5|Briefly described|Map Legend||Proterozoic|||||||
19928|Whitewater Volcanics|44231|5|Briefly described|Map Legend||Paleoproterozoic|Dacite and rhyodacite lava, tuff, agglomerate and minor volcaniclastic sedimentary rocks; commonly crystal-rich; thin pebble conglomerate at base.  Age: 1865-1850Ma. In the Hooper Complex and Lamboo Complex western zone (Bow River batholith).||||||28-SEP-11
19928|Whitewater Volcanics|44317|4|Described|Table 2||Carpentarian|||||||
19928|Whitewater Volcanics|44318|14|Not recorded|map legend||Carpentarian|Carpentarian.||||||
19928|Whitewater Volcanics|44363|5|Briefly described|p.6,7,9,11,12,13-29|||(Carpentarian).||||||
19928|Whitewater Volcanics|44364|14|Not recorded|map legend|||||||||
19928|Whitewater Volcanics|44366|14|Not recorded|p.13, Table 2||Carpentarian|||||||
19928|Whitewater Volcanics|44367|14|Not recorded|map legend|||(Reprinted 1971).||||||
19928|Whitewater Volcanics|44397|14|Not recorded|p.9,18,19, Table 2||Carpentarian|||||||
19928|Whitewater Volcanics|44398|14|Not recorded|map legend||Carpentarian|||||||
19928|Whitewater Volcanics|44868|5|Briefly described|Map Legend||Proterozoic|||||||
19928|Whitewater Volcanics|45038|14|Not recorded|p.27||Precambrian|||||||
19928|Whitewater Volcanics|45047|2|Defined|p69|Carpentarian|Carpentarian|See also p27.||||||14-NOV-06
19928|Whitewater Volcanics|45048|6|Mentioned|p63|||||||||
19928|Whitewater Volcanics|45050|6|Mentioned|p7|||||||||
19928|Whitewater Volcanics|45112|5|Briefly described|p48|||||||||
19928|Whitewater Volcanics|45140|6|Mentioned|p12-13, p21|||Kimberley region.|~1900 Ma.|||||
19928|Whitewater Volcanics|46797|4|Described|p80|||Dates given||||||
19928|Whitewater Volcanics|46864|6|Mentioned|p39|||Age dates discussed.||||||
19928|Whitewater Volcanics|48931|3|Fully described|p20|||||||||
19928|Whitewater Volcanics|48938|4|Described|p9|||See also p13.||||||14-NOV-06
19928|Whitewater Volcanics|48950|6|Mentioned|p36|||||||||
19928|Whitewater Volcanics|50437|5|Briefly described|p1.5, 2.1, 3.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Paperbark Supersuite. Age: 1854-1855 +/- 5Ma (Shrimp), 1850 +/- 3Ma (U-Pb con.).||||||07-NOV-08
19928|Whitewater Volcanics|60006|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Halls Creek Orogen. Of Lamboo Complex. Unconformably overlies Halls Creek Group. Porphyritic rhyolite, rhyodactite||||||07-NOV-08
19928|Whitewater Volcanics|60283|5|Briefly described|p25 Fig.2|||Halls Creek Orogen.|c.1855 Ma.||||Felsic volcanism.|
19928|Whitewater Volcanics|60533|5|Briefly described|p593|Paleoproterozoic|Paleoproterozoic|Co-magmatic with Paperbark Supersuite.||||||07-NOV-08
19928|Whitewater Volcanics|60682|4|Described|piii|Paleoproterozoic|Paleoproterozoic|Part of Lamboo Complex. Age: 1865-1850Ma. Porphyritic rhyolite and rhyodacite. Geological Province: Halls Creek Orogen.||||||07-NOV-08
19928|Whitewater Volcanics|60714|6|Mentioned|p121.|Orosirian|Orosirian|Halls Creek Orogen. Directly overlies ?glacial "boulder phyllite', implying yet another glacial episode in the Paleoproterozoic.|1855 +/- 5 Ma(U-Pb zircon: Page and Sun, 1994).|||||
19928|Whitewater Volcanics|60724|4|Described|p16, p5 Fig. 2|Paleoproterozoic|Paleoproterozoic|Thick-bedded, massive, med.to fine gr. qtz-feldspar porphyry, often with pumice fragments; minor laminated vol'clastics and amyg.basalt. Unconf. on Marboo Fm; unconf.under O'Donnell Fm. Intruded by Bow batholith granite. Age:1850+/-5Ma (U-Pb). Hooper Cmplx||||||18-JUN-13
19928|Whitewater Volcanics|62715|5|Briefly described|p1753, p1779|Paleoproterozoic|Paleoproterozoic|Age: 1865-1850Ma.||||||07-NOV-08
19928|Whitewater Volcanics|63866|5|Briefly described|p105, p129, p132-p133, p138|Orosirian|Orosirian|Litchfield Province, Pine Creek Orogen. Numeric age is interpreted as the crystallisation age. Comagmatic with the Castlereagh Hill Porphyry and Greenvale Porphyry.|1849 +/- 6 Ma (Worden et al, in review)|||Unconformably overlies the Marboo Formation. Overlain by the Speewah Group.|Felsic volcanics including quartz-phyric rhyolite, rhyodacite, welded ignimbrite and tuff.|
19928|Whitewater Volcanics|64104|6|Mentioned|p76 fig 10, p76|Paleoproterozoic|Paleoproterozoic|Possible source of some clasts in Duerdin Group.||||||
19928|Whitewater Volcanics|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Fine- to medium-grained quartz-feldspar rhyolite- to dacite-porphyry and welded ignimbrite; minor agglomerate, lapilli tuff, and volcaniclastic rock.||||||09-DEC-08
19928|Whitewater Volcanics|64725|5|Briefly described|p75.|Paleoproterozoic|Paleoproterozoic|Halls Creek Orogen. Host to low-sulfidation adularia-sericite epithermal Au deposit.|1855 Ma.|||||
19928|Whitewater Volcanics|64730|6|Mentioned|p141|Paleoproterozoic|Paleoproterozoic|Felsic. Age from Page and Hancock 1988; Tyler et al. 1999; Griffin et al. 2000.|ca. 1855-1850 Ma.|||Unconformably overlies Marboo Formation.||03-MAY-12
19928|Whitewater Volcanics|64731|5|Briefly described|p164|Paleoproterozoic|Paleoproterozoic|In Hooper Complex and Western Zone of Hall Creek Orogen.|1860 - 1850 Ma.|||Co-magmatic with Castlereagh Hill Porphyry.||12-APR-12
19928|Whitewater Volcanics|64956|5|Briefly described|p2 Tb. 26, p95-96|Paleoproterozoic|Paleoproterozoic|Cryst. Age: 1849+/-6Ma. Geological province: Halls Creek Orogen. Sample is a K-feldspar-quartz-phyric rhyodacite - generally massive and unfoliated. The sample is dark coloured with glassy matrix; subhedral K-feldspar and quartz phenocrysts are common.||||||07-FEB-11
19928|Whitewater Volcanics|65331|5|Briefly described|Map legend + overview geology map legend|Palaeoproterozoic|Palaeoproterozoic|Of Lamboo Complex, Halls Creek Orogen. Porphyritic rhyolite, rhyodacite||||||
19928|Whitewater Volcanics|66127|5|Briefly described|Plate 1, 2, 3, 4.|Paleoproterozoic|Paleoproterozoic||c.1855 Ma.||||Volcanic and sedimentary rocks.|
19928|Whitewater Volcanics|66845|5|Briefly described|p536, p538, p540|Paleoproterozoic|Paleoproterozoic|Unconformably overlies turbiditic quartz wacke. Western zone of Lamboo Complex. Closely related to Paperbark supersuite. Indistinguishable crystallisation ages for Paperbark supersuite, Whitewater Volcanics and related intrusions concludes the Western Zone of the Lamboo Complex is a continuation of the Hooper Complex in the west Kimberley.|c. 1855 Ma|||||
19928|Whitewater Volcanics|66846|6|Mentioned|p548, p549 Fig.2|Orosirian|Orosirian|In the Western Zone of the Lamboo Complex.||||Intruded by Paperbark supersuite granites.|Felsic volcanics.|
19928|Whitewater Volcanics|67323|5|Briefly described|p29|||Coeval with Paperbark Suite.|~1865-1850 Ma.||||Felsic volcanics.|
19928|Whitewater Volcanics|67563|6|Mentioned|p120 Fig.1|||||||||
19928|Whitewater Volcanics|68078|5|Briefly described|p5, p19|Paleoproterozoic|Paleoproterozoic|Age is age of crystallization and intrusion into marboo formation.|1855 Ma|||Unconformably overlies Marboo Formation, unconformably overlain by Speewah Group|Felsic volcanic rocks.|
19928|Whitewater Volcanics|68244|6|Mentioned|p661|||Mount House area, Kimberley region.||||||
19928|Whitewater Volcanics|68542|6|Mentioned|p12|||||||||
19928|Whitewater Volcanics|68576|5|Briefly described|Q_2: p12|||Kimberley region. Same age as Leichhardt Volcanics in the Mount Isa region; possibly part of a vast array of coalescing caldera fields across northern Australia.|||||Felsic tuffs.|
19928|Whitewater Volcanics|69003|5|Briefly described|p5, p18-19|Paleoproterozoic|Paleoproterozoic|W zone, Lamboo Province, Halls Creek Orogen.|c.1855 Ma.|||Overlies Marboo Formation.||
19928|Whitewater Volcanics|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen. Age from OZCHRON1. Comment: 'This is an excellent age for igneous crystallisation of the Whitewater Volcanics. It agrees with the conventional age (1850+/-5) and with the Whitewater age in the West Kimberley (1854+/-5) where Whitewater Volcanics are intruded by 1864-1852 Ma granite.'|crystallisation age 1857+/-4 Ma U/Pb SHRIMP|Paperbark Supersuite|Includes 3 unnamed units.||porphyritic rhyolite to dacite; coherent lavas, subvolcanic intrusions, and pyroclastic deposits; commonly crystal rich; minor volcanic breccia, lapilli tuff, and volcaniclastic rock; locally foliated|
19928|Whitewater Volcanics|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also GA_geochron.csv.|1850-1857 Ma|Paperbark Supersuite|||Porphyritic rhyolite to dacite; coherent lavas, subvolcanic intrusions, and pyroclastic deposits; commonly crystal rich; minor volcanic breccia, lapilli tuff, and volcaniclastic rock. Coarse grained feldspathic sandstone and pebble conglomerate.|
19928|Whitewater Volcanics|69417|5|Briefly described|p2:5|Orosirian|Orosirian|Halls Creek Orogen.||||Is intruded by Bow River Granite.||12-JUL-16
19928|Whitewater Volcanics|69422|5|Briefly described|p7:1-3|Orosirian|Orosirian|Western Zone, Halls Creek Orogen. Considered to be comagmatic with Bow River Granite (Paperbark Supersuite). Deformed, metamorphosed and intruded during the 1865-1850 Hooper Orogeny. SHRIMP U-Pb zircon age; agrees with WA ages.|1849 +/- 6 Ma (Worden et al., 2008).|||Unconfortmably overlies Marboo Volcanics. Is intruded by Bow River Granite.|Red-brown porphyritic rhyolite and rhyodacite; angular phenocrysts of quartz and feldspar up to 2-4mm long. Ignimbrites predominate over lava flows: probably subaerial.|12-JUL-16
19928|Whitewater Volcanics|69435|6|Mentioned|p20:4|||||||Is overlain unconformably by Legune Formation.||12-JUL-16
19928|Whitewater Volcanics|69452|6|Mentioned|p36:6|||Halls Creek Orogen.||||Is overlain unconformably by Ragged Range Conglomerate and Kellys Knob Sandstone.||12-JUL-16
19928|Whitewater Volcanics|69585|5|Briefly described|p4, p7|Orosirian|Orosirian|Western Lamboo Province.|c.1855 Ma.|||Is overlain unconformably by O'Donnell Formation (Speewah Group).||
19928|Whitewater Volcanics|69597|5|Briefly described|p3, p5 fig 2b|Paleoproterozoic|Paleoproterozoic|Western Lamboo Province. Thought to have formed by partial melting of Paleoproterozoic to Archean imtermediate to felsic rocks.|1855-1850 Ma|Paperbark Supersuite||||
19928|Whitewater Volcanics|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2; Hooper Orogeny; Hooper Orogeny D1/M1 - Western Zone; Hooper Orogeny D2/M2 - Western Zone. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|1864-1854 Ma (Inferred)|Unit of Paperbark Supersuite.|||Porphyritic rhyolite to dacite; coherent lavas, subvolcanic intrusions, and pyroclastic deposits; minor volcanic breccia, lapilli tuff, and volcaniclastic rock; locally foliated, coarse-grained feldspathic sandstone and pebble conglomerate|
19928|Whitewater Volcanics|69660|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Kimberley Craton.|1862 - 1854 Ma; Griffin et al. (2000).|Unit in Paperbark Supersuite.|||Porphyritic rhyolite to dacite; coherent lavas, subvolcanic intrusions, and pyroclastic deposits; commonly crystal-rich; minor volcanic breccia, lapilli tuff, and volcaniclastic rock; locally foliated.|
19928|Whitewater Volcanics|70126|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Lamboo Province; Halls Creek Orogen; North Australian Craton.|1864-1854 Ma (Griffin et al., 2000).|Paperbark Supersuite.|||Porphyritic rhyolite to dacite; coherent lavas, subvolcanic intrusions, and pyroclastic deposits; commonly crystal-rich; minor volcanic breccia, lapilli tuff, and volcaniclastic rock; locally foliated.|
19928|Whitewater Volcanics|70154|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|See also GA_geochron.csv.|1854-1864 Ma|Paperbark Supersuite|||Porphyritic rhyolite to dacite; coherent lavas, subvolcanic intrusions, and pyroclastic deposits; commonly crystal rich; minor volcanic breccia, lapilli tuff, and volcaniclastic rock; locally foliated.Metadacite and meta rhyodacite..|
19928|Whitewater Volcanics|70206|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|||Lamboo Complex|||Porphyritic rhyolite, rhyodacite.|
19928|Whitewater Volcanics|70731|5|Briefly described|p267-268,274,276,278|Orosirian|Orosirian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton. Felsic volcanics and volcaniclastics intepreted to be the last period of felsic magmatism. In contact with Speewah Group. Felsic equivalent to Paperbark Supersuite.|c. 1855 Ma|||Underlain by Marboo Formation.||
19928|Whitewater Volcanics|70812|5|Briefly described|p3, p6-p7, p19-p20, p29, p38|Orosirian|Orosirian|Age derived from cogenetic relationship with the Paperbark Supersuite. This unit may have formed as a result of extensional processes towards the end of the Hooper Orogoney. Hosts occurrences of Au, Ag, Pb, Cu, Mo and Zn.||||Overlies the Marboo Formation.|Felsic volcanic and volcaniclastic rocks.|
19928|Whitewater Volcanics|70851|5|Briefly described|p3-p5, p16, p20, p24, p29, p35|Paleoproterozoic|Paleoproterozoic|Western Zone, Lamboo Province. Geophysical response is discussed.|c. 1855 Ma|Paperbark Supersuite||||28-MAR-23
19928|Whitewater Volcanics|71113|5|Briefly described|p96,99|Orosirian|Orosirian|Geological province: Western Zone, Lamboo Province, Halls Creek Orogen. Developed during extension and partial melting toward the end of the Hooper Orogeny.|c. 1855 Ma|||Underlain unconformably by Marboo Formation.||
19928|Whitewater Volcanics|71140|6|Mentioned|p96, 99|Orosirian|Orosirian|Western Zone, Lamboo Province, Halls Creek Orogen. Produced by extension and partial melting toward the end of the Hooper Orogeny.|c.1855 Ma.|||Unconformably overlies Marboo Formation.|Felsic volcanic rocks.|
19928|Whitewater Volcanics|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma); Hooper Orogeny D2/M2-Western Zone (1864-1850 Ma); Hooper Orogeny (1870-1850 Ma); Hooper Orogeny D1/M1-Western Zone (1870-1864 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 500k_interpgeop_lut.csv, 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyp_lut.csv, 1m_interpgeop_lut.csv and geochron files.|1864 to 1854+\-5 Ma (inferred-isotopic)|Unit of Paperbark Supersuite.|||Thick-bedded, massive fine- to medium-grained quartz-feldspar rhyolite to dacite porphyry and welded ignimbrite; minor agglomerate, lapilli tuff, dacitic and rhyodacitic ash-flow tuff, and volcaniclastic sedimentary rock, minor siltstone interbeds.|
19928|Whitewater Volcanics|71281|4|Described|p421-422|Paleoproterozoic|Paleoproterozoic|Lamboo Province. Generated at the peak of the 1870-1850 Ma Hooper Orogeny. Age also given as c.1855 Ma.|1864-1852 Ma.|Paperbark Supersuite.||Is overlain unconformably by O'Donnell Formation (Speewah Group).|Late-stage erupted felsic-rich volcanics.|
19928|Whitewater Volcanics|71397|4|Described|p2,5|Orosirian|Orosirian|Geological province: Western Zone, Lamboo Province, Halls Creek Orogen. Considered to be the volcanic and subvolcanic equivalent to plutonic rocks in the Paperbark Supersuite 9see p2 for references). Three samples from Whitewater Volcanics yielded igneous crystallisation dates of 1854+\-5, 1854+\-6 and 1857+\-4 Ma, suggest contemporaneous felsic volcanism over a strike length >600 km (Griffin et al., 2000a).|c. 1854 Ma|Unit of Paperbark Supersuite.|||Volcaniclastic rocks interlayered with felsic to intermediate volcanic rocks.|
19928|Whitewater Volcanics|71592|5|Briefly described|Appendix A.|||Halls Creek Orogen.|1849+/-6 Ma (crystallisation: U-Pb zircon SHRIMP)||||Rhyodacite.|
19928|Whitewater Volcanics|71811|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen, North Australian Craton.|1857 - 1849 Ma.|Paperbark Supersuite.|||Porphyritic rhyolite to dacite; coherent lavas, subvolcanic intrusions, and pyroclastic deposits; commonly crystal-rich; minor volcanic breccia, lapilli tuff, and volcaniclastic rock; locally foliated.|
19928|Whitewater Volcanics|71873|5|Briefly described|p426,442-443|Orosirian|Orosirian|Geological province: Lamboo Province. Deformed by Hooper Orogeny c. 1860 Ma. Coincides with Rose Bore Granite and Panton Intrusion and Ruins Dolerite, which reflects the suturing of the Western and Central zones during the amphibolite-granulite facies Hooper Orogeny.|c. 1860-1850 Ma|Unit of Paperbark Supersuite.||Intruded into Marboo Formation.||
19928|Whitewater Volcanics|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Central Zone, Halls Creek Orogen.|Max age ~1864, Min age 1854+/-5 Ma.|Paperbark Supersuite.|||Porphyritic rhyolite to dacite; coherent lavas, subvolcanic intrusions, and pyroclastic deposits; commonly crystal rich; minor volcanic breccia, lapilli tuff, and volcaniclastic rock; locally foliated.|
19928|Whitewater Volcanics|72437|5|Briefly described|p5, p9, p24, p27, p33|Palaeoproterozoic|Palaeoproterozoic|Hooper Complex and Lamboo Complex. Previously described in Gellatly et al (1975), Griffin and Sheppard et al (1997). Comagmatic with rocks of the Paperbark Supersuite and the Greenvale Porphyry and Castlereagh Hill Porphyry. Alteration and low-grade metamorpism is widespread but textures are almost without exception igneous.|c. 1855|||||
19928|Whitewater Volcanics|72490|6|Mentioned|p3|Orosirian|Orosirian|Lamboo Province.|ca. 1855 Ma|||Underlain by Marboo Formation.|Felsic volcanic rocks.|
19936|Whitula Formation|23982|6|Mentioned|p97 Appendix 13|||Geological Province: Great Artesian Basin.||||||
19936|Whitula Formation|33078|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
19936|Whitula Formation|33079|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
19936|Whitula Formation|35793|6|Mentioned|Fig.2|||||||||
19936|Whitula Formation|37607|6|Mentioned|Fig.4|||||||||
19936|Whitula Formation|38226|6|Mentioned|Table 1|||||||||
19936|Whitula Formation|39445|5|Briefly described|Table 14|||||||||
19936|Whitula Formation|39478|6|Mentioned|Table 1|||||||||
19936|Whitula Formation|40739|6|Mentioned|p589|||||||||
19936|Whitula Formation|41198|6|Mentioned|Table 1|||||||||
19936|Whitula Formation|42375|5|Briefly described|Table 1 P11|||In Waite Basin. Previously used in Qld.||||||19-DEC-06
19936|Whitula Formation|42543|6|Mentioned|p6|||SA.||||||
19936|Whitula Formation|42746|6|Mentioned|p18|||||||||
19936|Whitula Formation|44041|6|Mentioned|Fig.1|||||||||
19936|Whitula Formation|44133|5|Briefly described|p190 Fig. 10.30|Early Pliocene|Late Miocene|||||||
19936|Whitula Formation|46802|6|Mentioned|Table 1|||||||||
19936|Whitula Formation|46854|6|Mentioned|Fig.1|||||||||
19936|Whitula Formation|46911|6|Mentioned|Fig.1|||Geological map and distribution of weathered profiles.||||||
19936|Whitula Formation|60080|5|Briefly described|Map legend|Pliocene|Miocene|Sandstone, siltstone, mudstone, and claystone, oxidised; minor gypsum and immature silcrete.  Overlies Glendower Formation; underlies Cadelga Limestone.||||||20-AUG-04
19936|Whitula Formation|61155|5|Briefly described|p17|Late Pliocene|Middle Miocene|Deposited in synclinal basins in southwest Queensland. Overlies the Cadelga Limestone. Age: 12-2Ma. Thickness: 220m. See also p4, p5.||||||
19936|Whitula Formation|64047|2|Defined|p61|Late Miocene|Late Miocene|Unconformably overlies Glendower Fm. or weathered Winton Fm. Overlain by Quaternary alluvium. Max. thickness: 160m. Contains interbedded quartzose sandstone, siltstone, mudstone and claystone with minor conglomerate; lignite and gypsum also present.||||||16-APR-08
19936|Whitula Formation|66131|6|Mentioned|p242 Fig.2, p245, p254|Miocene|Miocene|Senior and Mabbutt (1979) place the Cadelga Limestone and the Doonbara Formation at the top of this unit. Middle to Late Miocene in age (from Fig.2 - stratigraphic correlation chart).|||Includes Cadelga Limestone and Doonburra Formation.|||
19936|Whitula Formation|69599|5|Briefly described|p584, p599-602, p651|Miocene|Miocene|Senior et al. (1978). Eromanga, Lake Eyre Basins. Mostly known from drill holes. 53-160m thick. Fluviatile to lacustrine deposits. No fossils known. RELATED UNITS (continued): Also correlated (at least partly) with Horse Creek, Noranside, Austral Downs Limestones.||||Unconformably overlies Glendower and Winton Formations. Is overlain by Cadelga Limestone. Correlated with Doonbara, Poodyea Formations; and Mount Coley Sinter; see COMMENTS for more.|Interbedded quartzose sandstone, siltstone, mudstone and conglomerate; gypsiferous and lignitic in part.|
19936|Whitula Formation|70821|5|Briefly described|p25, p82|Miocene|Oligocene|Senior and Johnston (1974). Lake Eyre Basin (SA). Hydrostratigraphic properties.||||Equivalent to Namba Formation.||
19936|Whitula Formation|70823|5|Briefly described|p47|Pliocene|Late Oligocene|Maximum thickness of 160m.|ca 28 Ma||||Clay, fine-grained sand, carbonate and minor conglomerate.|17-SEP-18
19939|Whitworth Quartzite|22438|6|Mentioned|p549, Fig.12|||||||||
19939|Whitworth Quartzite|22585|5|Briefly described|Fig2 P737, Fig3|||Actually written as Whitworth Qtz.||||||19-DEC-06
19939|Whitworth Quartzite|23395|5|Briefly described|p386 Fig.3|||Of the Myally Subgroup.||||||19-DEC-06
19939|Whitworth Quartzite|23396|5|Briefly described|p407 Fig.2|||Of the Myally Subgroup (Haslingden Group).||||||19-DEC-06
19939|Whitworth Quartzite|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Myally Subgroup (Haslingden Group).  Overlies the Bortala Formation.||||||25-AUG-04
19939|Whitworth Quartzite|30534|2|Defined|p304|Precambrian|Precambrian|||||||
19939|Whitworth Quartzite|33900|4|Described|p12|||||||||
19939|Whitworth Quartzite|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
19939|Whitworth Quartzite|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
19939|Whitworth Quartzite|38232|6|Mentioned|p84|||See also p89.||||||19-DEC-06
19939|Whitworth Quartzite|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
19939|Whitworth Quartzite|39445|5|Briefly described|Table 2|||See also p40.||||||19-DEC-06
19939|Whitworth Quartzite|39556|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||
19939|Whitworth Quartzite|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Myally Subgroup (Haslinden Group). Feldspathic quartzite, purple sandstone, mudflake conglomerate; feldspathic quartzite, orhtoquartzite, labile sandstone; sandstones, siltstones, mudstones||||||15-JUN-06
19939|Whitworth Quartzite|39622|6|Mentioned|Fig.2|||||||||
19939|Whitworth Quartzite|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
19939|Whitworth Quartzite|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
19939|Whitworth Quartzite|40221|3|Fully described|p10|||||||||
19939|Whitworth Quartzite|40623|5|Briefly described|p99|||||||||
19939|Whitworth Quartzite|41298|6|Mentioned|Map legend|Carpentarian||||||||
19939|Whitworth Quartzite|41307|4|Described|p10|||||||||
19939|Whitworth Quartzite|42166|6|Mentioned|p110|||||||||
19939|Whitworth Quartzite|42523|5|Briefly described|Fig. 2 P373|||||||||
19939|Whitworth Quartzite|45136|5|Briefly described|p49|||||||||
19939|Whitworth Quartzite|45166|5|Briefly described|p14|||||||||
19939|Whitworth Quartzite|46801|6|Mentioned|Fig. 14|||||||||
19939|Whitworth Quartzite|47083|4|Described|p7-8|||Contains three informal members. Of Myally Subgp (Haslingden Gp). Conformably overlain by Lochness Fm. Conformably underlain by Bortala Fm.||||||19-DEC-06
19939|Whitworth Quartzite|50332|6|Mentioned|p17|Proterozoic|Proterozoic|Of the Myally Subgroup.||||||07-FEB-11
19939|Whitworth Quartzite|50536|6|Mentioned|p7.2|||Geological Province: Mount Isa Inlier.||||||
19939|Whitworth Quartzite|61929|5|Briefly described|p128 Fig. 2|||Of the Myally Subgroup.||||||
19939|Whitworth Quartzite|61936|6|Mentioned|p203|||Hosts the Mammoth Cu deposit. Geological Province: Leichhardt Superbasin (Mount Isa Inlier).||||||19-DEC-06
19939|Whitworth Quartzite|62988|5|Briefly described|p34|||Geological Province: Mount Isa Inlier.||||||25-JAN-07
19939|Whitworth Quartzite|63023|5|Briefly described|p1025 Fig. 2, p1029|Paleoproterozoic|Paleoproterozoic|Of Myally Subgroup (Haslingden Group). Age: 1768+/-8Ma. Overlies Bortala Formation; underlies Lochness Formation. Geological Province: Leichardt Superbasin. Pink, fine-grained, well-sorted sandstone. See also p1027 Tb. 1.||||||07-NOV-08
19939|Whitworth Quartzite|63109|6|Mentioned|p1108 Fig. 3|||Overlain by Lochness Formation, underlain by Bortala Formation. Geological Province: Leichhardt Superbasin. Consists of sandstone.||||||
19939|Whitworth Quartzite|63111|5|Briefly described|p1163 Fig. 3, p1164 Tb. 1|Statherian|Statherian|Of Myally Subgroup. Overlain by Lochness Formation, underlain by Bortalla Formation. Age: 1768+/-8Ma. Geological Province: Leichhardt Superbasin. Consists mostly of sandstone.||||||07-FEB-11
19939|Whitworth Quartzite|63113|5|Briefly described|p1214 Fig.2, p1225 Fig.13.|||||Of the Myally Subgroup||Overlies Bortala Formation. Is overlain by Lochness Formation.||
19939|Whitworth Quartzite|63114|5|Briefly described|p1253 Fig.2. |||||Of the Myally Subgroup||Overlies Bortala Formation. Is overlain by Lochness Formation.||
19939|Whitworth Quartzite|63115|6|Mentioned|p1279 Fig.4.|||Leichhardt superbasin.||||||
19939|Whitworth Quartzite|63116|6|Mentioned|p1297 Fig.2, |||Leichhardt superbasin. Material properties detailed.||||||
19939|Whitworth Quartzite|63866|5|Briefly described|p58|||Leichhardt Superbasin.||Myally Supersequence||||
19939|Whitworth 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.|1768 +/- 8 Ma (maximum depositional age).|Myally Subgroup.|||Massive medium to coarse feldspathic to quatzose sandstone, fine purple sandstone and mudflake conglomerate|
19939|Whitworth Quartzite|68020|5|Briefly described|p126||||c. 1760 Ma|Myally Subgroup|||Brittle feldspathic quartzite.|
19939|Whitworth 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.|1768 +/- 8 Ma|Of the Haslingden Group.|||Fine- to coarse-grained quartzites and arenites, fining upwards into thinly bedded sandstones.|01-DEC-17
19939|Whitworth Quartzite|69222|5|Briefly described|p222 Fig.2|Statherian|Statherian|Leichhardt River Fault Trough.||Myally Subgroup||Overlies Pickwick Metabasalt||09-FEB-18
19939|Whitworth Quartzite|69591|5|Briefly described|p33, p57|||Mount Oxide and Leichhardt River Domains, Leichhardt Superbasin. Part of Myally Supersequence. Tide-dominated shelf/aeolian deposits.|1768 +/- 8 Ma (MDA: Neumann et al., 2006).|Myally Subgroup.|||Massive medium to coarse feldspathic to quartzose sandstone, fine purple sandstone and mudflake conglomerate.|
19939|Whitworth Quartzite|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Myally Subgroup.||Overlies Bortala Formation. Is overlain by Lochness Formation.|Massive medium- to coarse-grained feldspathic to quartzose sandstone, fine-grained purple sandstone and mudflake conglomerate. (Separately mapped) white to pink feldspathic sandstone; minor siltstone.|
19939|Whitworth Quartzite|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Myally Subgroup.||Overlies Bortala Formation. Is overlain by Lochness Formation.|Massive medium- to coarse-grained feldspathic to quartzose sandstone, fine-grained purple sandstone and mudflake conglomerate. (Separately mapped) white to pink feldspathic sandstone; minor siltstone.|
19939|Whitworth Quartzite|71592|5|Briefly described|Appendix A.|||Leichhardt River Domain, Mount Isa Orogen.|1768+/-8 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
19939|Whitworth Quartzite|71980|5|Briefly described|map legend sheet 1|Proterozoic|Proterozoic|From base: Coastal onlap including washover facies; subtidal shelf; coastal offlap, coarsening up shoreface.||Of Myally Subgroup|||Arkose, felspathic sandstone, quartz arenite;|
19939|Whitworth 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 Lochness Formation and is shown to partially underlie Quilalar Formation.||
19939|Whitworth 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 Lochness Formation and is shown to partially underlie Quilalar Formation.||
19939|Whitworth Quartzite|72919|6|Mentioned|p63|||||Myally Subgroup, Myally Supersequence||||
19939|Whitworth Quartzite|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Mount Isa Province, Leichhardt Superbasin.||Myally Subgroup||Underlain by Lochness Formation. Partly overlain(?) Quilalar Formation.||
19939|Whitworth Quartzite|73525|6|Mentioned|p4-5 Fig.2, p19 Fig.13|||Leichhardt River Domain.|||||Clastics.|
20031|Wilgunya Subgroup|13516|5|Briefly described|p167 fig 10,  p169 fig 11|Early Cretaceous|Early Cretaceous|Eromanga Basin.||Of Rolling Downs Group||||
20031|Wilgunya Subgroup|23496|6|Mentioned|p59|||||||||
20031|Wilgunya Subgroup|29591|6|Mentioned|p69|||||||||
20031|Wilgunya Subgroup|31168|5|Briefly described|p11|||See also Table 2.||||||
20031|Wilgunya Subgroup|33528|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
20031|Wilgunya Subgroup|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
20031|Wilgunya Subgroup|36228|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
20031|Wilgunya Subgroup|39445|6|Mentioned|Table 11|||||||||
20031|Wilgunya Subgroup|39556|5|Briefly described|Map legend|Cretaceous|Cretaceous|||||||
20031|Wilgunya Subgroup|39899|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
20031|Wilgunya Subgroup|41307|6|Mentioned|p17|||||||||
20031|Wilgunya Subgroup|43110|5|Briefly described|p55|||||||||
20031|Wilgunya Subgroup|43630|6|Mentioned|p70|||||||||
20031|Wilgunya Subgroup|63979|6|Mentioned|p48|||Of the Rolling Downs Group. Superseded Wilgunya Formation. Lower part comprises Wallumbilla Formation.||||||07-FEB-11
20031|Wilgunya Subgroup|66623|6|Mentioned|p258.|||Laterally equivalent to Wallumbilla Formation in NSW.||Unit in Rolling Downs Group (QLD).||||06-JUN-13
20031|Wilgunya Subgroup|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Early Cretaceous|Early Cretaceous|Eromanga/Carpentaria Basins|||||Fossiliferous mudstone, minor labile, glauconitic and quartzose sandstone, calcareous concretions common|
20031|Wilgunya Subgroup|67784|5|Briefly described|p26|Aptian|Barremian|Carpentaria, Eromanga Basins.|||Gilbert River, Wallumbilla, Toolebuc, Allaru, Normanton FZs.|||
20031|Wilgunya Subgroup|69457|5|Briefly described|p41:2-4, 6-11, 14|Early Cretaceous|Early Cretaceous|Casey (1959); Australian Water Resources Council (1975). Eromanga Basin. This Subgroup's nomenclature is more appropriate (than the Marree Subgroup) in the NT, where the Coorikiana Sandstone has not been recognised.||Rolling Downs Group.|Wallumbilla, Toolebuc Formations; Allaru Mudstone.|Is overlain by Manuka Subgroup. Equivalent to Marree Subgroup.||12-JUL-16
20031|Wilgunya Subgroup|69458|6|Mentioned|p42:16|||Eromanga Basin. Some rocks of this unit are mapped as Rumbalara Shale in HALE RIVER, McDILLS map areas.||||Is overlain unconformably by Etingambra Formation.||12-JUL-16
20031|Wilgunya Subgroup|69594|5|Briefly described|p528|||Great Australian Superbasin.||Rolling Downs Group.|Wallumbilla Formation.|||
20031|Wilgunya Subgroup|69599|5|Briefly described|p599|Cretaceous|Cretaceous|||||Is overlain unconformably by the Noranside Limestone.||
20031|Wilgunya Subgroup|69673|6|Mentioned|p156|||||Rolling Downs Group|Includes Wallumbilla Formation, Toolebuc Formation, Allaru Mudstone|Overlain by Manuka Subgroup||
20031|Wilgunya Subgroup|70352|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|||Rolling Downs Group.|Wallumbilla Formation.|||
20031|Wilgunya Subgroup|70572|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|||Rolling Downs Group|Includes Allaru Mudstone, Toolebuc Formation, Wallumbilla Formation.|||20-JAN-22
20031|Wilgunya Subgroup|73083|6|Mentioned|p62, p65, p77|||Term used where the Wallumbilla Mudstone and Allaru Mudstone are indistinguishable. [Written as Wilgunyah Subgroup on p65 and p77].||||||
20124|Wills Creek 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
20124|Wills Creek Granite|37413|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
20124|Wills Creek Granite|37862|4|Described|p584|||||||||
20124|Wills Creek Granite|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
20124|Wills Creek Granite|38900|6|Mentioned|p55|||||||||
20124|Wills Creek Granite|39445|5|Briefly described|Table 2|||||||||
20124|Wills Creek Granite|40840|6|Mentioned|Map legend|||||||||
20124|Wills Creek Granite|45161|4|Described|p29|||||||||
20124|Wills Creek Granite|45166|6|Mentioned|p11|||||||||
20124|Wills Creek Granite|46962|6|Mentioned|p249|||||||||
20124|Wills Creek Granite|49009|2|Defined|p49|Proterozoic|Proterozoic|Mapped as Argylla Formation and Kalkadoon Group(Carter and Opik, 1963).||||||19-DEC-06
20124|Wills Creek Granite|49041|5|Briefly described|Table 2|||||||||
20124|Wills Creek Granite|50100|5|Briefly described|p16|Proterozoic|Proterozoic|Of the Kalkadoon Batholith.  Min. age: 1830Ma (Wyborn and Page, 1983).||||||
20124|Wills Creek Granite|50536|5|Briefly described|p1.4, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Kalkadoon Suite.||||||07-NOV-08
20124|Wills Creek Granite|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Medium to coarse leucocratic biotite granite.||||||
20124|Wills Creek Granite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map., p14|Paleoproterozoic|Paleoproterozoic|Kalkadoon Igneous Event. Kalkadoon-Leichhardt Domain, central Mount Isa Block.||Kalkadoon Suite or Supersuite|||Medium to coarse biotite granite and leucogranite; minor aplite.|
20124|Wills Creek Granite|69591|5|Briefly described|p31, p60|||Kalkadoon Batholith, Kalkadoon-Leichhardt Domain, Mount Isa Province.||Kalkadoon Suite.|||Medium to coarse biotite granite and leucogranite; minor aplite.|
20124|Wills Creek Granite|73553|6|Mentioned|p6, p8 Fig.1.2.3|||Kalkadoon-Leichhardt Domain.||Kalkadoon Suite||||
20256|Winnecke Granophyre|22716|5|Briefly described|table4, p232|Orosirian|Orosirian|Age: 1830-1815 Ma.||||||19-DEC-06
20256|Winnecke Granophyre|23621|5|Briefly described|p39|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20256|Winnecke Granophyre|23809|5|Briefly described|p13|Paleoproterozoic|Paleoproterozoic|Of the Winnecke Suite.  Age: 1815+/-5Ma (Ozchron, AGSO).||||||07-NOV-08
20256|Winnecke Granophyre|24197|5|Briefly described|p7, p26|Proterozoic|Proterozoic|Of the Granites Supersuite. Geological Province: Granites-Tanami Block.||||||07-FEB-11
20256|Winnecke Granophyre|29804|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20256|Winnecke Granophyre|29805|4|Described|Table 1|||||||||
20256|Winnecke Granophyre|29809|6|Mentioned|p417|||||||||
20256|Winnecke Granophyre|29811|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20256|Winnecke Granophyre|31361|4|Described|Table 1|||See also age Table 2.||||||
20256|Winnecke Granophyre|31412|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20256|Winnecke Granophyre|32659|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20256|Winnecke Granophyre|35231|4|Described|Table.1|||||||||
20256|Winnecke Granophyre|36532|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20256|Winnecke Granophyre|39571|6|Mentioned|p130|||||||||
20256|Winnecke Granophyre|39887|6|Mentioned|p453|||||||||
20256|Winnecke Granophyre|39888|6|Mentioned|Fig.7|||||||||
20256|Winnecke Granophyre|41465|6|Mentioned|p9|||||||||
20256|Winnecke Granophyre|41961|6|Mentioned|Table 1 P39|||||||||
20256|Winnecke Granophyre|41977|6|Mentioned|p483|||||||||
20256|Winnecke Granophyre|42504|5|Briefly described|Table 3 P60|||||||||
20256|Winnecke Granophyre|42754|6|Mentioned|p3|||||||||
20256|Winnecke Granophyre|43832|6|Mentioned|Table 17 p90||Paleoproterozoic|||||||07-NOV-08
20256|Winnecke Granophyre|44965|14|Not recorded|Not recorded|||||||||
20256|Winnecke Granophyre|45140|2|Defined|p12-13, p15, p18, p21-25, p30, p32-35|Paleoproterozoic|Paleoproterozoic|See also p37-39, p41, p62, p70, p74, Appx.p8-9. Traves (1955); Blake et al. (1975). Named after Winnecke Creek. The Granites-Tanami Block. The type area is at 18deg 46'S, 130deg 12'E on the W side of the Tanami-Hooker Creek track to the N of Winnecke Creek. Is probably co-magmatic with the acid lavas of the Mount Winnecke Formation. Has a thin metamorphic aureole. Described as an epizonal pluton. Chemically similar to Slatey Creek Granite; geochemistry detailed.|1802 +/- 15 Ma (Rb-Sr: Page et al., 1976).|||Intrudes the Tanami Complex and Mount Winnecke Formation. Is overlain by Antrim Plateau Volcanics,and ?Gardiner Sandstone against which it is faulted.|Granophyre, pale pink to grey, commonly porphyritic; adamellite, coarser-grained and generally non-porphyritic, occasional small dark xenoliths; and intrusive acid porphyry; locally cut by thin aplitic and andesitic veins or dykes.|
20256|Winnecke Granophyre|46788|4|Described|p4|||||||||
20256|Winnecke Granophyre|46797|6|Mentioned|p80|||Dates given||||||
20256|Winnecke Granophyre|46864|6|Mentioned|p37|||Age dates discussed.||||||
20256|Winnecke Granophyre|48950|2|Defined|p29|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20256|Winnecke Granophyre|50589|5|Briefly described|p1.4, 2.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Of the Granites Suite/Supersuite. Geological Province: Granites-Tanami Block. Age: 1815-1764 +/- 15Ma (Shrimp, Rb-Sr).||||||07-NOV-08
20256|Winnecke Granophyre|61056|5|Briefly described|p778, p785 Tb. 2|Paleoproterozoic|Paleoproterozoic|Included as part of the Mount Winnecke Formation.  Age: ca. 1830-1815Ma. See also "Winnecke Granophyre".||||||07-NOV-08
20256|Winnecke Granophyre|62580|5|Briefly described|p14, p47|||Intrusive of the Winnecke Suite.||||||07-FEB-11
20256|Winnecke Granophyre|63261|5|Briefly described|p12, p15|Paleoproterozoic|Paleoproterozoic|Part of Birthday Suite. Age: 1815Ma. Geochemically equivalent to the rhyolite within Mount Winnecke Formation. Commonly porphyritic, biotite-bearing; includes medium- to coarse-grained monzogranite and granodiorite with micrographic/myrmekitic textures.||||||07-FEB-11
20256|Winnecke Granophyre|64662|6|Mentioned|p43|Orosirian|Orosirian|Age: 1815+/-5Ma. Intrudes Ware Group.||||||07-FEB-11
20256|Winnecke Granophyre|64677|6|Mentioned|p20|||||||Intrudes Helena Creek beds.||
20256|Winnecke Granophyre|64733|6|Mentioned|p173|||High-level intrusive. Emplacement accompanied deposition of Ware Group.||||||20-APR-12
20256|Winnecke Granophyre|65358|5|Briefly described|p9-10, p9 Fig.8|||Of Birthday Suite. Has auriferous quartz veins.||||||
20256|Winnecke Granophyre|65359|4|Described|p1-38.|Statherian|Orosirian|Tanami Region. Intrudes Mount Winnecke Formation; comagmatic with Mount Winnecke Formation's volcanic component. Biotite granophyre, biotite-quartz-monzonite, biotite-hornblende syenogranite, quartz-feldspar porphyry, intrusive acid porphyry. Geochemistry detailed. 1815+/-5 Ma; SHRIMP U-Pb zircon (Ozchron). Abundant Zn and Sn.||||||
20256|Winnecke Granophyre|69426|5|Briefly described|p11:4 Fig.11.3, 11:7, 10-12|Orosirian|Orosirian|Magmatic crystallisation age.|1815 +/- 5 Ma (Page, 1998).|Birthday Suite.||Intrudes Mount Winnecke Formation.|Granophyre, quartz-feldspar porphyry and syenogranite; commonly porphyritic; features quartz, alkali feldspar, plagioclase and brown biotite in a quartz and alkali feldspar groundmass. Also medium- to coarse-grained monzogranite and granodiorite.|12-JUL-16
20256|Winnecke Granophyre|70291|5|Briefly described|p180-181|Orosirian|Orosirian|Geological province: Tanami. Coeval with deposition of, and intrudes Ware Group.||Unit of Birthday Suite.||||
20256|Winnecke Granophyre|70848|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region.|1825-1815 Ma.|Birthday Suite.|||Biotite-bearing syenogranite, monzogranite, including minor quartz-feldspar porphyry, quartz-phyric rhyolite.|
20256|Winnecke Granophyre|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite, granophyre|
20256|Winnecke Granophyre|71592|5|Briefly described|Appendix A.|||Tanami Orogen.|1815+/-5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granophyre.|
20256|Winnecke Granophyre|73089|5|Briefly described|p8, p39|Orosirian|Orosirian|Considered to be part of the same magmatic event that produced the felsic volcanic rocks [of the Ware Group?].|1815 +/- 5 Ma [1825 +/- 5 Ma elsewhere?]|Birthday Suite||Intrudes Mount Winnecke Formation.||
20268|Winton Formation|12597|5|Briefly described|p492 Tb.1, p500, p501|Cenomanian|Cenomanian|Eromanga Basin. 400-700m, locally up to 1200m, thick.||||Overlies Mackunda Formation.|Basal paralic-nonmarine transition zone, overlain by non-marine sequence of fine- to medium-grained labile sandstone, siltstone, mudstone and lenticular coal seams.|
20268|Winton Formation|13497|5|Briefly described|p13, p115, p115 fig 6.33|Late Cretaceous|Late Cretaceous|Eromanga Basin. Deposited in a high-sinuosity fluvial environment. See also p144, p144 fig 9.2, p146, p148-p154, .||||Overlies the Mackunda Formation and the Oodnadatta Formation. Unconformably overlain by the Mount Howie Sandstone and the Eyre Formation.|Sandstone, siltstone, shale and coal.|
20268|Winton Formation|13516|6|Mentioned|p167 fig 10, p169 fig 11, p171 fig 12|Late Cretaceous|Late Cretaceous|In Eromanga Basin.||||||
20268|Winton Formation|22464|6|Mentioned|p9||Late Cretaceous|Also p8. In the Eromanga Basin.||||||19-DEC-06
20268|Winton Formation|22587|5|Briefly described|p71|Cenomanian|Albian|In the Eromanga Basin.||||||19-DEC-06
20268|Winton Formation|22773|6|Mentioned|p338|||||||||
20268|Winton Formation|22839|6|Mentioned|P33|||||||||
20268|Winton Formation|22857|4|Described|p296-7 Tb 22.1, p326, p552 Tb A1.13|Cenomainian|Cenomainian|Of the Rolling Downs Group. Interbedded mudstone and lithic and feldspathic arenite. Max. thickness: 400m in NSW. Geological Province: Eromanga Basin. See also p312-3 Fig. 22.6.||||||
20268|Winton Formation|22862|6|Mentioned|p327||Cenomanian|||||||
20268|Winton Formation|22865|4|Described|p314,Table22.1p296-7|Cenomanian|Cenomanian|||||||
20268|Winton Formation|22883|5|Briefly described|P31, Fig2||Late Cretaceous|Underlying unit is Mackunda Formation.||||||19-DEC-06
20268|Winton Formation|22912|6|Mentioned|34|||Geological province: Eromanga Basin.||||||19-DEC-06
20268|Winton Formation|23054|6|Mentioned|Fig5p22|||||||||
20268|Winton Formation|23056|6|Mentioned|9|||Geol province Eromanga Basin. Parent Rolling Downs Group||||||
20268|Winton Formation|23154|5|Briefly described|Map Legend|Late Cretaceous|Late Cretaceous|Geological Province - Eromanga Basin. Of the Neales River Group.||||||19-DEC-06
20268|Winton Formation|23155|4|Described|p33|Late Cretaceous|Early Cretaceous|Uppermost Eromanga Basin unit known on STRZELECKI, and is disconformably overlain by Tertiary Eyre Formation.||||||19-DEC-06
20268|Winton Formation|23375|5|Briefly described|Fig2 p265||Cenomanian|In the Eromanga Basin.||||||19-DEC-06
20268|Winton Formation|23425|5|Briefly described|Plate 10.2|||Eromanga Basin Province.||||||
20268|Winton Formation|23818|5|Briefly described|p141 Fig.65, p144 Fig.66|Cenomanian|Cenomanian|Geological Province: Cooper Basin. Of the Manuka Sub-Group. Max. thickness: >2000 ft.||||||18-APR-05
20268|Winton Formation|23830|5|Briefly described|Fig. 3a|Cretaceous|Cretaceous|Geological Province: Boorthanna Trough, eastern Arckaringa Basin.||||||24-JAN-06
20268|Winton Formation|23883|5|Briefly described|p129 Fig. 11.2|Cretaceous|Cretaceous|Of Rolling Downs Group.  Geological Province: Great Australian Superbasin.||||||
20268|Winton Formation|23911|5|Briefly described|p97 Fig. 11|Cretaceous|Cretaceous|Geological Province: Eromanga Basin. Of the Rolling Downs Group.||||||
20268|Winton Formation|23916|5|Briefly described|p523|Cenomanian|Albian|Geological Province: Eromanga Basin.||||||
20268|Winton Formation|23982|5|Briefly described|p35 Fig.7|Cretaceous|Cretaceous|Of Rolling Downs Group. Geological Province: Great Artesian Basin.||||||
20268|Winton Formation|24092|5|Briefly described|p5|Cretaceous|Cretaceous|Geological Province: Great Artesian Basin.||||||
20268|Winton Formation|24112|5|Briefly described|p270|Cenomanian|Albian|Age: 97-90Ma (Krieg et al, 1995). Geological Province: Eromanga Basin||||||
20268|Winton Formation|24175|3|Fully described|p30, p17 Fig. 3|Cenomanian|Albian|Overlain by Eyre Formation; conformably overlies Mackunda Formation.  Max. thickness: 88m.  Geological Province: Eromanga Basin.||||||
20268|Winton Formation|24204|5|Briefly described|p263 Fig.4, p267|Late Cretaceous|Late Cretaceous|Geological Province: Eromanga Basin.||||||17-DEC-04
20268|Winton Formation|24210|5|Briefly described|p133 Fig. 2|Late Cretaceous|Late Cretaceous|Geological Province: Eromanga Basin.||||||
20268|Winton Formation|24243|5|Briefly described|p3 Fig.2|Cretaceous|Cretaceous|Of Rolling Downs Group.||||||
20268|Winton Formation|24251|5|Briefly described|p234 Fig.1|Cenomanian|Cenomanian|Geological Province: Eromanga Basin||||||
20268|Winton Formation|24321|5|Briefly described|Map legend|Cenomanian|Cenomanian|Of the Neales River Group.||||||19-DEC-06
20268|Winton Formation|29591|6|Mentioned|p71|||||||||
20268|Winton Formation|29721|6|Mentioned|Table 137|||||||||
20268|Winton Formation|30019|6|Mentioned|p2|||||||||
20268|Winton Formation|30055|6|Mentioned|p159|||||||||
20268|Winton Formation|30102|6|Mentioned|Table 4|||See also p36,37.||||||19-DEC-06
20268|Winton Formation|30104|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower to Upper? Cretaceous||||||
20268|Winton Formation|30514|6|Mentioned|p102|||Middle Cretaceous age.||||||
20268|Winton Formation|30539|6|Mentioned|p7|||Late Albian - early Cenomanian age||||||
20268|Winton Formation|30540|6|Mentioned|Fig.6|||||||||
20268|Winton Formation|30691|4|Described|p17|||See also p21,Table 4. Lower - Upper Cretaceous||||||19-DEC-06
20268|Winton Formation|30700|6|Mentioned|p28|||||||||
20268|Winton Formation|30803|6|Mentioned|p2|||Cretaceous age||||||
20268|Winton Formation|30804|6|Mentioned|p7|||On Table 1. See also Table 2.||||||
20268|Winton Formation|30807|6|Mentioned|p102|||Suggested map symbol||||||
20268|Winton Formation|30853|5|Briefly described|Table 3|||Lower to Upper Cretaceous||||||
20268|Winton Formation|30854|4|Described|Table 4|||Lower to Upper Cretaceous age.||||||19-DEC-06
20268|Winton Formation|30855|6|Mentioned|Map legend|Cretaceous|Cretaceous|Unit in Rolling Downs Group.||||||19-DEC-06
20268|Winton Formation|30856|4|Described|Table 3|||On p10. Lower-Upper Cretaceous.||||||19-DEC-06
20268|Winton Formation|30857|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
20268|Winton Formation|30914|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
20268|Winton Formation|30918|6|Mentioned|p82|||||||||
20268|Winton Formation|30919|6|Mentioned|Map legend|Cenomanian|Albian|Albian - Cenomanian||||||
20268|Winton Formation|30921|6|Mentioned|Map legend|Oligocene|Oligocene|||||||
20268|Winton Formation|31144|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|L. - U. Cretaceous||||||
20268|Winton Formation|31145|5|Briefly described|Table 1|||L. - U. Cretaceous||||||
20268|Winton Formation|31425|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower-Upper? Cretaceous||||||
20268|Winton Formation|31430|5|Briefly described|Table 1|||L.-U.Cretaceous||||||
20268|Winton Formation|31431|5|Briefly described|Table 3|||L.Cretaceous||||||
20268|Winton Formation|31432|4|Described|Table 1|||L.-U.Cretaceous||||||
20268|Winton Formation|31436|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower to Upper Cretaceous||||||
20268|Winton Formation|31438|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower to Upper Cretaceous||||||
20268|Winton Formation|31441|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
20268|Winton Formation|31443|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|31553|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
20268|Winton Formation|31649|6|Mentioned|p63|||||||||
20268|Winton Formation|31699|4|Described|p133|||Middle Cretaceous||||||
20268|Winton Formation|31706|6|Mentioned|p669|||Cretaceous correlation chart||||||
20268|Winton Formation|31923|6|Mentioned|p15|||||||||
20268|Winton Formation|32274|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
20268|Winton Formation|32275|6|Mentioned|p6|||||||||
20268|Winton Formation|32277|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower Cretaceous - Upper Cretaceous.||||||
20268|Winton Formation|32314|6|Mentioned|Fig. 4|||||||||
20268|Winton Formation|32396|6|Mentioned|p10|||Equivalents||||||
20268|Winton Formation|32413|6|Mentioned|p103|||||||||
20268|Winton Formation|32472|6|Mentioned|p17|||||||||
20268|Winton Formation|32618|6|Mentioned|Table 1|||Perm. Strat. table.||||||
20268|Winton Formation|32696|6|Mentioned|Fig.4|||||||||
20268|Winton Formation|32796|6|Mentioned|p303|||||||||
20268|Winton Formation|32918|6|Mentioned|p20|||||||||
20268|Winton Formation|33016|6|Mentioned|p1|||Table on P1||||||
20268|Winton Formation|33017|6|Mentioned|Table 1|||||||||
20268|Winton Formation|33067|4|Described|Table 1|Late Cretaceous|Early Cretaceous|Of the Rolling Downs Group.||||||07-JUL-04
20268|Winton Formation|33069|4|Described|p7|||||||||
20268|Winton Formation|33072|4|Described|Table 1|||L.Cret.||||||
20268|Winton Formation|33073|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|33075|6|Mentioned|Table 1|||||||||
20268|Winton Formation|33078|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper? Cretaceous||||||
20268|Winton Formation|33079|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
20268|Winton Formation|33081|6|Mentioned|p26|||||||||
20268|Winton Formation|33082|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
20268|Winton Formation|33083|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
20268|Winton Formation|33086|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower to Upper Cretaceous||||||
20268|Winton Formation|33087|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
20268|Winton Formation|33088|4|Described|Table 3|||Of the Rolling Downs Group.||||||19-DEC-06
20268|Winton Formation|33089|4|Described|Table 2|||L.-U.Cret.||||||
20268|Winton Formation|33095|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
20268|Winton Formation|33165|6|Mentioned|Chart|||Correlation chart only||||||
20268|Winton Formation|33368|6|Mentioned|p25|||Strat.Table.||||||
20268|Winton Formation|33372|6|Mentioned|Table 1|||||||||
20268|Winton Formation|33414|6|Mentioned|p212-214,Tb.||Cenomanian|Part of Manuka Sub-Group.||||||
20268|Winton Formation|33448|4|Described|Table 1|||L.-U.Cret.||||||11-JAN-10
20268|Winton Formation|33449|4|Described|Table 1|||L.-U.Cret.||||||
20268|Winton Formation|33452|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower to Upper Cretaceous||||||
20268|Winton Formation|33490|6|Mentioned|p30|||Cret. sediments. Correlation||||||
20268|Winton Formation|33521|6|Mentioned|p10|||Upper Cretaceous||||||
20268|Winton Formation|33561|6|Mentioned|p102|||||||||
20268|Winton Formation|33569|6|Mentioned|p63|||||||||
20268|Winton Formation|33639|5|Briefly described|p12|||L.-U.Cret.||||||
20268|Winton Formation|33640|4|Described|Table 2|||L.-U.Cret.||||||
20268|Winton Formation|33642|6|Mentioned|p144-45,147,148,Tb.1|||Refers Dunstan (1916) & Whitehouse (1954)||||||
20268|Winton Formation|33647|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper? Creataceous||||||
20268|Winton Formation|33648|6|Mentioned|p19|||Stratigraphy.||||||
20268|Winton Formation|33819|6|Mentioned|p1|||||||||
20268|Winton Formation|33820|6|Mentioned|Map legend|Cenomanian|Albian|Albian - Cenomanian||||||
20268|Winton Formation|33821|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
20268|Winton Formation|33822|6|Mentioned|Map legend|Cenomanian|Albian|Albian - Cenomanian||||||
20268|Winton Formation|33823|6|Mentioned|Map legend|Cenomanian|Neocomian|Neocomian - Cenomanian||||||
20268|Winton Formation|33824|6|Mentioned|p7|||P12, Tables 1 & 2||||||
20268|Winton Formation|33825|6|Mentioned|p8|||Strat. table. Lithology||||||
20268|Winton Formation|33827|6|Mentioned|p7|||See also p3 and Tables 1 and 3.||||||19-DEC-06
20268|Winton Formation|33828|6|Mentioned|p9|||See also Table 1||||||
20268|Winton Formation|33831|6|Mentioned|Map legend|Cenomanian|Neocomian|Neocomian - Cenomanian||||||
20268|Winton Formation|33832|6|Mentioned|p6|||Strat.||||||
20268|Winton Formation|33936|6|Mentioned|Fig.3A|||Cret.||||||
20268|Winton Formation|33937|6|Mentioned|p3|||||||||
20268|Winton Formation|33938|6|Mentioned|p19|||Refers Jack (1930).||||||
20268|Winton Formation|33964|4|Described|p6|||||||||
20268|Winton Formation|33971|5|Briefly described|p37|||See also Fig.15.||||||
20268|Winton Formation|34035|6|Mentioned|p544|||Cret.||||||
20268|Winton Formation|34061|6|Mentioned|p53|||||||||
20268|Winton Formation|34065|4|Described|p6|||L.-U. Cret.||||||
20268|Winton Formation|34174|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
20268|Winton Formation|34217|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|34218|4|Described|Table 1|||Lower - Upper Cretaceous. See also pp8,10-12 etc.||||||19-DEC-06
20268|Winton Formation|34254|6|Mentioned|p492|||||||||
20268|Winton Formation|34259|6|Mentioned|p451|||||||||
20268|Winton Formation|34282|6|Mentioned|p88|||See also PP90, 93 etc.||||||
20268|Winton Formation|34287|6|Mentioned|p199|||Cret.||||||
20268|Winton Formation|34356|6|Mentioned|p32|||||||||
20268|Winton Formation|34400|6|Mentioned|p14|||Lower Cretaceous||||||
20268|Winton Formation|34454|5|Briefly described|Table 1|||Cretaceous. See also pp6,12,15.||||||19-DEC-06
20268|Winton Formation|34485|5|Briefly described|Table 1|||Lower - Upper? Cretaceous.||||||19-DEC-06
20268|Winton Formation|34486|5|Briefly described|Table 1|||Lower - Upper? Cretaceous. See also Table 2||||||
20268|Winton Formation|34487|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
20268|Winton Formation|34543|6|Mentioned|p98|||||||||
20268|Winton Formation|34611|4|Described|p158|||Cretaceous. See Fig.65,66||||||
20268|Winton Formation|34909|6|Mentioned|p992|||||||||
20268|Winton Formation|34948|6|Mentioned|Fig. 70|||||||||
20268|Winton Formation|35067|6|Mentioned|Fig.4|||||||||
20268|Winton Formation|35139|6|Mentioned|p17|||||||||
20268|Winton Formation|35151|6|Mentioned|p147|||||||||
20268|Winton Formation|35239|6|Mentioned|p258|||||||||
20268|Winton Formation|35560|6|Mentioned|Fig.3|||||||||
20268|Winton Formation|35793|4|Described|p241|||Details of weathering and profiles.||||||
20268|Winton Formation|35811|5|Briefly described|Table 3|||||||||
20268|Winton Formation|35894|6|Mentioned|p275|||||||||
20268|Winton Formation|36172|6|Mentioned|Appendix|||||||||
20268|Winton Formation|36213|6|Mentioned|Fig.2|||||||||
20268|Winton Formation|36229|6|Mentioned|Map legend|Eocene|Eocene|||||||
20268|Winton Formation|36243|6|Mentioned|Table 6A|||||||||
20268|Winton Formation|36327|6|Mentioned|p7|||||||||
20268|Winton Formation|36571|6|Mentioned|p98|||See also Table 4.||||||
20268|Winton Formation|36912|6|Mentioned|Fig.3|||||||||
20268|Winton Formation|36922|6|Mentioned|Fig.3|||||||||
20268|Winton Formation|37065|5|Briefly described|p41|||||||||
20268|Winton Formation|37114|6|Mentioned|p308|||||||||
20268|Winton Formation|37116|4|Described|p312|||||||||
20268|Winton Formation|37261|6|Mentioned|p351|||||||||
20268|Winton Formation|37263|6|Mentioned|p319|||||||||
20268|Winton Formation|37287|6|Mentioned|p36|||||||||
20268|Winton Formation|37451|6|Mentioned|Table 2|||||||||
20268|Winton Formation|37603|6|Mentioned|p444|||||||||
20268|Winton Formation|37607|6|Mentioned|p333|||||||||
20268|Winton Formation|37608|3|Fully described|Table 1|||||||||
20268|Winton Formation|37776|6|Mentioned|Fig.2|||||||||
20268|Winton Formation|38068|5|Briefly described|p72|||||||||
20268|Winton Formation|38226|6|Mentioned|p414|||See also Fig.6.||||||
20268|Winton Formation|38373|6|Mentioned|p622|||||||||
20268|Winton Formation|38779|6|Mentioned|p3|||||||||
20268|Winton Formation|38814|6|Mentioned|Table 1|||||||||
20268|Winton Formation|39070|4|Described|p366|||||||||
20268|Winton Formation|39085|6|Mentioned|Fig.2|||||||||
20268|Winton Formation|39211|5|Briefly described|Fig.3, Fig.6|||See also Figs 4,5,7,14,15 etc. Correlation||||||
20268|Winton Formation|39352|6|Mentioned|Map legend|Albian|Aptian|Aptian to Albian||||||
20268|Winton Formation|39445|5|Briefly described|Table 11|||||||||
20268|Winton Formation|39478|6|Mentioned|Table 1|||||||||
20268|Winton Formation|39482|6|Mentioned|Fig.7|||||||||
20268|Winton Formation|39846|6|Mentioned|Fig.2|||||||||
20268|Winton Formation|39847|5|Briefly described|p40|||||||||
20268|Winton Formation|39914|6|Mentioned|p3|||||||||
20268|Winton Formation|39943|6|Mentioned|Table 8A|||||||||
20268|Winton Formation|40003|6|Mentioned|Fig.9   or|||||||||
20268|Winton Formation|40058|6|Mentioned|Fig.1|||||||||
20268|Winton Formation|40121|6|Mentioned|Table 1|||||||||
20268|Winton Formation|40150|6|Mentioned|p77|||||||||
20268|Winton Formation|40199|6|Mentioned|p16|||||||||
20268|Winton Formation|40220|6|Mentioned|p7|||||||||
20268|Winton Formation|40249|6|Mentioned|p41|||||||||
20268|Winton Formation|40322|6|Mentioned|Fig.3|||||||||
20268|Winton Formation|40670|6|Mentioned|Fig.9|||||||||
20268|Winton Formation|40675|6|Mentioned|Table 8A|||||||||
20268|Winton Formation|40681|6|Mentioned|Fig.2|||||||||
20268|Winton Formation|40756|6|Mentioned|Fig.1.2|||||||||
20268|Winton Formation|40757|6|Mentioned|p78|||Now known to be Eyre Formation||||||
20268|Winton Formation|40801|6|Mentioned|p29|||Mention also Fig.21||||||
20268|Winton Formation|40910|6|Mentioned|p15|||See also P17||||||
20268|Winton Formation|40911|6|Mentioned|Map legend|Cenomanian|Albian|Albian-?Cenomanian||||||
20268|Winton Formation|40925|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
20268|Winton Formation|40926|3|Fully described|p18|||||||||
20268|Winton Formation|41057|6|Mentioned|p82|||||||||
20268|Winton Formation|41060|6|Mentioned|p3|||Generalized stratigraphy||||||
20268|Winton Formation|41061|6|Mentioned|p19|||||||||
20268|Winton Formation|41062|6|Mentioned|p35|||||||||
20268|Winton Formation|41063|6|Mentioned|p40|||||||||
20268|Winton Formation|41064|6|Mentioned|p62|||||||||
20268|Winton Formation|41085|6|Mentioned|p90|||||||||
20268|Winton Formation|41086|3|Fully described|p98|||See also Fig.3||||||
20268|Winton Formation|41088|6|Mentioned|p144|||See also Fig.2||||||
20268|Winton Formation|41097|6|Mentioned|Table 1|||||||||
20268|Winton Formation|41098|4|Described|p177|||||||||
20268|Winton Formation|41099|6|Mentioned|Fig.9|||||||||
20268|Winton Formation|41165|5|Briefly described|p363|||See also Fig.15.||||||19-DEC-06
20268|Winton Formation|41174|6|Mentioned|p117|||||||||
20268|Winton Formation|41176|6|Mentioned|p206|||See also P211||||||
20268|Winton Formation|41177|6|Mentioned|p233|||||||||
20268|Winton Formation|41182|5|Briefly described|Fig.2|||||||||
20268|Winton Formation|41183|4|Described|p307|||||||||
20268|Winton Formation|41184|6|Mentioned|p346|||||||||
20268|Winton Formation|41187|6|Mentioned|Fig.2|||||||||
20268|Winton Formation|41198|6|Mentioned|Table 1|||||||||
20268|Winton Formation|41214|6|Mentioned|Fig.3|||||||||
20268|Winton Formation|41216|6|Mentioned|p299|||||||||
20268|Winton Formation|41219|6|Mentioned|p338|||||||||
20268|Winton Formation|41266|6|Mentioned|Fig.3|||||||||
20268|Winton Formation|41523|3|Fully described|p282|||See also p283.||||||19-DEC-06
20268|Winton Formation|41535|6|Mentioned|p369|||||||||
20268|Winton Formation|41707|6|Mentioned|Fig.8|||||||||
20268|Winton Formation|41720|6|Mentioned|p372|||||||||
20268|Winton Formation|41724|5|Briefly described|p383|||||||||
20268|Winton Formation|41950|5|Briefly described|Fig.2 P3|||||||||
20268|Winton Formation|42061|4|Described|Fig,11 P159|||See also Fig.11||||||
20268|Winton Formation|42067|6|Mentioned|Fig.2 P309|||||||||
20268|Winton Formation|42071|6|Mentioned|p117|||||||||
20268|Winton Formation|42084|6|Mentioned|Fig.3 P256|||||||||
20268|Winton Formation|42085|6|Mentioned|Fig.2 P374|||||||||
20268|Winton Formation|42187|6|Mentioned|Fig.5 P322|||||||||
20268|Winton Formation|42293|6|Mentioned|Fig.2 P.18|||||||||
20268|Winton Formation|42346|5|Briefly described|p84|Cretaceous||||||||
20268|Winton Formation|42375|6|Mentioned|p30, p121, p125|Late Cretaceous|Jurassic|Eromanga Basin.||||||
20268|Winton Formation|42395|5|Briefly described|Fig.13 P83|||||||||
20268|Winton Formation|42397|6|Mentioned|Fig.2 P3|||||||||
20268|Winton Formation|42429|5|Briefly described|p155|Cenomanian||||||||
20268|Winton Formation|42447|6|Mentioned|Fig. 1|||||||||
20268|Winton Formation|42496|5|Briefly described|p136, Fig.3 p132|||||||||
20268|Winton Formation|42520|5|Briefly described|p6|||||||||
20268|Winton Formation|42543|5|Briefly described|Fig.4 P6|||||||||
20268|Winton Formation|42645|6|Mentioned|p195|||||||||
20268|Winton Formation|42648|5|Briefly described|Fig.7 P43|||||||||
20268|Winton Formation|42673|5|Briefly described|Fig.2, P184|||||||||
20268|Winton Formation|42746|4|Described|p12|||See also Fig.2, Fig.6||||||
20268|Winton Formation|42749|6|Mentioned|Fig.2 P27|||||||||
20268|Winton Formation|42784|6|Mentioned|p492|||||||||
20268|Winton Formation|42905|5|Briefly described|p20, Fig 5.3|||||||||
20268|Winton Formation|42999|5|Briefly described|Table 2,p90||Late Cretaceous|||||||
20268|Winton Formation|43002|5|Briefly described|Fig.2,p135|||||||||
20268|Winton Formation|43004|5|Briefly described|Table 1,p179|||||||||
20268|Winton Formation|43053|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Fluviolaustrine mudstone and siltstone.||||||25-MAY-05
20268|Winton Formation|43085|5|Briefly described|Fig.3|||||||||
20268|Winton Formation|43105|6|Mentioned|p15|||||||||
20268|Winton Formation|43114|6|Mentioned|Table 2|||||||||
20268|Winton Formation|43122|5|Briefly described|Fig.2.|||||||||
20268|Winton Formation|43252|5|Briefly described|p163|||||||||
20268|Winton Formation|43258|5|Briefly described|Map Legend||Cretaceous|||||||
20268|Winton Formation|43298|5|Briefly described|Map Legend||Cretaceous|||||||
20268|Winton Formation|43344|14|Not recorded|p14|||||||||
20268|Winton Formation|43383|14|Not recorded|p27|||||||||
20268|Winton Formation|43384|14|Not recorded|Map Legend||Cretaceous|||||||
20268|Winton Formation|43390|14|Not recorded|p16|||Part of Rolling Downs Group||||||
20268|Winton Formation|43452|14|Not recorded|Map Legend||Cretaceous|Of the Rolling Downs Group.||||||14-FEB-05
20268|Winton Formation|43459|14|Not recorded|p315|||||||||
20268|Winton Formation|43591|6|Mentioned|p40|||||||||
20268|Winton Formation|43602|6|Mentioned|191|||In Eromanga Basin, Rolling Downs Group||||||
20268|Winton Formation|43628|6|Mentioned|Fig.3|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|43883|14|Not recorded|p18 Fig.4-3|||||||||
20268|Winton Formation|43985|14|Not recorded|7-10,12,Fig.3,Pl.1,2|||||||||
20268|Winton Formation|43995|14|Not recorded|Tb.p9,30,57-8,Fig.3||Late Cretaceous|Fig.15||||||
20268|Winton Formation|44016|14|Not recorded|Map Legend|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|44017|14|Not recorded|Map Legend|||||||||
20268|Winton Formation|44018|14|Not recorded|Map Legend|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|44019|14|Not recorded|Map Legend|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|44020|14|Not recorded|p8,10-11,13-15,Tb.1,|Late Cretaceous|Early Cretaceous|Of Rolling Downs Group. Tb.2,3, Fig.3,||||||
20268|Winton Formation|44031|14|Not recorded|p5,6,8,9||Cretaceous|||||||
20268|Winton Formation|44033|4|Described|map,4,8,9,Tb.1|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|44034|4|Described|Tb.1,p2,4-6,9,10|||||||||
20268|Winton Formation|44040|14|Not recorded|p35|||||||||
20268|Winton Formation|44041|6|Mentioned|p251|||||||||
20268|Winton Formation|44066|14|Not recorded|Map Legend||Cretaceous|||||||
20268|Winton Formation|44067|14|Not recorded|Map Legend|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|44068|14|Not recorded|p17,18|||||||||
20268|Winton Formation|44082|14|Not recorded|p28,30,Tb.p34|||||||||
20268|Winton Formation|44087|14|Not recorded|p4,8-12|||Lacustrine.||||||
20268|Winton Formation|44088|14|Not recorded|Tb.1,opp.p6,7,8,map|||||||||
20268|Winton Formation|44089|4|Described|p3-6,8-10,Tb.1|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|44090|14|Not recorded|Map Legend|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|44091|14|Not recorded|p61||Cretaceous|||||||
20268|Winton Formation|44098|14|Not recorded|p98|||||||||
20268|Winton Formation|44099|14|Not recorded|Map Legend|Late Cretaceous|Early Cretaceous|(Rolling Downs Group)||||||
20268|Winton Formation|44115|14|Not recorded|p17,20|||||||||
20268|Winton Formation|44119|14|Not recorded|Map Legend||Cretaceous|||||||
20268|Winton Formation|44120|14|Not recorded|Map Legend||Cretaceous|||||||
20268|Winton Formation|44121|14|Not recorded|p5-8,10,12||Cretaceous|See also Lexicon.||||||
20268|Winton Formation|44122|2|Defined|p318-324|||||||||
20268|Winton Formation|44133|4|Described|p123, 104 Fig. 9.11|Cretaceous|Cretaceous|Geological Province: Eromanga Basin. Maximum Thickness: ~1200m. Includes part of the now superseded Blanchewater Formation.||||||
20268|Winton Formation|44168|14|Not recorded|Tb.1p5,7,8,10,map|||||||||
20268|Winton Formation|44269|14|Not recorded|p18||Cretaceous|||||||
20268|Winton Formation|44291|14|Not recorded|p5|||||||||
20268|Winton Formation|44310|14|Not recorded|Map Legend||Cretaceous|||||||
20268|Winton Formation|44346|14|Not recorded|p4|||||||||
20268|Winton Formation|44374|14|Not recorded|p12||Cretaceous|Freshwater-final withdrawal of sea from Eromanga Basin.||||||
20268|Winton Formation|44375|14|Not recorded|p313|||||||||
20268|Winton Formation|44405|14|Not recorded|Map Legend|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|44406|14|Not recorded|p3-14|Cenomanian|Albian|||||||
20268|Winton Formation|44407|14|Not recorded|Map Legend|||||||||
20268|Winton Formation|44408|14|Not recorded|p4,8-13,opp.6|||||||||
20268|Winton Formation|44410|14|Not recorded|Map Legend|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|44413|14|Not recorded|p470,474|||||||||
20268|Winton Formation|44414|14|Not recorded|p110-112||Cretaceous|Mudstone, siltstone and characteristic coal seams.||||||
20268|Winton Formation|44415|14|Not recorded|p22|||||||||
20268|Winton Formation|44417|14|Not recorded|p416,417,420|||||||||
20268|Winton Formation|44418|14|Not recorded|Map Legend|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|44509|14|Not recorded|p342-343|||||||||
20268|Winton Formation|44548|14|Not recorded|p456||Cretaceous|||||||
20268|Winton Formation|44573|14|Not recorded|p98|||||||||
20268|Winton Formation|44611|14|Not recorded|p22,24|||||||||
20268|Winton Formation|44634|14|Not recorded|p29|||||||||
20268|Winton Formation|44715|14|Not recorded|Map Legend|||||||||
20268|Winton Formation|44732|14|Not recorded|Pl.1|||Taken from GeolMap QLD 1953.||||||
20268|Winton Formation|44807|14|Not recorded|p10|||||||||
20268|Winton Formation|44819|14|Not recorded|p89,90|||Non-marine sandstone, carbonaceous grey shale and coal. No age given.||||||
20268|Winton Formation|44848|14|Not recorded|p99-101|||||||||
20268|Winton Formation|44852|14|Not recorded|p78||Late Cretaceous|||||||
20268|Winton Formation|44915|14|Not recorded|p18,24|||Correlated with upper part of Blanchewater Formation in South Australia. Age not given.||||||
20268|Winton Formation|44998|14|Not recorded|p.169|||||||||
20268|Winton Formation|45004|14|Not recorded|p.8,9|||||||||
20268|Winton Formation|45110|6|Mentioned|Table 18|||||||||
20268|Winton Formation|45168|6|Mentioned|p6|||See also Table 1||||||
20268|Winton Formation|46791|5|Briefly described|p48|||||||||
20268|Winton Formation|46854|6|Mentioned|p241|||||||||
20268|Winton Formation|46911|5|Briefly described|p112|||Analyses of weathered profiles and parent rocks.||||||
20268|Winton Formation|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
20268|Winton Formation|46939|6|Mentioned|Fig.1|||See also Table 1.||||||
20268|Winton Formation|48627|14|Not recorded|p3|||||||||
20268|Winton Formation|48634|4|Described|p5,19,20|||See also Fig.2,6,Pl.1,2. Subsidy report. (G54-14).||||||
20268|Winton Formation|48751|6|Mentioned|p19|||||||||
20268|Winton Formation|48906|14|Not recorded|p5,9,Tb.2,Fig.1,Pl.1|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|48908|14|Not recorded|Tb.1||Late Cretaceous|||||||
20268|Winton Formation|48920|3|Fully described|p62|||Cretaceous age||||||
20268|Winton Formation|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
20268|Winton Formation|49011|6|Mentioned|Fig.3|||In the Eromanga Basin.||||||19-DEC-06
20268|Winton Formation|60080|5|Briefly described|Map legend|Late Cretaceous|Early Cretaceous|Very labile sandstone, siltstone and mudstone; calcareous in part, minor mud clast conglomerate.  Overlain by Glendower Formation.||||||22-JUL-04
20268|Winton Formation|60281|6|Mentioned|p11|||||||||
20268|Winton Formation|60331|5|Briefly described|p34 Fig.3||Cenomanian|Overlies Mackunda Formation. Geological Province: Eromanga Basin||||||
20268|Winton Formation|60717|5|Briefly described|p40 Fig. 2|Late Cretaceous|Late Cretaceous|Overlies Oodnadatta Formation and Mackunda Formation. Geological Province: Eromanga Basin. Non-marine to marginal marine deposits.||||||31-JAN-08
20268|Winton Formation|60726|6|Mentioned|p2 Fig.1, p6.|Late Cretaceous|Late Cretaceous|Winton area, Great Artesian Basin.||||||
20268|Winton Formation|60953|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Fluviolacustrine mudstone and siltstone.||||||
20268|Winton Formation|61108|5|Briefly described|map legend|Cretaceous|Cretaceous|Fluviolacustraine mudstone and siltstone.||||||
20268|Winton Formation|61312|5|Briefly described|p75, p79 Table E2|Cretaceous|Cretaceous|Of the Rolling Downs Group. Consists of interbedded mudstone and lithic and feldspathic sandstone deposited in terrestrial environments. Geological Province: Eromanga Basin (absent in NSW). See also p64, p67 Fig. E5.||||||19-DEC-06
20268|Winton Formation|61611|6|Mentioned|p265 Fig. 3|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||13-MAR-09
20268|Winton Formation|61613|6|Mentioned|p282 Fig. 2|Late Cretaceous|Late Cretaceous|Geological Province: Eromanga Basin.||||||07-FEB-11
20268|Winton Formation|61614|6|Mentioned|p290 Fig. 2|Late Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||17-MAR-09
20268|Winton Formation|61823|5|Briefly described|p118|Cenomanian|Late Albian|Predominantly alluvial deposits.  Geological Province: Eromanga Basin.||||||
20268|Winton Formation|62028|5|Briefly described|p10 Fig. 1|||||||||
20268|Winton Formation|62029|5|Briefly described|p15 Fig. 4|Cretaceous|Cretaceous|||||||
20268|Winton Formation|62046|5|Briefly described|p125 Fig. 2|Cretaceous|Cretaceous|Geological Province: Cooper-Eromanga Basins.||||||14-APR-08
20268|Winton Formation|62376|5|Briefly described|p84|Late Cretaceous|Early Cretaceous|Geological Province: Pedirka Basin.||||||09-FEB-10
20268|Winton Formation|62537|6|Mentioned|p191 Fig.2. |Late Cretaceous|Late Cretaceous|Eromanga Basin.||||Overlies Mackunda Formation.||
20268|Winton Formation|62730|5|Briefly described|p352 Fig. 1|Late Cretaceous|Late Cretaceous|Geological Province: Eromanga Basin.||||||21-APR-08
20268|Winton Formation|63979|2|Defined|p54-55, Fig. 44|Cenomanian|Albian|Formerly Winton Series (Dunstan 1916). Forms upper part of Rolling Downs Gp.Conformable on Mackunda Fm; unconformable below Glendower Fm. Max.thick:1000m. Interbedded sands., sandy siltst., siltst., mudst.+ coal with minor intraformational conglomerate.||||||07-FEB-11
20268|Winton Formation|64048|5|Briefly described|p64 Tb. 2|||Source of hydrocarbons - lignite. Geological Province: Eromanga Basin.||||||07-FEB-11
20268|Winton Formation|64197|6|Mentioned|p625 Fig.1c, p627, p630 Figs.6,7|Late Cretaceous|Late Cretaceous|Eromanga Basin. Deeply weathered upper surface.||||Overlies Oodnadatta and Mackunda Formations. Is overlain unconformably by Eyre Formation.||11-DEC-15
20268|Winton Formation|64232|5|Briefly described|p12|Cretaceous|Cretaceous|Geological Province: Eromanga Basin. Coal measures are present in this unit and are a potential target for CSM exploration activities.||||||24-JUL-08
20268|Winton Formation|64665|5|Briefly described|p62.|Cretaceous|Cretaceous|Eromanga Basin. Hosts coal seams up to 7 m thick; low rank lignites of no current (i.e. c.2008) commercial interest.||||||
20268|Winton Formation|64778|6|Mentioned|p13|Cretaceous|Cretaceous|Pedirka and Simpson Desert Basins.||||||
20268|Winton Formation|64856|6|Mentioned|p101|||Eromanga Basin. Younger than lithologically similar Griman Creek Formation in the Surat Basin.|| ||||29-NOV-17
20268|Winton Formation|65238|5|Briefly described|p7 Fig. 8, p10|Early Cretaceous|Early Cretaceous|Geological province: Eromanga Basin. Fluvial deposits.||||||
20268|Winton Formation|65342|5|Briefly described|p9.|||Eromanga Basin. Max. thickness at least 613 m. Seen as having potential as an insulating layer for geothermal energy.||||Overlies Oodnadatta Shale. Is overlain by Eyre Formation.|Sandstone, siltstone, mudstone; minor conglomerate, coal; predominantly alluvial deposits.|
20268|Winton Formation|65376|5|Briefly described|p9 Fig.1.2. |Cretaceous|Cretaceous||||||Marginal marine to fluvial mudstone and siltstone.|
20268|Winton Formation|65385|5|Briefly described|pS134 Fig.7|Late Cretaceous|Early Cretaceous|Of Eromanga Basin. Overlies Mackunda Formation.||||||08-MAR-12
20268|Winton Formation|65489|5|Briefly described|p49, p53, p55, p57-61, p96, p155-156|Late Cretaceous|Late Cretaceous|Eromanga Basin. 1200m thick. Rapid non-marine deposition: c.1100m in c.8 m.y.||||Overlies Mackunda and Oodnadatta Formations. Is locally overlain unconformably by Mount Howie Sandstone.||
20268|Winton Formation|65925|5|Briefly described|p15, Appendix 2.|||Thousand-metre thick package deposited in low-energy fluvial to lacustrine environment.|||||Sandstone, shale, siltstone; coal seams.|
20268|Winton Formation|66131|6|Mentioned|p239|Cenomanian|Cenomanian|||||||
20268|Winton Formation|66529|5|Briefly described|p10, p12 Fig.5 |||Eromanga Basin.||Unit in Rolling Downs Group.||Overlies Mackunda and Normanton Formations.|~1000m thick package of non-marine sandstones, shales and siltstones.|
20268|Winton Formation|66623|3|Fully described|p242, p245, pp256-257, pp266-267.|Cenomanian|Albian|Marks the stratigraphic top of the Rolling Downs Group throughout the Eromanga Basin. Correlates with upper half of Yalpunga Beds. Very poor outcrop; extensive post-deposition erosion reduced thickness from 0 to 1100 m. Fossils include vertebrates, plants, wood and microfossils.||Unit in Rolling Downs Group.||Conformably overlies Allaru Mudstone. Is overlain unconformably by fluvial Paleogene sedimentary rocks of Lake Eyre Basin, and by Cordillo Silcrete capping.|Medium-grained, cross-bedded sandstone with rounded intraclasts of siltstone and mudstone; calcareous labile sandstone, siltstone, carbonaceous and pyritic shale with intraclast conglomerate and minor coal; fresh volcanic detritus in sandstones.|07-JUN-13
20268|Winton Formation|66915|5|Briefly described|p6 Fig.3|Cretaceous|Cretaceous|Eromanga Basin.||||||
20268|Winton Formation|67119|5|Briefly described|Map legend.|Cretaceous|Cretaceous|Non-marine.|||||Shale, siltstone, sandstone; minor coal horizons.|
20268|Winton Formation|67323|5|Briefly described|p86-87, p92, p93 Fig.12.3, p95 Fig.12.5|Cretaceous|Cretaceous|See also GIS attrib tbl, Solid Geology Map. Eromanga/Carpentaria Basins. Oil shale was discovered in two wells (AAP Fermoy 1 and AAP Mayneside 1) in this unit by Australian Aquitaine Petroleum Pty Ltd in 1966. Attention shifted to outcrops in Julia Creek but activity ceased in 1969. Fluvial deposits. Underwent deep chemical weathering during Late Cretaceous to Palaeogene.||||Overlies Mackunda Formation.|Labile sandstone, siltstone, mudstone, minor coal.|
20268|Winton Formation|67402|4|Described|p26 tbl RRM4|Cenomanian|Cenomanian|Eromanga Basin. Maximum thickness of 1000m. Deposited in fluvial and lacustrine environments. Estimated porosity of 10-25% with likely favourable permeability for Carbon dioxide storage. See also p106, p108, p109, p111 fig ERO8, p115 tbl ERO2.||||Overlies the Mackunda Formation.|Interbedded sandstone, sandy siltstone, siltstone, mudstone and coal with minor intraformational conglomerate.|
20268|Winton Formation|67462|5|Briefly described|Map legend.|Late Cretaceous|Late Cretaceous|Eromanga Basin.||||Overlies Oodnadatta Formation.||
20268|Winton Formation|67578|6|Mentioned|p335 Fig.2|Cretaceous|Cretaceous|Lake Eyre region.||||||
20268|Winton Formation|67784|5|Briefly described|p25, p31|Cenomanian|Albian|Northern Eromanga Basin. Up to 400m thick. Non-marine deposits.||||Overlies Mackunda Formation||08-FEB-18
20268|Winton Formation|68003|5|Briefly described|p63 Fig.3-p.|Cretaceous|Cretaceous|Surat Basin.||||Overlies Coreena Member.||
20268|Winton Formation|68004|6|Mentioned|p204.|||Hosts opal. Ferruginisation increases toward the basal one-third of the profile.||||||
20268|Winton Formation|68068|5|Briefly described|Map legend|Cenomanian|Cenomanian|Eromanga Basin. Subsurface only. Fluvial to paludal-lacustrine. Fossil wood and leaves, freshwater bivalves, fish and vertebrates.||Unit in Neales River Group.||Conformably and gradationally overlies Mackunda Formation.|Dark grey-brown sandy silt-clay, finely laminated and cross-bedded, weakly bioturbated; basal portions carbonaceous to lignitic: lowest coal often taken as base of unit.|
20268|Winton Formation|68131|5|Briefly described|p2 Fig.1|Cretaceous|Cretaceous|Marginal marine to fluvial sediments. Mapped with Winton Formation as one unit.|||||Mudstone and siltstone.|
20268|Winton Formation|68206|6|Mentioned|p28|Cenomanian|Cenomanian|Great Artesian Basin. Marks a return to non-marine conditions after Barremian-Albian inundation.||||||
20268|Winton Formation|68553|6|Mentioned|Map legend; schematic diagram.|Cretaceous|Cretaceous|Eromanga and Carpentaria Basins.||Unit in Rolling Downs Group.||Conformably overlies Mackunda Formation.||
20268|Winton Formation|68713|5|Briefly described|p22|Cretaceous|Cretaceous|||Of the Neales River Group.||||
20268|Winton Formation|68715|6|Mentioned|p30 Fig.5|Cenomanian|Albian|Eromanga Basin.||||||
20268|Winton Formation|68731|6|Mentioned|pp209-211|||||||||
20268|Winton Formation|68734|5|Briefly described|p218 Fig.2, p218, p221 Fig.3|Cenomanian|Albian|Eromanga Basin (SW and NE). Fluvial to lacustrine. Late Albian maximum age. Opal is typically found in the upper 1-2 m of a claystone layer underlying a sandstone layer.||Of the Rolling Downs Group.|||Volcaniclastic.|18-JAN-22
20268|Winton Formation|68821|4|Described|p292 Fig.1, pp294-302, p307, p308 Fig.10|Cenomanian|Albian|Late Albian Maximum age. Contains ubiquitous disseminated pyrite. Preserved thickness is approximately 1200 m in the centre of the Eyre Basin. Fluvial to fluvial-lacustrine depositional environment.|97 - 93 Ma|Of the Rolling Downs Group.||Unconformably overlain by the Eyre Formation.|Comprises fluvial sandstone and siltstone.|
20268|Winton Formation|68901|5|Briefly described|p7 Fig. ii|||Eromanga Basin.||Rolling Downs Group|||Sandstone, siltstone, mudstone, calcareous in part.|27-SEP-18
20268|Winton Formation|69001|6|Mentioned|p18|Late Cretaceous||||||||
20268|Winton Formation|69019|4|Described|p83 Fig.20,p85,p94 Fig.24,p100-103,p169|Turonian|Cenomanian|Of Whitehouse (1953); formerly Winton Series (Dunstan, 1916). Named after Winton, Qld. Terrestrial deposition. Thickness from 0-150 m. Contains fossils of plants, lungfish teeth and possible dinosaur bone fragments. Of interest to explorers for biogenic coal seam gas.||Unit in Neales River Group.||Overlies Mackunda Formation. Is overlain disconformably by Eyre Formation and locally by Mount Howie Sandstone.|Dark khaki-grey to dark grey-brown, carbonaceous and pyritic mudstone interbedded with pale grey, fine-grained calcareous sandstone, sometimes feldspathic; seams of coal or lignite at/near the base; abundant plant fossils.|
20268|Winton Formation|69023|5|Briefly described|p79, p86-87, p89 Fig.20, p93, p100|Turonian|Cenomanian|See also p105-106, p110, p112, p163, p191-192. Whitehouse (1955); formerly the Winton Series of Dunstan (1916) for freshwater sediments with coal seams in bores around Winton, Qld. Eromanga Basin. Resembles underlying Mackunda Formation. <40m thick. Contains plant, invertebrate and vertebrate fossils. Stratigraphic wells intersection data.||||Conformably overlies Mackunda Formation and Marree Subgroup. Is overlain disconformably by Eyre Formation.|Dark khaki-grey to grey, carbonaceous and pyritic mudstone interbedded with pale grey, fine-grained, calcareous sandstone and coal seams. Typically weathers to yellow or white kaolinitic sandstone.|
20268|Winton Formation|69454|5|Briefly described|p38:3, 13|Late Cretaceous|Late Cretaceous|Eromanga Basin. Deposition of this thick unit initiated hydrocarbon generation in underlying Permian and post-Permian source rocks.||||||12-JUL-16
20268|Winton Formation|69457|3|Fully described|p41:2-6, 9, 11-13, 17|Late Cretaceous|Early Cretaceous|Whitehouse (1955). Uppermost unit in the Eromanga Basin. Formerly part of the superseded Blanchewater Formation, used for the combined undifferentiated Mackunda-Winton Formations interval. Fluviatile to paludal to lacustrine deposits; paralic, estuarine, deltaic and fluviatile near base. Maximum 620m thick in NT; c.1200m in the Patchawarra Trough in SA. Poorly exposed as highly weathered outcrops around dry lakes. Contains abundant micro- and macroflora and macrofauna. Late Albian to early Cenomanian. The seams of brown to black coal are uneconomic. Sediment loading by this thick unit is believed to have triggered hydrocarbon generation.||Manuka Subgroup.||Conformably overlies Mackunda Formation.|Claystone, siltstone and mudstone with interbedded very fine- to medium-bedded sandstone, and minor coal seams usually interbedded with carbonaceous mudstone; local minor intraformational conglomerate. Contains plant fragments and fossil wood.|12-JUL-16
20268|Winton Formation|69555|5|Briefly described|p43-44, p46-48|Turonian|Albian|Comprises the youngest Cretaceous strata of the Eromanga Basin. Fossil flora (palynological and macro) listed and described.||Rolling Downs Group|||Fossiliferous fine- to medium-grained, feldspatholithic or lithofeldspathic arenites, siltstones, mudstones and claystones, with very minor coal seams.|13-FEB-18
20268|Winton Formation|69582|6|Mentioned|p65|Late Cretaceous|Late Cretaceous|Eromanga Basin.||||Overlies the Mackunda Formation.||
20268|Winton Formation|69594|5|Briefly described|p519, p526, p530-532, p563, p574|Cenomanian|Albian|Whitehouse (1955); Gray et al. (2002). Youngest deposits in the Eromanga Basin. Up to 1000m thick. The Mackunda-Winton boundary is difficult to pick. Unweathered outcrop is mainly well-cemented nodular sandstone; weathered outcrop is kaolinitised and ferruginised sandstones, mudstones and siltstone. Paralic, estuarine, deltaic and fluvial deposits in lower part; fluvio-lacustrine higher up. Contains a rich and diverse fossil flora, fauna and ichnofauna (listed and photographs); supports an economically important tourism industry. Detrital zircon plot.|~95 Ma (detrital zircon MDA: Greentree 2011).|||Conformably overlies Mackunda Formation.|Interbedded labile volcanic lithic-crystal sandstone, sandy siltstone, siltstone, mudstone, intraformational conglomerate and coal. Much of the detritus is volcanogenic.|
20268|Winton Formation|69599|5|Briefly described|p599-600|Cretaceous|Cretaceous|||||Is overlain unconformably by Old Cork beds, Moses Sandstone, Edkins and Glendower Formations.||
20268|Winton Formation|69673|4|Described|p155 fig 127|Cretaceous|Cretaceous|Up to 620m thick.||Manuka Subgroup||Overlies Mackunda Formation, overlain by Mount Howie Sandstone Member|Claystone, siltstone and mudstone with interbedded very fine to fine to occasionally medium grained sandstone and minor coal seams.|
20268|Winton Formation|69742|5|Briefly described|p787, 788, 790, 793|Cenomanian|Albian|Great Artesian Basin. Hosts opal. Fluvial volcaniclastics. Geochemistry discussed.|||||Red-brown ironstone dominated by goethite and kaolinite with minor quartz and illite.|
20268|Winton Formation|69751|6|Mentioned|p35-38, 41|Cretaceous|Cretaceous|Eromanga Basin. Freshwater, broad fluvial-lacustrine environment of deposition (at least the upper part). Contains rich fossil assemblages; also silicified wood. Cenomanian-Turonian climate was seasonal and variable, with potential flooding and/or drought.|||||Fine- to medium-grained feldspatholithic or lithofeldspathic arenites, siltstones, mudstones and claystones; very minor coal seams.|
20268|Winton Formation|69797|5|Briefly described|p17 Fig.2|Late Cretaceous|Late Cretaceous|Geol. Prov: Eromanga Basin.||||||
20268|Winton Formation|69946|2|Defined|p27-28, p56-57, p124-125, p129|Late Cretaceous|Late Cretaceous|Eromanga Basin. Originally Winton Series (Dunstan, 1916), without formal definition. Renamed Winton Formation by Whitehouse (1955). His type section is 'blue shales and sandstones with intercalated coal seams met within the bores in and around Winton'. Distinguishing from Mackunda Formation is difficult in SA due to lack of coals, but easier in Qld due to coal seams, intraformational conglomerates and absence of marine fossils. 400-1100m thick. Late Albian - Cenomanian. Freshwater fossils listed. The top has been deeply (>40m) weathered.||||Conformably overlies Mackunda Formation. Is overlain unconformably by Eyre Formation.|Interbedded fine- to coarse-grained sandstone, carbonaceous and pyritic shale, siltstone and coal seams with intraclast conglomerates. Sandstone beds contain abundant fresh volcanogenic debris, lithics and feldspar.|
20268|Winton Formation|69947|5|Briefly described|p3, p9, p13 Fig.7.2|Late Cretaceous|Late Cretaceous|The final deposits in the Eromanga Basin. Is overlain by Tertiary sediments of the Lake Eyre Basin. On p9 the authors state: "the fluviolacustrine Winton Formation of the upper Marree Subgroup", which contradicts what appears in Fig.7.2.||||||
20268|Winton Formation|69948|6|Mentioned|p6; Figs.4.1, 18|||Eromanga Basin. Surface exposures of this and older units define the Birdsville Track Ridge.||||Overlies Mackunda Formation.||
20268|Winton Formation|69952|5|Briefly described|p16|Cretaceous|Cretaceous|Eromanga Basin.||Unit in Rolling Downs Group.|||Sandstone, siltstone, mudstone; calcareous in part.|
20268|Winton Formation|70383|5|Briefly described|p45|Cretaceous|Cretaceous|Eromanga Basin. Non-marine deposits.||||||
20268|Winton Formation|70649|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||Rolling Downs Group|||Non-marine mudstone and siltstone with subordinate interbedded coarse lithic and feldspathic labile sandstone.|18-JAN-22
20268|Winton Formation|70720|6|Mentioned|p6|||Eromanga Basin.||||Overlies Coreena Member. Is overlain by Glendower Formation.||
20268|Winton Formation|70789|5|Briefly described|p318, p320 Fig.4|Cenomanian|Cenomanian|Eromanga Basin.|c.93 Ma.||||Marine mudstones, siltstones and shales.|
20268|Winton Formation|70821|4|Described|p21-24, p30-31, p33, p79-80, p82|Late Cretaceous|Late Cretaceous|See also p85-87, p115-116. Youngest Formation in the Eromanga Basin. Much of this unit in the southern Thomson region has been removed by erosion. Crops out as low breakaways, intensely weathered (kaolinitised and ferruginised): the weathering profile can be up to 95m deep. One of the two main groundwater resources in the Great Artesian Basin. Paralic, estuarine, deltaic and fluvial deposits in the lower part; fluvio-lacustrine in the upper. Fossil biota is dominated by fish, crocodiles, dinosaurs and pterosaurs. Late Albian to Cenomanian. Hydrochemistry mentioned; hydrostratigraphic properties.||Rolling Downs Group.||Overlies Mackunda Formation and locally the Wallumbilla Formation (conformably). Is overlain unconformably by Glendower Formation.|Interbedded labile volcanic lithic-crystal sandstone, sandy siltstone, siltstone, mudstone, intraformational conglomerate and coal. Also pyritic black shale. Much of the clastic material is volcanogenic, presumably from volcanic arcs to the E.|
20268|Winton Formation|70823|5|Briefly described|p25-p27, p41, p43-p45, p78|Cenomanian|Cenomanian|Eromanga Basin. Up to 1200m thick. Deposited in a non-marine to marginal marine environment. Hosts lignite source rock. Age range derived from Bryan et al., 2012 and Tucker et al., 2013.|c. 99-93 Ma|||Overlies the Mackunda and Oodnadatta Formations. Overlain by the Mount Howe Sandstone.||
20268|Winton Formation|70824|5|Briefly described|p9|Cretaceous|Cretaceous|Eromanga Basin. Hosts lignite.||||Overlies the Mackunda Formation.||
20268|Winton Formation|70836|6|Mentioned|p474, 482|Turonian|Albian|Eromanga Basin. Preserves a rich and diverse vertebrate fauna including the only named Australian megaraptoran, Australovenator.|c.103-92 Ma (Tucker et al., 2013).|||||
20268|Winton Formation|70938|5|Briefly described|p816|Late Cretaceous|Late Cretaceous|Extensive, fluvial deposits. Paleocurrents and detrital zircons indicate a NE Queensland source.|||||Contains extensive labile volcanic detritus.|
20268|Winton Formation|71251|4|Described|p8, p11-13, p15, p17-20, p29, p49|||Senior (1971). Eromanga Basin. 47m total thickness in Eulo 1 borehole. Non-marine deposits. Natural gamma, magnetic susceptibility data tabulated. Conductivity data/diagram.||||Overlies Coreena Member (Wallumbilla Formation).|Dark grey siltstone, weathering to white, finely-bedded mudstone and claystone mottled by goethite and hematite, with gypsum prevalent throughout the top of the unit; capped by a 5m-thick duricrust of porcellanite (white silicified mudstone).|
20268|Winton Formation|71321|5|Briefly described|p15,65|Cenomanian|Cenomanian|Of Eromanga Basin. Regressivee depositional package following peak early Cretaceous marine transgression; fluvio-lacustrine siltstone and sandstones and locally coal-bearing.||||Overlain by Mount Howie Formation. Underlain by Mackunda Formation.|Fluvio-lacustrine siltstone and sandstones and locally coal-bearing.|
20268|Winton Formation|71342|3|Fully described|Ch 1 p6, Ch 1 p19, Ch3 p4, Ch4 p6|Cenomanian|Albian|Eromanga Basin. Originally termed the Winton Series by Dunstan (1916) without formal definition. The name was changed to Winton Formation and a type section was designated in Queensland by Whitehouse (1955). The type section is described as "blue shales and sandstones with intercalated coal seams met within the bores in and around Winton". Hosts a major confined aquifer. Lithology, sedimentology, distribution and outcrop characteristics are discussed. This unit is generally thicker than 400m in the Cooper region and has a maximum thickness of 1100m in the northern Patchawarra Trough. Age derived on the basis of palynology and macrofossil assemblage. Spore-pollen zone is given in Ch5 p57. See also Ch4 p8, Ch4 p25, Ch5 p27-p28, Ch5 p30, Ch5 p33, Ch5 p56-p57, Ch5 p126-p127, Ch5 p130, Ch6 p9-p10, Ch7 p3, Ch7 p9, Ch7 p13, Ch9 p4-p5, Ch9 p10-p11, Ch9 p18, Ch10 p3.||||Conformably overlies the Mackunda Formation. Overlies the Oodnadatta Formation. Unconformably overlain by the Eyre Formation.|Interbedded fine to coarse-grained sandstone, carbonaceous and pyritic shale, siltstone and coal seams with intraclast conglomerates.|
20268|Winton Formation|71601|6|Mentioned|p120, p121|Turonian|Albian|Central west Qld. Ankylosaurian remains have been identified.||||||
20268|Winton Formation|71855|6|Mentioned|p20, p27, p30|||||||||
20268|Winton Formation|71863|5|Briefly described|p5|Cenomanian|Albian|Eromanga Basin.||||Overlies the Allaru Mudstone and the Mackunda Formation.||
20268|Winton Formation|71864|4|Described|p8, p10, p13-p14, p16-p20, p26|||Intersected in GSQ Eulo 2 borehole between 2-23m depth. Originally mapped in the area by Senior (1971). Described in Senior, 1971 as non-marine fine sandstone and siltstone. Gamma log characteristics and magnetic susceptibility is provided.||||Overlies the Wallumbilla Formation.|Mottled, deeply weathered mudstone regolith with gypsum flakes throughout, blue siltstone and thin quartzose and lithic gravel bands.|
20268|Winton Formation|72297|5|Briefly described|p700, p724, p751, p758|Cretaceous|Cretaceous|Eromanga Basin. All coal seams are of uneconomic thickness and of poor quality. CSG exploration results not encouraging. Has a large kaolin deposit 35km W of Winton (70-80% kaolinite). Hosts QLD's opal fields within a 300km wide, NNW-trending belt from Hungerford to Kyuna.|||||White mudstone. Contains seams of subhydrous lignite - sub-bituminous black coal.|
20268|Winton Formation|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin. Confined aquifers, generally producing non-flowing artesian water bores.||Rolling Downs Group.||Overlies Rumbalara Shale, Mackunda FZ.||
20268|Winton Formation|72456|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marree 1:250k map sheet.|||||Shale, siltstone, sandstone that is non-marine with minor coal horizons.|
20268|Winton Formation|72915|6|Mentioned|p16|||Absent in the area of the Congararra 1 borehole (after Hawke and Cramsie, 1984).||||||
20268|Winton Formation|73106|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||||Shale, siltstone, sandstone. Non-marine, minor coal horizons.|
20268|Winton Formation|73167|6|Mentioned|p664 Fig. 2|Cretaceous|Cretaceous|Eromanga Basin.||||||
20268|Winton Formation|73249|6|Mentioned|p319|Cretaceous|Cretaceous|Eromanga Basin.||||Overlies the Mackunda Formation.||
20268|Winton Formation|73251|6|Mentioned|p62|Late Cretaceous|Late Cretaceous|Eromanga Basin. Non-marine to marginal marine.||||Underlain by Mackunda Formation and Oodnadatta Formation.||
20268|Winton Formation|73281|6|Mentioned|Appendix (DIP)|||See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
20268|Winton Formation|73343|6|Mentioned|p337|Cretaceous|Cretaceous|Eromanga Basin.||||Underlain by Oodnadatta Formation. Equivalent to Mackunda Formation.||
20268|Winton Formation|73393|6|Mentioned|p20||||||||Includes volcaniclastic sedimentary deposits.|
20268|Winton Formation|73479|5|Briefly described|p155, p156 Fig.2, p159-160|Cretaceous|Cretaceous|Eromanga Basin. Fluvial-lacustrine depositional environment. Significantly eroded following exhumation (late Cretaceous).|ca 97-93 Ma|||Overlies Oodnadatta Formation, unconformably underlies Eyre Formation||
20288|Wire Creek Sandstone|22479|5|Briefly described|fig4, pg10|Statherian|Statherian|||||||
20288|Wire Creek Sandstone|22673|6|Mentioned|64|||Geological  province: Mount Isa Basin.||||||19-DEC-06
20288|Wire Creek Sandstone|23065|6|Mentioned|11|Proterozoic|Proterozoic|Geological  province: Lawn Hill Subprovince. Overlain by Peters Creek Volcanics.||||||19-DEC-06
20288|Wire Creek Sandstone|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20288|Wire Creek Sandstone|23395|5|Briefly described|p389|||||||||
20288|Wire Creek Sandstone|23396|5|Briefly described|p407 Fig.2|||||||||
20288|Wire Creek Sandstone|24419|5|Briefly described|p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: Lawn Hill Subprovince (north).||||||07-NOV-08
20288|Wire Creek Sandstone|31421|6|Mentioned|p509|||||||||
20288|Wire Creek Sandstone|35640|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
20288|Wire Creek Sandstone|36012|3|Fully described|Table 3|||See also p11, 16.||||||19-DEC-06
20288|Wire Creek Sandstone|36439|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
20288|Wire Creek Sandstone|36442|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
20288|Wire Creek Sandstone|37568|6|Mentioned|Fig.5|||||||||
20288|Wire Creek Sandstone|38237|6|Mentioned|Fig.3|||||||||
20288|Wire Creek Sandstone|38584|4|Described|p15|||||||||
20288|Wire Creek Sandstone|39445|5|Briefly described|Table 2|||See also p39.||||||19-DEC-06
20288|Wire Creek Sandstone|39497|6|Mentioned|p7|||See also Fig.4||||||
20288|Wire Creek Sandstone|39685|6|Mentioned|p407|||||||||
20288|Wire Creek Sandstone|39925|6|Mentioned|p334|||||||||
20288|Wire Creek Sandstone|40840|6|Mentioned|Map legend|||||||||
20288|Wire Creek Sandstone|41319|6|Mentioned|Fig.1|||||||||
20288|Wire Creek Sandstone|41721|4|Described|p27|||Conformably overlain by Peters Creek Volcanics.Thickness: <70m. Medium to coarse sandstone with scattered pebbles, mostly quartz and volcanics; lenticular conglomeratic beds + clasts up to 30cm are common. Part of the Lawn Hill Platform sequence.||||||02-AUG-07
20288|Wire Creek Sandstone|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
20288|Wire Creek Sandstone|42812|6|Mentioned|p10|||||||||
20288|Wire Creek Sandstone|43010|5|Briefly described|Fig.6||Mesoproterozoic|Of "Mid Proterozoic" age.||||||19-DEC-06
20288|Wire Creek Sandstone|45166|6|Mentioned|p14|||||||||
20288|Wire Creek Sandstone|46804|6|Mentioned|p154|||||||||
20288|Wire Creek Sandstone|49001|2|Defined|p5|Carpentarian|Carpentarian|||||||
20288|Wire Creek Sandstone|63113|6|Mentioned|p1214 Fig.2.|||Southern Murphy Inlier, Lawn Hill platform, Leichhardt Superbasin. Written as Wire Cr Sst||||Correlated with Bottle Tree Formation and Mount Guide Quartzite. Is overlain by Buddawadda Basalt.||
20288|Wire Creek Sandstone|63866|5|Briefly described|p56|||Crops out on the southern flank of the Murphy Inlier.||||Equivalent to the Guide Supersequence.||
20288|Wire Creek Sandstone|64724|5|Briefly described|p46|Statherian|Statherian|Unit of the Leichhardt Superbasin (South Nicholson Basin), deposited during the Leichhardt Extension (1800-1750 Ma)||||||
20288|Wire Creek Sandstone|65228|6|Mentioned|Fig.07.|||Southern McArthur Basin.||||Is overlain by Peters Creek Volcanics.||
20288|Wire Creek Sandstone|67323|4|Described|GIS attrib tbl, Solid Geology Map, p9|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Lawn Hill Platform, Leichhardt Superbasin. Camooweal-Murphy Domain, Mount Isa Inlier.|1847 +/- 13 Ma (maximum depositional age).|Tawallah Group.||Correlated with Westmoreland Conglomerate and Mount Guide Quartzite.|Coarse gritty sandstone with scattered quartz pebbles; cobble and boulder conglomerate lenses|
20288|Wire Creek Sandstone|69383|4|Described|p49-52|Paleoproterozoic|Paleoproterozoic|McArthur Basin, base Lawn Hill Platform. Up to 70 m thick. LA-ICPMS U-Pb geochronology analyses.  Max deposition age.|1847+/-13 Ma|||Unconformable on Murphy Inlier basement. Stratigraphic equivalent to Westmoreland Conglomerate.|Medium- to coarse-grained cross-bedded sandstone with scattered pebbles mostly of quartz and volcanics, deposited in braided river and alluvial fan environments.|
20288|Wire Creek Sandstone|69423|6|Mentioned|p8:4 Fig.8.7|Paleoproterozoic|Paleoproterozoic|Lawn Hill Platform.||||||12-JUL-16
20288|Wire Creek Sandstone|69433|4|Described|p18:1-4|Statherian|Orosirian|Sweet (1981). Northern succession, Lawn Hill Platform. Unconformably overlies igneous and metamorphic rocks of the Murphy Inlier. Up to 70m thick. Fluvial braided river and alluvial fan deposits. Detrital zircon age. Correlated with Westmoreland Conglomerate of the Tawallah Group (McArthur Basin), and possibly with Don Creek Sandstone.|<1847 +/- 13 Ma (maximum deposition age).|||Unconformably overlies the Nicholson Granite Complex and Cliffdale Volcanics. Is overlain, probably conformably, by Peters Creek Volcanics.|Commonly cross-bedded, medium to coarse sandstone with scattered pebbles, mostly of vein quartz and volcanic rocks. Lenticular conglomerate beds with clasts to 30cm are common. Basal conglomerate bed is often developed.|12-JUL-16
20288|Wire Creek Sandstone|69591|5|Briefly described|p33-34, p58|||Camooweal-Murphy Domain, Leichhardt Superbasin. Fluvial deposits.|1847 +/- 13 Ma (MDA: Carson et al., 2011).|||Correlated with Westmoreland Conglomerate.|Coarse gritty sandstone with scattered quartz pebbles; cobble and boulder conglomerate lenses.|
20288|Wire Creek Sandstone|69673|5|Briefly described|p51|||Considered to be equivalent to the Tawallah Group of the McArthur Basin. Up to 70m thick.||||Unconformably overlain by Fickling Group|Sandstone with scattered pebbles, mostly of vein quartz and volcanic rocks.|
20288|Wire Creek Sandstone|70849|5|Briefly described|Map legend.|Statherian|Statherian|Lawn Hill Platform.||Tawallah Group.||Unconformably overlies Murphy Metamorphics. Is overlain by Peters Creek Volcanics.|Sandstone with scattered quartz pebbles, medium- to coarse-grained, cobble and boulder conglomerate lenses.|
20288|Wire Creek Sandstone|71592|5|Briefly described|Appendix A.|||McArthur Basin.|1847+/-13 Ma (MDA: U-Pb zircon LA-ICPMS).||||Cross-bedded sandstone.|
20288|Wire Creek Sandstone|71606|5|Briefly described|p137|Statherian|Statherian|South Nicholson Basin.||||Overlain by Peters Creek Volcanics. Underlain unconformably by Murphy Metamorphics.||
20288|Wire Creek Sandstone|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Lawn Hill Platform. Grouped with lower part of Peters Creek Volcanics on this map.||Lower Peters Creek Volcanics.||||05-MAR-20
20288|Wire Creek Sandstone|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as being located in the west of the South Nicholson Basin.||||Shown as unconformably overlying Nicholson Granite Complex and underlies Peters Creek Volcanics.||
20288|Wire Creek Sandstone|72527|4|Described|p7, p9, p176-180, p193, p194.|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin. Previous dating gave 1847+/-13 Ma from site 20 km further east. Depositional age bracketed  by underling and overlying units to 1845-1725 Ma range. Type locality in Hedleys Creek 1:100k area, Qld. Maximum thickness 70 m in Qld. Sample is of feldspathic coarse sandstone. Braided stream and/or alluvial fan depositional environment. Ages derived for this unit are similar to Westmoreland Conglomerate.|1854+/-4 Ma max.dep.age, Pb/Pb SHRIMP.|Tawallah Group||Equivalent to Westmoreland Conglomerate. Unconformably underlies Carrara Range Group and Peters Creek Volcanics and unconformably overlies Murphy Metamorphics and Nicholson Granite.|Coarse-grained, gritty quartz sandstone, occasionally cross-bedded, with pebble lags and local cobble to boulder conglomerate lenses, containing rounded clasts of predominantly white vein quartz, quartzite, felsic volcanics and rarely, granite.|
20288|Wire Creek Sandstone|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the west part of the South Nicholson Basin||||Unconformably overlies Nicholson Granite Complex and underlies Peters Creek Volcanics.||
20288|Wire Creek Sandstone|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin region. Age range indicated to be quite uncertain, with ? above and below.||||||
20312|Wiso gravel|31429|5|Briefly described|p2|||Mine fill properties. See p3-22.||||||19-DEC-06
20318|Withillindarmna Dolostone Member|8187|5|Briefly described|Map legend|Ordovician|Ordovician|Sandy dolostone.||||||
20318|Withillindarmna Dolostone Member|40136|6|Mentioned|p29|||||||||
20318|Withillindarmna Dolostone Member|60122|5|Briefly described|p29|||Not mapped as such in this study - although it is used on the Second Edition map sheet. This dolomitic upper portion of the Kelly Creek Fm in the Toko Range region was named by Radke and Duff (1980) and mapped as a distinct unit by Simpson et al (1979)||||||
20318|Withillindarmna Dolostone Member|64068|6|Mentioned|p75, 226|||Of Radke and Duff (1980). Upper portion in Toko Range. Now Kelly Creek Formation.||||||
20353|Wolfram Hill Granite|24197|5|Briefly described|p106 Tb. 15.1|Paleoproterozoic|Paleoproterozoic|Of the Cullen Supersuite. Age: ~1825Ma. Geological Province: Pine Creek Inlier.||||||07-FEB-11
20353|Wolfram Hill Granite|32660|5|Briefly described|Table 2|||||||||
20353|Wolfram Hill Granite|35061|6|Mentioned|p143|||||||||
20353|Wolfram Hill Granite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20353|Wolfram Hill Granite|40823|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20353|Wolfram Hill Granite|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20353|Wolfram Hill Granite|42756|6|Mentioned|Fig.5 P6|||||||||
20353|Wolfram Hill Granite|43140|4|Described|p61||Paleoproterozoic|Of Cullen Batholith.||||||07-NOV-08
20353|Wolfram Hill Granite|43624|6|Mentioned|p14|||||||||
20353|Wolfram Hill Granite|43832|4|Described|Table8p37;46,Tb12p61||Paleoproterozoic|||||||07-NOV-08
20353|Wolfram Hill Granite|44399|5|Briefly described|map legend||Paleoproterozoic|Biotite granite.||||||07-NOV-08
20353|Wolfram Hill Granite|45022|3|Fully described|p.136.||Carpentarian|On many pages.||||||
20353|Wolfram Hill Granite|46678|6|Mentioned|p9|||Mount Evelyn, N.T., Sheet D.53/5. BMR 1:250,000 Geol.Ser.Explan.Notes. Apophyis of Cullen Granite.||||||
20353|Wolfram Hill Granite|48867|14|Not recorded|p.19|||Probably represents a cupola rising from the underlying Cullen Granite batholith.||||||
20353|Wolfram Hill Granite|50586|5|Briefly described|p1.1, 4.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Of the Cullen Supersuite.||||||07-NOV-08
20353|Wolfram Hill Granite|60680|5|Briefly described|Map legend|Orosirian|Orosirian|Of the Cullen Supersuite.  Pink medium to coarse equigranular biotite leucogranite.   Age: 1810-1800Ma.||||||13-JAN-05
20353|Wolfram Hill Granite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1820-1850Ma. Of Cullen Supersuite. I-type. Grey, fine, equigranular leucogranite; Pink medium to coarse equigranular biotite leucogranite. Intrudes Finniss River Group.||||||07-JAN-09
20353|Wolfram Hill Granite|67564|3|Fully described|p7 Table 2, p24, p33 Fig.19, p36, p77.|Paleoproterozoic|Paleoproterozoic|I-type. 16 km2 pluton within Cullen Batholith, Pine Creek Orogen. Fault-controlled greisen zones, pegmatite and quartz veins are common; associated tungsten, tin and copper mineralisation has been exploited on a small scale, e.g. Wolfram Hill W-Cu mine.|1811 - 1800 Ma.|Unit in Cullen Supersuite.||Intrudes and contact metamorphoses Tollis Formation.|Pink, medium to coarse equigranular biotite leucogranite; grey, fine, equigranular leucogranite.|
20353|Wolfram Hill Granite|69420|5|Briefly described|p5:17-19, 109|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Leucogranite-dominated plutons; mineralogy and petrology/geochemistry summarised. Sn and W are present in greisens associated with this unit.||Tennysons Suite.|||Coarse-grained porphyritic quartz monzonite. I-type.|12-JUL-16
20358|Wollogorang Formation|22432|4|Described|p20-22, Fig.22|Statherian|Statherian|U-Pb SHRIMP ages 1730 +/- 3Ma , 1723 +/-4Ma.||||||19-DEC-06
20358|Wollogorang Formation|22457|5|Briefly described|P31|Statherian||Age of lower unit is 1730 Ma.||||||19-DEC-06
20358|Wollogorang Formation|22538|6|Mentioned|App1 P722|||||||||
20358|Wollogorang Formation|22644|5|Briefly described|5 fig 2|||Geological  province: McArthur Basin. ?Of the Murphy Metamorphics. Overlain by Gold Creek Volcanics.||||||19-DEC-06
20358|Wollogorang Formation|22670|6|Mentioned|52, fig 1,53,55|||Geological province: McArthur Basin. Of the Tawallah Group. Formation written as 'Fmt' in text||||||19-DEC-06
20358|Wollogorang Formation|22853|3|Fully described|13|Proterozoic|Proterozoic|Geological province: McArthur Basin. Of the Tawallah Group. Max thickness 150 m. Underlain by Settlement Creek Volcanics||||||19-DEC-06
20358|Wollogorang Formation|23065|5|Briefly described|16|||Of the Tawallah Group.||||||19-DEC-06
20358|Wollogorang Formation|23363|5|Briefly described|352 Tab.3|Statherian|Statherian|Age: 1730+/-3Ma.||||||19-DEC-06
20358|Wollogorang Formation|23395|5|Briefly described|p389|||||||||
20358|Wollogorang Formation|23396|5|Briefly described|p407 Fig.2|Statherian|Statherian|Of the Tawallah Group. Age: 1723+/-4Ma.||||||19-DEC-06
20358|Wollogorang Formation|23397|5|Briefly described|p480|Statherian|Statherian|||||||
20358|Wollogorang Formation|23398|4|Described|p435|Statherian|Statherian|||||||
20358|Wollogorang Formation|23733|5|Briefly described|p32 Fig. 19|||Of Tawallah Group.  Geological Province: MacArthur Basin.||||||
20358|Wollogorang Formation|23776|5|Briefly described|p705 Fig 2|||Of Tawallah Group.||||||
20358|Wollogorang Formation|23867|5|Briefly described|Fig. 30|||Of Tawallah Group.  Correlates with McCaw Formation (Katherine River Group).  Geological Province: McArthur Basin.||||||
20358|Wollogorang Formation|23910|5|Briefly described|p292 Fig. 3|||Of Tawallah Group.  Geological Province: McArthur Basin.||||||
20358|Wollogorang Formation|23963|5|Briefly described|p1238, 1239 Fig.2|||Geological Province: McArthur Basin. Of the Tawallah Group. Max. Thickness: 100m. Overlies the Settlement Creek Volcanics||||||
20358|Wollogorang Formation|23968|6|Mentioned|p1362|||Geological Province: McArthur Basin.||||||
20358|Wollogorang Formation|24048|5|Briefly described|p36|||Of the Tawallah Group.||||||19-DEC-06
20358|Wollogorang Formation|24179|4|Described|p82, 83, 84 Fig. 2|||Of the Tawallah Group.  Overlies the Settlement Creek Volcanics.  Overlain by the Gold Creek Volcanics.  Max. Thickness: 150m.  Geological Province:  McArthur Basin.  Age: 1729 +/- 4 and 1730 +/- 3 Ma (U-Pb).||||||19-DEC-06
20358|Wollogorang Formation|24432|5|Briefly described|p565 Fig.2|Statherian|Statherian|Of Upper Tawallah Group. Carbonate. Geological Province: Southern McArthur Basin.||||||
20358|Wollogorang Formation|26310|4|Described|p7, Fig. 2, Table 1|Proterozoic|Proterozoic|Dolomite, chert breccia, siltstone, sandstone. Maximum Thickness: 1000 feet.||||||
20358|Wollogorang Formation|32519|4|Described|Table 1|||||||||
20358|Wollogorang Formation|32660|5|Briefly described|Table 4|||||||||
20358|Wollogorang Formation|32904|6|Mentioned|p89|||||||||
20358|Wollogorang Formation|33214|6|Mentioned|Fig.1|||||||||
20358|Wollogorang Formation|33665|5|Briefly described|p368|||||||||
20358|Wollogorang Formation|35114|6|Mentioned|p203|||||||||
20358|Wollogorang Formation|35640|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
20358|Wollogorang Formation|35776|4|Described|p819|||See also Fig.1 and Table 1.||||||
20358|Wollogorang Formation|36012|3|Fully described|Table 2|||See also p16.||||||19-DEC-06
20358|Wollogorang Formation|37568|5|Briefly described|p78|||See also p75.||||||19-DEC-06
20358|Wollogorang Formation|37569|6|Mentioned|p91|||||||||
20358|Wollogorang Formation|37670|6|Mentioned|p71|||||||||
20358|Wollogorang Formation|38582|6|Mentioned|Fig.3|||||||||
20358|Wollogorang Formation|39210|6|Mentioned|p50|||||||||
20358|Wollogorang Formation|39445|6|Mentioned|p39|||Now Fickling Group.||||||
20358|Wollogorang Formation|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
20358|Wollogorang Formation|40105|6|Mentioned|p317|||||||||
20358|Wollogorang Formation|40109|4|Described|p302|||||||||
20358|Wollogorang Formation|40259|6|Mentioned|Table 1|||||||||
20358|Wollogorang Formation|40691|6|Mentioned|p7|||||||||
20358|Wollogorang Formation|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
20358|Wollogorang Formation|41220|6|Mentioned|Fig.3|||||||||
20358|Wollogorang Formation|41721|3|Fully described|p23|||Of the Tawallah Group. Overlain by Gold Creek Volcanics; overlies Settlement Creek Volcanics. Thickness: 180m. Geological province: McArthur Basin. Dolomite, siltstone and sandstone.||||||01-AUG-07
20358|Wollogorang Formation|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
20358|Wollogorang Formation|42385|4|Described|p13, p8 Fig. 5, p9 Tb. 3|Mesoproterozoic|Mesoproterozoic|Of Tawallah Group. Dark grey weathering, thinly bedded dololutite with rare columnar stromatolites. Parts have been reassigned to Aquarium Fm. and Settlement Creek Volcanics. Max. thick: <150m.||||||18-SEP-07
20358|Wollogorang Formation|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
20358|Wollogorang Formation|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.||Of Tawallah Group.||Not shown in schematic sections.|Dololutite, rare columnar stromatolites; dololutite breccia or shale with evaporaite mineral casts; upper unit of ferruginous sandstone, quartarenite, dolomitic in places. Detailed lithology given.|09-NOV-11
20358|Wollogorang Formation|42639|4|Described|p14, Table 4 p11|||||||||
20358|Wollogorang Formation|42700|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
20358|Wollogorang Formation|42739|5|Briefly described|map legend|Statherian|Statherian|Of the Tawallah Group. Sandstone, mudstone, dololutite.||||||19-OCT-05
20358|Wollogorang Formation|42812|3|Fully described|p23, Table 3|||Of the Tawallah Group.||||||19-DEC-06
20358|Wollogorang Formation|42873|5|Briefly described|p109|||see also Fig.1, p110.||||||19-DEC-06
20358|Wollogorang Formation|43010|5|Briefly described|Fig.6||Mesoproterozoic|Of the Tawallah Group. Of "Mid Proterozoic" age.||||||19-DEC-06
20358|Wollogorang Formation|43036|3|Fully described|p29|||Of the Tawallah Group.||||||19-DEC-06
20358|Wollogorang Formation|44112|6|Mentioned|p43,49|||||||||
20358|Wollogorang Formation|44271|2|Defined|p39,41|||Overlies Peters Creek Volcanics.||||||
20358|Wollogorang Formation|44272|14|Not recorded|Map Legend||Neoproterozoic|||||||
20358|Wollogorang Formation|44274|14|Not recorded|p8|||||||||
20358|Wollogorang Formation|44275|14|Not recorded|Map Legend|||||||||
20358|Wollogorang Formation|44280|2|Defined|p5-6,Tb.1,map||Neoproterozoic|||||||
20358|Wollogorang Formation|44287|14|Not recorded|p.8,18, opp.7|||opp.8. (E53-3).||||||
20358|Wollogorang Formation|44288|14|Not recorded|map legend||Paleoproterozoic|||||||07-NOV-08
20358|Wollogorang Formation|44305|14|Not recorded|p.6,12,13|||(E53-8). opp.6,18.||||||
20358|Wollogorang Formation|44306|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
20358|Wollogorang Formation|44436|5|Briefly described|p.4,7-9,12,opp.7,map|||(E53-4).||||||02-DEC-04
20358|Wollogorang Formation|44437|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Of the Tawallah Group.  Dolomitic siltstone and feldspathic sandstone, algal dolomite, dolarenite; silty and sandy dolomite; nodular dolomitic siltstone.  Conformably overlies Settlement Creek Formation; conformably overlain by Masterton Formation.||||||07-NOV-08
20358|Wollogorang Formation|44459|14|Not recorded|p.7,13, opp.p.6, map|||(E53-2).||||||
20358|Wollogorang Formation|44460|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
20358|Wollogorang Formation|44473|14|Not recorded|p.8, opp. p.7|||(E53-7).||||||
20358|Wollogorang Formation|44474|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
20358|Wollogorang Formation|44530|14|Not recorded|p.4,9, opp.8|||(D53-15).||||||
20358|Wollogorang Formation|44531|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
20358|Wollogorang Formation|44989|2|Defined|p.116-7, p.115-119|||Tb.II, IV. On many pages. Underlies Constance Sandstone [this is wrong]. (E54-5,E53-8).||||||22-FEB-18
20358|Wollogorang Formation|45162|2|Defined|p32|Proterozoic|Proterozoic|tyep section location given.||||||22-FEB-18
20358|Wollogorang Formation|45287|14|Not recorded|p.223,226|||||||||
20358|Wollogorang Formation|46804|6|Mentioned|p154|||||||||
20358|Wollogorang Formation|46915|6|Mentioned| P156|||||||||
20358|Wollogorang Formation|46968|6|Mentioned|Fig.2|||||||||
20358|Wollogorang Formation|47013|6|Mentioned|p333|||||||||
20358|Wollogorang Formation|60483|5|Briefly described|p7 Fig. 5, p29|Paleoproterozoic|Paleoproterozoic|Of the Tawallah Group. Age: 1730+/-3Ma, 1729+/-4Ma. Geological Province: McArthur Basin. Carbonaceous unit.||||||07-NOV-08
20358|Wollogorang Formation|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Tawallah Group. Overlain by Warramana Sandstone and Gold Creek Volcanics, underlain by Settlement Creek Volcanics.||||||
20358|Wollogorang Formation|60574|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Tawallah Group. Overlies the Settlement Creek Dolerite. Overlain by the Gold Creek Volcanics. Mudstone, dolostone, shale, siltstone and variably-dolomitic sandstone.||||||07-NOV-08
20358|Wollogorang Formation|62084|5|Briefly described|p936 Fig.5|||Calvert Superbasin. Shown as Wollogorang Fm.|1730+/-3 Ma U-Pb SHRIMP (after Page et al. 2000)|||||
20358|Wollogorang Formation|63112|6|Mentioned|p1191 Fig.2,p1192,p1194-1198,p1200-1206|||Calvert Superbasin. Ages from volcaniclastic mudstones and tuffs. 100-270 m thick.|1734 +/- 5 Ma (lower) to 1722 +/- 4 Ma (upper).|Unit in Big Supersequence.||Is overlain by Gold Creek Volcanics.|Lower dolostone-mudstone-carbonaceous shale unit; upper coarse-grained sandstone-dominated unit grading into stromatolitic dolostone facies.|
20358|Wollogorang Formation|63866|5|Briefly described|p54|||Two additional depositional ages of 1729 +/- 4 and 1722 +/- 4 Ma are also provided from Page et al., 2000.|1735 +/- 6 Ma (Page et al., 2000)||||Basal shales and carbonate-rich sedimentary rocks that contain green 'tuff' horizons.|
20358|Wollogorang Formation|64726|6|Mentioned|p86 Table 1, p87.||||1730 +/- 3 Ma.|||||
20358|Wollogorang Formation|64815|6|Mentioned|p4 Fig.2, p5 Fig.3|||||Of the Tawallah Group.||||
20358|Wollogorang Formation|64817|6|Mentioned|p353 Fig.4, p355 Fig.5, p367 Tb.2, p369 |Statherian|Statherian||1730 +/- 3 Ma; 1729 +/- 4 Ma; 1723 +/- 4 Ma.|Of the Tawallah Group.|||Carbonate-mudstone +/- sandstone.|
20358|Wollogorang Formation|65228|4|Described|p7, p22, p25, Figs.02, 04-07.|Statherian|Statherian|McArthur Basin. Diagnostic carbonate lithofacies of this unit  also occurs in the McCaw Formation, Katherine River Group [ i.e. they are considered time-equivalents?]. U-Pb SHRIMP ages from tuff beds (Page et al. 2000).|1730 +/- 3 Ma to 1723 +/- 4 Ma.|Unit in Tawallah Group.||Overlies Settlement Creek Volcanics. Is overlain by Gold Creek Volcanics and Warramana Sandstone.|Red mudstone, carbonate, black shale, sandstone.|13-DEC-17
20358|Wollogorang Formation|65232|5|Briefly described|p9|||Of Tawallah Group. Age: 1730-1720 Ma (tuff, OZCRHON). Correlated with upper part of Katherine River Group. Geol. Prov: McArthur Basin.||||||09-FEB-10
20358|Wollogorang Formation|65337|6|Mentioned|p18.|||Southern McArthur Basin. Contains 'beehive stromatolites'.||||||
20358|Wollogorang Formation|65340|3|Fully described|p5, p13 Tb4, pp16-27, p37, pp76-78, p92|||Was in sedimentological continuum with Aquarium Formation prior to intrusion by Settlement Creek Dolerite. Epeiric or marginal marine salina, intertidal, deep anoxic, storm- and wave-influenced shelf, shoreface depositional environments. MSc and related papers published (Jackson 1982, 1985). Hosts copper mineralisation in veins and disseminated in dolostone, at Foelsche River. Proposed as source of reduced hydrocarbon-bearing fluids into overlying Gold Creek Volcanics, causing deposition of siegenite and chalcopyrite.|c.1730 Ma (Jackson et al. 1997).|Unit in Tawallah Group.|Includes Wollogorang Formation - Lower and Wollogorang Formation - Upper.|Nonconformably overlies and is locally intruded by Settlement Creek Dolerite. Is intruded by Packsaddle Microgranite. Is overlain by Gold Creek Volcanics.|Lower red/brown mudstone, dolostone, carbonaceous shale, dolomitic siltstone; upper dolomitic sandstone, dolarenite and stromatolitic dolostone and chert; hornfelsed and brecciated adjacent to Settlement Creek Dolerite and Packsaddle Microgranite.|
20358|Wollogorang Formation|67144|5|Briefly described|Map legend.|Statherian|Statherian|Recessive.||Unit in Tawallah Group.||Overlies Settlement Creek Volcanics. Is overlain by Gold Creek Volcanics.|Thinly-bedded dololutite, pyritic with ovoid nodules, rare columnar stromatolites; local basal dololutite breccia or shale with evaporite mineral casts; upper unit of ferruginous, cross-bedded sandstone and white quartz arenite, locally dolomitic.|
20358|Wollogorang Formation|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map, p33|Paleoproterozoic|Paleoproterozoic|See also Eastern Australia Time-Space Plot. McArthur Basin, Calvert Superbasin.|1729 +/- 4 Ma to 1722 +/- 4 Ma.|Tawallah Group.|||Siltstone, dolomite, lithic and dolomitic sandstone.|
20358|Wollogorang Formation|67352|4|Described|p14 Tb.2|Statherian|Statherian|McArthur Basin. 150 m thick.||Tawallah Group||Overlies (conformably) Wununmantyala Sandstone or Settlement Creek Volcanics. Overlain conformably by Gold Creek Volcanics; unconformably by Masterton Sandstone.|Dolostone; coarse-grained quartz sandstone; thinly bedded to laminated siltstone, shale; minor breccia, conglomerate; basal mudstone, siltstone.|
20358|Wollogorang Formation|69418|4|Described|p3:15|||Hydrocarbon-bearing fluids from this unit have been proposed as an agent in formation of copper deposits in breccia pipes in the Redbank field.||||Is overlain by Gold Creek Volcanics.||12-JUL-16
20358|Wollogorang Formation|69430|4|Described|p15:3, 9-12, 44-48, 62|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin. Over 350m thick. Lower part is shallow-marine; upper part is locally reworked fluvial deposits in shoreface and intertidal channels. There is a paraconformity between lower and upper parts. Hosts Cu-bearing breccia pipes (described in some detail). Fair to good conventional hydrocarbon reservoirs occur.|1730 +/- 3 Ma; 1723 +/- 4 Ma.|Tawallah Group.||Overlies, and is also intruded at higher levels by, Settlement Creek Dolerite. Is overlain conformably by Warramana Sandstone and Gold Creek Volcanics. Is intruded by Packsaddle Microgranite.|Mudstone, dolostone, carbonaceous shale, dolomitic siltstone, dolomitic sandstone, dolarenite and stromatolitic dolostone and chert, lithic sandstone, evaporitic carbonaceous shale.|12-JUL-16
20358|Wollogorang Formation|69545|5|Briefly described|p99, p103, p105|Paleoproterozoic|Paleoproterozoic|A significant quantity of aromatic hydrocarbons generated in this unit was transported into the overlying Barney Creek Formation by mineralising fluid.||||Is overlain by Barney Creek Formation.||
20358|Wollogorang Formation|69591|5|Briefly described|p38, p56|||Camooweal-Murphy Domain, Mount Isa Province. N of the Murphy Tectonic Ridge. Part of Tawallah Supersequence. Shallow subaqueous deposits. Similar to sedimentary units in the Peters Creek Volcanics.||Tawallah Group.|||Siltstone, dolomite.|
20358|Wollogorang Formation|69673|5|Briefly described|p16 fig 13, p24, p25, p32, p33, p40|||Mixed carbonates and clastic sedimentary rock. Roughly 160m thick. Peperitic contact with Gold Creek Volcanics. Subdivided into dolostone and sandstone units by paraconformity. Some source rock potential.|1730 +/- 3 Ma, 1723 +/- 4 Ma|Tawallah Group||Overlain by Warramana Sandstone, Echo Sandstone, conformably overlain by Gold Creek Volcanics, Overlies Settlement Creek Dolerite|Dolostone, mudstone and sandstone.|
20358|Wollogorang Formation|70849|5|Briefly described|Map legend.|Statherian|Statherian|McArthur Basin.||Tawallah Group.||Overlies Settlement Creek Volcanics. Is overlain by Gold Creek Volcanics.|Two facies mapped separately. Dolomitic sandstone, dolomite, stromatolitic dolomite, oolitic dolomite; dolomitic and quartz sandstone, ferruginous in parts, feldspathic, dolomitic siltstone.|
20358|Wollogorang Formation|71374|6|Mentioned|p6|||McArthur Basin.||Tawallah Group||Unconformably overlain by the Masterton Sandstone.||
20358|Wollogorang Formation|71592|5|Briefly described|Appendix A.|||McArthur Basin.|1729+/-4 Ma (MDA: U-Pb zircon SHRIMP)||||Green ash tuff.|
20358|Wollogorang Formation|72377|5|Briefly described|iii|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. Likely time-equivalent with Dhunganda Formation (c. 1730-1723 Ma).|c. 1730-1723 Ma|Unit of Tawallah Group.||||
20358|Wollogorang Formation|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Urapunga Fault Zone, Beetaloo Sub-basin, Batten Fault Zone and Southeastern McArthur Basin. Three U-Pb zircon sedimentary depositional ages given 1730+/-3 Ma, 1729+/-4 Ma, 1723+/-4 Ma.|1723+/-4 Ma|Tawallah Group||Overlies Settlement Creek Dolorite and underlies Gold Creek Volcanics and Warramana Sandstone.||
20358|Wollogorang Formation|72718|6|Mentioned|p7|Statherian|Statherian|Southern McArthur Basin.|1730+/-3 Ma, 1729+/-4 Ma, 1723+/-4 Ma.|Tawallah Group||Underlain by Settlement Creek Dolerite. Partly overlain by Warramana Sandstone and Gold Creek Volcanics.||
20358|Wollogorang Formation|72912|5|Briefly described|p5 Fig.3, p19, p31 Fig.11, p36.|Statherian|Statherian|Located in the Beetaloo Sub-basin and the Batten Fault Zone in the Southern McArthur Basin.  Hydrocarbon shows known. TOC is discussed in addition to organic richness. Three U-Pb zircon sedimentary depositional ages given 1730+/-3 Ma, 1729+/-4 Ma, 1723+/-4 Ma. See also p37 Fig.14.|1723+/-4 Ma|Tawallah Group||Overlies Settlement Creek Dolorite and underlies Warramana Sandstone and Gold Creek Volcanics.||15-MAR-21
20358|Wollogorang Formation|73042|6|Mentioned|p4, p12|Statherian|Statherian|Southern McArthur Basin, Calvert Superbasin. Southern McArthur Basin, Roper Superbasin. Geochronology is U-Pb zircon sedimentary depositional ages (?maximum depositional age).|1730+/-3 Ma, 1729+/-4 Ma, 1723+/-4 Ma|Tawallah Group||Underlain by Settlement Creek Dolorite. Partly overlain by Gold Creek Volcanics and Warramana Sandstone.||
20358|Wollogorang Formation|73083|6|Mentioned|p39-40|||||||Overlain by Echo Sandstone.||
20358|Wollogorang 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].||||||
20358|Wollogorang Formation|73412|5|Briefly described|p2, 4, 8|||Southern McArthur Basin.|1730-1725 Ma (SHRIMP: Page et al., 2000).|Tawallah Group.||Overlies Settlement Creek Dolerite. Is overlain by Gold Creek Volcanics and Warramana Sandstone.||
20428|Wondoan Hill Formation|14019|5|Briefly described|p4 Fig. 3|||Of the Tijunna Group.  Geological Province: Victoria Basin.||||||
20428|Wondoan Hill Formation|24122|3|Fully described|p8, p5 Tb.1|Proterozoic|Proterozoic|Of Tijunna Group. Conformably overlain by Stubb Formation.  Max. thickness: 108m.  Geological Province: Victoria Basin.||||||19-DEC-06
20428|Wondoan Hill Formation|24297|3|Fully described|p14|Mesoproterozoic|Mesoproterozoic|Of Tijunna Group. Conformably overlain by Stubb Formation, unconformably overlies Bullita Group. Parts of this unit are now mapped as Jasper Gorge Sandstone. Maximum thickness: 145m.  Geological Province: Victoria Basin.  See also p5 Tb. 2.||||||19-DEC-06
20428|Wondoan Hill Formation|24298|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Tijunna Group. Glauconitic quartz sandstone, claystone, siltstone, mudstone.||||||19-DEC-06
20428|Wondoan Hill Formation|24300|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Tijunna Group.   Geological Province: Victoria Basin.||||||19-OCT-12
20428|Wondoan Hill Formation|24441|5|Briefly described|p1 Fig. 1,  Appendix 2-1:2|Mesoproterozoic|Mesoproterozoic|Of the Tijunna Group. Upper part is sandstone; lower is siltstone and mudstone. Unconformably overlies the Banyan Formation and Battle Creek Formation; overlain by Stubb Formation. Thickness: 111m. Geological Province: Victoria Basin.||||||08-AUG-05
20428|Wondoan Hill Formation|24442|5|Briefly described|p50 Fig. 1|||Of the Tijunna Group.  Geological Province: Victoria Basin.||||||
20428|Wondoan Hill Formation|28255|3|Fully described|p58, Tb. 11 (opp. p8)|Adelaidean|Adelaidean|Lower glauconitic sst-sltst sequence, middle claystone and upper sst. Unconformable on Bynoe Fm, Weaner Sst and Battle Creek Fm; on WAVE HILL sheet it  is unconf. on Nero Sltst and Mount Gordon Sst. Unconformable below Stubb Fm and Jasper Gorge Sst. 145m.||||||15-JUN-05
20428|Wondoan Hill Formation|30003|4|Described|p7, p13|||Of the Bullita Group.  White and purple blocky to flaggy medium-bedded fine quartz sandstone; grey to purple flaggy to fissile thin-bedded to laminated fine siltstone, glauconitic in part. Max. thickness: 120m. Carpentarian or Adelaidean.||||||19-DEC-06
20428|Wondoan Hill Formation|30004|6|Mentioned|Map legend|Proterozoic|Proterozoic|Carpentarian or Adelaidean||||||
20428|Wondoan Hill Formation|32175|5|Briefly described|Map legend|Adelaidean|Adelaidean|Glauconitic quartz sandstone, white claystone and siltstone, brown mudstone.||||||02-DEC-04
20428|Wondoan Hill Formation|32659|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
20428|Wondoan Hill Formation|32660|5|Briefly described|Table 6|||||||||
20428|Wondoan Hill Formation|32728|6|Mentioned|p16|||||||||
20428|Wondoan Hill Formation|32775|5|Briefly described|Map legend|Adelaidean|Carpentarian|Adelaidean or Carpentarian||||||02-DEC-04
20428|Wondoan Hill Formation|33373|3|Fully described|p9|||On Table 2.||||||
20428|Wondoan Hill Formation|33374|6|Mentioned|p8|||See also p12. Strat. table.||||||19-DEC-06
20428|Wondoan Hill Formation|33375|6|Mentioned|p8 Tb. 1, p12|Adelaidean|Adelaidean|Laminated green siltstone and shale; interbeds of glauconitic sandstone.  Unconformably overlies Bynoe Formation (Bullita Group); unconformably overlain by Jasper Gorge Sandstone.||||||27-APR-05
20428|Wondoan Hill Formation|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
20428|Wondoan Hill Formation|33377|5|Briefly described|Table 2|||Stratigraphy.||||||
20428|Wondoan Hill Formation|33378|5|Briefly described|Map legend|Adelaidean|Adelaidean|Green siltstone and shale; interbeds of glauconitic sandstone.||||||27-APR-05
20428|Wondoan Hill Formation|36473|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
20428|Wondoan Hill Formation|37462|4|Described|Table 4.VI|||||||||
20428|Wondoan Hill Formation|38157|6|Mentioned|p284|||||||||
20428|Wondoan Hill Formation|45112|3|Fully described|p29|||See also p30.||||||19-DEC-06
20428|Wondoan Hill Formation|45140|6|Mentioned|p13|||Victoria River region.||||||
20428|Wondoan Hill Formation|48942|2|Defined|p57|Adelaidean|Adelaidean|Strat. section p113. Prob. Adelaidean.||||||19-DEC-06
20428|Wondoan Hill Formation|48943|3|Fully described|p69|||||||||
20428|Wondoan Hill Formation|60672|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Fine quartz sandstone, siltstone. Of Tijunna Group. Geological Province: Victoria Basin.||||||11-JAN-05
20428|Wondoan Hill Formation|60685|3|Fully described|p4 Fig. 3, p1|Mesoproterozoic|Mesoproterozoic|Of the Tijunna Group. Unconformable on Bullita Group; conformable below Stubb Formation; also unconformable below Jasper Gorge Formation. Max. thickness: 145m. Geological Province: Victoria Basin.||||||
20428|Wondoan Hill Formation|65342|6|Mentioned|p11 Fig.13. |||Victoria Basin.||Unit in Tijunna Group.||Unconformably overlies uppermost units of Bullita Group. Is overlain by Stubb Formation.||
20428|Wondoan Hill Formation|67151|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Birindudu Basin.||Unit in Tijunna Group.||Unconformably overlies Bynoe Formation. Is overlain by Jasper Gorge Sandstone.|Siltstone and shale; interbeds of glauconitic sandstone.|
20428|Wondoan Hill Formation|68733|5|Briefly described|p177 Fig.2, p179, p183-186, p191-192|||Previously included in the Victoria Basin by Cutovinos et al. (2002). Now included in the Birrindudu Basin due to a recent subdivision by the NGTS (Dunster and Ahmad 2013). Sm-Nd isotope data tabulated.||Of the Tijunna Group.||Conformably overlain by the Stubb Formation.||06-DEC-17
20428|Wondoan Hill Formation|69432|4|Described|p17:2, 12-13, 15|||Birrindudu Basin. Thins from >140m in the N to <30m in the S. Considerable lateral variation in composition. Where the unit is thin, it is almost all sandstone, with subordinate shale and siltstone only in the lower part. Uplift was probably active prior to or during deposition of this unit. Thick shale may possibly have some potential as petroleum source rock.||Tijunna Group.||Unconformably overlies Banyan Formation (Bullita Group).|Basal cross-bedded sandstone, overlain by a succession of more thinly-bedded sandstone (commonly glauconitic), siltstone, mudstone and black shale. Upper parts contain diagenetic nodules, rare hematite, disseminated pyrite and galena.|12-JUL-16
20428|Wondoan Hill Formation|69673|6|Mentioned|p48 fig 35, p51|||||Tijunna Group||Unconformably overlies Banyan Formation, Battle Creek Formation, overlain by Stubb Formation||
20428|Wondoan Hill Formation|70655|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Birindudu Basin.||Tijunna Group.||Unconformably overlies Bynoe Formation. Is ?unconformably overlain by Jasper Gorge Sandstone.|Siltstone and shale; interbeds of glauconitic sandstone.|21-JAN-22
20428|Wondoan Hill Formation|70850|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Tijunna Group.||Unconformably overlies Bynoe Formation (Bullita Group). Is overlain conformably by Stubb Formation.|Glauconitic quartz sandstone, claystone, siltstone, mudstone.|
20428|Wondoan Hill Formation|70854|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Tijunna Group.||Unconformably overlies Mount Gordon Sandstone (Bullita Group). Unconformably overlain by the Jasper Gorge Sandstone.|Fine quartz sandstone, siltstone.|21-SEP-17
20428|Wondoan Hill Formation|70855|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Tijunna Group.||Unconformably overlies Battle Creek Formation. Is overlain by Stubb Formation.|Glauconitic quartz sandstone, claystone, siltstone, mudstone.|
20428|Wondoan Hill Formation|70968|2|Defined|p115-120, p124, p126-127, p129, p131-132|Mesoproterozoic|Mesoproterozoic|See also p138. Originally included in the former Victoria River Group by Traves (1955), and in the former Coolibah Formation by Laing and Allen (1956). Although recognised as occurring between Bynoe and Stubb Formations, was unassigned  by Sweet et al. (1974). Named after Wondoan Hill near Fitzroy homestead, but the exposures there were subsequently remapped as Jasper Gorge Sandstone. The type locality is at the E end of Fitzroy Range; the section measured by Sweet et al. (1974), 9km due S of Wondoan Hill, is now inaccessible and a new type locality is needed. Lithology well described and very well illustrated. 30-145m thick. Shallow-marine inner shelf to shoreface deposits. Various age determination attempts described. Detrital zircon diagram.|c.1575 Ma (maximum depositional age).|||Unconformably overlies Battle Creek, Bynoe Formations; Weaner, Mount Gordon Sandstones; Nero Siltstone. Is overlain by Stubb Formation conformably, and Jasper Gorge Sandstone unconformably.|Glauconitic and quartz sandstone, glauconitic siltstone, claystone and minor dolomitic siltstone. Shows considerable lateral variation in composition.|
20428|Wondoan Hill Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||sandstone, claystone|
20428|Wondoan Hill Formation|71302|5|Briefly described|p6,72,74||Paleoproterozoic|Of Birindudu Basin. Maximum depositional age: c. 1575 Ma (Carson, 2013; Munson, 2016 and Munson, in prep). Contain small c > 1560-1640 Ma age populations.||Unit of Tijunna Group.||Overlain by Stubb Formation. Underlain by Banyan Formation and Battle Creek Formation.||
20428|Wondoan Hill Formation|71893|4|Described|iii, p2-p3, p7-p8, p68-p71|||Birrindudu Basin. A maximum depositional age of 1575 +/- 16 Ma was derived and isolated younger ages to ca 1452 Ma were also found. A shallow marine shelf to shoreface environment is interpreted. Sedimentary structures provide evidence for energetic shallow marine conditions. Description, sampling location, zircon description, LAICPMS U-Pb and Hf analysis, results and interpretation are provided.||Tijunna Group||Unconformably overlies the Bullita Group. Conformably overlain by the Stubb Formation.|Interbedded glauyconitic and quartz sandstone, siltstone and claystone.|
20428|Wondoan Hill Formation|72718|6|Mentioned|p7|||Birrindudu Basin.||Tijunna Group||Overlain by Stubb Formation.||
20428|Wondoan Hill Formation|73083|6|Mentioned|p45-46|Mesoproterozoic|Mesoproterozoic|Victoria Basin. Weak magnetic response.|||||Siliciclastic.|
20481|Woodbine Group|13354|6|Mentioned|p375 Fig.6.|Tertiary|Late Cretaceous|Comprises Bassett, Grebe, Prion, Cartier, Oliver and Barracouta Formations. Overlies Bathurst Island Group.||107||||28-OCT-14
20481|Woodbine Group|23378|4|Described|p180 Fig.2|Quaternary|Tertiary|of Vulcan Sub-basin.||||||01-MAR-10
20481|Woodbine Group|42056|4|Described|p100|||||||||
20481|Woodbine Group|42066|5|Briefly described|Fig.3 P199|||||||||
20481|Woodbine Group|60634|6|Mentioned|p1168 Fig.3. |Cenozoic|Cenozoic||||Includes Johnson, Grebe, Hibernia, Prion, Oliver and Barracouta Formations.|Overlies Bathurst Island Group.||
20481|Woodbine Group|61550|6|Mentioned|p495 Fig.2. |Cenozoic|Cenozoic||||Includes the Barracouta, Oliver, Prion, Hibernia, Grebe and Johnson Formations.|Overlies Bathurst Island Group.||
20481|Woodbine Group|62508|5|Briefly described|p31|Tertiary|Tertiary|||||||
20481|Woodbine Group|62510|5|Briefly described|p4|Cenozoic|Cenozoic|Geological Province: Money Shoal Basin.||||||
20481|Woodbine Group|63062|4|Described|p9 Fig. 9, p36, p33 Fig. 30|Pleistocene|Miocene|Thickness: <400m in study area, ~800m at Tuatara. Geol.Prov: Arafura/Money Shoal Basins. Coarse, quartzitic sandstones with claystone interbeds, and minor coal and dolomite overlain by calcareous claystone and marl with calcarenite interbeds.||||||07-FEB-11
20481|Woodbine Group|66187|5|Briefly described|p413 Fig.2|Eocene|Oligocene|Mount Ashmore Dome. Includes Oliver, Prion, Hibernia, Grebe and Johnson Formations.||||||
20481|Woodbine Group|69297|6|Mentioned|p283,  p285, p305, p322|Upper Neogene|Upper Neogene|Money Shoal Basin.|||Includes the Bassett Formation, Cartier Formation, Oliver Formation and the Barracouta Shoal Formation.|Unconformably overlies the Bathurst Island Group.|Shallow marine carbonates.|
20481|Woodbine Group|69451|6|Mentioned|p35:3 Fig.35.4;|Cenozoic|Cenozoic|||||||12-JUL-16
20481|Woodbine Group|69452|4|Described|p36:4-5, 8, 15, 22|Holocene|Paleocene|McLennan et al. (1990). Petrel Sub-basin, Bonaparte Basin. Offshore; up to 1300m thick. A depositional hiatus occurred during the Miocene. Marine shelf deposits. The individual Formations have not been differentiated in the SE Bonaparte Basin.|||Johnson, Hibernia, Prion, Cartier, Oliver, Barracouta Shoal, Formations.|Unconformably overlies Bathurst Island Group.|A lower, sandy succession grading upwards into widespread shelf carbonate rocks.|12-JUL-16
20481|Woodbine Group|69456|4|Described|p40:1-2, 4, 6, 8-9, 15 Fig.40.16|Holocene|Miocene|McLennan et al. (1990). Bonaparte Basin. Rocks in the Money Shoal Basin are consistently referred to as "Woodbine Group equivalent" (to the Bonaparte Basin succession). Not yet recognised in onshore areas. Shallow-marine to deltaic depositional environment; alternating fluvial and shallow-marine at top. Generally <400m thick, thickening to the W to >1300m in Lynedoch-1. In the Bonaparte Basin, this Group contains Paleogene units of equivalent age to the Van Diemen Sandstone. Generally undeformed.||||Unconformably overlies offshore Bathurst Island Group and ?Van Diemen Sandstone.|Lower unit of coarse quartzite sandstone with claystone interbeds, minor coal and dolostone; upper unit of calcareous claystone and marl with calcarenite interbeds (drillhole Cobra-1A).|12-JUL-16
20481|Woodbine Group|69458|6|Mentioned|p42:6, 18|Neogene|Paleogene|Bonaparte Basin.||||||12-JUL-16
20481|Woodbine Group|69653|6|Mentioned|p8, 10|Oligocene|Paleocene|Petrel Sub-basin.||||Overlies Wangarlu Formation (Bathurst Island Group).||
20481|Woodbine Group|69673|6|Mentioned|p166 fig 136, p174||||||Includes Johnson Formation, Hibernia Formation, Prion Formation, Oliver Formation, Barracouta Shoal Formation|||
20481|Woodbine Group|70061|5|Briefly described|Petrel Sub-basin; Fig.2|Holocene|Danian|See also Regional geology: Figs.6-7. Sahul: Fig.2, p3. Vulcan: Fig.2, p3. Carbonates form an intraformational seal in Sahul Syncline and Vulcan Sub-basin.|||Johnson, Hibernia, Prion, Oliver and Barracouta Shoal Formations.|Overlies Bathurst Island Group.||12-JUL-16
20481|Woodbine Group|70064|5|Briefly described|Regional Fig. 6. Central: Fig.2|Holocene|Paleocene|See also Northern: Fig.2. Yampi: Fig.2. Browse Basin.|||Johnson, Bassett, Cartier, Oliver and Barracouta Shoal Formations.|Overlies Bathurst Island Group.||12-JUL-16
20481|Woodbine Group|70098|5|Briefly described|p18 Fig.4, p19 Fig.5|Cenozoic|Cenozoic|Money Shoal Basin.||||Overlies Bathurst Island Group.||
20494|Wooden Duck Member|23404|5|Briefly described|p645|||Of Mainoru Formation.||||||
20494|Wooden Duck Member|23937|2|Defined|p96  App. 1|Calymmian|Calymmian|Of the Mainoru Formation. Conformably overlain by Showell Member; conformably overlies the Mountain Valley Limestone Member. Age: >1493+/-4 Ma. Max. thickness: >350m.  Geological Province: McArthur Basin.||||||18-APR-05
20494|Wooden Duck Member|24050|4|Described|p44, p8 Tb. 2|Mesoproterozoic|Mesoproterozoic|Laminated mudstone; laminated siltstone and micaceous galuconitic sandstone; minor limestone.  Of the Mainoru Formation.  Max. thickness: ?70m.||||||20-DEC-06
20494|Wooden Duck Member|24051|5|Briefly described|Map Legend|Calymmian|Calymmian|Of Mainoru Formation (Roper Group). Geological Province: McArthur Basin.||||||20-DEC-06
20494|Wooden Duck Member|40691|6|Mentioned|Fig.4|||||||||
20494|Wooden Duck Member|41268|5|Briefly described|Fig.4|||||||||
20494|Wooden Duck Member|44434|14|Not recorded|p.7, opp. p.6, map|||Member of Mainoru Formation (Roper Group).||||||
20494|Wooden Duck Member|44435|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
20494|Wooden Duck Member|44471|14|Not recorded|p.9, opp.p.7, map|||(D53-10).||||||
20494|Wooden Duck Member|44472|5|Briefly described|map legend|||Of the Mainoru Formation.  Flaggy quartz greywacke, micaceous greywacke, few galuconitic bands.  Upper (?) Proterozoic.||||||02-DEC-04
20494|Wooden Duck Member|45162|6|Mentioned|Fig.4|||||||||
20494|Wooden Duck Member|60573|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Mainoru Formation (Roper Group).  Dark green to grey laminated mudstone; with thinly bedded siltstone and fine-grained sandstone; thin to thick bedded micaceous and glauconitic fine-grained sandstone; minor laminated limestone.||||||22-FEB-05
20494|Wooden Duck Member|61390|5|Briefly described|Map Legend|Ectasian|Calymmian|Of the Mainoru Formation. Dark grey to green laminated mudstone with thinly interbedded siltstone and fine grained sandstone; thin to thick bedded micaceous and glauconitic fine grained sandstone.||||||
20494|Wooden Duck Member|64975|6|Mentioned|p162 Fig.6.|Mesoproterozoic|Mesoproterozoic|||Unit in Mainoru Formation.||||
20494|Wooden Duck Member|69430|4|Described|p15:26-27, 30|Calymmian|Calymmian|Abbott et al. (2001). McArthur Basin. 55m to over 350m thick. Storm-dominated shelf deposits.||Mainoru Formation.||Conformably overlies Mountain Valley Limestone Member. Is overlain conformably by Showell Member.|Greyish-green mudstone and fine micaceous glauconitic sandstone.|12-JUL-16
20494|Wooden Duck Member|70734|5|Briefly described|p14, 16|||McArthur Basin. Age consistent with Re-Os age of Velkerri Formation, higher in succession. Storm-dominated shelf (mudstone-dominated), top sandstone-dominated.|SHRIMP age 1492+/-4 Ma from tuff.|Of Mainoru Formation.||||
20494|Wooden Duck Member|70822|5|Briefly described|p102 fig 1 (A)|Mesoproterozoic|Mesoproterozoic||1492 +/- 4 Ma (U-Pb zircon).|Mainoru Formation||Overlies Mountain Valley Limestone Member; overlain by Showell Creek Member.|Interbedded mudstone, siltstone and fine sandstone.|
20494|Wooden Duck Member|70968|2|Defined|p17-18,p20,p30-33,p130-131,p140,p143-144|Calymmian|Calymmian|Sweet and Abbott in Abbott et al. (2001) after Dunn (1963). Named after Wooden Duck Creek. The type section is from 373800mE 8437400mN (base) to 374000mE 8437300mN in NW URAPUNGA sheet. Very similar mineralogy and texture to Showell Member: difficult to tell apart. Forms prominent escarpments with sandstone caps. Lithology described and illustrated. Thickness from 17m to 130m. Shallowing-upward marine-shelf sucession.||Mainoru Formation.||Conformably overlies Mountain Valley Limestone Member. Is overlain conformably by Showell Member.|Dominantly mudstone interbedded with very fine- to rarely medium-grained, commonly micaceous and glauconitic sandstone that increases in frequency up-section. Rare limestone or dolostone in middle part.|
20494|Wooden Duck Member|71059|4|Described|p3, p20|Mesoproterozoic|Mesoproterozoic|McArthur Basin. 56-130m thick. Storm-dominated marine shelf deposits. Organic petrology reflectivity data tabulated.||Mainoru Formation.||Conformably overlies Mountain Valley Limestone Member. Is overlain conformably by Showell Member.|Grey-green mudrocks interbedded with usually very fine micaceous glauconitic sandstone, rare limestone.|
20494|Wooden Duck Member|71488|5|Briefly described|p141 fig 1b|Calymmian|Calymmian||1492 +/- 4 Ma|Mainoru Formation||Overlies the Mountain Valley Limestone Member. Overlain by the Showell Creek Member.||
20494|Wooden Duck Member|71494|4|Described|p2-p4, p6-p13, p15, p17-p19, p26|||Thickness ranges from 55 to 350 metres plus. Deposited in a storm-dominated shelf environment. Identified as the Wood sequence by Abbott and Sweet (2000) in their sequence stratigraphic interpretation of the Roper Group. Core log features presented in this volume.||Mainoru Formation||Conformably overlies the Mountain Valley Limestone Member. Conformably overlain by the Showell Member.|Greyish-green mudstone and fine micaceous glauconitic sandstone.|
20494|Wooden Duck Member|71779|5|Briefly described|p2 Fig. 1|||Urapunga Region, McArthur Basin.||Mainoru Formation||||24-SEP-18
20494|Wooden Duck Member|73242|5|Briefly described|p39|Calymmian|Calymmian|Geochron are U-Pb zircon ages [see Fig. 2].|1492 +/- 4 Ma, 1493 +/- 4 Ma|Mainoru Formation, Collara Subgroup, Roper Group||Underlain by Mountain Valley Limestone Member. Overlain by Showell Member.|Includes interbedded mudstone and fine sandstone with marine shelf sandstone.|
20549|Woolaston Formation|5952|5|Briefly described|p214 Fig. 4, p215 Fig. 5, p228 Fig. 18|Late Cretaceous|Late Creatceous|In figure, Fm = Formation. Geological Province: Bonaparte Basin.||||||01-MAR-10
20549|Woolaston Formation|7142|6|Mentioned|p350 Fig.4.|Late Cretaceous|Late Cretaceous|Browse Basin.||||Overlies Jamieson Formation. Is overlain by Fenelon and Gibson Formations.||
20549|Woolaston Formation|13353|6|Mentioned|p401 Fig.2.|Late Cretaceous|Late Cretaceous|||||Overlies Jamieson Formation. Is overlain by Fenelon and Gibson Formations.||
20549|Woolaston Formation|13354|6|Mentioned|p375 Fig.6.|Late Cretaceous|Late Cretaceous|Unit of Bathurst Island Group. Overlies Jamieson Formation and underlies Fenelon and Gibson Formations.||103||||28-OCT-14
20549|Woolaston Formation|22663|5|Briefly described|AC97 1-4 Fig.4||Cretaceous|Of the Bathurst Island Group.||||||01-MAR-10
20549|Woolaston Formation|23378|4|Described|p180 Fig.2, p182||Late Cretaceous|Of the Bathurst Island Group. In the Vulcan Sub-basin.||||||01-MAR-10
20549|Woolaston Formation|24171|6|Mentioned|p729|||See also the misspelt Woollaston Formation.||||||20-DEC-06
20549|Woolaston Formation|24207|5|Briefly described|p209 Fig.5, p218|Cenomanian|Cenomanian|Geological Province: Vulcan Sub-basin.||||||01-MAR-10
20549|Woolaston Formation|24218|5|Briefly described|p853 Fig. 5|Late Cretaceous|Late Cretaceous|Geological Province: Bonaparte Basin.||||||
20549|Woolaston Formation|42053|5|Briefly described|Fig.2 p29|||||||||20-SEP-17
20549|Woolaston Formation|42066|5|Briefly described|Fig.3 P199|||||||||
20549|Woolaston Formation|43826|6|Mentioned|Fig.2,p163||Late Cretaceous|||||||01-MAR-10
20549|Woolaston Formation|60385|6|Mentioned|p270, p272 Fig 3, p276|Campanian|Cenomanian|Browse Basin.|||||Pelagic marl, hemipelagic marl, limestone.|
20549|Woolaston Formation|60634|6|Mentioned|p1168 Fig.3. |Late Cretaceous|Late Cretaceous|||Unit in Bathurst Island Group.||Overlies Jamieson Formation. Is overlain by Gibson Formation.||
20549|Woolaston Formation|61548|6|Mentioned|p480 Fig.3|Late Cretaceous|Late Cretaceous|Northern Bonaparte Basin.||||||
20549|Woolaston Formation|61550|6|Mentioned|p495 Fig.2. |Late Cretaceous|Late Cretaceous|||Unit in Bathurst Island Group.||Overlies Jamieson Formation. Is overlain by Gibson Formation.||
20549|Woolaston Formation|62837|5|Briefly described|Stratigraphic columns|Late Cretaceous|Late Cretaceous|Of the Bathurst Island Group. Age: ~95-~86Ma. Geological Province: Vulcan Sub-basin, Londonderry High and Northern Bonaparte Basin.||||||01-MAR-10
20549|Woolaston Formation|63358|5|Briefly described|p4 Fig. 1.3|Santonian|Cenomanian|See also p133 Fig. 3.71.||||||01-MAR-10
20549|Woolaston Formation|64695|5|Briefly described|p262 Fig.8|Late Cretaceous|Late Cretaceous|Northern Bonaparte Basin.||||Is overlain by Gibson Formation.||
20549|Woolaston Formation|64697|5|Briefly described|p84 Fig.2 |Late Cretaceous|Late Cretaceous|||||||
20549|Woolaston Formation|66187|5|Briefly described|p413 Fig.2, p414 Tb.1|Campanian|Turonian|Bathurst Island Group. Underlies the Gibson Formation, overlies the Jamieson Formation. Mount Ashmore Dome. Deep water limestone.||||||
20549|Woolaston Formation|68223|6|Mentioned|p178 Fig.3|Coniacian|Cenomanian|||||||
20549|Woolaston Formation|69297|6|Mentioned|p305|Coniacian|Cenomanian|Caswell, Barcoo and Seringapatam Sub-basins of the Browse Basin. See also reference to lower Woolaston Formation p303.||Bathurst Island Group||Overlies the Upper Jamieson Formation. Overlain by the Gibson Formation.|Siltstone and shale.|20-SEP-17
20549|Woolaston Formation|69452|5|Briefly described|p36:15|Cretaceous|Cretaceous|Bonaparte Basin.||Bathurst Island Group.||||12-JUL-16
20549|Woolaston Formation|70061|5|Briefly described|Regional geology; Figs.6-7|Turonian|Cenomanian|See also Sahul: Fig.2, p1-2. Vulcan: Fig.2. Reservoir carbonates in Sahul Syncline.||Bathurst Island Group.||Overlies Jamieson and Wangarlu Formations. Is overlain by Brown Gannet Limestone.||12-JUL-16
20549|Woolaston Formation|70064|5|Briefly described|Regional Fig. 6. Central: Fig.2|Turonian|Cenomanian|See also Northern: Fig.2. Yampi: Fig.2. Browse Basin. Not present in Yampi and Leveque Shelves.||Bathurst Island Group.||Overlies Upper Jamieson Formation. Is overlain by Brown Gannet Limestone.||12-JUL-16
20664|Wuluma Granite|9199|5|Briefly described|Map legend|Precambrian|Precambrian|Of the Strangways Metamorphic Complex.  Geological Province: Arunta Block.||||||03-NOV-04
20664|Wuluma Granite|23363|5|Briefly described|352 Tab.3|Statherian|Statherian|Age: 1728+/-3Ma.||||||20-DEC-06
20664|Wuluma Granite|23732|5|Briefly described|p22|Paleoproterozoic|Paleoproterozoic|Age: 1728+/-3Ma (Lafrance et al, 1995).  Geological Province: Arunta Province.||||||30-SEP-15
20664|Wuluma Granite|23733|5|Briefly described|p34 Fig.20|||Age: 1726Ma.||||||
20664|Wuluma Granite|23868|5|Briefly described|p753|Paleoproterozoic|Paleoproterozoic|Age: 1728+/-3Ma.  Geological Province: Arunta Inlier.||||||07-NOV-08
20664|Wuluma Granite|24540|6|Mentioned|p8|||Example of a rare earth element-bearing granite. Also contains a phase which probably contains allanite. Geological Province: Arunta region.||||||07-FEB-11
20664|Wuluma Granite|37266|6|Mentioned|p64|||||||||
20664|Wuluma Granite|37267|6|Mentioned|p68|||||||||
20664|Wuluma Granite|39470|6|Mentioned|p43|||||||||
20664|Wuluma Granite|40079|6|Mentioned|p87|||||||||
20664|Wuluma Granite|44114|5|Briefly described|p327-329, 331, 339-340|||Wuluma area, Arunta Inlier. A series of steeply dipping sheets, generally concordant with high-T shear zones. Appears as Wuluma granite on p328.|~1730 Ma.||||Anatectic granite derived in situ from migmatites. Emplaced as steeply dipping sheets.|
20664|Wuluma Granite|48992|6|Mentioned|p50|||||||||
20664|Wuluma Granite|60547|5|Briefly described|Map Legend|Precambrian|Precambrian|Of the Strangways Metamorphic Complex. Granite. Geological Province: Arunta Block.||||||06-JUN-05
20664|Wuluma Granite|62595|6|Mentioned|p4.|||Strangways Range. Related to partial melting during high-grade metamorphism.||||||
20664|Wuluma Granite|64329|6|Mentioned|p16|Proterozoic|Proterozoic|A phase of this granite probably contains allanite.||||||29-JUL-08
20664|Wuluma Granite|64738|5|Briefly described|p247 Fig.2, p248, p250 Table 1. |Statherian|Statherian|An S-type anatectic partial melt of adjacent country rocks. Reported age could reflect inheritance.|Crystallised 1728 +/- 3 Ma.|||||
20664|Wuluma Granite|66860|6|Mentioned|p8, p16||||1728+/-3 Ma, SHRIMP zircon: La france et al. 1995|Strangways Metamorphic Complex||||
20664|Wuluma Granite|67114|5|Briefly described|p757-772, 774-778|||Aileron Province, North Australian Craton. More often than not it is referred to as the Wuluma Pluton (see article's title); later in the article it appears as Wuluma granite. All references are included here under this, the stratigraphic name. Mineralogy, petrologies detailed. Photographs, photomicrographs, geochemistry.|1.73-1.69 Ga.|||Intrudes Strangways Metamorphic Complex.|Elongate intrusion comprising a multitude of heterogeneous, sub-parallel sheets and cross-cutting dykes. Abundant screens of pelitic granulite country rocks, and schlieren (detailed description).|
20664|Wuluma Granite|67323|5|Briefly described|p32|||Arunta Inlier. Emplacement was synchronous with the Strangways Event.|~1735-1725 Ma.|||||
20664|Wuluma Granite|68150|5|Briefly described|p11 Tb.3.2|||Magmatic crystallisation 1728 +/- 3 Ma (MSWD 2.4; no. of analyses 10) Lafrance et al. (1995). See also Wuluma Suite in this paper. Aileron Province.||Wuluma Suite||||
20664|Wuluma Granite|69427|4|Described|p12:3, 9-10, 40-41, 62|Statherian|Statherian|Strangways Range, Aileron Province. Is thought to have formed in situ through melting of the Ingula Migmatite during the Strangways Event. 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). SHRIMP U-Pb zircon age. May have potential for allanite-related REE mineralisation.|1728 +/- 3 Ma (Lafrance et al., 1995).|||Grades into Ingula Migmatite.|A sheet-like body of weakly-deformed, equigranular biotite +/- muscovite granite. Emplaced in extensional fractures parallel to the regional gneissic fabric. Peraluminous. S-type.|12-JUL-16
20664|Wuluma Granite|70825|6|Mentioned|p41|||Ongeva Package, Arunta Region, North Australian Craton.||||||
20664|Wuluma Granite|71348|6|Mentioned|p201|Statherian|Statherian|Geological province: Aileron Province, Arunta Region.||||||
20664|Wuluma Granite|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen.|1728+/-3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
20664|Wuluma Granite|71839|5|Briefly described|p10, p12|Statherian|Statherian|Age is interpreted as a U-Pb zircon magmatic crystallisation age.|ca 1730 Ma|||Equivalent to the Gumtree Granite.||21-MAR-23
20664|Wuluma Granite|71858|5|Briefly described|p4, p11|||Aileron Province. Prospective for REE mineralisation.||||||
20737|Yabooma Formation|42058|4|Described|p115|||||||||
20737|Yabooma Formation|62506|5|Briefly described|p1-2|Carboniferous|Devonian|Of the Arafura Group. Thickness: 335m. Siltstone, dolomite, sandstone, shale.||||||
20737|Yabooma Formation|62510|5|Briefly described|p3|Late Devonian|Late Devonian|||||||
20737|Yabooma Formation|63062|5|Briefly described|p9 Fig. 9|Late Devonian|Late Devonian|Of the Arafura Group. Age: ?Frasnian- Famennian. Unconformably overlies Djabura Formation. Geological Province: Arafura and Money Shoal Basins. Interbedded clastics and carbonates.||||||07-FEB-11
20737|Yabooma Formation|69297|5|Briefly described|p283, p285|Famennian|Frasnian|Arafura Basin. Deposited in a shallow marine environment.||Arafura Group||Overlies the Djabura Formation. Overlain by the Darbilla Formation.|Interbedded clastics.|
20737|Yabooma 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). Nearshore shallow-marine deposits. 140-335m thick. Conodonts indicate a late Famennian age.||Arafura Group.||Unconformably overlies Djabura Formation. Is overlain by Darbilla Formation, apparently conformably.|Interbedded siltstone with dolomitic intervals, occasional thin sandstone beds; sparse fossil fauna of conodonts, fish and bryozoans.|12-JUL-16
20737|Yabooma Formation|69673|6|Mentioned|p197|||||Arafura Group||||
20737|Yabooma Formation|70098|4|Described|p5, p19 Fig.5|Famennian|Late Devonian|Age: ?Frasnian||||||
20740|Yackah beds|8217|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Cherty dolomite with columnar stromatolites, sandstone, siltstone. Overlies Mount Dobbie Granite.||||||20-DEC-06
20740|Yackah beds|22589|6|Mentioned|p128||Neoproterozoic|||||||
20740|Yackah beds|22907|6|Mentioned|41|||Geological Province: Georgina Basin.||||||11-JUN-08
20740|Yackah beds|23557|6|Mentioned|p98|||Geological Province: Georgina Basin.||||||
20740|Yackah beds|37929|5|Briefly described|p526|||||||||
20740|Yackah beds|39340|6|Mentioned|p359|||||||||
20740|Yackah beds|40538|5|Briefly described|Map legend|Adelaidean|Adelaidean|Sandstone; granule conglomerate; dolostone. Geological Province: Georgina Basin.||||||15-NOV-05
20740|Yackah beds|40906|6|Mentioned|p18|||||||||
20740|Yackah beds|42775|5|Briefly described|p322|||||||||
20740|Yackah beds|45155|6|Mentioned|Fig.7|||In the Georgina Basin.||||||20-DEC-06
20740|Yackah beds|48990|2|Defined|p15|Adelaidean|Adelaidean|||||||
20740|Yackah beds|49027|6|Mentioned|p2|||||||||
20740|Yackah beds|60122|5|Briefly described|p9, p11 Tb. 1|||In Supersequence 1 on HAY RIVER and HUCKITA; not in TOBERMORY sheet. Disconformably overlain by Yardida Tillite. Geological Province: Georgina Basin.||||||
20740|Yackah beds|60551|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Underlies Mount Cornish Formation. Geological province: Georgina Basin.  Sandstone, granule conglomerate, dolomite.||||||20-DEC-06
20740|Yackah beds|60590|5|Briefly described|Map legend|Cryogenian|Cryogenian|Chertified dolostone, sandstone and siltstone.||||||25-NOV-04
20740|Yackah beds|61404|5|Briefly described|Map legend|Cryogenian|Cryogenian|Of the Plenty Group. Chertified dolostone, sandstone and siltstone.  Geological Province: southern Georgina Basin.||||||11-OCT-05
20740|Yackah beds|62453|6|Mentioned|p16|||Geological Province: Georgina Basin.||||||
20740|Yackah beds|63450|5|Briefly described|p78 Fig. 5, p79|Neoproterozoic|Neoproterozoic|Disconformably overlain by Yardida Tillite. Geological province: Georgina Basin, West Toko Syncline. Comprise chertified dolostone, sandstone and siltstone; contain a stromatolite in common with Bitter Springs Formation.||||||07-FEB-11
20740|Yackah beds|63562|5|Briefly described|p338 fig 3, p342, p352 fig 10|Cryogenian|Neoproterozoic|Of Georgina Basin.|||||Basal sandstone overlain by a relatively thin carbonate unit.|08-DEC-17
20740|Yackah beds|64068|4|Described|p44, p164, p35, p223|Cryogenian||Lower siliciclastic rocks correlated with Amesbury Quartzite, Heavitree Quartzite, Vaughan Springs Quartzite; upper stromatolitic carbonate correlated with Bitter Springs Formation, Albinia Formation.||Of Plenty Group.||Overlies Mount Dobbie and Jervois Granites. Is disconformably overlain by Yardida Tillite and Mount Cornish Formation.|Interbedded fine to very coarse, grey arkose, sandstone and laminated anoxic shale overlain by stromatolitic dolostone.|05-APR-12
20740|Yackah beds|64793|6|Mentioned|p293|||Georgina Basin. Hosts Acaciella australica Stromatolite Assemblage.||||||
20740|Yackah beds|65363|6|Mentioned|p11.|||Presence of Acaciella australica Stromatolite Assemblage in the Woolnough Member of the Browne Formation enables correlation with this unit, Skates Hill Formation, Loves Creek Member of the Bitter Springs Formation, and Coominaree Dolomite.||||||
20740|Yackah beds|65366|5|Briefly described|p24|||Georgina Basin.  Includes the Acaciella australica Stromatolite Assemblage||||||
20740|Yackah beds|67870|6|Mentioned|p43|Neoproterozoic|Neoproterozoic|Georgina Basin.||||||
20740|Yackah beds|68270|5|Briefly described|p680,683|Tonian|Tonian|Southern Georgina Basin.||||Overlain disconformably by Mount Cornish Formation and Yardida Tillite.||
20740|Yackah beds|69437|5|Briefly described|p22:4-6|Cryogenian|Cryogenian|SE Georgina Basin, Centralian A Superbasin. Supersequence 1.||Plenty Group.||||12-JUL-16
20740|Yackah beds|69443|4|Described|p28:5-8|Cryogenian|Cryogenian|Walker (1980). Informal name. Southern Georgina Basin. Up to 250m thick. Poorly exposed. Dominantly fluviatile, minor intertidal to very shallow-marine deposits in the lower interval; partially emergent, metahaline-hypersaline lacustrine to anoxic deep marine conditions in upper interval.||Plenty Group.||Is overlain disconformably by Yardida Tillite and Mount Cornish Formation. Lower and upper intervals are correlated with Heavitree and Amesbury Quartzites and Bitter Springs Formation respectively.|Interbedded, fine to very coarse (to granule) arkose, sandstone and laminated shale; overlain by or interbedded with an upper interval of silicified, locally stromatolitic (Acaciella australica) dolostone.|12-JUL-16
20740|Yackah beds|69673|6|Mentioned|p112, p114 fig 92|||Up to 250m thick.||Plenty Group|||Interbedded sandstone, laminated shale and silicified, locallly stromatolitic dolostone.|
20740|Yackah beds|72375|5|Briefly described|p5|||Of SE Georgina Basin.||||Equivalent to Heavitree Formation.||
20740|Yackah beds|72516|3|Fully described|p13-15, p64, p85-86, p88, p154, p218|Tonian|Tonian|Georgina Basin. First described in HAY RIVER map sheet. These are the oldest Georgina Basin rocks in the map sheet area. Appears as Yackah Beds on p14 , Yakah beds p13, p15 (misspelling). Subdivided into an upper and lower interval. 26m thick in the map sheet area, 250m thick in HAY RIVER map sheet. The lower interval was deposited in a fluviatile and minor intertidal to very shallow marine environment. The upper interval was deposited in a metahaline-hypersaline lacustrine to anoxic deep marine environment. Contains rare columnar,branching stromatolites in the upper interval. Age correlative of the Vaughan Springs Quartzite in the Ngalia Basin.||Plenty Group||Disconformably overlain by the Mount Cornish Formation. Unconformably overlies the Tarlton Granite and the Denara Orthogneiss. Equivalent to the Heavitree Formation.|Fine- to very coarse-grained subarkose to arkosic granule conglomerate grading upwards into quartz arenite to lithic greywacke and laminated shale. Thinly bedded, lenticular, silicified, yellow, pink and grey dolostone.|04-JUL-22
20740|Yackah beds|73086|6|Mentioned|p18, p30, p39|||Georgina Basin. Deposited in a hypersaline lacustrine to anoxic, deep marine conditions (Walter and Veevers, 1997). [Misspelt as Yakah beds on p9 and p145].||||Correlates to Heavitree Formation.||
20758|Yalco Formation|22538|6|Mentioned|Fig3 P709|||||||||
20758|Yalco Formation|22664|5|Briefly described|39,40 fig 5,41,47|Paleoproterozoic|Paleoproterozoic|Of theBatten Subgroup (McArthur Group). In the McArthur Basin.||||||07-NOV-08
20758|Yalco Formation|22853|3|Fully described|23|Proterozoic|Proterozoic|Of the Batten Subgroup. Max thickness 250 m.||||||06-NOV-06
20758|Yalco Formation|23387|6|Mentioned|p18 fig.19|||Of Batten Subgroup.||||||
20758|Yalco Formation|23397|5|Briefly described|p474|||||||||
20758|Yalco Formation|23398|6|Mentioned|p443|||||||||
20758|Yalco Formation|23776|5|Briefly described|p705 Fig 2.|||Of Batten Subgroup.||||||
20758|Yalco Formation|23902|4|Described|p1568 Fig.2|||Of the Batten Subgroup. Overlies the Lynott Formation. Overlain by the Stretton Sandstone. Geological Province: McArthur Basin||||||
20758|Yalco Formation|23910|5|Briefly described|p292 Fig. 2|||Of Battern Subgroup.  Geological Province: McArthur Basin.||||||
20758|Yalco Formation|23937|4|Described|p9, p25 Tb. 2|Statherian|Statherian|Of the Batten Subgroup (McArthur Group).  Dolostone, siltstone, sandstone and tuff.  Overlies the Lynott Formation.  Geological Province: McArthur Basin.||||||03-NOV-04
20758|Yalco Formation|23963|5|Briefly described|p1239 Fig.2|||Geological Province: McArthur Basin. Of the Batten Subgroup.||||||
20758|Yalco Formation|24048|6|Mentioned|p57|||||||||
20758|Yalco Formation|24179|5|Briefly described|p84 Fig. 2|||Overlies the Lynott Formation.  Geological Province:  McArthur Basin.||||||
20758|Yalco Formation|24432|5|Briefly described|p565 Fig.2|Statherian|Statherian|Of Batten Subgroup. Overlies Lynott Formation. Overlain by Stretton Sandstone. Geological Province: Southern McArthur Basin.||||||
20758|Yalco Formation|30344|6|Mentioned|Fig.4|||Part of Batten Subgroup||||||
20758|Yalco Formation|32658|4|Described|Table 2|||||||||
20758|Yalco Formation|32660|5|Briefly described|Table 4|||||||||
20758|Yalco Formation|33666|6|Mentioned|Table 1|||||||||
20758|Yalco Formation|35261|6|Mentioned|Fig.2|||||||||
20758|Yalco Formation|37568|5|Briefly described|p79|||||||||
20758|Yalco Formation|38143|6|Mentioned|p21|||||||||
20758|Yalco Formation|38582|6|Mentioned|Fig.3|||||||||
20758|Yalco Formation|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
20758|Yalco Formation|40259|6|Mentioned|Table 1|||||||||
20758|Yalco Formation|40691|4|Described|p82|||||||||
20758|Yalco Formation|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
20758|Yalco Formation|41220|4|Described|p367|||||||||
20758|Yalco Formation|41277|6|Mentioned|Fig.2|||||||||
20758|Yalco Formation|42385|4|Described|p23|||See also Table 4 p16.||||||06-NOV-06
20758|Yalco Formation|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
20758|Yalco Formation|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.||Of Batten Subgroup (McArthur Group).||In schematic section, underlies Stretton Sandstone; overlies Donnegan Member (Lynott Formation).|Stromatolitic dololutite, silty dololutite, dolarenite, minor sandstone; domal stromatolites. Detailed lithology given.|09-NOV-11
20758|Yalco Formation|42639|4|Described|p32, Table 5 p20|||||||||
20758|Yalco Formation|42700|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
20758|Yalco Formation|42739|5|Briefly described|map legend|Statherian|Statherian|Of the Batten Subgroup. Thinly interbedded chertified stromatolitic dololutite, dolarenite and minor sandstone.||||||19-OCT-05
20758|Yalco Formation|42812|3|Fully described|p41, Table 4|||Of Batten Subgroup (McArthur Group).||||||06-NOV-06
20758|Yalco Formation|42846|5|Briefly described|Fig.1 502|||Of McArthur Group. Geological Province: McArthur Basin.||||||09-MAY-05
20758|Yalco Formation|42935|6|Mentioned|p529 Fig.2|||of Batten Subgroup||||||
20758|Yalco Formation|43010|6|Mentioned|p128|||||||||
20758|Yalco Formation|43036|4|Described|p55|||Of Batten Subgroup.||||||06-NOV-06
20758|Yalco Formation|44287|14|Not recorded|p.6,9,10, opp.9|||Foreeef seds. (E53-3).||||||
20758|Yalco Formation|44288|14|Not recorded|map legend|||Cherty siltstone, shale, chert. Lower (?) Proterozoic.||||||
20758|Yalco Formation|44434|14|Not recorded|p.7, opp. p.6, map|||Middle formation of Batten Subgroup (McArthur Group). (D53-11,12).||||||
20758|Yalco Formation|44435|14|Not recorded|map legend|||Lower (?) Proterozoic.||||||
20758|Yalco Formation|44530|14|Not recorded|p.10, opp.10|||(D53-15).||||||
20758|Yalco Formation|44531|14|Not recorded|map legend|||Lower (?) Proterozoic.||||||
20758|Yalco Formation|45162|2|Defined|p120|||||||||
20758|Yalco Formation|46915|6|Mentioned|Fig.1|||Stratigraphic section through McArthur Group.||||||
20758|Yalco Formation|46968|6|Mentioned|Fig.2|||||||||
20758|Yalco Formation|60483|5|Briefly described|p7 Fig. 5, p30|||Of Batten Subgroup (McArthur Group). Geological Province: McArthur Basin.||||||05-OCT-07
20758|Yalco Formation|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Batten Subgroup. Overlian by Stretton Sandstone, underlain by Lynott Formation.||||||
20758|Yalco Formation|60573|5|Briefly described|Map legend|Statherian|Statherian|Of the McArthur Group. Silicified dolarenite, quartz arenite and laminated dololutite.||||||
20758|Yalco Formation|61390|5|Briefly described|Map Legend|Statherian|Statherian|Of the McArthur Group. Silicified dolarenite, quartz arenite and laminated dololutite.||||||
20758|Yalco Formation|64815|6|Mentioned|p4 Fig.2, p5 Fig.3|||||Of the Batten Subgroup.||||
20758|Yalco Formation|64817|6|Mentioned|p353 Fig.4 |||||Of the Batten Subgroup.||||
20758|Yalco Formation|65228|5|Briefly described|p32, p33, Table 1, Figs.02, 04, 22-23.|||Top unit in River Supersequence. Measured section.||Unit in Batten Subgroup.||Overlies Lynott Formation. Is overlain unconformably by Stretton Sandstone.||
20758|Yalco Formation|66843|6|Mentioned|p38 Fig.10|||Shown only as Yalco.||||||12-SEP-19
20758|Yalco Formation|69418|6|Mentioned|p3:36|||McArthur Basin. Good potential hydrocarbon source rocks.||||||12-JUL-16
20758|Yalco Formation|69430|4|Described|p15:2-3, 16, 19, 22, 30, 34, 41, 61-62|Statherian|Statherian|Southern McArthur Basin. <50-250m thick. Shallow-marine to emergent deposits. Ridge-forming unit. Potential hydrocarbon source rock; fair to good conventional reservoirs occur.||Batten Subgroup.||Conformably overlies Donnegan Member (Lynott Formation). Is overlain conformably by Stretton Sandstone. Correlated with part of Zamia Creek Siltstone.|Thinly interbedded stromatolitic dololutite, silty dololutite, dolarenite and minor sandstone with abundant chert nodules and laminae; abundant small domal stromatolites and common dessication cracks, tepee structures and gypsum pseudomorphs.|12-JUL-16
20758|Yalco Formation|69673|4|Described|p16 fig 13, p24, p27, p32, p34, p40|||Batten Fault Zone. Potential source rock and reservoir rock. Maximum thickness of 250m. Deposited in shallow marine environment,||Batten Subgroup||Conformably overlies Lynott Formation, Donnegan Member, conformably overlain by Stretton Sandstone|Chert, thinly interbedded stromatolitic dolomudstone, silty dolomudstone, sandy dolostone and dolomitic sandstone. Intraclast chert breccias.|
20758|Yalco Formation|71374|4|Described|iii, p1 tbl 1, p9-p11, p18, p45-p46|Statherian|Statherian|McArthur Basin. SHRIMP age is interpreted as the maximum depositional age for this formation. A reference area is provided after Jackson et al (1987) around the grid coordinate 610051mE 8208479mN. Dolostone are commonly stromatolitic and contain numerous sedimentary structures (detailed). Sampling site provided along with zircon description and SHRIMP analytical discussion. Unconformably overlain by the Smythe Sandstone. Conformably overlain by the Stretton Sandstone and unconformably by Roper and Nathan Groups.|1655 +/- 17 Ma (SHRIMP U-Pb)|McArthur Group||Conformably overlies the Lynott Formation (Donnegan and Hot Spring members). Overlies the Umbolooga Subgroup.|Fine-grained and parallel-bedded, aphanitic dololutite and dolarenite with abundant nodules and laminae of early diagenetic chert and minor interbedded lithic sandstone.|09-MAY-18
20758|Yalco Formation|72248|5|Briefly described|p147|||Of McArthur Basin.||Unit of Batten Subgroup.||||
20758|Yalco Formation|72373|5|Briefly described|iii,p14, 17,27|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. Interpreted to be broadly equivalent with Stretton Sandstone and Nagi Formation (Vizard Group), likely shared similar source areas from the same or similar terranes.||Unit of Batten Subgroup.||||02-OCT-19
20758|Yalco Formation|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Batten Fault Zone of the Southern McArthur Basin.||Batten Subgroup||Overlies Lynott Formation and Hot Springs Member and underlies Stretton Sandstone.||
20758|Yalco Formation|72718|6|Mentioned|p7|||Southern McArthur Basin. Batten Fault Zone.||Batten Sub-group, McArthur Group||Underlain by Lynott Formation (including Donnegan Member). Partly overlain by Stretton Sandstone and Catfish Conglomerate.||
20758|Yalco Formation|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Batten Fault Zone of the Southern McArthur Basin.||Batten Subgroup||Overlies Lynott Formation and Hot Springs Member and underlies Stretton Sandstone.||
20758|Yalco Formation|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin, Isa Superbasin.||Batten Subgroup, McArthur Group||Underlain by Lynott Formation. Overlain by Stretton Sandstone.||
20758|Yalco Formation|73280|6|Mentioned|p1, p4-5, App.1A|||McArthur Basin. Sampled for XRD mineralogy to investigate brittleness and Kubler indices [see report].||||||
20758|Yalco Formation|73412|5|Briefly described|p4, 8|||Southern McArthur Basin.||Batten Subgroup.||Overlies Lynott Formation. Is overlain by Stretton Sandstone.||
20788|Yambah Granulite|9199|5|Briefly described|Map legend|Precambrian|Precambrian|Of the Strangways Metamorphic Complex.  Interlayered felsic, mafic and cordierite-quartz granulite, cordierite quartzite.  Geological Province: Arunta Block.||||||05-NOV-04
20788|Yambah Granulite|39470|6|Mentioned|p43|||||||||
20788|Yambah Granulite|40940|5|Briefly described|p214|||||||||
20788|Yambah Granulite|44114|5|Briefly described|p321|||Central Arunta Inlier. Bimodal extrusives.|>1780 Ma (Black and Shaw, 1995).||||Felsic and mafic granulites.|
20788|Yambah Granulite|48992|6|Mentioned|p62|||||||||
20788|Yambah Granulite|60547|5|Briefly described|Map Legend|Precambrian|Precambrian|Of the Strangways Metamorphic Complex. Interlayered felsic, mafic and cordierite-quartz granulite, cordierite quartzite. Geological Province: Arunta Block.||||||06-JUN-05
20788|Yambah Granulite|66860|4|Described|p7, p8, p10-16, p26, p38, p88|||Widespread unit of NW Strangways Metamorphic Complex. Hosts the Edwards Creek and Coles Hill base metal prospects; closely associated with marble lenses. Contains felsic intrusives, and mafic intrusives around Edwards Creek. Age is from zircon core (protolith). High-grade metamorphic overgrowth at 1716 +/- 3.2 Ma. Granulite grade metamorphic zircon crystallisation between 1730 - 1710 Ma.|1802.4 +/-4.8 Ma (SHRIMP U-Pb zircon).|Strangways Metamorphic Complex|||A thick package of intensely folded, predominantly felsic and mafic granulite with less abundant biotite-sillimanite gneiss, migmatite, marble and calcsilicate rocks. Pelites and semipelites may have originally been deepwater mudstone or greywacke.|
20788|Yambah Granulite|69427|3|Fully described|p12:9-11, 37-38, 52|Statherian|Orosirian|Shaw et al. (1979). Western Strangways Range, Aileron Province. Is distinguished (from Erontonga Metamorphics) by the predominance of felsic and mafic granulite. The type area [location not stated] contains mafic granulite, biotite-cordierite-garnet-orthopyroxene gneiss and orthopyroxene-bearing felsic granulite. Metamorphism briefly described. Hosts the sub-economic Coles Hill Zn-Pb-Cu prospect (detailed), and Edwards Creek VMS-style base metal mineralisation. SHRIMP U-Pb zircon age of volcaniclastic sedimentation. These zircons have metamorphic rims similarly dated at 1716 +/- 3 Ma.|1802 +/- 3 Ma (Hussey et al., 2006).|Strangways Metamorphic Complex.||Is structurally overlain by Cadney Metamorphics.|A thick package of intensely folded, predominantly felsic and mafic granulite, with less abundant cordierite-bearing felsic granulite, biotite-sillimanite gneiss, migmatite, cordierite-quartz granulite, marble and calc-silicate rock.|12-JUL-16
20788|Yambah Granulite|69917|6|Mentioned|p87|||||Of Strangways Metamorphic Complex.||||
20788|Yambah Granulite|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen. Both U-Pb zircon SHRIMP metamorphism ages.|1731+/-3 Ma and 1708+/-6 Ma.||||Garnetiferous felsic gneiss, quartz-cordierite-sillimanite-phlogopite gneiss.|
20788|Yambah Granulite|72711|6|Mentioned|p2, p4 Tb.1.|Statherian|Orosirian|Maximum mineralisation age of 1802 Ma based on a protolith age of 1802 +/- 5 Ma for the host Yambah Granulite (zircon 207Pb/206Pb age; Hussey et al 2006).|1802 +/- 5 Ma protolith age.||||Includes granulite.|
20852|Yaringa Metamorphics|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Fold Belt.||||||07-NOV-08
20852|Yaringa Metamorphics|24419|5|Briefly described|p14, p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Quartz-mica schist and gneiss, quartzite, migmatite and felsic metaporphyry.  No outcrop on URANDANGI 1:250K sheet.  Unconformably overlain by McNamara Group. Geol. Prov: Western Fold Belt, Leichardt River Subprovince.  See also p15 Fig. 6.||||||07-NOV-08
20852|Yaringa Metamorphics|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
20852|Yaringa Metamorphics|31342|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
20852|Yaringa Metamorphics|32659|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20852|Yaringa Metamorphics|32660|5|Briefly described|Table 5|||||||||
20852|Yaringa Metamorphics|32959|6|Mentioned|p31|||||||||
20852|Yaringa Metamorphics|33214|6|Mentioned|p1279|||||||||
20852|Yaringa Metamorphics|33893|5|Briefly described|p27|||Archaean.||||||
20852|Yaringa Metamorphics|33897|6|Mentioned|p1280|||||||||
20852|Yaringa Metamorphics|33900|6|Mentioned|p7|||Re dates||||||
20852|Yaringa Metamorphics|34395|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20852|Yaringa Metamorphics|35074|6|Mentioned|Fig.2|||||||||
20852|Yaringa Metamorphics|35139|6|Mentioned|p9|||||||||
20852|Yaringa Metamorphics|35167|6|Mentioned|p151|||||||||
20852|Yaringa Metamorphics|37462|4|Described|Table4.VII|||Also briefly described p266.||||||20-DEC-06
20852|Yaringa Metamorphics|37568|5|Briefly described|p81|||||||||
20852|Yaringa Metamorphics|37862|6|Mentioned|p586|||||||||
20852|Yaringa Metamorphics|38232|6|Mentioned|p83|||||||||
20852|Yaringa Metamorphics|38234|6|Mentioned|p103|||||||||
20852|Yaringa Metamorphics|38584|6|Mentioned|p4|||||||||
20852|Yaringa Metamorphics|39445|5|Briefly described|Table 2|||Minimum age of zircons 2000 Ma. See also p40.||||||20-DEC-06
20852|Yaringa Metamorphics|40840|6|Mentioned|Map legend|||||||||
20852|Yaringa Metamorphics|41298|6|Mentioned|Map legend|Proterozoic||||||||
20852|Yaringa Metamorphics|41381|6|Mentioned|p325|||||||||
20852|Yaringa Metamorphics|41465|5|Briefly described|p6|||||||||
20852|Yaringa Metamorphics|41466|4|Described|p24|||||||||
20852|Yaringa Metamorphics|41721|6|Mentioned|p4|||Geological province: Mt Isa Block.  Lithologically resembles Murphy Metamorphics (Murphy Inlier) and Burrell Creek Formation (Pine Creek Geosyncline).||||||13-MAR-18
20852|Yaringa Metamorphics|41978|6|Mentioned|p497|||||||||
20852|Yaringa Metamorphics|41979|6|Mentioned|p538|||||||||
20852|Yaringa Metamorphics|42367|5|Briefly described|p17|||Age about 1900 Ma U-Pb. Defined by Carter 1961||||||
20852|Yaringa Metamorphics|42565|5|Briefly described|Table 1 P6, P2|||||||||
20852|Yaringa Metamorphics|42706|5|Briefly described|map legend|Proterozoic|Proterozoic|Schist, gneiss, migmatite.   Age is pre-1890-1870Ma Barramundi Orogeny.||||||09-FEB-09
20852|Yaringa Metamorphics|43595|5|Briefly described|p353||Paleoproterozoic|Dated (U-Pb) at 1885+/-10 Ma||||||07-NOV-08
20852|Yaringa Metamorphics|43608|6|Mentioned|Fig.11,p11|||||||||
20852|Yaringa Metamorphics|43928|6|Mentioned|24|||||||||
20852|Yaringa Metamorphics|44195|6|Mentioned|p358||Paleoproterozoic|basement.||||||07-NOV-08
20852|Yaringa Metamorphics|44210|2|Defined|map,Tb.1,p8-10|||||||||
20852|Yaringa Metamorphics|44271|2|Defined|p26,38,45||Archean|||||||07-NOV-08
20852|Yaringa Metamorphics|44275|14|Not recorded|Map Legend|||||||||
20852|Yaringa Metamorphics|44290|2|Defined|p437|||Precambrian possibly Archaean.||||||
20852|Yaringa Metamorphics|44521|14|Not recorded|p8|||||||||
20852|Yaringa Metamorphics|44919|14|Not recorded|p596,(table)||Paleoproterozoic|||||||07-NOV-08
20852|Yaringa Metamorphics|44989|2|Defined|p.58-9|||Tb.III. On many pages. Intruded by Sybella Granite. (F54-1).||||||
20852|Yaringa Metamorphics|45161|6|Mentioned|p9|||||||||
20852|Yaringa Metamorphics|45166|4|Described|p8|||||||||
20852|Yaringa Metamorphics|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
20852|Yaringa Metamorphics|46919|6|Mentioned|p219|||||||||
20852|Yaringa Metamorphics|48997|6|Mentioned|Fig.1|||||||||
20852|Yaringa Metamorphics|49041|5|Briefly described|Table 1|||||||||
20852|Yaringa Metamorphics|50100|6|Mentioned|p26|||Age: >1870Ma.||||||
20852|Yaringa Metamorphics|50332|6|Mentioned|p25|Paleoproterozoic|Paleoproterozoic|||||||07-FEB-11
20852|Yaringa Metamorphics|50536|5|Briefly described|p11.2|Paleoproterozoic|Paleoproterozoic|Age: ~1890 +/- 8Ma. Intruded by Little Toby Granite.||||||07-NOV-08
20852|Yaringa Metamorphics|60513|6|Mentioned|p281, 282, 283,  p290, p287, 288, 289||||SHRIMP age  1.98 Ga.|||||
20852|Yaringa Metamorphics|61922|5|Briefly described|p19 Fig. 11|||See also p21 Fig.13.||||||
20852|Yaringa Metamorphics|61929|5|Briefly described|p128 Fig. 2|Paleoproterozoic|Paleoproterozoic|Age: 1890+/-8Ma.||||||07-NOV-08
20852|Yaringa Metamorphics|61933|5|Briefly described|p169 Fig.1, p181|||Metamorphosed to upper amphibolite grade between ca 1900 and 1870 Ma.||||||28-APR-06
20852|Yaringa Metamorphics|61936|6|Mentioned|p193|||Includes greenschist facies schist and phyllite||||||
20852|Yaringa Metamorphics|63593|6|Mentioned|p288 Fig.2. |||Western Fold Belt basement. Mis-spelt as Metamorphycs.|||||Schist, gneiss, migmatite.|
20852|Yaringa Metamorphics|63866|4|Described|p57-p58, p64|Orosirian|Orosirian|Leichhardt River Fault Trough. Ages are derived from Page and Williams 1988 and are U-Pb zircon TIMS analyses. A more recent U-PB zircon SHRIMP result of c. 1858 has been interpreted by Bierlein et al (in press).|1900 +/- 14 Ma and 1885 +/- 10 Ma|||Intruded by the Monoghans Granite.|Gneisses.|
20852|Yaringa Metamorphics|64250|6|Mentioned|p8, p9 fig 1, p11 fig 3, p19 |||A basement unit of Western Fold Belt, Mt Isa Inlier. Metamorphosed at 1890 +/- 8 Ma (Page and Williams 1998); crystallisation of igneous phases occurred ca. 1860 - 1850 Ma (Bierlein et al. 2008).|1890 +/- 8 - 1853 +/- 5 Ma|||||
20852|Yaringa Metamorphics|64254|5|Briefly described|p160 Fig. 1, p161, p162, p165, p169|Paleoproterozoic|Paleoproterozoic|Age: ca. 2200Ma (SHRIMP), 2380-2820Ma (Nd model). Geological Province: Kalkadoon - Leichhardt Belt.||||||
20852|Yaringa Metamorphics|64567|5|Briefly described|p1098||Paleoproterozoic|Actually spelt Yaringa metamorphics. About 45 km west of Black Angel Gneiss Complex, but different terranes, not juxtaposed until Mesoproterozoic.||||||21-APR-09
20852|Yaringa Metamorphics|65396|5|Briefly described|p7, p82, p84, p90, p171-172, p175, p186|Orosirian|Orosirian|See also p241, p437-438. Lawn Hill Platform. Basement to Mount Isa Inlier. Metamorphosed at 1890 +/- 8 Ma (Page and Williams, 1988). Crystallisation age c.1853 Ma suggests migmatisation.|1853 +/- 5 Ma (Bierlein and Black, 2005).|||||
20852|Yaringa Metamorphics|67323|5|Briefly described|p6-8, p23, p29, p39, p107|Paleoproterozoic|Paleoproterozoic|See also GIS attrib tbl, Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Pre-Barramundi basement to Ardmore - May Downs, Mount Oxide Domains, Mount Isa Inlier. Protoliths of this unit were metamorphosed during the ~1870-1850 Ma Barramundi Orogeny. Age of metamorphism ~1885 - 1900 Ma.|1890 +/- 8 Ma.|||Intruded by Big Toby, Little Toby and Moonaghans Granites|Quartz - muscovite and quartz - sericite schist and phyllite, quartz - muscovite - biotite gneiss, minor migmatite|
20852|Yaringa Metamorphics|67497|6|Mentioned|p910, p911 Fig.20|Orosirian|Orosirian|Include detrital zircon cores as old as 2200 Ma (Page and Williams 1988).||||||
20852|Yaringa Metamorphics|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province. Pre-Barramundi Orogeny basement. This unit, as well as Saint Ronans Metamorphics and Sulieman Gneiss, are all mapped under the symbol, -Px.||||||
20852|Yaringa Metamorphics|69222|5|Briefly described|p221, p222 Fig.2, p224 Fig.3|Paleoproterozoic|Paleoproterozoic|Basement to Lawn Hill Platform. Metamorphosed during the 1890-1840 Ma Barramundi Orogeny.|1890 +/- 8 Ma|||||09-FEB-18
20852|Yaringa Metamorphics|69591|5|Briefly described|p29-32, p58|Paleoproterozoic|Paleoproterozoic|One of the earliest known successions exposed within the Mount Isa Province: pre-Barramundi Orogeny (>1870 Ma). Considered part of the same depositional package as the Murphy and Yaringa Metamorphics. TIMS ages by Page and Williams (1988). Bierlein et al. (2008) date it at 1874 +/- 3 Ma. Intruded by ~1874 Ma granitoids.|1900 +/- 14 Ma and 1885 +/- 10 Ma.|||Is intruded by Monaghans, Big Toby, and Little Toby Granites.|Quartz-muscovite and quartz-sericite schist and phyllite, quartz-muscovite-biotite gneiss, minor migmatite.|
20852|Yaringa Metamorphics|69917|6|Mentioned|p140|||Western Mount Isa Inlier. Includes ca 1.86-1.88 Ga orthogneisses. Possible source for some of the Entia Dome metasediments (Entia Metamorphics?).||||||
20852|Yaringa Metamorphics|70282|6|Mentioned|p544 Tb.1|||Basement in the Western fold belt, Mount Isa.|1890-1870 Ma|||||13-FEB-18
20852|Yaringa Metamorphics|71592|5|Briefly described|Appendix A.|||Leichhardt River Domain, Mount Isa Orogen.|1900+/-14 Ma (metamorphism: U-Pb zircon SHRIMP)||||Paragneiss.|
20852|Yaringa Metamorphics|71606|5|Briefly described|p137|Orosirian|Orosirian|Leichardt River Fault Trough, Mount Isa Inlier.||||Overlain by Leichardt Volcanics. Equivalent to Murphy Metamorphics.||
20852|Yaringa Metamorphics|71960|5|Briefly described|p77|Paleoproterozoic||Basement to Mount Isa Group.|>1890 Ma, U-Pb zircon.|||||
20852|Yaringa Metamorphics|72527|6|Mentioned|p184.|Paleoproterozoic|Paleoproterozoic|Mount Isa Orogen. Given as an example of correlated units across the Northern Territory with the Murphy Metamorphics.||||||
20852|Yaringa Metamorphics|72912|5|Briefly described|p12.|Orosirian|Orosirian|Among the oldest known sedimentary rocks exposed in the Mount Isa province.||||||
20852|Yaringa Metamorphics|73413|6|Mentioned|p3|||Mount Isa Inlier, Western Fold Belt, Lawn Hill Platform.||||||
20852|Yaringa Metamorphics|73525|5|Briefly described|p4-5 Fig.2, p19 Fig.13|Orosirian|Orosirian|Leichhardt River Domain.|1890+/-8 Ma metamorphic age||||Metamorphics.|
20928|Yeldham Granite|22438|4|Described|p545-547, Fig.12||Paleoproterozoic|Age of unit 1820 Ma||||||07-NOV-08
20928|Yeldham Granite|22457|6|Mentioned|Fig31 P32, Fig29|||||||||
20928|Yeldham Granite|22680|6|Mentioned|85|||||||||
20928|Yeldham Granite|23198|6|Mentioned|p873, 876|||||||||
20928|Yeldham Granite|23393|4|Described|p18, p16 Fig. 4|Paleoproterozoic|Paleoproterozoic|Intrudes the Kamarga Volcanics.  Age: ~1820Ma.  Geological Province: Lawn Hill Sub-province.||||||07-NOV-08
20928|Yeldham Granite|23406|5|Briefly described|p601 Fig.3|||||||||
20928|Yeldham Granite|23408|6|Mentioned|p515, p516 Fig. 5|||Onlapped by Torpedo Creek Quartzite.  Includes igneous rocks.||||||15-JUN-09
20928|Yeldham Granite|23409|5|Briefly described|p535 Fig.2|||||||||
20928|Yeldham Granite|23545|5|Briefly described|Fig 1 p604|||||||||
20928|Yeldham Granite|23767|5|Briefly described|p1954 Fig. 1a|||Geological Province: Mount Isa Superbasin.||||||20-DEC-06
20928|Yeldham Granite|23958|5|Briefly described|p1133|||||||||
20928|Yeldham Granite|24197|5|Briefly described|p96 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Age: 1820Ma. Geological Province:Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
20928|Yeldham Granite|24309|5|Briefly described|p1017|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20928|Yeldham Granite|24419|6|Mentioned| p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: Western Fold Belt, Lawn Hill Subprovince (Mount Isa Orogen).||||||07-NOV-08
20928|Yeldham Granite|24432|6|Mentioned|p565 Fig.4|||||||||
20928|Yeldham Granite|36548|2|Defined|p517|Precambrian|Precambrian|||||||
20928|Yeldham Granite|37459|6|Mentioned|p423|||||||||
20928|Yeldham Granite|38291|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
20928|Yeldham Granite|38310|6|Mentioned|p237|||||||||
20928|Yeldham Granite|38348|4|Described|p5|||||||||
20928|Yeldham Granite|38900|6|Mentioned|p62|||||||||
20928|Yeldham Granite|39445|5|Briefly described|Table 2|||See also p40.||||||20-DEC-06
20928|Yeldham Granite|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
20928|Yeldham Granite|39925|6|Mentioned|p334|||See also Fig.9.||||||
20928|Yeldham Granite|39943|6|Mentioned|Table 1A|||||||||
20928|Yeldham Granite|39944|3|Fully described|p229|||||||||
20928|Yeldham Granite|40840|6|Mentioned|Map legend|||||||||
20928|Yeldham Granite|41465|6|Mentioned|p8|||||||||
20928|Yeldham Granite|41979|4|Described|p517|||||||||
20928|Yeldham Granite|42565|5|Briefly described|Table 2 P7|||||||||
20928|Yeldham Granite|45166|5|Briefly described|p17|||||||||
20928|Yeldham Granite|47083|5|Briefly described|p20|||Previously mapped as part of the Weberra Granite.||||||
20928|Yeldham Granite|49041|5|Briefly described|Table 1|||Mention Table 4.||||||20-DEC-06
20928|Yeldham Granite|50536|5|Briefly described|p1.5, 11.3, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Yeldham Suite. Age: ~1820Ma. Overlain by  McNamara Group.||||||07-NOV-08
20928|Yeldham Granite|50624|5|Briefly described|p234 Fig.2||Paleoproterozoic|||||||07-NOV-08
20928|Yeldham Granite|61929|5|Briefly described|p128 Fig. 2|||||||||
20928|Yeldham Granite|61936|6|Mentioned|p193|Paleoproterozoic|Paleoproterozoic|Age: ~1820Ma. Geological Province: Lawn Hill Platform, Western Fold Belt, Mount Isa Inlier.||||||07-NOV-08
20928|Yeldham Granite|63109|6|Mentioned|p1109|||Low density granite.||||||30-SEP-08
20928|Yeldham Granite|63866|5|Briefly described|p57|Statherian|Statherian|Lawn Hill Platform, Leichhardt Superbasin. Crops out in the Kamarga Dome. A zircon U-Pb TIMS age of c. 1820 Ma is derived from Wyborn et al., 1988.|1796 +/- 3 Ma (xenotime TIMS)|||Intrudes the Kamarga Volcanics.||
20928|Yeldham Granite|64250|6|Mentioned|p17 fig 7, p11 fig 3, p21|||Western Fold Belt, Mount Isa Inlier. Preceded the accumulation of the Leichhardt Superbasin (c.1800-1750 Ma).|~1820 Ma|||||
20928|Yeldham Granite|64575|6|Mentioned|p656|||Age: 1820Ma.||||||
20928|Yeldham Granite|65337|6|Mentioned|p6 Fig.3.|||||||||
20928|Yeldham Granite|65396|5|Briefly described|p82, p175, p192, p195, p241|Orosirian|Orosirian|Lawn Hill Platform. Its emplacement preceded the accumulation of the Leichhardt Superbasin. Formations with detrital zircons from this unit are listed.|1820 Ma|||||
20928|Yeldham Granite|67323|5|Briefly described|GIS attrib tbl, p6, p10, p23, p30, p107|Paleoproterozoic|Paleoproterozoic|See also Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Century Domain, Mount Isa Inlier. Lawn Hill region. Post-Barramundi Orogeny. Intrusions 1820-1800 Ma.Yeldham Igneous Event (intraplate magmatism). TIMS xenotime age ~1793 Ma. 1796+/-3 Ma (Wyborn et al 1988, Neumann & Fraser, 2007). U-Pb TIMS age ~1820 Ma (2001).|1796 +/- 3 Ma.|||intrudes Kamarga Volcanics. Age correlation with Big Toby and Monaghans Granites. Underlies McNamara Group.|Medium-grained muscovite leucogranite; pegmatite dykes and minor greisen|
20928|Yeldham Granite|68542|6|Mentioned|p1 |||||||||
20928|Yeldham Granite|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province.||||||
20928|Yeldham Granite|68576|6|Mentioned|Q_2: p1|Paleoproterozoic|Paleoproterozoic|Mount Isa area.||||||
20928|Yeldham Granite|69222|6|Mentioned|p222 Fig.2|||Associated with 1890-1840 Ma Barramundi Orogeny.||||||
20928|Yeldham Granite|69591|5|Briefly described|p28, p30, p32, p40, p42, p60, p105|Paleoproterozoic|Paleoproterozoic|Century Domain, Mount Isa Province. An age of ~1790 Ma (Hutton, 1983) is also given.|1796 +/- 3 Ma (Wyborn et al., 1988).|||Intrudes Kamarga Volcanics. Is overlain nonconformably by Torpedo Creek Quartzite (Gun Supersequence).|Medium-grained muscovite leucogranite; pegmatite dykes and minor greisen.|
20928|Yeldham Granite|71592|5|Briefly described|Appendix A.|||Century Domain, Mount Isa Orogen.|1796+/-3 Ma (crystallisation: xenotime U-Pb TIMS).||||Granite.|
20928|Yeldham Granite|72526|5|Briefly described|p6 Fig.1.2,|Paleoproterozoic|Paleoproterozoic|Shown with South Nicholson Granite Complex.||||||
20928|Yeldham Granite|72889|6|Mentioned|p6 Fig.i.|||||||||
20928|Yeldham Granite|73413|6|Mentioned|p3|||Mount Isa Inlier, Western Fold Belt, Lawn Hill Platform.||||||
20928|Yeldham Granite|73553|6|Mentioned|p259|Statherian|Statherian|Kamarga Dome.|1796+/-3 Ma (Wyborn et al., 1988)|||||
20978|Yeuralba Granite|9538|5|Briefly described|Map legend|Proterozoic|Proterozoic|Medium to coarse-grained pink equigranular biotite muscovite leucogranite, +/- tourmaline.||||||28-OCT-04
20978|Yeuralba Granite|23216|5|Briefly described|Table1p9,12,14,18|||||||||
20978|Yeuralba Granite|23733|5|Briefly described|p32 Fig. 19|||Of Edith River Group.||||||
20978|Yeuralba 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
20978|Yeuralba Granite|31435|6|Mentioned|p61|||||||||
20978|Yeuralba Granite|32660|5|Briefly described|Table 2|||||||||
20978|Yeuralba Granite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20978|Yeuralba Granite|40489|6|Mentioned|p89|||||||||
20978|Yeuralba Granite|41294|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
20978|Yeuralba Granite|41295|4|Described|p15|||||||||
20978|Yeuralba Granite|41406|6|Mentioned|Map legend|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
20978|Yeuralba Granite|43149|5|Briefly described|Map Legend||Paleoproterozoic|Of Orosirian age.||||||07-NOV-08
20978|Yeuralba Granite|44201|14|Not recorded|p.10|||Adamellite.||||||
20978|Yeuralba Granite|45022|3|Fully described|p.135.||Carpentarian|On many pages.||||||21-DEC-06
20978|Yeuralba Granite|46679|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
20978|Yeuralba 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
20978|Yeuralba Granite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1820-1850Ma. I-type. Medium to coarse biotite muscovite leucogranite, tourmaline, with muscovite or tourmaline greisen alteration near margins. Intrudes Tollis Formation.||||||07-JAN-09
20978|Yeuralba Granite|67564|6|Mentioned|p85.|Paleoproterozoic|Paleoproterozoic|Eastern Pine Creek Orogen.||Unit in David Suite.||||
20978|Yeuralba Granite|69420|5|Briefly described|p5:14, 18, 21, 23, 105, 109-110|Paleoproterozoic|Paleoproterozoic|Has contact metamorphosed the Maud Dolerite and Tollis Formation in an area ~15km E of Katherine. Mineralogy and petrology/geochemistry summarised. Associated with the Tollis Formation-hosted Sn deposit in the Maranboy tinfield, and is associated with the Yenberrie and Yeuralba W, Mo, Bi, Sn deposits.||Jim Jim Suite.||Intrudes Tollis Formation.|Coarse-grained equigranular leucogranite.|12-JUL-16
21009|Yiyintyi Sandstone|22538|6|Mentioned|P714||Statherian|||||||
21009|Yiyintyi Sandstone|22644|5|Briefly described|5|||Geological province: McArthur Basin. Overlain by Seigal Volcanics; underlain by Scrutton Volcanics. MIsspelt as Yiyinti in Figure2 (p5).||||||21-DEC-06
21009|Yiyintyi Sandstone|22670|6|Mentioned|52|||Geological province: McArthur Basin.||||||21-DEC-06
21009|Yiyintyi Sandstone|22853|3|Fully described|5|Proterozoic|Proterozoic|Geological province: McArthur Basin. Of the Tawallah Group.||||||29-NOV-06
21009|Yiyintyi Sandstone|23374|6|Mentioned|p41||Statherian|Equivalent to Mamadawerre Sandstone. Of the Tallawah Group. In the McArthur Basin.||||||21-DEC-06
21009|Yiyintyi Sandstone|23395|5|Briefly described|p395|||||||||
21009|Yiyintyi Sandstone|23396|5|Briefly described|p407 Fig.2|||Of the Tawallah Group.||||||21-DEC-06
21009|Yiyintyi Sandstone|23398|5|Briefly described|p434|||||||||29-FEB-08
21009|Yiyintyi Sandstone|23733|5|Briefly described|p32 Fig. 19|||See also p44 Appendix 1.  Of the Tawallah Group.  Geological Province: McArthur Basin.||||||
21009|Yiyintyi Sandstone|23776|5|Briefly described|p705 Fig 2.|||Of Tawallah Group.||||||
21009|Yiyintyi Sandstone|23809|5|Briefly described|p28|||Of the Tawallah Group.  Geological Province: McArthur Basin.||||||
21009|Yiyintyi Sandstone|23867|5|Briefly described|Fig. 30|||Of Tawallah Group. Correlates with part of Mamadewerre Sandstone of the Kombolgie Subgroup (Katherine River Group).||||||
21009|Yiyintyi Sandstone|23910|5|Briefly described|p292 Fig. 3|||Of Tawallah Group.  Geological Province: McArthur Basin.||||||
21009|Yiyintyi Sandstone|23963|5|Briefly described|p1239 Fig.2|||Geological Province: McArthur Basin. Of the Tawallah Group.||||||
21009|Yiyintyi Sandstone|24047|5|Briefly described|p55|||Quartz arenite.  Unconformably overlain by Walker River Formation.||||||
21009|Yiyintyi Sandstone|24432|5|Briefly described|p562 FIg.2|||Of Lower Katherine River Group (wrong). Geological Province: McArthur Basin.||||||29-FEB-08
21009|Yiyintyi Sandstone|32660|5|Briefly described|Table 4|||||||||
21009|Yiyintyi Sandstone|37568|5|Briefly described|p78|||||||||
21009|Yiyintyi Sandstone|40691|6|Mentioned|p9|||||||||
21009|Yiyintyi Sandstone|42385|3|Fully described|p5, p8 Fig. 5, p9 Tb. 3|Mesoproterozoic|Mesoproterozoic|Basal unit of Tawallah Group. Unconformable on Scrutton Volcanics in east.  Max. thickness: >3000m. Quartz sst, in places feldspathic, mainly medium-bedded and medium- to coarse-grained, moderately to porrly sorted with scattered quartz pebble interbeds||||||18-SEP-07
21009|Yiyintyi Sandstone|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
21009|Yiyintyi Sandstone|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.||Of Tawallah Group.||In schematic section, underlies Seigal Volcanics.|Quartz sandstone. Detailed lithology given.|09-NOV-11
21009|Yiyintyi Sandstone|42639|3|Fully described|p8, Table 4 p11|||||||||
21009|Yiyintyi Sandstone|42700|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
21009|Yiyintyi Sandstone|42739|5|Briefly described|map legend|Statherian|Statherian|Of the Tawallah Group. Arenite, litharenite.||||||19-OCT-05
21009|Yiyintyi Sandstone|42812|3|Fully described|p10, Table 3|||Of the of Tawallah Group.||||||21-DEC-06
21009|Yiyintyi Sandstone|43010|5|Briefly described|Fig.6||Mesoproterozoic|Of Tawallah Group. Of "Mid Proterozoic" age.||||||29-NOV-06
21009|Yiyintyi Sandstone|43036|3|Fully described|p13|||Of the Tawallah Group.||||||21-DEC-06
21009|Yiyintyi Sandstone|44287|14|Not recorded|p.8, opp.7|||Unit of Tawallah Group. (E53-3).||||||21-DEC-06
21009|Yiyintyi Sandstone|44288|14|Not recorded|map legend||Paleoproterozoic|Quartz sandstone minor pebble to boulder conglomerate. Lower Proterozoic.||||||07-NOV-08
21009|Yiyintyi Sandstone|44305|14|Not recorded|p.11|||(E53-8).||||||
21009|Yiyintyi Sandstone|44530|14|Not recorded|p.4,8, opp.8|||(D53-15).||||||
21009|Yiyintyi Sandstone|44531|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
21009|Yiyintyi Sandstone|49001|6|Mentioned|p5|||||||||
21009|Yiyintyi Sandstone|60483|5|Briefly described|p7 Fig. 5, p27|||Of the Tawallah Group(lower part). Geological Province: McArthur Basin.||||||
21009|Yiyintyi Sandstone|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Tawallah Group. Overlain by Seigal Volcanics.||||||03-JUN-09
21009|Yiyintyi Sandstone|62084|6|Mentioned|p936 Fig.5|||Leichhardt Superbasin. Shown as Yiyintyi Sst.||||||
21009|Yiyintyi Sandstone|63112|6|Mentioned|p1189-1192, p1194, p1205|||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. Mis-spelt twice as Yiyinti on p1192. Age approximated from Fig.2. >3500 m thick.|c.1795-1785 Ma.||||Lower part is proximal fluvial facies: poorly sorted and immature, coarse- to fine-grained. Upper part is medium- to fine-grained, better sorted, locally more mature near-shore facies association.|
21009|Yiyintyi Sandstone|63866|5|Briefly described|p54|||||||Overlain by the Seigal Volcanics. (Possibly) equivalent to the Guide Supersequence.||
21009|Yiyintyi Sandstone|64815|6|Mentioned|p4 Fig.2, p5 Fig.3, p12   |||||Of the Tawallah Group.||||
21009|Yiyintyi Sandstone|64817|6|Mentioned|p353 Fig.4, p355 Fig.5, p367 Tb.2, p370 |||||Of the Tawallah Group.||Shown as equivalent to Westmoreland Conglomerate.||06-JUN-18
21009|Yiyintyi Sandstone|65228|5|Briefly described|p7, Figs.02, 05, 07. |||McArthur Basin.||Basal unit in Tawallah Group.||Is overlain by Seigal Volcanics. Equivalent to Westmoreland Conglomerate.||
21009|Yiyintyi Sandstone|65337|6|Mentioned|pp12-13. |||Southern McArthur Basin. Correlative of Don Creek Sandstone.||||||
21009|Yiyintyi Sandstone|65340|6|Mentioned|p12 Fig.6. |||||Basal unit in Tawallah Group.||Is overlain by Seigal Volcanics.||23-MAR-18
21009|Yiyintyi Sandstone|67352|6|Mentioned|p15 Tb.2|||||||Is overlain conformably by Seigal Volcanics.||
21009|Yiyintyi Sandstone|69429|5|Briefly described|p14:3|||Basal unit of the McArthur Basin succession.||Tawallah Group.||Unconformably overlies Scrutton Volcanics.||12-JUL-16
21009|Yiyintyi Sandstone|69430|4|Described|p15:3, 10, 12|||Southern McArthur Basin. Up to 4000m thick. Fluvial to alluvial fan deposits near base; shallow-marine above.||Tawallah Group.||Unconformably overlies Scrutton Volcanics. Is overlain by Seigal Volcanics: the contact is stated as "conformable" and "sharp unconformable".|Predominantly a medium to thickly bedded quartzarenite, sublitharenite and litharenite.|12-JUL-16
21009|Yiyintyi Sandstone|69433|6|Mentioned|p18:5|||Southern McArthur Basin.||||Correlated with Don Creek Sandstone (Lawn Hill Platform).||12-JUL-16
21009|Yiyintyi Sandstone|69455|5|Briefly described|p39:11|||Manganese mineralisation in the Rosie Creek South prospect is hosted in basal claystone and conglomerate of the overlying Walker River Formation, at the unconformity with this unit.||||Is overlain unconformably by Walker River Formation.||12-JUL-16
21009|Yiyintyi Sandstone|69673|6|Mentioned|p16 fig 13, p17 fig 14|||Coarse clastic sedimentary rock.||Tawallah Group||Overlain by Seigal Volcanics||
21009|Yiyintyi Sandstone|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.||Lower Tawallah Group.||||
21009|Yiyintyi Sandstone|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Urapunga Fault Zone, Beetaloo Sub-basin, Batten Fault Zone and Southeastern McArthur Basin.||Tawallah Group||Shown as unconformably overlying Scrutton Volcanics and underlies Seigal Volcanics||
21009|Yiyintyi Sandstone|72718|6|Mentioned|p7|||Southern McArthur Basin.||Tawallah Group||Overlain by Seigal Volcanics. Equivalent to Westmoreland Conglomerate.||
21009|Yiyintyi Sandstone|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Beetaloo Sub-basin and the Batten Fault Zone in the Southern McArthur Basin.||Tawallah Group||Unconformably overlies Scrutton Volcanics and underlies Seigal Volcanics and is equivalent to Westmoreland Conglomerate.||
21009|Yiyintyi Sandstone|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin, Leichhardt Superbasin.||Tawallah Group||Overlain by Seigal Volcanics. Unconformably underlain(?) by Scrutton Volcanics.||
21009|Yiyintyi Sandstone|73412|5|Briefly described|p4, 8, 14|||Southern McArthur Basin. See also mis-spelt Yiyinti Sandstone (p2, 12).||Tawallah Group.||Lateral equivalent to Westmoreland Conglomerate.||
21071|Zamia Creek Siltstone|22538|6|Mentioned|Fig3 P708|||||||||
21071|Zamia Creek Siltstone|22600|4|Described|Map legend|Statherian|Statherian|||||||
21071|Zamia Creek Siltstone|23937|5|Briefly described|p13|||Of the Balma Group.  Correlates with parts of the Nagi Formation.  Geological Province: McArthur Basin.||||||03-NOV-04
21071|Zamia Creek Siltstone|24048|3|Fully described|p58|Mesoproterozoic|Paleoproterozoic|Of the Balma Group.  Overlain by Yarrawirrie Formation; underlain by Conway Formation.  Max. thickness: 300m.  Geological Province: McArthur Basin.||||||07-NOV-08
21071|Zamia Creek Siltstone|24049|5|Briefly described|Map Legend|Statherian|Statherian|Of Balma Group. Mudstone: grey, laminated, commonly dolomitic; dolostone: brown to grey, microbial laminations, fenestral fabrics, leached or silicified most outcrops; minor sandstone; cauliflower chert nodules. Geol. Prov: McArthur Basin.||||||13-OCT-05
21071|Zamia Creek Siltstone|32660|5|Briefly described|Table 4|||||||||
21071|Zamia Creek Siltstone|42597|5|Briefly described|Map Legend|Carpentarian||||||||
21071|Zamia Creek Siltstone|43010|2|Defined|p116||Paleoproterozoic|Of the McArthur Group. Of Statherian age.||||||07-NOV-08
21071|Zamia Creek Siltstone|44112|6|Mentioned|p30,58|||||||||
21071|Zamia Creek Siltstone|44299|4|Described|p.12|||SD/53-7,8. Lower?Proterozoic. Table 1.||||||
21071|Zamia Creek Siltstone|44300|14|Not recorded|map legend|||SD/53-7,8. Lower (?) Proterozoic.||||||
21071|Zamia Creek Siltstone|45162|6|Mentioned|p45|||||||||
21071|Zamia Creek Siltstone|61403|5|Briefly described|Map Legend|Statherian|Statherian|Of Balma Group. Mudstone: grey, laminated, commonly dolomitic; dolostone: brown to grey, microbial laminations, fenestral fabrics, leached or silicifi ed most outcrops; minor sandstone; cauliflower chert nodules. Geol. Prov: McArthur Basin.||||||
21071|Zamia Creek Siltstone|64817|6|Mentioned|p353 Fig.4 |||||Of the Balma Group.||||
21071|Zamia Creek Siltstone|67323|6|Mentioned|Eastern Australia Time-Space Plot|||McArthur region.||||||
21071|Zamia Creek Siltstone|69430|4|Described|p15:3, 21-22|Statherian|Statherian|Walker Fault Zone, northern McArthur Basin. Recessive unit. Up to c.300m thick. Subtidal to very shallow evaporitic sediments. Had been correlated (Haines, 1994) with Umbolooga Subgroup; geochronological data suggest possible correlation with upper Lynott and Talco Formations instead (Haines et al., 1999).||Balma Group.||Overlies Conway Formation probably conformably. Is overlain unconformably by Ngilipitji Conglomerate Member (Yarrawirrie Formation).|Grey, laminated, commonly dolomitic mudstone; brown to grey dolostone with microbial laminations, often leached and silicified; minor sandstone; cauliflower chert nodules.|12-JUL-16
21071|Zamia Creek Siltstone|69673|6|Mentioned|p16 fig 13|Mesoproterozoic|Paleoproterozoic|Walker Fault Zone||Balma Group||Overlain by Yarrawirrie Formation, Overlies Conway Formation||
21071|Zamia Creek Siltstone|71374|5|Briefly described|p12|Statherian|Statherian|May correlate with the Yarawoi Formation (Habgood Group).||Balma Group||||
21071|Zamia Creek Siltstone|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.||Middle Balma Group.||||
21089|Zimmermann Sandstone|32648|6|Mentioned|p32|||L.Carb.||||||
21089|Zimmermann Sandstone|32699|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Quartz sandstone and siltstone.||||||02-DEC-04
21089|Zimmermann Sandstone|34085|6|Mentioned|Cor.chart|||Tourn. - Visean||||||
21089|Zimmermann Sandstone|36473|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
21089|Zimmermann Sandstone|36890|3|Fully described|p380|||||||||
21089|Zimmermann Sandstone|39827|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
21089|Zimmermann Sandstone|42547|4|Described|p101|||||||||
21089|Zimmermann Sandstone|44994|6|Mentioned|Fig.6|||Correlation. See also p14.||||||21-DEC-06
21089|Zimmermann Sandstone|45038|2|Defined|p.86||Early Carboniferous|See also Figures and Plates. L.Carb.||||||21-DEC-06
21089|Zimmermann Sandstone|45039|6|Mentioned|p27|||Lower Carboniferous. See also p33.||||||21-DEC-06
21089|Zimmermann Sandstone|45063|6|Mentioned|p8|||See also p19 and Fig. 3. L.Carb.||||||21-DEC-06
21089|Zimmermann Sandstone|60364|4|Described|p184|Visean|Tournaisian|Of Langfield Group. Disconformably overlies Septimus Limestone. Disconformably overlain by Border Creek Formation. Quartz sandstone. Thickness in type section: 140m. Contains fossils. Ostracods described. Geological Province: Bonaparte Basin.||||||11-MAY-05
21089|Zimmermann Sandstone|61542|5|Briefly described|p277 Fig. 2|Tournaisian|Tournaisian|Of the Langfield Group. Geological Province: onshore Bonapart Basin/Petrel-Sub-basin.||||||07-FEB-11
21089|Zimmermann Sandstone|64694|5|Briefly described|p233, p234 Fig.2, p254 Fig.12|Tournaisian|Tournaisian|Burt Range Shelf, Onshore Bonaparte Basin.||Unit in Langfield Group.||Disconformably overlies the Septimus Limestone.||
21089|Zimmermann Sandstone|69452|3|Fully described|p36:12 Fig.36.12|Tournaisian|Tournaisian|Veevers and Roberts (1968). Petrel Sub-basin, Bonaparte Basin. The type section is at Mount Zimmermann, central Burt Range in WA, where it is 133m thick. Rapidly thins away from this area. Less than 30m thick in NT. Also crops out in Keep River National Park (NT). Shoreface and shallow-marine deposits. Uncommon marine fossils include brachiopods, bivalves, bryozoans, crinoids and trace fossils (Rhizocorallium). Onshore. See also references to [mis-spelt] Zimmerman Sandstone (36:6 Fig.36.5; 36:9, 12-14).||Langfield Group.||Conformably overlies Septimus Limestone. Is overlain by Keep Inlet and Border Creek Formations unconformably or disconformably.|Brown to white quartz sandstone with interbedded white siltstone in the upper part. NT exposures are friable, medium-grained, slightly calcareous sandstone; some beds almost entirely quartzose; others contain quartz, feldspar and lithic grains.|12-JUL-16
21089|Zimmermann Sandstone|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Langfield Group.|||Quartzose, feldspathic and lithic sandstone, minor siltstone and shale|
